{"meta":{"query_hash":"a30340bfc18c","filters":{"venue":"Tellus B"},"cohort_total":56,"direct_labels_cover":0,"predictions_cover":56,"exported":56,"export_cap":100000,"truncated":false,"label_status":"direct model label, unvalidated","prediction_status":"machine_predicted_unvalidated (Codex and Gemma teacher distillation)","score_status":"score_only:v0-immature-baseline","snapshot":{"source":"OpenAlex, pinned release, all 482 partitions","release":"2026-06-24","frame_built":"2026-07-12"},"permalink":"https://metacan.xera.ac/q/a30340bfc18c","api":"https://metacan.xera.ac/api/v1/cohort?venue=Tellus+B"},"results":[{"id":"W1968644285","doi":"10.1111/j.1600-0889.2006.00206.x","title":"Estimating regional carbon exchange in New England and Quebec by combining atmospheric, ground-based and satellite data","year":2006,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":86,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Waterloo","funders":"University of Wyoming; National Aeronautics and Space Administration; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Eddy covariance; Environmental science; Biosphere; Flux (metallurgy); Atmospheric model; Vegetation (pathology); Climatology; Atmospheric sciences; Meteorology; Geography; Geology; Ecosystem","score_opus":0.011909184637266345,"score_gpt":0.20492284434088767,"score_spread":0.19301365970362133,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1968644285","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99271387,0.0012220447,0.004535091,0.00017831371,0.000038447204,0.00013573836,0.0000027577512,0.000028302453,0.0011454218],"genre_scores_gemma":[0.9278344,0.00011499677,0.06915906,0.0002528214,0.00006582738,0.0000038792787,0.00009298701,0.000028740513,0.0024472831],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9989211,0.000034546505,0.00018210085,0.00042236055,0.00018543986,0.00025446498],"domain_scores_gemma":[0.9995097,0.000058968617,0.000067480236,0.0002684404,6.31458e-7,0.000094795745],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017163811,0.00016701248,0.00014854634,0.0000019922256,0.0000711047,0.000038155682,0.00016605154,0.00006864617,0.00008880458],"category_scores_gemma":[0.000007133893,0.0001674792,0.000009595747,0.00009999142,0.00023612347,0.00013859509,0.00029363207,0.000108115055,0.0000058189635],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000037655194,0.00008558042,0.839621,0.000021260068,0.000005008086,0.000021750026,0.00047635759,0.01912976,0.0007798236,0.000017191376,0.00070605247,0.13909854],"study_design_scores_gemma":[0.0014858772,0.000058330505,0.34391996,0.000028554912,0.000014014039,0.000016938897,0.00007283279,0.63434875,0.000010400779,0.00023918331,0.019491008,0.0003141534],"about_ca_topic_score_codex":0.107283,"about_ca_topic_score_gemma":0.016452102,"teacher_disagreement_score":0.615219,"about_ca_system_score_codex":0.00013294657,"about_ca_system_score_gemma":0.000011210458,"threshold_uncertainty_score":0.9180659},"labels":[],"label_agreement":null},{"id":"W1976587455","doi":"10.1111/j.1600-0889.2011.00571.x","title":"Sea ice contribution to the air–sea CO<sub>2</sub> exchange in the Arctic and Southern Oceans","year":2011,"lang":"en","type":"article","venue":"Tellus B","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":187,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"Danish Agency for Science and Higher Education; Natural Environment Research Council; Fonds De La Recherche Scientifique - FNRS; Canada Excellence Research Chairs, Government of Canada; Belgian Federal Science Policy Office; Forsknings- og Innovationsstyrelsen; Sight Research UK","keywords":"Oceanography; Environmental science; Sea ice; The arctic; Climatology; Arctic; Arctic ice pack; Atmospheric sciences; Geology","score_opus":0.014839469338721416,"score_gpt":0.19633063948859117,"score_spread":0.18149117014986976,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1976587455","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99097705,0.00052115484,0.000613045,0.0019983205,0.00021992179,0.00055027736,0.00028654435,0.000042740914,0.004790962],"genre_scores_gemma":[0.99658847,0.0002642078,0.00007357625,0.0025751085,0.00018385996,0.000005115485,0.00011898065,0.000007650009,0.00018306126],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99840224,0.00022406282,0.00023345482,0.00029833597,0.00034162708,0.00050026353],"domain_scores_gemma":[0.9990701,0.0003313534,0.00008415413,0.00032696506,0.00005470334,0.00013272562],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010545576,0.00020072292,0.00019186022,0.000064996944,0.00036587706,0.000051060793,0.00041009395,0.00009353656,0.00058446574],"category_scores_gemma":[0.0001128503,0.000118093514,0.000057660884,0.00028194647,0.00019349073,0.00013058075,0.000034241442,0.00026494937,0.0008437986],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000435874,0.0001519223,0.87993073,0.00010974884,0.00008421052,0.00013270424,0.05522986,0.00035076423,0.000119436205,0.0014960903,0.003179642,0.058778986],"study_design_scores_gemma":[0.0009959604,0.0005315854,0.93345827,0.000082324856,0.00012296552,0.00016663843,0.005130041,0.017010117,0.00009123428,0.0025586246,0.039249185,0.0006030684],"about_ca_topic_score_codex":0.0024293463,"about_ca_topic_score_gemma":0.011321547,"teacher_disagreement_score":0.058175918,"about_ca_system_score_codex":0.000014061785,"about_ca_system_score_gemma":0.00004394675,"threshold_uncertainty_score":0.99993414},"labels":[],"label_agreement":null},{"id":"W1979559284","doi":"10.3402/tellusb.v53i5.16644","title":"Analysis of regional budgets of sulfur species modeled for the COSAM exercise","year":2001,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University; Environment and Climate Change Canada","funders":"","keywords":"Sulfate; Sulfur; Sulfate aerosol; Deposition (geology); Aerosol; Northern Hemisphere; Sulfur cycle; Environmental science; Atmospheric sciences; Climate model; Climatology; Sulfur dioxide; Meteorology; Chemistry; Climate change; Geology; Structural basin; Geography; Inorganic chemistry","score_opus":0.03185395199346922,"score_gpt":0.22704572292860103,"score_spread":0.19519177093513182,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1979559284","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99099493,0.0010031912,0.0023084553,0.00017466367,0.00003758262,0.0001174353,0.00009572241,0.000009534095,0.0052584824],"genre_scores_gemma":[0.99579364,0.0003753253,0.00046682384,0.000030837633,0.000039427377,0.0000010389252,0.00007721846,0.0000012643499,0.0032144072],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99945533,0.0000069826438,0.00017033414,0.000106860054,0.00014168517,0.000118792166],"domain_scores_gemma":[0.9993956,0.0002596966,0.00009588065,0.00017171868,0.000044419183,0.00003266437],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00011405651,0.00006610729,0.0002021977,0.0000068658615,0.00006010172,0.0000061432784,0.00017883313,0.000031393403,0.002339471],"category_scores_gemma":[0.000017810024,0.00004231487,0.00014549436,0.00034707287,0.00011872589,0.00003605702,0.000005574694,0.000032255306,0.0000043683362],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00100374,0.00014544382,0.56557447,0.00011617795,0.0012261298,0.000009318798,0.0013528797,0.37179494,0.006608308,0.00024123324,0.0070410753,0.04488627],"study_design_scores_gemma":[0.0008109643,0.00013622383,0.5869166,0.00004347505,0.001628022,0.000007641322,0.0012215945,0.36648998,0.021659829,0.00082828855,0.019911386,0.0003459874],"about_ca_topic_score_codex":0.00043547762,"about_ca_topic_score_gemma":0.00028212025,"teacher_disagreement_score":0.044540282,"about_ca_system_score_codex":0.0000012743632,"about_ca_system_score_gemma":0.000021315775,"threshold_uncertainty_score":0.9985725},"labels":[],"label_agreement":null},{"id":"W1990357183","doi":"10.3402/tellusb.v57i3.16542","title":"Vegetation–soil water interaction within a dynamical ecosystem model of grassland in semi-arid areas","year":2005,"lang":"en","type":"article","venue":"Tellus B","topic":"Ecosystem dynamics and resilience","field":"Environmental Science","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Science Foundation of Inner Mongolia; Mitacs","keywords":"Grassland; Environmental science; Arid; Biomass (ecology); Vegetation (pathology); Ecosystem; Precipitation; Alternative stable state; Hydrology (agriculture); Water content; Ecology; Geography; Geology","score_opus":0.006304999275357897,"score_gpt":0.2063532791686761,"score_spread":0.2000482798933182,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1990357183","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9909324,0.000014228711,0.0028642376,0.000100487734,0.000091155656,0.00014422256,0.0000049095693,0.000017948018,0.0058304034],"genre_scores_gemma":[0.9992661,0.0000073090832,0.00032536153,0.000017957987,0.000016728218,0.0000108043605,0.000007901898,0.000009945502,0.00033790205],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9989934,0.00003835335,0.00034791345,0.00022750394,0.00020423446,0.00018860806],"domain_scores_gemma":[0.9996608,0.00002155453,0.00008339806,0.00017311373,0.0000071011023,0.000054045362],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025444155,0.0001035389,0.00015296314,0.00005145358,0.000036553054,0.000014434549,0.000152769,0.0000668006,0.000096728494],"category_scores_gemma":[0.000008332742,0.00007415716,0.00003970631,0.00008775025,0.000037658483,0.00019368884,0.000077885175,0.00011549656,0.0002333746],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016167323,0.00007482162,0.016972551,0.000032631167,0.0000036637357,0.0000025401662,0.0010043093,0.9558262,0.025359005,0.00009910011,0.000015326154,0.0005936844],"study_design_scores_gemma":[0.00021314289,0.000021250224,0.0037323409,0.00006045642,0.0000047562494,0.000013160774,0.00006615487,0.9893756,0.0061315116,0.00023855997,0.000038784357,0.000104297775],"about_ca_topic_score_codex":0.000295703,"about_ca_topic_score_gemma":0.015613538,"teacher_disagreement_score":0.033549383,"about_ca_system_score_codex":0.00024490696,"about_ca_system_score_gemma":0.000008132048,"threshold_uncertainty_score":0.8712721},"labels":[],"label_agreement":null},{"id":"W1991867732","doi":"10.3402/tellusb.v66.22486","title":"Carbon monitoring system flux estimation and attribution: impact of ACOS-GOSAT XCO<sub>2</sub> sampling on the inference of terrestrial biospheric sources and sinks","year":2014,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":147,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; University of Toronto","funders":"Japan Aerospace Exploration Agency; Goddard Space Flight Center; Ministry of Education, India; National Aeronautics and Space Administration; California Institute of Technology; Jet Propulsion Laboratory","keywords":"Environmental science; Flux (metallurgy); Greenhouse gas; Sampling (signal processing); Atmospheric sciences; Satellite; Carbon cycle; Monte Carlo method; Climatology; Meteorology; Statistics; Physics; Mathematics; Detector","score_opus":0.014630268747574891,"score_gpt":0.2293676057070911,"score_spread":0.21473733695951622,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1991867732","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.987927,0.00012479376,0.011236278,0.000020667481,0.00011321375,0.00023027013,0.000004447524,0.000029424917,0.00031389724],"genre_scores_gemma":[0.9982153,0.00006912036,0.001608255,0.000004645776,0.000059396105,0.0000070122233,0.000004087418,0.00001570503,0.000016458544],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987828,0.00008175146,0.00031193605,0.0002729162,0.00031704333,0.00023354827],"domain_scores_gemma":[0.99918514,0.00021459439,0.00024841088,0.00025867912,0.000004187004,0.000088987596],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000329175,0.00020868055,0.00026206384,0.0000074996865,0.0001393542,0.000028510383,0.00015865677,0.000113403905,0.000024560206],"category_scores_gemma":[0.000057327292,0.00015062702,0.000057702164,0.00015055979,0.00037489604,0.000104132,0.00018368177,0.0001230827,0.000007182617],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014354427,0.00009390136,0.34577388,0.00008311565,0.00005537408,0.0000015050937,0.0009520382,0.3184605,0.25771284,0.00019306643,0.000007907028,0.07652235],"study_design_scores_gemma":[0.0005970142,0.00051344594,0.5008775,0.00019967882,0.00006864397,0.000010979701,0.00023414765,0.48045668,0.016581632,0.00013577723,0.000040476858,0.00028398834],"about_ca_topic_score_codex":0.00037006167,"about_ca_topic_score_gemma":0.0000070538185,"teacher_disagreement_score":0.2411312,"about_ca_system_score_codex":0.00023259305,"about_ca_system_score_gemma":0.00000859069,"threshold_uncertainty_score":0.61423916},"labels":[],"label_agreement":null},{"id":"W1996709788","doi":"10.3402/tellusb.v64i0.11596","title":"How does the atmospheric variability drive the aerosol residence time in the Arctic region?","year":2012,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"ASTER","funders":"Cornell Center for Materials Research; European Commission; National Park Service; National Oceanic and Atmospheric Administration; Centre National de la Recherche Scientifique; U.S. Department of Energy","keywords":"Aerosol; Environmental science; Mineral dust; Atmospheric sciences; Arctic; Haze; Atmosphere (unit); Residence time (fluid dynamics); The arctic; Climatology; Sulfate; Meteorology; Geology; Chemistry; Geography; Oceanography","score_opus":0.011633450669890907,"score_gpt":0.19782491770738064,"score_spread":0.18619146703748973,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1996709788","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9783183,0.0006232364,0.000121613826,0.012701174,0.00024888752,0.00044091252,0.0000062626045,0.000038813123,0.007500834],"genre_scores_gemma":[0.9953881,0.000045469442,0.00017874561,0.0008252095,0.0003735974,0.000007871371,0.000006704991,0.000003357766,0.003170946],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99847764,0.000401554,0.00016458375,0.00022235955,0.00029657007,0.00043730484],"domain_scores_gemma":[0.9975528,0.0015777396,0.00009737759,0.0006835478,0.00002192311,0.000066595625],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012006126,0.00016030921,0.00013353562,5.877738e-7,0.0004028206,0.00014432974,0.0008003823,0.00006912515,0.0011987368],"category_scores_gemma":[0.00032955248,0.00005775984,0.00006985505,0.00034247464,0.00041351654,0.0002603003,0.000031258533,0.0003421718,0.00021004584],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000054726617,0.000069585185,0.97967136,0.000035392663,0.0000237423,0.000018957282,0.0066152904,0.0005906341,0.00032778567,0.00017490024,0.0038443867,0.008573239],"study_design_scores_gemma":[0.00026721714,0.000066584515,0.97432953,0.00005220947,0.00006010051,0.00016568275,0.005178741,0.0041962555,0.0008614881,0.0038999983,0.010496679,0.000425489],"about_ca_topic_score_codex":0.00083515386,"about_ca_topic_score_gemma":0.0002712488,"teacher_disagreement_score":0.017069831,"about_ca_system_score_codex":0.0000091375205,"about_ca_system_score_gemma":0.00003596323,"threshold_uncertainty_score":0.9997143},"labels":[],"label_agreement":null},{"id":"W1997868900","doi":"10.3402/tellusb.v52i2.16118","title":"Observations of the evolution of the aerosol, cloud and boundary-layer characteristics during the 1st ACE-2 Lagrangian experiment","year":2000,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Natural Environment Research Council; Astex Pharmaceuticals","keywords":"Aerosol; Cloud condensation nuclei; Atmospheric sciences; Troposphere; Boundary layer; Subsidence; Environmental science; Sea salt aerosol; Planetary boundary layer; Lagrangian; Meteorology; Sea