{"meta":{"query_hash":"2dae2b24004d","filters":{"topic":"Atmospheric aerosols and clouds"},"cohort_total":1467,"direct_labels_cover":1,"predictions_cover":1467,"exported":1467,"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/2dae2b24004d","api":"https://metacan.xera.ac/api/v1/cohort?topic=Atmospheric+aerosols+and+clouds"},"results":[{"id":"W1063783487","doi":"10.1016/j.jastp.2015.08.001","title":"Wave like signatures in aerosol optical depth and associated radiative impacts over the central Himalayan region","year":2015,"lang":"en","type":"article","venue":"Journal of Atmospheric and Solar-Terrestrial Physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institut National de la Recherche Scientifique","funders":"","keywords":"Radiative transfer; Aerosol; Remote sensing; Environmental science; Atmospheric sciences; Geology; Geography; Meteorology; Physics; Optics","score_opus":0.019008035995472412,"score_gpt":0.23231269701336715,"score_spread":0.21330466101789475,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1063783487","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":[0.9968941,0.0004144971,0.0013903013,0.00023458787,0.0003862334,0.00017810917,0.000001020658,0.00000776668,0.0004933355],"genre_scores_gemma":[0.9979838,0.00027003593,0.0009510262,0.00028115648,0.00043201906,0.0000016817471,9.879484e-7,0.000019219351,0.000060044746],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983426,0.00017213708,0.00041129108,0.00020300563,0.00046141987,0.00040955542],"domain_scores_gemma":[0.9989294,0.00015386875,0.00042216983,0.0001238144,0.000017933326,0.0003528383],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036999487,0.00022794664,0.0003834756,4.5653928e-7,0.00011232164,0.00010749995,0.0001664627,0.00015285908,0.000020353067],"category_scores_gemma":[0.00015855052,0.00014727336,0.00010610853,0.00022705947,0.0003205912,0.00044042518,0.0001352559,0.00051740167,0.0000016391808],"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":[0.0016142093,0.00066345796,0.92198956,0.000009173013,0.00022763749,0.00038864283,0.008427993,0.017615905,0.00085450104,0.00014969085,0.0146205705,0.03343866],"study_design_scores_gemma":[0.005122598,0.0011812892,0.9675836,0.00007212218,0.00012082165,0.000060078044,0.0012557062,0.021762757,0.00010443131,0.0016918718,0.00065697765,0.00038773578],"about_ca_topic_score_codex":0.0002987642,"about_ca_topic_score_gemma":0.00010692112,"teacher_disagreement_score":0.04559405,"about_ca_system_score_codex":0.00023795727,"about_ca_system_score_gemma":0.00008958718,"threshold_uncertainty_score":0.60056335},"labels":[],"label_agreement":null},{"id":"W13057458","doi":"10.1016/b978-0-12-382225-3.00203-6","title":"LIDAR | Atmospheric Sounding Introduction","year":2014,"lang":"en","type":"book-chapter","venue":"Encyclopedia of Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Depth sounding; Lidar; Remote sensing; Atmospheric sounding; Environmental science; Meteorology; Geology; Geography; Cartography","score_opus":0.007826389873704195,"score_gpt":0.21215703564795083,"score_spread":0.20433064577424664,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W13057458","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.013884769,0.0007548748,0.008580581,0.00032956456,0.0022102834,0.00043478177,0.000005154707,0.00015503021,0.973645],"genre_scores_gemma":[0.013430698,0.0019011473,0.08134834,0.00022309522,0.0017009949,0.000026366733,0.000009339909,0.00012633983,0.9012337],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99524426,0.00005589571,0.00096676615,0.0014193936,0.00156216,0.00075152266],"domain_scores_gemma":[0.9976685,0.00016544128,0.0010688418,0.0007873222,0.000041863746,0.00026805446],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00087744516,0.000753098,0.0009022904,0.0000011056537,0.0005191812,0.00007932281,0.0012988471,0.00045034804,0.038284704],"category_scores_gemma":[0.00010479656,0.00065982796,0.00034415166,0.00048392644,0.002508508,0.0003233974,0.00042340666,0.00048293354,0.0015571996],"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":[0.00013948092,0.0002927885,0.031619344,0.00029979157,0.0003408288,0.00006088357,0.0023282703,0.04118733,0.0003969501,0.0642491,0.19598722,0.663098],"study_design_scores_gemma":[0.0002299351,0.00056712,0.0011490458,0.00007984826,0.00012432726,0.000026352742,0.00014034426,0.0025102796,0.00002513547,0.007403628,0.9867331,0.0010109058],"about_ca_topic_score_codex":0.00023754164,"about_ca_topic_score_gemma":0.000049353745,"teacher_disagreement_score":0.79074585,"about_ca_system_score_codex":0.00029803722,"about_ca_system_score_gemma":0.00012947459,"threshold_uncertainty_score":0.9995853},"labels":[],"label_agreement":null},{"id":"W1486613422","doi":"10.1007/s00376-002-0040-x","title":"Analysis of the aerosol extinction characteristics in different areas of China","year":2002,"lang":"en","type":"article","venue":"Advances in Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":28,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Angstrom exponent; Aerosol; Angstrom; Sun photometer; Environmental science; Arid; Atmospheric sciences; Beijing; Extinction (optical mineralogy); Spring (device); Climatology; Meteorology; China; Geography; Geology; Physics; Mineralogy; Chemistry","score_opus":0.007877782813733799,"score_gpt":0.22731524547531765,"score_spread":0.21943746266158384,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1486613422","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":[0.9931815,0.0004971851,0.00040471935,0.00007810355,0.00018748145,0.00012728362,0.0000021800986,0.0000067178175,0.005514778],"genre_scores_gemma":[0.9981382,0.0005228813,0.0011060728,0.000034698358,0.000010340483,0.000012382111,4.1781632e-7,0.0000042676115,0.00017075645],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99839634,0.00007057195,0.00047243063,0.00032251544,0.00048576487,0.00025235745],"domain_scores_gemma":[0.99926454,0.000077276076,0.000352923,0.00026526564,0.0000059823155,0.000034014425],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00023809365,0.00014026533,0.00035660752,0.0000020445839,0.00010019582,0.0000130643175,0.000542387,0.00004201671,0.002176391],"category_scores_gemma":[0.00007752603,0.000086556225,0.00010829674,0.0033393044,0.0011392502,0.00028723554,0.00016049987,0.00009465396,0.0000048113984],"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":[0.000004447635,0.00013619872,0.94473135,0.000004825829,0.0000070523133,5.695537e-7,0.0005025346,0.030675815,0.00036272703,0.000029774945,0.0000051679194,0.023539558],"study_design_scores_gemma":[0.00011285782,0.000060568997,0.9011026,0.000020675589,0.00003072876,5.1612375e-7,0.00024044405,0.09777421,0.0002823276,0.00010929987,0.00016848615,0.000097296856],"about_ca_topic_score_codex":0.00031914614,"about_ca_topic_score_gemma":0.00089991913,"teacher_disagreement_score":0.067098394,"about_ca_system_score_codex":0.00008586081,"about_ca_system_score_gemma":0.0000065325175,"threshold_uncertainty_score":0.9987357},"labels":[],"label_agreement":null},{"id":"W1499106070","doi":"10.2172/947993","title":"Atmospheric Properties from the 2006 Niamey Deployment and Climate Simulation with a Geodesic Grid Coupled Climate Model Fourth Quarter 2008","year":2008,"lang":"en","type":"report","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Milestone; Environmental science; Meteorology; Aerosol; Quarter (Canadian coin); Climate model; Climatology; Software deployment; Computer science; Climate change; Geography; Geology; Cartography","score_opus":0.0212388407251042,"score_gpt":0.22309034757174545,"score_spread":0.20185150684664124,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1499106070","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":[0.9612376,0.0025096713,0.018577732,0.00039723702,0.00034928258,0.0021196809,0.0001725949,0.00032235085,0.014313818],"genre_scores_gemma":[0.96274155,0.016234862,0.014026319,0.00083436904,0.0003564043,0.00026564958,0.0001415803,0.00020559222,0.0051936414],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99615145,0.00006901869,0.00063849817,0.00094902085,0.0013825722,0.0008094338],"domain_scores_gemma":[0.99849635,0.000079489386,0.00047593148,0.00071243173,0.000056198474,0.00017959524],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00032880311,0.000687738,0.00063915795,9.0911345e-7,0.0006172116,0.00013217142,0.00033972913,0.00028268754,0.0010320981],"category_scores_gemma":[0.000015434056,0.0003717246,0.00012967798,0.00018099704,0.0005068195,0.00026461837,0.00034916162,0.0003733796,0.00016980915],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021103871,0.00013661348,0.16279942,0.00004976581,0.000119122094,0.00003221603,0.000638526,0.8109238,0.000064951026,0.0000017876564,0.022815052,0.002207665],"study_design_scores_gemma":[0.0006073948,0.00019416159,0.037373696,0.00012978307,0.0002008554,0.000039793304,0.00018985699,0.9538436,0.000007669387,0.000012826921,0.00667141,0.00072896783],"about_ca_topic_score_codex":0.008911802,"about_ca_topic_score_gemma":0.0031879733,"teacher_disagreement_score":0.14291975,"about_ca_system_score_codex":0.00040053556,"about_ca_system_score_gemma":0.00016381835,"threshold_uncertainty_score":0.9998811},"labels":[],"label_agreement":null},{"id":"W1502160970","doi":"10.2172/942122","title":"Final report for the project \"Improving the understanding of surface-atmosphere radiative interactions by mapping surface reflectance over the ARM CART site\" (award DE-FG02-02ER63351)","year":2008,"lang":"en","type":"report","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Research Canada; Natural Resources Canada","funders":"","keywords":"Albedo (alchemy); Environmental science; Shortwave; Radiative forcing; Earth's energy budget; Radiative transfer; Shortwave radiation; Climate model; Cloud forcing; Atmosphere (unit); Climatology; Climate change; Meteorology; Sky; Atmospheric sciences; Geography; Radiation; Geology; Physics","score_opus":0.07304089190583346,"score_gpt":0.30947646566411113,"score_spread":0.23643557375827767,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1502160970","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.36627212,0.005142765,0.38130996,0.0035720812,0.0034477059,0.00821987,0.00037920338,0.00028407568,0.2313722],"genre_scores_gemma":[0.876218,0.0032747374,0.006693022,0.00031422998,0.00038445846,0.00022294433,0.00008861318,0.0001737886,0.11263018],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99595505,0.00018745258,0.00096692867,0.00086028135,0.0012586216,0.0007716933],"domain_scores_gemma":[0.9958299,0.0014181442,0.0014771511,0.0010970494,0.000094960094,0.00008279676],"candidate_categories":["metaepi_narrow","sts"],"consensus_categories":[],"category_scores_codex":[0.0018576649,0.0005800526,0.000613519,0.0000015131426,0.0015503528,0.00012243161,0.000836505,0.00026769418,0.0008620538],"category_scores_gemma":[0.0003290784,0.0003006339,0.00050170947,0.00061613723,0.00085003866,0.0002399181,0.00039578142,0.00096552307,0.000011804838],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014823458,0.00027618662,0.054951333,0.00021765404,0.00091169716,0.000090414236,0.009233225,0.0576772,0.0071347533,0.00013959759,0.8666427,0.0025769663],"study_design_scores_gemma":[0.00087273127,0.0003612622,0.009479145,0.00032609885,0.0006498559,0.0018064444,0.027825085,0.07766272,0.00089228514,0.00024213528,0.878417,0.0014652051],"about_ca_topic_score_codex":0.015187415,"about_ca_topic_score_gemma":0.0030875832,"teacher_disagreement_score":0.50994587,"about_ca_system_score_codex":0.00305247,"about_ca_system_score_gemma":0.0009035059,"threshold_uncertainty_score":0.99994457},"labels":[],"label_agreement":null},{"id":"W1507035314","doi":"10.1016/j.atmosenv.2015.05.062","title":"Modelling aerosol–cloud–meteorology interaction: A case study with a fully coupled air quality model (GEM-MACH)","year":2015,"lang":"en","type":"article","venue":"Atmospheric Environment","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":113,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"National Research Council Canada","keywords":"Aerosol; Liquid water content; Environmental science; Atmospheric sciences; Sea salt aerosol; Cloud computing; Meteorology; Air quality index; Cloud condensation nuclei; Plume; Cloud physics; Physics","score_opus":0.03429265675186558,"score_gpt":0.26078844055557215,"score_spread":0.22649578380370658,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1507035314","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":[0.7641578,0.00007695858,0.2327418,0.00016228322,0.00014823324,0.00078359345,0.0000027612884,0.0001106081,0.0018159857],"genre_scores_gemma":[0.9446096,0.000027733751,0.052645307,0.0005098839,0.00009008123,0.00026963695,0.0000059614677,0.000084188345,0.0017576192],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9961512,0.0002513528,0.00071982166,0.0011534365,0.0009605465,0.000763618],"domain_scores_gemma":[0.9979435,0.000077440585,0.0003634405,0.0010329451,0.000014755445,0.00056788005],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007136997,0.0005872701,0.0005974858,7.838735e-7,0.0003300199,0.00004662763,0.00041407425,0.00016813962,0.0015781084],"category_scores_gemma":[0.000013483815,0.000488951,0.00012630566,0.0002628422,0.00040796187,0.00037512786,0.000534399,0.00042759007,0.00066263444],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032392325,0.0011247396,0.04410224,0.0000049756386,0.00008922812,0.00085509906,0.0031007554,0.9492006,0.00006350328,0.000015740456,0.00034610025,0.00077313464],"study_design_scores_gemma":[0.0023643742,0.0017739323,0.0007022615,0.0000066595485,0.00014287894,0.00077459496,0.0125642335,0.97941726,0.000014696711,0.00010096753,0.001413757,0.0007243679],"about_ca_topic_score_codex":0.0073583587,"about_ca_topic_score_gemma":0.00048380336,"teacher_disagreement_score":0.18045181,"about_ca_system_score_codex":0.0008918637,"about_ca_system_score_gemma":0.000049558337,"threshold_uncertainty_score":0.9997562},"labels":[],"label_agreement":null},{"id":"W1521995834","doi":"10.1029/2007jd009052","title":"Coarse mode optical information retrievable using ultraviolet to short‐wave infrared Sun photometry: Application to United Arab Emirates Unified Aerosol Experiment data","year":2008,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":43,"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 de Sherbrooke","funders":"","keywords":"AERONET; Aerosol; Angstrom exponent; Photometry (optics); Effective radius; Environmental science; Remote sensing; Mode (computer interface); Homogeneity (statistics); Physics; Atmospheric sciences; Astrophysics; Meteorology; Mathematics; Geology; Computer science; Statistics","score_opus":0.07266388381937626,"score_gpt":0.34933889149033437,"score_spread":0.2766750076709581,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1521995834","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":[0.9689877,0.000020587368,0.028961321,0.00023050322,0.00006153614,0.0006528965,0.000025007921,0.000022195687,0.0010382389],"genre_scores_gemma":[0.95595235,0.000044185887,0.04316424,0.0002813111,0.00016837419,0.00002357452,0.00003598297,0.000026953792,0.00030300536],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9956442,0.00017502383,0.00078948936,0.00040354158,0.0022155491,0.0007722117],"domain_scores_gemma":[0.9973997,0.00030342984,0.00018723481,0.00087160704,0.00033369614,0.000904338],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00092204503,0.000259173,0.00042775288,0.000014903505,0.00042624597,0.00014846284,0.0011317173,0.0001426172,0.00032348698],"category_scores_gemma":[0.0009374393,0.00021767222,0.000092010334,0.0025622612,0.00034869922,0.0012143209,0.00092591596,0.00068986136,0.00020521536],"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":[0.0043119574,0.0021773563,0.011944807,0.00005638082,0.0002185035,0.0002150131,0.004202416,0.07047294,0.8080588,0.000552136,0.06543592,0.032353785],"study_design_scores_gemma":[0.0037390834,0.0067814584,0.060606964,0.0004064349,0.00012382449,0.0002969629,0.007657925,0.5641697,0.30461138,0.0020277763,0.047441304,0.0021371783],"about_ca_topic_score_codex":0.0016942938,"about_ca_topic_score_gemma":0.00002827846,"teacher_disagreement_score":0.5034474,"about_ca_system_score_codex":0.00060347567,"about_ca_system_score_gemma":0.00019091327,"threshold_uncertainty_score":0.88764155},"labels":[],"label_agreement":null},{"id":"W1536258309","doi":"10.1029/2003gl017192","title":"Sensitivity study of the spectral dispersion of the cloud droplet size distribution on the indirect aerosol effect","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":133,"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":"Cloud albedo; Aerosol; Atmospheric sciences; Dispersion (optics); Albedo (alchemy); Liquid water content; Environmental science; Scaling; Atmosphere (unit); Cloud computing; Meteorology; Computational physics; Cloud cover; Physics; Optics; Mathematics","score_opus":0.013683548602339089,"score_gpt":0.25839411950570806,"score_spread":0.24471057090336898,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1536258309","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":[0.9958065,0.0000017686673,0.000016864542,0.0026769785,0.00012314999,0.0008885262,0.000011356576,0.0000067470105,0.00046811238],"genre_scores_gemma":[0.99958265,0.0000010531155,0.0000033238184,0.00021795396,0.000053771444,0.000022740462,6.9584996e-7,0.000009857066,0.0001079556],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99516857,0.0024941883,0.00016287371,0.00029789945,0.0014532001,0.00042325494],"domain_scores_gemma":[0.9975233,0.0016315891,0.000087131564,0.00068359316,0.000014163987,0.000060189373],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013794668,0.00014241312,0.00019290375,8.168867e-7,0.00048418937,0.000020491087,0.0004446443,0.00003953139,0.000116906114],"category_scores_gemma":[0.00092695066,0.000061745144,0.00017751448,0.0006945004,0.0010169835,0.00004347024,0.00037759406,0.0006072218,0.000051784362],"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":[0.00022822057,0.001377143,0.20912626,0.000016536756,0.000058216952,0.000009796834,0.0013194295,0.00082200253,0.77728766,0.0006973024,0.008139194,0.00091825204],"study_design_scores_gemma":[0.00040895055,0.0006017253,0.87136257,0.000024667612,0.000018045088,0.0000011187135,0.00043989348,0.00017570559,0.12661181,0.00009975066,0.00015677985,0.000098994686],"about_ca_topic_score_codex":0.0013047265,"about_ca_topic_score_gemma":0.000097315016,"teacher_disagreement_score":0.6622363,"about_ca_system_score_codex":0.00018428975,"about_ca_system_score_gemma":0.000016747263,"threshold_uncertainty_score":0.3747118},"labels":[],"label_agreement":null},{"id":"W1547225839","doi":"10.3390/rs70607157","title":"Seasonal Variations of the Relative Optical Air Mass Function for Background Aerosol and Thin Cirrus Clouds at Arctic and Antarctic Sites","year":2015,"lang":"en","type":"article","venue":"Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":15,"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":"Agenzia Nazionale per le Nuove Tecnologie, l'Energia e lo Sviluppo Economico Sostenibile","keywords":"Lidar; Cirrus; Aerosol; Environmental science; Atmospheric sciences; Arctic; Troposphere; Air mass (solar energy); Climatology; Remote sensing; Meteorology; Geology; Geography; Oceanography; Physics","score_opus":0.023576864612794884,"score_gpt":0.23555925687427332,"score_spread":0.21198239226147844,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1547225839","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":[0.93566465,0.000065911336,0.062379215,0.00063376594,0.000117075106,0.00021131507,0.0000031740246,0.000012928792,0.00091197185],"genre_scores_gemma":[0.95485747,0.000008685052,0.044517204,0.00016488844,0.000046373367,6.68645e-8,0.0000025153274,0.0000120187715,0.00039079724],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99918413,0.000057774876,0.00014682641,0.00022770434,0.00021150694,0.00017203049],"domain_scores_gemma":[0.99944884,0.00019049077,0.00009168775,0.00014338637,0.000025147507,0.00010047456],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023964913,0.00010798372,0.00012807974,0.0000011954668,0.00023601233,0.000018727616,0.000041406784,0.000072185176,0.000019489276],"category_scores_gemma":[0.000116707684,0.00008087638,0.00004167089,0.000119291544,0.0002884051,0.00014625156,0.00013469392,0.00010060695,0.0000067868045],"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":[0.0020642595,0.00027442462,0.29472375,0.00042024275,0.00066114654,0.000027194277,0.019517938,0.022751674,0.5276778,0.0108084,0.0022797384,0.11879349],"study_design_scores_gemma":[0.0015564648,0.00046278935,0.17121956,0.000107009095,0.0003092537,0.00015523264,0.001118338,0.8008379,0.0019893954,0.021268196,0.00057112135,0.00040474397],"about_ca_topic_score_codex":0.0001717436,"about_ca_topic_score_gemma":0.00008376703,"teacher_disagreement_score":0.77808625,"about_ca_system_score_codex":0.00018290931,"about_ca_system_score_gemma":0.000016832799,"threshold_uncertainty_score":0.3298043},"labels":[],"label_agreement":null},{"id":"W1549328980","doi":"10.1029/2012jd017753","title":"Analytical estimation of droplet concentration at cloud base","year":2012,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":72,"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":"Supersaturation; Mixing (physics); Base (topology); Cloud base; Spectral line; Mixing ratio; Cloud physics; Cloud computing; Statistical physics; Mechanics; Physics; Computational physics; Materials science; Thermodynamics; Mathematics; Mathematical analysis; Computer science","score_opus":0.029942909580154657,"score_gpt":0.32297578078749006,"score_spread":0.2930328712073354,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1549328980","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":[0.9938235,0.00013077201,0.0019816891,0.0003003635,0.00013588252,0.00011166688,0.0000020848754,0.0000051945194,0.0035088444],"genre_scores_gemma":[0.9950445,0.0000366415,0.0036309178,0.000037274527,0.00039352276,0.0000024153765,0.0000015305166,0.000013069498,0.00084011955],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9970688,0.0002552742,0.00048392575,0.00013524394,0.0015229355,0.0005338241],"domain_scores_gemma":[0.9985936,0.00041042588,0.00025813188,0.00020433911,0.000103472354,0.00042999652],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011549063,0.00011877235,0.00028064405,0.000001145174,0.00014476274,0.000024061575,0.00028332102,0.000076541386,0.004223306],"category_scores_gemma":[0.0005689973,0.00008836399,0.00015824802,0.0004284938,0.00056268007,0.00045197282,0.0002213415,0.00037697208,0.00034867026],"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":[0.0014795876,0.0030527983,0.75212246,0.000087100285,0.00019039321,0.00006617006,0.0019300473,0.017002454,0.05034638,0.008667377,0.09451285,0.070542395],"study_design_scores_gemma":[0.0016805382,0.0021684635,0.8354882,0.00010936213,0.00009582663,0.000060640443,0.00072095153,0.124057926,0.021583105,0.003793529,0.009847573,0.00039390812],"about_ca_topic_score_codex":0.00026537804,"about_ca_topic_score_gemma":0.000012867963,"teacher_disagreement_score":0.10705548,"about_ca_system_score_codex":0.00034483994,"about_ca_system_score_gemma":0.000053829306,"threshold_uncertainty_score":0.996687},"labels":[],"label_agreement":null},{"id":"W1551625515","doi":"10.2172/947999","title":"Science Overview Document Indirect and Semi-Direct Aerosol Campaign (ISDAC) April 2008","year":2007,"lang":"en","type":"report","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":5,"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; Cloud condensation nuclei; Environmental science; Liquid water content; Effective radius; Cloud computing; Meteorology; Atmospheric sciences; Cloud physics; Nephelometer; Drizzle; Geography; Physics; Precipitation; Scattering; Light scattering; Computer science; Optics","score_opus":0.026939969361679774,"score_gpt":0.2869666254922121,"score_spread":0.26002665613053233,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1551625515","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.123443455,0.011071062,0.00019611699,0.0001079572,0.00077946985,0.00082995376,0.000012956538,0.00018920015,0.8633698],"genre_scores_gemma":[0.6018592,0.09546491,0.010923025,0.0021323464,0.0006464009,0.00012122905,0.000029379862,0.00021686363,0.28860664],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9946461,0.00005024978,0.0006089163,0.0014086552,0.0023296343,0.0009564772],"domain_scores_gemma":[0.9982639,0.00009873213,0.00035521036,0.0006741618,0.00004784697,0.0005601773],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.002704617,0.0006045795,0.00074355124,0.000014439312,0.0005226735,0.00020046145,0.00054139935,0.0003633374,0.0065353196],"category_scores_gemma":[0.00014365712,0.00047875065,0.000115744486,0.0009947389,0.001757297,0.0003450226,0.0013128648,0.00044930377,0.000253476],"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":[0.000054563174,0.00041297686,0.30088416,0.0008106979,0.00020257814,0.00038744896,0.0018133455,0.00015316982,0.003585466,0.00025364527,0.3357052,0.35573676],"study_design_scores_gemma":[0.0005481002,0.00043923134,0.097378924,0.00044986568,0.00023108235,0.00059610663,0.00035084388,0.00016250623,0.0031013114,0.00017863228,0.89417183,0.0023915723],"about_ca_topic_score_codex":0.004307546,"about_ca_topic_score_gemma":0.00052186585,"teacher_disagreement_score":0.5747632,"about_ca_system_score_codex":0.0010575147,"about_ca_system_score_gemma":0.0005159571,"threshold_uncertainty_score":0.9997664},"labels":[],"label_agreement":null},{"id":"W1559090159","doi":"10.1002/2015jd023156","title":"Observed relations between snowfall microphysics and triple‐frequency radar measurements","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":216,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Academy of Finland","keywords":"Snowflake; Snow; Scattering; Radar; Atmospheric sciences; Particle (ecology); Meteorology; Environmental science; Geology; Physics; Remote sensing; Optics; Aerospace engineering","score_opus":0.1336609848661858,"score_gpt":0.32793996193398794,"score_spread":0.19427897706780214,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1559090159","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":[0.9921609,0.00042972606,0.0007559068,0.00073528534,0.00010834069,0.00019157764,0.0000038712333,0.000012068431,0.005602298],"genre_scores_gemma":[0.982661,0.00003672574,0.014932759,0.000042346972,0.00041801346,0.0000047127874,0.0000015863234,0.000027288937,0.0018755475],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99622023,0.00040358878,0.0005319163,0.00027665988,0.0020053864,0.0005622432],"domain_scores_gemma":[0.99816394,0.00028153838,0.00025421532,0.00027787816,0.00027736588,0.0007450754],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015344227,0.00019148692,0.00038357254,0.0000022417728,0.00025611324,0.0001033108,0.0005266662,0.00010423455,0.00034767448],"category_scores_gemma":[0.00072571664,0.00014900733,0.00014141694,0.00061045605,0.000577208,0.0005184763,0.000324753,0.00077081856,0.00034081837],"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":[0.00022940311,0.0005453052,0.9041136,0.000018424169,0.00018071024,0.000076366836,0.00087648566,0.00017349582,0.0306954,0.0004111016,0.03778784,0.024891885],"study_design_scores_gemma":[0.0022661574,0.0019386136,0.94124424,0.000082994695,0.00007549527,0.000016243366,0.0006900826,0.00022067553,0.0016467941,0.041031606,0.010418857,0.00036822687],"about_ca_topic_score_codex":0.0013256094,"about_ca_topic_score_gemma":0.000072671675,"teacher_disagreement_score":0.040620506,"about_ca_system_score_codex":0.0003985856,"about_ca_system_score_gemma":0.00019922802,"threshold_uncertainty_score":0.6076343},"labels":[],"label_agreement":null},{"id":"W1561569801","doi":"10.1029/2012jd018575","title":"Diagnosis of regime‐dependent cloud simulation errors in CMIP5 models using “A‐Train” satellite observations and reanalysis data","year":2012,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":96,"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; Troposphere; Cloud fraction; Climate model; Scale (ratio); Cloud computing; Cloud top; Satellite; Cloud height; Meteorology; Coupled model intercomparison project; Atmospheric sciences; Climatology; Convection; Divergence (linguistics); Atmosphere (unit); Cloud cover; Climate change; Geology; Computer science; Geography; Physics","score_opus":0.17243137993760688,"score_gpt":0.37568209785239964,"score_spread":0.20325071791479277,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1561569801","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":[0.99555296,0.0009528089,0.0027914098,0.00021148717,0.00005049309,0.00014576936,0.000012154085,0.0000035950502,0.0002793243],"genre_scores_gemma":[0.9897908,0.0007235721,0.009145772,0.000022808132,0.0001860871,0.0000031165637,0.000003488081,0.000017683777,0.000106651314],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9965803,0.00035633033,0.0006353883,0.00025556065,0.0016640557,0.00050837337],"domain_scores_gemma":[0.99793506,0.00079058646,0.00033564446,0.0005044959,0.00013983378,0.0002943761],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0025143651,0.00014580102,0.0003886209,0.0000053821864,0.00013531718,0.000041163847,0.0005725316,0.00008862622,0.00028249345],"category_scores_gemma":[0.0007148496,0.00011791606,0.00009304698,0.0008377013,0.0003737889,0.001338554,0.00060883857,0.00045830358,0.0000064640385],"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":[0.00013337014,0.00076693605,0.67731583,0.000032396187,0.00010199402,0.000017035525,0.0012383441,0.29516938,0.002804645,0.0003474203,0.0004070216,0.021665629],"study_design_scores_gemma":[0.0004927734,0.00018452523,0.531839,0.00011074477,0.0000792274,0.0000053649633,0.0011932547,0.46005926,0.00026968366,0.004834456,0.0007463851,0.00018534082],"about_ca_topic_score_codex":0.0033671653,"about_ca_topic_score_gemma":0.00030692664,"teacher_disagreement_score":0.16488987,"about_ca_system_score_codex":0.00026112449,"about_ca_system_score_gemma":0.0000709148,"threshold_uncertainty_score":0.50901693},"labels":[],"label_agreement":null},{"id":"W1563241029","doi":"10.1109/aero.2015.7119134","title":"Design of a new smaller lighter faraday rotator for ACERAD radar QOTL","year":2015,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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":"Faraday effect; Faraday rotator; Faraday cage; Radar; Polarizer; Computer science; Polarization (electrochemistry); Remote sensing; Optics; Physics; Magnetic field; Geology; Telecommunications; Birefringence","score_opus":0.04593637942071267,"score_gpt":0.24683591472886238,"score_spread":0.2008995353081497,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1563241029","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.15264985,0.00009037937,0.8315627,0.0010668003,0.00016801871,0.0006366015,0.000001597233,0.000049857925,0.0137741845],"genre_scores_gemma":[0.44996604,0.0000088282595,0.49167368,0.0007617567,0.00009315219,0.00003364584,0.0000015334214,0.000028725937,0.057432637],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99921274,0.000017889663,0.00016339846,0.00019516253,0.00020466314,0.00020612567],"domain_scores_gemma":[0.99953103,0.00002829985,0.000056962548,0.00018566327,0.0000075271437,0.00019050772],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00015818173,0.00010780684,0.00014189763,5.925909e-7,0.000031543776,0.00001082248,0.00018380195,0.000054200278,0.0025256074],"category_scores_gemma":[0.000017325108,0.00007819594,0.0000487821,0.00008318662,0.000059122598,0.00009805931,0.00007667978,0.000034336794,0.00024772028],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037392296,0.00023777498,0.013666159,0.000011969907,0.000057911962,0.0000047903454,0.0034540643,0.0042154216,0.02265155,0.0008778015,0.9153919,0.039056696],"study_design_scores_gemma":[0.006873992,0.0021715842,0.014696829,0.000025716892,0.00009516122,0.000017994209,0.0014406117,0.021760963,0.07721634,0.009801673,0.86462784,0.0012712859],"about_ca_topic_score_codex":0.00034460076,"about_ca_topic_score_gemma":0.000022001626,"teacher_disagreement_score":0.33988902,"about_ca_system_score_codex":0.000058470276,"about_ca_system_score_gemma":0.00003707248,"threshold_uncertainty_score":0.9983862},"labels":[],"label_agreement":null},{"id":"W1565137142","doi":"10.5772/9753","title":"Monitoring Spatial and Temporal Variability of Air Quality Using Satellite Observation Data: a Case Study of MODIS-Observed Aerosols in Southern Ontario, Canada","year":2010,"lang":"en","type":"book-chapter","venue":"Sciyo eBooks","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":5,"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","funders":"","keywords":"Aerosol; Environmental science; Atmospheric sciences; Air quality index; Radiative forcing; Atmosphere (unit); Satellite; Air pollution; Planetary boundary layer; Climate change; Climatology; Meteorology; Geography; Geology; Chemistry; Oceanography; Physics","score_opus":0.09348830363070083,"score_gpt":0.2718597835035483,"score_spread":0.17837147987284746,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1565137142","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":[0.9951997,0.000016439435,0.000060484508,0.000002961103,0.0002180719,0.0007512512,0.000121768324,0.000008988196,0.0036203624],"genre_scores_gemma":[0.99043244,7.9595e-7,0.0023418528,0.000007708351,0.00005003919,0.00000643718,0.000016193584,0.000031046417,0.007113475],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99741817,0.00010202858,0.0009242683,0.0007122633,0.0006007711,0.0002425219],"domain_scores_gemma":[0.99803025,0.00007317556,0.00067953585,0.0010663766,0.000034614743,0.00011607429],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0010196785,0.00033387862,0.00061972754,0.00000775724,0.00011494074,0.000016123677,0.00037744016,0.00025784096,0.0001664981],"category_scores_gemma":[0.000027868422,0.0003244723,0.000044542867,0.00005579754,0.0002840493,0.000105828825,0.0006736735,0.0004937521,7.371559e-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":[0.00005211623,0.0000715856,0.9900924,0.00005782715,0.000025417752,0.00010001186,0.0038392763,0.00011568725,0.001262195,0.000014700071,6.83854e-7,0.0043680957],"study_design_scores_gemma":[0.0021563347,0.00033569898,0.9838438,0.00034348213,0.00025740915,0.000054484794,0.007844802,0.00093755225,0.00040889962,0.0019939088,0.0004976725,0.001325937],"about_ca_topic_score_codex":0.9971772,"about_ca_topic_score_gemma":0.9989963,"teacher_disagreement_score":0.006248585,"about_ca_system_score_codex":0.00048677067,"about_ca_system_score_gemma":0.00039684385,"threshold_uncertainty_score":0.9999207},"labels":[],"label_agreement":null},{"id":"W1570025454","doi":"10.1029/2010gl046016","title":"Evidence of liquid dependent ice nucleation in high-latitude stratiform clouds from surface remote sensors","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":287,"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":"National Aeronautics and Space Administration","keywords":"Ice nucleus; Sea ice growth processes; Sea ice; Geology; Arctic ice pack; Microwave radiometer; Atmospheric sciences; Arctic; Sea ice thickness; Sea ice concentration; Nucleation; Lidar; Antarctic sea ice; Supersaturation; Environmental science; Climatology; Radiometer; Remote sensing; Oceanography; Physics","score_opus":0.054583927252895306,"score_gpt":0.29660463644366647,"score_spread":0.24202070919077118,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1570025454","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":[0.9974575,0.000022979908,0.00069889845,0.0007582518,0.000054040294,0.00026547004,0.0000047696576,0.000019968713,0.0007181402],"genre_scores_gemma":[0.9912132,0.000048347498,0.008370012,0.00017748178,0.00005661186,0.0000040479695,0.0000027695157,0.000018051282,0.00010949996],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9972153,0.00025296074,0.0003127943,0.00047272714,0.0011913201,0.00055494317],"domain_scores_gemma":[0.99893904,0.00033741476,0.0000849669,0.00045593688,0.000025661266,0.00015701243],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005796068,0.00015167525,0.00021950177,0.000004624308,0.00009554141,0.000022588205,0.0005014472,0.00008023074,0.0012873673],"category_scores_gemma":[0.00014941057,0.00013727514,0.000060785067,0.00046043933,0.00047537722,0.00035489394,0.00034211035,0.00046166967,0.00067650253],"study_design_candidate":"bench_or_experimental","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":[0.0008962625,0.00029938295,0.024926675,0.000025996946,0.000024963087,0.000079883226,0.0033312584,0.009566651,0.9553303,0.00030135564,0.00061022537,0.0046070577],"study_design_scores_gemma":[0.0006601275,0.0008948909,0.9063226,0.00024360335,0.000014475495,0.0000010216573,0.0005598577,0.010719136,0.07817137,0.0019258407,0.00007008479,0.0004169667],"about_ca_topic_score_codex":0.06021471,"about_ca_topic_score_gemma":0.0010205989,"teacher_disagreement_score":0.88139594,"about_ca_system_score_codex":0.00025510008,"about_ca_system_score_gemma":0.000023640221,"threshold_uncertainty_score":0.99962556},"labels":[],"label_agreement":null},{"id":"W1571688942","doi":"10.2172/1035864","title":"Parameterization of the Extinction Coefficient in Ice and Mixed-Phase Arctic Clouds during the ISDAC Field Campaign","year":2012,"lang":"en","type":"report","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"","keywords":"Extinction (optical mineralogy); Parametrization (atmospheric modeling); Ice crystals; Scale (ratio); Cloud computing; Phase (matter); Molar absorptivity; Radiative transfer; Remote sensing; Ice cloud; Environmental science; Computational physics; Meteorology; Physics; Optics; Computer science; Geology","score_opus":0.016756061922252066,"score_gpt":0.25502283539362874,"score_spread":0.23826677347137667,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1571688942","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":[0.986547,0.00020877218,0.0013132138,0.000104340375,0.0006531983,0.00043078847,0.0000034827522,0.000012741859,0.01072647],"genre_scores_gemma":[0.99564296,0.00028063578,0.00007869804,0.00008472733,0.00008021432,0.00002772133,0.0000036505417,0.00001628415,0.0037850814],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985059,0.00009972318,0.00036660986,0.00026372587,0.0005291766,0.00023487011],"domain_scores_gemma":[0.9991344,0.00010624627,0.00030265647,0.00039405184,0.000015464168,0.000047182522],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00053078355,0.00018065172,0.00020536459,0.0000019349359,0.00014073454,0.000020769081,0.00020917095,0.00017416589,0.001547637],"category_scores_gemma":[0.00013502828,0.00009828892,0.00007336532,0.00024724405,0.00018227387,0.00006320022,0.0002902733,0.00025514193,0.00001030261],"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":[0.00015508941,0.0010876927,0.9070234,0.0006670859,0.00008349868,0.000008695152,0.0029767896,0.009897709,0.011064377,0.00005641803,0.0036291059,0.06335014],"study_design_scores_gemma":[0.000964915,0.00026556515,0.9551505,0.00026521977,0.00018253217,0.00012011231,0.001370027,0.0033556684,0.008515242,0.00007649201,0.029098991,0.0006347517],"about_ca_topic_score_codex":0.0022343146,"about_ca_topic_score_gemma":0.0005376416,"teacher_disagreement_score":0.06271539,"about_ca_system_score_codex":0.00023767598,"about_ca_system_score_gemma":0.000032976997,"threshold_uncertainty_score":0.9993651},"labels":[],"label_agreement":null},{"id":"W1577912761","doi":"10.13016/m2q7rg-eo0d","title":"The Southern African Regional Science Initiative (SAFARI 2000) : overview of the dry season field campaign","year":2002,"lang":"en","type":"article","venue":"The Mathematics Enthusiast","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":125,"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":"National Research Foundation; McGill University; National Aeronautics and Space Administration","keywords":"Context (archaeology); Geography; Satellite; Environmental science; Atmosphere (unit); Meteorology; Atmospheric research; Climatology; Geology; Archaeology","score_opus":0.03839868912836698,"score_gpt":0.24307554775651202,"score_spread":0.20467685862814505,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1577912761","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":[0.6801343,0.0010865143,0.0029498148,0.008546773,0.00034449555,0.0011399688,0.000024026795,0.00006472414,0.30570936],"genre_scores_gemma":[0.9957619,0.000105466774,0.0006432601,0.00061959395,0.000036443227,0.000021117361,1.5504598e-7,0.000013675645,0.0027984397],"study_design_codex":"qualitative","study_design_gemma":"qualitative","domain_scores_codex":[0.9983029,0.00008223504,0.0002693094,0.00019484673,0.00081634877,0.00033440616],"domain_scores_gemma":[0.998503,0.0004006995,0.00027481955,0.00073545775,0.000022303688,0.00006369274],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00065146683,0.00015641024,0.00015077516,0.0000016177308,0.0008181908,0.000056361117,0.001285848,0.00003301361,0.0020696372],"category_scores_gemma":[0.0001576525,0.0000680451,0.00010999389,0.0005903689,0.0015852844,0.000076687116,0.0005063713,0.00018609334,0.00026993878],"study_design_candidate":"qualitative","study_design_consensus":"qualitative","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023615821,0.00058674894,0.0023777396,0.000067691195,0.000072755756,0.0000037089408,0.93734646,0.0009185571,0.0017630849,0.015925214,0.011711788,0.029202612],"study_design_scores_gemma":[0.003101629,0.001304004,0.1045046,0.0016981974,0.0008708134,0.00023652623,0.40486577,0.31481075,0.01652894,0.0423072,0.10602355,0.0037480085],"about_ca_topic_score_codex":0.000115302224,"about_ca_topic_score_gemma":0.0001593475,"teacher_disagreement_score":0.5324807,"about_ca_system_score_codex":0.00010439998,"about_ca_system_score_gemma":0.00003149538,"threshold_uncertainty_score":0.9988426},"labels":[],"label_agreement":null},{"id":"W1581332980","doi":"10.1029/2011jd016611","title":"Parameterization of cloud optical properties for semidirect radiative forcing","year":2011,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":10,"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; Environment and Climate Change Canada","funders":"","keywords":"Cloud albedo; Albedo (alchemy); Cloud fraction; Cloud forcing; Carbon black; Radiative transfer; Atmospheric sciences; Single-scattering albedo; Radiative forcing; Computational physics; Optical depth; Liquid water content; Solar zenith angle; Environmental science; Physics; Materials science; Cloud cover; Cloud computing; Meteorology; Optics","score_opus":0.07240151014468786,"score_gpt":0.3042954058517821,"score_spread":0.23189389570709423,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1581332980","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":[0.9872859,0.00012276611,0.0083547635,0.00007356176,0.000104200655,0.00028186166,0.0000020264936,0.000006771324,0.0037681165],"genre_scores_gemma":[0.98008645,0.0000531202,0.019106911,0.000017863074,0.000199907,0.000016202535,3.277434e-7,0.000019802836,0.00049940875],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99796796,0.00015579503,0.0004613267,0.0001814432,0.00081196893,0.00042152943],"domain_scores_gemma":[0.99881727,0.00037209628,0.0002519622,0.00016665536,0.00019120782,0.00020083608],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00085004466,0.00012621729,0.00033673394,0.0000017725177,0.00013462237,0.000023944738,0.00034814348,0.000073927666,0.0005006784],"category_scores_gemma":[0.0008441667,0.00008686009,0.00019616498,0.0003210088,0.0005897531,0.00028989225,0.00015830784,0.00029992778,0.000027785152],"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":[0.010058794,0.0043568034,0.11237154,0.00047227353,0.0007429944,0.000096755444,0.016793922,0.006383645,0.55309105,0.011084682,0.014479388,0.27006814],"study_design_scores_gemma":[0.0034070925,0.015569504,0.3398363,0.00056958676,0.00016934203,0.00003972374,0.0051868665,0.03916822,0.54202265,0.04813724,0.0050513744,0.0008420874],"about_ca_topic_score_codex":0.00035872762,"about_ca_topic_score_gemma":0.000015979751,"teacher_disagreement_score":0.26922604,"about_ca_system_score_codex":0.00012129588,"about_ca_system_score_gemma":0.00007623185,"threshold_uncertainty_score":0.5482077},"labels":[],"label_agreement":null},{"id":"W1598101504","doi":"10.54782/001c.133057","title":"Atmospheric Dc Corona Effect Ionization As A Potential Tool For Aerosol Deposition: An Experiment","year":2009,"lang":"en","type":"article","venue":"The Journal of Weather Modification","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Iogen Corporation","funders":"","keywords":"Aerosol; Cloud condensation nuclei; Ionization; Population; Atmospheric sciences; Environmental science; Deposition (geology); Charged particle; Meteorology; Ion; Physics; Geology","score_opus":0.008906662191210996,"score_gpt":0.25352793872748286,"score_spread":0.24462127653627186,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1598101504","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":[0.77838296,0.0001300516,0.2203954,0.00043152666,0.000097443415,0.00033966577,5.960288e-7,0.0000133568865,0.00020899565],"genre_scores_gemma":[0.9915942,0.00004250536,0.007660136,0.0002596164,0.00015362714,0.000014183951,0.0000049514074,0.000014234392,0.0002565464],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.998941,0.0001342543,0.00031291446,0.00012631968,0.00033094524,0.00015455653],"domain_scores_gemma":[0.9993032,0.000031397212,0.00033421288,0.00022906587,0.00003655023,0.000065580556],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048118917,0.00012746168,0.00013589935,8.642591e-7,0.0002376787,0.00004502982,0.00026030812,0.00005852142,0.0003358862],"category_scores_gemma":[0.000016742966,0.0000835055,0.00008695097,0.00011375432,0.000056080535,0.00031952997,0.00001507586,0.00008234161,0.000039480925],"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":[0.00094407663,0.00042764557,0.00096835295,0.0000045664424,0.000031483505,0.000002885692,0.0022329204,0.055179413,0.85916495,0.00019867842,0.0007409511,0.08010407],"study_design_scores_gemma":[0.008065474,0.020773303,0.17248964,0.00012640223,0.00094032084,0.0010327982,0.002140437,0.24793035,0.53878367,0.0047018994,0.0016020533,0.0014136378],"about_ca_topic_score_codex":0.000026954478,"about_ca_topic_score_gemma":0.0000011639993,"teacher_disagreement_score":0.32038128,"about_ca_system_score_codex":0.00016058711,"about_ca_system_score_gemma":0.000014463271,"threshold_uncertainty_score":0.36777183},"labels":[],"label_agreement":null},{"id":"W1624519712","doi":"","title":"Anatomy of cirrus clouds","year":2004,"lang":"en","type":"article","venue":"Research Explorer (The University of Manchester)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"York University","funders":"","keywords":"Cirrus; Ice crystals; Thunderstorm; Lidar; Outflow; Cloud physics; Cloud height; Geology; Atmospheric sciences; Meteorology; Latitude; Cloud top; Remote sensing; Environmental science; Geography; Cloud cover; Cloud computing; Physics; Astronomy; Satellite; Geodesy","score_opus":0.03893001420714614,"score_gpt":0.2813960456814082,"score_spread":0.24246603147426204,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1624519712","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":[0.994346,0.000038339396,0.00084478076,0.00092910806,0.00002316956,0.00016196512,0.0000017361424,0.000012833342,0.0036420275],"genre_scores_gemma":[0.99846727,0.00014293753,0.0012265318,0.000020420044,0.000014410701,4.7224404e-7,9.749394e-7,0.000007665766,0.00011933843],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99865484,0.00009639513,0.0001077591,0.00020662358,0.00063540344,0.00029896785],"domain_scores_gemma":[0.99933535,0.0000705534,0.00006274055,0.00040341535,0.00003243685,0.00009549623],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00051629834,0.00007960154,0.00013967707,0.000005106344,0.00020574727,0.000005522372,0.0006883506,0.00005540492,0.0014332018],"category_scores_gemma":[0.000021902633,0.00006695027,0.00008323923,0.00040694253,0.0012358661,0.00014979525,0.0005559805,0.00020654919,0.00037819834],"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":[0.0011689713,0.0023829173,0.38718212,0.00037678555,0.00038304258,0.00040953897,0.38696292,0.017264552,0.0679805,0.012275512,0.024995433,0.098617725],"study_design_scores_gemma":[0.0034428888,0.00096770946,0.7513903,0.00017128502,0.000054784115,0.000015647027,0.11179916,0.0003842948,0.020925602,0.010381867,0.09992806,0.0005384136],"about_ca_topic_score_codex":0.00023321321,"about_ca_topic_score_gemma":0.000014196334,"teacher_disagreement_score":0.3642082,"about_ca_system_score_codex":0.0001813118,"about_ca_system_score_gemma":0.00003506726,"threshold_uncertainty_score":0.99947965},"labels":[],"label_agreement":null},{"id":"W1627710482","doi":"10.1029/2010gl042440","title":"Mystery of ice multiplication in warm‐based precipitating shallow cumulus clouds","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Clear ice; Ice crystals; Supercooling; Atmospheric sciences; Geology; Sea ice growth processes; Ice cloud; Ice nucleus; Sea ice; Climatology; Meteorology; Sea ice thickness; Arctic ice pack; Physics; Antarctic sea ice; Optics; Radiative transfer; Thermodynamics","score_opus":0.025202703804189736,"score_gpt":0.31056152627896594,"score_spread":0.2853588224747762,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1627710482","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":[0.99539536,0.0000026238943,0.00069346174,0.0021546572,0.000068712456,0.00029766405,0.0000025871452,0.000019816307,0.001365125],"genre_scores_gemma":[0.99482036,0.0000010051164,0.0044706594,0.00038579045,0.0000938044,0.00007897253,0.000004813333,0.00001720262,0.00012740916],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99782187,0.00016221916,0.0002486806,0.00039259336,0.00083234377,0.0005423208],"domain_scores_gemma":[0.99871206,0.0006473743,0.00006491019,0.0004143564,0.000023567402,0.00013772793],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006900423,0.0001169643,0.00016477039,0.000006677846,0.000101340695,0.000024824178,0.0004406828,0.00007266802,0.00035129077],"category_scores_gemma":[0.00040586106,0.000106142266,0.00006865296,0.0005548456,0.00053950684,0.00014859205,0.00023881682,0.00067718263,0.00035877113],"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":[0.000045907025,0.0001986712,0.051919155,0.000017807812,0.0000031156012,0.0000062325503,0.00044660087,0.0010912069,0.93343776,0.00009156792,0.0004755256,0.012266453],"study_design_scores_gemma":[0.0010386441,0.00020174589,0.8703243,0.000049688497,0.000005131629,6.6765233e-7,0.00021100929,0.08662572,0.03895344,0.0005403555,0.0017260899,0.00032320558],"about_ca_topic_score_codex":0.0023345435,"about_ca_topic_score_gemma":0.00034604012,"teacher_disagreement_score":0.89448434,"about_ca_system_score_codex":0.00010057416,"about_ca_system_score_gemma":0.000022535898,"threshold_uncertainty_score":0.46113968},"labels":[],"label_agreement":null},{"id":"W1657365528","doi":"10.1029/2002jd003220","title":"A parameterization of cirrus cloud formation: Heterogeneous freezing","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":349,"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","funders":"","keywords":"Cirrus; Ice crystals; Ice nucleus; Clear ice; Atmospheric sciences; Saturation (graph theory); Aerosol; Nucleation; Supercooling; Ice formation; Cloud physics; Ice cloud; Particle (ecology); Homogeneous; Chemical physics; Liquid water content; Environmental science; Materials science; Chemistry; Thermodynamics; Meteorology; Physics; Geology; Cloud computing; Optics; Arctic ice pack; Sea ice; Radiative transfer","score_opus":0.03125158995083372,"score_gpt":0.2986046187692602,"score_spread":0.2673530288184265,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1657365528","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":[0.9867841,0.00016623468,0.00847726,0.00007696065,0.00012391116,0.00012523972,0.0000012679095,0.0000061228047,0.004238917],"genre_scores_gemma":[0.9918138,0.0000848615,0.0076258527,0.00003369687,0.0001229199,0.0000039224715,4.8100014e-7,0.00001547586,0.00029900591],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99733317,0.00033539569,0.0005391984,0.00015155258,0.0012400253,0.0004006563],"domain_scores_gemma":[0.99882066,0.00026783746,0.00032468673,0.00022977337,0.00014150927,0.00021550113],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00081177516,0.00012310191,0.00028352128,0.0000019680954,0.00015017908,0.00004476021,0.00035061673,0.000071618815,0.001612706],"category_scores_gemma":[0.0005528622,0.00009593808,0.00017335008,0.0005407125,0.00033866247,0.0003529296,0.000114300135,0.00036040356,0.000105978135],"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":[0.0017454091,0.0044374545,0.10486218,0.00037896965,0.0005287555,0.00064639596,0.005340583,0.089647375,0.571258,0.013832855,0.02896208,0.17835991],"study_design_scores_gemma":[0.008407456,0.01840518,0.11845228,0.0008964099,0.00024310926,0.0011799478,0.0058420324,0.05886703,0.527856,0.12930849,0.12833084,0.0022112455],"about_ca_topic_score_codex":0.00016382601,"about_ca_topic_score_gemma":0.000020480828,"teacher_disagreement_score":0.17614867,"about_ca_system_score_codex":0.00014922864,"about_ca_system_score_gemma":0.000057241785,"threshold_uncertainty_score":0.99929994},"labels":[],"label_agreement":null},{"id":"W1661375993","doi":"10.1029/2010gl044317","title":"Lidar measurements of clouds in the planetary boundary layer on Mars","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Canadian Space Agency; University of Arizona; Jet Propulsion Laboratory; National Aeronautics and Space Administration","keywords":"Lidar; Mars Exploration Program; Atmospheric sciences; Environmental science; Planetary boundary layer; Cloud physics; Liquid water content; Atmosphere of Mars; Boundary layer; Liquid water; Meteorology; Geology; Astrobiology; Remote sensing; Cloud computing; Physics; Martian","score_opus":0.044964255850712016,"score_gpt":0.3029329167165012,"score_spread":0.2579686608657892,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1661375993","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":[0.98347276,0.0000043035097,0.000005839583,0.0046160277,0.000093609684,0.00022093827,0.0000033545027,0.0000073352167,0.011575837],"genre_scores_gemma":[0.9973389,0.0000018563571,0.00022804791,0.002152374,0.00012197841,0.000023534873,0.0000043132104,0.000010579367,0.00011840065],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99722636,0.00024140095,0.00015876362,0.00028361133,0.0015794064,0.00051047804],"domain_scores_gemma":[0.9991784,0.00025587177,0.000030803174,0.00043794076,0.000008645645,0.00008835627],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010463145,0.00011078422,0.00012851226,0.0000042200186,0.00014443675,0.00003415705,0.00065704423,0.000053395335,0.0006557783],"category_scores_gemma":[0.000091597256,0.00007339381,0.000059149785,0.00037162704,0.00072742155,0.000076210585,0.0001716394,0.00092346134,0.0008242905],"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":[0.00019977287,0.00055813533,0.15759179,0.0000133816775,0.000017403043,0.000067654226,0.0009031885,0.00017253082,0.79391026,0.00020313522,0.033153906,0.013208839],"study_design_scores_gemma":[0.00039180598,0.00026474873,0.9798238,0.000014262483,0.0000037038465,0.0000019460902,0.00011683981,0.0001494071,0.0046982896,0.0007493727,0.013635032,0.00015077308],"about_ca_topic_score_codex":0.0019153309,"about_ca_topic_score_gemma":0.00019745308,"teacher_disagreement_score":0.822232,"about_ca_system_score_codex":0.00005111952,"about_ca_system_score_gemma":0.000017299824,"threshold_uncertainty_score":0.9999537},"labels":[],"label_agreement":null},{"id":"W1665170725","doi":"","title":"Instrumentation for the High Ice Water Content (HIWC) Flight Campaigns","year":2011,"lang":"en","type":"article","venue":"NASA Technical Reports Server (NASA)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"","keywords":"Instrumentation (computer programming); Remote sensing; Environmental science; Computer science; Geology; Operating system","score_opus":0.04355832609548842,"score_gpt":0.23259962333157227,"score_spread":0.18904129723608387,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1665170725","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":[0.9881282,0.000039322942,0.004270386,0.000606339,0.00062259356,0.0010271027,0.0000036714573,0.0001761718,0.005126247],"genre_scores_gemma":[0.99222165,0.000020738047,0.00414464,0.0009440085,0.00009496294,0.00030261028,0.000015507474,0.000030137986,0.0022257348],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99771184,0.00003503254,0.000615295,0.0005628959,0.0005616299,0.00051330146],"domain_scores_gemma":[0.99875486,0.00006674481,0.00022862197,0.0007539204,0.000033142434,0.00016270218],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005815859,0.00024780515,0.00024516683,0.0000024471758,0.00032152847,0.00004408881,0.0003670829,0.00019603762,0.0038592487],"category_scores_gemma":[0.00007698905,0.00014056449,0.00019250435,0.00014689364,0.000266709,0.00026662208,0.00033757862,0.00021232844,0.00014201202],"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":[0.00074583065,0.0020137585,0.67753756,0.0001032255,0.000339522,0.0007392729,0.0038618033,0.00041220352,0.22289306,0.004203463,0.03952048,0.047629848],"study_design_scores_gemma":[0.0010582266,0.00071327755,0.83464694,0.00004503919,0.00021793525,0.00032289815,0.00070789474,0.00018304559,0.08323539,0.006902246,0.07109541,0.0008716847],"about_ca_topic_score_codex":0.0013206055,"about_ca_topic_score_gemma":0.00030907817,"teacher_disagreement_score":0.15710942,"about_ca_system_score_codex":0.00021943776,"about_ca_system_score_gemma":0.000017822023,"threshold_uncertainty_score":0.99705136},"labels":[],"label_agreement":null},{"id":"W1732533790","doi":"10.1117/12.2189174","title":"Extinction cross section measurements for a single optically trapped particle","year":2015,"lang":"en","type":"article","venue":"Proceedings of SPIE, the International Society for Optical Engineering/Proceedings of SPIE","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Engineering and Physical Sciences Research Council; Natural Environment Research Council; Royal Society; Royal Society of Chemistry; Aerosol Society","keywords":"Mie scattering; Particle (ecology); Optics; RADIUS; Physics; Range (aeronautics); Aerosol; Light scattering; Scattering; Molecular physics; Materials science; Atomic physics","score_opus":0.027561132511245284,"score_gpt":0.24384443177706244,"score_spread":0.21628329926581716,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1732533790","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":[0.9939757,0.000024445031,0.00051685417,0.000842676,0.00034242184,0.0006232924,0.000011533625,0.0000752872,0.003587813],"genre_scores_gemma":[0.9131764,0.0000064930473,0.08584259,0.000072619376,0.00034996794,0.00021566222,0.0000038510366,0.000045247463,0.00028717023],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99790287,1.7044206e-8,0.0005376114,0.00037476645,0.0007879411,0.00039680264],"domain_scores_gemma":[0.99878895,0.000056548055,0.0002768665,0.000050054718,0.0006422291,0.00018533565],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008163278,0.00023502296,0.00026041886,0.0000053289355,0.00010871877,0.00011757227,0.0005135756,0.00016015515,0.00003942119],"category_scores_gemma":[0.00055267254,0.00019845918,0.0003981715,0.00025116475,0.00025728255,0.0005870646,0.00013379467,0.00015230307,0.000004473195],"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":[0.0002752163,0.00029670884,0.008598282,0.000108760105,0.00016332495,3.4605428e-8,0.00033382815,0.0013325625,0.97088706,0.015002538,0.0024984893,0.00050316355],"study_design_scores_gemma":[0.006497529,0.0024294467,0.01662525,0.00022221627,0.00039984868,0.000039540195,0.0039196555,0.14288375,0.8107368,0.003294643,0.011842762,0.0011085689],"about_ca_topic_score_codex":0.000016307336,"about_ca_topic_score_gemma":5.3943876e-7,"teacher_disagreement_score":0.1601503,"about_ca_system_score_codex":0.00036951026,"about_ca_system_score_gemma":0.00001806235,"threshold_uncertainty_score":0.80929303},"labels":[],"label_agreement":null},{"id":"W1769727502","doi":"10.1002/2013jd019860","title":"The effect of smoke emission amount on changes in cloud properties and precipitation: A case study of Canadian boreal wildfires of 2007","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":32,"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":"Smoke; Liquid water path; Environmental science; Atmospheric sciences; Aerosol; Moderate-resolution imaging spectroradiometer; Cloud top; Weather Research and Forecasting Model; Precipitation; Meteorology; Satellite; Geography; Geology; Physics","score_opus":0.030709813155854113,"score_gpt":0.2926199785189395,"score_spread":0.26191016536308537,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1769727502","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":[0.99829614,0.00024515734,4.2066475e-7,0.0002950416,0.000041164578,0.00053002563,0.000001237222,0.0000011504226,0.00058963563],"genre_scores_gemma":[0.9995998,0.00012503951,0.000039516002,0.0000065190434,0.00006730426,0.000020755606,1.0635116e-7,0.000009728068,0.00013123536],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9977617,0.00046455514,0.00040066155,0.00014202559,0.00090819795,0.00032284507],"domain_scores_gemma":[0.99852276,0.00070925854,0.0002354054,0.00019547835,0.000102960395,0.00023414765],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010391849,0.0001185291,0.0003213183,0.000006818009,0.00014254123,0.00002530475,0.00026968392,0.000052430172,0.00012699848],"category_scores_gemma":[0.00043463864,0.00006227723,0.000051319126,0.00048646066,0.00063979346,0.00011968467,0.00012477534,0.0003394026,0.0000028620832],"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":[0.0011876703,0.00077330443,0.8931058,0.00010617413,0.00009302929,0.00025848107,0.007510584,0.00055473694,0.0086970655,0.00002316744,0.0033794849,0.08431047],"study_design_scores_gemma":[0.0010115026,0.013648109,0.9633644,0.00019822446,0.00001650155,0.00003132837,0.014069945,0.00085395394,0.006411285,0.00013853895,0.00016697981,0.00008921373],"about_ca_topic_score_codex":0.63143677,"about_ca_topic_score_gemma":0.1488816,"teacher_disagreement_score":0.48255518,"about_ca_system_score_codex":0.00011640464,"about_ca_system_score_gemma":0.000072621486,"threshold_uncertainty_score":0.8666491},"labels":[],"label_agreement":null},{"id":"W1771480164","doi":"10.1109/leos.1990.690483","title":"Development Of New Atmospheric Aerosol And Ozone Lidar Profiler Development Of New Atmospheric Aerosol And Ozone Lidar Profiler","year":2005,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Lidar; Aerosol; Ozone; Environmental science; Wind profiler; Remote sensing; Atmospheric sciences; Meteorology; Geology; Geography; Radar; Aerospace engineering; Engineering","score_opus":0.014143765834683955,"score_gpt":0.22634549510858482,"score_spread":0.21220172927390085,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1771480164","genre_codex":"empirical","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97768724,0.00081329385,0.014785161,0.0003338048,0.000118000666,0.0011798727,0.0000034539378,0.000112771406,0.0049663726],"genre_scores_gemma":[0.41187406,0.000103250684,0.56720024,0.00021617049,0.00008003561,0.00005466592,0.000008479704,0.000064931926,0.020398157],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9954668,0.000051192997,0.001474722,0.0010799363,0.0009961108,0.0009311864],"domain_scores_gemma":[0.9979998,0.000047229103,0.0005708098,0.00057239993,0.000046636007,0.0007631464],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00037940856,0.000737716,0.0008916985,0.0000017746055,0.00033855237,0.00006603345,0.0004916341,0.00030415304,0.008594665],"category_scores_gemma":[0.000033878532,0.0006243545,0.00010466279,0.0006815644,0.00042814077,0.0004894567,0.00088549603,0.00027819138,0.00029417194],"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":[0.00038463017,0.0012054374,0.21487504,0.00032370022,0.0003817931,0.000012398485,0.024866404,0.00048031454,0.099350005,0.00010792878,0.014933158,0.64307916],"study_design_scores_gemma":[0.009667856,0.0011790823,0.49413744,0.0005598118,0.0002851079,0.00009366634,0.0060526184,0.0032974833,0.34204495,0.000097313896,0.138189,0.004395672],"about_ca_topic_score_codex":0.0004967579,"about_ca_topic_score_gemma":0.0005645949,"teacher_disagreement_score":0.6386835,"about_ca_system_score_codex":0.00031343693,"about_ca_system_score_gemma":0.0005355092,"threshold_uncertainty_score":0.9996208},"labels":[],"label_agreement":null},{"id":"W1783851562","doi":"10.1002/jgrd.50604","title":"Dominant roles of subgrid‐scale cloud structures in model diversity of cloud radiative effects","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":22,"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; Chinese Academy of Sciences; National Natural Science Foundation of China","keywords":"Cloud computing; Radiative transfer; Longwave; Cloud cover; Shortwave; Environmental science; Cloud forcing; Atmospheric sciences; Scale (ratio); Atmospheric radiative transfer codes; Cloud height; Meteorology; Parametrization (atmospheric modeling); Cloud feedback; Cloud top; Climate model; Physics; Computer science; Climate change; Climate sensitivity; Geology","score_opus":0.014002068558313914,"score_gpt":0.2714085982396066,"score_spread":0.2574065296812927,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1783851562","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":[0.99748147,0.00021623599,0.0008957889,0.00012709494,0.00009366462,0.00030136824,0.0000045670613,0.0000029081639,0.00087692967],"genre_scores_gemma":[0.9963196,0.000120737415,0.003146153,0.000019593586,0.00014133792,0.000005156789,3.563074e-7,0.000014823575,0.00023225792],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99675196,0.00035288685,0.00057020725,0.00024142078,0.0015439598,0.0005395597],"domain_scores_gemma":[0.99821013,0.00065868633,0.00040849508,0.00026721656,0.00017297827,0.00028248838],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00071377255,0.00018770203,0.00061512896,0.000004382355,0.00014470202,0.000020974521,0.00077719876,0.000115762065,0.0005889371],"category_scores_gemma":[0.00032976756,0.0001344835,0.00024021749,0.0005230057,0.00092673145,0.00035652914,0.0009316049,0.00066193467,0.00003787924],"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":[0.002021476,0.0024951554,0.634035,0.00030701733,0.00024732406,0.000111511414,0.010651484,0.101606146,0.18653432,0.0016849951,0.017385626,0.042919975],"study_design_scores_gemma":[0.0016821137,0.0015231356,0.8786118,0.00014065967,0.000029221854,0.000004688664,0.0015796071,0.027364485,0.04457059,0.04421301,0.000053750315,0.00022692772],"about_ca_topic_score_codex":0.005169712,"about_ca_topic_score_gemma":0.00036297477,"teacher_disagreement_score":0.24457683,"about_ca_system_score_codex":0.00021206398,"about_ca_system_score_gemma":0.00008634119,"threshold_uncertainty_score":0.7815093},"labels":[],"label_agreement":null},{"id":"W1784670537","doi":"10.1029/2009gl041375","title":"Pan‐Arctic sunphotometry during the ARCTAS‐A campaign of April 2008","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University; Environment and Climate Change Canada; York University; Université de Sherbrooke","funders":"Natural Sciences and Engineering Research Council of Canada; National Oceanic and Atmospheric Administration; U.S. Department of Energy; Fonds Québécois de la Recherche sur la Nature et les Technologies; Canadian Foundation for Climate and Atmospheric Sciences; National Aeronautics and Space Administration","keywords":"Environmental science; Aerosol; Arctic; Climatology; Smoke; The arctic; Atmospheric sciences; Meteorology; Geology; Geography; Oceanography","score_opus":0.013102204459532474,"score_gpt":0.2721381171064066,"score_spread":0.25903591264687414,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1784670537","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":[0.9958035,0.000008200434,0.000041693394,0.0024231703,0.00010775659,0.00024712423,0.0000035337914,0.000019817333,0.0013452035],"genre_scores_gemma":[0.9981286,0.000007629888,0.0003019253,0.00041662168,0.00020845287,0.00004033456,0.0000013041301,0.000019639921,0.00087549957],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99733055,0.00014822246,0.00018669358,0.0003493208,0.0012509457,0.000734257],"domain_scores_gemma":[0.9987392,0.0003914199,0.000051513132,0.0006202414,0.000024488256,0.00017312737],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0005945356,0.00013439375,0.00016464417,0.000005359581,0.0003497311,0.00004067818,0.0007351856,0.000059894122,0.0021455993],"category_scores_gemma":[0.0002581092,0.00008912756,0.00011355905,0.0008071779,0.0015917104,0.00011804434,0.00056215964,0.0010274496,0.0009821265],"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":[0.00003472146,0.000108642045,0.068748206,0.000019498235,0.000013558867,0.000016927803,0.0002996342,0.000031508414,0.92497224,0.000090791465,0.003928688,0.0017355699],"study_design_scores_gemma":[0.0002446599,0.00006800817,0.97665375,0.000009665455,0.000005324406,0.0000051894785,0.00017195875,0.00020086688,0.018704288,0.0004022375,0.0033783142,0.00015572798],"about_ca_topic_score_codex":0.003254085,"about_ca_topic_score_gemma":0.00010680591,"teacher_disagreement_score":0.9079056,"about_ca_system_score_codex":0.00008813301,"about_ca_system_score_gemma":0.000018046494,"threshold_uncertainty_score":0.99979573},"labels":[],"label_agreement":null},{"id":"W1797561859","doi":"10.1002/2013jd021279","title":"Remote sensing of aerosols in the Arctic for an evaluation of global climate model simulations","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":54,"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 Saskatchewan","funders":"Vetenskapsrådet; National Aeronautics and Space Administration; Norges Forskningsråd; Stockholms Universitet; National Science Council; Svenska Forskningsrådet Formas","keywords":"Environmental science; Aerosol; Moderate-resolution imaging spectroradiometer; Climatology; Subarctic climate; Arctic; AERONET; Atmospheric sciences; Climate model; Satellite; Latitude; Sun photometer; Remote sensing; Meteorology; Climate change; Geography; Geology; Oceanography","score_opus":0.07626031536549431,"score_gpt":0.38723566066751464,"score_spread":0.3109753453020203,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1797561859","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":[0.9736415,0.000022353019,0.025059411,0.00019257687,0.000023302111,0.0003084178,0.000005460653,0.0000017022764,0.00074525684],"genre_scores_gemma":[0.97770554,0.000007471471,0.022161718,0.000028843922,0.00007933874,8.5657325e-7,8.153106e-7,0.000008226074,0.000007206477],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9966583,0.0006190613,0.0004936602,0.00015120946,0.001743574,0.00033415723],"domain_scores_gemma":[0.998284,0.0006827556,0.0002962155,0.0002712576,0.00037235193,0.000093451185],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.004226796,0.00009294212,0.00025188542,0.0000010843322,0.000115686635,0.000025541683,0.00036871003,0.000054870554,0.00005062283],"category_scores_gemma":[0.0011947084,0.00006220945,0.0001246326,0.00043137168,0.00031470324,0.00022408222,0.000090554735,0.0002341144,0.000003608288],"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":[0.00043204427,0.00042490012,0.018472157,0.00004916695,0.000025125843,0.0000011182899,0.00062744395,0.8701019,0.013375447,0.0026744716,0.00016672468,0.09364948],"study_design_scores_gemma":[0.00056587794,0.0006828204,0.0715913,0.000052306925,0.000028288956,0.0000023589928,0.00026423406,0.846824,0.00022041968,0.07970341,0.000012810705,0.000052178824],"about_ca_topic_score_codex":0.0011392483,"about_ca_topic_score_gemma":0.0008816834,"teacher_disagreement_score":0.09359729,"about_ca_system_score_codex":0.00019916393,"about_ca_system_score_gemma":0.00009631193,"threshold_uncertainty_score":0.2536828},"labels":[],"label_agreement":null},{"id":"W1811890442","doi":"10.5194/acp-16-2997-2016","title":"Fingerprints of a riming event on cloud radar Doppler spectra: observations and modeling","year":2016,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":128,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Deutscher Akademischer Austauschdienst; Deutsche Forschungsgemeinschaft; U.S. Department of Energy","keywords":"Radar; Environmental science; Liquid water content; Meteorology; Doppler effect; Doppler radar; Snow; Atmospheric sciences; Geology; Cloud computing; Physics; Computer science","score_opus":0.016291540667810817,"score_gpt":0.21831998792705612,"score_spread":0.2020284472592453,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1811890442","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":[0.9712779,0.000046119712,0.025302239,0.00010727518,0.000022861908,0.000056296623,0.0000058831133,0.000016181262,0.0031652648],"genre_scores_gemma":[0.9868414,0.0001047247,0.011832783,0.00006139782,0.000086654945,0.0000060078924,0.0000012548962,0.00001208715,0.0010536805],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9992311,0.0000077371105,0.0001582587,0.0002592822,0.00018074014,0.00016287935],"domain_scores_gemma":[0.9996191,0.00004527076,0.00006664559,0.00018458735,0.000008663457,0.000075710675],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000708665,0.00013431002,0.0001413964,9.377832e-9,0.000094625444,0.000008664282,0.00008437281,0.00004870722,0.00076055306],"category_scores_gemma":[0.000013729939,0.00010104851,0.000037828864,0.00008237495,0.00012947088,0.000077357516,0.000081490434,0.00006505904,0.000008099954],"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":[0.00009317936,0.00034167958,0.047393054,0.00012660833,0.00007432526,0.0000059503254,0.0011029035,0.012189008,0.5668197,0.00097091513,0.0007604181,0.37012222],"study_design_scores_gemma":[0.0051816087,0.0004509682,0.09648078,0.000985564,0.00030083198,0.00006204818,0.0010868079,0.57291085,0.27333197,0.036055464,0.010296462,0.00285667],"about_ca_topic_score_codex":0.000104398656,"about_ca_topic_score_gemma":0.0000016605794,"teacher_disagreement_score":0.5607218,"about_ca_system_score_codex":0.000054628228,"about_ca_system_score_gemma":0.000011047464,"threshold_uncertainty_score":0.8327523},"labels":[],"label_agreement":null},{"id":"W1829392898","doi":"10.1007/s11069-010-9590-x","title":"A. Chandrasekhar: Basics pf atmospheric science","year":2010,"lang":"en","type":"article","venue":"Natural Hazards","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Chandrasekhar limit; Natural hazard; Hydrogeology; Environmental science; Meteorology; Geology; Geography; Physics; Astronomy; Geotechnical engineering","score_opus":0.00261223700794142,"score_gpt":0.2179713449982497,"score_spread":0.21535910799030827,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1829392898","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":[0.95780313,0.000059484457,0.00013387243,0.0003292356,0.0016834125,0.00013011343,0.0000024003173,0.00010393771,0.039754424],"genre_scores_gemma":[0.9827007,0.000009306388,0.012113288,0.0006068979,0.00018454947,0.000009511589,0.0000020547332,0.000017577879,0.00435611],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99811625,0.000010941551,0.00015917742,0.0004568142,0.000726649,0.0005301645],"domain_scores_gemma":[0.99925035,0.000020924377,0.000066675166,0.00041695315,0.000024164323,0.00022091331],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00032278188,0.00018250321,0.00014142977,7.5205634e-7,0.00041395615,0.00008225001,0.0006577921,0.00010020096,0.005522883],"category_scores_gemma":[0.00009460596,0.00014258697,0.00007236237,0.000777053,0.00097024144,0.00041783784,0.00035527235,0.00052830286,0.0012650483],"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":[0.000037760714,0.00015457919,0.12251114,0.000008563975,0.00001158865,0.00003800799,0.0004768463,0.00013780622,0.3248445,0.0032802157,0.01175734,0.5367417],"study_design_scores_gemma":[0.00092981796,0.00018244113,0.62060714,0.000012945625,0.00003163152,0.00010633133,0.00016353962,0.030212421,0.03396464,0.0013877858,0.31126046,0.001140832],"about_ca_topic_score_codex":0.00014080279,"about_ca_topic_score_gemma":0.000159285,"teacher_disagreement_score":0.53560084,"about_ca_system_score_codex":0.00011671226,"about_ca_system_score_gemma":0.00006425045,"threshold_uncertainty_score":0.99951255},"labels":[],"label_agreement":null},{"id":"W1857669031","doi":"10.1175/jhm-d-15-0087.1","title":"Surface Solar Radiation in North America: A Comparison of Observations, Reanalyses, Satellite, and Derived Products*","year":2015,"lang":"en","type":"article","venue":"Journal of Hydrometeorology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":51,"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":"Rural Development Administration","keywords":"Environmental science; Climatology; Cru; Data assimilation; Shortwave radiation; Satellite; Shortwave; Meteorology; Cloud cover; Atmospheric sciences; Radiation; Geography; Radiative transfer; Cloud computing; Geology","score_opus":0.036087016258842884,"score_gpt":0.26636035269632363,"score_spread":0.23027333643748074,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1857669031","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":[0.9973057,0.0014485955,0.00040105922,0.00058973994,0.00008245234,0.00007341266,0.000001223722,0.0000031360667,0.00009470724],"genre_scores_gemma":[0.98815906,0.0003294426,0.011369861,0.00008208187,0.000017310118,6.5340885e-7,0.0000033300903,0.000006485803,0.000031746666],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988012,0.00014509827,0.00054295186,0.00013311037,0.00022586893,0.00015179534],"domain_scores_gemma":[0.9990997,0.000055815817,0.00059081725,0.00012282879,0.000037477468,0.000093367846],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039724924,0.00008994042,0.0003754692,0.000008826736,0.000024412755,0.000006594913,0.00014020073,0.000052914376,0.00004498065],"category_scores_gemma":[0.00018908629,0.00007544353,0.00003202214,0.0005241453,0.00019143197,0.00019893017,0.0000587342,0.00016003901,0.000006311465],"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":[0.00006697286,0.00011220458,0.95949864,0.0000042435136,0.000022640552,0.000008215967,0.0012552281,0.021146389,0.0119447885,0.00000234164,0.00035674893,0.005581561],"study_design_scores_gemma":[0.0006216815,0.0007528933,0.9878618,0.0000040258087,0.000042135624,0.00003572148,0.00051888666,0.004021628,0.00092954974,0.00011867997,0.005000397,0.00009257036],"about_ca_topic_score_codex":0.0003750079,"about_ca_topic_score_gemma":0.00036646926,"teacher_disagreement_score":0.028363165,"about_ca_system_score_codex":0.00008444036,"about_ca_system_score_gemma":0.000036296744,"threshold_uncertainty_score":0.3076498},"labels":[],"label_agreement":null},{"id":"W1860256609","doi":"10.1002/qj.2438","title":"Assessing the quality of active–passive satellite retrievals using broad‐band radiances","year":2014,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","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; Environment and Climate Change Canada","funders":"","keywords":"Radiative transfer; Remote sensing; Satellite; Environmental science; Radiance; Radiometer; Meteorology; Atmospheric radiative transfer codes; Aerosol; Monte Carlo method; Computer science; Cloud computing; Closure (psychology); Physics; Geology; Mathematics; Statistics","score_opus":0.029908755455419662,"score_gpt":0.3039667405998016,"score_spread":0.27405798514438195,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1860256609","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":[0.99091715,0.00022050331,0.0066203037,0.00082084705,0.00026780766,0.0001122389,0.0000019542283,0.0000060991943,0.0010330981],"genre_scores_gemma":[0.99516404,0.000020910988,0.0040839124,0.00048080023,0.00016872532,9.849574e-7,1.2132882e-7,0.000008275557,0.000072247596],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9971649,0.0009513288,0.00068785885,0.0001964373,0.00069072115,0.0003087673],"domain_scores_gemma":[0.9975988,0.00067006686,0.0012963001,0.0002776836,0.00004802076,0.000109117],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0023602752,0.00017768875,0.0004403028,9.181267e-7,0.0003923782,0.00008413069,0.0007278616,0.0001589932,0.00038614258],"category_scores_gemma":[0.00022755767,0.00008039968,0.00066881144,0.00022921064,0.00086387363,0.00023606024,0.000075604985,0.0004959085,0.0000048309707],"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":[0.000444431,0.0005900662,0.26975012,0.000055264718,0.00063598086,0.000005620472,0.009091859,0.018028831,0.15043253,0.0005382823,0.0014696002,0.5489574],"study_design_scores_gemma":[0.0007785111,0.00088601455,0.9781365,0.00004468118,0.00015308968,0.000018578587,0.0036326575,0.0047377376,0.004226734,0.0052846107,0.0018474193,0.00025346095],"about_ca_topic_score_codex":0.00012590241,"about_ca_topic_score_gemma":0.000005117699,"teacher_disagreement_score":0.70838636,"about_ca_system_score_codex":0.0001365,"about_ca_system_score_gemma":0.000024456816,"threshold_uncertainty_score":0.42279905},"labels":[],"label_agreement":null},{"id":"W1860839844","doi":"10.1002/2014jd022255","title":"Insights from modeling and observational evaluation of a precipitating continental cumulus event observed during the MC3E field campaign","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Climate Program Office; Office of Naval Research; Office of Science","keywords":"Radar; Forcing (mathematics); Meteorology; Environmental science; Cloud computing; Cloud physics; Climatology; Geology; Geography; Computer science","score_opus":0.13029155804490408,"score_gpt":0.34961841938428695,"score_spread":0.21932686133938287,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1860839844","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":[0.99768376,0.0005065201,0.0008094951,0.00036111748,0.000078131285,0.00021279525,0.0000018953044,0.000003692561,0.00034260214],"genre_scores_gemma":[0.9973511,0.000018917994,0.0022656682,0.000030943705,0.0002201632,0.000010900655,0.0000011759706,0.000010633761,0.000090516245],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99625117,0.00048525745,0.00047854916,0.00018076417,0.0023688008,0.00023548276],"domain_scores_gemma":[0.9983012,0.0006714576,0.00025246546,0.00016989616,0.00040474645,0.00020020951],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013525838,0.00011330835,0.00022729395,0.000001374927,0.00018666807,0.00005253184,0.00032048477,0.0000566861,0.00022524752],"category_scores_gemma":[0.0015224515,0.000072593975,0.00009305645,0.00024301054,0.00018399338,0.00035084685,0.0002885097,0.00041283027,0.0000103614375],"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":[0.0016778108,0.00091224106,0.3914543,0.0000394166,0.000300623,0.00003250778,0.011524245,0.4622802,0.104081124,0.0005714116,0.0019936718,0.025132414],"study_design_scores_gemma":[0.0012754494,0.00047202798,0.39715886,0.00009446616,0.000037525308,0.0000035802864,0.0034826207,0.58025795,0.0018258395,0.015234288,0.000050355953,0.00010703551],"about_ca_topic_score_codex":0.002925471,"about_ca_topic_score_gemma":0.00025713997,"teacher_disagreement_score":0.11797774,"about_ca_system_score_codex":0.00021216666,"about_ca_system_score_gemma":0.00014153584,"threshold_uncertainty_score":0.44224563},"labels":[],"label_agreement":null},{"id":"W1864504472","doi":"10.1029/2004gl019502","title":"Sensitivity of Asian dust storm to natural and anthropogenic factors","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":52,"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 Toronto","funders":"Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Desertification; Precipitation; Storm; Dust storm; Environmental science; Natural (archaeology); China; Vegetation (pathology); Chine; Physical geography; Spring (device); Asian Dust; Climatology; Atmospheric sciences; Geology; Geography; Meteorology; Aerosol; Oceanography; Ecology","score_opus":0.018228818335962897,"score_gpt":0.2900949140003002,"score_spread":0.2718660956643373,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1864504472","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":[0.9943713,0.0000065408863,0.00030182104,0.0048919762,0.000050093142,0.00016764153,0.0000051786346,0.000014064759,0.00019136042],"genre_scores_gemma":[0.9990668,0.0000027236397,0.00044661065,0.00034167018,0.000054628174,0.0000040645778,0.0000018393055,0.000010775612,0.00007086747],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9983144,0.00010252281,0.00010210246,0.0003128289,0.00069173035,0.00047642275],"domain_scores_gemma":[0.99941885,0.00010833906,0.000020959831,0.00020822998,0.000012077492,0.00023151306],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000272556,0.00010918841,0.00015209864,0.0000038747703,0.00017094231,0.000021262651,0.00013166964,0.000035199282,0.00012073866],"category_scores_gemma":[0.000111738365,0.00008780191,0.000053530533,0.00036926378,0.00082861714,0.000114977396,0.00034867215,0.00031305055,0.00017762005],"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":[0.00004882794,0.00011939417,0.059846077,0.0000103222155,0.000016926102,0.000051182302,0.0015275396,0.00026703812,0.9274609,0.00022522415,0.0014221121,0.009004474],"study_design_scores_gemma":[0.00019239643,0.00014156471,0.9840937,0.000010166239,0.0000030241224,0.0000020056125,0.00043474825,0.000053743268,0.01435084,0.00015462747,0.00043562878,0.00012750774],"about_ca_topic_score_codex":0.0069511165,"about_ca_topic_score_gemma":0.0004821253,"teacher_disagreement_score":0.9242477,"about_ca_system_score_codex":0.00018353347,"about_ca_system_score_gemma":0.000013756554,"threshold_uncertainty_score":0.9996617},"labels":[],"label_agreement":null},{"id":"W1872372576","doi":"10.5194/acp-15-11729-2015","title":"High ice water content at low radar reflectivity near deep convection – Part 2: Evaluation of microphysical pathways in updraft parcel simulations","year":2015,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"Glenn Research Center; Biological and Environmental Research; Office of Science; National Aeronautics and Space Administration; U.S. Department of Energy","keywords":"Atmospheric sciences; Convection; Environmental science; Liquid water content; Water vapor; Ice nucleus; Ice crystals; Homogeneous; Meteorology; Geology; Chemistry; Physics","score_opus":0.02829685639302053,"score_gpt":0.23653713389063527,"score_spread":0.20824027749761473,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1872372576","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":[0.99782664,0.000032481494,0.0010268682,0.00003491053,0.000060374325,0.00018175533,0.000006660899,0.000017478154,0.00081280596],"genre_scores_gemma":[0.99715894,0.000007294321,0.0022713349,0.000038715156,0.000083854036,0.000018896955,0.000042621192,0.000014508702,0.00036381703],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9987415,0.0000716322,0.00023438511,0.0003300561,0.00039550025,0.00022689997],"domain_scores_gemma":[0.99948055,0.00003617487,0.00009354409,0.00022782169,0.000049286005,0.00011262893],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00022985594,0.0001715485,0.00022270942,2.4226798e-8,0.00011376498,0.000017563125,0.000083671366,0.00009014107,0.0009286104],"category_scores_gemma":[0.000020083537,0.00014616532,0.00005050438,0.00015457856,0.0002491608,0.00014595654,0.00010502641,0.00012043743,0.00003787005],"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":[0.0001615555,0.0005712233,0.03510779,0.000043192285,0.000032694858,0.0000029802618,0.002329124,0.14128095,0.78554285,0.000014660093,0.00013502015,0.034777954],"study_design_scores_gemma":[0.0030155554,0.00013606534,0.038166877,0.000034259472,0.00012737668,0.0000067224337,0.00040145277,0.52680516,0.42711452,0.0027014685,0.0009460548,0.0005445142],"about_ca_topic_score_codex":0.0006299627,"about_ca_topic_score_gemma":0.00004010923,"teacher_disagreement_score":0.38552418,"about_ca_system_score_codex":0.00032598458,"about_ca_system_score_gemma":0.000029844205,"threshold_uncertainty_score":0.9999847},"labels":[],"label_agreement":null},{"id":"W1878184188","doi":"10.1175/jas-d-15-0211.1","title":"Expansion of a Holepunch Cloud by a Gravity Wave Front","year":2015,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Front (military); Physics; Mechanics; Gravity current; Cloud computing; Cloud physics; Geology; Meteorology; Internal wave; Law","score_opus":0.020598632215334003,"score_gpt":0.2343183327852298,"score_spread":0.21371970056989578,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1878184188","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":[0.99374986,0.0004910817,0.0008427059,0.0008613914,0.0009071317,0.000087683555,0.0000011482371,0.00000541384,0.0030536114],"genre_scores_gemma":[0.9848608,0.000032437805,0.013753056,0.00029360203,0.00008574085,0.000001141646,5.6022813e-8,0.0000065569325,0.00096665474],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99777174,0.0001249467,0.00044972007,0.00017857089,0.0012167053,0.00025830852],"domain_scores_gemma":[0.9987658,0.000051619223,0.0007090488,0.00024128906,0.000046470723,0.00018571707],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013983595,0.00013551133,0.00026597,3.8084636e-7,0.00017500523,0.00003357162,0.0009176162,0.00005404498,0.00038608297],"category_scores_gemma":[0.00017296895,0.00007153772,0.000166814,0.000529278,0.000930312,0.00030187855,0.00030796917,0.000163181,0.000024137651],"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":[0.00024667563,0.00065211934,0.4424824,0.00001539533,0.00007008159,0.000027454185,0.0068699988,0.05433108,0.05829032,0.0001474719,0.4100902,0.02677676],"study_design_scores_gemma":[0.009980962,0.012879226,0.42563903,0.000812864,0.00068240555,0.001797765,0.04081937,0.16191784,0.07973768,0.054152112,0.20835078,0.0032299708],"about_ca_topic_score_codex":0.00043788264,"about_ca_topic_score_gemma":0.000014329705,"teacher_disagreement_score":0.20173943,"about_ca_system_score_codex":0.00014121208,"about_ca_system_score_gemma":0.00012434619,"threshold_uncertainty_score":0.42273378},"labels":[],"label_agreement":null},{"id":"W1882732971","doi":"10.1007/s10661-015-4806-x","title":"A new inventory for middle east dust source points","year":2015,"lang":"en","type":"article","venue":"Environmental Monitoring and Assessment","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":51,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Dust storm; Storm; Moderate-resolution imaging spectroradiometer; Environmental science; Middle East; Mineral dust; Spectroradiometer; Climatology; High resolution; Meteorology; Atmospheric sciences; Physical geography; Geography; Satellite; Geology; Remote sensing; Aerosol; Reflectivity; Physics","score_opus":0.03852265911923125,"score_gpt":0.25673854846782324,"score_spread":0.21821588934859198,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1882732971","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":[0.987704,0.00021314477,0.008324307,0.00024263047,0.00046170727,0.000272937,0.0000046760233,0.000044073684,0.00273256],"genre_scores_gemma":[0.9615919,0.000031469077,0.030944522,0.000051196377,0.0003469958,0.000050143215,0.000006278667,0.000029937886,0.0069475714],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99875546,0.000027043761,0.00018013909,0.00036836008,0.000348134,0.00032088254],"domain_scores_gemma":[0.9992824,0.00001634992,0.0000748757,0.00018991705,0.0000010411972,0.00043538344],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018007286,0.00019355665,0.00015171854,0.0000021036562,0.00016564783,0.000046824993,0.00014063308,0.00006503265,0.00028619866],"category_scores_gemma":[0.00000565542,0.00018366783,0.000054348635,0.000042871765,0.00010016328,0.00016096667,0.00025477202,0.00012684114,0.00010204321],"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":[0.000026385862,0.00015209506,0.9411935,0.000006879666,0.000022720744,0.0000038496164,0.0011191672,0.00039416802,0.0032989143,0.000026977272,0.003559145,0.050196197],"study_design_scores_gemma":[0.004057531,0.0009517177,0.69612586,0.00008288322,0.00009668261,0.000030183193,0.013363827,0.0029787677,0.0029571243,0.00097188394,0.27730665,0.0010769088],"about_ca_topic_score_codex":0.00016068108,"about_ca_topic_score_gemma":0.0000020731552,"teacher_disagreement_score":0.2737475,"about_ca_system_score_codex":0.0004132635,"about_ca_system_score_gemma":0.000018037335,"threshold_uncertainty_score":0.7489757},"labels":[],"label_agreement":null},{"id":"W1884808726","doi":"","title":"Determination of the atmospheric optical depth due to the El Chichon stratospheric aerosol cloud in the polluted atmosphere of Mexico City","year":2009,"lang":"en","type":"article","venue":"Atmósfera","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"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; Volcano; Environmental science; Atmosphere (unit); Atmospheric sciences; Volcanic ash; Mexico city; Vulcanian eruption; Meteorology; Climatology; Geology; Geography","score_opus":0.008566529766155882,"score_gpt":0.23362258777425357,"score_spread":0.2250560580080977,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1884808726","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":[0.9825501,0.00006765464,0.002925334,0.0027189509,0.00018125132,0.0007586699,0.00000415399,0.00002041955,0.010773494],"genre_scores_gemma":[0.9939422,0.000015945112,0.0041717617,0.0015768418,0.000063778876,0.000029335739,0.0000014101195,0.000017399314,0.00018131248],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99771154,0.00022542063,0.0005385778,0.00037351705,0.0007205227,0.00043041905],"domain_scores_gemma":[0.99870825,0.00011912246,0.00021136909,0.0008526299,0.000023535158,0.0000850979],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004925799,0.00026768196,0.00032333506,2.789272e-7,0.00020574116,0.000033620287,0.0011921737,0.0001402215,0.00043554066],"category_scores_gemma":[0.00010075774,0.0001388298,0.00017265278,0.0012406922,0.00030424647,0.00013609968,0.00019335188,0.0003241651,0.000038540045],"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":[0.0004834374,0.0024057915,0.5370665,0.000047285692,0.000075188145,0.000050826053,0.01712318,0.04986446,0.039134875,0.0038783744,0.005865393,0.3440047],"study_design_scores_gemma":[0.00044588212,0.00036771566,0.98517483,0.00003444061,0.00003494819,0.000023397377,0.0008449844,0.0074109477,0.00429305,0.0005934772,0.0005521363,0.00022416437],"about_ca_topic_score_codex":0.000450473,"about_ca_topic_score_gemma":0.0015980809,"teacher_disagreement_score":0.44810835,"about_ca_system_score_codex":0.00011638414,"about_ca_system_score_gemma":0.000041159503,"threshold_uncertainty_score":0.56613153},"labels":[],"label_agreement":null},{"id":"W1889819234","doi":"10.1029/2010gl043995","title":"Summertime trans‐Pacific transport of Asian dust","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":45,"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":"Outflow; Lidar; Atmosphere (unit); Asian Dust; Storm; Geology; Mineral dust; Altitude (triangle); Anomaly (physics); Environmental science; Atmospheric sciences; Aeolian processes; Dust storm; Climatology; Oceanography; Meteorology; Aerosol; Geomorphology; Geography; Remote sensing","score_opus":0.016889186776487583,"score_gpt":0.2730968929384584,"score_spread":0.2562077061619708,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1889819234","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":[0.97201824,0.0000022546587,0.00029244678,0.0071388287,0.000080360376,0.00018799122,0.00000712404,0.000023968754,0.020248769],"genre_scores_gemma":[0.99794203,0.000003334816,0.00065557053,0.00020137073,0.000110240726,0.00002179558,0.000005114511,0.000020251984,0.0010403102],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9977081,0.00006866255,0.00019988684,0.00036721348,0.001009586,0.0006465411],"domain_scores_gemma":[0.99921095,0.00008181261,0.000029709694,0.00041032498,0.000014788738,0.0002524343],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00036746715,0.00013145042,0.00018819916,0.000004120603,0.00014768555,0.000014262998,0.00047196474,0.00008019441,0.004051854],"category_scores_gemma":[0.000028540038,0.00011119953,0.00013255628,0.0004861141,0.0012579273,0.00013457678,0.00006310525,0.0007811336,0.00076196203],"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":[0.000046282486,0.00018436069,0.022871727,0.0000097687225,0.000010497579,0.000024402043,0.0005114198,0.000016518403,0.9586228,0.00023140537,0.006564086,0.01090671],"study_design_scores_gemma":[0.0005599157,0.00024432447,0.9277086,0.000013771966,0.000013876251,0.0000033631575,0.00034216998,0.00034631134,0.025468111,0.0006507759,0.04430073,0.00034804727],"about_ca_topic_score_codex":0.0010857699,"about_ca_topic_score_gemma":0.00011056495,"teacher_disagreement_score":0.9331547,"about_ca_system_score_codex":0.000034139946,"about_ca_system_score_gemma":0.000017463437,"threshold_uncertainty_score":0.9968586},"labels":[],"label_agreement":null},{"id":"W1895555186","doi":"10.5194/acp-16-9255-2016","title":"Theoretical investigation of mixing in warm clouds – Part 2: Homogeneousmixing","year":2016,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":42,"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":"Office of Science; Israel Science Foundation; U.S. Department of Energy","keywords":"Mixing (physics); Homogeneous; Supersaturation; Dispersity; Constant (computer programming); Evaporation; Chemistry; Thermodynamics; Physics","score_opus":0.005437279967396893,"score_gpt":0.19223976758442948,"score_spread":0.18680248761703258,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1895555186","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":[0.98991567,0.00004895385,0.0024470245,0.000097814576,0.000023132081,0.000051326813,0.00000217006,0.000016013923,0.0073978663],"genre_scores_gemma":[0.99134743,0.00006758813,0.007872122,0.000056563364,0.00007560863,0.000007909607,0.0000016425823,0.000012032948,0.0005590802],"study_design_codex":"design_other","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9991939,0.000019441077,0.00019737355,0.00024509509,0.00014721254,0.00019695482],"domain_scores_gemma":[0.9995923,0.00007430593,0.00007065141,0.00017476222,0.000005585785,0.00008241436],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00010913088,0.00012707135,0.00015277037,9.133179e-9,0.000043570813,0.000007055664,0.00010862242,0.00007003169,0.0032563682],"category_scores_gemma":[0.000017143115,0.000094434625,0.00003747358,0.00015793859,0.00055836886,0.00007921789,0.000082887906,0.000066248285,0.00001694471],"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":[0.000030949934,0.00006414475,0.2750626,0.000048469174,0.000013240601,0.0000068460554,0.00047744994,0.00037780058,0.3328171,0.0018575311,0.00016213658,0.38908175],"study_design_scores_gemma":[0.002325332,0.00015909887,0.073285535,0.00047377264,0.000073795825,0.000036844023,0.00033728947,0.0202053,0.78598523,0.110436246,0.005390843,0.0012907177],"about_ca_topic_score_codex":0.000038097678,"about_ca_topic_score_gemma":0.0000014988738,"teacher_disagreement_score":0.45316812,"about_ca_system_score_codex":0.00004992999,"about_ca_system_score_gemma":0.000010942324,"threshold_uncertainty_score":0.9976548},"labels":[],"label_agreement":null},{"id":"W1896388910","doi":"10.1029/2003gc000655","title":"Particles in the great Pinatubo volcanic cloud of June 1991: The role of ice","year":2004,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":97,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Aeronautics and Space Administration; National Science Foundation","keywords":"Volcanic ash; Volcano; Atmospheric sciences; Geology; Vulcanian eruption; Sulfate; Satellite; Advanced very-high-resolution radiometer; Phreatic eruption; Environmental science; Climatology; Magma; Geochemistry","score_opus":0.0043137148972371645,"score_gpt":0.18794768054687436,"score_spread":0.1836339656496372,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1896388910","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":[0.9933955,0.00037835047,0.000023468607,0.00020371162,0.00008919571,0.00021190496,0.000016071697,0.000011522162,0.0056702667],"genre_scores_gemma":[0.9995395,0.000017703342,0.000033464326,0.000045046294,0.000115570685,0.00003303769,0.000008221288,0.000010803424,0.00019664018],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9985655,0.000052651812,0.00037067485,0.00024648683,0.0004474382,0.00031724625],"domain_scores_gemma":[0.9989675,0.0000862306,0.00025072912,0.00063465623,0.000017521152,0.000043346838],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003146897,0.00017068561,0.00023863917,8.335449e-7,0.000091855014,0.000014826724,0.00064161693,0.00007785106,0.000108448934],"category_scores_gemma":[0.000026275235,0.000106542415,0.00011129655,0.0004067941,0.00029838778,0.00006716843,0.00015643041,0.00017327476,0.000059668557],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011089801,0.0009881814,0.070141055,0.00033745062,0.00009889545,0.00002010888,0.010029311,0.0184322,0.888021,0.004276871,0.00094012055,0.0066039073],"study_design_scores_gemma":[0.0029505277,0.0004371036,0.08715467,0.0004790499,0.00021753776,0.00007410246,0.030720236,0.004680962,0.7752317,0.076753795,0.020050492,0.0012497945],"about_ca_topic_score_codex":0.0069102226,"about_ca_topic_score_gemma":0.0004085656,"teacher_disagreement_score":0.11278927,"about_ca_system_score_codex":0.0000675772,"about_ca_system_score_gemma":0.000023708906,"threshold_uncertainty_score":0.9997029},"labels":[],"label_agreement":null},{"id":"W1903891751","doi":"10.1002/2014gl060213","title":"Laboratory chamber measurements of the longwave extinction spectra and complex refractive indices of African and Asian mineral dusts","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":44,"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 Toronto","funders":"University of Toronto; Centre National d’Etudes Spatiales","keywords":"Longwave; Mineral dust; Extinction (optical mineralogy); Particle-size distribution; Environmental science; Atmospheric sciences; Radiative transfer; Asian Dust; Particle (ecology); Particle size; Range (aeronautics); Aerosol; Mineralogy; Materials science; Chemistry; Geology; Physics; Optics; Meteorology","score_opus":0.031821677335439814,"score_gpt":0.2798729614333008,"score_spread":0.248051284097861,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1903891751","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":[0.99474066,0.0000056683825,0.00004797821,0.0019209968,0.000022850449,0.00015107832,0.0000029920513,0.0000036744675,0.003104084],"genre_scores_gemma":[0.99942744,0.0000023132634,0.0002499786,0.00017629826,0.000053857686,0.000006820709,7.216323e-7,0.0000071417367,0.00007544053],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99840987,0.00026342808,0.00012126572,0.00022220815,0.00073480495,0.00024844802],"domain_scores_gemma":[0.9995237,0.00009519637,0.0000828465,0.00018452352,0.000024393621,0.00008934162],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042795704,0.00008332459,0.00013671027,0.0000035741396,0.00011745671,0.000014410659,0.00011653474,0.00003175901,0.0001078545],"category_scores_gemma":[0.000095241754,0.000057916946,0.000025889487,0.0002822052,0.0010802168,0.000099231605,0.00021725545,0.00021334743,0.0000088674],"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":[0.00007030661,0.00010660514,0.13054003,0.000022281023,0.000023395507,0.000001416852,0.0010491721,0.000016559303,0.8603186,0.000056320696,0.0013522225,0.0064430647],"study_design_scores_gemma":[0.00022089753,0.00012632957,0.99227345,0.000012043884,0.0000059875383,6.154755e-7,0.0002261169,0.00022865807,0.006086905,0.00012658823,0.0006293843,0.000063006526],"about_ca_topic_score_codex":0.0008333725,"about_ca_topic_score_gemma":0.00009006399,"teacher_disagreement_score":0.86173344,"about_ca_system_score_codex":0.000054352753,"about_ca_system_score_gemma":0.000008643169,"threshold_uncertainty_score":0.39801037},"labels":[],"label_agreement":null},{"id":"W1916944651","doi":"10.5194/amt-8-3789-2015","title":"Synchronous polar winter starphotometry and lidar measurements at a High Arctic station","year":2015,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University; Université de Sherbrooke","funders":"Eurostars; Natural Sciences and Engineering Research Council of Canada; Fonds de recherche du Québec – Nature et technologies; Canadian Space Agency; Fonds Québécois de la Recherche sur la Nature et les Technologies; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Lidar; Sun photometer; Environmental science; Aerosol; Photometer; Photometry (optics); Remote sensing; Backscatter (email); Atmospheric sciences; Meteorology; Physics; Stars; Geology; Optics; Astrophysics","score_opus":0.02827186661385337,"score_gpt":0.23585013133295887,"score_spread":0.2075782647191055,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1916944651","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":[0.968823,0.0006229353,0.021292457,0.0002503002,0.00020822547,0.0010028429,0.000007046648,0.00047623806,0.0073169624],"genre_scores_gemma":[0.9261884,0.000055131048,0.072480105,0.00055070146,0.00005350598,0.00013374358,0.000009744974,0.000054838474,0.00047383452],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99645746,0.0001529956,0.00044792544,0.0006457611,0.0017601157,0.0005357298],"domain_scores_gemma":[0.9987512,0.000017424056,0.00022382122,0.0004916138,0.00012949479,0.000386437],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013511677,0.0003842244,0.00033648344,0.0000016435066,0.00020765951,0.000075549564,0.00030362807,0.00014218768,0.0013760977],"category_scores_gemma":[0.0001471865,0.00034435425,0.00007007964,0.00039505505,0.00023214256,0.00034702502,0.0003640631,0.00017738804,0.0002221629],"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":[0.00021758115,0.00041502732,0.8886798,0.00006836156,0.0001464605,0.000027450196,0.0010655207,0.00006990265,0.04560306,0.00002548182,0.018813448,0.04486789],"study_design_scores_gemma":[0.0052391086,0.0053390088,0.70454496,0.00060468307,0.0005955811,0.00018810667,0.001631539,0.0013807956,0.122481816,0.004862349,0.1488391,0.0042929784],"about_ca_topic_score_codex":0.003658305,"about_ca_topic_score_gemma":0.0004525687,"teacher_disagreement_score":0.18413489,"about_ca_system_score_codex":0.0024256809,"about_ca_system_score_gemma":0.000053670163,"threshold_uncertainty_score":0.9999008},"labels":[],"label_agreement":null},{"id":"W1928949504","doi":"10.1002/9783527600441.oe044","title":"Lidar (Laser Radar)","year":2007,"lang":"en","type":"other","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Lidar; Remote sensing; Radar; Atmosphere (unit); Wave radar; Laser; Environmental science; Radar imaging; Geology; Meteorology; Computer science; Radar engineering details; Geography; Physics; Optics; Telecommunications","score_opus":0.0058759757356705525,"score_gpt":0.2140123373137464,"score_spread":0.20813636157807583,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1928949504","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00013427949,0.00008325454,0.0023948199,0.000040117226,0.00019848719,0.00010819958,0.0000023658365,0.00017755436,0.9968609],"genre_scores_gemma":[0.00051223673,0.00003737586,0.011660216,0.00076311943,0.00018144796,0.000002845444,0.0000044170106,0.0002273665,0.98661095],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99915755,0.0000070398946,0.000095638345,0.0002617137,0.00024308825,0.00023494291],"domain_scores_gemma":[0.99957484,0.000006249294,0.000056659665,0.00026803566,5.7358875e-7,0.00009366782],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000057988487,0.0001696709,0.00013833145,0.0000011728333,0.000025183695,0.000010090474,0.00019563077,0.00021011352,0.58081675],"category_scores_gemma":[0.0000025066015,0.00013024834,0.00005543132,0.00011990078,0.00011411603,0.00001545663,0.00012389793,0.000104862476,0.023715887],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000011311486,0.000017627097,0.0015107344,0.0000022131694,0.000006403873,0.000011073764,0.000007303478,5.890171e-7,0.000013387561,0.000057302193,0.9856478,0.0127244415],"study_design_scores_gemma":[0.00007745284,0.000014192218,0.00058908336,0.000007721785,0.0000068732625,0.0000018249577,0.000013581031,0.0000048267807,0.000061598184,0.000025422547,0.9990059,0.00019152203],"about_ca_topic_score_codex":0.0011624721,"about_ca_topic_score_gemma":0.00041093552,"teacher_disagreement_score":0.5571009,"about_ca_system_score_codex":0.00004924587,"about_ca_system_score_gemma":0.0000043021755,"threshold_uncertainty_score":0.9770443},"labels":[],"label_agreement":null},{"id":"W1929218345","doi":"10.1029/2001jd001429","title":"A Parameterization of cirrus cloud formation: Homogeneous freezing including effects of aerosol size","year":2002,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":181,"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","funders":"","keywords":"Cirrus; Aerosol; Ice crystals; Atmospheric sciences; Troposphere; Cloud physics; Ice nucleus; Tropopause; Nucleation; Environmental science; Supercooling; Homogeneous; Liquid water content; Climate model; Climatology; Meteorology; Geology; Cloud computing; Climate change; Physics; Statistical physics; Thermodynamics","score_opus":0.03292594639912274,"score_gpt":0.28861248716846766,"score_spread":0.25568654076934494,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1929218345","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":[0.99469054,0.00039708888,0.0031417601,0.00010109115,0.00012728579,0.0002184599,0.0000017091078,0.000007350126,0.0013147176],"genre_scores_gemma":[0.99308175,0.0002690702,0.006109698,0.000024143845,0.00019496781,0.000006313207,3.1196876e-7,0.000019367466,0.00029439566],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9969175,0.00027726876,0.0006999828,0.00017355333,0.0015029497,0.00042877492],"domain_scores_gemma":[0.9975251,0.001276273,0.00055864983,0.00026397346,0.00016797746,0.00020802875],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00053461775,0.00015497704,0.00043937302,0.0000026601406,0.00016783692,0.00003380503,0.0004989207,0.00009315066,0.0010209342],"category_scores_gemma":[0.0011742695,0.00012401855,0.00021822193,0.0007132307,0.00045860335,0.00040295234,0.00031593267,0.00040651704,0.000054309177],"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":[0.00034918584,0.0014309257,0.0103307795,0.00046220538,0.00016040537,0.00014182436,0.003143696,0.006116756,0.8988673,0.00021337549,0.0053469427,0.07343657],"study_design_scores_gemma":[0.004817168,0.011089093,0.047805883,0.0014628164,0.00018852533,0.00018631922,0.0018427818,0.078751884,0.8447122,0.0064100577,0.0018194563,0.0009138151],"about_ca_topic_score_codex":0.000310478,"about_ca_topic_score_gemma":0.000017018652,"teacher_disagreement_score":0.07263513,"about_ca_system_score_codex":0.0001595373,"about_ca_system_score_gemma":0.000024499896,"threshold_uncertainty_score":0.9998923},"labels":[],"label_agreement":null},{"id":"W1933585260","doi":"10.1007/s40641-015-0026-2","title":"Cloud Phase Changes Induced by CO2 Warming—a Powerful yet Poorly Constrained Cloud-Climate Feedback","year":2015,"lang":"en","type":"article","venue":"Current Climate Change Reports","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":99,"is_retracted":false,"has_abstract":false,"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":"Cloud feedback; Cloud computing; Environmental science; Climate model; Climatology; Positive feedback; Global warming; Mechanism (biology); Cloud forcing; Phase (matter); Atmospheric sciences; Negative feedback; Arctic; The arctic; Climate sensitivity; Climate change; Meteorology; Computer science; Geology; Geography; Physics; Oceanography; Engineering","score_opus":0.06448000260699577,"score_gpt":0.3113892934029071,"score_spread":0.24690929079591134,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1933585260","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":[0.98002696,0.001678212,0.000041040745,0.00083571125,0.0069606095,0.0010462536,0.0002658219,0.00031435298,0.00883106],"genre_scores_gemma":[0.9963533,0.001379163,0.00013547383,0.00045443192,0.00081679877,0.00016893962,0.00031116363,0.00010392058,0.000276769],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99544185,0.000112836366,0.0008463446,0.0011304378,0.0009828205,0.0014857085],"domain_scores_gemma":[0.9972727,0.000047439262,0.0008659012,0.00083353283,0.00006607309,0.00091438845],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0010695405,0.0006566572,0.0006785308,0.000010807409,0.00027787616,0.00012738034,0.00036597106,0.00024079,0.002717073],"category_scores_gemma":[0.00012177966,0.0006023713,0.00016731319,0.00048745048,0.00040339405,0.00036514475,0.00069787755,0.00040422904,0.00087482703],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010113826,0.0070033064,0.14660901,0.00080881146,0.0002070773,0.0030229585,0.018426435,0.000029189774,0.057272658,0.0004330311,0.40602526,0.3591509],"study_design_scores_gemma":[0.010470782,0.0040529817,0.005648767,0.0010000136,0.0004950529,0.0020061794,0.0072024884,0.0015518995,0.015382085,0.0009950626,0.9457023,0.0054923454],"about_ca_topic_score_codex":0.00018467549,"about_ca_topic_score_gemma":0.0000777013,"teacher_disagreement_score":0.5396771,"about_ca_system_score_codex":0.0004049197,"about_ca_system_score_gemma":0.000044412198,"threshold_uncertainty_score":0.9999031},"labels":[],"label_agreement":null},{"id":"W1939433415","doi":"","title":"Understanding the Role of the Saharan Heat Low in Modifying Atmospheric Dust Distributions - Observations From Two Research Aircraft Flying Simultaneously Over Western Africa","year":2012,"lang":"en","type":"article","venue":"HAL (Le Centre pour la Communication Scientifique Directe)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"","keywords":"Climatology; Environmental science; Monsoon; Climate model; Lidar; Boreal; Climate change; Meteorology; Aerosol; Low-pressure area; Satellite; Mediterranean climate; Geography; Geology; Atmospheric pressure; Remote sensing; Oceanography","score_opus":0.05353007808748851,"score_gpt":0.25927669679463355,"score_spread":0.20574661870714506,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1939433415","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":[0.93574446,0.00050715014,0.054229714,0.0022770476,0.00006358474,0.0003325975,0.000029181912,0.000034641078,0.0067815892],"genre_scores_gemma":[0.9957487,0.00005989072,0.0031486338,0.000035320383,0.000016214304,0.000030103924,0.000021835047,0.000019172467,0.0009201568],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99616265,0.002182309,0.00032798824,0.00029143936,0.00055472925,0.00048085995],"domain_scores_gemma":[0.99678737,0.0018721553,0.00012081471,0.001003197,0.0001061056,0.00011035313],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0027150777,0.00014565051,0.00015068564,0.0000029573273,0.0010829932,0.00010892479,0.0008768278,0.00007624245,0.0003763995],"category_scores_gemma":[0.000564249,0.00010730901,0.00009091405,0.0010614804,0.0005366839,0.00027199317,0.0007220645,0.00040195102,0.000030234536],"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":[0.000007709507,0.00031598163,0.9516037,0.000006389882,0.000016422338,6.5022783e-7,0.018809335,0.003924829,0.015334184,0.0074961656,0.000171551,0.0023130802],"study_design_scores_gemma":[0.00067057763,8.631642e-7,0.75880814,0.00049442856,0.000030674615,0.0000037057139,0.0045689377,0.21559066,0.0061126654,0.005739973,0.007639742,0.00033965873],"about_ca_topic_score_codex":0.008519554,"about_ca_topic_score_gemma":0.00650587,"teacher_disagreement_score":0.21166582,"about_ca_system_score_codex":0.00047841467,"about_ca_system_score_gemma":0.00004283137,"threshold_uncertainty_score":0.9980828},"labels":[],"label_agreement":null},{"id":"W1946195610","doi":"10.1002/2013jd020386","title":"On using the relationship between Doppler velocity and radar reflectivity to identify microphysical processes in midlatitudinal ice clouds","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"McGill University","funders":"","keywords":"Radar; Doppler effect; Power law; Ice cloud; Reflectivity; Doppler radar; Meteorology; Atmospheric sciences; Environmental science; Computational physics; Remote sensing; Physics; Geology; Optics; Mathematics; Statistics; Radiative transfer","score_opus":0.0818497118224831,"score_gpt":0.3836233148772865,"score_spread":0.3017736030548034,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1946195610","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":[0.9967291,0.00005154757,0.00072879327,0.0018086276,0.000036961068,0.00034078103,0.0000016139753,0.000005633051,0.00029694007],"genre_scores_gemma":[0.99510396,0.000008399745,0.004301352,0.000102595455,0.00027602527,0.000012537884,2.5489183e-7,0.000018268871,0.00017661933],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9971174,0.0004405714,0.0003945611,0.00030759553,0.0012142747,0.0005256002],"domain_scores_gemma":[0.996795,0.0023791986,0.00015683119,0.00022970929,0.00013697868,0.00030230358],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009825099,0.00017550903,0.0003143279,0.00000390985,0.00041760868,0.00016935717,0.00046360225,0.000085488646,0.00021934502],"category_scores_gemma":[0.0018104117,0.00011305155,0.00007735315,0.0011661228,0.00046171935,0.00043921554,0.00036417894,0.001114147,0.0001716235],"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":[0.0002966503,0.00047572737,0.965714,0.00004730303,0.000040649793,0.000030882078,0.0011091913,0.0012212183,0.018330798,0.00042049328,0.0059235077,0.0063895746],"study_design_scores_gemma":[0.00030103885,0.0005179191,0.9811501,0.00008488235,0.000011263374,0.000008580861,0.00027616406,0.00034199486,0.000476628,0.01652082,0.00018012698,0.00013048272],"about_ca_topic_score_codex":0.0039053047,"about_ca_topic_score_gemma":0.0002085905,"teacher_disagreement_score":0.01785417,"about_ca_system_score_codex":0.0003403231,"about_ca_system_score_gemma":0.000111907626,"threshold_uncertainty_score":0.59036785},"labels":[],"label_agreement":null},{"id":"W1948277581","doi":"10.1002/met.289","title":"Lidar studies of the polar troposphere","year":2011,"lang":"en","type":"article","venue":"Meteorological Applications","topic":"Atmospheric aerosols and clouds","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":"Dalhousie University","funders":"","keywords":"Lidar; Troposphere; Environmental science; Polar; Trace gas; Arctic; The arctic; Remote sensing; Meteorology; Tropospheric ozone; Geology; Geography","score_opus":0.03770336357213998,"score_gpt":0.2537079522432803,"score_spread":0.2160045886711403,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1948277581","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":[0.94080544,0.00036556346,0.008548278,0.00042469506,0.000033813827,0.00040589203,0.0000060076727,0.000043769734,0.049366552],"genre_scores_gemma":[0.9859189,0.000034122557,0.01291842,0.0002929598,0.000013619083,0.00015087616,3.7932722e-7,0.000004434473,0.0006662829],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99936885,0.000040369578,0.00015907652,0.00017243017,0.00012741615,0.00013186864],"domain_scores_gemma":[0.9995155,0.000036702495,0.000080419995,0.00032045165,0.000009126289,0.000037819576],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000102299346,0.000076185985,0.00011830646,2.741667e-7,0.00015246624,0.0000021269448,0.0003280014,0.000048559185,0.0032713313],"category_scores_gemma":[0.000025824924,0.000039980903,0.00007363038,0.0002256936,0.00059422455,0.00002728759,0.00025700466,0.00008028851,0.00023934481],"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":[0.000039485865,0.00091122865,0.85569793,0.000015466763,0.00012040962,0.000001496269,0.0018342051,0.000117924166,0.028538255,0.06908702,0.0045312066,0.03910534],"study_design_scores_gemma":[0.00014271302,0.00015570605,0.9007803,0.000002409098,0.000055574983,0.0000033283077,0.0005934217,0.00003568987,0.0059063155,0.04323259,0.048941724,0.00015020593],"about_ca_topic_score_codex":0.000085060274,"about_ca_topic_score_gemma":0.000024283438,"teacher_disagreement_score":0.04870027,"about_ca_system_score_codex":0.000023588978,"about_ca_system_score_gemma":0.0000030203996,"threshold_uncertainty_score":0.99763983},"labels":[],"label_agreement":null},{"id":"W1954481479","doi":"10.1002/joc.4102","title":"AVHRR warm‐season cloud climatologies under various synoptic regimes across the Iberian Peninsula and the Balearic Islands","year":2014,"lang":"en","type":"article","venue":"International Journal of Climatology","topic":"Atmospheric aerosols and clouds","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":"Canarie","funders":"Ministerio de Economía y Competitividad; European Commission","keywords":"Climatology; Advanced very-high-resolution radiometer; Environmental science; Peninsula; Spatial distribution; Meteorology; Geography; Geology; Remote sensing; Satellite","score_opus":0.006238108948854586,"score_gpt":0.25315566426365704,"score_spread":0.24691755531480244,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1954481479","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":[0.9674773,0.00035926802,0.004527411,0.019603416,0.0011790964,0.00008806223,0.0000028949328,0.000013948533,0.0067485753],"genre_scores_gemma":[0.9966373,0.00046108803,0.0005910822,0.0018074779,0.00018644473,0.0000047225,0.0000011930858,0.000012745058,0.00029794266],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99834615,0.00027643534,0.00046819024,0.00017662154,0.00044121264,0.00029140912],"domain_scores_gemma":[0.9983739,0.0007945149,0.00050338753,0.00020325497,0.000058729023,0.00006620938],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009175346,0.00015553413,0.00031732663,0.000003933407,0.00023542854,0.000117116615,0.00088086404,0.000101388636,0.00036338242],"category_scores_gemma":[0.00029180918,0.00007937228,0.00013271508,0.00008150486,0.0012186914,0.00014912851,0.0004124134,0.00033906373,0.00007662903],"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":[0.0018167233,0.00024338959,0.81738013,0.000016888524,0.00063855323,0.00020938598,0.0069526806,0.003216311,0.00031947665,0.14701734,0.01139592,0.010793174],"study_design_scores_gemma":[0.017255208,0.0010607153,0.58354014,0.00015868628,0.0004609182,0.03223272,0.011949865,0.042491514,0.00037064284,0.12644511,0.18288153,0.0011529538],"about_ca_topic_score_codex":0.00007824859,"about_ca_topic_score_gemma":0.00005246995,"teacher_disagreement_score":0.23384003,"about_ca_system_score_codex":0.000059589325,"about_ca_system_score_gemma":0.00001887059,"threshold_uncertainty_score":0.4490319},"labels":[],"label_agreement":null},{"id":"W1959474333","doi":"10.1002/qj.2491","title":"Improving the modelling of short‐wave radiation through the use of a 3D scene construction algorithm","year":2014,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":24,"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 Aeronautics and Space Administration","keywords":"Radiance; Remote sensing; Environmental science; Lidar; Cloud top; Atmospheric radiative transfer codes; Satellite; Radiative transfer; Nadir; Moderate-resolution imaging spectroradiometer; Meteorology; Footprint; Liquid water path; Irradiance; Radiant energy; Radiation; Aerosol; Geology; Physics; Optics","score_opus":0.02930958072595297,"score_gpt":0.21206797582666218,"score_spread":0.1827583951007092,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1959474333","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":[0.564156,0.000060542174,0.43510902,0.00034674886,0.00016149752,0.000101275604,0.0000020434445,0.0000035782873,0.000059268074],"genre_scores_gemma":[0.9025888,0.000021909918,0.09699457,0.0002481863,0.0001173394,0.0000020588657,2.0484123e-7,0.0000063908246,0.000020550135],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99829435,0.00034528744,0.00054252753,0.00013450968,0.00048379347,0.0001995495],"domain_scores_gemma":[0.9986248,0.0003416068,0.00070098764,0.0002500104,0.000042146683,0.00004043551],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00094241096,0.00013052684,0.00025840543,6.6543777e-7,0.00026346237,0.000030374858,0.00039140973,0.000118904296,0.000121343735],"category_scores_gemma":[0.00004911167,0.00005345847,0.00041589857,0.0001306909,0.00071523513,0.00015727298,0.000071629605,0.0003745228,0.0000013912926],"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":[0.000055715238,0.00009997423,0.0041141054,0.000007651111,0.00011426083,5.022107e-7,0.0029008994,0.34587026,0.0019319832,0.0001915932,0.00032615583,0.6443869],"study_design_scores_gemma":[0.00028997,0.0008508902,0.00621175,0.000012703564,0.00013794756,0.000023331935,0.0010225702,0.9880205,0.0005495856,0.0022141133,0.00057064334,0.00009600674],"about_ca_topic_score_codex":0.0002293178,"about_ca_topic_score_gemma":0.0000025104075,"teacher_disagreement_score":0.6442909,"about_ca_system_score_codex":0.000064371685,"about_ca_system_score_gemma":0.000012332427,"threshold_uncertainty_score":0.26353136},"labels":[],"label_agreement":null},{"id":"W1964083645","doi":"10.1364/ao.51.002264","title":"Experimental validation of the MODTRAN 53 sea surface radiance model using MIRAMER campaign measurements","year":2012,"lang":"en","type":"article","venue":"Applied Optics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Defence Research and Development Canada; Agriculture Environmental Renewal Canada (Canada)","funders":"","keywords":"MODTRAN; Radiance; Bidirectional reflectance distribution function; Remote sensing; Radiative transfer; Atmosphere (unit); Environmental science; Atmospheric correction; Geology; Optics; Meteorology; Physics; Reflectivity","score_opus":0.048432003738353754,"score_gpt":0.2551790805958996,"score_spread":0.20674707685754584,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1964083645","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":[0.97856086,0.00004950807,0.0142172845,0.0000119332535,0.00008826617,0.0002446088,0.000003294601,0.000012490854,0.0068117552],"genre_scores_gemma":[0.9643947,0.0000021817957,0.03535628,0.000098804485,0.000023392824,0.0000060109164,0.000001549386,0.000018043545,0.000099046534],"study_design_codex":"simulation_or_modeling","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99900675,0.000018464352,0.00016716031,0.00014517583,0.00039497926,0.00026746863],"domain_scores_gemma":[0.99954164,0.000008700309,0.00010362899,0.00026216017,0.000005234896,0.00007862672],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016485086,0.000122226,0.00010924577,5.288328e-7,0.00012399236,0.000010622473,0.00020165334,0.00005747252,0.00015437862],"category_scores_gemma":[0.0000029390528,0.00009630327,0.000044571276,0.00012290654,0.0001407313,0.00011877035,0.00010077082,0.00007365627,0.000034761524],"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":[0.0000076118413,0.00011343407,0.03857928,0.0000028946263,0.000008248236,2.9386653e-8,0.0010529218,0.5364593,0.42348254,0.00013963382,0.00007740154,0.00007667801],"study_design_scores_gemma":[0.0003403547,0.000011981944,0.0048002573,0.000006886251,0.000035420046,0.000001135883,0.00055767945,0.13446923,0.85938245,0.0001310052,0.00004155073,0.00022205462],"about_ca_topic_score_codex":0.00005714896,"about_ca_topic_score_gemma":0.0000014947656,"teacher_disagreement_score":0.4358999,"about_ca_system_score_codex":0.00014394123,"about_ca_system_score_gemma":0.000011281396,"threshold_uncertainty_score":0.39271334},"labels":[],"label_agreement":null},{"id":"W1964770800","doi":"10.1007/s13762-012-0150-7","title":"Development of the models to estimate particulate matter from thermal infrared band of Landsat Enhanced Thematic Mapper","year":2013,"lang":"en","type":"article","venue":"International Journal of Environmental Science and Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":36,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"National and Kapodistrian University of Athens","keywords":"Thematic Mapper; Particulates; Correlation coefficient; Environmental science; Remote sensing; Pixel; Atmospheric correction; Coefficient of determination; Physics; Satellite imagery; Satellite; Geology; Chemistry; Mathematics; Statistics","score_opus":0.005541378770833407,"score_gpt":0.21289575618581222,"score_spread":0.2073543774149788,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1964770800","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":[0.9973895,0.00001691018,0.00080709055,0.000634775,0.00007139633,0.000098866556,0.000002521735,0.0000022601243,0.0009766999],"genre_scores_gemma":[0.99138457,0.0000050728822,0.008403422,0.00011833377,0.000006454899,0.000005397488,1.877405e-7,0.0000037423235,0.00007282648],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9988566,0.000007847625,0.00033979182,0.00012450849,0.00054069003,0.00013055354],"domain_scores_gemma":[0.99954355,0.000013810012,0.000251977,0.00012009991,0.000019212035,0.000051361007],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00015155139,0.00007787237,0.00012574393,0.0000125691395,0.000057678582,0.000014579496,0.0006079458,0.000038035807,0.0012728894],"category_scores_gemma":[0.000013245987,0.000047155077,0.000026540201,0.00013737685,0.00066793914,0.00025831844,0.00039309886,0.0000706042,0.000041563715],"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":[0.000008481117,0.00006550553,0.07511224,9.3566524e-7,0.000019577128,8.648286e-7,0.0009128309,0.00076431705,0.9096769,0.000034564306,0.000044951343,0.013358804],"study_design_scores_gemma":[0.00029281032,0.000049468992,0.45659843,0.000047339454,0.000009316656,0.000015789712,0.0006307519,0.00081336184,0.5371694,0.0041801482,0.000104292645,0.000088918314],"about_ca_topic_score_codex":0.000020765183,"about_ca_topic_score_gemma":0.0000048331935,"teacher_disagreement_score":0.3814862,"about_ca_system_score_codex":0.00008954474,"about_ca_system_score_gemma":0.000018100916,"threshold_uncertainty_score":0.9996401},"labels":[],"label_agreement":null},{"id":"W1965679259","doi":"10.1016/j.rse.2011.02.029","title":"Use of MODIS-derived surface reflectance data in the ORAC-AATSR aerosol retrieval algorithm: Impact of differences between sensor spectral response functions","year":2011,"lang":"en","type":"article","venue":"Remote Sensing of Environment","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":39,"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 Environment Research Council; Sight Research UK; Université de Sherbrooke; U.S. Geological Survey; National Aeronautics and Space Administration","keywords":"Aerosol; AERONET; Remote sensing; Radiometer; Albedo (alchemy); Environmental science; Moderate-resolution imaging spectroradiometer; Singular value decomposition; Brightness; Spectroradiometer; Computer science; Algorithm; Meteorology; Physics; Optics; Reflectivity; Satellite; Geology","score_opus":0.09207176403982582,"score_gpt":0.2790748552418719,"score_spread":0.1870030912020461,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1965679259","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":[0.98745704,0.000042552685,0.01185057,0.00005304065,0.0000374187,0.0003020123,0.00011830322,0.000010073122,0.00012902198],"genre_scores_gemma":[0.92253816,0.00012502617,0.07716403,0.0000100926945,0.000017537419,4.825272e-8,0.000014223938,0.000020403611,0.000110500194],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99754673,0.00043174767,0.0006064831,0.00047105426,0.00059463386,0.00034932696],"domain_scores_gemma":[0.9977989,0.0003953655,0.00044675026,0.0012704947,0.000007274533,0.000081213926],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000719953,0.00024876097,0.00044648934,0.0000053655667,0.000078386074,0.000010062821,0.0004669765,0.000109372806,0.0002479437],"category_scores_gemma":[0.00012175638,0.00017986199,0.00013169763,0.00027407258,0.00071447564,0.00019560444,0.0003162396,0.000215228,0.00001662297],"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":[0.001585151,0.00040392403,0.13613985,0.00002271601,0.00016563409,0.000036175035,0.0044225645,0.0070463386,0.8294627,9.3273684e-7,0.00011310512,0.020600924],"study_design_scores_gemma":[0.00038117022,0.0006913536,0.9449199,0.00006213673,0.00008496242,0.000011507501,0.000535767,0.027863821,0.025145829,0.00004599819,0.000016795542,0.00024076809],"about_ca_topic_score_codex":0.0033028899,"about_ca_topic_score_gemma":0.000071471535,"teacher_disagreement_score":0.80878,"about_ca_system_score_codex":0.00019120178,"about_ca_system_score_gemma":0.000033085187,"threshold_uncertainty_score":0.73345596},"labels":[],"label_agreement":null},{"id":"W1966628118","doi":"10.1029/2010jd014002","title":"Climatological aspects of the optical properties of fine/coarse mode aerosol mixtures","year":2010,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":449,"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 de Sherbrooke","funders":"NASA Headquarters; Goddard Space Flight Center; Indian Space Research Organisation; Oak Ridge Associated Universities; National Aeronautics and Space Administration","keywords":"Aerosol; Single-scattering albedo; Environmental science; AERONET; Atmospheric sciences; Mode (computer interface); Beijing; Absorption (acoustics); Range (aeronautics); Meteorology; Climatology; Remote sensing; Materials science; Geology; Physics; China; Geography","score_opus":0.02738920670976229,"score_gpt":0.2941194097277687,"score_spread":0.2667302030180064,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1966628118","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":[0.9935884,0.00009013542,0.00007633068,0.00080867787,0.0001534388,0.0001877176,0.0000020971759,0.000005607754,0.005087587],"genre_scores_gemma":[0.99443483,0.000023707187,0.005006152,0.000025498615,0.00016669363,0.000005395013,8.0672635e-8,0.000016499002,0.0003211661],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.996529,0.0002431959,0.0006342885,0.00022413844,0.0018525772,0.0005168254],"domain_scores_gemma":[0.9983505,0.00041127318,0.00034097958,0.0004426765,0.00020541991,0.00024914788],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00072067225,0.00017464963,0.00047954987,0.0000015401595,0.00016476505,0.000030317166,0.0010397007,0.00015635423,0.0008199853],"category_scores_gemma":[0.0015768607,0.00008912189,0.00034196323,0.00044479754,0.0024513274,0.00018104565,0.0006544001,0.0013723159,0.000026988919],"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":[0.0005091954,0.0011318378,0.02175714,0.00005156631,0.000059630278,0.000033723296,0.00026761176,0.0003766686,0.9557623,0.008609763,0.0028260194,0.008614487],"study_design_scores_gemma":[0.0013475651,0.0022362145,0.16826256,0.00024712304,0.00006705167,0.00011534669,0.0005220062,0.0050412826,0.7813839,0.039485,0.00091906695,0.000372903],"about_ca_topic_score_codex":0.0004303294,"about_ca_topic_score_gemma":0.00024571852,"teacher_disagreement_score":0.17437847,"about_ca_system_score_codex":0.000046599995,"about_ca_system_score_gemma":0.00014709016,"threshold_uncertainty_score":0.90320176},"labels":[],"label_agreement":null},{"id":"W1966934244","doi":"10.1117/12.617469","title":"&lt;title&gt;Lidar depolarization asymmetry measurements and its relation with the optical depth&lt;/title&gt;","year":2005,"lang":"en","type":"article","venue":"Proceedings of SPIE, the International Society for Optical Engineering/Proceedings of SPIE","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Defence Research and Development Canada","funders":"","keywords":"Lidar; Scattering; Optics; Polarization (electrochemistry); Asymmetry; Azimuth; Physics; Extinction (optical mineralogy); Forward scatter; Light scattering; Contrast (vision); Laser; Measure (data warehouse); Computer science; Chemistry","score_opus":0.010006362449158437,"score_gpt":0.20654271707314847,"score_spread":0.19653635462399005,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1966934244","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":[0.9352815,0.00010467081,0.00019608009,0.0013565582,0.00006158159,0.00020500059,0.0000031971754,0.000030261981,0.062761135],"genre_scores_gemma":[0.95845217,0.00004547103,0.040233277,0.00011028333,0.00018544325,0.000024656154,0.0000026312773,0.000027858228,0.0009181934],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9989517,1.924961e-8,0.00020178629,0.00018762419,0.0004886782,0.0001701988],"domain_scores_gemma":[0.999625,0.000028743574,0.00011629077,0.00003106678,0.00013982295,0.000059032438],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024466013,0.00013407726,0.00011979885,0.0000049491673,0.00007255123,0.000046645357,0.00026954693,0.00009577458,0.00011848811],"category_scores_gemma":[0.00009197699,0.00009079152,0.000098881086,0.00015698203,0.00012284619,0.00023940367,0.0000859477,0.00013820786,0.000028137354],"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":[0.00006319595,0.00013583088,0.0058928267,0.000120546785,0.00027808454,1.08214515e-7,0.0002430402,0.00055426173,0.54609025,0.4231313,0.01621093,0.0072796303],"study_design_scores_gemma":[0.0044406676,0.0013078128,0.13657117,0.0006956526,0.0010360334,0.00011517922,0.0012935945,0.31931835,0.2483898,0.0025267254,0.28198332,0.0023217],"about_ca_topic_score_codex":0.0000014217949,"about_ca_topic_score_gemma":4.168521e-7,"teacher_disagreement_score":0.42060456,"about_ca_system_score_codex":0.00010329163,"about_ca_system_score_gemma":0.00000866434,"threshold_uncertainty_score":0.37023705},"labels":[],"label_agreement":null},{"id":"W1967184305","doi":"10.1175/mwr-d-14-00254.1","title":"Cloud Trails Past the Lesser Antilles","year":2014,"lang":"en","type":"article","venue":"Monthly Weather Review","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"McGill University","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Radiosonde; Wake; Geology; Cloud height; Meteorology; Terrain; Diurnal cycle; Wind shear; Wind speed; Inversion (geology); Atmospheric sciences; Climatology; Environmental science; Cloud computing; Geography; Cloud cover; Oceanography; Physics; Seismology","score_opus":0.00813754562171394,"score_gpt":0.21695408663696839,"score_spread":0.20881654101525443,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1967184305","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.30744746,0.25485614,0.0024039354,0.025142616,0.00095492747,0.0019304382,0.0000081405915,0.00021055077,0.40704578],"genre_scores_gemma":[0.937056,0.027152948,0.0009579119,0.023581853,0.0007146474,0.00008482739,0.0000027263588,0.00007211162,0.010376973],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99892336,0.00012476301,0.00024658197,0.0002234034,0.00025026416,0.00023165005],"domain_scores_gemma":[0.99931186,0.000044964676,0.000109479624,0.00045653273,0.000005586392,0.0000715829],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000535804,0.00016387276,0.0002640495,3.6789075e-7,0.00012036923,0.00002619871,0.00043710248,0.000038035858,0.003612171],"category_scores_gemma":[0.000023033033,0.00008629994,0.00014475452,0.00015602514,0.0001238392,0.00007744293,0.00007207439,0.000102804835,0.0019281397],"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":[0.00001354332,0.0001788746,0.028161118,0.00029584536,0.00004772543,0.0000134034635,0.00083110994,0.00024762165,0.00021149288,0.0017564317,0.40866426,0.5595786],"study_design_scores_gemma":[0.00008692018,0.000046147707,0.009927095,0.00022789185,0.00004148055,0.000002626288,0.000024985839,0.00007965157,0.000015259136,0.00012579032,0.98928666,0.00013550137],"about_ca_topic_score_codex":0.0000723978,"about_ca_topic_score_gemma":0.00009934025,"teacher_disagreement_score":0.6296085,"about_ca_system_score_codex":0.000030402281,"about_ca_system_score_gemma":0.0000040711666,"threshold_uncertainty_score":0.998849},"labels":[],"label_agreement":null},{"id":"W1967775291","doi":"10.1029/2004jd005157","title":"Robust optical features of fine mode size distributions: Application to the Québec smoke event of 2002","year":2005,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université de Sherbrooke","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences; University of Maryland, Baltimore County; Carnegie Corporation of New York; Smithsonian Environmental Research Center; National Aeronautics and Space Administration; Goddard Space Flight Center; Smithsonian Institution","keywords":"Physics; Statistical physics; Monotonic function; AERONET; Mode (computer interface); Extinction (optical mineralogy); Angstrom exponent; Computational physics; Aerosol; Mathematics; Optics; Mathematical analysis; Meteorology","score_opus":0.02048559396109148,"score_gpt":0.30646048592380837,"score_spread":0.28597489196271686,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1967775291","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":[0.97308004,0.00045975906,0.016496705,0.008008528,0.00002918836,0.0002970744,0.000015519914,0.000005089706,0.0016081029],"genre_scores_gemma":[0.9892009,0.000047047462,0.009059463,0.00005108708,0.00027070395,0.000017582966,7.799455e-7,0.000012110079,0.0013403246],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9973066,0.00013879001,0.00054512074,0.00019265038,0.001429354,0.00038751907],"domain_scores_gemma":[0.99821705,0.00071295415,0.00024113354,0.00036966856,0.00019827223,0.00026091473],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00072571647,0.00013097681,0.0003072231,0.000001276375,0.00015285626,0.000022206761,0.0007303926,0.0000676705,0.0012474613],"category_scores_gemma":[0.00092505093,0.00008029059,0.0002014607,0.0005504434,0.000534822,0.00014253125,0.00031128354,0.00051401166,0.00010775833],"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":[0.0014820182,0.003818101,0.02289315,0.000063629974,0.0002408491,0.000015433307,0.0010720949,0.31725168,0.07335994,0.0062631103,0.14727977,0.42626023],"study_design_scores_gemma":[0.000837752,0.0017826393,0.92462873,0.00010564618,0.0000636948,0.00002097761,0.00054239837,0.014390837,0.020688882,0.0017499541,0.03493429,0.00025416535],"about_ca_topic_score_codex":0.009919411,"about_ca_topic_score_gemma":0.0053247386,"teacher_disagreement_score":0.9017356,"about_ca_system_score_codex":0.00028279974,"about_ca_system_score_gemma":0.00014448297,"threshold_uncertainty_score":0.99966556},"labels":[],"label_agreement":null},{"id":"W1968135231","doi":"10.1002/qj.49712657016","title":"Accounting for overlap of fractional cloud in infrared radiation","year":2000,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":17,"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":"Emissivity; Cloud computing; Water vapor; Sky; Radiative transfer; Flux (metallurgy); Environmental science; Radiative cooling; Cloud cover; Meteorology; Computational physics; Atmospheric sciences; Physics; Materials science; Optics; Computer science","score_opus":0.006756430455559288,"score_gpt":0.21984703062293218,"score_spread":0.21309060016737288,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1968135231","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":[0.99649,0.00006156509,0.001792046,0.0003709882,0.0001890134,0.000119877164,0.0000033576384,0.0000039456645,0.00096922],"genre_scores_gemma":[0.9950497,0.000010056862,0.0040615248,0.00037690368,0.00017194544,0.0000042663733,4.4200962e-7,0.0000054109,0.0003197512],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99883294,0.00008393294,0.00045369452,0.00011211464,0.00032711777,0.00019018132],"domain_scores_gemma":[0.99928546,0.00018432362,0.00037040462,0.000097196345,0.000016583128,0.000046009183],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00067826133,0.0000948177,0.00021355541,9.403757e-7,0.000099351084,0.000014957733,0.0002910336,0.00012401838,0.002641146],"category_scores_gemma":[0.000046745714,0.000057390676,0.00039352168,0.00013903128,0.0001323596,0.00012958888,0.000018870409,0.00024296167,0.000008184447],"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":[0.00081837986,0.0007427534,0.57181114,0.000023328463,0.00015622654,0.000003413921,0.0033539128,0.092172325,0.0042198617,0.0002600632,0.017570047,0.30886853],"study_design_scores_gemma":[0.0015923869,0.0013558937,0.9566651,0.000019843847,0.000049994775,0.00001046336,0.0007270136,0.01915439,0.0001949401,0.010200803,0.009858902,0.00017027948],"about_ca_topic_score_codex":0.000038202284,"about_ca_topic_score_gemma":0.0000030800454,"teacher_disagreement_score":0.38485396,"about_ca_system_score_codex":0.00011613476,"about_ca_system_score_gemma":0.00001449538,"threshold_uncertainty_score":0.9982706},"labels":[],"label_agreement":null},{"id":"W1968772981","doi":"10.1029/2008jd011130","title":"Parameterization of visibility in snow: Application in numerical weather prediction models","year":2009,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":22,"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","funders":"National Aeronautics and Space Administration","keywords":"Snow; Environmental science; Wind speed; Relative humidity; Meteorology; Linear regression; Atmospheric sciences; Visibility; Physics; Mathematics; Statistics","score_opus":0.022961146310330856,"score_gpt":0.3078295360186143,"score_spread":0.28486838970828343,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1968772981","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":[0.9736397,0.0000404208,0.024440672,0.00023759188,0.000018972234,0.00021649264,0.0000012376225,0.0000045250395,0.0014003875],"genre_scores_gemma":[0.9966766,0.000052933305,0.0031141494,0.000025078973,0.00005460569,0.0000071417844,9.692359e-7,0.0000075713137,0.000060902334],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99771816,0.00024879136,0.0005831552,0.0002198884,0.0009243734,0.000305608],"domain_scores_gemma":[0.99922675,0.0001902177,0.0001885947,0.0002106972,0.00006577755,0.000117937445],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009779102,0.00009961041,0.00027428777,0.0000037372017,0.00003548896,0.00001708208,0.00028612211,0.00008712842,0.00016505478],"category_scores_gemma":[0.00024124492,0.00008015179,0.000084138854,0.00087296707,0.0001688631,0.00040554025,0.00006813781,0.00045381775,0.00001864249],"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":[0.0012259724,0.0038164668,0.47759762,0.000023852192,0.00001743296,0.000027086286,0.0012559092,0.19285089,0.058719642,0.0017643042,0.00048178344,0.26221904],"study_design_scores_gemma":[0.00047352276,0.0008360478,0.76222575,0.00004671163,0.000003028893,0.0000021559567,0.00013586048,0.1978642,0.00076265703,0.03750347,0.00007831063,0.00006828028],"about_ca_topic_score_codex":0.0010389258,"about_ca_topic_score_gemma":0.000069472815,"teacher_disagreement_score":0.28462812,"about_ca_system_score_codex":0.00028909417,"about_ca_system_score_gemma":0.00004512315,"threshold_uncertainty_score":0.32684952},"labels":[],"label_agreement":null},{"id":"W1969653808","doi":"10.1002/qj.147","title":"<i>In situ</i> measurements of liquid water content profiles in midlatitude stratiform clouds","year":2007,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":90,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"National Research Council Canada","keywords":"Liquid water content; Middle latitudes; Supercooling; Environmental science; Liquid water; Icing; Atmospheric sciences; In situ; Ice crystals; Meteorology; Geology; Materials science; Physics; Cloud computing","score_opus":0.02617920732239701,"score_gpt":0.2404618525808036,"score_spread":0.2142826452584066,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1969653808","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":[0.99732554,0.000070576294,0.0005082781,0.0005470051,0.00020204387,0.00019190727,8.443837e-7,0.0000037155962,0.0011500885],"genre_scores_gemma":[0.99597603,0.0000035573446,0.003396853,0.00045292726,0.000057012865,0.0000027355522,2.2982118e-7,0.0000070097735,0.00010364186],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9977718,0.00013826009,0.00085191097,0.0001654926,0.0006477978,0.0004247494],"domain_scores_gemma":[0.9993196,0.000064589425,0.00032933915,0.00015889107,0.000027848979,0.00009974032],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0024428829,0.00016598537,0.00036083834,0.0000020577254,0.000062731066,0.000012282877,0.0004948859,0.00016063802,0.00050730567],"category_scores_gemma":[0.000024095152,0.0000802164,0.00036880016,0.00014025373,0.00026397686,0.00012557388,0.000075023614,0.00041834151,0.0000104661485],"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":[0.0009267191,0.00097022415,0.4725031,0.00002036883,0.000094474985,0.00003269855,0.005068803,0.002821167,0.513408,0.000046069046,0.0006589077,0.0034494745],"study_design_scores_gemma":[0.0026163696,0.005518208,0.8412227,0.00007207846,0.000058566016,0.000021314381,0.0025892318,0.00025081364,0.14572427,0.0012661058,0.00032574157,0.00033462496],"about_ca_topic_score_codex":0.00014991808,"about_ca_topic_score_gemma":0.00020774924,"teacher_disagreement_score":0.36871958,"about_ca_system_score_codex":0.00021624519,"about_ca_system_score_gemma":0.000012174737,"threshold_uncertainty_score":0.5554641},"labels":[],"label_agreement":null},{"id":"W1972011463","doi":"10.1016/j.atmosenv.2015.03.054","title":"Climatic analysis of satellite aerosol data on variations of submicron aerosols over East China","year":2015,"lang":"en","type":"article","venue":"Atmospheric Environment","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":36,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Science and Technology Support Program of Jiangsu Province; National Natural Science Foundation of China; National Aeronautics and Space Administration","keywords":"Aerosol; Environmental science; Air quality index; Satellite; Climatology; Atmospheric sciences; Haze; East Asia; Monsoon; China; Air mass (solar energy); Meteorology; Geography; Geology","score_opus":0.025615708437015793,"score_gpt":0.2450027217026361,"score_spread":0.2193870132656203,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1972011463","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":[0.98110116,0.00025660728,0.012119857,0.0001333697,0.00010017194,0.00039672147,0.00010040948,0.000026908872,0.005764829],"genre_scores_gemma":[0.97330284,0.00029296742,0.0253744,0.00012361034,0.00002495481,0.000021247091,0.00014400993,0.000034579934,0.00068136415],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9971956,0.00011664622,0.0007441235,0.00067483017,0.00087631604,0.00039245363],"domain_scores_gemma":[0.9972899,0.00006361348,0.0005442731,0.001861973,0.0000058763185,0.00023439336],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00049018196,0.00031078636,0.00060675817,0.00000162046,0.000075675925,0.000016137472,0.00082807784,0.000115942115,0.004932156],"category_scores_gemma":[0.00004137335,0.0002758995,0.0001767913,0.0007669329,0.0003652651,0.0002309181,0.00074068323,0.000139323,0.0003007543],"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":[0.00011531937,0.0015028013,0.8107864,0.000026662567,0.0009192439,0.0000065361087,0.002093126,0.1687303,0.0059092757,0.00022362894,0.0014973404,0.008189317],"study_design_scores_gemma":[0.00091935426,0.0004879501,0.93262637,0.00002457116,0.0013196674,0.0000016520454,0.00035712728,0.058938257,0.00045790963,0.00009509118,0.0042725746,0.0004994956],"about_ca_topic_score_codex":0.00076020294,"about_ca_topic_score_gemma":0.00006108525,"teacher_disagreement_score":0.1218399,"about_ca_system_score_codex":0.00028488017,"about_ca_system_score_gemma":0.000021058839,"threshold_uncertainty_score":0.9999693},"labels":[],"label_agreement":null},{"id":"W1972245569","doi":"10.1029/2000jd900245","title":"Bimodal size distribution influences on the variation of Angstrom derivatives in spectral and optical depth space","year":2001,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":285,"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 de Sherbrooke","funders":"National Aeronautics and Space Administration; National Science Foundation","keywords":"Optical depth; Spectral line; Aerosol; Refractive index; Optics; Filter (signal processing); Basis (linear algebra); Computational physics; Physics; Mathematics; Geometry; Meteorology","score_opus":0.02049267246350859,"score_gpt":0.29596705221880154,"score_spread":0.27547437975529293,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1972245569","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":[0.9959942,0.0000391806,0.0006417987,0.0018636273,0.00002145618,0.00011223075,0.0000016121004,0.0000026703924,0.0013232414],"genre_scores_gemma":[0.99850565,0.00011008857,0.0011613077,0.000026786021,0.00009755281,0.0000045140982,2.6806418e-7,0.000006105767,0.00008774236],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980637,0.00023529184,0.0002995663,0.00015688462,0.0009164631,0.00032811626],"domain_scores_gemma":[0.9983089,0.0012343836,0.0001501136,0.00012491473,0.000054260465,0.00012740695],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007645645,0.000103708226,0.00020311656,9.527711e-7,0.00011038732,0.000045316374,0.00026000352,0.00005443495,0.0003687645],"category_scores_gemma":[0.0011493239,0.00006238363,0.000064881475,0.00051846204,0.000683008,0.00023130132,0.00012394604,0.0004887882,0.000014685242],"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":[0.0014746246,0.0011799415,0.8741846,0.000017146469,0.000071153605,0.00011895438,0.0014498972,0.0032010954,0.073881656,0.02537245,0.0010644932,0.017983977],"study_design_scores_gemma":[0.000311512,0.00090020115,0.9865184,0.00004010889,0.0000049425366,0.000008110828,0.00074103725,0.0010994688,0.001413245,0.008733536,0.00016654376,0.00006290934],"about_ca_topic_score_codex":0.0007410107,"about_ca_topic_score_gemma":0.0001556383,"teacher_disagreement_score":0.112333775,"about_ca_system_score_codex":0.00013759604,"about_ca_system_score_gemma":0.000045070945,"threshold_uncertainty_score":0.40377128},"labels":[],"label_agreement":null},{"id":"W1974323811","doi":"10.1029/2001gl014188","title":"Sunphotometric observations of the 2001 Asian dust storm over Canada and the U.S.","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":56,"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 de Sherbrooke","funders":"","keywords":"Plume; Dust storm; Storm; Climatology; Asian Dust; Environmental science; Aerosol; Atmospheric sciences; Meteorology; Geography; Geology","score_opus":0.034113194280365196,"score_gpt":0.2525050242366044,"score_spread":0.21839182995623924,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1974323811","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":[0.97225404,0.000023743753,0.0000063282455,0.025334792,0.000047595924,0.00020815937,0.000005122724,0.0000036046742,0.0021166103],"genre_scores_gemma":[0.9960066,0.000019052835,0.000042282176,0.002011394,0.000048648777,0.000021129868,4.0785034e-7,0.000006828291,0.0018436472],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99818087,0.00014628956,0.00011319478,0.00017459095,0.000997178,0.00038790933],"domain_scores_gemma":[0.99919474,0.0003281798,0.000036085807,0.00033057513,0.00001215272,0.0000982706],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00028445906,0.00007384343,0.0001027856,0.0000023121818,0.00032173374,0.000024899833,0.00041417347,0.000022173424,0.0011431216],"category_scores_gemma":[0.00022542862,0.000039277988,0.00004554405,0.0011796412,0.0011016543,0.00006779062,0.00033467295,0.0003205661,0.000031328855],"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":[0.000032931373,0.0001430521,0.32186815,0.000012633422,0.000035910256,0.000010941799,0.00083577086,0.00017928037,0.021436889,0.0008605034,0.6483524,0.0062315473],"study_design_scores_gemma":[0.00028331476,0.000014396329,0.9861947,0.000003589592,0.000004084607,5.8800964e-7,0.000077205805,0.0015440434,0.000091348586,0.00010469467,0.011626562,0.000055488406],"about_ca_topic_score_codex":0.6639817,"about_ca_topic_score_gemma":0.21168184,"teacher_disagreement_score":0.66432655,"about_ca_system_score_codex":0.00017991406,"about_ca_system_score_gemma":0.000023436582,"threshold_uncertainty_score":0.99977},"labels":[],"label_agreement":null},{"id":"W1974334195","doi":"10.1175/jas-d-13-0359.1","title":"Analytical Investigation of Glaciation Time in Mixed-Phase Adiabatic Cloud Volumes","year":2014,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"Office of Science; Transport Canada; U.S. Department of Energy","keywords":"Glacial period; Adiabatic process; Geology; Phase (matter); Mechanics; Physics; Thermodynamics; Geomorphology","score_opus":0.008465649592127509,"score_gpt":0.2355925425402472,"score_spread":0.2271268929481197,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1974334195","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":[0.99708116,0.000043425393,0.00041636528,0.0009242362,0.00031237784,0.00006961707,2.535201e-7,0.0000036232848,0.001148959],"genre_scores_gemma":[0.99394375,0.0000074093223,0.005487281,0.00019392894,0.00007677007,8.316362e-7,8.584038e-8,0.0000044869844,0.00028543692],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9982985,0.00019082452,0.0005156115,0.00013915723,0.0006653349,0.00019055477],"domain_scores_gemma":[0.9989638,0.0001445164,0.0006327003,0.00015094917,0.000022836208,0.0000852323],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016346681,0.000096311385,0.00022464887,0.0000012179624,0.00011427704,0.000028944627,0.000599096,0.000045594847,0.00044041075],"category_scores_gemma":[0.00040096472,0.000058697336,0.00010449491,0.0010179338,0.00072605506,0.00031772204,0.00010289374,0.00012039211,0.00003270032],"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":[0.000025616198,0.000115263916,0.92521846,0.00000683178,0.000011321627,0.0000013551556,0.00065063,0.052942388,0.0069231116,0.00023087814,0.0027567088,0.011117417],"study_design_scores_gemma":[0.00057363237,0.0004991917,0.45867142,0.000058307578,0.00003296424,0.000015800108,0.00024162828,0.5345121,0.0009591113,0.0037534055,0.0005616949,0.00012074453],"about_ca_topic_score_codex":0.000098410346,"about_ca_topic_score_gemma":0.000026913998,"teacher_disagreement_score":0.4815697,"about_ca_system_score_codex":0.000106748244,"about_ca_system_score_gemma":0.00005722913,"threshold_uncertainty_score":0.48221886},"labels":[],"label_agreement":null},{"id":"W1975174365","doi":"10.1175/jas3437.1","title":"A Simple Parameterization Coupling the Convective Daytime Boundary Layer and Fair-Weather Cumuli","year":2005,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":40,"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 British Columbia","funders":"Pacific Northwest National Laboratory; Biological and Environmental Research; Natural Sciences and Engineering Research Council of Canada; University of British Columbia; Battelle; University of Wyoming; Laboratory Directed Research and Development; U.S. Department of Energy; National Science Foundation","keywords":"Convective Boundary Layer; Cloud cover; Boundary layer; Environmental science; Daytime; Cloud base; Meteorology; Planetary boundary layer; Atmospheric sciences; Cloud top; Potential temperature; Liquid water content; Cloud computing; Geology; Mechanics; Physics; Computer science","score_opus":0.012719886186651121,"score_gpt":0.2448002933203394,"score_spread":0.23208040713368827,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1975174365","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":[0.9938986,0.00042778518,0.0012890922,0.0027223588,0.00021339879,0.000121016186,5.3536905e-7,0.000007996709,0.0013192712],"genre_scores_gemma":[0.9918164,0.0000632024,0.006364435,0.0011033718,0.00012863411,0.000002403407,4.6794625e-8,0.000008111478,0.00051338325],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9986774,0.00006308043,0.00029248165,0.0001794015,0.0005522669,0.00023540732],"domain_scores_gemma":[0.99920285,0.00013293892,0.00040023317,0.00017008184,0.000021184165,0.000072712],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00083468086,0.00012627376,0.00015708752,3.941705e-7,0.0007425358,0.00015911616,0.0006406987,0.00003961122,0.00075570925],"category_scores_gemma":[0.00009279271,0.000059230693,0.000090888854,0.00048517835,0.0011457576,0.00047085565,0.000226066,0.00016774688,0.000025845564],"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":[0.000075517055,0.00017638314,0.49997017,0.0000059677677,0.000087770655,0.000006626393,0.00539475,0.4291933,0.022940317,0.0002163219,0.008186523,0.03374636],"study_design_scores_gemma":[0.00074394286,0.0005554462,0.24519421,0.00004918585,0.000117440875,0.000254205,0.003949858,0.6827508,0.002391375,0.00338321,0.060194287,0.00041599383],"about_ca_topic_score_codex":0.000091833914,"about_ca_topic_score_gemma":0.000028249497,"teacher_disagreement_score":0.25477594,"about_ca_system_score_codex":0.00009670595,"about_ca_system_score_gemma":0.00005184255,"threshold_uncertainty_score":0.8274486},"labels":[],"label_agreement":null},{"id":"W1976580360","doi":"10.1007/s00024-007-0211-x","title":"Fog Research: A Review of Past Achievements and Future Perspectives","year":2007,"lang":"en","type":"review","venue":"Pure and Applied Geophysics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":703,"is_retracted":false,"has_abstract":false,"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":"Snow; Environmental science; Meteorology; Tornado; Winter storm; Aviation; Aerosol; Geography; Engineering; Aerospace engineering","score_opus":0.053149949948350886,"score_gpt":0.3352247871268934,"score_spread":0.28207483717854254,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1976580360","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00014236609,0.98277867,0.0000130981125,0.00006364297,0.000034798664,0.0007825391,0.000016055606,0.000010529736,0.016158322],"genre_scores_gemma":[0.000057466583,0.9985573,0.0003589923,0.000110150926,0.00047065227,0.00007231657,0.000020056474,0.000030333094,0.00032270717],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99829787,0.000055426273,0.00032570574,0.00050859636,0.00047406353,0.0003383581],"domain_scores_gemma":[0.99927384,0.000067492074,0.00020642034,0.0003152842,0.000015703896,0.00012129205],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046745563,0.00030749585,0.0009346261,0.0000035140438,0.00014974317,0.000020006632,0.00022370688,0.00016873975,0.0001982448],"category_scores_gemma":[0.000004171248,0.00022509185,0.0001259639,0.0004976727,0.0004104384,0.000043911987,0.00043084004,0.0004691494,0.000059596583],"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":[0.0000027861352,0.000061335144,0.000010307565,0.01724947,0.000037260845,0.0000015998478,0.00029127538,2.084443e-8,0.0000014786,0.0020332572,0.0017501472,0.97856104],"study_design_scores_gemma":[0.00007332594,0.00004783912,0.00011665208,0.0050318157,0.00016291696,0.0000026061903,0.0003990698,1.3190888e-7,4.854318e-7,0.0005125066,0.9934318,0.00022085645],"about_ca_topic_score_codex":0.000017468417,"about_ca_topic_score_gemma":0.0000025977895,"teacher_disagreement_score":0.99168164,"about_ca_system_score_codex":0.000051714964,"about_ca_system_score_gemma":0.000020243948,"threshold_uncertainty_score":0.9178979},"labels":[],"label_agreement":null},{"id":"W1978279960","doi":"10.1029/2002jd003185","title":"Impact of the Mount Pinatubo eruption on cirrus clouds formed by homogeneous freezing in the ECHAM4 GCM","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":58,"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","funders":"","keywords":"Aerosol; Atmospheric sciences; Cirrus; Sulfate aerosol; Vulcanian eruption; Volcano; Plume; Atmosphere (unit); Climatology; Environmental science; Stratosphere; Tropopause; Geology; Meteorology; Physics; Geochemistry","score_opus":0.022453627109035493,"score_gpt":0.31848980145437067,"score_spread":0.2960361743453352,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1978279960","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":[0.9955206,0.00021060501,0.00009852991,0.00031492035,0.000080376805,0.00026375748,0.0000044629464,0.0000031809714,0.003503546],"genre_scores_gemma":[0.99914116,0.00010189456,0.00021170825,0.0000773001,0.00009142324,0.000008763539,3.5952957e-7,0.000018056646,0.00034931992],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9961103,0.00070975337,0.00046329005,0.00021050894,0.0018876782,0.0006184605],"domain_scores_gemma":[0.99848,0.0005693504,0.00027805948,0.00044155936,0.00007680479,0.0001541932],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016224282,0.00018364696,0.0002921931,0.000001975785,0.00025571857,0.000061486724,0.0009586601,0.000100673424,0.00064090034],"category_scores_gemma":[0.0006954698,0.00008974149,0.0003624919,0.0008462917,0.0004877245,0.00017394141,0.0001514641,0.0010579971,0.00005128986],"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":[0.002379122,0.00852746,0.39747468,0.000081331054,0.00043079758,0.00031568113,0.005864301,0.04037907,0.35034207,0.009395881,0.08313887,0.10167074],"study_design_scores_gemma":[0.0017865695,0.005759434,0.9532056,0.00017444018,0.00003097715,0.00009221198,0.00182053,0.0022911555,0.0076716403,0.021188198,0.005623856,0.00035541528],"about_ca_topic_score_codex":0.002431686,"about_ca_topic_score_gemma":0.00016565101,"teacher_disagreement_score":0.5557309,"about_ca_system_score_codex":0.0007317767,"about_ca_system_score_gemma":0.00013035862,"threshold_uncertainty_score":0.7017409},"labels":[],"label_agreement":null},{"id":"W1978556678","doi":"10.5194/acpd-11-20375-2011","title":"On the discrepancies between theoretical and measured below-cloud particle scavenging coefficients for rain – a numerical study","year":2011,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Scavenging; Aerosol; Diffusion; Particle (ecology); Turbulent diffusion; Precipitation; Atmospheric sciences; Turbulence; Meteorology; Chemistry; Environmental science; Physics; Thermodynamics; Geology","score_opus":0.023446664466031445,"score_gpt":0.23710002702122263,"score_spread":0.21365336255519118,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1978556678","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":[0.95512617,0.000003994867,0.0397237,0.00050411205,0.000039721584,0.000573974,0.0000029674989,0.00003990591,0.0039854655],"genre_scores_gemma":[0.9986167,3.860835e-7,0.0008465285,0.00023109585,0.000026405909,0.00006363567,4.5045036e-7,0.000013566486,0.00020122844],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99889445,0.000085886124,0.0001573535,0.0002812498,0.00027658278,0.00030447094],"domain_scores_gemma":[0.9994105,0.00022508333,0.000031539756,0.00021760138,0.000005458291,0.000109797285],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005851496,0.0001255582,0.0001411324,5.8681536e-7,0.0002947989,0.000028321234,0.00018367547,0.000030468616,0.0012024883],"category_scores_gemma":[0.00013841914,0.00006930541,0.00004526995,0.00012385093,0.00039866802,0.00004092805,0.00015495777,0.00007337426,0.00006087358],"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":[0.00015135489,0.0008148323,0.88393176,0.000003063185,0.000055697543,0.0000032498997,0.0083045885,0.000065340915,0.00032238004,0.09836559,0.0008054229,0.007176726],"study_design_scores_gemma":[0.001852477,0.0020515188,0.93306494,0.000016025742,0.0001401177,0.0000029418509,0.009610622,0.024438528,0.0026852654,0.024983961,0.0005677223,0.0005858573],"about_ca_topic_score_codex":0.00009457422,"about_ca_topic_score_gemma":0.000007255697,"teacher_disagreement_score":0.073381625,"about_ca_system_score_codex":0.000029099368,"about_ca_system_score_gemma":0.0000036430574,"threshold_uncertainty_score":0.99971056},"labels":[],"label_agreement":null},{"id":"W1978656138","doi":"10.1016/j.coldregions.2011.06.010","title":"Sun effect on surface hoar illustrated by three case studies","year":2011,"lang":"en","type":"article","venue":"Cold Regions Science and Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":8,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Shortwave; Surface (topology); Shortwave radiation; Elevation (ballistics); Environmental science; Atmospheric sciences; Crystal (programming language); Geology; Physics; Geometry; Radiative transfer; Mathematics; Optics; Astronomy; Computer science","score_opus":0.0221015388194047,"score_gpt":0.24331838925005894,"score_spread":0.22121685043065425,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1978656138","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":[0.9947326,0.00026311833,0.00009259913,0.0007518716,0.000086628635,0.00022657572,0.0000014980384,0.00013464296,0.0037104604],"genre_scores_gemma":[0.998584,0.00008005586,0.0005073077,0.00011192232,0.0000039395914,0.00001910617,1.2870858e-7,0.000006576617,0.00068699016],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.998829,0.000014996137,0.00011172138,0.000465065,0.00020411465,0.00037508504],"domain_scores_gemma":[0.99942863,0.0000379947,0.000055397657,0.00036173788,0.000026322954,0.00008990139],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00032844752,0.0001433152,0.00016283987,0.000008316512,0.0006220067,0.000015524636,0.0003451413,0.00011684531,0.00007618114],"category_scores_gemma":[0.00009919566,0.00010403359,0.000016625218,0.0014307193,0.005584211,0.00013658074,0.00030393165,0.00015371128,0.00009349719],"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":[0.00009744965,0.0007314008,0.38925686,0.0000392433,0.00010512456,0.004408378,0.002368394,0.00008142086,0.40714875,0.06588822,0.06055423,0.069320545],"study_design_scores_gemma":[0.0053126817,0.023132518,0.018678756,0.00025166332,0.00034418175,0.010991304,0.021147287,0.0053480486,0.8105542,0.029429896,0.07035152,0.004457916],"about_ca_topic_score_codex":0.00022325115,"about_ca_topic_score_gemma":0.00021184645,"teacher_disagreement_score":0.4034055,"about_ca_system_score_codex":0.00009186919,"about_ca_system_score_gemma":0.000021302807,"threshold_uncertainty_score":0.99712205},"labels":[],"label_agreement":null},{"id":"W1979060409","doi":"10.1175/2010jamc2505.1","title":"Uncertainty Analysis for CloudSat Snowfall Retrievals","year":2010,"lang":"en","type":"article","venue":"Journal of Applied Meteorology and Climatology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":94,"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":"Snow; Environmental science; Precipitation; Meteorology; Attenuation; Liquid water path; Radiometer; Radar; Climatology; Remote sensing; Geology; Computer science","score_opus":0.007179686807898964,"score_gpt":0.23983702779710764,"score_spread":0.23265734098920868,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1979060409","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":[0.99084026,0.000059338567,0.0038032583,0.0010069846,0.00031654528,0.00012510529,0.000004168819,0.000008557464,0.0038358085],"genre_scores_gemma":[0.98629606,0.000082111874,0.012565983,0.00089807477,0.000081343635,0.000008880666,0.0000028591082,0.000009410716,0.00005527415],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99878114,0.000036374044,0.0004961824,0.00023394525,0.00012581186,0.00032651325],"domain_scores_gemma":[0.9988348,0.00034551808,0.00046215032,0.00017928449,0.000028496232,0.00014977693],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000878025,0.00014705953,0.00060386804,0.000011849042,0.00013697444,0.000010111908,0.00023903475,0.00031202944,0.0012424759],"category_scores_gemma":[0.00008357714,0.00011221157,0.00019185356,0.00026943997,0.00051144615,0.000048688322,0.0000930381,0.0003904733,0.00001709025],"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":[0.004656134,0.00042538028,0.7655881,0.000037276404,0.0022360203,0.00006294101,0.0011003858,0.004028502,0.12531368,0.07062056,0.0075734286,0.01835757],"study_design_scores_gemma":[0.01075148,0.0034663288,0.41448918,0.0000066540547,0.0076552513,0.0018513805,0.0018388111,0.006094608,0.009783611,0.17119163,0.3713758,0.001495283],"about_ca_topic_score_codex":0.000012531004,"about_ca_topic_score_gemma":0.00016345299,"teacher_disagreement_score":0.36380237,"about_ca_system_score_codex":0.000017489387,"about_ca_system_score_gemma":0.000017786972,"threshold_uncertainty_score":0.9996705},"labels":[],"label_agreement":null},{"id":"W1979268012","doi":"10.1029/2002jd002975","title":"Spectral discrimination of coarse and fine mode optical depth","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":887,"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 de Sherbrooke","funders":"","keywords":"Radiance; Aerosol; Optical depth; Coherence (philosophical gambling strategy); Inversion (geology); Haze; Remote sensing; Sky; Physics; Environmental science; Computational physics; Optics; Astrophysics; Meteorology; Geology","score_opus":0.027698274304232048,"score_gpt":0.31937115111402203,"score_spread":0.29167287680979,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1979268012","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":[0.9836108,0.00014972528,0.0018819696,0.00022917011,0.000041350726,0.00008895958,8.9521524e-7,0.00000326367,0.01399384],"genre_scores_gemma":[0.98232716,0.00008430149,0.016730947,0.000013769153,0.00007331873,0.0000019143101,2.7756235e-7,0.0000119970455,0.0007563383],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99789834,0.0001710777,0.00034505693,0.00016764688,0.0010477715,0.00037011426],"domain_scores_gemma":[0.9990788,0.0002847724,0.00013382499,0.00015062717,0.00008144421,0.00027050916],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006037176,0.00011156444,0.0002605551,0.0000014686606,0.00009588134,0.00003177768,0.00021749639,0.000058314472,0.00069593446],"category_scores_gemma":[0.0005601091,0.00008049281,0.00009929948,0.00028436602,0.0006717244,0.00023655813,0.00011387093,0.00042545097,0.00003209154],"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":[0.0016805412,0.0047873436,0.26942715,0.00020250311,0.0002729485,0.00045251666,0.0026730767,0.007533354,0.24969442,0.1007217,0.020683736,0.34187073],"study_design_scores_gemma":[0.00263315,0.005134235,0.84868455,0.00017396049,0.00008493636,0.00014732464,0.002106963,0.018936608,0.048002712,0.06907899,0.0045188665,0.0004977059],"about_ca_topic_score_codex":0.00028860586,"about_ca_topic_score_gemma":0.0002463193,"teacher_disagreement_score":0.5792574,"about_ca_system_score_codex":0.0000939196,"about_ca_system_score_gemma":0.00005619238,"threshold_uncertainty_score":0.7619994},"labels":[],"label_agreement":null},{"id":"W1979452287","doi":"10.1051/photon/20199730","title":"Détection et analyse automatique des aérosols atmosphériques par lidar infrarouge","year":2019,"lang":"fr","type":"article","venue":"Photoniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Humanities; Political science; Geography; Forestry; Art","score_opus":0.008191871287971527,"score_gpt":0.2551560184821008,"score_spread":0.24696414719412926,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1979452287","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":[0.9437127,0.0019726725,0.009978167,0.00089702976,0.0005664976,0.00078858907,0.000028612782,0.0004102006,0.041645527],"genre_scores_gemma":[0.90611976,0.0033130157,0.07047981,0.0013492198,0.000111764435,0.00010611737,0.000014807635,0.000079677164,0.018425804],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9970479,0.00034198863,0.00058246375,0.0007825682,0.0004558881,0.0007892108],"domain_scores_gemma":[0.9985658,0.00012451803,0.0003046562,0.0006587045,0.000042986685,0.0003033272],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0007271705,0.0005187149,0.00053294876,0.0000037932205,0.00026516127,0.00024826633,0.00043307437,0.000412452,0.014542544],"category_scores_gemma":[0.000058040398,0.00050926575,0.00028661848,0.0004941713,0.00065009063,0.001223781,0.00031689028,0.0005098082,0.0022124744],"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":[0.00008847632,0.0008718323,0.72009706,0.00033652017,0.00021680146,0.000028311,0.011089729,0.0018695518,0.23516315,0.0035626362,0.0046962136,0.0219797],"study_design_scores_gemma":[0.00069056515,0.0011954921,0.43440104,0.00056373904,0.00013629318,0.00006793809,0.0010016109,0.018945837,0.38784134,0.008138417,0.145645,0.0013727375],"about_ca_topic_score_codex":0.012464262,"about_ca_topic_score_gemma":0.0014281117,"teacher_disagreement_score":0.28569603,"about_ca_system_score_codex":0.0006581777,"about_ca_system_score_gemma":0.00009158233,"threshold_uncertainty_score":0.9997359},"labels":[],"label_agreement":null},{"id":"W1979514218","doi":"10.1175/jtech-d-13-00239.1","title":"An Assessment of the Impact of Antishattering Tips and Artifact Removal Techniques on Cloud Ice Size Distributions Measured by the 2D Cloud Probe","year":2014,"lang":"en","type":"article","venue":"Journal of Atmospheric and Oceanic Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":77,"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","funders":"","keywords":"Ice crystals; Instrumentation (computer programming); Pixel; Remote sensing; Environmental science; Materials science; Meteorology; Computer science; Optics; Physics; Geology","score_opus":0.005631281465559793,"score_gpt":0.2591977379034468,"score_spread":0.253566456437887,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1979514218","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":[0.98143625,0.00017872699,0.017111622,0.00072702504,0.00007691254,0.0001757541,0.0000072977136,0.000022827107,0.00026356184],"genre_scores_gemma":[0.991347,0.00014280602,0.008373122,0.000051458777,0.000041373194,0.000002103059,2.9221184e-7,0.000013520503,0.000028304124],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99870837,0.000116376075,0.00047183162,0.00018737503,0.00028769768,0.00022835484],"domain_scores_gemma":[0.9987333,0.00009726081,0.000691585,0.00036823197,0.000038590224,0.00007104151],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00061198807,0.00017783188,0.0003570733,0.000001042741,0.00017413196,0.000019591627,0.00045473644,0.00015581324,0.00008181183],"category_scores_gemma":[0.00011823895,0.000094890805,0.00011512579,0.00034326618,0.00069566135,0.0001059246,0.00017942069,0.00038419513,4.295106e-7],"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":[0.00015317457,0.00067035604,0.51641554,0.000033881584,0.00021119474,0.0000102433,0.00027712277,0.00032514875,0.31132054,0.0016951489,0.004740263,0.1641474],"study_design_scores_gemma":[0.00090260943,0.0042968914,0.9562535,0.00016515511,0.00015746498,0.0010673162,0.0007112325,0.004731217,0.02270073,0.0050259777,0.003641233,0.0003466297],"about_ca_topic_score_codex":0.000093906056,"about_ca_topic_score_gemma":0.0000065241666,"teacher_disagreement_score":0.43983802,"about_ca_system_score_codex":0.00011294155,"about_ca_system_score_gemma":0.000037230002,"threshold_uncertainty_score":0.38695347},"labels":[],"label_agreement":null},{"id":"W1980448564","doi":"10.1029/2004jd004876","title":"Weather systems occurring over Fort Simpson, Northwest Territories, Canada, during three seasons of 1998–1999: 1. Cloud features","year":2004,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Wave Control Systems (Canada); McGill University; York University; McMaster University","funders":"","keywords":"Environmental science; Cloud top; Cloud computing; Radar; Cloud fraction; Cloud height; Climatology; Meteorology; Satellite; Cloud cover; Atmospheric sciences; Latitude; Remote sensing; Geology; Geography; Computer science","score_opus":0.010865069505371638,"score_gpt":0.2580603582580255,"score_spread":0.24719528875265384,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1980448564","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":[0.9974793,0.0008218526,0.00017928793,0.00018082926,0.00046336438,0.00023750885,0.000036750727,0.000011802823,0.00058928935],"genre_scores_gemma":[0.9976919,0.000060325376,0.00056452595,0.000030969102,0.0009954355,0.00000906731,0.0000019867016,0.000040913477,0.00060484937],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9955298,0.00011557713,0.00056939875,0.00032941575,0.002587754,0.000868113],"domain_scores_gemma":[0.99831045,0.00022732274,0.0003785057,0.00041911355,0.00012696117,0.00053765025],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005217344,0.00027739583,0.00053808815,0.0000027397518,0.00035123737,0.000095076335,0.00082773925,0.00012279823,0.00023770749],"category_scores_gemma":[0.0001973284,0.00021039613,0.00022452847,0.00055823283,0.00046643883,0.00035059056,0.00039471785,0.00092613854,0.000018913895],"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":[0.0007009594,0.00050926633,0.9297627,0.00020054489,0.0002826022,0.0006111036,0.0004972966,0.048592567,0.0064795553,0.00093320146,0.010236064,0.0011941398],"study_design_scores_gemma":[0.0012901514,0.0007283077,0.97998714,0.00030630128,0.000036825586,0.00006675037,0.0007554231,0.00041665637,0.0013572149,0.0006253024,0.014105324,0.00032460384],"about_ca_topic_score_codex":0.8459806,"about_ca_topic_score_gemma":0.72340727,"teacher_disagreement_score":0.12257336,"about_ca_system_score_codex":0.0011222239,"about_ca_system_score_gemma":0.00061128056,"threshold_uncertainty_score":0.85797054},"labels":[],"label_agreement":null},{"id":"W1980635879","doi":"10.1175/jcli-d-12-00695.1","title":"Climatology of High Cloud Dynamics Using Profiling ARM Doppler Radar Observations","year":2013,"lang":"en","type":"article","venue":"Journal of Climate","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"McGill University","funders":"Biological and Environmental Research; U.S. Department of Energy","keywords":"Standard deviation; Environmental science; Doppler effect; Radar; Atmospheric sciences; Ice cloud; Meteorology; Geology; Physics; Optics; Radiative transfer","score_opus":0.018129515600582326,"score_gpt":0.2453122517297271,"score_spread":0.22718273612914477,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1980635879","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":[0.99416286,0.000034847755,0.0038014299,0.0004174598,0.00037376967,0.0001073102,0.000006594496,0.000006934943,0.0010887781],"genre_scores_gemma":[0.91604185,0.0001504282,0.08355224,0.00013075599,0.00007094377,0.0000014080591,0.0000022109446,0.0000146021775,0.000035547288],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986631,0.000043143285,0.00065073493,0.000105672814,0.00026757823,0.00026977132],"domain_scores_gemma":[0.998923,0.000054090757,0.0007340421,0.00014739104,0.00005066311,0.00009080634],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000263829,0.00011071015,0.00030346427,0.0000037682862,0.0000972621,0.000019222663,0.0002195425,0.000075001095,0.0013088804],"category_scores_gemma":[0.000033096854,0.00008759369,0.00010415912,0.00016809446,0.00014142215,0.0003145549,0.00012489669,0.00017505256,0.00004300607],"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":[0.00005605875,0.00031344872,0.9438776,0.000057341957,0.00006107038,0.000022582835,0.00026174716,0.011036253,0.036105722,0.0050889356,0.0007629686,0.0023562978],"study_design_scores_gemma":[0.0033433116,0.0011243318,0.7795849,0.00028308432,0.00039225534,0.0013755589,0.003541413,0.17451501,0.011340158,0.022119872,0.001360322,0.0010197988],"about_ca_topic_score_codex":0.00020632497,"about_ca_topic_score_gemma":0.000021659389,"teacher_disagreement_score":0.1642927,"about_ca_system_score_codex":0.00013239929,"about_ca_system_score_gemma":0.00002178859,"threshold_uncertainty_score":0.99960405},"labels":[],"label_agreement":null},{"id":"W1981027636","doi":"10.1117/12.559993","title":"Aerosol optical depth approximation using an optimization-subdivision method","year":2004,"lang":"en","type":"article","venue":"Proceedings of SPIE, the International Society for Optical Engineering/Proceedings of SPIE","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Cégep de Sherbrooke","funders":"","keywords":"Delaunay triangulation; Photometer; Vignetting; AERONET; Interpolation (computer graphics); Algorithm; Sun photometer; Triangulation; Piecewise; Computer science; Mathematics; Aerosol; Optics; Computer vision; Physics; Meteorology; Geometry; Mathematical analysis","score_opus":0.014307478087016011,"score_gpt":0.24773260186180265,"score_spread":0.23342512377478664,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1981027636","genre_codex":"empirical","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9606018,0.000018677274,0.03505906,0.0006154139,0.0001437184,0.0005431812,0.000009406594,0.000086369,0.0029223454],"genre_scores_gemma":[0.33124915,0.000019351968,0.6683301,0.00008968109,0.00016235068,0.000051205836,0.000007604738,0.000048718193,0.00004185776],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9974383,2.9218777e-8,0.00068002153,0.00052494433,0.0009160389,0.00044067999],"domain_scores_gemma":[0.9988828,0.00006642889,0.00038009256,0.00008198299,0.00039127085,0.00019742649],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00068732974,0.0003383049,0.00037065434,0.000012255448,0.0001690563,0.00013398501,0.0008622508,0.0002342106,0.00006693136],"category_scores_gemma":[0.0002792612,0.0002838737,0.0004167776,0.00041941108,0.0002898639,0.0010648315,0.0002727837,0.00027710863,0.0000039519173],"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":[0.00007782559,0.00037974617,0.0010120822,0.0001395192,0.0001490361,1.4082183e-7,0.0004033576,0.21369179,0.5901378,0.1928906,0.00023158625,0.00088653556],"study_design_scores_gemma":[0.0015268356,0.00047631902,0.0015737077,0.00018367657,0.0001881295,0.000032766184,0.0013802404,0.82197565,0.16999444,0.0018783429,0.00021107259,0.0005788272],"about_ca_topic_score_codex":0.000043803197,"about_ca_topic_score_gemma":5.611146e-7,"teacher_disagreement_score":0.63327104,"about_ca_system_score_codex":0.0004013595,"about_ca_system_score_gemma":0.000027787868,"threshold_uncertainty_score":0.9999613},"labels":[],"label_agreement":null},{"id":"W1981992077","doi":"10.1029/2004jd005128","title":"A microphysical parameterization for convective clouds in the ECHAM5 climate model: Single‐column model results evaluated at the Oklahoma Atmospheric Radiation Measurement Program site","year":2005,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Research Council Canada; Natural Sciences and Engineering Research Council of Canada; National Science Council; Canadian Foundation for Climate and Atmospheric Sciences; U.S. Department of Energy","keywords":"Environmental science; Atmospheric sciences; Outgoing longwave radiation; Cloud cover; Convection; Middle latitudes; Precipitation; Longwave; Climate model; Meteorology; Radiation; Atmosphere (unit); Cloud physics; Cloud fraction; Atmospheric model; Geology; Cloud computing; Climate change; Physics","score_opus":0.05855437080606224,"score_gpt":0.3349859194703584,"score_spread":0.27643154866429615,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1981992077","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":[0.9875448,0.00017448408,0.0070597017,0.0025691022,0.00005769477,0.0019376428,0.000022429274,0.000024458888,0.00060973625],"genre_scores_gemma":[0.9860302,0.00010331509,0.012744082,0.0002670089,0.00031008243,0.00021305785,0.000009668236,0.000046098296,0.0002764955],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9938563,0.0008009576,0.00091566425,0.0005168189,0.0029070415,0.0010032137],"domain_scores_gemma":[0.997637,0.0007000147,0.00052325893,0.0005057417,0.0004209228,0.0002131108],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.004185764,0.00031432844,0.00043741986,0.0000019013888,0.00064242707,0.00022749981,0.00081527984,0.0001472176,0.00006218982],"category_scores_gemma":[0.0008449003,0.00018828844,0.00033562985,0.00095780357,0.00063693326,0.00042573718,0.00032242635,0.00076538586,0.00008364639],"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":[0.003941458,0.0025865317,0.0011333472,0.00002730786,0.00008605146,0.000011570954,0.0034273851,0.8031971,0.057903208,0.00016936194,0.007417498,0.120099224],"study_design_scores_gemma":[0.0020772237,0.0020002066,0.013020984,0.000051417366,0.000058096808,0.000009481247,0.0003467368,0.9764383,0.0019839373,0.0019205754,0.0018634215,0.00022963736],"about_ca_topic_score_codex":0.0002195468,"about_ca_topic_score_gemma":0.0006776598,"teacher_disagreement_score":0.17324123,"about_ca_system_score_codex":0.0016357001,"about_ca_system_score_gemma":0.0001793653,"threshold_uncertainty_score":0.767818},"labels":[],"label_agreement":null},{"id":"W1982280236","doi":"10.5539/mas.v9n1p189","title":"Influence of Concentrations Dried Sea Salt Aerosols to Decrease Solar Radiation","year":2014,"lang":"en","type":"article","venue":"Modern Applied Science","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Kasetsart University; King's College London","keywords":"Sea salt; Aerosol; Radiation; Seawater; Particle size; Environmental science; Sea salt aerosol; Particle (ecology); Atmospheric sciences; Chemistry; Meteorology; Optics; Physics; Oceanography; Geology","score_opus":0.005007890565530452,"score_gpt":0.2131984460404535,"score_spread":0.20819055547492304,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1982280236","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":[0.8120625,0.0000031396494,0.17873375,0.00015539893,0.000028175235,0.00029711757,0.0000034263444,0.00003831406,0.008678165],"genre_scores_gemma":[0.99212,0.0000028374357,0.006585747,0.0011479063,0.000016369979,0.00004409189,0.0000020895734,0.000010089442,0.00007083753],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9980889,0.000020749509,0.0002644434,0.00050738495,0.00069806655,0.0004204839],"domain_scores_gemma":[0.99881595,0.000046200752,0.00012173718,0.00045465637,0.000025870151,0.00053560425],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00054068136,0.0001387772,0.00015899669,0.0000046369323,0.0003587969,0.000056291323,0.00061731227,0.000046415607,0.00023242283],"category_scores_gemma":[0.00021679583,0.00013316191,0.000028706943,0.00073035806,0.00075701444,0.0002847546,0.00022032615,0.00008393471,0.00025337105],"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":[0.0000135378605,0.00004802018,0.01788286,0.000002844481,0.000001270357,2.243646e-7,0.000852947,0.12855081,0.8413675,0.0019707028,0.00018319483,0.009126125],"study_design_scores_gemma":[0.0007451745,0.00016446006,0.34529826,0.00001807736,0.000021124439,0.0000028540003,0.00010265726,0.36277708,0.2809679,0.00609816,0.0031607228,0.00064350385],"about_ca_topic_score_codex":0.00021895183,"about_ca_topic_score_gemma":0.00005943403,"teacher_disagreement_score":0.56039953,"about_ca_system_score_codex":0.00014066446,"about_ca_system_score_gemma":0.000106481464,"threshold_uncertainty_score":0.5430185},"labels":[],"label_agreement":null},{"id":"W1982418405","doi":"10.1029/2007jd008968","title":"Global modeling of multicomponent aerosol species: Aerosol optical parameters","year":2008,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","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":true,"ca_institutions":"University of Toronto","funders":"","keywords":"AERONET; Aerosol; Environmental science; Sun photometer; Single-scattering albedo; Atmospheric sciences; Lidar; Climatology; Optical depth; Albedo (alchemy); Remote sensing; Meteorology; Geology; Geography","score_opus":0.05537287710116692,"score_gpt":0.30726122929764904,"score_spread":0.2518883521964821,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1982418405","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":[0.9877522,0.0001488474,0.0075595337,0.0003159501,0.00014245126,0.00020068734,0.000004814057,0.000012638533,0.0038629046],"genre_scores_gemma":[0.9708883,0.00023355926,0.028154934,0.00004355534,0.00018854588,0.000005660166,6.8036195e-7,0.000022473956,0.00046225052],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9950675,0.00023084885,0.0008732096,0.00035293942,0.002636622,0.00083890476],"domain_scores_gemma":[0.99812084,0.00039576413,0.00027579555,0.00039971774,0.0002131687,0.0005946944],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00066758605,0.00025241886,0.0006115205,0.0000020364425,0.00027973874,0.000041280407,0.00087659794,0.00013089245,0.00089577516],"category_scores_gemma":[0.0005008783,0.0001914656,0.0004109696,0.00064797205,0.0014037034,0.0003343034,0.00050999544,0.0006899759,0.00018074854],"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":[0.0043083844,0.008333294,0.21465626,0.00014954494,0.0007104423,0.0018479584,0.0027781674,0.5869355,0.12727357,0.0022203135,0.02865096,0.022135604],"study_design_scores_gemma":[0.008853481,0.010754746,0.23345879,0.0007675858,0.000205792,0.0008283296,0.005876053,0.69784385,0.030361924,0.0067704483,0.0021772352,0.002101741],"about_ca_topic_score_codex":0.0012151069,"about_ca_topic_score_gemma":0.000053344625,"teacher_disagreement_score":0.110908374,"about_ca_system_score_codex":0.00044284033,"about_ca_system_score_gemma":0.0001404784,"threshold_uncertainty_score":0.98081094},"labels":[],"label_agreement":null},{"id":"W1982596084","doi":"10.1175/jas-d-12-077.1","title":"Supersaturation and Diffusional Droplet Growth in Liquid Clouds","year":2012,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Supersaturation; Dimensionless quantity; Adiabatic process; Condensation; Thermodynamics; Mixing (physics); Scaling; Mechanics; RADIUS; Cloud condensation nuclei; Cloud physics; Liquid water content; Physics; Materials science; Chemistry; Aerosol; Meteorology; Mathematics; Geometry; Cloud computing","score_opus":0.008392401182647653,"score_gpt":0.21822491250538267,"score_spread":0.20983251132273503,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1982596084","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":[0.9957317,0.00039917318,0.00007845632,0.0017166155,0.0005373468,0.000055605724,1.9781405e-7,0.000003189059,0.0014777065],"genre_scores_gemma":[0.9935893,0.000090788584,0.0055896076,0.0004636039,0.00013385364,0.0000010087427,3.2456615e-8,0.000004253278,0.00012755874],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987428,0.00008210477,0.00026655034,0.00010816123,0.0005362647,0.00026408446],"domain_scores_gemma":[0.9995328,0.00006569405,0.00020735318,0.0000778618,0.000010603643,0.00010566462],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008770899,0.00009519401,0.00013301085,5.204537e-7,0.00021889583,0.000034955377,0.00040589197,0.000040849292,0.00048515736],"category_scores_gemma":[0.000106527346,0.000051566833,0.00006079695,0.0005361122,0.00052674965,0.000597189,0.0002110008,0.00014766683,0.000010834044],"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":[0.000035540517,0.0000910816,0.986983,0.0000020914304,0.0000039989836,0.0000017601878,0.0012377412,0.0008368422,0.008124709,0.00040414868,0.0009919492,0.0012871482],"study_design_scores_gemma":[0.00031078004,0.00028344747,0.9914988,0.000027249434,0.000014089529,0.00016078114,0.0010706508,0.0033408916,0.0007304932,0.0007423607,0.0016729606,0.00014747104],"about_ca_topic_score_codex":0.0001476466,"about_ca_topic_score_gemma":0.000018674937,"teacher_disagreement_score":0.007394216,"about_ca_system_score_codex":0.00008682612,"about_ca_system_score_gemma":0.000026694015,"threshold_uncertainty_score":0.5312133},"labels":[],"label_agreement":null},{"id":"W1982878003","doi":"10.1029/2007jd009153","title":"Stratospheric impact of the Chisholm pyrocumulonimbus eruption: 1. Earth‐viewing satellite perspective","year":2008,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Canadian Urological Association","funders":"","keywords":"Plume; Stratosphere; Tropopause; Atmospheric sciences; Smoke; Cirrus; Environmental science; Troposphere; Geology; Satellite; Climatology; Meteorology; Geography; Physics; Astronomy","score_opus":0.03899725509903074,"score_gpt":0.3325592557226705,"score_spread":0.29356200062363974,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1982878003","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":[0.98936576,0.0010867823,0.00011731127,0.00026977074,0.0000990522,0.0002019656,0.0000024128003,0.0000086449545,0.008848303],"genre_scores_gemma":[0.99585974,0.00061883946,0.0013995561,0.000029883873,0.0002987947,0.0000035808723,1.7981156e-7,0.000026326235,0.0017630929],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9961531,0.00037645613,0.00055762316,0.00028004486,0.0019924552,0.00064028724],"domain_scores_gemma":[0.9982483,0.00029476956,0.00038859132,0.00043595702,0.00030864848,0.00032377645],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006611186,0.00022561853,0.0004485964,0.0000016698224,0.00046013712,0.000044587847,0.00086843525,0.000096937954,0.002501605],"category_scores_gemma":[0.0003859859,0.00013157341,0.00070517603,0.0012028674,0.0013856301,0.0004309638,0.00037093755,0.0010284912,0.0001585057],"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":[0.001249534,0.002336233,0.84663177,0.000045138328,0.0006310117,0.00038763278,0.0085198255,0.017904872,0.07620531,0.0013471527,0.010116521,0.03462498],"study_design_scores_gemma":[0.000505999,0.0013093615,0.99132633,0.00006331955,0.000019630796,0.00010991044,0.0009565154,0.0005330984,0.0012883107,0.0019495599,0.0017764727,0.00016150283],"about_ca_topic_score_codex":0.0026068564,"about_ca_topic_score_gemma":0.00006980128,"teacher_disagreement_score":0.14469452,"about_ca_system_score_codex":0.00047181957,"about_ca_system_score_gemma":0.00031904585,"threshold_uncertainty_score":0.9984102},"labels":[],"label_agreement":null},{"id":"W1982878623","doi":"10.1175/bams-d-13-00286.1","title":"Far-Infrared Radiative Properties of Water Vapor and Clouds in Antarctica","year":2015,"lang":"en","type":"article","venue":"Bulletin of the American Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":76,"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":"Institut Polaire Français Paul Emile Victor; Polar Knowledge Canada","keywords":"Water vapor; Cirrus; Radiative transfer; Environmental science; Atmosphere (unit); Radiance; Atmospheric sciences; Radiosonde; Remote sensing; Infrared; Meteorology; Physics; Geology; Astronomy; Optics","score_opus":0.017062639173416026,"score_gpt":0.21120578608007404,"score_spread":0.19414314690665802,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1982878623","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":[0.99566776,0.00011167329,0.000040167382,0.002523468,0.000026190592,0.0001692201,0.0000023771788,0.000010280565,0.0014488656],"genre_scores_gemma":[0.9929431,0.00007559512,0.0050664786,0.0014985828,0.000011654203,0.000013829895,3.401709e-7,0.000007089863,0.0003833045],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988288,0.0001850875,0.00025166423,0.0002262628,0.00025782984,0.00025035255],"domain_scores_gemma":[0.99948823,0.000049521685,0.000169793,0.00019780977,0.0000127984285,0.00008182465],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047232962,0.00012525942,0.00033797295,6.1702286e-7,0.000047067482,0.000005111363,0.00028401788,0.000050977906,0.0005170649],"category_scores_gemma":[0.00011533265,0.00005996814,0.00012910138,0.00014035185,0.0022735952,0.000014846946,0.00049636397,0.00014383791,0.000018051689],"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":[0.0008791209,0.0006702079,0.8287966,0.000040249568,0.0001415581,0.000004632525,0.012659441,0.0019535406,0.121997334,0.00014197904,0.022617504,0.01009783],"study_design_scores_gemma":[0.0014515274,0.0015439601,0.9115148,0.000023298528,0.00006511764,0.000010269471,0.0073232763,0.0011318346,0.032528333,0.0015701269,0.04240032,0.00043712652],"about_ca_topic_score_codex":0.0018174718,"about_ca_topic_score_gemma":0.0000056678214,"teacher_disagreement_score":0.089469,"about_ca_system_score_codex":0.000061590894,"about_ca_system_score_gemma":0.000008694441,"threshold_uncertainty_score":0.8377157},"labels":[],"label_agreement":null},{"id":"W1983506404","doi":"10.1002/qj.49712656913","title":"Ice particle habits in stratiform clouds","year":2000,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":148,"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":"National Aeronautics and Space Administration","keywords":"Ice crystals; Ice cloud; Range (aeronautics); Particle (ecology); Atmospheric sciences; Precipitation; Environmental science; SPHERES; Particle size; Atmosphere (unit); Radiative transfer; Meteorology; Remote sensing; Materials science; Geography; Physics; Geology; Optics; Astronomy","score_opus":0.008331594137896749,"score_gpt":0.21368654924503241,"score_spread":0.20535495510713567,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1983506404","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":[0.99403006,0.00007711214,0.00013577851,0.0014314764,0.000110239554,0.0000941836,9.290001e-7,0.000009696166,0.0041105347],"genre_scores_gemma":[0.99617076,0.0000108240365,0.0017787688,0.0008491571,0.0000852627,0.0000030937993,7.610427e-8,0.000006793042,0.0010952576],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998461,0.00015312234,0.0004633032,0.00015848636,0.00041254942,0.00035150474],"domain_scores_gemma":[0.9994216,0.00007647921,0.00017751323,0.00018442803,0.000009441122,0.00013053205],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006792455,0.00013898857,0.00023431996,3.8154988e-7,0.00014095097,0.000032575193,0.00052600674,0.00012576421,0.005022959],"category_scores_gemma":[0.000017440954,0.000075168995,0.0003654322,0.00021467001,0.00025508163,0.00012846036,0.000038558308,0.00042992437,0.00013153917],"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":[0.0004547646,0.0012828805,0.493224,0.000010938969,0.00012280763,0.000060379913,0.007315855,0.038906366,0.004831958,0.00045069843,0.013945078,0.43939427],"study_design_scores_gemma":[0.0013628153,0.0023450577,0.9691896,0.000019140753,0.000049435203,0.00004301565,0.0010439191,0.013068153,0.00036738743,0.0051238555,0.0071117575,0.00027588752],"about_ca_topic_score_codex":0.00009024627,"about_ca_topic_score_gemma":0.000032361313,"teacher_disagreement_score":0.4759656,"about_ca_system_score_codex":0.0001193237,"about_ca_system_score_gemma":0.0000122999845,"threshold_uncertainty_score":0.99588656},"labels":[],"label_agreement":null},{"id":"W1983747149","doi":"10.3137/ao1009.2010","title":"Drought and Associated Cloud Fields over the Canadian Prairie Provinces","year":2010,"lang":"en","type":"article","venue":"ATMOSPHERE-OCEAN","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McGill University","funders":"","keywords":"Cloud computing; Geography; Cloud forest; Physical geography; Environmental science; Political science; Ecology; Biology","score_opus":0.0049773449567014575,"score_gpt":0.20190982784738817,"score_spread":0.1969324828906867,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1983747149","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":[0.94710535,0.000046939444,0.000016181086,0.0028090565,0.0004356509,0.00024740008,0.000006559925,0.000054664357,0.049278174],"genre_scores_gemma":[0.9897348,0.000007870125,0.00043902828,0.0019575607,0.00015891052,0.00000473192,0.0000047742715,0.00002525137,0.007667073],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985945,0.000046920042,0.00019122183,0.00035697143,0.00031370966,0.0004966483],"domain_scores_gemma":[0.9991482,0.00007691177,0.00010095619,0.0003711537,0.000011398424,0.00029141025],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00031144294,0.000202844,0.00015663049,2.1560788e-7,0.00065435446,0.00013805245,0.0003935522,0.00022829916,0.004439674],"category_scores_gemma":[0.00009602323,0.00013927625,0.000056289413,0.0002154818,0.000473324,0.00017557034,0.00016124842,0.00046561367,0.00013952407],"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":[0.0000055692103,0.000037658865,0.88412803,0.00000250331,0.000026005351,0.000016039805,0.0007281292,0.00008836886,0.00005093431,0.0010413396,0.10891696,0.004958483],"study_design_scores_gemma":[0.00033134987,0.000088745066,0.7500904,0.000006469234,0.000030239278,0.000011899978,0.0002622845,0.0020630036,0.000056957637,0.0017684462,0.24495074,0.00033944362],"about_ca_topic_score_codex":0.25636047,"about_ca_topic_score_gemma":0.85630137,"teacher_disagreement_score":0.5999409,"about_ca_system_score_codex":0.00013420012,"about_ca_system_score_gemma":0.000096859825,"threshold_uncertainty_score":0.9964704},"labels":[],"label_agreement":null},{"id":"W1985453897","doi":"10.1175/jas-d-12-0122.1","title":"Analytical Delta-Four-Stream Doubling–Adding Method for Radiative Transfer Parameterizations","year":2012,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":42,"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":"National Natural Science Foundation of China","keywords":"Radiative transfer; Reflection (computer programming); Computational physics; Radiative flux; Absorption (acoustics); Physics; Environmental science; Optics; Meteorology; Computer science","score_opus":0.04094213402526941,"score_gpt":0.3076468443639946,"score_spread":0.26670471033872517,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1985453897","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":[0.7848082,0.00015715623,0.21038502,0.0013476938,0.0007515481,0.00020265563,0.0000038686567,0.000010253633,0.002333569],"genre_scores_gemma":[0.78523004,0.000019274616,0.2138747,0.00044293766,0.00018680378,0.000006325332,1.4398428e-7,0.000009220031,0.0002305518],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9982302,0.00013315896,0.00042860757,0.00017254801,0.0005809565,0.00045452674],"domain_scores_gemma":[0.9989673,0.00039292412,0.0002484074,0.00015805346,0.000031514865,0.00020180776],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016252405,0.0001520157,0.00025271613,9.656607e-7,0.0005444561,0.00008441377,0.00074975134,0.00005980709,0.00057546364],"category_scores_gemma":[0.000222774,0.000085356645,0.0002892195,0.0009627575,0.00048081984,0.0006440368,0.0000932817,0.00015397131,0.000010698639],"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":[0.0001288455,0.00047811464,0.55781174,0.000013331793,0.00019451507,0.000003332707,0.0043194313,0.37024394,0.0048937793,0.0040539955,0.007028321,0.05083064],"study_design_scores_gemma":[0.0018142192,0.0011451113,0.14488813,0.00009002287,0.00062785717,0.00036160764,0.0035900036,0.7788643,0.0040056226,0.0036956333,0.0600499,0.00086756],"about_ca_topic_score_codex":0.0000510376,"about_ca_topic_score_gemma":0.0000059883164,"teacher_disagreement_score":0.41292363,"about_ca_system_score_codex":0.00012488324,"about_ca_system_score_gemma":0.00005859128,"threshold_uncertainty_score":0.6300923},"labels":[],"label_agreement":null},{"id":"W1985527326","doi":"10.1029/2006jd007968","title":"GOES Aerosol/Smoke Product (GASP) over North America: Comparisons to AERONET and MODIS observations","year":2007,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":98,"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, Santa Barbara","keywords":"AERONET; Aerosol; Environmental science; Moderate-resolution imaging spectroradiometer; Climatology; Atmospheric sciences; Spectroradiometer; Meteorology; Satellite; Geography; Reflectivity; Physics; Geology; Astronomy","score_opus":0.05180778422020582,"score_gpt":0.3254685746779302,"score_spread":0.2736607904577244,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1985527326","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":[0.9937147,0.00017653524,0.0029903785,0.0013957059,0.000099957695,0.0002902916,0.0000073435763,0.000016141234,0.0013089735],"genre_scores_gemma":[0.9826678,0.000087334396,0.015196255,0.0003051761,0.00040605452,0.000008672344,0.0000021390085,0.000027649865,0.0012988888],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9964135,0.000140043,0.0005659736,0.00039568185,0.0016248268,0.0008599275],"domain_scores_gemma":[0.99801993,0.0004613529,0.00021117025,0.00036872746,0.00016020614,0.0007786037],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00082917657,0.0002248187,0.00042031825,0.0000034863026,0.00040401163,0.00012100753,0.00057253987,0.00005826411,0.00075680396],"category_scores_gemma":[0.00049873017,0.0001720891,0.00012826733,0.0011250144,0.0007077127,0.0004142615,0.0005263436,0.00077483663,0.00018406322],"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":[0.0004589189,0.0008681967,0.8498587,0.00001854025,0.000092725386,0.00009303726,0.0009779517,0.0032642717,0.0114930775,0.00019967626,0.09189217,0.04078275],"study_design_scores_gemma":[0.0003444908,0.0008576726,0.96655566,0.000025303938,0.000017285804,0.000009521092,0.00058164,0.0006806806,0.00047155452,0.00024475646,0.030009963,0.00020150264],"about_ca_topic_score_codex":0.0030477147,"about_ca_topic_score_gemma":0.0015644736,"teacher_disagreement_score":0.11669694,"about_ca_system_score_codex":0.00023136371,"about_ca_system_score_gemma":0.000071942,"threshold_uncertainty_score":0.82864726},"labels":[],"label_agreement":null},{"id":"W1985901712","doi":"10.1029/2008jd010641","title":"Cloud, thermodynamic, and precipitation observations in West Africa during 2006","year":2009,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Environmental science; Precipitation; Monsoon; Climatology; Atmospheric sciences; Troposphere; Cloud cover; Cloud condensation nuclei; Meteorology; Cloud computing; Geology; Geography","score_opus":0.027083543967589347,"score_gpt":0.28821468701043484,"score_spread":0.2611311430428455,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1985901712","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":[0.9952536,0.00020473052,0.00013571304,0.0010072634,0.000039442777,0.00012995266,0.0000011752315,0.0000067582355,0.0032213274],"genre_scores_gemma":[0.99656636,0.0001332136,0.0020349582,0.000030602347,0.00015680332,0.0000039124534,3.3654368e-7,0.000009776827,0.0010640435],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981232,0.00016135778,0.0003410965,0.00018590847,0.0007767388,0.00041166562],"domain_scores_gemma":[0.9992695,0.00021655692,0.00012275686,0.0001459755,0.000061595,0.00018363776],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005247259,0.0001126462,0.00020051708,0.000002498841,0.00016742374,0.000064532614,0.00026901672,0.00006220598,0.00037469054],"category_scores_gemma":[0.00023431184,0.00008889783,0.000063954714,0.0005407105,0.00021126299,0.00039849945,0.00010317965,0.0004998855,0.00005388166],"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":[0.0018335334,0.0031747113,0.5666727,0.0000569105,0.0000863137,0.0004130945,0.007521703,0.013183017,0.26857442,0.005392498,0.009378068,0.12371303],"study_design_scores_gemma":[0.00046616513,0.00058002607,0.9834178,0.000039496415,0.000004489777,0.000007931886,0.0003591406,0.003317387,0.00016109695,0.011010505,0.0005396063,0.00009636173],"about_ca_topic_score_codex":0.00035043206,"about_ca_topic_score_gemma":0.00020718762,"teacher_disagreement_score":0.4167451,"about_ca_system_score_codex":0.00020044943,"about_ca_system_score_gemma":0.000035319423,"threshold_uncertainty_score":0.41025987},"labels":[],"label_agreement":null},{"id":"W1986242555","doi":"10.1117/12.440109","title":"&lt;title&gt;Wide-angle imaging lidar (WAIL): a ground-based instrument for monitoring the thickness and density of optically thick clouds&lt;/title&gt;","year":2001,"lang":"en","type":"article","venue":"Proceedings of SPIE, the International Society for Optical Engineering/Proceedings of SPIE","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"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":"Los Alamos National Laboratory; Goddard Space Flight Center; Laboratory Directed Research and Development; McGill University; U.S. Department of Energy","keywords":"Lidar; Opacity; Radiance; Optics; Scattering; Remote sensing; Laser; Radiative transfer; Physics; Optical depth; Field of view; Detector; Photon; Geology; Meteorology","score_opus":0.009188355089401743,"score_gpt":0.21405401225986695,"score_spread":0.2048656571704652,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1986242555","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":[0.9900936,0.000077614146,0.00035951892,0.0015727499,0.00018792196,0.0003036249,0.000007916033,0.000031333948,0.0073657585],"genre_scores_gemma":[0.9376206,0.00007042993,0.061604187,0.000094513314,0.00019063715,0.000052111547,0.000001621175,0.000031907275,0.00033398968],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99879336,3.2569268e-8,0.00031079963,0.00022927918,0.00042643398,0.00024007823],"domain_scores_gemma":[0.99938077,0.00011236639,0.0001701107,0.000053126725,0.00021481252,0.00006880303],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039901005,0.00017017077,0.0002033033,0.000005980649,0.00009318352,0.000055500983,0.00043267672,0.000090684625,0.00008729238],"category_scores_gemma":[0.0001959445,0.00012510364,0.00022872457,0.00014742423,0.00029505303,0.00016296183,0.00015366978,0.00015336275,0.0000057901075],"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":[0.0002098806,0.00029281594,0.041287303,0.0005346542,0.00038181135,5.476807e-7,0.0006062244,0.0003719414,0.56390494,0.37649396,0.008696757,0.0072191753],"study_design_scores_gemma":[0.007702877,0.001870894,0.15158601,0.0020744666,0.0014408629,0.00017754704,0.0065714475,0.38897058,0.24242039,0.022327235,0.17153831,0.003319389],"about_ca_topic_score_codex":0.000010974164,"about_ca_topic_score_gemma":2.095898e-7,"teacher_disagreement_score":0.38859862,"about_ca_system_score_codex":0.0001129873,"about_ca_system_score_gemma":0.000016062744,"threshold_uncertainty_score":0.5101579},"labels":[],"label_agreement":null},{"id":"W1986402954","doi":"10.1029/2009jd013430","title":"Radiative feedback of dust aerosols on the East Asian dust storms","year":2010,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":74,"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":"Atmospheric sciences; Dust storm; Aerosol; Environmental science; Radiative transfer; Atmosphere (unit); Mesoscale meteorology; Mineral dust; Wind speed; Storm; Extinction (optical mineralogy); Asian Dust; Meteorology; Radiative cooling; Optical depth; Physics","score_opus":0.02686023400848183,"score_gpt":0.29340101422641873,"score_spread":0.2665407802179369,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1986402954","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":[0.97294194,0.000026824593,0.000079914375,0.0038107857,0.00021776694,0.00024400406,0.000005791021,0.0000070383526,0.02266595],"genre_scores_gemma":[0.99598795,0.000022672713,0.00089893583,0.00012424933,0.00053807325,0.000009049857,4.129339e-7,0.000028269289,0.002390407],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99616456,0.00030173679,0.0005113598,0.00026650078,0.0021094852,0.00064637506],"domain_scores_gemma":[0.9978595,0.0006573494,0.00039096887,0.00049796136,0.00018050185,0.0004137699],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013992868,0.00021670872,0.0003948985,0.0000019795536,0.00034532294,0.00008312133,0.0011284144,0.00013834456,0.006763836],"category_scores_gemma":[0.0010085356,0.00012075095,0.00027742062,0.00067147793,0.0015752921,0.00027433236,0.00032800477,0.0021177696,0.0006446081],"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":[0.0032383776,0.0059660166,0.2099872,0.000077962875,0.000652619,0.0003605967,0.008761361,0.0024462186,0.30816853,0.024755742,0.2669359,0.16864946],"study_design_scores_gemma":[0.0012947236,0.0034954774,0.949563,0.0001241908,0.000033210454,0.000032736585,0.0058041653,0.0013261571,0.008382904,0.0068196533,0.02273042,0.00039335218],"about_ca_topic_score_codex":0.00049457606,"about_ca_topic_score_gemma":0.00022041996,"teacher_disagreement_score":0.7395758,"about_ca_system_score_codex":0.00014377192,"about_ca_system_score_gemma":0.00013389315,"threshold_uncertainty_score":0.99414414},"labels":[],"label_agreement":null},{"id":"W1986544333","doi":"10.1007/s11806-007-0047-7","title":"Support vector machines for cloud detection over ice-snow areas","year":2007,"lang":"en","type":"article","venue":"Geo-spatial Information Science","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":12,"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":"Snow; Cirrus; Remote sensing; Cloud computing; Support vector machine; Albedo (alchemy); Meteorology; Environmental science; Geology; Computer science; Artificial intelligence; Geography","score_opus":0.007398340425338822,"score_gpt":0.24472721085096422,"score_spread":0.2373288704256254,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1986544333","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.49267998,0.0000017172573,0.49282756,0.000108751454,0.00092784764,0.00035103678,0.000010864176,0.00007153911,0.013020696],"genre_scores_gemma":[0.9967067,0.0000025035051,0.002035489,0.000770497,0.00016053069,0.000024950965,0.000014152819,0.0000062988806,0.00027883964],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99811447,0.000008221775,0.0004160337,0.00022453067,0.0007325686,0.00050415535],"domain_scores_gemma":[0.99920076,0.000063805404,0.00023467824,0.00024582824,0.0000621094,0.00019284534],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012906877,0.00015011414,0.00011642252,0.000012970889,0.0005915576,0.00015246261,0.00038418802,0.00007495695,0.0015222046],"category_scores_gemma":[0.00025863314,0.00012973737,0.00006364336,0.00067938573,0.00039767288,0.0027379515,0.00016153438,0.00009732899,0.00059586624],"study_design_candidate":"design_other","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":[0.00022983231,0.000076270706,0.03190333,0.000024010913,0.0000075898884,0.0000014366681,0.0040739984,0.0028147844,0.025928514,0.0008248382,0.0032243903,0.930891],"study_design_scores_gemma":[0.00079375884,0.0003581085,0.7549611,0.000009537426,0.000014222788,0.000019117166,0.00038558844,0.09660983,0.031332076,0.00045988514,0.114563085,0.00049371267],"about_ca_topic_score_codex":0.00200276,"about_ca_topic_score_gemma":0.0010611063,"teacher_disagreement_score":0.9303973,"about_ca_system_score_codex":0.00025464903,"about_ca_system_score_gemma":0.000050747938,"threshold_uncertainty_score":0.99939054},"labels":[],"label_agreement":null},{"id":"W1987367163","doi":"10.1029/2006jd007401","title":"An investigation into the aerosol dispersion effect through the activation process in marine stratus clouds","year":2007,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":45,"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":"Aerosol; Supersaturation; Sea salt aerosol; Cloud condensation nuclei; Atmospheric sciences; Dispersion (optics); Effective radius; Environmental science; Particle (ecology); Condensation; Meteorology; Sea salt; Physics; Optics; Geology; Thermodynamics; Oceanography; Astrophysics","score_opus":0.017384850959694782,"score_gpt":0.3263165159646801,"score_spread":0.3089316650049853,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1987367163","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":[0.9969024,0.000032586653,0.00039614376,0.001347269,0.00006664292,0.0003478218,1.7340962e-7,0.000007836566,0.0008991412],"genre_scores_gemma":[0.99863166,0.000030248913,0.0006838046,0.0001401552,0.0003488977,0.0000107001315,0.0000013729261,0.000017113965,0.00013603484],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99672997,0.0005301121,0.00041623876,0.00023256964,0.00158618,0.00050493947],"domain_scores_gemma":[0.9982983,0.0009035707,0.00021665507,0.00031138718,0.000092629125,0.00017746128],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002863539,0.00016128107,0.00020267325,0.0000014967233,0.00044091637,0.00011591423,0.0007624974,0.00009225363,0.00032123967],"category_scores_gemma":[0.0003848521,0.0000787701,0.00009427754,0.0010034972,0.00078711787,0.0007572325,0.0001922464,0.0010922372,0.000042631556],"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":[0.0024087417,0.0008722021,0.561588,0.000060216607,0.00006145944,0.0000757606,0.023168921,0.011777852,0.21874417,0.0010173618,0.0019110816,0.17831422],"study_design_scores_gemma":[0.000972911,0.0029991404,0.9067488,0.000097873846,0.00001748997,0.000011932262,0.008269289,0.0034958834,0.05706121,0.019611483,0.0004928879,0.00022113023],"about_ca_topic_score_codex":0.004936302,"about_ca_topic_score_gemma":0.0012005516,"teacher_disagreement_score":0.34516075,"about_ca_system_score_codex":0.0003118324,"about_ca_system_score_gemma":0.00007437669,"threshold_uncertainty_score":0.74622446},"labels":[],"label_agreement":null},{"id":"W1987665217","doi":"10.1029/2008jd011257","title":"Maritime Aerosol Network as a component of Aerosol Robotic Network","year":2009,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":382,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institut du Savoir Montfort","funders":"Institut Polaire Français Paul Emile Victor; Natural Environment Research Council; Sight Research UK","keywords":"AERONET; Aerosol; Sun photometer; Environmental science; Photometer; Remote sensing; Meteorology; Geology; Geography; Physics; Optics","score_opus":0.02025936523240504,"score_gpt":0.2931524855639389,"score_spread":0.2728931203315339,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1987665217","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":[0.9846591,0.00073191273,0.0018791871,0.0013085548,0.00023610363,0.00036100476,0.0000011445245,0.000020603444,0.010802443],"genre_scores_gemma":[0.9863913,0.00020197168,0.010191217,0.00031857137,0.0011282396,0.0000050758745,0.00000128998,0.000029783065,0.0017325409],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9946765,0.00044822722,0.0009155814,0.0003628462,0.0023313637,0.0012655266],"domain_scores_gemma":[0.9976494,0.00058888807,0.0004810889,0.00047134372,0.00018804928,0.0006212865],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013398133,0.00029237475,0.0007675532,0.0000017375712,0.0003445554,0.000088725144,0.0010107853,0.00015683734,0.003202527],"category_scores_gemma":[0.00026912786,0.00022972985,0.0004078234,0.0010112838,0.0007184483,0.0003252699,0.00039919282,0.0011215465,0.00048210408],"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":[0.0034637998,0.004380773,0.057893332,0.00007539103,0.00044228797,0.00090802164,0.00061928004,0.5015287,0.038883254,0.0067043575,0.30901533,0.0760855],"study_design_scores_gemma":[0.0068960474,0.029042238,0.7865962,0.0016421329,0.00031496643,0.0004271081,0.0009321153,0.042251687,0.0067301216,0.10787946,0.015102994,0.0021849237],"about_ca_topic_score_codex":0.00066327857,"about_ca_topic_score_gemma":0.000057285473,"teacher_disagreement_score":0.72870284,"about_ca_system_score_codex":0.00024036928,"about_ca_system_score_gemma":0.00013218085,"threshold_uncertainty_score":0.9977087},"labels":[],"label_agreement":null},{"id":"W1988174970","doi":"10.1016/j.atmosres.2006.03.003","title":"Detecting cloud vertical structures from radiosondes and MODIS over Arctic first-year sea ice","year":2006,"lang":"en","type":"article","venue":"Atmospheric Research","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":16,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"Canada Research Chairs; ArcticNet","keywords":"Radiosonde; Arctic; Cirrus; Cloud top; Cloud base; Environmental science; Atmospheric sciences; Meteorology; Cloud computing; The arctic; Climatology; Geology; Oceanography; Geography","score_opus":0.015742514723583585,"score_gpt":0.26839859809794503,"score_spread":0.25265608337436146,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1988174970","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":[0.9924212,0.00047919777,0.0007942792,0.000256498,0.000122417,0.00025627043,0.0000037006023,0.00006335412,0.0056030927],"genre_scores_gemma":[0.9891506,0.00007410917,0.00960981,0.0000737875,0.00034665174,0.000027905417,0.0000044907956,0.00004473382,0.0006679001],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9970276,0.00023656258,0.00027913772,0.00070729246,0.00090065144,0.0008487709],"domain_scores_gemma":[0.99859476,0.0006299908,0.00003739278,0.00046842778,0.000026217875,0.00024319178],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00056678045,0.00023588883,0.00024559328,7.1180654e-7,0.0006394057,0.00017626863,0.0003979322,0.00016696741,0.0058605624],"category_scores_gemma":[0.00023040661,0.00020201385,0.000070662754,0.00058161124,0.0007280051,0.00022103364,0.00043650606,0.00054732076,0.00027634963],"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":[0.00012288848,0.00009001642,0.9781256,0.000025756102,0.000033234304,0.000051755,0.00045177093,0.0038949281,0.004148594,0.00054302596,0.0064117745,0.006100712],"study_design_scores_gemma":[0.0006745893,0.00015264448,0.9521587,0.000021177191,0.000017665026,0.000009188704,0.0005167562,0.02527549,0.0011694542,0.015437396,0.004218799,0.00034817835],"about_ca_topic_score_codex":0.038679376,"about_ca_topic_score_gemma":0.0010153597,"teacher_disagreement_score":0.03766402,"about_ca_system_score_codex":0.0003132981,"about_ca_system_score_gemma":0.000023882789,"threshold_uncertainty_score":0.9950482},"labels":[],"label_agreement":null},{"id":"W1988536071","doi":"10.1080/01431160500181754","title":"Broadband solar radiances from visible band measurements: A method based on ScaRaB observations and model simulations","year":2005,"lang":"en","type":"article","venue":"International Journal of Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Radiance; Remote sensing; Narrowband; Broadband; Zenith; Environmental science; Satellite; Radiometer; Solar zenith angle; Physics; Optics; Geology; Astronomy","score_opus":0.038820428071961476,"score_gpt":0.2931554183053736,"score_spread":0.25433499023341216,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1988536071","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.48897853,0.0000559023,0.507782,0.0020637924,0.00013354907,0.000040489558,0.000013056117,0.0000063412376,0.0009263564],"genre_scores_gemma":[0.6208795,0.000013445876,0.37817028,0.0007467861,0.00013727712,1.2981973e-8,0.0000021901224,0.000007424799,0.0000431112],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.998601,0.000051084684,0.00031331653,0.00015461123,0.0007634325,0.00011652063],"domain_scores_gemma":[0.9993215,0.00012481035,0.00024372981,0.00009459585,0.00012381164,0.00009153453],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032043966,0.0001081864,0.00013642591,0.000011022556,0.000113889466,0.0000862196,0.00014926966,0.000044981458,0.00013356292],"category_scores_gemma":[0.00012887904,0.00009583774,0.00006791867,0.00008607181,0.000051579565,0.00034286696,0.000027342201,0.00014002183,0.0000057045495],"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":[0.000045527846,0.000023503359,0.0027206358,5.159914e-7,0.000037896625,0.000005563588,0.00017638835,0.8187904,0.014902212,0.000002855354,0.0002446069,0.16304992],"study_design_scores_gemma":[0.0006625967,0.000026754404,0.006409342,0.00007777204,0.000027537353,0.000016470549,0.000027908423,0.9865814,0.0031216203,0.0010325597,0.0019171267,0.00009893022],"about_ca_topic_score_codex":0.0002501023,"about_ca_topic_score_gemma":0.00019704775,"teacher_disagreement_score":0.16779101,"about_ca_system_score_codex":0.00025555986,"about_ca_system_score_gemma":0.000044639477,"threshold_uncertainty_score":0.390815},"labels":[],"label_agreement":null},{"id":"W1989351359","doi":"10.1175/bams-d-13-00180.1","title":"Clouds, Aerosols, and Precipitation in the Marine Boundary Layer: An Arm Mobile Facility Deployment","year":2014,"lang":"en","type":"article","venue":"Bulletin of the American Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":206,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Goddard Space Flight Center; Biological and Environmental Research; Office of Science; Colorado State University; U.S. Department of Energy","keywords":"Environmental science; Precipitation; Atmospheric sciences; Cloud base; Cloud cover; Aerosol; Marine stratocumulus; Troposphere; Climatology; Meteorology; Cloud computing; Geology; Geography","score_opus":0.00960490222926339,"score_gpt":0.22921358970125988,"score_spread":0.2196086874719965,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1989351359","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":[0.99558103,0.00003326214,0.00029280377,0.002397464,0.00003106138,0.00036172336,0.0000057070874,0.000022655682,0.0012742841],"genre_scores_gemma":[0.9898468,0.00008699952,0.005653955,0.0041938284,0.000023883333,0.00007990088,0.000003366083,0.0000061868745,0.000105075946],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99819744,0.00057347794,0.00025723525,0.00035188798,0.00034846595,0.00027147762],"domain_scores_gemma":[0.9990629,0.00024666014,0.00021236177,0.00040435843,0.000007210609,0.00006653061],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001218889,0.00015653533,0.00025611222,4.55192e-7,0.00020280357,0.000025670786,0.0005013235,0.0000564915,0.0011311399],"category_scores_gemma":[0.00009040707,0.0000824497,0.00014259024,0.0001773923,0.0015353988,0.000021800592,0.000467168,0.00023273999,0.000028001152],"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":[0.00019562818,0.0010724667,0.84671885,0.000016259652,0.000035821202,9.404449e-7,0.002627659,0.0023182842,0.0045587053,0.0002231461,0.012727248,0.129505],"study_design_scores_gemma":[0.00030609232,0.0011237782,0.9145937,0.0000023449916,0.000021590804,0.0000036774277,0.0014091441,0.0006869896,0.00016085006,0.001121208,0.08041087,0.00015978857],"about_ca_topic_score_codex":0.0017825506,"about_ca_topic_score_gemma":0.00006277991,"teacher_disagreement_score":0.12934521,"about_ca_system_score_codex":0.000055967448,"about_ca_system_score_gemma":0.000005233143,"threshold_uncertainty_score":0.99978197},"labels":[],"label_agreement":null},{"id":"W1989416203","doi":"10.1029/2008gl035680","title":"Evidence of the cloud lifetime effect from wildfire‐induced thunderstorms","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","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":"Cloud condensation nuclei; Thunderstorm; Cirrus; Atmospheric sciences; Environmental science; Convection; Effective radius; Aerosol; Cloud computing; Ice crystals; Meteorology; Climate change; Cloud physics; Smoke; RADIUS; Condensation; Climatology; Geology; Geography; Physics; Astrophysics","score_opus":0.04721253339305635,"score_gpt":0.29440247673605996,"score_spread":0.2471899433430036,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1989416203","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":[0.9941436,0.000046887955,0.00005091001,0.0044872286,0.00016199453,0.00032110373,0.0000015346167,0.000021926908,0.00076482305],"genre_scores_gemma":[0.9984179,0.000022785163,0.0000929242,0.0008380044,0.00027718954,0.000027071721,7.2002626e-7,0.000017768472,0.00030560247],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9967118,0.00045397802,0.00018854967,0.00042533854,0.0016355038,0.00058481883],"domain_scores_gemma":[0.9980041,0.0010596336,0.0000644847,0.0006914893,0.000009290119,0.00017104048],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00045043693,0.00015746384,0.00022340177,0.0000021877554,0.00041247977,0.000018451397,0.0009214517,0.00006743568,0.00047290698],"category_scores_gemma":[0.00036963445,0.00009651651,0.00017924367,0.0005775458,0.0014066664,0.00018168647,0.0006870637,0.00058374833,0.0010651957],"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":[0.00013236425,0.00009981918,0.08584824,0.000007803528,0.00002530595,0.000025209527,0.000773373,0.00007170197,0.8906196,0.00002269476,0.019087035,0.003286843],"study_design_scores_gemma":[0.00036727893,0.00041036663,0.9547617,0.00010573558,0.000011484309,0.0000026484709,0.000052982865,0.0004393446,0.042504475,0.00038229948,0.00074956927,0.0002121253],"about_ca_topic_score_codex":0.007930061,"about_ca_topic_score_gemma":0.000032333504,"teacher_disagreement_score":0.8689135,"about_ca_system_score_codex":0.00019920264,"about_ca_system_score_gemma":0.000032357664,"threshold_uncertainty_score":0.9997126},"labels":[],"label_agreement":null},{"id":"W1989920486","doi":"10.1175/1520-0450(2002)041<0640:aopalm>2.0.co;2","title":"Accuracy of Point and Line Measures of Boundary Layer Cloud Amount","year":2002,"lang":"en","type":"article","venue":"Journal of Applied Meteorology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":29,"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 British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Ceilometer; Pyranometer; Cloud cover; Environmental science; Cover (algebra); Meteorology; Boundary layer; Remote sensing; Planetary boundary layer; Sampling (signal processing); Lidar; Computer science; Cloud computing; Geology; Aerospace engineering; Geography; Irradiance; Physics","score_opus":0.021297217821746987,"score_gpt":0.2328347753533428,"score_spread":0.2115375575315958,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1989920486","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":[0.9899497,0.0008846021,0.0011405599,0.00039057015,0.00012985495,0.00007917581,0.0000018102935,0.000003287624,0.0074204127],"genre_scores_gemma":[0.9928833,0.00050670764,0.006149747,0.00030172456,0.00009025642,0.0000013704507,1.6380564e-7,0.0000097681195,0.000056943176],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9988225,0.000036442478,0.00055955164,0.00012177517,0.00028435883,0.00017538267],"domain_scores_gemma":[0.9989178,0.00012067846,0.0006950648,0.0001491779,0.000025488273,0.00009177663],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004984316,0.00011229807,0.0004041359,0.00000538604,0.00003941541,0.0000053621684,0.00019420442,0.00009736766,0.0017800384],"category_scores_gemma":[0.00005664952,0.00008394911,0.000080757134,0.00010972376,0.00041999164,0.00007289454,0.00010911156,0.0001959165,0.000013051829],"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":[0.0010548106,0.00065509736,0.018646091,0.00005332363,0.00027076554,0.000039844996,0.002942115,0.0030052748,0.8197152,0.0019612699,0.009582951,0.14207323],"study_design_scores_gemma":[0.015163591,0.011109461,0.23003617,0.00011959711,0.0012305722,0.0015590538,0.0033109211,0.0036586504,0.40689668,0.051268823,0.2740084,0.0016380945],"about_ca_topic_score_codex":0.00003096932,"about_ca_topic_score_gemma":0.000012836127,"teacher_disagreement_score":0.41281855,"about_ca_system_score_codex":0.00003400818,"about_ca_system_score_gemma":0.000011585983,"threshold_uncertainty_score":0.99913245},"labels":[],"label_agreement":null},{"id":"W1990727484","doi":"10.1175/jcli-d-14-00320.1","title":"Clouds, Precipitation, and Marine Boundary Layer Structure during the MAGIC Field Campaign","year":2015,"lang":"en","type":"article","venue":"Journal of Climate","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":112,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"U.S. Department of Energy","keywords":"Environmental science; Climatology; Atmospheric sciences; Inversion (geology); Precipitation; Boundary layer; Geology; Meteorology; Geography; Physics","score_opus":0.007490592715364349,"score_gpt":0.2296175984014317,"score_spread":0.22212700568606736,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1990727484","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":[0.9943429,0.00016344477,0.00009022217,0.0010163059,0.00021939645,0.00004898473,0.000002121004,0.0000045981565,0.004111997],"genre_scores_gemma":[0.9973396,0.00018624355,0.001512928,0.0003647929,0.00014546142,3.84359e-7,3.7485464e-7,0.000007309654,0.00044290966],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992777,0.000037284055,0.0002167542,0.00007352782,0.0002472522,0.00014747471],"domain_scores_gemma":[0.9995524,0.000037618214,0.00019275604,0.00009749288,0.000018802357,0.00010088319],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00024730098,0.000076864824,0.000109174245,0.0000012239911,0.000099734076,0.000054534205,0.00013589377,0.00003677368,0.001164096],"category_scores_gemma":[0.000043952463,0.000044612003,0.00003294387,0.00006610392,0.0000733337,0.0001762898,0.00014974033,0.00017017905,0.000018553625],"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":[0.00016438817,0.00002357235,0.9821859,0.000014925384,0.00002120668,0.00003367323,0.002380583,0.0011098733,0.0020027738,0.000040969393,0.0064241937,0.0055979304],"study_design_scores_gemma":[0.0008123123,0.0002740524,0.9736598,0.000018398932,0.000036876016,0.00041814352,0.0013376817,0.0002442961,0.0008921191,0.0054605296,0.016701229,0.00014457508],"about_ca_topic_score_codex":0.000031561838,"about_ca_topic_score_gemma":0.00004681147,"teacher_disagreement_score":0.010277035,"about_ca_system_score_codex":0.000047977195,"about_ca_system_score_gemma":0.000012800012,"threshold_uncertainty_score":0.999749},"labels":[],"label_agreement":null},{"id":"W1991373191","doi":"10.1029/2004gl021189","title":"The spectrum of waves and turbulence at the tropopause","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"York University; Dalhousie University","funders":"","keywords":"Turbulence; Turbulence kinetic energy; Wavelength; Tropopause; Physics; Kinetic energy; Equipartition theorem; Altitude (triangle); Gravity wave; Atmospheric sciences; Wave turbulence; Spectral line; Gravitational wave; Troposphere; Computational physics; Meteorology; Geology; Optics; Astrophysics; Classical mechanics; Geometry; Astronomy; Magnetic field","score_opus":0.01385861705243659,"score_gpt":0.27087341347531224,"score_spread":0.25701479642287567,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1991373191","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":[0.94731313,0.00009347771,0.000023282271,0.05102292,0.00001820481,0.00012937948,0.0000013424509,0.0000063205994,0.0013919467],"genre_scores_gemma":[0.9962588,0.00011716282,0.00009895434,0.0006718039,0.00011987137,0.000013158758,3.1502105e-7,0.000007130602,0.0027128158],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99844635,0.00012747265,0.00010634048,0.00020751826,0.0006728045,0.0004395442],"domain_scores_gemma":[0.9991006,0.00044990072,0.000028024177,0.00033183172,0.0000049195605,0.000084695625],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039602505,0.000075838354,0.0000771555,8.187717e-7,0.0005340184,0.00003795788,0.00037864444,0.000018567865,0.00033127033],"category_scores_gemma":[0.00007042703,0.000037008907,0.000037895603,0.00018953234,0.0021419767,0.00007346897,0.0005762145,0.00025242995,0.0004301108],"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":[0.00031670992,0.00024711795,0.021405254,0.000017039207,0.00005771178,0.000024439769,0.0025094743,0.0009809831,0.64027476,0.004312375,0.18680514,0.14304902],"study_design_scores_gemma":[0.0005974845,0.00042667944,0.74318683,0.000021459482,0.000015079523,0.000010823738,0.0006132853,0.00529143,0.03452449,0.0038407717,0.21112415,0.00034750908],"about_ca_topic_score_codex":0.00058981724,"about_ca_topic_score_gemma":0.0001983326,"teacher_disagreement_score":0.7217816,"about_ca_system_score_codex":0.000092236005,"about_ca_system_score_gemma":0.0000056118006,"threshold_uncertainty_score":0.7892203},"labels":[],"label_agreement":null},{"id":"W1991895422","doi":"10.1117/12.872969","title":"Quantitative retrieval of aerosol optical thickness from FY-2 VISSR data","year":2009,"lang":"en","type":"article","venue":"Proceedings of SPIE, the International Society for Optical Engineering/Proceedings of SPIE","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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; AERONET; Environmental science; Remote sensing; Satellite; Meteorology; Particulates; Atmospheric optics; Geology; Geography; Physics","score_opus":0.018118904470438894,"score_gpt":0.25098626776673116,"score_spread":0.23286736329629226,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1991895422","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":[0.9924772,0.000085968844,0.00032922145,0.0022888056,0.00016748623,0.00042310014,0.00012613136,0.000055296216,0.0040468285],"genre_scores_gemma":[0.7625301,0.00007903025,0.23680364,0.00016381548,0.00019842124,0.000014831897,0.000025024121,0.00003947641,0.00014569731],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9970242,2.8972428e-8,0.0008169599,0.00061624247,0.0011094696,0.0004331432],"domain_scores_gemma":[0.9985459,0.00021621528,0.00048393125,0.00015677197,0.00043339716,0.00016379986],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00068613025,0.00034437896,0.00053087896,0.000008669469,0.000091780086,0.00007499005,0.0020519951,0.00024253341,0.00012589339],"category_scores_gemma":[0.0008300458,0.00028072632,0.00040853702,0.00040912707,0.000570519,0.0007928168,0.0005582947,0.00037638328,0.000007686253],"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":[0.00032420212,0.00027421373,0.0011595871,0.00008516533,0.00024708366,1.9575549e-7,0.0003480691,0.00024449363,0.8399267,0.15301727,0.0038579884,0.0005150233],"study_design_scores_gemma":[0.0045513087,0.0033936286,0.03056923,0.0009461691,0.0008945676,0.00003429847,0.007612379,0.22222784,0.71398646,0.010596577,0.0032508192,0.00193674],"about_ca_topic_score_codex":0.000050179464,"about_ca_topic_score_gemma":4.7873397e-7,"teacher_disagreement_score":0.23647441,"about_ca_system_score_codex":0.0001504935,"about_ca_system_score_gemma":0.000026446072,"threshold_uncertainty_score":0.9999645},"labels":[],"label_agreement":null},{"id":"W1992797747","doi":"10.1175/2011jcli3672.1","title":"Tropical and Subtropical Cloud Transitions in Weather and Climate Prediction Models: The GCSS/WGNE Pacific Cross-Section Intercomparison (GPCI)","year":2011,"lang":"en","type":"article","venue":"Journal of Climate","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":171,"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; Université du Québec à Montréal; Pacific Institute for Climate Solutions","funders":"Office of Naval Research; California Institute of Technology; Jet Propulsion Laboratory; National Aeronautics and Space Administration","keywords":"Shortwave; Climatology; Cloud cover; Outgoing longwave radiation; Tropical cyclone; Shortwave radiation; Environmental science; Climate model; International Satellite Cloud Climatology Project; Intertropical Convergence Zone; Longwave; Rainband; Cloud forcing; Meteorology; Convection; Atmospheric sciences; Cloud computing; Climate change; Radiative transfer; Geography; Geology; Precipitation; Radiation; Oceanography","score_opus":0.02118634229015521,"score_gpt":0.2411727823824394,"score_spread":0.21998644009228419,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1992797747","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":[0.9926513,0.00014158316,0.0040425137,0.00031353757,0.00026870775,0.00009393123,0.0000065001395,0.000010723375,0.0024712014],"genre_scores_gemma":[0.9976778,0.0012941342,0.0008194505,0.000047363865,0.00012690642,0.0000040175482,5.244088e-7,0.0000111460195,0.000018656183],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988754,0.00008570425,0.00044892807,0.00015315863,0.00019604289,0.00024078373],"domain_scores_gemma":[0.999607,0.00002278851,0.00016247199,0.00009989217,0.00001233003,0.000095491276],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002965107,0.00011670271,0.00019696895,0.000005434775,0.00016259283,0.00005366071,0.00009784377,0.00008999333,0.00028298586],"category_scores_gemma":[0.000007510784,0.00007573943,0.0000642481,0.00009578556,0.00027846376,0.00039002163,0.000061196835,0.000320307,0.0000064083943],"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":[0.00039733158,0.00015724197,0.9910866,0.000012104833,0.000012945243,0.000013195477,0.0037033546,0.000465825,0.00070544274,0.000552308,0.000082507046,0.0028111516],"study_design_scores_gemma":[0.0007286401,0.00037087916,0.9790117,0.000035383164,0.000033072185,0.00018440682,0.0011797057,0.016848642,0.00003942579,0.0010679137,0.00041226792,0.00008796289],"about_ca_topic_score_codex":0.00003595692,"about_ca_topic_score_gemma":0.00011132507,"teacher_disagreement_score":0.016382819,"about_ca_system_score_codex":0.00006636968,"about_ca_system_score_gemma":0.000004756822,"threshold_uncertainty_score":0.30984968},"labels":[],"label_agreement":null},{"id":"W1992802510","doi":"10.1029/2010jd015237","title":"Cloud radar Doppler spectra in drizzling stratiform clouds: 1. Forward modeling and remote sensing applications","year":2011,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":180,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Drizzle; Radar; Remote sensing; Doppler effect; Skewness; Ceilometer; Environmental science; Doppler radar; Cloud computing; Meteorology; Physics; Computer science; Geology; Lidar; Telecommunications; Mathematics; Statistics","score_opus":0.03818446030204825,"score_gpt":0.2968044977223524,"score_spread":0.25862003742030415,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1992802510","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":[0.9304367,0.00019602649,0.06327179,0.0001221042,0.00005072928,0.00025998786,8.4797995e-7,0.000011937449,0.005649925],"genre_scores_gemma":[0.90345013,0.00023286224,0.095762834,0.000037119516,0.0003274994,0.0000013619572,3.2815285e-7,0.000025419982,0.00016243919],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9973989,0.0001318282,0.0005736816,0.0003130596,0.0009474025,0.0006351216],"domain_scores_gemma":[0.99898034,0.00017274746,0.00016745213,0.00026816886,0.0000678476,0.0003434583],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010488961,0.00018403253,0.00033744416,0.0000038452426,0.00024255326,0.00006939376,0.00036408586,0.0001002956,0.0003804045],"category_scores_gemma":[0.00009082063,0.00014895467,0.00011800731,0.00052867905,0.0003588323,0.00033267902,0.00025258036,0.0009188833,0.000054946322],"study_design_candidate":"design_other","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":[0.002148779,0.0013162814,0.030473072,0.00014029423,0.0002651178,0.0007503769,0.009477638,0.009639266,0.040085837,0.0076204953,0.0025009671,0.8955819],"study_design_scores_gemma":[0.0028882308,0.0025252036,0.03822655,0.0004302882,0.00008109239,0.00032294387,0.009657307,0.69920605,0.004125149,0.23764144,0.0037939649,0.0011017984],"about_ca_topic_score_codex":0.0035158936,"about_ca_topic_score_gemma":0.0007026637,"teacher_disagreement_score":0.89448005,"about_ca_system_score_codex":0.00022634381,"about_ca_system_score_gemma":0.00007635461,"threshold_uncertainty_score":0.6074195},"labels":[],"label_agreement":null},{"id":"W1993133049","doi":"10.1029/1999gl010928","title":"Convective boundary layer evolution to 4 km asl over High‐alpine terrain: Airborne lidar observations in the Alps","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","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":"University of British Columbia","funders":"Natural Environment Research Council","keywords":"Lidar; Troposphere; Atmospheric sciences; Tropopause; Climatology; Convective Boundary Layer; Convection; Boundary layer; Geology; Orography; Latitude; Aerosol; Planetary boundary layer; Environmental science; Meteorology; Precipitation; Geography; Remote sensing","score_opus":0.0271229314653146,"score_gpt":0.29184933670951474,"score_spread":0.26472640524420016,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1993133049","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":[0.9612209,0.000009894964,0.0002078368,0.035347246,0.00004394942,0.00037989358,0.000011717085,0.000024667455,0.0027538566],"genre_scores_gemma":[0.987779,0.0000045587985,0.00037577748,0.009486949,0.00022009213,0.00016230319,0.000012248115,0.000017166076,0.0019418711],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99714655,0.0003464117,0.00018920668,0.00046199065,0.0011228495,0.00073302],"domain_scores_gemma":[0.9991158,0.00024771382,0.000021656873,0.00044044858,0.000016789809,0.00015755674],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0005718269,0.00015369686,0.00015364989,0.000006679543,0.0003803909,0.00009675642,0.00054309407,0.000057666126,0.0030434695],"category_scores_gemma":[0.0000974682,0.00011397288,0.000070266586,0.0011415384,0.00055351714,0.00027578732,0.00019090444,0.0005829594,0.0025973772],"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":[0.0007532076,0.0019764327,0.0874772,0.000028145734,0.000087183376,0.0002643895,0.013142701,0.005735718,0.38322783,0.005913224,0.44056052,0.060833454],"study_design_scores_gemma":[0.00030651316,0.00018228946,0.95432514,0.0000123093505,0.000003374079,0.0000011219428,0.00022018752,0.00046142496,0.00014447632,0.0011962317,0.042995814,0.00015112375],"about_ca_topic_score_codex":0.009204564,"about_ca_topic_score_gemma":0.0005053896,"teacher_disagreement_score":0.86684793,"about_ca_system_score_codex":0.0004901384,"about_ca_system_score_gemma":0.000034139077,"threshold_uncertainty_score":0.9981792},"labels":[],"label_agreement":null},{"id":"W1993851071","doi":"10.1029/2009jd013650","title":"Lidar observations of Kasatochi volcano aerosols in the troposphere and stratosphere","year":2010,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"MEG-3 (Canada); Dalhousie University","funders":"","keywords":"Stratosphere; Troposphere; Tropopause; Atmospheric sciences; Plume; Volcano; Altitude (triangle); Environmental science; Aerosol; Lidar; Geology; Vulcanian eruption; Climatology; Meteorology; Physics; Remote sensing","score_opus":0.02752866631529986,"score_gpt":0.3014065883261181,"score_spread":0.27387792201081823,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1993851071","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":[0.9952557,0.00014322087,0.00008385967,0.0010956236,0.00007668737,0.00024604044,0.000003394968,0.0000044604367,0.0030909798],"genre_scores_gemma":[0.9929628,0.000079925776,0.006292591,0.00008850699,0.00018338439,0.000010420045,4.8250183e-7,0.000017735127,0.00036418685],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9970186,0.0002791522,0.00058271637,0.00022978711,0.0014012369,0.0004885568],"domain_scores_gemma":[0.9982997,0.0007138544,0.00026098124,0.00037829622,0.00013211674,0.00021500465],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013030092,0.00017177554,0.0003477291,0.00000133758,0.00019864166,0.00009051258,0.0007826999,0.0001213652,0.0014517128],"category_scores_gemma":[0.00051394687,0.00010755278,0.00014006517,0.0007834706,0.0010597423,0.000369628,0.0002283417,0.001470543,0.0000348564],"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":[0.000340825,0.0013523541,0.77975845,0.00005098906,0.000067490866,0.0001283862,0.0019082612,0.00035049458,0.17306055,0.014151846,0.008889246,0.019941077],"study_design_scores_gemma":[0.00065120735,0.0008596547,0.97986156,0.000044781864,0.000014530756,0.000031245534,0.0024692202,0.00042991198,0.00095636677,0.010569052,0.0039701653,0.00014229948],"about_ca_topic_score_codex":0.0018972581,"about_ca_topic_score_gemma":0.0021243168,"teacher_disagreement_score":0.20010309,"about_ca_system_score_codex":0.000048595703,"about_ca_system_score_gemma":0.0001359335,"threshold_uncertainty_score":0.9994611},"labels":[],"label_agreement":null},{"id":"W1995231762","doi":"10.1016/j.atmosenv.2009.07.063","title":"Simultaneous observations of boundary-layer aerosol layers with CL31 ceilometer and 1064/532 nm lidar","year":2009,"lang":"en","type":"article","venue":"Atmospheric Environment","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":37,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Ceilometer; Aerosol; Lidar; Environmental science; Advection; Boundary layer; Backscatter (email); Atmospheric sciences; Remote sensing; Air quality index; Meteorology; Geology; Geography; Physics","score_opus":0.008663638933040901,"score_gpt":0.19634149824215288,"score_spread":0.187677859309112,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1995231762","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":[0.9906188,0.0002571019,0.0053530717,0.00060941675,0.000044462373,0.00042071682,0.0000063743987,0.000048688325,0.002641333],"genre_scores_gemma":[0.92968893,0.00024317887,0.06660763,0.000986827,0.000031951648,0.000025458676,0.000006582177,0.0000354022,0.002374045],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978739,0.000050511946,0.00041163067,0.000596736,0.0005783181,0.000488888],"domain_scores_gemma":[0.99889874,0.00009171699,0.00021962656,0.00055400404,0.000005859005,0.00023003784],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00013576969,0.00035991686,0.00035816815,5.608896e-7,0.0002338889,0.000039140443,0.00026964242,0.000122068435,0.0024820152],"category_scores_gemma":[0.000016936825,0.00029358236,0.00007958601,0.00023731608,0.000533321,0.00022527383,0.00015568724,0.00018098195,0.0001607577],"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":[0.00036483884,0.00158413,0.7027027,0.0000412305,0.00021187888,0.00016529391,0.0032547794,0.14006609,0.079066336,0.00018871392,0.0022740406,0.070079945],"study_design_scores_gemma":[0.0023832747,0.0037060804,0.9046245,0.00006152734,0.000237037,0.00007024244,0.000962497,0.012268177,0.0030454723,0.0003800321,0.07074576,0.0015153787],"about_ca_topic_score_codex":0.00016973137,"about_ca_topic_score_gemma":0.00002104448,"teacher_disagreement_score":0.20192179,"about_ca_system_score_codex":0.0001962162,"about_ca_system_score_gemma":0.000015856325,"threshold_uncertainty_score":0.99995166},"labels":[],"label_agreement":null},{"id":"W1996367659","doi":"10.1175/2009jtecha1332.1","title":"PARSIVEL Snow Observations: A Critical Assessment","year":2009,"lang":"en","type":"article","venue":"Journal of Atmospheric and Oceanic Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":317,"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":"Deutsche Forschungsgemeinschaft","keywords":"Snowflake; Snow; Disdrometer; Cloud physics; Meteorology; Lidar; Environmental science; Remote sensing; Satellite; Precipitation; Particle (ecology); Atmospheric sciences; Physics; Computer science; Geology; Cloud computing","score_opus":0.008656422478266267,"score_gpt":0.25598833756012657,"score_spread":0.2473319150818603,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1996367659","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":[0.9573092,0.000608849,0.0306965,0.009697682,0.00014292111,0.00007792756,5.2531766e-7,0.000041071085,0.0014253389],"genre_scores_gemma":[0.86671615,0.00026255482,0.1320368,0.00080171094,0.000043665397,0.000001110191,1.3278415e-7,0.0000071633262,0.00013068541],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9989085,0.000022254197,0.0003979378,0.00017343015,0.0002376726,0.00026019485],"domain_scores_gemma":[0.9994067,0.00006719488,0.0002146514,0.00016373738,0.000036673227,0.00011102559],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018659838,0.00013830251,0.00026838644,0.0000010976232,0.0001276764,0.00002185289,0.00026858074,0.00015954943,0.0005155423],"category_scores_gemma":[0.00017167354,0.000109548346,0.00006766209,0.00041243865,0.00030444414,0.00021272548,0.00008862844,0.00033126125,0.000012147658],"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":[0.00008595493,0.00087464345,0.4238556,0.0000134244565,0.000085272,0.00035481763,0.0003626941,0.00027545157,0.010192457,0.05445749,0.020685192,0.488757],"study_design_scores_gemma":[0.0008285808,0.0019321201,0.89260226,0.000051502626,0.000081205384,0.00078032154,0.0010621583,0.002701676,0.00017747215,0.08224477,0.017241651,0.00029628302],"about_ca_topic_score_codex":0.0000039077117,"about_ca_topic_score_gemma":9.429056e-7,"teacher_disagreement_score":0.48846072,"about_ca_system_score_codex":0.00010911112,"about_ca_system_score_gemma":0.000036900383,"threshold_uncertainty_score":0.5644827},"labels":[],"label_agreement":null},{"id":"W1996550443","doi":"10.1175/jcli3605.1","title":"A Simulated Climatology of Asian Dust Aerosol and Its Trans-Pacific Transport. Part I: Mean Climate and Validation","year":2006,"lang":"en","type":"article","venue":"Journal of Climate","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":180,"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 British Columbia; Université du Québec à Montréal","funders":"National Natural Science Foundation of China; Canadian Foundation for Climate and Atmospheric Sciences; National Science Foundation","keywords":"Aerosol; Troposphere; Environmental science; Total Ozone Mapping Spectrometer; Climatology; Asian Dust; Atmospheric sciences; Precipitation; Mineral dust; Deposition (geology); Dust storm; Meteorology; Geology; Geography; Structural basin; Stratosphere; Ozone layer","score_opus":0.008294253650046624,"score_gpt":0.22350488723801584,"score_spread":0.2152106335879692,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1996550443","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":[0.99504113,0.00021242835,0.00016210297,0.00039084718,0.0000980315,0.00012967223,0.000023947518,0.000012314432,0.0039295005],"genre_scores_gemma":[0.9977359,0.0017494847,0.00038466693,0.000029944802,0.000039023576,9.856201e-7,0.000005889302,0.000018861656,0.000035213914],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983178,0.000067055014,0.0007979093,0.00019107535,0.00028071055,0.00034548942],"domain_scores_gemma":[0.9991412,0.000050378487,0.0005501073,0.0001044125,0.00002861553,0.00012529672],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043797115,0.00017453702,0.00042467983,0.00000735298,0.00011961872,0.00001919432,0.00010841583,0.00012283098,0.00044342293],"category_scores_gemma":[0.000009141956,0.00014449621,0.000093661474,0.00014890284,0.00017840069,0.00029729615,0.00002845715,0.00016696662,0.000007170865],"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":[0.00060373184,0.0003820595,0.9382338,0.00024001287,0.00006375224,0.00014036296,0.001594428,0.004808757,0.049742706,0.0005993911,0.0001826717,0.0034083216],"study_design_scores_gemma":[0.009103847,0.0021608244,0.93047154,0.0005233734,0.0008686896,0.0014637484,0.002907265,0.010390846,0.033572026,0.0013874247,0.005857732,0.0012926706],"about_ca_topic_score_codex":0.000021006095,"about_ca_topic_score_gemma":0.00004245897,"teacher_disagreement_score":0.016170679,"about_ca_system_score_codex":0.000026630347,"about_ca_system_score_gemma":0.000008780261,"threshold_uncertainty_score":0.58923846},"labels":[],"label_agreement":null},{"id":"W1997635519","doi":"10.1029/1999jd901199","title":"Indirect effect of sulfate and carbonaceous aerosols: A mechanistic treatment","year":2000,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":242,"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; Dalhousie University","funders":"","keywords":"Aerosol; Sulfate; Sulfate aerosol; Nucleation; Radiative forcing; Atmospheric sciences; Environmental science; Environmental chemistry; Chemistry; Meteorology; Physics","score_opus":0.015856013157324902,"score_gpt":0.29112232146109557,"score_spread":0.2752663083037707,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1997635519","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":[0.9943526,0.0004357016,0.00002231497,0.000095585594,0.00003655767,0.00022708368,0.0000031474913,0.00000789491,0.004819137],"genre_scores_gemma":[0.9962792,0.0005599534,0.0006472251,0.0000105832205,0.00011421551,0.000010774855,3.9511582e-7,0.000021090227,0.0023565672],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9974211,0.0004151956,0.00039291938,0.00024458466,0.001035637,0.0004905945],"domain_scores_gemma":[0.9985256,0.0007230389,0.00015241976,0.0002247812,0.00004345951,0.00033068124],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00073713035,0.0002032164,0.00054283213,0.0000017479284,0.00014969218,0.00004118551,0.00029085492,0.000080400736,0.0030098967],"category_scores_gemma":[0.00017051522,0.00012986176,0.00017730947,0.00037653933,0.00052221597,0.00013394323,0.00010923394,0.00033737175,0.00012454383],"study_design_candidate":"design_other","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":[0.004541354,0.0014049031,0.07871415,0.00010994449,0.00044336152,0.0007033445,0.0013208259,0.001445127,0.07212081,0.00019264825,0.00221256,0.836791],"study_design_scores_gemma":[0.016822137,0.12416999,0.6326855,0.0008117308,0.0007385093,0.00067309145,0.001019475,0.015611126,0.15502487,0.016694143,0.03385191,0.0018975534],"about_ca_topic_score_codex":0.0015983144,"about_ca_topic_score_gemma":0.00007976005,"teacher_disagreement_score":0.8348934,"about_ca_system_score_codex":0.0002190535,"about_ca_system_score_gemma":0.000052046853,"threshold_uncertainty_score":0.9979015},"labels":[],"label_agreement":null},{"id":"W1997728910","doi":"10.5194/acp-9-6881-2009","title":"Physical properties of High Arctic tropospheric particles during winter","year":2009,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":38,"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":"Ice crystals; Troposphere; Lidar; Atmospheric sciences; Depolarization ratio; Snow; Altitude (triangle); Ice nucleus; Ice cloud; Environmental science; Arctic; Particle (ecology); Scattering; Population; Geology; Meteorology; Physics; Remote sensing; Optics; Geometry","score_opus":0.005140812205609779,"score_gpt":0.18506475577264286,"score_spread":0.1799239435670331,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1997728910","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":[0.9981162,0.000090899404,0.0003562555,0.00008785468,0.000014991744,0.00007253025,0.0000010808883,0.000034509474,0.0012256622],"genre_scores_gemma":[0.9952083,0.000025652897,0.003150951,0.00006680544,0.00012388593,0.00000651009,0.0000013776998,0.0000133356225,0.0014031752],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.999079,0.0000126811865,0.00017296876,0.00028754346,0.00019247037,0.00025533795],"domain_scores_gemma":[0.9995639,0.000009705831,0.00008355172,0.00023611017,0.000010189059,0.00009655802],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000026396086,0.00018996124,0.00023671903,6.3980194e-9,0.00009761152,0.000019104415,0.00014183237,0.000045240744,0.0009635324],"category_scores_gemma":[0.0000070828924,0.00015714839,0.00007469468,0.00016653925,0.00027465197,0.00014025164,0.00006510914,0.00011148091,0.00002995802],"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":[0.000112782225,0.0005165061,0.025202962,0.00012117344,0.00003563532,0.0000065621566,0.0010994596,0.0033153458,0.87679017,0.000072669805,0.0000766223,0.09265011],"study_design_scores_gemma":[0.0011566824,0.00024285378,0.17752239,0.00011604998,0.00010403463,0.000026094653,0.00044552732,0.021776251,0.79135203,0.0062472094,0.00027771227,0.0007331639],"about_ca_topic_score_codex":0.0001327011,"about_ca_topic_score_gemma":0.0000010250933,"teacher_disagreement_score":0.15231943,"about_ca_system_score_codex":0.000046926307,"about_ca_system_score_gemma":0.000007069695,"threshold_uncertainty_score":0.9999497},"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":"W1998298133","doi":"10.1029/2001jd000877","title":"Optical properties of boreal forest fire smoke derived from Sun photometry","year":2002,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":104,"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 de Sherbrooke","funders":"National Aeronautics and Space Administration","keywords":"Sun photometer; Taiga; Environmental science; Aerosol; Angstrom exponent; Photometry (optics); Atmospheric sciences; Boreal; Smoke; Effective radius; Climatology; Physics; Meteorology; Geography; Geology; Astrophysics; Forestry","score_opus":0.0463789131337009,"score_gpt":0.2854388976926918,"score_spread":0.2390599845589909,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1998298133","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":[0.9911366,0.0007368439,0.000083593426,0.0003588237,0.00007901172,0.00015318864,0.0000042571714,0.000010530542,0.007437146],"genre_scores_gemma":[0.99575317,0.0002713067,0.0029078638,0.0000524603,0.00024962513,0.000007013759,6.4035123e-7,0.000028301996,0.0007296322],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9963006,0.00018547094,0.00060159975,0.00028089457,0.0019903032,0.00064116856],"domain_scores_gemma":[0.9984606,0.00035910524,0.00023933168,0.00034653477,0.00015851893,0.00043593647],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00044261283,0.00020346024,0.00048621048,0.0000022132954,0.00017104216,0.00006645654,0.000708266,0.00013131718,0.0039779423],"category_scores_gemma":[0.00059180893,0.00014001135,0.00026577624,0.00060474296,0.0011963701,0.00033907776,0.00041838555,0.0007928553,0.00023399528],"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":[0.0012971017,0.0036808287,0.62318146,0.00008716873,0.0003889515,0.000446845,0.0017558788,0.00092832546,0.22628114,0.00028348464,0.022253785,0.11941502],"study_design_scores_gemma":[0.0009206092,0.0014029876,0.9567052,0.00014516847,0.000033319542,0.000014947086,0.00074113614,0.010495381,0.026575446,0.0015382983,0.0011870203,0.00024049752],"about_ca_topic_score_codex":0.0059864568,"about_ca_topic_score_gemma":0.00017950666,"teacher_disagreement_score":0.33352372,"about_ca_system_score_codex":0.00017293608,"about_ca_system_score_gemma":0.00004609432,"threshold_uncertainty_score":0.99693257},"labels":[],"label_agreement":null},{"id":"W1998459619","doi":"10.1016/s0169-8095(02)00150-3","title":"Sea-salt optical properties and GCM forcing at solar wavelengths","year":2003,"lang":"en","type":"article","venue":"Atmospheric Research","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":26,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; University of Michigan","keywords":"Forcing (mathematics); Environmental science; Atmospheric sciences; Radiative forcing; Aerosol; Wavelength; Relative humidity; Northern Hemisphere; Climatology; Sea salt; Single-scattering albedo; Southern Hemisphere; Effective radius; Physics; Meteorology; Geology; Optics","score_opus":0.04928864946178143,"score_gpt":0.27971048708519103,"score_spread":0.2304218376234096,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1998459619","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":[0.9339216,0.0006200042,0.00037418897,0.00033877566,0.00006807732,0.00036412658,5.432445e-7,0.000048357004,0.06426433],"genre_scores_gemma":[0.96781814,0.00030495497,0.012726066,0.00011741382,0.00004231097,0.00006698603,7.2426843e-7,0.000043148546,0.018880263],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9969042,0.00024672848,0.00025446815,0.00061154773,0.0009787626,0.0010042982],"domain_scores_gemma":[0.9989674,0.00015774256,0.000036327252,0.00044934082,0.000033569027,0.00035560076],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0012413786,0.00020889926,0.00022508507,4.6808356e-7,0.0007739958,0.00010555054,0.00027902817,0.00013644,0.004050944],"category_scores_gemma":[0.0003529325,0.00016157723,0.000055470795,0.0005104395,0.00087667553,0.000230645,0.00064741896,0.00043253868,0.0010622522],"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":[0.00029325392,0.00056987157,0.7648101,0.00019559161,0.000113562644,0.00024413301,0.0042105974,0.0022103095,0.06790826,0.004476905,0.034458168,0.12050929],"study_design_scores_gemma":[0.0037195745,0.0023324257,0.26720923,0.00017508848,0.00007148477,0.00045327103,0.0067444383,0.090080686,0.06423908,0.0069845286,0.5552489,0.0027412476],"about_ca_topic_score_codex":0.00052194623,"about_ca_topic_score_gemma":0.00008010189,"teacher_disagreement_score":0.52079076,"about_ca_system_score_codex":0.0003573721,"about_ca_system_score_gemma":0.000047955666,"threshold_uncertainty_score":0.9997155},"labels":[],"label_agreement":null},{"id":"W1999108228","doi":"10.1117/12.578893","title":"Lidar-retrieved cloud and precipitation parameters","year":2005,"lang":"en","type":"article","venue":"Proceedings of SPIE, the International Society for Optical Engineering/Proceedings of SPIE","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Defence Research and Development Canada","funders":"","keywords":"Lidar; Remote sensing; Ranging; Extinction (optical mineralogy); Environmental science; Depolarization ratio; Precipitation; Scattering; Zenith; Atmospheric optics; Optics; Physics; Meteorology; Geodesy; Geology","score_opus":0.008337257692231035,"score_gpt":0.21230227494546974,"score_spread":0.2039650172532387,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1999108228","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":[0.9932015,0.000060146413,0.000065565066,0.0026804167,0.00014362634,0.0003928802,0.000012203351,0.000054347798,0.003389312],"genre_scores_gemma":[0.8189479,0.00007995742,0.1800167,0.00018967208,0.00023903801,0.0000677302,0.0000029477999,0.00003622162,0.00041981658],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99824756,1.0601126e-8,0.00048223377,0.00036166052,0.00058085035,0.0003276693],"domain_scores_gemma":[0.99923414,0.00010107275,0.0002767511,0.000045492838,0.000211467,0.00013107326],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043453168,0.00024426304,0.00027004583,0.000005592272,0.000091650654,0.000085906206,0.00053889246,0.00015003642,0.00006176301],"category_scores_gemma":[0.0003025198,0.00020197053,0.00029287284,0.0002454414,0.0003402513,0.0005526267,0.00020618728,0.00020974483,0.000006282217],"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":[0.00021119526,0.00025705417,0.015761852,0.0002398655,0.00038780997,9.303995e-8,0.0013145118,0.0011010827,0.76286393,0.19945417,0.012257703,0.006150719],"study_design_scores_gemma":[0.007417068,0.0026289618,0.12228127,0.0007683745,0.0008684073,0.00008561348,0.009210008,0.23188843,0.5349724,0.00957659,0.077346936,0.0029558875],"about_ca_topic_score_codex":0.00001941729,"about_ca_topic_score_gemma":4.2353338e-7,"teacher_disagreement_score":0.23078735,"about_ca_system_score_codex":0.00017815213,"about_ca_system_score_gemma":0.000009178864,"threshold_uncertainty_score":0.8236119},"labels":[],"label_agreement":null},{"id":"W1999326859","doi":"10.1007/s10712-011-9164-9","title":"Computation of Solar Radiative Fluxes by 1D and 3D Methods Using Cloudy Atmospheres Inferred from A-train Satellite Data","year":2011,"lang":"en","type":"article","venue":"Surveys in Geophysics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"European Space Agency","keywords":"Radiative transfer; Atmospheric radiative transfer codes; Zenith; Solar zenith angle; Environmental science; Atmosphere (unit); Satellite; Atmospheric sciences; Radiative flux; Flux (metallurgy); Remote sensing; Meteorology; Physics; Geology; Optics; Materials science","score_opus":0.07148296381907182,"score_gpt":0.31796695543803716,"score_spread":0.24648399161896534,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1999326859","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":[0.8064838,0.00029305439,0.19237138,0.000002410854,0.000086420994,0.0001313846,0.00010799595,0.000012543225,0.00051098416],"genre_scores_gemma":[0.8131592,0.00006594324,0.1865938,0.000023199507,0.000018337943,0.0000018886171,0.000102522514,0.000016981277,0.000018068462],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978454,0.0010407353,0.00030463136,0.00041058444,0.00018088109,0.0002177817],"domain_scores_gemma":[0.99914205,0.00023503373,0.00018816872,0.00036301083,0.000010194278,0.00006155828],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00126554,0.00017215144,0.00028461905,9.1879923e-7,0.00006200728,0.00001667678,0.0002948674,0.0000804636,0.0001723014],"category_scores_gemma":[0.00005187377,0.00016767628,0.00002451977,0.00024364209,0.00030550576,0.00033169947,0.00040309696,0.00012747952,0.000010714452],"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":[0.000015195246,0.0001940887,0.6349814,0.000010737689,0.000045362096,0.0000024818507,0.0047721225,0.001089774,0.009749684,0.000015292626,0.000060872626,0.349063],"study_design_scores_gemma":[0.00034175543,0.00005887,0.9322426,0.00001692396,0.000023384042,2.6849992e-7,0.00050983287,0.06051257,0.001788878,0.004214441,0.00006835454,0.00022212422],"about_ca_topic_score_codex":0.024600051,"about_ca_topic_score_gemma":0.0005393604,"teacher_disagreement_score":0.3488409,"about_ca_system_score_codex":0.000046918532,"about_ca_system_score_gemma":0.000016536413,"threshold_uncertainty_score":0.9818952},"labels":[],"label_agreement":null},{"id":"W1999386372","doi":"10.1029/2001jd001277","title":"Scattering of light by large Saharan dust particles in a modified ray optics approximation","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":92,"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","funders":"","keywords":"Scattering; Geometrical optics; Optics; Physics; Radiative transfer; Mie scattering; Radiance; Computational physics; Light scattering; Physical optics; Refractive index; Refraction; Particle (ecology); Surface roughness; Scattering theory; Wavelength; X-ray optics; Ray tracing (physics); Reflection (computer programming); Quantum mechanics; X-ray","score_opus":0.024075430367304335,"score_gpt":0.2907127223341953,"score_spread":0.266637291966891,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1999386372","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":[0.99428666,0.00019132854,0.002389173,0.00033261435,0.00003754515,0.00014578302,0.0000020116456,0.0000043409086,0.0026105552],"genre_scores_gemma":[0.99577296,0.0000856211,0.0037065668,0.000027121332,0.00004398342,0.000006896735,4.4615348e-7,0.00001597612,0.00034044147],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9973975,0.00029451336,0.00053384487,0.0001845399,0.0010529433,0.00053668435],"domain_scores_gemma":[0.99912095,0.00018991913,0.00021229549,0.00020010896,0.00006896454,0.00020778501],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012689693,0.00012697524,0.00030579412,0.000002335077,0.00009843585,0.00004285662,0.00032989684,0.00007521551,0.000565767],"category_scores_gemma":[0.00038604834,0.000099549194,0.000107278494,0.00056909776,0.00025067292,0.00030437007,0.00011796552,0.00046991688,0.000052071468],"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":[0.00058891356,0.003974823,0.12988868,0.0001253034,0.00009790154,0.00010661404,0.0018926936,0.010461748,0.81811774,0.004789308,0.013950349,0.016005894],"study_design_scores_gemma":[0.0092822695,0.0038477883,0.524657,0.00067921606,0.0000766017,0.000048312966,0.005839788,0.07680596,0.3244955,0.035825983,0.0171951,0.0012464562],"about_ca_topic_score_codex":0.00018878568,"about_ca_topic_score_gemma":0.000039853545,"teacher_disagreement_score":0.49362227,"about_ca_system_score_codex":0.0001482226,"about_ca_system_score_gemma":0.000047895603,"threshold_uncertainty_score":0.6194752},"labels":[],"label_agreement":null},{"id":"W1999837366","doi":"10.1155/2012/861026","title":"Synergistic Use of Remote Sensing and Modeling for Tracing Dust Storms in the Mediterranean","year":2012,"lang":"en","type":"article","venue":"Advances in Meteorology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":38,"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","funders":"Langley Research Center; Ministry of Environment","keywords":"Plume; Mineral dust; Dust storm; Atmospheric sciences; Outflow; Deposition (geology); Environmental science; Altitude (triangle); Asian Dust; Storm; Mediterranean climate; Lidar; Mediterranean sea; Latitude; Aerosol; Geology; Geography; Meteorology; Remote sensing; Geomorphology","score_opus":0.037025574314649756,"score_gpt":0.28706389130729415,"score_spread":0.2500383169926444,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1999837366","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":[0.82879287,0.00068503217,0.17004918,0.00007055466,0.00012270061,0.00011730064,8.1840426e-7,0.0000035821686,0.00015794103],"genre_scores_gemma":[0.9471866,0.00015461823,0.052420415,0.00018380425,0.000037604874,0.0000017124751,9.132962e-7,0.0000066795837,0.000007665481],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9992453,0.00007110945,0.00020043275,0.00013988401,0.00008563288,0.00025768185],"domain_scores_gemma":[0.99947256,0.00031758955,0.00006174196,0.000119364035,0.0000028004627,0.000025919662],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005276433,0.00007843497,0.00015376632,0.0000030271349,0.000040793282,0.0000038055307,0.000083018276,0.00005343095,0.000016189604],"category_scores_gemma":[0.00015442996,0.00005450433,0.000018231061,0.00010093425,0.00015758366,0.000293115,0.0000407761,0.00009754198,8.189637e-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":[0.00015198145,0.000054712582,0.055672757,0.000047320806,0.000007260518,0.000008936967,0.00836486,0.22615568,0.0072308076,0.00028787617,0.000016508784,0.7020013],"study_design_scores_gemma":[0.0005136421,0.00013903754,0.00961551,0.000028567543,0.000021854295,0.000022365097,0.001364451,0.98152834,0.00025362457,0.0043473644,0.0019865085,0.00017873145],"about_ca_topic_score_codex":0.0004031162,"about_ca_topic_score_gemma":0.00096044666,"teacher_disagreement_score":0.75537264,"about_ca_system_score_codex":0.000028122744,"about_ca_system_score_gemma":0.0000019202464,"threshold_uncertainty_score":0.2222622},"labels":[],"label_agreement":null},{"id":"W1999900991","doi":"10.1029/2008jd009971","title":"A comparison between CloudSat and aircraft data for a multilayer, mixed phase cloud system during the Canadian CloudSat‐CALIPSO Validation Project","year":2008,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"National Research Council Canada; Environment and Climate Change Canada","funders":"National Research Council Canada; Canadian Space Agency","keywords":"Lidar; Environmental science; Ceilometer; Cirrus; Remote sensing; Liquid water content; Radar; Transect; Meteorology; Liquid water path; Boundary layer; Cloud computing; Geology; Physics; Aerosol","score_opus":0.11012013689480697,"score_gpt":0.38242732139390323,"score_spread":0.27230718449909624,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1999900991","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":[0.9967427,0.00025144182,0.00086172123,0.0007700372,0.00018103194,0.000870949,0.000083872335,0.000019672418,0.00021853653],"genre_scores_gemma":[0.99542207,0.000036246114,0.0029394918,0.000024781639,0.0010934875,0.000029264336,0.000016218548,0.00003944753,0.00039897612],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.995939,0.00050919096,0.0007215875,0.00048325103,0.0014495103,0.0008974385],"domain_scores_gemma":[0.99731284,0.00085773313,0.00033291965,0.0007118443,0.00017226352,0.000612395],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0019522947,0.00025647838,0.0005558538,0.0000049521173,0.0016621839,0.00019697646,0.001292567,0.00014337871,0.00007383901],"category_scores_gemma":[0.0006050106,0.00017163849,0.00014869064,0.00055237266,0.0008290854,0.00042488665,0.00059867976,0.0008454342,0.000048533897],"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":[0.002833749,0.0019142329,0.76908004,0.0005941221,0.00086804054,0.00058488763,0.0059454003,0.003219736,0.008205837,0.00067812175,0.17065312,0.035422742],"study_design_scores_gemma":[0.009885273,0.004069545,0.77359504,0.00038273304,0.0002734955,0.0004164656,0.006706348,0.10050652,0.003666694,0.00049183134,0.098940924,0.0010651406],"about_ca_topic_score_codex":0.0759293,"about_ca_topic_score_gemma":0.01678913,"teacher_disagreement_score":0.09728678,"about_ca_system_score_codex":0.0007048977,"about_ca_system_score_gemma":0.00041814498,"threshold_uncertainty_score":0.99963754},"labels":[],"label_agreement":null},{"id":"W1999989774","doi":"10.1029/2005gl024926","title":"Comparisons of remote sensing retrievals and in situ measurements of aerosol fine mode fraction during ACE‐Asia","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":17,"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 de Sherbrooke","funders":"University of Maryland, Baltimore County; National Aeronautics and Space Administration","keywords":"Aerosol; Environmental science; In situ; Remote sensing; Mode (computer interface); Atmospheric sciences; Range (aeronautics); Meteorology; Materials science; Geology; Physics; Computer science","score_opus":0.03767587791021277,"score_gpt":0.3070740245932438,"score_spread":0.269398146683031,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1999989774","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":[0.997077,0.000011573981,0.0012353518,0.0007354741,0.000012288567,0.00018120374,0.0000015360497,0.0000075880716,0.00073796697],"genre_scores_gemma":[0.9952834,0.0000031096477,0.0045747347,0.000022583059,0.00003694987,6.690266e-7,0.000002097889,0.000010362094,0.000066062465],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99804306,0.00014084461,0.00026081933,0.00027067598,0.00090587523,0.0003787226],"domain_scores_gemma":[0.9995231,0.00009810559,0.00008407419,0.00020578722,0.000022431146,0.00006647691],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003588269,0.000098929995,0.00022677222,0.0000077035875,0.0000878606,0.000012672036,0.00011649926,0.00004777302,0.000030352106],"category_scores_gemma":[0.00008243157,0.00009461525,0.00004212607,0.00042650753,0.0003915929,0.000115021285,0.00018167497,0.00028794294,0.000017516657],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010910836,0.000062397965,0.018074306,0.000022682434,0.0000051949837,0.0000050555514,0.000058056332,0.0012332195,0.9783646,0.0000018297334,0.0005516684,0.0015119172],"study_design_scores_gemma":[0.0005133866,0.000054404736,0.4422975,0.00007232285,0.0000046953705,0.0000011596609,0.000053629083,0.0049690646,0.5517676,0.00013739403,0.000022417968,0.00010644321],"about_ca_topic_score_codex":0.008004843,"about_ca_topic_score_gemma":0.00049760385,"teacher_disagreement_score":0.42659697,"about_ca_system_score_codex":0.00015888273,"about_ca_system_score_gemma":0.000008842085,"threshold_uncertainty_score":0.99860096},"labels":[],"label_agreement":null},{"id":"W2000098142","doi":"10.1117/12.417083","title":"Lidar and Optical Particle Counter (OPC) measurements of polar and tropical stratospheric aerosols","year":2001,"lang":"en","type":"article","venue":"Proceedings of SPIE, the International Society for Optical Engineering/Proceedings of SPIE","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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; Lidar; Aerosol; Atmospheric sciences; Environmental science; Altitude (triangle); Backscatter (email); Arctic; Polar; Particle (ecology); Extinction (optical mineralogy); Climatology; Remote sensing; Meteorology; Geology; Physics; Mineralogy; Oceanography","score_opus":0.012763600983184967,"score_gpt":0.2178806362534004,"score_spread":0.20511703527021544,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2000098142","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":[0.9966041,0.00011196813,0.00005615849,0.00095920364,0.000058392332,0.000308078,0.000010381347,0.000027015489,0.0018647051],"genre_scores_gemma":[0.9540406,0.00009666326,0.045519814,0.00009075542,0.00008400657,0.00003464413,9.701631e-7,0.000028106802,0.000104455496],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99810606,2.5209197e-8,0.0005145756,0.00034320285,0.0006873136,0.00034882434],"domain_scores_gemma":[0.9992913,0.00005843078,0.00020870924,0.000048878817,0.00022340077,0.00016929068],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031873785,0.00023708367,0.0003354262,0.000003510675,0.00007339264,0.0000669204,0.0004017065,0.00013854768,0.00007511559],"category_scores_gemma":[0.0001830803,0.00019032675,0.00020593769,0.00019913494,0.00054861227,0.00039824267,0.00022223577,0.00018720818,0.0000017864506],"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":[0.00012824516,0.00018394824,0.19592816,0.00013590133,0.00018482585,1.7861571e-7,0.0002128837,0.000047269656,0.7592816,0.0428805,0.0005428865,0.00047363408],"study_design_scores_gemma":[0.0053541707,0.0023748782,0.50542384,0.0004934921,0.00053011323,0.00012253443,0.003949818,0.036101468,0.438293,0.0022079137,0.0038002108,0.0013485185],"about_ca_topic_score_codex":0.000026141362,"about_ca_topic_score_gemma":6.939228e-7,"teacher_disagreement_score":0.32098857,"about_ca_system_score_codex":0.00008908535,"about_ca_system_score_gemma":0.000010463738,"threshold_uncertainty_score":0.77612996},"labels":[],"label_agreement":null},{"id":"W2000210684","doi":"10.1016/j.rse.2004.11.011","title":"Mapping PAR using MODIS atmosphere products","year":2005,"lang":"en","type":"article","venue":"Remote Sensing of Environment","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":76,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"University of Alberta","keywords":"Remote sensing; Environmental science; Satellite; Photosynthetically active radiation; Atmosphere (unit); Aerosol; Atmospheric correction; Vegetation (pathology); Meteorology; Geology; Geography; Physics","score_opus":0.014805197736208671,"score_gpt":0.2062179485286766,"score_spread":0.19141275079246792,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2000210684","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":[0.9667097,0.00013383852,0.027859429,0.0004125616,0.00006919232,0.00020546705,0.0000011202764,0.000031777934,0.0045769685],"genre_scores_gemma":[0.68846804,0.000045558663,0.31082726,0.00010669104,0.00009212785,4.5555588e-8,0.000001308055,0.000024812129,0.00043420194],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9983398,0.000044359644,0.00035169662,0.00045216992,0.000429062,0.000382966],"domain_scores_gemma":[0.99918664,0.000015536154,0.00019419071,0.0004939991,0.0000037379107,0.00010590655],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018312798,0.00021944602,0.00024309954,9.978658e-7,0.00014890927,0.000012044494,0.0001419435,0.0000822671,0.00088222243],"category_scores_gemma":[0.000016111824,0.00021169806,0.00008011391,0.00014429819,0.00027629177,0.00011685996,0.00022735877,0.00012290978,0.00029659364],"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":[0.0000142187955,0.0000793626,0.0031678868,0.000019600626,0.000029444183,0.000017207634,0.0007657628,0.22153705,0.2275798,0.0000030715994,0.0004756498,0.54631096],"study_design_scores_gemma":[0.00065437064,0.00010264552,0.035691537,0.00011948232,0.00006000042,0.000106182284,0.00043954494,0.82271284,0.07086366,0.00021888623,0.068217866,0.0008129633],"about_ca_topic_score_codex":0.00051026547,"about_ca_topic_score_gemma":0.000012144072,"teacher_disagreement_score":0.6011758,"about_ca_system_score_codex":0.00037575734,"about_ca_system_score_gemma":0.000010335304,"threshold_uncertainty_score":0.9659717},"labels":[],"label_agreement":null},{"id":"W2000747888","doi":"10.5194/acpd-9-17073-2009","title":"The ARCTAS aircraft mission: design and execution","year":2009,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":28,"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":"Research center; Archaeology; Aeronautics; Library science; History; Engineering; Political science; Law","score_opus":0.009387317979215208,"score_gpt":0.21824297818890467,"score_spread":0.20885566020968946,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2000747888","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":[0.6481401,0.00041771954,0.20705004,0.014952907,0.00011349512,0.00039614516,1.696842e-7,0.00012182582,0.12880762],"genre_scores_gemma":[0.9803335,0.000073456125,0.010882407,0.00076478056,0.000015060219,0.0000011242347,1.370142e-7,0.0000020807363,0.007927425],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9996056,0.000019934641,0.000057071644,0.00010404609,0.00009918913,0.00011416738],"domain_scores_gemma":[0.99981046,0.000025643818,0.000013741405,0.00009458199,0.0000011155296,0.000054477892],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011620408,0.000047986916,0.000031971158,1.08138856e-7,0.00022106632,0.000023079498,0.00007051955,0.000021659358,0.0007996567],"category_scores_gemma":[0.0000069797015,0.00002580599,0.000011390547,0.00004687872,0.00007498735,0.000049008933,0.000027054008,0.00003339894,0.00011477725],"study_design_candidate":"design_other","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":[0.00006786827,0.00009379192,0.012194288,0.0000011210432,0.000006262786,0.000010696707,0.0004932388,0.002368586,0.026416408,0.0038144216,0.18776284,0.7667705],"study_design_scores_gemma":[0.0006424253,0.0007152491,0.58100075,0.000011969603,0.000020425747,0.000051971838,0.00063298777,0.039933603,0.008376654,0.029560113,0.33854535,0.0005085031],"about_ca_topic_score_codex":0.000026354059,"about_ca_topic_score_gemma":0.0000023963516,"teacher_disagreement_score":0.766262,"about_ca_system_score_codex":0.000018000477,"about_ca_system_score_gemma":0.0000021752676,"threshold_uncertainty_score":0.875568},"labels":[],"label_agreement":null},{"id":"W2001220004","doi":"10.1364/ors.2003.owa5","title":"NIR Spectral Investigations of Water in Clouds with FTS","year":2003,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"Trent University","funders":"","keywords":"Remote sensing; Liquid water; Environmental science; Water ice; Liquid water content; Aerospace engineering; Astrobiology; Materials science; Cloud computing; Geology; Physics; Earth science; Computer science; Engineering","score_opus":0.00682049199784552,"score_gpt":0.18944036199286235,"score_spread":0.18261986999501684,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2001220004","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":[0.86939067,0.0000020435734,0.00036119198,0.00012392523,0.00001223393,0.00005561166,2.6098257e-7,0.000008159693,0.13004588],"genre_scores_gemma":[0.98576367,0.0000013315831,0.011101396,0.00014512043,0.0000034111547,0.000004133738,6.756143e-7,0.000004817036,0.0029754166],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99951434,0.000016401733,0.00009998387,0.00011035149,0.0001082295,0.00015066248],"domain_scores_gemma":[0.999827,0.0000054951006,0.000014475684,0.00010544714,0.0000015672978,0.00004596272],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000067800946,0.00005641704,0.00006726399,5.5605244e-7,0.000022340932,0.000003825015,0.000059708305,0.000022373113,0.004282591],"category_scores_gemma":[0.0000043179557,0.000032668744,0.000012912191,0.00011815166,0.00015207495,0.000060116112,0.000018536526,0.000043255874,0.00010192247],"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":[0.0000041613785,0.000062807434,0.97674674,0.0000019157756,0.000002779614,0.0000034928555,0.0005142547,0.0019112757,0.016293276,0.0038359512,0.00051983807,0.00010351436],"study_design_scores_gemma":[0.0008122821,0.0002323907,0.63501626,0.000012651222,0.000009886204,0.000013693968,0.00066952145,0.00048614715,0.34980696,0.006886251,0.005734922,0.00031904812],"about_ca_topic_score_codex":0.000384116,"about_ca_topic_score_gemma":0.0005550625,"teacher_disagreement_score":0.34173048,"about_ca_system_score_codex":0.000031766165,"about_ca_system_score_gemma":0.0000060185075,"threshold_uncertainty_score":0.9966276},"labels":[],"label_agreement":null},{"id":"W2001393574","doi":"10.1029/2006gl026794","title":"Cloudless aerosol forcing efficiency in the UV region from AERONET and WOUDC databases","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Air Canada","funders":"","keywords":"AERONET; Aerosol; Environmental science; Forcing (mathematics); Atmospheric sciences; Climatology; Meteorology; Geography; Physics; Geology","score_opus":0.0325110527788559,"score_gpt":0.28497900282738153,"score_spread":0.2524679500485256,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2001393574","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":[0.99263924,0.000055333257,0.0021618248,0.0039544464,0.000034591987,0.00027919878,0.000005004693,0.000018566538,0.0008517971],"genre_scores_gemma":[0.9981617,0.00001555078,0.00032925003,0.0009957757,0.00023093469,0.000044625758,0.000016459966,0.000013881017,0.00019184953],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9975286,0.0002693323,0.00017643187,0.0004853687,0.0008718892,0.0006683737],"domain_scores_gemma":[0.99890685,0.00055281987,0.000034978253,0.0004201121,0.0000060124817,0.00007923196],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043473954,0.00014225788,0.00014737835,0.0000038673825,0.00030370444,0.00009182355,0.00045187405,0.00003724671,0.00009169143],"category_scores_gemma":[0.00006020736,0.00009873388,0.00004015242,0.0004733059,0.0007534191,0.00018713926,0.00039973485,0.00047048205,0.00018197283],"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":[0.00034627688,0.0015265364,0.39379472,0.00004746033,0.000023036342,0.0006422853,0.0050670784,0.004652594,0.40238035,0.002626932,0.1459031,0.042989653],"study_design_scores_gemma":[0.0013553587,0.00024393511,0.9714149,0.0000912298,0.000015705093,0.000010849826,0.0020048323,0.009020063,0.0034655072,0.002039577,0.009691705,0.0006462904],"about_ca_topic_score_codex":0.039591648,"about_ca_topic_score_gemma":0.0007738155,"teacher_disagreement_score":0.5776202,"about_ca_system_score_codex":0.00009737141,"about_ca_system_score_gemma":0.000008932649,"threshold_uncertainty_score":0.9668038},"labels":[],"label_agreement":null},{"id":"W2002971162","doi":"10.1029/2012jd017668","title":"The dependence of ice microphysics on aerosol concentration in arctic mixed‐phase stratus clouds during ISDAC and M‐PACE","year":2012,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":151,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"National Research Council Canada; Environment and Climate Change Canada","funders":"","keywords":"Aerosol; Atmospheric sciences; Liquid water content; Cloud base; Environmental science; Effective radius; Cloud condensation nuclei; Ice crystals; Cloud top; Arctic; Meteorology; Climatology; Cloud computing; Geology; Physics; Oceanography","score_opus":0.020854120957227846,"score_gpt":0.3103086867547496,"score_spread":0.28945456579752177,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2002971162","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":[0.9983276,0.0005550557,0.00008088127,0.00023050325,0.000112685266,0.00018471589,0.0000018512123,0.0000026088028,0.0005040823],"genre_scores_gemma":[0.9985779,0.00041520194,0.0004725407,0.000019657973,0.00021894492,0.0000054421016,2.4121175e-7,0.000014919786,0.00027515518],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99718386,0.00032783442,0.00046006046,0.00018595251,0.00115847,0.0006838213],"domain_scores_gemma":[0.9981912,0.0009055908,0.00027742106,0.0002379915,0.0000888167,0.00029902955],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009414489,0.00015838382,0.00026361656,0.0000012270765,0.0002678796,0.0000695793,0.00037831912,0.00007257066,0.00013275557],"category_scores_gemma":[0.00043240836,0.00010591659,0.00009334267,0.00041120857,0.0007381722,0.0004134653,0.00019014289,0.00077285705,0.00004768637],"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":[0.0026581523,0.0028347007,0.187288,0.000111761394,0.0000977278,0.000087249995,0.002269481,0.0018689759,0.7568331,0.0026542244,0.0008933609,0.042403273],"study_design_scores_gemma":[0.0038629477,0.0034646871,0.84209645,0.00035571062,0.000040171166,0.00004595541,0.0036664184,0.0022583632,0.14014365,0.0028612104,0.0007661876,0.0004382455],"about_ca_topic_score_codex":0.0005837798,"about_ca_topic_score_gemma":0.00011864163,"teacher_disagreement_score":0.65480846,"about_ca_system_score_codex":0.00022625175,"about_ca_system_score_gemma":0.000063040156,"threshold_uncertainty_score":0.4319153},"labels":[],"label_agreement":null},{"id":"W2003688041","doi":"10.1016/j.earscirev.2014.11.001","title":"Aerosol remote sensing in polar regions","year":2014,"lang":"en","type":"article","venue":"Earth-Science Reviews","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":162,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; Institut du Savoir Montfort; Université de Sherbrooke","funders":"National Oceanic and Atmospheric Administration; U.S. Department of Energy","keywords":"AERONET; Aerosol; Environmental science; Angstrom exponent; Sun photometer; Arctic; Atmospheric sciences; Climatology; Polar night; Oceanography; Geography; Geology; Meteorology","score_opus":0.016970639264792187,"score_gpt":0.250911482127045,"score_spread":0.2339408428622528,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2003688041","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.31567186,0.002223576,0.5184056,0.0023459943,0.0007078157,0.0013990223,0.0000012529833,0.00014754961,0.15909728],"genre_scores_gemma":[0.63517237,0.0024519847,0.35602146,0.0025413134,0.00014787866,0.0000028422244,0.0000012379443,0.000029286108,0.0036316293],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9980416,0.00013818941,0.00036546757,0.00051467185,0.00040162276,0.00053840387],"domain_scores_gemma":[0.9990453,0.000031829175,0.0001354084,0.00058722607,0.000006938515,0.00019330841],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001939352,0.00016347636,0.00028538928,0.0000046892205,0.00027957544,0.00005770456,0.00042757194,0.000047683894,0.0005188638],"category_scores_gemma":[0.00034747366,0.00012959725,0.00008230948,0.001124077,0.00064750656,0.0003206934,0.0002203689,0.000184514,0.002217694],"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":[0.0000026628575,0.000027084752,0.002892787,0.000014696598,7.5751353e-7,0.000007694074,0.00053084095,0.00017093211,0.26369393,0.00031539283,0.0016089098,0.7307343],"study_design_scores_gemma":[0.00030998164,0.000119970064,0.017319724,0.00025701578,0.000010687022,0.00005792454,0.00007909466,0.014425635,0.010852723,0.0009921836,0.9549518,0.000623238],"about_ca_topic_score_codex":0.0005385279,"about_ca_topic_score_gemma":0.00048527127,"teacher_disagreement_score":0.9533429,"about_ca_system_score_codex":0.00009136826,"about_ca_system_score_gemma":0.000024384697,"threshold_uncertainty_score":0.9985592},"labels":[],"label_agreement":null},{"id":"W2003761273","doi":"10.1029/2007jd009677","title":"Overlap of fractional cloud for radiation calculations in GCMs: A global analysis using CloudSat and CALIPSO data","year":2008,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":71,"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":"Parametrization (atmospheric modeling); Lidar; Environmental science; Cloud height; Atmospheric sciences; Radiative transfer; Precipitation; Radar; Satellite; Meteorology; Cloud top; Cloud computing; Remote sensing; Physics; Cloud cover; Geology; Astronomy","score_opus":0.07995242804449655,"score_gpt":0.3779498112621869,"score_spread":0.29799738321769037,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2003761273","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":[0.9846448,0.0002961504,0.014507499,0.00016503301,0.0000555175,0.00015299229,0.000048061564,0.0000024639223,0.0001275239],"genre_scores_gemma":[0.9901166,0.00013657827,0.009421586,0.000020366664,0.00022424367,0.0000024931207,0.000008844089,0.000007728079,0.00006153825],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99777555,0.00016605575,0.0004899529,0.00025448677,0.0009958479,0.00031810303],"domain_scores_gemma":[0.9986995,0.00046321226,0.00026204088,0.00028403066,0.00010808364,0.00018313048],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00076425564,0.00010830854,0.0003537701,0.0000034951656,0.00020121003,0.000022662292,0.00036564202,0.000077402736,0.00025934924],"category_scores_gemma":[0.00045357906,0.0000908911,0.00014556752,0.0012495359,0.0004486715,0.00042643334,0.00027299143,0.00026435565,0.0000045050792],"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":[0.00035685493,0.00053230056,0.925305,0.000014486975,0.00028715414,0.000025995025,0.00021567119,0.06371311,0.00088278385,0.00045387994,0.0022216078,0.005991125],"study_design_scores_gemma":[0.00058662385,0.00020794098,0.7639336,0.000013915295,0.000097605254,0.000017467371,0.00023857615,0.23217565,0.000029711844,0.001561489,0.0010512627,0.000086170134],"about_ca_topic_score_codex":0.0042571737,"about_ca_topic_score_gemma":0.0005797627,"teacher_disagreement_score":0.16846253,"about_ca_system_score_codex":0.0002897808,"about_ca_system_score_gemma":0.00016419246,"threshold_uncertainty_score":0.6435602},"labels":[],"label_agreement":null},{"id":"W2004877374","doi":"10.1002/joc.582","title":"Variability of cloud microphysical and optical parameters obtained from aircraft and satellite remote sensing measurements during RACE","year":2001,"lang":"en","type":"article","venue":"International Journal of Climatology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Research Council Canada; National Aeronautics and Space Administration","keywords":"Environmental science; Bay; Satellite; Lidar; Liquid water content; Remote sensing; Effective radius; Cloud fraction; Aerosol; Advanced very-high-resolution radiometer; Atmospheric sciences; Meteorology; Cloud cover; Cloud computing; Geology; Physics","score_opus":0.013472149426163607,"score_gpt":0.25061703685220105,"score_spread":0.23714488742603745,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2004877374","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":[0.9898513,0.00006489292,0.0085789375,0.000883514,0.0002617015,0.00003808081,0.0000018276478,0.0000036857857,0.00031605823],"genre_scores_gemma":[0.9587719,0.00019783142,0.04086113,0.000095814845,0.000057066012,4.5448655e-8,7.147103e-7,0.0000062809504,0.000009248541],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99884844,0.00009928049,0.00043116935,0.00016509849,0.00031618326,0.00013982128],"domain_scores_gemma":[0.99930257,0.00019840173,0.00026992458,0.000082088285,0.000055163484,0.00009182916],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028181716,0.000097170414,0.00026235578,0.0000047154954,0.00003281656,0.000016986103,0.0001444112,0.0000656596,0.00007009973],"category_scores_gemma":[0.00016231,0.000084188876,0.000057018457,0.000043105792,0.0003193598,0.000102236954,0.00014354457,0.0001460829,0.000004312229],"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":[0.00068126054,0.00008766483,0.8451627,0.000006484575,0.00015742866,0.0001910536,0.00035529135,0.00020430435,0.12883383,0.000052920386,0.00001335411,0.024253726],"study_design_scores_gemma":[0.0021950467,0.00017509612,0.9705209,0.00008799639,0.00009018001,0.0020701997,0.00018709392,0.0038477974,0.013275301,0.0068810694,0.00044747518,0.0002218477],"about_ca_topic_score_codex":0.00011513133,"about_ca_topic_score_gemma":0.000013948399,"teacher_disagreement_score":0.12535822,"about_ca_system_score_codex":0.00007321137,"about_ca_system_score_gemma":0.0000103500415,"threshold_uncertainty_score":0.34331226},"labels":[],"label_agreement":null},{"id":"W2006683097","doi":"10.1029/2005jd006200","title":"Reconciliation of coarse mode sea‐salt aerosol particle size measurements and parameterizations at a subtropical ocean receptor site","year":2006,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":105,"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 de Sherbrooke","funders":"Brookhaven National Laboratory; Office of Naval Research; University of Leeds","keywords":"Aerosol; Environmental science; Atmospheric sciences; Spectrometer; Sea salt; Single-scattering albedo; Meteorology; Physics; Optics","score_opus":0.032865016454344934,"score_gpt":0.2944161703079175,"score_spread":0.2615511538535726,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2006683097","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":[0.9985103,0.00007470958,0.00041935928,0.00042392782,0.000050646835,0.00018766982,0.000011315498,0.000008882463,0.0003132165],"genre_scores_gemma":[0.99199533,0.0000507745,0.0067540454,0.000032424483,0.00013184434,0.0000045641777,0.0000023678185,0.00001849549,0.0010101446],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99703014,0.00031763455,0.0005615243,0.00024752467,0.0013983274,0.00044486794],"domain_scores_gemma":[0.99852574,0.00052153063,0.00028332812,0.00021042836,0.00018846948,0.00027051035],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005702339,0.00014578259,0.00031685218,0.0000012882413,0.00022073348,0.000048310474,0.00023075187,0.000081182545,0.00086111424],"category_scores_gemma":[0.000706183,0.000116536954,0.00012066314,0.00039247106,0.0005405866,0.00029936607,0.00022232078,0.00029854442,0.000055413177],"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":[0.0004992917,0.0005965263,0.7260392,0.000021413283,0.0000398477,0.000009798272,0.00020085141,0.0017314684,0.2582672,0.00012035024,0.0098783625,0.002595693],"study_design_scores_gemma":[0.002780739,0.002653177,0.8714912,0.00012478775,0.00007573651,0.000020190222,0.00023505726,0.023502596,0.09054389,0.006332252,0.0017905241,0.00044987033],"about_ca_topic_score_codex":0.0019864978,"about_ca_topic_score_gemma":0.0004942195,"teacher_disagreement_score":0.16772331,"about_ca_system_score_codex":0.00029145568,"about_ca_system_score_gemma":0.000053065476,"threshold_uncertainty_score":0.9428597},"labels":[],"label_agreement":null},{"id":"W2006790147","doi":"10.1029/2011jd016675","title":"Ice clouds microphysical retrieval using 94‐GHz Doppler radar observations: Basic relations within the retrieval framework","year":2012,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"","keywords":"Ice cloud; Ice crystals; Doppler effect; Radiative transfer; Radar; Computational physics; Particle-size distribution; Remote sensing; Scattering; Wavelength; Physics; Observable; Environmental science; Optics; Particle size; Geology; Computer science","score_opus":0.05818298938647396,"score_gpt":0.3262469832492592,"score_spread":0.26806399386278523,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2006790147","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":[0.99275124,0.0005651268,0.003355257,0.0017875925,0.0005360878,0.00033352122,0.000006231522,0.000021713846,0.0006432466],"genre_scores_gemma":[0.9571039,0.000049879494,0.038898807,0.00028602764,0.0021754927,0.0000022013655,0.0000017582776,0.00005718572,0.0014247263],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9939992,0.0008416851,0.00088200066,0.00035284474,0.0028256096,0.0010986757],"domain_scores_gemma":[0.9958436,0.0020457585,0.0005451785,0.0006571058,0.00027773427,0.0006306081],"candidate_categories":["research_integrity","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0027879619,0.00031608995,0.00047253753,0.000003674683,0.0011276283,0.00019243393,0.0010835474,0.0002535762,0.0017124554],"category_scores_gemma":[0.0025709192,0.00020781164,0.00037884887,0.002079583,0.0013153236,0.001003928,0.0005876884,0.0026402015,0.000587291],"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":[0.0057153027,0.0057946895,0.35152692,0.00009231104,0.00095731707,0.00020040385,0.010756265,0.016452868,0.49431583,0.038057648,0.07234203,0.0037884044],"study_design_scores_gemma":[0.0021901217,0.0022322026,0.85624504,0.00047658265,0.00039837434,0.0002940007,0.005601259,0.017336912,0.016686236,0.065479934,0.031667642,0.00139168],"about_ca_topic_score_codex":0.0005284828,"about_ca_topic_score_gemma":0.0000130196895,"teacher_disagreement_score":0.5047181,"about_ca_system_score_codex":0.0006671721,"about_ca_system_score_gemma":0.0002603585,"threshold_uncertainty_score":0.99966073},"labels":[],"label_agreement":null},{"id":"W2007318301","doi":"10.1093/mnras/sts278","title":"The ultimate meteorological question from observational astronomers: how good is the cloud cover forecast?","year":2012,"lang":"en","type":"article","venue":"Monthly Notices of the Royal Astronomical Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; Western University","funders":"","keywords":"International Satellite Cloud Climatology Project; Cloud cover; Cloud computing; Meteorology; Environmental science; Global Forecast System; Satellite; Forecast skill; Climatology; Cloud height; Atmospheric sciences; Numerical weather prediction; Geography; Computer science; Physics; Geology","score_opus":0.015770640702259815,"score_gpt":0.21212598943689223,"score_spread":0.19635534873463242,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007318301","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":[0.9916536,0.00017402759,0.00043979858,0.006449146,0.00041615308,0.00025941015,0.00006682299,0.00001762187,0.00052341644],"genre_scores_gemma":[0.9913205,7.181021e-7,0.0071560876,0.0003697233,0.0003691778,0.0000298178,0.000011597104,0.000014223359,0.0007281388],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99842805,0.00016165987,0.0002750322,0.00025931824,0.00037600845,0.0004999208],"domain_scores_gemma":[0.99873054,0.0004333088,0.00030642908,0.0004077205,0.0000115556595,0.0001104449],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005965365,0.00021111821,0.00019861686,2.796561e-7,0.00057407084,0.00008160134,0.00082966627,0.00012198468,0.0007797123],"category_scores_gemma":[0.000047961206,0.00009933461,0.0004340109,0.00007509222,0.0008047474,0.00021386103,0.0005927751,0.00030057708,0.00008503986],"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":[0.000053388343,0.0001095066,0.68583626,0.0000015739464,0.00011198238,1.3429113e-8,0.0005002527,0.29751685,0.000052965366,0.00016374665,0.013139993,0.0025134769],"study_design_scores_gemma":[0.0002052559,0.0000407292,0.7849264,0.0000042888637,0.00006664989,8.798484e-9,0.00039123907,0.19733447,0.00017859192,0.00006320605,0.016679171,0.00010994512],"about_ca_topic_score_codex":0.0006445595,"about_ca_topic_score_gemma":0.000027809849,"teacher_disagreement_score":0.10018238,"about_ca_system_score_codex":0.00019969145,"about_ca_system_score_gemma":0.000013148164,"threshold_uncertainty_score":0.85373026},"labels":[],"label_agreement":null},{"id":"W2007426147","doi":"10.1029/2000gl012067","title":"Cloud optical depths and TOA fluxes: Comparison between satellite and surface retrievals from multiple platforms","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":22,"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; Natural Resources Canada","funders":"Centre National d’Etudes Spatiales; Langley Research Center; U.S. Department of Energy","keywords":"Radiative transfer; Environmental science; Remote sensing; Inversion (geology); Shortwave; Cloud computing; Satellite; Broadband; Meteorology; Atmospheric radiative transfer codes; Cloud top; Cloud fraction; Flux (metallurgy); Cloud cover; Computer science; Geology; Physics; Optics; Telecommunications; Materials science; Astronomy","score_opus":0.04181469243076415,"score_gpt":0.30951975065682213,"score_spread":0.267705058226058,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007426147","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":[0.9963133,0.0001440549,0.0006391852,0.0019020297,0.00004239848,0.00027796708,0.000011748469,0.00003897656,0.00063034263],"genre_scores_gemma":[0.99698615,0.00015623252,0.0019198819,0.00037722837,0.00027341698,0.000006620151,0.000014834499,0.000023736591,0.0002419043],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99720293,0.000090144546,0.00026552618,0.00062955776,0.0009817017,0.0008301159],"domain_scores_gemma":[0.9979519,0.0011799054,0.0000417287,0.00032411062,0.000013435793,0.0004889149],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045021565,0.00020663424,0.00034224498,0.0000033092408,0.00031680558,0.00013547877,0.00028963256,0.0001173077,0.0002506092],"category_scores_gemma":[0.00018539642,0.00016850565,0.00005343276,0.0003581404,0.0011147136,0.0002359024,0.0006086081,0.0006183513,0.00051092653],"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":[0.00017160611,0.000090999674,0.9011565,0.0000076797205,0.00003056962,0.000039234623,0.000603272,0.000082067934,0.06730339,0.000055027678,0.0026588598,0.027800797],"study_design_scores_gemma":[0.00072803214,0.00028860322,0.9814121,0.000023047225,0.000016125001,0.0000021722963,0.00039554964,0.0029870768,0.0033344815,0.0011364266,0.009354425,0.0003219289],"about_ca_topic_score_codex":0.0022542581,"about_ca_topic_score_gemma":0.00010448635,"teacher_disagreement_score":0.080255635,"about_ca_system_score_codex":0.00011136429,"about_ca_system_score_gemma":0.000008687714,"threshold_uncertainty_score":0.68714607},"labels":[],"label_agreement":null},{"id":"W2007704598","doi":"10.1029/2005eo410004","title":"Count‐a‐thon of airplane contrails","year":2005,"lang":"en","type":"article","venue":"Eos","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":5,"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":"U.S. Geological Survey; National Aeronautics and Space Administration; Canadian Space Agency; National Science Foundation","keywords":"Globe; Meteorology; Airplane; Satellite; Cloud computing; Cloud cover; Environmental science; Sky; Geography; Computer science; Engineering; Psychology; Aerospace engineering","score_opus":0.004081746864179549,"score_gpt":0.19839924383096805,"score_spread":0.1943174969667885,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007704598","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":[0.9329894,0.000056528832,0.0006241965,0.00025614607,0.0000446963,0.00006532104,0.00000382573,0.000017515924,0.06594237],"genre_scores_gemma":[0.994672,0.000009777286,0.0019851553,0.00028594222,0.00005037191,0.0000027707033,0.0000012792543,0.0000046196683,0.002988072],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9995456,0.000007620899,0.000096390075,0.00009421518,0.00013854934,0.00011762583],"domain_scores_gemma":[0.9998048,0.0000125338,0.000025918469,0.00011514154,0.000001942168,0.00003964495],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000060316306,0.00005052151,0.00007500888,2.2376372e-7,0.000026258509,0.0000036658016,0.00009539642,0.000028990133,0.0074553667],"category_scores_gemma":[0.0000060175903,0.000042223583,0.00002274811,0.00004369376,0.00007815988,0.000055316486,0.000030771163,0.000036628615,0.00074401207],"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":[0.000063216314,0.00036913165,0.37527415,0.000015048052,0.000029857894,0.000015350368,0.0018018467,0.004485115,0.125098,0.0010804074,0.11860997,0.3731579],"study_design_scores_gemma":[0.0006099642,0.00014885928,0.38831374,0.000012012102,0.00001638353,0.000012435776,0.00015533122,0.0025169873,0.02156935,0.00016200756,0.5862103,0.00027259404],"about_ca_topic_score_codex":0.00014404164,"about_ca_topic_score_gemma":0.000099920515,"teacher_disagreement_score":0.46760038,"about_ca_system_score_codex":0.00002956582,"about_ca_system_score_gemma":0.0000030516,"threshold_uncertainty_score":0.99345195},"labels":[],"label_agreement":null},{"id":"W2008331801","doi":"10.1175/jas3668.1","title":"Using MODIS and AERONET to Determine GCM Aerosol Size","year":2006,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"AERONET; Aerosol; Environmental science; Moderate-resolution imaging spectroradiometer; Forcing (mathematics); Atmospheric sciences; Atmosphere (unit); Range (aeronautics); Mode (computer interface); Climatology; Meteorology; Remote sensing; Satellite; Physics; Geography; Geology; Computer science; Materials science","score_opus":0.01901320151628644,"score_gpt":0.24383427870645136,"score_spread":0.22482107719016492,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2008331801","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":[0.99593073,0.00016257292,0.0006275989,0.0010076128,0.00033681336,0.00010208861,5.1621197e-7,0.000006473991,0.001825576],"genre_scores_gemma":[0.9261681,0.000010311155,0.07240858,0.00058065396,0.00013256898,0.0000010084265,1.0466497e-8,0.00000765458,0.0006911429],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99846804,0.00005361953,0.00035354155,0.00020376834,0.0006181933,0.00030281732],"domain_scores_gemma":[0.99926996,0.00008938487,0.00032903007,0.0001721954,0.000015716289,0.00012373697],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00049948203,0.00014100966,0.00019836001,3.9034066e-7,0.00041274203,0.000099652505,0.00068754505,0.000038624723,0.00044734048],"category_scores_gemma":[0.000093016075,0.000080989936,0.00008874925,0.0006393153,0.0005742905,0.00030920946,0.0003328244,0.00010685347,0.000013906909],"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":[0.00004926596,0.00014770302,0.4489644,0.000006651879,0.000017203127,0.000025061498,0.000505308,0.40124962,0.13125014,0.00006537787,0.008874972,0.008844303],"study_design_scores_gemma":[0.001612838,0.0015500339,0.74707896,0.00020147709,0.00019532535,0.0014708894,0.0015632954,0.21767724,0.012244519,0.004684661,0.010500328,0.0012204616],"about_ca_topic_score_codex":0.0006507763,"about_ca_topic_score_gemma":0.00006926705,"teacher_disagreement_score":0.29811454,"about_ca_system_score_codex":0.000101128586,"about_ca_system_score_gemma":0.000035745383,"threshold_uncertainty_score":0.48980644},"labels":[],"label_agreement":null},{"id":"W2008441326","doi":"10.1029/2001jd000652","title":"Micrometer‐sized hygroscopic particles in the atmosphere: Aircraft measurement in the Arctic","year":2001,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":8,"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":"U.S. Air Force","keywords":"Atmospheric sciences; Environmental science; Relative humidity; Arctic; Humidity; Meteorology; Altitude (triangle); Drizzle; Atmosphere (unit); Geology; Physics","score_opus":0.049159488001324025,"score_gpt":0.3108412878690433,"score_spread":0.2616817998677193,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2008441326","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":[0.9920486,0.0005491869,0.00012826297,0.005318455,0.00006986553,0.00039671976,3.8211022e-7,0.0000050228778,0.0014834612],"genre_scores_gemma":[0.9977627,0.00023489045,0.0010762501,0.00052079966,0.00018804202,0.000040332587,1.9725537e-7,0.000017677248,0.0001591516],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9935858,0.0014543026,0.00067445583,0.0002906209,0.0031003016,0.00089451316],"domain_scores_gemma":[0.99813515,0.0009380054,0.00018467427,0.00048499223,0.00010103191,0.0001561684],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.005462384,0.00021271646,0.00035626406,0.0000016423376,0.0002355734,0.00017933089,0.0015497077,0.00007904499,0.0010030281],"category_scores_gemma":[0.0008483026,0.00011048337,0.00019432938,0.0015901489,0.00058478327,0.0003060276,0.00020254262,0.0012430176,0.000253473],"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":[0.0010497743,0.0041404236,0.8909201,0.000049290626,0.000085868094,0.0015289383,0.0073345997,0.0030059,0.02192867,0.00055790733,0.015813902,0.053584613],"study_design_scores_gemma":[0.00139775,0.0009859556,0.97374886,0.000115514005,0.000017052877,0.00007880954,0.0043015964,0.001000563,0.00023892068,0.008578967,0.009362909,0.00017309464],"about_ca_topic_score_codex":0.00355013,"about_ca_topic_score_gemma":0.0029712683,"teacher_disagreement_score":0.08282875,"about_ca_system_score_codex":0.00045908694,"about_ca_system_score_gemma":0.00011277146,"threshold_uncertainty_score":0.9999102},"labels":[],"label_agreement":null},{"id":"W2008585834","doi":"10.1007/s10546-013-9872-4","title":"Turbulence in Continental Stratocumulus, Part II: Eddy Dissipation Rates and Large-Eddy Coherent Structures","year":2013,"lang":"en","type":"article","venue":"Boundary-Layer Meteorology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Dissipation; Turbulence kinetic energy; Turbulence; Cloud top; Radiative cooling; Atmospheric sciences; Marine stratocumulus; Physics; Meteorology; Computational physics; Environmental science; Thermodynamics","score_opus":0.009422335609617473,"score_gpt":0.2435817237473509,"score_spread":0.23415938813773343,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2008585834","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":[0.9966055,0.00039006607,0.0004883455,0.00066621235,0.00028086093,0.0005355441,0.000014395192,0.000040491348,0.0009785501],"genre_scores_gemma":[0.9966812,0.000044993187,0.0017522488,0.00061967754,0.000065322965,0.00012377302,0.000024103858,0.000020354915,0.00066831865],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99815094,0.00014169069,0.00037780183,0.0005293086,0.00023367765,0.0005665627],"domain_scores_gemma":[0.9993745,0.000058532514,0.00013657687,0.00025897124,0.000012759787,0.0001586627],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00022585079,0.00026178246,0.00030897494,0.000005380063,0.00031689648,0.000101043435,0.00022215743,0.00017285431,0.00986406],"category_scores_gemma":[0.000043030224,0.00021749844,0.000045109668,0.00014978029,0.00048183912,0.00036357736,0.00031280113,0.00023894903,0.00015459889],"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":[0.0001001714,0.00027335272,0.9515854,0.000015611171,0.000037089387,0.00002151588,0.0013767096,0.0003698405,0.018859548,0.0015618014,0.006920576,0.018878393],"study_design_scores_gemma":[0.0013130864,0.00044270145,0.9538371,0.000009499845,0.0000227136,0.000027865002,0.0004062954,0.0040507894,0.0014650343,0.0071347696,0.030891618,0.00039851322],"about_ca_topic_score_codex":0.0017666941,"about_ca_topic_score_gemma":0.0016370078,"teacher_disagreement_score":0.023971042,"about_ca_system_score_codex":0.000081319275,"about_ca_system_score_gemma":0.000025474354,"threshold_uncertainty_score":0.99104106},"labels":[],"label_agreement":null},{"id":"W2008820700","doi":"10.1007/s00162-012-0288-4","title":"Analysis and numerical simulation of a laboratory analog of radiatively induced cloud-top entrainment","year":2012,"lang":"en","type":"article","venue":"Theoretical and Computational Fluid Dynamics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":8,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Cascades (Canada)","funders":"Laboratory Directed Research and Development; Sandia National Laboratories; U.S. Department of Energy","keywords":"Entrainment (biomusicology); Richardson number; Mechanics; Stratification (seeds); Turbulence; Environmental science; Convection; Thermodynamics; Meteorology; Physics; Atmospheric sciences","score_opus":0.004161173789262589,"score_gpt":0.22495276735956812,"score_spread":0.22079159357030553,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2008820700","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":[0.7301981,0.00002730445,0.26939788,0.00004755027,0.000014119544,0.00004677276,0.000020951873,0.00000442229,0.0002429123],"genre_scores_gemma":[0.9964294,0.0000056375825,0.0034445846,0.00007709368,0.000015608799,0.0000018575696,0.000018682278,0.000004580728,0.0000025829918],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999212,0.00007118384,0.00022079433,0.0001295507,0.00023499588,0.00013143432],"domain_scores_gemma":[0.9994959,0.00023595874,0.00007714891,0.000060450733,0.000019494786,0.00011104642],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020058932,0.000087914144,0.0001962129,0.0000055666674,0.000040744468,0.0000049813502,0.000048944017,0.000048364665,0.0003112476],"category_scores_gemma":[0.00003075068,0.000074041774,0.000041746174,0.0003493486,0.00046349614,0.000061443774,0.00007476723,0.000050497423,0.0000023014948],"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":[0.00005922478,0.00018034266,0.45215052,0.0000096429985,0.00013312761,3.9033142e-7,0.0007419192,0.18904153,0.00072632136,0.35232422,0.0000023430478,0.00463042],"study_design_scores_gemma":[0.00012355763,0.000056578716,0.32857224,0.0000016539868,0.00008338884,4.266638e-7,0.00006359575,0.6625263,0.00005418594,0.008457279,0.000001985619,0.000058802772],"about_ca_topic_score_codex":0.000017045337,"about_ca_topic_score_gemma":7.51919e-7,"teacher_disagreement_score":0.47348478,"about_ca_system_score_codex":0.00004013776,"about_ca_system_score_gemma":0.000007967452,"threshold_uncertainty_score":0.3407943},"labels":[],"label_agreement":null},{"id":"W2009286001","doi":"10.1117/12.898577","title":"TICFIRE: a far infrared payload to monitor the evolution of thin ice clouds","year":2011,"lang":"en","type":"article","venue":"Proceedings of SPIE, the International Society for Optical Engineering/Proceedings of SPIE","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":17,"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; NGC Aerospace (Canada); Institut National d'Optique; Université de Sherbrooke; Université du Québec à Montréal","funders":"","keywords":"Radiance; Remote sensing; Environmental science; Payload (computing); Nadir; Microbolometer; Troposphere; Satellite; Atmosphere (unit); Meteorology; Far infrared; Computer science; Geology; Physics; Optics; Detector; Astronomy; Telecommunications; Bolometer","score_opus":0.009669093515844857,"score_gpt":0.2080502198949034,"score_spread":0.19838112637905855,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2009286001","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":[0.9892086,0.000058136946,0.00016437835,0.0010514862,0.0002176143,0.00056040357,0.000021253762,0.000050678475,0.0086674765],"genre_scores_gemma":[0.9224315,0.0000357419,0.07639934,0.0001662293,0.00018820041,0.00012960995,0.0000013084727,0.000041668714,0.0006063879],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9978533,2.9041816e-8,0.00062536576,0.0003517861,0.00078866846,0.00038086282],"domain_scores_gemma":[0.9989433,0.00007788925,0.00037097046,0.00009290575,0.00037746906,0.00013743434],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00059710885,0.0002734257,0.00031847524,0.000008552734,0.00011188713,0.00004003091,0.0012950115,0.00016229891,0.00010888444],"category_scores_gemma":[0.00036669307,0.00019089805,0.00043979794,0.00046474824,0.00039111386,0.00037867532,0.00039878627,0.00025461568,0.000011366178],"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":[0.00024692187,0.0003106781,0.009772329,0.00020981678,0.00036066858,1.1722304e-7,0.0031166577,0.00040212032,0.693866,0.28006947,0.010530454,0.0011147513],"study_design_scores_gemma":[0.0041886107,0.0035075191,0.30529267,0.0009396567,0.000993302,0.000055535187,0.03227311,0.10775391,0.49995565,0.021309191,0.021278655,0.0024521765],"about_ca_topic_score_codex":0.00019369701,"about_ca_topic_score_gemma":7.225603e-7,"teacher_disagreement_score":0.29552034,"about_ca_system_score_codex":0.00031574428,"about_ca_system_score_gemma":0.000017640788,"threshold_uncertainty_score":0.77845967},"labels":[],"label_agreement":null},{"id":"W2009521630","doi":"10.5194/amt-8-2449-2015","title":"The micro-orifice uniform deposit impactor–droplet freezing technique (MOUDI-DFT) for measuring concentrations of ice nucleating particles as a function of size: improvements and initial validation","year":2015,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Ministry of Environment; National Science Foundation","keywords":"Aerosol; Materials science; Particle (ecology); Substrate (aquarium); Nanotechnology; Meteorology; Geology; Physics","score_opus":0.031861547222760515,"score_gpt":0.2510642552611431,"score_spread":0.2192027080383826,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2009521630","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":[0.8477906,0.00020004068,0.14832821,0.00008189498,0.000091085756,0.0017991312,0.0000057828124,0.00014485011,0.0015583747],"genre_scores_gemma":[0.92840904,0.00004793685,0.07107873,0.000046973124,0.000037866495,0.00031696315,0.0000027534654,0.000029258521,0.00003047991],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9979301,0.000099106735,0.000622924,0.00030524886,0.00071162666,0.00033099097],"domain_scores_gemma":[0.9986903,0.00014037362,0.00052346324,0.0003083776,0.0002154519,0.00012202984],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016328518,0.00022031773,0.0002466669,0.0000010161231,0.00032320706,0.000059304726,0.00022986853,0.000105095336,0.000037278962],"category_scores_gemma":[0.00052421016,0.00017721673,0.00007780029,0.00026360195,0.0002282646,0.00032503327,0.00012501134,0.00011080935,0.0000016640904],"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":[0.00018411918,0.00010774367,0.023738926,0.000051355248,0.00005994366,4.2363422e-7,0.00051491737,0.00010601824,0.9404806,0.0002268119,0.00023372933,0.034295402],"study_design_scores_gemma":[0.00064586295,0.0009903176,0.0068989424,0.0001305753,0.00013199318,0.000004637414,0.0012788599,0.0011981447,0.9851153,0.0019713354,0.0013546515,0.00027938854],"about_ca_topic_score_codex":0.0013226168,"about_ca_topic_score_gemma":0.00011969016,"teacher_disagreement_score":0.08061841,"about_ca_system_score_codex":0.00036102685,"about_ca_system_score_gemma":0.0000727571,"threshold_uncertainty_score":0.7226688},"labels":[],"label_agreement":null},{"id":"W2009617466","doi":"10.1364/ao.51.007945","title":"New technique for retrieval of atmospheric temperature profiles from Rayleigh-scatter lidar measurements using nonlinear inversion","year":2012,"lang":"en","type":"article","venue":"Applied Optics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"York University; Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Lidar; Radiosonde; Rayleigh scattering; Remote sensing; Thermosphere; Environmental science; Atmospheric temperature; Altitude (triangle); Backscatter (email); Optics; Atmospheric optics; Inversion (geology); Monte Carlo method; Meteorology; Geology; Physics; Ionosphere; Computer science; Mathematics","score_opus":0.020718326554005104,"score_gpt":0.23714258180619846,"score_spread":0.21642425525219336,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2009617466","genre_codex":"empirical","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93331397,0.0000593383,0.06399193,0.000042355645,0.00016373112,0.0008768184,0.000018303243,0.000033001983,0.0015005454],"genre_scores_gemma":[0.4994174,0.0000033106473,0.5001458,0.00011774413,0.00015313794,0.000010907407,0.000015376721,0.0000243526,0.00011198653],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9987751,0.0000135575365,0.00025753307,0.00024999495,0.00036545607,0.0003383585],"domain_scores_gemma":[0.9993567,0.000029892459,0.00015868383,0.0002840548,0.000016020878,0.00015466005],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001845217,0.00019544216,0.00022194897,7.534257e-7,0.00010827159,0.00001602099,0.00022300165,0.00020772293,0.00044744715],"category_scores_gemma":[0.0000117479,0.00017094151,0.00007074221,0.00022093148,0.00008553073,0.0001251742,0.00015766663,0.00013607771,0.00003700035],"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":[0.00009143618,0.00008602238,0.02486396,0.000014757357,0.00002334945,1.8813081e-7,0.00023407555,0.00023065122,0.973168,0.000059095528,0.0007668594,0.0004615818],"study_design_scores_gemma":[0.00089565886,0.000097907214,0.0064325035,0.000032158052,0.00012862765,0.0000015370343,0.00034894972,0.0017735856,0.9872246,0.00032354795,0.0022996347,0.00044134058],"about_ca_topic_score_codex":0.00009267106,"about_ca_topic_score_gemma":0.000002510221,"teacher_disagreement_score":0.43615386,"about_ca_system_score_codex":0.00013345963,"about_ca_system_score_gemma":0.000029528575,"threshold_uncertainty_score":0.69707924},"labels":[],"label_agreement":null},{"id":"W2009812918","doi":"10.1117/12.558715","title":"A modeling approach for aerosol optical depth analysis during forest fire events","year":2004,"lang":"en","type":"article","venue":"Proceedings of SPIE, the International Society for Optical Engineering/Proceedings of SPIE","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Cégep de Sherbrooke; Université de Sherbrooke","funders":"Goddard Space Flight Center; National Oceanic and Atmospheric Administration; Fonds Québécois de la Recherche sur la Nature et les Technologies","keywords":"Aerosol; Remote sensing; Environmental science; Inversion (geology); Satellite; Photometry (optics); Atmospheric model; Data assimilation; Meteorology; Computer science; Geology; Geography; Physics","score_opus":0.010177449626592157,"score_gpt":0.21626166564586985,"score_spread":0.2060842160192777,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2009812918","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":[0.9903038,0.00003526033,0.0067324345,0.0005760569,0.0000751864,0.00074713526,0.000021840116,0.00007391757,0.0014343833],"genre_scores_gemma":[0.7365341,0.000026258405,0.26285753,0.000037650127,0.000140428,0.0002358079,0.000010752187,0.000046472935,0.000111008885],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9972987,1.17237065e-8,0.0007047581,0.00059443264,0.00082023384,0.0005818205],"domain_scores_gemma":[0.99909234,0.000047402795,0.0002573142,0.00008271607,0.00032571203,0.00019449522],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0004266998,0.00037035067,0.00050600397,0.000014532194,0.00018537427,0.00008202697,0.0009921527,0.00022225984,0.000018267743],"category_scores_gemma":[0.0002447165,0.0003093636,0.001114071,0.0005839271,0.00021746884,0.00051247876,0.00030794233,0.00026648023,0.0000021386293],"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":[0.00033880636,0.0007163979,0.016956018,0.0007748389,0.0022316873,2.1471786e-7,0.00061709067,0.53030044,0.3212584,0.12617041,0.00029754842,0.00033814769],"study_design_scores_gemma":[0.0021864858,0.00030787056,0.006631916,0.00012986438,0.00083706895,0.000013017181,0.0013596757,0.9595443,0.026907278,0.0014098573,0.00005632618,0.00061633915],"about_ca_topic_score_codex":0.00005733526,"about_ca_topic_score_gemma":0.0000017489938,"teacher_disagreement_score":0.4292439,"about_ca_system_score_codex":0.0003882527,"about_ca_system_score_gemma":0.000019493751,"threshold_uncertainty_score":0.99993587},"labels":[],"label_agreement":null},{"id":"W2010248728","doi":"10.1029/2009jd012811","title":"Impact of mesoscale vegetation heterogeneities on the dynamical and thermodynamic properties of the planetary boundary layer","year":2010,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":79,"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 Toronto","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Mesoscale meteorology; Atmospheric sciences; Climatology; Zonal and meridional; Planetary boundary layer; Geology; Boundary layer; Vegetation (pathology); Isoprene; Forcing (mathematics); Monsoon; Environmental science","score_opus":0.021810541458864154,"score_gpt":0.28208194517937035,"score_spread":0.2602714037205062,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2010248728","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":[0.99854416,0.0001793233,0.000010109967,0.0003680774,0.00006135162,0.00015961916,0.0000034203397,0.0000023046384,0.00067164545],"genre_scores_gemma":[0.99961406,0.00003368853,0.000116998875,0.000023896628,0.000069067566,0.0000033577828,2.1657708e-7,0.000012070029,0.00012662286],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9980548,0.00025690725,0.00030974974,0.00012616225,0.0009933803,0.00025898012],"domain_scores_gemma":[0.99902654,0.00032581075,0.00021116096,0.00026946832,0.00007170938,0.00009533366],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005549032,0.00012219674,0.00022641945,0.0000013685124,0.00018665913,0.000035610065,0.000489147,0.000066107925,0.00028297046],"category_scores_gemma":[0.00018947132,0.000051639952,0.00019728823,0.00018170851,0.0017164241,0.00013157401,0.00021150165,0.0007293557,0.000009727599],"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":[0.0006231066,0.00046794576,0.15932989,0.000039472074,0.00016989298,0.0000059953068,0.00093218795,0.0013871974,0.8275983,0.0005567008,0.00045948516,0.008429876],"study_design_scores_gemma":[0.00022238876,0.00092842925,0.9788341,0.000069771304,0.000017242031,0.000014904524,0.00022098116,0.009777863,0.0073935925,0.0023993822,0.0000510503,0.00007032947],"about_ca_topic_score_codex":0.0010054243,"about_ca_topic_score_gemma":0.0003015078,"teacher_disagreement_score":0.8202047,"about_ca_system_score_codex":0.00005141038,"about_ca_system_score_gemma":0.000090718546,"threshold_uncertainty_score":0.63242364},"labels":[],"label_agreement":null},{"id":"W2010827697","doi":"10.1080/02786820902889861","title":"The University of Toronto Continuous Flow Diffusion Chamber (UT-CFDC): A Simple Design for Ice Nucleation Studies","year":2009,"lang":"en","type":"article","venue":"Aerosol Science and Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":76,"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":"Ice nucleus; Aerosol; Chemistry; Settling; Particle (ecology); Nucleation; Mechanics; Analytical Chemistry (journal); Diffusion; Mineralogy; Materials science; Thermodynamics; Chromatography; Physics; Geology","score_opus":0.010168458427755676,"score_gpt":0.22944459178784032,"score_spread":0.21927613336008464,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2010827697","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":[0.98964053,0.0005050827,0.0066546453,0.0019418544,0.00005297476,0.0003697694,0.0000013437108,0.00005575987,0.00077801873],"genre_scores_gemma":[0.9940777,0.00062501384,0.004941149,0.0000862936,0.0000065971444,0.0000029314197,2.408674e-7,0.0000027966012,0.00025731485],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99918807,0.000011964232,0.00009816959,0.00025966275,0.00018200485,0.00026010518],"domain_scores_gemma":[0.99956495,0.00006134749,0.00008056189,0.00020190304,0.000053891705,0.000037332575],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003780966,0.0000814768,0.00012537217,0.0000017487868,0.0008737922,0.0000138294945,0.00026916986,0.000066538356,0.000040979972],"category_scores_gemma":[0.00011931291,0.000058176553,0.000018304403,0.00027945483,0.0016660319,0.00020617583,0.00017667095,0.000042399373,0.0000062168506],"study_design_candidate":"design_other","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":[0.0001242321,0.00015319478,0.0068025044,0.0000069730377,0.00001800241,0.0000051205297,0.0027566028,0.00017655424,0.32884997,0.005431516,0.007864507,0.6478108],"study_design_scores_gemma":[0.010654849,0.01744936,0.15977845,0.00020674871,0.00041232712,0.00017957436,0.12936993,0.23492101,0.19277067,0.07940089,0.17139572,0.0034604773],"about_ca_topic_score_codex":0.00023863987,"about_ca_topic_score_gemma":0.0005674526,"teacher_disagreement_score":0.64435035,"about_ca_system_score_codex":0.000118598764,"about_ca_system_score_gemma":0.000019142635,"threshold_uncertainty_score":0.6720591},"labels":[],"label_agreement":null},{"id":"W2010968187","doi":"10.5194/angeo-20-1891-2002","title":"Cloud microphysical characteristics versus temperature for three Canadian field projects","year":2002,"lang":"en","type":"article","venue":"Annales Geophysicae","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Research Council Canada; Transport Canada; National Aeronautics and Space Administration","keywords":"Environmental science; Bay; Arctic; Atmospheric sciences; Meteorology; Latitude; Climatology; Liquid water content; Cloud computing; Geography; Oceanography; Geology","score_opus":0.018677278616625485,"score_gpt":0.21504134423060994,"score_spread":0.19636406561398445,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2010968187","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":[0.99204826,0.00003917563,0.00004108519,0.0014291618,0.00043615382,0.00033504958,0.00004304379,0.00003756132,0.0055904794],"genre_scores_gemma":[0.9956699,0.000015545473,0.00031989778,0.0010547892,0.00071548566,0.000055029806,0.000016833174,0.000025364116,0.0021271606],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99886787,0.000011617745,0.00013525455,0.00034524515,0.00015732882,0.00048269518],"domain_scores_gemma":[0.9993469,0.000070485075,0.000053940377,0.00029588043,0.000015739104,0.00021701508],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000029026385,0.00019408108,0.0001874293,0.000002010582,0.00025729745,0.000049882827,0.0002622641,0.000105802916,0.00091236766],"category_scores_gemma":[0.000022987908,0.00017504924,0.00012457719,0.00017399571,0.00010386142,0.000102472884,0.00006349583,0.00016575554,0.0011710667],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006489895,0.000935237,0.023226226,0.00009143269,0.00022023899,0.0001248835,0.002911479,0.00009250083,0.05492245,0.003436599,0.6934692,0.21992075],"study_design_scores_gemma":[0.0036861184,0.004538776,0.21875516,0.000084464606,0.0002233147,0.000015310243,0.0004058144,0.010607365,0.012868937,0.0014132346,0.7447126,0.002688941],"about_ca_topic_score_codex":0.0073396806,"about_ca_topic_score_gemma":0.019752035,"teacher_disagreement_score":0.21723181,"about_ca_system_score_codex":0.000080142505,"about_ca_system_score_gemma":0.000018962177,"threshold_uncertainty_score":0.9996066},"labels":[],"label_agreement":null},{"id":"W2011089508","doi":"10.1029/2004jd004922","title":"Importance of vertical velocity variations in the cloud droplet nucleation process of marine stratus clouds","year":2005,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":93,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Killam Trusts; Dalhousie University; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Vertical velocity; Nucleation; Standard deviation; Adiabatic process; Meteorology; Atmospheric sciences; Mechanics; Physics; Thermodynamics; Mathematics; Statistics","score_opus":0.019320508329237998,"score_gpt":0.30968965457531444,"score_spread":0.29036914624607646,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2011089508","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":[0.99515194,0.000034647146,0.00037286087,0.0010244964,0.000033383698,0.00016565475,0.0000024088642,0.0000029133205,0.003211718],"genre_scores_gemma":[0.99716175,0.00004415486,0.0024205456,0.000051968418,0.0002313806,0.0000053298113,9.381766e-7,0.000010626181,0.00007330719],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9970051,0.00026207234,0.0006725832,0.0001647663,0.0015347764,0.00036071186],"domain_scores_gemma":[0.99878937,0.00043467464,0.00023837735,0.00025252494,0.00016398588,0.000121040364],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001330508,0.00011395013,0.00029642804,0.0000021224096,0.000093751834,0.000024182596,0.0006263939,0.000068811976,0.0011766824],"category_scores_gemma":[0.00054775336,0.00007528464,0.00012209563,0.0008162266,0.0005169711,0.0002725398,0.00015674862,0.0006180968,0.000024475894],"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":[0.0014093348,0.005225226,0.85307187,0.00012558477,0.00012466405,0.00006770034,0.0054192995,0.012432401,0.023756975,0.014917722,0.005451239,0.077998],"study_design_scores_gemma":[0.00060650037,0.0007778276,0.9756321,0.000036341058,0.0000173978,0.000009149917,0.00086133456,0.010566617,0.0015449453,0.00926745,0.0005839579,0.00009642426],"about_ca_topic_score_codex":0.00065381924,"about_ca_topic_score_gemma":0.00050189847,"teacher_disagreement_score":0.122560196,"about_ca_system_score_codex":0.00015264301,"about_ca_system_score_gemma":0.00012646812,"threshold_uncertainty_score":0.99973637},"labels":[],"label_agreement":null},{"id":"W2011328469","doi":"10.1080/02786820500444853","title":"Ice Nucleation Studies of Mineral Dust Particles with a New Continuous Flow Diffusion Chamber","year":2006,"lang":"en","type":"article","venue":"Aerosol Science and Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":93,"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":"Ice nucleus; Kaolinite; Aerosol; Relative humidity; Nucleation; Supersaturation; Particle (ecology); Mineralogy; Clear ice; Diffusion; Environmental chamber; Mineral dust; Cloud chamber; Chemistry; Materials science; Geology; Thermodynamics; Arctic ice pack; Physics; Climatology","score_opus":0.007519469419903982,"score_gpt":0.21641682395929263,"score_spread":0.20889735453938865,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2011328469","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":[0.99686193,0.00014097261,0.00024576232,0.0014791533,0.000031690575,0.00012573201,5.9277585e-7,0.00005891697,0.0010552689],"genre_scores_gemma":[0.99487704,0.000035290243,0.0044057183,0.00007147345,0.00001674119,0.000008106262,3.4117704e-7,0.000005639495,0.0005796327],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.998959,0.000005641669,0.00015466857,0.00030866932,0.00028954612,0.00028245628],"domain_scores_gemma":[0.9996203,0.000015456808,0.00009339043,0.00018234913,0.000039656556,0.00004885165],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014231607,0.00010591132,0.00016361366,0.000006830218,0.0002178766,0.00001726032,0.00014852974,0.00006304746,0.00006341547],"category_scores_gemma":[0.00004520187,0.000073303716,0.0000110010915,0.0009121588,0.002459221,0.00020330798,0.00021720208,0.000063508574,0.000017204475],"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":[0.000022603033,0.000103947736,0.38039678,0.0000053379067,0.0000064418764,0.000008343672,0.00039965924,0.00014667836,0.5813154,0.0013936207,0.0019086921,0.03429248],"study_design_scores_gemma":[0.0045772954,0.0032706459,0.5467881,0.00017815319,0.00014123705,0.0003258564,0.009694674,0.017538646,0.40190607,0.009541676,0.004601375,0.0014362902],"about_ca_topic_score_codex":0.00076399295,"about_ca_topic_score_gemma":0.0007090927,"teacher_disagreement_score":0.17940933,"about_ca_system_score_codex":0.000044113283,"about_ca_system_score_gemma":0.000024533972,"threshold_uncertainty_score":0.9061102},"labels":[],"label_agreement":null},{"id":"W2011637793","doi":"10.1016/j.jqsrt.2007.02.016","title":"Retrieval of aerosol physical and chemical properties from mid-infrared extinction spectra","year":2007,"lang":"en","type":"article","venue":"Journal of Quantitative Spectroscopy and Radiative Transfer","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":21,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Aerosol; Materials science; Extinction (optical mineralogy); Particle (ecology); SPHERES; Spectral line; Particle size; Scanning electron microscope; Scattering; Light scattering; Optics; Analytical Chemistry (journal); Chemistry; Physics; Composite material; Chromatography; Meteorology","score_opus":0.015521695795774575,"score_gpt":0.25983541159899487,"score_spread":0.24431371580322028,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2011637793","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":[0.96992874,0.00085728226,0.02808602,0.00012831151,0.000076400196,0.00012540622,0.000009215359,0.000006023856,0.0007825892],"genre_scores_gemma":[0.9903521,0.00034856974,0.009098439,0.000041536397,0.00011754819,5.3331195e-7,8.3240076e-7,0.000013207019,0.000027220596],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9987586,0.00006497484,0.0004106513,0.00020433222,0.0003400173,0.00022141995],"domain_scores_gemma":[0.99942994,0.0001799458,0.00014575224,0.00006643995,0.000034763452,0.00014316807],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031384546,0.00017940349,0.00040253083,0.000007672556,0.00007947504,0.000018403949,0.00009281326,0.000071615366,0.00021887927],"category_scores_gemma":[0.00004189281,0.00012810095,0.000104831684,0.0001762586,0.0007001766,0.0002986857,0.000019367044,0.00028303688,0.0000038037845],"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":[0.0016563666,0.00016534,0.00728049,0.00001112763,0.0000788093,0.000011241133,0.008061381,0.000020604508,0.982113,0.00023677725,0.000037788614,0.00032704143],"study_design_scores_gemma":[0.0011045089,0.0012847744,0.065204255,0.000043298816,0.00008129045,0.000014118736,0.0021697704,0.00025166813,0.9282843,0.0013481344,0.00005305215,0.00016081412],"about_ca_topic_score_codex":0.00004441571,"about_ca_topic_score_gemma":0.00001099123,"teacher_disagreement_score":0.057923768,"about_ca_system_score_codex":0.00007835582,"about_ca_system_score_gemma":0.000020451827,"threshold_uncertainty_score":0.5223805},"labels":[],"label_agreement":null},{"id":"W2012115288","doi":"10.1007/s00382-014-2055-2","title":"Synoptic weather conditions and aerosol episodes over Indo-Gangetic Plains, India","year":2014,"lang":"en","type":"article","venue":"Climate Dynamics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":62,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Indian Institute of Technology Kanpur; National Aeronautics and Space Administration","keywords":"Geopotential height; Climatology; Environmental science; Monsoon; Aerosol; Atmospheric circulation; AERONET; Teleconnection; Spatial distribution; Atmospheric sciences; Geography; Meteorology; Precipitation; Geology; El Niño Southern Oscillation","score_opus":0.0028135173385895663,"score_gpt":0.2015894756181513,"score_spread":0.19877595827956174,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012115288","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":[0.9799486,0.000025027228,0.0011896418,0.00011144915,0.000102122605,0.00014653955,0.00004715689,0.000064370426,0.018365124],"genre_scores_gemma":[0.9977278,0.00011387148,0.0011254167,0.00045100105,0.000028428658,0.00002235691,0.00004235118,0.000030260579,0.00045848195],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989595,0.00003826768,0.00017901832,0.0002946868,0.00016280863,0.00036574667],"domain_scores_gemma":[0.9994626,0.00007036214,0.00008069857,0.00025141906,0.0000046719747,0.00013022438],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00013875868,0.00017185313,0.00017056815,0.000002255586,0.00023763851,0.000058532692,0.00015402136,0.000105456835,0.001197062],"category_scores_gemma":[0.000027279877,0.00015560637,0.00004126018,0.00011107876,0.00035511787,0.00014446831,0.00020755865,0.00013111442,0.0004092959],"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":[0.000016674205,0.0001592388,0.9752959,0.000051108385,0.000027218319,0.000013923302,0.00058532716,0.0013283673,0.001825028,0.014327728,0.00084077375,0.005528727],"study_design_scores_gemma":[0.0007502825,0.00017110143,0.80856705,0.000040668896,0.00006198591,0.00002976644,0.00034196003,0.18633285,0.000057675385,0.0020054204,0.0011119557,0.00052929897],"about_ca_topic_score_codex":0.000059348244,"about_ca_topic_score_gemma":0.00017974082,"teacher_disagreement_score":0.18500447,"about_ca_system_score_codex":0.000119291835,"about_ca_system_score_gemma":0.000003956541,"threshold_uncertainty_score":0.999716},"labels":[],"label_agreement":null},{"id":"W2012247153","doi":"10.1029/2001jd900014","title":"An emerging ground‐based aerosol climatology: Aerosol optical depth from AERONET","year":2001,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2333,"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 de Sherbrooke","funders":"Division of Environmental Biology; NASA Headquarters; Centre National de la Recherche Scientifique; Centre National d’Etudes Spatiales; U.S. Department of Energy; National Science Foundation","keywords":"AERONET; Angstrom exponent; Aerosol; Environmental science; Middle latitudes; Climatology; Precipitable water; Atmospheric sciences; Optical depth; Angstrom; Forcing (mathematics); Meteorology; Precipitation; Geography; Geology","score_opus":0.037832192885681605,"score_gpt":0.3353371131240381,"score_spread":0.29750492023835645,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012247153","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":[0.98728865,0.00017985766,0.006263589,0.0010826555,0.00020789831,0.00022398817,0.0000038853996,0.000041537078,0.004707922],"genre_scores_gemma":[0.98108035,0.00011826158,0.017339638,0.00031022337,0.0007094519,0.000015826514,0.000006683008,0.000060021302,0.000359537],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99430573,0.000562898,0.0008287894,0.0006052255,0.0023670865,0.00133029],"domain_scores_gemma":[0.9970256,0.00079397234,0.00031854727,0.00067284016,0.00016819467,0.0010208333],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0010396922,0.00036068357,0.0006682792,0.000003850583,0.00049005914,0.00022599463,0.0013257365,0.00023857807,0.005183429],"category_scores_gemma":[0.00036596242,0.00028563634,0.00031773697,0.00078356644,0.0011120093,0.00080179336,0.000360932,0.001468727,0.0008961339],"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":[0.004226755,0.0065882266,0.61812675,0.000039483784,0.00035216348,0.003233212,0.0010785834,0.011344654,0.18542741,0.00094891235,0.025217349,0.14341652],"study_design_scores_gemma":[0.0077923825,0.010814809,0.8474521,0.0003246233,0.00022846616,0.00030694666,0.0043428536,0.081776105,0.018595658,0.009030949,0.017259413,0.0020756791],"about_ca_topic_score_codex":0.0024839041,"about_ca_topic_score_gemma":0.00090932864,"teacher_disagreement_score":0.22932538,"about_ca_system_score_codex":0.00035439446,"about_ca_system_score_gemma":0.00015614004,"threshold_uncertainty_score":0.9999596},"labels":[],"label_agreement":null},{"id":"W2014087504","doi":"10.1080/07055900.2011.581548","title":"An Aerosol Model of the Marine and Coastal Atmospheric Surface Layer","year":2011,"lang":"en","type":"article","venue":"ATMOSPHERE-OCEAN","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Russian Academy of Sciences","keywords":"Aerosol; Wind speed; Environmental science; Atmospheric sciences; Fetch; Extinction (optical mineralogy); Relative humidity; Meteorology; Physics; Geology; Optics; Oceanography","score_opus":0.015041952370582923,"score_gpt":0.206021705242715,"score_spread":0.19097975287213206,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2014087504","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":[0.9734673,0.00003354926,0.0012071145,0.00004650978,0.000100092424,0.0002659364,0.000009576489,0.0000635027,0.024806444],"genre_scores_gemma":[0.962567,0.00003300219,0.033376284,0.0002739396,0.000020911628,0.000002088466,0.0000022516656,0.000051052775,0.0036734783],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9982492,0.000070909715,0.000350794,0.00049367035,0.0003992403,0.00043619008],"domain_scores_gemma":[0.9987799,0.000021788592,0.00019684223,0.00076595985,0.000019611154,0.00021590959],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00019100842,0.00029939966,0.00028887385,6.0678445e-8,0.00020923224,0.000023774113,0.0006088282,0.00012977673,0.0037757014],"category_scores_gemma":[0.000012136929,0.00021336436,0.000104538085,0.00027111743,0.0005907839,0.00030812103,0.0007083455,0.00019553537,0.000051235675],"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":[0.000058469966,0.00023942025,0.9632146,0.0000106879825,0.000024653325,0.0000034179184,0.0015225569,0.025689684,0.004649447,0.00030543527,0.001303903,0.0029777184],"study_design_scores_gemma":[0.0014796073,0.0006066132,0.48588884,0.000029638657,0.00013511411,0.000033326793,0.0016447994,0.49394783,0.011779644,0.0027722865,0.00063486863,0.0010474414],"about_ca_topic_score_codex":0.0038718805,"about_ca_topic_score_gemma":0.00084808597,"teacher_disagreement_score":0.47732577,"about_ca_system_score_codex":0.000043950353,"about_ca_system_score_gemma":0.000028493187,"threshold_uncertainty_score":0.997135},"labels":[],"label_agreement":null},{"id":"W2014353994","doi":"10.5194/acp-15-1487-2015","title":"Corrigendum to &amp;quot;Size-resolved observations of refractory black carbon particles in cloud droplets at a marine boundary layer site&amp;quot; published in Atmos. Chem. Phys., 15, 1367–1383, 2015","year":2015,"lang":"en","type":"erratum","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada; University of British Columbia","funders":"","keywords":"Carbon black; Refractory (planetary science); Chemistry; Boundary layer; Layer (electronics); Carbon fibers; Physics; Materials science; Thermodynamics; Nanotechnology; Astrobiology; Organic chemistry","score_opus":0.023065492400358174,"score_gpt":0.2415983589925687,"score_spread":0.21853286659221052,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2014353994","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97321314,0.0005861611,0.000046005094,0.0003272732,0.0014193926,0.00065483816,0.00009644468,0.00007054399,0.023586204],"genre_scores_gemma":[0.34271586,0.0006459986,0.010281286,0.0007445936,0.0020627994,0.00032411164,0.0018902596,0.00032131973,0.6410138],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99553347,0.00010432207,0.001098616,0.0013555217,0.00090443133,0.0010036404],"domain_scores_gemma":[0.99720365,0.00010677637,0.00064253213,0.0013909541,0.000099731034,0.0005563635],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00045234538,0.00093045103,0.001259951,3.6567587e-7,0.00014739203,0.000118176315,0.0007313425,0.00079415634,0.0039422004],"category_scores_gemma":[0.0002239547,0.00095905276,0.00021441677,0.0013098669,0.0006720045,0.00038756317,0.0012292045,0.0012077858,0.00013263227],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037480632,0.0011172073,0.12151681,0.0005151833,0.00010531983,0.000030595333,0.004040881,0.0019143989,0.049713768,0.0000044623744,0.8163336,0.004332974],"study_design_scores_gemma":[0.0025594705,0.00016289682,0.06301647,0.00040936455,0.00017887859,0.000012343353,0.00047558226,0.008079865,0.0021410945,0.0011432415,0.9195462,0.0022745964],"about_ca_topic_score_codex":0.0051955306,"about_ca_topic_score_gemma":0.004367675,"teacher_disagreement_score":0.6304973,"about_ca_system_score_codex":0.0011424511,"about_ca_system_score_gemma":0.00034381627,"threshold_uncertainty_score":0.999286},"labels":[],"label_agreement":null},{"id":"W2014835144","doi":"10.1080/07055900.2011.557799","title":"Continuous 1064/532 nm Lidar Measurements (CORALNet-UBC) in Vancouver, British Columbia: Selected Results from a Year of Operation","year":2011,"lang":"en","type":"article","venue":"ATMOSPHERE-OCEAN","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada; University of British Columbia","funders":"","keywords":"Snow; Meteorology; Software deployment; Lidar; Environmental science; Air quality index; Aerosol; Range (aeronautics); Computer science; Remote sensing; Geography; Engineering; Aerospace engineering","score_opus":0.015589763000086881,"score_gpt":0.19303259472620193,"score_spread":0.17744283172611505,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2014835144","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":[0.9776319,0.0000706908,0.00012474296,0.000008746587,0.00028906594,0.00043305565,0.000052868156,0.0000726582,0.02131627],"genre_scores_gemma":[0.9865118,0.000031264415,0.008704124,0.00011576267,0.00004794698,0.0000072850694,0.00003601957,0.0000460916,0.004499672],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9975129,0.00012850807,0.0007012775,0.0006434196,0.00055679947,0.0004571193],"domain_scores_gemma":[0.9990286,0.000033652872,0.00028297483,0.00044451127,0.00005742031,0.00015283767],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00033395944,0.00020697963,0.0004095449,4.505778e-7,0.000118663134,0.000082031926,0.0004141063,0.00019241606,0.00543753],"category_scores_gemma":[0.00012244779,0.00028406802,0.0000787395,0.0004871136,0.00018160617,0.0003099857,0.00017193778,0.0002115958,0.00015770212],"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":[0.00015087653,0.00038905986,0.94685906,0.000005160145,0.000039159546,0.00003529027,0.0012047209,0.000216632,0.001153965,0.0000013525472,0.044396758,0.0055479375],"study_design_scores_gemma":[0.0033579692,0.00034923723,0.99078494,0.00008528233,0.000039647308,0.0000031765617,0.00079521345,0.00062516704,0.0009951179,0.00024425297,0.0022708455,0.0004491639],"about_ca_topic_score_codex":0.33251816,"about_ca_topic_score_gemma":0.39443845,"teacher_disagreement_score":0.06192029,"about_ca_system_score_codex":0.00020887062,"about_ca_system_score_gemma":0.000052666983,"threshold_uncertainty_score":0.99996114},"labels":[],"label_agreement":null},{"id":"W2015255530","doi":"10.1029/2003gl016917","title":"Satellite based retrieval of aerosol optical thickness: The effect of sun and satellite geometry","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":17,"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","funders":"","keywords":"Nadir; Remote sensing; Satellite; Aerosol; Pixel; Multispectral image; AERONET; Scattering; Near-infrared spectroscopy; Optics; Environmental science; Physics; Meteorology; Geology; Astronomy","score_opus":0.013584302830715662,"score_gpt":0.2737179429944709,"score_spread":0.26013364016375523,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015255530","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":[0.9960317,0.00017295808,0.0002491368,0.0011884503,0.00003885005,0.0003609092,0.0000029933578,0.00001023009,0.0019447806],"genre_scores_gemma":[0.9988576,0.0000642838,0.0006281671,0.00027224683,0.00003385527,0.00001136775,0.000001753218,0.000017871944,0.000112823254],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9967475,0.00069573673,0.00026977877,0.00038599604,0.0012956992,0.000605283],"domain_scores_gemma":[0.99717504,0.0020759376,0.00006849871,0.00047558217,0.000024408113,0.00018053807],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018418746,0.00017310173,0.00031555924,0.0000064393103,0.00015864435,0.00003121402,0.00036293012,0.000087890294,0.0002735616],"category_scores_gemma":[0.0007032015,0.00010773239,0.00012358998,0.0008586822,0.0023605835,0.00008953675,0.00021034885,0.0005326623,0.00010329713],"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":[0.0005512117,0.00013971301,0.07837368,0.00012928648,0.00004092738,0.000021417734,0.00025338275,0.00015939365,0.9054515,0.00080002344,0.00041362143,0.0136658875],"study_design_scores_gemma":[0.0017975928,0.0022120485,0.28853732,0.00009315018,0.000059595455,0.0000076092206,0.00015508053,0.0007365749,0.7017948,0.00048355327,0.0036814695,0.00044119728],"about_ca_topic_score_codex":0.00018012604,"about_ca_topic_score_gemma":0.0000039643933,"teacher_disagreement_score":0.21016365,"about_ca_system_score_codex":0.0000598462,"about_ca_system_score_gemma":0.000019423933,"threshold_uncertainty_score":0.86976683},"labels":[],"label_agreement":null},{"id":"W2015302898","doi":"10.1029/2008gl033733","title":"Occurrence of weak, sub‐micron, tropospheric aerosol events at high Arctic latitudes","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","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; Environment and Climate Change Canada; Université de Sherbrooke","funders":"Natural Sciences and Engineering Research Council of Canada; National Oceanic and Atmospheric Administration; Fonds Québécois de la Recherche sur la Nature et les Technologies; Canadian Foundation for Climate and Atmospheric Sciences; National Aeronautics and Space Administration","keywords":"Aerosol; Lidar; Environmental science; Troposphere; Arctic; Climatology; Atmospheric sciences; Observatory; Remote sensing; The arctic; Latitude; Meteorology; Geology; Geography; Oceanography; Astronomy; Physics","score_opus":0.023146818904169215,"score_gpt":0.2700265299739376,"score_spread":0.2468797110697684,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015302898","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":[0.9977578,0.000029426068,0.00020148022,0.0012149492,0.00008336746,0.00027657568,0.000020695818,0.000025849307,0.00038986513],"genre_scores_gemma":[0.99822766,0.00007090671,0.00060978404,0.00030879435,0.000068686975,0.00003908083,0.000017438006,0.000015065964,0.0006426055],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9967314,0.00020123029,0.00028129734,0.0005319988,0.0014047393,0.0008493369],"domain_scores_gemma":[0.99892235,0.00021844885,0.000087550485,0.00048436955,0.00003467931,0.00025259267],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00023129907,0.00020249236,0.00028212575,0.0000034807806,0.00040111662,0.000012060588,0.00059150235,0.000064283646,0.0020372714],"category_scores_gemma":[0.00010724667,0.00017538309,0.00013173529,0.00064423954,0.001493344,0.00018027559,0.0006830711,0.0004198782,0.002748542],"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":[0.00013931915,0.0004602198,0.24336596,0.00004157935,0.000035536625,0.000052356405,0.00038801567,0.0005755898,0.70864475,0.000077106546,0.044966795,0.0012527631],"study_design_scores_gemma":[0.0010547147,0.0005629524,0.95166147,0.000056117187,0.000017770011,0.000018435408,0.00007167417,0.0002768283,0.041977964,0.00036975296,0.0033660724,0.00056626333],"about_ca_topic_score_codex":0.0029400573,"about_ca_topic_score_gemma":0.00006098302,"teacher_disagreement_score":0.7082955,"about_ca_system_score_codex":0.00039810993,"about_ca_system_score_gemma":0.000029919602,"threshold_uncertainty_score":0.998875},"labels":[],"label_agreement":null},{"id":"W2015365010","doi":"10.1029/2010jd013905","title":"Investigation of the sulphate‐induced freezing inhibition effect from CloudSat and CALIPSO measurements","year":2010,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","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":"Université du Québec à Montréal","funders":"","keywords":"Lidar; Environmental science; Arctic; Depolarization ratio; Remote sensing; Correlation coefficient; Ice crystals; Proxy (statistics); Atmospheric sciences; The arctic; Meteorology; Geology; Mathematics; Physics; Statistics; Oceanography","score_opus":0.04028470549435704,"score_gpt":0.29169158534268447,"score_spread":0.25140687984832744,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015365010","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":[0.99884737,0.00004396929,0.000027524553,0.0004015484,0.00020100643,0.00017980147,0.000002108206,0.000004293078,0.00029241087],"genre_scores_gemma":[0.9989916,0.0000092283735,0.0006327277,0.000040318733,0.00024844048,0.0000036770841,5.43832e-7,0.000013676531,0.00005977732],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99727124,0.00041246272,0.00035284317,0.00018882567,0.0014875304,0.00028708033],"domain_scores_gemma":[0.99873,0.000428512,0.00026992988,0.0002447576,0.00010810477,0.00021872159],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012275178,0.00012748079,0.0002397934,0.0000012446047,0.00022215715,0.000052118885,0.00031587464,0.000099532925,0.0003299372],"category_scores_gemma":[0.00071529485,0.00007749132,0.0001144624,0.00035540242,0.00062252494,0.00025922008,0.00029287583,0.00085726584,0.000025535654],"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":[0.00007786439,0.000033707776,0.2337997,0.000007702174,0.000021154201,0.0000035680778,0.00022016416,0.000027334449,0.75982714,0.000030217594,0.00059677777,0.005354693],"study_design_scores_gemma":[0.000610543,0.0004750893,0.66234213,0.000081201826,0.00002215156,0.0000047275257,0.00009369635,0.00042056738,0.33081734,0.0049120565,0.00013426303,0.00008623131],"about_ca_topic_score_codex":0.0034509143,"about_ca_topic_score_gemma":0.00050116586,"teacher_disagreement_score":0.42900977,"about_ca_system_score_codex":0.00008325435,"about_ca_system_score_gemma":0.000047860627,"threshold_uncertainty_score":0.5216773},"labels":[],"label_agreement":null},{"id":"W2015621063","doi":"10.1117/12.519847","title":"Passive standoff detection of BG aerosol: method and field trial results","year":2004,"lang":"en","type":"article","venue":"Proceedings of SPIE, the International Society for Optical Engineering/Proceedings of SPIE","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Defence Research and Development Canada","funders":"","keywords":"Interferometry; Remote sensing; Depth sounding; Sensitivity (control systems); Atmospheric optics; Astronomical interferometer; Physics; Optics; Computer science; Geology","score_opus":0.00882535884021955,"score_gpt":0.23220031143378306,"score_spread":0.22337495259356352,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015621063","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":[0.99470514,0.000028460114,0.0011293627,0.0015437134,0.00016968198,0.0005166036,0.000022207112,0.00003324711,0.0018515752],"genre_scores_gemma":[0.89349055,0.00006640665,0.10598305,0.00007403031,0.00017604986,0.0000683437,0.000001569984,0.000026480338,0.00011352608],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9982008,1.9533514e-8,0.000609779,0.00034556355,0.00057887664,0.00026499198],"domain_scores_gemma":[0.99902666,0.00014905751,0.0004223643,0.000049000453,0.00025356992,0.00009935695],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005114366,0.00021896152,0.00033226356,0.000007468069,0.000077468736,0.00004245036,0.00043769597,0.00017797784,0.000018634948],"category_scores_gemma":[0.00060996367,0.00017554138,0.00033649773,0.00023506502,0.0002283004,0.0003366423,0.00019570853,0.00022376115,9.537912e-7],"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":[0.0034866321,0.00016590058,0.0001787267,0.0001499651,0.00021047312,1.0630378e-7,0.00046869286,0.00070842216,0.9371476,0.054476637,0.00062664464,0.0023802046],"study_design_scores_gemma":[0.01620219,0.002461751,0.0011491945,0.00020314517,0.00018181199,0.000015734648,0.0013777197,0.0068617966,0.9656439,0.0043131025,0.0011661116,0.00042355387],"about_ca_topic_score_codex":0.00008051287,"about_ca_topic_score_gemma":0.0000010740642,"teacher_disagreement_score":0.10485369,"about_ca_system_score_codex":0.00014938254,"about_ca_system_score_gemma":0.000014600249,"threshold_uncertainty_score":0.71583694},"labels":[],"label_agreement":null},{"id":"W2015638663","doi":"10.1117/12.922022","title":"Tilted pressure-tuned field-widened Michelson interferometer for high spectral resolution lidar","year":2012,"lang":"en","type":"article","venue":"Proceedings of SPIE, the International Society for Optical Engineering/Proceedings of SPIE","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"LightMachinery (Canada)","funders":"Langley Research Center; Oak Ridge Associated Universities","keywords":"Interferometry; Optics; Michelson interferometer; Backscatter (email); Remote sensing; Lidar; Interference (communication); Spectral resolution; Beam splitter; Astronomical interferometer; Laser; Field of view; Physics; Computer science; Geology; Spectral line; Telecommunications","score_opus":0.00906224588959904,"score_gpt":0.21713221998077112,"score_spread":0.2080699740911721,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015638663","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":[0.9945331,0.00009396877,0.0003951159,0.0019408816,0.00038087048,0.000669432,0.000028785194,0.00007029885,0.0018875417],"genre_scores_gemma":[0.87511337,0.000027210512,0.1232066,0.00018971642,0.00048823046,0.00017016848,0.0000071328777,0.000048195245,0.0007493487],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9979409,2.3248878e-8,0.00056288135,0.00036244176,0.00056021975,0.0005735577],"domain_scores_gemma":[0.99904233,0.00014642798,0.00032012552,0.00006868781,0.00026350195,0.00015892215],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0005636342,0.0003015278,0.0003564903,0.000010702314,0.000105226805,0.0000714953,0.0007746284,0.00022685879,0.00015620793],"category_scores_gemma":[0.00042807517,0.00024825285,0.00050261535,0.00023291905,0.00018468394,0.0006903222,0.0002448351,0.00023934476,0.0000064204155],"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":[0.0003198441,0.00023394925,0.0060470225,0.00024970088,0.00038420287,3.2031856e-8,0.00042058373,0.00011934306,0.87687016,0.10136954,0.013506641,0.00047900958],"study_design_scores_gemma":[0.0026789359,0.0015614468,0.028523965,0.00029926116,0.0005902043,0.000019066914,0.0012883978,0.024171231,0.9163564,0.0030796384,0.020431977,0.0009994799],"about_ca_topic_score_codex":0.00004452678,"about_ca_topic_score_gemma":4.0913048e-7,"teacher_disagreement_score":0.12281149,"about_ca_system_score_codex":0.00018168929,"about_ca_system_score_gemma":0.000009314028,"threshold_uncertainty_score":0.99999696},"labels":[],"label_agreement":null},{"id":"W2015645638","doi":"10.1115/mnhmt2009-18473","title":"Effects of the Fractal Prefactor on the Optical Properties of Fractal Soot Aggregates","year":2009,"lang":"en","type":"article","venue":"ASME 2009 Second International Conference on Micro/Nanoscale Heat and Mass Transfer, Volume 2","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"","keywords":"Fractal dimension; Fractal; Scattering; Physics; Rayleigh scattering; Mie scattering; Fractal derivative; Light scattering; Mathematical analysis; Mathematics; Optics; Fractal analysis","score_opus":0.009752767997770256,"score_gpt":0.2034195883382676,"score_spread":0.19366682034049734,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015645638","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":[0.98369396,0.00016747868,0.00013814232,0.002513478,0.00020168365,0.00038708805,0.000037594527,0.000013069152,0.012847495],"genre_scores_gemma":[0.9962456,0.00014703507,0.00007066608,0.00067522266,0.00003782296,0.000015497217,0.0000032179942,0.000011636273,0.002793302],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9986436,0.00006357187,0.00032205266,0.00031393857,0.0004124497,0.00024443824],"domain_scores_gemma":[0.9995563,0.000072115894,0.00005258212,0.00020545397,0.00003653975,0.000077030636],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00009680033,0.00023385396,0.00024840704,0.0000056242834,0.00012139885,0.000043768978,0.0004373694,0.00012243504,0.0032079373],"category_scores_gemma":[0.000029008335,0.00013390832,0.00013962215,0.00007826535,0.000479497,0.0001540256,0.000044072513,0.00028437588,0.00004257454],"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":[0.00019258077,0.00031057632,0.0054280926,0.000023411141,0.0000388145,0.0000021300955,0.00036661592,0.000018198714,0.98537946,0.0027228382,0.00054193236,0.0049753617],"study_design_scores_gemma":[0.0007090073,0.000844338,0.16184877,0.00023193726,0.00003231091,0.000007152514,0.00014678665,0.0012472658,0.8314057,0.00082039635,0.002452652,0.00025367367],"about_ca_topic_score_codex":0.00007419963,"about_ca_topic_score_gemma":0.00003187161,"teacher_disagreement_score":0.15642068,"about_ca_system_score_codex":0.000042689837,"about_ca_system_score_gemma":0.000030361432,"threshold_uncertainty_score":0.99770325},"labels":[],"label_agreement":null},{"id":"W2015719189","doi":"10.1029/2003jd004248","title":"Transport of smoke from Canadian forest fires to the surface near Washington, D.C.: Injection height, entrainment, and optical properties","year":2004,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":288,"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":"Smoke; Plume; Environmental science; Entrainment (biomusicology); Atmospheric sciences; Pollutant; Meteorology; Planetary boundary layer; Air quality index; Turbulence; Geology; Geography; Physics; Chemistry","score_opus":0.021965575252064325,"score_gpt":0.2584951675133277,"score_spread":0.23652959226126336,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015719189","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":[0.9953069,0.00022036587,0.00017935649,0.0031696605,0.00007022613,0.00023645279,0.000007624926,0.000004762194,0.00080464623],"genre_scores_gemma":[0.99750763,0.00007659354,0.002006896,0.00012651534,0.00014498956,0.000004175681,6.8494273e-7,0.000017492275,0.0001150452],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99767166,0.000099818986,0.00037449607,0.00022491925,0.0011049239,0.00052415696],"domain_scores_gemma":[0.9988829,0.00014277746,0.00009585177,0.0002162815,0.00008154186,0.00058068265],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005880007,0.00014870046,0.00026326257,0.0000014941427,0.00035151365,0.000080551865,0.00042593796,0.00007693591,0.00036322046],"category_scores_gemma":[0.00018079112,0.00008938568,0.00010426219,0.00034496418,0.00074005517,0.00023619912,0.000114816336,0.00051765895,0.000040617615],"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":[0.0013230245,0.00094974204,0.7787304,0.000052575608,0.0003124368,0.00023911751,0.013822081,0.13484262,0.036512587,0.0015292017,0.0041962066,0.027490038],"study_design_scores_gemma":[0.000530223,0.0012969481,0.98396194,0.00010247839,0.000025428362,0.000013935731,0.0013627356,0.00074552326,0.0041651283,0.003041371,0.004598285,0.00015597875],"about_ca_topic_score_codex":0.3841555,"about_ca_topic_score_gemma":0.14989343,"teacher_disagreement_score":0.23426208,"about_ca_system_score_codex":0.00031103464,"about_ca_system_score_gemma":0.00026648503,"threshold_uncertainty_score":0.86561877},"labels":[],"label_agreement":null},{"id":"W2015756862","doi":"10.1016/j.jastp.2015.01.005","title":"Lidar vertical profiling of water vapor and aerosols in the Great Lakes Region: A tool for understanding lower atmospheric dynamics","year":2015,"lang":"en","type":"article","venue":"Journal of Atmospheric and Solar-Terrestrial Physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":5,"is_retracted":false,"has_abstract":false,"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":"Lidar; Radiosonde; Water vapor; Mixing ratio; Aerosol; Environmental science; Remote sensing; Raman spectroscopy; Materials science; Laser; Atmospheric sciences; Meteorology; Optics; Geology; Physics","score_opus":0.03537477613400536,"score_gpt":0.24499142037417174,"score_spread":0.20961664424016638,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015756862","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":[0.8971154,0.00011731878,0.10164841,0.00031666426,0.00031298163,0.00033606353,0.0000015998006,0.0000058125825,0.00014572189],"genre_scores_gemma":[0.9891214,0.000080692094,0.010294716,0.00010992858,0.0003213934,0.000007983231,0.0000019406325,0.000023046021,0.000038952832],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99830276,0.00010406158,0.000596822,0.00022258757,0.0004251734,0.00034857137],"domain_scores_gemma":[0.99925745,0.00016740474,0.0002325282,0.0001770583,0.000026507993,0.00013905771],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006237353,0.0002279998,0.0004617974,3.1973883e-7,0.00012257174,0.00008931649,0.00023573279,0.000121405654,0.000012558726],"category_scores_gemma":[0.00007907413,0.00013652403,0.00014280214,0.00018168581,0.00034280238,0.0003956335,0.000111175,0.00026215278,0.0000011911425],"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":[0.010966774,0.0017813946,0.89729,0.00026491133,0.00049621915,0.0005240038,0.015596343,0.019168282,0.004024358,0.008849553,0.0028573007,0.038180873],"study_design_scores_gemma":[0.053184766,0.023938036,0.04887802,0.0012022861,0.002106635,0.001786756,0.049399506,0.5493593,0.0029954729,0.25759143,0.0050848103,0.0044729793],"about_ca_topic_score_codex":0.000046771012,"about_ca_topic_score_gemma":0.000017752589,"teacher_disagreement_score":0.848412,"about_ca_system_score_codex":0.00020367003,"about_ca_system_score_gemma":0.000057182075,"threshold_uncertainty_score":0.5567289},"labels":[],"label_agreement":null},{"id":"W2015872152","doi":"10.5194/acp-13-10005-2013","title":"Review and uncertainty assessment of size-resolved scavenging coefficient formulations for below-cloud snow scavenging of atmospheric aerosols","year":2013,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":67,"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":"Snow; Scavenging; Aerosol; Atmospheric sciences; Particle (ecology); Environmental science; Meteorology; Range (aeronautics); Particle size; Chemistry; Geography; Geology; Materials science","score_opus":0.007037660580992968,"score_gpt":0.2397285912332568,"score_spread":0.23269093065226382,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015872152","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":[0.92749846,0.0018890941,0.06732511,0.00012341313,0.000042466378,0.0011094401,0.000021921027,0.000032696516,0.0019574175],"genre_scores_gemma":[0.92271435,0.0008191823,0.07542161,0.00017421473,0.000053799737,0.00015640569,0.000018125393,0.000029439363,0.0006128715],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99851567,0.000021104535,0.00048894517,0.00039779462,0.00023188734,0.0003445905],"domain_scores_gemma":[0.99886394,0.0002671674,0.00031460074,0.00034733082,0.000058987884,0.00014798026],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001958367,0.00027898804,0.0005186598,2.1787903e-8,0.00019364132,0.000023800885,0.00015638302,0.00008654664,0.0012547431],"category_scores_gemma":[0.000055609973,0.00025692288,0.00013367546,0.00032648141,0.00029966238,0.00015438805,0.00015971174,0.00012376634,0.0000028196232],"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":[0.00007533814,0.0014879698,0.08650056,0.013654786,0.00055845967,0.0000027593628,0.0016646979,0.19867772,0.21855934,0.0010576453,0.00635152,0.4714092],"study_design_scores_gemma":[0.002267516,0.00029096444,0.026475899,0.0020097578,0.0006405874,0.0000156342,0.00055022974,0.95011073,0.011253717,0.0021354984,0.0030160763,0.0012333812],"about_ca_topic_score_codex":0.00019861008,"about_ca_topic_score_gemma":0.0000019567326,"teacher_disagreement_score":0.751433,"about_ca_system_score_codex":0.000081995124,"about_ca_system_score_gemma":0.00003292085,"threshold_uncertainty_score":0.9999883},"labels":[],"label_agreement":null},{"id":"W2016212393","doi":"10.1144/1467-7873/05-093","title":"Scanning lidar: a means of characterizing the Noranda-Hornesmelter plume","year":2006,"lang":"en","type":"article","venue":"Geochemistry Exploration Environment Analysis","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":12,"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":"Plume; Lidar; Geology; Remote sensing; Geography; Meteorology","score_opus":0.006895801160946103,"score_gpt":0.18830622401667255,"score_spread":0.18141042285572645,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2016212393","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":[0.9724902,0.000049878538,0.02223298,0.00076221925,0.000015250188,0.00014264089,0.000010596506,0.000024082794,0.004272161],"genre_scores_gemma":[0.9951466,0.00003365173,0.0008455291,0.00008472647,0.000079350946,0.00007493526,0.00014591884,0.000012738927,0.0035766053],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99851245,0.00003913339,0.00039483586,0.0003560427,0.00045800113,0.00023953324],"domain_scores_gemma":[0.99917525,0.000023189632,0.00028452807,0.00046073983,0.000005335883,0.000050954477],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00022449554,0.00018742861,0.00024191961,0.000004478209,0.00019830096,0.000037237292,0.00024580702,0.00007153886,0.006841258],"category_scores_gemma":[0.0000060532216,0.00014672839,0.00023072342,0.00043554665,0.00024003758,0.00024686218,0.00013452779,0.000101457015,0.0001399041],"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":[0.000021848618,0.00020021533,0.52900416,0.00001157667,0.0002926308,0.000004491863,0.0007378473,0.101845466,0.3651882,0.000018919884,0.0009295152,0.0017451239],"study_design_scores_gemma":[0.00096969376,0.000079254656,0.60391843,0.000031058204,0.0023024983,0.0000044221215,0.0018460696,0.05835511,0.28237158,0.0005773108,0.048418067,0.0011264599],"about_ca_topic_score_codex":0.0002618018,"about_ca_topic_score_gemma":0.000034993824,"teacher_disagreement_score":0.08281663,"about_ca_system_score_codex":0.000092076734,"about_ca_system_score_gemma":0.0000048029774,"threshold_uncertainty_score":0.9940666},"labels":[],"label_agreement":null},{"id":"W2016961897","doi":"10.1029/2009gl039429","title":"On the availability of uncoated mineral dust ice nuclei in cold cloud regions","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Dalhousie University","funders":"","keywords":"Ice nucleus; Atmospheric sciences; Environmental science; Mineral dust; Relative humidity; Clear ice; Saturation (graph theory); Liquid water; Nucleation; Sea ice growth processes; Mineral; Liquid water content; Homogeneous; Ice cloud; Geology; Arctic ice pack; Aerosol; Meteorology; Materials science; Climatology; Cloud computing; Sea ice thickness; Antarctic sea ice; Physics; Earth science; Sea ice; Thermodynamics","score_opus":0.02850881705845159,"score_gpt":0.2823977466553896,"score_spread":0.253888929596938,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2016961897","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":[0.9653592,0.0000028447896,0.000022330876,0.029113043,0.00003083432,0.00028785417,0.000002816712,0.000013816682,0.0051672533],"genre_scores_gemma":[0.9959894,0.0000031928146,0.000069184855,0.0031378234,0.000067423716,0.000015866099,0.0000013281116,0.00000772903,0.00070806046],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9977669,0.0003194149,0.00019748384,0.00033790994,0.00084396265,0.00053429685],"domain_scores_gemma":[0.99878377,0.00055437005,0.000039321214,0.0004921751,0.00001555602,0.00011483759],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006370637,0.00011382444,0.00015744811,0.000003562976,0.0001451442,0.000021721225,0.00047549035,0.00005076949,0.000644039],"category_scores_gemma":[0.00030464988,0.000076567434,0.000074250296,0.0008155302,0.00080924155,0.000071313945,0.00015095557,0.0005702151,0.00054845016],"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":[0.00024203453,0.0009888965,0.009250535,0.000007083885,0.000009737718,0.000040326144,0.00060910534,0.00089949474,0.6968347,0.016133875,0.27347437,0.0015098606],"study_design_scores_gemma":[0.0008677242,0.0009468292,0.96872276,0.000058817895,0.000006813011,0.0000010022065,0.00033491268,0.0025567536,0.007231667,0.009573334,0.009345254,0.00035411943],"about_ca_topic_score_codex":0.00208391,"about_ca_topic_score_gemma":0.0001007953,"teacher_disagreement_score":0.95947224,"about_ca_system_score_codex":0.00019994439,"about_ca_system_score_gemma":0.000015825219,"threshold_uncertainty_score":0.70517755},"labels":[],"label_agreement":null},{"id":"W2017704292","doi":"10.1117/12.689949","title":"Lidar and sunphotometry observations on the long-range transport of smoke and dust events","year":2006,"lang":"en","type":"article","venue":"Proceedings of SPIE, the International Society for Optical Engineering/Proceedings of SPIE","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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; Université de Sherbrooke; Environment and Climate Change Canada","funders":"","keywords":"Lidar; AERONET; Environmental science; Aerosol; Remote sensing; Zenith; Atmosphere (unit); Meteorology; Mineral dust; Storm; Range (aeronautics); Geography","score_opus":0.014236905670526658,"score_gpt":0.2153293502291881,"score_spread":0.20109244455866143,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2017704292","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":[0.99561644,0.00005909779,0.000018099672,0.0017940709,0.00005496257,0.00036912237,0.000031961405,0.000022088743,0.0020341403],"genre_scores_gemma":[0.9890467,0.00007205897,0.010365348,0.00010433068,0.00008153889,0.000054069842,0.0000030841634,0.000025300647,0.00024758486],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99855334,1.50479e-8,0.00041531125,0.00026499643,0.0005391746,0.00022715378],"domain_scores_gemma":[0.9993933,0.00010571772,0.0002265979,0.000045788394,0.000163267,0.00006537021],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003738976,0.00020022917,0.00023903351,0.000007654022,0.00009611438,0.000026212529,0.00042497873,0.00011358494,0.000044082448],"category_scores_gemma":[0.000105142106,0.0001403463,0.00021420074,0.0002739353,0.00037269562,0.00024850582,0.00010743269,0.00018151429,6.3839275e-7],"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":[0.000086275315,0.0002607349,0.567159,0.00028085482,0.00020238438,1.4081748e-7,0.00030282605,0.00018190271,0.20000869,0.22973213,0.0015712706,0.0002138083],"study_design_scores_gemma":[0.0007151764,0.00028458386,0.9701582,0.00016962246,0.00011989206,0.00000797948,0.000713598,0.0045678844,0.02052838,0.0016202665,0.0008474164,0.00026695215],"about_ca_topic_score_codex":0.00010652712,"about_ca_topic_score_gemma":0.0000013053227,"teacher_disagreement_score":0.40299928,"about_ca_system_score_codex":0.00006749628,"about_ca_system_score_gemma":0.000006974564,"threshold_uncertainty_score":0.5723156},"labels":[],"label_agreement":null},{"id":"W2018247646","doi":"10.1117/12.693479","title":"A spaceborne microwave radar system for looking inside clouds","year":2006,"lang":"en","type":"article","venue":"Proceedings of SPIE, the International Society for Optical Engineering/Proceedings of SPIE","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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":"Cloud computing; Remote sensing; Meteorology; Environmental science; Radar; Pathfinder; Jet propulsion; Space-based radar; Computer science; Aerospace engineering; Radar imaging; Geology; Radar engineering details; Geography; Engineering","score_opus":0.006591814479698353,"score_gpt":0.19982947389442007,"score_spread":0.1932376594147217,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2018247646","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":[0.98691666,0.00007638886,0.000563713,0.001065126,0.00025352297,0.00080078014,0.00003801254,0.00010468926,0.010181111],"genre_scores_gemma":[0.77358043,0.00001663551,0.22505529,0.00008269269,0.00049500813,0.00018682356,0.000007889946,0.000071119975,0.00050411443],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99761456,1.4209031e-8,0.0006997191,0.00048367985,0.000674433,0.00052758836],"domain_scores_gemma":[0.9988728,0.0001216275,0.0004510111,0.00006973873,0.0003689101,0.00011588695],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00060535676,0.00035691782,0.0004379752,0.000009571097,0.00014872839,0.00010635038,0.00083659036,0.00020738134,0.000025014544],"category_scores_gemma":[0.0001669005,0.00029807343,0.0007038301,0.0002939048,0.00030833506,0.00037771667,0.000253521,0.00022393717,0.000005230083],"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":[0.00009002541,0.000095276984,0.0016302805,0.0003634541,0.0001761571,1.3578362e-7,0.00012188184,0.0002893882,0.6643862,0.3247408,0.007840525,0.00026585188],"study_design_scores_gemma":[0.005663209,0.0010733228,0.010007495,0.0010787932,0.000791992,0.00010354725,0.006596819,0.057534438,0.86656755,0.009065586,0.039600834,0.0019164189],"about_ca_topic_score_codex":0.00008585004,"about_ca_topic_score_gemma":0.0000013954259,"teacher_disagreement_score":0.31567523,"about_ca_system_score_codex":0.00043364125,"about_ca_system_score_gemma":0.000018808725,"threshold_uncertainty_score":0.99994713},"labels":[],"label_agreement":null},{"id":"W2018564725","doi":"10.1109/aero.2008.4526260","title":"The CloudSat Mission and the A-Train: A Revolutionary Approach to Observing Earth's Atmosphere","year":2008,"lang":"en","type":"article","venue":"Proceedings - IEEE Aerospace Conference","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":12,"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":"Canadian Space Agency; U.S. Air Force; California Institute of Technology; National Aeronautics and Space Administration","keywords":"Satellite; Remote sensing; Lidar; Constellation; Radar; Environmental science; Meteorology; Atmosphere (unit); Profiling (computer programming); Cloud computing; Satellite constellation; Computer science; Aerospace engineering; Geology; Geography; Engineering; Telecommunications; Physics","score_opus":0.022383981367608354,"score_gpt":0.2097406853633147,"score_spread":0.18735670399570634,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2018564725","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":[0.95074385,0.00073085335,0.001909108,0.006124529,0.00015473244,0.00078034383,0.000001630839,0.00010633562,0.03944862],"genre_scores_gemma":[0.982592,0.0010379979,0.0070465454,0.00080643076,0.00010975924,0.000091273665,7.101264e-7,0.000028013246,0.008287274],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99792165,0.000036059897,0.0002780314,0.0006179826,0.0005606441,0.0005856158],"domain_scores_gemma":[0.9990936,0.00012708342,0.00015784564,0.00027559616,0.000067767396,0.0002780866],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0005749461,0.00030716514,0.00027487206,7.184234e-7,0.0017881278,0.00012685476,0.0007199091,0.000113983275,0.0001323623],"category_scores_gemma":[0.00018319546,0.00017581652,0.00008273195,0.00041555235,0.0012128492,0.0002879382,0.000474689,0.00033960736,0.00012379717],"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":[0.0016698372,0.0005132682,0.4974742,0.00020753869,0.00016701117,0.000021997887,0.058887217,0.0022653514,0.047611453,0.06572922,0.3013822,0.024070699],"study_design_scores_gemma":[0.0054847347,0.00063268386,0.6224354,0.00037160242,0.00015368054,0.00085481897,0.01813804,0.105666615,0.003517947,0.006738841,0.23329887,0.0027067682],"about_ca_topic_score_codex":0.0002722314,"about_ca_topic_score_gemma":0.000028337025,"teacher_disagreement_score":0.12496123,"about_ca_system_score_codex":0.00007566665,"about_ca_system_score_gemma":0.000041548996,"threshold_uncertainty_score":0.9995114},"labels":[],"label_agreement":null},{"id":"W2018987657","doi":"10.1029/2000gl011581","title":"The lognormal distribution as a reference for reporting aerosol optical depth statistics; Empirical tests using multi‐year, multi‐site AERONET Sunphotometer data","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":209,"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 de Sherbrooke","funders":"National Aeronautics and Space Administration; National Science Foundation","keywords":"AERONET; Log-normal distribution; Aerosol; Statistics; Environmental science; Meteorology; Mathematics; Geography","score_opus":0.17986106485943712,"score_gpt":0.4230865685575935,"score_spread":0.2432255036981564,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2018987657","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":[0.94756263,0.000009082165,0.050186638,0.0010005006,0.000044184144,0.0006898035,0.00029090504,0.000041826846,0.00017440575],"genre_scores_gemma":[0.95143455,0.000016811138,0.046425667,0.00048510387,0.00016623562,0.000094113464,0.00050531287,0.000037049664,0.00083515514],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9954333,0.0002538292,0.0007070008,0.0009546303,0.0012438152,0.00140748],"domain_scores_gemma":[0.9971544,0.0011424591,0.00020326952,0.0010635509,0.00006041936,0.0003758607],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016443342,0.0002537109,0.00028115828,0.0000033877975,0.0010566105,0.0002751308,0.00095427694,0.0001158929,0.000406186],"category_scores_gemma":[0.0023502836,0.00018477738,0.000081678765,0.00042534663,0.0012267795,0.00034620406,0.0009325513,0.0007605469,0.0007391695],"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":[0.0026802071,0.0028103928,0.25299737,0.0001288009,0.00025515398,0.0008821045,0.0011022801,0.00442446,0.34414288,0.00040344347,0.16580997,0.22436294],"study_design_scores_gemma":[0.002217579,0.0006255647,0.58453417,0.00006419123,0.00007075552,0.00005663795,0.00021228431,0.38315138,0.0020625559,0.0001886931,0.025877789,0.0009383881],"about_ca_topic_score_codex":0.0022362438,"about_ca_topic_score_gemma":0.00047428094,"teacher_disagreement_score":0.3787269,"about_ca_system_score_codex":0.0003121336,"about_ca_system_score_gemma":0.00007446567,"threshold_uncertainty_score":0.9500775},"labels":[],"label_agreement":null},{"id":"W2019723114","doi":"10.1029/2008jd010639","title":"Ice nucleation on mineral dust particles: Onset conditions, nucleation rates and contact angles","year":2008,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":139,"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 de Montréal; Université du Québec à Montréal; University of British Columbia","funders":"","keywords":"Ice nucleus; Nucleation; Muscovite; Kaolinite; Mineralogy; Amorphous ice; Calcite; Quartz; Ice crystals; Contact angle; Relative humidity; Sea ice growth processes; Saturation (graph theory); Classical nucleation theory; Materials science; Geology; Chemistry; Crystallography; Thermodynamics; Meteorology; Amorphous solid; Composite material; Arctic ice pack; Physics","score_opus":0.03271051954182279,"score_gpt":0.31130594409824874,"score_spread":0.27859542455642594,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2019723114","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":[0.997288,0.00007628418,0.000058552552,0.0008734138,0.00004719098,0.00014050437,0.0000051468205,0.000012407837,0.0014985318],"genre_scores_gemma":[0.9978209,0.0002003837,0.00082968915,0.00017234997,0.00019376529,0.000005816901,0.0000027241256,0.000018276349,0.0007560841],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.997915,0.00024666346,0.00033411034,0.00018726329,0.000944097,0.00037284984],"domain_scores_gemma":[0.9988043,0.00048185245,0.00017099203,0.00015794982,0.00010454003,0.00028037213],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00041261705,0.00014033863,0.00023155792,0.0000025926283,0.00045664047,0.00007088582,0.00020065301,0.000070673435,0.0012469984],"category_scores_gemma":[0.0002982855,0.00010713626,0.00008829531,0.0003149514,0.0005555923,0.00044365966,0.000094039955,0.0004213642,0.00030580116],"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":[0.002014037,0.0022851645,0.6947309,0.000037335198,0.00019718615,0.00045786338,0.003479622,0.0016235327,0.107904635,0.0036035348,0.15903406,0.02463215],"study_design_scores_gemma":[0.00078847806,0.0016628507,0.98741835,0.00005137134,0.000015118514,0.00006547993,0.0010889587,0.002572274,0.0014588769,0.0018171741,0.0029198625,0.00014121285],"about_ca_topic_score_codex":0.00054783636,"about_ca_topic_score_gemma":0.00005422018,"teacher_disagreement_score":0.29268748,"about_ca_system_score_codex":0.00016131617,"about_ca_system_score_gemma":0.00004869426,"threshold_uncertainty_score":0.999666},"labels":[],"label_agreement":null},{"id":"W2019906189","doi":"10.1175/2008jcli2186.1","title":"Boundary Layer, Cloud, and Drizzle Variability in the Southeast Pacific Stratocumulus Regime","year":2008,"lang":"en","type":"article","venue":"Journal of Climate","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Oceanic and Atmospheric Administration; Woods Hole Oceanographic Institution","keywords":"Drizzle; Environmental science; Boundary layer; Climatology; Cloud top; Cloud cover; Marine stratocumulus; Cloud fraction; Ceilometer; Meteorology; Liquid water path; Atmospheric sciences; Geology; Cloud computing; Geography; Aerosol; Precipitation","score_opus":0.012504982570369784,"score_gpt":0.23202560980560835,"score_spread":0.21952062723523857,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2019906189","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":[0.98174053,0.00010015447,0.00020699599,0.0006841067,0.00012388724,0.00008032424,0.0000030472067,0.0000046295804,0.017056312],"genre_scores_gemma":[0.9985309,0.0003997508,0.000760518,0.00012474298,0.00008471346,0.0000014721923,2.265355e-7,0.0000069346374,0.000090716894],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99880296,0.00017562145,0.00035222466,0.00012230413,0.00031728134,0.00022959533],"domain_scores_gemma":[0.99942756,0.00009506131,0.00021193996,0.00017732354,0.000008839854,0.000079307785],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014222562,0.0000994234,0.00017991764,0.0000017871762,0.0001896918,0.000036403122,0.00021018695,0.000049799535,0.00035495998],"category_scores_gemma":[0.000044252567,0.00006099174,0.000062616535,0.00013680835,0.00031467137,0.00018228224,0.00006938798,0.00026204035,0.000032805077],"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":[0.00017132613,0.00029214312,0.9842752,0.000015120906,0.000013165789,0.00027695863,0.0050699823,0.00027207003,0.0016330658,0.00035012435,0.002166151,0.0054646996],"study_design_scores_gemma":[0.0009536324,0.00030288284,0.9745537,0.000029683719,0.000024742285,0.0014505781,0.0036871359,0.00063772075,0.00007097323,0.003682438,0.014401638,0.00020485886],"about_ca_topic_score_codex":0.000033643704,"about_ca_topic_score_gemma":0.0000151158065,"teacher_disagreement_score":0.016965596,"about_ca_system_score_codex":0.00004787205,"about_ca_system_score_gemma":0.000023776198,"threshold_uncertainty_score":0.3886563},"labels":[],"label_agreement":null},{"id":"W2019974648","doi":"10.1364/ao.49.001630","title":"Inversion of water cloud lidar signals based on accumulated depolarization ratio","year":2010,"lang":"en","type":"article","venue":"Applied Optics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Royal Military College of Canada; Defence Research and Development Canada","funders":"","keywords":"Lidar; Molar absorptivity; Depolarization ratio; Optics; Depolarization; Inversion (geology); Scattering; Extinction (optical mineralogy); Remote sensing; Materials science; Geology; Physics","score_opus":0.007116151472130181,"score_gpt":0.20566877170541967,"score_spread":0.19855262023328948,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2019974648","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":[0.96945494,4.8556853e-7,0.016775902,0.000094052215,0.00012315164,0.00018030184,0.0000018143372,0.000030073788,0.013339248],"genre_scores_gemma":[0.9914697,0.0000011942492,0.007879013,0.00042575668,0.00003927672,0.00000536206,0.00002650293,0.00001534244,0.00013788296],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99921066,0.000010896284,0.0001770035,0.00018124093,0.00025057886,0.00016961503],"domain_scores_gemma":[0.99959123,0.000029990135,0.0000654366,0.00024082596,0.000008302268,0.000064224376],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00012063418,0.00010797698,0.00010674101,0.0000019000853,0.00008724255,0.0000156663,0.00014605366,0.00012470417,0.0015688107],"category_scores_gemma":[0.0000085295305,0.000080915226,0.000030467569,0.00011439566,0.00010045388,0.000044624005,0.00006971145,0.00014630576,0.00031469183],"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":[0.000035130506,0.0000885368,0.0051145074,0.0000043875402,0.000003900453,9.135503e-7,0.00015583131,0.047556184,0.94505423,0.00074692623,0.00019504603,0.0010443928],"study_design_scores_gemma":[0.0005276077,0.00009475824,0.0035678789,0.0000041033227,0.000020760497,3.131017e-7,0.000038449485,0.16319302,0.8308666,0.0005308624,0.0009646395,0.00019101918],"about_ca_topic_score_codex":0.000030041978,"about_ca_topic_score_gemma":0.0000092331165,"teacher_disagreement_score":0.115636826,"about_ca_system_score_codex":0.00002127169,"about_ca_system_score_gemma":0.0000074461614,"threshold_uncertainty_score":0.9993439},"labels":[],"label_agreement":null},{"id":"W2020616811","doi":"10.1029/2003gl019060","title":"Can aerosols spin down the water cycle in a warmer and moister world?","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":258,"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","funders":"","keywords":"Environmental science; Atmospheric sciences; Longwave; Radiative forcing; Aerosol; Climatology; Water cycle; Greenhouse gas; Climate model; Sensible heat; Atmosphere (unit); Forcing (mathematics); Liquid water path; Precipitation; Radiative transfer; Climate change; Meteorology; Physics; Geology","score_opus":0.015962085957645564,"score_gpt":0.27751859298728404,"score_spread":0.26155650702963845,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2020616811","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":[0.93159163,0.0000068461663,0.000029378883,0.066536136,0.000027512851,0.00025764157,0.0000012559582,0.000012256048,0.0015373694],"genre_scores_gemma":[0.994622,0.0000060584584,0.0001431657,0.0038793427,0.00008875514,0.00007009636,0.0000017153934,0.000014913518,0.0011739869],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99792063,0.00011512548,0.00014124309,0.00037719865,0.000640131,0.0008056811],"domain_scores_gemma":[0.9994526,0.000071391034,0.000012976727,0.0003059446,0.0000054559277,0.00015166333],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00037025262,0.00012932452,0.0001294118,0.0000044142666,0.00022833288,0.00008603161,0.00032370858,0.000031846677,0.0004320653],"category_scores_gemma":[0.000020762964,0.00006467703,0.00004570035,0.00035968932,0.00091098616,0.00011575225,0.00048449278,0.0004993714,0.0008231707],"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":[0.000213377,0.0006172082,0.059417754,0.00003670393,0.00003861203,0.00034477666,0.009691458,0.0062889527,0.8857402,0.0014044776,0.012440664,0.023765774],"study_design_scores_gemma":[0.0023894007,0.0002902748,0.939277,0.00006934537,0.000013510109,0.000010188237,0.00059855456,0.0006655788,0.021462759,0.017076366,0.017430583,0.0007164291],"about_ca_topic_score_codex":0.010824057,"about_ca_topic_score_gemma":0.0020529246,"teacher_disagreement_score":0.87985927,"about_ca_system_score_codex":0.0002193827,"about_ca_system_score_gemma":0.000010341945,"threshold_uncertainty_score":0.9999548},"labels":[],"label_agreement":null},{"id":"W2021831540","doi":"10.1029/2008jd010391","title":"Representing cloud overlap with an effective decorrelation length: An assessment using CloudSat and CALIPSO data","year":2008,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"","keywords":"Cloud fraction; Shortwave; Lidar; Radiative transfer; Longwave; Cloud height; Decorrelation; Environmental science; Cloud computing; Cloud top; Atmospheric radiative transfer codes; Satellite; Remote sensing; Physics; Meteorology; Mathematics; Statistics; Cloud cover; Geology; Computer science; Optics","score_opus":0.06542869909854435,"score_gpt":0.38325651544941963,"score_spread":0.3178278163508753,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2021831540","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":[0.99415016,0.00009582984,0.0047310777,0.00007073535,0.00009633213,0.00028099705,0.000004925461,0.000013759597,0.0005561763],"genre_scores_gemma":[0.97269124,0.00008716724,0.026425451,0.00002766758,0.00059589697,0.0000036436368,0.0000062666245,0.000033597113,0.00012906783],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9960237,0.00072434,0.00040983153,0.0005557558,0.0017138672,0.0005725195],"domain_scores_gemma":[0.99778444,0.0005292754,0.00030133326,0.00071782054,0.00013814596,0.0005289604],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015931589,0.00021079562,0.00036585485,0.0000026603325,0.000703976,0.00012107833,0.0006908937,0.000096587275,0.0002592952],"category_scores_gemma":[0.00027939864,0.0001522935,0.000058066475,0.00044552097,0.00079723203,0.0018089251,0.0007060308,0.0009197011,0.000018574035],"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":[0.0010745211,0.0012345936,0.92354506,0.000024643792,0.00014841474,0.00057424355,0.0011482004,0.012768235,0.008154776,0.00021269753,0.0012482707,0.04986632],"study_design_scores_gemma":[0.00094792293,0.0027417934,0.7918281,0.000064567685,0.000041581177,0.00026855292,0.0011873046,0.20100516,0.00012965097,0.00077027717,0.00076899386,0.00024606893],"about_ca_topic_score_codex":0.0035610772,"about_ca_topic_score_gemma":0.00027069956,"teacher_disagreement_score":0.18823694,"about_ca_system_score_codex":0.00028961746,"about_ca_system_score_gemma":0.00013314358,"threshold_uncertainty_score":0.62103486},"labels":[],"label_agreement":null},{"id":"W2022588621","doi":"10.1029/2009jf001444","title":"A review of snow and ice albedo and the development of a new physically based broadband albedo parameterization","year":2010,"lang":"en","type":"review","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":542,"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 Alberta","funders":"","keywords":"Snow; Albedo (alchemy); Radiative transfer; Environmental science; Atmospheric sciences; Cloud albedo; Solar zenith angle; Irradiance; Atmospheric radiative transfer codes; Cryosphere; Broadband; Atmosphere (unit); Range (aeronautics); Remote sensing; Sea ice; Meteorology; Geology; Climatology; Cloud cover; Physics; Optics; Materials science; Computer science; Cloud computing","score_opus":0.042228097130255285,"score_gpt":0.3468615853640045,"score_spread":0.30463348823374925,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2022588621","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0057167807,0.99185556,0.000852266,0.00024903633,0.000049176655,0.00085847965,0.000004517126,0.0000032682228,0.0004109056],"genre_scores_gemma":[0.0007513562,0.9862081,0.012419285,0.00008229658,0.00014452553,0.000022269423,0.0000033571205,0.000035677553,0.00033314523],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99583113,0.00064723456,0.0013575426,0.00034446933,0.0014249489,0.000394679],"domain_scores_gemma":[0.99572074,0.0020311198,0.0013251995,0.00040046824,0.00017593897,0.00034653378],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020229619,0.00034900446,0.0019655263,0.0000035699868,0.0001481813,0.000053842767,0.0007003596,0.000185044,0.00036729896],"category_scores_gemma":[0.0014493846,0.00019156632,0.00041971944,0.0006803997,0.0014501548,0.00015938195,0.00046746386,0.0011179335,0.0000151477925],"study_design_candidate":"design_other","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":[0.000111178066,0.00017385575,0.000035612557,0.010436483,0.00011046097,0.0000033602682,0.0001769589,0.000002626376,0.00006150685,0.00008182184,0.0013825818,0.98742354],"study_design_scores_gemma":[0.0014034617,0.0006991506,0.0009444139,0.06322615,0.0005478834,0.0000345534,0.00005534765,0.00029162996,0.00008699027,0.0008587643,0.931479,0.0003726659],"about_ca_topic_score_codex":0.00029429534,"about_ca_topic_score_gemma":0.000052491003,"teacher_disagreement_score":0.9870509,"about_ca_system_score_codex":0.00007891633,"about_ca_system_score_gemma":0.00074227556,"threshold_uncertainty_score":0.78118473},"labels":[],"label_agreement":null},{"id":"W2022839575","doi":"10.1175/2007jas2479.1","title":"Vertical Motions in Arctic Mixed-Phase Stratiform Clouds","year":2008,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":211,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Office of Science; U.S. Department of Energy","keywords":"Liquid water content; Context (archaeology); Arctic; Environmental science; Ice crystals; Atmospheric sciences; Ice nucleus; Cloud computing; Cloud physics; Ice cloud; Cloud top; Liquid water path; Meteorology; Precipitation; Geology; Physics; Nucleation; Oceanography","score_opus":0.020800757133850895,"score_gpt":0.2621530880823382,"score_spread":0.24135233094848732,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2022839575","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":[0.994949,0.0001088402,0.00031125537,0.0013156203,0.0005643977,0.000079546,3.1524638e-7,0.0000060701627,0.0026649819],"genre_scores_gemma":[0.9930855,0.00005656253,0.0061727767,0.00030569435,0.00007238287,0.0000018559823,3.5004156e-8,0.0000057713837,0.00029943927],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998187,0.00008350795,0.00046340344,0.00017097972,0.00076747173,0.00032762726],"domain_scores_gemma":[0.9994047,0.00006647645,0.0001883194,0.00019142614,0.000017799126,0.00013127395],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006139558,0.00012431764,0.00019554453,6.7256866e-7,0.00042988843,0.00003266605,0.0008770293,0.00004837458,0.0010511802],"category_scores_gemma":[0.00017021134,0.00007096631,0.00014798834,0.0010611513,0.0012140261,0.00039696603,0.00016441054,0.00024988825,0.00005258631],"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":[0.000045228873,0.0009029328,0.90332896,0.0000053417984,0.000019647558,0.00010775024,0.0013573972,0.07878423,0.0041257297,0.00046822583,0.0050705145,0.005784033],"study_design_scores_gemma":[0.0011177306,0.00077068986,0.9604788,0.000050462644,0.000026180607,0.0008007178,0.0010288295,0.030826816,0.0006117802,0.0025027045,0.0015506895,0.00023459966],"about_ca_topic_score_codex":0.00020871275,"about_ca_topic_score_gemma":0.00009378913,"teacher_disagreement_score":0.057149827,"about_ca_system_score_codex":0.00019195577,"about_ca_system_score_gemma":0.00010838106,"threshold_uncertainty_score":0.999862},"labels":[],"label_agreement":null},{"id":"W2025089392","doi":"10.1256/qj.05.04","title":"Bulk microphysics parametrization of ice fraction for application in climate models","year":2006,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Parametrization (atmospheric modeling); Ice crystals; Cloud physics; Atmospheric sciences; Environmental science; Ice cloud; Particle (ecology); Meteorology; Cloud computing; Geology; Physics; Radiative transfer","score_opus":0.007171193765475061,"score_gpt":0.2128471673366607,"score_spread":0.20567597357118564,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2025089392","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":[0.73305297,0.000030835712,0.266435,0.00015800478,0.000049147162,0.0001530064,0.0000030692822,0.0000035920687,0.0001143958],"genre_scores_gemma":[0.9841953,0.000008335291,0.01559526,0.00009666737,0.000068066,0.000009439924,0.0000013605044,0.000006066653,0.000019541985],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9989865,0.000064924316,0.00042522527,0.00012289421,0.00023091603,0.00016953204],"domain_scores_gemma":[0.9991479,0.0001339587,0.0005501656,0.000111859474,0.000029240613,0.000026892863],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046821384,0.00008984528,0.0001977933,0.0000011918083,0.00008263255,0.000012056217,0.00022281554,0.000112086665,0.000024017332],"category_scores_gemma":[0.000014699242,0.00005587902,0.0002771776,0.000205844,0.0001470866,0.00011399951,0.000024672889,0.00015927016,0.0000024257433],"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":[0.00026086177,0.0007365379,0.056019176,0.000027743728,0.000033481203,4.991333e-7,0.0003720761,0.8489179,0.056050062,0.0020821395,0.00062893995,0.03487058],"study_design_scores_gemma":[0.0017397876,0.001984639,0.18055321,0.000026149295,0.00012945259,0.00000478527,0.00066877156,0.7000861,0.0047460194,0.10916381,0.00060404337,0.00029320404],"about_ca_topic_score_codex":0.00022210546,"about_ca_topic_score_gemma":0.000013743008,"teacher_disagreement_score":0.25114232,"about_ca_system_score_codex":0.000114134644,"about_ca_system_score_gemma":0.0000059814997,"threshold_uncertainty_score":0.22786804},"labels":[],"label_agreement":null},{"id":"W2025545617","doi":"10.1016/j.jag.2012.07.017","title":"Methodology for estimating availability of cloud-free image composites: A case study for southern Canada","year":2012,"lang":"en","type":"article","venue":"International Journal of Applied Earth Observation and Geoinformation","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":8,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"Canadian Space Agency; National Aeronautics and Space Administration","keywords":"Cloud computing; Image (mathematics); Geography; Computer science; Artificial intelligence","score_opus":0.03516806495364217,"score_gpt":0.2785072218136306,"score_spread":0.24333915685998841,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2025545617","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":[0.8163624,0.000005159601,0.18267548,0.00013818206,0.0002972196,0.00034298364,0.000030103718,0.0000035214018,0.00014499639],"genre_scores_gemma":[0.73543423,6.5903237e-7,0.26423153,0.00017544106,0.00011154528,0.000012770826,0.000011127328,0.0000041074873,0.000018591572],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99893,0.000021163863,0.00059235306,0.00006190432,0.00027824027,0.00011633754],"domain_scores_gemma":[0.9987558,0.00026803865,0.0006694759,0.00008354232,0.0001615369,0.000061600316],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001020258,0.000082403065,0.00015686483,0.0000060170237,0.000079805555,0.000021943626,0.00014805047,0.00003198215,0.000079766614],"category_scores_gemma":[0.00018527295,0.00007099364,0.000042381096,0.000051283383,0.000040604806,0.00039776,0.000057009387,0.00005781725,0.0000013610379],"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":[0.003216114,0.0012173351,0.55087805,0.00032701553,0.0007178769,0.000018695291,0.0774564,0.07113597,0.014151266,0.002943338,0.0077291513,0.27020878],"study_design_scores_gemma":[0.018715698,0.0017178559,0.32877576,0.00008898601,0.00042538595,0.00123538,0.10600089,0.51243883,0.0078104283,0.005813334,0.015910175,0.0010673024],"about_ca_topic_score_codex":0.010960684,"about_ca_topic_score_gemma":0.012040916,"teacher_disagreement_score":0.44130284,"about_ca_system_score_codex":0.00006680663,"about_ca_system_score_gemma":0.000041692736,"threshold_uncertainty_score":0.99562544},"labels":[],"label_agreement":null},{"id":"W2026191966","doi":"10.1175/1520-0469(2004)061<2083:tmcwvp>2.0.co;2","title":"Testing Mixed-Phase Cloud Water Vapor Parameterizations with SHEBA/FIRE–ACE Observations","year":2004,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Langley Research Center; National Aeronautics and Space Administration; U.S. Department of Energy; Cure Cancer Australia Foundation; National Science Foundation","keywords":"Water vapor; Environmental science; Atmospheric sciences; Meteorology; Arctic; Liquid water content; Cloud computing; International Satellite Cloud Climatology Project; Vapour pressure of water; Cloud top; Climatology; Cloud cover; Geology; Physics","score_opus":0.030015991206565517,"score_gpt":0.2464376143619015,"score_spread":0.216421623155336,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2026191966","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":[0.9908001,0.000048442394,0.0044919276,0.0031958409,0.00055765634,0.00013797516,0.000001084356,0.000018886183,0.0007481165],"genre_scores_gemma":[0.8940312,0.000007148794,0.105022766,0.0005324819,0.000108222725,0.0000045665524,2.2767959e-7,0.000011662146,0.00028166597],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9981461,0.000060425737,0.00042973916,0.00022671116,0.00075626496,0.00038074705],"domain_scores_gemma":[0.9990587,0.00008874699,0.00041102685,0.0002530508,0.0000520157,0.00013643692],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005438602,0.00017025278,0.00019943104,5.779509e-7,0.0008869765,0.00013421498,0.0009488957,0.000042618492,0.00031999924],"category_scores_gemma":[0.00017108291,0.00007934204,0.00010191014,0.0012403465,0.0008648585,0.000567588,0.00020158489,0.00017857857,0.000033446],"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":[0.000028913786,0.00035725918,0.11811312,0.000004459167,0.00003105761,0.000025098245,0.0010399884,0.8411693,0.034755643,0.00016704347,0.0010343351,0.0032737777],"study_design_scores_gemma":[0.009701056,0.0093051875,0.73235655,0.0007588063,0.00060856855,0.003048757,0.007685474,0.1332003,0.040536143,0.023515886,0.036644973,0.00263829],"about_ca_topic_score_codex":0.00023570581,"about_ca_topic_score_gemma":0.000034966615,"teacher_disagreement_score":0.707969,"about_ca_system_score_codex":0.00015176061,"about_ca_system_score_gemma":0.000118023294,"threshold_uncertainty_score":0.68219954},"labels":[],"label_agreement":null},{"id":"W2028443463","doi":"10.5194/amtd-7-3645-2014","title":"Software and database structure to analyze the relationship between aerosol, clouds and precipitation: SAMAC","year":2014,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Universities Space Research Association","keywords":"Software; Cloud computing; Aerosol; Computer science; Precipitation; Filter (signal processing); Object (grammar); Database; Set (abstract data type); Remote sensing; Environmental science; Meteorology; Data mining; Operating system; Geography; Artificial intelligence; Programming language","score_opus":0.015945864563258468,"score_gpt":0.24860795511484818,"score_spread":0.2326620905515897,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2028443463","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":[0.9651336,0.000029936977,0.032398235,0.0012549805,0.00003475922,0.00016703189,0.000019440515,0.000032142372,0.00092989014],"genre_scores_gemma":[0.9739712,0.0000032311896,0.02431385,0.0006570685,0.000078509576,0.000006201382,0.00001598899,0.000009281807,0.00094470446],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991883,0.00006171206,0.00013273448,0.00027887672,0.00018083116,0.00015753019],"domain_scores_gemma":[0.99912894,0.0004157585,0.000039479724,0.00026831657,0.0000050133785,0.00014251449],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019765658,0.000112062036,0.00009931977,0.0000010234085,0.00030915072,0.000059057737,0.00013399616,0.00005116354,0.000745152],"category_scores_gemma":[0.00023442105,0.000071527764,0.000014332603,0.00017575391,0.00015513448,0.0001496049,0.0002302001,0.00011064092,0.000047226655],"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":[0.00000354793,0.0000026383552,0.9884637,0.0000037495236,0.0000036670338,1.3284244e-7,0.00033701572,0.00012529692,0.00009554337,0.00055306434,0.0022369516,0.0081746755],"study_design_scores_gemma":[0.00012645216,0.000046660618,0.99439365,0.0000049025157,0.000020377938,0.0000020645107,0.00011656275,0.00022675151,0.000054136293,0.0016793262,0.0032105765,0.00011856997],"about_ca_topic_score_codex":0.00017364701,"about_ca_topic_score_gemma":0.00029793332,"teacher_disagreement_score":0.008837582,"about_ca_system_score_codex":0.000019822988,"about_ca_system_score_gemma":0.0000034863003,"threshold_uncertainty_score":0.8158892},"labels":[],"label_agreement":null},{"id":"W2028583985","doi":"10.1016/j.atmosenv.2013.08.035","title":"Airborne investigation of the aerosols–cloud interactions in the vicinity and within a marine stratocumulus over the North Sea during EUCAARI (2008)","year":2013,"lang":"en","type":"article","venue":"Atmospheric Environment","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Agence Nationale de la Recherche","keywords":"Marine stratocumulus; Environmental science; Atmospheric sciences; Aerosol; Meteorology; Climatology; Geology; Geography","score_opus":0.006934491665717236,"score_gpt":0.18880977572539037,"score_spread":0.18187528405967313,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2028583985","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":[0.9968754,0.000042661726,0.000092455615,0.0013211659,0.00010709732,0.00079304405,0.0000022776308,0.000011935317,0.0007539506],"genre_scores_gemma":[0.9973711,0.000062347994,0.0011330609,0.00069755956,0.000047230053,0.00015364739,0.000002916316,0.00001814695,0.0005140309],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983397,0.0001994706,0.00039674205,0.00032776908,0.00044715716,0.00028913855],"domain_scores_gemma":[0.9989638,0.000097966935,0.00024359116,0.00061515777,0.0000035172402,0.000075974094],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002447417,0.00022391154,0.00016732284,3.5903926e-7,0.00031785795,0.000045095858,0.00044007177,0.0000458034,0.0022243122],"category_scores_gemma":[0.000017988436,0.000116603034,0.0000636634,0.0003102409,0.0006689254,0.00022456094,0.0005187565,0.00035741975,0.00009099308],"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":[0.000007614176,0.00007393105,0.9864697,0.000006578793,0.000013849463,0.0000014705515,0.0022060748,0.009544875,0.00051934976,0.000030938747,0.0004095969,0.00071605644],"study_design_scores_gemma":[0.00029360704,0.000046454075,0.99200857,0.000011506259,0.000024095456,0.000009033009,0.00091355725,0.005678784,0.00015434134,0.000322849,0.000395087,0.00014209637],"about_ca_topic_score_codex":0.0065271757,"about_ca_topic_score_gemma":0.002618372,"teacher_disagreement_score":0.005538924,"about_ca_system_score_codex":0.00017678703,"about_ca_system_score_gemma":0.000012892864,"threshold_uncertainty_score":0.9986878},"labels":[],"label_agreement":null},{"id":"W2028643991","doi":"10.1175/jcli4191.1","title":"The Sensitivity of the Radiation Budget in a Climate Simulation to Neglecting the Effect of Small Ice Particles","year":2007,"lang":"en","type":"article","venue":"Journal of Climate","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada; Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences; Cure Cancer Australia Foundation; Transport Canada","keywords":"Climatology; Cloud forcing; Atmospheric sciences; Environmental science; Radiative forcing; Cloud cover; Cirrus; Climate model; Radiative transfer; Longwave; Forcing (mathematics); Climate sensitivity; Precipitation; Earth's energy budget; Outgoing longwave radiation; Radiation; Climate change; Physics; Meteorology; Convection; Geology; Cloud computing","score_opus":0.0065226914857559205,"score_gpt":0.25451746344763587,"score_spread":0.24799477196187994,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2028643991","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":[0.9976973,0.000038493166,0.0012631895,0.0003980453,0.00010801279,0.00015783859,9.0561065e-7,0.0000020825635,0.00033413005],"genre_scores_gemma":[0.99963725,0.000048969487,0.00019559328,0.00007237676,0.000036150646,6.7719424e-7,5.221667e-8,0.0000054947204,0.0000034588852],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99871093,0.00030781399,0.00044185013,0.00006310528,0.00026275896,0.00021354218],"domain_scores_gemma":[0.9978793,0.0013701051,0.00056528073,0.00013428042,0.000017074373,0.000033911798],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0044809114,0.00006891482,0.0001432208,0.0000022937634,0.00015831247,0.000015474336,0.00013702273,0.00002898452,0.000010803452],"category_scores_gemma":[0.00042607402,0.00003108527,0.00008648984,0.00027015994,0.00008054115,0.00008038993,0.00009564922,0.0001336718,0.0000033006388],"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":[0.00027780715,0.000021010817,0.6258832,0.000010813426,0.0000075012613,0.000002534866,0.00088868104,0.28189293,0.039225355,0.000015381764,0.000008469834,0.0517663],"study_design_scores_gemma":[0.00031070854,0.00019817955,0.93574643,0.000043959655,0.00002392594,0.000008693506,0.00027060753,0.034558535,0.028618293,0.000047271165,0.00013142945,0.000041941355],"about_ca_topic_score_codex":0.00008918886,"about_ca_topic_score_gemma":0.00042220805,"teacher_disagreement_score":0.30986324,"about_ca_system_score_codex":0.000070331414,"about_ca_system_score_gemma":0.0000057657653,"threshold_uncertainty_score":0.15530035},"labels":[],"label_agreement":null},{"id":"W2028714153","doi":"10.1175/bams-d-14-00058.1","title":"CloudSat Observes a Labrador Sea Polar Low","year":2015,"lang":"en","type":"article","venue":"Bulletin of the American Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":6,"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":"Radar; Polar; Arctic; The arctic; Meteorology; Geology; Cloud top; Climatology; Environmental science; Satellite; Remote sensing; Geography; Oceanography; Computer science","score_opus":0.014941047928556703,"score_gpt":0.22098023094689978,"score_spread":0.20603918301834306,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2028714153","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":[0.98842186,0.00009372477,0.00020508238,0.008032746,0.00009333883,0.00016950603,0.000010548426,0.00005627503,0.002916905],"genre_scores_gemma":[0.97081923,0.000036157537,0.019717097,0.008046403,0.00006318343,0.000014021061,0.0000013691453,0.000015723199,0.0012868282],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99823445,0.0002519849,0.00025916996,0.00034795288,0.0005109599,0.00039550636],"domain_scores_gemma":[0.9988814,0.00012462014,0.00031264906,0.00045574416,0.000017029355,0.00020856719],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005762939,0.000194763,0.00036257048,3.4648207e-7,0.00013770361,0.000015201355,0.00079431554,0.00007834889,0.0026486586],"category_scores_gemma":[0.00022527292,0.00011266309,0.00041915866,0.00033133203,0.0019436552,0.000017914812,0.00078159553,0.00023929215,0.00037991125],"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":[0.00016322226,0.0004240773,0.5424375,0.000010308179,0.00009209158,0.0000045717834,0.00076385145,0.0014679995,0.0049945423,0.0001625393,0.4382238,0.011255523],"study_design_scores_gemma":[0.0007036609,0.00083842385,0.69650304,0.000009832486,0.000064830674,0.000011568189,0.0019272958,0.00060355425,0.0012779512,0.0010150358,0.29661152,0.00043328607],"about_ca_topic_score_codex":0.0033006798,"about_ca_topic_score_gemma":0.000011083814,"teacher_disagreement_score":0.1540656,"about_ca_system_score_codex":0.00010708295,"about_ca_system_score_gemma":0.00001588785,"threshold_uncertainty_score":0.99826306},"labels":[],"label_agreement":null},{"id":"W2028850213","doi":"10.1126/science.1075405","title":"Stronger Constraints on the Anthropogenic Indirect Aerosol Effect","year":2002,"lang":"en","type":"article","venue":"Science","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":202,"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","funders":"","keywords":"Aerosol; Environmental science; Atmospheric sciences; Meteorology; Geography; Geology","score_opus":0.013926937033503136,"score_gpt":0.22717036574683033,"score_spread":0.2132434287133272,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2028850213","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":[0.9289785,0.000032235654,0.000068335554,0.00058352394,0.00020812033,0.00019943275,0.0000016648855,0.000038222068,0.06988998],"genre_scores_gemma":[0.9983241,0.00001038515,0.0001473738,0.00047371487,0.000027050666,0.0000140506045,1.06474126e-7,0.000006618427,0.0009966299],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9983873,0.000052282492,0.00010619435,0.00038900448,0.0006273045,0.00043795852],"domain_scores_gemma":[0.9993421,0.00010744121,0.00005036676,0.00037951785,0.000004460967,0.000116130075],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0005720228,0.00012911847,0.000098241,0.0000016634051,0.0006414001,0.00006919802,0.00064170465,0.00003058568,0.03214612],"category_scores_gemma":[0.00010299124,0.000073935924,0.000048427493,0.00059830165,0.0044834134,0.00015818106,0.00017212468,0.00014302749,0.004351743],"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":[0.000029608946,0.00041237095,0.23764971,0.000007607137,0.000025387933,0.000052304094,0.0027389482,0.0014194326,0.21681057,0.0010819088,0.025307681,0.51446444],"study_design_scores_gemma":[0.0013636036,0.0023343796,0.66219133,0.000077252735,0.000050504645,0.000097723096,0.0009553063,0.01746309,0.29702824,0.00030373098,0.016563838,0.0015710008],"about_ca_topic_score_codex":0.000017131115,"about_ca_topic_score_gemma":0.0000073066817,"teacher_disagreement_score":0.51289344,"about_ca_system_score_codex":0.000113286726,"about_ca_system_score_gemma":0.000009445786,"threshold_uncertainty_score":0.9982258},"labels":[],"label_agreement":null},{"id":"W2028931556","doi":"10.1029/2006jd007596","title":"Evaluation of modeled cloud properties against aircraft observations for air quality applications","year":2007,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Environmental science; Meteorology; Liquid water content; Atmospheric model; Cloud height; Cloud computing; Atmospheric sciences; Cloud cover; Physics; Computer science","score_opus":0.14563004070212437,"score_gpt":0.38840325426104066,"score_spread":0.2427732135589163,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2028931556","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":[0.94353986,0.00019298067,0.053041827,0.00043526298,0.000056451598,0.00081106374,0.0000060469774,0.0000092532655,0.0019072798],"genre_scores_gemma":[0.9858946,0.00003058828,0.013142351,0.00005311189,0.00033602642,0.000085623324,0.0000025233276,0.00001828959,0.00043685426],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9954283,0.00032767392,0.00078120996,0.0002202996,0.002795437,0.00044706734],"domain_scores_gemma":[0.99722016,0.0005580001,0.00038755155,0.00031162656,0.0013044173,0.00021825121],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.008244095,0.00013041277,0.00030496862,0.0000026444552,0.00028025144,0.000023139844,0.00048428404,0.00008646095,0.00014533992],"category_scores_gemma":[0.0010917732,0.000098136625,0.00022114236,0.00059382844,0.00050573185,0.0003014403,0.00014098523,0.0003387488,0.0000231367],"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":[0.0016220082,0.0041485433,0.037162367,0.0002044551,0.0004122149,0.000004575412,0.0019073768,0.19139537,0.34314775,0.007919687,0.010610016,0.40146562],"study_design_scores_gemma":[0.004471321,0.0022220882,0.6837545,0.0001993384,0.000287538,0.0000055352707,0.0053421524,0.1774102,0.032895446,0.07562632,0.017103838,0.000681746],"about_ca_topic_score_codex":0.00050376647,"about_ca_topic_score_gemma":0.00021030715,"teacher_disagreement_score":0.6465921,"about_ca_system_score_codex":0.0004123947,"about_ca_system_score_gemma":0.00026861974,"threshold_uncertainty_score":0.40018955},"labels":[],"label_agreement":null},{"id":"W2028969959","doi":"10.1007/s00382-013-1884-8","title":"Diagnosis and testing of low-level cloud parameterizations for the NCEP/GFS model using satellite and ground-based measurements","year":2013,"lang":"en","type":"article","venue":"Climate Dynamics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":33,"is_retracted":false,"has_abstract":false,"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; Troposphere; Cloud fraction; Satellite; Shortwave; Cloud computing; Longwave; Cloud height; Cloud forcing; Meteorology; Liquid water path; Marine stratocumulus; Cloud albedo; Atmospheric sciences; Climatology; Water vapor; Cloud cover; Radiative transfer; Precipitation; Geology; Aerosol; Computer science; Geography; Physics","score_opus":0.08607609583261988,"score_gpt":0.26432557215725405,"score_spread":0.17824947632463417,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2028969959","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":[0.90108705,0.00006862515,0.09819566,0.00006014385,0.000041206218,0.00039375317,0.00005513115,0.000012523487,0.000085908105],"genre_scores_gemma":[0.9209756,0.00012207388,0.07866977,0.00011903961,0.000008019904,0.00007042879,0.000007829142,0.000016774762,0.000010447204],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99923897,0.000016254677,0.00019977822,0.000192713,0.00013295129,0.0002193555],"domain_scores_gemma":[0.9994372,0.00020905382,0.000119931996,0.00015599356,0.000024119352,0.000053674677],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016152933,0.00011584653,0.00012314995,0.0000015382619,0.00026521852,0.00005470496,0.00010351847,0.000045738172,0.000021862505],"category_scores_gemma":[0.00006937367,0.00008820906,0.000027731932,0.00010732036,0.00024974762,0.00012534217,0.00010595104,0.000042393443,0.000002086925],"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":[0.000009495728,0.00008239293,0.72021216,0.00010205329,0.000017076116,1.707865e-7,0.00020967386,0.22138931,0.007779001,0.00011365405,0.000008676911,0.05007632],"study_design_scores_gemma":[0.0001777021,0.000025704347,0.10219363,0.000030438223,0.0000333906,6.5293415e-7,0.000093143346,0.8964905,0.00009660414,0.00075558404,0.0000034863685,0.00009912872],"about_ca_topic_score_codex":0.00026501185,"about_ca_topic_score_gemma":0.000064777305,"teacher_disagreement_score":0.6751012,"about_ca_system_score_codex":0.000070453214,"about_ca_system_score_gemma":0.000008216622,"threshold_uncertainty_score":0.3597061},"labels":[],"label_agreement":null},{"id":"W2029401907","doi":"10.1175/jtech-d-13-00045.1","title":"Scanning ARM Cloud Radars. Part II: Data Quality Control and Processing","year":2013,"lang":"en","type":"article","venue":"Journal of Atmospheric and Oceanic Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"U.S. Department of Energy","keywords":"Depth sounding; Radar; Remote sensing; Doppler effect; Feature (linguistics); Wind speed; Computer science; Wind profiler; Doppler radar; Geology; Environmental science; Meteorology; Physics; Telecommunications","score_opus":0.011926691282241457,"score_gpt":0.24159293345164107,"score_spread":0.2296662421693996,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2029401907","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":[0.98736185,0.0034548722,0.005230208,0.0030040406,0.00016160186,0.00014133278,0.0000020017926,0.0000446959,0.00059941085],"genre_scores_gemma":[0.9762349,0.00039065667,0.022546336,0.00048750654,0.00009726679,0.0000020513341,4.849612e-7,0.000016952521,0.00022385598],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9984702,0.00004171183,0.00057516503,0.0003251456,0.00024858452,0.00033920468],"domain_scores_gemma":[0.9988484,0.00004780935,0.00057250937,0.0003467404,0.000033824297,0.00015075509],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00050681346,0.00018953715,0.00041120753,0.0000011712785,0.00028379308,0.000053442403,0.00051672594,0.00018489434,0.00046303796],"category_scores_gemma":[0.00012859909,0.00014445595,0.00003476434,0.00028262608,0.00059337914,0.000505935,0.0006052824,0.0003778216,0.000011096949],"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":[0.00006476934,0.00021773286,0.40669495,0.000035495865,0.000088825596,0.000036999387,0.00034928648,0.000054529537,0.0022838244,0.0005044729,0.016938845,0.5727303],"study_design_scores_gemma":[0.0064153085,0.0026010713,0.7815301,0.00030606787,0.000320682,0.0021917892,0.007635179,0.027428742,0.00022979657,0.015763635,0.15427451,0.0013031376],"about_ca_topic_score_codex":0.00007316149,"about_ca_topic_score_gemma":0.00000546949,"teacher_disagreement_score":0.57142717,"about_ca_system_score_codex":0.000056435765,"about_ca_system_score_gemma":0.00003843464,"threshold_uncertainty_score":0.58907425},"labels":[],"label_agreement":null},{"id":"W2029538616","doi":"10.1016/s1672-2515(07)60276-0","title":"A review of current knowledge concerning size-dependent aerosol removal","year":2006,"lang":"en","type":"review","venue":"China PARTICUOLOGY","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":50,"is_retracted":false,"has_abstract":false,"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":"Scavenging; Aerosol; Nucleation; Deposition (geology); Precipitation; Particle (ecology); Environmental science; Meteorology; Particle size; Atmospheric sciences; Chemistry; Mineralogy; Physics; Geology; Physical chemistry","score_opus":0.04647090997574763,"score_gpt":0.3453052472305104,"score_spread":0.29883433725476277,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2029538616","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00013922951,0.9877185,0.00016919246,0.000020454925,0.00066058047,0.0007577808,0.000016399717,0.000046820445,0.010471003],"genre_scores_gemma":[0.0001763921,0.99801904,0.00024085928,0.00006389511,0.00016906158,0.0001454572,0.000031566986,0.000053140906,0.0011006116],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9969302,0.00044050618,0.0011594319,0.0006745054,0.0002409337,0.00055445975],"domain_scores_gemma":[0.9981689,0.0002118826,0.00083235954,0.00062904024,0.000013719065,0.00014410443],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00046876838,0.00051061716,0.0021708736,0.0000024290543,0.00009303601,0.000009087577,0.0005833236,0.0002580779,0.0038655237],"category_scores_gemma":[0.00016522415,0.0003874441,0.0005540232,0.00033550747,0.0004825851,0.00005004361,0.00057070627,0.00044748903,0.0011359119],"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":[0.0000024759026,0.00019751591,0.00023192356,0.0430033,0.00004259507,0.000026816619,0.00005453229,0.000007104855,0.000002885259,0.00007710033,0.021501238,0.93485254],"study_design_scores_gemma":[0.00013569278,0.00007479306,0.00007083964,0.026749548,0.00052033004,0.00013120215,0.0000019405807,0.000008872803,0.0000027600981,0.00002626407,0.97191566,0.0003620779],"about_ca_topic_score_codex":0.00005702753,"about_ca_topic_score_gemma":0.000030612104,"teacher_disagreement_score":0.9504144,"about_ca_system_score_codex":0.00025488992,"about_ca_system_score_gemma":0.00011734839,"threshold_uncertainty_score":0.9998577},"labels":[],"label_agreement":null},{"id":"W2029646251","doi":"10.1175/jtech-d-11-00195.1","title":"Separating Cloud and Drizzle Radar Moments during Precipitation Onset Using Doppler Spectra","year":2013,"lang":"en","type":"article","venue":"Journal of Atmospheric and Oceanic Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"Biological and Environmental Research; U.S. Department of Energy","keywords":"Drizzle; Environmental science; Doppler effect; Cloud top; Radar; Meteorology; Cloud computing; Doppler radar; Remote sensing; Precipitation; Physics; Geography; Computer science","score_opus":0.0046936715411159645,"score_gpt":0.20973595858630756,"score_spread":0.2050422870451916,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2029646251","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":[0.9960268,0.0004587811,0.0026767438,0.00035430008,0.00013217604,0.00014224299,4.2755727e-7,0.000028731865,0.000179787],"genre_scores_gemma":[0.9378687,0.00020372748,0.061601494,0.00006735203,0.00005609682,0.0000018002563,1.696007e-7,0.00001612778,0.00018452336],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989018,0.000026146692,0.00039810094,0.00020330603,0.00019062134,0.00028002253],"domain_scores_gemma":[0.9993652,0.000024786665,0.0003744302,0.00012511757,0.000020358304,0.00009009066],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013229816,0.00016084396,0.00025940174,0.000001938562,0.00018813986,0.000040611485,0.00015123784,0.00014062111,0.0006077414],"category_scores_gemma":[0.000031352676,0.00013307875,0.0000396372,0.0002773388,0.00024051675,0.00032692493,0.00016540644,0.0002538871,0.000014651367],"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":[0.000066056295,0.000149512,0.8875016,0.00003499881,0.00011967733,0.000065686654,0.0010551478,0.0006492364,0.0903313,0.00019150633,0.002723161,0.017112147],"study_design_scores_gemma":[0.0028827316,0.001135376,0.9544578,0.0001314857,0.00015210998,0.004148387,0.005632979,0.016276024,0.004476276,0.0081369495,0.0018128006,0.0007570459],"about_ca_topic_score_codex":0.00007049845,"about_ca_topic_score_gemma":0.0000043246596,"teacher_disagreement_score":0.08585502,"about_ca_system_score_codex":0.0001221417,"about_ca_system_score_gemma":0.000015377185,"threshold_uncertainty_score":0.66543424},"labels":[],"label_agreement":null},{"id":"W2030341462","doi":"10.5194/acp-13-1293-2013","title":"Aerosol properties over Interior Alaska from lidar, DRUM Impactor sampler, and OPC-sonde measurements and their meteorological context during ARCTAS-A, April 2008","year":2013,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":11,"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":"National Aeronautics and Space Administration; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Aerosol; Environmental science; Haze; Troposphere; Context (archaeology); Lidar; Atmospheric sciences; Climatology; Arctic; Meteorology; Geography; Geology; Oceanography; Remote sensing","score_opus":0.014829034614975796,"score_gpt":0.19356627748539007,"score_spread":0.1787372428704143,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2030341462","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":[0.99774384,0.0011540226,0.0001896331,0.00009603061,0.000037155507,0.00022855814,0.000017402805,0.0000448341,0.00048854185],"genre_scores_gemma":[0.9963488,0.00022825217,0.0019470023,0.00024799383,0.00011220191,0.00004895884,0.000007835392,0.00002758727,0.001031389],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9985798,0.00003186949,0.00023779145,0.000548694,0.00020263638,0.00039919093],"domain_scores_gemma":[0.99931306,0.000042264077,0.00010741315,0.00025898693,0.000014355652,0.0002639089],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000058081627,0.00037279763,0.0003565644,3.1615645e-8,0.00024274169,0.00013718852,0.00016486266,0.00013583849,0.0039017128],"category_scores_gemma":[0.000020018942,0.00026741618,0.00006114861,0.000078216384,0.0005159105,0.00030015272,0.00033334608,0.00020492122,0.00002870391],"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":[0.00008432427,0.000093088456,0.23355503,0.000052649702,0.00010355361,0.0000022712989,0.0014390054,0.000019738925,0.70810974,5.15503e-7,0.00044390632,0.05609619],"study_design_scores_gemma":[0.0029648473,0.0002450881,0.6820192,0.00015935343,0.00010796784,0.000038118527,0.0025274784,0.007879672,0.2998329,0.00073497137,0.0019671791,0.0015232255],"about_ca_topic_score_codex":0.0011941326,"about_ca_topic_score_gemma":0.00001653118,"teacher_disagreement_score":0.44846416,"about_ca_system_score_codex":0.0000669297,"about_ca_system_score_gemma":0.000011047728,"threshold_uncertainty_score":0.9999778},"labels":[],"label_agreement":null},{"id":"W2030344470","doi":"10.3137/ao.460302","title":"Cloud type observations and trends in Canada, 1953–2003","year":2008,"lang":"en","type":"article","venue":"ATMOSPHERE-OCEAN","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Cirrus; Cloud cover; Environmental science; Meteorology; Cloud computing; Sky; Trend analysis; Atmospheric sciences; Climatology; Geography; Statistics; Computer science; Geology; Mathematics","score_opus":0.016540347396858408,"score_gpt":0.20305288464861093,"score_spread":0.1865125372517525,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2030344470","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":[0.9853152,0.00015792041,0.000018592287,0.00030533358,0.00024284016,0.00007563137,0.000006605018,0.000026244268,0.01385164],"genre_scores_gemma":[0.9869733,0.00009232625,0.0017959769,0.0007856566,0.000047269183,0.0000018575467,0.000007970512,0.000022146223,0.010273516],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987057,0.000030452373,0.00023613064,0.00032770092,0.000339202,0.0003608364],"domain_scores_gemma":[0.99947315,0.00002237002,0.000062162035,0.00026095443,0.000018189252,0.00016315423],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00008416252,0.00017260615,0.000184767,3.3586574e-7,0.00017908459,0.0000110677265,0.00018536556,0.00005985591,0.0035840685],"category_scores_gemma":[0.000031691732,0.00016342079,0.000021516173,0.00095861295,0.00014146566,0.00013645524,0.00011409841,0.00014467142,0.000043058848],"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":[0.000010177168,0.000026679083,0.88445234,0.0000013704584,0.0000045768847,0.00004508634,0.00025348627,0.0013169112,0.000021784228,0.0000749328,0.110289425,0.003503233],"study_design_scores_gemma":[0.00030528943,0.000053864485,0.9393033,0.0000050246786,0.0000066207886,0.00002272672,0.00024950886,0.0025817177,0.000023075094,0.000058576883,0.05716344,0.00022690369],"about_ca_topic_score_codex":0.7781536,"about_ca_topic_score_gemma":0.82991457,"teacher_disagreement_score":0.054850914,"about_ca_system_score_codex":0.0005172453,"about_ca_system_score_gemma":0.00017951333,"threshold_uncertainty_score":0.9973268},"labels":[],"label_agreement":null},{"id":"W2030379029","doi":"10.1364/ol.31.001809","title":"Simple relation between lidar multiple scattering and depolarization for water clouds","year":2006,"lang":"en","type":"article","venue":"Optics Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Defence Research and Development Canada","funders":"","keywords":"Lidar; Monte Carlo method; Scattering; Backscatter (email); Extinction (optical mineralogy); Mie scattering; Optics; Forward scatter; Physics; Remote sensing; Computational physics; Light scattering; Range (aeronautics); Atmospheric optics; Materials science; Geology; Statistics; Mathematics","score_opus":0.007300911237927832,"score_gpt":0.199213116210294,"score_spread":0.19191220497236616,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2030379029","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":[0.8835369,0.000003409614,0.11512777,0.000848211,0.000037722297,0.00014761322,0.000004295327,0.000024609548,0.00026947688],"genre_scores_gemma":[0.9806249,0.0000012840568,0.018688872,0.00036378793,0.00012517384,0.000010684174,0.00007997684,0.000017448912,0.0000878762],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993687,0.000009780478,0.0001386148,0.00017975674,0.00010039451,0.0002027318],"domain_scores_gemma":[0.99979067,0.000039154198,0.000035573197,0.00009770521,0.0000029064206,0.000034010714],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000079363876,0.00008764819,0.000076275835,0.0000012638429,0.00016129101,0.000042055293,0.00005645679,0.000048081616,0.000043509168],"category_scores_gemma":[0.0000070710166,0.00007442557,0.000024637427,0.00003947064,0.00006689914,0.00012900466,0.00006263373,0.000045649205,0.0000267043],"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":[0.0000037540165,0.000006992935,0.7036469,0.000004761195,0.0000036084637,5.620669e-7,0.00008352077,0.005864492,0.2892138,0.000025979156,0.0003110347,0.00083459466],"study_design_scores_gemma":[0.0005876555,0.00004619901,0.9401848,0.000006781061,0.000041916082,0.0000019793124,0.000024686091,0.022223681,0.03155443,0.0006520605,0.004383024,0.0002927967],"about_ca_topic_score_codex":0.00020215512,"about_ca_topic_score_gemma":0.00002279128,"teacher_disagreement_score":0.25765938,"about_ca_system_score_codex":0.00004521907,"about_ca_system_score_gemma":8.7658464e-7,"threshold_uncertainty_score":0.30349866},"labels":[],"label_agreement":null},{"id":"W2031132387","doi":"10.1175/1520-0469(2002)059<0620:aaopit>2.0.co;2","title":"Atmospheric Aerosol Optical Properties in the Persian Gulf","year":2002,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":200,"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 de Sherbrooke","funders":"NASA Headquarters; National Aeronautics and Space Administration","keywords":"Aerosol; AERONET; Angstrom exponent; Atmospheric sciences; Environmental science; Optical depth; Correlation coefficient; Sun photometer; Single-scattering albedo; Radiance; Sky; Angstrom; Precipitable water; Nephelometer; Water vapor; Meteorology; Physics; Chemistry; Light scattering; Optics; Scattering","score_opus":0.02412887356179168,"score_gpt":0.21431195669700837,"score_spread":0.19018308313521667,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2031132387","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":[0.971243,0.00078816817,0.00007526506,0.007734525,0.00048819016,0.0001839311,1.6332515e-7,0.000009024602,0.019477678],"genre_scores_gemma":[0.99006206,0.00011564831,0.006743153,0.0014336314,0.00013650274,0.0000063441016,1.1193128e-8,0.00001064965,0.0014919756],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9972205,0.0002035276,0.0005243583,0.00025623504,0.0013015228,0.0004938122],"domain_scores_gemma":[0.99904805,0.0001032478,0.0003727425,0.00035330016,0.000020071846,0.00010257486],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011718548,0.00020676469,0.0002579495,3.1976498e-7,0.0005631084,0.0001662944,0.0021707276,0.00006929104,0.0022126571],"category_scores_gemma":[0.00018184852,0.000090156165,0.00022810482,0.0014120322,0.0015673435,0.0005014658,0.00027140623,0.00038616615,0.00012844049],"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":[0.0000944743,0.0016851661,0.6281871,0.000025049385,0.00007543625,0.00016907824,0.02360635,0.22369751,0.009083375,0.00054858084,0.05580906,0.057018775],"study_design_scores_gemma":[0.0030022222,0.0034082786,0.54597205,0.00043745365,0.00025595428,0.0029979206,0.047066838,0.34172568,0.0016361221,0.0026625271,0.048930705,0.0019042674],"about_ca_topic_score_codex":0.00013043312,"about_ca_topic_score_gemma":0.000050135768,"teacher_disagreement_score":0.118028164,"about_ca_system_score_codex":0.00015244716,"about_ca_system_score_gemma":0.000034385113,"threshold_uncertainty_score":0.9986994},"labels":[],"label_agreement":null},{"id":"W2032539769","doi":"10.1029/2007jd008944","title":"Spatial and temporal variability of column‐integrated aerosol optical properties in the southern Arabian Gulf and United Arab Emirates in summer","year":2008,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":162,"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 de Sherbrooke","funders":"Utah Agricultural Experiment Station; Department of Water Resources; National Aeronautics and Space Administration","keywords":"AERONET; Angstrom exponent; Aerosol; Single-scattering albedo; Environmental science; Pollution; Mineral dust; Atmospheric sciences; Albedo (alchemy); Wavelength; Climatology; Meteorology; Geology; Geography; Physics","score_opus":0.03872870305718871,"score_gpt":0.2779723986638501,"score_spread":0.2392436956066614,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2032539769","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":[0.9986498,0.000097828764,0.00007657421,0.00046935814,0.000016136537,0.00027252795,0.0000035715564,0.000003101635,0.00041109876],"genre_scores_gemma":[0.9990318,0.000079366306,0.00060647447,0.000038878945,0.000049991868,0.000009683544,7.565233e-7,0.000011749514,0.00017134244],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9971402,0.00070542214,0.00055216317,0.00024462887,0.00093070074,0.00042683558],"domain_scores_gemma":[0.99885005,0.000543213,0.00014202918,0.00019737822,0.00010187001,0.00016545695],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016716877,0.00016102988,0.00038514775,0.000004339753,0.00013995565,0.000046901834,0.00033260265,0.00010252008,0.00019890943],"category_scores_gemma":[0.000736407,0.00009411055,0.00006287909,0.00070102507,0.0020053557,0.00018413209,0.00019074332,0.00085606996,0.00000920712],"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":[0.0005753339,0.000704423,0.9858945,0.000021429923,0.00001588072,0.00008749307,0.0026336245,0.0001864214,0.0068079988,0.000046781148,0.00020458635,0.0028215481],"study_design_scores_gemma":[0.0010838708,0.0010770417,0.9849109,0.0001025511,0.000008596353,0.00004450815,0.004335943,0.006110726,0.0008373908,0.0011526652,0.00018106683,0.00015475744],"about_ca_topic_score_codex":0.019321097,"about_ca_topic_score_gemma":0.0029205123,"teacher_disagreement_score":0.016400585,"about_ca_system_score_codex":0.00009493799,"about_ca_system_score_gemma":0.000108028464,"threshold_uncertainty_score":0.9872093},"labels":[],"label_agreement":null},{"id":"W2033834834","doi":"10.1175/2008bams2354.1","title":"The Fog Remote Sensing and Modeling Field Project","year":2008,"lang":"en","type":"article","venue":"Bulletin of the American Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":308,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"York University; Environment and Climate Change Canada","funders":"","keywords":"Nowcasting; Environmental science; Meteorology; Visibility; Dropsonde; Radiosonde; Weather Research and Forecasting Model; Precipitation; Aerosol; Remote sensing; Geography; Tropical cyclone","score_opus":0.019240129500030533,"score_gpt":0.2359030828932796,"score_spread":0.21666295339324906,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2033834834","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":[0.98276097,0.00008968369,0.007991687,0.006485616,0.000031683085,0.00014462176,5.020071e-7,0.00002321311,0.0024720118],"genre_scores_gemma":[0.95713747,0.0005263839,0.0377464,0.0040862844,0.000028844424,9.1741845e-7,8.791521e-8,0.0000071611507,0.0004664839],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9989872,0.00012996976,0.00017388671,0.00022390828,0.0002336528,0.00025138448],"domain_scores_gemma":[0.99925685,0.00029545935,0.00014289425,0.0002578017,0.0000074494365,0.000039557148],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034037782,0.00011191887,0.00018946594,2.1914067e-7,0.00058998115,0.000009726373,0.0002760906,0.000044976485,0.00010987053],"category_scores_gemma":[0.00016799814,0.00005369553,0.00019230372,0.00014346311,0.0013508172,0.0000070075243,0.0004498556,0.00019783193,0.000011166401],"study_design_candidate":"design_other","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":[0.00048337388,0.00013947864,0.055527553,0.000018349358,0.00023065768,0.000016686452,0.0032942058,0.010418831,0.0138523225,0.00013756531,0.21030977,0.7055712],"study_design_scores_gemma":[0.0011284058,0.0019289845,0.07988922,0.00003740811,0.0001605182,0.00027458186,0.0055477307,0.6123577,0.0020714186,0.004638536,0.29081574,0.0011498025],"about_ca_topic_score_codex":0.0034628464,"about_ca_topic_score_gemma":0.00000955942,"teacher_disagreement_score":0.7044214,"about_ca_system_score_codex":0.000026084861,"about_ca_system_score_gemma":0.0000069770554,"threshold_uncertainty_score":0.52348113},"labels":[],"label_agreement":null},{"id":"W2033865248","doi":"10.5194/angeo-29-1423-2011","title":"Influence of continental advection on aerosol characteristics over Bay of Bengal (BoB) in winter: results from W-ICARB cruise experiment","year":2011,"lang":"en","type":"article","venue":"Annales Geophysicae","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":24,"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","funders":"","keywords":"HYSPLIT; Aerosol; Angstrom exponent; Bay; BENGAL; Environmental science; Atmospheric sciences; Oceanography; Climatology; Advection; Geology; Meteorology; Geography; Physics","score_opus":0.01235384142926825,"score_gpt":0.22043399661903504,"score_spread":0.2080801551897668,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2033865248","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":[0.9968726,0.000014954143,0.000008932062,0.000017249933,0.00006288375,0.00015405331,0.00007763586,0.000013197529,0.002778462],"genre_scores_gemma":[0.99949443,0.00003113926,0.00018543914,0.000076854056,0.00003983232,0.000011975937,0.000019151143,0.000013113435,0.00012805965],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9987416,0.00004059399,0.00043524487,0.00031831447,0.00026525327,0.00019898123],"domain_scores_gemma":[0.99927825,0.0000446127,0.00028630896,0.00031359933,0.000014500943,0.000062745836],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000065266206,0.00016616941,0.00026982572,0.000003433303,0.00003251034,0.0000045080374,0.0002068853,0.00006054859,0.00028041753],"category_scores_gemma":[0.00002235853,0.00015210052,0.0000875188,0.00012915899,0.00023367551,0.00014568136,0.00010582005,0.00011915751,0.00008545417],"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":[0.0021153183,0.0024264362,0.43245274,0.000022904378,0.00006337,0.000024695548,0.015300821,0.0006825977,0.5422577,0.000111656904,0.0005065605,0.0040351725],"study_design_scores_gemma":[0.00059082906,0.00035134738,0.88905907,0.000063588835,0.000009488935,2.8433652e-7,0.0001890941,0.00017240281,0.10921869,0.000048444643,0.00015443574,0.00014231411],"about_ca_topic_score_codex":0.0036250632,"about_ca_topic_score_gemma":0.00018841964,"teacher_disagreement_score":0.45660633,"about_ca_system_score_codex":0.000046695866,"about_ca_system_score_gemma":0.000009344641,"threshold_uncertainty_score":0.6202479},"labels":[],"label_agreement":null},{"id":"W2034258903","doi":"10.1002/asl.91","title":"Cell detection at far ranges: supporting <i>T</i><sub>b</sub>—<i>Z</i> relationships","year":2005,"lang":"en","type":"article","venue":"Atmospheric Science Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"McGill University","keywords":"Radar; Satellite; Remote sensing; Microwave; Brightness temperature; Brightness; Reflectivity; Range (aeronautics); Meteorology; Representation (politics); Environmental science; Computer science; Geology; Geography; Physics; Telecommunications; Astronomy; Optics; Materials science","score_opus":0.00726154710562219,"score_gpt":0.19681344125760677,"score_spread":0.1895518941519846,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2034258903","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":[0.97984374,0.00006327495,0.011579067,0.0021123223,0.00031293926,0.00028413325,9.612496e-7,0.00018681768,0.005616762],"genre_scores_gemma":[0.97899544,0.000024257753,0.014023411,0.0063256607,0.00015341096,0.000038679216,0.0000016549807,0.000035634926,0.00040187576],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99661636,0.00007861108,0.00044982648,0.00088067265,0.0009805924,0.0009939618],"domain_scores_gemma":[0.9987331,0.000090923655,0.00029813324,0.0005391282,0.000015146794,0.0003235867],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001061057,0.00029828364,0.0002036192,0.0000014428471,0.0015142977,0.00011555265,0.00067078276,0.00009658262,0.0006816384],"category_scores_gemma":[0.000089166104,0.00028408715,0.00011741821,0.001612909,0.0011273125,0.001040552,0.00039408723,0.00033716005,0.002719133],"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":[0.000010138569,0.00003935811,0.051906873,0.0000030225535,0.000002417156,0.000006856347,0.00059818226,0.01290226,0.90519834,0.000003841146,0.004369913,0.02495883],"study_design_scores_gemma":[0.00086853,0.00012350164,0.16386038,0.000014152372,0.000049509228,0.000075604265,0.000645806,0.037095543,0.7518042,0.00004724212,0.044313163,0.0011023926],"about_ca_topic_score_codex":0.00011244463,"about_ca_topic_score_gemma":0.00019807245,"teacher_disagreement_score":0.15339413,"about_ca_system_score_codex":0.0010173712,"about_ca_system_score_gemma":0.000028806235,"threshold_uncertainty_score":0.99996114},"labels":[],"label_agreement":null},{"id":"W2036848236","doi":"10.1117/12.782364","title":"Assessing the radiative impact of aerosol smoke using MODTRAN5","year":2008,"lang":"en","type":"article","venue":"Proceedings of SPIE, the International Society for Optical Engineering/Proceedings of SPIE","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Air Force Research Laboratory; National Aeronautics and Space Administration; U.S. Department of Energy","keywords":"Aerosol; Smoke; Radiative transfer; Environmental science; Remote sensing; Atmospheric sciences; Meteorology; Computer science; Physics; Geology; Optics","score_opus":0.021289942678968127,"score_gpt":0.26550702162305817,"score_spread":0.24421707894409003,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2036848236","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":[0.99635375,0.00006167446,0.00016927108,0.00038991598,0.00010549303,0.0004138712,0.000019430921,0.000033710607,0.0024529113],"genre_scores_gemma":[0.95330644,0.000059773523,0.046268474,0.000051743915,0.00015892262,0.000033981585,0.000001767224,0.000042397565,0.00007647384],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99783206,2.9743639e-8,0.00062116556,0.00033456145,0.0008058663,0.0004063212],"domain_scores_gemma":[0.99880874,0.00013742733,0.0005187273,0.00007151359,0.00035150629,0.00011211169],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048616517,0.00030563437,0.0004024885,0.000008185128,0.0002008236,0.00006876081,0.00094100507,0.00015243335,0.000085713575],"category_scores_gemma":[0.00025572375,0.00020247384,0.00083424494,0.000405734,0.0007631152,0.0007914412,0.00023064224,0.00030007373,0.0000014829309],"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":[0.000069785856,0.00020987714,0.0342139,0.00012066416,0.00053744554,2.1994713e-7,0.0011523963,0.013100994,0.9307324,0.017877996,0.0016861424,0.00029812357],"study_design_scores_gemma":[0.0027211788,0.0010312535,0.16024692,0.0004654964,0.0004873829,0.0001254089,0.0054882667,0.5462666,0.280368,0.0012025245,0.0004005649,0.0011963794],"about_ca_topic_score_codex":0.00016557104,"about_ca_topic_score_gemma":1.8342043e-7,"teacher_disagreement_score":0.65036446,"about_ca_system_score_codex":0.00033955966,"about_ca_system_score_gemma":0.000042010182,"threshold_uncertainty_score":0.82566434},"labels":[],"label_agreement":null},{"id":"W2037327813","doi":"10.5194/acp-11-465-2011","title":"Californian forest fire plumes over Southwestern British Columbia: lidar, sunphotometry, and mountaintop chemistry observations","year":2011,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université de Sherbrooke; Environment and Climate Change Canada; University of British Columbia","funders":"University of British Columbia; Ministry of Environment; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Aerosol; Plume; Environmental science; Lidar; Atmospheric sciences; Smoke; Chemical transport model; Dominance (genetics); AERONET; Panache; Climatology; Meteorology; Geology; Geography; Remote sensing; Chemistry","score_opus":0.00954233249061289,"score_gpt":0.18572203115886912,"score_spread":0.17617969866825622,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2037327813","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":[0.9925474,0.00016186289,0.00030552733,0.000012423171,0.000023889166,0.00011474732,0.00004536165,0.00006239745,0.0067263963],"genre_scores_gemma":[0.98252904,0.00014337005,0.0044776546,0.00015234514,0.00010898348,0.00003332953,0.000034791326,0.000034015102,0.0124864485],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987138,0.000009047415,0.00022602161,0.00049137033,0.00020805415,0.00035170006],"domain_scores_gemma":[0.99932545,0.000026345377,0.000106746724,0.00029592044,0.000014499652,0.00023104627],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00005871915,0.00021306523,0.00023598982,9.155618e-9,0.00031232258,0.00018781135,0.0001937338,0.00016163153,0.008023217],"category_scores_gemma":[0.0000130674825,0.00029511334,0.000066871755,0.00022351631,0.00043126618,0.00019146997,0.0002160684,0.00019380623,0.000021053656],"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":[0.0000072063895,0.000108610104,0.9586143,0.00007666906,0.000028077897,0.000017785742,0.0003898153,0.000020862355,0.0025061327,0.000001142687,0.0006842336,0.03754517],"study_design_scores_gemma":[0.0005341124,0.000028331957,0.98432964,0.0000419221,0.000059257407,0.000054432712,0.00045959212,0.006390442,0.0006134806,0.00095323066,0.0059977314,0.00053780054],"about_ca_topic_score_codex":0.031225441,"about_ca_topic_score_gemma":0.0017760554,"teacher_disagreement_score":0.03700737,"about_ca_system_score_codex":0.00006768688,"about_ca_system_score_gemma":0.000017005856,"threshold_uncertainty_score":0.9999501},"labels":[],"label_agreement":null},{"id":"W2037961174","doi":"10.5194/amt-7-2531-2014","title":"Application of spectral analysis techniques to the intercomparison of aerosol data – Part 4: Synthesized analysis of multisensor satellite and ground-based AOD measurements using combined maximum covariance analysis","year":2014,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":35,"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":"Division of Mathematical Sciences; York University; National Aeronautics and Space Administration","keywords":"AERONET; Aerosol; Satellite; Environmental science; Data set; Remote sensing; Covariance; Principal component analysis; Meteorology; Climatology; Geography; Mathematics; Statistics; Geology","score_opus":0.050049138536499234,"score_gpt":0.27830799958057884,"score_spread":0.2282588610440796,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2037961174","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.2939553,0.000101092744,0.7046778,0.000090706075,0.00001808588,0.0008588297,0.000030031744,0.00008950713,0.00017860554],"genre_scores_gemma":[0.759367,0.000037088656,0.24036157,0.000077460965,0.000013368767,0.000077681165,0.000039028924,0.000020886557,0.0000059380955],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9954858,0.00045258985,0.0013221565,0.0008858695,0.0014846617,0.00036893185],"domain_scores_gemma":[0.99613565,0.00013020368,0.0012259961,0.0021561026,0.00022013343,0.00013191707],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.003376264,0.00039558817,0.0014685366,0.000025396836,0.00013317005,0.000036279507,0.0011323456,0.00013767647,0.00013897558],"category_scores_gemma":[0.00015973982,0.0003149236,0.000446675,0.0059770267,0.00036867298,0.00017170017,0.00035575655,0.00013176608,0.0000014603208],"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":[0.000311003,0.00069688214,0.74199426,0.00007587113,0.009310362,4.2223428e-7,0.0002358783,0.024580648,0.1827253,0.000038196104,0.00008733036,0.039943844],"study_design_scores_gemma":[0.00039490082,0.00040546656,0.22961938,0.00008808821,0.029466018,3.6105567e-7,0.00015198471,0.49778977,0.24084243,0.000065349865,0.00057765644,0.0005985692],"about_ca_topic_score_codex":0.00885826,"about_ca_topic_score_gemma":0.0038199069,"teacher_disagreement_score":0.5123749,"about_ca_system_score_codex":0.00027403183,"about_ca_system_score_gemma":0.00003064144,"threshold_uncertainty_score":0.99993026},"labels":[],"label_agreement":null},{"id":"W2038006265","doi":"10.1175/jtech1987.1","title":"SPARC: New Cloud, Snow, and Cloud Shadow Detection Scheme for Historical 1-km AVHHR Data over Canada","year":2007,"lang":"en","type":"article","venue":"Journal of Atmospheric and Oceanic Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":118,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Pixel; Advanced very-high-resolution radiometer; Remote sensing; Snow; Sky; Cloud computing; Satellite; Shadow (psychology); Image resolution; Meteorology; Environmental science; Radiometry; Polar orbit; Weather satellite; Computer science; Geology; Geography; Artificial intelligence; Astronomy; Physics","score_opus":0.009953319322166896,"score_gpt":0.2207516784945713,"score_spread":0.21079835917240441,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2038006265","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":[0.91502553,0.0024524666,0.07956459,0.0013790377,0.0011733782,0.00016377293,0.000004609494,0.000033452292,0.00020317385],"genre_scores_gemma":[0.95035416,0.0003746236,0.047361538,0.0003720233,0.000606213,9.309173e-7,0.0000013563775,0.000027945176,0.0009011866],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9984087,0.000012552099,0.00052083243,0.00035282294,0.00028605232,0.00041909202],"domain_scores_gemma":[0.9988658,0.00009989625,0.00040493024,0.0003509441,0.000024086034,0.0002543436],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043473952,0.00020484092,0.00036605287,0.0000018588185,0.00018308125,0.00001879396,0.00047258736,0.0002476942,0.0001976886],"category_scores_gemma":[0.00018035369,0.00017359493,0.00004543325,0.00034852885,0.00018065453,0.00019020328,0.00037590935,0.00037434167,0.000001914421],"study_design_candidate":"not_applicable","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":[0.00060077826,0.0001664671,0.18643203,0.000037976362,0.00017076933,0.00018393942,0.00014963537,0.000048720947,0.0069029042,0.0008723334,0.23921286,0.5652216],"study_design_scores_gemma":[0.0024499267,0.0012109583,0.082733825,0.00004038641,0.00015122697,0.0011367111,0.00073881354,0.0038325775,0.00087730505,0.0028134694,0.903458,0.0005568125],"about_ca_topic_score_codex":0.0253438,"about_ca_topic_score_gemma":0.04764012,"teacher_disagreement_score":0.6642451,"about_ca_system_score_codex":0.0007020249,"about_ca_system_score_gemma":0.00016305454,"threshold_uncertainty_score":0.9811465},"labels":[],"label_agreement":null},{"id":"W2038305315","doi":"10.1364/ao.44.005565","title":"Multiple-scattering-based lidar retrieval: method and results of cloud probings","year":2005,"lang":"en","type":"article","venue":"Applied Optics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Defence Research and Development Canada","funders":"","keywords":"Scattering; Lidar; Optics; Mie scattering; Forward scatter; Extinction (optical mineralogy); Remote sensing; Light scattering; Wavelength; Computational physics; Physics; Scattering theory; Computer science; Geology","score_opus":0.009440253763355017,"score_gpt":0.2322239649083276,"score_spread":0.22278371114497258,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2038305315","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":[0.9385678,0.000021225213,0.046395134,0.000581688,0.000048975144,0.000348482,0.000011459597,0.000060343886,0.01396485],"genre_scores_gemma":[0.74868745,0.00000761306,0.2507594,0.00028310766,0.00004788947,0.00000540735,0.0000037700568,0.000016483591,0.00018885806],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9988932,0.00001469873,0.00033532982,0.0003031833,0.00022585876,0.00022770476],"domain_scores_gemma":[0.99931705,0.00014209721,0.00016262199,0.00027846987,0.0000070011524,0.00009276589],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036750242,0.000142255,0.0001796987,0.0000016381503,0.00006814934,0.000015504145,0.0001617972,0.00008970995,0.00008839123],"category_scores_gemma":[0.00005656896,0.00012950596,0.00003313246,0.00016115028,0.00019642411,0.000040837193,0.00014678844,0.00011378666,0.00005270198],"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":[0.001764459,0.0006976376,0.01889066,0.00012083597,0.00007144715,0.000009262749,0.0040441817,0.14410481,0.72699606,0.0024182126,0.0040760185,0.096806385],"study_design_scores_gemma":[0.011066723,0.0007156518,0.032445252,0.00010051123,0.0001935447,0.000022144695,0.0006542791,0.22024114,0.6307596,0.0012810853,0.10075926,0.001760781],"about_ca_topic_score_codex":0.000038941012,"about_ca_topic_score_gemma":0.0000138149935,"teacher_disagreement_score":0.20436427,"about_ca_system_score_codex":0.00005066111,"about_ca_system_score_gemma":0.000009088337,"threshold_uncertainty_score":0.52811},"labels":[],"label_agreement":null},{"id":"W2039823909","doi":"10.1175/2011jcli3652.1","title":"Assessing Simulated Clouds and Radiative Fluxes Using Properties of Clouds Whose Tops are Exposed to Space","year":2011,"lang":"en","type":"article","venue":"Journal of Climate","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"","keywords":"Cloud fraction; Radiative transfer; Shortwave; Albedo (alchemy); Environmental science; Longwave; Cloud albedo; Cloud height; Atmospheric sciences; Sky; Climate model; Liquid water content; Radiative flux; Atmosphere (unit); Cloud top; Optical depth; Cloud cover; Meteorology; Cloud computing; Satellite; Geology; Physics; Climate change; Aerosol; Astronomy","score_opus":0.05233922391039807,"score_gpt":0.26952985158961124,"score_spread":0.21719062767921316,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2039823909","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":[0.99765915,0.00024256497,0.0005076591,0.00007671324,0.00014646878,0.0001071992,0.0000017492758,0.000008433636,0.0012500753],"genre_scores_gemma":[0.99098814,0.00010828001,0.008688416,0.00010564667,0.000053123633,4.0764738e-7,9.323653e-8,0.000018371511,0.00003752851],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987295,0.000080323574,0.00048092482,0.00014704498,0.00029561063,0.00026656524],"domain_scores_gemma":[0.9989781,0.000027588761,0.0006475205,0.00012976487,0.00004849262,0.00016853413],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038520893,0.00015542265,0.00036384052,0.000005837244,0.00012103996,0.000049312122,0.00016543885,0.00006719355,0.00026061185],"category_scores_gemma":[0.0000705281,0.000113450915,0.000078049685,0.0001887883,0.00015985622,0.00050284417,0.00016134525,0.00014492325,0.0000074684613],"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":[0.0005558766,0.00029205743,0.55293316,0.000090917245,0.000095825104,0.00009313422,0.016930202,0.01776456,0.40465638,0.00003241098,0.000096828946,0.0064586326],"study_design_scores_gemma":[0.0027809558,0.0016357225,0.69663686,0.0014588856,0.00031712002,0.00018140799,0.022672787,0.030473802,0.24177302,0.00041520633,0.0007043191,0.00094992534],"about_ca_topic_score_codex":0.00007944845,"about_ca_topic_score_gemma":0.0000071185677,"teacher_disagreement_score":0.16288337,"about_ca_system_score_codex":0.000092176175,"about_ca_system_score_gemma":0.00002146888,"threshold_uncertainty_score":0.46263942},"labels":[],"label_agreement":null},{"id":"W2039918738","doi":"10.1117/12.514453","title":"Ground-based lidar measurement of liquid water content and effective droplet diameter in water clouds: instrumentation, retrieval method, and results","year":2004,"lang":"en","type":"article","venue":"Proceedings of SPIE, the International Society for Optical Engineering/Proceedings of SPIE","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Defence Research and Development Canada","funders":"","keywords":"Lidar; Remote sensing; Liquid water content; Monte Carlo method; Scattering; Environmental science; Instrumentation (computer programming); Water content; Computation; Cloud computing; Computer science; Optics; Physics; Geology; Algorithm; Mathematics","score_opus":0.012876134535662777,"score_gpt":0.2213963239530715,"score_spread":0.2085201894174087,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2039918738","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":[0.9969238,0.000028003482,0.00027102375,0.0017723241,0.00007654455,0.0006690933,0.000014331358,0.00001875401,0.00022609139],"genre_scores_gemma":[0.9330676,0.000027651013,0.06664368,0.00009869114,0.00004730518,0.00006634026,0.000004186896,0.000026007458,0.000018550463],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99789965,7.8177834e-8,0.0006822291,0.00038925128,0.00070519873,0.00032357062],"domain_scores_gemma":[0.99927175,0.00006438917,0.00020216084,0.000044800036,0.0003208336,0.000096094336],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013332276,0.00024672144,0.0003523344,0.000013659369,0.000058062862,0.000047719695,0.00029539192,0.00012981184,0.0000139504355],"category_scores_gemma":[0.00024984012,0.00016091662,0.00019526118,0.00013597355,0.00034683585,0.00034003728,0.00019551723,0.00018661276,9.31754e-7],"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":[0.0007772767,0.00013744514,0.0023830691,0.00020867382,0.00013679425,1.4208265e-7,0.0011936713,0.0005451725,0.98782146,0.006505913,0.00003552706,0.00025486582],"study_design_scores_gemma":[0.0034476907,0.001065412,0.012032127,0.00023184225,0.00008957732,0.00000693866,0.0009087712,0.0026441435,0.9781893,0.0008886403,0.00022707181,0.00026849503],"about_ca_topic_score_codex":0.00012378185,"about_ca_topic_score_gemma":0.0000013739353,"teacher_disagreement_score":0.06637265,"about_ca_system_score_codex":0.00032314606,"about_ca_system_score_gemma":0.000009878339,"threshold_uncertainty_score":0.656199},"labels":[],"label_agreement":null},{"id":"W2040131415","doi":"10.1029/2007jd009636","title":"Ten years of multiwavelength Raman lidar observations of free‐tropospheric aerosol layers over central Europe: Geometrical properties and annual cycle","year":2008,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":129,"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":"European Commission","keywords":"Lidar; Troposphere; Aerosol; Environmental science; Tropopause; Pollution; Atmospheric sciences; Stratosphere; Planetary boundary layer; Mineral dust; Meteorology; Climatology; Geology; Remote sensing; Geography","score_opus":0.03785496050292805,"score_gpt":0.26834594179102683,"score_spread":0.23049098128809878,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2040131415","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":[0.99877316,0.000371027,0.0001285162,0.00017396777,0.00005779902,0.0001984306,0.000017347696,0.000008757208,0.0002709907],"genre_scores_gemma":[0.9923729,0.0005440468,0.006188233,0.000030732866,0.0001345245,0.0000036340823,7.3497023e-7,0.000030474048,0.0006947579],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9964142,0.00024606768,0.00067701,0.0002737594,0.0017650847,0.0006238736],"domain_scores_gemma":[0.9982778,0.00034746993,0.0003542548,0.00034579597,0.00028224866,0.00039242595],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043738325,0.00018633927,0.0005043092,0.000005020222,0.00018652852,0.000026149975,0.0006861657,0.00009971878,0.00042353052],"category_scores_gemma":[0.0012316972,0.00014430516,0.00018106679,0.0013154831,0.0015960111,0.00046192118,0.00057230354,0.0006262125,0.000018003617],"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":[0.0013679935,0.002911577,0.8146908,0.00012223246,0.00031647432,0.00030678182,0.004895874,0.0053047338,0.12959516,0.00021737322,0.014816417,0.025454538],"study_design_scores_gemma":[0.001059307,0.0013925346,0.99065614,0.000055355325,0.000021867267,0.000023866181,0.0007628953,0.0022691067,0.002367294,0.0001114408,0.0011159264,0.0001642894],"about_ca_topic_score_codex":0.0024056714,"about_ca_topic_score_gemma":0.00004270341,"teacher_disagreement_score":0.17596528,"about_ca_system_score_codex":0.00011985157,"about_ca_system_score_gemma":0.00015085589,"threshold_uncertainty_score":0.5884594},"labels":[],"label_agreement":null},{"id":"W2040631493","doi":"10.1029/2009jd013091","title":"Vertical velocity structure of nonprecipitating continental boundary layer stratocumulus clouds","year":2010,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Skewness; Atmospheric sciences; Cloud fraction; Flux (metallurgy); Environmental science; Marine stratocumulus; Boundary layer; Cloud top; Mixed layer; Planetary boundary layer; Climatology; Geology; Meteorology; Cloud computing; Turbulence; Cloud cover; Physics; Aerosol; Statistics; Chemistry","score_opus":0.01834823651920429,"score_gpt":0.3092387744900873,"score_spread":0.290890537970883,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2040631493","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":[0.9968478,0.000045884124,0.00024913455,0.000247263,0.00030872278,0.00014984029,0.000009781039,0.000008930877,0.0021326474],"genre_scores_gemma":[0.9899825,0.000009193255,0.009243779,0.000043678774,0.00047674924,0.0000016820537,0.0000010043786,0.000025378878,0.00021604585],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99633265,0.00021048085,0.00064812973,0.00027017723,0.0018890767,0.0006494708],"domain_scores_gemma":[0.998249,0.0005557528,0.00021347853,0.0003115271,0.0002229087,0.00044731345],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00072431256,0.00020237594,0.0004467619,0.000002047748,0.0002536319,0.00008934925,0.000724115,0.0001727538,0.0047640484],"category_scores_gemma":[0.0008494253,0.00015068303,0.00023984276,0.0004646806,0.0013609868,0.00035493617,0.00040969712,0.0018945809,0.00008075078],"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":[0.00051396346,0.0005405774,0.10654742,0.000026912838,0.000083502055,0.00008282962,0.00056647026,0.0001959245,0.8627678,0.0010031785,0.004624523,0.023046862],"study_design_scores_gemma":[0.0017491849,0.002098728,0.8867408,0.000076712415,0.00004595681,0.00008367312,0.0011135543,0.004704722,0.08371579,0.01310505,0.0061673108,0.00039852207],"about_ca_topic_score_codex":0.0007859205,"about_ca_topic_score_gemma":0.00038478986,"teacher_disagreement_score":0.7801934,"about_ca_system_score_codex":0.00010445184,"about_ca_system_score_gemma":0.00018232176,"threshold_uncertainty_score":0.9961457},"labels":[],"label_agreement":null},{"id":"W2041470284","doi":"10.1364/ao.47.004235","title":"Standoff determination of the particle size and concentration of small optical depth clouds based on double-scattering measurements: validation with calibrated target plates and limitations for daytime and nighttime measurements","year":2008,"lang":"en","type":"article","venue":"Applied Optics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Defence Research and Development Canada","funders":"","keywords":"Lidar; Optics; Daytime; Remote sensing; Scattering; Light scattering; Laser; Environmental science; Materials science; Physics; Geology; Atmospheric sciences","score_opus":0.05232142176082879,"score_gpt":0.22455812735362768,"score_spread":0.17223670559279888,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2041470284","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":[0.97762597,0.000008912153,0.020807663,0.000079258105,0.000011374907,0.00053732493,0.0000037990135,0.000008758555,0.00091695116],"genre_scores_gemma":[0.95517355,0.0000069519,0.04470911,0.000046584664,0.000004829867,0.000032600667,0.000005298975,0.000010094828,0.00001097165],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9992462,0.000018036682,0.00020065613,0.0001716687,0.00024230673,0.000121137076],"domain_scores_gemma":[0.9995482,0.00013901234,0.00012675158,0.000104534396,0.00003051404,0.000051017803],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016654114,0.00010133021,0.00012231863,0.000001122091,0.00013317546,0.000016381653,0.00004997552,0.000043065746,0.0000075487533],"category_scores_gemma":[0.00003294204,0.0000742748,0.000012073528,0.00009143773,0.0002567409,0.00007650863,0.000027238986,0.0000364551,3.0166316e-7],"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":[0.0010599017,0.00031052646,0.40467665,0.00008142403,0.00005033383,5.51555e-7,0.0016024199,0.02910858,0.55915385,0.0007813236,0.00001236077,0.0031620509],"study_design_scores_gemma":[0.004368627,0.00039509006,0.2292631,0.000035585676,0.00011187557,0.0000027980527,0.00015602606,0.12198772,0.64330226,0.00016387178,0.000012690424,0.00020035969],"about_ca_topic_score_codex":0.000009668466,"about_ca_topic_score_gemma":0.00002368994,"teacher_disagreement_score":0.17541355,"about_ca_system_score_codex":0.000030982646,"about_ca_system_score_gemma":0.00001853678,"threshold_uncertainty_score":0.30288386},"labels":[],"label_agreement":null},{"id":"W2042775027","doi":"10.5194/acp-12-1101-2012","title":"Statistical analysis of an LES shallow cumulus cloud ensemble using a cloud tracking algorithm","year":2012,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":93,"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":"Cloud computing; Cloud base; Liquid water content; Environmental science; Cloud height; Entrainment (biomusicology); Inversion (geology); Cloud top; Atmospheric sciences; Meteorology; Large eddy simulation; Geology; Cloud cover; Computer science; Physics; Turbulence","score_opus":0.015581221667765365,"score_gpt":0.2570239791910028,"score_spread":0.2414427575232374,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2042775027","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":[0.8306555,0.00011877243,0.16774827,0.0000032178912,0.00004721514,0.000048095804,0.00001982843,0.000021715092,0.001337362],"genre_scores_gemma":[0.8609243,0.00002042334,0.13845892,0.000028567541,0.0002761593,0.0000032749083,0.00002791695,0.000018988432,0.0002414581],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9987284,0.00003534823,0.0002603765,0.00031431028,0.0002728515,0.00038874446],"domain_scores_gemma":[0.9992681,0.00006434381,0.00013410462,0.0002837621,0.000013267795,0.00023640678],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001551909,0.00021733409,0.0003615698,3.771248e-8,0.00016525366,0.000025756692,0.00015150996,0.000108653214,0.0028704905],"category_scores_gemma":[0.000010510172,0.00021030055,0.000104944804,0.0004886962,0.00027305866,0.00022730093,0.000095381845,0.0001447802,0.0000074211794],"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":[0.000029077644,0.0005412735,0.27717406,0.00004932333,0.0003654227,0.0000073552833,0.0012916717,0.012672128,0.03948266,0.00010741785,0.000056069057,0.66822356],"study_design_scores_gemma":[0.00037566514,0.00005403073,0.10207633,0.00001486211,0.0011419798,0.000014541096,0.0006208882,0.88227224,0.011610693,0.00040744536,0.0008504177,0.0005609018],"about_ca_topic_score_codex":0.0007322299,"about_ca_topic_score_gemma":0.0000076237875,"teacher_disagreement_score":0.8696001,"about_ca_system_score_codex":0.00007228095,"about_ca_system_score_gemma":0.00001192321,"threshold_uncertainty_score":0.99804103},"labels":[],"label_agreement":null},{"id":"W2042989341","doi":"10.1109/ivelec.2009.5193406","title":"High power 94 GHz amplifier for EarthCARE mission Doppler radar","year":2009,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Japan Aerospace Exploration Agency; Canadian Space Agency","keywords":"Remote sensing; Radar; Doppler radar; Satellite; Aerospace; Payload (computing); Earth observation; Cloud computing; Aerospace engineering; Environmental science; Doppler effect; Computer science; Meteorology; Engineering; Geology; Geography; Physics","score_opus":0.009048026540124519,"score_gpt":0.2316020265344222,"score_spread":0.22255399999429767,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2042989341","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":[0.9375975,0.00004194461,0.015700867,0.0034906203,0.00019253934,0.0003555323,0.0000063054317,0.00009724918,0.04251742],"genre_scores_gemma":[0.9423187,0.000004925176,0.029394764,0.0023641444,0.00004547752,0.0000039577844,0.000006284788,0.000010027727,0.02585175],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991344,0.000009276487,0.00013101434,0.0002674013,0.00019317903,0.00026470906],"domain_scores_gemma":[0.99960643,0.0000153306,0.00003192271,0.00021661718,0.0000055584896,0.00012411347],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00006649887,0.000119860415,0.00011023816,5.2874225e-7,0.00012763262,0.000023218006,0.00014439356,0.0000749094,0.02020062],"category_scores_gemma":[0.00000895825,0.00008654919,0.00006915626,0.00008347641,0.000043752243,0.000098650446,0.000043637127,0.000056332552,0.00047557463],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016073577,0.00033931757,0.021596756,0.000005658986,0.000018631692,0.000013497519,0.00062640884,0.0008860832,0.066192076,0.005645914,0.8094854,0.09502955],"study_design_scores_gemma":[0.0013917736,0.0008060244,0.26566422,0.000015999778,0.000021009104,0.000014768393,0.000437456,0.0005820068,0.016364181,0.008729158,0.7052218,0.00075161137],"about_ca_topic_score_codex":0.00013387945,"about_ca_topic_score_gemma":0.000013307404,"teacher_disagreement_score":0.24406746,"about_ca_system_score_codex":0.00004098279,"about_ca_system_score_gemma":0.0000047543717,"threshold_uncertainty_score":0.98069507},"labels":[],"label_agreement":null},{"id":"W2043323308","doi":"10.1175/jas-d-10-05001.1","title":"Correlated k-Distribution Treatment of Cloud Optical Properties and Related Radiative Impact","year":2011,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":19,"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":"Radiative transfer; Cloud albedo; Longwave; Cloud top; Computational physics; Cloud computing; Radiative flux; Flux (metallurgy); Absorption (acoustics); Materials science; Physics; Environmental science; Atmospheric sciences; Cloud cover; Optics","score_opus":0.029132126279398537,"score_gpt":0.22944710507013222,"score_spread":0.20031497879073368,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2043323308","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":[0.99638796,0.00062763377,0.00006915114,0.00014272447,0.00033993757,0.00011053121,0.0000013160111,0.0000051905117,0.0023155322],"genre_scores_gemma":[0.998111,0.00016928244,0.0014283753,0.00001331551,0.000020675676,0.0000011245817,8.2049475e-8,0.0000044341523,0.0002516832],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988556,0.00008180358,0.00037514133,0.0001342766,0.00035769958,0.0001954722],"domain_scores_gemma":[0.9992309,0.000038449693,0.00048703433,0.00011916149,0.000025326208,0.00009912964],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035049426,0.00012593169,0.00022866888,3.9738927e-7,0.00019866366,0.000017532646,0.00028622954,0.00005539751,0.000587193],"category_scores_gemma":[0.00007367079,0.000057339195,0.00014600533,0.00048769033,0.0013175643,0.00023445026,0.00007937971,0.000083278705,0.000008641909],"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":[0.00042340052,0.00084559084,0.9253466,0.00000675417,0.0002461103,0.000026227839,0.012029638,0.027219694,0.010248928,0.0003885056,0.0011783119,0.022040226],"study_design_scores_gemma":[0.00079809764,0.0035386991,0.965955,0.000052528183,0.0001279643,0.00030338255,0.0016132073,0.019964525,0.005926306,0.0013154034,0.00022628198,0.0001785647],"about_ca_topic_score_codex":0.00034299266,"about_ca_topic_score_gemma":0.0000043881964,"teacher_disagreement_score":0.04060843,"about_ca_system_score_codex":0.00018396428,"about_ca_system_score_gemma":0.000064870386,"threshold_uncertainty_score":0.64293516},"labels":[],"label_agreement":null},{"id":"W2043644479","doi":"10.1002/joc.774","title":"Parameterization of effective ice particle size for high‐latitude clouds","year":2002,"lang":"en","type":"article","venue":"International Journal of Climatology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Research Council Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Ice crystals; Particle size; Particle (ecology); Latitude; Particle-size distribution; Environmental science; Atmospheric sciences; Physics; Chemistry; Meteorology; Geology","score_opus":0.009643249163625004,"score_gpt":0.25686126920275854,"score_spread":0.24721802003913354,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2043644479","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":[0.97812253,0.000045549335,0.019744234,0.0009614319,0.000565151,0.00010331858,0.0000057906195,0.0000046273594,0.00044739217],"genre_scores_gemma":[0.9894752,0.00004723113,0.010091382,0.00023189033,0.00007349568,0.000007310746,8.946128e-7,0.0000072925027,0.00006530676],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990946,0.000048444403,0.00040081056,0.00009208387,0.0002444288,0.00011960547],"domain_scores_gemma":[0.99896127,0.00040670924,0.00044034465,0.00006573648,0.000081426624,0.00004451768],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00016160838,0.00007040751,0.00019035576,0.000002610362,0.000025556465,0.0000096174745,0.00025111655,0.0000529466,0.0015568553],"category_scores_gemma":[0.00029249204,0.00005954204,0.00008623112,0.00006252593,0.00012310191,0.0001436496,0.00005382842,0.00006599709,0.000031061856],"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":[0.0010313208,0.0011912948,0.8191629,0.000033221688,0.0005520906,0.00008373493,0.0017984674,0.025692796,0.075709,0.016236654,0.0041052457,0.05440328],"study_design_scores_gemma":[0.011325219,0.0039663403,0.75041103,0.00015302506,0.00030891664,0.0012061727,0.00045235787,0.07829222,0.10851706,0.029222015,0.015398957,0.00074670126],"about_ca_topic_score_codex":0.00001944294,"about_ca_topic_score_gemma":0.00000712897,"teacher_disagreement_score":0.06875189,"about_ca_system_score_codex":0.00006042861,"about_ca_system_score_gemma":0.0000041809544,"threshold_uncertainty_score":0.99935585},"labels":[],"label_agreement":null},{"id":"W2045042251","doi":"10.1029/2008jd010029","title":"Preliminary comparison of CloudSAT‐derived microphysical quantities with ground‐based measurements for mixed‐phase cloud research in the Arctic","year":2008,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"","keywords":"Environmental science; Lidar; Cloud top; Ice cloud; Cloud computing; Precipitation; Arctic; Liquid water content; Radar; Latitude; Meteorology; Atmospheric sciences; Remote sensing; Computer science; Geology; Geography","score_opus":0.15067143946061273,"score_gpt":0.39005673372251676,"score_spread":0.23938529426190402,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045042251","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":[0.9966051,0.00027976348,0.0011928217,0.0007701759,0.000090582645,0.00073196396,0.000004804935,0.0000059501413,0.00031885153],"genre_scores_gemma":[0.99431527,0.000033581975,0.0050858883,0.000040952953,0.00031540444,0.000065256536,0.0000024912526,0.000036334273,0.00010481067],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9926151,0.0013521282,0.00081269327,0.00038521123,0.003854071,0.0009807978],"domain_scores_gemma":[0.99577963,0.00258611,0.0003507196,0.0004966293,0.0005385451,0.00024835367],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.003237588,0.00025139932,0.0006523745,0.000009305015,0.0006025782,0.00006943208,0.0012602691,0.00011076994,0.00013691885],"category_scores_gemma":[0.00052499806,0.00015532116,0.00026419968,0.0011951501,0.0027218487,0.00027161025,0.00022594164,0.0013592655,0.000038004866],"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":[0.06337508,0.04910766,0.41606852,0.0010801427,0.00068973954,0.0010589301,0.021051507,0.017377757,0.34311405,0.002164304,0.053667158,0.031245142],"study_design_scores_gemma":[0.01871024,0.06676074,0.8001959,0.0011864778,0.0001477028,0.0001462998,0.023827063,0.01743727,0.05637139,0.009533313,0.004649659,0.0010339925],"about_ca_topic_score_codex":0.0020725697,"about_ca_topic_score_gemma":0.00024224508,"teacher_disagreement_score":0.38412732,"about_ca_system_score_codex":0.00035601505,"about_ca_system_score_gemma":0.00032074467,"threshold_uncertainty_score":0.9999922},"labels":[],"label_agreement":null},{"id":"W2045202040","doi":"10.1175/jas-d-14-0124.1","title":"Evaluating the Diurnal Cycle of Upper-Tropospheric Ice Clouds in Climate Models Using SMILES Observations","year":2014,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":45,"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":"California Institute of Technology; Jet Propulsion Laboratory; National Aeronautics and Space Administration","keywords":"Diurnal cycle; Empirical orthogonal functions; Environmental science; Climatology; Atmospheric sciences; Troposphere; Diurnal temperature variation; Middle latitudes; Climate model; Amplitude; Annual cycle; Geology; Climate change; Oceanography; Physics","score_opus":0.06477399157033066,"score_gpt":0.31552621312425955,"score_spread":0.2507522215539289,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045202040","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":[0.9938941,0.00025917226,0.0033285462,0.0008085987,0.00045533563,0.00013361133,6.9621126e-7,0.0000055075484,0.0011144604],"genre_scores_gemma":[0.9347516,0.00007311433,0.06467034,0.00034556247,0.00009226069,0.0000021993267,3.7387967e-8,0.000011206678,0.00005370008],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9970602,0.00036612345,0.00079390866,0.00022029928,0.0011425711,0.00041689156],"domain_scores_gemma":[0.9981523,0.00029640333,0.0011016341,0.000323029,0.00005014489,0.000076449156],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0034329419,0.00017095878,0.000300718,9.040246e-7,0.0006685683,0.0000759057,0.0015405304,0.0000529008,0.0002570538],"category_scores_gemma":[0.00026346545,0.00008807875,0.00020602145,0.001325896,0.00095749536,0.00061454484,0.00041296653,0.0002717211,0.000003378621],"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":[0.000015849704,0.000050476207,0.17642644,0.0000038028952,0.0000067684095,4.460908e-7,0.0005052587,0.81352454,0.006415481,0.00031720282,0.000036404886,0.0026973072],"study_design_scores_gemma":[0.00024657245,0.00023315346,0.141958,0.0000760355,0.0000354539,0.000036907622,0.0011115986,0.850084,0.00015509436,0.0058807316,0.00007122631,0.000111186884],"about_ca_topic_score_codex":0.0007121125,"about_ca_topic_score_gemma":0.00006283963,"teacher_disagreement_score":0.061341792,"about_ca_system_score_codex":0.00016109363,"about_ca_system_score_gemma":0.00009907178,"threshold_uncertainty_score":0.51421547},"labels":[],"label_agreement":null},{"id":"W2045310135","doi":"10.1109/microrad.2014.6878923","title":"ISMAR: A new Submillimeter Airborne Radiometer","year":2014,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":12,"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":"Remote sensing; Radiometer; Nadir; Satellite; Instrumentation (computer programming); Environmental science; Radiometry; Ice cloud; Depth sounding; Spectrometer; Meteorology; Computer science; Aerospace engineering; Physics; Optics; Geology; Engineering","score_opus":0.005561815631947792,"score_gpt":0.1867504914499603,"score_spread":0.1811886758180125,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045310135","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":[0.6404941,0.000017466738,0.088055015,0.00094873563,0.00016160886,0.000091195194,2.9403563e-7,0.00009123886,0.27014032],"genre_scores_gemma":[0.920155,0.0000044701706,0.02399309,0.0024269526,0.0001050859,0.0000033655997,9.160173e-7,0.000013304614,0.053297814],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9992071,0.000020684522,0.000115830146,0.0002300791,0.00018170259,0.00024460396],"domain_scores_gemma":[0.99952906,0.000023131164,0.00002600965,0.00025211126,0.000001456609,0.00016823279],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000107955224,0.00010467994,0.00010479292,7.468017e-7,0.00005133161,0.000021968062,0.00017854433,0.000046252186,0.034699813],"category_scores_gemma":[0.000013140868,0.00007664195,0.000058636528,0.00016165034,0.00006993398,0.000097413635,0.00011114256,0.000055837794,0.004860297],"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":[0.000021796519,0.00008464138,0.14479874,0.0000032405308,0.000022675129,0.0000041697313,0.00034176104,0.00018897065,0.007882342,0.0011902287,0.37728482,0.4681766],"study_design_scores_gemma":[0.0005397073,0.00017022988,0.32703757,0.0000026918754,0.000015867336,0.000009567037,0.000024035724,0.0036045648,0.0023924876,0.0016944295,0.66416425,0.00034458947],"about_ca_topic_score_codex":0.0006269005,"about_ca_topic_score_gemma":0.000055342,"teacher_disagreement_score":0.46783203,"about_ca_system_score_codex":0.000037960595,"about_ca_system_score_gemma":0.0000035102598,"threshold_uncertainty_score":0.9959145},"labels":[],"label_agreement":null},{"id":"W2045461786","doi":"10.1029/2012jd017889","title":"Characterization of Arctic ice cloud properties observed during ISDAC","year":2012,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","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; Université du Québec à Montréal","funders":"","keywords":"Ice crystals; Ice nucleus; Environmental science; Atmospheric sciences; Arctic; Supersaturation; Precipitation; Nucleation; Geology; Meteorology; Physics; Oceanography","score_opus":0.050073371777117445,"score_gpt":0.2804749530795565,"score_spread":0.23040158130243904,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045461786","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":[0.99850917,0.00017096529,0.00011889069,0.00020231507,0.00017951378,0.0001494654,0.0000012763284,0.00000786782,0.0006605509],"genre_scores_gemma":[0.9971002,0.00010372712,0.00065542496,0.000024934681,0.00067760836,0.000006037826,6.816298e-7,0.00002297495,0.0014084225],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99715817,0.00026315745,0.00049384515,0.0001471402,0.0013239909,0.0006136767],"domain_scores_gemma":[0.99885166,0.00011561059,0.00031737497,0.00023285298,0.00016015166,0.00032236704],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008199207,0.00014333753,0.00031450603,0.0000017327743,0.00017498732,0.000037576057,0.00043498812,0.00007217281,0.0015343011],"category_scores_gemma":[0.00035771346,0.00010157403,0.00015702828,0.00046567447,0.0004248648,0.00072893786,0.00029659955,0.0004920048,0.00017365385],"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":[0.00031497312,0.00053898187,0.1635343,0.00007741499,0.000042913995,0.000007996439,0.0008199161,0.0000822166,0.8317334,0.00009894865,0.0001721706,0.002576768],"study_design_scores_gemma":[0.0003968789,0.00039999597,0.9212709,0.00012085106,0.000017610286,0.000015166952,0.0004737949,0.00021559974,0.0754591,0.00020277068,0.0012931523,0.00013417572],"about_ca_topic_score_codex":0.00052345084,"about_ca_topic_score_gemma":0.000013260251,"teacher_disagreement_score":0.7577366,"about_ca_system_score_codex":0.00019747287,"about_ca_system_score_gemma":0.000045634148,"threshold_uncertainty_score":0.99937844},"labels":[],"label_agreement":null},{"id":"W2045557944","doi":"10.1007/s10546-013-9873-3","title":"Turbulence in Continental Stratocumulus, Part I: External Forcings and Turbulence Structures","year":2013,"lang":"en","type":"article","venue":"Boundary-Layer Meteorology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":17,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Liquid water path; Marine stratocumulus; Environmental science; Radiative cooling; Sensible heat; Atmospheric sciences; Cloud height; Liquid water content; Diurnal cycle; Latent heat; Cloud forcing; Cloud top; Cloud base; Turbulence; Meteorology; Cloud cover; Geology; Cloud computing; Physics; Radiative forcing; Precipitation","score_opus":0.008534336264736622,"score_gpt":0.2192712343950844,"score_spread":0.21073689813034777,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045557944","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":[0.995446,0.0005798492,0.00051909836,0.0004967565,0.00026417556,0.00039347692,0.0000053025765,0.000041943164,0.0022533843],"genre_scores_gemma":[0.99325657,0.00006686821,0.0045867343,0.0012092517,0.00007461342,0.00007527698,0.0000028681984,0.000021967458,0.0007058488],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979843,0.00009989149,0.00038603,0.00061282294,0.00027260307,0.00064438157],"domain_scores_gemma":[0.9993029,0.000070580456,0.00013178572,0.00029137672,0.000011214721,0.00019213899],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021987008,0.00028178492,0.00032527692,0.0000058739984,0.00018380761,0.000122769,0.0003473753,0.0001774911,0.0076325843],"category_scores_gemma":[0.000042405383,0.00024090466,0.000053177035,0.00015136423,0.00082494656,0.00044817931,0.0003207177,0.0003135444,0.00024720855],"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":[0.000103236096,0.000100068006,0.9135578,0.000019187199,0.000023227125,0.000076126984,0.0010415914,0.00037014845,0.049114857,0.0012038164,0.0037243825,0.030665517],"study_design_scores_gemma":[0.0010734991,0.00033011468,0.96289307,0.00001845199,0.00001849081,0.00016718757,0.00021505624,0.0028985504,0.0022959686,0.018503899,0.011112536,0.0004731896],"about_ca_topic_score_codex":0.003668903,"about_ca_topic_score_gemma":0.000607472,"teacher_disagreement_score":0.04933521,"about_ca_system_score_codex":0.000079655896,"about_ca_system_score_gemma":0.000025250314,"threshold_uncertainty_score":0.99327457},"labels":[],"label_agreement":null},{"id":"W2045884461","doi":"10.1029/2000gl011944","title":"Cirrus horizontal inhomogeneity and OLR bias","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":59,"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","funders":"","keywords":"Cirrus; Outgoing longwave radiation; Troposphere; Radiative transfer; Longwave; Environmental science; Optical depth; Atmospheric sciences; Horizontal plane; Cloud cover; Meteorology; Physics; Cloud computing; Convection; Geology; Optics; Geodesy","score_opus":0.0342281182706324,"score_gpt":0.2881355950598995,"score_spread":0.2539074767892671,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045884461","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":[0.9848508,0.000022353317,0.000025345593,0.0026733722,0.000027037198,0.00015111417,0.000003290263,0.00003141507,0.012215219],"genre_scores_gemma":[0.99657565,0.000038947193,0.00033206542,0.001024187,0.00016296786,0.000022608205,0.000002547123,0.000014847808,0.0018261897],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9978906,0.00014632067,0.00011786236,0.00041986947,0.00078120956,0.0006441652],"domain_scores_gemma":[0.99932045,0.00011876894,0.000013798299,0.00026726935,0.000005782755,0.0002739571],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00031280064,0.00012450146,0.00013357081,0.000002093747,0.00029777666,0.00006711854,0.00025547814,0.000049139446,0.005058118],"category_scores_gemma":[0.00003992448,0.00010507556,0.000054461118,0.00033843462,0.0008326888,0.00015171348,0.0002612073,0.00037233587,0.0032466084],"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":[0.00019881844,0.00039742832,0.080190726,0.000015402235,0.00003528644,0.00022314732,0.0008092424,0.00011362468,0.26644257,0.00042002008,0.06859951,0.5825542],"study_design_scores_gemma":[0.0006235758,0.0004173396,0.9050701,0.000012507214,0.000008010546,0.000013274979,0.00010744674,0.00088124635,0.0028253007,0.0013148084,0.088304155,0.0004221986],"about_ca_topic_score_codex":0.0025490932,"about_ca_topic_score_gemma":0.000053311254,"teacher_disagreement_score":0.8248794,"about_ca_system_score_codex":0.00010500365,"about_ca_system_score_gemma":0.000009165541,"threshold_uncertainty_score":0.9975295},"labels":[],"label_agreement":null},{"id":"W2046336178","doi":"10.5194/acpd-12-30021-2012","title":"The albedo properties of four clean stratocumulus clouds studied during the VOCALS-REX field campaign","year":2012,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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 Manchester; Fund for Innovative Climate and Energy Research; Natural Environment Research Council; Met Office; University of Calgary; National Science Foundation","keywords":"Marine stratocumulus; Shortwave; Albedo (alchemy); Environmental science; Atmospheric sciences; Drizzle; Zenith; Radiometer; Solar zenith angle; Cloud albedo; Meteorology; Overcast; Cirrus; Transect; Radiative transfer; Cloud computing; Cloud cover; Geology; Remote sensing; Aerosol; Geography; Physics; Oceanography","score_opus":0.016423351635703562,"score_gpt":0.21455630818888202,"score_spread":0.19813295655317847,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2046336178","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":[0.9790699,0.00024006456,0.00019489191,0.0007474661,0.00015391485,0.00026480257,3.8920712e-7,0.000026902306,0.019301688],"genre_scores_gemma":[0.9928266,0.000047235644,0.0001221673,0.00025919775,0.000103816485,0.000025593774,6.4303286e-8,0.000011800789,0.006603531],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99885225,0.00006807623,0.00022814056,0.00014068514,0.0003056576,0.00040515937],"domain_scores_gemma":[0.99937415,0.000092287126,0.000082634404,0.0003672136,0.0000072952485,0.00007639187],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003797291,0.00013295881,0.0001240684,3.8133598e-7,0.00047884727,0.000033201846,0.00038213958,0.00004778144,0.00096167583],"category_scores_gemma":[0.000048765993,0.000057389385,0.000071613715,0.000094184245,0.0002887554,0.0001242358,0.00030293755,0.00013226995,0.00012478183],"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":[0.00023664639,0.00040294748,0.8679516,0.000052403753,0.00019849438,0.0000039388483,0.012067768,0.0012586005,0.05676896,0.0029291436,0.013996173,0.044133373],"study_design_scores_gemma":[0.0009715818,0.0004419057,0.74332994,0.000047839643,0.000090949405,0.000026619025,0.038481504,0.0016880009,0.19146635,0.0003597754,0.022332344,0.00076320715],"about_ca_topic_score_codex":0.0008658787,"about_ca_topic_score_gemma":0.00041833025,"teacher_disagreement_score":0.1346974,"about_ca_system_score_codex":0.000042930216,"about_ca_system_score_gemma":0.0000069265375,"threshold_uncertainty_score":0.9999516},"labels":[],"label_agreement":null},{"id":"W2046554225","doi":"10.1256/qj.03.120","title":"Aircraft observations of cloud droplet number concentration: Implications for climate studies","year":2004,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":96,"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; Environmental science; Radiative forcing; Cloud forcing; Cloud computing; Forcing (mathematics); Aerosol; Atmosphere (unit); Planetary boundary layer; Function (biology); Meteorology; Boundary layer; Physics; Thermodynamics","score_opus":0.03188814312685147,"score_gpt":0.2816927281957486,"score_spread":0.24980458506889713,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2046554225","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":[0.9819709,0.00012940787,0.010259178,0.0069642304,0.00028551547,0.00022223245,0.00001931546,0.000010342573,0.00013887603],"genre_scores_gemma":[0.9725149,0.000048953112,0.026503602,0.00071459566,0.00013774267,0.000017306398,0.00000100694,0.000006979021,0.000054859185],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987857,0.000065523935,0.00053975824,0.00014049067,0.00022203344,0.0002465244],"domain_scores_gemma":[0.9989618,0.00017752062,0.0005135455,0.00018372115,0.00008803315,0.000075402764],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047851214,0.00012411457,0.00028323138,2.821228e-7,0.00032761018,0.000015988579,0.00038077284,0.00009322049,0.00015720073],"category_scores_gemma":[0.000069234186,0.00007097264,0.00051425776,0.00015635525,0.00044037297,0.00010015382,0.000059165577,0.0001680672,0.000007751301],"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":[0.0002725757,0.0014846288,0.8221678,0.000101035774,0.0009859324,0.0000026933585,0.01196389,0.06630901,0.02784615,0.028325057,0.032116137,0.008425065],"study_design_scores_gemma":[0.002306255,0.0022033486,0.91468525,0.000046853016,0.0003404516,0.000032920245,0.003684346,0.00065382366,0.00062639604,0.07095112,0.004160466,0.00030878684],"about_ca_topic_score_codex":0.0000138497335,"about_ca_topic_score_gemma":0.000006017354,"teacher_disagreement_score":0.09251742,"about_ca_system_score_codex":0.00014895023,"about_ca_system_score_gemma":0.0000244615,"threshold_uncertainty_score":0.28941804},"labels":[],"label_agreement":null},{"id":"W2046752734","doi":"10.1029/2002jd002391","title":"Limitations of using an equilibrium approximation in an aerosol activation parameterization","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","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":"Dalhousie University","funders":"","keywords":"Aerosol; Cloud condensation nuclei; Supersaturation; Sulfate; Atmospheric sciences; Environmental science; Radiative forcing; Particle number; Meteorology; Condensation; Radiative transfer; Sea salt; Particle (ecology); Sea salt aerosol; Thermodynamics; Mechanics; Chemistry; Physics; Geology","score_opus":0.12846591377861696,"score_gpt":0.34374793147932386,"score_spread":0.2152820177007069,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2046752734","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":[0.987955,0.0000107479555,0.011186019,0.000038661732,0.00003672259,0.0001748673,6.9305014e-7,0.0000046761043,0.0005926528],"genre_scores_gemma":[0.9751007,0.000012560049,0.024758996,0.000014066867,0.000052948548,0.000004492908,0.0000023736834,0.000015597974,0.000038284306],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9975634,0.0005711815,0.00047469934,0.00018369338,0.00090443157,0.00030256505],"domain_scores_gemma":[0.9988931,0.00028412053,0.00028983905,0.00020548735,0.00015587444,0.00017160914],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008697401,0.00010436563,0.00021411819,0.0000044000594,0.00008681856,0.000056050438,0.00023951985,0.000076814074,0.00021996885],"category_scores_gemma":[0.0008018521,0.00008999534,0.000062696345,0.0007706747,0.0002367975,0.0014356134,0.00004900146,0.0003138441,0.000009000918],"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":[0.00020050813,0.0016018406,0.044387493,0.000018443141,0.00001361113,0.000006214332,0.0011918291,0.08542958,0.85141724,0.0010164895,0.000041339412,0.014675406],"study_design_scores_gemma":[0.002213751,0.0051183645,0.3670627,0.00020980168,0.000036663703,0.000020004274,0.005867923,0.41643134,0.17888252,0.023325238,0.00027277457,0.00055891485],"about_ca_topic_score_codex":0.00034078988,"about_ca_topic_score_gemma":0.00007104596,"teacher_disagreement_score":0.6725347,"about_ca_system_score_codex":0.00020063146,"about_ca_system_score_gemma":0.00009533119,"threshold_uncertainty_score":0.36699036},"labels":[],"label_agreement":null},{"id":"W2046826830","doi":"10.5194/amt-7-1089-2014","title":"Evaluation of gridded scanning ARM cloud radar reflectivity observations and vertical doppler velocity retrievals","year":2014,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Biological and Environmental Research; McGill University; U.S. Department of Energy","keywords":"Zenith; Radar; Remote sensing; Doppler radar; Doppler effect; Geology; Meteorology; Environmental science; Physics; Computer science","score_opus":0.06443179236074212,"score_gpt":0.2771559377750848,"score_spread":0.21272414541434267,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2046826830","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":[0.92623466,0.00014794704,0.063155405,0.0002120415,0.00010219699,0.0006698352,0.000001353245,0.00019348857,0.009283093],"genre_scores_gemma":[0.9348932,0.000033080563,0.0647067,0.00017165417,0.00006327915,0.00008476959,0.0000019196434,0.000022309647,0.00002311594],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9957312,0.00043552145,0.00043563897,0.00045229826,0.0026419654,0.0003034255],"domain_scores_gemma":[0.9989109,0.000061538005,0.00016702643,0.00041700352,0.00031999507,0.00012351431],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0076854113,0.00022328031,0.00030676444,7.627364e-7,0.00021020859,0.000028041411,0.00021046224,0.00013249132,0.00054586504],"category_scores_gemma":[0.0011424996,0.00020325425,0.00006867565,0.0004368624,0.0002666448,0.00021323244,0.00016295929,0.00016567338,0.000006785247],"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":[0.00014512632,0.0008941922,0.24805453,0.00007996967,0.00017585361,0.0000013095952,0.0009212007,0.00042998604,0.39156494,0.002265403,0.017007563,0.3384599],"study_design_scores_gemma":[0.0011967896,0.0009262001,0.74784297,0.00017186557,0.00053004536,0.0000096277045,0.00013954408,0.043475814,0.18098205,0.0138024185,0.010078286,0.00084438885],"about_ca_topic_score_codex":0.00058109045,"about_ca_topic_score_gemma":0.00009503949,"teacher_disagreement_score":0.49978843,"about_ca_system_score_codex":0.00072636234,"about_ca_system_score_gemma":0.000083949206,"threshold_uncertainty_score":0.8288468},"labels":[],"label_agreement":null},{"id":"W2046925220","doi":"10.1029/2003gl017828","title":"Comparing continental and oceanic cloud susceptibilities to aerosols","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","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":"Dalhousie University","funders":"","keywords":"Aerosol; Effective radius; Liquid water path; Environmental science; Cloud computing; Atmospheric sciences; RADIUS; Liquid water content; Meteorology; Climatology; Geology; Geography; Physics","score_opus":0.031010293993201477,"score_gpt":0.28649216073461786,"score_spread":0.2554818667414164,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2046925220","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":[0.9896465,0.000014882938,0.00022133619,0.0013828153,0.000084287756,0.0002843869,0.0000015153806,0.000030876545,0.008333382],"genre_scores_gemma":[0.9967057,0.0000044734666,0.0006699379,0.0011656414,0.00010620399,0.000023998153,0.0000013203813,0.000017080942,0.0013056602],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99774396,0.00017775371,0.00015744219,0.00046779096,0.00069081254,0.0007622573],"domain_scores_gemma":[0.9991461,0.00019322151,0.000019239968,0.00028208733,0.000011787675,0.00034756077],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00046612413,0.00014519674,0.0001938684,0.0000032743276,0.00028812158,0.00009633156,0.00023689955,0.00003561223,0.00082686584],"category_scores_gemma":[0.00018043847,0.00012890616,0.00005257679,0.0003221079,0.00063115254,0.0001255872,0.00037196523,0.00033179522,0.0010176721],"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":[0.00010449938,0.0002643633,0.39650655,0.000023802484,0.000027906677,0.000044868408,0.0018280331,0.00018343066,0.49321595,0.0066858726,0.09968427,0.0014304599],"study_design_scores_gemma":[0.0014734602,0.0007408868,0.92887986,0.000057167974,0.0000142322115,0.000015902942,0.0028561614,0.00082081626,0.010968734,0.0024352646,0.05080515,0.0009323508],"about_ca_topic_score_codex":0.000635386,"about_ca_topic_score_gemma":0.000042684926,"teacher_disagreement_score":0.5323733,"about_ca_system_score_codex":0.00014177705,"about_ca_system_score_gemma":0.000009355407,"threshold_uncertainty_score":0.99976015},"labels":[],"label_agreement":null},{"id":"W2047340247","doi":"10.1002/met.3","title":"Comparison of VAAC atmospheric dispersion models using the 1 November 2004 Grimsvötn eruption","year":2007,"lang":"en","type":"article","venue":"Meteorological Applications","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":111,"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","funders":"Met Office","keywords":"Volcanic ash; Volcano; Environmental science; Meteorology; Dispersion (optics); Atmospheric sciences; Atmospheric dispersion modeling; Tephra; Vulcanian eruption; Numerical weather prediction; Climatology; Geology; Geography; Air pollution; Seismology","score_opus":0.04074113172469053,"score_gpt":0.31201628489699745,"score_spread":0.27127515317230694,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2047340247","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.47857592,0.00012966878,0.51763916,0.00013254065,0.000018182745,0.00026971105,0.0000020058437,0.00002597298,0.0032068507],"genre_scores_gemma":[0.95475525,0.000010851879,0.044752117,0.00020872577,0.00003943962,0.000047184487,0.000005472627,0.000009234215,0.0001717272],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9987673,0.000037918027,0.0003492041,0.00028625675,0.00028722204,0.00027211028],"domain_scores_gemma":[0.9992685,0.000112139576,0.00017346523,0.00034634935,0.00001559172,0.00008399784],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00038282626,0.00013080357,0.00018921412,6.063366e-7,0.00027970586,0.000011063693,0.00031984312,0.0001161019,0.0011670897],"category_scores_gemma":[0.000010110334,0.00008090477,0.0000912544,0.00046474798,0.00038039265,0.000091192516,0.00017257089,0.00015895214,0.00008037222],"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":[0.00012520059,0.0016101893,0.24347098,0.000013853104,0.000046069938,0.0000013758574,0.0007612025,0.46167356,0.17561452,0.02174356,0.0014245287,0.09351496],"study_design_scores_gemma":[0.00064891926,0.00036738196,0.30094415,0.000009753463,0.00019314392,0.000013428941,0.0013047565,0.6359714,0.007144746,0.021740211,0.031004535,0.00065755524],"about_ca_topic_score_codex":0.00020472643,"about_ca_topic_score_gemma":0.000043794982,"teacher_disagreement_score":0.47617933,"about_ca_system_score_codex":0.000101320366,"about_ca_system_score_gemma":0.0000051763272,"threshold_uncertainty_score":0.99974597},"labels":[],"label_agreement":null},{"id":"W2047467297","doi":"10.1364/ao.40.002368","title":"Modified Ångström exponent for the characterization of submicrometer aerosols","year":2001,"lang":"en","type":"article","venue":"Applied Optics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":270,"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 de Sherbrooke","funders":"","keywords":"Angstrom exponent; Physics; Exponent; Optics; Angstrom; RADIUS; Effective radius; Computational physics; Wavelength; Astrophysics","score_opus":0.014568211684730303,"score_gpt":0.21074611837943827,"score_spread":0.19617790669470797,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2047467297","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":[0.909535,0.000004664838,0.08593146,0.00016983278,0.000071353286,0.00043603414,0.0000068196655,0.000016221798,0.0038286436],"genre_scores_gemma":[0.9945234,0.0000645507,0.0042472566,0.00023375367,0.000046957837,0.00009937574,0.000015944393,0.000015827129,0.0007529495],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9993042,0.0000047619446,0.0001905683,0.00015899258,0.00015185874,0.00018966282],"domain_scores_gemma":[0.9995606,0.00005020429,0.000105744926,0.00023937003,0.000007126727,0.000036943013],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010506452,0.0000985304,0.000111778434,7.507939e-7,0.00009935481,0.00001643489,0.00019958695,0.00005383245,0.00030281508],"category_scores_gemma":[0.0000053298622,0.00006968275,0.000046825295,0.0001229782,0.000116403346,0.000040434872,0.00008239882,0.000048176895,0.00004714421],"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":[0.00008368297,0.00010851524,0.0034258843,0.000008131582,0.000022361888,5.452418e-7,0.00038630833,0.0021275003,0.97737193,0.0035250268,0.00023329898,0.012706836],"study_design_scores_gemma":[0.005104938,0.0006506612,0.51039386,0.00003500687,0.0004035443,0.000023759798,0.0013413966,0.070187,0.3395039,0.004257296,0.06624687,0.0018517218],"about_ca_topic_score_codex":0.000014580315,"about_ca_topic_score_gemma":0.0000029646528,"teacher_disagreement_score":0.637868,"about_ca_system_score_codex":0.000029703115,"about_ca_system_score_gemma":0.000003923721,"threshold_uncertainty_score":0.33156127},"labels":[],"label_agreement":null},{"id":"W2048374182","doi":"10.1175/jtech-d-14-00112.1","title":"Developing and Evaluating Ice Cloud Parameterizations for Forward Modeling of Radar Moments Using in situ Aircraft Observations","year":2015,"lang":"en","type":"article","venue":"Journal of Atmospheric and Oceanic Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Remote sensing; Kurtosis; Skewness; Radar; Doppler effect; Zenith; Environmental science; Doppler radar; Meteorology; Computational physics; Physics; Geology; Computer science; Mathematics; Statistics","score_opus":0.06357290530243373,"score_gpt":0.30048665934190005,"score_spread":0.23691375403946632,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2048374182","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":[0.67342794,0.0003088596,0.3257891,0.00026737785,0.00006351852,0.000116430114,6.794353e-7,0.00000756505,0.000018514698],"genre_scores_gemma":[0.6039261,0.00006343784,0.39593962,0.000039126786,0.000012635008,0.0000019095694,2.7072016e-7,0.000008259601,0.0000086256705],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9988919,0.00002511805,0.0005486454,0.0001561226,0.00017855654,0.00019966751],"domain_scores_gemma":[0.99934816,0.00005076689,0.00036862338,0.00009774583,0.00006797291,0.00006673873],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004493464,0.00011545983,0.0002944995,0.0000033540414,0.00008578177,0.000011584028,0.00014871667,0.00012029459,0.00000542429],"category_scores_gemma":[0.00024045345,0.00010420973,0.000034204495,0.0004646045,0.00012889867,0.00020893656,0.00014434733,0.00013089637,2.2787054e-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":[0.00030502965,0.00030933524,0.60932577,0.00014147213,0.0002071613,0.00002128029,0.0035147448,0.26020548,0.06510739,0.0062716124,0.0001781727,0.054412547],"study_design_scores_gemma":[0.0023267595,0.00078480167,0.012038435,0.00015752646,0.00011480488,0.00014718155,0.005137069,0.9492586,0.0005643392,0.028866237,0.00030782,0.0002963839],"about_ca_topic_score_codex":0.000032304903,"about_ca_topic_score_gemma":0.000011586144,"teacher_disagreement_score":0.6890532,"about_ca_system_score_codex":0.00016444577,"about_ca_system_score_gemma":0.00009086384,"threshold_uncertainty_score":0.42495492},"labels":[],"label_agreement":null},{"id":"W2048694501","doi":"10.1063/1.1343481","title":"Effect of condensation and evaporation on the viscous-convective subrange","year":2001,"lang":"en","type":"article","venue":"Physics of Fluids","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":8,"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 British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Killam Trusts","keywords":"Physics; Convection; Scaling; Scalar (mathematics); Condensation; Isotropy; Radiative transfer; Mechanics; Classical mechanics; Statistical physics; Thermodynamics; Optics; Geometry","score_opus":0.008534494510091983,"score_gpt":0.23242528543793542,"score_spread":0.22389079092784345,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2048694501","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":[0.9940821,0.000014989173,0.0011562925,0.000086483094,0.000021237096,0.00014703827,0.0000014459735,0.00000492006,0.004485505],"genre_scores_gemma":[0.99983406,0.000012204549,0.000026476031,0.000041289924,0.000022833734,0.0000071327213,0.0000014114821,0.000004558287,0.00005004889],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9995754,0.000046642977,0.00007859972,0.00009071131,0.00014967562,0.000058979425],"domain_scores_gemma":[0.9997043,0.00010995933,0.000055469278,0.00010970721,0.000006850632,0.000013705131],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015911559,0.0000597497,0.00008760159,4.1411735e-7,0.000038149483,0.000003948912,0.0000534815,0.000018991235,0.00010425044],"category_scores_gemma":[0.000014959719,0.000038453527,0.00002569661,0.00008917787,0.00015470559,0.000075554024,0.000024443356,0.000035423345,0.000017158205],"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":[0.00025834868,0.00014890575,0.22070369,0.00003157322,0.000036164234,9.421974e-7,0.002251696,0.0010428538,0.7163283,0.009836376,0.00042355977,0.04893754],"study_design_scores_gemma":[0.0009183027,0.0022731067,0.18568842,0.000034614946,0.00006848545,0.0000016685281,0.00017401131,0.016770128,0.78402954,0.009666972,0.00016104248,0.00021368287],"about_ca_topic_score_codex":0.00010502483,"about_ca_topic_score_gemma":0.0000044561425,"teacher_disagreement_score":0.06770123,"about_ca_system_score_codex":0.00001812718,"about_ca_system_score_gemma":0.0000023314392,"threshold_uncertainty_score":0.15680893},"labels":[],"label_agreement":null},{"id":"W2049292513","doi":"10.5194/acpd-3-2353-2003","title":"Characteristics, impacts and direct radiative forcing of aerosols at the ARM Southern Great Plains Central Facility","year":2003,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Oceanic and Atmospheric Administration; Dalhousie University; U.S. Department of Energy","keywords":"Angstrom exponent; Aerosol; Single-scattering albedo; Atmospheric sciences; Environmental science; Radiative forcing; Albedo (alchemy); Relative humidity; Radiative transfer; Precipitation; Climatology; Meteorology; Physics; Geology","score_opus":0.010632488050506555,"score_gpt":0.21240491433560274,"score_spread":0.20177242628509617,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2049292513","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":[0.9819782,0.00015768239,0.00068520167,0.000092285285,0.00019184234,0.00054383004,0.00066862535,0.000028444772,0.015653936],"genre_scores_gemma":[0.9942673,0.00029246366,0.00029959192,0.00014839451,0.000031343425,0.000018742126,0.000043078657,0.000017176299,0.0048819496],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981531,0.00012261176,0.00037694606,0.00055598083,0.00031453214,0.00047682566],"domain_scores_gemma":[0.99885577,0.00009867794,0.00033244418,0.00050828344,0.000009991058,0.00019483568],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00028950907,0.00035376186,0.00046676892,9.642531e-7,0.00020930183,0.000046770452,0.00026328114,0.00020266972,0.005385609],"category_scores_gemma":[0.00007126231,0.00022447984,0.00014875633,0.00006174892,0.00056567416,0.000049970407,0.0009355383,0.00031356968,0.00008383853],"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":[0.00006535468,0.000086113905,0.9871721,0.0000851851,0.00008926526,0.000004977147,0.0058410224,0.0009894457,0.0009740618,0.000013777985,0.0011964359,0.003482207],"study_design_scores_gemma":[0.000506574,0.00012621224,0.9905006,0.00008021835,0.00013204924,0.000008622584,0.0010690734,0.0018180789,0.00299911,0.00020952497,0.0018198069,0.0007301129],"about_ca_topic_score_codex":0.0023885737,"about_ca_topic_score_gemma":0.00087060715,"teacher_disagreement_score":0.012289108,"about_ca_system_score_codex":0.00035729125,"about_ca_system_score_gemma":0.0000303615,"threshold_uncertainty_score":0.99552363},"labels":[],"label_agreement":null},{"id":"W2051041619","doi":"10.1063/1.4804802","title":"Scientific aspects of the Earth clouds, Aerosols, and Radiation Explorer (EarthCARE) mission","year":2013,"lang":"en","type":"article","venue":"AIP conference proceedings","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"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":"Remote sensing; Environmental science; Lidar; Radiometer; Shortwave; Satellite; Aerosol; Meteorology; Cloud computing; Radar; Computer science; Geology; Radiative transfer; Geography; Aerospace engineering; Physics","score_opus":0.015720093665793865,"score_gpt":0.2117058514493243,"score_spread":0.19598575778353045,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2051041619","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":[0.9893409,0.00005544631,0.00009736252,0.00085164426,0.00013930548,0.00033656982,0.0000011251984,0.000027396864,0.009150253],"genre_scores_gemma":[0.9979408,0.000030282554,0.000354252,0.00010648048,0.000027069276,0.000017516537,9.4135186e-7,0.000010099884,0.0015125773],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988543,0.000009980856,0.00018712673,0.00034179757,0.0003639095,0.00024287973],"domain_scores_gemma":[0.9995209,0.000012234045,0.00014221683,0.00014486459,0.00006597499,0.000113804585],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014434908,0.00013356535,0.00013135819,0.000002242806,0.00026315745,0.00018962423,0.00026644836,0.00006972264,0.0016187341],"category_scores_gemma":[0.0000620833,0.00008974113,0.000038300248,0.00026243366,0.00048214535,0.00048941287,0.00024386709,0.00012008741,0.00015594535],"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":[0.000006560391,0.00005450791,0.59563535,0.000022674658,0.000006659544,2.0136218e-7,0.0043072775,0.0000032394448,0.3769693,0.0024193297,0.003513131,0.01706173],"study_design_scores_gemma":[0.00035009775,0.00014531933,0.93227446,0.00008014034,0.000018032199,0.000007769684,0.0020249975,0.0067596566,0.044809718,0.007229334,0.0060043503,0.00029614227],"about_ca_topic_score_codex":0.00023343513,"about_ca_topic_score_gemma":0.000012147646,"teacher_disagreement_score":0.33663908,"about_ca_system_score_codex":0.000025408184,"about_ca_system_score_gemma":0.00002692601,"threshold_uncertainty_score":0.9992939},"labels":[],"label_agreement":null},{"id":"W2051436477","doi":"10.1109/igarss.2012.6351589","title":"A Bayesian approach to spaceborn hyperspectral optical flow estimation on dust aerosols","year":2012,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":5,"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 Waterloo","funders":"","keywords":"Hyperspectral imaging; Environmental science; Bayesian probability; Optical flow; Noise (video); Deposition (geology); Remote sensing; Computer science; Meteorology; Artificial intelligence; Geology; Physics","score_opus":0.01238902941105393,"score_gpt":0.22947353941756085,"score_spread":0.21708451000650691,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2051436477","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.25823596,0.0000046703626,0.3461605,0.000747966,0.0001029759,0.00030511018,0.0000011916251,0.00008904797,0.39435259],"genre_scores_gemma":[0.6831123,5.422759e-7,0.3140842,0.00058614096,0.000080738886,0.000026460733,0.0000026201997,0.000012960968,0.0020940264],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99878055,0.000020956553,0.00012721955,0.00026746697,0.00031707928,0.0004867453],"domain_scores_gemma":[0.9993266,0.000020789925,0.000021401946,0.0002497797,0.0000026714388,0.00037878126],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00016401267,0.00015584964,0.0001253984,0.0000012484986,0.000108347456,0.000035216704,0.00015171866,0.00007750435,0.0028448168],"category_scores_gemma":[0.00003102812,0.00012195329,0.0000509513,0.00019033684,0.000073053656,0.00018006309,0.00009012731,0.0001149117,0.0030943681],"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":[0.00038639974,0.0060916278,0.20577662,0.000037721624,0.00009041793,0.000012747479,0.009642926,0.29160407,0.02316942,0.061393622,0.13092124,0.27087316],"study_design_scores_gemma":[0.0014710572,0.00095740496,0.36010638,0.000028348048,0.00008086201,0.00007495983,0.0024186305,0.6061127,0.017822959,0.0004829145,0.008516929,0.0019268165],"about_ca_topic_score_codex":0.00006855749,"about_ca_topic_score_gemma":0.0000073715896,"teacher_disagreement_score":0.42487636,"about_ca_system_score_codex":0.00016721152,"about_ca_system_score_gemma":0.000004780358,"threshold_uncertainty_score":0.9980667},"labels":[],"label_agreement":null},{"id":"W2051571600","doi":"10.1175/jas3544.1","title":"Estimating Cloud Optical Depth from Surface Radiometric Observations: Sensitivity to Instrument Noise and Aerosol Contamination","year":2005,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":5,"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 du Québec à Montréal","funders":"Canadian Space Agency; Canadian Foundation for Climate and Atmospheric Sciences; Canadian Meteorological and Oceanographic Society; Université du Québec à Montréal","keywords":"Aerosol; Radiometry; Remote sensing; Environmental science; Albedo (alchemy); Noise (video); Monte Carlo method; Cloud base; Optical depth; Effective radius; Satellite; Wavelength; Optics; Cloud computing; Meteorology; Physics; Geology; Computer science; Statistics; Mathematics","score_opus":0.02184091288043881,"score_gpt":0.2458231173467898,"score_spread":0.22398220446635098,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2051571600","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":[0.98234797,0.0001326456,0.0125676645,0.0038914345,0.0005396203,0.00015054215,8.258618e-7,0.000009727104,0.0003595779],"genre_scores_gemma":[0.73663557,0.000012635277,0.2625337,0.0005801169,0.00014930793,9.834808e-7,8.814578e-8,0.00000508177,0.00008253092],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981995,0.00011319264,0.00040624422,0.00023612774,0.0007917364,0.0002531722],"domain_scores_gemma":[0.99896276,0.00029547003,0.00037172376,0.00016290775,0.00003320302,0.00017395947],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011801149,0.00014026662,0.00021471264,9.303508e-7,0.00042060387,0.00012728099,0.00039925284,0.000046220266,0.00009508813],"category_scores_gemma":[0.00047238954,0.00008956733,0.000072460454,0.001301072,0.00038544482,0.0005661424,0.00027194395,0.000153816,0.000021180442],"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":[0.000019650544,0.00010178351,0.48055726,0.0000019080924,0.000017034823,0.0000047218086,0.00076765526,0.41627383,0.019626439,0.000039262064,0.00086300244,0.08172745],"study_design_scores_gemma":[0.0003053914,0.00017993206,0.7093077,0.00004102849,0.00003188986,0.00005535171,0.00041064704,0.28646177,0.0025669304,0.00011397525,0.00036876736,0.00015666947],"about_ca_topic_score_codex":0.00031211137,"about_ca_topic_score_gemma":0.000147168,"teacher_disagreement_score":0.24996603,"about_ca_system_score_codex":0.0002544217,"about_ca_system_score_gemma":0.00004673674,"threshold_uncertainty_score":0.36524498},"labels":[],"label_agreement":null},{"id":"W2051720476","doi":"10.1175/2010jcli3395.1","title":"Long-Term Observations of the Convective Boundary Layer Using Insect Radar Returns at the SGP ARM Climate Research Facility","year":2010,"lang":"en","type":"article","venue":"Journal of Climate","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"Biological and Environmental Research; National Center for Atmospheric Research; Lawrence Livermore National Laboratory; University of Reading; U.S. Department of Energy","keywords":"Convective Boundary Layer; Boundary layer; Cloud cover; Environmental science; Atmospheric sciences; Convection; Turbulence; Daytime; Meteorology; Planetary boundary layer; Lidar; Radar; Free convective layer; Geology; Climatology; Mechanics; Physics; Cloud computing; Remote sensing","score_opus":0.07694697698936379,"score_gpt":0.3283793605637083,"score_spread":0.2514323835743445,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2051720476","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":[0.9966114,0.00007844899,0.000031036067,0.0008552771,0.00047755474,0.00020196848,0.00004628508,0.000004878879,0.0016931253],"genre_scores_gemma":[0.9989033,0.00025470514,0.0004905082,0.00013845917,0.00007174448,0.0000021523535,0.0000011060841,0.000011190786,0.00012684944],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99777216,0.0002789456,0.0005324046,0.00016629937,0.0008327552,0.00041745498],"domain_scores_gemma":[0.99856246,0.00024192008,0.0005446515,0.00044303283,0.0001107984,0.00009715989],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0024454126,0.00012953038,0.00022840194,0.0000038168973,0.0008986357,0.000062430394,0.0005772198,0.00009196643,0.0015694586],"category_scores_gemma":[0.00017861373,0.000068953486,0.00019714076,0.00034450577,0.0010748158,0.00027520306,0.0006373393,0.0007653055,0.000035402052],"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":[0.00012674474,0.00013102457,0.8233985,0.000019169385,0.000029229546,0.000010139092,0.0010742865,0.00015914124,0.17376444,0.000045595854,0.00024579256,0.0009959461],"study_design_scores_gemma":[0.00034123368,0.000106502775,0.9889946,0.00003515389,0.00003568867,0.000093575145,0.00031264097,0.00019078828,0.0077988524,0.00027787298,0.0017242233,0.00008889823],"about_ca_topic_score_codex":0.00011702929,"about_ca_topic_score_gemma":0.00091921014,"teacher_disagreement_score":0.16596559,"about_ca_system_score_codex":0.000234277,"about_ca_system_score_gemma":0.00008075303,"threshold_uncertainty_score":0.9993432},"labels":[],"label_agreement":null},{"id":"W2052724495","doi":"10.1002/joc.1966","title":"UV‐B cloud optical properties for Canada","year":2009,"lang":"en","type":"article","venue":"International Journal of Climatology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McMaster University; University of Winnipeg","funders":"","keywords":"Overcast; Cloud albedo; Optical depth; Albedo (alchemy); Environmental science; Effective radius; Atmospheric sciences; Irradiance; Radiative transfer; Single-scattering albedo; AERONET; Atmospheric radiative transfer codes; Snow; Arctic; Latitude; Solar zenith angle; Cloud cover; Middle latitudes; Cloud top; Climatology; Aerosol; Meteorology; Cloud computing; Physics; Sky; Satellite; Geography; Geology; Astrophysics; Geodesy; Optics","score_opus":0.010871501262708501,"score_gpt":0.2440343508924501,"score_spread":0.2331628496297416,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2052724495","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":[0.9762116,0.00007212436,0.0035758228,0.013571717,0.0013027037,0.000053182415,0.000002587422,0.0000040259856,0.005206219],"genre_scores_gemma":[0.9948312,0.000019408168,0.003026141,0.0017108661,0.00020655796,0.0000011897646,6.1989e-7,0.000003868301,0.00020015864],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991808,0.000012821384,0.00029902134,0.00007516879,0.00029102538,0.00014117097],"domain_scores_gemma":[0.99962765,0.000042747208,0.00015850305,0.000047691134,0.000057477915,0.00006593612],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010403826,0.000063796586,0.0001387141,0.0000018174483,0.000030806295,0.000013279002,0.00030259904,0.00003691606,0.00037187446],"category_scores_gemma":[0.00008541104,0.00004735038,0.00006118073,0.000024285586,0.000067144116,0.0000813445,0.000031699117,0.000085498905,0.000010240413],"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":[0.0029605378,0.0010037537,0.46237612,0.00001832586,0.00048297457,0.0012250101,0.0009371665,0.008920668,0.022777714,0.049915798,0.3074602,0.14192173],"study_design_scores_gemma":[0.0057806335,0.0022642452,0.40910104,0.00011941145,0.00012724094,0.0072994167,0.00095070055,0.0049346904,0.02093232,0.026132455,0.5214656,0.00089223107],"about_ca_topic_score_codex":0.0025254386,"about_ca_topic_score_gemma":0.008191245,"teacher_disagreement_score":0.21400541,"about_ca_system_score_codex":0.00014904296,"about_ca_system_score_gemma":0.000084586005,"threshold_uncertainty_score":0.45709068},"labels":[],"label_agreement":null},{"id":"W2054707521","doi":"10.1007/s00703-003-0009-z","title":"Dynamical and microphysical characteristics of Arctic clouds using integrated observations collected over SHEBA during the April 1998 FIRE.ACE flights of the Canadian Convair","year":2004,"lang":"en","type":"article","venue":"Meteorology and Atmospheric Physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":8,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Air Canada","funders":"","keywords":"Environmental science; Advanced very-high-resolution radiometer; Ice crystals; Arctic; Effective radius; Lidar; Satellite; International Satellite Cloud Climatology Project; Backscatter (email); Meteorology; Remote sensing; Sea ice; Atmospheric sciences; Geology; Cloud cover; Physics; Cloud computing; Oceanography","score_opus":0.007569386078984287,"score_gpt":0.19217293647793632,"score_spread":0.18460355039895204,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2054707521","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":[0.99811006,0.000047493464,0.0012519665,0.00022085116,0.000096414515,0.00021786572,0.000019032519,0.000008672918,0.000027639888],"genre_scores_gemma":[0.99633366,0.000021702632,0.003320991,0.00019991929,0.000029435503,0.000006928153,0.0000037743775,0.000014402846,0.00006920777],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990054,0.00010172999,0.0002542022,0.00023208298,0.00013987388,0.00026672627],"domain_scores_gemma":[0.9993814,0.00008699876,0.00018049368,0.00024205899,0.000022309701,0.00008672478],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008159916,0.00017574095,0.00029463362,2.7316432e-7,0.0004860486,0.000014167057,0.00020153406,0.00011605842,0.00003396616],"category_scores_gemma":[0.000027807679,0.00011133212,0.000060391078,0.00045607943,0.0012545832,0.000066018925,0.00015040589,0.00023324606,0.000001643338],"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":[0.00022227202,0.00041543102,0.7142078,0.00009627154,0.00030460092,0.000015109344,0.0034064648,0.023442443,0.25230658,0.0032354007,0.000045874418,0.0023017004],"study_design_scores_gemma":[0.0004993741,0.00009073254,0.95549166,0.000024391715,0.000094390125,0.000013078462,0.000071291586,0.040005077,0.001757106,0.0016801903,0.00011748036,0.00015521323],"about_ca_topic_score_codex":0.036556315,"about_ca_topic_score_gemma":0.008236818,"teacher_disagreement_score":0.25054947,"about_ca_system_score_codex":0.0001823074,"about_ca_system_score_gemma":0.00011215159,"threshold_uncertainty_score":0.96985936},"labels":[],"label_agreement":null},{"id":"W2055241533","doi":"10.1364/ao.48.004130","title":"Comparison of the relationships between lidar integrated backscattered light and accumulated depolarization ratios for linear and circular polarization for water droplets, fog oil, and dust","year":2009,"lang":"en","type":"article","venue":"Applied Optics","topic":"Atmospheric aerosols and clouds","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":"Defence Research and Development Canada; Royal Military College of Canada","funders":"","keywords":"Lidar; Optics; Scattering; Polarization (electrochemistry); Monte Carlo method; Circular polarization; Mie scattering; Linear polarization; Light scattering; Depolarization ratio; Materials science; Depolarization; Physics; Laser; Chemistry","score_opus":0.024506905520199334,"score_gpt":0.2591526247639945,"score_spread":0.23464571924379515,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2055241533","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":[0.9247491,0.000034563967,0.07392389,0.0006971953,0.000018750516,0.0004217995,0.000013379134,0.000017427283,0.00012390787],"genre_scores_gemma":[0.9848439,0.000010846854,0.0148171475,0.000080018406,0.00002553837,0.00001588222,0.00011888139,0.000014923794,0.000072879324],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992129,0.000024249537,0.00028285166,0.00021949927,0.000106820444,0.0001536633],"domain_scores_gemma":[0.9995977,0.00006778998,0.000115776194,0.0001416017,0.000022204014,0.00005487482],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016044657,0.00012834725,0.00018339265,0.0000033414688,0.00031998,0.00004180896,0.000075936245,0.00015461491,0.0000069618773],"category_scores_gemma":[0.000032146265,0.00008931006,0.00002142278,0.00011779813,0.000081706356,0.000090969486,0.00005181178,0.0001083466,0.0000010993517],"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":[0.00006177823,0.000089375215,0.5538582,0.000065605396,0.000042700336,8.809181e-8,0.0025352999,0.0013698484,0.42661878,0.0015333581,0.00008984343,0.013735093],"study_design_scores_gemma":[0.0031772894,0.00041068636,0.6259748,0.00005389157,0.00048814656,0.000003780801,0.0010995404,0.15687388,0.20454948,0.003825908,0.0028692328,0.0006733655],"about_ca_topic_score_codex":0.000011318009,"about_ca_topic_score_gemma":0.000009393702,"teacher_disagreement_score":0.22206931,"about_ca_system_score_codex":0.000022765082,"about_ca_system_score_gemma":0.000006460585,"threshold_uncertainty_score":0.36419585},"labels":[],"label_agreement":null},{"id":"W2056172598","doi":"10.1175/jas-d-11-0344.1","title":"Modeling Study of Ice Formation in Warm-Based Precipitating Shallow Cumulus Clouds","year":2012,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Chinese Academy of Sciences","keywords":"Ice nucleus; Cloud condensation nuclei; Ice crystals; Atmospheric sciences; Bin; Cloud physics; Condensation; Environmental science; Aerosol; Snow; Indoor bioaerosol; Sea ice growth processes; Meteorology; Nucleation; Physics; Cloud computing; Sea ice; Sea ice thickness; Cryosphere","score_opus":0.027471909932475277,"score_gpt":0.2693942868518787,"score_spread":0.24192237691940344,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2056172598","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":[0.9958177,0.0001439006,0.002625641,0.00015347025,0.00039998407,0.00017292378,1.44796e-7,0.0000046191285,0.0006815902],"genre_scores_gemma":[0.98562187,0.0000063486505,0.014180171,0.0000990511,0.000056068242,0.0000031893558,2.5071904e-8,0.000006206706,0.000027048705],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99792206,0.00016681293,0.0006186947,0.00011617986,0.0008642435,0.00031203157],"domain_scores_gemma":[0.999049,0.000115663,0.0005651735,0.0001643871,0.000026062555,0.00007970781],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018303558,0.00011648573,0.00021220036,0.0000011054786,0.0002112815,0.00002813854,0.0007537108,0.00003551516,0.00014153094],"category_scores_gemma":[0.00019000954,0.00006942518,0.00009243198,0.0009043558,0.00017059325,0.00087043265,0.00016095283,0.00016676287,0.000005629872],"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":[0.000015576226,0.00025931833,0.28429535,0.000003559687,0.0000035383828,6.4889286e-7,0.0038579288,0.70845354,0.0012693494,0.000004509162,0.00001944137,0.0018172391],"study_design_scores_gemma":[0.0005271846,0.0004007076,0.062214855,0.000051978914,0.000022826278,0.000011742602,0.010650889,0.9254595,0.00041047254,0.00011793531,0.000023086315,0.00010883283],"about_ca_topic_score_codex":0.0004622516,"about_ca_topic_score_gemma":0.00013507144,"teacher_disagreement_score":0.22208048,"about_ca_system_score_codex":0.00015149589,"about_ca_system_score_gemma":0.000032185657,"threshold_uncertainty_score":0.28310767},"labels":[],"label_agreement":null},{"id":"W2056370747","doi":"10.1016/j.jaerosci.2005.04.002","title":"Influence of aerosol concentration on precipitation formation in low-level, warm stratiform clouds","year":2005,"lang":"en","type":"article","venue":"Journal of Aerosol Science","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":28,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Natural Sciences and Engineering Research Council of Canada; York University; National Aeronautics and Space Administration","keywords":"Cloud condensation nuclei; Precipitation; Supersaturation; Aerosol; Atmospheric sciences; Environmental science; Chemistry; Meteorology; Geology; Physics","score_opus":0.011905692809647792,"score_gpt":0.24858704693147493,"score_spread":0.23668135412182714,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2056370747","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":[0.9960813,0.000017429998,0.0014790187,0.00036874515,0.00011468587,0.00021640697,0.0000028415325,0.0000071565887,0.001712426],"genre_scores_gemma":[0.99561876,0.000051473082,0.004005349,0.00020807503,0.000063395906,0.000003954309,7.695357e-7,0.0000067510714,0.000041491952],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99730456,0.00004326092,0.00088668044,0.00021555711,0.0011960901,0.0003538618],"domain_scores_gemma":[0.9986082,0.000063473526,0.0008596905,0.00019633763,0.000115064104,0.00015725322],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010090311,0.00015479246,0.00022479557,0.000012225856,0.00015018716,0.00006082603,0.0005430229,0.00007215012,0.00014885642],"category_scores_gemma":[0.00018481852,0.00012597158,0.00006513844,0.0008034767,0.0005303118,0.002861862,0.000068663336,0.00023294278,0.000051490326],"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":[0.00011000353,0.00025426125,0.0072962726,0.000014546063,0.0000029488806,0.000004008566,0.002823278,0.4192609,0.5587002,0.000117012416,0.00016970822,0.011246886],"study_design_scores_gemma":[0.0011970083,0.0010096328,0.0659838,0.00025821425,0.0000119847855,0.000049102513,0.0004840337,0.019780587,0.9107965,0.00011341151,0.000035875742,0.00027984873],"about_ca_topic_score_codex":0.00004796224,"about_ca_topic_score_gemma":0.00012567017,"teacher_disagreement_score":0.39948028,"about_ca_system_score_codex":0.0005709381,"about_ca_system_score_gemma":0.00011614789,"threshold_uncertainty_score":0.5136972},"labels":[],"label_agreement":null},{"id":"W2056498116","doi":"10.1145/2428736.2428744","title":"Developing a hybrid system for sand and dust storm detection using satellite imaging and WSNs","year":2012,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Acadia University","funders":"King Abdulaziz City for Science and Technology; King Fahd University of Petroleum and Minerals","keywords":"Context (archaeology); Storm; Wireless sensor network; Satellite; Computer science; Warning system; Real-time computing; Remote sensing; Scale (ratio); Environmental science; Image resolution; Meteorology; Artificial intelligence; Telecommunications; Engineering; Geography; Computer network; Cartography; Aerospace engineering","score_opus":0.01676459453564171,"score_gpt":0.23152939431000052,"score_spread":0.2147647997743588,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2056498116","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":[0.85733765,0.00038229185,0.14107959,0.000022838947,0.000100622594,0.0001374762,6.780436e-7,0.00002955922,0.0009093093],"genre_scores_gemma":[0.97736245,0.000023559234,0.022410389,0.00005953914,0.000055729222,0.000006721986,3.5788582e-7,0.000010064167,0.00007117735],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994499,0.000009875868,0.00009957418,0.0001460904,0.000069202295,0.00022537627],"domain_scores_gemma":[0.9998019,0.00001985073,0.000038367405,0.00005632912,0.000003413915,0.000080189],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016425639,0.000084504405,0.000081964754,0.0000010506826,0.00021684349,0.000036362897,0.000026539508,0.000018096918,0.000026119205],"category_scores_gemma":[0.000005487389,0.0000709437,0.000013065939,0.000044741115,0.000057493668,0.0002559205,0.00007016919,0.000029139823,0.0000050500107],"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":[0.000015750904,0.000010019556,0.81022394,0.000075337906,0.000009534744,0.0000012065284,0.00056888704,0.000023887307,0.034073077,0.00018862277,0.000017966246,0.15479176],"study_design_scores_gemma":[0.0011565171,0.00005922571,0.8407645,0.000118590855,0.000096882075,0.0005778563,0.0053866715,0.06727247,0.06871962,0.00017276905,0.0147957085,0.0008791656],"about_ca_topic_score_codex":0.00032374318,"about_ca_topic_score_gemma":0.000039179668,"teacher_disagreement_score":0.15391259,"about_ca_system_score_codex":0.00016082253,"about_ca_system_score_gemma":0.000003298478,"threshold_uncertainty_score":0.28930002},"labels":[],"label_agreement":null},{"id":"W2057193063","doi":"10.1139/p07-089","title":"The impact of sea-glint upon limb radiance","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Canadian Space Agency","keywords":"Radiance; Physics; Zenith; Remote sensing; Radiative transfer; Wavelength; Satellite; Spectrograph; Optics; Atmospheric radiative transfer codes; Astronomy; Spectral line; Geology","score_opus":0.008008620679978153,"score_gpt":0.23083822838596443,"score_spread":0.22282960770598628,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2057193063","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":[0.993493,0.00024824118,0.0017059346,0.00011412475,0.00016159692,0.000039616425,0.0000048360025,0.000001186384,0.0042314334],"genre_scores_gemma":[0.9991943,0.000024262103,0.0003687459,0.000050806066,0.00019456766,1.5606588e-7,2.4458532e-7,0.0000087275475,0.00015818293],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992441,0.000016086962,0.0002243831,0.00005919693,0.00015936462,0.00029688483],"domain_scores_gemma":[0.9991071,0.00005183648,0.00022191579,0.00014193071,0.000026000582,0.00045119005],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034213567,0.00007924604,0.000116984265,0.0000011409601,0.00013924082,0.00001924005,0.00028102347,0.000031117626,0.00026022035],"category_scores_gemma":[0.000031135256,0.000051180592,0.00015690173,0.00018243828,0.0001881059,0.00009821643,0.000011667134,0.00015860796,0.000027607814],"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":[0.00007801928,0.000058274116,0.61191005,0.0000053197036,0.00011676744,0.00020306736,0.0015539172,0.02715452,0.00470433,0.0011342515,0.024814473,0.32826698],"study_design_scores_gemma":[0.00044012957,0.000722552,0.97007024,0.00003652347,0.000029506264,0.000092033995,0.00046365245,0.0011854536,0.0049291966,0.00475083,0.017021133,0.00025876818],"about_ca_topic_score_codex":0.01578935,"about_ca_topic_score_gemma":0.023648135,"teacher_disagreement_score":0.35816014,"about_ca_system_score_codex":0.00035726337,"about_ca_system_score_gemma":0.00026373623,"threshold_uncertainty_score":0.99416775},"labels":[],"label_agreement":null},{"id":"W2058004983","doi":"10.5194/acpd-11-7851-2011","title":"Extremely large anthropogenic aerosol component over the Bay of Bengal during winter season","year":2011,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":14,"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","funders":"Indian Space Research Organisation","keywords":"Angstrom exponent; Aerosol; Bay; Dominance (genetics); BENGAL; Environmental science; Atmospheric sciences; Pollution; Climatology; Geography; Oceanography; Meteorology; Geology; Chemistry; Ecology","score_opus":0.01567749492257478,"score_gpt":0.21637787526442287,"score_spread":0.2007003803418481,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2058004983","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":[0.97918,0.000041999738,0.00077757624,0.000043823256,0.00009681665,0.00013911886,0.000003873128,0.000026795855,0.019690027],"genre_scores_gemma":[0.9973442,0.000018454879,0.00063843525,0.00012502572,0.000024376177,0.0000049035943,8.2956325e-7,0.000013723175,0.0018300782],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990253,0.000036537032,0.00018360608,0.0002132029,0.0002568283,0.0002845633],"domain_scores_gemma":[0.999535,0.000013513523,0.00007192025,0.00030661494,0.000004282387,0.000068637666],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000120512675,0.00012534628,0.00012376878,5.615962e-7,0.00017096511,0.000007986884,0.00027544764,0.000043102184,0.05521305],"category_scores_gemma":[0.0000033416259,0.000075979,0.00009829366,0.00008509573,0.00024136246,0.00010598601,0.00023496314,0.00009712231,0.00028364733],"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":[0.00004880787,0.00026500315,0.96416634,0.000006363769,0.000027512138,0.0000060277343,0.0018186002,0.000024999714,0.03221199,0.00023566789,0.00093658647,0.00025208096],"study_design_scores_gemma":[0.00036115616,0.0000544147,0.9672375,0.000006600653,0.000014553659,0.0000046029922,0.00043142823,0.000497835,0.03043581,0.000019838813,0.00080261455,0.00013369968],"about_ca_topic_score_codex":0.0004178961,"about_ca_topic_score_gemma":0.0005381478,"teacher_disagreement_score":0.0549294,"about_ca_system_score_codex":0.000046915015,"about_ca_system_score_gemma":0.0000045970114,"threshold_uncertainty_score":0.94565064},"labels":[],"label_agreement":null},{"id":"W2058379640","doi":"10.1029/2001jd001489","title":"A springtime cloud over the Beaufort Sea polynya: Three‐dimensional simulation with explicit spectral microphysics and comparison with observations","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":34,"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":"National Oceanic and Atmospheric Administration; Universität Hamburg; University of Arizona; University of Utah; National Aeronautics and Space Administration","keywords":"Environmental science; Cloud top; Planetary boundary layer; Lidar; Arctic; Boundary layer; Meteorology; Cloud height; Depth sounding; Atmospheric sciences; Cloud computing; Satellite; Climatology; Geology; Cloud cover; Turbulence; Remote sensing; Geography; Oceanography","score_opus":0.034076499325384854,"score_gpt":0.29523892072452584,"score_spread":0.261162421399141,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2058379640","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":[0.99544203,0.00011500903,0.0031657743,0.00034581748,0.000035329016,0.00025047763,0.0000019619774,0.000008379454,0.00063523644],"genre_scores_gemma":[0.99158233,0.000008400278,0.007768805,0.000091823385,0.00019250826,0.0000066465527,8.3602794e-7,0.000026932497,0.0003217385],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99730194,0.00015407233,0.00032700965,0.00026465315,0.0014470608,0.0005052823],"domain_scores_gemma":[0.99861884,0.0005206505,0.00022195194,0.00026864925,0.00012270869,0.0002471725],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046834783,0.000202476,0.0003016741,0.0000016688095,0.00049344904,0.000116600044,0.00028601981,0.000056401772,0.00037868912],"category_scores_gemma":[0.00007990948,0.000110007924,0.00008312816,0.00057515554,0.00062763126,0.00033910802,0.00012373952,0.0007268922,0.000032651],"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":[0.00083533727,0.00070073584,0.83980346,0.000012572177,0.0001737861,0.000060280905,0.0005118975,0.14509442,0.005581696,0.0034015449,0.0017778303,0.0020464358],"study_design_scores_gemma":[0.0010333876,0.0017190232,0.9444406,0.000059011447,0.00004966123,0.000031736563,0.00033264296,0.04482115,0.0006306611,0.0027393436,0.0039121876,0.00023062009],"about_ca_topic_score_codex":0.0009814531,"about_ca_topic_score_gemma":0.00045506176,"teacher_disagreement_score":0.104637116,"about_ca_system_score_codex":0.00015229326,"about_ca_system_score_gemma":0.000098861885,"threshold_uncertainty_score":0.44859928},"labels":[],"label_agreement":null},{"id":"W2058795591","doi":"10.1256/qj.03.116","title":"Neglect by GCMs of subgrid‐scale horizontal variations in cloud‐droplet effective radius: A diagnostic radiative analysis","year":2004,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":13,"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","funders":"U.S. Department of Energy","keywords":"Radiative transfer; Radiative flux; Atmospheric sciences; RADIUS; Physics; Albedo (alchemy); Environmental science; Computational physics","score_opus":0.0026303356124956823,"score_gpt":0.19615764763174645,"score_spread":0.19352731201925077,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2058795591","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":[0.96960473,0.00022490276,0.028924413,0.0005942466,0.00018048569,0.00028173608,0.00002251863,0.000008225544,0.0001587689],"genre_scores_gemma":[0.9971574,0.000024868803,0.0024962628,0.00018862056,0.00007989075,0.000017373717,0.00000190227,0.000009593391,0.000024098927],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99779356,0.00043917756,0.0006305972,0.00025901193,0.0005199417,0.000357695],"domain_scores_gemma":[0.99825126,0.0007482501,0.0006123193,0.00021072412,0.000028604873,0.00014883617],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00070835574,0.00021815217,0.00060657837,0.000004789736,0.00016319241,0.000024188012,0.0005344119,0.00018662235,0.00044591122],"category_scores_gemma":[0.00018992921,0.00013128971,0.0009895734,0.00097655406,0.00041260678,0.00012011247,0.00007207397,0.00053072354,0.000010398516],"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":[0.00037694463,0.002507072,0.7296912,0.000015798396,0.0021006013,0.0000364606,0.016883895,0.22070156,0.010071326,0.00025772583,0.0033434895,0.0140139265],"study_design_scores_gemma":[0.0022341672,0.004575219,0.98087555,0.000024514527,0.00086912577,0.0000132553105,0.0012525838,0.004708567,0.00073150155,0.004307379,0.00012330434,0.00028481154],"about_ca_topic_score_codex":0.00083287776,"about_ca_topic_score_gemma":0.00016103365,"teacher_disagreement_score":0.25118437,"about_ca_system_score_codex":0.0005023568,"about_ca_system_score_gemma":0.00002832492,"threshold_uncertainty_score":0.5353839},"labels":[],"label_agreement":null},{"id":"W2060285671","doi":"10.1364/ao.41.006307","title":"Multiple-scattering lidar retrieval method: tests on Monte Carlo simulations and comparisons with in situ measurements","year":2002,"lang":"en","type":"article","venue":"Applied Optics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Defence Research and Development Canada","funders":"","keywords":"Lidar; Monte Carlo method; Remote sensing; Scattering; Environmental science; Aerosol; Extinction (optical mineralogy); Mie scattering; Molar absorptivity; Wavelength; Meteorology; Optics; Computational physics; Light scattering; Physics; Statistics; Geology; Mathematics","score_opus":0.03930960218440544,"score_gpt":0.2544976234076426,"score_spread":0.21518802122323716,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060285671","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":[0.9867577,0.000018994326,0.003550708,0.00009629211,0.000018595869,0.00025396282,0.0000027011913,0.000028619812,0.009272438],"genre_scores_gemma":[0.9365337,0.000005217308,0.06315667,0.00016152175,0.00001408356,0.0000072313424,0.0000011306689,0.000017802964,0.00010263613],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990094,0.00001764101,0.00016728598,0.00028136035,0.0002878604,0.00023648121],"domain_scores_gemma":[0.99951977,0.00012231462,0.0000584741,0.00020508331,0.0000049145797,0.000089443805],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000106514155,0.00014844484,0.00016084754,0.0000029316438,0.00014173055,0.000028900025,0.00010282286,0.00005691765,0.00009133224],"category_scores_gemma":[0.00002209155,0.00013015544,0.000014046436,0.00020725015,0.0000887587,0.000050479433,0.00008211788,0.00014999822,0.000047182006],"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":[0.00010951857,0.0002976246,0.531881,0.000008340958,0.000025898546,0.000008885839,0.0018400546,0.4238437,0.03743641,0.000057735506,0.00021130426,0.004279545],"study_design_scores_gemma":[0.0028314434,0.00034532172,0.500291,0.000054500913,0.00006403943,0.0000067392525,0.0007004615,0.48648986,0.007564614,0.000051331655,0.00087788736,0.0007227787],"about_ca_topic_score_codex":0.000068252986,"about_ca_topic_score_gemma":0.0004386586,"teacher_disagreement_score":0.062646165,"about_ca_system_score_codex":0.000095033,"about_ca_system_score_gemma":0.0000023054633,"threshold_uncertainty_score":0.5307585},"labels":[],"label_agreement":null},{"id":"W2060398853","doi":"10.1175/jtech1980.1","title":"Reconstruction of the Sizes of Spherical Particles from Their Shadow Images. Part I: Theoretical Considerations","year":2007,"lang":"en","type":"article","venue":"Journal of Atmospheric and Oceanic Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":172,"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":"Pixel; Position (finance); Binary number; Optics; Monochromatic color; Computer science; Physics; Algorithm; Mathematics","score_opus":0.005032416609419725,"score_gpt":0.1962639849648789,"score_spread":0.19123156835545918,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060398853","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":[0.9924041,0.0006770724,0.004972082,0.0009955397,0.00017936726,0.000077194185,0.0000034677244,0.000013238333,0.0006779603],"genre_scores_gemma":[0.96683156,0.00017946519,0.032843564,0.0000836896,0.000039754937,5.4002527e-7,7.6256235e-8,0.000008610475,0.000012729489],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987948,0.000044350305,0.0006374599,0.00014159449,0.00019010542,0.000191724],"domain_scores_gemma":[0.99889594,0.00022199671,0.0005631431,0.00021261802,0.00004222447,0.00006405928],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00032031178,0.00012047147,0.00032054048,8.8844195e-7,0.00008734642,0.000007460669,0.00020554246,0.00015712701,0.0019138452],"category_scores_gemma":[0.0001946997,0.00007288748,0.000107931126,0.0003059071,0.0021441625,0.00009257552,0.0001483671,0.00025155474,0.000002085316],"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":[0.0001692807,0.00031795038,0.7257171,0.000010366335,0.00015071443,0.00002103051,0.0004991993,0.00014476247,0.07955889,0.028949413,0.0015661507,0.16289513],"study_design_scores_gemma":[0.0015171417,0.0008956229,0.4846169,0.00012241046,0.00020396161,0.00086829683,0.0071475934,0.0014046666,0.17628494,0.32540357,0.0012086869,0.00032620726],"about_ca_topic_score_codex":0.000024798064,"about_ca_topic_score_gemma":0.0000142964445,"teacher_disagreement_score":0.29645416,"about_ca_system_score_codex":0.00003889417,"about_ca_system_score_gemma":0.00003404844,"threshold_uncertainty_score":0.9989985},"labels":[],"label_agreement":null},{"id":"W2060773099","doi":"10.1029/2000jd000233","title":"Lindenberg Aerosol Characterization Experiment 1998 (LACE 98): Overview","year":2002,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":78,"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; Environmental science; Observatory; Meteorology; Troposphere; Radiative transfer; Remote sensing; Atmospheric sciences; Instrumentation (computer programming); Earth's energy budget; Radiation; Geology; Geography; Physics; Computer science","score_opus":0.04803765753735085,"score_gpt":0.3154680743908498,"score_spread":0.26743041685349894,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060773099","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":[0.9915885,0.00087956944,0.00054674887,0.00085253327,0.00018626878,0.00021584424,0.0000020291498,0.000017512075,0.0057110274],"genre_scores_gemma":[0.9873097,0.0011471495,0.0014516166,0.00019096571,0.0005774008,0.000015256455,0.0000016436812,0.000034148947,0.00927214],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.99623,0.00028751165,0.00055720186,0.00031047943,0.0019465246,0.0006682499],"domain_scores_gemma":[0.99863404,0.00019804995,0.00028775714,0.00034924402,0.00008915556,0.00044172382],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0006099148,0.00021565572,0.00038623947,0.0000019223191,0.00028115223,0.00012792996,0.00063749787,0.000111591944,0.012739586],"category_scores_gemma":[0.00017056802,0.00016471506,0.00022958328,0.0006053061,0.00037252455,0.00051956903,0.00035624916,0.0006999846,0.0026024932],"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":[0.000551805,0.004566495,0.02925604,0.00010137325,0.00027018742,0.0004810628,0.00382793,0.0007757784,0.6451438,0.0007912513,0.094280265,0.21995398],"study_design_scores_gemma":[0.0055369814,0.008870565,0.33457896,0.0007737931,0.00014163395,0.00019579627,0.002096439,0.04197141,0.07811063,0.0030424194,0.5226321,0.0020492198],"about_ca_topic_score_codex":0.000263456,"about_ca_topic_score_gemma":0.000020851352,"teacher_disagreement_score":0.5670332,"about_ca_system_score_codex":0.0003273317,"about_ca_system_score_gemma":0.000030605977,"threshold_uncertainty_score":0.9981741},"labels":[],"label_agreement":null},{"id":"W2061025621","doi":"10.1029/2007gl032165","title":"Wildfire smoke injection heights: Two perspectives from space","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":275,"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":"Smoke; Environmental science; Aerosol; Lidar; Troposphere; Atmospheric sciences; Meteorology; Planetary boundary layer; Atmosphere (unit); Plume; Boundary layer; Remote sensing; Geology; Physics","score_opus":0.030585574955269774,"score_gpt":0.2955878523401755,"score_spread":0.2650022773849057,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061025621","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":[0.9861772,0.000049955877,0.00025811544,0.0052193548,0.0000803825,0.00017363767,0.0000036424333,0.00006370551,0.007974002],"genre_scores_gemma":[0.9961911,0.00003813467,0.0007383368,0.0005829648,0.000504855,0.000031755542,0.0000052825912,0.000022403518,0.0018851603],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99734855,0.0001942448,0.00012402843,0.00057940546,0.0011099797,0.00064380356],"domain_scores_gemma":[0.9991565,0.00019081967,0.000032070726,0.00038473276,0.000013252553,0.00022265805],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00015637725,0.00015915054,0.00016338876,0.0000041776984,0.0005958077,0.0000410785,0.00034442396,0.000051085663,0.0020743757],"category_scores_gemma":[0.000081524406,0.00013422707,0.000100468525,0.0005275756,0.0012102142,0.00026877405,0.00030601287,0.0005648049,0.0029289254],"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":[0.00037476252,0.0011760875,0.21208142,0.000007066773,0.00013476891,0.0005704539,0.021116037,0.0009831474,0.4608179,0.0014940354,0.28887028,0.012374038],"study_design_scores_gemma":[0.0010171278,0.0004032404,0.9631389,0.000021448317,0.000011188359,0.000015368067,0.0020506133,0.0016769469,0.0037910894,0.0028070393,0.024503294,0.00056375633],"about_ca_topic_score_codex":0.028729305,"about_ca_topic_score_gemma":0.00010134312,"teacher_disagreement_score":0.75105745,"about_ca_system_score_codex":0.00036572872,"about_ca_system_score_gemma":0.000019977108,"threshold_uncertainty_score":0.9988379},"labels":[],"label_agreement":null},{"id":"W2061051171","doi":"10.1029/2006jd007307","title":"Cloud climatology at the Southern Great Plains and the layer structure, drizzle, and atmospheric modes of continental stratus","year":2007,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"National Aeronautics and Space Administration","keywords":"Drizzle; Cirrus; Climatology; Atmospheric sciences; Environmental science; Cloud top; Cloud base; Middle latitudes; Cloud cover; Geology; Meteorology; Cloud computing; Geography; Precipitation","score_opus":0.015649003408046418,"score_gpt":0.2832300662880202,"score_spread":0.2675810628799738,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061051171","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":[0.9958424,0.0011935123,0.0001835382,0.000589771,0.0000749432,0.00025603067,0.000010678984,0.000005267216,0.0018438884],"genre_scores_gemma":[0.99726593,0.00025853346,0.00092393643,0.000095335214,0.00020273824,0.0000025739414,5.2272674e-7,0.000022484777,0.0012279334],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9971182,0.0003619155,0.00055200193,0.0002613646,0.0010776097,0.0006289618],"domain_scores_gemma":[0.997619,0.0014031524,0.0003436141,0.00029053126,0.00009078079,0.0002529452],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0014869155,0.00021474872,0.00047110693,8.0727983e-7,0.00046900945,0.00006586217,0.0004898495,0.000118930424,0.0008261539],"category_scores_gemma":[0.0002104488,0.00010350829,0.00015340494,0.00033006762,0.0039504548,0.00013626475,0.00063841813,0.0007390516,0.000020508343],"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":[0.013738916,0.00058015337,0.80970246,0.000105299914,0.0006586753,0.00030717519,0.0069273873,0.0014750155,0.0794475,0.012471383,0.010556713,0.06402931],"study_design_scores_gemma":[0.013126861,0.0039936816,0.8711434,0.00016910843,0.0003068696,0.0011020434,0.028567707,0.014999313,0.013965965,0.039716553,0.011984198,0.0009242845],"about_ca_topic_score_codex":0.0015446075,"about_ca_topic_score_gemma":0.0015975125,"teacher_disagreement_score":0.065481536,"about_ca_system_score_codex":0.000091226815,"about_ca_system_score_gemma":0.000038152994,"threshold_uncertainty_score":0.9987602},"labels":[],"label_agreement":null},{"id":"W2061537181","doi":"10.1175/2010jtecha1511.1","title":"Incorporating Ice Crystal Scattering Databases in the Simulation of Millimeter-Wavelength Radar Reflectivity","year":2010,"lang":"en","type":"article","venue":"Journal of Atmospheric and Oceanic Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Research Council Canada","keywords":"Ice crystals; Snow; Environmental science; Radar; Lidar; Precipitation; Remote sensing; Satellite; Backscatter (email); Meteorology; Mie scattering; Graupel; Scattering; Atmospheric sciences; Geology; Light scattering; Optics; Physics","score_opus":0.011291488344894164,"score_gpt":0.2486592246117307,"score_spread":0.23736773626683655,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061537181","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":[0.9895672,0.00008946514,0.009500875,0.00042654693,0.00009139991,0.00008642056,0.0000011325122,0.00001088633,0.00022607995],"genre_scores_gemma":[0.95755607,0.000032496213,0.042276405,0.00008148412,0.000036289206,8.8054617e-7,2.5116367e-7,0.000008976767,0.000007173161],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989955,0.000048228023,0.00042292025,0.0001500502,0.00021331396,0.00017002958],"domain_scores_gemma":[0.9990794,0.00014472535,0.0005132637,0.00021061255,0.00001891496,0.00003305227],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005622987,0.000118268625,0.00023796411,0.0000022608297,0.00008489866,0.000011663761,0.00028904952,0.00008477589,0.000090146204],"category_scores_gemma":[0.000143541,0.00008114987,0.000043688473,0.00049964,0.00035647285,0.00023752575,0.00015978163,0.00048879563,0.000001352116],"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":[0.00010530156,0.00030292955,0.61677563,0.00002949051,0.000035342517,0.00006874038,0.000699212,0.0033679653,0.24153803,0.00049676315,0.00017261086,0.13640797],"study_design_scores_gemma":[0.0022870244,0.0015373074,0.90315723,0.00013205833,0.00012632916,0.0013033358,0.005236408,0.06446418,0.008268606,0.008035702,0.004805671,0.0006461169],"about_ca_topic_score_codex":0.000062467465,"about_ca_topic_score_gemma":0.00009307163,"teacher_disagreement_score":0.28638163,"about_ca_system_score_codex":0.00003328648,"about_ca_system_score_gemma":0.000021205227,"threshold_uncertainty_score":0.33091956},"labels":[],"label_agreement":null},{"id":"W2061899543","doi":"10.1175/2010jas3447.1","title":"Improvement and Implementation of a Parameterization for Shallow Cumulus in the Global Climate Model ECHAM5-HAM","year":2011,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":12,"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":"Convection; Context (archaeology); Environmental science; Atmospheric sciences; Climatology; Precipitation; Meteorology; Climate model; Geology; Climate change; Physics","score_opus":0.02458437491686562,"score_gpt":0.2799998589479925,"score_spread":0.2554154840311269,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061899543","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":[0.99554735,0.000045236582,0.003325262,0.00029185737,0.00010972209,0.00025036366,0.000002886675,0.0000017394269,0.00042556404],"genre_scores_gemma":[0.9681548,0.000053657408,0.031490378,0.00027199762,0.000011805226,0.000008928476,6.8212785e-8,0.0000026473022,0.000005704748],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989326,0.000040837316,0.00035540422,0.000121352175,0.0003623595,0.00018743849],"domain_scores_gemma":[0.99935365,0.000029213137,0.00046511108,0.000106727406,0.000015322243,0.000029955761],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001000112,0.00008056407,0.00011999116,3.9393254e-7,0.00015127778,0.000026628462,0.0004931822,0.000023096805,0.000068185116],"category_scores_gemma":[0.000019046776,0.000040636118,0.00006797267,0.00035216557,0.00027062075,0.00025590337,0.000119282544,0.000044073036,4.5436622e-7],"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":[0.00009999668,0.00020174625,0.9042187,0.000025689656,0.000020216645,0.0000012960063,0.006604424,0.047172595,0.009002811,0.0027032127,0.00015618837,0.029793147],"study_design_scores_gemma":[0.0010546466,0.0015914647,0.55786616,0.000039178,0.00006988263,0.00003340822,0.014056292,0.39491493,0.002248951,0.027879123,0.00005272237,0.0001932691],"about_ca_topic_score_codex":0.00030108396,"about_ca_topic_score_gemma":0.00018488383,"teacher_disagreement_score":0.34774232,"about_ca_system_score_codex":0.00006809238,"about_ca_system_score_gemma":0.000034305453,"threshold_uncertainty_score":0.16570929},"labels":[],"label_agreement":null},{"id":"W2062644486","doi":"10.1029/2005jd006766","title":"Laboratory studies of ice formation via deposition mode nucleation onto mineral dust and n‐hexane soot samples","year":2006,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":136,"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 Toronto","funders":"","keywords":"Ice nucleus; Soot; Mineral dust; Deposition (geology); Relative humidity; Cirrus; Nucleation; Mineralogy; Materials science; Aerosol; Mineral; Analytical Chemistry (journal); Chemistry; Environmental chemistry; Atmospheric sciences; Geology; Meteorology; Combustion; Geomorphology; Metallurgy","score_opus":0.026947417051484627,"score_gpt":0.3119625664386823,"score_spread":0.2850151493871977,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2062644486","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":[0.99457085,0.00054471125,0.0039391094,0.00026809552,0.000037910668,0.00011669174,0.000004328858,0.00000686605,0.00051145663],"genre_scores_gemma":[0.99077153,0.00017527658,0.008584145,0.000024416373,0.00021576908,0.000004299031,0.0000022775855,0.000012064306,0.00021021826],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99798673,0.0001894499,0.0004439576,0.00014555747,0.0009507142,0.00028359515],"domain_scores_gemma":[0.9989354,0.00030665976,0.000274671,0.000120684956,0.00024885425,0.00011370295],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00050549005,0.00012040643,0.00026506465,0.0000024938995,0.0001939007,0.000040649848,0.00016117442,0.0000652601,0.000109592016],"category_scores_gemma":[0.00018926017,0.000092732975,0.00006980618,0.00031757526,0.00044221204,0.0006779551,0.00012936344,0.00027076562,0.000016611875],"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":[0.00062391534,0.00075887545,0.047417875,0.00014799369,0.00009681387,0.000032514276,0.0013276852,0.008107663,0.8985483,0.0010424805,0.011972927,0.029922932],"study_design_scores_gemma":[0.0017837164,0.0026834805,0.8965365,0.00025971953,0.000084443025,0.00003394549,0.0038642327,0.03255227,0.043121997,0.016621333,0.0020495339,0.0004087905],"about_ca_topic_score_codex":0.002980622,"about_ca_topic_score_gemma":0.0009049177,"teacher_disagreement_score":0.8554263,"about_ca_system_score_codex":0.00022161084,"about_ca_system_score_gemma":0.00002882736,"threshold_uncertainty_score":0.45058286},"labels":[],"label_agreement":null},{"id":"W2063728222","doi":"10.1029/2008jd010927","title":"Study of polar thin ice clouds and aerosols seen by CloudSat and CALIPSO during midwinter 2007","year":2009,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":51,"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 du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Lidar; Aerosol; Effective radius; Environmental science; Ice crystals; Atmospheric sciences; Polar; Arctic; Satellite; Meteorology; Climatology; Remote sensing; Geology; Physics; Oceanography; Astrophysics; Astronomy","score_opus":0.017049748173332713,"score_gpt":0.2980908407596232,"score_spread":0.2810410925862905,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2063728222","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":[0.99760896,0.00067501457,0.000036656464,0.0004434493,0.000052264244,0.00026651166,0.000004523595,0.000008134035,0.0009045128],"genre_scores_gemma":[0.99771154,0.00019111659,0.0005488162,0.00008070034,0.00019074704,0.0000022926217,3.396848e-7,0.000018701186,0.0012557494],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99679923,0.00033402612,0.00056953577,0.00034292077,0.0013765503,0.00057772116],"domain_scores_gemma":[0.9986647,0.00026963776,0.00024897268,0.0002710252,0.00009287556,0.00045282862],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00092032977,0.0002221481,0.0004858453,0.0000021855242,0.000263907,0.00008953355,0.00043591397,0.00010211728,0.0004428971],"category_scores_gemma":[0.00020083356,0.00016632746,0.00009640849,0.00034256218,0.0005029765,0.0003600245,0.00037855445,0.0008052641,0.000024606892],"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":[0.0033734436,0.00749336,0.72594637,0.00011859216,0.00044486125,0.00068177946,0.010596867,0.00086003524,0.17143002,0.00021072075,0.053518213,0.025325734],"study_design_scores_gemma":[0.0028302695,0.0076869926,0.9766655,0.00010849369,0.000049479735,0.00008381556,0.005618997,0.00061467034,0.0027342832,0.0015639288,0.001687282,0.00035629305],"about_ca_topic_score_codex":0.0013988463,"about_ca_topic_score_gemma":0.000078097444,"teacher_disagreement_score":0.25071913,"about_ca_system_score_codex":0.00011162258,"about_ca_system_score_gemma":0.00002855181,"threshold_uncertainty_score":0.67826366},"labels":[],"label_agreement":null},{"id":"W2064262287","doi":"10.1175/2010jcli3449.1","title":"Vertical Velocity Statistics in Fair-Weather Cumuli at the ARM TWP Nauru Climate Research Facility","year":2010,"lang":"en","type":"article","venue":"Journal of Climate","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"U.S. Department of Energy","keywords":"Environmental science; Cloud fraction; Diurnal cycle; Climatology; Boundary layer; Westerlies; Cloud computing; Meteorology; Atmospheric sciences; Cloud cover; Geology; Geography","score_opus":0.02523702625618044,"score_gpt":0.3207083665026981,"score_spread":0.2954713402465176,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2064262287","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":[0.99171877,0.000028814286,0.00027877366,0.0008658706,0.00025271866,0.000116217656,0.00004511337,0.000006311369,0.006687428],"genre_scores_gemma":[0.99669975,0.00038730356,0.002444619,0.00015952968,0.000070935785,0.0000036028543,0.0000017974434,0.000011874457,0.00022061449],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9975202,0.00020473845,0.00055326655,0.00019567274,0.000889818,0.00063632295],"domain_scores_gemma":[0.99900055,0.0003259645,0.00013602179,0.00030128474,0.00004876025,0.0001874394],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0031404435,0.00013450906,0.00024054211,0.000004161633,0.00031304194,0.000057015135,0.00042723073,0.00010808743,0.0069926144],"category_scores_gemma":[0.0002861129,0.00008334306,0.000085359185,0.00022687735,0.00066316593,0.00015787892,0.0004612992,0.0010937011,0.0007734217],"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":[0.0006145285,0.00068940804,0.9303357,0.000036740716,0.000026297374,0.00021613229,0.0018020498,0.0007954201,0.016436102,0.0009218204,0.00779206,0.040333763],"study_design_scores_gemma":[0.0011446106,0.0004274469,0.9521633,0.000027734155,0.000027995899,0.00015041593,0.00069351814,0.0038552566,0.0014500616,0.0029613737,0.03681896,0.00027932454],"about_ca_topic_score_codex":0.00012392836,"about_ca_topic_score_gemma":0.0010896206,"teacher_disagreement_score":0.04005444,"about_ca_system_score_codex":0.00023497635,"about_ca_system_score_gemma":0.00003056347,"threshold_uncertainty_score":0.99410295},"labels":[],"label_agreement":null},{"id":"W2064766834","doi":"10.1256/qj.02.149","title":"Solar radiative transfer for stratiform clouds with horizontal variations in liquid‐water path and droplet effective radius","year":2003,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","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":"Dalhousie University","funders":"","keywords":"Liquid water path; Radiative transfer; Effective radius; Environmental science; Liquid water content; Albedo (alchemy); Atmospheric sciences; Cloud albedo; RADIUS; Radiation; Horizontal plane; Meteorology; Atmospheric radiative transfer codes; Physics; Cloud computing; Geology; Cloud cover; Optics; Astrophysics; Geodesy","score_opus":0.004264249517127416,"score_gpt":0.19062658103187677,"score_spread":0.18636233151474935,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2064766834","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":[0.9371349,0.00005291306,0.061696336,0.0003202309,0.00009746383,0.00046352108,0.000007706661,0.0000057512952,0.00022116922],"genre_scores_gemma":[0.9928539,0.000006396153,0.0067963977,0.0002177979,0.000046779354,0.000034528926,6.4350104e-7,0.00001112038,0.000032478172],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99859977,0.000258432,0.000329793,0.00020630864,0.0002616632,0.00034402884],"domain_scores_gemma":[0.99947,0.0001833535,0.00010358003,0.00010590164,0.000019335064,0.000117823045],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008465208,0.00018859097,0.00031278774,0.0000013643348,0.00023574547,0.000036178557,0.00019148586,0.00014622987,0.00022096108],"category_scores_gemma":[0.000021698765,0.00008746816,0.00026301623,0.00009851081,0.00026927228,0.00013602508,0.000015618789,0.00036991853,0.000002394047],"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":[0.015434002,0.0074063092,0.46449992,0.00022531168,0.0038765944,0.00022917375,0.2030743,0.04148714,0.10283762,0.022736205,0.0045044096,0.13368902],"study_design_scores_gemma":[0.026806619,0.1369637,0.72482896,0.00015067309,0.0012645721,0.00045698418,0.01557989,0.028510777,0.01643924,0.039554544,0.0070392354,0.0024048002],"about_ca_topic_score_codex":0.000036189605,"about_ca_topic_score_gemma":0.00003384668,"teacher_disagreement_score":0.26032904,"about_ca_system_score_codex":0.00016238316,"about_ca_system_score_gemma":0.000019227427,"threshold_uncertainty_score":0.3566848},"labels":[],"label_agreement":null},{"id":"W2064835592","doi":"10.1175/jtech-d-13-00115.1","title":"Quantification of the Effects of Shattering on Airborne Ice Particle Measurements","year":2013,"lang":"en","type":"article","venue":"Journal of Atmospheric and Oceanic Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":121,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"National Oceanic and Atmospheric Administration; Transport Canada; Federal Aviation Administration; National Aeronautics and Space Administration","keywords":"Instrumentation (computer programming); Particle (ecology); Spectrometer; Remote sensing; Environmental science; Ice crystals; Characterization (materials science); Materials science; Optics; Physics; Geology; Computer science","score_opus":0.00756027944695367,"score_gpt":0.20116568821282096,"score_spread":0.1936054087658673,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2064835592","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":[0.9975045,0.00029931805,0.0011777364,0.00058942207,0.0001304585,0.00013163697,1.2603357e-7,0.000007950819,0.00015888718],"genre_scores_gemma":[0.9975923,0.000068434776,0.002176111,0.000077305165,0.000009749343,0.000002290972,1.9235719e-8,0.000007448623,0.00006634977],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99915135,0.000029754345,0.00034760643,0.000103883496,0.00023190708,0.0001355039],"domain_scores_gemma":[0.9992012,0.00004262571,0.00048432275,0.00020447887,0.00003146104,0.000035936508],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014591585,0.000086320135,0.00019515515,6.643813e-7,0.000047530757,0.0000051460083,0.00026796322,0.00007733059,0.00015911798],"category_scores_gemma":[0.0001050786,0.00005445508,0.000054654156,0.0002991883,0.00025287457,0.00009235737,0.00010276102,0.00013102312,0.000009699483],"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":[0.000032245807,0.00023477837,0.4482034,0.00005481521,0.000056882018,0.0000020086143,0.00021569093,0.00036863697,0.4768644,0.00043981467,0.00075791345,0.0727694],"study_design_scores_gemma":[0.00053920865,0.00068849296,0.84754026,0.0001035898,0.000044157943,0.000023904642,0.00030616412,0.0008481512,0.14882323,0.00075738353,0.00023910616,0.00008635539],"about_ca_topic_score_codex":0.000027741815,"about_ca_topic_score_gemma":0.0000017170848,"teacher_disagreement_score":0.39933684,"about_ca_system_score_codex":0.000039760274,"about_ca_system_score_gemma":0.000009721026,"threshold_uncertainty_score":0.22206137},"labels":[],"label_agreement":null},{"id":"W2065148465","doi":"10.1063/1.2175958","title":"Development and characterization of a laminar aerosol flow tube","year":2006,"lang":"en","type":"article","venue":"Review of Scientific Instruments","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":14,"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 Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada; University of Waterloo","keywords":"Laminar flow; Aerosol; Turbulence; Mechanics; Reynolds number; Laminar flow reactor; Buoyancy; Materials science; Stratosphere; Mixing (physics); Meteorology; Flow (mathematics); Physics; Open-channel flow","score_opus":0.008197096325103686,"score_gpt":0.20798109441692525,"score_spread":0.19978399809182157,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2065148465","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":[0.99723786,0.00028562234,0.000058841957,0.0000320759,0.00014161969,0.0002566357,0.000008180822,0.0000069660127,0.0019721773],"genre_scores_gemma":[0.98753893,0.00077983266,0.010125914,0.00005742945,0.000008704712,0.000013815514,0.00005790655,0.0000071988584,0.0014102431],"study_design_codex":"design_other","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9987634,0.000021304844,0.0004308748,0.00024416638,0.0003886854,0.00015160564],"domain_scores_gemma":[0.99952227,0.0000033530018,0.00023265947,0.0001852335,0.000017314895,0.00003919243],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000366447,0.00010027681,0.00020811407,0.0000028798152,0.00010429857,0.000016189204,0.00014240337,0.000027540475,0.00065639906],"category_scores_gemma":[0.0000073448628,0.000083393454,0.000035266155,0.00030338,0.00026693475,0.00014700828,0.00013647831,0.000030403615,0.00005146589],"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":[0.000005197952,0.00021404507,0.04675461,0.0019419384,0.00001118828,9.925157e-7,0.00021372693,0.0000017816751,0.3291556,0.00010979222,0.00051158044,0.62107956],"study_design_scores_gemma":[0.00092538015,0.00011946222,0.41172567,0.0077019287,0.00009062824,0.00001784522,0.000072327275,0.0016783054,0.42223454,0.00007702764,0.15467998,0.00067689863],"about_ca_topic_score_codex":0.000018360231,"about_ca_topic_score_gemma":0.0000050978397,"teacher_disagreement_score":0.62040263,"about_ca_system_score_codex":0.000043399115,"about_ca_system_score_gemma":0.00001889098,"threshold_uncertainty_score":0.71871096},"labels":[],"label_agreement":null},{"id":"W2065209900","doi":"10.1029/2001jd000767","title":"First interactive simulations of cirrus clouds formed by homogeneous freezing in the ECHAM general circulation model","year":2002,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":183,"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","funders":"","keywords":"Cirrus; Atmospheric sciences; Ice crystals; Ice nucleus; Troposphere; Aerosol; Environmental science; Relative humidity; Tropopause; Liquid water content; Cloud physics; Climatology; Orographic lift; Sea ice growth processes; Homogeneous; Ice cloud; Nucleation; Meteorology; Radiative transfer; Chemistry; Cryosphere; Geology; Precipitation; Sea ice thickness; Thermodynamics; Physics; Sea ice","score_opus":0.03598270405373415,"score_gpt":0.3033451628227578,"score_spread":0.26736245876902365,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2065209900","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":[0.99288285,0.00015809451,0.004445142,0.00051726465,0.00003891669,0.00020590036,0.000007786398,0.0000041368507,0.0017398822],"genre_scores_gemma":[0.997439,0.000075403834,0.0019176058,0.00006026028,0.00012024215,0.000007253811,0.0000012086309,0.000016170046,0.00036284185],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9973749,0.0002203205,0.0005092423,0.00019200737,0.0012742837,0.0004292646],"domain_scores_gemma":[0.99858433,0.0006806775,0.000256144,0.000252416,0.00009935928,0.00012706858],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00054789375,0.00014034033,0.0002623627,0.0000030810272,0.00022404605,0.00005084662,0.00056795,0.00007978702,0.0008810743],"category_scores_gemma":[0.00031831497,0.00009691045,0.00016031213,0.0006072515,0.00031066706,0.00035714955,0.00015381395,0.00062416797,0.000034943343],"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":[0.00017264052,0.0012972166,0.023257071,0.000018136148,0.000060158243,0.0000462622,0.0043253694,0.9227215,0.025009701,0.0003605394,0.009662411,0.013068982],"study_design_scores_gemma":[0.000568631,0.0004142037,0.029629407,0.00004082247,0.00001303017,0.000013848706,0.00054838066,0.9595529,0.000505753,0.008068627,0.000517999,0.00012640402],"about_ca_topic_score_codex":0.0010617187,"about_ca_topic_score_gemma":0.00038103267,"teacher_disagreement_score":0.036831383,"about_ca_system_score_codex":0.0002793828,"about_ca_system_score_gemma":0.000028183695,"threshold_uncertainty_score":0.9647146},"labels":[],"label_agreement":null},{"id":"W2065516120","doi":"10.1002/joc.642","title":"Ice crystal number concentration versus temperature for climate studies","year":2001,"lang":"en","type":"article","venue":"International Journal of Climatology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":59,"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":"National Research Council Canada; National Aeronautics and Space Administration","keywords":"Ice crystals; Atmospheric sciences; Precipitation; Environmental science; Atmosphere (unit); Climatology; Latitude; Meteorology; Geology; Physics","score_opus":0.021457221177561124,"score_gpt":0.3336944031618951,"score_spread":0.312237181984334,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2065516120","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":[0.99019474,0.00014952115,0.0005688169,0.0024545114,0.0025763763,0.000069701746,0.0000075539697,0.000008202861,0.003970591],"genre_scores_gemma":[0.99561393,0.000880115,0.0026299765,0.00044594033,0.00029045632,0.000004889962,0.000004773525,0.000008345083,0.00012158764],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99901974,0.00003153125,0.00037231663,0.0001132733,0.00027501798,0.00018811013],"domain_scores_gemma":[0.9992517,0.00017912785,0.0003193708,0.00005700995,0.0001401894,0.00005256168],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00018635154,0.000093554445,0.00018843755,0.0000016240607,0.000068751244,0.00002553658,0.00025230862,0.00006888699,0.0009170787],"category_scores_gemma":[0.00013860056,0.000075242504,0.00010295756,0.00005203242,0.00013853109,0.00023663239,0.00007350203,0.000111450434,0.000064214895],"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":[0.005965562,0.0003703069,0.92479885,0.000021786389,0.00082068465,0.00048235996,0.0016158547,0.001971463,0.0153861,0.008839399,0.033638388,0.006089252],"study_design_scores_gemma":[0.03498779,0.0028975636,0.1528917,0.00028492277,0.0005579681,0.014127126,0.012119825,0.0036093823,0.0075049424,0.013729688,0.7556487,0.0016404189],"about_ca_topic_score_codex":0.0000046607774,"about_ca_topic_score_gemma":0.00001979872,"teacher_disagreement_score":0.77190715,"about_ca_system_score_codex":0.00013308742,"about_ca_system_score_gemma":0.000016242257,"threshold_uncertainty_score":0.99999624},"labels":[],"label_agreement":null},{"id":"W2065950667","doi":"10.5539/mas.v3n10p17","title":"Two-dimensional Simulation of Aerosol?Cloud Profile","year":2009,"lang":"en","type":"article","venue":"Modern Applied Science","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Universiti Sains Malaysia","keywords":"Aerosol; Remote sensing; Altitude (triangle); Environmental science; Meteorology; Cloud computing; Computer science; Software; Pixel; Atmosphere (unit); Lidar; Stability (learning theory); Atmospheric sciences; Geology; Geography; Mathematics; Computer vision","score_opus":0.009813591375438618,"score_gpt":0.24179419324006485,"score_spread":0.23198060186462624,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2065950667","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":[0.91302925,0.000008888656,0.03516152,0.00008666984,0.00006870113,0.00022436873,0.0000017146704,0.00004451066,0.05137436],"genre_scores_gemma":[0.9899027,3.0138577e-7,0.00941849,0.00032918545,0.000030757932,0.0000060981047,0.0000013478385,0.000005872971,0.0003052935],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99824286,0.000007720913,0.00020963096,0.00043301113,0.0007764861,0.00033029114],"domain_scores_gemma":[0.9994324,0.000023201912,0.00010720837,0.00030474507,0.000014718342,0.00011774935],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032627204,0.0001220921,0.00013293825,0.0000029869898,0.00023904363,0.0000235754,0.00039391906,0.000035644058,0.00074494013],"category_scores_gemma":[0.000014323303,0.00010487405,0.000032607335,0.0005103251,0.0006137711,0.00017897194,0.00014534962,0.00008147369,0.00021031646],"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":[0.00001381681,0.000058103946,0.00037234792,7.692413e-7,5.3431063e-7,4.4908168e-7,0.00024258265,0.3871519,0.6018521,0.00030891132,0.00007938574,0.009919099],"study_design_scores_gemma":[0.0002870052,0.00006379492,0.009714928,0.000004065404,0.0000042681622,0.0000012711071,0.000024926498,0.9353665,0.050587866,0.0037220025,0.000048255155,0.0001751236],"about_ca_topic_score_codex":0.000027792039,"about_ca_topic_score_gemma":0.000003671719,"teacher_disagreement_score":0.5512642,"about_ca_system_score_codex":0.00009240589,"about_ca_system_score_gemma":0.00003157991,"threshold_uncertainty_score":0.8156572},"labels":[],"label_agreement":null},{"id":"W2066991212","doi":"10.1029/2003jd003898","title":"Smoke over haze: Aircraft observations of chemical and optical properties and the effects on heating rates and stability","year":2004,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":61,"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; Environmental science; Plume; Aerosol; Planetary boundary layer; Radiative transfer; Atmosphere (unit); Radiative forcing; Atmospheric instability; Haze; Subsidence; Forcing (mathematics); Meteorology; Wind speed; Geology; Physics; Optics; Turbulence","score_opus":0.04023729203048553,"score_gpt":0.2910098589966852,"score_spread":0.25077256696619965,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2066991212","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":[0.997297,0.00036537863,0.000022273167,0.0019333817,0.00001711001,0.00021303879,7.122758e-7,0.0000035272337,0.00014758679],"genre_scores_gemma":[0.99800175,0.0001066386,0.0017019468,0.00007195756,0.00007257157,0.000007791766,9.394155e-8,0.0000087960125,0.000028470888],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99838775,0.00016673637,0.00028400248,0.00018700554,0.00070634787,0.00026816144],"domain_scores_gemma":[0.9985147,0.0009888168,0.00011031093,0.00014012244,0.00006185682,0.00018417992],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007942514,0.00011705784,0.00028516023,8.260312e-7,0.00017496181,0.000063971915,0.00014324563,0.00005522536,0.000040405466],"category_scores_gemma":[0.0016443882,0.00006313657,0.000057203004,0.00017163852,0.0020331512,0.00018329383,0.000282991,0.0004773554,0.0000017126114],"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":[0.00254792,0.00083902414,0.35679802,0.00029820745,0.00013538272,0.00003206017,0.0029032596,0.00027869403,0.6030505,0.006466338,0.00027444228,0.026376195],"study_design_scores_gemma":[0.0019817203,0.0010985353,0.93333614,0.0001772071,0.000022026672,0.000011904735,0.00044472693,0.0011013608,0.05067319,0.011013189,0.000036490164,0.000103492],"about_ca_topic_score_codex":0.0010934562,"about_ca_topic_score_gemma":0.000024292114,"teacher_disagreement_score":0.57653815,"about_ca_system_score_codex":0.000069550915,"about_ca_system_score_gemma":0.00004492076,"threshold_uncertainty_score":0.74912304},"labels":[],"label_agreement":null},{"id":"W2068196980","doi":"10.1175/2010jtecha1463.1","title":"Observational Studies of Atmospheric Aerosols over Bozeman, Montana, Using a Two-Color Lidar, a Water Vapor DIAL, a Solar Radiometer, and a Ground-Based Nephelometer over a 24-h Period","year":2010,"lang":"en","type":"article","venue":"Journal of Atmospheric and Oceanic Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":6,"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":"Office of Experimental Program to Stimulate Competitive Research; National Aeronautics and Space Administration","keywords":"Nephelometer; Lidar; Aerosol; Environmental science; AERONET; Sun photometer; Radiometer; Remote sensing; Optical depth; Atmospheric sciences; Meteorology; Geology; Physics; Light scattering; Scattering; Optics","score_opus":0.021924347754194006,"score_gpt":0.268026367661943,"score_spread":0.246102019907749,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2068196980","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":[0.9945035,0.0017441595,0.0023896047,0.00053737056,0.00045097986,0.00030308324,0.0000047857043,0.000041480587,0.000025063056],"genre_scores_gemma":[0.8938337,0.00022131726,0.10532097,0.00035490404,0.000098103366,0.000011522059,8.045243e-7,0.000047000034,0.00011167699],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9972937,0.000064794025,0.0010136832,0.0004880217,0.000532087,0.00060773204],"domain_scores_gemma":[0.9984169,0.00012478094,0.0007839055,0.0003738356,0.00010461304,0.00019593655],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0005315498,0.0004491073,0.0009983716,0.0000051828847,0.000284292,0.000066332184,0.0004155091,0.0003568269,0.000831263],"category_scores_gemma":[0.00015412031,0.0003177764,0.00021921413,0.00074538984,0.0013018368,0.0004925785,0.0004277092,0.00067105115,0.0000043993437],"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":[0.0007779114,0.0007522959,0.54630697,0.00015809097,0.0008204437,0.0004299097,0.0019365954,0.0008073068,0.4288467,0.00036630713,0.0008905921,0.017906895],"study_design_scores_gemma":[0.025377344,0.01043603,0.78017694,0.0005946412,0.0022369383,0.0067847343,0.0066552204,0.1166816,0.018526906,0.0104672145,0.018268963,0.0037934443],"about_ca_topic_score_codex":0.00013005063,"about_ca_topic_score_gemma":0.00006770692,"teacher_disagreement_score":0.4103198,"about_ca_system_score_codex":0.00018489637,"about_ca_system_score_gemma":0.00009249114,"threshold_uncertainty_score":0.9999274},"labels":[],"label_agreement":null},{"id":"W2068241548","doi":"10.5194/acp-13-2907-2013","title":"Observationally-constrained estimates of global fine-mode AOD","year":2013,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":48,"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":"Korea Meteorological Administration; National Aeronautics and Space Administration","keywords":"AERONET; Environmental science; Aerosol; Satellite; Angstrom exponent; Climatology; Atmospheric sciences; Meteorology; Geography","score_opus":0.005665397590862264,"score_gpt":0.21388087743954498,"score_spread":0.20821547984868272,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2068241548","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":[0.9744864,0.000041944284,0.0041975253,0.00011330804,0.00001589188,0.00008047528,0.000009884178,0.00002667295,0.021027898],"genre_scores_gemma":[0.93909353,0.000008170721,0.059804812,0.00008860702,0.000046097368,0.000015944708,0.000013247349,0.000007483735,0.0009220973],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992696,0.000004615791,0.00017153216,0.00021625769,0.00016082045,0.00017714588],"domain_scores_gemma":[0.9996129,0.000033982516,0.000081743725,0.00016815118,0.000015167203,0.00008802345],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000023432709,0.00014716142,0.00015852664,1.9158404e-9,0.00006429614,0.000018110846,0.00013520897,0.000060825463,0.0067831553],"category_scores_gemma":[0.00001284516,0.00013403108,0.000048335256,0.00015783882,0.00027138903,0.00013902105,0.000078545134,0.00005846622,0.00007170611],"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":[0.000013145109,0.00020542854,0.6832324,0.00008242571,0.0000494082,0.0000019840163,0.00012531303,0.004271907,0.071427904,0.0007398173,0.0025486667,0.23730156],"study_design_scores_gemma":[0.0009827171,0.000076680975,0.71872556,0.00004584769,0.00006943041,0.000019535553,0.00018363979,0.20220602,0.019903282,0.055648662,0.0013900191,0.00074863044],"about_ca_topic_score_codex":0.000550715,"about_ca_topic_score_gemma":0.0000037413267,"teacher_disagreement_score":0.23655294,"about_ca_system_score_codex":0.00004112591,"about_ca_system_score_gemma":0.000016394522,"threshold_uncertainty_score":0.99412477},"labels":[],"label_agreement":null},{"id":"W2068259205","doi":"10.1364/ao.45.006839","title":"Information content of data measured with a multiple-field-of-view lidar","year":2006,"lang":"en","type":"article","venue":"Applied Optics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Defence Research and Development Canada","funders":"","keywords":"Lidar; Depth sounding; Remote sensing; Scattering; Optics; Range (aeronautics); Computer science; Physics; Geology; Materials science","score_opus":0.02396083505879136,"score_gpt":0.22197298481552408,"score_spread":0.1980121497567327,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2068259205","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":[0.9078541,0.000037726408,0.047338482,0.00006546778,0.000024701145,0.00034309152,0.000019170046,0.000020572768,0.0442967],"genre_scores_gemma":[0.96511674,0.000013537801,0.034700777,0.000080158134,0.000009445704,0.0000065366708,0.000029845092,0.0000049611613,0.00003799482],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999289,0.0000045875527,0.00024733946,0.00008620413,0.00026375853,0.00010913495],"domain_scores_gemma":[0.9993842,0.00003442339,0.00016225477,0.0003799111,0.000012681612,0.000026527377],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000111790985,0.00007766612,0.00013355145,9.229665e-7,0.00002662332,0.00000727044,0.00025661578,0.000041905194,0.00008447636],"category_scores_gemma":[0.000012146983,0.000058968733,0.00001407855,0.000114855255,0.00008756864,0.00017263659,0.00014928976,0.000049025093,0.000031588686],"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":[0.0009579974,0.0012130942,0.4941049,0.0004555461,0.00020123723,0.000005272496,0.0029297688,0.02575205,0.15140398,0.033172898,0.00705402,0.28274924],"study_design_scores_gemma":[0.010362915,0.0014656433,0.7021881,0.00025776649,0.00050963584,0.000022996066,0.0064426837,0.041828487,0.16151567,0.0016116817,0.071811974,0.0019824645],"about_ca_topic_score_codex":0.00046239438,"about_ca_topic_score_gemma":0.000088369416,"teacher_disagreement_score":0.2807668,"about_ca_system_score_codex":0.000016146954,"about_ca_system_score_gemma":0.000010323739,"threshold_uncertainty_score":0.24046752},"labels":[],"label_agreement":null},{"id":"W2069018481","doi":"10.1002/met.175","title":"A seasonal forecast scheme for spring dust storm predictions in Northern China","year":2010,"lang":"en","type":"article","venue":"Meteorological Applications","topic":"Atmospheric aerosols and clouds","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":"Environment and Climate Change Canada","funders":"National Natural Science Foundation of China","keywords":"Climatology; Storm; Dust storm; Environmental science; Empirical orthogonal functions; Precipitation; Meteorology; Forecast skill; Geography; Geology","score_opus":0.010574394016427175,"score_gpt":0.22959321793037465,"score_spread":0.21901882391394747,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2069018481","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":[0.91387075,0.000010103114,0.08066679,0.00071303826,0.000040558287,0.00066497293,0.000019205689,0.00007292483,0.0039416254],"genre_scores_gemma":[0.95420533,0.0000023305447,0.043387417,0.00011436932,0.00009834198,0.0019471435,0.000011307415,0.000011117958,0.00022265724],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990569,0.000011207787,0.00018017807,0.000337415,0.00013507195,0.00027926738],"domain_scores_gemma":[0.99951273,0.00005999302,0.000055318156,0.0002463221,0.000008328583,0.0001173173],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00018880419,0.00011488009,0.00012059702,0.0000020763816,0.00023358146,0.000017675176,0.0002593385,0.00012307585,0.0010648486],"category_scores_gemma":[0.000041829528,0.000093275725,0.000071511444,0.0002486788,0.00019265177,0.00007081183,0.00012101666,0.00026845373,0.00017300314],"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":[0.000016510669,0.00028411223,0.95963657,0.0000027998801,0.000006404739,5.254238e-7,0.000051857744,0.0005624466,0.011453575,0.0052893995,0.00016152367,0.022534266],"study_design_scores_gemma":[0.00025717937,0.000062776024,0.90803003,9.489061e-7,0.0000088617735,0.0000034120937,0.000022353637,0.011815268,0.000079779646,0.0029279322,0.07666085,0.00013061902],"about_ca_topic_score_codex":0.00019153977,"about_ca_topic_score_gemma":0.0074283537,"teacher_disagreement_score":0.07649933,"about_ca_system_score_codex":0.00006134179,"about_ca_system_score_gemma":0.000009773624,"threshold_uncertainty_score":0.9998483},"labels":[],"label_agreement":null},{"id":"W2069269793","doi":"10.1002/qj.917","title":"Comparison of cloud products within IASI footprints for the assimilation of cloudy radiances","year":2011,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":32,"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","funders":"National Oceanic and Atmospheric Administration","keywords":"Radiance; Overcast; Environmental science; Cloud computing; Remote sensing; Footprint; Meteorology; Cloud cover; Depth sounding; Satellite; Data assimilation; Sky; Computer science; Geography; Cartography; Engineering","score_opus":0.0491835080137906,"score_gpt":0.2737147290469612,"score_spread":0.2245312210331706,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2069269793","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":[0.9920991,0.00020120473,0.00601999,0.0005053828,0.00056518166,0.0002998799,0.0000029953385,0.000004926582,0.00030135954],"genre_scores_gemma":[0.985292,0.000005913725,0.01440338,0.00009034763,0.00012571478,0.0000059156846,1.4942827e-7,0.00000711295,0.00006947197],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983798,0.00016508531,0.00069407304,0.00015223167,0.00041025007,0.0001985522],"domain_scores_gemma":[0.9981868,0.00023091266,0.0012165192,0.00024464916,0.000062029,0.000059053447],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012852312,0.00013364924,0.00036641594,8.312925e-7,0.00017022774,0.000009173199,0.0007015698,0.000112991496,0.00023037507],"category_scores_gemma":[0.00011504837,0.00006108702,0.00043095462,0.00015514201,0.0005708971,0.000061572726,0.000060834576,0.000268364,0.000002158341],"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":[0.000972707,0.0014145655,0.87282693,0.00007474717,0.00056535425,9.206064e-7,0.039296106,0.016890345,0.010886808,0.0011056458,0.008799846,0.047166027],"study_design_scores_gemma":[0.00093571213,0.004869991,0.95533264,0.000033781693,0.00028796648,0.0000067788387,0.0052401004,0.012507367,0.013885268,0.005922715,0.0007826582,0.00019501029],"about_ca_topic_score_codex":0.000057091773,"about_ca_topic_score_gemma":0.0000092625805,"teacher_disagreement_score":0.082505725,"about_ca_system_score_codex":0.000046427467,"about_ca_system_score_gemma":0.00001997968,"threshold_uncertainty_score":0.25224453},"labels":[],"label_agreement":null},{"id":"W2069715026","doi":"10.1175/jcli-d-12-00223.1","title":"Multiyear Summertime Observations of Daytime Fair-Weather Cumuli at the ARM Southern Great Plains Facility","year":2013,"lang":"en","type":"article","venue":"Journal of Climate","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Daytime; Environmental science; Meteorology; Cloud top; Radar; Cloud height; Cloud computing; Atmospheric sciences; Vertical velocity; Weather radar; Climatology; Geology; Cloud cover; Geography; Physics; Mechanics; Computer science","score_opus":0.02065677242079247,"score_gpt":0.2312601191434859,"score_spread":0.21060334672269343,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2069715026","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":[0.9949716,0.0000594901,0.00020520634,0.00080721785,0.0000715764,0.00014045356,0.00004631192,0.00000784726,0.0036902938],"genre_scores_gemma":[0.9946174,0.000108618115,0.0013632465,0.00022163353,0.000037321766,0.0000044647145,0.0000025669835,0.00001240316,0.0036323266],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987097,0.00006409628,0.00047942324,0.0001214793,0.0003771803,0.00024811752],"domain_scores_gemma":[0.99908435,0.000079619276,0.0004383843,0.00025761043,0.000036022266,0.00010401359],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0003379974,0.00012791216,0.00022503559,0.0000017624791,0.00016638228,0.000023471703,0.00030610972,0.000058464768,0.017534323],"category_scores_gemma":[0.000036907986,0.00007392217,0.00017449171,0.00011391659,0.00023935431,0.00021687496,0.00017729835,0.00015527409,0.0015926278],"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":[0.000078597266,0.00028501786,0.9406442,0.000015036123,0.00008280461,0.0000069770663,0.0035304318,0.004751502,0.033313155,0.000018098606,0.0065524643,0.010721724],"study_design_scores_gemma":[0.0012578163,0.0003630811,0.9602591,0.000045821518,0.00012078797,0.00004318802,0.0028233468,0.006436883,0.0020020527,0.0004012526,0.025905367,0.00034133036],"about_ca_topic_score_codex":0.00052274554,"about_ca_topic_score_gemma":0.0001223308,"teacher_disagreement_score":0.031311102,"about_ca_system_score_codex":0.0001027807,"about_ca_system_score_gemma":0.00001010788,"threshold_uncertainty_score":0.9991847},"labels":[],"label_agreement":null},{"id":"W2069968494","doi":"10.1029/2001jd001559","title":"On the features of clouds occurring over the Mackenzie River basin","year":2002,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"York University","funders":"","keywords":"Cloud cover; Environmental science; Cloud fraction; Climatology; Scale (ratio); Cloud computing; Structural basin; Atmospheric sciences; Geology; Geography; Geomorphology; Cartography","score_opus":0.029126598230747838,"score_gpt":0.2904457951288442,"score_spread":0.2613191968980964,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2069968494","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":[0.98537546,0.00027533725,0.000047071386,0.0018638734,0.00010483464,0.00016105897,0.0000037934424,0.0000051848165,0.012163371],"genre_scores_gemma":[0.99676466,0.0001050331,0.00028761764,0.0005184049,0.00027850567,0.000004666681,1.1272369e-7,0.000018028068,0.002022944],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99651676,0.0004242729,0.0003618878,0.00019256369,0.001996382,0.00050812634],"domain_scores_gemma":[0.9973561,0.0016993812,0.00024200075,0.00044643364,0.000084330546,0.00017174153],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001077882,0.00016588905,0.00026517277,0.0000012278638,0.00037251937,0.0000690324,0.0011034731,0.0000694292,0.008850399],"category_scores_gemma":[0.00068794674,0.00007644486,0.00027613278,0.00055761385,0.0013415202,0.00015697359,0.00036658646,0.0011152374,0.0002932289],"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":[0.00060630287,0.0014344184,0.05279995,0.000026659805,0.00025178754,0.00014416798,0.0029041262,0.0023343689,0.004485082,0.020417964,0.84935176,0.06524342],"study_design_scores_gemma":[0.00091653614,0.0018632893,0.91544944,0.00015829042,0.00004308192,0.000031736185,0.0010519837,0.0044621257,0.0024887798,0.025922343,0.04732653,0.00028586327],"about_ca_topic_score_codex":0.0010021788,"about_ca_topic_score_gemma":0.000041706266,"teacher_disagreement_score":0.8626495,"about_ca_system_score_codex":0.00013115541,"about_ca_system_score_gemma":0.000022595283,"threshold_uncertainty_score":0.99205565},"labels":[],"label_agreement":null},{"id":"W2069977802","doi":"10.1289/ehp.0901623","title":"Global Estimates of Ambient Fine Particulate Matter Concentrations from Satellite-Based Aerosol Optical Depth: Development and Application","year":2010,"lang":"en","type":"article","venue":"Environmental Health Perspectives","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1699,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Public Health Ontario; University of Toronto; University of British Columbia; Health Canada; Dalhousie University","funders":"","keywords":"Aerosol; Moderate-resolution imaging spectroradiometer; Satellite; Particulates; Environmental science; Spectroradiometer; Chemical transport model; Population; Atmospheric sciences; Climatology; Meteorology; Geography; Geology; Chemistry; Physics","score_opus":0.006365296990739295,"score_gpt":0.2470056803647766,"score_spread":0.24064038337403731,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2069977802","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":[0.9892845,0.00026146765,0.008721417,0.0007466435,0.00004468814,0.00038319657,0.00003008722,0.00002250388,0.00050550327],"genre_scores_gemma":[0.9551191,0.000026257032,0.04452204,0.00018600089,0.000020780646,0.00005245904,0.00004323635,0.000011641217,0.000018525741],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986664,0.00002873237,0.00031782975,0.00043343683,0.00025622392,0.0002973971],"domain_scores_gemma":[0.9993893,0.00004416802,0.00013005367,0.00021273618,0.0000021926185,0.00022154136],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0000980846,0.0001759383,0.00019134382,0.0000015630557,0.00020264533,0.0000166194,0.000103585786,0.000066595705,0.0012249148],"category_scores_gemma":[0.0000060041116,0.00016309353,0.000034782734,0.00006973242,0.00062768534,0.00008943591,0.00009427745,0.00011347461,0.00019639515],"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":[0.000027724089,0.00047708824,0.9571458,0.000008341704,0.0000122440115,0.0000010189236,0.0016660625,0.00032688127,0.026732007,0.00019769557,0.00004705642,0.013358097],"study_design_scores_gemma":[0.0003824775,0.00008190649,0.9780537,0.000008100438,0.000009907891,0.0000024802293,0.0008616484,0.001579301,0.0182638,0.0001318722,0.00046139577,0.00016339583],"about_ca_topic_score_codex":0.00039109585,"about_ca_topic_score_gemma":0.00078351214,"teacher_disagreement_score":0.03580062,"about_ca_system_score_codex":0.0003175088,"about_ca_system_score_gemma":0.00002531879,"threshold_uncertainty_score":0.9996881},"labels":[],"label_agreement":null},{"id":"W2070321532","doi":"10.1021/jp044823c","title":"Frequency Dependent Complex Refractive Indices of Supercooled Liquid Water and Ice Determined from Aerosol Extinction Spectra","year":2005,"lang":"en","type":"article","venue":"The Journal of Physical Chemistry A","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":77,"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 Waterloo","funders":"","keywords":"Extinction (optical mineralogy); Aerosol; Chemistry; Supercooling; Cirrus; Refractive index; Spectral line; Troposphere; Atmospheric sciences; Optics; Meteorology; Mineralogy; Geology; Physics","score_opus":0.008398747413265453,"score_gpt":0.223768461440671,"score_spread":0.21536971402740554,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2070321532","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":[0.99798465,0.000030111181,0.00028650617,0.00023793691,0.000008557475,0.000043203145,0.0000042783895,0.000004288515,0.0014004837],"genre_scores_gemma":[0.99917775,0.000017888244,0.00034545606,0.000055546778,0.00033644654,9.571655e-7,0.0000019271176,0.000007677342,0.00005632883],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9991636,0.00004094498,0.00024854034,0.00010670172,0.00029355672,0.00014664145],"domain_scores_gemma":[0.9994825,0.00008029434,0.00020712426,0.00013242644,0.000015606716,0.00008205003],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001375702,0.00011520932,0.00020024896,6.0576764e-7,0.000071278184,0.000010837904,0.00022049819,0.00004134276,0.0013810465],"category_scores_gemma":[0.000013848486,0.000064983564,0.00006620231,0.00003881455,0.00019287424,0.00020330946,0.0000898589,0.00022533878,0.000015206248],"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":[0.00021798132,0.00013412842,0.0003456807,0.0000050701483,0.000025481258,0.0000032031694,0.0013548599,0.00037819607,0.9968743,3.634902e-7,0.000019019448,0.0006417516],"study_design_scores_gemma":[0.00040605778,0.00021195534,0.005089253,0.000014687528,0.000075983604,0.000034294568,0.0003776417,0.0009494409,0.992537,0.00016075162,0.00005003018,0.000092856586],"about_ca_topic_score_codex":0.00010689825,"about_ca_topic_score_gemma":0.000012250588,"teacher_disagreement_score":0.0047435723,"about_ca_system_score_codex":0.000077415025,"about_ca_system_score_gemma":0.000007647023,"threshold_uncertainty_score":0.9995318},"labels":[],"label_agreement":null},{"id":"W2070538467","doi":"10.1175/jas-d-12-0334.1","title":"Doubling–Adding Method for Delta-Four-Stream Spherical Harmonic Expansion Approximation in Radiative Transfer Parameterization","year":2013,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":45,"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":"Radiative transfer; Ordinate; Computational physics; Physics; Harmonic; Spherical harmonics; Atmospheric radiative transfer codes; Mathematical analysis; Mathematics; Optics; Geometry; Quantum mechanics","score_opus":0.026948259274914458,"score_gpt":0.27076422064173283,"score_spread":0.24381596136681838,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2070538467","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":[0.81295216,0.000070058755,0.18505608,0.00097143697,0.00029383568,0.00040377388,7.181687e-7,0.000008356862,0.00024360414],"genre_scores_gemma":[0.7258133,0.000029930645,0.27372795,0.00026262237,0.000053561063,0.000027953172,2.7419023e-7,0.0000095187415,0.00007488184],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9980274,0.00018785364,0.0005786384,0.00026458467,0.00059588416,0.00034566846],"domain_scores_gemma":[0.9990959,0.00026048612,0.00035099773,0.00014929238,0.000044009008,0.000099298086],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011644239,0.00016988775,0.00027639515,0.0000015488267,0.00029880437,0.00013250725,0.0006548816,0.00007913385,0.00051893375],"category_scores_gemma":[0.00019870957,0.00010117875,0.00018473847,0.0010854785,0.0002807301,0.00092063897,0.00007951912,0.00017706903,0.000012542379],"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":[0.000115310155,0.00028580433,0.067433305,0.00002204173,0.000037266098,0.0000037293687,0.0029530765,0.71443105,0.074519634,0.00022124182,0.0015188149,0.13845876],"study_design_scores_gemma":[0.00091378274,0.0004737081,0.060416147,0.00006899385,0.000040358602,0.00004032587,0.0015364784,0.9261384,0.0060384693,0.0034955502,0.00057980075,0.00025795843],"about_ca_topic_score_codex":0.0003231838,"about_ca_topic_score_gemma":0.000021596123,"teacher_disagreement_score":0.2117074,"about_ca_system_score_codex":0.00021740086,"about_ca_system_score_gemma":0.00006717535,"threshold_uncertainty_score":0.56819606},"labels":[],"label_agreement":null},{"id":"W2072550620","doi":"10.1007/s10874-005-9010-x","title":"Numerical Investigation of Gas Scavenging by Weak Precipitation","year":2006,"lang":"en","type":"article","venue":"Journal of Atmospheric Chemistry","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":19,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University; Environment and Climate Change Canada","funders":"","keywords":"Scavenging; Precipitation; Chemistry; Aqueous solution; Analytical Chemistry (journal); Environmental chemistry; Meteorology","score_opus":0.002800654413370914,"score_gpt":0.18329161537226452,"score_spread":0.1804909609588936,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2072550620","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":[0.98616093,0.00021722994,0.006555321,0.0001623248,0.000066194254,0.00003731896,9.499305e-7,0.0000095368005,0.0067902007],"genre_scores_gemma":[0.97615016,0.000016863047,0.022709507,0.00002599195,0.00012206804,0.0000014089512,0.0000034053135,0.000014079786,0.0009565422],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99876,0.000019754414,0.00051414187,0.00012728992,0.00041528384,0.00016356689],"domain_scores_gemma":[0.99908566,0.00003960553,0.0006327582,0.0001162204,0.000031414496,0.00009432131],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00018027118,0.00012176543,0.00020474778,1.2432378e-7,0.000046945297,0.0000148392755,0.00018186515,0.00008110403,0.0012816371],"category_scores_gemma":[0.000034474655,0.000109255394,0.00010441679,0.00024811793,0.00013201807,0.0001784573,0.00003293189,0.0001563263,0.000010474009],"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":[0.00003770139,0.0001113618,0.16834815,0.000036987978,0.00002113231,0.0000053761823,0.00016452403,0.021554964,0.77853405,0.0000059179565,0.026568145,0.004611683],"study_design_scores_gemma":[0.0020891954,0.00035813855,0.18787296,0.00021567085,0.00014619245,0.00026074302,0.00097558467,0.025149247,0.7689247,0.0030356334,0.010223224,0.0007487096],"about_ca_topic_score_codex":0.0001216477,"about_ca_topic_score_gemma":7.153902e-7,"teacher_disagreement_score":0.01952481,"about_ca_system_score_codex":0.0001778358,"about_ca_system_score_gemma":0.00002952681,"threshold_uncertainty_score":0.99963135},"labels":[],"label_agreement":null},{"id":"W2073090076","doi":"10.1029/2002gl014828","title":"Analysis of lidar measurements of ice clouds at multiple incidence angles","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":26,"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":"Lidar; Depolarization ratio; Ice crystals; Polarization (electrochemistry); Optics; Remote sensing; Oscillation (cell signaling); Materials science; Geology; Physics","score_opus":0.06088820667780453,"score_gpt":0.2981005228705559,"score_spread":0.23721231619275135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2073090076","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":[0.9970414,0.000039222345,0.00015828386,0.0005176321,0.00002167585,0.00014242437,0.000008812312,0.000010945774,0.0020596005],"genre_scores_gemma":[0.99872166,0.000012963553,0.00060508726,0.00019138696,0.000029957426,0.000014686894,0.00000336744,0.000010840455,0.00041007588],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99680763,0.00020835569,0.00028243347,0.00037021792,0.0018347618,0.0004965727],"domain_scores_gemma":[0.998801,0.00041290093,0.00010483518,0.00047531334,0.00004627334,0.00015969346],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004981676,0.00012348618,0.0003148925,0.0000127445255,0.00013890523,0.0000113193655,0.00051722134,0.000048168677,0.001805542],"category_scores_gemma":[0.00035936336,0.00010706747,0.00020225676,0.0018148464,0.00084835925,0.000118871685,0.00053133804,0.00019681534,0.00038876064],"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":[0.000035804336,0.00021942935,0.46946195,0.000011054812,0.00015031209,0.0000058548276,0.00044815204,0.0016648972,0.5232612,0.000006084515,0.0020462763,0.0026890154],"study_design_scores_gemma":[0.0003390461,0.00016799729,0.9489893,0.000017772058,0.00011285491,2.5309018e-7,0.000082813334,0.013528855,0.03599066,0.00002823407,0.0005615167,0.00018074116],"about_ca_topic_score_codex":0.0028325582,"about_ca_topic_score_gemma":0.0002970683,"teacher_disagreement_score":0.48727053,"about_ca_system_score_codex":0.00020688976,"about_ca_system_score_gemma":0.000004857661,"threshold_uncertainty_score":0.99910694},"labels":[],"label_agreement":null},{"id":"W2073367573","doi":"10.1029/2005jd005760","title":"Comparison of Moderate Resolution Imaging Spectroradiometer (MODIS) and Aerosol Robotic Network (AERONET) remote‐sensing retrievals of aerosol fine mode fraction over ocean","year":2005,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":146,"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 de Sherbrooke","funders":"","keywords":"AERONET; Aerosol; Moderate-resolution imaging spectroradiometer; Environmental science; Remote sensing; Radiometer; Satellite; Spectroradiometer; Angstrom exponent; Atmospheric sciences; Meteorology; Geology; Physics; Reflectivity","score_opus":0.028929630476801114,"score_gpt":0.33451520072510493,"score_spread":0.3055855702483038,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2073367573","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":[0.961742,0.0007287905,0.036315072,0.0004259365,0.00006295447,0.00021763913,0.0000019494069,0.000010540184,0.0004951128],"genre_scores_gemma":[0.95896256,0.00014079598,0.040158603,0.000030201001,0.00049369666,2.3760875e-7,0.0000015637477,0.000033862383,0.00017847437],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9958516,0.00037831772,0.0010170727,0.0003597792,0.0016687529,0.0007245017],"domain_scores_gemma":[0.99790484,0.00047355104,0.0007737035,0.00034645176,0.00020007539,0.00030137366],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001088179,0.0002503649,0.00079479,0.000006328959,0.00026133703,0.000071249415,0.00031825065,0.0001157125,0.00034391016],"category_scores_gemma":[0.00030879726,0.00021042084,0.00020367993,0.0006701899,0.00070618046,0.00062912836,0.00027841592,0.0008906753,0.00001741121],"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":[0.0030788502,0.0007827857,0.0362472,0.00010596464,0.00019687945,0.000034654546,0.0008356362,0.61478925,0.24650319,0.00012386878,0.015951313,0.08135039],"study_design_scores_gemma":[0.0010467556,0.0009760803,0.026889322,0.0002883675,0.00006190548,0.000027035743,0.00022318569,0.9406903,0.02721772,0.0022055996,0.00011980994,0.0002539672],"about_ca_topic_score_codex":0.0012451039,"about_ca_topic_score_gemma":0.0001175302,"teacher_disagreement_score":0.325901,"about_ca_system_score_codex":0.00040174287,"about_ca_system_score_gemma":0.0000701344,"threshold_uncertainty_score":0.8580713},"labels":[],"label_agreement":null},{"id":"W2074147177","doi":"10.1130/0091-7613(2002)030<0663:ootmpc>2.0.co;2","title":"Origin of the Mount Pinatubo climactic eruption cloud: Implications for volcanic hazards and atmospheric impacts","year":2002,"lang":"en","type":"article","venue":"Geology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Queen (butterfly); Mount; Art history; Atmospheric research; History; Library science; Meteorology; Computer science; Geography","score_opus":0.014493945968437364,"score_gpt":0.24540395702723428,"score_spread":0.2309100110587969,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074147177","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":[0.9927547,0.00026594035,0.0022193345,0.0026040545,0.00018080408,0.00028290026,0.0000059574677,0.000016124777,0.0016701871],"genre_scores_gemma":[0.9967224,0.00014470871,0.0017462964,0.00038602127,0.000042452983,0.00004428652,0.0000014612941,0.000009338172,0.0009030163],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999278,0.000032311742,0.00016312627,0.000205425,0.00006920181,0.00025195596],"domain_scores_gemma":[0.99948996,0.00005376047,0.000119852615,0.00026988235,0.000010880256,0.000055645432],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000097395074,0.00009504736,0.00012814839,3.6969922e-7,0.00015094607,0.000005486819,0.0001559789,0.00008305859,0.0011619022],"category_scores_gemma":[0.000046178342,0.000068091416,0.000053172156,0.00016002529,0.00030143015,0.00006118934,0.00012187937,0.00007682954,0.000046517544],"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":[0.000027566923,0.00016015791,0.9326962,0.000027086155,0.000031768377,4.3691526e-7,0.000545992,0.0009149555,0.012191051,0.011444675,0.009172762,0.032787316],"study_design_scores_gemma":[0.00036736563,0.00017351483,0.9578509,0.0000032811226,0.000032395365,0.000026806703,0.000053904718,0.007096107,0.00008202792,0.002558539,0.031641766,0.00011343084],"about_ca_topic_score_codex":0.00042789427,"about_ca_topic_score_gemma":0.0002767179,"teacher_disagreement_score":0.032673888,"about_ca_system_score_codex":0.00011393101,"about_ca_system_score_gemma":0.000009249251,"threshold_uncertainty_score":0.99975115},"labels":[],"label_agreement":null},{"id":"W2074197832","doi":"10.3137/ao.410102","title":"Turbulent heat fluxes over leads and polynyas, and their effects on arctic clouds during FIRE.ACE: Aircraft observations for April 1998","year":2003,"lang":"en","type":"article","venue":"ATMOSPHERE-OCEAN","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"National Oceanic and Atmospheric Administration; University of Arizona; National Aeronautics and Space Administration","keywords":"Environmental science; Arctic; Atmospheric sciences; Sensible heat; Latent heat; Heat flux; Lead (geology); Climatology; Meteorology; Flux (metallurgy); Turbulence; Geology; Heat transfer; Materials science; Mechanics; Geography; Physics; Oceanography","score_opus":0.00830420659290629,"score_gpt":0.20618110640585863,"score_spread":0.19787689981295234,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074197832","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":[0.9971009,0.0009938702,0.00019919698,0.0004455709,0.00016286668,0.00061537256,0.0000059662575,0.00008354652,0.00039270375],"genre_scores_gemma":[0.9934866,0.00016319212,0.0028708056,0.00096137665,0.00008910159,0.000029187893,0.0000062957447,0.00005992568,0.0023335214],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982545,0.00006889384,0.0002691283,0.0006281168,0.00023196691,0.0005474342],"domain_scores_gemma":[0.9990413,0.00024417738,0.00007281936,0.00039178442,0.000008923593,0.00024095987],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0001720493,0.00038226167,0.00032082622,5.0090796e-7,0.0005073834,0.0000793085,0.00016294124,0.00014314293,0.00017453532],"category_scores_gemma":[0.00006550342,0.00030886382,0.00010233878,0.0001926423,0.00021626547,0.000199443,0.00011312832,0.00017885701,0.000026731012],"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":[0.00012144777,0.00026089774,0.9774817,0.00026569117,0.00009257492,0.000017345656,0.0015988519,0.0028737788,0.0064494414,0.00064530957,0.0061369715,0.004055986],"study_design_scores_gemma":[0.003233482,0.0009724295,0.94937664,0.00022400086,0.00010350725,0.00007393565,0.00058927876,0.008267516,0.009052325,0.0019953884,0.025016101,0.0010954181],"about_ca_topic_score_codex":0.00029670724,"about_ca_topic_score_gemma":0.00005899555,"teacher_disagreement_score":0.028105086,"about_ca_system_score_codex":0.00016527929,"about_ca_system_score_gemma":0.000015349731,"threshold_uncertainty_score":0.99993634},"labels":[],"label_agreement":null},{"id":"W2074333327","doi":"10.1364/ao.47.006563","title":"Relation between circular and linear depolarization ratios under multiple-scattering conditions","year":2008,"lang":"en","type":"article","venue":"Applied Optics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Defence Research and Development Canada","funders":"","keywords":"Azimuth; Lidar; Scattering; Optics; Depolarization; Polarization (electrochemistry); Circular polarization; Physics; Depolarization ratio; Forward scatter; Light scattering; Linear polarization; Computational physics; Remote sensing; Laser; Geology; Chemistry","score_opus":0.017109602639193942,"score_gpt":0.21742778165870194,"score_spread":0.200318179019508,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074333327","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":[0.8284004,0.0000062803238,0.16900773,0.00006524849,0.000022325432,0.00014278205,0.000002427241,0.000037031303,0.0023158158],"genre_scores_gemma":[0.9825259,0.000020812837,0.017073462,0.00015490784,0.000052716947,0.000012371364,0.000060577353,0.000014608828,0.00008462859],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994062,0.00000813165,0.00014467716,0.00017534486,0.00013831601,0.00012733697],"domain_scores_gemma":[0.9997083,0.00004816934,0.000054147215,0.00012370439,0.0000039933734,0.000061661805],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000042362808,0.000086616514,0.00008226495,0.000001452562,0.00029074826,0.000011773772,0.000052137962,0.00007522549,0.00010545798],"category_scores_gemma":[0.000009079296,0.00009034963,0.00001555904,0.00010655448,0.00014580322,0.000094729156,0.000060428953,0.00008436882,0.00010673798],"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":[0.0000028517427,0.00003230493,0.8901582,0.000005468604,0.000018598545,0.0000028980944,0.00057382626,0.042352878,0.06419221,0.0019544263,0.00008072602,0.0006256468],"study_design_scores_gemma":[0.0003309722,0.000015436199,0.97943544,0.000003275424,0.000024812984,0.000007752376,0.00010109915,0.017307296,0.0017383961,0.0006313416,0.00023597406,0.00016819181],"about_ca_topic_score_codex":0.000026000094,"about_ca_topic_score_gemma":0.0000053801227,"teacher_disagreement_score":0.15412556,"about_ca_system_score_codex":0.000041696007,"about_ca_system_score_gemma":0.0000053707968,"threshold_uncertainty_score":0.3684351},"labels":[],"label_agreement":null},{"id":"W2074612774","doi":"10.1029/2011jd015888","title":"Effects of ice number concentration on dynamics of a shallow mixed-phase stratiform cloud","year":2011,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":79,"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":"Sea ice growth processes; Buoyancy; Atmospheric sciences; Liquid water path; Environmental science; Cloud base; Radiative transfer; Ice cloud; Sea ice; Radiative cooling; Liquid water content; Mechanics; Arctic ice pack; Geology; Meteorology; Sea ice thickness; Physics; Cloud computing; Optics","score_opus":0.022375312867937803,"score_gpt":0.30880781218372466,"score_spread":0.28643249931578685,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074612774","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":[0.98913974,0.000037577178,0.0013537561,0.000053641103,0.00013479865,0.00022662066,0.00000480245,0.0000048178013,0.009044235],"genre_scores_gemma":[0.99685645,0.00006481314,0.0025742587,0.000019590881,0.00012547628,0.0000046732157,0.0000011286451,0.000017591547,0.00033602974],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.997129,0.0002223894,0.00058324967,0.00019397878,0.0014511107,0.00042022634],"domain_scores_gemma":[0.9982468,0.0006411422,0.00044858374,0.00022972982,0.00016911172,0.0002646524],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00059396616,0.00016215857,0.00039845458,9.833474e-7,0.000085784864,0.000017515034,0.0004897304,0.00010149874,0.0015706099],"category_scores_gemma":[0.00039509163,0.00012087695,0.00020931597,0.00039926285,0.00078724953,0.00026290733,0.00013358284,0.00051825395,0.000096417825],"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":[0.014993417,0.032871787,0.27536732,0.0011316031,0.001064286,0.00094302674,0.008875027,0.0018579909,0.2571878,0.089425854,0.01469889,0.301583],"study_design_scores_gemma":[0.008572018,0.02352375,0.6651943,0.0007835041,0.00018426479,0.00003432287,0.0028137844,0.024396097,0.23556635,0.037441205,0.00075359247,0.0007368171],"about_ca_topic_score_codex":0.00086014357,"about_ca_topic_score_gemma":0.00014657507,"teacher_disagreement_score":0.38982698,"about_ca_system_score_codex":0.00019858041,"about_ca_system_score_gemma":0.00009821203,"threshold_uncertainty_score":0.9993421},"labels":[],"label_agreement":null},{"id":"W2074862306","doi":"10.1029/2005jd006737","title":"Retrieving of particulate matter from optical measurements: A semiparametric approach","year":2007,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":90,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Association pour le Développement de la Recherche et de l'Innovation du Québec","funders":"","keywords":"Smoothing; Aerosol; Correlation coefficient; Smoothness; Linear regression; Particulates; Linear model; Environmental science; Data set; Coefficient of determination; Air quality index; Satellite; Mathematics; Meteorology; Statistics; Physics; Mathematical analysis; Chemistry","score_opus":0.04968465050989399,"score_gpt":0.31739495941626716,"score_spread":0.26771030890637315,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074862306","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":[0.97683793,0.00023196304,0.009797673,0.00012417918,0.000073415205,0.00014906659,0.0000013112488,0.0000062306203,0.0127782235],"genre_scores_gemma":[0.9718604,0.000020752497,0.027406814,0.000061166356,0.00022920965,0.0000021623944,6.694207e-7,0.000022802784,0.0003959849],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99523795,0.00020306307,0.0008001169,0.000292866,0.0027259332,0.00074004673],"domain_scores_gemma":[0.99788165,0.00079120556,0.0003245047,0.00033872356,0.00020366753,0.0004602769],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0028284031,0.00017674694,0.00045683546,0.000004380708,0.00012294474,0.0000555981,0.00062057254,0.00012292698,0.0023585556],"category_scores_gemma":[0.0009020925,0.0001289786,0.00024286668,0.0013140494,0.0006119273,0.0002889284,0.00034504375,0.00078952353,0.00032300878],"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":[0.000940687,0.0016677586,0.8835087,0.00003501703,0.00022684751,0.0000994535,0.0004908922,0.0015524215,0.07540081,0.00013165492,0.009509228,0.026436554],"study_design_scores_gemma":[0.00084111805,0.00070577627,0.9731702,0.00008308728,0.000050205887,0.000014469096,0.00058559247,0.0012905424,0.019713854,0.0021674733,0.0011599009,0.00021778584],"about_ca_topic_score_codex":0.0008429416,"about_ca_topic_score_gemma":0.00001793048,"teacher_disagreement_score":0.089661516,"about_ca_system_score_codex":0.00027326948,"about_ca_system_score_gemma":0.00005414966,"threshold_uncertainty_score":0.9985534},"labels":[],"label_agreement":null},{"id":"W2074893592","doi":"10.1029/2009gl037946","title":"Can cosmic rays affect cloud condensation nuclei by altering new particle formation rates?","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":161,"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","funders":"","keywords":"Cosmic ray; Cloud condensation nuclei; Aerosol; Cloud cover; Atmospheric sciences; Physics; Flux (metallurgy); Particle (ecology); Astrophysics; Environmental science; Cloud computing; Meteorology; Geology; Chemistry","score_opus":0.025246074704050783,"score_gpt":0.2972073887875738,"score_spread":0.27196131408352303,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074893592","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":[0.98256403,0.000011440204,0.0022562954,0.014163735,0.0000511126,0.00027681174,0.0000026409102,0.000050363735,0.0006235407],"genre_scores_gemma":[0.99632263,0.000008424059,0.00021728082,0.002680653,0.00017871022,0.000012117567,0.0000123569835,0.000012370623,0.0005554698],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99800116,0.00015266726,0.00016550973,0.000297234,0.00072415994,0.00065928133],"domain_scores_gemma":[0.9993356,0.000098869925,0.00004425011,0.00023782617,0.0000102355125,0.00027323986],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00031319246,0.00012720094,0.00013002337,0.0000024609055,0.0002641972,0.000108331216,0.0002431185,0.000040982846,0.00040895492],"category_scores_gemma":[0.00006129874,0.000115687246,0.000056351244,0.00035022557,0.00017667995,0.00033073378,0.00010007769,0.00028247808,0.0010680213],"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":[0.000038940412,0.0000589574,0.0008099448,0.0000034982065,0.0000040187983,0.000008244357,0.00043352798,0.00031508977,0.8854971,0.00023635513,0.09852569,0.014068644],"study_design_scores_gemma":[0.004258161,0.0022672173,0.37850633,0.00010411789,0.00003862847,0.000018608844,0.0007828751,0.08626233,0.4848741,0.016716564,0.02462042,0.001550636],"about_ca_topic_score_codex":0.0011430418,"about_ca_topic_score_gemma":0.00003043634,"teacher_disagreement_score":0.400623,"about_ca_system_score_codex":0.00030032088,"about_ca_system_score_gemma":0.000013396723,"threshold_uncertainty_score":0.9997098},"labels":[],"label_agreement":null},{"id":"W2075162893","doi":"10.1256/qj.01.204","title":"Microphysical characterization of mixed‐phase clouds","year":2003,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":369,"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":"National Aeronautics and Space Administration","keywords":"Liquid water content; Environmental science; Atmospheric sciences; Liquid water; Volume (thermodynamics); Mixed phase; Ice nucleus; Meteorology; Phase (matter); Cloud computing; Geography; Geology; Chemistry; Physics; Thermodynamics","score_opus":0.007453299158749281,"score_gpt":0.2163430186588106,"score_spread":0.2088897195000613,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2075162893","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":[0.99187803,0.000022701219,0.0070700087,0.00024819898,0.00033054256,0.00008622463,0.0000039037877,0.000005916797,0.00035448014],"genre_scores_gemma":[0.9961809,0.000005596417,0.00328449,0.00024035426,0.00007855058,0.0000011783355,5.0765976e-7,0.000008347259,0.00020008122],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9984917,0.00027007397,0.00047446316,0.00014437654,0.00038801582,0.00023138459],"domain_scores_gemma":[0.99908644,0.00006101025,0.00053119165,0.00018521461,0.000028132745,0.00010800177],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00050964084,0.00014277354,0.00030203423,6.564352e-7,0.00012555247,0.000016737358,0.00039108325,0.0001280178,0.0010489254],"category_scores_gemma":[0.000039449747,0.00007854854,0.0005662629,0.00017666472,0.00035103728,0.00007701519,0.000041703683,0.00029626745,0.000020954769],"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":[0.00018792764,0.001579192,0.029788064,0.000013717242,0.00015783134,0.000009312899,0.0014051044,0.00063326245,0.92992914,0.00082852197,0.0022700012,0.033197917],"study_design_scores_gemma":[0.008102172,0.01814326,0.81326455,0.00008127352,0.00062599155,0.00016989697,0.0017283064,0.0055546924,0.11044885,0.012034123,0.028696416,0.0011504431],"about_ca_topic_score_codex":0.000007058324,"about_ca_topic_score_gemma":4.3270876e-7,"teacher_disagreement_score":0.8194803,"about_ca_system_score_codex":0.00006693451,"about_ca_system_score_gemma":0.00001495806,"threshold_uncertainty_score":0.9998643},"labels":[],"label_agreement":null},{"id":"W2075544728","doi":"10.5194/acpd-10-18315-2010","title":"Airborne observation of aerosol optical depth during ARCTAS: vertical profiles, inter-comparison, fine-mode fraction and horizontal variability","year":2010,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","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":true,"ca_institutions":"Environment and Climate Change Canada; Université de Sherbrooke","funders":"Oak Ridge Associated Universities; Ames Research Center; National Aeronautics and Space Administration","keywords":"Angstrom exponent; Aerosol; Single-scattering albedo; Environmental science; Troposphere; Atmospheric sciences; Aethalometer; Mineral dust; Optical depth; Air mass (solar energy); Haze; Attenuation; Albedo (alchemy); Soot; Meteorology; Geology; Carbon black; Optics; Materials science; Physics; Chemistry; Boundary layer","score_opus":0.009691908106453644,"score_gpt":0.2458052475040715,"score_spread":0.23611333939761786,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2075544728","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":[0.9804438,0.0000020036719,0.01593499,0.00015887035,0.00009724204,0.00019907554,0.0000016534342,0.000044310942,0.0031180596],"genre_scores_gemma":[0.9788403,0.0000013383761,0.020979768,0.000022730603,0.000049752074,0.000017675406,0.000006098321,0.000010436956,0.00007188715],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988574,0.000030637915,0.00034057366,0.00034225459,0.00020711652,0.00022202487],"domain_scores_gemma":[0.9994865,0.000068503694,0.000055021083,0.00024613435,0.000013647219,0.00013017187],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00018813982,0.00013747663,0.00019777194,0.0000012709048,0.00008315684,0.000020992582,0.00012288433,0.00013146678,0.0010866418],"category_scores_gemma":[0.00014765777,0.000114582836,0.00004183774,0.00010311193,0.0002778476,0.00025701415,0.0001764753,0.00029686332,0.00003599295],"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":[0.000058757192,0.00019954289,0.642212,0.000013829416,0.0000059204854,5.0167523e-7,0.000069974594,0.000029998851,0.35188305,0.0005188059,0.000081228245,0.004926413],"study_design_scores_gemma":[0.00029797704,0.00011752179,0.85768276,0.000007202745,0.000014201484,0.0000057707202,0.000072266805,0.013666442,0.12775539,0.00018849339,0.000053480115,0.00013849535],"about_ca_topic_score_codex":0.0005715822,"about_ca_topic_score_gemma":0.0010579524,"teacher_disagreement_score":0.22412767,"about_ca_system_score_codex":0.00007701848,"about_ca_system_score_gemma":0.0000124434555,"threshold_uncertainty_score":0.9998265},"labels":[],"label_agreement":null},{"id":"W2076407889","doi":"10.1029/2003jd004443","title":"Sensitivity studies of cirrus clouds formed by heterogeneous freezing in the ECHAM GCM","year":2004,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":70,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Canadian Foundation for Climate and Atmospheric Sciences; Deutsches Klimarechenzentrum","keywords":"Cirrus; Ice nucleus; Clear ice; Atmospheric sciences; Homogeneous; Ice crystals; Supercooling; Ice cloud; Precipitation; Nucleation; Environmental science; Aerosol; Sea ice growth processes; Freezing point; Climatology; Arctic ice pack; Sea ice; Meteorology; Geology; Thermodynamics; Radiative transfer; Sea ice thickness; Physics; Antarctic sea ice","score_opus":0.0394345761273311,"score_gpt":0.3327830034742593,"score_spread":0.29334842734692823,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076407889","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":[0.9971599,0.00074502896,0.00033574837,0.0008750178,0.000067541114,0.00018877788,0.0000032776788,0.000004898725,0.0006198137],"genre_scores_gemma":[0.99827373,0.0003050198,0.0010507259,0.0001141505,0.00013517142,0.0000063552375,3.4881955e-7,0.000015561196,0.00009892882],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99651116,0.00046227477,0.0005309276,0.00021940682,0.001676665,0.0005995845],"domain_scores_gemma":[0.9982752,0.00091000047,0.00025155864,0.0002971522,0.000114613424,0.00015144952],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0021709483,0.00017284343,0.00043803247,0.0000018811055,0.0001978929,0.00003732553,0.000533535,0.00007718721,0.00010763509],"category_scores_gemma":[0.00069214404,0.00010611598,0.00020482573,0.0006193185,0.0008973915,0.00022529296,0.00032412834,0.00075344776,0.000041618285],"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":[0.0025433043,0.008502525,0.11275448,0.00031019462,0.0009896783,0.0040521175,0.026320413,0.085398264,0.5812636,0.0029781868,0.034863867,0.14002337],"study_design_scores_gemma":[0.013309991,0.02014593,0.45126852,0.0015171831,0.00022813499,0.0011262699,0.0530215,0.005699919,0.17368643,0.26616913,0.011636833,0.0021901582],"about_ca_topic_score_codex":0.0024491763,"about_ca_topic_score_gemma":0.0008066438,"teacher_disagreement_score":0.40757716,"about_ca_system_score_codex":0.00035228854,"about_ca_system_score_gemma":0.00007790692,"threshold_uncertainty_score":0.4327284},"labels":[],"label_agreement":null},{"id":"W2076448919","doi":"10.1029/2007gl029748","title":"Cloud seeding as a technique for studying aerosol‐cloud interactions in marine stratocumulus","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Marine stratocumulus; Aerosol; Seeding; Atmospheric sciences; Transect; Environmental science; Cloud computing; Plume; Drizzle; Meteorology; Geology; Oceanography; Physics; Precipitation","score_opus":0.04318922658651603,"score_gpt":0.3538858883693647,"score_spread":0.31069666178284866,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076448919","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":[0.9798941,0.000002536452,0.012109654,0.0020881135,0.00018575213,0.0011465969,0.0000023366308,0.00004535567,0.004525565],"genre_scores_gemma":[0.9935981,0.0000028402198,0.004156954,0.0006502703,0.00050809607,0.00033793625,0.0000038932394,0.000032189084,0.00070973573],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9971906,0.00009295059,0.00031606713,0.00053234625,0.0007679298,0.0011001384],"domain_scores_gemma":[0.99873257,0.0006481411,0.000053160824,0.00030295894,0.000025562522,0.00023759443],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014825177,0.00018449023,0.00021291449,0.000014462871,0.00032985516,0.00007903317,0.00042270252,0.000057965586,0.00051179965],"category_scores_gemma":[0.00021896596,0.00017384211,0.00010944138,0.00083170313,0.00035457528,0.0002398752,0.0005990975,0.0008172664,0.00035238417],"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":[0.00032035323,0.00040942623,0.023620795,0.000021993006,0.000019090228,0.00010412995,0.00068615784,0.00019296512,0.9587254,0.0008494138,0.0062837503,0.008766538],"study_design_scores_gemma":[0.007346505,0.0042711445,0.4288445,0.0005096639,0.000070100104,0.00010013865,0.012609512,0.0054643815,0.46407148,0.023119967,0.050000712,0.0035918797],"about_ca_topic_score_codex":0.0031320853,"about_ca_topic_score_gemma":0.0006905227,"teacher_disagreement_score":0.4946539,"about_ca_system_score_codex":0.00055095804,"about_ca_system_score_gemma":0.00002305761,"threshold_uncertainty_score":0.70890754},"labels":[],"label_agreement":null},{"id":"W2077273854","doi":"10.1364/ao.43.002777","title":"Measurement of the azimuthal dependence of cross-polarized lidar returns and its relation to optical depth","year":2004,"lang":"en","type":"article","venue":"Applied Optics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Defence Research and Development Canada","funders":"","keywords":"Optics; Azimuth; Scattering; Lidar; Physics; Forward scatter; Laser; Contrast (vision); Measure (data warehouse); Light scattering; Optical depth","score_opus":0.016085710498720887,"score_gpt":0.23883972488361802,"score_spread":0.22275401438489711,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2077273854","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":[0.9847451,0.000029273424,0.006001347,0.00010341865,0.000040175102,0.00028066538,0.0000016354446,0.0000082951865,0.008790103],"genre_scores_gemma":[0.98765236,0.0000074148593,0.012214799,0.00005845841,0.000011467462,0.0000071688814,2.5999944e-7,0.000008985846,0.000039054885],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99887353,0.000008668333,0.00023511829,0.00018473064,0.00054190774,0.00015607054],"domain_scores_gemma":[0.99957764,0.00001481364,0.000096611926,0.00020945628,0.000023249093,0.00007822305],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025151795,0.00009493884,0.00012725541,0.0000010531568,0.000073324394,0.0000123602695,0.00019039673,0.00007944989,0.000031184936],"category_scores_gemma":[0.00006315551,0.00007006173,0.000032059157,0.00015990938,0.0001672506,0.000050086353,0.00021350906,0.00010842325,0.000019691013],"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":[0.00009891541,0.0001616825,0.08609382,0.00003263948,0.000023756738,0.0000015205333,0.0013839809,0.019847644,0.86512494,0.025946261,0.0000060408215,0.0012788051],"study_design_scores_gemma":[0.0007927248,0.0001045126,0.79544365,0.000030050638,0.00003401078,0.0000044041317,0.00016118107,0.00035346413,0.20135099,0.0015287835,0.000037361035,0.00015884606],"about_ca_topic_score_codex":0.000032828957,"about_ca_topic_score_gemma":0.00006624581,"teacher_disagreement_score":0.7093499,"about_ca_system_score_codex":0.00009930289,"about_ca_system_score_gemma":0.000025072251,"threshold_uncertainty_score":0.28570345},"labels":[],"label_agreement":null},{"id":"W2077650774","doi":"10.1029/2003gl017861","title":"High aerosol optical depth biomass burning events: A comparison of optical properties for different source regions","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":241,"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 de Sherbrooke","funders":"","keywords":"AERONET; Aerosol; Single-scattering albedo; Smoke; Environmental science; Optical depth; Atmospheric sciences; Albedo (alchemy); Effective radius; Combustion; Boreal; Biomass (ecology); Peat; Taiga; Scattering; Meteorology; Geology; Optics; Chemistry; Physics; Geography","score_opus":0.052515707558356696,"score_gpt":0.309747326131131,"score_spread":0.25723161857277427,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2077650774","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":[0.96609056,0.000022150716,0.030027486,0.0025512325,0.00006563975,0.00056891126,0.0000020481061,0.000031629028,0.0006403324],"genre_scores_gemma":[0.99503493,0.0000029149326,0.004056189,0.00015037532,0.00008429088,0.00018498156,0.000004090041,0.00003208964,0.0004501102],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99682885,0.00021555962,0.00035891257,0.00051059335,0.0011345649,0.00095148775],"domain_scores_gemma":[0.99876136,0.0004335953,0.000069536436,0.00038542345,0.00003691726,0.0003132005],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035213024,0.0002160052,0.00039747113,0.000006471533,0.00033606924,0.000042725653,0.0003860552,0.00009183389,0.000111957765],"category_scores_gemma":[0.00046856966,0.00015898491,0.00018097066,0.0003306179,0.0010504331,0.00010973437,0.00028928608,0.00044179396,0.00013406499],"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":[0.00024847477,0.0013103632,0.018884607,0.0000788522,0.000068615474,0.000006208344,0.000629184,0.0010481314,0.9602053,0.0064701117,0.0056948196,0.0053553088],"study_design_scores_gemma":[0.0047039767,0.0037588063,0.16740678,0.00035059373,0.00014601575,0.0000125505,0.003289959,0.014467381,0.7916301,0.004353868,0.0081769135,0.0017030537],"about_ca_topic_score_codex":0.00025433916,"about_ca_topic_score_gemma":0.00002988391,"teacher_disagreement_score":0.16857523,"about_ca_system_score_codex":0.00018928791,"about_ca_system_score_gemma":0.000021686707,"threshold_uncertainty_score":0.6483217},"labels":[],"label_agreement":null},{"id":"W2078024018","doi":"10.5194/acpd-8-17691-2008","title":"Large surface radiative forcing from surface-based ice crystal events measured in the High Arctic at Eureka","year":2008,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Snow; Ice crystals; Arctic; Geology; Radiative transfer; Premelting; Atmospheric sciences; Sea ice; Boundary layer; Crystal (programming language); Forcing (mathematics); Infrared; Radiative forcing; Climatology; Meteorology; Materials science; Geomorphology; Oceanography; Physics; Optics; Climate change","score_opus":0.014541623356466577,"score_gpt":0.2075699438689088,"score_spread":0.19302832051244223,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2078024018","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":[0.9936337,0.00008181554,0.0030985319,0.0005192893,0.00009248282,0.00032995502,0.000025531048,0.000036490495,0.0021822138],"genre_scores_gemma":[0.9950479,0.000015553736,0.0024101567,0.0009304133,0.000023005556,0.000007219391,0.00002106774,0.000020774334,0.0015238939],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980254,0.00022943904,0.00024224412,0.0004011722,0.00064195157,0.00045978194],"domain_scores_gemma":[0.99923986,0.0002170874,0.00009589805,0.00034445853,0.000008520433,0.00009419186],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00039150502,0.00020965927,0.00020617347,8.709228e-7,0.00033872196,0.000013805709,0.00036987898,0.00008397309,0.0054924646],"category_scores_gemma":[0.00004146909,0.00014517468,0.00008191646,0.0003096937,0.00011885792,0.00015624714,0.00013697907,0.00017725013,0.0004092643],"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":[0.000053135722,0.00016389985,0.93697405,0.000002505641,0.000011884176,0.000026966529,0.002301449,0.054380767,0.004489949,0.000017394834,0.0015579974,0.000020014213],"study_design_scores_gemma":[0.0014993424,0.00006545426,0.9814731,0.00001332025,0.00001554115,0.0000044098165,0.00073556346,0.012785476,0.0014642508,0.00019239681,0.0014580492,0.00029308716],"about_ca_topic_score_codex":0.011251984,"about_ca_topic_score_gemma":0.004456268,"teacher_disagreement_score":0.04449907,"about_ca_system_score_codex":0.0004042985,"about_ca_system_score_gemma":0.000023827077,"threshold_uncertainty_score":0.99541664},"labels":[],"label_agreement":null},{"id":"W2078932557","doi":"10.1029/2009jd013019","title":"Detecting thin cirrus in Multiangle Imaging Spectroradiometer aerosol retrievals","year":2010,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":36,"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","funders":"","keywords":"Cirrus; Aerosol; Spectroradiometer; Remote sensing; Environmental science; Lidar; AERONET; Latitude; Satellite; Optical depth; Atmospheric sciences; Meteorology; Physics; Optics; Geology; Reflectivity; Astronomy","score_opus":0.019810900801654416,"score_gpt":0.31003052629090877,"score_spread":0.29021962548925434,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2078932557","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":[0.9939419,0.00012865437,0.00032504447,0.00052065577,0.00026791982,0.00017810566,9.4346433e-7,0.000015072285,0.004621691],"genre_scores_gemma":[0.9886971,0.000026547039,0.0100763915,0.000078970945,0.0004883084,0.0000053598505,2.172772e-7,0.000033978715,0.00059313345],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9962579,0.000260904,0.0006050885,0.00034723873,0.0016170118,0.00091182726],"domain_scores_gemma":[0.9982142,0.00067038025,0.0002516003,0.00036526602,0.00010545505,0.00039313312],"candidate_categories":["research_integrity","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0022129528,0.0002037539,0.0003898511,0.000006146233,0.00023088099,0.00014969237,0.0007853132,0.00008742445,0.0029813512],"category_scores_gemma":[0.0014999215,0.00015961027,0.0002085816,0.0011759319,0.0005495107,0.0005471899,0.00038060016,0.0023754165,0.0003376365],"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":[0.00033546868,0.00059424696,0.2786633,0.000015455158,0.00003237447,0.00059617433,0.00082618324,0.00040778005,0.6327149,0.000103449915,0.0028288427,0.08288181],"study_design_scores_gemma":[0.0031771509,0.0012856246,0.8704789,0.0001664965,0.000029727933,0.0002707109,0.0019133625,0.02527045,0.08024385,0.00913852,0.0071849665,0.00084020785],"about_ca_topic_score_codex":0.0020451483,"about_ca_topic_score_gemma":0.00076877786,"teacher_disagreement_score":0.59181565,"about_ca_system_score_codex":0.00027226622,"about_ca_system_score_gemma":0.00008652097,"threshold_uncertainty_score":0.99992615},"labels":[],"label_agreement":null},{"id":"W2079016599","doi":"10.1029/2011jd015889","title":"Testing cloud microphysics parameterizations in NCAR CAM5 with ISDAC and M-PACE observations","year":2011,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":143,"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":"U.S. Department of Energy","keywords":"Liquid water content; Environmental science; Cloud fraction; Atmospheric sciences; Liquid water path; Arctic; Cloud albedo; Cloud height; Aerosol; Cloud cover; Meteorology; Cloud computing; Geology; Physics","score_opus":0.07579127173364826,"score_gpt":0.2898487846094017,"score_spread":0.21405751287575348,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2079016599","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":[0.995716,0.000065287466,0.0009874335,0.00015939793,0.000034486715,0.00015093018,0.0000019670276,0.0000063056996,0.002878219],"genre_scores_gemma":[0.9479616,0.000034005385,0.051386923,0.000051991494,0.00010317728,0.000008320952,3.965867e-7,0.000020617896,0.00043291715],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981835,0.00015993364,0.00032793864,0.00022388708,0.00065940246,0.00044537484],"domain_scores_gemma":[0.9988474,0.00040061955,0.00017531673,0.00021086654,0.00013166337,0.00023412333],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038827915,0.00014393222,0.0002488696,0.0000022940994,0.00020194848,0.0000588385,0.0003276192,0.00005655211,0.0002893782],"category_scores_gemma":[0.0003647959,0.00010536677,0.00004834151,0.0010214674,0.0006140157,0.00036583462,0.00020890938,0.00055570033,0.00004888689],"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":[0.0002422159,0.0007451782,0.94371086,0.000021640673,0.00004644036,0.00016870927,0.0020766952,0.00085920625,0.033007357,0.0011981899,0.0012058847,0.016717594],"study_design_scores_gemma":[0.0004130188,0.00091621996,0.9902906,0.00007390551,0.00001354772,0.000021268314,0.0008038946,0.0014928343,0.00060568476,0.0045913113,0.0006298755,0.00014785638],"about_ca_topic_score_codex":0.0029305334,"about_ca_topic_score_gemma":0.00028149138,"teacher_disagreement_score":0.050399486,"about_ca_system_score_codex":0.00011329457,"about_ca_system_score_gemma":0.00008078461,"threshold_uncertainty_score":0.44301093},"labels":[],"label_agreement":null},{"id":"W2079102442","doi":"10.5194/acp-9-1847-2009","title":"Large surface radiative forcing from topographic blowing snow residuals measured in the High Arctic at Eureka","year":2009,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"Eurostars; Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency; Government of Canada; Canadian Foundation for Climate and Atmospheric Sciences; Ontario Innovation Trust; Goddard Space Flight Center; National Oceanic and Atmospheric Administration; Nova Scotia Research Innovation Trust; National Aeronautics and Space Administration","keywords":"Snow; Arctic; Ice crystals; Atmospheric sciences; Geology; Radiative transfer; Forcing (mathematics); Boundary layer; Radiosonde; Premelting; Sea ice; Climatology; Environmental science; Meteorology; Geomorphology; Materials science; Oceanography; Optics; Physics","score_opus":0.0060753581255345405,"score_gpt":0.20178558776522096,"score_spread":0.19571022963968643,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2079102442","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":[0.9957566,0.00036954676,0.00071438676,0.0003203995,0.000027401731,0.00014320092,0.0000102470885,0.000026115904,0.0026320852],"genre_scores_gemma":[0.9955048,0.00010441375,0.002906763,0.0005978268,0.00011337255,0.00000680833,0.000024565756,0.000013775516,0.0007276938],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99860483,0.00006460378,0.00020628347,0.00041629493,0.00032957274,0.0003784114],"domain_scores_gemma":[0.9993208,0.00015665118,0.00009202178,0.0003397371,0.000007425196,0.0000833469],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00023161327,0.00023531649,0.00023458786,1.6487752e-8,0.00027350275,0.000045528443,0.0002590519,0.000096546595,0.0012155769],"category_scores_gemma":[0.00002611249,0.00018728271,0.00007898834,0.00039098173,0.000116383,0.00014008554,0.0000760099,0.00023015765,0.000021981477],"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":[0.000174816,0.00072117883,0.8126154,0.000054024935,0.00011880434,0.000086799024,0.015734658,0.025754567,0.09508906,0.00021175994,0.002281268,0.047157664],"study_design_scores_gemma":[0.0024276678,0.00013243024,0.92895055,0.00014910074,0.00014769944,0.000013511954,0.0025444613,0.019190535,0.020592302,0.020751556,0.0039528366,0.001147334],"about_ca_topic_score_codex":0.0007305413,"about_ca_topic_score_gemma":0.000055132376,"teacher_disagreement_score":0.11633517,"about_ca_system_score_codex":0.000105667634,"about_ca_system_score_gemma":0.000009527334,"threshold_uncertainty_score":0.99969745},"labels":[],"label_agreement":null},{"id":"W2080174470","doi":"10.1029/2002jd003207","title":"Remote sensing of smoke, land, and clouds from the NASA ER‐2 during SAFARI 2000","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","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":"McGill University; University of Wisconsin-Madison; National Aeronautics and Space Administration","keywords":"Remote sensing; Moderate-resolution imaging spectroradiometer; Environmental science; Spectroradiometer; AERONET; Lidar; Radiometer; Satellite; Albedo (alchemy); Aerosol; Meteorology; Geography; Reflectivity; Physics","score_opus":0.023106668479599732,"score_gpt":0.2836984621453485,"score_spread":0.26059179366574875,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2080174470","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":[0.99534595,0.00053695636,0.0004302735,0.00037563572,0.00007958591,0.00010568657,0.0000029526943,0.0000048191446,0.0031181602],"genre_scores_gemma":[0.9926565,0.0002690089,0.0061414796,0.000056937093,0.00020614293,2.0242257e-7,2.6377396e-7,0.000019058993,0.0006504062],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99728703,0.00041722183,0.00042051202,0.00022474874,0.0011774941,0.00047299184],"domain_scores_gemma":[0.9983802,0.0007662012,0.00022149863,0.0003069055,0.00008589089,0.00023933966],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009169589,0.0001531106,0.0003233987,0.0000010067016,0.0003012806,0.000064664746,0.00034688626,0.000081607686,0.0009865188],"category_scores_gemma":[0.0005865874,0.00009526337,0.00013445407,0.0003927851,0.00068790256,0.00016263482,0.00023443093,0.00072387053,0.000042233096],"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":[0.0011943601,0.0004536474,0.7211561,0.000057914305,0.00037880038,0.00035244654,0.003081704,0.0017839012,0.07073396,0.00040871347,0.0069682784,0.19343017],"study_design_scores_gemma":[0.0011163115,0.00048053608,0.97106594,0.00013808293,0.00003429122,0.00006081166,0.0009541442,0.0023614285,0.006110208,0.010815024,0.006653194,0.0002100224],"about_ca_topic_score_codex":0.0067875087,"about_ca_topic_score_gemma":0.00025829312,"teacher_disagreement_score":0.24990983,"about_ca_system_score_codex":0.0001386595,"about_ca_system_score_gemma":0.000087101456,"threshold_uncertainty_score":0.9999267},"labels":[],"label_agreement":null},{"id":"W2082238833","doi":"10.1175/jtech2033.1","title":"The Atmospheric Radiation Measurement Program Cloud Profiling Radars: Second-Generation Sampling Strategies, Processing, and Cloud Data Products","year":2007,"lang":"en","type":"article","venue":"Journal of Atmospheric and Oceanic Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":181,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Remote sensing; Radar; Doppler effect; Doppler radar; Computer science; Environmental science; Cloud computing; Ceilometer; Sampling (signal processing); Meteorology; Filter (signal processing); Physics; Geology; Telecommunications; Lidar","score_opus":0.02682349040637729,"score_gpt":0.2663336155802584,"score_spread":0.23951012517388112,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082238833","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":[0.9621673,0.014206803,0.021240385,0.00081949815,0.0006965569,0.00054471206,0.0000012821081,0.000094675815,0.00022876577],"genre_scores_gemma":[0.8958982,0.0011587045,0.10209944,0.00007624225,0.00065345346,0.0000057298066,0.0000030413844,0.000030745094,0.00007440748],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99759835,0.00005151944,0.00079288287,0.00048179924,0.00056677515,0.00050868903],"domain_scores_gemma":[0.99841166,0.00004138044,0.00083379704,0.00046184703,0.00012195323,0.00012938582],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002253871,0.00027226948,0.00032327804,0.0000012556538,0.00057592744,0.00019624403,0.000590955,0.00022137372,0.000038796232],"category_scores_gemma":[0.00020922147,0.00018990242,0.000034990262,0.00070118596,0.0005041453,0.00059794635,0.0003452458,0.00048023177,0.00000264504],"study_design_candidate":"design_other","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":[0.00010930782,0.0001743775,0.022409007,0.000055130102,0.00008305893,0.000021375805,0.00031688105,0.00020193048,0.014620394,0.0007001733,0.002553771,0.9587546],"study_design_scores_gemma":[0.005047666,0.0050130426,0.16145207,0.00030575748,0.0006186906,0.0025823517,0.01994924,0.06073293,0.008765925,0.0056793033,0.72774905,0.0021039962],"about_ca_topic_score_codex":0.00001643887,"about_ca_topic_score_gemma":0.000082405015,"teacher_disagreement_score":0.9566506,"about_ca_system_score_codex":0.00023167998,"about_ca_system_score_gemma":0.00020632005,"threshold_uncertainty_score":0.77439964},"labels":[],"label_agreement":null},{"id":"W2082734341","doi":"10.1007/s00024-007-0214-7","title":"Inferring Low Cloud Base Heights at Night for Aviation Using Satellite Infrared and Surface Temperature Data","year":2007,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":35,"is_retracted":false,"has_abstract":false,"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 Oceanic and Atmospheric Administration","keywords":"Cloud base; Overcast; Environmental science; Geostationary orbit; Cirrus; Cloud top; Remote sensing; Brightness temperature; Meteorology; Cloud cover; Cloud computing; Geostationary Operational Environmental Satellite; Satellite; Cloud height; Relative humidity; Atmospheric sciences; Brightness; Geology; Geography; Optics; Computer science; Physics; Engineering; Aerospace engineering","score_opus":0.014055281408649714,"score_gpt":0.22835892064917895,"score_spread":0.21430363924052925,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082734341","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":[0.99552214,0.00020608955,0.0028672053,0.00002218389,0.00008140605,0.00029764284,0.000029714673,0.000024049825,0.0009495899],"genre_scores_gemma":[0.99217963,0.00007361457,0.0068142843,0.00021377267,0.00023377893,0.0000032296664,0.00010989109,0.00001914267,0.00035265577],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99901175,0.00000642627,0.00015398176,0.00039179742,0.00015111867,0.00028494635],"domain_scores_gemma":[0.9994604,0.00005262823,0.00007334324,0.00029831548,0.0000059629183,0.00010937379],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017312805,0.0001640064,0.00015082148,0.0000010130077,0.00030763922,0.000055094388,0.00012662496,0.000098674755,0.00002835869],"category_scores_gemma":[0.0000036927836,0.00014199002,0.000017936647,0.00012241241,0.00008583329,0.0001826228,0.00032837782,0.00009474162,0.000012632462],"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":[0.00038347888,0.00024145548,0.06677883,0.00024119153,0.00008215082,0.000013344404,0.0038995484,0.003048605,0.84349906,0.004781603,0.0018323101,0.07519842],"study_design_scores_gemma":[0.008497746,0.00042486875,0.48251572,0.00028210727,0.0006304502,0.000056769117,0.0022616426,0.05731501,0.25467497,0.06001858,0.12813504,0.0051871063],"about_ca_topic_score_codex":0.000033557022,"about_ca_topic_score_gemma":0.00006677303,"teacher_disagreement_score":0.5888241,"about_ca_system_score_codex":0.000048874965,"about_ca_system_score_gemma":0.0000064718397,"threshold_uncertainty_score":0.57901853},"labels":[],"label_agreement":null},{"id":"W2083458282","doi":"10.1175/2007jas2355.1","title":"The Effect of Dynamics on Mixed-Phase Clouds: Theoretical Considerations","year":2008,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":141,"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":"Mechanics; Liquid water content; Non-equilibrium thermodynamics; Oscillation (cell signaling); Cloud physics; Turbulence; Saturation (graph theory); Mixed phase; Environmental science; Cloud computing; Meteorology; Ice cloud; Phase (matter); Physics; Atmospheric sciences; Geology; Thermodynamics; Mathematics; Chemistry; Computer science","score_opus":0.007703102793474047,"score_gpt":0.2507785825395452,"score_spread":0.24307547974607116,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2083458282","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":[0.9915331,0.00012058767,0.00020074338,0.0023126455,0.0006978736,0.00012432701,0.0000010868487,0.000005248045,0.005004367],"genre_scores_gemma":[0.99781615,0.00006944761,0.0016775066,0.00021207117,0.00006128617,0.0000022142142,3.575188e-8,0.0000062421796,0.00015504443],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9980523,0.00028345783,0.00042826106,0.0001422577,0.0008484017,0.00024534843],"domain_scores_gemma":[0.99803656,0.0011078431,0.00047846086,0.0002664251,0.000023170836,0.00008752106],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0013372338,0.00013343428,0.00021977993,3.8144265e-7,0.0011381144,0.000040531817,0.00078268995,0.00004397977,0.0006361916],"category_scores_gemma":[0.00063556695,0.000054964647,0.0002091344,0.00046222252,0.004546152,0.00012789272,0.00015461468,0.0002129951,0.000019803669],"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":[0.0009493383,0.00094898476,0.4943618,0.00001904122,0.00022662795,0.00014367868,0.0023016399,0.25199726,0.0053478084,0.14752178,0.05946097,0.036721073],"study_design_scores_gemma":[0.009063164,0.033303637,0.2406163,0.00036642645,0.0005317672,0.0047548404,0.0043435623,0.5476328,0.03606028,0.11421937,0.007560451,0.0015473887],"about_ca_topic_score_codex":0.000024132783,"about_ca_topic_score_gemma":0.000014867548,"teacher_disagreement_score":0.29563555,"about_ca_system_score_codex":0.00010127056,"about_ca_system_score_gemma":0.00006640587,"threshold_uncertainty_score":0.9981629},"labels":[],"label_agreement":null},{"id":"W2084113589","doi":"10.1029/2007jd008658","title":"Evaluation of regional cloud climate simulations over Scandinavia using a 10‐year NOAA Advanced Very High Resolution Radiometer cloud climatology","year":2008,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":12,"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":"","keywords":"Cloud cover; Environmental science; Climatology; Satellite; Cloud fraction; Cloud computing; Downwelling; Radiometer; Advanced very-high-resolution radiometer; Cloud top; Meteorology; Climate model; International Satellite Cloud Climatology Project; Atmospheric sciences; Longwave; Cloud albedo; Climate change; Remote sensing; Geography; Radiation; Geology; Computer science","score_opus":0.06971986563071153,"score_gpt":0.35527247722215827,"score_spread":0.28555261159144674,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2084113589","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":[0.9977696,0.0002519732,0.0007689958,0.00012632052,0.000246072,0.0002689001,0.000010733861,0.00000908588,0.0005483306],"genre_scores_gemma":[0.9921878,0.00019325282,0.006954179,0.000029158527,0.0004528871,0.0000055614464,0.0000048951715,0.000028146023,0.00014411482],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9940148,0.00085282145,0.00074563234,0.00032987545,0.003370341,0.00068654673],"domain_scores_gemma":[0.997697,0.00056163,0.00052648253,0.0003463521,0.00060958555,0.00025896667],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0020892634,0.0002007727,0.00048082776,0.00000929362,0.00046081768,0.000025328018,0.00040150993,0.00015288043,0.0034764623],"category_scores_gemma":[0.0006929562,0.00016879874,0.0002482652,0.0009239301,0.00097822,0.000512492,0.000266825,0.000550977,0.00009436706],"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":[0.007392045,0.0033004333,0.2898384,0.00011542488,0.000593379,0.00022825268,0.0015895589,0.52481836,0.12585628,0.0025820907,0.02653823,0.017147519],"study_design_scores_gemma":[0.006064085,0.002552593,0.7229468,0.00025384416,0.000276049,0.00019555545,0.00048129892,0.25123194,0.001923449,0.010828901,0.002707701,0.00053772196],"about_ca_topic_score_codex":0.00064416707,"about_ca_topic_score_gemma":0.000052123905,"teacher_disagreement_score":0.43310845,"about_ca_system_score_codex":0.00076119957,"about_ca_system_score_gemma":0.00026717928,"threshold_uncertainty_score":0.9974345},"labels":[],"label_agreement":null},{"id":"W2084337506","doi":"10.1364/isa.2014.jtu2c.7","title":"CALIBRATION METHOD FOR PARTICLE CONCENTRATION MAPPING BASED ON LIDAR INVERSION","year":2014,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Institut National d'Optique","funders":"","keywords":"Lidar; Calibration; Remote sensing; Particle (ecology); Environmental science; Inversion (geology); Materials science; Geology; Mathematics; Statistics","score_opus":0.013612605529482425,"score_gpt":0.23842503216040395,"score_spread":0.22481242663092152,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2084337506","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.19060814,4.5799385e-7,0.8019799,0.0010689909,0.000045568442,0.00014910007,4.5759487e-7,0.000033269433,0.0061141243],"genre_scores_gemma":[0.89293087,2.1842523e-7,0.10413429,0.0024180934,0.000026813448,0.000015158542,0.000005125437,0.0000051641746,0.00046427312],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99945533,0.00004658359,0.000093581075,0.00015826919,0.00012123475,0.00012499548],"domain_scores_gemma":[0.99972945,0.00007958204,0.00003461053,0.000100864636,0.000003193118,0.000052268002],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021775585,0.000056742763,0.00005418551,2.99452e-7,0.000103845436,0.000019819769,0.000050433464,0.000033539,0.0011360687],"category_scores_gemma":[0.000033252345,0.000046379046,0.000028021495,0.00007110189,0.000022393384,0.00010389777,0.00001431332,0.000023709763,0.000058144313],"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":[0.00021446578,0.00032029074,0.23037323,0.00003161988,0.000010903104,7.164363e-7,0.0009341633,0.15383057,0.3751209,0.0251156,0.026018305,0.18802921],"study_design_scores_gemma":[0.0003232592,0.00011215558,0.0053179543,0.0000024660146,0.0000031034422,6.241798e-8,0.000050003422,0.94744766,0.0368097,0.00030532439,0.009560065,0.00006825417],"about_ca_topic_score_codex":0.00007389737,"about_ca_topic_score_gemma":0.000013778897,"teacher_disagreement_score":0.79361707,"about_ca_system_score_codex":0.00004651178,"about_ca_system_score_gemma":0.0000037836062,"threshold_uncertainty_score":0.999777},"labels":[],"label_agreement":null},{"id":"W2084416227","doi":"10.1117/12.482312","title":"Active probing of cloud multiple scattering, optical depth, vertical thickness, and liquid water content using wide-angle imaging lidar","year":2002,"lang":"en","type":"article","venue":"Proceedings of SPIE, the International Society for Optical Engineering/Proceedings of SPIE","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":7,"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":"Los Alamos National Laboratory; Goddard Space Flight Center; Laboratory Directed Research and Development; McGill University; U.S. Department of Energy","keywords":"Lidar; Scattering; Optics; Liquid water content; Radiative transfer; Physics; Forward scatter; Cloud chamber; Cloud physics; Remote sensing; Cloud computing; Optical depth; Meteorology; Geology; Computer science","score_opus":0.01596031623258174,"score_gpt":0.21084816068843032,"score_spread":0.19488784445584859,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2084416227","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":[0.99630827,0.00006599311,0.00019082233,0.0013958017,0.00015238705,0.0004590811,0.000009122257,0.000046511042,0.0013719894],"genre_scores_gemma":[0.95389587,0.000039010974,0.04564659,0.00012160447,0.00014234189,0.000048113896,0.0000019934253,0.00005190997,0.00005254439],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99769074,4.5685717e-8,0.0006623978,0.00046170686,0.0006643534,0.0005207625],"domain_scores_gemma":[0.9990946,0.00015438936,0.00019586223,0.0000673874,0.00031935895,0.0001683845],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00038077144,0.0003285,0.00043869836,0.000011636331,0.0001273937,0.000075057076,0.0005813551,0.00015444364,0.00009524113],"category_scores_gemma":[0.00046232538,0.0002469869,0.0003697323,0.00016527725,0.0007555661,0.0006097885,0.00050312636,0.00030390552,0.0000036067381],"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":[0.00016481546,0.00018982156,0.009845549,0.00019778969,0.00018173752,3.3885055e-7,0.0008672589,0.00026588872,0.9763736,0.0111485375,0.00028731415,0.00047732],"study_design_scores_gemma":[0.0017182541,0.0004801503,0.006822622,0.0004977904,0.00025276316,0.00006575807,0.0029239117,0.15742014,0.8281449,0.00029120207,0.0007591415,0.00062333135],"about_ca_topic_score_codex":0.000045580644,"about_ca_topic_score_gemma":5.443962e-7,"teacher_disagreement_score":0.15715426,"about_ca_system_score_codex":0.00021521786,"about_ca_system_score_gemma":0.0000077222185,"threshold_uncertainty_score":0.9999982},"labels":[],"label_agreement":null},{"id":"W2084826907","doi":"10.1175/jtech2045.1","title":"Lidar-Based Characterization of the Geometry and Structure of Water Clouds","year":2007,"lang":"en","type":"article","venue":"Journal of Atmospheric and Oceanic Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Defence Research and Development Canada","funders":"","keywords":"Lidar; Azimuth; Range (aeronautics); Remote sensing; Autocorrelation; Elevation (ballistics); Liquid water content; Histogram; Environmental science; Ranging; Geology; Meteorology; Physics; Geometry; Cloud computing; Geodesy; Optics; Materials science; Computer science; Mathematics","score_opus":0.002417281386639207,"score_gpt":0.182637892830821,"score_spread":0.18022061144418178,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2084826907","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":[0.99515355,0.0001479045,0.004120298,0.0003393906,0.0001138474,0.00006523531,0.0000018021857,0.0000066823286,0.00005131623],"genre_scores_gemma":[0.99569494,0.00005391848,0.0040801424,0.00009306048,0.00002171161,9.826316e-8,2.6988675e-7,0.000008774621,0.000047102618],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99912345,0.000015139127,0.00040356707,0.00010560791,0.00018465768,0.00016755945],"domain_scores_gemma":[0.9993423,0.000019578962,0.00041800895,0.00015003806,0.000027714097,0.000042317966],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018918813,0.00010353915,0.00024147333,0.0000017227919,0.000054689302,0.000004394867,0.0002080468,0.00017179202,0.00025639948],"category_scores_gemma":[0.000024333902,0.000056967187,0.00004908973,0.00034394508,0.0004739303,0.000066427245,0.00013618336,0.00019548486,4.6309523e-7],"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":[0.000053927895,0.000038245653,0.39487234,0.000017614191,0.000019804507,0.000003970678,0.00012387049,0.000031043357,0.5863079,0.00012842774,0.000017876873,0.018385015],"study_design_scores_gemma":[0.000568182,0.00041104248,0.77100956,0.00003100219,0.000047966987,0.000121224635,0.00029096944,0.00019202038,0.22507025,0.00081987196,0.0013364997,0.00010138342],"about_ca_topic_score_codex":0.00000702811,"about_ca_topic_score_gemma":0.0000027807969,"teacher_disagreement_score":0.37613723,"about_ca_system_score_codex":0.00002908652,"about_ca_system_score_gemma":0.000013369292,"threshold_uncertainty_score":0.28073946},"labels":[],"label_agreement":null},{"id":"W2085213147","doi":"10.1007/s11434-011-4405-3","title":"Dust direct radiative effects on the earth-atmosphere system over east Asia: Early spring cooling and late spring warming","year":2011,"lang":"en","type":"article","venue":"Chinese Science Bulletin","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":11,"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":"Chinese Academy of Meteorological Sciences; National Natural Science Foundation of China","keywords":"Radiative forcing; Atmospheric sciences; Albedo (alchemy); Environmental science; Radiative transfer; Atmosphere (unit); Cloud forcing; Forcing (mathematics); Radiative cooling; Climatology; Dust storm; Altitude (triangle); Atmospheric radiative transfer codes; Aerosol; Physics; Meteorology; Geology","score_opus":0.0067275922235248515,"score_gpt":0.18721902903876356,"score_spread":0.18049143681523871,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2085213147","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":[0.9667641,0.000089560526,0.00017901996,0.00014589653,0.00027762895,0.00034690995,8.740431e-7,0.0000957375,0.032100286],"genre_scores_gemma":[0.99784416,0.000008942711,0.0014109801,0.00014832891,0.00009699137,0.000025546813,6.357683e-8,0.000026043119,0.0004389651],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99785995,0.00008506748,0.0002218635,0.00068360515,0.0005615473,0.0005879517],"domain_scores_gemma":[0.9990374,0.00016233754,0.00014485663,0.0004141674,0.000013827233,0.00022742261],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009948344,0.00029256975,0.00024763183,0.0000029661394,0.00094857404,0.00015025875,0.0005583959,0.00006429122,0.0005301526],"category_scores_gemma":[0.00019687918,0.0001815015,0.000066615,0.0005862132,0.0007465716,0.00020369393,0.00048650248,0.00027925326,0.000571572],"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":[0.00007965111,0.000069533744,0.9700219,0.000059291622,0.000023791288,0.00011048375,0.0069090375,0.0017197815,0.013535558,0.001406239,0.0001085912,0.005956108],"study_design_scores_gemma":[0.00026423702,0.00009324268,0.98858833,0.00016723249,0.000012256915,0.0000076264864,0.00041335044,0.007072728,0.0023609176,0.000018774725,0.00071054476,0.0002907814],"about_ca_topic_score_codex":0.0017890033,"about_ca_topic_score_gemma":0.000044167544,"teacher_disagreement_score":0.03166132,"about_ca_system_score_codex":0.00013429899,"about_ca_system_score_gemma":0.00001953974,"threshold_uncertainty_score":0.74014163},"labels":[],"label_agreement":null},{"id":"W2085858998","doi":"10.1175/2010mwr3473.1","title":"Interpolation of LES Cloud Surfaces for Use in Direct Calculations of Entrainment and Detrainment","year":2010,"lang":"en","type":"article","venue":"Monthly Weather Review","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":92,"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":"Entrainment (biomusicology); Interpolation (computer graphics); Grid; Meteorology; Physics; Offset (computer science); Cloud computing; Environmental science; Atmospheric sciences; Geology; Geodesy; Computer science; Classical mechanics","score_opus":0.016232446523365796,"score_gpt":0.2506780016150652,"score_spread":0.2344455550916994,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2085858998","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":[0.98968476,0.0076627764,0.00051970535,0.00015396207,0.000044559925,0.0006595443,0.000021500955,0.0000052413147,0.0012479507],"genre_scores_gemma":[0.9898925,0.0027804237,0.0071500195,0.000055663393,0.000006227044,0.000039424092,0.0000035734593,0.000007856289,0.000064324464],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993454,0.000031776235,0.00027812604,0.00013964623,0.00011085905,0.00009419552],"domain_scores_gemma":[0.99963576,0.00006746274,0.00011993877,0.00014047475,0.000005440249,0.0000309078],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029477966,0.00008032415,0.00020765586,0.0000013714595,0.000022098979,0.000004122994,0.0000661676,0.00003308715,0.00045496496],"category_scores_gemma":[0.00003549272,0.00006284676,0.000053482916,0.0000747494,0.00009599966,0.00006352423,0.000038279246,0.000044754186,0.0000014503663],"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":[0.000021486676,0.00029190452,0.84612596,0.0006831942,0.000030265104,6.6429425e-7,0.0011242812,0.00032678706,0.03456456,0.0005584568,0.000766544,0.11550591],"study_design_scores_gemma":[0.0010515369,0.00030596647,0.846519,0.0020140256,0.0001783402,0.0000016526903,0.00020858498,0.017192617,0.0036266665,0.0005382268,0.12787989,0.00048350354],"about_ca_topic_score_codex":0.00042639993,"about_ca_topic_score_gemma":0.001179371,"teacher_disagreement_score":0.12711334,"about_ca_system_score_codex":0.000020831396,"about_ca_system_score_gemma":0.0000034171585,"threshold_uncertainty_score":0.4981547},"labels":[],"label_agreement":null},{"id":"W2086190558","doi":"10.1175/2010jamc2468.1","title":"Clouds at Arctic Atmospheric Observatories. Part II: Thermodynamic Phase Characteristics","year":2010,"lang":"en","type":"article","venue":"Journal of Applied Meteorology and Climatology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":317,"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":"U.S. Department of Energy","keywords":"Liquid water content; Radiosonde; Environmental science; Arctic; Atmospheric sciences; Troposphere; Lidar; Ice nucleus; Liquid water; Microwave radiometer; Cloud physics; Climatology; Meteorology; Cloud computing; Radiometer; Geology; Oceanography; Remote sensing; Geography; Physics","score_opus":0.00684798501417151,"score_gpt":0.22579407464349346,"score_spread":0.21894608962932197,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2086190558","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":[0.99499255,0.00008564679,0.0001513789,0.00052309147,0.0010767549,0.00011473433,0.000004232906,0.000017175093,0.0030344373],"genre_scores_gemma":[0.994346,0.00022590697,0.004069253,0.0010069492,0.00015773084,0.000011344687,0.000004446676,0.000024239493,0.0001540804],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983619,0.000052697113,0.0006548608,0.0002891132,0.00018178955,0.00045966305],"domain_scores_gemma":[0.9986648,0.00014823997,0.0006670207,0.00026630412,0.00002681895,0.00022683304],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00047395876,0.0002441997,0.0006249013,0.0000015017725,0.00034246917,0.000011405907,0.00031038144,0.00036667468,0.0040219394],"category_scores_gemma":[0.000055680375,0.00019459093,0.00010093972,0.00013949236,0.0008915235,0.000087983906,0.00033066227,0.00068326114,0.000070564194],"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":[0.0037069514,0.0012390527,0.6888226,0.000058213755,0.0003594624,0.00035548184,0.001748371,0.000041209052,0.23520146,0.028520646,0.002459797,0.037486695],"study_design_scores_gemma":[0.015287824,0.005855299,0.597784,0.000028950579,0.0012266772,0.009916008,0.00096521736,0.004413839,0.0032831249,0.037031155,0.32228976,0.0019181517],"about_ca_topic_score_codex":0.0000088068455,"about_ca_topic_score_gemma":0.000052652616,"teacher_disagreement_score":0.31982997,"about_ca_system_score_codex":0.000058416565,"about_ca_system_score_gemma":0.000028651619,"threshold_uncertainty_score":0.9968885},"labels":[],"label_agreement":null},{"id":"W2086836345","doi":"10.1175/jcli-d-12-00112.1","title":"Longwave Band-By-Band Cloud Radiative Effect and Its Application in GCM Evaluation","year":2012,"lang":"en","type":"article","venue":"Journal of Climate","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":17,"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","funders":"National Oceanic and Atmospheric Administration; Goddard Space Flight Center; Langley Research Center; University of Michigan; National Aeronautics and Space Administration; National Science Foundation","keywords":"Longwave; Outgoing longwave radiation; Environmental science; GCM transcription factors; Climatology; Cirrus; Radiative transfer; Atmospheric sciences; Climate model; Amplitude; Atmospheric Infrared Sounder; Meteorology; Physics; Climate change; Geology; Troposphere; General Circulation Model; Convection; Optics","score_opus":0.007303169858864641,"score_gpt":0.26485197213775286,"score_spread":0.2575488022788882,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2086836345","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":[0.99477005,0.0010026143,0.0002539949,0.000096743745,0.00012485424,0.0002057342,0.000002008261,0.0000026865898,0.0035413173],"genre_scores_gemma":[0.99922585,0.00047791406,0.00008767025,0.00006026631,0.00011156199,0.000008378144,0.0000015136375,0.000007128175,0.000019710342],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990379,0.00012150665,0.00025307317,0.00008449876,0.00030699227,0.00019599857],"domain_scores_gemma":[0.9994751,0.00007216949,0.00027957105,0.000059457987,0.000012336471,0.0001013567],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015293385,0.00008489239,0.00015708662,0.0000026473965,0.000048632883,0.00001337222,0.00006860506,0.000049912218,0.00026100574],"category_scores_gemma":[0.000051226998,0.000064151944,0.00003293417,0.00010251804,0.000033710043,0.0003312178,0.000022974715,0.00011736628,0.000052804644],"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":[0.00014789416,0.00011968329,0.93308955,0.000019571859,0.000015473752,0.0000019027933,0.000905961,0.0011138883,0.03142962,0.00004420943,0.0007975383,0.032314695],"study_design_scores_gemma":[0.0024782442,0.00044886983,0.9623103,0.000047464124,0.000104010105,0.00005532424,0.00016232267,0.0100525115,0.021490147,0.00037733658,0.0022419912,0.00023148049],"about_ca_topic_score_codex":0.00001280601,"about_ca_topic_score_gemma":0.0000072050966,"teacher_disagreement_score":0.032083217,"about_ca_system_score_codex":0.00014607015,"about_ca_system_score_gemma":0.0000057926172,"threshold_uncertainty_score":0.285783},"labels":[],"label_agreement":null},{"id":"W2087530478","doi":"10.1007/s00340-013-5357-x","title":"Diffuse surface calibration method to improve accuracy and dynamic range of aerosol elastic light scattering measurements","year":2013,"lang":"en","type":"article","venue":"Applied Physics B","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":5,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada; Carleton University","funders":"","keywords":"Rayleigh scattering; Optics; Calibration; Photodiode; Detector; Scattering; Integrating sphere; Photomultiplier; Elastic scattering; Physics; Light scattering; Dynamic range; Materials science; Computational physics","score_opus":0.010476860550583568,"score_gpt":0.23409139753849573,"score_spread":0.22361453698791217,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2087530478","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":[0.8715631,0.000006576089,0.12669209,0.00008612513,0.00003839261,0.00051057874,0.0000028920724,0.000021524695,0.001078774],"genre_scores_gemma":[0.9792367,0.0000023610535,0.020396775,0.00016877092,0.00001998672,0.00006464079,0.0000023044186,0.000021726404,0.00008668622],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9990416,0.00002116369,0.00018303767,0.00029724362,0.00024625132,0.00021070142],"domain_scores_gemma":[0.9995062,0.000049262966,0.00010295034,0.0002293265,0.000008186963,0.00010410592],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000090289366,0.000151875,0.00017442512,6.310675e-7,0.00007362276,0.000035522397,0.00014507242,0.00004065954,0.0001718596],"category_scores_gemma":[0.000005859354,0.0001359404,0.00002782227,0.00014131663,0.000048263057,0.0001855925,0.00019281502,0.00006782113,0.00014137653],"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":[0.000008774724,0.00006562965,0.004471223,0.0000141578985,0.000011498431,7.877502e-8,0.00039763434,0.0024665182,0.97785324,0.00004536043,0.00010849948,0.014557385],"study_design_scores_gemma":[0.0021972267,0.00019238895,0.08382901,0.00004312926,0.00011027897,0.000001321504,0.00034916878,0.07713916,0.832229,0.002781968,0.00012539802,0.0010019399],"about_ca_topic_score_codex":0.00031596274,"about_ca_topic_score_gemma":0.0000116590545,"teacher_disagreement_score":0.14562424,"about_ca_system_score_codex":0.000054130975,"about_ca_system_score_gemma":0.000004850537,"threshold_uncertainty_score":0.5543488},"labels":[],"label_agreement":null},{"id":"W2087949442","doi":"10.1016/j.atmosres.2007.10.004","title":"Spectral aerosol optical properties from AERONET Sun-photometric measurements over West Africa","year":2007,"lang":"en","type":"article","venue":"Atmospheric Research","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":68,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Angstrom exponent; AERONET; Aerosol; Single-scattering albedo; Environmental science; Mineral dust; Atmospheric sciences; Effective radius; Cape verde; Climatology; Physics; Meteorology; Geology; Astrophysics","score_opus":0.09377873170877585,"score_gpt":0.3164581359401695,"score_spread":0.22267940423139368,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2087949442","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":[0.9094804,0.0006529101,0.0011938107,0.00015070238,0.00029334956,0.00063736713,0.0000031573368,0.00010659941,0.08748171],"genre_scores_gemma":[0.9758316,0.00007822031,0.014024338,0.00009702318,0.00027356067,0.00006478935,0.000004713562,0.00007194099,0.009553814],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99300957,0.00020512014,0.00056661817,0.0009822268,0.0032957087,0.0019407482],"domain_scores_gemma":[0.9980914,0.0002780375,0.00009221329,0.000826553,0.00007376534,0.0006380523],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0025526632,0.0003733014,0.00038567316,0.0000031084448,0.00053868187,0.00020086762,0.0009501038,0.0002397794,0.021470277],"category_scores_gemma":[0.00034377276,0.00030205952,0.0001423781,0.0028932784,0.0009386905,0.0003696731,0.0007785837,0.0008107339,0.004561532],"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":[0.00061357627,0.001250423,0.7302235,0.000023970406,0.0001524179,0.00023792573,0.0017684071,0.000704298,0.19619823,0.000073347146,0.037208937,0.03154501],"study_design_scores_gemma":[0.0015302978,0.00081983465,0.93877214,0.000047778045,0.000036119483,0.000012564525,0.0010406778,0.002123536,0.03150794,0.00033302442,0.022847202,0.00092889],"about_ca_topic_score_codex":0.0059140534,"about_ca_topic_score_gemma":0.00065968384,"teacher_disagreement_score":0.20854868,"about_ca_system_score_codex":0.0009363637,"about_ca_system_score_gemma":0.00007558256,"threshold_uncertainty_score":0.99994314},"labels":[],"label_agreement":null},{"id":"W2088421352","doi":"10.5194/acp-13-4515-2013","title":"A pervasive and persistent Asian dust event over North America during spring 2010: lidar and sunphotometer observations","year":2013,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université de Sherbrooke; Environment and Climate Change Canada; University of British Columbia","funders":"Office of Naval Research; U.S. Naval Research Laboratory; Natural Sciences and Engineering Research Council of Canada; National Oceanic and Atmospheric Administration","keywords":"AERONET; Depolarization ratio; Lidar; HYSPLIT; Environmental science; Aerosol; Asian Dust; Mineral dust; Troposphere; Atmospheric sciences; Climatology; Meteorology; Geology; Geography; Remote sensing","score_opus":0.006781270804673467,"score_gpt":0.1821780890349612,"score_spread":0.17539681823028772,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2088421352","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":[0.9981152,0.00013551237,0.00015286212,0.00020708809,0.000021052696,0.00015833002,0.0000047681146,0.000025468142,0.0011797076],"genre_scores_gemma":[0.9918198,0.0001843047,0.005111822,0.00012901492,0.00006600285,0.00004111532,0.0000054674506,0.000019232957,0.002623213],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999016,0.000009861778,0.00015526824,0.00038876364,0.00015882641,0.00027132002],"domain_scores_gemma":[0.99948925,0.000017731152,0.0000781054,0.00020426334,0.000010773638,0.00019984893],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000020533918,0.00021396566,0.00018132287,2.8762338e-8,0.00030160852,0.000077698154,0.00008914514,0.00005855514,0.001859344],"category_scores_gemma":[0.0000063056104,0.00020023776,0.000060746504,0.00015560674,0.0002654896,0.00024588313,0.000203687,0.00014588988,0.00002233564],"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":[0.000010706888,0.00009815093,0.9238998,0.00009913917,0.00006816052,0.000006657633,0.0015860623,0.00039835987,0.025293978,0.0000036100148,0.00015861126,0.048376758],"study_design_scores_gemma":[0.00029678675,0.00003185954,0.9888466,0.000015951106,0.00004032586,0.0000116138335,0.000786587,0.007578941,0.00048424382,0.00003368902,0.0015843606,0.00028903957],"about_ca_topic_score_codex":0.001203283,"about_ca_topic_score_gemma":0.000015258798,"teacher_disagreement_score":0.0649468,"about_ca_system_score_codex":0.000057364145,"about_ca_system_score_gemma":0.0000065018853,"threshold_uncertainty_score":0.9990531},"labels":[],"label_agreement":null},{"id":"W2088560779","doi":"10.5194/acp-8-6939-2008","title":"Global simulations of aerosol processing in clouds","year":2008,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":91,"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","funders":"","keywords":"Aerosol; Atmospheric sciences; Scavenging; Environmental science; Ice nucleus; Boundary layer; Particle (ecology); Liquid water content; Sea salt aerosol; Meteorology; Nucleation; Cloud computing; Chemistry; Physics; Geology; Sea salt; Mechanics","score_opus":0.008258668270710041,"score_gpt":0.22200980902680287,"score_spread":0.21375114075609283,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2088560779","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":[0.98581415,0.00009225462,0.0022063726,0.000014658827,0.0000096865815,0.000052632382,0.0000043631117,0.000015870584,0.011789993],"genre_scores_gemma":[0.9908544,0.000027725964,0.008326145,0.000035779572,0.00003777387,0.0000035371102,0.0000039816928,0.00000691012,0.0007037662],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99931955,0.000007223477,0.00016843264,0.00020104619,0.00014068787,0.00016304692],"domain_scores_gemma":[0.9997243,0.000011538324,0.000067139976,0.00013277715,0.000006706624,0.000057517635],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000024849109,0.00011522237,0.0001460523,3.723756e-9,0.00008994603,0.000005398795,0.00009485297,0.000058134116,0.00087116787],"category_scores_gemma":[0.0000061403302,0.00011395615,0.000030675194,0.0003294371,0.00025871155,0.000098530305,0.00006160994,0.000063052685,0.00000686244],"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":[0.000023315923,0.00024138503,0.8375769,0.000057177895,0.000005850166,0.000009366406,0.00062059716,0.0530211,0.010968432,0.000015872529,0.00018074042,0.09727924],"study_design_scores_gemma":[0.0020715902,0.00009455372,0.49951798,0.000095640724,0.000047276553,0.000071843635,0.00039210232,0.4766782,0.01564335,0.0026469033,0.0017201818,0.0010203994],"about_ca_topic_score_codex":0.0001953651,"about_ca_topic_score_gemma":0.00000838697,"teacher_disagreement_score":0.4236571,"about_ca_system_score_codex":0.00005649264,"about_ca_system_score_gemma":0.000019797739,"threshold_uncertainty_score":0.95386773},"labels":[],"label_agreement":null},{"id":"W2089308728","doi":"10.1007/s00703-010-0117-5","title":"Characterization of aerosol optical depth, aerosol mass concentration, UV irradiance and black carbon aerosols over Indo-Gangetic plains, India, during fog period","year":2010,"lang":"en","type":"article","venue":"Meteorology and Atmospheric Physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":10,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Sherbrooke","funders":"National Oceanic and Atmospheric Administration","keywords":"Aerosol; Environmental science; HYSPLIT; Atmospheric sciences; Air mass (solar energy); Mass concentration (chemistry); Angstrom exponent; Irradiance; Atmosphere (unit); Climatology; Meteorology; Geology; Geography; Chemistry","score_opus":0.0040787937550676966,"score_gpt":0.1939669831893166,"score_spread":0.1898881894342489,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2089308728","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":[0.9968447,0.00005521658,0.0013837464,0.0001236436,0.00022384731,0.00038737975,0.000009145426,0.00004168939,0.000930606],"genre_scores_gemma":[0.99576706,0.00012320191,0.003517446,0.00022423947,0.00014906407,0.000041113723,0.000018061337,0.000035950605,0.00012389338],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99823546,0.000075385506,0.00038692297,0.0005655641,0.00024482512,0.0004918667],"domain_scores_gemma":[0.9991331,0.000057399444,0.00026401287,0.00031701068,0.00002230358,0.0002061419],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00013245846,0.00032562672,0.0004477848,4.4695514e-7,0.00021762235,0.000045966957,0.00019457127,0.0002971429,0.00019528407],"category_scores_gemma":[0.000036935344,0.0003158531,0.000058447833,0.00024256518,0.0012851784,0.00030734044,0.00014990903,0.0004097713,0.000012790809],"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":[0.00005703209,0.00007252596,0.28390235,0.000029183302,0.0000285006,0.000010048793,0.0007315517,0.000095464566,0.7130074,0.00022549155,0.000004446851,0.0018360368],"study_design_scores_gemma":[0.0018397607,0.00033028782,0.8770773,0.000021977594,0.00010909499,0.00004114457,0.00013265388,0.009311649,0.1100636,0.00036151925,0.000071881055,0.0006391699],"about_ca_topic_score_codex":0.000055037774,"about_ca_topic_score_gemma":0.000057701855,"teacher_disagreement_score":0.6029438,"about_ca_system_score_codex":0.000037957958,"about_ca_system_score_gemma":0.00002871418,"threshold_uncertainty_score":0.99992937},"labels":[],"label_agreement":null},{"id":"W2090152098","doi":"10.1029/2006jd007129","title":"Trans‐Pacific transport of Saharan dust to western North America: A case study","year":2007,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":102,"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 de Sherbrooke; Environment and Climate Change Canada; University of British Columbia","funders":"","keywords":"Angstrom exponent; Aerosol; Mineral dust; Atmospheric sciences; Particulates; Asian Dust; Altitude (triangle); Lidar; Chemical transport model; Climatology; Environmental science; Boundary layer; Storm; Geology; Oceanography; Geography; Meteorology; Physics","score_opus":0.030127613197070195,"score_gpt":0.3223406850802399,"score_spread":0.2922130718831697,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2090152098","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":[0.9949594,0.000049914357,0.0030459107,0.00020076551,0.00006926863,0.00047320992,0.0000063145367,0.000009986802,0.0011851967],"genre_scores_gemma":[0.99744296,0.00002616394,0.0014256763,0.000044366163,0.0001878499,0.000006836929,4.922686e-7,0.000031064694,0.00083459733],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99578154,0.00019163199,0.000855167,0.00033991903,0.0020503977,0.00078133855],"domain_scores_gemma":[0.9981227,0.00034214652,0.00023066878,0.00037927437,0.00016869526,0.0007565119],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012954543,0.00022810655,0.00056731567,0.0000050734334,0.0002026442,0.000029764082,0.00063344184,0.00006648112,0.0009990361],"category_scores_gemma":[0.000087660614,0.0001734607,0.0002513233,0.0013752525,0.0005164002,0.00025506743,0.00011451602,0.0007723695,0.00010294767],"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":[0.0010536166,0.0029964726,0.90796876,0.000022994192,0.00012297952,0.010407907,0.0075335535,0.0011139868,0.0045268903,0.000002320082,0.0013020809,0.062948436],"study_design_scores_gemma":[0.0010561303,0.0060080877,0.96549654,0.00003775059,0.000049761486,0.0003400437,0.018387355,0.0000651279,0.00031008065,0.00004494875,0.007960791,0.00024340989],"about_ca_topic_score_codex":0.0053881886,"about_ca_topic_score_gemma":0.0050063473,"teacher_disagreement_score":0.062705025,"about_ca_system_score_codex":0.00017219546,"about_ca_system_score_gemma":0.0000787203,"threshold_uncertainty_score":0.99991417},"labels":[],"label_agreement":null},{"id":"W2091570466","doi":"10.1175/jas3900.1","title":"Refinements to Ice Particle Mass Dimensional and Terminal Velocity Relationships for Ice Clouds. Part II: Evaluation and Parameterizations of Ensemble Ice Particle Sedimentation Velocities","year":2007,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Aeronautics and Space Administration; National Science Foundation","keywords":"Ice cloud; Particle (ecology); Range (aeronautics); Radar; Terminal velocity; Meteorology; Atmospheric sciences; Ice crystals; Geology; Environmental science; Physics; Mechanics; Materials science","score_opus":0.041511341226509284,"score_gpt":0.29494112834935005,"score_spread":0.25342978712284076,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2091570466","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":[0.9930408,0.00012850192,0.0047885636,0.0013582046,0.00023959581,0.00030052374,0.000002580841,0.0000049292225,0.00013628851],"genre_scores_gemma":[0.9417048,0.0000124757025,0.05773214,0.00031486785,0.000043648353,0.00001043958,4.2766166e-7,0.000005572338,0.00017559793],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982359,0.00011536012,0.00048960425,0.00019651347,0.00072524376,0.00023741774],"domain_scores_gemma":[0.998943,0.00026782023,0.0004538596,0.00011624931,0.00009318166,0.0001259191],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0029095598,0.00010712439,0.0001535442,0.0000013003696,0.0007885907,0.000045298682,0.00020270693,0.00003954714,0.000082438535],"category_scores_gemma":[0.0004246358,0.00007574006,0.00004694648,0.0005195635,0.00042377657,0.00039276714,0.00012870638,0.0000822933,0.0000017316806],"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":[0.00045910943,0.00037547905,0.6708334,0.000035615103,0.000070885806,0.0000027370913,0.007838217,0.11521019,0.14621322,0.001089018,0.0023155874,0.055556517],"study_design_scores_gemma":[0.0012673696,0.0011098193,0.8171688,0.0000891328,0.00022023512,0.0000460248,0.004003594,0.15049584,0.019561468,0.003753859,0.0020142514,0.00026965045],"about_ca_topic_score_codex":0.000067357825,"about_ca_topic_score_gemma":0.00005043332,"teacher_disagreement_score":0.14633533,"about_ca_system_score_codex":0.00009359602,"about_ca_system_score_gemma":0.00005686416,"threshold_uncertainty_score":0.60652816},"labels":[],"label_agreement":null},{"id":"W2092997451","doi":"10.1002/qj.230","title":"Rates of phase transformations in mixed‐phase clouds","year":2008,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":53,"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","funders":"","keywords":"Evaporation; Thermodynamics; Saturation (graph theory); Liquid water; Ice Ih; Phase (matter); Clear ice; Materials science; Chemistry; Physics; Meteorology; Mathematics; Sea ice; Arctic ice pack; Molecule","score_opus":0.019164132080210103,"score_gpt":0.2677716337740782,"score_spread":0.24860750169386808,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2092997451","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":[0.99418867,0.00011911357,0.0043037664,0.0005904631,0.00015274923,0.00011599924,0.000006326799,0.00000578179,0.0005171348],"genre_scores_gemma":[0.9965674,0.000032395255,0.0030486379,0.00020769774,0.00004488148,0.0000032954053,4.742922e-7,0.0000058326473,0.000089377914],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984165,0.00017966241,0.0006525642,0.00011483973,0.00038684485,0.00024960958],"domain_scores_gemma":[0.9992558,0.00010877767,0.00035856065,0.00014993834,0.000020479592,0.00010648829],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00058582367,0.00013713233,0.00032366923,0.0000014753892,0.00016591432,0.000008373623,0.0004554361,0.000121615325,0.0009982463],"category_scores_gemma":[0.000028693934,0.000076271725,0.00051865116,0.00025585914,0.00047831106,0.0001334181,0.000030535117,0.00036928078,0.000012504138],"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":[0.0029401155,0.023162816,0.38874817,0.000101431964,0.0008041134,0.00024943572,0.073710226,0.051846474,0.10484737,0.00094382715,0.05258397,0.30006206],"study_design_scores_gemma":[0.034440823,0.03140728,0.8208059,0.00012458078,0.00040086271,0.0005224337,0.010533999,0.06677335,0.012419427,0.011972096,0.009332944,0.0012662793],"about_ca_topic_score_codex":0.00004456846,"about_ca_topic_score_gemma":0.000008112963,"teacher_disagreement_score":0.43205777,"about_ca_system_score_codex":0.00007982251,"about_ca_system_score_gemma":0.000020806077,"threshold_uncertainty_score":0.999915},"labels":[],"label_agreement":null},{"id":"W2095967171","doi":"10.5194/acp-13-2487-2013","title":"Aerosol classification by airborne high spectral resolution lidar observations","year":2013,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":368,"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":"National Oceanic and Atmospheric Administration; Deutsche Forschungsgemeinschaft; European Space Agency","keywords":"Aerosol; Environmental science; Lidar; Remote sensing; Atmosphere (unit); Biomass burning; Atmospheric sciences; High resolution; Meteorology; Geology; Geography","score_opus":0.00934797038655804,"score_gpt":0.19314726475820096,"score_spread":0.1837992943716429,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2095967171","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":[0.9852498,0.000061781946,0.0064828265,0.00048661628,0.000033900276,0.00015309286,0.000007387536,0.00006882728,0.007455735],"genre_scores_gemma":[0.9704312,0.000071111775,0.019157523,0.00020821333,0.000141129,0.00006178845,0.00007202994,0.000019052019,0.009837961],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9990035,0.000014005715,0.00018348383,0.0003485984,0.00018687926,0.00026352957],"domain_scores_gemma":[0.999472,0.000023110124,0.00008942458,0.000273392,0.000013839527,0.00012821116],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000039935298,0.00017809986,0.00013349256,6.3815144e-9,0.00021625111,0.000057114838,0.00014748225,0.00009851389,0.0057760915],"category_scores_gemma":[0.000007830542,0.00017379782,0.000042462834,0.00021388855,0.00020300566,0.00029314018,0.00006040608,0.00014305388,0.0002953506],"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":[0.000017906652,0.00039193226,0.060136776,0.00004411886,0.000039038714,0.0000013965666,0.00032626232,0.001229398,0.72379714,0.00045320383,0.0651217,0.1484411],"study_design_scores_gemma":[0.0011384249,0.00012463595,0.7644621,0.000031888234,0.00008486528,0.000010772807,0.00048742827,0.15004468,0.052597947,0.0067491797,0.023033662,0.0012343707],"about_ca_topic_score_codex":0.0008113108,"about_ca_topic_score_gemma":0.0000027203914,"teacher_disagreement_score":0.7043254,"about_ca_system_score_codex":0.00010005765,"about_ca_system_score_gemma":0.000010192009,"threshold_uncertainty_score":0.99513274},"labels":[],"label_agreement":null},{"id":"W2096112487","doi":"10.1175/2010bams2935.1","title":"Indirect and Semi-direct Aerosol Campaign","year":2010,"lang":"en","type":"article","venue":"Bulletin of the American Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":308,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"National Research Council Canada; Environment and Climate Change Canada","funders":"","keywords":"Aerosol; Environmental science; Haze; Atmospheric sciences; Arctic; Cirrus; Marine stratocumulus; Sea salt aerosol; Boundary layer; Climatology; Meteorology; Sea salt; Geology; Geography; Oceanography","score_opus":0.005641119322063202,"score_gpt":0.2040663598071797,"score_spread":0.19842524048511648,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2096112487","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":[0.99138516,0.00004283619,0.000036278085,0.0025398901,0.000053683005,0.00013593382,0.0000034903646,0.000037018195,0.005765695],"genre_scores_gemma":[0.98319113,0.00010003297,0.012887075,0.003206109,0.000030219198,0.000013817293,2.6018014e-7,0.000009762283,0.0005616062],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99893886,0.00010673382,0.00016303785,0.00031770227,0.0002162353,0.00025742754],"domain_scores_gemma":[0.9992085,0.00021630527,0.00019884949,0.0002621965,0.0000053805343,0.00010873022],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00041872772,0.00014850285,0.00029158356,3.5445441e-7,0.0001896502,0.000013553471,0.00029394962,0.000077681,0.0021302612],"category_scores_gemma":[0.00014833514,0.000086036714,0.00015209152,0.00015346002,0.0027566522,0.000010616546,0.0005723316,0.00031862032,0.000032946442],"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":[0.00006803123,0.00017601039,0.7463919,0.000011246944,0.00008159717,0.0000020359594,0.00077960134,0.00006307181,0.16333677,0.00011540838,0.05332211,0.035652246],"study_design_scores_gemma":[0.00029722645,0.0003818552,0.9065116,0.0000047446947,0.0000584332,0.000022166645,0.000504465,0.0002272154,0.0053867484,0.00031104448,0.08596343,0.0003310771],"about_ca_topic_score_codex":0.0005964132,"about_ca_topic_score_gemma":0.000013494246,"teacher_disagreement_score":0.16011971,"about_ca_system_score_codex":0.000014821439,"about_ca_system_score_gemma":0.00000424862,"threshold_uncertainty_score":0.99995726},"labels":[],"label_agreement":null},{"id":"W2096474702","doi":"10.1002/qj.2597","title":"Application of a Monte Carlo solar radiative transfer modelin the McICA framework","year":2015,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":5,"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":"Freie Universität Berlin; European Space Agency; Pennsylvania State University; U.S. Department of Energy","keywords":"Radiative transfer; Monte Carlo method; Radiative flux; Physics; Zenith; Computational physics; Atmospheric radiative transfer codes; Photon; Flux (metallurgy); Meteorology; Environmental science; Statistical physics; Optics; Materials science; Statistics","score_opus":0.012859141362945794,"score_gpt":0.22392669071294952,"score_spread":0.2110675493500037,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2096474702","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":[0.7756278,0.00022911369,0.2216542,0.0019777473,0.0001180903,0.00017710721,0.0000037411128,0.0000070472174,0.00020516866],"genre_scores_gemma":[0.99222684,0.000011130138,0.0068887984,0.00068379723,0.00011516712,0.000009603465,1.0739038e-7,0.000008619874,0.000055936063],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99827445,0.00028590884,0.00046059853,0.00015848734,0.00058856496,0.00023200779],"domain_scores_gemma":[0.99909735,0.0001721553,0.00026948025,0.0002720829,0.000046420864,0.00014248754],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001089478,0.00014878892,0.00028847094,6.2372123e-7,0.00015378091,0.000018978977,0.0007473741,0.00018662978,0.0001312011],"category_scores_gemma":[0.00005423334,0.0000666342,0.0005390614,0.00016836883,0.0004413568,0.00007893931,0.000053845943,0.0005761794,0.000013057731],"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":[0.0007945096,0.00096019957,0.0645633,0.000016703756,0.0005736016,0.000006147197,0.045286294,0.7647329,0.002675669,0.0014757394,0.012626411,0.106288545],"study_design_scores_gemma":[0.0026097768,0.0069598984,0.12101915,0.000050733805,0.0005968043,0.000043740023,0.015168986,0.7795606,0.00073692785,0.064126715,0.008444082,0.0006825546],"about_ca_topic_score_codex":0.00013582881,"about_ca_topic_score_gemma":0.0000057860498,"teacher_disagreement_score":0.21659906,"about_ca_system_score_codex":0.000113420836,"about_ca_system_score_gemma":0.000023330866,"threshold_uncertainty_score":0.2717264},"labels":[],"label_agreement":null},{"id":"W2096635607","doi":"10.1029/2005gl025397","title":"Aerosol indirect effect over the Indian Ocean","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Aerosol; Environmental science; Atmospheric sciences; Effective radius; Moderate-resolution imaging spectroradiometer; Climatology; Ice nucleus; Nucleation; Ice crystals; Pollution; Satellite; Meteorology; Geology; Physics","score_opus":0.010128656848172391,"score_gpt":0.2637024311767829,"score_spread":0.2535737743286105,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2096635607","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":[0.9906374,0.000011666703,0.000039620147,0.0037060182,0.00006936962,0.00034638806,0.0000028365218,0.00004432867,0.0051423567],"genre_scores_gemma":[0.99727005,0.000002173312,0.000066550776,0.0013355905,0.0003899766,0.000034581954,0.0000055532346,0.000023891875,0.0008716523],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99697274,0.0003760653,0.00014369587,0.0004073471,0.0012253954,0.0008747526],"domain_scores_gemma":[0.99887013,0.00049693487,0.000034285076,0.0004537963,0.000006604145,0.00013824472],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0006559566,0.00016806764,0.00016161171,0.0000032770834,0.0005181942,0.000114442395,0.00059894146,0.00005929903,0.000986898],"category_scores_gemma":[0.00007319862,0.000103357306,0.00012029685,0.0006450952,0.0009521821,0.00013308412,0.0004182947,0.00063797814,0.0026117486],"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":[0.000101883146,0.0002553285,0.23665164,0.000018967648,0.0000362621,0.00019796289,0.00066109846,0.00056443486,0.20862661,0.00027770508,0.53794074,0.014667347],"study_design_scores_gemma":[0.0005073144,0.00027438108,0.97393674,0.000013463983,0.000009516782,0.0000041435273,0.000059240243,0.00028709264,0.01097209,0.00065538834,0.012971537,0.0003090805],"about_ca_topic_score_codex":0.0049695405,"about_ca_topic_score_gemma":0.00010690562,"teacher_disagreement_score":0.7372851,"about_ca_system_score_codex":0.00018443857,"about_ca_system_score_gemma":0.000011150167,"threshold_uncertainty_score":0.9999263},"labels":[],"label_agreement":null},{"id":"W2096729982","doi":"10.1029/2004gl021201","title":"Anatomy of cirrus clouds: Results from the Emerald airborne campaigns","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":113,"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":"Cirrus; Ice crystals; Outflow; Thunderstorm; Geology; Cloud physics; Lidar; Middle latitudes; Atmospheric sciences; Latitude; Meteorology; Remote sensing; Physics; Oceanography; Cloud computing; Geodesy","score_opus":0.024286833250340596,"score_gpt":0.2992660055135651,"score_spread":0.2749791722632245,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2096729982","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":[0.9661557,0.000020105403,0.00023754266,0.031701006,0.00006236173,0.00024537437,0.00004361132,0.00002475071,0.0015095671],"genre_scores_gemma":[0.9955806,0.000015079843,0.00070059067,0.0031960737,0.00026310465,0.000021998889,0.000014067119,0.000017620956,0.00019082936],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99715495,0.00018787698,0.00027582893,0.00046379454,0.0012626647,0.00065486314],"domain_scores_gemma":[0.9985523,0.0005003459,0.00007039571,0.0006776635,0.000021655966,0.00017761932],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005326897,0.00014755974,0.00018847629,0.0000021399628,0.00026406458,0.000036217523,0.0007789566,0.00005721219,0.0004566856],"category_scores_gemma":[0.00024539712,0.00009841701,0.00012055248,0.0006483529,0.0011815964,0.000118859934,0.00047201812,0.0005457296,0.00097474095],"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":[0.0012886963,0.0014880294,0.0144057805,0.000021861446,0.0002321175,0.00028550412,0.012924797,0.011305254,0.599034,0.003769773,0.31965184,0.03559236],"study_design_scores_gemma":[0.0034692243,0.0005223735,0.9145673,0.00008713379,0.000028470233,0.000002136028,0.0012238058,0.0003706381,0.017139195,0.015649727,0.046358068,0.0005819618],"about_ca_topic_score_codex":0.02684616,"about_ca_topic_score_gemma":0.00022273666,"teacher_disagreement_score":0.9001615,"about_ca_system_score_codex":0.00018447508,"about_ca_system_score_gemma":0.000033112185,"threshold_uncertainty_score":0.9998031},"labels":[],"label_agreement":null},{"id":"W2097240221","doi":"10.1175/bams-d-11-00123.1","title":"In Situ, Airborne Instrumentation: Addressing and Solving Measurement Problems in Ice Clouds","year":2011,"lang":"en","type":"article","venue":"Bulletin of the American Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":50,"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":"Natural Environment Research Council; Sight Research UK; National Aeronautics and Space Administration; U.S. Department of Energy; National Science Foundation","keywords":"Instrumentation (computer programming); Atmospheric research; Cloud computing; Ice formation; Systems engineering; Meteorology; Ice cloud; Environmental science; Remote sensing; Computer science; Aeronautics; Engineering; Geography; Geology; Atmospheric sciences","score_opus":0.03639461722914651,"score_gpt":0.23205582000660452,"score_spread":0.19566120277745802,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2097240221","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":[0.9938269,0.00009490618,0.00017092803,0.0014310773,0.000034850455,0.00022007132,5.803086e-7,0.0000123398795,0.004208344],"genre_scores_gemma":[0.984853,0.00008518593,0.012997342,0.0019742919,0.000011848916,0.000027579334,1.6583719e-7,0.000007978732,0.000042562093],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99855566,0.00018562748,0.00030985606,0.00030525232,0.00035385572,0.0002897225],"domain_scores_gemma":[0.9994511,0.000047366037,0.00025490797,0.00018165998,0.000008385097,0.000056601293],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008357819,0.00014049941,0.00026464532,0.0000011457307,0.00008426664,0.000009035929,0.00028840476,0.0000536776,0.00110724],"category_scores_gemma":[0.000072004135,0.00009381396,0.00009865582,0.00029369336,0.0009712706,0.000032773918,0.00039332776,0.00021314429,0.000014108029],"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":[0.0001036836,0.00053280854,0.92855155,0.000030320914,0.00003507737,0.0000044254894,0.004817598,0.00081221794,0.035598576,0.00011257704,0.0032003713,0.026200805],"study_design_scores_gemma":[0.00041502697,0.00019943809,0.9942958,0.000028331691,0.00001181907,0.000002900735,0.0011954583,0.0001443612,0.001262233,0.00053051603,0.0017671309,0.00014703156],"about_ca_topic_score_codex":0.0030116031,"about_ca_topic_score_gemma":0.00014118537,"teacher_disagreement_score":0.065744214,"about_ca_system_score_codex":0.00014887203,"about_ca_system_score_gemma":0.000008414672,"threshold_uncertainty_score":0.99980587},"labels":[],"label_agreement":null},{"id":"W2097258212","doi":"10.5194/acp-12-9387-2012","title":"Contrasting trends of mass and optical properties of aerosols over the Northern Hemisphere from 1992 to 2011","year":2012,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":65,"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":"National Natural Science Foundation of China; U.S. Department of Energy; National Science Foundation","keywords":"Aerosol; Visibility; Extinction (optical mineralogy); Environmental science; Atmospheric sciences; Aerodynamic diameter; Northern Hemisphere; Climatology; Particulates; Mass concentration (chemistry); Meteorology; Geography; Chemistry; Physics; Optics; Geology","score_opus":0.008239069582662713,"score_gpt":0.19345885266936574,"score_spread":0.18521978308670303,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2097258212","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":[0.99354565,0.00048045992,0.0007169917,0.000056944886,0.000017667198,0.000060775274,0.000008763441,0.000009257921,0.0051035164],"genre_scores_gemma":[0.99509746,0.000023960954,0.003926269,0.000052985568,0.00010551002,0.000009355015,0.0000020563375,0.000013785849,0.000768599],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99919015,0.000011607003,0.0001977246,0.00018913548,0.00018247319,0.00022891477],"domain_scores_gemma":[0.99951273,0.00004797649,0.00009580133,0.00020824742,0.000008104696,0.00012715496],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000070360256,0.00015918173,0.00021933111,9.057762e-9,0.00007421001,0.000011649543,0.00012250355,0.00006300262,0.0013941776],"category_scores_gemma":[0.000010599916,0.000109064866,0.00004546536,0.00009720455,0.00033118716,0.00009324517,0.000118322896,0.00009583676,0.0000071105173],"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":[0.00004865353,0.00009960689,0.37525287,0.000042825315,0.00004434841,4.052598e-7,0.0011385614,0.00029691748,0.5107116,0.000014467704,0.0001613992,0.11218838],"study_design_scores_gemma":[0.0011157374,0.00012235816,0.49184278,0.0001400443,0.00021586666,0.000008086879,0.0017716094,0.007412376,0.49390447,0.000417142,0.002249877,0.00079967664],"about_ca_topic_score_codex":0.000661433,"about_ca_topic_score_gemma":0.000009524039,"teacher_disagreement_score":0.116589904,"about_ca_system_score_codex":0.000018785058,"about_ca_system_score_gemma":0.0000063922266,"threshold_uncertainty_score":0.9995187},"labels":[],"label_agreement":null},{"id":"W2097304099","doi":"10.1175/1520-0493(2003)131<0656:coaowm>2.0.co;2","title":"Comparison of Aircraft Observations with Mixed-Phase Cloud Simulations","year":2003,"lang":"en","type":"article","venue":"Monthly Weather Review","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":15,"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":"Liquid water content; Environmental science; Meteorology; Drizzle; Cloud physics; Ice crystals; Phase (matter); Trajectory; Computer science; Cloud computing; Physics","score_opus":0.038832602563217127,"score_gpt":0.312906608721983,"score_spread":0.27407400615876587,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2097304099","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":[0.89933336,0.055085875,0.010648165,0.0009671796,0.00014767535,0.0013893917,0.0000418391,0.00008394252,0.0323026],"genre_scores_gemma":[0.98812556,0.0007207606,0.009430084,0.0005649716,0.000010788083,0.000035026937,0.000012767544,0.00002236591,0.0010776942],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9989432,0.00008323292,0.0003521684,0.00020927764,0.00023921317,0.00017291062],"domain_scores_gemma":[0.99932593,0.000041343836,0.00016510201,0.00037509488,0.000015133557,0.00007739236],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001454959,0.00014279365,0.00033811742,9.5936e-7,0.00009903488,0.0000072492767,0.00014994795,0.000034851273,0.0033427228],"category_scores_gemma":[0.000041487878,0.0001048428,0.00007493145,0.00035669177,0.00011197761,0.00009423647,0.00002865877,0.0000794065,0.00011833512],"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":[0.000019734576,0.0021572607,0.8875707,0.00050219684,0.00009108645,0.0000066890298,0.0008501555,0.038370587,0.0011298617,0.0032568339,0.042598512,0.023446398],"study_design_scores_gemma":[0.00080644834,0.00032968642,0.026976854,0.0007726055,0.00019860505,0.000002172169,0.00012303953,0.002795311,0.00047090702,0.00027506606,0.966878,0.0003713328],"about_ca_topic_score_codex":0.00005892488,"about_ca_topic_score_gemma":0.00013724585,"teacher_disagreement_score":0.92427945,"about_ca_system_score_codex":0.000043200846,"about_ca_system_score_gemma":0.000013982348,"threshold_uncertainty_score":0.99756837},"labels":[],"label_agreement":null},{"id":"W2097553621","doi":"10.1002/2015ea000102","title":"Radar signatures of snowflake riming: A modeling study","year":2015,"lang":"en","type":"article","venue":"Earth and Space Science","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":151,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Snowflake; Radar; Homogeneous; Precipitation; Meteorology; Physics; Computer science; Statistical physics; Telecommunications; Snow","score_opus":0.02016975777682011,"score_gpt":0.23921469660996075,"score_spread":0.21904493883314063,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2097553621","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":[0.9905638,0.000119641576,0.0015905033,0.00011473625,0.000071360635,0.000124368,4.493121e-7,0.000013963541,0.0074011716],"genre_scores_gemma":[0.99475986,0.000005016486,0.0046968525,0.00004328651,0.000014329083,0.0000015790159,7.637766e-8,0.0000033949793,0.00047559716],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9988624,0.000017572553,0.000099575635,0.0002750828,0.0005211396,0.00022424736],"domain_scores_gemma":[0.9995476,0.000009359134,0.000041580184,0.00017532022,0.00001625093,0.00020991241],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005767311,0.0000796867,0.00010288997,0.000002841435,0.00014795673,0.000033411066,0.00021817489,0.000021345579,0.00008198575],"category_scores_gemma":[0.00007049222,0.00006156287,0.000014831685,0.0003656136,0.00039128022,0.00021935742,0.00019860858,0.000075509044,0.000019161833],"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":[0.00014786715,0.00081825897,0.6639501,0.00001633963,0.000015898,0.000045006447,0.04109075,0.12839372,0.12763003,0.0016457179,0.0016966397,0.034549672],"study_design_scores_gemma":[0.0027338201,0.00250367,0.3277648,0.000040628154,0.000048395257,0.000017950568,0.036705945,0.61215,0.009166772,0.0019233822,0.005893531,0.0010511155],"about_ca_topic_score_codex":0.0004437925,"about_ca_topic_score_gemma":0.00017028108,"teacher_disagreement_score":0.48375627,"about_ca_system_score_codex":0.00001330229,"about_ca_system_score_gemma":0.00004517653,"threshold_uncertainty_score":0.2510461},"labels":[],"label_agreement":null},{"id":"W2097559174","doi":"10.5194/acp-8-3473-2008","title":"Data assimilation of dust aerosol observations for the CUACE/dust forecasting system","year":2008,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":124,"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":"Dust storm; Data assimilation; Environmental science; Meteorology; Aerosol; Asian Dust; Visibility; Storm; Atmospheric sciences; Satellite; Climatology; Geology; Geography","score_opus":0.06813646026606034,"score_gpt":0.23827491682936733,"score_spread":0.170138456563307,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2097559174","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":[0.93251747,0.00009334974,0.063316956,0.000098925324,0.000053636784,0.00025496702,0.00007917039,0.000034641584,0.003550875],"genre_scores_gemma":[0.9726272,0.00004169497,0.025286272,0.000040651103,0.00017807986,0.000031811313,0.00007657992,0.000016063237,0.0017016442],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99917156,0.000008370859,0.00021219731,0.00027017327,0.00016756672,0.00017010931],"domain_scores_gemma":[0.99912274,0.00016302292,0.00015816474,0.00048820334,0.00001855402,0.00004933417],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000107579166,0.00013175647,0.00014738837,5.775035e-9,0.00042626803,0.00001381278,0.00031391662,0.00006294416,0.0001512604],"category_scores_gemma":[0.000028880031,0.00010191215,0.000042555763,0.00017907334,0.00022859465,0.00017631656,0.0001728231,0.000085962936,0.0000030539975],"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":[0.00015031041,0.00054674357,0.5621835,0.0010887048,0.0003260358,0.000009080499,0.0027291654,0.08154316,0.0618718,0.00045125277,0.03858666,0.25051358],"study_design_scores_gemma":[0.00038912296,0.000024499446,0.027423956,0.000036501817,0.00008114431,0.000021795327,0.0006027696,0.962369,0.0032567105,0.00005016928,0.005522059,0.00022222135],"about_ca_topic_score_codex":0.00011086551,"about_ca_topic_score_gemma":0.00000464149,"teacher_disagreement_score":0.8808259,"about_ca_system_score_codex":0.00004166393,"about_ca_system_score_gemma":0.000020135552,"threshold_uncertainty_score":0.4155857},"labels":[],"label_agreement":null},{"id":"W2097663660","doi":"10.1478/c1v89s1p007","title":"Engineering with and for light absorption and scattering: A quarter century of experimental research at RTL","year":2011,"lang":"en","type":"article","venue":"ECS Journal of Solid State Science and Technology (The Electrochemical Society)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"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":"Türkiye Bilimsel ve Teknolojik Araştırma Kurumu; U.S. Department of Energy; National Science Foundation","keywords":"Quarter (Canadian coin); Absorption (acoustics); Scattering; Optics; Light scattering; Physics; Geography; Archaeology","score_opus":0.01188257147504749,"score_gpt":0.2493059752856043,"score_spread":0.23742340381055682,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2097663660","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":[0.99822336,0.00047864328,0.00052498124,0.00059925864,0.0000120968925,0.000101533435,3.6324536e-7,0.000006363764,0.00005341986],"genre_scores_gemma":[0.9952621,0.00028359526,0.0043886607,0.000024191244,0.000009901441,0.0000067715546,5.288796e-8,0.0000056834456,0.000019053985],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9990706,0.0000058877094,0.00015902577,0.00018117523,0.00026780972,0.00031550223],"domain_scores_gemma":[0.9996579,0.00002424175,0.0000969764,0.00008416557,0.00005860125,0.00007810141],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005308305,0.00008314517,0.00012878868,0.000010101815,0.00022420885,0.000013552372,0.00020250562,0.000051916162,0.000017771896],"category_scores_gemma":[0.000022693965,0.000052251777,0.000022936467,0.00041855522,0.0017694978,0.00014834812,0.00017636245,0.00021224,5.8646003e-7],"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":[0.00003872572,0.000028363746,0.0032997092,0.0000056491913,0.000011158969,8.3060223e-7,0.0013114299,5.8043724e-7,0.9947335,0.000061002556,0.00007970154,0.00042931124],"study_design_scores_gemma":[0.0003394974,0.00073625025,0.0016067035,0.000019245286,0.0000090119765,0.00016329905,0.0010484711,0.00046558326,0.9943253,0.0006725124,0.000531339,0.00008281353],"about_ca_topic_score_codex":0.000002530508,"about_ca_topic_score_gemma":6.8246425e-7,"teacher_disagreement_score":0.0038636795,"about_ca_system_score_codex":0.00009196556,"about_ca_system_score_gemma":0.000021331087,"threshold_uncertainty_score":0.65197885},"labels":[],"label_agreement":null},{"id":"W2098692875","doi":"10.5194/angeo-25-19-2007","title":"Upper altitude limit for Rayleigh lidar","year":2007,"lang":"en","type":"article","venue":"Annales Geophysicae","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Lidar; Rayleigh scattering; Altitude (triangle); Backscatter (email); Environmental science; Remote sensing; Atmospheric temperature; Atmospheric pressure; Atmospheric sciences; Meteorology; Geology; Physics; Optics; Mathematics; Computer science","score_opus":0.009686352474202483,"score_gpt":0.24206044106758326,"score_spread":0.23237408859338077,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2098692875","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":[0.9750459,0.000073921256,0.004546925,0.00037715194,0.00011689914,0.00029253244,0.000004990112,0.000058378137,0.019483276],"genre_scores_gemma":[0.9873157,0.000018023049,0.0053193937,0.0011289538,0.0002747554,0.00003472026,0.000007844324,0.000022631764,0.005877969],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9989101,0.000007667491,0.0001589787,0.0002933507,0.00020071628,0.00042917152],"domain_scores_gemma":[0.99948925,0.0000687235,0.000060336624,0.00024822156,0.00001028136,0.00012317905],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014434036,0.00014536025,0.00014164366,0.0000011616139,0.00015957483,0.00002018825,0.0002280343,0.00005542082,0.00071475684],"category_scores_gemma":[0.000013358291,0.00012637518,0.00013810623,0.00014450464,0.0001392408,0.00012939429,0.00010536686,0.00007608018,0.0016321613],"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":[0.00048220155,0.0016559908,0.323417,0.00006986359,0.00019555862,0.00006188389,0.0031094414,0.0006688356,0.11703013,0.011694616,0.11599348,0.425621],"study_design_scores_gemma":[0.00039026255,0.0002312071,0.5320234,0.000008860353,0.00002408754,0.0000028528123,0.00015906504,0.00020540087,0.008389629,0.0023179743,0.4559025,0.00034481005],"about_ca_topic_score_codex":0.00010597956,"about_ca_topic_score_gemma":0.00006594841,"teacher_disagreement_score":0.4252762,"about_ca_system_score_codex":0.00003939088,"about_ca_system_score_gemma":0.0000065495688,"threshold_uncertainty_score":0.9991452},"labels":[],"label_agreement":null},{"id":"W2098945115","doi":"10.1029/2003jd003902","title":"Evaluating aerosol/cloud/radiation process parameterizations with single‐column models and Second Aerosol Characterization Experiment (ACE‐2) cloudy column observations","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":64,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Pacific Northwest National Laboratory; Biological and Environmental Research; Natural Sciences and Engineering Research Council of Canada; European Commission; Canadian Foundation for Climate and Atmospheric Sciences; Battelle; National Aeronautics and Space Administration; Commonwealth Scientific and Industrial Research Organisation; U.S. Department of Energy; National Science Foundation","keywords":"Aerosol; Environmental science; Cloud base; Drizzle; Radiative transfer; Meteorology; Liquid water path; Boundary layer; Atmospheric sciences; Precipitation; Cloud computing; Geology; Physics; Mechanics; Computer science","score_opus":0.08407442095518308,"score_gpt":0.3441920631035001,"score_spread":0.260117642148317,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2098945115","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":[0.9879579,0.00010427439,0.010014772,0.00023102437,0.00011524938,0.0006637835,0.000008822647,0.000021487916,0.00088268507],"genre_scores_gemma":[0.9870501,0.0000525445,0.011392553,0.000097661556,0.00017738187,0.0000965785,0.000010969405,0.000047761197,0.0010744437],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9960671,0.00048951653,0.0006653266,0.00045402665,0.0016990147,0.00062498654],"domain_scores_gemma":[0.99809515,0.00032895527,0.00050163345,0.0003045446,0.00036800344,0.0004016965],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009311107,0.0002664103,0.00039843802,0.0000045339743,0.0006612691,0.0003186341,0.00032625376,0.00012051829,0.00097509415],"category_scores_gemma":[0.00045163708,0.00022394121,0.00008799341,0.00089930196,0.0004687091,0.0011761802,0.00011320219,0.0005286055,0.0000231698],"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":[0.00062960776,0.0026151845,0.038488407,0.00011338977,0.00022604923,0.000041292496,0.005848759,0.038837343,0.8970923,0.00127835,0.0010739854,0.013755333],"study_design_scores_gemma":[0.013266728,0.029825334,0.24430707,0.0010751019,0.00049616094,0.00031307427,0.014050916,0.41933587,0.2512823,0.016559575,0.005810918,0.0036769542],"about_ca_topic_score_codex":0.00011083925,"about_ca_topic_score_gemma":0.00009009103,"teacher_disagreement_score":0.64581,"about_ca_system_score_codex":0.00033766008,"about_ca_system_score_gemma":0.00021744,"threshold_uncertainty_score":0.99993813},"labels":[],"label_agreement":null},{"id":"W2099152130","doi":"10.5194/acp-12-6891-2012","title":"Simulation of mineral dust aerosol with Piecewise Log-normal Approximation (PLA) in CanAM4-PAM","year":2012,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada; University of Victoria","funders":"Australian Dental Research Foundation; Canadian Foundation for Climate and Atmospheric Sciences; National Aeronautics and Space Administration","keywords":"Aerosol; Radiative forcing; Atmospheric sciences; Mineral dust; Radiative transfer; Environmental science; Deposition (geology); Forcing (mathematics); Chemical transport model; Meteorology; Physics; Geology","score_opus":0.006330795820786144,"score_gpt":0.20185877583486547,"score_spread":0.19552798001407934,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2099152130","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":[0.9867537,0.000048036418,0.006915145,0.000014464681,0.000016965161,0.00010191689,0.0000028281809,0.000013359133,0.006133563],"genre_scores_gemma":[0.99134004,0.0000071929494,0.0076166987,0.000032553307,0.00008755795,0.00001217201,0.000013715306,0.000012641753,0.00087745185],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9992025,0.000012014267,0.00017334914,0.0001752177,0.00018226141,0.00025468026],"domain_scores_gemma":[0.9996012,0.00003450122,0.00010489486,0.00015574267,0.000008419498,0.00009524628],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007112113,0.0001503672,0.0001604201,1.7125425e-8,0.00005205367,0.000009305774,0.00007660019,0.0000726917,0.000791219],"category_scores_gemma":[0.0000069651132,0.00013224366,0.000025174411,0.00021561938,0.00014937707,0.0002749388,0.000044223772,0.000102886865,0.00000794761],"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":[0.00007872027,0.0002968896,0.6098398,0.000086790365,0.000015604304,0.0000017277107,0.0010700672,0.32317424,0.020312572,0.000020100033,0.00008968359,0.045013823],"study_design_scores_gemma":[0.0015750168,0.0001118105,0.24524444,0.00005760421,0.0000619037,0.000009996874,0.0006079481,0.73249525,0.018200751,0.000118697004,0.00083755684,0.00067902094],"about_ca_topic_score_codex":0.0004966852,"about_ca_topic_score_gemma":0.000025235056,"teacher_disagreement_score":0.409321,"about_ca_system_score_codex":0.000065599466,"about_ca_system_score_gemma":0.000011477272,"threshold_uncertainty_score":0.8663293},"labels":[],"label_agreement":null},{"id":"W2099856637","doi":"10.5194/amt-6-801-2013","title":"Developing a portable, autonomous aerosol backscatter lidar for network or remote operations","year":2013,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":29,"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","funders":"","keywords":"Lidar; Remote sensing; Backscatter (email); Laser; Environmental science; Computer science; Ceilometer; Optics; Telecommunications; Geology; Physics","score_opus":0.032527544995662544,"score_gpt":0.25164699151560277,"score_spread":0.21911944651994023,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2099856637","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.04520592,0.00014107923,0.9395329,0.0019387006,0.000242895,0.0034942802,0.0000024154185,0.0008142898,0.008627538],"genre_scores_gemma":[0.18959112,0.00006340317,0.80156845,0.003200982,0.00020383358,0.0010210987,0.000008256313,0.00007384886,0.0042689806],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99727166,0.00006311712,0.0006209406,0.00063925114,0.000614249,0.000790795],"domain_scores_gemma":[0.99894446,0.000035446443,0.00015326643,0.00056374347,0.00012178988,0.00018127804],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00067750865,0.00039291874,0.00036764366,5.413388e-7,0.0005176932,0.00017115218,0.00048789076,0.00017272744,0.0059070825],"category_scores_gemma":[0.000080971826,0.00030952189,0.00013056422,0.0004328221,0.00013287671,0.00043268513,0.00021314585,0.0001592714,0.00039125208],"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":[0.0001247175,0.00036019826,0.032399055,0.00013074641,0.00026410306,0.000017082551,0.00061458914,0.004646242,0.031454485,0.00086463545,0.4422915,0.48683265],"study_design_scores_gemma":[0.0022183075,0.0022079917,0.040369406,0.0007359466,0.00033231906,0.00009490763,0.0005806395,0.059976,0.053948723,0.007123919,0.8273617,0.0050501092],"about_ca_topic_score_codex":0.0015529696,"about_ca_topic_score_gemma":0.0004988265,"teacher_disagreement_score":0.48178256,"about_ca_system_score_codex":0.0007050024,"about_ca_system_score_gemma":0.00013453655,"threshold_uncertainty_score":0.9999357},"labels":[],"label_agreement":null},{"id":"W2100213511","doi":"10.5194/acp-11-7097-2011","title":"Extremely large anthropogenic-aerosol contribution to total aerosol load over the Bay of Bengal during winter season","year":2011,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":99,"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","funders":"Indian Space Research Organisation","keywords":"Aerosol; Angstrom exponent; Bay; Dominance (genetics); BENGAL; Environmental science; Atmospheric sciences; Pollution; Climatology; Oceanography; Geography; Meteorology; Geology; Chemistry; Ecology","score_opus":0.006870767910403835,"score_gpt":0.2052153715843765,"score_spread":0.19834460367397266,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2100213511","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":[0.99463654,0.000097283664,0.0022625576,0.000025788264,0.000058814992,0.00019287855,0.000021983024,0.000029021943,0.0026751305],"genre_scores_gemma":[0.99683326,0.000028695731,0.0012131977,0.000086547545,0.00012221228,0.00001698315,0.0000055344276,0.00002100687,0.0016725436],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9986815,0.00002308377,0.00023155614,0.00036902924,0.0003081872,0.00038667512],"domain_scores_gemma":[0.99933034,0.000023649773,0.00011590655,0.00035636313,0.000025553289,0.0001481773],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000107379834,0.00023619416,0.00022641031,1.3099018e-8,0.0002639622,0.000020743815,0.00021431927,0.00009460503,0.006614845],"category_scores_gemma":[0.000013942552,0.00018445821,0.00011248633,0.00018857088,0.0002587108,0.00014681861,0.00019788757,0.00016975262,0.000054286942],"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":[0.0005372112,0.00087527814,0.40813035,0.00011496784,0.00017735451,0.00002023185,0.0057033724,0.00059494877,0.57144463,0.00011419118,0.00086096313,0.011426489],"study_design_scores_gemma":[0.0019851094,0.00019237539,0.34025362,0.00007093289,0.00013129019,0.000033528802,0.00063762296,0.0052103247,0.6490326,0.0001110271,0.0014910396,0.0008505334],"about_ca_topic_score_codex":0.00015099128,"about_ca_topic_score_gemma":0.000019358973,"teacher_disagreement_score":0.07758796,"about_ca_system_score_codex":0.00010815614,"about_ca_system_score_gemma":0.00002125973,"threshold_uncertainty_score":0.9942933},"labels":[],"label_agreement":null},{"id":"W2101549461","doi":"10.1175/2009jas3029.1","title":"Arctic Mixed-Phase Stratiform Cloud Properties from Multiple Years of Surface-Based Measurements at Two High-Latitude Locations","year":2009,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":171,"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":"National Aeronautics and Space Administration; U.S. Department of Energy; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Radiosonde; Environmental science; Liquid water content; Cloud base; Atmospheric sciences; Lidar; Arctic; Precipitation; Cloud height; Cloud top; Radar; Cloud fraction; Depth sounding; Climatology; Meteorology; Geology; Cloud computing; Remote sensing; Satellite; Cloud cover; Geography; Physics","score_opus":0.032297493700515295,"score_gpt":0.2561319496981426,"score_spread":0.22383445599762733,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2101549461","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":[0.9975599,0.00024637417,0.00065149384,0.00072754564,0.000498816,0.00015995954,0.0000029099842,0.000008305585,0.0001447191],"genre_scores_gemma":[0.9686592,0.000012569228,0.030911006,0.0002460105,0.000060982075,0.0000011426923,3.0684882e-7,0.0000065379286,0.00010222434],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9977355,0.00010133485,0.00053213525,0.00020575296,0.0011643361,0.0002609217],"domain_scores_gemma":[0.9987622,0.00008288366,0.0007042586,0.00028651464,0.00005257592,0.00011158054],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006469908,0.00014967132,0.00024810075,7.064289e-7,0.00033134304,0.000052394134,0.0009549151,0.000039535847,0.0005331344],"category_scores_gemma":[0.00014870983,0.00009217146,0.00014925432,0.0005336098,0.00067100726,0.00031848683,0.00010135703,0.00012922412,0.000023197108],"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":[0.000084591455,0.0003800555,0.19687413,0.0000035212993,0.000026160984,0.0000028351328,0.00037182908,0.7169678,0.08052515,0.000010563692,0.00047229324,0.004281062],"study_design_scores_gemma":[0.0040648645,0.0014872764,0.83440393,0.00026800865,0.00016392846,0.000022940752,0.0009023289,0.10225225,0.053980093,0.0014704509,0.00051449594,0.00046939703],"about_ca_topic_score_codex":0.0012173603,"about_ca_topic_score_gemma":0.0003447809,"teacher_disagreement_score":0.63752985,"about_ca_system_score_codex":0.00026549693,"about_ca_system_score_gemma":0.00012557911,"threshold_uncertainty_score":0.58374476},"labels":[],"label_agreement":null},{"id":"W2104761232","doi":"10.1002/qj.2647","title":"Satellite‐based estimation of cloud‐base heights using constrained spectral radiance matching","year":2015,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University; Environment and Climate Change Canada","funders":"National Natural Science Foundation of China; National Aeronautics and Space Administration","keywords":"Radiance; Remote sensing; Cloud computing; Satellite; Environmental science; Computer science; Cloud fraction; Cloud top; Matching (statistics); Satellite imagery; Meteorology; Algorithm; Cloud cover; Geology; Mathematics; Physics; Statistics","score_opus":0.023803843867183073,"score_gpt":0.24490527427857658,"score_spread":0.22110143041139352,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2104761232","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":[0.9493767,0.00013542162,0.04929547,0.0004409441,0.00030609252,0.0001102564,0.0000029982473,0.000010507548,0.00032160545],"genre_scores_gemma":[0.91558754,0.0000020392429,0.083988674,0.00027336102,0.00011045209,7.6344963e-7,3.9082875e-7,0.000008230307,0.000028543987],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9982523,0.00022865058,0.0005404925,0.00016118602,0.0005374553,0.00027995344],"domain_scores_gemma":[0.998838,0.000115928015,0.0006226139,0.0001831494,0.000032489974,0.00020781007],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00091838744,0.00016771849,0.0003306736,0.0000013792169,0.0001336886,0.000028712468,0.00040841877,0.0001286567,0.00029784517],"category_scores_gemma":[0.00004535453,0.000097021315,0.000441246,0.00017376636,0.000483768,0.00012383494,0.00003666224,0.00032502136,0.000009095253],"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":[0.00041635643,0.00053474243,0.026066177,0.000029792693,0.00016018549,0.000040880026,0.005591997,0.920726,0.015709277,0.000553436,0.0010552164,0.029115926],"study_design_scores_gemma":[0.0050191567,0.0054381695,0.063086204,0.000167915,0.0004084288,0.00019597322,0.003550002,0.8572828,0.007545017,0.055996127,0.00049084827,0.0008193394],"about_ca_topic_score_codex":0.00009078164,"about_ca_topic_score_gemma":0.000003956013,"teacher_disagreement_score":0.06344319,"about_ca_system_score_codex":0.00020842404,"about_ca_system_score_gemma":0.000056387184,"threshold_uncertainty_score":0.39564145},"labels":[],"label_agreement":null},{"id":"W2105485029","doi":"10.1002/2014jd022950","title":"Observations of the variability of shallow trade wind cumulus cloudiness and mass flux","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":78,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Fonds Québécois de la Recherche sur la Nature et les Technologies; Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Cloud base; Cloud fraction; Outflow; Environmental science; Mass flux; Cloud cover; Atmospheric sciences; Flux (metallurgy); Cloud computing; Cloud height; Cloud top; Liquid water content; Wind profiler; Meteorology; Climatology; Geology; Radar; Physics; Materials