salt; Geology; Physics; Geomorphology; Mechanics","score_opus":0.00982041695046402,"score_gpt":0.19921543762443766,"score_spread":0.18939502067397365,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1997868900","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970759,0.00016307204,0.00002906921,0.0005419698,0.00012852432,0.00021274488,0.00001016654,0.000008321824,0.0018302392],"genre_scores_gemma":[0.99648887,0.000041418636,0.00009178682,0.00008780052,0.00004219988,0.000008614846,4.951547e-7,0.0000078840485,0.0032309487],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992705,0.000047754944,0.00018896532,0.0001233575,0.0002290355,0.00014039534],"domain_scores_gemma":[0.9994612,0.00002196528,0.00010762409,0.00037802415,0.000006214954,0.000025021453],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000098592274,0.00008779642,0.00009242136,4.3994638e-7,0.00037797506,0.000014305125,0.0002975115,0.000038688275,0.0012193035],"category_scores_gemma":[0.000010746423,0.000044009346,0.000058356065,0.00017120905,0.0005142481,0.000052498508,0.000164213,0.00008861348,0.000018967157],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004974262,0.00019027943,0.57152927,0.000027713068,0.000032468517,5.9247543e-7,0.0076373736,0.0007378811,0.4147547,0.00043086836,0.0011315115,0.0034776237],"study_design_scores_gemma":[0.00013825903,0.000017462382,0.9819416,0.000016632432,0.000017138664,0.0000031187874,0.00042662307,0.0003416619,0.012936598,0.00005570628,0.004038281,0.00006691048],"about_ca_topic_score_codex":0.00054811226,"about_ca_topic_score_gemma":0.00009164455,"teacher_disagreement_score":0.41041237,"about_ca_system_score_codex":0.00010104161,"about_ca_system_score_gemma":0.000015162467,"threshold_uncertainty_score":0.9996937},"labels":[],"label_agreement":null},{"id":"W2004771832","doi":"10.3402/tellusb.v52i2.16110","title":"An overview of the Lagrangian experiments undertaken during the North Atlantic regional Aerosol Characterisation Experiment (ACE-2)","year":2000,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":65,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Joint Research Centre; Max-Planck-Gesellschaft","keywords":"Lagrangian; Aerosol; Lagrangian analysis; Entrainment (biomusicology); Environmental science; Atmospheric sciences; Troposphere; Meteorology; Range (aeronautics); Lagrangian particle tracking; Air mass (solar energy); Boundary layer; Climatology; Physics; Geology; Mechanics; Materials science","score_opus":0.03906244710055687,"score_gpt":0.25011829786429796,"score_spread":0.2110558507637411,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2004771832","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976762,0.0008104038,0.000001892123,0.0001838766,0.00006823725,0.00017022298,0.000010602407,0.000021325232,0.0010572369],"genre_scores_gemma":[0.9985495,0.00021534498,0.000038365426,0.00021495859,0.000108403685,0.0000028120576,0.000051962736,0.000003745016,0.000814908],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991378,0.00005960533,0.00018903291,0.00017857415,0.00024837084,0.00018660983],"domain_scores_gemma":[0.99947,0.000028468254,0.00008758236,0.00034384817,0.000011013772,0.00005911827],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000064953565,0.00011997386,0.000114955095,0.000002005953,0.00025251295,0.000031541877,0.00033525855,0.00003815992,0.006872757],"category_scores_gemma":[0.0000025192048,0.00006800388,0.000071192444,0.00012728006,0.000103053135,0.00012296943,0.000008654657,0.0000829363,0.00007037676],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023380933,0.00020636695,0.9086026,0.00011391076,0.00008598007,0.000010090955,0.008311273,0.0029806502,0.06742349,0.000020905547,0.00042089217,0.011590045],"study_design_scores_gemma":[0.00027571002,0.000040705683,0.96950763,0.00004315439,0.000012929987,0.000017478917,0.00040825826,0.00061499316,0.026567342,0.000010231459,0.0023452742,0.00015629345],"about_ca_topic_score_codex":0.0009897477,"about_ca_topic_score_gemma":0.00030791768,"teacher_disagreement_score":0.060905043,"about_ca_system_score_codex":0.0000070783253,"about_ca_system_score_gemma":0.000024072897,"threshold_uncertainty_score":0.9940351},"labels":[],"label_agreement":null},{"id":"W2006480128","doi":"10.3402/tellusb.v56i3.16432","title":"Annual time-series of total filterable atmospheric mercury concentrations in the Arctic","year":2004,"lang":"en","type":"article","venue":"Tellus B","topic":"Mercury impact and mitigation studies","field":"Environmental Science","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada; Toronto Metropolitan University","funders":"","keywords":"Sunrise; Mercury (programming language); Environmental science; Arctic; Polar night; Elemental mercury; Environmental chemistry; MERCURE; Polar; Atmospheric chemistry; Atmospheric sciences; Chemistry; Meteorology; Ozone; Analytical Chemistry (journal); Geology; Oceanography; Geography","score_opus":0.009530196505161669,"score_gpt":0.22761835792985252,"score_spread":0.21808816142469084,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2006480128","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98647934,0.00013836415,0.00012693826,0.0007638479,0.00005139355,0.0001565649,0.000022024224,0.000012622045,0.012248921],"genre_scores_gemma":[0.9978619,0.000030791936,0.00067689794,0.00017561266,0.000014935821,0.000009372744,0.000003739435,0.0000033685922,0.0012233466],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994573,0.000029835252,0.00013709137,0.00008595352,0.0001513327,0.00013846516],"domain_scores_gemma":[0.9997729,0.000039536168,0.00003948061,0.000118613985,0.00000590202,0.00002356168],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000112503425,0.000064160464,0.00008663073,0.0000029232672,0.00007609175,0.000006890216,0.00008621019,0.000018588067,0.001859336],"category_scores_gemma":[0.000035801866,0.00004515725,0.000026026793,0.00019566117,0.0002038114,0.00019374183,0.00003379152,0.000054774428,0.00035689463],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022111091,0.0018418138,0.3624255,0.00013034666,0.00017316025,0.00009541482,0.26342872,0.14104472,0.15454313,0.00971294,0.04680367,0.01957944],"study_design_scores_gemma":[0.0022420033,0.00088020205,0.9134067,0.00010115902,0.000079023965,0.00014251743,0.01982912,0.0005215898,0.029435629,0.008340334,0.024284346,0.0007373727],"about_ca_topic_score_codex":0.0005448836,"about_ca_topic_score_gemma":0.00008971197,"teacher_disagreement_score":0.55098116,"about_ca_system_score_codex":0.000048082264,"about_ca_system_score_gemma":0.000012565061,"threshold_uncertainty_score":0.9990531},"labels":[],"label_agreement":null},{"id":"W2006784304","doi":"10.3402/tellusb.v64i0.18965","title":"Towards the improvements of simulating the chemical and optical properties of Chinese aerosols using an online coupled model – CUACE/Aero","year":2012,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":126,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"National Key Research and Development Program of China","keywords":"Aerosol; Environmental science; Moderate-resolution imaging spectroradiometer; Atmospheric sciences; Daytime; Correlation coefficient; Beijing; Meteorology; Carbon black; Atmosphere (unit); Nitrate; Chemistry; Satellite; China; Geography; Physics","score_opus":0.06331500158074858,"score_gpt":0.2592596699250481,"score_spread":0.19594466834429952,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2006784304","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99890053,0.00041132033,0.00024177687,0.000042793487,0.000033663655,0.00014643671,0.000020148897,0.000010105161,0.00019321953],"genre_scores_gemma":[0.9976122,0.0000087134795,0.002170937,0.000053260563,0.00011228765,5.056913e-7,0.000010577316,0.000003828226,0.000027690554],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9992052,0.000019873925,0.00023709946,0.00011467247,0.00020563575,0.00021755663],"domain_scores_gemma":[0.99952686,0.00006695716,0.000102643135,0.00019361901,0.000032841835,0.00007710998],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025349733,0.000117302305,0.00017246672,0.0000016466896,0.00010013396,0.000016240178,0.00017869663,0.000051822833,0.000075620126],"category_scores_gemma":[0.000079804224,0.000054947104,0.00003676403,0.000083266284,0.0002821852,0.00015384567,0.000043019263,0.00011824434,6.6810065e-7],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001093704,0.0001580197,0.08302126,0.00010022281,0.000037581096,4.114664e-7,0.0027039906,0.062453806,0.84522057,0.000011687928,0.0000019095562,0.0061811917],"study_design_scores_gemma":[0.00020777824,0.0000328286,0.00891161,0.000021393198,0.00002277231,0.0000053465374,0.00044251725,0.93823487,0.051950775,0.000076066375,0.0000015756934,0.00009246133],"about_ca_topic_score_codex":0.0002842768,"about_ca_topic_score_gemma":0.000013596691,"teacher_disagreement_score":0.87578106,"about_ca_system_score_codex":0.0000024906135,"about_ca_system_score_gemma":0.000034711527,"threshold_uncertainty_score":0.22406779},"labels":[],"label_agreement":null},{"id":"W2009240781","doi":"10.1111/j.1600-0889.2007.00288.x","title":"Temporal variations of atmospheric carbon dioxide in the southernmost part of Japan","year":2007,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Nature; Research Institute for Humanity and Nature","keywords":"Environmental science; Subtropics; Atmospheric sciences; Carbon dioxide in Earth's atmosphere; Climatology; Carbon dioxide; Carbon cycle; North Pacific High; Annual cycle; El Niño Southern Oscillation; Pacific decadal oscillation; Oceanography; Climate change; Geology; Ecosystem","score_opus":0.0069768121597092074,"score_gpt":0.19841183562080394,"score_spread":0.19143502346109473,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2009240781","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9779025,0.000028759725,0.0031480847,0.000040296432,0.000043940207,0.00014192327,0.000001768988,0.000008280242,0.018684492],"genre_scores_gemma":[0.9941913,0.000010243612,0.005210955,0.000064769105,0.000015578677,0.0000033891424,0.0000021275193,0.000010238771,0.00049138215],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990656,0.000034919845,0.00029671966,0.00013821959,0.0002718436,0.00019274808],"domain_scores_gemma":[0.9995158,0.000060911243,0.00013102397,0.0002574134,0.0000014971956,0.000033379092],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043620163,0.00009451006,0.0001307089,0.0000017006139,0.000030619096,0.0000020329571,0.00023731627,0.000052065458,0.0003618963],"category_scores_gemma":[0.000013314295,0.00007068588,0.00004471495,0.00028047082,0.00024927926,0.000038655257,0.00007805771,0.000088144734,0.000019977995],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016266815,0.00015040483,0.979332,0.000004029176,0.0000059574886,0.0000023652922,0.0025195854,0.011489347,0.0020316981,0.000120174256,0.000015923091,0.0043122605],"study_design_scores_gemma":[0.0002773587,0.00009321598,0.9872084,0.000009696488,0.00001866275,0.000004566512,0.0028106365,0.0073179067,0.0004460538,0.0003544913,0.0013214322,0.00013754943],"about_ca_topic_score_codex":0.003634424,"about_ca_topic_score_gemma":0.0005815865,"teacher_disagreement_score":0.018193109,"about_ca_system_score_codex":0.00008567046,"about_ca_system_score_gemma":0.000004959831,"threshold_uncertainty_score":0.5494186},"labels":[],"label_agreement":null},{"id":"W2011626819","doi":"10.1111/j.1600-0889.2007.00275.x","title":"Sensitivity of Lagrangian Stochastic footprints to turbulence statistics","year":2007,"lang":"en","type":"article","venue":"Tellus B","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Agriculture and Agri-Food Canada","funders":"","keywords":"Turbulence; Smoothing; Sensitivity (control systems); Decoupling (probability); Footprint; Eddy covariance; Meteorology; K-epsilon turbulence model; Environmental science; Stochastic modelling; Physics; Atmospheric sciences; Statistical physics; Mathematics; Statistics; Geology","score_opus":0.00682821276503931,"score_gpt":0.2140546644251939,"score_spread":0.2072264516601546,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2011626819","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5995862,0.0000017739065,0.39704582,0.000015529336,0.000045737295,0.000073827236,0.000040828312,0.000012908848,0.003177373],"genre_scores_gemma":[0.99154705,8.4482474e-7,0.007912866,0.00004876694,0.000008663533,6.240208e-7,0.00000640352,0.000005337485,0.00046947255],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9993723,0.000017101924,0.00012875708,0.00012822771,0.00017997975,0.00017365844],"domain_scores_gemma":[0.9996312,0.00009505502,0.000036084577,0.00014191143,0.000006514524,0.00008923725],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038590506,0.00006460323,0.00007932437,0.000028545614,0.000031744206,0.0000048352404,0.00006965079,0.00003124814,0.00014481644],"category_scores_gemma":[0.00003872891,0.000061001476,0.000016436808,0.00014097904,0.00006107244,0.000027485328,0.000079739046,0.000057580128,0.00030440764],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016921994,0.0003970801,0.10082795,0.000040209914,0.000043207096,0.0002715376,0.0037071777,0.5345421,0.1458209,0.00639133,0.00096748245,0.20682183],"study_design_scores_gemma":[0.0004441807,0.00018858649,0.76930493,0.00005182208,0.000050427403,0.00009026483,0.00008596002,0.21553889,0.008279858,0.0030915735,0.0022438308,0.00062969443],"about_ca_topic_score_codex":0.00046821448,"about_ca_topic_score_gemma":0.00080784544,"teacher_disagreement_score":0.66847694,"about_ca_system_score_codex":0.000051189196,"about_ca_system_score_gemma":0.000003695904,"threshold_uncertainty_score":0.39126462},"labels":[],"label_agreement":null},{"id":"W2017978156","doi":"10.3402/tellusb.v64i0.19138","title":"Relative contribution of transport/surface flux to the seasonal vertical synoptic CO<sub>2</sub> variability in the troposphere over Narita","year":2012,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Troposphere; Environmental science; Atmospheric sciences; Climatology; Flux (metallurgy); Planetary boundary layer; Boundary layer; Standard deviation; Geology; Physics; Chemistry","score_opus":0.00511746430353837,"score_gpt":0.20429422610521528,"score_spread":0.1991767618016769,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2017978156","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9775789,0.00011774627,0.016990637,0.0005734509,0.00010361281,0.0006464836,0.000021797423,0.000021647676,0.003945732],"genre_scores_gemma":[0.9982234,0.000023808438,0.0011166418,0.0003344581,0.000038985414,0.000020765612,0.000019689493,0.000019151124,0.0002030961],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9977064,0.00035246284,0.00038235114,0.00033680574,0.0006636168,0.0005583635],"domain_scores_gemma":[0.99892306,0.00036024113,0.00007221366,0.00046927264,0.000006523883,0.00016866153],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014298584,0.00024002034,0.0002652695,0.000002748206,0.00016448948,0.000011214256,0.00038998324,0.00015707679,0.0015464266],"category_scores_gemma":[0.000104090024,0.00015651465,0.00011912862,0.000306423,0.0005752725,0.00027325304,0.00011240039,0.00032506074,0.0003762517],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039776252,0.0012658958,0.867604,0.000019805122,0.000074496136,0.000013147537,0.0060266233,0.07955792,0.033697765,0.006976501,0.0012654045,0.0031006609],"study_design_scores_gemma":[0.0005215195,0.00014460251,0.9744169,0.000015606745,0.0000806859,0.000010268913,0.0002603047,0.018561175,0.0012514159,0.00048865424,0.003996425,0.00025240454],"about_ca_topic_score_codex":0.0001339703,"about_ca_topic_score_gemma":0.00013280704,"teacher_disagreement_score":0.10681292,"about_ca_system_score_codex":0.0005252513,"about_ca_system_score_gemma":0.000015994101,"threshold_uncertainty_score":0.9993663},"labels":[],"label_agreement":null},{"id":"W2021877375","doi":"10.3402/tellusb.v67.23930","title":"Impacts of additional HONO sources on O<sub>3</sub> and PM<sub>2.5</sub> chemical coupling and control strategies in the Beijing–Tianjin–Hebei region of China","year":2015,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Anhui Institute of Optics and Fine Mechanics, Chinese Academy of Sciences; Chinese Academy of Sciences; Institute of Atmospheric Physics, Chinese Academy of Sciences; National Natural Science Foundation of China; CERN","keywords":"Daytime; NOx; Ozone; Nitrogen dioxide; Particulates; Environmental chemistry; Atmospheric sciences; Aerosol; Beijing; Chemistry; Ammonia; Environmental science; Atmospheric chemistry; Nitrous acid; Meteorology; Inorganic