science","score_opus":0.06074857649972912,"score_gpt":0.3100494500428097,"score_spread":0.2493008735430806,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2105485029","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":[0.9966405,0.00008937932,0.00026326667,0.0011632022,0.00009086216,0.00015179643,0.000004651687,0.0000025928794,0.0015937323],"genre_scores_gemma":[0.9960273,0.000018923496,0.0033571695,0.000025544548,0.00010418873,0.0000017924702,2.4389064e-7,0.000010368284,0.0004544693],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99725115,0.0003924743,0.00048511193,0.00016744653,0.0014079257,0.00029589777],"domain_scores_gemma":[0.9984417,0.0005272209,0.00028879114,0.0003220166,0.00015837858,0.00026188226],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016493385,0.00011297474,0.00032551016,8.945468e-7,0.00010446023,0.000020753634,0.0005945911,0.000073213814,0.00028101387],"category_scores_gemma":[0.0011990678,0.000068831105,0.0001417801,0.0005921709,0.0010648015,0.0002209556,0.00032484034,0.0004520117,0.0000060990524],"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":[0.0002947667,0.0006754643,0.9193085,0.000049777485,0.00007236458,0.000008885927,0.0010611215,0.0034935493,0.065240905,0.0010868533,0.004461714,0.0042461352],"study_design_scores_gemma":[0.00057777733,0.0005078786,0.97460264,0.000046437643,0.000022972456,0.000005791452,0.00074084953,0.0035261286,0.0021693576,0.016312223,0.0014059653,0.0000819686],"about_ca_topic_score_codex":0.0005491831,"about_ca_topic_score_gemma":0.000041643703,"teacher_disagreement_score":0.06307155,"about_ca_system_score_codex":0.00012239057,"about_ca_system_score_gemma":0.00016454981,"threshold_uncertainty_score":0.39233053},"labels":[],"label_agreement":null},{"id":"W2105893968","doi":"10.1002/2014rg000468","title":"Representation of microphysical processes in cloud‐resolving models: Spectral (bin) microphysics versus bulk parameterization","year":2015,"lang":"en","type":"article","venue":"Reviews of Geophysics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":476,"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":"Biological and Environmental Research; National Oceanic and Atmospheric Administration; Hebrew University of Jerusalem; Bundesministerium für Bildung und Forschung; Deutsche Forschungsgemeinschaft; U.S. Department of Energy","keywords":"Bin; Mesoscale meteorology; Environmental science; Meteorology; Cloud physics; Cloud computing; Atmospheric models; Atmospheric sciences; Physics; Computer science; Atmosphere (unit)","score_opus":0.06202709551382758,"score_gpt":0.283658763959226,"score_spread":0.22163166844539844,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2105893968","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":[0.99340963,0.0007357904,0.004024544,0.000026608466,0.00013364159,0.0003952974,0.0000053848153,0.000011552221,0.0012575496],"genre_scores_gemma":[0.9903362,0.0015717195,0.007879709,0.000022905251,0.000093563984,0.000021476408,0.000017960192,0.000020049582,0.00003642768],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99854064,0.00008759344,0.0005418941,0.00030404463,0.00030823675,0.00021757731],"domain_scores_gemma":[0.9990631,0.000056362504,0.00042697464,0.00033716465,0.000044933622,0.0000714791],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014459384,0.0001800667,0.0005332243,0.0000032038179,0.000024412682,0.000011656324,0.00025218347,0.000053920678,0.000024619329],"category_scores_gemma":[0.00011102112,0.00016456847,0.000120724355,0.0008700011,0.00015305313,0.0003479957,0.00013146666,0.00010238755,0.00005350403],"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":[0.0013822006,0.0032361096,0.017445536,0.0020862834,0.0001147586,0.000015558386,0.012257877,0.22451423,0.5418323,0.0029853696,0.001588384,0.19254136],"study_design_scores_gemma":[0.020167172,0.0076721055,0.038697205,0.0036553063,0.0012495113,0.000018564528,0.0055820155,0.20809841,0.57650715,0.11769362,0.014355487,0.006303431],"about_ca_topic_score_codex":0.0008162065,"about_ca_topic_score_gemma":0.00004197886,"teacher_disagreement_score":0.18623793,"about_ca_system_score_codex":0.00010883409,"about_ca_system_score_gemma":0.000050568542,"threshold_uncertainty_score":0.6710907},"labels":[],"label_agreement":null},{"id":"W2106038834","doi":"10.5194/acp-10-8649-2010","title":"The potential influence of Asian and African mineral dust on ice, mixed-phase and liquid water clouds","year":2010,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":90,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Dalhousie University; European Commission","keywords":"Mineral dust; Ice nucleus; Atmospheric sciences; Environmental science; Relative humidity; Deposition (geology); Asian Dust; Liquid water path; Aerosol; Climatology; Meteorology; Geology; Nucleation; Chemistry; Geography; Geomorphology; Structural basin","score_opus":0.0025394125046243666,"score_gpt":0.19706158369098248,"score_spread":0.19452217118635812,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2106038834","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":[0.9959192,0.000031825508,0.000051860712,0.00021788618,0.000039842867,0.00007363096,0.0000058806063,0.000012533762,0.0036472904],"genre_scores_gemma":[0.99774384,0.00006462717,0.0008625728,0.000067613,0.000109638895,0.000008013007,0.000003981316,0.000012619188,0.0011270834],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99914414,0.00001254094,0.00015784301,0.00027952454,0.00016171116,0.00024424278],"domain_scores_gemma":[0.99952406,0.000029872406,0.000063454536,0.00023793272,0.000009654648,0.00013503151],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008742073,0.00017677188,0.00014955245,1.3466427e-8,0.0002481693,0.00003999706,0.00013517028,0.00008526455,0.0002497581],"category_scores_gemma":[0.000008783731,0.00011382069,0.00003135252,0.00007246656,0.000771757,0.00008498447,0.00014830867,0.0002142198,0.0000056926106],"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":[0.00023072063,0.00015890492,0.0042320625,0.00003498949,0.00002571297,0.000007729612,0.0006263589,0.00037037424,0.8876679,0.00008109548,0.00025111582,0.10631302],"study_design_scores_gemma":[0.00687673,0.0022077002,0.2236017,0.00009689398,0.00034004176,0.00024223086,0.0028373695,0.032191057,0.6416061,0.004615272,0.082836166,0.0025487288],"about_ca_topic_score_codex":0.0001152805,"about_ca_topic_score_gemma":0.000009061752,"teacher_disagreement_score":0.2460618,"about_ca_system_score_codex":0.000009118628,"about_ca_system_score_gemma":0.000006590752,"threshold_uncertainty_score":0.4641473},"labels":[],"label_agreement":null},{"id":"W2107573298","doi":"10.5539/mas.v4n11p131","title":"Estimating Particulate Matter Concentration over Arid Region Using Satellite Remote Sensing: A Case Study in Makkah, Saudi Arabia","year":2010,"lang":"en","type":"article","venue":"Modern Applied Science","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Particulates; Multispectral image; Environmental science; Aerosol; Remote sensing; Satellite; Meteorology; Air quality index; Geology; Geography; Physics","score_opus":0.020171887005891745,"score_gpt":0.26213313161992857,"score_spread":0.24196124461403684,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2107573298","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":[0.8758067,0.000002580179,0.122141294,0.000047812344,0.00015412495,0.0004604501,2.5039546e-7,0.00003306487,0.0013537565],"genre_scores_gemma":[0.94718593,4.1735507e-7,0.052483678,0.00024203736,0.000035537738,0.000002032304,4.0914796e-7,0.000016057567,0.00003389361],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9978374,0.000029120994,0.00033520814,0.0007300911,0.00051753403,0.0005505974],"domain_scores_gemma":[0.99919206,0.000023936376,0.00015710344,0.00046399407,0.000011396008,0.0001515142],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006391171,0.00019596232,0.00017619929,0.000005361224,0.00043823637,0.00017162216,0.00022186036,0.00006401276,0.00010739676],"category_scores_gemma":[0.000018624467,0.00018008488,0.000026216145,0.0005726246,0.0006227626,0.00031392052,0.0002218538,0.00027596334,0.00007233738],"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":[0.00002335527,0.00010480765,0.1710524,0.0000060408556,0.0000027648803,0.0007527355,0.006177767,0.037495792,0.722897,0.0000151653985,0.00001302234,0.061459165],"study_design_scores_gemma":[0.0003278691,0.000017263335,0.050471283,0.000009383287,0.000009931177,0.00042273762,0.0002879901,0.94573087,0.0015498253,0.00092528237,0.000012412178,0.00023512608],"about_ca_topic_score_codex":0.0021173968,"about_ca_topic_score_gemma":0.001074961,"teacher_disagreement_score":0.90823513,"about_ca_system_score_codex":0.00019335146,"about_ca_system_score_gemma":0.000035572222,"threshold_uncertainty_score":0.7343648},"labels":[],"label_agreement":null},{"id":"W2108476865","doi":"10.1029/2002jd002964","title":"Field comparison of network Sun photometers","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":67,"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 de Sherbrooke","funders":"","keywords":"Photometer; Sun photometer; Comparability; Aerosol; Instrumentation (computer programming); Remote sensing; Environmental science; Meteorology; Observatory; AERONET; Computer science; Geography; Physics; Optics; Mathematics; Astronomy","score_opus":0.035865396138528384,"score_gpt":0.3431149546763892,"score_spread":0.3072495585378608,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2108476865","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":[0.9803906,0.000288017,0.0011814468,0.00014540038,0.0001510506,0.000105248466,4.4592576e-7,0.000004711707,0.017733064],"genre_scores_gemma":[0.9909171,0.000051408344,0.007889084,0.000068778136,0.00014876465,0.0000026791367,1.4225546e-7,0.000014373903,0.00090765546],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9970392,0.00032789007,0.00053616165,0.00017292239,0.0013663055,0.0005575452],"domain_scores_gemma":[0.99824136,0.0008487114,0.00028237666,0.0002466873,0.000100888545,0.00027997492],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010544865,0.00012974483,0.00041585744,0.0000012946724,0.00014618604,0.000032138378,0.0004774965,0.00008389416,0.0043621785],"category_scores_gemma":[0.00068201555,0.00009712578,0.00021170823,0.000707503,0.00038138038,0.00016759953,0.00014739395,0.0006695239,0.00012582453],"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":[0.0007598898,0.0014211849,0.75765973,0.000039710067,0.00016529099,0.000078216064,0.00077568047,0.008167363,0.019088926,0.0024966937,0.17044294,0.038904376],"study_design_scores_gemma":[0.0040993327,0.021732822,0.5737025,0.0004624933,0.00014336432,0.00007716913,0.0057665557,0.008010498,0.09496409,0.047466375,0.24234322,0.0012315685],"about_ca_topic_score_codex":0.0004481148,"about_ca_topic_score_gemma":0.000051525207,"teacher_disagreement_score":0.18395722,"about_ca_system_score_codex":0.000100274105,"about_ca_system_score_gemma":0.00006547436,"threshold_uncertainty_score":0.996548},"labels":[],"label_agreement":null},{"id":"W2109076304","doi":"10.5194/acp-12-3205-2012","title":"Detection of particle layers in backscatter profiles: application to Antarctic lidar measurements","year":2012,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"Impact","funders":"Institut Polaire Français Paul Emile Victor","keywords":"Lidar; Backscatter (email); Remote sensing; Range (aeronautics); Environmental science; Robustness (evolution); Geology; Computer science; Materials science; Telecommunications","score_opus":0.009412992033990332,"score_gpt":0.21798428815588683,"score_spread":0.2085712961218965,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2109076304","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":[0.99042076,0.000039812345,0.007884014,0.000031166222,0.000016586248,0.00013434861,7.430985e-7,0.00001052512,0.001462067],"genre_scores_gemma":[0.9964474,0.0000053872727,0.00309472,0.00010505057,0.000054857057,0.000042325224,0.0000015075694,0.000008989091,0.00023978225],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9993487,0.000011261791,0.00013519391,0.00016102889,0.0001453571,0.00019845608],"domain_scores_gemma":[0.9996897,0.0000101153855,0.00004921453,0.00015019496,0.000005768574,0.0000949933],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009707665,0.00009376479,0.00010268412,1.0305809e-8,0.000037581787,0.0000056121357,0.00006731808,0.00003885001,0.00031834978],"category_scores_gemma":[0.0000049386936,0.00009165655,0.00002175149,0.00021965119,0.00005608797,0.00012327416,0.000044192897,0.000056986744,0.000060695453],"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":[0.000014656092,0.000104203944,0.44073954,0.000023492657,0.000004902713,6.714076e-8,0.00044265343,0.0004510237,0.48077306,0.0000014652735,0.000015627551,0.0774293],"study_design_scores_gemma":[0.00029881773,0.00003405941,0.37145242,0.000015474048,0.000021077649,0.0000019071261,0.0002580726,0.005189023,0.6215176,0.00006732296,0.00093563617,0.00020861258],"about_ca_topic_score_codex":0.00022818753,"about_ca_topic_score_gemma":0.0000055132577,"teacher_disagreement_score":0.1407445,"about_ca_system_score_codex":0.00006553768,"about_ca_system_score_gemma":0.0000036214005,"threshold_uncertainty_score":0.37376457},"labels":[],"label_agreement":null},{"id":"W2109218639","doi":"10.5194/acp-14-2015-2014","title":"Comparison of MODIS 3 km and 10 km resolution aerosol optical depth retrievals over land with airborne sunphotometer measurements during ARCTAS summer 2008","year":2014,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":39,"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":"National Aeronautics and Space Administration","keywords":"Environmental science; Aerosol; Moderate-resolution imaging spectroradiometer; AERONET; Remote sensing; Cirrus; Spectroradiometer; Troposphere; Altitude (triangle); Satellite; Meteorology; Deep blue; Atmospheric sciences; Geology; Geography; Reflectivity; Physics","score_opus":0.017654180242586994,"score_gpt":0.24702008093591157,"score_spread":0.22936590069332458,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2109218639","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":[0.99232036,0.00012220257,0.0014130243,0.00001670112,0.000013711704,0.00011864783,0.000005346955,0.000020933303,0.0059690573],"genre_scores_gemma":[0.9926798,0.000029632356,0.00633363,0.00002819552,0.0000635124,0.000009275709,0.000013480166,0.000021619328,0.0008208803],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986296,0.000025216501,0.0002472966,0.00039993916,0.0004012481,0.00029665141],"domain_scores_gemma":[0.9993714,0.00003966215,0.00013881974,0.00026879236,0.000020287456,0.00016101274],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012253317,0.0002334041,0.00033232645,4.21123e-8,0.0001415241,0.000028772545,0.00011348941,0.00010480255,0.0008513625],"category_scores_gemma":[0.000017868437,0.00019580351,0.000043031767,0.00018693894,0.0003707273,0.00013008522,0.00010922256,0.00014895255,0.000010851203],"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":[0.0002998655,0.00023235238,0.8793217,0.00013893166,0.000062629144,0.0000017241975,0.0002337909,0.0020095375,0.10558891,0.0000034362395,0.00038272084,0.011724434],"study_design_scores_gemma":[0.0024967727,0.0002944314,0.6841274,0.0001106693,0.00016408286,0.000014465936,0.000095527306,0.042728834,0.26819286,0.00008169543,0.0009861699,0.00070713303],"about_ca_topic_score_codex":0.00014162496,"about_ca_topic_score_gemma":0.000015592053,"teacher_disagreement_score":0.1951943,"about_ca_system_score_codex":0.000054557277,"about_ca_system_score_gemma":0.000009035514,"threshold_uncertainty_score":0.9321822},"labels":[],"label_agreement":null},{"id":"W2109527508","doi":"10.5194/asr-2-5-2008","title":"Analysis of aerosol optical depth evaluation in polar regions and associated uncertainties","year":2008,"lang":"en","type":"article","venue":"Advances in science and research","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":7,"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":"National Institute of Polar Research; Universität Bremen; Université de Sherbrooke","keywords":"Sun photometer; Photometer; Polar; Aerosol; Environmental science; Remote sensing; Meteorology; Atmospheric sciences; Optics; Geology; Physics; Astronomy","score_opus":0.05290372585914474,"score_gpt":0.38149217664039464,"score_spread":0.3285884507812499,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2109527508","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":[0.9922894,0.00081021746,0.000044033954,0.00014114183,0.0000130143435,0.0001340449,7.183298e-7,0.0000026760163,0.0065647285],"genre_scores_gemma":[0.9971923,0.0023267935,0.00037087058,0.000016659196,0.0000026964249,0.000013119727,8.3109796e-7,0.0000018858626,0.00007484663],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978122,0.00011220041,0.00016594068,0.0003100577,0.0012803752,0.00031921378],"domain_scores_gemma":[0.9995128,0.00017612295,0.00003381726,0.00013167049,0.000072200375,0.00007339934],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0034548414,0.00005349034,0.00014389669,0.0000419808,0.0002530583,0.000016396905,0.00019455938,0.000037118825,0.00004406614],"category_scores_gemma":[0.00085412746,0.000042102893,0.000014378907,0.0045037866,0.0038359421,0.00050028483,0.0001973632,0.00015043415,0.0000018007404],"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":[0.000008401491,0.00005185267,0.9811248,0.0000017639844,0.0000035944684,0.0000035975684,0.0011705296,0.0037401924,0.002086665,0.00017062426,0.000009194825,0.011628765],"study_design_scores_gemma":[0.00019312368,0.000077137825,0.9591597,0.00001206874,0.000009595934,0.0000013986706,0.0014397699,0.038113367,0.00042025137,0.0004460552,0.00006346014,0.00006407712],"about_ca_topic_score_codex":0.00091572595,"about_ca_topic_score_gemma":0.0050503276,"teacher_disagreement_score":0.034373175,"about_ca_system_score_codex":0.0001901528,"about_ca_system_score_gemma":0.00008010015,"threshold_uncertainty_score":0.998875},"labels":[],"label_agreement":null},{"id":"W2109587482","doi":"10.5194/acp-10-5685-2010","title":"Uncertainty assessment of current size-resolved parameterizations for below-cloud particle scavenging by rain","year":2010,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":180,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Dalhousie University; Helsingin Yliopisto","keywords":"Aerosol; Scavenging; Particle (ecology); Particle size; Range (aeronautics); Current (fluid); Particle-size distribution; Meteorology; Environmental science; Atmospheric sciences; Computational physics; Turbulence; Mechanics; Physics; Chemistry; Thermodynamics; Materials science","score_opus":0.007474306296747624,"score_gpt":0.2537330540537016,"score_spread":0.246258747756954,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2109587482","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":[0.94224346,0.00003559932,0.056275953,0.000053676486,0.000092357564,0.00022529325,0.000032044252,0.00002488751,0.0010167146],"genre_scores_gemma":[0.9715951,0.00002063194,0.02740913,0.00004292677,0.000098941826,0.0000785842,0.000026795728,0.000016654081,0.00071121345],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99907404,0.000011593711,0.00021729352,0.00028377867,0.00016421455,0.00024908822],"domain_scores_gemma":[0.99936944,0.00013828438,0.00011332373,0.00024539515,0.000015126258,0.00011845619],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000116863805,0.00016096902,0.00018484663,6.868175e-9,0.00016313727,0.000024054225,0.00012218811,0.00006082093,0.0010988876],"category_scores_gemma":[0.000034066055,0.00015319847,0.0000746273,0.00015592891,0.00023058041,0.00007536062,0.00007553602,0.00015035347,0.0000027508509],"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":[0.000019478572,0.00034180612,0.02972417,0.000096781965,0.000029509443,3.7916695e-7,0.00023086886,0.005419825,0.8534484,0.00030311072,0.0014841737,0.108901486],"study_design_scores_gemma":[0.0021232474,0.00014323527,0.01323734,0.000056913083,0.00014465053,0.0000045195147,0.0002757438,0.80165863,0.12809713,0.0038914285,0.049434,0.0009331625],"about_ca_topic_score_codex":0.000044584427,"about_ca_topic_score_gemma":0.0000028783645,"teacher_disagreement_score":0.7962388,"about_ca_system_score_codex":0.000031617674,"about_ca_system_score_gemma":0.000022863756,"threshold_uncertainty_score":0.9998143},"labels":[],"label_agreement":null},{"id":"W2109762177","doi":"10.5194/acpd-12-1687-2012","title":"Strong sensitivity of aerosol concentrations to convective wet scavenging parameterizations in a global model","year":2012,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; BioFrontiers Institute, University of Colorado Boulder; National Oceanic and Atmospheric Administration; Killam Trusts","keywords":"Aerosol; Atmospheric sciences; Scavenging; Ice crystals; Precipitation; Cloud base; Convection; Environmental science; Evaporation; Liquid water content; Free convective layer; Meteorology; Climatology; Cloud computing; Chemistry; Geology; Physics","score_opus":0.013939323559718001,"score_gpt":0.25246070948080795,"score_spread":0.23852138592108996,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2109762177","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":[0.6432811,0.00000225858,0.34865358,0.00006279703,0.000025130123,0.00014184635,0.000014573158,0.000012081509,0.007806606],"genre_scores_gemma":[0.982831,8.3039123e-7,0.016884543,0.0001473954,0.000008583082,0.000013230576,0.0000026255552,0.000004323059,0.00010744287],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9992804,0.0000463536,0.00014772707,0.00013395393,0.00012963422,0.00026194865],"domain_scores_gemma":[0.999692,0.000032114283,0.000036273144,0.000116375944,0.000006279037,0.000116958254],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001512816,0.00008017264,0.00011170856,8.394409e-7,0.000049707112,0.000007683037,0.000048961763,0.000033933673,0.00030732184],"category_scores_gemma":[0.00003439687,0.00007670543,0.000027561551,0.0002624645,0.00007999598,0.00020917637,0.00008494707,0.000041328032,0.000047652884],"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":[0.0000074166032,0.00014090353,0.6549038,0.0000016445848,0.0000055360915,5.2736175e-7,0.00089694996,0.3161714,0.022659155,0.004526864,0.000100956335,0.0005848061],"study_design_scores_gemma":[0.00030141656,0.000039401904,0.27165917,0.000012280567,0.000013464347,0.000003740173,0.00096386456,0.71669763,0.009940307,0.00011854978,0.000019481873,0.00023071583],"about_ca_topic_score_codex":0.0005947521,"about_ca_topic_score_gemma":0.000612097,"teacher_disagreement_score":0.4005262,"about_ca_system_score_codex":0.00017196224,"about_ca_system_score_gemma":0.000013017694,"threshold_uncertainty_score":0.33649585},"labels":[],"label_agreement":null},{"id":"W2111505112","doi":"10.1109/igarss.2007.4423805","title":"An investigation of air pollution in southern Ontario, Canada, with MODIS and MISR Aerosol Data","year":2007,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","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":true,"ca_institutions":"McMaster University","funders":"","keywords":"Aerosol; Environmental science; Moderate-resolution imaging spectroradiometer; Spectroradiometer; Relative humidity; Particulates; Wind speed; Atmospheric sciences; Air pollution; Meteorology; Linear regression; Humidity; Climatology; Pollution; Geography; Reflectivity; Geology; Satellite","score_opus":0.010383832425460164,"score_gpt":0.19940422276293737,"score_spread":0.1890203903374772,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2111505112","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":[0.99710053,0.00000496184,0.0012190782,0.00016011199,0.000008962529,0.00008003334,0.000008951058,0.000005660431,0.0014116938],"genre_scores_gemma":[0.99490875,4.482042e-7,0.0039591226,0.0003819653,0.000004969329,7.3249674e-7,0.000017652965,0.000004472921,0.0007218796],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993836,0.000010097438,0.000118739175,0.00018957505,0.00017162517,0.00012632168],"domain_scores_gemma":[0.99962157,0.0000058823903,0.000043625518,0.00024348487,0.000002527871,0.00008289153],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015961683,0.000062942025,0.00006719489,7.4730553e-7,0.00003204881,0.0000039187435,0.000131397,0.000028406852,0.00043880954],"category_scores_gemma":[0.0000019516656,0.000048268288,0.0000029223975,0.000090872876,0.00011276185,0.00015786919,0.000059368354,0.000047266283,0.000001989747],"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":[0.000018620345,0.000013629437,0.9931676,0.0000016239198,0.0000018113941,0.000002292973,0.0015451103,0.0012165,0.0026051612,0.0000124387725,0.00034706297,0.0010681812],"study_design_scores_gemma":[0.00020989963,0.000056482295,0.9945172,0.000005316212,0.0000041922326,0.0000021161009,0.0022085458,0.0017533668,0.001045748,0.000026317435,0.00008326437,0.000087546585],"about_ca_topic_score_codex":0.99576837,"about_ca_topic_score_gemma":0.9997515,"teacher_disagreement_score":0.003983134,"about_ca_system_score_codex":0.0001679678,"about_ca_system_score_gemma":0.000074447526,"threshold_uncertainty_score":0.48046568},"labels":[],"label_agreement":null},{"id":"W2111634535","doi":"10.5589/m10-033","title":"Spectral, spatial, and temporal sensitivity of correlating MODIS aerosol optical depth with ground-based fine particulate matter (PM<sub>2.5</sub>) across southern Ontario","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Moderate-resolution imaging spectroradiometer; Environmental science; Particulates; Spectroradiometer; Aerosol; Atmospheric sciences; Morning; Ground level; Remote sensing; Angstrom; Meteorology; Reflectivity; Geography; Satellite; Geology; Physics; Chemistry","score_opus":0.00801359120119589,"score_gpt":0.1948162947575407,"score_spread":0.18680270355634482,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2111634535","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":[0.97555745,0.000008896748,0.023695298,0.00030858815,0.0001470882,0.00009815166,0.000005919859,0.000005198774,0.00017339471],"genre_scores_gemma":[0.9589839,4.2373193e-7,0.040742062,0.00013783097,0.0000755551,1.9075006e-8,0.0000016559977,0.00002847723,0.000030071007],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985584,0.0000596826,0.0003852947,0.00022578772,0.00027221238,0.00049859955],"domain_scores_gemma":[0.9987372,0.00006089961,0.0003423755,0.00019637668,0.000046484314,0.0006166228],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045630927,0.00021140075,0.0003322591,0.000005698576,0.00024564847,0.00008831622,0.000073279116,0.00011744215,0.00009484603],"category_scores_gemma":[0.00004397951,0.00017557049,0.000086156,0.00011866408,0.0005861229,0.00014333612,0.000026801565,0.000588738,0.000017951108],"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":[0.00008961488,0.00001665172,0.78263444,0.000013122978,0.0000407215,0.0010511813,0.0031414437,0.004145952,0.13152602,9.047839e-7,0.00006634235,0.07727358],"study_design_scores_gemma":[0.0016079944,0.0004121728,0.84413713,0.00030516498,0.00014660772,0.0030187147,0.0009997668,0.09633201,0.05212412,0.00006883203,0.0001405353,0.0007069566],"about_ca_topic_score_codex":0.32800245,"about_ca_topic_score_gemma":0.9745822,"teacher_disagreement_score":0.64657974,"about_ca_system_score_codex":0.00021069386,"about_ca_system_score_gemma":0.00029625543,"threshold_uncertainty_score":0.7159557},"labels":[],"label_agreement":null},{"id":"W2112014702","doi":"10.5194/acp-13-7075-2013","title":"Spatial and seasonal distribution of Arctic aerosols observed by the CALIOP satellite instrument (2006–2012)","year":2013,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":69,"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","funders":"","keywords":"Aerosol; Lidar; Environmental science; Troposphere; Satellite; Arctic; Atmospheric sciences; Haze; Extinction (optical mineralogy); Daytime; Climatology; Remote sensing; Meteorology; Geology; Geography; Oceanography","score_opus":0.006903814902651612,"score_gpt":0.18181140998876694,"score_spread":0.17490759508611534,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2112014702","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":[0.9965288,0.00035183402,0.001872164,0.00026339354,0.000022897833,0.00015360139,0.000026810576,0.0000126811165,0.0007678177],"genre_scores_gemma":[0.99717265,0.00018131413,0.00076274085,0.000094503004,0.00007658547,0.000027774357,0.000056360906,0.000010373722,0.0016176839],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990948,0.000021130423,0.00018179287,0.00025539915,0.00021461397,0.00023230207],"domain_scores_gemma":[0.9995187,0.000041883162,0.00010522018,0.00020363662,0.000014263763,0.00011629884],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00006231261,0.00017499867,0.00016308819,3.9894763e-9,0.0001435092,0.000039857,0.00012705267,0.00007237468,0.0015906533],"category_scores_gemma":[0.000007931945,0.00012929089,0.00004297549,0.000112138034,0.00042011007,0.00014709914,0.000120668825,0.00012784316,0.000020745998],"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":[0.000034845983,0.00020780972,0.48189124,0.0001192638,0.00005673932,0.0000010259226,0.00026287028,0.00014240813,0.04841182,0.00005073902,0.0042583104,0.46456292],"study_design_scores_gemma":[0.0012355795,0.00014977803,0.9182033,0.000063442145,0.00011818906,0.000024446514,0.00036792082,0.027367944,0.028484114,0.0024698037,0.020771122,0.0007443732],"about_ca_topic_score_codex":0.002113998,"about_ca_topic_score_gemma":0.0000065298595,"teacher_disagreement_score":0.46381855,"about_ca_system_score_codex":0.000052804688,"about_ca_system_score_gemma":0.000009769877,"threshold_uncertainty_score":0.99932206},"labels":[],"label_agreement":null},{"id":"W2112100398","doi":"10.1002/qj.2606","title":"On the use of simulated photon paths to co‐register top‐of‐atmosphere radiances in <i>EarthCARE</i> radiative closure experiments","year":2015,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":12,"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":"Radiative transfer; Remote sensing; Environmental science; Atmospheric radiative transfer codes; Radiometer; Cloud top; Atmosphere (unit); Meteorology; Satellite; Radiance; Cloud computing; Computer science; Geology; Physics; Optics","score_opus":0.04487382338815933,"score_gpt":0.2632571770110592,"score_spread":0.2183833536228999,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2112100398","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":[0.99806654,0.0001250014,0.00021261221,0.0007999239,0.00017640293,0.00028549656,0.000008095455,0.0000044517283,0.0003214529],"genre_scores_gemma":[0.99668884,0.00000646213,0.0017703234,0.001359694,0.00003425138,0.0000044369585,2.7048074e-7,0.000009511325,0.00012621553],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99786043,0.00045584634,0.0005772783,0.0001945913,0.0006357244,0.0002761243],"domain_scores_gemma":[0.9985852,0.0003767918,0.0005388963,0.00028434768,0.000045439,0.00016930349],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00073235855,0.000189758,0.0004095294,8.5784336e-7,0.0000762639,0.000025630703,0.0005744128,0.00015312656,0.00047197577],"category_scores_gemma":[0.00014466459,0.00009082398,0.00040331495,0.00026626288,0.00036734252,0.00010914958,0.000067189365,0.00037563348,0.000012991497],"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":[0.0017968824,0.00119222,0.48304474,0.000015632342,0.0003289232,0.00003813959,0.034482308,0.42831343,0.005353796,0.00022485973,0.032622173,0.012586878],"study_design_scores_gemma":[0.012938336,0.046955995,0.74353135,0.0005752052,0.0003627414,0.000054328448,0.03615753,0.09202545,0.02552082,0.010451904,0.029449567,0.0019767687],"about_ca_topic_score_codex":0.00026256285,"about_ca_topic_score_gemma":0.000014714056,"teacher_disagreement_score":0.33628798,"about_ca_system_score_codex":0.00013819766,"about_ca_system_score_gemma":0.000024587333,"threshold_uncertainty_score":0.5167804},"labels":[],"label_agreement":null},{"id":"W2112326831","doi":"10.1029/2000jd000281","title":"The cloud albedo‐cloud droplet effective radius relationship for clean and polluted clouds from RACE and FIRE.ACE","year":2002,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":111,"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":"Drizzle; Liquid water content; Effective radius; Cloud albedo; Environmental science; Liquid water path; Aerosol; Atmospheric sciences; Cloud computing; Albedo (alchemy); Cloud top; Meteorology; Cloud fraction; RADIUS; Sea salt aerosol; Cloud cover; Physics; Astrophysics; Precipitation","score_opus":0.0227056172381312,"score_gpt":0.2858723820024765,"score_spread":0.2631667647643453,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2112326831","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":[0.99214035,0.0021835386,0.0006181481,0.0036775565,0.00021323573,0.0005288962,0.000012105157,0.0000125470715,0.00061361864],"genre_scores_gemma":[0.99257797,0.0006966047,0.0027281651,0.000090562055,0.0007088456,0.000026845852,9.407972e-7,0.00003350224,0.0031365596],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9971271,0.00049782783,0.00043025948,0.000362196,0.00093726447,0.00064534246],"domain_scores_gemma":[0.9932049,0.005716498,0.0002463504,0.0003011199,0.000095468095,0.00043565244],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011755811,0.00022209837,0.0003711733,0.000001368297,0.0010464664,0.00021569389,0.0004356112,0.00013194447,0.00035287483],"category_scores_gemma":[0.0014951791,0.00014572933,0.00015213626,0.00039003708,0.0011348298,0.00027121595,0.00031832757,0.0008484125,0.00007251373],"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":[0.0031668541,0.0008939546,0.17045309,0.00005312429,0.0004456843,0.00012005169,0.00487661,0.00061544805,0.0037446269,0.0037918047,0.24562865,0.5662101],"study_design_scores_gemma":[0.0034341512,0.0032496639,0.8194884,0.000115907475,0.00010641796,0.000054498865,0.0022955483,0.049275078,0.00058443536,0.036418628,0.084472135,0.00050511025],"about_ca_topic_score_codex":0.00093332847,"about_ca_topic_score_gemma":0.0002045761,"teacher_disagreement_score":0.64903533,"about_ca_system_score_codex":0.00018484754,"about_ca_system_score_gemma":0.000024826273,"threshold_uncertainty_score":0.8048679},"labels":[],"label_agreement":null},{"id":"W2112985153","doi":"10.1175/jtech-d-11-00199.1","title":"Improved Imaging and Image Analysis System for Application to Measurement of Small Ice Crystals","year":2012,"lang":"en","type":"article","venue":"Journal of Atmospheric and Oceanic Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":11,"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 Waterloo","funders":"Canadian Space Agency","keywords":"Polygon (computer graphics); Particle (ecology); Optics; Pixel; Materials science; Remote sensing; Computer science; Geology; Physics","score_opus":0.0055646573614841245,"score_gpt":0.20761634365568618,"score_spread":0.20205168629420206,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2112985153","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":[0.60766065,0.00096930156,0.39083168,0.00023145,0.000037151854,0.00017038586,0.0000011089878,0.000014697831,0.00008357379],"genre_scores_gemma":[0.90719783,0.00004258486,0.092656404,0.00003692575,0.00003015906,0.000008922799,1.5025455e-7,0.000010467978,0.000016555327],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99898136,0.000016758844,0.00043337946,0.00015923247,0.00016382376,0.00024547768],"domain_scores_gemma":[0.9991498,0.000022076856,0.0004639537,0.00016695005,0.000071779934,0.0001254214],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006191937,0.00012396237,0.0003608856,0.0000034455404,0.00006996918,0.000011024532,0.00016900866,0.00007645798,0.000020540598],"category_scores_gemma":[0.00004984378,0.000099616555,0.00008353093,0.0005363398,0.00012655268,0.00012000935,0.00012188813,0.00008753395,0.0000010803406],"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":[0.00015166451,0.0001861522,0.5449089,0.00013421064,0.00045749164,0.0000025978607,0.00047840743,0.00023659573,0.33935836,0.0006564862,0.00037128045,0.113057874],"study_design_scores_gemma":[0.005780177,0.0028426915,0.7576061,0.00024134167,0.006031495,0.00081601494,0.025805678,0.12698205,0.050127473,0.0012027619,0.020853044,0.0017111889],"about_ca_topic_score_codex":0.00003515309,"about_ca_topic_score_gemma":0.0000066226,"teacher_disagreement_score":0.29953718,"about_ca_system_score_codex":0.00014156435,"about_ca_system_score_gemma":0.000011725094,"threshold_uncertainty_score":0.40622452},"labels":[],"label_agreement":null},{"id":"W2113007518","doi":"10.1109/igarss.2000.860467","title":"Modelling of aerosol optical depth variability at regional scale","year":2002,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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 de Sherbrooke","funders":"","keywords":"Environmental science; Radiative transfer; Inversion (geology); Remote sensing; Aerosol; Atmospheric model; Photometry (optics); Atmospheric correction; Data assimilation; Spatial ecology; Atmospheric circulation; Meteorology; Computer science; Geology; Geography; Reflectivity","score_opus":0.032180499516163405,"score_gpt":0.20995172928069178,"score_spread":0.17777122976452836,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2113007518","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":[0.7021517,0.0000086400305,0.0868046,0.00015556274,0.000021331382,0.000063019885,4.6092742e-7,0.000020951305,0.21077369],"genre_scores_gemma":[0.9503107,0.000013286804,0.04269737,0.00012879776,0.000016920803,0.0000042231027,6.675853e-7,0.000006733644,0.0068212757],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9990851,0.000020542395,0.00018407134,0.0002460991,0.00026986087,0.0001942789],"domain_scores_gemma":[0.99957556,0.00004687639,0.000036712252,0.00023498434,0.000004802098,0.00010103984],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001286479,0.00008626883,0.000117572126,3.0729635e-7,0.000071083115,0.0000048045777,0.00014194445,0.00006207634,0.018937247],"category_scores_gemma":[0.0000068900804,0.000069120404,0.0000620256,0.000091747446,0.00026655194,0.00007116293,0.00015774556,0.00006112783,0.00050982443],"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":[0.00005917363,0.001028075,0.39864647,0.000022206923,0.000023082956,0.0000054497627,0.0008741378,0.5497369,0.014654129,0.0021116524,0.021241963,0.01159675],"study_design_scores_gemma":[0.0002805138,0.00007123212,0.0067947684,0.0000048898146,0.000012997077,0.000009946885,0.000044907865,0.98513585,0.005751399,0.0005306304,0.0011481514,0.00021469631],"about_ca_topic_score_codex":0.00014902838,"about_ca_topic_score_gemma":0.000049560113,"teacher_disagreement_score":0.43539897,"about_ca_system_score_codex":0.000089743735,"about_ca_system_score_gemma":0.0000017425068,"threshold_uncertainty_score":0.9819596},"labels":[],"label_agreement":null},{"id":"W2113116261","doi":"10.1175/2007jas2207.1","title":"Aerosol–Cloud Interactions in a Mesoscale Model. Part I: Sensitivity to Activation and Collision–Coalescence","year":2008,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","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":"McGill University","funders":"","keywords":"Aerosol; Coalescence (physics); Atmospheric sciences; Drop (telecommunication); Environmental science; Mesoscale meteorology; Collision; Meteorology; Effective radius; Liquid water content; Particle (ecology); Mechanics; Physics; Cloud computing; Astrophysics; Geology","score_opus":0.02558319577539207,"score_gpt":0.253933944930648,"score_spread":0.22835074915525597,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2113116261","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":[0.9926852,0.000022243023,0.0035311014,0.0023912145,0.00033432175,0.00012193805,5.486863e-7,0.0000057296406,0.00090767577],"genre_scores_gemma":[0.9829508,0.000052787644,0.015598898,0.00068493007,0.000063140586,0.0000027916635,2.6022459e-8,0.0000050534654,0.00064157846],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99859786,0.0001026936,0.00031861357,0.00020941829,0.0005459073,0.00022551595],"domain_scores_gemma":[0.99932253,0.000120464756,0.00026258721,0.00014752107,0.000023447283,0.00012347387],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006707116,0.000114097136,0.00017902184,0.0000010910469,0.0004513378,0.00003614849,0.00031792212,0.000027540811,0.000091760005],"category_scores_gemma":[0.00019164085,0.00007165795,0.000065458335,0.00089752366,0.00052228157,0.00053465593,0.0002373983,0.00018590614,0.000011526622],"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":[0.000049375984,0.00014921073,0.26038143,0.0000022952706,0.000005642021,0.00001537578,0.002087086,0.70563006,0.02242067,0.000028436345,0.0073856576,0.0018447357],"study_design_scores_gemma":[0.0006147754,0.00035107677,0.45705917,0.00023958107,0.000022664068,0.00074614625,0.001968758,0.52461934,0.009916893,0.0005882857,0.003424393,0.00044891945],"about_ca_topic_score_codex":0.00024316525,"about_ca_topic_score_gemma":0.00019813732,"teacher_disagreement_score":0.19667774,"about_ca_system_score_codex":0.00015459603,"about_ca_system_score_gemma":0.00006972975,"threshold_uncertainty_score":0.3471371},"labels":[],"label_agreement":null},{"id":"W2113345704","doi":"10.1364/josaa.18.001275","title":"Mie-scattering formalism for spherical particles embedded in an absorbing medium","year":2001,"lang":"en","type":"article","venue":"Journal of the Optical Society of America A","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":124,"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","funders":"National Science Foundation","keywords":"Mie scattering; Scattering; Optics; Extinction (optical mineralogy); Physics; Formalism (music); Bessel function; Diffraction; Molar absorptivity; Light scattering; Computational physics","score_opus":0.014629221103936729,"score_gpt":0.2566185982496455,"score_spread":0.24198937714570878,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2113345704","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":[0.97496986,0.00003024818,0.020872999,0.0036097604,0.000091711205,0.00010146951,6.025311e-7,0.000004784356,0.00031854425],"genre_scores_gemma":[0.85945153,0.00004528157,0.13946754,0.0008920271,0.00008679467,0.0000034638367,1.2915694e-7,0.0000109123675,0.00004230981],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9987567,0.000030909247,0.00044767343,0.00011500799,0.0003511363,0.00029859267],"domain_scores_gemma":[0.9993074,0.0000930381,0.00029236893,0.0001517058,0.00001907299,0.00013643496],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031935997,0.00010425007,0.00026163994,8.0252835e-7,0.00008245637,0.000018558352,0.00038464082,0.000058121583,0.00031712488],"category_scores_gemma":[0.000051080046,0.00006751203,0.00032675447,0.0002234347,0.00041500968,0.00022527136,0.00013558709,0.00019101887,0.000004056505],"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":[0.0007581104,0.0018766674,0.30764157,0.00007326629,0.00018437365,0.000021520067,0.019699069,0.054938886,0.48576483,0.000063052714,0.014639424,0.11433924],"study_design_scores_gemma":[0.005771169,0.003398351,0.6059463,0.00030845113,0.0002846045,0.00034113709,0.043023773,0.2852117,0.026166813,0.0043093306,0.024110332,0.0011280436],"about_ca_topic_score_codex":0.000044208566,"about_ca_topic_score_gemma":0.0000050843223,"teacher_disagreement_score":0.459598,"about_ca_system_score_codex":0.00010612709,"about_ca_system_score_gemma":0.000018741888,"threshold_uncertainty_score":0.3472295},"labels":[],"label_agreement":null},{"id":"W2114944083","doi":"10.3137/ao.450403","title":"A practical approach for the assimilation of cloudy infrared radiances and its evaluation using airs simulated observations","year":2007,"lang":"en","type":"article","venue":"ATMOSPHERE-OCEAN","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada; Université Laval; TransCanada (Canada)","funders":"","keywords":"Radiance; Emissivity; Overcast; Remote sensing; Cloud cover; Environmental science; Context (archaeology); Cloud computing; Data assimilation; Physics; Meteorology; Sky; Computer science; Optics; Geography","score_opus":0.07610650004064026,"score_gpt":0.32154797796868245,"score_spread":0.2454414779280422,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2114944083","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":[0.90492976,0.00018304151,0.09243354,0.00015908453,0.00007415983,0.0009159636,0.000004216743,0.000023168963,0.0012770847],"genre_scores_gemma":[0.9437264,0.000014291065,0.05587441,0.000120669654,0.000052659136,0.0000047465037,0.00001365721,0.000017324362,0.00017582817],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9987024,0.000060938488,0.00033088797,0.00026481244,0.00040118504,0.00023977624],"domain_scores_gemma":[0.99901223,0.0004184232,0.00023565999,0.00019543349,0.000062434585,0.00007579635],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001135557,0.00013469605,0.00014966863,4.2210291e-7,0.0002937369,0.000027872347,0.000119855926,0.00010194205,0.00021647266],"category_scores_gemma":[0.00031671746,0.00010199605,0.000052712912,0.0003476928,0.0001410689,0.0003178468,0.00006085675,0.00009642361,0.0000021994476],"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":[0.00013932773,0.00020244677,0.34173867,0.000026965075,0.000079899895,6.8359776e-7,0.0015387636,0.64259785,0.0013131319,0.00063696067,0.0017293602,0.00999591],"study_design_scores_gemma":[0.00046715513,0.000058189293,0.19118796,0.0000061895166,0.000099145574,0.0000027673273,0.00074791413,0.80624586,0.00019667107,0.00026655084,0.0006123997,0.00010919044],"about_ca_topic_score_codex":0.00017914183,"about_ca_topic_score_gemma":0.00003890629,"teacher_disagreement_score":0.16364798,"about_ca_system_score_codex":0.00011615071,"about_ca_system_score_gemma":0.000042554504,"threshold_uncertainty_score":0.4159278},"labels":[],"label_agreement":null},{"id":"W2115012166","doi":"10.1175/1520-0426(2002)019<1003:pcimap>2.0.co;2","title":"Profiling Cloud Ice Mass and Particle Characteristic Size from Doppler Radar Measurements","year":2002,"lang":"en","type":"article","venue":"Journal of Atmospheric and Oceanic Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":101,"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 Aeronautics and Space Administration","keywords":"Ice cloud; Doppler effect; Radar; Particle-size distribution; Remote sensing; Liquid water content; Particle size; Particle (ecology); Ice crystals; Environmental science; Geology; Meteorology; Atmospheric sciences; Optics; Physics; Cloud computing; Radiative transfer","score_opus":0.012045506777618498,"score_gpt":0.19841133449013826,"score_spread":0.18636582771251975,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2115012166","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":[0.994471,0.0019295382,0.0019069102,0.0010220027,0.00023392054,0.00010062452,0.0000018670531,0.00003890294,0.00029524026],"genre_scores_gemma":[0.9612154,0.00060292514,0.037605755,0.00023632385,0.00009809276,0.0000019437111,1.5918333e-7,0.000018470397,0.00022097796],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998689,0.000035455247,0.00043624858,0.0002516434,0.000277627,0.00031005012],"domain_scores_gemma":[0.99923563,0.00006496766,0.00035282967,0.00018185536,0.000022107759,0.00014262993],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00019860221,0.00018237517,0.00032929517,6.702631e-7,0.0001334288,0.000030545503,0.00022323671,0.00015979845,0.0015750669],"category_scores_gemma":[0.00011692895,0.00014671759,0.000048102236,0.00025703845,0.00025396625,0.00018037463,0.00013552391,0.00028895616,0.000036123944],"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":[0.00009481049,0.00020112736,0.81996053,0.000015100674,0.00013743364,0.000120082776,0.00037896537,0.0000196761,0.12836702,0.00016514963,0.0021252697,0.048414845],"study_design_scores_gemma":[0.009933384,0.0035190685,0.87787914,0.00026592435,0.00085580273,0.001657593,0.005811311,0.021119783,0.02930093,0.013812818,0.03367743,0.002166837],"about_ca_topic_score_codex":0.000016827713,"about_ca_topic_score_gemma":0.0000020454456,"teacher_disagreement_score":0.099066086,"about_ca_system_score_codex":0.00007903121,"about_ca_system_score_gemma":0.000007753984,"threshold_uncertainty_score":0.9993376},"labels":[],"label_agreement":null},{"id":"W2115307016","doi":"10.5194/acp-11-8489-2011","title":"Horizontal variability of aerosol optical depth observed during the ARCTAS airborne experiment","year":2011,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":58,"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":"National Aeronautics and Space Administration","keywords":"Aerosol; Environmental science; Satellite; Atmospheric sciences; Wavelength; Range (aeronautics); Standard deviation; Troposphere; Meteorology; Remote sensing; Climatology; Geology; Physics; Optics; Materials science","score_opus":0.014244951905901228,"score_gpt":0.19954690231389235,"score_spread":0.18530195040799113,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2115307016","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":[0.9732341,0.000045774384,0.0012045816,0.000016010215,0.000031653555,0.00012415649,0.0000022462018,0.000026385125,0.025315078],"genre_scores_gemma":[0.9823643,0.000020330319,0.016877687,0.000023449868,0.00007182444,0.000027233707,0.0000023410976,0.00001523087,0.00059762556],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99892515,0.000026401036,0.00023227466,0.0003402922,0.00021323685,0.0002626744],"domain_scores_gemma":[0.99932265,0.000041409286,0.00009074297,0.0004188894,0.000009238172,0.00011709143],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00011871154,0.00019827767,0.00020444939,4.805663e-9,0.00014583292,0.0000117716345,0.00025397007,0.00007674634,0.0028991739],"category_scores_gemma":[0.000012581092,0.00014596907,0.00008705189,0.00012911795,0.000507055,0.0000889223,0.0002158611,0.00015404461,0.000017230548],"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":[0.00027676043,0.0012194086,0.32699957,0.00018486557,0.00013220211,0.000015397205,0.004019666,0.00030850712,0.59171706,0.0003722776,0.00014970965,0.074604526],"study_design_scores_gemma":[0.00060713704,0.000103970575,0.33838394,0.000017680408,0.00005402356,0.000014443886,0.0005786636,0.0025530625,0.6564773,0.00062989106,0.00018574945,0.00039415708],"about_ca_topic_score_codex":0.00024569323,"about_ca_topic_score_gemma":0.0000042829065,"teacher_disagreement_score":0.07421037,"about_ca_system_score_codex":0.00006545787,"about_ca_system_score_gemma":0.000012510467,"threshold_uncertainty_score":0.9980123},"labels":[],"label_agreement":null},{"id":"W2116460859","doi":"10.1029/2000gl012051","title":"Can the direct and semi‐direct aerosol effect compete with the indirect effect on a global scale?","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":186,"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","funders":"Deutsches Klimarechenzentrum","keywords":"Aerosol; Environmental science; Atmospheric sciences; Cloud cover; Sea salt aerosol; Cloud albedo; Liquid water path; Liquid water content; Northern Hemisphere; Albedo (alchemy); Climatology; Cloud computing; Meteorology; Physics; Geology","score_opus":0.008549125456379461,"score_gpt":0.25677086725946824,"score_spread":0.24822174180308879,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2116460859","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":[0.9755153,0.000046967703,0.000007687352,0.013809201,0.000033055694,0.0007725568,0.0000067357946,0.00005043966,0.009758051],"genre_scores_gemma":[0.99724746,0.000025960888,0.000017555383,0.0020554403,0.00013531448,0.0001610113,0.0000018977814,0.000022706594,0.0003326561],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9961318,0.0011055467,0.00011043427,0.00061248895,0.001166007,0.0008737659],"domain_scores_gemma":[0.9973975,0.0018223473,0.00004058673,0.00048719606,0.000008699996,0.0002436891],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011229864,0.00028568957,0.00030816838,0.000002755402,0.000866972,0.00017102364,0.0004646175,0.000055984834,0.00006936301],"category_scores_gemma":[0.00009905568,0.00012946624,0.00007723516,0.000713888,0.001994009,0.00007420106,0.00042743943,0.0006086049,0.00016504682],"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":[0.0021669532,0.00026164594,0.75816953,0.00006866673,0.0002836262,0.0003727013,0.0016096721,0.00068110204,0.07170286,0.0001084426,0.037382875,0.1271919],"study_design_scores_gemma":[0.0013011389,0.0038477646,0.9813979,0.000091538655,0.00006469341,0.000050601713,0.000104034894,0.00068576663,0.0047772923,0.00005021769,0.007130213,0.000498786],"about_ca_topic_score_codex":0.0031783122,"about_ca_topic_score_gemma":0.0007702391,"teacher_disagreement_score":0.2232284,"about_ca_system_score_codex":0.000200087,"about_ca_system_score_gemma":0.000012443955,"threshold_uncertainty_score":0.73470086},"labels":[],"label_agreement":null},{"id":"W2116543418","doi":"10.1175/jtech-d-13-00044.1","title":"Scanning ARM Cloud Radars. Part I: Operational Sampling Strategies","year":2013,"lang":"en","type":"article","venue":"Journal of Atmospheric and Oceanic Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":96,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Biological and Environmental Research; U.S. Department of Energy","keywords":"Cloud computing; Computer science; Azimuth; Radar; Remote sensing; Elevation (ballistics); Environmental science; Cloud cover; Real-time computing; Geology; Telecommunications; Engineering; Physics","score_opus":0.007733381010454846,"score_gpt":0.2183647248702553,"score_spread":0.21063134385980045,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2116543418","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":[0.9746903,0.0008296224,0.019721115,0.0024561225,0.00030275554,0.000101248,4.654282e-7,0.00003702596,0.00186131],"genre_scores_gemma":[0.94527483,0.00022516437,0.053611428,0.00029557847,0.000161755,0.00000307154,3.0221983e-7,0.000016009231,0.00041187767],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985745,0.000026333082,0.00055976486,0.0002183735,0.00031572478,0.00030531632],"domain_scores_gemma":[0.99923325,0.000049938826,0.00036718932,0.00017904176,0.000052841828,0.00011775191],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00025709838,0.00017472886,0.00031301455,0.0000016051592,0.0001845017,0.00010697599,0.0003600513,0.00017254324,0.0034300636],"category_scores_gemma":[0.000067785666,0.00013300343,0.000072186886,0.00037758448,0.00036471398,0.0004879833,0.00019795515,0.00035748567,0.00007033088],"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":[0.00009287682,0.00052806886,0.54512256,0.000029719493,0.0002871635,0.000120397046,0.001084369,0.011772094,0.013837979,0.029805077,0.057440534,0.33987916],"study_design_scores_gemma":[0.003768793,0.003720286,0.4885243,0.00020972565,0.00020869306,0.003630494,0.029870432,0.0170789,0.0012174146,0.18829869,0.26172897,0.001743331],"about_ca_topic_score_codex":0.000039359977,"about_ca_topic_score_gemma":0.0000029076064,"teacher_disagreement_score":0.3381358,"about_ca_system_score_codex":0.00008828714,"about_ca_system_score_gemma":0.0000644221,"threshold_uncertainty_score":0.9974809},"labels":[],"label_agreement":null},{"id":"W2116655883","doi":"10.1175/1520-0469(2001)058<2989:iodobc>2.0.co;2","title":"Inferring Optical Depth of Broken Clouds above Green Vegetation Using Surface Solar Radiometric Measurements","year":2001,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"","keywords":"Irradiance; Solar zenith angle; Environmental science; Albedo (alchemy); Radiance; Zenith; Radiative transfer; Optical depth; Remote sensing; Atmospheric radiative transfer codes; Atmospheric sciences; Physics; Meteorology; Geology; Optics; Aerosol","score_opus":0.04828902451980122,"score_gpt":0.27834349994617474,"score_spread":0.23005447542637353,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2116655883","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":[0.9914165,0.000507647,0.0033913474,0.00018684761,0.00051414693,0.000107149295,1.2759021e-7,0.0000065592494,0.0038696432],"genre_scores_gemma":[0.9652427,0.000058754893,0.03437089,0.00011055478,0.00008032649,3.4490424e-7,2.7981908e-8,0.000010334658,0.00012608642],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9971635,0.000122035424,0.0006049758,0.00020701492,0.0015495135,0.00035296293],"domain_scores_gemma":[0.99868846,0.00009465804,0.00080357684,0.00021395038,0.000064530985,0.00013482539],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016558327,0.00016220611,0.00029505213,0.0000021793844,0.00031518747,0.000056791476,0.0010280033,0.00006512788,0.00017092546],"category_scores_gemma":[0.00021024734,0.000102135215,0.00018748235,0.0026657393,0.0006304462,0.0005730668,0.0002320362,0.00018704467,0.000011117057],"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":[0.000018696684,0.0000676997,0.68665695,0.0000053215035,0.000024689556,0.0000041145217,0.0002418453,0.27893785,0.027895372,0.000007831189,0.000041368497,0.006098235],"study_design_scores_gemma":[0.00066800613,0.0004140466,0.8743989,0.00011149907,0.00011692869,0.0002461203,0.0004973709,0.11642619,0.006025094,0.00047952074,0.00034648407,0.0002698397],"about_ca_topic_score_codex":0.00058199343,"about_ca_topic_score_gemma":0.000060693073,"teacher_disagreement_score":0.18774194,"about_ca_system_score_codex":0.00026860653,"about_ca_system_score_gemma":0.00009990834,"threshold_uncertainty_score":0.41649532},"labels":[],"label_agreement":null},{"id":"W2117075756","doi":"10.5194/acp-3-881-2003","title":"Dependence of solar radiative forcing of forest fire aerosol on ageing and state of mixture","year":2003,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":86,"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","keywords":"Plume; Atmospheric sciences; Radiative forcing; Radiative transfer; Environmental science; Forcing (mathematics); Aerosol; Radiative cooling; Panache; Dilution; Meteorology; Physics; Thermodynamics; Optics","score_opus":0.004463502500901008,"score_gpt":0.1925932646990621,"score_spread":0.1881297621981611,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2117075756","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":[0.99371994,0.0001938217,0.0031056376,0.00000460324,0.000010867457,0.000076760734,0.0000067416277,0.0000047393773,0.0028769048],"genre_scores_gemma":[0.99329066,0.00014810517,0.006188889,0.00001702697,0.0000095699515,0.0000031813622,0.0000016681182,0.000010379186,0.00033053997],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99925995,0.000016860711,0.00020089775,0.00020810701,0.0001659437,0.00014826002],"domain_scores_gemma":[0.99948907,0.000072178744,0.00020300213,0.00016446512,0.000011126108,0.00006013059],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000752455,0.00014005575,0.00023389008,1.3152951e-8,0.00005557765,0.0000055748787,0.00008304726,0.00005134839,0.00016953704],"category_scores_gemma":[0.000021669815,0.0001274998,0.000044516877,0.00012151025,0.0002680129,0.00009719517,0.000044732154,0.00010003945,7.6749063e-7],"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":[0.00013507166,0.0003706095,0.35261407,0.0007738562,0.00011908398,0.000013838047,0.004088095,0.042558156,0.32246485,0.00015571006,0.000103987964,0.27660266],"study_design_scores_gemma":[0.0010011032,0.00028264817,0.060202222,0.00021227369,0.00007088149,0.000009134412,0.00072664936,0.028314825,0.90532875,0.0032025704,0.00019149564,0.00045744076],"about_ca_topic_score_codex":0.00014454391,"about_ca_topic_score_gemma":0.0000048899265,"teacher_disagreement_score":0.58286387,"about_ca_system_score_codex":0.000017556888,"about_ca_system_score_gemma":0.000012861447,"threshold_uncertainty_score":0.5199292},"labels":[],"label_agreement":null},{"id":"W2117139757","doi":"10.1002/2015jd023078","title":"Accounting for dust aerosol size distribution in radiative transfer","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":28,"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":"Aerosol; Log-normal distribution; Skewness; Bin; AERONET; Radiative transfer; Particle-size distribution; Computational physics; Gamma distribution; Mathematics; Environmental science; Statistical physics; Physics; Particle size; Statistics; Meteorology; Optics; Chemistry; Algorithm","score_opus":0.03822168210192848,"score_gpt":0.3201948648464951,"score_spread":0.2819731827445666,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2117139757","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":[0.9917818,0.000093065806,0.005885847,0.00067928206,0.00010341256,0.00029871284,0.000008273159,0.0000065591466,0.0011430971],"genre_scores_gemma":[0.9973016,0.00002520602,0.0016691545,0.000051482864,0.00034130528,0.000022219238,0.0000020261098,0.000017914412,0.00056912843],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99738073,0.00019244554,0.0004384832,0.00021942412,0.001158851,0.0006100402],"domain_scores_gemma":[0.99835986,0.00086882344,0.00009508372,0.00014388352,0.00018750977,0.00034482297],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016618057,0.00014148801,0.00031098694,7.7478205e-7,0.00012955896,0.00007259561,0.00040249946,0.00009518037,0.00036449736],"category_scores_gemma":[0.001758524,0.00010898679,0.00015752966,0.00055927236,0.0003300007,0.00046598175,0.0001091379,0.00059102505,0.00008555404],"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":[0.008639956,0.0050695017,0.5600222,0.00014641348,0.00029066027,0.00042365975,0.009761929,0.027019098,0.039533693,0.004152084,0.18260154,0.16233929],"study_design_scores_gemma":[0.010457552,0.0060532955,0.8707971,0.0002525603,0.000060445098,0.000037773127,0.0082290275,0.026608907,0.009090642,0.022476466,0.0450321,0.0009041414],"about_ca_topic_score_codex":0.0007619318,"about_ca_topic_score_gemma":0.00017258599,"teacher_disagreement_score":0.31077492,"about_ca_system_score_codex":0.0005701811,"about_ca_system_score_gemma":0.00015426111,"threshold_uncertainty_score":0.4444352},"labels":[],"label_agreement":null},{"id":"W2117620267","doi":"10.1175/jas3534.1","title":"A Multimoment Bulk Microphysics Parameterization. Part I: Analysis of the Role of the Spectral Shape Parameter","year":2005,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":757,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Bin; Moment (physics); Sorting; Function (biology); Shape parameter; Statistical physics; Physics; Spectral shape analysis; Spectral density; Second moment of area; Constant (computer programming); Statistics; Mathematics; Spectral line; Classical mechanics; Computer science; Algorithm; Thermodynamics; Quantum mechanics","score_opus":0.00783226125184382,"score_gpt":0.2148595362399361,"score_spread":0.20702727498809226,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2117620267","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":[0.99762756,0.00017445623,0.00009571751,0.0011580172,0.00030155745,0.00013399821,0.0000030994174,0.000002532223,0.0005030754],"genre_scores_gemma":[0.9905728,0.00003918936,0.00868032,0.00035545017,0.0000637429,0.0000020523546,5.1759844e-8,0.0000060671073,0.0002803358],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9978386,0.0001464004,0.0005943857,0.00018506675,0.0009839777,0.00025156484],"domain_scores_gemma":[0.9981649,0.00011349141,0.0011937689,0.0004365987,0.000034756988,0.00005651538],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00051078596,0.00014644132,0.00031396298,0.0000010565677,0.00030340426,0.000040244617,0.0017619632,0.00004146139,0.00078294444],"category_scores_gemma":[0.00010018951,0.000061616476,0.0005938455,0.0023837925,0.0012523439,0.00020201376,0.00037310904,0.00015924106,0.000004608076],"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":[0.000016967651,0.00021270747,0.41787452,0.0000024936521,0.0002088378,2.4621838e-7,0.0010063688,0.52827746,0.043666746,0.000057824836,0.0002454093,0.008430437],"study_design_scores_gemma":[0.0002569955,0.00018006549,0.6273255,0.00004829205,0.00068825897,0.000012449714,0.00084295066,0.337114,0.028423512,0.00081141276,0.004107837,0.00018874301],"about_ca_topic_score_codex":0.00014536837,"about_ca_topic_score_gemma":0.000036593352,"teacher_disagreement_score":0.20945099,"about_ca_system_score_codex":0.00010610658,"about_ca_system_score_gemma":0.000063604864,"threshold_uncertainty_score":0.8572692},"labels":[],"label_agreement":null},{"id":"W2118881891","doi":"10.1109/eucap.2006.4584744","title":"Statistics on low-lying liquid and liquid-dominant mixed-phase clouds over Ottawa","year":2006,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Communications Research Centre Canada","funders":"","keywords":"Radiosonde; Liquid water path; Environmental science; Liquid water content; Meteorology; Humidity; Cloud top; Relative humidity; Radiometer; Water vapor; Cloud computing; Cloud base; Atmospheric sciences; Remote sensing; Geology; Geography; Precipitation; Computer science","score_opus":0.005546787868032179,"score_gpt":0.23726497739044,"score_spread":0.23171818952240783,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2118881891","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":[0.9602189,0.000041936124,0.016314438,0.00011055501,0.00015434863,0.00015779903,0.00002363477,0.000041880947,0.022936517],"genre_scores_gemma":[0.98849976,0.000025099625,0.005450581,0.0005686287,0.00009333961,0.000011411162,0.000010615856,0.000025361127,0.0053151892],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.998619,0.000032171567,0.00027898376,0.00037912076,0.00031192272,0.00037875932],"domain_scores_gemma":[0.9994618,0.00007320368,0.0000816737,0.00024334743,0.0000055242945,0.00013439546],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001610768,0.00020774276,0.00018274054,0.0000015155257,0.00018922413,0.00003639328,0.00013570307,0.000081367674,0.00421683],"category_scores_gemma":[0.000020024876,0.00016602267,0.000037629063,0.00011506103,0.00021831416,0.000100057136,0.00015106943,0.00011398056,0.00034649117],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.003756337,0.004739472,0.045346454,0.00013901893,0.00009122483,0.0007375544,0.0012230406,0.008247738,0.3131445,0.067750126,0.506327,0.048497543],"study_design_scores_gemma":[0.018425206,0.019923452,0.2524569,0.00024537664,0.00026970732,0.00013189633,0.0013432815,0.050351758,0.25834557,0.004554631,0.3886885,0.0052637015],"about_ca_topic_score_codex":0.0012964252,"about_ca_topic_score_gemma":0.00033878142,"teacher_disagreement_score":0.20711045,"about_ca_system_score_codex":0.00009937944,"about_ca_system_score_gemma":0.000009443071,"threshold_uncertainty_score":0.99669343},"labels":[],"label_agreement":null},{"id":"W2118943646","doi":"10.1029/2012gl053329","title":"Two distinct modes in one‐day rainfall event during MC3E field campaign: Analyses of disdrometer observations and WRF‐SBM simulation","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Aeronautics and Space Administration; U.S. Department of Energy","keywords":"Weather Research and Forecasting Model; Disdrometer; Environmental science; Middle latitudes; Bin; Graupel; Meteorology; Atmospheric sciences; RADIUS; Cloud physics; Convection; Climatology; Precipitation; Physics; Geology; Cloud computing; Mathematics","score_opus":0.1022679966278329,"score_gpt":0.3739133143025829,"score_spread":0.27164531767475,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2118943646","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":[0.99641323,0.000018578052,0.0022715058,0.000809359,0.000015316687,0.00017671425,0.0000041733165,0.000008914929,0.00028219822],"genre_scores_gemma":[0.99905133,0.0000047487865,0.00058075757,0.00015048581,0.000077991885,0.000027160315,0.000004292439,0.000009595328,0.0000936111],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99824506,0.00017473151,0.00020453338,0.00022314242,0.00068458903,0.0004679527],"domain_scores_gemma":[0.99899966,0.00059511454,0.000043880307,0.00020717115,0.000015138779,0.00013906634],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047583095,0.000100927726,0.00016426896,0.000008779248,0.00012380235,0.000022109307,0.0001487639,0.00003322492,0.00022639561],"category_scores_gemma":[0.00028831433,0.0000867249,0.000055522218,0.000428253,0.0002279774,0.00030790575,0.00027033978,0.00022579913,0.000021722275],"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":[0.00004710686,0.00028031206,0.55315363,0.000029665545,0.00002137372,0.000003475494,0.0010841567,0.026037334,0.41738576,0.00012274153,0.00012276258,0.0017116527],"study_design_scores_gemma":[0.00024730212,0.000046360678,0.9787184,0.000022986509,0.000007400458,1.6186931e-7,0.000105207066,0.01622848,0.0042279847,0.00024690988,0.00004200658,0.000106825784],"about_ca_topic_score_codex":0.0028000853,"about_ca_topic_score_gemma":0.00011262169,"teacher_disagreement_score":0.4255647,"about_ca_system_score_codex":0.00013050059,"about_ca_system_score_gemma":0.0000070702,"threshold_uncertainty_score":0.423291},"labels":[],"label_agreement":null},{"id":"W2119693517","doi":"10.1002/qj.2175","title":"Mixed‐phase clouds in a turbulent environment. Part 2: Analytic treatment","year":2013,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"Met Office","keywords":"Supercooling; Supersaturation; Turbulence; Clear ice; Liquid water content; Cloud physics; Mechanics; Forcing (mathematics); Phase (matter); Ice crystals; Thermodynamics; Environmental science; Physics; Statistical physics; Meteorology; Atmospheric sciences; Cloud computing; Sea ice; Arctic ice pack; Computer science","score_opus":0.01551042399252352,"score_gpt":0.2208000061119182,"score_spread":0.20528958211939466,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2119693517","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":[0.99642926,0.00016034521,0.0005142544,0.002095588,0.00018290922,0.00026688978,0.00000185389,0.000009015346,0.00033988385],"genre_scores_gemma":[0.996162,0.00004639776,0.002252644,0.00054765114,0.00012090638,0.000024363231,5.3561206e-7,0.000011589985,0.0008339313],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9978964,0.00025686587,0.00063486793,0.0002680757,0.0004880617,0.00045577038],"domain_scores_gemma":[0.99897736,0.00010208456,0.00038787897,0.00030312125,0.000008981603,0.00022058553],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00048119298,0.00025276394,0.0004116512,0.0000015588641,0.000144806,0.00004418161,0.00051737914,0.00016004182,0.00785527],"category_scores_gemma":[0.000015686235,0.00012898023,0.000704619,0.00015232881,0.00032905047,0.00012118888,0.000076825585,0.0003429123,0.00027318968],"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":[0.0005099212,0.010715628,0.3852815,0.000021639422,0.0009757827,0.00022787417,0.008651643,0.06535819,0.008023865,0.0002014298,0.07912029,0.44091225],"study_design_scores_gemma":[0.011470597,0.024392955,0.84031624,0.000068509136,0.0005358395,0.00018916623,0.0046337075,0.062080085,0.0007121068,0.009710476,0.04467947,0.0012108238],"about_ca_topic_score_codex":0.0002509644,"about_ca_topic_score_gemma":0.000009642946,"teacher_disagreement_score":0.45503476,"about_ca_system_score_codex":0.00052744284,"about_ca_system_score_gemma":0.0000135172995,"threshold_uncertainty_score":0.9930517},"labels":[],"label_agreement":null},{"id":"W2120358141","doi":"10.5194/acp-9-4653-2009","title":"Aerosol size-dependent below-cloud scavenging by rain and snow in the ECHAM5-HAM","year":2009,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":174,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Killam Trusts; Eidgenössische Technische Hochschule Zürich","keywords":"Scavenging; Aerosol; Atmospheric sciences; Snow; Troposphere; Environmental science; Cloud cover; Liquid water content; Cloud condensation nuclei; Ice nucleus; Sea salt aerosol; Effective radius; Deposition (geology); Cloud albedo; Climatology; Meteorology; Sea salt; Cloud computing; Nucleation; Chemistry; Geology; Geography; Physics","score_opus":0.0034182127714243666,"score_gpt":0.192512127701633,"score_spread":0.18909391493020863,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2120358141","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":[0.9884849,0.00030207838,0.0009780184,0.00048452005,0.000024765668,0.00014098526,0.0000039534075,0.000029122868,0.009551631],"genre_scores_gemma":[0.99446565,0.00018984184,0.0019648334,0.00082767534,0.00012011972,0.000012431537,0.0000052606033,0.000013171813,0.0024010302],"study_design_codex":"design_other","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.998831,0.000028873477,0.00018097559,0.0003826125,0.00024496284,0.00033160357],"domain_scores_gemma":[0.99947387,0.00010434613,0.00006456093,0.0002570843,0.000003634264,0.00009650714],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018036085,0.00022873568,0.00018777953,9.595446e-9,0.00019410891,0.00006409698,0.0002163568,0.00009135875,0.00061971456],"category_scores_gemma":[0.000018323592,0.00018243634,0.00004126408,0.00020002766,0.00016744729,0.00011601653,0.00007488023,0.00023938906,0.000015622709],"study_design_candidate":"design_other","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":[0.00007691107,0.00071911776,0.037033163,0.000069255955,0.00003751639,0.00005986932,0.0055701234,0.002079269,0.17468654,0.00012368806,0.011192543,0.76835203],"study_design_scores_gemma":[0.02053712,0.0018783165,0.28991395,0.00088588917,0.0006198879,0.00083608023,0.022860061,0.21824476,0.29519698,0.054073486,0.082719624,0.012233852],"about_ca_topic_score_codex":0.00011031002,"about_ca_topic_score_gemma":0.0000041078256,"teacher_disagreement_score":0.7561182,"about_ca_system_score_codex":0.00005271262,"about_ca_system_score_gemma":0.000007772634,"threshold_uncertainty_score":0.7439538},"labels":[],"label_agreement":null},{"id":"W2120899140","doi":"10.1175/1520-0442(2002)015<2321:hchias>2.0.co;2","title":"High-Cloud Horizontal Inhomogeneity and Solar Albedo Bias","year":2002,"lang":"en","type":"article","venue":"Journal of Climate","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":75,"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","funders":"Pacific Northwest National Laboratory; University of Utah; Battelle; National Aeronautics and Space Administration; U.S. Department of Energy; National Science Foundation","keywords":"Cloud albedo; Albedo (alchemy); Solar zenith angle; Environmental science; Radiative transfer; Standard deviation; Zenith; Lidar; Remote sensing; Atmospheric sciences; Cloud cover; Atmospheric radiative transfer codes; Geology; Cloud computing; Physics; Optics","score_opus":0.014485574928135703,"score_gpt":0.21223291551270823,"score_spread":0.19774734058457252,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2120899140","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":[0.9944178,0.00030290027,0.00016718092,0.00041738639,0.00037231884,0.000038997754,0.000003201902,0.000007841205,0.0042723613],"genre_scores_gemma":[0.9947801,0.0018022706,0.0027186724,0.00019909225,0.0002900819,5.1890925e-7,2.3377711e-7,0.000011892024,0.00019708823],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99896663,0.000039226303,0.0003334001,0.00011827024,0.00029718757,0.00024526616],"domain_scores_gemma":[0.9994052,0.000030480505,0.00028181568,0.00010812558,0.000009659245,0.00016470987],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003089322,0.00011468359,0.00021267435,0.000001911012,0.00012216298,0.000039963823,0.00014806274,0.00005856155,0.0027636734],"category_scores_gemma":[0.000029284118,0.00008639235,0.000079542944,0.000092626906,0.00012032972,0.00023359638,0.00012858218,0.00017234335,0.00018768445],"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":[0.00013069002,0.0004797129,0.84710896,0.000030471296,0.00008906579,0.0004141593,0.0012327558,0.0005663817,0.01600168,0.0003108,0.02403172,0.10960359],"study_design_scores_gemma":[0.004381784,0.002947753,0.85060185,0.0001262913,0.00025446157,0.0022536756,0.0008520626,0.003563526,0.008450067,0.0019544377,0.12347248,0.0011416201],"about_ca_topic_score_codex":0.00004670973,"about_ca_topic_score_gemma":0.000026685064,"teacher_disagreement_score":0.10846197,"about_ca_system_score_codex":0.000059792015,"about_ca_system_score_gemma":0.000002951914,"threshold_uncertainty_score":0.99814796},"labels":[],"label_agreement":null},{"id":"W2121539051","doi":"10.5194/acp-16-5009-2016","title":"Aerosol optical properties in the southeastern United States in summer – Part 2: Sensitivity of aerosol optical depth to relative humidity and aerosol parameters","year":2016,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":61,"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":"Georgia Institute of Technology; National Aeronautics and Space Administration; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Aerosol; Relative humidity; Atmospheric sciences; Environmental science; Range (aeronautics); Humidity; Mass concentration (chemistry); Boundary layer; Meteorology; Chemistry; Materials science; Geology; Thermodynamics; Physics","score_opus":0.018987638239497343,"score_gpt":0.2216636563461495,"score_spread":0.20267601810665217,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2121539051","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":[0.99616414,0.000031868294,0.002258513,0.00045878696,0.000016797036,0.00027162355,0.00001628276,0.000014169592,0.00076782325],"genre_scores_gemma":[0.9967228,0.000062990475,0.0026719747,0.00018623893,0.00003214447,0.000027756005,0.000007889765,0.000017399245,0.0002707735],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9983843,0.00012097782,0.00031266204,0.0005169247,0.00028304837,0.00038206796],"domain_scores_gemma":[0.9989809,0.00035569962,0.00008223246,0.0004265714,0.0000145438,0.00014007279],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000384298,0.00026119562,0.00031733201,8.728011e-8,0.00007874858,0.00003086386,0.00019952598,0.000113064525,0.00007329606],"category_scores_gemma":[0.000092214665,0.00016016609,0.00003864721,0.00030149342,0.0007964932,0.00021107752,0.0002984818,0.0002146045,0.0000133395915],"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":[0.0006581308,0.0013124478,0.6030834,0.00021116971,0.0001008401,0.00007621043,0.010681461,0.006079725,0.24949011,0.00008079213,0.00025193059,0.12797381],"study_design_scores_gemma":[0.007179016,0.0010476302,0.20235515,0.0014652039,0.00032037808,0.000116811876,0.015134493,0.11751532,0.64880395,0.0016367871,0.0007116173,0.003713628],"about_ca_topic_score_codex":0.00051495567,"about_ca_topic_score_gemma":0.0001975301,"teacher_disagreement_score":0.40072823,"about_ca_system_score_codex":0.00004320265,"about_ca_system_score_gemma":0.000016298858,"threshold_uncertainty_score":0.6531384},"labels":[],"label_agreement":null},{"id":"W2122286658","doi":"10.1256/qj.03.99","title":"Stochastic generation of subgrid‐scale cloudy columns for large‐scale models","year":2004,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":180,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Hydrographic Service; Dalhousie University","funders":"Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Radiative transfer; Cloud fraction; Cloud computing; Liquid water content; Meteorology; Column (typography); Scale (ratio); Cloud top; Environmental science; Generator (circuit theory); Monte Carlo method; Statistical physics; Remote sensing; Physics; Mathematics; Cloud cover; Geometry; Computer science; Statistics; Geology; Optics; Power (physics); Thermodynamics","score_opus":0.017799689551752543,"score_gpt":0.227520896967967,"score_spread":0.20972120741621447,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2122286658","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":[0.7168107,0.000056460423,0.28214327,0.00045382595,0.00022829227,0.0002060385,0.00001262069,0.000006924501,0.00008187533],"genre_scores_gemma":[0.97797817,0.0000034849706,0.021299267,0.0003417405,0.00020704676,0.00001171955,0.0000010912387,0.000011715444,0.00014574757],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99840206,0.00008885798,0.0005308013,0.00019506381,0.0004502519,0.0003329633],"domain_scores_gemma":[0.9990809,0.00007363405,0.0004714621,0.00019789077,0.000049672715,0.000126463],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000728823,0.00015854534,0.0003400229,9.4966293e-7,0.0002581447,0.00002386046,0.0004647412,0.00016901983,0.00023805174],"category_scores_gemma":[0.000022177552,0.00009524153,0.00066681375,0.00012890034,0.00021174617,0.00011964094,0.00006455421,0.00025764745,0.000006011207],"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":[0.00022149266,0.0010159467,0.003277302,0.000016539117,0.00013541049,0.0000017579479,0.0069657224,0.95881635,0.021065362,0.0006037486,0.0045268526,0.003353507],"study_design_scores_gemma":[0.011802076,0.019549806,0.050044075,0.00009744307,0.00089445716,0.00008711981,0.009469827,0.78519976,0.005396029,0.115228124,0.0010362201,0.0011950842],"about_ca_topic_score_codex":0.000045158267,"about_ca_topic_score_gemma":0.00004841095,"teacher_disagreement_score":0.26116747,"about_ca_system_score_codex":0.00016477377,"about_ca_system_score_gemma":0.000026811314,"threshold_uncertainty_score":0.3883837},"labels":[],"label_agreement":null},{"id":"W2122518875","doi":"10.1175/2010jamc2467.1","title":"Clouds at Arctic Atmospheric Observatories. Part I: Occurrence and Macrophysical Properties","year":2010,"lang":"en","type":"article","venue":"Journal of Applied Meteorology and Climatology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":349,"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":"U.S. Department of Energy; Office of Science; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Ceilometer; Noon; Environmental science; Arctic; Climatology; Diurnal cycle; Cloud cover; Atmospheric sciences; Cloud fraction; Annual cycle; Meteorology; Cloud computing; Aerosol; Geography; Geology; Oceanography","score_opus":0.008992008246536154,"score_gpt":0.20497604052930038,"score_spread":0.19598403228276423,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2122518875","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":[0.99738336,0.00027217332,0.000042577132,0.00065112545,0.0005080416,0.0000916855,0.0000018176642,0.000011010699,0.0010382014],"genre_scores_gemma":[0.9953808,0.00028561548,0.0034962897,0.0006638039,0.000088611814,0.000010311486,8.1800977e-7,0.000010011176,0.000063731546],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987626,0.000045676574,0.00041171303,0.00027155137,0.00015089242,0.00035757464],"domain_scores_gemma":[0.999192,0.00011006855,0.00031894533,0.00016607328,0.0000205651,0.00019235075],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028422443,0.00019166655,0.00046988967,9.699955e-7,0.00021386797,0.000014565225,0.00019361051,0.00023159965,0.00077731133],"category_scores_gemma":[0.000046504563,0.00013924002,0.000054064145,0.000105852545,0.0014576124,0.00009285155,0.00029631692,0.00054279773,0.000041614523],"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":[0.0014603983,0.0002452588,0.8513627,0.00006659753,0.00012411314,0.000109448905,0.0011481333,0.000042982676,0.117093556,0.012056958,0.0023361277,0.013953713],"study_design_scores_gemma":[0.0073009254,0.0036818741,0.66483843,0.000047929072,0.00088398973,0.010919959,0.0018127171,0.0012864708,0.013665059,0.040989853,0.25264612,0.0019267005],"about_ca_topic_score_codex":0.000011227576,"about_ca_topic_score_gemma":0.00004873413,"teacher_disagreement_score":0.25030997,"about_ca_system_score_codex":0.000024939058,"about_ca_system_score_gemma":0.000020390306,"threshold_uncertainty_score":0.8511014},"labels":[],"label_agreement":null},{"id":"W2123658823","doi":"10.5194/amt-6-1817-2013","title":"Radar-radiometer retrievals of cloud number concentration and dispersion parameter in nondrizzling marine stratocumulus","year":2013,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"McGill University","funders":"Biological and Environmental Research; U.S. Department of Energy","keywords":"Drizzle; Environmental science; Radiometer; Marine stratocumulus; Remote sensing; Effective radius; Zenith; Meteorology; Liquid water path; Radar; Atmospheric sciences; Physics; Aerosol; Geology; Computer science; Precipitation","score_opus":0.013157858390839456,"score_gpt":0.22389805464101778,"score_spread":0.2107401962501783,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2123658823","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":[0.98415273,0.000082835875,0.00801782,0.00012272644,0.00007076187,0.000886969,7.071864e-7,0.00008372001,0.0065817307],"genre_scores_gemma":[0.9078434,0.00014785901,0.0916262,0.00013994351,0.000025710882,0.00007720615,0.0000023303364,0.000021272617,0.00011608119],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979875,0.00009460355,0.0005089161,0.00039392346,0.0006794447,0.00033558594],"domain_scores_gemma":[0.99931806,0.000040489165,0.00019653983,0.00029361824,0.000042568485,0.000108699074],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005739188,0.00022972588,0.00031221728,4.5074148e-7,0.000059743023,0.000042384025,0.00017808501,0.00012721895,0.003639449],"category_scores_gemma":[0.000072857656,0.00019695575,0.00006078544,0.00038893518,0.000201274,0.0003470868,0.00016181986,0.00015046838,0.000040782288],"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":[0.000037875576,0.00015853129,0.7832059,0.00003201953,0.000020653952,0.0000040124364,0.00023879284,0.0000142566905,0.120416455,0.00008141471,0.0014694161,0.09432065],"study_design_scores_gemma":[0.001549666,0.0007824965,0.784288,0.00026566195,0.00008289644,0.000025263633,0.00040366212,0.008121188,0.19435073,0.004528484,0.0044191736,0.0011827821],"about_ca_topic_score_codex":0.0021425558,"about_ca_topic_score_gemma":0.00006412244,"teacher_disagreement_score":0.09313787,"about_ca_system_score_codex":0.00026688905,"about_ca_system_score_gemma":0.00001618197,"threshold_uncertainty_score":0.99727136},"labels":[],"label_agreement":null},{"id":"W2124075705","doi":"10.1175/2009jtecha1191.1","title":"The Effects of Precipitation on Cloud Droplet Measurement Devices","year":2009,"lang":"en","type":"article","venue":"Journal of Atmospheric and Oceanic Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":21,"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 Science Foundation","keywords":"Precipitation; Liquid water content; Environmental science; Spectrometer; Cloud computing; Atmospheric sciences; Volume (thermodynamics); Meteorology; Liquid water; Climatology; Geology; Physics; Computer science; Optics; Thermodynamics","score_opus":0.0035943964769840713,"score_gpt":0.1970399313035632,"score_spread":0.19344553482657914,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2124075705","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":[0.9936093,0.0021326828,0.0017505381,0.0015049523,0.00025165913,0.00011894889,1.0240086e-7,0.000016192042,0.0006156332],"genre_scores_gemma":[0.9959872,0.0006720922,0.0030292454,0.00019617607,0.00004228104,0.0000010506554,3.1959488e-8,0.0000062537783,0.00006566247],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99893105,0.000036923513,0.00035329378,0.000119523975,0.0003769374,0.00018224388],"domain_scores_gemma":[0.9992055,0.00008991325,0.0004563776,0.00015920984,0.000038994298,0.000049969036],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034718576,0.00011646116,0.00021018856,8.6241107e-7,0.00012702255,0.0000119066235,0.00026839494,0.00010159328,0.00003065964],"category_scores_gemma":[0.00018072236,0.00007022652,0.000059607115,0.00027208915,0.00020710872,0.0000697116,0.000044661683,0.00019552781,0.000005699746],"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":[0.0003095097,0.00044461706,0.055646412,0.000040146257,0.0001325797,0.000041199546,0.0005518538,0.00032201933,0.025579732,0.006706264,0.008922283,0.9013034],"study_design_scores_gemma":[0.0023883462,0.013131405,0.9071806,0.0002958542,0.00020167987,0.00021016247,0.0015899461,0.00084034237,0.012826854,0.023557048,0.03734818,0.00042958872],"about_ca_topic_score_codex":0.0000039738225,"about_ca_topic_score_gemma":0.0000044346853,"teacher_disagreement_score":0.9008738,"about_ca_system_score_codex":0.00009291087,"about_ca_system_score_gemma":0.000018538185,"threshold_uncertainty_score":0.28637543},"labels":[],"label_agreement":null},{"id":"W2125651991","doi":"10.1002/2014jd021885","title":"Supersaturation and diffusional droplet growth in liquid clouds: Polydisperse spectra","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":28,"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":"Supersaturation; Aerosol; RADIUS; Effective radius; Dispersity; Diffusion; Log-normal distribution; Adiabatic process; Materials science; Physics; Mechanics; Thermodynamics; Meteorology; Mathematics; Astrophysics; Statistics","score_opus":0.012800949405244814,"score_gpt":0.2710796680807232,"score_spread":0.2582787186754784,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2125651991","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":[0.9946137,0.00009314172,0.00045220225,0.0014082802,0.00007157193,0.00010304823,8.850836e-7,0.000006069472,0.0032511135],"genre_scores_gemma":[0.9966068,0.00015228726,0.0023970578,0.000116342846,0.0003757312,0.0000031160944,6.6713983e-7,0.000016221513,0.00033173122],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9974327,0.00030318162,0.0003656912,0.00024958304,0.0011627686,0.00048605126],"domain_scores_gemma":[0.9989791,0.00039337864,0.00010428713,0.00014473945,0.00006397487,0.00031451046],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000957118,0.00014753426,0.00027737694,0.0000029138284,0.00015611162,0.00006926081,0.00031873834,0.0000844972,0.0012255593],"category_scores_gemma":[0.0005323765,0.000108744214,0.00009569866,0.0004202597,0.00051258196,0.00033780804,0.00024599658,0.0006978529,0.00010975781],"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":[0.005468247,0.0033162218,0.48325074,0.00010426243,0.00012483755,0.0004425941,0.0053518126,0.0006991575,0.36676696,0.03542075,0.017134871,0.08191957],"study_design_scores_gemma":[0.0017815628,0.0037390392,0.96075267,0.0001011395,0.000015053826,0.00006184539,0.0012505654,0.009061547,0.0027345784,0.015637094,0.0045152428,0.0003496449],"about_ca_topic_score_codex":0.0014600591,"about_ca_topic_score_gemma":0.00026268413,"teacher_disagreement_score":0.47750196,"about_ca_system_score_codex":0.00017771221,"about_ca_system_score_gemma":0.000045188597,"threshold_uncertainty_score":0.99968743},"labels":[],"label_agreement":null},{"id":"W2125780026","doi":"10.1029/2004jd004518","title":"Smoke over haze: Comparative analysis of satellite, surface radiometer, and airborne in situ measurements of aerosol optical properties and radiative forcing over the eastern United States","year":2005,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":14,"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":"AERONET; Environmental science; Moderate-resolution imaging spectroradiometer; Radiometer; Aerosol; Radiative forcing; Optical depth; Remote sensing; Advanced very-high-resolution radiometer; Satellite; Forcing (mathematics); Radiative transfer; Albedo (alchemy); Atmospheric radiative transfer codes; Atmospheric sciences; Meteorology; Physics; Geology; Optics","score_opus":0.07920042110148777,"score_gpt":0.32608897438011347,"score_spread":0.2468885532786257,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2125780026","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":[0.9978478,0.0013174227,0.00006602332,0.00024019042,0.000011014316,0.00021052394,0.000004060797,0.0000021483272,0.0003008203],"genre_scores_gemma":[0.99836916,0.00043100925,0.0010059617,0.000031851556,0.000026696702,0.0000027130561,0.0000010724463,0.00000934136,0.00012222496],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9970833,0.00041724267,0.0005956317,0.0002267666,0.0012917173,0.0003853646],"domain_scores_gemma":[0.99865633,0.0005183921,0.00030512083,0.00018186793,0.00015058751,0.00018768215],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011002814,0.0001757236,0.00062024815,0.0000111773825,0.00009990657,0.000053805226,0.00026700486,0.000058706664,0.00011872426],"category_scores_gemma":[0.00015719938,0.000105741994,0.00012299069,0.0014854054,0.0012247799,0.0003446577,0.00024822308,0.00042243663,0.0000021630444],"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":[0.0012968774,0.0007078371,0.86457294,0.000045417764,0.0010754671,0.000010383758,0.008415342,0.0527046,0.061462566,0.000043718264,0.0001398391,0.009525008],"study_design_scores_gemma":[0.000930887,0.0007443304,0.9185692,0.00008626031,0.00013930122,0.0000015920529,0.0019082476,0.06345975,0.013879173,0.00006967432,0.00008767893,0.00012388929],"about_ca_topic_score_codex":0.0032038805,"about_ca_topic_score_gemma":0.0010510709,"teacher_disagreement_score":0.053996276,"about_ca_system_score_codex":0.00015128624,"about_ca_system_score_gemma":0.000039567767,"threshold_uncertainty_score":0.48433304},"labels":[],"label_agreement":null},{"id":"W2125855972","doi":"10.5194/acp-6-1815-2006","title":"An AeroCom initial assessment – optical properties in aerosol component modules of global models","year":2006,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":850,"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","funders":"","keywords":"Aerosol; AERONET; Context (archaeology); Environmental science; Radiative transfer; Atmospheric sciences; Radiative forcing; Satellite; Forcing (mathematics); Absorption (acoustics); Meteorology; Physics; Geography; Optics","score_opus":0.009382062728749398,"score_gpt":0.23235918134174177,"score_spread":0.22297711861299238,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2125855972","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":[0.97614974,0.00005951808,0.008631849,0.000021319556,0.000015621583,0.00011701574,0.00000704507,0.000023825629,0.014974069],"genre_scores_gemma":[0.9769532,0.000010902581,0.022769613,0.000024631849,0.00007313093,0.000021079231,0.000010790327,0.000011289945,0.00012533554],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.998881,0.000020533047,0.00026828647,0.0003201428,0.00026023693,0.00024979125],"domain_scores_gemma":[0.9995968,0.000010612828,0.000073365605,0.00022564974,0.000009442519,0.0000841722],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000057546975,0.00019415776,0.00024083804,7.884575e-9,0.000066361645,0.000025500822,0.00015925511,0.00008435326,0.00025805467],"category_scores_gemma":[0.0000010289599,0.00017471351,0.000046652192,0.0001380823,0.000331392,0.00020928109,0.000099374025,0.000112341535,0.0000036012482],"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":[0.00012690994,0.0026787915,0.21587794,0.00014769942,0.000029437937,0.000021780173,0.00023280703,0.4640259,0.23333226,0.0017022039,0.00014578781,0.081678465],"study_design_scores_gemma":[0.0012152367,0.00014499715,0.2062451,0.000057581543,0.00003571483,0.000013698767,0.00029230193,0.73896414,0.04271498,0.00961767,0.0000695987,0.0006289549],"about_ca_topic_score_codex":0.0011629359,"about_ca_topic_score_gemma":0.00003044109,"teacher_disagreement_score":0.27493826,"about_ca_system_score_codex":0.00013372905,"about_ca_system_score_gemma":0.000020865074,"threshold_uncertainty_score":0.712461},"labels":[],"label_agreement":null},{"id":"W2125940639","doi":"10.5194/acp-9-733-2009","title":"Intercomparison of Aerosol Optical Depth from Brewer Ozone spectrophotometers and CIMEL sunphotometers measurements","year":2009,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"GDG Environnement","funders":"Ministry of Environment","keywords":"AERONET; Aerosol; Environmental science; Ozone; Remote sensing; Correlation coefficient; Atmospheric sciences; Meteorology; Physics; Geology; Mathematics","score_opus":0.012222347276868077,"score_gpt":0.22387033304890158,"score_spread":0.2116479857720335,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2125940639","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":[0.9867419,0.00016652817,0.003159902,0.000035979825,0.00003047439,0.000104689185,0.00000405736,0.000025469326,0.009730979],"genre_scores_gemma":[0.9716295,0.00006875961,0.027776612,0.00015103995,0.000054985358,0.000004683879,0.000008396667,0.000013860744,0.00029218916],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99873745,0.000014499267,0.00025231013,0.0004178298,0.0003029884,0.00027493294],"domain_scores_gemma":[0.9994123,0.00003426967,0.00010618536,0.00026150543,0.00001018776,0.00017554387],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000066560555,0.00024194777,0.0003259035,3.0562408e-8,0.00007125122,0.00003168855,0.00016679685,0.00008893546,0.0009774758],"category_scores_gemma":[0.000009325475,0.00022677795,0.00006910952,0.00018680078,0.00028535648,0.00012292556,0.000091930924,0.0001546812,0.000013969205],"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":[0.000110823516,0.0002856104,0.079224735,0.000022319582,0.00006691172,0.0000055520545,0.0004246058,0.00015990033,0.7651527,0.0000031823902,0.00037129922,0.15417236],"study_design_scores_gemma":[0.0021370389,0.00044995066,0.23299234,0.0000891571,0.00020476249,0.000017790717,0.00040913894,0.011788151,0.7494846,0.0009552661,0.0004717024,0.0010001127],"about_ca_topic_score_codex":0.0002611961,"about_ca_topic_score_gemma":0.0000044646085,"teacher_disagreement_score":0.1537676,"about_ca_system_score_codex":0.00006836477,"about_ca_system_score_gemma":0.00000824728,"threshold_uncertainty_score":0.99993575},"labels":[],"label_agreement":null},{"id":"W2126189145","doi":"10.1029/2009jd012884","title":"Detection of supercooled liquid in mixed‐phase clouds using radar Doppler spectra","year":2010,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":132,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Office of Science; U.S. Department of Energy","keywords":"Lidar; Remote sensing; Ice crystals; Radar; Ceilometer; Radiosonde; Environmental science; Doppler radar; Ice nucleus; Liquid water content; Materials science; Meteorology; Geology; Cloud computing; Physics; Computer science","score_opus":0.025509449347548955,"score_gpt":0.3229051734534185,"score_spread":0.29739572410586956,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2126189145","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":[0.9976623,0.000063738735,0.0010690293,0.000121930716,0.00025202872,0.00016579538,0.000002107652,0.000006387352,0.00065669],"genre_scores_gemma":[0.9930786,0.00004101939,0.0063258996,0.00001587197,0.00038289063,0.000002754455,3.1861072e-7,0.000025308998,0.0001273726],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.996862,0.00025421305,0.0006469135,0.00025406378,0.0013827292,0.00060005893],"domain_scores_gemma":[0.9987413,0.0002941245,0.00022481172,0.00030315947,0.00012045738,0.0003161018],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013722546,0.00017447743,0.00041311927,0.000004666682,0.00013793164,0.000038998412,0.00052245334,0.00014369722,0.0019889264],"category_scores_gemma":[0.00043289489,0.00013820324,0.00020310981,0.00084369467,0.0006427851,0.00038127194,0.00022967203,0.001439384,0.000062730964],"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":[0.0009847115,0.0008036896,0.0049221627,0.000012542192,0.000021362317,0.00007760612,0.0002091525,0.00033611598,0.98223764,0.000103407074,0.0001958324,0.010095802],"study_design_scores_gemma":[0.0068166326,0.01015825,0.2743113,0.00018477408,0.00006621452,0.0002596267,0.0019826684,0.019812554,0.6739795,0.0062044817,0.0054864883,0.00073746685],"about_ca_topic_score_codex":0.0029864912,"about_ca_topic_score_gemma":0.0012548468,"teacher_disagreement_score":0.3082581,"about_ca_system_score_codex":0.0002130563,"about_ca_system_score_gemma":0.00012568892,"threshold_uncertainty_score":0.99892336},"labels":[],"label_agreement":null},{"id":"W2126591422","doi":"10.5194/acp-10-9851-2010","title":"Constraints on interactions between aerosols and clouds on a global scale from a combination of MODIS-CERES satellite data and climate simulations","year":2010,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":18,"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 Victoria; Environment and Climate Change Canada","funders":"Canadian Foundation for Climate and Atmospheric Sciences; Langley Research Center; National Aeronautics and Space Administration","keywords":"Aerosol; Effective radius; Cloud computing; Liquid water path; Environmental science; Atmospheric sciences; Cloud albedo; Liquid water content; Satellite; Meteorology; Cloud cover; Physics; Computer science","score_opus":0.01289818748358938,"score_gpt":0.2598763719792889,"score_spread":0.24697818449569955,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2126591422","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":[0.99368805,0.000018820247,0.00045677862,0.00006799182,0.000035161676,0.00009912329,0.00054707093,0.000017819548,0.0050692144],"genre_scores_gemma":[0.9955586,0.00006048433,0.004032125,0.000048507067,0.00006961839,0.0000029477108,0.00016637951,0.000008646915,0.000052665946],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99915296,0.000013847689,0.00017530349,0.00036987904,0.00014055519,0.00014747906],"domain_scores_gemma":[0.9992971,0.00013975885,0.00010484369,0.00034441892,0.000008859749,0.00010505537],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000050904335,0.00015667912,0.00017774523,2.2468333e-8,0.00015016919,0.000039929822,0.00013298102,0.00007561277,0.0005511938],"category_scores_gemma":[0.0000145894455,0.0001493144,0.000019816138,0.00009680912,0.0005067003,0.00014905592,0.0001880701,0.00016968948,0.000007398048],"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":[0.00005234335,0.00024147796,0.6041192,0.00003168143,0.000041566545,9.931425e-7,0.00029895516,0.0003680049,0.025394088,0.00019715476,0.000066395754,0.36918813],"study_design_scores_gemma":[0.001461127,0.00014230699,0.8943237,0.000095073985,0.00014545346,0.0000063951265,0.00034653777,0.0888684,0.007494737,0.005308859,0.0012822086,0.0005251939],"about_ca_topic_score_codex":0.00016660834,"about_ca_topic_score_gemma":0.0000375129,"teacher_disagreement_score":0.36866295,"about_ca_system_score_codex":0.00002042438,"about_ca_system_score_gemma":0.0000074415243,"threshold_uncertainty_score":0.6088864},"labels":[],"label_agreement":null},{"id":"W2126863703","doi":"10.5194/amt-7-1527-2014","title":"G band atmospheric radars: new frontiers in cloud physics","year":2014,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":61,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Cirrus; Remote sensing; Environmental science; Radar; Wavelength; Radiative transfer; Doppler effect; Snow; Meteorology; Physics; Geology; Optics; Computer science","score_opus":0.012053939843277005,"score_gpt":0.20258340223909535,"score_spread":0.19052946239581833,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2126863703","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"methods","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.07883078,0.00047805233,0.8701002,0.00036328784,0.0006919318,0.0009391513,8.246792e-7,0.00074161455,0.047854163],"genre_scores_gemma":[0.57665956,0.00015009634,0.4202119,0.00068596157,0.00037597233,0.00009668416,0.0000027437347,0.00008756049,0.0017295358],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99630743,0.00018338131,0.0006132415,0.000821754,0.0012752839,0.0007989209],"domain_scores_gemma":[0.99859816,0.000027496644,0.00024997385,0.00077722117,0.00003314969,0.00031398505],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010392773,0.00051642023,0.00057024934,4.042288e-7,0.00016391426,0.00007669627,0.0006988861,0.0002113209,0.0011606414],"category_scores_gemma":[0.00010300039,0.00048177133,0.00017116316,0.0009305379,0.0002209894,0.00035158766,0.00018720167,0.00033908663,0.00016928227],"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":[0.0000673595,0.00035057365,0.27959785,0.000024151701,0.000042866137,0.000009806039,0.00036566186,0.0008363949,0.0050351033,0.00023945417,0.21386364,0.49956712],"study_design_scores_gemma":[0.0026245061,0.0013502284,0.061746147,0.00031021747,0.00014644017,0.00001715595,0.00040252687,0.019790366,0.028708877,0.024863752,0.85718465,0.0028551403],"about_ca_topic_score_codex":0.0018439699,"about_ca_topic_score_gemma":0.00014008147,"teacher_disagreement_score":0.643321,"about_ca_system_score_codex":0.0008543311,"about_ca_system_score_gemma":0.00007113888,"threshold_uncertainty_score":0.99976337},"labels":[],"label_agreement":null},{"id":"W2126871307","doi":"10.5539/esr.v4n1p68","title":"Sensitivity of UV-B Irradiance to Cloud Optical Depth and Droplets Equivalent Radii","year":2015,"lang":"en","type":"article","venue":"Earth Science Research","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Winnipeg","funders":"","keywords":"Overcast; Irradiance; Zenith; Optical depth; Atmospheric radiative transfer codes; Solar zenith angle; Radiative transfer; RADIUS; Effective radius; Physics; Latitude; Cloud cover; Sensitivity (control systems); Environmental science; Atmospheric sciences; Computational physics; Optics; Astrophysics; Meteorology; Cloud computing; Astronomy; Sky","score_opus":0.08178804089116436,"score_gpt":0.35917011974307955,"score_spread":0.2773820788519152,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2126871307","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":[0.9699511,0.00004426599,0.0018115396,0.0010790405,0.000108852706,0.00025553364,0.0000016409914,0.000014145531,0.026733894],"genre_scores_gemma":[0.9906752,0.000014716742,0.008300698,0.000084259606,0.000057416946,0.000006489421,1.922224e-7,0.00000723866,0.0008537671],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9963829,0.0001639559,0.00016563681,0.00053461187,0.0019404858,0.00081244565],"domain_scores_gemma":[0.99837613,0.00014597028,0.000028383303,0.00038772525,0.000077822515,0.0009839457],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0064976234,0.00010098624,0.00015901685,0.000011557706,0.0002759682,0.00007962058,0.0003837861,0.000043181582,0.00016483515],"category_scores_gemma":[0.00083701283,0.00008500212,0.000023343415,0.0014449912,0.0031426745,0.00027822907,0.00092252804,0.00022940872,0.0004905137],"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":[0.00017270309,0.00034201448,0.46284333,0.000028108032,0.000007615174,0.00015776738,0.004720904,0.0033591846,0.33672673,0.004953415,0.005643128,0.18104509],"study_design_scores_gemma":[0.0003280235,0.0005994944,0.9552966,0.000025680061,0.0000023454493,0.00004458962,0.0008294,0.009357846,0.025366634,0.0004252251,0.007492784,0.00023139677],"about_ca_topic_score_codex":0.0009515688,"about_ca_topic_score_gemma":0.00050634454,"teacher_disagreement_score":0.49245325,"about_ca_system_score_codex":0.00013040467,"about_ca_system_score_gemma":0.00018542413,"threshold_uncertainty_score":0.9995702},"labels":[],"label_agreement":null},{"id":"W2127645710","doi":"10.1002/qj.2294","title":"Estimation of errors associated with the EarthCARE 3D scene construction algorithm","year":2013,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"McMaster University; Environment and Climate Change Canada","funders":"Freie Universität Berlin; European Space Agency","keywords":"Satellite; Remote sensing; Overcast; Radiative transfer; Cloud top; Atmosphere (unit); Environmental science; Atmospheric radiative transfer codes; Algorithm; Cirrus; Meteorology; Flux (metallurgy); Cloud computing; Nadir; Radiative flux; Cloud fraction; Computer science; Cloud cover; Geology; Physics; Sky; Optics","score_opus":0.005517398164708312,"score_gpt":0.1906178392403439,"score_spread":0.18510044107563559,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2127645710","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":[0.98267686,0.000032603828,0.015269508,0.001426144,0.00011774137,0.00016157943,0.0000021340277,0.000009200322,0.00030421172],"genre_scores_gemma":[0.9688983,0.0000020905425,0.030719705,0.00023070084,0.000035452977,0.0000045335332,4.0325543e-7,0.00000615623,0.00010267445],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9985752,0.00021675017,0.00031920848,0.00011411401,0.0005763462,0.00019837178],"domain_scores_gemma":[0.9990053,0.00011786692,0.0006063541,0.00014819445,0.00005428363,0.00006796317],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004920001,0.00012544487,0.00021914809,6.9447685e-7,0.00021931203,0.00002900288,0.00034418158,0.0001201901,0.0010181434],"category_scores_gemma":[0.000037534483,0.000052030882,0.00025705757,0.00016474843,0.0006525518,0.00012434552,0.000040975956,0.0003376591,0.000013728398],"study_design_candidate":"design_other","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":[0.000049024482,0.00023358254,0.052006856,0.0000055815726,0.0002999986,0.0000028038055,0.0023962501,0.043692093,0.0011421309,0.00004315312,0.0035105182,0.896618],"study_design_scores_gemma":[0.0011165019,0.003543742,0.70772475,0.0000474443,0.00022551492,0.00005574469,0.0051575135,0.27875134,0.00041042888,0.002509525,0.00019342024,0.00026405367],"about_ca_topic_score_codex":0.00006735268,"about_ca_topic_score_gemma":0.0000047672743,"teacher_disagreement_score":0.89635396,"about_ca_system_score_codex":0.000088601504,"about_ca_system_score_gemma":0.000014791224,"threshold_uncertainty_score":0.99989504},"labels":[],"label_agreement":null},{"id":"W2127752125","doi":"10.5194/acp-6-5261-2006","title":"Modeling of biomass smoke injection into the lower stratosphere by a large forest fire (Part II): sensitivity studies","year":2006,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":125,"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","keywords":"Plume; Atmospheric sciences; Environmental science; Convection; Smoke; Stratosphere; Water vapor; Tropopause; Cloud top; Meteorology; Climatology; Geology; Cloud computing; Geography","score_opus":0.007260513866971305,"score_gpt":0.2132157696980733,"score_spread":0.205955255831102,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2127752125","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":[0.99358207,0.00074490585,0.0033897997,0.000068084475,0.0000484024,0.00009334878,0.000010188274,0.000030087967,0.0020331158],"genre_scores_gemma":[0.99706286,0.00009706374,0.00096538104,0.00004875441,0.00013258102,0.000012087051,0.000013912562,0.000016110233,0.0016512537],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99897105,0.00002286638,0.00022041268,0.0003075062,0.00021348282,0.000264674],"domain_scores_gemma":[0.99955016,0.000037167676,0.000097353855,0.0002467945,0.000020635809,0.000047867503],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001474311,0.0002088874,0.00021380014,6.765354e-9,0.00040325237,0.000018462548,0.00009471847,0.00008629458,0.00023417473],"category_scores_gemma":[0.000008528519,0.00015873913,0.00007596411,0.00021147725,0.00028454408,0.00012614869,0.0001688435,0.00012992296,0.000004016131],"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":[0.00032622038,0.0032825756,0.2499634,0.0006540853,0.000528209,0.000035027726,0.005640838,0.42833295,0.14774197,0.00035772793,0.027141381,0.1359956],"study_design_scores_gemma":[0.00073048443,0.00017859915,0.003964955,0.00006985956,0.00011949278,0.000014417186,0.0024619123,0.96666694,0.016411485,0.0040002475,0.004729405,0.00065220194],"about_ca_topic_score_codex":0.0032662055,"about_ca_topic_score_gemma":0.00023422988,"teacher_disagreement_score":0.538334,"about_ca_system_score_codex":0.00006518954,"about_ca_system_score_gemma":0.0000119345,"threshold_uncertainty_score":0.6473194},"labels":[],"label_agreement":null},{"id":"W2128160222","doi":"10.1175/jcli-d-11-00610.1","title":"Marine Boundary Layer Cloud Observations in the Azores","year":2012,"lang":"en","type":"article","venue":"Journal of Climate","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":165,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Cloud base; Marine stratocumulus; Environmental science; Liquid water path; Atmospheric sciences; Boundary layer; Drizzle; Cloud top; Planetary boundary layer; Liquid water content; Context (archaeology); Aerosol; Ceilometer; Climatology; Precipitation; Geology; Meteorology; Cloud computing; Turbulence; Geography; Physics","score_opus":0.023990624414835807,"score_gpt":0.26059045154744376,"score_spread":0.23659982713260796,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2128160222","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":[0.98247766,0.00010879193,0.0000658256,0.0013160178,0.0002824234,0.00003907285,8.567202e-7,0.0000027236235,0.015706638],"genre_scores_gemma":[0.99587363,0.00027019848,0.0024393266,0.0010236508,0.00025185812,0.0000014623976,5.073311e-7,0.0000055647397,0.00013377561],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991901,0.000048533166,0.0002567848,0.00003945265,0.00024515603,0.00021996902],"domain_scores_gemma":[0.9996237,0.000052314484,0.00016398123,0.000100669706,0.0000058515648,0.000053440897],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00071536313,0.000059286685,0.00009536442,0.0000012619028,0.000088602384,0.000026400907,0.00020601395,0.000026256123,0.0015256346],"category_scores_gemma":[0.000027613998,0.000034257486,0.00005466657,0.00013621885,0.00006291267,0.0003017748,0.00009228395,0.00016062307,0.00009377806],"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":[0.000014049981,0.00008908014,0.99113804,0.0000022725774,0.0000036964213,0.000007049482,0.00068491575,0.00016478173,0.00031232854,0.00031668626,0.0040064887,0.0032606362],"study_design_scores_gemma":[0.00015288124,0.000035907167,0.9307872,0.0000056958047,0.000009510699,0.00004577016,0.00031937717,0.00004884964,0.0000274693,0.0005191729,0.06800386,0.000044273023],"about_ca_topic_score_codex":0.000041297313,"about_ca_topic_score_gemma":0.00004763834,"teacher_disagreement_score":0.06399737,"about_ca_system_score_codex":0.00004708598,"about_ca_system_score_gemma":0.000006691066,"threshold_uncertainty_score":0.9993871},"labels":[],"label_agreement":null},{"id":"W2128681823","doi":"10.5194/acp-12-10725-2012","title":"Uncertainty associated with convective wet removal of entrained aerosols in a global climate model","year":2012,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Killam Trusts","keywords":"Aerosol; Scavenging; Atmospheric sciences; Convection; Environmental science; Deposition (geology); Troposphere; Meteorology; Chemistry; Climatology; Geology; Physics","score_opus":0.0060819568456453605,"score_gpt":0.20947716619456608,"score_spread":0.20339520934892072,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2128681823","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":[0.9790131,0.00005760321,0.0018813743,0.000014304228,0.000012613933,0.00010797104,0.000026856802,0.00002140179,0.018864783],"genre_scores_gemma":[0.9930012,0.000021800459,0.006504249,0.00006315435,0.00003045564,0.000012383068,0.000013230809,0.000011746519,0.00034178092],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9989305,0.000020592395,0.00018632054,0.00023665317,0.00020551731,0.0004204033],"domain_scores_gemma":[0.9995345,0.000033163742,0.0001308774,0.0001638244,0.000011246279,0.0001263852],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012414089,0.0001927604,0.0002548942,7.346065e-9,0.0000594553,0.0000089961095,0.000108497465,0.00009200763,0.00038728365],"category_scores_gemma":[0.000014514111,0.00016637778,0.000044080163,0.00028407123,0.00027793567,0.00014836613,0.00008305047,0.000114511655,0.0000057385605],"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":[0.0002781948,0.0008203436,0.89746433,0.00006797164,0.00008787992,0.000017543549,0.001387572,0.07067071,0.013416505,0.00073798635,0.00010382909,0.0149471145],"study_design_scores_gemma":[0.004212635,0.0001959215,0.25241193,0.00018317411,0.00016565593,0.00007372296,0.0010970832,0.7279395,0.008445596,0.0037495585,0.000249353,0.0012758904],"about_ca_topic_score_codex":0.00013220031,"about_ca_topic_score_gemma":0.000015762127,"teacher_disagreement_score":0.65726876,"about_ca_system_score_codex":0.00017292348,"about_ca_system_score_gemma":0.000022253,"threshold_uncertainty_score":0.67846894},"labels":[],"label_agreement":null},{"id":"W2128757896","doi":"10.5194/acpd-12-2355-2012","title":"Aerosol observations and growth rates in the tropical tropopause layer","year":2012,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"York University","funders":"","keywords":"Aerosol; Atmospheric sciences; Cloud condensation nuclei; Tropopause; Environmental science; Particle (ecology); Monsoon; Condensation; Convection; Climatology; Troposphere; Chemistry; Meteorology; Physics; Geology","score_opus":0.028350627673936667,"score_gpt":0.24692879545391694,"score_spread":0.21857816777998026,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2128757896","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":[0.9898395,0.00003790387,0.00056467403,0.0022451633,0.000027787395,0.0000896835,6.19933e-7,0.000011631211,0.007183023],"genre_scores_gemma":[0.99592227,0.000020355677,0.0018987557,0.001384255,0.00003593491,0.000017299002,6.453516e-7,0.0000041596422,0.0007163475],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99945086,0.0000368042,0.00008734207,0.0000906199,0.00014495742,0.00018942704],"domain_scores_gemma":[0.99978936,0.00004568895,0.000014331904,0.00009924352,0.000002116802,0.000049266346],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00010441587,0.00006239104,0.000054999055,3.4140712e-7,0.00007681655,0.000019375118,0.000102633414,0.000028508906,0.0012304919],"category_scores_gemma":[0.000024833003,0.000035025576,0.0000132131,0.00011971064,0.00009829454,0.00019494368,0.0000605977,0.00006797583,0.00008866512],"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":[0.0000018720262,0.00005274661,0.9915221,6.396324e-7,9.3588864e-7,4.65463e-7,0.00039936005,0.0000033134131,0.0009925562,0.0036446168,0.0032269238,0.00015449895],"study_design_scores_gemma":[0.00011758868,0.000016439128,0.99719,7.696546e-7,0.0000032866453,0.000003152751,0.00027294367,0.00012361062,0.00026242295,0.00021261725,0.0017391882,0.000057988804],"about_ca_topic_score_codex":0.0003852352,"about_ca_topic_score_gemma":0.0002490947,"teacher_disagreement_score":0.006466675,"about_ca_system_score_codex":0.000025755433,"about_ca_system_score_gemma":0.0000021764922,"threshold_uncertainty_score":0.99968255},"labels":[],"label_agreement":null},{"id":"W2128765794","doi":"10.1175/bams-86-9-1275","title":"THE I3RC: Bringing Together the Most Advanced Radiative Transfer Tools for Cloudy Atmospheres","year":2005,"lang":"en","type":"article","venue":"Bulletin of the American Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":206,"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":"Radiative transfer; Environmental science; Remote sensing; Radiant energy; Computer science; Work (physics); Baseline (sea); Meteorology; Radiation; Physics; Geography; Geology","score_opus":0.009425106186766822,"score_gpt":0.22818647549848808,"score_spread":0.21876136931172127,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2128765794","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":[0.96632195,0.00032391743,0.0044874977,0.02523408,0.00008159783,0.00079660496,0.000012608985,0.000042445296,0.002699331],"genre_scores_gemma":[0.97205806,0.00024612862,0.016228203,0.009365141,0.00011445483,0.00015322669,7.299588e-7,0.000023869106,0.0018102044],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99819934,0.00023534232,0.0003282179,0.00035564232,0.00036147918,0.0005199993],"domain_scores_gemma":[0.99770087,0.0015216703,0.00021497997,0.0004726757,0.000018292323,0.00007149557],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007776532,0.00022802116,0.00031171436,1.5513447e-7,0.00085453154,0.000051780153,0.0010467669,0.00006357611,0.0014504764],"category_scores_gemma":[0.00028075822,0.00009753289,0.000551084,0.00024994687,0.0023411138,0.000034253237,0.00028362506,0.00027284052,0.000050368246],"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":[0.00086800504,0.00033971644,0.012867135,0.000009917655,0.00037474747,6.332716e-7,0.0032876052,0.056916688,0.011670639,0.0015941476,0.11767165,0.79439914],"study_design_scores_gemma":[0.00065953494,0.00045105105,0.070952736,0.0000070706146,0.00008049799,0.0000028306092,0.0042400453,0.0032073515,0.0020373482,0.0004213377,0.9176362,0.00030400784],"about_ca_topic_score_codex":0.0002738833,"about_ca_topic_score_gemma":0.000029401983,"teacher_disagreement_score":0.79996455,"about_ca_system_score_codex":0.00010739127,"about_ca_system_score_gemma":0.0000119181395,"threshold_uncertainty_score":0.9994623},"labels":[],"label_agreement":null},{"id":"W2129325965","doi":"10.5194/acp-10-7945-2010","title":"Volume nucleation rates for homogeneous freezing in supercooled water microdroplets: results from a combined experimental and modelling approach","year":2010,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":66,"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 Waterloo; Environment and Climate Change Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Supercooling; Nucleation; Ice nucleus; Cirrus; Aerosol; Evaporation; Classical nucleation theory; Thermodynamics; Chemistry; Volume (thermodynamics); Materials science; Atmospheric sciences; Geology; Physics","score_opus":0.006961336535307394,"score_gpt":0.20190751046710187,"score_spread":0.19494617393179448,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2129325965","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":[0.99069595,0.000056843688,0.008308739,0.00003148038,0.000030942418,0.00018483034,0.00002012796,0.000023430994,0.0006476405],"genre_scores_gemma":[0.9440192,0.000014252528,0.05505014,0.000041127652,0.00009422227,0.000034435216,0.00011445653,0.000022766155,0.00060941017],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99900883,0.000009175464,0.00020510318,0.0004393076,0.00009243803,0.0002451476],"domain_scores_gemma":[0.9996541,0.000032130967,0.000040024195,0.00018691538,0.0000064560445,0.00008037875],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000078586985,0.0001851049,0.00018154464,2.277289e-8,0.00015164883,0.000054237553,0.00010243365,0.000109043605,0.0002625777],"category_scores_gemma":[0.0000038822527,0.00016176034,0.000035561952,0.00005742128,0.00015415384,0.0001318311,0.00008839884,0.00014751877,0.000006730879],"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":[0.00016100015,0.00016916699,0.0070882547,0.000016267564,0.000013683597,0.0000017401469,0.002161348,0.008113933,0.97667605,0.0000049759683,0.00006458596,0.0055290256],"study_design_scores_gemma":[0.0015807381,0.000038444858,0.0008408299,0.000008495805,0.00001896343,0.0000044454728,0.0005190531,0.781417,0.21426518,0.00044463266,0.0005626138,0.00029961896],"about_ca_topic_score_codex":0.00089118065,"about_ca_topic_score_gemma":0.000007945896,"teacher_disagreement_score":0.77330303,"about_ca_system_score_codex":0.000032832573,"about_ca_system_score_gemma":0.0000049790383,"threshold_uncertainty_score":0.65963954},"labels":[],"label_agreement":null},{"id":"W2129339840","doi":"10.1256/qj.03.153","title":"Liquid fraction in stratiform mixed‐phase clouds from <i>in situ</i> observations","year":2004,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Canadian Foundation for Climate and Atmospheric Sciences; National Science Foundation","keywords":"Fraction (chemistry); Liquid water content; Ice crystals; Cloud fraction; Atmospheric sciences; Phase (matter); Environmental science; Mass fraction; Mixed phase; Mean radiant temperature; Liquid water; Materials science; Meteorology; Climate change; Thermodynamics; Geology; Chemistry; Physics; Cloud computing; Cloud cover; Chromatography","score_opus":0.01549601411316323,"score_gpt":0.23918876634158506,"score_spread":0.22369275222842183,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2129339840","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":[0.9936067,0.000078889345,0.0039289375,0.0016214086,0.0002706416,0.0001254063,0.0000044005687,0.000009265826,0.00035433492],"genre_scores_gemma":[0.99154174,0.000012197334,0.007510273,0.00077571545,0.00011075697,0.000005529514,0.0000013962799,0.0000075889616,0.0000348161],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99838525,0.00012983274,0.00059421675,0.00019357172,0.0004040287,0.00029308297],"domain_scores_gemma":[0.99925077,0.00010682977,0.00034373841,0.00018058244,0.000013414988,0.00010469233],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005519397,0.00015943641,0.00028266266,0.0000014176029,0.00012787759,0.00003223181,0.0004388851,0.0001948149,0.0004121595],"category_scores_gemma":[0.000037117523,0.00009748839,0.00034404438,0.00028131943,0.00017123601,0.00022605072,0.0000523177,0.00064548483,0.000023069748],"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":[0.0022234675,0.008198225,0.4635895,0.000018248618,0.0002683635,0.00020291001,0.01321171,0.24527535,0.20552158,0.0010736703,0.0057670125,0.054649975],"study_design_scores_gemma":[0.0038647172,0.003950347,0.96405256,0.000042189513,0.000050056464,0.000009481123,0.0024188154,0.0017265775,0.0014517268,0.021161377,0.000991421,0.00028071768],"about_ca_topic_score_codex":0.0006444523,"about_ca_topic_score_gemma":0.00057205284,"teacher_disagreement_score":0.50046307,"about_ca_system_score_codex":0.00042994888,"about_ca_system_score_gemma":0.000029539187,"threshold_uncertainty_score":0.45128578},"labels":[],"label_agreement":null},{"id":"W2129366130","doi":"10.5194/acp-13-11175-2013","title":"Feldspar minerals as efficient deposition ice nuclei","year":2013,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":95,"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 Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Jet Propulsion Laboratory; University of Toronto","keywords":"Orthoclase; Plagioclase; Kaolinite; Feldspar; Illite; Mineralogy; Geology; Clay minerals; Mineral; Ice nucleus; Geochemistry; Quartz; Chemistry; Nucleation","score_opus":0.0036334318277771913,"score_gpt":0.18818014946570813,"score_spread":0.18454671763793093,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2129366130","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":[0.9296574,0.00006433807,0.0017444858,0.00012425472,0.000030351168,0.00012321952,0.0000010742726,0.000049024413,0.06820585],"genre_scores_gemma":[0.97678554,0.000028538881,0.010789478,0.00040260542,0.0001313616,0.000033352197,0.000007715495,0.000019076168,0.01180235],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9990583,0.000011538652,0.00014827574,0.00032373064,0.0001947367,0.00026338446],"domain_scores_gemma":[0.9995194,0.000023384204,0.00006408668,0.00022772701,0.000009806755,0.00015561588],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000035137455,0.00018377323,0.00014281066,4.6596353e-9,0.0001659383,0.000058297774,0.00013249948,0.000081404185,0.012206132],"category_scores_gemma":[0.000005778275,0.00016783418,0.000053057054,0.00015063798,0.00015869095,0.00011321619,0.00009742005,0.00011025887,0.0010813418],"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":[0.000025951565,0.0004518155,0.015086938,0.000077853154,0.000047412283,0.000013502776,0.0007735673,0.015225934,0.62023133,0.00012555593,0.014755655,0.33318448],"study_design_scores_gemma":[0.0025572155,0.0003351971,0.089842804,0.00012765202,0.00019353657,0.00017921168,0.0013529758,0.6368277,0.21417092,0.0074897427,0.04388361,0.003039434],"about_ca_topic_score_codex":0.00086627173,"about_ca_topic_score_gemma":0.0000011297795,"teacher_disagreement_score":0.62160176,"about_ca_system_score_codex":0.00005379701,"about_ca_system_score_gemma":0.0000067077417,"threshold_uncertainty_score":0.99969643},"labels":[],"label_agreement":null},{"id":"W2129436226","doi":"10.1039/c3cp54233e","title":"Timescales of water transport in viscous aerosol: measurements on sub-micron particles and dependence on conditioning history","year":2013,"lang":"en","type":"article","venue":"Physical Chemistry Chemical Physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":72,"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":"Engineering and Physical Sciences Research Council","keywords":"Aerosol; Relative humidity; Particle (ecology); Condensation; Chemistry; Range (aeronautics); Particle size; Evaporation; Analytical Chemistry (journal); Thermodynamics; Materials science; Chemical physics; Chromatography; Composite material; Physics","score_opus":0.014100094158650949,"score_gpt":0.20258605219695416,"score_spread":0.1884859580383032,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2129436226","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":[0.9968713,0.000009071339,0.00003106466,0.000057545814,0.000010862675,0.00011337421,0.0000032673854,0.000021521282,0.0028819852],"genre_scores_gemma":[0.9996383,0.0000023837324,0.00007065304,0.00010383815,0.000059965423,0.000033484903,0.000015523701,0.000018848721,0.000056968413],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99874675,0.00001186059,0.00020138934,0.000374186,0.0003641551,0.0003016578],"domain_scores_gemma":[0.9995711,0.000037862766,0.00006139269,0.00019922487,0.000010861518,0.00011957673],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00004238026,0.0002011059,0.00024050577,4.756421e-7,0.000028610353,0.0000066003086,0.00015411942,0.000066217515,0.00031601993],"category_scores_gemma":[0.0000082310735,0.00016285521,0.000069514695,0.000050072627,0.0003791995,0.00012252011,0.000056799767,0.00021326267,0.00011747209],"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":[0.000027925294,0.0005049708,0.0040643797,0.00003100062,0.000007090027,0.0000014169998,0.00022428628,0.00041013953,0.99374825,0.0000091076445,0.00019778458,0.00077362696],"study_design_scores_gemma":[0.00034376557,0.00003851658,0.00276681,0.000038812974,0.000011697798,5.7208814e-7,0.000018664492,0.0008285062,0.9946555,0.0010838513,0.000013203594,0.00020011944],"about_ca_topic_score_codex":0.000079885554,"about_ca_topic_score_gemma":8.4124906e-7,"teacher_disagreement_score":0.0028250166,"about_ca_system_score_codex":0.00021554223,"about_ca_system_score_gemma":0.000007731871,"threshold_uncertainty_score":0.6641043},"labels":[],"label_agreement":null},{"id":"W2129575439","doi":"10.1175/2007jamc1495.1","title":"Atmospheric Response to a Partial Solar Eclipse over a Cotton Field in Central California","year":2007,"lang":"en","type":"article","venue":"Journal of Applied Meteorology and Climatology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada; Agriculture and Agri-Food Canada","funders":"Electric Power Research Institute; National Center for Atmospheric Research; National Science Foundation","keywords":"Eddy covariance; Sensible heat; Environmental science; Atmospheric sciences; Solar eclipse; Meteorology; Water vapor; Climatology; Geology; Physics","score_opus":0.004574602592087015,"score_gpt":0.23187782666462642,"score_spread":0.2273032240725394,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2129575439","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":[0.994028,0.00005562132,0.0028693583,0.0009835112,0.00025278586,0.00012709365,0.000001286767,0.000006286238,0.0016760585],"genre_scores_gemma":[0.99089104,0.000042404565,0.0057502063,0.0031748586,0.00010340467,0.0000044183134,3.4823282e-7,0.000010562219,0.000022786899],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998358,0.000098985074,0.0005808687,0.00022660915,0.00015128491,0.0005842598],"domain_scores_gemma":[0.9989872,0.00039296612,0.00023133912,0.00012900108,0.000007168739,0.0002523332],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012877665,0.00015471732,0.00042281978,0.0000053224203,0.00007389389,0.000007651514,0.00017555946,0.0002666245,0.0014682672],"category_scores_gemma":[0.00009742379,0.00012926217,0.00006441736,0.00019238701,0.00018315465,0.000052552656,0.00012975684,0.00038051506,0.00006255174],"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":[0.037175514,0.00036731508,0.901347,0.0000122536885,0.00007235247,0.00089498603,0.0026084569,0.0009871933,0.034052,0.0012815003,0.003922604,0.01727885],"study_design_scores_gemma":[0.005179028,0.0029917725,0.87463,0.000016844628,0.00011986933,0.0012743241,0.00161279,0.00056019233,0.0058565377,0.004193876,0.103010826,0.0005539607],"about_ca_topic_score_codex":0.0000356191,"about_ca_topic_score_gemma":0.00022804864,"teacher_disagreement_score":0.09908822,"about_ca_system_score_codex":0.00007639182,"about_ca_system_score_gemma":0.000025767808,"threshold_uncertainty_score":0.99944454},"labels":[],"label_agreement":null},{"id":"W2129835346","doi":"10.1029/2002jd002852","title":"Effects of absorbing aerosols on the determination of the surface solar radiation","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Environmental science; Aerosol; Atmospheric sciences; Satellite; Anomaly (physics); Radiative forcing; Earth's energy budget; Absorption (acoustics); Atmosphere (unit); Remote sensing; Radiation; Radiative transfer; Radiation flux; Meteorology; Physics; Geology; Optics","score_opus":0.0159858842509978,"score_gpt":0.27861045545316915,"score_spread":0.26262457120217136,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2129835346","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":[0.99684477,0.00010446591,0.00058814243,0.00029911357,0.000096186064,0.00025170846,5.7863906e-7,0.0000019848205,0.0018130229],"genre_scores_gemma":[0.99864846,0.00006520212,0.0007867807,0.000039678212,0.00003947324,0.0000029888397,5.321015e-8,0.000011482124,0.0004058992],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9971391,0.0006870651,0.00035800136,0.00012504212,0.0014129526,0.0002778684],"domain_scores_gemma":[0.99747217,0.0017046147,0.00038913626,0.00024947844,0.00010140119,0.00008320304],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012891663,0.00010463064,0.00021244577,8.26686e-7,0.00019764672,0.000024251754,0.00049805647,0.000058525882,0.00027849356],"category_scores_gemma":[0.0016002294,0.000053792915,0.00018424484,0.00048212588,0.00045455561,0.00014711231,0.00010578427,0.00047770247,0.000027993168],"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":[0.00046478017,0.001821154,0.094430976,0.0001820929,0.0001297362,0.000027706967,0.0022317097,0.009576091,0.8093772,0.007896707,0.006563756,0.06729808],"study_design_scores_gemma":[0.0008119038,0.0014419709,0.42621425,0.00022860321,0.00003586479,0.0000064759565,0.00048169584,0.0029158972,0.55842036,0.0077349828,0.0015575988,0.0001503888],"about_ca_topic_score_codex":0.00021587612,"about_ca_topic_score_gemma":0.0000140684115,"teacher_disagreement_score":0.33178326,"about_ca_system_score_codex":0.00012360673,"about_ca_system_score_gemma":0.00006644959,"threshold_uncertainty_score":0.30493093},"labels":[],"label_agreement":null},{"id":"W2130575440","doi":"10.1175/jas3784.1","title":"Relative Humidity in Liquid, Mixed-Phase, and Ice Clouds","year":2006,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":127,"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":"Glenn Research Center; Transport Canada; Langley Research Center; National Aeronautics and Space Administration","keywords":"Relative humidity; Ice cloud; Atmospheric sciences; Mesoscale meteorology; Environmental science; Saturation (graph theory); Humidity; Ice nucleus; Liquid water content; Liquid water; Climatology; Meteorology; Geology; Satellite; Geography; Thermodynamics; Physics; Cloud computing","score_opus":0.009674396235874788,"score_gpt":0.24572892642307861,"score_spread":0.23605453018720382,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2130575440","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":[0.99023646,0.0006684451,0.00024896688,0.0012056556,0.00041093762,0.00008148971,6.025076e-7,0.000005560447,0.007141865],"genre_scores_gemma":[0.9903764,0.000053092368,0.008717397,0.00019888536,0.00009838816,0.0000013253509,4.330498e-8,0.0000057198467,0.00054874265],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984173,0.00012312237,0.00041472266,0.00019914475,0.00057410134,0.00027159957],"domain_scores_gemma":[0.9992229,0.00011455563,0.00043729288,0.00014094026,0.000014735122,0.0000695987],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008322043,0.00013020421,0.00020421563,6.137517e-7,0.00029990525,0.00005150736,0.0006142974,0.000055250443,0.00039857818],"category_scores_gemma":[0.000089422385,0.000075478834,0.00008832486,0.00087776384,0.0010273656,0.0005134456,0.00023947557,0.00022202954,0.00001277966],"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":[0.00028786747,0.0008771161,0.87259185,0.000012819574,0.000031425967,0.00007599329,0.0019828298,0.072388895,0.018327018,0.002951878,0.018037122,0.012435184],"study_design_scores_gemma":[0.002450986,0.0021792934,0.9206742,0.00013873968,0.000073308176,0.00036350323,0.002847681,0.018119821,0.0036633518,0.02578087,0.02309102,0.00061719114],"about_ca_topic_score_codex":0.0006408858,"about_ca_topic_score_gemma":0.00019798447,"teacher_disagreement_score":0.054269075,"about_ca_system_score_codex":0.00012097515,"about_ca_system_score_gemma":0.000043834632,"threshold_uncertainty_score":0.43641514},"labels":[],"label_agreement":null},{"id":"W2130763121","doi":"10.1002/2013jd020683","title":"Effects of 3‐D clouds on atmospheric transmission of solar radiation: Cloud type dependencies inferred from A‐train satellite data","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":30,"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":"Oak Ridge Associated Universities; Langley Research Center; National Aeronautics and Space Administration","keywords":"Radiance; Irradiance; Nadir; Downwelling; Cloud top; Shortwave; Radiative transfer; Infrared window; Remote sensing; Atmospheric radiative transfer codes; Absorption (acoustics); Environmental science; Satellite; Solar irradiance; Atmosphere (unit); Meteorology; Optical depth; Cloud cover; Atmospheric model; Cloud fraction; Cloud computing; Physics; Optics; Geography; Geology; Computer science; Infrared; Astronomy; Aerosol","score_opus":0.02626330835231113,"score_gpt":0.30050639390737716,"score_spread":0.27424308555506605,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2130763121","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":[0.99212265,0.001099582,0.0047212807,0.00019582798,0.00025250352,0.00024178057,0.00000844188,0.000010744534,0.001347191],"genre_scores_gemma":[0.9889757,0.0010681776,0.009201203,0.00005276664,0.00039588843,0.0000023019509,0.0000078636995,0.00003427793,0.00026182557],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99536294,0.00073129224,0.0007999014,0.00040905134,0.0021756208,0.0005211965],"domain_scores_gemma":[0.9961145,0.0020840315,0.0005237199,0.00073077576,0.00017190742,0.00037505792],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014585447,0.00025289095,0.000666311,0.0000017589769,0.00014516123,0.000040841278,0.0014466993,0.00017016142,0.000997549],"category_scores_gemma":[0.0011401139,0.00018825299,0.00019992855,0.00076773943,0.00060283236,0.00037983837,0.00040326666,0.00074782205,0.000103528524],"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":[0.002369592,0.0021923576,0.054136008,0.00026292703,0.00035667446,0.000075787,0.0016322207,0.0036794865,0.21098715,0.000630214,0.009713362,0.7139642],"study_design_scores_gemma":[0.0036697285,0.008542221,0.8039483,0.000693361,0.00018766541,0.000009812989,0.0005621672,0.035356965,0.078969605,0.01250178,0.054932706,0.0006257091],"about_ca_topic_score_codex":0.0014523846,"about_ca_topic_score_gemma":0.000031407584,"teacher_disagreement_score":0.74981225,"about_ca_system_score_codex":0.00012410719,"about_ca_system_score_gemma":0.00014264928,"threshold_uncertainty_score":0.99991566},"labels":[],"label_agreement":null},{"id":"W2130890725","doi":"10.1364/ao.47.001336","title":"Standoff determination of the particle size and concentration of small optical depth clouds based on double scattering measurements: concept and experimental validation with bioaerosols","year":2008,"lang":"en","type":"article","venue":"Applied Optics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Defence Research and Development Canada","funders":"","keywords":"Lidar; Optics; Bioaerosol; Scattering; Mie scattering; Optical depth; Attenuation; Aerosol; Remote sensing; Forward scatter; Indoor bioaerosol; Light scattering; Particle (ecology); Atmospheric optics; Physics; Materials science; Meteorology; Geology","score_opus":0.02483668292978458,"score_gpt":0.22558092230272625,"score_spread":0.20074423937294167,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2130890725","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":[0.99303186,0.000010936575,0.0045479573,0.000033152544,0.000016686201,0.00032581185,0.0000013255101,0.000007786276,0.002024472],"genre_scores_gemma":[0.9889785,0.0000034293007,0.010916458,0.000057194222,0.0000069553053,0.000017517174,0.0000013735554,0.000008408338,0.000010178941],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.999262,0.000015654607,0.00017556956,0.00016142079,0.00026835618,0.00011699964],"domain_scores_gemma":[0.9996492,0.000046528734,0.000113788155,0.00013274307,0.000011980136,0.000045743534],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000090634436,0.00009484856,0.0001117987,5.0596856e-7,0.00009611981,0.000011335153,0.000063382424,0.000037483427,0.00002612761],"category_scores_gemma":[0.0000074143422,0.00006846164,0.000013775583,0.00008177993,0.0004968993,0.000052833013,0.0000436748,0.000041863135,7.216754e-7],"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":[0.00037807325,0.00022428305,0.15857504,0.000014843944,0.0000099091685,8.0258894e-7,0.0015390734,0.00849372,0.82879716,0.0006608645,0.0000035175142,0.0013026968],"study_design_scores_gemma":[0.0017718825,0.00020377318,0.06336259,0.000015042637,0.000018088931,0.0000024392286,0.00024371779,0.005322911,0.928957,0.000011002673,0.000002419813,0.000089122455],"about_ca_topic_score_codex":0.000016492848,"about_ca_topic_score_gemma":0.000008910803,"teacher_disagreement_score":0.10015984,"about_ca_system_score_codex":0.000043836655,"about_ca_system_score_gemma":0.0000130796725,"threshold_uncertainty_score":0.27917847},"labels":[],"label_agreement":null},{"id":"W2131538664","doi":"10.1029/2003jd004047","title":"Aerosol optical characterization by nephelometer and lidar: The Baltimore Supersite experiment during the Canadian forest fire smoke intrusion","year":2004,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":50,"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":"Johns Hopkins University","keywords":"Nephelometer; Aerosol; Lidar; Haze; Aethalometer; Environmental science; Atmospheric sciences; Mie scattering; Soot; Extinction (optical mineralogy); Molar absorptivity; Mass concentration (chemistry); Scattering; Light scattering; Remote sensing; Meteorology; Materials science; Mineralogy; Optics; Geology; Chemistry; Physics; Combustion","score_opus":0.014524164265521734,"score_gpt":0.26208583706437216,"score_spread":0.24756167279885044,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2131538664","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":[0.99351305,0.00015820049,0.00007464668,0.005548179,0.000067635614,0.00024577917,0.0000045513602,0.000005373583,0.0003825592],"genre_scores_gemma":[0.9986071,0.00015087663,0.00027716535,0.00024918834,0.0002292729,0.000012373835,0.00000253011,0.000019448642,0.00045205557],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99764454,0.00013428046,0.00029146165,0.0002239591,0.0011087025,0.00059708225],"domain_scores_gemma":[0.99897826,0.00013908953,0.000097058655,0.000253182,0.00006831616,0.00046410467],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00049796014,0.00016395691,0.00018910793,0.0000015071014,0.0011344297,0.00025909438,0.0005207675,0.00007664432,0.0006594016],"category_scores_gemma":[0.00012950251,0.00008726192,0.0000988982,0.00033974674,0.00082676,0.00032113006,0.0003411894,0.0007027303,0.0000618973],"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":[0.0010691795,0.0010906191,0.41309512,0.00006368229,0.00028969406,0.00052434177,0.0090429075,0.0022872891,0.50178295,0.0013820555,0.0064108674,0.06296129],"study_design_scores_gemma":[0.0008103606,0.00068802125,0.9833593,0.000061240724,0.000018169256,0.00006783997,0.0011419599,0.0007254036,0.007595997,0.0004229012,0.0049049105,0.00020393475],"about_ca_topic_score_codex":0.044700198,"about_ca_topic_score_gemma":0.014360891,"teacher_disagreement_score":0.57026416,"about_ca_system_score_codex":0.0005678602,"about_ca_system_score_gemma":0.0001250321,"threshold_uncertainty_score":0.9616612},"labels":[],"label_agreement":null},{"id":"W2132099862","doi":"10.1139/p06-091","title":"Calibration of the Purple Crow Lidar vibrational Raman water-vapour mixing ratio and temperature measurements","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Radiosonde; Calibration; Water vapor; Mixing ratio; Raman spectroscopy; Lidar; Altitude (triangle); Stratosphere; Physics; Mixing (physics); Atmospheric sciences; Remote sensing; Analytical Chemistry (journal); Environmental science; Meteorology; Optics; Chemistry; Geology; Environmental chemistry","score_opus":0.01141017307986375,"score_gpt":0.19625340688581686,"score_spread":0.1848432338059531,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2132099862","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":[0.99476707,0.000038321807,0.0040385355,0.00054594007,0.00016236388,0.000063714826,0.0000033221854,0.0000015689787,0.00037917506],"genre_scores_gemma":[0.9988149,0.0000012407438,0.00074226374,0.00020478613,0.00015407654,3.2686864e-7,8.9273686e-7,0.000010211214,0.00007134371],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.999303,0.000025338588,0.00020536588,0.000069099326,0.0002393951,0.0001578353],"domain_scores_gemma":[0.999575,0.000008247991,0.00012591378,0.00008014083,0.00003155555,0.00017914813],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026031624,0.00007162814,0.00008828839,0.0000015838846,0.00019174904,0.00004028437,0.00013117227,0.0000411259,0.00019060067],"category_scores_gemma":[0.000017437917,0.00004586453,0.00004619637,0.0000942778,0.000114750925,0.000282678,0.000015614152,0.00012165554,0.0000015029958],"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":[0.000020680096,0.000033633543,0.4905109,0.000010486959,0.000042238666,0.000012107487,0.0032910646,0.0055280738,0.49395195,0.000685927,0.0017967506,0.004116193],"study_design_scores_gemma":[0.0006446434,0.00016322269,0.42319977,0.000078833706,0.000049160913,0.000046307858,0.00063311984,0.00063212763,0.5701768,0.0023622545,0.0017609755,0.00025281863],"about_ca_topic_score_codex":0.0010389201,"about_ca_topic_score_gemma":0.010612324,"teacher_disagreement_score":0.076224834,"about_ca_system_score_codex":0.00011395792,"about_ca_system_score_gemma":0.00011205256,"threshold_uncertainty_score":0.5921926},"labels":[],"label_agreement":null},{"id":"W2133673175","doi":"10.1029/2004jd005119","title":"Simulations of midlatitude frontal clouds by single‐column and cloud‐resolving models during the Atmospheric Radiation Measurement March 2000 cloud intensive operational period","year":2005,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":119,"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","funders":"","keywords":"Middle latitudes; Environmental science; Cloud height; Lidar; Cloud top; Ice cloud; Meteorology; Cirrus; Cloud computing; Atmospheric sciences; Precipitation; Cloud physics; Remote sensing; Climatology; Cloud cover; Geology; Geography; Computer science","score_opus":0.025795817760802437,"score_gpt":0.27208076347041377,"score_spread":0.24628494570961132,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2133673175","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":[0.9937006,0.0016968065,0.0018239699,0.0016677999,0.00015613773,0.00039930304,0.000015528001,0.000010070084,0.0005297442],"genre_scores_gemma":[0.99454755,0.0001528762,0.0036202576,0.000105776155,0.0008754636,0.000011997698,0.0000026597138,0.000033661796,0.00064977957],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99525815,0.0003962382,0.00078585517,0.00035085267,0.0026055227,0.00060337],"domain_scores_gemma":[0.99808455,0.00036378216,0.00035513713,0.00029970586,0.0005936972,0.00030313228],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010785239,0.0002511738,0.00041489545,0.0000019876852,0.0006618936,0.0001563417,0.0005350416,0.00011331919,0.0012217042],"category_scores_gemma":[0.0005168838,0.00018552555,0.00017978605,0.0004713376,0.00077186903,0.00068414706,0.00038064664,0.0007296361,0.000028469409],"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":[0.0016592866,0.002034746,0.053756427,0.00008714116,0.00056024874,0.000040903407,0.00913016,0.571147,0.29759225,0.0005971388,0.032308545,0.031086141],"study_design_scores_gemma":[0.0042287824,0.0024603668,0.31836575,0.00029703844,0.00014605223,0.00010376271,0.0051722676,0.64246494,0.0070251706,0.002578317,0.016285293,0.0008722752],"about_ca_topic_score_codex":0.0010173869,"about_ca_topic_score_gemma":0.00038485436,"teacher_disagreement_score":0.2905671,"about_ca_system_score_codex":0.0010848794,"about_ca_system_score_gemma":0.00021177459,"threshold_uncertainty_score":0.9996913},"labels":[],"label_agreement":null},{"id":"W2134426855","doi":"10.1002/2015jd023094","title":"Phase transformations in an ascending adiabatic mixed‐phase cloud volume","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Environment Canada; Israel Science Foundation; U.S. Department of Energy","keywords":"Adiabatic process; Phase (matter); Basis (linear algebra); Transformation (genetics); Volume (thermodynamics); Constant (computer programming); Relaxation (psychology); Thermodynamics; Mechanics; Physics; Geology; Chemistry; Mathematics; Geometry","score_opus":0.05713735372851362,"score_gpt":0.37233436293405936,"score_spread":0.3151970092055457,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2134426855","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":[0.99377805,0.000119447584,0.0025350885,0.0004960696,0.00019515469,0.00021301527,0.0000051622155,0.000012483111,0.0026455552],"genre_scores_gemma":[0.9961069,0.00003249654,0.0028196804,0.000045890334,0.00037699443,0.000010922358,0.000002879363,0.00002349054,0.00058072247],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9963774,0.00044631283,0.00063657813,0.00022859409,0.001602882,0.00070819486],"domain_scores_gemma":[0.99832636,0.00018735667,0.00016935178,0.0002679411,0.0001322786,0.0009167332],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0017785825,0.00017563895,0.00036090604,0.0000049451937,0.00017519755,0.0001235404,0.00063272804,0.00008967075,0.0013735703],"category_scores_gemma":[0.00042295415,0.0001415329,0.00014404659,0.0008834284,0.00040034868,0.0011555813,0.00011847502,0.0008607661,0.0004814299],"study_design_candidate":"design_other","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":[0.004495456,0.036036298,0.10677449,0.0001011114,0.0001889274,0.0015518398,0.01886793,0.018925915,0.029437585,0.0023734516,0.13914427,0.6421027],"study_design_scores_gemma":[0.066770636,0.06642187,0.16936582,0.000630045,0.00018950489,0.00029520117,0.034354996,0.47600064,0.005693329,0.053065952,0.124744065,0.0024679436],"about_ca_topic_score_codex":0.0006358419,"about_ca_topic_score_gemma":0.00032503257,"teacher_disagreement_score":0.6396348,"about_ca_system_score_codex":0.00048337382,"about_ca_system_score_gemma":0.00018828448,"threshold_uncertainty_score":0.9995393},"labels":[],"label_agreement":null},{"id":"W2134920032","doi":"10.1007/s10584-005-9025-y","title":"Elicitation of Expert Judgments of Aerosol Forcing","year":2006,"lang":"en","type":"article","venue":"Climatic Change","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":89,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Aerosol; Forcing (mathematics); Radiative forcing; Environmental science; Atmospheric sciences; Atmosphere (unit); Cloud forcing; Climatology; Meteorology; Physics; Geology","score_opus":0.02674851925218357,"score_gpt":0.24913785405967964,"score_spread":0.22238933480749606,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2134920032","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":[0.98948455,0.000081674414,0.0011301677,0.00008850904,0.00005967409,0.0001855662,0.000002801151,0.000010029968,0.008957058],"genre_scores_gemma":[0.9955536,0.000016676026,0.0040773028,0.000093136434,0.000035804478,0.00003109471,0.000005428083,0.000008036712,0.000178937],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9993336,0.000012076503,0.00023364776,0.000101616555,0.00019117586,0.00012786881],"domain_scores_gemma":[0.9996587,0.00002500686,0.00015447309,0.00013531465,0.0000055554883,0.000020930293],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000080707614,0.00006778005,0.00013097559,0.000001227253,0.000029907536,0.0000028443114,0.000087659835,0.000031271997,0.0009672344],"category_scores_gemma":[0.000008911748,0.00005944241,0.000041567822,0.000111807174,0.0000781995,0.00009148305,0.000057941015,0.000021508615,0.000043166605],"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":[0.000049849303,0.00097444956,0.39805582,0.0004156536,0.00003146547,0.000004627629,0.01716889,0.00058798026,0.5128381,0.0011986245,0.0075925887,0.061081957],"study_design_scores_gemma":[0.003179216,0.0008999663,0.7085674,0.000610718,0.00010692838,0.000007923903,0.005727914,0.03595293,0.2384848,0.0036720354,0.0017661022,0.0010240923],"about_ca_topic_score_codex":0.0010519769,"about_ca_topic_score_gemma":0.000066793575,"teacher_disagreement_score":0.31051156,"about_ca_system_score_codex":0.000039818635,"about_ca_system_score_gemma":0.000001579922,"threshold_uncertainty_score":0.999946},"labels":[],"label_agreement":null},{"id":"W2134999299","doi":"10.1175/jcli-d-13-00663.1","title":"A Global Climatology of Outgoing Longwave Spectral Cloud Radiative Effect and Associated Effective Cloud Properties","year":2014,"lang":"en","type":"article","venue":"Journal of Climate","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":17,"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","funders":"","keywords":"Longwave; Atmospheric Infrared Sounder; Outgoing longwave radiation; Environmental science; Radiative transfer; Climate model; Meteorology; Spectroradiometer; Cloud computing; Radiative flux; Cloud cover; Earth's energy budget; Cloud top; Climatology; Atmospheric sciences; Cloud height; Remote sensing; Flux (metallurgy); Atmosphere (unit); Radiation; Climate change; Physics; Troposphere; Geology; Computer science; Reflectivity","score_opus":0.004481290120912429,"score_gpt":0.22237110222508158,"score_spread":0.21788981210416916,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2134999299","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":[0.9931109,0.00020663886,0.0004831107,0.00010356835,0.0004188244,0.00020894852,0.000006513868,0.00001201441,0.0054494697],"genre_scores_gemma":[0.9991785,0.00015540374,0.00042740605,0.000077369965,0.00012922849,0.0000030896617,5.319193e-7,0.000013257166,0.000015181018],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981608,0.00043381605,0.0005212077,0.0001818264,0.0003190856,0.0003832575],"domain_scores_gemma":[0.998675,0.00024502646,0.00080334157,0.00011117226,0.000030781266,0.00013471818],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011550627,0.0001984277,0.0006394284,0.0000040371865,0.000106429456,0.000024884439,0.0001724722,0.00011336685,0.000102990656],"category_scores_gemma":[0.00037553185,0.0001383354,0.00016285806,0.00017096066,0.00033575998,0.0001743753,0.00014828883,0.00020336757,0.000019416244],"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":[0.0005117977,0.00010421094,0.99010944,0.000055563403,0.000119707445,0.000025300697,0.0007789627,0.0008543376,0.0017340092,0.00017290341,0.00027875413,0.0052550165],"study_design_scores_gemma":[0.002840409,0.0032938516,0.98427296,0.00021504187,0.00021077057,0.0002456143,0.00030303418,0.0038848955,0.0033047437,0.00095297856,0.00018921094,0.00028652188],"about_ca_topic_score_codex":0.000055410852,"about_ca_topic_score_gemma":0.00004988636,"teacher_disagreement_score":0.0060676206,"about_ca_system_score_codex":0.00017898782,"about_ca_system_score_gemma":0.000014494268,"threshold_uncertainty_score":0.5641154},"labels":[],"label_agreement":null},{"id":"W2135832014","doi":"10.5194/amt-7-3399-2014","title":"Verification and application of the extended spectral deconvolution algorithm (SDA+) methodology to estimate aerosol fine and coarse mode extinction coefficients in the marine boundary layer","year":2014,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Université de Sherbrooke","funders":"Climate Program Office; Office of Naval Research; National Oceanic and Atmospheric Administration; National Aeronautics and Space Administration","keywords":"AERONET; Aerosol; Nephelometer; Deconvolution; Extinction (optical mineralogy); Remote sensing; Environmental science; Sun photometer; Single-scattering albedo; Algorithm; Mode (computer interface); Angstrom exponent; Meteorology; Scattering; Computer science; Physics; Optics; Light scattering; Geology","score_opus":0.02099464815177335,"score_gpt":0.28142645426497737,"score_spread":0.26043180611320405,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2135832014","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.41562328,0.000029754992,0.582938,0.00027131097,0.000035660556,0.0006745136,7.189654e-7,0.000040590785,0.00038616476],"genre_scores_gemma":[0.754865,0.000018221006,0.24474218,0.00015220666,0.000016596592,0.00017465353,0.0000020762857,0.000010391886,0.000018693707],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9984126,0.00031215794,0.00030511577,0.0003549621,0.00041273123,0.00020244328],"domain_scores_gemma":[0.9993285,0.000053309457,0.0001686386,0.00037379222,0.000030573025,0.000045174373],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016826104,0.00015794816,0.0001807351,0.0000010996636,0.00016349612,0.000022683958,0.00022102703,0.00007778485,0.000033069464],"category_scores_gemma":[0.000111009125,0.00010708293,0.000029754243,0.000295123,0.00022101079,0.000085837375,0.00015556416,0.00011810258,0.000002280824],"study_design_candidate":"design_other","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":[0.0000524133,0.00017780722,0.041017693,0.000018052939,0.0000090530175,2.6704535e-7,0.00047458452,0.00047567644,0.090569794,0.00045390023,0.00022755444,0.8665232],"study_design_scores_gemma":[0.00059333286,0.000530808,0.7535401,0.00004074208,0.00007212852,0.000024823124,0.00016504747,0.1867534,0.0458806,0.007867403,0.004148008,0.00038358627],"about_ca_topic_score_codex":0.00093919283,"about_ca_topic_score_gemma":0.0007441114,"teacher_disagreement_score":0.8661396,"about_ca_system_score_codex":0.00015600515,"about_ca_system_score_gemma":0.0000114418735,"threshold_uncertainty_score":0.43667153},"labels":[],"label_agreement":null},{"id":"W2135967342","doi":"10.1175/jtech-d-11-00046.1","title":"A Remotely Operated Lidar for Aerosol, Temperature, and Water Vapor Profiling in the High Arctic","year":2011,"lang":"en","type":"article","venue":"Journal of Atmospheric and Oceanic Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University; University of Toronto; Dalhousie University","funders":"","keywords":"Lidar; Water vapor; Environmental science; Mixing ratio; Troposphere; Remote sensing; Aerosol; Arctic; Rayleigh scattering; Depolarization ratio; Backscatter (email); Atmosphere (unit); Meteorology; Atmospheric sciences; Optics; Geology; Physics; Computer science","score_opus":0.009415410949514527,"score_gpt":0.20303878465162387,"score_spread":0.19362337370210933,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2135967342","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":[0.9975667,0.00056448305,0.00058768905,0.00078834366,0.00009629491,0.00025575218,8.0737874e-7,0.000016103193,0.00012381644],"genre_scores_gemma":[0.95537823,0.00022197927,0.04391215,0.0003393232,0.000032031418,0.000006219896,4.4654524e-7,0.00001565218,0.00009393631],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989278,0.0000354458,0.00038082438,0.00021081296,0.00013426063,0.00031088098],"domain_scores_gemma":[0.9995727,0.00003268037,0.00015010257,0.00016103424,0.000028354263,0.000055132306],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035584794,0.00016323183,0.00027837744,0.0000016895777,0.00013049234,0.000027078084,0.0002938225,0.00019961238,0.00015095761],"category_scores_gemma":[0.000052235606,0.00008695648,0.00004292173,0.00027131668,0.00029920493,0.00014954818,0.000115504554,0.00035756975,0.0000037555994],"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":[0.0017701014,0.001178226,0.7072612,0.00021095194,0.00031657278,0.0008395289,0.011315247,0.00016156044,0.20182791,0.006765683,0.0020079406,0.06634507],"study_design_scores_gemma":[0.017967291,0.016947147,0.72705144,0.0005216055,0.0007367795,0.011867719,0.03305594,0.0044615786,0.104986414,0.068766125,0.010876252,0.002761732],"about_ca_topic_score_codex":0.000066451736,"about_ca_topic_score_gemma":0.000013389662,"teacher_disagreement_score":0.0968415,"about_ca_system_score_codex":0.00004511568,"about_ca_system_score_gemma":0.000016528493,"threshold_uncertainty_score":0.35459825},"labels":[],"label_agreement":null},{"id":"W2135998068","doi":"10.1029/2005jd006843","title":"Remote sensing of cloud properties using ground‐based measurements of zenith radiance","year":2006,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Natural Resources Canada","funders":"","keywords":"Overcast; Radiance; Zenith; Remote sensing; Environmental science; Radiative transfer; Shortwave; Irradiance; Brightness temperature; Cloud top; Brightness; Microwave; Cloud height; Solar zenith angle; Cloud computing; Physics; Meteorology; Cloud cover; Optics; Geology; Computer science; Sky; Satellite; Astronomy","score_opus":0.07699372004236811,"score_gpt":0.30650173186111557,"score_spread":0.22950801181874747,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2135998068","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":[0.99237597,0.0002318511,0.0050882045,0.000100958096,0.00008979192,0.00015667854,0.0000012785391,0.0000052891746,0.0019499552],"genre_scores_gemma":[0.9654707,0.000008256974,0.033858627,0.000018694993,0.0002546542,1.7791024e-7,2.5260186e-7,0.000024600718,0.00036406468],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9960607,0.00033240285,0.0007091367,0.00021050173,0.0021820148,0.0005052086],"domain_scores_gemma":[0.9985356,0.00016841173,0.00052562595,0.00028358726,0.0003209163,0.00016587762],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011054341,0.00017087531,0.00045941686,0.000003278588,0.00016033206,0.0000344441,0.00041865263,0.00007704308,0.00025545736],"category_scores_gemma":[0.00027352228,0.0001270185,0.00021687851,0.0006313729,0.00088728976,0.000239486,0.00014902458,0.00042270293,0.00001604421],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009156183,0.00055754196,0.03458257,0.00013484614,0.00008761973,0.00006113024,0.00021363713,0.020379625,0.90890414,0.00003259087,0.0015192641,0.032611415],"study_design_scores_gemma":[0.0044849496,0.0036161651,0.34736654,0.0019012437,0.00016804924,0.0000752066,0.0011092973,0.16841647,0.46193308,0.007927775,0.0021176878,0.0008835472],"about_ca_topic_score_codex":0.0138247,"about_ca_topic_score_gemma":0.00017846545,"teacher_disagreement_score":0.44697106,"about_ca_system_score_codex":0.0002907602,"about_ca_system_score_gemma":0.00017834891,"threshold_uncertainty_score":0.9927423},"labels":[],"label_agreement":null},{"id":"W2136447060","doi":"10.5194/acp-8-4787-2008","title":"Parameterization of sea-salt optical properties and physics of the associated radiative forcing","year":2008,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"University of Victoria; Environment and Climate Change Canada","funders":"","keywords":"Longwave; Shortwave; Radiative forcing; Sea salt; Forcing (mathematics); Atmospheric sciences; Environmental science; Cloud forcing; Radiative transfer; Wavelength; Climatology; Aerosol; Meteorology; Physics; Geology; Optics","score_opus":0.012760470708590784,"score_gpt":0.1874955659371302,"score_spread":0.17473509522853942,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2136447060","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":[0.99641097,0.0000633887,0.0017303607,0.000020462609,0.000012779729,0.000085692736,0.000004163657,0.000008641203,0.0016635722],"genre_scores_gemma":[0.9963804,0.00008152024,0.002969922,0.00002633796,0.000026053776,0.000005153664,0.000002384668,0.000009383521,0.00049888145],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9993846,0.000017138516,0.00015160674,0.0001570471,0.00016691818,0.00012269297],"domain_scores_gemma":[0.9996411,0.000034395624,0.00013727935,0.00013303687,0.000014428527,0.000039718358],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00003956144,0.00011219544,0.00017573855,4.596724e-9,0.00011898978,0.000005280003,0.000079544356,0.000055000473,0.0000621954],"category_scores_gemma":[0.000026440146,0.00008118433,0.00004334849,0.00016606906,0.0005679674,0.00008413373,0.00009399263,0.00008109398,7.7214247e-7],"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":[0.000058928017,0.0003676453,0.55360115,0.00019675808,0.00010964899,0.0000020693583,0.0040959287,0.013519661,0.3404604,0.000108059015,0.00014474372,0.08733503],"study_design_scores_gemma":[0.00078709924,0.00011009633,0.2703297,0.00009959317,0.00009332091,0.000011166682,0.00033664508,0.20712224,0.51905173,0.0015840825,0.00009178303,0.0003825523],"about_ca_topic_score_codex":0.000104320534,"about_ca_topic_score_gemma":8.510975e-7,"teacher_disagreement_score":0.28327143,"about_ca_system_score_codex":0.000026811444,"about_ca_system_score_gemma":0.000015791467,"threshold_uncertainty_score":0.33106008},"labels":[],"label_agreement":null},{"id":"W2136963827","doi":"10.1175/2007jcli1828.1","title":"Impact of Dynamics and Atmospheric State on Cloud Vertical Overlap","year":2008,"lang":"en","type":"article","venue":"Journal of Climate","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Office of Science; National Oceanic and Atmospheric Administration; U.S. Department of Energy","keywords":"Middle latitudes; Convection; Environmental science; Radiative transfer; Atmospheric circulation; Climatology; Atmospheric sciences; Subsidence; Wind shear; Geology; Meteorology; Wind speed; Physics","score_opus":0.006944011160492291,"score_gpt":0.24388021884666777,"score_spread":0.2369362076861755,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2136963827","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":[0.99661964,0.00004754338,0.00037414403,0.000054619915,0.00010326409,0.00003679864,0.000004850252,0.000004216787,0.0027549127],"genre_scores_gemma":[0.9974313,0.0011406537,0.0012433612,0.00005447912,0.000034081262,2.377947e-7,2.910292e-7,0.00001159188,0.000083996994],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989752,0.000029273708,0.00035946886,0.00009331532,0.0003190131,0.00022372231],"domain_scores_gemma":[0.99947226,0.000049553346,0.00020334861,0.00010820697,0.00001444901,0.00015219337],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015872462,0.00011098872,0.0002505309,7.108458e-7,0.0000656567,0.000008249405,0.00011454017,0.000039930113,0.0005012965],"category_scores_gemma":[0.000027378908,0.00007606304,0.00013622583,0.00010956055,0.00020350459,0.00012868411,0.00007071461,0.00015383835,0.000027293954],"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":[0.0003444807,0.00017627393,0.98579276,0.000006819986,0.00003660198,0.00008892016,0.00024160792,0.006455015,0.0010339502,0.0000704773,0.0005094542,0.005243641],"study_design_scores_gemma":[0.00057818735,0.0013192445,0.9873022,0.00002124326,0.000018242745,0.0002291839,0.000046148987,0.010050046,0.0000989184,0.00015638869,0.000081048056,0.000099192024],"about_ca_topic_score_codex":0.000048342004,"about_ca_topic_score_gemma":0.000006430296,"teacher_disagreement_score":0.005144449,"about_ca_system_score_codex":0.00017507891,"about_ca_system_score_gemma":0.000020221894,"threshold_uncertainty_score":0.5488845},"labels":[],"label_agreement":null},{"id":"W2137743092","doi":"10.1029/2001jd001484","title":"A new statistically based autoconversion rate parameterization for use in large‐scale models","year":2002,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"Biological and Environmental Research; Natural Sciences and Engineering Research Council of Canada; U.S. Department of Energy; Office of Science; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Precipitation; Environmental science; Cloud computing; Scale (ratio); Grid; Climate model; Meteorology; Atmospheric sciences; Climatology; Climate change; Econometrics; Statistical physics; Mathematics; Computer science; Geology; Geography; Physics; Geometry","score_opus":0.05084534439551253,"score_gpt":0.30525621004289977,"score_spread":0.25441086564738724,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2137743092","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":[0.64197284,0.000021144428,0.35694146,0.00039684202,0.00004562596,0.0003294355,0.0000075793255,0.0000074003397,0.00027765328],"genre_scores_gemma":[0.8681356,0.00003277151,0.12972987,0.00014909187,0.00009365558,0.000015039999,0.0000020169025,0.000022183824,0.0018198005],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9976518,0.00025817665,0.00042147763,0.00025160844,0.0008404175,0.0005765153],"domain_scores_gemma":[0.99828565,0.0009174577,0.00014854046,0.00019123411,0.00009749758,0.00035963312],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007573694,0.00013750522,0.00027755497,0.0000029369337,0.00012972143,0.000111209585,0.00032432505,0.0000843061,0.0028284998],"category_scores_gemma":[0.0004857983,0.00010986237,0.00013109046,0.00047611236,0.00014321071,0.00063857227,0.00011234223,0.00039087737,0.00010800806],"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":[0.006392058,0.0067239315,0.11606499,0.00021784857,0.00016258775,0.00053071225,0.0036334398,0.30911198,0.051326018,0.004953078,0.26700032,0.23388304],"study_design_scores_gemma":[0.0018673366,0.0010739919,0.03835699,0.000053930395,0.000010382402,0.0000017842755,0.0001265165,0.9452217,0.00032780398,0.009787458,0.003026673,0.00014543283],"about_ca_topic_score_codex":0.0005415053,"about_ca_topic_score_gemma":0.00019500127,"teacher_disagreement_score":0.6361097,"about_ca_system_score_codex":0.00022210281,"about_ca_system_score_gemma":0.000066047265,"threshold_uncertainty_score":0.99808306},"labels":[],"label_agreement":null},{"id":"W2137822637","doi":"10.3137/ao.460201","title":"Satellite‐derived aerosol radiative forcing from the 2004 British Columbia wildfires","year":2008,"lang":"en","type":"article","venue":"ATMOSPHERE-OCEAN","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McGill University","funders":"","keywords":"Shortwave; Radiative forcing; Longwave; Aerosol; Environmental science; Moderate-resolution imaging spectroradiometer; Atmospheric sciences; Radiative transfer; Forcing (mathematics); Climatology; Shortwave radiation; Atmosphere (unit); Satellite; Latitude; Smoke; Longitude; Cloud forcing; Meteorology; Geography; Physics; Radiation; Geology","score_opus":0.0083144306845345,"score_gpt":0.188769065337025,"score_spread":0.1804546346524905,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2137822637","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":[0.9890634,0.0014953633,0.00033661525,0.00024346927,0.00025678062,0.00044882423,0.00003100925,0.00015774857,0.007966783],"genre_scores_gemma":[0.98705184,0.0006839296,0.0034970662,0.0017718414,0.00023887592,0.000012099753,0.00002597378,0.00006819253,0.0066501643],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99752593,0.00012189304,0.00041722207,0.00069844717,0.00055632566,0.000680202],"domain_scores_gemma":[0.99872136,0.00021537278,0.00020453759,0.0006039492,0.000016461983,0.00023831657],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00015458536,0.00027506446,0.00035479118,9.6847366e-8,0.001144329,0.00026034855,0.00069390255,0.00015828476,0.010306486],"category_scores_gemma":[0.000066929584,0.0003005877,0.00018844413,0.00034422913,0.0008023656,0.0003561643,0.00030173382,0.0003089437,0.0005900866],"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":[0.000014605407,0.00007656478,0.88850754,0.000001797396,0.0000500581,0.000094848496,0.0022166315,0.0012364782,0.0002924282,0.0000025539284,0.094357684,0.013148775],"study_design_scores_gemma":[0.00084510335,0.000108808854,0.9749746,0.000041093765,0.000042057593,0.000059608774,0.0010325864,0.0011351946,0.00027873807,0.0005426683,0.02039095,0.00054860587],"about_ca_topic_score_codex":0.23625062,"about_ca_topic_score_gemma":0.046027116,"teacher_disagreement_score":0.1902235,"about_ca_system_score_codex":0.00022547456,"about_ca_system_score_gemma":0.000046409932,"threshold_uncertainty_score":0.9999446},"labels":[],"label_agreement":null},{"id":"W2138884861","doi":"10.1002/qj.416","title":"Intercomparison of model simulations of mixed‐phase clouds observed during the ARM Mixed‐Phase Arctic Cloud Experiment. I: single‐layer cloud","year":2009,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":414,"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":"Liquid water path; Liquid water content; Environmental science; Parametrization (atmospheric modeling); Atmospheric sciences; Cloud physics; Cloud top; Meteorology; Cloud computing; Ice cloud; Physics; Radiative transfer; Optics; Aerosol","score_opus":0.03943777805658623,"score_gpt":0.28137419587353985,"score_spread":0.24193641781695363,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2138884861","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":[0.9881485,0.0002749443,0.009930273,0.000721122,0.00048455456,0.00026747785,0.00001430682,0.000016638927,0.00014217611],"genre_scores_gemma":[0.995022,0.000008904149,0.0043799453,0.00023925214,0.00020627739,0.000003647844,0.0000011172563,0.000017392027,0.000121452875],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9967175,0.00041537083,0.0012838747,0.0003031244,0.0008016535,0.00047846665],"domain_scores_gemma":[0.99768263,0.0002632746,0.001245407,0.0005323546,0.0000805645,0.00019579237],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00081803463,0.00033708516,0.0006840629,0.0000033268261,0.0003410941,0.000041497235,0.0011211936,0.00022049503,0.0005837511],"category_scores_gemma":[0.000087427194,0.00018364434,0.0011079073,0.00030014556,0.0006118989,0.00015463689,0.00015788748,0.0006524371,0.00000506198],"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":[0.0017545479,0.011125408,0.0110026635,0.000052824536,0.0005100736,0.000013551284,0.011056064,0.5046968,0.44149077,0.0003982999,0.0026729077,0.015226094],"study_design_scores_gemma":[0.01741819,0.031668905,0.08481346,0.00029832692,0.0011450388,0.00009427031,0.01056851,0.7293527,0.10368568,0.018843397,0.00071066624,0.0014008108],"about_ca_topic_score_codex":0.000046125206,"about_ca_topic_score_gemma":0.000007849851,"teacher_disagreement_score":0.3378051,"about_ca_system_score_codex":0.0002537962,"about_ca_system_score_gemma":0.000025040217,"threshold_uncertainty_score":0.7488799},"labels":[],"label_agreement":null},{"id":"W2138977661","doi":"10.1029/2001jd001253","title":"Monthly averages of aerosol properties: A global comparison among models, satellite data, and AERONET ground data","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":324,"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","funders":"","keywords":"Aerosol; AERONET; Environmental science; Atmospheric sciences; Total Ozone Mapping Spectrometer; Sea salt; Moderate-resolution imaging spectroradiometer; Optical depth; Satellite; Altitude (triangle); Mass concentration (chemistry); Climatology; Meteorology; Geology; Chemistry; Physics; Stratosphere","score_opus":0.095894248573664,"score_gpt":0.3314308284065712,"score_spread":0.23553657983290716,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2138977661","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":[0.99164337,0.0031253104,0.001061565,0.00011224126,0.0000670882,0.00025078095,0.000054635577,0.000008577173,0.0036764434],"genre_scores_gemma":[0.99273956,0.00066951074,0.0061377254,0.000023488663,0.00009791489,0.0000030148558,0.000010089397,0.000021441821,0.00029728533],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9957902,0.00046550488,0.00073708553,0.0005541917,0.0018096453,0.0006434118],"domain_scores_gemma":[0.9977141,0.00023089492,0.00028215244,0.0012269089,0.00011697772,0.00042898624],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015681548,0.000238494,0.0005776879,0.0000014217896,0.00021771007,0.00014874247,0.001889441,0.00011059462,0.00030033977],"category_scores_gemma":[0.0004658879,0.0001719672,0.00007046509,0.00045589916,0.0013119384,0.0015043622,0.0017294423,0.00063527055,0.000033529606],"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":[0.0021953033,0.0050474717,0.7937096,0.00037043713,0.0008247982,0.00030615338,0.0030296496,0.026092118,0.012887353,0.0021307773,0.057349358,0.096057],"study_design_scores_gemma":[0.0042416016,0.004510604,0.47563165,0.0006871691,0.00025342798,0.00009217947,0.00910128,0.46634957,0.0026430597,0.012582566,0.022567524,0.0013393793],"about_ca_topic_score_codex":0.0041588843,"about_ca_topic_score_gemma":0.0008180838,"teacher_disagreement_score":0.44025743,"about_ca_system_score_codex":0.00015545191,"about_ca_system_score_gemma":0.0001361438,"threshold_uncertainty_score":0.7012619},"labels":[],"label_agreement":null},{"id":"W2139988539","doi":"10.5194/acp-12-6157-2012","title":"Aerosol observations and growth rates downwind of the anvil of a deep tropical thunderstorm","year":2012,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","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","keywords":"Aerosol; Atmospheric sciences; Cloud condensation nuclei; Thunderstorm; Environmental science; Particle (ecology); Climatology; Meteorology; Physics; Geology; Oceanography","score_opus":0.009689271839270671,"score_gpt":0.19967781017519182,"score_spread":0.18998853833592114,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2139988539","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":[0.9957252,0.00019089629,0.0012394695,0.00008322707,0.000022655679,0.000065139255,0.0000039865463,0.0000057028783,0.0026637323],"genre_scores_gemma":[0.99492526,0.000050755152,0.0045387535,0.00006218335,0.000054860982,0.0000051539578,0.0000013445487,0.0000074363434,0.00035427025],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993829,0.0000127016,0.00014715879,0.00012805927,0.00016944566,0.00015974366],"domain_scores_gemma":[0.9996033,0.000044420958,0.00009851369,0.00016923556,0.000012068517,0.000072517694],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000043790526,0.00011057633,0.00014410526,5.604463e-9,0.000095516814,0.0000062701997,0.00011387518,0.000057657682,0.00048481557],"category_scores_gemma":[0.000016143047,0.00007966282,0.000046891782,0.00015112832,0.00045227708,0.00011967584,0.000116846626,0.00008303377,0.0000014458578],"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":[0.000010068851,0.00012663093,0.9425198,0.00005921991,0.000019688177,9.258228e-8,0.0008013859,0.00006371796,0.04989842,0.00029238782,0.00014136254,0.0060672546],"study_design_scores_gemma":[0.0003507745,0.000024873094,0.9301751,0.000016739026,0.00005598748,0.000005092209,0.0004199614,0.0025499202,0.064835176,0.0010611949,0.00032016356,0.00018496854],"about_ca_topic_score_codex":0.00009087553,"about_ca_topic_score_gemma":0.00000385758,"teacher_disagreement_score":0.014936757,"about_ca_system_score_codex":0.000025737761,"about_ca_system_score_gemma":0.000008844951,"threshold_uncertainty_score":0.530839},"labels":[],"label_agreement":null},{"id":"W2140060435","doi":"10.5194/acpd-13-25481-2013","title":"An explicit study of aerosol mass conversion and its parameterization in warm rain formation of cumulus clouds","year":2013,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; Health Canada","funders":"Chinese Academy of Sciences; Natural Sciences and Engineering Research Council of Canada; Institute of Atmospheric Physics, Chinese Academy of Sciences; National Natural Science Foundation of China","keywords":"Aerosol; Atmospheric sciences; Mass concentration (chemistry); Precipitation; Liquid water content; Air mass (solar energy); Environmental science; Meteorology; Chemistry; Cloud computing; Thermodynamics; Physics","score_opus":0.011812307021181256,"score_gpt":0.22950823543456333,"score_spread":0.2176959284133821,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2140060435","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":[0.9958373,0.0000044953313,0.0030684157,0.000020353165,0.00001979617,0.00052124716,6.9621905e-7,0.000009734797,0.0005179835],"genre_scores_gemma":[0.9990524,0.000011248717,0.0007958561,0.00003307673,0.000002966747,0.000021297601,0.0000030495119,0.0000051106563,0.0000750155],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9992863,0.0000508953,0.00025181146,0.00013822402,0.0001683899,0.00010440504],"domain_scores_gemma":[0.9996994,0.000016147544,0.000108902,0.00012124341,0.000009781887,0.000044492474],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000115106195,0.00007432945,0.00012695008,0.0000022181498,0.000026195916,0.000008362626,0.00008770136,0.00004175617,0.0008242451],"category_scores_gemma":[0.000007997266,0.000061626226,0.000011232347,0.00014721227,0.000027860393,0.00048569776,0.00005482829,0.00003259052,0.00002041726],"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":[0.000038925795,0.0006098145,0.261879,0.000034699184,0.000004517761,6.1575935e-7,0.0070657684,0.004685742,0.7211436,0.0000467931,0.000063551546,0.0044269557],"study_design_scores_gemma":[0.0022280582,0.0018175252,0.20594372,0.000019737088,0.000014864884,0.0000013349173,0.01645743,0.5705726,0.20254765,0.00013162813,0.000008649976,0.0002567714],"about_ca_topic_score_codex":0.0011021335,"about_ca_topic_score_gemma":0.00006697302,"teacher_disagreement_score":0.56588686,"about_ca_system_score_codex":0.000030804033,"about_ca_system_score_gemma":0.0000019521492,"threshold_uncertainty_score":0.9024906},"labels":[],"label_agreement":null},{"id":"W2140233185","doi":"10.5194/acp-11-9749-2011","title":"A comprehensive numerical study of aerosol-cloud-precipitation interactions in marine stratocumulus","year":2011,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":82,"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 Calgary; Fund for Innovative Climate and Energy Research; California Institute of Technology","keywords":"Drizzle; Aerosol; Marine stratocumulus; Atmospheric sciences; Sea salt aerosol; Environmental science; Cloud fraction; Precipitation; Entrainment (biomusicology); Troposphere; Cloud base; Cloud computing; Meteorology; Cloud cover; Geology; Physics; Sea salt","score_opus":0.01913327411005895,"score_gpt":0.24693817866225554,"score_spread":0.2278049045521966,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2140233185","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":[0.98621535,0.000008726993,0.0009291384,0.000005299398,0.00004045879,0.0001659107,0.00000135121,0.000016678528,0.012617083],"genre_scores_gemma":[0.99206525,0.0000071282047,0.0073001874,0.000022330389,0.000036525435,0.000027563914,0.0000039642887,0.000011741946,0.00052531785],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991597,0.000025376787,0.0002416744,0.00027041917,0.000141415,0.00016143729],"domain_scores_gemma":[0.9995772,0.000036392492,0.00010230801,0.0002021086,0.000012828627,0.0000691677],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000029936089,0.00015205283,0.00020323583,1.9743403e-8,0.000053798758,0.000008009956,0.000116296935,0.00003368383,0.0037447824],"category_scores_gemma":[0.000004847191,0.00014877782,0.000035232297,0.0002606825,0.00010999684,0.00012421963,0.00013438558,0.00014982116,0.000019765694],"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":[0.00021885848,0.0035016735,0.8246602,0.00006464996,0.0000716236,0.000023049557,0.013292171,0.0036867287,0.027431859,0.000027405988,0.00015877382,0.12686305],"study_design_scores_gemma":[0.0028151555,0.0006575288,0.92408633,0.000038015787,0.000096099575,0.00002103237,0.012666018,0.036504675,0.020343695,0.0015067952,0.00047038417,0.00079425104],"about_ca_topic_score_codex":0.0019516117,"about_ca_topic_score_gemma":0.0000345107,"teacher_disagreement_score":0.12606879,"about_ca_system_score_codex":0.000043629178,"about_ca_system_score_gemma":0.0000075292664,"threshold_uncertainty_score":0.9971659},"labels":[],"label_agreement":null},{"id":"W2140296069","doi":"10.5194/acp-16-799-2016","title":"Observations of cloud microphysics and ice formation during COPE","year":2016,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":85,"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":"Division of Atmospheric and Geospace Sciences; Sight Research UK; University of Manchester; Natural Environment Research Council; Met Office; National Science Foundation","keywords":"Drizzle; Ice nucleus; Atmospheric sciences; Ice crystals; Environmental science; Precipitation; Climatology; Geology; Meteorology; Geography; Chemistry","score_opus":0.006894169443579164,"score_gpt":0.1845828231106939,"score_spread":0.17768865366711475,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2140296069","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":[0.9942737,0.00005116165,0.0038343843,0.00007163255,0.000016645956,0.00005376452,0.0000064184633,0.000016179685,0.0016761171],"genre_scores_gemma":[0.99063796,0.00017397472,0.0069350665,0.00003307398,0.000072953866,0.00000580608,0.0000027244319,0.000009419356,0.0021290327],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9994572,0.0000068562304,0.00014090896,0.00016524662,0.00009967442,0.00013012088],"domain_scores_gemma":[0.99966544,0.000029564135,0.00008872561,0.00014853122,0.000009865578,0.000057859692],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000028422555,0.0001082788,0.00011510627,5.579936e-9,0.000102688995,0.000010022473,0.00007244967,0.000042734406,0.00037593857],"category_scores_gemma":[0.0000058211235,0.000083262996,0.000026116582,0.000107614345,0.00019349469,0.00021661635,0.00008550075,0.000041503376,0.000012157394],"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":[0.000014339682,0.000040443334,0.027747905,0.00006665592,0.0000096522845,6.366711e-7,0.0002629413,0.000075392156,0.9174558,0.00006946788,0.00016757428,0.054089226],"study_design_scores_gemma":[0.0017252679,0.00007459042,0.33665097,0.00014182153,0.000079684476,0.00002478797,0.0003584866,0.0052917674,0.6447963,0.0037751654,0.0063705277,0.00071058195],"about_ca_topic_score_codex":0.000043246124,"about_ca_topic_score_gemma":0.0000010463799,"teacher_disagreement_score":0.30890307,"about_ca_system_score_codex":0.0000315053,"about_ca_system_score_gemma":0.0000049888563,"threshold_uncertainty_score":0.41162637},"labels":[],"label_agreement":null},{"id":"W2140343930","doi":"10.1117/1.3492413","title":"Design, manufacturing, and qualification of an uncooled microbolometer focal plane array–based radiometric package for space applications","year":2010,"lang":"en","type":"article","venue":"Journal of Micro/Nanolithography MEMS and MOEMS","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institut National d'Optique","funders":"","keywords":"Microbolometer; Detector; Radiometry; Optics; Stray light; Cardinal point; Radiation; Radiometric dating; Bolometer; Remote sensing; Materials science; Environmental science; Optoelectronics; Physics; Geology","score_opus":0.00971617276873628,"score_gpt":0.23291178459386191,"score_spread":0.22319561182512562,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2140343930","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":[0.82049435,0.0003011096,0.17863357,0.000096915566,0.000080486745,0.0003316023,0.00001736515,0.000006900672,0.000037702037],"genre_scores_gemma":[0.8939964,0.000118481716,0.10567831,0.000057965746,0.0000673117,0.000020321531,0.0000062262066,0.000017349146,0.000037632337],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99890554,0.000040542414,0.00041905613,0.00023437444,0.00018006658,0.00022041448],"domain_scores_gemma":[0.9989183,0.00012487551,0.00049785775,0.00022500678,0.000034617246,0.00019936507],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006139201,0.00016841489,0.0002934308,0.00005054286,0.00012260997,0.00004231983,0.0001951904,0.00012957401,0.000050688286],"category_scores_gemma":[0.00001562743,0.00013206969,0.000117700576,0.00032201875,0.0002875914,0.00015904284,0.000021875741,0.00018602477,0.0000010858486],"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":[0.00011324517,0.0001995563,0.00649143,0.000026840362,0.00003314841,0.0000012149477,0.00016387843,0.00002289302,0.98152626,0.000018130244,0.0001982278,0.011205195],"study_design_scores_gemma":[0.00160018,0.0010174419,0.103258826,0.000018894334,0.0001227656,0.00013621736,0.00020152106,0.000067360554,0.87945545,0.0005453346,0.013294031,0.00028195468],"about_ca_topic_score_codex":0.0000501501,"about_ca_topic_score_gemma":0.000019969311,"teacher_disagreement_score":0.10207076,"about_ca_system_score_codex":0.000014008403,"about_ca_system_score_gemma":0.000018238858,"threshold_uncertainty_score":0.53856456},"labels":[],"label_agreement":null},{"id":"W2141236778","doi":"10.5194/acp-15-8455-2015","title":"Corrigendum to &amp;quot;In situ vertical profiles of aerosol extinction, mass, and composition over the southeast United States during SENEX and SEAC&amp;lt;sup&amp;gt;4&amp;lt;/sup&amp;gt;RS: observations of a modest aerosol enhancement aloft&amp;quot; published in Atmos. Chem. Phys., 15, 7085–7102, 2015","year":2015,"lang":"en","type":"erratum","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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":"Aerosol; Extinction (optical mineralogy); In situ; Atmospheric sciences; Extinction event; Composition (language); Environmental science; Chemistry; Meteorology; Physics; Mineralogy; Demography; Art; Population","score_opus":0.01894107523356292,"score_gpt":0.2341687742343154,"score_spread":0.21522769900075248,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2141236778","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":[0.99199325,0.00090879324,0.0032870758,0.00032218333,0.00039236053,0.0011042367,0.00033171425,0.00007057966,0.0015898334],"genre_scores_gemma":[0.90137964,0.0016076671,0.025513392,0.00032392397,0.0009568641,0.00060572964,0.008645164,0.00031241172,0.06065522],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.99485093,0.0001890323,0.001358021,0.0014947858,0.00109714,0.0010100743],"domain_scores_gemma":[0.99715877,0.00014888117,0.00065028266,0.0012728466,0.00023652459,0.00053270394],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005109647,0.0011228897,0.0013079594,0.000002176265,0.00038486926,0.00023520335,0.0006041436,0.0006914935,0.0011283072],"category_scores_gemma":[0.00012218778,0.0010188771,0.00018910842,0.0013732666,0.0010177329,0.00056091236,0.0006544771,0.0010748642,0.000039259092],"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":[0.0009474232,0.0021353036,0.030912675,0.0019782535,0.00044094116,0.0000061719925,0.01253679,0.019843506,0.8009839,0.0000252654,0.12870921,0.001480589],"study_design_scores_gemma":[0.029810503,0.0013480377,0.12476339,0.01081401,0.004161528,0.00032891452,0.0106986,0.09945151,0.10343701,0.0042445497,0.5901275,0.020814436],"about_ca_topic_score_codex":0.0010999773,"about_ca_topic_score_gemma":0.0010517607,"teacher_disagreement_score":0.6975469,"about_ca_system_score_codex":0.00050615834,"about_ca_system_score_gemma":0.00019840697,"threshold_uncertainty_score":0.99978477},"labels":[],"label_agreement":null},{"id":"W2141721644","doi":"10.1175/jam2267.1","title":"Optical Properties of Aerosol Particles over the Northeast Pacific","year":2005,"lang":"en","type":"article","venue":"Journal of Applied Meteorology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":8,"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; Environment and Climate Change Canada; Dalhousie University","funders":"","keywords":"Nephelometer; Aerosol; Scattering; Mie scattering; Particle (ecology); Absorption (acoustics); Wavelength; Particle-size distribution; Atmospheric sciences; Sea salt; Single-scattering albedo; Light scattering; Environmental science; Particle size; Materials science; Optics; Physics; Meteorology; Chemistry; Geology; Oceanography","score_opus":0.009904098684292807,"score_gpt":0.20220161087679575,"score_spread":0.19229751219250293,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2141721644","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":[0.9918412,0.00011879225,0.0002653921,0.0011611556,0.000063531515,0.000087678105,3.9699597e-7,0.0000046166942,0.0064572426],"genre_scores_gemma":[0.99597085,0.00003063038,0.0035074262,0.00028709508,0.00013026928,0.00000487722,5.4671617e-8,0.000009209608,0.00005956667],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99894863,0.000031478135,0.00041857973,0.0001042116,0.00027295068,0.00022416146],"domain_scores_gemma":[0.99941957,0.000043651642,0.00027796297,0.0001657043,0.000013413911,0.000079676414],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038778878,0.00010009831,0.00023615241,0.0000019127967,0.000068622474,0.000009185027,0.0002464744,0.000066062734,0.00077454676],"category_scores_gemma":[0.00001813559,0.000053588705,0.000088567554,0.00009773759,0.00053369306,0.00007252628,0.00009289064,0.00019161784,0.0000683201],"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":[0.0013214853,0.000629464,0.051259812,0.000014403832,0.0001747289,0.00001298061,0.0032292295,0.008647096,0.8274702,0.003856563,0.0030321518,0.10035187],"study_design_scores_gemma":[0.0062812013,0.0029684673,0.28699207,0.000053082294,0.00069066504,0.00070974045,0.007253041,0.005340978,0.60482496,0.0047271773,0.079042666,0.0011159702],"about_ca_topic_score_codex":0.000007500815,"about_ca_topic_score_gemma":0.00001702802,"teacher_disagreement_score":0.23573226,"about_ca_system_score_codex":0.00003621263,"about_ca_system_score_gemma":0.000017288088,"threshold_uncertainty_score":0.8480744},"labels":[],"label_agreement":null},{"id":"W2142432986","doi":"10.1029/2003je002219","title":"MATADOR 2002: A pilot field experiment on convective plumes and dust devils","year":2004,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":167,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Optech (Canada)","funders":"","keywords":"Mars Exploration Program; Martian; Environmental science; Atmospheric sciences; Mineral dust; Aeolian processes; Dust storm; Storm; Astrobiology; Geology; Aerosol; Meteorology; Physics; Oceanography","score_opus":0.030708636584455593,"score_gpt":0.3189400610206815,"score_spread":0.2882314244362259,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2142432986","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":[0.98952687,0.00029293203,0.00038973472,0.001554602,0.00007845478,0.00019485943,0.0000013568545,0.000009556936,0.007951617],"genre_scores_gemma":[0.99581295,0.00012565109,0.0021701162,0.00031713012,0.00024034806,0.000012266575,1.5056426e-7,0.000018434113,0.0013029358],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9976051,0.00012798137,0.00031569196,0.00027223164,0.0011682626,0.0005107227],"domain_scores_gemma":[0.9987703,0.00042622082,0.00013310662,0.00021276799,0.00007024438,0.00038738069],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00045270866,0.0001740217,0.00029442698,0.0000018276505,0.00023229135,0.00009054221,0.00034603078,0.00006523202,0.002723944],"category_scores_gemma":[0.00033017749,0.00012468423,0.000095286356,0.00027243566,0.0004571136,0.00024583036,0.000265372,0.00066635397,0.00042101485],"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":[0.016106201,0.017341327,0.092100926,0.00022016444,0.0011531576,0.003559747,0.011780548,0.008650369,0.30912355,0.029378012,0.24144727,0.26913875],"study_design_scores_gemma":[0.010842339,0.06309802,0.64919263,0.00086020655,0.000087996516,0.0002476352,0.009228198,0.00088111154,0.18851838,0.040864944,0.034700878,0.001477647],"about_ca_topic_score_codex":0.0012817411,"about_ca_topic_score_gemma":0.00007477353,"teacher_disagreement_score":0.5570917,"about_ca_system_score_codex":0.00029567664,"about_ca_system_score_gemma":0.0000808788,"threshold_uncertainty_score":0.9981877},"labels":[],"label_agreement":null},{"id":"W2142539941","doi":"10.1175/2009mwr2745.1","title":"Using ARM Observations to Evaluate Cloud and Clear-Sky Radiation Processes as Simulated by the Canadian Regional Climate Model GEM","year":2009,"lang":"en","type":"article","venue":"Monthly Weather Review","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Université du Québec à Montréal","funders":"","keywords":"Overcast; Environmental science; Downwelling; Shortwave; Sky; Shortwave radiation; Atmospheric sciences; Longwave; Climatology; Cloud fraction; Cloud cover; Radiation; Water vapor; Meteorology; Radiative transfer; Geology; Cloud computing; Physics; Upwelling","score_opus":0.05251693494784086,"score_gpt":0.2971540297677524,"score_spread":0.24463709481991153,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2142539941","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":[0.8995654,0.06639644,0.00036686746,0.022466129,0.00005818941,0.0020440053,0.00003872776,0.00007173181,0.008992499],"genre_scores_gemma":[0.95270365,0.013894664,0.0017214388,0.030630834,0.00004560816,0.00003052167,0.000025685478,0.000031034982,0.0009165553],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99884987,0.000058630732,0.00023467917,0.00028188765,0.00027160102,0.00030330967],"domain_scores_gemma":[0.9994265,0.00002051137,0.00009072777,0.00023860994,0.00002453374,0.00019913971],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035421053,0.0001597531,0.00018263562,0.0000016776416,0.0004326098,0.00005781619,0.00018848521,0.00005089594,0.00023136943],"category_scores_gemma":[0.000060209084,0.00011374012,0.000039817598,0.00035691218,0.00005391362,0.00014806587,0.000036235393,0.00009165133,0.00009582964],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000070339585,0.0002556944,0.011107887,0.0003765439,0.000055584493,0.0000100144125,0.0027149841,0.7713672,0.0007091342,0.0008339532,0.063091554,0.14940713],"study_design_scores_gemma":[0.00044260785,0.00024491467,0.017932147,0.00094875274,0.00025220946,0.00001212837,0.000072125826,0.60041595,0.000028348344,0.0021448338,0.37680817,0.0006977858],"about_ca_topic_score_codex":0.013790125,"about_ca_topic_score_gemma":0.011157357,"teacher_disagreement_score":0.31371662,"about_ca_system_score_codex":0.00022096466,"about_ca_system_score_gemma":0.00007730719,"threshold_uncertainty_score":0.9927771},"labels":[],"label_agreement":null},{"id":"W2144983649","doi":"10.1002/qj.2126","title":"Parametrization of instantaneous global horizontal irradiance: clear‐sky component","year":2013,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":24,"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; Environment and Climate Change Canada","funders":"","keywords":"Parametrization (atmospheric modeling); Radiative transfer; Albedo (alchemy); Sky; Atmospheric radiative transfer codes; Irradiance; Environmental science; Single-scattering albedo; Diffuse sky radiation; Radiance; Meteorology; Physics; Scattering; Optics","score_opus":0.005307901118892154,"score_gpt":0.19522568591487066,"score_spread":0.1899177847959785,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2144983649","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":[0.9952866,0.000111890964,0.002397141,0.00047839055,0.0003021907,0.00018083066,0.0000049742926,0.000010493504,0.001227509],"genre_scores_gemma":[0.9936281,0.000013055303,0.005873454,0.0003313072,0.00007371228,0.0000029507041,4.3850616e-7,0.000006722054,0.00007026649],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998255,0.00016344467,0.0005454693,0.0001644575,0.00058302534,0.00028856946],"domain_scores_gemma":[0.99897605,0.00008047459,0.0005566394,0.00018967885,0.00003868951,0.00015845364],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00033783593,0.0001597218,0.000324539,8.1971615e-7,0.00014594203,0.00003517586,0.0005681326,0.00015954992,0.0017334418],"category_scores_gemma":[0.000038684248,0.00008996523,0.00048599023,0.00027815168,0.00042471598,0.00012302666,0.00008300197,0.00029481362,0.00006199463],"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":[0.0007085412,0.0021247354,0.5996239,0.000047470843,0.00061037607,0.00005590962,0.002952389,0.026155658,0.024293508,0.0016240772,0.032921895,0.30888152],"study_design_scores_gemma":[0.0012303937,0.006601507,0.9677027,0.00003059972,0.00011659126,0.0001504145,0.0015662602,0.014091298,0.00025540194,0.0061418065,0.0017772807,0.00033573224],"about_ca_topic_score_codex":0.00025745004,"about_ca_topic_score_gemma":0.000006760513,"teacher_disagreement_score":0.3680788,"about_ca_system_score_codex":0.00021964387,"about_ca_system_score_gemma":0.000016109236,"threshold_uncertainty_score":0.9991791},"labels":[],"label_agreement":null},{"id":"W2146262226","doi":"","title":"Global, Multi-Year Analysis of Clouds and Earth's Radiant Energy System Terra Observations and Radiative Transfer Calculations","year":2005,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"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":"Atmosphere (unit); Radiative transfer; Environmental science; Radiative forcing; Aerosol; Forcing (mathematics); Climate model; Earth's energy budget; Radiant energy; Meteorology; Atmospheric radiative transfer codes; Remote sensing; Atmospheric sciences; Radiation; Geology; Physics; Climate change","score_opus":0.013371978523832763,"score_gpt":0.2178181649415174,"score_spread":0.20444618641768464,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2146262226","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":[0.9120524,0.00012258619,0.08341993,0.00019729222,0.0000147294795,0.00008580461,0.000072053685,0.00002650576,0.0040087346],"genre_scores_gemma":[0.9874799,0.000052381336,0.011833357,0.000116675095,0.000011735364,0.000008248235,0.000009188637,0.00000502267,0.0004834514],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99921674,0.000034280773,0.00021500365,0.0002241079,0.00016718736,0.00014268076],"domain_scores_gemma":[0.99967563,0.000025042102,0.000031525244,0.00014067756,0.000011283388,0.00011586328],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008320799,0.00010475075,0.00020313016,0.0000035956502,0.000114674614,0.000017009846,0.00006272742,0.000055797886,0.0006385043],"category_scores_gemma":[0.0000060872894,0.00008761715,0.000064642925,0.00058892,0.00016466205,0.0001361604,0.000035420464,0.000025408737,0.0000036328502],"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":[0.000012519723,0.000116361494,0.89349765,0.000009274219,0.0004265529,0.0000016689427,0.0011597609,0.075340055,0.00090066233,0.019527763,0.00028179376,0.008725925],"study_design_scores_gemma":[0.00025618455,0.000017362334,0.69326335,0.0000030067615,0.00019868708,0.0000011965049,0.00039868255,0.30423602,0.000048416852,0.000003949259,0.0014838077,0.00008934553],"about_ca_topic_score_codex":0.0033126965,"about_ca_topic_score_gemma":0.0058553834,"teacher_disagreement_score":0.22889598,"about_ca_system_score_codex":0.00008420345,"about_ca_system_score_gemma":0.000009664948,"threshold_uncertainty_score":0.6991174},"labels":[],"label_agreement":null},{"id":"W2147372260","doi":"10.1088/1748-9326/3/4/045021","title":"Dispersion bias, dispersion effect, and the aerosol–cloud conundrum","year":2008,"lang":"en","type":"article","venue":"Environmental Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":110,"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":"U.S. Department of Energy","keywords":"Radiative forcing; Aerosol; Cloud forcing; Atmospheric sciences; Cloud albedo; Dispersion (optics); Liquid water content; Environmental science; Shortwave; Radiative transfer; Albedo (alchemy); Effective radius; Forcing (mathematics); Climate model; Cloud computing; Climate change; Meteorology; Physics; Cloud cover; Optics; Geology; Astrophysics","score_opus":0.018221104670111544,"score_gpt":0.24767861011890482,"score_spread":0.2294575054487933,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2147372260","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":[0.99183446,0.00041710882,0.000101739926,0.005299627,0.00012496504,0.0006567328,0.000005562688,0.000027272894,0.0015325438],"genre_scores_gemma":[0.9952415,0.0010460517,0.00012995278,0.0013374914,0.00011922788,0.000060724604,0.000010559505,0.000032973152,0.002021496],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9965127,0.0006513494,0.00021522932,0.00057731825,0.0013071396,0.00073624274],"domain_scores_gemma":[0.99866724,0.00054877513,0.000056378445,0.00046397594,0.0000011987295,0.00026244723],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":["sts","insufficient_payload"],"category_scores_codex":[0.0011909899,0.00024568534,0.00023229774,0.000005001293,0.0013289236,0.000051610918,0.00043814495,0.0000799884,0.0024548885],"category_scores_gemma":[0.00007786519,0.00015429557,0.000118424745,0.00019280954,0.0053860573,0.00021578849,0.0009547177,0.00055028877,0.0016031974],"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":[0.0007661431,0.00021009137,0.7706533,0.000014590151,0.00004281211,0.00018685768,0.0020927477,0.00022764751,0.15540862,0.000057988924,0.059029415,0.01130975],"study_design_scores_gemma":[0.012137721,0.0012663684,0.8615749,0.00007453967,0.000064456755,0.0004056372,0.0020040828,0.0043258155,0.025081994,0.00012443232,0.09151863,0.0014214535],"about_ca_topic_score_codex":0.0004417443,"about_ca_topic_score_gemma":0.0000119486385,"teacher_disagreement_score":0.13032663,"about_ca_system_score_codex":0.00035829787,"about_ca_system_score_gemma":0.0000048083552,"threshold_uncertainty_score":0.9999712},"labels":[],"label_agreement":null},{"id":"W2147385407","doi":"10.5194/amt-4-2685-2011","title":"Inversion of tropospheric profiles of aerosol extinction and HCHO and NO <sub>2</sub> mixing ratios from MAX-DOAS observations in Milano during the summer of 2003 and comparison with independent data sets","year":2011,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":195,"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":"Goddard Space Flight Center; Max-Planck-Gesellschaft; Strong; National Aeronautics and Space Administration","keywords":"Aerosol; Trace gas; Troposphere; AERONET; Mixing ratio; Inversion (geology); Atmospheric sciences; Radiative transfer; Environmental science; Meteorology; Chemistry; Physics; Geology; Optics","score_opus":0.049045757862230116,"score_gpt":0.22603402074803536,"score_spread":0.17698826288580524,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2147385407","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":[0.99513215,0.00040936033,0.0033641157,0.000018735123,0.000020825293,0.0007282749,0.000008785956,0.000025824527,0.0002919214],"genre_scores_gemma":[0.9462386,0.0003864407,0.053271703,0.000021951508,0.0000058709984,0.000041954387,0.0000085717475,0.00001680075,0.000008138483],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983545,0.000104478,0.00047776967,0.00038585742,0.00050620467,0.00017120778],"domain_scores_gemma":[0.9990119,0.000025047953,0.0004182094,0.00042469107,0.00006656919,0.000053591346],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044207633,0.00019575735,0.0003191994,0.0000010657734,0.000093759714,0.0000115443445,0.00022245258,0.00008627472,0.00008043331],"category_scores_gemma":[0.000046920282,0.0001443727,0.000015764153,0.00031502868,0.00034811877,0.00030449618,0.000352468,0.00012792347,6.10425e-7],"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":[0.000097190416,0.00010967549,0.7138636,0.000047678266,0.000024154804,6.379885e-7,0.0006960673,0.000015932445,0.28217033,0.0000020736538,0.00016557534,0.0028070626],"study_design_scores_gemma":[0.00046585465,0.00026313946,0.69409716,0.0001630762,0.00006269512,0.0000020241087,0.00063843624,0.0033238735,0.3007283,0.000032998872,0.000047581052,0.00017484669],"about_ca_topic_score_codex":0.0035497164,"about_ca_topic_score_gemma":0.0014904118,"teacher_disagreement_score":0.049907587,"about_ca_system_score_codex":0.00006381111,"about_ca_system_score_gemma":0.000020652264,"threshold_uncertainty_score":0.58873475},"labels":[],"label_agreement":null},{"id":"W2147599079","doi":"10.1364/ol.36.003419","title":"Aerosol lenses propagation model","year":2011,"lang":"en","type":"article","venue":"Optics Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Defence Research and Development Canada; Agriculture Environmental Renewal Canada (Canada)","funders":"","keywords":"Optics; Optical transfer function; Irradiance; Point spread function; Monte Carlo method; Aerosol; Fourier transform; Physics; Atmospheric optics; Meteorology","score_opus":0.02174255019563177,"score_gpt":0.19720980312141304,"score_spread":0.17546725292578128,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2147599079","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":[0.9090598,0.0000024417495,0.05348136,0.00036744354,0.00005822452,0.000091657545,7.7703623e-7,0.0000392981,0.03689899],"genre_scores_gemma":[0.93248624,0.0000048087786,0.064548686,0.002101196,0.000019365869,0.000010511634,0.0000013153623,0.000012747953,0.0008151371],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9993896,0.000008600895,0.000099725316,0.00016733387,0.00015358861,0.00018113908],"domain_scores_gemma":[0.9997305,0.000004341698,0.00004118511,0.00016904433,0.000002671426,0.000052248542],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00004932755,0.0000860776,0.0000614004,5.503658e-7,0.00007427378,0.000012250745,0.00012775017,0.000031533527,0.00054351316],"category_scores_gemma":[0.0000055567675,0.00007564427,0.000030145075,0.000060752805,0.00012085406,0.0001267491,0.000068195186,0.000062128805,0.0004339825],"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":[0.000051121886,0.00026456313,0.045365334,0.000015370993,0.000028767156,0.00003741785,0.00518821,0.050930746,0.85685277,0.0019856154,0.030377984,0.008902128],"study_design_scores_gemma":[0.0017947463,0.00054072967,0.072138816,0.00005068687,0.00016456151,0.000045443194,0.00062693725,0.7721102,0.14520484,0.0032317773,0.0015876951,0.0025035487],"about_ca_topic_score_codex":0.000052785712,"about_ca_topic_score_gemma":0.0000066055327,"teacher_disagreement_score":0.7211795,"about_ca_system_score_codex":0.00004249744,"about_ca_system_score_gemma":0.00000331528,"threshold_uncertainty_score":0.5951088},"labels":[],"label_agreement":null},{"id":"W2148104872","doi":"10.1029/2002gl016606","title":"Optical and meteorological properties of smoke‐dominated haze at the ARM Southern Great Plains Central Facility","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Oceanic and Atmospheric Administration; Killam Trusts; Dalhousie University; U.S. Department of Energy","keywords":"Haze; Environmental science; Single-scattering albedo; Atmospheric sciences; Smoke; Angstrom exponent; Radiative forcing; Aerosol; Cloud cover; Albedo (alchemy); Precipitation; Climatology; Shortwave; Forcing (mathematics); Liquid water path; Optical depth; Shortwave radiation; Radiative transfer; Meteorology; Geology; Radiation; Physics; Cloud computing","score_opus":0.037318030740446075,"score_gpt":0.2583645664209935,"score_spread":0.2210465356805474,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2148104872","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":[0.99523723,0.00004376541,0.00007173696,0.0031776666,0.000022781045,0.0002951179,0.000012317479,0.000015151994,0.0011242154],"genre_scores_gemma":[0.99864244,0.000008447647,0.00011150812,0.00035464778,0.00002048627,0.000030148918,0.0000018596303,0.000007736832,0.0008226934],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9973787,0.00044219306,0.0001838405,0.00040991226,0.0008198221,0.0007655367],"domain_scores_gemma":[0.99923253,0.00018930917,0.000030773277,0.00031548616,0.000015991247,0.00021592069],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006010467,0.00015214889,0.00020965144,0.0000019670924,0.00032568417,0.000034653487,0.00027671902,0.0000734648,0.0011813574],"category_scores_gemma":[0.00032208956,0.00008371007,0.000085687716,0.00022151046,0.0032738047,0.00006254884,0.0004136784,0.00041926216,0.0002734066],"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":[0.0006615324,0.00056744396,0.076143816,0.000037871865,0.00007403433,0.000054748758,0.002573195,0.00031925194,0.9052271,0.00095677853,0.004209771,0.009174445],"study_design_scores_gemma":[0.002889028,0.0017289962,0.76583654,0.000049310052,0.0000842314,0.000037796144,0.0036377723,0.003155597,0.20152304,0.002005081,0.017955797,0.0010968355],"about_ca_topic_score_codex":0.0009213338,"about_ca_topic_score_gemma":0.00006839301,"teacher_disagreement_score":0.70370406,"about_ca_system_score_codex":0.00014273453,"about_ca_system_score_gemma":0.000013817804,"threshold_uncertainty_score":0.9997317},"labels":[],"label_agreement":null},{"id":"W2148403247","doi":"10.1109/igarss.1989.579073","title":"Lidar Studies Of Atmospheric Extinction","year":2005,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Lidar; Remote sensing; Environmental science; Extinction (optical mineralogy); Computer science; Geology; Physics; Optics","score_opus":0.014710920324945063,"score_gpt":0.25419401478733755,"score_spread":0.2394830944623925,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2148403247","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":[0.92194295,0.0002010435,0.0016301832,0.0002352245,0.000052845247,0.00004890471,1.3296805e-7,0.00003087749,0.075857826],"genre_scores_gemma":[0.9615861,0.00008074298,0.028331202,0.00019320784,0.000041099396,0.0000043695686,1.5487095e-7,0.000005149107,0.009757941],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99949664,0.000009496989,0.00013138822,0.000118931224,0.00013548699,0.00010805256],"domain_scores_gemma":[0.9997904,0.000014491112,0.000046586858,0.00011440405,0.000004851528,0.000029272378],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00006960067,0.00006232102,0.00009225909,6.83801e-8,0.000044840785,0.0000027084955,0.00007251556,0.000022794156,0.010573928],"category_scores_gemma":[0.000011565386,0.00004629888,0.00003280386,0.00011745711,0.000121917496,0.000097623386,0.00008292046,0.000028801825,0.00058791507],"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":[0.000031285963,0.00029593782,0.376863,0.000016035834,0.00006576235,0.0000022301583,0.0020255828,0.010780355,0.023295771,0.0005706676,0.030060736,0.55599266],"study_design_scores_gemma":[0.00097538554,0.0005209006,0.5079709,0.00002020128,0.000062484876,0.000014026388,0.0057632853,0.011449248,0.027007692,0.0010869525,0.4444703,0.00065857853],"about_ca_topic_score_codex":0.00005753571,"about_ca_topic_score_gemma":0.00007075986,"teacher_disagreement_score":0.5553341,"about_ca_system_score_codex":0.000059189308,"about_ca_system_score_gemma":0.000002126678,"threshold_uncertainty_score":0.9903305},"labels":[],"label_agreement":null},{"id":"W2148619832","doi":"10.5194/acp-11-11859-2011","title":"On the discrepancies between theoretical and measured below-cloud particle scavenging coefficients for rain – a numerical investigation using a detailed one-dimensional cloud microphysics model","year":2011,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":36,"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":"Scavenging; Aerosol; Diffusion; Particle (ecology); Turbulent diffusion; Atmospheric sciences; Precipitation; Meteorology; Turbulence; Liquid water content; Environmental science; Chemistry; Cloud computing; Physics; Thermodynamics; Geology","score_opus":0.023647255057016592,"score_gpt":0.2167722481154761,"score_spread":0.1931249930584595,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2148619832","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":[0.9032628,0.000020415702,0.096147,0.00011326859,0.000020597223,0.00020943342,0.000010496719,0.000025592135,0.00019043313],"genre_scores_gemma":[0.9727596,0.0000027705278,0.02677962,0.00020829157,0.000112146656,0.000025372592,0.0000067422884,0.000025676463,0.000079772675],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9988004,0.00003963323,0.00020068284,0.0003823103,0.00025854463,0.00031840298],"domain_scores_gemma":[0.9993543,0.00016431717,0.000091249254,0.0002170569,0.000018369828,0.00015471475],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019996209,0.00022068838,0.00021898169,2.6838231e-8,0.00041035266,0.00003610364,0.00013254427,0.00007824938,0.00013175547],"category_scores_gemma":[0.000044118235,0.00016953438,0.000069941634,0.0001614232,0.0007562333,0.00007797381,0.00012189112,0.0001470376,0.0000053270537],"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":[0.0010362173,0.001472279,0.15868849,0.00028352404,0.00049488066,0.0000078895855,0.014407935,0.101553224,0.61173594,0.05413007,0.0005060542,0.055683497],"study_design_scores_gemma":[0.00048350758,0.000060376646,0.0022985286,0.000039159477,0.000108399894,0.0000022825136,0.00015127382,0.9099634,0.03883824,0.04773557,0.000013485254,0.00030575486],"about_ca_topic_score_codex":0.00003207093,"about_ca_topic_score_gemma":4.4076756e-7,"teacher_disagreement_score":0.80841017,"about_ca_system_score_codex":0.000057929716,"about_ca_system_score_gemma":0.000023170936,"threshold_uncertainty_score":0.69134116},"labels":[],"label_agreement":null},{"id":"W2149848905","doi":"10.1029/2010jd015238","title":"Cloud radar Doppler spectra in drizzling stratiform clouds: 2. Observations and microphysical modeling of drizzle evolution","year":2011,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":80,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Drizzle; Doppler effect; Radar; Meteorology; Environmental science; Remote sensing; Geology; Physics; Astronomy; Precipitation; Computer science","score_opus":0.057156927610089274,"score_gpt":0.2867793755780023,"score_spread":0.22962244796791303,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2149848905","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":[0.99277556,0.00016674379,0.0050410894,0.00009535852,0.00007409314,0.00016995301,0.0000030448819,0.000006622173,0.0016675254],"genre_scores_gemma":[0.981097,0.0000937318,0.01844408,0.000014110643,0.00021850837,0.0000043195196,5.2138563e-7,0.000020258116,0.00010745814],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.997182,0.0001613189,0.0006768691,0.0002660681,0.0011912901,0.00052245735],"domain_scores_gemma":[0.99896395,0.00017502489,0.00022275843,0.00023094738,0.00016690014,0.00024042239],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009292833,0.00017343968,0.00038908323,0.0000045822217,0.00015388786,0.00003242368,0.00040305516,0.00010027676,0.00037775328],"category_scores_gemma":[0.00020714391,0.00014065548,0.00014072125,0.0006224599,0.0005071712,0.00045982172,0.00023622268,0.0007572416,0.000018954615],"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":[0.0031178978,0.005779431,0.4066564,0.00019323277,0.0002914295,0.00030170433,0.011770699,0.022115927,0.48005334,0.04926277,0.0032967683,0.017160388],"study_design_scores_gemma":[0.0024115264,0.0034539052,0.6626155,0.00037474476,0.00006338836,0.000055104578,0.0055667637,0.19451943,0.007515189,0.12246605,0.00032764327,0.00063079275],"about_ca_topic_score_codex":0.0048426823,"about_ca_topic_score_gemma":0.00052287383,"teacher_disagreement_score":0.47253814,"about_ca_system_score_codex":0.0003144396,"about_ca_system_score_gemma":0.00014562768,"threshold_uncertainty_score":0.73207194},"labels":[],"label_agreement":null},{"id":"W2150230102","doi":"10.1175/jas-d-11-012.1","title":"Experimental Study of Collection Efficiencies between Submicron Aerosols and Cloud Droplets","year":2011,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":59,"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","funders":"","keywords":"Aerosol; RADIUS; Evaporation; Nucleation; Laminar flow; Cloud chamber; Particle (ecology); Relative humidity; Materials science; Ice nucleus; Cloud physics; Mechanics; Analytical Chemistry (journal); Physics; Chemistry; Meteorology; Thermodynamics; Geology; Chromatography; Nuclear physics; Cloud computing","score_opus":0.028254561088494893,"score_gpt":0.24180818147142602,"score_spread":0.21355362038293113,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2150230102","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":[0.99764055,0.00021916904,0.00006798357,0.00004901575,0.00056162,0.00019993856,3.1428468e-7,0.0000059418585,0.0012554938],"genre_scores_gemma":[0.9969682,0.000011839376,0.0027218857,0.000038552673,0.000071552175,0.0000022932757,1.2691081e-8,0.000006642449,0.00017900784],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983246,0.00012251826,0.00045471042,0.00020012673,0.00067237276,0.00022569603],"domain_scores_gemma":[0.9990444,0.000058988928,0.0006201205,0.00016808022,0.000022013985,0.00008635208],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00077105005,0.00013736679,0.00026103837,9.736582e-7,0.00044185782,0.00003273961,0.00070072134,0.000040117164,0.00034527626],"category_scores_gemma":[0.00004455151,0.00008020706,0.00008428853,0.0007653212,0.0009781959,0.0002663264,0.00031615316,0.00012287735,0.0000042657557],"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":[0.00003713356,0.00057655264,0.9693504,0.000002301173,0.0000216202,0.0000028056993,0.011129329,0.0006639555,0.016951092,0.00001009958,0.00083201897,0.00042269705],"study_design_scores_gemma":[0.00075301,0.004386698,0.9438168,0.000026370164,0.00006623616,0.00006923266,0.024245687,0.0005690125,0.025606962,0.00011078779,0.00015532953,0.00019386908],"about_ca_topic_score_codex":0.0006499098,"about_ca_topic_score_gemma":0.000024074268,"teacher_disagreement_score":0.02553359,"about_ca_system_score_codex":0.00008417945,"about_ca_system_score_gemma":0.00003873719,"threshold_uncertainty_score":0.3780533},"labels":[],"label_agreement":null},{"id":"W2150313828","doi":"10.1029/2001gl014153","title":"Time‐series of zenith radiance and surface flux under cloudy skies: Radiative smoothing, optical thickness retrievals and large‐scale stationarity","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"York University","funders":"","keywords":"Radiance; Radiative transfer; Zenith; Radiative flux; Smoothing; Environmental science; Atmospheric radiative transfer codes; Scale (ratio); Flux (metallurgy); Solar zenith angle; Remote sensing; Physics; Atmospheric sciences; Optics; Geology; Materials science; Mathematics","score_opus":0.020086143471273712,"score_gpt":0.2716430817623174,"score_spread":0.2515569382910437,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2150313828","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":[0.99107605,0.000109924586,0.00082403223,0.0061354,0.000022755938,0.00025794498,0.000025879306,0.000020229954,0.0015277995],"genre_scores_gemma":[0.99343973,0.00008362419,0.0029423728,0.0005620828,0.000051285857,0.000009199542,0.0000049923656,0.000019254196,0.0028874422],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99758816,0.00026609324,0.00020589262,0.000462703,0.0008906563,0.0005864995],"domain_scores_gemma":[0.998767,0.000636333,0.00005724147,0.00024815975,0.000035631172,0.0002555977],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00059492275,0.00016225364,0.0002682899,0.0000042067923,0.0003269426,0.00006325465,0.00020912684,0.00008338167,0.0011752229],"category_scores_gemma":[0.00020757805,0.0001426846,0.000041661984,0.00040374792,0.0023660862,0.00035604133,0.0003273891,0.00045894465,0.00023516158],"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":[0.0013460878,0.0029738287,0.16094005,0.0004731106,0.00041747274,0.00020037557,0.07844114,0.0060618217,0.5236472,0.012762711,0.19686705,0.015869187],"study_design_scores_gemma":[0.0028569659,0.0011596261,0.91590554,0.00011122328,0.00005394106,0.000017202325,0.006637959,0.044637706,0.0067776856,0.008599949,0.012119179,0.0011230538],"about_ca_topic_score_codex":0.00027681197,"about_ca_topic_score_gemma":0.00001897308,"teacher_disagreement_score":0.7549655,"about_ca_system_score_codex":0.00009538757,"about_ca_system_score_gemma":0.000012548072,"threshold_uncertainty_score":0.99973786},"labels":[],"label_agreement":null},{"id":"W2150966988","doi":"10.1029/1999gl011098","title":"Why is the cloud albedo — Particle size relationship different in optically thick and optically thin clouds?","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","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":"Dalhousie University","funders":"","keywords":"Liquid water content; Albedo (alchemy); Cloud albedo; Effective radius; Adiabatic process; Sign (mathematics); RADIUS; Atmospheric sciences; Environmental science; Cloud computing; Cloud fraction; Materials science; Physics; Cloud cover; Astrophysics; Thermodynamics; Mathematics","score_opus":0.022883426043441568,"score_gpt":0.2792280906991944,"score_spread":0.25634466465575284,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2150966988","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":[0.89832574,0.0000196006,0.0000616282,0.09906135,0.000029920742,0.00032739763,0.0000020125258,0.000024457204,0.0021478897],"genre_scores_gemma":[0.9879692,0.000036632886,0.00043749993,0.0102336025,0.00013604411,0.00006160482,9.88169e-7,0.000021067992,0.0011033231],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9967367,0.00045402028,0.00028286988,0.00053562195,0.0010995261,0.0008912809],"domain_scores_gemma":[0.99709797,0.0020735213,0.000024532588,0.000495263,0.0000123000755,0.000296422],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0007240685,0.00019045267,0.00020056513,0.0000022191198,0.00040326998,0.00015541246,0.00049487175,0.00009177527,0.0036977737],"category_scores_gemma":[0.0004261812,0.00012492633,0.0000798525,0.00049194,0.0013738048,0.00017266521,0.0003564541,0.0009764434,0.0012898362],"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":[0.0016523725,0.0024745644,0.6970995,0.00007142921,0.00011841484,0.00030595725,0.01895322,0.002987776,0.067340456,0.022713749,0.1527284,0.033554174],"study_design_scores_gemma":[0.0005575111,0.00018701982,0.9792394,0.000023300285,0.000009943253,0.0000034853877,0.00025827726,0.008379219,0.00038241906,0.006317214,0.0043978626,0.0002443675],"about_ca_topic_score_codex":0.0011651078,"about_ca_topic_score_gemma":0.00013441005,"teacher_disagreement_score":0.2821399,"about_ca_system_score_codex":0.00013493,"about_ca_system_score_gemma":0.000012936477,"threshold_uncertainty_score":0.99948776},"labels":[],"label_agreement":null},{"id":"W2152092660","doi":"10.1109/micrad.2008.4579473","title":"A compact airborne G-band (183 GHz) water Vapor Radiometer and retrievals of liquid cloud parameters from coincident radiometer and millimeter wave radar measurements","year":2008,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"National Research Council Canada","funders":"","keywords":"Radiometer; Remote sensing; Water vapor; Environmental science; Radar; Liquid water content; Brightness temperature; Zenith; Effective radius; Liquid water path; Extremely high frequency; W band; Microwave radiometer; Millimeter; Meteorology; Brightness; Optics; Physics; Cloud computing; Geology; Aerosol; Telecommunications; Computer science","score_opus":0.038044432976429385,"score_gpt":0.22209742099148483,"score_spread":0.18405298801505543,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2152092660","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":[0.99659854,0.0005291881,0.00093685946,0.00020975877,0.00021012001,0.00046187782,0.000029226376,0.000038509213,0.0009859224],"genre_scores_gemma":[0.9882278,0.0002690029,0.010095121,0.0006027666,0.000051487037,0.0000074635855,0.000017849146,0.000042839336,0.00068568526],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99700785,0.00015684993,0.0006523197,0.00073390204,0.0008424608,0.00060660375],"domain_scores_gemma":[0.998794,0.0001291561,0.00017518672,0.00049205223,0.00002346439,0.00038611816],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004891946,0.00042737223,0.00069996854,0.000015685378,0.00019966268,0.000043363274,0.00021721578,0.00016746378,0.0028481563],"category_scores_gemma":[0.000037570117,0.0002880196,0.00015062648,0.00025661656,0.0008722552,0.00029422375,0.0001870495,0.00017112271,0.00006803152],"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":[0.0018862673,0.0004948859,0.23662129,0.000049557853,0.0007928714,0.00018922998,0.005940226,0.00009742152,0.7393841,0.0000024590374,0.0108656,0.0036760918],"study_design_scores_gemma":[0.0035915428,0.0015513512,0.2682621,0.000048772952,0.00023464402,0.00019584766,0.00018280055,0.00039094524,0.72165424,0.00012900041,0.0028497998,0.00090900715],"about_ca_topic_score_codex":0.0021579622,"about_ca_topic_score_gemma":0.00003900364,"teacher_disagreement_score":0.031640794,"about_ca_system_score_codex":0.00015611289,"about_ca_system_score_gemma":0.000012343234,"threshold_uncertainty_score":0.9999572},"labels":[],"label_agreement":null},{"id":"W2152142399","doi":"10.1175/jas3660.1","title":"Cloud Phase Structure: Experimental Data Analysis and Parameterization","year":2006,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":20,"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":"Depth sounding; Liquid water content; Environmental science; Cloud fraction; Relative humidity; Atmospheric sciences; Cloud computing; Meteorology; Physics; Cloud cover; Geology; Computer science","score_opus":0.01479380912640694,"score_gpt":0.27342338817640705,"score_spread":0.2586295790500001,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2152142399","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":[0.9970116,0.00036295078,0.0016866752,0.00028650233,0.00033426398,0.000057366127,0.0000045562824,0.0000050901845,0.0002509976],"genre_scores_gemma":[0.9792449,0.000014326742,0.020343468,0.00015661157,0.00011974109,3.6452158e-7,7.17658e-7,0.0000043264054,0.000115562856],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99863684,0.000071005874,0.0003222784,0.00023683948,0.00055779796,0.00017523847],"domain_scores_gemma":[0.9991288,0.000038818307,0.00043916103,0.00032484537,0.0000089730265,0.00005938217],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039969018,0.00011001707,0.00018499141,7.933755e-7,0.00032351233,0.00011073288,0.0010189728,0.000032358526,0.00076893537],"category_scores_gemma":[0.00003477321,0.000061762716,0.0000771507,0.0012727113,0.00065872376,0.00048321922,0.00043023378,0.00008303009,0.0000025303889],"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":[0.000095125186,0.0004823323,0.6988559,0.0000041759567,0.00020417632,0.000012061125,0.0005108052,0.16938473,0.11181172,0.00019295883,0.008360404,0.010085602],"study_design_scores_gemma":[0.0020579132,0.0012550373,0.30541763,0.000026016793,0.0010146822,0.000270526,0.0015651886,0.6539619,0.022963265,0.003265035,0.007530471,0.0006723279],"about_ca_topic_score_codex":0.0003139824,"about_ca_topic_score_gemma":0.000057250294,"teacher_disagreement_score":0.48457718,"about_ca_system_score_codex":0.00004826581,"about_ca_system_score_gemma":0.000021820637,"threshold_uncertainty_score":0.8419303},"labels":[],"label_agreement":null},{"id":"W2152678338","doi":"10.5194/amtd-7-10585-2014","title":"Characterization and first results of an ice nucleating particle measurement system based on counterflow virtual impactor technique","year":2014,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":9,"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":"Deutsche Forschungsgemeinschaft","keywords":"Aerosol; Characterization (materials science); Particle (ecology); Saturation (graph theory); Instrumentation (computer programming); Analytical Chemistry (journal); Materials science; Ice nucleus; Environmental science; Meteorology; Chemistry; Nucleation; Nanotechnology; Geology; Chromatography; Physics","score_opus":0.009263579745747605,"score_gpt":0.19258955687337284,"score_spread":0.18332597712762524,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2152678338","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":[0.9400973,3.841226e-7,0.057209842,0.00007516753,0.000025140249,0.00020532514,0.0000067871256,0.00005480314,0.0023252638],"genre_scores_gemma":[0.9983875,4.4336014e-7,0.0014066561,0.000112041744,0.00001937935,0.000014878211,0.0000040923155,0.000010736861,0.000044257195],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9990658,0.000056470693,0.00021043167,0.00020502397,0.00032822057,0.00013404294],"domain_scores_gemma":[0.9995671,0.000025290552,0.000108295564,0.0002030256,0.000012951813,0.00008336087],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00058060855,0.00009318516,0.000107506836,9.817797e-7,0.00009201378,0.00002231002,0.000080887236,0.00004204747,0.00011038139],"category_scores_gemma":[0.00004772633,0.000073215495,0.000016218131,0.00007552129,0.000052729432,0.00012914541,0.000030938358,0.000037767983,0.000015625],"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":[0.00024250546,0.00018023478,0.018435033,0.0000365358,0.0000047799545,7.8670706e-7,0.0004207398,0.0026999519,0.9670602,0.00019951734,0.00005123882,0.010668495],"study_design_scores_gemma":[0.0009164694,0.0013027334,0.15945354,0.00012753543,0.000011852902,0.0000019292293,0.0002880271,0.6738386,0.16309829,0.0000018611743,0.00075814384,0.00020099271],"about_ca_topic_score_codex":0.0002595561,"about_ca_topic_score_gemma":0.00008708687,"teacher_disagreement_score":0.8039619,"about_ca_system_score_codex":0.00012228344,"about_ca_system_score_gemma":0.000004481816,"threshold_uncertainty_score":0.29856414},"labels":[],"label_agreement":null},{"id":"W2152916584","doi":"10.1002/2013ms000282","title":"Intercomparison of large‐eddy simulations of Arctic mixed‐phase clouds: Importance of ice size distribution assumptions","year":2014,"lang":"en","type":"article","venue":"Journal of Advances in Modeling Earth Systems","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":188,"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":"Biological and Environmental Research; Oak Ridge Institute for Science and Education; Pacific Northwest National Laboratory; National Energy Research Scientific Computing Center; Battelle; Office of Science; National Aeronautics and Space Administration; U.S. Department of Energy; Oak Ridge Associated Universities; National Science Foundation","keywords":"Bin; Ice crystals; Liquid water path; Environmental science; Parametrization (atmospheric modeling); Atmospheric sciences; Aerosol; Meteorology; Statistical physics; Climatology; Physics; Geology; Radiative transfer; Mathematics","score_opus":0.012754297361136552,"score_gpt":0.2940653663755299,"score_spread":0.28131106901439334,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2152916584","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":[0.6762649,0.00083387556,0.32249784,0.000010606063,0.00022923402,0.00008336112,0.000023900406,0.0000026303396,0.0000536941],"genre_scores_gemma":[0.99540555,0.00015979134,0.004342499,0.000005015774,0.000057283258,0.0000016337647,0.000004143786,0.000008450686,0.000015632166],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9978266,0.00012284385,0.0013233861,0.00013229607,0.0004233022,0.00017159781],"domain_scores_gemma":[0.99804014,0.00026255133,0.001328234,0.00019686186,0.00010955845,0.0000626488],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008214329,0.00011417835,0.00047540708,0.0000060530288,0.00004124465,0.0000070757774,0.00021071506,0.000060191436,0.000052994994],"category_scores_gemma":[0.00034908028,0.00009801105,0.00011560092,0.00024033237,0.00008993445,0.00038704817,0.000044890385,0.0001751476,0.0000015530856],"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":[0.00005006583,0.00025832638,0.099677764,0.000093822644,0.000011065016,6.1186836e-7,0.00020460981,0.8964679,0.0026887422,0.00015183931,0.000009615567,0.00038558518],"study_design_scores_gemma":[0.0009807062,0.000331392,0.00522711,0.00049801293,0.00003346567,0.000007547536,0.00070823607,0.9908026,0.0004299729,0.0003911418,0.00048703456,0.00010279881],"about_ca_topic_score_codex":0.00011595775,"about_ca_topic_score_gemma":0.00020642253,"teacher_disagreement_score":0.31914067,"about_ca_system_score_codex":0.000069375004,"about_ca_system_score_gemma":0.00001842326,"threshold_uncertainty_score":0.39967746},"labels":[],"label_agreement":null},{"id":"W2152943685","doi":"10.1029/2004jd005293","title":"Intercomparison of shortwave radiative transfer codes and measurements","year":2005,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":144,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Shortwave; Irradiance; Atmosphere (unit); Aerosol; Solar irradiance; Environmental science; Longwave; Atmospheric sciences; Radiative transfer; Atmospheric radiative transfer codes; Atmospheric model; Absorptance; Shortwave radiation; Cloud forcing; Radiative forcing; Meteorology; Physics; Radiation; Optics","score_opus":0.05639853519856996,"score_gpt":0.33186331748537,"score_spread":0.27546478228680005,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2152943685","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":[0.9941693,0.00031841942,0.0012387767,0.0003374634,0.000029563964,0.000116729105,0.000002500752,0.0000036742886,0.0037835785],"genre_scores_gemma":[0.9956315,0.00013208657,0.0037545206,0.00003708005,0.00014627994,0.0000026940893,2.4501907e-7,0.000012346802,0.00028322416],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9975078,0.00022634231,0.00044045073,0.00017444509,0.001296443,0.00035447915],"domain_scores_gemma":[0.99913776,0.00024955763,0.00009700009,0.00013858781,0.00011704972,0.0002600699],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009059152,0.00012885292,0.00035699428,0.00000179935,0.00009693471,0.00003089838,0.0003154235,0.00004906653,0.00081856886],"category_scores_gemma":[0.000154727,0.00009350868,0.00012392283,0.00025905008,0.0006241055,0.00028920703,0.00012946325,0.00046361945,0.00003594104],"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":[0.0016447183,0.0023291323,0.49250394,0.00006573667,0.0004377697,0.000050623803,0.004823796,0.004025743,0.13887978,0.0006949877,0.017779434,0.33676434],"study_design_scores_gemma":[0.0022942426,0.0036123989,0.90298754,0.00020817263,0.00007865138,0.000034279197,0.0023518521,0.009357497,0.06462019,0.0026722993,0.011375512,0.00040735072],"about_ca_topic_score_codex":0.00041848095,"about_ca_topic_score_gemma":0.00019611092,"teacher_disagreement_score":0.41048363,"about_ca_system_score_codex":0.0001538236,"about_ca_system_score_gemma":0.000043450247,"threshold_uncertainty_score":0.8962755},"labels":[],"label_agreement":null},{"id":"W2153077058","doi":"10.5194/acp-12-12155-2012","title":"Numerical evidence for cloud droplet nucleation at the cloud-environment interface","year":2012,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Institute of Atmospheric Physics, Chinese Academy of Sciences; Chinese Academy of Sciences","keywords":"Cloud computing; Liquid water content; Cloud base; Cloud condensation nuclei; Nucleation; Meteorology; Cloud physics; Atmospheric sciences; Supersaturation; Mechanics; Condensation; Cloud cover; Supercooling; Aerosol; Environmental science; Physics; Thermodynamics; Computer science","score_opus":0.015755699298680766,"score_gpt":0.24589637066833067,"score_spread":0.2301406713696499,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2153077058","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":[0.95414394,0.0007049461,0.042187136,0.00039679857,0.00014328204,0.00024013844,0.0000042795823,0.000031435775,0.002148058],"genre_scores_gemma":[0.984462,0.00017091843,0.0055838823,0.00026005064,0.00064958434,0.000064679814,0.00000731115,0.000027007603,0.008774571],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9988838,0.000024676126,0.00017993482,0.00031128188,0.00022180495,0.00037854785],"domain_scores_gemma":[0.99924916,0.00015427286,0.00010365714,0.0003386824,0.0000043539703,0.00014988754],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00016245506,0.00020933985,0.000156135,5.240891e-9,0.00033878366,0.000028387392,0.00020360693,0.000077467834,0.0054205195],"category_scores_gemma":[0.00002060872,0.00015676467,0.000084977,0.00009097891,0.00027928592,0.00019418928,0.00020694223,0.0001239414,0.00029400643],"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":[0.0006141883,0.0009535177,0.22585718,0.0002710551,0.0001779514,0.0000030803835,0.005952687,0.029435482,0.13285378,0.00031512306,0.06534295,0.538223],"study_design_scores_gemma":[0.0015185842,0.00029377316,0.05106302,0.000103379985,0.0003196411,0.00007970564,0.0010035547,0.09603698,0.078670174,0.0014518223,0.76770294,0.0017564256],"about_ca_topic_score_codex":0.000062592946,"about_ca_topic_score_gemma":5.0147315e-7,"teacher_disagreement_score":0.70236,"about_ca_system_score_codex":0.00021207563,"about_ca_system_score_gemma":0.000005410638,"threshold_uncertainty_score":0.99548864},"labels":[],"label_agreement":null},{"id":"W2154084243","doi":"10.5194/acp-13-10385-2013","title":"Reduced efficacy of marine cloud brightening geoengineering due to in-plume aerosol coagulation: parameterization and global implications","year":2013,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Environment Research Council; Natural Sciences and Engineering Research Council of Canada; Forschungszentrum Jülich; Engineering and Physical Sciences Research Council; Eidgenössische Technische Hochschule Zürich; Academy of Finland; University of Oxford; Sight Research UK","keywords":"Aerosol; Environmental science; Atmospheric sciences; Plume; Sea spray; Sea salt aerosol; Cloud albedo; Meteorology; Sea salt; Climate model; Climatology; Cloud computing; Climate change; Cloud cover; Oceanography; Physics; Geology","score_opus":0.005233610031356094,"score_gpt":0.20583891020710202,"score_spread":0.20060530017574593,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2154084243","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":[0.9879117,0.00001648301,0.010268229,0.00010517023,0.000019336083,0.00018709525,0.0000026715688,0.000021515945,0.0014677836],"genre_scores_gemma":[0.9765253,0.000012401995,0.023120929,0.000039866103,0.000051033614,0.000028908145,0.000012735363,0.000009408348,0.00019938788],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99928343,0.000007165482,0.0001983042,0.00025348345,0.000089262925,0.00016836319],"domain_scores_gemma":[0.99961853,0.0000271213,0.00006240902,0.00017604894,0.000010985435,0.00010490554],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000031013984,0.00013234834,0.0001661431,2.2135064e-8,0.00005839266,0.000026135785,0.000083491796,0.000053227464,0.0005682338],"category_scores_gemma":[0.000011838311,0.0001356733,0.000022439923,0.00029332697,0.00007614267,0.00011898334,0.00012568508,0.00005791822,0.000011488416],"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":[0.00002713456,0.00016435317,0.29243517,0.00008899605,0.000027277893,0.0000021657743,0.00044799148,0.03841278,0.29916263,0.00016943357,0.0001785752,0.36888352],"study_design_scores_gemma":[0.00041536216,0.000030732717,0.94268996,0.000025108644,0.000016254215,0.000015668336,0.00004137294,0.046029624,0.009423295,0.000949638,0.00010398766,0.00025898367],"about_ca_topic_score_codex":0.00052119856,"about_ca_topic_score_gemma":0.0000037098487,"teacher_disagreement_score":0.6502548,"about_ca_system_score_codex":0.000052343705,"about_ca_system_score_gemma":0.000005698908,"threshold_uncertainty_score":0.6221762},"labels":[],"label_agreement":null},{"id":"W2154114222","doi":"10.5194/acp-8-787-2008","title":"Development and evaluation of an operational SDS forecasting system for East Asia: CUACE/Dust","year":2008,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":80,"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":"Dust storm; Environmental science; Aerosol; Storm; Asian Dust; Advection; Meteorology; Mesoscale meteorology; Climatology; Lidar; Data assimilation; East Asia; Atmospheric sciences; Geography; Geology; Remote sensing","score_opus":0.03195212233481709,"score_gpt":0.2340619442635616,"score_spread":0.20210982192874452,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2154114222","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":[0.99218935,0.00005239951,0.0036620619,0.000008924128,0.000018163113,0.00016718164,0.0000038670196,0.0000134763495,0.0038845635],"genre_scores_gemma":[0.922707,0.0000034064328,0.07676407,0.000009620155,0.000076928525,0.00004624587,0.000023071867,0.000009784682,0.00035984704],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9991902,0.0000120159475,0.00017428235,0.00023141269,0.0002630031,0.00012906658],"domain_scores_gemma":[0.99969524,0.00001675016,0.000081213075,0.00009991149,0.000033316363,0.00007357092],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018839128,0.00011793056,0.00013033765,1.0231144e-8,0.00025248717,0.000011756132,0.000060936723,0.00005352867,0.00018171435],"category_scores_gemma":[0.000008484107,0.0001117964,0.000020559386,0.000074994656,0.00012122598,0.00013074646,0.00004201286,0.000044249082,0.0000018277452],"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":[0.000079671634,0.0002872032,0.04645433,0.00036338487,0.00006485039,0.0000042385263,0.0044358643,0.021777455,0.040059354,0.00016292815,0.00023230836,0.8860784],"study_design_scores_gemma":[0.0012237519,0.000059495218,0.02659047,0.00004868062,0.00007108441,0.000087224296,0.0018582477,0.93107593,0.03695105,0.00010381075,0.0015812737,0.00034898162],"about_ca_topic_score_codex":0.00002424217,"about_ca_topic_score_gemma":0.0000022899796,"teacher_disagreement_score":0.9092985,"about_ca_system_score_codex":0.00008248576,"about_ca_system_score_gemma":0.00004737559,"threshold_uncertainty_score":0.45589247},"labels":[],"label_agreement":null},{"id":"W2154197430","doi":"10.5194/acp-7-3309-2007","title":"Global trends in visibility: implications for dust sources","year":2007,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":248,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Visibility; AERONET; Environmental science; Precipitation; Mineral dust; Climatology; Aerosol; Extinction (optical mineralogy); Atmospheric sciences; Climate change; Meteorology; Geography; Geology","score_opus":0.008754713978902715,"score_gpt":0.25550148409255724,"score_spread":0.24674677011365453,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2154197430","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":[0.95936185,0.000055857305,0.01807858,0.00013909694,0.000015237676,0.0000704523,0.0000099836725,0.000026293003,0.022242656],"genre_scores_gemma":[0.98520344,0.000008752299,0.012300997,0.00011889115,0.000094336945,0.000017154145,0.000015495492,0.000008416565,0.002232533],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9991844,0.0000038759817,0.00016434902,0.00030741384,0.00007365332,0.0002663069],"domain_scores_gemma":[0.99960816,0.000037460803,0.00004879062,0.00020396402,0.0000053913354,0.00009621604],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011824985,0.00012839462,0.00012491642,7.717642e-9,0.00010289943,0.00001818433,0.00012132956,0.00007337014,0.00074753334],"category_scores_gemma":[0.0000065548843,0.00012528639,0.000052739644,0.00038757396,0.00014878389,0.000071077426,0.000058261052,0.000055928922,0.0000063754906],"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":[0.000016910071,0.000084303654,0.49804315,0.00000890425,0.0000048008387,4.687712e-7,0.000095232164,0.0003809534,0.0013305292,0.00011436048,0.0004179545,0.49950242],"study_design_scores_gemma":[0.00041190494,0.000026117375,0.9796358,0.0000045601123,0.000014724196,0.0000048006455,0.00015498154,0.0030346871,0.00071862544,0.0056095403,0.010151975,0.00023228326],"about_ca_topic_score_codex":0.00017717885,"about_ca_topic_score_gemma":0.00005365309,"teacher_disagreement_score":0.49927014,"about_ca_system_score_codex":0.00011124042,"about_ca_system_score_gemma":0.000006365293,"threshold_uncertainty_score":0.8184966},"labels":[],"label_agreement":null},{"id":"W2155009288","doi":"10.5589/m12-048","title":"Comparison of dust source identification techniques over land in the Middle East region using MODIS data","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"HYSPLIT; Pixel; Plume; Meteorology; Environmental science; Remote sensing; Identification (biology); Asian Dust; Visibility; Algorithm; Geography; Computer science; Aerosol; Artificial intelligence","score_opus":0.10477342536955819,"score_gpt":0.2885909064445314,"score_spread":0.1838174810749732,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155009288","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":[0.9340254,0.00019197061,0.065094024,0.00015939242,0.00008829865,0.00005777311,0.0000018905331,0.0000018374009,0.00037943263],"genre_scores_gemma":[0.98087114,0.0000044416915,0.018922206,0.00007165033,0.00009738898,4.2460373e-9,0.0000019116624,0.000008050776,0.00002320039],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999178,0.00007394431,0.00029635357,0.00008107021,0.00017333824,0.00019729794],"domain_scores_gemma":[0.9992455,0.000017969078,0.0003119323,0.00027704405,0.000013521449,0.00013401247],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005541244,0.000067264125,0.0001317536,0.000008611421,0.000101377,0.000030846157,0.00025473587,0.00004928631,0.000020069876],"category_scores_gemma":[0.000049980878,0.000052254425,0.000027951744,0.00018777486,0.000118164586,0.00027401486,0.00003116864,0.00015917319,0.0000019528372],"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":[0.000012127235,0.000021298201,0.5404013,0.000012442498,0.000009947587,0.000029183278,0.010472169,0.00094294903,0.005059765,0.000004369963,0.0019854486,0.441049],"study_design_scores_gemma":[0.0005108622,0.00009474187,0.56437373,0.0007151432,0.00016418085,0.0016354553,0.01770324,0.35936934,0.0037073952,0.00019676363,0.05097597,0.00055318954],"about_ca_topic_score_codex":0.031483226,"about_ca_topic_score_gemma":0.021563847,"teacher_disagreement_score":0.44049582,"about_ca_system_score_codex":0.00016203077,"about_ca_system_score_gemma":0.00004827056,"threshold_uncertainty_score":0.9962901},"labels":[],"label_agreement":null},{"id":"W2155108279","doi":"10.5194/amt-4-583-2011","title":"Maritime aerosol network as a component of AERONET – first results and comparison with global aerosol models and satellite retrievals","year":2011,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":185,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Université du Québec à Rimouski; Institut du Savoir Montfort; Université de Sherbrooke","funders":"NASA Headquarters; Institut Polaire Français Paul Emile Victor; National Aeronautics and Space Administration","keywords":"AERONET; Aerosol; Satellite; Environmental science; Climatology; The arctic; Arctic; Oceanography; Meteorology; Remote sensing; Geography; Geology","score_opus":0.034930124008426,"score_gpt":0.2291493006104041,"score_spread":0.19421917660197807,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155108279","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":[0.8633154,0.004272848,0.060875975,0.0003050448,0.00010848926,0.002854442,0.000026205584,0.00065750425,0.06758408],"genre_scores_gemma":[0.82319164,0.0007760029,0.17568076,0.00015101228,0.000024627045,0.00006652905,0.0000047471885,0.000031380278,0.00007329563],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9967748,0.00011667527,0.0007555276,0.00075085124,0.0010215061,0.00058065064],"domain_scores_gemma":[0.99861014,0.000035604542,0.00045186124,0.0005566392,0.000072150135,0.0002736071],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0009173116,0.0004510598,0.0006323946,5.944353e-7,0.00023407268,0.000046579524,0.00032248104,0.00018983116,0.00020498296],"category_scores_gemma":[0.000028483755,0.0003733147,0.00006240374,0.0003940477,0.0006561532,0.00027950623,0.0003627589,0.00018315791,0.000012341076],"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":[0.007033386,0.002113681,0.8393194,0.00035355586,0.00060001184,0.00009113607,0.0045396723,0.0017511114,0.007223607,0.002375089,0.016818145,0.11778117],"study_design_scores_gemma":[0.0154526,0.026582029,0.71561503,0.0043464475,0.0018059667,0.00056722265,0.002436645,0.06070974,0.11636523,0.020227786,0.026625784,0.00926554],"about_ca_topic_score_codex":0.0031654667,"about_ca_topic_score_gemma":0.00078501104,"teacher_disagreement_score":0.123704426,"about_ca_system_score_codex":0.00024002415,"about_ca_system_score_gemma":0.000029177965,"threshold_uncertainty_score":0.99987185},"labels":[],"label_agreement":null},{"id":"W2155474590","doi":"10.1029/2007jd009349","title":"A satellite‐based assessment of transpacific transport of pollution aerosol","year":2008,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":156,"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; Satellite; Environmental science; Pollution; Meteorology; Remote sensing; Climatology; Geology; Geography; Aerospace engineering","score_opus":0.03880201304062457,"score_gpt":0.3229092931027624,"score_spread":0.2841072800621378,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155474590","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":[0.9900994,0.0001715725,0.0051271156,0.00025352387,0.000052113275,0.00018491482,0.000007784203,0.000006104043,0.004097517],"genre_scores_gemma":[0.98909956,0.00028737864,0.010126376,0.000020452339,0.000073769195,0.0000045324055,0.0000012947727,0.000019240273,0.00036737625],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9961338,0.00023480387,0.00078060693,0.00021775281,0.0021745586,0.00045850326],"domain_scores_gemma":[0.9986429,0.00022282504,0.00038439955,0.00028711284,0.00018809548,0.00027461874],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008164068,0.00016784553,0.00052069954,0.000003534401,0.00014241567,0.000006650567,0.000485447,0.00009951616,0.0013729305],"category_scores_gemma":[0.000060126855,0.00012825697,0.00037958415,0.0007395361,0.0012191373,0.00022180381,0.000040454262,0.00055377814,0.00001800217],"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":[0.001363037,0.0040913173,0.5310938,0.00020441254,0.00019630798,0.00029115222,0.0016673064,0.015929393,0.42426285,0.0006592532,0.0015149208,0.01872627],"study_design_scores_gemma":[0.0013009107,0.0026063703,0.96181685,0.00011880307,0.000034845933,0.000020777006,0.00033302294,0.0023881977,0.02956784,0.00056517735,0.0010671066,0.00018010077],"about_ca_topic_score_codex":0.0007913162,"about_ca_topic_score_gemma":0.000055456083,"teacher_disagreement_score":0.43072307,"about_ca_system_score_codex":0.0001690569,"about_ca_system_score_gemma":0.000289202,"threshold_uncertainty_score":0.99954},"labels":[],"label_agreement":null},{"id":"W2156349939","doi":"10.5589/m03-058","title":"Relative merits of the 1.6 and 3.75 μm channels of the AVHRR/3 for cloud detection","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Oceanic and Atmospheric Administration; National Aeronautics and Space Administration","keywords":"Advanced very-high-resolution radiometer; Remote sensing; Cloud computing; Environmental science; Moderate-resolution imaging spectroradiometer; Meteorology; Cloud top; Channel (broadcasting); Radiometry; Cirrus; Cloud cover; Satellite; Computer science; Geography; Telecommunications; Physics","score_opus":0.009030138766071739,"score_gpt":0.19463361743402208,"score_spread":0.18560347866795035,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2156349939","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":[0.9679038,0.000107171356,0.030233525,0.0007970659,0.00048167232,0.00010866517,0.000002381223,7.698373e-7,0.00036493802],"genre_scores_gemma":[0.9895712,0.000006747408,0.010156529,0.00010379101,0.000064463566,8.76409e-9,2.902953e-8,0.0000073837155,0.00008981561],"study_design_codex":"design_other","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9994494,0.00003251057,0.0001965699,0.00006616146,0.00011944437,0.00013595268],"domain_scores_gemma":[0.99943525,0.00002469157,0.0002954658,0.00010212875,0.000030832198,0.00011164957],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019118546,0.00006312757,0.000117416115,0.000002743683,0.00018003197,0.000007837314,0.00010008244,0.00004556102,0.00000807409],"category_scores_gemma":[0.000108178065,0.00003894918,0.000087473665,0.00015303248,0.0002699768,0.000064914304,0.000018781317,0.00012309018,3.7156286e-7],"study_design_candidate":"design_other","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":[0.0000956827,0.000015968837,0.007970382,0.000058276877,0.00015565625,0.000029124043,0.018345665,0.01378942,0.1119528,0.00040524206,0.00041261365,0.84676915],"study_design_scores_gemma":[0.0048293546,0.0013485212,0.27727172,0.002337168,0.00055849925,0.0026468502,0.005569,0.018376833,0.5660251,0.08980064,0.03025685,0.0009794775],"about_ca_topic_score_codex":0.00939549,"about_ca_topic_score_gemma":0.021300476,"teacher_disagreement_score":0.8457897,"about_ca_system_score_codex":0.00015620374,"about_ca_system_score_gemma":0.00009699332,"threshold_uncertainty_score":0.997201},"labels":[],"label_agreement":null},{"id":"W2156645902","doi":"10.5194/amt-5-73-2012","title":"Aerosol classification using airborne High Spectral Resolution Lidar measurements – methodology and examples","year":2012,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":642,"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":"Biological and Environmental Research; NASA Headquarters; Science Mission Directorate; Langley Research Center; Office of Science; National Aeronautics and Space Administration; U.S. Department of Energy; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Aerosol; Lidar; Remote sensing; Environmental science; Backscatter (email); Meteorology; Extinction (optical mineralogy); Atmospheric sciences; Geology; Mineralogy; Physics; Computer science","score_opus":0.16032862718440358,"score_gpt":0.29917210093445035,"score_spread":0.13884347375004677,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2156645902","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":[0.78129953,0.00082892674,0.21233685,0.00017357661,0.00026210482,0.00077034807,0.0000017603262,0.00042942283,0.0038974837],"genre_scores_gemma":[0.63514334,0.00007718098,0.36433488,0.00015866093,0.00012813254,0.00007002058,0.0000029112211,0.000033532113,0.000051318646],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99669504,0.0004598181,0.0004996856,0.0005562826,0.0010257212,0.00076346635],"domain_scores_gemma":[0.99886495,0.00004051372,0.00029751824,0.0004829112,0.00005898965,0.00025511335],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.002849751,0.00036635055,0.00036458115,0.0000015222658,0.00034026196,0.000042637184,0.00026812,0.00021525848,0.0006303191],"category_scores_gemma":[0.00015890904,0.00033810613,0.00007909556,0.00035545693,0.00030275312,0.00050763483,0.0001991916,0.00021023263,0.000046391913],"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":[0.000070873924,0.00031732794,0.25000712,0.000027326909,0.00007141857,0.0000015785719,0.00045790503,0.000057757996,0.68804216,0.00066128006,0.0012390421,0.059046198],"study_design_scores_gemma":[0.0007374055,0.00048739777,0.77484375,0.000106380096,0.00028655387,0.000058028665,0.00047979224,0.0019323351,0.20801975,0.0012311602,0.010517526,0.0012999108],"about_ca_topic_score_codex":0.0017568719,"about_ca_topic_score_gemma":0.00008377359,"teacher_disagreement_score":0.52483666,"about_ca_system_score_codex":0.0008925732,"about_ca_system_score_gemma":0.00002942265,"threshold_uncertainty_score":0.9999071},"labels":[],"label_agreement":null},{"id":"W2156674034","doi":"10.1029/2004jd005756","title":"Raman lidar observations of aged Siberian and Canadian forest fire smoke in the free troposphere over Germany in 2003: Microphysical particle characterization","year":2005,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":311,"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":"Lidar; Atmospheric sciences; Troposphere; Environmental science; Particle (ecology); Extinction (optical mineralogy); Wavelength; Aerosol; Altitude (triangle); Haze; Meteorology; Physics; Geology; Optics","score_opus":0.022919437096949855,"score_gpt":0.2741694101954664,"score_spread":0.25124997309851654,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2156674034","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":[0.997007,0.000062223815,0.000016415606,0.0023580429,0.00002601771,0.00023869844,0.000011144874,0.0000024340513,0.00027798783],"genre_scores_gemma":[0.9985629,0.000076969045,0.0007133631,0.00020773942,0.00016278712,0.000010623967,0.000003362516,0.000015283398,0.00024701675],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9977963,0.00029623407,0.0004775692,0.00019099288,0.00072309736,0.00051583117],"domain_scores_gemma":[0.99905777,0.00018740364,0.0001524491,0.00028426587,0.0000731313,0.000244951],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00061907305,0.00013557926,0.00026425888,0.0000026654734,0.00015062488,0.00007379913,0.0005005346,0.00008143245,0.0006442562],"category_scores_gemma":[0.00029833647,0.00009763726,0.00006676012,0.0009884374,0.0004086274,0.00044457125,0.00013474724,0.0005863975,0.000018183988],"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":[0.00017773168,0.0006674408,0.9231658,0.00001651535,0.000020299814,0.00009040793,0.0021427386,0.0005824611,0.05572476,0.00056490174,0.0021229943,0.014723929],"study_design_scores_gemma":[0.00071732054,0.00028527732,0.99054873,0.00004171587,0.0000065885993,0.0000045795223,0.00038398104,0.004351414,0.00028419704,0.0005223702,0.0027557362,0.00009808938],"about_ca_topic_score_codex":0.051792745,"about_ca_topic_score_gemma":0.3030093,"teacher_disagreement_score":0.25121653,"about_ca_system_score_codex":0.00021249318,"about_ca_system_score_gemma":0.00015164145,"threshold_uncertainty_score":0.9545215},"labels":[],"label_agreement":null},{"id":"W2156705617","doi":"10.5194/acp-11-3673-2011","title":"Airborne observation of aerosol optical depth during ARCTAS: vertical profiles, inter-comparison and fine-mode fraction","year":2011,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":56,"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; Université de Sherbrooke","funders":"Oak Ridge Associated Universities; Ames Research Center; National Aeronautics and Space Administration","keywords":"Aerosol; Angstrom exponent; Single-scattering albedo; Atmospheric sciences; Environmental science; Troposphere; Haze; Soot; Mineral dust; Albedo (alchemy); Optical depth; Meteorology; Chemistry; Geology; Physics","score_opus":0.015328854058037179,"score_gpt":0.23016347812134264,"score_spread":0.21483462406330545,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2156705617","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":[0.98992133,0.00004367809,0.0061344747,0.00001621784,0.00001619312,0.00008522151,0.0000014408205,0.000026114392,0.0037553152],"genre_scores_gemma":[0.97833383,0.000023515846,0.021279078,0.000017557117,0.0000549279,0.0000131862125,0.000007575154,0.000013422036,0.00025691264],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99915624,0.000010508535,0.00022805145,0.0002872297,0.00012936154,0.00018862193],"domain_scores_gemma":[0.9996193,0.000023414801,0.000067647896,0.0001741213,0.0000103174725,0.00010520149],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000037638,0.00015856692,0.00020114372,1.6203376e-8,0.00007835849,0.000012204065,0.00008814906,0.000092357426,0.00058406766],"category_scores_gemma":[0.000014234515,0.00014941805,0.00003660383,0.00010454912,0.00024008553,0.00016773738,0.000102509264,0.00015632012,0.000010385325],"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":[0.00018390459,0.00043060855,0.56366533,0.00018623263,0.00003761599,0.0000029913247,0.000859856,0.0002047492,0.3214398,0.00008347308,0.0001119967,0.11279341],"study_design_scores_gemma":[0.0005042278,0.000091824186,0.4854092,0.00005233782,0.000049707756,0.00000925658,0.0002337568,0.03325665,0.4795952,0.00042254993,0.00008245163,0.000292824],"about_ca_topic_score_codex":0.0002144501,"about_ca_topic_score_gemma":0.000008632892,"teacher_disagreement_score":0.1581554,"about_ca_system_score_codex":0.00004749556,"about_ca_system_score_gemma":0.000008486145,"threshold_uncertainty_score":0.63951313},"labels":[],"label_agreement":null},{"id":"W2158474521","doi":"10.1029/2003jd003377","title":"Sensitivity studies of the effect of increased aerosol concentrations and snow crystal shape on the snowfall rate in the Arctic","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Snow; Aerosol; Environmental science; Atmospheric sciences; Ice crystals; Coalescence (physics); Drizzle; Precipitation; Liquid water content; Accretion (finance); Arctic; Mesoscale meteorology; Supersaturation; Materials science; Meteorology; Cloud computing; Geology; Physics; Astrophysics; Astrobiology; Thermodynamics","score_opus":0.0264824628642429,"score_gpt":0.3044298458153967,"score_spread":0.27794738295115384,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2158474521","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":[0.997745,0.00016249964,0.000013459625,0.0010454274,0.00003472783,0.0003555741,0.0000023762339,0.0000012223394,0.0006397148],"genre_scores_gemma":[0.99964386,0.00009907572,0.000050941064,0.00009307015,0.000037958882,0.000008748595,8.508268e-8,0.00000727438,0.000058995833],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9949917,0.0032365362,0.0003397703,0.00014554721,0.0009821113,0.00030431245],"domain_scores_gemma":[0.9918341,0.007502164,0.0002331075,0.00026876872,0.00008918372,0.000072676885],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0038666944,0.00013241939,0.00031446878,9.917886e-7,0.00025342734,0.000030507887,0.00032328314,0.000040151604,0.0001418916],"category_scores_gemma":[0.004325591,0.000053702708,0.00014021837,0.00047938162,0.0016021689,0.00010126837,0.00014487977,0.0006252642,0.0000056848435],"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":[0.0015172949,0.0013518308,0.7387811,0.00018631398,0.0004179123,0.00012280211,0.0056105647,0.0041982424,0.23156896,0.0059069092,0.004733899,0.00560419],"study_design_scores_gemma":[0.0013603541,0.003096776,0.94870746,0.0003298614,0.00006106187,0.000024827224,0.0040941415,0.002046004,0.037315432,0.0026052124,0.00021420192,0.00014464594],"about_ca_topic_score_codex":0.0006813713,"about_ca_topic_score_gemma":0.0003608774,"teacher_disagreement_score":0.2099264,"about_ca_system_score_codex":0.000087286586,"about_ca_system_score_gemma":0.000058751924,"threshold_uncertainty_score":0.5903258},"labels":[],"label_agreement":null},{"id":"W2160436992","doi":"10.1175/jcli-d-13-00169.1","title":"Origins of the Solar Radiation Biases over the Southern Ocean in CFMIP2 Models*","year":2013,"lang":"en","type":"article","venue":"Journal of Climate","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":350,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Advanced Foods and Materials Network; Environment and Climate Change Canada","funders":"Japan Agency for Marine-Earth Science and Technology; University of Tokyo; European Commission; Center for Neuroscience and Regenerative Medicine; U.S. Department of Energy; Met Office; Langley Research Center; Department for Environment, Food and Rural Affairs, UK Government; National Aeronautics and Space Administration","keywords":"Environmental science; Shortwave; Lidar; International Satellite Cloud Climatology Project; Climate model; Cloud fraction; Cloud top; Climatology; Satellite; Atmospheric sciences; Meteorology; Cloud height; Cloud computing; Atmosphere (unit); Cloud albedo; Cloud feedback; Shortwave radiation; Radiative transfer; Cloud cover; Remote sensing; Climate change; Radiation; Climate sensitivity; Geology; Geography; Computer science; Physics","score_opus":0.011243373202153092,"score_gpt":0.222047945505797,"score_spread":0.2108045723036439,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2160436992","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":[0.99807036,0.000060825194,0.000102514605,0.00052268564,0.00010188138,0.00008221949,0.0000030985316,0.0000019373922,0.0010544892],"genre_scores_gemma":[0.9993246,0.0002080758,0.00013125816,0.00023445123,0.000036744095,6.623577e-7,1.1781662e-7,0.0000069227394,0.000057158006],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991808,0.00005461735,0.00029497241,0.00005487977,0.0002744036,0.0001403507],"domain_scores_gemma":[0.9994208,0.00005161146,0.00035103993,0.00013402644,0.000009881784,0.00003261258],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029736542,0.00006433593,0.000110411755,0.0000015046841,0.0000635663,0.000020359583,0.0002580812,0.000029874534,0.0008404748],"category_scores_gemma":[0.000026181711,0.000030096024,0.00008687529,0.00012348618,0.0000875085,0.00023353293,0.00007220225,0.00013245575,0.000041806954],"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":[0.000027412696,0.00012544548,0.8641649,0.000007246279,0.000018246988,0.0000028720478,0.0030643218,0.1184337,0.002434227,0.0003710316,0.0017767998,0.009573812],"study_design_scores_gemma":[0.00071249023,0.00010444082,0.92915916,0.00006935401,0.000033946242,0.000019610916,0.0018193865,0.060060367,0.00066614023,0.0039057329,0.0033153854,0.00013398365],"about_ca_topic_score_codex":0.0007546139,"about_ca_topic_score_gemma":0.000070094145,"teacher_disagreement_score":0.064994276,"about_ca_system_score_codex":0.00013049266,"about_ca_system_score_gemma":0.000012080983,"threshold_uncertainty_score":0.92026097},"labels":[],"label_agreement":null},{"id":"W2161816611","doi":"10.1175/jtech-d-13-00007.1","title":"Improved Airborne Hot-Wire Measurements of Ice Water Content in Clouds","year":2013,"lang":"en","type":"article","venue":"Journal of Atmospheric and Oceanic Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":128,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Glenn Research Center; Canadian Space Agency; Transport Canada; Federal Aviation Administration; National Aeronautics and Space Administration","keywords":"Wind tunnel; Environmental science; Ice crystals; Materials science; Particle (ecology); Wind speed; Atmospheric sciences; Meteorology; Remote sensing; Optics; Geology; Physics; Mechanics","score_opus":0.012456715342500936,"score_gpt":0.2015836026137809,"score_spread":0.18912688727127996,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2161816611","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":[0.99698675,0.0005836641,0.0006960587,0.0008978756,0.0001364715,0.00018105214,3.0038245e-7,0.000017028948,0.00050077523],"genre_scores_gemma":[0.9897558,0.00013495522,0.009574266,0.00017584297,0.000021138718,0.0000046395744,1.5214066e-7,0.000015819796,0.0003173528],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985131,0.00003244931,0.0006585462,0.00019617593,0.00024813542,0.00035158248],"domain_scores_gemma":[0.99927413,0.000020856316,0.00035296747,0.00020111393,0.00005646757,0.00009445748],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003032393,0.00017596551,0.0004227465,0.0000020568425,0.00004483603,0.000011533082,0.00034424887,0.00020158218,0.0012115857],"category_scores_gemma":[0.00005420447,0.00011523848,0.000077587414,0.00026814142,0.0003334735,0.0001664064,0.00020609832,0.00030188455,0.000026995305],"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":[0.00015323442,0.00041562974,0.6164606,0.000031016716,0.00011113295,0.00003333609,0.0005170337,0.00017023849,0.28247833,0.000085336644,0.0013924661,0.09815161],"study_design_scores_gemma":[0.005547293,0.0030650792,0.91340387,0.00015633904,0.00012670908,0.0003408407,0.0037667132,0.0034387535,0.062979184,0.0028144736,0.0036456913,0.0007150622],"about_ca_topic_score_codex":0.0003552972,"about_ca_topic_score_gemma":0.000024435223,"teacher_disagreement_score":0.29694325,"about_ca_system_score_codex":0.00012183533,"about_ca_system_score_gemma":0.000017725524,"threshold_uncertainty_score":0.99970144},"labels":[],"label_agreement":null},{"id":"W2162175978","doi":"10.1029/2004jd005021","title":"Comparing clouds and their seasonal variations in 10 atmospheric general circulation models with satellite measurements","year":2005,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":419,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Goddard Space Flight Center; Centre National de la Recherche Scientifique; Lawrence Livermore National Laboratory; Dalhousie University; Canadian Foundation for Climate and Atmospheric Sciences; National Aeronautics and Space Administration; U.S. Department of Energy; National Center for Atmospheric Research; Stony Brook University; National Science Foundation","keywords":"International Satellite Cloud Climatology Project; Longwave; Environmental science; Satellite; Shortwave; Atmospheric sciences; Climatology; Cloud cover; Cloud top; Meteorology; Radiative transfer; Cloud computing; Geography; Geology; Physics","score_opus":0.05730091918254306,"score_gpt":0.2920271994266927,"score_spread":0.23472628024414963,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2162175978","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":[0.9886484,0.000412007,0.006000637,0.0003502981,0.000025586147,0.0001811874,8.392699e-7,0.000009703769,0.0043713343],"genre_scores_gemma":[0.97838056,0.00009983384,0.020687278,0.00004950599,0.00025131146,0.0000090274825,0.0000011540832,0.000024101782,0.0004972001],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99718684,0.00026803187,0.0004425534,0.0002944145,0.0012529591,0.000555193],"domain_scores_gemma":[0.9990016,0.00017285768,0.00019051407,0.00019720588,0.00013045207,0.00030733287],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000983486,0.00020360501,0.0003509309,0.0000015187272,0.00021268366,0.0001122094,0.00031652657,0.00007660611,0.0006123222],"category_scores_gemma":[0.000065252854,0.00014255093,0.000083737024,0.0006359129,0.00030851012,0.000711836,0.00018260148,0.0005417785,0.000053507476],"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":[0.0006142713,0.0007094551,0.6343793,0.000015754775,0.00010596782,0.000022190403,0.0014173297,0.27083188,0.005273054,0.0009847679,0.00045758102,0.08518838],"study_design_scores_gemma":[0.00097324216,0.0003275346,0.62898964,0.000053729753,0.000011040427,0.000019006387,0.00021392257,0.36487988,0.00011552233,0.0031740344,0.0010694205,0.0001730446],"about_ca_topic_score_codex":0.0006664803,"about_ca_topic_score_gemma":0.000603524,"teacher_disagreement_score":0.09404799,"about_ca_system_score_codex":0.0004514582,"about_ca_system_score_gemma":0.000097267315,"threshold_uncertainty_score":0.67044985},"labels":[],"label_agreement":null},{"id":"W2162509780","doi":"10.5194/acp-15-2489-2015","title":"A comprehensive laboratory study on the immersion freezing behavior of illite NX particles: a comparison of 17 ice nucleation measurement techniques","year":2015,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":315,"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":"Pacific Northwest National Laboratory; Japan Society for the Promotion of Science; Deutsche Forschungsgemeinschaft; Sight Research UK; Alexander von Humboldt-Stiftung; Battelle; Natural Environment Research Council; U.S. Department of Energy; National Science Foundation","keywords":"Ice nucleus; Nucleation; Immersion (mathematics); Illite; Chemistry; Mineralogy; Clay minerals","score_opus":0.038021922794154624,"score_gpt":0.26647932937753294,"score_spread":0.22845740658337832,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2162509780","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":[0.9980261,0.000105262814,0.00047335646,0.000026254487,0.00001287331,0.00026478912,0.0000035406879,0.000017393191,0.0010704689],"genre_scores_gemma":[0.9977971,0.0000074931745,0.0020526012,0.000041764633,0.000022923046,0.000029150846,0.0000014826933,0.000010080502,0.000037429352],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9989815,0.000045289435,0.00023069704,0.00019143724,0.00043324704,0.00011786676],"domain_scores_gemma":[0.9993767,0.000035093966,0.00019366013,0.00026259886,0.00006911899,0.00006284223],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017555099,0.00013190969,0.00019863062,2.0361755e-8,0.00007804506,0.000009726926,0.0001338642,0.000041835527,0.00012097722],"category_scores_gemma":[0.000011387753,0.00009988398,0.000035416353,0.00019398208,0.00019699566,0.00006253013,0.00008043516,0.00009939104,0.000004938651],"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":[0.00009942071,0.0016765636,0.2541858,0.00004437472,0.000045058347,0.0000015054899,0.006716168,0.0008723998,0.6815701,0.00001315554,0.0012689636,0.05350644],"study_design_scores_gemma":[0.0010140456,0.0009043673,0.106224604,0.00011780318,0.00021461176,0.0000010891912,0.040365666,0.007962927,0.84001994,0.00012280013,0.0026147892,0.00043732947],"about_ca_topic_score_codex":0.00017046738,"about_ca_topic_score_gemma":0.0000017254622,"teacher_disagreement_score":0.15844983,"about_ca_system_score_codex":0.000074623895,"about_ca_system_score_gemma":0.000015784697,"threshold_uncertainty_score":0.40731508},"labels":[],"label_agreement":null},{"id":"W2162703778","doi":"10.1175/bams-d-12-00227.1","title":"The EarthCARE Satellite: The Next Step Forward in Global Measurements of Clouds, Aerosols, Precipitation, and Radiation","year":2014,"lang":"en","type":"article","venue":"Bulletin of the American Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":928,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; Environment and Climate Change Canada","funders":"Japan Aerospace Exploration Agency; Natural Environment Research Council; Sight Research UK","keywords":"Environmental science; Lidar; Aerosol; Remote sensing; Satellite; Meteorology; Cirrus; Cloud top; Geology; Geography; Physics","score_opus":0.013774798741323875,"score_gpt":0.2314669093086736,"score_spread":0.21769211056734974,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2162703778","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":[0.9896103,0.00045734146,0.0003495815,0.0078040757,0.000058245463,0.00031565013,0.0000031831846,0.000009702095,0.001391927],"genre_scores_gemma":[0.9943009,0.00041725766,0.0036079646,0.0015522073,0.000023447788,0.000021474403,6.7811214e-7,0.0000055842274,0.00007048516],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981914,0.0005164291,0.0003165324,0.00022759789,0.00050446676,0.00024356149],"domain_scores_gemma":[0.99885625,0.0003576239,0.00039935508,0.00031850653,0.00002145626,0.000046797813],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012172218,0.00012972353,0.00022656769,2.9993765e-7,0.00023258712,0.000021626676,0.00048304745,0.000054695753,0.00011134422],"category_scores_gemma":[0.00034058225,0.00005983909,0.00016622615,0.00026690288,0.0015728476,0.00001760064,0.00027798832,0.0001368188,0.000009567121],"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":[0.00009512428,0.00006337811,0.85033846,0.0000061830397,0.000038964783,5.251536e-8,0.00039659932,0.00068110053,0.0013018117,0.00024196912,0.0062897387,0.14054663],"study_design_scores_gemma":[0.00027131158,0.0002502579,0.96347374,0.0000059248573,0.000023755874,8.86952e-7,0.0010647549,0.0004902885,0.00023632725,0.0006412899,0.033451222,0.00009022628],"about_ca_topic_score_codex":0.0005388062,"about_ca_topic_score_gemma":0.000049160666,"teacher_disagreement_score":0.14045641,"about_ca_system_score_codex":0.00006476612,"about_ca_system_score_gemma":0.000007780638,"threshold_uncertainty_score":0.57952225},"labels":[],"label_agreement":null},{"id":"W2162982697","doi":"10.1029/2002jd003179","title":"Global monitoring of air pollution over land from the Earth Observing System‐Terra Moderate Resolution Imaging Spectroradiometer (MODIS)","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":612,"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":"AERONET; Aerosol; Moderate-resolution imaging spectroradiometer; Environmental science; Climatology; Particulates; Pollution; Spectroradiometer; Precipitation; Angstrom exponent; Satellite; Air pollution; Air quality index; HYSPLIT; Atmospheric sciences; Meteorology; Geography; Geology","score_opus":0.02427405345422175,"score_gpt":0.2878040570991598,"score_spread":0.26353000364493806,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2162982697","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":[0.9927909,0.00065097114,0.0036992163,0.00027694186,0.00022365023,0.0001352603,0.000009191252,0.000011012157,0.0022028727],"genre_scores_gemma":[0.9952386,0.00004933682,0.0041652704,0.000030423545,0.00041012443,0.0000033392384,5.409119e-7,0.000015600011,0.0000867388],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9967175,0.00053989,0.0004691472,0.00024979218,0.0014747466,0.0005489225],"domain_scores_gemma":[0.9988456,0.00024381962,0.00028623606,0.00032520373,0.00009963217,0.00019954258],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010325991,0.00016896766,0.00031507743,0.000001708983,0.0003316689,0.00008851449,0.00047713576,0.000060096736,0.00025180084],"category_scores_gemma":[0.00024499674,0.000110529385,0.00019461928,0.0006334304,0.00032597224,0.00044899026,0.0001931377,0.00044609295,0.00003416982],"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":[0.00051821966,0.00023412466,0.9491161,0.000025742933,0.00011768014,0.000073757255,0.00037592923,0.026336819,0.015449341,0.0009993998,0.0016467889,0.005106075],"study_design_scores_gemma":[0.00062705175,0.00021074076,0.9796068,0.0001781661,0.000029313098,0.000020792964,0.0011835207,0.013288043,0.0017470777,0.0023391463,0.0006314419,0.00013788856],"about_ca_topic_score_codex":0.0047922544,"about_ca_topic_score_gemma":0.00009883618,"teacher_disagreement_score":0.030490695,"about_ca_system_score_codex":0.0005147058,"about_ca_system_score_gemma":0.00008143492,"threshold_uncertainty_score":0.7244487},"labels":[],"label_agreement":null},{"id":"W2163512993","doi":"10.1029/2002jd003322","title":"A fast, flexible, approximate technique for computing radiative transfer in inhomogeneous cloud fields","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":439,"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":"Radiative transfer; Cloud computing; Statistical physics; Benchmark (surveying); Radiative flux; Parametrization (atmospheric modeling); Scale (ratio); Sampling (signal processing); Computer science; Computational physics; Physics; Environmental science; Meteorology; Applied mathematics; Remote sensing; Mathematics; Geology; Optics; Quantum mechanics","score_opus":0.026435904658052824,"score_gpt":0.3106689354055123,"score_spread":0.2842330307474595,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2163512993","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":[0.7608603,0.00015940798,0.2336357,0.0001855687,0.000098807795,0.0006470455,0.0000028336756,0.00001123477,0.004399107],"genre_scores_gemma":[0.9768587,0.000050679384,0.022170689,0.00007821327,0.00018963248,0.000037726288,4.59499e-7,0.000027526858,0.0005864027],"study_design_codex":"design_other","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9972729,0.00036236853,0.00052986335,0.0002859586,0.0008128021,0.0007360888],"domain_scores_gemma":[0.99871993,0.00063815824,0.00010169146,0.00019325614,0.00009524057,0.00025169883],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016410418,0.00018811795,0.00040563595,0.0000037261116,0.00019116286,0.000055018416,0.00043586825,0.00014244595,0.00048967375],"category_scores_gemma":[0.00041672232,0.00014892712,0.0002172049,0.00068320736,0.00032861804,0.00017600163,0.00009275244,0.00081861793,0.000026376527],"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":[0.007057997,0.010763526,0.16131885,0.0007591142,0.00075488957,0.0017678206,0.017611226,0.20864385,0.22423233,0.047676545,0.04553276,0.27388108],"study_design_scores_gemma":[0.019732913,0.023991954,0.12107554,0.0014171718,0.00017715298,0.0007509668,0.011523353,0.097530045,0.3981219,0.24731961,0.07447918,0.0038802256],"about_ca_topic_score_codex":0.00029825678,"about_ca_topic_score_gemma":0.00007617903,"teacher_disagreement_score":0.27000085,"about_ca_system_score_codex":0.00026024168,"about_ca_system_score_gemma":0.000117111085,"threshold_uncertainty_score":0.60730714},"labels":[],"label_agreement":null},{"id":"W2164008249","doi":"10.5194/acp-10-10017-2010","title":"Comment on \"Classification of aerosol properties derived from AERONET direct sun data\" by Gobbi et al. (2007)","year":2010,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":21,"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 Sherbrooke","funders":"Natural Sciences and Engineering Research Council of Canada; Goddard Space Flight Center; Fonds Québécois de la Recherche sur la Nature et les Technologies; Canadian Foundation for Climate and Atmospheric Sciences; National Aeronautics and Space Administration","keywords":"Aerosol; Angstrom exponent; AERONET; Discretization; Curvature; Space (punctuation); Simple (philosophy); Physics; Mathematics; Mathematical analysis; Meteorology; Geometry","score_opus":0.015272562590512838,"score_gpt":0.22406070301529904,"score_spread":0.2087881404247862,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2164008249","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":[0.9903824,0.00008296039,0.0006131767,0.0015059505,0.0000717864,0.00013119249,0.00009430104,0.0000349924,0.007083296],"genre_scores_gemma":[0.99022967,0.00013888288,0.006035519,0.002481307,0.000058834983,0.000020792317,0.00026761432,0.000022710377,0.0007446923],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9988363,0.00002520253,0.00020954007,0.00047714394,0.00025191493,0.0001999333],"domain_scores_gemma":[0.9989675,0.000058093046,0.00014272593,0.0007181502,0.000009890338,0.00010359059],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00010849882,0.00021179672,0.00021433023,9.244464e-9,0.00010311373,0.000031442778,0.0003640927,0.000081984406,0.0020308068],"category_scores_gemma":[0.000017332699,0.00018116212,0.000032411972,0.000085533706,0.00031738123,0.00015603266,0.00020390646,0.00023166911,0.000040732786],"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":[0.000043451837,0.0003032092,0.007920143,0.00001433637,0.000028739398,5.5787126e-7,0.00018083143,0.000121482146,0.8975236,0.000007699453,0.067978546,0.025877414],"study_design_scores_gemma":[0.0010665937,0.00012957504,0.012555668,0.000059710732,0.000078759294,0.0000020975783,0.0003264253,0.05131201,0.67492896,0.00012827112,0.2585948,0.00081712153],"about_ca_topic_score_codex":0.0007886997,"about_ca_topic_score_gemma":0.00001063032,"teacher_disagreement_score":0.22259462,"about_ca_system_score_codex":0.000028822204,"about_ca_system_score_gemma":0.000014742261,"threshold_uncertainty_score":0.99888146},"labels":[],"label_agreement":null},{"id":"W2164033587","doi":"10.1029/2007jd008443","title":"Simulation of entrainment and transport of dust particles within North America in April 2001 (“Red Dust Episode”)","year":2007,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":38,"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; Entrainment (biomusicology); Atmospheric sciences; Particulates; Mineral dust; Aeolian processes; Wind speed; Meteorology; Geology; Aerosol; Physics; Geomorphology","score_opus":0.026331455238642682,"score_gpt":0.3017384089937219,"score_spread":0.27540695375507923,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2164033587","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":[0.9967001,0.00008139481,0.002437441,0.00015139335,0.000025492856,0.00016559889,0.0000031794852,0.000002954935,0.00043241386],"genre_scores_gemma":[0.9963849,0.00007381661,0.0033746308,0.000023557512,0.000055548215,0.0000018040093,7.7721813e-7,0.00001234689,0.0000725952],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99716103,0.00012853382,0.0007978134,0.00018875867,0.0012409753,0.00048289902],"domain_scores_gemma":[0.99853235,0.0005564278,0.00037410515,0.00016440134,0.00009144431,0.0002812441],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012053231,0.0001305826,0.00038364792,0.000003657759,0.0000606309,0.000009384074,0.00024613854,0.0000637105,0.0005450642],"category_scores_gemma":[0.00028033726,0.00010181441,0.00009924742,0.00064547313,0.000745895,0.00020763102,0.00008535965,0.00039838575,0.0000075368284],"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":[0.00076311827,0.00083401345,0.8636861,0.000033777273,0.000037594655,0.00007396778,0.0014272282,0.089280136,0.014386824,0.00003347917,0.0001551911,0.029288594],"study_design_scores_gemma":[0.00075907796,0.0009241814,0.9688691,0.000056283945,0.000014651303,0.000002406823,0.0011896754,0.024022738,0.0030995605,0.00056353933,0.00039291693,0.000105884676],"about_ca_topic_score_codex":0.0017327688,"about_ca_topic_score_gemma":0.0012911058,"teacher_disagreement_score":0.105183005,"about_ca_system_score_codex":0.0001291451,"about_ca_system_score_gemma":0.000052353007,"threshold_uncertainty_score":0.5968071},"labels":[],"label_agreement":null},{"id":"W2164320060","doi":"10.1175/jas-d-14-0357.1","title":"Clarification of the Water Saturation Represented on Ice Crystal Growth Diagrams","year":2015,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":5,"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 du Québec à Montréal","funders":"Fonds Québécois de la Recherche sur la Nature et les Technologies; Université du Québec à Montréal","keywords":"Supersaturation; Saturation (graph theory); Water vapor; Relative humidity; Ice crystals; Vapor pressure; Humidity; Atmospheric sciences; Thermodynamics; Environmental science; Materials science; Meteorology; Geology; Physics; Mathematics","score_opus":0.02034409057907992,"score_gpt":0.23293732741553136,"score_spread":0.21259323683645143,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2164320060","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":[0.9904106,0.00003359537,0.00025089245,0.005053792,0.0007478659,0.0001134845,2.957172e-7,0.0000045931406,0.0033848763],"genre_scores_gemma":[0.9971745,0.000010138901,0.0016641661,0.00033474786,0.00008333763,0.0000014434687,8.434762e-8,0.000004689018,0.0007268862],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99812245,0.00018129089,0.00034796025,0.00014937248,0.0010210423,0.00017787056],"domain_scores_gemma":[0.9990647,0.000048271333,0.00048577573,0.00027058859,0.00005875072,0.000071942646],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011356191,0.00009516759,0.00012756175,4.0586247e-7,0.00025051733,0.000047625133,0.0009967653,0.00004785544,0.000121307225],"category_scores_gemma":[0.0002547906,0.000033386717,0.00012867831,0.00056297565,0.0006447571,0.00031351348,0.00018942043,0.00017399823,0.000016697702],"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":[0.00019763954,0.00042076036,0.7045172,0.000009067541,0.00004549272,0.0000036219585,0.0051009767,0.1354564,0.12428359,0.0007592293,0.023680512,0.0055255187],"study_design_scores_gemma":[0.0011145093,0.0011543862,0.85513306,0.00011540695,0.00010443452,0.0001428766,0.0045270044,0.026412968,0.0893247,0.011942047,0.009632316,0.00039628992],"about_ca_topic_score_codex":0.00021181439,"about_ca_topic_score_gemma":0.000019038467,"teacher_disagreement_score":0.15061587,"about_ca_system_score_codex":0.00010801653,"about_ca_system_score_gemma":0.000046535657,"threshold_uncertainty_score":0.23756346},"labels":[],"label_agreement":null},{"id":"W2164695358","doi":"10.1002/2014gl062279","title":"Vertical velocities and turbulence in midlatitude anvil cirrus: A comparison between in situ aircraft measurements and ground‐based Doppler cloud radar retrievals","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","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":"McGill University","funders":"U.S. Department of Energy; National Science Foundation","keywords":"Cirrus; Middle latitudes; Radar; Turbulence; Doppler effect; Turbulence kinetic energy; Geology; Lidar; Doppler radar; Atmospheric sciences; Remote sensing; Meteorology; Environmental science; Physics; Astronomy; Aerospace engineering","score_opus":0.050508543848171834,"score_gpt":0.30870986405723233,"score_spread":0.2582013202090605,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2164695358","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":[0.9957233,0.00004573974,0.00055285066,0.0029661914,0.000029195346,0.00029405995,0.0000019642569,0.000016209793,0.0003704568],"genre_scores_gemma":[0.9981849,0.0000089744735,0.0009538716,0.00068863505,0.000097477336,0.0000251799,0.000004230607,0.000016571796,0.00002016085],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99661815,0.00047928636,0.00031289304,0.0005699,0.0012514489,0.00076829595],"domain_scores_gemma":[0.99885863,0.00058910187,0.000028938253,0.00025662722,0.000013639489,0.000253052],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012534796,0.00019194899,0.00035882182,0.000013746091,0.00015252258,0.00008880575,0.00027567553,0.00009390706,0.00006218942],"category_scores_gemma":[0.00024549707,0.00017546171,0.000034608867,0.00047351178,0.0010768666,0.0001935991,0.00033445007,0.00061569695,0.000071054055],"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":[0.00018308732,0.00021934819,0.9164429,0.000053201024,0.000015027527,0.000019206305,0.0010927748,0.00019686321,0.07291327,0.00007848994,0.0016304277,0.0071554156],"study_design_scores_gemma":[0.0010572999,0.00019467002,0.99265563,0.00006371326,0.000006052819,5.030144e-7,0.00013374648,0.0032998908,0.0013209877,0.0005151687,0.000527557,0.00022475918],"about_ca_topic_score_codex":0.0025243044,"about_ca_topic_score_gemma":0.00038481745,"teacher_disagreement_score":0.076212764,"about_ca_system_score_codex":0.00026575147,"about_ca_system_score_gemma":0.000020010553,"threshold_uncertainty_score":0.7155121},"labels":[],"label_agreement":null},{"id":"W2165690655","doi":"10.1002/qj.824","title":"A 3D cloud‐construction algorithm for the EarthCARE satellite mission","year":2011,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":140,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Government of Canada; Environment and Climate Change Canada","funders":"Natural Environment Research Council; Sight Research UK; European Space Agency","keywords":"Radiative transfer; Remote sensing; Pixel; Algorithm; Moderate-resolution imaging spectroradiometer; Satellite; Cloud top; Computer science; Atmospheric radiative transfer codes; Environmental science; Cloud computing; Nadir; Meteorology; Geology; Physics; Artificial intelligence; Optics","score_opus":0.018711222937282876,"score_gpt":0.21959241650872824,"score_spread":0.20088119357144535,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2165690655","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":[0.8402687,0.0008782761,0.15269563,0.001617493,0.0019276276,0.00052957365,0.00000779456,0.000031507123,0.0020434463],"genre_scores_gemma":[0.8641178,0.000051523082,0.13443469,0.00062418566,0.00037228508,0.000006608004,2.2918013e-7,0.000012200714,0.00038045686],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99863046,0.00014225305,0.00036890907,0.00016919592,0.000405667,0.00028352113],"domain_scores_gemma":[0.9991247,0.00014880385,0.00036710838,0.00021330445,0.00003432407,0.00011176262],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007218502,0.00015415467,0.00020568618,5.8427355e-7,0.0004255158,0.00002959357,0.0005587072,0.00015747648,0.001192744],"category_scores_gemma":[0.000024359775,0.000065870874,0.0006485076,0.00010280135,0.00042596503,0.00007979482,0.00006827836,0.0003583698,0.000018791952],"study_design_candidate":"design_other","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":[0.00007941221,0.000083235835,0.008289857,0.0000031150032,0.000085518215,0.0000022931008,0.002032292,0.00016876779,0.00032710552,0.000076080476,0.0013993524,0.987453],"study_design_scores_gemma":[0.005507944,0.017149828,0.5843649,0.00012937053,0.0014163207,0.0006381026,0.026698591,0.13480747,0.0027267325,0.051821228,0.17313361,0.0016059377],"about_ca_topic_score_codex":0.000028786131,"about_ca_topic_score_gemma":0.0000019259999,"teacher_disagreement_score":0.98584706,"about_ca_system_score_codex":0.000064729546,"about_ca_system_score_gemma":0.00001213742,"threshold_uncertainty_score":0.9997203},"labels":[],"label_agreement":null},{"id":"W2166713864","doi":"10.1175/jas3674.1","title":"Aerosol Optical Properties and Particle Size Distributions on the East Coast of the United States Derived from Airborne In Situ and Remote Sensing Measurements","year":2006,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":26,"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; Environmental science; Troposphere; Atmospheric sciences; Spectroradiometer; Transect; Effective radius; Single-scattering albedo; Sun photometer; Albedo (alchemy); Remote sensing; Meteorology; Geology; Oceanography; Geography; Physics","score_opus":0.030270457131655052,"score_gpt":0.21636238924909157,"score_spread":0.18609193211743652,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2166713864","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":[0.99401516,0.000119167824,0.00016784765,0.0054056225,0.00009161037,0.0001157692,0.0000016371196,0.0000028776224,0.000080339356],"genre_scores_gemma":[0.9972823,0.000023857427,0.00241359,0.00022981186,0.0000205562,2.8325925e-7,6.747019e-8,0.000003891397,0.000025626912],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9986608,0.00016495006,0.00030335732,0.00013641176,0.0005390789,0.0001953699],"domain_scores_gemma":[0.9993372,0.00017675958,0.0002637044,0.00015010983,0.000026100748,0.00004611917],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00058743596,0.00010391716,0.00014147315,3.2061507e-7,0.00041480165,0.00006882602,0.00032052165,0.00002620261,0.000021604354],"category_scores_gemma":[0.00021698824,0.00004281448,0.000047417725,0.000541259,0.0013418043,0.00011745987,0.00021099675,0.00014069185,9.026123e-7],"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":[0.00014059363,0.00020072723,0.4109049,0.000006429742,0.000038351107,0.000005138619,0.0024122423,0.062875554,0.51651144,0.00006916509,0.00040048626,0.006434953],"study_design_scores_gemma":[0.00041464737,0.000140529,0.90126497,0.00015917055,0.000037894173,0.000017989118,0.0033786343,0.045378204,0.04780224,0.0012423971,0.00004973467,0.000113585826],"about_ca_topic_score_codex":0.0021398084,"about_ca_topic_score_gemma":0.000811136,"teacher_disagreement_score":0.49036008,"about_ca_system_score_codex":0.00006097445,"about_ca_system_score_gemma":0.00002813517,"threshold_uncertainty_score":0.4943934},"labels":[],"label_agreement":null},{"id":"W2167280668","doi":"10.5194/acp-10-1511-2010","title":"Influences of in-cloud aerosol scavenging parameterizations on aerosol concentrations and wet deposition in ECHAM5-HAM","year":2010,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":156,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"BioFrontiers Institute, University of Colorado Boulder; National Oceanic and Atmospheric Administration; Killam Trusts","keywords":"Aerosol; Scavenging; Atmospheric sciences; Ice nucleus; Ice crystals; Troposphere; Deposition (geology); Nucleation; Chemistry; Environmental science; Meteorology; Climatology; Geology; Physics","score_opus":0.004830497098746221,"score_gpt":0.20881103742016532,"score_spread":0.2039805403214191,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2167280668","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":[0.9975128,0.000019707453,0.00059154077,0.00004148175,0.00003645802,0.00012103968,0.000006252343,0.0000124441085,0.0016582852],"genre_scores_gemma":[0.99439245,0.00006687264,0.0053108567,0.00005438686,0.000037020636,0.0000147206765,0.0000102440945,0.000008998319,0.00010445792],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9992149,0.0000141786995,0.00021462102,0.00025361087,0.00012428503,0.00017839216],"domain_scores_gemma":[0.9996292,0.000059342823,0.00008160671,0.0001567103,0.00000612392,0.000067000314],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000058809026,0.0001375275,0.00015763528,3.9199787e-8,0.00008488043,0.000025034835,0.00008210553,0.000088099754,0.00028563102],"category_scores_gemma":[0.000016518788,0.00013876808,0.000022993647,0.00024482867,0.00026791779,0.00013744373,0.000044954282,0.00019804973,0.0000048739403],"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":[0.000019462728,0.00019847747,0.25939602,0.000040790346,0.0000072650264,0.0000038667686,0.0006974707,0.011187521,0.70814544,0.00010077882,0.000016349226,0.020186568],"study_design_scores_gemma":[0.0023428474,0.00020305315,0.19163308,0.00027133853,0.00005441953,0.000029265017,0.0009974636,0.15804468,0.6436764,0.0014343039,0.0001742177,0.001138933],"about_ca_topic_score_codex":0.00018139787,"about_ca_topic_score_gemma":0.000049704995,"teacher_disagreement_score":0.14685717,"about_ca_system_score_codex":0.000023999482,"about_ca_system_score_gemma":0.0000128081965,"threshold_uncertainty_score":0.56587976},"labels":[],"label_agreement":null},{"id":"W2167570928","doi":"10.1175/jamc-d-13-0182.1","title":"First Observations of Tracking Clouds Using Scanning ARM Cloud Radars","year":2014,"lang":"en","type":"article","venue":"Journal of Applied Meteorology and Climatology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; Fisheries and Oceans Canada","funders":"U.S. Department of Energy","keywords":"Cloud computing; Radar; Remote sensing; Meteorology; Cloud top; Precipitation; Environmental science; Context (archaeology); Tracking (education); Computer science; Geology; Geography; Telecommunications","score_opus":0.020515365331080948,"score_gpt":0.24053548464835153,"score_spread":0.22002011931727058,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2167570928","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":[0.98884434,0.00012066091,0.0083187735,0.00036045982,0.0002991585,0.000063219384,8.068758e-7,0.0000067787037,0.0019858317],"genre_scores_gemma":[0.9721291,0.00007171018,0.027278805,0.0004172586,0.00008117038,0.00000150632,5.277673e-7,0.000012425947,0.0000074622494],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998714,0.000066576984,0.00061513355,0.0001756223,0.0001463514,0.00028230343],"domain_scores_gemma":[0.99878806,0.00025544892,0.000694908,0.00013820738,0.000025813053,0.00009753459],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006916052,0.00014031473,0.0005098912,0.0000082130955,0.00019058271,0.0000070564224,0.00020661573,0.00019384045,0.0002726503],"category_scores_gemma":[0.00006794079,0.00012062891,0.00008363841,0.00015715095,0.0005223271,0.000088430046,0.00011192342,0.00027167363,0.0000044551884],"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":[0.0008037482,0.00036162662,0.84217936,0.000080291145,0.00022061725,0.00003210718,0.002366282,0.025172258,0.073248625,0.0474788,0.0005984558,0.007457854],"study_design_scores_gemma":[0.008217795,0.0030501522,0.82604486,0.00013999223,0.0012347028,0.0036818685,0.004643377,0.031220458,0.012307983,0.07514548,0.033014156,0.001299153],"about_ca_topic_score_codex":0.000025357824,"about_ca_topic_score_gemma":0.000030093954,"teacher_disagreement_score":0.060940646,"about_ca_system_score_codex":0.00003288205,"about_ca_system_score_gemma":0.000017793496,"threshold_uncertainty_score":0.4919104},"labels":[],"label_agreement":null},{"id":"W2168543820","doi":"10.1175/jtech-d-11-00202.1","title":"Evaluation of EarthCARE Cloud Profiling Radar Doppler Velocity Measurements in Particle Sedimentation Regimes","year":2013,"lang":"en","type":"article","venue":"Journal of Atmospheric and Oceanic Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":105,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Institute on Aging; Natural Environment Research Council; Sight Research UK; U.S. Department of Energy","keywords":"Doppler effect; Remote sensing; Doppler radar; Environmental science; Radar; Cirrus; Meteorology; Geology; Computer science; Physics","score_opus":0.021158871038190103,"score_gpt":0.2520708256565294,"score_spread":0.23091195461833927,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2168543820","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":[0.9974802,0.0007784832,0.00060271943,0.00048673464,0.00010402103,0.0002513392,2.482544e-7,0.000011746077,0.00028446602],"genre_scores_gemma":[0.9810749,0.00006652062,0.018751847,0.000041441603,0.000021368212,0.000006460411,2.3227348e-7,0.000008370092,0.000028803634],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99850357,0.00009017647,0.00046730947,0.00014805635,0.00060397945,0.0001868976],"domain_scores_gemma":[0.9992729,0.00001766326,0.00040624343,0.00012527705,0.00012635012,0.000051570947],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00096973963,0.00010469294,0.00022066974,0.0000016629803,0.00004555763,0.000009744784,0.00014527136,0.00011490004,0.000639589],"category_scores_gemma":[0.000107509455,0.00008575315,0.00003822862,0.00040283817,0.00016777628,0.00024245697,0.00007304527,0.00016578354,0.000011569637],"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":[0.000030947234,0.00013957563,0.8377121,0.000011194124,0.000048391586,0.0000025527224,0.00039753516,0.00089818053,0.029675772,0.0001354223,0.0005201746,0.13042814],"study_design_scores_gemma":[0.0034420763,0.0008254269,0.90602744,0.00008932206,0.00019008624,0.00010564655,0.005942083,0.02520878,0.048548874,0.009117706,0.00020643379,0.00029614172],"about_ca_topic_score_codex":0.00008723732,"about_ca_topic_score_gemma":0.000011822815,"teacher_disagreement_score":0.13013199,"about_ca_system_score_codex":0.00017529202,"about_ca_system_score_gemma":0.000047734924,"threshold_uncertainty_score":0.7003051},"labels":[],"label_agreement":null},{"id":"W2169181468","doi":"10.1051/0004-6361/201116489","title":"<i>Planck</i>early results. XII. Cluster Sunyaev-Zeldovich optical scaling relations","year":2011,"lang":"en","type":"article","venue":"Astronomy and Astrophysics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":122,"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 British Columbia; University of Toronto","funders":"Centre National de la Recherche Scientifique; Partenariat Canadien Contre Le Cancer; Centre National d’Etudes Spatiales; National Aeronautics and Space Administration","keywords":"Physics; Planck; Astrophysics; Scaling; Cluster (spacecraft); Cosmic microwave background; Astronomy; Optics","score_opus":0.008969719797616968,"score_gpt":0.18428834822609097,"score_spread":0.175318628428474,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2169181468","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":[0.8387178,0.0000069495272,0.114577785,0.00008611482,0.00007517297,0.0001060306,0.000008343484,0.00003570759,0.04638609],"genre_scores_gemma":[0.8204074,0.0000011892713,0.17887165,0.000061001163,0.00009573618,0.0000076859305,0.000010146209,0.000013484931,0.0005317263],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99897486,0.000022440337,0.0002189435,0.00032243982,0.00014035765,0.0003209335],"domain_scores_gemma":[0.9995152,0.000028448463,0.00007532553,0.00022265891,0.000006657308,0.0001517425],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007806176,0.00015902641,0.00013963673,0.0000014037963,0.00020599707,0.0000352432,0.00013978984,0.000060327093,0.00037208103],"category_scores_gemma":[0.000005776538,0.00014564033,0.00005567803,0.00010258854,0.00020560392,0.00026997703,0.00018278287,0.00019413428,0.00048599392],"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":[0.00033872735,0.00033964787,0.5433936,0.000004983652,0.000062852065,0.000010051263,0.002659322,0.0021327112,0.0005940411,0.004845389,0.0017816811,0.44383696],"study_design_scores_gemma":[0.0014555249,0.00051876396,0.9642512,0.000022784736,0.00007628938,0.000007068562,0.0005150746,0.0008948202,0.0008297749,0.0012212356,0.029664082,0.00054335414],"about_ca_topic_score_codex":0.00023306617,"about_ca_topic_score_gemma":0.000010115586,"teacher_disagreement_score":0.4432936,"about_ca_system_score_codex":0.000031052972,"about_ca_system_score_gemma":0.000009012948,"threshold_uncertainty_score":0.62466305},"labels":[],"label_agreement":null},{"id":"W2171450686","doi":"10.5194/amtd-4-5275-2011","title":"Contrasting aerosol trends over South Asia during the last decade based on MODIS observations","year":2011,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":111,"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","funders":"","keywords":"Aerosol; Environmental science; Climatology; Precipitation; Monsoon; Satellite; Climate change; Geography; South asia; Atmospheric sciences; Physical geography; Meteorology; Geology; Oceanography","score_opus":0.026681520980638744,"score_gpt":0.21105736683653042,"score_spread":0.18437584585589167,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2171450686","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":[0.88889986,0.0000020167927,0.0030699421,0.00012954387,0.000048756057,0.0000781286,0.0000044460503,0.00006631407,0.107700996],"genre_scores_gemma":[0.99277544,4.5505323e-7,0.0024011207,0.0006100264,0.000033283177,0.000023780949,0.0000017890744,0.000015695654,0.0041384264],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99905336,0.000026454773,0.00015909756,0.00024250774,0.00023883504,0.00027974308],"domain_scores_gemma":[0.99954057,0.00003823378,0.00006571273,0.0002705771,0.0000035294493,0.00008137944],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000088262954,0.00013643406,0.00009144529,0.0000012553522,0.00033254994,0.000026452975,0.0002293986,0.000049843715,0.010866413],"category_scores_gemma":[0.000019584795,0.00008614937,0.00006682814,0.00023291617,0.00012107252,0.0001056701,0.00007825052,0.000121512094,0.00017488938],"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":[0.00003105012,0.00012000964,0.9849074,0.000002568526,0.0000118791695,0.000004598733,0.0014061845,0.00508897,0.005084798,0.00041776255,0.0007753726,0.0021493945],"study_design_scores_gemma":[0.0003266521,0.00003722498,0.9752754,0.0000057888496,0.000010560424,7.3345916e-7,0.00031166343,0.021858744,0.001850149,0.000016933172,0.00017147211,0.00013467285],"about_ca_topic_score_codex":0.00028791762,"about_ca_topic_score_gemma":0.00020873045,"teacher_disagreement_score":0.10387556,"about_ca_system_score_codex":0.00006457872,"about_ca_system_score_gemma":0.000005558988,"threshold_uncertainty_score":0.9900378},"labels":[],"label_agreement":null},{"id":"W2172149670","doi":"10.5194/acp-10-51-2010","title":"Comparison of in situ and columnar aerosol spectral measurements during TexAQS-GoMACCS 2006: testing parameterizations for estimating aerosol fine mode properties","year":2010,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":21,"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 de Sherbrooke","funders":"National Oceanic and Atmospheric Administration; NOAA Research; Houston Advanced Research Center; Texas Commission on Environmental Quality","keywords":"AERONET; Angstrom exponent; Aerosol; Atmospheric sciences; Environmental science; Effective radius; Extinction (optical mineralogy); Wavelength; Optical depth; Remote sensing; Meteorology; Astrophysics; Physics; Optics; Geography","score_opus":0.028363022036337608,"score_gpt":0.25942460870983036,"score_spread":0.23106158667349275,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2172149670","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":[0.9949757,0.00003319231,0.0038895302,0.000017132106,0.000033318498,0.0002801808,0.0000071274235,0.000026126001,0.00073773536],"genre_scores_gemma":[0.8343688,0.0000017158058,0.16529186,0.000008432985,0.00006036966,0.000043896267,0.000005962491,0.000017783024,0.00020117195],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99889976,0.000010029298,0.00032019365,0.00032110763,0.00017201726,0.00027687548],"domain_scores_gemma":[0.99950635,0.000052989584,0.00016173397,0.0001738591,0.000020399342,0.0000846641],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007788734,0.00019483156,0.00028171216,4.274691e-8,0.00020431953,0.00003948713,0.000120631725,0.000080365615,0.000077439356],"category_scores_gemma":[0.00008172252,0.00019266341,0.000032638498,0.00018197551,0.00023904057,0.00014495468,0.000092891416,0.00017654743,0.00000128803],"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":[0.000018277133,0.000115805335,0.2580598,0.00012239855,0.000008229532,3.6270825e-7,0.00035806338,0.012383073,0.7212379,0.0000010502821,0.000010808093,0.0076841936],"study_design_scores_gemma":[0.0007585639,0.00006437308,0.02339584,0.00008173844,0.000033844528,0.000006298482,0.00013478936,0.44674316,0.5283477,0.000104026185,0.000007309392,0.0003223718],"about_ca_topic_score_codex":0.00023235338,"about_ca_topic_score_gemma":0.000085049156,"teacher_disagreement_score":0.4343601,"about_ca_system_score_codex":0.000033454686,"about_ca_system_score_gemma":0.000017320503,"threshold_uncertainty_score":0.7856586},"labels":[],"label_agreement":null},{"id":"W2174329979","doi":"10.5194/acp-16-4725-2016","title":"Long-range transport and mixing of aerosol sources during the 2013 North American biomass burning episode: analysis of multiple lidar observations in the western Mediterranean basin","year":2016,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":77,"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":"Centre National de la Recherche Scientifique; Ministerio de Ciencia e Innovación; Centre National d’Etudes Spatiales","keywords":"Aerosol; Lidar; Environmental science; Mineral dust; Atmospheric sciences; Mediterranean climate; Outflow; Climatology; Troposphere; Meteorology; Geology; Geography; Remote sensing","score_opus":0.010236460844654863,"score_gpt":0.20419224508564354,"score_spread":0.1939557842409887,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2174329979","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":[0.997618,0.00007559069,0.0019112544,0.0002238038,0.0000068302165,0.00009427589,0.000020350772,0.000007996546,0.00004184862],"genre_scores_gemma":[0.99872,0.00012137539,0.0009136262,0.000036830555,0.000032126765,0.000012410513,0.0000061768887,0.000009957887,0.00014748263],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990482,0.000034708963,0.00027113198,0.00024079245,0.00021962923,0.00018557787],"domain_scores_gemma":[0.9992763,0.00018728556,0.0002148332,0.00026556355,0.000009897102,0.000046165256],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000120949626,0.00015441391,0.00028158957,9.754056e-8,0.00012404741,0.000010675989,0.00022807016,0.00003096112,0.000081218735],"category_scores_gemma":[0.000008538501,0.00008721348,0.00008488805,0.00072376017,0.00062300934,0.000111066096,0.000050087157,0.000081826336,5.2685846e-7],"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":[0.00001533537,0.000048478163,0.97370315,0.00003597637,0.00007740617,0.0000018803319,0.0019240871,0.000795365,0.016899876,2.521597e-7,0.0000032567311,0.006494928],"study_design_scores_gemma":[0.0002523169,0.000017038383,0.9924615,0.00002287256,0.00014963627,0.0000016146176,0.0003516433,0.0030341372,0.003531209,0.0000035644512,0.00005204604,0.00012239754],"about_ca_topic_score_codex":0.0030159114,"about_ca_topic_score_gemma":0.0013577704,"teacher_disagreement_score":0.018758364,"about_ca_system_score_codex":0.000018970106,"about_ca_system_score_gemma":0.0000058368064,"threshold_uncertainty_score":0.4559176},"labels":[],"label_agreement":null},{"id":"W2175026245","doi":"10.1002/2015jd023632","title":"On the aerosol and cloud phase function expansion moments for radiative transfer simulations","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","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":"Environment and Climate Change Canada","funders":"","keywords":"Radiative transfer; Radiative flux; Aerosol; Atmospheric radiative transfer codes; Radiative forcing; Computational physics; Atmospheric sciences; Physics; Meteorology; Optics","score_opus":0.06146066136131515,"score_gpt":0.3457965246945153,"score_spread":0.2843358633332001,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2175026245","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":[0.9858282,0.00006369668,0.012008365,0.0010554302,0.0001744648,0.00037899666,0.00000748774,0.000005358625,0.00047797404],"genre_scores_gemma":[0.99840575,0.000019664392,0.0003755738,0.00016000406,0.00038577782,0.000017046958,0.0000012086741,0.000015233282,0.00061970984],"study_design_codex":"not_applicable","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9980292,0.00021704656,0.00025877007,0.00017991597,0.0009890385,0.00032604975],"domain_scores_gemma":[0.9982993,0.0010386208,0.000069500195,0.00015467736,0.00013152891,0.0003063454],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00077540806,0.00012080345,0.00018349742,0.0000013165285,0.00031501695,0.00006489944,0.00020899005,0.000055129873,0.00043382772],"category_scores_gemma":[0.00052224,0.00007066428,0.000096727155,0.00026386805,0.00033174397,0.00023805513,0.00006619675,0.00037161648,0.000049733855],"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":[0.028369369,0.010241642,0.01218597,0.000075648546,0.000805889,0.000081151695,0.014152481,0.11474835,0.12080906,0.029247116,0.45766485,0.21161847],"study_design_scores_gemma":[0.044970244,0.087515004,0.06477809,0.00044932132,0.0004309977,0.000040191855,0.01745239,0.35384896,0.025263183,0.28835425,0.115045935,0.0018514416],"about_ca_topic_score_codex":0.00010172676,"about_ca_topic_score_gemma":0.000021441016,"teacher_disagreement_score":0.3426189,"about_ca_system_score_codex":0.00015673271,"about_ca_system_score_gemma":0.00006345802,"threshold_uncertainty_score":0.47501093},"labels":[],"label_agreement":null},{"id":"W2175526908","doi":"10.1175/1520-0469(2002)059<3130:potopo>2.0.co;2","title":"Parameterization of the Optical Properties of Sulfate Aerosols in the Infrared","year":2002,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":13,"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":"Aerosol; Forcing (mathematics); Radiative forcing; Atmospheric sciences; Sulfate aerosol; Sulfate; Infrared; Ammonium sulfate; Environmental science; Meteorology; Materials science; Physics; Optics","score_opus":0.026705881122457427,"score_gpt":0.21001874069301205,"score_spread":0.18331285957055463,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2175526908","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":[0.99535865,0.00023609324,0.00005126656,0.0016783744,0.00022636841,0.00014837735,3.0163415e-7,0.0000016664749,0.0022989025],"genre_scores_gemma":[0.9973834,0.00006138888,0.0020491679,0.00022639081,0.000022584052,0.0000023810273,6.669072e-9,0.0000037687655,0.00025088433],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981671,0.00018486311,0.0004981062,0.00010808731,0.00085882546,0.00018304308],"domain_scores_gemma":[0.99900556,0.00007844397,0.00060523575,0.00025978332,0.000023195962,0.00002778188],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008773253,0.000094981064,0.00018358375,4.658095e-7,0.00017598638,0.00003558092,0.0014133209,0.000038306207,0.00025124583],"category_scores_gemma":[0.00026062137,0.000035346304,0.0001369279,0.00106864,0.0014857056,0.00025004364,0.00020345945,0.0001531911,0.000003894205],"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":[0.00006909696,0.000612105,0.6765749,0.000032901935,0.000034906614,0.0000042019656,0.009377512,0.1637884,0.1391325,0.00057848747,0.002074529,0.0077204667],"study_design_scores_gemma":[0.00076707394,0.00075993745,0.893834,0.00034294632,0.000075760036,0.00012639347,0.0054461006,0.05975736,0.034909,0.0027665864,0.00093377737,0.00028105397],"about_ca_topic_score_codex":0.00006972171,"about_ca_topic_score_gemma":0.000012724937,"teacher_disagreement_score":0.21725911,"about_ca_system_score_codex":0.000038042144,"about_ca_system_score_gemma":0.000026337435,"threshold_uncertainty_score":0.5474144},"labels":[],"label_agreement":null},{"id":"W2175592999","doi":"10.1117/12.2195479","title":"Langley Mobile Ozone Lidar (LMOL) results from the Denver, CO DISCOVER-AQ campaign","year":2015,"lang":"en","type":"article","venue":"Proceedings of SPIE, the International Society for Optical Engineering/Proceedings of SPIE","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Lidar; Environmental science; Ozone; Air quality index; Meteorology; Aerosol; Planetary boundary layer; Troposphere; Remote sensing; Tropospheric ozone; Atmospheric sciences; Geography; Geology","score_opus":0.012177908838990382,"score_gpt":0.22391754238653325,"score_spread":0.21173963354754285,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2175592999","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":[0.9893762,0.000110695386,0.000047314916,0.0017115964,0.00024108891,0.0005439644,0.00016942213,0.0000690629,0.0077306866],"genre_scores_gemma":[0.95735705,0.00008532601,0.040314957,0.00032764053,0.0006004365,0.00017233385,0.000029505323,0.00006678691,0.0010459623],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.9974663,3.520356e-8,0.0006162348,0.00046564502,0.0010299516,0.00042179617],"domain_scores_gemma":[0.9988176,0.00020550076,0.00037625918,0.000108308064,0.0002922076,0.0002001096],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00075193367,0.0003168193,0.00034070626,0.000004711701,0.000121411926,0.00012849884,0.0013261755,0.00017541193,0.00007449924],"category_scores_gemma":[0.00057261705,0.00021311417,0.00042511593,0.0002810288,0.00044942467,0.00051050505,0.00037425748,0.00032130373,0.000026617941],"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":[0.0014509365,0.00094635255,0.03737465,0.00019411738,0.0012337972,0.0000014245265,0.007598691,0.004078535,0.5676045,0.1174606,0.2601025,0.00195389],"study_design_scores_gemma":[0.019705389,0.004838934,0.08194366,0.0014162413,0.0014835086,0.00010595134,0.06460167,0.1206468,0.32416484,0.017516525,0.3587164,0.004860088],"about_ca_topic_score_codex":0.00029046246,"about_ca_topic_score_gemma":0.0000020985383,"teacher_disagreement_score":0.24343966,"about_ca_system_score_codex":0.0002887443,"about_ca_system_score_gemma":0.000030695202,"threshold_uncertainty_score":0.8690543},"labels":[],"label_agreement":null},{"id":"W2180046150","doi":"10.1175/jam2423.1","title":"A New Visibility Parameterization for Warm-Fog Applications in Numerical Weather Prediction Models","year":2006,"lang":"en","type":"article","venue":"Journal of Applied Meteorology and Climatology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":263,"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":"Visibility; Mesoscale meteorology; Meteorology; Environmental science; Numerical weather prediction; Liquid water content; Computer science; Cloud computing; Physics","score_opus":0.007305642536763587,"score_gpt":0.22494802757859608,"score_spread":0.2176423850418325,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2180046150","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":[0.5894225,0.000064678134,0.40857524,0.00021054792,0.000043457647,0.00022711582,0.0000025275713,0.000007428546,0.0014464943],"genre_scores_gemma":[0.96412957,0.00003454338,0.0355527,0.0001457139,0.000051445768,0.0000446977,0.0000057842085,0.00000876018,0.000026809721],"study_design_codex":"observational","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9990099,0.000034672474,0.000463389,0.00020596928,0.000081753285,0.00020433789],"domain_scores_gemma":[0.99944514,0.00012584627,0.0002517992,0.00010204422,0.000010454349,0.00006472005],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000275203,0.0001059548,0.00030080692,0.000007300349,0.000067319255,0.000006444428,0.0001025638,0.00018368698,0.00012887106],"category_scores_gemma":[0.000008664177,0.00008694646,0.000054128715,0.00012947089,0.00012505925,0.00009271788,0.00003850834,0.00014255206,0.000003939177],"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":[0.0027770817,0.0010717731,0.71866584,0.00005444842,0.000101584774,0.000010407562,0.0009794331,0.07472104,0.028083209,0.13187535,0.0026456658,0.039014168],"study_design_scores_gemma":[0.004714466,0.0010343511,0.18224494,0.000007668619,0.00021893666,0.0002599827,0.0004112111,0.04558433,0.001395585,0.75293416,0.010808563,0.0003858209],"about_ca_topic_score_codex":0.00004176916,"about_ca_topic_score_gemma":0.000027746468,"teacher_disagreement_score":0.62105876,"about_ca_system_score_codex":0.00004447192,"about_ca_system_score_gemma":0.000018422052,"threshold_uncertainty_score":0.35455737},"labels":[],"label_agreement":null},{"id":"W2180100829","doi":"10.1175/1520-0426(2001)018<1429:rhsold>2.0.co;2","title":"Range–Height Scans of Lidar Depolarization for Characterizing Properties and Phase of Clouds and Precipitation","year":2001,"lang":"en","type":"article","venue":"Journal of Atmospheric and Oceanic Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"","keywords":"Lidar; Precipitation; Backscatter (email); Elevation (ballistics); Snow; Scattering; Depolarization; Phase (matter); Ranging; Optics; Materials science; Remote sensing; Range (aeronautics); Environmental science; Geology; Physics; Meteorology; Geodesy","score_opus":0.012789074575973947,"score_gpt":0.22830020749042237,"score_spread":0.21551113291444843,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2180100829","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":[0.9824924,0.0019917632,0.014887566,0.00036119696,0.000049177954,0.00016082429,0.0000018851672,0.000009315484,0.00004590171],"genre_scores_gemma":[0.98285455,0.0015928425,0.015438146,0.000030542866,0.000022209386,0.0000024049125,3.7475615e-7,0.000010524722,0.00004842715],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992223,0.000016529268,0.00039488793,0.00012572709,0.000110247725,0.00013031016],"domain_scores_gemma":[0.9993283,0.000026419042,0.00048268834,0.00007668341,0.00003957227,0.000046320165],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017029351,0.00010303587,0.0002795435,0.0000021901803,0.00006748671,0.000008710697,0.0000869463,0.00012122482,0.000029046858],"category_scores_gemma":[0.000051499403,0.0000789842,0.00003153113,0.00020360219,0.00033650783,0.00018713827,0.00006167344,0.00008985689,1.518997e-7],"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":[0.0005741249,0.00023671435,0.4984609,0.000115840034,0.00007911208,0.0000065573618,0.0013775422,0.000029041961,0.30915037,0.00049250276,0.000059595783,0.1894177],"study_design_scores_gemma":[0.016199177,0.014509727,0.80827856,0.00067043834,0.0008371416,0.0018804405,0.0092321895,0.03053571,0.09856019,0.0075534265,0.010691754,0.0010512377],"about_ca_topic_score_codex":0.000012383302,"about_ca_topic_score_gemma":0.000003270205,"teacher_disagreement_score":0.30981767,"about_ca_system_score_codex":0.000021736296,"about_ca_system_score_gemma":0.00001509055,"threshold_uncertainty_score":0.3220882},"labels":[],"label_agreement":null},{"id":"W2180244580","doi":"10.1016/j.atmosenv.2015.10.058","title":"Trend estimates of AERONET-observed and model-simulated AOTs between 1993 and 2013","year":2015,"lang":"en","type":"article","venue":"Atmospheric Environment","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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 Toronto","funders":"","keywords":"AERONET; Aerosol; Environmental science; Atmospheric sciences; Percentile; Outlier; Satellite; Skewness; Climatology; Meteorology; Statistics; Mathematics; Geography","score_opus":0.026234213839224824,"score_gpt":0.21951460805008668,"score_spread":0.19328039421086185,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2180244580","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":[0.9937824,0.0008967749,0.004203467,0.00016183352,0.000026291,0.00023274227,0.000008748574,0.000035969177,0.000651781],"genre_scores_gemma":[0.94410634,0.0003607797,0.054738738,0.000069143134,0.000018261268,0.000010701744,0.000013374082,0.00003305723,0.0006496088],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99839383,0.000036762438,0.00035847086,0.00047772305,0.00038047912,0.00035272085],"domain_scores_gemma":[0.9990878,0.000056368317,0.00016163388,0.00033688667,0.0000018932003,0.0003554325],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0001913314,0.00028648713,0.00036822553,3.870505e-7,0.000083533916,0.000018271661,0.00016804357,0.00012058965,0.00048046117],"category_scores_gemma":[0.000010684647,0.00025142918,0.000041255407,0.00010128262,0.0004964011,0.00017899217,0.00042985534,0.00010851345,0.000055832556],"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":[0.000030062312,0.000110983,0.7928013,0.0000132449695,0.00004974496,0.0000052396435,0.00091244746,0.19016398,0.0009198868,0.000018465149,0.0012353212,0.013739299],"study_design_scores_gemma":[0.0014415617,0.0004398024,0.6539761,0.000018629651,0.0001347695,0.000006430651,0.0002095704,0.337842,0.00025718135,0.0013680091,0.0037770134,0.00052895193],"about_ca_topic_score_codex":0.0011811709,"about_ca_topic_score_gemma":0.000027276665,"teacher_disagreement_score":0.147678,"about_ca_system_score_codex":0.00011157901,"about_ca_system_score_gemma":0.0000066166813,"threshold_uncertainty_score":0.9999938},"labels":[],"label_agreement":null},{"id":"W2180409831","doi":"10.1175/1520-0450(2000)039<1434:asbcdo>2.0.co;2","title":"A Satellite-Based Climatic Description of Jet Aircraft Contrails and Associations with Atmospheric Conditions, 1977–79","year":2000,"lang":"en","type":"article","venue":"Journal of Applied Meteorology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":30,"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":"Climatology; Environmental science; Cloud cover; Satellite; Troposphere; Jet stream; Meteorology; Geography; Geology; Jet (fluid)","score_opus":0.0074394830327400826,"score_gpt":0.20833097850560953,"score_spread":0.20089149547286944,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2180409831","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":[0.99155927,0.00012001418,0.002702196,0.00030493378,0.00003198763,0.00016787846,0.0000075628864,0.00000922615,0.0050969156],"genre_scores_gemma":[0.970016,0.00012028157,0.029202543,0.0005439222,0.000025436102,0.000009466715,0.0000044831436,0.000012123799,0.00006571527],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998845,0.00006160253,0.0004868667,0.00014029688,0.00024781033,0.00021841523],"domain_scores_gemma":[0.9991233,0.0001438099,0.00048633813,0.00011690276,0.000024015757,0.000105649495],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00037090326,0.00013398052,0.0003919122,0.0000023950024,0.00008972215,0.000014258029,0.00011716988,0.000102850994,0.0025721022],"category_scores_gemma":[0.000015196692,0.00010033518,0.00006403563,0.0001937109,0.00032150713,0.0001120378,0.000013664479,0.00016656269,0.000028193732],"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":[0.0030048913,0.0016335539,0.6560254,0.000097067095,0.000729916,0.0000867939,0.0031138542,0.0431996,0.19378279,0.0022561012,0.0028166443,0.09325336],"study_design_scores_gemma":[0.005203616,0.0022011688,0.9719079,0.00003569516,0.0005344345,0.00013632455,0.000469337,0.0022204986,0.0027302525,0.007048349,0.0071201273,0.00039230066],"about_ca_topic_score_codex":0.000039997532,"about_ca_topic_score_gemma":0.000062533225,"teacher_disagreement_score":0.31588247,"about_ca_system_score_codex":0.00008753504,"about_ca_system_score_gemma":0.000035613113,"threshold_uncertainty_score":0.99833965},"labels":[],"label_agreement":null},{"id":"W2213797907","doi":"10.1016/j.scitotenv.2015.10.024","title":"High-resolution satellite-based analysis of ground-level PM 2.5 for the city of Montreal","year":2015,"lang":"en","type":"article","venue":"The Science of The Total Environment","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":14,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Concordia University","funders":"","keywords":"Environmental science; Satellite; Aerosol; Scale (ratio); Remote sensing; Meteorology; Spatial distribution; Image resolution; Geography; Computer science; Cartography","score_opus":0.025731261867007454,"score_gpt":0.22382608324720396,"score_spread":0.19809482138019652,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2213797907","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":[0.99310726,0.000077685436,0.0051194355,0.0007249227,0.00010046706,0.0003719879,0.000037229263,0.0000038768712,0.00045711],"genre_scores_gemma":[0.99767935,0.000017115235,0.0017168757,0.00002392083,0.000013264707,0.000017395249,0.0000014331692,0.0000054176867,0.0005252533],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9981174,0.00006253241,0.0003214113,0.00024737124,0.0009956856,0.00025559892],"domain_scores_gemma":[0.99861974,0.00013701979,0.00036616117,0.0007926683,0.000013982205,0.00007045179],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0014702114,0.00012393287,0.0002236099,0.000005247023,0.00024001583,0.0000102249205,0.0010528954,0.000033553933,0.00019942464],"category_scores_gemma":[0.00006939778,0.0000581737,0.0001998932,0.00081190304,0.0033721877,0.00009667734,0.0004314929,0.0000652712,0.000007112732],"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":[0.000074604046,0.00014794778,0.0028721571,0.0000030059305,0.00006947446,5.320132e-8,0.0006239317,0.9692546,0.023400452,0.0002719949,0.00004506856,0.0032367262],"study_design_scores_gemma":[0.00035476752,0.00017620616,0.8489916,0.000005557232,0.00046323554,5.435914e-7,0.0004672921,0.12378075,0.024991954,0.0006058281,0.000056336135,0.000105931744],"about_ca_topic_score_codex":0.005270041,"about_ca_topic_score_gemma":0.00006354196,"teacher_disagreement_score":0.84611946,"about_ca_system_score_codex":0.0002198468,"about_ca_system_score_gemma":0.000039531846,"threshold_uncertainty_score":0.99934006},"labels":[],"label_agreement":null},{"id":"W2239860875","doi":"","title":"Parameterization of ice crystal properties and liquid fraction in extra-tropical stratiform clouds.","year":2004,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Ice crystals; Cloud fraction; Environmental science; GCM transcription factors; Climatology; Atmospheric sciences; Cloud computing; Liquid water content; General Circulation Model; Climate model; Meteorology; Climate change; Geography; Geology; Cloud cover; Computer science","score_opus":0.015760272600031915,"score_gpt":0.2101532834608223,"score_spread":0.1943930108607904,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2239860875","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":[0.98850447,0.000020570009,0.0084628,0.00010072923,0.000019506508,0.00011003507,4.0419164e-7,0.000013174238,0.0027683256],"genre_scores_gemma":[0.9962893,0.0000285985,0.0035121983,0.000057368474,0.000009435491,0.000006196096,8.4538857e-7,0.0000044560165,0.000091580616],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9994739,0.000010390662,0.00015705143,0.00013116442,0.00012402982,0.0001034619],"domain_scores_gemma":[0.9998483,0.000006747828,0.000039586615,0.000069236135,0.000002898192,0.000033226468],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000035635327,0.00006401073,0.00008272702,9.221928e-7,0.000029169003,0.000010486847,0.00004265343,0.000048503814,0.000368356],"category_scores_gemma":[0.00001329819,0.000048433794,0.000013525686,0.00008587361,0.00011716566,0.00020102014,0.00003527766,0.000052626252,0.000009859054],"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":[0.0003664594,0.000436077,0.21121565,0.000045187116,0.000009407076,0.000005871878,0.0015557872,0.01292916,0.7618235,0.0027881467,0.000023494407,0.008801308],"study_design_scores_gemma":[0.0013172869,0.0014572687,0.87258285,0.000057887577,0.0000140838965,0.000013774002,0.0017385588,0.0049663573,0.11500487,0.0019919407,0.00047664615,0.00037848038],"about_ca_topic_score_codex":0.00080619036,"about_ca_topic_score_gemma":0.0003422682,"teacher_disagreement_score":0.6613672,"about_ca_system_score_codex":0.00006215432,"about_ca_system_score_gemma":0.000007864559,"threshold_uncertainty_score":0.403324},"labels":[],"label_agreement":null},{"id":"W2266058414","doi":"10.1063/1.3117015","title":"Preliminary Analysis of Night‐time Aerosol Optical Depth Retrievals at a Rural, Near‐urban Site in Southern Canada","year":2009,"lang":"en","type":"article","venue":"AIP conference proceedings","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":true,"ca_institutions":"Université de Sherbrooke","funders":"","keywords":"Environmental science; Remote sensing; Lidar; Aerosol; Zenith; Calibration; Backscatter (email); Homogeneous; Spectral line; Optical depth; Correlation coefficient; Extinction (optical mineralogy); Atmospheric sciences; Meteorology; Geology; Optics; Physics; Mathematics; Computer science","score_opus":0.007551477597690607,"score_gpt":0.20501423188130083,"score_spread":0.1974627542836102,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2266058414","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":[0.9888951,0.000037654416,0.00008353236,0.000535813,0.000015760648,0.00021135945,0.000012028292,0.000029299625,0.0101794265],"genre_scores_gemma":[0.9964698,0.000011888963,0.00068068464,0.00035969453,0.000013616813,0.0000092909,0.000012423602,0.000012775003,0.0024298236],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980132,0.000011953702,0.0004482856,0.0004402254,0.0005941081,0.0004922307],"domain_scores_gemma":[0.99931693,0.00003782239,0.00020512806,0.00018354398,0.000048849855,0.00020770048],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001954854,0.0002485956,0.0004846333,0.00000793142,0.000117056625,0.00005634204,0.00038995864,0.00012856173,0.0022400653],"category_scores_gemma":[0.000067010325,0.00022058516,0.00010443876,0.0011148866,0.0002351362,0.00019077385,0.00019283361,0.00018522737,0.00011484793],"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":[0.00014638004,0.00010482823,0.93879366,0.000008478359,0.000057639456,0.000010773419,0.0048175706,0.0001354284,0.05181646,0.00004523237,0.0026569117,0.0014066411],"study_design_scores_gemma":[0.000538269,0.0005593471,0.90551287,0.00006151614,0.00034968214,0.0000073021747,0.0018027247,0.08746886,0.0027277677,0.00008673071,0.00029589466,0.00058904133],"about_ca_topic_score_codex":0.07031523,"about_ca_topic_score_gemma":0.06792169,"teacher_disagreement_score":0.08733343,"about_ca_system_score_codex":0.00038066972,"about_ca_system_score_gemma":0.00010883413,"threshold_uncertainty_score":0.998672},"labels":[],"label_agreement":null},{"id":"W2280088189","doi":"10.1115/imece2014-38515","title":"Time Resolved Laser Induced Incandescence for Sizing Aerosolized Iron Nanoparticles","year":2014,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"Western University; University of Waterloo","funders":"","keywords":"Incandescence; Nanoparticle; Aerosolization; Materials science; Aerosol; Sizing; Thermal; Analytical Chemistry (journal); Nanotechnology; Chemistry; Combustion; Thermodynamics; Environmental chemistry; Physical chemistry; Physics","score_opus":0.010973460320148442,"score_gpt":0.2213633319044439,"score_spread":0.21038987158429545,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2280088189","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":[0.9867941,0.0000036916547,0.0019510571,0.00031080304,0.000056479443,0.00025299392,0.0000012003817,0.0000989281,0.010530735],"genre_scores_gemma":[0.985,0.0000017778596,0.009824233,0.000723183,0.000049991853,0.00004199209,0.0000027779738,0.000019998584,0.0043360023],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9988831,0.00003981008,0.00019441688,0.0003185417,0.00019507123,0.00036901442],"domain_scores_gemma":[0.9994571,0.000092502785,0.000059738224,0.00025321788,0.0000068067084,0.00013059979],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00027400907,0.00014078141,0.00015852551,7.915514e-7,0.00018875809,0.00003351136,0.00021369252,0.00007123755,0.002621469],"category_scores_gemma":[0.00008026863,0.00011249664,0.000056498728,0.00011532637,0.00013668186,0.00014530012,0.00013998381,0.00005873933,0.00083835714],"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":[0.00006104698,0.00006112931,0.0073674847,0.0000052542946,0.0000038221833,4.6855402e-7,0.00016734017,0.00024057119,0.97691905,0.0001364315,0.0026738427,0.012363531],"study_design_scores_gemma":[0.0047356742,0.001012806,0.040319424,0.00004634093,0.000066489694,0.000006329876,0.00033761593,0.12544155,0.7856208,0.0016746471,0.039361432,0.0013769147],"about_ca_topic_score_codex":0.00015302493,"about_ca_topic_score_gemma":0.000076315744,"teacher_disagreement_score":0.19129829,"about_ca_system_score_codex":0.00006060984,"about_ca_system_score_gemma":0.000006555993,"threshold_uncertainty_score":0.9999396},"labels":[],"label_agreement":null},{"id":"W2289243322","doi":"10.1002/2015jd023848","title":"The Two‐Column Aerosol Project: Phase I—Overview and impact of elevated aerosol layers on aerosol optical depth","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"McGill University","funders":"U.S. Department of Energy","keywords":"Aerosol; Environmental science; Lidar; Atmospheric sciences; Optical depth; Meteorology; Radiative forcing; Remote sensing; Geology; Geography","score_opus":0.06970837267430516,"score_gpt":0.391152609849791,"score_spread":0.32144423717548587,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2289243322","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":[0.9943575,0.00058268465,0.00011433763,0.000411341,0.00009988707,0.00056764355,0.0000070582273,0.000014510201,0.0038449985],"genre_scores_gemma":[0.9972613,0.00047142844,0.0011770546,0.000059101712,0.0002548502,0.000022056181,0.000001239135,0.00004308207,0.0007099136],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9945856,0.0005554912,0.0008033193,0.00040625522,0.0026228046,0.0010265547],"domain_scores_gemma":[0.9967814,0.0010546322,0.0004337032,0.00052841776,0.00034246966,0.00085936603],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020488382,0.00034176148,0.0006404396,0.0000035026637,0.0003781846,0.00020598846,0.0009001187,0.00013299065,0.00023699974],"category_scores_gemma":[0.0013122947,0.00019891943,0.00037242996,0.00090197107,0.0015433314,0.00039398522,0.0005032774,0.00116703,0.00013014875],"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":[0.024923867,0.013777929,0.07871469,0.00021063231,0.001885609,0.0009273913,0.0040159817,0.009206399,0.2918936,0.0027437687,0.19468975,0.37701038],"study_design_scores_gemma":[0.10446881,0.26198876,0.2641032,0.0031839542,0.001173301,0.0012960603,0.020172084,0.10226988,0.19482942,0.016584022,0.022925261,0.0070052296],"about_ca_topic_score_codex":0.002199721,"about_ca_topic_score_gemma":0.00033239066,"teacher_disagreement_score":0.37000516,"about_ca_system_score_codex":0.00049429876,"about_ca_system_score_gemma":0.00048675298,"threshold_uncertainty_score":0.8111699},"labels":[],"label_agreement":null},{"id":"W2290362512","doi":"10.5194/amt-9-2781-2016","title":"The SPectrometer for Ice Nuclei (SPIN): an instrument to investigate icenucleation","year":2016,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":108,"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 Toronto","funders":"National Aeronautics and Space Administration; Office of Science; Bundesministerium für Bildung und Forschung; Sight Research UK; Seventh Framework Programme; Natural Environment Research Council; U.S. Department of Energy","keywords":"Ice nucleus; Nucleation; Spectrometer; Particle (ecology); Spin (aerodynamics); Chemistry; Ice crystals; Chemical physics; Optics; Physics; Geology; Thermodynamics","score_opus":0.0264827627052927,"score_gpt":0.24557505596261317,"score_spread":0.21909229325732046,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2290362512","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":[0.7850309,0.000055429737,0.19651431,0.0070227287,0.00028611897,0.0026808027,0.000005164853,0.00072728813,0.007677277],"genre_scores_gemma":[0.8052485,0.00006566067,0.19153193,0.0015415903,0.00011299904,0.00063292333,0.0000010354762,0.000053867043,0.0008114831],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9977283,0.00008225896,0.00037022177,0.0005213421,0.0007656108,0.00053228653],"domain_scores_gemma":[0.9988655,0.000042694905,0.0001526912,0.00062657375,0.000057673136,0.00025489044],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001100557,0.0002609156,0.00018072847,5.6729243e-7,0.00045272327,0.00009376598,0.0005650307,0.00008168534,0.00048657315],"category_scores_gemma":[0.0001358354,0.00014967575,0.00008822151,0.00026328882,0.00019031382,0.00032289876,0.00017065827,0.00006833933,0.00018410361],"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":[0.00009043472,0.00010147975,0.0055449214,0.0000060098337,0.000028790711,8.405073e-7,0.00019543004,0.000007439381,0.28708842,0.0012145923,0.018846896,0.68687475],"study_design_scores_gemma":[0.0006610926,0.0023216973,0.035942744,0.000112218295,0.000059732363,0.0000050760054,0.00017178949,0.00047506008,0.16678883,0.0076519116,0.78496176,0.0008481055],"about_ca_topic_score_codex":0.00019213647,"about_ca_topic_score_gemma":0.00017772011,"teacher_disagreement_score":0.76611483,"about_ca_system_score_codex":0.0007233966,"about_ca_system_score_gemma":0.000026023934,"threshold_uncertainty_score":0.61035997},"labels":[],"label_agreement":null},{"id":"W2290813649","doi":"10.1002/2015ms000601","title":"A parametrization of 3‐D subgrid‐scale clouds for conventional GCMs: Assessment using A‐Train satellite data and solar radiative transfer characteristics","year":2016,"lang":"en","type":"article","venue":"Journal of Advances in Modeling Earth Systems","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":11,"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":"Pennsylvania State University; U.S. Department of Energy","keywords":"Parametrization (atmospheric modeling); Radiative transfer; Cloud fraction; Solar zenith angle; Environmental science; Satellite; Atmospheric radiative transfer codes; GCM transcription factors; Downwelling; Cloud computing; Zenith; Meteorology; Atmospheric sciences; Upwelling; Physics; Remote sensing; Geology; Computer science; Cloud cover; General Circulation Model; Climate change; Optics","score_opus":0.030412114789429373,"score_gpt":0.2994760656281038,"score_spread":0.2690639508386744,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2290813649","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.4810153,0.0007924623,0.51781166,0.000015825244,0.00017694365,0.00012374965,0.00005110122,0.000001481804,0.000011480371],"genre_scores_gemma":[0.97396517,0.0019793783,0.023914289,0.000008855246,0.00009947226,0.0000025371398,0.000005545006,0.000010719064,0.000014022191],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9985281,0.00008160823,0.00074199546,0.00017781822,0.00031532254,0.00015515674],"domain_scores_gemma":[0.99928284,0.00013151077,0.00034455655,0.0001302547,0.000049060145,0.00006175803],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010143333,0.00010407994,0.00032175134,0.000009186166,0.00004831976,0.00002018041,0.00017747533,0.000052568583,0.000016191905],"category_scores_gemma":[0.000048739148,0.00007309092,0.000047132544,0.000102274185,0.00009008911,0.0006551748,0.000036305348,0.00008120444,3.684432e-7],"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":[0.00027418428,0.0002475898,0.45794725,0.00028682256,0.00007456904,0.0000069559933,0.0007967807,0.46114266,0.039201364,0.0002926863,0.0000072015623,0.039721917],"study_design_scores_gemma":[0.0011901156,0.00021214012,0.008255581,0.0004647201,0.00003607623,0.00002538589,0.00039324936,0.9879214,0.00016391865,0.0002817463,0.00091797067,0.00013768418],"about_ca_topic_score_codex":0.000017502603,"about_ca_topic_score_gemma":0.000012305877,"teacher_disagreement_score":0.52677876,"about_ca_system_score_codex":0.0000692578,"about_ca_system_score_gemma":0.0000379426,"threshold_uncertainty_score":0.29805613},"labels":[],"label_agreement":null},{"id":"W2293055932","doi":"10.3390/rs8030222","title":"GLASS Daytime All-Wave Net Radiation Product: Algorithm Development and Preliminary Validation","year":2016,"lang":"en","type":"article","venue":"Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":61,"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":"Lawrence Berkeley National Laboratory; Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences; Natural Sciences and Engineering Research Council of Canada; Center for Neuroscience and Regenerative Medicine; University of Virginia; Natural Resources Canada; Università degli Studi della Tuscia; Université Laval; Oak Ridge National Laboratory; Biological and Environmental Research; National Natural Science Foundation of China; Canadian Foundation for Climate and Atmospheric Sciences; Microsoft Research; U.S. Department of Energy; National Science Foundation","keywords":"Algorithm; Satellite; Environmental science; Remote sensing; Root mean square; Daytime; Product (mathematics); Meteorology; Mean squared error; Computer science; Mathematics; Statistics; Atmospheric sciences; Physics; Geology","score_opus":0.013487137640595157,"score_gpt":0.21218535758463367,"score_spread":0.19869821994403852,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2293055932","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":[0.8887302,0.00005826701,0.10889219,0.0007286766,0.000121232,0.00018008659,7.793733e-7,0.000049925402,0.0012386169],"genre_scores_gemma":[0.77007335,0.00004493977,0.2278841,0.00014806769,0.0001121276,4.8772023e-8,0.000007624222,0.000019044735,0.0017107208],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99906856,0.00003741304,0.00016338774,0.00031466314,0.000204882,0.00021111484],"domain_scores_gemma":[0.99965376,0.000028163124,0.000081339334,0.00015377587,0.0000071605714,0.00007580588],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018726451,0.00011664883,0.00009303154,0.000001842807,0.000119478434,0.000024843503,0.00003511924,0.000044986016,0.00007028168],"category_scores_gemma":[0.00002750931,0.00008672034,0.000015549054,0.000071888244,0.000067532594,0.00016556177,0.000095791234,0.000042081272,0.0001296972],"study_design_candidate":"design_other","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":[0.000006163247,0.0000052951973,0.00019783106,0.000002201699,0.0000064607116,0.000009787606,0.0003879747,0.00004483989,0.015830794,0.000001112292,0.0002775185,0.98323],"study_design_scores_gemma":[0.0017308939,0.00028145977,0.12887132,0.00023887001,0.000092514856,0.0005429617,0.00023644874,0.4396499,0.28299776,0.00084914616,0.1431522,0.0013564904],"about_ca_topic_score_codex":0.00007462783,"about_ca_topic_score_gemma":0.0000038470707,"teacher_disagreement_score":0.9818735,"about_ca_system_score_codex":0.0001807015,"about_ca_system_score_gemma":0.000013421219,"threshold_uncertainty_score":0.35363528},"labels":[],"label_agreement":null},{"id":"W2294578692","doi":"10.5194/acp-16-15135-2016","title":"Comparison of retrieved noctilucent cloud particle properties from Odin tomography scans and model simulations","year":2016,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Canadian Space Agency; Vetenskapsrådet","keywords":"Remote sensing; Satellite; Ice cloud; Effective radius; Particle (ecology); Cloud top; Environmental science; Mesopause; Atmospheric sciences; Cloud computing; Computational physics; Meteorology; Physics; Geology; Mesosphere; Computer science; Astrophysics; Astronomy; Stratosphere","score_opus":0.017311208645721225,"score_gpt":0.23239879031762353,"score_spread":0.2150875816719023,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2294578692","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":[0.9866699,0.0001871503,0.012286161,0.00008432028,0.000015782256,0.000074774885,0.000021458309,0.000022549992,0.0006378824],"genre_scores_gemma":[0.9945748,0.000047570455,0.0045671575,0.000030108775,0.000044693294,0.000005133483,0.0000028213733,0.0000109977045,0.0007167575],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9992167,0.000010771378,0.0001945458,0.00025712585,0.00015353793,0.00016733294],"domain_scores_gemma":[0.99956596,0.000042365733,0.00008494835,0.00019749581,0.000010815195,0.000098417746],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000029995406,0.00013636069,0.00019001492,7.669494e-9,0.00010382821,0.000014397751,0.00008712536,0.00005757182,0.00055049674],"category_scores_gemma":[0.000009166121,0.000097233176,0.000038050443,0.00013024613,0.0003535444,0.00011412584,0.000087254884,0.000055175606,0.00000483794],"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":[0.000062058,0.00017908834,0.48056692,0.000020414771,0.00003029054,3.204658e-7,0.0009760436,0.016339973,0.44866592,0.000035013883,0.00017566768,0.052948285],"study_design_scores_gemma":[0.0006707922,0.00004662417,0.03097039,0.00004873842,0.00005569449,5.282024e-7,0.00025894554,0.70424795,0.2610692,0.0019423269,0.00038862656,0.00030014897],"about_ca_topic_score_codex":0.00015158321,"about_ca_topic_score_gemma":0.0000063263133,"teacher_disagreement_score":0.687908,"about_ca_system_score_codex":0.0000253733,"about_ca_system_score_gemma":0.000008592987,"threshold_uncertainty_score":0.6027553},"labels":[],"label_agreement":null},{"id":"W2313246445","doi":"10.5194/amtd-8-2013-2015","title":"Synchronous starphotometry and lidar measurements at Eureka in High Canadian Arctic","year":2015,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"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":"Lidar; Aerosol; Environmental science; Backscatter (email); Remote sensing; Atmospheric sciences; Meteorology; Geology; Physics; Computer science","score_opus":0.0201576670858789,"score_gpt":0.2124683089473727,"score_spread":0.1923106418614938,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2313246445","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":[0.964299,0.0000764304,0.000024479585,0.00026465647,0.00007668003,0.0001266339,0.0000017381693,0.000013215898,0.03511713],"genre_scores_gemma":[0.99605983,0.0000074858835,0.0012250878,0.0005857307,0.000011859623,0.000007002452,0.0000017297076,0.000010045978,0.0020912224],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990539,0.000024633408,0.00011419553,0.00022873396,0.00026536037,0.00031317232],"domain_scores_gemma":[0.9993624,0.0000074519476,0.000021668538,0.00014782553,0.0000063088687,0.00045432756],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021221869,0.00010045623,0.000101617676,0.0000030661815,0.000059921233,0.000018744784,0.00010942499,0.000050682716,0.0030547092],"category_scores_gemma":[0.000030629766,0.00008695052,0.00001131164,0.00020688292,0.000083940075,0.00008726387,0.0001094597,0.00006496409,0.00051994104],"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":[0.0000056735807,0.000018268249,0.9965019,0.0000022685065,0.0000034465463,0.0000166382,0.00019457092,0.00012003167,0.0002995648,0.00000883935,0.0012753808,0.0015533664],"study_design_scores_gemma":[0.00052152295,0.00008223492,0.9930263,0.000006459635,0.000005513734,0.000010106492,0.00020357373,0.00019556454,0.00027950603,0.00015364155,0.005328983,0.00018658926],"about_ca_topic_score_codex":0.5967041,"about_ca_topic_score_gemma":0.6912876,"teacher_disagreement_score":0.09458347,"about_ca_system_score_codex":0.001425002,"about_ca_system_score_gemma":0.00004711517,"threshold_uncertainty_score":0.9978566},"labels":[],"label_agreement":null},{"id":"W2314698718","doi":"10.5194/amt-9-1817-2016","title":"A microbolometer-based far infrared radiometer to study thin ice clouds in the Arctic","year":2016,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institut National d'Optique; Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency","keywords":"Radiance; Radiometer; Remote sensing; Responsivity; Microbolometer; Physics; Infrared; Optics; Radiative transfer; Pixel; Environmental science; Far infrared; Detector; Bolometer; Geology","score_opus":0.02426658244807143,"score_gpt":0.24377779383332276,"score_spread":0.21951121138525134,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2314698718","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":[0.9295131,0.00009055051,0.0629331,0.0014634544,0.000109295084,0.0026191028,0.0000021901842,0.00031521585,0.0029540183],"genre_scores_gemma":[0.93339705,0.000011969637,0.061918516,0.0034399054,0.000038731214,0.00083936146,5.3901647e-7,0.00004200725,0.00031188756],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99638474,0.00046712224,0.0005513224,0.0006961649,0.0012829985,0.0006176562],"domain_scores_gemma":[0.99856365,0.00011069372,0.00015261194,0.0009888406,0.000043176387,0.00014104291],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0025163237,0.00038598847,0.00034659728,0.0000023991406,0.00016961897,0.00006963215,0.0010882333,0.000105815605,0.0014320309],"category_scores_gemma":[0.00019770322,0.00021744956,0.00012136591,0.0012101274,0.00014836162,0.00017786944,0.00022459486,0.00018912766,0.00023457033],"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":[0.00023698653,0.0027964253,0.5896061,0.00002334691,0.00009294435,0.000085097934,0.003909037,0.0001011533,0.17323959,0.00003768716,0.0138846105,0.21598703],"study_design_scores_gemma":[0.0028675452,0.004840156,0.86912596,0.0002684876,0.00015037235,0.00002365517,0.0015249787,0.00024595638,0.03314082,0.0013361528,0.08473324,0.0017426709],"about_ca_topic_score_codex":0.0008673358,"about_ca_topic_score_gemma":0.0002375339,"teacher_disagreement_score":0.2795199,"about_ca_system_score_codex":0.000760038,"about_ca_system_score_gemma":0.00003238967,"threshold_uncertainty_score":0.9994808},"labels":[],"label_agreement":null},{"id":"W2315845830","doi":"10.5194/amtd-5-7507-2012","title":"Radar-radiometer retrievals of cloud number concentration and dispersion parameter in marine stratocumulus","year":2012,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"","keywords":"Drizzle; Environmental science; Radiometer; Marine stratocumulus; Remote sensing; Effective radius; Zenith; Radar; Meteorology; Cloud computing; Physics; Computer science; Geology; Aerosol; Precipitation","score_opus":0.013549430144927273,"score_gpt":0.2482422734417756,"score_spread":0.23469284329684834,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2315845830","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":[0.98258775,0.00006896467,0.0008511063,0.000085898195,0.00027283057,0.00041476457,0.0000075908683,0.000015614363,0.015695449],"genre_scores_gemma":[0.9884325,0.0001596008,0.010370948,0.00008377939,0.00005766167,0.000011129533,0.000023028002,0.000016516853,0.0008448141],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984891,0.00007586755,0.00041465356,0.00040388707,0.0003257035,0.0002908067],"domain_scores_gemma":[0.99928963,0.00006321893,0.00019214228,0.0003267982,0.0000066916855,0.000121493584],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00029591846,0.00023040597,0.00035299943,9.692833e-7,0.000026620735,0.000028287908,0.00016598536,0.0002723374,0.011726518],"category_scores_gemma":[0.000027105309,0.00018908257,0.00007279434,0.0001453968,0.00023435283,0.00013985121,0.00081960164,0.0002840736,0.0000614687],"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":[0.00005408163,0.000104282386,0.98654306,0.000043847103,0.000015938065,0.0000029533837,0.00033735237,0.00007931378,0.002683257,0.00014031597,0.000488491,0.009507079],"study_design_scores_gemma":[0.0008641093,0.00007560288,0.9856441,0.0000671478,0.00006488921,0.000010798495,0.00016260016,0.0021637392,0.007093628,0.0022793682,0.0009851187,0.0005888791],"about_ca_topic_score_codex":0.0016797058,"about_ca_topic_score_gemma":0.00010639156,"teacher_disagreement_score":0.014850635,"about_ca_system_score_codex":0.00014815427,"about_ca_system_score_gemma":0.000013380733,"threshold_uncertainty_score":0.98917687},"labels":[],"label_agreement":null},{"id":"W2316546267","doi":"10.1021/jp507875q","title":"Immersion Freezing of Supermicron Mineral Dust Particles: Freezing Results, Testing Different Schemes for Describing Ice Nucleation, and Ice Nucleation Active Site Densities","year":2014,"lang":"en","type":"article","venue":"The Journal of Physical Chemistry A","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":45,"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 British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Ice nucleus; Nucleation; Kaolinite; Immersion (mathematics); Supercooling; Chemistry; Thermodynamics; Atmospheric pressure; Mineralogy; Atmospheric sciences; Materials science; Meteorology; Physics; Mathematics; Geometry","score_opus":0.018787749819830352,"score_gpt":0.21889991945299334,"score_spread":0.20011216963316297,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2316546267","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":[0.99664646,0.000016666107,0.0028826809,0.00017253848,0.00001088142,0.0000634436,0.000005002301,0.0000066278512,0.00019566792],"genre_scores_gemma":[0.998672,0.000004625101,0.0010160807,0.000033303688,0.00022265542,0.0000010410998,0.0000019021421,0.0000123489945,0.000036025023],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9991677,0.000050832256,0.0002828443,0.00012060916,0.0002118358,0.00016620148],"domain_scores_gemma":[0.9988605,0.00054264494,0.00036297116,0.00011279365,0.000054653625,0.00006642945],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031366112,0.000122021884,0.00019280202,0.0000012579252,0.00018996673,0.000023653081,0.00013185125,0.00003754265,0.000011707214],"category_scores_gemma":[0.00027986814,0.00008447347,0.00006545686,0.00007869373,0.00017991882,0.00020782345,0.00009498945,0.00014983141,0.0000011912706],"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":[0.00021807721,0.00005901775,0.0023733967,0.00003140708,0.000015093901,2.356512e-7,0.0022240658,0.0017555191,0.98998207,0.0000073203814,0.00008407236,0.0032497232],"study_design_scores_gemma":[0.00081568846,0.00018023497,0.0114636235,0.00018843371,0.00011391145,0.000015446703,0.0035047897,0.101627536,0.8817804,0.00011112645,0.00006078593,0.00013802446],"about_ca_topic_score_codex":0.00006680315,"about_ca_topic_score_gemma":0.0000028974848,"teacher_disagreement_score":0.10820167,"about_ca_system_score_codex":0.00008218137,"about_ca_system_score_gemma":0.0000069875823,"threshold_uncertainty_score":0.34447283},"labels":[],"label_agreement":null},{"id":"W2319194734","doi":"10.1097/hp.0000000000000415","title":"Scanning Lidar Measurements of the Full-Scale RDD Field Trial Puff Plumes","year":2016,"lang":"en","type":"article","venue":"Health Physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Defence Research and Development Canada","funders":"","keywords":"Aerosol; Lidar; Environmental science; Visibility; Extinction (optical mineralogy); Remote sensing; Meteorology; Atmospheric sciences; Optics; Physics; Geology","score_opus":0.03281087446559357,"score_gpt":0.27718998321447924,"score_spread":0.2443791087488857,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2319194734","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":[0.985693,0.00004070733,0.00359459,0.0029530139,0.0004450982,0.0003723483,0.0000033291794,0.000019635097,0.006878328],"genre_scores_gemma":[0.99749196,0.000012512266,0.0006186413,0.0010074135,0.0001706792,0.000013994906,2.225972e-7,0.000009740667,0.000674835],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99891585,0.00006748187,0.00021452748,0.00016697381,0.00038092214,0.00025427272],"domain_scores_gemma":[0.9994101,0.00004191882,0.00017847071,0.0002839932,0.0000073325655,0.0000782111],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022546455,0.00008765308,0.000145893,2.516842e-7,0.00015925629,0.0000055304517,0.00021793785,0.000035675886,0.00032112552],"category_scores_gemma":[0.000022568593,0.00004858556,0.0000719421,0.00012105236,0.00009790978,0.00007590928,0.00012564345,0.00006954689,0.00007052394],"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":[0.0024876182,0.00062861317,0.36193946,0.00009238956,0.000042985503,6.165147e-7,0.0028858313,0.000276349,0.039967075,0.00025852947,0.043546576,0.547874],"study_design_scores_gemma":[0.07330463,0.009089841,0.66174483,0.001480425,0.00013551374,0.0000075660423,0.0012594791,0.0006508443,0.1600486,0.012359293,0.07772793,0.002191011],"about_ca_topic_score_codex":0.00040121723,"about_ca_topic_score_gemma":0.000096313095,"teacher_disagreement_score":0.54568297,"about_ca_system_score_codex":0.0001089792,"about_ca_system_score_gemma":0.00005086371,"threshold_uncertainty_score":0.35160995},"labels":[],"label_agreement":null},{"id":"W2325187418","doi":"10.1021/es3025319","title":"Improving the Accuracy of Daily Satellite-Derived Ground-Level Fine Aerosol Concentration Estimates for North America","year":2012,"lang":"en","type":"article","venue":"Environmental Science & Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":80,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"Government of Canada; National Aeronautics and Space Administration","keywords":"Aerosol; Satellite; Environmental science; Ground level; Meteorology; Atmospheric sciences; Remote sensing; Geography; Geology; Engineering","score_opus":0.011773650837085908,"score_gpt":0.22626345436301143,"score_spread":0.21448980352592553,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2325187418","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":[0.9850406,0.0003052433,0.013245018,0.00037669792,0.00014242434,0.00057875464,0.000028814213,0.00006042078,0.00022201666],"genre_scores_gemma":[0.9855291,0.00006125074,0.01403136,0.00014893021,0.000031181644,0.000100281235,0.000015301632,0.000016025078,0.00006652278],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99809176,0.000016270922,0.00032219847,0.00042463676,0.00040143612,0.0007437159],"domain_scores_gemma":[0.99898493,0.00011463102,0.00032047622,0.00046097906,0.0000044033486,0.000114561575],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0002729158,0.00021006228,0.00020059015,0.0000074611385,0.0005792776,0.000028060187,0.0008357444,0.00009130113,0.00047815716],"category_scores_gemma":[0.00015649013,0.00015302729,0.00006180323,0.0006499966,0.0047633536,0.0006293565,0.00054171274,0.00014799747,0.00012073062],"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":[0.000011993507,0.000117821124,0.23711856,0.000003106008,0.0000048917314,3.1895829e-7,0.00048190952,0.00022180655,0.6609893,0.00007823808,0.00002947257,0.10094262],"study_design_scores_gemma":[0.00057243364,0.0004313626,0.5548738,0.000008056603,0.000050517818,0.000022394213,0.0023551525,0.0040649106,0.43254018,0.00020922442,0.004401022,0.00047090996],"about_ca_topic_score_codex":0.00014590244,"about_ca_topic_score_gemma":0.000030173014,"teacher_disagreement_score":0.31775528,"about_ca_system_score_codex":0.0003010762,"about_ca_system_score_gemma":0.000020639984,"threshold_uncertainty_score":0.99794513},"labels":[],"label_agreement":null},{"id":"W2327732136","doi":"10.1097/hp.0000000000000366","title":"Radiation Modeling and Finite Cloud Effects for Atmospheric Dispersion Calculations in Near-field Applications","year":2016,"lang":"en","type":"article","venue":"Health Physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Canadian Nuclear Laboratories","funders":"","keywords":"Atmospheric dispersion modeling; Environmental science; Cloud computing; Dispersion (optics); Field (mathematics); Radiation; Meteorology; Atmospheric sciences; Physics; Computational physics; Air pollution; Optics; Computer science; Chemistry","score_opus":0.009641427238883315,"score_gpt":0.2624449652758336,"score_spread":0.25280353803695027,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2327732136","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.2957276,0.000089800196,0.7024255,0.0010912282,0.000043573775,0.000518688,0.0000029435728,0.000017386887,0.000083246865],"genre_scores_gemma":[0.98750365,0.00016171153,0.011236819,0.00072091003,0.00008748438,0.00019435988,0.000005168273,0.000011712946,0.00007817531],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9993526,0.000023638642,0.00014210798,0.00019790273,0.00008522656,0.00019853545],"domain_scores_gemma":[0.99953467,0.00019432763,0.000057438083,0.00012693509,0.000004350315,0.00008228379],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009254654,0.00007498263,0.000099718156,2.1440236e-7,0.00021502585,0.000010194932,0.0000482359,0.000038644685,0.000019093803],"category_scores_gemma":[0.000019898624,0.000058647463,0.000024907764,0.00014685509,0.000032093125,0.00010628988,0.000034361627,0.000042929478,0.000025691204],"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":[0.000022953207,0.00010777967,0.069965996,0.000081857645,0.000004033438,1.6057362e-7,0.00071114785,0.07485954,0.0005107658,0.0028181272,0.0006622424,0.8502554],"study_design_scores_gemma":[0.00074353674,0.00012264833,0.018426253,0.00004575918,0.0000062633235,2.7796622e-7,0.000036166988,0.9702419,0.000066450826,0.005000779,0.005150383,0.00015960749],"about_ca_topic_score_codex":0.0003857563,"about_ca_topic_score_gemma":0.00006044667,"teacher_disagreement_score":0.89538234,"about_ca_system_score_codex":0.00012929531,"about_ca_system_score_gemma":0.000021339363,"threshold_uncertainty_score":0.23915741},"labels":[],"label_agreement":null},{"id":"W2330123567","doi":"10.2514/6.2005-7129","title":"New Cloud Micro Sensors for the Aerosonde UAV","year":2005,"lang":"en","type":"article","venue":"Infotech@Aerospace","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Aerosan","funders":"","keywords":"Cloud computing; Computer science; Operating system","score_opus":0.008109204557189073,"score_gpt":0.2242875311657394,"score_spread":0.21617832660855033,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2330123567","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":[0.881463,0.0003902963,0.08782321,0.019663434,0.0007516033,0.0011432854,0.000016055956,0.0003127557,0.008436363],"genre_scores_gemma":[0.80860156,0.00013793411,0.093910456,0.003647255,0.0012168685,0.000083297484,0.0000051654065,0.000092300565,0.092305146],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9982932,0.00002280484,0.00028107266,0.0004178007,0.00036281234,0.00062228437],"domain_scores_gemma":[0.99879444,0.0001832758,0.00014442224,0.00065082405,0.00001217982,0.00021487121],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00026812553,0.0002906566,0.0002157724,0.0000015554738,0.0004124585,0.00009932024,0.0006281524,0.00018568082,0.0027607426],"category_scores_gemma":[0.00007006658,0.00021008476,0.00017877812,0.00027969075,0.00022078752,0.00020890177,0.0002653519,0.0002639319,0.0018413436],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011255035,0.00009652662,0.009116292,0.000012185018,0.00006730035,0.0000037533198,0.0018321603,0.020800652,0.065701425,0.0010040844,0.8289773,0.07227578],"study_design_scores_gemma":[0.00089971954,0.000120134486,0.005964795,0.000013183889,0.000046840592,0.000015704903,0.0004054637,0.0019715056,0.031447314,0.00026446828,0.95835316,0.0004976826],"about_ca_topic_score_codex":0.00066359504,"about_ca_topic_score_gemma":0.00037542338,"teacher_disagreement_score":0.12937589,"about_ca_system_score_codex":0.00021167661,"about_ca_system_score_gemma":0.000034332013,"threshold_uncertainty_score":0.9989358},"labels":[],"label_agreement":null},{"id":"W2334588610","doi":"10.5194/acp-16-6475-2016","title":"An evaluation of the impact of aerosol particles on weather forecasts from a biomass burning aerosol event over the Midwestern United States: observational-based analysis of surface temperature","year":2016,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":40,"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":"Office of Naval Research; National Aeronautics and Space Administration; Met Office; National Science Foundation","keywords":"Aerosol; Environmental science; Atmospheric sciences; Daytime; Moderate-resolution imaging spectroradiometer; Smoke; Climatology; Radiative forcing; Meteorology; Plume; Satellite; Geography; Geology","score_opus":0.01951184210767939,"score_gpt":0.2698331030742428,"score_spread":0.25032126096656343,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2334588610","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":[0.9990344,0.00003219884,0.00056878105,0.000054859698,0.000011327724,0.00014694572,0.000116930816,0.0000056616827,0.000028870167],"genre_scores_gemma":[0.9994552,0.000007666829,0.00035829548,0.000035452602,0.00001813357,0.000008325377,0.000047608988,0.000010970154,0.00005832931],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9987862,0.00010963318,0.00026179783,0.00022299966,0.00048335842,0.00013602427],"domain_scores_gemma":[0.9989256,0.000184782,0.00033718834,0.00044058388,0.00006343825,0.000048405844],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00022609721,0.00016146658,0.00021944579,6.5215126e-8,0.00007701874,0.000011151533,0.00021311641,0.000065614404,0.0010131736],"category_scores_gemma":[0.000020788722,0.00007910533,0.00017533662,0.0006712558,0.00025867182,0.00008526445,0.0000391032,0.000060614704,7.759485e-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":[0.000043225864,0.00013712782,0.30660602,0.0000059426925,0.0001855187,6.145946e-8,0.00038892185,0.29059145,0.39904055,9.219859e-7,0.000019009422,0.0029812453],"study_design_scores_gemma":[0.0004809146,0.00006457374,0.38248703,0.00004985827,0.00033456727,7.8884526e-8,0.0001254379,0.40389627,0.21233669,0.00011691697,0.0000036765312,0.00010399325],"about_ca_topic_score_codex":0.0017071837,"about_ca_topic_score_gemma":0.000033239892,"teacher_disagreement_score":0.18670388,"about_ca_system_score_codex":0.00008481342,"about_ca_system_score_gemma":0.000040515035,"threshold_uncertainty_score":0.99990004},"labels":[],"label_agreement":null},{"id":"W2336454125","doi":"10.5194/amt-9-619-2016","title":"Software to analyze the relationship between aerosol, clouds, and precipitation: SAMAC","year":2016,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada; Environment and Climate Change Canada; Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Universities Space Research Association","keywords":"Cloud computing; Replicate; Software; Computer science; Aerosol; Comparability; Remote sensing; Data set; Data mining; Meteorology; Environmental science; Geography; Operating system; Artificial intelligence","score_opus":0.03598960482248394,"score_gpt":0.25726089119164836,"score_spread":0.22127128636916443,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2336454125","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":[0.67972785,0.0002216941,0.31064537,0.004949512,0.00009423221,0.0011100018,0.0000062168174,0.0005481859,0.002696942],"genre_scores_gemma":[0.9088233,0.00002987962,0.0893247,0.0005602818,0.00010625405,0.00021199317,0.000001207014,0.000030756346,0.000911605],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99780995,0.00014340667,0.0003644079,0.00048770718,0.000827171,0.0003673681],"domain_scores_gemma":[0.9987794,0.0003107401,0.00013925745,0.00053062994,0.000046545774,0.0001934207],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010473237,0.00025041646,0.00021172767,6.142398e-7,0.00038196126,0.000057688183,0.00039049832,0.00010717252,0.00064051326],"category_scores_gemma":[0.0006125421,0.00014346612,0.00006750213,0.00044113942,0.00023302893,0.00022081663,0.00025250093,0.00012331709,0.00020251158],"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":[0.000011284848,0.000019499132,0.88076586,0.0000047374765,0.000016298405,7.73073e-7,0.00019335009,0.0000048067027,0.002048243,0.00016308906,0.01325844,0.10351365],"study_design_scores_gemma":[0.00018708798,0.00022543837,0.9653731,0.00008810232,0.000052195184,0.0000029490268,0.000066087254,0.0000060948914,0.0035293575,0.0028915303,0.027222423,0.00035562512],"about_ca_topic_score_codex":0.00017806762,"about_ca_topic_score_gemma":0.00009062463,"teacher_disagreement_score":0.22909549,"about_ca_system_score_codex":0.00032281037,"about_ca_system_score_gemma":0.000022646582,"threshold_uncertainty_score":0.7013171},"labels":[],"label_agreement":null},{"id":"W2338754006","doi":"10.1080/07038992.2015.1112729","title":"Cloud Detection Method Based on Spectral Area Ratios in MODIS Data","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Moderate-resolution imaging spectroradiometer; Pixel; Remote sensing; Cloud computing; Preprocessor; Spectroradiometer; Computer science; Environmental science; Geography; Artificial intelligence; Reflectivity; Physics; Satellite","score_opus":0.04254166970787606,"score_gpt":0.25842285565451345,"score_spread":0.21588118594663738,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2338754006","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":[0.57670957,0.000024959774,0.41833577,0.0007522969,0.00049208006,0.00006587719,0.0000040023197,0.0000041807416,0.003611272],"genre_scores_gemma":[0.8487015,0.0000010213225,0.15070386,0.00039165883,0.00013828783,3.8744035e-9,0.0000012966816,0.000010703583,0.000051704224],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9990427,0.00010295919,0.00022957592,0.00016000145,0.0002168658,0.00024793192],"domain_scores_gemma":[0.9990297,0.00003094472,0.00013325886,0.0002745113,0.000016531616,0.00051506114],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007358314,0.00009613192,0.00014527576,0.000011681688,0.00007111317,0.00004030534,0.00019716234,0.000056200974,0.00008296447],"category_scores_gemma":[0.00019818493,0.00008828844,0.000034158886,0.0002344521,0.000053793196,0.00015817666,0.000018152185,0.00024266951,0.000018081184],"study_design_candidate":"simulation_or_modeling","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":[0.000083803505,0.000008652566,0.0040123,0.0000024679698,0.000009364899,0.00081616535,0.0007206191,0.11635087,0.0012982902,0.000002505495,0.0033125647,0.8733824],"study_design_scores_gemma":[0.0004906182,0.00016869513,0.0034445291,0.00004919449,0.000014211454,0.00023699971,0.00038772586,0.982876,0.0012320006,0.0003695124,0.0105814915,0.00014902522],"about_ca_topic_score_codex":0.030097468,"about_ca_topic_score_gemma":0.21969031,"teacher_disagreement_score":0.8732334,"about_ca_system_score_codex":0.00066387677,"about_ca_system_score_gemma":0.00027913033,"threshold_uncertainty_score":0.9763612},"labels":[],"label_agreement":null},{"id":"W2340047292","doi":"10.1002/2015jd024699","title":"Evaluating and improving cloud phase in the Community Atmosphere Model version 5 using spaceborne lidar observations","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":150,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Aeronautics and Space Administration; National Center for Atmospheric Research; National Science Foundation","keywords":"Lidar; Environmental science; Cloud computing; Cloud height; Cloud top; Meteorology; Shortwave; International Satellite Cloud Climatology Project; Pathfinder; Cloud fraction; Atmospheric model; Atmosphere (unit); Climate model; Satellite; Cloud forcing; Cloud cover; Remote sensing; Climate change; Computer science; Radiative transfer; Geography; Geology; Physics; Oceanography","score_opus":0.14987927623765862,"score_gpt":0.40110658695933216,"score_spread":0.25122731072167354,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2340047292","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":[0.99454373,0.000104265906,0.0037265993,0.00096360256,0.000045005887,0.0002231167,0.0000037265497,0.0000062918807,0.00038364978],"genre_scores_gemma":[0.97892416,0.00005473374,0.020577857,0.00008654612,0.00015332461,0.000005459133,3.4469284e-7,0.000018355386,0.00017921798],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9961329,0.0013590885,0.00043823637,0.0001982272,0.0013492828,0.00052227563],"domain_scores_gemma":[0.9973837,0.0016829076,0.00024334854,0.00037276544,0.00012393491,0.0001933235],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0046867947,0.00016387319,0.00026155778,0.0000011029382,0.00082134805,0.00009838008,0.0006776581,0.00008205778,0.0002608204],"category_scores_gemma":[0.0014742848,0.00008959136,0.000102987804,0.0005314358,0.00058530155,0.00058206165,0.00050644105,0.0011598978,0.00002436359],"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":[0.0016275673,0.0030084914,0.12314983,0.0000798336,0.000085386564,0.00012136965,0.007822256,0.025453234,0.6054888,0.0012721692,0.0038105042,0.22808056],"study_design_scores_gemma":[0.007876281,0.0045608776,0.2370184,0.0005557998,0.00008689477,0.00006540405,0.013073282,0.7010328,0.0015460154,0.032815374,0.00080043497,0.00056844024],"about_ca_topic_score_codex":0.0026648778,"about_ca_topic_score_gemma":0.00029240613,"teacher_disagreement_score":0.67557955,"about_ca_system_score_codex":0.000346678,"about_ca_system_score_gemma":0.00013472988,"threshold_uncertainty_score":0.6317228},"labels":[],"label_agreement":null},{"id":"W2344762371","doi":"10.1051/epjconf/201611916002","title":"On Depolarization Lidar-Based Method for The Determination of Liquid-Cloud Microphysical Properties","year":2016,"lang":"en","type":"article","venue":"EPJ Web of Conferences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Sonaca (Canada); Defence Research and Development Canada","funders":"","keywords":"Lidar; Cloud computing; Remote sensing; Depolarization; Environmental science; Liquid water; Physics; Meteorology; Geography; Computer science; Thermodynamics","score_opus":0.018497151754320377,"score_gpt":0.2520034124977103,"score_spread":0.23350626074338993,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2344762371","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":[0.64797556,0.000014449526,0.35013837,0.00065066287,0.00007148587,0.00020540055,0.00000585608,0.000008030758,0.00093019154],"genre_scores_gemma":[0.9906016,0.0000070897345,0.00907545,0.00006453546,0.000027595068,0.000027461472,7.804075e-7,0.0000054239053,0.0001900649],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99935144,0.00005331141,0.00017341081,0.00013541285,0.00018775184,0.00009866517],"domain_scores_gemma":[0.99934447,0.0003249153,0.00014990674,0.00013322433,0.0000272438,0.000020226154],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016439249,0.00007897913,0.00012084889,0.0000016339925,0.00006108027,0.000008423471,0.00018652111,0.000041351628,0.00029944337],"category_scores_gemma":[0.000087214874,0.000037085552,0.00005554182,0.000066169334,0.00024895993,0.000054540127,0.000027850534,0.000025165979,0.000008334026],"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":[0.0002918306,0.00011678542,0.0057381378,0.00002133587,0.000010368127,1.2323824e-7,0.00018045082,0.00015469511,0.8697088,0.00400989,0.00009043716,0.119677186],"study_design_scores_gemma":[0.0004297507,0.00094154495,0.0076955957,0.00007191981,0.000028318042,2.3735171e-7,0.00008849061,0.015631322,0.97233605,0.0010527894,0.0016124429,0.000111527384],"about_ca_topic_score_codex":0.00011296512,"about_ca_topic_score_gemma":0.000037696882,"teacher_disagreement_score":0.34262604,"about_ca_system_score_codex":0.000015591266,"about_ca_system_score_gemma":0.00008120617,"threshold_uncertainty_score":0.32786947},"labels":[],"label_agreement":null},{"id":"W234928809","doi":"","title":"Preliminary study of the FCI instrument capability to detect dust aerosols","year":2015,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Impact","funders":"","keywords":"Geostationary orbit; Atmosphere (unit); Remote sensing; Radiative transfer; Environmental science; Sensitivity (control systems); Satellite; Aerosol; Atmospheric model; Transfer function; Geostationary Operational Environmental Satellite; Aerospace engineering; Meteorology; Computer science; Optics; Engineering; Physics; Geology; Electronic engineering","score_opus":0.02535917157043518,"score_gpt":0.25175963541749924,"score_spread":0.22640046384706405,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W234928809","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":[0.9835864,0.000019505556,0.0002178908,0.0002688866,0.00045682787,0.0024109248,0.000010535555,0.000041467047,0.012987612],"genre_scores_gemma":[0.9960583,0.0000022694235,0.0015863858,0.00015818217,0.00003484825,0.0002103845,0.0000011688553,0.000021664744,0.0019268054],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9975067,0.00017768689,0.000489894,0.0007249619,0.000797543,0.0003032403],"domain_scores_gemma":[0.997915,0.000030112787,0.00021849271,0.0016121112,0.000023330034,0.00020090198],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005252561,0.00031794852,0.00038646237,0.0000010539144,0.00010661361,0.00002766878,0.001172545,0.00018729655,0.0019197561],"category_scores_gemma":[0.0000762384,0.00019934244,0.00013149752,0.00020636647,0.00020102806,0.00004202255,0.006916903,0.00041817338,0.00014965073],"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":[0.00019353951,0.0016681137,0.89904785,0.000054427128,0.00008727685,0.0000057719644,0.008660863,0.048605833,0.0004893608,0.0000056976883,0.014417144,0.026764102],"study_design_scores_gemma":[0.000480506,0.0014584982,0.99092656,0.000040945506,0.00008208505,0.0000030145006,0.0030226496,0.00030072508,0.0016342236,0.0006981361,0.0008978137,0.00045482893],"about_ca_topic_score_codex":0.0060106,"about_ca_topic_score_gemma":0.0018962416,"teacher_disagreement_score":0.091878705,"about_ca_system_score_codex":0.0004753352,"about_ca_system_score_gemma":0.000063533706,"threshold_uncertainty_score":0.9989926},"labels":[],"label_agreement":null},{"id":"W2355107068","doi":"10.1080/16742834.2011.11446953","title":"Observations of Aerosol Optical Properties in the Beijing Urban Area in Summer","year":2011,"lang":"en","type":"article","venue":"Atmospheric and Oceanic Science Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":false,"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":"Aerosol; Single-scattering albedo; Beijing; Relative humidity; Atmospheric sciences; Environmental science; Albedo (alchemy); Wind speed; Absorption (acoustics); Scattering coefficient; Correlation coefficient; Particulates; Scattering; Climatology; Meteorology; Chemistry; Physics; Geography; Optics; Geology","score_opus":0.04150889190819058,"score_gpt":0.21009407761021845,"score_spread":0.16858518570202788,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2355107068","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":[0.9964136,0.000057785637,0.00024640383,0.0006504047,0.000050280058,0.00018221456,2.1675596e-7,0.000009433448,0.002389669],"genre_scores_gemma":[0.99239963,0.000016836117,0.0054445667,0.0020712481,0.000009194047,0.000013514129,1.4746158e-7,0.0000063164753,0.000038558584],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986334,0.00003216371,0.00025932566,0.0003273309,0.00037054476,0.00037727438],"domain_scores_gemma":[0.9995872,0.00003757359,0.00006716966,0.00024455265,0.0000055033443,0.000057998837],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005302981,0.00012400225,0.00014137862,9.02464e-7,0.00013858125,0.000027409666,0.00048956496,0.00003384041,0.00013973955],"category_scores_gemma":[0.00005386958,0.00008033088,0.000027949385,0.0009853988,0.0014981217,0.0004067069,0.00015924413,0.00014009513,0.000007810453],"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":[0.0000079772235,0.00007684395,0.97062886,0.000003601038,0.0000013504191,0.0000072774124,0.0050974335,0.00017888416,0.02272669,0.0002646941,0.00021533163,0.0007910621],"study_design_scores_gemma":[0.00017917797,0.000050209554,0.9920558,0.000022111559,0.000005211997,0.0000051927054,0.0022635842,0.004481184,0.0007245035,0.00003698255,0.00004441958,0.0001316582],"about_ca_topic_score_codex":0.00067803985,"about_ca_topic_score_gemma":0.0000939873,"teacher_disagreement_score":0.022002187,"about_ca_system_score_codex":0.00006557852,"about_ca_system_score_gemma":0.000020324836,"threshold_uncertainty_score":0.55198914},"labels":[],"label_agreement":null},{"id":"W2373440338","doi":"","title":"Comparison of Temperature and Ozone Profiles Derived from Lidar and SAGE II Measurements over Toronto Region:Part II","year":2001,"lang":"en","type":"article","venue":"Yunnan Daxue xuebao. Shehui kexue ban","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Altitude (triangle); Lidar; Dial; Ozone; Atmospheric sciences; Environmental science; SAGE; Range (aeronautics); Mixing ratio; Aerosol; Stratosphere; Density of air; Meteorology; Materials science; Physics; Optics; Mathematics; Nuclear physics","score_opus":0.022389342467251265,"score_gpt":0.2525020776643003,"score_spread":0.230112735197049,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2373440338","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":[0.992259,0.0027051617,0.000055895944,0.0002912692,0.00017814309,0.00042557906,0.000027179012,0.000055284792,0.0040024584],"genre_scores_gemma":[0.99480474,0.00032534404,0.0013470988,0.00020993668,0.00014347771,0.00002899183,0.00002912424,0.00003843675,0.0030728686],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99779844,0.00008520848,0.000467562,0.00067637634,0.00053292216,0.00043951368],"domain_scores_gemma":[0.99895895,0.00002907541,0.00023127254,0.0004991224,0.00001894047,0.00026262275],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00016901638,0.00036865307,0.00051728706,0.0000032311086,0.00056304084,0.00006369444,0.00027918548,0.00022461225,0.0020830487],"category_scores_gemma":[0.000032951353,0.0003225323,0.00006843849,0.00016200633,0.00037009528,0.00047129559,0.000529424,0.00020060939,0.000011539331],"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":[0.0001581286,0.00037225217,0.8811385,0.000020590218,0.000062671184,0.000017137916,0.0033528688,0.000022422286,0.09860218,0.000027605813,0.0088727465,0.0073529156],"study_design_scores_gemma":[0.0015855344,0.0005715387,0.94557285,0.00017045016,0.000089474284,0.000018873516,0.0011252587,0.00025109586,0.0128488615,0.00009239748,0.037064757,0.0006089314],"about_ca_topic_score_codex":0.003830852,"about_ca_topic_score_gemma":0.0037767503,"teacher_disagreement_score":0.08575332,"about_ca_system_score_codex":0.0001584648,"about_ca_system_score_gemma":0.000020346832,"threshold_uncertainty_score":0.9999227},"labels":[],"label_agreement":null},{"id":"W2389277551","doi":"10.1175/jamc-d-15-0248.1","title":"The Measured Relationship between Ice Water Content and Cloud Radar Reflectivity in Tropical Convective Clouds","year":2016,"lang":"en","type":"article","venue":"Journal of Applied Meteorology and Climatology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"Federal Aviation Administration; Transport Canada; Environment and Climate Change Canada; National Aeronautics and Space Administration; European Commission; Boeing","keywords":"Liquid water content; Radar; Environmental science; Atmospheric sciences; Convection; Altitude (triangle); Meteorology; Physics; Cloud computing; Mathematics","score_opus":0.02833113220317793,"score_gpt":0.2488543912751952,"score_spread":0.22052325907201728,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2389277551","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":[0.9935511,0.00015638245,0.0010379874,0.0037822342,0.00018082577,0.00011796818,9.735601e-7,0.0000052192954,0.0011673494],"genre_scores_gemma":[0.9990696,0.00011606105,0.0004748428,0.00021213651,0.00007553522,0.000007826055,1.7995764e-7,0.0000075652747,0.000036271984],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99863684,0.00026662668,0.0004380838,0.00020330325,0.00013133363,0.00032378818],"domain_scores_gemma":[0.9983649,0.0011945607,0.00020895849,0.00011396666,0.000015744537,0.00010181595],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009098144,0.00012866237,0.00038962346,0.000005344216,0.00020733867,0.000008578269,0.00013573226,0.00021885365,0.000056412107],"category_scores_gemma":[0.00013502564,0.000059897942,0.000043706987,0.000060738243,0.00094719057,0.000071919334,0.0001186366,0.00034415929,0.000014155491],"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":[0.0008330661,0.000027134041,0.97647893,0.0000024321928,0.000038277245,0.000013074723,0.00035326456,9.541947e-7,0.009008269,0.010126302,0.000087029395,0.003031267],"study_design_scores_gemma":[0.0018354389,0.00029624678,0.9668947,0.000004501968,0.000054408443,0.0001897908,0.00026526448,0.0000023392247,0.0019970676,0.026198363,0.0021642554,0.00009764678],"about_ca_topic_score_codex":0.000013515372,"about_ca_topic_score_gemma":0.00012045334,"teacher_disagreement_score":0.016072063,"about_ca_system_score_codex":0.000068216556,"about_ca_system_score_gemma":0.000013371709,"threshold_uncertainty_score":0.3489963},"labels":[],"label_agreement":null},{"id":"W2396769068","doi":"10.5194/acp-16-12753-2016","title":"Temporal and spectral cloud screening of polar winter aerosol optical depth(AOD): impact of homogeneous and inhomogeneous clouds and crystal layers onclimatological-scale AODs","year":2016,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University; National Research Council Canada; Université de Sherbrooke","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Aerosol; Lidar; Environmental science; Atmospheric sciences; Homogeneous; Polar; Mode (computer interface); Remote sensing; Climatology; Meteorology; Geology; Geography; Physics","score_opus":0.007028509242067068,"score_gpt":0.22299468443730144,"score_spread":0.21596617519523437,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2396769068","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":[0.9947024,0.00038331788,0.003380039,0.000040735424,0.000016235335,0.00011272892,0.000029203264,0.000020211603,0.0013151084],"genre_scores_gemma":[0.98543423,0.00026178037,0.013942363,0.000021464635,0.00007524012,0.0000039368942,0.0000039731444,0.000022667191,0.00023433927],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99863946,0.000027119642,0.00031927883,0.00045838903,0.00019615918,0.00035956205],"domain_scores_gemma":[0.99924994,0.000094533476,0.0001558424,0.00022316305,0.000013588786,0.0002629614],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009769584,0.00030220562,0.00045276474,7.5094555e-8,0.000105346575,0.000024099043,0.00011989513,0.00016237996,0.00040461778],"category_scores_gemma":[0.000014876493,0.00021296275,0.00010138201,0.00011151853,0.0012144744,0.000112173635,0.0002720539,0.00013181804,0.0000013105813],"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":[0.00018384842,0.00011326215,0.6350322,0.00006821903,0.00007482913,0.000019527133,0.0002540692,0.00009701641,0.30902642,0.000008576619,0.000055957604,0.055066083],"study_design_scores_gemma":[0.0064222114,0.0027112872,0.6822544,0.00038244275,0.00043466862,0.0019453671,0.0011562391,0.013083741,0.28666046,0.0020674563,0.00042269248,0.0024590688],"about_ca_topic_score_codex":0.00024708483,"about_ca_topic_score_gemma":0.000014520304,"teacher_disagreement_score":0.05260701,"about_ca_system_score_codex":0.000037479735,"about_ca_system_score_gemma":0.00001627868,"threshold_uncertainty_score":0.8684369},"labels":[],"label_agreement":null},{"id":"W2409114268","doi":"10.1051/epjconf/201611918005","title":"Lidar Measurements of Canadian Forest Fire Smoke Episode Observed in July 2013 over Warsaw, Poland","year":2016,"lang":"en","type":"article","venue":"EPJ Web of Conferences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":6,"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":"National Oceanic and Atmospheric Administration","keywords":"AERONET; Lidar; Environmental science; Satellite; Smoke; Meteorology; Remote sensing; Channel (broadcasting); Aerosol; Geography; Climatology; Geology; Engineering; Telecommunications","score_opus":0.046550321054782816,"score_gpt":0.23129114600889147,"score_spread":0.18474082495410865,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2409114268","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":[0.97435445,0.00015910975,0.000008686862,0.00059808535,0.000087912544,0.00012431496,0.000023757073,0.0000057830603,0.024637878],"genre_scores_gemma":[0.9988616,0.00012244846,0.000181559,0.00004769986,0.00001344888,0.000007119671,0.0000018446225,0.000007076546,0.0007571925],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99883354,0.00004141616,0.00029593142,0.0002048661,0.00033375868,0.00029050486],"domain_scores_gemma":[0.99945486,0.0000398679,0.00013648515,0.00020378105,0.000018356639,0.00014663192],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00020170612,0.00012771641,0.00022360822,0.000008120956,0.00003615534,0.000009159199,0.00031297794,0.00008088665,0.003529294],"category_scores_gemma":[0.000042137715,0.000085797496,0.000048065558,0.00021627304,0.00024387657,0.00013964482,0.00005747007,0.00005197549,0.00005940361],"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":[0.000011233296,0.000027799015,0.99262714,0.000005569444,0.0000095895775,0.0000015761343,0.00008759331,0.000016982664,0.0025004162,0.00011395101,0.0012929311,0.003305241],"study_design_scores_gemma":[0.0004589922,0.000080590784,0.9871091,0.0000792012,0.0000069031594,3.3163633e-7,0.00004033618,0.00009094772,0.001422188,0.00039144617,0.010193982,0.00012596659],"about_ca_topic_score_codex":0.55688643,"about_ca_topic_score_gemma":0.78516024,"teacher_disagreement_score":0.22827382,"about_ca_system_score_codex":0.00006958169,"about_ca_system_score_gemma":0.0002315153,"threshold_uncertainty_score":0.9973816},"labels":[],"label_agreement":null},{"id":"W2412354236","doi":"10.1002/qj.2848","title":"Determination of direct normal irradiance including circumsolar radiation in climate/NWP models","year":2016,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","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":"University of Victoria; Environment and Climate Change Canada","funders":"National Natural Science Foundation of China","keywords":"Physics; Irradiance; Solar irradiance; Radiation; Scaling; Computational physics; Meteorology; Optics; Mathematics","score_opus":0.013720550409161966,"score_gpt":0.2257719063090578,"score_spread":0.21205135589989582,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2412354236","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":[0.98616785,0.000107210246,0.01217975,0.00044826567,0.00016515597,0.00009589014,0.0000036415843,0.0000065023964,0.0008257435],"genre_scores_gemma":[0.9956969,0.00005591673,0.004005824,0.0001324491,0.00005847493,0.0000034155414,1.2508676e-7,0.000007038083,0.00003986315],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99845684,0.00020638715,0.00051938754,0.00015417508,0.00038321267,0.00027999002],"domain_scores_gemma":[0.9990407,0.00017456272,0.0005456434,0.00014421686,0.000019497495,0.00007538532],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010565572,0.00012258225,0.0002656069,0.0000021604812,0.00011093165,0.000013117834,0.00039449343,0.00013422879,0.00024503737],"category_scores_gemma":[0.00005390567,0.00006243786,0.000308536,0.00016928113,0.00021616423,0.00031810868,0.00006968583,0.00018605425,0.000006950019],"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":[0.00021994856,0.00038793415,0.41976446,0.000024027742,0.00005154108,0.000012349237,0.0039433534,0.016483296,0.042178202,0.0002795052,0.00049957784,0.5161558],"study_design_scores_gemma":[0.0023383843,0.002451228,0.8853464,0.00014175559,0.00008516974,0.00002956631,0.000594297,0.09362432,0.0026309856,0.011942075,0.00039914445,0.0004166468],"about_ca_topic_score_codex":0.000036302707,"about_ca_topic_score_gemma":0.000008915994,"teacher_disagreement_score":0.51573914,"about_ca_system_score_codex":0.00023940775,"about_ca_system_score_gemma":0.000012178237,"threshold_uncertainty_score":0.26829872},"labels":[],"label_agreement":null},{"id":"W2417723859","doi":"10.1051/epjconf/201611917005","title":"Extending and Merging the Purple Crow Lidar Temperature Climatologies Using the Inversion Method","year":2016,"lang":"en","type":"article","venue":"EPJ Web of Conferences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fanshawe College; Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Rayleigh scattering; Lidar; Raman spectroscopy; Environmental science; Inversion (geology); Stratosphere; Atmospheric temperature; Atmospheric sciences; Geology; Meteorology; Geodesy; Physics; Remote sensing; Optics; Seismology","score_opus":0.02059293573146683,"score_gpt":0.2713364069134457,"score_spread":0.25074347118197887,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2417723859","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":[0.99079394,0.00028936157,0.0014498627,0.003162836,0.0000961289,0.00009058976,0.0000020535615,0.000015361007,0.0040998664],"genre_scores_gemma":[0.99578637,0.00024771268,0.0035869116,0.00010593012,0.000020284966,0.0000032635146,1.5136355e-7,0.000004247677,0.0002451157],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999233,0.00011222986,0.00013272886,0.00017112873,0.00018569057,0.00016524292],"domain_scores_gemma":[0.99948055,0.00020901476,0.000108404856,0.0001656295,0.000008515398,0.000027914493],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037269673,0.00009795489,0.00012761718,0.0000014092974,0.00030653982,0.000043803007,0.00027302137,0.00004968308,0.0007494121],"category_scores_gemma":[0.00006373983,0.000037524285,0.00003501793,0.000102875776,0.0005274983,0.00014212096,0.00023597533,0.0000752679,0.0000065691934],"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":[0.000025077226,0.000018017532,0.56129515,0.0000127411895,0.000031158637,0.0000031649806,0.0012902172,0.0000855164,0.37430167,0.008226186,0.0013834193,0.053327657],"study_design_scores_gemma":[0.0019065634,0.00047626396,0.49079853,0.0007574318,0.0002983473,0.00013069557,0.054987825,0.0291699,0.24239793,0.02139824,0.15615913,0.0015191456],"about_ca_topic_score_codex":0.0002060285,"about_ca_topic_score_gemma":0.000050352595,"teacher_disagreement_score":0.15477571,"about_ca_system_score_codex":0.000014955758,"about_ca_system_score_gemma":0.000038828926,"threshold_uncertainty_score":0.8205537},"labels":[],"label_agreement":null},{"id":"W2419070419","doi":"10.1002/qj.2846","title":"A comparison of two representations of subgrid‐scale cloud structure in a global model: radiative effects as a function of cloud characteristics","year":2016,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Radiative transfer; Liquid water content; Cloud fraction; Cloud albedo; Cloud computing; Albedo (alchemy); Emissivity; Environmental science; Atmospheric radiative transfer codes; Atmospheric sciences; Meteorology; Cloud cover; Physics; Computer science; Optics","score_opus":0.008526980670265229,"score_gpt":0.2710665018197456,"score_spread":0.26253952114948037,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2419070419","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":[0.97957903,0.000060026767,0.01951599,0.0002289505,0.00027485067,0.00017621795,0.000037030546,0.000004055506,0.00012385953],"genre_scores_gemma":[0.99700505,0.000006554814,0.002813733,0.000060592913,0.00007320087,0.0000025541951,5.5364063e-7,0.0000059086183,0.00003183209],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998031,0.00030974823,0.0007937294,0.00017233953,0.0004828006,0.00021036521],"domain_scores_gemma":[0.9982411,0.00022359015,0.0011871697,0.00020789803,0.000053351665,0.00008688864],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039960913,0.00015386479,0.0005757905,0.0000018871121,0.00005633713,0.0000058030782,0.00037681797,0.00014768628,0.00020108535],"category_scores_gemma":[0.00009496594,0.00007929636,0.00043070444,0.00023958535,0.0004866595,0.00008279999,0.000077532844,0.0002342333,0.0000017881052],"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":[0.00085122866,0.00068201445,0.8919542,0.00004183866,0.00018646006,0.0000024214041,0.0043965853,0.024300234,0.054577872,0.00050771196,0.0009647521,0.02153468],"study_design_scores_gemma":[0.0020417848,0.0036156492,0.95583105,0.000085631655,0.0001929981,0.0000069898506,0.0009059686,0.01646188,0.0037143189,0.016972046,0.000017673414,0.00015401043],"about_ca_topic_score_codex":0.00011053175,"about_ca_topic_score_gemma":0.000027413302,"teacher_disagreement_score":0.063876845,"about_ca_system_score_codex":0.0001535322,"about_ca_system_score_gemma":0.000030176896,"threshold_uncertainty_score":0.3233612},"labels":[],"label_agreement":null},{"id":"W2427165299","doi":"10.4209/aaqr.2015.11.0631","title":"Coupled Aerosol-Cloud Systems over Northern Vietnam during 7-SEAS/BASELInE: A Radar and Modeling Perspective","year":2016,"lang":"en","type":"article","venue":"Aerosol and Air Quality Research","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"Goddard Space Flight Center; Vietnam Academy of Science and Technology; Oak Ridge Associated Universities; National Aeronautics and Space Administration","keywords":"Drizzle; Aerosol; Environmental science; Precipitation; Radar; Atmospheric sciences; Meteorology; Air quality index; Rainband; Atmosphere (unit); Climatology; Remote sensing; Geography; Geology","score_opus":0.04578714851666314,"score_gpt":0.3308450128759941,"score_spread":0.28505786435933095,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2427165299","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":[0.99381346,0.0010627955,0.0018116509,0.0016418446,0.000094032526,0.0005412257,0.000026519801,0.00007511165,0.0009333911],"genre_scores_gemma":[0.9963044,0.0005439609,0.00016337303,0.00008340838,0.00022811459,0.00007299639,0.0000021317294,0.000041536834,0.0025601091],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99595904,0.00058094435,0.00045548266,0.0009468913,0.0011742701,0.0008833883],"domain_scores_gemma":[0.9985108,0.00033849946,0.00008787071,0.0005016248,0.000120341545,0.00044086642],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002507493,0.00029402477,0.000394688,0.0000068074955,0.00086687715,0.00012268253,0.00029375247,0.00016447983,0.0004085259],"category_scores_gemma":[0.0003038714,0.0002007992,0.00009848149,0.0003178189,0.00081269426,0.00034692985,0.000670147,0.0003728161,0.00015257318],"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":[0.0018309149,0.0010330775,0.49279845,0.000629484,0.00037994422,0.00013900237,0.012309528,0.004154257,0.4734236,0.003821106,0.0014246575,0.008055961],"study_design_scores_gemma":[0.035652775,0.003363555,0.26629284,0.002821215,0.0003097124,0.00044316592,0.1266389,0.53516966,0.010666856,0.0064161704,0.0022356454,0.009989496],"about_ca_topic_score_codex":0.008706615,"about_ca_topic_score_gemma":0.0011165161,"teacher_disagreement_score":0.5310154,"about_ca_system_score_codex":0.0003938729,"about_ca_system_score_gemma":0.00005209782,"threshold_uncertainty_score":0.99789447},"labels":[],"label_agreement":null},{"id":"W2437167142","doi":"10.1175/jas-d-15-0317.1","title":"Analytical Infrared Delta-Four-Stream Adding Method from Invariance Principle","year":2016,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":36,"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; Environment and Climate Change Canada","funders":"","keywords":"Emissivity; Radiative transfer; Bounded function; Inverse; Exponential function; Matrix (chemical analysis); Computational physics; Physics; Mathematical analysis; Mathematics; Optics; Materials science; Geometry","score_opus":0.02388167545126642,"score_gpt":0.27839143299040736,"score_spread":0.25450975753914096,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2437167142","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":[0.97688144,0.00012221398,0.013147686,0.0022871916,0.0005929493,0.0000862536,0.000003257415,0.000014127092,0.0068648783],"genre_scores_gemma":[0.8252435,0.00004379267,0.1717441,0.0005387429,0.00019110854,0.0000022106713,3.734629e-8,0.000010513317,0.0022260128],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9976032,0.00018909032,0.0005437181,0.0003040469,0.0009716783,0.00038828448],"domain_scores_gemma":[0.998338,0.0004351822,0.0006669525,0.000336589,0.000031232306,0.00019206073],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012639399,0.00017673465,0.00029872972,6.8867547e-7,0.00037571345,0.00008647899,0.0015747292,0.000071545124,0.0032517284],"category_scores_gemma":[0.00057865545,0.00007931851,0.00022042678,0.00083901914,0.0007294639,0.0006051219,0.0004899234,0.00016835489,0.00007477439],"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":[0.00006345305,0.000114128205,0.9078733,0.000002162939,0.00007576393,0.000032192333,0.00037725983,0.014317792,0.011084401,0.00071404915,0.011212037,0.05413348],"study_design_scores_gemma":[0.0015360978,0.000616803,0.8164397,0.00030603184,0.00019176,0.00026220476,0.0006980961,0.04861152,0.0048321225,0.01938513,0.10638345,0.00073710666],"about_ca_topic_score_codex":0.00020307308,"about_ca_topic_score_gemma":0.00002408254,"teacher_disagreement_score":0.15859641,"about_ca_system_score_codex":0.00021255834,"about_ca_system_score_gemma":0.00010955458,"threshold_uncertainty_score":0.99765944},"labels":[],"label_agreement":null},{"id":"W2462001934","doi":"10.1021/bk-2009-1005.ch010","title":"Understanding Climatic Effects of Aerosols: Modeling Radiative Effects of Aerosols","year":2009,"lang":"en","type":"book-chapter","venue":"ACS symposium series","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Environmental science; Atmospheric sciences; Radiative transfer; Aerosol; Climatology; Meteorology; Geography; Physics; Geology","score_opus":0.019942473065903403,"score_gpt":0.20836929618000272,"score_spread":0.1884268231140993,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2462001934","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.14466158,0.003521418,0.029486569,0.00051268196,0.0017988924,0.00527271,0.00006884827,0.00036186256,0.81431544],"genre_scores_gemma":[0.960841,0.0022087388,0.0015081876,0.0001325757,0.00009677127,0.00003653075,0.00002183626,0.00013000828,0.03502436],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99726605,0.00006233817,0.00080260827,0.0006264602,0.00073208264,0.0005104414],"domain_scores_gemma":[0.9980316,0.00037676765,0.0007699015,0.0006361201,0.0000271802,0.00015842023],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00017472681,0.000685081,0.0011566682,0.000009963767,0.00019198188,0.00003670796,0.00049070327,0.00048754973,0.00016458439],"category_scores_gemma":[0.000053860796,0.00064125407,0.00030914808,0.000111535635,0.00061460503,0.00040199354,0.00032129508,0.00037298715,0.000057706784],"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":[0.0013250388,0.0011254611,0.004514576,0.02149876,0.002688355,0.0004959203,0.03429309,0.16759458,0.5241663,0.23456463,0.0036389679,0.0040943734],"study_design_scores_gemma":[0.013516218,0.022444004,0.0016345524,0.032911636,0.0077843866,0.00020778304,0.0031478084,0.028898932,0.47045943,0.3999919,0.0040444997,0.014958821],"about_ca_topic_score_codex":0.00006700783,"about_ca_topic_score_gemma":0.000029039089,"teacher_disagreement_score":0.8161794,"about_ca_system_score_codex":0.0004742729,"about_ca_system_score_gemma":0.000045743334,"threshold_uncertainty_score":0.99960387},"labels":[],"label_agreement":null},{"id":"W2463513384","doi":"10.5194/tc-10-2655-2016","title":"Refinement of the ice absorption spectrum in the visible using radiance profile measurements in Antarctic snow","year":2016,"lang":"en","type":"article","venue":"The cryosphere","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":118,"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":"Institut Polaire Français Paul Emile Victor; Agence Nationale de la Recherche","keywords":"Radiance; Radiative transfer; Snow; Absorption (acoustics); Environmental science; Attenuation coefficient; Atmospheric radiative transfer codes; Remote sensing; Optics; Atmospheric sciences; Geology; Physics; Meteorology","score_opus":0.022241535249617063,"score_gpt":0.2327120664060986,"score_spread":0.21047053115648154,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2463513384","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":[0.99291885,0.00012564543,0.00032970277,0.0015884945,0.0001288288,0.00049923797,0.0000026701998,0.000007308377,0.004399243],"genre_scores_gemma":[0.99823153,0.000027876551,0.00035671602,0.0003196615,0.0000356038,0.000031609,3.1688805e-7,0.00001245598,0.0009842312],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99852324,0.00016229128,0.00027050535,0.00024167234,0.0004892138,0.00031306126],"domain_scores_gemma":[0.9992632,0.00005185184,0.0001521838,0.00050085684,0.000005589856,0.000026308826],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00062627264,0.0001341672,0.00012566267,9.73156e-7,0.00012111857,0.000016985083,0.00056500046,0.00004820164,0.0023224608],"category_scores_gemma":[0.000019433257,0.00005831525,0.00005526565,0.00043708424,0.00019233118,0.00011685612,0.00013544102,0.00012947561,0.00010314816],"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":[0.000051556606,0.00021120829,0.9427461,0.000017085764,0.000012317363,0.000002710618,0.0012843714,0.002461131,0.039699122,0.00009894068,0.001455538,0.011959925],"study_design_scores_gemma":[0.0007638508,0.000068801644,0.9893578,0.00019321598,0.00001659726,0.0000061364785,0.00054096436,0.0014515247,0.0032554506,0.0008685713,0.0032995534,0.00017749255],"about_ca_topic_score_codex":0.0044156597,"about_ca_topic_score_gemma":0.014116117,"teacher_disagreement_score":0.046611745,"about_ca_system_score_codex":0.00033788205,"about_ca_system_score_gemma":0.000026984555,"threshold_uncertainty_score":0.9985896},"labels":[],"label_agreement":null},{"id":"W2464763130","doi":"10.5194/amt-2016-162","title":"Identification of the cloud base height over the centralHimalayan region: Intercomparison of Ceilometer and DopplerLidar","year":2016,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","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":"Institut National de la Recherche Scientifique","funders":"Indian Space Research Organisation; Indian Institute of Science; U.S. Department of Energy","keywords":"Ceilometer; Cloud base; Environmental science; Lidar; Doppler effect; Atmospheric sciences; Correlation coefficient; Sky; Altitude (triangle); Meteorology; Remote sensing; Cloud computing; Geology; Physics","score_opus":0.008333717691083412,"score_gpt":0.2022226790934187,"score_spread":0.1938889614023353,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2464763130","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":[0.9934334,0.00002868523,0.0027690255,0.001935122,0.00011885393,0.00013365039,0.0000024524154,0.000006041968,0.0015727758],"genre_scores_gemma":[0.9979429,0.000034186603,0.00010981752,0.00013913448,0.000021384642,0.0000037886612,1.37875e-7,0.0000051245675,0.0017435229],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992728,0.000053208772,0.00023477539,0.00014875292,0.00018023784,0.00011020726],"domain_scores_gemma":[0.9994018,0.0000483839,0.00015649007,0.0003571811,0.0000059983263,0.000030118903],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001503396,0.0000716266,0.00009126022,6.4385443e-7,0.000056561308,0.00000829762,0.00024000573,0.00002923151,0.0014844027],"category_scores_gemma":[0.00001402339,0.000027188973,0.000053917753,0.000104098326,0.00039945066,0.000088249835,0.0001748401,0.00003618152,0.00001632031],"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":[0.000029534438,0.00008554604,0.84467936,0.000008925207,0.000016700129,3.5067472e-7,0.0007926649,0.000012387726,0.12572114,0.0014785064,0.017248293,0.009926576],"study_design_scores_gemma":[0.0002708544,0.000037925984,0.9285271,0.000020197176,0.00001809482,0.0000043639193,0.0002588641,0.0002666293,0.06495069,0.00047262604,0.005091982,0.00008065699],"about_ca_topic_score_codex":0.000107916305,"about_ca_topic_score_gemma":0.000045532135,"teacher_disagreement_score":0.08384774,"about_ca_system_score_codex":0.000025577978,"about_ca_system_score_gemma":0.0000033327995,"threshold_uncertainty_score":0.9994284},"labels":[],"label_agreement":null},{"id":"W2474564939","doi":"10.1007/s00024-016-1343-7","title":"Ice Fog and Light Snow Measurements Using a High-Resolution Camera System","year":2016,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"Environment Canada; Swedish National Space Agency","keywords":"Ice crystals; Snow; Environmental science; Remote sensing; Visibility; Radiative transfer; Meteorology; Optics; Atmospheric sciences; Geology; Materials science; Physics","score_opus":0.01150278113862126,"score_gpt":0.1920427819563077,"score_spread":0.18054000081768642,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2474564939","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":[0.9907775,0.000064072294,0.005279662,0.00012402283,0.000060990882,0.00016549429,0.0000037916902,0.000035368754,0.0034891127],"genre_scores_gemma":[0.9984863,0.00001444835,0.0010909546,0.000088423614,0.00010695995,0.00001535589,0.0000010087601,0.0000133296435,0.0001832261],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9991402,0.000012577391,0.00011485953,0.00028568794,0.00022014386,0.00022650436],"domain_scores_gemma":[0.9996791,0.0000137582665,0.00006955183,0.0001422433,0.0000055021214,0.000089863795],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000077248274,0.0001394337,0.00014340805,9.0630544e-7,0.00019040292,0.000027734013,0.000069207854,0.00005641688,0.000034622622],"category_scores_gemma":[0.0000016182904,0.00009518707,0.000018956349,0.000089074994,0.0000873486,0.000097694145,0.00011852442,0.00004587232,0.00007090607],"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":[0.00009482105,0.00014243579,0.02212328,0.000095826916,0.00008088546,0.0000056378112,0.00092427246,0.00023491778,0.8139502,0.0111531885,0.0012728111,0.14992176],"study_design_scores_gemma":[0.016393488,0.0010500507,0.6882987,0.0015060509,0.0015194088,0.00014159195,0.005562129,0.009573965,0.19436741,0.02554076,0.04882628,0.0072201863],"about_ca_topic_score_codex":0.00018876816,"about_ca_topic_score_gemma":0.00001631914,"teacher_disagreement_score":0.66617537,"about_ca_system_score_codex":0.00007980483,"about_ca_system_score_gemma":0.0000052330342,"threshold_uncertainty_score":0.3881616},"labels":[],"label_agreement":null},{"id":"W2486303733","doi":"10.1002/2016jd025309","title":"Radiative characteristics of clouds embedded in smoke derived from airborne multiangular measurements","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":15,"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":"H2020 European Research Council; National Aeronautics and Space Administration","keywords":"Radiative transfer; Environmental science; Smoke; Atmospheric sciences; Single-scattering albedo; Cloud top; Satellite; Aerosol; Remote sensing; Atmospheric radiative transfer codes; Troposphere; Cloud albedo; Optical depth; Cirrus; Cloud cover; Albedo (alchemy); Radiometer; Meteorology; Cloud computing; Physics; Geology; Astronomy; Optics","score_opus":0.04570540642669307,"score_gpt":0.3128125535633711,"score_spread":0.26710714713667805,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2486303733","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":[0.9978258,0.00011987421,0.00089813344,0.00031033743,0.000114197435,0.00017626825,0.000015514379,0.000005474661,0.0005344206],"genre_scores_gemma":[0.99624354,0.00011607286,0.00313906,0.000042402167,0.00021380126,0.0000067790766,9.55456e-7,0.000024694427,0.00021269945],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9961754,0.00046180908,0.0007381821,0.0002858039,0.0017667437,0.0005720753],"domain_scores_gemma":[0.99808145,0.000651578,0.00043214494,0.00032140035,0.00019488407,0.00031856133],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009852211,0.00019515264,0.00054594164,0.0000032290302,0.00007713995,0.00002454186,0.0006428514,0.000112782116,0.0025664999],"category_scores_gemma":[0.001133137,0.00012450719,0.00018778352,0.00044880866,0.00064939994,0.0002963055,0.00028240655,0.00044213503,0.00013888699],"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":[0.00091377366,0.00090138573,0.5826305,0.000012176296,0.0001345397,0.000117079355,0.0009939073,0.00009515886,0.33183926,0.00003734386,0.0009816453,0.081343226],"study_design_scores_gemma":[0.0016378758,0.0005916219,0.9709981,0.00016858717,0.000015552867,0.0000015526515,0.00031000862,0.00043726954,0.023621727,0.001664339,0.00039883706,0.00015455016],"about_ca_topic_score_codex":0.0021656891,"about_ca_topic_score_gemma":0.00013920586,"teacher_disagreement_score":0.38836756,"about_ca_system_score_codex":0.0004005998,"about_ca_system_score_gemma":0.00011272256,"threshold_uncertainty_score":0.9983453},"labels":[],"label_agreement":null},{"id":"W2504850934","doi":"10.1080/02786826.2016.1219691","title":"Assessing the accuracy of complex refractive index retrievals from single aerosol particle cavity ring-down spectroscopy","year":2016,"lang":"en","type":"article","venue":"Aerosol Science and Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Environment Research Council; Engineering and Physical Sciences Research Council; Natural Sciences and Engineering Research Council of Canada; University of Bristol","keywords":"Aerosol; Cavity ring-down spectroscopy; Refractive index; Particle (ecology); RADIUS; Optics; Spectroscopy; Mie scattering; Extinction (optical mineralogy); Absorption (acoustics); Chemistry; Molecular physics; Materials science; Laser; Scattering; Light scattering; Physics","score_opus":0.021530587316087337,"score_gpt":0.2874072221213347,"score_spread":0.26587663480524737,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2504850934","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":[0.99072874,0.000049158632,0.0027540363,0.004333955,0.00008392881,0.00022415494,0.000006793282,0.00008366727,0.0017355987],"genre_scores_gemma":[0.99780285,0.0000371305,0.0018377731,0.00020812868,0.000023127708,0.000014569946,3.7349304e-7,0.0000105403715,0.00006551771],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9978844,0.000045547873,0.00030902243,0.0006168777,0.0005724893,0.0005716516],"domain_scores_gemma":[0.9985868,0.00030212555,0.00030291328,0.00063806557,0.000062670486,0.00010745578],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00059128914,0.00017991834,0.00025131938,0.0000068930667,0.0006029066,0.00010260482,0.0008077667,0.00013323601,0.00051878864],"category_scores_gemma":[0.00086321944,0.00010293552,0.000032180065,0.0013632551,0.0056021255,0.0009221865,0.0007792059,0.0001852444,0.00006428861],"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":[0.000008734315,0.000061054336,0.113756806,8.6766045e-7,0.0000046362006,0.0000021766832,0.000100683494,0.0000019937959,0.8666308,0.00017427665,0.00009321689,0.019164782],"study_design_scores_gemma":[0.00037691338,0.00019174065,0.08220472,0.000026238693,0.000013568574,0.000009276448,0.00066097354,0.00048170405,0.91353714,0.0020376632,0.00027148545,0.00018855938],"about_ca_topic_score_codex":0.00069116324,"about_ca_topic_score_gemma":0.00013836897,"teacher_disagreement_score":0.046906386,"about_ca_system_score_codex":0.00021026556,"about_ca_system_score_gemma":0.00006848836,"threshold_uncertainty_score":0.99710405},"labels":[],"label_agreement":null},{"id":"W2509469156","doi":"10.5194/acp-17-2359-2017","title":"Directional, horizontal inhomogeneities of cloud optical thickness fields retrieved from ground-based and airbornespectral imaging","year":2017,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":22,"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":"Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research; Deutsche Forschungsgemeinschaft; Aurora Research Institute","keywords":"Cirrus; Radiance; Radiative transfer; Cloud computing; Atmospheric sciences; Arctic; Remote sensing; Environmental science; Physics; Meteorology; Geology; Optics","score_opus":0.006641212779305227,"score_gpt":0.2110914886775187,"score_spread":0.20445027589821346,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2509469156","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":[0.98820406,0.0001760698,0.0032743572,0.0001675699,0.00008608137,0.000049904364,0.000011229013,0.000018885674,0.008011821],"genre_scores_gemma":[0.9911727,0.00004709171,0.007935326,0.000060618237,0.00024451932,0.000005820406,0.000009276158,0.000013418257,0.00051125855],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991542,0.000010436681,0.00015474755,0.00031489364,0.00018019407,0.00018550677],"domain_scores_gemma":[0.9993816,0.000076666416,0.00011948919,0.00031499015,0.00001034959,0.00009691755],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000060367634,0.00017266581,0.0002072627,8.044273e-9,0.00034665118,0.000078575846,0.00018282673,0.000087548135,0.0008997056],"category_scores_gemma":[0.00002422902,0.00016559732,0.000055969096,0.000043413085,0.00070968014,0.00016601231,0.00014108128,0.00015080013,0.0000039185384],"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":[0.00019634145,0.00022289119,0.788229,0.00008394359,0.0000702407,0.000019340072,0.0004902972,0.0002979776,0.09860303,0.0003266682,0.00037082317,0.11108947],"study_design_scores_gemma":[0.0015913296,0.000103232975,0.829411,0.0000787249,0.00012548492,0.000022319755,0.0004990158,0.031577162,0.12703672,0.0074112127,0.0013255987,0.000818205],"about_ca_topic_score_codex":0.0013664014,"about_ca_topic_score_gemma":0.00001580449,"teacher_disagreement_score":0.11027127,"about_ca_system_score_codex":0.000034697016,"about_ca_system_score_gemma":0.000018680943,"threshold_uncertainty_score":0.9851146},"labels":[],"label_agreement":null},{"id":"W2511790667","doi":"10.1016/j.jaerosci.2016.08.006","title":"Study of aerosol optical properties during long-range transport of biomass burning from Canada to Central Europe in July 2013","year":2016,"lang":"en","type":"article","venue":"Journal of Aerosol Science","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":78,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Aerosol; AERONET; Environmental science; Atmospheric sciences; Single-scattering albedo; Climatology; Lidar; Mineral dust; Anomaly (physics); Albedo (alchemy); Range (aeronautics); Forcing (mathematics); Meteorology; Geology; Remote sensing; Geography","score_opus":0.011435934328365304,"score_gpt":0.2050781832530908,"score_spread":0.19364224892472548,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2511790667","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":[0.99881047,0.00007032132,0.00014278428,0.0003466424,0.00022887238,0.0002299129,0.0000061567725,0.000004100759,0.00016074444],"genre_scores_gemma":[0.99918777,0.000024480776,0.0005992509,0.000022351383,0.000040436942,0.0000026103833,4.9049355e-8,0.000012057563,0.000111000365],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9968533,0.0000494976,0.00084743026,0.00032544904,0.0013910808,0.0005332275],"domain_scores_gemma":[0.9988543,0.0000399039,0.0004113607,0.00025515977,0.000085441934,0.00035382883],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004907895,0.00017798976,0.0003967962,0.000011998836,0.000109585955,0.000018824716,0.00084037945,0.00003612813,0.00018029452],"category_scores_gemma":[0.00010906612,0.000109151035,0.000057399535,0.0007947275,0.0005198996,0.00053556636,0.0001807905,0.00015054007,0.0000071797017],"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":[0.00010200134,0.00022000285,0.46670032,0.000006243178,0.0000075673747,0.00009357024,0.0013812627,0.0013217254,0.5299202,4.1648667e-7,0.00003662991,0.00021005161],"study_design_scores_gemma":[0.0009312747,0.0005300067,0.7995907,0.0001896945,0.000017050057,0.000018990637,0.00064346043,0.00002003344,0.19788198,8.595187e-7,0.0000070651945,0.00016886441],"about_ca_topic_score_codex":0.10542842,"about_ca_topic_score_gemma":0.13624462,"teacher_disagreement_score":0.3328904,"about_ca_system_score_codex":0.0003389808,"about_ca_system_score_gemma":0.00030155617,"threshold_uncertainty_score":0.9005286},"labels":[],"label_agreement":null},{"id":"W2512883043","doi":"10.5194/acp-17-1143-2017","title":"The surface aerosol optical properties in the urban area of Nanjing, west Yangtze River Delta, China","year":2017,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":38,"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 Toronto","funders":"Priority Academic Program Development of Jiangsu Higher Education Institutions; Nanjing University; National Natural Science Foundation of China; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Aerosol; Angstrom exponent; Single-scattering albedo; Environmental science; Atmospheric sciences; Relative humidity; Seasonality; Radiative transfer; Radiative forcing; Atmosphere (unit); Climatology; Extinction (optical mineralogy); Albedo (alchemy); Haze; Meteorology; Chemistry; Mineralogy; Physics; Optics; Geology","score_opus":0.009093430499852955,"score_gpt":0.20213736218008937,"score_spread":0.19304393168023642,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2512883043","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":[0.98076683,0.00020322496,0.00010275827,0.0002564156,0.00003276356,0.000113296875,0.000002180122,0.0000088033985,0.018513722],"genre_scores_gemma":[0.995853,0.00011877007,0.00086072896,0.000036044912,0.00006401883,0.000010251632,0.0000012031384,0.00001127333,0.0030446888],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990765,0.000020531663,0.00016994351,0.00023291845,0.00024678485,0.00025335656],"domain_scores_gemma":[0.99916935,0.000050327282,0.00012955874,0.00059143035,0.0000075017006,0.000051831088],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016493397,0.0001685665,0.00016157601,3.8023473e-9,0.0006176316,0.000094468414,0.0005706453,0.0000651868,0.0002158503],"category_scores_gemma":[0.000030828698,0.00009457507,0.00005739565,0.000060754923,0.0012188863,0.00013374469,0.00020521956,0.00019145984,0.000013046861],"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":[0.00015829201,0.00069501833,0.75402,0.000133847,0.00008209041,0.000024972936,0.012055798,0.0051133083,0.06771268,0.00037627734,0.0028274846,0.15680026],"study_design_scores_gemma":[0.0013079987,0.00014385811,0.89932483,0.00013048653,0.00009178929,0.000021654168,0.0022510374,0.037819825,0.047196656,0.0014484336,0.009385226,0.0008781813],"about_ca_topic_score_codex":0.0006394917,"about_ca_topic_score_gemma":0.000024246101,"teacher_disagreement_score":0.15592207,"about_ca_system_score_codex":0.000027611837,"about_ca_system_score_gemma":0.000013753592,"threshold_uncertainty_score":0.47503853},"labels":[],"label_agreement":null},{"id":"W2513196216","doi":"10.3390/rs8090739","title":"Global Surface Net-Radiation at 5 km from MODIS Terra","year":2016,"lang":"en","type":"article","venue":"Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McMaster University","funders":"","keywords":"Remote sensing; Environmental science; Meteorology; Geology; Geography","score_opus":0.007583019603677911,"score_gpt":0.20966494118538012,"score_spread":0.2020819215817022,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2513196216","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":[0.95445913,0.000047333644,0.03241611,0.00068216934,0.00018412495,0.000062119936,0.0000123671925,0.00005552633,0.012081139],"genre_scores_gemma":[0.9832041,0.0000281326,0.015362396,0.00024153978,0.0000840849,2.5168343e-9,0.000003993629,0.000011054818,0.0010646594],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9990996,0.00003553232,0.00013025365,0.00028256496,0.00021206465,0.00023996552],"domain_scores_gemma":[0.99957335,0.00003028925,0.000066715205,0.00023271564,0.000003230381,0.00009372235],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000059484613,0.000112330716,0.00010375287,2.8383187e-7,0.00012228561,0.000018482948,0.00007635875,0.000068784575,0.00083915546],"category_scores_gemma":[0.000017456185,0.00008126961,0.00004555866,0.00009793198,0.00008284474,0.00010611328,0.000130518,0.00002765383,0.0009921051],"study_design_candidate":"design_other","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":[0.000018316237,0.0000056169856,0.02347065,7.3452327e-7,0.000008861739,0.000013902725,0.00014177048,0.0025512488,0.06718176,0.0000034637362,0.0032377061,0.90336597],"study_design_scores_gemma":[0.0013764254,0.00007919284,0.5140643,0.00010448914,0.0000533949,0.000050296705,0.00013121893,0.4254797,0.010979844,0.0035419287,0.043217365,0.0009218187],"about_ca_topic_score_codex":0.00304342,"about_ca_topic_score_gemma":0.0003171536,"teacher_disagreement_score":0.9024441,"about_ca_system_score_codex":0.00055434956,"about_ca_system_score_gemma":0.0000056036442,"threshold_uncertainty_score":0.9997857},"labels":[],"label_agreement":null},{"id":"W2513698149","doi":"","title":"Atmospheric Ice Nuclei and Ice Cloud Formation: Field, Laboratory, and Modeling Studies II Posters","year":2014,"lang":"en","type":"article","venue":"2014 AGU Fall Meeting","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Ice formation; Cloud computing; Meteorology; Atmospheric sciences; Environmental science; Astrobiology; Ice nucleus; Geology; Chemistry; Physics; Computer science","score_opus":0.011156169788182154,"score_gpt":0.22829513658226566,"score_spread":0.2171389667940835,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2513698149","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":[0.9896786,0.0009054722,0.0034301565,0.0006548141,0.0001608622,0.000114965944,8.7377293e-7,0.000058425638,0.0049958257],"genre_scores_gemma":[0.9862677,0.00033435595,0.011809202,0.0012706786,0.00012597672,0.000008819155,8.1711494e-7,0.000018043303,0.00016439434],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99891096,0.000065923414,0.00024356418,0.00030514432,0.00019479117,0.00027960035],"domain_scores_gemma":[0.9994709,0.00011198467,0.00011231871,0.00017714783,0.000020774429,0.00010691333],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043311281,0.00017554138,0.00019959285,6.7428306e-7,0.0005081296,0.000053631218,0.00012521917,0.00007385518,0.000025777415],"category_scores_gemma":[0.00012185323,0.00015405225,0.000024531972,0.0000990245,0.00009846979,0.00032065192,0.000405924,0.00011656387,0.000046380625],"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":[0.00025185224,0.00023918171,0.62302125,0.0007563333,0.0002768505,0.000025930036,0.062162057,0.068043835,0.022359401,0.0021475211,0.045045704,0.17567009],"study_design_scores_gemma":[0.0012254394,0.0005602702,0.005252991,0.0002323188,0.00010477897,0.000026087506,0.010715451,0.9538733,0.0005508294,0.0006775634,0.025794353,0.0009866128],"about_ca_topic_score_codex":0.0006703537,"about_ca_topic_score_gemma":0.0003843217,"teacher_disagreement_score":0.88582945,"about_ca_system_score_codex":0.000043865384,"about_ca_system_score_gemma":0.0000036139925,"threshold_uncertainty_score":0.62820685},"labels":[],"label_agreement":null},{"id":"W2513757635","doi":"","title":"Dust Storm over the Middle East: Retrieval Approach, Source Identification, and Trend Analysis","year":2014,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Storm; Identification (biology); Middle East; Meteorology; Geography; Environmental science; Archaeology","score_opus":0.017465602612222568,"score_gpt":0.20953694912115298,"score_spread":0.1920713465089304,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2513757635","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":[0.9816195,0.00005596246,0.0007656965,0.00015024167,0.00007133416,0.00009574771,0.000001973817,0.00004522061,0.017194357],"genre_scores_gemma":[0.9962246,0.000007624672,0.00055153406,0.00016868029,0.00009122928,0.0000049739615,0.0000103848115,0.00001568377,0.0029253177],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985257,0.000073199444,0.0003121904,0.0004180905,0.00038786104,0.00028297523],"domain_scores_gemma":[0.9990886,0.00011196969,0.0002492327,0.0004175439,0.000007836701,0.00012481297],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009129262,0.00015745113,0.00017173373,0.0000038756525,0.0003630031,0.00012010727,0.00027531324,0.000084225576,0.000050772196],"category_scores_gemma":[0.00018297312,0.0001141673,0.00008577618,0.0004471509,0.00022987233,0.000120852965,0.0001283362,0.00016763306,0.00008129587],"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":[0.00001749951,0.00010331768,0.9436392,0.000011840204,0.00011844849,0.0000012820788,0.0034999405,0.045445234,0.0014303323,0.000032777745,0.0014238221,0.0042762575],"study_design_scores_gemma":[0.0001419343,0.000016720298,0.9786059,0.000005547258,0.00018478783,0.000003188255,0.0007867968,0.0138535155,0.000076648656,0.000037968526,0.0061195726,0.00016738752],"about_ca_topic_score_codex":0.004666074,"about_ca_topic_score_gemma":0.0032674486,"teacher_disagreement_score":0.034966685,"about_ca_system_score_codex":0.000048610305,"about_ca_system_score_gemma":0.0000041361795,"threshold_uncertainty_score":0.70537394},"labels":[],"label_agreement":null},{"id":"W2516402644","doi":"10.5194/amt-2016-244","title":"Radiative characteristics of aerosol under smoke mist conditions in Siberia during summer 2012","year":2016,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":5,"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; AERONET; Environmental science; Atmospheric sciences; Single-scattering albedo; Satellite; Angstrom exponent; Radiative transfer; Meteorology; Climatology; Geography; Physics; Geology","score_opus":0.01272286937095222,"score_gpt":0.23787099133299802,"score_spread":0.2251481219620458,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2516402644","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":[0.98883533,0.000007198723,0.0008338166,0.00028520083,0.00006791246,0.000101522885,0.000030470448,0.00001463948,0.009823924],"genre_scores_gemma":[0.99289584,0.000025247447,0.0002628706,0.00011733122,0.000020590189,0.000012565977,0.000003377016,0.000010307013,0.006651854],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999233,0.00002399045,0.0002221999,0.00017860548,0.00012918726,0.00021300426],"domain_scores_gemma":[0.99962735,0.000047923568,0.00008506441,0.0001634689,0.0000050529898,0.00007114167],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000055060413,0.000100326804,0.00014430573,0.00000137151,0.00004868368,0.0000056494323,0.00011050509,0.000051764575,0.021906406],"category_scores_gemma":[0.00001334229,0.000068223875,0.000037513677,0.000102647224,0.00024098632,0.00018011604,0.00007777611,0.00004458883,0.0002987985],"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":[0.00002300145,0.00014912857,0.8051567,0.000006712987,0.000014475613,0.000004948681,0.00022549431,0.000053453758,0.19173075,0.0006428328,0.0011853941,0.0008071014],"study_design_scores_gemma":[0.00044907542,0.000021049878,0.9855741,0.000015738107,0.000005186585,0.0000013297855,0.000107350024,0.000022867403,0.01338532,0.00012717558,0.00016554505,0.00012520999],"about_ca_topic_score_codex":0.00036311237,"about_ca_topic_score_gemma":0.00023514178,"teacher_disagreement_score":0.18041745,"about_ca_system_score_codex":0.000114393915,"about_ca_system_score_gemma":0.000008001249,"threshold_uncertainty_score":0.9789877},"labels":[],"label_agreement":null},{"id":"W2517564487","doi":"","title":"Multisensor, Model, and Measurement Synergy: Global Aerosol Characterization II","year":2015,"lang":"en","type":"article","venue":"2015 AGU Fall Meeting","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Aerosol; Remote sensing; Environmental science; Characterization (materials science); Computer science; Meteorology; Geography; Materials science; Nanotechnology","score_opus":0.028440167720220677,"score_gpt":0.2362093786486303,"score_spread":0.20776921092840964,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2517564487","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":[0.9848239,0.00008803014,0.0041945963,0.00026191716,0.00013020638,0.00015881965,0.0000058979376,0.00007440554,0.010262221],"genre_scores_gemma":[0.993476,0.000019198953,0.005629452,0.00024415765,0.000061948725,0.000014478351,0.0000073722686,0.000015634803,0.000531761],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99851406,0.000043636945,0.00021503572,0.00033915057,0.00058363884,0.00030445564],"domain_scores_gemma":[0.9994239,0.000004797962,0.00011372044,0.00017967811,0.000034415705,0.00024344797],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044153104,0.00016890143,0.00015164273,8.6088573e-7,0.00019217035,0.000041513576,0.00013469519,0.00007862096,0.000015890495],"category_scores_gemma":[0.00009256232,0.00015311076,0.000027546055,0.00010614029,0.000082552106,0.00020284472,0.00030175532,0.000067507994,0.000092718066],"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":[0.00011336012,0.00027526869,0.5978441,0.000029138086,0.000051463292,0.000018953793,0.003460649,0.080502644,0.2820253,0.00030065415,0.0076687583,0.02770969],"study_design_scores_gemma":[0.0023608638,0.00034943927,0.07563296,0.00014182534,0.00008407502,0.000031785683,0.00071196316,0.9072368,0.0025782757,0.00041782684,0.009234862,0.0012193103],"about_ca_topic_score_codex":0.0015064805,"about_ca_topic_score_gemma":0.0008470043,"teacher_disagreement_score":0.8267342,"about_ca_system_score_codex":0.00041366144,"about_ca_system_score_gemma":0.000026043592,"threshold_uncertainty_score":0.62436754},"labels":[],"label_agreement":null},{"id":"W2519107385","doi":"10.1002/2016ms000751","title":"Validation of a weather forecast model at radiance level against satellite observations allowing quantification of temperature, humidity, and cloud‐related biases","year":2016,"lang":"en","type":"article","venue":"Journal of Advances in Modeling Earth Systems","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada; McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Radiance; Environmental science; Water vapor; Infrared window; Overcast; Radiative transfer; Sky; Remote sensing; Troposphere; Brightness temperature; Atmospheric sciences; Atmospheric Infrared Sounder; Meteorology; Infrared; Brightness; Geology; Physics; Optics","score_opus":0.06323299177560394,"score_gpt":0.2677229895916908,"score_spread":0.20448999781608684,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2519107385","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":[0.95249784,0.0030801166,0.04387391,0.000044983783,0.0002472396,0.00013833749,0.000013844624,0.0000045957877,0.000099131954],"genre_scores_gemma":[0.99043566,0.003754833,0.005553471,0.0000078034245,0.000040023806,0.0000030059232,0.0000022427969,0.000012720998,0.00019023333],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99845856,0.00006643955,0.0008517173,0.00015973664,0.00032712016,0.00013643247],"domain_scores_gemma":[0.99895585,0.00009775084,0.0006805096,0.0001435837,0.00007062265,0.000051664156],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00058860495,0.00011380696,0.00028886864,0.000012494029,0.000059828144,0.000012950178,0.00013572887,0.00007629733,0.000008292636],"category_scores_gemma":[0.00009395578,0.00007997088,0.00006520067,0.00018590303,0.00009161753,0.00070133124,0.000038003847,0.00008386241,0.0000014231998],"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":[0.000027025944,0.000030174893,0.031335227,0.000028682694,0.000008695668,8.257101e-7,0.00030572043,0.8042265,0.16204785,0.00006324003,0.0000054727557,0.0019205362],"study_design_scores_gemma":[0.00083046895,0.000109203196,0.0052845087,0.0014791945,0.000024097535,0.000019973008,0.0003112886,0.97588325,0.015193009,0.0004866483,0.00018231856,0.00019604167],"about_ca_topic_score_codex":0.000035908928,"about_ca_topic_score_gemma":0.0000439436,"teacher_disagreement_score":0.1716567,"about_ca_system_score_codex":0.00007214692,"about_ca_system_score_gemma":0.00002234424,"threshold_uncertainty_score":0.32611176},"labels":[],"label_agreement":null},{"id":"W2527337019","doi":"10.5194/acp-16-15689-2016","title":"Airborne observations of far-infrared upwelling radiance in the Arctic","year":2016,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":7,"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 Toronto; Environment and Climate Change Canada; University of Guelph; Université de Sherbrooke","funders":"Canadian Space Agency; Max-Planck-Institut für Chemie; Environment and Climate Change Canada; Eurostars; University of Toronto; Natural Sciences and Engineering Research Council of Canada; Université de Sherbrooke","keywords":"Radiance; Environmental science; Arctic; Radiative transfer; Remote sensing; Atmospheric sciences; Atmospheric radiative transfer codes; Radiometry; Earth's energy budget; Atmosphere (unit); Radiometer; Irradiance; Liquid water path; Meteorology; Radiation; Geology; Physics; Optics","score_opus":0.011002739011269958,"score_gpt":0.20102690648497845,"score_spread":0.19002416747370848,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2527337019","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":[0.992047,0.000118459335,0.0036473388,0.00027020587,0.000013911827,0.00006786497,0.0000028556753,0.0000091062675,0.003823241],"genre_scores_gemma":[0.99053234,0.0001641982,0.0059875627,0.00017164797,0.00004569876,0.000014171798,0.0000016366366,0.0000075414678,0.0030752132],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993651,0.000014922898,0.0001520595,0.00017886737,0.00013166742,0.00015739175],"domain_scores_gemma":[0.9995582,0.00009655346,0.00006823598,0.00023476388,0.0000059431213,0.000036301608],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008315947,0.000101556725,0.000110961555,5.52708e-9,0.00006162764,0.000008440111,0.00018545789,0.000041257463,0.000889762],"category_scores_gemma":[0.000016601214,0.000063414576,0.000035784935,0.00022814522,0.00020763121,0.00010148217,0.000036822355,0.000068277186,0.000015662947],"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":[0.000031453077,0.000253843,0.48230562,0.0000915771,0.000024706198,0.0000070354336,0.0017056145,0.0020882734,0.15463483,0.0006393035,0.0008574527,0.35736027],"study_design_scores_gemma":[0.0009018973,0.000046853347,0.9500425,0.0001095506,0.000032221746,0.000008680909,0.00047572772,0.009942024,0.012331953,0.011566759,0.014122341,0.00041949755],"about_ca_topic_score_codex":0.00013854294,"about_ca_topic_score_gemma":0.000004374931,"teacher_disagreement_score":0.46773687,"about_ca_system_score_codex":0.000036084344,"about_ca_system_score_gemma":0.000009255618,"threshold_uncertainty_score":0.974227},"labels":[],"label_agreement":null},{"id":"W2531856869","doi":"10.54782/jwm.v17i1.111","title":"Prediction of Droplet Trajectories to Determine Sensor Placement On Cloud Physics Research Aircraft","year":2012,"lang":"en","type":"article","venue":"The Journal of Weather Modification","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"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":"Perturbation (astronomy); Trajectory; Meteorology; Aerospace engineering; Mass flux; Environmental science; Cloud computing; Flux (metallurgy); Physics; Atmospheric sciences; Mechanics; Engineering; Computer science; Materials science; Astronomy","score_opus":0.09317826249807702,"score_gpt":0.30854754113373434,"score_spread":0.2153692786356573,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2531856869","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":[0.9828992,0.000032192445,0.01548497,0.00043118576,0.00021399808,0.00017832707,0.0000037805764,0.000004946309,0.00075141486],"genre_scores_gemma":[0.9980329,0.00003662287,0.0008738489,0.00004514001,0.00041422664,0.0000048119623,7.1678056e-7,0.000011244719,0.0005804353],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9986745,0.00018662834,0.00027204107,0.000068244815,0.00061132474,0.0001872585],"domain_scores_gemma":[0.9993483,0.00010122712,0.00019181924,0.0002296756,0.00004649701,0.00008247065],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001454616,0.00007571283,0.000107552754,0.0000038660196,0.00010971572,0.000007476761,0.00020153911,0.000033185468,0.000182825],"category_scores_gemma":[0.00004058837,0.000047465135,0.000042243573,0.00020537236,0.0001059843,0.00012559381,0.000038383536,0.00015822162,0.000072626484],"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":[0.0011467616,0.0013608354,0.09377523,0.000022373351,0.00007933413,9.602622e-7,0.03321765,0.053388882,0.77456653,0.00060749025,0.014071678,0.027762286],"study_design_scores_gemma":[0.0014312192,0.0036738296,0.73675716,0.0001384612,0.00017354956,0.000056519402,0.0084776245,0.0055373395,0.22414431,0.0010316815,0.018226443,0.00035187643],"about_ca_topic_score_codex":0.00005098281,"about_ca_topic_score_gemma":0.0000021192761,"teacher_disagreement_score":0.64298195,"about_ca_system_score_codex":0.00016775276,"about_ca_system_score_gemma":0.000010063064,"threshold_uncertainty_score":0.20018055},"labels":[],"label_agreement":null},{"id":"W2532891280","doi":"10.1002/2016gl070776","title":"Estimation of cloud fraction profile in shallow convection using a scanning cloud radar","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","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":"McGill University","funders":"Biological and Environmental Research; Office of Science; Battelle; U.S. Department of Energy","keywords":"Radar; Meteorology; Zenith; Cloud computing; Wind profiler; Convection; Environmental science; Geology; Remote sensing; Computer science; Physics","score_opus":0.029160779675995483,"score_gpt":0.3103857933585106,"score_spread":0.28122501368251507,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2532891280","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":[0.98134005,0.000004319702,0.016791254,0.0010327247,0.00011510627,0.00024527396,0.0000019794306,0.00001825425,0.0004510553],"genre_scores_gemma":[0.99704695,0.0000036991203,0.0025176923,0.00009375924,0.00016747594,0.000022056542,0.000001832497,0.0000141445635,0.0001323792],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99811095,0.00019081616,0.00021260478,0.00031226585,0.00074079935,0.0004325481],"domain_scores_gemma":[0.9994356,0.00019023322,0.00007598651,0.00019564203,0.00001558232,0.000086925145],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005259346,0.000099549594,0.0001521906,0.000009239643,0.00012136549,0.000018016557,0.00015884668,0.00005820397,0.0005034212],"category_scores_gemma":[0.0001648946,0.000075469805,0.000051910152,0.00050803943,0.0003902477,0.0003255122,0.0001418227,0.00023213867,0.00026404348],"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":[0.00009330696,0.0000989768,0.016122151,0.000013571028,0.0000060475127,0.000007654755,0.00019379628,0.0016119545,0.94451654,0.00012868029,0.0011900783,0.03601725],"study_design_scores_gemma":[0.002474717,0.00061445305,0.6913506,0.00050266867,0.000020360356,0.000009040265,0.0006148506,0.18648356,0.11174111,0.0039715185,0.0015135148,0.00070359727],"about_ca_topic_score_codex":0.0034918783,"about_ca_topic_score_gemma":0.00003188903,"teacher_disagreement_score":0.8327754,"about_ca_system_score_codex":0.00052230945,"about_ca_system_score_gemma":0.000022938179,"threshold_uncertainty_score":0.5512109},"labels":[],"label_agreement":null},{"id":"W2533438009","doi":"10.5194/amt-10-2239-2017","title":"Evaluation of radar reflectivity factor simulations of ice crystal populations from in situ observations for the retrieval of condensed water content in tropical mesoscale convective systems","year":2017,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":12,"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":"Federal Aviation Administration; Centre National de la Recherche Scientifique; Centre National d’Etudes Spatiales; Transport Canada; National Aeronautics and Space Administration; European Commission; Boeing","keywords":"Ice crystals; Radar; Atmospheric sciences; Environmental science; Range (aeronautics); Mesoscale meteorology; Meteorology; Remote sensing; Materials science; Geology; Physics","score_opus":0.21728918874095451,"score_gpt":0.32778871274327154,"score_spread":0.11049952400231702,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2533438009","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":[0.9577377,0.00010561809,0.03969979,0.00012577932,0.00008832778,0.0019608755,0.000043487973,0.00001769899,0.00022073294],"genre_scores_gemma":[0.9902503,0.0000056997196,0.00954568,0.000009878787,0.000014533809,0.00012807055,0.000008213576,0.00001277494,0.000024864952],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9975601,0.00027127462,0.00066123315,0.00025854338,0.0010692573,0.00017963393],"domain_scores_gemma":[0.99841875,0.00019878002,0.0004888486,0.00050836796,0.00035437185,0.000030896626],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012764699,0.00014541455,0.00035918702,0.0000016229546,0.00015288175,0.000017005465,0.00029562836,0.000109497676,0.0001000428],"category_scores_gemma":[0.0008308329,0.000102826445,0.0000915291,0.00012645793,0.00025998228,0.00018473342,0.00008694994,0.000103751234,3.6534323e-7],"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":[0.000120772136,0.00025483168,0.36947927,0.000015868942,0.000046208424,1.4728334e-7,0.0007066474,0.003181401,0.62532705,0.00013296572,0.000028494904,0.000706344],"study_design_scores_gemma":[0.0008376364,0.00014341153,0.8255947,0.000067867055,0.000101683116,1.1129457e-7,0.000254858,0.028846916,0.14287882,0.0011213712,0.000043691525,0.00010892424],"about_ca_topic_score_codex":0.010879215,"about_ca_topic_score_gemma":0.0061392956,"teacher_disagreement_score":0.48244825,"about_ca_system_score_codex":0.000526125,"about_ca_system_score_gemma":0.000062582105,"threshold_uncertainty_score":0.99570745},"labels":[],"label_agreement":null},{"id":"W2535143197","doi":"10.5194/gmd-10-1447-2017","title":"A new aerosol wet removal scheme for the Lagrangian particle model FLEXPART v10","year":2017,"lang":"en","type":"article","venue":"Geoscientific model development","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":127,"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":"Leibniz-Institut für Troposphärenforschung; Leibniz-Gemeinschaft; National Oceanic and Atmospheric Administration; NordForsk; Environment and Climate Change Canada; U.S. Department of Energy; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; National Science Foundation","keywords":"Aerosol; Scavenging; Ice nucleus; Atmospheric sciences; Environmental science; Meteorology; Liquid water content; Ice crystals; Particle (ecology); Nucleation; Chemistry; Cloud computing; Geology; Physics","score_opus":0.034603533782187966,"score_gpt":0.25617822134961576,"score_spread":0.2215746875674278,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2535143197","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"methods","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.35936117,0.00004396269,0.6341206,0.0013370248,0.0005185776,0.00064563536,0.000015224704,0.00006526157,0.0038925237],"genre_scores_gemma":[0.52383304,0.000009225722,0.32075465,0.0004016833,0.00005265807,0.00016387895,0.000010907631,0.000030281555,0.1547437],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99754834,0.000011482891,0.0003573798,0.0007147148,0.0006244191,0.00074366917],"domain_scores_gemma":[0.9983326,0.000023626626,0.00018428806,0.0011445811,0.00002470109,0.0002901653],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0007235076,0.00025104085,0.0001889213,0.0000020604223,0.0026230034,0.00042247292,0.0011861243,0.000085010826,0.00055144477],"category_scores_gemma":[0.000051549876,0.0001821171,0.00011637804,0.000100088364,0.00030415217,0.0003248539,0.0006578303,0.000117005206,0.0005105296],"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":[0.00022207657,0.00042345974,0.0077940137,0.00004237501,0.000120949124,0.000014866754,0.008884755,0.3778872,0.048865635,0.004038736,0.34714654,0.20455939],"study_design_scores_gemma":[0.000533974,0.000011664922,0.002046202,0.000011249115,0.000017315733,0.0000037491031,0.00007008858,0.9426391,0.0041338257,0.00073882507,0.0494812,0.00031278376],"about_ca_topic_score_codex":0.00021821308,"about_ca_topic_score_gemma":0.0004887869,"teacher_disagreement_score":0.5647519,"about_ca_system_score_codex":0.00014372988,"about_ca_system_score_gemma":0.00020404984,"threshold_uncertainty_score":0.99867547},"labels":[],"label_agreement":null},{"id":"W2535986422","doi":"10.1117/12.2242112","title":"Performance of a compact elastic 355 nm airborne lidar in tropical and mid-latitude clouds","year":2016,"lang":"en","type":"article","venue":"Proceedings of SPIE, the International Society for Optical Engineering/Proceedings of SPIE","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"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; National Research Council Canada","funders":"","keywords":"Lidar; Ice crystals; Remote sensing; Supercooling; Cloud top; Environmental science; Atmospheric sciences; Meteorology; Geology; Satellite; Aerospace engineering; Geography","score_opus":0.007159064639155647,"score_gpt":0.20680592047127358,"score_spread":0.19964685583211794,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2535986422","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":[0.9970817,0.000038955382,0.000031933476,0.0012107006,0.00007970947,0.0002738258,0.000013411508,0.0000248698,0.0012449173],"genre_scores_gemma":[0.97781354,0.00011544336,0.02175665,0.00003779756,0.00009061889,0.000025887928,6.2083984e-7,0.000026540938,0.00013292565],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99824774,1.9487588e-8,0.0005612905,0.0003162701,0.00053875044,0.00033595465],"domain_scores_gemma":[0.9993065,0.00012040226,0.00025909665,0.000047904126,0.00015188918,0.00011420358],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002830858,0.00023370936,0.00036653146,0.000009922737,0.0000445226,0.000024669884,0.0005504816,0.00013662032,0.00006874609],"category_scores_gemma":[0.00023583647,0.00015833518,0.00023024647,0.00023574776,0.0004991916,0.00038726337,0.00019264202,0.00017669772,0.000002942573],"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":[0.00021841329,0.00020200087,0.2243142,0.00029455827,0.00014051457,1.3372663e-7,0.00029812442,0.00032687242,0.7250601,0.0473377,0.0006321339,0.0011752596],"study_design_scores_gemma":[0.003162394,0.0012749732,0.8268545,0.0008769403,0.00013319761,0.000022910554,0.0006409738,0.040623352,0.12328139,0.00087317714,0.001629216,0.0006269281],"about_ca_topic_score_codex":0.000024396095,"about_ca_topic_score_gemma":6.8001054e-7,"teacher_disagreement_score":0.6025404,"about_ca_system_score_codex":0.00017254714,"about_ca_system_score_gemma":0.00001330493,"threshold_uncertainty_score":0.64567214},"labels":[],"label_agreement":null},{"id":"W2549148406","doi":"","title":"Autonomous Ozone and Aerosol Lidar Platform: Preliminary Results","year":2014,"lang":"en","type":"article","venue":"2014 AGU Fall Meeting","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"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":"Aerosol; Lidar; Environmental science; Remote sensing; Meteorology; Ozone; Atmospheric sciences; Geography; Geology","score_opus":0.008893501557097842,"score_gpt":0.20844516730046772,"score_spread":0.19955166574336988,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2549148406","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":[0.92161494,0.00009346624,0.000645424,0.0002502627,0.00012246869,0.000152888,0.0000025260297,0.00010295881,0.07701507],"genre_scores_gemma":[0.989097,0.000031142823,0.008424508,0.000322603,0.00013692543,0.000013770036,0.0000056997874,0.000026655849,0.0019417155],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984853,0.0000473481,0.0003247383,0.00047031764,0.0002505788,0.0004216706],"domain_scores_gemma":[0.99920654,0.0001246905,0.00016144669,0.0003251805,0.0000064783417,0.00017565934],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006027954,0.00020094996,0.00019968182,0.0000017368171,0.00027611406,0.00006719421,0.00022548379,0.00011450033,0.000072288734],"category_scores_gemma":[0.00014467735,0.0001761822,0.000045444966,0.00007878323,0.0001705405,0.00023303817,0.00036984554,0.00016443107,0.00067085755],"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":[0.0010376464,0.0004286964,0.66485876,0.00012983479,0.00007368012,0.00006129129,0.00810139,0.007108707,0.02381157,0.00090758235,0.048799828,0.24468103],"study_design_scores_gemma":[0.0066871843,0.004513806,0.72214526,0.00041666432,0.00017806057,0.00018948806,0.0021213188,0.11609075,0.006834782,0.0014143334,0.13617973,0.0032286113],"about_ca_topic_score_codex":0.0020666837,"about_ca_topic_score_gemma":0.00037634454,"teacher_disagreement_score":0.24145243,"about_ca_system_score_codex":0.000058850095,"about_ca_system_score_gemma":0.000006750732,"threshold_uncertainty_score":0.86227405},"labels":[],"label_agreement":null},{"id":"W2550441896","doi":"10.5194/amt-10-2129-2017","title":"Thin ice clouds in the Arctic: cloud optical depth and particle size retrieved from ground-based thermal infrared radiometry","year":2017,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université de Sherbrooke","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency; U.S. Department of Energy; Fonds Québécois de la Recherche sur la Nature et les Technologies; Washington State University; Environment and Climate Change Canada","keywords":"Remote sensing; Ice cloud; Radiance; Downwelling; Cloud top; Environmental science; Arctic; Cirrus; Optical depth; Ice crystals; Radiative transfer; Atmospheric sciences; Geology; Cloud computing; Meteorology; Physics; Optics; Aerosol; Computer science","score_opus":0.025609208583921482,"score_gpt":0.24593457190431353,"score_spread":0.22032536332039204,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2550441896","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":[0.98170567,0.00027588083,0.005411664,0.0012486178,0.00016259769,0.00072402135,0.000002009886,0.00018899668,0.010280556],"genre_scores_gemma":[0.95007545,0.00005029566,0.048008054,0.001447658,0.00013893856,0.00013407721,0.0000017858314,0.000036904305,0.00010682166],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9968388,0.00026544777,0.0004726,0.00062676286,0.0012211679,0.0005751844],"domain_scores_gemma":[0.9979919,0.00025885715,0.00027527794,0.0012708819,0.00003560129,0.00016747342],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0020930066,0.00035478553,0.0003578291,3.6319452e-7,0.00057790196,0.00034075978,0.0011198279,0.00019918794,0.0005765928],"category_scores_gemma":[0.0007842409,0.00025659666,0.00010303377,0.0003050973,0.0005761198,0.00037410003,0.00030954674,0.00040733922,0.00003524113],"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":[0.00024046423,0.00045280598,0.91665417,0.000019040046,0.00004896183,0.00006042529,0.00095449376,0.00005582645,0.031545717,0.00027833277,0.0016588877,0.048030894],"study_design_scores_gemma":[0.0008086703,0.0002680807,0.97807115,0.00006435819,0.00005440176,0.0000036854267,0.00029419194,0.0025357422,0.012701928,0.0015585339,0.0032198145,0.0004194205],"about_ca_topic_score_codex":0.004255332,"about_ca_topic_score_gemma":0.0006090763,"teacher_disagreement_score":0.06141702,"about_ca_system_score_codex":0.000370053,"about_ca_system_score_gemma":0.00004312936,"threshold_uncertainty_score":0.9999886},"labels":[],"label_agreement":null},{"id":"W2550614314","doi":"10.1175/jtech-d-15-0246.1","title":"Ice Crystal Sizes in High Ice Water Content Clouds. Part II: Statistics of Mass Diameter Percentiles in Tropical Convection Observed during the HAIC/HIWC Project","year":2016,"lang":"en","type":"article","venue":"Journal of Atmospheric and Oceanic Technology","topic":"Atmospheric aerosols and clouds","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":"Ice crystals; Atmospheric sciences; Ice nucleus; Icing; Water vapor; Meteorology; Environmental science; Chemistry; Analytical Chemistry (journal); Geology; Geography; Nucleation; Environmental chemistry","score_opus":0.01206754586764837,"score_gpt":0.19961980993014006,"score_spread":0.18755226406249167,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2550614314","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":[0.9951215,0.0001869468,0.0033288184,0.0009567336,0.0001851685,0.00017963834,0.0000049586292,0.000014506731,0.000021741855],"genre_scores_gemma":[0.98953825,0.00058065733,0.009449601,0.000046057936,0.00003551894,0.0000059862823,2.3955621e-7,0.000014991002,0.00032869657],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99846554,0.00008321284,0.00066073716,0.00021614193,0.0002299498,0.0003444077],"domain_scores_gemma":[0.9993544,0.00008863287,0.0003069795,0.00017491638,0.000031073603,0.00004396996],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021736581,0.00017058283,0.00039063144,0.0000030317015,0.00008139431,0.000011575224,0.0002632945,0.00017071016,0.0003350095],"category_scores_gemma":[0.0000930645,0.000085329455,0.000060586084,0.00023025254,0.0005150589,0.00015568374,0.0001951147,0.0002875179,0.0000034027612],"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":[0.00040324425,0.00023643328,0.8905088,0.000035358527,0.00005298956,0.00008821168,0.0005741595,0.00008100596,0.097022094,0.00035973772,0.00025748776,0.010380482],"study_design_scores_gemma":[0.0029077218,0.0010144335,0.98178995,0.0001241637,0.000045540364,0.00015697244,0.0021448054,0.0003578738,0.0074976436,0.0013029992,0.0024205458,0.0002373253],"about_ca_topic_score_codex":0.00016664722,"about_ca_topic_score_gemma":0.0001212356,"teacher_disagreement_score":0.09128118,"about_ca_system_score_codex":0.0002090478,"about_ca_system_score_gemma":0.000024233912,"threshold_uncertainty_score":0.36681193},"labels":[],"label_agreement":null},{"id":"W2552031352","doi":"10.4209/aaqr.2016.08.0350","title":"Satellite-Surface Perspectives of Air Quality and Aerosol-Cloud Effects on the Environment: An Overview of 7-SEAS/BASELInE","year":2016,"lang":"en","type":"article","venue":"Aerosol and Air Quality Research","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"Environmental Protection Administration, Executive Yuan, R.O.C. Taiwan; National Central University; Ministry of Science and Technology, Taiwan; Vietnam Academy of Science and Technology; Silpakorn University; Chiang Mai University; National Aeronautics and Space Administration","keywords":"Aerosol; Environmental science; Air quality index; Trace gas; AERONET; Satellite; Baseline (sea); Atmospheric sciences; Meteorology; Planetary boundary layer; Cloud computing; Climatology; Geography; Oceanography; Geology","score_opus":0.10685237966418101,"score_gpt":0.3760466712260689,"score_spread":0.2691942915618879,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2552031352","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":[0.9906856,0.0030017514,0.000117366195,0.004674314,0.000027778133,0.0005494459,0.000051984407,0.000019833693,0.0008719449],"genre_scores_gemma":[0.9933794,0.0052030003,0.00030847042,0.0002552735,0.000050255643,0.00002375642,0.0000027680517,0.000023320856,0.0007537437],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9944093,0.0024878413,0.00056047615,0.00074987044,0.0012387285,0.0005537906],"domain_scores_gemma":[0.9960595,0.00255823,0.00020280197,0.00085668976,0.000045311426,0.00027746087],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0059606927,0.00026891063,0.00048919197,0.00000424695,0.00034297208,0.000020128824,0.000419274,0.0001376774,0.0007707335],"category_scores_gemma":[0.0004946322,0.0001514202,0.00012537818,0.00026336932,0.0023189425,0.00021329462,0.0005484079,0.0002982566,0.00006797508],"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":[0.00079886045,0.0017037486,0.21386589,0.000753612,0.00015046922,0.0000071079567,0.011093897,0.000083660896,0.6704703,0.017446361,0.0005593201,0.08306674],"study_design_scores_gemma":[0.0023917777,0.0025284728,0.7433004,0.00046135194,0.000044535955,0.0000040856626,0.010141883,0.000112592024,0.23366934,0.0049754046,0.0015226875,0.00084749766],"about_ca_topic_score_codex":0.001345471,"about_ca_topic_score_gemma":0.00008882084,"teacher_disagreement_score":0.5294345,"about_ca_system_score_codex":0.00010162569,"about_ca_system_score_gemma":0.00002623881,"threshold_uncertainty_score":0.854424},"labels":[],"label_agreement":null},{"id":"W2555752492","doi":"10.1002/2016jd025090","title":"The performance of the EarthCARE Cloud Profiling Radar in marine stratiform clouds","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Remote sensing; Environmental science; Radar; Doppler effect; Drizzle; Clutter; Doppler radar; Cloud computing; Meteorology; Geology; Computer science; Geography; Physics","score_opus":0.01765234355434686,"score_gpt":0.2788362661191046,"score_spread":0.26118392256475775,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2555752492","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":[0.9954807,0.000075173106,0.000016695416,0.0013293807,0.00015544308,0.00019660876,0.0000015199838,0.0000031896025,0.0027412495],"genre_scores_gemma":[0.9966462,0.00024018803,0.00077250786,0.000019456782,0.0002308309,0.0000057122375,6.542199e-8,0.000013640814,0.002071399],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99675214,0.0002597679,0.0005289492,0.00016445857,0.0017561188,0.00053853536],"domain_scores_gemma":[0.99849683,0.0006095739,0.00026113633,0.00038179546,0.00011651789,0.0001341371],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014940365,0.00013087825,0.0002301101,9.780017e-7,0.0002930283,0.000037297512,0.0009877011,0.00006386592,0.0004343094],"category_scores_gemma":[0.00039649737,0.000051759154,0.00016141862,0.0005479465,0.0009567434,0.00023977655,0.00059669104,0.0006203398,0.000042747673],"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":[0.00059629296,0.00022302393,0.7772063,0.00002413527,0.000035323545,0.000016876116,0.00020625148,0.00023289194,0.05853628,0.0016661655,0.0012183819,0.1600381],"study_design_scores_gemma":[0.00081944285,0.0010948913,0.9466549,0.00018130397,0.000007570407,0.000014112963,0.00072776614,0.00067766034,0.040886123,0.004388423,0.004406949,0.00014084185],"about_ca_topic_score_codex":0.00024966648,"about_ca_topic_score_gemma":0.00025318968,"teacher_disagreement_score":0.16944864,"about_ca_system_score_codex":0.00018642549,"about_ca_system_score_gemma":0.00014433824,"threshold_uncertainty_score":0.4755383},"labels":[],"label_agreement":null},{"id":"W2556346763","doi":"10.1175/jas-d-16-0172.1","title":"Variational Iteration Method for Infrared Radiative Transfer in a Scattering Medium","year":2016,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","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":"University of Victoria","funders":"Japan Society for the Promotion of Science; National Natural Science Foundation of China","keywords":"Radiative transfer; Scattering; Computational physics; Infrared; Atmospheric radiative transfer codes; Physics; Ordinate; Optics; Mathematics; Geometry","score_opus":0.012644154027269164,"score_gpt":0.2605214038860875,"score_spread":0.24787724985881837,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2556346763","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":[0.6823083,0.000042169457,0.30950767,0.0067335456,0.00055502367,0.00017985902,0.0000019235208,0.000004305042,0.00066720566],"genre_scores_gemma":[0.8580976,0.000013955688,0.1407162,0.00056218746,0.00011368471,0.0000104902065,4.5599855e-8,0.0000055886912,0.00048026477],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99876046,0.000103443825,0.00034868863,0.00014960235,0.00044447166,0.00019330897],"domain_scores_gemma":[0.99936426,0.00029128933,0.0001838656,0.0000875256,0.000021320942,0.000051728777],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012614417,0.00008914934,0.00014509482,8.3794987e-7,0.00016905315,0.000037721496,0.0004939612,0.00003624893,0.000594769],"category_scores_gemma":[0.00017085698,0.000042039057,0.00010453032,0.00045350182,0.00023462807,0.00052265736,0.00005312386,0.00006112935,0.000005815313],"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":[0.00028772108,0.00026958663,0.52787054,0.000014768781,0.00007027739,0.000006419878,0.0073298994,0.17782941,0.20720772,0.0017753496,0.0063891336,0.070949174],"study_design_scores_gemma":[0.0028018479,0.0007047536,0.81704015,0.00019121055,0.000050477836,0.00008827775,0.00078686036,0.13856721,0.008355724,0.021785378,0.009211895,0.00041619196],"about_ca_topic_score_codex":0.000033898665,"about_ca_topic_score_gemma":0.000025766902,"teacher_disagreement_score":0.28916964,"about_ca_system_score_codex":0.00016367387,"about_ca_system_score_gemma":0.00007635476,"threshold_uncertainty_score":0.65123034},"labels":[],"label_agreement":null},{"id":"W2567120496","doi":"10.1002/2016jd025797","title":"Quantifying the low bias of CALIPSO's column aerosol optical depth due to undetected aerosol layers","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":79,"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":"McGill University","keywords":"Aerosol; Lidar; Environmental science; Daytime; Atmospheric sciences; Meteorology; Extinction (optical mineralogy); Remote sensing; Climatology; Geology; Geography; Mineralogy","score_opus":0.06247760500712569,"score_gpt":0.32685732847398535,"score_spread":0.2643797234668597,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2567120496","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":[0.9906999,0.000058424044,0.0045293025,0.0023374797,0.00015192256,0.00037262813,0.0000048809266,0.000015644824,0.0018298385],"genre_scores_gemma":[0.99520606,0.000048740665,0.0031988742,0.0001426989,0.0002800077,0.000016861804,2.1165287e-7,0.000040792926,0.0010657299],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99480426,0.0005209504,0.0008130186,0.00038683577,0.0024939533,0.00098096],"domain_scores_gemma":[0.9961155,0.0020431648,0.00033469606,0.00056244124,0.000268881,0.0006753219],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0016359586,0.00026063915,0.00057144335,0.0000033209146,0.00033797746,0.00010398681,0.0012597328,0.0001419318,0.0014034266],"category_scores_gemma":[0.0020715804,0.00013484618,0.00033562488,0.0010267069,0.0012916045,0.00030257032,0.0006710853,0.0007321813,0.00055788754],"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":[0.002280515,0.0015290661,0.054918244,0.00007586524,0.00032990755,0.0004592086,0.0009924098,0.0027502894,0.7654611,0.0013433249,0.02818318,0.14167689],"study_design_scores_gemma":[0.005473383,0.011023107,0.5962605,0.0013986679,0.00015991207,0.00025978097,0.0039878055,0.0036033378,0.3659943,0.002755579,0.0076091383,0.0014744904],"about_ca_topic_score_codex":0.00121242,"about_ca_topic_score_gemma":0.001567074,"teacher_disagreement_score":0.54134226,"about_ca_system_score_codex":0.0003442422,"about_ca_system_score_gemma":0.00018584488,"threshold_uncertainty_score":0.99950945},"labels":[],"label_agreement":null},{"id":"W2573571850","doi":"10.5194/amt-10-179-2017","title":"Radiative characteristics of aerosol during extreme fire event over Siberia in summer 2012","year":2017,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":56,"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":"Goddard Space Flight Center; National Aeronautics and Space Administration","keywords":"Aerosol; AERONET; Environmental science; Atmospheric sciences; Single-scattering albedo; Albedo (alchemy); Smoke; Satellite; Radiative transfer; Moderate-resolution imaging spectroradiometer; Climatology; Meteorology; Geography; Geology; Physics","score_opus":0.029690912910512093,"score_gpt":0.2525925687301421,"score_spread":0.22290165581962998,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2573571850","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":[0.99027884,0.00018653044,0.002015404,0.00010689117,0.00016155056,0.00067377824,0.000007057173,0.000106507505,0.0064634364],"genre_scores_gemma":[0.9889995,0.00024413306,0.009565326,0.00007102085,0.00006523235,0.00013280554,0.000001758878,0.000041858882,0.0008784014],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99748164,0.00007805738,0.0006207858,0.00048128335,0.000852155,0.00048608865],"domain_scores_gemma":[0.9982324,0.000015914618,0.00066341937,0.00091922167,0.00004112541,0.00012790182],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006422624,0.00033024698,0.0004626487,7.180952e-7,0.00027602163,0.000054163258,0.000671863,0.00015115012,0.0032905233],"category_scores_gemma":[0.00011980773,0.0003056177,0.00013133402,0.0001298307,0.00030549383,0.00050388364,0.00038152223,0.00020554726,0.000039541315],"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":[0.000101109035,0.00041339282,0.8662845,0.00005730958,0.000046489276,0.000026306081,0.00046210433,0.000047555568,0.08432067,0.000031541076,0.0028993539,0.0453097],"study_design_scores_gemma":[0.0004858151,0.00012591352,0.95473725,0.00016983454,0.000026653941,0.0000018258835,0.00004492441,0.0007001396,0.04089714,0.00007836831,0.0023063929,0.00042575656],"about_ca_topic_score_codex":0.0016239432,"about_ca_topic_score_gemma":0.0003084806,"teacher_disagreement_score":0.08845277,"about_ca_system_score_codex":0.000538247,"about_ca_system_score_gemma":0.000032029595,"threshold_uncertainty_score":0.9999396},"labels":[],"label_agreement":null},{"id":"W2577369584","doi":"10.1002/2016gl072455","title":"On the role of ice‐nucleating aerosol in the formation of ice particles in tropical mesoscale convective systems","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":115,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada; Environment and Climate Change Canada","funders":"Natural Sciences and Engineering Research Council of Canada; Transport Canada; Environment and Climate Change Canada; National Aeronautics and Space Administration","keywords":"Ice nucleus; Mesoscale meteorology; Aerosol; Ice crystals; Atmospheric sciences; Convection; Particle (ecology); Nucleation; Climatology; Environmental science; Meteorology; Geology; Physics; Thermodynamics; Oceanography","score_opus":0.026229199742974323,"score_gpt":0.28690030944706674,"score_spread":0.2606711097040924,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2577369584","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":[0.9949034,0.0000072359235,0.00006405264,0.00295034,0.0000141103865,0.00034263474,0.0000017322154,0.0000026285418,0.0017138546],"genre_scores_gemma":[0.9997139,0.0000025532067,0.000024324969,0.00015568355,0.000027735921,0.000058834026,3.2476734e-7,0.0000051587394,0.000011457478],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9982084,0.0004115472,0.00020314084,0.00015512967,0.0007089762,0.00031279936],"domain_scores_gemma":[0.9983523,0.0011059737,0.000104180675,0.0003919633,0.000012297324,0.00003327775],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006587183,0.000070005364,0.00013733293,0.0000028948973,0.00020996807,0.000050178227,0.0005792518,0.000031458218,0.000029666939],"category_scores_gemma":[0.0005376143,0.000039734397,0.000042885884,0.00015764537,0.00069343485,0.00017554662,0.0001893609,0.000327056,0.000054611253],"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":[0.0003869435,0.0007970941,0.1466118,0.00006377895,0.00001875623,0.000017597968,0.016689293,0.0052369107,0.795477,0.02407925,0.0010424067,0.009579215],"study_design_scores_gemma":[0.0006418207,0.0003745209,0.86633873,0.00012836522,0.00000514418,6.3253765e-7,0.009804351,0.083384514,0.036316704,0.0027576305,0.000109531036,0.00013805227],"about_ca_topic_score_codex":0.003972473,"about_ca_topic_score_gemma":0.00020086323,"teacher_disagreement_score":0.7591603,"about_ca_system_score_codex":0.00008324052,"about_ca_system_score_gemma":0.0000068046234,"threshold_uncertainty_score":0.60052174},"labels":[],"label_agreement":null},{"id":"W2581428632","doi":"10.1109/jstars.2017.2650144","title":"Long Temporal Analysis of 3-km MODIS Aerosol Product Over East China","year":2017,"lang":"en","type":"article","venue":"IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":9,"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 Toronto","funders":"Natural Science Foundation of Jiangsu Province; National Natural Science Foundation of China","keywords":"AERONET; Aerosol; Environmental science; Moderate-resolution imaging spectroradiometer; Climatology; Correlation coefficient; Remote sensing; Deep blue; Atmospheric sciences; Meteorology; Satellite; Geography; Geology; Mathematics; Statistics","score_opus":0.018900508622860687,"score_gpt":0.23788992497861103,"score_spread":0.21898941635575034,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2581428632","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":[0.9906138,0.000033112134,0.007972024,0.0003234659,0.00011021153,0.000102714,0.0000034167692,0.000005195536,0.0008360457],"genre_scores_gemma":[0.96415603,0.00006191844,0.03542439,0.000036910336,0.000119533455,3.9662588e-8,0.0000024935068,0.000008644917,0.00019006322],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998813,0.0000232718,0.00047471636,0.00018057987,0.00032463795,0.00018383314],"domain_scores_gemma":[0.99894214,0.000015155298,0.0006249939,0.00028244444,0.00006490106,0.00007034106],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002817365,0.00012621742,0.00034672598,0.000019340936,0.00026535138,0.000066524786,0.0001589989,0.00006989489,0.000041495252],"category_scores_gemma":[0.00005977344,0.00010671209,0.000075517484,0.00056302384,0.00016960972,0.00015735414,0.000053180494,0.00025155747,4.6476922e-7],"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":[0.00007815259,0.00010160825,0.74624085,0.000025220534,0.00036892437,0.000032366508,0.0012169437,0.03299103,0.066571675,0.00004330087,0.00014364166,0.15218627],"study_design_scores_gemma":[0.00032394976,0.000028353581,0.939732,0.000033071665,0.00013906442,0.000010930091,0.0000363475,0.057352632,0.0019728728,0.0001290752,0.00012583178,0.00011588527],"about_ca_topic_score_codex":0.0008082874,"about_ca_topic_score_gemma":0.0017508344,"teacher_disagreement_score":0.19349113,"about_ca_system_score_codex":0.00004500474,"about_ca_system_score_gemma":0.000038567334,"threshold_uncertainty_score":0.43515927},"labels":[],"label_agreement":null},{"id":"W2588868939","doi":"10.1002/2016jd025771","title":"Aerosol and cloud microphysics covariability in the northeast Pacific boundary layer estimated with ship‐based and satellite remote sensing observations","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","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":"McGill University","funders":"Biological and Environmental Research; Basic Energy Sciences; Office of Science; Langley Research Center; National Aeronautics and Space Administration; U.S. Department of Energy","keywords":"Aerosol; Cloud condensation nuclei; Environmental science; Atmospheric sciences; Moderate-resolution imaging spectroradiometer; Satellite; Effective radius; Angstrom exponent; Meteorology; Cloud base; Liquid water path; Cloud computing; Physics","score_opus":0.059399645082593454,"score_gpt":0.31698283226874335,"score_spread":0.2575831871861499,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2588868939","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":[0.99514467,0.000106191634,0.0019618396,0.0019456509,0.000044857967,0.00024239154,0.00000432851,0.0000055555192,0.0005445231],"genre_scores_gemma":[0.98147154,0.000079552075,0.018111689,0.000093651885,0.00014726083,9.0458906e-7,0.0000010852202,0.000017648415,0.00007664214],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99764204,0.0003599831,0.0003268311,0.00029653136,0.00088464253,0.0004899898],"domain_scores_gemma":[0.99828315,0.0006112893,0.0002549693,0.00053443504,0.00012009089,0.0001960841],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014509953,0.00018050718,0.000297692,0.0000014744419,0.0010700922,0.0005029996,0.00044313484,0.00007141198,0.000034527064],"category_scores_gemma":[0.00037587577,0.000109520224,0.000059511884,0.00026254752,0.001648589,0.0003758431,0.00023853213,0.000809768,0.000010377565],"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":[0.0012358553,0.0005216366,0.89335907,0.00007489704,0.000063921325,0.00035024132,0.00210574,0.00051406294,0.013504623,0.00023685995,0.00052056694,0.087512515],"study_design_scores_gemma":[0.0008574783,0.0004996446,0.9721728,0.00012975025,0.000020153055,0.000032747997,0.0008103548,0.02119203,0.00013348648,0.0029763696,0.0010171105,0.00015808875],"about_ca_topic_score_codex":0.0021140664,"about_ca_topic_score_gemma":0.00082985696,"teacher_disagreement_score":0.08735443,"about_ca_system_score_codex":0.00010237951,"about_ca_system_score_gemma":0.0001264695,"threshold_uncertainty_score":0.82303923},"labels":[],"label_agreement":null},{"id":"W2597780925","doi":"10.1063/1.4975512","title":"Proper determination of direct solar radiation in NWP and climate models","year":2017,"lang":"en","type":"article","venue":"AIP conference proceedings","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"University of Victoria","funders":"","keywords":"Aerosol; Radiation; Radiation flux; Environmental science; Flux (metallurgy); Scattering; Meteorology; Physics; Atmospheric sciences; Computational physics; Optics; Materials science","score_opus":0.018752175943201246,"score_gpt":0.23827806074014338,"score_spread":0.21952588479694213,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2597780925","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":[0.9656471,0.000014828362,0.0009149561,0.00014889719,0.000021380503,0.00016089875,0.000001231207,0.00001163824,0.033079073],"genre_scores_gemma":[0.99828446,0.00018415764,0.0013342942,0.000025490559,0.000007651903,0.00001977392,5.477209e-7,0.0000064635183,0.00013713552],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999347,0.0000036788726,0.00014320367,0.00020780717,0.00013876281,0.00015956399],"domain_scores_gemma":[0.9996842,0.0000057001394,0.00016628497,0.00008517258,0.000019462585,0.00003913838],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020247736,0.00008350658,0.000120486744,0.000002222098,0.000133846,0.00008238126,0.000173533,0.00005365451,0.000080900805],"category_scores_gemma":[0.00004527671,0.00007208306,0.000013755298,0.00003581157,0.00017567238,0.00081798784,0.00015268389,0.000059868053,0.00000927007],"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":[0.000014227788,0.000027598677,0.90674937,0.000025281211,0.0000011926041,5.6519104e-7,0.0018274805,0.0000050629938,0.016114969,0.00054013456,0.000021379112,0.07467274],"study_design_scores_gemma":[0.00034410937,0.00010071418,0.72617245,0.000059041675,0.00000943963,0.0000022308368,0.00026437428,0.26666486,0.003510395,0.0025520406,0.0001477988,0.00017256924],"about_ca_topic_score_codex":0.0003319028,"about_ca_topic_score_gemma":0.000060601582,"teacher_disagreement_score":0.2666598,"about_ca_system_score_codex":0.00003546453,"about_ca_system_score_gemma":0.0000078874245,"threshold_uncertainty_score":0.29394618},"labels":[],"label_agreement":null},{"id":"W2604681542","doi":"10.5194/acp-17-12097-2017","title":"Classifying aerosol type using in situ surface spectral aerosol optical properties","year":2017,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":142,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Horizon 2020 Framework Programme; National Key Research and Development Program of China; Environment and Climate Change Canada; Environmental Protection Administration, Executive Yuan, R.O.C. Taiwan; Ministerio de Ciencia y Tecnología; National Natural Science Foundation of China; Bulgarian Academy of Sciences; European Commission; U.S. Department of Energy","keywords":"Aerosol; Angstrom exponent; Single-scattering albedo; Environmental science; Atmospheric sciences; Radiative forcing; Meteorology; Remote sensing; Physics; Geography","score_opus":0.02451088346464037,"score_gpt":0.24219043447429545,"score_spread":0.21767955100965508,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2604681542","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":[0.97779167,0.00009391401,0.00035666057,0.000068741036,0.00006523906,0.00010560111,7.4102064e-7,0.000028450673,0.021489],"genre_scores_gemma":[0.9833917,0.000053400516,0.0138229085,0.000043616714,0.000136409,0.0000031101479,0.0000013647732,0.000024497393,0.0025229785],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99877846,0.000012289176,0.00019242577,0.00041247616,0.00020606784,0.00039828487],"domain_scores_gemma":[0.9992898,0.0000151540835,0.00010701751,0.00044918427,0.000008943559,0.00012986631],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008066907,0.0002350943,0.00024210612,8.075699e-9,0.0004210189,0.0001473994,0.00028106308,0.000118489945,0.0006231926],"category_scores_gemma":[0.000022680659,0.00021365537,0.000050606348,0.00008904523,0.0004989283,0.00030184563,0.00025719797,0.00024837078,0.000050081628],"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":[0.00005225808,0.00011976232,0.09875758,0.000050127208,0.0000148851805,0.000022811148,0.0003138609,0.006324702,0.8806646,0.00001532331,0.00007020001,0.0135938795],"study_design_scores_gemma":[0.0018237851,0.0001310496,0.0714544,0.00022601639,0.00008908013,0.000060890172,0.0006886922,0.19723448,0.72539866,0.0005640256,0.000649489,0.0016794571],"about_ca_topic_score_codex":0.00038097214,"about_ca_topic_score_gemma":0.000023901977,"teacher_disagreement_score":0.19090977,"about_ca_system_score_codex":0.00012000353,"about_ca_system_score_gemma":0.000027938384,"threshold_uncertainty_score":0.8712613},"labels":[],"label_agreement":null},{"id":"W2604878345","doi":"10.5194/amt-2017-76","title":"Depolarization measurements using the CANDAC Rayleigh-Mie-Raman Lidar at Eureka, Canada","year":2017,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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; Western University; Dalhousie University","funders":"","keywords":"Lidar; Depolarization ratio; Remote sensing; Environmental science; Rayleigh scattering; Calibration; Ice cloud; Arctic; Mie scattering; Optics; Meteorology; Physics; Scattering; Light scattering; Geology; Radiative transfer","score_opus":0.031112830540225407,"score_gpt":0.23676972415517578,"score_spread":0.20565689361495038,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2604878345","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":[0.9600014,0.000022426993,0.0018465641,0.00052842114,0.00026133866,0.00014434717,0.000002279485,0.00001327281,0.03717992],"genre_scores_gemma":[0.99378973,0.0000032800622,0.0008203185,0.0006259869,0.00004777641,0.0000030312663,0.0000018536768,0.000012364369,0.0046956353],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988916,0.00003323134,0.00012813354,0.00020784374,0.0004914922,0.0002477286],"domain_scores_gemma":[0.999268,0.000009526959,0.00012664654,0.00049529545,0.000008652518,0.00009186508],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00015999813,0.00011421673,0.00008457918,2.9238927e-7,0.0016887479,0.000099646466,0.00043139787,0.000040428018,0.002418385],"category_scores_gemma":[0.000025191528,0.00007393887,0.000026171709,0.000040268682,0.00016327004,0.00014139958,0.00031123418,0.00007060175,0.000040592313],"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":[0.0000046987334,0.000009649323,0.98162115,0.0000013445557,0.000010136259,0.0000036422907,0.0000630522,0.00077228784,0.013148255,0.000025750618,0.003379309,0.0009607454],"study_design_scores_gemma":[0.00032238028,0.000018014325,0.9627607,0.00000802224,0.000032514796,0.000007809997,0.00013252214,0.0041943532,0.011908387,0.000055866843,0.020291127,0.00026830166],"about_ca_topic_score_codex":0.88834643,"about_ca_topic_score_gemma":0.9370351,"teacher_disagreement_score":0.04868864,"about_ca_system_score_codex":0.0006453419,"about_ca_system_score_gemma":0.00008498284,"threshold_uncertainty_score":0.9996109},"labels":[],"label_agreement":null},{"id":"W2605577717","doi":"10.5194/amt-10-3215-2017","title":"Combined retrieval of Arctic liquid water cloud and surface snow properties using airborne spectral solar remote sensing","year":2017,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":14,"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":"Deutsche Forschungsgemeinschaft","keywords":"Snow; Remote sensing; Albedo (alchemy); Environmental science; Effective radius; Solar zenith angle; Cloud computing; Materials science; Meteorology; Geology; Computer science; Physics; Astronomy","score_opus":0.033417581274880946,"score_gpt":0.232869149668312,"score_spread":0.19945156839343103,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2605577717","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":[0.97968936,0.00012645652,0.017925693,0.0003088792,0.00016048572,0.00058048236,7.314819e-7,0.00017019238,0.0010376963],"genre_scores_gemma":[0.9032828,0.00009738451,0.096253425,0.00008040203,0.00006533731,6.673305e-7,7.392547e-7,0.000046890636,0.00017235788],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99747247,0.00011247574,0.00047859864,0.00052357395,0.0008630113,0.00054984604],"domain_scores_gemma":[0.9985829,0.000011477688,0.000324413,0.00084906834,0.00009126011,0.00014088412],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00120167,0.00034752468,0.0004523817,6.0461673e-7,0.0006167399,0.00010460472,0.00041600113,0.00015069314,0.00020938626],"category_scores_gemma":[0.00015349468,0.00025853323,0.000102034384,0.0000856422,0.0007062501,0.00032563964,0.0004831699,0.0002232107,0.000012282523],"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":[0.00045061408,0.00007053111,0.007911391,0.00007704466,0.000059814018,0.000017298526,0.0004909382,0.00012507585,0.9825106,0.000009385844,0.00009703958,0.008180269],"study_design_scores_gemma":[0.00040129313,0.0007075437,0.005430261,0.00033282436,0.00008791432,0.000020298537,0.00010334136,0.010332255,0.9812336,0.00039551358,0.00048703654,0.00046810668],"about_ca_topic_score_codex":0.00358877,"about_ca_topic_score_gemma":0.000069252324,"teacher_disagreement_score":0.07832773,"about_ca_system_score_codex":0.00036765242,"about_ca_system_score_gemma":0.000031860825,"threshold_uncertainty_score":0.9999867},"labels":[],"label_agreement":null},{"id":"W2608585047","doi":"10.15407/rpra20.02.109","title":"SEVEN-DAY VARIATIONS IN THE ATMOSPHERIC AEROSOLS","year":2015,"lang":"en","type":"article","venue":"Radio physics and radio astronomy","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"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":"AERONET; Precipitable water; Angstrom exponent; Aerosol; Physics; Atmospheric sciences; Astron; Angstrom; Sun photometer; Atmosphere (unit); Meteorology; Climatology; Water vapor; Astrophysics; Chemistry; Geology","score_opus":0.01077909773626738,"score_gpt":0.210147832918372,"score_spread":0.19936873518210463,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2608585047","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":[0.90814316,0.00017881797,0.075651176,0.0007046991,0.00019591225,0.00040741346,0.000005300471,0.00003147569,0.01468205],"genre_scores_gemma":[0.98788375,0.000008537097,0.011248923,0.00015176155,0.00022063359,0.000051999436,0.0000065242984,0.000014924849,0.00041297392],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989639,0.000088389446,0.00017045064,0.00026578404,0.00021298171,0.00029847265],"domain_scores_gemma":[0.999477,0.00004825225,0.00007054625,0.00027241668,0.0000048254674,0.00012690999],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032234582,0.00016152475,0.00016746446,3.8487605e-7,0.0001339412,0.000063875086,0.00025335018,0.000042185515,0.00011740298],"category_scores_gemma":[0.0000060750795,0.00011705936,0.000049915274,0.00025655236,0.00016292225,0.00021900216,0.00007501336,0.00015458473,0.000090252965],"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":[0.000023894303,0.0005250635,0.7956203,0.0000068066247,0.00006278254,0.0000150472315,0.012186143,0.0309469,0.0004482271,0.0108209215,0.021445075,0.12789883],"study_design_scores_gemma":[0.002940921,0.00037028198,0.7231627,0.000024158358,0.00009098625,0.00004414035,0.0033989768,0.035968497,0.00009491868,0.0074244384,0.22546554,0.00101443],"about_ca_topic_score_codex":0.00027326253,"about_ca_topic_score_gemma":0.00002037658,"teacher_disagreement_score":0.20402046,"about_ca_system_score_codex":0.0001214596,"about_ca_system_score_gemma":0.000034084875,"threshold_uncertainty_score":0.47735423},"labels":[],"label_agreement":null},{"id":"W2610284820","doi":"10.1016/j.atmosres.2017.04.037","title":"Simulation of a severe convective storm using a numerical model with explicitly incorporated aerosols","year":2017,"lang":"en","type":"article","venue":"Atmospheric Research","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":32,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Science and Engineering Research Board","keywords":"Weather Research and Forecasting Model; Mesoscale meteorology; Meteorology; Environmental science; Precipitation; Storm; Climatology; Numerical weather prediction; Squall line; Weather radar; Atmospheric sciences; Radar; Geology; Geography; Computer science","score_opus":0.09182950854934596,"score_gpt":0.36416107049408625,"score_spread":0.2723315619447403,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2610284820","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":[0.8949222,0.000021241138,0.099583365,0.000063632826,0.000024015379,0.00045808044,0.0000030539793,0.000025693667,0.004898695],"genre_scores_gemma":[0.95741874,0.0000061351343,0.041338496,0.000027327436,0.000028414202,0.000034859422,0.0000016781713,0.000038410108,0.0011059523],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99748653,0.00012592439,0.00027346177,0.0005003244,0.001071065,0.0005426643],"domain_scores_gemma":[0.9983567,0.00016128604,0.0002962941,0.0008485788,0.00014707047,0.00019008596],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00056509976,0.00019690755,0.00030822106,6.661258e-7,0.00074915506,0.00008701759,0.0006423195,0.00012431663,0.0006979428],"category_scores_gemma":[0.0001974511,0.00015605165,0.000056831457,0.00044255226,0.00089047983,0.0005231645,0.00052994065,0.0003468069,0.00008116183],"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":[0.00021187148,0.00010889999,0.13928257,0.000008557826,0.000022572707,0.0000128324355,0.0005378808,0.85401833,0.0033226428,0.000047358375,0.00009339101,0.0023331088],"study_design_scores_gemma":[0.0005840862,0.0003129205,0.04679936,0.000028635495,0.000010866091,0.000004431323,0.0003485963,0.95082664,0.0003363709,0.0004933858,0.00005035613,0.00020434642],"about_ca_topic_score_codex":0.0042790486,"about_ca_topic_score_gemma":0.00013749006,"teacher_disagreement_score":0.09680834,"about_ca_system_score_codex":0.00036118057,"about_ca_system_score_gemma":0.00013950905,"threshold_uncertainty_score":0.7641984},"labels":[],"label_agreement":null},{"id":"W2610384203","doi":"10.5194/acp-17-12725-2017","title":"Impacts of solar-absorbing aerosol layers on the transition of stratocumulus to trade cumulus clouds","year":2017,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Brookhaven National Laboratory; Ames Research Center; National Aeronautics and Space Administration; U.S. Department of Energy","keywords":"Liquid water path; Atmospheric sciences; Aerosol; Longwave; Breakup; Marine stratocumulus; Environmental science; Liquid water content; Cloud forcing; Cloud albedo; Shortwave; Boundary layer; Drizzle; Entrainment (biomusicology); Atmosphere (unit); Cloud height; Water vapor; Meteorology; Precipitation; Cloud cover; Radiative transfer; Radiative forcing; Cloud computing; Geology; Physics; Mechanics","score_opus":0.01077684298790899,"score_gpt":0.23220478038894574,"score_spread":0.22142793740103675,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2610384203","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":[0.9911547,0.000018927038,0.001600192,0.00044110743,0.0000313376,0.00015663705,0.000011446811,0.000011335266,0.0065743565],"genre_scores_gemma":[0.99777424,0.00002784431,0.0017802755,0.00016967871,0.0000701047,0.000009252901,0.0000019694298,0.000015601394,0.000151008],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9990394,0.000016804433,0.00021247838,0.00024841807,0.00025313688,0.00022972458],"domain_scores_gemma":[0.99909616,0.000050068284,0.0001984021,0.0005283169,0.0000070964415,0.000119931974],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012184042,0.0001827971,0.00022520612,1.3326823e-8,0.00028539525,0.000034852284,0.0003344511,0.000077213735,0.0005884833],"category_scores_gemma":[0.0000215375,0.000140028,0.00009312066,0.000086577296,0.0003359333,0.00011819464,0.00007067157,0.00014289853,0.000009329719],"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":[0.0002200594,0.00035744577,0.013160859,0.00015826403,0.00008405872,0.0000055032797,0.0039227437,0.0110619115,0.8592673,0.00018269675,0.00069501164,0.11088417],"study_design_scores_gemma":[0.0009775035,0.00037042686,0.044909105,0.00017683276,0.00009380899,0.0000075766734,0.001090294,0.016936721,0.9333523,0.0010436653,0.00048134662,0.0005604488],"about_ca_topic_score_codex":0.00041290594,"about_ca_topic_score_gemma":0.000008269834,"teacher_disagreement_score":0.11032372,"about_ca_system_score_codex":0.000035726345,"about_ca_system_score_gemma":0.000016040758,"threshold_uncertainty_score":0.6443479},"labels":[],"label_agreement":null},{"id":"W2612386074","doi":"10.5194/acp-17-11227-2017","title":"Comparative measurements of ambient atmospheric concentrations of ice nucleating particles using multiple immersion freezing methods and a continuous flow diffusion chamber","year":2017,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":112,"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 British Columbia","funders":"Biological and Environmental Research; Division of Atmospheric and Geospace Sciences; University of California, San Diego; Natural Sciences and Engineering Research Council of Canada; National Park Service; University of California, Davis; U.S. Department of Energy; Japan Society for the Promotion of Science; National Institute of Polar Research; National Science Foundation; Nature Conservancy; Office of Science","keywords":"Aerosol; Ice nucleus; Immersion (mathematics); Ambient pressure; Supercooling; Chemistry; Environmental science; Meteorology; Analytical Chemistry (journal); Atmospheric sciences; Nucleation; Chromatography; Mathematics","score_opus":0.034774467862201314,"score_gpt":0.2942754250865002,"score_spread":0.2595009572242989,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2612386074","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":[0.9746726,0.00016235132,0.023971584,0.000011758216,0.00003418349,0.00015424029,0.0000047948433,0.000010249134,0.0009782107],"genre_scores_gemma":[0.78623134,0.00002838835,0.21360835,0.000011196438,0.000024230741,0.000004219611,0.0000022160334,0.000010682895,0.00007937316],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9988944,0.000052352825,0.00030406966,0.00030891664,0.00022167656,0.00021857383],"domain_scores_gemma":[0.99899536,0.000093870265,0.00045746274,0.00031518764,0.00003424942,0.00010385271],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018032907,0.00019207608,0.00037054293,1.4754684e-8,0.00047028984,0.00003810758,0.0001281563,0.000067125344,0.00030983455],"category_scores_gemma":[0.00004526442,0.00018008468,0.000060101615,0.00008275666,0.00055164937,0.00020562246,0.00022658672,0.000095068695,0.0000014090178],"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":[0.00003074467,0.000113379894,0.21900024,0.000045952922,0.00003382711,6.9953825e-7,0.0014357766,0.0036983239,0.7160227,0.0000028819395,0.000008016957,0.05960748],"study_design_scores_gemma":[0.0007536084,0.000044403212,0.038303316,0.00008914865,0.000077706005,0.0000031333013,0.0011931382,0.65819454,0.3010196,0.000059463186,0.000051362975,0.00021058202],"about_ca_topic_score_codex":0.00088446843,"about_ca_topic_score_gemma":0.000008076071,"teacher_disagreement_score":0.6544962,"about_ca_system_score_codex":0.000045465342,"about_ca_system_score_gemma":0.000012973004,"threshold_uncertainty_score":0.73436403},"labels":[],"label_agreement":null},{"id":"W2613083350","doi":"","title":"Arctic Aerosol-Cloud Interactions during ASCOS","year":2015,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Aerosol; Cloud computing; Arctic; Meteorology; The arctic; Environmental science; Climatology; Geology; Geography; Computer science; Oceanography","score_opus":0.019057323960382004,"score_gpt":0.24145559715558043,"score_spread":0.22239827319519842,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2613083350","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":[0.9074167,0.000028058204,0.000027962617,0.00027807377,0.00085388054,0.00012838634,0.0000011466379,0.00013122226,0.09113459],"genre_scores_gemma":[0.9929237,0.000006577564,0.0019721026,0.0001932386,0.0002661149,0.000018625624,0.0000034739994,0.000031104806,0.004585096],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99835354,0.000041940082,0.00034466985,0.00040053565,0.00039770777,0.0004616179],"domain_scores_gemma":[0.999031,0.00007720875,0.0001816091,0.0003430975,0.000020506675,0.00034655185],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003277977,0.00020129787,0.00016470382,0.0000023470525,0.00021586177,0.000075197204,0.0002726797,0.00007159662,0.0001463857],"category_scores_gemma":[0.00033605457,0.0001913975,0.000076576056,0.00017453585,0.0001115109,0.00028275544,0.00021777753,0.00029279618,0.0027794873],"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":[0.00006394222,0.00031744278,0.9113499,0.000033895194,0.000042267973,0.00013297431,0.002261363,0.059026636,0.015950594,0.000021092093,0.009367616,0.0014322596],"study_design_scores_gemma":[0.0015772693,0.00016664904,0.9636274,0.00025115328,0.00007383535,0.0002150185,0.002230281,0.0010588606,0.009593833,0.00044427384,0.019687459,0.0010739556],"about_ca_topic_score_codex":0.013871974,"about_ca_topic_score_gemma":0.0041400134,"teacher_disagreement_score":0.0865495,"about_ca_system_score_codex":0.00029036528,"about_ca_system_score_gemma":0.000020243753,"threshold_uncertainty_score":0.997997},"labels":[],"label_agreement":null},{"id":"W2614089147","doi":"","title":"First validation of the surface solar irradiance data set produced by the MACC/MACC-II projects","year":2014,"lang":"en","type":"preprint","venue":"HAL (Le Centre pour la Communication Scientifique Directe)","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"Impact","funders":"","keywords":"Irradiance; Environmental science; Solar irradiance; Atmospheric sciences; Shortwave; Downwelling; Atmosphere (unit); Radiative transfer; Atmospheric radiative transfer codes; Meteorology; Remote sensing; Geography; Upwelling; Geology; Physics","score_opus":0.021422161228677346,"score_gpt":0.22699031290831884,"score_spread":0.2055681516796415,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2614089147","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":[0.95079154,0.00052141835,0.0140573,0.023821011,0.0003536955,0.0013973523,0.00028180648,0.00009835639,0.008677526],"genre_scores_gemma":[0.9849482,0.00027821038,0.0053524687,0.00015490393,0.000021850483,0.000045690747,0.00040636706,0.00004199855,0.008750304],"study_design_codex":"not_applicable","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99454707,0.0029030913,0.00049645506,0.0009852103,0.0006870205,0.00038118183],"domain_scores_gemma":[0.99257725,0.0005286605,0.0008315155,0.005748063,0.00021790454,0.00009657358],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0056692515,0.00032136307,0.0003005458,0.0000031862244,0.0009338923,0.00018815539,0.004605181,0.00020854553,0.00038082176],"category_scores_gemma":[0.0010670051,0.00022453516,0.00012297442,0.0004142773,0.00059730024,0.00018366234,0.0077345185,0.00059377996,0.000054957847],"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":[0.000107379055,0.0037451573,0.29698792,0.0012601403,0.0005499637,0.0000030610638,0.08111771,0.044823322,0.07108177,0.008686353,0.42205003,0.0695872],"study_design_scores_gemma":[0.0013991268,0.0000039041647,0.06710773,0.0029247722,0.00032098696,0.0000182075,0.00061813206,0.30689645,0.3802146,0.0020255132,0.23649798,0.001972586],"about_ca_topic_score_codex":0.0048030796,"about_ca_topic_score_gemma":0.001839913,"teacher_disagreement_score":0.3091328,"about_ca_system_score_codex":0.00014088087,"about_ca_system_score_gemma":0.00012603967,"threshold_uncertainty_score":0.96405244},"labels":[],"label_agreement":null},{"id":"W2624024965","doi":"10.1002/2017jd026641","title":"Influences of drizzle on stratocumulus cloudiness and organization","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"U.S. Department of Energy","keywords":"Drizzle; Marine stratocumulus; Atmospheric sciences; Environmental science; Boundary layer; Mesoscale meteorology; Aerosol; Precipitation; Evaporation; Cloud cover; Meteorology; Cloud computing; Geology; Geography; Thermodynamics","score_opus":0.030809037248233445,"score_gpt":0.33284006538889893,"score_spread":0.3020310281406655,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2624024965","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":[0.99689955,0.00003755484,0.00007980085,0.00041579414,0.00006350365,0.00008056496,0.0000011158937,0.0000032340151,0.0024188734],"genre_scores_gemma":[0.99859554,0.00008595632,0.00070317875,0.000020916943,0.00014035896,0.0000010317166,1.4901542e-7,0.000011380632,0.00044147857],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982662,0.0000892713,0.00028081585,0.00015535254,0.0009550216,0.00025329748],"domain_scores_gemma":[0.99882126,0.00019285022,0.00034695223,0.0002903914,0.00016818193,0.00018034576],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004915959,0.000099123434,0.00023153392,0.0000011138421,0.00040414897,0.000119623655,0.00057074626,0.000058133108,0.0006128554],"category_scores_gemma":[0.00096571073,0.000069785696,0.000049435974,0.00018426425,0.00088744157,0.000368036,0.000304612,0.00032257466,0.00004919407],"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":[0.00027955472,0.0004825801,0.8954576,0.000029078885,0.000058419842,0.00006064122,0.0004287233,0.0007472287,0.04329623,0.0022261876,0.0030384012,0.053895306],"study_design_scores_gemma":[0.00037400905,0.00074271153,0.987393,0.000056746827,0.00000835702,0.000005875493,0.00020309526,0.00029709798,0.0062514073,0.0040435335,0.0005444077,0.00007973127],"about_ca_topic_score_codex":0.00073497137,"about_ca_topic_score_gemma":0.000044764492,"teacher_disagreement_score":0.09193538,"about_ca_system_score_codex":0.000051964103,"about_ca_system_score_gemma":0.000052361072,"threshold_uncertainty_score":0.67103374},"labels":[],"label_agreement":null},{"id":"W262511779","doi":"10.1023/a:1002641728075","title":"Numerical Study Of The Impact Of Coherent Structures On Vertical Transfers In The Atmospheric Boundary Layer","year":2000,"lang":"en","type":"article","venue":"Boundary-Layer Meteorology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":28,"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":"Centre National de la Recherche Scientifique; Institut national de la recherche scientifique","keywords":"Turbulence; Isotropy; Planetary boundary layer; Scale (ratio); Radar; Meteorology; Boundary layer; Mechanics; Physics; Statistical physics; Atmospheric sciences; Environmental science; Geology; Optics; Aerospace engineering; Engineering","score_opus":0.013965400281627112,"score_gpt":0.2693533586590721,"score_spread":0.255387958377445,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W262511779","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":[0.9946803,0.000072444105,0.000038554863,0.00027279768,0.00012447455,0.00069731846,0.000007792494,0.000013591481,0.0040927185],"genre_scores_gemma":[0.99925894,0.000008484244,0.00008308076,0.00047086467,0.000029358487,0.00004106506,0.0000014164015,0.000024169995,0.00008263876],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9972772,0.00070823124,0.0005434801,0.00043052476,0.0005403111,0.00050022925],"domain_scores_gemma":[0.9989469,0.00019199717,0.00007826405,0.0006893337,0.000009609468,0.00008390193],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00036921527,0.00030004868,0.0004880146,0.000001910804,0.00021590701,0.000027706297,0.00083704974,0.00015666554,0.010166562],"category_scores_gemma":[0.0000306839,0.00015581862,0.00026047524,0.0005334465,0.00096330297,0.00007523424,0.000075296535,0.00044752794,0.00004728834],"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":[0.0019615723,0.0032449996,0.8826178,0.000011864875,0.00024824118,0.00003764477,0.009947903,0.06441506,0.0072101913,0.00023725786,0.0018842249,0.028183265],"study_design_scores_gemma":[0.0013099256,0.0037153687,0.9906102,0.000004610516,0.000057438825,0.00002167218,0.0004525834,0.0012315039,0.00030614762,0.0011459817,0.0009685709,0.0001760167],"about_ca_topic_score_codex":0.005255554,"about_ca_topic_score_gemma":0.00046780598,"teacher_disagreement_score":0.1079924,"about_ca_system_score_codex":0.00015928099,"about_ca_system_score_gemma":0.00008499718,"threshold_uncertainty_score":0.9907383},"labels":[],"label_agreement":null},{"id":"W2714878629","doi":"10.5194/acp-2017-215","title":"The optical, physical properties and direct radiative forcing of urban columnar aerosols in Yangtze River Delta, China","year":2017,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"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 Toronto","funders":"National Natural Science Foundation of China; European Commission","keywords":"Aerosol; Single-scattering albedo; Sun photometer; Angstrom exponent; Environmental science; Radiative forcing; Radiative transfer; Atmospheric sciences; Scattering; Albedo (alchemy); Meteorology; Physics; Optics","score_opus":0.01236670778566763,"score_gpt":0.21843807529212583,"score_spread":0.20607136750645821,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2714878629","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":[0.97071606,0.00006434752,0.000081250015,0.0002322817,0.000025088842,0.00019546763,0.0000011999006,0.000008852383,0.028675472],"genre_scores_gemma":[0.99776095,0.000040857656,0.00057508185,0.000028539365,0.000023183768,0.000017639768,1.6441133e-7,0.000007658848,0.0015459073],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992995,0.000025057083,0.000120841025,0.0001875052,0.0001604286,0.00020663533],"domain_scores_gemma":[0.9995454,0.000047707406,0.00008048151,0.00026790227,0.0000037862367,0.000054715005],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013566446,0.00009744379,0.00015831426,4.2521916e-7,0.00043049935,0.000066953595,0.00025077764,0.000030284718,0.00005749502],"category_scores_gemma":[0.00007272043,0.000056143563,0.000035153043,0.000034593773,0.0011316024,0.00020306496,0.00027208583,0.000079953126,0.000014824241],"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":[0.00009639493,0.00020782954,0.9577312,0.000014522805,0.000030050733,0.00000578228,0.008228675,0.00066667836,0.0111750495,0.0020823278,0.0015582235,0.018203286],"study_design_scores_gemma":[0.0003609784,0.000139393,0.974583,0.000021370957,0.000010141993,8.424431e-7,0.00042792983,0.016815716,0.006692785,0.00035576266,0.00044466794,0.00014735543],"about_ca_topic_score_codex":0.0025251294,"about_ca_topic_score_gemma":0.00060299254,"teacher_disagreement_score":0.027129566,"about_ca_system_score_codex":0.000038055496,"about_ca_system_score_gemma":0.000007022336,"threshold_uncertainty_score":0.41694367},"labels":[],"label_agreement":null},{"id":"W2729648178","doi":"10.1002/qj.3105","title":"Exploring the convective grey zone with regional simulations of a cold air outbreak","year":2017,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","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":"Parametrization (atmospheric modeling); Convection; Meteorology; Environmental science; Radiative transfer; Climatology; Atmospheric sciences; Geology; Physics","score_opus":0.03852774145312575,"score_gpt":0.2363907428664506,"score_spread":0.19786300141332486,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2729648178","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":[0.99358577,0.000022550024,0.0028605226,0.0028121078,0.00014365069,0.00013674397,0.000003552443,0.000005625306,0.00042947807],"genre_scores_gemma":[0.997334,0.00000465182,0.0019013145,0.00036453444,0.000101647194,0.0000061847613,9.772291e-8,0.0000075357743,0.00028004465],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99871,0.0001321025,0.00030907147,0.00014313217,0.0004938643,0.00021186366],"domain_scores_gemma":[0.9985202,0.00022191099,0.0007486364,0.00037093222,0.000054179643,0.00008413718],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048298077,0.00013561716,0.00025291505,6.2574446e-7,0.00075242016,0.00003882326,0.0008329063,0.00006171935,0.00016783198],"category_scores_gemma":[0.000050741364,0.00005704183,0.00035949433,0.00007147668,0.0010215051,0.00022531596,0.00011338967,0.00036818598,0.0000055313008],"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":[0.0014400998,0.0013794114,0.7406943,0.000028859502,0.0014822112,0.000041141808,0.023302838,0.18088725,0.010090646,0.0035699622,0.0067655044,0.030317768],"study_design_scores_gemma":[0.00094204093,0.0020449522,0.98661333,0.00003216533,0.00013617455,0.000024528616,0.0020697261,0.004820816,0.00038087319,0.00092275365,0.0018566928,0.00015592999],"about_ca_topic_score_codex":0.00015751459,"about_ca_topic_score_gemma":0.000040045983,"teacher_disagreement_score":0.24591905,"about_ca_system_score_codex":0.000078602774,"about_ca_system_score_gemma":0.000019459514,"threshold_uncertainty_score":0.57870835},"labels":[],"label_agreement":null},{"id":"W2735659196","doi":"10.1088/1742-6596/869/1/012081","title":"Microphysical Characteristics of Atmospheric Particulate Matter from NASA’s MODIS, MISR, and AERONET Observations","year":2017,"lang":"en","type":"article","venue":"Journal of Physics Conference Series","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"AERONET; Angstrom exponent; Environmental science; Remote sensing; Aerosol; Radiometer; Sun photometer; Satellite; Particulates; Single-scattering albedo; Meteorology; Albedo (alchemy); Atmospheric sciences; Geology; Physics","score_opus":0.020425814183768633,"score_gpt":0.22403917249008343,"score_spread":0.2036133583063148,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2735659196","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":[0.99466866,0.000019162742,0.0041729985,0.00058812817,0.00013420789,0.000049854698,0.000023863364,0.0000031669372,0.00033997255],"genre_scores_gemma":[0.99227136,0.00008745625,0.007157072,0.000079225974,0.00013140887,0.0000011999923,0.0000032991716,0.000011349409,0.0002576376],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991,0.000025159077,0.0003510948,0.00013804702,0.00022737258,0.0001583163],"domain_scores_gemma":[0.99877,0.000025184861,0.0007517537,0.00029647377,0.000060685245,0.0000958987],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000565184,0.00014397928,0.00033308953,3.397441e-7,0.00019096052,0.00012152293,0.00031905164,0.000047444297,0.0004934752],"category_scores_gemma":[0.00001688513,0.00011760331,0.00007585147,0.000033666416,0.0005599405,0.00067056733,0.00018464582,0.00014408541,0.00002952657],"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":[0.00009519271,0.00017838033,0.8023728,0.000017733266,0.0000807084,0.000013210867,0.0011941919,0.00010289827,0.16904725,0.0012537789,0.0006983698,0.024945464],"study_design_scores_gemma":[0.00024376788,0.00011084036,0.97567755,0.000045445693,0.000054466575,0.000004998247,0.00014204594,0.00033710434,0.01855437,0.004269216,0.00041925875,0.0001409281],"about_ca_topic_score_codex":0.00023138523,"about_ca_topic_score_gemma":0.000016498241,"teacher_disagreement_score":0.17330474,"about_ca_system_score_codex":0.000022878927,"about_ca_system_score_gemma":0.000029621888,"threshold_uncertainty_score":0.54032075},"labels":[],"label_agreement":null},{"id":"W2738841874","doi":"10.1175/ei-d-16-0035.1","title":"Trans-Atlantic Connections between North African Dust Flux and Tree Growth in the Florida Keys, United States","year":2017,"lang":"en","type":"article","venue":"Earth Interactions","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"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 de Montréal","funders":"National Renewable Energy Laboratory","keywords":"Mineral dust; Aerosol; Environmental science; Atmospheric sciences; Photosynthetically active radiation; Context (archaeology); Subtropics; Angstrom exponent; Atmosphere (unit); Geology; Meteorology; Geography; Chemistry; Ecology","score_opus":0.01910868441193593,"score_gpt":0.24405269801016036,"score_spread":0.2249440135982244,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2738841874","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":[0.98512155,0.000004818859,0.0004512318,0.0037545343,0.00014980034,0.00014990874,0.00002387318,0.000024246207,0.010320047],"genre_scores_gemma":[0.99799466,0.000039130326,0.00015687628,0.00015269351,0.000087232955,0.000023875851,0.000042888514,0.000009218685,0.001493445],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992361,0.00005913813,0.00016126812,0.00020152697,0.00013354914,0.00020841182],"domain_scores_gemma":[0.99941254,0.00014780497,0.000079240264,0.00027752787,0.0000086614045,0.00007424203],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0000771452,0.00011566565,0.000113670634,0.0000063216967,0.0007904653,0.0001451882,0.00025684628,0.00002832005,0.0010511449],"category_scores_gemma":[0.000048813872,0.00008568814,0.000040089482,0.00019474191,0.00024058924,0.00029393993,0.00005587704,0.00025437665,0.00010195426],"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":[0.000007166276,0.000040556264,0.9931014,0.000002266111,0.00001599081,0.000007169925,0.002267202,0.0002057343,0.000053463446,0.000056441622,0.0018887932,0.0023537776],"study_design_scores_gemma":[0.00019310784,0.00005113683,0.9452499,0.000008532554,0.000022881446,0.000010051053,0.0012841449,0.0007992642,0.000033069122,0.00010853528,0.052133147,0.000106207386],"about_ca_topic_score_codex":0.011968109,"about_ca_topic_score_gemma":0.04089206,"teacher_disagreement_score":0.050244354,"about_ca_system_score_codex":0.000025716123,"about_ca_system_score_gemma":0.0000062310505,"threshold_uncertainty_score":0.999862},"labels":[],"label_agreement":null},{"id":"W2740436841","doi":"","title":"On the improvement of MACC aerosol spatial resolution for irradiance estimation in the United Arab Emirates","year":2013,"lang":"en","type":"preprint","venue":"HAL (Le Centre pour la Communication Scientifique Directe)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Impact","funders":"","keywords":"Downscaling; AERONET; Irradiance; Environmental science; Aerosol; Remote sensing; Image resolution; Spatial variability; Satellite; Meteorology; Atmospheric sciences; Geography; Geology; Computer science; Mathematics; Statistics","score_opus":0.014285723107919536,"score_gpt":0.22391211654205606,"score_spread":0.20962639343413653,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2740436841","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":[0.83585805,0.0000803909,0.14541192,0.010322533,0.00012014581,0.0017040638,0.000038509643,0.000035238754,0.006429128],"genre_scores_gemma":[0.9878412,0.00010745645,0.009991109,0.0003325401,0.000010588531,0.0005220239,0.00020334218,0.000021123817,0.0009706351],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9969899,0.00140101,0.00046486213,0.00045492043,0.00041644907,0.00027282853],"domain_scores_gemma":[0.9964725,0.0014124898,0.0005373678,0.0013406557,0.00018632929,0.000050678078],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0028241184,0.00023227664,0.00020667377,0.000010622789,0.00028176972,0.0001401383,0.0011546033,0.00016747322,0.00036037745],"category_scores_gemma":[0.00079214276,0.00016030374,0.00011738668,0.0003338915,0.00032713584,0.00007490175,0.000505246,0.00039223718,0.000039097675],"study_design_candidate":"simulation_or_modeling","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":[0.0003233388,0.005135115,0.018680565,0.00074377673,0.00024709708,0.0000044446083,0.071193546,0.17009602,0.05252477,0.2947735,0.03865893,0.34761888],"study_design_scores_gemma":[0.00086014037,0.0000074255145,0.030876009,0.0011503287,0.00005113199,0.0000016738187,0.00050383975,0.90544987,0.036310956,0.021981835,0.0022690012,0.00053777057],"about_ca_topic_score_codex":0.011462926,"about_ca_topic_score_gemma":0.0025979076,"teacher_disagreement_score":0.7353539,"about_ca_system_score_codex":0.00018128066,"about_ca_system_score_gemma":0.00004901838,"threshold_uncertainty_score":0.9951198},"labels":[],"label_agreement":null},{"id":"W2744893833","doi":"10.1175/amsmonographs-d-16-0007.1","title":"Processing of Ice Cloud In Situ Data Collected by Bulk Water, Scattering, and Imaging Probes: Fundamentals, Uncertainties, and Efforts toward Consistency","year":2017,"lang":"en","type":"article","venue":"Meteorological Monographs","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":135,"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":"U.S. Department of Energy; Office of Science; National Science Foundation","keywords":"Cloud computing; Computer science; Documentation; Remote sensing; Data processing; Process (computing); Benchmark (surveying); Consistency (knowledge bases); Field (mathematics); Data mining; Algorithm; Data science; Ice cloud; Systems engineering; Database; Artificial intelligence; Geology; Engineering","score_opus":0.024860140611428442,"score_gpt":0.25550314353097675,"score_spread":0.2306430029195483,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2744893833","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":[0.99678564,0.0012903073,0.00021609325,0.0004189596,0.000048758513,0.00030701252,0.000020165513,0.00002753123,0.00088554906],"genre_scores_gemma":[0.9971161,0.00027780398,0.0023011272,0.00018042733,0.000008999657,0.00002347555,0.000026288475,0.000010910174,0.000054880285],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984481,0.000058772883,0.00032978633,0.00058917276,0.00018725567,0.00038693217],"domain_scores_gemma":[0.9991897,0.00003791275,0.00017442732,0.00047598087,0.000008036158,0.00011397013],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004059615,0.00020498234,0.00033401768,0.0000056312965,0.00037478402,0.00014536513,0.0005122462,0.000083376035,0.00012578035],"category_scores_gemma":[0.00006409876,0.00014148437,0.000028504615,0.00010415961,0.0014375233,0.00033673452,0.0012483149,0.00013874713,0.0000019815934],"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":[0.000091529415,0.0001596891,0.91883004,0.00006706803,0.00001810349,0.000019393596,0.0009874093,0.000010231112,0.05576805,0.000010384494,0.000533608,0.0235045],"study_design_scores_gemma":[0.0026423435,0.00064832787,0.9635091,0.00016894312,0.00012217858,0.000053727177,0.0013708883,0.006802777,0.011862833,0.0024691536,0.009369015,0.0009807366],"about_ca_topic_score_codex":0.001064668,"about_ca_topic_score_gemma":0.00017076255,"teacher_disagreement_score":0.044679042,"about_ca_system_score_codex":0.000026635485,"about_ca_system_score_gemma":0.0000071462932,"threshold_uncertainty_score":0.5769565},"labels":[],"label_agreement":null},{"id":"W2747022243","doi":"10.1002/2017jd027146","title":"Scaling properties of observed and simulated satellite visible radiances","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"Academy of Finland","keywords":"Numerical weather prediction; Meteorology; Radiative transfer; Environmental science; Convection; Boundary layer; Satellite; Geology; Remote sensing; Physics; Optics","score_opus":0.08023319010868453,"score_gpt":0.3227386337389555,"score_spread":0.242505443630271,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2747022243","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":[0.9963737,0.0014748364,0.000029032619,0.00038263758,0.000060475413,0.000114606824,7.560561e-7,0.0000046784476,0.0015592827],"genre_scores_gemma":[0.99682456,0.00082295906,0.0013896425,0.000017135573,0.00013307226,0.000001114809,9.4702095e-8,0.00001451012,0.0007969257],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99791294,0.00013679726,0.00039730358,0.00019357662,0.000956834,0.00040252937],"domain_scores_gemma":[0.9987,0.00019344015,0.00036828712,0.0003465932,0.00013241399,0.00025923335],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00082807936,0.00012796062,0.00034834558,0.0000012589737,0.00047110123,0.00017711824,0.0006730018,0.00006906307,0.00027947727],"category_scores_gemma":[0.00081164634,0.00008607156,0.00011311052,0.00014139488,0.0013177292,0.00055651163,0.0004049386,0.00040123693,0.000038085014],"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":[0.0010975659,0.0005828435,0.5108933,0.00015824093,0.00017914572,0.00012020523,0.0014517474,0.0030940308,0.27023247,0.0003477454,0.0008121609,0.21103054],"study_design_scores_gemma":[0.0009623828,0.00087824307,0.95461804,0.00035159395,0.000023554967,0.000010374168,0.0006827319,0.0072917757,0.027786383,0.0031925314,0.003992085,0.00021033273],"about_ca_topic_score_codex":0.0024095504,"about_ca_topic_score_gemma":0.00008691438,"teacher_disagreement_score":0.44372472,"about_ca_system_score_codex":0.000058904447,"about_ca_system_score_gemma":0.000056257755,"threshold_uncertainty_score":0.4855228},"labels":[],"label_agreement":null},{"id":"W2747399443","doi":"10.1016/j.atmosenv.2017.08.044","title":"AEROCAN, the Canadian sub-network of AERONET: Aerosol monitoring and air quality applications","year":2017,"lang":"en","type":"article","venue":"Atmospheric Environment","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":33,"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","funders":"","keywords":"AERONET; Aerosol; Environmental science; Air quality index; Particulates; Air pollution; Atmospheric sciences; Pollution; Troposphere; Plume; Meteorology; Climatology; Geography; Geology","score_opus":0.012949671760926717,"score_gpt":0.23619393207765718,"score_spread":0.22324426031673048,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2747399443","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":[0.9892953,0.00049843115,0.0014602881,0.0010457105,0.0001181356,0.00060219783,0.0000052808946,0.000019227538,0.006955453],"genre_scores_gemma":[0.9917691,0.00041870982,0.0066184714,0.00015227204,0.00013960736,0.00018744901,0.000001877508,0.000025900232,0.00068664114],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983216,0.000057023837,0.00032875547,0.0004193718,0.00039518703,0.00047805693],"domain_scores_gemma":[0.9981845,0.000053831147,0.00032647382,0.0011573454,0.0000042695183,0.00027355616],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00039046674,0.00022105889,0.00023028396,1.3921671e-7,0.0016628043,0.000056238598,0.0006404429,0.000106058025,0.0005707156],"category_scores_gemma":[0.000016033975,0.00017414527,0.00006629723,0.000059152077,0.00095993147,0.00013733227,0.00041265404,0.00017701738,0.00016241672],"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":[0.000006774881,0.000041647952,0.9689684,0.0000069703046,0.000028402897,0.0000019031147,0.0001924529,0.008344597,0.0009535213,0.00018670612,0.0005053034,0.020763304],"study_design_scores_gemma":[0.00019440016,0.000042989814,0.97858906,0.000008969446,0.000028946448,0.0000026255075,0.00014864268,0.00020016971,0.0005475064,0.00019396865,0.019812811,0.00022993835],"about_ca_topic_score_codex":0.09134154,"about_ca_topic_score_gemma":0.03749109,"teacher_disagreement_score":0.053850453,"about_ca_system_score_codex":0.00036538113,"about_ca_system_score_gemma":0.000028638953,"threshold_uncertainty_score":0.9996369},"labels":[],"label_agreement":null},{"id":"W2749275209","doi":"10.1175/amsmonographs-d-17-0002.1","title":"Ice Fog: The Current State of Knowledge and Future Challenges","year":2017,"lang":"en","type":"article","venue":"Meteorological Monographs","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":56,"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; Ice nucleus; Fog; Icing; Ice crystals; Ice cloud; Atmospheric sciences; Lead (geology); Sea ice growth processes; Meteorology; Climate model; Water vapor; Atmosphere (unit); Climatology; Climate change; Arctic ice pack; Cloud computing; Sea ice; Drift ice; Geology; Nucleation; Geography; Computer science; Oceanography","score_opus":0.025549826374420232,"score_gpt":0.2661404408914346,"score_spread":0.24059061451701438,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2749275209","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":[0.9737003,0.013848533,0.00007939116,0.0014913724,0.00020606664,0.00015494072,0.00000406752,0.00001974886,0.010495584],"genre_scores_gemma":[0.98798174,0.011430856,0.00039966704,0.000048397007,0.00006439556,0.000020480924,4.019851e-7,0.000005361433,0.00004872081],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99916506,0.00007950344,0.0001487019,0.00025719922,0.00013126209,0.00021826389],"domain_scores_gemma":[0.9992697,0.00006156521,0.00014180018,0.0004381663,0.0000069814037,0.000081758575],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031063062,0.00012959485,0.00017557209,0.0000011424299,0.00036219225,0.000027071606,0.00047317322,0.000041555613,0.00015407983],"category_scores_gemma":[0.000025482674,0.00006755559,0.000081001104,0.000053073236,0.00084040285,0.000082987026,0.00042556535,0.00017690215,0.000024727378],"study_design_candidate":"design_other","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":[0.000020583011,0.000074834585,0.05062581,0.0000065338186,0.000011071178,0.0000011366362,0.00051786914,0.0000036060483,0.00009779028,0.00040798055,0.00032957358,0.9479032],"study_design_scores_gemma":[0.00014120962,0.00017061408,0.88977206,0.000003183595,0.000015277978,0.0000012952407,0.0000502557,0.00011245264,0.00005736762,0.006345753,0.103236966,0.00009357011],"about_ca_topic_score_codex":0.00001690436,"about_ca_topic_score_gemma":0.00006306638,"teacher_disagreement_score":0.94780964,"about_ca_system_score_codex":0.0000064896212,"about_ca_system_score_gemma":0.000002316613,"threshold_uncertainty_score":0.3096499},"labels":[],"label_agreement":null},{"id":"W2753045770","doi":"","title":"A far-infrared radiometer to study optically thin ice clouds in the Arctic","year":2015,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Remote sensing; Arctic; Sea ice; Environmental science; The arctic; Radiometer; Infrared; Arctic ice pack; Meteorology; Geology; Climatology; Astrobiology; Geography; Oceanography; Optics; Physics","score_opus":0.024088275258911107,"score_gpt":0.25754277781244833,"score_spread":0.23345450255353722,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2753045770","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":[0.95385855,0.000028083181,0.000033403274,0.00059834204,0.00019636583,0.00056925346,7.17844e-7,0.0000477194,0.044667587],"genre_scores_gemma":[0.9921687,0.000001691674,0.0054216078,0.001635597,0.000077969045,0.00005800875,0.0000011677743,0.000022542146,0.00061268033],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9977169,0.00018880994,0.00042315584,0.00045130827,0.0007173666,0.00050242693],"domain_scores_gemma":[0.998869,0.00023817114,0.00010505357,0.0005056271,0.000017099335,0.0002650464],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.002106837,0.00021307498,0.00020922796,0.000004297144,0.00011788063,0.00011063542,0.000700009,0.000076187374,0.00003910743],"category_scores_gemma":[0.00077889307,0.00015094731,0.000050740124,0.0005118218,0.00007858287,0.00013672592,0.00024765835,0.00030737504,0.00085900887],"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":[0.0000782121,0.0009089966,0.9359363,0.0000067462215,0.000024913876,0.0002555439,0.028414715,0.028375471,0.0005162882,0.000017572063,0.0022060887,0.0032592046],"study_design_scores_gemma":[0.0006109945,0.00042268998,0.98883724,0.00002071234,0.000023073439,0.000019767784,0.006929296,0.00042884727,0.000034740024,0.00025325746,0.0021634807,0.00025591863],"about_ca_topic_score_codex":0.014550669,"about_ca_topic_score_gemma":0.004710679,"teacher_disagreement_score":0.052900974,"about_ca_system_score_codex":0.00017296472,"about_ca_system_score_gemma":0.000021532907,"threshold_uncertainty_score":0.99991894},"labels":[],"label_agreement":null},{"id":"W2755214715","doi":"10.1038/s41598-017-12002-5","title":"Corona discharge induced snow formation in a cloud chamber","year":2017,"lang":"en","type":"article","venue":"Scientific Reports","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":17,"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","funders":"National Key Research and Development Program of China; National Natural Science Foundation of China; Chinese Academy of Meteorological Sciences; Ministry of Science and Technology of the People's Republic of China; Chinese Academy of Sciences; Université Laval","keywords":"Corona discharge; Cloud condensation nuclei; Snow; Ion wind; Ionization; Precipitation; Cloud chamber; Corona (planetary geology); Filamentation; Environmental science; Atmospheric sciences; Condensation; Cloud base; Materials science; Femtosecond; Meteorology; Cloud computing; Ion; Laser; Chemistry; Physics; Aerosol; Optics; Computer science; Astrobiology; Nuclear physics","score_opus":0.018654018126562158,"score_gpt":0.2521631814817697,"score_spread":0.23350916335520755,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2755214715","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":[0.9660792,0.0000072276907,0.00018725637,0.0002200786,0.0033330403,0.00023052645,5.787739e-7,0.00002451866,0.029917607],"genre_scores_gemma":[0.99221414,0.0000016144734,0.00020141006,0.000035931414,0.000049854338,0.000022102373,0.000009369172,0.000009175224,0.007456382],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983615,0.000020440906,0.00033741255,0.0004958691,0.00045917495,0.0003255484],"domain_scores_gemma":[0.998415,0.0000071143395,0.00037741882,0.0010865985,0.0000093670305,0.00010453639],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008268899,0.00011501086,0.00012745532,0.0000029531222,0.0007213331,0.0003461629,0.00020464094,0.00006340179,0.0019250232],"category_scores_gemma":[0.00012743802,0.000096635784,0.000050593673,0.00012728499,0.00028536675,0.0008023194,0.00030597174,0.00010486676,0.0004387787],"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":[0.000017679122,0.00027575137,0.82725626,0.000015966381,0.000007055652,0.00095223234,0.0035177898,0.00031781895,0.09148817,0.00022818975,0.045595754,0.030327303],"study_design_scores_gemma":[0.00044834023,0.000048888203,0.9045317,0.00006957547,0.0000105650815,0.0004015961,0.00033786285,0.0037786774,0.021761347,0.008165645,0.059880227,0.00056556344],"about_ca_topic_score_codex":0.0004827665,"about_ca_topic_score_gemma":0.00085299194,"teacher_disagreement_score":0.077275425,"about_ca_system_score_codex":0.00012429761,"about_ca_system_score_gemma":0.000015290114,"threshold_uncertainty_score":0.9989874},"labels":[],"label_agreement":null},{"id":"W2757529800","doi":"","title":"Aerosol Characterisitics Over Alberta Using Modis and OMI Satellite Data","year":2015,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Aerosol; Environmental science; Satellite; Meteorology; Remote sensing; Atmospheric sciences; Climatology; Geology; Geography; Engineering","score_opus":0.04468221695208293,"score_gpt":0.2641789399679363,"score_spread":0.21949672301585335,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2757529800","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":[0.98282844,0.00012830742,0.000031755622,0.00013150567,0.00022515008,0.00012741353,0.000011658772,0.00003558299,0.016480206],"genre_scores_gemma":[0.99374574,0.000053442465,0.0049352692,0.00038800863,0.00012590773,0.0000018561817,0.000034310287,0.000031334243,0.00068410934],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99834436,0.00003782812,0.00032275086,0.0005369699,0.00034344572,0.00041466515],"domain_scores_gemma":[0.99872535,0.000098390876,0.00018548401,0.000655988,0.000010567147,0.0003242117],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045001684,0.00021218759,0.00020092551,0.0000016330022,0.00013681741,0.0001144341,0.00040528495,0.00011150524,0.00003206253],"category_scores_gemma":[0.00021260351,0.00019688821,0.000024397457,0.00009682972,0.00015178995,0.0004792082,0.00069496257,0.00016578795,0.00021521871],"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":[0.000037028192,0.00011933562,0.9723958,0.00002264308,0.000030459143,0.000053858093,0.0015936682,0.0047082203,0.012384526,0.000009895371,0.0017987894,0.0068458016],"study_design_scores_gemma":[0.0011999243,0.00011652677,0.91750824,0.00015593937,0.00012858436,0.00010339252,0.0007400608,0.04863863,0.001429017,0.00015362112,0.028681278,0.0011447918],"about_ca_topic_score_codex":0.041021336,"about_ca_topic_score_gemma":0.0046073175,"teacher_disagreement_score":0.054887544,"about_ca_system_score_codex":0.000084455416,"about_ca_system_score_gemma":0.000022146734,"threshold_uncertainty_score":0.9653646},"labels":[],"label_agreement":null},{"id":"W2758500989","doi":"10.5194/acp-2017-692","title":"The topography contribution to the influence of the atmospheric boundary layer at high altitude stations","year":2017,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","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":"Environment and Climate Change Canada","funders":"","keywords":"Altitude (triangle); Effects of high altitude on humans; Latitude; Planetary boundary layer; Atmospheric sciences; Elevation (ballistics); Lapse rate; Boundary layer; Troposphere; Plateau (mathematics); Environmental science; Convection; Structural basin; Massif; Geology; Orography; Climatology; Meteorology; Geomorphology; Geography; Geodesy; Geometry; Precipitation; Mathematics","score_opus":0.004935018524142785,"score_gpt":0.22657270970205423,"score_spread":0.22163769117791143,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2758500989","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":[0.9889102,0.00003633797,0.000510604,0.0069285943,0.00017212835,0.00035331663,0.000007883365,0.000013235335,0.0030677186],"genre_scores_gemma":[0.9950469,0.00003670957,0.00043524537,0.0010114766,0.000021442971,0.000040277337,6.8580357e-7,0.000005786525,0.003401436],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99907357,0.000047612433,0.00016527843,0.00016319148,0.0003250646,0.00022531667],"domain_scores_gemma":[0.99881214,0.00007630067,0.0001579184,0.0008767947,0.00002312665,0.000053738884],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00024498536,0.00009400642,0.00007841131,1.2387125e-7,0.0029038917,0.00011077712,0.00092863926,0.000032617692,0.00055429345],"category_scores_gemma":[0.000102043065,0.000039374245,0.00007430943,0.00013891738,0.0007305287,0.00013443333,0.0006137868,0.00008092459,0.00016528682],"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":[0.000034149576,0.00004856309,0.94234437,0.0000017779347,0.000035018053,6.3728095e-7,0.0004832493,0.023664635,0.007120874,0.008810814,0.014148528,0.0033074135],"study_design_scores_gemma":[0.000105796586,0.000026030599,0.9148522,0.0000036011525,0.00001059201,7.987965e-7,0.00006536222,0.00019581933,0.0005899551,0.0007216625,0.08336597,0.00006221552],"about_ca_topic_score_codex":0.0026257492,"about_ca_topic_score_gemma":0.0046784575,"teacher_disagreement_score":0.06921744,"about_ca_system_score_codex":0.00007914423,"about_ca_system_score_gemma":0.000015642643,"threshold_uncertainty_score":0.9983942},"labels":[],"label_agreement":null},{"id":"W2761381305","doi":"10.1002/2016jd026423","title":"Added value of far‐infrared radiometry for remote sensing of ice clouds","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":24,"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 du Québec à Montréal","funders":"Canadian Space Agency","keywords":"Cirrus; Environmental science; Water vapor; Remote sensing; Radiometry; Atmosphere (unit); Ice cloud; Far infrared; Radiative transfer; Radiometer; Precipitation; Satellite; Cloud top; Cloud cover; Cloud computing; Atmospheric sciences; Meteorology; Geology; Physics; Computer science; Astronomy; Optics","score_opus":0.036928016600337024,"score_gpt":0.34113052367778074,"score_spread":0.30420250707744373,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2761381305","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":[0.9821346,0.00018205763,0.011911868,0.00029527285,0.00017306603,0.0002473712,0.00000903103,0.000005067482,0.005041676],"genre_scores_gemma":[0.9380851,0.000101965066,0.059415426,0.000026853952,0.00031487987,5.239445e-7,5.5296215e-7,0.00002834463,0.002026349],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9966704,0.00019802322,0.0007087315,0.00025594138,0.0015934048,0.00057348894],"domain_scores_gemma":[0.9966909,0.0010028564,0.00096484117,0.00070359337,0.0003354435,0.00030234756],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016634695,0.00017839896,0.0006221358,0.000003482629,0.00040456402,0.00007036251,0.0011141441,0.0001291103,0.0003653567],"category_scores_gemma":[0.0030196575,0.00013997666,0.00039965383,0.0003479409,0.0012219291,0.00033483174,0.00047047448,0.0005169034,0.00002130239],"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":[0.0027909603,0.0007067101,0.01353173,0.00027431585,0.00043296535,0.00009917698,0.0009343418,0.0018292331,0.37237784,0.0014036384,0.016675081,0.588944],"study_design_scores_gemma":[0.006617935,0.007904475,0.6331065,0.00087382743,0.00022471369,0.00006354824,0.002127776,0.11713622,0.13460694,0.07409715,0.022366233,0.00087464636],"about_ca_topic_score_codex":0.0020049533,"about_ca_topic_score_gemma":0.000033109394,"teacher_disagreement_score":0.6195748,"about_ca_system_score_codex":0.00015467138,"about_ca_system_score_gemma":0.00013991972,"threshold_uncertainty_score":0.57080823},"labels":[],"label_agreement":null},{"id":"W2762503443","doi":"","title":"New, Flexible Applications with the Multi-Spectral Titan Airborne Lidar","year":2015,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Optech (Canada)","funders":"","keywords":"Titan (rocket family); Lidar; Remote sensing; Environmental science; Meteorology; Geology; Geography; Aerospace engineering; Engineering","score_opus":0.019341714019979913,"score_gpt":0.24064843308351147,"score_spread":0.22130671906353155,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2762503443","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":[0.8907267,0.00008981541,0.003898348,0.0014252368,0.000070250564,0.0003254042,0.0000015379985,0.00015136515,0.10331137],"genre_scores_gemma":[0.9590263,0.0000038265216,0.033314228,0.00031211766,0.00013859925,0.000036031328,0.0000031111517,0.00002315616,0.007142643],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988428,0.000020665382,0.00016781225,0.00030206237,0.00032859767,0.00033809207],"domain_scores_gemma":[0.9991972,0.000047197354,0.00011788268,0.00036340317,0.000012826363,0.00026151087],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002832138,0.00015304127,0.000107185755,0.0000011219307,0.00019750177,0.000061208295,0.00035171062,0.000056895537,0.00004589369],"category_scores_gemma":[0.000028890183,0.000098852295,0.00003362051,0.00020821943,0.0001291548,0.00011787901,0.00009153193,0.00018513322,0.0011304574],"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":[0.000113973314,0.0005452487,0.7078958,0.000016527058,0.00008540332,0.000052744577,0.0047651534,0.14830883,0.005604775,0.00063548854,0.10000402,0.03197204],"study_design_scores_gemma":[0.0011051515,0.00022970019,0.7423527,0.000030618834,0.000054471297,0.00003493829,0.0018511111,0.00074661995,0.002866134,0.000367059,0.24979854,0.0005629374],"about_ca_topic_score_codex":0.013514875,"about_ca_topic_score_gemma":0.0081226155,"teacher_disagreement_score":0.14979452,"about_ca_system_score_codex":0.00010296953,"about_ca_system_score_gemma":0.000045807483,"threshold_uncertainty_score":0.99964726},"labels":[],"label_agreement":null},{"id":"W2762791688","doi":"10.1115/omae2017-61097","title":"Thermal Analysis of Saline Droplet Motion With Cooling in Cold Regions","year":2017,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Evaporation; Mechanics; Thermal; Evaporative cooler; Materials science; Convection; Heat transfer; Relative humidity; Thermodynamics; Humidity; Process (computing); Physics","score_opus":0.01096063134481395,"score_gpt":0.23062742075604373,"score_spread":0.21966678941122977,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2762791688","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":[0.9784972,0.0000026508885,0.008826389,0.00016835477,0.00000814224,0.00004878143,0.0000011370032,0.0000069307653,0.012440397],"genre_scores_gemma":[0.99716926,0.0000043604705,0.0016559177,0.00004933809,0.0000056804315,0.000002714598,0.0000017219786,0.0000036832491,0.001107305],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99955106,0.0000101640135,0.00010032299,0.000120715755,0.000121140656,0.00009659617],"domain_scores_gemma":[0.9995792,0.000008466109,0.00009456149,0.0002861434,0.0000034073864,0.000028226548],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00008930229,0.000049699218,0.000118895616,0.0000015966323,0.00008715402,0.000012974195,0.00014505524,0.000024485349,0.0013253553],"category_scores_gemma":[0.000007765557,0.000034714943,0.00003257237,0.00016930878,0.00013343856,0.00009198725,0.00006123633,0.00003552004,0.000011824518],"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":[0.000015402944,0.00004892464,0.9463377,8.047073e-7,0.000034760356,0.0000030205565,0.000110916924,0.04642113,0.005976741,0.00038682597,0.000052338648,0.0006114201],"study_design_scores_gemma":[0.00016777522,0.000027140313,0.9577913,0.000003382841,0.00007235006,1.6158214e-7,0.00008345396,0.04080603,0.0008923516,0.000008964449,0.00009028551,0.00005680312],"about_ca_topic_score_codex":0.0041385493,"about_ca_topic_score_gemma":0.005511517,"teacher_disagreement_score":0.018672062,"about_ca_system_score_codex":0.000026706193,"about_ca_system_score_gemma":0.000002792373,"threshold_uncertainty_score":0.9995876},"labels":[],"label_agreement":null},{"id":"W2762900324","doi":"10.5194/amt-11-861-2018","title":"Three-channel single-wavelength lidar depolarization calibration","year":2018,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":5,"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; Western University","funders":"","keywords":"Lidar; Depolarization; Rayleigh scattering; Polarization (electrochemistry); Optics; Depolarization ratio; Perpendicular; Linear polarization; Wavelength; Physics; Laser; Chemistry; Mathematics; Geometry","score_opus":0.02709055946177859,"score_gpt":0.2180019741135323,"score_spread":0.1909114146517537,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2762900324","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"methods","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.09437614,0.00007360828,0.8820894,0.00028009797,0.00022275168,0.0006584829,0.0000013509892,0.00084416824,0.021454047],"genre_scores_gemma":[0.89210874,0.000017348339,0.106701806,0.0006322471,0.00024719717,0.000081023034,0.000005547513,0.000048011516,0.00015809428],"study_design_codex":"design_other","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.997605,0.00005950909,0.00039802035,0.00052428787,0.0009800527,0.00043312492],"domain_scores_gemma":[0.999096,0.000011852569,0.00020173886,0.00046549115,0.00008354945,0.00014139533],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005427207,0.00029106447,0.00021048526,6.8591635e-7,0.00033539865,0.00008181239,0.00031805827,0.00017102947,0.0017404074],"category_scores_gemma":[0.00006644266,0.00026432655,0.00007802546,0.0004921354,0.0002793893,0.00040271043,0.00017286856,0.00013393976,0.00019856174],"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":[0.000121475474,0.0008950399,0.11442379,0.000034803583,0.00009453139,0.0000144248625,0.0009866196,0.000064707514,0.36396235,0.00089751143,0.033953216,0.48455152],"study_design_scores_gemma":[0.0011087001,0.0041094976,0.09212081,0.00024906633,0.00020675315,0.00004656408,0.00031249385,0.081742086,0.7088695,0.017600872,0.0907993,0.002834339],"about_ca_topic_score_codex":0.00076484156,"about_ca_topic_score_gemma":0.00064562616,"teacher_disagreement_score":0.7977326,"about_ca_system_score_codex":0.0004624185,"about_ca_system_score_gemma":0.000029384912,"threshold_uncertainty_score":0.99998087},"labels":[],"label_agreement":null},{"id":"W2763652786","doi":"10.3390/ecas2017-04146","title":"Sensitivity of Precipitation to Aerosol and Temperature Perturbation over the Foothills of the Nepal Himalayas","year":2017,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"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":"Natural Environment Research Council; Sight Research UK","keywords":"Aerosol; Environmental science; Orography; Precipitation; Atmospheric sciences; Perturbation (astronomy); Climatology; Weather Research and Forecasting Model; Meteorology; Geology; Geography; Physics","score_opus":0.0062946137476277385,"score_gpt":0.22191989293971065,"score_spread":0.2156252791920829,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2763652786","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":[0.9930461,0.0000054491347,0.00011440424,0.0012112032,0.00007263964,0.00021482949,0.0000036457982,0.000003444286,0.005328273],"genre_scores_gemma":[0.9972902,0.0000037816917,0.0004252678,0.0002628348,0.00001797471,0.0000034658754,2.8992244e-7,0.0000036973447,0.0019924652],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99949616,0.000048248792,0.00009064051,0.00011444079,0.0001775507,0.000072933624],"domain_scores_gemma":[0.99948883,0.00005121533,0.000107092295,0.00031902973,0.000010295278,0.000023544739],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020200254,0.000059433478,0.00007156387,3.034755e-7,0.0002274291,0.000023830278,0.00012662965,0.00004039289,0.00015028124],"category_scores_gemma":[0.000113056376,0.000028884513,0.000030792813,0.000036464466,0.00021821487,0.000110268265,0.00014706445,0.000051450315,0.0000033500876],"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":[0.000027814724,0.000042467756,0.5266257,0.000007720562,0.000010882724,2.5102733e-7,0.0026358925,0.0005109757,0.46036777,0.00077958964,0.0028180862,0.006172877],"study_design_scores_gemma":[0.00008847667,0.000033605444,0.9777847,0.000007945968,0.0000070354736,0.0000010217584,0.00012647561,0.0008070119,0.020869188,0.00010304222,0.00012908733,0.00004239423],"about_ca_topic_score_codex":0.00086254167,"about_ca_topic_score_gemma":0.00060978904,"teacher_disagreement_score":0.45115906,"about_ca_system_score_codex":0.000015667356,"about_ca_system_score_gemma":0.000004826473,"threshold_uncertainty_score":0.17492238},"labels":[],"label_agreement":null},{"id":"W2765316162","doi":"10.5194/amt-11-1615-2018","title":"A prototype method for diagnosing high ice water content probability using satellite imager data","year":2018,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","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":"Aurora College","funders":"","keywords":"Environmental science; Daytime; Meteorology; Geostationary orbit; Satellite; Collocation (remote sensing); Remote sensing; Icing; Convective storm detection; Liquid water content; Brightness temperature; Geostationary Operational Environmental Satellite; Tropopause; Cloud top; Air mass (solar energy); Convection; Atmospheric sciences; Troposphere; Computer science; Cloud computing; Brightness; Aerospace engineering; Geology; Geography; Physics; Engineering","score_opus":0.14173253288738216,"score_gpt":0.3163590155259183,"score_spread":0.1746264826385361,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2765316162","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.15581049,0.00013577144,0.8361481,0.00042207967,0.00022120668,0.0053122886,0.000012633065,0.0005080278,0.0014294268],"genre_scores_gemma":[0.20240352,0.000021306612,0.79601693,0.00054148486,0.00018656442,0.00064593356,0.000015457228,0.000057159297,0.00011164724],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9965663,0.00020046548,0.0005829014,0.00108542,0.0008348295,0.00073010294],"domain_scores_gemma":[0.9979943,0.0000538127,0.00019115396,0.0014138884,0.00019236837,0.00015445592],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.003144674,0.00038761093,0.0003981206,6.389698e-7,0.00039902012,0.00010512909,0.0007374935,0.00014860142,0.0010818138],"category_scores_gemma":[0.00020326827,0.00027694428,0.0001004044,0.00023274568,0.00037059892,0.00051812344,0.00074085203,0.00014825618,0.00006799965],"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":[0.0003560869,0.00055885914,0.025541322,0.00012369976,0.0001119634,0.0000072050525,0.00049051316,0.00002996906,0.7011921,0.0001344206,0.003186591,0.2682673],"study_design_scores_gemma":[0.0008688978,0.0015555688,0.01132319,0.00021186867,0.00028242246,0.000024564677,0.00010599546,0.017391203,0.80460995,0.007119212,0.15515202,0.0013550787],"about_ca_topic_score_codex":0.0021952968,"about_ca_topic_score_gemma":0.00016426276,"teacher_disagreement_score":0.26691222,"about_ca_system_score_codex":0.000605399,"about_ca_system_score_gemma":0.000042775722,"threshold_uncertainty_score":0.9999683},"labels":[],"label_agreement":null},{"id":"W2765793853","doi":"","title":"PMC-Turbo: a balloon-borne Mission to image gravity waves and turbulence in polar mesospheric clouds","year":2017,"lang":"en","type":"article","venue":"elib (German Aerospace Center)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Physics; Field of view; Remote sensing; Cadence; Astronomy; Geology; Optics","score_opus":0.0072672431549093836,"score_gpt":0.2545856845926281,"score_spread":0.2473184414377187,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2765793853","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":[0.9921969,0.00020593074,0.00017048161,0.0030013458,0.00043151597,0.00041269275,0.000016311596,0.000068845984,0.0034959393],"genre_scores_gemma":[0.98827094,0.00021055965,0.0056544864,0.0005428416,0.00007613604,0.00001390387,0.0000051658353,0.000045970362,0.0051799817],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99759686,0.00008298098,0.0003167904,0.0008109233,0.00045071062,0.00074176403],"domain_scores_gemma":[0.9982867,0.00002349815,0.00020865745,0.00096604164,0.000012717046,0.0005023705],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00033756558,0.00038904103,0.0003735573,0.000003485908,0.0005191345,0.0002814829,0.00081259373,0.00014362602,0.0008474542],"category_scores_gemma":[0.000090417496,0.00034835277,0.00009000896,0.00016820329,0.00041675876,0.00054313743,0.0010814329,0.0003122655,0.0004715134],"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":[0.00012305494,0.000359452,0.8947161,0.000035233286,0.000014459721,0.00013265164,0.0029352764,0.00003649519,0.079184644,0.000046541696,0.011392856,0.011023238],"study_design_scores_gemma":[0.00085124763,0.00012094623,0.98215693,0.000121469566,0.000010759392,0.000017972683,0.00015724511,0.00037100076,0.003793714,0.00012757946,0.011810739,0.00046041762],"about_ca_topic_score_codex":0.0010067559,"about_ca_topic_score_gemma":0.00030615507,"teacher_disagreement_score":0.08744081,"about_ca_system_score_codex":0.0001803884,"about_ca_system_score_gemma":0.000015275276,"threshold_uncertainty_score":0.9998968},"labels":[],"label_agreement":null},{"id":"W2765918963","doi":"10.1175/jas-d-17-0104.1","title":"A New Radiative Transfer Method for Solar Radiation in a Vertically Internally Inhomogeneous Medium","year":2017,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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; Environment and Climate Change Canada","funders":"Japan Society for the Promotion of Science; Priority Academic Program Development of Jiangsu Higher Education Institutions; Government of Jiangsu Province; Natural Science Foundation of Jiangsu Province; National Natural Science Foundation of China","keywords":"Radiative transfer; Absorption (acoustics); Computational physics; Wavelength; Optics; Radiation; Reflection (computer programming); Scattering; Atmospheric radiative transfer codes; Optical depth; Materials science; Snow; Physics; Aerosol; Meteorology","score_opus":0.01339663556457592,"score_gpt":0.2848076847390444,"score_spread":0.27141104917446846,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2765918963","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":[0.8315266,0.00017859634,0.15970317,0.006285234,0.0009931084,0.00025970588,9.614821e-7,0.0000049037426,0.0010477435],"genre_scores_gemma":[0.8737527,0.00004714271,0.12491902,0.00055401714,0.00014737753,0.000004689395,3.2771595e-8,0.0000092974415,0.00056571636],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998383,0.00009911408,0.00042924148,0.00020968636,0.00058003183,0.000298964],"domain_scores_gemma":[0.99906045,0.00016062905,0.00036611146,0.00024760197,0.000021914117,0.00014330454],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014249181,0.00013526499,0.00025078063,8.652159e-7,0.00046899117,0.00016010088,0.0017158017,0.000061771585,0.00034906852],"category_scores_gemma":[0.00050396676,0.000079915764,0.00020235607,0.00021812324,0.00039202874,0.00052117713,0.00014914823,0.00017227868,0.000008178971],"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":[0.0005083007,0.00023030966,0.5034755,0.000013284006,0.00010973528,0.00004012561,0.006034573,0.11939999,0.020837037,0.0003685622,0.008616996,0.34036562],"study_design_scores_gemma":[0.0029744213,0.0014118102,0.73497677,0.0001319932,0.0001229648,0.00018913453,0.00065954146,0.22589944,0.008136548,0.0114025725,0.013629341,0.00046544036],"about_ca_topic_score_codex":0.00078366994,"about_ca_topic_score_gemma":0.00041811986,"teacher_disagreement_score":0.33990017,"about_ca_system_score_codex":0.00017373396,"about_ca_system_score_gemma":0.00020682575,"threshold_uncertainty_score":0.38220555},"labels":[],"label_agreement":null},{"id":"W2767970493","doi":"10.5194/amt-10-4253-2017","title":"Depolarization calibration and measurements using the CANDAC Rayleigh–Mie–Raman lidar at Eureka, Canada","year":2017,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":12,"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; Dalhousie University; Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency; Indigenous and Northern Affairs Canada; Environment and Climate Change Canada; Eurostars; Strong; Ontario Innovation Trust","keywords":"Lidar; Depolarization ratio; Remote sensing; Environmental science; Calibration; Ice cloud; Rayleigh scattering; Depolarization; Optics; Physics; Geology; Radiative transfer","score_opus":0.035231812527016515,"score_gpt":0.2357692126301827,"score_spread":0.20053740010316617,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2767970493","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":[0.94670045,0.00038661895,0.044057492,0.0009426153,0.00031136992,0.0011283283,0.000004820502,0.0001808397,0.006287438],"genre_scores_gemma":[0.98541874,0.00005023602,0.013481577,0.0005630048,0.00007697548,0.000054539454,0.0000035322512,0.000038851504,0.00031254903],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9972946,0.00013288896,0.00035051358,0.00046746156,0.0013533719,0.00040113972],"domain_scores_gemma":[0.99857634,0.0000145068425,0.00040848096,0.0007883506,0.000059303646,0.00015300023],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00082993245,0.00029685476,0.00022334165,4.2728212e-7,0.0020947647,0.00023009386,0.00053802365,0.000107338135,0.00036318603],"category_scores_gemma":[0.00009258476,0.00022200042,0.000047054895,0.00010933058,0.00031575726,0.00037661762,0.0004226515,0.00015044885,0.000003233484],"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":[0.000028555387,0.000043889053,0.8977747,0.000016468057,0.000050030278,0.0000078479625,0.00014468908,0.00017272178,0.08379902,0.000042454398,0.005519125,0.012400514],"study_design_scores_gemma":[0.0010858199,0.00028223725,0.7106571,0.00020752271,0.00032279664,0.000054572167,0.0003058011,0.024941772,0.20784755,0.00060767034,0.051978312,0.0017088341],"about_ca_topic_score_codex":0.4948741,"about_ca_topic_score_gemma":0.4509813,"teacher_disagreement_score":0.18711758,"about_ca_system_score_codex":0.0015323292,"about_ca_system_score_gemma":0.00018018189,"threshold_uncertainty_score":0.9992044},"labels":[],"label_agreement":null},{"id":"W2776131517","doi":"","title":"Retrieval of Temperature From a Multiple Channel Rayleigh-Scatter Lidar Using an Optimal Estimation Method","year":2014,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Western University","funders":"","keywords":"Lidar; Remote sensing; Rayleigh scattering; Environmental science; Atmospheric temperature; Smoothing; Temperature measurement; Altitude (triangle); Meteorology; Optics; Mathematics; Physics; Geology; Statistics","score_opus":0.015759963061088754,"score_gpt":0.2545300664125289,"score_spread":0.23877010335144014,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2776131517","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":[0.98987776,0.000018907393,0.00849377,0.000068868394,0.00019295434,0.00014948274,0.000009008513,0.00005494524,0.0011343205],"genre_scores_gemma":[0.7907497,0.000001365671,0.20889767,0.00013679036,0.00012385237,0.0000020047198,0.000020224346,0.000025534593,0.000042840347],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9983166,0.00013436304,0.0003976142,0.00045330063,0.00037975717,0.0003183698],"domain_scores_gemma":[0.9989363,0.0002265797,0.00031178148,0.00035226624,0.000021113736,0.00015195498],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00071509765,0.00021187929,0.00025974627,0.0000033390063,0.0001651395,0.000051594965,0.00025609584,0.0001895236,0.000059451064],"category_scores_gemma":[0.00033566554,0.00019302365,0.00007077112,0.00015125627,0.00009092485,0.00029955487,0.00011137164,0.00022483942,0.000055237935],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007840189,0.00014149655,0.038802236,0.000013484257,0.000016849075,0.0000048698503,0.0012099245,0.6639324,0.29383403,0.0000012813988,0.000091440015,0.0018735863],"study_design_scores_gemma":[0.0007389992,0.00017886513,0.30823043,0.0001226739,0.00006725999,0.000009639927,0.00034285986,0.5613405,0.12816076,0.00014826468,0.000195373,0.00046435863],"about_ca_topic_score_codex":0.010272156,"about_ca_topic_score_gemma":0.00038065907,"teacher_disagreement_score":0.2694282,"about_ca_system_score_codex":0.00006624598,"about_ca_system_score_gemma":0.00001252927,"threshold_uncertainty_score":0.9963185},"labels":[],"label_agreement":null},{"id":"W2776325560","doi":"10.1016/j.jqsrt.2017.12.020","title":"Explicit solutions to the mixing rules with three-component inclusions","year":2017,"lang":"en","type":"article","venue":"Journal of Quantitative Spectroscopy and Radiative Transfer","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":25,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"National Natural Science Foundation of China","keywords":"Component (thermodynamics); Mixing (physics); Refractive index; Mathematics; Index (typography); Aerosol; Materials science; Applied mathematics; Computer science; Physics; Thermodynamics; Optics; Meteorology; Quantum mechanics","score_opus":0.02738843058735734,"score_gpt":0.2843590605589868,"score_spread":0.25697062997162945,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2776325560","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":[0.7762524,0.0002381947,0.21552537,0.006223226,0.000076823795,0.0001745155,0.000013912624,0.0000039076644,0.0014916612],"genre_scores_gemma":[0.9760655,0.00019948279,0.023330761,0.00025604636,0.00007308292,0.0000072679495,3.57419e-7,0.000012507743,0.00005499218],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9989358,0.00006732227,0.00024329865,0.00016927825,0.00031572368,0.00026853202],"domain_scores_gemma":[0.9993631,0.00012390727,0.00013347888,0.00018803024,0.000030995583,0.00016046499],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0003961829,0.00015923486,0.00024436894,0.000005904084,0.0017122823,0.000096869066,0.00036031028,0.00003252337,0.0002796781],"category_scores_gemma":[0.00003244091,0.000085091975,0.00008351925,0.00008014852,0.00043286296,0.0003617222,0.000087464825,0.00025929153,0.000034215835],"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":[0.0031165616,0.0011201297,0.29726064,0.000036925416,0.0010968263,0.00021076224,0.07709503,0.0113797905,0.41275913,0.1826592,0.0057510603,0.007513952],"study_design_scores_gemma":[0.0010184239,0.0018979035,0.98024696,0.00009672551,0.00011384154,0.00004427195,0.0024740351,0.00095311436,0.0058828075,0.0034951833,0.003504885,0.00027185646],"about_ca_topic_score_codex":0.00025584182,"about_ca_topic_score_gemma":0.0012471537,"teacher_disagreement_score":0.6829863,"about_ca_system_score_codex":0.00008587533,"about_ca_system_score_gemma":0.000027717444,"threshold_uncertainty_score":0.99958736},"labels":[],"label_agreement":null},{"id":"W2779282010","doi":"10.22323/1.301.0754","title":"TAIGA-HiSCORE detection of the CATS-Lidar on the ISS as fast moving point source","year":2017,"lang":"en","type":"article","venue":"Proceedings of 35th International Cosmic Ray Conference — PoS(ICRC2017)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":7,"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":"Russian Science Foundation; Russian Foundation for Basic Research; Deutsche Forschungsgemeinschaft; European Commission; McGill University","keywords":"Lidar; Remote sensing; Laser; Calibration; Optics; Physics; Cherenkov radiation; Environmental science; Detector; Geology","score_opus":0.015329571736899887,"score_gpt":0.23578103887398777,"score_spread":0.22045146713708788,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2779282010","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":[0.93727416,0.00000873876,0.000455581,0.0031215327,0.0004381348,0.0003033862,0.000013257062,0.00002270017,0.05836253],"genre_scores_gemma":[0.9943489,0.000027563492,0.00016795982,0.00035039854,0.00010870313,0.000029548824,0.000001197223,0.00002168706,0.0049440633],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9981157,0.000012971487,0.00039975837,0.00039107428,0.0008150575,0.00026542807],"domain_scores_gemma":[0.99836254,0.000058204972,0.0009524165,0.00035431617,0.00019886154,0.000073639625],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00042335986,0.00023449074,0.00021952527,0.0000071364766,0.0005514281,0.00019090528,0.002078931,0.000088928224,0.0009797557],"category_scores_gemma":[0.0005095989,0.0001490911,0.00015088412,0.00006693157,0.0007279764,0.0004121629,0.00066474127,0.00032868935,0.00012143997],"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":[0.00032425812,0.0002740068,0.15390328,0.000052913074,0.00015544296,0.0000017384062,0.0051265964,0.000297468,0.7858281,0.017624883,0.0030601176,0.03335117],"study_design_scores_gemma":[0.0012010512,0.00061176217,0.36367908,0.0006516352,0.00009491916,0.00005421265,0.005288354,0.013378818,0.5851079,0.015083753,0.01406777,0.0007807353],"about_ca_topic_score_codex":0.0011086146,"about_ca_topic_score_gemma":0.000058211885,"teacher_disagreement_score":0.2097758,"about_ca_system_score_codex":0.00016360586,"about_ca_system_score_gemma":0.000044570083,"threshold_uncertainty_score":0.9999335},"labels":[],"label_agreement":null},{"id":"W2779968693","doi":"10.5194/gmd-11-2333-2018","title":"The implementation of NEMS GFS Aerosol Component (NGAC) Version 2.0 for global multispecies forecasting at NOAA/NCEP – Part 2: Evaluation of aerosol optical thickness","year":2018,"lang":"en","type":"article","venue":"Geoscientific model development","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":25,"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":"Goddard Space Flight Center; National Weather Service; National Oceanic and Atmospheric Administration","keywords":"Aerosol; Environmental science; AERONET; Meteorology; Climatology; Atmospheric sciences; Satellite; Data assimilation; Geography; Geology; Physics","score_opus":0.048370280521541034,"score_gpt":0.29270904516888574,"score_spread":0.24433876464734472,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2779968693","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":[0.92834395,0.000027001746,0.06877829,0.00009465417,0.0008271258,0.0010210826,0.000059804403,0.000017458642,0.000830658],"genre_scores_gemma":[0.9693194,0.0000058982273,0.029640915,0.00002812076,0.000032673965,0.00016165685,0.00009113981,0.000011979714,0.000708201],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9967432,0.00006765259,0.0007136313,0.00052697555,0.0014574372,0.0004910722],"domain_scores_gemma":[0.99882513,0.00007654364,0.000398529,0.00034950665,0.00024485984,0.000105405714],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002140423,0.00020356856,0.00021434837,0.0000038115013,0.0010749056,0.000050484305,0.0003827529,0.00007696045,0.0005259155],"category_scores_gemma":[0.0000647063,0.00015631327,0.00008966165,0.00025936036,0.00070545886,0.00015481886,0.0005003754,0.00005232397,0.00004594997],"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":[0.00092673005,0.0010693201,0.068105645,0.00022801822,0.00024816307,0.0000014445603,0.021523392,0.13998799,0.21425486,0.0019363727,0.038116325,0.5136018],"study_design_scores_gemma":[0.0019190456,0.00015396537,0.02345968,0.000065060274,0.00009283757,0.000004591652,0.0020549204,0.8567547,0.11081239,0.00029271902,0.0039963354,0.0003937478],"about_ca_topic_score_codex":0.00015014553,"about_ca_topic_score_gemma":0.0014800126,"teacher_disagreement_score":0.7167667,"about_ca_system_score_codex":0.00077339687,"about_ca_system_score_gemma":0.00016577037,"threshold_uncertainty_score":0.8267414},"labels":[],"label_agreement":null},{"id":"W2781682963","doi":"10.5194/acp-18-11375-2018","title":"Transport of Canadian forest fire smoke over the UK as observed by lidar","year":2018,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":60,"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":"Natural Environment Research Council; Met Office; European Organization for the Exploitation of Meteorological Satellites; University of Manchester; Sight Research UK; National Aeronautics and Space Administration","keywords":"Lidar; Ceilometer; Aerosol; Environmental science; Plume; Smoke; Atmospheric sciences; Troposphere; Depolarization ratio; Range (aeronautics); Meteorology; Remote sensing; Geology; Geography; Materials science","score_opus":0.008674044352520813,"score_gpt":0.1930833245617529,"score_spread":0.18440928020923208,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2781682963","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":[0.97008544,0.000100960475,0.00006480788,0.000107788655,0.000029270463,0.00007590488,0.000018690123,0.000010699325,0.02950643],"genre_scores_gemma":[0.99422956,0.000079458456,0.0005322654,0.00035009754,0.00009680937,0.0000077693685,0.000015940286,0.00001480109,0.0046733306],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99918973,0.0000069967036,0.0001459871,0.00023251223,0.0001679132,0.00025684654],"domain_scores_gemma":[0.9994514,0.000019035235,0.0000642024,0.0002880704,0.000009856859,0.0001674492],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000052251486,0.00015621907,0.00013935482,8.023723e-9,0.00019898394,0.000012039958,0.00022954274,0.00008253622,0.008310383],"category_scores_gemma":[0.000004289252,0.00011983946,0.000059252463,0.00029716676,0.00052189815,0.000057764184,0.000032363165,0.000103015285,0.00003091462],"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":[0.000023558863,0.00006398821,0.94680387,0.00002741255,0.00004147092,0.0000051325455,0.0008064079,0.00010241136,0.009977945,0.000052486786,0.010418413,0.031676885],"study_design_scores_gemma":[0.0005780917,0.00013917983,0.8259252,0.000030765987,0.0000822411,0.000009693969,0.00035218976,0.004814499,0.022584215,0.0012980525,0.14362341,0.0005624957],"about_ca_topic_score_codex":0.1975573,"about_ca_topic_score_gemma":0.008936284,"teacher_disagreement_score":0.18862103,"about_ca_system_score_codex":0.000042340438,"about_ca_system_score_gemma":0.000037302147,"threshold_uncertainty_score":0.99259615},"labels":[],"label_agreement":null},{"id":"W2782190440","doi":"10.1016/j.atmosres.2018.01.004","title":"Comparison of three ice cloud optical schemes in climate simulations with community atmospheric model version 5","year":2018,"lang":"en","type":"article","venue":"Atmospheric Research","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":41,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"National Key Research and Development Program of China; National Natural Science Foundation of China","keywords":"Longwave; Shortwave; Cloud forcing; Climate model; Environmental science; Cloud albedo; Climatology; Atmospheric sciences; Cloud feedback; Atmospheric model; Radiative transfer; Parametrization (atmospheric modeling); Radiative flux; Albedo (alchemy); Meteorology; Cloud cover; Cloud computing; Climate change; Climate sensitivity; Geology; Physics; Computer science","score_opus":0.07786696562988402,"score_gpt":0.3776466404870914,"score_spread":0.29977967485720736,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2782190440","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":[0.96897167,0.000061365456,0.014695646,0.00011398932,0.000047207366,0.00042439674,0.0000048215948,0.0000439929,0.015636895],"genre_scores_gemma":[0.90763086,0.000021893862,0.09193222,0.000038937007,0.000042919695,0.000021713771,0.00000848591,0.000037425598,0.00026556788],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99660987,0.00034029115,0.0004976536,0.0004378012,0.0012110505,0.000903315],"domain_scores_gemma":[0.99818796,0.00045191505,0.00012810229,0.00089247926,0.0001277872,0.00021178418],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012961401,0.00023966898,0.00041914085,7.768932e-7,0.00075747597,0.000045688077,0.0008210129,0.00017174699,0.001777459],"category_scores_gemma":[0.00012314662,0.00019908829,0.00006126643,0.0018202077,0.0019405182,0.00029524462,0.0009829863,0.0009551755,0.00037295296],"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":[0.00039877105,0.00080189283,0.80173606,0.000034799592,0.000018921352,0.0000042499964,0.0014736882,0.18628268,0.0027630166,0.0005029238,0.00077290146,0.005210068],"study_design_scores_gemma":[0.00080415467,0.0009972083,0.11493418,0.00006362263,0.000013121409,0.0000018593747,0.0015781114,0.8789424,0.0008921668,0.00061860273,0.00090219063,0.00025241444],"about_ca_topic_score_codex":0.0026565655,"about_ca_topic_score_gemma":0.00328278,"teacher_disagreement_score":0.6926597,"about_ca_system_score_codex":0.00034136072,"about_ca_system_score_gemma":0.00008194978,"threshold_uncertainty_score":0.9991351},"labels":[],"label_agreement":null},{"id":"W2782829225","doi":"10.1007/s00376-017-7091-5","title":"Aerosol microphysical and radiative effects on continental cloud ensembles","year":2018,"lang":"en","type":"article","venue":"Advances in Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":49,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Biological and Environmental Research; Office of Science; Jet Propulsion Laboratory; National Aeronautics and Space Administration; U.S. Department of Energy","keywords":"Aerosol; Atmospheric sciences; Environmental science; Precipitation; Cloud condensation nuclei; Radiative transfer; Weather Research and Forecasting Model; Shortwave; Cloud physics; Liquid water content; Meteorology; Climatology; Cloud computing; Geology; Physics","score_opus":0.00436630107469734,"score_gpt":0.24338401518628713,"score_spread":0.23901771411158979,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2782829225","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":[0.9795588,0.0008498071,0.0005759555,0.00018035014,0.0005689948,0.00023038012,0.0000010273995,0.00003924029,0.017995441],"genre_scores_gemma":[0.9837198,0.000339618,0.014663456,0.00074944913,0.00024086174,0.000025714895,3.7183509e-7,0.000011741991,0.00024898959],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981743,0.000080265396,0.0002100648,0.00066300516,0.00038863192,0.0004837386],"domain_scores_gemma":[0.9993225,0.0002740064,0.000108396285,0.00017017851,0.0000070029446,0.00011796218],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002148215,0.00023095004,0.00024625912,7.2294097e-7,0.0003628179,0.00005454976,0.00035322874,0.000055266613,0.00032682926],"category_scores_gemma":[0.00007487997,0.00017761515,0.000041197483,0.000684297,0.0025949802,0.0004868883,0.00018956923,0.00012166525,0.00024525437],"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":[0.00021670057,0.00039515714,0.57937413,0.000029847108,0.000015155186,0.00005468463,0.003197705,0.0031680816,0.0257271,0.0027069058,0.0016310366,0.3834835],"study_design_scores_gemma":[0.0068773595,0.0150617855,0.6516612,0.00061521755,0.000072342606,0.00009754636,0.0056447196,0.06613731,0.14975229,0.017249035,0.08272406,0.0041071475],"about_ca_topic_score_codex":0.00016471758,"about_ca_topic_score_gemma":0.00015101816,"teacher_disagreement_score":0.37937635,"about_ca_system_score_codex":0.00008534525,"about_ca_system_score_gemma":0.000014278706,"threshold_uncertainty_score":0.9561313},"labels":[],"label_agreement":null},{"id":"W2786092450","doi":"10.1002/2017gl076763","title":"Stratospheric Smoke With Unprecedentedly High Backscatter Observed by Lidars Above Southern France","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":180,"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":"Institut national des sciences de l'Univers; Langley Research Center; Centre National d’Etudes Spatiales","keywords":"Lidar; Aerosol; Environmental science; Volcano; Plume; Smoke; Stratosphere; Backscatter (email); Atmospheric sciences; Climatology; Southern Hemisphere; Geology; Remote sensing; Meteorology; Geography; Seismology","score_opus":0.019659329184655502,"score_gpt":0.2610072908726081,"score_spread":0.24134796168795258,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2786092450","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":[0.99179536,0.000016951735,0.0007303505,0.0047585294,0.000081030754,0.0003111494,0.000024803692,0.00006300623,0.002218801],"genre_scores_gemma":[0.98903847,0.0000048187626,0.0010049922,0.0035001282,0.00032664306,0.00006196577,0.000012299211,0.000055421548,0.0059952885],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9961773,0.00018696333,0.00021268216,0.00077646086,0.0014842692,0.001162328],"domain_scores_gemma":[0.9987808,0.00012843111,0.000066287,0.0006293235,0.00004648759,0.00034865882],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0002695241,0.00027706884,0.0002469047,0.0000023714222,0.0003928065,0.00014237562,0.0007585303,0.00008948432,0.006145863],"category_scores_gemma":[0.000028845321,0.00021148405,0.00007996034,0.0008018115,0.0019996073,0.00024016059,0.00033421777,0.00060120795,0.0071700756],"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":[0.00038525317,0.0005754355,0.20144138,0.000024306904,0.0001128637,0.00007158115,0.001552119,0.00016042593,0.5350661,0.00008079018,0.24948695,0.011042761],"study_design_scores_gemma":[0.002578024,0.002328966,0.9088553,0.00010850069,0.000036996844,0.000007215511,0.0012084763,0.0009858154,0.024323761,0.00061099284,0.05744348,0.0015124469],"about_ca_topic_score_codex":0.0075585744,"about_ca_topic_score_gemma":0.0001849962,"teacher_disagreement_score":0.707414,"about_ca_system_score_codex":0.00015162655,"about_ca_system_score_gemma":0.00002416863,"threshold_uncertainty_score":0.9990502},"labels":[],"label_agreement":null},{"id":"W2786386606","doi":"10.5194/acp-18-1419-2018","title":"The optical properties, physical properties and direct radiative forcing of urban columnar aerosols in the Yangtze River Delta, China","year":2018,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","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":"University of Toronto","funders":"Priority Academic Program Development of Jiangsu Higher Education Institutions; Nanjing University; National Natural Science Foundation of China; European Commission","keywords":"Aerosol; Radiative forcing; Environmental science; Radiative transfer; Sun photometer; Atmospheric sciences; Delta; Scattering; Forcing (mathematics); Yangtze river; Meteorology; Physics; China; Optics; Geography","score_opus":0.008890489381660581,"score_gpt":0.19340683981172463,"score_spread":0.18451635043006404,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2786386606","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":[0.9917517,0.00034569998,0.00011596678,0.000113785856,0.000017229531,0.00021435464,0.000002363183,0.000011963881,0.00742697],"genre_scores_gemma":[0.99812645,0.00008012522,0.00066688034,0.000063774016,0.00018142478,0.00003772467,9.750079e-7,0.0000134572565,0.0008292126],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9990109,0.00004374744,0.00016794015,0.00027771445,0.00022748533,0.0002721801],"domain_scores_gemma":[0.99953485,0.00007243635,0.000077587094,0.00024404605,0.000012123149,0.00005893807],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015037836,0.00018305589,0.00020548157,1.40494585e-8,0.00034952478,0.000050020648,0.00021598162,0.000052228857,0.00004775536],"category_scores_gemma":[0.000027834574,0.00010099714,0.00004604939,0.00018355105,0.0018483049,0.00012620898,0.00014342336,0.00016549455,0.0000056919635],"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":[0.0008845618,0.0015134264,0.26412722,0.00041931332,0.00026906404,0.000019014244,0.11015808,0.0021343848,0.22762288,0.0010958906,0.0038138845,0.38794228],"study_design_scores_gemma":[0.0029293792,0.0012479451,0.4144224,0.00037616852,0.00027343442,0.000048007703,0.008968656,0.33462894,0.21893705,0.004636098,0.0116439145,0.001888035],"about_ca_topic_score_codex":0.00044056633,"about_ca_topic_score_gemma":0.000018482471,"teacher_disagreement_score":0.38605425,"about_ca_system_score_codex":0.00003832092,"about_ca_system_score_gemma":0.000018237024,"threshold_uncertainty_score":0.6810157},"labels":[],"label_agreement":null},{"id":"W2786446497","doi":"","title":"Cloud and precipitation physics - Vancouver 2010 Olympics","year":2010,"lang":"en","type":"article","venue":"13th Conference on Cloud Physics/13th Conference on Atmospheric Radiation (28 June–2 July 2010)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Cloud computing; Meteorology; Precipitation; Geography; Computer science; Operating system","score_opus":0.01709568642291158,"score_gpt":0.23582695522879804,"score_spread":0.21873126880588645,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2786446497","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":[0.88864887,0.000067432455,0.027157322,0.001995432,0.019972429,0.0023500917,0.00016930742,0.0006561962,0.0589829],"genre_scores_gemma":[0.9730204,0.00038328613,0.0057259426,0.001410335,0.0018580884,0.00020451349,0.00010066355,0.00016188688,0.017134892],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99411875,0.0002685503,0.0010025266,0.0018578435,0.0014791534,0.001273179],"domain_scores_gemma":[0.99606186,0.00031463988,0.0010370138,0.0015737192,0.00025398986,0.0007587515],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0005300916,0.0011992183,0.000960864,0.000005321925,0.0007892461,0.0004830984,0.0010468253,0.0006462087,0.00500792],"category_scores_gemma":[0.00017599967,0.0011584992,0.00026616344,0.00087301683,0.001009054,0.00095721526,0.00030175818,0.0016369873,0.0032245917],"study_design_candidate":"design_other","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":[0.0009376368,0.0026737582,0.024363723,0.00013013175,0.00031040047,0.00003488662,0.0073890914,0.008943137,0.02337457,0.13624144,0.27645257,0.51914865],"study_design_scores_gemma":[0.011454605,0.004519833,0.18606867,0.0005144491,0.00064682483,0.000029891391,0.002128878,0.43869796,0.010516394,0.12723385,0.20902687,0.009161764],"about_ca_topic_score_codex":0.0008757514,"about_ca_topic_score_gemma":0.0008340201,"teacher_disagreement_score":0.5099869,"about_ca_system_score_codex":0.0003217296,"about_ca_system_score_gemma":0.0003888392,"threshold_uncertainty_score":0.9990865},"labels":[],"label_agreement":null},{"id":"W2786535480","doi":"10.1175/jas-d-17-0228.1","title":"Theoretical Analysis of Liquid–Ice Interaction in the Unsaturated Environment with Application to the Problem of Homogeneous Mixing","year":2018,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Biological and Environmental Research; Environment and Climate Change Canada; Israel Science Foundation","keywords":"Sublimation (psychology); Homogenization (climate); Liquid water content; Materials science; Mixing (physics); Sea ice growth processes; Condensation; Latent heat; Liquid water; Homogeneous; Mechanics; Thermodynamics; Atmospheric sciences; Geology; Physics; Arctic ice pack; Sea ice; Sea ice thickness; Climatology; Cloud computing","score_opus":0.006004459128972294,"score_gpt":0.23155914336228173,"score_spread":0.22555468423330943,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2786535480","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":[0.99190146,0.000042668977,0.0046240133,0.0022560346,0.000042825726,0.00020116709,5.3418165e-7,0.0000015497225,0.0009297574],"genre_scores_gemma":[0.99033564,0.000018040137,0.009303804,0.00027977175,0.00003364685,0.0000062005433,7.744836e-8,0.0000035846017,0.000019258683],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99837613,0.00018348906,0.00040008838,0.00015586085,0.00072543876,0.00015899152],"domain_scores_gemma":[0.998933,0.00014865331,0.0005896928,0.00026596757,0.000027764425,0.000034894194],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014062878,0.00009413979,0.0001866053,0.000001888586,0.00018763014,0.000025331448,0.0010511633,0.000027555536,0.00032357246],"category_scores_gemma":[0.000028288265,0.000035750163,0.0001015096,0.002184291,0.0013292104,0.000117161195,0.00012507684,0.00012379895,0.0000056672657],"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":[0.0003921183,0.00028108514,0.08645885,0.000004810638,0.00017936813,0.000002046762,0.0087680975,0.8636014,0.028915657,0.0012862744,0.0001919587,0.009918353],"study_design_scores_gemma":[0.0006901136,0.0066906293,0.62826556,0.00018187506,0.001469989,0.00019707419,0.022891492,0.31158382,0.01988415,0.0020242662,0.005615941,0.00050511764],"about_ca_topic_score_codex":0.00023969883,"about_ca_topic_score_gemma":0.0001605861,"teacher_disagreement_score":0.55201757,"about_ca_system_score_codex":0.00007855907,"about_ca_system_score_gemma":0.000026604272,"threshold_uncertainty_score":0.4897531},"labels":[],"label_agreement":null},{"id":"W2787039265","doi":"10.1175/bams-d-16-0047.1","title":"WIVERN: A New Satellite Concept to Provide Global In-Cloud Winds, Precipitation, and Cloud Properties","year":2018,"lang":"en","type":"article","venue":"Bulletin of the American Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada; Environment and Climate Change Canada","funders":"Natural Environment Research Council; Sight Research UK; Jet Propulsion Laboratory; UK Space Agency; National Aeronautics and Space Administration; California Institute of Technology; Centre for Earth Observation Instrumentation","keywords":"Environmental science; Radar; Meteorology; Snow; Wind shear; Satellite; Cloud cover; Wind speed; Cloud computing; Geology; Climatology; Geography; Computer science","score_opus":0.01026913816752138,"score_gpt":0.22339464526972477,"score_spread":0.2131255071022034,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2787039265","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":[0.9883232,0.00016683052,0.0004541906,0.008268128,0.00012328973,0.00041105942,0.000004445721,0.00002738857,0.0022214844],"genre_scores_gemma":[0.97463304,0.000057749585,0.016416194,0.0074811825,0.00019831848,0.00001575436,3.7715753e-7,0.0000085374195,0.001188819],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99850684,0.00016189815,0.00027342603,0.00040551167,0.00030968923,0.00034264568],"domain_scores_gemma":[0.9993029,0.00006291521,0.00020420659,0.00025645611,0.000017522478,0.00015597694],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00026914052,0.00017679542,0.00030077482,5.1297565e-7,0.00013652476,0.000021133495,0.00042957405,0.00006271634,0.0010885885],"category_scores_gemma":[0.00018462988,0.00010618352,0.0001273989,0.00036686385,0.0024046078,0.000021148107,0.00057469803,0.00012212609,0.00012056851],"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":[0.0006448788,0.00026963686,0.6799441,0.000014652884,0.000082638864,0.000002227919,0.007946144,0.00071845466,0.0075913705,0.00037625988,0.1838934,0.11851627],"study_design_scores_gemma":[0.00042761824,0.0011419553,0.7069941,0.000019564171,0.000025180181,0.000004792113,0.0015689861,0.00006972102,0.00089073385,0.00059052545,0.28800735,0.00025943606],"about_ca_topic_score_codex":0.0030350385,"about_ca_topic_score_gemma":0.000078346246,"teacher_disagreement_score":0.11825683,"about_ca_system_score_codex":0.00011991681,"about_ca_system_score_gemma":0.000022863012,"threshold_uncertainty_score":0.9998245},"labels":[],"label_agreement":null},{"id":"W2787179311","doi":"10.1364/ao.57.000969","title":"Scattering phase function depolarization parameter model and its application to water droplets sizing using off-axis lidar measurements at multiple angles","year":2018,"lang":"en","type":"article","venue":"Applied Optics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Defence Research and Development Canada","funders":"","keywords":"Lidar; Scattering; Optics; Monte Carlo method; Depolarization; Polarimetry; Forward scatter; Mie scattering; Phase (matter); Sizing; Light scattering; Depolarization ratio; Materials science; Physics; Remote sensing; Computational physics; Geology","score_opus":0.030473010297116673,"score_gpt":0.2471768789023789,"score_spread":0.21670386860526225,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2787179311","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":[0.7653811,0.000010620019,0.23375557,0.000021684937,0.000037919257,0.00033824318,0.0000021700541,0.000033690718,0.00041899612],"genre_scores_gemma":[0.9703798,0.0000041439616,0.029126437,0.00030812708,0.000061807346,0.00004098811,0.000015359634,0.000029261237,0.000034046636],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9988896,0.000009841868,0.0001957485,0.0003734374,0.00025305978,0.00027828114],"domain_scores_gemma":[0.9996076,0.000010492363,0.000060065027,0.00019264629,0.000017889935,0.00011128554],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012583927,0.000156017,0.000113034104,0.0000038105902,0.00034214713,0.000042794407,0.00008981716,0.0000782744,0.000042624986],"category_scores_gemma":[0.000008194115,0.00013746697,0.0000189809,0.000106633284,0.00006493506,0.00013844208,0.00024067421,0.000050643317,0.00017502804],"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":[0.000045206456,0.000049950206,0.004743458,0.000006185473,0.000007931214,1.5777059e-7,0.00043336008,0.021404263,0.95906556,0.000016697622,0.0000057698853,0.0142214745],"study_design_scores_gemma":[0.00057946495,0.00008120681,0.0029078887,0.0000073964566,0.00004588751,0.0000020810112,0.0000495048,0.7636933,0.23187922,0.000128291,0.0003602716,0.00026551154],"about_ca_topic_score_codex":0.000028527305,"about_ca_topic_score_gemma":0.000057943962,"teacher_disagreement_score":0.742289,"about_ca_system_score_codex":0.00016420778,"about_ca_system_score_gemma":0.0000034129273,"threshold_uncertainty_score":0.560574},"labels":[],"label_agreement":null},{"id":"W2788068890","doi":"10.5194/acp-18-13115-2018","title":"Simulated and observed horizontal inhomogeneities of optical thickness of Arctic stratus","year":2018,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"European Research Council; Deutsche Forschungsgemeinschaft; European Commission; Aurora Research Institute","keywords":"Atmospheric sciences; Arctic; Environmental science; Cloud top; Geology; Meteorology; Wind speed; Remote sensing; Cloud computing; Physics","score_opus":0.0098297796602262,"score_gpt":0.20832167417456515,"score_spread":0.19849189451433896,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2788068890","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":[0.99445784,0.000118792916,0.0003580213,0.000012377594,0.000020643107,0.00005524767,0.000004658828,0.000009689483,0.004962711],"genre_scores_gemma":[0.9938367,0.000040852938,0.005566771,0.000016755062,0.00006578984,0.0000015195777,0.000003681882,0.000010731526,0.00045721375],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99926496,0.000010297433,0.00019206047,0.0002171399,0.00015158212,0.00016394578],"domain_scores_gemma":[0.99957806,0.000052716674,0.00009003997,0.00017387286,0.000021722697,0.000083567684],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00005115338,0.00014111913,0.00021610521,8.965001e-9,0.00006577877,0.000009676492,0.00009710167,0.000087848966,0.0010739699],"category_scores_gemma":[0.000014036237,0.00012827577,0.000038016995,0.00013666588,0.0009860842,0.00007805889,0.00011002355,0.00008334438,0.0000037800773],"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":[0.00019808927,0.0003560746,0.3263261,0.00042654813,0.00011354506,0.000005425136,0.0014463379,0.0009652917,0.5827331,0.00049946987,0.00006233021,0.086867675],"study_design_scores_gemma":[0.0021923345,0.0009920975,0.2951553,0.00018490187,0.00024290496,0.000048775928,0.001793716,0.060088594,0.63138336,0.0061881463,0.0006783984,0.0010514519],"about_ca_topic_score_codex":0.00026553287,"about_ca_topic_score_gemma":0.000006006708,"teacher_disagreement_score":0.08581622,"about_ca_system_score_codex":0.000017403589,"about_ca_system_score_gemma":0.00001339914,"threshold_uncertainty_score":0.9998392},"labels":[],"label_agreement":null},{"id":"W2788336062","doi":"10.1002/2017jd027903","title":"Comprehensive Assessment of Global Surface Net Radiation Products and Uncertainty Analysis","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":71,"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":"Environment Canada; National Natural Science Foundation of China; Université Laval; U.S. Department of Energy; National Science Foundation","keywords":"Environmental science; Satellite; Anomaly (physics); Earth's energy budget; Earth system science; Cloud cover; Meteorology; Climatology; Land cover; Atmospheric sciences; Biogeochemical cycle; Aerosol; Earth observation; Cloud computing; Radiation; Geography; Land use; Geology; Computer science","score_opus":0.024462286713018776,"score_gpt":0.3478488497418528,"score_spread":0.32338656302883406,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2788336062","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":[0.9968305,0.00017863125,0.0008353808,0.0004732688,0.000060557715,0.00013346002,0.0000062753106,0.0000043186756,0.0014775795],"genre_scores_gemma":[0.9918111,0.00010225627,0.0076839123,0.000033071818,0.00019728884,0.000001059261,0.000001228462,0.0000065256736,0.00016357536],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99737614,0.0003073474,0.00039686446,0.0002532392,0.0013041958,0.00036222837],"domain_scores_gemma":[0.99861056,0.00023686081,0.00029238852,0.00023831532,0.00039580473,0.00022605257],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006494465,0.00012772979,0.0003958552,0.0000013403528,0.00015972544,0.000047290334,0.00030581153,0.000057203575,0.00060061034],"category_scores_gemma":[0.00017278858,0.00009462745,0.00012413842,0.0015810162,0.0010170611,0.0002069734,0.0002569687,0.00028206603,0.000021769752],"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":[0.00029532495,0.0004895214,0.9339118,0.000031070398,0.0006002927,0.000021807875,0.00026854972,0.018246412,0.014439289,0.00074297783,0.006923031,0.024029918],"study_design_scores_gemma":[0.00037167274,0.0012253842,0.9737521,0.000012841271,0.00009141714,0.000004323848,0.0003166746,0.019991724,0.00042535987,0.0011261002,0.0025875317,0.00009487254],"about_ca_topic_score_codex":0.0027130542,"about_ca_topic_score_gemma":0.00019034176,"teacher_disagreement_score":0.039840296,"about_ca_system_score_codex":0.0002833425,"about_ca_system_score_gemma":0.00012857009,"threshold_uncertainty_score":0.6576262},"labels":[],"label_agreement":null},{"id":"W2788726153","doi":"","title":"Heterogeneous Ice Nucleation of Dusts: Overview of Results from the INUIT Project (Invited Presentation)","year":2018,"lang":"en","type":"article","venue":"98th American Meteorological Society Annual Meeting","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Presentation (obstetrics); Nucleation; Geography; Chemistry; Medicine","score_opus":0.025779203928043937,"score_gpt":0.28205300645728376,"score_spread":0.2562738025292398,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2788726153","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":[0.99745286,0.00009492712,0.0003303869,0.00071130245,0.000045086545,0.00030857607,0.00016571693,0.000041114832,0.0008500326],"genre_scores_gemma":[0.98140186,0.00012714842,0.01619724,0.0020685345,0.00012811458,0.00001535318,0.000017535152,0.00001330665,0.00003089226],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9978872,0.0003413475,0.0005608922,0.00042054974,0.0004832552,0.00030675408],"domain_scores_gemma":[0.99829125,0.0005484343,0.00072510424,0.0003106484,0.000061240025,0.0000633021],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006411351,0.00017656582,0.0003356796,0.000001115422,0.0002077755,0.000014427077,0.00042334027,0.000092705755,0.00036043278],"category_scores_gemma":[0.00057008525,0.0001139035,0.00021202842,0.00069262687,0.0019074234,0.000115204646,0.00033640023,0.00016422376,0.000025085334],"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":[0.002703512,0.0014134508,0.29463118,0.000087925204,0.00085695414,0.000011359697,0.16711785,0.009884506,0.103941016,0.00023237338,0.03420763,0.38491222],"study_design_scores_gemma":[0.0021816832,0.0047968864,0.89023936,0.00015110835,0.00031849762,0.000008702705,0.05014499,0.018311977,0.014702733,0.0007942016,0.017387966,0.00096192374],"about_ca_topic_score_codex":0.011250505,"about_ca_topic_score_gemma":0.00021049763,"teacher_disagreement_score":0.5956081,"about_ca_system_score_codex":0.00007564348,"about_ca_system_score_gemma":0.000015008871,"threshold_uncertainty_score":0.9953337},"labels":[],"label_agreement":null},{"id":"W2789748533","doi":"10.1002/qj.3241","title":"Computation of domain‐average radiative flux profiles using Gaussian quadrature","year":2018,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":12,"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; Pacific Institute for Climate Solutions; University of Victoria","funders":"","keywords":"Radiative transfer; Radiative flux; Quadrature (astronomy); Physics; Gaussian quadrature; Gaussian; Computational physics; Statistical physics; Algorithm; Mathematics; Optics","score_opus":0.010301051111543143,"score_gpt":0.23821823612785323,"score_spread":0.2279171850163101,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2789748533","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":[0.968485,0.00007212526,0.029760594,0.00032973688,0.00024266339,0.00012372619,0.0000033827293,0.00000713443,0.00097562297],"genre_scores_gemma":[0.97066903,0.0000013828451,0.028738199,0.00027226578,0.0002202224,9.21778e-7,3.1144808e-7,0.000007947236,0.00008972313],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984614,0.0002656735,0.00043208798,0.00015764138,0.00044460013,0.00023854656],"domain_scores_gemma":[0.9990227,0.00006645072,0.00063674204,0.00012987602,0.000045722583,0.00009848971],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005614783,0.00015111011,0.00029308753,0.0000011533924,0.00025451893,0.000024711355,0.00038174356,0.00016292246,0.00077922875],"category_scores_gemma":[0.00002335593,0.00008071825,0.00041900983,0.0002080022,0.0007048298,0.00010783991,0.000066103516,0.00033072068,0.000012620099],"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":[0.001602941,0.0019308332,0.3721091,0.00011898262,0.0014986043,0.00006563639,0.08132441,0.13547881,0.26198304,0.0019575018,0.037029125,0.104901046],"study_design_scores_gemma":[0.0025010703,0.009362573,0.86089766,0.0001294539,0.0002576068,0.0001032576,0.0072512897,0.087242275,0.004401271,0.02589899,0.001304477,0.00065007777],"about_ca_topic_score_codex":0.00003631341,"about_ca_topic_score_gemma":0.0000033321935,"teacher_disagreement_score":0.48878857,"about_ca_system_score_codex":0.00012664491,"about_ca_system_score_gemma":0.000021718117,"threshold_uncertainty_score":0.8532008},"labels":[],"label_agreement":null},{"id":"W2790803537","doi":"10.1175/amsmonographs-d-16-0010.1","title":"Cirrus Clouds","year":2016,"lang":"en","type":"article","venue":"Meteorological Monographs","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":278,"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":"Leibniz-Institut für Troposphärenforschung; University of Illinois at Urbana-Champaign; Forschungszentrum Jülich; Environment and Climate Change Canada; Eidgenössische Technische Hochschule Zürich; Sight Research UK; Leibniz-Gemeinschaft; National Aeronautics and Space Administration; Natural Environment Research Council; Met Office; National Science Foundation","keywords":"Cirrus; Ice crystals; Ice nucleus; Atmospheric sciences; Environmental science; Troposphere; Nucleation; Radiative transfer; Cloud physics; Ice cloud; Climatology; Liquid water content; Climate model; Climate change; Geology; Meteorology; Physics; Cloud computing; Thermodynamics","score_opus":0.01177429406382572,"score_gpt":0.21492909967606175,"score_spread":0.20315480561223603,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2790803537","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":[0.9659767,0.00006253591,0.006639357,0.0009107429,0.0001311351,0.00010643689,0.0000037831794,0.0001457929,0.026023494],"genre_scores_gemma":[0.9936231,0.00006388777,0.004159533,0.0009869818,0.000038641887,0.00003210447,6.500755e-7,0.0000103631855,0.0010847654],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99872893,0.00007188832,0.00018588861,0.00037585208,0.00022395405,0.00041346072],"domain_scores_gemma":[0.9993863,0.00009267301,0.000053493983,0.0002896229,0.000003934573,0.00017397561],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00020672892,0.00015659879,0.00016806563,0.0000014874836,0.000111085064,0.000013484353,0.0003144801,0.00012342742,0.016636364],"category_scores_gemma":[0.000052278807,0.00007905413,0.00014246121,0.00027983336,0.00044706793,0.00009455695,0.00021195719,0.00007962203,0.0018485863],"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":[0.00006631404,0.00013299809,0.7839921,9.4763095e-7,0.000020210111,0.000026800657,0.000060766528,0.000013913153,0.021701239,0.0016558679,0.010635237,0.18169357],"study_design_scores_gemma":[0.0006660833,0.0005896461,0.84607434,0.0000049418804,0.000021322709,0.000013012863,0.000033974662,0.000048401806,0.001871253,0.02195058,0.12832531,0.00040110256],"about_ca_topic_score_codex":0.000029728657,"about_ca_topic_score_gemma":0.0000075123535,"teacher_disagreement_score":0.18129247,"about_ca_system_score_codex":0.00003351047,"about_ca_system_score_gemma":0.0000019849763,"threshold_uncertainty_score":0.9989286},"labels":[],"label_agreement":null},{"id":"W2791343169","doi":"","title":"Modeling of Ice Clouds Observed during ISDAC in Polluted and Pristine Air Masses","year":2013,"lang":"en","type":"article","venue":"93rd American Meteorological Society Annual Meeting","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec","funders":"","keywords":"Environmental science; Atmospheric sciences; Astrobiology; Meteorology; Geology; Geography; Physics","score_opus":0.011330158446960338,"score_gpt":0.21456358502988687,"score_spread":0.20323342658292654,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2791343169","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":[0.9971639,0.00011534791,0.0008333368,0.0005972943,0.000025230347,0.00024440276,0.000006931543,0.00007475434,0.000938799],"genre_scores_gemma":[0.95361465,0.00008816045,0.04554015,0.0005851258,0.000042093172,0.000035202276,0.0000021143712,0.00001900247,0.00007348199],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978884,0.00015771341,0.0005200375,0.00052652106,0.00032129596,0.00058603415],"domain_scores_gemma":[0.99917173,0.00020906956,0.00023463018,0.0001883614,0.000025756655,0.00017043769],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004523589,0.00025296424,0.00049382914,0.000002138215,0.00017985525,0.000018839317,0.00027169386,0.00012175446,0.00032013436],"category_scores_gemma":[0.00027367266,0.00020439582,0.00014685544,0.0005755641,0.0007699417,0.00022354418,0.00050279783,0.00031312913,0.000019180094],"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":[0.00009976433,0.0002997854,0.78079355,0.00006849636,0.00006543889,0.000009711836,0.0042528627,0.11636089,0.08579554,0.00006661573,0.00013098138,0.01205636],"study_design_scores_gemma":[0.00069692597,0.00041070505,0.7688874,0.000045799847,0.000028377755,0.000005544847,0.014728524,0.21347089,0.00078797335,0.00031975523,0.00010510597,0.0005129829],"about_ca_topic_score_codex":0.0054555624,"about_ca_topic_score_gemma":0.000058369205,"teacher_disagreement_score":0.09711001,"about_ca_system_score_codex":0.00009282156,"about_ca_system_score_gemma":0.000008275841,"threshold_uncertainty_score":0.83350194},"labels":[],"label_agreement":null},{"id":"W2795782986","doi":"10.5194/acp-2018-358","title":"Extreme levels of Canadian wildfire smoke in the stratosphere over central Europe – Part 2: Lidar study of depolarization and lidar ratios at 355, 532, and 1064 nm and of microphysical properties","year":2018,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","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":"Horizon 2020 Framework Programme; Russian Science Foundation","keywords":"Depolarization ratio; Stratosphere; Lidar; Troposphere; Atmospheric sciences; Wavelength; Environmental science; Extinction (optical mineralogy); Aerosol; Meteorology; Remote sensing; Geology; Physics; Optics","score_opus":0.02755129028475134,"score_gpt":0.20499629628663,"score_spread":0.17744500600187865,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2795782986","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":[0.9984267,0.00006236791,0.000008594268,0.00006151504,0.000013832869,0.00033464123,0.000010383712,0.0000024812928,0.0010795179],"genre_scores_gemma":[0.9995842,0.000028457916,0.00012762868,0.00006422188,0.0000145021295,0.000002734769,7.088714e-7,0.000007959526,0.00016956334],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991601,0.000075768614,0.00022630213,0.00019685729,0.00017361394,0.00016736714],"domain_scores_gemma":[0.9996748,0.000014605397,0.00008210102,0.00014325406,0.000009946861,0.00007531327],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000090994625,0.000107551066,0.00015964854,0.0000026755924,0.00008842045,0.000017904904,0.00009161219,0.000039227365,0.0002395765],"category_scores_gemma":[0.000011945627,0.00006930157,0.000010774663,0.00021399057,0.00046484554,0.00012177547,0.000089902,0.000049620034,7.72765e-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":[0.000024951254,0.000120416495,0.93638575,0.000011651954,0.0000097059365,0.0000018418341,0.0056093335,0.000008154636,0.0562625,0.000023224447,0.000052778356,0.0014897104],"study_design_scores_gemma":[0.00039374267,0.0004277106,0.9867075,0.000016779912,0.00001603131,0.0000025112242,0.0025037753,0.00023655969,0.009452397,0.000007907527,0.00014962543,0.00008546614],"about_ca_topic_score_codex":0.084398165,"about_ca_topic_score_gemma":0.24726292,"teacher_disagreement_score":0.16286476,"about_ca_system_score_codex":0.000019645639,"about_ca_system_score_gemma":0.00002554586,"threshold_uncertainty_score":0.9216989},"labels":[],"label_agreement":null},{"id":"W2795978424","doi":"10.1175/jcli-d-17-0082.1","title":"The June–September Low Cloud Cover in Western Central Africa: Mean Spatial Distribution and Diurnal Evolution, and Associated Atmospheric Dynamics","year":2018,"lang":"en","type":"article","venue":"Journal of Climate","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":41,"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":"Agence Universitaire de la Francophonie","keywords":"Climatology; Spatial distribution; Atmospheric dynamics; Cloud cover; Environmental science; Atmospheric circulation; Atmospheric sciences; Cloud computing; Meteorology; Atmosphere (unit); Geography; Geology; Remote sensing","score_opus":0.003856066751690349,"score_gpt":0.20398554665608126,"score_spread":0.20012947990439092,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2795978424","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":[0.9937414,0.00013289544,0.0045499313,0.0003056525,0.00047073993,0.000071318704,0.000015499727,0.0000055395094,0.00070700876],"genre_scores_gemma":[0.99886096,0.0004602193,0.00011365376,0.000034450557,0.00015357645,8.25504e-7,0.0000024547014,0.000009909581,0.00036394605],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986661,0.000091218106,0.00041439885,0.00012864046,0.0003167873,0.00038287454],"domain_scores_gemma":[0.9992892,0.00005981561,0.00040491988,0.00008389503,0.000032641507,0.00012951905],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00053031155,0.0001249447,0.00018982447,6.696068e-7,0.00026131744,0.000082908075,0.00012490367,0.00007629873,0.00013267109],"category_scores_gemma":[0.000054501157,0.00008421493,0.000048889422,0.00015182237,0.0003607399,0.00022400144,0.000126279,0.00020529078,0.000019664696],"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":[0.00014117334,0.00007810344,0.99468,0.0000040642485,0.000021314047,0.000013546147,0.00039051645,0.00026818734,0.00008559739,0.00006132781,0.0018011022,0.0024550648],"study_design_scores_gemma":[0.0007664728,0.00018532634,0.9713897,0.000040729647,0.000029768898,0.000051973682,0.00018275793,0.02371937,0.000008664134,0.00034605814,0.0031641503,0.00011503178],"about_ca_topic_score_codex":0.000092173024,"about_ca_topic_score_gemma":0.001915773,"teacher_disagreement_score":0.023451183,"about_ca_system_score_codex":0.00048032208,"about_ca_system_score_gemma":0.000018052751,"threshold_uncertainty_score":0.3434185},"labels":[],"label_agreement":null},{"id":"W2795996969","doi":"10.5194/acp-2018-357","title":"Extreme levels of Canadian wildfire smoke in the stratosphere over central Europe – Part 1: AERONET, MODIS and lidar observations","year":2018,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"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":"Horizon 2020 Framework Programme; National Oceanic and Atmospheric Administration; Russian Science Foundation; National Aeronautics and Space Administration","keywords":"AERONET; Stratosphere; Lidar; Aerosol; Environmental science; Atmospheric sciences; Noon; Tropopause; Smoke; Sun photometer; Troposphere; Climatology; Meteorology; Remote sensing; Physics; Geology","score_opus":0.0596441571280186,"score_gpt":0.2238676736255937,"score_spread":0.1642235164975751,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2795996969","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":[0.94787246,0.000025323401,0.000041073625,0.0006677671,0.000041939424,0.00012469082,0.000017095197,0.000006908292,0.051202755],"genre_scores_gemma":[0.9969197,0.00002408932,0.0007382562,0.00093593274,0.000038443435,0.0000039489955,0.0000020089767,0.000007867786,0.0013297526],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99916047,0.000036041572,0.00015969956,0.0001829394,0.0001661038,0.00029477067],"domain_scores_gemma":[0.9996089,0.000016714615,0.0000368595,0.00021109123,0.000004704732,0.00012178362],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00010376489,0.000097022705,0.00008599072,0.0000013967324,0.000118677424,0.000025195879,0.00019846912,0.000043377226,0.005886816],"category_scores_gemma":[0.000012474719,0.00006680768,0.000017976887,0.0004333711,0.00028516699,0.00014357931,0.000047006088,0.00007027484,0.000024607732],"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":[0.0000026178095,0.00002805597,0.9880057,0.0000014214705,0.000004021415,0.0000040016303,0.0009343905,0.000046041212,0.00048919354,0.00084166764,0.007585658,0.0020572082],"study_design_scores_gemma":[0.00012181801,0.000047246354,0.9729605,0.000005618514,0.000004807785,0.0000016274125,0.0004157672,0.0005704432,0.00007354654,0.00008022681,0.025629528,0.0000888811],"about_ca_topic_score_codex":0.26554385,"about_ca_topic_score_gemma":0.6262947,"teacher_disagreement_score":0.36075085,"about_ca_system_score_codex":0.000040433195,"about_ca_system_score_gemma":0.00003810084,"threshold_uncertainty_score":0.99502194},"labels":[],"label_agreement":null},{"id":"W2796527059","doi":"10.1051/epjconf/201817605018","title":"Lidar Ice nuclei estimates and how they relate with airborne in-situ measurements","year":2018,"lang":"en","type":"article","venue":"EPJ Web of Conferences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Lidar; Aerosol; Ice nucleus; Remote sensing; Backscatter (email); In situ; Effective radius; Particle (ecology); Environmental science; Extinction (optical mineralogy); RADIUS; Atmospheric sciences; Meteorology; Geology; Mineralogy; Physics; Nucleation; Astrophysics; Oceanography; Computer science","score_opus":0.01976065065407658,"score_gpt":0.22471983152146818,"score_spread":0.2049591808673916,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2796527059","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":[0.90413564,0.000056721285,0.00009112257,0.00046862583,0.000037180067,0.000093096714,8.788214e-7,0.00001618304,0.09510054],"genre_scores_gemma":[0.99702024,0.000036474612,0.002575548,0.00004917629,0.0000168987,0.000004691177,5.653938e-7,0.0000073365377,0.00028903774],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991685,0.00002644967,0.00011046366,0.00022827521,0.0002787941,0.00018753017],"domain_scores_gemma":[0.9996505,0.000028268061,0.000097546166,0.00014322814,0.000018534474,0.00006194943],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018814405,0.00012303263,0.00016711962,0.0000022855513,0.00006671986,0.000035451554,0.00017523236,0.000048475224,0.0006178883],"category_scores_gemma":[0.000024174264,0.000085036125,0.000014090974,0.00010072539,0.00051756186,0.00016475793,0.00008491772,0.000068772526,0.000045093533],"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":[0.000041911528,0.00004352413,0.9795926,0.0000072534926,0.000016986993,0.0000026782036,0.00064812094,0.000011655954,0.012074129,0.00044203748,0.00017128194,0.0069478075],"study_design_scores_gemma":[0.00051871967,0.00047384354,0.98441386,0.0000866081,0.000020813573,0.0000035341736,0.0005135061,0.00045327554,0.009761393,0.00087374577,0.002687364,0.0001933051],"about_ca_topic_score_codex":0.00041256272,"about_ca_topic_score_gemma":0.0025316605,"teacher_disagreement_score":0.0948115,"about_ca_system_score_codex":0.000017456574,"about_ca_system_score_gemma":0.00005093844,"threshold_uncertainty_score":0.6765443},"labels":[],"label_agreement":null},{"id":"W2796644677","doi":"10.1051/epjconf/201817601030","title":"Reduction of multiple scattering to second order scattering for determination of liquid-cloud microphysical properties","year":2018,"lang":"en","type":"article","venue":"EPJ Web of Conferences","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"Defence Research and Development Canada","funders":"","keywords":"Scattering; Optics; Azimuth; Polarization (electrochemistry); Physics; Monte Carlo method; Light scattering; Computational physics; Scattering length; Mie scattering; Forward scatter; Lidar; Chemistry; Mathematics","score_opus":0.02035789320786675,"score_gpt":0.24193124252608098,"score_spread":0.22157334931821424,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2796644677","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":[0.9952899,0.0000073490683,0.0030839767,0.00011468281,0.00016286611,0.00022596636,0.00000651145,0.000007715505,0.0011010248],"genre_scores_gemma":[0.99034995,0.000002173609,0.009324369,0.000016377599,0.00008489471,0.00002136745,0.0000012734073,0.0000073456918,0.00019224672],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9992761,0.000016222992,0.00026363012,0.00017592806,0.00013956377,0.0001285291],"domain_scores_gemma":[0.99958575,0.000024326286,0.00016123941,0.00012718409,0.00006782152,0.000033668395],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000096260344,0.000089201436,0.000182116,0.0000042888705,0.00004770846,0.000007842589,0.0001627477,0.00003765581,0.0006208735],"category_scores_gemma":[0.00004207185,0.00007441078,0.000040819934,0.000113757145,0.00043917037,0.00010374726,0.00008844126,0.000026237982,0.000010164851],"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":[0.00012918134,0.000044068172,0.0051824846,0.000048146536,0.0000057466955,3.44931e-8,0.0008633849,0.000040163864,0.98487705,0.000025815632,0.000060435937,0.008723489],"study_design_scores_gemma":[0.00019113897,0.00089111325,0.010116749,0.00009491572,0.000009856051,0.0000010291202,0.00047031257,0.0022724518,0.9851069,0.000051921932,0.0006898896,0.00010373686],"about_ca_topic_score_codex":0.00021085927,"about_ca_topic_score_gemma":0.00012613735,"teacher_disagreement_score":0.008619753,"about_ca_system_score_codex":0.000016989186,"about_ca_system_score_gemma":0.00004601413,"threshold_uncertainty_score":0.67981297},"labels":[],"label_agreement":null},{"id":"W2796781881","doi":"10.1016/j.atmosenv.2018.04.024","title":"An analysis of high fine aerosol loading episodes in north-central Spain in the summer 2013 - Impact of Canadian biomass burning episode and local emissions","year":2018,"lang":"en","type":"article","venue":"Atmospheric Environment","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"AERONET; Aerosol; Angstrom exponent; Environmental science; Sun photometer; Biomass burning; Atmospheric sciences; Particulates; Pollution; Population; Mineral dust; Range (aeronautics); Climatology; Physical geography; Meteorology; Geography; Geology; Chemistry; Ecology","score_opus":0.00848235774923794,"score_gpt":0.22546838041943323,"score_spread":0.2169860226701953,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2796781881","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":[0.9969163,0.00012176084,0.0023668613,0.00015940788,0.000019373167,0.00023188685,0.0000150192245,0.0000049824703,0.00016442343],"genre_scores_gemma":[0.9958903,0.00016510827,0.0037665796,0.000065900414,0.000015867645,0.000018042472,0.00002158657,0.000018450692,0.00003816182],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979527,0.00018037183,0.0004925671,0.00044004986,0.00032923144,0.00060509634],"domain_scores_gemma":[0.9989662,0.0000781355,0.0001881958,0.00047790734,0.0000029492862,0.00028656836],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003809816,0.00025356066,0.0004244035,0.0000067638325,0.00011149177,0.0000140490265,0.00035384228,0.00010603094,0.0037254756],"category_scores_gemma":[0.000014824218,0.00018622907,0.00012059254,0.0015124057,0.00072071335,0.00015082133,0.000121368634,0.00015148582,0.00001623261],"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":[0.000016043552,0.00014421246,0.8679311,0.0000028438578,0.00006055053,0.000010659406,0.0013938019,0.12669441,0.0011570454,0.0000040108184,0.00010550178,0.0024797563],"study_design_scores_gemma":[0.00029849773,0.00026872972,0.9280154,0.000010389515,0.00010281218,0.0000017745969,0.00049303373,0.07029763,0.00013265529,0.000008342752,0.00017750142,0.00019319747],"about_ca_topic_score_codex":0.67936987,"about_ca_topic_score_gemma":0.65984625,"teacher_disagreement_score":0.06008428,"about_ca_system_score_codex":0.0005343637,"about_ca_system_score_gemma":0.000022461814,"threshold_uncertainty_score":0.99718523},"labels":[],"label_agreement":null},{"id":"W2797014096","doi":"","title":"Assessing radar reflectivity retrieval methods with in-situ observations of cloud hydrometeor spectra","year":2006,"lang":"en","type":"article","venue":"12th Conference on Atmospheric Radiation/12th Conference on Cloud Physics (10-14 July 2006)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"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":"Remote sensing; Reflectivity; Radar; Spectral line; Environmental science; Cloud computing; Meteorology; In situ; Geology; Computer science; Geography; Physics; Astronomy; Optics; Telecommunications","score_opus":0.039837380493922436,"score_gpt":0.3037902825954026,"score_spread":0.26395290210148015,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2797014096","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":[0.7740247,0.00010180586,0.0668971,0.00057991745,0.0006622739,0.0011565911,0.00006014912,0.00023103404,0.1562864],"genre_scores_gemma":[0.93234116,0.0000732041,0.060475808,0.00026460737,0.00043827054,0.00007739183,0.000103944025,0.00011518828,0.0061104433],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99359363,0.00061561406,0.0013172522,0.0016399969,0.0016141136,0.0012194074],"domain_scores_gemma":[0.9961295,0.0005795171,0.0013141428,0.0013655324,0.00027113312,0.00034013437],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010596026,0.0010329306,0.0012816514,0.000011386411,0.0005448046,0.00037714784,0.0010119749,0.0004135945,0.004645367],"category_scores_gemma":[0.0001934105,0.0009662009,0.00027189896,0.0028687953,0.00080979173,0.001019953,0.00017294523,0.00094409497,0.00047074482],"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":[0.004293797,0.011789871,0.088489264,0.00040541106,0.0007125258,0.00020554378,0.004124704,0.1254721,0.3638959,0.17117018,0.030821681,0.19861905],"study_design_scores_gemma":[0.009976785,0.0053509674,0.6822615,0.0010325173,0.0005357625,0.000030732685,0.0012882125,0.11408129,0.0953341,0.066561736,0.017361602,0.0061847637],"about_ca_topic_score_codex":0.0012542742,"about_ca_topic_score_gemma":0.00037321178,"teacher_disagreement_score":0.5937723,"about_ca_system_score_codex":0.0009388778,"about_ca_system_score_gemma":0.00067023706,"threshold_uncertainty_score":0.99927884},"labels":[],"label_agreement":null},{"id":"W2797303068","doi":"10.1051/epjconf/201817601011","title":"First application of the optimal estimation method to retrieve temperature from pure rotational raman scatter lidar measurements","year":2018,"lang":"en","type":"article","venue":"EPJ Web of Conferences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency","keywords":"Lidar; Remote sensing; Backscatter (email); Calibration; Raman spectroscopy; Environmental science; Atmospheric temperature; Temperature measurement; Computational physics; Materials science; Computer science; Physics; Meteorology; Optics; Geology; Telecommunications; Thermodynamics","score_opus":0.015931400704965296,"score_gpt":0.2615248790616525,"score_spread":0.2455934783566872,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2797303068","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":[0.94010824,0.000011246051,0.05353398,0.0014970397,0.00008930444,0.00031003816,0.00002117933,0.000009817059,0.004419152],"genre_scores_gemma":[0.9423808,8.243125e-7,0.0572561,0.00016981279,0.000053815493,0.000022515938,0.000008745374,0.0000049240602,0.00010246541],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989131,0.000055908975,0.00022518937,0.00021617832,0.00048634651,0.000103292994],"domain_scores_gemma":[0.99944603,0.000045695688,0.00018128808,0.0002191111,0.00006445393,0.00004339152],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00023838374,0.00009840842,0.00013098771,0.0000021220021,0.000113780436,0.00002142276,0.00033405278,0.000071230854,0.0014778221],"category_scores_gemma":[0.00004876831,0.000067431116,0.00004168142,0.00023001582,0.00019943583,0.00009614181,0.00009418402,0.00006575828,0.000064625565],"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":[0.00012254382,0.00014906419,0.7492659,0.000016846818,0.00006800432,1.278647e-7,0.0022559508,0.008579106,0.20787634,0.0012526768,0.0037210814,0.026692366],"study_design_scores_gemma":[0.00026937271,0.0001447821,0.87247455,0.00005306877,0.000032052143,4.7983133e-7,0.00023979682,0.01562022,0.10614586,0.0013623695,0.0035031433,0.00015432319],"about_ca_topic_score_codex":0.00045708215,"about_ca_topic_score_gemma":0.00026186064,"teacher_disagreement_score":0.123208635,"about_ca_system_score_codex":0.0000305814,"about_ca_system_score_gemma":0.00007332249,"threshold_uncertainty_score":0.99943495},"labels":[],"label_agreement":null},{"id":"W2797862228","doi":"10.1051/epjconf/201817605051","title":"Retrievals of ice-water content from an airborne elastic lidar in tropical convective clouds","year":2018,"lang":"en","type":"article","venue":"EPJ Web of Conferences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; National Research Council Canada","funders":"Environment and Climate Change Canada","keywords":"Lidar; Mesoscale meteorology; Context (archaeology); Environmental science; Radiative transfer; Instrumentation (computer programming); Remote sensing; Meteorology; Ice water; Atmospheric sciences; Convection; Water content; Liquid water content; Geography; Geology; Cloud computing; Physics","score_opus":0.024597104425326644,"score_gpt":0.25041540058135053,"score_spread":0.2258182961560239,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2797862228","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":[0.98997,0.0000320971,0.0005386229,0.00016172942,0.00017568877,0.00014252593,0.000015223818,0.0000128787115,0.008951208],"genre_scores_gemma":[0.9992295,0.000014751762,0.0004352642,0.000076957884,0.000072213275,0.0000057425837,0.0000045892016,0.0000073797623,0.00015360306],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99862146,0.00010620176,0.0004019189,0.00030346794,0.00032572617,0.00024120354],"domain_scores_gemma":[0.99938893,0.00011324485,0.00013713051,0.0002248698,0.000043104978,0.00009273893],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014965021,0.00014326701,0.00035355164,0.000003440864,0.00003527037,0.000012571732,0.00030614444,0.000102917074,0.010207968],"category_scores_gemma":[0.00007630402,0.000098658595,0.000051694326,0.00012467106,0.0009984876,0.00012934502,0.0001175722,0.00010673584,0.00012176717],"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":[0.0002320479,0.00019343098,0.93879354,0.000005061404,0.000025187896,0.0000035019925,0.0015297502,0.000014665035,0.05612159,0.0011786707,0.00005404439,0.0018485228],"study_design_scores_gemma":[0.00063497777,0.0008958452,0.8860768,0.000036428664,0.000018684124,4.3083637e-7,0.00094369566,0.0010228669,0.10793075,0.001525003,0.0007695079,0.00014502207],"about_ca_topic_score_codex":0.0025229491,"about_ca_topic_score_gemma":0.0012849688,"teacher_disagreement_score":0.05271674,"about_ca_system_score_codex":0.000037480833,"about_ca_system_score_gemma":0.00008106429,"threshold_uncertainty_score":0.99069685},"labels":[],"label_agreement":null},{"id":"W2797924504","doi":"10.1051/epjconf/201817608015","title":"A Calibration of the MeteoSwiss RAman Lidar for Meteorological Observations (RALMO)Water Vapour Mixing Ratio Measurements using a Radiosonde Trajectory Method","year":2018,"lang":"en","type":"article","venue":"EPJ Web of Conferences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Canadian Space Agency","keywords":"Radiosonde; Lidar; Calibration; Environmental science; Trajectory; Meteorology; Remote sensing; Water vapor; Geology; Geography; Physics; Mathematics; Statistics","score_opus":0.10639278642188989,"score_gpt":0.3002412621392098,"score_spread":0.19384847571731995,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2797924504","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":[0.8580907,0.000023399369,0.14012955,0.0002745924,0.00016065784,0.00033828305,0.0000068457534,0.000012658234,0.0009633347],"genre_scores_gemma":[0.93847793,0.0000016428543,0.061199788,0.00010836117,0.000057833367,0.000023473678,0.0000029105177,0.00000789256,0.00012016551],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9985978,0.0002192676,0.00037223072,0.00023554084,0.0003597033,0.00021546296],"domain_scores_gemma":[0.9993707,0.00009870063,0.00021950294,0.00020672845,0.000059067846,0.0000452898],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000674942,0.0001360448,0.0002550929,0.000003652268,0.00020880817,0.000024594972,0.00033345743,0.000086470005,0.0011137964],"category_scores_gemma":[0.00008786011,0.000079401965,0.00012118835,0.00015824802,0.0003470305,0.0001789214,0.00008841257,0.000065483015,0.0000019592335],"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":[0.000046387144,0.00006974,0.1205037,0.000013664345,0.000057192094,1.1843256e-7,0.0007809436,0.0007552502,0.87562364,0.00088953483,0.00012327242,0.0011365337],"study_design_scores_gemma":[0.0008186221,0.00048245737,0.10304076,0.000046269353,0.00018917023,0.0000030287792,0.00064836175,0.10407516,0.7850839,0.0034163522,0.0019043012,0.00029160452],"about_ca_topic_score_codex":0.00040126883,"about_ca_topic_score_gemma":0.00026733315,"teacher_disagreement_score":0.10331991,"about_ca_system_score_codex":0.000038107548,"about_ca_system_score_gemma":0.0001334353,"threshold_uncertainty_score":0.9997993},"labels":[],"label_agreement":null},{"id":"W2798115674","doi":"","title":"NASA GPM/PMM Participation in the Canadian CloudSat/Calipso Validation Project (C3VP): Physical process studies in snow","year":2007,"lang":"en","type":"article","venue":"33rd Conference on Radar Meteorology (6–10 August 2007)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":16,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Environmental science; Snow; Climatology; Meteorology; Snowmelt; Remote sensing; Geography; Geology","score_opus":0.06377259766561688,"score_gpt":0.3633369514192327,"score_spread":0.29956435375361584,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2798115674","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":[0.9712433,0.000035926903,0.00015255866,0.0011310877,0.0002218865,0.00071611913,0.0000061005176,0.000034486708,0.02645854],"genre_scores_gemma":[0.99767405,0.000021371747,0.0002689058,0.0011100636,0.000120135475,0.00014655315,0.00002062917,0.0000208975,0.0006173728],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99713916,0.00037355936,0.00046454565,0.0006068801,0.0005155105,0.0009003528],"domain_scores_gemma":[0.9989792,0.00028241443,0.00017273765,0.00038144033,0.000044555298,0.00013966017],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014228086,0.00031608195,0.00038819652,0.000028959208,0.00024914576,0.00004512658,0.00050547224,0.00022018589,0.0011084424],"category_scores_gemma":[0.00028400673,0.00023854831,0.00006149652,0.00077669555,0.00063335366,0.00021182587,0.0000660811,0.000500224,0.00030487537],"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":[0.0017818842,0.0037968988,0.7436291,0.00015019294,0.00025954953,0.0010812578,0.08167966,0.010688899,0.0028423297,0.02997032,0.033624124,0.09049579],"study_design_scores_gemma":[0.0039123683,0.002456343,0.92290354,0.0001729673,0.00016890102,0.000055007367,0.01892652,0.010897345,0.004930133,0.015613204,0.018045787,0.0019178997],"about_ca_topic_score_codex":0.032227114,"about_ca_topic_score_gemma":0.2720769,"teacher_disagreement_score":0.2398498,"about_ca_system_score_codex":0.00054287614,"about_ca_system_score_gemma":0.00020713884,"threshold_uncertainty_score":0.9998047},"labels":[],"label_agreement":null},{"id":"W2799372251","doi":"","title":"Aerosol Impact on Warm Rain Initiation in Turbulent Clouds Using Direct Numerical Simulation (DNS)","year":2018,"lang":"en","type":"article","venue":"15th Conference on Cloud Physics/15th Conference on Atmospheric Radiation","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Aerosol; Meteorology; Atmospheric sciences; Turbulence; Environmental science; Direct numerical simulation; Mechanics; Geology; Physics; Reynolds number","score_opus":0.037058152419161966,"score_gpt":0.3075244044758644,"score_spread":0.2704662520567024,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2799372251","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":[0.9521361,0.000014972952,0.021565568,0.00045385803,0.00087960006,0.0012075726,0.000030484956,0.00022257777,0.023489257],"genre_scores_gemma":[0.99583745,0.000064083164,0.0014032007,0.0011696321,0.00095151697,0.00009866031,0.00009701995,0.00011210997,0.00026635223],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9942663,0.00057642354,0.0010122107,0.0015661804,0.0013965858,0.0011823104],"domain_scores_gemma":[0.99720246,0.00033199086,0.00085147546,0.0010030707,0.00017108317,0.00043995265],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000588822,0.0010153629,0.0009021574,0.000009079149,0.00051136856,0.0002921961,0.0006764888,0.00042498513,0.0047024647],"category_scores_gemma":[0.00017657332,0.00092252746,0.00029232333,0.0014090757,0.00044328542,0.0006282159,0.00013651155,0.0007541956,0.0016114706],"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":[0.0014596182,0.0016534195,0.026347855,0.000029146458,0.000094208175,0.000028542134,0.0035312292,0.86010057,0.004451167,0.0089215515,0.0009066869,0.09247602],"study_design_scores_gemma":[0.0017221966,0.0021498308,0.037546888,0.00020502576,0.00004699765,0.000003001234,0.00020591951,0.95249057,0.0017266505,0.002479048,0.0003269442,0.001096946],"about_ca_topic_score_codex":0.0012184163,"about_ca_topic_score_gemma":0.00006154519,"teacher_disagreement_score":0.09239,"about_ca_system_score_codex":0.0018995658,"about_ca_system_score_gemma":0.00032579605,"threshold_uncertainty_score":0.99932253},"labels":[],"label_agreement":null},{"id":"W2800013380","doi":"","title":"Dust Devils and Convective Vortices Detected by MSL","year":2017,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Vortex; Convection; Meteorology; Atmospheric sciences; Environmental science; Geology; Physics; Astrobiology","score_opus":0.00697403730857112,"score_gpt":0.22299709198145384,"score_spread":0.21602305467288271,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2800013380","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":[0.93705755,0.000040821804,0.00061719184,0.0002441603,0.000040481995,0.00007412156,0.0000014482864,0.000025193378,0.061899032],"genre_scores_gemma":[0.99277264,0.000018647042,0.0008440348,0.00017597321,0.000011816036,0.000005895749,3.5862757e-7,0.0000054840066,0.0061651245],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99949205,0.000009826222,0.000069068454,0.00018529921,0.00009758812,0.00014615907],"domain_scores_gemma":[0.9996281,0.000016529308,0.00006382576,0.00020784132,0.0000028975082,0.00008077647],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000053881635,0.000073612224,0.00007309313,1.5851619e-7,0.00033611286,0.000080507954,0.00016393076,0.000039639002,0.0035681725],"category_scores_gemma":[0.00003714886,0.000055563094,0.000013420751,0.000016918071,0.00029691617,0.00018429778,0.00018699671,0.000047437683,0.00020464079],"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":[0.0000087114,0.000025348249,0.9439026,0.0000019609968,0.000010578286,0.0000035244107,0.00016604758,0.0000021495252,0.029518006,0.000076978075,0.0066791684,0.019604929],"study_design_scores_gemma":[0.00019813942,0.00004485889,0.9857111,0.0000021414278,0.000008570823,0.0000023870011,0.00014577027,0.000600282,0.0066906046,0.00013674921,0.0063398313,0.00011957497],"about_ca_topic_score_codex":0.0012614583,"about_ca_topic_score_gemma":0.00041939033,"teacher_disagreement_score":0.055733908,"about_ca_system_score_codex":0.000021368138,"about_ca_system_score_gemma":0.000002343845,"threshold_uncertainty_score":0.9973427},"labels":[],"label_agreement":null},{"id":"W2800043999","doi":"","title":"Lidar data remote sensing of aerosols and anisotropic space-time generalizations of Corrsin-Obukov and Kolmogorov laws","year":2006,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"","keywords":"Lidar; Remote sensing; Mathematics; Space (punctuation); Computer science; Environmental science; Geography","score_opus":0.010186324608439332,"score_gpt":0.21195525184523134,"score_spread":0.20176892723679202,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2800043999","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":[0.9595012,0.00012532494,0.029156825,0.00018515484,0.000028063434,0.000118093565,0.000022672439,0.000018534232,0.010844132],"genre_scores_gemma":[0.8913443,0.00006362927,0.10481179,0.000061103856,0.000023403532,7.2852245e-8,0.000022073293,0.000011748039,0.0036618765],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9991652,0.000027729446,0.00022443576,0.0002718701,0.00016015899,0.0001506105],"domain_scores_gemma":[0.9994091,0.000027508886,0.00010756461,0.00039352546,0.000009276516,0.000053015625],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008605448,0.000106420106,0.00018595638,0.000001462943,0.00008105946,0.0000167919,0.0001234546,0.000052047162,0.00041680798],"category_scores_gemma":[0.000012812111,0.000092677685,0.000015422447,0.00013945687,0.0003233797,0.00013968548,0.00036122304,0.000037025406,0.000010334062],"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":[0.00003460535,0.000145886,0.30633688,0.000074214026,0.000040017294,0.000012850516,0.0003561053,0.0014724578,0.64372456,0.0019781955,0.020396667,0.025427537],"study_design_scores_gemma":[0.002343754,0.00050926086,0.5162606,0.00013214952,0.00025048567,0.00012430544,0.0006344612,0.41305488,0.046875484,0.0034837087,0.015178185,0.0011526975],"about_ca_topic_score_codex":0.0042308643,"about_ca_topic_score_gemma":0.00038217325,"teacher_disagreement_score":0.5968491,"about_ca_system_score_codex":0.000015805248,"about_ca_system_score_gemma":0.0000081406415,"threshold_uncertainty_score":0.63958293},"labels":[],"label_agreement":null},{"id":"W2800128569","doi":"10.1002/qj.3318","title":"Evaluation of a high‐resolution numerical weather prediction model's simulated clouds using observations from CloudSat, GOES‐13 and <i>in situ</i> aircraft","year":2018,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Aurora College; National Research Council Canada; McGill University; Environment and Climate Change Canada","funders":"Seventh Framework Programme; Federal Aviation Administration","keywords":"Graupel; Environmental science; Radar; Meteorology; Snow; Ice cloud; Mesoscale meteorology; Data assimilation; Climate model; Cloud computing; Remote sensing; Atmospheric sciences; Climate change; Geology; Computer science; Geography","score_opus":0.028977470393119747,"score_gpt":0.2510383725317462,"score_spread":0.22206090213862648,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2800128569","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":[0.96179324,0.00009329859,0.037301548,0.00030139153,0.00020451404,0.00019376574,0.000010338089,0.0000105395275,0.00009138188],"genre_scores_gemma":[0.9867033,0.0000056730964,0.0129024675,0.00020394578,0.00015391201,0.0000023639752,0.0000014454456,0.000010370624,0.000016530696],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.997606,0.00047163517,0.00059029396,0.00023227095,0.00086489297,0.00023493977],"domain_scores_gemma":[0.99902964,0.0001052921,0.0004630291,0.00019016839,0.000121217316,0.000090635775],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001638104,0.00016051435,0.00030087915,0.0000020560701,0.0001914574,0.000021149324,0.0002576581,0.00021631701,0.00027234879],"category_scores_gemma":[0.00008444121,0.00010249947,0.00022728505,0.00025477356,0.00039033996,0.00016589469,0.00007832692,0.0003058745,0.0000031593843],"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":[0.00019593284,0.00028129376,0.08707728,0.0000026017635,0.00010633441,7.715253e-7,0.001889531,0.87846166,0.026004866,0.000020960677,0.00037342508,0.0055853156],"study_design_scores_gemma":[0.00079154875,0.0005267162,0.25504965,0.000017174885,0.00020573806,0.0000024728795,0.00019389685,0.73663783,0.00013928162,0.0063367262,0.000018997283,0.00007998881],"about_ca_topic_score_codex":0.0005822845,"about_ca_topic_score_gemma":0.000053915235,"teacher_disagreement_score":0.16797237,"about_ca_system_score_codex":0.0003117857,"about_ca_system_score_gemma":0.00004050621,"threshold_uncertainty_score":0.4179807},"labels":[],"label_agreement":null},{"id":"W2800321911","doi":"10.1007/s00024-018-1882-1","title":"Fog Occurrence and Associated Meteorological Factors Over Kempegowda International Airport, India","year":2018,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":34,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ontario Tech University; Environment and Climate Change Canada","funders":"University Grants Commission; Jawaharlal Nehru University","keywords":"Monsoon; Environmental science; Climatology; Aviation; Meteorology; Wind speed; International airport; Geography; Geology; Engineering","score_opus":0.007326658051718786,"score_gpt":0.21193713488276944,"score_spread":0.20461047683105066,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2800321911","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":[0.9872466,0.000009621756,0.00011193065,0.000039597453,0.00010237271,0.00008634741,0.000023657365,0.000029433657,0.012350488],"genre_scores_gemma":[0.9991401,0.000018673361,0.00015620471,0.0003861324,0.000087979504,0.000008502254,0.000026817634,0.000005459192,0.00017017196],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992104,0.0000082866,0.00010742234,0.00028325326,0.00019640896,0.00019420328],"domain_scores_gemma":[0.99971193,0.000030139132,0.0000762526,0.000090405425,0.000005612137,0.00008565668],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00005943675,0.00013437861,0.00013032273,0.0000010179702,0.00013874337,0.00003897858,0.00012170014,0.00008357835,0.0006759007],"category_scores_gemma":[0.00000918447,0.00010481995,0.00002390919,0.00009816357,0.00032413652,0.000080920014,0.00021757906,0.00011449708,0.000057923156],"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":[0.000037980146,0.00017969347,0.9538217,0.000003782561,0.00006559876,0.0000041264734,0.001406455,0.000008054824,0.0056345006,0.0036708033,0.0057364563,0.029430814],"study_design_scores_gemma":[0.00027125166,0.00008370971,0.987923,0.000002222935,0.000018648681,8.774726e-7,0.0000740292,0.0001187463,0.0005019684,0.0051321415,0.005676596,0.00019678613],"about_ca_topic_score_codex":0.000048676735,"about_ca_topic_score_gemma":0.000016400489,"teacher_disagreement_score":0.03410129,"about_ca_system_score_codex":0.000023111792,"about_ca_system_score_gemma":0.0000044807366,"threshold_uncertainty_score":0.7400639},"labels":[],"label_agreement":null},{"id":"W2800587015","doi":"","title":"Quantifying the Oscillatory Evolution of Simulated Boundary-Layer Cloud Fields Using Gaussian Processes","year":2018,"lang":"en","type":"article","venue":"15th Conference on Cloud Physics/15th Conference on Atmospheric Radiation","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Cloud computing; Boundary layer; Statistical physics; Layer (electronics); Boundary (topology); Computer science; Geology; Mathematics; Physics; Mathematical analysis; Materials science; Mechanics","score_opus":0.05011014669452199,"score_gpt":0.29115899701836107,"score_spread":0.24104885032383908,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2800587015","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":[0.94422394,0.00009255275,0.036087494,0.00043733756,0.0013840981,0.00080276444,0.000020052672,0.00015035772,0.016801376],"genre_scores_gemma":[0.9969968,0.000104334984,0.00109209,0.00045055224,0.0008384816,0.000027905588,0.000015391352,0.00006764032,0.00040680668],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99592257,0.00030613222,0.0008152222,0.0010215286,0.0011155102,0.00081903324],"domain_scores_gemma":[0.99732864,0.00019601427,0.0009093837,0.0010173883,0.00031073566,0.00023786156],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000480846,0.00065832335,0.000620346,0.0000039794445,0.0009301124,0.00022683837,0.00086790574,0.00034170694,0.002533967],"category_scores_gemma":[0.00017910618,0.00052581256,0.00017673858,0.0013009266,0.0011661713,0.00047074066,0.00018321213,0.0005614229,0.00046190267],"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":[0.0023951603,0.0025599543,0.22474949,0.0006280249,0.00066491135,0.000028744938,0.023380917,0.27574056,0.048547264,0.24579877,0.0072313957,0.16827479],"study_design_scores_gemma":[0.0017707761,0.0019037274,0.051774863,0.0005027598,0.00018641718,0.000007367257,0.0019816572,0.9169868,0.006224228,0.014260725,0.0028180403,0.0015825917],"about_ca_topic_score_codex":0.0016746181,"about_ca_topic_score_gemma":0.00034868848,"teacher_disagreement_score":0.64124626,"about_ca_system_score_codex":0.00061709277,"about_ca_system_score_gemma":0.00067136536,"threshold_uncertainty_score":0.9997193},"labels":[],"label_agreement":null},{"id":"W2801005346","doi":"10.1029/2018jd028313","title":"Observations of the Interaction and Transport of Fine Mode Aerosols With Cloud and/or Fog in Northeast Asia From Aerosol Robotic Network and Satellite Remote Sensing","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"Université de Sherbrooke","funders":"Office of Naval Research; NASA Headquarters; Goddard Space Flight Center; Ministry of Science and ICT, South Korea; Ministry of Environment; Yonsei University; National Research Foundation; National Research Foundation of Korea; National Aeronautics and Space Administration","keywords":"AERONET; Aerosol; Environmental science; Moderate-resolution imaging spectroradiometer; Remote sensing; Satellite; Sun photometer; Meteorology; Cloud cover; Mode (computer interface); Cloud computing; Geography; Computer science","score_opus":0.03273416929208528,"score_gpt":0.29061685295778666,"score_spread":0.2578826836657014,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2801005346","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":[0.99739206,0.00013626798,0.001729399,0.0003995944,0.000044888293,0.00016962337,0.0000025196218,0.00000213537,0.00012353402],"genre_scores_gemma":[0.9845516,0.00018872671,0.01496003,0.000020435285,0.0001590748,3.7921848e-7,5.2214085e-7,0.00001273681,0.00010647549],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984188,0.00015447946,0.0004104969,0.00019116605,0.00055692706,0.00026809933],"domain_scores_gemma":[0.9990005,0.00034885664,0.00024609212,0.00017828985,0.00009672654,0.00012954432],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003439286,0.00012287479,0.00032305304,0.0000013722125,0.00013622963,0.000022075974,0.0001494601,0.00005643519,0.00005045535],"category_scores_gemma":[0.000074047384,0.00007178116,0.000046325702,0.00042060204,0.000971168,0.00021601243,0.00012009406,0.00039008976,9.769385e-7],"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":[0.003402488,0.00026953616,0.8612234,0.0000708615,0.00013280471,0.000041780262,0.0030622517,0.009794085,0.038429134,0.00010949064,0.00017543104,0.08328874],"study_design_scores_gemma":[0.00067415426,0.0010102553,0.9644978,0.0004755663,0.00003270832,0.000023057733,0.00075138576,0.02993834,0.0010516591,0.0013747457,0.0000701595,0.000100184145],"about_ca_topic_score_codex":0.005844693,"about_ca_topic_score_gemma":0.0109456275,"teacher_disagreement_score":0.10327438,"about_ca_system_score_codex":0.000044946457,"about_ca_system_score_gemma":0.000050520564,"threshold_uncertainty_score":0.88354665},"labels":[],"label_agreement":null},{"id":"W2801027424","doi":"10.5194/acp-18-13687-2018","title":"Surface roughness during depositional growth and sublimation of ice crystals","year":2018,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":25,"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":"University of Hertfordshire; Natural Environment Research Council; Sight Research UK","keywords":"Ice crystals; Sublimation (psychology); Supersaturation; Surface roughness; Cirrus; Surface finish; Materials science; Clear ice; Sea ice growth processes; Relative humidity; Crystal growth; Atmospheric sciences; Optics; Meteorology; Chemistry; Sea ice; Thermodynamics; Composite material; Geology; Cryosphere; Crystallography; Sea ice thickness; Physics; Antarctic sea ice","score_opus":0.004665314856593319,"score_gpt":0.19787361875788573,"score_spread":0.1932083039012924,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2801027424","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":[0.99113137,0.00005355562,0.0029961886,0.000036824036,0.00001426693,0.00004538469,0.0000040049,0.000016385657,0.0057019973],"genre_scores_gemma":[0.9884918,0.000044844066,0.010897725,0.000024106737,0.000099471436,0.0000023640896,0.000005472676,0.00000916237,0.00042505108],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99937534,0.000009130084,0.00012801113,0.00020822318,0.00014415853,0.00013516213],"domain_scores_gemma":[0.9997126,0.000027997417,0.00007637463,0.000106196894,0.000014151643,0.00006269796],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000037311136,0.00011081573,0.000116437055,5.624328e-9,0.00014085269,0.000018740862,0.000067840876,0.000049988164,0.00076898595],"category_scores_gemma":[0.0000068182276,0.00010855883,0.000021825279,0.0001353198,0.000325355,0.0001701107,0.00008406804,0.00005184314,0.0000067646306],"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":[0.000050100396,0.00007494235,0.17242971,0.00018338255,0.000023596867,0.0000020531818,0.0006070993,0.0005554313,0.8185025,0.00011952516,0.0000581311,0.00739352],"study_design_scores_gemma":[0.0008623969,0.0000839857,0.34572098,0.00005668278,0.000054006076,0.000028984185,0.0003152905,0.023165945,0.6265402,0.0024578597,0.00020451902,0.000509182],"about_ca_topic_score_codex":0.000119845194,"about_ca_topic_score_gemma":0.0000011342115,"teacher_disagreement_score":0.19196235,"about_ca_system_score_codex":0.000019192836,"about_ca_system_score_gemma":0.0000058984756,"threshold_uncertainty_score":0.8419857},"labels":[],"label_agreement":null},{"id":"W2801270613","doi":"10.5194/acp-2018-437","title":"Observations of the microphysical evolution of convective clouds in southwest United Kingdom","year":2018,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":5,"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":"Natural Environment Research Council; Sight Research UK; National Science Foundation","keywords":"Precipitation; Ice crystals; Atmospheric sciences; Convection; Environmental science; Entrainment (biomusicology); Wind shear; Radar; Climatology; Meteorology; Geology; Geography; Wind speed; Physics","score_opus":0.020064645442632822,"score_gpt":0.23062159201179422,"score_spread":0.2105569465691614,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2801270613","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":[0.99612445,0.0000012629795,0.0012982269,0.00010474864,0.000054790045,0.00009462216,0.0000034626432,0.000005594657,0.002312841],"genre_scores_gemma":[0.9986861,2.0224148e-7,0.0009704587,0.000062828476,0.000017152208,0.0000026755638,7.707867e-7,0.0000036965482,0.00025615544],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995068,0.0000344584,0.00014540607,0.00010119584,0.00012059024,0.00009158942],"domain_scores_gemma":[0.9997035,0.000025862948,0.000076672775,0.00015994968,0.00001762527,0.000016351896],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00005959974,0.000050964958,0.00007869324,0.0000010818534,0.000043671065,0.0000017661207,0.00014835573,0.000033894357,0.00041054745],"category_scores_gemma":[0.000022929353,0.000033536937,0.000034683526,0.0006027097,0.00056930527,0.00004045157,0.000109884044,0.0000495472,0.000027076445],"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":[0.0000096342,0.00008026522,0.838596,0.0000013942639,0.0000032329208,5.460994e-8,0.00052748783,0.00024518964,0.15476778,0.0056072623,0.00011749957,0.000044212913],"study_design_scores_gemma":[0.000159919,0.00004991943,0.983234,0.0000074696745,0.000004973328,2.1055861e-7,0.00033644907,0.0018398764,0.013537266,0.00059910957,0.00018932251,0.000041477164],"about_ca_topic_score_codex":0.011770942,"about_ca_topic_score_gemma":0.0014347957,"teacher_disagreement_score":0.14463802,"about_ca_system_score_codex":0.00008806841,"about_ca_system_score_gemma":0.00001298935,"threshold_uncertainty_score":0.99480975},"labels":[],"label_agreement":null},{"id":"W2803426336","doi":"10.1117/12.2303513","title":"Customized packaged bolometers in niche applications at INO","year":2018,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"Institut National d'Optique","funders":"","keywords":"Bolometer; Radiometer; Multispectral image; Terahertz radiation; Cardinal point; Microbolometer; Remote sensing; Broadband; Detector; Optics; Materials science; Optoelectronics; Physics; Geology","score_opus":0.005302365925945146,"score_gpt":0.21947441067323648,"score_spread":0.21417204474729132,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2803426336","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":[0.856985,0.0000062855893,0.004711128,0.00018882455,0.00002827137,0.00019865247,6.9796266e-7,0.000038331495,0.13784283],"genre_scores_gemma":[0.9809822,0.000006477756,0.0050204066,0.0007073337,0.000027172528,0.00007353719,0.0000016964169,0.0000074268064,0.013173782],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993397,0.000023470975,0.00012527753,0.00020967078,0.00011365992,0.00018823029],"domain_scores_gemma":[0.9996554,0.000024686411,0.000030455978,0.00022365974,0.000002304777,0.00006346132],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000118421485,0.00007277059,0.00008622017,9.0170107e-7,0.00009371357,0.000008226956,0.00015748876,0.000044166776,0.015484483],"category_scores_gemma":[0.000009115679,0.000057867575,0.000027278114,0.00025465788,0.0002237885,0.000055232642,0.000176863,0.0000522845,0.0051743365],"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":[0.000078336125,0.00016994629,0.8708331,0.000002818338,0.00000947594,0.0000025615063,0.0007490376,0.00006043115,0.06181494,0.00051126303,0.04412919,0.021638893],"study_design_scores_gemma":[0.0024183143,0.00014340924,0.70941514,0.0000046712807,0.000015414318,0.000006261287,0.00048766643,0.0018765244,0.013345466,0.0012457822,0.27050695,0.000534426],"about_ca_topic_score_codex":0.00029566744,"about_ca_topic_score_gemma":0.00068882096,"teacher_disagreement_score":0.22637777,"about_ca_system_score_codex":0.00014991839,"about_ca_system_score_gemma":0.000003361693,"threshold_uncertainty_score":0.9956002},"labels":[],"label_agreement":null},{"id":"W2803587973","doi":"","title":"Possible effects of aerosol-induced ice clouds","year":2001,"lang":"en","type":"article","venue":"The 81st AMS Annual Meeting","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Aerosol; Environmental science; Atmospheric sciences; Meteorology; Astrobiology; Geology; Geography; Physics","score_opus":0.007324967240667814,"score_gpt":0.22225069235023226,"score_spread":0.21492572510956445,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2803587973","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":[0.9497698,0.00010426206,0.00013354191,0.0002481777,0.00022723216,0.00021111456,0.000001475557,0.000051713247,0.04925271],"genre_scores_gemma":[0.99633074,0.000029617553,0.00051599555,0.00028366054,0.00014242827,0.000013816988,8.767799e-7,0.000023833743,0.0026590452],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99860376,0.00009809702,0.00026354348,0.00026131145,0.00035973848,0.00041353406],"domain_scores_gemma":[0.9991718,0.00019176606,0.00016758096,0.0003636624,0.000014788993,0.000090383815],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004138969,0.00017555116,0.00020430169,0.0000011895229,0.00027119534,0.000023606093,0.0004490665,0.00007563657,0.0004024247],"category_scores_gemma":[0.000118859185,0.00011874352,0.000086764034,0.00037100565,0.0001826231,0.00015261986,0.00031553712,0.00017017595,0.00041083398],"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":[0.00021240351,0.0005224247,0.18522586,0.00011609399,0.00010521599,0.000068284346,0.018624844,0.004757099,0.68838924,0.00058934075,0.006010462,0.09537874],"study_design_scores_gemma":[0.0043007312,0.002733988,0.30105284,0.0008484282,0.0003699408,0.00018347781,0.01411479,0.0075177564,0.6410853,0.0014071398,0.023686318,0.0026992615],"about_ca_topic_score_codex":0.0013201063,"about_ca_topic_score_gemma":0.000048852926,"teacher_disagreement_score":0.115826994,"about_ca_system_score_codex":0.000051161715,"about_ca_system_score_gemma":0.000008832376,"threshold_uncertainty_score":0.52805763},"labels":[],"label_agreement":null},{"id":"W2804620056","doi":"10.1007/s00024-018-1880-3","title":"A Meteorological Supersite for Aviation and Cold Weather Applications","year":2018,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":48,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ontario Tech University; Environment and Climate Change Canada","funders":"Environment and Climate Change Canada","keywords":"Environmental science; Ceilometer; Snow; Meteorology; Radiosonde; Wind speed; Weather Research and Forecasting Model; Surface weather observation; Visibility; Atmospheric sciences; Weather forecasting; Aerosol; Geography; Geology","score_opus":0.0062301316438588905,"score_gpt":0.2019711189705202,"score_spread":0.19574098732666131,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2804620056","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":[0.9593941,0.000029727731,0.032278504,0.00017994082,0.0000118707,0.00044751872,0.000007801343,0.000026207756,0.007624307],"genre_scores_gemma":[0.9948647,0.000013638252,0.0039382284,0.0004587273,0.00013120343,0.0001756122,0.0000049102755,0.000006504494,0.00040646628],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.99956274,0.000003086341,0.00005678236,0.00019535607,0.00006109542,0.00012093406],"domain_scores_gemma":[0.99982077,0.000020859647,0.000023903787,0.00008258068,0.000004401998,0.000047455458],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000041381983,0.00007210323,0.00007629774,4.437604e-7,0.0001792038,0.000018492025,0.000046587807,0.000046437945,0.00008814302],"category_scores_gemma":[9.692612e-7,0.000059033675,0.000015635449,0.00006661351,0.00017221377,0.00003596946,0.0000593907,0.000032678527,0.00006303739],"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":[0.00018229465,0.0003937709,0.03913481,0.000045400906,0.00007786443,4.96667e-7,0.003261261,0.000035164525,0.30964553,0.3694872,0.0074037462,0.2703325],"study_design_scores_gemma":[0.0025961415,0.0009829351,0.2432512,0.000007435361,0.0002817415,0.00000557148,0.001045283,0.0029326659,0.013278652,0.17006658,0.5643516,0.0012001626],"about_ca_topic_score_codex":0.000010185495,"about_ca_topic_score_gemma":0.000007766764,"teacher_disagreement_score":0.5569479,"about_ca_system_score_codex":0.000008581947,"about_ca_system_score_gemma":0.0000016893518,"threshold_uncertainty_score":0.24073234},"labels":[],"label_agreement":null},{"id":"W2804757460","doi":"10.1016/j.atmosres.2018.05.021","title":"Precipitation enhancement by cloud seeding using the shell structured TiO2/NaCl aerosol as revealed by new model for cloud seeding experiments","year":2018,"lang":"en","type":"article","venue":"Atmospheric Research","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":20,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Utah Agricultural Experiment Station","keywords":"Seeding; Aerosol; Precipitation; Environmental science; Cloud computing; Meteorology; Materials science; Relative humidity; Cloud seeding; Cloud condensation nuclei; Cloud physics; Atmospheric sciences; Computer science; Physics; Thermodynamics","score_opus":0.05982856271534696,"score_gpt":0.36195077003501797,"score_spread":0.302122207319671,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2804757460","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":[0.8421731,0.00039656664,0.15106496,0.00045348483,0.000574202,0.0016566414,0.0000110113315,0.00005721228,0.0036128461],"genre_scores_gemma":[0.9123159,0.00010495072,0.049025368,0.0003944643,0.0007985599,0.00020375938,0.000023650415,0.00009666534,0.037036695],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9954659,0.0001948533,0.0005559207,0.00094631664,0.0015535504,0.0012834594],"domain_scores_gemma":[0.9984638,0.00020971769,0.0002236702,0.00061579066,0.00012045139,0.00036654013],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013292907,0.00038131085,0.0003245204,0.0000011578093,0.0014728346,0.00026405777,0.00094160566,0.00021373405,0.0025878425],"category_scores_gemma":[0.00017670779,0.00030140375,0.00012401148,0.00076525874,0.0006269238,0.00042782785,0.0005731867,0.00040969177,0.00022594888],"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":[0.00024989963,0.00011350134,0.0020917167,0.000018604575,0.0000614943,9.2734e-7,0.0063060015,0.0030499867,0.675286,0.00009044985,0.30702642,0.0057050083],"study_design_scores_gemma":[0.001924984,0.001045412,0.00021648308,0.00008299257,0.000052733907,0.0000071686122,0.004234962,0.8511304,0.11530792,0.0023220766,0.022863809,0.0008110232],"about_ca_topic_score_codex":0.0017569528,"about_ca_topic_score_gemma":0.000035242527,"teacher_disagreement_score":0.84808046,"about_ca_system_score_codex":0.0009292313,"about_ca_system_score_gemma":0.00013025917,"threshold_uncertainty_score":0.9999438},"labels":[],"label_agreement":null},{"id":"W2805603117","doi":"","title":"First result from the NRC Airborne W and X-band (NAWX) radar system—Observations of winter clouds during the Canadian CloudSat and CALIPSO validation project","year":2007,"lang":"en","type":"article","venue":"33rd Conference on Radar Meteorology (6–10 August 2007)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Remote sensing; Environmental science; Radar; Meteorology; Lidar; Geology; Geography; Engineering; Telecommunications","score_opus":0.02171593980555261,"score_gpt":0.2313225385272748,"score_spread":0.2096065987217222,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2805603117","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":[0.98660034,0.00016418341,0.00029300814,0.0029045108,0.00026604024,0.0006172682,0.00010505058,0.000039605064,0.009009977],"genre_scores_gemma":[0.9971634,0.000068443354,0.0007533258,0.0005653092,0.00013181729,0.000023479355,0.000021079466,0.000025759628,0.0012473416],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99770916,0.00023248553,0.00050842937,0.0005527079,0.00044791354,0.0005493014],"domain_scores_gemma":[0.9984982,0.00039910083,0.00026723024,0.0005814218,0.00006709728,0.0001869343],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012337214,0.00030354824,0.0003413468,0.000011149561,0.0008631129,0.00007767557,0.00045941604,0.00025367216,0.0010279204],"category_scores_gemma":[0.00015604042,0.00019644405,0.00006081266,0.00028123122,0.0009939934,0.00013872911,0.0001320644,0.00036777233,0.000035685705],"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":[0.0032873363,0.00044785693,0.8197666,0.000278636,0.0009775544,0.00026862728,0.017389668,0.0010711905,0.03174154,0.029159905,0.080861665,0.014749452],"study_design_scores_gemma":[0.0012208789,0.00030350088,0.95745814,0.00008376554,0.0001398433,0.000046607423,0.0021117919,0.0006552248,0.0020782528,0.00035737484,0.035136748,0.00040787825],"about_ca_topic_score_codex":0.15339874,"about_ca_topic_score_gemma":0.2797841,"teacher_disagreement_score":0.13769157,"about_ca_system_score_codex":0.00032894738,"about_ca_system_score_gemma":0.00014163056,"threshold_uncertainty_score":0.99988526},"labels":[],"label_agreement":null},{"id":"W2806140496","doi":"","title":"The Fog Remote Sensing and Modeling (FRAM) field project and preliminary results","year":2006,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":14,"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","funders":"","keywords":"Meteorology; Winter storm; Aviation; Storm; Environmental science; Tornado; Geography; Climatology; Aeronautics; Engineering; Geology","score_opus":0.011628903840914457,"score_gpt":0.2268259432447294,"score_spread":0.21519703940381496,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2806140496","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":[0.9212401,0.00014793454,0.03330926,0.0011242254,0.000031146672,0.00014912523,5.365165e-7,0.00003233334,0.043965377],"genre_scores_gemma":[0.9792727,0.0000825986,0.01768832,0.00018954334,0.000034157274,2.4662577e-7,6.5097055e-7,0.0000059183353,0.0027258135],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9993992,0.000017551916,0.00012372115,0.00019968871,0.0001009636,0.0001589052],"domain_scores_gemma":[0.9997275,0.00008459223,0.000023859398,0.0001375214,0.000002527218,0.00002402696],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015734855,0.000074074516,0.000057173915,3.939507e-7,0.00027140483,0.000050497158,0.0000482673,0.000041419175,0.000010889373],"category_scores_gemma":[0.000024473296,0.00004576226,0.0000125676725,0.00005113543,0.0000627056,0.000060612896,0.00015294334,0.00006827942,0.000005034424],"study_design_candidate":"simulation_or_modeling","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":[0.00047382287,0.000021876924,0.0033099744,0.000010874251,0.0000102918875,0.000024676196,0.00067161897,0.008588947,0.0017175227,0.00015983137,0.019541325,0.96546924],"study_design_scores_gemma":[0.00020227638,0.00012793427,0.001758445,0.000008635195,0.000006325669,0.000022560072,0.0002602875,0.9930418,0.00022974896,0.0015087215,0.0027297735,0.00010346054],"about_ca_topic_score_codex":0.008998372,"about_ca_topic_score_gemma":0.00072085374,"teacher_disagreement_score":0.9844529,"about_ca_system_score_codex":0.000012542409,"about_ca_system_score_gemma":0.0000034041054,"threshold_uncertainty_score":0.9976008},"labels":[],"label_agreement":null},{"id":"W2807055455","doi":"10.5194/acp-18-13075-2018","title":"Springtime aerosol load as observed from ground-based and airborne lidars over northern Norway","year":2018,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":20,"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":"Grand Équipement National De Calcul Intensif; Centre National de la Recherche Scientifique; Langley Research Center; National Aeronautics and Space Administration","keywords":"Lidar; Aerosol; Environmental science; Troposphere; Atmospheric sciences; Nadir; Arctic; Meteorology; Remote sensing; Satellite; Geology; Geography; Physics","score_opus":0.007103831151355985,"score_gpt":0.19728561656013338,"score_spread":0.1901817854087774,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2807055455","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":[0.9872067,0.00013043036,0.00090613135,0.00006629597,0.00005305941,0.000103967424,0.0000098580085,0.00005443374,0.011469129],"genre_scores_gemma":[0.9882172,0.000029160337,0.0071637123,0.00045023172,0.00029482142,0.000012505376,0.000012532605,0.000036120768,0.003783727],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985389,0.000016436368,0.00019977303,0.000588795,0.0003118354,0.00034425352],"domain_scores_gemma":[0.99919504,0.00005472761,0.00010761977,0.00040291846,0.000020810985,0.00021889867],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00006410364,0.00030956854,0.00024797677,1.02299635e-8,0.00025109647,0.00007802069,0.00020595122,0.00013596864,0.008701532],"category_scores_gemma":[0.000012964592,0.00029538674,0.00006811834,0.00017213688,0.00060280424,0.0001616207,0.0001735318,0.00016758662,0.00040669995],"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":[0.00031383525,0.00046148774,0.52570266,0.000073400544,0.00014612007,0.00003425181,0.0012628079,0.00054004655,0.23065606,0.000022355045,0.0008366817,0.2399503],"study_design_scores_gemma":[0.005074689,0.0006794181,0.7053601,0.00016328535,0.00030918248,0.000018927085,0.0004377459,0.10319183,0.147555,0.0033044328,0.030992787,0.0029126198],"about_ca_topic_score_codex":0.0035575812,"about_ca_topic_score_gemma":0.00012503818,"teacher_disagreement_score":0.23703767,"about_ca_system_score_codex":0.00011985878,"about_ca_system_score_gemma":0.000038536862,"threshold_uncertainty_score":0.9999498},"labels":[],"label_agreement":null},{"id":"W2807811738","doi":"10.1007/s00024-019-02348-4","title":"Simultaneous Model Calibration and Source Inversion in Atmospheric Dispersion Models","year":2019,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University; Advanced Micro Devices (Canada)","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Inversion (geology); Atmospheric dispersion modeling; Inverse problem; Calibration; Dispersion (optics); Inverse; Point source; Gaussian process","score_opus":0.004003115118648089,"score_gpt":0.16948534224393497,"score_spread":0.16548222712528687,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2807811738","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":[0.98535097,0.000032411943,0.0114529,0.000053457345,0.000013588459,0.0002029628,0.0000010978059,0.000020598616,0.0028720289],"genre_scores_gemma":[0.99720967,0.000060015107,0.0015928637,0.00028827364,0.000014440307,0.0000067497544,0.000005591398,0.000013072658,0.00080930477],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99929655,0.000006577406,0.000096092255,0.0002863287,0.00014464797,0.00016980109],"domain_scores_gemma":[0.9997562,0.000022544335,0.00003751217,0.00011773582,0.0000017093519,0.00006430831],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00003375618,0.00012307033,0.00012633808,4.1501318e-7,0.000066986744,0.000023542905,0.00006127984,0.00007098568,0.0000489773],"category_scores_gemma":[9.585764e-7,0.0001088157,0.000015932812,0.00011726498,0.000059220663,0.00016241595,0.0001498596,0.000095463,0.00003406976],"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":[0.000037513426,0.000037664122,0.00786581,0.000014177881,0.0000024095584,8.7986956e-7,0.0012952811,0.95139945,0.009137895,0.001121707,0.00007515036,0.02901204],"study_design_scores_gemma":[0.00029401793,0.000026906744,0.0006604545,0.0000050630306,0.0000058813957,5.319748e-7,0.0002621283,0.9919605,0.0001235632,0.006388994,0.0001236224,0.00014829247],"about_ca_topic_score_codex":0.00011856735,"about_ca_topic_score_gemma":0.000017987142,"teacher_disagreement_score":0.040561073,"about_ca_system_score_codex":0.000029962555,"about_ca_system_score_gemma":0.0000042698043,"threshold_uncertainty_score":0.44373754},"labels":[],"label_agreement":null},{"id":"W2807857912","doi":"10.1039/c8cp02966k","title":"Measuring the size and complex refractive index of an aqueous aerosol particle using electromagnetic heating and cavity-enhanced Raman scattering","year":2018,"lang":"en","type":"article","venue":"Physical Chemistry Chemical Physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Aerosol; Refractive index; Raman scattering; RADIUS; Raman spectroscopy; Particle (ecology); Scattering; Optics; Materials science; Mie scattering; Rayleigh scattering; Particle size; Aqueous solution; Effective radius; Light scattering; Molecular physics; Chemistry; Physics; Meteorology; Physical chemistry","score_opus":0.016410163309787687,"score_gpt":0.24247609702495235,"score_spread":0.22606593371516465,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2807857912","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":[0.9988201,0.000008587119,0.0003726211,0.000036332207,0.0000063234766,0.00009609124,0.0000018870909,0.000026025971,0.0006320272],"genre_scores_gemma":[0.9987723,0.0000012392288,0.00086159795,0.00006604387,0.0002569472,0.000007929482,0.0000015331365,0.00002107466,0.000011334306],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.998856,0.000026948992,0.00017000888,0.0003775357,0.00024848813,0.00032098553],"domain_scores_gemma":[0.99934936,0.00012527076,0.00011443783,0.00025307425,0.000020152127,0.00013769642],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000064320084,0.00018945303,0.00023491826,1.7581533e-7,0.00019639461,0.00003588341,0.00017060015,0.000048131482,0.00004550367],"category_scores_gemma":[0.00004650506,0.00015705155,0.00004134644,0.00014446319,0.0009783417,0.00015388867,0.00027648435,0.00022937279,0.0000024885903],"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":[0.00003474177,0.00012247474,0.0006159102,0.00002437799,0.000010376694,4.9973914e-7,0.000601777,0.00009009909,0.99464786,0.0000029878804,0.0000019627803,0.0038469266],"study_design_scores_gemma":[0.00025873742,0.00006177598,0.0022169428,0.000017531751,0.00002666016,0.000005830386,0.00012982513,0.06805456,0.92799777,0.0010478898,0.0000016999985,0.00018081012],"about_ca_topic_score_codex":0.00017569376,"about_ca_topic_score_gemma":0.0000018148047,"teacher_disagreement_score":0.06796446,"about_ca_system_score_codex":0.000073200834,"about_ca_system_score_gemma":0.0000085646025,"threshold_uncertainty_score":0.6404376},"labels":[],"label_agreement":null},{"id":"W2808125284","doi":"10.3390/rs10060926","title":"Comparison of SNAP-Derived Sentinel-2A L2A Product to ESA Product over Europe","year":2018,"lang":"en","type":"article","venue":"Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"Natural Resources Canada; Canadian Space Agency; European Space Agency","keywords":"Environmental science; AERONET; Radiance; Remote sensing; Atmospheric correction; Aerosol; Sky; Satellite; Meteorology; Geology; Geography; Physics","score_opus":0.020557391156777502,"score_gpt":0.2844733943768892,"score_spread":0.26391600322011166,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2808125284","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":[0.98198915,0.00003642305,0.0036574472,0.00054347195,0.00029434328,0.00026263625,7.7129147e-7,0.000059508442,0.013156277],"genre_scores_gemma":[0.9703488,0.000003918638,0.02756395,0.00029927507,0.00036864605,1.5760444e-8,0.0000018996612,0.00003316113,0.0013803325],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99832493,0.00006974273,0.00032556162,0.0005402671,0.00036695268,0.0003725431],"domain_scores_gemma":[0.9991159,0.00001571106,0.00015730214,0.00054222107,0.000046655427,0.00012223785],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021285779,0.00018870771,0.00028374506,0.0000031653897,0.00015447206,0.000027377624,0.00016007951,0.000033694658,0.00034309513],"category_scores_gemma":[0.00013455376,0.00016910868,0.000053131072,0.00050903624,0.0002637146,0.00008528947,0.00028633105,0.00011820375,0.000533718],"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":[0.000036693815,0.00004666885,0.01405147,0.000014055183,0.000014095283,0.000007081396,0.0013620333,0.0005288701,0.8704688,0.0000028872262,0.006618269,0.10684908],"study_design_scores_gemma":[0.00047604533,0.00026174614,0.19278553,0.00014560354,0.0000623646,0.000044570446,0.00025295472,0.0747747,0.66194737,0.00006536038,0.06840644,0.00077729434],"about_ca_topic_score_codex":0.0003880968,"about_ca_topic_score_gemma":0.000059844504,"teacher_disagreement_score":0.20852141,"about_ca_system_score_codex":0.00006188141,"about_ca_system_score_gemma":0.00001509748,"threshold_uncertainty_score":0.6896052},"labels":[],"label_agreement":null},{"id":"W2808371772","doi":"10.1038/s41598-018-27744-z","title":"Aerosol optical, microphysical, chemical and radiative properties of high aerosol load cases over the Arctic based on AERONET measurements","year":2018,"lang":"en","type":"article","venue":"Scientific Reports","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":42,"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 Oceanic and Atmospheric Administration; Chinese Academy of Sciences; National Natural Science Foundation of China","keywords":"Aerosol; AERONET; Radiative forcing; Atmospheric sciences; Radiative transfer; Environmental science; Arctic; Albedo (alchemy); Angstrom exponent; Atmosphere (unit); Atmospheric radiative transfer codes; Extinction (optical mineralogy); Meteorology; Physics; Geology; Optics","score_opus":0.020212687936483568,"score_gpt":0.22164102549380343,"score_spread":0.20142833755731987,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2808371772","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":[0.9977384,0.000042111722,0.000063965075,0.00017231658,0.0007888635,0.0004215134,0.0000021671144,0.000023452185,0.0007471604],"genre_scores_gemma":[0.9984777,0.0000014143246,0.0007202517,0.00019724126,0.000075067815,0.00003417715,0.0000030415642,0.000018195458,0.00047294013],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9971939,0.000063531166,0.00041688615,0.00079934596,0.0011420832,0.00038430805],"domain_scores_gemma":[0.99862427,0.000052716005,0.00027120567,0.00081960874,0.0000800046,0.00015219818],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0006319698,0.00022597912,0.0002510762,0.0000031594484,0.0004349306,0.00015050729,0.0002235334,0.000069602764,0.00065803103],"category_scores_gemma":[0.000279446,0.00013928351,0.000079741774,0.00032344315,0.003827648,0.00013648233,0.00020634918,0.00013138984,0.000077392855],"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":[0.00008841994,0.0003636834,0.010249637,0.000022423861,0.00002273004,0.000038937185,0.00047146794,0.00028697017,0.9808661,0.0000075343696,0.00682148,0.00076066464],"study_design_scores_gemma":[0.00034540807,0.00030846443,0.006431383,0.00009629849,0.000052601543,0.00004890129,0.00008933569,0.0011849795,0.9903586,0.00013896194,0.0006526396,0.00029244975],"about_ca_topic_score_codex":0.0005715394,"about_ca_topic_score_gemma":0.000052832573,"teacher_disagreement_score":0.009492526,"about_ca_system_score_codex":0.00018292568,"about_ca_system_score_gemma":0.00008506481,"threshold_uncertainty_score":0.99888337},"labels":[],"label_agreement":null},{"id":"W2811232680","doi":"10.3390/atmos9070246","title":"Simulation of Severe Dust Events over Egypt Using Tuned Dust Schemes in Weather Research Forecast (WRF-Chem)","year":2018,"lang":"en","type":"article","venue":"Atmosphere","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":33,"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":"AERONET; Weather Research and Forecasting Model; Environmental science; Aerosol; Meteorology; Dust storm; Moderate-resolution imaging spectroradiometer; Storm; Atmospheric sciences; Satellite; Climatology; Geography; Physics; Geology","score_opus":0.04854366574948969,"score_gpt":0.3311871194555032,"score_spread":0.2826434537060135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2811232680","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":[0.9881413,0.000059426005,0.00082212297,0.000047602283,0.000092649985,0.00031015833,0.0000035755888,0.000021937716,0.010501219],"genre_scores_gemma":[0.9905067,0.0000068912323,0.005846249,0.000058559755,0.00011341255,0.000009126689,0.0000028414418,0.000039187893,0.0034170153],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979438,0.00010497251,0.0003500059,0.0004262979,0.00065403135,0.0005208839],"domain_scores_gemma":[0.9991916,0.000114635244,0.00012628581,0.00041080633,0.000051340805,0.00010533564],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00046680708,0.00019172617,0.00023039691,9.924947e-7,0.00018479265,0.000019844367,0.00030415066,0.00019742534,0.0131842205],"category_scores_gemma":[0.00010520235,0.00017571953,0.0000711615,0.00073293055,0.00039522117,0.0003064008,0.0003424049,0.00024091873,0.00030036495],"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":[0.00011940062,0.00021249942,0.9144611,0.000020546326,0.000022062677,0.000008097216,0.00092731445,0.06765526,0.0067095277,0.000057241567,0.0008011772,0.0090057915],"study_design_scores_gemma":[0.0020416526,0.00039099707,0.54289466,0.00023270128,0.00002721007,0.000006817343,0.0016562976,0.4321425,0.0044722543,0.0013666746,0.014113137,0.00065510924],"about_ca_topic_score_codex":0.0020552594,"about_ca_topic_score_gemma":0.00062769616,"teacher_disagreement_score":0.3715664,"about_ca_system_score_codex":0.0003135004,"about_ca_system_score_gemma":0.00003852218,"threshold_uncertainty_score":0.98771787},"labels":[],"label_agreement":null},{"id":"W2811433246","doi":"","title":"Mixed Phase Clouds Observed During the Canadian CloudSat/CALIPSO Validation Project","year":2007,"lang":"en","type":"article","venue":"33rd Conference on Radar Meteorology (6–10 August 2007)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Phase (matter); Environmental science; Remote sensing; Geography; Physics","score_opus":0.05001388961158969,"score_gpt":0.2756602316285194,"score_spread":0.22564634201692968,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2811433246","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":[0.9261758,0.000047562015,0.0006884059,0.0012242001,0.00079121103,0.00072431413,0.000030450185,0.00012764373,0.070190445],"genre_scores_gemma":[0.9862111,0.000021626047,0.0013847539,0.0012435472,0.0002482946,0.000051191993,0.000047519974,0.000051785366,0.01074018],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9963107,0.00033179452,0.0006020132,0.00082152215,0.0006120541,0.0013219286],"domain_scores_gemma":[0.99821275,0.00016145418,0.00027698366,0.0008494616,0.00005426162,0.00044507487],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.001467526,0.0004743595,0.00041577342,0.000019335237,0.0009808674,0.00011194439,0.00091401726,0.00041441337,0.01978796],"category_scores_gemma":[0.00014113751,0.00036764404,0.00015742435,0.000573551,0.0007536399,0.00019315285,0.00018010092,0.00063264434,0.0014022987],"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":[0.007687951,0.00400955,0.275546,0.00018343367,0.0012844226,0.0026185852,0.00789828,0.0033634799,0.13014255,0.06876052,0.31890506,0.17960015],"study_design_scores_gemma":[0.00982202,0.0028666637,0.5057347,0.000068256355,0.0003544317,0.00027278665,0.002434718,0.003562478,0.033991937,0.0030160313,0.43489262,0.00298336],"about_ca_topic_score_codex":0.06353798,"about_ca_topic_score_gemma":0.13470086,"teacher_disagreement_score":0.23018867,"about_ca_system_score_codex":0.00068788254,"about_ca_system_score_gemma":0.00028726846,"threshold_uncertainty_score":0.9998776},"labels":[],"label_agreement":null},{"id":"W2812803172","doi":"10.5194/acp-2018-655","title":"A study of long-range transported smoke aerosols in the Upper Troposphere/Lower Stratosphere","year":2018,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":14,"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; Troposphere; Depolarization ratio; Lidar; Aerosol; Atmospheric sciences; Environmental science; Smoke; Range (aeronautics); Tropopause; Chemistry; Materials science; Remote sensing; Geology","score_opus":0.015963127488875684,"score_gpt":0.24975031217393576,"score_spread":0.23378718468506007,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2812803172","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":[0.95843416,0.00001989878,0.00042580167,0.00010423749,0.00007845087,0.0006320534,0.0000017384737,0.000027211492,0.040276438],"genre_scores_gemma":[0.99809736,0.00000526519,0.00046163093,0.00035311913,0.000037342466,0.000035496454,0.0000010303024,0.000017834362,0.000990922],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983249,0.000084775675,0.00037315316,0.00035244095,0.0004938662,0.00037089677],"domain_scores_gemma":[0.999301,0.000030781026,0.000081315586,0.00050749216,0.000011526988,0.00006785304],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00027311727,0.0001946766,0.00022673687,6.893747e-7,0.000099294855,0.00002160808,0.0004718805,0.00008103558,0.028138535],"category_scores_gemma":[0.0000061840815,0.00011894132,0.00007706204,0.00047387514,0.00033927712,0.0001418368,0.000051924413,0.00015144277,0.00018656759],"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":[0.000059733073,0.0012320044,0.9925335,0.0000025185036,0.000014976424,0.000036609257,0.0037691651,0.000047519312,0.00014989616,0.00006991722,0.0006153349,0.0014687972],"study_design_scores_gemma":[0.0009991603,0.0012050597,0.98773426,0.0000069195135,0.000024526167,0.000004551674,0.009331661,0.000100385485,0.00012812112,0.00005308994,0.00023942674,0.00017285318],"about_ca_topic_score_codex":0.0041419803,"about_ca_topic_score_gemma":0.019453898,"teacher_disagreement_score":0.03966319,"about_ca_system_score_codex":0.000041305757,"about_ca_system_score_gemma":0.0000124233375,"threshold_uncertainty_score":0.99843854},"labels":[],"label_agreement":null},{"id":"W2883163649","doi":"10.1175/bams-d-17-0180.1","title":"Cloud System Evolution in the Trades (CSET): Following the Evolution of Boundary Layer Cloud Systems with the NSF–NCAR GV","year":2018,"lang":"en","type":"article","venue":"Bulletin of the American Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":92,"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":"National Aeronautics and Space Administration; U.S. Department of Energy","keywords":"Drizzle; Aerosol; Environmental science; Boundary layer; Cloud computing; Meteorology; Lidar; Precipitation; Ceilometer; Mesoscale meteorology; Liquid water path; Atmospheric research; Atmospheric sciences; Climatology; Geology; Geography; Remote sensing; Aerospace engineering; Computer science","score_opus":0.0074049078390451845,"score_gpt":0.20861909218601585,"score_spread":0.20121418434697066,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2883163649","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":[0.98748595,0.0004563388,0.0026495724,0.0066382117,0.0002541757,0.0006953991,0.000008363713,0.000033041302,0.001778978],"genre_scores_gemma":[0.99786156,0.000015218516,0.00054496253,0.0010964902,0.00023372965,0.00007444472,6.0530516e-7,0.000015901278,0.00015709993],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99672145,0.0011980037,0.00043736637,0.00036548186,0.0008354795,0.0004422334],"domain_scores_gemma":[0.99809825,0.00048889214,0.0006185619,0.0007262874,0.000024068322,0.00004392483],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0023888603,0.00024272014,0.00042576835,0.0000012983318,0.00070930214,0.00003907588,0.0013623988,0.00009965987,0.0001018095],"category_scores_gemma":[0.00007627142,0.00008790522,0.0004556902,0.0007035955,0.0042894343,0.000027027672,0.00031920898,0.0003893515,0.00003350315],"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":[0.0021193284,0.0014798176,0.6387058,0.00026288503,0.0013710874,0.000018914972,0.025429988,0.022163207,0.036291324,0.019583387,0.24854913,0.0040251305],"study_design_scores_gemma":[0.0012196584,0.0030279912,0.78513336,0.00016914561,0.000505951,0.00008005841,0.12564477,0.005489905,0.0003218216,0.00045954826,0.077300236,0.0006475271],"about_ca_topic_score_codex":0.006414422,"about_ca_topic_score_gemma":0.00007926555,"teacher_disagreement_score":0.1712489,"about_ca_system_score_codex":0.0004289006,"about_ca_system_score_gemma":0.00003481894,"threshold_uncertainty_score":0.9984203},"labels":[],"label_agreement":null},{"id":"W2885854886","doi":"10.22323/1.301.0445","title":"Results of the EUSO-Balloon flight","year":2017,"lang":"en","type":"preprint","venue":"Proceedings of 35th International Cosmic Ray Conference — PoS(ICRC2017)","topic":"Atmospheric aerosols and clouds","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":"Balloon; Altitude (triangle); Laser; Remote sensing; Environmental science; Physics; Intensity (physics); International Space Station; Range (aeronautics); Wavelength; Optics; Aerospace engineering; Astronomy; Engineering; Geography; Mathematics","score_opus":0.02309287590803351,"score_gpt":0.2576109938781339,"score_spread":0.23451811797010041,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2885854886","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":[0.77608234,0.00008005961,0.00014865624,0.0029288435,0.0016941469,0.000605844,0.00031257299,0.000045284694,0.21810228],"genre_scores_gemma":[0.9858625,0.00030601776,0.001682909,0.0001377171,0.000207023,0.000047013662,0.000030324443,0.000036758294,0.01168972],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99633366,0.000016919117,0.0010166643,0.0008842467,0.0013588206,0.00038969476],"domain_scores_gemma":[0.9961857,0.00005416835,0.0025396068,0.00060397526,0.00048399964,0.00013253462],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006409274,0.0004823955,0.0006030737,0.000013267287,0.00020146872,0.0001994933,0.004574792,0.0003622721,0.000920417],"category_scores_gemma":[0.0005754743,0.00036661213,0.00035060753,0.0000942955,0.00093934214,0.00032835294,0.0034906408,0.000770568,0.00009202781],"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":[0.0026021325,0.001860562,0.33704048,0.001178139,0.0016119203,0.00001637797,0.011012615,0.0022670794,0.3375834,0.037091024,0.22453374,0.04320255],"study_design_scores_gemma":[0.0062632672,0.00077118416,0.5163471,0.0053516165,0.0006265642,0.00006704794,0.0012353222,0.020581314,0.19477352,0.08319852,0.16720283,0.003581677],"about_ca_topic_score_codex":0.0012337735,"about_ca_topic_score_gemma":0.00004768331,"teacher_disagreement_score":0.2097802,"about_ca_system_score_codex":0.0002626555,"about_ca_system_score_gemma":0.00017567583,"threshold_uncertainty_score":0.99999285},"labels":[],"label_agreement":null},{"id":"W2886248597","doi":"10.1175/bams-d-17-0175.1","title":"Overview of the NOAA/ESRL Federated Aerosol Network","year":2018,"lang":"en","type":"article","venue":"Bulletin of the American Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":112,"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":"Aerosol; Meteorology; Environmental science; Radiative forcing; Atmosphere (unit); Geography","score_opus":0.016905535134140445,"score_gpt":0.2415026810630417,"score_spread":0.22459714592890126,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2886248597","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":[0.98765033,0.0001434283,0.00025130252,0.0050907633,0.00014917598,0.00024981395,0.000004529619,0.000025308887,0.0064353314],"genre_scores_gemma":[0.98278826,0.00012167769,0.006464255,0.009555533,0.000108586486,0.000012315528,3.4243538e-7,0.000012514465,0.0009365025],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99824566,0.00031393304,0.000336492,0.00030123355,0.00042251113,0.000380185],"domain_scores_gemma":[0.99868345,0.00015366866,0.0005665118,0.00050552184,0.000025029627,0.00006584227],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00048811227,0.00017959847,0.0003850669,1.9302175e-7,0.00038352105,0.000010958733,0.00090782566,0.000079282625,0.0063204216],"category_scores_gemma":[0.00011231906,0.00008594178,0.0005206811,0.0005290855,0.0042849947,0.00000979048,0.0010331677,0.00021602515,0.00012502073],"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":[0.00019143536,0.00041704,0.3554949,0.000023507564,0.00020498174,6.8226905e-7,0.00045991645,0.0015445477,0.025656063,0.00040997137,0.60156703,0.014029955],"study_design_scores_gemma":[0.00046977235,0.0008921627,0.8262659,0.000040025094,0.000110145025,0.0000057629204,0.00036289782,0.0007053343,0.0071686655,0.0007192775,0.16289692,0.00036314418],"about_ca_topic_score_codex":0.0008603814,"about_ca_topic_score_gemma":0.000017827091,"teacher_disagreement_score":0.470771,"about_ca_system_score_codex":0.00005150259,"about_ca_system_score_gemma":0.0000123597165,"threshold_uncertainty_score":0.99842477},"labels":[],"label_agreement":null},{"id":"W2886690783","doi":"10.1029/2018jd028886","title":"Radiosonde‐Derived Temperature Inversions and Their Association With Fog Over 37 Melt Seasons in East Greenland","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":28,"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 Lethbridge","funders":"Natural Sciences and Engineering Research Council of Canada; National Oceanic and Atmospheric Administration; Alberta Innovates; Alberta Innovates - Technology Futures; University of Washington; University of Alberta; University of Lethbridge; National Aeronautics and Space Administration","keywords":"Radiosonde; Arctic; Climatology; Depth sounding; Environmental science; Geology; Inversion (geology); Lidar; Atmospheric Infrared Sounder; Satellite; Meteorology; Atmospheric sciences; Remote sensing; Troposphere; Geography; Structural basin; Oceanography","score_opus":0.013878147874935104,"score_gpt":0.26419026143729857,"score_spread":0.2503121135623635,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2886690783","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":[0.99677294,0.000102559236,0.000043807482,0.0014671822,0.000048504655,0.00014580808,0.0000042145402,0.0000065037693,0.0014084901],"genre_scores_gemma":[0.9972399,0.000095679825,0.0009411794,0.00012088799,0.00032105861,0.0000041542326,6.786768e-7,0.000017765484,0.0012587288],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99776447,0.0002735043,0.00020919801,0.00024414586,0.0009919946,0.0005166814],"domain_scores_gemma":[0.9988841,0.00031872158,0.00016914199,0.00017286227,0.00013061817,0.00032457273],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00073061127,0.00016410297,0.0002937574,0.0000022443262,0.0002785485,0.00009856043,0.0002885279,0.00012614527,0.0009138041],"category_scores_gemma":[0.00028716822,0.00010151978,0.00007489105,0.00062752294,0.00051876745,0.00038137325,0.00021364944,0.0008037985,0.000055248856],"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":[0.00066281325,0.000333067,0.9103134,0.000011435037,0.00010553971,0.00007996243,0.0018284902,0.000077415905,0.052242536,0.00008460991,0.028294541,0.0059661595],"study_design_scores_gemma":[0.0014995058,0.0014972995,0.98551846,0.000106610525,0.000013754903,0.000022868415,0.0017050533,0.0014672066,0.0022420613,0.0009740234,0.004761394,0.00019174647],"about_ca_topic_score_codex":0.00062378234,"about_ca_topic_score_gemma":0.0011416167,"teacher_disagreement_score":0.07520504,"about_ca_system_score_codex":0.00038097647,"about_ca_system_score_gemma":0.00009813003,"threshold_uncertainty_score":0.9999995},"labels":[],"label_agreement":null},{"id":"W2887088388","doi":"","title":"Small ice particle observations in tropospheric clouds: fact or artifact?","year":2010,"lang":"en","type":"article","venue":"13th Conference on Cloud Physics/13th Conference on Atmospheric Radiation (28 June–2 July 2010)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":false,"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":"Artifact (error); Troposphere; Geology; Meteorology; Environmental science; Climatology; Geography; Computer science; Artificial intelligence","score_opus":0.055398417478922525,"score_gpt":0.25724806973100833,"score_spread":0.20184965225208581,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2887088388","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":[0.96571195,0.0000254589,0.0070789,0.0026868496,0.0032820115,0.0015490338,0.00006546528,0.0004021084,0.01919825],"genre_scores_gemma":[0.978542,0.00022708288,0.0065921955,0.0016430953,0.00056269224,0.00035272617,0.00008560206,0.00014613157,0.011848476],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99346983,0.00036943125,0.0013821702,0.0018642052,0.0012476713,0.0016666941],"domain_scores_gemma":[0.9958443,0.00042609026,0.00092154386,0.0018176207,0.00019639505,0.00079406315],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00061832415,0.0011786016,0.0010607801,0.00000528161,0.0007063544,0.0004894236,0.0014814619,0.0005701122,0.014702191],"category_scores_gemma":[0.00035213438,0.0010528076,0.00030112895,0.0018568878,0.00074065494,0.0008177499,0.00026916002,0.0017883029,0.0063602957],"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":[0.0030095025,0.008884614,0.21578403,0.00018315658,0.00039596966,0.00021948159,0.011272054,0.054780148,0.08153596,0.16116883,0.042653333,0.42011294],"study_design_scores_gemma":[0.006645649,0.0023064574,0.5126451,0.0002836852,0.00019800193,0.000021164797,0.0018905981,0.38201562,0.005969232,0.014867748,0.068730734,0.004426009],"about_ca_topic_score_codex":0.0025466043,"about_ca_topic_score_gemma":0.003991651,"teacher_disagreement_score":0.41568694,"about_ca_system_score_codex":0.000526129,"about_ca_system_score_gemma":0.0005554486,"threshold_uncertainty_score":0.99919224},"labels":[],"label_agreement":null},{"id":"W2887831052","doi":"","title":"Analysis of cloud retrievals from MODIS and their impact on radiative fluxes over Canada in the context of application for the CloudSat mission","year":2006,"lang":"en","type":"article","venue":"12th Conference on Atmospheric Radiation/12th Conference on Cloud Physics (10-14 July 2006)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Context (archaeology); Environmental science; Radiative transfer; Remote sensing; Cloud computing; Meteorology; Atmospheric sciences; Climatology; Geography; Computer science; Geology; Physics","score_opus":0.013144707990704087,"score_gpt":0.24779617703340323,"score_spread":0.23465146904269915,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2887831052","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":[0.9830844,0.00022886448,0.0073394966,0.0008431379,0.00022769526,0.0017266714,0.0012832135,0.00002819306,0.0052383617],"genre_scores_gemma":[0.99787885,0.00018259755,0.00012356987,0.00058248924,0.00021146839,0.00013110813,0.0002897617,0.000040245366,0.00055990997],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9963245,0.00028903296,0.0009393738,0.00089343754,0.000985626,0.00056802464],"domain_scores_gemma":[0.9956452,0.0018085504,0.0011500743,0.0010663173,0.00017616448,0.00015364953],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00056360895,0.0006766514,0.0010045355,0.0000069495986,0.0003270214,0.000100467216,0.0008957804,0.00021764338,0.0018168443],"category_scores_gemma":[0.00012486588,0.00041166318,0.00033638816,0.0014725033,0.0004911503,0.00016268858,0.000078876394,0.00035959051,0.000025535152],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0042557986,0.0028870413,0.105482265,0.00009624759,0.0021698554,0.0000062205445,0.010917691,0.53154504,0.0089805145,0.043227907,0.07532602,0.21510543],"study_design_scores_gemma":[0.002389386,0.0010692951,0.34357676,0.00011356595,0.00057167944,4.8264786e-7,0.002116628,0.6311594,0.0043224315,0.0080339,0.005704091,0.00094233203],"about_ca_topic_score_codex":0.15261011,"about_ca_topic_score_gemma":0.022658663,"teacher_disagreement_score":0.2380945,"about_ca_system_score_codex":0.0005083731,"about_ca_system_score_gemma":0.00045705977,"threshold_uncertainty_score":0.9998335},"labels":[],"label_agreement":null},{"id":"W2888494744","doi":"10.5194/acp-18-11847-2018","title":"Depolarization and lidar ratios at 355, 532, and 1064 nm and microphysical properties of aged tropospheric and stratospheric Canadian wildfire smoke","year":2018,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":317,"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":"Horizon 2020 Framework Programme; Russian Science Foundation","keywords":"Depolarization ratio; Stratosphere; Troposphere; Lidar; Atmospheric sciences; Wavelength; Aerosol; Environmental science; Mineral dust; Materials science; Meteorology; Optics; Physics","score_opus":0.0053818360224851015,"score_gpt":0.17640080482139048,"score_spread":0.17101896879890538,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2888494744","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":[0.99749786,0.001026566,0.00023293392,0.00007096089,0.00002002854,0.00018487978,0.000007648072,0.000019665173,0.00093945186],"genre_scores_gemma":[0.9948645,0.00045538874,0.0037187205,0.00013383752,0.000098177195,0.000009507493,0.0000069857624,0.000028177066,0.0006846953],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.998775,0.00003264485,0.00022439088,0.0005000826,0.00015800721,0.0003098638],"domain_scores_gemma":[0.99933404,0.000022932882,0.000113492235,0.00019777629,0.000014374086,0.00031740882],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00006325631,0.00029217312,0.00029971157,5.7624593e-8,0.00045040133,0.0000793597,0.000082562394,0.00013728469,0.0001948964],"category_scores_gemma":[0.000010700152,0.00026438656,0.000024938556,0.00019111947,0.001528003,0.00021412745,0.00016121952,0.00013369907,0.0000026570929],"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":[0.00009343436,0.00008162253,0.3394504,0.00021307114,0.00006353718,0.000007313909,0.0023485296,0.000023296398,0.5652016,0.000027525693,0.00011200805,0.092377655],"study_design_scores_gemma":[0.0023543767,0.00064489583,0.76406306,0.00017424056,0.00027876566,0.00015797802,0.0015850003,0.026129548,0.19993654,0.0009712488,0.0021177847,0.0015865748],"about_ca_topic_score_codex":0.011720613,"about_ca_topic_score_gemma":0.0013155309,"teacher_disagreement_score":0.42461264,"about_ca_system_score_codex":0.00006562151,"about_ca_system_score_gemma":0.00004535453,"threshold_uncertainty_score":0.9999808},"labels":[],"label_agreement":null},{"id":"W2888534752","doi":"10.5194/acp-18-11831-2018","title":"Extreme levels of Canadian wildfire smoke in the stratosphere over central Europe on 21–22 August 2017","year":2018,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":190,"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":"Horizon 2020 Framework Programme; National Oceanic and Atmospheric Administration; Russian Science Foundation; National Aeronautics and Space Administration","keywords":"AERONET; Stratosphere; Lidar; Aerosol; Environmental science; Atmospheric sciences; Troposphere; Sun photometer; Tropopause; Altitude (triangle); Climatology; Smoke; Meteorology; Remote sensing; Geology; Geography","score_opus":0.020953810709089363,"score_gpt":0.21859956451815032,"score_spread":0.19764575380906096,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2888534752","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":[0.8663663,0.0000372358,0.000030052413,0.00008364331,0.000039361927,0.000087617926,0.000016966147,0.000008762975,0.13333003],"genre_scores_gemma":[0.99602145,0.000046275814,0.00061860867,0.0004284421,0.00018620158,0.0000047610347,0.0000049500845,0.000016974607,0.0026723167],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99882877,0.000027446687,0.00018446981,0.0003149701,0.00024010609,0.000404267],"domain_scores_gemma":[0.9993415,0.000030586514,0.00008263965,0.00037754202,0.000007724948,0.00016003274],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000088322064,0.00020438085,0.00016626909,3.1619432e-8,0.00015898833,0.00003158573,0.00033597607,0.000087176195,0.007674955],"category_scores_gemma":[0.00001037902,0.00015927719,0.000047030648,0.00049542583,0.000434179,0.0001014615,0.00004998625,0.00019135457,0.000038277045],"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":[0.000116041236,0.00056824775,0.71145964,0.00008670488,0.00007202689,0.00010479309,0.0038680297,0.0012505753,0.02285154,0.00068747916,0.044648107,0.21428679],"study_design_scores_gemma":[0.00046923882,0.00011360661,0.9547784,0.000042501186,0.000021921254,0.000009781933,0.0004371289,0.0025362908,0.003627282,0.0003447726,0.037249573,0.0003695397],"about_ca_topic_score_codex":0.033693872,"about_ca_topic_score_gemma":0.004496947,"teacher_disagreement_score":0.2433187,"about_ca_system_score_codex":0.000067652094,"about_ca_system_score_gemma":0.000059234953,"threshold_uncertainty_score":0.9932322},"labels":[],"label_agreement":null},{"id":"W2890722430","doi":"","title":"Evidence for Ice Particle Multiplication from In-Situ Measurements","year":2006,"lang":"en","type":"article","venue":"12th Conference on Atmospheric Radiation/12th Conference on Cloud Physics (10-14 July 2006)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Advanced Foods and Materials Network","funders":"","keywords":"In situ; Multiplication (music); Geology; Computer science; Mathematics; Physics; Meteorology; Combinatorics","score_opus":0.07359171303896939,"score_gpt":0.28715002030237763,"score_spread":0.21355830726340824,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2890722430","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":[0.8833424,0.00032274,0.04082096,0.0017486741,0.0009895934,0.003082149,0.00016539053,0.00036919114,0.06915894],"genre_scores_gemma":[0.9861647,0.00012926965,0.0046878806,0.00075652753,0.0005765516,0.00068448315,0.00017341762,0.00009208884,0.0067351],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9944659,0.00021973095,0.0010893858,0.001681039,0.0014065912,0.0011373867],"domain_scores_gemma":[0.9968345,0.00052962545,0.0007840109,0.0012414253,0.00026690724,0.00034352418],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0005754503,0.0008279127,0.0007379209,0.0000038045632,0.0004532853,0.00032662353,0.0010384568,0.00032337353,0.006081345],"category_scores_gemma":[0.00026927685,0.0008388114,0.00023989615,0.0009244725,0.0003542537,0.0007444666,0.00014528568,0.00042523452,0.0038002292],"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":[0.0034501094,0.0066214213,0.1796597,0.00015300384,0.00029213214,0.000027557806,0.0028274925,0.14802232,0.14412087,0.034513306,0.107381076,0.372931],"study_design_scores_gemma":[0.0105039505,0.0021850755,0.50489795,0.0010417759,0.00032187634,0.0000027866377,0.00051241316,0.35858452,0.045480467,0.04226473,0.029693581,0.004510837],"about_ca_topic_score_codex":0.0021844637,"about_ca_topic_score_gemma":0.0008491019,"teacher_disagreement_score":0.36842018,"about_ca_system_score_codex":0.00083059864,"about_ca_system_score_gemma":0.00028449105,"threshold_uncertainty_score":0.9994063},"labels":[],"label_agreement":null},{"id":"W2892018637","doi":"10.5194/acp-19-4595-2019","title":"Lidar measurements of thin laminations within Arctic clouds","year":2019,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency; Indigenous and Northern Affairs Canada; Environment and Climate Change Canada; Eurostars; Strong; Ontario Innovation Trust","keywords":"Lidar; Environmental science; Radiosonde; Atmospheric sciences; Snow; Arctic; Altitude (triangle); The arctic; Relative humidity; Context (archaeology); Humidity; Meteorology; Remote sensing; Geology; Geography; Oceanography","score_opus":0.008951164683102508,"score_gpt":0.20859709609280958,"score_spread":0.19964593140970707,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2892018637","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":[0.95807445,0.000039208724,0.0004985651,0.000025001063,0.000052352698,0.000099011355,0.0000021264452,0.000020245106,0.041189026],"genre_scores_gemma":[0.9805847,0.00000887267,0.011090419,0.00007123104,0.000040990555,0.000006775385,0.0000053871754,0.000014290139,0.008177324],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9990994,0.000014592474,0.00018944907,0.00025360598,0.00027872119,0.0001642842],"domain_scores_gemma":[0.9995004,0.000025046531,0.00011988335,0.000266785,0.000016098898,0.00007181024],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00011149535,0.00014549706,0.00017062492,6.9009585e-9,0.00006668197,0.000013060427,0.0001554633,0.00006506218,0.003944176],"category_scores_gemma":[0.000010640796,0.00013582007,0.000052204916,0.00018655873,0.00014800753,0.000103384475,0.00008666601,0.00011291472,0.00012267029],"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":[0.000032740983,0.00033166053,0.7707026,0.00025105986,0.00007388033,0.0000021788235,0.0015467254,0.008557667,0.17923705,0.00014894121,0.00023198585,0.038883515],"study_design_scores_gemma":[0.0038830105,0.00046273408,0.3694225,0.00030365237,0.0003215058,0.00004564185,0.0017288178,0.09529464,0.5088591,0.011481742,0.0058792997,0.0023173774],"about_ca_topic_score_codex":0.00011875755,"about_ca_topic_score_gemma":0.0000018194819,"teacher_disagreement_score":0.4012801,"about_ca_system_score_codex":0.000054880446,"about_ca_system_score_gemma":0.000014649459,"threshold_uncertainty_score":0.99696636},"labels":[],"label_agreement":null},{"id":"W2892341989","doi":"10.1175/jas-d-18-0060.1","title":"Relationship between Turbulence and Drizzle in Continental and Marine Low Stratiform Clouds","year":2018,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Brookhaven National Laboratory; Biological and Environmental Research; U.S. Department of Energy","keywords":"Drizzle; Turbulence; Environmental science; Precipitation; Atmospheric sciences; Cloud base; Liquid water path; Cloud condensation nuclei; Meteorology; Cloud computing; Physics; Aerosol","score_opus":0.013297471783831397,"score_gpt":0.24250627215636358,"score_spread":0.2292088003725322,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2892341989","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":[0.99608165,0.00008369185,0.000044233868,0.0009628501,0.0001782111,0.00007410634,4.798662e-7,0.00000364102,0.0025711174],"genre_scores_gemma":[0.9930742,0.000020134079,0.0062932824,0.00014564248,0.00010911513,7.2089625e-7,4.861684e-8,0.000003901332,0.00035295513],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989042,0.00004127938,0.00031474902,0.00016315425,0.00037526962,0.00020133704],"domain_scores_gemma":[0.9993973,0.00012084341,0.00027594133,0.0001045813,0.0000120969735,0.00008928858],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00074310065,0.000100906334,0.00015492729,6.69567e-7,0.00030278892,0.00006851432,0.00038483558,0.000042757074,0.00026900446],"category_scores_gemma":[0.000114917246,0.00005948138,0.00003491329,0.0004924108,0.0014906285,0.00037441798,0.00030148568,0.00016114976,0.000006087595],"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":[0.000007725069,0.0000132954265,0.9963612,0.0000017920191,0.0000018773143,0.0000015601428,0.0003096885,0.00011509119,0.00014350555,0.000063545725,0.0002006704,0.0027800403],"study_design_scores_gemma":[0.00023800472,0.00023032108,0.993187,0.000025065467,0.000009549658,0.000048995058,0.0004029169,0.002593411,0.000113914604,0.0028416773,0.00022620671,0.00008290511],"about_ca_topic_score_codex":0.00026290078,"about_ca_topic_score_gemma":0.00017322836,"teacher_disagreement_score":0.0062490487,"about_ca_system_score_codex":0.00005030088,"about_ca_system_score_gemma":0.000029009865,"threshold_uncertainty_score":0.54922825},"labels":[],"label_agreement":null},{"id":"W2892760810","doi":"10.1175/jcli-d-18-0023.1","title":"How Well Are Clouds Simulated over Greenland in Climate Models? Consequences for the Surface Cloud Radiative Effect over the Ice Sheet","year":2018,"lang":"en","type":"article","venue":"Journal of Climate","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":27,"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":"Centre National d’Etudes Spatiales; National Aeronautics and Space Administration; National Science Foundation","keywords":"Greenland ice sheet; Radiative transfer; Atmospheric sciences; Longwave; Environmental science; Cloud fraction; Climate model; Cloud cover; Cloud forcing; Climatology; Lidar; Ice sheet; Shortwave; Cloud top; Radiative flux; Meteorology; Climate change; Cloud computing; Geology; Remote sensing; Satellite; Geography; Physics; Astronomy","score_opus":0.012638718177726663,"score_gpt":0.25551551146876283,"score_spread":0.24287679329103617,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2892760810","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":[0.99459493,0.00043309078,0.00087371614,0.0018138203,0.00056539255,0.0004596227,0.000032648426,0.00001131064,0.0012154648],"genre_scores_gemma":[0.9975862,0.0010934771,0.0002493921,0.00062267284,0.00030007935,0.0000042006595,9.064756e-7,0.000026180634,0.00011688767],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.998001,0.00025830054,0.00046502278,0.00023623886,0.00047578936,0.00056364085],"domain_scores_gemma":[0.99771947,0.0010589598,0.00079134165,0.00028114291,0.000044909502,0.000104189035],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018072391,0.00025590844,0.0004098123,0.0000034269472,0.00040206144,0.00016142434,0.0005618904,0.0001125669,0.00039755498],"category_scores_gemma":[0.000095606665,0.00012575071,0.00020893077,0.00027341858,0.0007269948,0.00045360837,0.00017457988,0.00033523512,0.000031014173],"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":[0.0028921745,0.00016082154,0.58424973,0.00006643508,0.00022201144,0.000082106715,0.0025080752,0.39606568,0.0021864276,0.00033319613,0.008394488,0.0028388365],"study_design_scores_gemma":[0.0058889366,0.0020049333,0.35841164,0.00026005186,0.00032583895,0.00009733301,0.002064547,0.6137233,0.0016477045,0.0029231913,0.011974481,0.0006780612],"about_ca_topic_score_codex":0.00015960715,"about_ca_topic_score_gemma":0.00027871478,"teacher_disagreement_score":0.2258381,"about_ca_system_score_codex":0.00014862698,"about_ca_system_score_gemma":0.000021706308,"threshold_uncertainty_score":0.5127965},"labels":[],"label_agreement":null},{"id":"W2894410433","doi":"","title":"Airborne Radar Observation of A Major Winter Storm: Use of Dual-frequency and Polarimetric Measurements in Studies Cloud Structures and Processes","year":2010,"lang":"en","type":"article","venue":"13th Conference on Cloud Physics/13th Conference on Atmospheric Radiation (28 June–2 July 2010)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"","keywords":"Meteorology; Remote sensing; Radar; Storm; Environmental science; Cloud computing; Polarimetry; Climatology; Geology; Geography; Computer science; Telecommunications; Physics","score_opus":0.061636376488231476,"score_gpt":0.27105163899901463,"score_spread":0.20941526251078316,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2894410433","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":[0.9960631,0.00027510512,0.00065449096,0.00048256738,0.0010056486,0.00084600545,0.00006275158,0.000052156265,0.0005581861],"genre_scores_gemma":[0.99070966,0.0007584544,0.0076044453,0.00022832611,0.00014723284,0.000051068004,0.000028891125,0.000052046216,0.00041988326],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9962369,0.0002053637,0.0010016265,0.0009776118,0.001012304,0.0005661441],"domain_scores_gemma":[0.99729705,0.000299906,0.0010771753,0.0006927127,0.00039267915,0.00024048086],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0004811983,0.00065935805,0.00092750805,0.000013465758,0.00019443483,0.00012598246,0.00041240087,0.00029379176,0.0004445888],"category_scores_gemma":[0.0006685052,0.0005878246,0.00008877697,0.0011875659,0.0008776634,0.00077402516,0.00018693168,0.00064724847,0.000031586504],"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":[0.0007954848,0.0014808403,0.7908465,0.00070759933,0.00042835082,0.000011144604,0.0084073255,0.0011127561,0.09255702,0.023997419,0.0033350524,0.07632048],"study_design_scores_gemma":[0.002809064,0.0011165023,0.9650411,0.00036195753,0.00016288793,0.0000063448047,0.0008747336,0.0036403155,0.009354671,0.014505985,0.0009769343,0.0011495108],"about_ca_topic_score_codex":0.0032066768,"about_ca_topic_score_gemma":0.0016807771,"teacher_disagreement_score":0.17419456,"about_ca_system_score_codex":0.00017618504,"about_ca_system_score_gemma":0.00030009865,"threshold_uncertainty_score":0.99965733},"labels":[],"label_agreement":null},{"id":"W2896236463","doi":"10.1029/2018jd028965","title":"The Great Slave Lake PyroCb of 5 August 2014: Observations, Simulations, Comparisons With Regular Convection, and Impact on UTLS Water Vapor","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":32,"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":"Microwave Limb Sounder; Water vapor; Environmental science; Plume; Atmospheric sciences; Convection; Cirrus; Tropopause; Cloud top; Climatology; Stratosphere; Meteorology; Geology; Satellite; Geography; Physics","score_opus":0.02990221824632,"score_gpt":0.31142126222115474,"score_spread":0.28151904397483474,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2896236463","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":[0.9977319,0.0000764676,0.0005025276,0.0008365738,0.000050340783,0.0001928546,0.0000072103276,0.0000065122354,0.0005955683],"genre_scores_gemma":[0.996692,0.00006730113,0.0008346444,0.000038916893,0.00022273563,0.0000040140762,0.000002041076,0.000018036424,0.0021202972],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9976853,0.00019616156,0.00038950233,0.0001988924,0.0010908884,0.00043924176],"domain_scores_gemma":[0.9983518,0.00058919453,0.00020365126,0.00030990844,0.00031554748,0.0002298912],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006734098,0.0001601423,0.00028178797,0.0000021881701,0.0006757242,0.00009754235,0.00032190926,0.000063025924,0.0018938134],"category_scores_gemma":[0.00014523408,0.000073193914,0.00010008632,0.00029093403,0.0014681855,0.00026043752,0.00014963471,0.00041277043,0.0000896377],"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":[0.0031478102,0.0007462493,0.8069598,0.000023807179,0.00041111623,0.00003383608,0.0008452018,0.008099415,0.019491402,0.0007029429,0.14852974,0.011008672],"study_design_scores_gemma":[0.00087536994,0.0045185145,0.95793235,0.000063019914,0.000038369308,0.000019883255,0.0004471442,0.004466575,0.0072918534,0.0024829437,0.021698298,0.0001656803],"about_ca_topic_score_codex":0.00088404753,"about_ca_topic_score_gemma":0.0009114625,"teacher_disagreement_score":0.15097255,"about_ca_system_score_codex":0.000108679335,"about_ca_system_score_gemma":0.000068017864,"threshold_uncertainty_score":0.9990186},"labels":[],"label_agreement":null},{"id":"W2896356256","doi":"","title":"In-situ observation of Arctic mixed phase clouds during the ISDAC flight campaign","year":2010,"lang":"en","type":"article","venue":"13th Conference on Cloud Physics/13th Conference on Atmospheric Radiation (28 June–2 July 2010)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":false,"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":"Mixed phase; In situ; Phase (matter); Arctic; Environmental science; The arctic; Meteorology; Astrobiology; Atmospheric sciences; Remote sensing; Geology; Geography; Oceanography; Chemistry; Physics","score_opus":0.01939808604995215,"score_gpt":0.24999265324420916,"score_spread":0.23059456719425703,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2896356256","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":[0.979487,0.000027214062,0.0020984549,0.0018993266,0.003629908,0.0012407646,0.000041995805,0.00013256483,0.011442763],"genre_scores_gemma":[0.9910452,0.00017942641,0.0015796332,0.000784901,0.0006219929,0.00020497879,0.000059130816,0.00009635529,0.005428428],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99459285,0.00037249795,0.0012562582,0.0013235251,0.0013631027,0.0010917427],"domain_scores_gemma":[0.99617845,0.000328483,0.0011874557,0.0016839702,0.00022593947,0.00039571765],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00073949737,0.00091064494,0.0009117454,0.0000070585047,0.000523441,0.00022271603,0.0014060432,0.00044324607,0.0046294997],"category_scores_gemma":[0.00022102434,0.0007557556,0.00028969435,0.0013490524,0.00084748684,0.00073133706,0.00022927663,0.001483042,0.0014559272],"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":[0.0024194862,0.0075824005,0.06929168,0.0003954575,0.0003921801,0.0000898104,0.015258761,0.017255628,0.5779847,0.15425861,0.027256876,0.12781444],"study_design_scores_gemma":[0.0153961405,0.0026850835,0.70598483,0.00063554884,0.00033186923,0.000033426946,0.0024617806,0.12367807,0.072550714,0.032878023,0.038490694,0.0048738006],"about_ca_topic_score_codex":0.0013079987,"about_ca_topic_score_gemma":0.0009014728,"teacher_disagreement_score":0.6366932,"about_ca_system_score_codex":0.00042440827,"about_ca_system_score_gemma":0.00034560333,"threshold_uncertainty_score":0.99948937},"labels":[],"label_agreement":null},{"id":"W2896953485","doi":"10.3390/rs10101638","title":"Ground Reflectance Retrieval on Horizontal and Inclined Terrains Using the Software Package REFLECT","year":2018,"lang":"en","type":"article","venue":"Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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; Université de Montréal; Université de Sherbrooke","funders":"","keywords":"Remote sensing; Environmental science; Aerosol; Multispectral image; Atmospheric correction; Irradiance; Satellite; Software; Reflectivity; Calibration; Software package; Terrain; Geology; Optics; Meteorology; Computer science; Physics; Geography","score_opus":0.023921786147122613,"score_gpt":0.2804006997752084,"score_spread":0.2564789136280858,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2896953485","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":[0.97136873,0.000029875146,0.023640055,0.00025715173,0.00022069021,0.00014024427,0.000001350825,0.00006505483,0.0042768484],"genre_scores_gemma":[0.9685132,0.00001266285,0.029982114,0.0007935666,0.00036231635,5.5167764e-9,0.000001019434,0.000030131772,0.00030499342],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9986858,0.00008849864,0.00018061894,0.00038842196,0.00030319003,0.00035349416],"domain_scores_gemma":[0.99936897,0.00007651997,0.00010127748,0.00035589747,0.000012463616,0.0000848663],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027059237,0.00018250929,0.00015459114,0.0000021072406,0.000692545,0.00006859526,0.00011991907,0.00009121174,0.000060291342],"category_scores_gemma":[0.0001263351,0.00013052004,0.000045859597,0.00028430115,0.00054601504,0.000101249425,0.00018604165,0.00021222541,0.00005700405],"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":[0.00036787658,0.00002701487,0.0010085542,0.000010414558,0.000032550568,0.00008918934,0.003474546,0.00008401412,0.79235893,0.00002186107,0.00055411103,0.20197093],"study_design_scores_gemma":[0.0040871594,0.0052937847,0.05130931,0.000997837,0.00033055615,0.0020468473,0.004014339,0.7576997,0.13669132,0.011405083,0.022127287,0.003996734],"about_ca_topic_score_codex":0.00021788517,"about_ca_topic_score_gemma":0.00022954727,"teacher_disagreement_score":0.75761575,"about_ca_system_score_codex":0.0002379595,"about_ca_system_score_gemma":0.0000143435345,"threshold_uncertainty_score":0.5326566},"labels":[],"label_agreement":null},{"id":"W2897471139","doi":"10.5194/amt-2018-347","title":"A practical method to remove a priori information from lidar optimal estimation method retrievals","year":2018,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"Western University","funders":"Strong","keywords":"A priori and a posteriori; Lidar; Remote sensing; Optimal estimation; Grid; Environmental science; Polyphemus; Meteorology; Computer science; Algorithm; Mathematics; Geography; Geology; Machine learning","score_opus":0.016670922369239616,"score_gpt":0.3407874672998559,"score_spread":0.32411654493061626,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2897471139","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.058114238,0.0000011289889,0.91229856,0.0017697929,0.000103126426,0.00029869846,0.0000050138137,0.00008379411,0.027325656],"genre_scores_gemma":[0.057265732,8.7419863e-7,0.93989766,0.002106827,0.000091669746,0.000012473672,0.000008587336,0.000009564849,0.000606637],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99854267,0.00013615846,0.00033055476,0.0002715349,0.00046017655,0.0002588846],"domain_scores_gemma":[0.99914384,0.00020555315,0.00012924662,0.0002975516,0.000029693392,0.00019412374],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00088841777,0.00014481266,0.00016711286,0.0000026638352,0.00013759588,0.00010008598,0.00016009933,0.00011818657,0.009159658],"category_scores_gemma":[0.0005268558,0.00011916203,0.00004699713,0.00037839284,0.00006259899,0.0010471817,0.00023802023,0.00011999807,0.0053174766],"study_design_candidate":"design_other","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":[0.0006444219,0.0001927605,0.004147476,0.000009684906,0.000070555245,0.000008851328,0.009692218,0.005474378,0.025978453,0.0036946347,0.06326872,0.8868179],"study_design_scores_gemma":[0.000852632,0.00097625254,0.05032351,0.000023184062,0.00009627547,0.00003910446,0.0012737765,0.7095554,0.062588975,0.0033763368,0.1701469,0.00074764906],"about_ca_topic_score_codex":0.0010555282,"about_ca_topic_score_gemma":0.000023524364,"teacher_disagreement_score":0.8860702,"about_ca_system_score_codex":0.00017109387,"about_ca_system_score_gemma":0.000028120206,"threshold_uncertainty_score":0.995457},"labels":[],"label_agreement":null},{"id":"W2897837642","doi":"10.1117/12.2324321","title":"The EarthCARE cloud profiling radar (CPR) doppler measurements in deep convection: challenges, post-processing, and science applications","year":2018,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Doppler effect; Remote sensing; Doppler radar; Convection; Radar; Satellite; Meteorology; Environmental science; Physics; Geology; Aerospace engineering; Astronomy","score_opus":0.024493798830138098,"score_gpt":0.25413883252712305,"score_spread":0.22964503369698494,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2897837642","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":[0.8537338,0.0026129805,0.005301966,0.004252713,0.00031095406,0.0011707229,0.0000013346439,0.00012987044,0.13248567],"genre_scores_gemma":[0.99526674,0.00013579759,0.0037696927,0.00025341686,0.00009420552,0.00006776539,4.644737e-7,0.000008336363,0.0004035658],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99863964,0.0000229832,0.0001585562,0.00038115418,0.00047092803,0.00032672661],"domain_scores_gemma":[0.99954146,0.000014709331,0.000054734188,0.00023650243,0.000051909417,0.00010067323],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005975887,0.00010412764,0.000073539246,0.0000021715437,0.00089033856,0.00008245443,0.0002749995,0.000040248942,0.0002544573],"category_scores_gemma":[0.000025247395,0.00007044388,0.000013649934,0.0003562167,0.0012212375,0.0002121093,0.0001847228,0.00009012668,0.00009383893],"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":[0.000059267564,0.00017257937,0.270055,0.000031970867,0.000012736829,0.0000014616974,0.0036566935,0.000048056907,0.041196432,0.004814269,0.00034900516,0.67960256],"study_design_scores_gemma":[0.0016566729,0.0006042558,0.8300262,0.00006158278,0.000032635886,0.00008696354,0.02143458,0.010146949,0.033205483,0.0041495822,0.09739127,0.0012037925],"about_ca_topic_score_codex":0.0001274268,"about_ca_topic_score_gemma":0.0012851937,"teacher_disagreement_score":0.6783987,"about_ca_system_score_codex":0.00010108683,"about_ca_system_score_gemma":0.00003949953,"threshold_uncertainty_score":0.6847854},"labels":[],"label_agreement":null},{"id":"W2898002340","doi":"10.5194/amt-2018-246","title":"Calibration of a Water Vapour Lidar using a Radiosonde TrajectoryMethod","year":2018,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Strong","keywords":"Radiosonde; Lidar; Calibration; Environmental science; Water vapor; Remote sensing; Meteorology; Troposphere; Trajectory; Geology; Geography; Physics","score_opus":0.018392432774207452,"score_gpt":0.25355982600487664,"score_spread":0.23516739323066918,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2898002340","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":[0.85298455,0.0000036114336,0.13795117,0.000044704844,0.000058317495,0.000057001227,4.3362817e-7,0.000017731978,0.008882473],"genre_scores_gemma":[0.93074477,6.452391e-7,0.0679382,0.0001326748,0.00005981667,0.0000012793234,4.7586425e-7,0.000007521645,0.0011146339],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9994205,0.000034767174,0.00012466928,0.00013763575,0.00013199779,0.00015039151],"domain_scores_gemma":[0.99979097,0.000008167967,0.000028032826,0.00012534461,0.000004034995,0.000043433658],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00012327028,0.00006535609,0.000085628584,6.676877e-7,0.000059871803,0.000008176339,0.000083685554,0.00004018664,0.012999068],"category_scores_gemma":[0.00000513205,0.000041926396,0.000034187164,0.00007606926,0.00013958837,0.00011327637,0.000055420427,0.000029367979,0.000076077326],"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":[0.000017794962,0.000045956866,0.027417595,0.000003373273,0.000007756481,0.0000014040149,0.0013163243,0.00030141324,0.967282,0.00008159008,0.000500708,0.0030240694],"study_design_scores_gemma":[0.00031043775,0.00019683663,0.010118015,0.000005686842,0.000018996347,0.000011527792,0.00026038344,0.06188822,0.9242989,0.0005248145,0.0021738114,0.00019239531],"about_ca_topic_score_codex":0.0005920692,"about_ca_topic_score_gemma":0.00004736424,"teacher_disagreement_score":0.07776019,"about_ca_system_score_codex":0.000035832276,"about_ca_system_score_gemma":0.000005191651,"threshold_uncertainty_score":0.9879032},"labels":[],"label_agreement":null},{"id":"W2898008832","doi":"10.1175/jtech-d-18-0083.1","title":"EarthCARE’s Broadband Radiometer: Uncertainties Associated with Cloudy Atmospheres","year":2018,"lang":"en","type":"article","venue":"Journal of Atmospheric and Oceanic Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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":"European Space Agency","keywords":"Remote sensing; Radiometer; Environmental science; Radiance; Shortwave; Nadir; Radiative transfer; Spectroradiometer; Longwave; Meteorology; Satellite; Atmospheric sciences; Physics; Geology; Optics; Reflectivity","score_opus":0.005075459935488372,"score_gpt":0.20133824295687483,"score_spread":0.19626278302138644,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2898008832","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":[0.9937394,0.00086241734,0.002742891,0.0005971557,0.00021025758,0.00011176177,0.0000011784172,0.00007682473,0.0016580853],"genre_scores_gemma":[0.9843379,0.00021188922,0.014049292,0.00018556764,0.000111606925,0.0000020085924,3.3111584e-7,0.00003118873,0.0010702026],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99836594,0.00005191526,0.00047080388,0.00029247502,0.00037117294,0.00044770836],"domain_scores_gemma":[0.99888927,0.000063578744,0.0005455981,0.00026032983,0.00009107889,0.00015015206],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00024125684,0.00026343393,0.00047828996,0.0000017512682,0.00022920984,0.000041170915,0.00040469365,0.00025730586,0.0013122578],"category_scores_gemma":[0.00012123241,0.00018397106,0.000081895654,0.0009509947,0.0014836218,0.00021670802,0.00018510838,0.00036206466,0.000029454373],"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":[0.00034596113,0.00023591633,0.9013783,0.000009726812,0.00037758463,0.00023198326,0.00074447115,0.00012771755,0.0016941336,0.0006603957,0.008790074,0.08540373],"study_design_scores_gemma":[0.0074278703,0.020890731,0.85604,0.00039202115,0.00060957775,0.0039895996,0.008514044,0.0038334758,0.0034431634,0.008895225,0.084151044,0.0018132564],"about_ca_topic_score_codex":0.000054251206,"about_ca_topic_score_gemma":0.00006715995,"teacher_disagreement_score":0.08359048,"about_ca_system_score_codex":0.00014666044,"about_ca_system_score_gemma":0.000049714752,"threshold_uncertainty_score":0.99960065},"labels":[],"label_agreement":null},{"id":"W2898158268","doi":"10.5194/acp-18-15329-2018","title":"Observations of the microphysical evolution of convective clouds in the southwest of the United Kingdom","year":2018,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":11,"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":"Natural Environment Research Council; Sight Research UK; National Science Foundation","keywords":"Ice crystals; Precipitation; Atmospheric sciences; Environmental science; Convection; Entrainment (biomusicology); Wind shear; Radar; Meteorology; Climatology; Geology; Wind speed; Geography; Physics","score_opus":0.013123694557720523,"score_gpt":0.2147234882467236,"score_spread":0.20159979368900308,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2898158268","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":[0.99842876,0.000010111544,0.00037659035,0.00008495843,0.000030943607,0.00010849539,0.000008528978,0.0000026181544,0.00094896357],"genre_scores_gemma":[0.99923086,0.0000019844622,0.00050673867,0.000054572873,0.00005297339,0.000005018184,0.0000014123326,0.0000053100994,0.00014114846],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99936235,0.000046969108,0.00017786921,0.00012750489,0.00018149335,0.0001038193],"domain_scores_gemma":[0.9993763,0.000069169095,0.0001844045,0.00032838108,0.000027328078,0.000014428372],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007904417,0.00009216378,0.00012283237,1.3504446e-8,0.000104128325,0.000003679726,0.00032712196,0.000047828595,0.00009301147],"category_scores_gemma":[0.000020055924,0.000050051916,0.00007132552,0.0006811517,0.0011753608,0.00003366994,0.00012438362,0.00011568162,0.0000013018674],"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":[0.000027927144,0.00025145325,0.54173565,0.000038205457,0.000022463657,1.0554684e-7,0.0033033756,0.0013912757,0.45083123,0.0012498534,0.00012204796,0.0010264033],"study_design_scores_gemma":[0.00026031554,0.00003316207,0.916747,0.000036366375,0.000036786707,0.0000012200884,0.00092115806,0.005842912,0.0738594,0.0018544522,0.000322282,0.00008495279],"about_ca_topic_score_codex":0.0019698627,"about_ca_topic_score_gemma":0.000026959362,"teacher_disagreement_score":0.37697184,"about_ca_system_score_codex":0.00003952267,"about_ca_system_score_gemma":0.000024750792,"threshold_uncertainty_score":0.43306658},"labels":[],"label_agreement":null},{"id":"W2899452206","doi":"10.1364/hise.2016.hw2f.3","title":"Towards the Thin Ice Clouds in the Far-InfraRed Experiment (TICFIRE)","year":2016,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Institut National d'Optique; Université du Québec à Montréal","funders":"","keywords":"Remote sensing; Infrared; Radiometer; Satellite; Arctic; The arctic; Environmental science; Radiometry; Polar; Meteorology; Astrobiology; Geology; Physics; Astronomy; Oceanography","score_opus":0.015755380111065812,"score_gpt":0.23559024525343242,"score_spread":0.2198348651423666,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2899452206","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":[0.6728484,0.00008607475,0.0028135644,0.012836318,0.00015536885,0.00030997864,0.000001246613,0.000043426637,0.3109056],"genre_scores_gemma":[0.9788892,0.000041998086,0.0006956766,0.004491037,0.000048489506,0.00005727734,2.5970388e-7,0.000009354669,0.01576669],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9988064,0.00010052413,0.00018120652,0.00023322638,0.00038447298,0.00029415658],"domain_scores_gemma":[0.99934447,0.00009295352,0.000040951476,0.00047308818,0.0000027929277,0.000045744586],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00044581946,0.00013071974,0.00009269683,4.5207224e-7,0.00013842643,0.000036299476,0.0006823214,0.000048450922,0.010339607],"category_scores_gemma":[0.000027354059,0.000045313656,0.00005732665,0.00016501953,0.00023827996,0.00010565963,0.00022827667,0.00008506714,0.0009147142],"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":[0.00016944834,0.0009793404,0.11041125,0.000008394816,0.00006399458,0.00006753613,0.056161348,0.00034593316,0.05933509,0.045779064,0.33746544,0.38921317],"study_design_scores_gemma":[0.0012244589,0.00025690158,0.50830996,0.000022384766,0.000018333243,0.000021507642,0.013328498,0.0012354909,0.012045467,0.0075087305,0.45544922,0.0005790595],"about_ca_topic_score_codex":0.0010677428,"about_ca_topic_score_gemma":0.00015747114,"teacher_disagreement_score":0.3978987,"about_ca_system_score_codex":0.00011769491,"about_ca_system_score_gemma":0.000010982256,"threshold_uncertainty_score":0.9998632},"labels":[],"label_agreement":null},{"id":"W2900750689","doi":"10.5194/acp-19-3341-2019","title":"Lidar observations of pyrocumulonimbus smoke plumes in the UTLS over Tomsk (Western Siberia, Russia) from 2000 to 2017","year":2019,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":16,"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":"U.S. Naval Research Laboratory; Office of Naval Research; Strong","keywords":"Environmental science; Troposphere; Stratosphere; Volcano; Atmospheric sciences; Aerosol; Smoke; Boreal; Climatology; Geology; Geography; Meteorology","score_opus":0.01292726761676979,"score_gpt":0.23071632412647428,"score_spread":0.21778905650970448,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2900750689","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":[0.99449456,0.00009327741,0.00014964916,0.00016357281,0.000036451904,0.00018042522,0.000020860336,0.000013328645,0.004847872],"genre_scores_gemma":[0.9926903,0.00003224641,0.0028804415,0.00047865545,0.00008388486,0.000019209088,0.000014825699,0.000014751371,0.0037856698],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989649,0.0000189688,0.00021626968,0.00032368742,0.00025162904,0.00022452035],"domain_scores_gemma":[0.99928373,0.00008333332,0.00009530159,0.00045924503,0.0000063759185,0.00007203331],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00007288464,0.00017977146,0.00022260413,1.8537584e-8,0.00006493335,0.000036017984,0.0003366458,0.000082279264,0.00254439],"category_scores_gemma":[0.0000070094466,0.00014400958,0.00005809099,0.0002534918,0.00010778983,0.0001508247,0.00012560608,0.00013513632,0.000089133435],"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":[0.000036832407,0.00017361861,0.93279994,0.000028052627,0.000024305318,0.0000042841402,0.0028965075,0.0034381237,0.045782708,0.000024274064,0.0007576468,0.014033736],"study_design_scores_gemma":[0.00042542,0.000041609033,0.98317033,0.00003457284,0.000022099628,0.000001341225,0.00041075193,0.0022855557,0.003816818,0.00056713895,0.00895705,0.00026731167],"about_ca_topic_score_codex":0.001823216,"about_ca_topic_score_gemma":0.000035179408,"teacher_disagreement_score":0.05037042,"about_ca_system_score_codex":0.000054806078,"about_ca_system_score_gemma":0.000021752949,"threshold_uncertainty_score":0.9983674},"labels":[],"label_agreement":null},{"id":"W2902044979","doi":"","title":"A comparison of visibility parameterizations using surface observations","year":2007,"lang":"en","type":"preprint","venue":"INRIA a CCSD electronic archive server","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"","keywords":"Visibility; Computer science; Meteorology; Physics","score_opus":0.055198560367602144,"score_gpt":0.33451491576580056,"score_spread":0.27931635539819843,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2902044979","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":[0.88245267,0.00016212346,0.11561702,0.00005980155,0.00014999454,0.00063177705,0.00006620626,0.000059591344,0.0008008418],"genre_scores_gemma":[0.97187316,0.000034713892,0.027609563,0.00009165723,0.000042155738,0.000015187575,0.00015569273,0.00004631223,0.00013156053],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9968694,0.00020569276,0.00085501245,0.00077756523,0.00051941816,0.00077292905],"domain_scores_gemma":[0.9980873,0.0001865537,0.0006018404,0.0009506839,0.000034536544,0.00013910333],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00047102227,0.00039737913,0.00063226174,0.000006168754,0.0002129515,0.00003392796,0.0006989041,0.00026337773,0.0009958585],"category_scores_gemma":[0.000073194584,0.00040563176,0.00027404682,0.00041870473,0.00041722288,0.00012419898,0.0014184584,0.00095033523,0.000039034203],"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":[0.00006590961,0.000470506,0.50697386,0.00007074661,0.00012844529,0.000001546293,0.0015228033,0.47076756,0.017053176,0.0022116872,0.00028228248,0.0004514754],"study_design_scores_gemma":[0.0006324274,0.00031545621,0.52568454,0.00015261683,0.0002903637,0.0000051558764,0.00026452454,0.43228763,0.0029951816,0.03274817,0.0035426915,0.0010812031],"about_ca_topic_score_codex":0.0023737927,"about_ca_topic_score_gemma":0.004456783,"teacher_disagreement_score":0.08942051,"about_ca_system_score_codex":0.0006259844,"about_ca_system_score_gemma":0.00027801222,"threshold_uncertainty_score":0.9999174},"labels":[],"label_agreement":null},{"id":"W2902908554","doi":"10.1525/elementa.331","title":"Harnessing remote sensing to address critical science questions on ocean-atmosphere interactions","year":2018,"lang":"en","type":"article","venue":"Elementa Science of the Anthropocene","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":36,"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":"European Space Agency; National Aeronautics and Space Administration","keywords":"Atmosphere (unit); Interface (matter); Remote sensing; Environmental science; Earth system science; Scale (ratio); Meteorology; Ocean observations; Computer science; Data science; Geography; Oceanography; Geology","score_opus":0.01728656592050027,"score_gpt":0.33063214801459345,"score_spread":0.3133455820940932,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2902908554","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":[0.96381724,0.0000067741353,0.0058632386,0.004631282,0.0014711893,0.00022992553,0.0000055052706,0.000039732633,0.023935098],"genre_scores_gemma":[0.97228074,0.0000033538604,0.026458273,0.00086880027,0.00011105402,3.4462934e-7,1.8495099e-7,0.000012786464,0.0002644771],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99714184,0.000049086022,0.00030490244,0.00064415036,0.0011979255,0.0006620847],"domain_scores_gemma":[0.9986724,0.00006527102,0.00012235255,0.00075884524,0.00012274619,0.00025838523],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":["sts"],"category_scores_codex":[0.00092697405,0.000171698,0.00014932756,0.000006823723,0.0026679132,0.00016207025,0.0012486073,0.000024136783,0.0021122878],"category_scores_gemma":[0.00068105,0.00012440185,0.00005917748,0.002502756,0.012563351,0.0006778765,0.0010524794,0.00015971357,0.0002693526],"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":[0.000090037174,0.00048281878,0.02378471,0.00001637038,0.00001358859,0.000008808258,0.0023380728,0.002973814,0.78390634,0.0033349043,0.014750328,0.1683002],"study_design_scores_gemma":[0.00035948324,0.00076388544,0.09698163,0.0005312126,0.00004488909,0.000059186885,0.0027725946,0.042937707,0.8486059,0.0022058769,0.0040714093,0.0006662273],"about_ca_topic_score_codex":0.00081392465,"about_ca_topic_score_gemma":0.000112024776,"teacher_disagreement_score":0.16763397,"about_ca_system_score_codex":0.0004888443,"about_ca_system_score_gemma":0.00016445051,"threshold_uncertainty_score":0.9987999},"labels":[],"label_agreement":null},{"id":"W2903872581","doi":"10.1007/s00024-018-2058-8","title":"Review of Lidar-Based Applications for Aviation Weather","year":2018,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":102,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ontario Tech University; Environment and Climate Change Canada","funders":"Environment and Climate Change Canada; Civil Aviation Administration of China; Deutsches Zentrum für Luft- und Raumfahrt","keywords":"Lidar; Wind shear; Meteorology; Environmental science; Takeoff; Aviation safety; Wind speed; Takeoff and landing; Aviation; Civil aviation; Wake; Wake turbulence; Planetary boundary layer; Crew; Maximum sustained wind; Doppler effect; Remote sensing; Vortex; Aeronautics; Aerospace engineering; Geology; Wind gradient; Geography; Engineering","score_opus":0.006685409583415705,"score_gpt":0.22712061420428253,"score_spread":0.22043520462086683,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2903872581","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.29006213,0.0033222707,0.5995801,0.0016125499,0.00010575832,0.005110745,0.00007857486,0.00012611732,0.10000173],"genre_scores_gemma":[0.98996484,0.00025274008,0.0069999383,0.001996896,0.00014897954,0.00035983094,0.000019449115,0.000011888061,0.00024543487],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9996004,0.000002944439,0.00009894197,0.00013713515,0.00007328333,0.00008726673],"domain_scores_gemma":[0.9997378,0.000016325554,0.00007114235,0.00013631594,0.000010326615,0.000028097036],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00005500298,0.000064093445,0.000098675606,3.7317372e-7,0.0000729045,0.0000044490575,0.000065106644,0.000025491,0.00018680625],"category_scores_gemma":[0.0000017130146,0.000054163385,0.000029190098,0.000107230015,0.000106575164,0.0000206127,0.000024239751,0.000022988304,0.00007219577],"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":[0.00008615674,0.00064410403,0.0066869045,0.0034895046,0.000051460232,9.511231e-8,0.0007141368,0.000050777777,0.06157511,0.0700876,0.026887063,0.8297271],"study_design_scores_gemma":[0.0012406892,0.00039414773,0.023515528,0.00049477315,0.00024369376,6.66576e-7,0.00011377944,0.0008643277,0.028284168,0.059814006,0.8843085,0.00072568865],"about_ca_topic_score_codex":0.000007987869,"about_ca_topic_score_gemma":0.000002741917,"teacher_disagreement_score":0.85742146,"about_ca_system_score_codex":0.0000087689405,"about_ca_system_score_gemma":0.000005434397,"threshold_uncertainty_score":0.22087188},"labels":[],"label_agreement":null},{"id":"W2905409521","doi":"10.1175/jas-d-18-0278.1","title":"Parameterization of the Bulk Liquid Fraction on Mixed-Phase Particles in the Predicted Particle Properties (P3) Scheme: Description and Idealized Simulations","year":2018,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; Université du Québec à Montréal","funders":"Fonds de recherche du Québec – Nature et technologies; Natural Sciences and Engineering Research Council of Canada; Fonds Québécois de la Recherche sur la Nature et les Technologies; Université du Québec à Montréal","keywords":"Sublimation (psychology); Snow; Condensation; Materials science; Precipitation; Cloud physics; Ice crystals; Particle (ecology); Mechanics; Thermodynamics; Liquid water content; Phase (matter); Meteorology; Physics; Geology; Computer science","score_opus":0.031824391083307806,"score_gpt":0.27049015815266386,"score_spread":0.23866576706935605,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2905409521","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":[0.997346,0.000060704722,0.00039759194,0.0017127685,0.00022549294,0.00018898866,8.2351255e-7,0.00000447432,0.00006317544],"genre_scores_gemma":[0.9981627,0.000019701596,0.0014453554,0.00029149273,0.000048693568,0.0000038878775,5.6240395e-8,0.0000038455582,0.000024293824],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9985631,0.00024635682,0.00035712848,0.00012192726,0.0005561377,0.00015531835],"domain_scores_gemma":[0.9992441,0.00007523176,0.0004315,0.00018154705,0.00003477361,0.000032869175],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00074288767,0.00008367574,0.00011271693,7.096807e-7,0.00043375848,0.00006664835,0.00043002452,0.000032859094,0.00008235263],"category_scores_gemma":[0.00033236595,0.00003528397,0.000052539628,0.0007896634,0.0010920984,0.00038681336,0.00008804248,0.00010544715,0.0000022142106],"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":[0.00078812917,0.00081390934,0.29503965,0.000011583947,0.000023381404,0.0000012346195,0.006141365,0.12424055,0.5649586,0.00029230525,0.0005546241,0.0071346834],"study_design_scores_gemma":[0.0010670787,0.0025233603,0.35753095,0.00013638572,0.000053980053,0.000025703928,0.0026762544,0.58642197,0.047544606,0.0013680342,0.00051288464,0.00013877027],"about_ca_topic_score_codex":0.0001227623,"about_ca_topic_score_gemma":0.000069119094,"teacher_disagreement_score":0.517414,"about_ca_system_score_codex":0.000051579238,"about_ca_system_score_gemma":0.000032891883,"threshold_uncertainty_score":0.40238822},"labels":[],"label_agreement":null},{"id":"W2905962561","doi":"10.5194/amt-12-3269-2019","title":"Detecting layer height of smoke aerosols over vegetated land and water surfaces via oxygen absorption bands: hourly results from EPIC/DSCOVR in deep space","year":2019,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":71,"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":"Office of Naval Research; Multidisciplinary University Research Initiative; University of Maryland, Baltimore County; National Aeronautics and Space Administration","keywords":"Aerosol; AERONET; Environmental science; Remote sensing; Atmospheric sciences; Radiative transfer; Lidar; Meteorology; Geology; Physics; Optics","score_opus":0.01371510687956949,"score_gpt":0.21101888104340927,"score_spread":0.1973037741638398,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2905962561","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":[0.9937478,0.00037718232,0.0029322272,0.00008787757,0.00008817957,0.0007288645,0.000006209949,0.00015186697,0.0018798107],"genre_scores_gemma":[0.98390293,0.00015120312,0.015632173,0.00009265935,0.000026689002,0.0000400521,0.000011589305,0.000041344825,0.000101363185],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9973373,0.00013969741,0.00062987977,0.0006599452,0.00076533534,0.00046788348],"domain_scores_gemma":[0.9990739,0.000055679444,0.0002627553,0.000463516,0.000041672098,0.00010246236],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0010368484,0.00033716692,0.00044487402,0.0000016467081,0.000078264464,0.000045625828,0.00025604162,0.00020618063,0.0008588211],"category_scores_gemma":[0.000041821644,0.00025598385,0.00007367966,0.00024884997,0.00011177804,0.00032529666,0.00020130057,0.0002197166,0.00005022433],"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":[0.00016915989,0.00008593225,0.62469,0.000023324474,0.000035191762,0.0000045949882,0.000738515,0.0005648473,0.36833316,0.0000015439557,0.00008714291,0.0052666273],"study_design_scores_gemma":[0.0014039795,0.0003590647,0.6537447,0.00020660175,0.000041510288,0.0000029997975,0.00014743792,0.0058630877,0.3362933,0.00042420224,0.00095073285,0.0005623921],"about_ca_topic_score_codex":0.012053604,"about_ca_topic_score_gemma":0.0017546706,"teacher_disagreement_score":0.03203983,"about_ca_system_score_codex":0.00024244827,"about_ca_system_score_gemma":0.000011899215,"threshold_uncertainty_score":0.9999892},"labels":[],"label_agreement":null},{"id":"W2906235231","doi":"10.1029/2018jd029518","title":"A New Stochastic Model for the Boundary Layer Clouds and Stratocumulus Phase Transition Regimes: Open Cells, Closed Cells, and Convective Rolls","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland; University of Victoria","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Statistical physics; Convection; Forcing (mathematics); Metastability; Convection cell; Mechanics; Physics; Meteorology; Atmospheric sciences; Natural convection; Combined forced and natural convection","score_opus":0.04405919395400496,"score_gpt":0.3470133502866404,"score_spread":0.3029541563326354,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2906235231","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":[0.8411007,0.0003276993,0.15597664,0.0011208461,0.000099077915,0.0009566594,0.000019302493,0.0000072335465,0.00039182696],"genre_scores_gemma":[0.9889849,0.00010229745,0.008633898,0.00018860474,0.00044731708,0.000021709635,6.0805024e-7,0.00002824417,0.0015924321],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99784976,0.00016251627,0.0003509389,0.00034759543,0.0007660076,0.00052319036],"domain_scores_gemma":[0.998304,0.00068042276,0.00017879419,0.00024050666,0.00014968668,0.00044660785],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00095414935,0.00020354676,0.0003474627,0.000001667342,0.00066989876,0.0003705933,0.0005845155,0.0000949214,0.000343151],"category_scores_gemma":[0.000089138106,0.00013155355,0.00010653802,0.000250479,0.0011178906,0.00050679984,0.00031843188,0.00050779927,0.000024580564],"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":[0.024512466,0.0035365913,0.00025031343,0.00015586888,0.0010412689,0.00011124084,0.028165933,0.027985234,0.35325894,0.002759369,0.1907926,0.36743015],"study_design_scores_gemma":[0.009503656,0.00946145,0.0024211523,0.00012753475,0.00018476076,0.000033959124,0.0035842434,0.9183932,0.010397209,0.040755052,0.004661382,0.00047639542],"about_ca_topic_score_codex":0.0011514232,"about_ca_topic_score_gemma":0.0002451424,"teacher_disagreement_score":0.890408,"about_ca_system_score_codex":0.00011707901,"about_ca_system_score_gemma":0.00028590212,"threshold_uncertainty_score":0.5364598},"labels":[],"label_agreement":null},{"id":"W2909045417","doi":"10.1007/s00376-018-7308-2","title":"Determining Atmospheric Boundary Layer Height with the Numerical Differentiation Method Using Bending Angle Data from COSMIC","year":2019,"lang":"en","type":"article","venue":"Advances in Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ministry of Education and Child Care","funders":"","keywords":"COSMIC cancer database; Regularization (linguistics); Planetary boundary layer; Numerical differentiation; Physics; Second derivative; Computational physics; Radio occultation; Astrophysics; Mathematical analysis; Mathematics; Meteorology; Geology; Boundary layer; Mechanics; Computer science","score_opus":0.025236513846533585,"score_gpt":0.3029840936021026,"score_spread":0.277747579755569,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2909045417","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":[0.8579441,0.0013518108,0.13642529,0.00012775305,0.00044441456,0.0003260615,0.000006735567,0.000053864816,0.0033200346],"genre_scores_gemma":[0.7167681,0.00010869903,0.28254825,0.0003178884,0.000062030034,0.000014480859,0.000008287652,0.00002350539,0.00014876622],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99670017,0.00020296489,0.00038144618,0.0011697111,0.0008693383,0.00067637773],"domain_scores_gemma":[0.9982664,0.00044972342,0.00034133322,0.0008292948,0.000010434387,0.00010279542],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00064236444,0.00033928818,0.000375281,6.298798e-7,0.0006080176,0.00021484982,0.0017384621,0.000076288576,0.0026927663],"category_scores_gemma":[0.00003840477,0.00021203126,0.000051076255,0.0015563439,0.0006768267,0.0021742654,0.0008166061,0.00026115504,0.00013235075],"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":[0.00003340847,0.000070098475,0.8056249,0.0000073667593,0.000014481393,0.000010439001,0.0005719047,0.15000518,0.0015671194,0.000047712045,0.000085856605,0.04196154],"study_design_scores_gemma":[0.0004843489,0.00019522403,0.097865015,0.00006815124,0.00003136405,0.000018104745,0.002170117,0.8889551,0.00015067852,0.00060037896,0.008972792,0.0004887192],"about_ca_topic_score_codex":0.0008962042,"about_ca_topic_score_gemma":0.00038701872,"teacher_disagreement_score":0.7389499,"about_ca_system_score_codex":0.00022574714,"about_ca_system_score_gemma":0.000070476,"threshold_uncertainty_score":0.9982189},"labels":[],"label_agreement":null},{"id":"W2911806957","doi":"10.5194/acp-19-8879-2019","title":"Is positive correlation between cloud droplet effective radius and aerosol optical depth over land due to retrieval artifacts or real physical processes?","year":2019,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ocean Networks Canada Society; University of Victoria","funders":"Government of Jiangsu Province; National Natural Science Foundation of China; National Aeronautics and Space Administration","keywords":"Aerosol; Effective radius; Liquid water path; Environmental science; Moderate-resolution imaging spectroradiometer; Atmospheric sciences; Cloud top; Liquid water content; Meteorology; Climatology; Cloud computing; Satellite; Geology; Geography; Physics","score_opus":0.005118729572245155,"score_gpt":0.2275903694109147,"score_spread":0.22247163983866955,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2911806957","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":[0.9903609,0.0000144797705,0.0020500156,0.00006474008,0.000039380746,0.00044039325,0.000017389142,0.000037283815,0.0069753816],"genre_scores_gemma":[0.9960738,0.00002041146,0.0015138264,0.00015884651,0.00034467422,0.000014208902,0.000023721124,0.000028913055,0.0018216006],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985699,0.0000241869,0.00016931741,0.000590529,0.0003073049,0.00033873215],"domain_scores_gemma":[0.9991592,0.00024071189,0.00008838411,0.00021696986,0.000020714466,0.00027398946],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006940623,0.00028981414,0.00036474434,3.655258e-8,0.00013713521,0.00006281572,0.00009681872,0.00013857654,0.00052433665],"category_scores_gemma":[0.00003105991,0.00024109732,0.0000488144,0.0003295308,0.00018555016,0.00019805168,0.00016006512,0.00023582937,0.00013826876],"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":[0.0013038518,0.0004213043,0.8306695,0.00034918022,0.0001818129,0.000057301728,0.004785887,0.0012072369,0.043627433,0.00003988425,0.00075773493,0.116598874],"study_design_scores_gemma":[0.001982186,0.00080073945,0.9012829,0.00011687654,0.00020419076,0.000052146668,0.00019150137,0.020556038,0.07274086,0.00055104913,0.00051318976,0.0010083049],"about_ca_topic_score_codex":0.00013314413,"about_ca_topic_score_gemma":0.000005763624,"teacher_disagreement_score":0.11559057,"about_ca_system_score_codex":0.000102766695,"about_ca_system_score_gemma":0.000030225283,"threshold_uncertainty_score":0.98316634},"labels":[],"label_agreement":null},{"id":"W2912696810","doi":"10.5194/acp-19-1173-2019","title":"Long-range-transported Canadian smoke plumes in the lower stratosphere over northern France","year":2019,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":187,"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":"Horizon 2020 Framework Programme; Vedecká Grantová Agentúra MŠVVaŠ SR a SAV; Russian Science Foundation; Centre National de la Recherche Scientifique; Association Nationale de la Recherche et de la Technologie; Agence Nationale de la Recherche; National Aeronautics and Space Administration","keywords":"Stratosphere; Smoke; Aerosol; Lidar; Atmospheric sciences; Environmental science; Radiosonde; Troposphere; Plume; Depolarization ratio; Meteorology; Remote