chemistry","score_opus":0.012257530537493547,"score_gpt":0.2004491058995779,"score_spread":0.18819157536208436,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2021877375","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9926258,0.0031300713,0.00007913514,0.00038498917,0.00013425775,0.0004112621,0.0006269777,0.000057186167,0.0025503696],"genre_scores_gemma":[0.99829537,0.00042488668,0.0001491738,0.00015326662,0.00045108344,0.000008658052,0.00045865646,0.000019235546,0.00003968656],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99708194,0.000114637034,0.00072124123,0.00063577347,0.0007884207,0.0006579838],"domain_scores_gemma":[0.99773455,0.000861734,0.00050363503,0.0004207462,0.0001150036,0.0003643443],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.000802426,0.0004946589,0.0007266686,0.000039692397,0.00021661396,0.00016835265,0.0004600674,0.0003298737,0.0003553315],"category_scores_gemma":[0.00029720116,0.0003799798,0.0001388255,0.0003620579,0.0007745326,0.0004227647,0.00005545629,0.00044795003,0.000023975737],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00467492,0.0009355757,0.07649639,0.0011565378,0.000529505,0.0004165196,0.009573797,0.018381307,0.8446243,0.0010497132,0.025344858,0.016816625],"study_design_scores_gemma":[0.020327507,0.0042473036,0.48307067,0.0029296756,0.00080613233,0.0013769722,0.0075783553,0.076404475,0.3758991,0.010720418,0.01180202,0.004837377],"about_ca_topic_score_codex":0.00016660626,"about_ca_topic_score_gemma":0.00038282652,"teacher_disagreement_score":0.46872514,"about_ca_system_score_codex":0.000024631776,"about_ca_system_score_gemma":0.00026283492,"threshold_uncertainty_score":0.99986523},"labels":[],"label_agreement":null},{"id":"W2030064926","doi":"10.1111/j.1600-0889.2007.00333.x","title":"Vulnerability of permafrost carbon to global warming. Part I: model description and role of heat generated by organic matter decomposition","year":2008,"lang":"en","type":"article","venue":"Tellus B","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":117,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Science North","funders":"","keywords":"Permafrost; Methane; Soil respiration; Methanogenesis; Environmental science; Soil organic matter; Soil carbon; Carbon cycle; Organic matter; Carbon fibers; Soil science; Atmospheric sciences; Chemistry; Environmental chemistry; Ecosystem; Ecology; Soil water; Geology; Materials science","score_opus":0.02739488898956178,"score_gpt":0.23427866224392105,"score_spread":0.20688377325435928,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2030064926","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99426425,0.00068774645,0.00005125585,0.00011094573,0.00006877544,0.00013129467,0.0037200176,0.000012591376,0.0009531002],"genre_scores_gemma":[0.9980423,0.000120764314,0.00010384012,0.00017648548,0.00003608562,8.65316e-7,0.0014686575,0.000003167182,0.000047875754],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999233,0.000042624444,0.00021884908,0.00019337289,0.00014097129,0.00017115653],"domain_scores_gemma":[0.9996611,0.000017699578,0.00003848949,0.0001338506,0.000049142567,0.00009973742],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00009348559,0.00010646147,0.00018001512,0.000027706423,0.00007424077,0.00000963523,0.000069155474,0.000059934544,0.0013456953],"category_scores_gemma":[0.0000045714983,0.00009656294,0.00002569015,0.00014403368,0.0000715793,0.000087993234,0.000013506854,0.00004732289,0.000026918577],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006767515,0.000035232355,0.79912853,0.000022182006,0.000005375103,0.0000012461342,0.0007286008,0.0010475881,0.19720702,6.043267e-7,0.0013175132,0.00043842712],"study_design_scores_gemma":[0.0005234732,0.00033419614,0.70241654,0.00003943333,0.000041952844,0.00008757509,0.0002466767,0.22747697,0.067896426,0.00017390087,0.00041395417,0.0003488997],"about_ca_topic_score_codex":0.005534796,"about_ca_topic_score_gemma":0.0034443506,"teacher_disagreement_score":0.22642939,"about_ca_system_score_codex":0.000010791321,"about_ca_system_score_gemma":0.000020679112,"threshold_uncertainty_score":0.9995672},"labels":[],"label_agreement":null},{"id":"W2041398829","doi":"10.3402/tellusb.v54i2.16652","title":"Tropospheric carbon dioxide concentrations at a northern boreal site in Finland: basic variations and source areas","year":2002,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Academy of Finland","keywords":"Environmental science; Atmospheric sciences; Diurnal cycle; Troposphere; Aerosol; Boreal; Climatology; Annual cycle; Air mass (solar energy); Diurnal temperature variation; Ozone; Seasonality; Tropospheric ozone; Peninsula; Daytime; Oceanography; Meteorology; Geology; Geography; Boundary layer","score_opus":0.004798319504628835,"score_gpt":0.16560331174222703,"score_spread":0.1608049922375982,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2041398829","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9846676,0.00013375722,0.003074717,0.00016005481,0.000029628527,0.00016204662,0.0000036819845,0.000029462299,0.011739052],"genre_scores_gemma":[0.99222594,0.00014930213,0.0010649523,0.00014532257,0.000019218847,0.000014659339,0.000008087476,0.000018161443,0.0063543343],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990925,0.000035178084,0.00017203133,0.00027099787,0.00016591385,0.00026335832],"domain_scores_gemma":[0.99961567,0.000035743986,0.000055162673,0.0001839837,0.0000011611298,0.00010829238],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000047927697,0.0001407242,0.00012609495,0.0000031328518,0.000114705676,0.000012440972,0.00008531146,0.00006133507,0.0013373444],"category_scores_gemma":[0.000009091813,0.00013658585,0.000028743307,0.00016095105,0.00018526596,0.00008066151,0.00012267298,0.000098901925,0.00022680862],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000073441433,0.000085691565,0.93777466,0.0000017847572,0.0000053008334,0.000010711999,0.0014862415,0.053249247,0.00041399064,0.000013701564,0.00007168638,0.006879618],"study_design_scores_gemma":[0.00042872113,0.000043032953,0.61889696,0.0000043957975,0.000016797094,0.00001704566,0.00009778147,0.37758353,0.000016214146,0.000051781193,0.002658345,0.00018539015],"about_ca_topic_score_codex":0.00356426,"about_ca_topic_score_gemma":0.0042255293,"teacher_disagreement_score":0.32433426,"about_ca_system_score_codex":0.0003991766,"about_ca_system_score_gemma":0.0000025897102,"threshold_uncertainty_score":0.99957556},"labels":[],"label_agreement":null},{"id":"W2041695015","doi":"10.1111/j.1600-0889.2006.00188.x","title":"Climatic effect on DMS producers in the NE sub-Arctic Pacific: ENSO on the upper ocean","year":2006,"lang":"en","type":"article","venue":"Tellus B","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval; Fisheries and Oceans Canada","funders":"Fisheries and Oceans Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Phytoplankton; Oceanography; Arctic; Environmental science; El Niño Southern Oscillation; Climatology; Dimethyl sulfide; Mixed layer; Pacific ocean; Atmospheric sciences; Geology; Chemistry; Nutrient; Ecology; Biology","score_opus":0.00808174315733014,"score_gpt":0.18260443554574066,"score_spread":0.1745226923884105,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2041695015","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8650686,0.000063842104,3.8842393e-7,0.0012587678,0.00017816391,0.0004571878,0.000008719904,0.000022847336,0.13294147],"genre_scores_gemma":[0.99844414,0.000008152277,0.0000017381992,0.0004641849,0.00018700227,0.000003141373,0.000037958824,0.000004146286,0.0008495164],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987178,0.00030668077,0.00017883147,0.00021660348,0.00029073117,0.0002893429],"domain_scores_gemma":[0.9988759,0.00067469425,0.000051270476,0.000361243,0.000008593673,0.000028293258],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000905699,0.00014206758,0.00013910685,0.00005370055,0.0001466537,0.000082173865,0.00025829635,0.00003589858,0.00054191716],"category_scores_gemma":[0.000058833506,0.00006439342,0.00005914486,0.00023942335,0.000043866115,0.00003854431,0.000008266529,0.0002150388,0.0010815373],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021499294,0.00012115449,0.90121716,0.00017832791,0.000019374287,0.0000789344,0.0008832427,0.003364133,0.000036215875,0.001168247,0.011150999,0.081567205],"study_design_scores_gemma":[0.0006627843,0.0022350007,0.93889105,0.00017356192,0.000036175355,0.0000612215,0.0010144066,0.014946796,0.0006440901,0.0019924394,0.03885607,0.00048639567],"about_ca_topic_score_codex":0.004803727,"about_ca_topic_score_gemma":0.0038385924,"teacher_disagreement_score":0.13337554,"about_ca_system_score_codex":0.0000065374556,"about_ca_system_score_gemma":0.000013886532,"threshold_uncertainty_score":0.99969625},"labels":[],"label_agreement":null},{"id":"W2042843833","doi":"10.1111/j.1600-0889.2009.00423.x","title":"Atmospheric circulation controls on precipitation isotope–climate relations in western Canada","year":2009,"lang":"en","type":"article","venue":"Tellus B","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":82,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Waterloo","funders":"","keywords":"Climatology; Precipitation; Atmospheric circulation; Stable isotope ratio; Isotope; Atmospheric sciences; Ridge; Environmental science; δ18O; Trough (economics); Geology; Geography; Meteorology","score_opus":0.011970185569565507,"score_gpt":0.22766694631080944,"score_spread":0.21569676074124394,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2042843833","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9709028,0.00016424534,0.000027572913,0.0013186383,0.00012527235,0.00021931333,0.00000941626,0.000020405929,0.02721232],"genre_scores_gemma":[0.9988299,0.000018419069,0.00009360595,0.00051983463,0.000022339693,0.0000016490994,0.00010311619,0.0000012628395,0.0004098946],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990911,0.00013897297,0.00017143272,0.00016807644,0.0001464587,0.00028397157],"domain_scores_gemma":[0.9994894,0.00027040552,0.00004549758,0.00011713885,0.000021509692,0.000056036213],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022705965,0.000078086734,0.00012086177,0.000023284147,0.00012376849,0.000013644591,0.00009123555,0.00007958627,0.00070965954],"category_scores_gemma":[0.000055652657,0.00007118799,0.00001662012,0.00018463955,0.000029241897,0.000096670745,0.0000021866038,0.00017353751,0.00044577676],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000046369685,0.000010201917,0.97374487,0.0000023342961,0.0000027652425,0.000020981755,0.00009021244,0.023406923,0.0000028936256,0.00017673161,0.00005618023,0.0024395625],"study_design_scores_gemma":[0.0003275485,0.000087678614,0.9835644,0.000008940609,0.000003246089,0.000008915779,0.000025087369,0.014980009,0.000003545655,0.00041831093,0.0004972288,0.000075102726],"about_ca_topic_score_codex":0.038362253,"about_ca_topic_score_gemma":0.8420321,"teacher_disagreement_score":0.80366987,"about_ca_system_score_codex":0.0000063014927,"about_ca_system_score_gemma":0.00011001937,"threshold_uncertainty_score":0.96804136},"labels":[],"label_agreement":null},{"id":"W2044061235","doi":"10.1111/j.1600-0889.2007.00332.x","title":"A Kalman-filter bias correction method applied to deterministic, ensemble averaged and probabilistic forecasts of surface ozone","year":2008,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":60,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"Office of Science; National Oceanic and Atmospheric Administration","keywords":"Ozone; Ensemble Kalman filter; Probabilistic logic; Environmental science; Kalman filter; Mean squared error; Statistics; Ensemble forecasting; Meteorology; Mathematics; Atmospheric sciences; Extended Kalman filter; Physics","score_opus":0.038062069410863084,"score_gpt":0.23663142315594693,"score_spread":0.19856935374508383,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2044061235","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9785623,0.000054054897,0.009009262,0.000019326464,0.00015962256,0.00023982092,0.000015296542,0.00003528369,0.0119050555],"genre_scores_gemma":[0.98157424,0.000012935763,0.015904406,0.000065256834,0.00004909147,0.0000016261764,0.00001864037,0.0000043190585,0.0023695012],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99913746,0.000036120164,0.00021388361,0.00025486035,0.0001511598,0.00020649197],"domain_scores_gemma":[0.9992883,0.00031427384,0.00008037877,0.00016138912,0.000026914458,0.00012874129],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017221147,0.00013162484,0.00022535834,0.0000058000655,0.00012688583,0.000012613591,0.000089258676,0.000061314866,0.00057267165],"category_scores_gemma":[0.000092235634,0.00011315226,0.00003091021,0.00016035605,0.00007768062,0.00004526711,0.00001544877,0.000091562746,0.00007603658],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022601776,0.00036456189,0.17135458,0.00075504556,0.00017289384,0.00030965588,0.01321421,0.1973136,0.16171053,0.00007497437,0.010636144,0.44183362],"study_design_scores_gemma":[0.0031510813,0.0018040331,0.38536134,0.00020930267,0.00019861365,0.0019415253,0.0008327842,0.26616827,0.3265776,0.001814181,0.009796229,0.0021450298],"about_ca_topic_score_codex":0.00026912533,"about_ca_topic_score_gemma":0.00013191828,"teacher_disagreement_score":0.4396886,"about_ca_system_score_codex":0.00000435725,"about_ca_system_score_gemma":0.000034882876,"threshold_uncertainty_score":0.6270353},"labels":[],"label_agreement":null},{"id":"W2048225693","doi":"10.3402/tellusb.v57i4.16545","title":"Modelling of hydrogen and oxygen isotope compositions for local precipitation","year":2005,"lang":"en","type":"article","venue":"Tellus B","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Transpiration; Evaporation; Isotope fractionation; Equilibrium fractionation; Isotopes of oxygen; Deuterium; Chemistry; Hydrogen; Fractionation; Stable isotope ratio; Oxygen isotope ratio cycle; Oxygen; Precipitation; Condensation; Thermodynamics; Meteorology; Nuclear chemistry; Chromatography","score_opus":0.02107064755746523,"score_gpt":0.20898249176279304,"score_spread":0.1879118442053278,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2048225693","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.89456004,0.00042737758,0.10132697,0.000116749026,0.000021568705,0.00014024976,0.000064275395,0.000014469452,0.0033283248],"genre_scores_gemma":[0.9932347,0.00001929685,0.006277455,0.000039349175,0.000056989833,0.0000015243721,0.00014220022,0.0000016274356,0.00022683768],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99962014,0.0000072924227,0.00011120589,0.000099119745,0.00005913507,0.00010310142],"domain_scores_gemma":[0.99980867,0.00004038012,0.00002576079,0.00006133724,0.000022389775,0.00004147021],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000069945905,0.000050445997,0.00007264509,0.000018434654,0.000062898886,0.000011676936,0.000052790194,0.000030091314,0.00018475375],"category_scores_gemma":[0.0000018592395,0.00004507503,0.000023181241,0.000031960077,0.000043154985,0.00009239747,0.0000038904464,0.00002738954,0.000020546215],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007019866,0.000031951553,0.0102340905,0.00008053853,0.00002581203,5.5148604e-7,0.0010994104,0.9128113,0.0018505383,0.00010061965,0.0002925842,0.073402435],"study_design_scores_gemma":[0.00022645258,0.00006271769,0.0021802988,0.0000096789345,0.000014849095,0.000006742328,0.00009203031,0.98012614,0.013050576,0.0010862771,0.0030616096,0.00008261098],"about_ca_topic_score_codex":0.00028355967,"about_ca_topic_score_gemma":0.000090868445,"teacher_disagreement_score":0.09867471,"about_ca_system_score_codex":0.0000018053848,"about_ca_system_score_gemma":0.0000096488775,"threshold_uncertainty_score":0.2022924},"labels":[],"label_agreement":null},{"id":"W2055523201","doi":"10.1111/j.1600-0889.2006.00235.x","title":"Global monthly CO<sub>2</sub> flux inversion with a focus over North America","year":2007,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":70,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"","keywords":"Environmental science; Carbon sink; Sink (geography); Inversion (geology); Spatial distribution; Atmospheric sciences; Flux (metallurgy); Climatology; Geography; Geology; Climate change; Oceanography; Chemistry; Remote sensing; Cartography; Geomorphology","score_opus":0.0035341571726119655,"score_gpt":0.18187194127980172,"score_spread":0.17833778410718976,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2055523201","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9318158,0.00009435324,0.013902184,0.000059009126,0.000094428855,0.0003031581,0.000023599161,0.00011915689,0.053588327],"genre_scores_gemma":[0.9920475,0.00007392245,0.0059118657,0.0006713688,0.00006311712,0.000008032662,0.000041375115,0.00004169566,0.0011411256],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99753386,0.000033591205,0.0003031648,0.0006088754,0.0007765818,0.00074393157],"domain_scores_gemma":[0.99894184,0.000034705907,0.00016478667,0.00048017033,0.0000042938436,0.00037421763],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00014174626,0.0003732054,0.00028228422,0.000009891833,0.00023403476,0.00003024187,0.00038901434,0.00013433745,0.0014584325],"category_scores_gemma":[0.000008852169,0.00032167393,0.00010263539,0.0005147861,0.0006847592,0.00026516512,0.0003176669,0.0001704874,0.0017067168],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005577299,0.0005695824,0.73193264,0.00001575625,0.00008083346,0.00039065964,0.0007338323,0.0974319,0.007227126,0.000058501697,0.015919214,0.1450822],"study_design_scores_gemma":[0.0013853103,0.00065970066,0.871383,0.00002102088,0.00008358671,0.00003423167,0.00023394315,0.020938966,0.0010257782,0.000167375,0.10313514,0.0009319123],"about_ca_topic_score_codex":0.00075555436,"about_ca_topic_score_gemma":0.0019441746,"teacher_disagreement_score":0.1441503,"about_ca_system_score_codex":0.0009602902,"about_ca_system_score_gemma":0.00001588513,"threshold_uncertainty_score":0.9999235},"labels":[],"label_agreement":null},{"id":"W2065273841","doi":"10.3402/tellusb.v65i0.20480","title":"Atmospheric nitrogen deposition to forest and estuary environments in the Pearl River Delta region, southern China","year":2013,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Sun Yat-sen University; National Natural Science Foundation of China","keywords":"Deposition (geology); Environmental science; Nitrogen; Estuary; Nitrate; Environmental chemistry; Reactive nitrogen; Dry season; Wet season; Hydrology (agriculture); Ecology; Chemistry; Geology; Biology; Sediment","score_opus":0.006377352429279659,"score_gpt":0.16802972537587235,"score_spread":0.16165237294659268,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2065273841","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968808,0.00027311806,0.0004558364,0.0003245459,0.000021338004,0.00023502375,0.000005289832,0.000012442072,0.0017915472],"genre_scores_gemma":[0.9979093,0.000025921794,0.00108987,0.00040361157,0.000058736507,0.0000054477305,0.000032030133,0.0000033356598,0.0004717302],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99934256,0.000037655667,0.00011196299,0.0001823842,0.000128935,0.00019648243],"domain_scores_gemma":[0.99968886,0.000037946822,0.0000326902,0.00015769328,0.000002976001,0.00007980858],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006894746,0.00010448455,0.00008209039,0.0000011823399,0.000113823815,0.000046163725,0.00016246688,0.00004461373,0.0005768769],"category_scores_gemma":[0.000008415859,0.00007113577,0.000021875967,0.00010320181,0.000073595555,0.00011274584,0.000015663836,0.000088790606,0.0005366466],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015845164,0.000021791982,0.9721446,0.000006823459,0.0000070607357,0.00002614233,0.0032674945,0.0018288698,0.00019981731,0.0000019755325,0.00066033023,0.021819258],"study_design_scores_gemma":[0.00017317911,0.00006143249,0.99301887,0.000011325084,0.000008139241,0.000047267633,0.0009857465,0.004100945,0.000054560558,0.00085262005,0.00054741837,0.00013848269],"about_ca_topic_score_codex":0.009345226,"about_ca_topic_score_gemma":0.00056768494,"teacher_disagreement_score":0.021680774,"about_ca_system_score_codex":0.0000038923636,"about_ca_system_score_gemma":0.0000063510097,"threshold_uncertainty_score":0.99725163},"labels":[],"label_agreement":null},{"id":"W2067857992","doi":"10.3402/tellusb.v55i2.16731","title":"North American influence on atmospheric carbon dioxide data collected at Sable Island, Canada","year":2003,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Air mass (solar energy); Environmental science; Climatology; Diurnal cycle; Vegetation (pathology); Atmospheric sciences; Carbon dioxide in Earth's atmosphere; Arctic; The arctic; Noon; Oceanography; Physical geography; Geography; Geology; Climate change; Boundary layer","score_opus":0.005392924560376688,"score_gpt":0.1767054142189872,"score_spread":0.1713124896586105,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2067857992","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97644705,0.00002444817,0.00013915627,0.000041634226,0.00008615647,0.00019211888,0.000023023958,0.00003917499,0.023007222],"genre_scores_gemma":[0.9860213,0.000058461974,0.0031063983,0.0008236502,0.000012427245,0.000010061543,0.00003470465,0.00003504866,0.009897978],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998125,0.0000660694,0.0002239139,0.00058758,0.00048689632,0.0005105252],"domain_scores_gemma":[0.9986418,0.000057509693,0.00012469474,0.00096428476,0.000002586472,0.00020913764],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000079078265,0.00025103314,0.0002291566,0.0000014175174,0.00020009828,0.000012177111,0.0005574146,0.000034274115,0.0009803188],"category_scores_gemma":[0.000052668252,0.00023425592,0.000022532216,0.00057882955,0.00032088353,0.000092987546,0.00039714688,0.0001574924,0.00017092563],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000031592943,0.00006016176,0.8049829,0.0000026313955,0.000015992098,0.00004486599,0.000059204714,0.1897082,0.00020290157,0.0000039028487,0.0035224194,0.0013651905],"study_design_scores_gemma":[0.0004332997,0.00016606708,0.8657258,0.000006058528,0.000030825093,0.000025150646,0.000116813244,0.029783739,0.00022833857,0.000011142098,0.102882326,0.00059045537],"about_ca_topic_score_codex":0.62051237,"about_ca_topic_score_gemma":0.9263213,"teacher_disagreement_score":0.30580896,"about_ca_system_score_codex":0.0015289931,"about_ca_system_score_gemma":0.00007152797,"threshold_uncertainty_score":0.99993294},"labels":[],"label_agreement":null},{"id":"W2073511397","doi":"10.1111/j.1600-0889.2007.00328.x","title":"Forest floor versus ecosystem CO<sub>2</sub> exchange along boreal ecotone between upland forest and lowland mire","year":2008,"lang":"en","type":"article","venue":"Tellus B","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canada Research Chairs; University of Toronto","funders":"","keywords":"Mire; Peat; Ecotone; Deserts and xeric shrublands; Atmospheric sciences; Biomass (ecology); Environmental science; Hydrology (agriculture); Forestry; Physics; Ecology; Geography; Geology","score_opus":0.01724935568654502,"score_gpt":0.21980006569628885,"score_spread":0.20255071000974384,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2073511397","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9848758,0.0003702345,0.000057318513,0.00013988293,0.0002886353,0.00051686744,0.00023425989,0.00010232783,0.013414678],"genre_scores_gemma":[0.9977395,0.0007160083,0.00007515909,0.000062446234,0.00039714403,0.000054986063,0.00040343183,0.00004509517,0.00050623354],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9976346,0.00008077717,0.00042824057,0.000671253,0.0003792326,0.0008058854],"domain_scores_gemma":[0.9987808,0.00021141897,0.0001651523,0.0004233892,0.0000134087495,0.00040586301],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0003201949,0.0003930686,0.00055531954,0.00009523334,0.000460456,0.0000477187,0.00034181267,0.00028654447,0.0004760602],"category_scores_gemma":[0.000033899203,0.00033997957,0.00009982876,0.00018933607,0.00030748983,0.000228314,0.00027733305,0.00021065654,0.0006350777],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020794592,0.00007217401,0.9809388,0.0000499137,0.000056972127,0.00028652424,0.0003879245,0.00007383512,0.0006934655,0.000009906183,0.014617668,0.002604856],"study_design_scores_gemma":[0.003379377,0.0005632716,0.9565654,0.000030331581,0.00007438646,0.00018999403,0.000020636458,0.002062727,0.0005960606,0.000059727834,0.03594419,0.00051391067],"about_ca_topic_score_codex":0.00053979515,"about_ca_topic_score_gemma":0.038522363,"teacher_disagreement_score":0.03798257,"about_ca_system_score_codex":0.00017398638,"about_ca_system_score_gemma":0.00002839871,"threshold_uncertainty_score":0.9999052},"labels":[],"label_agreement":null},{"id":"W2076463675","doi":"10.3402/tellusb.v56i5.16458","title":"The Arctic: a sink for mercury","year":2004,"lang":"en","type":"article","venue":"Tellus B","topic":"Mercury impact and mitigation studies","field":"Environmental Science","cited_by":219,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal; Université du Québec à Montréal; Environment and Climate Change Canada; McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Mercury (programming language); Arctic; Troposphere; Ozone depletion; Environmental chemistry; Halogen; Sink (geography); Ozone; Snow; Chemistry; Atmospheric sciences; Environmental science; Meteorology; Oceanography; Geology","score_opus":0.020887609282624398,"score_gpt":0.2671603618742697,"score_spread":0.24627275259164533,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076463675","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.86302763,0.0007448627,0.010198234,0.019087762,0.00074703654,0.0010307032,0.000014730625,0.00014596303,0.10500305],"genre_scores_gemma":[0.995731,0.000057440076,0.0006796802,0.0005348591,0.000046765465,0.00002801713,0.0000011640137,0.0000055855585,0.0029154797],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9995626,0.0000069142125,0.00007753829,0.00008545043,0.00010329726,0.00016415367],"domain_scores_gemma":[0.99972904,0.000084212355,0.000024521341,0.000117174,0.0000046115956,0.00004045153],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001376391,0.000053492702,0.000048035574,0.0000043209607,0.00031523232,0.00001860425,0.00009298238,0.000015436171,0.00023693386],"category_scores_gemma":[0.00007691281,0.000032704316,0.00003562381,0.00006148222,0.00014933437,0.000053505897,0.00004377604,0.000032436594,0.0006381945],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003099642,0.0005134486,0.044088833,0.00008225214,0.0002920589,0.00001760864,0.026514908,0.006935101,0.08350799,0.095051594,0.18131788,0.56136835],"study_design_scores_gemma":[0.0008883625,0.00014240293,0.036422197,0.0000127915955,0.00003107035,0.000012982685,0.0007071019,0.0000732472,0.012208798,0.056068897,0.89318424,0.00024792552],"about_ca_topic_score_codex":0.00013100795,"about_ca_topic_score_gemma":0.00009375783,"teacher_disagreement_score":0.7118663,"about_ca_system_score_codex":0.000062096864,"about_ca_system_score_gemma":0.000005845465,"threshold_uncertainty_score":0.8202912},"labels":[],"label_agreement":null},{"id":"W2081326776","doi":"10.3402/tellusb.v57i4.16556","title":"Temporal and spatial distribution of dimethylsulfide in the subarctic northeast Pacific Ocean: a high-nutrient–low-chlorophyll region","year":2005,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Subarctic climate; Oceanography; Chlorophyll a; Environmental science; Nutrient; Flux (metallurgy); Nitrate; Chlorophyll; Mixed layer; Salinity; Geology; Chemistry","score_opus":0.007637651403665224,"score_gpt":0.18393505329956894,"score_spread":0.1762974018959037,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2081326776","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99809265,0.00029156927,0.00047009916,0.0005129375,0.000053363685,0.00013563716,0.000045344204,0.000013668116,0.00038470092],"genre_scores_gemma":[0.999387,0.000055830154,0.00007928272,0.000035181936,0.00015213517,5.943813e-7,0.00020714264,0.0000021816688,0.00008063279],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99915105,0.00005846402,0.00022190841,0.0001883728,0.00018579939,0.00019438902],"domain_scores_gemma":[0.99954236,0.000115464274,0.000092351846,0.00017549263,0.000017776822,0.00005653654],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020058287,0.000111868765,0.00014697154,0.0000049022724,0.00008539371,0.000024441777,0.00014019094,0.000058226808,0.00012309475],"category_scores_gemma":[0.000032819455,0.00007717914,0.000035870307,0.00019544084,0.0001513652,0.00010473603,0.000009619371,0.00013299403,0.000016402615],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020973473,0.000095189986,0.96630114,0.000060435894,0.00000840877,0.000035201716,0.0008386089,0.00051443913,0.00013485376,0.000058887803,0.00027999192,0.031463094],"study_design_scores_gemma":[0.00082011713,0.00017271056,0.9876651,0.000050064842,0.000021183605,0.000063771964,0.00072095596,0.0046105976,0.0018748844,0.0006038673,0.0031568496,0.00023990241],"about_ca_topic_score_codex":0.0038078032,"about_ca_topic_score_gemma":0.00074853713,"teacher_disagreement_score":0.031223193,"about_ca_system_score_codex":0.0000059867507,"about_ca_system_score_gemma":0.000023710782,"threshold_uncertainty_score":0.57562846},"labels":[],"label_agreement":null},{"id":"W2086079033","doi":"10.1111/j.1600-0889.2007.00291.x","title":"The influence of below-cloud secondary effects on the stable isotope composition of hydrogen and oxygen in precipitation at Calgary, Alberta, Canada","year":2007,"lang":"en","type":"article","venue":"Tellus B","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":107,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"International Atomic Energy Agency","keywords":"Oxygen-18; Precipitation; Fractionation; Stable isotope ratio; Isotopes of oxygen; Snow; Relative humidity; Chemistry; Isotope; Hydrogen; Analytical Chemistry (journal); Atmospheric sciences; Environmental chemistry; Meteorology; Geology; Physics; Nuclear chemistry","score_opus":0.0035753378026539403,"score_gpt":0.170466587639802,"score_spread":0.16689124983714806,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2086079033","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9929482,0.00029425183,0.0000019548422,0.00010777497,0.000045219167,0.00020160597,0.000013985423,0.0000021675532,0.006384858],"genre_scores_gemma":[0.99951416,0.000020457665,0.000010665973,0.00012285198,0.000014736571,0.00000109157,0.00003621687,0.0000016613637,0.00027814542],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99933916,0.000048236067,0.00017915858,0.000106038235,0.00016254188,0.0001648543],"domain_scores_gemma":[0.99894863,0.00079046073,0.00006914179,0.0001316477,0.000021819924,0.00003827606],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003293563,0.00007247317,0.000094691924,0.000015454627,0.00011502838,0.000008989609,0.00012511857,0.000031542688,0.000083803636],"category_scores_gemma":[0.000025708012,0.000043647477,0.0000134547645,0.0000877024,0.00006928853,0.000049659804,0.000014789849,0.00008201851,0.0000044548124],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003774687,0.000025706351,0.9416308,0.00021970562,0.000041010404,0.00001522626,0.0019757254,0.0031463169,0.031568523,0.00010343468,0.00077707926,0.02011901],"study_design_scores_gemma":[0.0001680629,0.000067005836,0.8684903,0.000034243385,0.000005351428,0.000004710804,0.00008718319,0.00046141198,0.12945218,0.00015349586,0.0010136415,0.00006242797],"about_ca_topic_score_codex":0.6185607,"about_ca_topic_score_gemma":0.8070581,"teacher_disagreement_score":0.18849742,"about_ca_system_score_codex":0.0000139671165,"about_ca_system_score_gemma":0.000066972745,"threshold_uncertainty_score":0.38397938},"labels":[],"label_agreement":null},{"id":"W2091810257","doi":"10.3402/tellusb.v66.23279","title":"Close relationship between spectral vegetation indices and V<sub>cmax</sub> in deciduous and mixed forests","year":2014,"lang":"en","type":"article","venue":"Tellus B","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Normalized Difference Vegetation Index; Deciduous; Mathematics; Eddy covariance; Atmospheric sciences; Vegetation (pathology); Geography; Leaf area index; Ecosystem; Ecology; Physics","score_opus":0.009736090258557954,"score_gpt":0.20655407569685688,"score_spread":0.19681798543829893,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2091810257","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960331,0.000123339,0.0004379684,0.000088021865,0.000053074036,0.00019007141,0.000008988921,0.000037289148,0.003028192],"genre_scores_gemma":[0.9992417,0.000042240517,0.0004902455,0.000024748499,0.000042063293,0.000008726458,0.00004983718,0.000014058482,0.000086348846],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99891675,0.00008591391,0.00024307655,0.00029756266,0.00021143469,0.00024524014],"domain_scores_gemma":[0.99940574,0.0002377029,0.00009091897,0.00015498484,0.0000035882163,0.00010709052],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003780323,0.00014279786,0.0001560242,0.00010149595,0.00012475825,0.00005491811,0.00010264061,0.00012673797,0.000012290982],"category_scores_gemma":[0.0000651652,0.00013661622,0.000023606897,0.00019844972,0.0001435565,0.00025672928,0.00008675335,0.00016210903,0.0000829792],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000870532,0.00001712836,0.9873765,0.000010060559,0.000004356543,0.0000048325996,0.0004528554,0.0008675054,0.0014302548,0.0010009905,0.000020078623,0.00880675],"study_design_scores_gemma":[0.0004434102,0.000052760355,0.9726955,0.000021405123,0.0000224369,0.000013719343,0.0000065021864,0.012291657,0.0004921967,0.013545891,0.0002411863,0.00017328352],"about_ca_topic_score_codex":0.00007004201,"about_ca_topic_score_gemma":0.0032736051,"teacher_disagreement_score":0.0146809295,"about_ca_system_score_codex":0.000073545365,"about_ca_system_score_gemma":0.000006326905,"threshold_uncertainty_score":0.55710477},"labels":[],"label_agreement":null},{"id":"W2100945747","doi":"10.3402/tellusb.v53i5.16642","title":"A