sensing; Geology; Physics","score_opus":0.003262339406625791,"score_gpt":0.18244752386212051,"score_spread":0.17918518445549472,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2912696810","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":[0.9776399,0.00019007782,0.00005195917,0.000108612956,0.0000523435,0.0001840015,0.000009224177,0.00001793077,0.021745937],"genre_scores_gemma":[0.9942941,0.000042798903,0.00022836417,0.00057807873,0.00007591965,0.000015136356,0.000012034787,0.000021986483,0.004731553],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99875075,0.000015684378,0.000173242,0.00037730517,0.00025094635,0.00043204904],"domain_scores_gemma":[0.9993656,0.000028007637,0.000054988588,0.00039411584,0.0000068344193,0.00015041101],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000087834356,0.00023182124,0.00018769587,1.31162246e-8,0.000107557375,0.000041475505,0.000314166,0.00012028933,0.011325186],"category_scores_gemma":[0.000002316755,0.00018373616,0.000067636305,0.00030556493,0.00016085443,0.00013846444,0.000024206265,0.0002611417,0.00014379837],"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":[0.000010442188,0.00007869408,0.9801727,0.000023046556,0.000011594107,0.000027365426,0.00064685504,0.001316286,0.000335901,0.000007903656,0.00016373006,0.017205471],"study_design_scores_gemma":[0.00049475225,0.000036191817,0.9838724,0.000024021718,0.000017421806,0.0000064411356,0.0003040414,0.004321989,0.000113168564,0.00021564231,0.010230923,0.000362985],"about_ca_topic_score_codex":0.05153022,"about_ca_topic_score_gemma":0.031855643,"teacher_disagreement_score":0.019674575,"about_ca_system_score_codex":0.000084455496,"about_ca_system_score_gemma":0.000050588842,"threshold_uncertainty_score":0.9895786},"labels":[],"label_agreement":null},{"id":"W2918484584","doi":"10.1063/1.5082157","title":"Mie scattering from strongly absorbing airborne particles in a photophoretic trap","year":2019,"lang":"en","type":"article","venue":"Journal of Applied Physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Mie scattering; Scattering; Light scattering; Optics; Attenuation; Refractive index; Polystyrene; Multiangle light scattering; Materials science; Spectral line; Particle (ecology); Aerosol; Rayleigh scattering; Molecular physics; Chemistry; Physics","score_opus":0.007549456252392815,"score_gpt":0.20008224896516305,"score_spread":0.19253279271277024,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2918484584","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":[0.9963252,0.000021858948,0.0003553773,0.000027437856,0.000085369655,0.0000871359,0.000001087702,0.000005243079,0.0030912869],"genre_scores_gemma":[0.99760425,0.000010205901,0.002145439,0.0001025224,0.000103957245,0.000002395798,4.9452143e-7,0.0000146027505,0.000016107493],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9990932,0.000009548838,0.000288134,0.00013712324,0.00026729697,0.00020470652],"domain_scores_gemma":[0.99954695,0.000033309618,0.00020602759,0.00013797886,0.000004278886,0.00007148468],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000111098256,0.00010899049,0.00021158379,0.0000011184057,0.000024715939,0.000023179351,0.00019550361,0.000035284505,0.00072692055],"category_scores_gemma":[0.0000015090617,0.00009424181,0.00006743415,0.00014177215,0.00006736888,0.0001173853,0.00006223117,0.00019755977,0.0001920917],"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":[0.00016852553,0.00023623012,0.0954019,0.000009896624,0.000033730015,0.000017985461,0.0024505872,0.18925865,0.6875985,0.00020446039,0.00017855868,0.024440961],"study_design_scores_gemma":[0.0039152727,0.00033076483,0.7616148,0.00016136811,0.00007846346,0.000010149459,0.0026412043,0.056285348,0.1526778,0.020526415,0.0010367368,0.0007216824],"about_ca_topic_score_codex":0.00006144028,"about_ca_topic_score_gemma":0.00000825985,"teacher_disagreement_score":0.6662129,"about_ca_system_score_codex":0.000103231876,"about_ca_system_score_gemma":0.000010952824,"threshold_uncertainty_score":0.79592705},"labels":[],"label_agreement":null},{"id":"W2918894268","doi":"10.5194/amt-12-3673-2019","title":"The Mineral Aerosol Profiling from Infrared Radiances (MAPIR) algorithm: version 4.1 description and evaluation","year":2019,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":22,"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":"European Centre for Medium-Range Weather Forecasts; European Organization for the Exploitation of Meteorological Satellites; National Aeronautics and Space Administration; Institut de Recherche pour le Développement; European Space Agency; McGill University; Belgian Federal Science Policy Office","keywords":"Aerosol; Environmental science; Radiative transfer; AERONET; Atmospheric radiative transfer codes; Remote sensing; Mineral dust; Radiance; Meteorology; Physics; Geology","score_opus":0.01750460602265865,"score_gpt":0.2232013120499609,"score_spread":0.20569670602730225,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2918894268","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":[0.97697014,0.0013017934,0.010423486,0.00020384206,0.00031146122,0.0015895811,0.0000028083944,0.00023421073,0.008962682],"genre_scores_gemma":[0.85494673,0.00036645343,0.14338063,0.000244986,0.00009242641,0.00024420573,0.000016196269,0.000028065215,0.0006803214],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9975937,0.00015429163,0.0003017042,0.00045543647,0.001181321,0.0003135731],"domain_scores_gemma":[0.99925596,0.000038371058,0.0001767005,0.00037423492,0.0000659441,0.00008882353],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011919772,0.00022295753,0.00017721526,4.2409675e-7,0.00031929152,0.00012350717,0.0002573582,0.0001085704,0.0008132097],"category_scores_gemma":[0.000048912112,0.00016269812,0.00005596077,0.0002003997,0.00014526388,0.0003957371,0.00012898585,0.00014469562,0.00012705928],"study_design_candidate":"design_other","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":[0.000074703974,0.00009923403,0.15061562,0.000011510844,0.00005514957,0.0000016079825,0.0003230011,0.0001182588,0.20047224,0.00004624206,0.013006082,0.63517636],"study_design_scores_gemma":[0.0041545862,0.0021862572,0.28026918,0.000491787,0.00046841375,0.000015386948,0.0033217191,0.3269332,0.20527866,0.0134608485,0.16060425,0.0028157097],"about_ca_topic_score_codex":0.00074701814,"about_ca_topic_score_gemma":0.00006902496,"teacher_disagreement_score":0.63236064,"about_ca_system_score_codex":0.00047085137,"about_ca_system_score_gemma":0.000034594363,"threshold_uncertainty_score":0.89040756},"labels":[],"label_agreement":null},{"id":"W2920033347","doi":"10.5194/amt-2019-34","title":"Calibration of the 2007–2017 record of ARM Cloud Radar Observations using CloudSat","year":2019,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Office of Science","keywords":"Radar; Environmental science; Cloud computing; Remote sensing; Calibration; Meteorology; Precipitation; Computer science; Geology; Telecommunications; Geography; Physics","score_opus":0.026324500130514922,"score_gpt":0.2292112760682253,"score_spread":0.20288677593771037,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2920033347","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":[0.9829246,0.000011131211,0.0028757772,0.00014392393,0.00042955237,0.00018538017,0.0000034199695,0.000008917215,0.013417298],"genre_scores_gemma":[0.9856586,0.000009356536,0.010136067,0.00018091289,0.00003520775,0.0000010884663,0.0000012626205,0.000007351072,0.003970179],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992841,0.00003114866,0.00023000855,0.00013195619,0.0002113254,0.00011146662],"domain_scores_gemma":[0.9994308,0.000026278643,0.00017671539,0.00033146233,0.000008308791,0.000026477346],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00010968413,0.000071126604,0.00011504367,5.244454e-7,0.00005927962,0.0000049973964,0.00021607436,0.000047480735,0.004962255],"category_scores_gemma":[0.000013955955,0.000047240144,0.00006397723,0.00017721832,0.00011159351,0.00013041185,0.00013295379,0.000052351646,0.00003018496],"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":[0.000013442941,0.00009411897,0.860327,0.000011942316,0.000010629997,1.4652133e-7,0.0002342106,0.0049395678,0.12587671,0.00210806,0.0053909095,0.0009932601],"study_design_scores_gemma":[0.00091345236,0.0002656514,0.7956489,0.00007417117,0.00007306889,0.0000063410885,0.0011163774,0.10881259,0.062123824,0.0031460102,0.027327674,0.0004919628],"about_ca_topic_score_codex":0.001985382,"about_ca_topic_score_gemma":0.00010615943,"teacher_disagreement_score":0.10387302,"about_ca_system_score_codex":0.000043238924,"about_ca_system_score_gemma":0.000016912712,"threshold_uncertainty_score":0.99594736},"labels":[],"label_agreement":null},{"id":"W2921264147","doi":"10.5194/amt-12-5897-2019","title":"Determination of ice water content (IWC) in tropical convective clouds from X-band dual-polarization airborne radar","year":2019,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; National Research Council Canada","funders":"Environment and Climate Change Canada; National Aeronautics and Space Administration","keywords":"Ice crystals; Remote sensing; Radar; Meteorology; Environmental science; Atmospheric sciences; Liquid water content; Polarization (electrochemistry); Geology; Physics; Chemistry","score_opus":0.017888639534052092,"score_gpt":0.21206082705104756,"score_spread":0.19417218751699547,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2921264147","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":[0.95122033,0.00007784737,0.044853114,0.00011776443,0.0001327422,0.00089119264,0.00000331821,0.00011453754,0.0025891806],"genre_scores_gemma":[0.96853936,0.00002560564,0.030862486,0.00017388121,0.000030757,0.00007239716,0.000011433556,0.00002850903,0.00025555276],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9976629,0.0001537102,0.0005428189,0.00047667566,0.000832314,0.00033158364],"domain_scores_gemma":[0.9992665,0.000039877865,0.00019127136,0.0003623591,0.00006589286,0.00007410033],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00044090216,0.0002494724,0.00037379726,0.000001189888,0.000050080802,0.000020725427,0.00021663962,0.00017117399,0.0018230765],"category_scores_gemma":[0.000049870778,0.00019515198,0.00008527511,0.00020575481,0.0001351827,0.00025817764,0.00009965572,0.00017314339,0.00009249668],"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":[0.00009685353,0.0002168929,0.4081402,0.000015367896,0.000017866085,0.0000048022594,0.00050334947,0.000023598928,0.5754057,0.00006280379,0.000085595355,0.015426949],"study_design_scores_gemma":[0.00076275435,0.00037147405,0.4305702,0.000080232756,0.00003169592,0.0000014667747,0.00019987837,0.00135665,0.56442225,0.00056241575,0.0013226712,0.00031832317],"about_ca_topic_score_codex":0.0023217346,"about_ca_topic_score_gemma":0.00023132008,"teacher_disagreement_score":0.022429984,"about_ca_system_score_codex":0.0005453576,"about_ca_system_score_gemma":0.000020755027,"threshold_uncertainty_score":0.9990894},"labels":[],"label_agreement":null},{"id":"W2921809760","doi":"10.1175/jcli-d-18-0648.1","title":"Accounting for Several Infrared Radiation Processes in Climate Models","year":2019,"lang":"en","type":"article","venue":"Journal of Climate","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":7,"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","funders":"","keywords":"Intertropical Convergence Zone; Environmental science; Longwave; Troposphere; Atmospheric sciences; Shortwave; Emissivity; Outgoing longwave radiation; Water vapor; Hadley cell; Climate model; Zenith; Climatology; Cloud albedo; Atmosphere (unit); Cloud cover; Radiative transfer; Precipitation; Meteorology; Physics; Remote sensing; Climate change; Geology; Convection","score_opus":0.008460623732220177,"score_gpt":0.2373451873579324,"score_spread":0.22888456362571222,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2921809760","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":[0.99122727,0.000068563924,0.0010636566,0.000094565614,0.00016157594,0.00016238843,0.000004363301,0.000006611765,0.007211001],"genre_scores_gemma":[0.9945755,0.00054443063,0.004488438,0.00019751787,0.00006391414,0.0000044760905,0.0000014920706,0.00001293915,0.00011130202],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990009,0.000013831097,0.0003941403,0.00010396586,0.0002151359,0.0002719907],"domain_scores_gemma":[0.9994041,0.000054934226,0.0004007639,0.00007273237,0.000024631223,0.000042878422],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046679575,0.00008549913,0.00018508655,0.000004000328,0.0000479449,0.00004038956,0.0001470123,0.00004880537,0.00029301984],"category_scores_gemma":[0.00003904215,0.000069813024,0.00005783896,0.00015275867,0.00001738158,0.00086858345,0.000057992227,0.000097515716,0.000043861102],"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":[0.00034433923,0.00013104224,0.7244319,0.00022322901,0.000013782276,0.000007345214,0.0014903946,0.2594068,0.0021056577,0.0001619131,0.0004930348,0.011190591],"study_design_scores_gemma":[0.0086660385,0.001110952,0.50342715,0.0005421308,0.00009315653,0.00012381397,0.0019514292,0.44857812,0.002171691,0.014074941,0.018223677,0.0010369056],"about_ca_topic_score_codex":0.0000074277905,"about_ca_topic_score_gemma":0.000009710453,"teacher_disagreement_score":0.22100472,"about_ca_system_score_codex":0.00010091738,"about_ca_system_score_gemma":0.000023494742,"threshold_uncertainty_score":0.32083616},"labels":[],"label_agreement":null},{"id":"W2921983865","doi":"10.1016/j.jastp.2019.03.006","title":"Long-term variation of dust episodes over the United Arab Emirates","year":2019,"lang":"en","type":"article","venue":"Journal of Atmospheric and Solar-Terrestrial Physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":19,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institut National de la Recherche Scientifique","funders":"","keywords":"Dust storm; Storm; Environmental science; Climatology; Atmospheric sciences; Wind speed; Asian Dust; Diurnal temperature variation; Meteorology; Geography; Aerosol; Geology","score_opus":0.011024061470065776,"score_gpt":0.22911160954080834,"score_spread":0.21808754807074257,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2921983865","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":[0.9920915,0.00010395782,0.0067959195,0.00008122362,0.000464493,0.0001655983,0.0000015815133,0.00000622922,0.0002895234],"genre_scores_gemma":[0.99809307,0.0001862106,0.0010003259,0.00012054461,0.00037965763,0.0000011952629,0.00000210626,0.000016780043,0.00020011018],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986455,0.00010160865,0.0004885741,0.00015226992,0.00040849118,0.00020355397],"domain_scores_gemma":[0.9988002,0.00014268342,0.0007369304,0.00020795384,0.000024712432,0.00008749165],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003120343,0.00017602506,0.00033399573,4.5474428e-7,0.00010341729,0.000056377776,0.00027638863,0.00009231243,0.00048080395],"category_scores_gemma":[0.000031156167,0.000112410606,0.00014931116,0.00031619138,0.00018852319,0.00035346317,0.00011073686,0.00026608736,0.000019078097],"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":[0.00040458704,0.000254841,0.9617327,0.00002283667,0.00015319245,0.000011185669,0.0011693964,0.013121234,0.0066781538,0.00022279406,0.0004925116,0.015736585],"study_design_scores_gemma":[0.0015356261,0.0004924879,0.98732907,0.000055205976,0.00010712421,0.000017503738,0.00014851162,0.008269075,0.00028606373,0.0011222938,0.00044995834,0.00018708911],"about_ca_topic_score_codex":0.00022956361,"about_ca_topic_score_gemma":0.0000051521693,"teacher_disagreement_score":0.02559638,"about_ca_system_score_codex":0.000056458546,"about_ca_system_score_gemma":0.000036603702,"threshold_uncertainty_score":0.5264466},"labels":[],"label_agreement":null},{"id":"W2922978381","doi":"10.5194/acp-2019-223","title":"Retrieving the global distribution of threshold of wind erosion from satellite data and implementing it into the GFDL AM4.0/LM4.0 model","year":2019,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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 de Sherbrooke","funders":"National Park Service; National Aeronautics and Space Administration; NASA Astrobiology Institute; National Oceanic and Atmospheric Administration; Desert Research Institute; University of California, Davis; Princeton University; U.S. Environmental Protection Agency","keywords":"Environmental science; Moderate-resolution imaging spectroradiometer; Aerosol; Satellite; Aeolian processes; Atmosphere (unit); Wind speed; Atmospheric sciences; Climatology; Erosion; Spatial distribution; Meteorology; Remote sensing; Geology; Physics","score_opus":0.017193772728137855,"score_gpt":0.25506353864790826,"score_spread":0.2378697659197704,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2922978381","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":[0.99116856,0.00018850653,0.0058412342,0.00025917977,0.00002453791,0.0001698518,0.00011309767,0.000004259849,0.0022307457],"genre_scores_gemma":[0.99873024,0.00014358858,0.0009309108,0.00005593152,0.000008270886,4.713826e-7,0.00005518831,0.0000037622613,0.00007161564],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99904364,0.000022873237,0.00028825254,0.00021923445,0.00028468293,0.00014131308],"domain_scores_gemma":[0.9991239,0.00005802626,0.00018866845,0.0005969409,0.000008477297,0.00002402377],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004606273,0.00008278792,0.00013153834,2.592817e-7,0.00008039762,0.000013354717,0.00047997985,0.000037927115,0.0003169102],"category_scores_gemma":[0.000020144334,0.000044149405,0.000028193444,0.00014474451,0.00020076353,0.00016028606,0.0011907313,0.000057204277,0.000004950881],"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":[0.000023968925,0.00002341348,0.95810056,0.000009838379,0.000013688287,6.38086e-8,0.0006933567,0.0013841814,0.031967558,0.0009789104,0.00030236156,0.006502081],"study_design_scores_gemma":[0.0004813217,0.00009184865,0.638006,0.0000672035,0.00007697086,7.662739e-7,0.0038765275,0.34024754,0.011356841,0.0040459204,0.0015607697,0.00018833729],"about_ca_topic_score_codex":0.0026743799,"about_ca_topic_score_gemma":0.0003667342,"teacher_disagreement_score":0.33886334,"about_ca_system_score_codex":0.000035108995,"about_ca_system_score_gemma":0.000008530712,"threshold_uncertainty_score":0.404288},"labels":[],"label_agreement":null},{"id":"W2923568062","doi":"10.5194/amt-12-4591-2019","title":"Development and validation of a supervised machine learning radar Doppler spectra peak-finding algorithm","year":2019,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Leibniz-Institut für Troposphärenforschung; Leibniz-Gemeinschaft; Office of Science; Biological and Environmental Research; European Commission; Deutsche Forschungsgemeinschaft; U.S. Department of Energy","keywords":"Algorithm; Radar; Doppler effect; Doppler radar; Zenith; Remote sensing; Computer science; Smoothing; Spectral line; Cloud computing; Meteorology; Environmental science; Geology; Physics; Computer vision","score_opus":0.01818093698511782,"score_gpt":0.21546254477705434,"score_spread":0.19728160779193651,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2923568062","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":[0.92660654,0.00025100904,0.0649767,0.000052972573,0.00006636007,0.0007080986,9.693581e-7,0.00025892767,0.007078415],"genre_scores_gemma":[0.53648996,0.0000629161,0.46301636,0.000041874257,0.000014346751,0.00003089339,0.0000056315193,0.00002533112,0.00031266682],"study_design_codex":"design_other","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9979256,0.000072813054,0.00041451768,0.00041965317,0.00085459853,0.00031283015],"domain_scores_gemma":[0.99940884,0.00001704218,0.00020869124,0.00024130545,0.000032018434,0.00009213001],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00088388927,0.00024842314,0.0002934597,0.0000010894901,0.00013489492,0.000030491443,0.000203437,0.00008888906,0.0018243256],"category_scores_gemma":[0.000023412242,0.00022240567,0.000054272758,0.00027347638,0.00007684882,0.00018600699,0.00017916477,0.00017425789,0.000055489883],"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":[0.000034411172,0.00019134206,0.2606764,0.000077068566,0.00007809152,0.0000055816236,0.0017073137,0.00010728725,0.29824257,0.00009412133,0.00036878441,0.438417],"study_design_scores_gemma":[0.0012858714,0.00068097725,0.07069405,0.00024979154,0.000085504886,0.00003288578,0.00085210614,0.013227419,0.84532917,0.00027496167,0.06602655,0.0012607335],"about_ca_topic_score_codex":0.00032324324,"about_ca_topic_score_gemma":0.000016722135,"teacher_disagreement_score":0.5470866,"about_ca_system_score_codex":0.00029670706,"about_ca_system_score_gemma":0.00003173949,"threshold_uncertainty_score":0.99908817},"labels":[],"label_agreement":null},{"id":"W2926227414","doi":"10.1002/qj.3543","title":"Accelerating radiative transfer calculations for high‐resolution atmospheric models","year":2019,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Environment and Climate Change Canada","keywords":"Radiative transfer; Radiative flux; Column (typography); Atmospheric radiative transfer codes; Meteorology; Environmental science; Physics; Mathematics; Geometry; Optics","score_opus":0.014371801533824903,"score_gpt":0.21562837225452836,"score_spread":0.20125657072070346,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2926227414","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":[0.8253861,0.000055105145,0.17298692,0.0005599712,0.0002609638,0.00030088905,0.000004733683,0.000011161783,0.00043412906],"genre_scores_gemma":[0.9630728,0.0000035648432,0.035908308,0.00047221076,0.000115042785,0.000012258855,7.917591e-7,0.000011819921,0.0004032525],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9985881,0.00013532968,0.00042103566,0.00019507756,0.0003562277,0.0003042675],"domain_scores_gemma":[0.99933314,0.0001702998,0.000205603,0.00015935322,0.00003496854,0.00009663919],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005017261,0.0001588965,0.00028207246,3.0815315e-7,0.0002856565,0.00003848215,0.00038333287,0.00015384449,0.0010777315],"category_scores_gemma":[0.000017484093,0.000090064226,0.0005943217,0.00015188438,0.00013887238,0.00021053513,0.000034438053,0.00029696658,0.00002012575],"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":[0.00012865812,0.00017823277,0.012289526,0.000009161721,0.0001386725,8.4155334e-7,0.0023726511,0.9650606,0.0030055651,0.0025671904,0.0020161048,0.012232833],"study_design_scores_gemma":[0.0016252596,0.0023345316,0.08513621,0.000015713415,0.00013268995,0.000008148858,0.0010252472,0.89373094,0.00013619935,0.014888096,0.0006913719,0.0002755792],"about_ca_topic_score_codex":0.00005928662,"about_ca_topic_score_gemma":0.0000047059852,"teacher_disagreement_score":0.13768663,"about_ca_system_score_codex":0.00017955383,"about_ca_system_score_gemma":0.000017935066,"threshold_uncertainty_score":0.99983543},"labels":[],"label_agreement":null},{"id":"W2926707308","doi":"10.1175/jas-d-18-0168.1","title":"The Importance of the Ice-Phase Microphysics Parameterization for Simulating the Effects of Changes to CCN Concentrations in Deep Convection","year":2019,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":19,"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":"Graupel; Squall line; Environmental science; Ice crystals; Atmospheric sciences; Mesoscale meteorology; Cloud condensation nuclei; Precipitation; Orography; Meteorology; Storm; Weather Research and Forecasting Model; Cloud physics; Convection; Geology; Aerosol; Physics; Cloud computing; Computer science","score_opus":0.00713337599069399,"score_gpt":0.2543381142171232,"score_spread":0.24720473822642922,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2926707308","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":[0.9956936,0.0001345591,0.0011925837,0.0016479687,0.0007059843,0.0005621933,7.088218e-7,0.0000015047721,0.000060868202],"genre_scores_gemma":[0.99783325,0.000026628197,0.0016248161,0.00038073256,0.000038189446,0.000008372755,4.3340023e-8,0.0000046291325,0.00008332701],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9988794,0.00011055997,0.00033854513,0.000112745576,0.00038804274,0.00017070524],"domain_scores_gemma":[0.998293,0.0006247562,0.0008053384,0.00021355815,0.000037962862,0.000025429985],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00065833423,0.00008322439,0.00014420289,3.980346e-7,0.00035140105,0.000035892008,0.00072796113,0.000025428653,0.000018268149],"category_scores_gemma":[0.00032586526,0.000033583587,0.00009979627,0.00076594215,0.0004568806,0.00013297617,0.00010986471,0.00008741416,9.858765e-7],"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":[0.000074631746,0.00012511712,0.4422728,0.000029838551,0.000020883244,2.135469e-7,0.003060685,0.27874386,0.26573694,0.00031173864,0.00016379185,0.009459469],"study_design_scores_gemma":[0.0021613077,0.0023883698,0.40050784,0.0003184018,0.00012175397,0.000013371199,0.0063458923,0.45821738,0.12455375,0.003226243,0.0018332888,0.00031237578],"about_ca_topic_score_codex":0.00006452882,"about_ca_topic_score_gemma":0.00013526919,"teacher_disagreement_score":0.17947352,"about_ca_system_score_codex":0.00006385775,"about_ca_system_score_gemma":0.000044242188,"threshold_uncertainty_score":0.27027282},"labels":[],"label_agreement":null},{"id":"W2937970224","doi":"10.5194/acp-2019-289","title":"Towards continuous monitoring of aerosol hygroscopicity by Raman lidar measurements at the EARLINET station of Payerne","year":2019,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"Western University","funders":"European Commission; Université de Lille; Agencia Estatal de Investigación; Ministerio de Ciencia, Innovación y Universidades; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; Bundesamt für Umwelt; Ministerio de Economía y Competitividad; National Science Foundation","keywords":"Radiosonde; Aerosol; Lidar; Environmental science; Remote sensing; Altitude (triangle); Backscatter (email); Meteorology; Atmospheric sciences; Relative humidity; Geography; Geology","score_opus":0.013860289449085047,"score_gpt":0.23543503874269636,"score_spread":0.22157474929361132,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2937970224","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":[0.9897725,0.00005221156,0.0006957784,0.00007301374,0.00014081373,0.00026675485,0.000008530137,0.000012657478,0.008977736],"genre_scores_gemma":[0.9938327,0.000013594085,0.0011009625,0.000042712592,0.000013499428,0.0000060917164,0.000003450293,0.000009232975,0.0049777487],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99886066,0.00003917596,0.0002548122,0.00017722556,0.0005018328,0.00016631752],"domain_scores_gemma":[0.9995071,0.00002085513,0.00016704448,0.0002461159,0.000017502289,0.000041366886],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00022494407,0.000101194215,0.00016943738,5.358309e-7,0.000047129986,0.00000857468,0.00019820237,0.000045117904,0.0022753705],"category_scores_gemma":[0.000014879804,0.000065803164,0.000045528566,0.00008965133,0.000109135864,0.00008231199,0.00014971859,0.000056512577,0.000107087166],"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":[0.000016696757,0.000045900044,0.7108151,0.000007871118,0.0000102695685,7.016279e-8,0.00021193817,0.00020100638,0.2856056,0.0000030057893,0.0007380297,0.0023445305],"study_design_scores_gemma":[0.0005069767,0.0001946917,0.29218534,0.000017121192,0.000014760791,3.1988114e-7,0.00047969283,0.00014022863,0.70585775,0.000013478854,0.000477625,0.00011203076],"about_ca_topic_score_codex":0.0026484716,"about_ca_topic_score_gemma":0.000051171046,"teacher_disagreement_score":0.4202521,"about_ca_system_score_codex":0.000086157524,"about_ca_system_score_gemma":0.0000072353273,"threshold_uncertainty_score":0.99863666},"labels":[],"label_agreement":null},{"id":"W2942617881","doi":"10.3390/rs11090994","title":"Alternate Mapping Correlated k-Distribution Method for Infrared Radiative Transfer Forward Simulation","year":2019,"lang":"en","type":"article","venue":"Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":19,"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 Natural Science Foundation of China","keywords":"Longwave; Environmental science; Remote sensing; Radiative transfer; Atmospheric radiative transfer codes; Satellite; Brightness; Meteorology; Physics; Optics; Geology","score_opus":0.011783061049451328,"score_gpt":0.25642160706727796,"score_spread":0.24463854601782664,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2942617881","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.36073634,0.000011279976,0.6372471,0.00004409483,0.00015217983,0.00032566214,0.000007560557,0.000039620547,0.0014361532],"genre_scores_gemma":[0.9119841,0.000005870668,0.0868117,0.00016212024,0.00004103131,4.823466e-8,0.00005169229,0.000019964898,0.0009234865],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99901515,0.000057887744,0.00021100379,0.0002865381,0.00016807826,0.0002613511],"domain_scores_gemma":[0.9995669,0.00014080176,0.00006193586,0.00015130031,0.00001792273,0.000061137864],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023629447,0.00013278228,0.00017058,0.000001906169,0.000118256256,0.000025271194,0.000057998954,0.0000990123,0.00013340887],"category_scores_gemma":[0.0000386233,0.0001295244,0.000093720315,0.00018027765,0.000026928115,0.0001413119,0.000027216374,0.00010119865,0.00013494628],"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":[0.00007162494,0.000007409315,0.00056868425,0.000013121434,0.000028352013,0.000002440668,0.0009430481,0.7299673,0.027508477,0.00003409701,0.00011192737,0.2407435],"study_design_scores_gemma":[0.0005980535,0.000043399275,0.0018262763,0.000029584255,0.000019034676,0.000004851944,0.00011566216,0.9890037,0.0016361244,0.0009827627,0.005569816,0.0001707294],"about_ca_topic_score_codex":0.00020381653,"about_ca_topic_score_gemma":0.0000069359685,"teacher_disagreement_score":0.5512477,"about_ca_system_score_codex":0.00023638047,"about_ca_system_score_gemma":0.00000858819,"threshold_uncertainty_score":0.5281852},"labels":[],"label_agreement":null},{"id":"W2944636923","doi":"10.1175/jas-d-18-0366.1","title":"Entrapment: An Important Mechanism to Explain the Shortwave 3D Radiative Effect of Clouds","year":2019,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":57,"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":"Université de Toulouse; Agence Nationale de la Recherche","keywords":"Radiative transfer; Shortwave; Atmospheric radiative transfer codes; Parametrization (atmospheric modeling); Physics; Computational physics; Environmental science; Atmospheric sciences; Optics","score_opus":0.005136388016603518,"score_gpt":0.22783715736437704,"score_spread":0.22270076934777353,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2944636923","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":[0.9961033,0.000109199005,0.0002907032,0.0007879673,0.0009149756,0.00039158948,0.0000012384322,0.000005771241,0.0013952985],"genre_scores_gemma":[0.99443734,0.000031936666,0.004576445,0.0005314501,0.00009505091,0.000005039573,5.7637433e-8,0.000010112482,0.00031254132],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9974098,0.0002943691,0.0005522165,0.00025231755,0.001131866,0.00035939275],"domain_scores_gemma":[0.9984857,0.00021559137,0.0007293418,0.00038510346,0.000020811405,0.00016348212],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.002714861,0.00019249755,0.00033678015,7.679034e-7,0.00029527335,0.000055533183,0.0016466273,0.000049455142,0.0014503369],"category_scores_gemma":[0.00010221524,0.00008383136,0.0002062901,0.000837419,0.00043832575,0.00033126958,0.00029345963,0.00019272392,0.000039243754],"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":[0.00030512497,0.00023400376,0.77466124,0.000016278429,0.00012739994,0.000018115968,0.008788086,0.12772657,0.07047211,0.0009910015,0.0026599246,0.014000166],"study_design_scores_gemma":[0.0039771562,0.029354552,0.53309655,0.00044608043,0.000582603,0.0006507382,0.017338164,0.24081281,0.14639387,0.010001748,0.01542324,0.0019224804],"about_ca_topic_score_codex":0.0001389456,"about_ca_topic_score_gemma":0.000014237156,"teacher_disagreement_score":0.24156466,"about_ca_system_score_codex":0.00012926605,"about_ca_system_score_gemma":0.00006483473,"threshold_uncertainty_score":0.9994625},"labels":[],"label_agreement":null},{"id":"W2946502683","doi":"10.5194/amt-12-5801-2019","title":"Retrieval of temperature from a multiple channel pure rotational Raman backscatter lidar using an optimal estimation method","year":2019,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Canadian Space Agency; Strong","keywords":"Lidar; Calibration; Radiosonde; Remote sensing; Backscatter (email); Range (aeronautics); Environmental science; Computational physics; Meteorology; Physics; Materials science; Computer science; Mathematics; Statistics; Geology","score_opus":0.022288523467875184,"score_gpt":0.25978984291815466,"score_spread":0.23750131945027947,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2946502683","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":[0.80204874,0.00006656053,0.19636615,0.0000736466,0.00011152765,0.0007470273,0.000011329865,0.00015795008,0.00041704363],"genre_scores_gemma":[0.57012194,0.0000042050783,0.42955834,0.00014297206,0.000050443476,0.000020231271,0.000021909655,0.000029462892,0.00005050902],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9972465,0.00017992748,0.00047586742,0.0006001963,0.0011687638,0.00032876985],"domain_scores_gemma":[0.99889654,0.000043026655,0.00031624813,0.0005187968,0.00009870677,0.00012670494],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00081399985,0.00031596678,0.0003676549,0.0000011832698,0.00012426039,0.000053560332,0.00037192836,0.00023053064,0.0028288672],"category_scores_gemma":[0.00006415518,0.0002855858,0.00011971623,0.00036488954,0.00009443171,0.0004986268,0.0001403536,0.00023018353,0.000053385505],"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":[0.00023087263,0.0003722069,0.0456223,0.000030300254,0.00007117651,0.000003389354,0.000773583,0.030715642,0.91272795,0.000015162596,0.0006169167,0.008820483],"study_design_scores_gemma":[0.0009946519,0.00071367854,0.057151143,0.00020020407,0.00011853059,0.000011149466,0.0005092425,0.37372747,0.5641081,0.00070091954,0.0008682938,0.0008966761],"about_ca_topic_score_codex":0.0005468871,"about_ca_topic_score_gemma":0.000019828425,"teacher_disagreement_score":0.3486199,"about_ca_system_score_codex":0.00034870396,"about_ca_system_score_gemma":0.00005071509,"threshold_uncertainty_score":0.99995965},"labels":[],"label_agreement":null},{"id":"W2946928166","doi":"10.3390/atmos10060294","title":"Three-Dimensional Modelling of Precipitation Enhancement by Cloud Seeding in Three Different Climate Zones","year":2019,"lang":"en","type":"article","venue":"Atmosphere","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Precipitation; Seeding; Arid; Weather Research and Forecasting Model; Environmental science; Relative humidity; Cloud seeding; Atmospheric sciences; Climatology; Aerosol; Humidity; Climate change; Climate model; Cloud condensation nuclei; Meteorology; Geography; Geology; Oceanography","score_opus":0.011390087846658245,"score_gpt":0.20824513956733412,"score_spread":0.19685505172067588,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2946928166","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":[0.9681687,0.00022276287,0.029062975,0.00006321159,0.0002506653,0.0003445051,0.000004364399,0.000020656358,0.0018621796],"genre_scores_gemma":[0.9909822,0.00004377565,0.008566975,0.000050180464,0.000026251322,0.00002300055,0.000010677795,0.000022078806,0.0002748721],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9984592,0.00001801149,0.0003713654,0.00037613485,0.00041613478,0.0003591632],"domain_scores_gemma":[0.99947935,0.000052865074,0.00016457478,0.0002299071,0.000010032355,0.000063263244],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00016338058,0.00019478865,0.00025503407,3.35349e-7,0.00005968121,0.000013548215,0.00018407077,0.00008882796,0.0040315725],"category_scores_gemma":[0.000003645749,0.00016573108,0.000066118635,0.00014909534,0.00006519502,0.00016319868,0.00019560374,0.00012489411,0.0002719539],"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":[0.00007641197,0.00022621268,0.71705914,0.00003682473,0.000016657941,0.0000012637369,0.0003197304,0.26358297,0.013382788,0.00042501214,0.00056146615,0.0043115034],"study_design_scores_gemma":[0.001115465,0.00033452248,0.1188633,0.00017368197,0.000023199167,0.000001356141,0.0002591042,0.8706422,0.00488338,0.002977225,0.00026736478,0.00045921013],"about_ca_topic_score_codex":0.0008437699,"about_ca_topic_score_gemma":0.0006373777,"teacher_disagreement_score":0.6070592,"about_ca_system_score_codex":0.00014270896,"about_ca_system_score_gemma":0.0000070067217,"threshold_uncertainty_score":0.99687886},"labels":[],"label_agreement":null},{"id":"W2948650461","doi":"10.1029/2018jd029924","title":"Effects of Aerosols on the Precipitation of Convective Clouds: A Case Study in the Yangtze River Delta of China","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"Ministry of Education and Child Care","funders":"Nanjing Audit University; Ministry of Science and Technology of the People's Republic of China; National Natural Science Foundation of China","keywords":"Precipitation; Environmental science; Yangtze river; Precipitation types; Climatology; Atmospheric sciences; Convection; Cloud condensation nuclei; Delta; Water cycle; Convective available potential energy; Aerosol; Meteorology; China; Geography; Geology; Physics","score_opus":0.018106424833486356,"score_gpt":0.3049054730557864,"score_spread":0.28679904822230007,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2948650461","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":[0.99801254,0.00006128627,0.00003509808,0.00012914918,0.000049547285,0.0010069442,0.0000023402079,0.0000013572803,0.00070172036],"genre_scores_gemma":[0.99963367,0.000018094568,0.00015350891,0.00002133784,0.00004254922,0.000016758033,1.2364667e-7,0.000011225865,0.00010271363],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99632597,0.001138867,0.0005106718,0.00017823362,0.0015633166,0.00028291272],"domain_scores_gemma":[0.9957917,0.003218152,0.00045445972,0.0003333366,0.00013324432,0.00006914942],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018294859,0.00013467848,0.00039486407,0.0000024708168,0.00007557677,0.000015289732,0.00063198776,0.00005319646,0.00025237902],"category_scores_gemma":[0.000691706,0.00006825246,0.00016798826,0.00066711113,0.0006348337,0.00015280518,0.00019367789,0.0006153827,0.000024708108],"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":[0.0038285025,0.013516256,0.79430044,0.00032868638,0.0005147863,0.0010582603,0.08873413,0.0067546493,0.071253814,0.0022613027,0.00222824,0.015220928],"study_design_scores_gemma":[0.0014194711,0.0073922635,0.9655805,0.00014943378,0.000034234185,0.000027512591,0.015357757,0.0008682859,0.0071568443,0.0019073779,0.000017606299,0.00008867869],"about_ca_topic_score_codex":0.0055610077,"about_ca_topic_score_gemma":0.00024812162,"teacher_disagreement_score":0.17128009,"about_ca_system_score_codex":0.0000937958,"about_ca_system_score_gemma":0.00006299925,"threshold_uncertainty_score":0.8406617},"labels":[],"label_agreement":null},{"id":"W2949105982","doi":"","title":"Microphysical properties of clouds over Eureka, Canada between 2006 and 2009","year":2010,"lang":"en","type":"article","venue":"13th Conference on Cloud Physics/13th Conference on Atmospheric Radiation (28 June–2 July 2010)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Environmental science; Meteorology; Atmospheric sciences; Geography; Geology","score_opus":0.015520601878958184,"score_gpt":0.213883801632573,"score_spread":0.19836319975361483,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2949105982","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":[0.98551536,0.000056328634,0.0006323454,0.0011296967,0.0017735977,0.00081419107,0.00019264176,0.00010449243,0.009781326],"genre_scores_gemma":[0.9922232,0.00013798074,0.001031147,0.0007448499,0.0007168139,0.000055239776,0.000050930365,0.00009278438,0.004947069],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99524426,0.00020471308,0.0009359503,0.0012920186,0.0013131076,0.001009946],"domain_scores_gemma":[0.9970966,0.00015571306,0.00082131656,0.0011397237,0.00018564821,0.0006010225],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00030263112,0.0009106811,0.0010253262,0.0000038075707,0.0004192582,0.00019699238,0.0009368304,0.00038820843,0.0023398183],"category_scores_gemma":[0.000104266284,0.00080886134,0.00018095315,0.00062810036,0.0010147421,0.0003785838,0.00025764183,0.0012031262,0.0004620511],"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":[0.0011439321,0.002730383,0.21638064,0.00036635672,0.00063449144,0.000059118473,0.0044644126,0.0044626067,0.26819292,0.04196733,0.19481748,0.2647803],"study_design_scores_gemma":[0.006955924,0.0024811195,0.7288647,0.00062210206,0.00052388373,0.000018272482,0.0009387786,0.07459789,0.07051776,0.009916439,0.09839973,0.006163385],"about_ca_topic_score_codex":0.09428944,"about_ca_topic_score_gemma":0.018862251,"teacher_disagreement_score":0.5124841,"about_ca_system_score_codex":0.00026941788,"about_ca_system_score_gemma":0.000857657,"threshold_uncertainty_score":0.9994362},"labels":[],"label_agreement":null},{"id":"W2949243094","doi":"10.5539/enrr.v9n3p9","title":"Multi-Layered Cloud Distribution Over Tropical Station Using Radiosonde Humidity Observations and CloudSat Measurements","year":2019,"lang":"en","type":"article","venue":"Environment and Natural Resources Research","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Radiosonde; Environmental science; Cloud computing; Atmosphere (unit); Climatology; Meteorology; Humidity; Atmospheric sciences; Geology; Geography; Computer science","score_opus":0.08676486575645002,"score_gpt":0.3156145875010108,"score_spread":0.22884972174456075,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2949243094","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":[0.998038,0.00064617733,0.00052040175,0.00019362963,0.000072682924,0.0004363093,0.000022959299,0.000015546682,0.00005429455],"genre_scores_gemma":[0.99651,0.00026762785,0.001991028,0.000039564286,0.00006997855,0.0000102466465,0.000036103742,0.000014984154,0.0010604474],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99748325,0.00023175814,0.00020653872,0.00047557053,0.0011635085,0.00043935588],"domain_scores_gemma":[0.99944407,0.00009787859,0.00006289584,0.00021660436,0.000011057874,0.00016752245],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00057623844,0.00016373952,0.00015938457,0.0000051940888,0.00046115596,0.000081313774,0.00015115264,0.00011124697,0.0007457734],"category_scores_gemma":[0.00007493751,0.00013778204,0.000033280878,0.00016257164,0.00039011615,0.00023321906,0.0003764455,0.00039502644,0.0000610423],"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":[0.00008663149,0.00007275096,0.8861196,0.00001260195,0.00001594835,0.0000018287336,0.00032661998,0.0005982776,0.11015989,0.000022231645,0.00034930088,0.002234312],"study_design_scores_gemma":[0.0007838634,0.000111434056,0.952418,0.000013348044,0.000009777347,0.0000025540655,0.00021230157,0.03061631,0.0005643177,0.000070131966,0.0150217125,0.00017624618],"about_ca_topic_score_codex":0.00034836662,"about_ca_topic_score_gemma":0.000028684939,"teacher_disagreement_score":0.10959557,"about_ca_system_score_codex":0.0004980577,"about_ca_system_score_gemma":0.000008064666,"threshold_uncertainty_score":0.81656957},"labels":[],"label_agreement":null},{"id":"W2949685075","doi":"10.82308/36327","title":"Observations of shallow trade-wind cumulus cloudiness and mass flux variability and their relationship to boundary layer structure","year":2015,"lang":"en","type":"article","venue":"eScholarship@McGill (McGill)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Fonds Québécois de la Recherche sur la Nature et les Technologies; Strong; Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Atmospheric sciences; Boundary layer; Troposphere; Mass flux; Flux (metallurgy); Environmental science; Cloud cover; Climatology; Cloud fraction; Geology; Cloud computing; Materials science; Physics","score_opus":0.03302218994809299,"score_gpt":0.23065576205459315,"score_spread":0.19763357210650015,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2949685075","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":[0.99301916,0.000046721085,0.000020640437,0.0002783261,0.00019441829,0.00041933754,0.0005155165,0.000059126247,0.005446723],"genre_scores_gemma":[0.9924696,0.000005522915,0.0067373635,0.00044451386,0.000018016428,0.000015109945,0.000024427956,0.00003259056,0.00025282428],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99792975,0.00025630058,0.0004612213,0.0005881806,0.00039036362,0.0003741768],"domain_scores_gemma":[0.99856097,0.00024377233,0.00015838344,0.00050338847,0.000046659632,0.00048681718],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0008380059,0.00032196505,0.0003487601,0.000008090029,0.0005861527,0.00006111955,0.00030685109,0.00024620432,0.00031640928],"category_scores_gemma":[0.0007364237,0.0002786812,0.00006410682,0.00051643857,0.0002913453,0.0008698898,0.00034903694,0.00042156398,0.000027118287],"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":[0.00019618603,0.00021700424,0.8081795,0.000089011744,0.00009051714,0.000009828665,0.00031903465,0.0030350438,0.12566717,0.027788142,0.000071280694,0.03433729],"study_design_scores_gemma":[0.00093577825,0.0001919326,0.87499267,0.000032388303,0.00005608036,0.00002455748,0.00049014954,0.0004789051,0.0045238757,0.08205209,0.035640925,0.00058063585],"about_ca_topic_score_codex":0.00021274359,"about_ca_topic_score_gemma":0.00018673566,"teacher_disagreement_score":0.12114329,"about_ca_system_score_codex":0.0002923847,"about_ca_system_score_gemma":0.000022615504,"threshold_uncertainty_score":0.99996656},"labels":[],"label_agreement":null},{"id":"W2950211049","doi":"10.82308/19577","title":"Characterizing dust storms and modeling diffusion in viscous atmospheric aerosol particles","year":2017,"lang":"en","type":"article","venue":"eScholarship@McGill (McGill)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Fonds de recherche du Québec – Nature et technologies; Natural Sciences and Engineering Research Council of Canada; National Oceanic and Atmospheric Administration; U.S. Geological Survey; National Aeronautics and Space Administration","keywords":"Aerosol; Context (archaeology); Dust storm; Environmental science; Mineral dust; Atmospheric sciences; Moderate-resolution imaging spectroradiometer; Particle (ecology); Storm; Meteorology; Geology; Physics; Satellite","score_opus":0.019033008868337215,"score_gpt":0.22894225265536758,"score_spread":0.20990924378703035,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2950211049","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":[0.99159133,0.000046522364,0.000010528869,0.00009791118,0.00040159767,0.00031608526,0.000031752377,0.00009414947,0.0074101165],"genre_scores_gemma":[0.99675757,0.00016944004,0.00215592,0.00037529634,0.00003800399,0.000049083446,0.0000041958756,0.00005543223,0.0003950777],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99747014,0.000095299685,0.0004864185,0.0007297479,0.0004743378,0.00074402586],"domain_scores_gemma":[0.9985183,0.00003918314,0.00028519,0.0008027286,0.000017495657,0.00033712178],"candidate_categories":["metaepi_narrow","sts"],"consensus_categories":[],"category_scores_codex":[0.00051748805,0.00038956007,0.00038208623,0.000002515774,0.0019783962,0.0002393601,0.00062355446,0.00021708437,0.0005418635],"category_scores_gemma":[0.00022401787,0.00035865905,0.00009172883,0.00014616341,0.00024494706,0.0021284292,0.0010210304,0.0005184848,0.00037028367],"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":[0.00019405456,0.00044723167,0.10239562,0.00005322795,0.000037986953,0.00013727274,0.00008253366,0.0029834234,0.4440755,0.0020842233,0.0000070892384,0.44750184],"study_design_scores_gemma":[0.009394108,0.0009627899,0.6050369,0.00078765297,0.0002161122,0.0001815987,0.0018286213,0.27975076,0.043542802,0.014161896,0.03833639,0.005800333],"about_ca_topic_score_codex":0.0025942111,"about_ca_topic_score_gemma":0.00087310525,"teacher_disagreement_score":0.5026413,"about_ca_system_score_codex":0.00039048088,"about_ca_system_score_gemma":0.000006621541,"threshold_uncertainty_score":0.9998865},"labels":[],"label_agreement":null},{"id":"W2950314734","doi":"10.1016/j.atmosres.2019.06.011","title":"Development of a new visibility parameterization based on the measurement of fog microphysics at a mountain site in Korea","year":2019,"lang":"en","type":"article","venue":"Atmospheric Research","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":19,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Korea Meteorological Administration","keywords":"Visibility; Fog; Drizzle; Environmental science; Meteorology; Precipitation; Liquid water content; Cloud physics; Cloud computing; Aerosol; Remote sensing; Atmospheric sciences; Computer science; Physics; Geology","score_opus":0.04830720959296038,"score_gpt":0.2887863527575357,"score_spread":0.24047914316457536,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2950314734","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":[0.99424446,0.000013985556,0.0013465087,0.00012876671,0.000022261414,0.0007185925,0.0000010863105,0.0000060730717,0.003518286],"genre_scores_gemma":[0.9812877,0.0000047885637,0.01825265,0.00005334412,0.0000062700124,0.000032573982,0.0000022559075,0.000015192984,0.0003452162],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9968604,0.00020930916,0.00039874998,0.00037129183,0.001799956,0.00036031],"domain_scores_gemma":[0.9989823,0.000166283,0.00012414886,0.000583248,0.000069080466,0.00007494788],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0023651565,0.00013347308,0.00021408097,8.447923e-7,0.00008571568,0.000013079374,0.00036429046,0.00006148629,0.0018752681],"category_scores_gemma":[0.00012814165,0.00009340432,0.00005639411,0.0009124665,0.0001945023,0.000055763652,0.00029101266,0.00017747025,0.00024304658],"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":[0.000508528,0.0004923617,0.5608356,0.00006438843,0.000017008932,0.0000013392643,0.0030536451,0.02473653,0.38676634,0.00006847409,0.00043754673,0.023018252],"study_design_scores_gemma":[0.0009465314,0.00046526545,0.8284373,0.00011441489,0.0000051000907,2.3524647e-7,0.00054991554,0.093007796,0.07361168,0.00035170218,0.0022774301,0.00023261926],"about_ca_topic_score_codex":0.0020683687,"about_ca_topic_score_gemma":0.00040573248,"teacher_disagreement_score":0.31315467,"about_ca_system_score_codex":0.0010577264,"about_ca_system_score_gemma":0.00024501633,"threshold_uncertainty_score":0.99903715},"labels":[],"label_agreement":null},{"id":"W2951032547","doi":"10.82308/4515","title":"Drought and associated cloud fields over the Canadian Prairies","year":2009,"lang":"en","type":"article","venue":"eScholarship@McGill (McGill)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"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; Precipitation; Albedo (alchemy); Cloud cover; Forestry; Geography; Meteorology; Cloud computing","score_opus":0.008583276332499692,"score_gpt":0.2039764008296367,"score_spread":0.195393124497137,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2951032547","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":[0.8877524,0.00005231145,4.2994924e-7,0.0011450408,0.00022911234,0.00022512056,0.000094800955,0.00007558594,0.11042516],"genre_scores_gemma":[0.9905322,0.000033164884,0.00018352273,0.0067743063,0.000027009923,0.000012182001,0.000009788346,0.00002046471,0.0024073296],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99805325,0.00015158963,0.00027865559,0.00041899877,0.00044769954,0.0006498187],"domain_scores_gemma":[0.99897075,0.00008960874,0.00012243805,0.00040212122,0.000020979727,0.00039408467],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00050640985,0.00027950763,0.00022830919,0.0000046715836,0.0018765853,0.00012652397,0.0004256737,0.0002861321,0.0010975071],"category_scores_gemma":[0.0003004293,0.00021697646,0.000090359106,0.0003761582,0.0002441573,0.000613804,0.00015884716,0.00058914843,0.00031543215],"study_design_candidate":"design_other","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":[0.0001341317,0.0005065029,0.10381161,0.000022795473,0.00028730827,0.00027941325,0.00020192841,0.000666753,0.0042572306,0.26545626,0.0059591397,0.61841697],"study_design_scores_gemma":[0.0006119183,0.00022194177,0.5057442,0.000023072807,0.00005486842,0.00002756898,0.00008774165,0.000109405395,0.0007274618,0.032298364,0.45946273,0.00063068833],"about_ca_topic_score_codex":0.09071185,"about_ca_topic_score_gemma":0.39352962,"teacher_disagreement_score":0.6177863,"about_ca_system_score_codex":0.000640506,"about_ca_system_score_gemma":0.00002103367,"threshold_uncertainty_score":0.99981564},"labels":[],"label_agreement":null},{"id":"W2954400259","doi":"10.5194/amt-12-6541-2019","title":"Analysis of global three-dimensional aerosol structure with spectral radiance matching","year":2019,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":9,"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":"Natural Science Foundation of Zhejiang Province; National Natural Science Foundation of China","keywords":"Radiance; Lidar; Remote sensing; Aerosol; Nadir; Spectroradiometer; Environmental science; Moderate-resolution imaging spectroradiometer; Satellite; Subpixel rendering; Meteorology; Pixel; Geology; Geography; Optics; Physics; Reflectivity","score_opus":0.007469359092906881,"score_gpt":0.20615732890061833,"score_spread":0.19868796980771145,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2954400259","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":[0.9765526,0.00013071603,0.018639445,0.00006846385,0.000060266153,0.0005306025,0.000012863799,0.00017706284,0.0038279817],"genre_scores_gemma":[0.8976936,0.000004961496,0.10197123,0.00019248552,0.000019393514,0.00001834787,0.0000053115486,0.000021214144,0.0000734956],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9972644,0.00004541523,0.00037842875,0.00056280225,0.0013313367,0.0004176115],"domain_scores_gemma":[0.998952,0.000014055765,0.0002817787,0.00058177416,0.000049717026,0.00012070095],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00029698308,0.0003171282,0.00051432167,7.592532e-7,0.0000875898,0.00002638696,0.0004021798,0.00011547934,0.00460963],"category_scores_gemma":[0.000007847852,0.00024355976,0.00016068805,0.0013378756,0.000172579,0.0001934214,0.00012694832,0.00015826173,0.000037489626],"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":[0.00007900613,0.00008707393,0.9521529,0.000014140068,0.00043960393,0.000005829123,0.000051085353,0.012299763,0.028769268,0.00017244268,0.0003677008,0.0055611916],"study_design_scores_gemma":[0.0005410107,0.0006390811,0.97075075,0.00010000924,0.0007910799,0.000014349759,0.00006644303,0.0073857754,0.017491436,0.0009311911,0.00047452535,0.00081433443],"about_ca_topic_score_codex":0.0017774018,"about_ca_topic_score_gemma":0.002502479,"teacher_disagreement_score":0.083331786,"about_ca_system_score_codex":0.0005531607,"about_ca_system_score_gemma":0.000049365935,"threshold_uncertainty_score":0.9963003},"labels":[],"label_agreement":null},{"id":"W2954873937","doi":"10.3390/rs11131509","title":"Developing an Aircraft-Based Angular Distribution Model of Solar Reflection from Wildfire Smoke to Aid Satellite-Based Radiative Flux Estimation","year":2019,"lang":"en","type":"article","venue":"Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"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":"National Aeronautics and Space Administration","keywords":"Environmental science; Remote sensing; Radiative transfer; Radiative flux; Satellite; Albedo (alchemy); Atmosphere (unit); Radiometer; Single-scattering albedo; Smoke; Meteorology; Atmospheric sciences; Physics; Geology; Optics","score_opus":0.020361916125259543,"score_gpt":0.25659617092391696,"score_spread":0.23623425479865742,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2954873937","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":[0.5112575,0.000007740362,0.48830605,0.00011277106,0.000048135822,0.00014839302,0.000007946861,0.000035434023,0.00007602365],"genre_scores_gemma":[0.7176813,0.0000014852261,0.28182724,0.0002617154,0.000017703316,5.1067587e-8,0.00017665175,0.000017261997,0.000016587677],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9986711,0.00008560131,0.00027044705,0.00039609638,0.00032832703,0.0002483863],"domain_scores_gemma":[0.99937737,0.000041421146,0.000153887,0.0003050725,0.000021333488,0.00010093536],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019700947,0.00017494563,0.00020775702,0.0000048495035,0.00013967368,0.00002819892,0.000087266846,0.000115855146,0.000031387375],"category_scores_gemma":[0.000043617412,0.00018152288,0.000060863873,0.00031815708,0.000054194676,0.00020432592,0.00003384764,0.000106179716,0.000066675486],"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":[0.00006219234,0.0000146123975,0.0023635011,0.000008289987,0.0000058134356,0.0000013667708,0.00028134722,0.7383719,0.09842192,0.0000058976702,0.0000095039,0.16045365],"study_design_scores_gemma":[0.00031193419,0.00007978708,0.010086074,0.000085793145,0.00001744211,5.7114227e-7,0.00007208412,0.8941617,0.094445236,0.00043353724,0.00009703706,0.00020878835],"about_ca_topic_score_codex":0.0018597348,"about_ca_topic_score_gemma":0.00012702122,"teacher_disagreement_score":0.20647879,"about_ca_system_score_codex":0.00062813394,"about_ca_system_score_gemma":0.00006692312,"threshold_uncertainty_score":0.7402288},"labels":[],"label_agreement":null},{"id":"W2955488144","doi":"10.1175/jcli-d-18-0666.1","title":"Causes of Dimming and Brightening in China Inferred from Homogenized Daily Clear-Sky and All-Sky in situ Surface Solar Radiation Records (1958–2016)","year":2019,"lang":"en","type":"article","venue":"Journal of Climate","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":91,"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":"Young Scientists Fund; National Key Research and Development Program of China; Eidgenössische Technische Hochschule Zürich; National Natural Science Foundation of China; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; National Science Foundation","keywords":"Sky; Environmental science; Climatology; China; Atmospheric sciences; Meteorology; Geography; Physics; Geology","score_opus":0.0057993592995924026,"score_gpt":0.22243617195983711,"score_spread":0.2166368126602447,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2955488144","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":[0.9985227,0.0005320053,0.000044496686,0.00011251754,0.00010132329,0.0000952814,0.0000043839527,0.000003593776,0.0005837044],"genre_scores_gemma":[0.9953997,0.0023529928,0.0021175472,0.00003494142,0.000017903805,3.773655e-7,0.0000017391616,0.000012592767,0.00006216805],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99883515,0.00007745646,0.00051118404,0.00015618865,0.00021253724,0.00020748896],"domain_scores_gemma":[0.9993111,0.00007783878,0.0004321732,0.000097530996,0.0000075758167,0.00007381177],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005209254,0.00011254197,0.00034057966,0.0000071015206,0.000033330114,0.000033785815,0.00010151336,0.000074025746,0.00027904814],"category_scores_gemma":[0.000036646416,0.00009733865,0.00003989347,0.000122057136,0.000058215373,0.0004584025,0.00010599979,0.00019754595,0.0000148274175],"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":[0.00024483036,0.000042678617,0.91278964,0.000013407358,0.000018144588,0.000017884015,0.00157509,0.0013660247,0.074562505,0.0000021091741,0.000027692753,0.009339985],"study_design_scores_gemma":[0.0016169166,0.00019361096,0.99316335,0.00011870092,0.000022712955,0.000016308457,0.00029817925,0.002289373,0.0015895816,0.00012371132,0.00044220212,0.00012533659],"about_ca_topic_score_codex":0.0010634093,"about_ca_topic_score_gemma":0.00043875934,"teacher_disagreement_score":0.08037372,"about_ca_system_score_codex":0.00007539007,"about_ca_system_score_gemma":0.000014231173,"threshold_uncertainty_score":0.39693546},"labels":[],"label_agreement":null},{"id":"W2955849415","doi":"","title":"In cloud horizontal wind profiles using the Scanning W-Band ARM Cloud Radar","year":2011,"lang":"en","type":"article","venue":"35th Conference on Radar Meteorology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Cloud computing; Remote sensing; Radar; Environmental science; Meteorology; Geodesy; Geology; Computer science; Geography; Telecommunications","score_opus":0.03908097456950561,"score_gpt":0.2553498665664544,"score_spread":0.21626889199694882,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2955849415","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":[0.9626097,0.00008565098,0.0011237214,0.00042080545,0.0009180545,0.00038381634,0.00000683362,0.000038644735,0.034412775],"genre_scores_gemma":[0.993841,0.00002776914,0.004642963,0.0008817182,0.00020383626,0.000015403226,0.0000028021682,0.000030968276,0.00035357097],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99763757,0.00029512995,0.00039680593,0.0006154428,0.00034344918,0.0007116126],"domain_scores_gemma":[0.9990809,0.00007816376,0.0002027723,0.00048545416,0.000013874393,0.00013884126],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005617487,0.00032870632,0.00038918955,0.000008120657,0.00027666957,0.00003104229,0.0006386609,0.00021371113,0.007103918],"category_scores_gemma":[0.00004422996,0.00023843753,0.00008705337,0.00028826392,0.00080678076,0.0001785946,0.0002060146,0.00049459405,0.00021230623],"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":[0.0036267934,0.0026916075,0.40949607,0.000071832605,0.0003907881,0.0012979533,0.038571846,0.0010128819,0.31294328,0.17072757,0.010996121,0.04817326],"study_design_scores_gemma":[0.015334875,0.015844814,0.5268884,0.00045045378,0.0007308162,0.0012821387,0.027635923,0.021461988,0.19335893,0.098398015,0.09045093,0.008162738],"about_ca_topic_score_codex":0.003029862,"about_ca_topic_score_gemma":0.00046352498,"teacher_disagreement_score":0.119584344,"about_ca_system_score_codex":0.00016435371,"about_ca_system_score_gemma":0.00007699534,"threshold_uncertainty_score":0.99380374},"labels":[],"label_agreement":null},{"id":"W2958750102","doi":"10.5194/acp-19-15183-2019","title":"The unprecedented 2017–2018 stratospheric smoke event: decay phase and aerosol properties observed with the EARLINET","year":2019,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":175,"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":"Horizon 2020; Fundação para a Ciência e a Tecnologia; Horizon 2020 Framework Programme; Interreg; Leibniz-Gemeinschaft; Russian Science Foundation; Uniwersytet Warszawski; Bundesministerium für Bildung und Forschung; European Space Agency; National Science Foundation; Science Foundation Ireland; Irish Research Council; European Regional Development Fund; European Commission; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung","keywords":"Stratosphere; Aerosol; Atmospheric sciences; Troposphere; Environmental science; Northern Hemisphere; Climatology; Southern Hemisphere; Smoke; Lidar; Meteorology; Physics; Geology; Remote sensing","score_opus":0.013013230163159896,"score_gpt":0.21200216542161088,"score_spread":0.198988935258451,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2958750102","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":[0.9947279,0.00071517687,0.00033628748,0.00035312382,0.000039299994,0.00033776273,0.0000049644386,0.000038931954,0.003446573],"genre_scores_gemma":[0.98755014,0.0002952622,0.00058291253,0.00017919212,0.00008449537,0.000044661927,0.0000063648117,0.00002850422,0.011228445],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9986839,0.000035142708,0.00019013275,0.000421071,0.00029695526,0.00037277423],"domain_scores_gemma":[0.9991684,0.00006952004,0.00013322009,0.00048767208,0.000015923995,0.00012529118],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012814293,0.0002953678,0.00020531417,7.036425e-9,0.00051139726,0.0001477309,0.0003230713,0.00007716608,0.00077062985],"category_scores_gemma":[0.000004225036,0.0001534581,0.000051595205,0.0002038995,0.0006457069,0.00017452908,0.00016312157,0.00022764876,0.000046071844],"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":[0.0015979415,0.0012590303,0.23796652,0.00040884785,0.0006686109,0.00002963717,0.004982708,0.012314179,0.30721468,0.0001937229,0.010715101,0.42264903],"study_design_scores_gemma":[0.021789594,0.0031653512,0.16677207,0.0005970842,0.0009905003,0.00040428794,0.019500468,0.33075914,0.22334921,0.0008275221,0.22548991,0.006354871],"about_ca_topic_score_codex":0.00020904739,"about_ca_topic_score_gemma":0.00003422075,"teacher_disagreement_score":0.41629416,"about_ca_system_score_codex":0.00003870685,"about_ca_system_score_gemma":0.000025146384,"threshold_uncertainty_score":0.84378564},"labels":[],"label_agreement":null},{"id":"W2962057619","doi":"10.5194/amt-12-3943-2019","title":"A practical information-centered technique to remove a priori information from lidar optimal-estimation-method retrievals","year":2019,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Strong","keywords":"A priori and a posteriori; Lidar; Remote sensing; Optimal estimation; Grid; Environmental science; Computer science; Meteorology; Mathematics; Geology; Geography; Machine learning","score_opus":0.015646744260222677,"score_gpt":0.270123201988199,"score_spread":0.25447645772797634,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2962057619","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.030746307,0.00001129039,0.9501709,0.0010020786,0.00016830399,0.0032639888,0.000016253427,0.00071024575,0.013910637],"genre_scores_gemma":[0.18609889,0.000016805121,0.8112829,0.0019846805,0.000033160897,0.00042120056,0.00003491303,0.000027018245,0.000100441364],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9961638,0.00016726216,0.0009787322,0.000429447,0.001733435,0.0005273525],"domain_scores_gemma":[0.99805576,0.00009173232,0.0005255881,0.0008553706,0.00018990657,0.0002816636],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0017077269,0.00042081278,0.00043098317,0.0000039320826,0.00016804761,0.00024047878,0.0004985058,0.0002841269,0.003380397],"category_scores_gemma":[0.0006457156,0.00039175304,0.0001350964,0.00082745426,0.00006309689,0.0037745878,0.00038407362,0.00035010514,0.002968839],"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":[0.0011956764,0.00084235665,0.05378584,0.00022864476,0.0003128578,0.000017354947,0.0063888216,0.0043096133,0.09132005,0.0017081492,0.13563746,0.70425314],"study_design_scores_gemma":[0.0017758956,0.0020768899,0.039269783,0.0006555373,0.00018593212,0.00006737083,0.0013473356,0.04248786,0.14372543,0.002504437,0.76320106,0.002702473],"about_ca_topic_score_codex":0.0009786565,"about_ca_topic_score_gemma":0.000011774278,"teacher_disagreement_score":0.70155066,"about_ca_system_score_codex":0.0010495951,"about_ca_system_score_gemma":0.00012567312,"threshold_uncertainty_score":0.99985343},"labels":[],"label_agreement":null},{"id":"W2963380018","doi":"10.1029/2018jd030122","title":"A Review of Ice Particle Shapes in Cirrus formed In Situ and in Anvils","year":2019,"lang":"en","type":"review","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":149,"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; York University","funders":"U.S. Air Force; National Oceanic and Atmospheric Administration; European Centre for Medium-Range Weather Forecasts; National Ethnic Affairs Commission of the People's Republic of China; Langley Research Center; National Aeronautics and Space Administration; Natural Environment Research Council; U.S. Department of Energy; National Center for Atmospheric Research; Bureau of Reclamation; National Science Foundation","keywords":"Cirrus; Middle latitudes; Particle (ecology); Ice crystals; Troposphere; Atmospheric sciences; Radiative transfer; Materials science; Convection; Geology; Physics; Meteorology; Optics","score_opus":0.06839446358185945,"score_gpt":0.38101944730819604,"score_spread":0.31262498372633657,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2963380018","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0773271,0.92107826,0.0000027635792,0.000095797004,0.000023284436,0.0006308841,0.0000020598932,0.0000014867251,0.00083835993],"genre_scores_gemma":[0.03036738,0.96909386,0.00022601287,0.000051100513,0.00004729501,0.000026679518,6.5655325e-7,0.0000240811,0.00016295268],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9959659,0.00067736674,0.0013434049,0.0003409163,0.0010224541,0.0006499455],"domain_scores_gemma":[0.99776816,0.0012247793,0.00050775625,0.00024735418,0.00004572168,0.00020620572],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0022895026,0.00026189827,0.0019393384,0.000005695413,0.000024864976,0.000027134025,0.00052830455,0.00016633022,0.0005093294],"category_scores_gemma":[0.0009959034,0.00018466884,0.00028070292,0.001468005,0.00033679508,0.00029029665,0.00045038637,0.0013089371,0.00009328903],"study_design_candidate":"design_other","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":[0.00009466111,0.0005961696,0.0041220956,0.028520502,0.000031573138,0.0002183846,0.00015660422,0.000033457032,0.000098526594,0.00005002265,0.00068046094,0.96539754],"study_design_scores_gemma":[0.0026393991,0.002255121,0.079840355,0.37059438,0.00020797529,0.00009739896,0.0005395729,0.00068329705,0.00003181131,0.002324726,0.53976357,0.0010223711],"about_ca_topic_score_codex":0.0010846684,"about_ca_topic_score_gemma":0.0011094207,"teacher_disagreement_score":0.9643752,"about_ca_system_score_codex":0.00041651924,"about_ca_system_score_gemma":0.00025389803,"threshold_uncertainty_score":0.75305766},"labels":[],"label_agreement":null},{"id":"W2964360779","doi":"10.3390/atmos10080433","title":"Simulating Arctic Ice Clouds during Spring Using an Advanced Ice Cloud Microphysics in the WRF Model","year":2019,"lang":"en","type":"article","venue":"Atmosphere","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"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 du Québec à Montréal","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Weather Research and Forecasting Model; Ice crystals; Ice nucleus; Environmental science; Arctic; Atmospheric sciences; Meteorology; Spring (device); Climatology; Lidar; Nucleation; Geology; Remote sensing; Geography; Oceanography; Physics","score_opus":0.01143508709867382,"score_gpt":0.23427874294410814,"score_spread":0.2228436558454343,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2964360779","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":[0.99496937,0.0000776461,0.0017631511,0.00003748885,0.00015900611,0.00037824054,0.0000010591531,0.000051507803,0.0025625224],"genre_scores_gemma":[0.97931427,0.000009877724,0.019826632,0.00032749394,0.00010970508,0.000008949693,0.0000011856407,0.00005454285,0.00034736545],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9980307,0.00009162306,0.0003310402,0.000560431,0.00039489145,0.00059128593],"domain_scores_gemma":[0.9989873,0.00007301225,0.0001600312,0.00067653606,0.000011572014,0.00009152188],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024240497,0.0002834929,0.00024865742,3.078732e-7,0.0002686513,0.00007314279,0.00057183683,0.000101403966,0.00039142268],"category_scores_gemma":[0.000017730763,0.00023609877,0.00009020368,0.00039795294,0.000092535076,0.00052376033,0.00028443013,0.00036658655,0.00021335302],"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":[0.000024039024,0.00008000148,0.12356684,0.000024149509,0.0000053799927,0.0000095333335,0.0014534309,0.83428866,0.039141685,0.00008780331,0.0000019659,0.0013165239],"study_design_scores_gemma":[0.00076389045,0.000065016546,0.054913282,0.00007861696,0.000021723225,0.000009744126,0.0025229848,0.93975,0.0008246571,0.00048326078,0.000115455616,0.0004513565],"about_ca_topic_score_codex":0.0019628485,"about_ca_topic_score_gemma":0.0002793639,"teacher_disagreement_score":0.10546137,"about_ca_system_score_codex":0.00030169208,"about_ca_system_score_gemma":0.000020863483,"threshold_uncertainty_score":0.9627828},"labels":[],"label_agreement":null},{"id":"W2965141591","doi":"10.5194/acp-20-1391-2020","title":"A new look at the environmental conditions favorable to secondary ice production","year":2020,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":184,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada; Environment and Climate Change Canada","funders":"Federal Aviation Administration; Glenn Research Center; Transport Canada; Environment and Climate Change Canada; University of Waterloo; Massachusetts Institute of Technology; National Aeronautics and Space Administration","keywords":"Graupel; Ice crystals; Supercooling; Middle latitudes; Mesoscale meteorology; Clear ice; Ice nucleus; Atmospheric sciences; Environmental science; Materials science; Geology; Meteorology; Sea ice; Antarctic sea ice; Climatology; Chemistry; Arctic ice pack; Physics","score_opus":0.005259895870003935,"score_gpt":0.18692715288207823,"score_spread":0.18166725701207428,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2965141591","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":[0.9837378,0.000101334415,0.0016000351,0.0022926435,0.000038338152,0.00017960115,0.000014282066,0.00003851208,0.011997436],"genre_scores_gemma":[0.9512311,0.00004275426,0.004827106,0.0022583595,0.00039650028,0.000024154953,0.000030217348,0.000022225968,0.041167535],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991039,0.000011654519,0.00011994163,0.00038762312,0.00017393661,0.0002029662],"domain_scores_gemma":[0.999467,0.00001683276,0.000048029306,0.00021938296,0.0000017006305,0.00024705462],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000032220636,0.00016130814,0.00011550375,4.033138e-9,0.0003168762,0.000027291251,0.00014920982,0.000044041044,0.02244033],"category_scores_gemma":[0.0000067727196,0.00013245181,0.0000462073,0.00015471017,0.00015588767,0.00011702081,0.00021038632,0.00014524351,0.00077469734],"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":[0.00008578864,0.00012519478,0.02831157,0.000047005065,0.00006117816,0.000008488655,0.0034619742,0.012893186,0.5162727,0.000020969757,0.2051754,0.23353654],"study_design_scores_gemma":[0.0011906357,0.00025253254,0.068873465,0.00002811273,0.0001762621,0.00007769668,0.0021925753,0.008246693,0.17291279,0.0012819561,0.743367,0.0014002923],"about_ca_topic_score_codex":0.000086550506,"about_ca_topic_score_gemma":0.000003973325,"teacher_disagreement_score":0.5381916,"about_ca_system_score_codex":0.00009143291,"about_ca_system_score_gemma":0.000017737406,"threshold_uncertainty_score":0.99574256},"labels":[],"label_agreement":null},{"id":"W2968374954","doi":"10.1175/jas-d-19-0004.1","title":"Sensitivity of Lake-Effect Cloud Microphysical Processes to Ice Crystal Habit and Nucleation during OWLeS IOP4","year":2019,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":6,"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":"Office of International Science and Engineering; University at Albany; State University of New York; National Science Foundation","keywords":"Ice nucleus; Ice crystals; Crystal habit; Nucleation; Precipitation; Atmospheric sciences; Environmental science; Cloud physics; Cloud condensation nuclei; Liquid water content; Storm; Condensation; Mesoscale meteorology; Meteorology; Climatology; Aerosol; Geology; Physics; Crystallization; Thermodynamics; Cloud computing","score_opus":0.003738032768547986,"score_gpt":0.2040173483821003,"score_spread":0.20027931561355233,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2968374954","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":[0.9985394,0.00004973457,0.00012796225,0.00043757874,0.00026965098,0.00016095652,0.0000010315033,0.000005596523,0.00040812828],"genre_scores_gemma":[0.9963373,0.000014791479,0.0032356768,0.000092504124,0.00008394929,8.5955185e-7,2.7388321e-8,0.0000069219827,0.00022797564],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986673,0.00012365742,0.00025941254,0.00019677878,0.00055076834,0.00020210633],"domain_scores_gemma":[0.9992527,0.00013126232,0.00035834857,0.00013667544,0.000033777447,0.00008725835],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00072200614,0.00012360931,0.00024303739,6.779285e-7,0.00020337678,0.000050216164,0.0003370877,0.000034864897,0.00013587481],"category_scores_gemma":[0.00018396287,0.000071341696,0.00008258512,0.0006485574,0.00038110052,0.00032277164,0.00026099425,0.000111308196,0.000021562288],"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":[0.00008825651,0.000068612135,0.49188513,0.000056443674,0.00001387866,0.0000042981906,0.0008234808,0.02435637,0.4809721,0.000010801568,0.00019671049,0.0015239266],"study_design_scores_gemma":[0.00049450324,0.0010587671,0.9501198,0.00019166268,0.000047642196,0.0002105383,0.0009025284,0.0049703335,0.04101182,0.00014169712,0.00060169643,0.00024899363],"about_ca_topic_score_codex":0.00008615426,"about_ca_topic_score_gemma":0.00008505261,"teacher_disagreement_score":0.4582347,"about_ca_system_score_codex":0.0000473975,"about_ca_system_score_gemma":0.00003996727,"threshold_uncertainty_score":0.290923},"labels":[],"label_agreement":null},{"id":"W2972715463","doi":"10.5194/amt-12-4949-2019","title":"Calibration of the 2007–2017 record of Atmospheric Radiation Measurements cloud radar observations using CloudSat","year":2019,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":64,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Office of Science; U.S. Department of Energy","keywords":"Radar; Environmental science; Remote sensing; Calibration; Cloud computing; Meteorology; Computer science; Geology; Geography; Telecommunications; Physics","score_opus":0.047990173498583026,"score_gpt":0.2428861241514585,"score_spread":0.19489595065287546,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2972715463","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":[0.9538209,0.00035120497,0.036488134,0.00012825962,0.0008581373,0.0018064077,0.0000058556498,0.00015671623,0.006384387],"genre_scores_gemma":[0.8472185,0.00010121313,0.15191682,0.0002097718,0.00008925794,0.00004622807,0.000004195986,0.00004925776,0.00036473613],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99616057,0.00025853325,0.0009417786,0.000492608,0.0017525153,0.00039398734],"domain_scores_gemma":[0.9977042,0.000033781405,0.0010489973,0.00096215756,0.00015832704,0.00009250319],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011919974,0.00034503627,0.00046885482,6.872575e-7,0.00019629367,0.000023346443,0.00071036816,0.00019087897,0.0013165133],"category_scores_gemma":[0.00010271579,0.00027459883,0.00024014768,0.000863491,0.00022189994,0.00041317684,0.00024704917,0.00018950744,0.000018509547],"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":[0.000053526932,0.00024032671,0.682299,0.00006548791,0.00008031185,3.8817296e-7,0.00022430773,0.0018715082,0.29156783,0.00015113734,0.006051462,0.017394723],"study_design_scores_gemma":[0.0023545187,0.0012247411,0.46617267,0.000871195,0.00059365993,0.000016113918,0.0005960397,0.0462043,0.4134676,0.0026093854,0.06382232,0.0020674588],"about_ca_topic_score_codex":0.0026326473,"about_ca_topic_score_gemma":0.00008652385,"teacher_disagreement_score":0.21612632,"about_ca_system_score_codex":0.0006802574,"about_ca_system_score_gemma":0.00012268117,"threshold_uncertainty_score":0.9999706},"labels":[],"label_agreement":null},{"id":"W2973897941","doi":"10.5194/acp-19-11651-2019","title":"Characterization of aerosol hygroscopicity using Raman lidar measurements at the EARLINET station of Payerne","year":2019,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"European Commission; Université de Lille; Agencia Estatal de Investigación; Ministerio de Ciencia, Innovación y Universidades; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; Bundesamt für Umwelt; Ministerio de Economía y Competitividad; National Science Foundation","keywords":"Aerosol; Radiosonde; Lidar; Troposphere; Environmental science; Backscatter (email); Altitude (triangle); Relative humidity; Atmospheric sciences; Remote sensing; Meteorology; Mineral dust; Physics; Geology","score_opus":0.011989463681341997,"score_gpt":0.2164673631628097,"score_spread":0.20447789948146772,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2973897941","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":[0.9966116,0.000017117965,0.0021042295,0.000013470686,0.00003052098,0.00014304732,0.000009956643,0.000006499786,0.0010635698],"genre_scores_gemma":[0.99689996,0.000016752669,0.0016792867,0.000036281155,0.000029184199,0.0000028672612,0.000023680048,0.000010087514,0.0013018984],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9992535,0.00001843477,0.00019414323,0.00017581286,0.00024075317,0.00011734269],"domain_scores_gemma":[0.99951196,0.00001540179,0.00021559715,0.00020702419,0.000017048456,0.000032951197],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00008067188,0.00011010179,0.00015320999,8.21665e-9,0.000064949345,0.000007870379,0.00009988367,0.000047393707,0.001462995],"category_scores_gemma":[0.0000042173724,0.000086191765,0.000036780246,0.00012405426,0.00013672069,0.000092477916,0.00008616522,0.000055510016,0.000011880843],"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":[0.000019272478,0.000043913155,0.14828643,0.00005067823,0.000011829982,6.770647e-8,0.0002108739,0.0012180192,0.8441528,0.0000013314119,0.000005997739,0.005998795],"study_design_scores_gemma":[0.00038012885,0.000040595554,0.06559861,0.000031603104,0.00003343042,0.00000107712,0.00006959394,0.016617667,0.9168964,0.000034903678,0.00015372269,0.00014226811],"about_ca_topic_score_codex":0.0002130961,"about_ca_topic_score_gemma":0.0000027075878,"teacher_disagreement_score":0.082687825,"about_ca_system_score_codex":0.000050866165,"about_ca_system_score_gemma":0.000010272605,"threshold_uncertainty_score":0.9994498},"labels":[],"label_agreement":null},{"id":"W2980941129","doi":"10.5194/acp-2019-886","title":"Impact of hygroscopic CCN and turbulence on cloud dropletgrowth: A parcel-DNS approach","year":2019,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Center for Atmospheric Research; National Science Foundation","keywords":"Drizzle; Turbulence; Seeding; Cloud condensation nuclei; Condensation; RADIUS; Aerosol; Liquid water content; Mechanics; Fluid parcel; Meteorology; Cloud physics; Environmental science; Atmospheric sciences; Chemical physics; Cloud computing; Chemistry; Flow (mathematics); Physics; Thermodynamics; Computer science","score_opus":0.005736007926913919,"score_gpt":0.2212203878178929,"score_spread":0.215484379890979,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2980941129","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":[0.928794,0.000018754712,0.00046405007,0.000023754608,0.000045847333,0.00019036839,0.0000027194696,0.00002053588,0.07043991],"genre_scores_gemma":[0.99459267,0.000019665467,0.0019047447,0.000088105175,0.00001815228,0.0000053500194,0.0000016435084,0.000010917566,0.0033587813],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99906015,0.000023075057,0.00014692836,0.00030813707,0.00022564063,0.0002360449],"domain_scores_gemma":[0.999526,0.000029995328,0.00006139798,0.00027762618,0.0000031872328,0.00010178357],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00008807204,0.00014057964,0.0001808765,0.000001125811,0.000038472263,0.000013583647,0.00016517797,0.000059340513,0.003734437],"category_scores_gemma":[0.000007740041,0.000094650255,0.00006481257,0.00013623858,0.00015231057,0.000078957106,0.00013268004,0.00009165278,0.00032126612],"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":[0.000028678842,0.00016996912,0.9874689,0.000013526033,0.00001263138,8.1917955e-7,0.00032608575,0.0008379995,0.008467628,0.0003627301,0.00081450795,0.0014965442],"study_design_scores_gemma":[0.00052152196,0.00079579145,0.9910314,0.000013349308,0.000008569689,0.0000056991917,0.00014926081,0.00602417,0.000866475,0.00016975278,0.00020222309,0.00021179125],"about_ca_topic_score_codex":0.00089687994,"about_ca_topic_score_gemma":0.0000061327883,"teacher_disagreement_score":0.06708113,"about_ca_system_score_codex":0.00006083478,"about_ca_system_score_gemma":0.000008528904,"threshold_uncertainty_score":0.9971763},"labels":[],"label_agreement":null},{"id":"W2981242874","doi":"10.1080/02786826.2019.1676394","title":"Chemical and microphysical properties of wind-blown dust near an actively retreating glacier in Yukon, Canada","year":2019,"lang":"en","type":"article","venue":"Aerosol Science and Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":50,"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 de Montréal","funders":"","keywords":"Mineral dust; Particulates; Deposition (geology); Aerosol; Environmental science; Radiative forcing; Atmospheric sciences; Aeolian processes; Environmental chemistry; Air quality index; Biogeochemical cycle; Chemistry; Geology; Sediment; Meteorology; Geomorphology","score_opus":0.003974680956719982,"score_gpt":0.17801840849235964,"score_spread":0.17404372753563965,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2981242874","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":[0.9989379,0.000029633984,0.0000010035235,0.00037009094,0.000023624176,0.00013425786,8.870051e-7,0.000015130764,0.00048749518],"genre_scores_gemma":[0.9992452,0.0000074847126,0.00058769045,0.00008001036,0.0000045325487,0.0000038464414,2.1587495e-7,0.000005276095,0.00006570452],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9988773,0.000008720417,0.0001400754,0.00040722522,0.0002532888,0.00031342456],"domain_scores_gemma":[0.99964815,0.000009075191,0.000057236135,0.00019577688,0.000018942486,0.00007081646],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013487568,0.000104745595,0.00017103761,0.000004588064,0.00011566068,0.00002214896,0.00026642284,0.00008881045,0.000036521003],"category_scores_gemma":[0.000044172943,0.00008180637,0.000006989451,0.00070042786,0.0022835527,0.00024282638,0.00032433512,0.00015390827,0.000004591539],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000069623684,0.000026007385,0.19881609,0.0000044242142,9.741435e-7,0.000002208322,0.00014784643,0.00000552237,0.79566705,0.000051845655,0.0000058525907,0.0052652247],"study_design_scores_gemma":[0.0005034703,0.00024564916,0.071257874,0.00004449154,0.000005879837,0.00003227682,0.00158119,0.0029270353,0.9228383,0.00010457355,0.00016836892,0.00029090725],"about_ca_topic_score_codex":0.056403484,"about_ca_topic_score_gemma":0.014931965,"teacher_disagreement_score":0.12755822,"about_ca_system_score_codex":0.0001160903,"about_ca_system_score_gemma":0.00014628671,"threshold_uncertainty_score":0.94988},"labels":[],"label_agreement":null},{"id":"W2981974467","doi":"10.3390/app9214487","title":"Gridded Visibility Products over Marine Environments Based on Artificial Neural Network Analysis","year":2019,"lang":"en","type":"article","venue":"Applied Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":10,"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 Aeronautics and Space Administration","keywords":"Visibility; Artificial neural network; Computer science; Satellite; Remote sensing; Meteorology; Artificial intelligence; Environmental science; Geography; Engineering","score_opus":0.00941428873002787,"score_gpt":0.21662829045087154,"score_spread":0.20721400172084367,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2981974467","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":[0.9685851,0.0000026020803,0.00030016084,0.00020238389,0.00017748737,0.00035808,0.0000017053673,0.000031079922,0.03034143],"genre_scores_gemma":[0.99652094,8.329785e-7,0.002019951,0.00085685914,0.00008882709,0.000019702944,0.000007711526,0.0000078926,0.00047725675],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9975098,0.000044220025,0.00024734062,0.0009026785,0.0008061924,0.0004898102],"domain_scores_gemma":[0.99919885,0.000064322885,0.00012364627,0.00050983,0.0000018705251,0.000101461796],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0006746455,0.00019373547,0.00023640515,0.000005183329,0.00030089507,0.000067976885,0.0004542291,0.000055050215,0.009110405],"category_scores_gemma":[0.000011945614,0.00014881496,0.00008671806,0.0015751446,0.00051346957,0.00011704376,0.00025200343,0.00012194546,0.0009732009],"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":[0.000040291416,0.00011610165,0.5450464,0.000001659867,0.000013741245,8.6064694e-7,0.000034795,0.4449673,0.005145742,0.00027680828,0.00032771676,0.004028573],"study_design_scores_gemma":[0.00016314848,0.00013488324,0.8550965,0.0000011525666,0.000051763473,1.4478042e-7,0.0000415671,0.14124803,0.0013369457,0.0006794517,0.0009920454,0.00025433302],"about_ca_topic_score_codex":0.00012243661,"about_ca_topic_score_gemma":0.00006211464,"teacher_disagreement_score":0.31005013,"about_ca_system_score_codex":0.00008637575,"about_ca_system_score_gemma":0.000014376273,"threshold_uncertainty_score":0.9998047},"labels":[],"label_agreement":null},{"id":"W2983395416","doi":"10.5194/amt-13-2309-2020","title":"Microwave and submillimeter wave scattering of oriented ice particles","year":2020,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":52,"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":"European Organization for the Exploitation of Meteorological Satellites; Universität Hamburg; Swedish National Space Agency; Environment and Climate Change Canada; Deutsche Forschungsgemeinschaft","keywords":"Scattering; Ice crystals; Microwave; Polarization (electrochemistry); Physics; Radiative transfer; Computational physics; Optics; Ice cloud; Discrete dipole approximation; Orientation (vector space); Geometry; Chemistry","score_opus":0.029883763142620225,"score_gpt":0.20753090579944833,"score_spread":0.1776471426568281,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2983395416","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":[0.94196963,0.00025630396,0.053563293,0.00061599404,0.000029468236,0.00035043934,0.0000014268909,0.00020446043,0.003008972],"genre_scores_gemma":[0.8747654,0.000059598307,0.12427314,0.0007950543,0.000026298865,0.00003219703,7.1869e-7,0.000023072804,0.000024539582],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99842477,0.000053021733,0.00034337968,0.00038288935,0.0005122078,0.0002837082],"domain_scores_gemma":[0.99940825,0.000014745463,0.00015152658,0.00022358706,0.000032970012,0.00016889899],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030155573,0.00020220928,0.00025057176,2.785504e-7,0.00007591633,0.000018613431,0.00014977614,0.00006588849,0.0005880846],"category_scores_gemma":[0.00005278543,0.00017771106,0.00006191822,0.0002735022,0.0002651551,0.00013482803,0.00023948507,0.000098676814,0.000024227098],"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":[0.000038281632,0.000058495,0.08534668,0.000036294812,0.000029698813,0.00000600164,0.0005788536,0.0000065628633,0.8307394,0.0000508727,0.0016766622,0.08143223],"study_design_scores_gemma":[0.00039410155,0.00044452946,0.08250847,0.00007329454,0.000076107375,0.00001019041,0.0003279407,0.0025140701,0.8998458,0.00029666602,0.0130072795,0.000501562],"about_ca_topic_score_codex":0.00017578503,"about_ca_topic_score_gemma":0.000014419136,"teacher_disagreement_score":0.08093067,"about_ca_system_score_codex":0.000082859566,"about_ca_system_score_gemma":0.00001025636,"threshold_uncertainty_score":0.72468466},"labels":[],"label_agreement":null},{"id":"W2984195945","doi":"10.5194/amt-13-4219-2020","title":"Synergistic radar and radiometer retrievals of ice hydrometeors","year":2020,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":47,"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":"Environment and Climate Change Canada; Universität Hamburg; Swedish National Space Agency","keywords":"Remote sensing; Environmental science; Ice cloud; Radiometer; Ice crystals; Meteorology; Radar; Precipitation; Cloud computing; Computer science; Geology; Physics","score_opus":0.022066616284302953,"score_gpt":0.20944295365799215,"score_spread":0.1873763373736892,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2984195945","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":[0.8750501,0.0012157661,0.10551436,0.0009359725,0.000084924366,0.0008862528,0.0000046831574,0.00049511576,0.015812773],"genre_scores_gemma":[0.89584684,0.00016654564,0.10315161,0.0006476407,0.000038014216,0.000027922562,9.838584e-7,0.00003123001,0.000089220586],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99779487,0.00008743335,0.00044136317,0.0004664899,0.000907069,0.00030276747],"domain_scores_gemma":[0.9991698,0.00004679824,0.00021719973,0.00030590186,0.000033166812,0.00022709792],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00059151324,0.00025196158,0.00038548166,5.794329e-7,0.000085036016,0.000021793776,0.00031115243,0.00010135636,0.0013314561],"category_scores_gemma":[0.00029014234,0.00022010799,0.00008613972,0.00065710937,0.0002954434,0.00015150185,0.00021509049,0.00013563767,0.00003372953],"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":[0.00013697043,0.00018223916,0.033021882,0.00015544129,0.00012860657,0.000026507192,0.0008464374,0.00006868656,0.82878613,0.00023226839,0.012794122,0.123620726],"study_design_scores_gemma":[0.001869161,0.0042935177,0.045722384,0.000297177,0.00052665663,0.00002217412,0.0005614461,0.008029298,0.80521774,0.0021288213,0.12878406,0.0025475495],"about_ca_topic_score_codex":0.00020661068,"about_ca_topic_score_gemma":0.000004215231,"teacher_disagreement_score":0.12107318,"about_ca_system_score_codex":0.00013496891,"about_ca_system_score_gemma":0.000018244598,"threshold_uncertainty_score":0.99958146},"labels":[],"label_agreement":null},{"id":"W2988841161","doi":"","title":"Lidar Observations of Volcanic Aerosol Layers Over Halifax, Canada","year":2008,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Lidar; Aerosol; Volcano; Environmental science; Remote sensing; Geology; Volcanic ash; Meteorology; Geography; Geochemistry","score_opus":0.018360461981329058,"score_gpt":0.20928679939607087,"score_spread":0.1909263374147418,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2988841161","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":[0.9781669,0.000037678867,0.000007635278,0.0001941298,0.0002160553,0.00010981276,0.000011860389,0.000032405416,0.021223564],"genre_scores_gemma":[0.9962709,0.000020381229,0.0014125142,0.0004891121,0.000045453955,0.0000069880825,0.000007922349,0.000019931813,0.0017267741],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985098,0.000023438795,0.00037456793,0.00027218243,0.0004768914,0.00034312287],"domain_scores_gemma":[0.9992114,0.000098760334,0.000230334,0.0002905672,0.000016780627,0.00015219867],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013936982,0.00015757984,0.00018026272,0.0000011937354,0.00021802704,0.000008763826,0.00026181174,0.00007013229,0.00013198465],"category_scores_gemma":[0.0001420262,0.00015266541,0.000055624765,0.00019231549,0.00014155068,0.00012036096,0.00009390002,0.00014512382,0.00005278768],"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":[0.0000055633604,0.000053859283,0.94945264,0.000008271146,0.000013958377,0.00003935733,0.00027344935,0.01958563,0.011361549,0.0000073941956,0.019075597,0.00012271524],"study_design_scores_gemma":[0.00018971859,0.000028799104,0.9901735,0.000024449839,0.000011772266,0.0000099520075,0.00012992346,0.00027139683,0.0025250714,0.00000997666,0.0064304103,0.00019501647],"about_ca_topic_score_codex":0.94706374,"about_ca_topic_score_gemma":0.92631274,"teacher_disagreement_score":0.040720858,"about_ca_system_score_codex":0.00019034918,"about_ca_system_score_gemma":0.0001478079,"threshold_uncertainty_score":0.62255144},"labels":[],"label_agreement":null},{"id":"W2991425876","doi":"10.5194/amt-13-1427-2020","title":"The 2018 fire season in North America as seen by TROPOMI: aerosol layer height intercomparisons and evaluation of model-derived plume heights","year":2020,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":52,"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; Environment and Climate Change Canada","funders":"","keywords":"Aerosol; Plume; Environmental science; Spectroradiometer; Lidar; Atmospheric sciences; Altitude (triangle); Meteorology; Remote sensing; Troposphere; Air quality index; Satellite; Panache; Geology; Geography; Reflectivity; Mathematics","score_opus":0.03984130164782797,"score_gpt":0.2557300903228179,"score_spread":0.21588878867498995,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2991425876","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":[0.97837895,0.0015007757,0.014817967,0.0014449045,0.000030928986,0.0011795548,0.0000062954705,0.0001385087,0.002502143],"genre_scores_gemma":[0.98626554,0.0007241974,0.012160952,0.00049610686,0.000021035212,0.00023104,0.0000071544587,0.000031214026,0.00006278952],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9970284,0.00024183263,0.0004978803,0.0005168796,0.0013479459,0.00036704907],"domain_scores_gemma":[0.9990877,0.000031299813,0.00027460817,0.00036001788,0.00007478672,0.00017161995],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00060968654,0.000299432,0.0003570372,3.970076e-7,0.0001965834,0.00003535568,0.00041631868,0.00009694871,0.00031818042],"category_scores_gemma":[0.0000818726,0.0002195217,0.00007779194,0.00038885244,0.00032829872,0.00021031495,0.00022822655,0.00021614059,0.000027442278],"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":[0.00061919994,0.000930237,0.20583628,0.000082502476,0.00026729386,0.000007689929,0.0091533875,0.012869881,0.20119144,0.000044671346,0.15984622,0.4091512],"study_design_scores_gemma":[0.0015034174,0.0012164657,0.022531172,0.00010403558,0.00021994757,0.0000032918986,0.0012525249,0.893435,0.055558536,0.00040229663,0.022752954,0.0010203668],"about_ca_topic_score_codex":0.0009898407,"about_ca_topic_score_gemma":0.0006469164,"teacher_disagreement_score":0.8805651,"about_ca_system_score_codex":0.00038427536,"about_ca_system_score_gemma":0.00006212691,"threshold_uncertainty_score":0.8951835},"labels":[],"label_agreement":null},{"id":"W2993210125","doi":"","title":"In-situ single particle composition analysis of free tropospheric ice nuclei and ice residues in mixed-phase clouds during INUIT-JFJ 2013","year":2014,"lang":"en","type":"article","venue":"EGU General Assembly Conference Abstracts","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"In situ; Ice crystals; Ice nucleus; Phase (matter); Particle (ecology); Arctic ice pack; Atmospheric sciences; Environmental science; Geology; Climatology; Chemistry; Meteorology; Sea ice; Geography; Oceanography","score_opus":0.011848552583269858,"score_gpt":0.23971976799355207,"score_spread":0.2278712154102822,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2993210125","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":[0.9974866,0.00004540179,0.00018233016,0.00037788026,0.0000835835,0.00016333033,0.0000064497635,0.000025375153,0.0016290563],"genre_scores_gemma":[0.99773896,0.000040792256,0.0017992842,0.00011111815,0.000043026106,0.000012388053,0.000009007244,0.000016831798,0.00022860875],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99797136,0.00013990689,0.0005948945,0.00050167384,0.00034480475,0.00044737745],"domain_scores_gemma":[0.9990544,0.00007302374,0.00026168008,0.0004223124,0.000023073906,0.00016551206],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033731942,0.000235976,0.00044489276,0.000012925588,0.00008698021,0.00007186661,0.00032222245,0.00012304887,0.00043300056],"category_scores_gemma":[0.00003748258,0.0002331152,0.00007316439,0.00069590646,0.00017729173,0.00047929084,0.00021644309,0.0001769502,0.000033380325],"study_design_candidate":"bench_or_experimental","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":[0.00008112949,0.00045215015,0.062000945,0.000014229925,0.000038716506,0.000018920311,0.0009722071,0.030203214,0.9037206,0.00017149802,0.00010939571,0.0022169831],"study_design_scores_gemma":[0.0010950344,0.0001804668,0.86584616,0.00002452722,0.000081868544,0.0000028514542,0.00021867146,0.014328268,0.1176584,0.00023890693,0.00005979086,0.00026504067],"about_ca_topic_score_codex":0.006681354,"about_ca_topic_score_gemma":0.032325674,"teacher_disagreement_score":0.8038452,"about_ca_system_score_codex":0.00015926783,"about_ca_system_score_gemma":0.000018489683,"threshold_uncertainty_score":0.99993324},"labels":[],"label_agreement":null},{"id":"W2993257360","doi":"10.5194/acp-2017-629","title":"Response to marine cloud brightening in a multi-model ensemble","year":2017,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Robarts Clinical Trials","funders":"Universitetet i Oslo","keywords":"Forcing (mathematics); Environmental science; Climatology; Radiative forcing; Atmospheric sciences; Albedo (alchemy); Precipitation; Climate model; Greenhouse gas; Cloud albedo; Subtropics; Cloud forcing; Latitude; Climate change; Meteorology; Cloud computing; Cloud cover; Geography; Physics; Geology; Oceanography","score_opus":0.031520723272723025,"score_gpt":0.28650705750791733,"score_spread":0.2549863342351943,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2993257360","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":[0.88923806,0.000009795825,0.07291268,0.001038096,0.00026342022,0.00044678742,0.000004644894,0.00006719321,0.03601934],"genre_scores_gemma":[0.79405296,0.000013180961,0.1370581,0.00056931656,0.000030982785,0.000066906694,0.000004121139,0.000032676733,0.06817179],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99801815,0.00007998314,0.000322825,0.00079715136,0.00032026184,0.00046165922],"domain_scores_gemma":[0.99852246,0.000041383017,0.00014011648,0.0010722517,0.0000071222103,0.00021664571],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0007151001,0.00031321577,0.00035825936,0.00000348338,0.0001490742,0.00010305095,0.0008673847,0.000272614,0.0023376942],"category_scores_gemma":[0.00012502176,0.00027554,0.0001058743,0.000068323316,0.000101884034,0.000073770636,0.005503218,0.00046946004,0.0009932964],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022847978,0.00064040686,0.2588599,0.000052374875,0.000046209218,0.00038146606,0.0049725003,0.61557543,0.030259322,0.00019035168,0.02539582,0.06134141],"study_design_scores_gemma":[0.0012772749,0.00010420596,0.35024855,0.00014193005,0.00002186535,0.0000115091725,0.00011956505,0.63010144,0.0010976888,0.0032955022,0.012231756,0.0013487433],"about_ca_topic_score_codex":0.0072436538,"about_ca_topic_score_gemma":0.00423554,"teacher_disagreement_score":0.095185116,"about_ca_system_score_codex":0.00037169646,"about_ca_system_score_gemma":0.000056174897,"threshold_uncertainty_score":0.99996966},"labels":[],"label_agreement":null},{"id":"W2995850864","doi":"10.1029/2019jd031465","title":"Importance of Bias Correction in Data Assimilation of Multiple Observations Over Eastern China Using WRF‐Chem/DART","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":38,"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 Toronto","funders":"Natural Science Foundation of Jiangsu Province; National Natural Science Foundation of China","keywords":"Aerosol; Weather Research and Forecasting Model; Environmental science; Data assimilation; Atmospheric sciences; Meteorology; Moderate-resolution imaging spectroradiometer; Boundary layer; Climatology; Geography; Geology; Physics","score_opus":0.11795739789693757,"score_gpt":0.35145855788491925,"score_spread":0.23350115998798168,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2995850864","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":[0.9982531,0.000040803014,0.00071876036,0.000100500685,0.00015817677,0.00018341206,0.000007637657,0.0000028852107,0.00053471216],"genre_scores_gemma":[0.9956904,0.000026747219,0.003648594,0.000014074185,0.00008208576,0.000001136802,0.000004572985,0.000014356093,0.0005180131],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99748236,0.00015559516,0.00064211566,0.00023523929,0.0011975382,0.00028717172],"domain_scores_gemma":[0.99835354,0.0004073049,0.0005421416,0.00046699733,0.00010464708,0.00012534365],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010626618,0.000112718706,0.0003318325,0.0000034259504,0.00005507805,0.000020434476,0.0005495281,0.00006643185,0.0006992332],"category_scores_gemma":[0.0009904457,0.00009180109,0.00009083173,0.0007216974,0.00021499746,0.00071815954,0.00038923172,0.0004383609,0.000018955945],"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":[0.00014638728,0.00030229712,0.9420335,0.000019799503,0.000017689117,0.0000034554812,0.00016387226,0.011975952,0.041760717,0.000012675785,0.0011137329,0.0024499157],"study_design_scores_gemma":[0.00042615327,0.00020417405,0.7764948,0.0000980234,0.0000069738,0.0000022670222,0.00020079741,0.22083268,0.001177797,0.00024454977,0.00024575976,0.00006602226],"about_ca_topic_score_codex":0.0032163355,"about_ca_topic_score_gemma":0.0007558208,"teacher_disagreement_score":0.20885672,"about_ca_system_score_codex":0.00017919154,"about_ca_system_score_gemma":0.00013393092,"threshold_uncertainty_score":0.7656113},"labels":[],"label_agreement":null},{"id":"W2996332817","doi":"10.1029/2019ms001862","title":"Error Analysis for an Algorithm That Reduces Radiative Transfer Calculations in High‐Resolution Atmospheric Models","year":2019,"lang":"en","type":"article","venue":"Journal of Advances in Modeling Earth Systems","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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":"Radiative transfer; Longwave; Radiative flux; Series (stratigraphy); Algorithm; Atmospheric radiative transfer codes; Irradiance; Solar irradiance; Mathematics; Meteorology; Environmental science; Physics; Geology; Optics","score_opus":0.0242031249520348,"score_gpt":0.2693653199216262,"score_spread":0.2451621949695914,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2996332817","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":[0.52082473,0.00091138907,0.4777456,0.000011589777,0.00019972303,0.0002096661,0.0000059658846,0.0000043802647,0.00008698703],"genre_scores_gemma":[0.9569629,0.00028695696,0.042548325,0.0000138458345,0.00006689646,0.000016959582,0.0000054349966,0.000014825303,0.00008385326],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9982858,0.0001189367,0.0006633512,0.00025681208,0.00040452083,0.00027061132],"domain_scores_gemma":[0.99945253,0.000057663365,0.00022089714,0.00014549054,0.000035360725,0.00008804398],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00065681874,0.00015329308,0.0004746817,0.000011749725,0.000060743747,0.000034344463,0.00020088126,0.00009359013,0.00004251146],"category_scores_gemma":[0.000008226718,0.0001280095,0.0001446892,0.00057744846,0.000036934114,0.0015167595,0.000014808284,0.00018661382,0.0000035634785],"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":[0.00004369706,0.00006620615,0.017510423,0.000009380164,0.000032361757,0.0000017434785,0.0007551774,0.97927755,0.00012882627,0.00005790798,0.000001491773,0.0021152426],"study_design_scores_gemma":[0.0006690542,0.00019478844,0.0029103642,0.00005672671,0.00005323335,0.000004745597,0.0014769142,0.99396044,0.000014502367,0.00041918567,0.00008508226,0.00015495143],"about_ca_topic_score_codex":0.0006764282,"about_ca_topic_score_gemma":0.0005588595,"teacher_disagreement_score":0.4361382,"about_ca_system_score_codex":0.00017220221,"about_ca_system_score_gemma":0.000026696267,"threshold_uncertainty_score":0.5220076},"labels":[],"label_agreement":null},{"id":"W2996409744","doi":"","title":"Statistics on Low-Lying Liquid and Liquid-Dominant Mixed-Phase Clouds over Ottawa","year":2006,"lang":"en","type":"article","venue":"ESASP","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Communications Research Centre Canada","funders":"","keywords":"Radiosonde; Liquid water path; Environmental science; Liquid water content; Cloud top; Meteorology; Relative humidity; Humidity; Radiometer; Cloud base; Water vapor; Cloud computing; Cloud height; Atmospheric sciences; Remote sensing; Cloud cover; Geography; Geology; Precipitation; Computer science","score_opus":0.005318179063539641,"score_gpt":0.23576355938953833,"score_spread":0.23044538032599868,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2996409744","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":[0.9836583,0.00009118912,0.005199339,0.000085698666,0.00022246696,0.00014817908,0.00003369838,0.000034907,0.010526238],"genre_scores_gemma":[0.99339706,0.000028859251,0.0028352407,0.00038847834,0.00014479588,0.000012829512,0.000013315534,0.000027974358,0.0031514731],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9986931,0.000036370617,0.000252159,0.00035506117,0.00029969923,0.0003635889],"domain_scores_gemma":[0.999466,0.00006664263,0.00009234664,0.00024755727,0.0000052271253,0.00012219486],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001610746,0.00019614135,0.00017763888,0.000001733632,0.00018268495,0.00003323483,0.00013804887,0.00008007556,0.0014396318],"category_scores_gemma":[0.000025514319,0.00016946057,0.000038236463,0.000093263865,0.00020225608,0.000088921624,0.0001357979,0.00013071907,0.00027881807],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0043769605,0.0050302455,0.042307734,0.00020011228,0.00012072517,0.0013568463,0.0029905997,0.00979892,0.32077095,0.051992614,0.48816544,0.07288885],"study_design_scores_gemma":[0.012176025,0.0119373165,0.22599831,0.00025968385,0.00020413261,0.00009737343,0.0006199444,0.018403191,0.12706803,0.0026384187,0.59715533,0.0034422248],"about_ca_topic_score_codex":0.000953015,"about_ca_topic_score_gemma":0.00016834088,"teacher_disagreement_score":0.1937029,"about_ca_system_score_codex":0.00009964613,"about_ca_system_score_gemma":0.000010233511,"threshold_uncertainty_score":0.9994732},"labels":[],"label_agreement":null},{"id":"W2996766131","doi":"10.5194/acp-20-55-2020","title":"Retrieving the global distribution of the threshold of wind erosion from satellite data and implementing it into the Geophysical Fluid Dynamics Laboratory land–atmosphere model (GFDL AM4.0/LM4.0)","year":2020,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":72,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Sherbrooke O.E.M (Canada); Université de Sherbrooke","funders":"National Park Service; National Aeronautics and Space Administration; NASA Astrobiology Institute; Desert Research Institute; National Oceanic and Atmospheric Administration; University of California, Davis; U.S. Environmental Protection Agency","keywords":"Environmental science; Aeolian processes; Atmosphere (unit); Satellite; Aerosol; Moderate-resolution imaging spectroradiometer; Wind speed; Atmospheric sciences; Spatial distribution; Climatology; Erosion; Meteorology; Remote sensing; Geology; Geography; Physics","score_opus":0.009060284550203093,"score_gpt":0.21755722798427907,"score_spread":0.208496943434076,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2996766131","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":[0.9948107,0.000435892,0.003296841,0.0005348278,0.000018323566,0.00013563893,0.00038819705,0.000008561345,0.00037103286],"genre_scores_gemma":[0.99811167,0.00025530826,0.0012877646,0.00013325449,0.00007474019,0.0000019032639,0.00009900987,0.000011097863,0.000025243142],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9987613,0.000039774495,0.0003289277,0.0003490622,0.00032889334,0.00019204165],"domain_scores_gemma":[0.9989076,0.00009570209,0.0002800593,0.0006260892,0.000024997747,0.00006553497],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018041578,0.00018847051,0.00024523822,4.227342e-9,0.00024951532,0.000024937215,0.0006265837,0.0000766848,0.00006546569],"category_scores_gemma":[0.000038395487,0.000111356676,0.0000613954,0.00036072085,0.00059792615,0.0001372932,0.001056299,0.00020542504,8.276953e-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":[0.00013902663,0.00014728514,0.8487255,0.00021343368,0.00012828963,9.480207e-7,0.0032860772,0.012752614,0.07205486,0.0004410926,0.000587195,0.06152369],"study_design_scores_gemma":[0.00037683794,0.0000353429,0.059252955,0.00006247241,0.00015580795,6.813908e-7,0.0014462097,0.9257919,0.010180034,0.0017227161,0.00076389697,0.00021112128],"about_ca_topic_score_codex":0.00061944826,"about_ca_topic_score_gemma":0.000035468274,"teacher_disagreement_score":0.9130393,"about_ca_system_score_codex":0.00004956896,"about_ca_system_score_gemma":0.000035643665,"threshold_uncertainty_score":0.45409933},"labels":[],"label_agreement":null},{"id":"W2996857950","doi":"","title":"Fingerprinting of microphysical processes in Arctic clouds by tracking Doppler radar spectra features","year":2014,"lang":"en","type":"article","venue":"14th Conference on Cloud Physics/14th Conference on Atmospheric Radiation/Anthony Slingo Symposium","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Doppler effect; Radar; Doppler radar; Remote sensing; Tracking (education); Arctic; Meteorology; Environmental science; Radar tracker; Spectral line; Computer science; Geography; Geology; Physics; Telecommunications; Oceanography","score_opus":0.011215148423477204,"score_gpt":0.23253844538028642,"score_spread":0.22132329695680922,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2996857950","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":[0.961121,0.00010458004,0.013413674,0.0019550936,0.0010976305,0.0010954526,0.000049756105,0.00023361595,0.02092916],"genre_scores_gemma":[0.99281996,0.00034782448,0.004497098,0.0006291052,0.0007276214,0.00011533256,0.0000576895,0.00012839506,0.00067699497],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99421626,0.0003750863,0.0012007178,0.001685355,0.0012556082,0.0012669556],"domain_scores_gemma":[0.9967647,0.0005147434,0.0010565473,0.0010664298,0.00021066552,0.0003869112],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0005696502,0.0010292568,0.0012109374,0.000007455669,0.0003983073,0.00030226106,0.001238114,0.00037503755,0.00090002624],"category_scores_gemma":[0.0002860239,0.0009969181,0.00027185772,0.0013377378,0.0005964012,0.00044941917,0.00022164649,0.001071313,0.00028483104],"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":[0.0013924296,0.006432789,0.09829608,0.0010812382,0.00037458577,0.00004689462,0.0178269,0.05725071,0.59030443,0.075043954,0.007585045,0.14436492],"study_design_scores_gemma":[0.015257991,0.008050081,0.17566831,0.005234134,0.0007011873,0.00006920843,0.006022119,0.32539693,0.3971462,0.041859318,0.011736351,0.012858192],"about_ca_topic_score_codex":0.0013410012,"about_ca_topic_score_gemma":0.00012733054,"teacher_disagreement_score":0.26814622,"about_ca_system_score_codex":0.00044971434,"about_ca_system_score_gemma":0.00031470263,"threshold_uncertainty_score":0.99924815},"labels":[],"label_agreement":null},{"id":"W2996980315","doi":"","title":"Ground-Based Millimeter-Wave Radiometer for Stratospheric Observation at Eureka, Canada","year":2001,"lang":"en","type":"article","venue":"aprs","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Radiometer; Remote sensing; Meteorology; Environmental science; Extremely high frequency; Microwave radiometer; Atmospheric sciences; Geology; Optics; Geography; Physics","score_opus":0.02374314763367727,"score_gpt":0.20477247906559784,"score_spread":0.18102933143192057,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2996980315","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":[0.98905,0.000045191366,0.008409054,0.00045410614,0.00020453343,0.00025985815,0.000009840362,0.000025521475,0.001541953],"genre_scores_gemma":[0.982086,0.00000754469,0.010142142,0.0021596607,0.00005300933,0.000049253496,0.000030509322,0.000022263277,0.005449609],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99895483,0.000018124732,0.00017274162,0.00027362592,0.00026019986,0.00032045468],"domain_scores_gemma":[0.9995354,0.000059241862,0.00007339753,0.00021562896,0.000007697371,0.00010866411],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000079591526,0.00014071808,0.0001239626,6.4114954e-7,0.00016906415,0.00002018174,0.00013128573,0.00005186423,0.002144496],"category_scores_gemma":[0.00001362072,0.00012765765,0.00005936181,0.00025408642,0.00006122461,0.00009687723,0.000038436472,0.000046952253,0.000043966316],"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":[0.00015069224,0.00014539414,0.82929903,0.000026423604,0.000050709652,0.000066636574,0.00017011682,0.007971987,0.02509697,0.000055266344,0.09774547,0.0392213],"study_design_scores_gemma":[0.0010196603,0.00022403976,0.6829733,0.00000765797,0.000037028767,0.000013732552,0.00007855972,0.022297129,0.0027452614,0.00015271109,0.28996006,0.0004908196],"about_ca_topic_score_codex":0.1803268,"about_ca_topic_score_gemma":0.29881376,"teacher_disagreement_score":0.1922146,"about_ca_system_score_codex":0.00053972105,"about_ca_system_score_gemma":0.00004585316,"threshold_uncertainty_score":0.9987677},"labels":[],"label_agreement":null},{"id":"W2998381107","doi":"10.1175/bams-d-18-0288.1","title":"The ARM Radar Network: At the Leading Edge of Cloud and Precipitation Observations","year":2019,"lang":"en","type":"article","venue":"Bulletin of the American Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":102,"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":"Pacific Northwest National Laboratory; McGill University; U.S. Department of Energy","keywords":"Cloud computing; Radar; Computer science; Environmental science; Remote sensing; Doppler radar; Meteorology; Weather radar; Geology; Telecommunications; Geography","score_opus":0.01150291254644448,"score_gpt":0.2161824398836773,"score_spread":0.20467952733723282,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2998381107","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":[0.988513,0.00020409276,0.0003119984,0.008721275,0.00010742717,0.00027752842,0.0000023487828,0.000010242404,0.0018520888],"genre_scores_gemma":[0.98980325,0.0002842179,0.0048945397,0.0020164866,0.000047111702,0.000014864149,8.2475236e-7,0.000007656368,0.0029310414],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99886477,0.0002139811,0.00022949508,0.00019449423,0.00025983033,0.00023740217],"domain_scores_gemma":[0.9984249,0.0007981223,0.00040093804,0.00033105628,0.000011549286,0.000033430795],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00073906814,0.00010533696,0.00020052795,1.6918072e-7,0.0004255566,0.0000101582045,0.00042801216,0.000040637762,0.000705714],"category_scores_gemma":[0.0000870221,0.000045733766,0.00019211989,0.00020438392,0.0019481962,0.000011461937,0.0005791019,0.00014905471,0.0000531881],"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":[0.00019436797,0.00015630093,0.69788945,0.00001335534,0.00016295418,1.729622e-7,0.0014158878,0.01221136,0.02576429,0.0019973945,0.2257712,0.034423243],"study_design_scores_gemma":[0.00019923161,0.0003317642,0.80144733,0.000006299119,0.000046360143,0.000002168947,0.00083040446,0.00095846923,0.00037929544,0.0013647368,0.19431053,0.00012342124],"about_ca_topic_score_codex":0.00024016704,"about_ca_topic_score_gemma":0.000013504413,"teacher_disagreement_score":0.103557855,"about_ca_system_score_codex":0.00005030735,"about_ca_system_score_gemma":0.000004795074,"threshold_uncertainty_score":0.77270734},"labels":[],"label_agreement":null},{"id":"W2999635004","doi":"","title":"Lidar Measurements of Gravity Waves from Eureka During the Canadian Arctic ACE Validation Campaign","year":2009,"lang":"en","type":"article","venue":"AGUSM","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Lidar; Arctic; The arctic; Meteorology; Remote sensing; Environmental science; Climatology; Geodesy; Geography; Geology; Oceanography","score_opus":0.015177285237514715,"score_gpt":0.21421033199920186,"score_spread":0.19903304676168715,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2999635004","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":[0.9955942,0.000043826436,0.000044812667,0.0005613759,0.000074862706,0.000120280434,0.000003350747,0.00001072308,0.0035465923],"genre_scores_gemma":[0.998731,0.0000045568,0.00054798933,0.0002235779,0.00003299791,0.0000026504106,0.0000036718895,0.000005436489,0.00044809774],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99917924,0.00004920734,0.00012278574,0.00016114651,0.00029327988,0.00019431388],"domain_scores_gemma":[0.9995769,0.000013501322,0.00006622507,0.00023628004,0.000009346934,0.000097745484],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015859169,0.00008511785,0.00008294821,0.000001033607,0.00022052716,0.000021402555,0.00020333612,0.000042416512,0.0005592015],"category_scores_gemma":[0.00003218853,0.00006245955,0.00003633822,0.0001204622,0.00007211618,0.00008365564,0.000027656295,0.00008085159,0.00009868527],"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":[0.000008114671,0.000037045138,0.9650282,0.0000027823373,0.000013867538,0.0000037020707,0.001287916,0.00063536805,0.02924535,0.000020993673,0.00028989074,0.003426767],"study_design_scores_gemma":[0.000110644745,0.000022338669,0.9856878,0.0000096521535,0.000012592478,8.65787e-7,0.00007156316,0.0000268599,0.012814204,0.00077552284,0.00038888192,0.00007910859],"about_ca_topic_score_codex":0.30605283,"about_ca_topic_score_gemma":0.17477697,"teacher_disagreement_score":0.13127588,"about_ca_system_score_codex":0.00025424143,"about_ca_system_score_gemma":0.000021514683,"threshold_uncertainty_score":0.8402812},"labels":[],"label_agreement":null},{"id":"W3003580172","doi":"10.5194/acp-2017-1181","title":"Transport of Canadian forest fire smoke over the UK as observed bylidar","year":2018,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"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":"Met Office; Natural Environment Research Council; Sight Research UK; National Aeronautics and Space Administration","keywords":"Lidar; Aerosol; Ceilometer; Smoke; Environmental science; Depolarization ratio; Plume; Atmospheric sciences; Range (aeronautics); Meteorology; Climatology; Remote sensing; Geography; Geology; Materials science","score_opus":0.019417458019079646,"score_gpt":0.21101213506093133,"score_spread":0.19159467704185168,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3003580172","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":[0.8462941,0.000009413025,0.000024952838,0.00043437083,0.000060161256,0.00009075782,0.000004718117,0.0000085871825,0.15307294],"genre_scores_gemma":[0.9915688,0.0000089917185,0.0002462422,0.001184361,0.00003094769,0.0000044045055,0.0000023266616,0.000008102183,0.006945804],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993219,0.000008402289,0.00012383582,0.00014410214,0.00017384106,0.00022792039],"domain_scores_gemma":[0.9995618,0.000010340343,0.000031070624,0.00025698708,0.000005204196,0.00013461449],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00008386498,0.00008195501,0.000079518846,7.4917676e-7,0.00013533741,0.0000060650773,0.0002588566,0.00004953762,0.04439623],"category_scores_gemma":[0.0000053233657,0.00005024542,0.000051072937,0.00024017238,0.00033248097,0.000047137033,0.000025012583,0.000048838436,0.00028639624],"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":[0.000003941198,0.00000889244,0.9920174,8.7351816e-7,0.000005526716,0.0000027991919,0.00029095841,0.000026140588,0.00014928934,0.00041923847,0.006270097,0.00080486725],"study_design_scores_gemma":[0.00009002447,0.00006631284,0.9542071,0.0000025098707,0.0000074527834,0.0000013270021,0.0001397019,0.00022594313,0.00041757594,0.00019539145,0.044570964,0.000075672615],"about_ca_topic_score_codex":0.8686747,"about_ca_topic_score_gemma":0.90740705,"teacher_disagreement_score":0.14612713,"about_ca_system_score_codex":0.00004761878,"about_ca_system_score_gemma":0.000032529715,"threshold_uncertainty_score":0.95647734},"labels":[],"label_agreement":null},{"id":"W3003763400","doi":"10.1007/978-3-030-33566-3_9","title":"Remote Sensing of Arctic Atmospheric Aerosols","year":2020,"lang":"en","type":"book-chapter","venue":"Springer polar sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada; Université du Québec à Rimouski","funders":"","keywords":"Remote sensing; Aerosol; Radiometer; Environmental science; Arctic; Satellite; Instrumentation (computer programming); Lidar; Meteorology; The arctic; Geography; Geology; Oceanography; Computer science; Engineering; Aerospace engineering","score_opus":0.01690540286942031,"score_gpt":0.21883617488492396,"score_spread":0.20193077201550366,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3003763400","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.022745823,0.0013554479,0.004856083,0.000728128,0.00070301956,0.00044668623,0.000012323429,0.00013672421,0.9690158],"genre_scores_gemma":[0.6131297,0.00033961196,0.18900824,0.0011957412,0.00039577042,6.1218134e-7,0.0000042769116,0.00013976252,0.19578633],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9973246,0.000023232042,0.00046366086,0.00082336646,0.0009435211,0.00042165353],"domain_scores_gemma":[0.99884075,0.000055178076,0.0004466801,0.0004319939,0.000017301507,0.00020808974],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00034007782,0.0003925432,0.00049161323,0.0000016507701,0.00027638813,0.00006461923,0.0007244121,0.00020842146,0.003209466],"category_scores_gemma":[0.00005315202,0.00034587597,0.00022627828,0.00021245427,0.0016188115,0.00016606289,0.0005790168,0.0003632229,0.00091148994],"study_design_candidate":"design_other","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":[0.00017763294,0.00015814656,0.0655975,0.0009750146,0.0006258715,0.0006607128,0.0050120153,0.0059109214,0.057505507,0.06668987,0.012794586,0.7838922],"study_design_scores_gemma":[0.0017478527,0.0033630822,0.023187624,0.003085044,0.00093888777,0.00029028812,0.00073057483,0.05789648,0.0066596223,0.13978694,0.7531412,0.009172393],"about_ca_topic_score_codex":0.0011708165,"about_ca_topic_score_gemma":0.00010701779,"teacher_disagreement_score":0.77471983,"about_ca_system_score_codex":0.00013705957,"about_ca_system_score_gemma":0.00006912834,"threshold_uncertainty_score":0.9998993},"labels":[],"label_agreement":null},{"id":"W3004890840","doi":"10.5194/acp-20-8003-2020","title":"Smoke of extreme Australian bushfires observed in the stratosphere over Punta Arenas, Chile, in January 2020: optical thickness, lidar ratios, and depolarization ratios at 355 and 532 nm","year":2020,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":172,"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":"Goddard Space Flight Center; National Oceanic and Atmospheric Administration; Bundesministerium für Wirtschaft und Energie; European Commission; Deutsche Forschungsgemeinschaft; National Aeronautics and Space Administration","keywords":"Depolarization ratio; Lidar; Stratosphere; Wavelength; Aerosol; Atmospheric sciences; Smoke; Depolarization; Environmental science; Southern Hemisphere; Materials science; Remote sensing; Climatology; Optics; Meteorology; Geology; Physics","score_opus":0.018145533141095318,"score_gpt":0.21032011438846746,"score_spread":0.19217458124737213,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3004890840","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":[0.997461,0.0003815044,0.00015187748,0.0006044331,0.000010839981,0.00021701271,0.000009974289,0.000011392213,0.0011519267],"genre_scores_gemma":[0.9972973,0.0003167587,0.0018168134,0.00029681882,0.00007086972,0.0000145471295,0.000030099734,0.000013957257,0.00014285359],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987814,0.00004505774,0.00030845255,0.00040612664,0.00023661037,0.00022236517],"domain_scores_gemma":[0.9995176,0.00006896813,0.000108768436,0.00018611575,0.000006724457,0.00011183113],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009990961,0.00022899301,0.0002532339,2.9205577e-8,0.00010792058,0.00005458664,0.00015815003,0.00014248329,0.0005348626],"category_scores_gemma":[0.00002144642,0.00018954402,0.000032429743,0.00030850197,0.0003150437,0.00022462265,0.00014321807,0.00024843702,0.0000021616706],"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":[0.00007544881,0.00012093839,0.9276245,0.00015236546,0.00001935838,0.000020564556,0.002280521,0.0009841879,0.057808846,0.00007336765,0.00028432807,0.010555533],"study_design_scores_gemma":[0.00092885905,0.00006897317,0.9749994,0.000053189957,0.000036450037,0.000015026048,0.0011031616,0.013871822,0.0077398275,0.00045221654,0.00038492578,0.0003461134],"about_ca_topic_score_codex":0.0006424145,"about_ca_topic_score_gemma":0.00015231402,"teacher_disagreement_score":0.05006902,"about_ca_system_score_codex":0.000032674012,"about_ca_system_score_gemma":0.000021169892,"threshold_uncertainty_score":0.7729381},"labels":[],"label_agreement":null},{"id":"W3005983083","doi":"10.1029/2019jd031137","title":"Long‐Term Trends of High Aerosol Pollution Events and Their Climatic Impacts in North America Using Multiple Satellite Retrievals and Modern‐Era Retrospective Analysis for Research and Applications version 2","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":28,"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":"National Aeronautics and Space Administration","keywords":"Aerosol; Environmental science; Climatology; Shortwave radiation; Magnitude (astronomy); Atmospheric sciences; Satellite; Trend analysis; Precipitation; Pollution; Meteorology; Geography; Radiation; Geology","score_opus":0.046075742448783534,"score_gpt":0.33556065487798353,"score_spread":0.2894849124292,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3005983083","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":[0.99369234,0.000551364,0.0049703126,0.0003638032,0.000006088869,0.00034786802,0.000042518026,0.0000033298131,0.000022365528],"genre_scores_gemma":[0.996714,0.0011305212,0.0020109823,0.000019123154,0.00007026001,0.000010757846,0.0000053401614,0.000014890555,0.000024135257],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99766,0.00024632816,0.00044110202,0.00035962276,0.00082797016,0.0004649907],"domain_scores_gemma":[0.99846977,0.0005461702,0.00025000444,0.00017276392,0.00017343088,0.00038786264],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007366447,0.00015078239,0.0005035863,0.000015459229,0.000260892,0.00005674514,0.00021126996,0.00007361501,0.000047600744],"category_scores_gemma":[0.0003613251,0.0001145833,0.000102921265,0.0022991865,0.0006762665,0.00030999503,0.0003184743,0.0005075825,0.0000017745704],"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":[0.0009607043,0.0002763215,0.93481535,0.000069283196,0.00016308101,0.000004755237,0.0014770188,0.0016672286,0.013221261,0.0000139510375,0.000024330146,0.0473067],"study_design_scores_gemma":[0.0008753487,0.0012984419,0.95793533,0.000038134167,0.00004627572,0.0000016711541,0.00053319195,0.03777313,0.00042191497,0.00095656654,0.000019346697,0.00010062459],"about_ca_topic_score_codex":0.00085845205,"about_ca_topic_score_gemma":0.00044048252,"teacher_disagreement_score":0.047206074,"about_ca_system_score_codex":0.00025222576,"about_ca_system_score_gemma":0.000045483288,"threshold_uncertainty_score":0.46725714},"labels":[],"label_agreement":null},{"id":"W3006467930","doi":"","title":"Optical analysis of summer-time aerosol events over two southern Canadian sites using ground-based remote sensing techniques","year":2010,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Aerosol; Remote sensing; Environmental science; Meteorology; Geography","score_opus":0.013610703797924744,"score_gpt":0.25637874410674616,"score_spread":0.2427680403088214,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3006467930","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":[0.9942997,0.000005147481,0.0002884488,0.000063616404,0.000074954274,0.00015432865,0.000014959203,0.000068402696,0.005030456],"genre_scores_gemma":[0.9369605,5.6055416e-7,0.06260835,0.0002064298,0.00005576937,3.8424858e-7,0.000018585148,0.000034769717,0.00011463095],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9980133,0.000049496928,0.00046899178,0.00045590213,0.00044318906,0.0005691213],"domain_scores_gemma":[0.99874234,0.00014302843,0.00028882994,0.00045064604,0.000030221401,0.00034494317],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006206777,0.0002431895,0.0003622507,0.000019870904,0.00022655418,0.000048055652,0.00026009884,0.00018381292,0.00018346266],"category_scores_gemma":[0.00018767863,0.00024470282,0.00019120153,0.00055926247,0.00020999549,0.00010908118,0.000083465,0.00032331664,0.000095467636],"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":[0.000015217873,0.000051425974,0.44142562,0.000008959387,0.00013989634,0.00003941274,0.00026758917,0.025716312,0.52546495,0.0000013509199,0.00004018318,0.006829065],"study_design_scores_gemma":[0.00053436845,0.00008594902,0.55949223,0.00015495798,0.0011678855,0.000015298248,0.0002168098,0.3959754,0.040896248,0.00010268038,0.00023891199,0.0011192592],"about_ca_topic_score_codex":0.77688015,"about_ca_topic_score_gemma":0.6957475,"teacher_disagreement_score":0.48456872,"about_ca_system_score_codex":0.00017921465,"about_ca_system_score_gemma":0.00006903297,"threshold_uncertainty_score":0.99786913},"labels":[],"label_agreement":null},{"id":"W3006773386","doi":"10.5194/acp-20-14005-2020","title":"Is the near-spherical shape the “new black” for smoke?","year":2020,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":48,"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":"H2020 European Research Council; European Regional Development Fund; Deutscher Akademischer Austauschdienst; European Commission","keywords":"AERONET; Stratosphere; Wavelength; Aerosol; Smoke; Particle (ecology); Environmental science; Lidar; Scattering; Remote sensing; Troposphere; Atmospheric sciences; Computational physics; Physics; Meteorology; Optics; Geology","score_opus":0.014060555138809546,"score_gpt":0.22282433263253498,"score_spread":0.20876377749372543,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3006773386","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":[0.95123166,0.00021740528,0.017561935,0.020335454,0.000040150997,0.0003440012,0.000008810539,0.000058366102,0.010202193],"genre_scores_gemma":[0.9638528,0.00008513215,0.01459912,0.012499012,0.0007564822,0.000038012586,0.0000060872535,0.00003886289,0.0081244465],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990105,0.000012905184,0.00013880145,0.00035400706,0.00020559436,0.00027817328],"domain_scores_gemma":[0.9993486,0.00011042097,0.00007056714,0.00028617235,0.000007129748,0.00017710518],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00006125758,0.00020091316,0.0001575911,9.404166e-10,0.0003822361,0.000090406305,0.0003885389,0.00007053497,0.0068603023],"category_scores_gemma":[0.000020659594,0.000118768,0.00012206417,0.00021632244,0.00053907523,0.000069841444,0.00017111866,0.00018818471,0.00010836399],"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":[0.00015090122,0.00011545015,0.0192733,0.00009025991,0.0001290324,0.0000038953954,0.008087917,0.0047784466,0.010381412,0.00017744904,0.33928978,0.6175221],"study_design_scores_gemma":[0.00061194587,0.00009021827,0.006361002,0.0000075349612,0.00009154039,0.000004907053,0.0006587168,0.39105278,0.0045328615,0.00210278,0.59407085,0.00041485057],"about_ca_topic_score_codex":0.00008364025,"about_ca_topic_score_gemma":8.0099585e-7,"teacher_disagreement_score":0.6171073,"about_ca_system_score_codex":0.000024763101,"about_ca_system_score_gemma":0.000027748976,"threshold_uncertainty_score":0.9940476},"labels":[],"label_agreement":null},{"id":"W3006784488","doi":"10.1175/bams-d-18-0278.1","title":"AWARE: The Atmospheric Radiation Measurement (ARM) West Antarctic Radiation Experiment","year":2020,"lang":"en","type":"article","venue":"Bulletin of the American Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":98,"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":"Byrd Polar and Climate Research Center, Ohio State University; Deutsche Forschungsgemeinschaft; Goddard Space Flight Center; National Oceanic and Atmospheric Administration; Sight Research UK; National Aeronautics and Space Administration; Natural Environment Research Council; U.S. Department of Energy; U.S. Department of Defense; National Science Foundation","keywords":"Aerosol; Radiosonde; Environmental science; Arctic; Radiometer; Earth's energy budget; Cloud top; Meteorology; Atmospheric sciences; Remote sensing; Climatology; Cloud computing; Oceanography; Geology; Radiation; Geography; Physics","score_opus":0.016399715809037953,"score_gpt":0.21819052951059573,"score_spread":0.20179081370155777,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3006784488","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":[0.9422905,0.00037101744,0.0017498265,0.05393787,0.00011852834,0.0005199738,0.0000032577498,0.00006147136,0.0009475972],"genre_scores_gemma":[0.9789162,0.00020681969,0.003002532,0.017633082,0.00010728561,0.0000575196,0.0000012638086,0.00001554927,0.00005969642],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99780846,0.00033200704,0.00033093747,0.00038555713,0.0008179161,0.00032515373],"domain_scores_gemma":[0.9989293,0.00011262064,0.00046190707,0.00034914873,0.000017892027,0.00012910164],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005550411,0.00020737703,0.00029515996,1.4313513e-7,0.00032463102,0.000022393331,0.0006649739,0.00005572553,0.005125012],"category_scores_gemma":[0.0001684356,0.000110888206,0.00037628392,0.00040304632,0.0010093884,0.00002153015,0.00038090043,0.00023087472,0.00021143888],"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":[0.0004914591,0.001052285,0.26693964,0.00003669483,0.00044263486,0.000003584135,0.0064392667,0.03196219,0.07037667,0.00022030897,0.47773507,0.1443002],"study_design_scores_gemma":[0.0007262508,0.0011993524,0.6322144,0.000007008806,0.00012958463,0.0000036247397,0.0021406345,0.007742117,0.004615268,0.00010716199,0.350702,0.00041257686],"about_ca_topic_score_codex":0.000937397,"about_ca_topic_score_gemma":0.0000023232453,"teacher_disagreement_score":0.36527482,"about_ca_system_score_codex":0.00026171733,"about_ca_system_score_gemma":0.000017964474,"threshold_uncertainty_score":0.99578446},"labels":[],"label_agreement":null},{"id":"W3007903066","doi":"10.3390/atmos11030225","title":"Investigations on the Influence of Chemical Compounds on Fog Microphysical Parameters","year":2020,"lang":"en","type":"article","venue":"Atmosphere","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ontario Tech University; Environment and Climate Change Canada","funders":"","keywords":"Aerosol; Distilled water; Volume (thermodynamics); Chemical composition; Environmental science; Particle (ecology); Particle size; Particle counter; Environmental chemistry; Potassium; Chemistry; Materials science; Chromatography; Thermodynamics","score_opus":0.014589473862909952,"score_gpt":0.2049811447206606,"score_spread":0.19039167085775063,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3007903066","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":[0.98992246,0.0000040038744,0.00003072765,0.004879457,0.000017659439,0.00013624066,0.0000032323412,0.00002691073,0.004979299],"genre_scores_gemma":[0.99053705,0.0000018277187,0.0025924589,0.006760686,0.000024451088,0.000012994592,0.0000016114238,0.000012578791,0.000056347653],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9991194,0.00003664013,0.00016330877,0.00024597018,0.0002653227,0.00016934177],"domain_scores_gemma":[0.9993927,0.00015390458,0.00007545347,0.00024816307,0.0000057128213,0.00012405976],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000037394337,0.00013032414,0.00013622099,5.2008055e-8,0.0000740787,0.0000143219,0.00032944645,0.000050863866,0.00046087915],"category_scores_gemma":[0.000080568,0.00008787244,0.00007216401,0.0002312527,0.000510569,0.000047302023,0.00011348694,0.00019104146,0.00062864285],"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":[0.00017412027,0.0004835036,0.10367163,0.000025376596,0.00007645053,0.000014238058,0.0028045136,0.18972088,0.6292621,0.011465599,0.05836223,0.003939343],"study_design_scores_gemma":[0.002354614,0.003384112,0.4049804,0.0002654476,0.00016271432,0.00001046138,0.0016183433,0.041509554,0.5005657,0.010487757,0.032682784,0.0019781291],"about_ca_topic_score_codex":0.00012433581,"about_ca_topic_score_gemma":0.0000021020296,"teacher_disagreement_score":0.30130875,"about_ca_system_score_codex":0.00004096732,"about_ca_system_score_gemma":0.000010829518,"threshold_uncertainty_score":0.8080142},"labels":[],"label_agreement":null},{"id":"W3007966155","doi":"10.3390/rs12040668","title":"Construction of Nighttime Cloud Layer Height and Classification of Cloud Types","year":2020,"lang":"en","type":"article","venue":"Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":15,"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 Science Foundation of Zhejiang Province; State Key Laboratory of Modern Optical Instrumentation; Fundamental Research Funds for the Central Universities; National Key Research and Development Program of China; Environment and Climate Change Canada; National Natural Science Foundation of China","keywords":"Lidar; Remote sensing; Cloud top; Nadir; Radiance; Environmental science; Cloud computing; Satellite; Cloud height; Meteorology; Moderate-resolution imaging spectroradiometer; Spectroradiometer; Cloud base; Cloud fraction; Cloud cover; Pixel; Geology; Computer science; Geography","score_opus":0.017807976604608044,"score_gpt":0.21993288398637525,"score_spread":0.20212490738176722,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3007966155","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":[0.9819109,0.00005303271,0.011442718,0.0005123201,0.0000874023,0.000060403247,0.0000012359661,0.000014997145,0.005917003],"genre_scores_gemma":[0.97205925,0.000031201038,0.027702946,0.000077506935,0.00007055717,2.8022134e-9,0.000001109306,0.00000709654,0.0000503057],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99944025,0.000029210416,0.00017031992,0.0001509691,0.00012667621,0.000082567625],"domain_scores_gemma":[0.9997,0.00001990375,0.00012454331,0.00009511371,0.000010021901,0.0000503908],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000059297086,0.00006538135,0.00012779598,8.857466e-7,0.000037115642,0.000004690504,0.000035682973,0.000049645147,0.000098474135],"category_scores_gemma":[0.000021524555,0.000058642574,0.000026151536,0.00012493251,0.00019629025,0.000043349046,0.00004436329,0.00005391282,0.000024161787],"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":[0.0000504581,0.000011665529,0.0058468687,0.000038162612,0.000020656027,0.0000027573144,0.0013155071,0.00030984127,0.7766181,0.00041964478,0.00052527135,0.21484102],"study_design_scores_gemma":[0.0010710924,0.00032301847,0.06512786,0.00013510625,0.00013757613,0.00008484992,0.0016411868,0.7067902,0.20766635,0.0028201079,0.013628724,0.000573904],"about_ca_topic_score_codex":0.000075270924,"about_ca_topic_score_gemma":0.000005120618,"teacher_disagreement_score":0.7064804,"about_ca_system_score_codex":0.000017857978,"about_ca_system_score_gemma":0.0000058281767,"threshold_uncertainty_score":0.23913747},"labels":[],"label_agreement":null},{"id":"W3008959039","doi":"10.1175/jas-d-19-0179.1","title":"Perturbation Solution for Four-Stream Infrared Radiative Transfer","year":2020,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"","keywords":"Longwave; Radiative transfer; Perturbation (astronomy); Physics; Wavelength; Atmospheric radiative transfer codes; Computational physics; Scattering; Infrared; Environmental science; Optics; Quantum mechanics","score_opus":0.02783025526168792,"score_gpt":0.23016344079843604,"score_spread":0.20233318553674812,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3008959039","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":[0.9264164,0.00018645723,0.056314506,0.012787938,0.00054483383,0.0002812864,0.0000024518013,0.000013815883,0.0034523366],"genre_scores_gemma":[0.97594523,0.00002874553,0.021434622,0.0018396575,0.00018903981,0.0000045949237,1.1273184e-7,0.0000069134267,0.00055106345],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99879265,0.000059533966,0.0002956984,0.0001599787,0.00048739454,0.00020475154],"domain_scores_gemma":[0.9994698,0.000095126976,0.00021463445,0.000082444996,0.000026996375,0.0001109834],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038257724,0.00010593809,0.00015677605,2.5029075e-7,0.0003642768,0.000050004153,0.00060318195,0.000041756906,0.00044739823],"category_scores_gemma":[0.00020766821,0.000060651495,0.00018707813,0.00054208643,0.00037261756,0.00041817856,0.000059848517,0.000105860534,0.000012948143],"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":[0.0006377568,0.00034805652,0.19200394,0.000044477103,0.00017259411,0.000011195897,0.021479104,0.4874302,0.056927238,0.0012554554,0.11417104,0.12551895],"study_design_scores_gemma":[0.0019237187,0.0025334721,0.10477558,0.000054009928,0.00015537105,0.00006520462,0.0023166945,0.82430357,0.0037769296,0.008261529,0.05132801,0.00050590554],"about_ca_topic_score_codex":0.000019584597,"about_ca_topic_score_gemma":0.000004365474,"teacher_disagreement_score":0.33687338,"about_ca_system_score_codex":0.00009302184,"about_ca_system_score_gemma":0.00006278419,"threshold_uncertainty_score":0.48986968},"labels":[],"label_agreement":null},{"id":"W3009514934","doi":"10.5194/acp-2020-186","title":"Finely laminated Arctic mixed-phase clouds occur frequently and are correlated with snow","year":2020,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Snow; Environmental science; Precipitation; Arctic; Atmospheric sciences; Lidar; Climatology; The arctic; Sky; Meteorology; Geography; Geology; Remote sensing; Oceanography","score_opus":0.011205057837696921,"score_gpt":0.21110808767138636,"score_spread":0.19990302983368943,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3009514934","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":[0.98887867,0.0000469519,0.0029253329,0.0015189921,0.000047551428,0.00019073566,0.000007601634,0.0001199243,0.006264245],"genre_scores_gemma":[0.9948667,0.000015696833,0.0015068738,0.0017948408,0.000022468295,0.000008455244,0.000010137555,0.000020731888,0.0017540384],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988998,0.000030720446,0.00017073184,0.00039766481,0.00022437642,0.00027671683],"domain_scores_gemma":[0.9994367,0.000033878277,0.00008878524,0.00015987302,0.000010101759,0.00027069353],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000052482013,0.00019373234,0.00018943731,7.2257944e-7,0.00011151161,0.000037115984,0.00015101567,0.00007698651,0.005236448],"category_scores_gemma":[0.000041456573,0.00014020922,0.00002887295,0.0003195686,0.00022291116,0.00012744062,0.00012647148,0.00016915904,0.0004195504],"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":[0.00054420426,0.0006097982,0.9276226,0.00006240059,0.000115932184,0.0005338125,0.0019146765,0.00179743,0.006978149,0.00039100324,0.035410002,0.024019973],"study_design_scores_gemma":[0.013678848,0.004407774,0.8406074,0.00018291747,0.0002841629,0.00018943532,0.0043629683,0.10116929,0.0059787375,0.00036891262,0.026600886,0.0021686354],"about_ca_topic_score_codex":0.00034659315,"about_ca_topic_score_gemma":0.00014992556,"teacher_disagreement_score":0.09937186,"about_ca_system_score_codex":0.0000470333,"about_ca_system_score_gemma":0.000008756359,"threshold_uncertainty_score":0.9956729},"labels":[],"label_agreement":null},{"id":"W3010402549","doi":"10.1007/s10546-020-00505-0","title":"Suppression of “Handover” Processes in a Mountain Convective Boundary Layer due to Persistent Wildfire Smoke","year":2020,"lang":"en","type":"article","venue":"Boundary-Layer Meteorology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":false,"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 British Columbia","funders":"","keywords":"Mesoscale meteorology; Anticyclone; Lidar; Environmental science; Smoke; Meteorology; Boundary layer; Planetary boundary layer; Climatology; Convective available potential energy; Air quality index; Ceilometer; Atmospheric sciences; Convection; Atmospheric instability; Plume; Geology; Remote sensing; Geography","score_opus":0.020516377403472785,"score_gpt":0.2489368008080692,"score_spread":0.22842042340459642,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3010402549","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":[0.9904245,0.00073658396,0.00071314164,0.0034120798,0.00019480033,0.0006100991,0.000029824918,0.00005217457,0.0038267712],"genre_scores_gemma":[0.9936294,0.000040181487,0.0011484411,0.0047351127,0.00007312227,0.000097678756,0.000011772037,0.00004035238,0.0002239618],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9973955,0.00021261192,0.00051685,0.0007907412,0.00045874275,0.0006255124],"domain_scores_gemma":[0.99900097,0.0001380264,0.00018883198,0.00033117313,0.00002953523,0.00031144207],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003065627,0.0003380116,0.00063268875,0.0000101257165,0.00021312229,0.00005100764,0.0004978653,0.00022808617,0.002268453],"category_scores_gemma":[0.00028495913,0.0003010665,0.00014486583,0.0006893808,0.0005873204,0.00025644206,0.0005132984,0.00032616622,0.00018969575],"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":[0.004441867,0.00090940745,0.8132463,0.0002912012,0.00027052686,0.00043605463,0.034857914,0.0032025515,0.11669946,0.00019612169,0.014883403,0.010565191],"study_design_scores_gemma":[0.007839304,0.007627063,0.61773986,0.00016089698,0.00029576305,0.00023268718,0.0069522643,0.0039186077,0.04878513,0.002236601,0.30208495,0.0021269042],"about_ca_topic_score_codex":0.0014820494,"about_ca_topic_score_gemma":0.0007741058,"teacher_disagreement_score":0.28720155,"about_ca_system_score_codex":0.00024516677,"about_ca_system_score_gemma":0.00019779897,"threshold_uncertainty_score":0.99994415},"labels":[],"label_agreement":null},{"id":"W3010987304","doi":"","title":"Aerosol Radiative Forcing over Western Canada from CERES and MODIS Observations","year":2004,"lang":"en","type":"article","venue":"AGUSM","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Aerosol; Radiative forcing; Climatology; Environmental science; Forcing (mathematics); Atmospheric sciences; Meteorology; Remote sensing; Geography; Geology","score_opus":0.009587308864481872,"score_gpt":0.19133335568555632,"score_spread":0.18174604682107445,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3010987304","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":[0.9972719,0.00008718551,0.0010133986,0.0005017851,0.000068601046,0.00007850342,0.000020291074,0.000013937202,0.0009444111],"genre_scores_gemma":[0.9970242,0.000015709493,0.0014377388,0.00095622835,0.00003366309,0.000008316828,0.0000070840997,0.000008358404,0.0005087229],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99942017,0.000008140228,0.00009093479,0.00018046645,0.00014610142,0.00015421878],"domain_scores_gemma":[0.9997309,0.000028695948,0.000038263526,0.00011967414,0.000002200128,0.00008029942],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000018293269,0.00008524404,0.00008221898,3.0107353e-7,0.00012975074,0.000020194,0.00008465049,0.000029715657,0.00036632048],"category_scores_gemma":[0.000008794132,0.000076125725,0.000015015634,0.0000631527,0.00005839429,0.0001468493,0.000079392936,0.000055927183,0.000018904742],"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":[0.0000030445622,0.000013266904,0.98773855,0.000001157229,0.000011109138,0.000007423777,0.0008736247,0.007659154,0.0011870576,0.00008032215,0.0014974187,0.00092788116],"study_design_scores_gemma":[0.00031165231,0.0000144085925,0.9961397,0.000008367282,0.000008628535,6.971166e-7,0.00018962103,0.0005138616,0.00061362115,0.0006158741,0.0014611895,0.00012237376],"about_ca_topic_score_codex":0.90247536,"about_ca_topic_score_gemma":0.86359036,"teacher_disagreement_score":0.03888501,"about_ca_system_score_codex":0.00020075885,"about_ca_system_score_gemma":0.00003527538,"threshold_uncertainty_score":0.40109524},"labels":[],"label_agreement":null},{"id":"W3013577255","doi":"10.5194/amt-14-391-2021","title":"Classification of lidar measurements using supervised and unsupervised machine learning methods","year":2021,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Vector Institute; Western University","funders":"","keywords":"Lidar; Computer science; Artificial intelligence; Random forest; Support vector machine; Cluster analysis; Machine learning; Pattern recognition (psychology); Remote sensing; Geology","score_opus":0.0764194829131274,"score_gpt":0.30385557827589543,"score_spread":0.22743609536276804,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3013577255","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":[0.77502865,0.0018228895,0.2146543,0.00012959579,0.00008701906,0.00047574003,0.0000016597305,0.00027032444,0.0075298348],"genre_scores_gemma":[0.57120126,0.00014431603,0.42841497,0.00008054612,0.000015496396,0.00002552895,0.0000037001219,0.000029682291,0.00008447015],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9970594,0.0005210468,0.0005472284,0.00055980217,0.0009720396,0.00034048964],"domain_scores_gemma":[0.9989883,0.00003639441,0.00024272321,0.00043102738,0.00016148743,0.00014009293],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0017917143,0.00028914338,0.0003975887,0.0000011506994,0.00023724849,0.000040785875,0.00022718622,0.00013961004,0.0010064633],"category_scores_gemma":[0.00019506189,0.00027542663,0.00010387007,0.00055519026,0.00019746045,0.00020653923,0.0002443673,0.0002119841,0.000007242812],"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":[0.000016659633,0.000115169794,0.19775459,0.000033265595,0.000040506595,0.000002633709,0.00015980021,0.00006553047,0.71653587,0.00002699357,0.000039951272,0.08520902],"study_design_scores_gemma":[0.0010489302,0.00038037193,0.1965329,0.00022975609,0.00027560059,0.000037001395,0.0008905609,0.05411902,0.7335745,0.000551422,0.011376325,0.0009835756],"about_ca_topic_score_codex":0.00053869514,"about_ca_topic_score_gemma":0.000049317052,"teacher_disagreement_score":0.21376067,"about_ca_system_score_codex":0.0003230431,"about_ca_system_score_gemma":0.000063930966,"threshold_uncertainty_score":0.9999698},"labels":[],"label_agreement":null},{"id":"W3017261383","doi":"","title":"Lidar depolarization measurements of ice-precipitating liquid cloud layers during the 2012 Canadian Arctic ACE Validation Campaign","year":2012,"lang":"en","type":"article","venue":"AGUFM","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Lidar; Environmental science; Arctic; Remote sensing; Cloud computing; The arctic; Atmospheric sciences; Meteorology; Climatology; Geology; Oceanography; Geography; Computer science","score_opus":0.016822874048557483,"score_gpt":0.2230685266963491,"score_spread":0.20624565264779163,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3017261383","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":[0.995551,0.00012712013,0.0007051067,0.00015986444,0.00028578864,0.00019380846,0.0000023469868,0.000016065607,0.002958909],"genre_scores_gemma":[0.99842656,0.00000669638,0.00097009214,0.00012234594,0.0001160806,0.000012703755,0.0000053993376,0.000016953467,0.00032318578],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988505,0.00009797914,0.00019938109,0.00014251538,0.00033047367,0.00037914334],"domain_scores_gemma":[0.9994091,0.000041379997,0.0001380827,0.0002216762,0.000017579054,0.00017218315],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044743306,0.0001107221,0.000091459944,0.0000026837322,0.0002856254,0.000018408486,0.00019074335,0.00006034839,0.0008264474],"category_scores_gemma":[0.00010180499,0.00008852917,0.00003974896,0.00021501936,0.0000716409,0.00038279657,0.000063707506,0.000096332435,0.00016950212],"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":[0.00001840012,0.000040911986,0.9164901,0.000018725677,0.000025478754,5.418008e-7,0.0042769485,0.0070689404,0.07105347,0.00004040768,0.000106737825,0.0008593761],"study_design_scores_gemma":[0.0003626313,0.00009779673,0.91352266,0.00005076006,0.000074455784,0.000007150392,0.0014591212,0.00045133458,0.08188888,0.000041779494,0.0016792376,0.000364193],"about_ca_topic_score_codex":0.07153142,"about_ca_topic_score_gemma":0.02028657,"teacher_disagreement_score":0.051244855,"about_ca_system_score_codex":0.00034371618,"about_ca_system_score_gemma":0.000025479485,"threshold_uncertainty_score":0.99759066},"labels":[],"label_agreement":null},{"id":"W3019684140","doi":"","title":"Ice fog and light snow measurements using a high resolution camera system","year":2016,"lang":"en","type":"article","venue":"EGUGA","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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","funders":"","keywords":"Ice crystals; Snow; Remote sensing; Environmental science; Visibility; Radiative transfer; Meteorology; Optics; Atmospheric sciences; Geology; Physics","score_opus":0.019398187860343544,"score_gpt":0.21291016773770918,"score_spread":0.19351197987736563,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3019684140","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":[0.989916,0.00009162479,0.0036610225,0.0003261223,0.00018809174,0.000112583424,0.0000019658532,0.000043855915,0.005658699],"genre_scores_gemma":[0.99645585,0.0000064474852,0.0022938652,0.00006666591,0.00006823072,0.0000058246455,2.7959896e-7,0.000010774663,0.001092066],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99914956,0.000039180057,0.0001203407,0.00022999442,0.00025478538,0.00020616359],"domain_scores_gemma":[0.999676,0.0000125825845,0.00005965459,0.00016448784,0.000005815507,0.000081492726],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016181573,0.00009383989,0.00009490019,8.5950813e-7,0.00014474225,0.000017273276,0.000086790926,0.000047407775,0.00034500303],"category_scores_gemma":[0.000012498058,0.00006209612,0.000020548585,0.00007924337,0.00006657195,0.00013911031,0.000097566866,0.000031099007,0.0002044234],"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":[0.000052125168,0.00007685299,0.5364238,0.00003344799,0.00003988539,0.00001859476,0.0005373409,0.00019227262,0.4295106,0.00057671394,0.0074209427,0.02511739],"study_design_scores_gemma":[0.0042133857,0.0004508642,0.87740046,0.0010652184,0.0001984569,0.00014898909,0.0012395917,0.002705328,0.050333116,0.00040867657,0.06020546,0.0016304696],"about_ca_topic_score_codex":0.0006386595,"about_ca_topic_score_gemma":0.00004845012,"teacher_disagreement_score":0.37917748,"about_ca_system_score_codex":0.00028300952,"about_ca_system_score_gemma":0.000006031773,"threshold_uncertainty_score":0.37775415},"labels":[],"label_agreement":null},{"id":"W3021976739","doi":"","title":"Long-term Observations of the Convective Boundary Layer Using Insect Radar Returns at the SGP ARM Climate Research Facility","year":2009,"lang":"en","type":"article","venue":"University of North Texas Digital Library (University of North Texas)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"","keywords":"Convective Boundary Layer; Boundary layer; Meteorology; Planetary boundary layer; Cloud cover; Environmental science; Turbulence; Atmospheric sciences; Convection; Lidar; Daytime; Radar; Free convective layer; Plume; Geology; Mechanics; Geography; Physics; Remote sensing; Cloud computing","score_opus":0.03737729919220013,"score_gpt":0.21573361853874204,"score_spread":0.17835631934654192,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3021976739","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":[0.99307024,0.000041544503,0.00009583669,0.0004983224,0.00004321973,0.00044519964,0.0011394783,0.00003961891,0.0046265423],"genre_scores_gemma":[0.9958134,0.00008199341,0.0003191256,0.00006346031,0.000009253312,1.729134e-8,0.000117924865,0.000009686197,0.0035850862],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979514,0.0001873205,0.0002222107,0.00046574383,0.0007284684,0.0004448838],"domain_scores_gemma":[0.9985234,0.00016173386,0.00037467878,0.0007094362,0.00007465252,0.00015607981],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001623314,0.00022622297,0.00034633995,0.00002087481,0.001071301,0.00003640492,0.0014408956,0.0001018005,0.0012612682],"category_scores_gemma":[0.00002228247,0.00020610516,0.00031173363,0.0011548308,0.0025977942,0.0020086558,0.0018788584,0.00033706677,0.000068813824],"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":[0.00026046214,0.00030949904,0.99510366,0.000026943648,0.000057972185,0.0000295667,0.0003220354,0.00037434013,0.000012282375,0.000037659658,0.000951556,0.0025140236],"study_design_scores_gemma":[0.0005145406,0.000217172,0.9945797,0.00003415933,0.00005385585,0.000005580956,0.00020995326,0.00012517425,0.0000716961,0.00007187543,0.003913098,0.00020324647],"about_ca_topic_score_codex":0.000763628,"about_ca_topic_score_gemma":0.003827814,"teacher_disagreement_score":0.003064186,"about_ca_system_score_codex":0.00023336441,"about_ca_system_score_gemma":0.00015614503,"threshold_uncertainty_score":0.99965173},"labels":[],"label_agreement":null},{"id":"W3022110278","doi":"10.1016/0967-0653(96)86176-x","title":"10.1016/0967-0653(96)86176-x","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Large eddy simulation; Cloud computing; Marine stratocumulus; Meteorology; Atmospheric sciences; Environmental science; Boundary layer; Planetary boundary layer; Aerosol; Drizzle; Mechanics; Physics; Turbulence; Precipitation; Computer science","score_opus":0.0039205671724501364,"score_gpt":0.15701976181426455,"score_spread":0.15309919464181443,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3022110278","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.009833019,0.00001791332,0.0000043401074,0.00022962037,0.0000015206721,0.00012704785,0.0000038563544,0.00008861817,0.98969406],"genre_scores_gemma":[0.0016009272,2.572766e-7,0.00051006407,0.00013758772,0.000068619134,0.000014885432,0.000004372592,0.000020367861,0.99764293],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990182,0.000022051312,0.00013789836,0.0002754799,0.00023360705,0.00031278012],"domain_scores_gemma":[0.99948764,0.00001537468,0.000022087404,0.00028564717,0.0000029147072,0.00018632476],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00008835593,0.0001354228,0.00012220394,7.8842226e-7,0.00010711218,0.000027367218,0.00027399615,0.00005619904,0.99983954],"category_scores_gemma":[0.000008421756,0.00012172123,0.000052135976,0.00019725459,0.00007942995,0.00009980116,0.00009392117,0.000082367886,0.9994331],"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":[0.000020096815,0.000039338196,0.0000067936203,7.832113e-7,0.0000038437324,0.000004407246,0.000024925997,0.00063597655,0.00006556614,3.425536e-7,0.3426051,0.6565928],"study_design_scores_gemma":[0.00011878522,0.000098392695,0.00062194414,0.000003626052,0.000007296584,0.0000048713796,0.0000018938271,0.00034865548,0.00007194496,0.00000997346,0.9985329,0.00017972026],"about_ca_topic_score_codex":0.00013250906,"about_ca_topic_score_gemma":8.1476037e-7,"teacher_disagreement_score":0.6564131,"about_ca_system_score_codex":0.000070872185,"about_ca_system_score_gemma":0.000005365823,"threshold_uncertainty_score":0.49636474},"labels":[],"label_agreement":null},{"id":"W3022353906","doi":"10.5194/acp-20-13217-2020","title":"Environmental sensitivities of shallow-cumulus dilution – Part 1: Selected thermodynamic conditions","year":2020,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Compute Canada; Natural Sciences and Engineering Research Council of Canada; École de technologie supérieure; McGill University; U.S. Department of Energy","keywords":"Dilution; Cloud base; Atmospheric sciences; Environmental science; Buoyancy; Turbulence kinetic energy; Mixed layer; Turbulence; Meteorology; Geology; Physics; Cloud computing; Thermodynamics","score_opus":0.005056425673736332,"score_gpt":0.17954757959127507,"score_spread":0.17449115391753875,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3022353906","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":[0.99262285,0.000048235273,0.0016531461,0.00009489116,0.000014959975,0.00008004567,0.00004244876,0.00003929243,0.0054041035],"genre_scores_gemma":[0.99783397,0.00006154108,0.0011641275,0.00015514315,0.00008693232,0.00000824368,0.000054394233,0.000015924585,0.000619707],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99920917,0.000018331359,0.0001632884,0.0002649233,0.00016494795,0.00017936899],"domain_scores_gemma":[0.9996422,0.000026957976,0.00008725394,0.00012806675,0.0000038951107,0.000111640955],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000024804749,0.00016173143,0.00017435658,6.2479524e-9,0.000110688125,0.000010342533,0.00008400791,0.00006428995,0.004079668],"category_scores_gemma":[0.000006078445,0.00016179845,0.00005491256,0.00014797453,0.0003410073,0.00010243019,0.000080846425,0.00010754743,0.00004377683],"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":[0.000047355712,0.00020210535,0.04880883,0.00006592111,0.00006877076,0.000009515639,0.0013577071,0.0036155302,0.9074543,0.00005225932,0.000736298,0.037581403],"study_design_scores_gemma":[0.0017917586,0.0002980682,0.35691974,0.00005717899,0.00024338641,0.000039645078,0.0022989404,0.5238314,0.105054215,0.0014114822,0.006634411,0.0014197172],"about_ca_topic_score_codex":0.000045840927,"about_ca_topic_score_gemma":0.0000013673562,"teacher_disagreement_score":0.8024001,"about_ca_system_score_codex":0.000045107565,"about_ca_system_score_gemma":0.00000980263,"threshold_uncertainty_score":0.99683076},"labels":[],"label_agreement":null},{"id":"W3024776126","doi":"","title":"A 2-year climatology of Arctic clouds for Eureka, Canada prepared from High Spectral Resolution Lidar data.","year":2007,"lang":"en","type":"article","venue":"AGUFM","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Lidar; Arctic; Climatology; The arctic; Meteorology; Environmental science; Remote sensing; High resolution; Geography; Oceanography; Geology","score_opus":0.012345236232648507,"score_gpt":0.23215611819882415,"score_spread":0.21981088196617565,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3024776126","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":[0.994665,0.000064768414,0.0028489225,0.0002050512,0.00027565376,0.00020051196,0.0001448943,0.00001687052,0.0015783146],"genre_scores_gemma":[0.9865155,0.000009446504,0.012837668,0.00016535087,0.000092113514,0.000004712012,0.00011806281,0.000012974388,0.00024417858],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99884427,0.000021804924,0.0002546596,0.0003320571,0.00021089606,0.00033633536],"domain_scores_gemma":[0.99918276,0.000107316555,0.00011753708,0.0004963612,0.00000859033,0.00008745554],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020731021,0.000102694576,0.00017277643,8.832097e-7,0.000072076786,0.0000053464246,0.0003622383,0.00006824834,0.0007777399],"category_scores_gemma":[0.000063834836,0.00009710178,0.000030179124,0.00010504895,0.00011807503,0.00007502978,0.00018506315,0.000071631745,0.000024179752],"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":[0.00075253175,0.0002483516,0.9492481,0.00004899902,0.00010992649,0.00006046954,0.00063770777,0.0015127135,0.012222792,0.0019273112,0.029561982,0.0036691618],"study_design_scores_gemma":[0.0012510534,0.0002619672,0.9463243,0.000024118835,0.00009057132,0.000011599032,0.0005502213,0.004275976,0.0044566146,0.0021074705,0.04025732,0.00038878873],"about_ca_topic_score_codex":0.7316187,"about_ca_topic_score_gemma":0.7332391,"teacher_disagreement_score":0.01069534,"about_ca_system_score_codex":0.00018679674,"about_ca_system_score_gemma":0.00005698745,"threshold_uncertainty_score":0.85157067},"labels":[],"label_agreement":null},{"id":"W3025983844","doi":"10.5194/amt-13-3909-2020","title":"Using two-stream theory to capture fluctuations of satellite-perceived TOA SW radiances reflected from clouds over ocean","year":2020,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":5,"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":"Freie Universität Berlin; European Space Agency; Langley Research Center; National Aeronautics and Space Administration","keywords":"Effective radius; Radiance; Cloud albedo; Cloud fraction; Radiative transfer; Remote sensing; Environmental science; Cloud top; Albedo (alchemy); Cloud height; Atmospheric radiative transfer codes; Solar zenith angle; Shortwave; Meteorology; Optical depth; Cloud computing; Satellite; Physics; Cloud cover; Geology; Optics; Aerosol; Computer science","score_opus":0.040062678829773,"score_gpt":0.27179393667466306,"score_spread":0.23173125784489007,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3025983844","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":[0.89950633,0.0006795194,0.08826202,0.00043681776,0.00011037483,0.0009769066,0.000024478488,0.0004900706,0.009513479],"genre_scores_gemma":[0.78942704,0.00008124837,0.20870258,0.0015235529,0.00010377037,0.000023711475,0.000009491894,0.000046015717,0.000082623104],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9971642,0.00019955283,0.00055845466,0.0006786598,0.00097322196,0.00042590775],"domain_scores_gemma":[0.9987925,0.000051473085,0.00024780416,0.00050852983,0.000076656135,0.00032302365],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00039148767,0.00037802802,0.00044248783,8.8947326e-7,0.00016748557,0.000043171287,0.0005377929,0.00014333756,0.0033899609],"category_scores_gemma":[0.0001621088,0.00033854684,0.00014494774,0.0007224218,0.00021847042,0.00020582388,0.00018301266,0.00020836461,0.000058755155],"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":[0.00020978169,0.00020182034,0.06236655,0.000025341877,0.00014518593,0.000012402787,0.0046864813,0.0017228612,0.86998343,0.00027643738,0.003595122,0.05677457],"study_design_scores_gemma":[0.0030376678,0.0022814532,0.49721968,0.0008226026,0.0010258416,0.000013056537,0.0053191856,0.01737405,0.35622433,0.011424547,0.10056477,0.0046928297],"about_ca_topic_score_codex":0.0023567518,"about_ca_topic_score_gemma":0.00015072427,"teacher_disagreement_score":0.51375914,"about_ca_system_score_codex":0.00040499173,"about_ca_system_score_gemma":0.000059715017,"threshold_uncertainty_score":0.99990666},"labels":[],"label_agreement":null},{"id":"W3028454223","doi":"","title":"Surface Radiative Forcing by Clouds and Diamond Dust Measured During Winter 2006-2007 at Eureka, Canada","year":2007,"lang":"en","type":"article","venue":"AGUFM","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Radiative forcing; Forcing (mathematics); Environmental science; Atmospheric sciences; Radiative transfer; Meteorology; Climatology; Geography; Aerosol; Geology; Physics; Optics","score_opus":0.0048511428198952326,"score_gpt":0.18695886840201004,"score_spread":0.1821077255821148,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3028454223","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":[0.98941416,0.0005933315,0.00027137971,0.00016925977,0.0002167053,0.00014303433,0.000019469924,0.000024132778,0.009148549],"genre_scores_gemma":[0.98716176,0.000028714354,0.00025581254,0.00037523897,0.00005961606,0.000002036173,0.0000047620756,0.000023686407,0.012088375],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99858195,0.000025332156,0.00020298816,0.00034202496,0.00034983005,0.00049789],"domain_scores_gemma":[0.9994322,0.000056603327,0.00008365689,0.0001821868,0.000007239993,0.00023810084],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00023188899,0.00018567203,0.0001659456,8.075552e-7,0.00026433571,0.000019620065,0.00014297511,0.000073671494,0.0011451745],"category_scores_gemma":[0.000022752814,0.00017062576,0.000031963707,0.00012871422,0.00013376812,0.00011631387,0.00018053708,0.0001365334,0.000055227],"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":[0.000061993014,0.000027291178,0.9059703,0.00000990697,0.000030249794,0.000070188675,0.0007803126,0.0026999868,0.032852605,0.0000035575783,0.056366477,0.0011271546],"study_design_scores_gemma":[0.00091937045,0.000059577218,0.9108051,0.000022792603,0.00002862127,0.000028482273,0.0006957615,0.0010624287,0.035012882,0.00001550744,0.050755728,0.00059375743],"about_ca_topic_score_codex":0.28137287,"about_ca_topic_score_gemma":0.48194617,"teacher_disagreement_score":0.2005733,"about_ca_system_score_codex":0.00062999234,"about_ca_system_score_gemma":0.000020586316,"threshold_uncertainty_score":0.9997679},"labels":[],"label_agreement":null},{"id":"W3033869568","doi":"10.1080/02786826.2020.1777252","title":"Determining the cutoff diameter and counting efficiency of optical particle counters with an aerodynamic aerosol classifier and an inkjet aerosol generator","year":2020,"lang":"en","type":"article","venue":"Aerosol Science and Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":22,"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":"Japan Society for the Promotion of Science; Mitacs","keywords":"Aerosol; Dispersity; Particle counter; Particle size; Particle (ecology); Particle number; Aerodynamic diameter; Cutoff; Materials science; Optics; Analytical Chemistry (journal); Chemistry; Chromatography; Physics; Volume (thermodynamics)","score_opus":0.010489882328938846,"score_gpt":0.22563372572786605,"score_spread":0.2151438433989272,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3033869568","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":[0.9971698,0.00004977054,0.00078486995,0.0014460604,0.000033221786,0.0002855945,0.000003831894,0.000075812146,0.00015107548],"genre_scores_gemma":[0.9955413,0.000033898225,0.0034076038,0.00094349583,0.000021304215,0.000025280748,8.673147e-7,0.000018248682,0.000008043509],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9978164,0.00003499678,0.0002870478,0.00080922176,0.0004773063,0.000575048],"domain_scores_gemma":[0.9990973,0.000054929387,0.00014107572,0.0003705554,0.00005672693,0.0002794344],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00045242233,0.00023680522,0.00027517191,0.000007619643,0.0006180745,0.0001565698,0.00051685894,0.00013364726,0.000029875095],"category_scores_gemma":[0.00012911178,0.00015626682,0.000014837658,0.0008984639,0.006363154,0.00070464733,0.0005063022,0.00024410826,0.0000048051743],"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":[0.000041177205,0.000110917776,0.4955709,0.000013819617,0.000009008402,0.0000094994,0.0014272918,0.000046100755,0.48651797,0.0004989577,0.000025929616,0.01572843],"study_design_scores_gemma":[0.0055052326,0.014682042,0.15851553,0.0001271746,0.00028384136,0.00033127176,0.01560993,0.4141988,0.38758814,0.00025089982,0.00026815062,0.0026390287],"about_ca_topic_score_codex":0.0000578686,"about_ca_topic_score_gemma":0.00016500583,"teacher_disagreement_score":0.41415268,"about_ca_system_score_codex":0.000038539947,"about_ca_system_score_gemma":0.000054165284,"threshold_uncertainty_score":0.99634093},"labels":[],"label_agreement":null},{"id":"W3034446243","doi":"10.5194/acp-21-1507-2021","title":"An overview of the ORACLES (ObseRvations of Aerosols above CLouds and their intEractionS) project: aerosol–cloud–radiation interactions in the southeast Atlantic basin","year":2021,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":315,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Mount Allison University","funders":"Agence Nationale de la Recherche; Natural Environment Research Council; Sight Research UK; National Aeronautics and Space Administration","keywords":"Aerosol; Environmental science; Climatology; Climate model; Meteorology; Atmospheric sciences; Climate change; Geography; Geology; Oceanography","score_opus":0.027557168368818795,"score_gpt":0.2689839567802514,"score_spread":0.24142678841143259,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3034446243","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":[0.99796367,0.0002469317,0.00034691524,0.00027042368,0.000059057616,0.00016296968,0.000024693103,0.00000858751,0.000916731],"genre_scores_gemma":[0.9980722,0.00028186454,0.0011168789,0.0001345872,0.00007668581,0.000024735265,0.00002059751,0.000011773275,0.00026066494],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990672,0.000097435244,0.00028959374,0.00025079856,0.0001512394,0.00014373114],"domain_scores_gemma":[0.99919873,0.00014203622,0.00019971968,0.00039878144,0.000026889014,0.000033864904],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012062576,0.00016073228,0.00020521547,4.9660873e-8,0.00016090497,0.000036564452,0.00020212392,0.000040949577,0.00029713876],"category_scores_gemma":[0.000027101014,0.00010600549,0.00007655506,0.0005181369,0.00024661457,0.00021405255,0.000094378294,0.00019746741,0.0000016674242],"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":[0.000060519225,0.0013994161,0.6073483,0.0003127319,0.00009731376,0.000002981289,0.01680186,0.0027126477,0.30411693,0.0008760402,0.00066770485,0.06560353],"study_design_scores_gemma":[0.0012501471,0.0001130919,0.826005,0.00049518544,0.00020435039,0.00012489896,0.030086653,0.054595105,0.07535538,0.0027306068,0.00825162,0.00078800396],"about_ca_topic_score_codex":0.0009771715,"about_ca_topic_score_gemma":0.0002190573,"teacher_disagreement_score":0.22876157,"about_ca_system_score_codex":0.000033285152,"about_ca_system_score_gemma":0.000041845648,"threshold_uncertainty_score":0.43227783},"labels":[],"label_agreement":null},{"id":"W3035896573","doi":"10.5194/amt-13-5681-2020","title":"A technical description of the Balloon Lidar Experiment (BOLIDE)","year":2020,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"National Aeronautics and Space Administration","keywords":"Lidar; Payload (computing); Remote sensing; Backscatter (email); Balloon; Environmental science; Altitude (triangle); Geology; High resolution; Meteorology; Physics; Engineering; Computer science","score_opus":0.032556289754048534,"score_gpt":0.223942513744415,"score_spread":0.19138622399036648,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3035896573","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":[0.68683124,0.00096160837,0.22713305,0.0054914486,0.0003440346,0.0032357697,0.000004232675,0.0014004292,0.07459816],"genre_scores_gemma":[0.9326684,0.000037503523,0.06575725,0.0012070677,0.00005408621,0.00012912942,5.004585e-7,0.00002861249,0.000117480704],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9975436,0.00010461554,0.0004586301,0.00041199208,0.0011790304,0.0003021378],"domain_scores_gemma":[0.9991098,0.000009599107,0.00022742125,0.0004713894,0.00003951993,0.00014227368],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004308793,0.00024142627,0.00026735518,2.2889266e-7,0.00013279931,0.000024397124,0.0006367196,0.000120550205,0.0012897494],"category_scores_gemma":[0.00010244904,0.00016892905,0.00017790783,0.00047402416,0.00025781972,0.00014286206,0.0004201801,0.00019862296,0.000050805975],"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":[0.000044860953,0.00019240691,0.041393217,0.000020596774,0.000017365674,0.000002296996,0.00042815812,0.00005452103,0.92264724,0.00020270236,0.017727247,0.01726939],"study_design_scores_gemma":[0.00050142396,0.0008533124,0.07907409,0.00013585799,0.00009980101,0.000010559205,0.00038177197,0.0010740837,0.81701565,0.0006252761,0.099526756,0.0007013958],"about_ca_topic_score_codex":0.00026356822,"about_ca_topic_score_gemma":0.000024815983,"teacher_disagreement_score":0.2458371,"about_ca_system_score_codex":0.00034157265,"about_ca_system_score_gemma":0.00003348902,"threshold_uncertainty_score":0.9996232},"labels":[],"label_agreement":null},{"id":"W3036117470","doi":"10.5194/acp-20-11767-2020","title":"Review of experimental studies of secondary ice production","year":2020,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":294,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Federal Aviation Administration; Helmholtz Association; Environment and Climate Change Canada; Transport Canada","keywords":"Fragmentation (computing); Ice crystals; Environmental science; Hard rime; Ice formation; Ice nucleus; Atmospheric sciences; Meteorology; Computer science; Chemistry; Geography; Geology; Nucleation","score_opus":0.016540751480705062,"score_gpt":0.25225629622027707,"score_spread":0.235715544739572,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3036117470","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":[0.9583059,0.03484916,0.00008915706,0.00022584153,0.0000249574,0.00009951365,0.0000026263056,0.000012920098,0.0063899113],"genre_scores_gemma":[0.9816174,0.011005403,0.0061028115,0.0006281233,0.00011169312,0.000010656505,0.0000041155654,0.000010850088,0.00050893775],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9994042,0.000010068843,0.00018782058,0.00019891557,0.00011792674,0.00008107057],"domain_scores_gemma":[0.99967885,0.000012371762,0.00012368805,0.00012310046,0.000012445088,0.00004954294],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00004485936,0.000102391816,0.00022926448,2.0442403e-9,0.00003366899,0.0000015450162,0.000079860365,0.000022895028,0.0016463519],"category_scores_gemma":[0.000021494032,0.00009154733,0.00004743025,0.00014741084,0.00024981616,0.00007301485,0.000091613605,0.00006366393,0.0000066750836],"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":[0.000045158613,0.00022028599,0.0046657403,0.008960893,0.00010363825,0.0000016972504,0.0024680165,0.00019357134,0.8056743,0.000019845013,0.014398613,0.16324823],"study_design_scores_gemma":[0.0003382501,0.00015860601,0.0011440358,0.0009909861,0.000083152845,0.000006557566,0.0018429983,0.00080189505,0.97997946,0.00015123456,0.014186746,0.00031609103],"about_ca_topic_score_codex":0.00001325382,"about_ca_topic_score_gemma":6.931229e-8,"teacher_disagreement_score":0.17430514,"about_ca_system_score_codex":0.000016929007,"about_ca_system_score_gemma":0.000008908854,"threshold_uncertainty_score":0.99926627},"labels":[],"label_agreement":null},{"id":"W3036740076","doi":"10.1680/jenes.20.00019","title":"Spatio-temporal variation of aerosols in ENSO events over Western India using satellite data","year":2020,"lang":"en","type":"article","venue":"Journal of Environmental Engineering and Science","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Aerosol; Moderate-resolution imaging spectroradiometer; Environmental science; Climatology; Satellite; Spectroradiometer; Seasonality; Atmospheric sciences; Spatial variability; El Niño Southern Oscillation; Spring (device); Atmosphere (unit); Variation (astronomy); Meteorology; Geography; Geology; Reflectivity","score_opus":0.016736436902298594,"score_gpt":0.223917900669842,"score_spread":0.2071814637675434,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3036740076","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":[0.9969322,0.00010288211,0.0027734744,0.000040113944,0.00006933157,0.000053403528,0.0000072330877,0.0000024897583,0.00001883924],"genre_scores_gemma":[0.99205345,0.00008591497,0.007777245,0.00004057216,0.000029737756,1.999974e-7,0.0000012795879,0.000006892579,0.0000047188437],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99885345,0.000012693197,0.00033682797,0.00019430995,0.00044121293,0.00016153761],"domain_scores_gemma":[0.9994964,0.000017045364,0.00021055488,0.0001364109,0.0000017470452,0.00013783269],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038813287,0.00009586595,0.00015976377,0.0000073133697,0.00003734612,0.000017197764,0.00035293953,0.000031236963,0.00010012899],"category_scores_gemma":[0.000034381443,0.00008636106,0.000021317044,0.00021654388,0.00014329086,0.0006786824,0.00030371154,0.00012213444,0.0000030225008],"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":[0.000015147355,0.00003979225,0.82128334,0.000007568247,0.0000039771876,0.000008322323,0.00060560287,0.036210608,0.14053082,0.0000030180552,0.0000019713978,0.0012898486],"study_design_scores_gemma":[0.0002732181,0.00010298753,0.946389,0.000026230511,0.000007962948,0.000017260732,0.000048602487,0.052176718,0.00068747636,0.0000065390486,0.00017271366,0.00009129257],"about_ca_topic_score_codex":0.000033235294,"about_ca_topic_score_gemma":0.000001932775,"teacher_disagreement_score":0.13984334,"about_ca_system_score_codex":0.00010479943,"about_ca_system_score_gemma":0.000015061105,"threshold_uncertainty_score":0.3521702},"labels":[],"label_agreement":null},{"id":"W3041045700","doi":"10.1051/epjconf/202023702017","title":"Is Near-Spherical Shape “the New Black” for Smoke ?","year":2020,"lang":"en","type":"article","venue":"EPJ Web of Conferences","topic":"Atmospheric aerosols and clouds","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":"Stavros Niarchos Foundation","keywords":"Wavelength; Smoke; Stratosphere; Scattering; Lidar; Depolarization ratio; Physics; Particle (ecology); Computational physics; Environmental science; Optics; Meteorology; Geology","score_opus":0.03824753335875648,"score_gpt":0.2584694825070708,"score_spread":0.22022194914831433,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3041045700","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":[0.92068326,0.0000949528,0.004433313,0.029724468,0.00010355694,0.00029470213,0.000009764506,0.00003584397,0.044620115],"genre_scores_gemma":[0.9925978,0.00002628107,0.0032418012,0.0028698791,0.00009566065,0.0000075898815,0.0000013190046,0.0000076203037,0.0011520309],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991287,0.000017880224,0.00019153509,0.00022505176,0.00024375612,0.0001930704],"domain_scores_gemma":[0.9995471,0.00007455732,0.00009087495,0.00013809609,0.000009348666,0.0001400246],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0000734652,0.00011183544,0.00017005838,2.07443e-7,0.000090348054,0.000042446805,0.00041008028,0.000051638683,0.024146408],"category_scores_gemma":[0.000046885758,0.00007329498,0.000090574074,0.00014035084,0.00045755025,0.00006430907,0.000116208066,0.000077264835,0.00020841358],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020305724,0.00011961122,0.37989932,0.000041454874,0.00009143216,0.0000032109965,0.008811713,0.0006688015,0.0051397406,0.0056808125,0.43295,0.16639087],"study_design_scores_gemma":[0.0004652358,0.00041317355,0.05665545,0.000009186704,0.000031197826,6.435195e-7,0.0007934894,0.06675077,0.0018715573,0.0013179792,0.8714764,0.0002149047],"about_ca_topic_score_codex":0.00034478275,"about_ca_topic_score_gemma":0.000038167625,"teacher_disagreement_score":0.43852642,"about_ca_system_score_codex":0.000009321669,"about_ca_system_score_gemma":0.00018138146,"threshold_uncertainty_score":0.97674567},"labels":[],"label_agreement":null},{"id":"W3041453154","doi":"","title":"Recent work in Canada for the proposed Chemical and Aerosol Sounding Satellite (CASS) mission","year":2010,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Depth sounding; Satellite; Work (physics); Aerosol; Remote sensing; Earth observation satellite; Meteorology; Environmental science; Astrobiology; Engineering; Geology; Geography; Aerospace engineering; Oceanography; Physics; Mechanical engineering","score_opus":0.012429283723938598,"score_gpt":0.22029132345258262,"score_spread":0.20786203972864403,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3041453154","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":[0.99639285,0.000115329516,0.0000042762013,0.00090897834,0.00031705434,0.0003266356,9.043849e-7,0.000014326878,0.0019196623],"genre_scores_gemma":[0.99705243,0.00009204431,0.0024153087,0.00021296262,0.00006391461,0.0000052055793,0.000002136086,0.000015459385,0.00014054336],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988826,0.000014499669,0.00024155526,0.00028287712,0.00022426354,0.00035421128],"domain_scores_gemma":[0.9992639,0.00031753173,0.00010546794,0.00017802631,0.000006956852,0.00012814719],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040101187,0.0001315912,0.00011510122,7.811267e-7,0.0001631721,0.000042091084,0.00018474102,0.000072251154,0.000027105656],"category_scores_gemma":[0.00027128364,0.0000912306,0.000020790558,0.000110719484,0.0000833875,0.00005239305,0.00008941961,0.0002798614,0.00000869278],"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":[0.00009324203,0.000056634683,0.7320099,0.000019794998,0.00000955134,0.000016984037,0.00073413685,0.0019322817,0.13770863,0.000006526222,0.0014141093,0.12599823],"study_design_scores_gemma":[0.0009436332,0.000042180523,0.90043736,0.00014847856,0.000031065934,0.000020241447,0.0013636309,0.00212617,0.03738607,0.00013564617,0.05674053,0.0006249878],"about_ca_topic_score_codex":0.5497494,"about_ca_topic_score_gemma":0.8352245,"teacher_disagreement_score":0.28547513,"about_ca_system_score_codex":0.00017528234,"about_ca_system_score_gemma":0.00007023721,"threshold_uncertainty_score":0.4532489},"labels":[],"label_agreement":null},{"id":"W3041479724","doi":"10.1051/epjconf/202023701005","title":"Development of ATLID Retrieval Algorithms","year":2020,"lang":"en","type":"article","venue":"EPJ Web of Conferences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":11,"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":"Lidar; Remote sensing; Aerosol; Cloud computing; Environmental science; Meteorology; Computer science; Spectral resolution; Key (lock); Physics; Geology; Astronomy","score_opus":0.0290342568083385,"score_gpt":0.23861030621465495,"score_spread":0.20957604940631647,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3041479724","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":[0.9508301,0.00003886896,0.0015819826,0.00029512047,0.000051656225,0.000068286965,0.0000026078055,0.000015082437,0.0471163],"genre_scores_gemma":[0.9800743,0.000014792195,0.019644735,0.000080456935,0.000019661013,0.0000012118593,0.0000016480865,0.0000039049837,0.00015930827],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99912137,0.000014317926,0.00026851098,0.00015850531,0.00031678408,0.00012048559],"domain_scores_gemma":[0.99967605,0.000019610956,0.0001315079,0.00008169937,0.000010293414,0.00008084621],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00009954632,0.000082649574,0.00017477327,7.03918e-7,0.000033959488,0.000006017658,0.00023746661,0.000039008333,0.005889297],"category_scores_gemma":[0.00002513294,0.00006687243,0.00003497372,0.00015493036,0.0001892978,0.00005102298,0.00012431154,0.000051586892,0.000082803286],"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":[0.0002311874,0.00028537505,0.55087745,0.00010687795,0.00012331265,0.000009494251,0.012518553,0.00027228973,0.21974601,0.00423303,0.0045653107,0.20703109],"study_design_scores_gemma":[0.0011610728,0.0006575045,0.31199476,0.00007203775,0.000041150808,0.0000021032229,0.0042995913,0.009384291,0.37500623,0.0005334955,0.296172,0.00067574624],"about_ca_topic_score_codex":0.000037176815,"about_ca_topic_score_gemma":0.000014233628,"teacher_disagreement_score":0.2916067,"about_ca_system_score_codex":0.000011701595,"about_ca_system_score_gemma":0.00017954376,"threshold_uncertainty_score":0.99501944},"labels":[],"label_agreement":null},{"id":"W3041552389","doi":"","title":"Radar, Radiometers, Interferometer and Lidar in Eureka, Canada and Barrow, Alaska for Cloud and Aerosol Studies","year":2008,"lang":"en","type":"article","venue":"AGUFM","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Lidar; Remote sensing; Environmental science; Radiometer; Aerosol; Meteorology; Radar; Cloud computing; Geology; Geography; Computer science; Telecommunications","score_opus":0.015546161059536332,"score_gpt":0.22075367485743538,"score_spread":0.20520751379789906,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3041552389","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":[0.9972823,0.0017364988,0.000055787674,0.00041486847,0.00013003894,0.00020886098,0.000009131566,0.000008848331,0.0001536445],"genre_scores_gemma":[0.9960399,0.0008228799,0.0018763954,0.0004819199,0.000031566007,0.000021894803,0.0000013682638,0.000013074317,0.00071096816],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991337,0.000023291705,0.00016400362,0.00030821774,0.00012392057,0.00024688992],"domain_scores_gemma":[0.999636,0.0000995479,0.000039971303,0.00011067374,0.00000451684,0.00010928694],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000100351506,0.00014828428,0.00022465867,0.0000026648145,0.00013901008,0.000013883713,0.000072708324,0.000040991777,0.000042685777],"category_scores_gemma":[0.000035899557,0.00012441349,0.00001598415,0.00010315072,0.00032571427,0.000101709295,0.00016185241,0.000073561925,0.0000012509057],"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":[0.00011530898,0.000056271605,0.9519755,0.00008217084,0.000099881945,0.00012177107,0.0068421867,0.000035864512,0.0052872086,0.000018928768,0.01901572,0.016349154],"study_design_scores_gemma":[0.005610142,0.0014207574,0.935395,0.00013864717,0.00010593657,0.0004841,0.00500705,0.0011333273,0.006488295,0.00044911337,0.042164292,0.0016033489],"about_ca_topic_score_codex":0.06436522,"about_ca_topic_score_gemma":0.17553917,"teacher_disagreement_score":0.111173935,"about_ca_system_score_codex":0.00008762174,"about_ca_system_score_gemma":0.000016175458,"threshold_uncertainty_score":0.94186527},"labels":[],"label_agreement":null},{"id":"W3042211954","doi":"10.1051/epjconf/202023708016","title":"Optical Properties of Canadian Biomass Burning Particles Over Europe Observed with Calipso and Ground-Based Lidar Systems","year":2020,"lang":"en","type":"article","venue":"EPJ Web of Conferences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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":"Lidar; Backscatter (email); Angstrom exponent; Biomass (ecology); Biomass burning; Environmental science; Atmospheric sciences; Aerosol; Depolarization ratio; Angstrom; Remote sensing; Meteorology; Physics; Geology; Chemistry; Oceanography","score_opus":0.046404845413595096,"score_gpt":0.19613545639839702,"score_spread":0.14973061098480192,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3042211954","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":[0.9949542,0.00018656226,0.00009622681,0.0007182746,0.000022517792,0.0001201102,0.000005227302,0.0000132030855,0.00388362],"genre_scores_gemma":[0.9994452,0.00001158102,0.00040964969,0.000071996685,0.000014287239,0.000005467921,8.4648394e-7,0.000007602577,0.000033377608],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991436,0.000046553196,0.00020219795,0.00018735167,0.0002333151,0.00018697114],"domain_scores_gemma":[0.9995546,0.000022708125,0.0000922544,0.00009332827,0.000021863358,0.0002152849],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009120726,0.000109021465,0.00020584614,0.000003417887,0.000058743364,0.000040930503,0.00013623378,0.000036965026,0.00023601815],"category_scores_gemma":[0.000033954086,0.0000724524,0.000018233863,0.00027153592,0.00048600376,0.000086797925,0.000041905834,0.000053312695,0.000007487709],"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":[0.00007246395,0.000031482876,0.9343804,0.00011085249,0.000029027822,0.000013671105,0.0006472585,0.0009774797,0.06134926,0.0017396803,0.00008488412,0.0005635343],"study_design_scores_gemma":[0.0010965682,0.0012754377,0.8548367,0.00032512055,0.00008200442,0.000005095335,0.0029802993,0.07810578,0.04820052,0.0000213395,0.01255627,0.0005148355],"about_ca_topic_score_codex":0.09593031,"about_ca_topic_score_gemma":0.018861609,"teacher_disagreement_score":0.07954367,"about_ca_system_score_codex":0.000013026839,"about_ca_system_score_gemma":0.00025367303,"threshold_uncertainty_score":0.9990416},"labels":[],"label_agreement":null},{"id":"W3042216271","doi":"10.1051/epjconf/202023702036","title":"Wildfire Smoke in the Stratosphere Over Europe–First Measurements of Depolarization and Lidar Ratios at 355, 532, and 1064 nm","year":2020,"lang":"en","type":"article","venue":"EPJ Web of Conferences","topic":"Atmospheric aerosols and clouds","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":"Stratosphere; Lidar; Depolarization ratio; Environmental science; Wavelength; Altitude (triangle); Atmospheric sciences; Smoke; Troposphere; Plume; Aerosol; Remote sensing; Meteorology; Physics; Optics; Geography","score_opus":0.029985244360407698,"score_gpt":0.22255133639240557,"score_spread":0.19256609203199787,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3042216271","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":[0.98542786,0.00020172134,0.000058141923,0.000573623,0.000016708917,0.00015258402,0.0000034858035,0.0000052518253,0.0135606],"genre_scores_gemma":[0.99948514,0.00011481833,0.00014968915,0.00019850598,0.000011079152,0.000003271348,0.0000021714613,0.0000047652397,0.000030580246],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991392,0.00006472921,0.00020906227,0.00018028221,0.0003069622,0.00009977602],"domain_scores_gemma":[0.9996924,0.000034349763,0.00012639853,0.00009232307,0.000008081613,0.00004646161],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001402581,0.00009758555,0.00014259793,8.715984e-7,0.000068821755,0.000025868188,0.00015398247,0.000040544255,0.0006482432],"category_scores_gemma":[0.000036668556,0.000067933266,0.000015023318,0.00015611094,0.00023652762,0.00012366491,0.0000940642,0.00006008588,0.0000036244048],"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":[0.000017711176,0.000022899314,0.9904564,0.000015378191,0.000006825298,9.64807e-7,0.0011226514,0.000031841915,0.0065999115,0.00016894586,0.000115352865,0.0014411154],"study_design_scores_gemma":[0.00035962078,0.00014891101,0.9935928,0.000024747016,0.000014034231,9.597061e-7,0.0005530153,0.00095189165,0.0026352806,0.000054276734,0.0015732945,0.000091152666],"about_ca_topic_score_codex":0.0005735892,"about_ca_topic_score_gemma":0.0014016721,"teacher_disagreement_score":0.014057235,"about_ca_system_score_codex":0.000007904832,"about_ca_system_score_gemma":0.0000421088,"threshold_uncertainty_score":0.7097808},"labels":[],"label_agreement":null},{"id":"W3043145035","doi":"10.5194/egusphere-egu2020-13461","title":"Validation for ESA&amp;#8217;s Aeolus Mission using the in-situ instruments at Canadian Arctic and reanalysis data","year":2020,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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; Environment and Climate Change Canada; University of Toronto","funders":"","keywords":"Radiosonde; Lidar; Environmental science; Meteorology; Rayleigh scattering; Atmospheric sciences; Remote sensing; Physics; Geography; Optics","score_opus":0.06710588017865922,"score_gpt":0.2760648879851202,"score_spread":0.20895900780646098,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3043145035","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":[0.99334735,0.000015541647,0.0018957072,0.0028798063,0.00002295641,0.0001887037,0.000007857449,0.000006311864,0.0016357978],"genre_scores_gemma":[0.99248445,0.000015254048,0.0061250273,0.000823698,0.000018465911,0.000001924096,0.000052647098,0.000007070213,0.0004714394],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99924904,0.000025225234,0.00012802286,0.00028336357,0.00013712165,0.00017724444],"domain_scores_gemma":[0.9994845,0.000020682868,0.000040459578,0.00027922404,0.0000031840761,0.00017194619],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014690726,0.00007667211,0.000083493636,0.0000012929038,0.00020853843,0.000032381184,0.00023218872,0.000034283286,0.00086630293],"category_scores_gemma":[0.00005473079,0.00005310767,0.000016711583,0.00019067212,0.00005620387,0.00015837535,0.00031551262,0.000043739474,0.00002702739],"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":[0.000043872173,0.000027664466,0.9229414,0.000022361024,0.000041333467,0.000003891073,0.0017285006,0.0041639153,0.034287564,0.000041946692,0.0043788557,0.032318696],"study_design_scores_gemma":[0.0021376899,0.00015132269,0.3250141,0.000056087054,0.00040349536,0.000030608808,0.0024858331,0.50560236,0.0051423972,0.0007711406,0.1571544,0.0010505755],"about_ca_topic_score_codex":0.10170395,"about_ca_topic_score_gemma":0.21123607,"teacher_disagreement_score":0.5979273,"about_ca_system_score_codex":0.00025249145,"about_ca_system_score_gemma":0.00002170224,"threshold_uncertainty_score":0.948541},"labels":[],"label_agreement":null},{"id":"W3045706240","doi":"10.1364/ao.393059","title":"Physical model of snow precipitation interaction with a 3D lidar scanner","year":2020,"lang":"en","type":"article","venue":"Applied Optics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Defence Research and Development Canada","funders":"","keywords":"Snowflake; Lidar; Snow; Visibility; Remote sensing; Optics; Probability density function; Randomness; Environmental science; Meteorology; Physics; Geology; Mathematics; Statistics","score_opus":0.01226122815911101,"score_gpt":0.2146343169278156,"score_spread":0.20237308876870458,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3045706240","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":[0.8871109,6.580582e-7,0.0905097,0.00014369414,0.000010013311,0.00011251629,0.0000016847373,0.00001968061,0.022091165],"genre_scores_gemma":[0.9613069,0.0000016338809,0.03836355,0.00019149037,0.00003565127,0.0000122343845,0.0000033031813,0.000011041799,0.00007418354],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99949497,0.0000037752143,0.00008688632,0.00014995216,0.00017126527,0.0000931413],"domain_scores_gemma":[0.9997727,0.00001552155,0.00006362051,0.00008667728,0.0000054356324,0.000056003464],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00001893503,0.00007469216,0.00009224134,3.9736602e-7,0.000028505827,0.000007925317,0.0000758848,0.000025313895,0.00007513106],"category_scores_gemma":[0.000004743221,0.00005968206,0.000018022276,0.00010296681,0.00007406912,0.000068303874,0.000050986655,0.00007270101,0.00008088818],"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":[0.00017133307,0.00015920581,0.0011720111,0.000014018208,0.000018783741,6.611184e-7,0.005887669,0.9039985,0.067785405,0.0029329665,0.00036609508,0.017493358],"study_design_scores_gemma":[0.000290427,0.00017843867,0.0008288952,0.000005895777,0.000030203691,5.445114e-7,0.00054347917,0.9811315,0.016324662,0.00040307513,0.00012866412,0.0001342141],"about_ca_topic_score_codex":0.0000102065105,"about_ca_topic_score_gemma":0.000004198677,"teacher_disagreement_score":0.07713301,"about_ca_system_score_codex":0.000026563652,"about_ca_system_score_gemma":0.000006463103,"threshold_uncertainty_score":0.24337637},"labels":[],"label_agreement":null},{"id":"W3046128621","doi":"10.1364/oe.400130","title":"Efficient radiative transfer model for thermal infrared brightness temperature simulation in cloudy atmospheres","year":2020,"lang":"en","type":"article","venue":"Optics Express","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"Environment and Climate Change Canada","funders":"National Key Research and Development Program of China; National Natural Science Foundation of China","keywords":"Radiative transfer; Atmospheric radiative transfer codes; Brightness temperature; Brightness; MODTRAN; Infrared; Infrared window; Radiance; Computational physics; Atmospheric model; Physics; Ice cloud; Optics; Materials science; Remote sensing; Meteorology","score_opus":0.01472452167512322,"score_gpt":0.2317818996028087,"score_spread":0.21705737792768548,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3046128621","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":[0.87387174,0.00003096301,0.12405987,0.00014054125,0.000047062404,0.00050773204,0.000025444982,0.000032702883,0.0012839433],"genre_scores_gemma":[0.9892004,0.0000029805876,0.009838607,0.00037912454,0.000060865605,0.00005939386,0.000009590629,0.000028370085,0.0004206674],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9988891,0.000031434123,0.00022428924,0.00034980918,0.00022636603,0.00027903894],"domain_scores_gemma":[0.99960464,0.00007235374,0.000033106873,0.00015673513,0.000013321162,0.00011982782],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007138346,0.00017824842,0.00018968519,5.8665995e-7,0.00010139629,0.00003898277,0.00021688643,0.00012347697,0.00025923428],"category_scores_gemma":[0.000024188397,0.00015466096,0.00006997183,0.00016238811,0.00008375516,0.000081200225,0.000061710656,0.00014007257,0.000018261146],"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":[0.00012995134,0.000076831115,0.0010222481,0.000011337771,0.000006418916,0.0000023689379,0.0062251044,0.96845627,0.023517735,0.00015897524,0.00010400158,0.00028875904],"study_design_scores_gemma":[0.00092395785,0.00006243929,0.0018013946,0.000009437598,0.000011469359,1.2944544e-7,0.00022944451,0.9934542,0.0030219506,0.000098422606,0.00017325804,0.00021390228],"about_ca_topic_score_codex":0.00001698165,"about_ca_topic_score_gemma":0.000008029336,"teacher_disagreement_score":0.11532866,"about_ca_system_score_codex":0.00006743493,"about_ca_system_score_gemma":0.000015696683,"threshold_uncertainty_score":0.6306891},"labels":[],"label_agreement":null},{"id":"W3047025634","doi":"10.1029/2020jd032660","title":"Laboratory Investigation of Particle‐Scale Factors Affecting the Settling Velocity of Volcaniclastic Dust","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Trent University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Foundation for Innovation","keywords":"Settling; Materials science; Mineralogy; Particle (ecology); Relative humidity; Atmospheric sciences; Chemistry; Geology; Meteorology; Physics; Thermodynamics","score_opus":0.03636331638150111,"score_gpt":0.28600457121223744,"score_spread":0.24964125483073632,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3047025634","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":[0.998468,0.00007990264,0.00043734768,0.00073872786,0.000042835214,0.000114472656,0.000003863115,0.0000057826273,0.00010906464],"genre_scores_gemma":[0.998747,0.000015571253,0.0009883854,0.00005883379,0.00014714761,0.0000011364617,2.636047e-7,0.000013370384,0.00002827424],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99750197,0.0003702471,0.00046797388,0.00015520392,0.00119265,0.00031195936],"domain_scores_gemma":[0.9980601,0.0009471414,0.00038520593,0.00015656282,0.00017337357,0.00027762871],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008804401,0.0001122274,0.00028944362,7.4344376e-7,0.00015956795,0.000025013598,0.00043756395,0.00005629806,0.0003585354],"category_scores_gemma":[0.0012321182,0.00007045624,0.00012810463,0.00083407504,0.00079544395,0.00022167673,0.00023296742,0.0005972312,0.000021835516],"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":[0.00020626883,0.00015299924,0.6349192,0.000080893464,0.00007067353,0.000010154347,0.007809856,0.004716845,0.346579,0.00011065808,0.00225016,0.0030933006],"study_design_scores_gemma":[0.00036477495,0.0010508258,0.8601703,0.00007490443,0.0000308894,0.0000011910715,0.0065996214,0.015665567,0.11533427,0.00044482874,0.00015293394,0.00010989144],"about_ca_topic_score_codex":0.00048326177,"about_ca_topic_score_gemma":0.000045257613,"teacher_disagreement_score":0.23124471,"about_ca_system_score_codex":0.00008821055,"about_ca_system_score_gemma":0.0001171777,"threshold_uncertainty_score":0.39257115},"labels":[],"label_agreement":null},{"id":"W3074297675","doi":"10.1175/jtech-d-20-0061.1","title":"Separating Cloud and Drizzle Signals in Radar Doppler Spectra Using a Parametric Time Domain Method","year":2020,"lang":"en","type":"article","venue":"Journal of Atmospheric and Oceanic Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"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; National Research Council Canada","funders":"Biological and Environmental Research","keywords":"Drizzle; Environmental science; Radar; Meteorology; Remote sensing; Precipitation; Physics; Geology; Computer science","score_opus":0.0088051347529116,"score_gpt":0.24071268120952052,"score_spread":0.23190754645660894,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3074297675","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":[0.9543839,0.0012296118,0.04265646,0.0012675616,0.00004491199,0.00012663234,6.430634e-7,0.000028993163,0.00026125743],"genre_scores_gemma":[0.663501,0.00013831517,0.33594614,0.00031234368,0.000059261623,6.510677e-7,9.0986674e-8,0.000016507967,0.000025640147],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99847835,0.00008427974,0.0005659426,0.00030291174,0.00022714457,0.00034139212],"domain_scores_gemma":[0.9991841,0.00010021913,0.00042061278,0.00011702259,0.0000122338715,0.00016584393],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045127823,0.00020595232,0.0005189521,0.0000034983304,0.00009571568,0.000029582643,0.00023634477,0.00020400224,0.0005921505],"category_scores_gemma":[0.000103635946,0.00017169451,0.00006397805,0.001245477,0.00023760626,0.00016831748,0.00022803096,0.00045932387,0.000012392254],"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":[0.000600077,0.00048515014,0.5820851,0.00009939939,0.00032441996,0.0015143896,0.0042967396,0.012597432,0.2857623,0.0015938488,0.0061586844,0.10448251],"study_design_scores_gemma":[0.017439364,0.01102312,0.13915531,0.0004828854,0.00077118387,0.015550958,0.021479785,0.67419624,0.011322182,0.06387992,0.040392563,0.004306484],"about_ca_topic_score_codex":0.000038464375,"about_ca_topic_score_gemma":0.0000029049197,"teacher_disagreement_score":0.6615988,"about_ca_system_score_codex":0.00010571263,"about_ca_system_score_gemma":0.00003273189,"threshold_uncertainty_score":0.7001499},"labels":[],"label_agreement":null},{"id":"W3080094537","doi":"10.1117/1.jrs.14.034513","title":"Efficient dust detection based on spectral and thermal observations of MODIS imagery","year":2020,"lang":"en","type":"article","venue":"Journal of Applied Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institut National de la Recherche Scientifique","funders":"","keywords":"Dust storm; Remote sensing; Environmental science; Spectroradiometer; Storm; Aerosol; Brightness temperature; Satellite; Moderate-resolution imaging spectroradiometer; Meteorology; Satellite imagery; Spectral bands; Brightness; Reflectivity; Geology; Geography","score_opus":0.013962880657848424,"score_gpt":0.1966573145027693,"score_spread":0.18269443384492087,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3080094537","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":[0.9501196,0.0000048378774,0.046589106,0.00049055414,0.000047599864,0.000058737343,5.079122e-7,0.0000064027026,0.002682609],"genre_scores_gemma":[0.9673747,0.0000018941937,0.032103688,0.00041875217,0.00008789163,7.679128e-9,1.3744234e-7,0.000009077261,0.0000038711164],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99928236,0.000015021378,0.00024169341,0.00010374484,0.00024833513,0.00010882634],"domain_scores_gemma":[0.9995621,0.000036192243,0.00023701185,0.00006610616,0.000011122673,0.00008750447],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013230386,0.0000812062,0.00014383892,0.0000027206947,0.00007585507,0.000013191682,0.00004657258,0.000037291375,0.000033455864],"category_scores_gemma":[0.000018153756,0.00006551593,0.00005639132,0.00015470874,0.000085244006,0.000022512082,0.000024906492,0.00016836653,0.0000039140873],"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":[0.00013412077,0.000015558348,0.00011767359,0.0000051385805,0.0000059143863,0.00000937219,0.00030437324,0.31425703,0.6334892,0.0000031903471,0.000020981108,0.05163744],"study_design_scores_gemma":[0.00037633267,0.00013773174,0.035374675,0.000018331337,0.000024676712,0.000012222828,0.00023198621,0.9141332,0.049520373,0.00003963877,0.000049334623,0.00008148336],"about_ca_topic_score_codex":0.000022133047,"about_ca_topic_score_gemma":0.0000025071254,"teacher_disagreement_score":0.59987617,"about_ca_system_score_codex":0.00005274376,"about_ca_system_score_gemma":0.000010915057,"threshold_uncertainty_score":0.2671662},"labels":[],"label_agreement":null},{"id":"W3081006245","doi":"10.1002/qj.415","title":"Intercomparison of model simulations of mixed‐phase clouds observed during the ARM Mixed‐Phase Arctic Cloud Experiment. II: Multilayer cloud","year":2009,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":106,"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":"Liquid water path; Liquid water content; Environmental science; Arctic; Cloud physics; Cloud fraction; Atmospheric sciences; Cloud height; Cloud top; Cloud computing; Meteorology; Ice cloud; Mixed phase; Phase (matter); Geology; Cloud cover; Aerosol; Physics","score_opus":0.030083198326095854,"score_gpt":0.2821380956994108,"score_spread":0.25205489737331493,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3081006245","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":[0.9906544,0.00025909054,0.0074911406,0.00070158474,0.00047412104,0.00029748483,0.000017089686,0.000016330918,0.00008874675],"genre_scores_gemma":[0.9943272,0.000011547478,0.0050596097,0.00022711308,0.0001894671,0.000004620647,0.000001123037,0.000016644139,0.00016266124],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99677515,0.0003798087,0.0012825371,0.00030788663,0.0007777072,0.0004769236],"domain_scores_gemma":[0.9977316,0.0002349665,0.0012139493,0.00054001156,0.00008083639,0.00019862976],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00084504124,0.00034063737,0.00068765815,0.0000032716898,0.00048037662,0.000031708176,0.001150222,0.0002243356,0.00063251785],"category_scores_gemma":[0.000084800326,0.00018366422,0.001132325,0.0002781385,0.0006004548,0.00015135577,0.00020620092,0.0006899504,0.0000043440527],"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":[0.0019042843,0.01054008,0.011260505,0.000049264618,0.00052147976,0.00001193001,0.016049715,0.70961773,0.23222718,0.00036111916,0.0032476664,0.014209043],"study_design_scores_gemma":[0.012161544,0.017337888,0.06246586,0.00016146984,0.00063570595,0.00004496448,0.006227155,0.853758,0.038565736,0.007342941,0.0004789772,0.000819754],"about_ca_topic_score_codex":0.000060658072,"about_ca_topic_score_gemma":0.000008611703,"teacher_disagreement_score":0.19366145,"about_ca_system_score_codex":0.00021286788,"about_ca_system_score_gemma":0.000026206953,"threshold_uncertainty_score":0.7489609},"labels":[],"label_agreement":null},{"id":"W3082610663","doi":"10.5194/amt-13-6901-2020","title":"Determining cloud thermodynamic phase from the polarized Micro Pulse Lidar","year":2020,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"Goddard Space Flight Center; Langley Research Center; National Aeronautics and Space Administration","keywords":"Lidar; Pathfinder; Remote sensing; Aerosol; Satellite; Environmental science; Orthogonal polarization spectral imaging; Polarization (electrochemistry); Cloud computing; Supercooling; Phase (matter); Meteorology; Atmospheric sciences; Physics; Optics; Geology; Chemistry; Laser; Computer science; Astronomy","score_opus":0.026167179718203926,"score_gpt":0.23913439353086036,"score_spread":0.21296721381265643,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3082610663","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":[0.85912377,0.0004784949,0.12930448,0.0027387228,0.00018671133,0.0010319514,0.000014876767,0.00084453076,0.00627644],"genre_scores_gemma":[0.9354829,0.000068155394,0.058371793,0.0055487463,0.0002787791,0.00011040398,0.0000080288255,0.00006584096,0.000065339256],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.99717826,0.00019442943,0.0004866152,0.0006730504,0.00095262687,0.000515034],"domain_scores_gemma":[0.998811,0.00006224439,0.00024374366,0.000618883,0.000031176547,0.00023296055],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005607004,0.0004046236,0.00035739748,2.1000925e-7,0.0003532083,0.00010832426,0.00095096644,0.00014392337,0.0038829003],"category_scores_gemma":[0.00012773668,0.00028702515,0.00018305829,0.00039030684,0.00024556404,0.00019657542,0.0003783979,0.0003522401,0.0002781896],"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":[0.00011703488,0.00019537138,0.02998841,0.0000065452105,0.00007669906,0.000026061147,0.0013211552,0.000009282253,0.8333248,0.000020541065,0.0064647505,0.12844935],"study_design_scores_gemma":[0.009895928,0.0044318084,0.10995925,0.0004706503,0.0010394297,0.000047910085,0.003239528,0.05537416,0.37947518,0.0037361372,0.42650148,0.005828549],"about_ca_topic_score_codex":0.0011137881,"about_ca_topic_score_gemma":0.000065273285,"teacher_disagreement_score":0.45384964,"about_ca_system_score_codex":0.00029002404,"about_ca_system_score_gemma":0.00004211375,"threshold_uncertainty_score":0.9999582},"labels":[],"label_agreement":null},{"id":"W3082755731","doi":"10.3390/atmos11090916","title":"CNT Parameterization Based on the Observed INP Concentration during Arctic Summer Campaigns in a Marine Environment","year":2020,"lang":"en","type":"article","venue":"Atmosphere","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"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 British Columbia; Environment and Climate Change Canada; Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Ice nucleus; Arctic; Atmospheric sciences; Aerosol; Representativeness heuristic; Environmental science; The arctic; Nucleation; Particle (ecology); Climatology; Meteorology; Physics; Geology; Oceanography; Mathematics; Statistics; Thermodynamics","score_opus":0.02436362434066332,"score_gpt":0.19589949532959927,"score_spread":0.17153587098893594,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3082755731","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":[0.99521023,0.000008675223,0.0008730506,0.0021234218,0.000039296516,0.00040810506,0.0000016589745,0.000030878145,0.0013046956],"genre_scores_gemma":[0.99557614,0.000015266702,0.0014990899,0.0026511678,0.000031978463,0.0000623564,0.0000127662715,0.000020872116,0.00013035708],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987488,0.000104101884,0.00023328618,0.00034798094,0.00029935056,0.00026649403],"domain_scores_gemma":[0.99948394,0.000069390626,0.00009017941,0.00025143375,0.0000025170946,0.00010251681],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00009613262,0.000171691,0.00013666575,1.0769488e-7,0.000115076546,0.000033904147,0.00018842959,0.00006168429,0.012084255],"category_scores_gemma":[0.00005191859,0.00012812678,0.000051510822,0.00020594167,0.000096672964,0.00009919887,0.00011680044,0.00016095614,0.00043373226],"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":[0.00007963221,0.00009528153,0.8040326,0.000013113811,0.000006108111,0.00001666295,0.00055014156,0.18745741,0.006708079,0.000049566253,0.000106202235,0.0008851569],"study_design_scores_gemma":[0.00086537196,0.00020779663,0.7972678,0.000027941189,0.000014995359,9.945818e-7,0.00050741597,0.19706696,0.0027258603,0.00007791913,0.0009577108,0.00027924532],"about_ca_topic_score_codex":0.00023064067,"about_ca_topic_score_gemma":0.000063863445,"teacher_disagreement_score":0.011650522,"about_ca_system_score_codex":0.00022558676,"about_ca_system_score_gemma":0.000010186584,"threshold_uncertainty_score":0.9888188},"labels":[],"label_agreement":null},{"id":"W3082766643","doi":"10.5194/acp-2020-840","title":"Stratospheric pollution from Canadian forest fires","year":2020,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"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":"Natural Environment Research Council; Sight Research UK","keywords":"Microwave Limb Sounder; Stratosphere; Environmental science; Northern Hemisphere; Pollution; Atmospheric sciences; Southern Hemisphere; Smoke; Water vapor; Climatology; Meteorology; Geography; Geology; Ecology","score_opus":0.008412114644270524,"score_gpt":0.17947182087078747,"score_spread":0.17105970622651695,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3082766643","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":[0.9140288,0.000024934869,0.0015866079,0.0042017587,0.0000427548,0.00006519247,0.000008661125,0.000043656193,0.07999762],"genre_scores_gemma":[0.9913158,0.000004448757,0.0025024558,0.0055033327,0.000059469847,0.000002730154,0.000005967206,0.0000071611494,0.0005986368],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99943674,0.0000079170795,0.000077541394,0.00017752043,0.00010992466,0.00019035873],"domain_scores_gemma":[0.9995538,0.000004514716,0.000016375847,0.00008732751,0.0000011902432,0.00033681482],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000013858502,0.00007195751,0.000059828242,1.2433746e-7,0.0000841208,0.000021039541,0.00013001847,0.000039462062,0.033558257],"category_scores_gemma":[0.0000081711205,0.00006125164,0.000025415606,0.0001314929,0.000050175542,0.000085495005,0.000038888695,0.000049056784,0.001990096],"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":[0.000007411561,0.00001351333,0.90490174,0.0000010294207,0.000009059991,0.00001761041,0.00048645496,0.004797854,0.0019990716,0.00047084808,0.07317447,0.014120955],"study_design_scores_gemma":[0.0001237632,0.000049497154,0.9196954,0.000001157312,0.0000055894243,4.4419718e-7,0.00030441835,0.011614465,0.00018785993,0.0003972345,0.06746599,0.00015420537],"about_ca_topic_score_codex":0.6137713,"about_ca_topic_score_gemma":0.5551091,"teacher_disagreement_score":0.07939898,"about_ca_system_score_codex":0.000080227954,"about_ca_system_score_gemma":0.000022620241,"threshold_uncertainty_score":0.998787},"labels":[],"label_agreement":null},{"id":"W3082840893","doi":"10.5194/acp-20-10111-2020","title":"Impact of aerosols and turbulence on cloud droplet growth: an in-cloud seeding case study using a parcel–DNS (direct numerical simulation) approach","year":2020,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Compute Canada; National Center for Atmospheric Research; National Science Foundation","keywords":"Drizzle; Seeding; Turbulence; Cloud condensation nuclei; Condensation; Liquid water content; Environmental science; Atmospheric sciences; Turbulence kinetic energy; Meteorology; Mechanics; Aerosol; Cloud computing; Physics; Thermodynamics; Computer science","score_opus":0.023530115175143845,"score_gpt":0.27160300587161434,"score_spread":0.2480728906964705,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3082840893","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":[0.99581426,0.000026645792,0.0031266455,0.000008295778,0.00001583762,0.00023842452,0.0000069041525,0.00002726776,0.0007357054],"genre_scores_gemma":[0.9958223,0.000008393252,0.0038862904,0.00005035901,0.00017594507,0.000008101938,0.0000039320767,0.00002570054,0.000018964944],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9985611,0.00005295864,0.0002833558,0.00057524187,0.00024368514,0.00028365976],"domain_scores_gemma":[0.9993053,0.000084971434,0.00013419853,0.00020958838,0.000012946935,0.0002529587],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00010061311,0.00028683676,0.00037466775,4.344326e-8,0.00014547085,0.000040700677,0.00013402774,0.000081394224,0.00021925161],"category_scores_gemma":[0.000025784284,0.00025805313,0.000068483016,0.00043685408,0.00018274468,0.00019164343,0.00013559441,0.00022577812,0.0000023177042],"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":[0.00013801473,0.00090088736,0.6431855,0.00007706594,0.0000485644,0.00016057846,0.00679986,0.3327096,0.009239204,0.0000028285053,0.000012313602,0.0067255828],"study_design_scores_gemma":[0.00082355447,0.00053842756,0.0247578,0.000019382755,0.00005440211,0.000081957376,0.002305113,0.9704837,0.00047608148,0.000038606042,0.000006483001,0.00041447263],"about_ca_topic_score_codex":0.0014266473,"about_ca_topic_score_gemma":0.0000018013668,"teacher_disagreement_score":0.6377741,"about_ca_system_score_codex":0.00008814568,"about_ca_system_score_gemma":0.000020249434,"threshold_uncertainty_score":0.9999872},"labels":[],"label_agreement":null},{"id":"W3084715812","doi":"10.5194/amt-2020-289","title":"Validation of temperature data from the RAman Lidar for Meteorological Observations (RALMO) at Payerne. An application to liquid cloud supersaturation","year":2020,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung","keywords":"Radiosonde; Troposphere; Standard deviation; Environmental science; Lidar; Atmospheric sciences; Supersaturation; Daytime; Raman spectroscopy; Meteorology; Mean radiant temperature; Remote sensing; Chemistry; Physics; Optics; Geology; Climate change; Mathematics; Statistics","score_opus":0.06024887370822714,"score_gpt":0.27058155234741177,"score_spread":0.21033267863918464,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3084715812","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":[0.9511835,0.000012558635,0.034429576,0.013288217,0.00004623179,0.00070975214,0.00016576367,0.00004569808,0.00011871791],"genre_scores_gemma":[0.9782124,0.0000057502357,0.015874062,0.0039066467,0.00020165807,0.00006810248,0.001621358,0.000011030228,0.00009899584],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9989147,0.00006148279,0.00023027427,0.00044634411,0.00021694107,0.00013023267],"domain_scores_gemma":[0.99912214,0.00010605336,0.00007670674,0.00057278137,0.000019403238,0.00010289668],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00018514178,0.00011140881,0.00012147125,4.777306e-7,0.00019571361,0.000033924265,0.0006196842,0.000095315685,0.0009494289],"category_scores_gemma":[0.00011672337,0.00007115164,0.000035329205,0.00020781993,0.00005965748,0.00031354363,0.0003546705,0.000071154995,0.000081872364],"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":[0.00030175297,0.00009376379,0.021946032,0.0000035517667,0.000015773701,1.2993601e-7,0.0013554143,0.0031720202,0.9532474,0.0006696039,0.018409094,0.0007854169],"study_design_scores_gemma":[0.0014442087,0.0032874714,0.4119356,0.000012708663,0.00025449417,0.0000018200608,0.003627593,0.13326985,0.31533766,0.0010821042,0.12877218,0.0009743143],"about_ca_topic_score_codex":0.00046996752,"about_ca_topic_score_gemma":0.000292081,"teacher_disagreement_score":0.63790977,"about_ca_system_score_codex":0.0000455002,"about_ca_system_score_gemma":0.000008493928,"threshold_uncertainty_score":0.9999638},"labels":[],"label_agreement":null},{"id":"W3085866211","doi":"10.1504/ijspacese.2020.10032063","title":"Radiance enhancement and shortwave upwelling radiative flux methods for efficient detection of cloud scenes","year":2020,"lang":"en","type":"article","venue":"International Journal of Space Science and Engineering","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; York University","funders":"University of Toronto; York University","keywords":"Radiance; Shortwave; Upwelling; Remote sensing; Cloud computing; Radiative transfer; Flux (metallurgy); Shortwave radiation; Environmental science; Radiative flux; Geology; Meteorology; Computer science; Physics; Optics; Oceanography; Materials science; Radiation","score_opus":0.010367962626581203,"score_gpt":0.26841694500456087,"score_spread":0.2580489823779797,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3085866211","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":[0.5216584,0.00023025922,0.47740498,0.00035645367,0.0002672468,0.00004453111,5.799179e-7,0.00000235045,0.000035160036],"genre_scores_gemma":[0.9289096,0.00012074976,0.07079587,0.000055251043,0.00010449469,0.0000015591852,7.262263e-8,0.000003938868,0.00000845898],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9992635,0.000006137999,0.00018427265,0.0001261387,0.00030675187,0.00011318141],"domain_scores_gemma":[0.99959403,0.000057110523,0.00013100987,0.000029647603,0.0000771661,0.000111006855],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005507945,0.00006758157,0.00010887362,0.000009216887,0.000050474686,0.00003229073,0.00016306649,0.000017196266,0.000017819953],"category_scores_gemma":[0.00016340092,0.00005836607,0.000028786473,0.00016485297,0.00014732988,0.00017551323,0.00006444218,0.00006354326,5.5967064e-7],"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":[0.000035629855,0.000011903201,0.0007792338,0.000010232416,0.00001830028,0.0000013624835,0.001547615,0.13419075,0.8126022,0.000114404254,0.0000140642105,0.05067425],"study_design_scores_gemma":[0.00029439403,0.0001926943,0.0048781103,0.00004302687,0.000012428683,0.000019019171,0.00040644867,0.6439462,0.34814867,0.000038566166,0.0019226139,0.000097863944],"about_ca_topic_score_codex":0.000009596956,"about_ca_topic_score_gemma":5.293357e-7,"teacher_disagreement_score":0.5097554,"about_ca_system_score_codex":0.00008583544,"about_ca_system_score_gemma":0.0000193627,"threshold_uncertainty_score":0.23800993},"labels":[],"label_agreement":null},{"id":"W3086455191","doi":"10.5194/egusphere-egu2020-5140","title":"Stratospheric Australian fire smoke layers over Punta Arenas, Chile, measured by ground-based lidar and AEOLUS","year":2020,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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; Smoke; Atmospheric sciences; Aerosol; Southern Hemisphere; Northern Hemisphere; Lidar; Wavelength; Environmental science; Chemistry; Climatology; Meteorology; Physics; Geology; Optics","score_opus":0.01582719729349332,"score_gpt":0.21476471605346795,"score_spread":0.19893751875997462,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3086455191","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":[0.98909104,0.00011062498,0.0005329205,0.0025141288,0.000058852864,0.0002219038,0.000019999938,0.000118291384,0.0073322663],"genre_scores_gemma":[0.9930159,0.000018713656,0.0013427207,0.0035629221,0.00004374047,0.00001185737,0.000014726605,0.000028336093,0.0019610699],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99839747,0.000037265825,0.00022334862,0.00052239315,0.00042331935,0.0003961872],"domain_scores_gemma":[0.99926746,0.000017487162,0.00007431632,0.00022480072,0.0000046830046,0.0004112258],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00007649857,0.00026170682,0.00021844995,3.8523171e-7,0.00016529221,0.0000891119,0.00025224415,0.00011992996,0.012963707],"category_scores_gemma":[0.000013872707,0.00022333991,0.00007036023,0.00027589453,0.00023711273,0.00019791716,0.00010980309,0.00017789686,0.00016436129],"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":[0.00011877142,0.0002269984,0.7789624,0.00004360814,0.0000681398,0.000044342614,0.0006566063,0.0014398507,0.02074506,0.00008025359,0.18316355,0.0144504085],"study_design_scores_gemma":[0.0022755428,0.0006460373,0.89429724,0.000022044334,0.00007448359,0.000008043959,0.0009917986,0.013203071,0.004744733,0.00008321495,0.082442045,0.0012117131],"about_ca_topic_score_codex":0.0032100494,"about_ca_topic_score_gemma":0.00019773486,"teacher_disagreement_score":0.11533487,"about_ca_system_score_codex":0.00007787674,"about_ca_system_score_gemma":0.000019100771,"threshold_uncertainty_score":0.9879386},"labels":[],"label_agreement":null},{"id":"W3088313224","doi":"10.1175/jtech-d-19-0170.1","title":"A 1D Var Retrieval of Relative Humidity Using the ERA5 Dataset for the Assimilation of Raman Lidar Measurements","year":2020,"lang":"en","type":"article","venue":"Journal of Atmospheric and Oceanic Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Canadian Space Agency","keywords":"Relative humidity; Lidar; Environmental science; Humidity; Water vapor; Boundary layer; Data assimilation; Atmospheric sciences; Meteorology; Remote sensing; Geology; Physics","score_opus":0.04177828437456183,"score_gpt":0.2682826478869416,"score_spread":0.2265043635123798,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3088313224","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":[0.9160128,0.0007200473,0.080089435,0.0027271085,0.00009193931,0.00026863386,0.00003570916,0.000007361452,0.000046939185],"genre_scores_gemma":[0.9820772,0.000116255,0.017575055,0.00017255968,0.000040101375,6.507628e-7,0.0000015318732,0.000009550769,0.0000071377162],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988903,0.000047763882,0.00047875123,0.00013527997,0.00029993666,0.0001480131],"domain_scores_gemma":[0.99875814,0.00012624788,0.00083374896,0.00018721951,0.000050634826,0.000044010096],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00051637186,0.00011268791,0.00027246293,6.7971666e-7,0.00015501326,0.000007615232,0.00038133425,0.000117171745,0.00011252007],"category_scores_gemma":[0.00028141768,0.00006306058,0.000079123034,0.00041331872,0.00047978363,0.00014161521,0.00016702582,0.00025035013,6.915328e-7],"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":[0.0033990908,0.0007642306,0.6475723,0.0002441067,0.00190969,0.000025268318,0.007183515,0.019674607,0.23222746,0.0024480387,0.025783999,0.05876772],"study_design_scores_gemma":[0.012852938,0.013853875,0.513153,0.00040795782,0.003901952,0.00058762304,0.021214157,0.22994052,0.09265923,0.02170902,0.08811331,0.0016063887],"about_ca_topic_score_codex":0.000015001381,"about_ca_topic_score_gemma":0.0000023594853,"teacher_disagreement_score":0.2102659,"about_ca_system_score_codex":0.000054000582,"about_ca_system_score_gemma":0.00003778347,"threshold_uncertainty_score":0.25715357},"labels":[],"label_agreement":null},{"id":"W3088420038","doi":"10.5194/cp-17-969-2021","title":"On the phenomenon of the blue sun","year":2021,"lang":"en","type":"article","venue":"Climate of the past","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":26,"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":"Deutsche Forschungsgemeinschaft","keywords":"Rayleigh scattering; Scattering; Aerosol; Radiative transfer; Optics; Single-scattering albedo; Spectral line; Wavelength; Computational physics; Physics; Materials science; Astronomy; Meteorology","score_opus":0.009232135178490773,"score_gpt":0.20246686004532818,"score_spread":0.1932347248668374,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3088420038","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":[0.94839865,0.000023457995,0.000009409322,0.0024117336,0.0001598636,0.00008294466,0.0000098641485,0.0000036661438,0.04890041],"genre_scores_gemma":[0.99783903,0.00002234371,0.000044018423,0.0004583069,0.0000185306,0.0000036184324,3.2104904e-7,0.0000070896217,0.001606758],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99935466,0.00006445484,0.00012618929,0.00010894604,0.0002047852,0.00014094787],"domain_scores_gemma":[0.99927735,0.00006162082,0.000111584945,0.00052737806,0.000005383566,0.000016669044],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014047328,0.00006685419,0.00008462877,1.8554415e-7,0.00014803579,0.000006899673,0.0004442945,0.000022448803,0.0022051593],"category_scores_gemma":[0.000026607942,0.000027995417,0.00009267492,0.00016350966,0.00028603795,0.000016538308,0.00050208997,0.000079244164,0.00008078068],"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":[0.00008972537,0.0009402922,0.6478154,0.000107126616,0.00010565511,0.000004791493,0.0067510693,0.019723708,0.25331646,0.036290437,0.029050995,0.0058043227],"study_design_scores_gemma":[0.000430612,0.000110621804,0.8937332,0.00012570152,0.000072160554,0.000007989694,0.0034916997,0.00081785425,0.084145874,0.004515789,0.012308381,0.00024013918],"about_ca_topic_score_codex":0.000032993506,"about_ca_topic_score_gemma":0.00002955858,"teacher_disagreement_score":0.24591777,"about_ca_system_score_codex":0.000028521828,"about_ca_system_score_gemma":0.0000062202553,"threshold_uncertainty_score":0.99870694},"labels":[],"label_agreement":null},{"id":"W3088808432","doi":"","title":"Initiation of deep convection over an idealized mesoscale convergence line","year":2017,"lang":"en","type":"article","venue":"eScholarship@McGill (McGill)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"","keywords":"Mesoscale meteorology; Convection; Geology; Lapse rate; Atmospheric convection; Meteorology; Boundary layer; Troposphere; Thermal; Mechanics; Atmospheric sciences; Climatology; Geophysics; Physics","score_opus":0.017430102789526416,"score_gpt":0.25329653644156425,"score_spread":0.23586643365203783,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3088808432","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":[0.9633353,0.000015799786,0.000046608682,0.000028137942,0.00050422107,0.00027042133,0.000103982355,0.0000825515,0.03561302],"genre_scores_gemma":[0.9975421,0.000058360074,0.001570457,0.00032521068,0.00002695188,0.000028792116,0.000023529465,0.00003463674,0.00038996869],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9978491,0.00016843948,0.00050808716,0.0005176644,0.00056269753,0.00039398848],"domain_scores_gemma":[0.99811524,0.000050842074,0.00059784733,0.0009128789,0.000059288475,0.00026389156],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006002123,0.0002727156,0.0003260728,0.000006092084,0.0012074831,0.00006527743,0.0006641664,0.00022096382,0.0055442327],"category_scores_gemma":[0.00036111154,0.0002717597,0.00013079129,0.00015380941,0.0003337017,0.0022619807,0.00035853096,0.0003015122,0.0004357411],"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":[0.00054398895,0.0008278505,0.11066902,0.00009010818,0.00012775918,0.000045101435,0.000054989676,0.0013818904,0.55830145,0.05239436,0.000029058518,0.27553442],"study_design_scores_gemma":[0.0041360236,0.00093224057,0.6110753,0.000074646494,0.00017838775,0.000034390378,0.00019792271,0.0066847466,0.30575216,0.032701213,0.036765404,0.0014675889],"about_ca_topic_score_codex":0.002369261,"about_ca_topic_score_gemma":0.0010099259,"teacher_disagreement_score":0.50040627,"about_ca_system_score_codex":0.0002717327,"about_ca_system_score_gemma":0.0000073602528,"threshold_uncertainty_score":0.9999735},"labels":[],"label_agreement":null},{"id":"W3089567104","doi":"10.5194/egusphere-egu2020-1692","title":"A scheme for forecasting severe space weather","year":2020,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Space weather; Physics; Shock (circulatory); Meteorology; Environmental science; Internal medicine; Medicine","score_opus":0.031293857334798524,"score_gpt":0.21543492729899086,"score_spread":0.18414106996419233,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3089567104","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":[0.6799744,0.000017268054,0.09370846,0.00610555,0.000043594184,0.00032199887,0.0000027340388,0.00010842128,0.21971759],"genre_scores_gemma":[0.8763114,9.1596667e-7,0.11259469,0.002145757,0.00006754954,0.0000149666985,7.7043796e-7,0.00001279208,0.008851161],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9995187,0.0000034385794,0.000065256405,0.00016893107,0.0000848429,0.00015886768],"domain_scores_gemma":[0.999807,0.000017074686,0.000022079314,0.000064383545,0.0000020030482,0.00008744167],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000034805624,0.00006607638,0.00006394851,8.850426e-8,0.00006258462,0.000012005151,0.000092737224,0.000026861215,0.0074274773],"category_scores_gemma":[0.00002688007,0.000051951676,0.00004043845,0.00007450745,0.00002884802,0.000061523075,0.000086238106,0.000033885244,0.0003699905],"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":[0.00017894553,0.00013418218,0.43396527,0.0000658748,0.000057009514,0.000016254668,0.004714064,0.004239602,0.05312792,0.0053849616,0.42043254,0.07768337],"study_design_scores_gemma":[0.0014151258,0.00043389513,0.008789769,0.000011460656,0.000021478492,0.000013490167,0.0017033977,0.38446015,0.0034244251,0.0011322638,0.5979141,0.0006804054],"about_ca_topic_score_codex":0.00004098922,"about_ca_topic_score_gemma":0.000012359648,"teacher_disagreement_score":0.42517552,"about_ca_system_score_codex":0.000019789803,"about_ca_system_score_gemma":0.000003008154,"threshold_uncertainty_score":0.99347985},"labels":[],"label_agreement":null},{"id":"W3089826081","doi":"10.1002/qj.3922","title":"Partial validation of a lossy compression approach to computing radiative transfer in cloud system‐resolving models","year":2020,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"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 Waterloo; Environment and Climate Change Canada","funders":"Environment and Climate Change Canada; European Space Agency","keywords":"Radiative transfer; Lossy compression; Radiative flux; Grid; Cloud computing; Computer science; Convection; Atmospheric radiative transfer codes; Algorithm; Physics; Computational physics; Mathematics; Meteorology; Optics; Artificial intelligence; Geometry","score_opus":0.02028516566541558,"score_gpt":0.21676185094202607,"score_spread":0.1964766852766105,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3089826081","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":[0.73064095,0.000033680775,0.26838782,0.00031864867,0.00008712014,0.00017258163,0.0000020722225,0.000007930336,0.00034919096],"genre_scores_gemma":[0.99140435,0.0000011508317,0.008127551,0.00031890196,0.00013317347,0.0000024735043,3.5149492e-7,0.000008016913,0.0000040183654],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9980463,0.0003981154,0.00062023505,0.00020870515,0.0004808214,0.00024582204],"domain_scores_gemma":[0.9993555,0.0001046166,0.00024766586,0.000107808104,0.00002090381,0.00016352697],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00070879393,0.00014711209,0.00039840644,0.0000012408863,0.000116190735,0.000022182367,0.00046561743,0.000119920915,0.000052195002],"category_scores_gemma":[0.000023920345,0.00008632987,0.0003547663,0.00025284145,0.0001274188,0.00010196378,0.000082648265,0.00037277766,0.0000037140824],"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":[0.00017595894,0.00015915146,0.008392068,0.000029961842,0.00003720607,0.0000022800095,0.015361947,0.9690922,0.004470039,0.0001894206,0.00032184136,0.0017679603],"study_design_scores_gemma":[0.0009497857,0.0012418763,0.012659802,0.000070571594,0.000052607724,0.0000063384655,0.004360738,0.9786617,0.0015864756,0.00020566645,0.000039330193,0.00016509456],"about_ca_topic_score_codex":0.000053249572,"about_ca_topic_score_gemma":4.812726e-7,"teacher_disagreement_score":0.2607634,"about_ca_system_score_codex":0.0001261772,"about_ca_system_score_gemma":0.00001175322,"threshold_uncertainty_score":0.352043},"labels":[],"label_agreement":null},{"id":"W3090656336","doi":"10.1029/2004jd004929","title":"Weather systems occurring over Fort Simpson, Northwest Territories, Canada, during three seasons of 1998–1999: 2. Precipitation features","year":2004,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Wave Control Systems (Canada); McMaster University; York University; Ministry of the Environment, Conservation and Parks; McGill University","funders":"","keywords":"Precipitation; Snow; Climatology; Radar; Environmental science; Sublimation (psychology); Precipitation types; Atmospheric sciences; Meteorology; Geology; Geography","score_opus":0.011005249001388434,"score_gpt":0.2622026261118387,"score_spread":0.25119737711045026,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3090656336","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":[0.9980078,0.00055733934,0.00027729457,0.00014078547,0.00029057893,0.00024237254,0.000028261888,0.000009297963,0.00044632418],"genre_scores_gemma":[0.99810386,0.000042450985,0.00080244103,0.00001850401,0.00051942695,0.000010827004,0.0000026597372,0.000030773193,0.0004690346],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99625665,0.0001068929,0.000489405,0.00027222995,0.0022327635,0.0006420362],"domain_scores_gemma":[0.9985983,0.00022365787,0.00035508064,0.00030650035,0.00013636678,0.00038011468],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045450506,0.0002172348,0.0004029261,0.0000026671953,0.00028654747,0.00008435039,0.0005737925,0.00009890409,0.00015555641],"category_scores_gemma":[0.00021719983,0.00016731961,0.00016199937,0.00047833723,0.00031798542,0.00041944886,0.00023959044,0.0006667086,0.000012454545],"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":[0.0006667,0.00043232762,0.90219134,0.00018506075,0.00021754125,0.00024775128,0.00079284434,0.07979663,0.0080341,0.0006855872,0.004946857,0.0018032758],"study_design_scores_gemma":[0.0009345123,0.00058490987,0.9908356,0.00024072336,0.00002539542,0.000027957534,0.00064605946,0.00055044284,0.001074501,0.00055410655,0.0043170154,0.00020879209],"about_ca_topic_score_codex":0.78890187,"about_ca_topic_score_gemma":0.7063235,"teacher_disagreement_score":0.08864425,"about_ca_system_score_codex":0.001010305,"about_ca_system_score_gemma":0.00049309264,"threshold_uncertainty_score":0.68230957},"labels":[],"label_agreement":null},{"id":"W3092126801","doi":"10.5194/tc-15-2781-2021","title":"The retrieval of snow properties from SLSTR Sentinel-3 – Part 2: Results and validation","year":2021,"lang":"en","type":"article","venue":"The cryosphere","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":13,"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":"Environment and Climate Change Canada; Deutsche Forschungsgemeinschaft; University of Oxford","keywords":"Snow; Environmental science; Aerosol; Remote sensing; Satellite; Radiometer; Lookup table; Meteorology; Atmospheric sciences; Geology; Computer science; Aerospace engineering; Physics","score_opus":0.012954410668148168,"score_gpt":0.20160868647031413,"score_spread":0.18865427580216595,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3092126801","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":[0.99246615,0.0006582224,0.000083598636,0.0013541387,0.00016164503,0.00011983185,0.000013099966,0.000018662662,0.005124623],"genre_scores_gemma":[0.9866241,0.00018571384,0.00018055085,0.00011482019,0.00008919844,0.000004882164,0.000009906704,0.000011293557,0.012779503],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989037,0.000098757424,0.00025415194,0.000253659,0.000304925,0.00018481635],"domain_scores_gemma":[0.99929494,0.00011022573,0.00013023609,0.00039747343,0.000020381678,0.00004672661],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024119775,0.00011032939,0.00011598975,1.4159835e-7,0.00028687163,0.000067077504,0.0001951014,0.000058025078,0.0008538265],"category_scores_gemma":[0.00008323645,0.000060690236,0.000045932007,0.00015857145,0.00039447402,0.00008089858,0.0002352497,0.00010934862,0.000080065016],"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":[0.0019134814,0.0005505418,0.45426872,0.00006944086,0.00041413197,0.000071248076,0.008395139,0.003987077,0.17457908,0.0007161818,0.16964766,0.1853873],"study_design_scores_gemma":[0.002155743,0.000162419,0.5103622,0.00018144319,0.00017678701,0.000030007915,0.0055190274,0.0070540765,0.1643032,0.0030412062,0.30630356,0.0007103622],"about_ca_topic_score_codex":0.0005473898,"about_ca_topic_score_gemma":0.00063180097,"teacher_disagreement_score":0.18467695,"about_ca_system_score_codex":0.000026000847,"about_ca_system_score_gemma":0.000020200785,"threshold_uncertainty_score":0.9348802},"labels":[],"label_agreement":null},{"id":"W3092349203","doi":"10.5194/acp-21-10557-2021","title":"Forest-fire aerosol–weather feedbacks over western North America using a high-resolution, online coupled air-quality model","year":2021,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; Environment and Climate Change Canada","funders":"","keywords":"Environmental science; Aerosol; Air quality index; Meteorology; Plume; Atmospheric sciences; Climatology; Geography; Geology","score_opus":0.012224746229418134,"score_gpt":0.2401186936010562,"score_spread":0.22789394737163807,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3092349203","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":[0.961252,0.00014831344,0.037776865,0.00006930101,0.00003620561,0.000094871364,0.000050006136,0.000060696213,0.0005117551],"genre_scores_gemma":[0.9555927,0.00010148375,0.037485417,0.0007041238,0.00019539706,0.000011097013,0.00013429901,0.00004541471,0.0057300897],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9982005,0.000029576539,0.0003360281,0.0006325982,0.00036317998,0.00043813288],"domain_scores_gemma":[0.999029,0.000035726418,0.0001805408,0.0005131027,0.000033444925,0.00020823086],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00004766753,0.000347511,0.00037933633,1.3802618e-8,0.00027090881,0.00004406799,0.00020059838,0.00013114259,0.0015701867],"category_scores_gemma":[0.000013123239,0.00034425437,0.00012035535,0.00035056786,0.00034030425,0.00019891639,0.00027545466,0.00023837069,0.000029802277],"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":[0.00007261581,0.0007652214,0.30135205,0.00010447642,0.00010158282,0.000029535351,0.00075015955,0.62844193,0.03288973,0.000015018916,0.0004464149,0.035031248],"study_design_scores_gemma":[0.0006597904,0.000024713541,0.0507412,0.00002602354,0.00008000245,0.00001534866,0.0002122613,0.9455655,0.001024632,0.0003969596,0.00064614706,0.00060739386],"about_ca_topic_score_codex":0.0009122968,"about_ca_topic_score_gemma":0.00011176444,"teacher_disagreement_score":0.31712356,"about_ca_system_score_codex":0.00015135652,"about_ca_system_score_gemma":0.000066582325,"threshold_uncertainty_score":0.99990094},"labels":[],"label_agreement":null},{"id":"W3092448415","doi":"10.1364/noma.2020.notu3c.3","title":"Surface Tension Measurements Through Optical Deformation","year":2020,"lang":"en","type":"article","venue":"OSA Advanced Photonics Congress (AP) 2020 (IPR, NP, NOMA, Networks, PVLED, PSC, SPPCom, SOF)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"","keywords":"Surface tension; Deformation (meteorology); Materials science; Raman spectroscopy; Tension (geology); Particle (ecology); Optics; Optical tweezers; Aerosol; Beam (structure); Composite material; Chemistry; Physics; Geology; Ultimate tensile strength","score_opus":0.021597640542950897,"score_gpt":0.24222915778479281,"score_spread":0.2206315172418419,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3092448415","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":[0.92313045,0.0023270538,0.047888476,0.002422827,0.0032935971,0.0025248418,0.00008200337,0.0007447447,0.017585993],"genre_scores_gemma":[0.94377786,0.0013210685,0.04951189,0.003970434,0.00024193861,0.00011853912,0.00018630859,0.00019348766,0.00067847915],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99374795,0.00022996539,0.0012748751,0.0016225127,0.0015016154,0.0016230848],"domain_scores_gemma":[0.9970215,0.00020981264,0.0006773431,0.0011099565,0.00012879969,0.00085259095],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00051795307,0.0010225712,0.001063395,0.000005282671,0.00076280604,0.00023594813,0.0012010835,0.00052053697,0.0026953297],"category_scores_gemma":[0.00017253237,0.0009742544,0.00037861458,0.0010272323,0.00054388103,0.0014894493,0.0010393672,0.0010860657,0.0008423362],"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":[0.0011047024,0.00045577384,0.026282579,0.00009917739,0.00021128217,0.0001533349,0.001136251,0.91890603,0.019363955,0.0002963374,0.023020357,0.00897024],"study_design_scores_gemma":[0.006323757,0.0008039688,0.0041760355,0.00023807625,0.00029886756,0.00009015467,0.00086538016,0.8702152,0.012337025,0.0007237713,0.10108831,0.0028394784],"about_ca_topic_score_codex":0.00014411747,"about_ca_topic_score_gemma":0.00012221932,"teacher_disagreement_score":0.07806795,"about_ca_system_score_codex":0.0006542721,"about_ca_system_score_gemma":0.0000822896,"threshold_uncertainty_score":0.9999356},"labels":[],"label_agreement":null},{"id":"W3092513506","doi":"10.1063/5.0016129","title":"A multi-spectral polarimetric imager for atmospheric profiling of aerosol and thin cloud: Prototype design and sub-orbital performance","year":2020,"lang":"en","type":"article","venue":"Review of Scientific Instruments","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":21,"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 Saskatchewan","funders":"Canadian Space Agency","keywords":"Polarimetry; Remote sensing; Profiling (computer programming); Cloud computing; Aerosol; Atmospheric optics; Environmental science; Materials science; Optics; Computer science; Meteorology; Physics; Geology","score_opus":0.023716492225233442,"score_gpt":0.24672890510823117,"score_spread":0.22301241288299772,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3092513506","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":[0.99222046,0.0032163837,0.0017531753,0.00006797003,0.00012498962,0.00251416,0.0000128672,0.000014493434,0.00007548703],"genre_scores_gemma":[0.81127316,0.0020099613,0.18646246,0.00010368833,0.000013502929,0.000064676846,0.0000055779165,0.0000146954035,0.00005225957],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99834955,0.000049844533,0.00048583356,0.00047133738,0.0003625121,0.0002809398],"domain_scores_gemma":[0.9993075,0.000025156567,0.00030520564,0.00018823818,0.000034135093,0.000139757],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00073429773,0.00017847531,0.0003732558,0.0000021622895,0.00017368814,0.000038120845,0.00022227426,0.00004743905,0.00010020119],"category_scores_gemma":[0.00010686558,0.00014455957,0.000071692346,0.00072264124,0.00048254442,0.00032345086,0.00019202786,0.00009421925,0.000013106781],"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":[0.00041315815,0.0005099584,0.29649672,0.019468794,0.000105990395,0.0000034778266,0.0011061801,0.00008050102,0.49038723,0.000069207075,0.000780653,0.1905781],"study_design_scores_gemma":[0.004419277,0.0034023304,0.08630157,0.0049271123,0.00038009838,0.00004728323,0.00026128447,0.21108393,0.68605363,0.00005292438,0.0016839579,0.0013866074],"about_ca_topic_score_codex":0.000022081887,"about_ca_topic_score_gemma":4.4015496e-7,"teacher_disagreement_score":0.21100342,"about_ca_system_score_codex":0.000036877547,"about_ca_system_score_gemma":0.00003635358,"threshold_uncertainty_score":0.58949685},"labels":[],"label_agreement":null},{"id":"W3092711786","doi":"10.5194/acp-21-5597-2021","title":"Measurement Report: Lidar measurements of stratospheric aerosol following the 2019 Raikoke and Ulawun volcanic eruptions","year":2021,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":53,"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":"Natural Environment Research Council; Sight Research UK","keywords":"Aerosol; Lidar; Volcano; Stratosphere; Troposphere; Atmospheric sciences; Environmental science; Vulcanian eruption; Radiosonde; Plume; Volcanic ash; Sulfate aerosol; Altitude (triangle); Meteorology; Geology; Remote sensing; Physics; Seismology","score_opus":0.014915615850525228,"score_gpt":0.2222662884621174,"score_spread":0.20735067261159218,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3092711786","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":[0.98675793,0.0016592717,0.0024323754,0.00014138807,0.00009008916,0.00014906687,0.00000403169,0.000026378471,0.00873947],"genre_scores_gemma":[0.9920435,0.00012395746,0.0051404047,0.00010192142,0.00008190006,0.000017695793,0.000008244852,0.000023549985,0.0024588434],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9981939,0.000042941916,0.00035510838,0.00046685422,0.0006504367,0.0002907684],"domain_scores_gemma":[0.9991048,0.000026705104,0.00018788538,0.0005005512,0.00004740527,0.00013263174],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030687737,0.0002476107,0.00027998028,1.1815145e-8,0.0002905835,0.000051677685,0.00016952174,0.00008596197,0.00073823525],"category_scores_gemma":[0.00004158785,0.00020389429,0.00013076766,0.00030145614,0.00024836106,0.0001324337,0.00017823931,0.00017377516,0.000011466957],"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":[0.000021766462,0.00038109906,0.13600004,0.00011732506,0.0003341712,0.000081216895,0.00066805864,0.0013095797,0.79050994,0.000022495002,0.0010327046,0.069521606],"study_design_scores_gemma":[0.0039878953,0.0002450139,0.21148562,0.00047911436,0.0012711599,0.0005767708,0.0026617325,0.006356735,0.7566828,0.002107906,0.011570279,0.0025749623],"about_ca_topic_score_codex":0.00020471883,"about_ca_topic_score_gemma":0.000032716853,"teacher_disagreement_score":0.07548557,"about_ca_system_score_codex":0.00008833123,"about_ca_system_score_gemma":0.00007321501,"threshold_uncertainty_score":0.8314568},"labels":[],"label_agreement":null},{"id":"W3092790950","doi":"","title":"How consistent is cloudiness over Canada from satellite observations and modeling data","year":2004,"lang":"en","type":"article","venue":"AGU Spring Meeting Abstracts","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Cloud cover; Climatology; Satellite; Environmental science; Meteorology; Remote sensing; Geography; Computer science; Cloud computing; Geology","score_opus":0.0474782514601975,"score_gpt":0.22430949645516735,"score_spread":0.17683124499496986,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3092790950","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":[0.9963053,0.0002992544,0.00035419123,0.0014699855,0.00020622739,0.00008631786,0.000038065682,0.000034933095,0.0012057322],"genre_scores_gemma":[0.991241,0.00008618054,0.007879493,0.0005621999,0.0000696258,0.0000024898234,0.000017241024,0.00001791366,0.00012385522],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99863064,0.000010060745,0.00022012992,0.00047519425,0.00038239153,0.0002815751],"domain_scores_gemma":[0.9991635,0.000056827994,0.00011149987,0.0005166313,0.000012963817,0.00013854734],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019142256,0.00015494098,0.00014009059,9.290915e-7,0.00022353676,0.00011536626,0.00029938712,0.000053699558,0.000024008963],"category_scores_gemma":[0.00013201649,0.00015106962,0.000017980172,0.000086046806,0.000058650094,0.0002616525,0.00039866054,0.00013594903,0.00000625703],"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":[0.0000095081605,0.000055252454,0.6239759,0.00002404663,0.000053854157,0.000068765126,0.00050406286,0.3570673,0.0135599915,0.00006545869,0.000571277,0.0040446096],"study_design_scores_gemma":[0.00042408262,0.000008015352,0.9543475,0.00013128578,0.00004500755,0.0000036270612,0.00037325162,0.032987338,0.0010829032,0.00031820356,0.009888598,0.00039020184],"about_ca_topic_score_codex":0.88874096,"about_ca_topic_score_gemma":0.62056553,"teacher_disagreement_score":0.3303716,"about_ca_system_score_codex":0.00022016674,"about_ca_system_score_gemma":0.00008529148,"threshold_uncertainty_score":0.61604404},"labels":[],"label_agreement":null},{"id":"W3092817443","doi":"10.5194/acp-20-11799-2020","title":"Possible mechanisms of summer cirrus clouds over the Tibetan Plateau","year":2020,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","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":"McGill University","funders":"National Natural Science Foundation of China","keywords":"Cirrus; Plateau (mathematics); Orographic lift; Atmospheric sciences; Lidar; Climatology; Environmental science; Geology; Meteorology; Geography; Remote sensing; Precipitation","score_opus":0.009417231466431029,"score_gpt":0.20661116546522487,"score_spread":0.19719393399879384,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3092817443","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":[0.97025067,0.000063248895,0.00838056,0.0002566262,0.00002977084,0.00008810963,0.00000692438,0.000028984137,0.020895118],"genre_scores_gemma":[0.9934068,0.000040340656,0.004148198,0.0007071306,0.00010893966,0.0000061215505,0.000004534687,0.000018499815,0.0015594395],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99908996,0.000016327482,0.00017482911,0.0002794846,0.00022586397,0.00021356685],"domain_scores_gemma":[0.99949557,0.00003764275,0.00009829263,0.00023488929,0.0000062145164,0.0001273845],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000068338624,0.00017389595,0.00018664188,3.0583034e-9,0.00012522396,0.000020069478,0.0002431247,0.00007259372,0.0054403213],"category_scores_gemma":[0.000007778601,0.00012781256,0.000075779346,0.0002291325,0.00023413106,0.00007718533,0.00015789457,0.00015261873,0.000052966952],"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":[0.00022880679,0.00043261037,0.121543236,0.00031162528,0.00027918487,0.000029171571,0.004963968,0.007436579,0.53740555,0.0034686092,0.014044617,0.30985606],"study_design_scores_gemma":[0.003571778,0.00059493637,0.1318652,0.00009184779,0.0004817761,0.000039493392,0.002464935,0.24754451,0.50284475,0.050662287,0.0572316,0.0026068746],"about_ca_topic_score_codex":0.000121265344,"about_ca_topic_score_gemma":9.221475e-7,"teacher_disagreement_score":0.30724916,"about_ca_system_score_codex":0.00002182828,"about_ca_system_score_gemma":0.000012307804,"threshold_uncertainty_score":0.99546885},"labels":[],"label_agreement":null},{"id":"W3093612862","doi":"","title":"Multi-event analysis of Lidar and Sunphotometer observations acquired at a site in Southern Canada","year":2009,"lang":"en","type":"article","venue":"AGU Spring Meeting Abstracts","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Lidar; Remote sensing; Geography; Meteorology; Environmental science; Geology","score_opus":0.013684031124419928,"score_gpt":0.21797431504644985,"score_spread":0.2042902839220299,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3093612862","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":[0.9992832,0.000033254168,0.000013789368,0.00014790683,0.000025500896,0.00007748596,0.000006217096,0.000011953482,0.00040068608],"genre_scores_gemma":[0.99626034,0.0000041784833,0.0032892004,0.00012588929,0.0000054832744,0.0000025269223,0.0000031656027,0.0000064722176,0.00030276805],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99899143,0.00001935156,0.00030567142,0.0002421013,0.00021770944,0.00022373073],"domain_scores_gemma":[0.9995229,0.000047270434,0.00016011804,0.00018125925,0.0000064937612,0.00008193491],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022354504,0.00010720972,0.00019167573,0.000006253353,0.00008572394,0.0000120246805,0.00010076729,0.000041668955,0.00006668651],"category_scores_gemma":[0.00006532803,0.00010326092,0.000046646313,0.00042995738,0.000038698752,0.000052787127,0.000078813006,0.00005174722,0.000005762458],"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":[0.0000044780886,0.000034632634,0.87619597,0.0000027516328,0.000023106037,0.000010571184,0.0007070006,0.081032865,0.04156509,4.2612606e-7,0.000006412514,0.00041671746],"study_design_scores_gemma":[0.00015538507,0.000011345546,0.98813605,0.00001727712,0.00005988222,4.1249953e-7,0.00018951675,0.010130038,0.0010478013,0.0000013886743,0.00014254537,0.00010835088],"about_ca_topic_score_codex":0.7400362,"about_ca_topic_score_gemma":0.87118924,"teacher_disagreement_score":0.13115306,"about_ca_system_score_codex":0.00019821692,"about_ca_system_score_gemma":0.00001533315,"threshold_uncertainty_score":0.42108583},"labels":[],"label_agreement":null},{"id":"W3093953501","doi":"10.5194/egusphere-egu2020-19164","title":"Comparing Halo Doppler lidar depolarization ratio with PollyXT","year":2020,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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; Depolarization; Depolarization ratio; Wavelength; Doppler effect; Lidar; Halo; Analytical Chemistry (journal); Chemistry; Optics; Physics; Astrophysics; Meteorology; Internal medicine; Medicine; Astronomy","score_opus":0.014939506866627024,"score_gpt":0.18964064576053782,"score_spread":0.1747011388939108,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3093953501","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":[0.6166589,0.000007423225,0.3028162,0.0010700435,0.000018307668,0.00010819135,3.8292154e-7,0.00008349091,0.07923702],"genre_scores_gemma":[0.9888704,0.0000017549053,0.008600581,0.0017236661,0.000034819477,0.0000035466035,0.0000037332761,0.000010090463,0.0007514528],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99941,0.000010786562,0.00009238334,0.00018227025,0.00017167318,0.0001329377],"domain_scores_gemma":[0.99976724,0.000005362564,0.000031796724,0.000087394874,0.0000026540197,0.000105519364],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000023134777,0.00008000687,0.00008187087,2.3023777e-7,0.00009308095,0.000035957328,0.000099358374,0.000024789877,0.004022594],"category_scores_gemma":[0.000003825309,0.000058023354,0.000015226685,0.00016375653,0.000052464227,0.00014496653,0.00007556848,0.00005680748,0.0005490375],"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":[0.00001750367,0.000019187904,0.9815265,0.0000024149674,0.000006236598,0.0000039166275,0.00044646277,0.0070591588,0.00730406,0.000716532,0.0021159125,0.000782092],"study_design_scores_gemma":[0.0010086535,0.00031774514,0.84303355,0.000008480781,0.000029812136,0.000016100512,0.00070138,0.13137287,0.009478506,0.00008490295,0.013409609,0.000538395],"about_ca_topic_score_codex":0.00035270434,"about_ca_topic_score_gemma":0.00017296486,"teacher_disagreement_score":0.37221143,"about_ca_system_score_codex":0.00002610346,"about_ca_system_score_gemma":0.000005868131,"threshold_uncertainty_score":0.99688786},"labels":[],"label_agreement":null},{"id":"W3096118521","doi":"","title":"Stratospheric Injection of Canadian Forest Fire Emissions on August 4, 1998: A Satellite Image Analysis of the Causal Supercell Convection","year":2003,"lang":"en","type":"article","venue":"EGS - AGU - EUG Joint Assembly","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Satellite; Meteorology; Environmental science; Convection; Causal analysis; Climatology; Supercell; Satellite image; Satellite imagery; Atmospheric sciences; Remote sensing; Geology; Geography; Physics; Thunderstorm","score_opus":0.013113621344245454,"score_gpt":0.21664275088388268,"score_spread":0.20352912953963723,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3096118521","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":[0.9657828,0.0000354723,0.00017084998,0.00010371768,0.00017259635,0.00021823478,0.00001805249,0.00001843869,0.033479836],"genre_scores_gemma":[0.99763894,0.00005322483,0.0004814443,0.000098526856,0.000016936314,0.000010246933,0.000011626775,0.000019780668,0.001669273],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984199,0.0001343675,0.00040789336,0.00033250102,0.0003676222,0.00033776482],"domain_scores_gemma":[0.9990909,0.000040057323,0.00020771287,0.00043279617,0.000019907344,0.00020860723],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00024698055,0.00020217008,0.0003156263,0.000017472341,0.00022883667,0.000024371617,0.00017885784,0.00012996618,0.0015105456],"category_scores_gemma":[0.0000616018,0.00015157864,0.0002583627,0.0023369498,0.00018921701,0.00013765278,0.00004238961,0.00019514219,0.000061889565],"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":[0.000029844852,0.00029870216,0.849986,0.000026107406,0.00029245878,0.0000106534335,0.0013445677,0.020069059,0.11968613,0.0005309431,0.0056087077,0.0021168357],"study_design_scores_gemma":[0.00021256863,0.0002118738,0.9774176,0.000027145023,0.00030774702,0.0000074580335,0.0009087536,0.0042357696,0.013191587,0.000085933694,0.003163579,0.00023002336],"about_ca_topic_score_codex":0.24771956,"about_ca_topic_score_gemma":0.2689404,"teacher_disagreement_score":0.12743157,"about_ca_system_score_codex":0.00028675876,"about_ca_system_score_gemma":0.00009660535,"threshold_uncertainty_score":0.9994022},"labels":[],"label_agreement":null},{"id":"W3097017117","doi":"10.1016/j.atmosres.2020.105345","title":"Climatological aspects of size-resolved column aerosol optical properties over a rural site in the southern peninsular India","year":2020,"lang":"en","type":"article","venue":"Atmospheric Research","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":31,"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":"Universität Hamburg; Indian Space Research Organisation; National Atmospheric Research Laboratory; Université de Sherbrooke","keywords":"Aerosol; Single-scattering albedo; Angstrom exponent; Environmental science; Atmospheric sciences; Dominance (genetics); Climatology; AERONET; Optical depth; Meteorology; Geology; Physics; Chemistry","score_opus":0.03719395118698282,"score_gpt":0.2780933706251639,"score_spread":0.2408994194381811,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3097017117","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":[0.98484945,0.0002164421,0.000069809204,0.0015632719,0.00002264909,0.0009322552,0.0000028819697,0.000032601147,0.012310663],"genre_scores_gemma":[0.9977402,0.000035659108,0.0012031535,0.00057663966,0.000057546134,0.00013232652,0.000001481899,0.000027982864,0.00022500457],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9961203,0.0005396105,0.0004561867,0.00047547155,0.0015638325,0.0008445963],"domain_scores_gemma":[0.99880576,0.00040532945,0.00008443515,0.00045196607,0.000031942862,0.00022054464],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0010514698,0.00022047278,0.00037669146,4.5946527e-7,0.00021856446,0.00009497261,0.0008855856,0.00017074062,0.003184092],"category_scores_gemma":[0.00062362564,0.00013833276,0.00012395148,0.001223272,0.0012323451,0.00014025436,0.00073967205,0.0007702163,0.000872432],"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":[0.00073702296,0.0006362204,0.90789205,0.00009623875,0.000038124123,0.00033243187,0.02114309,0.0013184114,0.062059723,0.00073181314,0.002183027,0.0028318313],"study_design_scores_gemma":[0.0031363373,0.0025669048,0.9315401,0.00011906185,0.000034873126,0.000041868494,0.022865307,0.032516386,0.0026196684,0.0010868252,0.0025979718,0.0008747483],"about_ca_topic_score_codex":0.0014307305,"about_ca_topic_score_gemma":0.00017282808,"teacher_disagreement_score":0.059440054,"about_ca_system_score_codex":0.00010501823,"about_ca_system_score_gemma":0.00006864214,"threshold_uncertainty_score":0.9999055},"labels":[],"label_agreement":null},{"id":"W3107587298","doi":"10.1175/bams-d-19-0227.1","title":"The Shortwave Spectral Radiometer for Atmospheric Science: Capabilities and Applications from the ARM User Facility","year":2020,"lang":"en","type":"article","venue":"Bulletin of the American Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":27,"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":"U.S. Department of Energy","keywords":"Shortwave; Environmental science; Remote sensing; Aerosol; Shortwave radiation; Radiometer; Cloud computing; Meteorology; Radiative transfer; Radiation; Computer science; Physics; Optics; Geology","score_opus":0.010416417710779806,"score_gpt":0.21826084244498936,"score_spread":0.20784442473420955,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3107587298","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":[0.9690131,0.00016778786,0.0031075128,0.026369141,0.000029280389,0.00071913336,0.000056008586,0.000028072618,0.00050995115],"genre_scores_gemma":[0.97757477,0.000112622045,0.015019826,0.006870343,0.00008546698,0.00016940177,0.0000012700358,0.000006953684,0.00015935823],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9984228,0.00012009481,0.00024847614,0.0004560775,0.00038370639,0.00036882496],"domain_scores_gemma":[0.99826115,0.00095675857,0.00020528972,0.0004378266,0.000018717847,0.00012024072],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0006540713,0.00016143685,0.0002451304,1.0390929e-7,0.0009913596,0.000056958277,0.0010192903,0.000039695376,0.0007316899],"category_scores_gemma":[0.0002768157,0.00006938509,0.00028982892,0.0004114208,0.010107771,0.000020183534,0.000593885,0.0002019809,0.000020873194],"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":[0.0006497205,0.0005075266,0.62838966,0.000030117944,0.00039776045,6.030472e-7,0.0072729345,0.0021244225,0.041525904,0.0039389976,0.15860994,0.1565524],"study_design_scores_gemma":[0.00029008964,0.00049734523,0.44738838,0.0000016421108,0.00008489928,0.0000015724496,0.0068511507,0.0014811475,0.000895662,0.0025144396,0.53973675,0.00025690734],"about_ca_topic_score_codex":0.0006941757,"about_ca_topic_score_gemma":0.000008918866,"teacher_disagreement_score":0.38112682,"about_ca_system_score_codex":0.000072145245,"about_ca_system_score_gemma":0.000020010571,"threshold_uncertainty_score":0.99258614},"labels":[],"label_agreement":null},{"id":"W3107617234","doi":"10.1016/j.atmosenv.2020.118102","title":"Remote sensing of a high-Arctic, local dust event over Lake Hazen (Ellesmere Island, Nunavut, Canada)","year":2020,"lang":"en","type":"article","venue":"Atmospheric Environment","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":28,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université de Montréal; Université de Sherbrooke","funders":"Natural Sciences and Engineering Research Council of Canada; Networks of Centres of Excellence of Canada; Canadian Space Agency","keywords":"Arctic; Plume; Aeolian processes; Remote sensing; Terrain; Environmental science; Geology; Satellite; Oceanography; Meteorology; Geomorphology; Geography; Cartography","score_opus":0.004920731256655522,"score_gpt":0.1761018295894056,"score_spread":0.17118109833275008,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3107617234","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":[0.8674059,0.00012523186,0.12698314,0.0031991191,0.00016217458,0.00037456947,0.000035629302,0.000035298573,0.0016789435],"genre_scores_gemma":[0.9761003,0.00013899042,0.019498304,0.0030593164,0.0000894154,0.0000021512492,0.000018367407,0.000058131805,0.0010349858],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99723,0.00007907998,0.00052187714,0.00066388637,0.00095379824,0.0005513813],"domain_scores_gemma":[0.99881196,0.000049991228,0.00025465162,0.00049225247,0.0000045842835,0.0003865383],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00011078842,0.00037467282,0.0004415617,2.2368056e-7,0.00015141588,0.000014104005,0.00032722423,0.00012748582,0.020720702],"category_scores_gemma":[0.000018896766,0.00034947292,0.00012537258,0.00020615911,0.00036392486,0.00008685379,0.0004643365,0.00026544792,0.0002183019],"study_design_candidate":"simulation_or_modeling","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":[0.0003704347,0.00035737915,0.25952998,0.00013086227,0.000382648,0.00078658864,0.001914712,0.50009614,0.0029346428,0.00008252545,0.066438496,0.16697559],"study_design_scores_gemma":[0.0024018667,0.0006488359,0.40265808,0.00008079147,0.00021935224,0.000052084455,0.0012929023,0.23097955,0.0011402523,0.00020661586,0.35882655,0.0014931344],"about_ca_topic_score_codex":0.1816553,"about_ca_topic_score_gemma":0.30835924,"teacher_disagreement_score":0.29238805,"about_ca_system_score_codex":0.0005820791,"about_ca_system_score_gemma":0.00007054164,"threshold_uncertainty_score":0.99989575},"labels":[],"label_agreement":null},{"id":"W3110448726","doi":"10.1080/07055900.2020.1843393","title":"Neural Network Classification of Ice-Crystal Images Observed by an Airborne Cloud Imaging Probe","year":2020,"lang":"en","type":"article","venue":"ATMOSPHERE-OCEAN","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"China Meteorological Administration; National Natural Science Foundation of China","keywords":"Ice crystals; Convolutional neural network; Artificial intelligence; Computer science; Cloud computing; Remote sensing; Artificial neural network; Radiative transfer; Meteorology; Geology; Physics; Optics","score_opus":0.017528389842784542,"score_gpt":0.2191528854553327,"score_spread":0.20162449561254817,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3110448726","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":[0.9890433,0.00032519945,0.005385097,0.0016541375,0.00018250677,0.0003664195,0.000017673367,0.00018549016,0.0028401576],"genre_scores_gemma":[0.990685,0.000021207692,0.007320398,0.0011033638,0.00030862505,0.0000057350926,0.000052672847,0.00006309893,0.0004399369],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9977057,0.00012627029,0.00050617324,0.0006685488,0.00044557988,0.000547708],"domain_scores_gemma":[0.9988087,0.0000490357,0.00031522027,0.00045572437,0.000024645447,0.00034668756],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00020626558,0.0003128391,0.00033365886,1.6720107e-7,0.0001939008,0.000063827814,0.000581568,0.000089785,0.0017754954],"category_scores_gemma":[0.000041404233,0.00029434852,0.0001224917,0.00045815416,0.00033497342,0.00052913185,0.00025411512,0.00023738992,0.00008445119],"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":[0.000123301,0.0002244078,0.81147593,0.000034572484,0.00003082409,0.000014262527,0.0009828699,0.024154846,0.036011416,0.00014081343,0.11171663,0.01509013],"study_design_scores_gemma":[0.0015378974,0.00064571743,0.64117813,0.000038814575,0.0001176787,0.000010909274,0.0024203043,0.32594475,0.0031296937,0.0005563794,0.023274913,0.0011448167],"about_ca_topic_score_codex":0.00044988957,"about_ca_topic_score_gemma":0.000026553784,"teacher_disagreement_score":0.30178988,"about_ca_system_score_codex":0.00008347412,"about_ca_system_score_gemma":0.000020712916,"threshold_uncertainty_score":0.9999509},"labels":[],"label_agreement":null},{"id":"W3110725524","doi":"10.1029/2020gl091236","title":"Observational Constraints on Warm Cloud Microphysical Processes Using Machine Learning and Optimization Techniques","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","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":"Université de Montréal; Université du Québec à Montréal","funders":"U.S. Department of Energy","keywords":"Drizzle; Accretion (finance); Environmental science; Cloud computing; Liquid water content; Meteorology; Cloud physics; Representation (politics); Atmospheric sciences; Computer science; Astrophysics; Physics","score_opus":0.05776324653679146,"score_gpt":0.31339839167107086,"score_spread":0.25563514513427943,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3110725524","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":[0.9759822,0.000010229846,0.014323353,0.008975933,0.000015391384,0.00024270428,0.000005841742,0.00006914129,0.00037522495],"genre_scores_gemma":[0.9782315,0.000020080484,0.018863872,0.0025180178,0.00027576147,0.000016595835,0.000014696246,0.000021579395,0.000037931306],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99831915,0.00012673246,0.00013368549,0.0004058055,0.0006490726,0.00036558026],"domain_scores_gemma":[0.9994835,0.00017872793,0.00004057795,0.00007742126,0.000029012059,0.00019073774],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014149737,0.00013418484,0.00014257431,0.0000029333733,0.0003069257,0.00007011816,0.0001608842,0.000044864766,0.00034426473],"category_scores_gemma":[0.00029781827,0.000117912095,0.000032187367,0.00045833824,0.0006792326,0.00014188353,0.0002479836,0.00049349625,0.00008508847],"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":[0.00020801871,0.00022639781,0.016374588,0.000081317485,0.000024672825,0.000044384677,0.00067473185,0.034628924,0.9316325,0.00028320478,0.0020627254,0.013758488],"study_design_scores_gemma":[0.0015547172,0.0023429825,0.016421238,0.00021275283,0.000044954788,0.000015876565,0.0006028494,0.8504348,0.10997592,0.0007352397,0.016145512,0.0015131786],"about_ca_topic_score_codex":0.00016927882,"about_ca_topic_score_gemma":0.000001487355,"teacher_disagreement_score":0.82165664,"about_ca_system_score_codex":0.00008417544,"about_ca_system_score_gemma":0.000026660216,"threshold_uncertainty_score":0.4808316},"labels":[],"label_agreement":null},{"id":"W3111035455","doi":"","title":"Summertime Trans-Pacific Transport of Asian Dust","year":2010,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"","keywords":"Outflow; Lidar; Atmosphere (unit); Asian Dust; Mineral dust; Altitude (triangle); Environmental science; Anomaly (physics); Storm; Geology; Atmospheric sciences; Aeolian processes; Dust storm; Climatology; Oceanography; Meteorology; Aerosol; Geography; Geomorphology; Remote sensing","score_opus":0.008201805538293883,"score_gpt":0.20931434086861433,"score_spread":0.20111253533032045,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3111035455","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":[0.78575414,0.000009227673,0.00002283989,0.00028473363,0.0002388913,0.000109614295,0.0000045504453,0.000050189785,0.21352579],"genre_scores_gemma":[0.99572843,0.0000073953365,0.002747276,0.00005673034,0.000060331655,0.000006372548,0.000006393023,0.000027102327,0.001359974],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99848485,0.000016408398,0.00042009936,0.0003400061,0.00035619354,0.00038242762],"domain_scores_gemma":[0.9992626,0.00004175311,0.00016437408,0.00033596696,0.000010030241,0.00018529542],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036528773,0.00018579264,0.00021353878,0.0000021814712,0.00010897955,0.000011839886,0.00030899217,0.00016022837,0.0004847012],"category_scores_gemma":[0.000037301845,0.0001704167,0.000110805515,0.00016021209,0.00025892264,0.00012881636,0.00002179799,0.00034306245,0.00023719283],"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":[0.000023389724,0.00019248981,0.83349097,0.000020802114,0.00001561496,0.00003077871,0.0012171982,0.0012618019,0.15439859,0.00002091227,0.0007761139,0.008551341],"study_design_scores_gemma":[0.00026727395,0.000057866524,0.9756242,0.000025459552,0.00002772515,0.000010614137,0.0003426201,0.000092772556,0.009898939,0.00006766707,0.013329736,0.00025513666],"about_ca_topic_score_codex":0.007012093,"about_ca_topic_score_gemma":0.007887155,"teacher_disagreement_score":0.21216582,"about_ca_system_score_codex":0.000018791683,"about_ca_system_score_gemma":0.00001597928,"threshold_uncertainty_score":0.9996003},"labels":[],"label_agreement":null},{"id":"W3111368246","doi":"","title":"Night-time aerosol optical depths retrievals using starphotometry in Canada","year":2009,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Aerosol; Environmental science; Remote sensing; Meteorology; Atmospheric sciences; Climatology; Geography; Geology","score_opus":0.010455128952592332,"score_gpt":0.22263605658942653,"score_spread":0.21218092763683422,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3111368246","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":[0.96815735,0.000049848455,0.000013189439,0.0001606088,0.00014265873,0.00018196627,0.0000026705366,0.000037988983,0.031253733],"genre_scores_gemma":[0.99343014,0.0000071447885,0.0055017616,0.00068341015,0.000052548516,0.0000018612134,0.0000031007673,0.000020496533,0.00029954253],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9976143,0.00004483178,0.0005182441,0.00047100714,0.00064648123,0.00070508715],"domain_scores_gemma":[0.99909633,0.00014689668,0.00016611641,0.0003057037,0.000010820927,0.00027412616],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004493796,0.0002400997,0.0002901537,0.000004150969,0.0001323777,0.000046783814,0.0003211465,0.00011816726,0.00018854643],"category_scores_gemma":[0.00027711233,0.00023126006,0.00005085597,0.00045555955,0.00006605651,0.00016770714,0.00009238478,0.00031633963,0.00018168069],"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":[0.00005732195,0.00018313984,0.74791163,0.000011124107,0.000013616299,0.0005298563,0.00021233736,0.14058426,0.10392997,0.000004393291,0.0020771425,0.00448523],"study_design_scores_gemma":[0.0005212433,0.00009695962,0.97260875,0.00010279307,0.000020042442,0.000033115342,0.00021579974,0.009386181,0.015940001,0.00005883495,0.00040761652,0.00060865557],"about_ca_topic_score_codex":0.89458406,"about_ca_topic_score_gemma":0.7892608,"teacher_disagreement_score":0.22469714,"about_ca_system_score_codex":0.0011199905,"about_ca_system_score_gemma":0.0002041523,"threshold_uncertainty_score":0.94305116},"labels":[],"label_agreement":null},{"id":"W3111576666","doi":"10.5194/acp-21-9779-2021","title":"Tropospheric and stratospheric wildfire smoke profiling with lidar: mass, surface area, CCN, and INP retrieval","year":2021,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":138,"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":"Horizon 2020; Research and Innovation Foundation; Russian Science Foundation; European Commission; Horizon 2020 Framework Programme; Deutsche Forschungsgemeinschaft; U.S. Department of Energy","keywords":"Smoke; Environmental science; Lidar; AERONET; Cloud condensation nuclei; Atmospheric sciences; Troposphere; Stratosphere; Meteorology; Aerosol; Climatology; Remote sensing; Geology; Geography","score_opus":0.005957758687896193,"score_gpt":0.1923106811565528,"score_spread":0.18635292246865662,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3111576666","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":[0.9900882,0.0017637283,0.0024709192,0.000108656284,0.000028237442,0.00015018925,0.0000071405752,0.000067473135,0.0053154505],"genre_scores_gemma":[0.9439056,0.00083020504,0.05173115,0.00015511968,0.00008123362,0.000006213241,0.00001911548,0.000047096513,0.0032242711],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99813724,0.000033693632,0.0002512726,0.00079786393,0.00033270454,0.00044720506],"domain_scores_gemma":[0.9991365,0.00005861178,0.00012995179,0.00036460918,0.000021159907,0.00028913943],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000094503244,0.00041335527,0.00038558073,1.2141793e-8,0.0003145346,0.00014487465,0.00012758949,0.00016197735,0.0011805579],"category_scores_gemma":[0.000014117829,0.00036938433,0.000046807345,0.00047102498,0.0005656491,0.00025637704,0.00017237048,0.00031759305,0.0000076036195],"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":[0.00024835765,0.0002531233,0.77371025,0.00025916522,0.00015793002,0.00018934834,0.00063641166,0.0026616794,0.17101021,0.000057591307,0.0002687786,0.05054712],"study_design_scores_gemma":[0.010582478,0.0014699723,0.34785536,0.0006095945,0.001117819,0.0014865946,0.011659689,0.19732116,0.3953146,0.006422901,0.018683964,0.007475859],"about_ca_topic_score_codex":0.00010497808,"about_ca_topic_score_gemma":0.0000047592293,"teacher_disagreement_score":0.42585492,"about_ca_system_score_codex":0.000067009096,"about_ca_system_score_gemma":0.00006478336,"threshold_uncertainty_score":0.9998758},"labels":[],"label_agreement":null},{"id":"W3112906047","doi":"","title":"A fast, flexible, approximate technique for computing radiative transfer in inhomogeneous cloud fields","year":2003,"lang":"en","type":"article","venue":"EGS - AGU - EUG Joint Assembly","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"","keywords":"Radiative transfer; Cloud computing; Benchmark (surveying); Statistical physics; Scale (ratio); Computer science; Radiative flux; Meteorology; Environmental science; Remote sensing; Applied mathematics; Physics; Mathematics; Geology; Optics","score_opus":0.016461991093757396,"score_gpt":0.24172142966865043,"score_spread":0.22525943857489303,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3112906047","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.46348944,0.000082918385,0.5208811,0.00015147659,0.0001794073,0.0010573944,0.0000071729955,0.000090446934,0.0140605895],"genre_scores_gemma":[0.9676387,0.000019038938,0.030835181,0.00043194857,0.00007690406,0.00018458825,0.0000061663395,0.00004438181,0.00076314766],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9979474,0.00012135706,0.00047257583,0.000548909,0.0002626204,0.000647164],"domain_scores_gemma":[0.99938625,0.000093011426,0.00008447197,0.00028399198,0.0000125852275,0.00013969644],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0006252345,0.0003049684,0.0003891943,0.000008001225,0.00018456139,0.00004486243,0.00023399125,0.00021354022,0.0003309584],"category_scores_gemma":[0.00006188889,0.00028572392,0.00016684594,0.00040190158,0.000108835644,0.00013645175,0.00007635641,0.00028544324,0.000060537932],"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":[0.00075572374,0.003849178,0.15857032,0.00066628907,0.0003784244,0.00055301003,0.030543609,0.18399881,0.46710882,0.028933024,0.035162054,0.08948076],"study_design_scores_gemma":[0.007978058,0.0024283964,0.045661774,0.00044811922,0.00015991868,0.00033404215,0.0032480732,0.07053048,0.81418794,0.013338313,0.037225436,0.00445944],"about_ca_topic_score_codex":0.00029684434,"about_ca_topic_score_gemma":0.00016861531,"teacher_disagreement_score":0.5041492,"about_ca_system_score_codex":0.00021910391,"about_ca_system_score_gemma":0.00003607514,"threshold_uncertainty_score":0.99995947},"labels":[],"label_agreement":null},{"id":"W3113184199","doi":"10.1109/jstars.2020.3036815","title":"A Probability-Based Daytime Algorithm for Sea Fog Detection Using GOES-16 Imagery","year":2020,"lang":"en","type":"article","venue":"IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":26,"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":"Daytime; Meteorology; Remote sensing; Geostationary orbit; Environmental science; Twilight; Fog; False alarm; Satellite; Geostationary Operational Environmental Satellite; Computer science; Algorithm; Artificial intelligence; Geography; Geology; Engineering","score_opus":0.03578073006741373,"score_gpt":0.22908002177193146,"score_spread":0.19329929170451773,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3113184199","genre_codex":"empirical","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"methods","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5162347,0.000012535093,0.48311386,0.0003219871,0.000064783286,0.00017526773,0.0000022224613,0.000010176352,0.00006444293],"genre_scores_gemma":[0.46550435,0.000008490659,0.533863,0.00038804574,0.00020821494,1.3768235e-7,0.000001633698,0.000013060836,0.000013042312],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9989289,0.000034840985,0.00041462894,0.00019443776,0.00022058676,0.00020660253],"domain_scores_gemma":[0.99942064,0.000065078304,0.00024131626,0.00008275754,0.00008854839,0.00010163359],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025992826,0.00012804857,0.00022107066,0.000008053373,0.00017769038,0.00004571117,0.00006445314,0.00007847817,0.000011532819],"category_scores_gemma":[0.00006976566,0.000116905896,0.000055182838,0.0005573184,0.000077493445,0.00010239403,0.000019375193,0.00025514528,7.218004e-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":[0.000077141536,0.000041385163,0.0021857433,0.00004250777,0.00002499619,0.0000093211465,0.0002969758,0.030711686,0.15998337,0.0000061230116,0.000053056123,0.8065677],"study_design_scores_gemma":[0.000752484,0.00010503361,0.010726345,0.000036864465,0.00003432391,0.000025306688,0.000052971878,0.971541,0.0142623335,0.00083756214,0.0014611081,0.00016469516],"about_ca_topic_score_codex":0.000120479024,"about_ca_topic_score_gemma":0.0001314266,"teacher_disagreement_score":0.9408293,"about_ca_system_score_codex":0.00013518047,"about_ca_system_score_gemma":0.00007851758,"threshold_uncertainty_score":0.4767284},"labels":[],"label_agreement":null},{"id":"W3115860312","doi":"","title":"Modeling of Aerosol Optical Depth Variability during the 1998 Canadian Forest Fire Smoke Event","year":2003,"lang":"en","type":"article","venue":"EGS - AGU - EUG Joint Assembly","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Smoke; Aerosol; Environmental science; Event (particle physics); Meteorology; Remote sensing; Atmospheric sciences; Geography; Geology","score_opus":0.015002009311101233,"score_gpt":0.22228835112049966,"score_spread":0.20728634180939842,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3115860312","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":[0.97513217,0.000043323187,0.0035388472,0.00026620226,0.0001653694,0.00033194307,0.0000050838116,0.000029583915,0.02048748],"genre_scores_gemma":[0.9974404,0.000013229452,0.0019790437,0.00014557081,0.000044876542,0.00003234623,0.0000030142137,0.000028130878,0.00031337043],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978522,0.00012561605,0.00047418516,0.0004487657,0.00044983294,0.00064937444],"domain_scores_gemma":[0.99888575,0.000058609512,0.00009667142,0.00059620274,0.000014391549,0.00034835277],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007449627,0.00024288619,0.00027647777,0.0000025547943,0.00037142183,0.000040856085,0.00033401538,0.00013277674,0.00042535213],"category_scores_gemma":[0.00018921761,0.00018057597,0.00016778328,0.00023414698,0.00018025862,0.00014996013,0.00014184369,0.00028207543,0.00011838683],"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":[0.00002699656,0.000278948,0.63574815,0.000052914384,0.00006324778,0.000039794155,0.0009781206,0.35191387,0.006866798,0.0016677199,0.0004739106,0.0018895144],"study_design_scores_gemma":[0.00080980983,0.00016839648,0.6563315,0.000076270815,0.00008556308,0.000055262924,0.00070192263,0.33231986,0.0065719765,0.0010697002,0.0009776014,0.00083216664],"about_ca_topic_score_codex":0.094170496,"about_ca_topic_score_gemma":0.15032914,"teacher_disagreement_score":0.056158647,"about_ca_system_score_codex":0.0004888155,"about_ca_system_score_gemma":0.00011068635,"threshold_uncertainty_score":0.9118615},"labels":[],"label_agreement":null},{"id":"W3116374115","doi":"10.1029/2020jd034201","title":"Seasonal and Solar Wind Sector Duration Influences on the Correlation of High Latitude Clouds With Ionospheric Potential","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":19,"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; Solar wind; Interplanetary magnetic field; Ionosphere; Environmental science; Latitude; Physics; Meteorology; Magnetic field; Geophysics; Astronomy","score_opus":0.017608018547632595,"score_gpt":0.25459799557653345,"score_spread":0.23698997702890084,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3116374115","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":[0.9946654,0.00005876732,0.002507448,0.002304869,0.00004621713,0.00016355405,0.0000022276643,0.0000052302507,0.00024633174],"genre_scores_gemma":[0.99735874,0.000042412397,0.0020343661,0.00016855956,0.00030495456,0.0000022508245,6.85699e-7,0.00001272112,0.00007529139],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9976063,0.00019765206,0.0003263899,0.0001941679,0.0014190212,0.00025648178],"domain_scores_gemma":[0.99893636,0.00032517506,0.00028624453,0.00012188654,0.000115721756,0.00021462442],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00042427343,0.00013210948,0.00022872452,7.309122e-7,0.00022806127,0.00006906587,0.00028807044,0.00006044117,0.0011021043],"category_scores_gemma":[0.00023348116,0.00007404723,0.00007026749,0.00043521376,0.00059034576,0.00028822751,0.00012821732,0.0005516027,0.000043717497],"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":[0.005420096,0.000957964,0.5595084,0.00009005414,0.00042556965,0.00016657928,0.0032449383,0.33151388,0.04871006,0.0052401265,0.011371814,0.033350527],"study_design_scores_gemma":[0.00071939896,0.0032549738,0.9590226,0.00006342597,0.000032125623,0.000011989655,0.0006352947,0.0320022,0.0012916616,0.002207592,0.00061997486,0.00013875372],"about_ca_topic_score_codex":0.0003687107,"about_ca_topic_score_gemma":0.000025084224,"teacher_disagreement_score":0.39951423,"about_ca_system_score_codex":0.000060477625,"about_ca_system_score_gemma":0.0000783578,"threshold_uncertainty_score":0.99981105},"labels":[],"label_agreement":null},{"id":"W3117700198","doi":"10.5194/acp-21-10671-2021","title":"Airborne and ground-based measurements of aerosol optical depth of freshly emitted anthropogenic plumes in the Athabasca Oil Sands Region","year":2021,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada; National Research Council Canada; Université de Sherbrooke; Canadian Space Agency","funders":"Ames Research Center; Environment and Climate Change Canada; National Aeronautics and Space Administration","keywords":"AERONET; Plume; Environmental science; Aerosol; Atmospheric sciences; Oil sands; Context (archaeology); Panache; Meteorology; Geology; Geography","score_opus":0.014917087419482788,"score_gpt":0.224783218100697,"score_spread":0.20986613068121424,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3117700198","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":[0.9943557,0.00044463726,0.000713369,0.00009485717,0.000014531049,0.000044704557,0.0000023239988,0.0000074923514,0.0043223794],"genre_scores_gemma":[0.9950728,0.00012991657,0.0044009173,0.00008566536,0.000029735507,0.0000086761165,0.000009304115,0.000011614304,0.00025137217],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99891293,0.000039771112,0.00024829924,0.00029465117,0.00031215552,0.00019218029],"domain_scores_gemma":[0.99944705,0.00007102078,0.000111794376,0.00029041324,0.000019853975,0.000059865044],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001180095,0.00016559527,0.00024634958,2.339665e-8,0.00007053267,0.00001504524,0.00015002176,0.00008535776,0.00025770252],"category_scores_gemma":[0.000022145734,0.00013393935,0.00006596371,0.00029967827,0.0005078851,0.00007013819,0.00007960761,0.00012890808,0.0000014630737],"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":[0.00013219652,0.00089352665,0.62294346,0.00038403246,0.00007668968,0.000037940958,0.0011225338,0.0010705316,0.18756855,0.00003314351,0.0002923204,0.18544506],"study_design_scores_gemma":[0.0027394649,0.00017287058,0.44606477,0.00019931745,0.00015759593,0.000045648558,0.0013296878,0.01188145,0.5362668,0.00028149248,0.00028268056,0.0005782415],"about_ca_topic_score_codex":0.000251297,"about_ca_topic_score_gemma":0.000046291036,"teacher_disagreement_score":0.34869823,"about_ca_system_score_codex":0.0000335414,"about_ca_system_score_gemma":0.000034743476,"threshold_uncertainty_score":0.54618883},"labels":[],"label_agreement":null},{"id":"W3118506728","doi":"10.1175/jtech-d-20-0107.1","title":"Changes in TOA SW Fluxes over Marine Clouds When Estimated via Semiphysical Angular Distribution Models","year":2021,"lang":"en","type":"article","venue":"Journal of Atmospheric and Oceanic Technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":9,"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":"Freie Universität Berlin; Langley Research Center; National Aeronautics and Space Administration","keywords":"Zenith; Environmental science; Atmosphere (unit); Cloud fraction; Flux (metallurgy); Atmospheric sciences; Shortwave; Effective radius; Liquid water content; Satellite; Radiative flux; Defense Meteorological Satellite Program; Northern Hemisphere; Cloud cover; Radiative transfer; Cloud top; Meteorology; Remote sensing; Cloud computing; Physics; Geology; Astrophysics; Optics; Astronomy","score_opus":0.006097770400765306,"score_gpt":0.21085702816513696,"score_spread":0.20475925776437165,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3118506728","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":[0.97585064,0.0006900415,0.021679673,0.0013136395,0.00012349726,0.00006816562,0.000002907172,0.000038748298,0.0002326924],"genre_scores_gemma":[0.9827365,0.0005345917,0.016265264,0.00016989636,0.000057600537,0.0000024258215,0.000004761467,0.000017204175,0.00021172673],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987592,0.000036851496,0.00036769852,0.00026139352,0.00024241304,0.00033241833],"domain_scores_gemma":[0.9993957,0.000028163542,0.00023895386,0.00020652225,0.00003285287,0.000097761185],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001531294,0.00018923254,0.00039368676,0.0000012466224,0.000070781294,0.000020376825,0.00021848013,0.00023898362,0.00091057766],"category_scores_gemma":[0.000043201526,0.00016096613,0.00006709259,0.0005598059,0.00024542454,0.00018374943,0.00038630352,0.00036996734,0.000007767015],"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":[0.00019746754,0.0008434155,0.65438557,0.000044244563,0.00014769468,0.001234494,0.00048494732,0.005343691,0.033536367,0.003471512,0.0048931846,0.2954174],"study_design_scores_gemma":[0.003687413,0.0014271236,0.64143443,0.00019102379,0.00021348677,0.0018150447,0.0013204544,0.21141386,0.008806001,0.117783286,0.010896759,0.001011088],"about_ca_topic_score_codex":0.00006021712,"about_ca_topic_score_gemma":0.00008044414,"teacher_disagreement_score":0.29440632,"about_ca_system_score_codex":0.00018990197,"about_ca_system_score_gemma":0.00003120332,"threshold_uncertainty_score":0.9970187},"labels":[],"label_agreement":null},{"id":"W3123197693","doi":"10.3390/atmos12020152","title":"Evolution of Aerosols in the Atmospheric Boundary Layer and Elevated Layers during a Severe, Persistent Haze Episode in a Central China Megacity","year":2021,"lang":"en","type":"article","venue":"Atmosphere","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":16,"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":"National Natural Science Foundation of China; National Oceanic and Atmospheric Administration; Université de Sherbrooke","keywords":"Haze; Aerosol; Atmospheric sciences; HYSPLIT; Environmental science; Troposphere; Planetary boundary layer; Convective Boundary Layer; Daytime; Depolarization ratio; Boundary layer; Climatology; Meteorology; Geology; Physics","score_opus":0.006120843930996668,"score_gpt":0.19745676066704787,"score_spread":0.19133591673605121,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3123197693","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":[0.9962914,0.0009568587,0.00009116722,0.0003888111,0.00007553411,0.00030224278,0.0000051607635,0.000021500233,0.0018673069],"genre_scores_gemma":[0.9973939,0.00010649625,0.0017779665,0.000119259756,0.000020401492,0.00002843771,0.000004194876,0.000020696709,0.00052861904],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99794805,0.00019931482,0.00039688128,0.00048415313,0.0004078054,0.00056380127],"domain_scores_gemma":[0.99935687,0.000038198992,0.00012614181,0.00037000544,0.000011678248,0.00009710465],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00025497942,0.00023914046,0.00030695988,2.6112724e-7,0.00015561121,0.000047535108,0.0002597957,0.00013333843,0.0011333055],"category_scores_gemma":[0.000051143303,0.0001966659,0.00012410904,0.0007950907,0.00025651566,0.0002573906,0.0002283838,0.00030494982,0.000017204306],"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":[0.00006935972,0.00022730567,0.9673407,0.000039161565,0.000020903928,0.00008519459,0.0021153057,0.024202341,0.005213476,0.000099145866,0.00015199535,0.00043509447],"study_design_scores_gemma":[0.0009946974,0.000066855595,0.9852999,0.00006091358,0.000021091466,0.000071369446,0.0030987868,0.009232902,0.00037221276,0.0002543117,0.00028536882,0.00024162132],"about_ca_topic_score_codex":0.0062477146,"about_ca_topic_score_gemma":0.006287576,"teacher_disagreement_score":0.017959153,"about_ca_system_score_codex":0.00049518514,"about_ca_system_score_gemma":0.000060318172,"threshold_uncertainty_score":0.9997798},"labels":[],"label_agreement":null},{"id":"W3125453616","doi":"10.5194/acp-21-17185-2021","title":"Seasonality of the particle number concentration and size distribution: a global analysis retrieved from the network of Global Atmosphere Watch (GAW) near-surface observatories","year":2021,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":77,"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":"Agencia Estatal de Investigación; Staatssekretariat für Bildung, Forschung und Innovation; Agència de Gestió d'Ajuts Universitaris i de Recerca; National Oceanic and Atmospheric Administration; Miljødirektoratet; Environmental Protection Administration, Executive Yuan, R.O.C. Taiwan; Magnus Bergvalls Stiftelse; Ministerio de Asuntos Económicos y Transformación Digital, Gobierno de España; Horizon 2020; North-West University; U.S. Department of Energy; Vetenskapsrådet; National Research Foundation of Korea; Chinese Academy of Meteorological Sciences; Ministerio de Economía y Competitividad; China Meteorological Administration; Generalitat de Catalunya; Commonwealth Scientific and Industrial Research Organisation; Office of Science; Desert Research Institute; Academy of Finland; Ministry of Science and Technology of the People's Republic of China; Horizon 2020 Framework Programme; Région Occitanie Pyrénées-Méditerranée; Korea Meteorological Administration; Svenska Forskningsrådet Formas; National Research Foundation; Helsingin Yliopisto; European Commission; Biological and Environmental Research; Centre National de la Recherche Scientifique; European Regional Development Fund; Ministerstvo Školství, Mládeže a Tělovýchovy","keywords":"Environmental science; Seasonality; Atmospheric sciences; Diel vertical migration; Annual cycle; Aerosol; Atmosphere (unit); Range (aeronautics); Climatology; Meteorology; Statistics; Geography; Physics; Geology; Mathematics","score_opus":0.00544628784616884,"score_gpt":0.2085351799555206,"score_spread":0.20308889210935174,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3125453616","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":[0.9972292,0.0006258048,0.0009295957,0.0004952619,0.000037652433,0.0000724945,0.00018161195,0.000010176233,0.00041816296],"genre_scores_gemma":[0.99680996,0.00008054875,0.0027610136,0.00008041354,0.000056810808,0.0000024050933,0.00002950175,0.0000040313994,0.00017532778],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988809,0.00007063211,0.00024826123,0.00029582766,0.00029996198,0.0002043896],"domain_scores_gemma":[0.9991889,0.00012199574,0.00018116744,0.0003797788,0.000048955055,0.00007917727],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00009716422,0.00015710527,0.00026041878,1.0966801e-12,0.00022839272,0.000043177006,0.00016562092,0.0000835935,0.0010831297],"category_scores_gemma":[0.000035119647,0.00011004575,0.00012311841,0.00093917345,0.0006219789,0.000085801126,0.00020788619,0.00008796406,0.0000017099007],"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":[0.00003388632,0.0000633259,0.99293494,0.000014859874,0.0002162528,0.0000011333777,0.00010717867,0.0034630417,0.0005669252,0.00022565335,0.00038614086,0.0019866636],"study_design_scores_gemma":[0.00025299875,0.0000061413507,0.9829507,0.000016454642,0.00037656445,0.0000018277982,0.00024027938,0.01107095,0.0026895716,0.0017179566,0.0005582491,0.00011829348],"about_ca_topic_score_codex":0.0010338,"about_ca_topic_score_gemma":0.00006614741,"teacher_disagreement_score":0.009984225,"about_ca_system_score_codex":0.00009043576,"about_ca_system_score_gemma":0.000070615664,"threshold_uncertainty_score":0.99983},"labels":[{"model":"gemma","categories":[],"domain":null,"study_design":"observational","genre":"empirical","about_ca_system":false,"about_ca_topic":false,"confidence":"low"},{"model":"gpt","categories":[],"domain":null,"study_design":"observational","genre":"empirical","about_ca_system":false,"about_ca_topic":false,"confidence":"high"}],"label_agreement":"agree"},{"id":"W3126845821","doi":"10.1016/j.renene.2021.02.025","title":"Ground-based validation of aerosol optical depth from CAMS reanalysis project: An uncertainty input on direct normal irradiance under cloud-free conditions","year":2021,"lang":"en","type":"article","venue":"Renewable Energy","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":34,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Impact","funders":"Hellenic Foundation for Research and Innovation; General Secretariat for Research and Technology","keywords":"AERONET; Environmental science; Aerosol; Irradiance; Atmospheric sciences; Calibration; Radiative transfer; Meteorology; Solar irradiance; Atmospheric radiative transfer codes; Remote sensing; Mathematics; Statistics; Geography; Geology","score_opus":0.014925363030974992,"score_gpt":0.23993142694494143,"score_spread":0.22500606391396644,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3126845821","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":[0.94409114,0.000052795385,0.020022325,0.00019402275,0.00017146592,0.00008640153,0.00008768025,0.000065077504,0.035229076],"genre_scores_gemma":[0.99265385,0.000033146844,0.0038994416,0.0004963463,0.00012684711,0.000042920135,0.0006312541,0.000027921642,0.00208828],"study_design_codex":"simulation_or_modeling","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99803346,0.00017245862,0.00034434156,0.00057581556,0.0005248213,0.00034911663],"domain_scores_gemma":[0.9986377,0.00014414763,0.00015821174,0.0008584779,0.000034960245,0.00016653938],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00013047783,0.00022089572,0.00032190033,0.0000060514008,0.00019469304,0.000052544496,0.00033228836,0.00014367314,0.001764651],"category_scores_gemma":[0.00006802516,0.00021055425,0.00014074586,0.00064136536,0.00021210765,0.00020441563,0.00011634209,0.00009107661,0.000019210334],"study_design_candidate":"simulation_or_modeling","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":[0.000041400024,0.0002994475,0.0037255469,0.0000038404764,0.000052680887,0.000015329862,0.000056818917,0.9657944,0.027810542,0.000332149,0.0012851239,0.00058274466],"study_design_scores_gemma":[0.0027289325,0.00073012116,0.02805809,0.000121438585,0.00044205133,0.000010133774,0.0010026773,0.16363741,0.794332,0.0032288702,0.0044005746,0.001307652],"about_ca_topic_score_codex":0.09594638,"about_ca_topic_score_gemma":0.041720748,"teacher_disagreement_score":0.802157,"about_ca_system_score_codex":0.00029200022,"about_ca_system_score_gemma":0.00014126512,"threshold_uncertainty_score":0.9991479},"labels":[],"label_agreement":null},{"id":"W3127203479","doi":"10.5194/acp-2019-611","title":"A new look at the environmental conditions favorable to secondary ice production","year":2019,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada; Environment and Climate Change Canada","funders":"Federal Aviation Administration; Environment and Climate Change Canada; Transport Canada","keywords":"Graupel; Ice crystals; Clear ice; Mesoscale meteorology; Materials science; Drop (telecommunication); Atmospheric sciences; Environmental science; Geology; Meteorology; Sea ice; Climatology; Antarctic sea ice; Arctic ice pack; Geography","score_opus":0.0036921262508780224,"score_gpt":0.18902944325755996,"score_spread":0.18533731700668193,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3127203479","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":[0.8998471,0.000020744837,0.0003105742,0.0020171641,0.0002133141,0.00041010848,0.0000055782266,0.000032313634,0.097143106],"genre_scores_gemma":[0.65962887,0.0000044402245,0.00081958866,0.0012503823,0.000042472988,0.0000130752915,0.0000074338304,0.000008701077,0.33822504],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991395,0.000018664472,0.00010722677,0.00031352168,0.00021165247,0.0002094402],"domain_scores_gemma":[0.9994974,0.0000138715295,0.00003151359,0.0003398727,7.689346e-7,0.000116548414],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00008099566,0.000102126585,0.00007403617,6.515047e-7,0.00020410467,0.000020097881,0.00016263437,0.000032480468,0.21089105],"category_scores_gemma":[0.000003606899,0.0000691991,0.00003948345,0.00009981199,0.00007281787,0.0001634308,0.0002553087,0.00008460924,0.038542353],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026176209,0.00008360135,0.17004403,0.0000031979362,0.000017812594,0.0000017064002,0.0008481048,0.0055970456,0.18372983,0.00016574192,0.6285575,0.010925266],"study_design_scores_gemma":[0.00034688352,0.00017292818,0.43874767,0.000005342189,0.000018854278,0.000034964374,0.0012588867,0.00014137887,0.017161468,0.00032854758,0.54144245,0.00034062398],"about_ca_topic_score_codex":0.00045366673,"about_ca_topic_score_gemma":0.0002672994,"teacher_disagreement_score":0.26870364,"about_ca_system_score_codex":0.00022044926,"about_ca_system_score_gemma":0.000012162078,"threshold_uncertainty_score":0.96220624},"labels":[],"label_agreement":null},{"id":"W3129161549","doi":"10.1002/qj.3996","title":"Representativity of cloud‐profiling radar observations for data assimilation in numerical weather prediction","year":2021,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Acadia University; Environment and Climate Change Canada","funders":"","keywords":"Numerical weather prediction; Remote sensing; Data assimilation; Nadir; Meteorology; Radar; Environmental science; Cloud top; Radiance; Satellite; Profiling (computer programming); Cloud computing; Computer science; Geology; Geography; Physics","score_opus":0.04767254118928195,"score_gpt":0.2762803196747009,"score_spread":0.22860777848541897,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3129161549","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":[0.8989632,0.000063995634,0.09928164,0.0011101161,0.00026941622,0.00014349293,0.000030715164,0.000005756748,0.00013166502],"genre_scores_gemma":[0.93105954,0.0000072578287,0.06855361,0.00015853262,0.00011516999,0.0000043808654,0.0000082086735,0.000006449102,0.000086834785],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985042,0.00024272961,0.00051658374,0.00021707495,0.00034933636,0.00017003846],"domain_scores_gemma":[0.9988968,0.0002738014,0.00040535958,0.0003312037,0.000040612864,0.00005224684],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009883028,0.000095550095,0.00024577373,8.224456e-7,0.00011153355,0.00001575537,0.0004278354,0.000113699534,0.00019556624],"category_scores_gemma":[0.00022195258,0.00005993596,0.0002625503,0.00023327612,0.00013402679,0.00017414399,0.0001344339,0.0002583583,9.0789297e-7],"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":[0.00018683057,0.0006632902,0.9329129,0.000019059586,0.00012666419,0.0000053192257,0.0014484673,0.018758027,0.023821065,0.00025255067,0.005982736,0.015823117],"study_design_scores_gemma":[0.0010673628,0.00071201986,0.8353457,0.000023520113,0.00010737806,0.000011951042,0.0015707911,0.15337515,0.001289914,0.005348629,0.0010174586,0.00013013722],"about_ca_topic_score_codex":0.00004224039,"about_ca_topic_score_gemma":0.000009220639,"teacher_disagreement_score":0.13461712,"about_ca_system_score_codex":0.00008926425,"about_ca_system_score_gemma":0.00003067339,"threshold_uncertainty_score":0.24441174},"labels":[],"label_agreement":null},{"id":"W3130696683","doi":"","title":"Multi-year and Multi-sensor investigations of Aerosol Optical Properties over the Canadian High Arctic","year":2013,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Aerosol; Arctic; Remote sensing; Environmental science; The arctic; Meteorology; Atmospheric sciences; Climatology; Geography; Geology; Oceanography","score_opus":0.021896780752081783,"score_gpt":0.21379156964793225,"score_spread":0.19189478889585046,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3130696683","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":[0.9974272,0.000031685875,0.0000052976898,0.00082873827,0.00006916207,0.00031522877,0.0000033364406,0.00001781652,0.0013014907],"genre_scores_gemma":[0.97885716,0.000006346211,0.020121504,0.00031912865,0.00002387935,0.000028722598,0.000001838498,0.000016054872,0.00062534347],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989586,0.00003410034,0.00024861022,0.00023095953,0.00020762435,0.0003201043],"domain_scores_gemma":[0.99932206,0.00007402431,0.00009825786,0.00021964296,0.000022538818,0.0002635064],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017552552,0.00013398836,0.00012382,0.0000021558044,0.00029406414,0.00007152967,0.00016017084,0.00008481644,0.00011455937],"category_scores_gemma":[0.00035607282,0.000089641486,0.000029131732,0.000085906344,0.0006018953,0.00013494625,0.00008546476,0.00017831211,0.0002289522],"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":[0.0000025449683,0.00007316005,0.9642182,0.000023481542,0.000018497509,0.000004091023,0.0011802498,0.006307904,0.027236538,0.000033979504,0.00046292567,0.0004384142],"study_design_scores_gemma":[0.00023131484,0.000025026407,0.99340856,0.000043386968,0.00001508807,0.0000038481476,0.00038372885,0.004076095,0.0015327787,0.000023740798,0.00011882569,0.0001376116],"about_ca_topic_score_codex":0.8640563,"about_ca_topic_score_gemma":0.6618006,"teacher_disagreement_score":0.20225567,"about_ca_system_score_codex":0.00008317464,"about_ca_system_score_gemma":0.000038753187,"threshold_uncertainty_score":0.3655474},"labels":[],"label_agreement":null},{"id":"W3135672666","doi":"10.1175/jhm-d-20-0147.1","title":"Improvement of Snow Gauge Collection Efficiency through a Knowledge of Solid Precipitation Fall Speed","year":2021,"lang":"en","type":"article","venue":"Journal of Hydrometeorology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":20,"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 du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; National Center for Atmospheric Research","keywords":"Wind speed; Disdrometer; Environmental science; Meteorology; Precipitation; Snow; Rain gauge; Atmospheric sciences; Physics","score_opus":0.010273264410324187,"score_gpt":0.2595931226184646,"score_spread":0.24931985820814043,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3135672666","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":[0.9912889,0.00026756435,0.0042882976,0.00016077794,0.0004605196,0.00009419927,0.000003797291,0.0000033925407,0.0034325442],"genre_scores_gemma":[0.995859,0.00012085939,0.00319927,0.00005291773,0.000043862317,0.0000013734086,0.0000013410246,0.000009242316,0.0007121083],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.998614,0.0000981008,0.0006945443,0.00015475921,0.0002436458,0.00019496016],"domain_scores_gemma":[0.9988398,0.00010003599,0.00076001463,0.00014816332,0.00009685913,0.00005513731],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00038827394,0.00010866275,0.00038475037,0.000008390571,0.000048429163,0.0000037234306,0.00017628689,0.000094786825,0.0011329049],"category_scores_gemma":[0.00015657132,0.00009251801,0.00015566175,0.00047742523,0.0001868907,0.00013823823,0.00010393279,0.00014391825,0.000015415568],"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":[0.0001956921,0.0011780143,0.020718189,0.000040901195,0.00012289081,0.00001708595,0.0037580794,0.0039980505,0.9611653,0.00011851047,0.0019302693,0.006756992],"study_design_scores_gemma":[0.004752415,0.013813894,0.12320557,0.00011811916,0.00035771917,0.0007490791,0.001958416,0.0069205044,0.83493656,0.008059862,0.0046639317,0.00046394582],"about_ca_topic_score_codex":0.0001353168,"about_ca_topic_score_gemma":0.0001350655,"teacher_disagreement_score":0.12622878,"about_ca_system_score_codex":0.00012635111,"about_ca_system_score_gemma":0.00007735463,"threshold_uncertainty_score":0.9997802},"labels":[],"label_agreement":null},{"id":"W3147603295","doi":"10.5194/amt-2020-518-rc1","title":"Comment on amt-2020-518","year":2021,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Canadian Space Agency; Université de Lille; Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Radiance; Remote sensing; Environmental science; Effective radius; Meteorology; Hyperspectral imaging; Radiative transfer; Water vapor; Cloud top; Cloud computing; Overcast; Numerical weather prediction; Computer science; Geology; Physics; Optics; Sky","score_opus":0.017770849905615435,"score_gpt":0.2685183689664801,"score_spread":0.2507475190608647,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3147603295","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00004145346,0.0059819827,0.00015745132,0.33415315,0.0014674363,0.00035837718,0.000036159705,0.000049747407,0.65775424],"genre_scores_gemma":[0.00008565677,0.009364108,0.0013463824,0.21497826,0.0002029458,0.000052329917,0.0002747694,0.00003099219,0.77366453],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9979559,0.000065374916,0.0003131125,0.0006021335,0.00072617945,0.00033728193],"domain_scores_gemma":[0.99896294,0.00004586196,0.0001271382,0.00069577486,0.00000917827,0.00015911456],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00019220034,0.0003410156,0.0004960934,3.9222485e-7,0.00009882223,0.000032567503,0.00044659057,0.00018275944,0.28300834],"category_scores_gemma":[0.000029855488,0.00026139236,0.00022321743,0.00019427024,0.000094268755,0.000027855825,0.0005357929,0.0003875625,0.008976915],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000011208971,0.000082055434,0.00008733728,0.00012876913,0.000016149826,0.00002858498,0.000008695484,0.00001355455,0.0000022123788,0.0000636592,0.9874547,0.012113148],"study_design_scores_gemma":[0.000086087326,0.000071157825,0.00020024634,0.00063832256,0.000048506092,0.0000049792116,0.000016129326,0.000019863077,0.000016210082,0.000034725723,0.9985361,0.00032763503],"about_ca_topic_score_codex":0.0007432805,"about_ca_topic_score_gemma":0.00020149472,"teacher_disagreement_score":0.27403143,"about_ca_system_score_codex":0.00028752585,"about_ca_system_score_gemma":0.000025143134,"threshold_uncertainty_score":0.99998385},"labels":[],"label_agreement":null},{"id":"W3151387854","doi":"","title":"Using Cloud Radar to Retrieve Entrainment Rates in Stratocumulus Clouds","year":2020,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Marine stratocumulus; Cloud computing; Entrainment (biomusicology); Meteorology; Environmental science; Cloud top; Atmospheric sciences; Computer science; Geology; Geography; Operating system","score_opus":0.03504264256974492,"score_gpt":0.27346429801864847,"score_spread":0.23842165544890354,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3151387854","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":[0.96949553,0.00002496911,0.012062489,0.0018735785,0.0001044393,0.00032365174,0.0000026541247,0.00004441742,0.01606828],"genre_scores_gemma":[0.97567266,0.000006451605,0.019057024,0.0049449317,0.000091409565,0.0000051709153,0.0000010641312,0.000015832871,0.00020543176],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99861276,0.000037515623,0.00025604537,0.00038514825,0.00033678432,0.00037173103],"domain_scores_gemma":[0.99947613,0.000019006056,0.000039211656,0.00015738799,0.0000028342913,0.0003054159],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014994627,0.00015812395,0.00017502827,8.237692e-7,0.00006107609,0.000037143687,0.000252227,0.000059180245,0.0071086744],"category_scores_gemma":[0.000030781808,0.0001393339,0.000043443317,0.0005044739,0.00006263075,0.00009831902,0.0002528261,0.00012064608,0.00053179497],"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":[0.00040242865,0.000400538,0.63259524,0.00002854071,0.000042813324,0.00025419676,0.010303541,0.030616138,0.27896386,0.0034584217,0.027748387,0.015185929],"study_design_scores_gemma":[0.007937684,0.0032584132,0.24543467,0.00013154486,0.000110518624,0.0000467888,0.022107713,0.22030078,0.25566888,0.0034931982,0.23640032,0.0051094815],"about_ca_topic_score_codex":0.0006628596,"about_ca_topic_score_gemma":0.00008685751,"teacher_disagreement_score":0.38716054,"about_ca_system_score_codex":0.00021235392,"about_ca_system_score_gemma":0.00001706172,"threshold_uncertainty_score":0.993799},"labels":[],"label_agreement":null},{"id":"W3151538421","doi":"","title":"In situ cloud and aerosol observations in the arctic region during the RadSnowExp campaign","year":2019,"lang":"en","type":"article","venue":"NPARC","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Aerosol; Cloud computing; Meteorology; Arctic; Environmental science; In situ; The arctic; Climatology; Geography; Geology; Computer science; Oceanography","score_opus":0.011587817715934992,"score_gpt":0.20386371689262972,"score_spread":0.19227589917669474,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3151538421","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":[0.9896553,0.000019469302,0.000028397535,0.0028374544,0.000067478264,0.00027967143,2.244925e-7,0.000006786697,0.0071051815],"genre_scores_gemma":[0.9976573,0.000030471447,0.00018475774,0.0008415441,0.000032775988,0.000027459402,4.27019e-7,0.000006190104,0.0012190518],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99929154,0.0000751861,0.00012112426,0.00017302528,0.00015508229,0.00018405147],"domain_scores_gemma":[0.99960023,0.00007966898,0.00003621368,0.00026060405,0.000001776336,0.000021509331],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021041401,0.00007582484,0.000074009,9.286813e-7,0.00009082104,0.000024992993,0.00021281072,0.00003497663,0.00037458894],"category_scores_gemma":[0.000018796003,0.000044251694,0.000019319108,0.00021988913,0.00009725071,0.00012485201,0.00009360828,0.00015353078,0.000089171095],"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":[0.000013404299,0.00004542936,0.9527421,0.000009010481,0.0000018137943,0.0000104998435,0.0052844514,0.00041124123,0.039755803,0.0006054284,0.0008384648,0.00028237526],"study_design_scores_gemma":[0.00031540735,0.000024683883,0.9941755,0.0000146252105,0.0000026712778,0.000014605695,0.0017977384,0.0004109945,0.0002840641,0.0020069266,0.00086413464,0.00008865505],"about_ca_topic_score_codex":0.00027148833,"about_ca_topic_score_gemma":0.0006638009,"teacher_disagreement_score":0.041433416,"about_ca_system_score_codex":0.0000752596,"about_ca_system_score_gemma":0.0000045213496,"threshold_uncertainty_score":0.41014862},"labels":[],"label_agreement":null},{"id":"W3153962425","doi":"10.5194/amt-2020-518","title":"An observing system simulation experiment (OSSE)-basedassessment of the retrieval of above-cloud temperature and watervapor using hyperspectral infrared sounder","year":2021,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; McGill University","funders":"Canadian Space Agency; Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Water vapor; Environmental science; Remote sensing; Hyperspectral imaging; Infrared; Meteorology; Convective storm detection; Cloud computing; Humidity; Atmospheric sciences; Cloud top; Convection; Infrared window; Geology; Computer science; Physics; Optics","score_opus":0.016261773419048664,"score_gpt":0.2628166110297489,"score_spread":0.24655483761070024,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3153962425","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":[0.9976137,0.00008643262,0.0010582776,0.00004372099,0.00013157699,0.00015894034,0.0000038392245,0.000015592092,0.0008878951],"genre_scores_gemma":[0.9933566,0.0000025202605,0.006240094,0.000059515452,0.000032813554,0.0000013479406,0.0000025294028,0.000011583489,0.00029301745],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.998886,0.00008313861,0.00027725252,0.00025067077,0.00034364226,0.00015933586],"domain_scores_gemma":[0.9994213,0.00002605049,0.00012567433,0.00033985308,0.000027989763,0.000059146085],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014195278,0.00012248811,0.00017936016,9.837049e-7,0.00012207453,0.000033598288,0.0001319753,0.00007564392,0.0004793011],"category_scores_gemma":[0.000009237976,0.00008193906,0.00005842407,0.00019045472,0.000108003755,0.00015044042,0.00014216117,0.00007304438,8.2702115e-7],"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":[0.000024801506,0.00008721134,0.059018243,0.000042946805,0.00001627499,0.000002743497,0.0011559955,0.07173446,0.8675866,0.00028217662,0.0000124561775,0.000036056805],"study_design_scores_gemma":[0.0006723747,0.00013303838,0.13138135,0.00010511823,0.000053621035,0.0000133556305,0.017435243,0.1642705,0.6855543,0.000081864804,0.000044130367,0.00025504272],"about_ca_topic_score_codex":0.000195831,"about_ca_topic_score_gemma":0.000015125334,"teacher_disagreement_score":0.18203229,"about_ca_system_score_codex":0.00019079044,"about_ca_system_score_gemma":0.000039194056,"threshold_uncertainty_score":0.5248011},"labels":[],"label_agreement":null},{"id":"W3155173625","doi":"10.5194/amt-2020-470-ac4","title":"Reply on CC1","year":2021,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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 Saskatchewan","funders":"Universität Bremen; Academy of Finland; National Aeronautics and Space Administration; European Space Agency; Freie Hansestadt Bremen; Canadian Space Agency; Nuclear Safety and Security Commission; Deutsche Forschungsgemeinschaft","keywords":"Radiative transfer; Scattering; Refraction; Tangent; Span (engineering); Scalar (mathematics); Optics; Physics; Wavelength; Computational physics; Monte Carlo method; Polarization (electrochemistry); Mathematics; Geometry; Statistics; Chemistry; Engineering; Structural engineering","score_opus":0.01903858026084979,"score_gpt":0.2686507312348429,"score_spread":0.2496121509739931,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3155173625","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0000568879,0.006576205,0.000083458646,0.07918371,0.0012426786,0.00021797243,0.000016360884,0.000058522903,0.9125642],"genre_scores_gemma":[0.000057693498,0.0056473557,0.0011212095,0.09019508,0.00017965729,0.000025644733,0.0001226453,0.000026673419,0.902624],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9983614,0.00003664769,0.00023759424,0.0005681271,0.00054849684,0.0002477093],"domain_scores_gemma":[0.99905217,0.000028881574,0.00010129359,0.0007049931,0.0000074777145,0.00010518733],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00015275131,0.00024301156,0.00036711677,2.9800006e-7,0.00006222884,0.000021294907,0.00032095445,0.00012923457,0.25590402],"category_scores_gemma":[0.00005833794,0.00018236741,0.00017833039,0.00016829789,0.000072152325,0.000025543159,0.00030022883,0.00029773172,0.008114563],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[6.7869877e-7,0.000032690503,0.000053042608,0.000090476366,0.0000075784037,0.000023586506,0.0000048019333,0.000008150867,0.0000030020046,0.000026449163,0.98645866,0.01329088],"study_design_scores_gemma":[0.000044785153,0.000041865376,0.00024545784,0.0005174212,0.000029669072,0.000005987829,0.000006273614,0.000007809594,0.000015862592,0.000025476025,0.9988194,0.00024000477],"about_ca_topic_score_codex":0.0009443089,"about_ca_topic_score_gemma":0.00013469574,"teacher_disagreement_score":0.24778946,"about_ca_system_score_codex":0.00014557259,"about_ca_system_score_gemma":0.000025064808,"threshold_uncertainty_score":0.9926577},"labels":[],"label_agreement":null},{"id":"W3156231661","doi":"10.1007/s10546-021-00609-1","title":"Discriminating Fog and Rain at the Kilometre Scale Using the Extinction from Collocated Infrared and Microwave Scintillometers","year":2021,"lang":"en","type":"article","venue":"Boundary-Layer Meteorology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ontario Tech University; Environment and Climate Change Canada","funders":"Office of Naval Research","keywords":"Visibility; Scintillometer; Attenuation; Microwave; Environmental science; Remote sensing; Wavelength; Extinction (optical mineralogy); Infrared; Meteorology; Daytime; Atmospheric sciences; Physics; Optics; Geology; Turbulence","score_opus":0.015492167364406825,"score_gpt":0.23623966690966827,"score_spread":0.22074749954526146,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3156231661","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":[0.9933063,0.0013398734,0.0019929726,0.0014678844,0.0002525918,0.00019555587,0.000013454519,0.000021417452,0.0014099617],"genre_scores_gemma":[0.99169415,0.00005825091,0.0054132007,0.0013632783,0.00005357421,0.000010953006,0.000014258969,0.000021985397,0.0013703443],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.998399,0.00031609242,0.00024566177,0.00049430755,0.00020029033,0.00034463598],"domain_scores_gemma":[0.9991347,0.00029574367,0.0001339317,0.00033479338,0.000017269082,0.0000835497],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004179651,0.00019287739,0.00022653906,0.0000040537466,0.0010923775,0.0001431586,0.00016192725,0.00011739572,0.001344601],"category_scores_gemma":[0.000119990655,0.00012305734,0.00006505369,0.00037750567,0.0012854278,0.00013414891,0.0007444431,0.0001960282,0.000020741922],"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":[0.00012383313,0.00004602075,0.24946679,0.000010740005,0.00014224187,0.000036216225,0.0051863515,0.00031342352,0.6934643,0.000034344605,0.0015735363,0.049602203],"study_design_scores_gemma":[0.0024656802,0.00036040804,0.8492941,0.00003522302,0.0006347844,0.0006353131,0.011106333,0.021644495,0.038847726,0.008264537,0.065761894,0.00094945147],"about_ca_topic_score_codex":0.00084335357,"about_ca_topic_score_gemma":0.0019722716,"teacher_disagreement_score":0.6546166,"about_ca_system_score_codex":0.00014164785,"about_ca_system_score_gemma":0.000030913656,"threshold_uncertainty_score":0.9995683},"labels":[],"label_agreement":null},{"id":"W3156734278","doi":"10.5194/egusphere-egu2020-5653","title":"Lidar observations of volcanic aerosol over the UK since June 2019","year":2020,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"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":"Natural Environment Research Council; Sight Research UK","keywords":"Stratosphere; Aerosol; Lidar; Volcano; Troposphere; Atmospheric sciences; Radiosonde; Backscatter (email); Environmental science; Plume; Extinction (optical mineralogy); Vulcanian eruption; Meteorology; Geology; Mineralogy; Remote sensing; Physics; Seismology","score_opus":0.017844818918293412,"score_gpt":0.21561527834477615,"score_spread":0.19777045942648275,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3156734278","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":[0.9793064,0.000043611482,0.0023254165,0.007725356,0.00008220752,0.00015461663,0.00000642952,0.000028880577,0.010327105],"genre_scores_gemma":[0.9879436,0.000018649424,0.0014950752,0.003686188,0.000034544697,0.000004702484,0.0000019607671,0.0000076064293,0.006807694],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993132,0.00001574749,0.00015528756,0.00016229099,0.00021415543,0.00013935365],"domain_scores_gemma":[0.9996226,0.000034642973,0.000061586725,0.00020979371,0.0000048901834,0.000066514236],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00005183538,0.00007966199,0.000091373164,1.5328744e-7,0.00008586077,0.000011630455,0.00028232063,0.000031610078,0.009392318],"category_scores_gemma":[0.00002417277,0.000049993185,0.000050892482,0.00024153317,0.00014924725,0.00007972799,0.00018290363,0.00007288696,0.00046520546],"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":[0.00002119137,0.000096192125,0.52895844,0.000008951158,0.000027656813,0.000002441893,0.0014386714,0.002657315,0.13760705,0.00365256,0.32456407,0.0009654408],"study_design_scores_gemma":[0.00033156946,0.00011685584,0.93901145,0.000005914531,0.000025429685,0.0000010715662,0.00038782283,0.0056458083,0.005182064,0.00013812112,0.048923958,0.00022990287],"about_ca_topic_score_codex":0.00070061686,"about_ca_topic_score_gemma":0.0003486248,"teacher_disagreement_score":0.410053,"about_ca_system_score_codex":0.0000226196,"about_ca_system_score_gemma":0.000010664105,"threshold_uncertainty_score":0.99151325},"labels":[],"label_agreement":null},{"id":"W3156784097","doi":"10.1021/acsearthspacechem.1c00034","title":"Effects of Inorganic Acids and Organic Solutes on the Ice Nucleating Ability and Surface Properties of Potassium-Rich Feldspar","year":2021,"lang":"en","type":"article","venue":"ACS Earth and Space Chemistry","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":46,"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 British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Vetenskapsrådet","keywords":"Feldspar; Chemistry; Dissolution; Carboxylic acid; Mineral; Potassium; Amino acid; Ice nucleus; Mineralogy; Inorganic chemistry; Nucleation; Organic chemistry; Materials science; Biochemistry; Metallurgy","score_opus":0.0048452783248652985,"score_gpt":0.16546417934263027,"score_spread":0.16061890101776496,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3156784097","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":[0.9978079,0.0012022556,0.0000044468084,0.00037887698,0.000008816531,0.00007315463,0.0000013423384,0.000008048776,0.0005151347],"genre_scores_gemma":[0.99906087,0.0002575252,0.00018286616,0.000051964456,0.000008882261,0.0000011739196,3.9801762e-7,0.000007843055,0.0004284884],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9993762,0.000027214013,0.00010902137,0.00021923719,0.00012979162,0.00013855362],"domain_scores_gemma":[0.99958414,0.00010830978,0.00006857229,0.0001667769,0.000012673399,0.000059549646],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001046498,0.00010786091,0.00015423619,2.648024e-7,0.0001056088,0.000018723164,0.00006506321,0.000065852146,0.0001509075],"category_scores_gemma":[0.00018258716,0.00007438777,0.000013990131,0.00009899415,0.00032816606,0.000045213306,0.00020044799,0.00011098015,0.0000016619487],"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":[0.000007460798,0.000027395065,0.10175465,0.00019027146,0.00000851403,0.0000012985545,0.00052977336,0.0000064374453,0.8971881,0.0000036414585,0.000025248411,0.0002571809],"study_design_scores_gemma":[0.00015872774,0.00003246451,0.08713829,0.000044040775,0.000015789208,0.0000067297265,0.0007567639,0.00006498601,0.9116525,0.000016090129,0.000034231747,0.00007939839],"about_ca_topic_score_codex":0.00006094904,"about_ca_topic_score_gemma":0.000014808437,"teacher_disagreement_score":0.014616369,"about_ca_system_score_codex":0.000008077161,"about_ca_system_score_gemma":0.000015609692,"threshold_uncertainty_score":0.3033445},"labels":[],"label_agreement":null},{"id":"W3157318702","doi":"","title":"Cloud fraction statistics derived from 34-months of high spectral resolution lidar data acquired at Eureka, Canada.","year":2008,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Fraction (chemistry); Remote sensing; Lidar; High resolution; Environmental science; Cloud computing; Statistics; Geography; Computer science; Mathematics; Chemistry","score_opus":0.018135883820400118,"score_gpt":0.21959161074700534,"score_spread":0.2014557269266052,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3157318702","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":[0.9952378,0.00009624792,0.0004857219,0.00013949697,0.0005470174,0.00015661414,0.00036959452,0.00004278438,0.0029247105],"genre_scores_gemma":[0.98320884,0.00008086302,0.015592072,0.00012454418,0.00020905964,0.000003040173,0.00034448682,0.000027384525,0.00040969058],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99785185,0.00006724639,0.00049766497,0.00053195754,0.000638171,0.00041312736],"domain_scores_gemma":[0.9984666,0.00021165184,0.0004439915,0.0006821002,0.000020789656,0.0001748739],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020874008,0.00021116015,0.00026197868,0.0000019155991,0.00032389874,0.000014201455,0.00046905022,0.000114016744,0.00019482363],"category_scores_gemma":[0.00027694297,0.00021520183,0.000027342488,0.00011953121,0.00019312615,0.00020252277,0.0003457934,0.00014657858,0.00009024296],"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":[0.0003163991,0.00026318376,0.8127082,0.000024317904,0.00009768904,0.00039292875,0.00063946785,0.03370021,0.057071995,0.000017645636,0.092817396,0.0019505691],"study_design_scores_gemma":[0.00035377408,0.000058424215,0.98576957,0.000029433802,0.00004067643,0.00001188046,0.00013465366,0.0021329308,0.006730508,0.000087463726,0.004389411,0.00026127585],"about_ca_topic_score_codex":0.9530209,"about_ca_topic_score_gemma":0.9215836,"teacher_disagreement_score":0.17306137,"about_ca_system_score_codex":0.000583636,"about_ca_system_score_gemma":0.000122876,"threshold_uncertainty_score":0.8775676},"labels":[],"label_agreement":null},{"id":"W3160585888","doi":"10.5194/egusphere-egu21-1673","title":"Evaluation of a numerically efficient aerosol activation scheme by using worldwide cloud data from multiple field campaigns in continental and marine regions","year":2021,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","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":"Environment and Climate Change Canada","funders":"","keywords":"Aerosol; Environmental science; Meteorology; Atmospheric sciences; Cloud computing; Relative humidity; Physics; Computer science","score_opus":0.04111412394249388,"score_gpt":0.28159289536125626,"score_spread":0.2404787714187624,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3160585888","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":[0.9784146,0.000027872187,0.019923447,0.00023743557,0.000044892626,0.00018503118,0.000018795892,0.000009559478,0.0011383945],"genre_scores_gemma":[0.98636335,0.0000074712857,0.013157803,0.00017353454,0.00001712754,0.0000057721772,0.00013735646,0.0000070390906,0.00013055014],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99877167,0.000087949644,0.00023123587,0.0003475367,0.0004247614,0.00013686351],"domain_scores_gemma":[0.9993535,0.00013694091,0.00009487892,0.00034187126,0.00002273793,0.00005002438],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00032530865,0.000092658636,0.00013639321,0.0000014341383,0.000051393985,0.000016637428,0.00013323223,0.000048590486,0.0032068694],"category_scores_gemma":[0.00031755277,0.00008688461,0.000017940838,0.00022189671,0.00006244469,0.000116589,0.0005200305,0.00008111385,0.000005062184],"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":[0.000042873806,0.00037519028,0.44613194,0.0000033494323,0.000021499092,0.0000021120627,0.00030532642,0.003914894,0.5397174,0.000008848395,0.0019568666,0.0075197094],"study_design_scores_gemma":[0.0012719479,0.000029945137,0.047013063,0.000030964784,0.000045577286,0.000002083025,0.0011600207,0.903051,0.046990484,0.00006061201,0.00016520554,0.00017909624],"about_ca_topic_score_codex":0.0064445143,"about_ca_topic_score_gemma":0.0020351594,"teacher_disagreement_score":0.8991361,"about_ca_system_score_codex":0.00010480143,"about_ca_system_score_gemma":0.00003070525,"threshold_uncertainty_score":0.9977043},"labels":[],"label_agreement":null},{"id":"W3161149806","doi":"10.5194/amt-2021-139","title":"Canadian biomass burning aerosols observations from a multi-wavelength Raman polarization lidar and a ceilometer in Finland","year":2021,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"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":"Academy of Finland; National Oceanic and Atmospheric Administration; The Ministry of Economic Affairs and Employment; National Aeronautics and Space Administration","keywords":"Depolarization ratio; Lidar; AERONET; Aerosol; Mass concentration (chemistry); Ceilometer; Environmental science; Plume; Atmospheric sciences; Troposphere; Wavelength; Meteorology; Chemistry; Remote sensing; Optics; Physics; Geology","score_opus":0.018432766688517,"score_gpt":0.21236984813374887,"score_spread":0.19393708144523186,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3161149806","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":[0.9946002,0.000044268214,0.0029768052,0.00079781725,0.000044457545,0.00010009263,0.0000185594,0.000013633266,0.0014041859],"genre_scores_gemma":[0.9696748,0.000010219424,0.026892575,0.0006110807,0.000015468904,0.000009052534,0.000045311157,0.000010919421,0.0027305377],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99915045,0.00003998587,0.00016438623,0.00029244873,0.00011004637,0.00024270065],"domain_scores_gemma":[0.99960345,0.00003633026,0.000032517404,0.00014937842,0.0000069968155,0.00017133092],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00007218026,0.00010507479,0.0001120167,0.0000031402285,0.00013342508,0.00007302414,0.00007306888,0.00008191341,0.0025171652],"category_scores_gemma":[0.000048921924,0.00009935203,0.000020655812,0.00035805395,0.000040355782,0.00017521944,0.00008716622,0.00008723696,0.00007225851],"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":[0.0000011804698,0.00002289081,0.98114085,0.0000013341142,0.000004758451,0.000019595283,0.0004742087,0.00003148026,0.016747868,0.000023125513,0.00007424598,0.0014584792],"study_design_scores_gemma":[0.00037003105,0.000011306391,0.9874612,0.000009763112,0.0000056971853,0.000002416226,0.00033615445,0.009341962,0.00069866684,0.00007756141,0.001540542,0.00014468288],"about_ca_topic_score_codex":0.35274938,"about_ca_topic_score_gemma":0.59770745,"teacher_disagreement_score":0.24495806,"about_ca_system_score_codex":0.00015516183,"about_ca_system_score_gemma":0.000046725207,"threshold_uncertainty_score":0.99839467},"labels":[],"label_agreement":null},{"id":"W3161243839","doi":"","title":"Atmospheric Height by Twilight's Glow","year":2010,"lang":"en","type":"article","venue":"Journal of the Royal Astronomical Society of Canada","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Twilight; Environmental science; Atmospheric sciences; Meteorology; Astronomy; Geography; Geology; Physics","score_opus":0.0013061450389628012,"score_gpt":0.14784528957332413,"score_spread":0.14653914453436132,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3161243839","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":[0.9956395,0.00004157792,0.00026031295,0.0025637224,0.00053539313,0.000046467572,0.0000053223125,0.000002001815,0.0009056932],"genre_scores_gemma":[0.9868094,9.4158804e-7,0.010491942,0.0002746631,0.00014187461,5.948146e-7,2.2941138e-7,0.00001002302,0.0022703432],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9988227,0.000023047582,0.00035705173,0.0001077087,0.00043424932,0.00025523588],"domain_scores_gemma":[0.9991897,0.000037851078,0.00038183198,0.00017819507,0.000014567778,0.00019787622],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00018282319,0.000120593395,0.00021863171,8.237924e-8,0.00012188109,0.000012501868,0.00058702537,0.000067003966,0.0025456743],"category_scores_gemma":[0.0000139765025,0.00007599404,0.0003073381,0.00006814843,0.00023914094,0.000056459576,0.00015371894,0.00042503636,0.0000033244833],"study_design_candidate":"not_applicable","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":[0.000021858357,0.00006833224,0.16446453,0.00000338453,0.00006490505,3.498653e-7,0.00005637123,0.018836606,0.0051050247,0.000007634884,0.80819076,0.0031802591],"study_design_scores_gemma":[0.00094398437,0.0001649237,0.5237734,0.000017621554,0.00006997539,0.0000059986496,0.00031354118,0.019657992,0.0067063193,0.00009636155,0.44791952,0.00033036762],"about_ca_topic_score_codex":0.050749253,"about_ca_topic_score_gemma":0.02984459,"teacher_disagreement_score":0.36027122,"about_ca_system_score_codex":0.0002923473,"about_ca_system_score_gemma":0.0002255602,"threshold_uncertainty_score":0.9983661},"labels":[],"label_agreement":null},{"id":"W3162233016","doi":"10.1175/jas-d-20-0377.1","title":"Climatological sensitivities of shallow-cumulus bulk entrainment in continental and oceanic locations","year":2021,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","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":"McGill University","funders":"","keywords":"Entrainment (biomusicology); Cloud base; Environmental science; Atmospheric sciences; Mass flux; Cloud top; Climatology; Atmosphere (unit); Geology; Cloud computing; Meteorology; Physics","score_opus":0.009981833819039608,"score_gpt":0.2268118174679821,"score_spread":0.2168299836489425,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3162233016","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":[0.9954844,0.0004660725,0.000084211264,0.0015563442,0.00019596466,0.00005186545,7.714938e-7,0.000002369488,0.002158016],"genre_scores_gemma":[0.9941534,0.00013335762,0.0052381796,0.00030040886,0.000018615701,6.7176427e-7,5.963744e-8,0.0000028197944,0.00015249933],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987511,0.00009542575,0.00037093917,0.00014618538,0.00044721176,0.00018915508],"domain_scores_gemma":[0.99940735,0.000118125055,0.00029189998,0.000106072504,0.000018115279,0.00005845667],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005399844,0.00008734716,0.00021024153,4.7671404e-7,0.00013153492,0.000029485214,0.00027842767,0.000034268487,0.00046501332],"category_scores_gemma":[0.00012013547,0.000052471158,0.00008346859,0.00042498263,0.0009048792,0.00016302356,0.0002470652,0.00011498609,0.0000024580668],"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":[0.00001666943,0.00020817127,0.9725319,0.000006914644,0.000014850204,0.00005226389,0.0010638635,0.0070879557,0.016309781,0.00045481842,0.00036067946,0.0018921228],"study_design_scores_gemma":[0.00059863273,0.00022728255,0.9686977,0.00009463919,0.0000322436,0.0007007843,0.008782443,0.014102788,0.0045295847,0.0014142822,0.00065112894,0.0001684802],"about_ca_topic_score_codex":0.000052197745,"about_ca_topic_score_gemma":0.00005257866,"teacher_disagreement_score":0.011780197,"about_ca_system_score_codex":0.000065283595,"about_ca_system_score_gemma":0.00006128633,"threshold_uncertainty_score":0.509157},"labels":[],"label_agreement":null},{"id":"W3163652488","doi":"10.5194/acp-21-14039-2021","title":"Environmental sensitivities of shallow-cumulus dilution – Part 2: Vertical wind profile","year":2021,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Department of Energy, Labor and Economic Growth","keywords":"Wind shear; Dilution; Thermal wind; Atmospheric sciences; Geostrophic wind; Entrainment (biomusicology); Environmental science; Meteorology; Wind speed; Geology; Wind stress; Wind direction; Climatology; Physics","score_opus":0.004792712419373721,"score_gpt":0.1841674473150104,"score_spread":0.17937473489563666,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3163652488","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":[0.98619384,0.00012022328,0.0005372033,0.000041883966,0.000034540957,0.00004938843,0.000014769579,0.00001701167,0.012991133],"genre_scores_gemma":[0.99231267,0.00007655978,0.0032102088,0.000071254246,0.00010052084,0.000004176801,0.000028237426,0.000013327684,0.0041830167],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9990964,0.000020278296,0.00016497348,0.0002956047,0.000213817,0.00020890853],"domain_scores_gemma":[0.9996218,0.000032814274,0.00003962656,0.0002071747,0.0000042762963,0.000094322255],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000041863765,0.0001517693,0.0001797504,5.068774e-9,0.000094451665,0.000013575965,0.0000622535,0.00007684633,0.0072973296],"category_scores_gemma":[0.0000081994995,0.00015231402,0.00006558988,0.000090739835,0.00035913446,0.000100803176,0.00013830155,0.000104086175,0.00005195255],"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":[0.00005752087,0.0006217775,0.118062735,0.00010833853,0.00007631294,0.00006318872,0.0007985596,0.0015543174,0.720414,0.000095897674,0.0010624607,0.15708488],"study_design_scores_gemma":[0.001268434,0.00011748235,0.19512925,0.00007812911,0.0001598184,0.00010784151,0.0019709463,0.04219272,0.7412393,0.0011912643,0.015564154,0.0009806373],"about_ca_topic_score_codex":0.000026741674,"about_ca_topic_score_gemma":0.0000012796684,"teacher_disagreement_score":0.15610425,"about_ca_system_score_codex":0.000055496195,"about_ca_system_score_gemma":0.000015708343,"threshold_uncertainty_score":0.99361014},"labels":[],"label_agreement":null},{"id":"W3165832035","doi":"10.1177/11786302211018390","title":"Global Health Impacts of Dust Storms: A Systematic Review","year":2021,"lang":"en","type":"review","venue":"Environmental Health Insights","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":130,"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":"Storm; Scopus; Environmental health; Public health; Natural disaster; Health impact assessment; Medicine; Environmental science; Geography; MEDLINE; Meteorology; Political science","score_opus":0.02186806306578744,"score_gpt":0.32755181233718456,"score_spread":0.30568374927139713,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3165832035","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000030589985,0.99456185,0.000057424222,0.00012222523,0.00028130595,0.004239231,0.00021516318,0.00004019288,0.00045203642],"genre_scores_gemma":[0.00018759236,0.99567604,0.00043199648,0.0026268337,0.00006154412,0.00024277419,0.0003130898,0.00007841822,0.00038170908],"study_design_codex":"systematic_review","study_design_gemma":"systematic_review","domain_scores_codex":[0.99298865,0.0011519513,0.0028527924,0.0009813202,0.001125239,0.0009000457],"domain_scores_gemma":[0.9948389,0.00008738458,0.0029328195,0.0012753598,0.0000027147655,0.0008628147],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0007452849,0.00087921065,0.005969851,0.000005956962,0.0002989855,0.000020613134,0.0006992308,0.00028842688,0.0023124353],"category_scores_gemma":[0.00003816081,0.0006469119,0.0008443577,0.00064489554,0.00031342093,0.00015853459,0.00059787824,0.00042208083,0.0008500247],"study_design_candidate":"systematic_review","study_design_consensus":"systematic_review","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000128051,0.00032703936,0.000050777686,0.88165337,0.00011592112,0.000024952295,0.0001974727,0.000001924265,4.8752945e-8,0.000043097614,0.00786469,0.109719425],"study_design_scores_gemma":[0.00014794883,0.0003213527,0.00011016606,0.50306606,0.0003997388,0.00016041927,0.000090740046,0.0000029636471,1.05431155e-7,0.000011535402,0.49518162,0.0005073521],"about_ca_topic_score_codex":0.0008571955,"about_ca_topic_score_gemma":0.00024148637,"teacher_disagreement_score":0.48731694,"about_ca_system_score_codex":0.0061537223,"about_ca_system_score_gemma":0.0005455029,"threshold_uncertainty_score":0.99992794},"labels":[],"label_agreement":null},{"id":"W3165951392","doi":"10.5194/egusphere-egu21-11379","title":"Aerosol classification using sun photometer and lidar data within a machine learning algorithm-a possible nowcasting application","year":2021,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Angstrom exponent; AERONET; Aerosol; Lidar; Sun photometer; Environmental science; Algorithm; Remote sensing; Meteorology; Single-scattering albedo; Computer science; Geography","score_opus":0.04272733161468485,"score_gpt":0.273703794561987,"score_spread":0.23097646294730217,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3165951392","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":[0.6345922,0.00009360166,0.36202893,0.00009133019,0.000041463132,0.00013805184,0.000008472326,0.00005384881,0.0029521484],"genre_scores_gemma":[0.8047661,0.000023321552,0.19314823,0.0001373387,0.000039052095,0.000008053219,0.00009974447,0.000018990142,0.001759151],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9987299,0.00005261577,0.00022710298,0.0005603656,0.00022815415,0.0002019062],"domain_scores_gemma":[0.99929804,0.000035156794,0.0001256958,0.0004414912,0.0000103171715,0.00008929605],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002882756,0.00012999382,0.00012498835,0.0000017339675,0.00027917445,0.000098036566,0.00019825817,0.00006440725,0.0006628343],"category_scores_gemma":[0.00004892307,0.0001182824,0.00001757274,0.00032820637,0.000089901776,0.00035165757,0.00054657826,0.00016690107,0.00006642385],"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":[0.000009344921,0.00010593006,0.23321731,0.000015381784,0.000021053296,0.000011520679,0.0005131407,0.0010724162,0.6496382,0.000052037525,0.00007737083,0.11526633],"study_design_scores_gemma":[0.00019813952,0.000020263506,0.011141597,0.00000923968,0.000021777341,0.000047474055,0.0004250711,0.9780867,0.0085052615,0.000030109031,0.0013329209,0.00018143826],"about_ca_topic_score_codex":0.0008460605,"about_ca_topic_score_gemma":0.00017397974,"teacher_disagreement_score":0.9770143,"about_ca_system_score_codex":0.00006788447,"about_ca_system_score_gemma":0.000018667393,"threshold_uncertainty_score":0.7257571},"labels":[],"label_agreement":null},{"id":"W3171730784","doi":"10.5194/acp-21-13593-2021","title":"Supercooled liquid water and secondary ice production in Kelvin–Helmholtz instability as revealed by radar Doppler spectra observations","year":2021,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"China Scholarship Council; Horizon 2020; Academy of Finland","keywords":"Supercooling; Drizzle; Ice crystals; Ice nucleus; Atmospheric sciences; Instability; Precipitation; Mechanics; Geology; Nucleation; Meteorology; Physics; Thermodynamics","score_opus":0.006635968061423851,"score_gpt":0.19571659884118112,"score_spread":0.18908063077975726,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3171730784","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":[0.99401265,0.0002644525,0.000093991745,0.00070515944,0.00004385024,0.0001356435,0.00000891487,0.000030150082,0.004705163],"genre_scores_gemma":[0.9865935,0.00028097833,0.005857505,0.00031050429,0.00010491297,0.000026172416,0.00009666659,0.000020052903,0.006709719],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99869376,0.000038385864,0.00023854313,0.0005770186,0.00016941671,0.00028288603],"domain_scores_gemma":[0.99949014,0.000025749217,0.00003792206,0.0003158816,0.00001690283,0.000113381044],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00012752795,0.00020541751,0.0002170747,1.78309e-8,0.000165517,0.000038306487,0.000090525886,0.00010076968,0.003861949],"category_scores_gemma":[0.000024938985,0.00018522321,0.00003881147,0.00022944213,0.00023738033,0.00029756757,0.00013794389,0.00025283865,0.000020504944],"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":[0.000078031204,0.00032250883,0.057835426,0.00012630799,0.000022334481,0.000015673255,0.0012877749,0.00013069753,0.9229271,0.00001544629,0.001682128,0.015556612],"study_design_scores_gemma":[0.0017538174,0.00014620429,0.1543928,0.00006593362,0.00008178667,0.00014270896,0.0016871573,0.0014041506,0.7960926,0.0031366795,0.039893523,0.0012025934],"about_ca_topic_score_codex":0.00031876884,"about_ca_topic_score_gemma":0.0000329705,"teacher_disagreement_score":0.12683439,"about_ca_system_score_codex":0.00010110466,"about_ca_system_score_gemma":0.000035660556,"threshold_uncertainty_score":0.9970487},"labels":[],"label_agreement":null},{"id":"W3173293621","doi":"10.5194/amt-14-6885-2021","title":"Retrieving microphysical properties of concurrent pristine ice and snow using polarimetric radar observations","year":2021,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"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":"European Research Council; Office of Science; Natural Environment Research Council; U.S. Department of Energy; Met Office; University of Leeds; Sight Research UK","keywords":"Snow; Polarimetry; Environmental science; Radar; Remote sensing; Precipitation; Ice cloud; Meteorology; Atmospheric sciences; Scattering; Geology; Cloud computing; Computer science; Geography; Physics; Optics","score_opus":0.05997204233692078,"score_gpt":0.23517152805302607,"score_spread":0.1751994857161053,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3173293621","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":[0.9545839,0.0023386045,0.0417602,0.00013759814,0.00007879166,0.00036530616,0.0000025138604,0.00012807795,0.0006050503],"genre_scores_gemma":[0.83729094,0.00014455453,0.16228345,0.00010643241,0.000034381515,0.000012995017,0.0000018374473,0.000022408649,0.000103025035],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9980909,0.00009993491,0.00042343768,0.0004047164,0.0007058539,0.00027511205],"domain_scores_gemma":[0.99921095,0.000024256042,0.00021809607,0.00031368705,0.00013641261,0.00009662322],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004008316,0.00021796998,0.00031990238,7.983521e-7,0.00018048387,0.000038308863,0.00017965371,0.00008410567,0.00016163188],"category_scores_gemma":[0.0003075027,0.0001931096,0.00007612158,0.0008577169,0.00025507563,0.00017832973,0.0002904645,0.0001590169,0.000003776897],"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":[0.000009560017,0.00019013023,0.04774872,0.000051852025,0.000030971125,0.0000047185886,0.000119114346,0.0000130233675,0.92618555,0.00007430705,0.0003138692,0.025258187],"study_design_scores_gemma":[0.00028762565,0.00017545007,0.06554842,0.00032858583,0.00012026702,0.000020879423,0.00019318446,0.001548894,0.9247272,0.000102645085,0.006496625,0.00045020288],"about_ca_topic_score_codex":0.0008647861,"about_ca_topic_score_gemma":0.000022012116,"teacher_disagreement_score":0.120523244,"about_ca_system_score_codex":0.00028440892,"about_ca_system_score_gemma":0.00007872383,"threshold_uncertainty_score":0.7874781},"labels":[],"label_agreement":null},{"id":"W3174458634","doi":"10.5194/acp-2021-344","title":"Surface deposition of marine fog and its treatment in the WRF model","year":2021,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Impact; Oceans Limited (Canada); Barrie Urology Group; York University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Weather Research and Forecasting Model; Deposition (geology); Settling; Surface roughness; Environmental science; Atmospheric sciences; Meteorology; Surface water; Sink (geography); Planetary boundary layer; Boundary layer; Surface finish; Dew; Materials science; Turbulence; Geology; Mechanics; Physics; Geography; Environmental engineering; Composite material","score_opus":0.01307508779618808,"score_gpt":0.2227553469805944,"score_spread":0.20968025918440633,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3174458634","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":[0.967059,0.00004634126,0.00060163246,0.0003133855,0.0000046745186,0.000059479054,6.750524e-7,0.0000029455875,0.03191184],"genre_scores_gemma":[0.9936756,0.00007355518,0.0036256653,0.000115524635,0.0000019029333,0.0000029187486,0.0000015582532,0.0000020232428,0.0025012875],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99969745,0.000013899243,0.000062457235,0.000089680136,0.000074085976,0.000062412604],"domain_scores_gemma":[0.9998863,0.000012332526,0.000012735142,0.00007278914,0.0000016267196,0.000014249108],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000035081204,0.000040242234,0.000049674825,1.1913205e-7,0.000021102747,0.0000049275677,0.000032535783,0.000015684678,0.0005645043],"category_scores_gemma":[0.0000015928777,0.000024103789,0.00001255345,0.00006174321,0.00001803249,0.00003485971,0.00004127482,0.000015794007,0.000008820616],"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":[0.00004054795,0.00095911935,0.63845986,0.00001722529,0.000022564074,0.000058508704,0.0039668535,0.16447413,0.15066701,0.0039348346,0.00048062814,0.036918696],"study_design_scores_gemma":[0.0007363647,0.00017901485,0.35494208,0.000005788209,0.000021796077,0.00002423371,0.0011377336,0.5845774,0.057010658,0.0010656425,0.00014613951,0.00015315705],"about_ca_topic_score_codex":0.0006104793,"about_ca_topic_score_gemma":0.0009371102,"teacher_disagreement_score":0.42010325,"about_ca_system_score_codex":0.000029011599,"about_ca_system_score_gemma":0.0000041113417,"threshold_uncertainty_score":0.6180926},"labels":[],"label_agreement":null},{"id":"W3174756112","doi":"10.1016/j.scitotenv.2021.148624","title":"Nocturnal surface radiation cooling modulated by cloud cover change reinforces PM2.5 accumulation: Observational study of heavy air pollution in the Sichuan Basin, Southwest China","year":2021,"lang":"en","type":"article","venue":"The Science of The Total Environment","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":29,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Environmental science; Cloud cover; Atmospheric sciences; Boundary layer; Daytime; Planetary boundary layer; Climatology; Diurnal cycle; Radiative cooling; Air pollution; Meteorology; Geology; Cloud computing; Chemistry; Geography","score_opus":0.03468041025236106,"score_gpt":0.25218025896631674,"score_spread":0.21749984871395567,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3174756112","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":[0.99655926,0.00007128271,0.000115974595,0.0024166508,0.00015221063,0.0005304585,0.000014038084,0.000005188501,0.0001349615],"genre_scores_gemma":[0.99932235,0.000023300332,0.00010553414,0.00020674744,0.00003932217,0.000010986659,0.0000055353,0.000006991107,0.00027922232],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9976972,0.00019109875,0.00037202716,0.00028576242,0.0012035868,0.00025033698],"domain_scores_gemma":[0.99906456,0.000053602307,0.00031969554,0.000511825,0.00000881871,0.000041519896],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010685257,0.00014583567,0.00015501124,0.0000030384813,0.00045865428,0.000029120343,0.0006550048,0.000040334297,0.0003300786],"category_scores_gemma":[0.000045522404,0.00008217067,0.00006475168,0.0006579836,0.0007303522,0.00036640416,0.00036090045,0.00015401295,0.000016448263],"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":[0.000029353145,0.00019936355,0.012332541,0.000001995143,0.000006858865,4.3040717e-7,0.005454623,0.96041584,0.02125497,0.000034017456,0.00007811145,0.00019189322],"study_design_scores_gemma":[0.00036144553,0.000104182436,0.9493659,0.000010728648,0.00002008449,0.0000050687413,0.0017763483,0.041842308,0.006276072,0.00008151161,0.000055975983,0.00010034778],"about_ca_topic_score_codex":0.0012835198,"about_ca_topic_score_gemma":0.000019070312,"teacher_disagreement_score":0.93703336,"about_ca_system_score_codex":0.00023483216,"about_ca_system_score_gemma":0.000032951364,"threshold_uncertainty_score":0.3614129},"labels":[],"label_agreement":null},{"id":"W3178474477","doi":"10.5194/acp-21-10457-2021","title":"Empirical evidence for deep convection being a major source of stratospheric ice clouds over North America","year":2021,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":14,"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":"Goddard Space Flight Center; European Centre for Medium-Range Weather Forecasts; Forschungszentrum Jülich; National Natural Science Foundation of China; Deutsche Forschungsgemeinschaft; Langley Research Center; National Aeronautics and Space Administration","keywords":"Climatology; Mesoscale meteorology; Convection; Middle latitudes; Atmospheric sciences; Environmental science; Thunderstorm; Geology; Storm; Meteorology; Geography; Oceanography","score_opus":0.01563857509545262,"score_gpt":0.2536711169963766,"score_spread":0.238032541900924,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3178474477","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":[0.90915656,0.0003239178,0.08855331,0.00005992949,0.00004638126,0.00013028103,0.0000042055462,0.000035929697,0.0016895151],"genre_scores_gemma":[0.9644245,0.00016053379,0.03168554,0.0003369183,0.00019182202,0.000039167582,0.000018800718,0.000031904616,0.0031108141],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99856484,0.000029202396,0.0002983539,0.00051814056,0.00026562632,0.0003238401],"domain_scores_gemma":[0.9991048,0.00020100136,0.00018054941,0.00032697886,0.000038046936,0.0001486307],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00006358536,0.00024579532,0.00031754785,1.2964099e-8,0.00018145303,0.0000345224,0.0001648655,0.00010140079,0.0022817934],"category_scores_gemma":[0.000057611127,0.00024725788,0.00014051891,0.0004797442,0.00029844086,0.0001814964,0.00013665823,0.00015926363,0.000014528758],"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":[0.00022052645,0.0004647347,0.5464369,0.00046518087,0.00015000576,0.000014996656,0.0019400012,0.012190785,0.07010403,0.000020282841,0.001411613,0.36658093],"study_design_scores_gemma":[0.0039105657,0.0006849365,0.37217107,0.00032418498,0.000828277,0.000109088054,0.0032901007,0.42946133,0.103888564,0.0029425612,0.07958159,0.002807723],"about_ca_topic_score_codex":0.00018150691,"about_ca_topic_score_gemma":0.00001635767,"teacher_disagreement_score":0.41727054,"about_ca_system_score_codex":0.00008080746,"about_ca_system_score_gemma":0.000048219303,"threshold_uncertainty_score":0.999998},"labels":[],"label_agreement":null},{"id":"W3181268545","doi":"10.5194/egusphere-egu21-11933","title":"Meteorological conditions favourable for strong aerosol impacts on clouds","year":2021,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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; Environmental science; Pollution; Relative humidity; Atmospheric sciences; Forcing (mathematics); Meteorology; Track (disk drive); Cloud computing; Climatology; Geography; Geology","score_opus":0.021252777981813176,"score_gpt":0.27035088279630914,"score_spread":0.24909810481449596,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3181268545","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":[0.8848354,0.000020962492,0.008120142,0.0010870303,0.0001303492,0.0002067645,0.000025480442,0.000070607704,0.10550323],"genre_scores_gemma":[0.98192084,0.000011065696,0.006394422,0.0016657249,0.000047138336,0.000049133025,0.000025615187,0.0000115899975,0.009874459],"study_design_codex":"not_applicable","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99898857,0.000029637518,0.00014537972,0.00030547852,0.00017618768,0.0003547406],"domain_scores_gemma":[0.9994722,0.00010980236,0.000037428184,0.00022013235,0.0000096297035,0.00015080045],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00009783304,0.00012384963,0.00014819042,4.4100076e-7,0.00022003808,0.000037047157,0.00012282318,0.00008044768,0.023853946],"category_scores_gemma":[0.00006964257,0.000094163806,0.00010313499,0.00012085309,0.00010249151,0.000088633,0.00008761602,0.00009223182,0.00060747477],"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":[0.00024709513,0.0019100675,0.08356339,0.00003090163,0.00018912234,0.00012827916,0.00035780593,0.0246289,0.29815912,0.08991234,0.49167392,0.009199039],"study_design_scores_gemma":[0.008787073,0.0056799846,0.33817583,0.000072358736,0.00032087517,0.00017417592,0.0045730276,0.025930375,0.4154519,0.020402022,0.17717656,0.00325579],"about_ca_topic_score_codex":0.00005333248,"about_ca_topic_score_gemma":0.00007983618,"teacher_disagreement_score":0.31449735,"about_ca_system_score_codex":0.00008544183,"about_ca_system_score_gemma":0.000016418247,"threshold_uncertainty_score":0.9770384},"labels":[],"label_agreement":null},{"id":"W3181419372","doi":"10.1175/jas-d-21-0015.1","title":"Dependence of Ice Microphysical Properties On Environmental Parameters: Results from HAIC-HIWC Cayenne Field Campaign","year":2021,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Supercomputing Center for Education and Research, University of Oklahoma; Centre National de la Recherche Scientifique; European Commission; Environment and Climate Change Canada; National Aeronautics and Space Administration; China Scholarship Council; Centre National d’Etudes Spatiales; National Science Foundation; University of Oklahoma; Boeing; Transport Canada; Aeronautics Research Mission Directorate","keywords":"Ice crystals; Mesoscale meteorology; Precipitation; Atmospheric sciences; Convection; Environmental science; Altitude (triangle); Water vapor; Meteorology; Climatology; Geology; Physics","score_opus":0.015956661355557487,"score_gpt":0.20883402593531267,"score_spread":0.19287736457975518,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3181419372","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":[0.99656475,0.00025369183,0.00016000475,0.0015066643,0.00047255476,0.000076874676,0.0000069972843,0.0000047651124,0.0009536883],"genre_scores_gemma":[0.9857543,0.00009058198,0.012771264,0.00076644047,0.00006962917,0.0000013718413,2.336104e-7,0.000007866344,0.00053832214],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9977064,0.00016346753,0.00054771715,0.00032532724,0.0009794291,0.0002776606],"domain_scores_gemma":[0.99852264,0.00037185257,0.00062167813,0.00036322925,0.00001511191,0.00010551085],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041369448,0.00017198084,0.00028598343,5.2776886e-7,0.00025220562,0.000055233744,0.0010034429,0.000066519766,0.00054019655],"category_scores_gemma":[0.00036550095,0.00009798521,0.00021709457,0.00039137452,0.00080118835,0.00027579657,0.00033567907,0.00025896516,0.00004034641],"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":[0.00070357515,0.0010394617,0.072078176,0.000009996404,0.0001236998,0.00012472074,0.0039942097,0.158714,0.73859525,0.00002686135,0.005444757,0.019145306],"study_design_scores_gemma":[0.0015667485,0.0022146034,0.08835952,0.00039600572,0.0001504253,0.00014961937,0.0083381785,0.014061805,0.88031644,0.0014326489,0.0023838084,0.00063021405],"about_ca_topic_score_codex":0.0006349669,"about_ca_topic_score_gemma":0.00004255435,"teacher_disagreement_score":0.14465219,"about_ca_system_score_codex":0.00010955325,"about_ca_system_score_gemma":0.00007745799,"threshold_uncertainty_score":0.59147733},"labels":[],"label_agreement":null},{"id":"W3183097053","doi":"10.2172/1804710","title":"Eastern Pacific Cloud Aerosol Precipitation Experiment (EPCAPE) Science Plan","year":2021,"lang":"en","type":"report","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":27,"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; Dalhousie University","funders":"","keywords":"Aerosol; Cloud condensation nuclei; Environmental science; Atmospheric sciences; Meteorology; Drizzle; Radiative transfer; Precipitation; Geology; Geography; Physics","score_opus":0.029086492913730694,"score_gpt":0.2750301422587153,"score_spread":0.2459436493449846,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3183097053","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.22829206,0.0004217859,0.0008571977,0.00010716751,0.0032930586,0.0005255741,0.000015243825,0.0001285698,0.7663593],"genre_scores_gemma":[0.75692916,0.00054908695,0.003967442,0.00011144414,0.0006544097,0.00013950207,0.00012066903,0.00007874874,0.23744951],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9945587,0.000052902404,0.00057522627,0.0012804855,0.0028274532,0.0007052383],"domain_scores_gemma":[0.9983258,0.000034515495,0.00034367578,0.00087769795,0.000086363994,0.00033194554],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00073690317,0.0004703732,0.00045162113,0.0000047174344,0.00039077617,0.00025258874,0.0005850423,0.0002774753,0.020824084],"category_scores_gemma":[0.00008495925,0.00040030238,0.00017217216,0.0005553248,0.0007585089,0.00029270133,0.00080969784,0.0003345803,0.0020312222],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000091629685,0.0016348979,0.11727433,0.000309617,0.00024686364,0.0005317042,0.009741903,0.0011837204,0.15274525,0.00024844502,0.6295505,0.08644113],"study_design_scores_gemma":[0.0012455168,0.00081291253,0.021947041,0.00060849456,0.00024385656,0.00047481235,0.014570011,0.0021410403,0.06182858,0.00010144131,0.89135736,0.0046689585],"about_ca_topic_score_codex":0.0010359763,"about_ca_topic_score_gemma":0.0001347952,"teacher_disagreement_score":0.5289098,"about_ca_system_score_codex":0.001370661,"about_ca_system_score_gemma":0.0006398298,"threshold_uncertainty_score":0.9998449},"labels":[],"label_agreement":null},{"id":"W3183224505","doi":"10.1175/bams-d-19-0220.1","title":"Aerosol and Cloud Experiments in the Eastern North Atlantic (ACE-ENA)","year":2021,"lang":"en","type":"article","venue":"Bulletin of the American Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":143,"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":"Los Alamos National Laboratory; Biological and Environmental Research; Office of Science; Korea Meteorological Administration; U.S. Department of Energy","keywords":"Cloud condensation nuclei; Aerosol; Environmental science; Precipitation; Climatology; Drizzle; Climate model; Atmospheric sciences; Meteorology; Climate change; Oceanography; Geography; Geology","score_opus":0.012320031391731623,"score_gpt":0.22647945266363073,"score_spread":0.2141594212718991,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3183224505","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":[0.99234205,0.0001277929,0.00008201229,0.0058856173,0.000061095976,0.00015226107,0.0000017281933,0.000011316275,0.001336092],"genre_scores_gemma":[0.9890948,0.00015598978,0.003156934,0.0070852945,0.000044769433,0.000022002772,0.0000011319186,0.00000790253,0.00043115296],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984783,0.00032875498,0.00021725758,0.00032843676,0.0003498774,0.00029739103],"domain_scores_gemma":[0.9992261,0.00017064958,0.00018213298,0.0003585963,0.000006748756,0.00005577915],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002940401,0.0001516713,0.0002726143,3.1172004e-7,0.00014541611,0.00002116445,0.00048847904,0.000044946883,0.0011525729],"category_scores_gemma":[0.000072132025,0.00007868882,0.000195813,0.00028160165,0.0012339023,0.000011051306,0.0006317284,0.00022500863,0.000060281873],"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":[0.000026112004,0.00017651569,0.97974056,0.0000041464114,0.000021403197,0.000007766055,0.0009852977,0.00011647929,0.0020036113,0.000024443536,0.015541725,0.0013519516],"study_design_scores_gemma":[0.00042719973,0.000239796,0.95540327,0.00000911429,0.000032227585,0.000019745317,0.003781838,0.000271686,0.00051663304,0.00006992958,0.039013907,0.00021464632],"about_ca_topic_score_codex":0.0010245468,"about_ca_topic_score_gemma":0.00004356881,"teacher_disagreement_score":0.024337271,"about_ca_system_score_codex":0.00003526585,"about_ca_system_score_gemma":0.0000075656667,"threshold_uncertainty_score":0.9997605},"labels":[],"label_agreement":null},{"id":"W3183262208","doi":"10.5194/amt-2021-148","title":"Coincident In-situ and Triple-Frequency Radar Airborne Observations in the Arctic","year":2021,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"National Research Council Canada","funders":"Environment and Climate Change Canada; Natural Environment Research Council; Sight Research UK; Université du Québec à Montréal","keywords":"Radar; Snow; Remote sensing; Environmental science; Meteorology; Rayleigh scattering; Particle (ecology); Geology; Geography; Physics; Optics; Computer science; Telecommunications","score_opus":0.017728887380571372,"score_gpt":0.22534403779646686,"score_spread":0.20761515041589548,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3183262208","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":[0.9746738,0.00014715985,0.00024835308,0.0033738092,0.000036184818,0.00011071425,3.9661418e-7,0.000007280061,0.02140228],"genre_scores_gemma":[0.99236053,0.00008017998,0.0046657207,0.0015510872,0.000009601275,0.000014895877,0.0000022780964,0.0000038545854,0.0013118306],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993057,0.000054179065,0.00015091525,0.00017617614,0.00016550261,0.00014751533],"domain_scores_gemma":[0.9997137,0.000052352596,0.000021626422,0.00017860415,0.000003409079,0.00003029262],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00018773245,0.00006546349,0.00008034266,7.180124e-7,0.000052790012,0.000022963963,0.000117013624,0.00002791014,0.001073542],"category_scores_gemma":[0.00004812603,0.00004547472,0.00001779455,0.00035350097,0.00007319927,0.00010815126,0.00008124076,0.00009537361,0.00004222285],"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":[0.0000023569626,0.00014856689,0.9845138,0.000004162516,0.00000215126,0.000082715014,0.0011062921,0.00006752659,0.005913865,0.0044801147,0.000694349,0.0029840996],"study_design_scores_gemma":[0.00024745901,0.000018526185,0.99480754,0.0000057964544,0.0000029181854,0.000014895228,0.0011468964,0.00012308134,0.00014583202,0.0024607307,0.00095930084,0.000067048066],"about_ca_topic_score_codex":0.0021530094,"about_ca_topic_score_gemma":0.01722982,"teacher_disagreement_score":0.02009045,"about_ca_system_score_codex":0.000084875974,"about_ca_system_score_gemma":0.000015257862,"threshold_uncertainty_score":0.9998396},"labels":[],"label_agreement":null},{"id":"W3184176283","doi":"","title":"3D Radiative Transfer in Cloudy Atmospheres","year":2004,"lang":"en","type":"article","venue":"NASA Technical Reports Server (NASA)","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"McGill University","funders":"","keywords":"Radiative transfer; Atmosphere (unit); Cloud computing; Atmospheric radiative transfer codes; Environmental science; Meteorology; Remote sensing; Atmospheric sciences; Computer science; Physics; Geology; Optics","score_opus":0.008102751367740595,"score_gpt":0.22797189597147374,"score_spread":0.21986914460373314,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3184176283","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":[0.9779901,0.0002095085,0.0021590043,0.00043604066,0.00024512823,0.0005693259,0.0000021947478,0.0002355334,0.018153146],"genre_scores_gemma":[0.9933016,0.00006434411,0.005159605,0.0006168125,0.00007750905,0.00008491119,0.0000050216036,0.000040838357,0.0006494083],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99678206,0.000055856723,0.0008136707,0.0008685926,0.00079953554,0.00068029755],"domain_scores_gemma":[0.9987571,0.00005473779,0.00012987606,0.0007603037,0.0000151780705,0.00028277942],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004786936,0.0003558836,0.0004454521,0.0000024247322,0.00013501788,0.000041447798,0.0003640419,0.0003549679,0.0034109906],"category_scores_gemma":[0.00012804609,0.00031356426,0.00020518314,0.00068215193,0.00035563298,0.0003069926,0.00022988475,0.0005367966,0.00021037587],"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":[0.00018666958,0.0018386634,0.92130107,0.00003850864,0.000058964502,0.0049928073,0.001027484,0.03641048,0.013372777,0.0014041438,0.0031832058,0.016185217],"study_design_scores_gemma":[0.0014076682,0.00041148395,0.9693181,0.00009741187,0.000040829225,0.00032454712,0.00016405816,0.00013573104,0.0025713402,0.0073214686,0.01733345,0.00087390817],"about_ca_topic_score_codex":0.0020691697,"about_ca_topic_score_gemma":0.0018978928,"teacher_disagreement_score":0.048017025,"about_ca_system_score_codex":0.00072644727,"about_ca_system_score_gemma":0.00007774211,"threshold_uncertainty_score":0.99993163},"labels":[],"label_agreement":null},{"id":"W3187523415","doi":"10.1016/0967-0653(96)90976-x","title":"10.1016/0967-0653(96)90976-x","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Aerosol; Cloud