comparison of large-scale atmospheric sulphate aerosol models (COSAM): overview and highlights","year":2001,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":107,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University; Environment and Climate Change Canada","funders":"","keywords":"Aerosol; Troposphere; Environmental science; Atmospheric sciences; Climatology; Northern Hemisphere; Planetary boundary layer; Climate model; Scale (ratio); Mixing (physics); Atmospheric models; Southern Hemisphere; Variance (accounting); Meteorology; Climate change; Geography; Atmosphere (unit); Geology; Oceanography","score_opus":0.0342920930516244,"score_gpt":0.2680089323101161,"score_spread":0.23371683925849168,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2100945747","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9785754,0.008775514,0.0010937533,0.00011210746,0.000095936244,0.00013265392,0.000034849334,0.000056064906,0.011123697],"genre_scores_gemma":[0.99419355,0.0014648386,0.0027475574,0.00009908788,0.00006713821,0.000001007308,0.000041677926,0.0000051787033,0.0013799345],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9988423,0.0000314622,0.00030556737,0.0002789693,0.00021091031,0.00033081774],"domain_scores_gemma":[0.9993877,0.000073665295,0.00012784089,0.00022948736,0.00002732338,0.00015399136],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00012478285,0.00017335417,0.0003568606,0.000001545502,0.00012885801,0.000028672295,0.00017997627,0.00008829127,0.0024310383],"category_scores_gemma":[0.000006162834,0.00014222621,0.00006176302,0.0002272834,0.000098561926,0.00020143847,0.000024250861,0.00010611452,0.0000674453],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026070524,0.00035807333,0.9420508,0.0003500384,0.00009205627,0.00006446708,0.0028439735,0.023573779,0.0020899535,0.00038446306,0.0027849164,0.025146779],"study_design_scores_gemma":[0.0030116793,0.0006071829,0.16205496,0.00031317532,0.0001798315,0.00015004608,0.0017043978,0.7485356,0.022318589,0.0030341514,0.056580584,0.0015098177],"about_ca_topic_score_codex":0.0005342472,"about_ca_topic_score_gemma":0.0005262165,"teacher_disagreement_score":0.77999586,"about_ca_system_score_codex":0.000003256523,"about_ca_system_score_gemma":0.000024067642,"threshold_uncertainty_score":0.99848086},"labels":[],"label_agreement":null},{"id":"W2102494754","doi":"10.3402/tellusb.v55i2.16711","title":"Spatial distribution of carbon sources and sinks in Canada’s forests","year":2003,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":190,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia; Canadian Forest Service; University of Saskatchewan; University of Toronto","funders":"University of East Anglia; National Center for Atmospheric Research","keywords":"Environmental science; Carbon sink; Sink (geography); Ecosystem; Carbon cycle; Atmospheric sciences; Physical geography; Spatial distribution; Climate change; Primary production; Remote sensing; Ecology; Geography; Geology","score_opus":0.0032535397206782885,"score_gpt":0.15872963214790947,"score_spread":0.15547609242723118,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2102494754","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963187,0.000039863717,0.0008158131,0.000017648857,0.000028452276,0.000057434234,0.0000020323628,0.0000027715791,0.0027172877],"genre_scores_gemma":[0.9996456,0.000014733494,0.00020017476,0.000017060946,0.0000027917968,0.0000013932972,0.0000029935766,0.0000041146627,0.000111161906],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99952686,0.00001711521,0.00010102048,0.000108148175,0.0001208183,0.0001260459],"domain_scores_gemma":[0.9998422,0.000011620653,0.00003332091,0.00007163761,4.3377653e-7,0.00004074547],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000049203507,0.000060213668,0.000075067444,0.000001253763,0.000018224031,0.000001815769,0.000041304622,0.000026116664,0.000114609116],"category_scores_gemma":[0.000009071356,0.000056980323,0.000007860737,0.000044952074,0.000094767136,0.000021983726,0.00003547901,0.00004670469,0.0000015375826],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000043902455,0.000012895171,0.9812422,0.0000022002619,0.0000010749594,0.0000035637383,0.00007000746,0.01462738,0.0001368497,0.000026974698,0.000013213654,0.0038592585],"study_design_scores_gemma":[0.0001612229,0.000018790955,0.9882232,0.000003080195,0.0000031993804,0.0000032328535,0.00011769301,0.010089982,0.00036802006,0.00013949834,0.00080240355,0.00006968796],"about_ca_topic_score_codex":0.9027983,"about_ca_topic_score_gemma":0.92453367,"teacher_disagreement_score":0.021735346,"about_ca_system_score_codex":0.00036020286,"about_ca_system_score_gemma":0.000024183611,"threshold_uncertainty_score":0.23235902},"labels":[],"label_agreement":null},{"id":"W2105311488","doi":"10.1111/j.1600-0889.2004.00113.x","title":"The surface CO2 gradient and pore-space storage flux in a high-porosity litter layer","year":2004,"lang":"en","type":"article","venue":"Tellus B","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"University of California, Irvine; Andrew W. Mellon Foundation; National Aeronautics and Space Administration; U.S. Department of Energy; Harvard University; National Science Foundation","keywords":"Porosity; Characterisation of pore space in soil; Flux (metallurgy); Layer (electronics); Environmental science; Materials science; Surface layer; Litter; Geology; Composite material; Biology; Ecology; Metallurgy","score_opus":0.005805004702674714,"score_gpt":0.18327573757885515,"score_spread":0.17747073287618043,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2105311488","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967178,0.000078360674,0.00017265021,0.0009194364,0.00006536575,0.00011614466,0.000007853957,0.000018646777,0.001903711],"genre_scores_gemma":[0.9973694,0.000051163726,0.00026898098,0.00009277803,0.000006938448,0.0000023813723,0.00000812267,0.0000059367603,0.0021942758],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993974,0.000023622435,0.00009645684,0.00016182417,0.0001314215,0.00018929885],"domain_scores_gemma":[0.9997326,0.00002493399,0.000028432032,0.00016071936,0.0000017391421,0.000051590803],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017951315,0.00008042839,0.00007047393,0.000009531304,0.000117398515,0.000033766337,0.00010245829,0.000041113486,0.000056482484],"category_scores_gemma":[0.000004300178,0.00005575542,0.00001549347,0.000100565805,0.00011407064,0.00007458305,0.00010361504,0.00011327194,0.00010893522],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007463124,0.0002863266,0.53128546,0.000011561345,0.000023929204,0.00027994916,0.006274756,0.43221587,0.017689107,0.007817721,0.0014739085,0.0025667981],"study_design_scores_gemma":[0.001370979,0.00010257959,0.94867694,0.000027302614,0.000019642273,0.00007921835,0.00013434225,0.016187746,0.0023188144,0.009556876,0.021062372,0.00046318333],"about_ca_topic_score_codex":0.0016443963,"about_ca_topic_score_gemma":0.0017359136,"teacher_disagreement_score":0.4173915,"about_ca_system_score_codex":0.00013896388,"about_ca_system_score_gemma":0.0000048361762,"threshold_uncertainty_score":0.24858464},"labels":[],"label_agreement":null},{"id":"W2120249458","doi":"10.1111/j.1600-0889.2010.00487.x","title":"Implications of future disturbance regimes on the carbon balance of Canada’s managed forest (2010–2100)","year":2010,"lang":"en","type":"article","venue":"Tellus B","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":85,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; Canadian Forest Service","funders":"Canadian Forest Service","keywords":"Environmental science; Sink (geography); Carbon sink; Climate change; Disturbance (geology); Ecosystem; Global change; Atmospheric sciences; Climatology; Geography; Ecology","score_opus":0.0038442420833854087,"score_gpt":0.17389939035092689,"score_spread":0.17005514826754148,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2120249458","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9478848,0.00003362728,0.000009738346,0.003747535,0.0004059576,0.00030141717,0.000022915425,0.000014374457,0.047579627],"genre_scores_gemma":[0.99785686,0.0000041574717,0.000048578975,0.00011948358,0.000070227085,0.000022061662,0.0000025500112,0.000010986319,0.0018651077],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99920416,0.00003770332,0.00016464874,0.00018155706,0.00023350208,0.00017841478],"domain_scores_gemma":[0.99890065,0.0001567158,0.00016488058,0.0007213133,0.000009045798,0.000047415288],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021020713,0.00009839816,0.0001371781,0.000011082094,0.00007102318,0.0000034397085,0.00042998669,0.00004725941,0.00017279836],"category_scores_gemma":[0.00006405255,0.00006683367,0.000030380992,0.00014310952,0.00013960419,0.000029055307,0.00006238748,0.00017410053,0.000013627659],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000054299824,0.00020557763,0.73450977,0.0001416746,0.000052613068,0.00000819771,0.0008765802,0.0010786215,0.0939729,0.01645202,0.1461043,0.0065434254],"study_design_scores_gemma":[0.000094202485,0.00003116863,0.97154844,0.000015613232,0.0000074076747,0.000003354153,0.000037638263,0.0016594471,0.0063788164,0.00022758932,0.019896403,0.0000998937],"about_ca_topic_score_codex":0.2501181,"about_ca_topic_score_gemma":0.64924014,"teacher_disagreement_score":0.39912203,"about_ca_system_score_codex":0.00007215592,"about_ca_system_score_gemma":0.00003748276,"threshold_uncertainty_score":0.7548754},"labels":[],"label_agreement":null},{"id":"W2124414449","doi":"10.1111/j.1600-0889.2006.00215.x","title":"Climate-carbon cycle feedbacks under stabilization: uncertainty and observational constraints","year":2006,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":65,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Department for Environment, Food and Rural Affairs, UK Government; University of Victoria","keywords":"Carbon cycle; Environmental science; Climate change; Greenhouse gas; Carbon sink; Carbon fibers; Carbon sequestration; Atmospheric sciences; Climatology; Atmospheric carbon cycle; Carbon dioxide; Computer science; Ecology; Ecosystem","score_opus":0.01021230683428869,"score_gpt":0.20262284047900658,"score_spread":0.19241053364471788,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2124414449","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9656484,0.00002841389,0.003947053,0.00017922248,0.000052586183,0.00011889276,0.0000047651465,0.00004556985,0.029975083],"genre_scores_gemma":[0.995132,0.00003032307,0.0038696134,0.0002730029,0.00003155902,0.000005813408,0.000026445976,0.000013297778,0.0006179423],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991321,0.000019638228,0.00016566082,0.0002462217,0.0002086175,0.00022778103],"domain_scores_gemma":[0.99972624,0.00003275878,0.00005117653,0.00012854364,0.000002258868,0.000059004597],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0000925825,0.0001212154,0.00009475812,0.0000028895354,0.000111285684,0.000019298952,0.0000782169,0.000062011495,0.0020036178],"category_scores_gemma":[0.0000041565163,0.00011591434,0.000021824475,0.00009523104,0.0005642176,0.00009283578,0.00012262068,0.00006484856,0.00006903058],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001108214,0.000077324425,0.499569,0.000004981878,0.0000039669735,0.000003112458,0.00006145041,0.49056375,0.00091495056,0.0035159974,0.000076218144,0.00519818],"study_design_scores_gemma":[0.00037944736,0.000030764295,0.8662388,0.0000057586203,0.000012624985,0.000012128604,0.00022383947,0.12423688,0.000050042956,0.007706501,0.0008745998,0.00022861388],"about_ca_topic_score_codex":0.0004942601,"about_ca_topic_score_gemma":0.00010926824,"teacher_disagreement_score":0.3666698,"about_ca_system_score_codex":0.00016784556,"about_ca_system_score_gemma":0.000004852218,"threshold_uncertainty_score":0.9989087},"labels":[],"label_agreement":null},{"id":"W2129008910","doi":"10.1034/j.1600-0889.2003.00037.x","title":"Reconciling apparent inconsistencies in estimates of terrestrial CO2 sources and sinks","year":2003,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":133,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Environmental science; Astrobiology; Atmospheric sciences; Geology; Biology","score_opus":0.012082058194411237,"score_gpt":0.2029360357849671,"score_spread":0.19085397759055586,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2129008910","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938223,0.00017297018,0.0006444836,0.000015000207,0.000053741638,0.00009131222,6.736386e-7,0.000011081847,0.005188461],"genre_scores_gemma":[0.9874811,0.000060200076,0.012279549,0.000028688031,0.000005280616,0.0000034611814,8.4705164e-7,0.000006927142,0.000133937],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99934167,0.000024965455,0.0001931037,0.00016820936,0.00011804484,0.00015399503],"domain_scores_gemma":[0.9997276,0.00006201403,0.00006121973,0.00010207985,5.3471734e-7,0.00004655654],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015046436,0.000095220246,0.00014183846,0.000005309765,0.00003939525,0.0000076153697,0.000068902016,0.000049609873,0.000289182],"category_scores_gemma":[0.000048099577,0.00008597116,0.00002168393,0.00007341338,0.00034336976,0.00006442888,0.00007178827,0.00006906094,0.000015770553],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017652723,0.00006093814,0.9543522,0.000007671971,0.0000051169054,0.000005470373,0.0008566533,0.03256134,0.0022936822,0.000047882317,0.00001683108,0.009774541],"study_design_scores_gemma":[0.0035862145,0.00052827864,0.86557645,0.0001464689,0.00008424896,0.00010341212,0.008495685,0.08759006,0.014797095,0.007982662,0.009901142,0.0012082633],"about_ca_topic_score_codex":0.0004877548,"about_ca_topic_score_gemma":0.00012682613,"teacher_disagreement_score":0.088775754,"about_ca_system_score_codex":0.00007637503,"about_ca_system_score_gemma":0.0000053546155,"threshold_uncertainty_score":0.35058022},"labels":[],"label_agreement":null},{"id":"W2145680013","doi":"10.3402/tellusb.v67.28385","title":"The first regular measurements of ozone, carbon monoxide and water vapour in the Pacific UTLS by IAGOS","year":2015,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Stratosphere; Environmental science; Ozone; Troposphere; Atmospheric sciences; Northern Hemisphere; Water vapor; Climatology; Atmosphere (unit); Extratropical cyclone; Carbon monoxide; Meteorology; Geology; Chemistry; Geography","score_opus":0.026940152772016165,"score_gpt":0.20264799633183517,"score_spread":0.175707843559819,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2145680013","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.978882,0.0028130563,0.0000038047217,0.00093052135,0.00009195891,0.00015060137,0.000005365899,0.000008925362,0.017113779],"genre_scores_gemma":[0.99931914,0.00014171672,0.000034067478,0.000087202134,0.00002392382,0.0000016343479,0.000008636454,0.0000025171498,0.0003811674],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999131,0.000076990415,0.00016411014,0.00012246124,0.00027530818,0.00023009538],"domain_scores_gemma":[0.9996304,0.00005892834,0.000040622977,0.00020121096,0.000020143803,0.000048694954],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00079884985,0.00008658977,0.00010620014,0.000004807503,0.00009057601,0.000035011224,0.00019414826,0.000037107846,0.000049892595],"category_scores_gemma":[0.000017525448,0.000038728416,0.000019008825,0.00008029957,0.00008776808,0.000052021293,0.000011521005,0.000074057476,0.000033821118],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010169302,0.000033596687,0.97208023,0.000020214386,0.000028967035,0.000013260057,0.0046874993,0.00041909568,0.0002631837,0.000006129769,0.008704019,0.013642132],"study_design_scores_gemma":[0.004666536,0.0013859819,0.556378,0.00011373766,0.00016561392,0.00009979951,0.030044038,0.023395741,0.02076925,0.0062907073,0.35534686,0.0013437043],"about_ca_topic_score_codex":0.0028891233,"about_ca_topic_score_gemma":0.0017888921,"teacher_disagreement_score":0.4157022,"about_ca_system_score_codex":0.0000033930562,"about_ca_system_score_gemma":0.0000137007755,"threshold_uncertainty_score":0.43675092},"labels":[],"label_agreement":null},{"id":"W2151615172","doi":"10.3402/tellusb.v52i2.16127","title":"Boundary layer and aerosol evolution during the 3rd Lagrangian experiment of ACE-2","year":2000,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Aerosol; Troposphere; Boundary layer; Atmospheric sciences; Environmental science; Entrainment (biomusicology); Planetary boundary layer; Lagrangian; Subsidence; Pollution; Air mass (solar energy); Meteorology; Geology; Mechanics; Physics","score_opus":0.007951730367588058,"score_gpt":0.19675353533740086,"score_spread":0.1888018049698128,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2151615172","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9869819,0.0023130726,0.000009759642,0.00012129457,0.000038075515,0.00007281361,0.000010879621,0.00001927527,0.010432901],"genre_scores_gemma":[0.9965442,0.00007706521,0.0001559437,0.00004112332,0.00007023733,7.1701055e-7,0.000006139133,0.0000017186527,0.0031028742],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9995063,0.000017168404,0.00010535287,0.000118223536,0.00011142745,0.00014152894],"domain_scores_gemma":[0.99976283,0.00002768015,0.000028585855,0.00012820012,0.0000063772786,0.000046325305],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0000653936,0.00007205405,0.00007855409,0.0000015449396,0.00017346282,0.000021606802,0.00009218454,0.000034410747,0.006705233],"category_scores_gemma":[0.0000033780598,0.00004828178,0.000027126265,0.00006762236,0.00013192375,0.000069664646,0.000006391558,0.000062100036,0.000069257025],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007311684,0.00016199843,0.40405107,0.00029559064,0.00014872746,0.00005662303,0.009183646,0.005443121,0.4380414,0.000063591906,0.0031530273,0.13867007],"study_design_scores_gemma":[0.0010073285,0.00015541726,0.71683526,0.00006782514,0.000034094377,0.00010151143,0.0013953383,0.0020679627,0.25643054,0.00018276763,0.021272918,0.00044904614],"about_ca_topic_score_codex":0.00051529414,"about_ca_topic_score_gemma":0.00006589058,"teacher_disagreement_score":0.3127842,"about_ca_system_score_codex":0.0000034737736,"about_ca_system_score_gemma":0.000015418987,"threshold_uncertainty_score":0.9942028},"labels":[],"label_agreement":null},{"id":"W2153383208","doi":"10.1111/j.1600-0889.2010.00468.x","title":"Novel design of an enclosed CO<sub>2</sub>/H<sub>2</sub>O gas analyser for eddy covariance flux measurements","year":2010,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"University of British Columbia; Università degli Studi della Tuscia; Florida International University","keywords":"Eddy covariance; Gas analyzer; Path (computing); Analyser; Path length; Field (mathematics); Flux (metallurgy); Physics; Environmental science; Analytical Chemistry (journal); Optics; Computer science; Chemistry; Mathematics","score_opus":0.02631294811948155,"score_gpt":0.23435525631719661,"score_spread":0.20804230819771508,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2153383208","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7563117,0.00019805874,0.23695093,0.0001272872,0.00081749895,0.002158493,0.00015202472,0.00022902875,0.0030549827],"genre_scores_gemma":[0.88399714,0.00022307073,0.11254785,0.0005908695,0.0003244958,0.00023931178,0.00022664285,0.0002677401,0.0015829033],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.992032,0.00026706635,0.0015498305,0.0019861008,0.0022815461,0.0018834594],"domain_scores_gemma":[0.99573255,0.00027818486,0.00095777836,0.002023373,0.00008466653,0.00092345534],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0020958895,0.0012563766,0.0012777131,0.00008355014,0.00072286295,0.00014891548,0.0019130997,0.0007566565,0.0017979721],"category_scores_gemma":[0.0002106751,0.001258521,0.0005213492,0.00088180485,0.0014052531,0.0009836482,0.00060238893,0.00073866814,0.0010288898],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043598143,0.0013481632,0.0034083615,0.000068551286,0.00022413558,0.00002574535,0.00050749804,0.06570942,0.9122366,0.00014422846,0.002102984,0.013788369],"study_design_scores_gemma":[0.010473665,0.0023581889,0.062217366,0.00022532296,0.001224378,0.0001685247,0.0003004861,0.28857768,0.5998416,0.0020720314,0.027704697,0.0048360825],"about_ca_topic_score_codex":0.00017612946,"about_ca_topic_score_gemma":0.00066682394,"teacher_disagreement_score":0.312395,"about_ca_system_score_codex":0.00091852294,"about_ca_system_score_gemma":0.00014668268,"threshold_uncertainty_score":0.99974895},"labels":[],"label_agreement":null},{"id":"W2155393798","doi":"10.1034/j.1600-0889.2003.00068.x","title":"Effects of diapycnal and isopycnal mixing on the ventilation of CFCs in the North Atlantic in an isopycnic coordinate OGCM","year":2003,"lang":"en","type":"article","venue":"Tellus B","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Bjerknessenteret for klimaforskning, Universitetet i Bergen; Norges Forskningsråd","keywords":"Isopycnal; Isopycnic; Mixing (physics); Ocean general circulation model; Environmental science; Geology; Climatology; Chemistry; Oceanography; General Circulation Model; Climate change; Chromatography; Physics","score_opus":0.008433249097376815,"score_gpt":0.19052470810363242,"score_spread":0.18209145900625562,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155393798","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983994,0.0008039385,0.000040699917,0.000035531026,0.000036382273,0.00015164194,0.0000022032677,0.0000038588564,0.0005263436],"genre_scores_gemma":[0.9997343,0.00011347424,0.00005616486,0.00007138994,0.000010404911,6.880171e-7,0.000005661571,0.0000016667111,0.000006262655],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992982,0.00014829429,0.0001620968,0.00011133804,0.00014581643,0.00013421816],"domain_scores_gemma":[0.99935454,0.00043919656,0.000080516664,0.00009450461,0.000011447409,0.000019797637],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034924148,0.00007621724,0.00012117254,0.000025685204,0.000049468897,0.000012013317,0.0001341618,0.0000279826,0.000048093574],"category_scores_gemma":[0.00006530445,0.00004267227,0.00002182637,0.0004143062,0.00010222295,0.00008659326,0.0000037212847,0.000107336346,0.000002249916],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000316542,0.000036126712,0.99611455,0.000060175378,0.0000033658625,0.000006741367,0.0005885986,0.0005021147,0.000030361887,0.00021762929,0.000007663243,0.0024010432],"study_design_scores_gemma":[0.00019495022,0.00017627125,0.9960761,0.00005125435,0.000008633675,0.0000032471596,0.00025467956,0.0023060057,0.00029953723,0.000535894,0.000039458853,0.000053940315],"about_ca_topic_score_codex":0.0003719814,"about_ca_topic_score_gemma":0.0016273373,"teacher_disagreement_score":0.0023471029,"about_ca_system_score_codex":0.0000010649989,"about_ca_system_score_gemma":0.000020066309,"threshold_uncertainty_score":0.17401247},"labels":[],"label_agreement":null},{"id":"W2155580250","doi":"10.1111/j.1600-0889.2009.00420.x","title":"Reply to L. Kutzbach","year":2009,"lang":"en","type":"article","venue":"Tellus B","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Science North","funders":"","keywords":"Forcing (mathematics); Environmental science; Thermodynamics; Balance (ability); Flux (metallurgy); Atmospheric sciences; Heat flux; Function (biology); Climatology; Meteorology; Physics; Mathematics; Chemistry; Geology; Heat transfer; Psychology","score_opus":0.03828267986943486,"score_gpt":0.24961265094253415,"score_spread":0.2113299710730993,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155580250","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.78043115,0.0004304029,0.00002729465,0.007856843,0.0003439797,0.0001398013,0.0002920945,0.00009384154,0.21038458],"genre_scores_gemma":[0.973807,0.0000414849,0.00016536828,0.022969067,0.00029571992,1.916381e-7,0.0003006212,0.0000015244901,0.0024190487],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9994671,0.000010404931,0.000082075676,0.00013981166,0.00010308568,0.0001975346],"domain_scores_gemma":[0.99967325,0.000026387877,0.000012987356,0.0001547916,0.000011100652,0.000121477984],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000091683185,0.000063109976,0.000073439885,0.000038588096,0.00006462617,0.000032139236,0.000114160735,0.000021920876,0.014855991],"category_scores_gemma":[0.000013152302,0.000051613802,0.000024930874,0.00014152793,0.000009185924,0.000056951623,0.000003279675,0.00004742889,0.005385225],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008391611,0.000031521136,0.32881668,0.000008284451,0.000005705097,0.000091946575,0.0020266545,0.00027444426,0.0011673187,0.00010174329,0.23878421,0.42860758],"study_design_scores_gemma":[0.000078826255,0.0001813822,0.60118026,0.0000061419505,0.0000030229216,0.000014960376,0.00006012549,0.0003149491,0.00023031545,0.0003981151,0.39741167,0.00012025401],"about_ca_topic_score_codex":0.0018239511,"about_ca_topic_score_gemma":0.0014579613,"teacher_disagreement_score":0.4284873,"about_ca_system_score_codex":0.0000015836871,"about_ca_system_score_gemma":0.0000071888844,"threshold_uncertainty_score":0.9953892},"labels":[],"label_agreement":null},{"id":"W2157661631","doi":"10.3402/tellusb.v52i4.17089","title":"Very low ozone episodes due to polar vortex displacement","year":2000,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Bundesministerium für Bildung und Forschung; National Aeronautics and Space Administration","keywords":"Stratosphere; Polar vortex; Troposphere; Ozone; Atmospheric sciences; Vortex; Advection; Northern Hemisphere; Baroclinity; Environmental science; Ozone layer; Climatology; Ozone depletion; Atmosphere (unit); Geology; Meteorology; Physics","score_opus":0.006841072530938565,"score_gpt":0.20145648265903252,"score_spread":0.19461541012809394,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2157661631","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9482167,0.0005190696,0.00018564911,0.00038450464,0.00017326599,0.00014394682,0.00004694998,0.000069971815,0.05025998],"genre_scores_gemma":[0.98565584,0.0001417465,0.0009294065,0.0011853266,0.00014264409,0.0000013423322,0.000055465945,0.0000053205895,0.011882917],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99893826,0.000033059787,0.00017949122,0.00024327985,0.00022036047,0.00038551897],"domain_scores_gemma":[0.99949193,0.00004508613,0.000024825993,0.00023076992,0.00001023113,0.00019717234],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0001439041,0.00013824347,0.00017091991,0.000009410348,0.00014309892,0.000046673857,0.00018374324,0.000046502886,0.06731145],"category_scores_gemma":[0.000007897661,0.000113446185,0.000051547508,0.0001940898,0.00003820853,0.000127021,0.000009266729,0.00008221052,0.015675237],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029302985,0.00013630856,0.25873938,0.00004708887,0.00006209217,0.0002777725,0.0010041123,0.0097131925,0.00016467238,0.00007285975,0.011983206,0.7175063],"study_design_scores_gemma":[0.00044765344,0.0004126309,0.85326827,0.00003919838,0.000033085897,0.0000465852,0.00024369697,0.0062946235,0.00033004466,0.00044838927,0.13792074,0.0005150755],"about_ca_topic_score_codex":0.0029216022,"about_ca_topic_score_gemma":0.00095437496,"teacher_disagreement_score":0.7169912,"about_ca_system_score_codex":0.0000056670306,"about_ca_system_score_gemma":0.000022956643,"threshold_uncertainty_score":0.98509115},"labels":[],"label_agreement":null},{"id":"W2159982266","doi":"10.1111/j.1600-0889.2008.00376.x","title":"Ocean ventilation as a driver of interannual variability in atmospheric potential oxygen","year":2008,"lang":"en","type":"article","venue":"Tellus B","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Drawdown (hydrology); Environmental science; Climatology; Southern Hemisphere; Oceanography; Atmospheric sciences; Northern Hemisphere; Biosphere; Geology","score_opus":0.006037789748900766,"score_gpt":0.1798285518317091,"score_spread":0.17379076208280833,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2159982266","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9805995,0.000032637883,0.0002154564,0.000014173152,0.00017735624,0.00010225138,0.000012514083,0.000014729637,0.018831357],"genre_scores_gemma":[0.99908066,0.000010770509,0.00013806176,0.000022170054,0.00004716131,1.18722475e-7,0.000035879246,0.0000016074071,0.0006635872],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993088,0.000075182455,0.00020924144,0.00013922715,0.00014236408,0.00012515819],"domain_scores_gemma":[0.9997306,0.000033392003,0.00005690896,0.00011476824,0.000023507047,0.00004080986],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00022601981,0.00006490418,0.00012516169,0.000013192186,0.000033562595,0.000005874744,0.00010037513,0.00003851743,0.0034169245],"category_scores_gemma":[0.000025834353,0.00005799133,0.000043542594,0.00016199473,0.000037158352,0.000115294126,0.000015201788,0.000064515545,0.00014436149],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013015587,0.00004775023,0.969221,0.000029883831,0.000010121264,0.00004886704,0.0007897208,0.003952253,0.000042288735,0.000023158042,0.0002607484,0.025444059],"study_design_scores_gemma":[0.00024316492,0.00010861984,0.9511854,0.00000997274,0.000004829619,0.00003625812,0.00007928171,0.04606669,0.00008170821,0.00037755928,0.0017176124,0.000088879904],"about_ca_topic_score_codex":0.008931799,"about_ca_topic_score_gemma":0.0012718732,"teacher_disagreement_score":0.042114437,"about_ca_system_score_codex":0.000003820029,"about_ca_system_score_gemma":0.000038945018,"threshold_uncertainty_score":0.9976678},"labels":[],"label_agreement":null},{"id":"W2160107081","doi":"10.1111/j.1600-0889.2010.00459.x","title":"Spatially simulating changes of soil water content and their effects on carbon sequestration in Canada’s forests and wetlands","year":2010,"lang":"en","type":"article","venue":"Tellus B","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Queen's University; University of British Columbia; University of Toronto","funders":"","keywords":"Wetland; Carbon sequestration; Environmental science; Soil water; Primary production; Ecosystem; Soil carbon; Carbon cycle; Deposition (geology); Climate change; Disturbance (geology); Hydrology (agriculture); Atmospheric sciences; Ecology; Soil science; Carbon dioxide; Geology; Biology","score_opus":0.009657433920959817,"score_gpt":0.19022355308594197,"score_spread":0.18056611916498214,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2160107081","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99818444,0.000005810233,0.000002731108,0.00024906587,0.00006809161,0.000115480165,0.0000019212548,0.0000042936513,0.0013681735],"genre_scores_gemma":[0.9998337,0.0000069906605,0.000011524375,0.00007972536,0.000025877021,0.0000048318047,0.000006646203,0.000004569506,0.000026122705],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99954104,0.00002159009,0.00008995239,0.00013209635,0.00006610215,0.0001492032],"domain_scores_gemma":[0.9997705,0.000081983046,0.00003004003,0.00007157569,0.000002663395,0.000043192817],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011562902,0.00007838163,0.000120397104,0.000018894323,0.000026165835,0.000005599487,0.000036311976,0.000042861964,0.000022194063],"category_scores_gemma":[0.000015548085,0.000049086866,0.000005504314,0.000016987375,0.000039700695,0.000020824275,0.000044714885,0.000082942825,4.5190188e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019199659,0.0000078045605,0.88967407,0.000012007772,0.0000022797597,0.00000760751,0.00039186564,0.0002401829,0.09947954,0.000008008495,0.0000041439584,0.010153319],"study_design_scores_gemma":[0.0004414348,0.0001900431,0.90169835,0.000012089314,0.0000027451645,0.0000037009665,0.000020011168,0.0151769165,0.08222385,0.00011630133,0.000039565508,0.0000750123],"about_ca_topic_score_codex":0.55989313,"about_ca_topic_score_gemma":0.9945237,"teacher_disagreement_score":0.43463063,"about_ca_system_score_codex":0.000040919844,"about_ca_system_score_gemma":0.000017950091,"threshold_uncertainty_score":0.4430376},"labels":[],"label_agreement":null},{"id":"W2161626957","doi":"10.3402/tellusb.v56i3.16424","title":"On