condensation nuclei; Atmospheric sciences; Environmental science; Cloud physics; Sea salt aerosol; Precipitation; Albedo (alchemy); Meteorology; Climatology; Cloud computing; Geology; Geography; Sea salt","score_opus":0.0038916546279109854,"score_gpt":0.15670120352092123,"score_spread":0.15280954889301024,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3187523415","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00967887,0.000017686321,0.0000042832394,0.00023044678,0.0000015230911,0.00012725177,0.00000389788,0.00008860979,0.9898474],"genre_scores_gemma":[0.0015455326,2.56255e-7,0.00051017746,0.00013710847,0.00006879738,0.000014891215,0.0000044256576,0.000020369936,0.9976984],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990178,0.000022059554,0.00013800676,0.0002755952,0.00023368996,0.00031287284],"domain_scores_gemma":[0.9994876,0.000015337968,0.000022108086,0.00028572342,0.00000291621,0.00018636034],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00008874504,0.00013545297,0.00012223185,7.901563e-7,0.0001073177,0.000027423781,0.00027451696,0.00005625482,0.9998405],"category_scores_gemma":[0.000008413805,0.00012174293,0.000052147807,0.00019779993,0.00007954181,0.00009942609,0.00009400584,0.00008237054,0.9994387],"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":[0.000020208261,0.00003956095,0.0000067072297,7.844949e-7,0.0000038605476,0.000004507839,0.000024903135,0.0006308898,0.00006605577,3.465313e-7,0.34359172,0.65561044],"study_design_scores_gemma":[0.000118984506,0.00009845464,0.0005919639,0.0000035884361,0.000007309157,0.0000049041796,0.0000018808189,0.0003498395,0.000073304545,0.000010157994,0.99855983,0.00017976409],"about_ca_topic_score_codex":0.00013057259,"about_ca_topic_score_gemma":8.443424e-7,"teacher_disagreement_score":0.6554307,"about_ca_system_score_codex":0.000071237126,"about_ca_system_score_gemma":0.000005362502,"threshold_uncertainty_score":0.49645326},"labels":[],"label_agreement":null},{"id":"W3190162753","doi":"10.5194/amt-2021-2","title":"Assessing synergistic radar and radiometer capability in retrieving ice cloud microphysics based on hybrid Bayesian algorithms","year":2021,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"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":"Goddard Space Flight Center; Stony Brook University; Nuclear Safety and Security Commission; National Center for Atmospheric Research; Environment and Climate Change Canada; Colorado State University; National Aeronautics and Space Administration","keywords":"Environmental science; Radiometer; Radar; Remote sensing; Computer science; Cloud computing; Brightness temperature; Algorithm; Meteorology; Precipitation; Ice cloud; Bayesian probability; Geology; Artificial intelligence; Geography","score_opus":0.010120861639802201,"score_gpt":0.2361113111107877,"score_spread":0.2259904494709855,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3190162753","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":[0.91002375,0.000042911426,0.08388764,0.00024615618,0.00013683856,0.00009302794,0.0000027851524,0.000027005986,0.0055398825],"genre_scores_gemma":[0.957438,0.0000076743245,0.041553017,0.00066179415,0.000053601554,0.000003613485,0.0000052455725,0.00001737208,0.00025968638],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9985291,0.00012270798,0.00023759315,0.00053177006,0.0002737212,0.0003051259],"domain_scores_gemma":[0.999298,0.0001836601,0.00005619852,0.00033601004,0.000007959507,0.000118177966],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00028555494,0.00017367619,0.00022092633,0.000002365684,0.000126177,0.000116978525,0.00011424894,0.000050913684,0.001106325],"category_scores_gemma":[0.00010013032,0.00015766715,0.000051078056,0.0004333077,0.00018636632,0.00018815581,0.00011672939,0.00018849355,0.00002332165],"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":[0.000103559505,0.0014333382,0.30793703,0.00017857052,0.00004142737,0.0012547661,0.0006233619,0.008892155,0.23753045,0.00021483717,0.0017329524,0.44005755],"study_design_scores_gemma":[0.0023307302,0.00027076073,0.40832284,0.000191236,0.00007045199,0.000049244703,0.0010156692,0.48423272,0.098205425,0.0014561,0.0023334548,0.0015213607],"about_ca_topic_score_codex":0.00047523875,"about_ca_topic_score_gemma":0.000046128047,"teacher_disagreement_score":0.47534057,"about_ca_system_score_codex":0.00025757047,"about_ca_system_score_gemma":0.0000335722,"threshold_uncertainty_score":0.9998068},"labels":[],"label_agreement":null},{"id":"W3191253014","doi":"10.5194/acp-2021-448","title":"The 2019 Raikoke volcanic eruption part 2: Particle phase dispersion and concurrent wildﬁre smoke emissions","year":2021,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"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":"Met Office; University of Exeter; Natural Environment Research Council; Sight Research UK","keywords":"Aerosol; Volcano; Atmospheric sciences; Environmental science; Stratosphere; Troposphere; Lidar; Volcanic ash; Plume; Vulcanian eruption; Sulfate aerosol; Meteorology; Geology; Remote sensing; Geography; Seismology","score_opus":0.013222460101824164,"score_gpt":0.2631524362815083,"score_spread":0.24992997617968415,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3191253014","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":[0.9930141,0.0006004554,0.00070321053,0.002375577,0.00021088227,0.00010086804,0.000005643796,0.000028597404,0.002960671],"genre_scores_gemma":[0.98595536,0.0008352557,0.000081556565,0.0003053363,0.000037598733,0.000008070839,0.000008061807,0.000007113342,0.012761654],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991388,0.000045856053,0.00014526781,0.0002450358,0.0001935829,0.00023150415],"domain_scores_gemma":[0.99953383,0.000047717684,0.00003710294,0.00021109112,0.0000067994392,0.00016342939],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00012610473,0.00009432203,0.00007913804,2.0689066e-7,0.00042399138,0.000057051206,0.000090050526,0.00003666107,0.0051819184],"category_scores_gemma":[0.00003452831,0.00005827237,0.000040525596,0.00011159812,0.00017201778,0.00010921442,0.00019980136,0.00008117803,0.00016647886],"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":[0.00005694465,0.00080711104,0.19740294,0.000007789144,0.000041064017,0.000031412994,0.00092351995,0.00024546648,0.11062261,0.003454595,0.1677018,0.5187048],"study_design_scores_gemma":[0.0029372443,0.00031255512,0.17673346,0.00004411867,0.000078644574,0.000040518236,0.0024781283,0.02890051,0.023060527,0.00040573007,0.76443833,0.00057025993],"about_ca_topic_score_codex":0.000113003865,"about_ca_topic_score_gemma":0.00014063757,"teacher_disagreement_score":0.5967365,"about_ca_system_score_codex":0.00004724058,"about_ca_system_score_gemma":0.000013856253,"threshold_uncertainty_score":0.9957275},"labels":[],"label_agreement":null},{"id":"W3193070000","doi":"10.5194/gmd-2021-148","title":"Evaluation of a Quasi-steady state approximation of the cloud Droplet Growth Equation (QDGE) scheme for aerosol activation in global models using multiple aircraft data over both continental and marine environments","year":2021,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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","funders":"Ministry of Science and Technology of the People's Republic of China; National Natural Science Foundation of China","keywords":"Aerosol; Environmental science; Cloud computing; Meteorology; Relative humidity; Atmospheric sciences; Computer science; Physics","score_opus":0.05706898456363743,"score_gpt":0.2808519427650802,"score_spread":0.22378295820144276,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3193070000","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":[0.73608994,0.00000781852,0.26306158,0.000039540944,0.00003259369,0.0005686013,0.000051520838,0.000003527881,0.00014486325],"genre_scores_gemma":[0.98193675,0.000008064876,0.017774217,0.000033143395,0.000010373177,0.000020084133,0.0001641969,0.000009167897,0.00004401152],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9983265,0.00013418852,0.00037687985,0.00033211536,0.0006831785,0.00014713603],"domain_scores_gemma":[0.999285,0.00004799838,0.0002819885,0.00032971145,0.000027021386,0.00002831411],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007965154,0.00011895731,0.00016381362,0.0000019787792,0.000060174527,0.000015913865,0.00015478104,0.00005572958,0.00015439373],"category_scores_gemma":[0.00015031923,0.00009947149,0.000031191506,0.00018604286,0.000098026365,0.0005758282,0.0004666003,0.000046520283,4.8417866e-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":[0.00013955362,0.00073950976,0.66277826,0.00005540804,0.00004875925,1.4648913e-7,0.0006274058,0.054414917,0.2674498,0.0004138781,0.000055085908,0.013277254],"study_design_scores_gemma":[0.0016548074,0.000031502874,0.06628389,0.00002056941,0.000042286687,7.0108763e-7,0.00025115107,0.9147789,0.015182356,0.0016537177,0.0000038328126,0.000096315256],"about_ca_topic_score_codex":0.0022919285,"about_ca_topic_score_gemma":0.00066596334,"teacher_disagreement_score":0.86036396,"about_ca_system_score_codex":0.00030494467,"about_ca_system_score_gemma":0.00004268387,"threshold_uncertainty_score":0.40563294},"labels":[],"label_agreement":null},{"id":"W3194366956","doi":"10.5194/amt-14-5717-2021","title":"A simulation-experiment-based assessment of retrievals of above-cloud temperature and water vapor using a hyperspectral infrared sounder","year":2021,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; McGill University","funders":"Canadian Space Agency; Université de Lille; Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Radiance; Environmental science; Remote sensing; Hyperspectral imaging; Effective radius; Water vapor; Meteorology; Radiative transfer; Atmospheric Infrared Sounder; Brightness temperature; Cloud top; Infrared; Cloud computing; Numerical weather prediction; Computer science; Brightness; Geology; Physics; Optics","score_opus":0.02509825081046297,"score_gpt":0.28001067656090534,"score_spread":0.2549124257504424,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3194366956","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":[0.9636797,0.00036923104,0.033557214,0.00007755034,0.00007371929,0.0004697962,0.000004258917,0.00008981608,0.0016787568],"genre_scores_gemma":[0.8032497,0.000017187438,0.19641705,0.00013722295,0.0000261182,0.000021581993,0.0000045042107,0.000026844087,0.000099771445],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99755406,0.00012418539,0.0005558376,0.0004473856,0.0009930198,0.00032548586],"domain_scores_gemma":[0.99901617,0.000042390948,0.00022872018,0.00044019034,0.0001726493,0.0000998542],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005730282,0.00026954667,0.0004298112,0.0000011769029,0.00011723988,0.00003415004,0.00016503122,0.0001581662,0.0014504142],"category_scores_gemma":[0.000066731154,0.00021508095,0.00012260156,0.0003380694,0.00022936819,0.00014768544,0.0001410528,0.00014867689,0.0000013615276],"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":[0.000032144704,0.0002792814,0.03207798,0.000054608692,0.000059474518,0.0000074223076,0.00032243942,0.008580131,0.9579267,0.000057070014,0.000115901414,0.0004868345],"study_design_scores_gemma":[0.00058381615,0.00028879335,0.009961996,0.00011421095,0.00008762152,0.000004283056,0.00043265885,0.02392689,0.96330523,0.0003573702,0.00057845964,0.00035863655],"about_ca_topic_score_codex":0.00015689731,"about_ca_topic_score_gemma":0.000006984175,"teacher_disagreement_score":0.16285983,"about_ca_system_score_codex":0.00037058967,"about_ca_system_score_gemma":0.00012462959,"threshold_uncertainty_score":0.99946237},"labels":[],"label_agreement":null},{"id":"W3195922006","doi":"10.5194/amt-2021-247","title":"Validation of the Aeolus Level-2B wind product over Northern Canada and the Arctic","year":2021,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":6,"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 Waterloo; Environment and Climate Change Canada; University of Toronto","funders":"Canadian Space Agency","keywords":"Arctic; Environmental science; Lidar; Radiosonde; Meteorology; Satellite; Radar; Climatology; Atmospheric sciences; Remote sensing; Geography; Geology; Computer science; Telecommunications; Oceanography","score_opus":0.006826667079062677,"score_gpt":0.17778628414069717,"score_spread":0.17095961706163448,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3195922006","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":[0.99333644,0.000042059542,0.00003474686,0.0019347215,0.00007909207,0.00009318239,0.0000016002426,0.0000021237886,0.004476063],"genre_scores_gemma":[0.99165916,0.000005458906,0.00009821617,0.00040044956,0.000016189466,0.0000015654634,5.8856347e-7,0.0000036305632,0.007814721],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994493,0.00004231349,0.000086760534,0.00012463468,0.00021390001,0.00008306533],"domain_scores_gemma":[0.99968517,0.000028375038,0.00004261312,0.0002163635,0.000008007824,0.000019458537],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00009163476,0.00004981318,0.00005989038,8.7241e-8,0.00008943972,0.000009206011,0.000096935306,0.000010474139,0.0015815969],"category_scores_gemma":[0.000040341187,0.000023881865,0.000019178942,0.00010391969,0.0001860999,0.000033020962,0.0001388858,0.00004473168,0.0000039746114],"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":[0.000006774686,0.000013569095,0.9930736,0.000004856504,0.000010799408,0.0000011304735,0.00037702112,0.0011835445,0.0016844196,0.00013767563,0.00108255,0.0024241013],"study_design_scores_gemma":[0.00025164714,0.000004031892,0.9878799,0.0000035849173,0.000013775996,0.000006418392,0.00022579732,0.00020993031,0.009139182,0.0002541232,0.001955316,0.000056337092],"about_ca_topic_score_codex":0.6231245,"about_ca_topic_score_gemma":0.8374314,"teacher_disagreement_score":0.21430688,"about_ca_system_score_codex":0.000061598366,"about_ca_system_score_gemma":0.00006614652,"threshold_uncertainty_score":0.9993311},"labels":[],"label_agreement":null},{"id":"W3196601944","doi":"10.5194/amt-2021-251","title":"Laser Imaging Nephelometer for aircraft deployment","year":2021,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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 Alberta","funders":"National Oceanic and Atmospheric Administration; National Aeronautics and Space Administration","keywords":"Nephelometer; Polarimetry; Remote sensing; Optics; Polarization (electrochemistry); Wavelength; Lidar; Linear polarization; Laser; Detector; Environmental science; Physics; Scattering; Materials science; Light scattering; Geology","score_opus":0.007990489803688912,"score_gpt":0.2237594748765427,"score_spread":0.2157689850728538,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3196601944","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":[0.77443594,0.00006953232,0.1617115,0.0028781218,0.0002376221,0.00020580697,0.0000031769348,0.00010206353,0.06035622],"genre_scores_gemma":[0.90314233,0.000006703277,0.062698826,0.0044008545,0.00004794858,0.000039515253,0.0000039118077,0.0000172053,0.029642692],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99937147,0.00000823062,0.000091619804,0.00021250032,0.00011701869,0.00019915697],"domain_scores_gemma":[0.99974483,0.000021318547,0.000015766022,0.00014964605,0.0000051497764,0.00006326062],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000051966148,0.000071818424,0.00006711784,2.4655202e-7,0.00007165058,0.000024088216,0.00007485477,0.000016107757,0.012310255],"category_scores_gemma":[0.000008327787,0.000059320664,0.0000583477,0.00008162921,0.00003370786,0.00008083933,0.00012425333,0.00002781662,0.00043461155],"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":[0.00001216545,0.0002222858,0.5730422,0.000009096813,0.000026760466,0.000040768722,0.0002277534,0.00078697776,0.026691036,0.0002889067,0.16879308,0.22985893],"study_design_scores_gemma":[0.0012869657,0.00006639559,0.14773726,0.00001021117,0.000044005457,0.000031494612,0.0007586493,0.021394795,0.0995445,0.0013731883,0.7271264,0.0006260783],"about_ca_topic_score_codex":0.00006381576,"about_ca_topic_score_gemma":0.000057907786,"teacher_disagreement_score":0.5583334,"about_ca_system_score_codex":0.000060920967,"about_ca_system_score_gemma":0.0000063765724,"threshold_uncertainty_score":0.9885926},"labels":[],"label_agreement":null},{"id":"W3196861671","doi":"10.5194/acp-2021-448-rc2","title":"A well-written paper describing a unique study of multiple clouds","year":2021,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Natural Environment Research Council; Met Office; University of Exeter","keywords":"Aerosol; Volcano; Stratosphere; Environmental science; Troposphere; Atmospheric sciences; Lidar; Volcanic ash; Plume; Meteorology; Sulfate aerosol; Vulcanian eruption; Explosive eruption; Atmospheric dispersion modeling; Geology; Remote sensing; Geography; Pyroclastic rock; Air pollution; Seismology","score_opus":0.03277509256464774,"score_gpt":0.26330930081464793,"score_spread":0.2305342082500002,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3196861671","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.20092209,0.021597097,0.0011392469,0.0129817845,0.0026791121,0.0060594548,0.00010159095,0.0003095731,0.75421005],"genre_scores_gemma":[0.19997036,0.0061135567,0.007650368,0.008211649,0.00025432228,0.00030952523,0.00020214122,0.00016129884,0.7771268],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99704576,0.00020992589,0.00071520987,0.00079502846,0.0008168189,0.00041723804],"domain_scores_gemma":[0.9984548,0.000100044046,0.00030284902,0.00094496756,0.0000409124,0.00015643347],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004379095,0.0004487376,0.0009360927,0.0000016816556,0.00010889705,0.000026624997,0.0006344574,0.00025101684,0.054705214],"category_scores_gemma":[0.000105039166,0.0003612367,0.0002567695,0.00044850938,0.00012641995,0.00009650045,0.00096762745,0.00046558087,0.00031704784],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007817664,0.0009209,0.014158772,0.00040767028,0.00010792078,0.000063255415,0.0003983526,0.0001344293,0.00021978198,0.000007723439,0.9733224,0.010250999],"study_design_scores_gemma":[0.0005798996,0.0002831623,0.0034400914,0.0011806579,0.00025287233,0.000012494355,0.0015092457,0.00017495261,0.000052620617,0.000012586289,0.9919055,0.00059589196],"about_ca_topic_score_codex":0.012194401,"about_ca_topic_score_gemma":0.008283248,"teacher_disagreement_score":0.054388165,"about_ca_system_score_codex":0.00018291244,"about_ca_system_score_gemma":0.000057528454,"threshold_uncertainty_score":0.99988395},"labels":[],"label_agreement":null},{"id":"W3197789549","doi":"","title":"Exploring Alternate Parameterizations for Snowfall with Validation from Satellite and Terrestrial Radars","year":2009,"lang":"en","type":"article","venue":"34th Conference on Radar Meteorology (5-9 October 2009)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Meteorology; Environmental science; Radar; Snow; Numerical weather prediction; Satellite; Weather Research and Forecasting Model; Weather radar; Remote sensing; Computer science; Geography","score_opus":0.0648719611344335,"score_gpt":0.2551335420013642,"score_spread":0.19026158086693068,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3197789549","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":[0.9723385,0.00005342247,0.02276971,0.0010900549,0.00022557854,0.00047874838,0.000046394176,0.00007098629,0.002926605],"genre_scores_gemma":[0.97095823,0.00030712018,0.02740361,0.0008350017,0.00009993347,0.000057688594,0.00007030372,0.000021556149,0.0002465315],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.998383,0.00009260545,0.0002913824,0.000595165,0.00023437431,0.00040349684],"domain_scores_gemma":[0.9992276,0.0001274038,0.00016097534,0.00031962048,0.000012571715,0.00015185439],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015447612,0.0002742648,0.0003073884,0.000008213675,0.00018489572,0.00007196229,0.0002232366,0.00010845088,0.00038745446],"category_scores_gemma":[0.000035302866,0.00022673473,0.000049983515,0.00013594393,0.00021457212,0.0003312459,0.00004228088,0.00015699622,0.000044852994],"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":[0.0052296338,0.0009973776,0.086007126,0.000019344045,0.00038453683,0.00011164006,0.0033964692,0.006350475,0.101122916,0.02134072,0.0014748896,0.7735649],"study_design_scores_gemma":[0.014731796,0.010148541,0.7808436,0.00020339074,0.0007275032,0.000078522084,0.00072739844,0.01432945,0.027298734,0.0600034,0.087564915,0.0033427363],"about_ca_topic_score_codex":0.0004041674,"about_ca_topic_score_gemma":0.00012436441,"teacher_disagreement_score":0.7702221,"about_ca_system_score_codex":0.000051287858,"about_ca_system_score_gemma":0.000025027175,"threshold_uncertainty_score":0.9245974},"labels":[],"label_agreement":null},{"id":"W3201004561","doi":"10.1117/12.2596792","title":"Straylight analyses and mitigation strategies for the ELT METIS instrument","year":2021,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Metis; Computer science; World Wide Web","score_opus":0.02859584621288472,"score_gpt":0.2865654400628759,"score_spread":0.25796959384999113,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3201004561","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":[0.9358457,0.00023411271,0.04311289,0.0023985829,0.00005307696,0.00014111881,0.00000327421,0.000017721268,0.01819357],"genre_scores_gemma":[0.98703855,0.00007813273,0.010707119,0.00029680185,0.000016997967,0.000019034895,0.0000029808925,0.0000034747784,0.0018368775],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99957156,0.000011523476,0.00008027801,0.00013692593,0.00010370865,0.00009598943],"domain_scores_gemma":[0.99979687,0.000045633467,0.000022258591,0.00010099039,0.0000049882096,0.000029256382],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000053438685,0.000056584387,0.000055481436,2.2369873e-7,0.0001366281,0.0000724584,0.00005349388,0.000020426918,0.0023685663],"category_scores_gemma":[0.000006256882,0.000033236443,0.000028947561,0.00007858674,0.00008569115,0.000114304574,0.000050616854,0.000023924513,0.000012117915],"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":[0.000044307882,0.00027084636,0.11021135,0.000054654676,0.00039177662,0.000016491746,0.0030757014,0.01171022,0.34545097,0.08348415,0.034563005,0.41072652],"study_design_scores_gemma":[0.0012166734,0.00028679543,0.6087192,0.000017149632,0.0002960703,0.00003055447,0.03997241,0.027134486,0.19676432,0.034669846,0.09021664,0.00067583536],"about_ca_topic_score_codex":0.00022102954,"about_ca_topic_score_gemma":0.00046349288,"teacher_disagreement_score":0.49850786,"about_ca_system_score_codex":0.000017858963,"about_ca_system_score_gemma":0.000011150325,"threshold_uncertainty_score":0.9985434},"labels":[],"label_agreement":null},{"id":"W3201416030","doi":"10.5194/acp-2020-537","title":"Review of experimental studies on secondary ice production","year":2020,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Federal Aviation Administration; Helmholtz Association; Environment and Climate Change Canada; Transport Canada","keywords":"Fragmentation (computing); Environmental science; Hard rime; Ice crystals; Ice nucleus; Atmospheric sciences; Meteorology; Climatology; Computer science; Chemistry; Geography; Geology; Nucleation","score_opus":0.03419582179149035,"score_gpt":0.2856983039059077,"score_spread":0.2515024821144174,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3201416030","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":[0.85099715,0.035100367,0.000031651885,0.0069730477,0.00025729116,0.00038479405,0.0000011507713,0.00005906472,0.1061955],"genre_scores_gemma":[0.98259,0.003980077,0.0010750092,0.0113328025,0.000054994907,0.000012587266,7.9093337e-7,0.00000602652,0.0009477149],"study_design_codex":"not_applicable","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99951214,0.000015413616,0.00013091255,0.00016336015,0.00011811113,0.000060073846],"domain_scores_gemma":[0.9998203,0.000005810258,0.000048465,0.00008723222,0.0000033800025,0.000034814497],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000061185696,0.00005856005,0.00011138773,1.2938034e-7,0.000028842313,0.0000012515015,0.00006350896,0.000009841973,0.00525572],"category_scores_gemma":[0.000037690843,0.000042295665,0.00002949082,0.00008992294,0.00007780573,0.00005547929,0.00007748576,0.00003939653,0.00028108628],"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":[0.00006542113,0.00040438285,0.0038765583,0.0020401867,0.00007225819,0.0000047113886,0.004919956,0.00024413285,0.19025785,0.00053642155,0.7702268,0.027351325],"study_design_scores_gemma":[0.00040889758,0.0013988396,0.0047331336,0.0014196977,0.000041040304,0.0000064706574,0.0075788614,0.0001308376,0.85046315,0.00006433978,0.13328588,0.00046886166],"about_ca_topic_score_codex":0.000009628456,"about_ca_topic_score_gemma":0.0000010756493,"teacher_disagreement_score":0.6602053,"about_ca_system_score_codex":0.000028509183,"about_ca_system_score_gemma":0.0000030536414,"threshold_uncertainty_score":0.9956536},"labels":[],"label_agreement":null},{"id":"W3203626251","doi":"10.5194/acp-21-14687-2021","title":"Surface deposition of marine fog and its treatment in the Weather Research and Forecasting (WRF) model","year":2021,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Impact; Oceans Limited (Canada); Barrie Urology Group; York University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Weather Research and Forecasting Model; Deposition (geology); Settling; Environmental science; Surface roughness; Meteorology; Atmospheric sciences; Planetary boundary layer; Boundary layer; Surface water; Turbulence; Materials science; Geology; Mechanics; Geography; Physics; Environmental engineering","score_opus":0.03526051336005757,"score_gpt":0.264177053660253,"score_spread":0.22891654030019545,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3203626251","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":[0.9895633,0.00032875428,0.0002158703,0.00007985753,0.0000030518968,0.00007969697,0.0000022094694,0.0000035614628,0.009723691],"genre_scores_gemma":[0.99116063,0.00032445363,0.0061739394,0.000021045687,0.000018872894,0.0000086180235,0.0000043377227,0.0000074372892,0.0022806753],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9993461,0.000023810586,0.00010927874,0.00021977726,0.00014700639,0.0001540513],"domain_scores_gemma":[0.99971414,0.000080932754,0.000032322132,0.00012104474,0.000011958633,0.000039617647],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011525906,0.00009574562,0.00011758581,9.726119e-9,0.00010436097,0.000020803109,0.000050169536,0.000043297423,0.00014422773],"category_scores_gemma":[0.0000069095863,0.00007215401,0.000016005295,0.00015848446,0.00012680623,0.000060301456,0.00009397776,0.00008869411,9.269849e-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":[0.00010224286,0.00074182125,0.30361307,0.00024226498,0.000049801398,0.000050256767,0.0054400857,0.021136014,0.30502588,0.00037591445,0.0000729132,0.36314973],"study_design_scores_gemma":[0.001050137,0.00015827427,0.036029674,0.00004920883,0.000032081556,0.000063828214,0.0018714723,0.87466836,0.08026228,0.0053529036,0.00016699245,0.0002947725],"about_ca_topic_score_codex":0.00022040108,"about_ca_topic_score_gemma":0.000025680243,"teacher_disagreement_score":0.8535324,"about_ca_system_score_codex":0.0000346739,"about_ca_system_score_gemma":0.000011998587,"threshold_uncertainty_score":0.29423553},"labels":[],"label_agreement":null},{"id":"W3204579747","doi":"10.5194/amt-14-6159-2021","title":"Mass concentration estimates of long-range-transported Canadian biomass burning aerosols from a multi-wavelength Raman polarization lidar and a ceilometer in Finland","year":2021,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":11,"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":"Academy of Finland; National Oceanic and Atmospheric Administration; The Ministry of Economic Affairs and Employment; Langley Research Center; National Aeronautics and Space Administration","keywords":"Aerosol; Lidar; Depolarization ratio; Ceilometer; Mass concentration (chemistry); Plume; Atmospheric sciences; Environmental science; Wavelength; Soot; Troposphere; Mineral dust; HYSPLIT; Meteorology; Chemistry; Optics; Physics; Combustion","score_opus":0.017082317789903066,"score_gpt":0.2188665957326985,"score_spread":0.20178427794279544,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3204579747","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":[0.92813724,0.0004664856,0.07025656,0.00011658958,0.000045372934,0.0004666098,0.00001540525,0.00007177055,0.00042394278],"genre_scores_gemma":[0.8795961,0.00009804435,0.120029256,0.00011868059,0.0000133488475,0.000044891764,0.00003904206,0.000024929464,0.00003569149],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981428,0.00009139719,0.00046167016,0.00046340248,0.00047319138,0.0003675486],"domain_scores_gemma":[0.9993006,0.000029608353,0.00017420227,0.00025836387,0.000062297404,0.0001749454],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003739758,0.00024568618,0.0003208722,0.0000016267192,0.0001039454,0.00005129215,0.00014077769,0.0001684563,0.0006836244],"category_scores_gemma":[0.000078347155,0.00024339386,0.00005157708,0.00047688253,0.0001287726,0.00021784616,0.000037680646,0.000138603,0.0000062502068],"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":[0.000012352739,0.00006319049,0.8019794,0.000018925884,0.00002357482,0.000038074177,0.00045590315,0.000015948455,0.1893109,0.00000443232,0.000023267998,0.008053994],"study_design_scores_gemma":[0.0006545143,0.00009451732,0.8756576,0.00017978634,0.00005352949,0.000004300984,0.00014518737,0.0077052093,0.114832714,0.00013860309,0.00018308025,0.00035094237],"about_ca_topic_score_codex":0.07237019,"about_ca_topic_score_gemma":0.054468974,"teacher_disagreement_score":0.07447818,"about_ca_system_score_codex":0.00034707697,"about_ca_system_score_gemma":0.000100970115,"threshold_uncertainty_score":0.99253136},"labels":[],"label_agreement":null},{"id":"W3205656495","doi":"10.5194/amt-2021-333","title":"Identification of Smoke and Sulfuric Acid Aerosol in SAGE III/ISS Extinction Spectra Following the 2019 Raikoke Eruption","year":2021,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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":"Human Exploration and Operations Mission Directorate; Science Mission Directorate; European Space Agency; Langley Research Center; National Aeronautics and Space Administration","keywords":"Aerosol; Sulfuric acid; Smoke; Volcano; Plume; Extinction (optical mineralogy); Environmental science; Context (archaeology); Atmospheric sciences; Vulcanian eruption; Northern Hemisphere; Geology; Meteorology; Mineralogy; Environmental chemistry; Chemistry; Geography; Geochemistry; Inorganic chemistry","score_opus":0.009129802866788711,"score_gpt":0.23234161656070726,"score_spread":0.22321181369391854,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3205656495","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":[0.98904246,0.00024062741,0.007293011,0.00029482378,0.00014474003,0.0001475136,0.000001311183,0.000015403522,0.0028201279],"genre_scores_gemma":[0.99621415,0.00014094761,0.00031165802,0.000073391966,0.000019833693,0.000008922636,0.000004842836,0.000007368564,0.0032189118],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99906695,0.000054217733,0.00026825035,0.00024758038,0.00021554682,0.00014743589],"domain_scores_gemma":[0.99962735,0.000027637765,0.00008972223,0.00022001854,0.000004648163,0.000030636264],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00032505687,0.00008662089,0.00010888673,0.0000015823011,0.00009388805,0.000032718846,0.000091052876,0.000052679898,0.0012408316],"category_scores_gemma":[0.000022905151,0.0000659678,0.00005245999,0.00029636634,0.00007145834,0.00020363404,0.00009062381,0.00008485757,0.00003598413],"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":[0.0000104180235,0.000067152134,0.07859115,0.000004339047,0.000008127187,0.0000051089783,0.0006199518,0.0002519729,0.9061283,0.00008168794,0.00013096258,0.014100847],"study_design_scores_gemma":[0.00048163207,0.000030222158,0.74015296,0.000012291724,0.000022319957,0.000008759248,0.0012228107,0.0016247327,0.2558886,0.00028987657,0.00012490687,0.00014090037],"about_ca_topic_score_codex":0.0004512947,"about_ca_topic_score_gemma":0.0006659143,"teacher_disagreement_score":0.6615618,"about_ca_system_score_codex":0.000070274975,"about_ca_system_score_gemma":0.000008097218,"threshold_uncertainty_score":0.9996722},"labels":[],"label_agreement":null},{"id":"W3206977199","doi":"10.1175/jas-d-20-0269.1","title":"Combined Effect of the Wegener–Bergeron–Findeisen Mechanism and Large Eddies on Microphysics of Mixed-Phase Stratiform Clouds","year":2021,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":14,"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":"U.S. Department of Energy","keywords":"Ice crystals; Aerosol; Atmospheric sciences; Arctic; Particle (ecology); Ice nucleus; Evaporation; Phase (matter); Geology; Environmental science; Meteorology; Physics; Thermodynamics; Oceanography","score_opus":0.005819139109011052,"score_gpt":0.23560484276444807,"score_spread":0.22978570365543702,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3206977199","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":[0.99742526,0.00023388531,0.00011496247,0.00055776857,0.00071420503,0.00011774553,0.0000063327743,0.0000026836653,0.000827166],"genre_scores_gemma":[0.99745727,0.000076857505,0.0017837147,0.00014366985,0.000045070006,0.0000013901061,1.10851104e-7,0.000007909955,0.00048402438],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9981085,0.00020637663,0.00044849046,0.00018935475,0.0007985848,0.00024868824],"domain_scores_gemma":[0.9986325,0.00018445359,0.00076920586,0.00030459467,0.000038028877,0.00007125289],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000854819,0.00017071844,0.0003643671,5.1726624e-7,0.00034407753,0.000032955202,0.0007696642,0.00005493118,0.00020459354],"category_scores_gemma":[0.000117880576,0.00008119185,0.00023908856,0.00066819973,0.0007852265,0.00014554894,0.00039447917,0.0001772895,0.000002701427],"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":[0.0005814571,0.0017809279,0.2587143,0.00014349357,0.00034819607,0.0000352565,0.0025386626,0.019273456,0.67441833,0.008709065,0.009024322,0.02443252],"study_design_scores_gemma":[0.0030754951,0.0043011475,0.09571559,0.00026451857,0.0002484965,0.00008516499,0.00163504,0.0071348217,0.87775385,0.008462467,0.0009617362,0.00036165296],"about_ca_topic_score_codex":0.00005933983,"about_ca_topic_score_gemma":0.000030585823,"teacher_disagreement_score":0.20333552,"about_ca_system_score_codex":0.000052097737,"about_ca_system_score_gemma":0.00008783663,"threshold_uncertainty_score":0.33109078},"labels":[],"label_agreement":null},{"id":"W3207015022","doi":"10.1109/igarss47720.2021.9553536","title":"CloudSat Cloud Length, Thickness Distributions Again Confirm the 23/9 (2.55 D) Scaling, Stratified, Turbulence Model","year":2021,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Scaling; Turbulence; Isotropy; Physics; Dimension (graph theory); Statistical physics; Meteorology; Geometry; Mathematics; Optics; Combinatorics","score_opus":0.014171107103342706,"score_gpt":0.23355001911269674,"score_spread":0.21937891200935403,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3207015022","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":[0.7027812,0.00024957422,0.20501302,0.0051987553,0.00050284225,0.00032000308,0.00007300982,0.00016827116,0.08569334],"genre_scores_gemma":[0.9791559,0.00008270684,0.003429356,0.001491902,0.000114601964,0.000030781455,0.000044110064,0.000019400768,0.015631251],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9980138,0.00010637502,0.00033878232,0.0005433434,0.00049140264,0.0005062789],"domain_scores_gemma":[0.99887556,0.000113906586,0.00009159363,0.0007090305,0.00003270648,0.00017719134],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0003447265,0.0002483752,0.00020271624,6.09088e-7,0.00065015303,0.0001361246,0.00053556415,0.00014614937,0.0058453595],"category_scores_gemma":[0.000077695004,0.00016904382,0.00013850682,0.00034336804,0.00053543004,0.00015957694,0.0003878224,0.0003569337,0.001037904],"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":[0.00009693341,0.0014156437,0.017585475,0.000061006453,0.00017221861,0.00020351516,0.0054303845,0.32748458,0.03987995,0.32021132,0.25683284,0.030626107],"study_design_scores_gemma":[0.0014326088,0.000086457665,0.011251037,0.00005943636,0.00019916677,0.00020151146,0.0077142394,0.8433943,0.026696514,0.042179585,0.06484678,0.0019384102],"about_ca_topic_score_codex":0.00031828208,"about_ca_topic_score_gemma":0.00042075771,"teacher_disagreement_score":0.5159097,"about_ca_system_score_codex":0.00012311821,"about_ca_system_score_gemma":0.000084239466,"threshold_uncertainty_score":0.9997399},"labels":[],"label_agreement":null},{"id":"W3208013444","doi":"10.1364/sensors.2021.sm2c.1","title":"Spectral Laser Induced Fluorescence for standoff detection and classification of aerosolized biological threats","year":2021,"lang":"en","type":"article","venue":"OSA Optical Sensors and Sensing Congress 2021 (AIS, FTS, HISE, SENSORS, ES)","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"Defence Research and Development Canada","funders":"","keywords":"Aerosolization; Fluorescence; Laser; Warning system; Laser-induced fluorescence; Materials science; Environmental science; Remote sensing; Computer science; Optics; Physics; Medicine; Telecommunications; Geology","score_opus":0.025742912233395157,"score_gpt":0.2523567866481676,"score_spread":0.22661387441477243,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3208013444","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":[0.9970323,0.00018370744,0.0005003945,0.00072725106,0.0003331459,0.00042058443,0.00003810862,0.000049399427,0.0007151441],"genre_scores_gemma":[0.9867911,0.00082627055,0.011568952,0.000083523635,0.00013179227,0.0000057476323,0.000026956504,0.000035916328,0.0005297829],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99732804,0.00020077893,0.0005708261,0.00093123317,0.0003849571,0.0005841617],"domain_scores_gemma":[0.9984935,0.00042570924,0.00021663192,0.0003701209,0.00011833295,0.00037574067],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00030183268,0.00037802238,0.0006253029,0.0000094027155,0.0003582564,0.00012488166,0.00009594148,0.0003603317,0.00030397304],"category_scores_gemma":[0.00054321985,0.0003256644,0.00014176319,0.00029661748,0.00076104363,0.00016410102,0.00016219981,0.00029696987,0.000018066838],"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":[0.0005386454,0.0001431231,0.005993362,0.00004032613,0.00006155846,0.00009193863,0.00023792413,0.00008097185,0.88410807,0.00079871016,0.00014924289,0.107756145],"study_design_scores_gemma":[0.005942104,0.001026381,0.17670508,0.00026772975,0.0003811,0.00051300786,0.0023577304,0.11549296,0.6890763,0.0013236426,0.005001236,0.0019127043],"about_ca_topic_score_codex":0.000077417,"about_ca_topic_score_gemma":0.00013347188,"teacher_disagreement_score":0.19503173,"about_ca_system_score_codex":0.00010559824,"about_ca_system_score_gemma":0.00003229764,"threshold_uncertainty_score":0.99991953},"labels":[],"label_agreement":null},{"id":"W3208337906","doi":"10.1007/s10546-021-00675-5","title":"Microphysics and Optical Attenuation in Fog: Observations from Two Coastal Sites","year":2021,"lang":"en","type":"article","venue":"Boundary-Layer Meteorology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":14,"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":"Naval Postgraduate School; Office of Naval Research; Multidisciplinary University Research Initiative; University of Notre Dame","keywords":"Visibility; Parametrization (atmospheric modeling); Environmental science; Attenuation; Liquid water content; Meteorology; Wind speed; Range (aeronautics); Mie scattering; Lidar; Fog; Atmospheric sciences; Remote sensing; Physics; Scattering; Light scattering; Geography; Optics; Computer science; Materials science; Radiative transfer","score_opus":0.02326380239297862,"score_gpt":0.25003623428406246,"score_spread":0.22677243189108384,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3208337906","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":[0.99365646,0.00017929694,0.0033094147,0.0014849765,0.00011144179,0.00008318856,0.000021113512,0.000019049035,0.0011350884],"genre_scores_gemma":[0.9761796,0.000027480619,0.022244537,0.0010568345,0.00007279622,0.00001238562,0.00008475151,0.000013679473,0.00030793852],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989095,0.00009100165,0.00021208439,0.00038518797,0.00014216987,0.00026005472],"domain_scores_gemma":[0.99951893,0.00013970667,0.00004992803,0.00020332125,0.000013707514,0.00007441537],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00010514987,0.00012885724,0.00019245039,0.0000018128844,0.00013735697,0.00005280929,0.00009950871,0.00009064045,0.001082993],"category_scores_gemma":[0.00006186747,0.0001309446,0.000037240083,0.00020215828,0.00033884103,0.00015622973,0.00024697187,0.00015932223,0.00013088438],"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":[0.000022434942,0.00006861539,0.6800642,0.0000015943143,0.000014219689,0.00004211214,0.00033350964,0.00028251688,0.31239215,0.0009201148,0.0003089254,0.0055496325],"study_design_scores_gemma":[0.00074600085,0.00006847129,0.9756786,0.0000031147838,0.000028098588,0.000014930672,0.00014421246,0.0024506052,0.003731734,0.00959717,0.007355474,0.00018157998],"about_ca_topic_score_codex":0.0011183451,"about_ca_topic_score_gemma":0.006381621,"teacher_disagreement_score":0.3086604,"about_ca_system_score_codex":0.000053180414,"about_ca_system_score_gemma":0.000040733306,"threshold_uncertainty_score":0.9998301},"labels":[],"label_agreement":null},{"id":"W3208423788","doi":"10.1029/2021jd035358","title":"Aerosol Activation in Radiation Fog at the Atmospheric Radiation Program Southern Great Plains Site","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":10,"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","funders":"Office of Naval Research; Biological and Environmental Research; Office of Science; U.S. Department of Energy","keywords":"Supersaturation; Aerosol; Cloud condensation nuclei; Atmospheric sciences; Particle (ecology); Environmental science; Particle-size distribution; Particle size; Condensation; Radiation; Radiative transfer; Meteorology; Chemistry; Geography; Physics; Geology; Physical chemistry; Oceanography","score_opus":0.018612430226269697,"score_gpt":0.2997135534964152,"score_spread":0.2811011232701455,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3208423788","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":[0.99572295,0.0003026816,0.00028828616,0.0014850273,0.00010629661,0.00040727056,0.0000031138034,0.000018246697,0.0016661235],"genre_scores_gemma":[0.9928609,0.00021545349,0.0015059013,0.00014154361,0.00038607794,0.000044760367,0.000010263767,0.000034571553,0.004800544],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9961414,0.00062168227,0.00055390876,0.00035512532,0.0016774274,0.00065046526],"domain_scores_gemma":[0.99833506,0.00058177306,0.0003326293,0.00036809433,0.00014720124,0.00023524654],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009511381,0.00020858076,0.00031458584,0.0000012523103,0.00041324133,0.00015505814,0.00040047345,0.00013594996,0.0029686044],"category_scores_gemma":[0.00054036017,0.00014410315,0.00021148795,0.0013391983,0.00036970078,0.00046715306,0.00032982146,0.00079850707,0.0005720572],"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":[0.0006724615,0.001269566,0.30138123,0.000029354482,0.00009827174,0.00014945283,0.0030255776,0.014190863,0.051778242,0.00010436416,0.016144799,0.6111558],"study_design_scores_gemma":[0.0031302418,0.0017027644,0.8950215,0.00014763861,0.00005036506,0.000055174794,0.0030248489,0.03507845,0.015866498,0.0020044297,0.043332867,0.00058521796],"about_ca_topic_score_codex":0.0014820816,"about_ca_topic_score_gemma":0.0012337221,"teacher_disagreement_score":0.6105706,"about_ca_system_score_codex":0.0009890718,"about_ca_system_score_gemma":0.00016447617,"threshold_uncertainty_score":0.9979428},"labels":[],"label_agreement":null},{"id":"W3211767801","doi":"10.3390/rs13224623","title":"Remote Sensing of Aerosols at Night with the CoSQM Sky Brightness Data","year":2021,"lang":"en","type":"article","venue":"Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Cégep de Sherbrooke; Bishop's University; Université de Sherbrooke","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Aerosol; Environmental science; Remote sensing; Sky brightness; Brightness; Photometer; Angstrom exponent; Sky; Sun photometer; Zenith; Meteorology; Daytime; Atmospheric sciences; Geography; Geology; Optics; Physics","score_opus":0.018846622821028294,"score_gpt":0.2341848754752703,"score_spread":0.215338252654242,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3211767801","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":[0.9197056,0.00014754393,0.0662227,0.0016173506,0.00014727893,0.00015694907,0.0000086109385,0.00004548547,0.011948464],"genre_scores_gemma":[0.90820616,0.00004981386,0.086711094,0.000668071,0.00011326437,1.0840105e-9,0.000029234001,0.000047717283,0.0041746492],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99797386,0.0001466026,0.0002825351,0.00062815554,0.0005479126,0.00042091476],"domain_scores_gemma":[0.9979641,0.000133182,0.00020718524,0.001551752,0.000037029666,0.00010674384],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032884476,0.0002292699,0.00030611255,0.0000014074392,0.00041063747,0.000054973036,0.00032831283,0.00009095671,0.00021493644],"category_scores_gemma":[0.00005432264,0.00015284319,0.00006106975,0.0004342224,0.00044462527,0.0001435649,0.0009768682,0.00020628591,0.00009172821],"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":[0.00012595774,0.000031048537,0.00065116293,0.000052178173,0.00012558063,0.0009330321,0.0016204761,0.0047872863,0.3831147,0.000014124381,0.0075830603,0.6009614],"study_design_scores_gemma":[0.0011141035,0.000086186825,0.0037653202,0.00044786395,0.00022800376,0.0021023548,0.0012004871,0.78608024,0.13720557,0.00032221264,0.0664837,0.0009639551],"about_ca_topic_score_codex":0.0011055747,"about_ca_topic_score_gemma":0.0017295968,"teacher_disagreement_score":0.781293,"about_ca_system_score_codex":0.00014840867,"about_ca_system_score_gemma":0.00004475895,"threshold_uncertainty_score":0.6232764},"labels":[],"label_agreement":null},{"id":"W3212214242","doi":"10.1002/essoar.10507289.1","title":"Analysis of local dust plumes using ground- and satellite-based remote sensing supported by surface measurements","year":2021,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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 de Montréal; Université de Sherbrooke","funders":"","keywords":"Satellite; Remote sensing; Meteorology; Geography; Physics; Astronomy","score_opus":0.0248630320013356,"score_gpt":0.24362786305503845,"score_spread":0.21876483105370284,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3212214242","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":[0.85129505,0.00013439117,0.14713459,0.00005853543,0.000020869145,0.00004356453,0.0000036828976,0.000015471998,0.0012938204],"genre_scores_gemma":[0.9717608,0.000017376358,0.027449468,0.00020158877,0.000003000408,2.4543855e-8,0.00001841831,0.000010449702,0.0005388621],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99873674,0.00007012515,0.00025169677,0.00032963324,0.00039214935,0.00021963417],"domain_scores_gemma":[0.99953085,0.00003145306,0.00009229123,0.00022080305,0.000023448894,0.00010116749],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021335078,0.00013019227,0.00026418568,0.0000020849307,0.00008845764,0.000029017623,0.00005920473,0.00006598776,0.0018171943],"category_scores_gemma":[0.000011087195,0.000120122655,0.00008111535,0.000759012,0.00020921155,0.000076443575,0.00007958307,0.00005666506,0.00000621319],"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":[0.00002199024,0.00006690151,0.42317423,0.000013064559,0.0003621296,0.000023590443,0.0001397612,0.027984088,0.5067935,0.0000014309953,0.00014194193,0.041277383],"study_design_scores_gemma":[0.0004574185,0.000031097476,0.13147368,0.000016315917,0.00076175295,0.0000056177223,0.0009953396,0.75031,0.115161955,0.000013756944,0.0004595016,0.00031359424],"about_ca_topic_score_codex":0.005212537,"about_ca_topic_score_gemma":0.00093717827,"teacher_disagreement_score":0.72232586,"about_ca_system_score_codex":0.00011812708,"about_ca_system_score_gemma":0.000023784645,"threshold_uncertainty_score":0.99909526},"labels":[],"label_agreement":null},{"id":"W3215834466","doi":"10.1177/11786302211060152","title":"Effect of Dust Storms on Non-Accidental, Cardiovascular, and Respiratory Mortality: A Case of Dezful City in Iran","year":2021,"lang":"en","type":"article","venue":"Environmental Health Insights","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":11,"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":"Tehran University of Medical Sciences and Health Services","keywords":"Accidental; Storm; Respiratory system; Medicine; Internal medicine; Intensive care medicine; Emergency medicine; Geography; Meteorology; Physics","score_opus":0.01796061606258775,"score_gpt":0.2738468237574711,"score_spread":0.25588620769488335,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3215834466","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":[0.99686277,0.0018594605,0.000029910987,0.000017085358,0.00009397211,0.0004332401,0.000016445447,0.000007478947,0.00067965273],"genre_scores_gemma":[0.9993029,0.00022405242,0.00010701079,0.00024778768,0.00002085685,0.000023403923,0.0000074808127,0.000021042017,0.00004542496],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99789834,0.00033609502,0.00051049836,0.00050471927,0.00044985814,0.00030050642],"domain_scores_gemma":[0.9990248,0.000063443265,0.0001807905,0.00051897776,0.0000010640267,0.00021091694],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005451256,0.0002317266,0.00057732145,0.00000699034,0.00012414985,0.000005880745,0.000104420666,0.00010970143,0.00043441777],"category_scores_gemma":[0.000012830913,0.00019993325,0.00015403643,0.0001874343,0.00035176112,0.00012261387,0.00022876674,0.00021014363,0.00002117461],"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":[0.000109915185,0.00045539974,0.9633312,0.00019678936,0.00007840509,0.0014123736,0.0022972,0.0006850857,0.005000932,0.000009729688,0.000080506405,0.026342431],"study_design_scores_gemma":[0.0019384678,0.0016451714,0.9627496,0.00009344615,0.000041849853,0.00018213637,0.0007630416,0.00019530495,0.030885456,0.000025604564,0.001201848,0.0002780678],"about_ca_topic_score_codex":0.002302277,"about_ca_topic_score_gemma":0.001163914,"teacher_disagreement_score":0.026064362,"about_ca_system_score_codex":0.0004066079,"about_ca_system_score_gemma":0.000019391953,"threshold_uncertainty_score":0.8153041},"labels":[],"label_agreement":null},{"id":"W3216654922","doi":"10.26443/msurj.v3i1.127","title":"Using CloudSat data to look at the cloud and precipitation structure in the Arctic","year":2008,"lang":"en","type":"article","venue":"McGill Science Undergraduate Research Journal","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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 Manitoba; McGill University","funders":"McGill University","keywords":"Storm; Arctic; Environmental science; Precipitation; Climatology; Cloud top; Cloud base; Winter storm; Meteorology; Context (archaeology); Cloud computing; Atmospheric sciences; Geology; Geography; Oceanography; Computer science","score_opus":0.1555118846859041,"score_gpt":0.37634438808812676,"score_spread":0.22083250340222266,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3216654922","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":[0.98497355,0.00010312842,0.00020064821,0.013354266,0.00014547483,0.00033015193,0.000011399145,0.000004897469,0.00087648095],"genre_scores_gemma":[0.9971589,0.00029530944,0.0016902329,0.0004721836,0.000100868616,0.000002986672,9.5235765e-7,0.000009495075,0.00026910182],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.995549,0.0005322608,0.00025159935,0.00051197986,0.002333052,0.0008220838],"domain_scores_gemma":[0.9985958,0.00029670366,0.00008128136,0.0006838147,0.000062757856,0.00027966587],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.005831584,0.00013215526,0.00011101303,0.000016963062,0.0052385097,0.00022748682,0.0020733352,0.000038230195,0.0002053011],"category_scores_gemma":[0.00067061925,0.00006863703,0.000022776025,0.0019330732,0.0026560654,0.0007363741,0.0018231695,0.0007323601,0.000056264045],"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":[0.00038939697,0.00049168046,0.46056753,0.000041720952,0.00005439891,0.0008245678,0.01796874,0.077082194,0.31956735,0.0059675337,0.041359283,0.075685605],"study_design_scores_gemma":[0.0016435144,0.0008721858,0.7786408,0.00016532504,0.00003415827,0.0106093995,0.009101541,0.058727812,0.002384944,0.057754435,0.07906111,0.0010047728],"about_ca_topic_score_codex":0.00086801744,"about_ca_topic_score_gemma":0.0014334293,"teacher_disagreement_score":0.31807327,"about_ca_system_score_codex":0.0007923077,"about_ca_system_score_gemma":0.000108831475,"threshold_uncertainty_score":0.99605656},"labels":[],"label_agreement":null},{"id":"W331040916","doi":"10.2172/952496","title":"A Year of Radiation Measurements at the North Slope of Alaska Second Quarter 2009 ARM and Climate Change Prediction Program Metric Report","year":2009,"lang":"en","type":"report","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Pacific Northwest National Laboratory; Biological and Environmental Research; Office of Science; U.S. Department of Energy","keywords":"Milestone; Quarter (Canadian coin); Environmental science; Climatology; Meteorology; Aerosol; Series (stratigraphy); Geography; Geology; Archaeology","score_opus":0.028961428936876706,"score_gpt":0.2570301238773727,"score_spread":0.22806869494049598,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W331040916","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":[0.83788073,0.0009583606,0.000031353116,0.00005685126,0.00033222509,0.0018078419,0.000095733754,0.00005034093,0.15878657],"genre_scores_gemma":[0.99159133,0.0021851033,0.00046133844,0.000042521468,0.00014313127,0.00012014932,0.00015641538,0.000026298436,0.0052737067],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9973729,0.000041082672,0.00069494836,0.00041991562,0.0012104269,0.00026068272],"domain_scores_gemma":[0.9984773,0.00001530528,0.0009523462,0.0004199779,0.000056726374,0.000078337056],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008605753,0.00023067354,0.00037867946,0.000008158442,0.0000865973,0.000015423653,0.00013810767,0.0001850718,0.002389127],"category_scores_gemma":[0.000038794617,0.00015450302,0.00011586461,0.00041835036,0.0001415809,0.000124669,0.000121779,0.0001389943,0.000018732382],"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":[0.000018384942,0.00019686732,0.8418339,0.00007750529,0.000055275956,0.0000058972564,0.0001629176,0.000012992663,0.000040971787,2.8778067e-7,0.015964843,0.14163014],"study_design_scores_gemma":[0.00021630518,0.00041369663,0.97139126,0.000031176856,0.00012820995,0.00005304265,0.0000455862,0.000042046682,0.00018668098,0.000003246182,0.027342962,0.00014579495],"about_ca_topic_score_codex":0.00046491213,"about_ca_topic_score_gemma":0.0011176185,"teacher_disagreement_score":0.1537106,"about_ca_system_score_codex":0.00028020784,"about_ca_system_score_gemma":0.000042044838,"threshold_uncertainty_score":0.9985228},"labels":[],"label_agreement":null},{"id":"W4200025399","doi":"10.5194/amt-2021-247-ac1","title":"Reply on RC1","year":2021,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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 Space Agency; Environment and Climate Change Canada","keywords":"Radiosonde; Lidar; Meteorology; Environmental science; Arctic; Satellite; Numerical weather prediction; Climatology; Radar; Geography; Remote sensing; Geology; Computer science; Physics","score_opus":0.019045943199940407,"score_gpt":0.26867678518543386,"score_spread":0.24963084198549346,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200025399","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00006607583,0.0066246907,0.00008358195,0.06611104,0.0012463267,0.00021778535,0.00001632845,0.00005834043,0.92557585],"genre_scores_gemma":[0.000047809244,0.005730618,0.001113133,0.091443926,0.00017908085,0.000025415846,0.00012150557,0.000026417789,0.9013121],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9983573,0.00003678846,0.00023805822,0.0005689052,0.00055049354,0.00024848705],"domain_scores_gemma":[0.99905044,0.000029057855,0.00010139777,0.00070614857,0.0000074974614,0.00010547344],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00015442375,0.00024336661,0.0003678549,2.982753e-7,0.00006312454,0.00002135781,0.00032187183,0.00012935654,0.26420373],"category_scores_gemma":[0.00005882589,0.00018247814,0.00017858099,0.00016856668,0.00007215849,0.0000255684,0.00030729384,0.000298005,0.008318856],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[6.82403e-7,0.000029503397,0.00006274954,0.00009036476,0.0000075665826,0.000023549655,0.000004346158,0.000008694163,0.0000031192837,0.000026622176,0.9836856,0.016057199],"study_design_scores_gemma":[0.000041501626,0.000041872965,0.0002871282,0.000516973,0.000029730001,0.0000059928143,0.0000062887857,0.0000078315,0.000016019232,0.000027443215,0.998779,0.00024019465],"about_ca_topic_score_codex":0.00091079273,"about_ca_topic_score_gemma":0.00012870388,"teacher_disagreement_score":0.2558849,"about_ca_system_score_codex":0.00014605986,"about_ca_system_score_gemma":0.000025189,"threshold_uncertainty_score":0.9924533},"labels":[],"label_agreement":null},{"id":"W4200034789","doi":"10.3390/rs13245150","title":"Evaluations of the Climatologies of Three Latest Cloud Satellite Products Based on Passive Sensors (ISCCP-H, Two CERES) against the CALIPSO-GOCCP","year":2021,"lang":"en","type":"article","venue":"Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":17,"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":"Southern Hemisphere; Environmental science; International Satellite Cloud Climatology Project; Satellite; Northern Hemisphere; Climatology; Cloud cover; Meteorology; Atmospheric sciences; Remote sensing; Cloud computing; Geography; Geology; Computer science","score_opus":0.02174952872830775,"score_gpt":0.25602889950507735,"score_spread":0.23427937077676958,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200034789","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":[0.9874079,0.000082775405,0.00076171395,0.0048811142,0.00024371543,0.000298579,0.000009401018,0.000021931692,0.0062928456],"genre_scores_gemma":[0.99489266,0.00004549964,0.0043834606,0.000461605,0.0000507423,6.042762e-8,0.000004632056,0.000018025172,0.00014332449],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99829024,0.00028889556,0.00033085412,0.000323246,0.0005092822,0.00025749556],"domain_scores_gemma":[0.9984976,0.00032035625,0.0002790821,0.0007914715,0.0000762919,0.000035194287],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003265979,0.00016392725,0.00022676474,0.0000020292307,0.0002535851,0.000019123523,0.0001937889,0.00006289593,0.000054616146],"category_scores_gemma":[0.0005475684,0.00009664745,0.00012234574,0.0005136198,0.0005042538,0.00003654152,0.00018942528,0.00019712653,0.000026784464],"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":[0.000055423243,0.00012258929,0.016054984,0.00007905075,0.00007451915,0.00004541234,0.0016070228,0.7204233,0.11711586,0.00018928123,0.0007685973,0.14346397],"study_design_scores_gemma":[0.00057026005,0.0000642662,0.06127649,0.00031051863,0.0001250691,0.000029701345,0.0013173489,0.7505936,0.18249667,0.0009152222,0.0019798027,0.00032104205],"about_ca_topic_score_codex":0.00026868342,"about_ca_topic_score_gemma":0.0004613082,"teacher_disagreement_score":0.14314294,"about_ca_system_score_codex":0.0000856981,"about_ca_system_score_gemma":0.000074277224,"threshold_uncertainty_score":0.39411685},"labels":[],"label_agreement":null},{"id":"W4200037993","doi":"10.3390/atmos12121616","title":"The Relationship between Clouds Containing Multiple Layers 7.5–30 m Thick and Surface Weather Conditions","year":2021,"lang":"en","type":"article","venue":"Atmosphere","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"Canadian Space Agency; Environment and Climate Change Canada","keywords":"Snow; Arctic; Precipitation; Environmental science; Atmospheric sciences; Climatology; The arctic; Lidar; Meteorology; Geology; Geography; Remote sensing; Oceanography","score_opus":0.02187876569194702,"score_gpt":0.2524522186384692,"score_spread":0.23057345294652215,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200037993","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":[0.98116714,0.00050602684,0.00051752425,0.0012833775,0.00009415891,0.00013713076,0.000010113268,0.000059488688,0.016225068],"genre_scores_gemma":[0.98967224,0.000041955947,0.0022300761,0.0002653103,0.000055863555,0.000011010151,0.000011447162,0.000025036486,0.0076870625],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987992,0.000122020145,0.00021370639,0.00031814972,0.00022903745,0.00031791045],"domain_scores_gemma":[0.9982444,0.0012004271,0.00008289463,0.00032731373,0.000015252318,0.00012971228],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00024414688,0.00015534462,0.00014882935,6.3882894e-8,0.0009287921,0.00009235758,0.0001635464,0.00011408813,0.002423594],"category_scores_gemma":[0.0002406414,0.000120210505,0.000059132206,0.00019504203,0.0003291407,0.00013096628,0.00019536488,0.0002527137,0.00048216118],"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":[0.000004598476,0.000012007789,0.9933443,0.000002239075,0.000019530786,0.000008403733,0.00043993082,0.0011205951,0.00014861581,0.0016435572,0.0024155693,0.00084063975],"study_design_scores_gemma":[0.00041355882,0.000039188188,0.96865433,0.00001527595,0.000030762367,0.000008346653,0.0028547114,0.00095516915,0.000094908166,0.002337577,0.024399897,0.00019626446],"about_ca_topic_score_codex":0.00035274282,"about_ca_topic_score_gemma":0.0004433942,"teacher_disagreement_score":0.024689972,"about_ca_system_score_codex":0.00007767954,"about_ca_system_score_gemma":0.000029919252,"threshold_uncertainty_score":0.9984883},"labels":[],"label_agreement":null},{"id":"W4200048541","doi":"10.3103/s1060992x21040020","title":"State of the Stratospheric Aerosol Layer over Tomsk in 2017 Using Data from Sensing at Siberian Lidar Station in Tomsk","year":2021,"lang":"en","type":"article","venue":"Optical Memory and Neural Networks","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Altitude (triangle); Aerosol; Lidar; Angstrom exponent; Stratosphere; Atmospheric sciences; Environmental science; Angstrom; Wavelength; Atmosphere (unit); Tropopause; Scattering; Effects of high altitude on humans; Meteorology; Remote sensing; Physics; Geology; Optics; Chemistry","score_opus":0.029393710226518436,"score_gpt":0.2578005328758259,"score_spread":0.22840682264930745,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200048541","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":[0.99814403,0.00016090022,0.00091480796,0.0001453793,0.00016806615,0.000118975935,0.000016048594,0.000005789341,0.0003259836],"genre_scores_gemma":[0.99759465,0.00004242918,0.0018864592,0.0002503713,0.0000415474,6.476177e-7,0.000016146048,0.000011617859,0.00015609968],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99871683,0.00011897344,0.00027291453,0.00038118465,0.00021891927,0.00029117064],"domain_scores_gemma":[0.99932855,0.00011942786,0.000076132135,0.0003945512,0.000006499875,0.00007482882],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016529793,0.00013111679,0.00019201796,7.8656166e-7,0.000092519804,0.00003750221,0.00016981,0.00007447701,0.00036112938],"category_scores_gemma":[0.00003635008,0.00010252288,0.000026042277,0.00023550034,0.0001898596,0.00023105595,0.0006873547,0.00022936212,0.000002522754],"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":[0.00029937268,0.00018048532,0.24298875,0.000017714101,0.00002351414,0.00033236793,0.00077352626,0.576765,0.11595107,0.000010823397,0.00039402576,0.06226335],"study_design_scores_gemma":[0.00039822477,0.000020037642,0.22099905,0.000038477683,0.000013156957,0.000009227889,0.00012041266,0.77531815,0.00283735,0.000079451725,0.00002378485,0.00014266225],"about_ca_topic_score_codex":0.00048310016,"about_ca_topic_score_gemma":0.003808861,"teacher_disagreement_score":0.19855317,"about_ca_system_score_codex":0.000060449773,"about_ca_system_score_gemma":0.000012202911,"threshold_uncertainty_score":0.41807616},"labels":[],"label_agreement":null},{"id":"W4200056275","doi":"10.1007/s00445-021-01511-x","title":"Progress in protecting air travel from volcanic ash clouds","year":2021,"lang":"en","type":"article","venue":"Bulletin of Volcanology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":33,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"International Air Transport Association","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Volcanic ash; Cloud computing; Meteorology; Aviation; Environmental science; Vulnerability (computing); Volcanic hazards; Volcano; Satellite; Geology; Computer science; Computer security; Engineering; Geography; Aerospace engineering; Seismology","score_opus":0.0072413876332204155,"score_gpt":0.2125822650152305,"score_spread":0.2053408773820101,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200056275","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":[0.9852931,0.0005371049,0.00023387407,0.0033125787,0.00016538911,0.00019777897,0.000006193584,0.000028660315,0.0102253435],"genre_scores_gemma":[0.9912544,0.000023786257,0.006269616,0.00041513564,0.000054346467,0.000051506566,0.0000059326967,0.000020534277,0.0019047707],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984702,0.00015813299,0.00035081562,0.0004500571,0.00019177761,0.00037901918],"domain_scores_gemma":[0.9993871,0.000078905374,0.00014476039,0.00031266463,0.000013136156,0.00006347638],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00019418263,0.00015488845,0.00030458395,0.0000023066398,0.000063203515,0.000006086537,0.00026910746,0.00018000146,0.013769926],"category_scores_gemma":[0.00010221066,0.0001548665,0.00006751401,0.00021792493,0.00033277247,0.000014489038,0.0003064189,0.00029202065,0.00036092484],"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":[0.000091995134,0.0005198863,0.9109489,0.000027336844,0.0000439967,0.00024392206,0.0011756988,0.00028806936,0.018975528,0.00028825845,0.010223285,0.057173174],"study_design_scores_gemma":[0.0010705357,0.00020605742,0.8926844,0.00005058036,0.000017224953,0.000033227356,0.0012354573,0.00019758663,0.019343073,0.00076749205,0.08406422,0.0003301164],"about_ca_topic_score_codex":0.0022503706,"about_ca_topic_score_gemma":0.0011623262,"teacher_disagreement_score":0.07384094,"about_ca_system_score_codex":0.00009867918,"about_ca_system_score_gemma":0.000035824345,"threshold_uncertainty_score":0.9871316},"labels":[],"label_agreement":null},{"id":"W4200146047","doi":"10.5194/acp-21-18263-2021","title":"Constant flux layers with gravitational settling: links to aerosols, fog and deposition velocities","year":2021,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Settling; Deposition (geology); Mechanics; Aerosol; Flux (metallurgy); Surface roughness; Turbulence; Boundary layer; Planetary boundary layer; Atmospheric sciences; Gravitation; Shear velocity; Momentum (technical analysis); Thermophoresis; Materials science; Meteorology; Physics; Classical mechanics; Geology; Heat transfer; Thermodynamics; Composite material; Geomorphology","score_opus":0.005023308472954711,"score_gpt":0.1960711777441051,"score_spread":0.1910478692711504,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200146047","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":[0.9845355,0.0001165961,0.0078979125,0.0002890778,0.000018369105,0.00006900224,0.000011033808,0.000026344853,0.0070361434],"genre_scores_gemma":[0.93542075,0.000034542798,0.060587246,0.00060976,0.00007210297,0.000017710516,0.00004569119,0.000015920346,0.003196304],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9991723,0.000011113767,0.00011680367,0.00032410334,0.00018690011,0.00018877923],"domain_scores_gemma":[0.99962497,0.000039065475,0.000042087653,0.00012990495,0.000019922492,0.00014407937],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000034280605,0.00015860291,0.00014091867,9.425249e-9,0.00019062829,0.000059627386,0.000053357577,0.000082857616,0.00068062905],"category_scores_gemma":[0.000006375713,0.00014733996,0.000023981107,0.00016436014,0.00020482516,0.00009273013,0.000073923075,0.00014585938,0.000016073745],"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":[0.0003039597,0.0004782732,0.24467032,0.0003634927,0.00026741356,0.0002284697,0.0060424367,0.0131942015,0.45029536,0.0014928915,0.005752194,0.276911],"study_design_scores_gemma":[0.009025954,0.0012438514,0.25582573,0.000838549,0.00079502066,0.0014624932,0.022744011,0.08017876,0.5506728,0.024590937,0.04561246,0.0070093954],"about_ca_topic_score_codex":0.000051646104,"about_ca_topic_score_gemma":0.000007974604,"teacher_disagreement_score":0.2699016,"about_ca_system_score_codex":0.00004332591,"about_ca_system_score_gemma":0.00003084217,"threshold_uncertainty_score":0.7452411},"labels":[],"label_agreement":null},{"id":"W4200249385","doi":"10.5194/gmd-2021-148-ac1","title":"Reply on RC1","year":2021,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"National Natural Science Foundation of China; National Science Foundation","keywords":"Scalable Vector Graphics; Aerosol; Span (engineering); Cloud computing; Meteorology; Mathematics; Environmental science; Atmospheric sciences; Simulation; Computer science; Geography; Engineering; Physics; Structural engineering; Operating system","score_opus":0.019045943199940407,"score_gpt":0.26867678518543386,"score_spread":0.24963084198549346,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200249385","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00006607583,0.0066246907,0.00008358195,0.06611104,0.0012463267,0.00021778535,0.00001632845,0.00005834043,0.92557585],"genre_scores_gemma":[0.000047809244,0.005730618,0.001113133,0.091443926,0.00017908085,0.000025415846,0.00012150557,0.000026417789,0.9013121],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9983573,0.00003678846,0.00023805822,0.0005689052,0.00055049354,0.00024848705],"domain_scores_gemma":[0.99905044,0.000029057855,0.00010139777,0.00070614857,0.0000074974614,0.00010547344],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00015442375,0.00024336661,0.0003678549,2.982753e-7,0.00006312454,0.00002135781,0.00032187183,0.00012935654,0.26420373],"category_scores_gemma":[0.00005882589,0.00018247814,0.00017858099,0.00016856668,0.00007215849,0.0000255684,0.00030729384,0.000298005,0.008318856],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[6.82403e-7,0.000029503397,0.00006274954,0.00009036476,0.0000075665826,0.000023549655,0.000004346158,0.000008694163,0.0000031192837,0.000026622176,0.9836856,0.016057199],"study_design_scores_gemma":[0.000041501626,0.000041872965,0.0002871282,0.000516973,0.000029730001,0.0000059928143,0.0000062887857,0.0000078315,0.000016019232,0.000027443215,0.998779,0.00024019465],"about_ca_topic_score_codex":0.00091079273,"about_ca_topic_score_gemma":0.00012870388,"teacher_disagreement_score":0.2558849,"about_ca_system_score_codex":0.00014605986,"about_ca_system_score_gemma":0.000025189,"threshold_uncertainty_score":0.9924533},"labels":[],"label_agreement":null},{"id":"W4200378330","doi":"10.3389/frsen.2021.712093","title":"A Comparison of Multi-Angle Implementation of Atmospheric Correction and MOD09 Daily Surface Reflectance Products From MODIS","year":2021,"lang":"en","type":"article","venue":"Frontiers in Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":15,"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":"Goddard Space Flight Center; National Aeronautics and Space Administration","keywords":"Atmospheric correction; Remote sensing; Environmental science; Reflectivity; Radiative transfer; Aerosol; Bidirectional reflectance distribution function; Atmospheric sciences; Meteorology; Geology; Geography; Physics; Optics","score_opus":0.017222381836680015,"score_gpt":0.28577843839837114,"score_spread":0.2685560565616911,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200378330","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":[0.83935255,0.0006643104,0.15917687,0.000045595665,0.00047974059,0.00012416112,0.0000035780618,0.000010695261,0.00014251153],"genre_scores_gemma":[0.6091287,0.00004030016,0.3906927,0.000012484087,0.000008381484,3.7371663e-8,0.0000062781564,0.000008596601,0.00010250033],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9988852,0.0000825437,0.00033368246,0.00033467912,0.00019456891,0.00016931853],"domain_scores_gemma":[0.99949676,0.000019749425,0.00022080365,0.00020139385,0.000026889693,0.00003441748],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000104445695,0.000114723625,0.0002943001,0.0000010362133,0.00005153658,0.000009805584,0.000052380972,0.000058868205,0.00003110793],"category_scores_gemma":[0.000035903016,0.00012450606,0.000027788783,0.00040635825,0.000116782154,0.00010599271,0.00007509638,0.000098274824,0.0000011751085],"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":[0.000038840823,0.000051039904,0.506489,0.000016890697,0.000020032237,0.000005425691,0.0037700825,0.0209345,0.17853457,3.287464e-7,0.0013983403,0.28874093],"study_design_scores_gemma":[0.00048304204,0.000041075677,0.16145171,0.000047914724,0.000021753436,0.000002721807,0.0063730795,0.7474815,0.08379723,0.0000700473,0.000094373325,0.00013550925],"about_ca_topic_score_codex":0.0063544945,"about_ca_topic_score_gemma":0.0017974993,"teacher_disagreement_score":0.72654706,"about_ca_system_score_codex":0.00013991498,"about_ca_system_score_gemma":0.000023336253,"threshold_uncertainty_score":0.9606137},"labels":[],"label_agreement":null},{"id":"W4200382832","doi":"10.5194/amt-2021-251-rc2","title":"Comment on amt-2021-251","year":2021,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"University of Alberta","funders":"National Oceanic and Atmospheric Administration; National Aeronautics and Space Administration","keywords":"Scalable Vector Graphics; Nephelometer; Polarimetry; Optics; Span (engineering); Remote sensing; Physics; Computer science; Geology; Engineering","score_opus":0.01956864716923483,"score_gpt":0.26937505930354433,"score_spread":0.24980641213430949,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200382832","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000026856384,0.007284824,0.00018100529,0.31098104,0.0015710194,0.00037057427,0.00003831276,0.000038765622,0.6795076],"genre_scores_gemma":[0.00006639953,0.012741162,0.0014303967,0.17904279,0.00023385973,0.000058210073,0.00031942272,0.00003593669,0.8060718],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99789804,0.000071370036,0.00031765958,0.0006149462,0.0007467945,0.00035119592],"domain_scores_gemma":[0.99890876,0.00004966299,0.000128948,0.0007429987,0.000009950139,0.00015967774],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00020633418,0.00035078803,0.0005100772,5.675654e-7,0.000102864986,0.000034537134,0.0004433442,0.00018978084,0.340908],"category_scores_gemma":[0.000031256484,0.00026898997,0.00023354657,0.00019718232,0.00009579835,0.000029391327,0.00054512627,0.0003981348,0.008682243],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000010903223,0.00008841442,0.00007821897,0.0001096632,0.000016891423,0.000023050312,0.000009252384,0.0000112216685,0.0000024748363,0.0000901736,0.97699755,0.022572001],"study_design_scores_gemma":[0.00008766141,0.00006839795,0.00014586122,0.0006952413,0.000049993952,0.0000032695327,0.000018217193,0.000016644883,0.000019637386,0.00003522697,0.9985223,0.00033754917],"about_ca_topic_score_codex":0.00089132466,"about_ca_topic_score_gemma":0.0002128154,"teacher_disagreement_score":0.33222574,"about_ca_system_score_codex":0.00030567282,"about_ca_system_score_gemma":0.000027216618,"threshold_uncertainty_score":0.9999762},"labels":[],"label_agreement":null},{"id":"W4200452030","doi":"10.5194/amt-2021-333-rc1","title":"Comment on amt-2021-333","year":2021,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Human Exploration and Operations Mission Directorate; Science Mission Directorate; European Space Agency; Langley Research Center; National Aeronautics and Space Administration","keywords":"Aerosol; Sulfuric acid; Plume; Volcano; Smoke; Environmental science; Context (archaeology); Atmospheric sciences; Extinction (optical mineralogy); Vulcanian eruption; Northern Hemisphere; Meteorology; Atmosphere (unit); Geology; Remote sensing; Mineralogy; Chemistry; Geography; Geochemistry","score_opus":0.019582044100413466,"score_gpt":0.2693918815644849,"score_spread":0.24980983746407143,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200452030","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00003119078,0.005889392,0.00021689854,0.30959862,0.0016054254,0.0003731044,0.000040092225,0.000039015158,0.6822063],"genre_scores_gemma":[0.00008830168,0.009793085,0.0014604558,0.17889659,0.00023364884,0.000058459136,0.0003169192,0.000036020905,0.80911654],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99790025,0.00007128979,0.000317327,0.00061490404,0.0007453635,0.0003508526],"domain_scores_gemma":[0.9989086,0.000049509687,0.00012885238,0.0007435666,0.000009937355,0.00015957557],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00020611411,0.00035069973,0.0005091825,5.6885807e-7,0.000102735416,0.0000346462,0.0004439283,0.0001897092,0.339871],"category_scores_gemma":[0.000031010375,0.00026905182,0.00023337349,0.0001972758,0.00009584436,0.000029406034,0.0005483984,0.00039969618,0.008917451],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000001087667,0.00008850965,0.00006789791,0.00010970762,0.000016924609,0.000030418772,0.000009123288,0.000013842547,0.0000025189754,0.000091238944,0.979676,0.019892693],"study_design_scores_gemma":[0.00008744628,0.00006714182,0.00014023775,0.00069252687,0.0000499733,0.000004478444,0.000017894077,0.000019199893,0.000017837796,0.00003670234,0.99852896,0.00033760033],"about_ca_topic_score_codex":0.00087192765,"about_ca_topic_score_gemma":0.0002081114,"teacher_disagreement_score":0.33095354,"about_ca_system_score_codex":0.00030526012,"about_ca_system_score_gemma":0.000027444878,"threshold_uncertainty_score":0.99997616},"labels":[],"label_agreement":null},{"id":"W4205125203","doi":"10.1002/essoar.10504688.1","title":"Seasonal and solar wind sector duration influences on the correlations of high latitude clouds with ionospheric potential.","year":2020,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"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":"Preprint; Space Science; Ionosphere; China; High latitude; Latitude; Christian ministry; Meteorology; Solar wind; Atmospheric sciences; Geography; Geology; Geophysics; Computer science; World Wide Web; Physics; Geodesy; Political science; Astronomy","score_opus":0.010419483753796798,"score_gpt":0.2009141079758252,"score_spread":0.1904946242220284,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4205125203","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":[0.97792757,0.00003146718,0.017390622,0.0018109577,0.00014947949,0.0003862178,0.000016433212,0.000033407192,0.0022538465],"genre_scores_gemma":[0.99254906,0.000037239424,0.006524625,0.00039173412,0.00008143363,0.000016993334,0.00001789099,0.000015552934,0.0003654512],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9987264,0.000051294734,0.00024812133,0.0003944406,0.00043699902,0.00014274336],"domain_scores_gemma":[0.9993359,0.000059635287,0.00025208996,0.00025577896,0.000015384367,0.000081232356],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000103119826,0.00021496152,0.00020937785,7.4579657e-7,0.0001812926,0.000059610207,0.00023042991,0.00013469892,0.0035272879],"category_scores_gemma":[0.000019575553,0.00012821119,0.000050555187,0.00014909732,0.00032432206,0.00008364345,0.00037458533,0.00033534988,0.00005444958],"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":[0.00011055354,0.00012842903,0.34245908,0.0000442624,0.00015775414,0.000007629817,0.00093060994,0.6463494,0.0013527877,0.003925391,0.0028860918,0.0016480465],"study_design_scores_gemma":[0.00022684303,0.00020366148,0.9584126,0.00005216789,0.00008434889,0.0000038859744,0.00023575245,0.037066437,0.0002619789,0.0028386894,0.00034196608,0.00027168306],"about_ca_topic_score_codex":0.0008991887,"about_ca_topic_score_gemma":0.0001369486,"teacher_disagreement_score":0.6159535,"about_ca_system_score_codex":0.00005078687,"about_ca_system_score_gemma":0.000043642718,"threshold_uncertainty_score":0.9973836},"labels":[],"label_agreement":null},{"id":"W4205524195","doi":"10.5194/acp-2020-982","title":"Measurement Report: Lidar measurements of stratospheric aerosol following the Raikoke and Ulawun volcanic eruptions","year":2020,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Natural Environment Research Council; Sight Research UK","keywords":"Lidar; Aerosol; Volcano; Stratosphere; Troposphere; Radiosonde; Atmospheric sciences; Plume; Environmental science; Backscatter (email); Vulcanian eruption; Extinction (optical mineralogy); Geology; Meteorology; Mineralogy; Remote sensing; Physics; Seismology","score_opus":0.04958570798723626,"score_gpt":0.25695133372292206,"score_spread":0.2073656257356858,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4205524195","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":[0.92316157,0.0015443219,0.019195868,0.002434003,0.0011264068,0.002039423,0.000012312195,0.0001846066,0.050301496],"genre_scores_gemma":[0.9943532,0.000051646457,0.004551282,0.00029253596,0.00007368113,0.0000964135,0.0000064600304,0.00004409416,0.00053072086],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9960162,0.00013061153,0.00081301434,0.0008818118,0.0017700219,0.00038836323],"domain_scores_gemma":[0.99826837,0.000020855745,0.00052579865,0.00092299713,0.000042197087,0.0002197707],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010199915,0.00044162586,0.00053085916,0.0000012401027,0.0002700184,0.00009340113,0.0006294347,0.00021517764,0.0010066107],"category_scores_gemma":[0.00013216039,0.000316028,0.00033561286,0.00023968036,0.0002713208,0.00009633135,0.0014937146,0.00050973345,0.000056478453],"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":[0.000100634315,0.0009513902,0.6727449,0.0005573596,0.002448298,0.00031671027,0.0041648177,0.012148096,0.27476984,0.00021467773,0.011272712,0.020310525],"study_design_scores_gemma":[0.0054098507,0.0013520324,0.86924374,0.0018691402,0.004460051,0.00028226853,0.0061316877,0.007906302,0.07650552,0.007168546,0.012533025,0.007137826],"about_ca_topic_score_codex":0.0014743322,"about_ca_topic_score_gemma":0.0010256834,"teacher_disagreement_score":0.19826432,"about_ca_system_score_codex":0.00029352022,"about_ca_system_score_gemma":0.00012924227,"threshold_uncertainty_score":0.9999292},"labels":[],"label_agreement":null},{"id":"W4205784516","doi":"10.5194/amt-2021-148-rc3","title":"Comment on amt-2021-148","year":2021,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"National Research Council Canada","funders":"Environment and Climate Change Canada; Université du Québec à Montréal","keywords":"Snow; Radar; Remote sensing; Meteorology; Particle (ecology); Environmental science; Snowflake; Range (aeronautics); Ice crystals; Storm; Atmospheric sciences; Geology; Geography; Materials science; Computer science; Telecommunications","score_opus":0.01949749239060603,"score_gpt":0.2692027377827111,"score_spread":0.24970524539210506,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4205784516","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000034661,0.0060755853,0.00020994782,0.30658886,0.0016015328,0.0003726642,0.000039751496,0.00003927186,0.68503773],"genre_scores_gemma":[0.00008525884,0.009840629,0.0014228115,0.18009642,0.0002329405,0.000058690297,0.00031320457,0.000036154244,0.8079139],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9979041,0.00007101377,0.0003171195,0.00061391824,0.00074314035,0.0003506662],"domain_scores_gemma":[0.99891126,0.00004825576,0.00012868323,0.0007427793,0.000009897022,0.00015912612],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00020555382,0.0003504301,0.0005083644,5.6892594e-7,0.000102559345,0.00003451894,0.00044453013,0.00018949261,0.34507737],"category_scores_gemma":[0.000031065407,0.00026886738,0.00023083106,0.00019896697,0.00009571938,0.000029021237,0.0005487196,0.00040279716,0.009017746],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000001125333,0.00010859992,0.000067376655,0.00011124551,0.000016576718,0.00002260681,0.000008938078,0.00001368819,0.0000023396708,0.00008771593,0.97347844,0.026081344],"study_design_scores_gemma":[0.000092653085,0.00010274985,0.00012941525,0.0007136148,0.00004972856,0.0000031101993,0.000017949498,0.000018890883,0.000019389063,0.000035738503,0.99847937,0.000337372],"about_ca_topic_score_codex":0.00084991154,"about_ca_topic_score_gemma":0.00020970893,"teacher_disagreement_score":0.3360596,"about_ca_system_score_codex":0.00029690797,"about_ca_system_score_gemma":0.000027456937,"threshold_uncertainty_score":0.99997634},"labels":[],"label_agreement":null},{"id":"W4205964911","doi":"10.1029/2021jd035483","title":"Uncertainty in Aerosol Optical Depth From Modern Aerosol‐Climate Models, Reanalyses, and Satellite Products","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":58,"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":"Natural Environment Research Council; Centre National d’Etudes Spatiales; Sight Research UK; Deutsche Forschungsgemeinschaft; Bundesministerium für Verkehr und Digitale Infrastruktur; Langley Research Center; National Aeronautics and Space Administration","keywords":"Aerosol; Satellite; Coupled model intercomparison project; Environmental science; Meteorology; Climatology; Climate model; Scale (ratio); Remote sensing; Atmospheric sciences; Climate change; Geography; Geology","score_opus":0.03762607466118828,"score_gpt":0.2971672837814599,"score_spread":0.2595412091202716,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4205964911","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":[0.99378777,0.0014512086,0.000260078,0.00091322674,0.0000794862,0.00026457486,0.000012712065,0.000014033083,0.003216902],"genre_scores_gemma":[0.99379116,0.0008544063,0.004589648,0.000109389075,0.00018620113,0.000027300226,0.000006074547,0.00003832342,0.00039746778],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9948205,0.00057081314,0.0006889097,0.0006060376,0.0023409505,0.00097284093],"domain_scores_gemma":[0.99830705,0.00048648065,0.00023167602,0.00043627826,0.000097206284,0.00044132108],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015147512,0.00026173284,0.000555265,0.0000044778867,0.00044644522,0.00012523943,0.00075801526,0.00007913243,0.0007134016],"category_scores_gemma":[0.00026995703,0.000213691,0.00014615578,0.0009123528,0.000604937,0.00048238292,0.001436261,0.0015908101,0.000046420726],"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":[0.004962147,0.004105568,0.108958565,0.000090358924,0.00034164955,0.0017990498,0.0045718066,0.5188465,0.09948565,0.0019341533,0.006235365,0.24866915],"study_design_scores_gemma":[0.0063877064,0.0056785154,0.29401255,0.00024428667,0.00019290559,0.00019530285,0.007390982,0.59175277,0.00475998,0.08113813,0.006379749,0.001867148],"about_ca_topic_score_codex":0.004393128,"about_ca_topic_score_gemma":0.0010772909,"teacher_disagreement_score":0.246802,"about_ca_system_score_codex":0.0005514654,"about_ca_system_score_gemma":0.00014383407,"threshold_uncertainty_score":0.8714066},"labels":[],"label_agreement":null},{"id":"W4206566133","doi":"10.5194/acp-2021-338-rc2","title":"Comment on acp-2021-338","year":2021,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"Academy of Finland","keywords":"Drizzle; Ice crystals; Supercooling; Span (engineering); Precipitation; Ice nucleus; Cloud physics; Atmospheric sciences; Materials science; Meteorology; Physics; Nucleation; Cloud computing; Thermodynamics","score_opus":0.020220068159900562,"score_gpt":0.2715584665216206,"score_spread":0.25133839836172,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4206566133","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000033198532,0.0059098992,0.0001960452,0.32386124,0.0016018926,0.0003703671,0.00003965389,0.000038131566,0.66794956],"genre_scores_gemma":[0.000076399716,0.009834774,0.0014081058,0.17479627,0.00023566895,0.000057519665,0.00030983478,0.00003584985,0.8132456],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99790734,0.00007154596,0.00031425917,0.00061427074,0.0007394509,0.00035311296],"domain_scores_gemma":[0.9989008,0.000050836217,0.00012762529,0.00075179635,0.000009898733,0.00015907393],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00021066146,0.00035164508,0.00050836103,5.5814155e-7,0.0001018513,0.0000356667,0.00045932105,0.00019691128,0.35292107],"category_scores_gemma":[0.00003423481,0.00026865708,0.00023253897,0.00019620817,0.00009221516,0.0000316911,0.00057947816,0.00040575044,0.0090389],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000011225256,0.00008846373,0.00006189433,0.00010957459,0.000017255934,0.000022642562,0.0000093145845,0.000013291463,0.0000035739076,0.000079513266,0.97872823,0.0208651],"study_design_scores_gemma":[0.00008809497,0.00006762398,0.00015363655,0.0006788924,0.000050218223,0.0000033596696,0.000018773113,0.000018414068,0.000022818369,0.000033514465,0.99853003,0.00033459673],"about_ca_topic_score_codex":0.00072295265,"about_ca_topic_score_gemma":0.00017553559,"teacher_disagreement_score":0.34388217,"about_ca_system_score_codex":0.00030278633,"about_ca_system_score_gemma":0.000028476365,"threshold_uncertainty_score":0.9999766},"labels":[],"label_agreement":null},{"id":"W4206625620","doi":"10.1029/2021jg006707","title":"Advancing Cross‐Disciplinary Understanding of Land‐Atmosphere Interactions","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Biogeosciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":22,"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","funders":"Lawrence Livermore National Laboratory; National Science Foundation","keywords":"Discipline; Breakout; Instrumentation (computer programming); Political science; Computer science; Business","score_opus":0.05675936837922226,"score_gpt":0.37061090822863707,"score_spread":0.31385153984941483,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4206625620","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":[0.9934995,0.000077679295,0.00085276994,0.0007445335,0.00031488374,0.00007902926,0.000007859867,0.0000050448803,0.0044186865],"genre_scores_gemma":[0.997952,0.000034043587,0.0011156817,0.000025350213,0.000098486926,0.000004776843,4.5672903e-7,0.0000067776614,0.0007624391],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99681437,0.00022105128,0.0003878599,0.00021037541,0.0019201522,0.0004462072],"domain_scores_gemma":[0.99888957,0.00041161705,0.00028658865,0.00015553186,0.000058871432,0.00019783652],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0019960802,0.00008925504,0.00020481943,0.000008151493,0.0010674329,0.000060464958,0.00075478485,0.00001922748,0.0029474031],"category_scores_gemma":[0.00020629502,0.0000667851,0.00015119064,0.0013639593,0.0011033954,0.00051153306,0.00096128485,0.0006265783,0.000022199314],"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":[0.00023268422,0.00070525863,0.9546228,0.000016656968,0.00002332496,0.00007495306,0.0012387069,0.0040307413,0.030253537,0.0011790742,0.0040831505,0.0035391124],"study_design_scores_gemma":[0.0008755299,0.0050264555,0.8902337,0.00010913602,0.000023761908,0.00017139353,0.027591085,0.013377726,0.0021419688,0.04493793,0.015127374,0.00038395505],"about_ca_topic_score_codex":0.0016101508,"about_ca_topic_score_gemma":0.00012508176,"teacher_disagreement_score":0.06438912,"about_ca_system_score_codex":0.0005312579,"about_ca_system_score_gemma":0.00013445629,"threshold_uncertainty_score":0.997964},"labels":[],"label_agreement":null},{"id":"W4206856018","doi":"10.5194/acpd-7-8309-2007","title":"Data assimilation of dust aerosol observations for CUACE/Dust forecasting system","year":2007,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","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":"Environment and Climate Change Canada","funders":"National Key Research and Development Program of China","keywords":"Dust storm; Data assimilation; Environmental science; Visibility; Meteorology; Aerosol; Asian Dust; Storm; Satellite; Atmospheric sciences; Geostationary orbit; Climatology; Remote sensing; Geography; Geology","score_opus":0.1841188684833483,"score_gpt":0.30427702768093773,"score_spread":0.12015815919758943,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4206856018","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.24439965,0.000045864505,0.7116731,0.00024199323,0.00080079545,0.0018021864,0.00082495355,0.00017102357,0.040040452],"genre_scores_gemma":[0.8400893,0.0000088155975,0.15592575,0.0000820149,0.00019882628,0.000078329336,0.0010116808,0.00004234396,0.0025629462],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99784756,0.000025774452,0.0006836793,0.00070024014,0.0004119011,0.0003308657],"domain_scores_gemma":[0.9979146,0.0001622236,0.0005665542,0.001218794,0.000041065457,0.000096754746],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000736159,0.00026170062,0.00035337318,0.0000026303921,0.0001851036,0.000045602228,0.00093075586,0.00035451446,0.00042364243],"category_scores_gemma":[0.00012365484,0.0002376173,0.00010384204,0.00018493507,0.00011921929,0.00021040595,0.0021760415,0.00025316858,0.000019169263],"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":[0.00013337673,0.00056218065,0.6090552,0.0027535446,0.00032575786,0.0000090906715,0.0009847023,0.20895249,0.004237652,0.0034408297,0.13351709,0.036028095],"study_design_scores_gemma":[0.00043338875,0.000063263346,0.052666485,0.00032946505,0.00016847752,0.0000054920465,0.0010641133,0.93834543,0.0007240459,0.00013731659,0.0054783756,0.0005841446],"about_ca_topic_score_codex":0.0008088057,"about_ca_topic_score_gemma":0.000635194,"teacher_disagreement_score":0.72939295,"about_ca_system_score_codex":0.00028244485,"about_ca_system_score_gemma":0.000048904985,"threshold_uncertainty_score":0.96897525},"labels":[],"label_agreement":null},{"id":"W4206974307","doi":"10.5194/gmd-2021-148-rc2","title":"Comment on gmd-2021-148","year":2021,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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","funders":"National Natural Science Foundation of China; National Science Foundation","keywords":"Scalable Vector Graphics; Span (engineering); Aerosol; Cloud computing; Meteorology; Mathematics; Environmental science; Atmospheric sciences; Simulation; Computer science; Engineering; Geography; Physics; Structural engineering; Operating system","score_opus":0.019572122615733666,"score_gpt":0.2693864209049547,"score_spread":0.24981429828922103,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4206974307","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000032050284,0.006292314,0.00019738385,0.30102098,0.0015920902,0.00036340076,0.000039325518,0.00003801364,0.69042444],"genre_scores_gemma":[0.00008210095,0.00978548,0.0013899643,0.1744411,0.00023464728,0.000053695578,0.0003052081,0.000036171245,0.81367165],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9979032,0.00007118619,0.00031823458,0.00061540236,0.00074025086,0.00035169802],"domain_scores_gemma":[0.9989094,0.000049239985,0.00012762133,0.00074457686,0.000009923914,0.00015925252],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00020984575,0.0003511914,0.00050847745,5.686758e-7,0.000102529884,0.000033993823,0.00044235357,0.00019264594,0.35731673],"category_scores_gemma":[0.000032755514,0.00026941363,0.00023145387,0.00019797847,0.00009307566,0.000029095196,0.00054791704,0.0004035573,0.009030802],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000011245287,0.000109611385,0.00006544589,0.000113875925,0.000016629141,0.000022712175,0.000008850454,0.0000139675385,0.0000023341418,0.00008426145,0.9732868,0.026274404],"study_design_scores_gemma":[0.00009362264,0.00010292467,0.00011465803,0.0007165381,0.000050037375,0.00000325518,0.000018067365,0.000020085517,0.000020261014,0.00003455016,0.998488,0.00033801337],"about_ca_topic_score_codex":0.0007998268,"about_ca_topic_score_gemma":0.00018719134,"teacher_disagreement_score":0.3482859,"about_ca_system_score_codex":0.00029689836,"about_ca_system_score_gemma":0.000028442133,"threshold_uncertainty_score":0.9999758},"labels":[],"label_agreement":null},{"id":"W4210379937","doi":"10.1029/2021jd035871","title":"Meteorological Conditions Favorable for Strong Anthropogenic Aerosol Impacts on Clouds","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":5,"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":"Eesti Teadusagentuur","keywords":"Aerosol; Environmental science; Anticyclone; Cloud computing; Atmospheric sciences; Pollution; Meteorology; Track (disk drive); Synoptic scale meteorology; Climatology; Geography; Geology","score_opus":0.043722045613608054,"score_gpt":0.347363546722939,"score_spread":0.30364150110933097,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4210379937","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":[0.9949218,0.00013633113,0.0007396866,0.001074147,0.00021580036,0.0004130255,0.000044210643,0.00001697768,0.0024380172],"genre_scores_gemma":[0.99619836,0.000045453344,0.0016739914,0.00021911314,0.00032538435,0.000079748585,0.000005278235,0.000031525306,0.0014211315],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99587417,0.0004893246,0.0004801512,0.00034436793,0.0019044995,0.000907461],"domain_scores_gemma":[0.9978373,0.0010307044,0.00026126066,0.00031190782,0.000103511455,0.00045532652],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014593173,0.00020121757,0.00040626165,0.0000028050147,0.0012930656,0.00007915743,0.0007960563,0.00007017601,0.012827662],"category_scores_gemma":[0.0005033823,0.00015353382,0.00038571522,0.0005987645,0.00068442395,0.00022459052,0.00053897465,0.0011779165,0.00017519863],"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":[0.008696708,0.010611272,0.046429552,0.000079550635,0.00082580885,0.0007154042,0.001099691,0.12822425,0.17477244,0.022894626,0.57678974,0.028860936],"study_design_scores_gemma":[0.017124683,0.13670835,0.3981158,0.0001902534,0.0004208926,0.00052281184,0.018269125,0.04202135,0.025973095,0.08853606,0.26912054,0.002997033],"about_ca_topic_score_codex":0.00033864757,"about_ca_topic_score_gemma":0.000029178025,"teacher_disagreement_score":0.35168624,"about_ca_system_score_codex":0.0006071114,"about_ca_system_score_gemma":0.0001575343,"threshold_uncertainty_score":0.99453455},"labels":[],"label_agreement":null},{"id":"W4210455668","doi":"10.5194/amt-2021-2-cc1","title":"Comment on amt-2021-2","year":2021,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Goddard Space Flight Center; Stony Brook University; Nuclear Safety and Security Commission; National Center for Atmospheric Research; Environment and Climate Change Canada; Colorado State University; National Aeronautics and Space Administration","keywords":"Environmental science; Remote sensing; Radar; Radiometer; Cloud computing; Computer science; Brightness temperature; Precipitation; Meteorology; Bayesian probability; Geology; Geography; Artificial intelligence","score_opus":0.01982775222583304,"score_gpt":0.26983734121286157,"score_spread":0.2500095889870285,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4210455668","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000021447056,0.0053208303,0.0001730204,0.31968212,0.0013551554,0.00030635463,0.000030570725,0.000031879354,0.67307866],"genre_scores_gemma":[0.00005494476,0.009215997,0.0013151692,0.18963534,0.00020362432,0.00004992225,0.0002856781,0.00003064227,0.7992087],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9981196,0.000062126055,0.000279869,0.0005517205,0.00067702075,0.0003096643],"domain_scores_gemma":[0.99902236,0.000043486834,0.00011218207,0.00067461637,0.000008544432,0.00013877806],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00018224769,0.000310978,0.00045555277,4.5978592e-7,0.00008908738,0.000029175231,0.0003925528,0.00016775419,0.35394165],"category_scores_gemma":[0.000027836273,0.0002372671,0.00020791893,0.00017586985,0.00008319897,0.000024789437,0.0004896895,0.00035781148,0.008677546],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[8.7903027e-7,0.00007696447,0.00006481486,0.00009718433,0.000014291464,0.00002026231,0.0000074094933,0.0000113590995,0.0000019607432,0.000084434534,0.9799147,0.019705689],"study_design_scores_gemma":[0.00007483124,0.000059519338,0.00011895913,0.0006514871,0.00004312062,0.000002767302,0.000014522419,0.00001558172,0.000018153856,0.000032089196,0.9986708,0.00029817803],"about_ca_topic_score_codex":0.000770917,"about_ca_topic_score_gemma":0.00018249374,"teacher_disagreement_score":0.3452641,"about_ca_system_score_codex":0.00026887117,"about_ca_system_score_gemma":0.000023231874,"threshold_uncertainty_score":0.99209434},"labels":[],"label_agreement":null},{"id":"W4210669631","doi":"10.3390/atmos13020187","title":"Simulation of Arctic Thin Ice Clouds with Canadian Regional Climate Model Version 6: Verification against CloudSat-CALIPSO","year":2022,"lang":"en","type":"article","venue":"Atmosphere","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université de Sherbrooke; Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency; Université du Québec à Montréal; Environment and Climate Change Canada; Colorado State University","keywords":"Environmental science; Stratosphere; Troposphere; Atmospheric sciences; Climatology; Arctic; Latitude; Ice cloud; Polar; Cirrus; Effective radius; Climate model; Altitude (triangle); Climate change; Geology; Satellite; Oceanography","score_opus":0.011145528001863494,"score_gpt":0.21023142109598103,"score_spread":0.19908589309411753,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4210669631","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":[0.9912819,0.000056175206,0.0015632167,0.0003726024,0.00007405012,0.00026192167,0.000028878578,0.000038135553,0.006323095],"genre_scores_gemma":[0.9945767,0.0000149784,0.003887767,0.00072197296,0.000024271123,0.000029013492,0.00007586187,0.000031190702,0.00063823495],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9983543,0.00007606898,0.00024900417,0.00037681803,0.0005801093,0.00036369546],"domain_scores_gemma":[0.9991643,0.000059339316,0.00018635421,0.0003829271,0.000024267127,0.0001828331],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00024554748,0.0001718712,0.00016698631,6.9472e-7,0.0005489126,0.000015064551,0.00029800547,0.00006737492,0.002119168],"category_scores_gemma":[0.000017045266,0.0001648532,0.00006259915,0.000379647,0.00013842994,0.00016564535,0.00014714124,0.00020902605,0.000101834594],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000111983914,0.00006498173,0.07624316,0.000012288318,0.00001034926,0.0000046660243,0.0004873978,0.92110175,0.00012603196,0.00023347492,0.0009187368,0.00068520335],"study_design_scores_gemma":[0.00043745528,0.00015915785,0.030592145,0.0000152427965,0.000029123652,0.000002800188,0.000871894,0.9626001,0.000021446198,0.00019305291,0.0048493445,0.0002282015],"about_ca_topic_score_codex":0.026355973,"about_ca_topic_score_gemma":0.009770054,"teacher_disagreement_score":0.04565102,"about_ca_system_score_codex":0.00072506454,"about_ca_system_score_gemma":0.00010901911,"threshold_uncertainty_score":0.998793},"labels":[],"label_agreement":null},{"id":"W4211108427","doi":"10.5194/acpd-14-22045-2014","title":"A comprehensive laboratory study on the immersion freezing behavior of illite NX particles: a comparison of seventeen ice nucleation measurement techniques","year":2014,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":9,"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":"Pacific Northwest National Laboratory; Japan Society for the Promotion of Science; Alexander von Humboldt-Stiftung; Battelle; Deutsche Forschungsgemeinschaft; Natural Environment Research Council; U.S. Department of Energy; National Science Foundation","keywords":"Ice nucleus; Nucleation; Immersion (mathematics); Illite; Mineralogy; Chemistry; Materials science; Thermodynamics; Physics; Clay minerals","score_opus":0.05026382932976424,"score_gpt":0.29318868463249687,"score_spread":0.2429248553027326,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4211108427","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":[0.9950752,0.000053205556,0.002345727,0.000096020754,0.00006432616,0.0014544501,0.000009499329,0.0000419202,0.000859628],"genre_scores_gemma":[0.9979325,0.000010488517,0.0017698306,0.00009990528,0.000015897345,0.00013120616,0.0000029971775,0.000020103633,0.000017086402],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9976503,0.00029251614,0.0005650264,0.0003801121,0.00094321347,0.00016881515],"domain_scores_gemma":[0.9985552,0.00006411724,0.00058523973,0.0006397267,0.00010619312,0.000049530132],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006263628,0.00023230133,0.00041762763,0.0000033711847,0.00009556021,0.000016078162,0.00040106333,0.000118372336,0.00034046735],"category_scores_gemma":[0.000022241575,0.00015923657,0.000103593455,0.00014153396,0.00019308919,0.000039423445,0.0006515456,0.00027676165,0.000026021067],"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":[0.00012217298,0.00363919,0.66919863,0.00012636822,0.00013319754,0.0000014943614,0.008883866,0.0030380304,0.2987006,0.00007843033,0.0021768545,0.013901186],"study_design_scores_gemma":[0.0005676895,0.0016334526,0.7039817,0.0005136869,0.0003920241,3.1926888e-7,0.0332716,0.0041270945,0.25358954,0.000073402254,0.0012711922,0.00057830714],"about_ca_topic_score_codex":0.0011826038,"about_ca_topic_score_gemma":0.00007864602,"teacher_disagreement_score":0.045111056,"about_ca_system_score_codex":0.00020759755,"about_ca_system_score_gemma":0.000019019593,"threshold_uncertainty_score":0.6493479},"labels":[],"label_agreement":null},{"id":"W4211187250","doi":"10.1002/9781119300762.wsts0140","title":"Low‐Level Ice Clouds–Ice Fog","year":2019,"lang":"en","type":"other","venue":"Encyclopedia of Water","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ontario Tech University","funders":"","keywords":"Ice nucleus; Environmental science; Ice cloud; Ice crystals; Meteorology; Sea ice growth processes; Visibility; Water cycle; Atmospheric sciences; Cloud computing; Sea ice thickness; Arctic ice pack; Geology; Geography; Sea ice; Nucleation; Computer science; Physics","score_opus":0.007576961356494485,"score_gpt":0.20679284237058568,"score_spread":0.19921588101409118,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4211187250","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.01070167,0.000121553254,0.00023183177,0.00011064617,0.0011018168,0.0003771893,0.00004557193,0.00008226872,0.98722744],"genre_scores_gemma":[0.004879356,0.0004568212,0.002075583,0.0002438188,0.00044983724,0.000020297759,0.000035262256,0.00035349902,0.99148554],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9981268,0.000040671228,0.0003247013,0.0005386181,0.0004756795,0.0004935401],"domain_scores_gemma":[0.9989995,0.000020907592,0.00017885529,0.00067867356,0.0000057854454,0.000116297335],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00012213737,0.00038248047,0.0004466119,0.000004179014,0.00003548195,0.000012235134,0.0005768651,0.00037348885,0.06500831],"category_scores_gemma":[0.000009334603,0.00026265235,0.00014767773,0.000092341885,0.0001951723,0.00006755719,0.0004291493,0.00023291165,0.019524334],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011618738,0.0000970629,0.0038053428,0.00008297203,0.000039017337,0.00001158681,0.00047151448,0.000037207024,0.00051301613,0.000020911775,0.9895651,0.0053447024],"study_design_scores_gemma":[0.00028079058,0.000057783513,0.0012839617,0.000063814005,0.00003952752,0.0000027713663,0.000038973652,0.000010423994,0.0006888938,0.000079104546,0.99703014,0.00042384173],"about_ca_topic_score_codex":0.0016186639,"about_ca_topic_score_gemma":0.00018060082,"teacher_disagreement_score":0.045483977,"about_ca_system_score_codex":0.000064493186,"about_ca_system_score_gemma":0.000016123353,"threshold_uncertainty_score":0.9999826},"labels":[],"label_agreement":null},{"id":"W4212899034","doi":"10.5194/amt-2021-247-rc1","title":"Comment on amt-2021-247","year":2021,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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; Environment and Climate Change Canada; University of Toronto","funders":"","keywords":"Radiosonde; Lidar; Environmental science; Arctic; Meteorology; Satellite; Radar; Climatology; Atmospheric sciences; Remote sensing; Geography; Geology; Computer science; Telecommunications","score_opus":0.01956864716923483,"score_gpt":0.26937505930354433,"score_spread":0.24980641213430949,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4212899034","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000034158456,0.006031768,0.0001680313,0.30544332,0.0015514247,0.00036649578,0.00003786877,0.00003832316,0.68632865],"genre_scores_gemma":[0.00007372642,0.007274021,0.0013597963,0.1737843,0.00022753028,0.00005672756,0.00031056622,0.000034991794,0.8168783],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.997901,0.00007077239,0.00031774378,0.00061406364,0.0007457247,0.00035065637],"domain_scores_gemma":[0.9989095,0.00004968091,0.00012888863,0.0007424962,0.000009949379,0.00015951926],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00020682758,0.00035054437,0.00050954,5.696085e-7,0.000102819504,0.000034603276,0.0004440577,0.0001895559,0.29324657],"category_scores_gemma":[0.000031154257,0.00026883706,0.00023338983,0.00019738052,0.000095691896,0.000029020042,0.00054776453,0.00039964705,0.0085311355],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000010934814,0.00008857659,0.000088118904,0.000109585395,0.000016922173,0.000023091701,0.000009332713,0.0000140747725,0.0000031026927,0.00007010272,0.9798541,0.019721886],"study_design_scores_gemma":[0.00008787558,0.000068284826,0.00014349674,0.0006945147,0.000049980503,0.0000032741975,0.000018360732,0.000015061248,0.000027220378,0.000035561665,0.99851924,0.00033711144],"about_ca_topic_score_codex":0.00089093886,"about_ca_topic_score_gemma":0.00018089589,"teacher_disagreement_score":0.28471544,"about_ca_system_score_codex":0.00030537907,"about_ca_system_score_gemma":0.000027071379,"threshold_uncertainty_score":0.9999764},"labels":[],"label_agreement":null},{"id":"W4214831516","doi":"10.5194/amt-15-1093-2022","title":"Laser imaging nephelometer for aircraft deployment","year":2022,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":8,"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 Alberta","funders":"National Oceanic and Atmospheric Administration; National Aeronautics and Space Administration","keywords":"Nephelometer; Polarimetry; Remote sensing; Optics; Lidar; Polarization (electrochemistry); Wavelength; Laser; Linear polarization; Detector; Physics; Environmental science; Scattering; Light scattering; Geology","score_opus":0.016249236622810123,"score_gpt":0.2239587368575465,"score_spread":0.2077095002347364,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4214831516","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.27079663,0.0008421078,0.6857345,0.0030559115,0.0009601094,0.0053520883,0.000027745959,0.0027309486,0.030499943],"genre_scores_gemma":[0.8217065,0.00001637077,0.17111158,0.0028804033,0.00007519008,0.0027617905,0.0000067663673,0.000079441445,0.0013620055],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99723613,0.00009506172,0.00036816532,0.0005756017,0.0011742353,0.0005507785],"domain_scores_gemma":[0.999194,0.000026018766,0.00015678404,0.0004640816,0.00003245301,0.00012660954],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010678467,0.00028116684,0.0002386963,7.027447e-7,0.00061167387,0.0000425514,0.0005100387,0.000034531404,0.0057185614],"category_scores_gemma":[0.000027532715,0.00027251535,0.00017563956,0.0003506682,0.00009220163,0.00016340971,0.00054242706,0.00017887045,0.000051009727],"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":[0.00010402963,0.0006675691,0.14802195,0.000024336503,0.00008228977,0.000020728496,0.0003899703,0.00105659,0.033708952,0.0001132112,0.27268443,0.543126],"study_design_scores_gemma":[0.00066655787,0.0005293129,0.009445845,0.000015222482,0.000076919416,0.00002150918,0.00035231235,0.006627343,0.022278683,0.0010803737,0.95809925,0.00080669066],"about_ca_topic_score_codex":0.0003292438,"about_ca_topic_score_gemma":0.000023041302,"teacher_disagreement_score":0.6854148,"about_ca_system_score_codex":0.0012411162,"about_ca_system_score_gemma":0.000031365893,"threshold_uncertainty_score":0.9999727},"labels":[],"label_agreement":null},{"id":"W4214883384","doi":"10.2172/1035875","title":"Investigations of the Microphysical, Radiative, and Dynamical Properties of Mixed-Phase Clouds (Final Report)","year":2010,"lang":"en","type":"report","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Brookhaven National Laboratory; McGill University","keywords":"Mixed phase; Radiative transfer; Phase (matter); Physics; Environmental science; Meteorology; Optics; Quantum mechanics","score_opus":0.028700927279088975,"score_gpt":0.2643135180322893,"score_spread":0.23561259075320035,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4214883384","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":[0.9841557,0.00012316495,0.00013492619,0.00019777243,0.00029692167,0.00032052278,0.000027964961,0.000012889742,0.014730112],"genre_scores_gemma":[0.9849244,0.00009576382,0.0026217438,0.00002797515,0.00007087151,0.000020493711,0.000011424969,0.00002424097,0.012203106],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99810266,0.00005394144,0.00062285934,0.0003659692,0.0006738129,0.00018073557],"domain_scores_gemma":[0.9985743,0.000029794497,0.000686048,0.00055248174,0.00005487579,0.000102474885],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002495059,0.00023012575,0.00044012797,0.0000017405296,0.00011463643,0.000013041266,0.0002992976,0.00025204112,0.00042573942],"category_scores_gemma":[0.00025181234,0.00013298677,0.0001608946,0.00018952903,0.0026072487,0.000056303277,0.00042152547,0.0004235974,0.000006314813],"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":[0.000061171406,0.0014924641,0.121651806,0.0005446841,0.00024135978,0.00004630699,0.0009298029,0.00023985468,0.82512933,0.0005414864,0.034699515,0.014422191],"study_design_scores_gemma":[0.0029377025,0.0011636593,0.4678521,0.001065349,0.0012304838,0.001326792,0.0007627589,0.0060513807,0.31540743,0.0025610575,0.19710027,0.0025410475],"about_ca_topic_score_codex":0.0024593817,"about_ca_topic_score_gemma":0.00035641805,"teacher_disagreement_score":0.50972193,"about_ca_system_score_codex":0.00008960224,"about_ca_system_score_gemma":0.00031358039,"threshold_uncertainty_score":0.96065164},"labels":[],"label_agreement":null},{"id":"W4214950510","doi":"10.5194/acp-2020-22","title":"Is the near-spherical shape the new black for smoke?","year":2020,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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":"H2020 European Research Council; European Regional Development Fund; Langley Research Center; Deutscher Akademischer Austauschdienst","keywords":"Stratosphere; Smoke; Troposphere; Particle (ecology); Computational physics; Materials science; Environmental science; Physics; Molecular physics; Optics; Atmospheric sciences; Meteorology; Geology","score_opus":0.0370066116699861,"score_gpt":0.2679335858100131,"score_spread":0.230926974140027,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4214950510","genre_codex":"commentary","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.19994588,0.00034284906,0.15614589,0.47816253,0.0011314575,0.003950376,0.000043037413,0.00030856088,0.15996943],"genre_scores_gemma":[0.8339774,0.00015565404,0.039447863,0.06096507,0.0010326173,0.00021129964,0.000015879776,0.00010441841,0.06408979],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99841315,0.000039919363,0.00022403624,0.0005949649,0.0003850953,0.0003428362],"domain_scores_gemma":[0.9988511,0.000140329,0.00012058361,0.00071721146,0.0000056398344,0.00016512818],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00016062231,0.00028366398,0.0002348607,9.807014e-8,0.0002910792,0.00020038293,0.001290457,0.0001945013,0.033524454],"category_scores_gemma":[0.000042554682,0.00013470462,0.0003150484,0.00012706795,0.0005444534,0.000033218563,0.0021161588,0.00051087444,0.0012939242],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024929848,0.000024572686,0.0036229182,0.000012209613,0.000049126862,0.0000013044008,0.0018471917,0.0031294555,0.000055872286,0.00039356004,0.97040194,0.0204369],"study_design_scores_gemma":[0.00022899488,0.00008379414,0.023586567,0.00000975561,0.00008478063,0.0000017562536,0.0005143552,0.1570262,0.0001215848,0.011187246,0.8067662,0.00038872406],"about_ca_topic_score_codex":0.0013995913,"about_ca_topic_score_gemma":0.000078159326,"teacher_disagreement_score":0.63403153,"about_ca_system_score_codex":0.000085179396,"about_ca_system_score_gemma":0.000072021234,"threshold_uncertainty_score":0.9994837},"labels":[],"label_agreement":null},{"id":"W4220678346","doi":"10.5194/acp-22-2975-2022","title":"The 2019 Raikoke volcanic eruption – Part 2: Particle-phase dispersion and concurrent wildfire smoke emissions","year":2022,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":65,"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":"Natural Environment Research Council; Sight Research UK","keywords":"Aerosol; Volcano; Environmental science; Stratosphere; Atmospheric sciences; Troposphere; Volcanic ash; Lidar; Plume; Sulfate aerosol; Vulcanian eruption; Meteorology; Explosive eruption; Geology; Pyroclastic rock; Remote sensing; Seismology; Geography","score_opus":0.00790285139776031,"score_gpt":0.23133719681969306,"score_spread":0.22343434542193275,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220678346","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":[0.9973009,0.0008138339,0.00023174907,0.00038155486,0.00010467998,0.00012126075,0.000017291499,0.00003071887,0.000998013],"genre_scores_gemma":[0.99265724,0.0006194151,0.000116667434,0.00013802243,0.00009749419,0.00004059401,0.000024951769,0.000014648322,0.006290964],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.998941,0.00003750244,0.00016547511,0.00032908283,0.00025578018,0.00027115064],"domain_scores_gemma":[0.99944556,0.00005789467,0.00008571555,0.00024197421,0.000003626368,0.00016520606],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00012952281,0.00016508401,0.00012492122,6.5254824e-9,0.0011925496,0.000046190227,0.00015467788,0.00003538421,0.002328289],"category_scores_gemma":[0.000009786958,0.00012863395,0.00005087609,0.00015622747,0.0002933814,0.00008993048,0.0003127486,0.00021006112,0.000013493773],"study_design_candidate":"design_other","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":[0.000079115496,0.00038926254,0.038382765,0.000016924683,0.000035899815,0.000007571374,0.00075412117,0.000998831,0.02927047,0.00013063948,0.013518366,0.91641605],"study_design_scores_gemma":[0.0034453047,0.0004336551,0.0361993,0.00003710125,0.00017885242,0.00007017126,0.0025304183,0.20596889,0.0066032116,0.0013203158,0.74208814,0.001124618],"about_ca_topic_score_codex":0.000118283526,"about_ca_topic_score_gemma":0.000002347429,"teacher_disagreement_score":0.9152914,"about_ca_system_score_codex":0.00008340343,"about_ca_system_score_gemma":0.000016006092,"threshold_uncertainty_score":0.99858373},"labels":[],"label_agreement":null},{"id":"W4220718088","doi":"10.5194/egusphere-egu22-8213","title":"Intercomparison of Ceilometer aerosol profiling versus Raman lidar including &amp;#160;pollution events and transported biomass burning aerosols across the United Kingdom","year":2022,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Lidar; Ceilometer; Aerosol; Environmental science; AERONET; Sun photometer; Remote sensing; Meteorology; Physics; Geography","score_opus":0.08300715952770726,"score_gpt":0.33188616067978677,"score_spread":0.2488790011520795,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220718088","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":[0.98669046,0.00007664418,0.01018839,0.00023483377,0.0008529669,0.0009877592,0.00007155083,0.00012926938,0.00076813524],"genre_scores_gemma":[0.9937232,0.000045143643,0.0053532007,0.000092070826,0.00006391593,0.00013569117,0.00024325623,0.00006428644,0.00027922876],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99635637,0.00027425817,0.00092678884,0.00094727665,0.00081939035,0.0006759148],"domain_scores_gemma":[0.99818426,0.00014689303,0.0007180404,0.0007689086,0.000026849866,0.00015504325],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010121193,0.0005615702,0.0006492399,0.00001299856,0.00079743844,0.000104224266,0.00091152434,0.00032912797,0.0019748441],"category_scores_gemma":[0.00006196808,0.0004354689,0.00026570645,0.0007445687,0.00047718498,0.0001665323,0.0030802179,0.0011026633,0.00001677227],"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":[0.0019381403,0.00071603426,0.7647143,0.0005799444,0.00090222206,0.0000198496,0.020136496,0.041068047,0.16370195,0.00018870973,0.00039377384,0.005640503],"study_design_scores_gemma":[0.022014698,0.0028939643,0.7351142,0.0022035888,0.0022457489,0.00007384836,0.03914414,0.053341255,0.10053991,0.0012657932,0.03140912,0.009753694],"about_ca_topic_score_codex":0.0056973095,"about_ca_topic_score_gemma":0.0005545567,"teacher_disagreement_score":0.06316205,"about_ca_system_score_codex":0.00043343386,"about_ca_system_score_gemma":0.00003195914,"threshold_uncertainty_score":0.9998097},"labels":[],"label_agreement":null},{"id":"W4220997579","doi":"10.1029/2021gl097154","title":"Extratropical Shortwave Cloud Feedbacks in the Context of the Global Circulation and Hydrological Cycle","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Pacific Northwest National Laboratory; Lawrence Livermore National Laboratory; University of Wyoming; Biological and Environmental Research; Natural Sciences and Engineering Research Council of Canada; National Oceanic and Atmospheric Administration; Nuclear Safety and Security Commission; Battelle; Office of Science; National Aeronautics and Space Administration; U.S. Department of Energy; Division of Earth Sciences; National Science Foundation","keywords":"Extratropical cyclone; Climatology; Context (archaeology); Shortwave; General Circulation Model; Environmental science; Water cycle; Cloud computing; Meteorology; Circulation (fluid dynamics); Geology; Climate change; Geography; Oceanography; Computer science; Radiative transfer; Physics","score_opus":0.01995985537436864,"score_gpt":0.2756739091265563,"score_spread":0.2557140537521877,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220997579","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":[0.9927889,0.000015186333,0.000038031005,0.0061553577,0.0000321794,0.00022069266,0.000005553714,0.0000026656396,0.0007414063],"genre_scores_gemma":[0.9989958,0.0000018996242,0.00002537499,0.00090389606,0.000034561504,0.000027226459,8.8111204e-7,0.0000027802882,0.0000075942066],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979726,0.00053473667,0.00014877859,0.00019567541,0.0008877443,0.00026045286],"domain_scores_gemma":[0.9994897,0.0002113367,0.000035553436,0.00022070254,0.0000049824025,0.00003772848],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047243372,0.000060601385,0.00010756512,0.0000011791906,0.00018639246,0.000010130411,0.00041136402,0.000024128682,0.00021719777],"category_scores_gemma":[0.000062450104,0.000035263554,0.00006013161,0.00044719302,0.00094345957,0.00003386736,0.00057706295,0.00038201528,0.0000069076445],"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":[0.00016707386,0.00042271038,0.9186893,0.00000882411,0.0000127233025,0.000022022718,0.0017606105,0.003413117,0.05279482,0.0105731245,0.002056381,0.010079253],"study_design_scores_gemma":[0.000188084,0.0001245393,0.99235356,0.0000019678303,0.000002795661,0.0000037895277,0.00075819745,0.0024955308,0.00007908869,0.0034977975,0.0004494293,0.000045208322],"about_ca_topic_score_codex":0.0012014444,"about_ca_topic_score_gemma":0.000053626984,"teacher_disagreement_score":0.07366423,"about_ca_system_score_codex":0.000111077985,"about_ca_system_score_gemma":0.000010534835,"threshold_uncertainty_score":0.34762162},"labels":[],"label_agreement":null},{"id":"W4221085947","doi":"10.5194/egusphere-egu22-6578","title":"Assessment of present-day aerosol optical depth from modern aerosol-climate models, reanalyses, and satellite products","year":2022,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"","keywords":"Aerosol; Satellite; Environmental science; Climatology; Radiative forcing; Meteorology; Climate model; Scale (ratio); Forcing (mathematics); Atmospheric sciences; Climate change; Geography; Cartography; Geology","score_opus":0.027356632186950173,"score_gpt":0.2747055485410516,"score_spread":0.24734891635410144,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4221085947","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":[0.8412062,0.0018730937,0.03253179,0.0005928073,0.00040701663,0.0014608355,0.00022096567,0.00017897281,0.121528305],"genre_scores_gemma":[0.9270373,0.0027404446,0.06793824,0.0001092586,0.000097690856,0.00015623572,0.00028436654,0.000076876364,0.0015596177],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99510145,0.00023056586,0.00086900947,0.0017989242,0.0013091299,0.00069094304],"domain_scores_gemma":[0.99757916,0.000119661876,0.00044997645,0.0015251258,0.000030463305,0.0002956026],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006084518,0.0006236673,0.0009046528,0.0000051804045,0.00021281364,0.00012351242,0.00084437063,0.00030264317,0.0034303516],"category_scores_gemma":[0.000025675943,0.00054676784,0.00020402604,0.00022130879,0.00044337704,0.00023433362,0.0069812587,0.00088255625,0.000021987218],"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":[0.00015050602,0.0017923807,0.19464816,0.0005272617,0.00091598264,0.00010707385,0.002023447,0.71409893,0.03790669,0.0029772557,0.002066677,0.042785607],"study_design_scores_gemma":[0.0011222393,0.00030430156,0.13496594,0.00014082046,0.00082333386,0.00001039589,0.00066668814,0.8433882,0.007131984,0.008057717,0.0012076484,0.0021807516],"about_ca_topic_score_codex":0.0043886066,"about_ca_topic_score_gemma":0.0004555629,"teacher_disagreement_score":0.12928924,"about_ca_system_score_codex":0.00043222698,"about_ca_system_score_gemma":0.000100326186,"threshold_uncertainty_score":0.9996984},"labels":[],"label_agreement":null},{"id":"W4221129504","doi":"10.5194/egusphere-egu22-3116","title":"Angularly-resolved measurements of light scattering by smoke from wildfires during FIREX-AQ","year":2022,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"University of Alberta","funders":"","keywords":"Aerosol; Radiative forcing; Radiative transfer; Backscatter (email); Scattering; Mie scattering; Smoke; Phase (matter); Light scattering; Environmental science; Forcing (mathematics); Atmospheric sciences; Physics; Particle (ecology); Computational physics; Chemistry; Meteorology; Optics; Geology","score_opus":0.0198695401341996,"score_gpt":0.22907345306495716,"score_spread":0.20920391293075757,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4221129504","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":[0.9859663,0.00055528776,0.00021398958,0.00023533714,0.00040823172,0.000339609,0.00007087688,0.00009521055,0.012115155],"genre_scores_gemma":[0.9954481,0.000050032828,0.0023491152,0.00016166453,0.00006143045,0.00008753881,0.00007386445,0.00005569723,0.0017125492],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9970606,0.000084583204,0.0005334861,0.0008671108,0.0010414026,0.00041284418],"domain_scores_gemma":[0.99862057,0.000020312073,0.00033058214,0.00087443227,0.000007300973,0.00014680157],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00020669847,0.0003979438,0.0004637927,0.0000027359793,0.0002181427,0.00005824125,0.0009711258,0.00019170374,0.038680416],"category_scores_gemma":[0.000017043472,0.00038390097,0.00021546026,0.00013162145,0.00013443081,0.00010857981,0.0038246643,0.00044620925,0.00006402985],"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":[0.000030718773,0.00015249083,0.76450217,0.000041750434,0.00012289538,0.000008263493,0.00057472615,0.001654416,0.22833405,7.0554836e-7,0.0034191,0.0011587047],"study_design_scores_gemma":[0.00066043524,0.000058154437,0.858043,0.00012333407,0.00010068116,0.0000012690591,0.0003171412,0.00027947107,0.13600843,0.00020541773,0.0033023434,0.00090031733],"about_ca_topic_score_codex":0.03114917,"about_ca_topic_score_gemma":0.00025253688,"teacher_disagreement_score":0.09354083,"about_ca_system_score_codex":0.00041997252,"about_ca_system_score_gemma":0.000020563079,"threshold_uncertainty_score":0.9998613},"labels":[],"label_agreement":null},{"id":"W4223971208","doi":"10.1016/j.jqsrt.2022.108220","title":"A note on computing stokes phase matrices for macroscopically isotropic mirror symmetric scattering medium stokes scattering matrices","year":2022,"lang":"en","type":"article","venue":"Journal of Quantitative Spectroscopy and Radiative Transfer","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"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":"USAF Phillips Laboratory; Defence Research and Development Canada; U.S. Department of Energy","keywords":"Scattering; Stokes parameters; Isotropy; Physics; Phase (matter); Azimuth; Optics; Mathematical analysis; Classical mechanics; Mathematics; Quantum mechanics","score_opus":0.01919817496409663,"score_gpt":0.3180827594342437,"score_spread":0.29888458447014704,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4223971208","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":[0.893085,0.0012756026,0.10343971,0.0012055909,0.00035845037,0.00037994442,0.00007139602,0.00001803898,0.00016625365],"genre_scores_gemma":[0.9577807,0.00040332027,0.041200362,0.0004378539,0.000084560765,0.00001921298,0.0000030619296,0.00003546406,0.000035443907],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99770457,0.00020249284,0.0006514029,0.0003749228,0.000590151,0.0004764818],"domain_scores_gemma":[0.99875337,0.000596183,0.000322394,0.000107310174,0.000037373673,0.00018338085],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00058328616,0.00031074262,0.00055298716,0.000058875357,0.0007879952,0.000088173176,0.0003521558,0.000049825398,0.00053788966],"category_scores_gemma":[0.00003853528,0.0002575287,0.0002116251,0.000605984,0.0003073566,0.00035775817,0.00008283771,0.00048271476,0.000009105415],"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":[0.0047049206,0.0016184828,0.03122629,0.00031593753,0.0005347031,0.0001471106,0.020438101,0.011578451,0.9179774,0.0033155517,0.0009286099,0.007214435],"study_design_scores_gemma":[0.043903407,0.08635722,0.45781946,0.00096781284,0.0020462025,0.0005892297,0.03279589,0.06337993,0.2812538,0.004403825,0.021882739,0.004600461],"about_ca_topic_score_codex":0.00006473436,"about_ca_topic_score_gemma":0.000018990719,"teacher_disagreement_score":0.6367236,"about_ca_system_score_codex":0.00028621624,"about_ca_system_score_gemma":0.000046445,"threshold_uncertainty_score":0.9999877},"labels":[],"label_agreement":null},{"id":"W4224232894","doi":"10.1080/15481603.2022.2060596","title":"Gap-filling MODIS daily aerosol optical depth products by developing a spatiotemporal fitting algorithm","year":2022,"lang":"en","type":"article","venue":"GIScience & Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":41,"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":"Ministry of Innovation and Advanced Education","keywords":"Moderate-resolution imaging spectroradiometer; Remote sensing; Residual; Aerosol; Environmental science; Pixel; Atmospheric correction; Spectroradiometer; Image resolution; Smoothing; Algorithm; Meteorology; Computer science; Geography; Mathematics; Satellite; Artificial intelligence; Statistics","score_opus":0.018545212223598343,"score_gpt":0.23387727390121074,"score_spread":0.2153320616776124,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4224232894","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":[0.64596784,0.00007902361,0.3462729,0.0016646716,0.00038942616,0.0003157331,0.000005345179,0.0001403838,0.0051647075],"genre_scores_gemma":[0.62572205,0.000006244012,0.37302592,0.000575528,0.00007564763,5.7402525e-7,0.000008896827,0.000027104988,0.0005580123],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9963,0.00011916343,0.00045093088,0.0010358478,0.0011745682,0.00091951946],"domain_scores_gemma":[0.99906003,0.000058173286,0.00022855331,0.0004312868,0.000027162703,0.00019477229],"candidate_categories":["metaepi_narrow","sts"],"consensus_categories":[],"category_scores_codex":[0.0009814407,0.00029326542,0.0002682572,0.000006939059,0.0018216183,0.000163534,0.0004865307,0.000061114624,0.00013462914],"category_scores_gemma":[0.0001637428,0.00029426342,0.000072924784,0.0011921449,0.0004690488,0.00039202167,0.0010070251,0.00044198774,0.00007035739],"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":[0.0000097621,0.00003146443,0.0008379683,0.000008956943,0.0000055846385,0.00007405022,0.0016526863,0.020827489,0.059266243,0.000012471274,0.0016708063,0.9156025],"study_design_scores_gemma":[0.00031110778,0.00011623051,0.0011262855,0.00004005167,0.000016316744,0.0002220415,0.001668224,0.97107846,0.017764641,0.00019659843,0.0067102057,0.00074983493],"about_ca_topic_score_codex":0.0012858111,"about_ca_topic_score_gemma":0.000071040224,"teacher_disagreement_score":0.950251,"about_ca_system_score_codex":0.0006197248,"about_ca_system_score_gemma":0.00011972367,"threshold_uncertainty_score":0.99995095},"labels":[],"label_agreement":null},{"id":"W4225417759","doi":"10.5194/amt-2022-72","title":"Ice crystals images from Optical Array Probes: classification with Convolutional Neural Networks","year":2022,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"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":"Horizon 2020; Environment and Climate Change Canada; Centre National de la Recherche Scientifique; Centre National d’Etudes Spatiales; Institut Polaire Français Paul Emile Victor; Transport Canada; Aeronautics Research Mission Directorate; Agence Nationale de la Recherche; National Aeronautics and Space Administration; European Commission; Boeing","keywords":"Convolutional neural network; Dropout (neural networks); Computer science; Artificial intelligence; Artifact (error); Pattern recognition (psychology); Crystal (programming language); Ice crystals; Pixel; Artificial neural network; Remote sensing; Machine learning; Geology; Optics; Physics","score_opus":0.01471135056497035,"score_gpt":0.22779003691117455,"score_spread":0.2130786863462042,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4225417759","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.4588242,0.00019785634,0.46620813,0.0016010607,0.00049517216,0.00090239866,0.00008411443,0.00023362174,0.07145347],"genre_scores_gemma":[0.96633804,0.000031360996,0.029126335,0.00041211428,0.00020113526,0.00026405003,0.00037990228,0.00003618476,0.0032108717],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99769676,0.000091295704,0.00032131642,0.00086458254,0.00062982447,0.00039621914],"domain_scores_gemma":[0.9990003,0.000089321824,0.0002030663,0.0005351426,0.000017506778,0.0001546755],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00017906252,0.00031799744,0.00028194094,0.0000012947681,0.00025694762,0.000104919454,0.0005292063,0.000195584,0.032507956],"category_scores_gemma":[0.000015714553,0.0002503574,0.00008731122,0.000156918,0.00043779917,0.000121588186,0.0010170126,0.0007747365,0.00008181193],"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":[0.00016745212,0.00037656023,0.17394595,0.000019049898,0.00011271004,0.000024083993,0.0002484198,0.80040354,0.0045498256,0.0010190472,0.015781704,0.0033516663],"study_design_scores_gemma":[0.00061640225,0.00022216166,0.5992358,0.000035268265,0.00014933702,0.000014372345,0.0012560167,0.3878607,0.000266334,0.0013458558,0.0077906786,0.0012071164],"about_ca_topic_score_codex":0.0010595997,"about_ca_topic_score_gemma":0.000077313074,"teacher_disagreement_score":0.5075139,"about_ca_system_score_codex":0.00034727302,"about_ca_system_score_gemma":0.000048813272,"threshold_uncertainty_score":0.9999949},"labels":[],"label_agreement":null},{"id":"W4225975083","doi":"10.5194/amt-15-927-2022","title":"Assessing synergistic radar and radiometer capability in retrieving ice cloud microphysics based on hybrid Bayesian algorithms","year":2022,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":11,"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":"Goddard Space Flight Center; Stony Brook University; Nuclear Safety and Security Commission; National Center for Atmospheric Research; Environment and Climate Change Canada; Colorado State University; National Aeronautics and Space Administration","keywords":"Radiometer; Environmental science; Radar; Remote sensing; Computer science; Algorithm; Meteorology; Bayesian probability; Cloud computing; Artificial intelligence; Geology; Geography","score_opus":0.017567502138089747,"score_gpt":0.23498033740064805,"score_spread":0.2174128352625583,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4225975083","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":[0.80301934,0.00021947814,0.19155136,0.00029276486,0.00024190937,0.00091032946,0.000006317176,0.00031690273,0.0034416162],"genre_scores_gemma":[0.891093,0.000014747748,0.10788596,0.0006864554,0.000053882413,0.00017282099,0.0000047109966,0.00004759879,0.00004079265],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99648756,0.00040498615,0.0004875193,0.00081016537,0.0012940539,0.00051574653],"domain_scores_gemma":[0.9989447,0.00009639319,0.000214537,0.00058020325,0.000023299059,0.00014086216],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0019677056,0.00035477502,0.0003868073,0.0000022540075,0.00046636147,0.00010616489,0.00038954493,0.000059097438,0.00082343427],"category_scores_gemma":[0.000115967065,0.00035570623,0.00009480651,0.0007961689,0.00023111649,0.00023085282,0.00031395865,0.000470597,0.0000056120107],"study_design_candidate":"design_other","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":[0.00026376915,0.0019150503,0.12547092,0.0001601486,0.00006402143,0.00029399394,0.00059931853,0.0057887603,0.15528241,0.00007728654,0.005357691,0.70472664],"study_design_scores_gemma":[0.005602695,0.0058004744,0.23038344,0.0008113289,0.00042691725,0.00012635914,0.0025794886,0.49129078,0.18603471,0.0063817254,0.063128605,0.0074334866],"about_ca_topic_score_codex":0.0009985063,"about_ca_topic_score_gemma":0.00001934897,"teacher_disagreement_score":0.69729316,"about_ca_system_score_codex":0.0018128128,"about_ca_system_score_gemma":0.00006359351,"threshold_uncertainty_score":0.9998895},"labels":[],"label_agreement":null},{"id":"W4226167637","doi":"10.1175/jcli-d-21-0812.1","title":"Observational Constraints on Southern Ocean Cloud-Phase Feedback","year":2022,"lang":"en","type":"article","venue":"Journal of Climate","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Oceanic and Atmospheric Administration; Nuclear Safety and Security Commission; National Aeronautics and Space Administration","keywords":"Cloud feedback; Cloud albedo; Cloud fraction; Environmental science; Cloud computing; Climate model; Shortwave; Cloud forcing; International Satellite Cloud Climatology Project; Albedo (alchemy); Cloud height; Climatology; Liquid water content; Radiative transfer; Climate sensitivity; Cloud cover; Atmospheric sciences; Climate change; Physics; Geology; Computer science","score_opus":0.023211867684267494,"score_gpt":0.2685776343312626,"score_spread":0.24536576664699508,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4226167637","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":[0.9866385,0.000015848944,0.00010853904,0.00078931794,0.00037443318,0.000051007675,0.00004689974,0.000007899718,0.011967581],"genre_scores_gemma":[0.9974338,0.000020233594,0.00076265103,0.0011839665,0.00014003663,9.57975e-7,0.0000033099086,0.000012446967,0.0004426314],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987147,0.000059726088,0.0003478087,0.0001047172,0.0005702648,0.00020281856],"domain_scores_gemma":[0.999368,0.0000451208,0.00037333425,0.00009994682,0.000011355042,0.000102206504],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00047553887,0.00009195479,0.0001493954,0.000002045934,0.00024152921,0.000019569228,0.00024141787,0.000020779536,0.027848657],"category_scores_gemma":[0.000021716703,0.00007647557,0.00010876292,0.00011746423,0.00012420578,0.00008219384,0.00013745484,0.0002544946,0.00024064154],"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":[0.0026018836,0.003939821,0.6060551,0.000031645377,0.00020954761,0.0009443746,0.0063665635,0.11639298,0.01147983,0.003748138,0.12034046,0.12788965],"study_design_scores_gemma":[0.025407229,0.011912259,0.47125125,0.0001596456,0.0003084522,0.0025141386,0.028202279,0.011266779,0.0010879389,0.011412709,0.4342824,0.002194923],"about_ca_topic_score_codex":0.0000051041275,"about_ca_topic_score_gemma":0.0000010765747,"teacher_disagreement_score":0.31394193,"about_ca_system_score_codex":0.00014911844,"about_ca_system_score_gemma":0.000023095597,"threshold_uncertainty_score":0.97304004},"labels":[],"label_agreement":null},{"id":"W4226175460","doi":"10.5194/amt-15-775-2022","title":"Coincident in situ and triple-frequency radar airborne observations in the Arctic","year":2022,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"National Research Council Canada","funders":"Environment and Climate Change Canada; Natural Environment Research Council; Sight Research UK; Université du Québec à Montréal","keywords":"Radar; Snow; Remote sensing; Environmental science; Meteorology; Snowflake; Range (aeronautics); Ice crystals; Particle (ecology); Arctic; Storm; Winter storm; Atmospheric sciences; Geology; Materials science; Geography; Computer science; Telecommunications","score_opus":0.02831209039493327,"score_gpt":0.22690664599119087,"score_spread":0.1985945555962576,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4226175460","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":[0.98671323,0.0007262699,0.0020346444,0.0022485657,0.00008646568,0.0013638997,0.000001785845,0.00013441463,0.006690727],"genre_scores_gemma":[0.9704991,0.00010513852,0.027063489,0.0013734079,0.000015781092,0.00080722483,0.000003177626,0.000018803885,0.00011389797],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9974649,0.0003099261,0.00041654485,0.00039494963,0.0010660795,0.00034762218],"domain_scores_gemma":[0.99936587,0.00004315618,0.00012429009,0.00040072453,0.000014264482,0.0000517187],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020696807,0.0001961067,0.00021066847,0.0000011578421,0.0002669123,0.000032986838,0.0004927704,0.000043483647,0.0007072704],"category_scores_gemma":[0.00008490027,0.00016059949,0.00004796976,0.0008786033,0.00012612133,0.00016598003,0.0002788875,0.0003483873,0.0000073642],"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":[0.000043420234,0.000989319,0.9223173,0.000026504542,0.000016916198,0.00010459438,0.0031360686,0.00027531607,0.028870316,0.0017543525,0.0060936646,0.036372207],"study_design_scores_gemma":[0.0005112394,0.00040687964,0.9774389,0.000030029092,0.000018915376,0.000030591513,0.0016766528,0.00036720047,0.0004980096,0.0050596157,0.013603857,0.0003581074],"about_ca_topic_score_codex":0.004699502,"about_ca_topic_score_gemma":0.0026761577,"teacher_disagreement_score":0.055121582,"about_ca_system_score_codex":0.0009934497,"about_ca_system_score_gemma":0.000039262028,"threshold_uncertainty_score":0.7744115},"labels":[],"label_agreement":null},{"id":"W4228997617","doi":"10.1007/s00371-022-02504-3","title":"Correction: Observation-driven generation of texture maps depicting dust accumulation over time","year":2022,"lang":"en","type":"article","venue":"The Visual Computer","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Texture (cosmology); Computer graphics; Computer graphics (images); Computer science; Artificial intelligence; Image (mathematics)","score_opus":0.03360249636138627,"score_gpt":0.27040121308758297,"score_spread":0.2367987167261967,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4228997617","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":[0.97553074,0.0000061689298,0.02315963,0.0001594628,0.0005819202,0.00013373501,0.0000022557758,0.000028664968,0.00039741216],"genre_scores_gemma":[0.996509,6.491166e-7,0.0011284222,0.00046528774,0.00026496267,0.000010580477,0.000036020367,0.00000938478,0.0015756765],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9992422,0.00009262349,0.00015536907,0.00015066727,0.0002608734,0.000098287564],"domain_scores_gemma":[0.9996813,0.00004799883,0.00011600542,0.00012792094,0.000007764575,0.000019006258],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00015439895,0.00007330122,0.000075157535,0.0000014017015,0.0003689859,0.000018924047,0.00014077206,0.000025107365,0.011749341],"category_scores_gemma":[0.000004730029,0.000057600744,0.000038616618,0.00021384918,0.000036562487,0.000106933716,0.00025961452,0.00011672755,0.000048122587],"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":[0.000021192953,0.00009694758,0.13620205,0.0000022655772,0.000017217015,0.0000011380376,0.0012735113,0.74849087,0.016868267,0.00007080691,0.072357476,0.024598269],"study_design_scores_gemma":[0.00010406886,0.00008994489,0.19853383,0.000001533877,0.000007187506,0.0000037737448,0.000028661847,0.7973806,0.00020088434,0.00002518329,0.003558029,0.000066272136],"about_ca_topic_score_codex":0.00012635697,"about_ca_topic_score_gemma":0.000011666083,"teacher_disagreement_score":0.06879945,"about_ca_system_score_codex":0.00009074299,"about_ca_system_score_gemma":0.000006338371,"threshold_uncertainty_score":0.98915404},"labels":[],"label_agreement":null},{"id":"W4229065072","doi":"10.1029/2021jd036249","title":"Contrasting Stratospheric Smoke Mass and Lifetime From 2017 Canadian and 2019/2020 Australian Megafires: Global Simulations and Satellite Observations","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":25,"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":"Los Alamos National Laboratory; Goddard Space Flight Center; National Nuclear Security Administration; National Aeronautics and Space Administration; U.S. Department of Energy","keywords":"Stratosphere; Smoke; Environmental science; Plume; Atmospheric sciences; Climatology; Volcano; Satellite; Atmospheric model; Meteorology; Geology; Geography; Physics","score_opus":0.038398072803754686,"score_gpt":0.30180631149264625,"score_spread":0.26340823868889157,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4229065072","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":[0.9954068,0.0011082394,0.00004244231,0.0025247128,0.00006140467,0.00018038736,0.00014475058,0.000007431673,0.0005238071],"genre_scores_gemma":[0.99503493,0.00030324826,0.0037279227,0.00013667466,0.0001433347,0.0000053605672,0.0000074624013,0.000014421792,0.00062664604],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9976722,0.00025092319,0.00036849282,0.00031858697,0.000841179,0.0005486327],"domain_scores_gemma":[0.99831814,0.0004663551,0.00016130465,0.00017021206,0.00006333409,0.00082062994],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00043589517,0.00017102968,0.00028199313,0.000001565575,0.0009811395,0.00021112741,0.00028647075,0.00006433264,0.0012399924],"category_scores_gemma":[0.0002297035,0.00015531102,0.000053255644,0.00045827669,0.0005241387,0.00035411,0.00029528033,0.00062412955,0.0000092068],"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":[0.00009907974,0.0001016924,0.96855664,0.0000088554925,0.00010416323,0.00017313316,0.0004063045,0.0029851706,0.003930117,0.0003439137,0.007686636,0.015604309],"study_design_scores_gemma":[0.00048292425,0.00038277757,0.9738204,0.000018988401,0.00002938303,0.000023129316,0.0011321771,0.006878406,0.000011069105,0.004985238,0.012070654,0.0001648485],"about_ca_topic_score_codex":0.14269112,"about_ca_topic_score_gemma":0.022133801,"teacher_disagreement_score":0.120557316,"about_ca_system_score_codex":0.00030797522,"about_ca_system_score_gemma":0.00020403092,"threshold_uncertainty_score":0.999673},"labels":[],"label_agreement":null},{"id":"W4230448262","doi":"10.2172/1374165","title":"Evolution of Precipitation Particle Size Distributions within MC3E Systems and its Impact on Aerosol-Cloud-Precipitation Interactions: Final Report","year":2017,"lang":"en","type":"report","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"","keywords":"Cloud computing; Precipitation; Aerosol; Meteorology; Environmental science; Radar; Remote sensing; Computer science; Geography","score_opus":0.032321740623312424,"score_gpt":0.3242242445882295,"score_spread":0.29190250396491707,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4230448262","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":[0.9659022,0.0003539995,0.0034365184,0.00009039225,0.00212125,0.00091000437,0.00017885906,0.00007309557,0.026933653],"genre_scores_gemma":[0.97319317,0.00014197892,0.00030158236,0.000003961951,0.00024050573,0.0001365846,0.00014024386,0.00003062244,0.025811337],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99699825,0.00011803975,0.0009610411,0.00063808134,0.000969868,0.00031474506],"domain_scores_gemma":[0.99704087,0.00024343301,0.0017003821,0.00064194616,0.00019837305,0.0001750224],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0009476863,0.00036517775,0.0004907476,0.0000049108094,0.0004090839,0.000119475815,0.00021080687,0.00026180624,0.00069333764],"category_scores_gemma":[0.0016389441,0.0002927615,0.00017745918,0.00016268292,0.00019703669,0.0005193717,0.00014472676,0.00032672106,0.00010754324],"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":[0.0015360478,0.0034704385,0.56713676,0.0014404646,0.0014498843,0.00031731834,0.0040401923,0.12116733,0.042464755,0.0035876015,0.24347633,0.009912841],"study_design_scores_gemma":[0.0009890524,0.001288881,0.9492076,0.0010887746,0.0005166112,0.0008475429,0.000885902,0.036102563,0.0025325092,0.0004886212,0.004844629,0.0012073392],"about_ca_topic_score_codex":0.0055764276,"about_ca_topic_score_gemma":0.0002799875,"teacher_disagreement_score":0.38207078,"about_ca_system_score_codex":0.0017562689,"about_ca_system_score_gemma":0.0003388789,"threshold_uncertainty_score":0.99995244},"labels":[],"label_agreement":null},{"id":"W4230480611","doi":"10.5194/acp-2017-255","title":"Impacts of solar-absorbing aerosol layers on the transition of stratocumulus to trade cumulus clouds","year":2017,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Brookhaven National Laboratory","keywords":"Aerosol; Atmospheric sciences; Longwave; Liquid water path; Breakup; Environmental science; Marine stratocumulus; Cloud forcing; Shortwave; Liquid water content; Cloud albedo; Boundary layer; Drizzle; Entrainment (biomusicology); Cloud height; Meteorology; Radiative transfer; Precipitation; Cloud cover; Radiative forcing; Cloud computing; Physics; Mechanics","score_opus":0.023446966066754334,"score_gpt":0.2650654135310067,"score_spread":0.24161844746425237,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4230480611","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":[0.9718684,0.000026469974,0.005341745,0.0023485953,0.00026630433,0.00088070275,0.00005030142,0.000034648263,0.019182827],"genre_scores_gemma":[0.9975415,0.000043629672,0.0015989912,0.00049301,0.00006271866,0.000036457288,0.000006631465,0.000034515924,0.00018255188],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99776596,0.000093579474,0.00053020683,0.0005279022,0.0006760352,0.00040633074],"domain_scores_gemma":[0.9980851,0.00008296093,0.0004642711,0.0011637869,0.000011156325,0.00019276874],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00049242825,0.00037115742,0.00050962175,0.0000031450002,0.00019293252,0.00005675299,0.0009778306,0.0003021367,0.0016968299],"category_scores_gemma":[0.000054898046,0.00025414498,0.00030254276,0.00009887426,0.0003347521,0.000093211675,0.00043165247,0.0004947146,0.000063491025],"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":[0.0012210284,0.0018897956,0.017029664,0.0007922675,0.00065817416,0.000044345383,0.032732546,0.39937425,0.48064858,0.00269999,0.01830065,0.04460871],"study_design_scores_gemma":[0.0027900047,0.003368398,0.13839854,0.002182014,0.0005804791,0.000023035805,0.006253474,0.026166229,0.80971795,0.0059173377,0.0012384611,0.0033640428],"about_ca_topic_score_codex":0.003684585,"about_ca_topic_score_gemma":0.0004945551,"teacher_disagreement_score":0.37320802,"about_ca_system_score_codex":0.00015525054,"about_ca_system_score_gemma":0.00005985717,"threshold_uncertainty_score":0.99999106},"labels":[],"label_agreement":null},{"id":"W4230631828","doi":"10.5194/amtd-6-6329-2013","title":"Characterization of disdrometer uncertainties and impacts on estimates of snowfall rate and radar reflectivity","year":2013,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Jet Propulsion Laboratory; Colorado State University; National Aeronautics and Space Administration","keywords":"Disdrometer; Snow; Environmental science; Radar; Precipitation; Meteorology; Snowflake; Remote sensing; Particle (ecology); Atmospheric sciences; Geology; Computer science; Physics","score_opus":0.012394501913574127,"score_gpt":0.23761377427363037,"score_spread":0.22521927236005623,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4230631828","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":[0.9968236,0.000019705694,0.0012033564,0.000099795936,0.000053093274,0.00024912204,0.000017016497,0.000014085273,0.001520222],"genre_scores_gemma":[0.9967624,0.00025722152,0.0025287902,0.00004325725,0.000008581764,0.000009905954,0.000015457528,0.000012069994,0.00036234385],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9991778,0.000038387305,0.0002164184,0.00029516284,0.00014072779,0.00013149934],"domain_scores_gemma":[0.99941653,0.000054683493,0.00024588345,0.00020928473,0.000010215252,0.00006338994],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001405646,0.00018356535,0.0003170357,0.0000026777554,0.000032833163,0.000025830153,0.00008981925,0.000120419005,0.0005998909],"category_scores_gemma":[0.000031508578,0.00013473818,0.000032535838,0.000053977976,0.00030101067,0.000106684536,0.0004698421,0.00011216603,0.0000054763264],"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":[0.00006633812,0.00012112624,0.15034215,0.0002629488,0.000055041794,8.687508e-7,0.00088502903,0.00016178346,0.83843607,0.00021957242,0.00009651396,0.0093525285],"study_design_scores_gemma":[0.00015168822,0.00020330751,0.9346877,0.00009790455,0.00002897382,0.0000011830834,0.000037203085,0.0027190216,0.05963015,0.0022109987,0.00003300897,0.00019889986],"about_ca_topic_score_codex":0.0015393501,"about_ca_topic_score_gemma":0.000041280793,"teacher_disagreement_score":0.7843455,"about_ca_system_score_codex":0.000035591736,"about_ca_system_score_gemma":0.000009002781,"threshold_uncertainty_score":0.6568384},"labels":[],"label_agreement":null},{"id":"W4231665971","doi":"10.5194/acpd-9-22929-2009","title":"Size dependence of volume and surface nucleation rates for homogeneous freezing of supercooled water droplets","year":2009,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":5,"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 Waterloo; Environment and Climate Change Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Nucleation; Supercooling; Ice nucleus; Aerosol; Volume (thermodynamics); RADIUS; Surface tension; Materials science; Classical nucleation theory; Homogeneous; Thermodynamics; Chemistry; Physics","score_opus":0.00845776332981936,"score_gpt":0.23266574127682632,"score_spread":0.22420797794700698,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4231665971","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":[0.9906351,0.00010335815,0.0075991997,0.00013174492,0.000062502906,0.0004426358,0.000016746879,0.000020793921,0.0009879182],"genre_scores_gemma":[0.96545875,0.00011120431,0.032372043,0.000045928533,0.000016255717,0.0000076502865,0.000010404189,0.000017944447,0.0019598007],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99876124,0.000030868465,0.00036007026,0.0003986053,0.00022403878,0.00022520583],"domain_scores_gemma":[0.99943984,0.00006123929,0.00012461242,0.00028952694,0.000025238687,0.000059568814],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00022590454,0.00019427168,0.0003436897,9.792027e-7,0.00005840692,0.00002021576,0.00023571705,0.00019040387,0.0021323597],"category_scores_gemma":[0.000026104071,0.0001467399,0.000088452536,0.000036780813,0.00015951041,0.000073256844,0.00044031258,0.00010430854,0.000016864084],"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":[0.00009627024,0.00015989676,0.12609841,0.00024776254,0.00006222874,0.0000037112036,0.0013683897,0.049521275,0.8146457,0.000045597848,0.00077263324,0.006978134],"study_design_scores_gemma":[0.0011905505,0.00067397306,0.15028208,0.00019751636,0.0002594293,0.00001841699,0.00064794335,0.0829738,0.75677353,0.0051206457,0.0007428709,0.0011192024],"about_ca_topic_score_codex":0.0015881852,"about_ca_topic_score_gemma":0.00019541584,"teacher_disagreement_score":0.05787214,"about_ca_system_score_codex":0.000050257368,"about_ca_system_score_gemma":0.000012208059,"threshold_uncertainty_score":0.99877983},"labels":[],"label_agreement":null},{"id":"W4231885569","doi":"10.5194/amtd-5-8609-2012","title":"Developing a portable, autonomous aerosol backscatter lidar for network or remote operations","year":2012,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":7,"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","funders":"","keywords":"Lidar; Remote sensing; Backscatter (email); Laser; Environmental science; Computer science; Ceilometer; Real-time computing; Optics; Telecommunications; Geology; Physics","score_opus":0.03487773321031299,"score_gpt":0.2777095009490594,"score_spread":0.2428317677387464,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4231885569","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.05786838,0.00013921242,0.9117304,0.0020950853,0.001454147,0.0019032452,0.00002637145,0.00022179143,0.024561346],"genre_scores_gemma":[0.15443291,0.00007501518,0.7748066,0.0039876504,0.0009759412,0.00024869022,0.00012351794,0.00009397866,0.06525568],"study_design_codex":"simulation_or_modeling","study_design_gemma":"not_applicable","domain_scores_codex":[0.99767715,0.000035870547,0.0005363645,0.0007054318,0.00023979097,0.0008053703],"domain_scores_gemma":[0.99892664,0.000054893368,0.00014518175,0.0006495934,0.000020633359,0.00020308656],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00033391212,0.0004196644,0.00041821948,0.0000012857626,0.00040344894,0.00015266049,0.0005348752,0.00038170416,0.013928647],"category_scores_gemma":[0.00002577471,0.00032226066,0.0001681619,0.00014948369,0.000112831825,0.00016843784,0.0013541837,0.00033696613,0.00075002055],"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":[0.00024411797,0.00038977095,0.057934888,0.0004696855,0.00054408703,0.000031529707,0.0025286118,0.5182935,0.00072768383,0.0036468105,0.3165942,0.0985951],"study_design_scores_gemma":[0.0024106863,0.00035721395,0.050761767,0.00073712546,0.0007187573,0.00012088549,0.000585763,0.16627814,0.001881178,0.0056487285,0.7630428,0.0074569476],"about_ca_topic_score_codex":0.0010356731,"about_ca_topic_score_gemma":0.0014678596,"teacher_disagreement_score":0.4464486,"about_ca_system_score_codex":0.00041762085,"about_ca_system_score_gemma":0.00018863252,"threshold_uncertainty_score":0.99992293},"labels":[],"label_agreement":null},{"id":"W4232504229","doi":"10.1364/ao.39.001879","title":"Microphysical particle parameters from extinction and backscatter lidar data by inversion with regularization: experiment","year":2000,"lang":"en","type":"article","venue":"Applied Optics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":76,"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":"Lidar; Aerosol; Effective radius; Single-scattering albedo; Mie scattering; Refractive index; Wavelength; Optics; Molar absorptivity; Scattering; Environmental science; Materials science; Light scattering; Physics; Meteorology; Astrophysics","score_opus":0.008328819556510478,"score_gpt":0.1917000928439585,"score_spread":0.183371273287448,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4232504229","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":[0.994077,0.00001828271,0.0032632293,0.00019814109,0.000013088807,0.000118489545,0.000008533948,0.000021266673,0.002281959],"genre_scores_gemma":[0.97366047,0.000029680767,0.025287768,0.00048673403,0.000022781613,0.0000066085286,0.00008567019,0.000012796897,0.0004074924],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9992623,0.000009616905,0.00009423958,0.00033358278,0.0001592187,0.00014104224],"domain_scores_gemma":[0.9995078,0.000013875223,0.000028998733,0.00036976833,0.0000015538992,0.00007800406],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00002803248,0.000099584984,0.000081694,2.8298837e-7,0.000094936775,0.00003882181,0.00013909311,0.00004130763,0.0014679405],"category_scores_gemma":[6.833838e-7,0.000082473256,0.000007181577,0.0000722004,0.00017015493,0.00011086614,0.00012903402,0.00005435005,0.00024893152],"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":[0.00050748175,0.0007171712,0.029876525,0.000008178293,0.00008641695,0.000010545014,0.0021501123,0.0028771851,0.8155249,0.00023957409,0.01933373,0.12866822],"study_design_scores_gemma":[0.005487271,0.00080695807,0.045711916,0.000038420505,0.0003321319,0.000011918357,0.0027367054,0.112310074,0.747568,0.0014448671,0.08152376,0.002027964],"about_ca_topic_score_codex":0.00006317075,"about_ca_topic_score_gemma":0.000002994308,"teacher_disagreement_score":0.12664026,"about_ca_system_score_codex":0.000029317012,"about_ca_system_score_gemma":0.0000026448747,"threshold_uncertainty_score":0.99944484},"labels":[],"label_agreement":null},{"id":"W4232565045","doi":"10.5194/acp-2019-1203","title":"Evaluation of climate model aerosol trends with ground-based observations over the last two decades – an AeroCom and CMIP6 analysis","year":2020,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":7,"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":"Leibniz-Institut für Troposphärenforschung; Leibniz-Gemeinschaft; Horizon 2020 Framework Programme; Eidgenössische Technische Hochschule Zürich; European Commission; University of Oxford; Forschungszentrum Jülich; National Center for Atmospheric Research; National Science Foundation","keywords":"Aerosol; Angstrom; Climatology; Environmental science; Angstrom exponent; Climate model; Atmospheric sciences; Meteorology; Climate change; Geography; Geology","score_opus":0.058239654169076345,"score_gpt":0.30410605823295456,"score_spread":0.24586640406387822,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4232565045","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":[0.9434966,0.00002962325,0.052182555,0.00031995669,0.000015893713,0.0003120658,0.000053515912,0.00004290372,0.00354689],"genre_scores_gemma":[0.9812247,0.00001556936,0.018006701,0.0002924702,0.000021011716,0.00012581355,0.00019326214,0.000022705828,0.000097754884],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9974789,0.00017672795,0.00035769952,0.00062307075,0.0011407087,0.00022290325],"domain_scores_gemma":[0.9988774,0.000048119222,0.00032495125,0.00059539534,0.000054158358,0.00009994465],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006687329,0.00028624118,0.0003620054,0.0000061420783,0.00019615999,0.00010170686,0.00035386984,0.00011569399,0.00085647916],"category_scores_gemma":[0.0000103141065,0.000180793,0.0001403941,0.0007048178,0.0002861882,0.00016288368,0.0004231476,0.00022436767,0.0000031109707],"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":[0.000015126971,0.00007124049,0.17093572,0.000008234816,0.00013822486,2.0646478e-7,0.00020229936,0.8260213,0.000422357,0.00010153004,0.00006898933,0.0020147816],"study_design_scores_gemma":[0.00030903623,0.000038786653,0.36983943,0.0000065010877,0.0015212246,1.3585935e-7,0.00008183093,0.6276855,0.00005956656,0.00029993046,0.000005384122,0.00015267779],"about_ca_topic_score_codex":0.0032672596,"about_ca_topic_score_gemma":0.017368976,"teacher_disagreement_score":0.19890372,"about_ca_system_score_codex":0.00014186854,"about_ca_system_score_gemma":0.00006354543,"threshold_uncertainty_score":0.96922964},"labels":[],"label_agreement":null},{"id":"W4232793666","doi":"10.5194/acp-2018-1254","title":"Regional New Particle Formation as Modulators of Cloud Condensation Nuclei and Cloud Droplet Number in the Eastern Mediterranean","year":2018,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Impact","funders":"Horizon 2020 Framework Programme; European Regional Development Fund; European Research Council; European Social Fund; State Scholarships Foundation; European Commission","keywords":"Cloud condensation nuclei; Condensation; Cloud computing; Particle (ecology); Particle number; Cloud physics; Chemical physics; Atmospheric sciences; Environmental science; Materials science; Physics; Meteorology; Aerosol; Geology; Nuclear physics; Computer science; Plasma","score_opus":0.02738168256634759,"score_gpt":0.25882956910509974,"score_spread":0.23144788653875215,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4232793666","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":[0.9911456,0.000013722126,0.001822729,0.0010077757,0.0003121024,0.00029509517,0.00000211875,0.00001611712,0.0053847264],"genre_scores_gemma":[0.9976565,0.000021647871,0.00069549395,0.00054733135,0.00030467575,0.000009278982,0.000013808396,0.000011210127,0.00074003125],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99872625,0.00008203192,0.0003368391,0.0002581454,0.00042777933,0.00016898318],"domain_scores_gemma":[0.99938196,0.000033785986,0.00020059259,0.00030139647,0.0000089647665,0.00007328473],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00031388405,0.00015360127,0.00016611582,0.0000011411996,0.000052515777,0.000038054553,0.00024012911,0.00014713139,0.0026696846],"category_scores_gemma":[0.000015853522,0.00010819525,0.000047801852,0.00008642274,0.00023401035,0.00014718137,0.00031627808,0.00016205412,0.0002494187],"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":[0.00024739295,0.00035213877,0.8120613,0.00015177549,0.000065036234,0.000011531136,0.06731443,0.004285089,0.0017751692,0.0066578225,0.08889787,0.018180456],"study_design_scores_gemma":[0.002708117,0.00038972686,0.5039828,0.00027198947,0.000127005,0.00011605843,0.008368604,0.38774818,0.0022877601,0.07693487,0.015830826,0.0012340745],"about_ca_topic_score_codex":0.0032024619,"about_ca_topic_score_gemma":0.0004806417,"teacher_disagreement_score":0.38346308,"about_ca_system_score_codex":0.00006406871,"about_ca_system_score_gemma":0.000017800767,"threshold_uncertainty_score":0.998242},"labels":[],"label_agreement":null},{"id":"W4232939495","doi":"10.5194/acp-2019-502","title":"Statistical Analysis of Ice Microphysical Properties in Tropical Mesoscale Convective Systems Derived from Cloud Radar and In-Situ Microphysical Observations","year":2019,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"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":"Federal Aviation Administration; Centre National de la Recherche Scientifique; Centre National d’Etudes Spatiales; Transport Canada; National Aeronautics and Space Administration; European Commission; Boeing","keywords":"Ice crystals; Mesoscale meteorology; Environmental science; Radar; Atmospheric sciences; Remote sensing; Meteorology; Liquid water content; Extinction (optical mineralogy); Ice water; Physics; Geology; Cloud computing; Optics","score_opus":0.017020488066709586,"score_gpt":0.21960975354532217,"score_spread":0.20258926547861258,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4232939495","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":[0.9859372,0.00011712298,0.012559052,0.00008927483,0.00015873459,0.0006215125,0.00014624605,0.00001814054,0.0003527547],"genre_scores_gemma":[0.99337846,0.000038009664,0.006135418,0.00006274192,0.000052068415,0.00005942548,0.00008516831,0.000023409688,0.00016528396],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9974102,0.00026863642,0.0006901305,0.00090307894,0.0003883052,0.00033964345],"domain_scores_gemma":[0.99887085,0.00031651245,0.00020268637,0.00046691185,0.000023366661,0.00011968215],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.000079311496,0.00035994832,0.0012101913,0.00001284146,0.000039425555,0.00005311971,0.0003314568,0.00030316086,0.00016649422],"category_scores_gemma":[0.000048860846,0.00029540824,0.00015639908,0.00045814074,0.00065361126,0.00008072245,0.0009232438,0.00057078403,0.000032135427],"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":[0.00024322564,0.00080079114,0.69623655,0.00009097757,0.000523209,0.00001978686,0.0016547673,0.028481705,0.27121302,0.0004475496,0.00007739554,0.00021102112],"study_design_scores_gemma":[0.00048299157,0.00006074816,0.9455548,0.00006708525,0.0003766345,3.228545e-7,0.00061584986,0.048999656,0.0033104243,0.00016572964,0.000020754029,0.0003450132],"about_ca_topic_score_codex":0.019412994,"about_ca_topic_score_gemma":0.0028449567,"teacher_disagreement_score":0.26790258,"about_ca_system_score_codex":0.00031061284,"about_ca_system_score_gemma":0.00005821006,"threshold_uncertainty_score":0.9999498},"labels":[],"label_agreement":null},{"id":"W4233046528","doi":"10.5194/acpd-11-16245-2011","title":"Horizontal variability of aerosol optical depth observed during the ARCTAS airborne experiment","year":2011,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"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; Environmental science; Satellite; Atmospheric sciences; Wavelength; Range (aeronautics); Standard deviation; Phase (matter); Remote sensing; Meteorology; Geology; Physics; Optics; Materials science; Mathematics; Statistics","score_opus":0.026868398031152634,"score_gpt":0.23063429711428932,"score_spread":0.2037658990831367,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4233046528","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":[0.92674315,0.000045239747,0.0023970036,0.00009719487,0.00031951178,0.0006351558,0.000006027796,0.00006720487,0.06968948],"genre_scores_gemma":[0.9832359,0.000023160914,0.015565812,0.000044558637,0.000078023775,0.00013890691,0.000006170343,0.000030726456,0.0008767741],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9975347,0.00013694499,0.0005723251,0.00078539515,0.0005287276,0.0004418859],"domain_scores_gemma":[0.9982376,0.00007029324,0.0002257977,0.0012770855,0.000013857971,0.00017538412],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00048343532,0.00038788503,0.00045480588,8.557449e-7,0.00013619605,0.0000303356,0.00097152696,0.00029259684,0.008964392],"category_scores_gemma":[0.00004777182,0.00024913056,0.0002796006,0.00008957803,0.0006551091,0.000064833075,0.003316004,0.0005427887,0.00013618213],"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":[0.00078266766,0.0044175778,0.73977107,0.0005658308,0.00065784727,0.000061171755,0.008185119,0.00538091,0.21894038,0.0077930233,0.0019229569,0.011521424],"study_design_scores_gemma":[0.0005224257,0.00020903158,0.79618126,0.000050117265,0.00008767619,0.000009081153,0.0005448885,0.00071715534,0.19957156,0.0012703658,0.00011887383,0.0007175321],"about_ca_topic_score_codex":0.0024806506,"about_ca_topic_score_gemma":0.00030153047,"teacher_disagreement_score":0.06881271,"about_ca_system_score_codex":0.00031899023,"about_ca_system_score_gemma":0.000038894785,"threshold_uncertainty_score":0.99999607},"labels":[],"label_agreement":null},{"id":"W4233340239","doi":"10.5194/amt-2021-168","title":"Retrieving microphysical properties of concurrent pristine ice and snow using polarimetric radar observations","year":2021,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"Université de Montréal; Université du Québec à Montréal","funders":"European Research Council; Office of Science; Natural Environment Research Council; Sight Research UK","keywords":"Snow; Polarimetry; Environmental science; Remote sensing; Radar; Precipitation; Meteorology; Ground truth; Atmospheric sciences; Scattering; Geology; Computer science; Geography; Physics; Optics","score_opus":0.05325045153740746,"score_gpt":0.2424367925905252,"score_spread":0.18918634105311774,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4233340239","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":[0.98758906,0.0012689616,0.010216088,0.00009350478,0.00017755476,0.0002478411,0.000007906308,0.000023349821,0.00037570402],"genre_scores_gemma":[0.96197516,0.000111185924,0.03737819,0.00005733781,0.000048254016,0.000003547165,0.000011811536,0.000018150506,0.00039634178],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9986116,0.000055418568,0.0003618273,0.00046091303,0.0003113745,0.00019884194],"domain_scores_gemma":[0.9993168,0.000037142952,0.00022702971,0.00030219127,0.00003371844,0.00008313138],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000121486584,0.00021707201,0.00036710783,0.0000028598122,0.000114932314,0.000067238434,0.00020791094,0.0001424689,0.00032027424],"category_scores_gemma":[0.00014952032,0.00018090899,0.00008809581,0.00039255014,0.00029866802,0.00009371776,0.0016709917,0.0003305098,0.0000035469045],"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":[0.000018339713,0.00042003018,0.18283784,0.0004445149,0.000111101705,0.000009038226,0.0010409447,0.001575296,0.8003332,0.0001139903,0.00023735949,0.012858351],"study_design_scores_gemma":[0.00089677464,0.00019237302,0.7148932,0.0015051585,0.0005124905,0.000030596857,0.0017360665,0.0444096,0.23227261,0.00012285804,0.0016290213,0.0017992147],"about_ca_topic_score_codex":0.0046472396,"about_ca_topic_score_gemma":0.000035060508,"teacher_disagreement_score":0.5680606,"about_ca_system_score_codex":0.00014462069,"about_ca_system_score_gemma":0.00006880866,"threshold_uncertainty_score":0.73772544},"labels":[],"label_agreement":null},{"id":"W4233446949","doi":"10.5194/acp-2018-1201","title":"Technical Note: The Role of Evolving Surface Tension in theFormation of Cloud Droplets","year":2018,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Basic Energy Sciences; Natural Sciences and Engineering Research Council of Canada; U.S. Department of Energy","keywords":"Surface tension; Aerosol; Chemistry; Surface (topology); Chemical physics; Mechanics; Thermodynamics; Physics; Organic chemistry; Geometry","score_opus":0.006504953583363868,"score_gpt":0.2255456953127276,"score_spread":0.21904074172936375,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4233446949","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":[0.9622603,0.00007995237,0.0077010174,0.00013865653,0.00012378315,0.00033315638,0.0000033053043,0.000021210362,0.029338617],"genre_scores_gemma":[0.989366,0.000040527157,0.010391688,0.000033695855,0.000025158588,0.000004705421,0.000003772879,0.000010097231,0.00012437715],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99877566,0.000058532925,0.00042163124,0.00022159747,0.0003650461,0.0001575246],"domain_scores_gemma":[0.9991188,0.000052388903,0.00029219157,0.0004910983,0.000018830386,0.000026714308],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00051381654,0.00013801653,0.00023266312,0.000001224839,0.000032935062,0.000008151566,0.00042804106,0.00022434391,0.0016214704],"category_scores_gemma":[0.00004916407,0.000082139784,0.00007933618,0.00013868154,0.0003034099,0.000061562605,0.0013008566,0.00027824164,0.000049588398],"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":[0.00012466032,0.00059061084,0.35160008,0.00015478602,0.00001854247,0.0000023269183,0.0059339018,0.07173939,0.52978337,0.0006365882,0.005746429,0.033669334],"study_design_scores_gemma":[0.0003697686,0.00019646985,0.42866698,0.00031292497,0.000041993524,0.000007633183,0.0013189445,0.49991906,0.056672867,0.010385069,0.0015971885,0.0005110905],"about_ca_topic_score_codex":0.002747364,"about_ca_topic_score_gemma":0.0003201046,"teacher_disagreement_score":0.47311047,"about_ca_system_score_codex":0.00012335423,"about_ca_system_score_gemma":0.000020259336,"threshold_uncertainty_score":0.9992912},"labels":[],"label_agreement":null},{"id":"W4233474910","doi":"10.5194/amt-2018-139","title":"Lidar temperature series in the middle atmosphere as a reference data set. Part B: Assessment of temperature observations from MLS/Aura and SABER/TIMED satellites","year":2018,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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","funders":"","keywords":"Stratopause; Lidar; Microwave Limb Sounder; Environmental science; Mesosphere; Depth sounding; Altitude (triangle); Atmospheric sciences; Atmosphere (unit); Mesopause; Stratosphere; Satellite; Atmospheric temperature; Remote sensing; Meteorology; Geology; Geography; Physics","score_opus":0.07055145597284586,"score_gpt":0.2856574636295319,"score_spread":0.21510600765668608,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4233474910","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":[0.9854557,0.0007238636,0.000010377901,0.0014349704,0.00020064902,0.0007525233,0.0007972547,0.000048699152,0.01057596],"genre_scores_gemma":[0.9503764,0.0014838862,0.04102336,0.0009485879,0.00017777477,0.00011656992,0.00213405,0.000041960313,0.0036974484],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99682736,0.0002553469,0.00063168234,0.0012322861,0.00067530986,0.00037799307],"domain_scores_gemma":[0.9969694,0.00019893017,0.0003169796,0.002352516,0.00004803976,0.0001141067],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005250856,0.0005174618,0.0005665463,0.0000012647897,0.00023936751,0.0003234545,0.0018161001,0.0006276449,0.0057513174],"category_scores_gemma":[0.00009400803,0.00033720175,0.000064326145,0.0003532,0.0006102193,0.000489356,0.0030618166,0.0010466978,0.000045985165],"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":[0.0001034123,0.00053558743,0.913283,0.0002419274,0.00025916452,0.00004694691,0.007121658,0.0007465194,0.016960382,0.0011471504,0.058468662,0.0010855738],"study_design_scores_gemma":[0.0004835073,0.00022082597,0.95587355,0.0005354311,0.00014697356,0.000014512811,0.0070500453,0.0014843763,0.0008307436,0.004492279,0.027964875,0.00090285967],"about_ca_topic_score_codex":0.0059134304,"about_ca_topic_score_gemma":0.0047507724,"teacher_disagreement_score":0.04259056,"about_ca_system_score_codex":0.00010276407,"about_ca_system_score_gemma":0.00016516732,"threshold_uncertainty_score":0.99990803},"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":"W4234220078","doi":"10.5194/acpd-3-1273-2003","title":"Dependence of solar radiative forcing of forest fire aerosol on ageing and state of mixture","year":2003,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","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":"Plume; Atmospheric sciences; Environmental science; Radiative transfer; Radiative forcing; Forcing (mathematics); Aerosol; Radiative cooling; Convection; Meteorology; Physics; Optics","score_opus":0.008416510922797459,"score_gpt":0.21743913991834474,"score_spread":0.20902262899554727,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4234220078","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":[0.98500866,0.00019450767,0.008808478,0.000020035543,0.00006869044,0.00033430106,0.000025146104,0.000008178909,0.005532015],"genre_scores_gemma":[0.9920415,0.00026588724,0.007077156,0.00004449696,0.0000062917356,0.0000086591,0.0000036694457,0.000017425531,0.0005349075],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99856,0.000055276872,0.0004284698,0.0003889702,0.0003592132,0.00020803839],"domain_scores_gemma":[0.9989406,0.00008787865,0.00053930667,0.0003446704,0.000016041018,0.000071488925],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021429092,0.00023015785,0.0004538909,0.0000019622519,0.000043772456,0.00000942857,0.0002474971,0.00015510785,0.00035297847],"category_scores_gemma":[0.00004694211,0.00019029125,0.00010148676,0.00008714035,0.00029195732,0.0000849157,0.00047639405,0.00028080418,0.000002860494],"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":[0.00019883407,0.00040162372,0.60733956,0.0012234501,0.000238356,0.000037326852,0.007074472,0.30109346,0.027414773,0.0002738846,0.0006968533,0.05400741],"study_design_scores_gemma":[0.0016047404,0.0012294765,0.688153,0.0015886535,0.00020604845,0.000010488895,0.0016131899,0.04087958,0.25493702,0.008212927,0.00012211996,0.0014427318],"about_ca_topic_score_codex":0.0018696162,"about_ca_topic_score_gemma":0.00043196342,"teacher_disagreement_score":0.26021388,"about_ca_system_score_codex":0.00005681418,"about_ca_system_score_gemma":0.000027158761,"threshold_uncertainty_score":0.7759852},"labels":[],"label_agreement":null},{"id":"W4234320334","doi":"10.5194/acpd-12-30589-2012","title":"A pervasive and persistent Asian dust event over North America during spring 2010: lidar and sunphotometer observations","year":2012,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université de Sherbrooke; Environment and Climate Change Canada; University of British Columbia","funders":"Office of Naval Research; U.S. Naval Research Laboratory; Natural Sciences and Engineering Research Council of Canada; National Oceanic and Atmospheric Administration","keywords":"HYSPLIT; Depolarization ratio; AERONET; Mineral dust; Asian Dust; Troposphere; Environmental science; Lidar; Atmospheric sciences; Altitude (triangle); Climatology; Geology; Aerosol; Geography; Meteorology; Remote sensing","score_opus":0.018323417247751196,"score_gpt":0.21553798213269743,"score_spread":0.19721456488494624,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4234320334","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":[0.9956992,0.0002564162,0.00028938468,0.00053896825,0.00019682318,0.0004222116,0.000019096404,0.00004874186,0.0025291063],"genre_scores_gemma":[0.9912487,0.00029826243,0.0052377665,0.00019798384,0.00007885508,0.00007040938,0.000011581299,0.00003350217,0.0028228946],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982963,0.000033323657,0.00027883227,0.0006371224,0.00031789177,0.0004364891],"domain_scores_gemma":[0.9990823,0.0000171499,0.00016711987,0.00041579662,0.0000098639985,0.00030772062],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000074072625,0.0003446906,0.0003109694,0.000004141218,0.00030234194,0.00009960308,0.00020133483,0.00015830573,0.0028768769],"category_scores_gemma":[0.000013533736,0.0003019168,0.0001512305,0.000115565075,0.00025774856,0.00018996498,0.0020087257,0.000388901,0.000055970824],"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":[0.000008290924,0.000065403154,0.99515206,0.000057461377,0.000068997426,0.000006691833,0.0018476922,0.00043696232,0.0004913939,0.000006637304,0.00009969671,0.0017586949],"study_design_scores_gemma":[0.00018140922,0.00002940357,0.99534017,0.00003030607,0.00008704278,0.0000095787245,0.0008681626,0.0007280487,0.000027545368,0.000007541318,0.0023012802,0.00038950253],"about_ca_topic_score_codex":0.0046152375,"about_ca_topic_score_gemma":0.00091157947,"teacher_disagreement_score":0.004948382,"about_ca_system_score_codex":0.00021595597,"about_ca_system_score_gemma":0.000012685629,"threshold_uncertainty_score":0.9999433},"labels":[],"label_agreement":null},{"id":"W4234685505","doi":"10.1007/978-3-662-44185-5_100080","title":"Atmospheric Dusts","year":2015,"lang":"en","type":"book-chapter","venue":"Encyclopedia of Astrobiology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Environmental science","score_opus":0.010453591762737005,"score_gpt":0.2126937699442163,"score_spread":0.2022401781814793,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4234685505","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0048160967,0.0004477734,0.00021060983,0.000062265775,0.00059290224,0.00021273931,0.000029220226,0.000044210152,0.99358416],"genre_scores_gemma":[0.0066472413,0.00047623363,0.008658906,0.00007948806,0.0002814625,0.0000105130075,0.00006172972,0.00006981518,0.9837146],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99843365,0.000024508157,0.00045866118,0.00050145434,0.00022033793,0.00036139705],"domain_scores_gemma":[0.998908,0.000042203566,0.00039703603,0.00046198402,0.000022569904,0.00016823449],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00014675537,0.0003853719,0.00058631145,9.415317e-7,0.000038901722,0.000003342613,0.00044667508,0.0005320791,0.031756908],"category_scores_gemma":[0.000022667547,0.00033972075,0.0001594471,0.000040271378,0.00060584076,0.00004980845,0.0004316108,0.000351174,0.0027084444],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001649213,0.00016065754,0.03997444,0.000049262115,0.0002709049,0.00010323341,0.00050458347,0.0018296007,0.00034496366,0.022413258,0.80491936,0.12926485],"study_design_scores_gemma":[0.00023086407,0.00033878567,0.0019256846,0.000018548757,0.000047782476,0.000016484672,0.000014094369,0.0000141939,0.000003348995,0.003675346,0.9933798,0.00033508564],"about_ca_topic_score_codex":0.000077955134,"about_ca_topic_score_gemma":0.00004924758,"teacher_disagreement_score":0.18846045,"about_ca_system_score_codex":0.00015051628,"about_ca_system_score_gemma":0.000062159765,"threshold_uncertainty_score":0.99990547},"labels":[],"label_agreement":null},{"id":"W4234956140","doi":"10.1360/zd-2013-43-4-523","title":"东亚地区云的垂直重叠特性及其对云辐射强迫的影响","year":2013,"lang":"zh","type":"article","venue":"SCIENTIA SINICA Terrae","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Political science","score_opus":0.01016375234470503,"score_gpt":0.22091864676175596,"score_spread":0.21075489441705092,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4234956140","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":[0.6456451,0.0005265771,0.00060015614,0.004373062,0.0031882913,0.0008022619,0.000021573895,0.00014716905,0.34469584],"genre_scores_gemma":[0.9460892,0.00008086135,0.00429516,0.0017966521,0.00026591893,0.000046402933,0.00000823864,0.000051413477,0.047366135],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99548537,0.00014161055,0.0007153952,0.0012783572,0.0010657639,0.0013135353],"domain_scores_gemma":[0.99760246,0.0000734792,0.00029441266,0.0012924747,0.000038834463,0.0006983361],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00056759256,0.00047717246,0.00042155033,0.0000062110607,0.0007186938,0.00059223454,0.0013943807,0.00027483903,0.15568545],"category_scores_gemma":[0.000084467705,0.00041972837,0.0003130397,0.0009097686,0.0017000333,0.0008674351,0.0011270235,0.0004156386,0.08282516],"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":[0.000023546687,0.0011328018,0.13290015,0.000053488584,0.00012505647,0.00003185431,0.0024052034,0.00026674854,0.034993343,0.0026310524,0.66452,0.16091676],"study_design_scores_gemma":[0.0010829926,0.00044228262,0.7704093,0.00010565596,0.00012080768,0.00003109688,0.0010883207,0.0062014167,0.00066423643,0.0059351763,0.21252748,0.00139126],"about_ca_topic_score_codex":0.0015561294,"about_ca_topic_score_gemma":0.00010307251,"teacher_disagreement_score":0.6375091,"about_ca_system_score_codex":0.00022121798,"about_ca_system_score_gemma":0.00008210273,"threshold_uncertainty_score":0.9998255},"labels":[],"label_agreement":null},{"id":"W4234962043","doi":"10.5194/acp-2020-449","title":"An overview of the ORACLES (ObseRvations of Aerosols above CLouds and their intEractionS) project: aerosol-cloud-radiation interactions in the Southeast Atlantic basin","year":2020,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":100,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Mount Allison University","funders":"Armstrong Flight Research Center; Jet Propulsion Laboratory; Ames Research Center; University of Illinois at Urbana-Champaign; University of Namibia; California State University, Monterey Bay; Sight Research UK; Marshall Space Flight Center; University of Maryland, Baltimore County; Universities Space Research Association; Goddard Space Flight Center; Universiteit Stellenbosch; NASA Headquarters; University of Washington; University of Wisconsin-Madison; North-West University; Langley Research Center; National Aeronautics and Space Administration; Natural Environment Research Council; University of Miami; Purdue University","keywords":"Aerosol; Environmental science; Climatology; Climate model; Meteorology; Atmospheric sciences; Climate change; Geography; Geology; Oceanography","score_opus":0.07248668322479512,"score_gpt":0.30901868328767296,"score_spread":0.23653200006287783,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4234962043","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":[0.99238694,0.00016017146,0.0009505803,0.0030901686,0.00041246339,0.0012453349,0.00013090817,0.00003309156,0.0015903631],"genre_scores_gemma":[0.9977791,0.00032407974,0.0009709707,0.0004911417,0.0001034855,0.00013261997,0.000052193005,0.000029043673,0.00011740818],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99766123,0.00043942733,0.00077667926,0.00053569535,0.00035410703,0.00023285317],"domain_scores_gemma":[0.998084,0.000264312,0.0006759522,0.0008801235,0.000035620513,0.000059970993],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004005614,0.00034758012,0.00046699902,0.0000071218724,0.00018887735,0.00008784753,0.0008590866,0.000119394324,0.00047762465],"category_scores_gemma":[0.0000984285,0.00020074233,0.00021664852,0.0006382222,0.00036238867,0.00028006601,0.0007300349,0.00070919556,0.000012464726],"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":[0.00016634546,0.0019222179,0.8763076,0.00056189863,0.00024029994,0.0000028510874,0.05562183,0.009382794,0.035284165,0.006056301,0.0056165447,0.008837171],"study_design_scores_gemma":[0.0005325564,0.0001686163,0.9411674,0.0006167056,0.00017565231,0.000026138405,0.022239018,0.026354901,0.0019442752,0.002598501,0.0035484747,0.00062772253],"about_ca_topic_score_codex":0.012284317,"about_ca_topic_score_gemma":0.008047668,"teacher_disagreement_score":0.06485985,"about_ca_system_score_codex":0.00011426053,"about_ca_system_score_gemma":0.00009010094,"threshold_uncertainty_score":0.994293},"labels":[],"label_agreement":null},{"id":"W4235173134","doi":"10.5194/acpd-12-31663-2012","title":"Observationally-constrained estimates of global small-mode AOD","year":2012,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","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":"AERONET; Environmental science; Angstrom exponent; Mode (computer interface); Angstrom; Climatology; Aerosol; Satellite; China; Scale (ratio); Meteorology; Geography; Computer science","score_opus":0.02410032345640712,"score_gpt":0.26206909596514116,"score_spread":0.23796877250873405,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4235173134","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":[0.86544913,0.00007429121,0.029723452,0.0003021227,0.00026034456,0.00023771918,0.000065096974,0.000072221104,0.10381564],"genre_scores_gemma":[0.85678405,0.00000845113,0.14234686,0.00017429763,0.0000492016,0.000019581052,0.00004113795,0.000010630455,0.0005657978],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99873,0.000016491225,0.00033613507,0.00033407725,0.0003006277,0.00028269077],"domain_scores_gemma":[0.99926317,0.00003664534,0.00020443411,0.00035985338,0.000013425733,0.00012248558],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00011998365,0.00023662865,0.0002815544,3.2356994e-7,0.000042870575,0.000017887385,0.00042843143,0.00022565662,0.009226455],"category_scores_gemma":[0.00003302568,0.00020016132,0.00012840818,0.00009322201,0.0002750145,0.000060388476,0.0010428205,0.00015288386,0.00020914114],"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":[0.000010404268,0.00015464188,0.9762223,0.000044342425,0.000048461312,0.0000013777543,0.0000923336,0.008375232,0.0009273228,0.00790331,0.0012172145,0.0050031054],"study_design_scores_gemma":[0.00021810483,0.0000237941,0.9672218,0.000039474606,0.000069213114,0.0000048121055,0.0000697185,0.0082548335,0.00046058625,0.022765934,0.00044143476,0.00043027272],"about_ca_topic_score_codex":0.002497469,"about_ca_topic_score_gemma":0.00034196072,"teacher_disagreement_score":0.11262341,"about_ca_system_score_codex":0.00018606418,"about_ca_system_score_gemma":0.000050853163,"threshold_uncertainty_score":0.99167925},"labels":[],"label_agreement":null},{"id":"W4235917980","doi":"10.5194/amtd-8-13285-2015","title":"The Aerosol Limb Imager: acousto-optic imaging of limb scattered sunlight for stratospheric aerosol profiling","year":2015,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Canadian Space Agency","keywords":"Radiance; Aerosol; Remote sensing; Stratosphere; Hyperspectral imaging; Environmental science; Satellite; Sunlight; Optics; Physics; Geology; Meteorology; Astronomy","score_opus":0.015992675520444657,"score_gpt":0.2523168207996573,"score_spread":0.23632414527921264,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4235917980","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":[0.9380796,0.0016186786,0.028313465,0.0016581564,0.0015706139,0.0041904976,0.00010665295,0.00030774478,0.024154581],"genre_scores_gemma":[0.9307363,0.00015279437,0.061001077,0.00026096118,0.00025648947,0.00054937456,0.00005351484,0.0001383846,0.0068510943],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99583066,0.00010470966,0.0010471384,0.0011664425,0.00082897366,0.0010220705],"domain_scores_gemma":[0.99707067,0.00024914683,0.0007890359,0.0014589849,0.00012338268,0.00030878466],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0008982521,0.000728998,0.00074670435,0.0000027660687,0.00046096233,0.00028261862,0.0015946787,0.00031686484,0.0007374653],"category_scores_gemma":[0.00012314098,0.000514607,0.00049123605,0.00024296982,0.0008492287,0.00022553367,0.0020576676,0.0006561476,0.00016128615],"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":[0.0019153415,0.002480387,0.113094404,0.002143566,0.0011509524,0.00009778781,0.0035117278,0.07054404,0.55678815,0.0010324921,0.17895907,0.0682821],"study_design_scores_gemma":[0.008384316,0.0030336939,0.01030365,0.0010647377,0.002059701,0.00018222671,0.014958913,0.4175616,0.51122767,0.011779134,0.008519678,0.010924661],"about_ca_topic_score_codex":0.00032410416,"about_ca_topic_score_gemma":0.00009513319,"teacher_disagreement_score":0.34701756,"about_ca_system_score_codex":0.00039381077,"about_ca_system_score_gemma":0.00022395176,"threshold_uncertainty_score":0.9997305},"labels":[],"label_agreement":null},{"id":"W4236035331","doi":"10.5194/acp-2020-96","title":"Smoke of extreme Australian bushfires observed in the stratosphere over Punta Arenas, Chile, in January 2020: optical thickness, lidar ratios, and depolarization ratios at 355 and 532 nm","year":2020,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":15,"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":"Guangdong Academy of Sciences; National Oceanic and Atmospheric Administration","keywords":"Lidar; Depolarization ratio; Stratosphere; Smoke; Wavelength; Depolarization; Atmospheric sciences; Aerosol; Extinction (optical mineralogy); Environmental science; Materials science; Remote sensing; Optics; Meteorology; Geology; Physics","score_opus":0.03584527320514632,"score_gpt":0.23947488122907118,"score_spread":0.20362960802392485,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4236035331","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":[0.9932961,0.00037543487,0.000283797,0.0023106677,0.00006657681,0.0008913045,0.000028237611,0.00002199951,0.002725884],"genre_scores_gemma":[0.9962198,0.0005071408,0.002388494,0.0004201424,0.000051312512,0.0000488877,0.00009696782,0.00002318227,0.00024407131],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9975938,0.00018885321,0.00065561826,0.0007607778,0.00049340725,0.00030754166],"domain_scores_gemma":[0.9991286,0.00009931214,0.00022285304,0.00041368676,0.000009043663,0.00012653007],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00031677957,0.0003829315,0.0004506364,0.0000027844092,0.00010396234,0.00013197433,0.0003965665,0.00043305563,0.0013989327],"category_scores_gemma":[0.000058482805,0.00028757824,0.00006306093,0.0002806817,0.00037352348,0.0002311914,0.0009665133,0.0006682664,0.000007849401],"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":[0.00005956912,0.00011275322,0.98957753,0.00011606731,0.00002339829,0.000036873113,0.0016081072,0.0014047336,0.0048953234,0.00043953373,0.00080410193,0.0009219958],"study_design_scores_gemma":[0.00051901524,0.00006324683,0.9929986,0.0000968386,0.000032912005,0.000010579383,0.0008942515,0.0032900663,0.0006470974,0.0009770418,0.000133058,0.00033729352],"about_ca_topic_score_codex":0.0074654375,"about_ca_topic_score_gemma":0.015592481,"teacher_disagreement_score":0.008127043,"about_ca_system_score_codex":0.00010291768,"about_ca_system_score_gemma":0.00005589109,"threshold_uncertainty_score":0.9999576},"labels":[],"label_agreement":null},{"id":"W4236168772","doi":"10.1002/0471443395.img061","title":"Lidar","year":2002,"lang":"en","type":"other","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Western University","funders":"","keywords":"Lidar; Remote sensing; Radar; Laser; Wavelength; Optics; Atmosphere (unit); Diffuse sky radiation; Scattering; Environmental science; Ranging; Geology; Physics; Meteorology; Computer science; Geodesy","score_opus":0.00639238368268185,"score_gpt":0.18992422400945982,"score_spread":0.18353184032677797,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4236168772","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0000227935,0.00008640455,0.00043761538,0.000045292432,0.00009416329,0.00005881319,0.0000013609315,0.00014907667,0.9991045],"genre_scores_gemma":[0.0003656808,0.000073814546,0.0042422065,0.00030167738,0.000093636234,0.0000037028851,0.000001113859,0.00016414601,0.994754],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99953336,0.0000045213806,0.000046823763,0.00016798954,0.00012604096,0.00012128881],"domain_scores_gemma":[0.9997337,0.0000019060918,0.00003067299,0.00018738591,1.9182148e-7,0.00004618207],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000011376955,0.00010089485,0.000084778534,2.5142003e-7,0.000013672191,0.0000063722587,0.00013149671,0.000113267415,0.83941],"category_scores_gemma":[0.0000012613723,0.00007567577,0.00003200777,0.000048898848,0.00005966132,0.000008652131,0.000079241705,0.000053329153,0.04977308],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[9.1610794e-8,0.000010044857,0.0011495327,0.0000010225046,0.0000021839862,0.0000028305253,0.000005540707,0.0000014615763,0.0000031382092,0.000026222808,0.9931228,0.0056751333],"study_design_scores_gemma":[0.00003335154,0.000007998466,0.00030566883,0.0000041755106,0.0000034219854,9.3204005e-7,0.000004103585,0.00002486981,0.0000029799644,0.000015327252,0.99948335,0.00011381108],"about_ca_topic_score_codex":0.00077878824,"about_ca_topic_score_gemma":0.00011647709,"teacher_disagreement_score":0.7896369,"about_ca_system_score_codex":0.000021763608,"about_ca_system_score_gemma":7.226899e-7,"threshold_uncertainty_score":0.9509668},"labels":[],"label_agreement":null},{"id":"W4236330837","doi":"10.5194/acp-2016-296","title":"Temporal and spectral cloud screening of polar-winter aerosol optical depth (AOD): impact of homogeneous and inhomogeneous clouds and crystal layers on climatological-scale AODs","year":2016,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University; Université de Sherbrooke","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Aerosol; Environmental science; Lidar; Atmospheric sciences; Homogeneous; Polar; Mode (computer interface); Remote sensing; Meteorology; Geology; Geography; Physics","score_opus":0.013554935925306669,"score_gpt":0.25604810571562575,"score_spread":0.2424931697903191,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4236330837","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":[0.98640037,0.00031319563,0.0045699966,0.000120724544,0.00010376723,0.0004692418,0.00011610829,0.000048171925,0.007858435],"genre_scores_gemma":[0.98747945,0.00026267525,0.011823832,0.00006290528,0.00008513701,0.000010869222,0.000011787423,0.000048362854,0.00021501094],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.997081,0.00011546677,0.000722188,0.0009922948,0.0004528298,0.0006362256],"domain_scores_gemma":[0.99850506,0.00015440877,0.00037146098,0.0005112073,0.000019705343,0.0004381651],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00030644616,0.00061538775,0.0009988133,0.000009405366,0.00011431761,0.000060382044,0.00032352426,0.00055122934,0.00074886257],"category_scores_gemma":[0.00003981565,0.00041080688,0.00028386206,0.000093006754,0.0015741235,0.000079548285,0.0018381884,0.0004724626,0.000005728307],"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":[0.0006164042,0.00022524087,0.96854967,0.000097361946,0.00017531679,0.00007594745,0.00031625535,0.0005380887,0.021723475,0.00007040197,0.00028508273,0.0073267627],"study_design_scores_gemma":[0.0035352677,0.0057304865,0.9566653,0.0005687619,0.00032186013,0.001381587,0.0006800883,0.0044782497,0.022182552,0.0020620155,0.000091190814,0.0023026643],"about_ca_topic_score_codex":0.0009851168,"about_ca_topic_score_gemma":0.0003320762,"teacher_disagreement_score":0.011884387,"about_ca_system_score_codex":0.00011287552,"about_ca_system_score_gemma":0.000036582253,"threshold_uncertainty_score":0.99983436},"labels":[],"label_agreement":null},{"id":"W4236474535","doi":"10.5194/acpd-12-17913-2012","title":"Contrasting trends of mass and optical properties of aerosols over the Northern Hemisphere from 1992 to 2011","year":2012,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":9,"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; Environmental science; Visibility; Extinction (optical mineralogy); Aerodynamic diameter; Atmospheric sciences; Climatology; Particulates; Northern Hemisphere; Mass concentration (chemistry); Human health; Meteorology; Geography; Physics; Chemistry; Optics; Environmental health; Geology","score_opus":0.01648275004194424,"score_gpt":0.21280520120610621,"score_spread":0.19632245116416197,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4236474535","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":[0.9797117,0.0004138555,0.001408084,0.00024285534,0.00007952308,0.00019943719,0.00002528083,0.0000155579,0.01790367],"genre_scores_gemma":[0.9945124,0.000019647212,0.0038342173,0.000083533196,0.0000624074,0.000024891651,0.0000030194392,0.000020355685,0.0014395465],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986618,0.00003274627,0.0003696149,0.0003370165,0.0003381878,0.0002606195],"domain_scores_gemma":[0.9992145,0.000050713516,0.00018363129,0.0004143398,0.000010025374,0.00012682875],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00015739664,0.00023186485,0.00037686055,7.334145e-7,0.000049873244,0.00002080594,0.0003267309,0.00016889811,0.005998421],"category_scores_gemma":[0.000021142478,0.00013330528,0.000090664646,0.000050349045,0.00036888153,0.000049234146,0.0009881523,0.00022091983,0.000033480355],"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":[0.000107562606,0.00015260241,0.78307414,0.00007382956,0.00013870276,0.0000013566395,0.002283077,0.0020953435,0.17448941,0.00006820079,0.0010030464,0.036512755],"study_design_scores_gemma":[0.0006240315,0.00013056943,0.93916804,0.0002767895,0.00023476213,0.0000025779607,0.0014134296,0.0024439846,0.053712904,0.00039093426,0.0007890169,0.00081294624],"about_ca_topic_score_codex":0.009114337,"about_ca_topic_score_gemma":0.001070448,"teacher_disagreement_score":0.15609394,"about_ca_system_score_codex":0.000042296007,"about_ca_system_score_gemma":0.000012994331,"threshold_uncertainty_score":0.997484},"labels":[],"label_agreement":null},{"id":"W4236515549","doi":"10.5194/acpd-13-15007-2013","title":"Comparison of MODIS 3 km and 10 km resolution aerosol optical depth retrievals over land with airborne sunphotometer measurements during ARCTAS summer 2008","year":2013,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","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":"National Aeronautics and Space Administration","keywords":"Environmental science; Aerosol; Moderate-resolution imaging spectroradiometer; AERONET; Remote sensing; Spectroradiometer; Cirrus; Troposphere; Altitude (triangle); Deep blue; Satellite; Meteorology; Smoke; Atmospheric sciences; Geology; Geography; Reflectivity; Physics","score_opus":0.046466424254282865,"score_gpt":0.28673494568647795,"score_spread":0.24026852143219507,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4236515549","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":[0.9861129,0.00022261444,0.0010144749,0.000058231304,0.00008289005,0.00075330766,0.000020011981,0.000047144214,0.011688444],"genre_scores_gemma":[0.9895974,0.000063373365,0.008245325,0.000044629356,0.00004086825,0.00005366684,0.000034728204,0.00004383552,0.0018761747],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99689186,0.000080590835,0.0005985888,0.00083450915,0.0010756261,0.00051882426],"domain_scores_gemma":[0.9986971,0.000038651488,0.00033907336,0.000614577,0.000045614004,0.0002649665],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002937668,0.0004476146,0.0006946778,0.000006757424,0.00013072322,0.00007921418,0.00032187896,0.00036138666,0.0059711747],"category_scores_gemma":[0.000037468737,0.00033434137,0.000101430625,0.00017706287,0.0004848077,0.00017373856,0.0010123096,0.0004493859,0.00012701047],"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":[0.00029265904,0.00025541097,0.98299736,0.000115972354,0.000118805445,0.0000036797903,0.00020674455,0.0037313537,0.008745507,0.0000041737303,0.0030645123,0.00046383837],"study_design_scores_gemma":[0.001212672,0.0002480227,0.9645323,0.00016045234,0.00013698568,0.0000064087108,0.000066741915,0.006972944,0.02583627,0.000030403293,0.00018797278,0.0006088236],"about_ca_topic_score_codex":0.0024822245,"about_ca_topic_score_gemma":0.0007876538,"teacher_disagreement_score":0.01846504,"about_ca_system_score_codex":0.00024055506,"about_ca_system_score_gemma":0.00002652468,"threshold_uncertainty_score":0.9999109},"labels":[],"label_agreement":null},{"id":"W4236926778","doi":"10.5194/acpd-10-21047-2010","title":"Californian wildfire plumes over Southwestern British Columbia: <i>lidar</i> , sunphotometry, and mountaintop chemistry observations","year":2010,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université de Sherbrooke; Environment and Climate Change Canada; University of British Columbia","funders":"Ministry of Environment; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Aerosol; Plume; Smoke; Environmental science; Lidar; Atmospheric sciences; Dominance (genetics); Climatology; Meteorology; Geography; Geology; Chemistry; Remote sensing","score_opus":0.0076582819857489125,"score_gpt":0.2039493956890984,"score_spread":0.19629111370334948,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4236926778","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":[0.9894063,0.00009299938,0.00028863884,0.00017624983,0.00022736253,0.0003920873,0.00024981837,0.00015390698,0.009012622],"genre_scores_gemma":[0.9678464,0.000121470766,0.0033621653,0.0008971122,0.00015568503,0.00009804982,0.00014041296,0.000061802406,0.02731692],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9976521,0.000021315658,0.00041104286,0.00095466716,0.00048296654,0.00047789334],"domain_scores_gemma":[0.9987448,0.000035934776,0.00021328552,0.00067379646,0.000012890286,0.0003192984],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00016790589,0.00032091342,0.00040741306,9.6069e-7,0.000334112,0.0009802518,0.00053433725,0.0007378054,0.014997491],"category_scores_gemma":[0.000039647664,0.0004567289,0.0001416513,0.00017157073,0.0005409277,0.00013276335,0.002001914,0.000980476,0.000088356195],"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":[0.0000021700434,0.000069976195,0.98715854,0.000052674266,0.000027641667,0.000021827715,0.00012367463,0.000038692142,0.0020399068,6.7524485e-7,0.00726732,0.0031968895],"study_design_scores_gemma":[0.00035145512,0.000014511862,0.9598712,0.00006682374,0.000059900514,0.000048901755,0.0002495385,0.0012187306,0.00009110323,0.0005791427,0.036709733,0.000738991],"about_ca_topic_score_codex":0.26958063,"about_ca_topic_score_gemma":0.2091999,"teacher_disagreement_score":0.060380723,"about_ca_system_score_codex":0.0001766772,"about_ca_system_score_gemma":0.00005528149,"threshold_uncertainty_score":0.99978846},"labels":[],"label_agreement":null},{"id":"W4237062980","doi":"10.5194/acp-2018-759","title":"Lidar measurements of thin laminations within Arctic clouds","year":2018,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency; Indigenous and Northern Affairs Canada; Environment and Climate Change Canada; Eurostars; Strong; Ontario Innovation Trust","keywords":"Lidar; Arctic; The arctic; Remote sensing; Environmental science; Geography; Geology; Oceanography","score_opus":0.03135359781036441,"score_gpt":0.25863304312594637,"score_spread":0.22727944531558197,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4237062980","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":[0.8086081,0.000030480744,0.0045525692,0.0001778936,0.0007543671,0.00039766834,0.000009197958,0.000072271636,0.18539743],"genre_scores_gemma":[0.9626489,0.0000067056626,0.029490178,0.00017245642,0.00007670316,0.00002907546,0.0000110834835,0.000024501034,0.0075403713],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980892,0.00007078356,0.00043273304,0.0004658879,0.0007157344,0.00022566604],"domain_scores_gemma":[0.99888176,0.000020859956,0.0003273949,0.000632095,0.000041583648,0.00009630107],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005211125,0.00024016273,0.00027449813,0.0000018028451,0.000094287774,0.000026600932,0.0005707795,0.00022798245,0.010176647],"category_scores_gemma":[0.000074213036,0.00020166909,0.00012206025,0.00014378122,0.00037857037,0.00006174931,0.0011918668,0.00028332873,0.0006145459],"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":[0.000047630525,0.0009803986,0.9484677,0.00035893495,0.00030507473,0.00000831734,0.0059325825,0.01711542,0.007084488,0.0008380762,0.014969194,0.003892239],"study_design_scores_gemma":[0.0016975526,0.00086147664,0.8447857,0.0007675465,0.0006072532,0.000021291866,0.0011446436,0.017054545,0.07872961,0.047392495,0.003877811,0.0030600668],"about_ca_topic_score_codex":0.0013672624,"about_ca_topic_score_gemma":0.00032880073,"teacher_disagreement_score":0.17785706,"about_ca_system_score_codex":0.00022990517,"about_ca_system_score_gemma":0.000044429304,"threshold_uncertainty_score":0.9907282},"labels":[],"label_agreement":null},{"id":"W4237076087","doi":"10.5194/amt-2019-495","title":"Classification of Lidar Measurements Using Supervised and Unsupervised Machine Learning Methods","year":2020,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","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":"Vector Institute; Western University","funders":"","keywords":"Lidar; Artificial intelligence; Computer science; Random forest; Machine learning; Support vector machine; Cluster analysis; sort; Identification (biology); Pattern recognition (psychology); Remote sensing; Geology","score_opus":0.12152598654804954,"score_gpt":0.33140742816619645,"score_spread":0.20988144161814692,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4237076087","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":[0.8682412,0.00027330875,0.12273695,0.00023415826,0.000108419685,0.00034656128,0.0000050800045,0.00006809246,0.007986249],"genre_scores_gemma":[0.73664916,0.000060427727,0.26300815,0.000077349774,0.000021790802,0.000008202332,0.000017146813,0.000026910688,0.00013084269],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9980524,0.0003216879,0.00041820246,0.00059535576,0.0004118458,0.00020046382],"domain_scores_gemma":[0.9992612,0.000040910134,0.00023051225,0.00030446285,0.000019093035,0.00014384685],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00058597437,0.0002682468,0.00040423914,0.0000026451664,0.00011985012,0.000037818423,0.00028598626,0.00020643545,0.0017460055],"category_scores_gemma":[0.00007164048,0.00024021702,0.00009668186,0.00016422253,0.00016947719,0.00007334771,0.00108245,0.00042893697,0.000016846217],"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":[0.000036589758,0.000067298846,0.4194055,0.0001439371,0.00007337218,0.0000012275333,0.0008378275,0.005188455,0.5412188,0.00003398781,0.000026546773,0.032966442],"study_design_scores_gemma":[0.00060712703,0.00009875479,0.26033926,0.000075760596,0.00017607186,0.000002665615,0.000563127,0.7254479,0.010799619,0.00061726524,0.00071176415,0.000560707],"about_ca_topic_score_codex":0.0014994488,"about_ca_topic_score_gemma":0.000027795033,"teacher_disagreement_score":0.7202594,"about_ca_system_score_codex":0.0001229256,"about_ca_system_score_gemma":0.000029116703,"threshold_uncertainty_score":0.99916655},"labels":[],"label_agreement":null},{"id":"W4237082660","doi":"10.5194/acpd-11-26477-2011","title":"Simulation of mineral dust aerosol with piecewise log-normal approximation (PLA) in CanAM4-PAM","year":2011,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada; University of Victoria","funders":"Australian Dental Research Foundation; Canadian Foundation for Climate and Atmospheric Sciences; National Aeronautics and Space Administration","keywords":"Aerosol; Atmospheric sciences; Radiative transfer; Environmental science; Mineral dust; Satellite; Deposition (geology); Consistency (knowledge bases); Piecewise; Meteorology; Mathematics; Physics; Geology; Geometry; Optics","score_opus":0.015668218774731166,"score_gpt":0.22049090656547626,"score_spread":0.20482268779074508,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4237082660","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":[0.934605,0.000013832945,0.02703121,0.000038570608,0.00009266899,0.0005319948,0.000007918444,0.00003422829,0.037644558],"genre_scores_gemma":[0.9873928,0.0000061952637,0.01054873,0.000057458834,0.000032673343,0.000046954017,0.00004028836,0.000023333858,0.0018515744],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99841,0.000043790507,0.00042140073,0.00046117415,0.00037471487,0.00028895985],"domain_scores_gemma":[0.99915713,0.000029559298,0.0003025146,0.0004041565,0.000017379012,0.000089288216],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00017100087,0.00027171013,0.00032400643,0.0000043290443,0.000038062746,0.000017840515,0.00027992213,0.00026591422,0.0032664635],"category_scores_gemma":[0.000016912581,0.00021791134,0.000059541315,0.00017114915,0.00018486285,0.00016856955,0.00042386245,0.00030411012,0.000044831613],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000075723256,0.0001398941,0.16114654,0.000046225214,0.000012203876,0.000004519933,0.00067900727,0.8355754,0.00039591477,0.00005773442,0.00016975353,0.0016970865],"study_design_scores_gemma":[0.0011287378,0.0002664669,0.3266121,0.00013380447,0.00006179831,0.0000034845434,0.0003623897,0.6685901,0.0014351105,0.0004604931,0.000120161036,0.0008253246],"about_ca_topic_score_codex":0.018775105,"about_ca_topic_score_gemma":0.010863641,"teacher_disagreement_score":0.16698524,"about_ca_system_score_codex":0.00021046247,"about_ca_system_score_gemma":0.000045767072,"threshold_uncertainty_score":0.99764466},"labels":[],"label_agreement":null},{"id":"W4237331772","doi":"10.5194/cp-2020-117","title":"On the phenomenon of the blue Sun","year":2020,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Universität Bremen; Deutsche Forschungsgemeinschaft","keywords":"Rayleigh scattering; Scattering; Aerosol; Radiative transfer; Optics; Spectral line; Wavelength; Single-scattering albedo; Computational physics; Physics; Materials science; Meteorology; Astronomy","score_opus":0.01724469312378142,"score_gpt":0.2093284228025785,"score_spread":0.19208372967879705,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4237331772","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":[0.7253869,0.000014199925,0.0006097599,0.0068522138,0.00022438593,0.00031536623,0.000005687963,0.000019708104,0.26657176],"genre_scores_gemma":[0.9920234,0.0000120570685,0.00023854348,0.0022307031,0.00003791636,0.000016942637,8.3959384e-7,0.000011314411,0.005428258],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99910593,0.000050454477,0.00014852505,0.00026088778,0.0003108289,0.00012340149],"domain_scores_gemma":[0.9991889,0.000057396388,0.00011876222,0.0005971148,0.0000022240702,0.000035601974],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00010726676,0.00013609217,0.0001314034,1.3749636e-7,0.00007831111,0.000014584685,0.00080834783,0.00007765054,0.012914237],"category_scores_gemma":[0.000024989253,0.000058832717,0.00011573172,0.00008668578,0.00021790153,0.000009182853,0.001803765,0.00033200384,0.0003715488],"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":[0.00016156153,0.0008988269,0.0771322,0.00019535163,0.00038744963,0.000011108799,0.01697238,0.17078932,0.017404435,0.20186031,0.4862806,0.027906477],"study_design_scores_gemma":[0.0010483027,0.0007295357,0.49212027,0.00034147856,0.00030803218,0.0000049640257,0.005293564,0.028765261,0.032961633,0.28801396,0.14789388,0.002519121],"about_ca_topic_score_codex":0.0004763178,"about_ca_topic_score_gemma":0.000044853445,"teacher_disagreement_score":0.41498807,"about_ca_system_score_codex":0.0000614818,"about_ca_system_score_gemma":0.000013725795,"threshold_uncertainty_score":0.9879881},"labels":[],"label_agreement":null},{"id":"W4238306951","doi":"10.5194/acp-2020-1311-rc1","title":"Reviewer comment","year":2021,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"Agencia Estatal de Investigación; Staatssekretariat für Bildung, Forschung und Innovation; Agència de Gestió d'Ajuts Universitaris i de Recerca; National Oceanic and Atmospheric Administration; Horizon 2020 Framework Programme; Svenska Forskningsrådet Formas; Korea Meteorological Administration; Région Occitanie Pyrénées-Méditerranée; Miljødirektoratet; Environmental Protection Administration, Executive Yuan, R.O.C. Taiwan; Magnus Bergvalls Stiftelse; Ministerio de Asuntos Económicos y Transformación Digital, Gobierno de España; North-West University; U.S. Department of Energy; Vetenskapsrådet; National Research Foundation of Korea; Ministerio de Economía y Competitividad; China Meteorological Administration; Generalitat de Catalunya; Commonwealth Scientific and Industrial Research Organisation; Office of Science; Desert Research Institute; Academy of Finland; Ministry of Science and Technology of the People's Republic of China; National Research Foundation; Helsingin Yliopisto; European Commission; Biological and Environmental Research; Centre National de la Recherche Scientifique; European Regional Development Fund; Ministerstvo Školství, Mládeže a Tělovýchovy","keywords":"Environmental science; Atmospheric sciences; Annual cycle; Diel vertical migration; Range (aeronautics); Aerosol; Polar; Meteorology; Climatology; Geography; Geology; Physics","score_opus":0.022448137786697613,"score_gpt":0.2789819646859945,"score_spread":0.2565338268992969,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4238306951","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000003223085,0.14807774,0.0003434521,0.18903968,0.0040302686,0.00050718343,0.000023631166,0.000051511593,0.65792334],"genre_scores_gemma":[0.000002424107,0.08668059,0.0016764756,0.1293314,0.00024199161,0.0000527121,0.0002223657,0.000023414725,0.7817686],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99827975,0.00006495544,0.0003483403,0.0004682359,0.0005669018,0.00027180978],"domain_scores_gemma":[0.9990013,0.00002212047,0.00013469186,0.0006749923,0.000041710402,0.00012517672],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00026633136,0.00027623773,0.00056511816,2.380533e-7,0.00006569368,0.000021113248,0.0003744769,0.00014043425,0.42191285],"category_scores_gemma":[0.00013670225,0.00020399624,0.00024015686,0.0001800443,0.00007694304,0.000032129767,0.0006209549,0.0002814537,0.00649912],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[1.0780342e-7,0.000031299172,0.00006510208,0.0004300609,0.000010873863,0.000008456537,0.0000032102048,0.0000012589738,6.7794554e-7,0.000009000691,0.96894234,0.030497637],"study_design_scores_gemma":[0.000041569852,0.000014508144,0.000072480274,0.0014450917,0.00007632869,0.00000322004,0.0000046155674,0.000004875376,0.0000032189016,0.000011533887,0.9980529,0.00026968657],"about_ca_topic_score_codex":0.00048825,"about_ca_topic_score_gemma":0.00013801726,"teacher_disagreement_score":0.41541374,"about_ca_system_score_codex":0.00017961914,"about_ca_system_score_gemma":0.000023140947,"threshold_uncertainty_score":0.99427444},"labels":[],"label_agreement":null},{"id":"W4238314144","doi":"10.5194/acp-2021-540-rc1","title":"Comment on acp-2021-540","year":2021,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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; Environmental science; Lagrangian; Meteorology; Cloud computing; Atmospheric sciences; Software deployment; Geography; Computer science; Geology; Physics","score_opus":0.020214455272038537,"score_gpt":0.27152768706127833,"score_spread":0.2513132317892398,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4238314144","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000035463734,0.00607827,0.00019288414,0.32449418,0.0015687445,0.0003681329,0.000038491875,0.000038268943,0.66718554],"genre_scores_gemma":[0.00008078539,0.009963484,0.0013819683,0.17539059,0.0002363464,0.000058809248,0.00030799478,0.000035988352,0.81254405],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9979112,0.00007147652,0.00031364863,0.0006132553,0.00073798856,0.0003524003],"domain_scores_gemma":[0.99890274,0.00005128524,0.00012751047,0.00074966287,0.000009888524,0.0001589018],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0002095797,0.00035115957,0.00051259046,5.575823e-7,0.000103377024,0.000035638135,0.00045955725,0.00019636977,0.3541338],"category_scores_gemma":[0.000034363507,0.00026834983,0.00023216293,0.0001962678,0.000092702176,0.000031639025,0.0005797967,0.0004048035,0.008842665],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000011584133,0.0000868966,0.000052829735,0.00010872784,0.00001713358,0.000022471011,0.0000091492075,0.000013438213,0.0000030081164,0.000070434464,0.9724338,0.027180938],"study_design_scores_gemma":[0.00008789939,0.000067459696,0.00018015102,0.0006782036,0.000050091116,0.00000335717,0.000018734409,0.000017971937,0.000022496592,0.000032563126,0.9985068,0.00033430415],"about_ca_topic_score_codex":0.0009958247,"about_ca_topic_score_gemma":0.00024037228,"teacher_disagreement_score":0.34529114,"about_ca_system_score_codex":0.00030223673,"about_ca_system_score_gemma":0.000028447108,"threshold_uncertainty_score":0.9999769},"labels":[],"label_agreement":null},{"id":"W4239031549","doi":"10.5194/acpd-8-11997-2008","title":"Intercomparison of aerosol optical depth from Brewer ozone spectrophotometers and CIMEL sunphotometers measurements","year":2008,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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":"AERONET; Environmental science; Aerosol; Ozone; Remote sensing; Correlation coefficient; Atmospheric sciences; Meteorology; Physics; Geology; Mathematics; Statistics","score_opus":0.036882115707699815,"score_gpt":0.2527000228258574,"score_spread":0.2158179071181576,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4239031549","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":[0.96441627,0.00017792414,0.006623893,0.000050984818,0.00037347237,0.00049739215,0.000018778728,0.000061984065,0.027779302],"genre_scores_gemma":[0.9553846,0.00033609162,0.04357666,0.00017890625,0.000045264795,0.00003510234,0.000026004092,0.000045983863,0.00037140117],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99691224,0.000070532245,0.00066012156,0.0009832173,0.0008984111,0.0004754647],"domain_scores_gemma":[0.9986226,0.00006263251,0.00029675246,0.00070666836,0.000018996909,0.00029235973],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00017711996,0.00050528004,0.00080232,0.000007683552,0.00007409142,0.00005097672,0.000589721,0.00033587572,0.0028931338],"category_scores_gemma":[0.00003174222,0.00044107894,0.00022267395,0.00017377941,0.0006713626,0.000100541336,0.0018873549,0.000542913,0.0001339427],"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":[0.00039266335,0.0009833848,0.7472129,0.000094673116,0.00069431914,0.000061014067,0.0019540994,0.0017222748,0.22365156,0.0000053001,0.010489481,0.012738368],"study_design_scores_gemma":[0.0034671973,0.00092926336,0.6686091,0.00038002935,0.0005393839,0.000048839513,0.000813095,0.007949862,0.3131709,0.00039828836,0.00070888625,0.002985131],"about_ca_topic_score_codex":0.006617921,"about_ca_topic_score_gemma":0.0004420627,"teacher_disagreement_score":0.08951937,"about_ca_system_score_codex":0.00032419906,"about_ca_system_score_gemma":0.000029328126,"threshold_uncertainty_score":0.9999971},"labels":[],"label_agreement":null},{"id":"W4239102934","doi":"10.5194/acp-2021-344-ac2","title":"Reply on RC1","year":2021,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"York University","funders":"","keywords":"Weather Research and Forecasting Model; Settling; Surface roughness; Deposition (geology); Meteorology; Surface finish; Environmental science; Span (engineering); Boundary layer; Surface water; Atmospheric sciences; Planetary boundary layer; Turbulence; Materials science; Mechanics; Physics; Geology; Composite material; Engineering","score_opus":0.019045943199940407,"score_gpt":0.26867678518543386,"score_spread":0.24963084198549346,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4239102934","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00006607583,0.0066246907,0.00008358195,0.06611104,0.0012463267,0.00021778535,0.00001632845,0.00005834043,0.92557585],"genre_scores_gemma":[0.000047809244,0.005730618,0.001113133,0.091443926,0.00017908085,0.000025415846,0.00012150557,0.000026417789,0.9013121],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9983573,0.00003678846,0.00023805822,0.0005689052,0.00055049354,0.00024848705],"domain_scores_gemma":[0.99905044,0.000029057855,0.00010139777,0.00070614857,0.0000074974614,0.00010547344],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00015442375,0.00024336661,0.0003678549,2.982753e-7,0.00006312454,0.00002135781,0.00032187183,0.00012935654,0.26420373],"category_scores_gemma":[0.00005882589,0.00018247814,0.00017858099,0.00016856668,0.00007215849,0.0000255684,0.00030729384,0.000298005,0.008318856],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[6.82403e-7,0.000029503397,0.00006274954,0.00009036476,0.0000075665826,0.000023549655,0.000004346158,0.000008694163,0.0000031192837,0.000026622176,0.9836856,0.016057199],"study_design_scores_gemma":[0.000041501626,0.000041872965,0.0002871282,0.000516973,0.000029730001,0.0000059928143,0.0000062887857,0.0000078315,0.000016019232,0.000027443215,0.998779,0.00024019465],"about_ca_topic_score_codex":0.00091079273,"about_ca_topic_score_gemma":0.00012870388,"teacher_disagreement_score":0.2558849,"about_ca_system_score_codex":0.00014605986,"about_ca_system_score_gemma":0.000025189,"threshold_uncertainty_score":0.9924533},"labels":[],"label_agreement":null},{"id":"W4239813900","doi":"10.5194/acp-2021-90-cc1","title":"Comment on acp-2021-90","year":2021,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Goddard Space Flight Center; European Centre for Medium-Range Weather Forecasts; Forschungszentrum Jülich; National Natural Science Foundation of China; Deutsche Forschungsgemeinschaft; Langley Research Center; National Aeronautics and Space Administration","keywords":"Mesoscale meteorology; Climatology; Thunderstorm; Middle latitudes; Convection; Atmospheric sciences; Storm; Environmental science; Stratosphere; Geology; Geography; Meteorology; Oceanography","score_opus":0.0201382623075808,"score_gpt":0.27146127495665695,"score_spread":0.25132301264907614,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4239813900","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000027595162,0.0055872453,0.00017799156,0.30901217,0.0014529647,0.00034427404,0.000035449615,0.000035111094,0.6833272],"genre_scores_gemma":[0.0000572775,0.009691501,0.0013432251,0.16740936,0.00022220136,0.0000554583,0.00029078842,0.000033624172,0.82089657],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9979505,0.00006987423,0.00030713805,0.00060181605,0.0007253183,0.00034534003],"domain_scores_gemma":[0.998925,0.000048756632,0.00012453324,0.0007367277,0.000009577648,0.00015543852],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00020608712,0.00034378222,0.00049768854,5.359977e-7,0.000100266596,0.000034779063,0.00045069796,0.00019241762,0.3576749],"category_scores_gemma":[0.000033212928,0.00026225648,0.00022738159,0.00019173718,0.000089986024,0.000030864,0.0005699091,0.00039675354,0.008962759],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000001072007,0.00008634113,0.00006034778,0.00010881916,0.000016730763,0.000021962574,0.000009240273,0.000013242923,0.000003274452,0.00008046034,0.9790725,0.02052598],"study_design_scores_gemma":[0.00008625412,0.00006605349,0.00015585517,0.00066418503,0.000049095594,0.000003194103,0.00001845904,0.000017736746,0.000020416042,0.00003217343,0.9985597,0.00032685534],"about_ca_topic_score_codex":0.00073341536,"about_ca_topic_score_gemma":0.00017747804,"teacher_disagreement_score":0.34871215,"about_ca_system_score_codex":0.0002966049,"about_ca_system_score_gemma":0.000027661426,"threshold_uncertainty_score":0.99998295},"labels":[],"label_agreement":null},{"id":"W4239872302","doi":"10.5194/acp-2021-652-rc1","title":"Comment on acp-2021-652","year":2021,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Assertion; The arctic; AERONET; Climatology; Arctic; Environmental science; Scale (ratio); Meteorology; Geography; Aerosol; Computer science; Geology; Cartography; Oceanography","score_opus":0.020229250919800396,"score_gpt":0.27157847910670874,"score_spread":0.25134922818690836,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4239872302","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000035164514,0.0061184578,0.00019210724,0.32701182,0.0015703406,0.0003720922,0.00003878361,0.000038411992,0.66462284],"genre_scores_gemma":[0.00008052197,0.009957998,0.0014102478,0.17657559,0.00023754389,0.000059120917,0.0003114977,0.00003614819,0.81133133],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99790514,0.00007156481,0.00031438615,0.0006144839,0.0007412284,0.0003531806],"domain_scores_gemma":[0.9989003,0.000050829203,0.00012767572,0.0007522173,0.00000990627,0.00015907799],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00021102287,0.00035172424,0.0005085213,5.58098e-7,0.00010445033,0.000036540812,0.00046003822,0.00019734337,0.35479674],"category_scores_gemma":[0.000034240995,0.0002687022,0.00023260711,0.00019617431,0.000093887735,0.000031682197,0.00057997927,0.00040763567,0.008858044],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000011313996,0.000088409295,0.00006183408,0.00010964727,0.000017230048,0.000022637205,0.000009436197,0.0000133265885,0.000003460755,0.00008104728,0.9783976,0.021194229],"study_design_scores_gemma":[0.00008894022,0.000067493376,0.0001586873,0.0006795983,0.00005019925,0.0000033604663,0.000018951763,0.0000180579,0.000023122153,0.00003267842,0.99852425,0.00033465266],"about_ca_topic_score_codex":0.00074847636,"about_ca_topic_score_gemma":0.00018167698,"teacher_disagreement_score":0.34593868,"about_ca_system_score_codex":0.0003027838,"about_ca_system_score_gemma":0.000028941235,"threshold_uncertainty_score":0.9999765},"labels":[],"label_agreement":null},{"id":"W4239979072","doi":"10.5194/acp-2021-344-ac1","title":"Reply on RC2","year":2021,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"York University","funders":"","keywords":"Weather Research and Forecasting Model; Settling; Surface roughness; Deposition (geology); Meteorology; Environmental science; Surface finish; Span (engineering); Planetary boundary layer; Atmospheric sciences; Boundary layer; Turbulence; Materials science; Mechanics; Physics; Geology; Composite material","score_opus":0.019045943199940407,"score_gpt":0.26867678518543386,"score_spread":0.24963084198549346,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4239979072","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00007339376,0.006626174,0.000085339314,0.06749334,0.0012775032,0.000223656,0.00001605374,0.00006696423,0.9241376],"genre_scores_gemma":[0.000057928308,0.0055187903,0.0011050716,0.09161222,0.0001791239,0.000025475869,0.00011688475,0.000028613716,0.90135586],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99835926,0.00003672849,0.00023783771,0.0005683055,0.00054970686,0.00024817928],"domain_scores_gemma":[0.99905145,0.000029003035,0.00010134984,0.0007053351,0.0000074847317,0.00010538376],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00015200194,0.00024323845,0.0003675679,2.9780944e-7,0.000060103863,0.00002131874,0.00032117395,0.00012925117,0.25259578],"category_scores_gemma":[0.000058684054,0.00018239078,0.00017851648,0.00016815777,0.000072031144,0.000025551371,0.0003066321,0.0002976342,0.007907454],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[6.827807e-7,0.000029477997,0.00008260506,0.00009033812,0.0000075728058,0.000023572531,0.00000432246,0.0000065736435,0.0000032153307,0.000025244235,0.9850034,0.014722963],"study_design_scores_gemma":[0.000041244875,0.000041802254,0.00031945313,0.00051612896,0.000029716552,0.0000059897075,0.0000062704107,0.0000074732698,0.000016257993,0.000027179212,0.9987484,0.0002400377],"about_ca_topic_score_codex":0.0008581043,"about_ca_topic_score_gemma":0.00013444075,"teacher_disagreement_score":0.24468833,"about_ca_system_score_codex":0.0001438652,"about_ca_system_score_gemma":0.00002506277,"threshold_uncertainty_score":0.992865},"labels":[],"label_agreement":null},{"id":"W4240426560","doi":"10.5194/amtd-7-2545-2014","title":"Verification and application of the extended Spectral Deconvolution Algorithm (SDA+) methodology to estimate aerosol fine and coarse mode extinction coefficients in the marine boundary layer","year":2014,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"Université de Sherbrooke","funders":"","keywords":"AERONET; Aerosol; Nephelometer; Deconvolution; Extinction (optical mineralogy); Remote sensing; Environmental science; Mode (computer interface); Absorption (acoustics); Scattering; Algorithm; Mathematics; Computer science; Meteorology; Optics; Physics; Light scattering; Geology","score_opus":0.018262613743780565,"score_gpt":0.30055778751210993,"score_spread":0.28229517376832935,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4240426560","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":[0.54494154,0.000015609692,0.45359868,0.00033837315,0.0000899324,0.0006067135,0.0000044655376,0.000012442956,0.00039221943],"genre_scores_gemma":[0.8973723,0.000024211973,0.10212581,0.00014999857,0.0000300795,0.00013977838,0.000022429635,0.000012333414,0.0001230387],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99842227,0.00029375707,0.00033639825,0.00051679055,0.00023658783,0.00019417412],"domain_scores_gemma":[0.999111,0.0001035785,0.00022156918,0.0005008565,0.000014286482,0.000048727616],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00086148875,0.0001931364,0.00023737775,0.0000045506117,0.00013799581,0.00003336482,0.00028049175,0.000166964,0.00009194408],"category_scores_gemma":[0.00005924316,0.0001258802,0.000039464925,0.00015416932,0.00030416454,0.000048264796,0.000694808,0.00024957865,0.0000062919066],"study_design_candidate":"design_other","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":[0.00018594803,0.00041889047,0.06621999,0.000102158774,0.00003198343,0.0000010156447,0.002094503,0.061604932,0.026528688,0.0014719313,0.00040855125,0.8409314],"study_design_scores_gemma":[0.00031932874,0.00007763958,0.49874857,0.000012886853,0.00004008765,0.000014107365,0.000099132114,0.4918662,0.0015882503,0.006734477,0.00031089663,0.00018840416],"about_ca_topic_score_codex":0.0021167423,"about_ca_topic_score_gemma":0.00181259,"teacher_disagreement_score":0.840743,"about_ca_system_score_codex":0.00011225117,"about_ca_system_score_gemma":0.000015825564,"threshold_uncertainty_score":0.51332456},"labels":[],"label_agreement":null},{"id":"W4240692390","doi":"10.5194/acpd-9-7781-2009","title":"Physical properties of High Arctic tropospheric particles during winter","year":2009,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"Eurostars; Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency; National Science Foundation; Government of Canada; National Oceanic and Atmospheric Administration; Nova Scotia Research Innovation Trust; Canadian Foundation for Climate and Atmospheric Sciences; Ontario Innovation Trust","keywords":"Troposphere; Ice crystals; Lidar; Snow; Depolarization ratio; Atmospheric sciences; Ice cloud; Environmental science; Ice nucleus; Arctic; Planetary boundary layer; Geology; Meteorology; Remote sensing; Turbulence; Geomorphology; Physics; Optics; Radiative transfer","score_opus":0.01008052178592663,"score_gpt":0.20311217217052968,"score_spread":0.19303165038460304,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4240692390","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":[0.9971483,0.00005845172,0.00043849577,0.00022149392,0.00007649787,0.00019111589,0.0000010706318,0.00005243439,0.0018121497],"genre_scores_gemma":[0.99519897,0.00001865736,0.002939426,0.000069102076,0.00007974947,0.000019258392,0.0000010624632,0.000018115326,0.0016556822],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99879265,0.000035307698,0.00024048224,0.00038082016,0.0002921312,0.00025858308],"domain_scores_gemma":[0.9994084,0.0000055445953,0.00012362286,0.0003808059,0.000007739286,0.000073839445],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00004250433,0.00021838186,0.00031841287,4.726422e-7,0.000047269656,0.000024569643,0.00030140503,0.00008520823,0.002230698],"category_scores_gemma":[0.000009730671,0.00015390893,0.00014016949,0.00007115137,0.00025711252,0.00006501947,0.0007085289,0.00021961424,0.00018294077],"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":[0.00048101624,0.0032032768,0.2309006,0.0010454003,0.00031928852,0.000048451177,0.006961169,0.15191244,0.57262236,0.00092098233,0.001514648,0.030070348],"study_design_scores_gemma":[0.00072494353,0.00034332645,0.6823584,0.00040718412,0.00015382859,0.000010216656,0.00056477723,0.010273178,0.29227778,0.011684019,0.000121556564,0.0010808294],"about_ca_topic_score_codex":0.0015682712,"about_ca_topic_score_gemma":0.00006388883,"teacher_disagreement_score":0.45145774,"about_ca_system_score_codex":0.00012287188,"about_ca_system_score_gemma":0.00001028114,"threshold_uncertainty_score":0.9986814},"labels":[],"label_agreement":null},{"id":"W4240871926","doi":"10.5194/amt-2019-48","title":"Development and validation of a supervised machine learning radar Doppler spectra peak finding algorithm","year":2019,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Radar; Algorithm; Doppler radar; Doppler effect; Zenith; Cloud computing; Computer science; Remote sensing; Smoothing; Spectral line; Meteorology; Geology; Physics; Computer vision","score_opus":0.016202795125417575,"score_gpt":0.22539383640507402,"score_spread":0.20919104127965643,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4240871926","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":[0.93375343,0.00009269636,0.055812996,0.000059653416,0.00013403257,0.00033382935,0.0000053322597,0.00004568605,0.009762315],"genre_scores_gemma":[0.60857326,0.000088207984,0.38695836,0.000033696484,0.000028962158,0.000012198727,0.00008517236,0.000026634745,0.0041935206],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99858725,0.000041581923,0.00032892884,0.00046090456,0.0003600173,0.00022132456],"domain_scores_gemma":[0.99949104,0.000032008593,0.00018537551,0.00021297019,0.0000065252457,0.000072104776],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002909754,0.00023455996,0.00029354444,0.0000030899616,0.00009340031,0.000037718717,0.00019483066,0.00014972509,0.0046286327],"category_scores_gemma":[0.00001276474,0.00020300043,0.00005497116,0.00007842762,0.00006590977,0.00006763778,0.0009544253,0.00034198927,0.0001038088],"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":[0.000059376063,0.0003519672,0.46575144,0.00050278613,0.00029479642,0.000022458888,0.016895285,0.03587623,0.02857043,0.00019953575,0.0010867692,0.45038894],"study_design_scores_gemma":[0.0035924853,0.00037105833,0.37354282,0.0005222526,0.0002526928,0.00006700499,0.0042511793,0.43779182,0.13558269,0.0009187068,0.039331924,0.0037753838],"about_ca_topic_score_codex":0.0006648108,"about_ca_topic_score_gemma":0.000029958004,"teacher_disagreement_score":0.44661355,"about_ca_system_score_codex":0.00014755594,"about_ca_system_score_gemma":0.000034868324,"threshold_uncertainty_score":0.99628127},"labels":[],"label_agreement":null},{"id":"W4240981817","doi":"10.5194/amt-2019-182","title":"Analysis of Global Three-Dimensional Aerosol Structure with Spectral Radiance Matching","year":2019,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","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":"Environment and Climate Change Canada","funders":"Natural Science Foundation of Zhejiang Province; National Natural Science Foundation of China","keywords":"Radiance; Nadir; Remote sensing; Lidar; Aerosol; Environmental science; Track (disk drive); Pixel; Meteorology; Geology; Satellite; Computer science; Geography; Optics; Physics","score_opus":0.005725789815775107,"score_gpt":0.21479408913116602,"score_spread":0.20906829931539092,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4240981817","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":[0.9812022,0.00007067987,0.012153119,0.00009683624,0.0001633986,0.0002756724,0.00016256538,0.000036709385,0.0058388133],"genre_scores_gemma":[0.9744294,0.0000035964144,0.024826143,0.00017082141,0.000034746725,0.000004140468,0.000050605955,0.00001649348,0.00046401063],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99794585,0.000024700787,0.00031489352,0.0007205538,0.0006550975,0.00033890532],"domain_scores_gemma":[0.9988607,0.000020143649,0.00029983345,0.00069162785,0.000011866637,0.00011581245],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00007297049,0.00034772162,0.0006422327,0.0000020721345,0.000058545465,0.000033861204,0.0004983527,0.00023831317,0.011382707],"category_scores_gemma":[0.0000027582046,0.0002498558,0.00023352038,0.00054862956,0.00022064429,0.00007321142,0.0007304609,0.0003464151,0.000063036685],"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":[0.000025517627,0.000020191643,0.47814626,0.000010444265,0.0003817009,0.0000042616043,0.00003060295,0.5206311,0.00023309475,0.000100546764,0.00016777538,0.0002485502],"study_design_scores_gemma":[0.00026002736,0.00006847259,0.95437306,0.000038282764,0.0008508332,0.0000065170166,0.000035457226,0.042295095,0.00022914383,0.0013196026,0.00001887231,0.0005046291],"about_ca_topic_score_codex":0.0058117723,"about_ca_topic_score_gemma":0.013194841,"teacher_disagreement_score":0.47833595,"about_ca_system_score_codex":0.0003064865,"about_ca_system_score_gemma":0.00006372234,"threshold_uncertainty_score":0.99999535},"labels":[],"label_agreement":null},{"id":"W4241494195","doi":"10.5194/amtd-4-1-2011","title":"Maritime Aerosol Network as a component of AERONET – first results and comparison with global aerosol models and satellite retrievals","year":2011,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Université du Québec à Rimouski; Institut du Savoir Montfort; Université de Sherbrooke","funders":"NASA Headquarters; National Aeronautics and Space Administration","keywords":"AERONET; Aerosol; Satellite; Environmental science; Climatology; The arctic; Oceanography; Arctic; Meteorology; Geography; Geology","score_opus":0.022897719465905284,"score_gpt":0.23777128440903728,"score_spread":0.21487356494313198,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4241494195","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":[0.9060672,0.002418451,0.007751921,0.00033647005,0.0001823899,0.0015372402,0.0001472397,0.00012660911,0.08143248],"genre_scores_gemma":[0.9652886,0.0017138808,0.0318125,0.00016865702,0.000059128124,0.00003397486,0.00006790941,0.000040690116,0.0008146784],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9963753,0.00010876088,0.0009268218,0.0012640976,0.0006673355,0.00065768335],"domain_scores_gemma":[0.99798816,0.000092852686,0.00064683385,0.00084213517,0.00003116872,0.00039883287],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0004423805,0.00065498153,0.0010664918,0.0000020889734,0.00020881632,0.00010434494,0.00046680873,0.0004909944,0.0005013107],"category_scores_gemma":[0.000014673774,0.00052836107,0.0000949741,0.00020409639,0.0010095902,0.00016436637,0.0023895153,0.00046640125,0.000043287815],"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":[0.013870585,0.0021298435,0.66651285,0.0011765589,0.001185276,0.00015452482,0.0064190333,0.25095522,0.0004462653,0.0055380845,0.02983897,0.021772806],"study_design_scores_gemma":[0.020106135,0.008668252,0.53909445,0.0047251345,0.002075496,0.00051895203,0.001819241,0.3600444,0.0036094047,0.0417423,0.006952839,0.010643411],"about_ca_topic_score_codex":0.008593611,"about_ca_topic_score_gemma":0.002644704,"teacher_disagreement_score":0.12741838,"about_ca_system_score_codex":0.0001626429,"about_ca_system_score_gemma":0.00003896542,"threshold_uncertainty_score":0.9997168},"labels":[],"label_agreement":null},{"id":"W4241620382","doi":"10.5194/gmd-2016-267","title":"A new aerosol wet removal scheme for the Lagrangian particle model FLEXPART","year":2016,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":6,"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":"Leibniz-Institut für Troposphärenforschung; Leibniz-Gemeinschaft; NordForsk; National Oceanic and Atmospheric Administration; U.S. Department of Energy; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; Environment and Climate Change Canada","keywords":"Aerosol; Scavenging; Ice nucleus; Atmospheric sciences; Environmental science; Meteorology; Nucleation; Chemistry; Geology; Physics; Thermodynamics","score_opus":0.024360303761236567,"score_gpt":0.25570606508954324,"score_spread":0.23134576132830667,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4241620382","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"methods","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.09380644,0.00017629686,0.8586649,0.008102419,0.00037613866,0.001173967,0.000028321883,0.00016466863,0.03750688],"genre_scores_gemma":[0.5783118,0.000079014346,0.19434123,0.002035378,0.00045868606,0.0002960959,0.0000074847503,0.000074015945,0.22439632],"study_design_codex":"not_applicable","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99841833,0.000016396067,0.00025407487,0.0005362144,0.0003145598,0.00046045074],"domain_scores_gemma":[0.9988625,0.00006809204,0.000104553445,0.00076141895,0.000008172865,0.00019525677],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021597394,0.00025969578,0.00021376905,3.7944497e-7,0.00019185308,0.00007132213,0.00066299044,0.00019144015,0.004527015],"category_scores_gemma":[0.000022776583,0.00014168643,0.00022349549,0.000057623147,0.0001401919,0.00008009492,0.0010031711,0.00018353722,0.00065713486],"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":[0.00029660505,0.00021799878,0.0065088663,0.000060530558,0.00023420951,0.000010574884,0.0013955352,0.05553575,0.041037492,0.013019854,0.78770614,0.09397642],"study_design_scores_gemma":[0.0013510315,0.00009256834,0.00081167585,0.00006540218,0.00012396317,0.000010646724,0.00016319806,0.8844129,0.00944431,0.021926435,0.08059283,0.0010050389],"about_ca_topic_score_codex":0.00044137487,"about_ca_topic_score_gemma":0.0002150141,"teacher_disagreement_score":0.82887715,"about_ca_system_score_codex":0.00009610382,"about_ca_system_score_gemma":0.00006221282,"threshold_uncertainty_score":0.996383},"labels":[],"label_agreement":null},{"id":"W4241703595","doi":"10.5194/acp-2018-459","title":"Interpretation of Measured Aerosol Mass Scattering Efficiency Over North America Using a Chemical Transport Model","year":2018,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","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":"Dalhousie University","funders":"Health Effects Institute; U.S. Environmental Protection Agency","keywords":"Aerosol; Scattering; Atmospheric sciences; Environmental science; Particle (ecology); Visibility; Mass concentration (chemistry); Computational physics; Physics; Meteorology; Optics; Geology; Thermodynamics","score_opus":0.016046705651482203,"score_gpt":0.23756341132336697,"score_spread":0.22151670567188478,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4241703595","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":[0.60710883,0.000008079627,0.39030102,0.000010061014,0.0000821201,0.00019389579,0.000013350624,0.000030048017,0.0022525946],"genre_scores_gemma":[0.9415186,0.000007426564,0.05814911,0.00010922627,0.000035816855,0.000018457109,0.000019585152,0.000035327612,0.00010642909],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9978457,0.000023434764,0.0005334719,0.0006726889,0.0005909389,0.00033378231],"domain_scores_gemma":[0.9990389,0.0000107495935,0.00031924614,0.0004908791,0.000023545623,0.000116698335],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00010045873,0.00033010682,0.00042990092,0.000003110533,0.000056822344,0.000017631615,0.00049429527,0.00020205026,0.0014248247],"category_scores_gemma":[0.0000104965875,0.00030129534,0.00021522435,0.00017337085,0.0004989065,0.00007828367,0.00039309284,0.00027628406,0.000034046523],"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":[0.00006952263,0.00012323422,0.039519858,0.000080627084,0.00003589123,0.0000020271589,0.0015531632,0.76167154,0.19507147,0.0000010752967,0.000075950826,0.0017956472],"study_design_scores_gemma":[0.00015302908,0.000030861458,0.0031087548,0.00007709482,0.00006659165,0.0000012392478,0.000040623305,0.98884636,0.0072296485,0.00007397634,0.000007642568,0.00036416433],"about_ca_topic_score_codex":0.0008344042,"about_ca_topic_score_gemma":0.000054769724,"teacher_disagreement_score":0.3344098,"about_ca_system_score_codex":0.0002670192,"about_ca_system_score_gemma":0.000055262484,"threshold_uncertainty_score":0.9999439},"labels":[],"label_agreement":null},{"id":"W4241709277","doi":"10.5194/acp-2015-1003","title":"An evaluation of the impact of aerosol particles on weather forecasts from a biomass burning aerosol event over the Midwestern US: Observational-based analysis of surface temperature","year":2016,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Office of Naval Research; National Aeronautics and Space Administration; National Science Foundation","keywords":"Aerosol; Environmental science; Daytime; Atmospheric sciences; Moderate-resolution imaging spectroradiometer; Climatology; Smoke; Meteorology; Plume; Radiative forcing; Overcast; Geography; Satellite; Geology","score_opus":0.03930549232270588,"score_gpt":0.31116919749659827,"score_spread":0.2718637051738924,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4241709277","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":[0.9978686,0.00005301538,0.0007348246,0.00016481364,0.00007958539,0.0006619588,0.00030978103,0.000010190676,0.000117250434],"genre_scores_gemma":[0.9993467,0.0000037264338,0.00038841824,0.000063124906,0.000024943536,0.0000318313,0.000056501107,0.000020785365,0.000064007756],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99690366,0.0004989725,0.0006033135,0.00046368985,0.0013222431,0.00020809865],"domain_scores_gemma":[0.99751383,0.0002285935,0.00094342645,0.0011427876,0.000108414606,0.0000629759],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009134923,0.0002979275,0.00047335203,0.0000046676987,0.000085531035,0.00002765056,0.00066043367,0.00022020636,0.0034638767],"category_scores_gemma":[0.000062498075,0.00013514179,0.0006254117,0.00047795672,0.00027327563,0.00009544682,0.00026825294,0.00017196327,0.0000039527717],"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":[0.000037667603,0.00013667198,0.46680573,0.000004474605,0.0003511374,5.6272203e-8,0.00029787616,0.39300072,0.13912408,0.0000025162608,0.00003785566,0.00020120191],"study_design_scores_gemma":[0.00032622315,0.00008527568,0.7172255,0.000099545236,0.00063517125,4.4879478e-8,0.00006719745,0.21982497,0.06145421,0.00014842788,6.8840853e-7,0.00013272287],"about_ca_topic_score_codex":0.009078071,"about_ca_topic_score_gemma":0.0015876726,"teacher_disagreement_score":0.2504198,"about_ca_system_score_codex":0.00028108901,"about_ca_system_score_gemma":0.00013738027,"threshold_uncertainty_score":0.99752057},"labels":[],"label_agreement":null},{"id":"W4242497309","doi":"10.5194/acp-2020-336","title":"Environmental sensitivities of shallow-cumulus dilution. Part I: Selected thermodynamic conditions","year":2020,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Compute Canada; Natural Sciences and Engineering Research Council of Canada; École de technologie supérieure; McGill University; U.S. Department of Energy","keywords":"Dilution; Cloud base; Atmospheric sciences; Environmental science; Buoyancy; Turbulence kinetic energy; Mixed layer; Turbulence; Meteorology; Cloud computing; Physics; Thermodynamics","score_opus":0.010430019808352618,"score_gpt":0.21041903953180058,"score_spread":0.19998901972344796,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4242497309","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":[0.9700271,0.000049898124,0.0031949372,0.0003853179,0.00020492547,0.00039849375,0.00038165468,0.00012967797,0.025228014],"genre_scores_gemma":[0.9960593,0.00009168643,0.001203328,0.00024124082,0.000069815396,0.000046801204,0.00032001606,0.000037969712,0.0019298355],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99817544,0.0000925236,0.00040664655,0.00059251627,0.00042578034,0.00030711284],"domain_scores_gemma":[0.99916434,0.00004758852,0.00023761929,0.00040337138,0.0000053459225,0.00014175722],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00007463379,0.00033803418,0.00039839547,0.0000020442906,0.00012612955,0.000022993998,0.00029470288,0.00023885776,0.017893406],"category_scores_gemma":[0.000015616084,0.0003162981,0.00018655887,0.00012760866,0.0005776315,0.000078745965,0.0011306709,0.0003941255,0.0004883103],"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":[0.00018831891,0.0019641297,0.24533273,0.00031325253,0.001110155,0.00018910073,0.006039449,0.061783113,0.6316694,0.003131859,0.04066075,0.007617752],"study_design_scores_gemma":[0.0006364426,0.00020341412,0.9051656,0.00008890233,0.0002435965,0.000024753197,0.0014824694,0.07899693,0.0047237817,0.0047458825,0.002372459,0.0013157725],"about_ca_topic_score_codex":0.0005517311,"about_ca_topic_score_gemma":0.00015158832,"teacher_disagreement_score":0.65983284,"about_ca_system_score_codex":0.00027057808,"about_ca_system_score_gemma":0.00003761148,"threshold_uncertainty_score":0.9999289},"labels":[],"label_agreement":null},{"id":"W4242620103","doi":"10.5194/amt-2020-470","title":"Systematic Comparison of Vectorial Spherical Radiative TransferModels in Limb Scattering Geometry","year":2021,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"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 Saskatchewan","funders":"Universität Bremen; Canadian Space Agency; Deutsche Forschungsgemeinschaft; Nuclear Safety and Security Commission; Academy of Finland; European Space Agency; National Aeronautics and Space Administration","keywords":"Radiative transfer; Refraction; Physics; Scattering; Computational physics; Scalar (mathematics); Wavelength; Geometry; Tangent; Monte Carlo method; Optics; Mathematics; Statistics","score_opus":0.018200010990926944,"score_gpt":0.2669355371991877,"score_spread":0.24873552620826078,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4242620103","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":[0.9417839,0.00034704502,0.052879453,0.000037479615,0.00066001934,0.0006000355,0.000004447976,0.000028815371,0.0036587988],"genre_scores_gemma":[0.99361503,0.000029836881,0.0060268785,0.000030384104,0.00007388262,0.00007202491,0.000009784278,0.000025522495,0.0001166615],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99752575,0.00017839728,0.00091453275,0.0005545592,0.000522781,0.00030400103],"domain_scores_gemma":[0.9990979,0.00012858237,0.00022225057,0.00044080758,0.0000099569115,0.000100489946],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00026947935,0.00030030336,0.0011668842,0.0000034378263,0.00003173014,0.000043059303,0.00042872515,0.00030167832,0.00334328],"category_scores_gemma":[0.000043954,0.00026651,0.00023134137,0.00032891627,0.00014748561,0.0000768216,0.0006238315,0.00049933564,0.000034824614],"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":[0.00013148262,0.0014386318,0.23712772,0.018509017,0.00029872224,0.000048398768,0.013992481,0.71150374,0.015476089,0.00012546823,0.00028590448,0.0010623529],"study_design_scores_gemma":[0.0031734225,0.00085600937,0.257026,0.01587389,0.0006269011,0.000017077604,0.017037988,0.67920977,0.02165966,0.000846398,0.000034003275,0.0036389278],"about_ca_topic_score_codex":0.001858273,"about_ca_topic_score_gemma":0.00033883227,"teacher_disagreement_score":0.05183112,"about_ca_system_score_codex":0.0003710858,"about_ca_system_score_gemma":0.000040906154,"threshold_uncertainty_score":0.9999787},"labels":[],"label_agreement":null},{"id":"W4243430801","doi":"10.5194/amt-2021-148-rc2","title":"Comment on amt-2021-148","year":2021,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"National Research Council Canada","funders":"Environment and Climate Change Canada; Université du Québec à Montréal","keywords":"Radar; Snow; Remote sensing; Snowflake; Particle (ecology); Meteorology; Environmental science; Range (aeronautics); Ice crystals; Atmospheric sciences; Geology; Geography; Materials science; Computer science; Telecommunications","score_opus":0.01949749239060603,"score_gpt":0.2692027377827111,"score_spread":0.24970524539210506,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4243430801","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000034661,0.0060755853,0.00020994782,0.30658886,0.0016015328,0.0003726642,0.000039751496,0.00003927186,0.68503773],"genre_scores_gemma":[0.00008525884,0.009840629,0.0014228115,0.18009642,0.0002329405,0.000058690297,0.00031320457,0.000036154244,0.8079139],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9979041,0.00007101377,0.0003171195,0.00061391824,0.00074314035,0.0003506662],"domain_scores_gemma":[0.99891126,0.00004825576,0.00012868323,0.0007427793,0.000009897022,0.00015912612],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00020555382,0.0003504301,0.0005083644,5.6892594e-7,0.000102559345,0.00003451894,0.00044453013,0.00018949261,0.34507737],"category_scores_gemma":[0.000031065407,0.00026886738,0.00023083106,0.00019896697,0.00009571938,0.000029021237,0.0005487196,0.00040279716,0.009017746],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000001125333,0.00010859992,0.000067376655,0.00011124551,0.000016576718,0.00002260681,0.000008938078,0.00001368819,0.0000023396708,0.00008771593,0.97347844,0.026081344],"study_design_scores_gemma":[0.000092653085,0.00010274985,0.00012941525,0.0007136148,0.00004972856,0.0000031101993,0.000017949498,0.000018890883,0.000019389063,0.000035738503,0.99847937,0.000337372],"about_ca_topic_score_codex":0.00084991154,"about_ca_topic_score_gemma":0.00020970893,"teacher_disagreement_score":0.3360596,"about_ca_system_score_codex":0.00029690797,"about_ca_system_score_gemma":0.000027456937,"threshold_uncertainty_score":0.99997634},"labels":[],"label_agreement":null},{"id":"W4243543239","doi":"10.5194/amt-2021-148-ac2","title":"Reply on RC1","year":2021,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"National Research Council Canada","funders":"Environment and Climate Change Canada; Université du Québec à Montréal","keywords":"Radar; Snow; Snowflake; Remote sensing; Particle (ecology); Meteorology; Environmental science; Ice crystals; Range (aeronautics); Atmospheric sciences; Geology; Geography; Materials science; Computer science; Telecommunications","score_opus":0.019045943199940407,"score_gpt":0.26867678518543386,"score_spread":0.24963084198549346,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4243543239","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00006607583,0.0066246907,0.00008358195,0.06611104,0.0012463267,0.00021778535,0.00001632845,0.00005834043,0.92557585],"genre_scores_gemma":[0.000047809244,0.005730618,0.001113133,0.091443926,0.00017908085,0.000025415846,0.00012150557,0.000026417789,0.9013121],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9983573,0.00003678846,0.00023805822,0.0005689052,0.00055049354,0.00024848705],"domain_scores_gemma":[0.99905044,0.000029057855,0.00010139777,0.00070614857,0.0000074974614,0.00010547344],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00015442375,0.00024336661,0.0003678549,2.982753e-7,0.00006312454,0.00002135781,0.00032187183,0.00012935654,0.26420373],"category_scores_gemma":[0.00005882589,0.00018247814,0.00017858099,0.00016856668,0.00007215849,0.0000255684,0.00030729384,0.000298005,0.008318856],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[6.82403e-7,0.000029503397,0.00006274954,0.00009036476,0.0000075665826,0.000023549655,0.000004346158,0.000008694163,0.0000031192837,0.000026622176,0.9836856,0.016057199],"study_design_scores_gemma":[0.000041501626,0.000041872965,0.0002871282,0.000516973,0.000029730001,0.0000059928143,0.0000062887857,0.0000078315,0.000016019232,0.000027443215,0.998779,0.00024019465],"about_ca_topic_score_codex":0.00091079273,"about_ca_topic_score_gemma":0.00012870388,"teacher_disagreement_score":0.2558849,"about_ca_system_score_codex":0.00014605986,"about_ca_system_score_gemma":0.000025189,"threshold_uncertainty_score":0.9924533},"labels":[],"label_agreement":null},{"id":"W4243569682","doi":"10.4095/219772","title":"Quantifying Uncertainties in Determining SW Cloud Radiative Forcing and Cloud Absorption due to Variability in Atmospheric Conditions","year":2001,"lang":"en","type":"report","venue":"","topic":"Atmospheric aerosols and clouds","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":"Natural Resources Canada","funders":"","keywords":"Radiative forcing; Radiative transfer; Atmospheric sciences; Environmental science; Forcing (mathematics); Cloud forcing; Cloud computing; Absorption (acoustics); Meteorology; Climatology; Physics; Geology; Aerosol; Computer science; Optics","score_opus":0.032957211669551394,"score_gpt":0.2971049744488246,"score_spread":0.2641477627792732,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4243569682","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":[0.94677114,0.00009789407,0.0108379945,0.000097447264,0.0009941764,0.0008560007,0.0000150252945,0.00006637161,0.04026395],"genre_scores_gemma":[0.99034464,0.0004164537,0.006106641,0.00016478715,0.0002695696,0.00015436453,0.000033100478,0.000051343086,0.0024591105],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9966472,0.0002328141,0.00088452594,0.0009853741,0.00059836893,0.0006517203],"domain_scores_gemma":[0.9986709,0.00039798743,0.0003147551,0.00039643346,0.000028510602,0.00019141972],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0019411881,0.00046447694,0.00077218044,0.0000060809157,0.00018618701,0.00008052208,0.00024248043,0.0003987366,0.0023613693],"category_scores_gemma":[0.000498656,0.00044990453,0.0001020941,0.00066826714,0.00023288424,0.0002598825,0.0003687342,0.00053664995,0.00006412082],"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":[0.000035422054,0.00013215495,0.9514929,0.00011782172,0.000025732668,0.00015888659,0.003265993,0.022936128,0.00028317946,0.00008747337,0.0021144573,0.019349871],"study_design_scores_gemma":[0.0007539232,0.00019627718,0.95754784,0.0005394158,0.000058957256,0.00014079784,0.003995357,0.024250813,0.00006574444,0.0011695535,0.009959317,0.0013219825],"about_ca_topic_score_codex":0.020557862,"about_ca_topic_score_gemma":0.02017769,"teacher_disagreement_score":0.04357349,"about_ca_system_score_codex":0.001994287,"about_ca_system_score_gemma":0.0001795407,"threshold_uncertainty_score":0.99979526},"labels":[],"label_agreement":null},{"id":"W4243841059","doi":"10.5194/acpd-12-17723-2012","title":"Numerical evidence for cloud droplet nucleation at the cloud-environment interface","year":2012,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Chinese Academy of Sciences","keywords":"Cloud computing; Liquid water content; Nucleation; Cloud condensation nuclei; Cloud base; Meteorology; Cloud physics; Spurious relationship; Supercooling; Supersaturation; Mechanics; Condensation; Cloud cover; Atmospheric sciences; Aerosol; Environmental science; Geology; Physics; Computer science; Thermodynamics","score_opus":0.03907488263985879,"score_gpt":0.28508448636143824,"score_spread":0.24600960372157946,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4243841059","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":[0.55888844,0.0016617854,0.41535115,0.007441437,0.003183161,0.0029474893,0.000032428412,0.00018258479,0.0103115095],"genre_scores_gemma":[0.9725315,0.0003214358,0.0060890806,0.0007412136,0.0006602559,0.00033767568,0.00002099729,0.000063666695,0.01923416],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9974984,0.000117220625,0.00044365242,0.00079780445,0.0005682571,0.00057468924],"domain_scores_gemma":[0.99822223,0.0002581489,0.000303764,0.0010184573,0.0000063220127,0.00019109527],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0005531581,0.00041989158,0.00032858987,9.4104934e-7,0.0003547558,0.00007589596,0.00085729104,0.00029451647,0.028049504],"category_scores_gemma":[0.00006158881,0.00027795142,0.0002668846,0.000065461485,0.00037405585,0.00013852472,0.0030013495,0.00042261853,0.0041397708],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00085395813,0.00092968805,0.11516943,0.00028513576,0.00029978316,0.0000048820057,0.0062322533,0.2549047,0.007671924,0.0009847265,0.54666466,0.06599892],"study_design_scores_gemma":[0.000953557,0.00046840007,0.077328406,0.00026972813,0.00051018444,0.000032468888,0.00077728205,0.05640556,0.0057466826,0.00278801,0.8521651,0.0025546188],"about_ca_topic_score_codex":0.0006195187,"about_ca_topic_score_gemma":0.000035234552,"teacher_disagreement_score":0.41364306,"about_ca_system_score_codex":0.0011162073,"about_ca_system_score_gemma":0.000015156587,"threshold_uncertainty_score":0.9999673},"labels":[],"label_agreement":null},{"id":"W4244149587","doi":"10.5194/amt-2017-328","title":"Three-channel single-wavelength lidar depolarization calibration","year":2017,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University; Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency; Indigenous and Northern Affairs Canada; Environment and Climate Change Canada; Strong; Ontario Innovation Trust","keywords":"Lidar; Depolarization; Polarization (electrochemistry); Rayleigh scattering; Optics; Depolarization ratio; Perpendicular; Wavelength; Physics; Materials science; Chemistry; Mathematics; Geometry","score_opus":0.02638241729365835,"score_gpt":0.23061046395507567,"score_spread":0.20422804666141733,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4244149587","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.20159402,0.000060448045,0.71915114,0.0007035109,0.00090837944,0.0005394559,0.000014541434,0.00021138272,0.07681713],"genre_scores_gemma":[0.98681784,0.00003000173,0.009959615,0.0002286165,0.00021542604,0.000028533177,0.000087818975,0.00003870993,0.002593469],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99844974,0.0000238465,0.0002718139,0.0005932992,0.00038496495,0.00027631622],"domain_scores_gemma":[0.9987617,0.000014345842,0.00031418464,0.0007807882,0.000010164983,0.00011879207],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00013275338,0.00028110694,0.00022777992,0.0000013962101,0.00032741946,0.00025279104,0.0004997606,0.00040179028,0.002479194],"category_scores_gemma":[0.000037215457,0.00024981424,0.0001023669,0.00004439216,0.00015806913,0.00024252512,0.0013045926,0.0003241279,0.00028875444],"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":[0.0001474839,0.0017315805,0.47378227,0.00033456873,0.0003171625,0.00011034695,0.0034857846,0.07080772,0.023484299,0.004552453,0.04603699,0.37520936],"study_design_scores_gemma":[0.0007667743,0.00027766827,0.19816461,0.0001819493,0.00017175233,0.000018325381,0.00015494719,0.71158177,0.008137694,0.07153332,0.0065777055,0.0024334618],"about_ca_topic_score_codex":0.0029341192,"about_ca_topic_score_gemma":0.0016613307,"teacher_disagreement_score":0.7852238,"about_ca_system_score_codex":0.00018256308,"about_ca_system_score_gemma":0.00003035352,"threshold_uncertainty_score":0.9999954},"labels":[],"label_agreement":null},{"id":"W4244177141","doi":"10.5194/acp-2021-338","title":"Supercooled liquid water and secondary ice production in Kelvin–Helmholtz instability as revealed by radar Doppler spectra observations","year":2021,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"Environment and Climate Change Canada","funders":"China Scholarship Council; Horizon 2020; Academy of Finland","keywords":"Supercooling; Ice crystals; Drizzle; Ice nucleus; Instability; Precipitation; Atmospheric sciences; Materials science; Mechanics; Nucleation; Physics; Meteorology; Thermodynamics","score_opus":0.012773704501466053,"score_gpt":0.21728391166251826,"score_spread":0.2045102071610522,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4244177141","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":[0.98684394,0.00021908579,0.00014605254,0.0037752562,0.00035789667,0.00082737004,0.000019248506,0.0000779925,0.007733183],"genre_scores_gemma":[0.9845459,0.000344705,0.0071148165,0.0006832582,0.00008422783,0.00012497041,0.0003326865,0.000036112557,0.0067333346],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99717766,0.00017786513,0.00056454947,0.0012778697,0.00036605189,0.0004360178],"domain_scores_gemma":[0.99894524,0.00002788848,0.00007782424,0.00077506027,0.000023898965,0.00015012053],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00055497774,0.000374844,0.0004345762,0.0000034149868,0.0001574704,0.00010591899,0.00028136143,0.0003320579,0.015297901],"category_scores_gemma":[0.000073528034,0.00030300187,0.00009114723,0.00019644998,0.00028717326,0.0004083134,0.0012335778,0.00082647544,0.00007624977],"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":[0.00038780554,0.001578908,0.37168592,0.00059298764,0.00013180287,0.00006942838,0.011555162,0.0013519633,0.58284,0.00008882096,0.02531002,0.004407169],"study_design_scores_gemma":[0.0014120737,0.000336402,0.87018317,0.00017854213,0.00011290325,0.0000883374,0.004029296,0.0003895643,0.09686719,0.0018247364,0.022454185,0.0021236262],"about_ca_topic_score_codex":0.006358229,"about_ca_topic_score_gemma":0.0034188123,"teacher_disagreement_score":0.49849722,"about_ca_system_score_codex":0.00042909422,"about_ca_system_score_gemma":0.00008539709,"threshold_uncertainty_score":0.9999422},"labels":[],"label_agreement":null},{"id":"W4244184576","doi":"10.5194/amt-2016-371","title":"Thin ice clouds in the Arctic: Cloud optical depth and particle size retrieved from ground-based thermal infrared radiometry","year":2016,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université de Sherbrooke","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency; Fonds Québécois de la Recherche sur la Nature et les Technologies; Washington State University; U.S. Department of Energy","keywords":"Remote sensing; Ice cloud; Radiance; Arctic; Environmental science; Infrared; Cloud top; Optical depth; Lidar; Snow; Meteorology; Radiative transfer; Optics; Geology; Physics; Satellite; Aerosol","score_opus":0.014253611995375826,"score_gpt":0.23398660306107474,"score_spread":0.2197329910656989,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4244184576","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":[0.9755849,0.00016430685,0.0034757045,0.002056399,0.00037099747,0.00048812773,0.000014359009,0.000070484944,0.017774707],"genre_scores_gemma":[0.9901617,0.00003293407,0.006389776,0.0022881438,0.00025032245,0.000054648226,0.000008654573,0.000035229074,0.000778583],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9971629,0.00032006434,0.0004811795,0.0008125506,0.0006688303,0.0005545044],"domain_scores_gemma":[0.9974825,0.0012393949,0.00015933863,0.0009133166,0.000010084095,0.00019541357],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00085029204,0.00039379668,0.00040631456,0.0000012767148,0.00013576333,0.00018136018,0.0008459194,0.00041154432,0.0035132782],"category_scores_gemma":[0.00032335983,0.00023089521,0.000128693,0.0003265681,0.00052845094,0.00013014245,0.00095967023,0.000719653,0.00016476659],"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":[0.0004910793,0.0005092728,0.97311723,0.00004023488,0.00008771421,0.00009902485,0.002615897,0.0011064063,0.0075411783,0.0010793064,0.0018276568,0.0114849815],"study_design_scores_gemma":[0.0012038476,0.00009757233,0.98233336,0.000059582457,0.000051721338,0.0000030754827,0.0004941203,0.0056959805,0.0012148994,0.007668315,0.0006873801,0.0004901222],"about_ca_topic_score_codex":0.0028017904,"about_ca_topic_score_gemma":0.00040725007,"teacher_disagreement_score":0.016996123,"about_ca_system_score_codex":0.00026198264,"about_ca_system_score_gemma":0.00005100852,"threshold_uncertainty_score":0.99739766},"labels":[],"label_agreement":null},{"id":"W4244284429","doi":"10.5194/amt-2018-414","title":"Detecting layer height of smoke aerosols over vegetated land andwater surfaces via oxygen absorption bands: Hourly results fromEPIC/DSCOVR satellite in deep space","year":2018,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","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":"Office of Naval Research; Multidisciplinary University Research Initiative; National Aeronautics and Space Administration","keywords":"Aerosol; Environmental science; Remote sensing; AERONET; Satellite; Atmospheric sciences; Radiative transfer; Lidar; Meteorology; Optics; Geology; Physics","score_opus":0.015356576449997363,"score_gpt":0.23815811093982006,"score_spread":0.2228015344898227,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4244284429","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":[0.9908548,0.0003659212,0.0016458958,0.000093865645,0.00035552593,0.0005821814,0.000035418554,0.00008433878,0.005982081],"genre_scores_gemma":[0.9938124,0.00038073107,0.0042986413,0.00008421808,0.00010053728,0.000025651318,0.000073724215,0.000058464568,0.0011656309],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9966119,0.00017415245,0.0009277254,0.0010724707,0.0005931507,0.0006205991],"domain_scores_gemma":[0.99839365,0.00009947091,0.0005627617,0.00075058703,0.000034511137,0.00015903113],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00075330114,0.00053755724,0.0006816815,0.000010741325,0.00009872493,0.00009728603,0.00049617526,0.0005924104,0.002189402],"category_scores_gemma":[0.000043419164,0.00042820597,0.00016950928,0.00029296134,0.00026195918,0.00023795564,0.00093477237,0.0005340147,0.00023892678],"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":[0.0004557037,0.0001609237,0.9422098,0.00010379326,0.00009639296,0.000020896063,0.0025195517,0.015519575,0.03620219,0.0000014547012,0.00024958074,0.002460183],"study_design_scores_gemma":[0.0014120004,0.00017342846,0.9555363,0.0002182468,0.000048176138,0.0000043170917,0.000119115175,0.010548234,0.030069161,0.00044571608,0.00068803807,0.000737231],"about_ca_topic_score_codex":0.01661704,"about_ca_topic_score_gemma":0.011119511,"teacher_disagreement_score":0.01332658,"about_ca_system_score_codex":0.00023266602,"about_ca_system_score_gemma":0.000021599952,"threshold_uncertainty_score":0.99981695},"labels":[],"label_agreement":null},{"id":"W4244336188","doi":"10.5194/acp-2016-22","title":"Comparison of retrieved Noctilucent cloud particle properties from Odin tomography scans and model simulations","year":2016,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"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":"Canadian Space Agency","keywords":"Satellite; Ice cloud; Effective radius; Remote sensing; Cloud computing; Cloud top; Particle (ecology); Cloud physics; Environmental science; Atmospheric sciences; Meteorology; Computational physics; Physics; Geology; Computer science; Astrophysics; Astronomy","score_opus":0.0419764362334392,"score_gpt":0.2728177747905275,"score_spread":0.2308413385570883,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4244336188","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":[0.9642162,0.0002064117,0.032453045,0.00027491967,0.000103490594,0.00029320526,0.00007126114,0.00004464862,0.0023368178],"genre_scores_gemma":[0.9953124,0.000029354554,0.0038816603,0.000053390733,0.000032011707,0.0000131617235,0.000007142366,0.000015440026,0.0006554641],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99869,0.000033693126,0.00037126723,0.0004134816,0.00028676708,0.00020476493],"domain_scores_gemma":[0.9992834,0.000034669545,0.0001676539,0.0003901513,0.000014087577,0.000110053064],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00006793786,0.00019252667,0.00032074298,0.0000010013292,0.000088728455,0.000029009723,0.00020813402,0.00015124698,0.0010427576],"category_scores_gemma":[0.000015510452,0.00013126271,0.000079188016,0.000086385466,0.00033871835,0.00007179029,0.0007308117,0.00014632125,0.000017954839],"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":[0.000061403436,0.00019542004,0.77499145,0.000016943208,0.00004547327,2.461843e-7,0.0016687667,0.19513173,0.02511318,0.00017042563,0.000863907,0.001741053],"study_design_scores_gemma":[0.00031648576,0.000046715526,0.06397744,0.00007226567,0.000057345344,9.2456695e-8,0.00026715742,0.9024145,0.028112521,0.004293205,0.00013643902,0.000305855],"about_ca_topic_score_codex":0.0011850375,"about_ca_topic_score_gemma":0.00028523526,"teacher_disagreement_score":0.71101403,"about_ca_system_score_codex":0.00005940475,"about_ca_system_score_gemma":0.000017200202,"threshold_uncertainty_score":0.9998704},"labels":[],"label_agreement":null},{"id":"W4245029582","doi":"10.5194/amt-2017-391","title":"Airborne Lidar Measurements of Aerosol and Ozone Above the Canadian Oil Sands Region","year":2017,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada; York University","funders":"Natural Sciences and Engineering Research Council of Canada; FedDev Ontario; Environment and Climate Change Canada; University of Wyoming","keywords":"Lidar; Aerosol; Environmental science; Planetary boundary layer; Ozone; Atmospheric sciences; Mixing ratio; Plume; Boundary layer; Backscatter (email); Ozone Monitoring Instrument; Oil sands; Remote sensing; Meteorology; Materials science; Geology; Geography","score_opus":0.03630448860472203,"score_gpt":0.24186984330709344,"score_spread":0.20556535470237142,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4245029582","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":[0.5758727,0.00045214884,0.00018286618,0.0031237805,0.000427494,0.0002943585,0.00001482653,0.000027483984,0.4196043],"genre_scores_gemma":[0.98845255,0.00021088767,0.000706197,0.00031927152,0.00006069458,0.000024414068,0.0000056374915,0.00002010009,0.010200256],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99847394,0.000045251298,0.00024727473,0.00044641778,0.00046306985,0.00032405497],"domain_scores_gemma":[0.99849474,0.000013722911,0.00027839225,0.0009544095,0.000020267593,0.00023848643],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003423831,0.0002471113,0.00027826143,0.0000016534899,0.00044968392,0.00009954509,0.0006814571,0.00026032032,0.0007627987],"category_scores_gemma":[0.000040418246,0.00016542846,0.00008110729,0.00004210823,0.0005659998,0.00006379386,0.00076167873,0.00032904648,0.00005210913],"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":[0.0000799785,0.00018726573,0.7856725,0.00021207528,0.0003077744,0.000047298992,0.0031121061,0.0011577392,0.0017359512,0.00024797197,0.03738454,0.1698548],"study_design_scores_gemma":[0.0015738431,0.00025121044,0.9662471,0.00047112047,0.00031831968,0.000037799953,0.00042924393,0.001024273,0.005648808,0.0015310872,0.020723315,0.0017438689],"about_ca_topic_score_codex":0.5208357,"about_ca_topic_score_gemma":0.5691442,"teacher_disagreement_score":0.4125798,"about_ca_system_score_codex":0.00026430486,"about_ca_system_score_gemma":0.00012611167,"threshold_uncertainty_score":0.8352111},"labels":[],"label_agreement":null},{"id":"W4246565420","doi":"10.5194/amt-2020-149","title":"Using Two-Stream Theory to Capture Fluctuations of Satellite-Perceived TOA SW Radiances Reflected from Clouds over Ocean","year":2020,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Freie Universität Berlin; European Space Agency; Langley Research Center; National Aeronautics and Space Administration","keywords":"Cloud albedo; Cloud fraction; Radiance; Effective radius; Cloud top; Remote sensing; Radiative transfer; Environmental science; Albedo (alchemy); Cloud computing; Cloud height; Atmospheric radiative transfer codes; Shortwave; Meteorology; Satellite; Cloud cover; Physics; Geology; Computer science; Optics","score_opus":0.030446899037392144,"score_gpt":0.2911706707088119,"score_spread":0.2607237716714198,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4246565420","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":[0.95568806,0.00028930916,0.01417633,0.00034406644,0.00036518963,0.00054791145,0.00018010041,0.0001165716,0.028292472],"genre_scores_gemma":[0.93276024,0.00009796176,0.064353235,0.0010570072,0.00019005794,0.00000875374,0.00012217552,0.000049401206,0.0013611909],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99755937,0.00015938595,0.00051518786,0.0009250095,0.0004803437,0.00036070365],"domain_scores_gemma":[0.9985894,0.00011767612,0.00025000426,0.00071408664,0.000023284882,0.00030556787],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00013271962,0.00043193338,0.00053847604,0.000003622474,0.00012369231,0.00006329593,0.00066356367,0.0002981987,0.014523902],"category_scores_gemma":[0.00007644836,0.00037414345,0.00020203949,0.0003289557,0.00026930292,0.00009416633,0.00087636657,0.00045596217,0.00019166764],"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":[0.0006478547,0.00059441786,0.15354088,0.0001570228,0.0008875378,0.0000778792,0.040371682,0.23118193,0.5177823,0.0035558105,0.008331765,0.042870965],"study_design_scores_gemma":[0.0015861016,0.00025100363,0.87992084,0.0004651238,0.00072868663,0.000006445929,0.0057439366,0.031127939,0.009088286,0.057477113,0.0105546955,0.0030498558],"about_ca_topic_score_codex":0.009796697,"about_ca_topic_score_gemma":0.0007648509,"teacher_disagreement_score":0.72637993,"about_ca_system_score_codex":0.00029321178,"about_ca_system_score_gemma":0.000078074016,"threshold_uncertainty_score":0.9998711},"labels":[],"label_agreement":null},{"id":"W4246577097","doi":"10.2172/1467425","title":"Final Technical Report","year":2018,"lang":"en","type":"report","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Aerosol; Environmental science; Shortwave; Atmospheric sciences; Troposphere; Shortwave radiation; Climatology; Outflow; Meteorology; Geography; Geology; Radiative transfer; Radiation","score_opus":0.036529793828932906,"score_gpt":0.2959707213698709,"score_spread":0.259440927540938,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4246577097","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.005431763,0.000037794736,0.0017657162,0.00011569058,0.00071991974,0.00016004009,0.000002835537,0.00014926109,0.99161696],"genre_scores_gemma":[0.048085183,0.00017335013,0.015596456,0.00022407042,0.001027413,0.00003983286,0.000047806792,0.000057994937,0.9347479],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9974238,0.000012303466,0.0004368515,0.0006145294,0.0011905953,0.00032191334],"domain_scores_gemma":[0.9988672,0.000014578264,0.00024392028,0.0007157497,0.000026022239,0.0001324944],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0005591376,0.00024636154,0.0003021026,6.9169556e-7,0.00009546786,0.00002381964,0.00034825405,0.00042605287,0.09997523],"category_scores_gemma":[0.00014578359,0.00018619011,0.00016237554,0.0001411472,0.00038780778,0.000047074052,0.00053636817,0.00029665293,0.0044786283],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000023051898,0.000035015666,0.017686704,0.000005498226,0.000007277536,0.00037737816,0.0000032691114,0.0000018567573,0.00006930672,0.0000062529944,0.9774203,0.004384894],"study_design_scores_gemma":[0.000040253828,0.0000638963,0.041188832,0.00001475377,0.000026416452,0.0018648324,0.0000043648597,0.000007749578,0.00003559242,0.00012221407,0.9563589,0.00027219846],"about_ca_topic_score_codex":0.0015719301,"about_ca_topic_score_gemma":0.0003808574,"teacher_disagreement_score":0.095496595,"about_ca_system_score_codex":0.0005100002,"about_ca_system_score_gemma":0.00018747865,"threshold_uncertainty_score":0.9962965},"labels":[],"label_agreement":null},{"id":"W4246614550","doi":"10.5194/acp-2018-254","title":"Surface roughness during depositional growth and sublimation of ice crystals","year":2018,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"University of British Columbia","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Ice crystals; Sublimation (psychology); Supersaturation; Surface roughness; Cirrus; Materials science; Surface finish; Clear ice; Crystal growth; Relative humidity; Sea ice growth processes; Optics; Atmospheric sciences; Meteorology; Composite material; Thermodynamics; Sea ice; Chemistry; Crystallography; Geology; Cryosphere; Sea ice thickness; Physics","score_opus":0.009195422111789479,"score_gpt":0.22117637037689525,"score_spread":0.21198094826510577,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4246614550","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":[0.9792483,0.000042565265,0.007933442,0.00012838864,0.00008769943,0.00016109613,0.000012232707,0.000030486985,0.012355799],"genre_scores_gemma":[0.98525035,0.000055154567,0.014205495,0.000027988282,0.000047189103,0.0000061504693,0.00001675338,0.0000127392605,0.000378191],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989487,0.000031294032,0.00023664544,0.00033908233,0.0002937251,0.00015055944],"domain_scores_gemma":[0.9995375,0.000030354511,0.00016875277,0.0001866692,0.000015629996,0.00006103909],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00010578273,0.00015327733,0.00018098518,9.53978e-7,0.000087243694,0.00003504837,0.00016393917,0.00014333193,0.0019056803],"category_scores_gemma":[0.000015346797,0.00013811006,0.00004371378,0.00007431116,0.00021576237,0.00013572001,0.00086464937,0.00011117966,0.000027103662],"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":[0.000079946236,0.00014878203,0.84584534,0.00065856945,0.00007137728,0.000006819733,0.00097253406,0.014182197,0.13629048,0.00084109616,0.0006116018,0.00029128004],"study_design_scores_gemma":[0.00029390145,0.00004400436,0.94846636,0.00008630802,0.00003593417,0.000009341357,0.00012617387,0.004376468,0.043339495,0.0028132363,0.000022955208,0.00038580262],"about_ca_topic_score_codex":0.0009294623,"about_ca_topic_score_gemma":0.00003467235,"teacher_disagreement_score":0.102621056,"about_ca_system_score_codex":0.000057867997,"about_ca_system_score_gemma":0.000010999973,"threshold_uncertainty_score":0.9990067},"labels":[],"label_agreement":null},{"id":"W4246863130","doi":"10.5194/amt-2019-411","title":"The 2018 fire season in North America as seen by TROPOMI: aerosol layer height validation and evaluation of model-derived plume heights","year":2019,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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; Environment and Climate Change Canada","funders":"Netherlands Space Office; European Space Agency; Langley Research Center; National Aeronautics and Space Administration","keywords":"Plume; Aerosol; Environmental science; Altitude (triangle); Meteorology; Atmospheric sciences; Air quality index; Satellite; Remote sensing; Panache; Geography; Geology; Mathematics","score_opus":0.02039029660543222,"score_gpt":0.2565901535607454,"score_spread":0.23619985695531315,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4246863130","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":[0.9896569,0.00041624153,0.002489994,0.00039252383,0.000109065324,0.0011328192,0.000029998175,0.000022593771,0.0057498426],"genre_scores_gemma":[0.9951873,0.0010318222,0.0010678835,0.00010389414,0.000021952279,0.000109367626,0.00013602615,0.000026384161,0.002315364],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9975411,0.00021920585,0.00041648213,0.00062523875,0.00091078127,0.0002871395],"domain_scores_gemma":[0.9988734,0.000060285365,0.0003631798,0.000577731,0.00003853933,0.00008684914],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00039661583,0.00030091254,0.00033772644,0.0000017839811,0.00013368485,0.000048523332,0.00036415376,0.00021500506,0.0009896425],"category_scores_gemma":[0.000026984133,0.00020656871,0.000079280755,0.00013769328,0.00025411375,0.00016371385,0.000610206,0.00028199493,0.0001323312],"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":[0.00015865378,0.00027447217,0.07841196,0.000056009845,0.00010241797,8.264764e-7,0.0027786375,0.8573284,0.007480355,0.000022461574,0.01620734,0.037178457],"study_design_scores_gemma":[0.0006981626,0.00009659628,0.021704888,0.000029257646,0.00008610897,7.7040534e-7,0.00026376633,0.9725665,0.0029188087,0.0005527114,0.0006875153,0.00039493816],"about_ca_topic_score_codex":0.0028182182,"about_ca_topic_score_gemma":0.00093450415,"teacher_disagreement_score":0.11523806,"about_ca_system_score_codex":0.00032601613,"about_ca_system_score_gemma":0.00008524222,"threshold_uncertainty_score":0.9999236},"labels":[],"label_agreement":null},{"id":"W4247874459","doi":"10.1002/essoar.10503122.1","title":"Gravity Wave Breaking and Vortex Ring Formation Observed by PMC Turbo","year":2020,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","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":"National Aeronautics and Space Administration","keywords":"Physics; Instability; Wavelength; Vortex; Atmospheric sciences; Computational physics; Meteorology; Optics; Mechanics","score_opus":0.03034330807621594,"score_gpt":0.22063700389645902,"score_spread":0.19029369582024308,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4247874459","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":[0.9653537,0.00009829025,0.019585026,0.0005371143,0.0001398763,0.00027782613,0.000010918709,0.00010669343,0.013890539],"genre_scores_gemma":[0.9899998,0.000075418946,0.00882363,0.00029429077,0.000042055985,0.000017141208,0.00003275546,0.000017828972,0.00069708994],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99875844,0.000032288317,0.000254364,0.0004603058,0.00026758626,0.0002270492],"domain_scores_gemma":[0.9994386,0.00001827232,0.00015941514,0.00024059275,0.0000043468194,0.00013881632],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00012554579,0.00022986159,0.00022863617,5.5231675e-7,0.00012140216,0.00010070124,0.00018192829,0.00017603747,0.00093218964],"category_scores_gemma":[0.000015264068,0.00020304356,0.00006807511,0.00006590891,0.0000814618,0.00017887224,0.0014203867,0.00033586903,0.000077197146],"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":[0.000104655825,0.00029392063,0.49426246,0.0008792707,0.00019862493,0.00007669808,0.010041511,0.0040723826,0.15319842,0.00063829066,0.025280919,0.31095284],"study_design_scores_gemma":[0.0007336546,0.00009745861,0.86021775,0.000163131,0.000120823264,0.000026360573,0.0008091003,0.10420539,0.014967099,0.011214012,0.005912118,0.0015331238],"about_ca_topic_score_codex":0.001466841,"about_ca_topic_score_gemma":0.00010862556,"teacher_disagreement_score":0.36595526,"about_ca_system_score_codex":0.00013319188,"about_ca_system_score_gemma":0.000006257761,"threshold_uncertainty_score":0.9999811},"labels":[],"label_agreement":null},{"id":"W4248119590","doi":"10.5194/acpd-8-5813-2008","title":"Parameterization of sea-salt optical properties and physics of the associated radiative forcing","year":2008,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"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; Environment and Climate Change Canada","funders":"","keywords":"Longwave; AERONET; Radiative forcing; Forcing (mathematics); Sea salt; Shortwave; Cloud forcing; Atmospheric sciences; Environmental science; Radiative transfer; Wavelength; Albedo (alchemy); Effective radius; Climatology; Aerosol; Meteorology; Physics; Geology; Optics","score_opus":0.025030371102045833,"score_gpt":0.20962008275815117,"score_spread":0.18458971165610533,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4248119590","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":[0.9898017,0.000026273321,0.0053962036,0.00004909501,0.00005024001,0.000256013,0.000006797529,0.000009999436,0.0044036987],"genre_scores_gemma":[0.9972766,0.00010441698,0.0022192108,0.000032066917,0.000009763461,0.000009162213,0.0000027596031,0.000008929635,0.0003370611],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992484,0.000045839788,0.00019890736,0.00017426774,0.00023062792,0.00010194204],"domain_scores_gemma":[0.99954134,0.000026653892,0.00022665635,0.0001678142,0.000013172521,0.000024348952],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000069075955,0.00011046461,0.00021191646,2.779127e-7,0.00005085265,0.0000067858014,0.00012925282,0.00010792841,0.00004599205],"category_scores_gemma":[0.00006277953,0.000066734836,0.000061501574,0.00008051373,0.00040997766,0.000040038758,0.0005929136,0.00013183194,0.0000012959205],"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":[0.00005025532,0.00041743505,0.7456553,0.00021618493,0.00021202165,0.0000012977116,0.007341322,0.19275987,0.032348122,0.0007591918,0.00041281965,0.019826164],"study_design_scores_gemma":[0.00037672216,0.0001358214,0.63417846,0.00021406503,0.00009343067,0.0000017603339,0.0003164366,0.26584893,0.09585952,0.0025915022,0.000021566666,0.00036178457],"about_ca_topic_score_codex":0.000614305,"about_ca_topic_score_gemma":0.000024101035,"teacher_disagreement_score":0.11147686,"about_ca_system_score_codex":0.000059449212,"about_ca_system_score_gemma":0.000021612519,"threshold_uncertainty_score":0.27213678},"labels":[],"label_agreement":null},{"id":"W4248131933","doi":"10.5194/acpd-9-7873-2009","title":"Aerosol size-dependent below-cloud scavenging by rain and snow in the ECHAM5-HAM","year":2009,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Killam Trusts","keywords":"Scavenging; Aerosol; Atmospheric sciences; Snow; Troposphere; Environmental science; Cloud cover; Ice nucleus; Liquid water content; Cloud albedo; Cloud condensation nuclei; Deposition (geology); Sea salt aerosol; Meteorology; Climatology; Cloud computing; Sea salt; Nucleation; Chemistry; Geology; Geography","score_opus":0.006341777091275218,"score_gpt":0.21516847179401516,"score_spread":0.20882669470273993,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4248131933","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":[0.9397729,0.0005351773,0.004536053,0.0032136627,0.0003101089,0.0010024189,0.000016306107,0.0001050863,0.0505083],"genre_scores_gemma":[0.98990655,0.00038020805,0.0027373368,0.0021129164,0.00010400043,0.00006178148,0.000010780962,0.000029675855,0.004656729],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9975623,0.00015708311,0.00038756386,0.00078908156,0.0005804824,0.0005234887],"domain_scores_gemma":[0.9989455,0.00017218478,0.00014060402,0.0006155464,0.000004014421,0.00012218318],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00084939227,0.0004088731,0.0003544506,0.0000017086348,0.00017602202,0.00015479022,0.00073266926,0.000315426,0.002146798],"category_scores_gemma":[0.00005846697,0.0002883558,0.000099303084,0.00014983905,0.00018688019,0.00007946842,0.0010798639,0.00079225603,0.00012773571],"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":[0.00021382104,0.0027766428,0.18199885,0.00029752837,0.00023519355,0.00056182244,0.028159596,0.04335563,0.022402411,0.0017303759,0.35961744,0.35865068],"study_design_scores_gemma":[0.018425709,0.0026391542,0.57970697,0.0029840507,0.0008859055,0.00074946316,0.039980996,0.10010728,0.027887532,0.105258845,0.09811575,0.023258325],"about_ca_topic_score_codex":0.0015455163,"about_ca_topic_score_gemma":0.0005576221,"teacher_disagreement_score":0.39770815,"about_ca_system_score_codex":0.00020784691,"about_ca_system_score_gemma":0.000019025441,"threshold_uncertainty_score":0.99995685},"labels":[],"label_agreement":null},{"id":"W4248462857","doi":"10.5194/amt-2020-150","title":"A technical description of the Balloon Lidar Experiment BOLIDE","year":2020,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":5,"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":"National Aeronautics and Space Administration","keywords":"Lidar; Payload (computing); Remote sensing; Backscatter (email); Balloon; Environmental science; Altitude (triangle); High resolution; Geology; Meteorology; Physics; Engineering; Computer science; Telecommunications","score_opus":0.022278258141976502,"score_gpt":0.2378647739018816,"score_spread":0.2155865157599051,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4248462857","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":[0.8374733,0.00014418148,0.023764325,0.0025283631,0.0005232665,0.0008118222,0.0000064833666,0.00012211416,0.13462617],"genre_scores_gemma":[0.9852858,0.000022686309,0.012506695,0.00044349083,0.000044704324,0.000049236398,0.0000019950655,0.000014549706,0.001630809],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9987726,0.000041545034,0.00026981442,0.00036745856,0.00039508226,0.00015345872],"domain_scores_gemma":[0.9992799,0.000008185579,0.00014362976,0.0004917505,0.0000040975838,0.0000723971],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0000902172,0.00016838826,0.00020344685,3.7241816e-7,0.00005030632,0.000020209925,0.00057852006,0.00018054577,0.0036109115],"category_scores_gemma":[0.000020461079,0.00010651928,0.00017690106,0.00009299406,0.0002002062,0.000029747462,0.0026790558,0.0003214585,0.00011579632],"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":[0.000066269,0.00046593178,0.07350974,0.00008276524,0.000045491346,0.000007420629,0.0014925512,0.0037211499,0.86382675,0.0019272469,0.048799302,0.006055405],"study_design_scores_gemma":[0.0008357054,0.00038776154,0.6765596,0.0002923887,0.00021158713,0.00001787618,0.0012847892,0.0068114805,0.24847256,0.014393582,0.049199417,0.0015331978],"about_ca_topic_score_codex":0.0007580378,"about_ca_topic_score_gemma":0.000058404064,"teacher_disagreement_score":0.6153542,"about_ca_system_score_codex":0.00017821466,"about_ca_system_score_gemma":0.000022798444,"threshold_uncertainty_score":0.9972999},"labels":[],"label_agreement":null},{"id":"W4248943471","doi":"10.5194/acp-2018-1153","title":"Lidar observations of pyrocumulonimbus smoke plumes in the UTLS over Tomsk (Western Siberia, Russia) from 2000 to 2017","year":2018,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"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":"U.S. Naval Research Laboratory; Office of Naval Research; Strong","keywords":"Environmental science; Troposphere; Stratosphere; Volcano; Smoke; Atmospheric sciences; Climatology; Aerosol; Boreal; Geography; Geology; Meteorology","score_opus":0.04425586374417163,"score_gpt":0.2859769384853557,"score_spread":0.2417210747411841,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4248943471","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":[0.98325473,0.000079734134,0.00070874416,0.0011510823,0.00029515664,0.0006182678,0.000105979816,0.00003580132,0.013750477],"genre_scores_gemma":[0.98542947,0.000047659116,0.0065438724,0.0017941927,0.00017689145,0.00009886716,0.000038523893,0.000029715422,0.005840796],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9977747,0.00008881779,0.0005228546,0.00066401664,0.00058784214,0.0003617441],"domain_scores_gemma":[0.99829805,0.00010906281,0.00024133551,0.0012276729,0.000012995621,0.00011089876],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00027433742,0.00033062213,0.00040921412,0.0000034741886,0.00009856572,0.00009995651,0.0013169931,0.00029328186,0.009048983],"category_scores_gemma":[0.000036396108,0.00023450243,0.00014159482,0.00021982982,0.00025610297,0.00013706442,0.0014790302,0.00032971767,0.00051340426],"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":[0.000038160688,0.00023383294,0.9678092,0.000015413614,0.000046408823,0.000010461061,0.005948016,0.0035383229,0.0011370385,0.000054726013,0.019803748,0.0013646736],"study_design_scores_gemma":[0.00019307165,0.000060869657,0.98523235,0.000064151565,0.000028772347,5.6566887e-7,0.0002743772,0.0003640545,0.00028794934,0.0012596864,0.011918896,0.00031523587],"about_ca_topic_score_codex":0.035851415,"about_ca_topic_score_gemma":0.0075707594,"teacher_disagreement_score":0.028280657,"about_ca_system_score_codex":0.00020481559,"about_ca_system_score_gemma":0.00006603038,"threshold_uncertainty_score":0.9918569},"labels":[],"label_agreement":null},{"id":"W4249055848","doi":"10.5194/acp-2020-1311-rc2","title":"Comment on acp-2020-1311","year":2021,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"Agencia Estatal de Investigación; Staatssekretariat für Bildung, Forschung und Innovation; Agència de Gestió d'Ajuts Universitaris i de Recerca; National Oceanic and Atmospheric Administration; Horizon 2020 Framework Programme; Svenska Forskningsrådet Formas; Korea Meteorological Administration; Région Occitanie Pyrénées-Méditerranée; Miljødirektoratet; Environmental Protection Administration, Executive Yuan, R.O.C. Taiwan; Magnus Bergvalls Stiftelse; Ministerio de Asuntos Económicos y Transformación Digital, Gobierno de España; North-West University; U.S. Department of Energy; Vetenskapsrådet; National Research Foundation of Korea; Ministerio de Economía y Competitividad; China Meteorological Administration; Generalitat de Catalunya; Commonwealth Scientific and Industrial Research Organisation; Office of Science; Desert Research Institute; Academy of Finland; Ministry of Science and Technology of the People's Republic of China; National Research Foundation; Helsingin Yliopisto; European Commission; Biological and Environmental Research; Centre National de la Recherche Scientifique; European Regional Development Fund; Ministerstvo Školství, Mládeže a Tělovýchovy","keywords":"Environmental science; Atmospheric sciences; Diel vertical migration; Annual cycle; Range (aeronautics); Aerosol; Polar; Scale (ratio); Meteorology; Climatology; Geography; Cartography; Geology; Ecology; Physics; Biology","score_opus":0.018575590756182665,"score_gpt":0.2694561122542017,"score_spread":0.25088052149801904,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4249055848","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000045538436,0.00641283,0.00015230352,0.35730633,0.0015457046,0.00038392775,0.000037998772,0.00006155986,0.6340538],"genre_scores_gemma":[0.000098375065,0.008727032,0.0014254123,0.22473104,0.00021800576,0.00005824461,0.00024235029,0.000037319205,0.76446223],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99793214,0.00006625717,0.00031555688,0.00061265344,0.0007270921,0.00034632554],"domain_scores_gemma":[0.9989371,0.00004785984,0.00012863288,0.0007150272,0.00000926723,0.00016213988],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00019441897,0.0003506826,0.00050532335,4.0205052e-7,0.000099955294,0.00003363217,0.00047064968,0.00019405247,0.23658912],"category_scores_gemma":[0.00003316067,0.0002674514,0.00022771153,0.00019717867,0.000090809815,0.000030905067,0.00057873415,0.00033572706,0.005430951],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000011907572,0.00008493001,0.00008121226,0.00013543243,0.0000167866,0.00002930473,0.0000094715315,0.00001317022,0.0000025761906,0.00008931384,0.98935133,0.010185255],"study_design_scores_gemma":[0.000088325236,0.00007106233,0.00016137591,0.00064604223,0.0000501986,0.0000052847877,0.000017077155,0.000018201748,0.000018661976,0.00004160572,0.9985495,0.00033265003],"about_ca_topic_score_codex":0.00060656114,"about_ca_topic_score_gemma":0.00022937731,"teacher_disagreement_score":0.23115817,"about_ca_system_score_codex":0.00028608946,"about_ca_system_score_gemma":0.000026742366,"threshold_uncertainty_score":0.99997777},"labels":[],"label_agreement":null},{"id":"W4249222599","doi":"10.5194/gmd-2017-307","title":"The implementation of NEMS GFS Aerosol Component (NGAC) Version 2.0 for global multispecies forecasting at NOAA/NCEP: Part II Evaluation of Aerosol Optical Thickness","year":2017,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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":"Goddard Space Flight Center; National Weather Service; National Oceanic and Atmospheric Administration","keywords":"Aerosol; Environmental science; Climatology; AERONET; Meteorology; Atmospheric sciences; Satellite; Data assimilation; Sea surface temperature; Geography; Geology; Physics","score_opus":0.06021392909415395,"score_gpt":0.33017545344330457,"score_spread":0.2699615243491506,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4249222599","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":[0.98687977,0.00010560919,0.0050892965,0.00041795295,0.0009350865,0.0021984503,0.00015408466,0.000025764873,0.0041939868],"genre_scores_gemma":[0.9925639,0.00007212733,0.00632538,0.000025121013,0.00010277145,0.00026918153,0.00017542587,0.000020927991,0.00044516454],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99651474,0.0001287613,0.00083474687,0.00061691547,0.001458372,0.0004464773],"domain_scores_gemma":[0.99756294,0.00020151492,0.001161217,0.0007885007,0.00018038625,0.00010543278],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0016492121,0.00034505263,0.00046016186,0.0000016962664,0.0011820173,0.00007149346,0.00076857157,0.00026218052,0.0012542314],"category_scores_gemma":[0.00016786985,0.00025306805,0.0002858713,0.000062105806,0.0006788799,0.00015263904,0.0026177282,0.00018689073,0.000015544858],"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":[0.001997714,0.001575481,0.268883,0.001023018,0.00095680816,0.0000044089566,0.008366229,0.18364646,0.08055302,0.004762593,0.03884366,0.40938762],"study_design_scores_gemma":[0.01178614,0.0017521022,0.18147354,0.00083280227,0.0018818458,0.000027307606,0.011579727,0.627295,0.15181908,0.0037428513,0.005397627,0.0024119536],"about_ca_topic_score_codex":0.0018143787,"about_ca_topic_score_gemma":0.003174089,"teacher_disagreement_score":0.44364858,"about_ca_system_score_codex":0.00089902437,"about_ca_system_score_gemma":0.00010508608,"threshold_uncertainty_score":0.99999213},"labels":[],"label_agreement":null},{"id":"W4249407498","doi":"10.4095/219748","title":"Cloud optical depths and TOA fluxes: Comparison between satellite and surface retrievals from multiple platforms","year":2001,"lang":"en","type":"report","venue":"","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Shortwave; Radiative transfer; Inversion (geology); Remote sensing; Cloud computing; Environmental science; Satellite; Broadband; Meteorology; Atmospheric radiative transfer codes; Cloud fraction; Cloud top; Flux (metallurgy); Computer science; Cloud cover; Physics; Geology; Optics; Telecommunications; Materials science; Astronomy","score_opus":0.038256160160578576,"score_gpt":0.28297576138667985,"score_spread":0.24471960122610126,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4249407498","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":[0.92888606,0.0027354585,0.0014473174,0.0000518363,0.00028807163,0.00042779706,0.00007022561,0.000096226635,0.065997005],"genre_scores_gemma":[0.9667971,0.0079388665,0.010483943,0.0000755962,0.0004411391,0.000005026457,0.00017122026,0.00007325657,0.0140138455],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99651927,0.00002556878,0.00077739207,0.0010029871,0.0010827247,0.0005920526],"domain_scores_gemma":[0.99827445,0.00045359062,0.0002891321,0.00048731262,0.000022095626,0.00047342712],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00051888544,0.0005513259,0.0010242412,0.0000021311519,0.00020077209,0.00013428055,0.00028400234,0.00075282156,0.0026552223],"category_scores_gemma":[0.00013623231,0.000426633,0.000107822394,0.00018552046,0.0005197502,0.00017564053,0.0006383055,0.000573338,0.00021787875],"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":[0.0000301362,0.000042697335,0.9621639,0.00002347244,0.00007107445,0.0000203225,0.00017283812,0.00005039442,0.00014000305,0.000004243538,0.006337229,0.030943688],"study_design_scores_gemma":[0.000814782,0.0003034273,0.7512431,0.00011449832,0.00026491206,0.00003637088,0.0006217375,0.0010696843,0.00079854403,0.00036333446,0.24317442,0.001195162],"about_ca_topic_score_codex":0.006778829,"about_ca_topic_score_gemma":0.0012775421,"teacher_disagreement_score":0.2368372,"about_ca_system_score_codex":0.0002909803,"about_ca_system_score_gemma":0.00005438119,"threshold_uncertainty_score":0.99983513},"labels":[],"label_agreement":null},{"id":"W4250267667","doi":"10.5194/acpd-11-21171-2011","title":"Deposition freezing on mineral dust particles: a case against classical nucleation theory with the assumption of a single contact angle","year":2011,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"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 British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Nucleation; Contact angle; Classical nucleation theory; Illite; Ice nucleus; Deposition (geology); Kaolinite; Mineralogy; Surface (topology); Materials science; Chemistry; Optics; Thermodynamics; Geology; Physics; Geometry; Clay minerals; Mathematics","score_opus":0.02115896080353887,"score_gpt":0.21669334947227337,"score_spread":0.1955343886687345,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4250267667","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":[0.9654215,0.000010893616,0.01571307,0.00019571278,0.000056043344,0.0003522176,0.000005492058,0.000046282472,0.018198792],"genre_scores_gemma":[0.9973563,0.000003876174,0.0018656506,0.00028718082,0.00005246724,0.000037980397,0.000013633295,0.0000225915,0.000360346],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.998826,0.00015586936,0.00022118025,0.00034150662,0.00026240025,0.00019303917],"domain_scores_gemma":[0.9992549,0.000070817965,0.00023709997,0.0003573586,0.000012989064,0.000066857916],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023263853,0.00019862072,0.00018452457,0.0000019325835,0.0001346938,0.000041399144,0.00015015448,0.00015897182,0.0006116761],"category_scores_gemma":[0.000014018652,0.000117855925,0.000084073276,0.000075456555,0.00021320481,0.000093975985,0.00019584979,0.00025137624,0.000050115374],"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":[0.0028151576,0.0046683126,0.058949716,0.00019754331,0.0004412298,0.0010918053,0.0177946,0.03978675,0.687728,0.0148808705,0.00718599,0.16446005],"study_design_scores_gemma":[0.009244704,0.01310968,0.4529599,0.002485258,0.002142133,0.0014971066,0.032136187,0.23241451,0.23364092,0.012831316,0.0015816253,0.0059566502],"about_ca_topic_score_codex":0.00091423444,"about_ca_topic_score_gemma":0.0013499322,"teacher_disagreement_score":0.45408705,"about_ca_system_score_codex":0.00018514364,"about_ca_system_score_gemma":0.00001186166,"threshold_uncertainty_score":0.6697424},"labels":[],"label_agreement":null},{"id":"W4250275550","doi":"10.1002/3527600434.eap629","title":"Lidar (Laser Radar)","year":2004,"lang":"en","type":"other","venue":"digital Encyclopedia of Applied Physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Western University","funders":"","keywords":"Lidar; Remote sensing; Radar; Atmosphere (unit); Laser; Wave radar; Environmental science; Radar imaging; Geology; Meteorology; Geography; Computer science; Radar engineering details; Physics; Optics; Telecommunications","score_opus":0.003780743168565265,"score_gpt":0.18418696780316848,"score_spread":0.1804062246346032,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4250275550","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0017262936,0.00003642032,0.00062204374,0.000005635406,0.0001587591,0.00033897313,0.00012269797,0.00013227448,0.9968569],"genre_scores_gemma":[0.07729183,0.00034270712,0.003893361,0.00018270272,0.00093220954,0.000064631575,0.0002734222,0.000956576,0.91606253],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9984696,0.0000027677181,0.00025900305,0.0004642221,0.00047488377,0.00032954066],"domain_scores_gemma":[0.9990898,0.000015665064,0.00028834917,0.00047591512,0.0000035031687,0.00012676105],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000021051384,0.00039758033,0.00042612068,0.0000015842245,0.000030006968,0.000030145875,0.00040446044,0.00022311158,0.0040014023],"category_scores_gemma":[0.0000032131863,0.0003704434,0.00014487338,0.00023413738,0.00033729104,0.00009294108,0.00026820484,0.00019021588,0.0022994205],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000051223775,0.0008308863,0.0013862237,0.00017171123,0.00015937378,0.000019875908,0.0005030289,0.00093836867,0.00010158029,0.0059959716,0.72050655,0.26933518],"study_design_scores_gemma":[0.00036422577,0.000039708757,0.00020151633,0.000041852007,0.000033041066,5.6016165e-7,0.00004305836,0.000004330369,0.00016659874,0.006313105,0.992271,0.00052101153],"about_ca_topic_score_codex":0.00011772678,"about_ca_topic_score_gemma":0.000010775256,"teacher_disagreement_score":0.27176443,"about_ca_system_score_codex":0.00008230215,"about_ca_system_score_gemma":0.00004405814,"threshold_uncertainty_score":0.9998748},"labels":[],"label_agreement":null},{"id":"W4250551958","doi":"10.5194/acpd-9-17465-2009","title":"Comparison of in situ and columnar aerosol spectral measurements during TexAQS-GoMACCS 2006: testing parameterizations for estimating aerosol fine mode properties","year":2009,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Université de Sherbrooke","funders":"National Oceanic and Atmospheric Administration; NOAA Research; Houston Advanced Research Center; Texas Commission on Environmental Quality","keywords":"AERONET; Angstrom exponent; Aerosol; Environmental science; Atmospheric sciences; Extinction (optical mineralogy); Effective radius; Wavelength; Remote sensing; Meteorology; Physics; Astrophysics; Optics; Geography","score_opus":0.07715402187295924,"score_gpt":0.30071640714736647,"score_spread":0.22356238527440725,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4250551958","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":[0.9709459,0.00009018529,0.025371548,0.00006843197,0.00009055506,0.0014935023,0.000017912307,0.000075956516,0.0018460208],"genre_scores_gemma":[0.72584766,0.0000030078104,0.27373713,0.000020376125,0.000035117286,0.00012361669,0.000014371207,0.000028085451,0.00019064208],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9974367,0.00005766206,0.00088964106,0.00068335334,0.00042896505,0.00050368765],"domain_scores_gemma":[0.9989776,0.0000646614,0.00046183926,0.0003465651,0.000036444726,0.00011286089],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00024700726,0.0003951531,0.00068304833,0.000006902503,0.00022890209,0.0000982541,0.0003308974,0.00020674775,0.00007885669],"category_scores_gemma":[0.0002571472,0.0003727666,0.00008258271,0.00021005348,0.00019904567,0.00015313296,0.0005675997,0.00032263482,0.0000041392823],"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":[0.000039490034,0.00027367094,0.3670667,0.00025389792,0.000020721494,0.0000011378289,0.00066245167,0.39142874,0.23804297,0.0000025154964,0.000068881265,0.0021388275],"study_design_scores_gemma":[0.0011684472,0.00031939338,0.08781998,0.0007998049,0.00008965557,0.0000061870746,0.00026313556,0.7698154,0.13862187,0.00025404728,0.000001924034,0.0008401784],"about_ca_topic_score_codex":0.0012716143,"about_ca_topic_score_gemma":0.0017876494,"teacher_disagreement_score":0.37838665,"about_ca_system_score_codex":0.00023698228,"about_ca_system_score_gemma":0.00004498944,"threshold_uncertainty_score":0.99987245},"labels":[],"label_agreement":null},{"id":"W4250640675","doi":"10.5194/acp-2018-426","title":"Springtime aerosol load as observed from ground-based and airborne lidars over Northern Norway","year":2018,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Lidar; Aerosol; Environmental science; Troposphere; Atmospheric sciences; Nadir; Meteorology; Arctic; Zenith; Remote sensing; Geography; Satellite; Geology; Physics","score_opus":0.01464608644305282,"score_gpt":0.21931854397597508,"score_spread":0.20467245753292226,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4250640675","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":[0.96958387,0.00014110167,0.0015594937,0.00025970675,0.00044641425,0.00047860297,0.000039214614,0.00014725007,0.027344367],"genre_scores_gemma":[0.9822157,0.00003865536,0.009029635,0.0011671489,0.00021482844,0.000050168317,0.00004317047,0.00008206152,0.0071586045],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99681294,0.00006874882,0.00045251002,0.0013392346,0.0007824071,0.00054417],"domain_scores_gemma":[0.9981831,0.00007837107,0.00027598604,0.001100179,0.000027528848,0.00033483445],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00021404786,0.00061246916,0.00052223937,0.0000017239905,0.00019767667,0.00020583735,0.0007112423,0.00052063854,0.042163234],"category_scores_gemma":[0.0000379701,0.00053373846,0.00020274766,0.00011724955,0.0005709847,0.0001352655,0.0020398009,0.00051549904,0.005033053],"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":[0.00025420627,0.00043287216,0.9747796,0.000058260073,0.00021529512,0.000069546215,0.0007162652,0.0026411552,0.0066402527,0.000027430253,0.0040963683,0.010068725],"study_design_scores_gemma":[0.0014072711,0.00031474512,0.97329515,0.00014134978,0.00015295857,0.0000026441217,0.00008960731,0.01124622,0.0030841155,0.0014707675,0.0071776668,0.0016174795],"about_ca_topic_score_codex":0.05969932,"about_ca_topic_score_gemma":0.0115006715,"teacher_disagreement_score":0.048198648,"about_ca_system_score_codex":0.0005308038,"about_ca_system_score_gemma":0.0001165004,"threshold_uncertainty_score":0.9997114},"labels":[],"label_agreement":null},{"id":"W4250713463","doi":"10.5194/amtd-6-9579-2013","title":"Evaluation of gridded Scanning ARM Cloud Radar reflectivity observations and vertical Doppler velocity retrievals","year":2013,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Biological and Environmental Research; McGill University; U.S. Department of Energy","keywords":"Zenith; Radar; Remote sensing; Doppler effect; Geology; Doppler radar; Cartesian coordinate system; Meteorology; Geography; Physics; Computer science; Geometry","score_opus":0.07473021042584088,"score_gpt":0.3023387562573105,"score_spread":0.2276085458314696,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4250713463","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":[0.982558,0.00009734418,0.003961979,0.00033071786,0.00027761128,0.0006840392,0.000009928587,0.000043892596,0.01203649],"genre_scores_gemma":[0.9880528,0.000041474887,0.011375441,0.000111923924,0.000078691024,0.000058496615,0.000015026863,0.000017717244,0.00024846848],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9969769,0.00026465562,0.000407923,0.0005648878,0.0015371063,0.00024850667],"domain_scores_gemma":[0.99899185,0.00009496238,0.00016495927,0.0004586063,0.00015921133,0.00013038506],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0023882722,0.00023237547,0.00034276114,0.0000022869672,0.00014109857,0.000045936118,0.00022334547,0.00029011106,0.0050757737],"category_scores_gemma":[0.00056351343,0.00020322711,0.00008126365,0.00019749225,0.000313685,0.00014886455,0.00095838745,0.0003738408,0.000033627566],"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":[0.00024889378,0.002099031,0.6582255,0.00041766555,0.00078837783,0.0000049097303,0.0060324543,0.03932807,0.09697576,0.007022323,0.087413415,0.101443626],"study_design_scores_gemma":[0.00050022744,0.00008066491,0.8814509,0.000055494205,0.0002900942,0.000002662496,0.00012248676,0.09384752,0.0044678394,0.018504614,0.00028694997,0.00039054698],"about_ca_topic_score_codex":0.0029420084,"about_ca_topic_score_gemma":0.00016974086,"teacher_disagreement_score":0.22322543,"about_ca_system_score_codex":0.0005689902,"about_ca_system_score_gemma":0.00015002405,"threshold_uncertainty_score":0.9958337},"labels":[],"label_agreement":null},{"id":"W4251076715","doi":"10.5194/acp-2021-21-rc2","title":"Comment on acp-2021-21","year":2021,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"National Research Council Canada","funders":"FP7 Ideas: European Research Council; Staatssekretariat für Bildung, Forschung und Innovation; Horizon 2020 Framework Programme; European Commission","keywords":"Lidar; Aerosol; Relative humidity; Sun photometer; Atmospheric sciences; Environmental science; Physics; Meteorology; Optics","score_opus":0.02003873070866118,"score_gpt":0.27014386303401905,"score_spread":0.25010513232535786,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4251076715","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000034914192,0.0060474807,0.0001912779,0.33866793,0.0015616325,0.0003669551,0.000038327275,0.000036475303,0.653055],"genre_scores_gemma":[0.000068647736,0.009667813,0.001432473,0.16991605,0.00022939856,0.00005746221,0.00031745838,0.00003487791,0.8182758],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9979253,0.00007161174,0.00031079186,0.00061007927,0.0007332618,0.0003489606],"domain_scores_gemma":[0.9989086,0.000050187286,0.00012591305,0.00074727077,0.000009927126,0.00015810208],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0002076131,0.00034752375,0.0005049547,5.428945e-7,0.00010117334,0.00003564702,0.00045100265,0.00019547268,0.3530852],"category_scores_gemma":[0.000034154225,0.00026571343,0.00023126532,0.00019491996,0.00009073676,0.00003096197,0.00057630416,0.00040146318,0.0085559655],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000011281808,0.00008805809,0.00006162336,0.00010828104,0.000017155746,0.000023147306,0.000009297634,0.000013287697,0.00000346557,0.00007492834,0.97840095,0.02119866],"study_design_scores_gemma":[0.000086587606,0.00006554301,0.00016135328,0.00068410253,0.00004952979,0.0000033915221,0.000019693776,0.000017855113,0.000023228902,0.00003133317,0.9985264,0.000331015],"about_ca_topic_score_codex":0.00071643834,"about_ca_topic_score_gemma":0.00017351251,"teacher_disagreement_score":0.34452924,"about_ca_system_score_codex":0.00029916587,"about_ca_system_score_gemma":0.000028388344,"threshold_uncertainty_score":0.9999795},"labels":[],"label_agreement":null},{"id":"W4251076740","doi":"10.5194/acp-2019-47","title":"Is Positive Correlation between Cloud Droplet Effective Radius andAerosol Index over Land Due to Retrieval Artifacts or Real PhysicalProcesses?","year":2019,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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":"National Natural Science Foundation of China; National Aeronautics and Space Administration","keywords":"Aerosol; Liquid water path; Effective radius; Environmental science; Moderate-resolution imaging spectroradiometer; Atmospheric sciences; Cloud top; Liquid water content; Meteorology; Climatology; Cloud computing; Geography; Satellite; Geology; Physics","score_opus":0.009468566046709382,"score_gpt":0.25809660952657415,"score_spread":0.24862804347986478,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4251076740","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":[0.9517105,0.000007970454,0.032454673,0.0002643793,0.00052174996,0.002002723,0.00015536383,0.00010970571,0.012772919],"genre_scores_gemma":[0.99250233,0.000019861698,0.00047884107,0.00067175797,0.0005245589,0.000049011203,0.00012725573,0.00006645775,0.0055599445],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99677885,0.00012843462,0.00043259337,0.0012522932,0.00084106036,0.0005667773],"domain_scores_gemma":[0.99831885,0.00032188106,0.00033765807,0.0006313021,0.00004217431,0.00034811063],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00024468242,0.0005784752,0.0007889871,0.00000537825,0.00017127185,0.00014405805,0.00037121965,0.00059435563,0.0035745753],"category_scores_gemma":[0.00008186288,0.0004475971,0.00018238105,0.00041956373,0.00016602589,0.00021481045,0.0013199237,0.0008025982,0.0018858239],"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":[0.0013898626,0.00023854371,0.9603167,0.000117736934,0.00024245323,0.00006386386,0.0029969728,0.015152489,0.00080878934,0.000023485452,0.011608395,0.0070406646],"study_design_scores_gemma":[0.0008360967,0.00053796725,0.9870827,0.00013199516,0.0001274805,0.0000065714985,0.00005936526,0.0061527137,0.0034250498,0.00043267978,0.000428363,0.0007789863],"about_ca_topic_score_codex":0.0034189092,"about_ca_topic_score_gemma":0.00018714312,"teacher_disagreement_score":0.040791795,"about_ca_system_score_codex":0.00063375925,"about_ca_system_score_gemma":0.000091892885,"threshold_uncertainty_score":0.9997976},"labels":[],"label_agreement":null},{"id":"W4251512057","doi":"10.5194/amtd-4-5631-2011","title":"Aerosol classification using airborne High Spectral Resolution Lidar measurements – methodology and examples","year":2011,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":30,"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":"NASA Headquarters; Science Mission Directorate; Langley Research Center; National Aeronautics and Space Administration; U.S. Department of Energy","keywords":"Aerosol; Lidar; Remote sensing; Environmental science; Backscatter (email); Extinction (optical mineralogy); Atmospheric sciences; Meteorology; Geology; Mineralogy; Physics; Computer science","score_opus":0.24328210069966616,"score_gpt":0.3112250433248721,"score_spread":0.06794294262520595,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4251512057","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":[0.87578475,0.00014063357,0.11148221,0.00011274935,0.00042405727,0.00041562656,0.0000055118962,0.00009172468,0.011542714],"genre_scores_gemma":[0.746446,0.000081064936,0.25282493,0.00008772439,0.00009074046,0.000022705019,0.000016263642,0.000026021045,0.00040450966],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99767333,0.0003394204,0.00039075816,0.00085221056,0.0003542665,0.00038998888],"domain_scores_gemma":[0.9989792,0.000041239018,0.00029590583,0.00052773516,0.000017091583,0.00013883949],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000806985,0.00032105212,0.00036428918,0.0000036203635,0.00018228627,0.000042615193,0.00030410776,0.0004052557,0.0023382017],"category_scores_gemma":[0.0000566586,0.00029016848,0.00007625432,0.00009577565,0.00035055514,0.00011534347,0.0008667844,0.00035757516,0.00008255345],"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":[0.00041347183,0.00072276423,0.30054778,0.00023184082,0.00042182548,0.000018904528,0.0035684493,0.00860229,0.622633,0.008316626,0.002265327,0.05225776],"study_design_scores_gemma":[0.0005945635,0.00016903042,0.9543339,0.00007190441,0.00025543116,0.000023668279,0.000354576,0.0079676015,0.02008381,0.014674433,0.0004144776,0.0010566309],"about_ca_topic_score_codex":0.01051133,"about_ca_topic_score_gemma":0.00058079284,"teacher_disagreement_score":0.6537861,"about_ca_system_score_codex":0.00036229962,"about_ca_system_score_gemma":0.000033406635,"threshold_uncertainty_score":0.99995506},"labels":[],"label_agreement":null},{"id":"W4251546653","doi":"10.22215/etd/2008-07780","title":"Sky-scattered solar radiation based plume transmissivity measurements","year":2008,"lang":"en","type":"dissertation","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Library and Archives Canada","funders":"","keywords":"Sky; Radiation; Physics; Plume; Optics; Environmental science; Astronomy; Meteorology","score_opus":0.01699523175521304,"score_gpt":0.23127289586387445,"score_spread":0.21427766410866142,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4251546653","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":[0.80000365,0.0001610414,0.006942046,0.00020746919,0.00074733526,0.00081619195,0.000013750887,0.00019282853,0.1909157],"genre_scores_gemma":[0.95739967,0.000073234754,0.0023027186,0.0005404356,0.000057178055,0.000060668215,0.00064363034,0.00006223206,0.038860265],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9979169,0.00006391094,0.00033033843,0.00053437613,0.0008138762,0.00034060047],"domain_scores_gemma":[0.9992847,0.000015345622,0.00019341317,0.00032941927,0.000013657952,0.00016348786],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00014879732,0.00034013693,0.0002883629,0.0000027047713,0.00024287293,0.000032338918,0.0002954419,0.00031759677,0.01692544],"category_scores_gemma":[0.000014790916,0.00031510778,0.00018187509,0.00018366092,0.000052806827,0.00015687442,0.000012065502,0.00022286079,0.00093162013],"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":[0.00060296856,0.0016441612,0.2772655,0.00033611144,0.00029054243,0.000056680157,0.0044601816,0.0063605434,0.08138708,0.000010801543,0.16008452,0.46750093],"study_design_scores_gemma":[0.0018424849,0.00018622405,0.90271026,0.00007965423,0.00017745499,0.000003878706,0.00026673786,0.005597181,0.04259809,0.000066820445,0.044956688,0.0015144978],"about_ca_topic_score_codex":0.0010761616,"about_ca_topic_score_gemma":0.0009664013,"teacher_disagreement_score":0.6254448,"about_ca_system_score_codex":0.00028027565,"about_ca_system_score_gemma":0.000062843996,"threshold_uncertainty_score":0.9999301},"labels":[],"label_agreement":null},{"id":"W4251578657","doi":"10.5194/amt-2019-369","title":"Synergistic radar and radiometer retrievals of ice hydrometeors","year":2019,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":12,"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":"Universität Hamburg; Swedish National Space Agency; Environment and Climate Change Canada; Deutsche Forschungsgemeinschaft","keywords":"Remote sensing; Radiometer; Satellite; Environmental science; Ice cloud; Microwave radiometer; Radar; Meteorology; Microwave; Atmosphere (unit); Computer science; Geology; Physics","score_opus":0.009256173589083396,"score_gpt":0.21936082850854713,"score_spread":0.21010465491946373,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4251578657","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":[0.9471829,0.0003307283,0.007071158,0.00007413766,0.00031596486,0.0003137173,0.000014682669,0.000030845964,0.044665854],"genre_scores_gemma":[0.97801036,0.00019550226,0.010999981,0.00011070612,0.000028446351,0.000006291903,0.00000711145,0.00002516657,0.010616448],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984327,0.000049410468,0.00034440137,0.00054225675,0.00039450004,0.00023672276],"domain_scores_gemma":[0.99893504,0.00013452447,0.00022523588,0.0005890339,0.0000066883454,0.00010944967],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002855482,0.00024689906,0.00045909913,0.0000033255349,0.00003308121,0.000024179464,0.00034291093,0.00024438323,0.0064638103],"category_scores_gemma":[0.00007790819,0.00020025446,0.0001048161,0.0001862042,0.00030354047,0.00005304259,0.0013190175,0.00024958028,0.00020304887],"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":[0.0005698537,0.0012675782,0.4750055,0.0036372321,0.001571827,0.00015883219,0.0045982245,0.069783986,0.2589914,0.0028984724,0.06435635,0.11716076],"study_design_scores_gemma":[0.0065580485,0.0028590325,0.69596976,0.0013705686,0.0021485074,0.000081025435,0.0014271989,0.1033381,0.08215906,0.028433152,0.06540813,0.010247432],"about_ca_topic_score_codex":0.00079192105,"about_ca_topic_score_gemma":0.000008746694,"teacher_disagreement_score":0.22096424,"about_ca_system_score_codex":0.00008929278,"about_ca_system_score_gemma":0.000017541366,"threshold_uncertainty_score":0.99444443},"labels":[],"label_agreement":null},{"id":"W4252053747","doi":"10.5194/acp-2019-615","title":"The unprecedented 2017–2018 stratospheric smoke event: Decay phase and aerosol properties observed with EARLINET","year":2019,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","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":"Horizon 2020; European Regional Development Fund; Horizon 2020 Framework Programme; Russian Science Foundation; European Commission; Irish Research Council; Science Foundation Ireland; Bundesministerium für Bildung und Forschung; European Space Agency","keywords":"Stratosphere; Aerosol; Atmospheric sciences; Troposphere; Environmental science; Smoke; Climatology; Northern Hemisphere; Lidar; Southern Hemisphere; Meteorology; Geography; Physics; Geology; Remote sensing","score_opus":0.03715966208834097,"score_gpt":0.24988815328710262,"score_spread":0.21272849119876164,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4252053747","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":[0.98720104,0.0009659826,0.0018432221,0.00048751297,0.00030882214,0.0012816526,0.0000193409,0.00011138817,0.007781068],"genre_scores_gemma":[0.9788773,0.0006680104,0.0012725699,0.00021149951,0.00006302796,0.00014038727,0.000021561007,0.000057737834,0.018687906],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99744487,0.00010226964,0.0004343598,0.00086758373,0.0005870499,0.0005638469],"domain_scores_gemma":[0.9984206,0.000050054467,0.00029738247,0.001003435,0.000023965906,0.0002045497],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00027492832,0.00053574337,0.0004140724,8.426261e-7,0.00038218373,0.00031630526,0.00075661653,0.00026238762,0.0014465863],"category_scores_gemma":[0.000012411284,0.00028343618,0.000104049774,0.00013658918,0.0006714186,0.00016243308,0.0013172796,0.00052949577,0.00021861074],"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":[0.004063528,0.0034937616,0.67793053,0.0009145827,0.0019482987,0.00013850731,0.005975214,0.1293143,0.027241027,0.00046823308,0.07306953,0.07544247],"study_design_scores_gemma":[0.029089244,0.009514706,0.4925311,0.0026817075,0.0018125076,0.00036663775,0.015444592,0.26503015,0.050128806,0.00084801327,0.118663274,0.013889285],"about_ca_topic_score_codex":0.0021323967,"about_ca_topic_score_gemma":0.002051892,"teacher_disagreement_score":0.18539946,"about_ca_system_score_codex":0.00013114966,"about_ca_system_score_gemma":0.00007868625,"threshold_uncertainty_score":0.9999618},"labels":[],"label_agreement":null},{"id":"W4252234925","doi":"10.5194/amt-2019-107","title":"Retrieval of Temperature From a Multiple Channel Pure Rotational Raman-Scatter Lidar Using an Optimal Estimation Method","year":2019,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Canadian Space Agency; École Polytechnique Fédérale de Lausanne","keywords":"Lidar; Calibration; Radiosonde; Remote sensing; Range (aeronautics); Environmental science; Computational physics; Sky; Materials science; Physics; Meteorology; Mathematics; Statistics; Geology","score_opus":0.021593452270430944,"score_gpt":0.2808196879405456,"score_spread":0.25922623567011466,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4252234925","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":[0.70945317,0.000030167734,0.28924182,0.00010926689,0.0002631617,0.00042797465,0.00010585608,0.000033765467,0.000334784],"genre_scores_gemma":[0.608029,0.0000027770031,0.39111656,0.00014171306,0.0001011524,0.0000076110236,0.0002814944,0.00002687228,0.00029282164],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99786806,0.00013277793,0.00041499193,0.000745056,0.000591794,0.00024730145],"domain_scores_gemma":[0.9988775,0.00009090031,0.00033976886,0.00054807373,0.000034720793,0.000109037086],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00029451703,0.0003325627,0.00041025374,0.0000038365197,0.00009328385,0.000081515616,0.00040855145,0.00053479953,0.004620918],"category_scores_gemma":[0.00004538141,0.00029098487,0.00015225564,0.00013393752,0.00009990017,0.00025738828,0.00067325635,0.0005100656,0.000084945794],"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":[0.000105874235,0.00012470863,0.006639541,0.000027250619,0.000043070806,0.0000021137164,0.000906331,0.956802,0.03437058,0.000006301221,0.00024462756,0.0007276092],"study_design_scores_gemma":[0.00042337793,0.00006259946,0.035432264,0.00006548602,0.00006544999,0.0000036241627,0.00028344762,0.9482586,0.014486305,0.0004890473,0.000033003827,0.00039682284],"about_ca_topic_score_codex":0.0012401391,"about_ca_topic_score_gemma":0.00003123548,"teacher_disagreement_score":0.10187473,"about_ca_system_score_codex":0.00017823424,"about_ca_system_score_gemma":0.0000639196,"threshold_uncertainty_score":0.9999542},"labels":[],"label_agreement":null},{"id":"W4253185986","doi":"10.5194/acpd-9-22041-2009","title":"Influences of in-cloud aerosol scavenging parameterizations on aerosol concentrations and wet deposition in ECHAM5-HAM","year":2009,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"BioFrontiers Institute, University of Colorado Boulder; National Oceanic and Atmospheric Administration; Killam Trusts","keywords":"Aerosol; Scavenging; Atmospheric sciences; Environmental science; Ice nucleus; Deposition (geology); Ice crystals; Cloud computing; Nucleation; Meteorology; Mass concentration (chemistry); Sulfate; Chemistry; Physics; Geology","score_opus":0.011257205354301894,"score_gpt":0.2401431900452974,"score_spread":0.22888598469099553,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4253185986","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":[0.99148583,0.00005315352,0.003415857,0.0002165964,0.00011057463,0.0005791466,0.000017159615,0.00003160801,0.0040900465],"genre_scores_gemma":[0.9930531,0.00026999376,0.0062674717,0.00021885085,0.000021501579,0.000039476075,0.000034365978,0.0000129960945,0.00008226942],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.998288,0.00008958042,0.0005477464,0.0005076384,0.00028129644,0.00028578046],"domain_scores_gemma":[0.9993289,0.00007049787,0.00020780702,0.0003015327,0.000008729274,0.000082549355],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00016555192,0.00025382338,0.00033497886,0.0000073379974,0.00007959498,0.000057372938,0.00020736226,0.00023919916,0.00031093814],"category_scores_gemma":[0.00003579001,0.00024550932,0.000055382676,0.0002879908,0.00022034552,0.00013820517,0.00024333117,0.00034947527,0.00001933091],"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":[0.0000471896,0.0005940784,0.3756908,0.0000792224,0.00002140785,0.000019877363,0.0018295303,0.57486546,0.0392544,0.00079942326,0.00014283677,0.0066557457],"study_design_scores_gemma":[0.0029342514,0.00090228923,0.7598086,0.0023691647,0.00011582589,0.000024109677,0.0018392276,0.13616027,0.088413104,0.0047602835,0.000056701323,0.0026161936],"about_ca_topic_score_codex":0.000997213,"about_ca_topic_score_gemma":0.0009627015,"teacher_disagreement_score":0.4387052,"about_ca_system_score_codex":0.00016351276,"about_ca_system_score_gemma":0.0000323215,"threshold_uncertainty_score":0.9999997},"labels":[],"label_agreement":null},{"id":"W4253232939","doi":"10.5194/acp-2017-38-supplement","title":"Supplementary material to \"Classifying aerosol type using in situ surface spectral aerosoloptical properties\"","year":2017,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"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":"Aerosol; In situ; Surface (topology); Chemistry; Mathematics; Organic chemistry; Geometry","score_opus":0.04767705127171255,"score_gpt":0.2794757240377325,"score_spread":0.23179867276601995,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4253232939","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":[0.98820084,0.000011276029,0.0003891723,0.00065232516,0.0014615254,0.000922208,0.0000654717,0.00005610748,0.008241099],"genre_scores_gemma":[0.9584378,0.000016894135,0.03935146,0.000317128,0.00022301516,0.000019276134,0.00006419338,0.000061637045,0.0015085818],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9969319,0.00007880283,0.0005462085,0.0010374767,0.0005284017,0.0008772231],"domain_scores_gemma":[0.9986159,0.000012235577,0.00016591881,0.00091183843,0.000012555352,0.00028154952],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00030541202,0.0005124318,0.00056241616,0.0000032419134,0.00025255213,0.0003177121,0.00095692626,0.00035260952,0.018044043],"category_scores_gemma":[0.00003326084,0.00044227208,0.000109703375,0.00010546307,0.00025878052,0.00015095745,0.0038280182,0.00056794455,0.0003034616],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040385447,0.0002605095,0.106955856,0.000092398914,0.00004622033,0.00013374769,0.0008999518,0.05111858,0.83547807,0.000028966786,0.0041228915,0.00045894246],"study_design_scores_gemma":[0.0039865444,0.0014278466,0.07577965,0.0015548551,0.00039108063,0.00013006828,0.0024557963,0.044625815,0.85182834,0.0008004685,0.008041829,0.0089777],"about_ca_topic_score_codex":0.009961048,"about_ca_topic_score_gemma":0.0042195,"teacher_disagreement_score":0.03896229,"about_ca_system_score_codex":0.0009098526,"about_ca_system_score_gemma":0.00010420081,"threshold_uncertainty_score":0.9998029},"labels":[],"label_agreement":null},{"id":"W4254427148","doi":"10.5194/amt-2021-139-rc3","title":"Review","year":2021,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"National Oceanic and Atmospheric Administration; Academy of Finland; Langley Research Center; National Aeronautics and Space Administration","keywords":"Aerosol; Span (engineering); Depolarization ratio; Smoke; Meteorology; Atmospheric sciences; Analytical Chemistry (journal); Materials science; Chemistry; Physics; Chromatography","score_opus":0.021630112036149906,"score_gpt":0.28619373066355386,"score_spread":0.26456361862740396,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4254427148","genre_codex":"review","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[4.749409e-7,0.534322,0.0000649671,0.04801298,0.0005313766,0.0002495104,0.000010153989,0.000029013396,0.41677952],"genre_scores_gemma":[3.070012e-7,0.43353257,0.00080732384,0.08684682,0.00006881812,0.000029131286,0.0001322818,0.000014061176,0.4785687],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99841267,0.00005378506,0.0003374792,0.0004927564,0.0004455782,0.00025775228],"domain_scores_gemma":[0.9990508,0.000018496914,0.00013633056,0.0006624284,0.000013004846,0.00011894501],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00024649888,0.00026503365,0.0006275329,1.7619975e-7,0.00004975067,0.000012739913,0.00040385415,0.00012835643,0.4883709],"category_scores_gemma":[0.00007751908,0.00019667305,0.0002607482,0.00025955756,0.00007356633,0.00003642728,0.00048229465,0.00027829065,0.008658563],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[6.933623e-8,0.000014427163,0.000020417103,0.0047132247,0.000007907498,0.000010815831,9.0701013e-7,3.303078e-7,8.789518e-7,0.0000053971335,0.96504813,0.030177493],"study_design_scores_gemma":[0.000022406177,0.000009585587,0.000035461384,0.018428227,0.00012236433,0.000014502153,0.0000012608406,0.0000017234141,0.0000012914381,0.000010950031,0.98109317,0.0002590646],"about_ca_topic_score_codex":0.00040326084,"about_ca_topic_score_gemma":0.00016228981,"teacher_disagreement_score":0.47971234,"about_ca_system_score_codex":0.00010994176,"about_ca_system_score_gemma":0.000035780813,"threshold_uncertainty_score":0.9921133},"labels":[],"label_agreement":null},{"id":"W4254561892","doi":"10.5194/amt-2017-50","title":"Combined retrieval of Arctic liquid water cloud and surface snow properties using airborne spectral solar remote sensing","year":2017,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"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":"Deutsche Forschungsgemeinschaft","keywords":"Snow; Remote sensing; Albedo (alchemy); Arctic; Environmental science; Cloud computing; Effective radius; Sea ice; Meteorology; Materials science; Geology; Computer science; Geography; Physics; Oceanography; Astronomy","score_opus":0.02572449170808313,"score_gpt":0.2335317870627732,"score_spread":0.20780729535469006,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4254561892","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":[0.9936472,0.000086254324,0.0034937293,0.0003988158,0.00047094558,0.0004006815,0.0000037493626,0.00005039868,0.0014481839],"genre_scores_gemma":[0.98064655,0.00009550064,0.016968183,0.00005885574,0.00010002534,8.115742e-8,0.0000051322927,0.000044889577,0.0020807695],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99792826,0.000090567955,0.00042154532,0.0006556753,0.000415935,0.00048800567],"domain_scores_gemma":[0.99875975,0.000018079963,0.00026064087,0.0007962633,0.000028491007,0.0001367788],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00046504167,0.0003795772,0.0005581373,0.0000019159122,0.00029120035,0.00010526858,0.000347885,0.00029696638,0.0004926355],"category_scores_gemma":[0.00005905376,0.00026166905,0.00012580825,0.000036647743,0.00075682456,0.00012480319,0.0019987908,0.00048486987,0.000032220396],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002134069,0.00014637128,0.009211006,0.0007503698,0.00026587638,0.00010430359,0.0045371936,0.030687915,0.9490715,0.000018968993,0.00016126547,0.0029111644],"study_design_scores_gemma":[0.00087870227,0.00055625295,0.00521244,0.0008351367,0.00022451584,0.000058663565,0.00033182136,0.16705628,0.8219074,0.0015789219,0.00017891577,0.0011809173],"about_ca_topic_score_codex":0.007681519,"about_ca_topic_score_gemma":0.00010359941,"teacher_disagreement_score":0.13636836,"about_ca_system_score_codex":0.00020409892,"about_ca_system_score_gemma":0.00003746883,"threshold_uncertainty_score":0.99998355},"labels":[],"label_agreement":null},{"id":"W4254673231","doi":"10.5194/amtd-4-3891-2011","title":"Inversion of tropospheric profiles of aerosol extinction and HCHO and NO <sub>2</sub> mixing ratios from MAX-DOAS observations in Milano during the summer of 2003 and comparison with independent data sets","year":2011,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":11,"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; Trace gas; Troposphere; AERONET; Inversion (geology); Atmospheric sciences; Radiative transfer; Mixing ratio; Environmental science; Meteorology; Geology; Physics; Optics","score_opus":0.03397141660120272,"score_gpt":0.23038075988115536,"score_spread":0.19640934327995263,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4254673231","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":[0.99773866,0.00024442503,0.0008809508,0.0000263308,0.000047628175,0.0006375071,0.000054328164,0.000007493695,0.00036269278],"genre_scores_gemma":[0.9911002,0.00045338838,0.008263361,0.000016873319,0.000008397621,0.000018782532,0.00007721127,0.000015370182,0.000046413752],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99848765,0.00008562759,0.00047567798,0.00050791586,0.00029627586,0.00014685684],"domain_scores_gemma":[0.9988523,0.000045975303,0.00050040905,0.0005175144,0.000028986315,0.00005482699],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019194507,0.00021715305,0.00039097155,0.0000032327775,0.000079037054,0.000018248225,0.0002539082,0.00015237741,0.00019215477],"category_scores_gemma":[0.000026136762,0.00015388358,0.000016802253,0.00015970848,0.000386799,0.00021535122,0.0014738323,0.00023969224,0.0000012813923],"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":[0.00010819612,0.0000897822,0.91219914,0.000113897215,0.00003291541,6.06445e-7,0.0010367878,0.00062142045,0.08509843,0.0000021542821,0.0001669883,0.00052966835],"study_design_scores_gemma":[0.0006690511,0.00009107967,0.9308291,0.00017275052,0.0000762928,0.0000017058138,0.0011437201,0.016802108,0.04996109,0.000039876788,0.000011402604,0.00020184401],"about_ca_topic_score_codex":0.008162504,"about_ca_topic_score_gemma":0.0051162336,"teacher_disagreement_score":0.035137337,"about_ca_system_score_codex":0.000037186794,"about_ca_system_score_gemma":0.00002362283,"threshold_uncertainty_score":0.99844223},"labels":[],"label_agreement":null},{"id":"W4254939633","doi":"10.5194/acpd-12-25983-2012","title":"Aerosol classification by airborne high spectral resolution lidar observations","year":2012,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":15,"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":"National Oceanic and Atmospheric Administration; Coordenação de Aperfeiçoamento de Pessoal de Nível Superior; Deutsche Forschungsgemeinschaft; European Space Agency","keywords":"Aerosol; Environmental science; Lidar; Remote sensing; Atmosphere (unit); Biomass burning; Atmospheric sciences; High resolution; Meteorology; Geology; Geography","score_opus":0.031592296322402236,"score_gpt":0.23690302471153815,"score_spread":0.20531072838913592,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4254939633","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":[0.9155576,0.00019768701,0.044131927,0.0030442432,0.0008887809,0.00068485696,0.00007531118,0.00030747108,0.0351121],"genre_scores_gemma":[0.9639131,0.00011120815,0.02233007,0.00035849647,0.00026705305,0.0001229574,0.0004406264,0.000038337792,0.012418147],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9979643,0.00006728195,0.00040412546,0.0006296018,0.00045456956,0.00048007752],"domain_scores_gemma":[0.99877995,0.000025047828,0.00025679573,0.00072902185,0.000014205958,0.00019500112],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00021704163,0.00031762556,0.00024498315,0.0000014778225,0.00021587002,0.000072108,0.00045917908,0.00041385615,0.008719533],"category_scores_gemma":[0.000021439779,0.0002949793,0.00011845558,0.00017960914,0.0002010018,0.0002310204,0.0006502593,0.0004994069,0.0014106805],"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":[0.00006339965,0.0013379817,0.23313083,0.000079244564,0.000121728706,0.0000032160171,0.00092584186,0.0069683194,0.09504126,0.014279704,0.63631785,0.011730646],"study_design_scores_gemma":[0.0002826857,0.000049083097,0.96525055,0.000026068934,0.00008750404,0.0000022994907,0.0001293198,0.0066427714,0.00261273,0.0017709235,0.022353414,0.00079267257],"about_ca_topic_score_codex":0.0028661413,"about_ca_topic_score_gemma":0.00019387818,"teacher_disagreement_score":0.7321197,"about_ca_system_score_codex":0.00057324616,"about_ca_system_score_gemma":0.000029050687,"threshold_uncertainty_score":0.99995023},"labels":[],"label_agreement":null},{"id":"W4255241205","doi":"10.5194/acp-2020-1311","title":"Seasonality of the particle number concentration and sizedistribution: a global analysis retrieved from the network of GlobalAtmosphere Watch (GAW) near-surface observatories","year":2021,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":25,"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":"Agencia Estatal de Investigación; Horizon 2020; National Oceanic and Atmospheric Administration; Ministerio de Asuntos Económicos y Transformación Digital, Gobierno de España; Miljødirektoratet; Environmental Protection Administration, Executive Yuan, R.O.C. Taiwan; Magnus Bergvalls Stiftelse; Centre National de la Recherche Scientifique; Vetenskapsrådet; National Research Foundation of Korea; National Research Foundation; Horizon 2020 Framework Programme; Svenska Forskningsrådet Formas; Korea Meteorological Administration; Chinese Academy of Meteorological Sciences; Ministerio de Economía y Competitividad; Generalitat de Catalunya; Agència de Gestió d'Ajuts Universitaris i de Recerca; China Meteorological Administration; Academy of Finland; Ministry of Science and Technology of the People's Republic of China; European Regional Development Fund; European Commission; Helsingin Yliopisto","keywords":"Environmental science; Seasonality; Diel vertical migration; Annual cycle; Atmospheric sciences; Aerosol; Atmosphere (unit); Climatology; Range (aeronautics); Meteorology; Geography; Statistics; Geology; Oceanography; Mathematics","score_opus":0.010043896475237606,"score_gpt":0.2297636481089705,"score_spread":0.2197197516337329,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4255241205","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":[0.9937525,0.000626188,0.0024717518,0.0017650066,0.00019496754,0.00026137292,0.0002391551,0.000016065036,0.00067301147],"genre_scores_gemma":[0.99627894,0.000091699054,0.0032400119,0.00015414415,0.000043611937,0.0000045932647,0.000066340486,0.000004800453,0.00011583082],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99799854,0.00026805405,0.00045854837,0.0004385102,0.00059434253,0.00024199867],"domain_scores_gemma":[0.99859625,0.00012775582,0.00040206514,0.0007222408,0.00007094974,0.00008073998],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003360887,0.00020993568,0.00044292054,1.4669654e-10,0.00019585007,0.000096776464,0.0004054866,0.00020557283,0.0032486855],"category_scores_gemma":[0.00008458309,0.00012627707,0.0002638614,0.0008796602,0.00073495915,0.00007764943,0.0012388903,0.00019108318,0.0000030974188],"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":[0.00003344564,0.00004753166,0.9785763,0.000007840296,0.0003713474,5.610583e-7,0.0001940173,0.018821554,0.000045592944,0.0003499529,0.0014044018,0.00014742264],"study_design_scores_gemma":[0.00017754275,0.000006919132,0.98461807,0.000025129475,0.0006555381,4.2363249e-7,0.00044068144,0.012184058,0.0003283977,0.0011408154,0.00029148007,0.00013092105],"about_ca_topic_score_codex":0.013664455,"about_ca_topic_score_gemma":0.002835821,"teacher_disagreement_score":0.010828635,"about_ca_system_score_codex":0.00018511075,"about_ca_system_score_gemma":0.00012509641,"threshold_uncertainty_score":0.9976625},"labels":[],"label_agreement":null},{"id":"W4255281040","doi":"10.5194/amt-2020-518-rc2","title":"Comment on amt-2020-518","year":2021,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; McGill University","funders":"Canadian Space Agency; Université de Lille; Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Radiance; Remote sensing; Environmental science; Effective radius; Meteorology; Hyperspectral imaging; Radiative transfer; Water vapor; Cloud top; Overcast; Cloud computing; Atmospheric Infrared Sounder; Convective storm detection; Storm; Computer science; Geology; Physics; Optics; Sky","score_opus":0.017770849905615435,"score_gpt":0.2685183689664801,"score_spread":0.2507475190608647,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4255281040","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00004145346,0.0059819827,0.00015745132,0.33415315,0.0014674363,0.00035837718,0.000036159705,0.000049747407,0.65775424],"genre_scores_gemma":[0.00008565677,0.009364108,0.0013463824,0.21497826,0.0002029458,0.000052329917,0.0002747694,0.00003099219,0.77366453],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9979559,0.000065374916,0.0003131125,0.0006021335,0.00072617945,0.00033728193],"domain_scores_gemma":[0.99896294,0.00004586196,0.0001271382,0.00069577486,0.00000917827,0.00015911456],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00019220034,0.0003410156,0.0004960934,3.9222485e-7,0.00009882223,0.000032567503,0.00044659057,0.00018275944,0.28300834],"category_scores_gemma":[0.000029855488,0.00026139236,0.00022321743,0.00019427024,0.000094268755,0.000027855825,0.0005357929,0.0003875625,0.008976915],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000011208971,0.000082055434,0.00008733728,0.00012876913,0.000016149826,0.00002858498,0.000008695484,0.00001355455,0.0000022123788,0.0000636592,0.9874547,0.012113148],"study_design_scores_gemma":[0.000086087326,0.000071157825,0.00020024634,0.00063832256,0.000048506092,0.0000049792116,0.000016129326,0.000019863077,0.000016210082,0.000034725723,0.9985361,0.00032763503],"about_ca_topic_score_codex":0.0007432805,"about_ca_topic_score_gemma":0.00020149472,"teacher_disagreement_score":0.27403143,"about_ca_system_score_codex":0.00028752585,"about_ca_system_score_gemma":0.000025143134,"threshold_uncertainty_score":0.99998385},"labels":[],"label_agreement":null},{"id":"W4255586627","doi":"10.5194/amt-2019-62","title":"Determination of Ice Water Content (IWC) in tropical convective clouds from X-band dual-polarization airborne radar","year":2019,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; National Research Council Canada","funders":"Environment and Climate Change Canada; National Aeronautics and Space Administration","keywords":"Ice crystals; Radar; Remote sensing; Meteorology; Environmental science; Atmospheric sciences; Geology; Physics; Engineering","score_opus":0.015565721892101784,"score_gpt":0.22103880276482618,"score_spread":0.2054730808727244,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4255586627","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":[0.9511069,0.000032376207,0.044238947,0.00018286287,0.00041474067,0.00060731947,0.000028668226,0.000026099147,0.003362066],"genre_scores_gemma":[0.9939481,0.00002200955,0.003904636,0.00014847808,0.00005386446,0.000026806967,0.0001204185,0.000023815497,0.0017518583],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99809206,0.00012740586,0.00051870197,0.00059839425,0.00040049342,0.000262948],"domain_scores_gemma":[0.9992368,0.00007988743,0.0002020568,0.00038977756,0.000023778779,0.00006767983],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00013836674,0.0002675809,0.0004463809,0.0000039257684,0.000032661843,0.000026694215,0.00023165614,0.00038474155,0.0033030452],"category_scores_gemma":[0.000032399905,0.00019858217,0.00010594589,0.00006829936,0.00017510238,0.00012236173,0.0004707551,0.0003581828,0.00019299654],"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":[0.00023927107,0.00042972885,0.8616871,0.00006923477,0.000054515524,0.000017712455,0.0030342427,0.002945733,0.124504164,0.00019458943,0.00014488731,0.006678804],"study_design_scores_gemma":[0.0010765512,0.00011953842,0.89316773,0.000067181725,0.00004805816,0.000001048238,0.00031858403,0.011721351,0.09166615,0.0012104047,0.00021511142,0.000388305],"about_ca_topic_score_codex":0.006840084,"about_ca_topic_score_gemma":0.00066818093,"teacher_disagreement_score":0.042841192,"about_ca_system_score_codex":0.0003361456,"about_ca_system_score_gemma":0.00002300941,"threshold_uncertainty_score":0.99977344},"labels":[],"label_agreement":null},{"id":"W4255863381","doi":"10.5194/acp-2020-938","title":"Forest Fire Aerosol – Weather Feedbacks over Western North America Using a High-Resolution, Fully Coupled, Air-Quality Model","year":2020,"lang":"en","type":"preprint","venue":"","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":true,"ca_institutions":"Wind Energy Institute of Canada; Environment and Climate Change Canada","funders":"","keywords":"Environmental science; Radiosonde; Aerosol; Troposphere; Air quality index; Meteorology; Plume; Atmospheric sciences; Climatology; Geography; Geology","score_opus":0.0275448629171373,"score_gpt":0.26353998561202774,"score_spread":0.23599512269489042,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4255863381","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":[0.7690968,0.000051706094,0.22746897,0.0006677591,0.00020681252,0.00060222676,0.00011495018,0.00020720245,0.0015835885],"genre_scores_gemma":[0.9679527,0.000055509565,0.02482945,0.0027949417,0.00020456736,0.00007619312,0.00013781,0.0001087618,0.003840062],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9959196,0.00009674292,0.00079956965,0.0014670981,0.00095357024,0.00076343375],"domain_scores_gemma":[0.9978618,0.000038222435,0.00055251,0.0010948834,0.0000310302,0.00042155548],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014336716,0.00075353973,0.00081500405,0.000002198926,0.00031541157,0.00011763207,0.0009138723,0.0004324128,0.003625659],"category_scores_gemma":[0.000027269385,0.00067581993,0.0003408795,0.00027807892,0.0005096044,0.00021701123,0.0030289362,0.00078338076,0.00067163835],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006663896,0.0001474755,0.18590523,0.000051676183,0.00006504381,0.000011663496,0.0004797124,0.8092547,0.00042164393,0.00002894904,0.0027332082,0.00083404215],"study_design_scores_gemma":[0.0004173362,0.0000666142,0.1027486,0.000039833503,0.00009654232,0.0000038828525,0.00010120788,0.8942316,0.000016670969,0.00050923816,0.0007913661,0.0009770592],"about_ca_topic_score_codex":0.028601203,"about_ca_topic_score_gemma":0.0055807927,"teacher_disagreement_score":0.20263952,"about_ca_system_score_codex":0.00061772525,"about_ca_system_score_gemma":0.00013349806,"threshold_uncertainty_score":0.9995693},"labels":[],"label_agreement":null},{"id":"W4255957746","doi":"10.5194/acpd-5-8285-2005","title":"An AeroCom initial assessment – optical properties in aerosol component modules of global models","year":2005,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Aerosol; AERONET; Context (archaeology); Environmental science; Radiative transfer; Atmospheric sciences; Satellite; Radiative forcing; Absorption (acoustics); Meteorology; Physics; Geography","score_opus":0.029638885979629048,"score_gpt":0.29176413957161873,"score_spread":0.2621252535919897,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4255957746","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":[0.9397277,0.000055988527,0.023525687,0.00016583448,0.00012668502,0.00062582624,0.00002364792,0.00006106831,0.035687543],"genre_scores_gemma":[0.94541615,0.000033196062,0.05412941,0.00011062306,0.00007344521,0.00010161982,0.000017398994,0.000021620586,0.000096518466],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9973449,0.00010419981,0.0006750034,0.00071930286,0.00072331954,0.0004332496],"domain_scores_gemma":[0.99898356,0.000011329337,0.00017117485,0.00062742695,0.000015286905,0.00019124817],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021645536,0.00039345038,0.0005605902,0.0000016393799,0.00005388699,0.000057731002,0.00066603575,0.00032934485,0.0011003095],"category_scores_gemma":[0.0000034958716,0.00031812894,0.0001320586,0.00009724183,0.0004243541,0.00024008624,0.0015310866,0.00042803597,0.000031085347],"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":[0.000064299704,0.0015679725,0.035238095,0.000046413166,0.00002637811,0.000011848005,0.00022886225,0.94938385,0.0031239702,0.001899449,0.0001128263,0.0082960585],"study_design_scores_gemma":[0.00081428606,0.0002756804,0.22016883,0.00014961517,0.0000408332,0.000007987846,0.00043270324,0.7707364,0.00274002,0.0037489394,0.000031505966,0.00085319753],"about_ca_topic_score_codex":0.0033750846,"about_ca_topic_score_gemma":0.0014495226,"teacher_disagreement_score":0.18493074,"about_ca_system_score_codex":0.0007380303,"about_ca_system_score_gemma":0.00007731728,"threshold_uncertainty_score":0.9999271},"labels":[],"label_agreement":null},{"id":"W4255961532","doi":"10.5194/acpd-11-885-2011","title":"Manipulating marine stratocumulus cloud amount and albedo: a process-modelling study of aerosol-cloud-precipitation interactions in response to injection of cloud condensation nuclei","year":2011,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":22,"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":"National Oceanic and Atmospheric Administration; University of Calgary; Fund for Innovative Climate and Energy Research","keywords":"Cloud condensation nuclei; Cloud albedo; Liquid water content; Aerosol; Marine stratocumulus; Precipitation; Supersaturation; Cloud computing; Liquid water path; Environmental science; Atmospheric sciences; Condensation; Sea salt aerosol; Boundary layer; Albedo (alchemy); Meteorology; Cloud cover; Physics; Mechanics; Thermodynamics","score_opus":0.03661176712808154,"score_gpt":0.29315313079407446,"score_spread":0.2565413636659929,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4255961532","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":[0.9828199,0.000006511338,0.012983776,0.000032544925,0.00048912043,0.0016628334,0.000005940351,0.000041285854,0.0019580855],"genre_scores_gemma":[0.99457985,0.000007182716,0.004834308,0.000023995512,0.00006862702,0.0001306399,0.00001146302,0.000039980892,0.00030395488],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99720174,0.00026492536,0.0010730757,0.0007400157,0.00045682388,0.00026340852],"domain_scores_gemma":[0.9985154,0.00014834663,0.00071006425,0.00043883693,0.00007916883,0.00010814791],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00079158833,0.000344143,0.00050939637,0.00002765587,0.000100307465,0.000041670217,0.0002432772,0.00017556295,0.0006903583],"category_scores_gemma":[0.00010219272,0.0003479515,0.00006732466,0.00039167792,0.000099819845,0.00023685269,0.00079866935,0.00045841053,0.0000133381345],"study_design_candidate":"simulation_or_modeling","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":[0.0018763683,0.0010394563,0.22379604,0.00015096144,0.000060894123,0.0000038338444,0.033301614,0.73044676,0.00807398,0.000094745985,0.000025598061,0.0011297277],"study_design_scores_gemma":[0.0031463117,0.0035293663,0.55636185,0.000661178,0.00027017356,0.000026864702,0.055065453,0.36895528,0.005170569,0.00530609,0.000013618534,0.0014932674],"about_ca_topic_score_codex":0.02247288,"about_ca_topic_score_gemma":0.012563541,"teacher_disagreement_score":0.3614915,"about_ca_system_score_codex":0.0002644698,"about_ca_system_score_gemma":0.00004340592,"threshold_uncertainty_score":0.99989724},"labels":[],"label_agreement":null},{"id":"W4255994268","doi":"10.5194/acp-2021-90-rc2","title":"Comment on acp-2021-90","year":2021,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Goddard Space Flight Center; European Centre for Medium-Range Weather Forecasts; Forschungszentrum Jülich; National Natural Science Foundation of China; Deutsche Forschungsgemeinschaft; Langley Research Center; National Aeronautics and Space Administration","keywords":"Mesoscale meteorology; Climatology; Thunderstorm; Middle latitudes; Convection; Atmospheric sciences; Storm; Environmental science; Geology; Geography; Meteorology","score_opus":0.0201382623075808,"score_gpt":0.27146127495665695,"score_spread":0.25132301264907614,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4255994268","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000027595162,0.0055872453,0.00017799156,0.30901217,0.0014529647,0.00034427404,0.000035449615,0.000035111094,0.6833272],"genre_scores_gemma":[0.0000572775,0.009691501,0.0013432251,0.16740936,0.00022220136,0.0000554583,0.00029078842,0.000033624172,0.82089657],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9979505,0.00006987423,0.00030713805,0.00060181605,0.0007253183,0.00034534003],"domain_scores_gemma":[0.998925,0.000048756632,0.00012453324,0.0007367277,0.000009577648,0.00015543852],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00020608712,0.00034378222,0.00049768854,5.359977e-7,0.000100266596,0.000034779063,0.00045069796,0.00019241762,0.3576749],"category_scores_gemma":[0.000033212928,0.00026225648,0.00022738159,0.00019173718,0.000089986024,0.000030864,0.0005699091,0.00039675354,0.008962759],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000001072007,0.00008634113,0.00006034778,0.00010881916,0.000016730763,0.000021962574,0.000009240273,0.000013242923,0.000003274452,0.00008046034,0.9790725,0.02052598],"study_design_scores_gemma":[0.00008625412,0.00006605349,0.00015585517,0.00066418503,0.000049095594,0.000003194103,0.00001845904,0.000017736746,0.000020416042,0.00003217343,0.9985597,0.00032685534],"about_ca_topic_score_codex":0.00073341536,"about_ca_topic_score_gemma":0.00017747804,"teacher_disagreement_score":0.34871215,"about_ca_system_score_codex":0.0002966049,"about_ca_system_score_gemma":0.000027661426,"threshold_uncertainty_score":0.99998295},"labels":[],"label_agreement":null},{"id":"W4256342353","doi":"10.5194/amt-2021-247-rc2","title":"Comment on amt-2021-247","year":2021,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Lidar; Radiosonde; Environmental science; Arctic; Meteorology; Satellite; Radar; Sampling (signal processing); Climatology; Atmospheric sciences; Remote sensing; Geography; Geology; Computer science; Telecommunications; Physics","score_opus":0.01956864716923483,"score_gpt":0.26937505930354433,"score_spread":0.24980641213430949,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4256342353","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000034158456,0.006031768,0.0001680313,0.30544332,0.0015514247,0.00036649578,0.00003786877,0.00003832316,0.68632865],"genre_scores_gemma":[0.00007372642,0.007274021,0.0013597963,0.1737843,0.00022753028,0.00005672756,0.00031056622,0.000034991794,0.8168783],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.997901,0.00007077239,0.00031774378,0.00061406364,0.0007457247,0.00035065637],"domain_scores_gemma":[0.9989095,0.00004968091,0.00012888863,0.0007424962,0.000009949379,0.00015951926],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00020682758,0.00035054437,0.00050954,5.696085e-7,0.000102819504,0.000034603276,0.0004440577,0.0001895559,0.29324657],"category_scores_gemma":[0.000031154257,0.00026883706,0.00023338983,0.00019738052,0.000095691896,0.000029020042,0.00054776453,0.00039964705,0.0085311355],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000010934814,0.00008857659,0.000088118904,0.000109585395,0.000016922173,0.000023091701,0.000009332713,0.0000140747725,0.0000031026927,0.00007010272,0.9798541,0.019721886],"study_design_scores_gemma":[0.00008787558,0.000068284826,0.00014349674,0.0006945147,0.000049980503,0.0000032741975,0.000018360732,0.000015061248,0.000027220378,0.000035561665,0.99851924,0.00033711144],"about_ca_topic_score_codex":0.00089093886,"about_ca_topic_score_gemma":0.00018089589,"teacher_disagreement_score":0.28471544,"about_ca_system_score_codex":0.00030537907,"about_ca_system_score_gemma":0.000027071379,"threshold_uncertainty_score":0.9999764},"labels":[],"label_agreement":null},{"id":"W4256387174","doi":"10.5194/amtd-6-43-2013","title":"Quantification of atmospheric visibility with dual digital cameras during daytime and nighttime","year":2013,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"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 Toronto; Chinese Academy of Sciences","keywords":"Visibility; Remote sensing; Metre; Sky; Environmental science; Daytime; Calibration; Zoom; Digital photography; Computer science; Meteorology; Optics; Photography; Geography; Mathematics; Geology; Physics; Statistics","score_opus":0.0061962721946057136,"score_gpt":0.19857026042562953,"score_spread":0.1923739882310238,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4256387174","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":[0.9873249,0.00005214613,0.0025694424,0.00007540321,0.000046814737,0.00044874108,0.0000132769555,0.000060616338,0.009408667],"genre_scores_gemma":[0.9866133,0.000022083412,0.008222501,0.000015050854,0.000022181948,0.000030526702,0.000020184614,0.000025836314,0.0050283857],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982939,0.000025800298,0.00036571035,0.0007195108,0.00035416483,0.0002409432],"domain_scores_gemma":[0.9989239,0.00002835366,0.00027006038,0.0006303448,0.000019216212,0.00012810128],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000096135205,0.00028604388,0.00034582755,4.781511e-7,0.000081030106,0.00010636734,0.00020391725,0.00016934935,0.0040386855],"category_scores_gemma":[0.0000140531265,0.00020878806,0.000059132868,0.00011521344,0.00047610636,0.00026361243,0.0008406885,0.00022494221,0.00020875965],"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":[0.00010606836,0.0003986263,0.96808296,0.00022983797,0.00012110508,0.000008696117,0.00092250644,0.010271329,0.009534759,0.00015327301,0.00065663824,0.009514211],"study_design_scores_gemma":[0.00033374445,0.000121216835,0.98573136,0.00004471519,0.000045480923,0.00001411354,0.00022281622,0.010418692,0.0018944079,0.00047005803,0.00018106426,0.0005223013],"about_ca_topic_score_codex":0.0017385896,"about_ca_topic_score_gemma":0.000044641143,"teacher_disagreement_score":0.017648442,"about_ca_system_score_codex":0.00010266198,"about_ca_system_score_gemma":0.000023858622,"threshold_uncertainty_score":0.99687177},"labels":[],"label_agreement":null},{"id":"W4280607108","doi":"10.1080/07055900.2022.2072266","title":"Development of High Resolution Cloud Cover Climatology Databank Using Merged Manual and Satellite Datasets over Ghana, West Africa","year":2022,"lang":"en","type":"article","venue":"ATMOSPHERE-OCEAN","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Satellite; Cloud cover; Cover (algebra); Remote sensing; Climatology; Cloud computing; High resolution; Geography; Meteorology; Computer science; Geology; Engineering; Aerospace engineering","score_opus":0.015581316376833007,"score_gpt":0.2389378188355596,"score_spread":0.22335650245872657,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4280607108","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":[0.99645793,0.0005154274,0.0007506582,0.000055864883,0.00028148794,0.00022719029,0.0002612711,0.00003558529,0.0014145639],"genre_scores_gemma":[0.96271986,0.00005433578,0.03605769,0.00015658006,0.000033226173,0.000005508365,0.00035400063,0.000034522738,0.00058428285],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99767196,0.00014719096,0.00053063175,0.0005996101,0.0005462012,0.0005044089],"domain_scores_gemma":[0.99902207,0.000051184994,0.0002844173,0.0004897867,0.000007314592,0.00014525537],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00043572765,0.00025655804,0.0003425295,9.560953e-7,0.00055983063,0.00002020504,0.0003730096,0.00007724722,0.008245254],"category_scores_gemma":[0.000015891092,0.00025899315,0.00004648692,0.00033369055,0.00027093518,0.00023331521,0.0014408391,0.00021678566,0.00007460099],"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":[0.0012705276,0.0015811558,0.72532856,0.00020916885,0.0005036623,0.00028279013,0.013823756,0.02405782,0.010105069,0.004356396,0.1969689,0.021512192],"study_design_scores_gemma":[0.0018584218,0.00018200799,0.16081102,0.00003029516,0.00015096247,0.00008456095,0.0029887387,0.007706938,0.00090944354,0.00029713864,0.82394356,0.001036912],"about_ca_topic_score_codex":0.00077046733,"about_ca_topic_score_gemma":0.00022092846,"teacher_disagreement_score":0.62697464,"about_ca_system_score_codex":0.00026575837,"about_ca_system_score_gemma":0.00004846275,"threshold_uncertainty_score":0.99998623},"labels":[],"label_agreement":null},{"id":"W4280617560","doi":"10.3390/atmos13050814","title":"Updated Climatology of Mesospheric Temperature Inversions Detected by Rayleigh Lidar above Observatoire de Haute Provence, France, Using a K-Mean Clustering Technique","year":2022,"lang":"en","type":"article","venue":"Atmosphere","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Lidar; Climatology; Amplitude; Rayleigh scattering; Environmental science; Inversion (geology); Atmospheric sciences; Meteorology; Geology; Remote sensing; Geography; Physics","score_opus":0.005764263662713302,"score_gpt":0.20530394790359613,"score_spread":0.19953968424088284,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4280617560","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":[0.993731,0.00033376046,0.0039069303,0.000117779055,0.00015085941,0.0007018378,0.00005273967,0.00016075649,0.0008443072],"genre_scores_gemma":[0.9349798,0.000031710206,0.06321289,0.000553792,0.000017909233,0.00015494942,0.000029568637,0.00006703217,0.00095235615],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99758357,0.00021366276,0.0004858275,0.00061664113,0.00044111148,0.0006591654],"domain_scores_gemma":[0.99885005,0.000037089914,0.00035121402,0.0005604326,0.000024426714,0.00017680546],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00025779346,0.0003433848,0.00045567032,8.213942e-7,0.00068764685,0.000025864425,0.00068469625,0.00023214803,0.0059316573],"category_scores_gemma":[0.000018862143,0.00034841915,0.00014500516,0.0012300528,0.00030397053,0.00021418625,0.00089313736,0.00060862204,0.000019224033],"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":[0.000104764054,0.00030954366,0.41096836,0.000061955725,0.00008158432,0.00009034723,0.0009643844,0.05819877,0.5144125,0.000035220844,0.013478194,0.0012943905],"study_design_scores_gemma":[0.00742451,0.0025682433,0.15555947,0.0004316833,0.0005747088,0.0013825861,0.013614531,0.4915983,0.12704264,0.00085711735,0.19347441,0.005471781],"about_ca_topic_score_codex":0.0016078867,"about_ca_topic_score_gemma":0.000111329864,"teacher_disagreement_score":0.43339956,"about_ca_system_score_codex":0.00037456167,"about_ca_system_score_gemma":0.00010019895,"threshold_uncertainty_score":0.99989676},"labels":[],"label_agreement":null},{"id":"W4281613693","doi":"10.5194/acp-2022-343-rc1","title":"Comment on acp-2022-343","year":2022,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"European Commission; National Aeronautics and Space Administration","keywords":"Radiosonde; Aerosol; Environmental science; Atmospheric sciences; Troposphere; Shortwave; Tropopause; Stratosphere; Overcast; Lidar; Radiative transfer; Moderate-resolution imaging spectroradiometer; Meteorology; Remote