the CO<sub>2</sub> exchange between the atmosphere and the biosphere: the role of synoptic and mesoscale processes","year":2004,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"Canadian Foundation for Climate and Atmospheric Sciences; National Institute of Advanced Industrial Science and Technology","keywords":"Mesoscale meteorology; Troposphere; Atmosphere (unit); Atmospheric sciences; Biosphere; Environmental science; Climatology; Biosphere model; Planetary boundary layer; Eddy covariance; Boundary layer; Meteorology; Geology; Geography; Physics","score_opus":0.004555320539848523,"score_gpt":0.17581548080319917,"score_spread":0.17126016026335064,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2161626957","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98280525,0.003330598,0.00025536644,0.0026619318,0.00003311721,0.0007583286,0.000010288609,0.00003030257,0.010114793],"genre_scores_gemma":[0.99683183,0.0017740618,0.00020058978,0.0005948434,0.000052932355,0.000058863057,0.000002259698,0.000033204138,0.00045141278],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99841094,0.00012411995,0.0002635642,0.00035706052,0.00047965327,0.0003646812],"domain_scores_gemma":[0.99859613,0.00058383937,0.00017504203,0.00055622705,0.000005539939,0.00008324765],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00054104574,0.00028565692,0.0002523027,0.0000011900806,0.00060361077,0.000060268252,0.00060323224,0.000100285484,0.000358534],"category_scores_gemma":[0.00006208318,0.00011970458,0.00006754672,0.00025768194,0.0026741708,0.000106712,0.0003403833,0.00025343688,0.000101140446],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014459575,0.0017002498,0.2725341,0.0006247285,0.0012939022,0.00005162011,0.061891794,0.13399573,0.030700218,0.0378864,0.00802635,0.44984895],"study_design_scores_gemma":[0.010876909,0.0023689049,0.6371805,0.0005486722,0.0016769554,0.00024332546,0.021071784,0.026754271,0.04580665,0.12644461,0.12367567,0.0033517214],"about_ca_topic_score_codex":0.00025742367,"about_ca_topic_score_gemma":0.00019965188,"teacher_disagreement_score":0.44649723,"about_ca_system_score_codex":0.00009644484,"about_ca_system_score_gemma":0.000015643198,"threshold_uncertainty_score":0.9853094},"labels":[],"label_agreement":null},{"id":"W2168807835","doi":"10.3402/tellusb.v53i5.16643","title":"Vertical distributions of sulfur species simulated by large scale atmospheric models in COSAM: Comparison with observations","year":2001,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"","keywords":"Environmental science; Scale (ratio); Atmospheric sciences; Climatology; Atmospheric models; Meteorology; Geography; Geology; Atmosphere (unit)","score_opus":0.02644539499741727,"score_gpt":0.2230008338404952,"score_spread":0.19655543884307794,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2168807835","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9827489,0.00024795934,0.01229033,0.00014318377,0.000025872654,0.00011026495,0.00022187395,0.000036984737,0.0041746073],"genre_scores_gemma":[0.9973331,0.000033910135,0.0011904301,0.000034346423,0.000018138118,7.15867e-7,0.0005895763,0.0000031301977,0.00079663075],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99905264,0.0000240113,0.00026443502,0.0001840727,0.00018189181,0.00029296847],"domain_scores_gemma":[0.9995447,0.000110203415,0.000044709435,0.00016596947,0.00003838331,0.00009603794],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00007468863,0.00011857361,0.00021979708,0.0000014764573,0.00010010773,0.000019345665,0.00014754504,0.00006636219,0.0016861468],"category_scores_gemma":[0.000017707065,0.000097502074,0.000032618507,0.00051901804,0.00012778418,0.0001594618,0.000010563511,0.00013134882,0.000023647062],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007322337,0.00016401865,0.8736476,0.00000963523,0.000010367097,0.000007538793,0.00018046897,0.12375124,0.00092643173,0.00006584501,0.0009905156,0.00017312684],"study_design_scores_gemma":[0.0008164418,0.00010267266,0.47438926,0.000036162917,0.000022170212,0.000006733284,0.00059712894,0.51590574,0.002834474,0.00025700248,0.004794895,0.00023732231],"about_ca_topic_score_codex":0.0008220219,"about_ca_topic_score_gemma":0.0014933054,"teacher_disagreement_score":0.39925835,"about_ca_system_score_codex":0.00000998564,"about_ca_system_score_gemma":0.00004103155,"threshold_uncertainty_score":0.99922645},"labels":[],"label_agreement":null},{"id":"W2254181589","doi":"10.3402/tellusb.v68.26206","title":"Factors controlling stable isotope composition of precipitation in arid conditions: an observation network in the Tianshan Mountains, central Asia","year":2016,"lang":"en","type":"article","venue":"Tellus B","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":103,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Science North","funders":"National Key Research and Development Program of China; National Natural Science Foundation of China; Northwest Normal University","keywords":"Precipitation; Arid; δ18O; Meteoric water; Environmental science; Stable isotope ratio; Atmospheric sciences; Evaporation; Climatology; Physical geography; Geology; Geography; Meteorology","score_opus":0.026771143877147394,"score_gpt":0.2262175599464089,"score_spread":0.1994464160692615,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2254181589","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980765,0.00008709771,0.0006022267,0.00014469655,0.000103595645,0.0002549457,0.00007327699,0.000011948201,0.0006457323],"genre_scores_gemma":[0.99894917,0.000017330163,0.00010854003,0.000063971886,0.0000647475,0.0000033820818,0.0007523595,0.0000020892294,0.000038417485],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99909294,0.00013043321,0.00024299898,0.00013796435,0.00015630203,0.00023938267],"domain_scores_gemma":[0.99958205,0.00016346002,0.00007716707,0.00011959151,0.000025218118,0.000032539203],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032786434,0.00008645277,0.00012256976,0.00003814749,0.00006351833,0.000037569785,0.00014906036,0.00005152876,0.00029852687],"category_scores_gemma":[0.000015366875,0.00005142081,0.000023559489,0.00016263234,0.000039082825,0.00042061834,0.0000030820677,0.00006980322,0.0000073467427],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000043775515,0.000029308516,0.9896701,0.000010251522,0.0000036544513,0.0000014711885,0.00075350836,0.005794449,0.0024913193,0.000135724,0.00004868026,0.001017781],"study_design_scores_gemma":[0.00045995417,0.00006868369,0.98902005,0.000053664622,0.0000054323677,0.0000010357357,0.0006882827,0.005815281,0.0017764058,0.0018748258,0.00015494724,0.00008142825],"about_ca_topic_score_codex":0.0020431662,"about_ca_topic_score_gemma":0.0035626623,"teacher_disagreement_score":0.0017391018,"about_ca_system_score_codex":0.00001474299,"about_ca_system_score_gemma":0.000024979261,"threshold_uncertainty_score":0.32686597},"labels":[],"label_agreement":null},{"id":"W2806520244","doi":"10.1080/16000889.2018.1468704","title":"The impact of future atmospheric circulation changes over the Euro-Atlantic sector on urban PM<sub>2.5</sub> concentrations","year":2018,"lang":"en","type":"article","venue":"Tellus B","topic":"Air Quality and Health Impacts","field":"Environmental Science","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Stockholms Universitet; Vetenskapsrådet; Universiteit van Amsterdam","keywords":"Environmental science; Air quality index; Context (archaeology); Downscaling; Climatology; Atmospheric circulation; Atmospheric sciences; Representative Concentration Pathways; North Atlantic oscillation; Climate change; Current (fluid); Climate model; Geography; Meteorology; Oceanography; Geology","score_opus":0.02483977653538384,"score_gpt":0.27770401128254124,"score_spread":0.2528642347471574,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2806520244","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99238294,0.00023774835,0.00014557723,0.0030952012,0.00035582375,0.0005073318,0.000026107928,0.000048411697,0.0032008593],"genre_scores_gemma":[0.9974781,0.00022315636,0.000037528658,0.0012283737,0.0008257362,0.00001051744,0.000013036066,0.000019688521,0.00016380612],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99838793,0.00020798219,0.00026015722,0.0002466191,0.00043376387,0.00046355044],"domain_scores_gemma":[0.99886805,0.0002349453,0.00023144505,0.00048439356,0.000023300114,0.00015787962],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00049139804,0.00018706171,0.00016779281,0.0000068494332,0.0006866885,0.00005291546,0.00029652097,0.00010520081,0.0012404147],"category_scores_gemma":[0.000083973035,0.00010572522,0.000090602174,0.00036610413,0.00047156995,0.00012706671,0.00006682248,0.00017905212,0.00042280534],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005564119,0.00064662995,0.17075801,0.00009402392,0.00020858498,0.000010252385,0.035912924,0.0050472547,0.095405854,0.0053027202,0.6401975,0.045859817],"study_design_scores_gemma":[0.00032808806,0.00053703395,0.9413214,0.0000258721,0.000025767635,0.0000059326767,0.00014288595,0.010222308,0.0013991597,0.00021817438,0.04558449,0.00018890927],"about_ca_topic_score_codex":0.00038759114,"about_ca_topic_score_gemma":0.0011374801,"teacher_disagreement_score":0.77056336,"about_ca_system_score_codex":0.00026370987,"about_ca_system_score_gemma":0.00006228317,"threshold_uncertainty_score":0.9996726},"labels":[],"label_agreement":null},{"id":"W2911387626","doi":"10.1080/16000889.2018.1565030","title":"Methane budget estimates in Finland from the CarbonTracker Europe-CH<sub>4</sub> data assimilation system","year":2019,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Rijksinstituut voor Volksgezondheid en Milieu; Natural Environment Research Council; Università degli Studi di Urbino Carlo Bo; Umweltbundesamt; Environment and Climate Change Canada; Vetenskapsrådet; Lunds Universitet; Chinese Academy of Meteorological Sciences; Eidgenössische Materialprüfungs- und Forschungsanstalt; Horizon 2020 Framework Programme; Commonwealth Scientific and Industrial Research Organisation; Academy of Finland; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; Rijksuniversiteit Groningen; National Oceanic and Atmospheric Administration; University of Bristol; Sight Research UK; National Institute of Water and Atmospheric Research; National Science Foundation","keywords":"Data assimilation; Environmental science; Methane; Assimilation (phonology); Atmospheric sciences; Animal science; Meteorology; Chemistry; Geography; Physics; Biology","score_opus":0.01045533214271886,"score_gpt":0.20122388580598713,"score_spread":0.19076855366326828,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2911387626","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9878761,0.0003335817,0.0023429377,0.00020661956,0.000313464,0.00047652575,0.000083307845,0.00006674543,0.008300729],"genre_scores_gemma":[0.99469906,0.00013695273,0.0038363195,0.0002207427,0.00007443663,0.000011267723,0.00025104076,0.000048532496,0.0007216546],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979397,0.00013156203,0.0003661066,0.0006641828,0.00048549962,0.00041294604],"domain_scores_gemma":[0.99832773,0.00025067662,0.00015856192,0.001156833,0.0000034955126,0.00010270464],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004970618,0.00028261123,0.0002954758,0.000007091343,0.00009043203,0.000052436153,0.00084370316,0.00012718832,0.0006335285],"category_scores_gemma":[0.000050307855,0.00020878026,0.000043177177,0.00024919308,0.00018444397,0.0003333655,0.0008021421,0.00023254791,0.002627031],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011728327,0.00018465637,0.78211945,0.0000355453,0.00007041308,0.00008163089,0.00093436183,0.14729327,0.051486302,0.00009829734,0.0035883498,0.013990442],"study_design_scores_gemma":[0.00058362813,0.000042740656,0.59115607,0.00004941091,0.000057711546,0.00001192345,0.00013347348,0.39896905,0.0005742647,0.000073396935,0.008005773,0.00034257123],"about_ca_topic_score_codex":0.0007987551,"about_ca_topic_score_gemma":0.00043950096,"teacher_disagreement_score":0.25167578,"about_ca_system_score_codex":0.0002874701,"about_ca_system_score_gemma":0.000012946736,"threshold_uncertainty_score":0.9981495},"labels":[],"label_agreement":null},{"id":"W2990777673","doi":"10.3402/tellusb.v62i5.16588","title":"Net ecosystem productivity of temperate and boreal forests after clearcutting–a Fluxnet-Canada measurement and modelling synthesis","year":2010,"lang":"en","type":"article","venue":"Tellus B","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université Laval; Canadian Forest Service; Queen's University; University of British Columbia; University of Alberta","funders":"","keywords":"Clearcutting; FluxNet; Taiga; Temperate rainforest; Environmental science; Boreal; Boreal ecosystem; Temperate climate; Productivity; Ecosystem; Primary production; Temperate forest; Forest ecology; Agroforestry; Ecology; Forestry; Geography; Eddy covariance","score_opus":0.007541604398298358,"score_gpt":0.1607475545784764,"score_spread":0.15320595018017805,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2990777673","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998679,0.00002633449,0.00022763952,0.0000561013,0.000051278817,0.00012971881,0.000027305745,0.000008938388,0.000793671],"genre_scores_gemma":[0.9993925,0.000009083668,0.00050807575,0.000006905861,0.000015925052,0.0000103128405,0.0000015429525,0.000007719743,0.000047913938],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99926025,0.000025728175,0.0001319314,0.00020136946,0.00024032866,0.00014040398],"domain_scores_gemma":[0.99971455,0.000020098676,0.000045863057,0.00014469167,0.000009291179,0.00006553011],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003293366,0.00008653308,0.00010908637,0.000014590607,0.000056850375,0.000017718132,0.000055270673,0.00003826007,0.00003081369],"category_scores_gemma":[0.000013947227,0.000072853916,0.000010900365,0.000044659526,0.000055750595,0.00008034771,0.00006601849,0.00009426228,0.000002115699],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007557516,0.0000719659,0.92703855,0.00011171096,0.000041280735,0.000016494676,0.0005054967,0.03282294,0.021677427,0.0001207696,0.00011494026,0.017402869],"study_design_scores_gemma":[0.00018040025,0.00003334889,0.32491073,0.000047784073,0.000045684938,0.000050293685,0.000025677697,0.6652291,0.0076991357,0.00028457172,0.0012075444,0.00028577357],"about_ca_topic_score_codex":0.04713592,"about_ca_topic_score_gemma":0.3821195,"teacher_disagreement_score":0.6324061,"about_ca_system_score_codex":0.000044353998,"about_ca_system_score_gemma":0.000019784706,"threshold_uncertainty_score":0.95920926},"labels":[],"label_agreement":null},{"id":"W3047715967","doi":"10.1080/16000889.2020.1803708","title":"Aerosol carbonaceous, elemental and ionic composition variability and origin at the Siberian High Arctic, Cape Baranova","year":2020,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Aerosol; Arctic; The arctic; Environmental science; Atmospheric sciences; Sulfate; Ionic bonding; Cape; Environmental chemistry; Geology; Oceanography; Chemistry; Meteorology; Geography; Ion","score_opus":0.010795637063995485,"score_gpt":0.19490388505243605,"score_spread":0.18410824798844058,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3047715967","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958715,0.00023492727,0.000027505213,0.0020928418,0.00007070467,0.0001658179,0.00010807004,0.000029382514,0.0013992451],"genre_scores_gemma":[0.9984247,0.000052119707,0.00024046702,0.0008601379,0.00012953712,0.0000010851332,0.00016103774,0.000002721759,0.00012816204],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992513,0.000054118544,0.00013443653,0.0002612272,0.00012400986,0.00017489128],"domain_scores_gemma":[0.99956745,0.00012900459,0.000042584354,0.000117887976,0.000010009755,0.00013307252],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00013077138,0.00011620899,0.00012333001,9.617952e-7,0.00024474403,0.000047756377,0.00008489697,0.00004451559,0.0036146573],"category_scores_gemma":[0.000014346092,0.00008277079,0.000020439893,0.00007423459,0.00018361758,0.00006449341,0.000031430027,0.00011362948,0.000035478035],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00067491183,0.000074097465,0.915618,0.00035195652,0.00013688639,0.00007841423,0.0026076129,0.0021495428,0.06216578,0.00024467675,0.00208602,0.013812091],"study_design_scores_gemma":[0.0051852525,0.0011353418,0.83950907,0.00009965902,0.00036021168,0.00060901063,0.0013448856,0.057648987,0.06315502,0.0012654928,0.027610043,0.0020770577],"about_ca_topic_score_codex":0.0012833368,"about_ca_topic_score_gemma":0.00039750847,"teacher_disagreement_score":0.07610896,"about_ca_system_score_codex":0.000008492505,"about_ca_system_score_gemma":0.00001995082,"threshold_uncertainty_score":0.99729615},"labels":[],"label_agreement":null},{"id":"W4233700562","doi":"10.3402/tellusb.v52i2.16121","title":"Evolution