sensing; Satellite; Geology; Geography; Physics; Sky","score_opus":0.019422510857725436,"score_gpt":0.26838715579880756,"score_spread":0.2489646449410821,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281613693","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000034265722,0.0036374582,0.000060204595,0.30387735,0.0020979,0.00057986396,0.000090985166,0.00008409456,0.6895379],"genre_scores_gemma":[0.000055944223,0.0054019624,0.00039765597,0.2221679,0.00012477482,0.00017561596,0.0003123232,0.00004035329,0.77132344],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.997616,0.00008781504,0.00030938446,0.0005866377,0.0010407359,0.00035940963],"domain_scores_gemma":[0.9989359,0.000051398718,0.0001563214,0.00071518926,0.0000038562353,0.0001373673],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0003318674,0.00033883553,0.00043534779,8.6828146e-7,0.00021807507,0.000020001553,0.00071119965,0.00011464672,0.6614519],"category_scores_gemma":[0.000020859843,0.00026793074,0.00021229633,0.00021779248,0.00008634385,0.000030616255,0.0010429025,0.0005931325,0.005392227],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000254187,0.000097449934,0.00006804037,0.000082801205,0.000013661295,0.0000113497435,0.000012495722,0.000034191136,0.0000013093465,0.00013195889,0.98522544,0.014318746],"study_design_scores_gemma":[0.00009670263,0.0001630485,0.00010820804,0.00012314251,0.000042870226,0.000003083521,0.000023863531,0.00002239989,0.000003851063,0.000056916622,0.9990185,0.00033740755],"about_ca_topic_score_codex":0.0011258378,"about_ca_topic_score_gemma":0.00010261587,"teacher_disagreement_score":0.6560596,"about_ca_system_score_codex":0.0005767829,"about_ca_system_score_gemma":0.000020479252,"threshold_uncertainty_score":0.9999773},"labels":[],"label_agreement":null},{"id":"W4281740424","doi":"10.5281/zenodo.6592041","title":"Cloud Feedback on Earth's Long-term Climate Simulated by a Near-global Cloud-permitting Model","year":2022,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"","keywords":"Cloud computing; Term (time); Cloud feedback; Meteorology; Environmental science; Computer science; Climate model; Climatology; Climate change; Geology; Geography; Climate sensitivity; Physics; Oceanography; Operating system","score_opus":0.017476125807655625,"score_gpt":0.23255496739876239,"score_spread":0.21507884159110677,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281740424","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":[0.921709,0.000031638265,0.0014403308,0.00032598578,0.00014623044,0.000407135,0.00036628149,0.0005984922,0.074974924],"genre_scores_gemma":[0.99574226,0.00002720993,0.00019231162,0.00058737874,0.000071008995,9.5873744e-8,0.00054176437,0.0007009684,0.002137004],"study_design_codex":"simulation_or_modeling","study_design_gemma":"not_applicable","domain_scores_codex":[0.9974288,0.0003037403,0.0002909119,0.000614319,0.0007177147,0.0006445258],"domain_scores_gemma":[0.9990892,0.000015725576,0.00013640884,0.0004761161,0.000042341686,0.00024021503],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0005396846,0.00021026,0.00016942942,0.000004771687,0.004670404,0.00047232254,0.0010585504,0.000056317727,0.05365958],"category_scores_gemma":[0.00009103105,0.00022772081,0.00007680177,0.0006393824,0.00023568897,0.0001750874,0.0031138042,0.0003890373,0.0099719325],"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":[0.000878539,0.0012661213,0.002264063,0.000060234015,0.00009614161,0.00018276481,0.002161325,0.5151081,0.008527659,0.0014550774,0.3312866,0.13671336],"study_design_scores_gemma":[0.0019625844,0.0013107229,0.009119019,0.000027543552,0.00003681399,0.00021377802,0.00045302248,0.2028502,0.0002861175,0.00016235639,0.78273237,0.0008454903],"about_ca_topic_score_codex":0.000033871296,"about_ca_topic_score_gemma":6.00098e-7,"teacher_disagreement_score":0.45144576,"about_ca_system_score_codex":0.000441819,"about_ca_system_score_gemma":0.000003437082,"threshold_uncertainty_score":0.99662536},"labels":[],"label_agreement":null},{"id":"W4281778576","doi":"10.5194/amt-2022-153","title":"The Microfluidic Ice Nuclei Counter Zürich (MINCZ): A platform for homogeneous and heterogeneous ice nucleation","year":2022,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"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; Eidgenössische Technische Hochschule Zürich","keywords":"Ice nucleus; Nucleation; Microfluidics; Polydimethylsiloxane; Materials science; Freezing point; Homogeneous; Chemical physics; Thermal; Nanotechnology; Chemical engineering; Mechanics; Chemistry; Thermodynamics; Physics","score_opus":0.011808209678906445,"score_gpt":0.23075477851122497,"score_spread":0.21894656883231853,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281778576","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":[0.9824105,0.002448327,0.003613477,0.00041790796,0.0006321887,0.0014008941,0.00007724534,0.000110206296,0.008889289],"genre_scores_gemma":[0.9815947,0.0025815547,0.0024443544,0.001387344,0.00015000899,0.0005201903,0.0000668245,0.00010431382,0.011150701],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9979045,0.000037354574,0.0003902628,0.00076710066,0.0004199119,0.00048090718],"domain_scores_gemma":[0.9988656,0.00014206841,0.00022123246,0.00062971225,0.000016383085,0.00012499459],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003492312,0.0003713843,0.00027824863,0.0000021961425,0.0010253771,0.0002331121,0.00066318037,0.00021330254,0.0036246215],"category_scores_gemma":[0.000022276374,0.00027724373,0.00016758074,0.00009505808,0.00025864397,0.00007483815,0.0021548402,0.00034503857,0.00010159703],"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":[0.0020870375,0.0012351646,0.030258542,0.00071001006,0.0013183162,0.00019965712,0.014124041,0.027962023,0.037593704,0.0012481154,0.36406967,0.5191937],"study_design_scores_gemma":[0.0008241367,0.00042286207,0.004350369,0.000023911161,0.00019758238,0.00016447483,0.0014276846,0.018617362,0.0014845371,0.002038348,0.9693349,0.0011138238],"about_ca_topic_score_codex":0.0010626994,"about_ca_topic_score_gemma":0.00021598297,"teacher_disagreement_score":0.6052652,"about_ca_system_score_codex":0.0004328537,"about_ca_system_score_gemma":0.000031515916,"threshold_uncertainty_score":0.999968},"labels":[],"label_agreement":null},{"id":"W4281784600","doi":"10.5194/amt-2022-174","title":"Sizing ice hydrometeor populations using dual-wavelength radar ratio","year":2022,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"National Research Council Canada; Environment and Climate Change Canada","funders":"National Oceanic and Atmospheric Administration; Federal Aviation Administration; U.S. Department of Energy","keywords":"Radar; Remote sensing; Environmental science; Rayleigh scattering; Optics; Wavelength; Meteorology; Physics; Geology; Aerospace engineering","score_opus":0.048150773696016606,"score_gpt":0.2817739015900451,"score_spread":0.2336231278940285,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281784600","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":[0.93232304,0.00007604812,0.021365212,0.00031675983,0.00088358467,0.0004854923,0.000026047206,0.00016270144,0.044361096],"genre_scores_gemma":[0.8767987,0.000021783851,0.11483472,0.00031296283,0.00011739085,0.00003988568,0.00006720706,0.00004964613,0.007757744],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9978085,0.00010505812,0.00041994388,0.00070054026,0.00059304846,0.0003729094],"domain_scores_gemma":[0.9989619,0.00003842433,0.00024059006,0.00062216463,0.000005954931,0.00013095982],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00027339003,0.0003142341,0.00030649547,0.000003408378,0.0005770401,0.000089037545,0.00034807273,0.00016091274,0.05125606],"category_scores_gemma":[0.0000321195,0.00031200564,0.00016690337,0.00029067224,0.00010219221,0.00014265625,0.002675747,0.0005913941,0.00017341872],"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":[0.000031339445,0.0005148769,0.066742696,0.00010107758,0.00017948043,0.00012594432,0.0029622985,0.8729379,0.020474693,0.004513973,0.008008764,0.023406914],"study_design_scores_gemma":[0.00097041257,0.00018766239,0.12874688,0.00008443995,0.0004563555,0.000092714465,0.0031833162,0.7983135,0.0008372951,0.014844286,0.04859606,0.0036871005],"about_ca_topic_score_codex":0.0045765736,"about_ca_topic_score_gemma":0.00019934648,"teacher_disagreement_score":0.09346951,"about_ca_system_score_codex":0.0006666437,"about_ca_system_score_gemma":0.000051899493,"threshold_uncertainty_score":0.9999332},"labels":[],"label_agreement":null},{"id":"W4281921892","doi":"10.1364/ao.458566","title":"Polarimetric multiple scattering LiDAR model based on Poisson distribution","year":2022,"lang":"en","type":"article","venue":"Applied Optics","topic":"Atmospheric aerosols and clouds","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":"Defence Research and Development Canada","funders":"","keywords":"Lidar; Scattering; Optics; Remote sensing; Polarimetry; Poisson distribution; Physics; Monte Carlo method; Mie scattering; Aerosol; SIGNAL (programming language); Range (aeronautics); Forward scatter; Backscatter (email); Photon counting; Atmospheric optics; Field of view; Light scattering; Photon; Materials science; Meteorology; Geology; Computer science; Statistics","score_opus":0.008239178666373,"score_gpt":0.1964063364274909,"score_spread":0.1881671577611179,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281921892","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":[0.8718462,0.000006097132,0.11387121,0.00019689575,0.000077497934,0.00023395366,0.00006769397,0.00007921467,0.013621256],"genre_scores_gemma":[0.98868924,0.0000011844622,0.010303502,0.0006132947,0.00001985173,0.00004781929,0.000090223635,0.000020351094,0.00021454366],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9989161,0.0000130890885,0.00013561855,0.0002736026,0.00039792716,0.00026368917],"domain_scores_gemma":[0.9995444,0.00004782195,0.000060977854,0.00026627272,0.000002374848,0.00007816758],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014438857,0.00012425364,0.00010063434,0.000002294968,0.0003864488,0.000022062004,0.00022176225,0.00003723639,0.0006075299],"category_scores_gemma":[0.000015737545,0.00013002471,0.000042527092,0.00039438967,0.000052146457,0.000030238847,0.00026965045,0.00019987383,0.0001430154],"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":[0.000054441367,0.00018343027,0.010015198,0.000002399156,0.0000033221277,0.0000024921571,0.0000532443,0.97567666,0.008695709,0.00089358503,0.0007388985,0.0036806273],"study_design_scores_gemma":[0.00044929326,0.00011797491,0.01547898,0.0000015310319,0.000012984322,0.0000010548688,0.00009415664,0.9795175,0.0016596912,0.0002523828,0.0021814138,0.00023301863],"about_ca_topic_score_codex":0.00009107598,"about_ca_topic_score_gemma":0.0000036261251,"teacher_disagreement_score":0.11684305,"about_ca_system_score_codex":0.000353758,"about_ca_system_score_gemma":0.000011029,"threshold_uncertainty_score":0.6652027},"labels":[],"label_agreement":null},{"id":"W4281922687","doi":"10.5194/acp-2022-343","title":"Self-lofting of wildfire smoke in the troposphere and stratosphere caused by radiative heating: simulations vs space lidar observations","year":2022,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","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":"European Commission","keywords":"Troposphere; Stratosphere; Environmental science; Atmospheric sciences; Aerosol; Radiosonde; Tropopause; Overcast; Shortwave; Lidar; Radiative transfer; Cirrus; Cloud cover; Smoke; Meteorology; Climatology; Remote sensing; Geology; Sky; Physics","score_opus":0.017859142851172034,"score_gpt":0.2479053222852075,"score_spread":0.23004617943403546,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281922687","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":[0.9871063,0.00026463688,0.00052797835,0.0012625315,0.000061066305,0.0008089247,0.00009217124,0.00005635554,0.009819986],"genre_scores_gemma":[0.98888636,0.00008113389,0.0097310925,0.00030154758,0.00002216903,0.00007601136,0.00007225317,0.000030038484,0.00079939136],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99795914,0.00023095333,0.00048297888,0.00054554566,0.0004870936,0.00029427375],"domain_scores_gemma":[0.99875885,0.00032926985,0.00033842633,0.0004915138,0.000009001741,0.000072911214],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002853399,0.0003049618,0.00035434135,0.000001502612,0.00036548873,0.00006901519,0.00043243007,0.00017176318,0.0034716253],"category_scores_gemma":[0.000059016507,0.00024648645,0.000087232314,0.00042964434,0.00017977037,0.00013387587,0.000713808,0.0006895362,0.0000030775955],"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":[0.000008115027,0.00020242287,0.8684655,0.000040384508,0.000042943826,0.0000034708544,0.007073291,0.12184996,0.0001506104,0.0004493689,0.0014191823,0.00029475367],"study_design_scores_gemma":[0.0007170546,0.00020100884,0.8566043,0.000052951622,0.0001006596,0.0000016801494,0.01909925,0.116563484,0.00009865562,0.001294397,0.004647021,0.0006195635],"about_ca_topic_score_codex":0.007827724,"about_ca_topic_score_gemma":0.0018227138,"teacher_disagreement_score":0.01202596,"about_ca_system_score_codex":0.0002473139,"about_ca_system_score_gemma":0.00007502065,"threshold_uncertainty_score":0.99999875},"labels":[],"label_agreement":null},{"id":"W4283330440","doi":"10.3390/rs14132978","title":"A Coupled Evaluation of Operational MODIS and Model Aerosol Products for Maritime Environments Using Sun Photometry: Evaluation of the Fine and Coarse Mode","year":2022,"lang":"en","type":"article","venue":"Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":24,"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 de Sherbrooke","funders":"U.S. Naval Research Laboratory; Office of Naval Research; National Aeronautics and Space Administration","keywords":"AERONET; Environmental science; Aerosol; Mode (computer interface); Remote sensing; Satellite; Climatology; Radiometer; Ocean color; Meteorology; Sun photometer; Atmospheric sciences; Geography; Geology; Computer science; Physics","score_opus":0.04238801777314766,"score_gpt":0.28651219361921154,"score_spread":0.24412417584606388,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283330440","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":[0.97338885,0.00007929987,0.025374815,0.00009717175,0.000037209895,0.0009496298,0.000021327245,0.0000022812292,0.000049390666],"genre_scores_gemma":[0.9750772,0.0000048590987,0.02479006,0.0000357121,0.000011347669,8.8598506e-7,0.000012028253,0.000012873995,0.00005500732],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99822605,0.00014905672,0.00021643243,0.00026581655,0.0010218332,0.000120786615],"domain_scores_gemma":[0.99955624,0.000034121513,0.00016667556,0.00018196755,0.00003621739,0.000024756962],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014178529,0.000097259006,0.00013818381,0.0000038292897,0.00026689656,0.000009650183,0.00005563191,0.000029724708,0.000045681812],"category_scores_gemma":[0.00014364684,0.00008638632,0.000027089842,0.00015401955,0.00013996141,0.000091561815,0.0001887384,0.000060763887,1.2328289e-7],"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":[0.000020896248,0.0000190033,0.00014485096,0.00000614167,0.000008442821,4.0104098e-8,0.00025056963,0.5834634,0.40598682,0.0000027575,0.0000079960555,0.010089128],"study_design_scores_gemma":[0.0007212676,0.000031866697,0.00078130333,0.000012180869,0.00016728793,0.0000089156265,0.000090590904,0.9777658,0.019542877,0.00078696304,0.000004049261,0.000086917506],"about_ca_topic_score_codex":0.00032235793,"about_ca_topic_score_gemma":0.0000333892,"teacher_disagreement_score":0.39430243,"about_ca_system_score_codex":0.0002573409,"about_ca_system_score_gemma":0.000067420755,"threshold_uncertainty_score":0.3522732},"labels":[],"label_agreement":null},{"id":"W4283383536","doi":"10.5194/essd-2022-158","title":"The polar mesospheric cloud dataset of the Balloon Lidar Experiment BOLIDE","year":2022,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"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":"National Aeronautics and Space Administration","keywords":"Lidar; Remote sensing; Physics; Geology; Meteorology; Environmental science","score_opus":0.009689386300003133,"score_gpt":0.23919002339553702,"score_spread":0.2295006370955339,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283383536","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":[0.89354134,0.003785524,0.0010636604,0.0030886312,0.004688961,0.0022217147,0.0017992026,0.00012009784,0.08969085],"genre_scores_gemma":[0.9774647,0.0006027378,0.004454549,0.0013799252,0.00020060211,0.00029260907,0.00034508097,0.0000746265,0.015185222],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99746555,0.0002256871,0.00049138407,0.00055270345,0.00088402483,0.00038063302],"domain_scores_gemma":[0.99753255,0.00007089889,0.00037633153,0.0019247071,0.000005183776,0.000090307585],"candidate_categories":["open_science","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005418697,0.0003096171,0.00027476915,3.9319528e-7,0.0005735332,0.00006293124,0.0023326278,0.0001228577,0.029179676],"category_scores_gemma":[0.000027454531,0.0001638121,0.0002195782,0.00018498358,0.00044732937,0.00004321798,0.00953784,0.0006169733,0.000119185635],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011156637,0.0006228953,0.066616185,0.00005702527,0.00030113448,0.000015407813,0.0024524326,0.01595415,0.0059086527,0.002684155,0.8953793,0.009897093],"study_design_scores_gemma":[0.00018433713,0.00006778781,0.023698702,0.000013653917,0.000060439637,0.000003824614,0.00201323,0.0006369964,0.0033393719,0.00077768957,0.96880555,0.0003984425],"about_ca_topic_score_codex":0.005294522,"about_ca_topic_score_gemma":0.00021008558,"teacher_disagreement_score":0.08392329,"about_ca_system_score_codex":0.00030128643,"about_ca_system_score_gemma":0.00005900952,"threshold_uncertainty_score":0.9984728},"labels":[],"label_agreement":null},{"id":"W4283573824","doi":"10.5194/egusphere-2022-491","title":"Observation of secondary ice production in clouds at low temperatures","year":2022,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada; Environment and Climate Change Canada","funders":"Federal Aviation Administration; Environment and Climate Change Canada; National Science Foundation","keywords":"Ice nucleus; Clear ice; Environmental science; Precipitation; Atmosphere (unit); Atmospheric sciences; Hard rime; Ice formation; Climatology; Ice crystals; Cryosphere; Nucleation; Meteorology; Geology; Sea ice; Antarctic sea ice; Chemistry; Geography","score_opus":0.01272055554615727,"score_gpt":0.2275176725167478,"score_spread":0.2147971169705905,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283573824","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":[0.9867745,0.00009966351,0.0000191619,0.00032668817,0.0006997923,0.00038396433,0.000010111998,0.00003375256,0.011652367],"genre_scores_gemma":[0.9750672,0.00007671786,0.0022474278,0.000194156,0.00006425737,0.00008115302,0.00008637638,0.000018209807,0.02216452],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985396,0.0000728711,0.0003351775,0.0005269011,0.00035971825,0.00016568069],"domain_scores_gemma":[0.9993204,0.000014878651,0.0001918666,0.00043116967,0.000007126469,0.000034548524],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002823813,0.00017463956,0.00022038624,0.0000020707093,0.000080996884,0.000011646898,0.00027925833,0.00013222694,0.025120687],"category_scores_gemma":[0.000028206176,0.00016349921,0.00007131875,0.00022304604,0.000094840885,0.00008578093,0.0015008482,0.0004949553,0.000035771627],"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":[0.0001119809,0.00034987245,0.79093933,0.0002806073,0.00002667855,0.000010992603,0.0021749288,0.12210592,0.049097333,0.00010983117,0.02829642,0.006496089],"study_design_scores_gemma":[0.00021389103,0.000064071224,0.9777945,0.0000428791,0.000013829118,0.000004313668,0.0005406549,0.0008199313,0.011442075,0.0006761328,0.008002674,0.00038503556],"about_ca_topic_score_codex":0.0017267289,"about_ca_topic_score_gemma":0.00073208177,"teacher_disagreement_score":0.18685517,"about_ca_system_score_codex":0.000530683,"about_ca_system_score_gemma":0.000037407808,"threshold_uncertainty_score":0.9757705},"labels":[],"label_agreement":null},{"id":"W4283642295","doi":"10.5194/ems2022-669","title":"A L1 transformational operator for the objective evaluation of the EarthCARE Cloud Profiling Radar data products","year":2022,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"","keywords":"Remote sensing; Cloud computing; Satellite; Radar; Environmental science; Meteorology; Computer science; Engineering; Aerospace engineering; Geology; Geography; Telecommunications","score_opus":0.07124786203811327,"score_gpt":0.30795175702829125,"score_spread":0.23670389499017797,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283642295","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":[0.9482566,0.00081179215,0.012323403,0.0070032952,0.002648184,0.0146999555,0.0016752429,0.000055920224,0.012525594],"genre_scores_gemma":[0.9910094,0.000021264907,0.007059426,0.00017289167,0.00016444485,0.00069623615,0.00026035853,0.000018236256,0.0005977314],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9975178,0.00020458025,0.00029699758,0.0004836644,0.001339979,0.00015694424],"domain_scores_gemma":[0.99849206,0.00008163411,0.0001769842,0.0011473711,0.00008042683,0.000021529528],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0021092917,0.00016057646,0.00015029119,8.26124e-7,0.000416435,0.000033118307,0.001313544,0.0000713046,0.0027472293],"category_scores_gemma":[0.00020032573,0.000086454944,0.00008385218,0.0001730919,0.00015379325,0.00013338095,0.0017540772,0.00031880834,0.000004832553],"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":[0.000460102,0.00068454474,0.027748076,0.00070882705,0.0008757725,5.38416e-7,0.027160779,0.7767172,0.010714763,0.005482833,0.02703536,0.1224112],"study_design_scores_gemma":[0.0019651304,0.00019812632,0.084743656,0.00010326627,0.0011391421,0.000008566774,0.020107284,0.82237494,0.027662635,0.004433842,0.036226396,0.0010369928],"about_ca_topic_score_codex":0.00020169621,"about_ca_topic_score_gemma":0.00009573062,"teacher_disagreement_score":0.121374205,"about_ca_system_score_codex":0.00020398879,"about_ca_system_score_gemma":0.00037939064,"threshold_uncertainty_score":0.9981644},"labels":[],"label_agreement":null},{"id":"W4285230689","doi":"10.1039/9781839161186-00191","title":"Evaporation and Precipitation Dynamics of a Respiratory Droplet","year":2022,"lang":"en","type":"book-chapter","venue":"","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Evaporation; Precipitation; Respiratory system; Environmental science; Dynamics (music); Atmospheric sciences; Meteorology; Physics; Biology; Anatomy; Acoustics","score_opus":0.010920754612388022,"score_gpt":0.20983693632883338,"score_spread":0.19891618171644534,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4285230689","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.010838209,0.00006687805,0.0006526091,0.000067675915,0.00006479166,0.00020445387,0.000020447618,0.000018590588,0.9880663],"genre_scores_gemma":[0.13395816,0.00014793534,0.0020372237,0.00034418175,0.000040817627,0.000022923981,0.00013123185,0.000055164925,0.86326236],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.9992556,0.000010571069,0.00019348787,0.00021139458,0.00026332965,0.00006563985],"domain_scores_gemma":[0.9996155,0.00001807456,0.00017648363,0.00015188199,0.000005335257,0.000032709082],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000112465925,0.00011290631,0.0001307416,0.0000014569938,0.000058991307,0.000006365705,0.000073381074,0.000091592134,0.026394702],"category_scores_gemma":[0.000005223815,0.00010850373,0.000033382064,0.00001985227,0.00012360296,0.000076545904,0.00015677391,0.0001065956,0.000038854956],"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":[0.00008031966,0.00007265076,0.012192456,0.00008828506,0.00007115918,0.000012156155,0.001020468,0.0015542646,0.0008728055,0.84354436,0.014588647,0.12590244],"study_design_scores_gemma":[0.0007219331,0.0013165135,0.016734513,0.000048117465,0.00016535672,0.000008662273,0.00035142273,0.012093976,0.000065364016,0.06642369,0.9009362,0.0011342712],"about_ca_topic_score_codex":0.000105838044,"about_ca_topic_score_gemma":0.00036983818,"teacher_disagreement_score":0.88634753,"about_ca_system_score_codex":0.00016582613,"about_ca_system_score_gemma":0.000012123678,"threshold_uncertainty_score":0.9744953},"labels":[],"label_agreement":null},{"id":"W4285586975","doi":"10.5194/acp-2022-42-ac1","title":"Response to reviewers' comments","year":2022,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"National Natural Science Foundation of China; National Aeronautics and Space Administration","keywords":"Environmental science; Arctic; Aerosol; Albedo (alchemy); Snow; Climatology; Atmospheric sciences; The arctic; Range (aeronautics); Physical geography; Meteorology; Geography; Oceanography; Geology","score_opus":0.020290466709970312,"score_gpt":0.2954593012470983,"score_spread":0.275168834537128,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4285586975","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00025197476,0.02838573,0.00024376619,0.4618204,0.00367483,0.002387031,0.0002012356,0.00014625888,0.5028888],"genre_scores_gemma":[0.000025487494,0.0060148695,0.001854855,0.15691762,0.000049373055,0.0002573953,0.000108383836,0.000038543843,0.8347335],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9973134,0.000334121,0.00040756885,0.0005989413,0.0009748365,0.00037116965],"domain_scores_gemma":[0.9986283,0.00009011346,0.00014539025,0.0008843314,0.000009003185,0.00024284529],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0013931644,0.00032058705,0.0005547438,0.0000013438863,0.00018683195,0.000019433857,0.00086678326,0.00008980205,0.5486774],"category_scores_gemma":[0.00024380043,0.00026653422,0.00020261413,0.00043521696,0.00005482007,0.00003988479,0.0016699741,0.0003682876,0.010562187],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002751046,0.000037029404,0.00010627757,0.00012747014,0.000011310443,0.000011823188,0.000022481772,0.000011352529,0.0000067707915,0.0000024880194,0.98861533,0.011020167],"study_design_scores_gemma":[0.000078189216,0.00012389776,0.0003812728,0.00038251802,0.00005725169,0.000004983204,0.00001321994,0.0000024003268,0.0000012192254,0.000007769248,0.9986061,0.0003411915],"about_ca_topic_score_codex":0.0006355625,"about_ca_topic_score_gemma":0.00007078107,"teacher_disagreement_score":0.5381152,"about_ca_system_score_codex":0.0005727672,"about_ca_system_score_gemma":0.000033009117,"threshold_uncertainty_score":0.99997866},"labels":[],"label_agreement":null},{"id":"W4285800457","doi":"10.3390/rs14143449","title":"Numerical Modeling of the Ash Cloud Movement from the Catastrophic Eruption of the Sheveluch Volcano in November 1964","year":2022,"lang":"en","type":"article","venue":"Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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":"Pyroclastic rock; Geology; Volcano; Explosive eruption; Volcanic ash; Seismology","score_opus":0.010551455278788114,"score_gpt":0.2021750997942304,"score_spread":0.19162364451544228,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4285800457","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":[0.9914729,0.000039144667,0.0063971644,0.0009451263,0.0002639533,0.00018607048,0.000009713565,0.000004187855,0.0006817263],"genre_scores_gemma":[0.9975695,0.00000440125,0.0017101297,0.0005883749,0.00004563733,8.3367155e-8,0.0000014032407,0.000012062852,0.0000683978],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99864566,0.00017756298,0.0002763298,0.00019977738,0.00051614,0.00018453671],"domain_scores_gemma":[0.99932724,0.000044291097,0.00015727752,0.0004442708,0.0000067140395,0.000020183528],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027656835,0.000099751975,0.00013134857,8.9957257e-7,0.00023425756,0.0000073725655,0.00031802384,0.000027980654,0.00017224347],"category_scores_gemma":[0.000024559695,0.00005605002,0.00009310114,0.0003487267,0.0001180437,0.000020655012,0.0005868047,0.0002659597,0.0000036980005],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019225783,0.00003073866,0.008078968,0.0000024267897,0.000010213714,0.0000011320685,0.0013871839,0.9151814,0.055938806,0.000014246326,0.00009773079,0.019237936],"study_design_scores_gemma":[0.00018154265,0.000015604744,0.026661333,0.000028662349,0.000015185746,0.0000031633504,0.00084353815,0.9692976,0.0017450196,0.00086633285,0.0002593335,0.000082710285],"about_ca_topic_score_codex":0.015660426,"about_ca_topic_score_gemma":0.00038259226,"teacher_disagreement_score":0.054193784,"about_ca_system_score_codex":0.00022824385,"about_ca_system_score_gemma":0.00002615542,"threshold_uncertainty_score":0.9908944},"labels":[],"label_agreement":null},{"id":"W4286631882","doi":"10.3389/frsen.2022.904505","title":"Effect of Spectral Variability of Aerosol Optical Properties on Direct Aerosol Radiative Effect","year":2022,"lang":"en","type":"article","venue":"Frontiers in Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"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":"Langley Research Center; National Aeronautics and Space Administration","keywords":"Aerosol; Radiance; Lidar; Environmental science; Radiative transfer; Single-scattering albedo; Angstrom exponent; Remote sensing; Atmospheric sciences; Irradiance; Shortwave; Wavelength; AERONET; Atmosphere (unit); Optical depth; Spectrometer; Atmospheric radiative transfer codes; Meteorology; Optics; Physics; Geology","score_opus":0.005017070541973634,"score_gpt":0.20728755758117176,"score_spread":0.20227048703919812,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4286631882","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":[0.9851068,0.00005768728,0.003911672,0.00004228394,0.0005878493,0.0006701747,0.0000060422663,0.000028586686,0.0095889075],"genre_scores_gemma":[0.9881014,0.000005597478,0.011688825,0.00002911923,0.000027853803,0.0000012765713,0.0000018838365,0.000025592066,0.00011840547],"study_design_codex":"design_other","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9971406,0.001078153,0.00039346353,0.00046557636,0.00053575984,0.00038645786],"domain_scores_gemma":[0.9990646,0.00029616265,0.00017742971,0.00038010228,0.0000061933024,0.000075491276],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015252758,0.00024673852,0.0006396564,0.000007786926,0.00014390318,0.000008630401,0.00019221818,0.0000749604,0.00010080999],"category_scores_gemma":[0.0003264282,0.00020143925,0.00016641576,0.00040009603,0.0004704727,0.00006460996,0.00024384659,0.00037714123,0.0000045579714],"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":[0.0061772275,0.0003786025,0.19323212,0.00041308947,0.00019815336,0.00011522044,0.0042427,0.15747342,0.19025832,0.0000115186,0.0022434902,0.44525614],"study_design_scores_gemma":[0.0021610507,0.005734023,0.01084975,0.00015134345,0.00010704903,0.000017730974,0.0003279568,0.21174343,0.76816714,0.00010014887,0.000074077,0.0005663127],"about_ca_topic_score_codex":0.00053103175,"about_ca_topic_score_gemma":0.000010305024,"teacher_disagreement_score":0.5779088,"about_ca_system_score_codex":0.0005485869,"about_ca_system_score_gemma":0.000019955027,"threshold_uncertainty_score":0.8214454},"labels":[],"label_agreement":null},{"id":"W4287115850","doi":"10.5281/zenodo.4901479","title":"GEM-MACH, Feedback-DMS","year":2021,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"","keywords":"Mach number; Aerospace engineering; Computer science; Environmental science; Aeronautics; Mechanics; Physics; Engineering","score_opus":0.0186461332239018,"score_gpt":0.21754117761669767,"score_spread":0.19889504439279587,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4287115850","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.20202412,0.000084028135,0.004956647,0.001225949,0.00012996537,0.000194792,0.00004220149,0.0005758019,0.7907665],"genre_scores_gemma":[0.9841127,0.00008946097,0.001327066,0.0005591103,0.000113443195,2.5223853e-8,0.00038012443,0.00089788757,0.012520222],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9986019,0.00015481414,0.0001603318,0.00039319546,0.00035714434,0.00033257733],"domain_scores_gemma":[0.9992903,0.0000101113255,0.00005272135,0.00040022057,0.00007090687,0.00017576756],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00024775692,0.00011037383,0.000101807724,0.0000033834726,0.0014388477,0.0003536191,0.000596714,0.00005054577,0.20798178],"category_scores_gemma":[0.00019177285,0.0001136936,0.000049261205,0.00048733086,0.00019143484,0.00018000991,0.0016091933,0.00017636592,0.044538345],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003381245,0.0002836559,0.00027084764,0.000022952048,0.00003567012,0.000104202234,0.001274435,0.0005272743,0.031009266,0.0024224522,0.6507779,0.31323752],"study_design_scores_gemma":[0.00025423086,0.00006456497,0.0059083044,0.000006601151,0.00000706386,0.000101393445,0.00031152385,0.0003322032,0.0011280108,0.0001830467,0.9915537,0.00014933922],"about_ca_topic_score_codex":0.000026939992,"about_ca_topic_score_gemma":8.506769e-7,"teacher_disagreement_score":0.7820885,"about_ca_system_score_codex":0.00015265268,"about_ca_system_score_gemma":0.0000017503826,"threshold_uncertainty_score":0.9998611},"labels":[],"label_agreement":null},{"id":"W4288721293","doi":"10.3390/rs14153619","title":"Retrieval of Aged Biomass-Burning Aerosol Properties by Using GRASP Code in Synergy with Polarized Micro-Pulse Lidar and Sun/Sky Photometer","year":2022,"lang":"en","type":"article","venue":"Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":6,"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":"Universidad de Valladolid; Horizon 2020 Framework Programme; Ministerio de Ciencia e Innovación; European Commission; National Aeronautics and Space Administration","keywords":"Lidar; AERONET; Environmental science; Remote sensing; Aerosol; Sun photometer; Backscatter (email); Radiative transfer; Photometer; Extinction (optical mineralogy); Sky; Optics; Materials science; Atmospheric sciences; Meteorology; Geology; Physics; Computer science","score_opus":0.01276471898393495,"score_gpt":0.21202721608476136,"score_spread":0.1992624971008264,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4288721293","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":[0.9975676,0.0003012107,0.0016115777,0.0000509714,0.000049348426,0.00021142981,0.000007595022,0.00002672203,0.00017354314],"genre_scores_gemma":[0.9868778,0.000015083094,0.0127637945,0.00010150834,0.000010816317,4.661784e-8,0.000004080766,0.00003835441,0.00018849074],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99836653,0.00017039078,0.0003057506,0.00039378632,0.0003950406,0.0003685117],"domain_scores_gemma":[0.9994859,0.000033343527,0.00018106893,0.00021234863,0.000009253909,0.000078092344],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034062797,0.00019937933,0.00030845156,0.000010337996,0.00031266877,0.000039635474,0.00011073154,0.0000593803,0.0000928595],"category_scores_gemma":[0.000030236046,0.00017237672,0.000043364915,0.00059389934,0.00028091707,0.0001226175,0.0003057043,0.00025182482,0.000001407441],"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":[0.00023566253,0.000021995773,0.005758803,0.000015879263,0.000015132133,0.00004935047,0.00083743135,0.000410695,0.9895862,7.9313985e-8,0.000008244102,0.0030605632],"study_design_scores_gemma":[0.002610933,0.00047580976,0.0058802906,0.00024757368,0.00008143718,0.0004614424,0.002305651,0.12704584,0.8596815,0.000018251732,0.00035091405,0.0008403569],"about_ca_topic_score_codex":0.0050340476,"about_ca_topic_score_gemma":0.00015974505,"teacher_disagreement_score":0.12990467,"about_ca_system_score_codex":0.00026427073,"about_ca_system_score_gemma":0.000025925674,"threshold_uncertainty_score":0.76100075},"labels":[],"label_agreement":null},{"id":"W4289204373","doi":"10.3390/rs14153668","title":"Evaluation of CanESM Cloudiness, Cloud Type and Cloud Radiative Forcing Climatologies Using the CALIPSO-GOCCP and CERES Datasets","year":2022,"lang":"en","type":"article","venue":"Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Impact; Barrie Urology Group; Environment and Climate Change Canada","funders":"","keywords":"Environmental science; Cloud forcing; Longwave; Shortwave; Cloud feedback; Atmospheric sciences; Forcing (mathematics); Radiative forcing; Climatology; Climate model; Latitude; Satellite; Cloud cover; Cloud fraction; Radiative transfer; Cloud computing; Meteorology; Climate change; Climate sensitivity; Physics; Geography; Geology; Computer science; Geodesy","score_opus":0.04136171760302283,"score_gpt":0.2886569928608376,"score_spread":0.2472952752578148,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4289204373","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":[0.9973066,0.00081471266,0.00076060684,0.00017880676,0.00036375166,0.00022585709,0.000020471867,0.000014712355,0.00031451622],"genre_scores_gemma":[0.99729925,0.00006939342,0.0024091783,0.000112437665,0.00007179655,5.819907e-8,0.00001423669,0.000013303658,0.0000103328675],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.998493,0.00034787043,0.00019854918,0.00026293815,0.0004930476,0.00020458663],"domain_scores_gemma":[0.9994038,0.00012339168,0.0001781271,0.00022645429,0.000029012917,0.000039230006],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011182992,0.00012501238,0.00017778826,0.0000027794222,0.00058090955,0.000023605795,0.00009088681,0.00003600991,0.00007083051],"category_scores_gemma":[0.00017115408,0.00009807804,0.0000200077,0.00026884428,0.00028694668,0.00008014367,0.00047583578,0.00014498571,0.0000011658124],"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":[0.00032860678,0.000068914764,0.0471913,0.0001060863,0.00030283988,0.00007203247,0.01722897,0.4650367,0.041014675,0.00033624572,0.006298245,0.4220154],"study_design_scores_gemma":[0.00035574025,0.0000507726,0.00448146,0.000022927265,0.00020632242,0.00016791519,0.0047659758,0.9871615,0.00049161114,0.0010955242,0.0010206274,0.0001795849],"about_ca_topic_score_codex":0.0037475564,"about_ca_topic_score_gemma":0.0002812194,"teacher_disagreement_score":0.5221248,"about_ca_system_score_codex":0.0001763882,"about_ca_system_score_gemma":0.000044491386,"threshold_uncertainty_score":0.5665209},"labels":[],"label_agreement":null},{"id":"W4289523602","doi":"10.1175/jas-d-22-0008.1","title":"Dependence of Ice Crystal Size Distributions in High Ice Water Content Conditions on Environmental Conditions: Results from the HAIC-HIWC Cayenne Campaign","year":2022,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada; Environment and Climate Change Canada","funders":"National Science Foundation of Sri Lanka; National Science Foundation","keywords":"Ice crystals; Mesoscale meteorology; Atmospheric sciences; Materials science; Environmental science; Physics; Meteorology","score_opus":0.014835769759476954,"score_gpt":0.2187522797270542,"score_spread":0.20391650996757724,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4289523602","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":[0.9932989,0.00010372756,0.000084282496,0.0047548288,0.0005933846,0.00025872205,0.000536995,0.0000068973613,0.00036226492],"genre_scores_gemma":[0.99801284,0.000040677398,0.00071875344,0.0007012002,0.000054537744,0.000023463354,0.000011217105,0.000008721174,0.0004285612],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9967983,0.00040847974,0.0007928926,0.00032804016,0.0012809403,0.0003913582],"domain_scores_gemma":[0.9977657,0.0010120563,0.0007165995,0.00038469728,0.000016710967,0.00010419981],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012753538,0.00019184602,0.00028143128,0.0000011955123,0.0013342627,0.000054461172,0.0015035642,0.0000437379,0.004215432],"category_scores_gemma":[0.00033356113,0.000100362886,0.00019874844,0.00054634863,0.0014650219,0.00034183668,0.0005707012,0.00045794673,0.00002880252],"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":[0.0004703314,0.0014984972,0.18434396,0.0000036252516,0.00011533423,0.00007965529,0.0054002036,0.62879425,0.16696955,0.0006851704,0.011313572,0.00032582707],"study_design_scores_gemma":[0.00209116,0.0010332696,0.95632154,0.000078085846,0.00011369071,0.00014150955,0.022450753,0.0033807147,0.005609322,0.0048344014,0.0035498934,0.00039567245],"about_ca_topic_score_codex":0.0026984662,"about_ca_topic_score_gemma":0.0002382616,"teacher_disagreement_score":0.77197754,"about_ca_system_score_codex":0.00054045685,"about_ca_system_score_gemma":0.00008034608,"threshold_uncertainty_score":0.99996585},"labels":[],"label_agreement":null},{"id":"W4289868228","doi":"10.5194/amt-15-4443-2022","title":"Validation of the Aeolus Level-2B wind product over Northern Canada and the Arctic","year":2022,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":25,"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 Waterloo; Environment and Climate Change Canada; University of Toronto","funders":"Canadian Space Agency","keywords":"Lidar; Arctic; Radiosonde; Environmental science; Meteorology; Satellite; Numerical weather prediction; Climatology; Atmospheric sciences; Geography; Remote sensing; Geology; Physics","score_opus":0.013253678506282854,"score_gpt":0.18739209794058428,"score_spread":0.17413841943430142,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4289868228","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":[0.9951849,0.00025674896,0.00043423809,0.0012191774,0.0001556809,0.0009268716,0.0000043786204,0.000043151886,0.0017748451],"genre_scores_gemma":[0.99736047,0.000015883414,0.0014058833,0.0004980941,0.000025365374,0.00012377831,9.795083e-7,0.00001839999,0.0005511325],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99764335,0.00024302013,0.0002802552,0.00028898148,0.0013311685,0.00021320641],"domain_scores_gemma":[0.99915314,0.000029232657,0.00024165993,0.0005028481,0.000034356544,0.00003875505],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010599754,0.00015942687,0.00017411263,1.8699157e-7,0.00046271287,0.00001569673,0.0004542552,0.000019740633,0.00092132075],"category_scores_gemma":[0.000080604084,0.000094917625,0.000059540576,0.00033184193,0.0003284382,0.00006280258,0.0004916045,0.0001879397,0.0000010994266],"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":[0.0001050675,0.00012848608,0.9473045,0.000031280997,0.00007752838,0.0000026853274,0.0010149716,0.002353886,0.010080713,0.00017287156,0.010054052,0.028673947],"study_design_scores_gemma":[0.0013287035,0.00024184954,0.8831834,0.000050635685,0.00019133641,0.000037255046,0.00080616836,0.00097536854,0.044309147,0.0021039962,0.06606651,0.0007056039],"about_ca_topic_score_codex":0.48757267,"about_ca_topic_score_gemma":0.18780518,"teacher_disagreement_score":0.2997675,"about_ca_system_score_codex":0.0007338871,"about_ca_system_score_gemma":0.00014536922,"threshold_uncertainty_score":0.99999195},"labels":[],"label_agreement":null},{"id":"W4292313259","doi":"10.3390/atmos13081266","title":"Long-Term Variability of Aerosol Concentrations and Optical Properties over the Indo-Gangetic Plain in South Asia","year":2022,"lang":"en","type":"article","venue":"Atmosphere","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Concordia University","funders":"","keywords":"Aerosol; Moderate-resolution imaging spectroradiometer; New delhi; Environmental science; South asia; Climatology; Air pollutants; Geography; Atmospheric sciences; Satellite; Air pollution; Meteorology; Geology","score_opus":0.0095809912874478,"score_gpt":0.20604679491272893,"score_spread":0.19646580362528113,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4292313259","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":[0.9963725,0.0001410184,0.00016841874,0.0002213513,0.000051144958,0.00038012548,0.0000061757846,0.000013713477,0.0026455207],"genre_scores_gemma":[0.9991436,0.0000062877884,0.00036138855,0.000119861936,0.00001259685,0.00008066519,0.0000016602827,0.000010525437,0.00026342674],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99887013,0.00014256619,0.00022932242,0.00025681147,0.00028000868,0.00022115374],"domain_scores_gemma":[0.9995475,0.00006425234,0.00007015489,0.0002593214,0.000004291005,0.000054475655],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00029075117,0.00011397831,0.00014707519,1.2809618e-7,0.00021650048,0.000020418796,0.00020168642,0.000040550723,0.0050310143],"category_scores_gemma":[0.00003999268,0.0000800467,0.000035631125,0.00018727256,0.00047114494,0.00007814957,0.00038212264,0.00021205859,0.000010884567],"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":[0.000030152496,0.000115695395,0.9902211,0.0000097877955,0.000008078711,0.0000056903627,0.0026346124,0.0041934373,0.0012215792,0.0003007545,0.000086256936,0.001172901],"study_design_scores_gemma":[0.00042107335,0.00010492622,0.99424684,0.000008148237,0.000016482034,0.00000675901,0.001521729,0.0030493217,0.00033064766,0.0000874033,0.000077043354,0.00012961315],"about_ca_topic_score_codex":0.00020054613,"about_ca_topic_score_gemma":0.00017865913,"teacher_disagreement_score":0.00502013,"about_ca_system_score_codex":0.00011016605,"about_ca_system_score_gemma":0.000028268885,"threshold_uncertainty_score":0.9958785},"labels":[],"label_agreement":null},{"id":"W4292428650","doi":"10.1007/s40808-022-01492-6","title":"Development of visibility equation based on fog microphysical observations and its verification using the WRF model","year":2022,"lang":"en","type":"article","venue":"Modeling Earth Systems and Environment","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":20,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ontario Tech University; Environment and Climate Change Canada","funders":"","keywords":"Visibility; Liquid water content; Weather Research and Forecasting Model; Environmental science; Meteorology; Atmospheric sciences; Population; Geography; Physics; Demography","score_opus":0.07782536112880144,"score_gpt":0.22950530196508573,"score_spread":0.15167994083628428,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4292428650","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":[0.76080585,0.000052327534,0.23881233,0.000052402618,0.000020318736,0.0002226469,0.000007290582,0.000005112076,0.00002172832],"genre_scores_gemma":[0.99051964,0.000008113152,0.00930507,0.00004827953,0.000007947268,0.00005195097,0.000006910331,0.000008344695,0.00004375291],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9989477,0.00005509201,0.00024585216,0.00025033113,0.00038928978,0.00011172956],"domain_scores_gemma":[0.99967545,0.000015539817,0.00009041729,0.00017750297,0.0000034682394,0.000037628328],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041654892,0.00009285339,0.000102270336,0.0000019480494,0.00047775934,0.00001459824,0.00006871027,0.000022290433,0.000034748315],"category_scores_gemma":[0.0000037998007,0.000073883195,0.000019782949,0.000046907408,0.000037340506,0.000049647384,0.00011781873,0.00007444783,0.0000020369428],"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":[0.000009901738,0.000056825058,0.00091172516,0.000009440775,0.0000030143758,7.133746e-8,0.0005589065,0.9672301,0.030461716,0.0000777031,0.0000018713852,0.00067871716],"study_design_scores_gemma":[0.00013065786,0.000030801668,0.0035993846,0.0000073592228,0.000009066302,4.5250593e-7,0.00025116163,0.9954706,0.00020660658,0.000031173637,0.0001795631,0.00008318764],"about_ca_topic_score_codex":0.00009672679,"about_ca_topic_score_gemma":0.0000026134849,"teacher_disagreement_score":0.2297138,"about_ca_system_score_codex":0.00013014795,"about_ca_system_score_gemma":0.000017101995,"threshold_uncertainty_score":0.3674587},"labels":[],"label_agreement":null},{"id":"W4293056574","doi":"10.5194/acp-2022-343-rc2","title":"Review of &amp;amp;#8220;Self-lofting of wildfire smoke in the troposphere and stratosphere caused by radiative heating: simulations vs space lidar observations&amp;amp;#8221; by Ohneiser et al. (2022)","year":2022,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Universität Leipzig; European Commission","keywords":"Troposphere; Environmental science; Atmospheric sciences; Aerosol; Stratosphere; Overcast; Shortwave; Tropopause; Radiosonde; Cirrus; Radiative transfer; Cloud cover; Lidar; Smoke; Climatology; Meteorology; Remote sensing; Geology; Geography; Sky; Physics","score_opus":0.03394815710265213,"score_gpt":0.3030126065378819,"score_spread":0.2690644494352298,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4293056574","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.106060065,0.70721316,0.0020885477,0.14586607,0.00071334507,0.009730668,0.0049220524,0.00026475947,0.023141297],"genre_scores_gemma":[0.009616903,0.6397555,0.042727463,0.104251325,0.00012978364,0.0010033003,0.012465496,0.00044529056,0.18960498],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99352235,0.0011203232,0.0018991502,0.0011855873,0.0015924777,0.0006801401],"domain_scores_gemma":[0.9955005,0.001088584,0.0016271576,0.0014801668,0.00009397938,0.00020963042],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0018928844,0.0009017548,0.0017534189,0.0000063090765,0.00043450826,0.0000698711,0.0010244182,0.00030276176,0.032333735],"category_scores_gemma":[0.0008163488,0.0007180864,0.00038573504,0.0017772082,0.0004163591,0.00037186217,0.00056666275,0.0013003822,0.000048719525],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000101198075,0.00034386694,0.017072134,0.0033386569,0.00011248982,8.852473e-7,0.0006929399,0.000597777,0.00017078641,0.000051765644,0.97670525,0.00090332405],"study_design_scores_gemma":[0.0004910076,0.0000844586,0.002493606,0.0046784873,0.00032428795,0.00000474069,0.00034467556,0.000110191184,0.0000068012105,0.00005139208,0.99069715,0.00071319594],"about_ca_topic_score_codex":0.0097355135,"about_ca_topic_score_gemma":0.007365298,"teacher_disagreement_score":0.16646369,"about_ca_system_score_codex":0.0004345184,"about_ca_system_score_gemma":0.00026155493,"threshold_uncertainty_score":0.99952704},"labels":[],"label_agreement":null},{"id":"W4294733087","doi":"10.1155/2022/1030330","title":"Wavelet Analysis of the Interconnection between Atmospheric Aerosol Types and Direct Irradiation over Cameroon","year":2022,"lang":"en","type":"article","venue":"Advances in Meteorology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"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":"Deutscher Akademischer Austauschdienst; International Development Research Centre; United Nations Educational, Scientific and Cultural Organization","keywords":"Interconnection; Wavelet; Aerosol; Geography; Atmospheric sciences; Environmental science; Meteorology; Computer science; Geology; Artificial intelligence; Telecommunications","score_opus":0.004228107284434425,"score_gpt":0.2268972875084812,"score_spread":0.22266918022404678,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4294733087","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":[0.997126,0.0007237478,0.00034856776,0.0000938752,0.00015267287,0.000098037446,0.0000073928304,0.000008418013,0.0014413234],"genre_scores_gemma":[0.998777,0.0001528734,0.0007419582,0.00014323194,0.000011641967,0.000029553428,0.0000044707836,0.00000597225,0.00013329693],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999094,0.00019828397,0.00019131372,0.0002309194,0.00014307458,0.00014241059],"domain_scores_gemma":[0.99953634,0.00012795636,0.0001458588,0.00016802542,0.0000026748962,0.00001916465],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00022624955,0.00008005978,0.0002234201,0.0000025146892,0.00010868399,0.000003014871,0.00015934504,0.00003313604,0.0013681465],"category_scores_gemma":[0.000037076992,0.00006288616,0.000056592766,0.0008847633,0.00016803715,0.000119733006,0.00023607313,0.00012339752,0.0000019957097],"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":[0.000018219698,0.000017623302,0.9287627,0.000001909227,0.000051673378,4.477135e-7,0.00029079485,0.042729843,0.00073381595,0.00005907643,0.000019667814,0.027314236],"study_design_scores_gemma":[0.0001767851,0.00014984627,0.9847264,0.0000010637086,0.00017367986,8.4096826e-7,0.00017305865,0.00968186,0.00014627431,0.00034040934,0.004341411,0.0000883324],"about_ca_topic_score_codex":0.00058915315,"about_ca_topic_score_gemma":0.0011520786,"teacher_disagreement_score":0.055963747,"about_ca_system_score_codex":0.00010617719,"about_ca_system_score_gemma":0.0000038410935,"threshold_uncertainty_score":0.99954474},"labels":[],"label_agreement":null},{"id":"W4295599243","doi":"10.1029/2022gl099578","title":"How Are Mixed‐Phase Clouds Mixed?","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":73,"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":"Mixed phase; Phase (matter); Environmental science; Precipitation; Cascade; Atmospheric sciences; Meteorology; Physics; Chemistry","score_opus":0.03050027110425248,"score_gpt":0.2953650286793617,"score_spread":0.26486475757510924,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4295599243","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":[0.96662396,0.000028799708,0.00036109058,0.0310402,0.0002549818,0.00026303573,0.000023903196,0.000056285287,0.0013477338],"genre_scores_gemma":[0.99213415,0.0000040555287,0.00029036132,0.0019269555,0.00027203115,0.00020808709,0.000013645597,0.000032687625,0.005118015],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9956965,0.00047391444,0.00014228442,0.0006119117,0.0020533297,0.0010220998],"domain_scores_gemma":[0.9988669,0.00019556015,0.0000596115,0.0005439341,0.000013394095,0.00032060448],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00058657455,0.00017885715,0.00020511195,0.000004958204,0.0010102238,0.00013229864,0.0008216121,0.000035813187,0.00281245],"category_scores_gemma":[0.00011267875,0.00016663945,0.00014505108,0.00085100567,0.00066459476,0.00017763763,0.0017134956,0.00097630697,0.0009833012],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017708921,0.0010771975,0.0066044084,0.000014544727,0.000041616022,0.00047219245,0.00042759214,0.00084767607,0.19800428,0.00080649584,0.75398624,0.03754065],"study_design_scores_gemma":[0.0023954113,0.0013230732,0.10548611,0.00001212333,0.000023628027,0.000020245687,0.0036308463,0.0037419815,0.004615637,0.0026400972,0.8751937,0.0009171187],"about_ca_topic_score_codex":0.0005361248,"about_ca_topic_score_gemma":0.000025235257,"teacher_disagreement_score":0.19338864,"about_ca_system_score_codex":0.00044233812,"about_ca_system_score_gemma":0.000019277077,"threshold_uncertainty_score":0.99979454},"labels":[],"label_agreement":null},{"id":"W4295681501","doi":"10.1016/j.jqsrt.2022.108368","title":"Polarized discrete ordinate adding approximation for infrared and microwave radiative transfer","year":2022,"lang":"en","type":"article","venue":"Journal of Quantitative Spectroscopy and Radiative Transfer","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":5,"is_retracted":false,"has_abstract":false,"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; National Natural Science Foundation of China","keywords":"Radiative transfer; Microwave; Infrared; Ordinate; Atmospheric radiative transfer codes; Computational physics; Materials science; Physics; Optics; Geometry; Mathematics; Quantum mechanics","score_opus":0.013169883161331428,"score_gpt":0.2618251871932223,"score_spread":0.24865530403189084,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4295681501","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":[0.5287543,0.00083526404,0.46807322,0.0005544377,0.00016250652,0.0005000441,0.00011394663,0.000009116313,0.0009971798],"genre_scores_gemma":[0.9709485,0.00035671075,0.02806739,0.0002342827,0.000050874558,0.000041964187,0.000010055114,0.000030871113,0.00025934965],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9982699,0.0002639947,0.0004943785,0.0003055968,0.00033448386,0.0003316368],"domain_scores_gemma":[0.9993036,0.00029438979,0.00012972434,0.00007501769,0.000037476562,0.00015983747],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00066520664,0.00025613414,0.00048422106,0.00002197847,0.0005904868,0.000053902077,0.00015011524,0.000059223446,0.00046961525],"category_scores_gemma":[0.000037962654,0.00021193425,0.00017245777,0.00028856835,0.00037194896,0.00054048304,0.000035807152,0.00044150706,0.0000016765669],"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":[0.0037787745,0.00032861897,0.011142525,0.000087660126,0.0006248107,0.00003257718,0.052082755,0.0017761707,0.89294755,0.03338275,0.001133692,0.0026821326],"study_design_scores_gemma":[0.054554652,0.045166288,0.29878333,0.0003637335,0.0024733285,0.00063335913,0.096839994,0.073374964,0.29582065,0.08363322,0.043281145,0.005075315],"about_ca_topic_score_codex":0.000026400397,"about_ca_topic_score_gemma":0.000014173031,"teacher_disagreement_score":0.5971269,"about_ca_system_score_codex":0.00020903423,"about_ca_system_score_gemma":0.000044848573,"threshold_uncertainty_score":0.8642428},"labels":[],"label_agreement":null},{"id":"W4295926387","doi":"10.5194/egusphere-2022-491-ac1","title":"Reply on CC1","year":2022,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Environment and Climate Change Canada","keywords":"Ice nucleus; Clear ice; Precipitation; Atmosphere (unit); Environmental science; Ice formation; Hard rime; Ice crystals; Atmospheric sciences; Ice core; Climatology; Nucleation; Geology; Cryosphere; Meteorology; Geography; Physics; Sea ice; Antarctic sea ice; Thermodynamics","score_opus":0.018445482789994406,"score_gpt":0.26515448127362007,"score_spread":0.24670899848362565,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4295926387","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000041079424,0.0026782053,0.000025365169,0.07104179,0.0014308565,0.0003196124,0.000035200563,0.00007882583,0.92434907],"genre_scores_gemma":[0.000056689492,0.0030674848,0.0004109865,0.09588467,0.00011523298,0.00008116446,0.00012915934,0.000030590738,0.90022403],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99819314,0.00004624425,0.0002323134,0.00053796155,0.0007393697,0.0002509441],"domain_scores_gemma":[0.99908406,0.000031165546,0.00012239759,0.0006694479,0.0000028245743,0.000090095964],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0002353003,0.00023335668,0.00031340006,4.520903e-7,0.00013317642,0.000012363165,0.00049231335,0.00007115017,0.6688762],"category_scores_gemma":[0.00003646194,0.00018111635,0.00016240157,0.00017900033,0.00006761186,0.000024720006,0.0005374463,0.00041530607,0.006871632],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000015718367,0.00003549051,0.000050155162,0.000055429282,0.0000060155116,0.000011837197,0.0000070274214,0.000030919924,8.630333e-7,0.000037160913,0.988144,0.011619573],"study_design_scores_gemma":[0.000047777692,0.000100509045,0.00017319774,0.000094599,0.000025579147,0.0000045600245,0.000008000639,0.0000100207135,0.000001940971,0.000042911764,0.9992499,0.00024105408],"about_ca_topic_score_codex":0.0015926447,"about_ca_topic_score_gemma":0.0000633384,"teacher_disagreement_score":0.66200453,"about_ca_system_score_codex":0.00027767583,"about_ca_system_score_gemma":0.000018013203,"threshold_uncertainty_score":0.9939016},"labels":[],"label_agreement":null},{"id":"W4296756220","doi":"10.5194/amt-15-5367-2022","title":"The Microfluidic Ice Nuclei Counter Zürich (MINCZ): a platform for homogeneous and heterogeneous ice nucleation","year":2022,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":17,"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; Eidgenössische Technische Hochschule Zürich","keywords":"Ice nucleus; Nucleation; Supercooling; Mashing; Ice crystals; Microfluidics; Materials science; Homogeneous; Polydimethylsiloxane; Chemical physics; Atmosphere (unit); Chemical engineering; Amorphous ice; Nanotechnology; Chemistry; Thermodynamics; Meteorology; Organic chemistry; Physics","score_opus":0.015318877287469957,"score_gpt":0.2160628827647423,"score_spread":0.20074400547727236,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4296756220","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":[0.94958395,0.0059714443,0.034414656,0.0007548659,0.00039614493,0.0032634712,0.000022718645,0.0006707836,0.0049219714],"genre_scores_gemma":[0.98203635,0.00070946064,0.013813997,0.0012140903,0.000070206464,0.0012684758,0.0000068785125,0.00007790774,0.0008026228],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9974848,0.00008132312,0.00041010632,0.0005505901,0.00094434887,0.0005288386],"domain_scores_gemma":[0.9990744,0.00006355253,0.00021952097,0.00047779584,0.000051073614,0.00011364995],"candidate_categories":["metaepi_narrow","sts"],"consensus_categories":[],"category_scores_codex":[0.0011382513,0.00030361884,0.00023033905,7.122707e-7,0.0017258031,0.00011779453,0.0005290727,0.00007680742,0.00066720234],"category_scores_gemma":[0.00004233439,0.0002452875,0.000116050825,0.00026413752,0.0002134415,0.00013583475,0.00047901605,0.00018852558,0.000021566793],"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":[0.0007250391,0.0006274185,0.012751981,0.00007478674,0.00026668594,0.000037962644,0.002359127,0.0005335972,0.18961605,0.00032662041,0.14428377,0.64839697],"study_design_scores_gemma":[0.00054800085,0.0010763191,0.001971866,0.000016545664,0.00009998427,0.00013690081,0.000733258,0.0037539266,0.017050931,0.0008948589,0.9730896,0.00062783627],"about_ca_topic_score_codex":0.00048841815,"about_ca_topic_score_gemma":0.00007164315,"teacher_disagreement_score":0.8288058,"about_ca_system_score_codex":0.0008252035,"about_ca_system_score_gemma":0.00003309538,"threshold_uncertainty_score":0.99999994},"labels":[],"label_agreement":null},{"id":"W4297000570","doi":"10.5194/epsc2022-868","title":"Preliminary results of nadir retrievals from NOMAD/UVIS using new dust properties from lab measurements","year":2022,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Nadir; Atmospheric sciences; Shortwave; Aerosol; Environmental science; Atmosphere (unit); Physics; Radiative transfer; Chemistry; Meteorology; Satellite; Optics","score_opus":0.09174747997002011,"score_gpt":0.259265944736513,"score_spread":0.16751846476649287,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4297000570","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":[0.979744,0.0009060025,0.00062347844,0.00024160997,0.0006862468,0.0006584942,0.0003988716,0.000084123065,0.016657181],"genre_scores_gemma":[0.9667641,0.000067230176,0.022578005,0.00020675719,0.00018783454,0.00002026227,0.00017889394,0.000061856976,0.009935059],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99615484,0.00018675749,0.0008579194,0.0011046267,0.0013088916,0.00038696034],"domain_scores_gemma":[0.9979634,0.000058357666,0.00060512085,0.0011340291,0.000023545334,0.0002155047],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00040168277,0.0004460088,0.00060166453,0.0000035443861,0.00018961844,0.00006213368,0.0010101155,0.00031811863,0.024273144],"category_scores_gemma":[0.00014539773,0.000385835,0.00019863478,0.00021493937,0.000203385,0.00014197342,0.0039939596,0.000557829,0.000110045854],"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":[0.009796735,0.0017337067,0.31400195,0.00022388162,0.0016249965,0.00011630012,0.018968336,0.16380425,0.33158976,0.000009380927,0.13148315,0.026647523],"study_design_scores_gemma":[0.008961999,0.002236549,0.68918586,0.0018996039,0.001723059,0.000008560448,0.0070533785,0.0423263,0.19198617,0.0041397708,0.044534598,0.0059441403],"about_ca_topic_score_codex":0.19623691,"about_ca_topic_score_gemma":0.00059133675,"teacher_disagreement_score":0.3751839,"about_ca_system_score_codex":0.0006981629,"about_ca_system_score_gemma":0.00019711877,"threshold_uncertainty_score":0.99985933},"labels":[],"label_agreement":null},{"id":"W4297859024","doi":"10.5194/acp-2022-492-supplement","title":"Supplementary material to \"The impacts of dust aerosol and convective available potential energy on precipitation vertical structure in eastern China as seen from multiple source observations\"","year":2022,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec en Abitibi-Témiscamingue","funders":"","keywords":"Aerosol; Precipitation; Environmental science; Convection; Atmospheric sciences; China; Earth science; Meteorology; Geology; Geography","score_opus":0.009267832168558237,"score_gpt":0.21473249540128775,"score_spread":0.20546466323272952,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4297859024","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":[0.9960697,0.000009797683,0.0008122676,0.0006088189,0.00039878703,0.0005557019,0.0013170651,0.000013759159,0.00021406895],"genre_scores_gemma":[0.9960314,0.000009899366,0.0014888545,0.00053165073,0.00009144835,0.000079643534,0.0010328979,0.00002546625,0.00070873223],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99821126,0.0001589462,0.00035667117,0.00056750147,0.00044763615,0.00025795712],"domain_scores_gemma":[0.99936205,0.00006389154,0.00010965144,0.00034575147,0.00000831354,0.00011035675],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000105070925,0.00025443424,0.00026752902,0.0000043387054,0.00013009526,0.000048224323,0.00032340985,0.00014296739,0.04258297],"category_scores_gemma":[0.000031103064,0.00020177699,0.000050497692,0.000111856534,0.000095854855,0.00007619975,0.0014293225,0.0002754997,0.000016874343],"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":[0.0015603928,0.00031951183,0.80040896,0.000032765933,0.00014102142,0.000012015199,0.00654148,0.123309836,0.05608164,0.000051683313,0.009581301,0.0019593963],"study_design_scores_gemma":[0.0013939155,0.0005594199,0.9323158,0.00004892642,0.0000793744,0.0000028628892,0.0017603453,0.03663909,0.023413977,0.0006178495,0.0026180379,0.00055039563],"about_ca_topic_score_codex":0.117824316,"about_ca_topic_score_gemma":0.010609648,"teacher_disagreement_score":0.13190685,"about_ca_system_score_codex":0.00026491223,"about_ca_system_score_gemma":0.00003690215,"threshold_uncertainty_score":0.95829225},"labels":[],"label_agreement":null},{"id":"W4297922255","doi":"10.5194/acp-2022-492","title":"The impacts of dust aerosol and convective available potential energy on precipitation vertical structure in eastern China as seen from multiple source observations","year":2022,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Université du Québec en Abitibi-Témiscamingue","funders":"National Key Research and Development Program of China; National Natural Science Foundation of China","keywords":"Precipitation; Atmospheric sciences; Convective available potential energy; Aerosol; Environmental science; Convection; Precipitation types; Cape; Scavenging; Growth rate; Mineral dust; Climatology; Wind shear; Wind speed; Meteorology; Geology; Geography; Chemistry","score_opus":0.009993071611584114,"score_gpt":0.2135009630151755,"score_spread":0.20350789140359138,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4297922255","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":[0.99613446,0.00007541445,0.0012695825,0.00025781983,0.00018647776,0.0002938462,0.00006670213,0.000018489422,0.0016972339],"genre_scores_gemma":[0.99677074,0.000055988115,0.00054702925,0.00013970715,0.00003533475,0.000041045198,0.00009107653,0.000020245141,0.0022988184],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984865,0.00014136992,0.00028956064,0.0004644823,0.0003931133,0.00022493459],"domain_scores_gemma":[0.99926996,0.00017051586,0.00012903922,0.0003352476,0.000009468505,0.0000857402],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00009652621,0.0002113051,0.00021821809,0.0000022558243,0.00020486992,0.000044992,0.0002788495,0.00016997484,0.0041328175],"category_scores_gemma":[0.00007851046,0.00015597435,0.00005665464,0.00010510378,0.00019054263,0.00008215175,0.0009506327,0.00040314175,0.000016154081],"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":[0.00045943132,0.00022343498,0.85919136,0.000016091193,0.00011421328,0.000006125403,0.0039062372,0.11447661,0.016102394,0.0002195337,0.0014606325,0.0038239497],"study_design_scores_gemma":[0.00065082224,0.00017862243,0.87937254,0.00002685083,0.00003493105,0.0000011788,0.0009916598,0.11365302,0.0026305115,0.0015935558,0.0005981769,0.00026810498],"about_ca_topic_score_codex":0.0395877,"about_ca_topic_score_gemma":0.005268201,"teacher_disagreement_score":0.034319498,"about_ca_system_score_codex":0.00019347113,"about_ca_system_score_gemma":0.00004186469,"threshold_uncertainty_score":0.99677753},"labels":[],"label_agreement":null},{"id":"W4298145816","doi":"10.3390/rs14194865","title":"Seasonal and Microphysical Characteristics of Fog at a Northern Airport in Alberta, Canada","year":2022,"lang":"en","type":"article","venue":"Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Impact; Barrie Urology Group; Environment and Climate Change Canada","funders":"","keywords":"Fog; Environmental science; Nowcasting; Meteorology; Visibility; Advection; Liquid water content; Atmospheric sciences; Haze; Climatology; Geography; Cloud computing; Physics","score_opus":0.0035258529208406623,"score_gpt":0.17011483400095795,"score_spread":0.1665889810801173,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4298145816","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":[0.9984661,0.0000065217437,0.000046824724,0.00021826272,0.00006108467,0.000048114554,0.0000051367947,0.0000023956063,0.0011455669],"genre_scores_gemma":[0.99864817,0.0000018721379,0.000659391,0.0001491369,0.000018753468,1.3555442e-8,0.000003438688,0.00000907505,0.00051013764],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99930334,0.000025754294,0.00012281892,0.0001550384,0.00024512078,0.00014789951],"domain_scores_gemma":[0.99976134,0.000028135792,0.000064484055,0.00009389148,0.0000037125535,0.00004843782],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00005686755,0.000069197005,0.00012219831,6.1771567e-7,0.00009920735,0.000002981035,0.000044812194,0.000013487242,0.0001267981],"category_scores_gemma":[0.000008836055,0.000071987575,0.0000182116,0.00008578536,0.000060704377,0.000013566697,0.00023863724,0.000088123714,0.0000029929834],"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":[0.00007540103,0.000040316238,0.7148906,0.000016032433,0.000013860291,0.00020930529,0.0010377262,0.0013565401,0.053005878,0.000005176103,0.0005006284,0.22884852],"study_design_scores_gemma":[0.00025552913,0.000045042834,0.9039359,0.000012427431,0.000010916403,0.00011051083,0.00017158859,0.087680966,0.0007325441,0.000031233372,0.0068006096,0.00021272851],"about_ca_topic_score_codex":0.77513206,"about_ca_topic_score_gemma":0.81487614,"teacher_disagreement_score":0.22863579,"about_ca_system_score_codex":0.00046488224,"about_ca_system_score_gemma":0.000065201224,"threshold_uncertainty_score":0.2935568},"labels":[],"label_agreement":null},{"id":"W4300124625","doi":"10.48550/arxiv.1512.08517","title":"A Stochastic Closure for Two-Moment Bulk Microphysics of Warm Clouds: Part I, Derivations","year":2015,"lang":"en","type":"preprint","venue":"arXiv (Cornell University)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Statistical physics; Collision; Moment (physics); Stochastic process; Standard deviation; Kernel (algebra); Closure (psychology); Aggregate (composite); Physics; Mathematics; Classical mechanics; Statistics; Computer science; Materials science","score_opus":0.057592399517587343,"score_gpt":0.19870686304194068,"score_spread":0.14111446352435333,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4300124625","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":[0.7341271,0.000026793268,0.26365674,0.00005033703,0.00030801227,0.00055488286,0.00010518573,0.00003964678,0.0011312738],"genre_scores_gemma":[0.9949273,0.000020030937,0.0021579242,0.00005731532,0.00011023836,0.00000766209,0.000055999604,0.000031273405,0.0026322913],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9985614,0.000040923376,0.0002496026,0.0006864058,0.00012791155,0.00033378133],"domain_scores_gemma":[0.99870837,0.000055546658,0.0003447118,0.00064510765,0.000067731955,0.00017853947],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00016186018,0.0002952283,0.0003646303,0.0000048325733,0.00012475961,0.000017404675,0.0005878626,0.00018339783,0.0002868058],"category_scores_gemma":[0.000020336534,0.00032457037,0.00023474808,0.00028394983,0.0003128198,0.00008221118,0.0009534278,0.00024846283,0.000086124994],"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":[0.00008903484,0.00025133003,0.0034165145,0.00005548558,0.000101818805,0.000009805054,0.00032759254,0.98693144,0.00061333517,0.004380453,0.0034532389,0.0003699545],"study_design_scores_gemma":[0.012316234,0.0019340713,0.006042907,0.00081335136,0.0030226936,0.000014051477,0.0026354436,0.6507868,0.003737891,0.24518305,0.06772286,0.0057906443],"about_ca_topic_score_codex":0.0003769026,"about_ca_topic_score_gemma":0.00007428382,"teacher_disagreement_score":0.33614463,"about_ca_system_score_codex":0.0004177801,"about_ca_system_score_gemma":0.00010212443,"threshold_uncertainty_score":0.9999206},"labels":[],"label_agreement":null},{"id":"W4300781744","doi":"10.31399/asm.cp.itsc2001p0723","title":"Significant Increase in the Sensitivity of In-Flight Particle Detector Through Improvements and Innovation","year":2001,"lang":"en","type":"article","venue":"Thermal spray","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"National Research Council Canada","funders":"","keywords":"Pyrometer; Emissivity; Detector; Materials science; Sensitivity (control systems); Wavelength; Particle (ecology); Temperature measurement; Optics; Optoelectronics; Engineering; Electronic engineering; Physics","score_opus":0.013538830094418822,"score_gpt":0.2335094545282164,"score_spread":0.21997062443379756,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4300781744","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":[0.9974336,0.000008755594,0.000108528555,0.00014223509,0.00001204018,0.00016099012,0.0000010776491,0.000005087464,0.0021276805],"genre_scores_gemma":[0.999483,0.0000069457824,0.0001359757,0.00030939258,0.000011282479,0.000008651828,5.519186e-7,0.000004307976,0.000039905473],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99932146,0.0001056926,0.00016183092,0.00012253519,0.0001379128,0.00015057146],"domain_scores_gemma":[0.9997587,0.000048461105,0.00005704512,0.00011823434,0.0000034075426,0.000014104443],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00052382227,0.00006507844,0.000080536585,0.0000013610678,0.00002951814,0.0000071275113,0.000062486535,0.000026682525,0.00020550017],"category_scores_gemma":[0.000025328549,0.000043535958,0.000009344095,0.00045239145,0.000103153274,0.00012665393,0.000054366315,0.00006607944,0.000014142209],"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":[0.000034623812,0.00007653231,0.53252536,0.0000014760423,0.0000011911056,0.000012468644,0.000649023,0.00009310204,0.46063146,0.00013775546,0.000004461539,0.005832569],"study_design_scores_gemma":[0.0003141987,0.000055145752,0.95808834,0.000004499822,0.000002658229,0.0000020985624,0.0002129102,0.0005508056,0.040407244,0.00011627778,0.00018306958,0.00006276387],"about_ca_topic_score_codex":0.003183847,"about_ca_topic_score_gemma":0.00062062923,"teacher_disagreement_score":0.42556298,"about_ca_system_score_codex":0.00002980477,"about_ca_system_score_gemma":0.000003919401,"threshold_uncertainty_score":0.48130456},"labels":[],"label_agreement":null},{"id":"W4301245856","doi":"","title":"Intercomparison of model simulations of mixed-phase clouds observed during the ARM Mixed-Phase Arctic Cloud Experiment. Part I: Single layer cloud","year":2009,"lang":"en","type":"article","venue":"eScholarship (California Digital Library)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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":"Pacific Northwest National Laboratory; Army Research Laboratory; Lawrence Berkeley National Laboratory; Lawrence Livermore National Laboratory; Chinese Academy of Meteorological Sciences; Canadian Foundation for Climate and Atmospheric Sciences; Colorado State University; Deutscher Akademischer Austauschdienst; Battelle; Office of Science; National Aeronautics and Space Administration; U.S. Department of Energy; U.S. Department of Defense; National Science Foundation","keywords":"Mixed phase; Cloud computing; Mixed layer; Arctic; Environmental science; Phase (matter); Atmospheric sciences; Meteorology; Layer (electronics); The arctic; Physics; Materials science; Geology; Computer science; Oceanography","score_opus":0.03603409565136151,"score_gpt":0.260443994500005,"score_spread":0.22440989884864349,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4301245856","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":[0.99305636,0.00019969215,0.0013883214,0.0002915974,0.00023148081,0.00045124485,0.00080959534,0.00013332626,0.0034383798],"genre_scores_gemma":[0.9975045,0.000009777001,0.0012025457,0.00021632445,0.00015650691,0.00001582388,0.00017611716,0.000067666195,0.0006507365],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9969007,0.00013630683,0.0010876738,0.00059365813,0.0006552685,0.00062640815],"domain_scores_gemma":[0.9981581,0.0001559632,0.00048360467,0.0008485706,0.00002644097,0.00032734624],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00019160667,0.00046334995,0.000545889,0.000012186445,0.00025288793,0.00028303784,0.0008898133,0.00017813218,0.0016063183],"category_scores_gemma":[0.00013298218,0.00036947097,0.00034926183,0.0005862247,0.00039806042,0.0018492644,0.0004667557,0.0004310264,0.00021550001],"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":[0.004889531,0.04320436,0.38774824,0.000419326,0.0005506938,0.000101575635,0.0026317493,0.18367694,0.32506046,0.004584064,0.015699834,0.03143324],"study_design_scores_gemma":[0.015818944,0.0045488966,0.02953327,0.00072653784,0.00032969605,0.0000413602,0.0014078026,0.12041189,0.75520474,0.024584832,0.044209804,0.0031822342],"about_ca_topic_score_codex":0.000013454821,"about_ca_topic_score_gemma":0.0000051904476,"teacher_disagreement_score":0.43014428,"about_ca_system_score_codex":0.00012272655,"about_ca_system_score_gemma":0.000038242895,"threshold_uncertainty_score":0.9998757},"labels":[],"label_agreement":null},{"id":"W4301430869","doi":"10.5194/amt-2022-262","title":"Use of Lidar Aerosol Extinction and Backscatter Coefficients to Estimate Cloud Condensation Nuclei (CCN) Concentrations in the Southeast Atlantic","year":2022,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Mount Allison University","funders":"HORIZON EUROPE Excellent Science; Supercomputing Center for Education and Research, University of Oklahoma; Horizon 2020 Framework Programme; University of Oklahoma; National Aeronautics and Space Administration; U.S. Department of Energy","keywords":"Aerosol; Cloud condensation nuclei; Lidar; Environmental science; Atmospheric sciences; Extinction (optical mineralogy); Backscatter (email); Remote sensing; In situ; Relative humidity; Meteorology; Chemistry; Geology; Geography; Mineralogy","score_opus":0.02329588738736269,"score_gpt":0.2645487855464592,"score_spread":0.24125289815909653,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4301430869","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":[0.98952776,0.0000072265175,0.007306312,0.00059913326,0.00025180858,0.00084444013,0.000028646338,0.000023560791,0.0014110974],"genre_scores_gemma":[0.99727714,0.000008375388,0.0016409671,0.00048743354,0.000025875257,0.0000740889,0.000050204122,0.000017031909,0.00041885333],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984195,0.00014653015,0.00036873817,0.00043587835,0.00040611168,0.00022324763],"domain_scores_gemma":[0.9992853,0.000080904356,0.00016997135,0.00038712943,0.0000110061455,0.000065702305],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00027434333,0.00019400119,0.00020846103,0.0000036059787,0.00016268237,0.00010064717,0.00026114387,0.00009629702,0.0046981205],"category_scores_gemma":[0.000032594282,0.00014986272,0.000053140426,0.00018857371,0.00017210713,0.00008386058,0.000673208,0.00028162939,0.00008259504],"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":[0.00006892373,0.00031724625,0.8338449,0.000046352456,0.000022071907,0.0000062028453,0.007532817,0.15007636,0.0045760614,0.0003853559,0.0019809713,0.0011427422],"study_design_scores_gemma":[0.0007754494,0.00025642925,0.93205017,0.00010290771,0.00012257547,0.000018865412,0.0056343763,0.054477356,0.00052315864,0.0002819504,0.004967466,0.0007892755],"about_ca_topic_score_codex":0.001821255,"about_ca_topic_score_gemma":0.0006557216,"teacher_disagreement_score":0.0982053,"about_ca_system_score_codex":0.000115068346,"about_ca_system_score_gemma":0.000018426792,"threshold_uncertainty_score":0.9962117},"labels":[],"label_agreement":null},{"id":"W4303491737","doi":"10.5194/acp-2022-492-rc1","title":"Comment on acp-2022-492","year":2022,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Université du Québec en Abitibi-Témiscamingue","funders":"National Key Research and Development Program of China; National Natural Science Foundation of China","keywords":"Computer science","score_opus":0.019411189464978273,"score_gpt":0.26834059948544176,"score_spread":0.24892941002046348,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4303491737","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000034125565,0.003538788,0.00006113594,0.30470327,0.0020384446,0.00057798857,0.00009042398,0.00008374875,0.6888721],"genre_scores_gemma":[0.00006196462,0.005484921,0.00039894585,0.21637146,0.00011747486,0.00017522289,0.00031924224,0.00004033716,0.7770304],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9976114,0.00008799507,0.00030870724,0.0005873232,0.0010444279,0.00036013062],"domain_scores_gemma":[0.9989342,0.000052571417,0.00015592102,0.00071601867,0.0000038181856,0.00013749115],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00033165808,0.00033914542,0.00043642515,8.680019e-7,0.00021632486,0.00002004902,0.00071404997,0.00011484321,0.65623116],"category_scores_gemma":[0.000021556945,0.00026814287,0.00021216454,0.0002179201,0.00008699104,0.00003059773,0.0010462309,0.0005985599,0.005280697],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000025676861,0.000097828575,0.00006938856,0.00008200816,0.000013812733,0.000011417156,0.000012674946,0.000034882247,0.0000012887303,0.00012755112,0.9858562,0.013690385],"study_design_scores_gemma":[0.00009616116,0.00016079,0.00011240598,0.0001246751,0.000043202996,0.0000030789486,0.000023025192,0.000022818074,0.00000387829,0.000059615428,0.9990127,0.0003376423],"about_ca_topic_score_codex":0.0011378324,"about_ca_topic_score_gemma":0.000101596845,"teacher_disagreement_score":0.6509505,"about_ca_system_score_codex":0.00057119253,"about_ca_system_score_gemma":0.00002056294,"threshold_uncertainty_score":0.99997705},"labels":[],"label_agreement":null},{"id":"W4303945634","doi":"","title":"Evaluation of a high-resolution numerical weather prediction model's simulated clouds using observations from CloudSat, GOES-13 and in situ aircraft","year":2018,"lang":"en","type":"preprint","venue":"HAL (Le Centre pour la Communication Scientifique Directe)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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; Meteorology; In situ; Climatology; Numerical weather prediction; Weather prediction; High resolution; Remote sensing; Geology; Geography","score_opus":0.030801871320314474,"score_gpt":0.24791085253315626,"score_spread":0.21710898121284178,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4303945634","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":[0.8076089,0.00022095551,0.18872851,0.0005200953,0.00012574553,0.0005334464,0.00008070627,0.0000680925,0.0021135432],"genre_scores_gemma":[0.94434726,0.00009747369,0.054843403,0.000033870267,0.00002692346,0.000034148376,0.000333385,0.000038777645,0.00024473213],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9940332,0.0031956274,0.00069184287,0.00082657,0.0009558621,0.0002968684],"domain_scores_gemma":[0.99717975,0.00033718024,0.00056263566,0.0011354273,0.00065661,0.00012840435],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0048490837,0.000312181,0.0003887104,0.000017531007,0.00022823978,0.00009033262,0.00050305045,0.00039609405,0.00039285593],"category_scores_gemma":[0.0006752782,0.00033589997,0.00010780405,0.0004429472,0.00038938952,0.00021324841,0.0010990413,0.0004109743,0.000013918744],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000056448134,0.0007816793,0.09658178,0.000036146645,0.000100866826,9.92825e-7,0.00792307,0.8599252,0.02258033,0.0005424701,0.00026076328,0.011210247],"study_design_scores_gemma":[0.0006292581,9.14908e-7,0.1320712,0.0003927729,0.000152604,7.9458096e-7,0.000055282027,0.85597515,0.0023907935,0.008036693,0.000061014667,0.00023354929],"about_ca_topic_score_codex":0.018184064,"about_ca_topic_score_gemma":0.0048298417,"teacher_disagreement_score":0.13673839,"about_ca_system_score_codex":0.0006054749,"about_ca_system_score_gemma":0.00018638076,"threshold_uncertainty_score":0.9999093},"labels":[],"label_agreement":null},{"id":"W4306164068","doi":"10.3389/frsen.2022.1040835","title":"Editorial: Remote sensing of cloud, aerosols, and radiation from satellites","year":2022,"lang":"en","type":"editorial","venue":"Frontiers in Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"","keywords":"Remote sensing; Cloud computing; Environmental science; Meteorology; Astrobiology; Computer science; Geography; Physics; Operating system","score_opus":0.0047941565994393375,"score_gpt":0.21217325133216186,"score_spread":0.20737909473272254,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4306164068","genre_codex":"editorial","genre_gemma":"editorial","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"editorial","genre_consensus":"editorial","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.009854621,0.0019461509,0.022251332,0.0000500852,0.96465385,0.0003403133,0.000090023816,0.00006345955,0.0007501621],"genre_scores_gemma":[0.00040043684,0.0024614395,0.2254891,0.00003751025,0.77087605,3.5873928e-8,0.00028312908,0.000113994,0.00033829844],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99582076,0.00033968556,0.0008173878,0.0010332657,0.0014187262,0.0005702011],"domain_scores_gemma":[0.9980265,0.00044693798,0.00070632633,0.0006335445,0.00003615082,0.00015057875],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0007268433,0.00052811287,0.0009446694,0.0000184793,0.00024255164,0.00008296622,0.00028961617,0.0009460573,0.00009448961],"category_scores_gemma":[0.0006431721,0.0005925531,0.00015380235,0.0004642686,0.0003590536,0.00015610247,0.00051454786,0.001297936,0.000008695552],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007961405,0.00000525075,0.00014652094,0.000021076772,0.000030424524,0.000018892475,0.0005001935,0.00030470797,0.0004693093,7.232479e-8,0.6835977,0.31482622],"study_design_scores_gemma":[0.00070499076,0.000073332325,0.00009979279,0.00019112692,0.00009917566,0.00000249397,0.0005826644,0.036473397,0.00023321644,0.001360594,0.9595628,0.00061646645],"about_ca_topic_score_codex":0.018596174,"about_ca_topic_score_gemma":0.00024764083,"teacher_disagreement_score":0.31420976,"about_ca_system_score_codex":0.0009182554,"about_ca_system_score_gemma":0.00009977886,"threshold_uncertainty_score":0.99965256},"labels":[],"label_agreement":null},{"id":"W4306661112","doi":"10.5194/acp-2022-492-rc2","title":"Comment on acp-2022-492","year":2022,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Université du Québec en Abitibi-Témiscamingue","funders":"National Key Research and Development Program of China; National Natural Science Foundation of China","keywords":"Span (engineering); Precipitation; Atmospheric sciences; Meteorology; Environmental science; Geology; Physics","score_opus":0.019411189464978273,"score_gpt":0.26834059948544176,"score_spread":0.24892941002046348,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4306661112","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000034125565,0.003538788,0.00006113594,0.30470327,0.0020384446,0.00057798857,0.00009042398,0.00008374875,0.6888721],"genre_scores_gemma":[0.00006196462,0.005484921,0.00039894585,0.21637146,0.00011747486,0.00017522289,0.00031924224,0.00004033716,0.7770304],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9976114,0.00008799507,0.00030870724,0.0005873232,0.0010444279,0.00036013062],"domain_scores_gemma":[0.9989342,0.000052571417,0.00015592102,0.00071601867,0.0000038181856,0.00013749115],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00033165808,0.00033914542,0.00043642515,8.680019e-7,0.00021632486,0.00002004902,0.00071404997,0.00011484321,0.65623116],"category_scores_gemma":[0.000021556945,0.00026814287,0.00021216454,0.0002179201,0.00008699104,0.00003059773,0.0010462309,0.0005985599,0.005280697],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000025676861,0.000097828575,0.00006938856,0.00008200816,0.000013812733,0.000011417156,0.000012674946,0.000034882247,0.0000012887303,0.00012755112,0.9858562,0.013690385],"study_design_scores_gemma":[0.00009616116,0.00016079,0.00011240598,0.0001246751,0.000043202996,0.0000030789486,0.000023025192,0.000022818074,0.00000387829,0.000059615428,0.9990127,0.0003376423],"about_ca_topic_score_codex":0.0011378324,"about_ca_topic_score_gemma":0.000101596845,"teacher_disagreement_score":0.6509505,"about_ca_system_score_codex":0.00057119253,"about_ca_system_score_gemma":0.00002056294,"threshold_uncertainty_score":0.99997705},"labels":[],"label_agreement":null},{"id":"W4307765597","doi":"10.5194/amt-2022-284","title":"Relationship between the sub-micron fraction (SMF) and fine mode fraction (FMF) in the context of AERONET retrievals","year":2022,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University; National Research Council Canada; Université de Sherbrooke","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency; Goddard Space Flight Center; Brookhaven National Laboratory; Environment and Climate Change Canada; Strong; National Aeronautics and Space Administration","keywords":"AERONET; Aerosol; Cutoff; Effective radius; Context (archaeology); Angstrom exponent; Radiance; RADIUS; Physics; Astrophysics; Optics; Meteorology; Galaxy; Geography","score_opus":0.03116105681153355,"score_gpt":0.28002460421424935,"score_spread":0.2488635474027158,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4307765597","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":[0.990946,0.00016326879,0.0019269399,0.0020334846,0.000088943605,0.00062130496,0.000026909565,0.000019214607,0.00417393],"genre_scores_gemma":[0.9986786,0.00008886163,0.000262831,0.00023546311,0.00006211991,0.000060359023,0.000068249195,0.000015683234,0.00052780705],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982128,0.00034352078,0.00042082896,0.0003834989,0.00046251714,0.00017682869],"domain_scores_gemma":[0.998396,0.0006878494,0.00037118225,0.0005056726,0.000007523975,0.000031774616],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009711354,0.00019084856,0.0002546567,0.0000035410724,0.00025168862,0.000040433748,0.0003679395,0.00020830391,0.0016779312],"category_scores_gemma":[0.00011751604,0.000121248784,0.000072520896,0.00023133455,0.00020140526,0.00012607934,0.0005642979,0.0010339152,0.000026297292],"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":[0.0000390523,0.00004973522,0.9878433,0.00001812562,0.000011920539,7.694431e-7,0.001042932,0.002579045,0.000654161,0.00015404506,0.0034111927,0.00419574],"study_design_scores_gemma":[0.00019084835,0.00006246446,0.98965865,0.0000141380415,0.000044491666,0.0000021100109,0.0021078498,0.0011118118,0.00056193816,0.0036414254,0.0024413657,0.00016288312],"about_ca_topic_score_codex":0.0066808215,"about_ca_topic_score_gemma":0.00073477015,"teacher_disagreement_score":0.007732622,"about_ca_system_score_codex":0.00027915224,"about_ca_system_score_gemma":0.000021223233,"threshold_uncertainty_score":0.9999338},"labels":[],"label_agreement":null},{"id":"W4307765648","doi":"10.5194/acp-2022-343-ac1","title":"Reply on RC1","year":2022,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"European Commission; National Aeronautics and Space Administration","keywords":"Radiosonde; Aerosol; Environmental science; Atmospheric sciences; Troposphere; Shortwave; Tropopause; Overcast; Stratosphere; Lidar; Radiative transfer; Meteorology; Lapse rate; Atmosphere (unit); Climatology; Remote sensing; Geology; Geography; Physics; Sky","score_opus":0.018452288800312036,"score_gpt":0.2651782121851479,"score_spread":0.2467259233848359,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4307765648","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000047844806,0.0027054334,0.000025472167,0.059435334,0.0014389819,0.0003202119,0.000035226913,0.00007879509,0.9359127],"genre_scores_gemma":[0.000047009034,0.0031150281,0.00040830302,0.09726066,0.00011494103,0.00008049447,0.00012804566,0.000030318068,0.8988152],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9981883,0.00004642187,0.00023276696,0.0005386982,0.0007420604,0.00025173192],"domain_scores_gemma":[0.9990824,0.000031355772,0.00012252349,0.00067054527,0.0000028320337,0.00009034104],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00023787633,0.00023369763,0.0003140302,4.525079e-7,0.00013509319,0.000012399685,0.00049372035,0.00007121732,0.67835915],"category_scores_gemma":[0.000036766924,0.0001812263,0.00016262979,0.0001792862,0.00006761763,0.000024744435,0.00055009045,0.00041568722,0.0070448546],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000015809115,0.000032040483,0.00005935234,0.000055378285,0.000006008013,0.0000118224125,0.000006362411,0.00003299119,8.970309e-7,0.00003741573,0.9857086,0.014047548],"study_design_scores_gemma":[0.000044272365,0.0001005218,0.00020259227,0.00009451188,0.000025630281,0.000004563573,0.0000080195505,0.000010048276,0.0000019600313,0.000046222714,0.99922043,0.00024123168],"about_ca_topic_score_codex":0.0015361527,"about_ca_topic_score_gemma":0.000060520633,"teacher_disagreement_score":0.6713143,"about_ca_system_score_codex":0.00027860515,"about_ca_system_score_gemma":0.000018102455,"threshold_uncertainty_score":0.9937283},"labels":[],"label_agreement":null},{"id":"W4307853836","doi":"10.5194/acp-2022-343-ac2","title":"Reply on RC2","year":2022,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"European Commission; National Aeronautics and Space Administration","keywords":"Radiosonde; Environmental science; Aerosol; Atmospheric sciences; Troposphere; Shortwave; Tropopause; Stratosphere; Radiative transfer; Lidar; Overcast; Meteorology; Moderate-resolution imaging spectroradiometer; Remote sensing; Satellite; Geology; Geography; Sky; Physics","score_opus":0.018452288800312036,"score_gpt":0.2651782121851479,"score_spread":0.2467259233848359,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4307853836","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000052796422,0.002688117,0.000025837777,0.060280133,0.00146534,0.00032669472,0.00003440796,0.000089851244,0.93503684],"genre_scores_gemma":[0.000056938865,0.0029985055,0.00040520157,0.097406454,0.000114928545,0.00008065643,0.00012313321,0.000032826734,0.89878136],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9981905,0.000046346187,0.00023255135,0.0005381303,0.00074100017,0.0002514201],"domain_scores_gemma":[0.9990834,0.000031296608,0.00012246554,0.0006697726,0.0000028272248,0.000090264206],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00023414608,0.00023357457,0.0003137852,4.518011e-7,0.00012862905,0.000012377002,0.00049265,0.00007115931,0.66500044],"category_scores_gemma":[0.000036678273,0.00018113955,0.00016257104,0.0001788513,0.000067498295,0.000024727955,0.00054890616,0.00041517004,0.0066960314],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000015815522,0.000032008156,0.00007812141,0.000055353754,0.0000060120637,0.000011832144,0.000006326782,0.000024941044,9.245148e-7,0.00003547389,0.9868713,0.012876129],"study_design_scores_gemma":[0.000043998072,0.00010035114,0.00022540025,0.000094356656,0.000025618456,0.000004561166,0.000007996046,0.000009588559,0.0000019892275,0.00004577765,0.9991993,0.00024107186],"about_ca_topic_score_codex":0.0014473402,"about_ca_topic_score_gemma":0.00006321848,"teacher_disagreement_score":0.6583044,"about_ca_system_score_codex":0.00027441944,"about_ca_system_score_gemma":0.000018011739,"threshold_uncertainty_score":0.9940774},"labels":[],"label_agreement":null},{"id":"W4308376678","doi":"10.1175/bams-d-21-0209.1","title":"The Secondary Production of Ice in Cumulus Experiment (SPICULE)","year":2022,"lang":"en","type":"article","venue":"Bulletin of the American Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":28,"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":"Nuclear Safety and Security Commission; National Aeronautics and Space Administration; National Center for Atmospheric Research; National Science Foundation","keywords":"Coalescence (physics); Cloud base; Ice crystals; Ice cloud; Environmental science; Atmospheric sciences; Aerosol; Supercooling; Ice nucleus; Cloud computing; Geology; Meteorology; Nucleation; Materials science; Physics; Astrobiology; Computer science","score_opus":0.006850900109950483,"score_gpt":0.21736301608975184,"score_spread":0.21051211597980135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4308376678","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":[0.9898254,0.00016453286,0.00002198717,0.007831256,0.00013260556,0.00023030401,0.0000021037768,0.000010690089,0.0017811112],"genre_scores_gemma":[0.99555033,0.00006550278,0.0020692793,0.0012374058,0.000019916259,0.000083689294,4.1785603e-7,0.0000065271,0.0009669294],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9985358,0.00032663485,0.00027131784,0.00024627688,0.0003974577,0.00022251348],"domain_scores_gemma":[0.99913377,0.00015253825,0.00034749965,0.00033168314,0.0000058547257,0.000028676306],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007639322,0.00009948344,0.00020493103,4.3134577e-7,0.00032667632,0.000004039629,0.0005682189,0.000020133813,0.0031899577],"category_scores_gemma":[0.000094834555,0.00005423273,0.00021824718,0.0003136939,0.0013701572,0.00000796253,0.00092568697,0.00027150314,0.000010081141],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009966808,0.0023444705,0.22609745,0.000029020128,0.00021267384,0.0000053076305,0.007420033,0.05581452,0.22523804,0.00089695037,0.32406873,0.15687612],"study_design_scores_gemma":[0.0004584822,0.0010591475,0.47050476,0.0000041968196,0.000027459502,0.000007626079,0.014010923,0.00041876567,0.009189184,0.00055605266,0.5034992,0.0002642228],"about_ca_topic_score_codex":0.0010644364,"about_ca_topic_score_gemma":0.000007829266,"teacher_disagreement_score":0.2444073,"about_ca_system_score_codex":0.00013692342,"about_ca_system_score_gemma":0.000010888922,"threshold_uncertainty_score":0.99772125},"labels":[],"label_agreement":null},{"id":"W4308527095","doi":"10.1038/s41612-022-00312-z","title":"Faint yet widespread glories reflect microphysics of marine clouds","year":2022,"lang":"en","type":"article","venue":"npj Climate and Atmospheric Science","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Schwartz/Reisman Emergency Medicine Institute","funders":"European Commission; National Science Foundation","keywords":"Glory; Atmosphere (unit); Satellite; Physics; Atmospheric sciences; Geography; Astrophysics; Meteorology; Astronomy; Optics","score_opus":0.006575178372153467,"score_gpt":0.22355934974909789,"score_spread":0.21698417137694442,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4308527095","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":[0.97886837,0.0000828707,0.00015505352,0.00016653659,0.0003186537,0.00015128872,0.000011125153,0.000043102027,0.020202985],"genre_scores_gemma":[0.98446417,0.00016230965,0.014443467,0.00034235526,0.0000213838,0.000026516867,0.0000026577814,0.000015976506,0.000521183],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99783164,0.000043516535,0.00029927393,0.00055407675,0.0007086081,0.0005628851],"domain_scores_gemma":[0.9991954,0.00005970221,0.00019120495,0.00038913166,0.000019040854,0.00014551985],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00059220695,0.0001918628,0.00024835905,6.8769873e-7,0.00091431505,0.000054285083,0.0005653082,0.00002735673,0.003166145],"category_scores_gemma":[0.000041072886,0.00017108781,0.00005977895,0.0013487814,0.0015652871,0.00026839157,0.0022105875,0.00016965388,0.000035158642],"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":[0.00019320993,0.0004275589,0.42891312,0.00005785585,0.00002103077,0.000041217816,0.002995628,0.006687673,0.43614984,0.005224361,0.0023598664,0.116928644],"study_design_scores_gemma":[0.0025867529,0.0038270007,0.79531324,0.000070481525,0.00015840092,0.00025311764,0.012806149,0.03695419,0.05243509,0.016429396,0.076497905,0.0026682753],"about_ca_topic_score_codex":0.00065544405,"about_ca_topic_score_gemma":0.000019541752,"teacher_disagreement_score":0.38371477,"about_ca_system_score_codex":0.00017975575,"about_ca_system_score_gemma":0.000052416515,"threshold_uncertainty_score":0.9977451},"labels":[],"label_agreement":null},{"id":"W4308630672","doi":"10.5194/amt-15-6373-2022","title":"Sizing ice hydrometeor populations using the dual-wavelength radar ratio","year":2022,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"National Research Council Canada; Environment and Climate Change Canada","funders":"Federal Aviation Administration; National Oceanic and Atmospheric Administration","keywords":"Radar; Remote sensing; Environmental science; Rayleigh scattering; Wavelength; Optics; Meteorology; Atmospheric sciences; Physics; Geology","score_opus":0.05224138650647826,"score_gpt":0.25575355451763526,"score_spread":0.203512168011157,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4308630672","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":[0.8066551,0.000639329,0.17057395,0.0017427433,0.000621537,0.0023658106,0.0000099846375,0.0010674071,0.016324129],"genre_scores_gemma":[0.8653781,0.000017730863,0.13299797,0.0007551905,0.00007182127,0.00026992874,0.0000041309863,0.000045807075,0.0004593058],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.9967857,0.0002934575,0.0004405834,0.00047073144,0.001552668,0.00045686137],"domain_scores_gemma":[0.99897385,0.000031311916,0.00025688042,0.0006141195,0.000029595178,0.000094255476],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001439116,0.00027470166,0.0002278942,7.713996e-7,0.0016985047,0.00006594447,0.00047793012,0.000052199273,0.00431826],"category_scores_gemma":[0.000059276827,0.0002212204,0.0001301856,0.00081606157,0.00015553061,0.00021823187,0.0005821736,0.0003413598,0.000026813736],"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":[0.00014962305,0.0014523645,0.0893325,0.000049466005,0.0003082249,0.00010448704,0.004791344,0.033118907,0.5159494,0.005262349,0.054214697,0.29526663],"study_design_scores_gemma":[0.0016832905,0.0017253071,0.054056868,0.000108569104,0.00069813017,0.00041816937,0.007373158,0.1965194,0.041659273,0.011614905,0.68001133,0.0041316045],"about_ca_topic_score_codex":0.001471852,"about_ca_topic_score_gemma":0.00007641736,"teacher_disagreement_score":0.6257966,"about_ca_system_score_codex":0.0011211667,"about_ca_system_score_gemma":0.000053097527,"threshold_uncertainty_score":0.9996011},"labels":[],"label_agreement":null},{"id":"W4309377602","doi":"10.5194/egusphere-2022-1217","title":"The classification of atmospheric hydrometeors and aerosols from the EarthCARE radar and lidar: the A-TC, C-TC and AC-TC products","year":2022,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Natural Environment Research Council; Sight Research UK; European Space Agency","keywords":"Lidar; Remote sensing; Radar; Snow; Environmental science; Aerosol; Meteorology; Atmosphere (unit); Precipitation; Atmospheric sciences; Geology; Computer science; Geography","score_opus":0.013004960212133805,"score_gpt":0.2175028640690398,"score_spread":0.204497903856906,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4309377602","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":[0.98335975,0.0054196855,0.00010607868,0.007220806,0.0002557797,0.0011079939,0.000039333794,0.000037386806,0.0024531987],"genre_scores_gemma":[0.99083614,0.0036686473,0.0024753774,0.0002860053,0.00008800519,0.00014223366,0.000018769422,0.000035193847,0.0024496512],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99743843,0.000313375,0.00041196131,0.0008620121,0.00066285144,0.00031137376],"domain_scores_gemma":[0.99792373,0.00044020006,0.0003694286,0.0011555935,0.000019062578,0.00009199146],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007378673,0.0003565443,0.00032704233,4.991808e-7,0.00096913654,0.00022579587,0.0007226052,0.0001599937,0.0007811058],"category_scores_gemma":[0.000112262554,0.00017387298,0.00006800872,0.00024299133,0.0013678401,0.00009959104,0.0026640147,0.0006519136,0.0000072486987],"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":[0.0003183727,0.00028978015,0.657248,0.00021895622,0.00066893536,0.00001320924,0.019933846,0.0011166746,0.03442017,0.0025101039,0.022562468,0.26069945],"study_design_scores_gemma":[0.000335193,0.00014900195,0.940018,0.00003752842,0.00014860329,0.0000125156785,0.008862298,0.002800929,0.0005126932,0.002233489,0.04441004,0.00047973447],"about_ca_topic_score_codex":0.0019062179,"about_ca_topic_score_gemma":0.0003562687,"teacher_disagreement_score":0.28276995,"about_ca_system_score_codex":0.00006588834,"about_ca_system_score_gemma":0.00004524632,"threshold_uncertainty_score":0.855256},"labels":[],"label_agreement":null},{"id":"W4310289578","doi":"10.5194/egusphere-2022-1241","title":"HETEAC – The Hybrid End-To-End Aerosol Classification model for EarthCARE","year":2022,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":12,"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":"European Space Agency","keywords":"Aerosol; Radiative transfer; Environmental science; Remote sensing; Lidar; Radiative forcing; Atmospheric sciences; Troposphere; Mode (computer interface); Meteorology; Computer science; Physics; Geology; Optics","score_opus":0.03970189315229423,"score_gpt":0.2719971706317701,"score_spread":0.23229527747947587,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4310289578","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":[0.5218224,0.00009283201,0.40801728,0.009901503,0.00088626915,0.0036951285,0.00042987376,0.0002533342,0.054901425],"genre_scores_gemma":[0.95026433,0.0000293885,0.0126434,0.0016526022,0.000091429385,0.0014192624,0.00013646155,0.000046100915,0.033717044],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9979143,0.000059240483,0.0003087362,0.0008029264,0.0005395983,0.0003752061],"domain_scores_gemma":[0.9986534,0.00006275856,0.00015092736,0.000985918,0.00001287411,0.0001341022],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00033353246,0.00028581772,0.00022581231,0.0000014068801,0.00046373208,0.000088344204,0.00091914507,0.000104435814,0.012177001],"category_scores_gemma":[0.000027467351,0.0002079507,0.00022521216,0.00009711349,0.00013334032,0.000058675814,0.0019975686,0.00046556722,0.0002396435],"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":[0.000068609785,0.00016061123,0.004748244,0.000045628738,0.00006041626,0.0000027606259,0.00195163,0.8346639,0.0034325211,0.0018034094,0.0989592,0.05410307],"study_design_scores_gemma":[0.00018247058,0.0000783501,0.00564681,0.000008738459,0.000048143214,0.0000030318051,0.0008230174,0.9462615,0.000473284,0.0022788458,0.04363898,0.00055680407],"about_ca_topic_score_codex":0.0004927814,"about_ca_topic_score_gemma":0.0002641144,"teacher_disagreement_score":0.42844194,"about_ca_system_score_codex":0.00031171742,"about_ca_system_score_gemma":0.000051689985,"threshold_uncertainty_score":0.988726},"labels":[],"label_agreement":null},{"id":"W4310372168","doi":"10.5194/egusphere-2022-1284","title":"Processing reflectivity and Doppler velocity from EarthCARE’s cloud profiling radar: the C-FMR, C-CD and C-APC products","year":2022,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":10,"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; McGill University","funders":"Natural Environment Research Council; Sight Research UK; European Space Agency","keywords":"Doppler effect; Remote sensing; Radar; Attenuation; Geology; Optics; Physics; Computer science; Telecommunications","score_opus":0.019717494081785265,"score_gpt":0.248338601550014,"score_spread":0.22862110746822872,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4310372168","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":[0.98787296,0.001236659,0.00068311725,0.001981331,0.00037980048,0.0008977093,0.000029191273,0.00011864471,0.0068006124],"genre_scores_gemma":[0.9777482,0.00018187008,0.01912097,0.00038888663,0.00026053342,0.00012530685,0.000029037832,0.00004020004,0.0021049618],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9973518,0.00019584844,0.00028789218,0.0012415963,0.00054202665,0.00038080526],"domain_scores_gemma":[0.9989778,0.00007144944,0.00022046734,0.0005958511,0.00001645717,0.0001179843],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006137264,0.00037844855,0.0003553809,0.0000017421191,0.00078851834,0.00022812247,0.00038391285,0.0001860538,0.0015106886],"category_scores_gemma":[0.00007028478,0.00026467408,0.000050545535,0.00019698846,0.00047513001,0.0001485174,0.0037799662,0.0010484261,0.000011172602],"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":[0.00024378739,0.00037094747,0.7576797,0.0004996228,0.00019752857,0.00004870365,0.01099138,0.0018626761,0.013042541,0.00030559552,0.008569627,0.2061879],"study_design_scores_gemma":[0.00096539286,0.0002116822,0.9270388,0.00014688271,0.0002611668,0.00006265364,0.0040382133,0.011448455,0.006353173,0.013034727,0.03412597,0.002312872],"about_ca_topic_score_codex":0.0056811776,"about_ca_topic_score_gemma":0.0006696534,"teacher_disagreement_score":0.20387502,"about_ca_system_score_codex":0.00017958098,"about_ca_system_score_gemma":0.00008948786,"threshold_uncertainty_score":0.99998057},"labels":[],"label_agreement":null},{"id":"W4310493112","doi":"10.5194/acp-2022-492-ac1","title":"Reply on RC1","year":2022,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Université du Québec en Abitibi-Témiscamingue","funders":"National Key Research and Development Program of China; National Natural Science Foundation of China","keywords":"Span (engineering); Precipitation; Atmospheric sciences; Meteorology; Environmental science; Geology; Physics","score_opus":0.018452288800312036,"score_gpt":0.2651782121851479,"score_spread":0.2467259233848359,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4310493112","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000047844806,0.0027054334,0.000025472167,0.059435334,0.0014389819,0.0003202119,0.000035226913,0.00007879509,0.9359127],"genre_scores_gemma":[0.000047009034,0.0031150281,0.00040830302,0.09726066,0.00011494103,0.00008049447,0.00012804566,0.000030318068,0.8988152],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9981883,0.00004642187,0.00023276696,0.0005386982,0.0007420604,0.00025173192],"domain_scores_gemma":[0.9990824,0.000031355772,0.00012252349,0.00067054527,0.0000028320337,0.00009034104],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00023787633,0.00023369763,0.0003140302,4.525079e-7,0.00013509319,0.000012399685,0.00049372035,0.00007121732,0.67835915],"category_scores_gemma":[0.000036766924,0.0001812263,0.00016262979,0.0001792862,0.00006761763,0.000024744435,0.00055009045,0.00041568722,0.0070448546],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000015809115,0.000032040483,0.00005935234,0.000055378285,0.000006008013,0.0000118224125,0.000006362411,0.00003299119,8.970309e-7,0.00003741573,0.9857086,0.014047548],"study_design_scores_gemma":[0.000044272365,0.0001005218,0.00020259227,0.00009451188,0.000025630281,0.000004563573,0.0000080195505,0.000010048276,0.0000019600313,0.000046222714,0.99922043,0.00024123168],"about_ca_topic_score_codex":0.0015361527,"about_ca_topic_score_gemma":0.000060520633,"teacher_disagreement_score":0.6713143,"about_ca_system_score_codex":0.00027860515,"about_ca_system_score_gemma":0.000018102455,"threshold_uncertainty_score":0.9937283},"labels":[],"label_agreement":null},{"id":"W4310904787","doi":"10.5194/amt-2022-284-ac1","title":"Reply on RC1","year":2022,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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 Sherbrooke","funders":"Natural Sciences and Engineering Research Council of Canada; Goddard Space Flight Center; Brookhaven National Laboratory; Environment and Climate Change Canada; Strong; National Aeronautics and Space Administration","keywords":"AERONET; Aerosol; Cutoff; Effective radius; RADIUS; Radiance; Mathematics; Physics; Astrophysics; Optics; Meteorology; Galaxy","score_opus":0.018452288800312036,"score_gpt":0.2651782121851479,"score_spread":0.2467259233848359,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4310904787","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000047844806,0.0027054334,0.000025472167,0.059435334,0.0014389819,0.0003202119,0.000035226913,0.00007879509,0.9359127],"genre_scores_gemma":[0.000047009034,0.0031150281,0.00040830302,0.09726066,0.00011494103,0.00008049447,0.00012804566,0.000030318068,0.8988152],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9981883,0.00004642187,0.00023276696,0.0005386982,0.0007420604,0.00025173192],"domain_scores_gemma":[0.9990824,0.000031355772,0.00012252349,0.00067054527,0.0000028320337,0.00009034104],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00023787633,0.00023369763,0.0003140302,4.525079e-7,0.00013509319,0.000012399685,0.00049372035,0.00007121732,0.67835915],"category_scores_gemma":[0.000036766924,0.0001812263,0.00016262979,0.0001792862,0.00006761763,0.000024744435,0.00055009045,0.00041568722,0.0070448546],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000015809115,0.000032040483,0.00005935234,0.000055378285,0.000006008013,0.0000118224125,0.000006362411,0.00003299119,8.970309e-7,0.00003741573,0.9857086,0.014047548],"study_design_scores_gemma":[0.000044272365,0.0001005218,0.00020259227,0.00009451188,0.000025630281,0.000004563573,0.0000080195505,0.000010048276,0.0000019600313,0.000046222714,0.99922043,0.00024123168],"about_ca_topic_score_codex":0.0015361527,"about_ca_topic_score_gemma":0.000060520633,"teacher_disagreement_score":0.6713143,"about_ca_system_score_codex":0.00027860515,"about_ca_system_score_gemma":0.000018102455,"threshold_uncertainty_score":0.9937283},"labels":[],"label_agreement":null},{"id":"W4311225960","doi":"10.5194/egusphere-2022-1292","title":"Parameterization of Size of Organic and Secondary Inorganic Aerosol for Efficient Representation of Global Aerosol Optical Properties","year":2022,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"Dalhousie University","funders":"Nuclear Safety and Security Commission; National Aeronautics and Space Administration; National Science Foundation","keywords":"Aerosol; AERONET; Environmental science; Ammonium sulfate; Atmospheric sciences; Chemical transport model; Sulfate; RADIUS; Effective radius; Meteorology; Chemistry; Physics; Computer science","score_opus":0.015037333407838489,"score_gpt":0.24117640684175032,"score_spread":0.22613907343391182,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4311225960","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":[0.9888405,0.00009389419,0.008403138,0.000063253945,0.00014782268,0.0010498929,0.0000783798,0.00002062614,0.0013024742],"genre_scores_gemma":[0.9898851,0.000038697828,0.009699791,0.000025778567,0.000011769557,0.00007439176,0.000022215356,0.000020752042,0.00022154082],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9981402,0.000068987705,0.00069721526,0.0004925459,0.0004156017,0.00018546224],"domain_scores_gemma":[0.99887115,0.00010199216,0.00051513856,0.00040933702,0.000040274615,0.00006208027],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00019006552,0.00021234214,0.00050205115,0.000001663774,0.000059405553,0.000013605848,0.0002648677,0.000159573,0.002875914],"category_scores_gemma":[0.00020572534,0.00018492939,0.00012062101,0.00024163372,0.00042925202,0.00004988701,0.0013880152,0.00014758576,0.0000017134673],"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":[0.0003960516,0.00064058235,0.082841404,0.0010869079,0.00013550535,8.9614474e-7,0.0013087074,0.031164397,0.87915677,0.0002941116,0.00018350467,0.0027911535],"study_design_scores_gemma":[0.0020251067,0.0014573534,0.13486347,0.0001664272,0.00036124195,0.0000122166875,0.0029943879,0.020959087,0.83551794,0.000810305,0.000017579981,0.00081487384],"about_ca_topic_score_codex":0.00030236543,"about_ca_topic_score_gemma":0.000044391323,"teacher_disagreement_score":0.052022062,"about_ca_system_score_codex":0.00016815796,"about_ca_system_score_gemma":0.000100804056,"threshold_uncertainty_score":0.9980356},"labels":[],"label_agreement":null},{"id":"W4312120386","doi":"10.5194/amt-2022-262-rc2","title":"Comment on amt-2022-262","year":2022,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Mount Allison University","funders":"HORIZON EUROPE Excellent Science; Supercomputing Center for Education and Research, University of Oklahoma; Horizon 2020 Framework Programme; University of Oklahoma; National Aeronautics and Space Administration; U.S. Department of Energy","keywords":"Aerosol; Cloud condensation nuclei; Lidar; Environmental science; Atmospheric sciences; In situ; Extinction (optical mineralogy); Backscatter (email); Remote sensing; Relative humidity; Meteorology; Chemistry; Geology; Geography; Mineralogy; Computer science","score_opus":0.018811217697970107,"score_gpt":0.26624867935396523,"score_spread":0.24743746165599512,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4312120386","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00003177111,0.0035785986,0.0000701199,0.28452384,0.002113258,0.0005838995,0.000092870105,0.00008587875,0.70891976],"genre_scores_gemma":[0.000059327816,0.0054143732,0.00042359068,0.21799193,0.00012018789,0.00017443755,0.0003306617,0.000040521612,0.775445],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99760044,0.000088594265,0.00031221574,0.0005881294,0.0010526067,0.00035803314],"domain_scores_gemma":[0.99894,0.000052049214,0.00015757832,0.00070853677,0.000003880822,0.0001379726],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00032780404,0.00033833887,0.0004379143,8.870355e-7,0.00021691153,0.000019470775,0.0006902163,0.00011051672,0.64453065],"category_scores_gemma":[0.000020089792,0.0002686495,0.0002130294,0.00021938265,0.00009067231,0.000028396233,0.0009900399,0.0005879763,0.0053258254],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002504496,0.00009788333,0.00008206765,0.00008119628,0.000013531421,0.000011651371,0.000012693581,0.00003729698,0.0000011083935,0.00014591879,0.98685193,0.012662195],"study_design_scores_gemma":[0.00009611672,0.00016078417,0.00012441601,0.0001276606,0.000042939424,0.0000030520694,0.000022563285,0.000024512086,0.0000033685446,0.000065697095,0.9989882,0.00034069977],"about_ca_topic_score_codex":0.0013972152,"about_ca_topic_score_gemma":0.00011941691,"teacher_disagreement_score":0.63920486,"about_ca_system_score_codex":0.00058744935,"about_ca_system_score_gemma":0.00002036831,"threshold_uncertainty_score":0.9999766},"labels":[],"label_agreement":null},{"id":"W4313476683","doi":"10.5194/acp-2022-751-supplement","title":"Supplementary material to \"Measurement Report: Rapid decline of aerosol absorption coefficient and aerosol optical properties effects on radiative forcing in urban areas of Beijing from 2018 to 2021\"","year":2023,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Science North","funders":"","keywords":"Aerosol; Beijing; Radiative forcing; Environmental science; Radiative transfer; Forcing (mathematics); Atmospheric sciences; Absorption (acoustics); Attenuation coefficient; Meteorology; Materials science; Geography; Physics; Optics; China","score_opus":0.02418383219120204,"score_gpt":0.23987836663611134,"score_spread":0.2156945344449093,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313476683","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":[0.99234486,0.000029377145,0.003824228,0.00052928587,0.00068509026,0.0022031807,0.00019922512,0.000023302922,0.000161467],"genre_scores_gemma":[0.99430066,0.000026997906,0.004793492,0.00015722253,0.00015335965,0.00026836997,0.00014502746,0.000044338707,0.000110499124],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99636286,0.00011951544,0.0010508928,0.0009807429,0.0010580159,0.00042795695],"domain_scores_gemma":[0.99874645,0.00008779948,0.00034894896,0.0005518183,0.00003707687,0.0002278778],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008614013,0.00042188892,0.00075078994,0.000017057702,0.00006535204,0.000045036653,0.00027850372,0.00018154032,0.0013756667],"category_scores_gemma":[0.00019048531,0.00034566363,0.00010750348,0.00022254947,0.00013164103,0.000050084913,0.0018367097,0.00021766676,0.00002690087],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0019090545,0.000872476,0.25000706,0.00057027134,0.00024554427,0.00012679702,0.0061113094,0.1236873,0.603419,0.000012370499,0.0066858586,0.0063529667],"study_design_scores_gemma":[0.0018264775,0.0020757734,0.17629819,0.0024084114,0.00016016072,0.000004215878,0.0010892573,0.0063666315,0.8085088,0.00007228667,0.00010661193,0.001083156],"about_ca_topic_score_codex":0.0083591845,"about_ca_topic_score_gemma":0.0023622357,"teacher_disagreement_score":0.20508982,"about_ca_system_score_codex":0.0005874442,"about_ca_system_score_gemma":0.000049125323,"threshold_uncertainty_score":0.99989957},"labels":[],"label_agreement":null},{"id":"W4313487081","doi":"10.5194/egusphere-2022-1241-rc1","title":"Comment on egusphere-2022-1241","year":2023,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"","keywords":"Aerosol; Radiative transfer; Remote sensing; Environmental science; Troposphere; Radiative forcing; Meteorology; Mode (computer interface); Lidar; Atmospheric sciences; Computer science; Physics; Geology; Optics","score_opus":0.024463589318254854,"score_gpt":0.2773156230606338,"score_spread":0.2528520337423789,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313487081","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000040210958,0.002455482,0.00012697361,0.32874328,0.0031122128,0.00073574233,0.000083465624,0.00029509095,0.66440755],"genre_scores_gemma":[0.00003576784,0.0066537806,0.00047078772,0.11831246,0.00020603568,0.00011442343,0.00022282252,0.000075557735,0.87390834],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99747497,0.000062390616,0.00038005406,0.00067349605,0.00094289746,0.00046620032],"domain_scores_gemma":[0.9987818,0.00008733479,0.00016123003,0.00078060466,0.0000076023707,0.0001814306],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00032732205,0.000419007,0.0005319997,8.885432e-7,0.00013226594,0.000029185305,0.0006522069,0.00023178934,0.18794411],"category_scores_gemma":[0.000041993488,0.00031752454,0.0002379653,0.00033142217,0.00011855486,0.00003323208,0.0006376194,0.00047248873,0.046751305],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002177692,0.00006192691,0.00008272146,0.0001492038,0.000019877023,0.0000148143135,0.000009462429,0.0000284586,0.0000014226235,0.000097207274,0.9825256,0.017007163],"study_design_scores_gemma":[0.000109620494,0.000113599344,0.00025802018,0.0005721826,0.000049512553,0.0000015555084,0.00001910865,0.00004692623,0.0000067082033,0.0001319839,0.9982951,0.00039566198],"about_ca_topic_score_codex":0.002253373,"about_ca_topic_score_gemma":0.0007153853,"teacher_disagreement_score":0.21043083,"about_ca_system_score_codex":0.000369123,"about_ca_system_score_gemma":0.000021759583,"threshold_uncertainty_score":0.9999277},"labels":[],"label_agreement":null},{"id":"W4313508364","doi":"10.3390/rs15010029","title":"Stratospheric Aerosol Characteristics from the 2017–2019 Volcanic Eruptions Using the SAGE III/ISS Observations","year":2022,"lang":"en","type":"article","venue":"Remote Sensing","topic":"Atmospheric aerosols and clouds","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":"Agence Nationale de la Recherche","keywords":"Aerosol; Environmental science; Atmospheric sciences; Volcano; Effective radius; Stratosphere; Forcing (mathematics); Vulcanian eruption; Climatology; Meteorology; Geology; Physics; Astrophysics","score_opus":0.029895710235293853,"score_gpt":0.23763732770449258,"score_spread":0.20774161746919872,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313508364","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":[0.95430535,0.00012762101,0.042914286,0.0012486412,0.00047319202,0.00028201158,0.000057643374,0.000054943965,0.00053628534],"genre_scores_gemma":[0.98766506,0.00004193543,0.009397612,0.001564778,0.0002066376,1.8560742e-7,0.000030321951,0.00003256305,0.0010609147],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9984206,0.0001796969,0.00028914856,0.0003231174,0.00043298694,0.0003544662],"domain_scores_gemma":[0.9989198,0.00016289059,0.00020834745,0.00063081173,0.000010720801,0.000067468856],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00025827164,0.00018260098,0.00016186535,7.382631e-7,0.0022801051,0.00010581272,0.00038222029,0.000044760323,0.0010820159],"category_scores_gemma":[0.000032565455,0.00012876854,0.000101649515,0.0004451458,0.00021020336,0.00011289799,0.0004873197,0.00041715754,0.000064044354],"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":[0.00008015057,0.00020383956,0.021859078,0.000008852367,0.0002444513,0.00015505099,0.01336341,0.1297035,0.56595683,0.00013198853,0.017920537,0.25037232],"study_design_scores_gemma":[0.00034909832,0.00004709303,0.090976536,0.00003070465,0.00015292429,0.000103271974,0.0048266673,0.8838811,0.000208354,0.0004136656,0.018512698,0.0004978925],"about_ca_topic_score_codex":0.005308506,"about_ca_topic_score_gemma":0.00052600785,"teacher_disagreement_score":0.7541776,"about_ca_system_score_codex":0.00028360053,"about_ca_system_score_gemma":0.000046059202,"threshold_uncertainty_score":0.99983114},"labels":[],"label_agreement":null},{"id":"W4313646454","doi":"10.4209/aaqr.220309","title":"A Synoptic- and Remote Sensing-based Analysis of a Severe Dust Storm Event over Central Asia","year":2023,"lang":"en","type":"article","venue":"Aerosol and Air Quality Research","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":24,"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":"Iran National Science Foundation; National Aeronautics and Space Administration; National Science Foundation","keywords":"Dust storm; Storm; HYSPLIT; Anticyclone; Climatology; Aeolian processes; Desertification; Central asia; Subsidence; Environmental science; Geology; Meteorology; Structural basin; Physical geography; Geography; Aerosol; Oceanography; Geomorphology","score_opus":0.04828207044734548,"score_gpt":0.3536722883490661,"score_spread":0.3053902179017206,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313646454","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":[0.99751276,0.000052201576,0.00044836904,0.001030611,0.00002201437,0.00019081435,0.000026475014,0.00003419688,0.0006825385],"genre_scores_gemma":[0.99793255,0.000071433824,0.0006512442,0.00011016554,0.000018698938,0.0000014682007,0.000014654257,0.000011912828,0.0011878655],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9974423,0.00032635895,0.00030547677,0.00045170097,0.0008874854,0.00058669556],"domain_scores_gemma":[0.99899286,0.00031030254,0.000072824565,0.0003429179,0.00003059019,0.00025051658],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017054244,0.00013891308,0.00032526487,0.000014964439,0.00026144626,0.000035462224,0.00013802748,0.00010037154,0.0004935332],"category_scores_gemma":[0.00014407375,0.00011817071,0.00012660037,0.0016792717,0.0005981471,0.0000809527,0.00033692783,0.0002432273,0.000032659696],"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":[0.00048753325,0.0002897535,0.8464785,0.00029725948,0.000843195,0.00009553114,0.0044402806,0.008992289,0.02396652,0.00023672749,0.0062474064,0.10762499],"study_design_scores_gemma":[0.00042708198,0.00013051281,0.9251119,0.000027137556,0.00007976721,0.0000018658168,0.0011174642,0.071965955,0.00048257716,0.00011758071,0.00035626403,0.00018187218],"about_ca_topic_score_codex":0.0073450846,"about_ca_topic_score_gemma":0.0022443351,"teacher_disagreement_score":0.10744312,"about_ca_system_score_codex":0.000100067715,"about_ca_system_score_gemma":0.00003600059,"threshold_uncertainty_score":0.9992651},"labels":[],"label_agreement":null},{"id":"W4313812340","doi":"10.5194/egusphere-2022-1217-rc1","title":"Comment on egusphere-2022-1217","year":2023,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Lidar; Remote sensing; Radar; Snow; Environmental science; Aerosol; Meteorology; Precipitation; Atmosphere (unit); Atmospheric sciences; Geology; Computer science; Geography","score_opus":0.024892315060571272,"score_gpt":0.27853292602126417,"score_spread":0.2536406109606929,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313812340","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000040243824,0.002270929,0.00012225001,0.32752877,0.0030995002,0.00072254485,0.00008261106,0.00028391147,0.6658492],"genre_scores_gemma":[0.0000384287,0.006447889,0.0004585714,0.11542543,0.00020748487,0.0001139847,0.00022367093,0.00007488076,0.87700963],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9974853,0.00006159877,0.00037653188,0.0006728223,0.00093887973,0.0004648771],"domain_scores_gemma":[0.9987642,0.000086542146,0.0001640994,0.0007968394,0.0000075908265,0.00018072719],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00032754918,0.00041814015,0.0005321293,8.804048e-7,0.00013705634,0.00003002778,0.00066977355,0.00023149475,0.18642451],"category_scores_gemma":[0.0000429158,0.00031700893,0.0002412224,0.00031759427,0.00012110619,0.000033491044,0.0006473525,0.00047161622,0.04748317],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000022259512,0.0000612715,0.00008299151,0.00015091254,0.000019883712,0.000015682861,0.000009877196,0.00002731329,0.0000013629576,0.00009669254,0.9824406,0.017091168],"study_design_scores_gemma":[0.00011001639,0.00011352604,0.00027487936,0.0005811137,0.000048832637,0.0000015981985,0.000018823643,0.00004462551,0.000006666239,0.00013117214,0.99827385,0.0003948801],"about_ca_topic_score_codex":0.0022173885,"about_ca_topic_score_gemma":0.00067418383,"teacher_disagreement_score":0.21210335,"about_ca_system_score_codex":0.00036321735,"about_ca_system_score_gemma":0.000021592225,"threshold_uncertainty_score":0.9999282},"labels":[],"label_agreement":null},{"id":"W4313830822","doi":"10.1029/2022gl100247","title":"Understanding the History of Two Complex Ice Crystal Habits Deduced From a Holographic Imager","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":14,"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":"HORIZON EUROPE European Research Council; Swiss Polar Institute; Horizon 2020 Framework Programme; Deutsche Forschungsgemeinschaft; EEA Grants/Norway Grants; European Commission; EEA Grants; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; National Science Foundation","keywords":"Ice crystals; Atmospheric sciences; Aerosol; Radiative transfer; Precipitation; Materials science; Crystal (programming language); Arctic; Ice core; Arctic ice pack; Geology; Sea ice; Environmental science; Climatology; Meteorology; Optics; Physics; Oceanography","score_opus":0.14214586129878304,"score_gpt":0.3217222831446394,"score_spread":0.17957642184585637,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313830822","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":[0.98956376,0.000014705976,0.0011677899,0.005513543,0.000143246,0.00019741587,0.000008359598,0.00005036801,0.003340784],"genre_scores_gemma":[0.99776506,0.0000071231357,0.00027140082,0.00093528803,0.00010763411,0.000028333598,0.000010362923,0.000019070278,0.0008557303],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9975387,0.00029134203,0.00016502663,0.000365153,0.0010199875,0.00061981415],"domain_scores_gemma":[0.9987411,0.00068051665,0.000050306116,0.0003888884,0.000012108617,0.0001270721],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005034401,0.00012136192,0.00016425275,0.0000081201615,0.00021948821,0.000023025304,0.0005312921,0.000034199144,0.0010621338],"category_scores_gemma":[0.00008697739,0.00008843382,0.00012143045,0.0008339917,0.0020448484,0.00010859689,0.0005060329,0.0004250719,0.0006885462],"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":[0.000029985365,0.000049333477,0.0061364844,0.000004293832,0.000021191878,0.000027330007,0.0009585499,0.00021476652,0.827052,0.00032032194,0.16485396,0.00033178736],"study_design_scores_gemma":[0.0011941312,0.00021886994,0.9561003,0.000036475463,0.000029760067,0.000002086921,0.0020928863,0.010597418,0.0010674143,0.01681354,0.011376413,0.0004707203],"about_ca_topic_score_codex":0.0034443962,"about_ca_topic_score_gemma":0.000077577664,"teacher_disagreement_score":0.9499638,"about_ca_system_score_codex":0.00056941435,"about_ca_system_score_gemma":0.000029696543,"threshold_uncertainty_score":0.99985105},"labels":[],"label_agreement":null},{"id":"W4316371783","doi":"10.5194/egusphere-2022-1156","title":"The importance of detection thresholds for the quantification of source and timing of high-latitude dust emission using remote sensing","year":2023,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; University of Sheffield","keywords":"AERONET; Environmental science; Remote sensing; Albedo (alchemy); Aerosol; Mineral dust; Satellite; Meteorology; Cloud cover; Geology; Geography; Cloud computing; Physics","score_opus":0.05190905988431722,"score_gpt":0.2864046152163157,"score_spread":0.2344955553319985,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4316371783","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":[0.5601135,0.000067522225,0.43936145,0.00009075552,0.00008990063,0.0002382357,0.0000023926625,0.000009152395,0.000027067565],"genre_scores_gemma":[0.9760244,0.00013414591,0.023492841,0.0000073212823,0.000023187493,0.0000010344584,0.0000018738654,0.000017549904,0.0002976751],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9989563,0.000027975408,0.00041722984,0.00025165602,0.00022912347,0.00011767607],"domain_scores_gemma":[0.998643,0.00025277247,0.0006489514,0.00040792636,0.000026643023,0.000020700254],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006134049,0.000115581606,0.00018634133,0.0000017898394,0.00022167033,0.000015045867,0.00016258354,0.00012195282,0.000012922889],"category_scores_gemma":[0.000088483546,0.00006899778,0.00006782218,0.000111496396,0.0002683849,0.00003093189,0.00036950802,0.00012370947,3.1329685e-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":[0.00009160415,0.000017087761,0.024342773,0.0002479081,0.000067603425,2.3518007e-7,0.0007886299,0.41055924,0.41236743,0.00005950709,0.00009223503,0.15136573],"study_design_scores_gemma":[0.00008760814,0.00002239188,0.027997553,0.00012611793,0.000063620304,0.0000018478936,0.00057733624,0.9085079,0.06120042,0.0012697496,0.000049870625,0.000095575735],"about_ca_topic_score_codex":0.0035365138,"about_ca_topic_score_gemma":0.00070432236,"teacher_disagreement_score":0.49794868,"about_ca_system_score_codex":0.000046439352,"about_ca_system_score_gemma":0.000014090228,"threshold_uncertainty_score":0.5346175},"labels":[],"label_agreement":null},{"id":"W4317103661","doi":"10.5194/egusphere-2023-56","title":"Cloud and Precipitation Microphysical Retrievals from the EarthCARE Cloud Profiling Radar: the C-CLD product","year":2023,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","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":"McGill University","funders":"National Centre for Earth Observation; Natural Environment Research Council; University of Leicester; Sight Research UK; European Space Agency","keywords":"Environmental science; Meteorology; Radar; Drizzle; Cloud computing; Grid; Satellite; Doppler radar; Remote sensing; Precipitation; Computer science; Geography; Geodesy; Aerospace engineering","score_opus":0.023432732548337398,"score_gpt":0.24634346994797565,"score_spread":0.22291073739963826,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4317103661","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":[0.9858028,0.00047600636,0.00067024294,0.008871254,0.0014973027,0.0013965202,0.00006160539,0.00014804912,0.0010761913],"genre_scores_gemma":[0.983035,0.00026580002,0.00489072,0.00061342405,0.0019382808,0.00010716793,0.0000705926,0.00006889068,0.009010067],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9974454,0.000244476,0.0003543502,0.00094025396,0.0006763278,0.00033915782],"domain_scores_gemma":[0.99838305,0.00035356573,0.00020683104,0.00095618103,0.000021552607,0.000078833],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005649342,0.00033765155,0.00028793528,8.620285e-7,0.00041278498,0.0002077005,0.00068470713,0.00018394622,0.00043561216],"category_scores_gemma":[0.00017028495,0.0001786764,0.00013375247,0.0002165345,0.00048586607,0.00006566397,0.002016137,0.00080330734,0.00035406873],"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":[0.0006579969,0.0005322182,0.46669865,0.00035012577,0.0010469245,0.000058297082,0.03340222,0.01055494,0.122298606,0.0038785632,0.24169719,0.11882426],"study_design_scores_gemma":[0.0011571528,0.0004281044,0.80200315,0.00046659147,0.00064689154,0.000014187996,0.009375338,0.009252389,0.06297457,0.058010608,0.052840356,0.0028306746],"about_ca_topic_score_codex":0.0015770089,"about_ca_topic_score_gemma":0.00014221466,"teacher_disagreement_score":0.33530447,"about_ca_system_score_codex":0.00007517152,"about_ca_system_score_gemma":0.000040181265,"threshold_uncertainty_score":0.72862124},"labels":[],"label_agreement":null},{"id":"W4317739110","doi":"10.3390/rs15030641","title":"Study on the Boundary Layer of the Haze at Xianyang Airport Based on Multi-Source Detection Data","year":2023,"lang":"en","type":"article","venue":"Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Royal Military College of Canada","funders":"","keywords":"Haze; Environmental science; Microwave radiometer; Planetary boundary layer; Wind speed; Atmospheric sciences; Meteorology; Relative humidity; Sensible heat; Sink (geography); Remote sensing; Radiometer; Turbulence; Geography; Geology","score_opus":0.05982202507394435,"score_gpt":0.2737161852625033,"score_spread":0.21389416018855895,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4317739110","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":[0.9941142,0.0000025763568,0.003266803,0.0006550679,0.00019129751,0.00031048764,0.0000035064613,0.000055162815,0.0014009],"genre_scores_gemma":[0.9971647,0.0000010683549,0.00035330313,0.00048803273,0.00003646301,2.5189037e-8,0.0000022958643,0.00002159433,0.0019324891],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9987668,0.00013777589,0.00015255893,0.00031962685,0.0004293989,0.00019385702],"domain_scores_gemma":[0.99870497,0.000097367505,0.00010451222,0.0010562027,0.0000047742124,0.00003219682],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005172041,0.00011691373,0.00010135043,0.0000019021896,0.0004915597,0.000023016291,0.0002931281,0.000040839885,0.000049200644],"category_scores_gemma":[0.00009733879,0.000067590525,0.000049473838,0.00034367948,0.0001384259,0.000038031958,0.0004763639,0.00015890977,0.00021589907],"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":[0.00019727909,0.00035026876,0.03558423,0.000017229699,0.00007727544,0.000098348726,0.004607126,0.14511694,0.19856766,0.000001545448,0.005362721,0.6100194],"study_design_scores_gemma":[0.0002453022,0.00007466282,0.17016494,0.000033477558,0.000020765074,0.000005265676,0.0010065297,0.81701505,0.0073537687,0.0000061991555,0.003962187,0.00011185994],"about_ca_topic_score_codex":0.0005834931,"about_ca_topic_score_gemma":0.0005452455,"teacher_disagreement_score":0.6718981,"about_ca_system_score_codex":0.0001274626,"about_ca_system_score_gemma":0.000010311276,"threshold_uncertainty_score":0.37807295},"labels":[],"label_agreement":null},{"id":"W4318425567","doi":"10.1007/s00376-022-2077-3","title":"Parameterization and Explicit Modeling of Cloud Microphysics: Approaches, Challenges, and Future Directions","year":2023,"lang":"en","type":"article","venue":"Advances in Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Brookhaven National Laboratory; Office of Energy Efficiency; Solar Energy Technologies Office; Office of Science; Japan Society for the Promotion of Science; Biological and Environmental Research; Laboratory Directed Research and Development; Office of Energy Efficiency and Renewable Energy; U.S. Department of Energy","keywords":"Meteorology; Turbulence; Statistical physics; Cloud physics; Bin; Cloud computing; Large eddy simulation; Environmental science; Physics; Computer science","score_opus":0.03022948509853511,"score_gpt":0.2435627509893501,"score_spread":0.21333326589081497,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4318425567","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":[0.97380245,0.019722635,0.001172294,0.0002511942,0.00021512408,0.00014456855,0.0000011624733,0.000046184625,0.0046443734],"genre_scores_gemma":[0.89072794,0.08790455,0.021189645,0.000025700376,0.00007133183,0.00002826895,0.0000010579602,0.000008584493,0.000042920503],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9988975,0.00003575274,0.00019608451,0.00042115749,0.00021392104,0.0002356188],"domain_scores_gemma":[0.9996893,0.00005286188,0.00008194012,0.0001212643,0.0000042649754,0.000050400875],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024638363,0.00012463241,0.00016844092,0.0000012217967,0.0001624669,0.000018876946,0.00015773521,0.000046251113,0.00003112803],"category_scores_gemma":[0.000014508978,0.00010521714,0.000019584133,0.00087183306,0.0004369653,0.00048813203,0.00015103926,0.00006517931,0.0000061888636],"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":[0.0000118685175,0.000058647467,0.021275684,0.000047224232,0.000005183923,0.0000021645617,0.0039181905,0.118262865,0.00071508216,0.0039065657,0.000009507263,0.85178703],"study_design_scores_gemma":[0.0002823404,0.00019812406,0.022464415,0.000044690365,0.000011060835,0.000007677479,0.011624708,0.9414861,0.00009349816,0.011298779,0.012126862,0.00036174836],"about_ca_topic_score_codex":0.00009589646,"about_ca_topic_score_gemma":0.00007436994,"teacher_disagreement_score":0.8514253,"about_ca_system_score_codex":0.000023050141,"about_ca_system_score_gemma":0.000007552983,"threshold_uncertainty_score":0.42906305},"labels":[],"label_agreement":null},{"id":"W4319296045","doi":"10.5194/egusphere-2023-56-rc1","title":"Comment on egusphere-2023-56","year":2023,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"National Centre for Earth Observation; University of Leicester; European Space Agency","keywords":"Drizzle; Meteorology; Environmental science; Grid; Radar; Satellite; Doppler radar; Standard deviation; Remote sensing; Precipitation; Geography; Geodesy; Mathematics; Statistics; Aerospace engineering; Engineering","score_opus":0.02655412624620515,"score_gpt":0.27888481505720714,"score_spread":0.25233068881100196,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4319296045","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000018423267,0.0019996422,0.00013275878,0.286543,0.0026090876,0.0006172455,0.00007796948,0.00022487913,0.70777696],"genre_scores_gemma":[0.000029610674,0.0047601173,0.0006902375,0.11057345,0.00025227637,0.00010485731,0.00021770751,0.00006774125,0.883304],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99758255,0.000058135716,0.0003734623,0.0006516494,0.00087318476,0.00046101937],"domain_scores_gemma":[0.99882215,0.00008717599,0.00015558151,0.0007479782,0.000007659648,0.0001794359],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00030254803,0.00041219508,0.0005234427,8.413541e-7,0.0001250718,0.000030065505,0.0006331762,0.00023060139,0.19274126],"category_scores_gemma":[0.000041717678,0.00031133465,0.0003307224,0.00032385826,0.00011837038,0.0000324418,0.0005992209,0.000433207,0.06965167],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000020227349,0.000054028093,0.00005868599,0.00014960306,0.000026264242,0.000013939131,0.000007621004,0.000039612667,9.621785e-7,0.000080686994,0.98831004,0.011256509],"study_design_scores_gemma":[0.00009975751,0.00010559031,0.00021467269,0.0006309272,0.00006140799,0.0000011801071,0.000017521075,0.000040454455,0.0000037646726,0.00011936245,0.9983169,0.00038848893],"about_ca_topic_score_codex":0.0031017296,"about_ca_topic_score_gemma":0.0008264113,"teacher_disagreement_score":0.17596957,"about_ca_system_score_codex":0.00034273422,"about_ca_system_score_gemma":0.000020719066,"threshold_uncertainty_score":0.9999339},"labels":[],"label_agreement":null},{"id":"W4319722247","doi":"10.5194/acp-2022-343-ec1","title":"Justification of decision on acp-2022-343","year":2023,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"European Commission; National Aeronautics and Space Administration","keywords":"Radiosonde; Aerosol; Environmental science; Atmospheric sciences; Troposphere; Shortwave; Tropopause; Stratosphere; Overcast; Lidar; Radiative transfer; Moderate-resolution imaging spectroradiometer; Meteorology; AERONET; Remote sensing; Satellite; Geography; Geology; Sky; Physics","score_opus":0.029265459823471243,"score_gpt":0.30371104801336235,"score_spread":0.2744455881898911,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4319722247","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.009241156,0.010454337,0.009217119,0.057163075,0.013458894,0.0033481254,0.00042147958,0.0006055477,0.89609027],"genre_scores_gemma":[0.0015353699,0.0117593445,0.0021314463,0.002076207,0.00014686867,0.000057080313,0.00026653535,0.00005522443,0.9819719],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99804205,0.000029906494,0.00042542545,0.0004797117,0.00082441483,0.00019847184],"domain_scores_gemma":[0.9988686,0.00012986021,0.0002489773,0.0006600028,0.000016468663,0.000076089535],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00035706646,0.00021892453,0.00037832384,0.0000019975846,0.000058561247,0.00000942856,0.0004586914,0.00020187895,0.031182889],"category_scores_gemma":[0.00015396076,0.00016432263,0.00015401308,0.00042003236,0.00009596946,0.000036548397,0.00026022963,0.0002146338,0.008331278],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000039328725,0.000034006312,0.00004428763,0.0001488874,0.0000054231646,0.0000019562995,0.000008055914,0.000088246816,0.000054949425,0.00004697316,0.8857659,0.11379737],"study_design_scores_gemma":[0.00006855174,0.00007416825,0.0023492815,0.0008462709,0.000054487202,0.0000010627656,0.000014522241,0.0001276072,0.00008138317,0.00020662665,0.99597615,0.00019986714],"about_ca_topic_score_codex":0.00044586635,"about_ca_topic_score_gemma":0.00018852408,"teacher_disagreement_score":0.1135975,"about_ca_system_score_codex":0.00013881261,"about_ca_system_score_gemma":0.000019584979,"threshold_uncertainty_score":0.9924409},"labels":[],"label_agreement":null},{"id":"W4320025708","doi":"10.5194/amt-2022-262-rc1","title":"Comment on amt-2022-262","year":2022,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Mount Allison University","funders":"HORIZON EUROPE Excellent Science; Supercomputing Center for Education and Research, University of Oklahoma; Horizon 2020 Framework Programme; University of Oklahoma; National Aeronautics and Space Administration; U.S. Department of Energy","keywords":"Aerosol; Cloud condensation nuclei; Lidar; Environmental science; Atmospheric sciences; In situ; Backscatter (email); Extinction (optical mineralogy); Remote sensing; Relative humidity; Meteorology; Chemistry; Geology; Geography; Mineralogy; Computer science","score_opus":0.018811217697970107,"score_gpt":0.26624867935396523,"score_spread":0.24743746165599512,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4320025708","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00003177111,0.0035785986,0.0000701199,0.28452384,0.002113258,0.0005838995,0.000092870105,0.00008587875,0.70891976],"genre_scores_gemma":[0.000059327816,0.0054143732,0.00042359068,0.21799193,0.00012018789,0.00017443755,0.0003306617,0.000040521612,0.775445],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99760044,0.000088594265,0.00031221574,0.0005881294,0.0010526067,0.00035803314],"domain_scores_gemma":[0.99894,0.000052049214,0.00015757832,0.00070853677,0.000003880822,0.0001379726],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00032780404,0.00033833887,0.0004379143,8.870355e-7,0.00021691153,0.000019470775,0.0006902163,0.00011051672,0.64453065],"category_scores_gemma":[0.000020089792,0.0002686495,0.0002130294,0.00021938265,0.00009067231,0.000028396233,0.0009900399,0.0005879763,0.0053258254],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002504496,0.00009788333,0.00008206765,0.00008119628,0.000013531421,0.000011651371,0.000012693581,0.00003729698,0.0000011083935,0.00014591879,0.98685193,0.012662195],"study_design_scores_gemma":[0.00009611672,0.00016078417,0.00012441601,0.0001276606,0.000042939424,0.0000030520694,0.000022563285,0.000024512086,0.0000033685446,0.000065697095,0.9989882,0.00034069977],"about_ca_topic_score_codex":0.0013972152,"about_ca_topic_score_gemma":0.00011941691,"teacher_disagreement_score":0.63920486,"about_ca_system_score_codex":0.00058744935,"about_ca_system_score_gemma":0.00002036831,"threshold_uncertainty_score":0.9999766},"labels":[],"label_agreement":null},{"id":"W4321332421","doi":"10.5194/egusphere-2022-1217-ac2","title":"Reply on RC2","year":2023,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Lidar; Remote sensing; Radar; Snow; Environmental science; Aerosol; Meteorology; Precipitation; Atmosphere (unit); Atmospheric physics; Atmospheric sciences; Computer science; Geology; Geography","score_opus":0.026633848648375483,"score_gpt":0.281739915765091,"score_spread":0.2551060671167155,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321332421","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00006548601,0.001205787,0.0000470888,0.08849661,0.0021571363,0.00036911818,0.00003044481,0.00028642063,0.9073419],"genre_scores_gemma":[0.000033521246,0.004197328,0.00034701996,0.051794935,0.00019426917,0.00004353826,0.000086621694,0.0000505827,0.9432522],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99833435,0.000025311665,0.00024159427,0.0005325583,0.000581824,0.0002843503],"domain_scores_gemma":[0.9991102,0.000045346613,0.00010298396,0.00063471514,0.0000044947315,0.0001022104],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00022004108,0.00024343908,0.00032931328,5.365427e-7,0.00006589008,0.000015709722,0.00039730524,0.00012775707,0.088166036],"category_scores_gemma":[0.00006913707,0.00017711028,0.00015615257,0.00024002179,0.00007906676,0.000024001372,0.0003112692,0.00028044882,0.060281694],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[9.0633006e-7,0.000014688772,0.000075859316,0.000086867134,0.000006622682,0.000012957176,0.0000045206316,0.000012000564,0.0000011091901,0.000022404636,0.98738784,0.012374245],"study_design_scores_gemma":[0.00003803681,0.000055945402,0.0006705168,0.0004082378,0.00002428574,0.0000017790625,0.000004380457,0.000016187134,0.0000036556626,0.00008328983,0.9984608,0.00023283964],"about_ca_topic_score_codex":0.0015587653,"about_ca_topic_score_gemma":0.00019214509,"teacher_disagreement_score":0.03670168,"about_ca_system_score_codex":0.00013718694,"about_ca_system_score_gemma":0.0000137275065,"threshold_uncertainty_score":0.94045},"labels":[],"label_agreement":null},{"id":"W4321442792","doi":"10.1039/d2cp05301b","title":"Optical trapping and light scattering in atmospheric aerosol science","year":2023,"lang":"en","type":"review","venue":"Physical Chemistry Chemical Physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Fonds de recherche du Québec – Nature et technologies","keywords":"Aerosol; Trapping; Scattering; Light scattering; Environmental science; Atmospheric sciences; Materials science; Chemical physics; Physics; Optics; Meteorology; Geography","score_opus":0.022637862607892807,"score_gpt":0.2799465281442767,"score_spread":0.2573086655363839,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321442792","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.27698162,0.66418785,0.0004375762,0.00031212618,0.00036913817,0.0028352255,0.00006330857,0.0012679243,0.053545203],"genre_scores_gemma":[0.09271533,0.90132374,0.0016973235,0.0001119456,0.0022374606,0.000564376,0.00007547489,0.0004766452,0.00079771556],"study_design_codex":"design_other","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99643487,0.000017568489,0.0005449751,0.0013666092,0.00069917535,0.00093683414],"domain_scores_gemma":[0.99862266,0.00016700862,0.00020705015,0.00057723705,0.000010901895,0.0004151304],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0001540474,0.0007028784,0.0014700202,7.461727e-7,0.00013336177,0.000112541624,0.0008953133,0.0002562713,0.00007722711],"category_scores_gemma":[0.0000761663,0.0006259492,0.0003424583,0.0016693384,0.0014100203,0.00023035464,0.0013796822,0.0009512378,0.0003152297],"study_design_candidate":"design_other","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":[0.000008724482,0.00062553847,0.000034068864,0.009699928,0.00006187049,0.000053522243,0.00026582807,0.00008441679,0.21428552,0.00007697991,0.00031809026,0.7744855],"study_design_scores_gemma":[0.00428314,0.00028989243,0.00011055673,0.049926862,0.003348064,0.0003226798,0.00046569525,0.03881238,0.47764173,0.01079818,0.39227036,0.02173046],"about_ca_topic_score_codex":0.000017085114,"about_ca_topic_score_gemma":3.1365886e-7,"teacher_disagreement_score":0.75275505,"about_ca_system_score_codex":0.0005688654,"about_ca_system_score_gemma":0.00009421541,"threshold_uncertainty_score":0.9996192},"labels":[],"label_agreement":null},{"id":"W4321489842","doi":"10.5194/egusphere-egu23-4129","title":"Anthropogenic aerosols turn liquid cloud droplets into ice crystals, produce snow and eat holes in the clouds","year":2023,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"","keywords":"Aerosol; Environmental science; Ice nucleus; Snow; Glacial period; Atmospheric sciences; Climatology; Geology; Meteorology; Geography; Chemistry","score_opus":0.019960678025265383,"score_gpt":0.2617948462335958,"score_spread":0.2418341682083304,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321489842","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":[0.98826474,0.0006549673,0.0010762824,0.004943018,0.00086107396,0.0012548647,0.000019795465,0.00019858788,0.0027266613],"genre_scores_gemma":[0.9917175,0.0014154981,0.0014847654,0.0007851032,0.0004117229,0.00021344377,0.000038076356,0.0000897507,0.003844136],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9960108,0.00029430032,0.00065253273,0.0015068728,0.0008003087,0.0007352298],"domain_scores_gemma":[0.9980005,0.00019454789,0.00025451768,0.0013595449,0.000016071757,0.00017479536],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011151979,0.00064250274,0.0005868298,0.000005308581,0.00033623955,0.00023125009,0.0012763336,0.0004588768,0.0013560519],"category_scores_gemma":[0.00014944539,0.00044438953,0.00017789533,0.00048700484,0.0012019771,0.0001445445,0.003558103,0.0010221225,0.00048496778],"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":[0.0015358576,0.003754958,0.4784164,0.0022016128,0.0007937468,0.0015430539,0.105833836,0.036284097,0.08837515,0.0039060328,0.22851336,0.048841868],"study_design_scores_gemma":[0.005690261,0.0040767733,0.72724825,0.002559609,0.0009296727,0.0005125181,0.046491455,0.01044977,0.027442778,0.034411628,0.126787,0.01340027],"about_ca_topic_score_codex":0.005862801,"about_ca_topic_score_gemma":0.0025104305,"teacher_disagreement_score":0.24883184,"about_ca_system_score_codex":0.00024077737,"about_ca_system_score_gemma":0.000058983213,"threshold_uncertainty_score":0.9998008},"labels":[],"label_agreement":null},{"id":"W4321489891","doi":"10.5194/egusphere-egu23-4331","title":"Evaluate parameterizations of cloud droplet spectral dispersion by using worldwide aircraft data","year":2023,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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; Environmental science; Effective radius; Meteorology; Dispersion (optics); Cloud computing; RADIUS; Liquid water content; Atmospheric sciences; Physics; Computer science","score_opus":0.06403847164954865,"score_gpt":0.30672329856926656,"score_spread":0.2426848269197179,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321489891","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":[0.9264912,0.00005510206,0.0691069,0.0004786135,0.0007727092,0.00046687643,0.00048177212,0.00012664005,0.0020201718],"genre_scores_gemma":[0.9476212,0.00018945367,0.04250271,0.0001514052,0.00012801912,0.000013855038,0.0012895367,0.00008205037,0.008021762],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9976225,0.0000904738,0.00047947076,0.0008730119,0.0005808205,0.0003537403],"domain_scores_gemma":[0.9980127,0.00006118754,0.00025489955,0.0015400266,0.000008868315,0.000122285],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00037907044,0.00028538602,0.0003592609,0.0000029610333,0.00012151019,0.000062190935,0.0011856771,0.00017492493,0.0055684675],"category_scores_gemma":[0.0000645596,0.000253285,0.00010599944,0.0003054256,0.000271595,0.00013256079,0.0051346584,0.0003029283,0.00028858575],"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":[0.00007814198,0.00070745865,0.25561532,0.0002286248,0.0003356498,0.000031737614,0.00083897857,0.36192384,0.103137255,0.00015780129,0.2669538,0.009991367],"study_design_scores_gemma":[0.0003611848,0.000085730215,0.017686676,0.00018248682,0.00035612634,0.000005522365,0.0003283844,0.9682271,0.0025087385,0.0020795777,0.007088257,0.001090247],"about_ca_topic_score_codex":0.004763015,"about_ca_topic_score_gemma":0.0002622863,"teacher_disagreement_score":0.6063032,"about_ca_system_score_codex":0.00018060542,"about_ca_system_score_gemma":0.000044659904,"threshold_uncertainty_score":0.99999195},"labels":[],"label_agreement":null},{"id":"W4321490137","doi":"10.5194/egusphere-egu23-3721","title":"What are coarse dust aerosols, and how do they impact the Earth's climate system?","year":2023,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Dalhousie University","funders":"","keywords":"Mineral dust; Aerosol; Atmospheric sciences; Atmosphere (unit); Earth system science; Environmental science; Atmospheric dust; Biogeochemistry; Earth (classical element); Particle (ecology); Climate system; Meteorology; Climate change; Physics; Geology; Oceanography; Astronomy","score_opus":0.020842897268779925,"score_gpt":0.24616483962691127,"score_spread":0.22532194235813136,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321490137","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":[0.98664194,0.0005829874,0.00014770895,0.0031963459,0.001516519,0.0010021853,0.0000830537,0.0003603204,0.006468912],"genre_scores_gemma":[0.9896835,0.0025999534,0.00030990646,0.00018687278,0.00014458054,0.000092676004,0.000016052256,0.00006621698,0.0069002267],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9976793,0.00014668812,0.00023979785,0.00080319616,0.00052240357,0.0006086435],"domain_scores_gemma":[0.9983655,0.00010253862,0.00030087712,0.0010097529,0.000012144168,0.00020917154],"candidate_categories":["metaepi_narrow","scholarly_communication","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00061881164,0.00047182414,0.0004521142,0.0000016115516,0.00038067828,0.0012750343,0.000638836,0.00035625385,0.000779904],"category_scores_gemma":[0.000023465032,0.00026133787,0.00021544013,0.000116593714,0.00029743323,0.00029077093,0.0031484598,0.0006299928,0.00088389224],"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":[0.00013822383,0.00020419042,0.8695847,0.001046149,0.00055021525,0.0003742072,0.0058538015,0.02566944,0.0010474873,0.0013201296,0.07738693,0.016824568],"study_design_scores_gemma":[0.0009772202,0.00024476412,0.9009117,0.0019104787,0.00032123484,0.00015158502,0.06648095,0.01881723,0.00019042972,0.001025025,0.0065580434,0.0024113697],"about_ca_topic_score_codex":0.0014342149,"about_ca_topic_score_gemma":0.001355288,"teacher_disagreement_score":0.070828885,"about_ca_system_score_codex":0.00017015851,"about_ca_system_score_gemma":0.000021263686,"threshold_uncertainty_score":0.9999839},"labels":[],"label_agreement":null},{"id":"W4321498065","doi":"10.5194/acp-23-2421-2023","title":"The impacts of dust aerosol and convective available potential energy on precipitation vertical structure in southeastern China as seen from multisource observations","year":2023,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":19,"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 en Abitibi-Témiscamingue","funders":"National Key Research and Development Program of China; National Natural Science Foundation of China","keywords":"Precipitation; Atmospheric sciences; Convective available potential energy; Aerosol; Environmental science; Convection; Mineral dust; Precipitation types; Wind shear; Climatology; Geology; Wind speed; Meteorology; Geography","score_opus":0.005719441375481821,"score_gpt":0.19716112308222788,"score_spread":0.19144168170674605,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321498065","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":[0.99880606,0.00005104974,0.00023678172,0.000083094455,0.000025850737,0.000069427675,0.000021989526,0.000016591628,0.0006891671],"genre_scores_gemma":[0.9981514,0.00007630718,0.00038382853,0.000038330225,0.00005152553,0.000008382346,0.000028779035,0.000012111765,0.0012492959],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99924314,0.000024307754,0.00014428687,0.00024337537,0.00016528275,0.0001795794],"domain_scores_gemma":[0.99961555,0.00009855132,0.000052874795,0.00015576182,0.0000072517905,0.000069997826],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000038028713,0.00013112537,0.00012730395,2.450965e-8,0.00014718783,0.00002266045,0.00009247086,0.000077539305,0.0003504476],"category_scores_gemma":[0.000020385198,0.00010246201,0.000025781834,0.00019472842,0.00020090374,0.00007884719,0.00008453336,0.00011451543,0.000016163687],"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":[0.0004272398,0.0002565287,0.4281899,0.000054881348,0.00012319857,0.000012949014,0.00684317,0.020085221,0.46834373,0.00014853127,0.00088689645,0.07462775],"study_design_scores_gemma":[0.0010975829,0.00012978971,0.7094084,0.000049965303,0.000042663618,0.0000030690237,0.0012741785,0.24252693,0.041173298,0.0035642604,0.00039804,0.0003318195],"about_ca_topic_score_codex":0.0018115253,"about_ca_topic_score_gemma":0.00006150124,"teacher_disagreement_score":0.42717043,"about_ca_system_score_codex":0.000025709098,"about_ca_system_score_gemma":0.00001265527,"threshold_uncertainty_score":0.41782793},"labels":[],"label_agreement":null},{"id":"W4321995793","doi":"10.5194/egusphere-egu23-10455","title":"The spectrally and vertically decomposed outgoing longwave radiation and its climate trends in the far-infrared","year":2023,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"","keywords":"Outgoing longwave radiation; Longwave; Environmental science; Radiant energy; Radiative transfer; Tropopause; Atmosphere (unit); Infrared; Atmospheric sciences; Far infrared; Satellite; Atmospheric Infrared Sounder; Stratosphere; Atmosphere of Earth; Radiation; Meteorology; Remote sensing; Troposphere; Physics; Geography; Optics; Astronomy; Convection","score_opus":0.017677888345184325,"score_gpt":0.25691367073154614,"score_spread":0.2392357823863618,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321995793","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":[0.97481024,0.00030676852,0.00025573457,0.003036934,0.00016523426,0.00030385578,0.000006663577,0.000060053768,0.02105454],"genre_scores_gemma":[0.99507564,0.0017637042,0.0005690988,0.00043763788,0.00003793882,0.000031062056,0.000011742087,0.000019172472,0.002053991],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986171,0.00009409476,0.00027609203,0.0004088249,0.00026297735,0.000340927],"domain_scores_gemma":[0.99938655,0.00020314466,0.00008108797,0.00027089397,0.0000031811533,0.00005512275],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00055599277,0.00019474918,0.0001679267,0.0000027619533,0.00023910427,0.00021888225,0.00030883515,0.0001263352,0.00022326382],"category_scores_gemma":[0.000036951686,0.00011037136,0.000047663238,0.00015316128,0.00012437081,0.00006611867,0.0007153288,0.0003193579,0.00005303754],"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":[0.0003194928,0.00025223108,0.49801278,0.00013446748,0.00018703859,0.00017730982,0.017858483,0.008017183,0.0032313932,0.009242808,0.0120040225,0.4505628],"study_design_scores_gemma":[0.00025111716,0.000040731622,0.95308685,0.0000141475075,0.00001982584,0.0000047191966,0.0003463288,0.043339886,0.000038883132,0.0020000543,0.00066859834,0.00018884047],"about_ca_topic_score_codex":0.00018721723,"about_ca_topic_score_gemma":0.0010984801,"teacher_disagreement_score":0.4550741,"about_ca_system_score_codex":0.00007559914,"about_ca_system_score_gemma":0.000008578045,"threshold_uncertainty_score":0.45008132},"labels":[],"label_agreement":null},{"id":"W4321995841","doi":"10.5194/egusphere-egu23-10484","title":"Profiling of Shallow Marine Fog using a UAV and Remote Sensing Observations over the Sable Island during FATIMA","year":2023,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Ontario Tech University","funders":"","keywords":"Radiosonde; Environmental science; Wind speed; Microwave radiometer; Planetary boundary layer; Meteorology; Relative humidity; Radiometer; Atmospheric sciences; Wind profiler; Remote sensing; Turbulence; Geology; Geography; Radar","score_opus":0.043626812469273905,"score_gpt":0.2560204207565652,"score_spread":0.2123936082872913,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321995841","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":[0.9797854,0.00001817382,0.016361654,0.00017102787,0.000121237616,0.00037018865,0.000007657694,0.000053068663,0.0031116002],"genre_scores_gemma":[0.7845856,0.00006634743,0.21113141,0.00007831005,0.000060288396,0.0000015328787,0.000012991399,0.000046107998,0.0040173926],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9986908,0.000030776853,0.00032185233,0.0004221336,0.00028036878,0.0002541012],"domain_scores_gemma":[0.99925935,0.000065484826,0.00019905518,0.00041535977,0.000012581268,0.00004817025],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022965642,0.00020591775,0.00024716838,0.0000023476048,0.00024132861,0.00006318658,0.00018173187,0.00012937552,0.00045004874],"category_scores_gemma":[0.00004465831,0.00015021868,0.000073328745,0.00018368632,0.00015995467,0.00007717982,0.0019044145,0.00028154772,0.000008432991],"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":[0.000030440113,0.000030233594,0.80420345,0.00036407623,0.00013018049,0.000023529668,0.0011456113,0.13704179,0.04992436,0.000085525244,0.00019537384,0.006825405],"study_design_scores_gemma":[0.00016591321,0.000008756743,0.4107659,0.00011530649,0.00004703173,0.0000080024965,0.00026709336,0.5857306,0.0008784942,0.0017678555,0.00002794562,0.00021707466],"about_ca_topic_score_codex":0.011946505,"about_ca_topic_score_gemma":0.0030332203,"teacher_disagreement_score":0.44868883,"about_ca_system_score_codex":0.00010871597,"about_ca_system_score_gemma":0.000022297498,"threshold_uncertainty_score":0.994633},"labels":[],"label_agreement":null},{"id":"W4322004965","doi":"10.5194/egusphere-egu23-9208","title":"Tomographic retrievals of Hunga Tonga-Hunga Ha’apai volcanic aerosol","year":2023,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"University of Saskatchewan","funders":"","keywords":"Aerosol; Volcano; Occultation; Extinction (optical mineralogy); Lidar; Environmental science; Atmospheric sciences; Altitude (triangle); Atmosphere (unit); Stratosphere; Water vapor; Remote sensing; Geology; Meteorology; Physics; Astrophysics; Mineralogy; Seismology","score_opus":0.02616593188993517,"score_gpt":0.25346455319231487,"score_spread":0.2272986213023797,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4322004965","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":[0.9686281,0.00021421225,0.001977918,0.0006491841,0.0013025311,0.000936067,0.0000672616,0.00043607887,0.025788646],"genre_scores_gemma":[0.9665846,0.0004440184,0.0027498633,0.0002755292,0.00012702336,0.00008132726,0.000040707084,0.00010156701,0.02959535],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9961057,0.0001251077,0.0008750453,0.001170642,0.0010426273,0.0006808807],"domain_scores_gemma":[0.9976255,0.00013003056,0.00049779995,0.001445539,0.00003214083,0.00026898854],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00072744803,0.00055613276,0.0007867862,0.0000078618295,0.00014928631,0.00006471234,0.0012262628,0.0005091566,0.011959527],"category_scores_gemma":[0.00011411078,0.0004978327,0.00053181726,0.00080216274,0.00052966777,0.000104779574,0.0030349004,0.00084915216,0.0012075634],"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":[0.00024907637,0.0012336904,0.7030655,0.0009342321,0.00093436724,0.00019153453,0.002209461,0.022606233,0.039926928,0.0013558111,0.21410632,0.013186808],"study_design_scores_gemma":[0.003344064,0.0019164121,0.8523851,0.0014077501,0.0011910191,0.000052412983,0.0028716458,0.0185864,0.069248594,0.022356201,0.018459959,0.008180454],"about_ca_topic_score_codex":0.0038402206,"about_ca_topic_score_gemma":0.001801116,"teacher_disagreement_score":0.19564636,"about_ca_system_score_codex":0.00021012603,"about_ca_system_score_gemma":0.00007410087,"threshold_uncertainty_score":0.99974734},"labels":[],"label_agreement":null},{"id":"W4322005374","doi":"10.5194/egusphere-egu23-7474","title":"Measurements of microphyscs in cold air Outbreks","year":2023,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Cloud condensation nuclei; Environmental science; Meteorology; Climatology; Ice crystals; Cloud physics; Sea ice; Aerosol; Atmospheric sciences; Cloud computing; Geography; Geology; Computer science","score_opus":0.04715673878793576,"score_gpt":0.25668438341766775,"score_spread":0.209527644629732,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4322005374","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":[0.9692817,0.000029575798,0.0003807818,0.00016849692,0.00036317427,0.0003390485,0.000007033706,0.000053483665,0.029376756],"genre_scores_gemma":[0.9859542,0.000021265258,0.0042478363,0.00015278345,0.000019337334,0.000033063534,0.00000465157,0.000025558355,0.009541291],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99859864,0.0000322248,0.0003332253,0.00040174008,0.00040579995,0.00022836633],"domain_scores_gemma":[0.9994192,0.000012276153,0.00010861403,0.0003983688,0.0000065431173,0.000055003402],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00022583808,0.00017891002,0.00027181397,0.000001762388,0.000019640007,0.0000071313425,0.00041110392,0.00018216575,0.0013609593],"category_scores_gemma":[0.000014459524,0.00016173054,0.000092469745,0.00015907454,0.000108374836,0.000024368317,0.0013458926,0.00023793893,0.0006551863],"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":[0.000016732127,0.00022629937,0.8834051,0.000089129375,0.00003556895,0.000011891863,0.00041000822,0.059043072,0.04524064,0.000019063873,0.009655704,0.0018467931],"study_design_scores_gemma":[0.00056114176,0.000070644026,0.95042735,0.00019445774,0.00002849461,4.7712484e-7,0.00015360542,0.0009791513,0.045044057,0.0006983272,0.0012248943,0.00061741174],"about_ca_topic_score_codex":0.0075003603,"about_ca_topic_score_gemma":0.0016767996,"teacher_disagreement_score":0.06702224,"about_ca_system_score_codex":0.00020108405,"about_ca_system_score_gemma":0.00002275196,"threshold_uncertainty_score":0.99955195},"labels":[],"label_agreement":null},{"id":"W4322007031","doi":"10.5194/egusphere-egu23-7153","title":"The relationship between surface tension and atmospheric ice-nucleating activity of agricultural soil","year":2023,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"University of British Columbia","funders":"","keywords":"Ice nucleus; Surface tension; Nucleation; Soil water; Environmental science; Chemistry; Atmospheric sciences; Soil science; Chemical physics; Environmental chemistry; Chemical engineering; Geology; Thermodynamics; Organic chemistry","score_opus":0.03715989861780562,"score_gpt":0.252529959818791,"score_spread":0.2153700612009854,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4322007031","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":[0.99525005,0.000046768095,0.00056332425,0.00070152065,0.0001390275,0.000251837,0.000005436345,0.00009109101,0.0029509675],"genre_scores_gemma":[0.98938227,0.0000536739,0.003571255,0.000011491662,0.00004552816,0.0000064874266,0.000006169875,0.000021417572,0.006901734],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99862415,0.000099214616,0.000272733,0.0004134702,0.0003462743,0.00024415078],"domain_scores_gemma":[0.9984185,0.0008563415,0.00029152227,0.00034195627,0.000013104511,0.00007858453],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038241307,0.00021386269,0.00025402743,1.786822e-7,0.00042996535,0.0000596959,0.00026194667,0.00021734806,0.000087452696],"category_scores_gemma":[0.00017558939,0.00012444636,0.00008880005,0.00020166289,0.00027492328,0.000084951906,0.0015979368,0.00045462226,0.00008580612],"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":[0.000004074927,0.000009151431,0.9835521,0.000020822441,0.000015764635,3.9410642e-7,0.00021000324,0.011627705,0.0010848192,0.000039793285,0.0010068542,0.002428491],"study_design_scores_gemma":[0.00006957721,0.000022590702,0.9959092,0.000036557583,0.000031409454,7.631666e-7,0.0004132261,0.0025071504,0.00014170063,0.0006439381,0.00005005722,0.00017383277],"about_ca_topic_score_codex":0.00329204,"about_ca_topic_score_gemma":0.00042263928,"teacher_disagreement_score":0.01235707,"about_ca_system_score_codex":0.00009881094,"about_ca_system_score_gemma":0.000013124903,"threshold_uncertainty_score":0.5074775},"labels":[],"label_agreement":null},{"id":"W4322099492","doi":"10.5194/egusphere-egu23-17546","title":"Local dust plume analysis and classification using ground-based remote sensing and microphysical measurement acquired at Lhù’ààn Mân’ (Kluane Lake), Yukon","year":2023,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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 de Montréal; Université de Sherbrooke","funders":"","keywords":"AERONET; Environmental science; Lidar; Plume; Aerosol; Meteorology; Atmospheric sciences; Remote sensing; Physics; Geography","score_opus":0.057882716077777736,"score_gpt":0.2570543819378205,"score_spread":0.19917166586004276,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4322099492","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":[0.6728423,0.000042368934,0.32609066,0.00034890106,0.00010595294,0.00027064257,0.000009923288,0.00008906835,0.0002001653],"genre_scores_gemma":[0.9773057,0.000047165122,0.021602334,0.00017487675,0.0000707107,0.0000021225012,0.00007173469,0.000051177194,0.000674167],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99682754,0.00014925783,0.0004800731,0.0012428666,0.00086282194,0.0004374592],"domain_scores_gemma":[0.99875885,0.000048419963,0.00028714855,0.00063308683,0.000037002763,0.00023550319],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00052701763,0.00044920697,0.0005925296,0.000013052122,0.00034149748,0.000164673,0.0001780043,0.00035638871,0.00033997308],"category_scores_gemma":[0.00002533534,0.00041673402,0.00019695508,0.00051340135,0.00061764556,0.000074805524,0.0010780152,0.00025134115,0.00007171001],"study_design_candidate":"simulation_or_modeling","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":[0.00046730015,0.00029649126,0.1012432,0.0004440257,0.001712291,0.00015885461,0.0010763214,0.12454104,0.6176428,0.000022867389,0.0010444196,0.15135036],"study_design_scores_gemma":[0.00028606018,0.000030397066,0.25894302,0.000057035606,0.000699684,0.0000053068347,0.00013538597,0.7380756,0.0010347811,0.0001198357,0.00016812165,0.00044474236],"about_ca_topic_score_codex":0.009632809,"about_ca_topic_score_gemma":0.012896451,"teacher_disagreement_score":0.616608,"about_ca_system_score_codex":0.0010247091,"about_ca_system_score_gemma":0.00004628358,"threshold_uncertainty_score":0.99982846},"labels":[],"label_agreement":null},{"id":"W4322627214","doi":"10.5194/egusphere-2023-336-supplement","title":"Supplementary material to \"A thermodynamic framework for bulk–surface partitioning in finite-volume mixed organic–inorganic aerosol particles and cloud droplets\"","year":2023,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Aerosol; Volume (thermodynamics); Materials science; Surface (topology); Cloud computing; Chemical engineering; Thermodynamics; Chemistry; Physics; Mathematics; Computer science; Organic chemistry; Geometry","score_opus":0.015252449302386792,"score_gpt":0.2430723874896498,"score_spread":0.227819938187263,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4322627214","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":[0.9495601,0.00001016366,0.045023765,0.001978548,0.0013510938,0.0012559815,0.000652835,0.00013460823,0.000032875258],"genre_scores_gemma":[0.95554495,0.000045705237,0.04238588,0.00048148664,0.00022846847,0.00024404717,0.00032517826,0.000110827765,0.0006334328],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9972893,0.00009102772,0.0005931961,0.0009876454,0.0003094823,0.00072932616],"domain_scores_gemma":[0.99886405,0.00021548396,0.00015935425,0.0005312393,0.00001065718,0.00021918134],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004043671,0.00042624152,0.00046553515,0.0000041810426,0.00020252762,0.0001911127,0.00044579318,0.0003370703,0.016407002],"category_scores_gemma":[0.00011196199,0.00041933404,0.000087957254,0.0002592887,0.00013785662,0.00007325996,0.0019765128,0.00035207224,0.0003249322],"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":[0.0007618092,0.00080678426,0.5497553,0.00057833845,0.00031683609,0.0000840378,0.008622313,0.15077168,0.24599531,0.0020382872,0.03745395,0.0028153544],"study_design_scores_gemma":[0.0058062356,0.0021965075,0.42182714,0.0015949657,0.0007034277,0.000026937514,0.0092531005,0.30554166,0.081906326,0.15482685,0.0070934664,0.00922339],"about_ca_topic_score_codex":0.0034893532,"about_ca_topic_score_gemma":0.0052751084,"teacher_disagreement_score":0.164089,"about_ca_system_score_codex":0.00035209247,"about_ca_system_score_gemma":0.00004220013,"threshold_uncertainty_score":0.99982584},"labels":[],"label_agreement":null},{"id":"W4322766303","doi":"10.5194/egusphere-2022-1156-rc2","title":"Comment on egusphere-2022-1156","year":2023,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"AERONET; Remote sensing; Environmental science; Albedo (alchemy); Aerosol; Mineral dust; Satellite; Cloud cover; Snow; Angstrom exponent; Meteorology; Geology; Geography; Cloud computing; Physics; Computer science","score_opus":0.024473228243980825,"score_gpt":0.2773127089217598,"score_spread":0.25283948067777895,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4322766303","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000040652958,0.0022893625,0.00012940199,0.33216622,0.0030932222,0.00072895014,0.000081434315,0.00029266064,0.6611781],"genre_scores_gemma":[0.000036520767,0.0061925007,0.0004701419,0.118353665,0.000205844,0.00011425834,0.00022279419,0.00007545139,0.87432885],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99747354,0.00006243764,0.00038033017,0.00067368906,0.0009434169,0.00046658897],"domain_scores_gemma":[0.99878186,0.00008728815,0.00016132389,0.00078048825,0.000007608337,0.00018145527],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00032772828,0.0004190542,0.00053222757,8.8887265e-7,0.00013249496,0.00002919867,0.00065268157,0.00023183877,0.18921219],"category_scores_gemma":[0.000042126838,0.00031758644,0.00024502096,0.0003316724,0.00011933361,0.000033247845,0.0006383273,0.00046615818,0.046024892],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000021854412,0.000059237867,0.0000843134,0.00014948507,0.000020136828,0.000014826212,0.000009535979,0.000029492043,0.0000014046728,0.00009946423,0.9826438,0.01688614],"study_design_scores_gemma":[0.00010604998,0.00011084783,0.00026315064,0.0005728074,0.000050006955,0.0000015563553,0.00001847333,0.000046880155,0.0000066348425,0.00013140318,0.9982965,0.0003956986],"about_ca_topic_score_codex":0.0021933578,"about_ca_topic_score_gemma":0.0007081178,"teacher_disagreement_score":0.21381256,"about_ca_system_score_codex":0.0003653464,"about_ca_system_score_gemma":0.000021496233,"threshold_uncertainty_score":0.99992764},"labels":[],"label_agreement":null},{"id":"W4323042619","doi":"10.5194/acp-23-2901-2023","title":"Self-lofting of wildfire smoke in the troposphere and stratosphere: simulations and space lidar observations","year":2023,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":44,"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":"European Commission","keywords":"Troposphere; Radiosonde; Environmental science; Aerosol; Atmospheric sciences; Stratosphere; Tropopause; Lidar; Shortwave; Radiative transfer; Overcast; Meteorology; Remote sensing; Geology; Sky; Geography; Physics","score_opus":0.011657284960868921,"score_gpt":0.22244516719393304,"score_spread":0.2107878822330641,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4323042619","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":[0.99667263,0.00015438301,0.00012281621,0.00025827883,0.000009575812,0.00012443258,0.0000064748815,0.000036629575,0.0026148085],"genre_scores_gemma":[0.9917474,0.00020199358,0.0074050943,0.00006597815,0.000037408732,0.000009169645,0.000008741125,0.00001291986,0.00051129493],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99919325,0.000022415927,0.0001774909,0.0002541384,0.00016035249,0.00019236038],"domain_scores_gemma":[0.99952024,0.0001474152,0.000078091995,0.00019239307,0.0000054826214,0.0000563899],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009617775,0.00014925914,0.00015358577,1.7511036e-8,0.00019081641,0.000035242105,0.00010168967,0.00006995475,0.00017568923],"category_scores_gemma":[0.000016354885,0.00012368712,0.000025158275,0.00051203114,0.00021186564,0.0001357766,0.00009330506,0.00013871002,0.0000028692066],"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":[0.000010067007,0.000114710376,0.94892573,0.0001274421,0.000027821554,0.000006679944,0.0035851395,0.005010933,0.007682022,0.00033186236,0.00025489563,0.033922702],"study_design_scores_gemma":[0.0006166252,0.000052116353,0.83339715,0.000041158444,0.000055708624,0.000008985529,0.0040300675,0.15454303,0.0008196763,0.0030817105,0.0030130595,0.0003407052],"about_ca_topic_score_codex":0.0002904983,"about_ca_topic_score_gemma":0.00002745386,"teacher_disagreement_score":0.1495321,"about_ca_system_score_codex":0.000018674715,"about_ca_system_score_gemma":0.000012974662,"threshold_uncertainty_score":0.5043815},"labels":[],"label_agreement":null},{"id":"W4323044636","doi":"10.5194/amt-16-1103-2023","title":"Relationship between the sub-micron fraction (SMF) and fine-mode fraction (FMF) in the context of AERONET retrievals","year":2023,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University; National Research Council Canada; Université de Sherbrooke","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency; Goddard Space Flight Center; Brookhaven National Laboratory; Environment and Climate Change Canada; Strong; National Aeronautics and Space Administration","keywords":"AERONET; Aerosol; Cutoff; Effective radius; Angstrom exponent; Context (archaeology); RADIUS; Radiance; Physics; Astrophysics; Optics; Meteorology; Galaxy","score_opus":0.04331009244039162,"score_gpt":0.2783545600397223,"score_spread":0.23504446759933068,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4323044636","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":[0.9913873,0.0001684425,0.0047258963,0.0014129574,0.000038503404,0.00079930737,0.0000030580009,0.00016143579,0.0013031038],"genre_scores_gemma":[0.99777454,0.00012692905,0.0016150901,0.00021631215,0.0000532703,0.00011808837,0.000008323844,0.000020404628,0.00006703535],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99788934,0.00028302422,0.00043694573,0.00030889024,0.000815208,0.00026658518],"domain_scores_gemma":[0.99893105,0.00032111324,0.00027083713,0.0004068578,0.000030751846,0.000039377326],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0022625872,0.0001874547,0.00022418455,0.0000013928126,0.00024375536,0.000036377525,0.00029690424,0.00014004747,0.000087445515],"category_scores_gemma":[0.00026261868,0.00012218446,0.00005989542,0.0008256806,0.00021443648,0.00022424564,0.00009733227,0.0003193938,0.000045500325],"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":[0.000030129995,0.000047643654,0.9306047,0.000016969734,0.00001213234,0.0000014168266,0.0006377018,0.000031481515,0.021440309,0.00008958497,0.011793254,0.035294678],"study_design_scores_gemma":[0.00018300346,0.00016001823,0.9684401,0.00004675538,0.000038022798,0.0000025076272,0.000948601,0.00033969394,0.021391716,0.002015177,0.006255501,0.00017888969],"about_ca_topic_score_codex":0.0015888775,"about_ca_topic_score_gemma":0.00028974138,"teacher_disagreement_score":0.037835415,"about_ca_system_score_codex":0.0002741306,"about_ca_system_score_gemma":0.000018841049,"threshold_uncertainty_score":0.49825373},"labels":[],"label_agreement":null},{"id":"W4323537876","doi":"10.5194/egusphere-2022-1284-ac2","title":"Reply on RC2","year":2023,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"European Space Agency","keywords":"Doppler effect; Remote sensing; Attenuation; Satellite; Microwave; Radar; Environmental science; Computer science; Geology; Meteorology; Optics; Physics; Telecommunications","score_opus":0.026633848648375483,"score_gpt":0.281739915765091,"score_spread":0.2551060671167155,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4323537876","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00006548601,0.001205787,0.0000470888,0.08849661,0.0021571363,0.00036911818,0.00003044481,0.00028642063,0.9073419],"genre_scores_gemma":[0.000033521246,0.004197328,0.00034701996,0.051794935,0.00019426917,0.00004353826,0.000086621694,0.0000505827,0.9432522],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99833435,0.000025311665,0.00024159427,0.0005325583,0.000581824,0.0002843503],"domain_scores_gemma":[0.9991102,0.000045346613,0.00010298396,0.00063471514,0.0000044947315,0.0001022104],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00022004108,0.00024343908,0.00032931328,5.365427e-7,0.00006589008,0.000015709722,0.00039730524,0.00012775707,0.088166036],"category_scores_gemma":[0.00006913707,0.00017711028,0.00015615257,0.00024002179,0.00007906676,0.000024001372,0.0003112692,0.00028044882,0.060281694],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[9.0633006e-7,0.000014688772,0.000075859316,0.000086867134,0.000006622682,0.000012957176,0.0000045206316,0.000012000564,0.0000011091901,0.000022404636,0.98738784,0.012374245],"study_design_scores_gemma":[0.00003803681,0.000055945402,0.0006705168,0.0004082378,0.00002428574,0.0000017790625,0.000004380457,0.000016187134,0.0000036556626,0.00008328983,0.9984608,0.00023283964],"about_ca_topic_score_codex":0.0015587653,"about_ca_topic_score_gemma":0.00019214509,"teacher_disagreement_score":0.03670168,"about_ca_system_score_codex":0.00013718694,"about_ca_system_score_gemma":0.0000137275065,"threshold_uncertainty_score":0.94045},"labels":[],"label_agreement":null},{"id":"W4323537994","doi":"10.5194/egusphere-2022-1284-ac1","title":"Reply on RC1","year":2023,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"European Space Agency","keywords":"Doppler effect; Remote sensing; Attenuation; Satellite; Radar; Microwave; Computer science; Geology; Environmental science; Meteorology; Optics; Physics; Aerospace engineering; Telecommunications; Engineering","score_opus":0.026633848648375483,"score_gpt":0.281739915765091,"score_spread":0.2551060671167155,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4323537994","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000058078247,0.0011877151,0.00004543212,0.0853886,0.002073141,0.00035407513,0.000030504487,0.0002458215,0.91061664],"genre_scores_gemma":[0.000027702192,0.0043644817,0.00035001742,0.051770918,0.00019447974,0.000043493215,0.00009016552,0.000046762725,0.94311196],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9983323,0.000025353,0.00024181827,0.00053312036,0.00058265665,0.00028470292],"domain_scores_gemma":[0.99910927,0.00004543233,0.00010303268,0.0006354473,0.0000045023767,0.00010229738],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00022354668,0.00024356734,0.0003295704,5.3738205e-7,0.000069201546,0.000015738513,0.0003981685,0.00012786122,0.09315952],"category_scores_gemma":[0.000069304166,0.0001771951,0.000156209,0.00024060541,0.00007920655,0.000024017369,0.0003119409,0.00028079824,0.06324427],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[9.0600514e-7,0.000014704292,0.000057636375,0.00008690968,0.000006618528,0.000012947123,0.000004546301,0.000015874757,0.0000010762662,0.000023632181,0.9862739,0.013501277],"study_design_scores_gemma":[0.0000382743,0.00005604107,0.0006027008,0.000408913,0.000024297176,0.0000017800179,0.000004393374,0.000016963368,0.0000036020417,0.00008410035,0.9985259,0.00023299616],"about_ca_topic_score_codex":0.0016544036,"about_ca_topic_score_gemma":0.00018394631,"teacher_disagreement_score":0.033617683,"about_ca_system_score_codex":0.00013927974,"about_ca_system_score_gemma":0.000013796646,"threshold_uncertainty_score":0.9374851},"labels":[],"label_agreement":null},{"id":"W4323538902","doi":"10.5194/egusphere-2022-1284-ac3","title":"Reply on RC3","year":2023,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"European Space Agency","keywords":"Doppler effect; Remote sensing; Attenuation; Satellite; Radar; Microwave; Computer science; Geology; Environmental science; Physics; Optics; Aerospace engineering; Engineering; Telecommunications","score_opus":0.026633848648375483,"score_gpt":0.281739915765091,"score_spread":0.2551060671167155,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4323538902","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000057902744,0.0011319964,0.000049461538,0.09246093,0.002110414,0.00036898244,0.00003058091,0.00025906388,0.90353066],"genre_scores_gemma":[0.00002931231,0.004068366,0.00034510292,0.05310241,0.00019613974,0.00004342743,0.0000902239,0.000046680423,0.94207835],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99833053,0.000024771807,0.0002411194,0.0005397896,0.0005802115,0.00028354733],"domain_scores_gemma":[0.99912465,0.00004423267,0.000103275175,0.00062300824,0.00000447672,0.00010037358],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00022455919,0.000242957,0.00032761027,5.388124e-7,0.0000688406,0.000015988015,0.00039722747,0.00012758917,0.09847091],"category_scores_gemma":[0.000068024994,0.00017685289,0.00015573783,0.00024058216,0.00008041738,0.000024503688,0.00031178448,0.00027882773,0.06333811],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[9.3211844e-7,0.000014719058,0.000053560478,0.00008757458,0.000006586059,0.000012736312,0.0000043158343,0.000016168962,0.0000014641738,0.000026023525,0.98855233,0.011223569],"study_design_scores_gemma":[0.000037932343,0.00005578271,0.0006008019,0.0003897072,0.0000239321,0.0000017438849,0.0000042182833,0.000017269687,0.0000044386225,0.000094026655,0.9985376,0.00023254892],"about_ca_topic_score_codex":0.0016726335,"about_ca_topic_score_gemma":0.00017862981,"teacher_disagreement_score":0.03935852,"about_ca_system_score_codex":0.00013943181,"about_ca_system_score_gemma":0.000013723495,"threshold_uncertainty_score":0.93739116},"labels":[],"label_agreement":null},{"id":"W4360608896","doi":"10.1175/bams-d-21-0197.1","title":"WiFEX: Walk into the Warm Fog over Indo-Gangetic Plain Region","year":2023,"lang":"en","type":"article","venue":"Bulletin of the American Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"Indian Institute of Science Education and Research Mohali; Indian Institute of Technology Madras; Ministry of Earth Sciences; Indian Institute of Science","keywords":"Weather Research and Forecasting Model; Aerosol; Meteorology; Environmental science; Predictability; Radiative transfer; Atmospheric sciences; Geography; Geology; Physics","score_opus":0.009691512686644964,"score_gpt":0.22391261763307077,"score_spread":0.2142211049464258,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4360608896","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":[0.971934,0.00005200876,0.00017455844,0.024722155,0.000094342875,0.000253033,0.0000017226955,0.00009039612,0.0026777624],"genre_scores_gemma":[0.9861915,0.00022919742,0.0017721774,0.009595211,0.00006976594,0.000046261266,0.0000013509797,0.000018894052,0.0020756102],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99809766,0.00029035786,0.00026920205,0.00038637206,0.00051709247,0.00043928844],"domain_scores_gemma":[0.99863386,0.00040286517,0.00031394124,0.0005529125,0.000008504017,0.000087891356],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006614535,0.00020093373,0.00030654008,8.009475e-7,0.000396497,0.00001777986,0.00096534495,0.000088264926,0.0019274323],"category_scores_gemma":[0.00019145028,0.000098134245,0.00044767564,0.00069863343,0.0026127868,0.000013721983,0.0008499779,0.0003286674,0.0004687294],"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":[0.0001427908,0.0001959814,0.15489715,0.000013467556,0.0001229656,0.000011839123,0.0032359262,0.0025356961,0.00854213,0.0003353709,0.78774446,0.042222243],"study_design_scores_gemma":[0.00038274494,0.00042320145,0.61957985,0.000009723877,0.00006263057,0.000007883426,0.0021842145,0.00094554375,0.00062373496,0.0025553557,0.37291163,0.00031351516],"about_ca_topic_score_codex":0.0017482465,"about_ca_topic_score_gemma":0.000013901081,"teacher_disagreement_score":0.46468267,"about_ca_system_score_codex":0.00010052786,"about_ca_system_score_gemma":0.000008339809,"threshold_uncertainty_score":0.99898493},"labels":[],"label_agreement":null},{"id":"W4362737484","doi":"10.1364/ao.488571","title":"Design of a single aspheric beam homogenizer for accurate particle sizing application","year":2023,"lang":"en","type":"article","venue":"Applied Optics","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"McMaster University","funders":"China Scholarship Council","keywords":"Sizing; Optics; Homogenizer; Metrology; Beam (structure); Lens (geology); Materials science; Gaussian beam; Particle (ecology); Physics","score_opus":0.02809641278653611,"score_gpt":0.23772869777735076,"score_spread":0.20963228499081465,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4362737484","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":[0.51515746,0.000013625621,0.48293343,0.000050465398,0.000028015449,0.00052537164,0.0000023811544,0.00008189357,0.0012073634],"genre_scores_gemma":[0.9362312,0.0000129548735,0.06314885,0.00007743595,0.000025212075,0.00022612298,0.000006488725,0.000023109298,0.0002486514],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99916726,0.000006736605,0.00019868148,0.00021443205,0.00015354385,0.00025932558],"domain_scores_gemma":[0.9995105,0.00010790046,0.00009898048,0.00021914016,0.000008435091,0.00005501325],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018172232,0.00009774986,0.00012293669,8.261593e-7,0.00009319105,0.000014659093,0.00015849977,0.000054124797,0.00007902906],"category_scores_gemma":[0.000015268482,0.00009393166,0.000033792003,0.00042932061,0.000088310895,0.000047702524,0.00009309212,0.000035379046,0.00028647325],"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":[0.000035400448,0.00009056766,0.00067190966,0.000011621306,0.000012132484,4.192216e-7,0.00033020688,0.15608214,0.8211329,0.00092719315,0.000433657,0.020271871],"study_design_scores_gemma":[0.0016045079,0.00044368007,0.008076316,0.000010098376,0.000118982716,0.00000241485,0.0013224554,0.5361067,0.43943003,0.007985111,0.0042061973,0.000693527],"about_ca_topic_score_codex":0.000009401138,"about_ca_topic_score_gemma":0.0000018722282,"teacher_disagreement_score":0.4210737,"about_ca_system_score_codex":0.000042206684,"about_ca_system_score_gemma":0.0000073278707,"threshold_uncertainty_score":0.3830422},"labels":[],"label_agreement":null},{"id":"W4365137150","doi":"10.5194/amt-16-1901-2023","title":"Processing reflectivity and Doppler velocity from EarthCARE's cloud-profiling radar: the C-FMR, C-CD and C-APC products","year":2023,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Centre for Earth Observation; European Space Agency","keywords":"Doppler effect; Remote sensing; Radar; Attenuation; Environmental science; Geology; Computer science; Optics; Physics; Telecommunications","score_opus":0.029602467058829768,"score_gpt":0.24314352897992514,"score_spread":0.21354106192109537,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4365137150","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":[0.9888372,0.0010885373,0.004331762,0.001574313,0.00013470443,0.00094525405,0.00000402728,0.0008737283,0.002210508],"genre_scores_gemma":[0.94050264,0.00034658835,0.05820646,0.0003373123,0.0001599925,0.00015675338,0.000004799096,0.000043668824,0.00024177294],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99737096,0.00015921547,0.0003115549,0.0007879725,0.0008872147,0.00048306983],"domain_scores_gemma":[0.9991401,0.00004953202,0.00016604702,0.00046196036,0.000059023063,0.00012334963],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014263329,0.00032550987,0.00028973093,7.911792e-7,0.00062920916,0.00014346685,0.0002815696,0.00013093173,0.00011445879],"category_scores_gemma":[0.00015158362,0.00023487021,0.000042998803,0.0007080983,0.00041186032,0.00027474228,0.0004549931,0.0003039574,0.000028855382],"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":[0.00008895616,0.000121874924,0.27063322,0.00010066469,0.00007803789,0.000023129971,0.0017717406,0.000031238636,0.18438046,0.00010154693,0.01408658,0.5285826],"study_design_scores_gemma":[0.0007898932,0.00045806143,0.7861991,0.00028084815,0.0001845756,0.00004133682,0.0013683038,0.0058058086,0.14086501,0.0069585363,0.055385385,0.0016631784],"about_ca_topic_score_codex":0.001768425,"about_ca_topic_score_gemma":0.00024387175,"teacher_disagreement_score":0.52691936,"about_ca_system_score_codex":0.00018841703,"about_ca_system_score_gemma":0.000045909514,"threshold_uncertainty_score":0.9577729},"labels":[],"label_agreement":null},{"id":"W4366263172","doi":"10.1016/j.atmosenv.2023.119798","title":"The extreme forest fires in California/Oregon in 2020: Aerosol optical and physical properties and comparisons of aged versus fresh smoke","year":2023,"lang":"en","type":"article","venue":"Atmospheric Environment","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":30,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Sherbrooke","funders":"","keywords":"AERONET; Aerosol; Environmental science; Atmospheric sciences; Cloud condensation nuclei; Particulates; Plume; Smoke; Range (aeronautics); Climatology; Meteorology; Chemistry; Geography; Geology; Materials science","score_opus":0.027714447759622594,"score_gpt":0.21846869884829076,"score_spread":0.19075425108866817,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4366263172","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":[0.9983354,0.00045800098,0.00004902243,0.00045513446,0.00004420121,0.00033090237,0.0000035511353,0.0000190826,0.0003046903],"genre_scores_gemma":[0.9978262,0.0009859572,0.0008612207,0.000028217104,0.00002027583,0.00008677244,0.0000029365624,0.000020592382,0.00016783272],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984779,0.00006992703,0.00030872444,0.00038631534,0.00033811724,0.0004190394],"domain_scores_gemma":[0.9993606,0.00019042067,0.00007594149,0.00026775405,0.0000010699857,0.00010421956],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022150578,0.00020759492,0.00027457564,4.9594263e-7,0.00013861124,0.000024523324,0.00018471708,0.000069840855,0.00012382414],"category_scores_gemma":[0.000035550478,0.00014477094,0.000040967403,0.00021616646,0.0009017645,0.000072889,0.00046503125,0.0001928725,0.00005920131],"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":[0.00019145303,0.00019486957,0.9731874,0.000015491662,0.000016224478,0.000023949391,0.0013066593,0.01485658,0.002256936,0.000043469816,0.0007696292,0.0071373493],"study_design_scores_gemma":[0.0010433001,0.00020538222,0.9577489,0.000023285484,0.000014967212,0.0000018378643,0.001709702,0.037585143,0.00023489301,0.00007688657,0.0011535361,0.00020218642],"about_ca_topic_score_codex":0.00097020133,"about_ca_topic_score_gemma":0.0015456241,"teacher_disagreement_score":0.022728564,"about_ca_system_score_codex":0.0001239909,"about_ca_system_score_gemma":0.0000068427403,"threshold_uncertainty_score":0.59035873},"labels":[],"label_agreement":null},{"id":"W4366548021","doi":"10.5194/egusphere-2022-1156-ac2","title":"Reply on RC2","year":2023,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"AERONET; Environmental science; Remote sensing; Albedo (alchemy); Aerosol; Mineral dust; Satellite; Cloud cover; Snow; Meteorology; Angstrom exponent; Moderate-resolution imaging spectroradiometer; Geography; Cloud computing; Physics; Computer science","score_opus":0.026633848648375483,"score_gpt":0.281739915765091,"score_spread":0.2551060671167155,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4366548021","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00006548601,0.001205787,0.0000470888,0.08849661,0.0021571363,0.00036911818,0.00003044481,0.00028642063,0.9073419],"genre_scores_gemma":[0.000033521246,0.004197328,0.00034701996,0.051794935,0.00019426917,0.00004353826,0.000086621694,0.0000505827,0.9432522],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99833435,0.000025311665,0.00024159427,0.0005325583,0.000581824,0.0002843503],"domain_scores_gemma":[0.9991102,0.000045346613,0.00010298396,0.00063471514,0.0000044947315,0.0001022104],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00022004108,0.00024343908,0.00032931328,5.365427e-7,0.00006589008,0.000015709722,0.00039730524,0.00012775707,0.088166036],"category_scores_gemma":[0.00006913707,0.00017711028,0.00015615257,0.00024002179,0.00007906676,0.000024001372,0.0003112692,0.00028044882,0.060281694],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[9.0633006e-7,0.000014688772,0.000075859316,0.000086867134,0.000006622682,0.000012957176,0.0000045206316,0.000012000564,0.0000011091901,0.000022404636,0.98738784,0.012374245],"study_design_scores_gemma":[0.00003803681,0.000055945402,0.0006705168,0.0004082378,0.00002428574,0.0000017790625,0.000004380457,0.000016187134,0.0000036556626,0.00008328983,0.9984608,0.00023283964],"about_ca_topic_score_codex":0.0015587653,"about_ca_topic_score_gemma":0.00019214509,"teacher_disagreement_score":0.03670168,"about_ca_system_score_codex":0.00013718694,"about_ca_system_score_gemma":0.0000137275065,"threshold_uncertainty_score":0.94045},"labels":[],"label_agreement":null},{"id":"W4366596355","doi":"10.5194/egusphere-2022-1156-ac1","title":"Reply on RC1","year":2023,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"AERONET; Environmental science; Remote sensing; Albedo (alchemy); Mineral dust; Aerosol; Satellite; Meteorology; Snow; Cloud cover; Angstrom exponent; Moderate-resolution imaging spectroradiometer; Geology; Geography; Cloud computing; Physics; Computer science","score_opus":0.026633848648375483,"score_gpt":0.281739915765091,"score_spread":0.2551060671167155,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4366596355","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000058078247,0.0011877151,0.00004543212,0.0853886,0.002073141,0.00035407513,0.000030504487,0.0002458215,0.91061664],"genre_scores_gemma":[0.000027702192,0.0043644817,0.00035001742,0.051770918,0.00019447974,0.000043493215,0.00009016552,0.000046762725,0.94311196],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9983323,0.000025353,0.00024181827,0.00053312036,0.00058265665,0.00028470292],"domain_scores_gemma":[0.99910927,0.00004543233,0.00010303268,0.0006354473,0.0000045023767,0.00010229738],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00022354668,0.00024356734,0.0003295704,5.3738205e-7,0.000069201546,0.000015738513,0.0003981685,0.00012786122,0.09315952],"category_scores_gemma":[0.000069304166,0.0001771951,0.000156209,0.00024060541,0.00007920655,0.000024017369,0.0003119409,0.00028079824,0.06324427],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[9.0600514e-7,0.000014704292,0.000057636375,0.00008690968,0.000006618528,0.000012947123,0.000004546301,0.000015874757,0.0000010762662,0.000023632181,0.9862739,0.013501277],"study_design_scores_gemma":[0.0000382743,0.00005604107,0.0006027008,0.000408913,0.000024297176,0.0000017800179,0.000004393374,0.000016963368,0.0000036020417,0.00008410035,0.9985259,0.00023299616],"about_ca_topic_score_codex":0.0016544036,"about_ca_topic_score_gemma":0.00018394631,"teacher_disagreement_score":0.033617683,"about_ca_system_score_codex":0.00013927974,"about_ca_system_score_gemma":0.000013796646,"threshold_uncertainty_score":0.9374851},"labels":[],"label_agreement":null},{"id":"W4376643871","doi":"10.5194/gmd-2023-75","title":"Spherical Air Mass Factors in One and Two Dimensions with SASKTRAN 1.6.0","year":2023,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada; University of Saskatchewan","funders":"Environment and Climate Change Canada","keywords":"Air mass (solar energy); Geostationary orbit; Monte Carlo method; Atmosphere (unit); Air quality index; Radiative transfer; Environmental science; Meteorology; Troposphere; Clear-air turbulence; Physics; Mathematics; Aerospace engineering; Satellite; Mechanics; Engineering; Statistics; Optics","score_opus":0.025166205734956495,"score_gpt":0.237444457719762,"score_spread":0.2122782519848055,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4376643871","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":[0.98804915,0.00001797156,0.004629641,0.0004401623,0.000094362804,0.00030643493,0.0000062062377,0.00012962353,0.0063264435],"genre_scores_gemma":[0.97387385,0.00005125166,0.022342334,0.00014015619,0.000019582627,0.000028142544,0.00001078566,0.000039725222,0.0034941523],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99844414,0.000036393445,0.00021777183,0.0006376879,0.00032707662,0.00033693036],"domain_scores_gemma":[0.9993649,0.000055841756,0.000063519736,0.00034048982,0.0000028738198,0.00017235496],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00009417635,0.0002723309,0.0003269322,0.0000015125983,0.0000673994,0.000024754885,0.00019909056,0.00015708231,0.0018451958],"category_scores_gemma":[0.0000081850685,0.00019722362,0.000045721965,0.00019316313,0.00025524438,0.000050523027,0.0007414633,0.00044768755,0.00015404724],"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":[0.000019222349,0.00009187033,0.9785293,0.000015379313,0.000023828256,0.000034548517,0.00046355207,0.018575756,0.001219073,0.000064437634,0.00043685635,0.0005262069],"study_design_scores_gemma":[0.00043455802,0.00009502332,0.9936391,0.00006576383,0.000028080363,0.00000179925,0.0007113505,0.0020987655,0.0003265605,0.0017442177,0.00036703804,0.0004877516],"about_ca_topic_score_codex":0.008543022,"about_ca_topic_score_gemma":0.0059249704,"teacher_disagreement_score":0.017712692,"about_ca_system_score_codex":0.00013363623,"about_ca_system_score_gemma":0.000019910007,"threshold_uncertainty_score":0.99906725},"labels":[],"label_agreement":null},{"id":"W4376643947","doi":"10.5194/egusphere-2023-821","title":"Shallow and Deep Convection Characteristics in the Greater Houston, Texas Area Using Cell Tracking Methodology","year":2023,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Convection; Diurnal cycle; Convection cell; Radar; Atmospheric sciences; Environmental science; Radiative transfer; Meteorology; Geology; Climatology; Geography; Physics; Optics; Natural convection; Computer science; Combined forced and natural convection","score_opus":0.13231702594265288,"score_gpt":0.2935678067906299,"score_spread":0.161250780847977,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4376643947","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":[0.9474704,0.000025093106,0.049850482,0.00015857867,0.00033650862,0.00029059532,0.0000034157829,0.00004825942,0.0018166136],"genre_scores_gemma":[0.9861077,0.000097538876,0.012523424,0.00036195945,0.00006912573,0.000016377344,0.000009519634,0.000030233079,0.0007841172],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984702,0.00025709288,0.00029946846,0.0005070651,0.00018266331,0.00028353214],"domain_scores_gemma":[0.9993433,0.00015449528,0.00016032138,0.0002919361,0.0000058692567,0.000044114116],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008065738,0.00023170614,0.00030234337,0.000003552835,0.0000938583,0.00008082724,0.0002572112,0.00028465016,0.00082662026],"category_scores_gemma":[0.00003612321,0.00016211445,0.00005827271,0.00011709917,0.00017287856,0.000052072668,0.00059862045,0.00047211387,0.00006196356],"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":[0.000033003573,0.00004970279,0.98364496,0.00006405593,0.00001656626,0.000074793716,0.0035973797,0.004072356,0.0024036372,0.000018109791,0.00009722002,0.0059282347],"study_design_scores_gemma":[0.00015617342,0.00004560856,0.960332,0.000026082938,0.000054983022,0.00003186805,0.00080757536,0.03697718,0.00024125833,0.00081096136,0.00020699503,0.00030931475],"about_ca_topic_score_codex":0.0026351071,"about_ca_topic_score_gemma":0.00075365946,"teacher_disagreement_score":0.03863725,"about_ca_system_score_codex":0.0001280913,"about_ca_system_score_gemma":0.000010363791,"threshold_uncertainty_score":0.9050912},"labels":[],"label_agreement":null},{"id":"W4376863068","doi":"10.5194/amt-2023-67","title":"Analysis of Lhù’ààn Mân’ (Kluane Lake) dust plumes using passive and active ground-based remote sensing supported by physical surface measurements","year":2023,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université de Montréal; Université de Sherbrooke","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Foundation for Innovation","keywords":"AERONET; Environmental science; Lidar; Arctic; Remote sensing; Aerosol; Satellite; Snow; Meteorology; Geology; Geography; Physics; Oceanography","score_opus":0.04339092941301023,"score_gpt":0.2801028071558285,"score_spread":0.2367118777428183,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4376863068","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":[0.9711375,0.000013635752,0.027432745,0.00014685598,0.00012551922,0.0003699887,0.00014695717,0.000086850465,0.00053989684],"genre_scores_gemma":[0.9905351,0.000015388021,0.008147793,0.000085550135,0.000029352248,8.3776393e-7,0.00021391166,0.000052928906,0.0009191471],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99689597,0.00016967216,0.0004686153,0.0010265914,0.0009798101,0.00045935594],"domain_scores_gemma":[0.9985106,0.000118196505,0.0005429884,0.00058246887,0.000054985554,0.00019078581],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00028425743,0.00047520202,0.00094213104,0.000010443988,0.00016709504,0.00007042433,0.00025600838,0.0002817224,0.0007168886],"category_scores_gemma":[0.000049512688,0.00043652838,0.00032322836,0.00083347346,0.00042333078,0.00010662753,0.000773466,0.00040231543,0.000018347248],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028050784,0.0004815299,0.17935833,0.00019708667,0.0061361813,0.000083899875,0.0025255657,0.50001454,0.2810807,0.0000026061116,0.0016271197,0.028211921],"study_design_scores_gemma":[0.00044792303,0.000055082844,0.11425442,0.00008058844,0.0023308466,0.0000012669474,0.0006904926,0.8666914,0.014633691,0.00010711684,0.00005574635,0.0006514257],"about_ca_topic_score_codex":0.016961832,"about_ca_topic_score_gemma":0.0031401361,"teacher_disagreement_score":0.36667684,"about_ca_system_score_codex":0.00036882545,"about_ca_system_score_gemma":0.0000709089,"threshold_uncertainty_score":0.99980867},"labels":[],"label_agreement":null},{"id":"W4377013752","doi":"10.1175/jas-d-22-0173.1","title":"Kinetic Energy Spectra and Spectral Budget of Radiative–Convective Equilibrium","year":2023,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"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 Waterloo","funders":"","keywords":"Stratosphere; Kinetic energy; Troposphere; Dissipation; Atmospheric sciences; Radiative transfer; Energy flux; Convection; Radiative cooling; Physics; Radiative flux; Buoyancy; Energy budget; Radiant energy; Mechanics; Environmental science; Meteorology; Thermodynamics; Classical mechanics","score_opus":0.008363577119572153,"score_gpt":0.2215591681266035,"score_spread":0.21319559100703137,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4377013752","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":[0.9931601,0.00028854428,0.00018917481,0.0009804555,0.00044266626,0.000062909676,8.371103e-7,0.0000101172745,0.004865149],"genre_scores_gemma":[0.9955218,0.00013914883,0.003261329,0.00015678987,0.00009676454,0.0000016578365,4.046777e-8,0.0000076041333,0.00081486255],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984764,0.00009089545,0.0003430284,0.00018946156,0.0006080798,0.00029212286],"domain_scores_gemma":[0.99914324,0.00013138779,0.00046101448,0.00014814874,0.000017045848,0.00009914578],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005876386,0.00012738633,0.00023960677,0.0000012056712,0.00014866127,0.00003481152,0.0006656678,0.000037046328,0.0004664897],"category_scores_gemma":[0.000092669514,0.0000743725,0.00012751253,0.0013570102,0.0012432048,0.00026165743,0.00026258346,0.00011413035,0.000011844821],"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":[0.00012404312,0.00020834412,0.6879003,0.000022136614,0.00013665918,0.000055974353,0.0038838678,0.12466919,0.1488855,0.0027040276,0.015689064,0.015720872],"study_design_scores_gemma":[0.0005923674,0.0010123203,0.91970533,0.000051711297,0.0000604472,0.00016799853,0.0019589197,0.0449217,0.016647508,0.011789848,0.0028061636,0.0002856601],"about_ca_topic_score_codex":0.00022274182,"about_ca_topic_score_gemma":0.000018859077,"teacher_disagreement_score":0.23180504,"about_ca_system_score_codex":0.00006642221,"about_ca_system_score_gemma":0.000055792683,"threshold_uncertainty_score":0.51077354},"labels":[],"label_agreement":null},{"id":"W4378220389","doi":"10.5194/amt-16-2485-2023","title":"HETEAC – the Hybrid End-To-End Aerosol Classification model for EarthCARE","year":2023,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","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":"Environment and Climate Change Canada","funders":"European Space Agency","keywords":"Aerosol; Radiative transfer; Environmental science; Remote sensing; Atmospheric sciences; Radiative forcing; Troposphere; Lidar; Meteorology; Physics; Geology; Optics","score_opus":0.05685792715333954,"score_gpt":0.2678441849240116,"score_spread":0.21098625777067204,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4378220389","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.2594702,0.000116763425,0.7165496,0.0065637175,0.00028984586,0.0045009437,0.000033337983,0.0023571483,0.010118468],"genre_scores_gemma":[0.9388938,0.00006201822,0.05539267,0.001180648,0.000086240485,0.0018066203,0.000016232498,0.00006288233,0.0024988945],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9972304,0.000072108174,0.00039253768,0.0006225858,0.0010894587,0.00059288],"domain_scores_gemma":[0.9988173,0.000048726946,0.00014392666,0.0007511859,0.000075812815,0.00016303714],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012652938,0.000300499,0.00023359549,8.513303e-7,0.00047808772,0.00007723299,0.00063499564,0.000089787274,0.0004504812],"category_scores_gemma":[0.000116824594,0.00022350207,0.00016358458,0.00058320997,0.00016075512,0.00016142693,0.00023738582,0.00016218623,0.00038246528],"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":[0.000100329176,0.00019791386,0.010534241,0.00004765875,0.0000810972,0.0000059168647,0.001297041,0.009509569,0.19109166,0.00081247336,0.33412603,0.4521961],"study_design_scores_gemma":[0.00059892953,0.0006856958,0.027281607,0.000107008724,0.0001317699,0.000010301284,0.00083462143,0.7048884,0.072942495,0.0040390855,0.18698473,0.0014953339],"about_ca_topic_score_codex":0.00017710523,"about_ca_topic_score_gemma":0.00012941354,"teacher_disagreement_score":0.69537884,"about_ca_system_score_codex":0.00037184317,"about_ca_system_score_gemma":0.000044063967,"threshold_uncertainty_score":0.911415},"labels":[],"label_agreement":null},{"id":"W4378533394","doi":"10.5194/amt-2023-67-rc1","title":"Comment on amt-2023-67","year":2023,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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 de Sherbrooke","funders":"","keywords":"AERONET; Lidar; Environmental science; Arctic; Aerosol; Remote sensing; Satellite; Mineral dust; Meteorology; Geography; Geology; Physics; Oceanography","score_opus":0.028999854015114592,"score_gpt":0.2838758062322327,"score_spread":0.2548759522171181,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4378533394","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000027008291,0.0012795257,0.00009704689,0.3555096,0.0025010838,0.0005717032,0.00008109476,0.00019545492,0.6397375],"genre_scores_gemma":[0.000031602092,0.0054951455,0.00040288534,0.11779131,0.00018226095,0.00008870605,0.00022555528,0.00005257654,0.87573],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.997904,0.000046834266,0.00031697983,0.000559756,0.000778827,0.00039359884],"domain_scores_gemma":[0.9989969,0.00007289224,0.00012867348,0.00064353505,0.0000058180576,0.00015219337],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00028556702,0.00034320576,0.00043333796,9.694705e-7,0.00010979985,0.0000247703,0.0005463568,0.00018671088,0.10796221],"category_scores_gemma":[0.00003511599,0.0002559356,0.00019979708,0.00026328588,0.00010290307,0.000026719736,0.0005488561,0.0003738072,0.063978724],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000001363191,0.000043084932,0.00008334841,0.00012542271,0.000014548229,0.000011660657,0.000007083176,0.000025051457,8.315111e-7,0.00007886452,0.99015397,0.009454757],"study_design_scores_gemma":[0.0000780575,0.000087642286,0.00042300817,0.0005387954,0.00004002253,0.0000011422833,0.000011711769,0.000037984115,0.000004055424,0.00010123569,0.99835515,0.00032118542],"about_ca_topic_score_codex":0.0020264373,"about_ca_topic_score_gemma":0.00039039322,"teacher_disagreement_score":0.23771828,"about_ca_system_score_codex":0.00028463136,"about_ca_system_score_gemma":0.0000146637085,"threshold_uncertainty_score":0.9999893},"labels":[],"label_agreement":null},{"id":"W4379519453","doi":"10.5194/egusphere-2023-821-rc1","title":"Comment on egusphere-2023-821","year":2023,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"","keywords":"Convection; Diurnal cycle; Radar; Convection cell; Atmospheric sciences; Radiative transfer; Environmental science; Meteorology; Climatology; Geology; Geography; Physics; Optics; Computer science; Natural convection","score_opus":0.026519451065640357,"score_gpt":0.2787614837128978,"score_spread":0.2522420326472574,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4379519453","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000026869115,0.0017392719,0.00010614558,0.29057825,0.002603985,0.0006268358,0.000079378566,0.00022069445,0.7040186],"genre_scores_gemma":[0.000030923748,0.0050057084,0.0005593071,0.10925082,0.00020833308,0.00010748516,0.0002272621,0.0000691094,0.88454103],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9975294,0.000060311766,0.00038315012,0.00066549086,0.00089243177,0.00046923975],"domain_scores_gemma":[0.99879265,0.000090912305,0.00015889478,0.0007659824,0.0000078993,0.00018364076],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00031004022,0.0004198152,0.000537524,8.6919823e-7,0.00012686872,0.00003112813,0.0006385304,0.0002355387,0.20077589],"category_scores_gemma":[0.000043714306,0.00031787404,0.000242349,0.00033290332,0.0001199187,0.0000331788,0.000610077,0.000441745,0.07043006],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000020480795,0.00005557872,0.000073873634,0.00015504782,0.00002036663,0.000014800619,0.000007824531,0.00004074576,9.494928e-7,0.00008113628,0.98545045,0.014097202],"study_design_scores_gemma":[0.000102286685,0.00010589774,0.0002937824,0.0006566592,0.000049985865,0.0000014929335,0.000018477604,0.000047173722,0.000004760983,0.000115740564,0.9982078,0.00039595415],"about_ca_topic_score_codex":0.0030773457,"about_ca_topic_score_gemma":0.00083232415,"teacher_disagreement_score":0.18132743,"about_ca_system_score_codex":0.0003476254,"about_ca_system_score_gemma":0.00002149148,"threshold_uncertainty_score":0.99992734},"labels":[],"label_agreement":null},{"id":"W4379537572","doi":"10.5194/amt-16-2795-2023","title":"The classification of atmospheric hydrometeors and aerosols from the EarthCARE radar and lidar: the A-TC, C-TC and AC-TC products","year":2023,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"European Space Agency","keywords":"Lidar; Remote sensing; Radar; Snow; Environmental science; Aerosol; Meteorology; Atmosphere (unit); Precipitation; Atmospheric sciences; Geology; Computer science; Geography","score_opus":0.02295763987894373,"score_gpt":0.22196808090580908,"score_spread":0.19901044102686535,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4379537572","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":[0.9868395,0.004454268,0.0006962766,0.005290863,0.0001168631,0.0014209764,0.000006807654,0.00027599267,0.0008984739],"genre_scores_gemma":[0.9845777,0.0040906724,0.010313621,0.00027123975,0.00007880833,0.00024793393,0.000004210821,0.000045407327,0.00037036833],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99700487,0.00028861576,0.0004797102,0.00066098716,0.0011216472,0.00044419055],"domain_scores_gemma":[0.99835294,0.00027791192,0.00031794413,0.00087338185,0.000070707,0.00010710119],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018393344,0.00034963276,0.0003073319,3.531021e-7,0.0009047439,0.00016883205,0.00054049754,0.00013077803,0.000068280606],"category_scores_gemma":[0.00026367998,0.00018433374,0.000060862538,0.0007621338,0.0011665658,0.00019878946,0.0004898413,0.0002772996,0.000013316873],"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":[0.00013363759,0.00012671085,0.25558028,0.00007687009,0.00024844488,0.000007733569,0.003904467,0.00002503217,0.22628458,0.00069460477,0.029391007,0.48352665],"study_design_scores_gemma":[0.00042598348,0.00042868737,0.894383,0.00013314407,0.0001666108,0.000015295855,0.003705332,0.0023343607,0.015309946,0.0022984103,0.08019612,0.00060309935],"about_ca_topic_score_codex":0.00079284114,"about_ca_topic_score_gemma":0.0001985954,"teacher_disagreement_score":0.6388027,"about_ca_system_score_codex":0.00009398983,"about_ca_system_score_gemma":0.000038416765,"threshold_uncertainty_score":0.75169116},"labels":[],"label_agreement":null},{"id":"W4379740065","doi":"10.2139/ssrn.4472159","title":"Stokes Parameters Measurement System Designed by Symmetric Polarization Spectrophotometry with Double Quarter-Wave Plate","year":2023,"lang":"en","type":"preprint","venue":"SSRN Electronic Journal","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Waveplate; Quarter (Canadian coin); Stokes parameters; Polarization (electrochemistry); Spectrophotometry; Optics; Physics; Chemistry; Geography","score_opus":0.019256689048496697,"score_gpt":0.2082158668380606,"score_spread":0.1889591777895639,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4379740065","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":[0.8138529,0.001872695,0.18140216,0.00025022172,0.00058906665,0.0009165802,0.000013053475,0.00023837363,0.0008649763],"genre_scores_gemma":[0.9958068,0.0010018582,0.0015217272,0.00003432735,0.00011234484,0.000059189904,0.000029896646,0.00011925776,0.0013145908],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9936333,0.00020044205,0.0006527367,0.00081878563,0.0018562764,0.0028384891],"domain_scores_gemma":[0.99835336,0.000036556426,0.00078649324,0.0005067907,0.00005927683,0.0002575251],"candidate_categories":["metaepi_narrow","research_integrity"],"consensus_categories":[],"category_scores_codex":[0.0026074683,0.00059594825,0.00058096595,0.000039834165,0.00043472956,0.0002777161,0.00063223974,0.0003362621,0.000079476275],"category_scores_gemma":[0.000020962427,0.0004844546,0.00022510967,0.0010643268,0.000120778954,0.00019504267,0.0002837106,0.003129182,0.00020740001],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.012418206,0.004487006,0.34498876,0.0022242519,0.022921914,0.0014816849,0.006685348,0.3009676,0.16615035,0.021918569,0.023711892,0.09204441],"study_design_scores_gemma":[0.092927754,0.061035834,0.19542287,0.011463925,0.01687076,0.02139933,0.14441659,0.1571187,0.068938285,0.17523448,0.008286215,0.04688526],"about_ca_topic_score_codex":0.0021573848,"about_ca_topic_score_gemma":0.00063082407,"teacher_disagreement_score":0.18195394,"about_ca_system_score_codex":0.010917104,"about_ca_system_score_gemma":0.00081101316,"threshold_uncertainty_score":0.9997607},"labels":[],"label_agreement":null},{"id":"W4380079591","doi":"10.5194/amt-16-2865-2023","title":"Cloud and precipitation microphysical retrievals from the EarthCARE Cloud Profiling Radar: the C-CLD product","year":2023,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Centre for Earth Observation; University of Leicester; European Space Agency","keywords":"Environmental science; Meteorology; Radar; Remote sensing; Drizzle; Grid; Satellite; Cloud computing; Precipitation; Computer science; Geology; Geodesy; Geography; Aerospace engineering","score_opus":0.02276599365278859,"score_gpt":0.23324189892310518,"score_spread":0.2104759052703166,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4380079591","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":[0.9873846,0.0008819878,0.0027073363,0.0047237636,0.0004100727,0.0018297936,0.000008554719,0.00071866653,0.001335197],"genre_scores_gemma":[0.97954565,0.00031110586,0.017868675,0.0006915557,0.00063288707,0.0002420004,0.000010144913,0.00005178307,0.0006462067],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9970513,0.0002748688,0.00036148436,0.0006195203,0.0012687253,0.00042412692],"domain_scores_gemma":[0.9988445,0.0001418679,0.0001776211,0.00069477985,0.00005920177,0.00008203918],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001485426,0.00028969112,0.00023371271,3.832912e-7,0.0005659079,0.000119917604,0.0005144862,0.000089826775,0.00018710786],"category_scores_gemma":[0.00023561408,0.00016836736,0.000094945884,0.0007267081,0.00038091876,0.00014880009,0.00035418625,0.00030831125,0.00012587426],"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":[0.00016829013,0.00018446191,0.14815788,0.000043929507,0.00018453857,0.000015643507,0.0038620194,0.000105168365,0.47522923,0.00064567965,0.11631914,0.25508404],"study_design_scores_gemma":[0.0007347909,0.00084152847,0.29910612,0.0002726763,0.00028835697,0.000013805554,0.0030390967,0.002409992,0.44473734,0.0100079905,0.23704375,0.0015045394],"about_ca_topic_score_codex":0.0004578111,"about_ca_topic_score_gemma":0.000040827785,"teacher_disagreement_score":0.2535795,"about_ca_system_score_codex":0.00014191923,"about_ca_system_score_gemma":0.000033505345,"threshold_uncertainty_score":0.68658215},"labels":[],"label_agreement":null},{"id":"W4380090652","doi":"10.5194/acp-23-6299-2023","title":"The (mis)identification of high-latitude dust events using remote sensing methods in the Yukon, Canada: a sub-daily variability analysis","year":2023,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université de Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Environment and Climate Change Canada; University of Sheffield","keywords":"AERONET; Environmental science; Mineral dust; Latitude; Remote sensing; Aerosol; Meteorology; Satellite; Plume; Atmospheric sciences; Climatology; Geology; Geography; Geodesy","score_opus":0.010569898991790868,"score_gpt":0.259404245716368,"score_spread":0.24883434672457713,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4380090652","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":[0.93552905,0.000021130445,0.06398929,0.00011176797,0.000034787514,0.00009279664,0.000004134834,0.000010223766,0.00020680329],"genre_scores_gemma":[0.9743636,0.00003280091,0.025276044,0.000034442666,0.000034221554,0.0000012724552,0.000009311529,0.000008270298,0.00024003962],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9987028,0.00016772504,0.0003292611,0.00028984732,0.00029060323,0.00021974689],"domain_scores_gemma":[0.9989681,0.00033094763,0.00019181095,0.00045132497,0.000016449258,0.00004134451],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010149683,0.00013408111,0.00019696043,3.547577e-8,0.0002667125,0.0000250463,0.00022457392,0.000053565014,0.000051796942],"category_scores_gemma":[0.00007445089,0.00009482039,0.00006523545,0.0014091666,0.00016258672,0.000054074546,0.00007832874,0.00013989989,0.0000014899509],"study_design_candidate":"simulation_or_modeling","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":[0.00003509296,0.0000743612,0.07368845,0.00008480964,0.0003005737,0.000009460906,0.0015669513,0.346964,0.14712878,0.000035038163,0.00024088225,0.42987162],"study_design_scores_gemma":[0.00011874249,0.000003680134,0.28932443,0.000007727121,0.00017696402,0.0000020677812,0.00047190583,0.70123684,0.006174787,0.0021516362,0.00018019944,0.00015099806],"about_ca_topic_score_codex":0.15398003,"about_ca_topic_score_gemma":0.013561547,"teacher_disagreement_score":0.4297206,"about_ca_system_score_codex":0.00015539766,"about_ca_system_score_gemma":0.000055918987,"threshold_uncertainty_score":0.8516537},"labels":[],"label_agreement":null},{"id":"W4380265264","doi":"10.5194/egusphere-2023-821-rc2","title":"Comment on egusphere-2023-821","year":2023,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"","keywords":"Convection; Diurnal cycle; Radar; Convection cell; Atmospheric sciences; Radiative transfer; Environmental science; Meteorology; Climatology; Geology; Geography; Physics; Optics; Computer science; Natural convection","score_opus":0.026519451065640357,"score_gpt":0.2787614837128978,"score_spread":0.2522420326472574,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4380265264","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000026869115,0.0017392719,0.00010614558,0.29057825,0.002603985,0.0006268358,0.000079378566,0.00022069445,0.7040186],"genre_scores_gemma":[0.000030923748,0.0050057084,0.0005593071,0.10925082,0.00020833308,0.00010748516,0.0002272621,0.0000691094,0.88454103],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9975294,0.000060311766,0.00038315012,0.00066549086,0.00089243177,0.00046923975],"domain_scores_gemma":[0.99879265,0.000090912305,0.00015889478,0.0007659824,0.0000078993,0.00018364076],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00031004022,0.0004198152,0.000537524,8.6919823e-7,0.00012686872,0.00003112813,0.0006385304,0.0002355387,0.20077589],"category_scores_gemma":[0.000043714306,0.00031787404,0.000242349,0.00033290332,0.0001199187,0.0000331788,0.000610077,0.000441745,0.07043006],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000020480795,0.00005557872,0.000073873634,0.00015504782,0.00002036663,0.000014800619,0.000007824531,0.00004074576,9.494928e-7,0.00008113628,0.98545045,0.014097202],"study_design_scores_gemma":[0.000102286685,0.00010589774,0.0002937824,0.0006566592,0.000049985865,0.0000014929335,0.000018477604,0.000047173722,0.000004760983,0.000115740564,0.9982078,0.00039595415],"about_ca_topic_score_codex":0.0030773457,"about_ca_topic_score_gemma":0.00083232415,"teacher_disagreement_score":0.18132743,"about_ca_system_score_codex":0.0003476254,"about_ca_system_score_gemma":0.00002149148,"threshold_uncertainty_score":0.99992734},"labels":[],"label_agreement":null},{"id":"W4380488018","doi":"10.5194/egusphere-2023-1193","title":"Sensitivity of cloud phase distribution to cloud microphysics and thermodynamics in simulated deep convective clouds and SEVIRI retrievals","year":2023,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"European Organization for the Exploitation of Meteorological Satellites; European Commission; Deutsches Klimarechenzentrum","keywords":"Cloud fraction; Liquid water content; Cloud computing; Radiative transfer; Convection; Cloud top; Atmospheric sciences; Cloud physics; Computational physics; Meteorology; Materials science; Environmental science; Cloud cover; Physics; Optics","score_opus":0.01249288242536293,"score_gpt":0.2640372175179503,"score_spread":0.25154433509258733,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4380488018","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":[0.9564594,0.000041291045,0.04154299,0.00017979165,0.00028606813,0.0008493792,0.00032060727,0.00006464952,0.0002558012],"genre_scores_gemma":[0.99884486,0.00014181455,0.00050267554,0.00009532302,0.00006459849,0.000008172083,0.00012916955,0.000040284707,0.00017307626],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9977705,0.00024972705,0.0004765909,0.0008348942,0.00030104243,0.00036726633],"domain_scores_gemma":[0.9988527,0.00026959405,0.0002438931,0.00041789812,0.000035276058,0.00018060462],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0007386706,0.0003882876,0.0006340718,0.000004206086,0.0000800644,0.000042045005,0.00014544374,0.00037121575,0.00006617837],"category_scores_gemma":[0.00014154674,0.00036913433,0.000082504426,0.000429715,0.00042556901,0.00006415907,0.0015880845,0.00046630696,0.000025658188],"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":[0.0038599726,0.0026911348,0.22763103,0.00092604477,0.0006550406,0.00040591724,0.015146251,0.37653756,0.29251522,0.0022632894,0.0011440912,0.07622445],"study_design_scores_gemma":[0.0027112341,0.00050467445,0.2682855,0.0002376515,0.00017266878,0.0000136021135,0.00128331,0.70802903,0.009441067,0.007730523,0.00018210478,0.0014085976],"about_ca_topic_score_codex":0.0039978577,"about_ca_topic_score_gemma":0.00080071995,"teacher_disagreement_score":0.3314915,"about_ca_system_score_codex":0.00037129474,"about_ca_system_score_gemma":0.000029801799,"threshold_uncertainty_score":0.9998761},"labels":[],"label_agreement":null},{"id":"W4381162058","doi":"10.5194/egusphere-2023-821-rc3","title":"Comment on egusphere-2023-821","year":2023,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"","keywords":"Convection; Diurnal cycle; Radar; Atmospheric sciences; Convection cell; Radiative transfer; Environmental science; Meteorology; Climatology; Geology; Geography; Physics; Optics; Computer science; Natural convection","score_opus":0.026519451065640357,"score_gpt":0.2787614837128978,"score_spread":0.2522420326472574,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4381162058","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000026869115,0.0017392719,0.00010614558,0.29057825,0.002603985,0.0006268358,0.000079378566,0.00022069445,0.7040186],"genre_scores_gemma":[0.000030923748,0.0050057084,0.0005593071,0.10925082,0.00020833308,0.00010748516,0.0002272621,0.0000691094,0.88454103],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9975294,0.000060311766,0.00038315012,0.00066549086,0.00089243177,0.00046923975],"domain_scores_gemma":[0.99879265,0.000090912305,0.00015889478,0.0007659824,0.0000078993,0.00018364076],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00031004022,0.0004198152,0.000537524,8.6919823e-7,0.00012686872,0.00003112813,0.0006385304,0.0002355387,0.20077589],"category_scores_gemma":[0.000043714306,0.00031787404,0.000242349,0.00033290332,0.0001199187,0.0000331788,0.000610077,0.000441745,0.07043006],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000020480795,0.00005557872,0.000073873634,0.00015504782,0.00002036663,0.000014800619,0.000007824531,0.00004074576,9.494928e-7,0.00008113628,0.98545045,0.014097202],"study_design_scores_gemma":[0.000102286685,0.00010589774,0.0002937824,0.0006566592,0.000049985865,0.0000014929335,0.000018477604,0.000047173722,0.000004760983,0.000115740564,0.9982078,0.00039595415],"about_ca_topic_score_codex":0.0030773457,"about_ca_topic_score_gemma":0.00083232415,"teacher_disagreement_score":0.18132743,"about_ca_system_score_codex":0.0003476254,"about_ca_system_score_gemma":0.00002149148,"threshold_uncertainty_score":0.99992734},"labels":[],"label_agreement":null},{"id":"W4381743298","doi":"10.22541/essoar.168748426.65924684/v1","title":"Fine and Coarse Dust Effects on Radiative Forcing, Mass Deposition, and Solar Devices over the Middle East","year":2023,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Kootenay Association for Science & Technology","funders":"King Abdullah University of Science and Technology","keywords":"Atmospheric sciences; Mineral dust; Environmental science; Deposition (geology); Shortwave; Radiative forcing; Aerosol; Air quality index; Mass concentration (chemistry); Forcing (mathematics); Radiative transfer; Meteorology; Physics; Geology","score_opus":0.019791978997862475,"score_gpt":0.22088327167224184,"score_spread":0.20109129267437936,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4381743298","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":[0.99091804,0.00021500749,0.003189134,0.00068044965,0.00020683545,0.0005743314,0.000014759408,0.00006720392,0.00413421],"genre_scores_gemma":[0.9953044,0.000090446156,0.0014066692,0.0006627255,0.00008758621,0.00007328398,0.000013134299,0.000028713526,0.002333039],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988081,0.000070359965,0.00015463453,0.0004959161,0.00024021664,0.00023081056],"domain_scores_gemma":[0.9993418,0.00016980161,0.00011369881,0.00026933503,0.000004713019,0.00010066218],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016814037,0.00025255245,0.0002109002,0.0000016184002,0.00025768785,0.00010952215,0.00017339893,0.00015675023,0.00036583887],"category_scores_gemma":[0.000024024303,0.00016123029,0.000047818357,0.000078682584,0.00020027821,0.000068607864,0.0006766396,0.0002983874,0.00010168691],"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":[0.00013108777,0.00015285544,0.9175792,0.0005998645,0.00032290595,0.000114290124,0.0073816255,0.011144417,0.0015394236,0.00074342045,0.021678798,0.03861215],"study_design_scores_gemma":[0.00057962246,0.00021072608,0.9602487,0.0002563744,0.000112330395,0.000007142207,0.0006633078,0.033844296,0.0009010006,0.0016923258,0.0009630089,0.0005211795],"about_ca_topic_score_codex":0.0014861407,"about_ca_topic_score_gemma":0.0016199575,"teacher_disagreement_score":0.042669524,"about_ca_system_score_codex":0.00006890132,"about_ca_system_score_gemma":0.000008988171,"threshold_uncertainty_score":0.65747803},"labels":[],"label_agreement":null},{"id":"W4381950191","doi":"10.22541/essoar.168771423.33231547/v1","title":"A Dissection of the Inter-model Spread of the Aerosol Direct Radiative Effect in CMIP6 Models","year":2023,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Radiative transfer; Aerosol; Anomaly (physics); Atmospheric radiative transfer codes; Environmental science; Atmospheric sciences; Shortwave; Climate model; Albedo (alchemy); Single-scattering albedo; Climatology; Meteorology; Physics; Climate change; Geology","score_opus":0.01693631404621325,"score_gpt":0.24174411911026356,"score_spread":0.2248078050640503,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4381950191","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":[0.9685985,0.000023989882,0.008058714,0.00018662986,0.00048036623,0.00095277396,0.000024783289,0.00003183327,0.0216424],"genre_scores_gemma":[0.9958696,0.000029462764,0.00023773305,0.000039000115,0.00001534039,0.00010801112,0.0000016558051,0.000025667137,0.0036735763],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99841195,0.00020998661,0.00038461926,0.00041767923,0.00037096557,0.00020479718],"domain_scores_gemma":[0.9987847,0.00013083043,0.00031361458,0.00073129544,0.000007616227,0.000031918575],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037491848,0.00023991261,0.0003851926,0.0000021736562,0.000054541233,0.000010622872,0.0007716149,0.0001881405,0.00014046373],"category_scores_gemma":[0.0000621445,0.00012308477,0.00030970888,0.00031263783,0.00031277564,0.00006264768,0.0021589103,0.0004208515,0.000011885679],"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":[0.00003369157,0.000068159155,0.06494581,0.00005861593,0.000029960338,3.294706e-7,0.0017132808,0.92889535,0.0026207266,0.00006429536,0.0005589734,0.0010107904],"study_design_scores_gemma":[0.00030097467,0.00007601713,0.08135456,0.0003512086,0.000053900094,5.8273923e-7,0.00018250913,0.88558924,0.02586926,0.005962042,0.0000040217574,0.00025570707],"about_ca_topic_score_codex":0.0064076823,"about_ca_topic_score_gemma":0.0030731917,"teacher_disagreement_score":0.043306153,"about_ca_system_score_codex":0.00022993902,"about_ca_system_score_gemma":0.000031507512,"threshold_uncertainty_score":0.96865416},"labels":[],"label_agreement":null},{"id":"W4382244151","doi":"10.1175/bams-d-22-0095.1","title":"P-Type Processes and Predictability: The Winter Precipitation Type Research Multiscale Experiment (WINTRE-MIX)","year":2023,"lang":"en","type":"article","venue":"Bulletin of the American Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"National Research Council Canada; Université du Québec à Montréal; Ontario Tech University; Environment and Climate Change Canada; McGill University","funders":"Fonds de recherche du Québec – Nature et technologies; Natural Sciences and Engineering Research Council of Canada; University at Albany; Environment and Climate Change Canada; National Aeronautics and Space Administration; Canada Research Chairs; McGill University; U.S. Department of Homeland Security; National Science Foundation","keywords":"Environmental science; Snow; Drizzle; Precipitation; Graupel; Meteorology; Mesoscale meteorology; Terrain; Predictability; Radiosonde; Precipitation types; Climatology; Atmospheric sciences; Geology; Geography","score_opus":0.03300861257530529,"score_gpt":0.3048853824288343,"score_spread":0.271876769853529,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4382244151","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":[0.9891575,0.00013144233,0.000031736487,0.009346055,0.000072079194,0.00035926737,0.0000026988057,0.00004654481,0.0008526826],"genre_scores_gemma":[0.9956702,0.00024236875,0.0018832522,0.0007985738,0.00004169366,0.000047852453,0.0000014215059,0.000010432064,0.0013042333],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9982624,0.00036466782,0.0001964923,0.00034580976,0.0005024109,0.0003282352],"domain_scores_gemma":[0.99876475,0.0006665643,0.00012421836,0.00033055453,0.000050787785,0.000063141844],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011037526,0.00011795261,0.00018827744,8.7238993e-7,0.00033600198,0.000021905777,0.00045211727,0.000052341875,0.0014231631],"category_scores_gemma":[0.0007644585,0.000057814224,0.00009219969,0.0008048627,0.0029214208,0.00001630498,0.0008718265,0.00024390768,0.00015820195],"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":[0.00055000157,0.00048624573,0.44616076,0.00006752785,0.000140368,0.0000020381397,0.011163715,0.0010980973,0.037841883,0.000075853815,0.47728223,0.025131289],"study_design_scores_gemma":[0.00031787532,0.0014328914,0.86344165,0.000018492101,0.000035145316,0.0000033158085,0.009872375,0.0009250219,0.0034995894,0.00093603134,0.11929227,0.00022537401],"about_ca_topic_score_codex":0.00040801283,"about_ca_topic_score_gemma":0.000009543522,"teacher_disagreement_score":0.41728085,"about_ca_system_score_codex":0.00005730495,"about_ca_system_score_gemma":0.000014995455,"threshold_uncertainty_score":0.99979204},"labels":[],"label_agreement":null},{"id":"W4382678754","doi":"10.5194/amt-2023-67-rc3","title":"Comment on amt-2023-67","year":2023,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"AERONET; Lidar; Environmental science; Arctic; Aerosol; Remote sensing; Satellite; Mineral dust; Meteorology; Geography; Geology; Physics; Oceanography","score_opus":0.028999854015114592,"score_gpt":0.2838758062322327,"score_spread":0.2548759522171181,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4382678754","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000027008291,0.0012795257,0.00009704689,0.3555096,0.0025010838,0.0005717032,0.00008109476,0.00019545492,0.6397375],"genre_scores_gemma":[0.000031602092,0.0054951455,0.00040288534,0.11779131,0.00018226095,0.00008870605,0.00022555528,0.00005257654,0.87573],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.997904,0.000046834266,0.00031697983,0.000559756,0.000778827,0.00039359884],"domain_scores_gemma":[0.9989969,0.00007289224,0.00012867348,0.00064353505,0.0000058180576,0.00015219337],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00028556702,0.00034320576,0.00043333796,9.694705e-7,0.00010979985,0.0000247703,0.0005463568,0.00018671088,0.10796221],"category_scores_gemma":[0.00003511599,0.0002559356,0.00019979708,0.00026328588,0.00010290307,0.000026719736,0.0005488561,0.0003738072,0.063978724],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000001363191,0.000043084932,0.00008334841,0.00012542271,0.000014548229,0.000011660657,0.000007083176,0.000025051457,8.315111e-7,0.00007886452,0.99015397,0.009454757],"study_design_scores_gemma":[0.0000780575,0.000087642286,0.00042300817,0.0005387954,0.00004002253,0.0000011422833,0.000011711769,0.000037984115,0.000004055424,0.00010123569,0.99835515,0.00032118542],"about_ca_topic_score_codex":0.0020264373,"about_ca_topic_score_gemma":0.00039039322,"teacher_disagreement_score":0.23771828,"about_ca_system_score_codex":0.00028463136,"about_ca_system_score_gemma":0.0000146637085,"threshold_uncertainty_score":0.9999893},"labels":[],"label_agreement":null},{"id":"W4383370732","doi":"10.5194/ems2023-345","title":"Ice nucleation by anthropogenic aerosols downwind of industrial point sources of air pollution","year":2023,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"","keywords":"Aerosol; Ice nucleus; Environmental science; Glacial period; Atmospheric sciences; Snow; Precipitation; Climatology; Geology; Meteorology; Geography","score_opus":0.023752637521117167,"score_gpt":0.24462636497103235,"score_spread":0.22087372744991518,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4383370732","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":[0.9926762,0.000050224688,0.0025538723,0.0006667718,0.00041711165,0.0004627325,0.00011629648,0.000077056684,0.0029797168],"genre_scores_gemma":[0.9969423,0.00009054278,0.0008668567,0.00007234988,0.00009068351,0.000013955957,0.00005385051,0.000032825348,0.0018366671],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979953,0.00007736552,0.0006273177,0.0004907194,0.00055543444,0.00025384058],"domain_scores_gemma":[0.9988191,0.00003718626,0.0005941453,0.00045002508,0.0000163246,0.00008317633],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003188744,0.00025162127,0.00041581944,0.000003659935,0.00007797574,0.000013452001,0.00039608974,0.0004799674,0.0047392566],"category_scores_gemma":[0.000049024493,0.00022350268,0.0001949449,0.00025619945,0.00048250036,0.00009581016,0.0009769769,0.00032155038,0.00016829396],"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":[0.0005373081,0.0014328868,0.38535517,0.0003061792,0.00057187735,0.00000886417,0.0045975926,0.18991223,0.1533789,0.00054992567,0.22929837,0.034050684],"study_design_scores_gemma":[0.0072751218,0.0024463888,0.48028523,0.0012745337,0.0010190443,0.000019362233,0.012803541,0.011997508,0.45555687,0.007244558,0.015478129,0.0045997393],"about_ca_topic_score_codex":0.007427993,"about_ca_topic_score_gemma":0.00012672879,"teacher_disagreement_score":0.30217797,"about_ca_system_score_codex":0.0001663595,"about_ca_system_score_gemma":0.00004021724,"threshold_uncertainty_score":0.9991816},"labels":[],"label_agreement":null},{"id":"W4383682228","doi":"10.5194/egusphere-2023-1193-rc1","title":"Comment on egusphere-2023-1193","year":2023,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"European Organization for the Exploitation of Meteorological Satellites; European Commission; Deutsches Klimarechenzentrum","keywords":"Cloud fraction; Liquid water content; Radiative transfer; Cloud computing; Convection; Cloud top; Cloud physics; Atmospheric sciences; Phase (matter); Materials science; Chemistry; Thermodynamics; Physics; Cloud cover; Optics","score_opus":0.026337537673866398,"score_gpt":0.2784345015012307,"score_spread":0.25209696382736435,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4383682228","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000028532007,0.0016623619,0.00010620606,0.29608738,0.0026274547,0.0006400504,0.00008161757,0.00023384717,0.6985325],"genre_scores_gemma":[0.00003318817,0.0048411065,0.00054901105,0.109825,0.00021232251,0.00011119197,0.0002276309,0.00007125738,0.8841293],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9974261,0.000060057162,0.0003907254,0.00067687745,0.00096645666,0.00047976876],"domain_scores_gemma":[0.9987725,0.000090496746,0.00016228113,0.0007784461,0.000008485432,0.00018777033],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00032225292,0.00042962225,0.00054604013,9.1566767e-7,0.0001301516,0.00003141038,0.0006571344,0.00024047139,0.19429018],"category_scores_gemma":[0.000044929453,0.00032533615,0.00024608048,0.00033953344,0.00012423714,0.000034050543,0.00061948784,0.0004462599,0.070876844],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000021441908,0.000056584486,0.000078367026,0.00015999014,0.000020807458,0.000014836316,0.000007867695,0.000041810596,9.432891e-7,0.000085502215,0.98662835,0.012902783],"study_design_scores_gemma":[0.000104358325,0.00010866547,0.00031485764,0.000666955,0.00005131479,0.0000015182085,0.000017752936,0.000048613034,0.0000046883324,0.00012720039,0.9981491,0.00040496094],"about_ca_topic_score_codex":0.0031593272,"about_ca_topic_score_gemma":0.0008496995,"teacher_disagreement_score":0.18626238,"about_ca_system_score_codex":0.00035555213,"about_ca_system_score_gemma":0.000021911124,"threshold_uncertainty_score":0.9999199},"labels":[],"label_agreement":null},{"id":"W4384339067","doi":"10.1007/s11869-023-01391-4","title":"Validation of MODIS AOD retrievals in West Africa: a comparison with AERONET observations","year":2023,"lang":"en","type":"article","venue":"Air Quality Atmosphere & Health","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":11,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"AERONET; Environmental science; Satellite; Aerosol; Remote sensing; Climatology; Mineral dust; Meteorology; Cloud cover; Range (aeronautics); Geography; Cloud computing; Geology; Computer science","score_opus":0.0765926829715342,"score_gpt":0.3248144540222336,"score_spread":0.24822177105069937,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4384339067","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":[0.99127465,0.0000738034,0.0013456467,0.0034486223,0.00005092387,0.0005035321,0.000024747958,0.00012218591,0.0031558916],"genre_scores_gemma":[0.9923038,0.000056059984,0.0063605933,0.0003644565,0.000019601282,0.000041993426,0.00006040058,0.000024500145,0.0007686091],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99722445,0.00034027983,0.0008504889,0.0004393966,0.00063745095,0.0005079332],"domain_scores_gemma":[0.99868035,0.00018279966,0.00047197362,0.00047123016,0.000021715121,0.00017189875],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013692835,0.00019506356,0.00048896216,0.0000010585173,0.000179428,0.000014188876,0.00025902636,0.00010314052,0.0007947761],"category_scores_gemma":[0.000082221435,0.00017439459,0.00004873251,0.001791266,0.00019078437,0.00020398803,0.00012525145,0.00020782714,0.00020652381],"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":[0.00008412333,0.00033473462,0.9037323,0.00010231349,0.000014415669,0.0000022130441,0.004885999,0.07975593,0.00032088603,0.001191654,0.005890159,0.003685283],"study_design_scores_gemma":[0.0005968657,0.00039802628,0.9883117,0.00006008224,0.000007269189,7.3423763e-7,0.0024577202,0.00432454,0.00018188274,0.00043307405,0.0030124276,0.00021565818],"about_ca_topic_score_codex":0.012482624,"about_ca_topic_score_gemma":0.00437461,"teacher_disagreement_score":0.08457943,"about_ca_system_score_codex":0.0003724558,"about_ca_system_score_gemma":0.00012437886,"threshold_uncertainty_score":0.99409336},"labels":[],"label_agreement":null},{"id":"W4384701489","doi":"10.1029/2023ms003674","title":"A Functionalized Monte Carlo 3D Radiative Transfer Model: Radiative Effects of Clouds Over Reflecting Surfaces","year":2023,"lang":"en","type":"article","venue":"Journal of Advances in Modeling Earth Systems","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":12,"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":"Radiative transfer; Albedo (alchemy); Monte Carlo method; Computational physics; Atmospheric radiative transfer codes; Zenith; Physics; Atmosphere (unit); Solar zenith angle; Surface (topology); Optics; Atmospheric sciences; Meteorology; Geometry; Mathematics","score_opus":0.016212592358491876,"score_gpt":0.280393983956093,"score_spread":0.2641813915976011,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4384701489","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":[0.8977317,0.0053728903,0.09544208,0.000015952299,0.0006954501,0.00024572873,0.000004830695,0.00002138604,0.00046993533],"genre_scores_gemma":[0.9958822,0.0016010848,0.0021013923,0.000020802861,0.000105793966,0.000011364552,5.292815e-7,0.000025926012,0.00025088005],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9977138,0.000187012,0.0008488479,0.00023788663,0.00069392024,0.00031852614],"domain_scores_gemma":[0.999074,0.0002770533,0.00036459503,0.00013012337,0.000055931512,0.00009828937],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00085484766,0.00020132489,0.00056807604,0.0000205648,0.00009178786,0.000021827058,0.00020289734,0.00009181262,0.000030488916],"category_scores_gemma":[0.00010295382,0.00016362613,0.00015887416,0.00057899056,0.000080355814,0.00067137636,0.00003896277,0.00030330406,0.000006810946],"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":[0.00014651599,0.00003670888,0.008234425,0.000088068504,0.00003679938,0.000017190112,0.002716505,0.9861581,0.0016542602,0.000025911077,0.00002237162,0.0008631825],"study_design_scores_gemma":[0.001122367,0.00021875172,0.0011163723,0.00032283392,0.000026982918,0.0000097345655,0.00074153295,0.9957442,0.00015230052,0.0001891195,0.00019185622,0.00016393934],"about_ca_topic_score_codex":0.00023590807,"about_ca_topic_score_gemma":0.00007317411,"teacher_disagreement_score":0.09815048,"about_ca_system_score_codex":0.00014448648,"about_ca_system_score_gemma":0.00004785103,"threshold_uncertainty_score":0.667248},"labels":[],"label_agreement":null},{"id":"W4385274353","doi":"10.5194/egusphere-2023-1193-rc2","title":"Comment on egusphere-2023-1193","year":2023,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"European Organization for the Exploitation of Meteorological Satellites; European Commission; Deutsches Klimarechenzentrum","keywords":"Cloud fraction; Cloud computing; Radiative transfer; Liquid water content; Convection; Cloud physics; Cloud top; Phase (matter); Atmospheric sciences; Materials science; Chemistry; Thermodynamics; Physics; Cloud cover; Optics","score_opus":0.026337537673866398,"score_gpt":0.2784345015012307,"score_spread":0.25209696382736435,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385274353","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000028532007,0.0016623619,0.00010620606,0.29608738,0.0026274547,0.0006400504,0.00008161757,0.00023384717,0.6985325],"genre_scores_gemma":[0.00003318817,0.0048411065,0.00054901105,0.109825,0.00021232251,0.00011119197,0.0002276309,0.00007125738,0.8841293],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9974261,0.000060057162,0.0003907254,0.00067687745,0.00096645666,0.00047976876],"domain_scores_gemma":[0.9987725,0.000090496746,0.00016228113,0.0007784461,0.000008485432,0.00018777033],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00032225292,0.00042962225,0.00054604013,9.1566767e-7,0.0001301516,0.00003141038,0.0006571344,0.00024047139,0.19429018],"category_scores_gemma":[0.000044929453,0.00032533615,0.00024608048,0.00033953344,0.00012423714,0.000034050543,0.00061948784,0.0004462599,0.070876844],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000021441908,0.000056584486,0.000078367026,0.00015999014,0.000020807458,0.000014836316,0.000007867695,0.000041810596,9.432891e-7,0.000085502215,0.98662835,0.012902783],"study_design_scores_gemma":[0.000104358325,0.00010866547,0.00031485764,0.000666955,0.00005131479,0.0000015182085,0.000017752936,0.000048613034,0.0000046883324,0.00012720039,0.9981491,0.00040496094],"about_ca_topic_score_codex":0.0031593272,"about_ca_topic_score_gemma":0.0008496995,"teacher_disagreement_score":0.18626238,"about_ca_system_score_codex":0.00035555213,"about_ca_system_score_gemma":0.000021911124,"threshold_uncertainty_score":0.9999199},"labels":[],"label_agreement":null},{"id":"W4385305098","doi":"10.22323/1.444.1496","title":"Exploring the Potential of the Pulsed Laser onboard the CALIPSO Satellite to Improve Calibration with VERITAS","year":2023,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Arthur B. McDonald-Canadian Astroparticle Physics Research Institute; Queen's University; McGill University","funders":"","keywords":"Calibration; Satellite; Remote sensing; Lidar; Atmosphere (unit); Cherenkov radiation; Laser; Physics; Nanosecond; Environmental science; Optics; Detector; Astronomy; Meteorology; Geology","score_opus":0.018117806562571948,"score_gpt":0.1988453688042118,"score_spread":0.18072756224163986,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385305098","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":[0.991522,0.0000031561372,0.0008491469,0.0041200644,0.00019431727,0.00031250407,0.0000031119907,0.000032961816,0.0029627208],"genre_scores_gemma":[0.99584645,0.000012515613,0.00017605007,0.0005525646,0.000047855363,0.000054466196,9.1697393e-7,0.000011438412,0.0032977236],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9990758,0.000045521578,0.00012202989,0.00016513349,0.00040429502,0.00018726214],"domain_scores_gemma":[0.9995253,0.000032740998,0.00003907381,0.0003583322,0.0000061510805,0.00003836891],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020403482,0.00008770202,0.00006673444,5.825817e-7,0.00022696971,0.00003294972,0.00031604883,0.000017828104,0.00037666273],"category_scores_gemma":[0.00001294813,0.000032490447,0.000047309717,0.00038670065,0.00015261282,0.0001312615,0.00023982617,0.000079279955,0.00013429717],"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":[0.00048188196,0.00019654646,0.071611,0.000032591335,0.0001713618,0.000021006543,0.012698785,0.42629984,0.3365324,0.0016921778,0.021337204,0.12892519],"study_design_scores_gemma":[0.0005673406,0.00031523182,0.81813437,0.00002262395,0.00007567072,0.0000050530844,0.008459281,0.03104001,0.11950126,0.00037224026,0.021117557,0.0003893876],"about_ca_topic_score_codex":0.00091781776,"about_ca_topic_score_gemma":0.00048851536,"teacher_disagreement_score":0.7465233,"about_ca_system_score_codex":0.000036791887,"about_ca_system_score_gemma":0.000010070293,"threshold_uncertainty_score":0.4124193},"labels":[],"label_agreement":null},{"id":"W4385579665","doi":"10.5194/egusphere-2023-1682","title":"An intercomparison of EarthCARE cloud, aerosol and precipitation retrieval products","year":2023,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; Environment and Climate Change Canada","funders":"Natural Environment Research Council; Sight Research UK; European Space Agency","keywords":"Remote sensing; Environmental science; Meteorology; Cloud computing; Aerosol; Radiative transfer; Radiometer; Computer science; Radar; Context (archaeology); Earth's energy budget; Geology; Geography; Radiation","score_opus":0.029267402949982365,"score_gpt":0.27659482768402405,"score_spread":0.24732742473404168,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385579665","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":[0.9961931,0.00005172833,0.0010068738,0.00028357885,0.0005764233,0.00047577702,0.0000182821,0.00011292533,0.0012813013],"genre_scores_gemma":[0.98974985,0.00006402361,0.0070751845,0.000024262414,0.00010878493,0.000012916222,0.000060294722,0.000030704818,0.0028740016],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99837023,0.000075769625,0.00034256236,0.000664954,0.0003467901,0.00019968522],"domain_scores_gemma":[0.9991189,0.00002651302,0.00019774784,0.000532401,0.000027439411,0.00009696607],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026204615,0.00021353793,0.00029634128,0.000002234395,0.000052349245,0.000043499153,0.00028598303,0.00021263277,0.00056509377],"category_scores_gemma":[0.00005962517,0.00018951597,0.000047015623,0.00016644175,0.0002049022,0.00011183954,0.0008489387,0.00029402447,0.00013589644],"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":[0.0005369165,0.0006862218,0.7842719,0.001002364,0.00016905794,0.000015930971,0.01669133,0.017330972,0.123994574,0.00028064547,0.026055578,0.02896452],"study_design_scores_gemma":[0.0010174263,0.0016215119,0.84261036,0.0004609347,0.000190409,0.000009833452,0.005392463,0.02786623,0.11465025,0.0027903744,0.0014710744,0.0019191283],"about_ca_topic_score_codex":0.00094749464,"about_ca_topic_score_gemma":0.00030436978,"teacher_disagreement_score":0.058338482,"about_ca_system_score_codex":0.00006012386,"about_ca_system_score_gemma":0.000020347901,"threshold_uncertainty_score":0.7728237},"labels":[],"label_agreement":null},{"id":"W4385896284","doi":"10.5194/egusphere-2023-1682-rc1","title":"Comment on egusphere-2023-1682","year":2023,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University; Environment and Climate Change Canada","funders":"","keywords":"Remote sensing; Environmental science; Meteorology; Computer science; Radiometer; Cloud computing; Radar; Radiative transfer; Context (archaeology); Multispectral image; Geography; Physics","score_opus":0.026457212958070846,"score_gpt":0.2787271751557607,"score_spread":0.2522699621976898,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385896284","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000027067419,0.0017267098,0.00010501879,0.29086322,0.0026555501,0.00064531167,0.00008257843,0.00023596166,0.7036586],"genre_scores_gemma":[0.00003257465,0.0050197556,0.00055057957,0.1098678,0.00021319608,0.00011079574,0.00023127504,0.00007137186,0.88390267],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9974825,0.000059347574,0.0003915798,0.000677252,0.00090939604,0.00047992778],"domain_scores_gemma":[0.99877363,0.00008894245,0.00016299274,0.0007785804,0.000008009037,0.00018782065],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000313362,0.00042972743,0.0005465807,9.150679e-7,0.00013008605,0.00003153016,0.00065746036,0.00024046222,0.19892938],"category_scores_gemma":[0.00004307624,0.00032539832,0.0002466673,0.00033931131,0.00012335043,0.000034030327,0.0006194273,0.0004522879,0.07334173],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000021601968,0.00005656226,0.00007187601,0.00015814525,0.000020795898,0.000015094454,0.000007945942,0.00004139419,9.698298e-7,0.000083782914,0.9863808,0.01316044],"study_design_scores_gemma":[0.00010545692,0.00010941074,0.00030359716,0.00065668696,0.000051323997,0.0000015454193,0.000017944123,0.000048565824,0.0000048379457,0.00012349706,0.99817204,0.00040507223],"about_ca_topic_score_codex":0.0031254685,"about_ca_topic_score_gemma":0.00083027355,"teacher_disagreement_score":0.18099543,"about_ca_system_score_codex":0.0003531001,"about_ca_system_score_gemma":0.000021729762,"threshold_uncertainty_score":0.99991983},"labels":[],"label_agreement":null},{"id":"W4386282781","doi":"10.1175/mwr-d-22-0294.1","title":"Identifying Important Microphysical Properties and Processes for Marine Fog Forecasts","year":2023,"lang":"en","type":"article","venue":"Monthly Weather Review","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"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":"Office of Naval Research","keywords":"Drizzle; Environmental science; Visibility; Aerosol; Meteorology; Atmospheric sciences; Precipitation; Geology; Geography","score_opus":0.04050069113413245,"score_gpt":0.2546338982823648,"score_spread":0.21413320714823236,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386282781","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":[0.9146691,0.07859776,0.00013771035,0.0017306027,0.00009328248,0.001892579,0.000015163419,0.00017022788,0.0026935886],"genre_scores_gemma":[0.8390015,0.12952183,0.007119561,0.0027181092,0.00025124257,0.002017114,0.00005148872,0.000185274,0.019133927],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99908185,0.000012583247,0.00023634595,0.00029198176,0.00012728486,0.00024995624],"domain_scores_gemma":[0.9996606,0.00001879909,0.00007979351,0.00016577044,0.000009855817,0.00006516572],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018179997,0.00014648034,0.00025135727,0.0000010503342,0.00011448635,0.000031068746,0.00013302703,0.000027379656,0.00023141575],"category_scores_gemma":[0.000053658157,0.00009967649,0.000066311455,0.0002500642,0.000086860186,0.00010966624,0.00017077991,0.00004612237,0.00011815303],"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":[0.00007229472,0.00026465877,0.14804687,0.01806783,0.00011392801,0.0000445934,0.0016451546,0.000054673274,0.012680135,0.00013841587,0.045778543,0.7730929],"study_design_scores_gemma":[0.0013552083,0.0006349856,0.10398521,0.006903035,0.00048544694,0.000035457833,0.0003758668,0.003523654,0.0043286155,0.0059379493,0.87066925,0.0017653242],"about_ca_topic_score_codex":0.00006728215,"about_ca_topic_score_gemma":0.00006724859,"teacher_disagreement_score":0.82489073,"about_ca_system_score_codex":0.000025083527,"about_ca_system_score_gemma":0.000009249921,"threshold_uncertainty_score":0.4064689},"labels":[],"label_agreement":null},{"id":"W4386393879","doi":"10.5281/zenodo.8310097","title":"OPS particle size distribution, AERONET and Lidar aerosol optical depth data employed in amt-2023-67","year":2023,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"Université de Sherbrooke","funders":"","keywords":"AERONET; Aerosol; Lidar; Environmental science; Particle-size distribution; Remote sensing; Atmospheric sciences; Particle (ecology); Distribution (mathematics); Particle size; Meteorology; Geography; Geology; Mathematics","score_opus":0.038356925723697664,"score_gpt":0.2547874165110723,"score_spread":0.2164304907873746,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386393879","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":[0.98100734,0.000026569736,0.0012369684,0.001187871,0.000044998087,0.0003206632,0.00027510544,0.00046557572,0.015434903],"genre_scores_gemma":[0.9967696,0.00008403807,0.00027528687,0.00008907685,0.000042192925,9.706641e-8,0.0014717069,0.00032306163,0.0009449252],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9982839,0.00015500409,0.00023008804,0.0005271298,0.00035381707,0.00045003986],"domain_scores_gemma":[0.9990939,0.00004602867,0.000046574474,0.0005701631,0.000028861306,0.00021447122],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0006398998,0.00012372875,0.0001247176,0.0000031640088,0.0008402044,0.00032541252,0.00087329146,0.000056967372,0.009150944],"category_scores_gemma":[0.0007245082,0.00012440546,0.000017193304,0.0007922925,0.00031301184,0.00032384705,0.003422473,0.00018818559,0.0132682305],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022740984,0.00057904277,0.015978023,0.00006383131,0.000053931682,0.00016603521,0.002009144,0.0008451524,0.028307024,0.0020878175,0.7878388,0.16184378],"study_design_scores_gemma":[0.0010881666,0.00027310126,0.3619389,0.000023539642,0.000017361777,0.0000537727,0.0006868987,0.007989761,0.0007071908,0.00015881409,0.62668324,0.00037924544],"about_ca_topic_score_codex":0.000085528394,"about_ca_topic_score_gemma":0.000013646971,"teacher_disagreement_score":0.3459609,"about_ca_system_score_codex":0.00011852348,"about_ca_system_score_gemma":0.0000022884437,"threshold_uncertainty_score":0.99175483},"labels":[],"label_agreement":null},{"id":"W4386690331","doi":"10.5194/amt-16-4115-2023","title":"Detection and analysis of Lhù'ààn Mân' (Kluane Lake) dust plumes using passive and active ground-based remote sensing supported by physical surface measurements","year":2023,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université de Montréal; Université de Sherbrooke","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Foundation for Innovation","keywords":"AERONET; Environmental science; Lidar; Arctic; Remote sensing; Aerosol; Snow; Satellite; Meteorology; Geology; Geography; Physics; Oceanography","score_opus":0.029037033815210448,"score_gpt":0.25606503260639185,"score_spread":0.2270279987911814,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386690331","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":[0.9263623,0.000051602896,0.07246497,0.00006416977,0.00003985384,0.00050369924,0.000013959841,0.0002933617,0.00020610314],"genre_scores_gemma":[0.97660434,0.00005158224,0.023133274,0.00007507435,0.000018170364,0.000004866125,0.000017941127,0.000041777286,0.000052968735],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9970522,0.00019173355,0.00041927415,0.0006809874,0.0012065028,0.0004493107],"domain_scores_gemma":[0.9989453,0.00005622561,0.0003750453,0.00035515585,0.00010737235,0.00016088183],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00072843174,0.0003687967,0.000583472,0.000004644971,0.00027247588,0.00005147098,0.00014116113,0.00014872316,0.00010224219],"category_scores_gemma":[0.000080656995,0.00034986393,0.00013917043,0.0017543023,0.0003388056,0.00022160339,0.00015077078,0.00017763473,0.0000037464326],"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":[0.00008539621,0.00008702148,0.02988123,0.00003207382,0.00047988206,0.000007630586,0.00037556078,0.0011112983,0.8408421,6.3837115e-7,0.00019792341,0.12689923],"study_design_scores_gemma":[0.0005824093,0.00035019213,0.13599677,0.00009653259,0.0014544366,0.000004955999,0.00050283776,0.48189768,0.3777696,0.00012416816,0.00052610313,0.000694305],"about_ca_topic_score_codex":0.002922269,"about_ca_topic_score_gemma":0.0007808609,"teacher_disagreement_score":0.48078638,"about_ca_system_score_codex":0.00039394118,"about_ca_system_score_gemma":0.000033950473,"threshold_uncertainty_score":0.99989533},"labels":[],"label_agreement":null},{"id":"W4386827284","doi":"10.5194/egusphere-2023-1682-rc2","title":"Comment on egusphere-2023-1682","year":2023,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University; Environment and Climate Change Canada","funders":"","keywords":"Remote sensing; Environmental science; Meteorology; Radiometer; Computer science; Cloud computing; Radar; Radiative transfer; Context (archaeology); Multispectral image; Geography; Physics","score_opus":0.026457212958070846,"score_gpt":0.2787271751557607,"score_spread":0.2522699621976898,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386827284","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000027067419,0.0017267098,0.00010501879,0.29086322,0.0026555501,0.00064531167,0.00008257843,0.00023596166,0.7036586],"genre_scores_gemma":[0.00003257465,0.0050197556,0.00055057957,0.1098678,0.00021319608,0.00011079574,0.00023127504,0.00007137186,0.88390267],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9974825,0.000059347574,0.0003915798,0.000677252,0.00090939604,0.00047992778],"domain_scores_gemma":[0.99877363,0.00008894245,0.00016299274,0.0007785804,0.000008009037,0.00018782065],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000313362,0.00042972743,0.0005465807,9.150679e-7,0.00013008605,0.00003153016,0.00065746036,0.00024046222,0.19892938],"category_scores_gemma":[0.00004307624,0.00032539832,0.0002466673,0.00033931131,0.00012335043,0.000034030327,0.0006194273,0.0004522879,0.07334173],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000021601968,0.00005656226,0.00007187601,0.00015814525,0.000020795898,0.000015094454,0.000007945942,0.00004139419,9.698298e-7,0.000083782914,0.9863808,0.01316044],"study_design_scores_gemma":[0.00010545692,0.00010941074,0.00030359716,0.00065668696,0.000051323997,0.0000015454193,0.000017944123,0.000048565824,0.0000048379457,0.00012349706,0.99817204,0.00040507223],"about_ca_topic_score_codex":0.0031254685,"about_ca_topic_score_gemma":0.00083027355,"teacher_disagreement_score":0.18099543,"about_ca_system_score_codex":0.0003531001,"about_ca_system_score_gemma":0.000021729762,"threshold_uncertainty_score":0.99991983},"labels":[],"label_agreement":null},{"id":"W4387431356","doi":"10.5194/amt-16-2319-2023","title":"Across-track extension of retrieved cloud and aerosol properties for the EarthCARE mission: the ACMB-3D product","year":2023,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Environment and Climate Change Canada; European Space Agency","keywords":"Nadir; Radiance; Remote sensing; Environmental science; Radiative transfer; Radiometer; Pixel; Track (disk drive); Cloud top; Atmospheric radiative transfer codes; Satellite; Aerosol; Meteorology; Computer science; Cloud computing; Geology; Geography; Physics; Optics; Artificial intelligence","score_opus":0.056362662290605235,"score_gpt":0.27076639679617126,"score_spread":0.21440373450556602,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387431356","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":[0.9826167,0.0026913376,0.0048512593,0.0046631005,0.00033253836,0.0036601357,0.0000068398613,0.0005989994,0.0005790953],"genre_scores_gemma":[0.98909074,0.00061379006,0.00841343,0.00029471214,0.00012736995,0.00027698,0.0000015990215,0.00004071236,0.0011406435],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9975323,0.000093016846,0.0004028623,0.0005053272,0.0010207826,0.00044570147],"domain_scores_gemma":[0.99872947,0.00008371608,0.00020658813,0.00078257156,0.00012529542,0.00007233286],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020342227,0.0002598309,0.0002602386,2.5726337e-7,0.00067307823,0.000060634615,0.00049199734,0.00009477505,0.000114272145],"category_scores_gemma":[0.00039387666,0.00013121092,0.000104929495,0.0005375085,0.0005708197,0.00012834524,0.00037500853,0.0001741588,0.000015096129],"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":[0.0003421571,0.00014727526,0.025412472,0.00017739466,0.00010292003,0.00000444014,0.0035099965,0.00031737928,0.57425976,0.000050892286,0.05982749,0.33584785],"study_design_scores_gemma":[0.0008061552,0.0011134943,0.11001369,0.00044464547,0.00017397976,0.000025813011,0.004705804,0.008231163,0.7119063,0.0005948069,0.16100705,0.0009771108],"about_ca_topic_score_codex":0.00017363687,"about_ca_topic_score_gemma":0.000035883146,"teacher_disagreement_score":0.33487076,"about_ca_system_score_codex":0.00007823975,"about_ca_system_score_gemma":0.000031186082,"threshold_uncertainty_score":0.5350626},"labels":[],"label_agreement":null},{"id":"W4387438410","doi":"10.5194/acp-23-5023-2023","title":"Parameterization of size of organic and secondary inorganic aerosol for efficient representation of global aerosol optical properties","year":2023,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":11,"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","funders":"National Aeronautics and Space Administration; National Science Foundation","keywords":"Aerosol; AERONET; Ammonium sulfate; Atmospheric sciences; Environmental science; Sulfate; Chemical transport model; RADIUS; Meteorology; Chemistry; Physics","score_opus":0.009206062544204481,"score_gpt":0.21947878324092507,"score_spread":0.2102727206967206,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387438410","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":[0.9968311,0.000050912484,0.002458129,0.000021819174,0.000019894496,0.00019143609,0.00001647027,0.000016994913,0.00039322322],"genre_scores_gemma":[0.99494207,0.00004593747,0.0047395066,0.000009145809,0.000019152993,0.000013108861,0.000008730454,0.0000108357945,0.000211505],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9991971,0.000011423168,0.00026923127,0.00022958372,0.00015568073,0.00013695566],"domain_scores_gemma":[0.9995293,0.00007620202,0.00015850404,0.0001627897,0.000024356594,0.000048826638],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000061281404,0.00011728064,0.00023553953,1.6440618e-8,0.000046809284,0.000007196087,0.00007839567,0.00006741169,0.0001944729],"category_scores_gemma":[0.000060980423,0.00010668544,0.000045406967,0.00036110837,0.00034350096,0.000054368786,0.000110332745,0.000042831314,0.0000017730556],"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":[0.0000680235,0.00009395794,0.022230454,0.0003352147,0.000025876336,2.8403227e-7,0.00035422063,0.0022261064,0.9611709,0.000021381526,0.000039282393,0.013434262],"study_design_scores_gemma":[0.00069887907,0.00014671094,0.034548994,0.00004557163,0.00006374093,0.0000037321865,0.0004770922,0.031183766,0.9322957,0.00034720436,0.000007764058,0.00018084345],"about_ca_topic_score_codex":0.00003902785,"about_ca_topic_score_gemma":0.0000012950877,"teacher_disagreement_score":0.028957661,"about_ca_system_score_codex":0.000027471116,"about_ca_system_score_gemma":0.000025846137,"threshold_uncertainty_score":0.43505058},"labels":[],"label_agreement":null},{"id":"W4387875154","doi":"10.5194/amt-2023-210","title":"Derivation of aerosol fluorescence and water vapor Raman depolarization ratios from lidar measurements","year":2023,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"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":"European Regional Development Fund; Russian Science Foundation; Agence Nationale de la Recherche","keywords":"Depolarization ratio; Lidar; Fluorescence; Wavelength; Laser-induced fluorescence; Aerosol; Raman spectroscopy; Plume; Ceilometer; Materials science; Environmental science; Optics; Analytical Chemistry (journal); Atmospheric sciences; Chemistry; Physics; Meteorology","score_opus":0.03426404526920099,"score_gpt":0.23500718894494457,"score_spread":0.20074314367574358,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387875154","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":[0.9669555,0.000020010086,0.031167565,0.0001930436,0.00026686286,0.00047883997,0.000014304324,0.000084045314,0.0008198327],"genre_scores_gemma":[0.985024,0.000043651668,0.014001022,0.00007744495,0.00004573665,0.00003740938,0.0001970254,0.000030249665,0.00054347963],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99829155,0.000055431705,0.00040091277,0.00052891846,0.00051184493,0.00021132955],"domain_scores_gemma":[0.99934894,0.00001862895,0.00017101206,0.0003641078,0.000020895928,0.000076418604],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00018938481,0.00022295049,0.00024057603,0.0000024280191,0.00009754532,0.000061053404,0.00023588199,0.00022393692,0.0010522844],"category_scores_gemma":[0.00002941823,0.00017111764,0.000050177467,0.00007743483,0.00012438494,0.00013211308,0.0008897506,0.00016846128,0.00014926861],"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":[0.000019839512,0.000058101632,0.4311128,0.00004302071,0.00004511048,0.000001877792,0.00088831905,0.002065948,0.56119,0.000007637069,0.00036143014,0.0042058793],"study_design_scores_gemma":[0.0004984313,0.00006541129,0.39121145,0.00011577896,0.000092419155,7.046169e-7,0.00015719139,0.008587841,0.5970176,0.0016406215,0.00005631192,0.0005562911],"about_ca_topic_score_codex":0.0043490855,"about_ca_topic_score_gemma":0.0003976018,"teacher_disagreement_score":0.039901365,"about_ca_system_score_codex":0.00008227777,"about_ca_system_score_gemma":0.000014030382,"threshold_uncertainty_score":0.9998609},"labels":[],"label_agreement":null},{"id":"W4387906724","doi":"10.5194/gmd-2023-86-rc2","title":"Comment on gmd-2023-86","year":2023,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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","funders":"","keywords":"Scavenging; Precipitation; Aerosol; Liquid water content; Ammonium sulfate; Chemistry; Particulates; Atmospheric sciences; Meteorology; Cloud computing; Physics","score_opus":0.029185626454761183,"score_gpt":0.28417957751832656,"score_spread":0.25499395106356537,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387906724","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000025710153,0.0013309129,0.00009233632,0.35730204,0.0024955326,0.00055961206,0.00007958759,0.00018968881,0.6379246],"genre_scores_gemma":[0.000030868778,0.0055182376,0.0003941818,0.12062771,0.00018347203,0.00008095713,0.00021759572,0.00005246516,0.8728945],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9978638,0.000046994755,0.0003185775,0.0005611853,0.00081456226,0.00039485644],"domain_scores_gemma":[0.9989907,0.00007793502,0.00012765895,0.0006453471,0.0000058352707,0.0001525033],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00030488096,0.00034401947,0.00044979225,9.729459e-7,0.00010946813,0.00002472256,0.000543922,0.00018987722,0.10899769],"category_scores_gemma":[0.000037936203,0.00025647372,0.00020041135,0.00027761253,0.00010005679,0.00002679564,0.00054844626,0.0003746448,0.06088639],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000001369183,0.000043692107,0.00007037158,0.00012845418,0.000014601297,0.000011826376,0.0000070510705,0.000025952077,8.234673e-7,0.000076916236,0.9901477,0.009471227],"study_design_scores_gemma":[0.00007959699,0.000089005225,0.00034811787,0.0005413803,0.00004036418,0.0000011927685,0.000011689126,0.00004100478,0.000004167421,0.000102854734,0.99841887,0.00032177847],"about_ca_topic_score_codex":0.0018890154,"about_ca_topic_score_gemma":0.00034751973,"teacher_disagreement_score":0.23667432,"about_ca_system_score_codex":0.0002841368,"about_ca_system_score_gemma":0.000015184686,"threshold_uncertainty_score":0.99998873},"labels":[],"label_agreement":null},{"id":"W4388015486","doi":"10.1029/2023gl105112","title":"A Dissection of the Inter‐Model Spread of the Aerosol Direct Radiative Effect in CMIP6 Models","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Aerosol; Radiative transfer; Environmental science; Anomaly (physics); Atmospheric sciences; Shortwave; Climate model; Albedo (alchemy); Climatology; Meteorology; Climate change; Physics; Geology","score_opus":0.023721630216569763,"score_gpt":0.29285273189948524,"score_spread":0.2691311016829155,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388015486","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":[0.9956969,0.0000037735595,0.00023280534,0.0018855148,0.000066797664,0.00043047548,0.00000626375,0.00001195083,0.0016655355],"genre_scores_gemma":[0.99929863,0.0000054133966,0.000020248297,0.00012638253,0.000026171636,0.00006917293,6.827317e-7,0.00001218678,0.00044112568],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99793726,0.0004406619,0.00017371486,0.00025965626,0.00079502433,0.00039368356],"domain_scores_gemma":[0.9990501,0.00042590484,0.000058955346,0.00040594136,0.000010387839,0.00004872073],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005806233,0.000103901635,0.0001815085,0.0000047815456,0.00011512191,0.00001055416,0.00056719506,0.00004090288,0.000029146446],"category_scores_gemma":[0.00018634756,0.000056573925,0.00015407913,0.0012583459,0.00075664563,0.000108725915,0.0006781258,0.00038796835,0.000049630966],"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":[0.00017297437,0.00017498896,0.041475493,0.000049479506,0.00002888922,0.000003969791,0.0034360182,0.235764,0.70542413,0.00022503846,0.0084348805,0.004810161],"study_design_scores_gemma":[0.00058133993,0.0002315417,0.35564208,0.00014651012,0.000011593528,3.793005e-7,0.0002127168,0.5561807,0.083377995,0.0034029414,0.000029382492,0.00018284823],"about_ca_topic_score_codex":0.0021926984,"about_ca_topic_score_gemma":0.00016672845,"teacher_disagreement_score":0.6220461,"about_ca_system_score_codex":0.00015104329,"about_ca_system_score_gemma":0.000017333465,"threshold_uncertainty_score":0.33147186},"labels":[],"label_agreement":null},{"id":"W4388495636","doi":"10.1002/qj.4615","title":"A case study of the life cycle of a stratus‐lowering coastal‐fog event in Newfoundland, Canada","year":2023,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Thornhill Medical (Canada); Environment and Climate Change Canada","funders":"Office of Naval Research","keywords":"Environmental science; Advection; Atmospheric sciences; Radiative cooling; Fog; Meteorology; Liquid water content; Turbulence; Diurnal cycle; Dissipation; Convection; Turbulence kinetic energy; Entrainment (biomusicology); Geology; Physics; Cloud computing","score_opus":0.0111515355364963,"score_gpt":0.2245285260742773,"score_spread":0.213376990537781,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388495636","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":[0.99908996,0.000024857058,0.000044231165,0.0003196818,0.00022972492,0.00019465663,0.000005170784,0.0000038469752,0.0000878842],"genre_scores_gemma":[0.9996944,0.0000023828554,0.00007680307,0.000117287185,0.000030870207,0.000003633744,7.2745536e-8,0.000006573967,0.00006797151],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99816304,0.00022052311,0.0006000504,0.00013956032,0.0006148343,0.0002619897],"domain_scores_gemma":[0.99901646,0.0001450607,0.00048541382,0.00023019883,0.000018523118,0.00010434347],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00072748214,0.00012994674,0.00031951987,0.000001240815,0.00013756163,0.000011143664,0.0005246568,0.0000706796,0.0001883082],"category_scores_gemma":[0.00005318698,0.00006433441,0.00029735427,0.00041338045,0.00016903147,0.000043380536,0.00017697894,0.000381164,0.0000010852165],"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":[0.00010292553,0.00069401396,0.8432429,0.0000161634,0.00016507825,0.0003445076,0.008125212,0.14051884,0.0010247052,0.000007112311,0.0011666244,0.0045919083],"study_design_scores_gemma":[0.0013640829,0.0020851376,0.9552049,0.000026751493,0.000085360996,0.00014249767,0.032673236,0.007896808,0.00003061932,0.00027570716,0.000073751944,0.00014111458],"about_ca_topic_score_codex":0.24704437,"about_ca_topic_score_gemma":0.37208676,"teacher_disagreement_score":0.13262203,"about_ca_system_score_codex":0.00015026864,"about_ca_system_score_gemma":0.00009302494,"threshold_uncertainty_score":0.7579696},"labels":[],"label_agreement":null},{"id":"W4388573524","doi":"10.5194/egusphere-2023-2238","title":"Technical note: Characterization of a single-beam gradient force aerosol optical tweezer for droplet trapping, phase transitions monitoring, and morphology studies","year":2023,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"McGill University","funders":"Key Research and Development Program of Zhejiang Province; Fundamental Research Funds for the Central Universities; National Natural Science Foundation of China","keywords":"Aerosol; Optical tweezers; Raman spectroscopy; Particle (ecology); Trapping; Materials science; Phase (matter); Optics; Mie scattering; Analytical Chemistry (journal); Chemistry; Scattering; Light scattering; Chromatography","score_opus":0.04981093313491995,"score_gpt":0.3145550006282007,"score_spread":0.2647440674932807,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388573524","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":[0.7451177,0.000037208825,0.2523937,0.0007585787,0.00039197024,0.0009455401,0.00010586584,0.00012534011,0.0001240675],"genre_scores_gemma":[0.9811161,0.00024795212,0.016763907,0.000053109507,0.00013286418,0.0005553198,0.00012038548,0.000051023846,0.0009593521],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99804646,0.000029017949,0.0005736229,0.0007104603,0.00026165147,0.0003787741],"domain_scores_gemma":[0.9991893,0.00009968025,0.00020885545,0.00033739963,0.000033836106,0.00013091476],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00021523407,0.0003272242,0.00057597196,0.000007117229,0.00015142195,0.000026991629,0.00022023532,0.00035122057,0.00011033083],"category_scores_gemma":[0.000059119593,0.00029254943,0.00018033976,0.00014808317,0.00064907066,0.00007629967,0.00045628447,0.000267341,0.000009710959],"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":[0.000074641626,0.000507395,0.0006035308,0.00014058824,0.000052253967,0.0000069495704,0.00084241014,0.0003955786,0.9940676,0.00013655967,0.0002685656,0.002903933],"study_design_scores_gemma":[0.011656942,0.008032602,0.047036704,0.0013721028,0.0021988037,0.00017740332,0.0033145742,0.018336011,0.8960188,0.0052131163,0.0022575534,0.0043853675],"about_ca_topic_score_codex":0.000038197126,"about_ca_topic_score_gemma":0.000021765109,"teacher_disagreement_score":0.23599835,"about_ca_system_score_codex":0.00016176788,"about_ca_system_score_gemma":0.00001798804,"threshold_uncertainty_score":0.9999527},"labels":[],"label_agreement":null},{"id":"W4388669983","doi":"10.5194/acp-23-14077-2023","title":"Sensitivity of cloud-phase distribution to cloud microphysics and thermodynamics in simulated deep convective clouds and SEVIRI retrievals","year":2023,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Cloud fraction; Cloud computing; Cloud top; Liquid water content; Convection; Atmospheric sciences; Radiative transfer; Ice nucleus; Environmental science; Meteorology; Cloud cover; Geology; Thermodynamics; Physics; Nucleation; Optics","score_opus":0.005290435950016488,"score_gpt":0.23121681756064175,"score_spread":0.22592638161062525,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388669983","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":[0.99343103,0.00005599919,0.0057613994,0.00005759735,0.00004109751,0.00022133077,0.00006659283,0.000039207516,0.000325732],"genre_scores_gemma":[0.99891347,0.00014692581,0.00053247047,0.00005717632,0.00007639909,0.0000046011723,0.000056581062,0.000021384274,0.00019099563],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99876773,0.00005955923,0.00024458364,0.00045443053,0.00017425203,0.00029943083],"domain_scores_gemma":[0.9993302,0.00016926524,0.00010828942,0.00021818366,0.000021455615,0.00015260959],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00024768533,0.00024380734,0.0003416172,5.7870718e-8,0.00010916716,0.000024272462,0.00007080903,0.00012954087,0.000058545447],"category_scores_gemma":[0.000043198233,0.00024705182,0.00004117582,0.000678912,0.00037194046,0.00009294562,0.0002246305,0.00017635782,0.000009571395],"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":[0.0007050112,0.0005393902,0.07432046,0.00029666338,0.00010671964,0.000070309914,0.0040662615,0.029050076,0.6418509,0.00020445719,0.00020184401,0.2485879],"study_design_scores_gemma":[0.0024894206,0.00023535218,0.124671,0.0000857106,0.000092761155,0.000020658155,0.0010974953,0.82476616,0.04184699,0.0032161104,0.00062373717,0.0008546337],"about_ca_topic_score_codex":0.00034274437,"about_ca_topic_score_gemma":0.0000123458085,"teacher_disagreement_score":0.79571605,"about_ca_system_score_codex":0.000095906216,"about_ca_system_score_gemma":0.000014121372,"threshold_uncertainty_score":0.99999815},"labels":[],"label_agreement":null},{"id":"W4388743786","doi":"10.5194/egusphere-2023-2238-rc1","title":"Comment on egusphere-2023-2238","year":2023,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"Fundamental Research Funds for the Central Universities; National Natural Science Foundation of China","keywords":"Aerosol; Raman spectroscopy; Relative humidity; Particle (ecology); Chemistry; Analytical Chemistry (journal); Materials science; Optics; Chromatography","score_opus":0.0264834475686202,"score_gpt":0.278785158674475,"score_spread":0.2523017111058548,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388743786","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000026837186,0.0017166042,0.000104081286,0.28659737,0.0025690233,0.00064234855,0.00007998027,0.00023289403,0.7080309],"genre_scores_gemma":[0.000031787673,0.0050107697,0.0005192547,0.11014159,0.00021695331,0.00010677779,0.00022995382,0.00007060972,0.8836723],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99747586,0.000060899034,0.0003896445,0.00067551667,0.0009133998,0.0004846986],"domain_scores_gemma":[0.9987869,0.00009001839,0.00016282304,0.00076142245,0.000007814397,0.00019097372],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00031734759,0.00042902536,0.0005440111,8.846183e-7,0.00013193749,0.000031749245,0.0006570001,0.00024007697,0.19937801],"category_scores_gemma":[0.00004332473,0.00032413736,0.00024648078,0.00034100187,0.00012195162,0.000033766133,0.00062235753,0.0004498008,0.07214466],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000021799858,0.000060444352,0.00007914415,0.00015148606,0.000020783733,0.000014361979,0.000007652845,0.000040655425,9.0650866e-7,0.00008066431,0.98479956,0.014742167],"study_design_scores_gemma":[0.000109765184,0.00010943774,0.00031609728,0.0006361945,0.000050776343,0.0000014582968,0.000016815482,0.000047311394,0.0000044845933,0.00012411109,0.9981775,0.0004060024],"about_ca_topic_score_codex":0.0036143826,"about_ca_topic_score_gemma":0.00093751383,"teacher_disagreement_score":0.17645578,"about_ca_system_score_codex":0.00036919143,"about_ca_system_score_gemma":0.000020967524,"threshold_uncertainty_score":0.9999211},"labels":[],"label_agreement":null},{"id":"W4388851891","doi":"10.5194/egusphere-2023-1945-rc2","title":"Comment on egusphere-2023-1945","year":2023,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"HORIZON EUROPE Excellent Science; H2020 Excellent Science; Horizon 2020 Framework Programme; Hellenic Foundation for Research and Innovation; H2020 Environment; European Commission; Universidad de Granada; Agencia Estatal de Investigación; National Aeronautics and Space Administration","keywords":"Ceilometer; Lidar; Smoke; Aerosol; Environmental science; Atmospheric sciences; Meteorology; Mass concentration (chemistry); Climatology; Remote sensing; Geography; Geology; Chemistry","score_opus":0.025853219295157895,"score_gpt":0.27775868461259395,"score_spread":0.2519054653174361,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388851891","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000027914282,0.0013950743,0.00011299717,0.2888127,0.002636537,0.0006481277,0.00008325495,0.00023784033,0.70604557],"genre_scores_gemma":[0.00003270201,0.004758832,0.0005450325,0.11354175,0.00020813635,0.000108600485,0.00023065484,0.00007072434,0.8805036],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99749553,0.0000600698,0.00039004753,0.0006743679,0.0009044446,0.00047550973],"domain_scores_gemma":[0.9987734,0.00009365904,0.00016255603,0.000774743,0.000007848513,0.00018781997],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00031527356,0.0004269114,0.0005435928,9.146428e-7,0.00013052339,0.00003096356,0.0006527106,0.00023869565,0.19053581],"category_scores_gemma":[0.000044334025,0.00032426478,0.00024562003,0.00033393866,0.00012419932,0.000034170876,0.0006148537,0.00044891922,0.07041175],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002180162,0.000055695877,0.00007283311,0.0001594027,0.000020682193,0.000014827808,0.000008902333,0.00004228716,9.683419e-7,0.00006915622,0.9866175,0.012935533],"study_design_scores_gemma":[0.00010508968,0.00010940658,0.00028561227,0.000657324,0.00005101716,0.0000014851138,0.000016942555,0.000047832847,0.0000045504644,0.00012882346,0.9981886,0.0004033274],"about_ca_topic_score_codex":0.0030826058,"about_ca_topic_score_gemma":0.0009231598,"teacher_disagreement_score":0.17527096,"about_ca_system_score_codex":0.00036346944,"about_ca_system_score_gemma":0.000022362716,"threshold_uncertainty_score":0.99992096},"labels":[],"label_agreement":null},{"id":"W4388912287","doi":"10.5194/egusphere-2023-874","title":"Simulating the seeder-feeder impacts on cloud ice and precipitation over the Alps","year":2023,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"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":"H2020 Research Infrastructures; H2020 European Research Council; Horizon 2020 Framework Programme; European Commission; National Supercomputing Center, Korea Institute of Science and Technology Information; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; National Science Foundation","keywords":"Seeder; Ice crystals; Precipitation; Environmental science; Cloud computing; Atmospheric sciences; Meteorology; Hydrology (agriculture); Geology; Seeding; Computer science; Engineering; Physics; Geotechnical engineering","score_opus":0.023738473157481527,"score_gpt":0.2714729825371927,"score_spread":0.24773450937971117,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388912287","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":[0.97374696,0.000047039597,0.0009469018,0.0030152216,0.0005351648,0.00057641213,0.0000051441284,0.00009785171,0.021029301],"genre_scores_gemma":[0.989161,0.00006188733,0.0003413352,0.0016677505,0.0002136421,0.000035247842,0.0000066497328,0.000035886846,0.008476598],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99847466,0.00010348201,0.00022867482,0.0004598379,0.00044518025,0.0002881567],"domain_scores_gemma":[0.9987143,0.0005271947,0.00016696073,0.00051367993,0.0000067293754,0.000071098504],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005030183,0.00024883187,0.00015379935,9.557e-7,0.00041657808,0.00019605794,0.0003556035,0.00016182245,0.0011747525],"category_scores_gemma":[0.00011499481,0.0001225677,0.000078771925,0.000121324505,0.00019718069,0.000064679676,0.0012123517,0.00047494489,0.00034794342],"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":[0.00007327952,0.000114249924,0.13920793,0.00007679627,0.00017873473,0.000008064223,0.013653201,0.74934065,0.0008259203,0.0017177983,0.07468555,0.020117851],"study_design_scores_gemma":[0.00021475587,0.00007143199,0.88746524,0.000064874526,0.00005066143,0.0000018979135,0.0018354327,0.10181051,0.0000674843,0.0045295344,0.0035323363,0.0003558691],"about_ca_topic_score_codex":0.0026075144,"about_ca_topic_score_gemma":0.0005483537,"teacher_disagreement_score":0.7482573,"about_ca_system_score_codex":0.000107166685,"about_ca_system_score_gemma":0.000014031459,"threshold_uncertainty_score":0.99973834},"labels":[],"label_agreement":null},{"id":"W4389005794","doi":"10.5194/amt-2023-210-rc2","title":"Comment on amt-2023-210","year":2023,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"European Regional Development Fund; Russian Science Foundation; Agence Nationale de la Recherche","keywords":"Depolarization ratio; Lidar; Fluorescence; Wavelength; Ceilometer; Plume; Laser-induced fluorescence; Polarization (electrochemistry); Raman spectroscopy; Optics; Environmental science; Atmospheric sciences; Materials science; Analytical Chemistry (journal); Remote sensing; Meteorology; Physics; Chemistry; Geology; Environmental chemistry","score_opus":0.028554541268717534,"score_gpt":0.2838382871156696,"score_spread":0.25528374584695207,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389005794","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000029511855,0.0012786946,0.00009396578,0.35973403,0.0026028128,0.00056919805,0.000082623425,0.00020029877,0.6354089],"genre_scores_gemma":[0.000030433912,0.0055825575,0.0004134785,0.11945376,0.00018657141,0.0000885421,0.0002290617,0.000053801938,0.8739618],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.997864,0.000047056394,0.00032344167,0.00057045056,0.0007938784,0.00040113705],"domain_scores_gemma":[0.99897206,0.00007704576,0.00013159991,0.00065730524,0.000006058281,0.00015594753],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0002906686,0.00035047936,0.00045637664,0.0000010164676,0.00011142325,0.000025303501,0.0005578074,0.00019264425,0.10362672],"category_scores_gemma":[0.00003803211,0.00026186227,0.00020368486,0.00028506524,0.00010603093,0.000027307904,0.00055706507,0.00039410414,0.059796277],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000014266258,0.000044330976,0.00006849005,0.00012726884,0.00001472297,0.000011998242,0.000007206561,0.000024794248,8.9908303e-7,0.00007512072,0.9896571,0.009966611],"study_design_scores_gemma":[0.00008045055,0.000090751746,0.0003641025,0.0005404433,0.000040752922,0.0000012014945,0.000011841732,0.00003917396,0.0000042573974,0.00010385174,0.99839497,0.00032820547],"about_ca_topic_score_codex":0.0020430328,"about_ca_topic_score_gemma":0.0004299143,"teacher_disagreement_score":0.24028027,"about_ca_system_score_codex":0.0002837972,"about_ca_system_score_gemma":0.000015125725,"threshold_uncertainty_score":0.9999834},"labels":[],"label_agreement":null},{"id":"W4389079986","doi":"10.3390/rs15235542","title":"A Satellite Observational Study of Topographical Effects on Daytime Shallow Convective Clouds","year":2023,"lang":"en","type":"article","venue":"Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":5,"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 Toronto","funders":"Natural Science Foundation of Fujian Province; National Natural Science Foundation of China; U.S. Geological Survey; National Aeronautics and Space Administration","keywords":"Elevation (ballistics); Daytime; Terrain; Satellite; Scale (ratio); Environmental science; Elevation angle; Remote sensing; Cloud computing; Meteorology; Geology; Atmospheric sciences; Geography; Physics; Astronomy; Cartography; Computer science","score_opus":0.036338699450934424,"score_gpt":0.2756350275688235,"score_spread":0.2392963281178891,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389079986","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":[0.9957881,0.000008578664,0.0002963671,0.00016791858,0.00014222393,0.00030828084,8.1847463e-7,0.00008151588,0.003206222],"genre_scores_gemma":[0.99778366,0.000008873846,0.0015803073,0.00020218013,0.000057573954,6.317685e-8,0.0000037018158,0.000017668828,0.00034596276],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99871933,0.0001038693,0.0001959308,0.00031787722,0.00042571392,0.00023726426],"domain_scores_gemma":[0.9993679,0.00024218783,0.00007757831,0.00022810038,0.0000120572395,0.00007218701],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022522063,0.00013567731,0.00019796526,0.0000044033077,0.000110238245,0.0000127647945,0.00009238409,0.00006499547,0.000051077917],"category_scores_gemma":[0.00006365038,0.0001214071,0.0000696326,0.0007122964,0.0000916033,0.000045229794,0.00011343515,0.00013571503,0.0002066004],"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":[0.00026121884,0.00040534392,0.2446495,0.0000520727,0.00018603899,0.00036841165,0.00886962,0.008296952,0.07918428,0.00016645789,0.0006115918,0.6569485],"study_design_scores_gemma":[0.00062819466,0.00052060897,0.9257262,0.000052712767,0.00002690361,0.0000057262437,0.0005141835,0.06927245,0.0016265282,0.0010810755,0.0003438399,0.00020161428],"about_ca_topic_score_codex":0.0003017453,"about_ca_topic_score_gemma":0.00007112129,"teacher_disagreement_score":0.68107665,"about_ca_system_score_codex":0.000065654756,"about_ca_system_score_gemma":0.000007600668,"threshold_uncertainty_score":0.4950838},"labels":[],"label_agreement":null},{"id":"W4389138689","doi":"10.1364/pcaop.2023.ptu5f.3","title":"Target Dependent Detection Range Variations Through Aerosol when using Polarimetric LiDAR","year":2023,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"Defence Research and Development Canada","funders":"","keywords":"Polarimetry; Lidar; Remote sensing; Range (aeronautics); Aerosol; Environmental science; Meteorology; Geology; Materials science; Optics; Scattering; Physics","score_opus":0.02261828430763719,"score_gpt":0.24604930489909926,"score_spread":0.22343102059146208,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389138689","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":[0.5820074,0.00003061288,0.40079093,0.0001658479,0.00033275818,0.00023797939,0.0000060605616,0.00027921895,0.01614918],"genre_scores_gemma":[0.95685446,0.000011942035,0.039036658,0.00022766649,0.00007193257,0.0000115972525,0.000004732527,0.000021237895,0.0037597937],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99879307,0.00004228847,0.00018650875,0.00030077764,0.00035338243,0.00032395954],"domain_scores_gemma":[0.99959594,0.00003618035,0.00006331093,0.00022421578,0.000007070671,0.000073265044],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00018374962,0.0001289192,0.00011581703,0.000003966097,0.00034224987,0.00005045843,0.00016433369,0.0000903827,0.00715169],"category_scores_gemma":[0.00003784612,0.00011500014,0.000063650215,0.0009774531,0.000048338206,0.00032775573,0.00019647976,0.00010940523,0.0022066873],"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":[0.000058828773,0.00044428805,0.6437927,0.00002553073,0.00013964005,0.00005506944,0.0044582626,0.041615684,0.28413436,0.0008393436,0.007037811,0.01739852],"study_design_scores_gemma":[0.0027013803,0.00045850367,0.6720406,0.000022676475,0.0002304237,0.00007256526,0.0020815148,0.19467993,0.088389866,0.012277586,0.024895985,0.0021489991],"about_ca_topic_score_codex":0.008235867,"about_ca_topic_score_gemma":0.00034494617,"teacher_disagreement_score":0.37484705,"about_ca_system_score_codex":0.00020714977,"about_ca_system_score_gemma":0.000010916805,"threshold_uncertainty_score":0.9985702},"labels":[],"label_agreement":null},{"id":"W4389639887","doi":"10.1029/2023jd039971","title":"The Effects of Aminium and Ammonium Cations on the Ice Nucleation Activity of K‐Feldspar","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"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":"Sorbonne Université; National Natural Science Foundation of China","keywords":"Ice nucleus; Nucleation; Chemistry; Feldspar; Ammonium; Mineral; Inorganic chemistry; Steric effects; Ion; Geology; Organic chemistry","score_opus":0.02135778783292896,"score_gpt":0.30216435600654734,"score_spread":0.2808065681736184,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389639887","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":[0.9963284,0.000057627374,0.000049149698,0.0019922736,0.00007138862,0.00017606767,0.0000011579801,0.0000046069667,0.0013193259],"genre_scores_gemma":[0.99854,0.00038064827,0.00008153621,0.000018152274,0.00007737788,0.000007683308,1.2323693e-7,0.0000095285895,0.0008849805],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9980834,0.00031599362,0.00022727896,0.00011564311,0.000995061,0.0002626097],"domain_scores_gemma":[0.9954924,0.0038597025,0.00022363786,0.00024144878,0.000088002984,0.0000947821],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00096881523,0.00008215697,0.00017021902,0.000001336622,0.0003316059,0.00003152301,0.00037246902,0.00004354461,0.0000614512],"category_scores_gemma":[0.0011271237,0.000042100422,0.00008881766,0.0006045134,0.00080429803,0.000117220385,0.00021157201,0.0004025862,0.000046640555],"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":[0.0024469797,0.0018259041,0.05705853,0.0002823603,0.00040656546,0.00005077365,0.00441726,0.0024729976,0.5523764,0.018495185,0.0843482,0.27581882],"study_design_scores_gemma":[0.00030257204,0.0015316233,0.9509273,0.00008113602,0.00001921693,0.0000019551007,0.00081492856,0.0026160409,0.037229363,0.0039490107,0.00245385,0.00007297007],"about_ca_topic_score_codex":0.0006343303,"about_ca_topic_score_gemma":0.00008058332,"teacher_disagreement_score":0.8938688,"about_ca_system_score_codex":0.000057532583,"about_ca_system_score_gemma":0.000041410796,"threshold_uncertainty_score":0.29634696},"labels":[],"label_agreement":null},{"id":"W4389832722","doi":"10.1002/9781119700357.ch6","title":"Extratropical Cloud Feedbacks","year":2023,"lang":"en","type":"other","venue":"Geophysical monograph","topic":"Atmospheric aerosols and clouds","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":"McGill University","funders":"Pacific Northwest National Laboratory; Lawrence Livermore National Laboratory; Nuclear Safety and Security Commission; Battelle; University of Wyoming; National Aeronautics and Space Administration; U.S. Department of Energy; National Science Foundation","keywords":"Extratropical cyclone; Cloud feedback; Environmental science; Context (archaeology); Shortwave; Climatology; Longwave; Climate model; Positive feedback; Global warming; Cloud computing; Climate change; Cloud cover; Cloud forcing; Cloud height; Atmospheric sciences; Climate sensitivity; Geography; Computer science; Geology; Radiative transfer; Physics; Ecology; Biology","score_opus":0.005771560258282253,"score_gpt":0.20769571053498023,"score_spread":0.20192415027669797,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389832722","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.010925654,0.00012762182,0.0005884313,0.00017783983,0.0012921575,0.0003737386,0.0000305274,0.001786502,0.9846975],"genre_scores_gemma":[0.024398604,0.00023804037,0.0016138589,0.00032082482,0.002022785,0.000095150004,0.000017035827,0.0014748875,0.96981883],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99819237,0.000034379867,0.00019407297,0.00061854464,0.00042803408,0.00053262274],"domain_scores_gemma":[0.99910927,0.00003331889,0.00010968388,0.00052180944,0.000002166186,0.00022378105],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000036038797,0.00036838753,0.00038010487,0.0000045432657,0.0000751521,0.00003219643,0.00041214467,0.00034935627,0.013454617],"category_scores_gemma":[0.000008495531,0.0003165599,0.00032120154,0.0005497959,0.00042241937,0.00003682676,0.00028861806,0.00035816035,0.019629601],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000066141147,0.000099055746,0.007499962,0.000007623701,0.00004398996,0.000025419647,0.000025806408,0.000007355792,0.00004033869,0.00047641643,0.9782019,0.013565502],"study_design_scores_gemma":[0.00022493151,0.000107142834,0.051842857,0.00004085375,0.000048234924,0.0000014894794,0.000024329478,0.000062078965,0.000007234962,0.0014866828,0.9456043,0.00054985593],"about_ca_topic_score_codex":0.0022461573,"about_ca_topic_score_gemma":0.0005241738,"teacher_disagreement_score":0.044342894,"about_ca_system_score_codex":0.000040879604,"about_ca_system_score_gemma":0.0000065380254,"threshold_uncertainty_score":0.99992865},"labels":[],"label_agreement":null},{"id":"W4389833006","doi":"10.1002/9781119700357.ch5","title":"A Review of the Factors Influencing Arctic Mixed‐Phase Clouds: Progress and Outlook","year":2023,"lang":"en","type":"review","venue":"Geophysical monograph","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":"McGill University","funders":"Goddard Space Flight Center; Vetenskapsrådet; Deutsche Forschungsgemeinschaft; Nuclear Safety and Security Commission; Svenska Forskningsrådet Formas; National Aeronautics and Space Administration","keywords":"Arctic; Environmental science; Troposphere; Atmospheric sciences; Arctic geoengineering; Climatology; Climate model; Sea ice; Cloud physics; Arctic ice pack; Meteorology; Climate change; Cloud computing; Geology; Geography; Oceanography; Drift ice","score_opus":0.02909343337429051,"score_gpt":0.30459480045469073,"score_spread":0.27550136708040024,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389833006","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.014787761,0.98370695,0.0000026898124,0.00002502774,0.00017138434,0.0011361557,0.000029438097,0.00005159285,0.00008898775],"genre_scores_gemma":[0.0007717146,0.9986542,0.00008833127,0.000094288596,0.000048987054,0.00016564646,0.000011959494,0.000053895586,0.00011097827],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9977768,0.00018606888,0.0006653853,0.0005427362,0.00042229248,0.00040668657],"domain_scores_gemma":[0.9984443,0.0001499752,0.00056067854,0.00067249377,0.000012461859,0.00016005918],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00018645376,0.00047034287,0.001418223,0.0000044546273,0.00014689598,0.000025340954,0.0006120443,0.00016308963,0.00008914218],"category_scores_gemma":[0.00006614332,0.00026715247,0.0008857084,0.0013013051,0.00079092,0.000076776196,0.00073608436,0.00043204686,0.00011057949],"study_design_candidate":"design_other","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":[0.0000022715762,0.00018994564,0.003426505,0.07260318,0.00016423389,0.0000043096875,0.00013911276,4.0686672e-7,7.7351774e-7,0.000046279754,0.0010247267,0.92239827],"study_design_scores_gemma":[0.00027026053,0.0002452197,0.010535595,0.15003403,0.0018955825,0.000008931572,0.000085808024,0.0000099373,0.0000015958418,0.00054090034,0.83551925,0.0008529055],"about_ca_topic_score_codex":0.00026119576,"about_ca_topic_score_gemma":0.000010248559,"teacher_disagreement_score":0.9215453,"about_ca_system_score_codex":0.00006174456,"about_ca_system_score_gemma":0.00003367296,"threshold_uncertainty_score":0.99997807},"labels":[],"label_agreement":null},{"id":"W4389894545","doi":"10.5194/egusphere-2023-1945-ac1","title":"Reply on RC1","year":2023,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"HORIZON EUROPE Excellent Science; H2020 Excellent Science; Horizon 2020 Framework Programme; Hellenic Foundation for Research and Innovation; H2020 Environment; European Commission; Universidad de Granada; Agencia Estatal de Investigación; National Aeronautics and Space Administration","keywords":"Ceilometer; Lidar; Smoke; Aerosol; Environmental science; Atmospheric sciences; Meteorology; Mass concentration (chemistry); Climatology; Remote sensing; Geography; Geology; Chemistry","score_opus":0.026633848648375483,"score_gpt":0.281739915765091,"score_spread":0.2551060671167155,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389894545","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000058078247,0.0011877151,0.00004543212,0.0853886,0.002073141,0.00035407513,0.000030504487,0.0002458215,0.91061664],"genre_scores_gemma":[0.000027702192,0.0043644817,0.00035001742,0.051770918,0.00019447974,0.000043493215,0.00009016552,0.000046762725,0.94311196],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9983323,0.000025353,0.00024181827,0.00053312036,0.00058265665,0.00028470292],"domain_scores_gemma":[0.99910927,0.00004543233,0.00010303268,0.0006354473,0.0000045023767,0.00010229738],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00022354668,0.00024356734,0.0003295704,5.3738205e-7,0.000069201546,0.000015738513,0.0003981685,0.00012786122,0.09315952],"category_scores_gemma":[0.000069304166,0.0001771951,0.000156209,0.00024060541,0.00007920655,0.000024017369,0.0003119409,0.00028079824,0.06324427],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[9.0600514e-7,0.000014704292,0.000057636375,0.00008690968,0.000006618528,0.000012947123,0.000004546301,0.000015874757,0.0000010762662,0.000023632181,0.9862739,0.013501277],"study_design_scores_gemma":[0.0000382743,0.00005604107,0.0006027008,0.000408913,0.000024297176,0.0000017800179,0.000004393374,0.000016963368,0.0000036020417,0.00008410035,0.9985259,0.00023299616],"about_ca_topic_score_codex":0.0016544036,"about_ca_topic_score_gemma":0.00018394631,"teacher_disagreement_score":0.033617683,"about_ca_system_score_codex":0.00013927974,"about_ca_system_score_gemma":0.000013796646,"threshold_uncertainty_score":0.9374851},"labels":[],"label_agreement":null},{"id":"W4389980610","doi":"10.5194/amt-2023-215-rc2","title":"Comment on amt-2023-215","year":2023,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"National Research Council Canada; McGill University","funders":"","keywords":"Environmental science","score_opus":0.029721038284547644,"score_gpt":0.2847269984584924,"score_spread":0.2550059601739448,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389980610","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000026613303,0.0013185656,0.00009347881,0.35169396,0.002526627,0.0005779873,0.000082698534,0.00019900185,0.6434811],"genre_scores_gemma":[0.000030702195,0.005440867,0.00039679176,0.118753016,0.00018398317,0.00008945035,0.00023145515,0.000053397805,0.87482035],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99785656,0.00004832945,0.0003238241,0.0005689179,0.0008018505,0.00040051015],"domain_scores_gemma":[0.9989773,0.00007365272,0.00013148223,0.0006535843,0.0000061685364,0.00015779714],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0002968768,0.00035002673,0.00045875218,0.0000010143725,0.00010993211,0.000025310503,0.0005553562,0.00018860317,0.101711676],"category_scores_gemma":[0.000036700323,0.000261451,0.0002015981,0.00028795298,0.00010478757,0.000027401824,0.00055924087,0.00038057854,0.060445476],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000014172072,0.000044258104,0.00006822057,0.00012629454,0.000014888566,0.000012125339,0.0000072729267,0.000026647758,8.4800007e-7,0.000075146476,0.9904508,0.009172064],"study_design_scores_gemma":[0.0000813791,0.00009100876,0.00035168423,0.00054333993,0.000041045212,0.0000011957146,0.000012256754,0.00004048958,0.0000040377663,0.00010231615,0.99840355,0.000327706],"about_ca_topic_score_codex":0.0020320762,"about_ca_topic_score_gemma":0.00044855435,"teacher_disagreement_score":0.23294093,"about_ca_system_score_codex":0.00028193404,"about_ca_system_score_gemma":0.000017220927,"threshold_uncertainty_score":0.9999838},"labels":[],"label_agreement":null},{"id":"W4390082684","doi":"10.20944/preprints202312.1681.v1","title":"Lidar Optical and Microphysical Characterization of Tropospheric and Stratospheric Fire Smoke Layers Due to Canadian Wildfires Passing over Naples (Italy)","year":2023,"lang":"en","type":"preprint","venue":"Preprints.org","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"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":"National Oceanic and Atmospheric Administration; Barcelona Supercomputing Center; European Commission","keywords":"Aerosol; Lidar; Troposphere; Atmospheric sciences; Environmental science; Atmosphere (unit); Altitude (triangle); Sun photometer; Stratosphere; Meteorology; Remote sensing; Geology; Geography","score_opus":0.03933681406960292,"score_gpt":0.2717956635319543,"score_spread":0.23245884946235135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4390082684","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":[0.99788153,0.000031012903,0.00021658,0.000626004,0.00019392847,0.0004999892,0.000047047255,0.000065380635,0.0004385054],"genre_scores_gemma":[0.99817723,0.00011930775,0.00096770504,0.00019468868,0.00007742281,0.000052409752,0.000033233264,0.000064324464,0.00031366784],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99767005,0.00006752544,0.00043443055,0.0010139813,0.0003370403,0.0004769702],"domain_scores_gemma":[0.9986721,0.000041884727,0.00019010557,0.0005608565,0.000018718662,0.00051629613],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00018205048,0.0003878594,0.0005102594,0.000004957725,0.00017240978,0.000067469766,0.00034398737,0.0003019206,0.0008200474],"category_scores_gemma":[0.000074602394,0.0003968618,0.00009582165,0.000275189,0.00040353087,0.00013144106,0.0015179557,0.00040285845,0.00015959816],"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":[0.000030218875,0.00005973492,0.8630161,0.0000803754,0.00005625159,0.00003915667,0.0008915655,0.0005711614,0.13095951,0.000040748142,0.00002232635,0.004232829],"study_design_scores_gemma":[0.00014881388,0.000048585032,0.99191415,0.00010850951,0.000048593356,0.000006935159,0.00013584856,0.0012247106,0.005455573,0.00016410537,0.00034407855,0.00040007595],"about_ca_topic_score_codex":0.08190996,"about_ca_topic_score_gemma":0.0056073996,"teacher_disagreement_score":0.12889804,"about_ca_system_score_codex":0.0002772613,"about_ca_system_score_gemma":0.0001224937,"threshold_uncertainty_score":0.9998483},"labels":[],"label_agreement":null},{"id":"W4390228125","doi":"10.1007/978-3-031-37818-8_41","title":"Cloud Base Height Correlation Between a Co-located Micro-Pulse LiDAR and a Lufft CHM15k Ceilometer","year":2023,"lang":"en","type":"book-chapter","venue":"Springer atmospheric sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Ceilometer; Cloud base; Lidar; Cloud computing; Remote sensing; Base (topology); Algorithm; Meteorology; Correlation coefficient; Environmental science; Computer science; Scale (ratio); Geography; Mathematics; Cartography; Machine learning","score_opus":0.02122504156138936,"score_gpt":0.23585446317736591,"score_spread":0.21462942161597656,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4390228125","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.542123,0.00093461387,0.001030254,0.00059014733,0.0017810672,0.0012320171,0.000081557875,0.0006024106,0.4516249],"genre_scores_gemma":[0.3142517,0.0010240794,0.019056404,0.0007407603,0.0011197753,0.0000758278,0.00006343803,0.0003122453,0.66335577],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99569213,0.000052567408,0.00070413685,0.001565992,0.0011486717,0.0008365021],"domain_scores_gemma":[0.99829394,0.0002174404,0.00048672353,0.00057752035,0.000026826465,0.0003975758],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00075426075,0.00074563385,0.0007193482,0.0000043368186,0.00075991405,0.00023625806,0.0007055138,0.0004885069,0.0072107892],"category_scores_gemma":[0.00005256035,0.00064619136,0.00021564213,0.0005470491,0.002099311,0.00036493826,0.00069724966,0.0005583544,0.0032439367],"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":[0.0002899888,0.00029373035,0.70946246,0.00037330363,0.0006912474,0.0007014894,0.0051761153,0.0039212834,0.00350171,0.008167364,0.035265155,0.23215613],"study_design_scores_gemma":[0.0030690676,0.0029036675,0.47512713,0.0012320718,0.0011525587,0.00016832926,0.00089349103,0.014412409,0.0014899861,0.021254215,0.46953687,0.00876018],"about_ca_topic_score_codex":0.00047508592,"about_ca_topic_score_gemma":0.000086745786,"teacher_disagreement_score":0.43427172,"about_ca_system_score_codex":0.00024473688,"about_ca_system_score_gemma":0.00009132675,"threshold_uncertainty_score":0.9995989},"labels":[],"label_agreement":null},{"id":"W4390228247","doi":"10.1007/978-3-031-37818-8_96","title":"Regional Changes in the Dominant Aerosol Type Over Europe During the ACTRIS COVID-19 Campaign","year":2023,"lang":"en","type":"book-chapter","venue":"Springer atmospheric sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Aerosol; Coronavirus disease 2019 (COVID-19); Lidar; Environmental science; Meteorology; Severe acute respiratory syndrome coronavirus 2 (SARS-CoV-2); Atmospheric sciences; Troposphere; 2019-20 coronavirus outbreak; Quarter (Canadian coin); Climatology; Geography; Remote sensing; Outbreak; Physics; Geology; Virology; Medicine","score_opus":0.03523145470621976,"score_gpt":0.26075719891803356,"score_spread":0.22552574421181382,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4390228247","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.49053854,0.002390572,0.00016778805,0.014582489,0.002902476,0.002871681,0.000023233502,0.00040899953,0.4861142],"genre_scores_gemma":[0.2665391,0.005206709,0.0013157116,0.009367236,0.0009723934,0.0001716544,0.000006827837,0.00020366805,0.7162167],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99608356,0.00011384131,0.00041324287,0.001052847,0.0015489456,0.0007875655],"domain_scores_gemma":[0.99823344,0.00041037367,0.00036987304,0.0007769838,0.000017214263,0.00019209478],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0015710022,0.0005307967,0.000395335,0.0000022677048,0.0011215728,0.00022019437,0.0022301397,0.0002149022,0.005022659],"category_scores_gemma":[0.00016532929,0.00029222414,0.00014971569,0.0010002651,0.0021144692,0.00016203377,0.0007911027,0.00060288835,0.0011453271],"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":[0.0012840484,0.00091088214,0.36853668,0.0008615886,0.0007462324,0.004707329,0.0721867,0.08203982,0.013784159,0.088887386,0.32296097,0.043094225],"study_design_scores_gemma":[0.0008413757,0.0005211642,0.08205311,0.00021584425,0.00012105484,0.00014226926,0.0022075572,0.0016162578,0.00009529019,0.0035126584,0.9067078,0.001965581],"about_ca_topic_score_codex":0.0013442767,"about_ca_topic_score_gemma":0.0023151503,"teacher_disagreement_score":0.58374685,"about_ca_system_score_codex":0.0003453958,"about_ca_system_score_gemma":0.00018763712,"threshold_uncertainty_score":0.999953},"labels":[],"label_agreement":null},{"id":"W4390970407","doi":"10.1063/5.0182767","title":"The UV index in the 21st century over Thessaloniki, Greece, from measurements and simulations in relation to the Montreal Protocol","year":2024,"lang":"en","type":"article","venue":"AIP conference proceedings","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Relation (database); Index (typography); Protocol (science); Computer science; Environmental science; Data mining; World Wide Web","score_opus":0.02179515322433123,"score_gpt":0.2598336311868825,"score_spread":0.2380384779625513,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4390970407","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":[0.9633666,0.000055521927,0.0001499781,0.004308468,0.00006382083,0.015221689,0.0000055155056,0.000032976095,0.016795387],"genre_scores_gemma":[0.9934955,0.000017198285,0.00004085772,0.00033946426,0.000038442755,0.005951117,0.0000013043715,0.000009919787,0.000106193016],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988145,0.000029611872,0.000211654,0.00029907608,0.00041403907,0.00023111887],"domain_scores_gemma":[0.9996591,0.000112843736,0.00004848613,0.00012439389,0.000015323732,0.00003982033],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046417332,0.00013398366,0.00008298522,0.0000037922632,0.00022759539,0.00033169947,0.00035085203,0.00006238854,0.00015468811],"category_scores_gemma":[0.00006654569,0.000065737666,0.00002034059,0.0004122969,0.00011628055,0.0002815441,0.00014797403,0.0002596214,0.000035167894],"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":[0.00003342798,0.000034268898,0.9600349,0.000005933588,0.0000068269924,9.663341e-7,0.011548727,0.0001553623,0.00047566032,0.0010425416,0.0006008116,0.02606055],"study_design_scores_gemma":[0.00020904871,0.00003166708,0.9341677,0.00006054672,0.00000648095,7.488447e-7,0.0020953396,0.04832475,0.000008967731,0.0036569934,0.011338691,0.000099067576],"about_ca_topic_score_codex":0.002744455,"about_ca_topic_score_gemma":0.0047741826,"teacher_disagreement_score":0.048169386,"about_ca_system_score_codex":0.00010386597,"about_ca_system_score_gemma":0.000023019109,"threshold_uncertainty_score":0.4148813},"labels":[],"label_agreement":null},{"id":"W4391134210","doi":"10.1007/s11869-024-01510-9","title":"Variability of Middle East springtime dust events between 2011 and 2022","year":2024,"lang":"en","type":"article","venue":"Air Quality Atmosphere & Health","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Nazarbayev University","keywords":"Environmental science; Topsoil; Climatology; Wind speed; Atmospheric sciences; Middle East; Dust storm; Asian Dust; Storm; Geography; Aerosol; Meteorology; Soil water; Geology; Soil science","score_opus":0.036671373976307854,"score_gpt":0.28968249818270186,"score_spread":0.253011124206394,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391134210","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":[0.9889659,0.0008150605,0.0031290615,0.0026861867,0.00021351116,0.00038743616,0.0000604407,0.000113411916,0.0036289915],"genre_scores_gemma":[0.99309117,0.00011202346,0.0047209724,0.00042756216,0.00009163595,0.000014430896,0.0000111419695,0.00002924962,0.001501842],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99713075,0.00043574974,0.00074941077,0.0006799488,0.0005017719,0.00050239294],"domain_scores_gemma":[0.99871236,0.00020314699,0.00019900707,0.00052580936,0.000012018707,0.00034766874],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0024205218,0.0002408684,0.0004833784,4.588067e-7,0.00019558024,0.000017106844,0.00026544905,0.00013866565,0.0058018127],"category_scores_gemma":[0.000052835825,0.00022048727,0.00011354929,0.0002812436,0.00028685006,0.00020816499,0.00034850542,0.00031675797,0.00041235174],"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":[0.000019390274,0.00014687545,0.95544195,0.00046284636,0.000042564156,0.0000022996812,0.0015545436,0.00010657048,0.000053599815,0.0014962162,0.0027656779,0.037907463],"study_design_scores_gemma":[0.00024413744,0.00021273505,0.97936726,0.00009543146,0.000021969396,0.000003179292,0.0004628795,0.00066639856,0.000025185705,0.0027302143,0.015898546,0.00027207757],"about_ca_topic_score_codex":0.0119683435,"about_ca_topic_score_gemma":0.00032542262,"teacher_disagreement_score":0.037635386,"about_ca_system_score_codex":0.00032982414,"about_ca_system_score_gemma":0.000118294454,"threshold_uncertainty_score":0.995107},"labels":[],"label_agreement":null},{"id":"W4391229659","doi":"10.3390/atmos15020150","title":"Quantification of Shortwave Surface Albedo Feedback Using a Neural Network Approach","year":2024,"lang":"en","type":"article","venue":"Atmosphere","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Radiative transfer; Radiative flux; Shortwave; Albedo (alchemy); Cloud albedo; Nonlinear system; Environmental science; Remote sensing; Computer science; Physics; Cloud cover; Cloud computing; Optics; Geology","score_opus":0.02110996780698496,"score_gpt":0.24290628444290288,"score_spread":0.22179631663591792,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391229659","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":[0.97023684,0.0010817858,0.014175601,0.000066569235,0.000291741,0.00020006324,0.0000026888854,0.00008012416,0.013864603],"genre_scores_gemma":[0.9605708,0.000024750043,0.037500914,0.00005000769,0.00009084332,0.000003847316,0.000007405114,0.000033141634,0.0017182917],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9986838,0.00004681724,0.0002748209,0.0004064186,0.00027393902,0.0003141704],"domain_scores_gemma":[0.99948347,0.000040384002,0.000071274226,0.00031877152,0.000008028241,0.00007805899],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00018900694,0.00016952919,0.00018717455,1.04821154e-7,0.000098947574,0.000050998042,0.00021106096,0.00008057059,0.001839463],"category_scores_gemma":[0.0000064822984,0.00014718666,0.000102202124,0.00050059234,0.00017825779,0.00018933578,0.00013457921,0.00014204471,0.00017392577],"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":[0.0000128749,0.00005035599,0.062064473,0.000039084072,0.000027752156,0.0000073733804,0.00026650366,0.92132324,0.0037931108,0.0006326996,0.0051797796,0.0066027544],"study_design_scores_gemma":[0.000080660226,0.000040290328,0.017205913,0.000033912052,0.00004323953,0.00002008644,0.00029022817,0.9775216,0.00028292663,0.00023740648,0.0040256935,0.00021804693],"about_ca_topic_score_codex":0.0007804581,"about_ca_topic_score_gemma":0.000042446176,"teacher_disagreement_score":0.05619836,"about_ca_system_score_codex":0.00008814591,"about_ca_system_score_gemma":0.00001856145,"threshold_uncertainty_score":0.99907297},"labels":[],"label_agreement":null},{"id":"W4391375845","doi":"10.5194/acp-24-1329-2024","title":"Monitoring biomass burning aerosol transport using CALIOP observations and reanalysis models: a Canadian wildfire event in 2019","year":2024,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":17,"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":"H2020 Environment; HORIZON EUROPE Widening participation and spreading excellence; Horizon 2020; China Scholarship Council; Hellenic Foundation for Research and Innovation; H2020 Excellent Science; Academy of Finland; Universidad de Granada; Agencia Estatal de Investigación; National Aeronautics and Space Administration","keywords":"Ceilometer; Aerosol; Lidar; Environmental science; Smoke; Chemical transport model; Biomass burning; Atmospheric sciences; AERONET; Meteorology; Mass concentration (chemistry); Climatology; Remote sensing; Geology; Geography; Chemistry","score_opus":0.016602677294006156,"score_gpt":0.22626952246848464,"score_spread":0.20966684517447848,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391375845","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":[0.994028,0.001126882,0.0037469482,0.000079499616,0.000037300557,0.00007069629,0.000012547538,0.000029049583,0.0008690907],"genre_scores_gemma":[0.99328226,0.00025098593,0.0055410424,0.000022180184,0.000084307765,0.000009968959,0.000010894901,0.000021379523,0.00077700714],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99892366,0.000009851631,0.00019938112,0.0003852088,0.00019192958,0.00028996408],"domain_scores_gemma":[0.9995884,0.00001983068,0.00003178792,0.00016239258,0.000005466528,0.00019217182],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010424546,0.00018509451,0.00017619229,7.829931e-8,0.00017283636,0.000053005955,0.00009028236,0.00008964976,0.00015252543],"category_scores_gemma":[0.0000029964212,0.00018766441,0.000054043026,0.0005279764,0.00010050104,0.00026709266,0.000033105323,0.00015965797,0.000002751937],"study_design_candidate":"simulation_or_modeling","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":[0.0000111322115,0.00007136593,0.6997116,0.0002009628,0.0001231767,0.00013268959,0.0030760984,0.13494594,0.062024537,0.000029515722,0.00010265627,0.09957031],"study_design_scores_gemma":[0.00017144388,0.000010092998,0.036311086,0.00019534737,0.000107024076,0.000015415744,0.0004206082,0.95920926,0.0018611528,0.0006427025,0.00064758625,0.0004082561],"about_ca_topic_score_codex":0.13649996,"about_ca_topic_score_gemma":0.0026459205,"teacher_disagreement_score":0.82426333,"about_ca_system_score_codex":0.0002847527,"about_ca_system_score_gemma":0.000072110524,"threshold_uncertainty_score":0.8692502},"labels":[],"label_agreement":null},{"id":"W4391403458","doi":"10.3390/rs16030538","title":"Lidar Optical and Microphysical Characterization of Tropospheric and Stratospheric Fire Smoke Layers Due to Canadian Wildfires Passing over Naples (Italy)","year":2024,"lang":"en","type":"article","venue":"Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":8,"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":"National Oceanic and Atmospheric Administration; Barcelona Supercomputing Center; Ministero dell’Istruzione, dell’Università e della Ricerca; European Commission","keywords":"Environmental science; Troposphere; Smoke; Lidar; Atmospheric sciences; Remote sensing; Climatology; Meteorology; Geology; Geography","score_opus":0.005458316737687018,"score_gpt":0.204699757592996,"score_spread":0.19924144085530898,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391403458","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":[0.9952172,0.00012268264,0.0035060572,0.0005423634,0.00009092551,0.000117828335,0.0000056218178,0.00003011771,0.0003672085],"genre_scores_gemma":[0.98989403,0.00003720753,0.009678645,0.00023138417,0.00006181317,3.003958e-8,0.00000387014,0.00002681384,0.00006619337],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99903226,0.000025174366,0.00017230351,0.0003364155,0.00015716761,0.00027667944],"domain_scores_gemma":[0.999563,0.000028477369,0.000030782918,0.00012096827,0.0000061874393,0.00025061512],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000058853828,0.00015688932,0.00019064396,0.0000024252533,0.00012974109,0.00012569274,0.00004622724,0.00007742615,0.000056240504],"category_scores_gemma":[0.000015711244,0.00014612054,0.000035381643,0.0002897603,0.00019275381,0.00013836549,0.00007054332,0.00010620142,0.000010333871],"study_design_candidate":"bench_or_experimental","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":[0.000010757336,0.000006621773,0.0016118875,0.000032551452,0.000017437284,0.00011169274,0.0006685369,0.00010937954,0.58063996,0.000028816039,0.00003471709,0.41672766],"study_design_scores_gemma":[0.0002830472,0.00027666413,0.57810926,0.0004664282,0.00010105796,0.00024119609,0.0005234817,0.39849073,0.017027885,0.00022507487,0.0034961547,0.00075900566],"about_ca_topic_score_codex":0.03292638,"about_ca_topic_score_gemma":0.0028366537,"teacher_disagreement_score":0.5764974,"about_ca_system_score_codex":0.00013704142,"about_ca_system_score_gemma":0.000043298085,"threshold_uncertainty_score":0.9735134},"labels":[],"label_agreement":null},{"id":"W4391462275","doi":"10.5194/amt-17-875-2024","title":"An intercomparison of EarthCARE cloud, aerosol, and precipitation retrieval products","year":2024,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; Environment and Climate Change Canada","funders":"Natural Environment Research Council; Sight Research UK; European Space Agency","keywords":"Aerosol; Environmental science; Precipitation; Atmospheric sciences; Meteorology; Cloud computing; Remote sensing; Climatology; Computer science; Geography; Geology","score_opus":0.020039157402735968,"score_gpt":0.25465254887199845,"score_spread":0.2346133914692625,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391462275","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":[0.97927105,0.0013444612,0.015305295,0.00023514038,0.00026169245,0.00064413337,0.0000031047882,0.0005320437,0.002403054],"genre_scores_gemma":[0.94597214,0.00013659046,0.053500053,0.000043823955,0.00008730818,0.00003345692,0.000004873822,0.000032610555,0.00018913148],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9980324,0.000099453646,0.00036852347,0.00053807534,0.0007167769,0.0002447551],"domain_scores_gemma":[0.9993451,0.000017054192,0.00009570819,0.00037682892,0.00006669038,0.000098589924],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007788136,0.00021897117,0.00023523947,8.3567403e-7,0.000077623205,0.00007228935,0.00021717303,0.00010430532,0.00037093987],"category_scores_gemma":[0.00005922004,0.00018903399,0.00004903072,0.00044414678,0.00020083821,0.0003844166,0.00010422288,0.00016418572,0.000031473286],"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":[0.00012726069,0.00027199805,0.03868274,0.00027271523,0.00006661084,0.000010168949,0.0022869962,0.00005145989,0.74771655,0.00032754624,0.010770356,0.19941562],"study_design_scores_gemma":[0.00034134425,0.002852488,0.033856798,0.0006831714,0.0001644911,0.00002891314,0.0009648816,0.008200059,0.9145034,0.0010143913,0.036325336,0.00106474],"about_ca_topic_score_codex":0.00024646043,"about_ca_topic_score_gemma":0.000044150533,"teacher_disagreement_score":0.19835089,"about_ca_system_score_codex":0.00017637566,"about_ca_system_score_gemma":0.000031212956,"threshold_uncertainty_score":0.7708582},"labels":[],"label_agreement":null},{"id":"W4391745515","doi":"10.5194/amt-17-1023-2024","title":"Derivation of depolarization ratios of aerosol fluorescence and water vapor Raman backscatters from lidar measurements","year":2024,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","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":"European Regional Development Fund; Russian Science Foundation; Agence Nationale de la Recherche","keywords":"Depolarization ratio; Lidar; Laser-induced fluorescence; Fluorescence; Raman spectroscopy; Water vapor; Aerosol; Optics; Wavelength; Materials science; Analytical Chemistry (journal); Environmental science; Remote sensing; Chemistry; Physics; Meteorology; Geology","score_opus":0.01851152561177428,"score_gpt":0.22107858457855634,"score_spread":0.20256705896678207,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391745515","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":[0.88621,0.00049410167,0.1107885,0.00019109517,0.00014440338,0.00074439275,0.0000054623815,0.00022592186,0.0011961114],"genre_scores_gemma":[0.93103915,0.00008916135,0.068622254,0.0000794481,0.000028882949,0.000058869395,0.0000146289085,0.00003207641,0.00003554998],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9976633,0.00008760259,0.00056574674,0.00044837428,0.0009837548,0.0002511764],"domain_scores_gemma":[0.9993555,0.000020515134,0.00015163179,0.00032697673,0.000068046356,0.00007732228],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00059450686,0.00024132087,0.00027762057,0.0000015475863,0.000080946425,0.00004664328,0.00022385812,0.00011645637,0.00056727725],"category_scores_gemma":[0.000034254488,0.00018834956,0.000072830444,0.00025880538,0.00020924857,0.00034030725,0.0001382512,0.00010665176,0.000018300092],"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":[0.000020599735,0.00006700008,0.06805569,0.00006740424,0.000049849055,0.0000014227542,0.0004997801,0.000026350044,0.8917028,0.000014512546,0.00041623513,0.03907836],"study_design_scores_gemma":[0.0001584711,0.00016396111,0.018804904,0.00022329175,0.00007676718,0.0000015641476,0.00006830087,0.001195282,0.9783695,0.00025816215,0.0004403707,0.00023945037],"about_ca_topic_score_codex":0.001100699,"about_ca_topic_score_gemma":0.00005370835,"teacher_disagreement_score":0.08666668,"about_ca_system_score_codex":0.00018067994,"about_ca_system_score_gemma":0.000025350762,"threshold_uncertainty_score":0.76806724},"labels":[],"label_agreement":null},{"id":"W4392264168","doi":"","title":"Apport de la mesure lidar dans l'étude des aérosols et nuages stratosphériques polaires et de leurs perturbations climatiques","year":2023,"lang":"en","type":"dissertation","venue":"theses.fr (ABES)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Lidar; Polar; Environmental science; Atmospheric sciences; Remote sensing; Meteorology; Climatology; Geography; Geology; Physics; Astronomy","score_opus":0.02094915974814221,"score_gpt":0.32327849272015674,"score_spread":0.30232933297201453,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392264168","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":[0.82532686,0.00029515085,0.00060706824,0.0001461644,0.00009973025,0.00034944518,0.00008213447,0.0004487411,0.1726447],"genre_scores_gemma":[0.98729247,0.0027209283,0.004655932,0.00047291646,0.00009085727,0.00019665128,0.00044921174,0.00018186659,0.003939174],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99682707,0.00071940763,0.00049989426,0.0006359563,0.0005991305,0.00071856263],"domain_scores_gemma":[0.99837404,0.0005130535,0.00031807143,0.0005122465,0.00003232762,0.00025026107],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0015009722,0.00058038504,0.00049960247,0.000009775137,0.0003867019,0.0002863991,0.00070921984,0.00056555367,0.00088176044],"category_scores_gemma":[0.00030960343,0.0005236679,0.00025496254,0.00032693546,0.00041843415,0.00038840764,0.00014170296,0.0007060527,0.0001857748],"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":[0.00011552159,0.0007246117,0.4967839,0.00047708506,0.00038093803,0.00023007052,0.42099926,0.0020245465,0.042660348,0.02314244,0.006466894,0.0059943553],"study_design_scores_gemma":[0.00021392119,0.00015316697,0.9151686,0.0003917207,0.00015552626,0.00002880846,0.06288621,0.00017315571,0.0063379887,0.011018625,0.0026470742,0.000825217],"about_ca_topic_score_codex":0.016230257,"about_ca_topic_score_gemma":0.020724172,"teacher_disagreement_score":0.41838467,"about_ca_system_score_codex":0.00042436388,"about_ca_system_score_gemma":0.00029028644,"threshold_uncertainty_score":0.99972147},"labels":[],"label_agreement":null},{"id":"W4392582647","doi":"10.5194/egusphere-egu24-7997","title":"Impact of Hunga Tonga Hunga Ha&amp;#8217;apai eruption on the global stratospheric aerosol layer in comparison with other eruptions and extreme fire events of the past decade&amp;#160;","year":2024,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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; Layer (electronics); Environmental science; Atmospheric sciences; Climatology; Meteorology; Geology; Physics; Chemistry","score_opus":0.04413673908320208,"score_gpt":0.3036430159273445,"score_spread":0.2595062768441424,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392582647","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":[0.99079657,0.00022395438,0.00069948926,0.0004648468,0.00015221177,0.0010245903,0.00008660569,0.000040571806,0.006511164],"genre_scores_gemma":[0.99651986,0.000053671138,0.0016644388,0.000099429155,0.000043820677,0.00007931297,0.000011113269,0.000045104796,0.0014832448],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9971308,0.00024051552,0.0006863425,0.0007306514,0.0007763382,0.0004353706],"domain_scores_gemma":[0.99833125,0.00009217506,0.00045215493,0.0009766325,0.000025747362,0.000122030484],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003651695,0.0005384728,0.0005771864,0.0000033539638,0.0001465593,0.00006482735,0.0006871775,0.00029818882,0.0036217854],"category_scores_gemma":[0.000023566323,0.00027995085,0.00030034286,0.0006166245,0.0005178929,0.00007893529,0.0010666731,0.000854664,0.00011566001],"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":[0.000106609834,0.00046241152,0.96406054,0.0000690002,0.00015177162,7.2400957e-7,0.00071077776,0.029145887,0.0018192893,0.0001978466,0.0008432929,0.0024318579],"study_design_scores_gemma":[0.0004364486,0.00026106628,0.99391806,0.00051792985,0.00014779817,0.000009788369,0.00048554124,0.0021945145,0.00017202037,0.0010122831,0.00037883493,0.00046569135],"about_ca_topic_score_codex":0.0064883837,"about_ca_topic_score_gemma":0.01183458,"teacher_disagreement_score":0.029857552,"about_ca_system_score_codex":0.00050995575,"about_ca_system_score_gemma":0.000098592805,"threshold_uncertainty_score":0.99996525},"labels":[],"label_agreement":null},{"id":"W4392597730","doi":"10.5194/egusphere-egu24-2702","title":"Exploring the Influence of Turbulence on Droplet Size Growth and Precipitation in Warm Clouds","year":2024,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"University of Toronto","funders":"","keywords":"Turbulence; Precipitation; Atmospheric sciences; Environmental science; Meteorology; Mechanics; Climatology; Statistical physics; Physics; Geology","score_opus":0.02197221645640999,"score_gpt":0.23155929975009112,"score_spread":0.20958708329368114,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392597730","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":[0.9932063,0.00006130194,0.00002897947,0.00065478904,0.00019393174,0.00031492364,0.0000042372026,0.00003152606,0.0055040033],"genre_scores_gemma":[0.99805605,0.000504359,0.00084224617,0.00015543867,0.00002776103,0.000120172175,9.394951e-7,0.00001619217,0.00027682053],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9986721,0.000051791045,0.0002925859,0.0004668264,0.00033055924,0.00018610597],"domain_scores_gemma":[0.9993212,0.00022349846,0.000095569034,0.00030831207,0.000005997472,0.00004537762],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025197776,0.00019903913,0.0001906515,0.000002111078,0.00004128533,0.000037027803,0.00032076554,0.0000819056,0.0001486532],"category_scores_gemma":[0.000117052456,0.00013071751,0.000046004672,0.00019878605,0.00022987931,0.0000914926,0.001307439,0.00048297778,0.000050110833],"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":[0.00022773736,0.00042339155,0.2754023,0.0014398276,0.00010228691,0.000054624383,0.043596454,0.6072427,0.022099206,0.01112925,0.000912974,0.037369225],"study_design_scores_gemma":[0.00015377048,0.0001322898,0.97177166,0.0004677029,0.00002663999,0.0000024581038,0.0006018765,0.003721602,0.003289118,0.019394843,0.00008281568,0.0003552343],"about_ca_topic_score_codex":0.0021146203,"about_ca_topic_score_gemma":0.00012478138,"teacher_disagreement_score":0.69636935,"about_ca_system_score_codex":0.000085685424,"about_ca_system_score_gemma":0.000015853157,"threshold_uncertainty_score":0.53305054},"labels":[],"label_agreement":null},{"id":"W4392678013","doi":"10.48550/arxiv.2403.04840","title":"Atmospheric Waves Driving Variability and Cloud Modulation on a Planetary-Mass Object","year":2024,"lang":"en","type":"preprint","venue":"arXiv (Cornell University)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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":"Air Force Institute of Technology; Institut national des sciences de l'Univers; Centre National de la Recherche Scientifique; Science Mission Directorate; Ohio State University; National Aeronautics and Space Administration; U.S. Department of Defense; U.S. Air Force Academy; National Science Foundation","keywords":"Cloud computing; Object (grammar); Environmental science; Modulation (music); Atmospheric sciences; Meteorology; Physics; Computer science; Acoustics; Artificial intelligence","score_opus":0.019510720661592193,"score_gpt":0.16379311667593352,"score_spread":0.14428239601434134,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392678013","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":[0.9686787,0.000025546356,0.017251525,0.00005183791,0.0006766648,0.00031977243,0.000015674908,0.00014465378,0.012835598],"genre_scores_gemma":[0.99633235,0.0001022116,0.0013055074,0.00005722306,0.00014223398,0.0000012576047,0.000022274164,0.000030493287,0.002006429],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9979888,0.00013973496,0.00018932957,0.0012301231,0.00013032473,0.00032169023],"domain_scores_gemma":[0.998958,0.00012103027,0.00013245443,0.0006126742,0.0000081937,0.00016768443],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00027739478,0.0003624026,0.00030407653,0.0000021110134,0.0001647214,0.000070290924,0.00033597075,0.00031062373,0.0010185364],"category_scores_gemma":[0.000029711322,0.00037099104,0.00012708572,0.00029729612,0.00024438187,0.00009423619,0.00120375,0.0006310616,0.0003221246],"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":[0.000044628883,0.000059388458,0.14773665,0.00007375176,0.00006539664,0.00011772674,0.0002353475,0.84629315,0.00010217202,0.0035029834,0.0004097918,0.001359002],"study_design_scores_gemma":[0.00020121572,0.00008958495,0.12371631,0.00008756537,0.000120523466,0.0000030556885,0.00009364267,0.8225373,0.000015291267,0.0520877,0.0005403672,0.0005074433],"about_ca_topic_score_codex":0.00062759634,"about_ca_topic_score_gemma":0.00010145372,"teacher_disagreement_score":0.04858472,"about_ca_system_score_codex":0.00041305512,"about_ca_system_score_gemma":0.000033723765,"threshold_uncertainty_score":0.9998947},"labels":[],"label_agreement":null},{"id":"W4392759483","doi":"10.5194/egusphere-egu24-15182","title":"Using synthetic EarthCARE Cloud Profiling Radar data to develop validation methodologies for ground-based cloud radar sites","year":2024,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"","keywords":"Cloud computing; Profiling (computer programming); Radar; Remote sensing; Environmental science; Computer science; Meteorology; Geology; Geography; Telecommunications","score_opus":0.22280690583039128,"score_gpt":0.37374461089296707,"score_spread":0.15093770506257578,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392759483","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.4486245,0.00021380611,0.54542935,0.0008203935,0.0016961804,0.0017871256,0.00032015351,0.00033565966,0.00077284774],"genre_scores_gemma":[0.17727183,0.000013796913,0.8206275,0.00032729996,0.0003766369,0.00010139543,0.0006639127,0.000092287904,0.00052535476],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99604887,0.00030444516,0.00066111237,0.0017939353,0.00058129564,0.0006103311],"domain_scores_gemma":[0.9973394,0.000562265,0.00023149724,0.0016331829,0.00006370736,0.00016991823],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0020214762,0.00057200505,0.0005971181,0.000009633614,0.00030143652,0.00032387013,0.0014475394,0.00041463197,0.0009035038],"category_scores_gemma":[0.00096868625,0.0004923315,0.0001477395,0.0005249831,0.00018061954,0.00014283408,0.00631352,0.00050995086,0.00020128592],"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":[0.0010677201,0.000531846,0.018985203,0.0066519426,0.0012400595,0.00014005238,0.004927966,0.39808404,0.37154955,0.0079234,0.038319714,0.1505785],"study_design_scores_gemma":[0.0016493669,0.0006622652,0.0028332192,0.0019390666,0.0022686836,0.00006225992,0.008757312,0.45478836,0.3990369,0.065742806,0.054048352,0.0082113985],"about_ca_topic_score_codex":0.0011075021,"about_ca_topic_score_gemma":0.00014984119,"teacher_disagreement_score":0.27519816,"about_ca_system_score_codex":0.00047740628,"about_ca_system_score_gemma":0.00027414196,"threshold_uncertainty_score":0.9997528},"labels":[],"label_agreement":null},{"id":"W4392965491","doi":"10.5194/egusphere-2024-581","title":"CAECENET: An automatic system processing photometer and ceilometer data from different networks to provide columnar and vertically-resolved aerosol properties","year":2024,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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":"Agencia Estatal de Investigación; European Metrology Programme for Innovation and Research; Junta de Castilla y León; Ministerio de Ciencia e Innovación; European Commission","keywords":"Photometer; Aerosol; Ceilometer; Environmental science; Computer science; Remote sensing; Optics; Physics; Geology; Meteorology","score_opus":0.03294780099408761,"score_gpt":0.2460085686941719,"score_spread":0.21306076770008428,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392965491","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":[0.9884197,0.0010827162,0.0074639,0.00021024793,0.00027744492,0.0016681646,0.000068678644,0.00034151514,0.00046762452],"genre_scores_gemma":[0.98836577,0.000037605387,0.01004588,0.00036203678,0.00013978269,0.00029777782,0.00007348102,0.00008811614,0.0005895766],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9964949,0.00011421347,0.0005854175,0.0017563172,0.00050502364,0.0005441487],"domain_scores_gemma":[0.9981037,0.000042648968,0.00011467554,0.0012408245,0.000012697702,0.00048550314],"candidate_categories":["metaepi_narrow","open_science"],"consensus_categories":[],"category_scores_codex":[0.00023588611,0.0005826902,0.0006658321,0.0000059817894,0.00019489859,0.00097474863,0.0008180866,0.00031755175,0.00048214244],"category_scores_gemma":[0.000023585051,0.0004011808,0.000045663135,0.00012771218,0.00027376116,0.000225331,0.008869763,0.0005107964,0.00006792974],"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":[0.0009633373,0.0018528083,0.16172482,0.017070297,0.0017337318,0.0004218367,0.020784462,0.012712208,0.07870426,0.000043127475,0.01938588,0.6846032],"study_design_scores_gemma":[0.00023980666,0.0001653262,0.013435663,0.0011792658,0.00025909377,0.00000957444,0.0006186343,0.9827243,0.00037938255,0.000048181395,0.00020481076,0.00073597534],"about_ca_topic_score_codex":0.0021512099,"about_ca_topic_score_gemma":0.001253951,"teacher_disagreement_score":0.97001207,"about_ca_system_score_codex":0.00023896182,"about_ca_system_score_gemma":0.00003883479,"threshold_uncertainty_score":0.999844},"labels":[],"label_agreement":null},{"id":"W4393386538","doi":"10.1175/aies-d-23-0063.1","title":"Development of a Full-Scale Connected U-Net for Reflectivity Inpainting in Spaceborne Radar Blind Zones","year":2024,"lang":"en","type":"article","venue":"Artificial Intelligence for the Earth Systems","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":8,"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 Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada; European Centre for Medium-Range Weather Forecasts; Nuclear Safety and Security Commission; Microsoft; National Aeronautics and Space Administration; U.S. Department of Energy","keywords":"Snow; Environmental science; Remote sensing; Cloud height; Meteorology; Radar; Cloud cover; Computer science; Cloud computing; Geology; Geography","score_opus":0.05659008781572819,"score_gpt":0.30411594915631246,"score_spread":0.24752586134058427,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4393386538","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":[0.6177001,0.0002684585,0.37983882,0.00016440931,0.00058362674,0.0012163997,0.000013866868,0.00004006114,0.00017424772],"genre_scores_gemma":[0.981004,0.00000784527,0.018288594,0.000015480786,0.00013688786,0.0002537127,0.000005306128,0.000021761796,0.0002663927],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99840486,0.000056654513,0.00060979027,0.00035434432,0.00022320336,0.0003511639],"domain_scores_gemma":[0.9988767,0.0007339598,0.000121394616,0.00019418562,0.00002439734,0.000049377242],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014868445,0.00015864456,0.00024135964,0.000006329179,0.00021231169,0.000081898645,0.0002371548,0.000080808284,0.000098535806],"category_scores_gemma":[0.00013838575,0.00011567167,0.0000925657,0.00045804345,0.00014583484,0.00010566997,0.00007590855,0.00010566388,0.000068734866],"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":[0.0015990853,0.00064437214,0.005187137,0.0008526703,0.00025853192,0.000008951059,0.045420673,0.039003022,0.3588822,0.036479786,0.0011333026,0.5105303],"study_design_scores_gemma":[0.00036674555,0.00082725903,0.004089671,0.0009874697,0.00010030195,0.000024564859,0.028208455,0.73325753,0.15935594,0.0085066315,0.06316141,0.001113994],"about_ca_topic_score_codex":0.0006586256,"about_ca_topic_score_gemma":0.00840965,"teacher_disagreement_score":0.6942545,"about_ca_system_score_codex":0.00006975765,"about_ca_system_score_gemma":0.00005032411,"threshold_uncertainty_score":0.47169536},"labels":[],"label_agreement":null},{"id":"W4393564125","doi":"10.5281/zenodo.8187942","title":"A Parsec-Scale Galactic 3D Dust Map out to 1.25 kpc from the Sun -- Dataset for the 1.25 kpc 3D Dust Map and the 2 kpc 3D Dust Map","year":2023,"lang":"en","type":"dataset","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"University of Toronto","funders":"","keywords":"Parsec; Scale (ratio); Astrophysics; Environmental science; Astronomy; Physics; Geography; Cartography; Galaxy","score_opus":0.02912610982417089,"score_gpt":0.24703019418121716,"score_spread":0.21790408435704628,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4393564125","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0003050799,0.00030467592,0.0010607074,0.011877879,0.0008408983,0.0029892167,0.9807019,0.00032015363,0.001599456],"genre_scores_gemma":[0.0012019675,0.0007565343,0.00043619671,0.0031428717,0.0010846583,0.000007563916,0.98049027,0.0018387885,0.011041157],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9949105,0.0008295269,0.0006629951,0.0013395979,0.0012136587,0.0010437696],"domain_scores_gemma":[0.9959864,0.0006048371,0.00040329425,0.0024769856,0.000118595184,0.0004099142],"candidate_categories":["metaepi_narrow","sts","scholarly_communication","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.002043417,0.0006287389,0.000525035,0.000020133688,0.004712786,0.001812727,0.0043516043,0.00029937795,0.0377501],"category_scores_gemma":[0.0009105507,0.0003967533,0.00014880461,0.00063153193,0.001370846,0.0003196005,0.0072564823,0.0011625049,0.07810468],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022770368,0.00011187272,0.000017089875,0.00007650477,0.00013632693,0.000024457608,0.0008125984,0.00010447147,0.000032154436,0.000026649446,0.99101967,0.0074105063],"study_design_scores_gemma":[0.0010803066,0.0001981696,0.0010168975,0.000076083255,0.00023823777,0.000025859195,0.0012433267,0.0010415015,0.0000064764936,0.00005128494,0.99451387,0.0005079717],"about_ca_topic_score_codex":0.0027754616,"about_ca_topic_score_gemma":0.00032170804,"teacher_disagreement_score":0.040354583,"about_ca_system_score_codex":0.00033708665,"about_ca_system_score_gemma":0.000016541784,"threshold_uncertainty_score":0.9998484},"labels":[],"label_agreement":null},{"id":"W4393700206","doi":"10.5281/zenodo.4337092","title":"Data archive for the peer-reviewed journal article \"Detailed characterization of the CAPS single scattering albedo monitor (CAPS PMssa) as a field-deployable instrument for measuring aerosol light absorption with the extinction-minus-scattering method\"","year":2020,"lang":"en","type":"dataset","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"National Research Council Canada","funders":"","keywords":"Single-scattering albedo; Extinction (optical mineralogy); Characterization (materials science); Aerosol; Scattering; Albedo (alchemy); Absorption (acoustics); Remote sensing; Field (mathematics); Environmental science; Physics; Optics; Geography; Meteorology; History","score_opus":0.043070815126184075,"score_gpt":0.2464413098036952,"score_spread":0.20337049467751112,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4393700206","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.06113236,0.0001906333,0.3260434,0.04856795,0.0017970845,0.011968807,0.54891217,0.00040935996,0.0009782568],"genre_scores_gemma":[0.13997647,0.0012888819,0.014215258,0.0054267473,0.0046601626,0.000039183913,0.8265375,0.0046913093,0.00316452],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.997662,0.00036062594,0.00042931706,0.00050491333,0.0006817945,0.00036134446],"domain_scores_gemma":[0.99803096,0.00012958764,0.0005783402,0.0009751518,0.00017086392,0.000115116774],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012651132,0.00024436787,0.00024875219,0.000009904056,0.0026495606,0.0006822503,0.0022334154,0.00007397194,0.0021419274],"category_scores_gemma":[0.0006565469,0.00014707127,0.00010446962,0.0003213145,0.00017288656,0.00033572514,0.0020358127,0.00041895942,0.00034233776],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020066218,0.00009693161,0.000010154838,0.00015885563,0.00011626324,0.0000013107272,0.00055013923,0.0003132874,0.12757824,0.0000026092675,0.8473235,0.023648072],"study_design_scores_gemma":[0.00042672176,0.0003408385,0.00029831362,0.00012996916,0.00016377788,0.00005827192,0.00033848517,0.0013395464,0.0057712444,0.000016973734,0.99092317,0.00019270879],"about_ca_topic_score_codex":0.00006694611,"about_ca_topic_score_gemma":0.000018980207,"teacher_disagreement_score":0.31182814,"about_ca_system_score_codex":0.00019565508,"about_ca_system_score_gemma":0.000009894399,"threshold_uncertainty_score":0.99877024},"labels":[],"label_agreement":null},{"id":"W4393703129","doi":"10.5281/zenodo.8187943","title":"A Parsec-Scale Galactic 3D Dust Map out to 1.25 kpc from the Sun -- Dataset for the 1.25 kpc 3D Dust Map and the 2 kpc 3D Dust Map","year":2023,"lang":"en","type":"dataset","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"University of Toronto","funders":"","keywords":"Astrophysics; Parsec; Scale (ratio); Dust lane; Physics; Astronomy; Mineral dust; Galaxy; Star formation; Meteorology; Aerosol","score_opus":0.02912610982417089,"score_gpt":0.24703019418121716,"score_spread":0.21790408435704628,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4393703129","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0003050799,0.00030467592,0.0010607074,0.011877879,0.0008408983,0.0029892167,0.9807019,0.00032015363,0.001599456],"genre_scores_gemma":[0.0012019675,0.0007565343,0.00043619671,0.0031428717,0.0010846583,0.000007563916,0.98049027,0.0018387885,0.011041157],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9949105,0.0008295269,0.0006629951,0.0013395979,0.0012136587,0.0010437696],"domain_scores_gemma":[0.9959864,0.0006048371,0.00040329425,0.0024769856,0.000118595184,0.0004099142],"candidate_categories":["metaepi_narrow","sts","scholarly_communication","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.002043417,0.0006287389,0.000525035,0.000020133688,0.004712786,0.001812727,0.0043516043,0.00029937795,0.0377501],"category_scores_gemma":[0.0009105507,0.0003967533,0.00014880461,0.00063153193,0.001370846,0.0003196005,0.0072564823,0.0011625049,0.07810468],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022770368,0.00011187272,0.000017089875,0.00007650477,0.00013632693,0.000024457608,0.0008125984,0.00010447147,0.000032154436,0.000026649446,0.99101967,0.0074105063],"study_design_scores_gemma":[0.0010803066,0.0001981696,0.0010168975,0.000076083255,0.00023823777,0.000025859195,0.0012433267,0.0010415015,0.0000064764936,0.00005128494,0.99451387,0.0005079717],"about_ca_topic_score_codex":0.0027754616,"about_ca_topic_score_gemma":0.00032170804,"teacher_disagreement_score":0.040354583,"about_ca_system_score_codex":0.00033708665,"about_ca_system_score_gemma":0.000016541784,"threshold_uncertainty_score":0.9998484},"labels":[],"label_agreement":null},{"id":"W4393873853","doi":"10.5281/zenodo.3373929","title":"The wavelength-dependent complex refractive index of hygroscopic aerosol particles and other aqueous media: an effective oscillator model","year":2019,"lang":"en","type":"dataset","venue":"Figshare","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"","keywords":"Aerosol; Refractive index; Wavelength; Aqueous solution; Index (typography); Materials science; Aqueous medium; Chemistry; Optoelectronics; Physics; Meteorology; Physical chemistry; Computer science","score_opus":0.030012715700219333,"score_gpt":0.26746277316358064,"score_spread":0.2374500574633613,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4393873853","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.01317415,0.00015017577,0.000002511564,0.000014634164,0.000057397105,0.00075648533,0.9856853,0.000016254282,0.00014310495],"genre_scores_gemma":[0.13193053,0.000031538148,0.000050212166,0.0002156092,0.00006921756,0.00024462852,0.86734164,0.00003786409,0.000078772224],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.998155,0.00010917817,0.0002865304,0.0005455814,0.0005313648,0.0003723425],"domain_scores_gemma":[0.9983661,0.00037979067,0.00036675297,0.000707363,0.000022888798,0.00015706701],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000100425634,0.00034048848,0.00038917203,0.0000022810225,0.0002085005,0.00006415462,0.00054970494,0.0002949134,0.03255367],"category_scores_gemma":[0.00025444728,0.00023505207,0.00006707905,0.00009087348,0.00012389064,0.00013402654,0.0005863849,0.00037920242,0.001030166],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000041942214,0.00006449364,0.00017157367,0.000064472064,0.00003420492,0.000004420749,0.00017529177,0.0005810224,0.00012647649,4.4510836e-7,0.99476045,0.0039752224],"study_design_scores_gemma":[0.0014189393,0.00068009825,0.014652719,0.00084627414,0.00013177904,0.000020648447,0.0005509215,0.0487682,0.0010416119,0.00020182466,0.9303693,0.0013176893],"about_ca_topic_score_codex":0.00038534385,"about_ca_topic_score_gemma":0.00096395,"teacher_disagreement_score":0.11875638,"about_ca_system_score_codex":0.00013939267,"about_ca_system_score_gemma":0.000034323915,"threshold_uncertainty_score":0.99974763},"labels":[],"label_agreement":null},{"id":"W4394027951","doi":"10.5281/zenodo.8212070","title":"A Parsec-Scale Galactic 3D Dust Map out to 1.25 kpc from the Sun -- Dataset for the 1.25 kpc 3D Dust Map and the 2 kpc 3D Dust Map","year":2023,"lang":"en","type":"dataset","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"University of Toronto","funders":"","keywords":"Parsec; Scale (ratio); Astrophysics; Physics; Astronomy; Galaxy","score_opus":0.02912610982417089,"score_gpt":0.24703019418121716,"score_spread":0.21790408435704628,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4394027951","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0003050799,0.00030467592,0.0010607074,0.011877879,0.0008408983,0.0029892167,0.9807019,0.00032015363,0.001599456],"genre_scores_gemma":[0.0012019675,0.0007565343,0.00043619671,0.0031428717,0.0010846583,0.000007563916,0.98049027,0.0018387885,0.011041157],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9949105,0.0008295269,0.0006629951,0.0013395979,0.0012136587,0.0010437696],"domain_scores_gemma":[0.9959864,0.0006048371,0.00040329425,0.0024769856,0.000118595184,0.0004099142],"candidate_categories":["metaepi_narrow","sts","scholarly_communication","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.002043417,0.0006287389,0.000525035,0.000020133688,0.004712786,0.001812727,0.0043516043,0.00029937795,0.0377501],"category_scores_gemma":[0.0009105507,0.0003967533,0.00014880461,0.00063153193,0.001370846,0.0003196005,0.0072564823,0.0011625049,0.07810468],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022770368,0.00011187272,0.000017089875,0.00007650477,0.00013632693,0.000024457608,0.0008125984,0.00010447147,0.000032154436,0.000026649446,0.99101967,0.0074105063],"study_design_scores_gemma":[0.0010803066,0.0001981696,0.0010168975,0.000076083255,0.00023823777,0.000025859195,0.0012433267,0.0010415015,0.0000064764936,0.00005128494,0.99451387,0.0005079717],"about_ca_topic_score_codex":0.0027754616,"about_ca_topic_score_gemma":0.00032170804,"teacher_disagreement_score":0.040354583,"about_ca_system_score_codex":0.00033708665,"about_ca_system_score_gemma":0.000016541784,"threshold_uncertainty_score":0.9998484},"labels":[],"label_agreement":null},{"id":"W4394057048","doi":"10.5281/zenodo.3373928","title":"The wavelength-dependent complex refractive index of hygroscopic aerosol particles and other aqueous media: an effective oscillator model","year":2019,"lang":"en","type":"dataset","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"","keywords":"Aerosol; Refractive index; Wavelength; Aqueous solution; Index (typography); Aqueous medium; Materials science; Chemistry; Meteorology; Physics; Optoelectronics; Computer science; Physical chemistry","score_opus":0.028668224292114415,"score_gpt":0.25366624286794615,"score_spread":0.22499801857583174,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4394057048","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.1873888,0.0001670619,0.001075208,0.00020731724,0.00020602516,0.0023631714,0.8028737,0.00022230536,0.0054964754],"genre_scores_gemma":[0.80210614,0.00043995565,0.0002152848,0.00029539486,0.00013915267,6.831335e-7,0.19523038,0.0012213478,0.00035167954],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9978585,0.00036006395,0.00028490444,0.0005361359,0.0005914179,0.00036895103],"domain_scores_gemma":[0.9986802,0.00009356133,0.0002681708,0.00069992663,0.00007735906,0.00018078415],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00053190615,0.0002335566,0.0002619528,0.000008026694,0.0012656705,0.00028263152,0.000981121,0.00014807157,0.005120718],"category_scores_gemma":[0.0002696493,0.00018181089,0.000041829833,0.00018720007,0.000630037,0.00016513951,0.00169599,0.00038965675,0.0019986737],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001552868,0.00017669945,0.000031658317,0.00005011389,0.00006295404,0.000004900857,0.00083304977,0.0007852264,0.0021578274,0.000040366165,0.95029944,0.045402497],"study_design_scores_gemma":[0.0005333939,0.00041607977,0.0012282782,0.000027362357,0.00004007131,0.000023803655,0.00043972686,0.009536424,0.00023274493,0.00012280357,0.98711807,0.0002812413],"about_ca_topic_score_codex":0.0002508854,"about_ca_topic_score_gemma":0.000023166702,"teacher_disagreement_score":0.61471736,"about_ca_system_score_codex":0.00020215297,"about_ca_system_score_gemma":0.0000040171476,"threshold_uncertainty_score":0.9987784},"labels":[],"label_agreement":null},{"id":"W4394520536","doi":"10.6084/m9.figshare.17056145","title":"Contrasting Stratospheric Smoke Mass and Lifetime from 2017 Canadian and 2019/2020 Australian Megafires: Global Simulations and Satellite Observations","year":2021,"lang":"en","type":"dataset","venue":"Figshare","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"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":"Satellite; Smoke; Environmental science; Meteorology; Atmospheric sciences; Climatology; Geography; Geology; Physics; Astronomy","score_opus":0.03144376709048015,"score_gpt":0.24910749724202505,"score_spread":0.2176637301515449,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4394520536","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.007031051,0.0018378155,3.9187051e-7,0.0002769738,0.000052620002,0.00025604002,0.9903935,0.000017944125,0.00013362021],"genre_scores_gemma":[0.0064899246,0.00026608142,0.00054492103,0.00037289772,0.00011007997,0.00002365439,0.99193394,0.000015997637,0.00024251243],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99844354,0.000045523964,0.00027042502,0.0006265979,0.00021673752,0.0003972013],"domain_scores_gemma":[0.9987953,0.0001295012,0.00015727509,0.00033835648,0.000019310919,0.0005602903],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00002862847,0.00033446884,0.00030764082,0.0000015561681,0.0003849779,0.0003273937,0.0002121396,0.00033713947,0.08692168],"category_scores_gemma":[0.00023948844,0.00035187375,0.00003520872,0.00020218683,0.00006837571,0.00020889267,0.00021736398,0.0002582325,0.00018002208],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000013767213,0.00000712017,0.013355424,0.000032824762,0.00003176596,0.000060782062,0.000019626059,0.000098229204,0.000008855951,3.0914347e-7,0.9858112,0.0005725084],"study_design_scores_gemma":[0.00013627658,0.000014468066,0.3311129,0.00028528855,0.000048544403,0.0000070502065,0.000055997116,0.00034962493,6.8965494e-7,0.000021808777,0.6676761,0.00029130638],"about_ca_topic_score_codex":0.12602599,"about_ca_topic_score_gemma":0.2252643,"teacher_disagreement_score":0.3181351,"about_ca_system_score_codex":0.00014660369,"about_ca_system_score_gemma":0.0001348885,"threshold_uncertainty_score":0.9998933},"labels":[],"label_agreement":null},{"id":"W4394857060","doi":"10.5194/egusphere-2024-581-ec1","title":"Comment on egusphere-2024-581","year":2024,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Agencia Estatal de Investigación; European Metrology Programme for Innovation and Research; Junta de Castilla y León; Ministerio de Ciencia e Innovación; European Commission","keywords":"Ceilometer; Aerosol; Sky; Radiance; Environmental science; Meteorology; Remote sensing; Range (aeronautics); Event (particle physics); Sun photometer; Angstrom; Geography; Physics; Astrophysics; Materials science; Chemistry","score_opus":0.01886285670912351,"score_gpt":0.2737386486588328,"score_spread":0.2548757919497093,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4394857060","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000006499314,0.008653587,0.0001056464,0.28159314,0.0038186172,0.00043563696,0.000058755293,0.00011166892,0.70521647],"genre_scores_gemma":[0.000044347704,0.0033435745,0.00082916534,0.13310012,0.00026117286,0.00008718157,0.00010195436,0.000057242134,0.8621752],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9976462,0.000045046505,0.00037113845,0.0007343882,0.000805257,0.0003979659],"domain_scores_gemma":[0.9989852,0.000046475154,0.00009598816,0.00069312303,0.0000059338804,0.00017331803],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00024362394,0.00045062441,0.00050393795,8.552945e-7,0.00008174481,0.000046106692,0.00048392877,0.00022953894,0.46815813],"category_scores_gemma":[0.00001627007,0.00031649356,0.00027633464,0.00024513775,0.00009277158,0.00003095836,0.00058969995,0.00060726,0.053793717],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000018681416,0.0000541924,0.000018967841,0.00045967186,0.000028452892,0.000022189699,0.000012244036,0.000016488933,6.5547357e-7,0.00030831737,0.9768967,0.02218023],"study_design_scores_gemma":[0.00005974052,0.00010983784,0.000042147647,0.0011019115,0.00011076878,0.000004256836,0.000014025243,0.000061033617,0.0000054544003,0.000195167,0.997897,0.00039863016],"about_ca_topic_score_codex":0.0014091715,"about_ca_topic_score_gemma":0.00040668255,"teacher_disagreement_score":0.4143644,"about_ca_system_score_codex":0.00044555767,"about_ca_system_score_gemma":0.000024873205,"threshold_uncertainty_score":0.9999287},"labels":[],"label_agreement":null},{"id":"W4394914715","doi":"10.1175/jas-d-20-0257.1","title":"CORRIGENDUM","year":2024,"lang":"en","type":"erratum","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Physics","score_opus":0.01573230554017244,"score_gpt":0.24001272760571074,"score_spread":0.2242804220655383,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4394914715","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.040304538,0.013875123,0.00011654513,0.007266322,0.4026956,0.00033879664,0.000007833513,0.00005639732,0.5353388],"genre_scores_gemma":[0.017649235,0.0008812539,0.0045418064,0.001438247,0.0029537152,0.0000036483536,4.2179943e-7,0.00005243641,0.9724792],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9967023,0.00009796953,0.00064721593,0.0003652478,0.0017413888,0.0004458645],"domain_scores_gemma":[0.99839425,0.000037762125,0.0009948476,0.00039438048,0.000028046545,0.00015072728],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009845594,0.0003230797,0.00044619877,7.2301776e-7,0.00041858238,0.00021774757,0.002875722,0.00024932463,0.005060306],"category_scores_gemma":[0.00012760489,0.0001622697,0.0005512565,0.0013823204,0.0013183306,0.00025376232,0.00083303876,0.0012554284,0.0006310354],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000035364458,0.000024902645,0.0019567688,0.000012440665,0.000029772269,0.000029237264,0.00015161456,0.0011938404,0.000040768573,0.00003395689,0.99426186,0.0022612961],"study_design_scores_gemma":[0.00006326062,0.00019826226,0.0029578556,0.00022468263,0.0001246494,0.00023799967,0.00024045481,0.0038934096,0.000013731474,0.0021060253,0.98969436,0.00024531517],"about_ca_topic_score_codex":0.00015962361,"about_ca_topic_score_gemma":0.000043052103,"teacher_disagreement_score":0.4371404,"about_ca_system_score_codex":0.00031794724,"about_ca_system_score_gemma":0.0003953464,"threshold_uncertainty_score":0.9958492},"labels":[],"label_agreement":null},{"id":"W4394934142","doi":"10.1029/2023jd040540","title":"Contributions From Cloud Morphological Changes to the Interannual Shortwave Cloud Feedback Based on MODIS and ISCCP Satellite Observations","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Lawrence Livermore National Laboratory; Jet Propulsion Laboratory; Nuclear Safety and Security Commission; California Institute of Technology; National Aeronautics and Space Administration; U.S. Department of Energy","keywords":"Cloud computing; International Satellite Cloud Climatology Project; Cloud feedback; Shortwave; Environmental science; Cloud forcing; Cloud height; Climatology; Global warming; Liquid water content; Cloud albedo; Climate model; Cloud cover; Cloud top; Cloud fraction; Climate change; Atmospheric sciences; Satellite; Radiative transfer; Meteorology; Computer science; Climate sensitivity; Geography; Geology; Physics; Oceanography","score_opus":0.04109883057254648,"score_gpt":0.31855117380836706,"score_spread":0.2774523432358206,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4394934142","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":[0.96326697,0.00057069195,0.0030685903,0.031375322,0.00039224708,0.0003064949,0.00010515188,0.00002370301,0.0008908329],"genre_scores_gemma":[0.99476457,0.00020764979,0.001543475,0.0011859926,0.001247685,0.000025108871,0.0000068270947,0.000021567876,0.0009971091],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9971294,0.0003769309,0.00035337682,0.00037918318,0.0012134701,0.0005476469],"domain_scores_gemma":[0.9973852,0.001680251,0.000069557966,0.00030988,0.00012451419,0.00043057307],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00095328386,0.000204604,0.00030159042,0.0000031534944,0.00037242653,0.00029731408,0.0005544959,0.00010732663,0.0014567843],"category_scores_gemma":[0.00059657596,0.00011807405,0.00016475706,0.00070076005,0.0005508773,0.00016389642,0.0003543714,0.0010423865,0.00045084686],"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":[0.0033310151,0.0023102928,0.03158933,0.00006411713,0.00062728423,0.0014536482,0.005727228,0.021465996,0.046922177,0.0118768355,0.57857466,0.2960574],"study_design_scores_gemma":[0.0010437608,0.0048784954,0.49379832,0.00048010147,0.0001133496,0.000033747816,0.0022918624,0.06842133,0.0018664406,0.01569301,0.4107894,0.00059019204],"about_ca_topic_score_codex":0.0009665764,"about_ca_topic_score_gemma":0.0004273178,"teacher_disagreement_score":0.462209,"about_ca_system_score_codex":0.00025106105,"about_ca_system_score_gemma":0.000072389535,"threshold_uncertainty_score":0.99945605},"labels":[],"label_agreement":null},{"id":"W4395012991","doi":"10.1029/2023jd039908","title":"Local and Regional Diurnal Variability of Aerosol Properties Retrieved by DSCOVR/EPIC UV Algorithm","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":6,"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":"EPIC; Aerosol; Environmental science; Diurnal temperature variation; Algorithm; Meteorology; Atmospheric sciences; Computer