of the aerosol, cloud and boundary-layer dynamic and thermodynamic characteristics during the 2nd Lagrangian experiment of ACE-2","year":2000,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Aerosol; Drizzle; Atmospheric sciences; Troposphere; Boundary layer; Entrainment (biomusicology); Environmental science; Marine stratocumulus; Cloud condensation nuclei; Planetary boundary layer; Plume; Sea salt aerosol; Meteorology; Geology; Mechanics; Physics; Sea salt","score_opus":0.003401744712314909,"score_gpt":0.1917465425276673,"score_spread":0.18834479781535238,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4233700562","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99774593,0.00051834795,0.000060314018,0.00011579448,0.00006201256,0.00019034708,0.0000088762445,0.0000091720885,0.0012891898],"genre_scores_gemma":[0.9986286,0.00015001885,0.000079873935,0.000029116623,0.000016451037,0.0000053076105,6.1797635e-7,0.000010810484,0.0010792081],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99928427,0.000040889376,0.00017810392,0.00016422993,0.00017698659,0.00015550027],"domain_scores_gemma":[0.999585,0.000018662085,0.00009372893,0.00026552513,0.0000037061936,0.000033403063],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000099736746,0.000108301436,0.00012651012,8.520257e-7,0.00019726419,0.000013490827,0.00016534106,0.00004650958,0.000956371],"category_scores_gemma":[0.0000040698324,0.00006373698,0.000036754405,0.00009036686,0.0006028112,0.000048900307,0.00012903936,0.00008125967,0.00000904803],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013057336,0.0001480831,0.1147027,0.000056316472,0.000038717615,0.0000022722222,0.0062564756,0.00025644747,0.8569467,0.00013098825,0.00006978311,0.02126092],"study_design_scores_gemma":[0.00028767675,0.000053277294,0.9873278,0.000024366356,0.000023904544,0.000013742907,0.00041265806,0.0069864746,0.004151773,0.00009836283,0.0005004956,0.000119441174],"about_ca_topic_score_codex":0.00032757065,"about_ca_topic_score_gemma":0.00008919594,"teacher_disagreement_score":0.8726251,"about_ca_system_score_codex":0.00008545286,"about_ca_system_score_gemma":0.000007894159,"threshold_uncertainty_score":0.9999569},"labels":[],"label_agreement":null},{"id":"W4235423054","doi":"10.3402/tellusb.v55i2.16728","title":"TransCom 3 CO<sub>2</sub> inversion intercomparison: 1. Annual mean control results and sensitivity to transport and prior flux information","year":2003,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":82,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Environmental science; Sensitivity (control systems); Inversion (geology); Flux (metallurgy); Atmospheric sciences; Meteorology; Chemistry; Physics; Geology","score_opus":0.004267087328958788,"score_gpt":0.18169020079427387,"score_spread":0.17742311346531509,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4235423054","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96702534,0.000032900956,0.027504249,0.00018212594,0.000076729586,0.0004832551,0.00006898135,0.000054803844,0.004571643],"genre_scores_gemma":[0.9966563,0.00007108535,0.0023821902,0.00060829247,0.000013628989,0.0000066521106,0.000031829466,0.000015437667,0.00021459852],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9984965,0.000096449876,0.00037588828,0.0003500511,0.0003415951,0.0003395351],"domain_scores_gemma":[0.9993397,0.000056039455,0.00009596913,0.00021483409,0.0000057567486,0.00028771014],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00048256494,0.00025612136,0.00028228987,0.000016312468,0.0001900988,0.000028038332,0.00007636585,0.00012858477,0.00009730675],"category_scores_gemma":[0.000018813333,0.00024580996,0.000052087405,0.00013082034,0.0002924473,0.00061103626,0.000041939627,0.00016236771,0.00019218933],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0041394094,0.0009414564,0.19811332,0.00020762748,0.00020685789,0.00021479533,0.07944993,0.10490105,0.15484148,0.0004278815,0.0110893,0.44546688],"study_design_scores_gemma":[0.0088577,0.0010481864,0.765647,0.000087917666,0.00019040024,0.00019900598,0.0024949717,0.070951656,0.011190026,0.00010729978,0.13769029,0.0015355714],"about_ca_topic_score_codex":0.00010149168,"about_ca_topic_score_gemma":0.00029256698,"teacher_disagreement_score":0.5675337,"about_ca_system_score_codex":0.00016817635,"about_ca_system_score_gemma":0.000008543597,"threshold_uncertainty_score":0.9999994},"labels":[],"label_agreement":null},{"id":"W4242037180","doi":"10.3402/tellusb.v54i5.16679","title":"Carbon balance of a southern taiga spruce stand in European Russia","year":2002,"lang":"en","type":"article","venue":"Tellus B","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Eddy covariance; Taiga; Ecosystem respiration; Environmental science; Atmospheric sciences; Flux (metallurgy); Ecosystem; Boreal ecosystem; Atmosphere (unit); Boreal; Productivity; Canopy; Soil respiration; Carbon cycle; Photosynthesis; Primary production; Ecology; Soil water; Geography; Soil science; Botany; Chemistry; Meteorology; Biology; Physics","score_opus":0.0074477405294550375,"score_gpt":0.16654791897833118,"score_spread":0.15910017844887614,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4242037180","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8229607,0.000071460345,0.00002825683,0.000028271019,0.000021235857,0.000048270234,0.000016098618,0.000013443204,0.1768123],"genre_scores_gemma":[0.99626863,0.000031224376,0.00012082312,0.000016781241,0.0000076579845,8.6443936e-7,0.0000019501942,0.000008358328,0.0035437362],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9994551,0.000037312333,0.00013550061,0.00012233025,0.000120854354,0.00012892301],"domain_scores_gemma":[0.9997722,0.000008992321,0.000043100517,0.00014348916,0.0000011815675,0.000031024],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000113200855,0.00006324122,0.0000782309,0.000021485466,0.000014265057,0.0000056480353,0.00011571012,0.0000220517,0.00063945825],"category_scores_gemma":[0.0000043384953,0.000055282966,0.000018021052,0.000102190104,0.00005667613,0.000027616887,0.000052409756,0.00007021053,0.00039861907],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001875506,0.0002076886,0.9428099,0.000018580215,0.0000103130715,0.00012525269,0.0063472455,0.019598152,0.018997358,0.00011748981,0.0002556667,0.0114936],"study_design_scores_gemma":[0.0014892251,0.00012812961,0.20856689,0.00011265681,0.000024396817,0.00004084557,0.00022425038,0.77056134,0.001086034,0.0007513115,0.016362432,0.0006525076],"about_ca_topic_score_codex":0.00026014246,"about_ca_topic_score_gemma":0.0001178938,"teacher_disagreement_score":0.75096315,"about_ca_system_score_codex":0.000040818704,"about_ca_system_score_gemma":0.0000011755054,"threshold_uncertainty_score":0.70016193},"labels":[],"label_agreement":null},{"id":"W4244848189","doi":"10.1111/j.1600-0889.2005.00144.x","title":"Importance of submicron surface-active organic aerosols for pristine Arctic clouds","year":2005,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Aerosol; Arctic; Cloud condensation nuclei; Dimethyl sulfide; Environmental science; Atmospheric sciences; Population; The arctic; Phytoplankton; Oceanography; Meteorology; Chemistry; Geology; Nutrient; Geography; Sulfur","score_opus":0.013650673416318503,"score_gpt":0.21847598255335823,"score_spread":0.20482530913703972,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4244848189","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958544,0.00043045796,0.00039449448,0.00016179353,0.00008491492,0.00022211633,0.00010100202,0.00003567521,0.0027151634],"genre_scores_gemma":[0.9925071,0.000031801585,0.0054234457,0.000095396,0.00018298795,9.41703e-7,0.00009876146,0.0000058372384,0.0016537572],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99911714,0.000012013758,0.0002522851,0.00022867716,0.00012087887,0.00026903208],"domain_scores_gemma":[0.9993608,0.00014423436,0.00015684118,0.00020111355,0.00005207552,0.00008492224],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00013150173,0.00013213672,0.00020587159,0.0000018474697,0.00007800487,0.000012515448,0.0001795729,0.000059206144,0.0041583832],"category_scores_gemma":[0.00006373088,0.000116787,0.00006488006,0.00013252466,0.00009144949,0.00009898594,0.00000903846,0.000092460745,0.00008480099],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000693233,0.00018372036,0.7590331,0.000393566,0.00012107645,0.000011639915,0.0009440801,0.0057872217,0.19754563,0.00005307671,0.002429869,0.0328038],"study_design_scores_gemma":[0.0017651556,0.00045395424,0.2985147,0.00008638799,0.000089391775,0.00005268273,0.0003242828,0.0061702966,0.67388576,0.00052735815,0.017318191,0.0008118553],"about_ca_topic_score_codex":0.00014490176,"about_ca_topic_score_gemma":0.00036555523,"teacher_disagreement_score":0.47634012,"about_ca_system_score_codex":0.00001082192,"about_ca_system_score_gemma":0.000057479425,"threshold_uncertainty_score":0.99675196},"labels":[],"label_agreement":null},{"id":"W4247950990","doi":"10.1111/j.1600-0889.2005.00159.x","title":"Analysis of atmospheric CO2 growth rates at Mauna Loa using CO2 fluxes derived from an inverse model","year":2005,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":45,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Resources Canada","keywords":"Environmental science; Atmospheric sciences; Inverse; Climatology; Physics; Geology; Mathematics","score_opus":0.012569396851437705,"score_gpt":0.2256724134482321,"score_spread":0.2131030165967944,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4247950990","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9625298,0.00005389225,0.03633565,0.00003532803,0.000026702033,0.00011503313,0.00002124794,0.0000434266,0.00083896867],"genre_scores_gemma":[0.8752878,0.000073948235,0.12338035,0.00030662867,0.000020501151,0.0000032535206,0.000046713478,0.000028825336,0.00085203344],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99846655,0.000051588482,0.0003349239,0.00046314823,0.00034804203,0.00033571932],"domain_scores_gemma":[0.9991805,0.000034504596,0.00017813212,0.00041446724,0.0000048872666,0.00018749588],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00008454879,0.00025115247,0.00038863975,0.0000060698644,0.00014851453,0.000015592857,0.0003157907,0.00011410745,0.00447473],"category_scores_gemma":[0.0000075573257,0.00024306319,0.00015983073,0.0005352999,0.00044218428,0.00034528345,0.00033365656,0.00009351338,0.00017047951],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000028843033,0.000108899796,0.22663113,0.0000017653664,0.00012014405,0.0000029502844,0.0005889274,0.74270874,0.028989822,0.0000034099048,0.00004061688,0.00077474944],"study_design_scores_gemma":[0.00025382335,0.000028788238,0.07805089,0.0000032135863,0.00046337125,0.000001162142,0.00020439683,0.9179124,0.002671002,0.00010062672,0.000055998396,0.00025428098],"about_ca_topic_score_codex":0.0032186038,"about_ca_topic_score_gemma":0.0012911032,"teacher_disagreement_score":0.17520371,"about_ca_system_score_codex":0.00058346434,"about_ca_system_score_gemma":0.0000090613885,"threshold_uncertainty_score":0.99643534},"labels":[],"label_agreement":null},{"id":"W4256197680","doi":"10.3402/tellusb.v55i2.16712","title":"Reconciling apparent inconsistencies in estimates of terrestrial CO<sub>2</sub> sources and sinks","year":2003,"lang":"en","type":"article","venue":"Tellus B","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Environmental science; Carbon sink; Extratropical cyclone; Carbon cycle; Primary production; Atmospheric sciences; Biosphere; Tropics; Terrestrial ecosystem; Land use, land-use change and forestry; Sink (geography); Inversion (geology); Climatology; Land use; Climate change; Geography; Ecosystem; Geology; Ecology","score_opus":0.011870137831275163,"score_gpt":0.20485319609330707,"score_spread":0.1929830582620319,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4256197680","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99232715,0.0004452438,0.0007963835,0.000024682355,0.00011007526,0.00021530944,0.0000038754856,0.00002971231,0.006047549],"genre_scores_gemma":[0.9926828,0.00026928572,0.006813471,0.000053639033,0.000017812623,0.000010709763,0.0000048849015,0.00002025868,0.00012712031],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99854547,0.000062112245,0.00040221884,0.0003647539,0.00028586676,0.00033958815],"domain_scores_gemma":[0.99938816,0.00012633964,0.00014935691,0.0002213808,0.0000018461042,0.000112921545],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031990444,0.00022362135,0.00030362717,0.000014510087,0.000101649064,0.00002276161,0.00015985164,0.00012236,0.00027924465],"category_scores_gemma":[0.00008805878,0.00020913003,0.000056796613,0.00014458055,0.000659517,0.00013581874,0.00013565457,0.00014062566,0.000053741216],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010512803,0.0003021166,0.8013564,0.00004520617,0.00003455295,0.0000343863,0.0024584327,0.05965505,0.09871829,0.00013217403,0.00018793972,0.03697033],"study_design_scores_gemma":[0.0075069107,0.0012595338,0.67730755,0.0004099921,0.00026241087,0.0002547431,0.0059107705,0.13384587,0.13587143,0.007149612,0.027019706,0.00320147],"about_ca_topic_score_codex":0.00018628196,"about_ca_topic_score_gemma":0.000254505,"teacher_disagreement_score":0.124048844,"about_ca_system_score_codex":0.00018916313,"about_ca_system_score_gemma":0.000015390371,"threshold_uncertainty_score":0.8528075},"labels":[],"label_agreement":null},{"id":"W4297835458","doi":"10.3402/tellusb.v56i4.16449","title":"The surface CO<sub>2</sub> gradient and pore-space storage flux in a high-porosity litter layer","year":2004,"lang":"en","type":"article","venue":"Tellus B","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Atmospheric sciences; Flux (metallurgy); Wind speed; Shear velocity; Environmental science; Surface layer; Mixed layer; Turbulence; Eddy covariance; Laminar flow; Meteorology; Chemistry; Geology; Mechanics; Physics; Layer (electronics); Ecosystem","score_opus":0.0058576086803147735,"score_gpt":0.1851470409889282,"score_spread":0.17928943230861344,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4297835458","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955116,0.0002136927,0.00025465337,0.0008153407,0.000121823214,0.0002599537,0.000032108463,0.000044848108,0.002745994],"genre_scores_gemma":[0.99786663,0.00020846531,0.00022916624,0.00013998088,0.000018896115,0.0000073237015,0.000031444255,0.000016959,0.0014811442],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99868476,0.000060791277,0.00021332224,0.00034409863,0.0003048673,0.0003921655],"domain_scores_gemma":[0.99941856,0.00005438927,0.00007420598,0.0003277597,0.0000053454187,0.00011974716],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037800265,0.00018683671,0.00016290722,0.000027680331,0.0002306141,0.0000747622,0.00021607839,0.000101110345,0.0000709942],"category_scores_gemma":[0.000010155251,0.00013936183,0.00004146904,0.00019837209,0.00022517302,0.00015181101,0.00017348476,0.00021106232,0.00026080513],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022781796,0.0008006476,0.2622935,0.000043525873,0.000085752545,0.0007054656,0.0094212135,0.30979726,0.3946327,0.009596485,0.0061617475,0.0062339287],"study_design_scores_gemma":[0.0033202672,0.00029362863,0.87235457,0.00009318944,0.0000739062,0.00021083449,0.00014296915,0.0287553,0.029096188,0.008995114,0.05525809,0.0014059374],"about_ca_topic_score_codex":0.0005019057,"about_ca_topic_score_gemma":0.002274033,"teacher_disagreement_score":0.6100611,"about_ca_system_score_codex":0.00028737495,"about_ca_system_score_gemma":0.000013533207,"threshold_uncertainty_score":0.5683011},"labels":[],"label_agreement":null}]}