science; Geography; Physics","score_opus":0.024352256017455918,"score_gpt":0.2841055047301574,"score_spread":0.25975324871270145,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4395012991","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":[0.98025477,0.001986515,0.015587944,0.0010182083,0.00012260246,0.00018990209,0.000009357191,0.000015609181,0.0008151209],"genre_scores_gemma":[0.99386394,0.00039352657,0.003962372,0.00004498269,0.0001906687,0.0000062227496,9.089592e-7,0.000025696285,0.001511706],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99613255,0.00040885247,0.00063555414,0.00037460684,0.0019019896,0.00054642855],"domain_scores_gemma":[0.99843615,0.0006049482,0.00015429713,0.00024559244,0.00015837747,0.00040062654],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0017784085,0.00020754295,0.00043591004,0.000001952545,0.00018265353,0.00012941669,0.00047146654,0.00013180109,0.0011797445],"category_scores_gemma":[0.00036527385,0.00013945706,0.00019656305,0.00062361103,0.0020155874,0.00047666937,0.0003766188,0.0010507036,0.00005735854],"study_design_candidate":"design_other","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":[0.0020405245,0.002701759,0.042122897,0.0006007584,0.0006798923,0.00043445054,0.0022670887,0.0006842286,0.23609613,0.0015507116,0.15906435,0.5517572],"study_design_scores_gemma":[0.007698048,0.024489254,0.29569486,0.0039540157,0.0005102236,0.0011811336,0.0077909436,0.31294706,0.14502735,0.08519391,0.112152815,0.0033603923],"about_ca_topic_score_codex":0.0008667,"about_ca_topic_score_gemma":0.000014672546,"teacher_disagreement_score":0.5483968,"about_ca_system_score_codex":0.00026164736,"about_ca_system_score_gemma":0.00020480256,"threshold_uncertainty_score":0.9997333},"labels":[],"label_agreement":null},{"id":"W4395109583","doi":"10.21203/rs.3.rs-4019064/v1","title":"Ground radiative measurements reveal negative longwave cloud feedback","year":2024,"lang":"en","type":"preprint","venue":"Research Square","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"McGill University; Princeton University","keywords":"Longwave; Cloud feedback; Environmental science; Cloud forcing; Radiative forcing; Climate model; Radiative transfer; Radiance; Atmospheric sciences; Climate change; Downwelling; Cloud computing; Climatology; Meteorology; Remote sensing; Climate sensitivity; Physics; Computer science; Geography; Geology; Aerosol","score_opus":0.08538690411185124,"score_gpt":0.36415066798577617,"score_spread":0.27876376387392493,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4395109583","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":[0.8106199,0.0018261712,0.00024660726,0.0018605939,0.0016723252,0.0030631605,0.00021343332,0.00021894161,0.18027885],"genre_scores_gemma":[0.97730017,0.00019915096,0.001289552,0.00009137351,0.00080960523,0.00035252993,0.000053178075,0.00010937287,0.019795058],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9926654,0.000867607,0.00047982918,0.0015090709,0.0032488275,0.0012292461],"domain_scores_gemma":[0.9979482,0.00029186776,0.00014717896,0.0009894589,0.00014155977,0.0004816975],"candidate_categories":["metaepi_narrow","research_integrity","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0023970967,0.00051835575,0.00051378645,0.000014855724,0.0004455137,0.00038820834,0.001061922,0.0005044503,0.0061073927],"category_scores_gemma":[0.0003971121,0.00045238854,0.00030345737,0.0008681179,0.0009695138,0.0001211228,0.006764952,0.0033091162,0.008954036],"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":[0.0007554414,0.0014019255,0.11308277,0.0034537106,0.0014661347,0.0010258924,0.033513796,0.014364156,0.0027909796,0.001559479,0.7644045,0.062181216],"study_design_scores_gemma":[0.0030204875,0.0022002477,0.6100703,0.005618377,0.00033060412,0.000040060862,0.014180092,0.0096712345,0.004741958,0.305549,0.039766133,0.004811509],"about_ca_topic_score_codex":0.004280265,"about_ca_topic_score_gemma":0.0004556748,"teacher_disagreement_score":0.7246384,"about_ca_system_score_codex":0.0026769175,"about_ca_system_score_gemma":0.00027623732,"threshold_uncertainty_score":0.9997928},"labels":[],"label_agreement":null},{"id":"W4395699045","doi":"10.1007/978-3-031-53618-2_30","title":"Scientific Challenges for Lidar-Based Dust and Ice Cloud Characterization on Mars","year":2024,"lang":"en","type":"book-chapter","venue":"Springer aerospace technology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Mars Exploration Program; Lidar; Martian; Remote sensing; Astrobiology; Environmental science; Atmosphere of Mars; Atmospheric sciences; Geology; Physics","score_opus":0.014529589369431432,"score_gpt":0.2184974599008539,"score_spread":0.20396787053142246,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4395699045","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.45777172,0.00820715,0.0046258196,0.04919272,0.008643808,0.005884495,0.00045976727,0.0039097047,0.46130484],"genre_scores_gemma":[0.24163102,0.0009944703,0.002839131,0.0003082751,0.00031789954,0.00023800686,0.00008314157,0.0002958523,0.7532922],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.99773836,0.000005741631,0.0002704688,0.0012220948,0.00030390188,0.0004594465],"domain_scores_gemma":[0.99892026,0.0000417516,0.00020199559,0.0007132246,0.000024382358,0.000098358214],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021753997,0.00048204287,0.00041609124,0.00003170612,0.00026251335,0.00011812296,0.00038522307,0.000888885,0.0005906454],"category_scores_gemma":[0.000025660664,0.00046608647,0.000115470655,0.00013130653,0.0010329639,0.00006857838,0.00039841118,0.0005274386,0.000804728],"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":[0.00020157025,0.00020883711,0.002264556,0.0007955442,0.00021901027,0.0001020047,0.0004342217,0.00007713959,0.051103815,0.7543492,0.004208945,0.18603522],"study_design_scores_gemma":[0.00040981942,0.0004907982,0.001380099,0.00036103718,0.000121350306,0.000010592903,0.00005851986,0.00034730643,0.002645306,0.016255947,0.97704935,0.00086989754],"about_ca_topic_score_codex":0.0000056025556,"about_ca_topic_score_gemma":0.00006864618,"teacher_disagreement_score":0.97284037,"about_ca_system_score_codex":0.00022129343,"about_ca_system_score_gemma":0.000027093956,"threshold_uncertainty_score":0.99997324},"labels":[],"label_agreement":null},{"id":"W4396223708","doi":"10.1007/s41748-024-00398-w","title":"A Comprehensive Machine and Deep Learning Approach for Aerosol Optical Depth Forecasting: New Evidence from the Arabian Peninsula","year":2024,"lang":"en","type":"article","venue":"Earth Systems and Environment","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":13,"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 Toronto","funders":"Qatar National Library; Qatar National Research Fund; Qatar University; Fonds National de la Recherche Luxembourg; Qatar Foundation","keywords":"Peninsula; Aerosol; Artificial intelligence; Deep learning; Meteorology; Computer science; Geology; Climatology; History; Geography; Archaeology","score_opus":0.03522510705998537,"score_gpt":0.2239608526726299,"score_spread":0.18873574561264456,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4396223708","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":[0.8288847,0.026008034,0.14275879,0.0004331523,0.0001494561,0.00093321217,0.000007911953,0.00005219988,0.0007725437],"genre_scores_gemma":[0.9862679,0.00085249037,0.010965997,0.00006916003,0.00017673004,0.000068860485,0.000011370989,0.000025933954,0.0015615298],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9986252,0.0000616974,0.000229545,0.00053271884,0.00026019488,0.00029062887],"domain_scores_gemma":[0.99929017,0.00028364235,0.000053382144,0.00018597904,0.0000015015323,0.00018533858],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019357883,0.00021255699,0.00021636476,0.00000134814,0.0002889928,0.00019107442,0.00012002978,0.0000739015,0.00013489513],"category_scores_gemma":[0.000019168012,0.00013991931,0.00005195864,0.000049495375,0.00020659699,0.00012849909,0.00021683378,0.00019724564,0.00004168506],"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":[0.00021136034,0.00013927835,0.32005695,0.0004349595,0.00030622032,0.00006616012,0.012990422,0.21467383,0.012226393,0.00040426,0.0020792154,0.43641096],"study_design_scores_gemma":[0.0004444158,0.00031572682,0.08939651,0.00016288215,0.00008768915,0.00007993932,0.0012358512,0.858895,0.00006886291,0.000041274252,0.048907686,0.0003641445],"about_ca_topic_score_codex":0.0011598605,"about_ca_topic_score_gemma":0.000043641176,"teacher_disagreement_score":0.6442212,"about_ca_system_score_codex":0.00003686691,"about_ca_system_score_gemma":0.0000055583814,"threshold_uncertainty_score":0.5705744},"labels":[],"label_agreement":null},{"id":"W4396561900","doi":"10.3390/atmos15050564","title":"Wide and Deep Learning Model for Satellite-Based Real-Time Aerosol Retrievals in China","year":2024,"lang":"en","type":"article","venue":"Atmosphere","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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 Toronto","funders":"Natural Science Foundation of Beijing Municipality; National Natural Science Foundation of China","keywords":"Interpretability; Geostationary orbit; Deep blue; Aerosol; Deep learning; Satellite; Environmental science; Remote sensing; Mean squared error; Gradient boosting; Meteorology; Computer science; Artificial intelligence; Geology; Mathematics; Geography; Statistics; Random forest","score_opus":0.006569664434663874,"score_gpt":0.223596976021004,"score_spread":0.21702731158634014,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4396561900","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":[0.9713988,0.0011422323,0.017462026,0.00034396446,0.00005583151,0.00039494704,0.000003196348,0.00015795809,0.009041047],"genre_scores_gemma":[0.9681045,0.0003969688,0.022706658,0.00013683825,0.000027486109,0.000045912784,0.000009377489,0.000051229734,0.008521023],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9986132,0.000038557522,0.0002481157,0.00050397444,0.0002032131,0.000392945],"domain_scores_gemma":[0.99948037,0.0001671863,0.00004540155,0.00018690586,0.000004664735,0.00011544565],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00029673704,0.000207088,0.00021812045,3.769973e-7,0.0001245759,0.00008609896,0.00014394788,0.00012998014,0.0011181874],"category_scores_gemma":[0.000059354854,0.00018614519,0.00007614306,0.00027706995,0.00012464583,0.00017978846,0.000089292706,0.00019213272,0.00019681828],"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":[0.000199,0.00011015762,0.24739477,0.0001843969,0.000033159187,0.00005981343,0.0025373735,0.5958711,0.011403647,0.00035669838,0.0018721557,0.13997774],"study_design_scores_gemma":[0.00037110856,0.00011265035,0.01808198,0.00006076242,0.000018826717,0.0000022257789,0.00007086932,0.97777677,0.000344527,0.000739727,0.0021581165,0.0002624399],"about_ca_topic_score_codex":0.00032576534,"about_ca_topic_score_gemma":0.00015805798,"teacher_disagreement_score":0.38190567,"about_ca_system_score_codex":0.00014358616,"about_ca_system_score_gemma":0.00002427661,"threshold_uncertainty_score":0.9997949},"labels":[],"label_agreement":null},{"id":"W4396685249","doi":"10.5194/acp-24-5235-2024","title":"Technical note: Characterization of a single-beam gradient force aerosol optical tweezer for droplet trapping, phase transition monitoring, and morphology studies","year":2024,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Key Research and Development Program of Zhejiang Province; Fundamental Research Funds for the Central Universities; National Natural Science Foundation of China","keywords":"Aerosol; Optical tweezers; Particle (ecology); Chemistry; Raman spectroscopy; Trapping; Analytical Chemistry (journal); Mie scattering; Phase (matter); Optics; Materials science; Scattering; Molecular physics; Light scattering; Chromatography","score_opus":0.014334503119503074,"score_gpt":0.26467034980051374,"score_spread":0.25033584668101067,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4396685249","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":[0.8950763,0.0002585295,0.10409229,0.00011198215,0.000068327005,0.0001870291,0.000017061133,0.00004469378,0.00014381201],"genre_scores_gemma":[0.98988664,0.00024098427,0.0091593135,0.000027237455,0.00017466024,0.00006582641,0.000028474471,0.00002051476,0.00039635235],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9990887,0.000007522199,0.00022229276,0.0003589293,0.00012185047,0.0002007062],"domain_scores_gemma":[0.99967694,0.00005887878,0.000053821288,0.00012030018,0.000013545369,0.00007650233],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000070847454,0.00017888285,0.0002400358,4.2791978e-8,0.00009208477,0.000024523859,0.00006300458,0.000106149295,0.00008179329],"category_scores_gemma":[0.000009262352,0.00016379288,0.000066703135,0.00013799107,0.0003780374,0.000120643876,0.000042187432,0.000102894744,0.0000016459373],"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":[0.000047550424,0.00016724577,0.000121192345,0.00021105833,0.000022121703,0.000003840753,0.00065903296,0.00007543588,0.9264733,0.000028828365,0.000043927936,0.072146416],"study_design_scores_gemma":[0.0013348757,0.0006290999,0.00079820753,0.00018912953,0.00024232954,0.000063649146,0.00031477908,0.026823873,0.96698475,0.0007157926,0.0014221629,0.00048135032],"about_ca_topic_score_codex":0.0000060230145,"about_ca_topic_score_gemma":2.2088474e-7,"teacher_disagreement_score":0.09493297,"about_ca_system_score_codex":0.000059233622,"about_ca_system_score_gemma":0.000008404297,"threshold_uncertainty_score":0.667928},"labels":[],"label_agreement":null},{"id":"W4396724775","doi":"10.5194/acp-24-5389-2024","title":"Simulating the seeder–feeder impacts on cloud ice and precipitation over the Alps","year":2024,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":10,"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":"H2020 European Research Council; China Scholarship Council; National Supercomputing Center, Korea Institute of Science and Technology Information; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung","keywords":"Seeder; Ice crystals; Precipitation; Environmental science; Cloud computing; Atmospheric sciences; Meteorology; Geology; Seeding; Computer science; Engineering; Physics","score_opus":0.006112393593120681,"score_gpt":0.22627723727112903,"score_spread":0.22016484367800834,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4396724775","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":[0.9869126,0.00045624303,0.00065025035,0.00044271222,0.00007613783,0.00011190549,0.0000023049279,0.00003964057,0.011308212],"genre_scores_gemma":[0.99537414,0.00009318406,0.00042998945,0.0005119804,0.0003093278,0.000010409665,0.0000029704229,0.000018161709,0.0032498327],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9992063,0.000021253423,0.00011470723,0.00027349364,0.00019205971,0.00019216962],"domain_scores_gemma":[0.9994386,0.0002558138,0.000040322037,0.00019999543,0.0000041968015,0.00006109651],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012198652,0.00016403227,0.000090545334,6.719274e-9,0.00032936307,0.00015482143,0.00011165043,0.000054623342,0.00075838884],"category_scores_gemma":[0.000015488295,0.00009324715,0.000041575462,0.00016779856,0.00021821939,0.00011729728,0.00009211618,0.00020208137,0.00003532286],"study_design_candidate":"design_other","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":[0.00008859952,0.00016636262,0.033416677,0.00029515487,0.00020588949,0.000016775435,0.013088267,0.04882574,0.0407797,0.0012839211,0.015104711,0.8467282],"study_design_scores_gemma":[0.00056839857,0.00013488438,0.13376671,0.00017100044,0.00016935816,0.000031312207,0.0021481195,0.7957963,0.0045436965,0.0072197216,0.054684553,0.0007659544],"about_ca_topic_score_codex":0.00013383392,"about_ca_topic_score_gemma":0.0000031943164,"teacher_disagreement_score":0.8459622,"about_ca_system_score_codex":0.000039297858,"about_ca_system_score_gemma":0.000009442312,"threshold_uncertainty_score":0.8303826},"labels":[],"label_agreement":null},{"id":"W4396857047","doi":"10.1029/2023gl107780","title":"Top of the Atmosphere Shortwave Arctic Cloud Feedbacks: A Comparison of Diagnostic Methods","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Fonds de recherche du Québec – Nature et technologies","keywords":"Shortwave; Atmosphere (unit); Environmental science; Cloud computing; Arctic; The arctic; Meteorology; Atmospheric sciences; Shortwave radiation; Climatology; Astrobiology; Geology; Oceanography; Geography; Radiative transfer; Computer science; Physics; Radiation","score_opus":0.03318716214228209,"score_gpt":0.3709249011622266,"score_spread":0.3377377390199445,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4396857047","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":[0.9920593,0.00027941752,0.002268513,0.0032262858,0.00027161697,0.00031970988,0.000004697653,0.000020917967,0.0015495507],"genre_scores_gemma":[0.9959222,0.00001790569,0.0032405574,0.00019040372,0.0001432748,0.00003400899,0.0000011267165,0.000021424528,0.00042908077],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.997164,0.0005277138,0.00032607774,0.00038443395,0.0010825809,0.0005151811],"domain_scores_gemma":[0.99623054,0.0030436332,0.000054967375,0.0005219609,0.000025354053,0.00012352194],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00075878727,0.00014586588,0.00029154436,0.0000015371635,0.00012448472,0.00003736373,0.0006385737,0.0000626676,0.0009961125],"category_scores_gemma":[0.00090001634,0.00009535948,0.00021599398,0.0010044473,0.0013435155,0.000087948465,0.0006822098,0.0006314904,0.00023004622],"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":[0.00010927784,0.00086748984,0.21184096,0.0005769371,0.00022805054,0.000047216625,0.0058382377,0.005487063,0.5072659,0.0053171944,0.07515453,0.18726711],"study_design_scores_gemma":[0.0006471104,0.001027587,0.78899765,0.000951499,0.0001770729,0.000008706159,0.0026240938,0.046757784,0.10448777,0.013047844,0.04044374,0.00082915043],"about_ca_topic_score_codex":0.0018729371,"about_ca_topic_score_gemma":0.00003417916,"teacher_disagreement_score":0.57715666,"about_ca_system_score_codex":0.00016320203,"about_ca_system_score_gemma":0.000037015074,"threshold_uncertainty_score":0.9999171},"labels":[],"label_agreement":null},{"id":"W4396927381","doi":"10.5194/acp-24-5637-2024","title":"Shallow- and deep-convection characteristics in the greater Houston, Texas, area using cell tracking methodology","year":2024,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"U.S. Department of Energy","keywords":"Convection; Convection cell; Diurnal cycle; Atmospheric sciences; Environmental science; Radar; Geostationary orbit; Irradiance; Meteorology; Geology; Satellite; Optics; Physics; Natural convection; Combined forced and natural convection","score_opus":0.02616755936488729,"score_gpt":0.24267370832865928,"score_spread":0.216506148963772,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4396927381","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":[0.98417,0.00033473296,0.013105412,0.00004505577,0.00005672141,0.0000779744,0.0000019424995,0.00002599414,0.0021821705],"genre_scores_gemma":[0.990639,0.00013491214,0.008358057,0.00014220331,0.00013199517,0.0000063261655,0.0000044156177,0.000017612972,0.0005655286],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99914616,0.000047253176,0.0001601987,0.00032837354,0.00010840393,0.0002096141],"domain_scores_gemma":[0.9996677,0.0000960369,0.00004285383,0.00014431374,0.000003923576,0.00004518652],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020573156,0.0001694458,0.00016606181,2.6347255e-8,0.000102240345,0.000085102634,0.000098366276,0.00009445416,0.0005634901],"category_scores_gemma":[0.0000071089516,0.0001286456,0.00003678625,0.00018584054,0.00017783129,0.00011986608,0.000060955004,0.00021609668,0.000009802493],"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":[0.00007579246,0.00016030212,0.37270385,0.00046440997,0.000048859456,0.0001494323,0.008149801,0.0014014608,0.13778393,0.000060012753,0.00014650478,0.47885564],"study_design_scores_gemma":[0.00077650405,0.00015543199,0.37415072,0.00016140183,0.00029559137,0.0004129857,0.002185283,0.59138185,0.016615998,0.0032025848,0.009407841,0.0012537739],"about_ca_topic_score_codex":0.0001609783,"about_ca_topic_score_gemma":0.0000048932948,"teacher_disagreement_score":0.5899804,"about_ca_system_score_codex":0.00005247863,"about_ca_system_score_gemma":0.00000855365,"threshold_uncertainty_score":0.61698216},"labels":[],"label_agreement":null},{"id":"W4397022945","doi":"10.1175/bams-d-23-0014.1","title":"Experiment of Sea Breeze Convection, Aerosols, Precipitation, and Environment (ESCAPE)","year":2024,"lang":"en","type":"article","venue":"Bulletin of the American Meteorological Society","topic":"Atmospheric aerosols and clouds","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":"McGill University; National Research Council Canada","funders":"U.S. Department of Energy; Biological and Environmental Research; Office of Science; National Science Foundation","keywords":"Sea breeze; Precipitation; Environmental science; Meteorology; Convection; Atmospheric sciences; Climatology; Geology; Geography","score_opus":0.007100944866043662,"score_gpt":0.21404164356937852,"score_spread":0.20694069870333487,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4397022945","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":[0.9925536,0.00056501146,0.0011088215,0.0044575916,0.00007385693,0.00022128568,0.000007849371,0.000032027914,0.0009799369],"genre_scores_gemma":[0.9862807,0.00046382143,0.011696898,0.0007878145,0.000025223113,0.000033396787,0.0000011079621,0.000011658506,0.0006994147],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99872464,0.00012916072,0.00028079242,0.000335317,0.00033441983,0.00019564251],"domain_scores_gemma":[0.9993509,0.00015292192,0.00018330207,0.00023774835,0.000006256593,0.00006885284],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000330936,0.00014697392,0.00025732224,6.7268616e-7,0.00010002663,0.000012591603,0.00023302254,0.00005240565,0.003804346],"category_scores_gemma":[0.0000311715,0.00009073902,0.0002248125,0.00015393796,0.0017896873,0.000016187223,0.00036409454,0.00013224795,0.000059990947],"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":[0.00028424093,0.0011120575,0.3116162,0.0001729193,0.0006707054,0.0000063339908,0.0062401984,0.004454475,0.2937245,0.0014850126,0.28366488,0.09656844],"study_design_scores_gemma":[0.00063590787,0.0018935888,0.60788965,0.00005252256,0.00020710727,0.000028267443,0.0032145865,0.0028167448,0.03368198,0.0015354286,0.34741142,0.00063279126],"about_ca_topic_score_codex":0.00057213806,"about_ca_topic_score_gemma":0.0000013341419,"teacher_disagreement_score":0.29627344,"about_ca_system_score_codex":0.00007083363,"about_ca_system_score_gemma":0.000006650735,"threshold_uncertainty_score":0.9971063},"labels":[],"label_agreement":null},{"id":"W4398280876","doi":"10.7910/dvn/hbikkv/5wr3uv","title":"RunD3.coldat","year":2020,"lang":"en","type":"dataset","venue":"Harvard Dataverse","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"","keywords":"Seeding; Cloud computing; Turbulence; Environmental science; Meteorology; Mechanics; Computer science; Physics; Thermodynamics; Operating system","score_opus":0.010277352513257615,"score_gpt":0.21050263895707183,"score_spread":0.2002252864438142,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4398280876","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000046656583,3.8338806e-7,0.000050356226,0.000016417722,0.00045491746,0.00023258766,0.9971365,0.000060472543,0.0020017277],"genre_scores_gemma":[0.000023785262,0.00019415177,0.0007647579,0.0021508366,0.0002547253,0.000021834447,0.9954828,0.000027384345,0.001079748],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99804294,0.00004872547,0.00028105042,0.0007085859,0.0005224393,0.00039624146],"domain_scores_gemma":[0.99830097,0.000028013052,0.0001714299,0.0011925821,0.000003978398,0.00030299992],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00010578931,0.0003606178,0.00033768636,0.0000015088832,0.00014845261,0.0000797652,0.0010992128,0.0002569768,0.36698517],"category_scores_gemma":[0.00007464728,0.00033643987,0.00012189365,0.00020681863,0.0002209786,0.00022964591,0.0017098328,0.00042835154,0.83130795],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017440936,0.00004891795,0.00007671492,0.000021694996,0.000021853877,0.00014652281,0.000012242314,0.00002069698,0.000033035856,0.0000036284227,0.9992783,0.0003189253],"study_design_scores_gemma":[0.00021581913,0.000056173943,0.0002210303,0.000014924762,0.00008030473,0.000009010336,0.000029425328,0.000036234484,0.00000849345,0.000013174587,0.99891555,0.00039985857],"about_ca_topic_score_codex":0.0011532804,"about_ca_topic_score_gemma":0.00024992475,"teacher_disagreement_score":0.46432278,"about_ca_system_score_codex":0.00015832573,"about_ca_system_score_gemma":0.000032053023,"threshold_uncertainty_score":0.99990875},"labels":[],"label_agreement":null},{"id":"W4398620145","doi":"10.7910/dvn/hbikkv/yo4jec","title":"RunC.nc","year":2020,"lang":"en","type":"dataset","venue":"Harvard Dataverse","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"","keywords":"Cloud computing; Seeding; Turbulence; Meteorology; Environmental science; Cloud seeding; Mechanics; Statistical physics; Atmospheric sciences; Computer science; Physics; Thermodynamics; Operating system","score_opus":0.010110045715613438,"score_gpt":0.20933135928428143,"score_spread":0.19922131356866798,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4398620145","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000030575397,3.6594514e-7,0.000074535375,0.000015486621,0.00042492972,0.00018177282,0.9968197,0.000055483622,0.0023971626],"genre_scores_gemma":[0.000022220485,0.00017251146,0.00077817636,0.0020309903,0.00024358962,0.000017594135,0.99563515,0.000024384779,0.0010754104],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9982119,0.000042893535,0.00025356232,0.00063589297,0.000496012,0.00035972206],"domain_scores_gemma":[0.99847525,0.000023787026,0.00015365926,0.0010701126,0.0000037496193,0.00027346238],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00009623892,0.0003313319,0.00030972424,0.000001242282,0.00012732012,0.000059184746,0.0009879193,0.00023548261,0.36777395],"category_scores_gemma":[0.00007246983,0.0003047821,0.000113657676,0.00018132578,0.00020461802,0.0001868953,0.0014146254,0.00040772313,0.84263617],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014827753,0.00004082589,0.00008172914,0.000018857409,0.000019667934,0.00013766794,0.00001344548,0.000028455946,0.000019293511,0.0000025402296,0.999217,0.00040572966],"study_design_scores_gemma":[0.00018907107,0.000050407652,0.00026409992,0.000012925616,0.000072326846,0.000008418354,0.00002448405,0.000047190708,0.0000065742147,0.000014046763,0.9989469,0.00036354226],"about_ca_topic_score_codex":0.0011412388,"about_ca_topic_score_gemma":0.00017142695,"teacher_disagreement_score":0.4748622,"about_ca_system_score_codex":0.00013474391,"about_ca_system_score_gemma":0.000029211697,"threshold_uncertainty_score":0.99994045},"labels":[],"label_agreement":null},{"id":"W4398854787","doi":"10.7910/dvn/ryrxk7","title":"Spatial Power Spectra of Dust in the Local Group","year":2019,"lang":"en","type":"dataset","venue":"Harvard Dataverse","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"University of Alberta","funders":"","keywords":"Group (periodic table); Spectral line; Power (physics); Physics; Geography; Environmental science; Astronomy; Quantum mechanics","score_opus":0.00867326026247683,"score_gpt":0.21297750312308109,"score_spread":0.20430424286060425,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4398854787","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0014653543,7.88117e-7,0.0005660958,0.00000779859,0.00036346223,0.00033625693,0.99541485,0.0000058268347,0.0018395438],"genre_scores_gemma":[0.016079068,0.00007583391,0.00018103959,0.0004989703,0.00007604163,0.000012030883,0.98290306,0.000015915566,0.00015804217],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9982927,0.000096438656,0.00031370064,0.00041574624,0.0005701987,0.00031125863],"domain_scores_gemma":[0.99841,0.000059651597,0.00018273217,0.0012903353,0.0000031394277,0.000054140917],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0003311113,0.00024784126,0.00030038157,0.000003027487,0.00004151483,0.000025216015,0.0011740605,0.00021678697,0.14989793],"category_scores_gemma":[0.00002798343,0.00017528422,0.00009336992,0.00017934867,0.0003657372,0.0001376395,0.0005639374,0.00043115183,0.09206819],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003357516,0.00013923072,0.0008193773,0.000017516197,0.0000095372225,0.00006141578,0.00005869483,0.00007012731,0.000018055212,0.000011913184,0.9985018,0.00025879798],"study_design_scores_gemma":[0.00030887246,0.00011414663,0.010123891,0.000024022635,0.00003268951,0.000009528743,0.00028147842,0.00006943581,0.000005208073,0.000010496083,0.9888136,0.00020662621],"about_ca_topic_score_codex":0.008834927,"about_ca_topic_score_gemma":0.002832045,"teacher_disagreement_score":0.05782974,"about_ca_system_score_codex":0.000115386545,"about_ca_system_score_gemma":0.000021480766,"threshold_uncertainty_score":0.9977653},"labels":[],"label_agreement":null},{"id":"W4398860243","doi":"10.7910/dvn/ryrxk7/tjxdsc","title":"all_1Dpspec_coldens.pdf","year":2019,"lang":"en","type":"dataset","venue":"Harvard Dataverse","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"University of Alberta","funders":"","keywords":"Spectral line; Group (periodic table); Geography; Environmental science; Physics; Astronomy","score_opus":0.010544077290849047,"score_gpt":0.21762643398845194,"score_spread":0.2070823566976029,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4398860243","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00016340581,6.196483e-7,0.000029775621,0.000005513557,0.00087048055,0.00033871786,0.98961455,0.000031871983,0.008945097],"genre_scores_gemma":[0.000020405027,0.00021430296,0.00038598262,0.000978357,0.00019226543,0.000020639769,0.9774237,0.000026354897,0.020737957],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99782956,0.000049421087,0.0002985735,0.0007378399,0.0006081567,0.00047642706],"domain_scores_gemma":[0.99769145,0.000040462106,0.00020032223,0.0018695316,0.000006461112,0.00019177032],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00016212568,0.00039302182,0.0003719574,0.000002639147,0.000113929935,0.00008133186,0.0011561891,0.00032428245,0.81610966],"category_scores_gemma":[0.000044629873,0.0003680034,0.00014415673,0.00016899877,0.00019103539,0.00022974057,0.0015069137,0.00042613418,0.9562827],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001641082,0.00006799733,0.00019413438,0.000023075605,0.00002558506,0.000078846875,0.000007370787,0.000066534,0.000022739428,0.0000022250113,0.9992594,0.0002356882],"study_design_scores_gemma":[0.00027110672,0.000056529538,0.0005826304,0.000022911314,0.000081893624,0.000014703253,0.000026333852,0.000042878353,0.0000053956014,0.000009820311,0.9984241,0.0004617055],"about_ca_topic_score_codex":0.001260895,"about_ca_topic_score_gemma":0.00039745454,"teacher_disagreement_score":0.14017305,"about_ca_system_score_codex":0.00024572547,"about_ca_system_score_gemma":0.00003632226,"threshold_uncertainty_score":0.9998772},"labels":[],"label_agreement":null},{"id":"W4398922839","doi":"10.7910/dvn/ryrxk7/gzvkyj","title":"all_1Dpspec_pacs100_mod.pdf","year":2019,"lang":"en","type":"dataset","venue":"Harvard Dataverse","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"University of Alberta","funders":"","keywords":"Mod; Group (periodic table); Spectral line; Power (physics); Physics; Geography; Mathematics; Combinatorics; Astronomy","score_opus":0.011438445472474117,"score_gpt":0.22137455710842296,"score_spread":0.20993611163594886,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4398922839","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00015573557,6.907967e-7,0.0000555749,0.0000053964454,0.0008190051,0.00032300258,0.98639077,0.00003387003,0.012215953],"genre_scores_gemma":[0.000025888019,0.00023466819,0.00050376647,0.0010045483,0.00019279445,0.000019747844,0.98175645,0.000029726316,0.01623243],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9976886,0.000057466805,0.00031445612,0.0007825741,0.0006296183,0.0005272694],"domain_scores_gemma":[0.99755245,0.00003915804,0.00021305254,0.0019716132,0.0000062545187,0.00021746254],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00018118588,0.000428014,0.00040791117,0.000003001617,0.00012138516,0.00007797492,0.0011422475,0.00036346473,0.7468983],"category_scores_gemma":[0.00004721425,0.0003954707,0.00015139724,0.00016699957,0.00022048134,0.0002716832,0.0013879668,0.00047063676,0.9532821],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016932909,0.00007356274,0.00021719022,0.000024846653,0.000028485685,0.0000688648,0.000009214555,0.000089599765,0.000031406762,0.000002780401,0.99922967,0.00020742648],"study_design_scores_gemma":[0.0002854347,0.000056464472,0.0005438359,0.000023919905,0.000082112245,0.000015427342,0.00002786441,0.00005470676,0.000007203087,0.000013411124,0.9983973,0.00049233256],"about_ca_topic_score_codex":0.0016039681,"about_ca_topic_score_gemma":0.00029349438,"teacher_disagreement_score":0.20638387,"about_ca_system_score_codex":0.00026183444,"about_ca_system_score_gemma":0.000040651652,"threshold_uncertainty_score":0.99984974},"labels":[],"label_agreement":null},{"id":"W4398993567","doi":"10.7910/dvn/ryrxk7/azls7q","title":"all_1Dpspec_mips70_orig.pdf","year":2019,"lang":"en","type":"dataset","venue":"Harvard Dataverse","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"University of Alberta","funders":"","keywords":"Physics; Geography; Humanities; Art","score_opus":0.010915762706251672,"score_gpt":0.21929331476567956,"score_spread":0.2083775520594279,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4398993567","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0001294262,7.179385e-7,0.00004530507,0.000005249548,0.0009794342,0.00031782262,0.9879469,0.000033478613,0.010541631],"genre_scores_gemma":[0.000014398967,0.00026072437,0.00053259573,0.0009513958,0.00022736694,0.000019247713,0.9778598,0.00002985786,0.020104602],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9976766,0.000055764107,0.00032646878,0.0007913867,0.0006306899,0.000519085],"domain_scores_gemma":[0.9975442,0.000040027586,0.00022001045,0.0019780758,0.000006407148,0.00021123131],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00018629825,0.00043211415,0.00040244134,0.0000028724476,0.000121768695,0.00007924178,0.0012462069,0.00036226198,0.8243957],"category_scores_gemma":[0.000045518304,0.00039522606,0.00015470426,0.00017558438,0.00021012264,0.00026716053,0.0013934689,0.00047795512,0.96044624],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017077764,0.000073167954,0.00019950206,0.000025843363,0.000028759749,0.000074618765,0.000008743448,0.0000644813,0.000021366452,0.0000035767807,0.9992758,0.00020707081],"study_design_scores_gemma":[0.0002837912,0.000058706068,0.0003460047,0.0000228156,0.00008571001,0.000016375176,0.000028685987,0.00003622815,0.0000071761665,0.000014773284,0.998601,0.0004987168],"about_ca_topic_score_codex":0.0014602572,"about_ca_topic_score_gemma":0.00028754392,"teacher_disagreement_score":0.13605054,"about_ca_system_score_codex":0.0002531302,"about_ca_system_score_gemma":0.000039212966,"threshold_uncertainty_score":0.99985},"labels":[],"label_agreement":null},{"id":"W4399012274","doi":"10.7910/dvn/ryrxk7/zsiyfd","title":"all_1Dpspec_spire350_mod.pdf","year":2019,"lang":"en","type":"dataset","venue":"Harvard Dataverse","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"University of Alberta","funders":"","keywords":"Mod; Group (periodic table); Spectral line; Physics; Mathematics; Combinatorics; Astronomy","score_opus":0.011366429067046581,"score_gpt":0.22089616640951534,"score_spread":0.20952973734246877,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399012274","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00021581695,6.7984956e-7,0.000045397155,0.0000063725597,0.00088609237,0.000334977,0.989278,0.000035598805,0.009197058],"genre_scores_gemma":[0.00002228431,0.00021101075,0.0005201731,0.001120718,0.00020594132,0.00002198427,0.98306376,0.000031352385,0.014802782],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.997663,0.000049450493,0.00032696317,0.00080172566,0.00063540525,0.00052345294],"domain_scores_gemma":[0.99754673,0.00003548056,0.00021602552,0.001983203,0.0000063442203,0.00021219192],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00017726242,0.00043266983,0.0004057449,0.000002948028,0.00012209352,0.00007826368,0.0012239306,0.00036746458,0.78355557],"category_scores_gemma":[0.000045103203,0.00040013954,0.00015617724,0.00016827096,0.00021618512,0.0002708602,0.0014397211,0.0004580976,0.95278627],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016382817,0.000076489596,0.000228533,0.000025049003,0.000027472,0.00006819574,0.00000817322,0.000087533204,0.000024763804,0.0000029293035,0.99913055,0.00030394414],"study_design_scores_gemma":[0.0002877362,0.000063996515,0.0005374544,0.000024334902,0.00008346975,0.0000135217815,0.000028493916,0.000057386875,0.000007024479,0.000012334871,0.99838513,0.00049912825],"about_ca_topic_score_codex":0.0017246497,"about_ca_topic_score_gemma":0.00031388487,"teacher_disagreement_score":0.16923068,"about_ca_system_score_codex":0.00026144693,"about_ca_system_score_gemma":0.000038848673,"threshold_uncertainty_score":0.999845},"labels":[],"label_agreement":null},{"id":"W4399013349","doi":"10.7910/dvn/ryrxk7/zvdyba","title":"all_1Dpspec_spire500_orig.pdf","year":2019,"lang":"en","type":"dataset","venue":"Harvard Dataverse","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"University of Alberta","funders":"","keywords":"Physics; Humanities; Art","score_opus":0.01083472514099407,"score_gpt":0.22139615137098043,"score_spread":0.21056142622998636,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399013349","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00013512354,6.9625304e-7,0.00003419363,0.000006809966,0.0011020671,0.00032412697,0.9880343,0.000037536087,0.010325143],"genre_scores_gemma":[0.000014923634,0.00022719018,0.0005104327,0.0011166758,0.00024564654,0.000021411164,0.98029804,0.000031417785,0.017534243],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9976362,0.000048476853,0.0003337562,0.00080476113,0.0006487497,0.0005280312],"domain_scores_gemma":[0.99752593,0.000034830413,0.00022731969,0.0019925176,0.000006450779,0.00021297732],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00017861638,0.00044139024,0.0004110755,0.0000029779476,0.00012581992,0.0000820892,0.0012616076,0.00036784582,0.7980388],"category_scores_gemma":[0.00004429825,0.0004044554,0.00015998632,0.00018459678,0.0002448532,0.0002831702,0.0013847691,0.0004662135,0.9589592],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016241489,0.00007515424,0.00027234724,0.000024165214,0.000028680779,0.0000716996,0.0000076051,0.000064264605,0.000019606057,0.0000036361184,0.99914503,0.00027154767],"study_design_scores_gemma":[0.00029310942,0.00006686028,0.0005394952,0.000023424293,0.00008895885,0.000014263547,0.000023715284,0.00003616106,0.0000071690924,0.000013344024,0.99838144,0.0005120598],"about_ca_topic_score_codex":0.0017491118,"about_ca_topic_score_gemma":0.0003228883,"teacher_disagreement_score":0.16092047,"about_ca_system_score_codex":0.000315187,"about_ca_system_score_gemma":0.00003864434,"threshold_uncertainty_score":0.99984074},"labels":[],"label_agreement":null},{"id":"W4399164047","doi":"10.1016/b978-0-323-99931-1.00246-4","title":"Dust sources","year":2024,"lang":"en","type":"book-chapter","venue":"Elsevier eBooks","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal","funders":"","keywords":"Mineral dust; Environmental science; Earth science; Remote sensing; Geography; Aerosol; Meteorology; Geology","score_opus":0.008811036807635496,"score_gpt":0.20661204022817553,"score_spread":0.19780100342054002,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399164047","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0003600942,0.0010700026,0.000002525856,0.00008514265,0.0004139067,0.00022386327,0.000012154405,0.00012575586,0.99770653],"genre_scores_gemma":[0.0018131539,0.00006274791,0.00023473382,0.0004248118,0.000333271,0.000017546692,0.0000056272793,0.00010755222,0.9970006],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99850506,0.0000055314717,0.00027007202,0.00054048543,0.0003914464,0.00028742367],"domain_scores_gemma":[0.9993115,0.000017082144,0.00009980268,0.00042627522,0.000004104243,0.00014120205],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0000983407,0.00037671122,0.00030827377,0.000001994588,0.00010576232,0.00006272166,0.0003356357,0.00029559602,0.025000388],"category_scores_gemma":[0.000002347293,0.0003119475,0.00022571956,0.000011650289,0.0003298869,0.000026719692,0.00045087968,0.0004542915,0.027370024],"study_design_candidate":"design_other","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":[0.0000030023714,0.0000034926854,0.0000685445,0.000026309483,0.00004396353,0.00007424952,0.00018402864,0.000005852259,0.00002536397,0.004071963,0.0046907505,0.99080247],"study_design_scores_gemma":[0.000048151636,0.000033448174,0.000049234273,0.000111532725,0.000082441315,0.000014578858,0.000010529939,0.000014008214,0.000013437229,0.02003077,0.97921747,0.00037437276],"about_ca_topic_score_codex":0.0000029580274,"about_ca_topic_score_gemma":0.000039343337,"teacher_disagreement_score":0.9904281,"about_ca_system_score_codex":0.00014113958,"about_ca_system_score_gemma":0.000015770756,"threshold_uncertainty_score":0.99993324},"labels":[],"label_agreement":null},{"id":"W4399444246","doi":"10.21203/rs.3.rs-4422268/v1","title":"Impacts of aerosol concentration on precipitation pattern of tropical cyclones in South China area","year":2024,"lang":"en","type":"preprint","venue":"Research Square","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Aerosol; Tropical cyclone; Precipitation; Typhoon; Environmental science; Climatology; Atmospheric sciences; Weather Research and Forecasting Model; Meteorology; Geography; Geology","score_opus":0.029656748926539075,"score_gpt":0.32984192961288095,"score_spread":0.30018518068634187,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399444246","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":[0.9969156,0.00015334341,0.0002458874,0.00022185565,0.000107856315,0.0007531616,0.00010765527,0.000015927211,0.0014787143],"genre_scores_gemma":[0.999508,0.00009738168,0.000109064,0.000006960315,0.000048827886,0.000068978836,0.000052341016,0.000021931128,0.00008648136],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9973537,0.00026639272,0.00041905168,0.00046516958,0.001128472,0.00036725358],"domain_scores_gemma":[0.99922216,0.000116257135,0.00014064783,0.00038087147,0.000034522363,0.00010551286],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042475245,0.0001776825,0.0003015547,0.000010461357,0.000037650127,0.00003423653,0.00028774148,0.0002354021,0.0006884589],"category_scores_gemma":[0.00015366856,0.00014735501,0.00010937685,0.00032130364,0.00028665387,0.00004522414,0.00071518484,0.0008639009,0.00007992147],"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":[0.0002216109,0.00046163777,0.94804686,0.0013926269,0.00003398483,0.000022975248,0.017720133,0.012113437,0.007439635,0.00014196504,0.0006501893,0.011754915],"study_design_scores_gemma":[0.00038184208,0.0006142947,0.9777906,0.0014437296,0.000010430947,5.393043e-7,0.0009904742,0.008058508,0.009053754,0.0014477768,0.000013543843,0.00019452849],"about_ca_topic_score_codex":0.0016850823,"about_ca_topic_score_gemma":0.00044435286,"teacher_disagreement_score":0.02974369,"about_ca_system_score_codex":0.000328659,"about_ca_system_score_gemma":0.00008726268,"threshold_uncertainty_score":0.7538142},"labels":[],"label_agreement":null},{"id":"W4399574499","doi":"10.5194/essd-2023-397-rc1","title":"Comment on essd-2023-397","year":2024,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"","keywords":"Environmental science","score_opus":0.019950513541635042,"score_gpt":0.2786485037169018,"score_spread":0.2586979901752668,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399574499","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0000080734735,0.010426057,0.00007824856,0.34525573,0.002473072,0.00036530278,0.000067859306,0.00009379983,0.64123183],"genre_scores_gemma":[0.000046017067,0.008128329,0.00047740192,0.13654177,0.00021285367,0.00007395024,0.00015134441,0.000042272164,0.85432607],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9980043,0.000035900648,0.00030368418,0.00061977125,0.00070100534,0.00033532965],"domain_scores_gemma":[0.99914837,0.000039314265,0.00008138995,0.00058559404,0.000004653912,0.00014067878],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00023051206,0.00036582493,0.00042126607,9.624897e-7,0.000073349576,0.00004490045,0.00047984056,0.00018863457,0.15059595],"category_scores_gemma":[0.000013755044,0.000256141,0.00021934754,0.00021699253,0.00010254002,0.000026999924,0.00056774245,0.0004981547,0.047709394],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000011835549,0.000046282123,0.000015138876,0.00038192235,0.000019837153,0.000025227106,0.000007807729,0.000011967375,9.0570074e-7,0.00027047916,0.9860435,0.01317575],"study_design_scores_gemma":[0.00004934589,0.000083595056,0.000037304726,0.0015268205,0.00008447817,0.0000039888937,0.000007674709,0.000056652298,0.0000058861556,0.00021443491,0.9976033,0.00032651605],"about_ca_topic_score_codex":0.00082780956,"about_ca_topic_score_gemma":0.0002037911,"teacher_disagreement_score":0.21309422,"about_ca_system_score_codex":0.00032076772,"about_ca_system_score_gemma":0.00001710112,"threshold_uncertainty_score":0.9999891},"labels":[],"label_agreement":null},{"id":"W4399670265","doi":"10.1117/12.3016827","title":"Limiting atmospheric emission lines with on-detector subarrays","year":2024,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Limiting; Detector; Environmental science; Remote sensing; Physics; Optics; Engineering; Geology","score_opus":0.00718481980380763,"score_gpt":0.2109646242865731,"score_spread":0.20377980448276545,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399670265","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":[0.90408254,0.00008296419,0.003922395,0.0004088953,0.00012588328,0.00009330375,5.6605757e-7,0.0002695383,0.0910139],"genre_scores_gemma":[0.9708491,0.000015216382,0.0100232605,0.00033672788,0.000112224785,0.000012068735,9.3047146e-7,0.000028406874,0.018622093],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990327,0.000012452176,0.000116963616,0.00034038725,0.00025591566,0.00024159043],"domain_scores_gemma":[0.999642,0.00004977342,0.000019472316,0.00017389534,0.0000028806273,0.0001119811],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00007199511,0.00014872022,0.00009576378,2.3665075e-7,0.0001146457,0.00006793459,0.00012661763,0.00004979043,0.0092059625],"category_scores_gemma":[0.000011716889,0.00008891022,0.00004293051,0.00029637304,0.0000744126,0.00010904938,0.00006900288,0.00012244665,0.0012160927],"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":[0.00021431086,0.0003053417,0.30446777,0.00013506392,0.000092969014,0.00044452105,0.0019533585,0.013113895,0.118075,0.0014246504,0.068332426,0.49144068],"study_design_scores_gemma":[0.0013563472,0.0034812875,0.13355227,0.00082173606,0.00013814073,0.00018345736,0.002664313,0.33813098,0.0706848,0.0010585624,0.4449807,0.0029473838],"about_ca_topic_score_codex":0.00010276359,"about_ca_topic_score_gemma":0.00002472589,"teacher_disagreement_score":0.48849332,"about_ca_system_score_codex":0.00007582507,"about_ca_system_score_gemma":0.0000113833785,"threshold_uncertainty_score":0.99956155},"labels":[],"label_agreement":null},{"id":"W4399716446","doi":"10.5194/essd-2023-397-rc2","title":"Comment on essd-2023-397","year":2024,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"","keywords":"Environmental science","score_opus":0.019950513541635042,"score_gpt":0.2786485037169018,"score_spread":0.2586979901752668,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399716446","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0000080734735,0.010426057,0.00007824856,0.34525573,0.002473072,0.00036530278,0.000067859306,0.00009379983,0.64123183],"genre_scores_gemma":[0.000046017067,0.008128329,0.00047740192,0.13654177,0.00021285367,0.00007395024,0.00015134441,0.000042272164,0.85432607],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9980043,0.000035900648,0.00030368418,0.00061977125,0.00070100534,0.00033532965],"domain_scores_gemma":[0.99914837,0.000039314265,0.00008138995,0.00058559404,0.000004653912,0.00014067878],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00023051206,0.00036582493,0.00042126607,9.624897e-7,0.000073349576,0.00004490045,0.00047984056,0.00018863457,0.15059595],"category_scores_gemma":[0.000013755044,0.000256141,0.00021934754,0.00021699253,0.00010254002,0.000026999924,0.00056774245,0.0004981547,0.047709394],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000011835549,0.000046282123,0.000015138876,0.00038192235,0.000019837153,0.000025227106,0.000007807729,0.000011967375,9.0570074e-7,0.00027047916,0.9860435,0.01317575],"study_design_scores_gemma":[0.00004934589,0.000083595056,0.000037304726,0.0015268205,0.00008447817,0.0000039888937,0.000007674709,0.000056652298,0.0000058861556,0.00021443491,0.9976033,0.00032651605],"about_ca_topic_score_codex":0.00082780956,"about_ca_topic_score_gemma":0.0002037911,"teacher_disagreement_score":0.21309422,"about_ca_system_score_codex":0.00032076772,"about_ca_system_score_gemma":0.00001710112,"threshold_uncertainty_score":0.9999891},"labels":[],"label_agreement":null},{"id":"W4399920911","doi":"10.1038/s41597-024-03477-9","title":"Spatially distributed atmospheric boundary layer properties in Houston – A value-added observational dataset","year":2024,"lang":"en","type":"article","venue":"Scientific Data","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Texas Commission on Environmental Quality; U.S. Department of Energy; National Science Foundation","keywords":"Planetary boundary layer; Wind speed; Meteorology; Environmental science; Convective Boundary Layer; Relative humidity; Shortwave; RADIUS; Boundary layer; Atmospheric sciences; Geology; Geography; Computer science; Turbulence; Radiative transfer; Physics; Mechanics","score_opus":0.07452173068592607,"score_gpt":0.28003448562847194,"score_spread":0.20551275494254587,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399920911","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":[0.94218755,0.0009627433,0.005987657,0.0017014752,0.002835396,0.00065542775,0.04421817,0.00023967683,0.0012119199],"genre_scores_gemma":[0.9154368,0.000016460244,0.0078105615,0.00031375675,0.000102803824,0.000038171635,0.07138692,0.000035706245,0.004858798],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9974106,0.00006246531,0.00032218962,0.0010949897,0.0006990522,0.00041072804],"domain_scores_gemma":[0.99833876,0.00003152865,0.000049063106,0.0014652747,0.000008661998,0.00010673623],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000918402,0.00018404746,0.000151642,0.0000018874092,0.0002988578,0.0007656308,0.0014299048,0.00006269517,0.0038497138],"category_scores_gemma":[0.00010329765,0.00014776053,0.000029182758,0.0010669072,0.00064738403,0.0011956927,0.0017481667,0.0001827357,0.001424096],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002784089,0.00019283059,0.017729705,0.00004462843,0.000018368302,0.000074198084,0.0002735149,0.0036232392,0.0066004973,0.00015878104,0.95875084,0.012505536],"study_design_scores_gemma":[0.00015578589,0.000024431354,0.04284757,0.000057212663,0.000018054126,0.0000074492127,0.00007565182,0.1744679,0.00014994663,0.00032458777,0.7816114,0.0002600397],"about_ca_topic_score_codex":0.001095603,"about_ca_topic_score_gemma":0.0011104348,"teacher_disagreement_score":0.17713949,"about_ca_system_score_codex":0.00018490451,"about_ca_system_score_gemma":0.0001756815,"threshold_uncertainty_score":0.9993534},"labels":[],"label_agreement":null},{"id":"W4400016884","doi":"10.1002/qj.4729","title":"Is a more physical representation of aerosol chemistry needed for fog forecasting?","year":2024,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ontario Tech University","funders":"Science and Engineering Research Board; Indian Institute of Technology Madras; Ministry of Earth Sciences","keywords":"Aerosol; Parametrization (atmospheric modeling); Visibility; Environmental science; Atmospheric sciences; Scale (ratio); Meteorology; Cloud condensation nuclei; Condensation; Particle (ecology); Liquid water content; Effective radius; Physics; Geology; Computer science; Optics","score_opus":0.02063043859288635,"score_gpt":0.26696353416242313,"score_spread":0.24633309556953678,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400016884","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":[0.99132645,0.00008423573,0.00629128,0.0016246537,0.00017438918,0.00015361844,0.000009431916,0.000013629608,0.00032228252],"genre_scores_gemma":[0.9946978,0.0000025338745,0.00425304,0.00030849382,0.00024998572,0.0000099696745,6.0674427e-7,0.000011468201,0.00046611228],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99875194,0.0000454892,0.0003791618,0.0002005355,0.0003986959,0.00022420361],"domain_scores_gemma":[0.9992136,0.00023100249,0.0002770349,0.00016449267,0.000029784309,0.00008413352],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030732446,0.00014148535,0.0002894919,5.557755e-7,0.000110791276,0.000037013564,0.00037755474,0.00011828321,0.00043943108],"category_scores_gemma":[0.000057001253,0.00007806776,0.0009819401,0.00019326281,0.0002955057,0.00008794749,0.00006466782,0.00028055257,0.0000044301028],"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":[0.0012357348,0.0018577597,0.027940765,0.00063932163,0.0017246947,0.000046057896,0.055838697,0.020015147,0.47708592,0.00021386496,0.20040537,0.21299666],"study_design_scores_gemma":[0.0031066197,0.0064039845,0.014455525,0.0002835892,0.0010732181,0.0001697183,0.015509594,0.81075835,0.12347079,0.0207785,0.003086191,0.0009039405],"about_ca_topic_score_codex":0.000028017514,"about_ca_topic_score_gemma":3.8432796e-7,"teacher_disagreement_score":0.7907432,"about_ca_system_score_codex":0.00007732016,"about_ca_system_score_gemma":0.000016232221,"threshold_uncertainty_score":0.48114622},"labels":[],"label_agreement":null},{"id":"W4400363603","doi":"10.5194/ems2024-1043","title":"Challenges in High Latitude Dust (HLD) measurements and HLD interactions with clouds and solar radiation","year":2024,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Radiation; High latitude; Latitude; Environmental science; Astrobiology; Atmospheric sciences; Meteorology; Physics; Astronomy; Optics","score_opus":0.0424831515014023,"score_gpt":0.2567727333488633,"score_spread":0.214289581847461,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400363603","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":[0.9701286,0.0019462807,0.00038706837,0.0021537156,0.00030453881,0.0003895153,0.0000055154496,0.00006479521,0.024619997],"genre_scores_gemma":[0.9934727,0.0024264925,0.0030452171,0.00007941925,0.000047738835,0.00005549123,0.000007383947,0.000023285793,0.0008422475],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987272,0.00004127377,0.00019661896,0.00058098626,0.00026878357,0.00018511046],"domain_scores_gemma":[0.9995893,0.000022706616,0.00007312386,0.00022094337,0.0000058477426,0.00008804681],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020832279,0.00022697375,0.0002111856,0.0000043131213,0.00006367304,0.00008558137,0.0001033014,0.0001380531,0.000546416],"category_scores_gemma":[0.000009161075,0.00017801014,0.000021926755,0.00007676319,0.000105087565,0.00009859378,0.00070676603,0.00045574084,0.000052109488],"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":[0.00012091372,0.00041901952,0.6809706,0.00055270817,0.0003662842,0.000058074922,0.006943289,0.023681568,0.00080312934,0.001289209,0.002736684,0.2820585],"study_design_scores_gemma":[0.0007278148,0.0001613656,0.9795051,0.00038036538,0.00013217608,0.000024208848,0.0010074925,0.008005206,0.0002215136,0.00449215,0.004633753,0.0007088515],"about_ca_topic_score_codex":0.002131107,"about_ca_topic_score_gemma":0.009707712,"teacher_disagreement_score":0.29853448,"about_ca_system_score_codex":0.00018160525,"about_ca_system_score_gemma":0.000016389855,"threshold_uncertainty_score":0.7259043},"labels":[],"label_agreement":null},{"id":"W4400363904","doi":"10.5194/ems2024-986","title":"Multi-scale analysis of the meteorological processes forcing African dust ablation and transport in the extreme mid-march 2022 case","year":2024,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Forcing (mathematics); Environmental science; Scale (ratio); Climatology; Atmospheric sciences; Meteorology; Ablation; Geography; Physics; Aerospace engineering; Geology; Cartography; Engineering","score_opus":0.03182739881964427,"score_gpt":0.25817374291101036,"score_spread":0.2263463440913661,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400363904","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":[0.9935974,0.00023713618,0.0024982337,0.0006152023,0.000048720398,0.00042560438,0.000028896951,0.000014944041,0.0025338707],"genre_scores_gemma":[0.99700874,0.000059904527,0.0021255545,0.00007344077,0.000010832902,0.000075389835,0.000009343345,0.000008325098,0.00062845857],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985757,0.00009918942,0.00033186807,0.00047233485,0.00033785994,0.00018307153],"domain_scores_gemma":[0.9993921,0.00011400906,0.000111565154,0.0003384149,0.000009002624,0.000034911194],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00059544697,0.00017649164,0.00029094174,0.0000062899353,0.00009922596,0.000026271344,0.00033566635,0.0001431231,0.0011392173],"category_scores_gemma":[0.000026239639,0.00008703159,0.00014846431,0.0011652289,0.00027078626,0.000032517935,0.00050645566,0.0004158781,0.0000020157327],"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":[0.000029354806,0.00022141707,0.9199314,0.0002075782,0.00024418457,0.00015364894,0.010269733,0.06327414,0.0016606232,0.00001986061,0.00007857924,0.003909465],"study_design_scores_gemma":[0.00014924382,0.00003803059,0.86919343,0.000029611947,0.0012233855,0.00003410269,0.0060150623,0.12229739,0.00016699803,0.00044620392,0.00015532119,0.0002511897],"about_ca_topic_score_codex":0.0064393086,"about_ca_topic_score_gemma":0.04215678,"teacher_disagreement_score":0.059023254,"about_ca_system_score_codex":0.00006382624,"about_ca_system_score_gemma":0.000024635352,"threshold_uncertainty_score":0.99977386},"labels":[],"label_agreement":null},{"id":"W4400804397","doi":"10.1016/j.envres.2024.119629","title":"Changes in aerosol properties at the El Arenosillo site in Southern Europe as a result of the 2023 Canadian forest fires","year":2024,"lang":"en","type":"article","venue":"Environmental Research","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":18,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Lanzhou Jiaotong University","keywords":"AERONET; Aerosol; Angstrom exponent; Environmental science; HYSPLIT; Single-scattering albedo; Visible Infrared Imaging Radiometer Suite; Moderate-resolution imaging spectroradiometer; Atmospheric sciences; Air quality index; Climatology; Meteorology; Geography; Satellite; Geology","score_opus":0.026669246354767428,"score_gpt":0.2615159087618222,"score_spread":0.23484666240705476,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400804397","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":[0.9883242,0.0009721396,1.238053e-7,0.0037046212,0.00006104132,0.000564154,0.00006374518,0.000006651292,0.0063033053],"genre_scores_gemma":[0.9670902,0.00030781887,0.0000040070877,0.00013838503,0.00003066673,0.00010227181,0.0000049610226,0.000029816309,0.03229189],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.997648,0.00028103666,0.00020963594,0.00041019387,0.0008221673,0.00062896084],"domain_scores_gemma":[0.99930286,0.00010528601,0.000026826021,0.00044030257,0.0000020019909,0.00012269244],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0007886153,0.00015171994,0.00012304193,0.000011604974,0.00027081146,0.00005133456,0.00058590167,0.0000757472,0.003464016],"category_scores_gemma":[0.00008400742,0.000084484214,0.00004753517,0.00061184727,0.0011051989,0.00007335654,0.00092867116,0.0004844454,0.002707163],"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":[0.00007578049,0.00010374833,0.889698,0.000026229984,0.000011543601,0.00010417688,0.013149699,0.0022278111,0.08506099,0.000019831934,0.0021220394,0.007400111],"study_design_scores_gemma":[0.00030903766,0.00019064231,0.9583428,0.00020064192,0.0000056703484,0.000012238666,0.005941145,0.0019497706,0.0067289434,0.00014613204,0.025914911,0.00025808153],"about_ca_topic_score_codex":0.2807532,"about_ca_topic_score_gemma":0.845505,"teacher_disagreement_score":0.5647518,"about_ca_system_score_codex":0.0008561679,"about_ca_system_score_gemma":0.000056489444,"threshold_uncertainty_score":0.99806935},"labels":[],"label_agreement":null},{"id":"W4401267592","doi":"10.1029/2023jd039396","title":"Estimating the Impact of a 2017 Smoke Plume on Surface Climate Over Northern Canada With a Climate Model, Satellite Retrievals, and Weather Forecasts","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"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":"National Aeronautics and Space Administration","keywords":"Environmental science; Aerosol; Plume; Atmospheric sciences; Smoke; Satellite; Climatology; Meteorology; Climate model; Shortwave radiation; Shortwave; Atmosphere (unit); Planetary boundary layer; Climate change; Radiative transfer; Radiation; Geography; Geology","score_opus":0.025712417454671694,"score_gpt":0.31621348818161965,"score_spread":0.290501070726948,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401267592","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":[0.99719226,0.0006871704,0.00012755662,0.00029860155,0.00004317942,0.00019786254,0.000022428101,0.0000079302,0.0014230191],"genre_scores_gemma":[0.99777395,0.00031991093,0.0014966782,0.000027607954,0.00009487159,0.0000025458712,6.2832436e-7,0.000037986523,0.00024581584],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9968818,0.00015875032,0.00040070855,0.00028977022,0.0015540434,0.00071496074],"domain_scores_gemma":[0.9985502,0.00056031055,0.00021058306,0.00030505576,0.00009584404,0.00027804155],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010718633,0.00023025778,0.00036434873,0.0000016535627,0.00026110464,0.00015356325,0.00040081315,0.00005992837,0.00024748073],"category_scores_gemma":[0.00011783231,0.000115188086,0.00015494358,0.00044625407,0.00048744614,0.00025748272,0.0002569576,0.00075197435,0.000015675947],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0026695777,0.00036786238,0.289886,0.0002008036,0.0004777154,0.000573176,0.0017678847,0.6548235,0.0042078765,0.00024556645,0.005596701,0.03918338],"study_design_scores_gemma":[0.00048418026,0.0020574525,0.24839081,0.0004862477,0.00004197536,0.000054843033,0.00026355986,0.74641913,0.00018446108,0.0011502964,0.00023918394,0.0002278562],"about_ca_topic_score_codex":0.15892105,"about_ca_topic_score_gemma":0.057226617,"teacher_disagreement_score":0.101694435,"about_ca_system_score_codex":0.00045206814,"about_ca_system_score_gemma":0.0004205479,"threshold_uncertainty_score":0.95997655},"labels":[],"label_agreement":null},{"id":"W4401574715","doi":"10.1175/jas-d-24-0018.1","title":"Direct Entrainment as a Measure of Dilution","year":2024,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Entrainment (biomusicology); Measure (data warehouse); Dilution; Environmental science; Atmospheric sciences; Meteorology; Climatology; Geology; Thermodynamics; Physics; Computer science; Data mining","score_opus":0.008090253359260018,"score_gpt":0.23226391740337796,"score_spread":0.22417366404411793,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401574715","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":[0.97050977,0.0015016464,0.0003600916,0.001422539,0.0011159619,0.00007930714,5.456466e-7,0.0000102986,0.024999835],"genre_scores_gemma":[0.9963987,0.00009146445,0.0025098836,0.00017877603,0.00007785143,0.0000012116789,1.5758983e-8,0.0000054176035,0.0007366824],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99827516,0.0000756833,0.0003252997,0.000150172,0.0009849499,0.00018876077],"domain_scores_gemma":[0.99946773,0.000070908834,0.00024384323,0.00013546049,0.000013161996,0.00006887571],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010490419,0.00009829521,0.00015835122,4.570356e-7,0.00015838927,0.00005374118,0.0006505146,0.00003351524,0.001302462],"category_scores_gemma":[0.000097610486,0.00005026764,0.00019565936,0.00082198804,0.0006096103,0.00026174344,0.00013842597,0.00011722899,0.000041985146],"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":[0.00018192233,0.0007630963,0.23584834,0.00011345565,0.0004063182,0.00013120199,0.010736477,0.16563803,0.2811389,0.004671934,0.06602032,0.23435001],"study_design_scores_gemma":[0.0018962886,0.005798,0.3842343,0.0025656705,0.00091364677,0.0020589095,0.010023354,0.13290925,0.11673896,0.02658348,0.31441063,0.0018675096],"about_ca_topic_score_codex":0.00011238048,"about_ca_topic_score_gemma":0.0000075055646,"teacher_disagreement_score":0.2483903,"about_ca_system_score_codex":0.00013718785,"about_ca_system_score_gemma":0.00009528328,"threshold_uncertainty_score":0.9996105},"labels":[],"label_agreement":null},{"id":"W4401575818","doi":"10.1175/jas-d-23-0092.1","title":"Cloud-Edge Motion by a Ducted Gravity Wave","year":2024,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Gravity wave; Mechanics; Boussinesq approximation (buoyancy); Buoyancy; Physics; Advection; Atmospheric duct; Cloud physics; Amplitude; Meteorology; Cloud computing; Wave propagation; Geology; Convection; Optics; Natural convection; Atmosphere (unit); Computer science","score_opus":0.010689055930891181,"score_gpt":0.22742262881944442,"score_spread":0.21673357288855324,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401575818","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":[0.9893541,0.0011279325,0.0014216743,0.0027546003,0.002465691,0.000087057866,0.0000015254635,0.000024781444,0.0027626732],"genre_scores_gemma":[0.9933667,0.00008082679,0.0036844064,0.00034013652,0.00021771244,0.0000015189986,8.84735e-8,0.00000959388,0.0022990233],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9982336,0.00009836507,0.00034697622,0.00023447735,0.0008043285,0.00028220902],"domain_scores_gemma":[0.99939024,0.00007005555,0.0002326139,0.00017954383,0.000017230444,0.00011028339],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009141163,0.00014127417,0.00016900682,4.633958e-7,0.00034994495,0.0001667979,0.00072840205,0.000054275213,0.0013219153],"category_scores_gemma":[0.000082365725,0.00007550615,0.00019358471,0.0012197882,0.0007335398,0.000454869,0.00020685664,0.00024660697,0.00009010564],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008503702,0.00046178675,0.1033459,0.000044565193,0.00014302119,0.00012162928,0.0031445043,0.023429079,0.093163274,0.0012052701,0.64113367,0.13372225],"study_design_scores_gemma":[0.0013259412,0.0025176038,0.20852442,0.00055378274,0.0004339249,0.0024593691,0.0036083262,0.30093446,0.0150301885,0.039666872,0.42323393,0.001711193],"about_ca_topic_score_codex":0.00011844551,"about_ca_topic_score_gemma":0.0000104543,"teacher_disagreement_score":0.27750537,"about_ca_system_score_codex":0.00017478764,"about_ca_system_score_gemma":0.00005756559,"threshold_uncertainty_score":0.999591},"labels":[],"label_agreement":null},{"id":"W4401610233","doi":"10.22541/essoar.172374105.56686934/v1","title":"Quantifying the Direct Radiative Effect of Stratospheric Aerosols Using Radiative Kernels","year":2024,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency","keywords":"Radiative transfer; Radiative forcing; Atmospheric sciences; Environmental science; Atmospheric radiative transfer codes; Aerosol; Atmosphere (unit); Remote sensing; Meteorology; Physics; Geology; Optics","score_opus":0.025771285028883654,"score_gpt":0.29069571146156853,"score_spread":0.2649244264326849,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401610233","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":[0.94831896,0.001658645,0.0022046242,0.00011206498,0.0008587694,0.0012738801,0.000043735494,0.0001230941,0.045406215],"genre_scores_gemma":[0.9963804,0.00012738968,0.0021768196,0.00009032318,0.00012471457,0.00007962408,0.00000623387,0.000071229166,0.0009433027],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9970405,0.00042796956,0.00055901735,0.00088461855,0.0006055674,0.00048233537],"domain_scores_gemma":[0.99819994,0.0005354629,0.00042875312,0.00070205407,0.0000126249415,0.00012116442],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00080335705,0.0005945126,0.00080874463,0.000002221013,0.00019023339,0.00012825237,0.0007191496,0.00030798698,0.0029529312],"category_scores_gemma":[0.00008094199,0.00035231098,0.00044599298,0.00048127002,0.00058867334,0.000084522,0.0021816746,0.0009149924,0.0002653587],"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":[0.0002028987,0.00017922385,0.16431843,0.0009993546,0.0013140795,0.000073985124,0.008674367,0.78264415,0.015956556,0.0007285283,0.0064763813,0.01843205],"study_design_scores_gemma":[0.0018367363,0.0015087988,0.07055363,0.0017717198,0.0024020013,0.000035065037,0.0029829678,0.80463684,0.10371023,0.0045043165,0.001974032,0.0040836753],"about_ca_topic_score_codex":0.0033023236,"about_ca_topic_score_gemma":0.00012396129,"teacher_disagreement_score":0.0937648,"about_ca_system_score_codex":0.0003939132,"about_ca_system_score_gemma":0.000082484745,"threshold_uncertainty_score":0.9998929},"labels":[],"label_agreement":null},{"id":"W4401677739","doi":"10.5194/egusphere-2024-1546-rc2","title":"Comment on egusphere-2024-1546","year":2024,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"","keywords":"Geolocation; Remote sensing; Computer science; Environmental science; Geography; World Wide Web","score_opus":0.018866539413862037,"score_gpt":0.2737089629361412,"score_spread":0.2548424235222792,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401677739","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000009363657,0.008176495,0.00009933925,0.3065591,0.003772553,0.00042008996,0.000057163925,0.000112210946,0.6807937],"genre_scores_gemma":[0.000044149532,0.0030686953,0.00087498326,0.14521211,0.0002577616,0.00008205246,0.00010316284,0.000057776982,0.8502993],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99760664,0.000044615495,0.00037261468,0.00074872916,0.000819507,0.00040789877],"domain_scores_gemma":[0.99896127,0.000049996463,0.000096024014,0.00070897123,0.000006112207,0.00017763673],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0002476441,0.00045980813,0.0005034332,8.97862e-7,0.000084039944,0.000047509373,0.0004937996,0.00023384448,0.38500935],"category_scores_gemma":[0.000018040317,0.00032421446,0.00028148765,0.00025300714,0.00012333594,0.000032578217,0.00062176946,0.0006299054,0.05373034],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000019579813,0.000057396966,0.00002085517,0.00038450892,0.000028823732,0.000023602803,0.000012449604,0.000015877753,9.205636e-7,0.00034895612,0.980236,0.01886868],"study_design_scores_gemma":[0.000060891583,0.00011408885,0.000031193154,0.0012585068,0.00011256689,0.0000042551005,0.000013733966,0.00005874539,0.00000625598,0.00023239752,0.99769866,0.00040868248],"about_ca_topic_score_codex":0.0015053516,"about_ca_topic_score_gemma":0.0003864269,"teacher_disagreement_score":0.331279,"about_ca_system_score_codex":0.0004266357,"about_ca_system_score_gemma":0.000025857466,"threshold_uncertainty_score":0.99992096},"labels":[],"label_agreement":null},{"id":"W4401827352","doi":"10.5194/amt-2024-97-rc2","title":"Comment on amt-2024-97","year":2024,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Saint Mary's University","funders":"","keywords":"Environmental science","score_opus":0.023051776189809497,"score_gpt":0.27697204013123,"score_spread":0.25392026394142053,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401827352","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000010206634,0.0068756905,0.000053175696,0.31301385,0.0034061666,0.00035317626,0.000048007263,0.000090366644,0.67614937],"genre_scores_gemma":[0.00004030566,0.0042705447,0.00044885048,0.1693641,0.00020554736,0.000062337494,0.0001107988,0.000040385374,0.82545716],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9980373,0.000033457858,0.00030208848,0.00061240146,0.00068551605,0.00032924622],"domain_scores_gemma":[0.99917006,0.000037043035,0.00007546245,0.0005710938,0.000004350695,0.0001419712],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00021262279,0.00036542563,0.0004105471,9.324009e-7,0.00006747002,0.00004434847,0.00044765533,0.00017990467,0.20163812],"category_scores_gemma":[0.000012936877,0.00025364803,0.0002273572,0.00020001884,0.00009544293,0.00002481479,0.00054130825,0.00052253937,0.06747393],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000011541584,0.000041777657,0.000016919057,0.00030106242,0.00002001991,0.000018023,0.000010309971,0.000014239072,8.577152e-7,0.00014773344,0.97611654,0.023311347],"study_design_scores_gemma":[0.00004420487,0.00007769822,0.000023841863,0.0010822201,0.000076837925,0.0000017376043,0.000008628993,0.00005870052,0.000005997267,0.00018230738,0.9981158,0.00032206255],"about_ca_topic_score_codex":0.0006271304,"about_ca_topic_score_gemma":0.00011648124,"teacher_disagreement_score":0.14930777,"about_ca_system_score_codex":0.00032959328,"about_ca_system_score_gemma":0.000017061999,"threshold_uncertainty_score":0.9999916},"labels":[],"label_agreement":null},{"id":"W4401859181","doi":"10.22541/essoar.172462420.05897542/v1","title":"Exploring causal relationships and adjustment timescales of cloud-aerosol interactions in geostationary satellite observations and CAM6 using wavelet phase coherence analysis","year":2024,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Dalhousie University","funders":"","keywords":"Liquid water path; Environmental science; Entrainment (biomusicology); Coherence (philosophical gambling strategy); Context (archaeology); Satellite; Lag; Meteorology; Atmospheric sciences; Cloud top; Geostationary orbit; Causality (physics); Precipitation; Mathematics; Physics; Statistics; Computer science; Geography","score_opus":0.17802539359331288,"score_gpt":0.31850850443149104,"score_spread":0.14048311083817816,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401859181","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":[0.9947839,0.0007875339,0.0029261794,0.00017208206,0.00017793011,0.00036011694,0.0001570986,0.000032732678,0.00060244725],"genre_scores_gemma":[0.9778777,0.00096499786,0.02032531,0.00002184549,0.00003307063,0.00009179439,0.00013580314,0.000018766026,0.0005307475],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998275,0.00010068648,0.0005699338,0.0005671314,0.00029259827,0.00019464137],"domain_scores_gemma":[0.99921143,0.00019505923,0.00018987477,0.00027269762,0.00002663833,0.00010428457],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028475613,0.00024387897,0.00035234707,0.000025920051,0.00012141103,0.000047597012,0.000105413026,0.000086743355,0.00046279532],"category_scores_gemma":[0.00004384869,0.00023530993,0.00008297236,0.00065042207,0.00021419176,0.0002496811,0.00082248804,0.00051198265,0.000010160967],"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":[0.00011231885,0.00094046444,0.7566093,0.00055425236,0.0013718322,0.000051675393,0.01708439,0.16291983,0.01725866,0.0021800506,0.00041289782,0.040504318],"study_design_scores_gemma":[0.00048740488,0.000059812213,0.7292352,0.00032893053,0.0012086016,0.00001149738,0.0037915662,0.26143226,0.00049894676,0.002165437,0.00016481166,0.0006155666],"about_ca_topic_score_codex":0.003810745,"about_ca_topic_score_gemma":0.0044729626,"teacher_disagreement_score":0.09851242,"about_ca_system_score_codex":0.00028701726,"about_ca_system_score_gemma":0.000050396087,"threshold_uncertainty_score":0.959566},"labels":[],"label_agreement":null},{"id":"W4401964298","doi":"10.5194/egusphere-2024-1651","title":"Radiative Closure Assessment of Retrieved Cloud and Aerosol Properties for the EarthCARE Mission: The ACMB-DF Product","year":2024,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":56,"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":"Natural Environment Research Council; Sight Research UK","keywords":"Radiative transfer; Shortwave; Remote sensing; Environmental science; Atmospheric radiative transfer codes; Satellite; Radiometer; Meteorology; Depth sounding; Cloud top; Atmospheric sciences; Computer science; Physics; Geology; Optics","score_opus":0.029207666772277527,"score_gpt":0.27805084688189596,"score_spread":0.24884318010961842,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401964298","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":[0.93427074,0.010156176,0.0018099298,0.0327796,0.0019526617,0.0067087924,0.000101735845,0.00012305105,0.012097284],"genre_scores_gemma":[0.9850523,0.00043916772,0.0021002856,0.00022996229,0.00029348463,0.00021449501,0.000005398441,0.000034129516,0.011630787],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99804074,0.00010802826,0.00036257494,0.0006683505,0.0005543678,0.00026595953],"domain_scores_gemma":[0.9987721,0.00015101605,0.00019844566,0.0007727187,0.00003672919,0.00006900886],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000638424,0.0003203843,0.00033393,8.7209156e-7,0.00029813836,0.00011476977,0.0005789542,0.00016454827,0.00055149855],"category_scores_gemma":[0.000093405906,0.00013488637,0.00017705228,0.0001504863,0.0006118326,0.000038024107,0.0020871686,0.0006240604,0.000009774921],"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":[0.0012606462,0.0009935122,0.22165357,0.0063935868,0.0037350706,0.000030817806,0.05822464,0.06557619,0.048211128,0.009185895,0.4160595,0.16867544],"study_design_scores_gemma":[0.0034100518,0.002715236,0.37794465,0.0028087206,0.0029228951,0.00007218153,0.042042505,0.22111487,0.116529465,0.024202967,0.20111223,0.0051242327],"about_ca_topic_score_codex":0.00023417489,"about_ca_topic_score_gemma":0.00004790472,"teacher_disagreement_score":0.21494727,"about_ca_system_score_codex":0.00009026913,"about_ca_system_score_gemma":0.0001255317,"threshold_uncertainty_score":0.6038522},"labels":[],"label_agreement":null},{"id":"W4403225896","doi":"10.5194/egusphere-2024-2984","title":"Shallow cloud variability in Houston, Texas during the ESCAPE and TRACER field experiments","year":2024,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"McGill University","funders":"U.S. Department of Energy; National Science Foundation","keywords":"TRACER; Cloud computing; Field (mathematics); Environmental science; Physics; Computer science; Nuclear physics; Mathematics; Operating system","score_opus":0.007411755247789657,"score_gpt":0.23512473158742514,"score_spread":0.22771297633963547,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403225896","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":[0.9447698,0.00025715958,0.00017170359,0.0008248991,0.00046562965,0.00041059413,0.0000027538542,0.00005998046,0.053037483],"genre_scores_gemma":[0.991514,0.00007864573,0.0007242884,0.0002970257,0.00009709816,0.00006345907,0.0000010423247,0.000022955355,0.0072014676],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983604,0.0000976411,0.00028801322,0.0007078535,0.00025792202,0.00028814492],"domain_scores_gemma":[0.999245,0.00009461176,0.00005254771,0.00052767067,0.0000025230293,0.0000776708],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00041292855,0.0002601893,0.00022388791,0.0000013837409,0.000076795804,0.000094935414,0.00036148087,0.00025928012,0.007951994],"category_scores_gemma":[0.000034170294,0.00017058571,0.00008020313,0.000101019,0.00015036965,0.00003829402,0.0028093166,0.0007336921,0.0001732095],"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":[0.00011869675,0.00042905266,0.96188754,0.0003942189,0.0001041644,0.00009170861,0.006434598,0.0038688304,0.004556775,0.0007070618,0.006429664,0.014977706],"study_design_scores_gemma":[0.000503001,0.00008339341,0.9653955,0.00015656589,0.00006028725,0.00001759319,0.0009235868,0.008805358,0.004874418,0.01480154,0.0033888642,0.0009898666],"about_ca_topic_score_codex":0.0023656553,"about_ca_topic_score_gemma":0.0005247578,"teacher_disagreement_score":0.04674422,"about_ca_system_score_codex":0.0002000143,"about_ca_system_score_gemma":0.000016030655,"threshold_uncertainty_score":0.99295485},"labels":[],"label_agreement":null},{"id":"W4403403301","doi":"10.5194/acp-24-11431-2024","title":"Long-term (2010–2021) lidar observations of stratospheric aerosols in Wuhan, China","year":2024,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":11,"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":"China Scholarship Council; Natural Science Foundation of Hubei Province; National Natural Science Foundation of China","keywords":"Environmental science; Term (time); China; Lidar; Atmospheric sciences; Climatology; Meteorology; Remote sensing; Geography; Geology; Physics","score_opus":0.009846742492694805,"score_gpt":0.2199794986149825,"score_spread":0.2101327561222877,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403403301","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":[0.9916639,0.00080331345,0.002524642,0.00007951832,0.0000967051,0.0001309362,0.000008122397,0.000042161297,0.0046507083],"genre_scores_gemma":[0.9881382,0.00029209367,0.006439305,0.000034908204,0.00012462269,0.000025416979,0.0000168881,0.000028550334,0.0049000075],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99871355,0.000015837039,0.00030997995,0.00043933754,0.00022611152,0.00029519698],"domain_scores_gemma":[0.99945724,0.000044282908,0.000069563896,0.00031365134,0.000007572613,0.00010771226],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00008688547,0.0002417011,0.00025512557,2.1876472e-8,0.00007463241,0.00005473769,0.00020850383,0.000116491916,0.0050368584],"category_scores_gemma":[0.000007917862,0.00023126011,0.00008624248,0.000641207,0.00025011066,0.00024133208,0.00012039822,0.00024002448,0.0000562054],"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":[0.000026632173,0.00036022585,0.7168873,0.0005537645,0.00006384659,0.000060181224,0.0009794986,0.0028724833,0.11373883,0.0002910353,0.00059699925,0.16356918],"study_design_scores_gemma":[0.00037833248,0.00006430627,0.96992886,0.00021853451,0.000050117433,0.000014935976,0.00011879526,0.016776938,0.009661974,0.0014861127,0.0007888291,0.0005122857],"about_ca_topic_score_codex":0.0002631985,"about_ca_topic_score_gemma":0.000017186663,"teacher_disagreement_score":0.2530415,"about_ca_system_score_codex":0.00007394777,"about_ca_system_score_gemma":0.000037697275,"threshold_uncertainty_score":0.9958727},"labels":[],"label_agreement":null},{"id":"W4403404468","doi":"10.34987/vestnik.sibpsa.2024.30.95.001.","title":"Современные тенденции изменения повторяемости гроз над Сибирью и смещение Северного магнитного полюса","year":2024,"lang":"ru","type":"article","venue":"Сибирский пожарно-спасательный вестник.","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Computer science","score_opus":0.006729058355670287,"score_gpt":0.2261976164187511,"score_spread":0.21946855806308083,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403404468","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":[0.5997634,0.043726917,0.011902683,0.018591233,0.027022216,0.0055146185,0.0016831496,0.004397358,0.28739843],"genre_scores_gemma":[0.86693764,0.0049160095,0.0037872375,0.0038078693,0.0036656987,0.00036784692,0.00022919498,0.00089136953,0.11539712],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9802918,0.0009040477,0.003345274,0.005673642,0.004173081,0.0056121624],"domain_scores_gemma":[0.99105215,0.0009274227,0.0008359197,0.0042924103,0.00016491093,0.002727188],"candidate_categories":["metaepi_narrow","sts","scholarly_communication","research_integrity","insufficient_payload"],"consensus_categories":["metaepi_narrow","sts","research_integrity","insufficient_payload"],"category_scores_codex":[0.0025671574,0.0035297256,0.0026986324,0.00011304651,0.0020635976,0.0025330388,0.0042222245,0.0021827,0.076339915],"category_scores_gemma":[0.00035430506,0.0034235907,0.0021513682,0.0043346668,0.002719836,0.002671975,0.0030007327,0.003804903,0.07399919],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007964981,0.0030699784,0.027043974,0.0020621892,0.0022083418,0.0056167785,0.010878048,0.0034864112,0.04145529,0.01974594,0.6031765,0.28046006],"study_design_scores_gemma":[0.0027535944,0.0016450313,0.038689464,0.0015830346,0.0013608005,0.0007932425,0.003117685,0.018932242,0.004823133,0.005381063,0.9148442,0.006076491],"about_ca_topic_score_codex":0.002793931,"about_ca_topic_score_gemma":0.0006377466,"teacher_disagreement_score":0.31166774,"about_ca_system_score_codex":0.0026947751,"about_ca_system_score_gemma":0.00089032785,"threshold_uncertainty_score":0.9999942},"labels":[],"label_agreement":null},{"id":"W4403809404","doi":"10.1016/j.scitotenv.2024.177037","title":"Three-dimensional distribution of aerosols of multiple types at daily scale using TROPOMI spaceborne observations","year":2024,"lang":"en","type":"article","venue":"The Science of The Total Environment","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":5,"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":"Institut national des sciences de l'Univers; Université Paris-Est Créteil Val-de-Marne; Centre National d’Etudes Spatiales","keywords":"Aerosol; Environmental science; Lidar; Remote sensing; Satellite; Radiometer; Troposphere; Meteorology; Plume; Sea salt aerosol; Atmospheric sciences; Sea salt; Geology; Geography","score_opus":0.01749934656142002,"score_gpt":0.21593143703114986,"score_spread":0.19843209046972984,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403809404","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":[0.99799806,0.00015220017,0.0008467706,0.0004208188,0.00014730931,0.00023349328,0.0000521842,0.0000071389322,0.00014200587],"genre_scores_gemma":[0.997396,0.000009038839,0.0021815698,0.0000056800786,0.000013989028,0.0000035801058,0.000002558561,0.000007466766,0.00038012434],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9985208,0.000027830692,0.00026411403,0.00024855777,0.000729409,0.00020931514],"domain_scores_gemma":[0.9992721,0.0000644449,0.00015660882,0.0004528181,0.000006139554,0.000047858488],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00044990415,0.0001109921,0.00013856895,0.000001993067,0.0002747209,0.000010131895,0.000467857,0.000031403757,0.00047718396],"category_scores_gemma":[0.000031721065,0.00006319851,0.00013151263,0.00037171034,0.002778913,0.00014893596,0.0008322066,0.00007771169,0.0000345387],"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":[0.000016661354,0.000057390993,0.006589808,0.000008351953,0.000011099612,1.9062749e-7,0.00017971991,0.35408446,0.6384655,0.00021785358,0.00010757793,0.0002613805],"study_design_scores_gemma":[0.00019499246,0.00010134477,0.5775082,0.00007372299,0.00008366708,0.0000097711545,0.000111957146,0.2618274,0.15908308,0.00076587324,0.00008457428,0.00015541459],"about_ca_topic_score_codex":0.0005618068,"about_ca_topic_score_gemma":0.000020326246,"teacher_disagreement_score":0.5709184,"about_ca_system_score_codex":0.00029009682,"about_ca_system_score_gemma":0.00003241697,"threshold_uncertainty_score":0.999935},"labels":[],"label_agreement":null},{"id":"W4403901363","doi":"10.5194/amt-17-6301-2024","title":"An improved geolocation methodology for spaceborne radar and lidar systems","year":2024,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"European Space Agency; Jet Propulsion Laboratory; National Aeronautics and Space Administration","keywords":"Geolocation; Remote sensing; Lidar; Environmental science; Radar; Computer science; Meteorology; Geology; Geography; Telecommunications","score_opus":0.040126463132751915,"score_gpt":0.2833243526325118,"score_spread":0.2431978894997599,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403901363","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"methods","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.06325842,0.002926491,0.9284557,0.00044344185,0.00037943892,0.0017406751,0.0000043265077,0.0010137252,0.0017777522],"genre_scores_gemma":[0.59229916,0.00014388557,0.4064735,0.00012774603,0.00010970612,0.0005173847,0.0000048453735,0.00004020328,0.0002835768],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.998193,0.0001753145,0.00031406197,0.0006124332,0.00035241683,0.0003527607],"domain_scores_gemma":[0.99929786,0.000072224466,0.00008543909,0.0003681154,0.00004256298,0.00013378248],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020995296,0.0002486531,0.0002703364,7.8845864e-7,0.00015340273,0.00012402178,0.00021487924,0.00015950383,0.00016405195],"category_scores_gemma":[0.000071787756,0.00020978657,0.000062662744,0.00022589226,0.0001300283,0.00026873764,0.000073239375,0.00012253528,0.000016914908],"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":[0.0001162973,0.00018412659,0.005418036,0.0003484455,0.00013783124,0.0000095758205,0.0008120905,0.000085735825,0.52549064,0.0050766375,0.010502212,0.45181838],"study_design_scores_gemma":[0.0013321993,0.0060702474,0.019309754,0.0005279044,0.0006537316,0.00014667203,0.0019842219,0.24419509,0.10717028,0.016473576,0.5991487,0.002987604],"about_ca_topic_score_codex":0.0011793774,"about_ca_topic_score_gemma":0.00006931001,"teacher_disagreement_score":0.58864653,"about_ca_system_score_codex":0.00029009453,"about_ca_system_score_gemma":0.000035501147,"threshold_uncertainty_score":0.8554848},"labels":[],"label_agreement":null},{"id":"W4404109732","doi":"10.1175/jas-d-24-0076.1","title":"Primary Modes of Northern Hemisphere Snowfall Particle Size Distributions","year":2024,"lang":"en","type":"article","venue":"Journal of the Atmospheric Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"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; National Aeronautics and Space Administration","keywords":"Northern Hemisphere; Snow; Primary (astronomy); Atmospheric sciences; Environmental science; Climatology; Southern Hemisphere; Meteorology; Geology; Physics; Astronomy","score_opus":0.007999971012438758,"score_gpt":0.2230916319544775,"score_spread":0.21509166094203874,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404109732","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":[0.9907569,0.0014263145,0.00073785865,0.0016858353,0.00035836044,0.00006671093,0.0000030554759,0.000014310253,0.00495063],"genre_scores_gemma":[0.9929427,0.00009841995,0.0057931677,0.00013171697,0.000070016395,0.0000017821263,6.754189e-8,0.000007702025,0.0009544256],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99842155,0.00005619883,0.0004121654,0.00017356731,0.0006882122,0.00024830922],"domain_scores_gemma":[0.9992435,0.00018439819,0.00025597602,0.00019616704,0.000027234473,0.00009271957],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00058435387,0.00011814911,0.00019063432,1.9151308e-7,0.0002314296,0.00007157443,0.00083188916,0.00003908465,0.0010760543],"category_scores_gemma":[0.00012869871,0.00006459263,0.00021614289,0.00092931924,0.0008959594,0.0003591433,0.00022740378,0.00015653233,0.000034974284],"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":[0.000057581794,0.0003949517,0.64271855,0.00007677149,0.00012060751,0.000036118814,0.0011717081,0.13991204,0.16423911,0.001407284,0.014445665,0.035419635],"study_design_scores_gemma":[0.0012037595,0.001556315,0.68787414,0.0009353043,0.00048729184,0.000670743,0.004816575,0.184374,0.05185915,0.02244165,0.04260396,0.0011771017],"about_ca_topic_score_codex":0.0001312345,"about_ca_topic_score_gemma":0.000049164042,"teacher_disagreement_score":0.11237996,"about_ca_system_score_codex":0.0001505883,"about_ca_system_score_gemma":0.00013094566,"threshold_uncertainty_score":0.9998371},"labels":[],"label_agreement":null},{"id":"W4404349924","doi":"10.1126/science.adl0303","title":"Glaciation of liquid clouds, snowfall, and reduced cloud cover at industrial aerosol hot spots","year":2024,"lang":"en","type":"article","venue":"Science","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":5,"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":"Natural Environment Research Council; Sight Research UK","keywords":"Glacial period; Aerosol; Environmental science; Snow; Atmospheric sciences; Supercooling; Cloud cover; Climatology; Physical geography; Geology; Meteorology; Cloud computing; Geography; Geomorphology","score_opus":0.015366756843210296,"score_gpt":0.2401449367812947,"score_spread":0.2247781799380844,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404349924","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":[0.9943445,0.00017084944,0.00011197113,0.00029145004,0.00089139433,0.00016981078,0.000007616815,0.000041980904,0.003970462],"genre_scores_gemma":[0.99727774,0.000052985873,0.0003355096,0.00009183173,0.00013981198,0.0000057136144,0.0000014942918,0.000008994106,0.002085933],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9983726,0.000025499388,0.0002131663,0.0004798771,0.000597066,0.00031180197],"domain_scores_gemma":[0.99950373,0.000042641455,0.00007247587,0.00022775328,0.000011296308,0.00014208537],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006087824,0.00012312685,0.00013563417,0.0000041218277,0.00021358869,0.00007158235,0.00031214184,0.00008134127,0.0011922382],"category_scores_gemma":[0.00009236125,0.00010307071,0.00003757138,0.00080015644,0.0010836318,0.00040689198,0.0004240787,0.00012067182,0.00029699228],"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":[0.00018064528,0.000052815594,0.009879223,0.000017016266,0.000008148453,0.000010667604,0.0014445933,0.0003344498,0.96648747,0.00042782087,0.0090456335,0.0121115185],"study_design_scores_gemma":[0.0013468846,0.0015961909,0.14363508,0.00026976547,0.00009609306,0.000086475564,0.0005279097,0.013018008,0.7499138,0.00071955856,0.087452285,0.0013379118],"about_ca_topic_score_codex":0.00010440586,"about_ca_topic_score_gemma":0.00001375036,"teacher_disagreement_score":0.21657364,"about_ca_system_score_codex":0.00024021832,"about_ca_system_score_gemma":0.000081648046,"threshold_uncertainty_score":0.9997208},"labels":[],"label_agreement":null},{"id":"W4404382571","doi":"10.1080/07055900.2024.2425859","title":"How Skilful Are Cloud Cover Products in Representing Observed Cloudiness in Québec?","year":2024,"lang":"en","type":"article","venue":"ATMOSPHERE-OCEAN","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Ouranos; Université de Montréal","funders":"","keywords":"Cloud cover; Cover (algebra); Cloud computing; Environmental science; Computer science; Engineering; Operating system","score_opus":0.017562672601849096,"score_gpt":0.21926720942148145,"score_spread":0.20170453681963235,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404382571","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":[0.9879771,0.0015116367,0.00009968361,0.0044559096,0.0007439187,0.00043880203,0.000003899408,0.00017842437,0.0045906617],"genre_scores_gemma":[0.9748788,0.00006422607,0.0010824691,0.00024840518,0.0003065324,0.000015065316,0.0000064938276,0.00007696279,0.023321066],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9970924,0.00011258172,0.00046025767,0.0011011957,0.0004911257,0.0007424373],"domain_scores_gemma":[0.99893886,0.00010899564,0.00012991995,0.0006714902,0.000015918418,0.00013480207],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00047679266,0.00037110006,0.00040627565,0.0000012221535,0.00010127822,0.00024314219,0.0005159621,0.00016843059,0.0012968798],"category_scores_gemma":[0.00024264806,0.00033565133,0.00011030489,0.0014279279,0.00019959659,0.0005669286,0.00046261068,0.00046794955,0.00044625334],"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":[0.000030487161,0.00014304722,0.9580949,0.00008992014,0.000017409844,0.0003960314,0.0011350029,0.006067823,0.00045903234,0.00011084889,0.02995177,0.0035037554],"study_design_scores_gemma":[0.0012236158,0.00010122097,0.8202755,0.0005209183,0.00003934568,0.00004241188,0.0031978362,0.022162888,0.0013634841,0.00095093314,0.14887466,0.0012472033],"about_ca_topic_score_codex":0.016652703,"about_ca_topic_score_gemma":0.011317962,"teacher_disagreement_score":0.13781938,"about_ca_system_score_codex":0.00056198466,"about_ca_system_score_gemma":0.000086240914,"threshold_uncertainty_score":0.9999096},"labels":[],"label_agreement":null},{"id":"W4404449269","doi":"10.1016/j.atmosres.2024.107800","title":"Dynamics of a severe summer Shamal wind and its induced dust storm in the Middle East: A diagnostic study based on numerical simulation","year":2024,"lang":"en","type":"article","venue":"Atmospheric Research","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Abdus Salam International Centre for Theoretical Physics; National Aeronautics and Space Administration","keywords":"Storm; Meteorology; Dust storm; Climatology; Environmental science; Atmospheric sciences; Wind speed; Dynamics (music); Severe weather; Geology; Geography; Physics","score_opus":0.08103480137524302,"score_gpt":0.33446362744560404,"score_spread":0.253428826070361,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404449269","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":[0.9968707,0.00011137181,0.00019587479,0.000562596,0.000051566487,0.0009131118,0.0000041089047,0.00001821092,0.0012724836],"genre_scores_gemma":[0.9994452,0.000007784301,0.00014148033,0.00007160323,0.00003452336,0.000048671343,0.000003439765,0.0000254444,0.0002218362],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99727607,0.00043475724,0.00026421918,0.00046852432,0.0011329402,0.0004235119],"domain_scores_gemma":[0.99778265,0.0017488062,0.00003504497,0.00031462798,0.000023729755,0.00009513089],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012523353,0.0001648234,0.00018982172,0.0000018650467,0.00013499545,0.00008455207,0.00034428397,0.000094750096,0.00086069416],"category_scores_gemma":[0.00044028164,0.000114617476,0.000043336186,0.001483893,0.00014054637,0.00014682066,0.00019837893,0.0005639029,0.00011123543],"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":[0.00017899816,0.0016499803,0.69681084,0.00006985756,0.000028071585,0.00022423267,0.011478053,0.26909584,0.00010008978,0.00017537258,0.00019869726,0.019989964],"study_design_scores_gemma":[0.0003020953,0.0007089475,0.3655487,0.00004110077,0.00000746817,0.0000018889061,0.0036063627,0.6295365,0.0000023661544,0.000054317556,0.00009183379,0.00009843911],"about_ca_topic_score_codex":0.0013701341,"about_ca_topic_score_gemma":0.00042155088,"teacher_disagreement_score":0.36044064,"about_ca_system_score_codex":0.00028982072,"about_ca_system_score_gemma":0.000059150785,"threshold_uncertainty_score":0.94239974},"labels":[],"label_agreement":null},{"id":"W4404507197","doi":"10.5194/egusphere-2024-2727","title":"Optical Properties of North Atlantic Aerosols Through a compact dual-wavelength depolarization Lidar Observations","year":2024,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"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":"Lidar; Wavelength; Dual (grammatical number); Depolarization; Remote sensing; Environmental science; Depolarization ratio; Geology; Physics; Optics; Biology","score_opus":0.042014325972740574,"score_gpt":0.23977638447323207,"score_spread":0.1977620585004915,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404507197","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":[0.9867128,0.00013629429,0.0030772265,0.00068209117,0.00026689845,0.00059166,0.000020609132,0.00014777132,0.008364647],"genre_scores_gemma":[0.9893339,0.000120626944,0.008641825,0.00016043022,0.000078881705,0.000029567347,0.00006156917,0.00004554544,0.0015276056],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99793357,0.000045745015,0.0005736827,0.0005845481,0.0005390584,0.00032340013],"domain_scores_gemma":[0.9991543,0.000028127279,0.00017711493,0.0005177145,0.00002701014,0.0000956971],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00009866637,0.00034626274,0.00043138923,0.0000021294734,0.00011273005,0.000099612145,0.00028213597,0.0002151886,0.00060123665],"category_scores_gemma":[0.000040942552,0.00025843567,0.00017764,0.0003001979,0.00033294264,0.00013048809,0.0013057688,0.0005386149,0.0003016971],"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":[0.000045745666,0.00059876073,0.9421455,0.000884639,0.00027629422,0.000030217025,0.0029441395,0.03212684,0.011599812,0.0037675533,0.004024374,0.0015561035],"study_design_scores_gemma":[0.00023596032,0.00013913731,0.96787614,0.00046037027,0.0002750765,0.000016530441,0.00019035065,0.021371853,0.0047049094,0.0031657636,0.0007280166,0.0008359219],"about_ca_topic_score_codex":0.004000174,"about_ca_topic_score_gemma":0.001237852,"teacher_disagreement_score":0.025730588,"about_ca_system_score_codex":0.00015185955,"about_ca_system_score_gemma":0.00008998841,"threshold_uncertainty_score":0.99998677},"labels":[],"label_agreement":null},{"id":"W4404755514","doi":"10.22541/essoar.173272440.08582693/v1","title":"Measuring the shape of cloud particle size distributions in high-latitude marine cold air outbreaks","year":2024,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"National Cancer Institute; Met Office; Natural Environment Research Council; National Computational Infrastructure; University of Leeds; UK Research and Innovation","keywords":"Latitude; Environmental science; Outbreak; Meteorology; Cloud computing; Atmospheric sciences; Particle (ecology); Geography; Climatology; Geology; Geodesy; Computer science; Oceanography; Biology; Virology","score_opus":0.013423898762422294,"score_gpt":0.22027188529752165,"score_spread":0.20684798653509937,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404755514","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":[0.988532,0.00006746484,0.00062078104,0.0017773664,0.00030996598,0.00033681717,0.000036435216,0.000057943533,0.008261211],"genre_scores_gemma":[0.99618477,0.00003038956,0.0016653751,0.00009448644,0.000058178637,0.00007043532,0.0000059132044,0.000016700516,0.0018737762],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985696,0.00004802481,0.0003842247,0.000387206,0.00033703257,0.00027390235],"domain_scores_gemma":[0.99924386,0.000101307756,0.000095023446,0.00048330214,0.000007715707,0.000068777204],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00031578846,0.00019325207,0.0002437108,6.912717e-7,0.000067336914,0.000029397128,0.00044340495,0.00012533044,0.0048495578],"category_scores_gemma":[0.000057336438,0.0001305413,0.00010585808,0.00022455848,0.00022551962,0.0000285122,0.0036233424,0.0004684415,0.00024171984],"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":[0.00005396944,0.0007122011,0.7168715,0.00023744226,0.00017426694,0.00004672325,0.0011423475,0.21858059,0.010421332,0.037837032,0.005417342,0.008505252],"study_design_scores_gemma":[0.00035896394,0.000046306133,0.9371644,0.0001208832,0.00009656368,0.0000026656428,0.00020802389,0.034853373,0.00809714,0.016822005,0.001771357,0.00045829508],"about_ca_topic_score_codex":0.0072331163,"about_ca_topic_score_gemma":0.0028672135,"teacher_disagreement_score":0.22029293,"about_ca_system_score_codex":0.00023345446,"about_ca_system_score_gemma":0.000028975986,"threshold_uncertainty_score":0.9993778},"labels":[],"label_agreement":null},{"id":"W4404872196","doi":"10.1016/j.jqsrt.2024.109293","title":"Corrigendum to “Combined stochastic and transfer model for atmospheric radiation” [Journal of Quantitative Spectroscopy and Radiative Transfer 73 (2002) 249–259]","year":2024,"lang":"en","type":"erratum","venue":"Journal of Quantitative Spectroscopy and Radiative Transfer","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"","keywords":"Radiative transfer; Atmospheric radiative transfer codes; Environmental science; Radiation; Atmospheric sciences; Physics; Optics","score_opus":0.021256052342802603,"score_gpt":0.28539609527187193,"score_spread":0.26414004292906934,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404872196","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"methods","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.10382013,0.021579316,0.8642149,0.001643306,0.0051546893,0.0019220813,0.0008313186,0.000029413743,0.00080485054],"genre_scores_gemma":[0.6499126,0.058078155,0.25800225,0.0025438983,0.0031030811,0.0003073774,0.00012654036,0.0011833447,0.026742736],"study_design_codex":"not_applicable","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99382734,0.00044620398,0.0022532935,0.0011230025,0.0012347839,0.0011153537],"domain_scores_gemma":[0.9971593,0.00073165563,0.00048045476,0.0002684447,0.00037867852,0.0009814505],"candidate_categories":["metaepi_narrow","research_integrity"],"consensus_categories":["metaepi_narrow"],"category_scores_codex":[0.0013981168,0.001385341,0.0027521118,0.0001008425,0.00051181915,0.00028201548,0.00056621176,0.00066096534,0.00057742157],"category_scores_gemma":[0.00017518303,0.0011165079,0.0007639847,0.00092526217,0.0013471072,0.001060128,0.00005926849,0.002348348,0.000019530957],"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":[0.03542963,0.0029377996,0.0016673902,0.002615161,0.012113398,0.0006173512,0.26964113,0.06133677,0.10153695,0.07283028,0.43494517,0.0043289694],"study_design_scores_gemma":[0.051310267,0.14561892,0.032416455,0.0073109283,0.018188162,0.0014317128,0.041441564,0.534688,0.022110337,0.054056495,0.07815812,0.0132690305],"about_ca_topic_score_codex":0.00006263574,"about_ca_topic_score_gemma":0.00016149973,"teacher_disagreement_score":0.6062126,"about_ca_system_score_codex":0.0006918901,"about_ca_system_score_gemma":0.00068113575,"threshold_uncertainty_score":0.99995327},"labels":[],"label_agreement":null},{"id":"W4405368870","doi":"10.5194/egusphere-2024-3214-rc2","title":"Comment on egusphere-2024-3214","year":2024,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Office of Naval Research","keywords":"Settling; Aerosol; Fog; Environmental science; Entrainment (biomusicology); Deposition (geology); Atmospheric sciences; Liquid water path; Flux (metallurgy); Meteorology; Chemistry; Physics; Geology; Environmental engineering; Geomorphology","score_opus":0.018621657537863618,"score_gpt":0.27323809477852357,"score_spread":0.25461643724065997,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405368870","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000007249124,0.007318356,0.00010331826,0.3402732,0.0035821071,0.00039577094,0.000053082564,0.000107201595,0.64815974],"genre_scores_gemma":[0.00003385403,0.0029453952,0.0008441315,0.18020964,0.00025002865,0.00007851154,0.00010015108,0.000055550114,0.81548274],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9976145,0.000044990895,0.0003731885,0.00074894674,0.0008120318,0.00040633298],"domain_scores_gemma":[0.99896884,0.0000489114,0.00009633588,0.00070282386,0.000006008668,0.0001770547],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000247601,0.0004591708,0.0005053811,8.863822e-7,0.0000835565,0.00004675508,0.00049233966,0.00023322373,0.3711721],"category_scores_gemma":[0.000016827766,0.00032387525,0.00028139632,0.00025023168,0.00012224789,0.000031633932,0.000617091,0.0006270439,0.05451141],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002017004,0.000057363257,0.000017289256,0.0003715796,0.000030450361,0.000022361402,0.000012587002,0.000016214959,9.0809954e-7,0.00034948936,0.9818958,0.017223906],"study_design_scores_gemma":[0.00006190812,0.00011585082,0.000025954752,0.0012016492,0.00011473312,0.0000042095876,0.000013977855,0.000059275146,0.000005901386,0.00022254049,0.9977657,0.0004082927],"about_ca_topic_score_codex":0.0015237754,"about_ca_topic_score_gemma":0.00032907247,"teacher_disagreement_score":0.3166607,"about_ca_system_score_codex":0.00040898702,"about_ca_system_score_gemma":0.000025251342,"threshold_uncertainty_score":0.9999213},"labels":[],"label_agreement":null},{"id":"W4405848644","doi":"10.1371/journal.pone.0311990","title":"CAECENET: An automatic system processing photometer and ceilometer data from different networks to provide columnar and vertically-resolved aerosol properties","year":2024,"lang":"en","type":"article","venue":"PLoS ONE","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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":"Agencia Estatal de Investigación; European Metrology Programme for Innovation and Research; Junta de Castilla y León; Ministerio de Ciencia e Innovación; European Commission","keywords":"Ceilometer; Aerosol; Photometer; Environmental science; Radiance; Sky; Sun photometer; Remote sensing; Meteorology; Range (aeronautics); Geology; Physics; Optics; Materials science","score_opus":0.05143266816073483,"score_gpt":0.2241270761293385,"score_spread":0.17269440796860366,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405848644","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":[0.99573404,0.000985604,0.0020119587,0.00017065651,0.00004100363,0.00073206617,0.00002429106,0.000210205,0.00009019835],"genre_scores_gemma":[0.9928412,0.000028324182,0.0064515257,0.00020603009,0.00008731023,0.000121029225,0.0000196714,0.000042792934,0.00020210564],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9982169,0.00005990197,0.00027325322,0.00071914133,0.0003877408,0.00034304752],"domain_scores_gemma":[0.9991484,0.00004189561,0.000034286266,0.0004912282,0.0000073950423,0.00027678526],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012807413,0.00022335185,0.00030831902,0.00000360927,0.00015679038,0.000428318,0.00030872505,0.00008063687,0.00022489748],"category_scores_gemma":[0.000023587174,0.00016294149,0.00001505103,0.00014297875,0.00015042641,0.00041927613,0.00069378904,0.0001412133,0.000053619657],"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":[0.00032469138,0.0026232142,0.15739757,0.0040512527,0.0008349581,0.00013998887,0.00832307,0.00029928112,0.68996024,0.000011554085,0.00144783,0.13458635],"study_design_scores_gemma":[0.00022019936,0.0002576194,0.021550767,0.0011584493,0.00023396841,0.000003828561,0.0002776754,0.97253376,0.0033438224,0.0000069167827,0.00007372896,0.00033926227],"about_ca_topic_score_codex":0.00032435232,"about_ca_topic_score_gemma":0.00021685132,"teacher_disagreement_score":0.9722345,"about_ca_system_score_codex":0.00010379078,"about_ca_system_score_gemma":0.000012345515,"threshold_uncertainty_score":0.6644561},"labels":[],"label_agreement":null},{"id":"W4406112213","doi":"10.5194/acp-25-27-2025","title":"Remote-sensing detectability of airborne Arctic dust","year":2025,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"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 du Québec à Montréal; National Research Council Canada; Université de Sherbrooke","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency","keywords":"Arctic; Environmental science; Snow; Albedo (alchemy); Asian Dust; Atmospheric sciences; Remote sensing; Geology; Meteorology; Aerosol; Geography; Oceanography","score_opus":0.004574316921621247,"score_gpt":0.20545871549944186,"score_spread":0.20088439857782062,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406112213","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":[0.95821214,0.000089308356,0.020609584,0.00006187742,0.000031555122,0.00006600492,0.0000011465105,0.00002510924,0.020903282],"genre_scores_gemma":[0.96585363,0.000026487729,0.031186925,0.00008763343,0.000032450786,4.778809e-7,0.0000015396768,0.000007762664,0.0028030917],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9992272,0.000014008674,0.00018197748,0.000281038,0.00011920087,0.00017653141],"domain_scores_gemma":[0.99950033,0.000056777935,0.00006718963,0.00030630777,0.000012305893,0.000057060046],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00007532662,0.00013901819,0.00018646367,6.149888e-9,0.00009050958,0.00001031326,0.000109266446,0.000073491945,0.001068738],"category_scores_gemma":[0.000027771968,0.00013421442,0.000058566446,0.00028149,0.00031296883,0.000048185997,0.00011837161,0.00012400575,0.000011220316],"study_design_candidate":"design_other","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":[0.000024583025,0.0000533644,0.025724411,0.00016280639,0.000019359086,0.0000020510295,0.00012327256,0.0006047435,0.038211145,0.000020182448,0.00015725965,0.9348968],"study_design_scores_gemma":[0.001816912,0.00012254034,0.3033939,0.00031740687,0.00027296218,0.000021445543,0.0007735074,0.3422588,0.30144286,0.034580283,0.013752697,0.0012466721],"about_ca_topic_score_codex":0.00058537454,"about_ca_topic_score_gemma":0.000006117045,"teacher_disagreement_score":0.93365014,"about_ca_system_score_codex":0.00006759278,"about_ca_system_score_gemma":0.00001680725,"threshold_uncertainty_score":0.99984443},"labels":[],"label_agreement":null},{"id":"W4406255972","doi":"10.22541/essoar.173655440.05475709/v1","title":"Ship-based lidar evaluation of Southern Ocean clouds in the storm-resolving general circulation model ICON and the ERA5 and MERRA-2 reanalyses","year":2025,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Impact","funders":"European Commission","keywords":"Storm; Circulation (fluid dynamics); Environmental science; Icon; General Circulation Model; Climatology; Meteorology; Oceanography; Geology; Geography; Computer science; Climate change; Engineering; Aerospace engineering","score_opus":0.032645109353025774,"score_gpt":0.28205877062366136,"score_spread":0.24941366127063558,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406255972","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":[0.98679966,0.00036899617,0.007992871,0.00057502056,0.00003724094,0.00065080996,0.0000146074235,0.000012428123,0.0035483763],"genre_scores_gemma":[0.9979479,0.000036278812,0.0014343332,0.00030529618,0.000026357517,0.000028596183,0.00001646431,0.000008839315,0.00019593663],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99796,0.0004734963,0.0003519468,0.00039563776,0.0006670121,0.00015195526],"domain_scores_gemma":[0.9991753,0.00012777389,0.00021279599,0.0004300378,0.000025747733,0.000028330098],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002658212,0.00019985683,0.0002606878,0.0000047244835,0.00013765869,0.00006275476,0.00027430433,0.00014680026,0.00017693892],"category_scores_gemma":[0.00007943643,0.00011299435,0.00007973477,0.00013535786,0.00031990572,0.000047060996,0.00031850848,0.00025767874,0.0000015370155],"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":[0.000050892995,0.00003512508,0.1037749,0.0000293614,0.000030296978,2.4385062e-7,0.0056361104,0.8856927,0.0002441323,0.0003914435,0.00006919144,0.0040455894],"study_design_scores_gemma":[0.0006852974,0.000008785802,0.052056953,0.00003358385,0.00020005858,4.0420048e-7,0.0010438341,0.9404178,0.00003561915,0.005387444,0.000005327665,0.00012485869],"about_ca_topic_score_codex":0.0051702247,"about_ca_topic_score_gemma":0.0015501719,"teacher_disagreement_score":0.05472512,"about_ca_system_score_codex":0.00012075242,"about_ca_system_score_gemma":0.00007362753,"threshold_uncertainty_score":0.7815867},"labels":[],"label_agreement":null},{"id":"W4406379516","doi":"10.5194/gmd-18-101-2025","title":"Orbital-Radar v1.0.0: a tool to transform suborbital radar observations to synthetic EarthCARE cloud radar data","year":2025,"lang":"en","type":"article","venue":"Geoscientific model development","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Brookhaven National Laboratory; Stony Brook University; Universität zu Köln; European Space Agency; McGill University; U.S. Department of Energy","keywords":"Radar; Remote sensing; Meteorology; Cloud computing; Satellite; Computer science; Environmental science; Cloud top; Aerospace engineering; Geology; Geography; Engineering","score_opus":0.030208381415624343,"score_gpt":0.2457831481432158,"score_spread":0.21557476672759146,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406379516","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":[0.7386657,0.00006738509,0.24777721,0.003224386,0.0013543485,0.0014527658,0.00040000473,0.00016362347,0.0068945535],"genre_scores_gemma":[0.59903175,0.000009611882,0.3468558,0.001762117,0.000042226948,0.00022413128,0.0004313369,0.00005166817,0.051591374],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9954645,0.00004099532,0.0007964431,0.001651194,0.001085121,0.00096176536],"domain_scores_gemma":[0.9976974,0.0000368832,0.0000789088,0.0017169296,0.000051605108,0.0004182627],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000881135,0.00043672614,0.00037963132,0.000026815944,0.00094432273,0.00024872035,0.0017772223,0.00012780221,0.00081564876],"category_scores_gemma":[0.0000899671,0.0004193447,0.000089898116,0.0016064957,0.0001726884,0.00043660987,0.0015412669,0.00020727818,0.0012894318],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003392432,0.0016252521,0.009282469,0.00030570757,0.00028031744,0.00012306949,0.018684935,0.044762816,0.030032663,0.005169411,0.5510191,0.33837506],"study_design_scores_gemma":[0.0008335009,0.00008317124,0.033085346,0.0002228134,0.0000818695,0.000013857992,0.0010572746,0.043256667,0.003952447,0.001259616,0.914454,0.0016994688],"about_ca_topic_score_codex":0.00048661567,"about_ca_topic_score_gemma":0.0012471292,"teacher_disagreement_score":0.3634349,"about_ca_system_score_codex":0.00056446216,"about_ca_system_score_gemma":0.00043789198,"threshold_uncertainty_score":0.99982584},"labels":[],"label_agreement":null},{"id":"W4406399318","doi":"10.1016/0967-0653(94)92864-9","title":"10.1016/0967-0653(94)92864-9","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Cloud computing; Computer science","score_opus":0.003924475145999713,"score_gpt":0.15774377910006743,"score_spread":0.1538193039540677,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406399318","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.008137197,0.00001923365,0.0000042321185,0.00022158297,0.0000015230252,0.00012796413,0.000003888961,0.00013944227,0.9913449],"genre_scores_gemma":[0.0016124202,2.5307472e-7,0.000504846,0.00013638384,0.00006793509,0.000015004735,0.0000036969968,0.00002774208,0.9976317],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99901927,0.000021509812,0.00013805626,0.00027491144,0.00023378604,0.00031245087],"domain_scores_gemma":[0.99948984,0.000015221453,0.000022084736,0.00028402903,0.0000029140867,0.00018588205],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00008741878,0.00013500683,0.00012196308,7.840743e-7,0.00010699704,0.000027143944,0.00027374786,0.000056133988,0.999746],"category_scores_gemma":[0.000008305657,0.000121642435,0.00005212374,0.00019609569,0.000079506564,0.00009938411,0.00009527189,0.000081440565,0.99948496],"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":[0.000020286032,0.000039561422,0.0000050884782,7.69618e-7,0.0000038530793,0.0000045343636,0.00002393689,0.0006103335,0.000057568774,3.7076217e-7,0.35696447,0.64226925],"study_design_scores_gemma":[0.00011919489,0.00009859723,0.00070528453,0.000003593945,0.0000072885396,0.000004808911,0.0000017499024,0.00034422285,0.000061093444,0.000010428734,0.99846405,0.00017969019],"about_ca_topic_score_codex":0.00013695126,"about_ca_topic_score_gemma":9.769714e-7,"teacher_disagreement_score":0.64208955,"about_ca_system_score_codex":0.00007131773,"about_ca_system_score_gemma":0.0000053596686,"threshold_uncertainty_score":0.49604344},"labels":[],"label_agreement":null},{"id":"W4406415864","doi":"10.1016/s0967-0653(97)80793-4","title":"10.1016/s0967-0653(97)80793-4","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Transmittance; Planetary boundary layer; Layer (electronics); Environmental science; Content (measure theory); Boundary layer; Remote sensing; Materials science; Geology; Physics; Mathematics; Optoelectronics; Composite material; Mathematical analysis; Mechanics","score_opus":0.004680173171104193,"score_gpt":0.16109368637627958,"score_spread":0.15641351320517538,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406415864","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.002957181,0.000020580706,0.0000041584976,0.0002044272,0.0000013897837,0.00013110854,0.0000035273808,0.00008837388,0.99658924],"genre_scores_gemma":[0.00043556705,3.0644813e-7,0.00053898356,0.00012515025,0.00006633626,0.000015120079,0.000003667881,0.000020538248,0.9987943],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990113,0.000021894593,0.00013972359,0.0002768853,0.00023587837,0.00031436523],"domain_scores_gemma":[0.99948573,0.00001555558,0.000022515685,0.0002857025,0.000003019261,0.00018749907],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00008878856,0.00013770619,0.00012363071,8.0680996e-7,0.000108127846,0.000027816724,0.0002759626,0.000056995927,0.9999187],"category_scores_gemma":[0.000008607797,0.00012355119,0.000053016054,0.00019643019,0.00008019613,0.00010042944,0.00009762948,0.00008315034,0.9999201],"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":[0.000022441327,0.00003804387,0.0000022225556,7.580506e-7,0.0000037370378,0.000004328496,0.0000234889,0.00050065777,0.000023482185,2.8012388e-7,0.123761415,0.8756192],"study_design_scores_gemma":[0.0001343284,0.00010032232,0.00014632754,0.0000037145899,0.0000074036207,0.000004407696,0.0000019129823,0.00031056613,0.00006428799,0.000010298999,0.99903446,0.00018195272],"about_ca_topic_score_codex":0.000138957,"about_ca_topic_score_gemma":9.537094e-7,"teacher_disagreement_score":0.8754372,"about_ca_system_score_codex":0.000070923794,"about_ca_system_score_gemma":0.000005382284,"threshold_uncertainty_score":0.50382715},"labels":[],"label_agreement":null},{"id":"W4406435623","doi":"10.1016/0967-0653(94)91145-2","title":"10.1016/0967-0653(94)91145-2","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Cloud computing; Cloud condensation nuclei; Boundary layer; Layer (electronics); Environmental science; Condensation; Atmospheric sciences; Meteorology; Climatology; Geology; Oceanography; Geography; Materials science; Physics; Computer science; Mechanics; Nanotechnology","score_opus":0.00400486185700772,"score_gpt":0.1585007956855564,"score_spread":0.15449593382854868,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406435623","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00865943,0.000019382414,0.0000042986035,0.00021829105,0.0000015081818,0.00012816294,0.000004008217,0.00008887854,0.990876],"genre_scores_gemma":[0.0015140594,2.7194756e-7,0.0005124686,0.00013780709,0.00006745303,0.000014998912,0.000004398574,0.000020366155,0.99772817],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99901825,0.000021481621,0.00013809971,0.000275306,0.00023407026,0.00031281784],"domain_scores_gemma":[0.9994897,0.000015144345,0.000022095037,0.0002851254,0.0000029161959,0.00018497283],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0000872953,0.0001351277,0.0001222465,7.875304e-7,0.00010703198,0.000027378721,0.00027497532,0.000055694065,0.9998319],"category_scores_gemma":[0.000008291909,0.00012177594,0.00005213316,0.00019714725,0.000079124125,0.000099584,0.000095721916,0.00008204181,0.99942994],"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":[0.000019550704,0.000039126768,0.0000044919348,7.363359e-7,0.0000037160721,0.0000043708997,0.000024270059,0.0005485293,0.00006557529,3.200685e-7,0.33767053,0.66161877],"study_design_scores_gemma":[0.00011890495,0.000100091216,0.00064046326,0.000003632479,0.000007250556,0.00000474796,0.0000017716354,0.00033889036,0.00006172155,0.000009944973,0.9985328,0.00017983752],"about_ca_topic_score_codex":0.00014323238,"about_ca_topic_score_gemma":9.728232e-7,"teacher_disagreement_score":0.66143894,"about_ca_system_score_codex":0.00007051343,"about_ca_system_score_gemma":0.0000053317576,"threshold_uncertainty_score":0.49658787},"labels":[],"label_agreement":null},{"id":"W4406446102","doi":"10.1016/s0967-0653(98)80215-9","title":"10.1016/s0967-0653(98)80215-9","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Marine stratocumulus; Boundary layer; Atmospheric sciences; Simple (philosophy); Environmental science; Layer (electronics); Meteorology; Geology; Chemistry; Geography; Physics; Mechanics; Aerosol","score_opus":0.004169553610003716,"score_gpt":0.16182976401151478,"score_spread":0.15766021040151107,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406446102","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.004895964,0.00001658227,0.0000034296809,0.00021278343,0.0000013638245,0.00012427516,0.0000033553083,0.00008347057,0.99465877],"genre_scores_gemma":[0.0007187644,2.949942e-7,0.0005219653,0.00012062,0.00006747148,0.000014460923,0.0000035994133,0.000019942563,0.9985329],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99904054,0.000021285936,0.00013496669,0.0002691227,0.00022940713,0.00030465372],"domain_scores_gemma":[0.9995002,0.000014599711,0.000021626818,0.00027908522,0.0000029472612,0.00018153088],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000085700514,0.00013281722,0.00012465523,7.821402e-7,0.00010154364,0.0000271151,0.0002658625,0.000055624645,0.9999392],"category_scores_gemma":[0.000008052599,0.000119408556,0.000051477517,0.00019153419,0.000075828924,0.000096216754,0.0000947715,0.00008052863,0.9998372],"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":[0.000019191626,0.00003530783,0.0000015291746,7.092904e-7,0.0000037194895,0.0000040538607,0.000022220576,0.00045517756,0.00003592894,2.9058927e-7,0.456201,0.5432209],"study_design_scores_gemma":[0.0001232657,0.00009301546,0.0003226638,0.0000037127857,0.000007438858,0.00000413267,0.0000018170391,0.0003027263,0.00006295029,0.000009857174,0.9988923,0.00017608817],"about_ca_topic_score_codex":0.00015605341,"about_ca_topic_score_gemma":0.0000010816533,"teacher_disagreement_score":0.5430448,"about_ca_system_score_codex":0.00006987359,"about_ca_system_score_gemma":0.000005432831,"threshold_uncertainty_score":0.48693398},"labels":[],"label_agreement":null},{"id":"W4406446805","doi":"10.1016/s0967-0653(98)84038-6","title":"10.1016/s0967-0653(98)84038-6","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Satellite; Cloud computing; Meteorology; Environmental science; Climatology; Geography; Geology; Computer science; Engineering; Aerospace engineering; Operating system","score_opus":0.004094873045780378,"score_gpt":0.16082043608203864,"score_spread":0.15672556303625826,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406446805","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0050979275,0.000017335047,0.0000034494387,0.00021349563,0.0000013692008,0.00012486069,0.0000033083845,0.0000855557,0.9944527],"genre_scores_gemma":[0.00069291564,3.116641e-7,0.0005148723,0.00011875159,0.00006988366,0.000014524952,0.0000033433341,0.000019865727,0.99856555],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99904656,0.000020734382,0.00013389338,0.00026769764,0.00022902086,0.00030207835],"domain_scores_gemma":[0.99950224,0.000014487221,0.000021878566,0.00027824892,0.0000028689287,0.0001802763],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00008447642,0.00013225581,0.00012339014,7.683232e-7,0.00009984288,0.000025858524,0.00027143434,0.000054573906,0.9999381],"category_scores_gemma":[0.000008074811,0.00011880133,0.000051070543,0.00018400088,0.00007674683,0.00009263939,0.00009480992,0.00007992723,0.99984187],"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":[0.00001913608,0.00003331873,0.0000014878658,6.733544e-7,0.0000035569324,0.000003892915,0.000021632912,0.00045563222,0.00003358487,2.6169036e-7,0.46224552,0.5371813],"study_design_scores_gemma":[0.00012441551,0.00009284426,0.0003453478,0.0000036208023,0.0000072548296,0.0000041115277,0.0000017877527,0.00029203328,0.00006272276,0.000009686751,0.9988812,0.00017493925],"about_ca_topic_score_codex":0.0001881337,"about_ca_topic_score_gemma":0.0000012014491,"teacher_disagreement_score":0.5370064,"about_ca_system_score_codex":0.00007134976,"about_ca_system_score_gemma":0.0000054164575,"threshold_uncertainty_score":0.48445776},"labels":[],"label_agreement":null},{"id":"W4406462086","doi":"10.1016/0967-0653(96)85712-7","title":"10.1016/0967-0653(96)85712-7","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Cloud computing; Particle (ecology); Scattering; Environmental science; Atmospheric sciences; Remote sensing; Geology; Physics; Oceanography; Optics; Computer science","score_opus":0.003973965682462819,"score_gpt":0.15707051594655952,"score_spread":0.1530965502640967,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406462086","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.010948974,0.000016986041,0.000003868414,0.00021204232,0.0000015200116,0.0001252224,0.0000041491962,0.00008826789,0.98859894],"genre_scores_gemma":[0.0015283397,2.3511602e-7,0.00050111813,0.00012971592,0.00006638161,0.0000149760035,0.00000441289,0.000019829173,0.99773496],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990235,0.000021277909,0.00013752743,0.0002740577,0.00023216603,0.00031144993],"domain_scores_gemma":[0.999492,0.000015030003,0.000021829082,0.0002824184,0.0000029507796,0.00018576848],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00008639575,0.00013463151,0.000121619465,7.7743107e-7,0.00010692357,0.000026957707,0.0002721374,0.000055909706,0.999838],"category_scores_gemma":[0.00000835513,0.00012134263,0.000051936775,0.00019528883,0.000078006626,0.000096239244,0.000090406924,0.00008136041,0.9994308],"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":[0.000019859042,0.000038702015,0.0000064897035,7.747684e-7,0.0000038066328,0.0000043604673,0.000024716383,0.00059510936,0.00006616257,3.3371256e-7,0.33884653,0.6603932],"study_design_scores_gemma":[0.00011894693,0.00009823702,0.00061619637,0.0000035430821,0.0000071991303,0.0000045258917,0.0000019073962,0.00032868603,0.00007533578,0.000009869303,0.99855644,0.00017914636],"about_ca_topic_score_codex":0.00013301052,"about_ca_topic_score_gemma":9.568275e-7,"teacher_disagreement_score":0.660214,"about_ca_system_score_codex":0.00006989883,"about_ca_system_score_gemma":0.000005235012,"threshold_uncertainty_score":0.49482086},"labels":[],"label_agreement":null},{"id":"W4406463652","doi":"10.1016/0967-0653(96)83396-5","title":"10.1016/0967-0653(96)83396-5","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Remote sensing; Satellite; Environmental science; Geology; Aerospace engineering; Engineering","score_opus":0.003916724511149896,"score_gpt":0.15699603974613743,"score_spread":0.15307931523498755,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406463652","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.01016568,0.000018206647,0.0000037474115,0.00022584987,0.000001513586,0.00012708921,0.0000040384375,0.000088619345,0.9893653],"genre_scores_gemma":[0.0017340941,2.6498583e-7,0.0004971109,0.00013826315,0.00006556265,0.000014900216,0.0000043898526,0.00002035764,0.99752504],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990201,0.000021559974,0.00013781634,0.00027479397,0.00023347873,0.0003122718],"domain_scores_gemma":[0.9994882,0.000015182866,0.000022057544,0.00028577162,0.0000028844422,0.00018594385],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000087573986,0.00013536192,0.0001220719,7.833172e-7,0.00010719183,0.000027353655,0.00027410634,0.000046015863,0.9998339],"category_scores_gemma":[0.000008214601,0.000121678124,0.000052097206,0.00019442229,0.000079397214,0.000099245335,0.000095093885,0.000081343045,0.9994203],"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":[0.000019661593,0.00003872234,0.0000060708044,7.6391916e-7,0.0000037845448,0.000005252088,0.0000218987,0.0005620927,0.00006202983,3.3137488e-7,0.33916575,0.66011363],"study_design_scores_gemma":[0.000117707816,0.00009884252,0.0005974999,0.0000035751752,0.000007219527,0.00000588138,0.0000018460074,0.0003348338,0.000074415315,0.0000104169485,0.99856806,0.00017969622],"about_ca_topic_score_codex":0.00014045523,"about_ca_topic_score_gemma":0.0000010983701,"teacher_disagreement_score":0.659934,"about_ca_system_score_codex":0.00007180656,"about_ca_system_score_gemma":0.00000533832,"threshold_uncertainty_score":0.496189},"labels":[],"label_agreement":null},{"id":"W4406465432","doi":"10.5194/acp-25-535-2025","title":"OMPS-LP aerosol extinction coefficients and their applicability in GloSSAC","year":2025,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","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":"Science Mission Directorate; Nuclear Safety and Security Commission; University of Exeter; Aeronautics Research Mission Directorate; National Aeronautics and Space Administration","keywords":"Extinction (optical mineralogy); Aerosol; Atmospheric sciences; Environmental science; Meteorology; Chemistry; Physics; Mineralogy","score_opus":0.00353460889616534,"score_gpt":0.20149661743556985,"score_spread":0.19796200853940452,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406465432","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":[0.9768495,0.00013799188,0.008493173,0.000067057685,0.000028066293,0.0001399872,0.0000028106806,0.000029771874,0.01425166],"genre_scores_gemma":[0.99659806,0.00006978592,0.0013575257,0.00013618395,0.000033844834,0.000027855152,0.000004602084,0.000007721292,0.001764389],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99910796,0.000015171802,0.0001655256,0.00041320885,0.000087416505,0.00021072749],"domain_scores_gemma":[0.99961334,0.00004267724,0.000042817646,0.00022871878,0.0000053270896,0.00006713532],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000912329,0.00017564058,0.00017743446,9.965034e-9,0.00012509215,0.000028110006,0.00010553542,0.000088621586,0.00058526976],"category_scores_gemma":[0.000008088053,0.0001550191,0.000032085783,0.00030118146,0.00028258286,0.00007210999,0.00015458994,0.00014311711,0.00001069189],"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":[0.000052880372,0.00034654833,0.26646325,0.00010547667,0.000016796354,0.0000020000814,0.00044618902,0.0015958797,0.0383622,0.000035274006,0.00038738805,0.6921861],"study_design_scores_gemma":[0.0045004664,0.00015311329,0.5639256,0.0001859041,0.00009118906,0.000026664731,0.0026437088,0.28431708,0.08454361,0.014910346,0.042716105,0.001986218],"about_ca_topic_score_codex":0.00013687412,"about_ca_topic_score_gemma":0.000008390283,"teacher_disagreement_score":0.6901999,"about_ca_system_score_codex":0.00007806152,"about_ca_system_score_gemma":0.000010338725,"threshold_uncertainty_score":0.6408293},"labels":[],"label_agreement":null},{"id":"W4406480431","doi":"10.1016/0967-0653(94)93865-2","title":"10.1016/0967-0653(94)93865-2","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Lidar; Southern Hemisphere; Extinction (optical mineralogy); Backscatter (email); Environmental science; Atmospheric sciences; Northern Hemisphere; Remote sensing; Oceanography; Climatology; Geology; Mineralogy","score_opus":0.00397858114752155,"score_gpt":0.1582285825288953,"score_spread":0.15425000138137374,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406480431","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.009787846,0.000019426208,0.0000041296325,0.0002192102,0.0000015090857,0.00012811841,0.000003938742,0.00008887289,0.9897469],"genre_scores_gemma":[0.0015763617,2.596981e-7,0.00051027007,0.00014723287,0.00006727135,0.000014996511,0.000004322443,0.00002038158,0.9976589],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990177,0.00002160602,0.0001381909,0.00027541333,0.0002339952,0.000313071],"domain_scores_gemma":[0.9994894,0.000015262864,0.000022104738,0.00028523937,0.00000291732,0.0001850307],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000087521934,0.00013519185,0.0001223528,7.8733564e-7,0.000107293075,0.000027426197,0.00027498193,0.000056212444,0.999834],"category_scores_gemma":[0.000008318682,0.000121824785,0.000052153493,0.00019678596,0.00007948279,0.000099569654,0.00009426466,0.00008155436,0.99941593],"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":[0.000020104964,0.000039181017,0.0000048019947,7.563622e-7,0.0000038108624,0.000004487163,0.000023882274,0.00085151615,0.00006989676,2.9851932e-7,0.33746967,0.6615116],"study_design_scores_gemma":[0.00011925953,0.00009843094,0.00055510417,0.0000035956896,0.0000072564444,0.000004815644,0.0000017619858,0.0004165492,0.000055113436,0.000010306041,0.99854785,0.0001799273],"about_ca_topic_score_codex":0.0001412758,"about_ca_topic_score_gemma":9.733473e-7,"teacher_disagreement_score":0.66133165,"about_ca_system_score_codex":0.00007141933,"about_ca_system_score_gemma":0.000005347364,"threshold_uncertainty_score":0.49678704},"labels":[],"label_agreement":null},{"id":"W4406480904","doi":"10.1016/0967-0653(93)91224-z","title":"10.1016/0967-0653(93)91224-z","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Cluster (spacecraft); Cloud computing; Climatology; Geography; Geology; Computer science","score_opus":0.0035130651623527876,"score_gpt":0.1530800778206396,"score_spread":0.1495670126582868,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406480904","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.008971333,0.000017903427,0.000004212378,0.00020184918,0.0000015065319,0.00012806531,0.0000039465267,0.00008851948,0.99058264],"genre_scores_gemma":[0.0016114194,2.445112e-7,0.0005246965,0.00013505424,0.00006647224,0.000014594199,0.000004471422,0.000020304642,0.9976227],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99902505,0.000021574262,0.00013724684,0.0002741212,0.00023308855,0.00030892718],"domain_scores_gemma":[0.9994901,0.0000144541045,0.000022324348,0.0002844115,0.0000030030158,0.00018573702],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00008754178,0.00013504412,0.00012248279,7.836462e-7,0.00010603647,0.000028306697,0.00027638924,0.00005593844,0.9998295],"category_scores_gemma":[0.000007988371,0.000121404,0.000050919643,0.00020284811,0.00007969302,0.00010124453,0.00009640707,0.0000806963,0.9994248],"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":[0.000020637437,0.00004190243,0.0000051132643,7.8130256e-7,0.0000037675015,0.0000046528085,0.000024326404,0.0006250508,0.000064318614,3.4079875e-7,0.33555984,0.66364926],"study_design_scores_gemma":[0.00012139315,0.000099190394,0.00054142857,0.0000035923883,0.0000071933187,0.0000045330166,0.0000018619924,0.00035412982,0.00006211507,0.000010541598,0.9986148,0.00017925941],"about_ca_topic_score_codex":0.00013857485,"about_ca_topic_score_gemma":9.1371766e-7,"teacher_disagreement_score":0.66347003,"about_ca_system_score_codex":0.00006993734,"about_ca_system_score_gemma":0.0000054561838,"threshold_uncertainty_score":0.49507114},"labels":[],"label_agreement":null},{"id":"W4406483205","doi":"10.1016/0967-0653(96)86181-3","title":"10.1016/0967-0653(96)86181-3","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Marine stratocumulus; Cloud computing; Geology; Wavelet; Meteorology; Environmental science; Climatology; Computer science; Geography; Artificial intelligence","score_opus":0.003917726611167818,"score_gpt":0.15698236119243283,"score_spread":0.153064634581265,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406483205","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.011501189,0.000017718823,0.0000042043,0.00021886238,0.000001583771,0.00012730379,0.0000039204133,0.00008856712,0.98803663],"genre_scores_gemma":[0.0015978927,2.6196085e-7,0.00050395285,0.00013656716,0.00006798757,0.000014955863,0.0000043725554,0.000020376265,0.9976536],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990183,0.000021598913,0.0001380635,0.00027522462,0.00023348484,0.00031332855],"domain_scores_gemma":[0.99948823,0.000015174971,0.000022083486,0.00028498037,0.0000029078572,0.00018663828],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00008794042,0.00013545058,0.00012216743,7.887407e-7,0.00010722333,0.00002730295,0.0002734667,0.000056148074,0.9998404],"category_scores_gemma":[0.000008332911,0.00012175425,0.000052217463,0.00019707959,0.00007920905,0.000099265264,0.000095567695,0.00008138259,0.999435],"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":[0.000019952138,0.00003888921,0.000006639276,7.688681e-7,0.0000037879029,0.000004356091,0.000024824241,0.00056706514,0.000067126144,3.137101e-7,0.34968245,0.6495838],"study_design_scores_gemma":[0.000119451906,0.00009759144,0.0005290315,0.0000035997602,0.0000072836046,0.0000048917586,0.0000018639286,0.00033796614,0.00007547353,0.000010067424,0.99863297,0.00017980524],"about_ca_topic_score_codex":0.00013123211,"about_ca_topic_score_gemma":8.4442877e-7,"teacher_disagreement_score":0.649404,"about_ca_system_score_codex":0.000070928836,"about_ca_system_score_gemma":0.000005307395,"threshold_uncertainty_score":0.49649942},"labels":[],"label_agreement":null},{"id":"W4406493937","doi":"10.1016/0967-0653(93)94645-f","title":"10.1016/0967-0653(93)94645-f","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Planetary boundary layer; Atmospheric sciences; Boundary layer; Layer (electronics); Boundary (topology); Environmental science; Geology; Climatology; Meteorology; Geography; Mathematics; Materials science; Physics; Mathematical analysis; Mechanics; Composite material","score_opus":0.003501426390273531,"score_gpt":0.1530649897585969,"score_spread":0.14956356336832335,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406493937","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0081334375,0.000017845205,0.000004491209,0.00021058031,0.0000015448154,0.00012927197,0.00000399965,0.00008780998,0.99141103],"genre_scores_gemma":[0.001499587,2.5763973e-7,0.00048538696,0.00013565438,0.00006881948,0.000014968113,0.0000045088163,0.00002020027,0.9977706],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990221,0.0000212675,0.0001375033,0.00027450765,0.00023313344,0.00031144073],"domain_scores_gemma":[0.9994906,0.000014645134,0.000021953654,0.00028390536,0.000002917557,0.00018595239],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000085884436,0.00013529006,0.00012178752,7.8632746e-7,0.00010810737,0.000027439952,0.0002734494,0.00005605034,0.9998411],"category_scores_gemma":[0.000007837493,0.00012051419,0.000051619976,0.00019550558,0.00008060419,0.00010028042,0.0000939599,0.00008093745,0.99942046],"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":[0.000020291123,0.000040423936,0.0000049762057,8.0453833e-7,0.000003978741,0.0000047121857,0.000025801155,0.00055699045,0.00006859211,4.0169283e-7,0.33820346,0.6610696],"study_design_scores_gemma":[0.00012041227,0.000096798394,0.00057067594,0.0000036266817,0.0000071614563,0.000005023799,0.0000018222457,0.00036101945,0.000056615994,0.000011309558,0.99858594,0.00017961925],"about_ca_topic_score_codex":0.00011539176,"about_ca_topic_score_gemma":0.0000010376644,"teacher_disagreement_score":0.66089,"about_ca_system_score_codex":0.000072544535,"about_ca_system_score_gemma":0.000005371364,"threshold_uncertainty_score":0.4914426},"labels":[],"label_agreement":null},{"id":"W4406495188","doi":"10.1016/0967-0653(96)80777-0","title":"10.1016/0967-0653(96)80777-0","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Lidar; Environmental science; Remote sensing; Atmospheric sciences; Meteorology; Geography; Geology","score_opus":0.003960458895579254,"score_gpt":0.15746738327849708,"score_spread":0.15350692438291783,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406495188","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.010087388,0.000017500897,0.0000041764274,0.00022865465,0.0000015133528,0.0001290402,0.0000039977404,0.00008992373,0.9894378],"genre_scores_gemma":[0.0015822737,2.6348624e-7,0.0005245111,0.00013818816,0.000066553155,0.000015169948,0.000004460763,0.000020679858,0.9976479],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.999007,0.000021960197,0.00013981474,0.000278419,0.00023632728,0.00031651577],"domain_scores_gemma":[0.9994825,0.000015473579,0.000022411394,0.00028800164,0.0000029637354,0.00018865822],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000089045425,0.00013718643,0.00012375148,7.99901e-7,0.00010866481,0.000027787544,0.0002772752,0.000056885732,0.9998414],"category_scores_gemma":[0.000008462899,0.0001233692,0.000052826388,0.00019793345,0.000080486076,0.000100711775,0.00009732638,0.000082572325,0.99944323],"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":[0.000020749543,0.000040549832,0.000006756771,8.027607e-7,0.000003965321,0.000004546136,0.000025332105,0.0005573722,0.00006792618,3.6022783e-7,0.33900952,0.6602621],"study_design_scores_gemma":[0.00012041372,0.00009974289,0.0006005218,0.0000036685826,0.0000074032455,0.000004929103,0.0000018449796,0.00034060673,0.00007563445,0.000010536359,0.9985526,0.00018205399],"about_ca_topic_score_codex":0.00013915014,"about_ca_topic_score_gemma":8.919686e-7,"teacher_disagreement_score":0.6600801,"about_ca_system_score_codex":0.00007205577,"about_ca_system_score_gemma":0.000005436253,"threshold_uncertainty_score":0.503085},"labels":[],"label_agreement":null},{"id":"W4406512813","doi":"10.1016/s0967-0653(98)83100-1","title":"10.1016/s0967-0653(98)83100-1","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Lidar; Aerosol; Environmental science; SAGE; Atmospheric sciences; Meteorology; Cloud computing; Remote sensing; Geology; Geography; Physics; Computer science; Nuclear physics","score_opus":0.0041058848069205605,"score_gpt":0.16110159232067311,"score_spread":0.15699570751375255,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406512813","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.005193415,0.000016196655,0.0000035303433,0.00020175336,0.0000013745848,0.00012643925,0.0000033712936,0.000087121654,0.9943668],"genre_scores_gemma":[0.000718693,2.823855e-7,0.0005312915,0.0001204651,0.00006939984,0.000014664274,0.0000035392793,0.000020159046,0.9985215],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990377,0.000021208607,0.00013561608,0.00026912763,0.00023096996,0.00030538384],"domain_scores_gemma":[0.9994995,0.000014676991,0.000021789127,0.00027922285,0.0000029293744,0.00018190597],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000086707805,0.0001333619,0.00012504373,8.1008125e-7,0.00010202922,0.000026943253,0.00026946512,0.00005589214,0.9999378],"category_scores_gemma":[0.000007885878,0.00011973452,0.000051392875,0.00019473338,0.00007761148,0.00009517316,0.000095121926,0.00008013174,0.9998387],"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":[0.000019598721,0.000034153643,0.0000015226229,6.9976653e-7,0.000003653463,0.0000039153156,0.000021998292,0.0005039346,0.00003440047,2.710208e-7,0.46364424,0.5357316],"study_design_scores_gemma":[0.00012417375,0.000095503456,0.00031572382,0.0000036366748,0.000007573502,0.0000039930173,0.0000017757794,0.00030962026,0.00006244378,0.000009491313,0.99888897,0.00017708028],"about_ca_topic_score_codex":0.00015391495,"about_ca_topic_score_gemma":0.0000010275326,"teacher_disagreement_score":0.5355545,"about_ca_system_score_codex":0.00007180122,"about_ca_system_score_gemma":0.000005377184,"threshold_uncertainty_score":0.4882632},"labels":[],"label_agreement":null},{"id":"W4406526856","doi":"10.1016/0967-0653(96)89947-9","title":"10.1016/0967-0653(96)89947-9","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Closure (psychology); Turbulence; Environmental science; Mechanics; Meteorology; Arctic; Atmospheric sciences; Order (exchange); Geology; Physics; Economics; Oceanography","score_opus":0.0039162665026787405,"score_gpt":0.15696371579953902,"score_spread":0.1530474492968603,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406526856","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.010000116,0.000017603312,0.0000041532085,0.00022154169,0.0000015170286,0.00012749596,0.000003988926,0.000088728695,0.98953485],"genre_scores_gemma":[0.001569944,2.6156283e-7,0.0005173578,0.00013622662,0.000068033725,0.000014944682,0.0000044372264,0.000020377549,0.99766845],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990177,0.000021593973,0.00013809846,0.00027523295,0.00023442143,0.0003129563],"domain_scores_gemma":[0.99948776,0.00001523246,0.000022091235,0.00028573285,0.0000028465715,0.00018632843],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00008786581,0.00013548559,0.00012222833,7.8659696e-7,0.00010740223,0.000027428167,0.00027422205,0.00005617968,0.9998366],"category_scores_gemma":[0.000008238895,0.00012177696,0.00005214003,0.0001967819,0.000079547724,0.000099560646,0.00009566307,0.00008153737,0.9994136],"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":[0.000020220214,0.000039655075,0.000006496396,7.8174287e-7,0.0000038645235,0.000004448343,0.000024806177,0.000605417,0.00006866535,3.4167218e-7,0.3544117,0.6448136],"study_design_scores_gemma":[0.00011887281,0.000098707074,0.00058973563,0.0000036141241,0.000007293728,0.000004845365,0.0000018274046,0.000358645,0.00007194937,0.000010346808,0.99855435,0.00017981723],"about_ca_topic_score_codex":0.00013473819,"about_ca_topic_score_gemma":8.59477e-7,"teacher_disagreement_score":0.64463377,"about_ca_system_score_codex":0.00007130943,"about_ca_system_score_gemma":0.000005344346,"threshold_uncertainty_score":0.49659204},"labels":[],"label_agreement":null},{"id":"W4406527074","doi":"10.1016/0967-0653(96)87019-0","title":"10.1016/0967-0653(96)87019-0","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Microwave Limb Sounder; Environmental science; Water vapor; Cirrus; Troposphere; Microwave; Advanced Microwave Sounding Unit; Atmospheric sciences; Meteorology; Atmospheric sounding; Remote sensing; Geology; Geography; Physics","score_opus":0.003899481068763408,"score_gpt":0.15701775008051463,"score_spread":0.15311826901175124,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406527074","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.01113329,0.000017818904,0.000004216171,0.00021944298,0.0000014985344,0.00012825693,0.0000039947613,0.00008804682,0.98840344],"genre_scores_gemma":[0.0016075603,2.6411143e-7,0.0005047605,0.00013671405,0.0000670299,0.000014530984,0.000004458871,0.000020382318,0.9976443],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990204,0.000021468139,0.00013792719,0.000275164,0.00023314434,0.00031189423],"domain_scores_gemma":[0.9994906,0.000015279227,0.00002209055,0.00028510994,0.0000028825716,0.00018404207],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00008688491,0.00013519874,0.00012225607,7.8459914e-7,0.00010542747,0.000027299286,0.00027306407,0.0000560938,0.99983174],"category_scores_gemma":[0.000008175866,0.000121565754,0.000052150546,0.00019575644,0.00007825511,0.000099174154,0.00009546454,0.0000813436,0.99944705],"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":[0.000020632062,0.000040027866,0.000006985264,7.9741324e-7,0.000003971472,0.000004353737,0.000029035662,0.0006133764,0.00006794876,3.5139297e-7,0.35430083,0.6449117],"study_design_scores_gemma":[0.00011972539,0.000098911914,0.0005966956,0.0000036033962,0.0000073074402,0.000004884074,0.0000020182827,0.00033996822,0.00007249082,0.00000983222,0.9985649,0.00017969304],"about_ca_topic_score_codex":0.000113691014,"about_ca_topic_score_gemma":6.869556e-7,"teacher_disagreement_score":0.644732,"about_ca_system_score_codex":0.00007101479,"about_ca_system_score_gemma":0.000005361267,"threshold_uncertainty_score":0.49573076},"labels":[],"label_agreement":null},{"id":"W4406527573","doi":"10.1016/0967-0653(96)84933-7","title":"10.1016/0967-0653(96)84933-7","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Environmental science; Water vapor; Atmospheric sciences; Meteorology; Climatology; Geology; Geography","score_opus":0.00391685875324343,"score_gpt":0.15697112708759506,"score_spread":0.15305426833435162,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406527573","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.009024071,0.000017296088,0.000005037285,0.00022848602,0.0000015030773,0.00012701798,0.0000039797555,0.00008867887,0.9905039],"genre_scores_gemma":[0.0016475277,2.4127752e-7,0.0005047014,0.00013610898,0.00006729489,0.00001498654,0.000004401017,0.000020347083,0.99760437],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99902105,0.000021591622,0.00013778025,0.00027425363,0.00023362768,0.0003116656],"domain_scores_gemma":[0.99948996,0.0000153145,0.0000220847,0.00028418947,0.0000029097748,0.0001855282],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00008760715,0.00013513629,0.000121436795,7.8622395e-7,0.00010694677,0.000027156226,0.00027286966,0.000056129713,0.9998314],"category_scores_gemma":[0.000008252298,0.000121445286,0.000052170617,0.00019636513,0.00007927887,0.000095911324,0.00009179382,0.00008146092,0.99939024],"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":[0.000019973468,0.000039913815,0.0000068084805,7.9030957e-7,0.000003845607,0.000004339573,0.000023581264,0.0007207903,0.00006895494,2.9829255e-7,0.33678985,0.66232085],"study_design_scores_gemma":[0.00011695788,0.00009748114,0.00062992005,0.0000036305016,0.0000073285055,0.0000046616215,0.0000017949466,0.00041755225,0.00007530062,0.0000101436135,0.99845594,0.00017927434],"about_ca_topic_score_codex":0.0001336891,"about_ca_topic_score_gemma":8.2207504e-7,"teacher_disagreement_score":0.66214156,"about_ca_system_score_codex":0.00007123826,"about_ca_system_score_gemma":0.000005364003,"threshold_uncertainty_score":0.4952395},"labels":[],"label_agreement":null},{"id":"W4406529735","doi":"10.1016/0967-0653(96)81816-3","title":"10.1016/0967-0653(96)81816-3","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Simple (philosophy); Cloud computing; Boundary layer; Layer (electronics); Environmental science; Computer science; Materials science; Mechanics; Physics","score_opus":0.00393946009232691,"score_gpt":0.1572921317080565,"score_spread":0.1533526716157296,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406529735","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.010163845,0.000017792576,0.0000040787736,0.00022580876,0.0000015236772,0.00012739566,0.0000039288616,0.00008860695,0.989367],"genre_scores_gemma":[0.0016537852,2.594003e-7,0.0005005396,0.00013695771,0.00006819331,0.0000149389325,0.000004377118,0.000020308573,0.9976006],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990189,0.000021114387,0.00013873816,0.00027497901,0.00023358628,0.00031264932],"domain_scores_gemma":[0.99948883,0.000015270438,0.000022195856,0.00028456634,0.0000029114276,0.00018623497],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0000882853,0.00013540084,0.00012217992,7.8840986e-7,0.00010737746,0.000027449187,0.00027411632,0.000056178542,0.99983597],"category_scores_gemma":[0.000008284123,0.00012170981,0.000052207215,0.00019459568,0.00007947594,0.00009980385,0.00009564226,0.00008147304,0.99942815],"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":[0.000020386557,0.000039863637,0.0000066401576,7.832096e-7,0.000003882094,0.000004463899,0.000024466004,0.00060753623,0.000067552224,3.4311643e-7,0.34077847,0.6584456],"study_design_scores_gemma":[0.00011894674,0.00009758281,0.0006186357,0.0000036154945,0.0000072421194,0.0000046921664,0.0000019064171,0.0003258766,0.00007547651,0.000010318226,0.998556,0.0001797156],"about_ca_topic_score_codex":0.00013918872,"about_ca_topic_score_gemma":8.9922935e-7,"teacher_disagreement_score":0.6582659,"about_ca_system_score_codex":0.0000741191,"about_ca_system_score_gemma":0.000005381649,"threshold_uncertainty_score":0.4963182},"labels":[],"label_agreement":null},{"id":"W4406531843","doi":"10.1016/0967-0653(95)91756-x","title":"10.1016/0967-0653(95)91756-x","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Spectroradiometer; Aerosol; Environmental science; Moderate-resolution imaging spectroradiometer; Remote sensing; Climatology; Geology; Meteorology; Geography; Optics; Reflectivity; Physics; Satellite; Astronomy","score_opus":0.003989519745876751,"score_gpt":0.15806020281554367,"score_spread":0.15407068306966692,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406531843","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0077610705,0.00002976147,0.000003738005,0.00019144022,0.0000015079006,0.00012792363,0.000003894058,0.000072965704,0.9918077],"genre_scores_gemma":[0.001324902,4.278815e-7,0.00045844735,0.00012899376,0.000068335954,0.000015011583,0.000004456956,0.000020356141,0.99797904],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99902225,0.00002187219,0.00013719837,0.00027415,0.00023323107,0.00031131512],"domain_scores_gemma":[0.9994896,0.000015303523,0.000022006601,0.00028477717,0.0000029058203,0.00018541828],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00008764363,0.00013503083,0.00012154271,6.151913e-7,0.00010624973,0.000026604252,0.00027277428,0.00005596452,0.9998362],"category_scores_gemma":[0.000008292714,0.00012141442,0.000051359064,0.0001964333,0.00007894844,0.00009857682,0.00009339981,0.00008195232,0.9994409],"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":[0.000019889903,0.00003907201,0.0000045838847,7.827625e-7,0.0000037932707,0.00000441274,0.000022574954,0.00061132625,0.000098716344,3.321412e-7,0.4155993,0.5835952],"study_design_scores_gemma":[0.00011806797,0.00009870165,0.0006285631,0.0000036409315,0.0000072085863,0.000004882587,0.0000018598461,0.00040092866,0.000057131627,0.000009747268,0.99849004,0.00017924336],"about_ca_topic_score_codex":0.00013461217,"about_ca_topic_score_gemma":8.809543e-7,"teacher_disagreement_score":0.583416,"about_ca_system_score_codex":0.000069648886,"about_ca_system_score_gemma":0.0000053269873,"threshold_uncertainty_score":0.49511364},"labels":[],"label_agreement":null},{"id":"W4406536405","doi":"10.1016/0967-0653(93)93735-a","title":"10.1016/0967-0653(93)93735-a","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Marine stratocumulus; Oceanography; Cloud computing; Environmental science; Climatology; Meteorology; Geology; Geography; Computer science; Aerosol","score_opus":0.0035115819732750436,"score_gpt":0.1530694898271603,"score_spread":0.14955790785388523,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406536405","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.009214271,0.000017334238,0.0000046779764,0.0002015608,0.000001548275,0.00012811691,0.000004027272,0.00008845965,0.99034],"genre_scores_gemma":[0.001565839,2.531599e-7,0.00052225986,0.00013893194,0.00006741488,0.0000150099195,0.0000044962585,0.000020383473,0.9976654],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990189,0.000021371408,0.00013772833,0.00027551135,0.0002338627,0.0003126306],"domain_scores_gemma":[0.99948835,0.000015372598,0.000022002387,0.0002852934,0.0000028744078,0.00018612554],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00008703294,0.00013541349,0.0001219157,7.8370664e-7,0.00010717951,0.000027365264,0.00027213813,0.0000561937,0.9998377],"category_scores_gemma":[0.000008232392,0.00012164229,0.000052136125,0.00019598815,0.0000792405,0.000099444704,0.00009555182,0.000081614555,0.99941355],"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":[0.00002125232,0.000038741437,0.0000051730317,7.674137e-7,0.000003896387,0.0000043896835,0.000024113551,0.0006420373,0.000066566114,3.576507e-7,0.33736056,0.66183215],"study_design_scores_gemma":[0.00012002611,0.00010164508,0.00062439765,0.0000035978796,0.000007373193,0.0000047448475,0.0000018343059,0.00037464846,0.00006012329,0.0000103377,0.9985117,0.00017959316],"about_ca_topic_score_codex":0.00014072898,"about_ca_topic_score_gemma":9.587233e-7,"teacher_disagreement_score":0.66165257,"about_ca_system_score_codex":0.00007127976,"about_ca_system_score_gemma":0.0000054514867,"threshold_uncertainty_score":0.49604285},"labels":[],"label_agreement":null},{"id":"W4406763136","doi":"10.1029/2024gl111961","title":"Exploring Causal Relationships and Adjustment Timescales of Aerosol‐Cloud Interactions in Geostationary Satellite Observations and CAM6 Using Wavelet Phase Coherence Analysis","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"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","funders":"Office of Science; National Oceanic and Atmospheric Administration; U.S. Department of Energy","keywords":"Liquid water path; Environmental science; Cloud top; Atmospheric sciences; Entrainment (biomusicology); Satellite; Meteorology; Context (archaeology); Lag; Cloud computing; Geostationary orbit; Coherence (philosophical gambling strategy); Daytime; Geostationary Operational Environmental Satellite; Aerosol; Mathematics; Physics; Statistics; Computer science; Geology","score_opus":0.18038537988592715,"score_gpt":0.36202176586446366,"score_spread":0.1816363859785365,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406763136","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":[0.9962339,0.000091869624,0.0018959712,0.001355071,0.000035135297,0.00021512379,0.000018497663,0.00000891309,0.00014551918],"genre_scores_gemma":[0.99661803,0.00012559026,0.0029058894,0.00010801273,0.000023355691,0.000056047535,0.000018730929,0.000005934037,0.0001384119],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984893,0.00022013781,0.00026173494,0.0003268982,0.0004173583,0.0002845218],"domain_scores_gemma":[0.9990104,0.0006312243,0.000050234714,0.00018267588,0.00003433909,0.000091115304],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003831419,0.000103918544,0.00018470328,0.000032799268,0.00023689175,0.000027966067,0.0001015191,0.00002317191,0.00006377943],"category_scores_gemma":[0.00016203847,0.00010183556,0.000041820047,0.0015087727,0.00047409584,0.00036815286,0.00022450449,0.00034450594,0.0000062340027],"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":[0.00020510271,0.0009257767,0.55121684,0.00009720157,0.0003603096,0.00003080981,0.0049418025,0.011177392,0.3871059,0.0026637004,0.0009877065,0.04028743],"study_design_scores_gemma":[0.00037809915,0.00003888957,0.9700603,0.000051743973,0.000064651256,6.1044756e-7,0.00091753807,0.027146654,0.0007342045,0.0003416806,0.00015351067,0.0001121257],"about_ca_topic_score_codex":0.0031488636,"about_ca_topic_score_gemma":0.00076677825,"teacher_disagreement_score":0.41884345,"about_ca_system_score_codex":0.00020650374,"about_ca_system_score_gemma":0.000029599232,"threshold_uncertainty_score":0.47601607},"labels":[],"label_agreement":null},{"id":"W4406885146","doi":"10.1007/s13351-024-4064-3","title":"Exploring Marine Cloud Brightening with a Reduced Complexity Model","year":2024,"lang":"en","type":"article","venue":"Journal of Meteorological Research","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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 Waterloo","funders":"","keywords":"Cloud computing; Meteorology; Climatology; Geography; Atmospheric sciences; Geology; Computer science","score_opus":0.3679184448174263,"score_gpt":0.3730913630336326,"score_spread":0.0051729182162063014,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406885146","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":[0.9800382,0.00012157038,0.0063447915,0.0014884393,0.00010551358,0.000091452246,7.239724e-7,0.000024499801,0.011784801],"genre_scores_gemma":[0.9705999,0.00018538484,0.028155632,0.000057201363,0.00020986977,0.000009365351,3.301231e-7,0.000014876232,0.00076743617],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9973372,0.0002279984,0.00033774532,0.0002618521,0.0013321862,0.00050297996],"domain_scores_gemma":[0.9991139,0.00032324393,0.000064111904,0.0001627401,0.000059656297,0.0002763018],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0029529657,0.00012323054,0.000254164,0.000010789769,0.00018892421,0.00010870366,0.00044492065,0.00006327336,0.0026066138],"category_scores_gemma":[0.00022079676,0.000067761495,0.0001066248,0.0005864658,0.0005663244,0.00036612063,0.00047047538,0.0011359927,0.00011362689],"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":[0.0071674194,0.0015095035,0.044450916,0.00020981496,0.000686153,0.010068403,0.0051681185,0.12984423,0.25476906,0.038782038,0.02908652,0.47825783],"study_design_scores_gemma":[0.0028840469,0.013335499,0.18761763,0.0005146968,0.00017336218,0.0024491325,0.001963873,0.583084,0.011203909,0.15801275,0.037451524,0.0013096081],"about_ca_topic_score_codex":0.00008641921,"about_ca_topic_score_gemma":0.000015730071,"teacher_disagreement_score":0.4769482,"about_ca_system_score_codex":0.00022340172,"about_ca_system_score_gemma":0.000058044563,"threshold_uncertainty_score":0.99830514},"labels":[],"label_agreement":null},{"id":"W4407797604","doi":"10.5194/tc-19-769-2025","title":"Improving large-scale snow albedo modeling using a climatology of light-absorbing particle deposition","year":2025,"lang":"en","type":"article","venue":"The cryosphere","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"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":"Horizon 2020; European Commission","keywords":"Snow; Albedo (alchemy); Particle deposition; Environmental science; Deposition (geology); Atmospheric sciences; Scale (ratio); Climatology; Particle (ecology); Meteorology; Aerosol; Geography; Geology; Oceanography; Geomorphology; Cartography","score_opus":0.008070543930799543,"score_gpt":0.22743741898705525,"score_spread":0.2193668750562557,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407797604","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":[0.80324143,0.0002447737,0.19383265,0.00016159244,0.00012395195,0.00015794797,0.0000014528035,0.00003704653,0.0021991576],"genre_scores_gemma":[0.99141884,0.000010154633,0.007767011,0.00028077464,0.000026720536,0.000014371473,0.0000012719794,0.000017940434,0.0004629416],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99864,0.00006823933,0.00035462942,0.00031605727,0.00019026133,0.0004308341],"domain_scores_gemma":[0.99939656,0.000045511864,0.00013082611,0.0003542405,0.000015209561,0.000057663023],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023568606,0.00015582121,0.00021550784,0.0000010373378,0.00034214,0.00003180585,0.00027050276,0.000108740656,0.0005052086],"category_scores_gemma":[0.0000137840825,0.00012374908,0.00009784934,0.00031673786,0.00009641531,0.0001534295,0.0003160771,0.00015649665,0.00004626665],"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":[0.00016080569,0.00049718696,0.3123487,0.0001442369,0.000102211554,0.00002066585,0.0043090004,0.28642312,0.3610383,0.0012592529,0.0005922997,0.033104245],"study_design_scores_gemma":[0.00035779466,0.000032160555,0.0014383341,0.000058929312,0.000063026055,0.000009513534,0.0013683175,0.9871462,0.008584512,0.00060434407,0.00018051507,0.00015635366],"about_ca_topic_score_codex":0.0020578005,"about_ca_topic_score_gemma":0.002074767,"teacher_disagreement_score":0.7007231,"about_ca_system_score_codex":0.000107359076,"about_ca_system_score_gemma":0.000023753466,"threshold_uncertainty_score":0.553168},"labels":[],"label_agreement":null},{"id":"W4407897436","doi":"10.22541/essoar.174042992.24306472/v1","title":"Corrected Estimation of Ocean TOA Instantaneous Clear-Sky Albedo from CERES for Shortwave Cloud Radiative Effect Analysis","year":2025,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"","keywords":"Shortwave; Sky; Albedo (alchemy); Environmental science; Radiative transfer; Cloud computing; Shortwave radiation; Remote sensing; Meteorology; Climatology; Geography; Geology; Computer science; Physics; History; Optics","score_opus":0.005511036172137496,"score_gpt":0.24438512920522606,"score_spread":0.23887409303308857,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407897436","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":[0.8687757,0.00006585656,0.11821249,0.000054058695,0.00049874897,0.0011641163,0.0005310241,0.0000956067,0.010602386],"genre_scores_gemma":[0.97967803,0.00003821153,0.01692508,0.000100503494,0.000056920257,0.00004430684,0.0006227348,0.000021492777,0.0025126974],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9977915,0.00014977284,0.0005746595,0.0008029238,0.00038735868,0.00029376455],"domain_scores_gemma":[0.9981197,0.00071819435,0.00041201155,0.0006155234,0.000027271313,0.00010731083],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00022562835,0.00040226174,0.0008920951,0.000009870586,0.000108879576,0.00004548945,0.00046435598,0.00036053968,0.0031777385],"category_scores_gemma":[0.00017372325,0.00034441095,0.00050056656,0.000548213,0.00018638535,0.00005716013,0.0006986498,0.00028855595,0.00002392192],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006210641,0.00016143717,0.08258049,0.0001128356,0.0019765326,0.000008776862,0.0016542725,0.8688097,0.00013995467,0.000105803214,0.006718198,0.037110902],"study_design_scores_gemma":[0.0005945898,0.00041322567,0.04746412,0.00008935484,0.002683579,8.5859375e-7,0.0003401754,0.94305104,0.003022551,0.0013617397,0.00036643163,0.00061232195],"about_ca_topic_score_codex":0.008959506,"about_ca_topic_score_gemma":0.0015324061,"teacher_disagreement_score":0.11090234,"about_ca_system_score_codex":0.00036415312,"about_ca_system_score_gemma":0.000049047394,"threshold_uncertainty_score":0.9999008},"labels":[],"label_agreement":null},{"id":"W4408136224","doi":"10.1038/s41612-025-00948-7","title":"Moderate climate sensitivity due to opposing mixed-phase cloud feedbacks","year":2025,"lang":"en","type":"article","venue":"npj Climate and Atmospheric Science","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Alliance de recherche numérique du Canada","keywords":"Climate sensitivity; Environmental science; Sensitivity (control systems); Phase (matter); Mixed phase; Climatology; Atmospheric sciences; Climate change; Meteorology; Climate model; Geography; Geology; Physics; Oceanography; Engineering","score_opus":0.007581500318002349,"score_gpt":0.26377173994422065,"score_spread":0.2561902396262183,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408136224","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":[0.96657366,0.000088985784,0.010337683,0.00085680216,0.00067430554,0.00034858414,0.000013947344,0.00013402548,0.020972025],"genre_scores_gemma":[0.97536904,0.00017003303,0.021755815,0.0022330475,0.000054546425,0.000022452228,0.0000019851184,0.000020164693,0.00037293008],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9966249,0.0000802273,0.000395615,0.0010979348,0.0005556359,0.0012456792],"domain_scores_gemma":[0.99876934,0.000096762626,0.00011793176,0.0005294901,0.000039389783,0.0004470626],"candidate_categories":["metaepi_narrow","sts"],"consensus_categories":[],"category_scores_codex":[0.0013929431,0.0003522469,0.00040319623,0.0000022610361,0.0015394668,0.00038775057,0.00042261594,0.00009690774,0.0003247728],"category_scores_gemma":[0.000096258154,0.00031256193,0.000073906725,0.0018329909,0.0010641578,0.0006042622,0.0012997028,0.00019860515,0.00029774266],"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":[0.00069161097,0.0010571863,0.11163074,0.00017523365,0.000044995497,0.0004907655,0.0026033802,0.025290716,0.3236233,0.007511562,0.006899886,0.5199806],"study_design_scores_gemma":[0.0042117424,0.00095506094,0.34882215,0.0004671755,0.00018275066,0.0002889525,0.0037500407,0.5745847,0.042160355,0.0018144693,0.019878794,0.0028837929],"about_ca_topic_score_codex":0.0002837597,"about_ca_topic_score_gemma":0.000117277305,"teacher_disagreement_score":0.549294,"about_ca_system_score_codex":0.00022739514,"about_ca_system_score_gemma":0.00007162891,"threshold_uncertainty_score":0.99993265},"labels":[],"label_agreement":null},{"id":"W4408221340","doi":"10.1029/2024ms004404","title":"Impacts of Predicted Liquid Fraction and Multiple Ice‐Phase Categories on the Simulation of Hail in the Predicted Particle Properties (P3) Microphysics Scheme","year":2025,"lang":"en","type":"article","venue":"Journal of Advances in Modeling Earth Systems","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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":"Particle (ecology); Phase (matter); Environmental science; Meteorology; Fraction (chemistry); Atmospheric sciences; Mechanics; Materials science; Geology; Physics; Chemistry; Chromatography","score_opus":0.016484105343254195,"score_gpt":0.26386838567350374,"score_spread":0.24738428033024953,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408221340","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":[0.9859724,0.0012547212,0.012324097,0.000079745194,0.000098128316,0.00023354107,0.000003143801,0.000003276958,0.000030962197],"genre_scores_gemma":[0.9994959,0.0002476346,0.00019279725,0.000021686034,0.00002703738,0.0000037981058,4.5347028e-7,0.0000043544323,0.00000629923],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99884784,0.00012585956,0.0005458137,0.00008707758,0.00028285276,0.00011054331],"domain_scores_gemma":[0.9993145,0.00013864167,0.00036109533,0.00011669614,0.000049961298,0.00001913928],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005089774,0.00008237168,0.00019478677,0.0000066837215,0.000056946606,0.000017927938,0.0001257141,0.00003872584,0.0000026142577],"category_scores_gemma":[0.00017068766,0.000044748427,0.00003064615,0.0002550024,0.000107897715,0.000363256,0.000025613306,0.00016678346,2.0463179e-7],"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":[0.00051414693,0.00012985413,0.025847105,0.00005138349,0.000006885449,8.415138e-7,0.0013440982,0.9360379,0.035639144,0.000020592368,0.000002622707,0.0004054046],"study_design_scores_gemma":[0.0006763038,0.0004638614,0.002067468,0.00037341585,0.000010296721,0.0000017087823,0.0030216852,0.9883059,0.004926503,0.00006181367,0.000047656562,0.000043379212],"about_ca_topic_score_codex":0.0002665622,"about_ca_topic_score_gemma":0.00007332998,"teacher_disagreement_score":0.052267987,"about_ca_system_score_codex":0.00003634986,"about_ca_system_score_gemma":0.000024311028,"threshold_uncertainty_score":0.1824788},"labels":[],"label_agreement":null},{"id":"W4408272205","doi":"10.15372/aoo20250104","title":"ЧЕРНЫЙ И КОРИЧНЕВЫЙ УГЛЕРОД И СЕЛЕКТИВНОЕ ПОГЛОЩЕНИЕ РАДИАЦИИ ДЫМОВЫМ АЭРОЗОЛЕМ ПРИ МАССОВЫХ ЛЕСНЫХ ПОЖАРАХ НА АЛЯСКЕ В 2019 Г. И В КАНАДЕ В 2023 Г","year":2025,"lang":"ru","type":"article","venue":"Optika atmosfery i okeana","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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","score_opus":0.00481821229232582,"score_gpt":0.22703800866629878,"score_spread":0.22221979637397296,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408272205","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":[0.5145687,0.0144537445,0.0058113965,0.008706948,0.010766001,0.003221241,0.00063064776,0.0008736018,0.44096777],"genre_scores_gemma":[0.67692864,0.005858489,0.006009286,0.004308947,0.0010980894,0.00017180825,0.00018896098,0.0003219567,0.30511382],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9865906,0.00065800245,0.002587433,0.0038350334,0.0023833544,0.0039455355],"domain_scores_gemma":[0.9927793,0.0006695126,0.0008538423,0.0040961956,0.00016665847,0.0014344897],"candidate_categories":["metaepi_narrow","sts","research_integrity","insufficient_payload"],"consensus_categories":["metaepi_narrow","insufficient_payload"],"category_scores_codex":[0.0016292499,0.0024569046,0.0023480158,0.000038702856,0.0020619768,0.00086291553,0.003697902,0.0016689268,0.036891554],"category_scores_gemma":[0.00033877298,0.0024830448,0.0013810173,0.003585935,0.0020986556,0.0013498588,0.0030362706,0.0022041455,0.027552756],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008642231,0.0028514066,0.129864,0.0006413869,0.0016209412,0.00087840774,0.0021530723,0.011525947,0.011148849,0.008207785,0.7033097,0.12693428],"study_design_scores_gemma":[0.0072890925,0.0016509561,0.21917558,0.001774543,0.0018298565,0.00014013331,0.005803945,0.019264666,0.005574944,0.0040426827,0.72603416,0.0074194465],"about_ca_topic_score_codex":0.006825408,"about_ca_topic_score_gemma":0.0011439087,"teacher_disagreement_score":0.16235998,"about_ca_system_score_codex":0.0019121544,"about_ca_system_score_gemma":0.0007165023,"threshold_uncertainty_score":0.9997882},"labels":[],"label_agreement":null},{"id":"W4408283730","doi":"10.1038/s41598-025-90169-y","title":"3D volumetric tomography of clouds using machine learning for climate analysis","year":2025,"lang":"en","type":"article","venue":"Scientific Reports","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Institute for Theoretical Astrophysics; University of Toronto","funders":"European Research Council","keywords":"Computer science; Rendering (computer graphics); Remote sensing; Radiation; Cloud computing; Tomography; Meteorology; Environmental science; Geology; Artificial intelligence; Geography; Physics; Optics","score_opus":0.008819883123711831,"score_gpt":0.2471656514872166,"score_spread":0.23834576836350477,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408283730","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":[0.95815057,0.00025053544,0.036858916,0.000012657462,0.0013251784,0.00023519031,0.0000026558187,0.000037091162,0.0031272224],"genre_scores_gemma":[0.98006415,0.0000061843657,0.016663909,0.000016653936,0.000009656486,0.000010649523,0.000024405272,0.000008419872,0.0031959815],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99806935,0.000035146626,0.00052908255,0.00063453434,0.00038590745,0.00034596983],"domain_scores_gemma":[0.9989367,0.000039996637,0.00039132635,0.0005234814,0.00003992726,0.00006855231],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014163769,0.00012771909,0.00028795344,0.00004698828,0.0004831254,0.0000864752,0.00016079049,0.000058587408,0.0006879155],"category_scores_gemma":[0.00012535599,0.000114044975,0.00031967164,0.0063003777,0.00033241598,0.00011057681,0.00021067288,0.00007956742,0.0000046393247],"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":[0.000007687275,0.000053237523,0.96215016,0.000023251483,0.0000921426,0.000008270358,0.00006224483,0.024351422,0.0097685605,0.000016266024,0.0003398098,0.0031269402],"study_design_scores_gemma":[0.0003452291,0.00009240957,0.195663,0.000040819123,0.0014740783,0.000017046577,0.0001803463,0.7351364,0.011469187,0.0019000984,0.053178072,0.0005032987],"about_ca_topic_score_codex":0.00048375916,"about_ca_topic_score_gemma":0.000085387765,"teacher_disagreement_score":0.7664872,"about_ca_system_score_codex":0.00006847428,"about_ca_system_score_gemma":0.00002353817,"threshold_uncertainty_score":0.75321925},"labels":[],"label_agreement":null},{"id":"W4408430645","doi":"10.5194/egusphere-egu25-14129","title":"Overview of French efforts for the innovative characterisation of aerosols and cloud interactions with the future Atmosphere Observing System","year":2025,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Atmosphere (unit); Cloud computing; Environmental science; Meteorology; Atmospheric sciences; Remote sensing; Computer science; Geography; Geology","score_opus":0.018649031993305143,"score_gpt":0.25704749589483505,"score_spread":0.2383984639015299,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408430645","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":[0.971855,0.0009213436,0.01929874,0.0013838676,0.0008873005,0.0019026272,0.00009993038,0.000029043094,0.0036221782],"genre_scores_gemma":[0.9945736,0.00022567675,0.0031084584,0.00015842583,0.00017201657,0.00021957814,0.000021024767,0.000013115453,0.0015080945],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988338,0.00005459859,0.00040502424,0.00032328046,0.00023501579,0.00014830905],"domain_scores_gemma":[0.9984716,0.00023939085,0.0006539883,0.00052628765,0.000085450156,0.000023274039],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029828635,0.00023378913,0.00036571996,6.4563574e-7,0.00017413084,0.000033947745,0.00038952896,0.00012320098,0.0002669511],"category_scores_gemma":[0.000011519981,0.000113603295,0.00008505262,0.00031091063,0.00020711296,0.000084253115,0.00071973755,0.00028014797,0.000001202277],"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":[0.00074124336,0.00072264695,0.64589393,0.017612701,0.003519554,0.0000048189568,0.037532773,0.030969834,0.005479308,0.048191156,0.052180257,0.1571518],"study_design_scores_gemma":[0.00091556174,0.000321781,0.91666985,0.0031727466,0.000631263,0.000014949355,0.021206247,0.019535871,0.0018281577,0.00031060874,0.034641564,0.0007514175],"about_ca_topic_score_codex":0.001311329,"about_ca_topic_score_gemma":0.0010402702,"teacher_disagreement_score":0.2707759,"about_ca_system_score_codex":0.000106955835,"about_ca_system_score_gemma":0.00005203334,"threshold_uncertainty_score":0.46326077},"labels":[],"label_agreement":null},{"id":"W4408431773","doi":"10.5194/egusphere-egu25-12448","title":"Potential Influence of Microplastics on Cloud Formation through Heterogeneous Ice Nucleation","year":2025,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"University of British Columbia; University of British Columbia Hospital","funders":"","keywords":"Microplastics; Ice nucleus; Nucleation; Cloud computing; Environmental science; Atmospheric sciences; Ice formation; Chemical physics; Oceanography; Chemistry; Geology; Computer science","score_opus":0.006965140113882161,"score_gpt":0.22455660442703387,"score_spread":0.2175914643131517,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408431773","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":[0.9032376,0.000013298043,0.08448733,0.00007152784,0.00036451014,0.00027679818,0.000030105957,0.000045529152,0.011473325],"genre_scores_gemma":[0.98842144,0.00009488023,0.009958441,0.00041133323,0.000048126512,0.000011739622,0.000028200493,0.000010389503,0.0010154587],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9987318,0.000037619044,0.0003869171,0.00033200614,0.00033136312,0.00018032047],"domain_scores_gemma":[0.99926746,0.000021866002,0.00027400028,0.00037892687,0.000022325237,0.000035403817],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006573716,0.00021193917,0.00021189457,0.0000018724801,0.00008224139,0.00002714961,0.00032134386,0.00023683668,0.000727162],"category_scores_gemma":[0.000022117129,0.00019253652,0.00010274274,0.00009956996,0.000117443524,0.000111852285,0.00071871746,0.00022822672,0.00018234864],"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":[0.00004033414,0.0000766529,0.0004984705,0.000076004806,0.000015638781,0.000002341027,0.00034338946,0.9918964,0.003950234,0.0002078177,0.0010530966,0.0018396584],"study_design_scores_gemma":[0.0031851036,0.0017306126,0.10345037,0.0018067033,0.000844281,0.000080455015,0.0009463311,0.54428715,0.29087842,0.022200692,0.026398564,0.0041913143],"about_ca_topic_score_codex":0.0007891342,"about_ca_topic_score_gemma":0.00003689011,"teacher_disagreement_score":0.44760922,"about_ca_system_score_codex":0.00018285195,"about_ca_system_score_gemma":0.000019819116,"threshold_uncertainty_score":0.7961914},"labels":[],"label_agreement":null},{"id":"W4408433949","doi":"10.5194/egusphere-egu25-7821","title":"&amp;#160;Cloud microphysics in Arctic and Antarctic environments derived from infrared emission spectroscopy","year":2025,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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; University of Toronto","funders":"","keywords":"The arctic; Cloud computing; Environmental science; Arctic; Infrared; Atmospheric sciences; Spectroscopy; Meteorology; Climatology; Oceanography; Physics; Geology; Astronomy; Computer science","score_opus":0.00861017799006609,"score_gpt":0.22918492951980268,"score_spread":0.2205747515297366,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408433949","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":[0.981114,0.00024728634,0.010064829,0.00015392022,0.00030660507,0.00048657454,0.00003183251,0.00003802506,0.0075569325],"genre_scores_gemma":[0.9261529,0.001317337,0.061009686,0.0005519272,0.000100967896,0.000053206288,0.00013498295,0.000035587393,0.010643425],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99765563,0.0000928182,0.00042946902,0.0010459754,0.0003412434,0.0004348843],"domain_scores_gemma":[0.9988857,0.00007529631,0.00017309474,0.0006887038,0.000002436825,0.0001747655],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00009197655,0.00046977834,0.00048496947,0.000004353296,0.00010878812,0.000073479954,0.0004267383,0.00034373475,0.004389579],"category_scores_gemma":[0.000020128016,0.00044103188,0.00009824783,0.0001421877,0.0002733459,0.000089181594,0.0024221856,0.00069617375,0.00018824605],"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":[0.00012795028,0.00045223438,0.58881295,0.00012167974,0.00008914393,0.000026292892,0.001889682,0.0018585288,0.3996777,0.000013962625,0.0019182836,0.0050115692],"study_design_scores_gemma":[0.0020158992,0.00012040133,0.8964315,0.00078819296,0.00020870157,0.00000436013,0.00055994926,0.0028353084,0.04590827,0.031145617,0.01797052,0.0020112956],"about_ca_topic_score_codex":0.0071161287,"about_ca_topic_score_gemma":0.00023373598,"teacher_disagreement_score":0.35376945,"about_ca_system_score_codex":0.00061806146,"about_ca_system_score_gemma":0.000038233895,"threshold_uncertainty_score":0.99980414},"labels":[],"label_agreement":null},{"id":"W4408445455","doi":"10.5194/egusphere-egu25-2187","title":"Development of a Dual-Beam Optical Trap for Monitoring Water Uptake and Activation of Single Aerosol Particles","year":2025,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"","keywords":"Trap (plumbing); Aerosol; Dual (grammatical number); Beam (structure); Environmental science; Materials science; Nanotechnology; Physics; Optics; Meteorology; Environmental engineering","score_opus":0.030558183235987323,"score_gpt":0.2566244520396003,"score_spread":0.226066268803613,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408445455","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":[0.97968,0.000008588057,0.01882271,0.000059708935,0.00007845777,0.00030843052,0.0000024819208,0.0000136087165,0.0010260275],"genre_scores_gemma":[0.85862297,0.000004320355,0.14090455,0.000007360638,0.000014877702,0.00005514074,0.0000037516702,0.0000056821677,0.00038133858],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99906385,0.0000062678296,0.00034939137,0.0002494195,0.00016652448,0.00016456978],"domain_scores_gemma":[0.99969894,0.00003261616,0.000077756835,0.00013613787,0.000012196113,0.000042342337],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013385153,0.00012569319,0.00020720022,0.0000014196405,0.000048161935,0.000012256342,0.00008301634,0.00011342326,0.00011275222],"category_scores_gemma":[0.000013354073,0.00009163251,0.000045757955,0.000031803982,0.00009155147,0.000043239776,0.00040988615,0.00006449365,0.0000015122565],"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":[0.000045292534,0.00019156218,0.006347924,0.00017682789,0.00004173232,1.4235347e-7,0.0023814186,0.0015301954,0.9470201,0.000048767364,0.000028239656,0.042187758],"study_design_scores_gemma":[0.0001763966,0.00003665698,0.011793301,0.00007747669,0.000018709019,1.6118359e-7,0.00036916378,0.00037499572,0.9867023,0.00014300163,0.0001987941,0.00010901609],"about_ca_topic_score_codex":0.00003740532,"about_ca_topic_score_gemma":0.000008191998,"teacher_disagreement_score":0.12208183,"about_ca_system_score_codex":0.00006456809,"about_ca_system_score_gemma":0.000019345385,"threshold_uncertainty_score":0.3736665},"labels":[],"label_agreement":null},{"id":"W4408523401","doi":"10.1175/bams-d-25-0027.1","title":"Scientific Directions for Cloud Chamber Research: Instrumentation, Modeling, New Chambers, and Emerging Chamber Concepts","year":2025,"lang":"en","type":"article","venue":"Bulletin of the American Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"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":"Pacific Northwest National Laboratory; HORIZON EUROPE Framework Programme; Office of Science; Korea Institute of Science and Technology; Bundesministerium für Bildung und Forschung; European Commission; Battelle; Pusan National University; Deutsche Forschungsgemeinschaft; U.S. Department of Energy; National Science Foundation","keywords":"Cloud chamber; Instrumentation (computer programming); Environmental science; Physics; Computer science; Nuclear physics; Operating system","score_opus":0.03164860930815006,"score_gpt":0.3213548314890965,"score_spread":0.28970622218094644,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408523401","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":[0.9788428,0.00018324332,0.0036056626,0.014130695,0.00026478746,0.0004868959,0.0000074862464,0.00003743296,0.002440999],"genre_scores_gemma":[0.96656317,0.0001522487,0.020608734,0.0019774574,0.000059902955,0.00007021544,0.0000027758103,0.000012402799,0.010553114],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9982001,0.00019311806,0.0002869875,0.00050295313,0.00038831652,0.00042850195],"domain_scores_gemma":[0.99910593,0.00023634036,0.00016668177,0.0003295797,0.00005025005,0.00011121627],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011183457,0.00015443689,0.0002701689,0.0000025077231,0.0011117011,0.00006704031,0.0002405989,0.00006965066,0.0010693342],"category_scores_gemma":[0.0002575874,0.000105953404,0.00023231775,0.00071269803,0.0033937027,0.000028418568,0.0006001339,0.00023843543,0.000021295078],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002588704,0.00035313042,0.050962646,0.000043687447,0.00024126179,9.3100135e-7,0.0046670157,0.010371686,0.006062347,0.0037798013,0.8561832,0.06707547],"study_design_scores_gemma":[0.0011794707,0.0003772599,0.03837982,0.000040527964,0.00009685997,0.0000063397138,0.0053560073,0.039445084,0.0006759566,0.007270677,0.9067594,0.00041262238],"about_ca_topic_score_codex":0.0021905305,"about_ca_topic_score_gemma":0.00003561485,"teacher_disagreement_score":0.06666285,"about_ca_system_score_codex":0.00010435659,"about_ca_system_score_gemma":0.000043077478,"threshold_uncertainty_score":0.99984384},"labels":[],"label_agreement":null},{"id":"W4408955683","doi":"10.1029/2024jd042091","title":"Direct Measurements and Implications of the Aerosol Asymmetry Parameter in Wildfire Smoke During FIREX‐AQ","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Aerosol; Smoke; Asymmetry; Environmental science; Atmospheric sciences; Meteorology; Physics; Particle physics","score_opus":0.03342879376766119,"score_gpt":0.31765614290638483,"score_spread":0.28422734913872366,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408955683","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":[0.9931178,0.00031262235,0.00003007363,0.0009863859,0.0000550645,0.00018818547,0.0000014615295,0.0000033356155,0.005305055],"genre_scores_gemma":[0.9985914,0.000095566415,0.0004574018,0.000062658735,0.000034217195,0.000010872686,9.550593e-8,0.000009108479,0.0007386308],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979164,0.00024789906,0.0004241905,0.00020795761,0.0008367452,0.00036680035],"domain_scores_gemma":[0.9989402,0.00040484007,0.00016666678,0.00031636405,0.000055002103,0.00011690495],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006732414,0.000119075354,0.00027305397,0.0000027610795,0.00020542389,0.000039779035,0.00053566304,0.00006700915,0.00012030266],"category_scores_gemma":[0.0005642889,0.00007695608,0.00013085452,0.0008966321,0.0005314399,0.00016700357,0.0004546327,0.00050378765,0.0000066051934],"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":[0.00010018122,0.00028959644,0.95708424,0.000023740786,0.00004739264,0.0000035666494,0.00012447863,0.00016535835,0.026736254,0.000043046144,0.0011125797,0.014269539],"study_design_scores_gemma":[0.00045373663,0.00011103763,0.98633677,0.00013319807,0.00001281268,0.000002716914,0.00012837771,0.00016938808,0.010833451,0.0015224578,0.00022797995,0.00006809709],"about_ca_topic_score_codex":0.0012556254,"about_ca_topic_score_gemma":0.00025453325,"teacher_disagreement_score":0.029252479,"about_ca_system_score_codex":0.00020813565,"about_ca_system_score_gemma":0.000075085685,"threshold_uncertainty_score":0.3138178},"labels":[],"label_agreement":null},{"id":"W4408972612","doi":"10.1029/2024jd042453","title":"Assessing Cloud Fraction in the Canadian Regional Climate Model Over North America Using Satellite Data and a Satellite Simulator Package","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada; Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Satellite; Cloud computing; Meteorology; Environmental science; Remote sensing; Climate model; Computer science; Climatology; Climate change; Geography; Engineering; Geology; Aerospace engineering; Operating system","score_opus":0.07251212289097574,"score_gpt":0.3735898859250628,"score_spread":0.30107776303408706,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408972612","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":[0.9956407,0.00054648385,0.0015017869,0.00082980964,0.00004986702,0.00016272934,0.000008723018,0.0000039224765,0.0012559734],"genre_scores_gemma":[0.9944047,0.0007658631,0.0040107644,0.0005745748,0.00015246663,0.0000018800278,0.000005592032,0.000014421688,0.000069741065],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9971202,0.00037108164,0.00041922432,0.00034147827,0.001081423,0.0006666199],"domain_scores_gemma":[0.99845254,0.00054559164,0.00018031486,0.0004862219,0.000065499764,0.00026984172],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012258437,0.00016498259,0.00028081154,0.0000061990486,0.0006483671,0.0005206521,0.0007796424,0.0000853457,0.00008864891],"category_scores_gemma":[0.00023500773,0.000114149734,0.000070673705,0.00089863344,0.00065175316,0.0009276864,0.00042334633,0.00095670944,0.000018773779],"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":[0.00052758964,0.0005086754,0.6745608,0.000066577275,0.00010361254,0.00033810365,0.0015976343,0.06155144,0.002153402,0.0004706754,0.0035573507,0.25456414],"study_design_scores_gemma":[0.00030092453,0.0000782498,0.5560538,0.000083215404,0.000021073969,0.000008277038,0.0009368554,0.42437914,0.00000657648,0.002451445,0.015553325,0.00012712512],"about_ca_topic_score_codex":0.05833858,"about_ca_topic_score_gemma":0.078701116,"teacher_disagreement_score":0.3628277,"about_ca_system_score_codex":0.00053044874,"about_ca_system_score_gemma":0.00046408782,"threshold_uncertainty_score":0.947932},"labels":[],"label_agreement":null},{"id":"W4409106213","doi":"10.2139/ssrn.5203085","title":"Direct Inversion for Bidimensional Distributions of Aerosol Characteristics","year":2025,"lang":"en","type":"preprint","venue":"SSRN Electronic Journal","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"","keywords":"Aerosol; Inversion (geology); Environmental science; Meteorology; Econometrics; Atmospheric sciences; Geography; Geology; Mathematics; Seismology","score_opus":0.007577708942639407,"score_gpt":0.23397676171361848,"score_spread":0.22639905277097908,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409106213","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":[0.86432374,0.0009350357,0.12802133,0.00082640245,0.001325279,0.0007299128,0.00068033196,0.000046347963,0.0031116083],"genre_scores_gemma":[0.9913655,0.002298902,0.0014444597,0.00006612897,0.00016022571,0.000026915008,0.00014200162,0.000016564825,0.004479285],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9976068,0.000055450415,0.00044979466,0.00032883068,0.00032051967,0.0012385764],"domain_scores_gemma":[0.9990704,0.00007580138,0.00045552998,0.00026207516,0.000047314126,0.0000888896],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00071945245,0.00024103139,0.00037880114,0.0000047860694,0.0002635506,0.000023245648,0.0004342141,0.00023433797,0.00024083485],"category_scores_gemma":[0.00009371168,0.00021588673,0.00031617592,0.00013032023,0.00014678478,0.000055273726,0.0005932133,0.001444137,0.000016471324],"study_design_candidate":"theoretical_or_conceptual","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":[0.003502273,0.005783533,0.25078765,0.0014352537,0.006149635,0.000035994868,0.0020185104,0.020183008,0.07219286,0.19756527,0.104833454,0.33551255],"study_design_scores_gemma":[0.011004665,0.005579017,0.04887634,0.0029341674,0.0044822246,0.00044535162,0.003182227,0.035248958,0.04019106,0.73914534,0.10147747,0.007433209],"about_ca_topic_score_codex":0.00013472466,"about_ca_topic_score_gemma":0.00013184836,"teacher_disagreement_score":0.54158,"about_ca_system_score_codex":0.0015251242,"about_ca_system_score_gemma":0.0011685153,"threshold_uncertainty_score":0.88036054},"labels":[],"label_agreement":null},{"id":"W4409163560","doi":"10.1016/j.jes.2025.04.001","title":"Investigation of natural and anthropogenic effects on aerosols optical properties over the Western Pacific ocean by the research vessel KEXUE","year":2025,"lang":"en","type":"article","venue":"Journal of Environmental Sciences","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Science and Technology Innovation Plan Of Shanghai Science and Technology Commission; National Key Research and Development Program of China; Ministry of Science and Technology of the People's Republic of China; Chinese Academy of Sciences; Canadian Anesthesiologists' Society","keywords":"Oceanography; Environmental science; Natural (archaeology); Pacific ocean; Research vessel; Climatology; Geography; Geology; Archaeology","score_opus":0.019272790430593406,"score_gpt":0.26624211693437966,"score_spread":0.24696932650378625,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409163560","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":[0.9957472,0.0009797846,0.000007096972,0.0024970616,0.00012240307,0.00018927742,0.0000011300218,0.0000020363275,0.0004539838],"genre_scores_gemma":[0.99895257,0.00023723992,0.000046251807,0.00024371309,0.000032502223,0.0000022810332,1.41052e-7,0.0000041398944,0.00048114106],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982126,0.00021343473,0.00026845757,0.0001884322,0.0008847448,0.00023234148],"domain_scores_gemma":[0.9993273,0.0003091299,0.0001566584,0.00013906007,0.0000040309733,0.00006384269],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0012793052,0.00011013605,0.00013894313,0.00000573108,0.0005754504,0.00008255573,0.00045886933,0.000041329004,0.00006197847],"category_scores_gemma":[0.000053881657,0.000049475515,0.00005173232,0.00027271663,0.0048580193,0.00025244916,0.00024481144,0.0003170494,0.000007349631],"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":[0.000074089774,0.000089992376,0.6954609,0.000015102738,0.000027584229,0.0000036721876,0.0011150888,0.0001822806,0.28701362,0.00008434369,0.0067970282,0.009136283],"study_design_scores_gemma":[0.00033259342,0.000800212,0.9336736,0.00009013628,0.000020100846,0.000020271815,0.0017612636,0.00025403418,0.061798234,0.0003740431,0.0007830062,0.00009250038],"about_ca_topic_score_codex":0.000048996422,"about_ca_topic_score_gemma":0.0000051103593,"teacher_disagreement_score":0.2382127,"about_ca_system_score_codex":0.00010517202,"about_ca_system_score_gemma":0.000020629728,"threshold_uncertainty_score":0.9978502},"labels":[],"label_agreement":null},{"id":"W4409178341","doi":"10.1029/2024ms004644","title":"A Complete Three‐Moment Representation of Ice in the Predicted Particle Properties (P3) Microphysics Scheme","year":2025,"lang":"en","type":"article","venue":"Journal of Advances in Modeling Earth Systems","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"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 Science Foundation","keywords":"Scheme (mathematics); Moment (physics); Representation (politics); Particle (ecology); Statistical physics; Atmospheric sciences; Meteorology; Physics; Environmental science; Geology; Classical mechanics; Mathematics; Mathematical analysis; Oceanography","score_opus":0.025353555444138986,"score_gpt":0.261464442402237,"score_spread":0.236110886958098,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409178341","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":[0.93344617,0.0020809113,0.06375353,0.00011474243,0.00016070755,0.00020265489,0.0000013222134,0.0000029619496,0.00023697363],"genre_scores_gemma":[0.99693793,0.00021919451,0.0027313835,0.000033299708,0.00003099459,0.000008832815,3.168788e-7,0.0000039717684,0.00003406575],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9986952,0.000097178505,0.0006184893,0.00010810836,0.00034335177,0.0001376518],"domain_scores_gemma":[0.99950004,0.000038165752,0.00026889387,0.00014150284,0.00003272539,0.00001869339],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043906004,0.00007656506,0.00021726277,0.000005250256,0.000039835115,0.00002152586,0.00022448802,0.000025373247,0.0000056097197],"category_scores_gemma":[0.00003271706,0.000049067487,0.000045354504,0.0003705388,0.00007248135,0.0003061887,0.00004499935,0.00014501871,0.0000012306301],"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":[0.00007551841,0.00008048002,0.06675581,0.000041697014,0.0000057076713,0.000003363461,0.00088418415,0.9081968,0.022855913,0.00008904062,0.000007258129,0.0010042166],"study_design_scores_gemma":[0.00049211096,0.00011525903,0.00392176,0.00039031584,0.000008521334,0.000004968011,0.0021744384,0.9917457,0.000563632,0.00027783046,0.0002462886,0.000059138896],"about_ca_topic_score_codex":0.00028287477,"about_ca_topic_score_gemma":0.00015220897,"teacher_disagreement_score":0.083548926,"about_ca_system_score_codex":0.000051106366,"about_ca_system_score_gemma":0.000019162382,"threshold_uncertainty_score":0.2000914},"labels":[],"label_agreement":null},{"id":"W4409306968","doi":"10.5194/acp-25-3995-2025","title":"Invisible aerosol layers: improved lidar detection capabilities by means of laser-induced aerosol fluorescence","year":2025,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":11,"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":"Leibniz-Gemeinschaft; Sächsische Aufbaubank; Bundesministerium für Bildung und Forschung","keywords":"Aerosol; Lidar; Environmental science; Remote sensing; Fluorescence; Materials science; Optics; Meteorology; Geology; Physics","score_opus":0.004348276320206799,"score_gpt":0.2002585250923629,"score_spread":0.1959102487721561,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409306968","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":[0.99053615,0.00007173911,0.0028514385,0.00005462003,0.00006384976,0.00018025399,0.000014546432,0.00005519084,0.006172235],"genre_scores_gemma":[0.99199367,0.00006439154,0.003393116,0.000104536106,0.000046619338,0.00003732781,0.000008778823,0.000018106066,0.0043334756],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.998717,0.000024775181,0.00029344714,0.00045757942,0.00019596284,0.00031120126],"domain_scores_gemma":[0.9992981,0.00006264834,0.00012774144,0.00038679232,0.000022126145,0.00010257822],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.000087732624,0.00026267403,0.0002847275,2.956239e-8,0.00018428524,0.000032868225,0.00023374295,0.00015155185,0.0006940645],"category_scores_gemma":[0.000026323552,0.0002584628,0.000090141126,0.00036515167,0.0003331499,0.0001810292,0.00014540376,0.00020163164,0.000012515349],"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":[0.000039425166,0.00012339825,0.0050131655,0.00011764633,0.000029405484,5.475306e-7,0.00027117349,0.00015024983,0.9058191,0.000004231169,0.00043082438,0.08800082],"study_design_scores_gemma":[0.0004585175,0.00007752439,0.00050967274,0.000038028003,0.000041099967,0.0000014542219,0.00047305552,0.016415885,0.98084813,0.00023911321,0.0006149042,0.00028261496],"about_ca_topic_score_codex":0.0009222119,"about_ca_topic_score_gemma":0.000022572242,"teacher_disagreement_score":0.0877182,"about_ca_system_score_codex":0.000104325285,"about_ca_system_score_gemma":0.00003091984,"threshold_uncertainty_score":0.99998677},"labels":[],"label_agreement":null},{"id":"W4409509020","doi":"10.5194/egusphere-2025-1396","title":"Radiative impact of increased middle atmospheric water vapour in the aftermath of the Hunga 2022 volcanic eruption at two locations in the Northern Hemisphere","year":2025,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Canadian Space Agency","keywords":"Radiative transfer; Northern Hemisphere; Volcano; Atmospheric sciences; Vulcanian eruption; Water vapor; Southern Hemisphere; Radiant heat; Geology; Environmental science; Climatology; Meteorology; Geography; Seismology; Physics; Materials science; Optics","score_opus":0.009389417272299827,"score_gpt":0.24365549683973187,"score_spread":0.23426607956743203,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409509020","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":[0.9897826,0.00016988299,0.0002040318,0.00043063678,0.00007099188,0.0010345462,0.00005002398,0.0000087624085,0.008248551],"genre_scores_gemma":[0.997659,0.000064627326,0.00016642884,0.00027338933,0.000021943499,0.0002076654,0.000030081836,0.0000138256755,0.001563005],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99763227,0.0005681333,0.0005577165,0.00040029487,0.00051012204,0.0003314684],"domain_scores_gemma":[0.9984011,0.0001741884,0.00030291855,0.0010663767,0.00002037158,0.000035022935],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00072026026,0.00031154967,0.00035264596,0.0000014059774,0.00012487147,0.000024703455,0.0013868861,0.00015363682,0.002784078],"category_scores_gemma":[0.000033773915,0.00013237941,0.00032040535,0.0004921945,0.00028218032,0.0000679017,0.0010309606,0.0005309331,0.000031498916],"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":[0.00006694,0.000386434,0.8493838,0.00005833422,0.00005943614,0.0000028120542,0.015149809,0.13090353,0.002220278,0.000025635416,0.00064360717,0.0010993948],"study_design_scores_gemma":[0.00059867254,0.000059274415,0.97694415,0.00010828346,0.000069705835,0.0000045704387,0.00318061,0.017161936,0.00067581894,0.00080557936,0.00014513706,0.00024624798],"about_ca_topic_score_codex":0.053909436,"about_ca_topic_score_gemma":0.057480928,"teacher_disagreement_score":0.12756036,"about_ca_system_score_codex":0.0007765112,"about_ca_system_score_gemma":0.00013254357,"threshold_uncertainty_score":0.9981275},"labels":[],"label_agreement":null},{"id":"W4409787098","doi":"10.5194/amt-18-1885-2025","title":"Compact dual-wavelength depolarization lidar for aerosol characterization over the subtropical North Atlantic","year":2025,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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":"Lidar; Aerosol; Subtropics; Wavelength; Environmental science; Characterization (materials science); Remote sensing; Depolarization; Geography; Meteorology; Physics; Optics","score_opus":0.015032652260433935,"score_gpt":0.23159528591311532,"score_spread":0.21656263365268139,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409787098","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":[0.68488216,0.000037825692,0.31150624,0.0006435448,0.00015441999,0.0013722767,0.000004630317,0.00029876694,0.0011001357],"genre_scores_gemma":[0.98919535,0.00008689985,0.008682318,0.0012574927,0.00008748267,0.00021019868,0.00004886188,0.00003200986,0.0003994047],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99798554,0.00010130018,0.00043214113,0.00044323894,0.00063449924,0.0004033053],"domain_scores_gemma":[0.9991526,0.000047492482,0.00020105025,0.0004594209,0.00006593673,0.00007348477],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040247923,0.00028464937,0.00026309324,8.658024e-7,0.00043948097,0.0001013087,0.00032419438,0.00012357441,0.00031337308],"category_scores_gemma":[0.000082857536,0.00020580203,0.00012675406,0.0005206857,0.00015458371,0.0002003978,0.000111535854,0.00016487182,0.00002185237],"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":[0.000081348546,0.00024804054,0.87170213,0.000047132442,0.000079070705,0.000002606325,0.00013989372,0.00004411329,0.07747901,0.00041729258,0.0064821774,0.043277197],"study_design_scores_gemma":[0.00040696134,0.00020064085,0.93682104,0.00006518499,0.00010765212,0.0000033848141,0.000027360067,0.0059821336,0.014599204,0.00023197201,0.04117723,0.00037720893],"about_ca_topic_score_codex":0.0004429534,"about_ca_topic_score_gemma":0.00029648383,"teacher_disagreement_score":0.30431315,"about_ca_system_score_codex":0.0003872666,"about_ca_system_score_gemma":0.000050423838,"threshold_uncertainty_score":0.8392363},"labels":[],"label_agreement":null},{"id":"W4409848966","doi":"10.5194/egusphere-2025-1680-cc1","title":"Comment on egusphere-2025-1680 - Commonalities to Doppler wind lidar on Aeolus","year":2025,"lang":"en","type":"peer-review","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"","keywords":"Lidar; Doppler effect; Geography; Environmental science; Meteorology; Remote sensing; Physics; Astronomy","score_opus":0.024236452473377426,"score_gpt":0.2830127400732265,"score_spread":0.2587762875998491,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409848966","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00035965792,0.0023747599,0.00007644667,0.35071033,0.001857094,0.0012668278,0.0002701419,0.00011493277,0.6429698],"genre_scores_gemma":[0.000492185,0.001214836,0.0006805631,0.31747434,0.00022045658,0.00010336911,0.0002077777,0.00004182596,0.67956465],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9963542,0.00015125934,0.000620714,0.0009636346,0.0012505151,0.0006596336],"domain_scores_gemma":[0.9980329,0.0002369818,0.00017958895,0.0012081931,0.000019808804,0.00032251634],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0003720541,0.0007380647,0.000942632,0.0000039487295,0.000262797,0.00007587748,0.001050481,0.00031487623,0.09774275],"category_scores_gemma":[0.000054744232,0.0005802994,0.00031580322,0.0003173324,0.00018512184,0.00006312138,0.0009928647,0.00068016764,0.00799874],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027218708,0.00019335379,0.00015975085,0.00028178297,0.00005012293,0.000011918283,0.000053746237,0.00024893263,0.0000010034121,0.0020670597,0.98741215,0.009492977],"study_design_scores_gemma":[0.00022345419,0.00040769318,0.0005319767,0.0021130934,0.00008328017,0.000001695898,0.00006622564,0.000013480814,0.000031798652,0.00030378695,0.99557936,0.0006441345],"about_ca_topic_score_codex":0.005174162,"about_ca_topic_score_gemma":0.0008346716,"teacher_disagreement_score":0.08974401,"about_ca_system_score_codex":0.0008042674,"about_ca_system_score_gemma":0.000067473804,"threshold_uncertainty_score":0.99966484},"labels":[],"label_agreement":null},{"id":"W4409971054","doi":"10.1021/acs.estlett.5c00364","title":"Increased UV–Visible Particle Absorption via Evaporation and Drying of Aqueous Droplets Containing Catechol/HONO Solutions","year":2025,"lang":"en","type":"article","venue":"Environmental Science & Technology Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Environment and Climate Change Canada","keywords":"Catechol; Aqueous solution; Evaporation; Absorption (acoustics); Particle (ecology); Photochemistry; Chemical engineering; Chemistry; Materials science; Organic chemistry; Meteorology; Composite material; Physics","score_opus":0.004963813708176999,"score_gpt":0.2044253088612439,"score_spread":0.1994614951530669,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409971054","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":[0.9893144,0.00009156318,0.0074932524,0.0023128737,0.000066014676,0.00024716966,0.0000022923475,0.000084394436,0.00038804175],"genre_scores_gemma":[0.99780136,0.00002610722,0.0014793735,0.0005986667,0.000005841316,0.000035738496,0.0000027226654,0.000007905122,0.000042252188],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9984619,0.000026873187,0.00027545093,0.0004922926,0.00029472384,0.00044877027],"domain_scores_gemma":[0.9994475,0.000022438204,0.00013863272,0.0003141565,0.0000026015616,0.00007462399],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00041328897,0.00015292698,0.00016180049,0.00003113182,0.00058271876,0.00002728342,0.00033298088,0.00010097645,0.00019959152],"category_scores_gemma":[0.000030075784,0.00015383815,0.000031239317,0.0009116058,0.0031650527,0.00039118112,0.00047914078,0.00016842183,0.000053983527],"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":[0.000008297925,0.00004873687,0.19267964,0.0000017908521,0.000004013315,0.0000028712207,0.00010789084,0.000345786,0.7947125,0.00021473413,0.000035643126,0.011838106],"study_design_scores_gemma":[0.00095992064,0.0002627388,0.52890503,0.000040341252,0.00005541913,0.00002962431,0.0013133186,0.015209241,0.45042342,0.0016048728,0.0007407283,0.0004553254],"about_ca_topic_score_codex":0.0004002165,"about_ca_topic_score_gemma":0.000038569986,"teacher_disagreement_score":0.34428903,"about_ca_system_score_codex":0.00042321597,"about_ca_system_score_gemma":0.000016358903,"threshold_uncertainty_score":0.9995478},"labels":[],"label_agreement":null},{"id":"W4410254366","doi":"10.22541/essoar.174690768.83700237/v1","title":"Kernel-Based Estimation of Stratospheric Aerosol Radiative Effects from Volcanic and Wildfire Events","year":2025,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"McGill University","funders":"","keywords":"Volcano; Aerosol; Radiative transfer; Environmental science; Kernel (algebra); Estimation; Atmospheric sciences; Remote sensing; Meteorology; Geography; Geology; Mathematics; Physics; Economics","score_opus":0.004759210939746303,"score_gpt":0.22286135072991978,"score_spread":0.21810213979017348,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410254366","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":[0.93122745,0.00027588935,0.06349083,0.00007019891,0.00024413792,0.00068544055,0.000046643258,0.000054951983,0.0039044826],"genre_scores_gemma":[0.9785578,0.00004324131,0.020194845,0.00017938693,0.000018728284,0.0000657402,0.00005746838,0.000015206844,0.00086756446],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984486,0.00009140095,0.00032956593,0.00060137716,0.0003190878,0.00020994255],"domain_scores_gemma":[0.9990228,0.00017032083,0.00028100237,0.00041441454,0.0000058407722,0.00010563666],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00009254268,0.0003206,0.00042732764,0.000001400854,0.00006810668,0.00002166858,0.00028984493,0.00027129767,0.0009283407],"category_scores_gemma":[0.000044383884,0.00028888855,0.00010214644,0.00015080556,0.00017058314,0.000074018135,0.0005314494,0.00026681018,0.00003353981],"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":[0.00013866975,0.0005532973,0.45101023,0.00063473196,0.00031624018,0.000011226308,0.001226426,0.43913537,0.002206038,0.000073724514,0.003084363,0.10160966],"study_design_scores_gemma":[0.0010280467,0.00015502513,0.50096744,0.0004410977,0.00018298063,2.6238283e-7,0.000076604345,0.4857924,0.008046736,0.002727237,0.00004078753,0.0005414168],"about_ca_topic_score_codex":0.004129867,"about_ca_topic_score_gemma":0.00025315396,"teacher_disagreement_score":0.10106825,"about_ca_system_score_codex":0.00017582656,"about_ca_system_score_gemma":0.00008303291,"threshold_uncertainty_score":0.9999849},"labels":[],"label_agreement":null},{"id":"W4410838830","doi":"10.1038/s41612-025-01062-4","title":"Microphysical detection of nano-ice nuclei to ice crystals: a platform for ice nucleation research","year":2025,"lang":"en","type":"article","venue":"npj Climate and Atmospheric Science","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"European Space Agency; Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Ice nucleus; Ice crystals; Nucleation; Ice formation; Nano-; Materials science; Nanotechnology; Geology; Physics; Atmospheric sciences; Meteorology; Composite material; Thermodynamics","score_opus":0.01976905397347048,"score_gpt":0.303378732441485,"score_spread":0.28360967846801455,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410838830","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":[0.98427224,0.000059350554,0.0072299764,0.00028586542,0.00016344705,0.00054141943,0.0000062097574,0.000037542333,0.007403938],"genre_scores_gemma":[0.9808072,0.000087574794,0.01822826,0.00028879844,0.000031627605,0.00004388616,6.7875646e-7,0.000013297564,0.0004987064],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99779445,0.000029778104,0.00030325633,0.0006446665,0.00057830586,0.00064954144],"domain_scores_gemma":[0.9991413,0.00017995344,0.00009491373,0.000320211,0.000098010016,0.00016563827],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011210805,0.00015834424,0.00021342485,0.0000030700955,0.00093144504,0.00012075161,0.0004732818,0.000077560835,0.00012559965],"category_scores_gemma":[0.00019114466,0.0001401905,0.000055067918,0.0022234386,0.00095129,0.00047292103,0.0005175032,0.00012877611,0.00006119138],"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":[0.00011939452,0.000092914874,0.0022400392,0.000047024056,0.0000042466672,6.188784e-7,0.00064775755,0.0003505923,0.9229191,0.0006842744,0.00030486606,0.07258917],"study_design_scores_gemma":[0.0025784224,0.0028245328,0.26504084,0.00046746398,0.00010995507,0.000018052213,0.0114475405,0.118434325,0.5173637,0.0050656535,0.0752797,0.0013697945],"about_ca_topic_score_codex":0.000499403,"about_ca_topic_score_gemma":0.00006293302,"teacher_disagreement_score":0.4055554,"about_ca_system_score_codex":0.00023452572,"about_ca_system_score_gemma":0.000058172885,"threshold_uncertainty_score":0.71640164},"labels":[],"label_agreement":null},{"id":"W4410896146","doi":"10.1175/bams-d-23-0309.1","title":"The High-Altitude Aerosols, Water Vapor, and Clouds Mission: Concept, Scientific Objectives, and Data Products","year":2025,"lang":"en","type":"article","venue":"Bulletin of the American Meteorological Society","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"St. Francis Xavier University; University of Waterloo; Wilfrid Laurier University; Western University; Université de Sherbrooke; University of Toronto; National Research Council Canada; Environment and Climate Change Canada; Dalhousie University; University of New Brunswick; University of Saskatchewan; University of Victoria; McGill University; Saint Mary's University; Université du Québec à Montréal","funders":"","keywords":"Environmental science; Meteorology; Water vapor; Atmospheric sciences; Altitude (triangle); Effects of high altitude on humans; Geology; Geography; Mathematics","score_opus":0.010972220767537882,"score_gpt":0.24398658659244787,"score_spread":0.23301436582491,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410896146","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":[0.97086686,0.00081250607,0.000106398526,0.027049078,0.00020307822,0.00032825445,0.00001401255,0.00002705812,0.0005927656],"genre_scores_gemma":[0.9876665,0.00030763887,0.005925255,0.002108294,0.000035984514,0.000010013158,0.0000055281917,0.000007824133,0.003932967],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9981064,0.00024216485,0.00024836772,0.000711743,0.00031640838,0.00037490323],"domain_scores_gemma":[0.9985747,0.0002279182,0.00016648749,0.00093201484,0.000019813204,0.000079064725],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0010326124,0.00018119044,0.00028418624,5.8563603e-7,0.0010191535,0.000088737725,0.0010227336,0.000058754416,0.00033406308],"category_scores_gemma":[0.0002406222,0.00007810145,0.00007475775,0.00026353778,0.0073221275,0.00002728346,0.003054364,0.00023387748,0.000013817345],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003373507,0.00045564034,0.09384428,0.00005174338,0.0003225664,0.0000042562333,0.001612021,0.00024783442,0.08463659,0.0016029291,0.7555695,0.06131528],"study_design_scores_gemma":[0.00061029376,0.0003065957,0.30270612,0.000021119005,0.000117164505,0.000009098017,0.0013617079,0.0003265517,0.007496896,0.0018661182,0.68484426,0.00033408077],"about_ca_topic_score_codex":0.0006105025,"about_ca_topic_score_gemma":0.0000071567183,"teacher_disagreement_score":0.20886184,"about_ca_system_score_codex":0.000039067912,"about_ca_system_score_gemma":0.000018664012,"threshold_uncertainty_score":0.9953794},"labels":[],"label_agreement":null},{"id":"W4410949612","doi":"10.5194/acp-25-5433-2025","title":"Counteracting influences of gravitational settling modulate aerosol impacts on cloud-base-lowering fog characteristics","year":2025,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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":"Office of Naval Research","keywords":"Settling; Aerosol; Cloud base; Cloud computing; Environmental science; Atmospheric sciences; Gravitation; Base (topology); Environmental chemistry; Meteorology; Chemistry; Physics; Environmental engineering; Computer science; Classical mechanics; Mathematics","score_opus":0.005960048201473557,"score_gpt":0.23221841095987641,"score_spread":0.22625836275840286,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410949612","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":[0.99459684,0.000038401882,0.0012098243,0.00005040472,0.00010388452,0.00007706441,0.000013909764,0.000026250491,0.0038834496],"genre_scores_gemma":[0.99593365,0.000036515394,0.003007716,0.0002095297,0.00009971832,0.000008246466,0.000016239193,0.000013009942,0.0006753973],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9989595,0.000010849375,0.00028182467,0.00029905164,0.00021777312,0.00023104457],"domain_scores_gemma":[0.9993974,0.00012768286,0.00018190163,0.00019933989,0.000020312305,0.00007336042],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000090515154,0.0002010199,0.00022692139,3.5310325e-8,0.00016974866,0.00003763512,0.00014596285,0.00007200353,0.00037706824],"category_scores_gemma":[0.00003807202,0.00019543828,0.00006250446,0.00022851527,0.00017285817,0.0001308339,0.00008626095,0.00017062212,0.000012226662],"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":[0.00019086177,0.00034961593,0.2935257,0.00046068625,0.00014638228,0.000012591068,0.0012038826,0.034994196,0.50519705,0.00014230634,0.00043883524,0.1633379],"study_design_scores_gemma":[0.0023796796,0.00024531144,0.42761567,0.0013434152,0.0002180522,0.000018626939,0.0013205105,0.17314771,0.38361946,0.0056098998,0.002621162,0.0018604902],"about_ca_topic_score_codex":0.00009103887,"about_ca_topic_score_gemma":0.0000011082798,"teacher_disagreement_score":0.16147742,"about_ca_system_score_codex":0.000072466166,"about_ca_system_score_gemma":0.000026330623,"threshold_uncertainty_score":0.7969742},"labels":[],"label_agreement":null},{"id":"W4411389195","doi":"10.3389/fenvs.2025.1602145","title":"An updated VIIRS dark target aerosol product for continuity with MODIS: assessing regional aerosol trends","year":2025,"lang":"en","type":"article","venue":"Frontiers in Environmental Science","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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":"Goddard Space Flight Center; National Aeronautics and Space Administration","keywords":"Aerosol; Environmental science; Climatology; Remote sensing; Meteorology; Atmospheric sciences; Geography; Geology","score_opus":0.005847509206919676,"score_gpt":0.2346907027390985,"score_spread":0.22884319353217883,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411389195","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":[0.93515193,0.00009968693,0.057198763,0.00042073283,0.00047948028,0.00064690976,0.00003082554,0.00006968369,0.005901993],"genre_scores_gemma":[0.90716404,0.000011022418,0.090691335,0.00040615408,0.000032468422,0.00011680464,0.000059795053,0.000023526994,0.001494853],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9965386,0.00006642734,0.0003782982,0.0013487241,0.00077548844,0.00089248543],"domain_scores_gemma":[0.9989111,0.000015209592,0.00017296577,0.000651124,0.000005785422,0.00024385576],"candidate_categories":["metaepi_narrow","sts"],"consensus_categories":[],"category_scores_codex":[0.00067735143,0.0003588768,0.00035076178,0.000025839514,0.0007007004,0.00017783095,0.001045002,0.00009248684,0.00037091968],"category_scores_gemma":[0.000014113111,0.00030867316,0.00007236595,0.0011478073,0.003021766,0.0015309886,0.00026916224,0.00023261186,0.0000115657585],"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":[0.00022267728,0.0007375354,0.8405213,0.000007930689,0.000021436063,0.000010270788,0.0005840531,0.010439819,0.092583574,0.000042873682,0.019417983,0.03541055],"study_design_scores_gemma":[0.0027802605,0.00050473365,0.9097133,0.000063172985,0.000062180734,0.000014499525,0.0032184618,0.03589424,0.036453992,0.0006336677,0.009399879,0.0012615985],"about_ca_topic_score_codex":0.000121121186,"about_ca_topic_score_gemma":0.0000514557,"teacher_disagreement_score":0.06919201,"about_ca_system_score_codex":0.0010565759,"about_ca_system_score_gemma":0.00007776627,"threshold_uncertainty_score":0.9999365},"labels":[],"label_agreement":null},{"id":"W4411418816","doi":"10.5194/acp-25-6025-2025","title":"Shallow cloud variability in Houston, Texas, during the ESCAPE and TRACER field experiments","year":2025,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"National Research Council Canada; McGill University","funders":"U.S. Department of Energy; National Science Foundation","keywords":"Convection; Precipitation; Troposphere; Atmospheric sciences; Environmental science; Cloud fraction; Diurnal cycle; Waves and shallow water; Liquid water path; Climatology; Geology; TRACER; Meteorology; Cloud computing; Cloud cover; Oceanography; Geography","score_opus":0.003138933870154301,"score_gpt":0.20720479283208074,"score_spread":0.20406585896192644,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411418816","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":[0.9791511,0.00018311362,0.0006606139,0.00017606861,0.000042519452,0.00011229238,9.577207e-7,0.000019014344,0.01965431],"genre_scores_gemma":[0.9928002,0.00008750832,0.0011504607,0.00024581666,0.00005712701,0.0000190928,9.1920236e-7,0.000007720473,0.0056311917],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991693,0.000029382833,0.00015481382,0.0003335764,0.00010588557,0.00020706332],"domain_scores_gemma":[0.9995564,0.00009382114,0.00003692169,0.00025789515,0.0000035139888,0.00005143727],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00011611147,0.00015610733,0.00014546856,1.07431655e-8,0.00014589244,0.000032632415,0.00014714802,0.00008475703,0.0012764683],"category_scores_gemma":[0.000018729921,0.00012322921,0.000032259468,0.0001850148,0.00017900283,0.000075235825,0.00017408462,0.00018218425,0.0000061596234],"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":[0.000087207416,0.00024588002,0.85407525,0.00012901562,0.000033936594,0.0000071595286,0.000880282,0.00061199,0.033610377,0.000106799576,0.0006633695,0.10954873],"study_design_scores_gemma":[0.0013995788,0.000044156353,0.91225,0.00007462962,0.0000489407,0.000009827972,0.0007460927,0.018156948,0.054399095,0.0041546584,0.008086831,0.0006292674],"about_ca_topic_score_codex":0.00026264586,"about_ca_topic_score_gemma":0.000009254659,"teacher_disagreement_score":0.108919464,"about_ca_system_score_codex":0.00006209351,"about_ca_system_score_gemma":0.000010132981,"threshold_uncertainty_score":0.9996365},"labels":[],"label_agreement":null},{"id":"W4411419300","doi":"10.5194/egusphere-2025-2697","title":"Evaluation of the EarthCARE Cloud Profiling Radar (CPR) Doppler velocity measurements using surface-based observations","year":2025,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Nuclear Safety and Security Commission; European Space Agency; National Aeronautics and Space Administration","keywords":"Doppler effect; Remote sensing; Doppler radar; Radar; Environmental science; Meteorology; Cloud computing; Geology; Computer science; Geography; Physics; Astronomy; Telecommunications","score_opus":0.1767127914163321,"score_gpt":0.31644354374274153,"score_spread":0.13973075232640944,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411419300","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":[0.9815342,0.00006936946,0.009546717,0.00021986144,0.00066097296,0.0012582864,0.000045867488,0.00003537407,0.0066293813],"genre_scores_gemma":[0.9412959,0.0000013136796,0.05798971,0.00011873047,0.00003658214,0.000027427748,0.000028809278,0.000013207476,0.0004883025],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9961464,0.00040663974,0.0004436804,0.00046343563,0.0023218777,0.00021798591],"domain_scores_gemma":[0.998666,0.000032443924,0.00034495263,0.00069624884,0.00022190304,0.000038436643],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018554524,0.00024028539,0.00024267683,0.0000015910504,0.0002497707,0.00003214544,0.00048491155,0.0002184166,0.00082353037],"category_scores_gemma":[0.00009871439,0.00018046553,0.00017881951,0.00032243834,0.00014952646,0.000056835353,0.00077384734,0.00029839776,0.000004986118],"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":[0.0000041570433,0.00005436003,0.30576175,0.000036755944,0.000031446147,4.6693806e-8,0.00004389746,0.68570465,0.0075017717,0.00002322967,0.00031965662,0.0005182699],"study_design_scores_gemma":[0.0004885805,0.000009649432,0.33331797,0.00019581904,0.0004349628,1.8310227e-7,0.00014261351,0.6293824,0.034647148,0.000964208,0.000096296775,0.00032019586],"about_ca_topic_score_codex":0.0032405735,"about_ca_topic_score_gemma":0.0005995813,"teacher_disagreement_score":0.056322277,"about_ca_system_score_codex":0.0007524087,"about_ca_system_score_gemma":0.000577901,"threshold_uncertainty_score":0.901708},"labels":[],"label_agreement":null},{"id":"W4411474806","doi":"10.1016/j.jaerosci.2025.106636","title":"Direct inversion for bidimensional distributions of aerosol characteristics","year":2025,"lang":"en","type":"article","venue":"Journal of Aerosol Science","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"National Research Council Canada","keywords":"Aerosol; Inversion (geology); Environmental science; Atmospheric sciences; Meteorology; Statistical physics; Geology; Physics; Geomorphology","score_opus":0.008141367944034717,"score_gpt":0.2491253233773688,"score_spread":0.2409839554333341,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411474806","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":[0.9815498,0.000041460655,0.014836759,0.00065963547,0.0006648979,0.00015390954,0.0000306606,0.0000073753904,0.0020554962],"genre_scores_gemma":[0.99185723,0.000035943707,0.0074221683,0.00016572846,0.000040886927,0.0000029585424,0.0000015906293,0.000004394505,0.00046912296],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9984124,0.000021512373,0.0005007695,0.00020358028,0.00057479803,0.0002869556],"domain_scores_gemma":[0.998934,0.00012114813,0.0004644773,0.00019205485,0.00014281206,0.00014554615],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007525532,0.00011561759,0.0002603818,0.000009237033,0.00034074407,0.000033924876,0.00055048196,0.000052700016,0.00020274516],"category_scores_gemma":[0.00038497508,0.00008957185,0.00014242761,0.0007918901,0.00093265076,0.00035936775,0.00023361655,0.00011887609,0.000010970113],"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":[0.00011295269,0.0002594912,0.018800216,0.00002054388,0.000017704222,0.000004082,0.00013948607,0.0003264037,0.9629394,0.00039497862,0.013152636,0.0038321116],"study_design_scores_gemma":[0.0013343896,0.0007982121,0.035538692,0.0002607554,0.000120171055,0.00002963182,0.0002408158,0.0038160158,0.9532904,0.000278518,0.0039317817,0.00036058994],"about_ca_topic_score_codex":0.000022150572,"about_ca_topic_score_gemma":0.0000044197272,"teacher_disagreement_score":0.016738478,"about_ca_system_score_codex":0.00022232218,"about_ca_system_score_gemma":0.00020522422,"threshold_uncertainty_score":0.36526337},"labels":[],"label_agreement":null},{"id":"W4411554877","doi":"10.1016/j.atmosenv.2025.121365","title":"Enhanced continuous aerosol optical depth (AOD) estimation using geostationary satellite data: focusing on nighttime AOD over East Asia","year":2025,"lang":"en","type":"article","venue":"Atmospheric Environment","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Ministry of Science and ICT, South Korea; National Institute of Environmental Research; National Research Foundation of Korea; Ministry of Environment","keywords":"Geostationary orbit; Aerosol; Satellite; Environmental science; Meteorology; East Asia; Remote sensing; Climatology; Meteorological satellite; Geography; Atmospheric sciences; Geology; China; Aerospace engineering","score_opus":0.013781878147778997,"score_gpt":0.2514539164051041,"score_spread":0.2376720382573251,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411554877","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":[0.72163016,0.0002746045,0.25807518,0.00032074828,0.00025864862,0.0006241166,0.000010914799,0.00008923549,0.0187164],"genre_scores_gemma":[0.85200846,0.00012943748,0.14489691,0.00062126404,0.00007325865,0.000035703393,0.00008782065,0.000049350096,0.0020977834],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9968686,0.00009848311,0.0005883919,0.0010890075,0.0007206476,0.00063483266],"domain_scores_gemma":[0.99835175,0.00011076086,0.00022805737,0.0011193365,0.000005531742,0.00018457501],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00026145307,0.00045321824,0.00039802695,0.0000012570963,0.0003884142,0.00009234681,0.00056043844,0.0001847071,0.0022540516],"category_scores_gemma":[0.00003932608,0.00043298007,0.00009753913,0.00029150987,0.00037415134,0.00049381756,0.00072487764,0.00026974094,0.00082067377],"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":[0.00037108187,0.0015820041,0.0578217,0.00005656107,0.0002728723,0.00010921142,0.0008123807,0.45589292,0.05754841,0.0011018807,0.0023496337,0.42208135],"study_design_scores_gemma":[0.0030469806,0.0005704822,0.43053845,0.0002761425,0.00043123486,0.000032098364,0.0008595678,0.53313226,0.009867366,0.0008408914,0.018460369,0.0019441881],"about_ca_topic_score_codex":0.00015916137,"about_ca_topic_score_gemma":0.000021351003,"teacher_disagreement_score":0.42013717,"about_ca_system_score_codex":0.00077262154,"about_ca_system_score_gemma":0.000037728205,"threshold_uncertainty_score":0.9999573},"labels":[],"label_agreement":null},{"id":"W4412379294","doi":"10.5194/amt-18-3095-2025","title":"Radiative closure assessment of retrieved cloud and aerosol properties for the EarthCARE mission: the ACMB-DF product","year":2025,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Environment and Climate Change Canada","keywords":"Radiative transfer; Aerosol; Environmental science; Atmospheric sciences; Cloud computing; Closure (psychology); Product (mathematics); Meteorology; Remote sensing; Computer science; Physics; Mathematics; Geography; Optics; Geometry; Political science","score_opus":0.028368682434907304,"score_gpt":0.26740930368200316,"score_spread":0.23904062124709585,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412379294","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":[0.64588094,0.02467728,0.23343164,0.04139489,0.0015860723,0.023456164,0.000027609005,0.0010380845,0.028507356],"genre_scores_gemma":[0.9755005,0.00041918067,0.021705296,0.0005338441,0.00007779839,0.00046366075,9.724532e-7,0.000022161239,0.0012765859],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9977905,0.00016683825,0.00042668107,0.00046176114,0.0008383179,0.00031589114],"domain_scores_gemma":[0.9987913,0.000109189656,0.00023421813,0.00067656365,0.00013461767,0.000054148186],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015580364,0.00027456222,0.00030555262,4.2421865e-7,0.0005385651,0.000056807894,0.0005375959,0.00009184327,0.00012398488],"category_scores_gemma":[0.0002478005,0.00014031188,0.00011987336,0.0004340896,0.00053333316,0.000107666645,0.000280225,0.00021857602,0.0000012104546],"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":[0.0005557567,0.00063040317,0.33975577,0.00053190946,0.0007893955,0.000003187826,0.0032944628,0.00080536533,0.20602544,0.002737221,0.12431193,0.32055917],"study_design_scores_gemma":[0.0015826558,0.001506535,0.2535886,0.0008064171,0.0006203282,0.000009109852,0.004246641,0.010964277,0.47979346,0.002112778,0.24359834,0.001170865],"about_ca_topic_score_codex":0.00017093841,"about_ca_topic_score_gemma":0.000033613283,"teacher_disagreement_score":0.3296196,"about_ca_system_score_codex":0.00019635867,"about_ca_system_score_gemma":0.00011596346,"threshold_uncertainty_score":0.57217526},"labels":[],"label_agreement":null},{"id":"W4412472246","doi":"10.3390/rs17142458","title":"Retrieval of Cloud, Atmospheric, and Surface Properties from Far-Infrared Spectral Radiances Measured by FIRMOS-B During the 2022 HEMERA Stratospheric Balloon Campaign","year":2025,"lang":"en","type":"article","venue":"Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"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; Remote sensing; Cloud computing; Atmospheric sciences; Meteorology; Geology; Physics; Computer science","score_opus":0.006288845016196767,"score_gpt":0.1905345602067291,"score_spread":0.18424571519053234,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412472246","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":[0.9898251,0.005213648,0.0023701244,0.0003201148,0.00023663962,0.00031106506,0.00000961467,0.00005740939,0.0016562345],"genre_scores_gemma":[0.9866798,0.0005010772,0.009403327,0.00017378078,0.000054453747,4.3760345e-8,0.0000027270346,0.000025474335,0.0031593058],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99816513,0.00014234743,0.00037464593,0.00048065966,0.00042515137,0.00041206263],"domain_scores_gemma":[0.99925995,0.000066078646,0.00017371292,0.00039007465,0.000018986724,0.000091169255],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002353897,0.0002724698,0.0003482044,5.2478254e-7,0.00038409108,0.00007781466,0.00023072143,0.00011355122,0.00023428371],"category_scores_gemma":[0.00005636721,0.00020487771,0.000087577144,0.0004905486,0.00043685109,0.00013865835,0.0001697932,0.00025194994,0.00000950968],"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":[0.0002766062,0.000029571676,0.0106847035,0.00004420973,0.00011559406,0.000014773445,0.0013810672,0.0035083117,0.96146905,0.000004451972,0.0015382805,0.020933405],"study_design_scores_gemma":[0.0028004986,0.0002815356,0.16369185,0.00055495306,0.0002988773,0.000046500994,0.007986665,0.41733998,0.3944551,0.001261736,0.009628965,0.001653357],"about_ca_topic_score_codex":0.0035837076,"about_ca_topic_score_gemma":0.00018551142,"teacher_disagreement_score":0.5670139,"about_ca_system_score_codex":0.00017984431,"about_ca_system_score_gemma":0.00004068429,"threshold_uncertainty_score":0.83546704},"labels":[],"label_agreement":null},{"id":"W4412478979","doi":"10.5194/egusphere-2025-3355","title":"Aerosol Composition and Extinction of the 2022 Hunga Plume Using CALIOP","year":2025,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"University of Saskatchewan","funders":"Centre National d’Etudes Spatiales; Agence Nationale de la Recherche","keywords":"Plume; Aerosol; Extinction (optical mineralogy); Environmental science; Composition (language); Atmospheric sciences; Environmental chemistry; Chemistry; Meteorology; Geography; Physics; Mineralogy; Philosophy","score_opus":0.011930392003692811,"score_gpt":0.23705673475263944,"score_spread":0.22512634274894663,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412478979","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":[0.9761919,0.00006432305,0.008921223,0.0001594571,0.0003655511,0.0002903706,0.000013142656,0.000018963163,0.013975108],"genre_scores_gemma":[0.99422836,0.000037077614,0.00283352,0.00015917222,0.000026986527,0.000009212632,0.000004643569,0.000006132378,0.002694887],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9991265,0.00005734002,0.00020208806,0.00028412024,0.00021533144,0.000114612965],"domain_scores_gemma":[0.9995052,0.000016047175,0.00014599996,0.00029592228,0.0000065272316,0.000030294117],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00010727523,0.00013295842,0.00015942218,9.2515035e-7,0.00013857098,0.000019868232,0.0001860561,0.00014367262,0.0015960296],"category_scores_gemma":[0.000004595085,0.000095963915,0.00007146201,0.00011051264,0.00018841689,0.00003869205,0.0014296464,0.0002275834,0.0000047140297],"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":[0.000099801975,0.00044581166,0.37081447,0.00047646541,0.00015805317,0.000004916261,0.0016922955,0.15591446,0.4397332,0.0005783925,0.005394149,0.02468797],"study_design_scores_gemma":[0.0016769334,0.00017212961,0.400942,0.0010127071,0.0007909045,0.000061659746,0.0014670942,0.4526781,0.13135414,0.0040879543,0.0036867347,0.0020696113],"about_ca_topic_score_codex":0.0015817671,"about_ca_topic_score_gemma":0.00012056375,"teacher_disagreement_score":0.30837905,"about_ca_system_score_codex":0.00013361532,"about_ca_system_score_gemma":0.000018794673,"threshold_uncertainty_score":0.99931663},"labels":[],"label_agreement":null},{"id":"W4412633040","doi":"10.22541/essoar.175336446.61872125/v1","title":"Estimation of Global Ocean TOA Instantaneous Clear-Sky Albedo from CERES for Shortwave Cloud Radiative Effect Analysis Based on A Deep Learning Model","year":2025,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"","keywords":"Shortwave; Albedo (alchemy); Sky; Environmental science; Radiative transfer; Cloud computing; Shortwave radiation; Meteorology; Remote sensing; Climatology; Computer science; Geography; Geology; Physics; History","score_opus":0.005985504491512097,"score_gpt":0.24913554731954007,"score_spread":0.243150042828028,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412633040","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.48112524,0.000023419378,0.5072295,0.000042811906,0.00008453608,0.0006152345,0.00021586298,0.00006091166,0.010602472],"genre_scores_gemma":[0.95722055,0.000011276552,0.041754134,0.00015939069,0.000029467761,0.0000401608,0.0003119727,0.000018353367,0.00045469854],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9976304,0.00017319329,0.0004939194,0.0008746689,0.0005056699,0.00032211762],"domain_scores_gemma":[0.99848974,0.0004908118,0.0003719011,0.0005103555,0.000019567358,0.0001175987],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00027672402,0.0004309069,0.0007856411,0.0000068402633,0.00014868892,0.000052309297,0.00041552412,0.00034610342,0.0007508895],"category_scores_gemma":[0.00016923415,0.00037804246,0.00054634264,0.00045754688,0.00013891679,0.000051465293,0.0004405154,0.00034706763,0.000013134584],"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":[0.00045725593,0.00007877824,0.03333655,0.000042533113,0.00036127557,0.0000031950601,0.00020758077,0.94508886,0.000009689531,0.000121579214,0.00014888524,0.02014382],"study_design_scores_gemma":[0.00044749965,0.00035850465,0.006905971,0.000057204863,0.0010254321,1.8293441e-7,0.00008865939,0.98916954,0.00021985725,0.001369674,0.000017874016,0.0003396055],"about_ca_topic_score_codex":0.0034349896,"about_ca_topic_score_gemma":0.0010148996,"teacher_disagreement_score":0.47609532,"about_ca_system_score_codex":0.00078721193,"about_ca_system_score_gemma":0.00006383966,"threshold_uncertainty_score":0.99986714},"labels":[],"label_agreement":null},{"id":"W4412841067","doi":"10.1007/s44274-025-00311-w","title":"Seasonal AOD analysis based on AERONET observations in North and West Africa over 2010–2019","year":2025,"lang":"en","type":"article","venue":"Discover Environment","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"Centre de réadaptation Lethbridge-Layton-Mackay","funders":"National Oceanic and Atmospheric Administration","keywords":"AERONET; Geography; Climatology; Environmental science; Meteorology; Geology; Aerosol","score_opus":0.00840743643038669,"score_gpt":0.20035822895937655,"score_spread":0.19195079252898986,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412841067","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":[0.99220693,0.000066011715,0.0030153391,0.0006009448,0.00004537187,0.00019590043,0.00005350703,0.000010837974,0.003805143],"genre_scores_gemma":[0.99406797,0.000044163615,0.00084269076,0.00090427074,0.000009206259,0.000044359,0.000055082077,0.000009555297,0.0040227296],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99868214,0.00004266348,0.0002027719,0.00046042737,0.00034189408,0.00027011137],"domain_scores_gemma":[0.99944025,0.0000531356,0.00005652907,0.000367797,7.1807386e-7,0.000081556],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000079245016,0.00018527958,0.00019654556,0.000008845438,0.00009816203,0.000033204724,0.00015682448,0.000056938934,0.003265104],"category_scores_gemma":[0.000006474888,0.0001646601,0.00008353912,0.00049923576,0.00015719511,0.00013006851,0.00017581809,0.000121966434,0.0001497974],"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":[0.000018843797,0.00022352293,0.858245,0.0000021035605,0.000035131758,0.0000031933268,0.00008595988,0.13888885,0.00009301254,0.000061497914,0.0017581745,0.00058467407],"study_design_scores_gemma":[0.00040583182,0.00003985959,0.9571991,0.00000530779,0.00010149902,5.918236e-8,0.000038136965,0.033748664,0.000012430734,0.000040435632,0.008242295,0.00016638744],"about_ca_topic_score_codex":0.0005413253,"about_ca_topic_score_gemma":0.001022096,"teacher_disagreement_score":0.10514018,"about_ca_system_score_codex":0.00027672312,"about_ca_system_score_gemma":0.000012270015,"threshold_uncertainty_score":0.99764603},"labels":[],"label_agreement":null},{"id":"W4412893015","doi":"10.3390/rs17152674","title":"Effects of Large- and Meso-Scale Circulation on Uprising Dust over Bodélé in June 2006 and June 2011","year":2025,"lang":"en","type":"article","venue":"Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Institut National de la Recherche Scientifique","funders":"","keywords":"Environmental science; Circulation (fluid dynamics); Climatology; Meteorology; Atmospheric sciences; Geology; Geography; Physics; Mechanics","score_opus":0.003193451690339321,"score_gpt":0.21647375621201376,"score_spread":0.21328030452167443,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412893015","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":[0.992408,0.0002618215,0.004322109,0.00021736654,0.00013308259,0.00014056322,5.3469495e-7,0.000012301618,0.0025042521],"genre_scores_gemma":[0.9962798,0.00005470485,0.0026763156,0.00018210102,0.000014065038,1.2607037e-8,7.883628e-7,0.000008322014,0.0007839066],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99927706,0.000044165572,0.0001510894,0.00022962657,0.00012449818,0.0001735836],"domain_scores_gemma":[0.9997227,0.00006923823,0.000057171233,0.000111416215,0.0000036489116,0.000035818164],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015714797,0.00009923884,0.00015743848,0.0000052449627,0.00007521633,0.000014215151,0.000025368618,0.000075257085,0.000020180652],"category_scores_gemma":[0.000022396744,0.000095722105,0.000020117102,0.00014878016,0.00007594236,0.00006540447,0.00008010831,0.000094321025,0.000005892503],"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":[0.000115698764,0.00013807387,0.15873091,0.00029853932,0.00003407044,0.00006468838,0.0017835628,0.003105587,0.5241857,0.00011356063,0.002329963,0.30909964],"study_design_scores_gemma":[0.00096405693,0.000025809855,0.8250892,0.0003307864,0.000031433345,0.0000070535557,0.000103552826,0.15807825,0.0135029955,0.0006351545,0.001041621,0.00019009541],"about_ca_topic_score_codex":0.00073224556,"about_ca_topic_score_gemma":0.00033850985,"teacher_disagreement_score":0.6663583,"about_ca_system_score_codex":0.00006410001,"about_ca_system_score_gemma":0.00000505071,"threshold_uncertainty_score":0.3903434},"labels":[],"label_agreement":null},{"id":"W4412894949","doi":"10.5194/egusphere-2025-3465","title":"Reconciling Satellite–Model Discrepancies in Aerosol–Cloud Interactions Using Near-LES Simulations of Marine Boundary Layer Clouds","year":2025,"lang":"en","type":"preprint","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Biological and Environmental Research; Canada First Research Excellence Fund","keywords":"Aerosol; Cloud computing; Satellite; Boundary layer; Environmental science; Meteorology; Atmospheric sciences; Planetary boundary layer; Layer (electronics); Boundary (topology); Remote sensing; Geology; Physics; Computer science; Materials science; Mathematics; Astronomy; Mechanics; Nanotechnology","score_opus":0.04159283575333022,"score_gpt":0.30191477600026273,"score_spread":0.2603219402469325,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412894949","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":[0.9338303,0.00014543325,0.0218522,0.00018922456,0.00046877438,0.00041071666,0.00006553799,0.00006992088,0.04296784],"genre_scores_gemma":[0.9183727,0.00011973779,0.075305894,0.00010271104,0.000058240785,0.000018758281,0.000052649473,0.000026116562,0.005943225],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99764866,0.00008459829,0.00086982525,0.00068646687,0.00032843786,0.00038202666],"domain_scores_gemma":[0.99873036,0.00016644501,0.00030340045,0.0006750226,0.000034855413,0.00008992082],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00025496614,0.00038051844,0.0005354448,0.000008695251,0.00027180018,0.00010677821,0.00041936623,0.0002742642,0.0045823855],"category_scores_gemma":[0.000078674806,0.00036667744,0.00022791959,0.0003636529,0.00040870902,0.00019266672,0.0024661208,0.0007130406,0.000021046715],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002648033,0.00013242877,0.117142394,0.000068729394,0.000034019293,0.0000021454348,0.0010153197,0.8743641,0.0011022794,0.00012356223,0.000088377026,0.0059002126],"study_design_scores_gemma":[0.00022597048,0.000015839876,0.010545399,0.00021727543,0.00006786809,0.000002362466,0.00043986496,0.982893,0.0006655666,0.0021694957,0.0023161236,0.00044124603],"about_ca_topic_score_codex":0.023980573,"about_ca_topic_score_gemma":0.02020416,"teacher_disagreement_score":0.108528934,"about_ca_system_score_codex":0.0005534633,"about_ca_system_score_gemma":0.00020875754,"threshold_uncertainty_score":0.9998785},"labels":[],"label_agreement":null},{"id":"W4413038252","doi":"10.3390/rs17152728","title":"Freezing Fog Microphysics and Visibility Based on CFACT Feb 19 Case","year":2025,"lang":"en","type":"article","venue":"Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Ontario Tech University","funders":"Türkiye Bilimsel ve Teknolojik Araştırma Kurumu","keywords":"Environmental science; Aerosol; Atmospheric sciences; Visibility; Relative humidity; Ice crystals; Effective radius; Meteorology; Physics","score_opus":0.007197724086308419,"score_gpt":0.2360280145437971,"score_spread":0.22883029045748868,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413038252","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":[0.94948614,0.000022401047,0.040969517,0.00026020754,0.00008316476,0.00010854548,0.0000015294462,0.00003879215,0.009029684],"genre_scores_gemma":[0.9760186,0.0000029155663,0.022622494,0.0010402737,0.000022931037,6.234514e-9,8.523135e-7,0.000009480999,0.00028243067],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99917334,0.000048825434,0.0001263089,0.00033509347,0.00011443762,0.00020199838],"domain_scores_gemma":[0.9994968,0.00008873786,0.000040393705,0.00029604245,0.0000045364304,0.000073447976],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013775376,0.00012633565,0.00012863634,0.0000016662342,0.00024708692,0.000038485592,0.000044528784,0.00005453853,0.0000366202],"category_scores_gemma":[0.00004218627,0.00011651603,0.000045035806,0.00017860715,0.000123194,0.000042091015,0.00009319212,0.00012623933,0.000028378405],"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":[0.000057020487,0.000041787942,0.004690455,0.00003687967,0.000013445141,0.00077867426,0.0002657374,0.008174077,0.107977755,0.00001631408,0.00063036435,0.8773175],"study_design_scores_gemma":[0.00048043352,0.000056525358,0.006507515,0.00008301399,0.000030762363,0.00011221213,0.00016391277,0.97900707,0.010841441,0.00091547146,0.0015313625,0.00027027845],"about_ca_topic_score_codex":0.0021707285,"about_ca_topic_score_gemma":0.00013620626,"teacher_disagreement_score":0.970833,"about_ca_system_score_codex":0.00015282839,"about_ca_system_score_gemma":0.000014368208,"threshold_uncertainty_score":0.47513857},"labels":[],"label_agreement":null},{"id":"W4414077665","doi":"10.1029/2025jd044121","title":"Analysis of CCCma Radiative Transfer Calculations for Low‐Level Overcast Liquid Clouds Over ARM SGP and ENA Sites","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Pacific Institute for Climate Solutions; Canadian Forest Service; Environment and Climate Change Canada","funders":"National Aeronautics and Space Administration","keywords":"Overcast; Effective radius; Shortwave; Radiative transfer; Liquid water content; Atmospheric radiative transfer codes; Atmosphere (unit); RADIUS; Shortwave radiation; Ice cloud","score_opus":0.032797085628604845,"score_gpt":0.33735784646016237,"score_spread":0.30456076083155753,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414077665","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":[0.9857427,0.0002436927,0.012121402,0.00037881813,0.000041232266,0.00024168966,0.000049192677,0.000004672939,0.0011766094],"genre_scores_gemma":[0.9966114,0.00013501525,0.001873535,0.000081819766,0.00009007259,0.000013032024,0.000003811799,0.000013270588,0.001178024],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99770766,0.00016985307,0.0005415126,0.00027930245,0.00086758984,0.00043406317],"domain_scores_gemma":[0.9980705,0.00115659,0.00012644945,0.00022204725,0.00019578535,0.00022867393],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006871589,0.00017150477,0.0005662837,0.000009861465,0.0002298785,0.00004864305,0.00032577533,0.00010076918,0.0010540646],"category_scores_gemma":[0.00040245918,0.0001322933,0.00042825227,0.0016842736,0.00064088963,0.00023923784,0.0001577949,0.00031136634,0.000006774874],"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":[0.012685309,0.009463809,0.4962022,0.0005158819,0.01347942,0.00010424117,0.007855176,0.08381388,0.18365623,0.029285822,0.027296051,0.13564198],"study_design_scores_gemma":[0.001608932,0.0018600133,0.9372917,0.000083078376,0.0006203934,0.0000014992022,0.0006371217,0.046932694,0.004001804,0.003540526,0.0031964588,0.00022578976],"about_ca_topic_score_codex":0.0007701492,"about_ca_topic_score_gemma":0.0003660244,"teacher_disagreement_score":0.44108948,"about_ca_system_score_codex":0.00018143147,"about_ca_system_score_gemma":0.00011024355,"threshold_uncertainty_score":0.9998591},"labels":[],"label_agreement":null},{"id":"W4414122920","doi":"10.1016/j.jaerosci.2025.106677","title":"Flash atomisation of saltwater through convergent-divergent nozzles: implications for marine cloud brightening","year":2025,"lang":"en","type":"article","venue":"Journal of Aerosol Science","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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":"Great Barrier Reef Foundation","keywords":"Aerosol; Nozzle; Evaporation; Flux (metallurgy); Flash (photography); Flash evaporation; Volumetric flow rate","score_opus":0.012751011937830424,"score_gpt":0.2749947524591613,"score_spread":0.26224374052133087,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414122920","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":[0.93617815,0.000036334102,0.0580248,0.0015876335,0.00071134785,0.00024883542,0.000005057422,0.000008814029,0.0031990518],"genre_scores_gemma":[0.9734214,0.00005788344,0.025230242,0.0003126707,0.00006354305,0.000008065179,9.4604565e-7,0.000005970071,0.0008992913],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9985179,0.000019257377,0.00057148957,0.00022668694,0.00038206152,0.00028262244],"domain_scores_gemma":[0.9989895,0.00006423652,0.0004833378,0.0002252964,0.00013735461,0.00010022279],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006191276,0.00011484613,0.00021761555,0.000007420062,0.00029630464,0.00003797318,0.0006222923,0.000044588363,0.00049654586],"category_scores_gemma":[0.00010000148,0.00008772793,0.00013311753,0.0006049809,0.0006102205,0.0005144099,0.00028273225,0.000094616065,0.000018332992],"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":[0.00013630967,0.0002606032,0.28037468,0.00004105966,0.000048597136,0.0000014937461,0.0012256271,0.003161832,0.6818028,0.004281288,0.018836763,0.009828975],"study_design_scores_gemma":[0.0026552917,0.00077208877,0.2927002,0.00016785008,0.0001842619,0.000052900778,0.0005681728,0.0026292496,0.67245364,0.011197071,0.016080095,0.00053914846],"about_ca_topic_score_codex":0.00007789092,"about_ca_topic_score_gemma":0.00002082307,"teacher_disagreement_score":0.037243262,"about_ca_system_score_codex":0.00023945047,"about_ca_system_score_gemma":0.00013644177,"threshold_uncertainty_score":0.5436829},"labels":[],"label_agreement":null},{"id":"W4414213420","doi":"10.3389/frsen.2025.1654779","title":"Climatology and variability of smoke aerosols from MAIAC EPIC observations over North America (2016–2024)","year":2025,"lang":"en","type":"article","venue":"Frontiers in Remote Sensing","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Office of Naval Research; National Aeronautics and Space Administration","keywords":"Smoke; Aerosol; EPIC; Atmosphere (unit); Biomass burning","score_opus":0.009404566012717297,"score_gpt":0.22378750333110142,"score_spread":0.21438293731838412,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414213420","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":[0.83960366,0.00010502835,0.15656248,0.0002561897,0.00064854353,0.00015074476,0.000014376264,0.000017398625,0.002641598],"genre_scores_gemma":[0.76551056,0.00009859592,0.23360533,0.0004202052,0.000012561908,1.7057067e-7,0.000009948861,0.000008863137,0.0003337427],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99873424,0.000119955694,0.00035384134,0.0003983254,0.00012964255,0.00026398106],"domain_scores_gemma":[0.9993476,0.000109107335,0.00012343754,0.00035670522,0.000009444195,0.000053674823],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014169379,0.00014452451,0.00034364598,0.000005616503,0.00009068216,0.0000134591955,0.000118287746,0.00010525079,0.00012811074],"category_scores_gemma":[0.00012299401,0.00014432878,0.000047203335,0.0004436368,0.0005421284,0.000088379405,0.0002058428,0.00017450188,0.000003855321],"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":[0.000020807081,0.000018944354,0.93522274,0.000010383887,0.000019027697,0.0000051421093,0.0002461421,0.00041402603,0.00041450257,0.0000110821065,0.003526474,0.060090717],"study_design_scores_gemma":[0.00029027637,0.00001605933,0.92213875,0.000042795935,0.000030276682,9.719972e-7,0.00026723286,0.06866789,0.00006391245,0.005206782,0.0031296005,0.00014544124],"about_ca_topic_score_codex":0.005915003,"about_ca_topic_score_gemma":0.00049808406,"teacher_disagreement_score":0.07704284,"about_ca_system_score_codex":0.000139432,"about_ca_system_score_gemma":0.000026281072,"threshold_uncertainty_score":0.8941754},"labels":[],"label_agreement":null},{"id":"W4414260187","doi":"10.1029/2025jd043713","title":"Going Off Grid: A Comparative Study of the Lagrangian and Eulerian Perspectives of New Particle Formation Events","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"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","funders":"Office of Science; U.S. Department of Energy","keywords":"Lagrangian; Eulerian path; Aerosol; Lagrangian and Eulerian specification of the flow field; Range (aeronautics); Particle (ecology); Outflow; Event (particle physics)","score_opus":0.03156561091804061,"score_gpt":0.3354957253251873,"score_spread":0.3039301144071467,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414260187","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":[0.9980053,0.00026236955,0.00013779511,0.00034633014,0.000038352693,0.00024833754,9.270403e-7,0.000001895772,0.0009587386],"genre_scores_gemma":[0.99887854,0.000038212413,0.0002946121,0.000008487657,0.000041627573,0.0000022551671,5.1406726e-8,0.000003695081,0.00073249574],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99833536,0.00027020765,0.0003470123,0.00011487952,0.00073239504,0.00020017078],"domain_scores_gemma":[0.999217,0.00020518778,0.00022341582,0.00016076003,0.00009607796,0.000097568125],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044511058,0.000081961094,0.00025159775,0.000001457468,0.00014449711,0.000018824827,0.00031043257,0.00002646347,0.00013211528],"category_scores_gemma":[0.00016194757,0.00005051191,0.00008323581,0.0005606999,0.00029085067,0.0002540799,0.00027227902,0.00025830444,0.0000055186733],"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":[0.0016939258,0.0049215807,0.7833292,0.000092019975,0.00044750798,0.00001045238,0.095953725,0.0029279653,0.0475836,0.0021435707,0.009161901,0.05173456],"study_design_scores_gemma":[0.0011266709,0.0012353163,0.935637,0.000104444036,0.000030263398,0.0000018394525,0.05344003,0.0026486095,0.0033432385,0.0019871136,0.00038629395,0.000059178863],"about_ca_topic_score_codex":0.0009190173,"about_ca_topic_score_gemma":0.00040861417,"teacher_disagreement_score":0.15230781,"about_ca_system_score_codex":0.000087468965,"about_ca_system_score_gemma":0.00006420051,"threshold_uncertainty_score":0.2059816},"labels":[],"label_agreement":null},{"id":"W4414444727","doi":"10.1016/j.aeolia.2025.101002","title":"Validation of a 10-meter wind in simulating a dust event in northwestern Iran mountains (October 28–31, 2017)","year":2025,"lang":"en","type":"article","venue":"Aeolian Research","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Wind speed; Visibility; Altitude (triangle); Boundary layer; Planetary boundary layer; Mineral dust; Wind direction; Maximum sustained wind; Atmospheric model","score_opus":0.047574517790460874,"score_gpt":0.3587452197002133,"score_spread":0.3111707019097524,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414444727","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":[0.98399144,0.000025081612,0.00007424799,0.00030795267,0.000027858005,0.00036579548,0.0000027632627,0.000006687065,0.015198194],"genre_scores_gemma":[0.9907395,0.00000867436,0.00021539998,0.00004979716,0.00001423588,0.000022613629,0.0000054782386,0.000009202749,0.008935052],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981306,0.00018815997,0.00035263773,0.0003349997,0.0005289063,0.00046465252],"domain_scores_gemma":[0.9993922,0.00015934235,0.000050468538,0.00031312622,0.000020435436,0.00006442821],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010586487,0.00010663982,0.00017090209,0.000023447648,0.00007543242,0.000025834948,0.00030103466,0.000093571405,0.0011385134],"category_scores_gemma":[0.00009474262,0.00010043782,0.000043539992,0.0010550934,0.00020679171,0.00015830358,0.00037738614,0.00029752834,0.00015966015],"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":[0.00004465707,0.00014834854,0.97608477,0.00002364197,0.000005133792,0.000018908368,0.001531904,0.015209548,0.0033873324,0.000024937817,0.0006725375,0.0028482669],"study_design_scores_gemma":[0.0007673423,0.00008678622,0.9806367,0.0001181852,0.0000028367037,7.4917955e-7,0.0009858189,0.013516208,0.0021891738,0.0004819425,0.0010877273,0.00012648565],"about_ca_topic_score_codex":0.009523266,"about_ca_topic_score_gemma":0.009910809,"teacher_disagreement_score":0.006748126,"about_ca_system_score_codex":0.00036740917,"about_ca_system_score_gemma":0.000045421468,"threshold_uncertainty_score":0.9997746},"labels":[],"label_agreement":null},{"id":"W4414539876","doi":"10.1029/2025jd044878","title":"Estimation of Global Ocean TOA Instantaneous Clear‐Sky Albedo From CERES for Shortwave Cloud Radiative Effect Analysis Based on a Deep Learning Model","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"Government of Jiangsu Province; National Natural Science Foundation of China","keywords":"Shortwave; Albedo (alchemy); Cloud albedo; Moderate-resolution imaging spectroradiometer; Cloud top; Radiative transfer; Shortwave radiation; Climate model; Satellite; Atmospheric radiative transfer codes","score_opus":0.011173048473159254,"score_gpt":0.31100165210487474,"score_spread":0.2998286036317155,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414539876","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":[0.8931743,0.00008339884,0.10399815,0.00019262188,0.000055879133,0.00032270869,0.000022031067,0.000011805356,0.0021390887],"genre_scores_gemma":[0.98867,0.00001972072,0.010874248,0.000069726855,0.000088106084,0.000008618862,0.000007799129,0.000016931652,0.00024483446],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.996674,0.0004765744,0.00058780704,0.0003798208,0.001369436,0.0005123786],"domain_scores_gemma":[0.9967764,0.0022038377,0.00034902286,0.00028794206,0.00014467209,0.00023812831],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00090694206,0.00023869064,0.0006841125,0.000006372468,0.00027382074,0.00007782183,0.00051871693,0.00013271667,0.00030560573],"category_scores_gemma":[0.0013124516,0.00018487831,0.0005407801,0.0014333944,0.00039164748,0.00017327824,0.00016901188,0.00060346874,0.000016653408],"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":[0.0028834743,0.0003152048,0.036258545,0.000024599853,0.00042130498,0.000022627939,0.00014410098,0.9116998,0.00034731615,0.00040150198,0.00079999893,0.046681553],"study_design_scores_gemma":[0.0009671418,0.0025581454,0.04847503,0.00007973608,0.00029134445,7.0312615e-7,0.00021402026,0.9407528,0.0006986508,0.0057291333,0.00009095286,0.0001423544],"about_ca_topic_score_codex":0.0012920329,"about_ca_topic_score_gemma":0.00026834453,"teacher_disagreement_score":0.09549569,"about_ca_system_score_codex":0.00068131345,"about_ca_system_score_gemma":0.00015048061,"threshold_uncertainty_score":0.7539119},"labels":[],"label_agreement":null},{"id":"W4414546674","doi":"10.5194/acp-25-11363-2025","title":"Different responses of cold-air outbreak clouds to aerosol and ice production depending on cloud temperature","year":2025,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Natural Environment Research Council","keywords":"Albedo (alchemy); Aerosol; Atmosphere (unit); Cloud cover; Cloud albedo; Cloud computing; Liquid water content","score_opus":0.005036781978138009,"score_gpt":0.21900521537382772,"score_spread":0.21396843339568972,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414546674","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":[0.99530727,0.000087076194,0.00022939726,0.00031627694,0.00012694899,0.00019574973,0.0000070312367,0.000031630167,0.003698595],"genre_scores_gemma":[0.9842918,0.00006667044,0.0015017943,0.0002702875,0.00013181176,0.000023821936,0.0000034190589,0.000013616464,0.013696811],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9989469,0.00002699311,0.000188407,0.00044810103,0.00018130658,0.00020829076],"domain_scores_gemma":[0.9994594,0.000065485314,0.000070643015,0.00028864475,0.0000126090645,0.00010320873],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007871634,0.0002230691,0.00024166089,4.0809017e-8,0.00018038192,0.000023161381,0.00012365349,0.000100793455,0.00013910524],"category_scores_gemma":[0.00003498512,0.00019406671,0.000043737877,0.00026827608,0.00015726546,0.00006072982,0.00015431807,0.000165076,0.0000065532827],"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":[0.0004365491,0.00029362968,0.04842699,0.00020840643,0.000056602392,0.0000037250059,0.00062693376,0.0017591032,0.90499675,0.00028272974,0.0032042118,0.039704394],"study_design_scores_gemma":[0.00062593655,0.00018973737,0.06221617,0.00022263861,0.000083079285,0.000008169882,0.00052570115,0.00077589095,0.928583,0.0003689425,0.0058926353,0.0005080675],"about_ca_topic_score_codex":0.00005711892,"about_ca_topic_score_gemma":0.000004296638,"teacher_disagreement_score":0.039196324,"about_ca_system_score_codex":0.0000729899,"about_ca_system_score_gemma":0.000013578599,"threshold_uncertainty_score":0.79138106},"labels":[],"label_agreement":null},{"id":"W4415026078","doi":"10.1029/2024jd043033","title":"Characterizing the Shape of Cloud Particle Size Distributions in High‐Latitude Marine Cold‐Air Outbreaks","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Liquid water content; Marine stratocumulus; Northern Hemisphere; Cloud computing; Cloud top; Predictability; Radiative transfer; Climate model; Arctic","score_opus":0.015199572030769739,"score_gpt":0.2941640022637353,"score_spread":0.2789644302329656,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415026078","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":[0.994276,0.000061571634,0.00022573106,0.0037354724,0.00011390239,0.00018187749,0.0000056592976,0.0000057329175,0.0013940909],"genre_scores_gemma":[0.9977291,0.00007183957,0.00092673005,0.000115644674,0.0001292817,0.000011808465,6.6850924e-7,0.000009050302,0.0010058443],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99763626,0.00027112625,0.00056749117,0.00018388167,0.0008519245,0.0004893412],"domain_scores_gemma":[0.99823457,0.0010371255,0.0001987786,0.00028561763,0.000101121404,0.00014277494],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010256403,0.0001280269,0.00032630833,0.0000013116193,0.00020239178,0.000041935153,0.00063520786,0.000064089654,0.0014557089],"category_scores_gemma":[0.00078719,0.00008327297,0.00014486765,0.00095794065,0.00063419866,0.000199259,0.00063734053,0.0006740736,0.000053286814],"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":[0.0008457199,0.0021674428,0.7352392,0.00006156582,0.00017801164,0.000111604946,0.00061347923,0.0021363713,0.1901338,0.021672407,0.0071886955,0.039651725],"study_design_scores_gemma":[0.0006263225,0.00029891526,0.9782861,0.00007320258,0.000016353944,0.0000024202018,0.00032412846,0.0027918185,0.008517725,0.005069898,0.0039068754,0.00008624914],"about_ca_topic_score_codex":0.0023090348,"about_ca_topic_score_gemma":0.00035755197,"teacher_disagreement_score":0.24304691,"about_ca_system_score_codex":0.00023515949,"about_ca_system_score_gemma":0.00010712872,"threshold_uncertainty_score":0.9994571},"labels":[],"label_agreement":null},{"id":"W4415382946","doi":"10.5194/amt-18-5607-2025","title":"EarthCARE's cloud profiling radar antenna pointing correction using surface Doppler measurements","year":2025,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"European Space Agency; California Institute of Technology; Jet Propulsion Laboratory; National Aeronautics and Space Administration","keywords":"Doppler effect; Doppler radar; Cloud computing; Radar; Profiling (computer programming); Payload (computing); Radiation","score_opus":0.03229543915677357,"score_gpt":0.2599639101330137,"score_spread":0.2276684709762401,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415382946","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":[0.64430344,0.00063569937,0.32167423,0.0002972198,0.0020147825,0.001740563,0.0000017273886,0.0012723937,0.028059954],"genre_scores_gemma":[0.7954691,0.00004365574,0.20288917,0.0003865354,0.00009712619,0.000047214493,0.0000030700721,0.00005226364,0.0010118779],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9960622,0.00022053932,0.00070377276,0.00084246905,0.0014320795,0.00073894195],"domain_scores_gemma":[0.9987246,0.000028255525,0.00031217243,0.00063026283,0.00016501882,0.0001397386],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0015940492,0.00048066734,0.0004406277,0.0000018629809,0.00057071424,0.000114909184,0.00046956583,0.0002129723,0.00062325393],"category_scores_gemma":[0.00016590311,0.00046093896,0.00018369145,0.0010255494,0.0001874996,0.00035470104,0.00033585,0.000359219,0.00005839744],"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":[0.00007812148,0.00023540309,0.37063962,0.000051547442,0.00012072304,0.000010547104,0.00014368267,0.0007956259,0.58999217,0.000055600907,0.009497148,0.028379837],"study_design_scores_gemma":[0.0017184512,0.0005232069,0.039031934,0.001452658,0.00046305923,0.00008800743,0.0013999498,0.06219976,0.85907775,0.0011398942,0.030165186,0.0027401573],"about_ca_topic_score_codex":0.001834969,"about_ca_topic_score_gemma":0.0001171901,"teacher_disagreement_score":0.33160767,"about_ca_system_score_codex":0.0012875636,"about_ca_system_score_gemma":0.00010534844,"threshold_uncertainty_score":0.99978423},"labels":[],"label_agreement":null},{"id":"W4415620897","doi":"10.1039/d5ea00127g","title":"Chemical imaging of individual stratospheric particles sampled over North America","year":2025,"lang":"en","type":"article","venue":"Environmental Science Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Light Source (Canada)","funders":"National Oceanic and Atmospheric Administration; Canadian Light Source; Nuclear Safety and Security Commission; Biological and Environmental Research; Environmental Molecular Sciences Laboratory; Office of Science; National Aeronautics and Space Administration; U.S. Department of Energy","keywords":"Troposphere; Stratosphere; Mixing (physics); Carbon fibers; Total organic carbon; Carbon black","score_opus":0.005015879861199218,"score_gpt":0.2159786135752028,"score_spread":0.21096273371400356,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415620897","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":[0.9934454,0.00017027628,0.0010790146,0.00008687024,0.000104206796,0.00021432801,0.000017065866,0.000045919878,0.0048369467],"genre_scores_gemma":[0.9898743,0.000029058538,0.00926597,0.0005197647,0.000018338971,0.000021107662,0.000006966363,0.000014563195,0.00024994195],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9972543,0.000035421373,0.00041019655,0.0006780363,0.00096707634,0.00065497507],"domain_scores_gemma":[0.9990943,0.000059998554,0.00017651761,0.00046561184,0.0000032606738,0.00020030548],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00020994448,0.00026332992,0.0002619017,0.000001574572,0.00030306508,0.0000745469,0.0010293494,0.0000450107,0.0075955098],"category_scores_gemma":[0.00003983265,0.00023519983,0.00010304832,0.0010126738,0.0036493521,0.0004987449,0.000968778,0.0001553225,0.00017135985],"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":[0.000020039584,0.00022493223,0.8122529,0.0000039191355,0.000014203098,0.0000040557447,0.0004165246,0.001594557,0.11056769,0.000068397625,0.0008429542,0.07398982],"study_design_scores_gemma":[0.0004336843,0.000046809357,0.9663602,0.000012702189,0.000036317353,0.0000026015343,0.0014715458,0.0035856771,0.024158003,0.00031488918,0.0032636537,0.0003139175],"about_ca_topic_score_codex":0.00036531372,"about_ca_topic_score_gemma":0.00004977053,"teacher_disagreement_score":0.1541073,"about_ca_system_score_codex":0.00027852145,"about_ca_system_score_gemma":0.00005190954,"threshold_uncertainty_score":0.9990621},"labels":[],"label_agreement":null},{"id":"W4415649308","doi":"10.1016/j.jqsrt.2026.109996","title":"Combining ALI Space-based and MPL Ground-based Measurements for Improved Aerosol Characterization","year":2025,"lang":"en","type":"article","venue":"Journal of Quantitative Spectroscopy and Radiative Transfer","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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 Saskatchewan; Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency","keywords":"Lidar; Aerosol; Backscatter (email); Troposphere; Atmosphere (unit); Satellite; Stratosphere; Radiative transfer","score_opus":0.02315887859679816,"score_gpt":0.2856236336187684,"score_spread":0.26246475502197025,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415649308","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":[0.58617556,0.00014547716,0.41198444,0.0011422613,0.00010439476,0.00028118223,0.000017478313,0.000005999931,0.0001431981],"genre_scores_gemma":[0.9778062,0.00008680032,0.021380343,0.00061766244,0.000024037645,0.000015530379,0.000007687324,0.000015464446,0.00004624056],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99886787,0.00011191407,0.0003722193,0.00022898192,0.00018507888,0.00023396312],"domain_scores_gemma":[0.9994275,0.00019004692,0.00015027092,0.000068037996,0.00006275378,0.00010141985],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004475392,0.00020043894,0.00035578563,0.000015337664,0.00024945452,0.000057939622,0.000094324634,0.00006964262,0.000058937603],"category_scores_gemma":[0.00004110925,0.00016189198,0.000099794444,0.00020654511,0.00029532955,0.000278054,0.00000937321,0.00016281242,0.0000010508255],"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":[0.00089444296,0.00014409045,0.01976446,0.000041895004,0.00009847285,0.0000013081698,0.00066376384,0.00015432632,0.97642267,0.0012904537,0.0000361169,0.00048799498],"study_design_scores_gemma":[0.01300889,0.004582072,0.34700754,0.0003360296,0.00042185173,0.0000043091886,0.000919479,0.026329216,0.60420275,0.0015255364,0.0010353924,0.00062691374],"about_ca_topic_score_codex":0.000025749321,"about_ca_topic_score_gemma":0.000030569383,"teacher_disagreement_score":0.39163068,"about_ca_system_score_codex":0.00010282712,"about_ca_system_score_gemma":0.00007020433,"threshold_uncertainty_score":0.66017634},"labels":[],"label_agreement":null},{"id":"W4415772909","doi":"10.1029/2025ea004781","title":"Combined Retrieval of Cloud Parameters for TEMPO Measurements Over Canada Using Oxygen Dimer and B Band Absorption","year":2025,"lang":"en","type":"article","venue":"Earth and Space Science","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada; University of Saskatchewan","funders":"Environment and Climate Change Canada","keywords":"Reflectivity; Troposphere; Absorption (acoustics); Air pollution; Cloud computing; Atmosphere (unit); Air quality index","score_opus":0.015203211189177317,"score_gpt":0.23369365346597437,"score_spread":0.21849044227679706,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415772909","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":[0.9977921,0.00006633234,0.0010464122,0.00016515495,0.00015248268,0.00018698115,0.0000038784256,0.0000036851434,0.00058293686],"genre_scores_gemma":[0.99669904,0.000009252853,0.002637326,0.00014180796,0.0000051934608,0.0000010518694,4.0170207e-7,0.0000024318658,0.00050349795],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9991354,0.000012003538,0.00010439844,0.00024087852,0.00030821652,0.00019915479],"domain_scores_gemma":[0.9997081,0.000025135952,0.00005529854,0.00010610874,0.000014873996,0.00009049252],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003429624,0.00007516191,0.000102996455,0.0000031114416,0.00022093666,0.000029869103,0.00009384837,0.00002358866,0.00003522155],"category_scores_gemma":[0.00006698367,0.00006424179,0.000013506994,0.0002915218,0.0004523458,0.00012457724,0.00006307408,0.000036088455,3.2811735e-7],"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":[0.00013929784,0.000021785503,0.4512499,0.000028413633,0.000012463976,5.984664e-7,0.00022246575,0.0017044063,0.5450382,0.0001139854,0.0006572439,0.0008112364],"study_design_scores_gemma":[0.0008022808,0.0001213008,0.9465161,0.000029998122,0.000022759055,9.703587e-7,0.00017880648,0.012674271,0.037961807,0.00018042275,0.0013394187,0.00017185792],"about_ca_topic_score_codex":0.05291599,"about_ca_topic_score_gemma":0.018049302,"teacher_disagreement_score":0.5070764,"about_ca_system_score_codex":0.00006345362,"about_ca_system_score_gemma":0.0001367813,"threshold_uncertainty_score":0.99986875},"labels":[],"label_agreement":null},{"id":"W4415913428","doi":"10.1038/s41467-025-65127-x","title":"Reduced aerosol pollution diminished cloud reflectivity over the North Atlantic and Northeast Pacific","year":2025,"lang":"en","type":"article","venue":"Nature Communications","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"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 Toronto; Environment and Climate Change Canada","funders":"Environment and Climate Change Canada; National Oceanic and Atmospheric Administration; Imperial College London; University of Washington","keywords":"Reflectivity; Aerosol; Cloud computing; Sulfur dioxide; Cloud height; Climate model; Pollution; Climate change","score_opus":0.010001045774611908,"score_gpt":0.2647691217697463,"score_spread":0.2547680759951344,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415913428","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":[0.96928215,0.00072290807,0.00013606178,0.009897419,0.00016870639,0.00028234007,0.000007821411,0.00005363195,0.019448962],"genre_scores_gemma":[0.9974116,0.00036532574,0.00070272083,0.00071702246,0.000025380032,0.00003919361,0.000019476216,0.0000082856495,0.00071098894],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991396,0.00015312454,0.00015694946,0.00022279244,0.00015017179,0.00017735867],"domain_scores_gemma":[0.9983236,0.00013270197,0.00007601558,0.0014067774,0.000013828791,0.000047053752],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016580321,0.00012386176,0.00011485388,0.000002590738,0.00087340054,0.00005032971,0.0007063057,0.00014552278,0.00007317454],"category_scores_gemma":[0.00007517634,0.00008877955,0.000048714493,0.0005508175,0.00047880257,0.00009606602,0.0006577951,0.0006691555,0.000024134617],"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":[0.000020702097,0.00015126822,0.9741408,0.000004394214,0.000030289793,3.9648154e-7,0.0005259157,0.0000359698,0.0012825031,0.00338788,0.017043993,0.00337588],"study_design_scores_gemma":[0.0001576832,0.000015695116,0.96693903,0.000010490484,0.000034138106,0.0000030948484,0.00016546917,0.0008573279,0.00002786111,0.00023932688,0.031439517,0.00011034489],"about_ca_topic_score_codex":0.0003805413,"about_ca_topic_score_gemma":0.0052416944,"teacher_disagreement_score":0.028129457,"about_ca_system_score_codex":0.000095850075,"about_ca_system_score_gemma":0.000023373143,"threshold_uncertainty_score":0.6717579},"labels":[],"label_agreement":null},{"id":"W4416135566","doi":"10.5194/acp-25-15389-2025","title":"Evaluation of the EarthCARE Cloud Profiling Radar (CPR) Doppler velocity measurements using surface-based observations","year":2025,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; European Space Agency; National Aeronautics and Space Administration","keywords":"Doppler effect; Doppler radar; Radar; Profiling (computer programming); Cloud computing; Smoothing","score_opus":0.052863656827241146,"score_gpt":0.2676210909932627,"score_spread":0.21475743416602155,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416135566","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":[0.99158275,0.00009623658,0.0045425124,0.000058975264,0.00007318408,0.0002188821,0.0000057418524,0.000013938336,0.0034077878],"genre_scores_gemma":[0.97400826,0.0000017323182,0.025475187,0.00006486581,0.000035918336,0.000007718667,0.0000071577406,0.000008131724,0.00039103744],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9987199,0.00006479722,0.00018948372,0.00022821609,0.0006524242,0.00014518162],"domain_scores_gemma":[0.9994723,0.000024228706,0.00011690727,0.00027616258,0.0000820334,0.000028353817],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036998064,0.000133056,0.000128212,9.737343e-9,0.00023656402,0.00001685008,0.00015137909,0.00006605389,0.00026461712],"category_scores_gemma":[0.000024493238,0.00010995812,0.00006366602,0.0003740446,0.00016867371,0.00006579955,0.0000812652,0.00010000948,0.0000010992345],"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":[0.000011466389,0.00011459733,0.46399006,0.00007274152,0.00004381365,1.0295882e-7,0.000066241344,0.24185622,0.2769995,0.000026063028,0.00022524536,0.01659395],"study_design_scores_gemma":[0.0006690412,0.0000068142845,0.14395624,0.00006981075,0.00024334063,4.2061626e-7,0.00013690855,0.6249293,0.22834142,0.0012170332,0.00022719255,0.00020247158],"about_ca_topic_score_codex":0.0002509758,"about_ca_topic_score_gemma":0.0000070325405,"teacher_disagreement_score":0.3830731,"about_ca_system_score_codex":0.00016470805,"about_ca_system_score_gemma":0.00013177688,"threshold_uncertainty_score":0.4483962},"labels":[],"label_agreement":null},{"id":"W4416231624","doi":"10.5194/acp-26-4619-2026","title":"EarthCARE Cloud Profiling Radar Observations of the Vertical Structure of Marine Stratocumulus Clouds","year":2025,"lang":"en","type":"article","venue":"Atmospheric chemistry and physics","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"McGill University","funders":"Goddard Space Flight Center; Nuclear Safety and Security Commission; European Space Agency; National Aeronautics and Space Administration","keywords":"Drizzle; Marine stratocumulus; Clutter; Radar; Reflectivity; Cloud top; Doppler effect; Cloud computing","score_opus":0.006694816569381189,"score_gpt":0.21069521434156582,"score_spread":0.20400039777218462,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416231624","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":[0.99535346,0.0000487383,0.0005609449,0.00010075845,0.000061232626,0.00011478113,0.000012613629,0.00001054199,0.003736925],"genre_scores_gemma":[0.9893913,0.000012471496,0.009354566,0.000056356825,0.00004460185,0.0000027119936,0.000006668703,0.00000711594,0.0011242017],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9992558,0.00001624221,0.00021813776,0.00019476503,0.00017238123,0.00014268565],"domain_scores_gemma":[0.9995265,0.000036090896,0.00006503981,0.0003138998,0.000019288098,0.000039193743],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000026030471,0.00012963368,0.00017751832,8.943721e-9,0.00009940409,0.000007843365,0.00020826058,0.000082525905,0.0007017092],"category_scores_gemma":[0.000018078712,0.00009812451,0.00007108356,0.00035059947,0.00033419614,0.00004733881,0.0002333912,0.00015161326,7.5557136e-7],"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":[0.000032483968,0.00009044254,0.4681155,0.00018737398,0.00004952911,7.4562354e-7,0.0001597869,0.0018393697,0.5031292,0.0016361481,0.0001910345,0.024568386],"study_design_scores_gemma":[0.00056804233,0.00003494503,0.34112096,0.00006852381,0.00010665901,0.0000035588057,0.0003528492,0.012994572,0.6344083,0.009087456,0.0009998819,0.00025426867],"about_ca_topic_score_codex":0.00014848907,"about_ca_topic_score_gemma":0.000008073536,"teacher_disagreement_score":0.1312791,"about_ca_system_score_codex":0.00002684846,"about_ca_system_score_gemma":0.0000375084,"threshold_uncertainty_score":0.76832235},"labels":[],"label_agreement":null},{"id":"W4416233204","doi":"10.5194/egusphere-2025-5205","title":"Microphysics of Arctic Stratiform Boundary-layer Clouds during ARCSIX ","year":2025,"lang":"","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"Nuclear Safety and Security Commission; National Aeronautics and Space Administration","keywords":"Ice nucleus; Sea ice; Arctic; Aerosol; Arctic ice pack; Ice cloud; Cryosphere; Cloud computing","score_opus":0.006482413044031898,"score_gpt":0.22804367638654258,"score_spread":0.22156126334251067,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416233204","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":[0.92531186,0.00044208672,0.0026067456,0.00036756342,0.00055653777,0.0003693833,0.000015894464,0.000029534362,0.07030037],"genre_scores_gemma":[0.96274567,0.00026067896,0.0028950265,0.00028280873,0.00007449811,0.000009813632,0.0000017987037,0.000025545563,0.033704188],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99727374,0.00003994701,0.0008084371,0.00066577387,0.0004912602,0.00072083663],"domain_scores_gemma":[0.9987556,0.000047240042,0.0002467316,0.00074711756,0.000033064767,0.00017026099],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00016697435,0.0004256055,0.0005005504,0.000003360038,0.00045517177,0.00011546718,0.0006194934,0.00019856467,0.013838767],"category_scores_gemma":[0.000015606383,0.0003959789,0.0002819301,0.00076073746,0.0010571469,0.00027511924,0.00061020843,0.00035925314,0.00042369135],"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":[0.00028556527,0.0014179166,0.22444952,0.0011233941,0.0004047742,0.000029534678,0.0017786977,0.0022768346,0.71023226,0.0118716825,0.0011558537,0.04497399],"study_design_scores_gemma":[0.0017696709,0.00040697414,0.6520922,0.000395295,0.00026492547,0.00001011187,0.0022363726,0.0024821768,0.3273921,0.007723729,0.0042811343,0.00094531255],"about_ca_topic_score_codex":0.0013576655,"about_ca_topic_score_gemma":0.00018043579,"teacher_disagreement_score":0.42764267,"about_ca_system_score_codex":0.00041976135,"about_ca_system_score_gemma":0.00015792299,"threshold_uncertainty_score":0.9998492},"labels":[],"label_agreement":null},{"id":"W4416345008","doi":"10.1016/j.scib.2025.11.025","title":"Divergent hemispheric trends in marine dust deposition over the past two decades","year":2025,"lang":"en","type":"article","venue":"Science Bulletin","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"National Key Research and Development Program of China; State Key Laboratory of Satellite Ocean Environment Dynamics; National Natural Science Foundation of China; Natural Science Foundation of Zhejiang Province; Ontario Ministry of Natural Resources and Forestry; Safety, Infrastructure, and Operations; Oregon State University; Langley Research Center; National Aeronautics and Space Administration; Decatur Area Arts Council","keywords":"Deposition (geology); Climate change; Northern Hemisphere","score_opus":0.004809989787220616,"score_gpt":0.2371784969779434,"score_spread":0.2323685071907228,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416345008","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":[0.9284209,0.000027253895,0.000315097,0.0036422145,0.00017161122,0.000085469226,6.297095e-7,0.000023122757,0.06731372],"genre_scores_gemma":[0.99000084,0.000012715172,0.0014389823,0.0010786435,0.000027071574,0.000023202228,0.0000011458549,0.0000045021325,0.007412922],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99861884,0.000031458716,0.00017411959,0.00040114348,0.0004013116,0.00037315287],"domain_scores_gemma":[0.99956715,0.000026090021,0.000049548955,0.0002822546,0.0000063735533,0.00006857527],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00044210328,0.00011891105,0.00009187094,0.000005579278,0.00037680595,0.00007598068,0.00058536895,0.000030734587,0.013709667],"category_scores_gemma":[0.000023954435,0.000081307444,0.00004114277,0.0016825406,0.00078524475,0.000076189455,0.0006671245,0.00013108445,0.00026292543],"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":[0.000019655683,0.000112110996,0.87055993,0.0000027768012,0.0000027787562,0.000009274247,0.00020621813,0.0022652743,0.01154049,0.0005921506,0.022115773,0.092573576],"study_design_scores_gemma":[0.0002534176,0.000021050191,0.97084737,0.00000970587,0.0000055564574,0.000002838864,0.00015670246,0.0009908952,0.0012164251,0.00017467156,0.026201535,0.000119816046],"about_ca_topic_score_codex":0.0015873838,"about_ca_topic_score_gemma":0.00028185442,"teacher_disagreement_score":0.10028747,"about_ca_system_score_codex":0.0002431601,"about_ca_system_score_gemma":0.000016911019,"threshold_uncertainty_score":0.9871919},"labels":[],"label_agreement":null},{"id":"W4416453424","doi":"10.5194/amt-19-3625-2026","title":"From real-time to long-term source apportionment of PM <sub>10</sub> using high-time-resolution measurements of aerosol physical properties: methodology and example application at an urban background site (Aosta, Italy)","year":2025,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Apportionment; Aerosol; Air quality index; Aethalometer; Biomass burning; AERONET","score_opus":0.05755201367310392,"score_gpt":0.27087864766795555,"score_spread":0.21332663399485163,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416453424","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":[0.829778,0.00010252455,0.16833523,0.000032112013,0.000024755283,0.0012962518,0.0000072237353,0.00014429349,0.00027958662],"genre_scores_gemma":[0.92104745,0.000022565448,0.078199364,0.00007077891,0.000050896426,0.00023870489,0.000032332773,0.000046439483,0.00029147777],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9964146,0.00040317452,0.00078265934,0.00089476706,0.0010715644,0.0004332588],"domain_scores_gemma":[0.9983245,0.000050646155,0.000539251,0.00077675626,0.00012851648,0.00018034434],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0012830639,0.00040640752,0.00066957896,0.0000040540044,0.00022274905,0.00002810849,0.00035337734,0.0001835137,0.00041582822],"category_scores_gemma":[0.000047370173,0.00038142345,0.00011281393,0.00045015287,0.00033978926,0.00026279522,0.00046331433,0.00010878472,0.000061871324],"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":[0.00021644669,0.00042310305,0.02748671,0.0000541683,0.00009265242,4.9665334e-7,0.0004963017,0.0006144324,0.95532286,0.0000034290088,0.0005280246,0.014761394],"study_design_scores_gemma":[0.000407643,0.0005178735,0.032258336,0.00017533275,0.00023395914,0.0000013944315,0.00005789319,0.0047816057,0.96096957,0.00007340161,0.00011336323,0.00040962343],"about_ca_topic_score_codex":0.0044360426,"about_ca_topic_score_gemma":0.0000934623,"teacher_disagreement_score":0.09126941,"about_ca_system_score_codex":0.0010303247,"about_ca_system_score_gemma":0.000051593808,"threshold_uncertainty_score":0.99986374},"labels":[],"label_agreement":null},{"id":"W4416505932","doi":"10.1029/2024jd043145","title":"Ship‐Based Lidar Evaluation of Southern Ocean Low Clouds in the Storm‐Resolving General Circulation Model ICON and the ERA5 and MERRA‐2 Reanalyses","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Dalhousie University","funders":"European Commission; Deutsches Klimarechenzentrum; Swedish e-Science Research Centre; Wenner-Gren Foundation; U.S. Department of Energy","keywords":"Radiosonde; Lidar; Shortwave; Cloud top; Outgoing longwave radiation; Cloud fraction; Longwave; Cloud height; Cloud cover; Climate model","score_opus":0.03885034320231199,"score_gpt":0.3359127178268634,"score_spread":0.2970623746245514,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416505932","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":[0.99624956,0.00054892484,0.001103287,0.001163694,0.000020295984,0.0002765784,0.0000018780356,0.000002364389,0.0006334342],"genre_scores_gemma":[0.9989772,0.00005492474,0.00067020004,0.00011365545,0.000066524655,0.000005896085,6.2432827e-7,0.000008263212,0.000102712394],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9964713,0.0010403907,0.00041394244,0.0001915086,0.001618804,0.0002640436],"domain_scores_gemma":[0.9986272,0.0007125483,0.00020236992,0.0002321055,0.00015616388,0.00006962178],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.005215586,0.00012110927,0.00026635695,0.000003956897,0.00023418127,0.00008870455,0.00034892157,0.00006182954,0.00008848892],"category_scores_gemma":[0.0006663731,0.00006511235,0.00010098336,0.00048712618,0.0007550289,0.00015462632,0.0001395002,0.00047560871,0.0000027622893],"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":[0.0022681283,0.00081245694,0.40733436,0.000113436334,0.0002442915,0.000017025504,0.011491163,0.48702067,0.017207798,0.0043429914,0.0017077817,0.0674399],"study_design_scores_gemma":[0.0014128331,0.000106012434,0.2236647,0.00006683669,0.000068749294,0.0000017062418,0.0018756184,0.7580538,0.0001410019,0.014524156,0.000020425854,0.00006420112],"about_ca_topic_score_codex":0.0017023552,"about_ca_topic_score_gemma":0.0003742874,"teacher_disagreement_score":0.27103308,"about_ca_system_score_codex":0.0001396569,"about_ca_system_score_gemma":0.00015424115,"threshold_uncertainty_score":0.27819353},"labels":[],"label_agreement":null},{"id":"W4416662894","doi":"10.1016/j.envres.2025.123393","title":"Spatio-temporal distribution of AOD and its response to regional energy consumption and air pollution factors in China","year":2025,"lang":"en","type":"article","venue":"Environmental Research","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Concordia University","funders":"Science and Technology Projects of Fujian Province","keywords":"Air pollution; Pollution; Aerosol; China; Distribution (mathematics); Coal; Energy consumption","score_opus":0.020308471450108355,"score_gpt":0.2915138605661459,"score_spread":0.2712053891160376,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416662894","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":[0.9983853,0.00017274768,0.00021921542,0.0008405632,0.000016799857,0.00019393531,0.000031718755,0.0000053504195,0.00013434327],"genre_scores_gemma":[0.99868804,0.00020552732,0.00005013082,0.0000490422,0.000004864985,0.000019582925,0.000045859597,0.000005548664,0.00093142194],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99865407,0.00023238135,0.00017258315,0.0002975495,0.0004052503,0.00023815403],"domain_scores_gemma":[0.99966264,0.00008715006,0.00003058897,0.00011555657,0.0000017391046,0.00010230315],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00056429935,0.000095834206,0.00010948826,0.000013011119,0.0001374661,0.0000094670495,0.0000883902,0.00007362067,0.0003524623],"category_scores_gemma":[0.000059649286,0.000091281625,0.000017569067,0.00021122696,0.00033998216,0.000114244474,0.0003202884,0.00012815786,0.000016134092],"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":[0.0006398565,0.00012312188,0.9639682,0.000008248851,0.000004452672,0.000002796347,0.00030585154,0.0002784287,0.028509088,0.00027166656,0.00030191266,0.005586334],"study_design_scores_gemma":[0.00032387002,0.00014638864,0.9909635,0.000021122394,0.0000019541355,0.0000013120979,0.00022790748,0.00051691267,0.004887357,0.00030875154,0.002524732,0.000076188175],"about_ca_topic_score_codex":0.0007624861,"about_ca_topic_score_gemma":0.00018396054,"teacher_disagreement_score":0.026995262,"about_ca_system_score_codex":0.00041087766,"about_ca_system_score_gemma":0.000012241258,"threshold_uncertainty_score":0.3859215},"labels":[],"label_agreement":null},{"id":"W4416666839","doi":"10.1038/s41598-025-25895-4","title":"Aerosol optical depth trends and variability over the Middle East from MODIS, MISR, OMI, and AERONET observations","year":2025,"lang":"en","type":"article","venue":"Scientific Reports","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"AERONET; Aerosol; Deep blue; Satellite; Arid; Calibration","score_opus":0.024315864717282885,"score_gpt":0.22720382600727257,"score_spread":0.20288796128998968,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416666839","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":[0.9857706,0.00013482953,0.0010771861,0.00090853235,0.0010541743,0.00016563624,0.00000608473,0.000032286032,0.010850668],"genre_scores_gemma":[0.9905069,0.0000052346036,0.0025883163,0.00016017079,0.000023760129,0.000024628094,0.000023582259,0.0000066140187,0.00666081],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981904,0.000053952816,0.0003390608,0.0008131507,0.00034081232,0.00026261833],"domain_scores_gemma":[0.99890804,0.00007703675,0.00010555816,0.0007703555,0.000012672673,0.00012634469],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00076913415,0.00014788222,0.00015825234,0.000003064488,0.0006028288,0.0002902534,0.00015284303,0.00007735897,0.00093755475],"category_scores_gemma":[0.000117145544,0.000102882324,0.00004652138,0.00046835162,0.0013497982,0.00018797835,0.00037506214,0.00012316328,0.000008615842],"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":[0.0000121189905,0.00016284079,0.93954146,0.000008551899,0.000028204933,0.00002711088,0.000980919,0.00027339472,0.0128962705,0.0005463147,0.029015873,0.016506923],"study_design_scores_gemma":[0.00014389982,0.000011017894,0.9771083,0.000013568794,0.000042706495,0.000013059153,0.00017526315,0.0034055912,0.00037445495,0.007486802,0.011075773,0.00014954655],"about_ca_topic_score_codex":0.00052031124,"about_ca_topic_score_gemma":0.00065010897,"teacher_disagreement_score":0.03756684,"about_ca_system_score_codex":0.00006185863,"about_ca_system_score_gemma":0.000030594303,"threshold_uncertainty_score":0.99997574},"labels":[],"label_agreement":null},{"id":"W4416771979","doi":"10.3390/atmos16121329","title":"Sensitivity of Atmospheric Energetics to Optically Thin Ice Clouds During the Arctic Polar Night","year":2025,"lang":"en","type":"article","venue":"Atmosphere","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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 du Québec à Montréal","funders":"","keywords":"Arctic; Energetics; Polar; Cloud cover; Atmosphere (unit); Radiative forcing; Climate model; Radiative transfer; Forcing (mathematics); Radiative cooling","score_opus":0.0036463105199559223,"score_gpt":0.2050303987685459,"score_spread":0.20138408824858997,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416771979","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":[0.97666216,0.00019717803,0.006512701,0.0015160302,0.0002879975,0.00032858978,0.000004519732,0.000070507485,0.014420331],"genre_scores_gemma":[0.97014356,0.00003858449,0.019578287,0.0010429871,0.000057148114,0.00001985109,0.0000012054463,0.000029969784,0.009088388],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99787885,0.00020318675,0.00042225994,0.0004967378,0.00046522918,0.00053374574],"domain_scores_gemma":[0.9986443,0.00023763967,0.00012254421,0.0007879189,0.00003871342,0.00016886576],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004969147,0.0002941479,0.00033928387,1.7648429e-7,0.00034427416,0.0000435923,0.0004870589,0.00014402629,0.0018209543],"category_scores_gemma":[0.00019154845,0.00021619041,0.00015968093,0.0008913249,0.0003347773,0.00011454807,0.00067726104,0.00028246822,0.00027223685],"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":[0.00018398726,0.0003877419,0.81823987,0.00013385147,0.00017175145,0.000075173535,0.0016452954,0.12756978,0.034847833,0.0036818848,0.0048593446,0.008203463],"study_design_scores_gemma":[0.00056030607,0.00015345277,0.9589253,0.00011357291,0.000118885146,0.00002228983,0.0011042947,0.01561451,0.0057236413,0.0006953793,0.01642316,0.00054518844],"about_ca_topic_score_codex":0.0029415588,"about_ca_topic_score_gemma":0.00090884155,"teacher_disagreement_score":0.14068542,"about_ca_system_score_codex":0.00025152325,"about_ca_system_score_gemma":0.000045627123,"threshold_uncertainty_score":0.9990915},"labels":[],"label_agreement":null},{"id":"W4416776194","doi":"10.3788/col202624.010101","title":"Spaceborne high-spectral-resolution lidar ACDL/DQ-1 measurement and validation of aerosol optical properties in 2023 Canadian wildfire smoke","year":2025,"lang":"en","type":"article","venue":"Chinese Optics Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Chinese Academy of Sciences","keywords":"Lidar; Aerosol; Atmospheric optics; Smoke; Reflectivity; Atmospheric composition","score_opus":0.010973655913796806,"score_gpt":0.20423423924885536,"score_spread":0.19326058333505855,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416776194","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":[0.99043036,0.00009180847,0.00033762326,0.0067790844,0.00014483667,0.00029337447,0.0000034184845,0.000014735779,0.001904768],"genre_scores_gemma":[0.9974659,0.000036399408,0.0018125132,0.000519215,0.000028441387,0.000023109818,0.00000397159,0.000012191888,0.00009825605],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99877375,0.000039453975,0.00025745766,0.0002891706,0.00032347892,0.00031671155],"domain_scores_gemma":[0.9995772,0.000015311147,0.000055369204,0.00022131499,0.000011117542,0.000119681165],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027485532,0.00017962685,0.00020203764,0.000011364789,0.00010324642,0.000037554455,0.00014438023,0.000081367434,0.000069720125],"category_scores_gemma":[0.000085415035,0.00014742593,0.0000374676,0.00031587595,0.00024071752,0.00013404839,0.000088661465,0.00015006383,0.000014089639],"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":[0.000069773516,0.00015261954,0.7413463,0.000075641256,0.000060459104,0.000022820488,0.00075933826,0.017739829,0.23702465,0.0004187637,0.0010491237,0.0012806564],"study_design_scores_gemma":[0.00073459354,0.000053714917,0.9831245,0.00012322691,0.000038295428,0.0000025504166,0.00010854451,0.0038202927,0.011452966,0.00015909853,0.000084465675,0.00029775465],"about_ca_topic_score_codex":0.03964861,"about_ca_topic_score_gemma":0.023883745,"teacher_disagreement_score":0.24177817,"about_ca_system_score_codex":0.00044511363,"about_ca_system_score_gemma":0.00004855842,"threshold_uncertainty_score":0.99392784},"labels":[],"label_agreement":null},{"id":"W4416827581","doi":"10.1029/2024ms004645","title":"The Climatic Impacts of a Satellite‐Based Parameterization of the Wegener‐Bergeron‐Findeisen Process for Large‐Scale Models","year":2025,"lang":"en","type":"article","venue":"Journal of Advances in Modeling Earth Systems","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Cloud computing; Cloud fraction; Cloud cover; Cloud top; Ice cloud; Satellite; Liquid water content; Scaling; Cloud height","score_opus":0.01337308156163268,"score_gpt":0.2805747887029294,"score_spread":0.2672017071412967,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416827581","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":[0.7559946,0.0036848176,0.23940818,0.00006550359,0.00030349893,0.0003260607,0.0000064548844,0.0000023707637,0.00020847982],"genre_scores_gemma":[0.9965331,0.0006111911,0.0027310972,0.00002531739,0.000021372492,0.000012862192,5.2707935e-7,0.000008411946,0.000056099936],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99839777,0.00008884183,0.0008498632,0.000108049506,0.0003577825,0.00019769646],"domain_scores_gemma":[0.9988146,0.00014184207,0.0007470211,0.00018890593,0.000075947995,0.00003167728],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00086415414,0.000102099475,0.00028931932,0.0000065556746,0.0001003334,0.000018480092,0.00032216468,0.000051569263,0.0000024280766],"category_scores_gemma":[0.00007869797,0.00005656764,0.00011907841,0.00029440914,0.00006627408,0.00026888688,0.00003452892,0.00010290997,2.1277866e-7],"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":[0.000077222816,0.000051100586,0.011135728,0.00020206672,0.000009307138,1.3623436e-7,0.00037441705,0.9862528,0.0010884111,0.00010048014,0.0000044936833,0.0007038304],"study_design_scores_gemma":[0.00043727492,0.00008003547,0.00030284753,0.00056704966,0.000021807247,0.0000016196426,0.00093231065,0.99395925,0.00167719,0.001809661,0.00015309991,0.000057851088],"about_ca_topic_score_codex":0.000024038618,"about_ca_topic_score_gemma":0.000111039044,"teacher_disagreement_score":0.2405385,"about_ca_system_score_codex":0.000045695277,"about_ca_system_score_gemma":0.00006619355,"threshold_uncertainty_score":0.23067613},"labels":[],"label_agreement":null},{"id":"W4416839384","doi":"10.1007/s10546-025-00948-3","title":"Doppler Lidar Observations of Urban Boundary Layer Response to the 8 April 2024 Total Solar Eclipse in Montreal","year":2025,"lang":"en","type":"article","venue":"Boundary-Layer Meteorology","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Fonds de recherche du Québec – Nature et technologies; Natural Sciences and Engineering Research Council of Canada; Canada Foundation for Innovation","keywords":"Solar eclipse; Eclipse; Noon; Boundary layer; Planetary boundary layer; Lidar; Subsidence; Solar irradiance","score_opus":0.014688117016006441,"score_gpt":0.24742635591837858,"score_spread":0.23273823890237214,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416839384","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":[0.9795735,0.00041697896,0.0009269236,0.0065077743,0.0009057581,0.000561817,0.000048504873,0.000035047535,0.011023709],"genre_scores_gemma":[0.9679751,0.000020667527,0.0022159833,0.003468963,0.00014408013,0.00013619027,0.000009253427,0.00002687386,0.026002906],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9971792,0.00052960264,0.00063892,0.00063085253,0.00036692416,0.0006544831],"domain_scores_gemma":[0.9985255,0.00032773303,0.00013630933,0.00084107264,0.000030352992,0.00013904292],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012399498,0.0003071816,0.00045171313,0.000021688013,0.00041892368,0.00008070594,0.00066760543,0.0002463649,0.0032078496],"category_scores_gemma":[0.0002955993,0.00024288113,0.0001577236,0.000981686,0.0006626918,0.00019472871,0.0006625875,0.00043341483,0.00045361125],"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":[0.004101832,0.0006438048,0.5560841,0.000028664448,0.00020603549,0.00008232859,0.0080056535,0.0044013467,0.06388536,0.0013168859,0.3493483,0.011895687],"study_design_scores_gemma":[0.0006990066,0.0003260783,0.70472586,0.000011839245,0.00004714884,0.00001569386,0.00031871095,0.00051555806,0.00045926083,0.001888829,0.2907735,0.00021850537],"about_ca_topic_score_codex":0.0030449168,"about_ca_topic_score_gemma":0.0072905086,"teacher_disagreement_score":0.14864175,"about_ca_system_score_codex":0.00026009182,"about_ca_system_score_gemma":0.00020045933,"threshold_uncertainty_score":0.9977034},"labels":[],"label_agreement":null},{"id":"W4416978722","doi":"10.5194/amt-18-7369-2025","title":"Water vapor content retrieval under cloudy sky conditions from SWIR satellite measurements in the context of C <sup>3</sup> IEL space mission project","year":2025,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Université du Québec à Montréal","funders":"Centre National d’Etudes Spatiales","keywords":"Water vapor; Cirrus; Context (archaeology); Satellite; Radiance; Cloud computing; Cloud fraction; Liquid water content; Liquid water path; Cloud top","score_opus":0.055628799883033035,"score_gpt":0.2744218898048745,"score_spread":0.21879308992184143,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416978722","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":[0.97145545,0.0008323388,0.0065939324,0.0018838726,0.00016526852,0.0029971318,0.00001600085,0.0002421083,0.015813883],"genre_scores_gemma":[0.99139744,0.00017409108,0.005937709,0.0015366822,0.000035098456,0.0001430766,0.000026061382,0.000033751265,0.00071609364],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9957556,0.0004541881,0.0008808881,0.0006935469,0.001618544,0.0005972044],"domain_scores_gemma":[0.9986287,0.000087806664,0.00023958806,0.00082571723,0.00013147749,0.00008672103],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0019089514,0.00044771793,0.00052919524,0.0000034650561,0.00024122935,0.00006445199,0.000770238,0.00022727708,0.00076914864],"category_scores_gemma":[0.00011558927,0.00028408607,0.00020224672,0.0006608139,0.0003433185,0.00020447253,0.00024315825,0.0003516566,0.000047508714],"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":[0.0008385764,0.0023787892,0.24178594,0.00011579866,0.00045659562,0.00002580389,0.008244489,0.0006259557,0.6940926,0.0008273417,0.027246378,0.023361756],"study_design_scores_gemma":[0.003377735,0.00096451846,0.1262299,0.0009873603,0.00043314794,0.000008129722,0.01644883,0.001538204,0.7808232,0.005006079,0.06278961,0.0013933289],"about_ca_topic_score_codex":0.005626948,"about_ca_topic_score_gemma":0.00028484463,"teacher_disagreement_score":0.11555605,"about_ca_system_score_codex":0.00074058573,"about_ca_system_score_gemma":0.00009856147,"threshold_uncertainty_score":0.99996114},"labels":[],"label_agreement":null},{"id":"W4417358441","doi":"10.5194/amt-18-7651-2025","title":"Retrieval of aerosol properties from aerosol optical depth measurements with high temporal resolution and spectral range","year":2025,"lang":"en","type":"article","venue":"Atmospheric measurement techniques","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"European Metrology Programme for Innovation and Research; Eidgenössische Technische Hochschule Zürich; European Cooperation in Science and Technology","keywords":"Aerosol; AERONET; Radiance; Effective radius; Sun photometer; Single-scattering albedo; Radiative transfer; Radiometer; Angstrom exponent; Optical depth","score_opus":0.0253443845254179,"score_gpt":0.22028077256034748,"score_spread":0.19493638803492958,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4417358441","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":[0.96053225,0.00076417375,0.027939994,0.00033644168,0.000100135665,0.0012017174,0.0000036390502,0.000315114,0.008806561],"genre_scores_gemma":[0.8909002,0.00007792013,0.10844763,0.00016850111,0.00003811395,0.00008186128,0.0000042898446,0.000032459528,0.00024902954],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9967023,0.00012954786,0.00057952316,0.0006897717,0.001414506,0.00048431545],"domain_scores_gemma":[0.9989719,0.00002128705,0.00023248329,0.000527833,0.00010586169,0.00014065277],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00073821243,0.000404422,0.0005070678,0.0000016811993,0.00020273817,0.00005720104,0.00036232866,0.00018790275,0.0002356027],"category_scores_gemma":[0.000087774584,0.0003079986,0.00008183253,0.0004835408,0.0006080937,0.00026504285,0.00023205104,0.00023933366,0.000010504957],"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":[0.0015386908,0.0005735292,0.5035534,0.000098715755,0.00025620643,0.000011894086,0.0002975009,0.00009659914,0.4759804,0.00013528415,0.0029131908,0.014544639],"study_design_scores_gemma":[0.0016190734,0.0011118973,0.12835017,0.00057686964,0.0002608675,0.0000054023844,0.00020793219,0.00049936486,0.8657521,0.000322824,0.0005745196,0.00071896845],"about_ca_topic_score_codex":0.0027471753,"about_ca_topic_score_gemma":0.00079512707,"teacher_disagreement_score":0.38977173,"about_ca_system_score_codex":0.0004939834,"about_ca_system_score_gemma":0.000082991435,"threshold_uncertainty_score":0.99993724},"labels":[],"label_agreement":null},{"id":"W6884520262","doi":"10.1051/epjconf/201611920004/pdf","title":"Airborne Lidar Measurements of Pollution above the Oil Sands Region in Northern Alberta","year":2016,"lang":"en","type":"article","venue":"Springer Link (Chiba Institute of Technology)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Lidar; Oil sands; Aerosol; Pollution; Plume; Backscatter (email); Air pollution; Depolarization ratio; Planetary boundary layer","score_opus":0.013181862182884562,"score_gpt":0.21104208292898008,"score_spread":0.19786022074609552,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6884520262","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":[0.9831099,0.00011209162,0.0005382227,0.0063096494,0.00022443796,0.00012139869,0.0000013552849,0.000043686512,0.009539288],"genre_scores_gemma":[0.99778885,0.00009798359,0.0014314228,0.000059069902,0.000031956035,0.00001877313,4.321037e-7,0.000014079118,0.0005574304],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987316,0.00001607346,0.00039131948,0.00030741576,0.00027660994,0.00027696544],"domain_scores_gemma":[0.9990782,0.000011164599,0.00025654334,0.0005989541,0.000020316691,0.00003483017],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021056223,0.00016590966,0.00023150332,0.000015432734,0.0000711141,0.0000037539692,0.0005716731,0.00022338508,0.000057047488],"category_scores_gemma":[0.00013565326,0.00010025261,0.00007657037,0.000536697,0.0009208785,0.00016529126,0.00029772622,0.00016379893,0.0000657312],"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":[0.00003669432,0.00010696714,0.7301633,0.000012491439,0.000026278038,0.0000031304714,0.00010029892,0.00018361508,0.04807163,0.0011470615,0.000045993063,0.22010256],"study_design_scores_gemma":[0.0023033486,0.00031900813,0.8242222,0.0005184217,0.000058459776,0.000015590713,0.00009977319,0.00005602372,0.12516125,0.0021696375,0.04454851,0.0005277683],"about_ca_topic_score_codex":0.0013615433,"about_ca_topic_score_gemma":0.007788283,"teacher_disagreement_score":0.2195748,"about_ca_system_score_codex":0.0001690884,"about_ca_system_score_gemma":0.00003092989,"threshold_uncertainty_score":0.43460447},"labels":[],"label_agreement":null},{"id":"W6888908209","doi":"10.23673/re-485","title":"MODIS and HYSPLIT data to study anthropogenic glaciation of supercooled liquid-water clouds","year":2024,"lang":"en","type":"other","venue":"DataDOI (University of Tartu)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"HYSPLIT; Longitude; Glacial period; Aerosol; Latitude; Supercooling","score_opus":0.021587056108236125,"score_gpt":0.235637956412451,"score_spread":0.21405090030421486,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6888908209","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":[0.96209884,0.00032853786,0.0018223074,0.00042517335,0.00026426357,0.0010895211,0.004381293,0.00009841787,0.029491676],"genre_scores_gemma":[0.79722285,0.0003331867,0.006679027,0.00007182033,0.0000871712,8.8376885e-7,0.001869226,0.00021027935,0.19352557],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9987578,0.000044135708,0.00012750823,0.000598651,0.00029378693,0.00017815815],"domain_scores_gemma":[0.9987921,0.000007503904,0.00007910141,0.0010179192,0.000005602586,0.00009776724],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00018110711,0.00017830587,0.0003203194,0.000009832991,0.000060034934,0.000010664719,0.0008209996,0.000116031704,0.015903296],"category_scores_gemma":[0.0000055276223,0.00017118697,0.000038444246,0.00015832776,0.00023186965,0.0001768644,0.0026538982,0.000101496655,0.0008190147],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035742242,0.00073817355,0.011693027,0.0003114323,0.00071774435,0.000115835006,0.008904451,0.000056050747,0.007659969,0.00005046792,0.96321464,0.006180806],"study_design_scores_gemma":[0.0015013446,0.0014129989,0.015833676,0.00020593585,0.0011128539,0.0000060683647,0.014030737,0.0008343475,0.00025731814,0.000064607935,0.9637191,0.001020987],"about_ca_topic_score_codex":0.010441668,"about_ca_topic_score_gemma":0.0033746378,"teacher_disagreement_score":0.16487597,"about_ca_system_score_codex":0.000043268952,"about_ca_system_score_gemma":0.000009369811,"threshold_uncertainty_score":0.999959},"labels":[],"label_agreement":null},{"id":"W6890000651","doi":"10.34657/7953","title":"Lidar Measurements of Canadian Forest Fire Smoke Episode Observed in July 2013 over Warsaw, Poland","year":2016,"lang":"en","type":"book-chapter","venue":"TIB Repositorium","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Lidar; AERONET; Smoke; Satellite; Aerosol","score_opus":0.03021691408456493,"score_gpt":0.210736137838743,"score_spread":0.1805192237541781,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6890000651","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.10487996,0.0010752794,0.000005245033,0.00030081018,0.0017405072,0.00057098106,0.00007273921,0.00003417264,0.8913203],"genre_scores_gemma":[0.519881,0.00013538348,0.00016632998,0.00008293175,0.00039916523,0.00001342846,0.000017568662,0.00008285698,0.4792213],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99766904,0.00002435607,0.00056189025,0.00054014416,0.0006961999,0.0005083455],"domain_scores_gemma":[0.9986169,0.000024357189,0.00033040065,0.00064469303,0.000028042654,0.00035561682],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00018676805,0.00039650846,0.0004619539,0.000013025415,0.00010254736,0.000027069482,0.00044305937,0.00047918208,0.0013820464],"category_scores_gemma":[0.000016053902,0.00033019987,0.0001550237,0.000089736444,0.00017597435,0.00012714762,0.00015942843,0.0002701217,0.00032945123],"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":[0.000059027163,0.00005610067,0.96161205,0.00006271249,0.00011345844,0.00018891435,0.00023541671,0.000057660607,0.0022104217,0.000436921,0.032958344,0.0020089773],"study_design_scores_gemma":[0.0008333029,0.00018312343,0.5360508,0.0004986444,0.00008962148,0.00001761354,0.0000051975935,0.000028219061,0.0005179156,0.0008762702,0.45999444,0.00090483896],"about_ca_topic_score_codex":0.4362561,"about_ca_topic_score_gemma":0.37885982,"teacher_disagreement_score":0.4270361,"about_ca_system_score_codex":0.00080718996,"about_ca_system_score_gemma":0.000105191684,"threshold_uncertainty_score":0.999915},"labels":[],"label_agreement":null},{"id":"W6890069095","doi":"10.34657/5276","title":"Smoke of extreme Australian bushfires observed in the stratosphere over Punta Arenas, Chile, in January 2020 : optical thickness, lidar ratios, and depolarization ratios at 355 and 532nm","year":2020,"lang":"en","type":"article","venue":"TIB Repositorium","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Lidar; Depolarization ratio; Stratosphere; Smoke; Aerosol; Depolarization; Southern Hemisphere; Polarization (electrochemistry)","score_opus":0.022145781760782846,"score_gpt":0.21728404980451307,"score_spread":0.19513826804373022,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6890069095","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":[0.9961883,0.00029324804,0.000050310042,0.0017647075,0.00008851569,0.0003479028,0.0000044819885,0.0000147004075,0.0012478651],"genre_scores_gemma":[0.99887747,0.000073617244,0.0005069462,0.00023832246,0.00012870887,0.000013777707,0.000014415689,0.000012580285,0.00013417666],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99856794,0.000105511375,0.00039321833,0.00037476604,0.00034567446,0.00021289058],"domain_scores_gemma":[0.9995067,0.000053799256,0.00012141725,0.00020344756,0.000007696318,0.00010690844],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000159928,0.00017601895,0.00021363155,0.0000013782338,0.00010886017,0.000073543284,0.00018271955,0.00014670179,0.00014329045],"category_scores_gemma":[0.000045432404,0.00013671676,0.00002883904,0.00029365957,0.00018501635,0.00025866,0.00016989156,0.00022327784,0.000003802795],"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":[0.000056109868,0.000058774214,0.9389509,0.000033339078,0.000008263803,0.000049023543,0.0020739636,0.00019171982,0.057608422,0.0000926488,0.0005661991,0.00031066083],"study_design_scores_gemma":[0.00045755596,0.00011179857,0.9917518,0.000028370841,0.000018576002,0.0000223222,0.00056738243,0.0011461102,0.0052547855,0.00004618107,0.00042762165,0.00016751848],"about_ca_topic_score_codex":0.0019980548,"about_ca_topic_score_gemma":0.0010838582,"teacher_disagreement_score":0.0528009,"about_ca_system_score_codex":0.000053904314,"about_ca_system_score_gemma":0.000022188586,"threshold_uncertainty_score":0.5575147},"labels":[],"label_agreement":null},{"id":"W6890089597","doi":"10.34657/866","title":"Dependence of solar radiative forcing of forest fire aerosol on ageing and state of mixture","year":2003,"lang":"en","type":"article","venue":"TIB Repositorium","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Plume; Forcing (mathematics); Aerosol; Radiative forcing; Dilution; Radiative cooling; Radiative transfer; Panache","score_opus":0.004850771478701822,"score_gpt":0.2002959122088477,"score_spread":0.19544514073014588,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6890089597","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":[0.99477136,0.00015053323,0.0011988439,0.0000091752845,0.00014667616,0.00013149864,0.000002936761,0.0000064724127,0.0035824778],"genre_scores_gemma":[0.9979324,0.000029320663,0.0015846568,0.000011366094,0.000017681283,0.0000029922023,5.72807e-7,0.0000101895685,0.00041082717],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99905556,0.000045067427,0.0002727546,0.00019483468,0.00027420183,0.00015757751],"domain_scores_gemma":[0.99938744,0.000064744105,0.00027410747,0.00020031964,0.00001527129,0.000058095102],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014768781,0.00010849655,0.00020735525,0.0000013820151,0.000060221348,0.0000068879203,0.000104067185,0.00005288226,0.000034120938],"category_scores_gemma":[0.000054456763,0.00009271996,0.00004530243,0.000112324684,0.00015266004,0.00011397716,0.000054277858,0.000090047295,0.0000017347418],"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":[0.00009721858,0.00017491747,0.63971174,0.00014979944,0.00005224096,0.000043049826,0.0037794318,0.010566937,0.33907163,0.00018728359,0.00022766952,0.0059380573],"study_design_scores_gemma":[0.00047239955,0.00057808775,0.19739394,0.00013322172,0.000035866888,0.000016448503,0.00033477286,0.0016792193,0.79866546,0.0002879259,0.00018638646,0.0002162381],"about_ca_topic_score_codex":0.00056710816,"about_ca_topic_score_gemma":0.00004545887,"teacher_disagreement_score":0.45959386,"about_ca_system_score_codex":0.000037783615,"about_ca_system_score_gemma":0.000013646649,"threshold_uncertainty_score":0.37810102},"labels":[],"label_agreement":null},{"id":"W6892356262","doi":"10.5281/zenodo.10530625","title":"cfe-lab/Kive: Update Bulbasaur physical drive settings in the template; finalize Bulbasaur deployment","year":2024,"lang":"en","type":"other","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Crosslight Software (Canada); University of British Columbia; AIDS Vancouver","funders":"","keywords":"Software deployment; Key (lock); Process (computing); Troubleshooting; Software; Focus (optics)","score_opus":0.014639128605839968,"score_gpt":0.23994431858579254,"score_spread":0.22530518997995258,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6892356262","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0057481197,0.00024195203,0.0004468185,0.0023007202,0.00016125772,0.0009387059,0.00025708033,0.0008997953,0.98900557],"genre_scores_gemma":[0.1798934,0.0007998854,0.0011895212,0.0033420706,0.001276234,0.0000018199115,0.002159055,0.021299694,0.7900383],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.997365,0.00033519664,0.00026249027,0.000774095,0.0007307171,0.00053247623],"domain_scores_gemma":[0.9990301,0.00002037228,0.00015590985,0.0006339136,0.000024677793,0.00013504257],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00053786207,0.00033185317,0.00026197406,0.000021887563,0.000574753,0.00054224505,0.0015763723,0.00014433442,0.08943258],"category_scores_gemma":[0.00008690716,0.0002627185,0.000098326986,0.0006907601,0.0003445911,0.00009819192,0.0018565138,0.0006332847,0.097148],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015853679,0.00016833631,0.000008012367,0.0000564933,0.00003360415,0.00010429746,0.0014423768,0.00003780866,0.0001887374,0.0005797851,0.9871076,0.010257094],"study_design_scores_gemma":[0.00026124486,0.0001496195,0.00019695394,0.00010480663,0.000033698514,0.00006604212,0.00041666074,0.00022707946,0.000029917901,0.00028632034,0.9979205,0.00030716436],"about_ca_topic_score_codex":0.0002384725,"about_ca_topic_score_gemma":0.000008073301,"teacher_disagreement_score":0.19896723,"about_ca_system_score_codex":0.00025878608,"about_ca_system_score_gemma":0.0000032640871,"threshold_uncertainty_score":0.9999825},"labels":[],"label_agreement":null},{"id":"W6893296547","doi":"10.5281/zenodo.15025626","title":"Best Practice Protocol for the validation of Aerosol, Cloud, and Precipitation Profiles (ACPPV)","year":2025,"lang":"en","type":"article","venue":"elib (German Aerospace Center)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"Japan Aerospace Exploration Agency; Jet Propulsion Laboratory; National Oceanic and Atmospheric Administration; Hellenic Foundation for Research and Innovation; European Commission; Bundesministerium für Bildung und Forschung; European Space Agency; National Aeronautics and Space Administration","keywords":"Protocol (science); Software deployment; Best practice; Data assimilation; Baseline (sea); Data validation; Calibration; Data quality; Field (mathematics)","score_opus":0.012270487218537848,"score_gpt":0.3146633897318151,"score_spread":0.3023929025132773,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6893296547","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":[0.68641204,0.00013408494,0.041378506,0.011695625,0.0011433596,0.23427936,0.00006625296,0.00017966195,0.024711104],"genre_scores_gemma":[0.7848088,0.000075459444,0.017047215,0.0011869611,0.00024454782,0.177197,0.0000400194,0.00007375105,0.019326251],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99882936,0.00007722961,0.00029310893,0.00031523482,0.000247071,0.00023800493],"domain_scores_gemma":[0.9990894,0.00024491452,0.00027093195,0.00030037138,0.00004430463,0.000050051116],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003354482,0.00016905238,0.00015598518,0.0000026227574,0.0002479472,0.00006700304,0.00022107191,0.00007549803,0.0001589281],"category_scores_gemma":[0.00015709082,0.00012404293,0.00006068533,0.0002020568,0.00023269968,0.00035922683,0.00018531436,0.00010670602,0.0000318815],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0039443667,0.0052719275,0.35149112,0.0017929943,0.0005255481,0.0000063366283,0.017993134,0.0025660181,0.107804716,0.01045086,0.43070695,0.06744603],"study_design_scores_gemma":[0.009823984,0.0016857476,0.053686287,0.00080486975,0.00037905955,0.000021655895,0.0048618726,0.006086561,0.18233012,0.0009077541,0.7383052,0.00110686],"about_ca_topic_score_codex":0.00006763472,"about_ca_topic_score_gemma":0.000022675977,"teacher_disagreement_score":0.3075983,"about_ca_system_score_codex":0.0000702468,"about_ca_system_score_gemma":0.000021102422,"threshold_uncertainty_score":0.5058324},"labels":[],"label_agreement":null},{"id":"W6893327205","doi":"10.5281/zenodo.16419563","title":"Drivers of Droplet Formation in East Mediterranean Orographic Clouds","year":2025,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Impact","funders":"","keywords":"Aerosol; Orographic lift; Troposphere; Cloud condensation nuclei; Sea salt aerosol; Boundary layer; Particle (ecology); Planetary boundary layer; Scanning mobility particle sizer","score_opus":0.017293881858122275,"score_gpt":0.22373690139765168,"score_spread":0.2064430195395294,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6893327205","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":[0.80058366,0.000028204198,0.0061278134,0.0006288752,0.00009680486,0.0003538097,0.000028358827,0.00019880073,0.19195366],"genre_scores_gemma":[0.9989334,0.00004040828,0.00025771366,0.00008850488,0.000014658261,3.447346e-8,0.00014583247,0.00015469635,0.00036479105],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9989471,0.0001281406,0.00023220094,0.00021147788,0.00026395003,0.00021714318],"domain_scores_gemma":[0.9995682,0.000008931692,0.000078361,0.00023932544,0.00004140697,0.00006374271],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0003289363,0.00008639064,0.000108640495,0.000020874595,0.00046035647,0.0000809721,0.0005435327,0.000048357368,0.0132231945],"category_scores_gemma":[0.00009904545,0.00008837911,0.000037773363,0.00092489726,0.00023729523,0.00022775956,0.0006470285,0.00013522865,0.0010783965],"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":[0.00025239415,0.00075939996,0.00413415,0.00024083546,0.00006915377,0.000035583696,0.014672002,0.0028439688,0.051389873,0.008658011,0.2646555,0.65228915],"study_design_scores_gemma":[0.0012688028,0.0002754309,0.039473996,0.00008835657,0.000018887571,0.000028466853,0.002509523,0.005909306,0.0013701691,0.00068869686,0.9481055,0.00026283754],"about_ca_topic_score_codex":0.000058383193,"about_ca_topic_score_gemma":0.000004865537,"teacher_disagreement_score":0.68345004,"about_ca_system_score_codex":0.0001355767,"about_ca_system_score_gemma":0.0000010595559,"threshold_uncertainty_score":0.99969935},"labels":[],"label_agreement":null},{"id":"W6893499196","doi":"10.5281/zenodo.3585577","title":"Airborne elastic cloud lidar for ice-water content retrievals during the HAIC-HIWC 2015 campaign","year":2017,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","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":"Environment and Climate Change Canada","funders":"","keywords":"Lidar; Backscatter (email); Cloud computing; Inversion (geology); Ice crystals; Liquid water content; Altitude (triangle); Data processing","score_opus":0.03550088296078095,"score_gpt":0.24037008255322112,"score_spread":0.20486919959244015,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6893499196","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":[0.9384732,0.0000634074,0.007760105,0.004177297,0.00040711058,0.0013016602,0.00013221157,0.0004291679,0.047255814],"genre_scores_gemma":[0.98841953,0.000034780976,0.00018358727,0.0001559698,0.00024256902,2.2511576e-7,0.0000836374,0.00061073323,0.010268994],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9982323,0.00014324502,0.00024834662,0.00043366416,0.00041608495,0.000526331],"domain_scores_gemma":[0.9986666,0.00002672139,0.00015279876,0.0008493777,0.0001224352,0.00018210377],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000822119,0.0001685683,0.00015621001,0.0000048730953,0.006209874,0.00093003485,0.0015983132,0.00006631542,0.020446466],"category_scores_gemma":[0.000666441,0.000115820236,0.000080041755,0.00009510267,0.0004769091,0.00030039414,0.0019166776,0.00020743822,0.010572485],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013387123,0.00067036675,0.001668729,0.00023755828,0.0002858773,0.000076334276,0.009380635,0.0014356187,0.2090924,0.0030872212,0.7146927,0.058033817],"study_design_scores_gemma":[0.00089411135,0.00026517455,0.03168029,0.000022349761,0.000026882717,0.000040585182,0.0004354011,0.00047093944,0.0055255787,0.00020405775,0.9601799,0.00025472796],"about_ca_topic_score_codex":0.00006937481,"about_ca_topic_score_gemma":0.0000021105423,"teacher_disagreement_score":0.24548717,"about_ca_system_score_codex":0.00023734987,"about_ca_system_score_gemma":0.0000019294419,"threshold_uncertainty_score":0.9950839},"labels":[],"label_agreement":null},{"id":"W6901830049","doi":"10.60692/tbza0-amn53","title":"Identification of topographic features influencing aerosol observations at high altitude stations","year":2018,"lang":"en","type":"article","venue":"Greater South Information System","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"","keywords":"Altitude (triangle); Effects of high altitude on humans; Elevation (ballistics); Troposphere; Digital elevation model; Planetary boundary layer; Lapse rate; Atmosphere (unit)","score_opus":0.018148314639192736,"score_gpt":0.20462286344080619,"score_spread":0.18647454880161346,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6901830049","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":[0.9828955,0.0000012289685,0.014910568,0.00004311888,0.00022416195,0.00028326802,0.000058093286,0.00009201716,0.0014920245],"genre_scores_gemma":[0.9982008,1.918345e-7,0.001129002,0.00012305786,0.000039591167,0.00005244598,0.00002388817,0.0000073087913,0.00042373606],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986464,0.00003393029,0.0006328255,0.00014279624,0.00036310378,0.00018095992],"domain_scores_gemma":[0.999003,0.0000067003716,0.00047620668,0.00035855663,0.000089460635,0.000066065666],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021058352,0.00012497391,0.00013686257,0.000012123144,0.00034687037,0.00006571233,0.00019525239,0.000078493766,0.00026666807],"category_scores_gemma":[0.00001915944,0.000108733315,0.000054313114,0.00044806857,0.00015963927,0.00079190824,0.00010945636,0.000051165734,0.0008768687],"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":[0.000021845637,0.000004285242,0.94360095,0.00007168006,0.00002701491,2.5610066e-7,0.051383063,0.0019107172,0.0015052598,0.0006195816,0.0006460514,0.00020926124],"study_design_scores_gemma":[0.00028601437,0.00003755497,0.9866589,0.00003002298,0.000022949058,0.0000053678637,0.004315988,0.0011897397,0.0071846517,0.0000052351443,0.00012497233,0.00013863316],"about_ca_topic_score_codex":0.00015026216,"about_ca_topic_score_gemma":0.00001742048,"teacher_disagreement_score":0.047067076,"about_ca_system_score_codex":0.00017981496,"about_ca_system_score_gemma":0.0000116120555,"threshold_uncertainty_score":0.99990106},"labels":[],"label_agreement":null},{"id":"W6903422454","doi":"10.1051/epjconf/202023708016/pdf","title":"Optical Properties of Canadian Biomass Burning Particles Over Europe Observed with Calipso and Ground-Based Lidar Systems","year":2020,"lang":"en","type":"article","venue":"Springer Link (Chiba Institute of Technology)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Lidar; Backscatter (email); Aerosol; Biomass burning; Biomass (ecology); Depolarization ratio","score_opus":0.025542164275414413,"score_gpt":0.1918524561349289,"score_spread":0.1663102918595145,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6903422454","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":[0.99565125,0.0002766121,0.00046491338,0.0025670063,0.00007274338,0.00023408858,0.0000040413424,0.00009396485,0.0006353958],"genre_scores_gemma":[0.99122113,0.000017151713,0.008595304,0.000087095206,0.000026179381,0.0000141901355,7.788748e-7,0.000020024232,0.000018155775],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988463,0.00001269378,0.0003000303,0.00033112295,0.000201683,0.00030819484],"domain_scores_gemma":[0.99938345,0.000005028591,0.00013076188,0.00026408164,0.000023697048,0.00019297544],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000912461,0.00017693145,0.00028856014,0.000019579276,0.00010665176,0.000023727613,0.00027634262,0.00015053256,0.000024449388],"category_scores_gemma":[0.000076416036,0.00013462633,0.000031274267,0.00086488825,0.0011541935,0.00014678671,0.00017833593,0.00018616082,0.000013579658],"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":[0.00009806523,0.00008235375,0.673527,0.000299154,0.000088896566,0.0000873486,0.00028484268,0.006094814,0.30945283,0.0056540365,0.00004429708,0.0042863605],"study_design_scores_gemma":[0.003242987,0.002055522,0.44098505,0.0010475363,0.000260097,0.000044189885,0.0007853304,0.040086873,0.4082779,0.00008251792,0.10161232,0.0015196893],"about_ca_topic_score_codex":0.026345162,"about_ca_topic_score_gemma":0.006485813,"teacher_disagreement_score":0.23254193,"about_ca_system_score_codex":0.00005045232,"about_ca_system_score_gemma":0.00008297675,"threshold_uncertainty_score":0.9801385},"labels":[],"label_agreement":null},{"id":"W6907629162","doi":"10.25316/ir-10174","title":"Nanaimo Free Press [Saturday, September 4, 1897]","year":2019,"lang":"en","type":"other","venue":"VIUSpace (Vancouver Island University Library)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"","score_opus":0.004820857145183688,"score_gpt":0.1673179340477538,"score_spread":0.16249707690257012,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6907629162","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00010490175,0.00020734844,0.00030056192,0.00018740614,0.0010710949,0.00046576216,0.00022784118,0.00041899353,0.9970161],"genre_scores_gemma":[0.0005289895,0.00035466137,0.0017883634,0.0002457134,0.00020253847,0.0000010983229,0.000008089489,0.0003543697,0.99651617],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9980081,0.00008282241,0.00013361637,0.00078492914,0.0004619855,0.00052859774],"domain_scores_gemma":[0.9983743,0.00003411036,0.00025058142,0.0011095862,0.0000035858475,0.0002278754],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000026193957,0.00050917425,0.00047091936,0.000012516934,0.0001269779,0.00005634849,0.0012093869,0.00056083663,0.0399289],"category_scores_gemma":[0.0000043971977,0.0004817675,0.0002192071,0.00031671676,0.00024058387,0.0005579801,0.001431679,0.0004042013,0.0026363118],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000036590205,0.000058614594,0.000557518,0.000037605612,0.000078365076,0.00009610908,0.00011737232,0.0001011492,0.000005151251,0.000096474694,0.9985787,0.00023632287],"study_design_scores_gemma":[0.00094012235,0.00005826556,0.00019057495,0.00007712635,0.000078510675,0.0000014055503,0.00018364139,0.00006932556,0.000027143442,0.000039750885,0.9976715,0.0006626209],"about_ca_topic_score_codex":0.0025924058,"about_ca_topic_score_gemma":0.14440504,"teacher_disagreement_score":0.14181262,"about_ca_system_score_codex":0.00011725957,"about_ca_system_score_gemma":0.000050215087,"threshold_uncertainty_score":0.9997634},"labels":[],"label_agreement":null},{"id":"W6908746975","doi":"10.34657/10755","title":"Extreme levels of Canadian wildfire smoke in the stratosphere over central Europe on 21-22 August 2017","year":2018,"lang":"en","type":"article","venue":"TIB Repositorium","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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; Lidar; Stratosphere; Sun photometer; Troposphere; Smoke; Photometer; Altitude (triangle); Spectroradiometer; AERONET","score_opus":0.02903238443364092,"score_gpt":0.23286650769363615,"score_spread":0.20383412325999523,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6908746975","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":[0.77711564,0.000021877693,0.0000048136517,0.00019185961,0.00056607794,0.00012716877,0.000007408716,0.000010713599,0.2219544],"genre_scores_gemma":[0.99423486,0.00000731035,0.000104355306,0.00034476543,0.00043263432,0.000003792918,0.0000017266135,0.000016473767,0.004854065],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985764,0.0000712921,0.00023370452,0.00028758502,0.00038527302,0.00044572988],"domain_scores_gemma":[0.99922365,0.000021402573,0.00009739799,0.00047925924,0.00000927929,0.00016898975],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00015677084,0.00015408546,0.00013418167,0.0000030484994,0.00017222142,0.00004297218,0.0004571513,0.00008810922,0.002386861],"category_scores_gemma":[0.00002109386,0.00011109933,0.000045592715,0.0004477003,0.00025052932,0.00011005454,0.000057887795,0.00016848529,0.00012365666],"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":[0.00004612378,0.0001759235,0.8623621,0.000008007309,0.000018765595,0.0002250943,0.0020468049,0.000120912664,0.012243865,0.00051431055,0.1195461,0.0026920093],"study_design_scores_gemma":[0.00016991046,0.00017341018,0.9416861,0.00001856814,0.0000083269715,0.000013927786,0.00016510682,0.00008144769,0.0017410122,0.000019509876,0.05577899,0.00014367967],"about_ca_topic_score_codex":0.22695792,"about_ca_topic_score_gemma":0.07688071,"teacher_disagreement_score":0.2171192,"about_ca_system_score_codex":0.00016109904,"about_ca_system_score_gemma":0.000071885974,"threshold_uncertainty_score":0.9985251},"labels":[],"label_agreement":null},{"id":"W6911147608","doi":"10.5281/zenodo.10213091","title":"Aerosols and clouds affecting the radiation budget at Pituffik (Thule), northern Greenland: Insights on the installed and newly developed ground-based instruments at the Thule High Arctic Atmospheric Observatory (THAAO)","year":2023,"lang":"en","type":"dissertation","venue":"ARCA (Università Ca' Foscari Venezia)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Arctic; Observatory; Earth's energy budget; Satellite; Zenith; The arctic; Climate model; Radiative transfer","score_opus":0.01151051915018315,"score_gpt":0.20177720745620892,"score_spread":0.19026668830602578,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6911147608","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":[0.99429333,0.0002923779,0.000013040986,0.0010348427,0.0006541723,0.0011867872,0.000025351466,0.00008793537,0.0024121713],"genre_scores_gemma":[0.9899477,0.00030275676,0.00013959441,0.00061517034,0.00008313137,0.000059532053,0.0004093566,0.00010465647,0.008338134],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.996872,0.00040057203,0.0003427922,0.0009214727,0.0008668388,0.00059629866],"domain_scores_gemma":[0.9977595,0.00067851675,0.00056479254,0.0007748306,0.000039849263,0.00018250216],"candidate_categories":["metaepi_narrow","sts"],"consensus_categories":[],"category_scores_codex":[0.00042268736,0.0006366456,0.00045767403,0.000006479783,0.0028711148,0.00015025781,0.00074380846,0.00035337254,0.00067274633],"category_scores_gemma":[0.00007381957,0.00041715946,0.0001577879,0.0007217285,0.00047378332,0.00027287658,0.00060232036,0.00059641636,0.00022855043],"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":[0.002459381,0.0004460733,0.8626776,0.0004045191,0.0014006018,0.00021992909,0.054524805,0.008996147,0.0031134838,0.0015859257,0.0048695696,0.059301995],"study_design_scores_gemma":[0.0018209644,0.0004048935,0.97997266,0.0001542172,0.0003201576,0.000013390291,0.0080241775,0.0032905913,0.00012206062,0.00055360736,0.0045466763,0.00077662116],"about_ca_topic_score_codex":0.005127639,"about_ca_topic_score_gemma":0.059157062,"teacher_disagreement_score":0.11729508,"about_ca_system_score_codex":0.0013742978,"about_ca_system_score_gemma":0.00012714288,"threshold_uncertainty_score":0.99982804},"labels":[],"label_agreement":null},{"id":"W6912020579","doi":"10.5281/zenodo.15025627","title":"Best Practice Protocol for the validation of Aerosol, Cloud, and Precipitation Profiles (ACPPV)","year":2025,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"Japan Aerospace Exploration Agency; Jet Propulsion Laboratory; National Oceanic and Atmospheric Administration; Hellenic Foundation for Research and Innovation; European Commission; Bundesministerium für Bildung und Forschung; European Space Agency; National Aeronautics and Space Administration","keywords":"Protocol (science); Software deployment; Best practice; Data assimilation; Baseline (sea); Data validation; Calibration; Data quality; Field (mathematics)","score_opus":0.026006270939410495,"score_gpt":0.2898258933858911,"score_spread":0.2638196224464806,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6912020579","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.10293028,0.00008722519,0.20782475,0.010628188,0.0003693772,0.22354327,0.00022453124,0.00076204183,0.45363033],"genre_scores_gemma":[0.96560556,0.00009413368,0.016336622,0.0007728639,0.00032884127,0.0006669774,0.00051090313,0.0014622562,0.014221823],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.999046,0.00015381219,0.00019683976,0.00023628763,0.00021294219,0.00015409711],"domain_scores_gemma":[0.9993394,0.00010811607,0.00014106117,0.00022818547,0.00014326292,0.000039952596],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005971597,0.000082849736,0.00007747962,0.000005348951,0.0011585093,0.0002039114,0.00036627994,0.000040017876,0.002640164],"category_scores_gemma":[0.0008146159,0.000065789856,0.000024892559,0.0003053314,0.00022447886,0.0002726218,0.00052669033,0.00009013795,0.00031632883],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001283025,0.0011877384,0.000412998,0.000584032,0.00016271196,0.0000017452959,0.005693834,0.0022872759,0.043043826,0.016816119,0.5068659,0.42166075],"study_design_scores_gemma":[0.0006743334,0.0003604415,0.00080091483,0.0000391989,0.000031076834,0.000007153679,0.0009516476,0.001389847,0.0063340073,0.00025040994,0.98906523,0.000095732146],"about_ca_topic_score_codex":0.000035711746,"about_ca_topic_score_gemma":3.9784925e-7,"teacher_disagreement_score":0.8626753,"about_ca_system_score_codex":0.000068998444,"about_ca_system_score_gemma":0.0000027007843,"threshold_uncertainty_score":0.9982716},"labels":[],"label_agreement":null},{"id":"W6912335475","doi":"10.5281/zenodo.15400054","title":"Presentation of the Best Practice Protocol for the Validation of Aerosol, Cloud, and Precipitation Profiles (ACPPV) to the 2nd ESA-JAXA EarthCARE In-Orbit validation workshop","year":2025,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"European Commission","keywords":"Space research; Agency (philosophy); Observatory; Presentation (obstetrics); Space Science; Aerospace; Atmospheric research; Space weather; Space (punctuation)","score_opus":0.029382759961368608,"score_gpt":0.3000581228096026,"score_spread":0.27067536284823396,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6912335475","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":[0.70658773,0.00006138698,0.051246397,0.025703186,0.0003802282,0.17560302,0.00017344183,0.00018099877,0.04006362],"genre_scores_gemma":[0.9970608,0.000012892665,0.0009027001,0.00014036345,0.000057232417,0.00021346101,0.00007464674,0.00016942793,0.0013684789],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9985266,0.00040052543,0.00030523507,0.0002537687,0.0003545347,0.00015935638],"domain_scores_gemma":[0.99893755,0.00021438717,0.00023753797,0.00035965777,0.0002190272,0.000031820015],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009225288,0.00009668626,0.0000922814,0.000010830171,0.0008959948,0.00018513695,0.00056361343,0.000047922716,0.0006769378],"category_scores_gemma":[0.0015460207,0.00006172402,0.000034816843,0.00075472693,0.00020282665,0.00029757048,0.00065991003,0.00013360169,0.000068126334],"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":[0.0033379025,0.0020292273,0.00956904,0.0012085879,0.00028703123,0.000001608115,0.05233253,0.09787389,0.08270516,0.014462713,0.2509032,0.48528913],"study_design_scores_gemma":[0.0022628892,0.00078622863,0.0306464,0.00039217438,0.00012714292,0.000012562017,0.016606146,0.006219645,0.07611981,0.00066657265,0.8658182,0.00034222045],"about_ca_topic_score_codex":0.000110572706,"about_ca_topic_score_gemma":0.000009563276,"teacher_disagreement_score":0.614915,"about_ca_system_score_codex":0.00008078518,"about_ca_system_score_gemma":0.0000060342454,"threshold_uncertainty_score":0.74119943},"labels":[],"label_agreement":null},{"id":"W6912358031","doi":"10.5281/zenodo.3517172","title":"4STAR hyperspectral sunphotometry measurements during the Oil Sands 2018 campaign near Fort McMurray, Alberta","year":2019,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Oil sands; Hyperspectral imaging; Aerosol; Extinction (optical mineralogy); Column (typography)","score_opus":0.018603277389895416,"score_gpt":0.21164706378079162,"score_spread":0.1930437863908962,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6912358031","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":[0.73342204,0.000023961748,0.00006949543,0.00021460683,0.00009415241,0.00019071781,0.0000136605495,0.0001460407,0.2658253],"genre_scores_gemma":[0.98264164,0.000027733184,0.0002342329,0.00015962646,0.000068382695,7.702734e-8,0.00006634495,0.0005952595,0.016206732],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99799865,0.00015711757,0.00021189917,0.0004535437,0.00066992437,0.0005088805],"domain_scores_gemma":[0.9990749,0.00001740418,0.0000911822,0.0005940668,0.000051257615,0.00017118776],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000521667,0.00017209325,0.00013980617,0.000007461767,0.0020991752,0.0004578831,0.0010845237,0.00006106397,0.09293954],"category_scores_gemma":[0.0001259251,0.00013849496,0.000073616844,0.0005680363,0.0002643309,0.0002610319,0.0011063908,0.0002486066,0.029810414],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007305324,0.0012611396,0.058552198,0.00030268103,0.00048510008,0.000042790758,0.019541318,0.0052195666,0.2826694,0.00089459855,0.56566805,0.06463264],"study_design_scores_gemma":[0.0010409866,0.00028096445,0.092451125,0.000025795542,0.000021219284,0.00009960494,0.0013603027,0.000517411,0.0022240998,0.000032864795,0.90152526,0.00042038056],"about_ca_topic_score_codex":0.00030693712,"about_ca_topic_score_gemma":0.0000051227935,"teacher_disagreement_score":0.33585718,"about_ca_system_score_codex":0.00036576114,"about_ca_system_score_gemma":0.000002862764,"threshold_uncertainty_score":0.9991999},"labels":[],"label_agreement":null},{"id":"W6917692975","doi":"10.57757/iugg23-0825","title":"Regional and seasonal variability of clouds in relation with environmental parameters in the Arctic region based on spaceborne remote sensing","year":2023,"lang":"en","type":"article","venue":"Publication Database GFZ (GFZ German Research Centre for Geosciences)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Canadian Nautical Research Society","funders":"","keywords":"Cloud computing; Arctic; Cloud top; Climate model; Climate change; The arctic; Cloud cover","score_opus":0.03675035660183781,"score_gpt":0.2939260570977641,"score_spread":0.2571757004959263,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6917692975","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":[0.98291385,0.0000047288904,0.003514098,0.012182805,0.000023778292,0.0010072129,0.00010067762,0.000017966311,0.00023488299],"genre_scores_gemma":[0.99338394,0.000025874166,0.005707769,0.00023285503,0.00001488899,0.000019811296,0.0005049545,0.000010060582,0.0000998294],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9966574,0.0005716727,0.0002873676,0.0006689569,0.0012625263,0.00055210845],"domain_scores_gemma":[0.9979869,0.0011479822,0.0001353256,0.0005683633,0.00003147678,0.00012994785],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.005405369,0.00013617158,0.00013338849,0.00004777227,0.0002658847,0.00007201456,0.00037174503,0.000058960613,0.00006769486],"category_scores_gemma":[0.0007205058,0.00010037682,0.00003256997,0.0017964887,0.00094630825,0.0004074809,0.00015973666,0.00028905374,0.00001733037],"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":[0.00070729136,0.000541901,0.9496522,0.00010837949,0.000007790728,0.000023420562,0.0026035386,0.0052034054,0.0007374826,0.0019055705,0.007988864,0.030520158],"study_design_scores_gemma":[0.00059354474,0.00010989213,0.5910058,0.000054258115,0.0000037253553,0.0000057430434,0.000679128,0.40400738,0.0000420466,0.00105264,0.0023279653,0.00011789774],"about_ca_topic_score_codex":0.0016165364,"about_ca_topic_score_gemma":0.0006975561,"teacher_disagreement_score":0.39880398,"about_ca_system_score_codex":0.00031154885,"about_ca_system_score_gemma":0.0000778729,"threshold_uncertainty_score":0.4093248},"labels":[],"label_agreement":null},{"id":"W6920320897","doi":"10.60692/sn52s-y0663","title":"South African dust contribution to the high southern latitudes and East Antarctica during interglacial stages","year":2022,"lang":"en","type":"article","venue":"Greater South Information System","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Université de Montréal","funders":"","keywords":"Southern Hemisphere; Mineral dust; Interglacial; Latitude; Northern Hemisphere; Quaternary; Middle latitudes; Natural (archaeology)","score_opus":0.009816856099518696,"score_gpt":0.1750252847263444,"score_spread":0.16520842862682572,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6920320897","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":[0.9948121,0.0000010615745,0.003575309,0.00027200987,0.00017725762,0.0003901797,0.00018853067,0.00008253339,0.000501039],"genre_scores_gemma":[0.9992985,3.5862136e-8,0.000077962715,0.00018111852,0.00005742503,0.00011291793,0.000009263537,0.000008275482,0.0002544918],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988041,0.00008014395,0.0003145507,0.00015841881,0.0003964407,0.0002463445],"domain_scores_gemma":[0.99949485,0.000004204317,0.00017393143,0.00021795066,0.000016052183,0.00009302292],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002992281,0.00013915704,0.0001404562,0.000007006992,0.00075508433,0.00013937932,0.00020476517,0.000031078413,0.0004745643],"category_scores_gemma":[0.000011992965,0.00009871154,0.000036468897,0.00017947676,0.000061444865,0.00024487686,0.00047908077,0.0001187907,0.0005407766],"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":[0.00010401693,0.000002341872,0.8115117,0.000021779393,0.000019122186,0.0000018057949,0.18503387,0.0030219036,0.000013860162,0.0000821212,0.000059483307,0.00012798069],"study_design_scores_gemma":[0.000900771,0.000122396,0.79152125,0.000023242688,0.000030850766,0.00004042639,0.2039962,0.0010517952,0.00008818108,0.0000016524912,0.001924437,0.00029880207],"about_ca_topic_score_codex":0.00018549139,"about_ca_topic_score_gemma":0.000013126647,"teacher_disagreement_score":0.019990461,"about_ca_system_score_codex":0.00028221376,"about_ca_system_score_gemma":0.0000075522994,"threshold_uncertainty_score":0.6950769},"labels":[],"label_agreement":null},{"id":"W6920557074","doi":"10.60692/byn73-dsv50","title":"Identification of topographic features influencing aerosol observations at high altitude stations","year":2018,"lang":"en","type":"article","venue":"Greater South Information System","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"","keywords":"Altitude (triangle); Effects of high altitude on humans; Elevation (ballistics); Troposphere; Digital elevation model; Planetary boundary layer; Lapse rate; Atmosphere (unit)","score_opus":0.018148314639192736,"score_gpt":0.20462286344080619,"score_spread":0.18647454880161346,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6920557074","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":[0.9828955,0.0000012289685,0.014910568,0.00004311888,0.00022416195,0.00028326802,0.000058093286,0.00009201716,0.0014920245],"genre_scores_gemma":[0.9982008,1.918345e-7,0.001129002,0.00012305786,0.000039591167,0.00005244598,0.00002388817,0.0000073087913,0.00042373606],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986464,0.00003393029,0.0006328255,0.00014279624,0.00036310378,0.00018095992],"domain_scores_gemma":[0.999003,0.0000067003716,0.00047620668,0.00035855663,0.000089460635,0.000066065666],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021058352,0.00012497391,0.00013686257,0.000012123144,0.00034687037,0.00006571233,0.00019525239,0.000078493766,0.00026666807],"category_scores_gemma":[0.00001915944,0.000108733315,0.000054313114,0.00044806857,0.00015963927,0.00079190824,0.00010945636,0.000051165734,0.0008768687],"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":[0.000021845637,0.000004285242,0.94360095,0.00007168006,0.00002701491,2.5610066e-7,0.051383063,0.0019107172,0.0015052598,0.0006195816,0.0006460514,0.00020926124],"study_design_scores_gemma":[0.00028601437,0.00003755497,0.9866589,0.00003002298,0.000022949058,0.0000053678637,0.004315988,0.0011897397,0.0071846517,0.0000052351443,0.00012497233,0.00013863316],"about_ca_topic_score_codex":0.00015026216,"about_ca_topic_score_gemma":0.00001742048,"teacher_disagreement_score":0.047067076,"about_ca_system_score_codex":0.00017981496,"about_ca_system_score_gemma":0.0000116120555,"threshold_uncertainty_score":0.99990106},"labels":[],"label_agreement":null},{"id":"W6920794981","doi":"10.6084/m9.figshare.19947368","title":"Additional file 1 of The impact of IgG subclass deficiency on the risk of mortality in hospitalized patients with COPD","year":2022,"lang":"en","type":"article","venue":"Figshare","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"University of British Columbia","funders":"","keywords":"Subclass; COPD; Antibody; Pulmonary disease; Population; Primary care","score_opus":0.009389252365392342,"score_gpt":0.20373574549318196,"score_spread":0.19434649312778962,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6920794981","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.47032288,0.0000014518956,1.9859574e-8,0.0000022083384,0.0000026158514,0.000115439834,0.5274982,0.0000013046999,0.0020559027],"genre_scores_gemma":[0.9301018,1.1814798e-7,0.000013134238,0.000015900065,0.0000018315843,0.00020746369,0.069589496,0.000005032965,0.00006518977],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99911726,0.00007942046,0.00014841523,0.00011576597,0.00043577867,0.00010336375],"domain_scores_gemma":[0.9991612,0.0002699523,0.0002954868,0.00024332578,0.000012853864,0.000017201775],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0000370702,0.00007199847,0.00010255798,9.768802e-7,0.00008047231,0.000002077866,0.0002988653,0.000016687976,0.98744726],"category_scores_gemma":[0.0003792681,0.000036422596,0.00009208303,0.00029606328,0.00005388096,0.000030824525,0.00021002175,0.00010632406,0.000042386528],"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":[0.000014786601,0.00017761876,0.23070922,0.0000037555012,0.0000065199883,1.8004086e-7,0.000076769335,0.0031732651,0.0000017659875,0.0000012411525,0.7657811,0.000053783053],"study_design_scores_gemma":[0.00015151247,0.0002294032,0.99698114,0.00007619434,0.0000030221413,1.0569461e-7,0.00005859222,0.00025170896,0.000018754838,0.000027908427,0.0021544723,0.00004719399],"about_ca_topic_score_codex":0.00036384823,"about_ca_topic_score_gemma":0.000037544203,"teacher_disagreement_score":0.9874049,"about_ca_system_score_codex":0.00008641871,"about_ca_system_score_gemma":0.000035633475,"threshold_uncertainty_score":0.14852704},"labels":[],"label_agreement":null},{"id":"W6921935901","doi":"10.1051/epjconf/201611920003/pdf","title":"Lidar Measurements of Tropospheric Ozone in the Arctic","year":2016,"lang":"en","type":"article","venue":"Springer Link (Chiba Institute of Technology)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Troposphere; Ozone; Arctic; Tropospheric ozone; Lidar; The arctic; Ozone layer","score_opus":0.015613116349404738,"score_gpt":0.2234417648709956,"score_spread":0.20782864852159086,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6921935901","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":[0.9888546,0.00013005605,0.0015975046,0.002561943,0.0002032865,0.00024737857,0.0000012920025,0.00004933395,0.006354646],"genre_scores_gemma":[0.9869309,0.000055627,0.012744101,0.00006760008,0.00002456624,0.000024885243,2.3180691e-7,0.00001190058,0.00014019625],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986706,0.000019829422,0.00039002617,0.00028122746,0.00035283,0.00028549586],"domain_scores_gemma":[0.99913055,0.0000137498255,0.00020241881,0.0006072043,0.000016376196,0.000029687038],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003111823,0.0001571049,0.0002460006,0.000009338931,0.000053299605,0.000004148493,0.00079487206,0.00016419718,0.0002626364],"category_scores_gemma":[0.00013127696,0.0000914547,0.00007547563,0.00067809364,0.000985873,0.00014920077,0.00026536622,0.0001722712,0.00009796493],"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":[0.000023405566,0.00021430805,0.8180866,0.000023935529,0.000027801376,0.0000074060977,0.00011329175,0.00009758549,0.104462795,0.0019437918,0.00005874395,0.07494033],"study_design_scores_gemma":[0.0024197665,0.0006354468,0.8581457,0.00043003925,0.00007417966,0.000021904143,0.00021350292,0.000039484414,0.09543102,0.0064010452,0.035605572,0.0005823132],"about_ca_topic_score_codex":0.00027941258,"about_ca_topic_score_gemma":0.00018704579,"teacher_disagreement_score":0.074358016,"about_ca_system_score_codex":0.00011354006,"about_ca_system_score_gemma":0.000021674336,"threshold_uncertainty_score":0.37294143},"labels":[],"label_agreement":null},{"id":"W6924332496","doi":"10.15468/dl.53fmmj","title":"Occurrence Download","year":2024,"lang":"en","type":"dataset","venue":"Global Biodiversity Information Facility","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Geodetic datum; Coordinate system; Matching (statistics); Download; Range (aeronautics); Geographic coordinate conversion","score_opus":0.008200382899391599,"score_gpt":0.20104710746212964,"score_spread":0.19284672456273805,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6924332496","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0013232502,0.000017629365,0.0000043432506,0.00013391857,0.00063417334,0.0002104354,0.9965217,0.00009629557,0.0010582603],"genre_scores_gemma":[0.00003986932,0.000049771268,0.0000031928032,0.00055891613,0.000001445525,0.0000035141961,0.9993425,1.4374727e-8,7.754723e-7],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9985771,0.000027707852,0.0002945626,0.00027300697,0.00053784257,0.00028973835],"domain_scores_gemma":[0.99924815,0.000007689439,0.00014475203,0.00041741293,0.00001913003,0.00016284644],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00016161444,0.0002695391,0.00020066735,0.0000024801411,0.00020452926,0.00014491675,0.0005184239,0.00029310372,0.027533565],"category_scores_gemma":[0.0000351964,0.0002494066,0.0001426397,0.0003426198,0.0002821902,0.00065771805,0.00082859775,0.0002915192,0.9082427],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013175541,0.000019482175,0.0031248091,0.00006222441,0.000013716491,0.0000037531518,0.000035029396,0.000035148838,3.956241e-8,2.6322192e-8,0.99490875,0.0017838619],"study_design_scores_gemma":[0.00010234691,0.000027080318,0.0002514926,0.0000019646511,0.000049152706,0.000004388254,0.0000862244,5.8743194e-7,7.788651e-7,0.0000020259665,0.99920595,0.00026800224],"about_ca_topic_score_codex":0.001026917,"about_ca_topic_score_gemma":0.000038209473,"teacher_disagreement_score":0.8807092,"about_ca_system_score_codex":0.00054203585,"about_ca_system_score_gemma":0.000038814345,"threshold_uncertainty_score":0.9999958},"labels":[],"label_agreement":null},{"id":"W6925443213","doi":"10.17611/dp/15396426","title":"Magnetotelluric Transfer Functions","year":2017,"lang":"en","type":"other","venue":"NSF Seismological Facility for the Advancement of Geoscience (SAGE)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Magnetotellurics; Transfer function; Field (mathematics); Transfer (computing); Interpretation (philosophy)","score_opus":0.01989083542928368,"score_gpt":0.2500710547942921,"score_spread":0.2301802193650084,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6925443213","genre_codex":"methods","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0012111888,0.0006757017,0.9891168,0.0009210794,0.00065850996,0.0012226561,0.0006368995,0.000085409425,0.0054717534],"genre_scores_gemma":[0.00849356,0.0011173974,0.001991037,0.0005065378,0.00006368126,0.00019053998,0.00003104645,0.00003958084,0.9875666],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.997551,0.000051307547,0.0003387074,0.0008099936,0.00064432074,0.00060463446],"domain_scores_gemma":[0.9984879,0.00013063582,0.00020543185,0.0010279887,0.000011371595,0.00013666337],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004905067,0.00038634005,0.00044826017,0.000004828988,0.00058254285,0.00003715577,0.0012243198,0.00025334404,0.015410188],"category_scores_gemma":[0.00009392262,0.0002399188,0.00029447203,0.00018094058,0.0020940078,0.0001254787,0.00031573029,0.00022736363,0.000310909],"study_design_candidate":"design_other","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":[0.000037284157,0.00017180352,0.00084487506,0.000032727123,0.000018957773,0.0000022466088,0.000030233552,0.00044558806,0.00021410288,0.00006907512,0.00037141156,0.99776167],"study_design_scores_gemma":[0.00032000314,0.00038231263,0.003271952,0.000034704535,0.00006595003,0.0000022877311,0.00004807429,0.00030089339,0.000047933896,0.00018445673,0.99503976,0.0003016964],"about_ca_topic_score_codex":0.0011223339,"about_ca_topic_score_gemma":0.00013623056,"teacher_disagreement_score":0.99746,"about_ca_system_score_codex":0.00010331984,"about_ca_system_score_gemma":0.00002727395,"threshold_uncertainty_score":0.98548985},"labels":[],"label_agreement":null},{"id":"W6930110830","doi":"10.5281/zenodo.12292785","title":"how to write a journal article in 12 weeks pdf","year":2024,"lang":"en","type":"other","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Publishing; Reading (process); Workbook; Academic writing; Citation; Feeling; Plan (archaeology); Journal writing; Writing style","score_opus":0.015881914716631564,"score_gpt":0.2182450325740912,"score_spread":0.20236311785745964,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6930110830","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0011941852,0.000116176525,0.0017350295,0.0018609748,0.00014082411,0.00028680507,0.000030566538,0.00027705551,0.99435836],"genre_scores_gemma":[0.01820104,0.00010093472,0.00071090856,0.00025365446,0.00029811615,4.3878458e-8,0.000045252127,0.004119274,0.9762708],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9985805,0.00012497714,0.00015772642,0.0003792131,0.00039144373,0.00036609516],"domain_scores_gemma":[0.9993827,0.000003880124,0.000069723,0.00028685533,0.000017216491,0.00023966693],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0003465997,0.00015522668,0.00014331806,0.000023130913,0.000328444,0.0010006912,0.0007159541,0.000102301514,0.29431733],"category_scores_gemma":[0.00012609464,0.00014821852,0.000047518617,0.000472202,0.000110786015,0.000102178674,0.0012158592,0.00041626958,0.20805727],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000095982405,0.000044502,0.000011799408,0.000017778408,0.000012786589,0.00005785414,0.00041408173,0.000025797564,0.0006754351,0.000104418614,0.9621531,0.036472876],"study_design_scores_gemma":[0.00016776052,0.00011707799,0.0003170219,0.000074927426,0.0000080348245,0.000081353086,0.00023118807,0.000077173216,0.000019092815,0.00010232552,0.99863166,0.00017239833],"about_ca_topic_score_codex":0.000056195855,"about_ca_topic_score_gemma":0.000009976337,"teacher_disagreement_score":0.08626008,"about_ca_system_score_codex":0.0002486176,"about_ca_system_score_gemma":0.0000014940762,"threshold_uncertainty_score":0.9649688},"labels":[],"label_agreement":null},{"id":"W6936199654","doi":"10.57757/iugg23-1116","title":"Secondary ice processes: Results from seven airborne field campaigns","year":2023,"lang":"en","type":"article","venue":"Publication Database GFZ (GFZ German Research Centre for Geosciences)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"","keywords":"Supercooling; Graupel; Aerosol; Particle-size distribution; Ice cloud; Drop (telecommunication); Sea ice; Ice shelf","score_opus":0.03674360940739628,"score_gpt":0.32451575310018255,"score_spread":0.28777214369278625,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6936199654","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":[0.8776844,0.00011519125,0.0053043873,0.06527048,0.00078082253,0.0037371486,0.023072269,0.0008580806,0.023177205],"genre_scores_gemma":[0.9222118,0.0003306753,0.008054344,0.002621754,0.0006722699,0.00083066436,0.022905253,0.00008331104,0.04228992],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9949901,0.00018803503,0.00052824634,0.001305545,0.0016837391,0.0013043203],"domain_scores_gemma":[0.99633205,0.0014737934,0.00019868431,0.0011600574,0.00028998972,0.0005454318],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0034148695,0.00022990687,0.00020369346,0.00003958948,0.0010488483,0.00038775796,0.0016840773,0.000119535034,0.004895397],"category_scores_gemma":[0.004876533,0.00020421724,0.0000728703,0.0039005491,0.0005247495,0.0015740109,0.0011257795,0.00042194515,0.0023365042],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000119849174,0.000205785,0.004573212,0.00005806189,0.0000128404745,0.000008461902,0.0023772446,0.00005483616,0.0007958097,0.00032241468,0.9670326,0.024438884],"study_design_scores_gemma":[0.0010164906,0.00012944434,0.028944198,0.000044259,0.000011216693,0.0000025814752,0.0025626766,0.011798791,0.0021371,0.0014270233,0.951498,0.0004282513],"about_ca_topic_score_codex":0.0049700565,"about_ca_topic_score_gemma":0.002965016,"teacher_disagreement_score":0.06264873,"about_ca_system_score_codex":0.00020870478,"about_ca_system_score_gemma":0.00042408676,"threshold_uncertainty_score":0.99844027},"labels":[],"label_agreement":null},{"id":"W6939187104","doi":"10.60692/x7r14-z5w65","title":"Satellite-Surface Perspectives of Air Quality and Aerosol-Cloud Effects on the Environment: An Overview of 7-SEAS/BASELInE","year":2016,"lang":"en","type":"article","venue":"Greater South Information System","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"National Research Council Canada","funders":"","keywords":"Air quality index; Aerosol; Trace gas; Radar; Cloud computing; Satellite; Atmospheric model; Air pollution","score_opus":0.03911177837106077,"score_gpt":0.24124932913417882,"score_spread":0.20213755076311804,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6939187104","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":[0.9957056,0.000051165156,0.0026011176,0.00015129575,0.00004680936,0.00033106704,0.00004794962,0.00002564591,0.0010393654],"genre_scores_gemma":[0.9995466,0.000014126927,0.00021733428,0.000105158026,0.000016920285,0.000011699609,0.0000014517972,0.0000068707436,0.00007983411],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99861073,0.0002345935,0.00046716793,0.00016389007,0.0003694516,0.00015418087],"domain_scores_gemma":[0.9990441,0.00006483858,0.0003749181,0.00042678954,0.000014424139,0.00007490709],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007146273,0.00015440892,0.00023510223,0.0000025855718,0.00008196599,0.00001291427,0.00016152428,0.0000620553,0.00019280253],"category_scores_gemma":[0.000027638367,0.00007913699,0.000059075635,0.00008469298,0.0001925273,0.0003413496,0.00009242108,0.00004294431,0.00022390994],"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":[0.00020405602,0.00003575595,0.83423024,0.0007885447,0.00007125206,8.788898e-7,0.14915101,0.00072357943,0.002265666,0.002740072,0.00004913794,0.009739798],"study_design_scores_gemma":[0.0012856947,0.00039149704,0.93649375,0.00041921722,0.00004130084,0.000004396038,0.030022385,0.0005590966,0.030119728,0.000015626703,0.00029275825,0.0003545219],"about_ca_topic_score_codex":0.000034205477,"about_ca_topic_score_gemma":3.4657128e-7,"teacher_disagreement_score":0.11912862,"about_ca_system_score_codex":0.00009383535,"about_ca_system_score_gemma":0.0000049826767,"threshold_uncertainty_score":0.3227113},"labels":[],"label_agreement":null},{"id":"W6939258352","doi":"10.60692/09xxt-z1v11","title":"A global analysis of climate-relevant aerosol properties retrieved from the network of Global Atmosphere Watch (GAW) near-surface observatories","year":2020,"lang":"en","type":"article","venue":"Greater South Information System","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"","keywords":"Aerosol; Earth's energy budget; Atmosphere (unit); Absorption (acoustics); Air quality index; Particle (ecology); Atmospheric optics","score_opus":0.02257646480333594,"score_gpt":0.1906692729157737,"score_spread":0.16809280811243776,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6939258352","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":[0.99422765,0.00003844371,0.0035419692,0.0002538971,0.00013684265,0.00033944275,0.00048546688,0.00007773824,0.0008985271],"genre_scores_gemma":[0.9981922,0.000001973474,0.0015171987,0.00021169153,0.00003140301,0.00000981891,0.000020995436,0.0000061955393,0.0000085439115],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978554,0.00008824696,0.0009189825,0.00020954727,0.00061006064,0.0003177485],"domain_scores_gemma":[0.99872655,0.000010203739,0.00065136224,0.0004285057,0.000069919966,0.00011343655],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022187967,0.00022617972,0.00050939387,1.0461657e-8,0.00019146562,0.000101792364,0.00044513485,0.00012209857,0.0001977065],"category_scores_gemma":[0.000018942112,0.00014035788,0.00020029346,0.0015657408,0.00020693157,0.00041992852,0.00032023148,0.000066353045,0.00015370973],"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":[0.00015214061,0.0000025732331,0.91345173,0.00006495556,0.0003093693,6.116683e-7,0.013514357,0.0721335,0.0000028550235,0.000039907893,0.00023290925,0.000095102594],"study_design_scores_gemma":[0.00034410896,0.000060364826,0.93134815,0.00007662438,0.00042353777,7.8382703e-7,0.012608274,0.054776017,0.00007298523,9.320386e-7,0.00012629769,0.00016191986],"about_ca_topic_score_codex":0.00087464554,"about_ca_topic_score_gemma":0.00002143277,"teacher_disagreement_score":0.01789643,"about_ca_system_score_codex":0.00020130636,"about_ca_system_score_gemma":0.000038176717,"threshold_uncertainty_score":0.57236284},"labels":[],"label_agreement":null},{"id":"W6939499570","doi":"10.60692/zyn6v-0ff82","title":"South African dust contribution to the high southern latitudes and East Antarctica during interglacial stages","year":2022,"lang":"en","type":"article","venue":"Greater South Information System","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Université de Montréal","funders":"","keywords":"Southern Hemisphere; Mineral dust; Interglacial; Latitude; Northern Hemisphere; Quaternary; Middle latitudes; Natural (archaeology)","score_opus":0.009816856099518696,"score_gpt":0.1750252847263444,"score_spread":0.16520842862682572,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6939499570","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":[0.9948121,0.0000010615745,0.003575309,0.00027200987,0.00017725762,0.0003901797,0.00018853067,0.00008253339,0.000501039],"genre_scores_gemma":[0.9992985,3.5862136e-8,0.000077962715,0.00018111852,0.00005742503,0.00011291793,0.000009263537,0.000008275482,0.0002544918],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988041,0.00008014395,0.0003145507,0.00015841881,0.0003964407,0.0002463445],"domain_scores_gemma":[0.99949485,0.000004204317,0.00017393143,0.00021795066,0.000016052183,0.00009302292],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002992281,0.00013915704,0.0001404562,0.000007006992,0.00075508433,0.00013937932,0.00020476517,0.000031078413,0.0004745643],"category_scores_gemma":[0.000011992965,0.00009871154,0.000036468897,0.00017947676,0.000061444865,0.00024487686,0.00047908077,0.0001187907,0.0005407766],"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":[0.00010401693,0.000002341872,0.8115117,0.000021779393,0.000019122186,0.0000018057949,0.18503387,0.0030219036,0.000013860162,0.0000821212,0.000059483307,0.00012798069],"study_design_scores_gemma":[0.000900771,0.000122396,0.79152125,0.000023242688,0.000030850766,0.00004042639,0.2039962,0.0010517952,0.00008818108,0.0000016524912,0.001924437,0.00029880207],"about_ca_topic_score_codex":0.00018549139,"about_ca_topic_score_gemma":0.000013126647,"teacher_disagreement_score":0.019990461,"about_ca_system_score_codex":0.00028221376,"about_ca_system_score_gemma":0.0000075522994,"threshold_uncertainty_score":0.6950769},"labels":[],"label_agreement":null},{"id":"W6939556204","doi":"10.60692/ze7a6-ywt55","title":"A global analysis of climate-relevant aerosol properties retrieved from the network of Global Atmosphere Watch (GAW) near-surface observatories","year":2020,"lang":"en","type":"article","venue":"Greater South Information System","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"","keywords":"Aerosol; Earth's energy budget; Atmosphere (unit); Absorption (acoustics); Air quality index; Particle (ecology); Atmospheric optics","score_opus":0.02257646480333594,"score_gpt":0.1906692729157737,"score_spread":0.16809280811243776,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6939556204","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":[0.99422765,0.00003844371,0.0035419692,0.0002538971,0.00013684265,0.00033944275,0.00048546688,0.00007773824,0.0008985271],"genre_scores_gemma":[0.9981922,0.000001973474,0.0015171987,0.00021169153,0.00003140301,0.00000981891,0.000020995436,0.0000061955393,0.0000085439115],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978554,0.00008824696,0.0009189825,0.00020954727,0.00061006064,0.0003177485],"domain_scores_gemma":[0.99872655,0.000010203739,0.00065136224,0.0004285057,0.000069919966,0.00011343655],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022187967,0.00022617972,0.00050939387,1.0461657e-8,0.00019146562,0.000101792364,0.00044513485,0.00012209857,0.0001977065],"category_scores_gemma":[0.000018942112,0.00014035788,0.00020029346,0.0015657408,0.00020693157,0.00041992852,0.00032023148,0.000066353045,0.00015370973],"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":[0.00015214061,0.0000025732331,0.91345173,0.00006495556,0.0003093693,6.116683e-7,0.013514357,0.0721335,0.0000028550235,0.000039907893,0.00023290925,0.000095102594],"study_design_scores_gemma":[0.00034410896,0.000060364826,0.93134815,0.00007662438,0.00042353777,7.8382703e-7,0.012608274,0.054776017,0.00007298523,9.320386e-7,0.00012629769,0.00016191986],"about_ca_topic_score_codex":0.00087464554,"about_ca_topic_score_gemma":0.00002143277,"teacher_disagreement_score":0.01789643,"about_ca_system_score_codex":0.00020130636,"about_ca_system_score_gemma":0.000038176717,"threshold_uncertainty_score":0.57236284},"labels":[],"label_agreement":null},{"id":"W6939569795","doi":"10.60692/7m5p4-e5z14","title":"Airborne and ground-based measurements of aerosol optical depth of freshly emitted anthropogenic plumes in the Athabasca Oil Sands Region","year":2021,"lang":"en","type":"article","venue":"Greater South Information System","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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; National Research Council Canada; Université de Sherbrooke; Canadian Space Agency","funders":"","keywords":"AERONET; Plume; Aerosol; Oil sands; Context (archaeology); Panache; Dilution","score_opus":0.03256021595491577,"score_gpt":0.21463220703994457,"score_spread":0.1820719910850288,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6939569795","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":[0.9927621,0.000013046533,0.0033613634,0.000055305038,0.00005210131,0.000108820306,0.000007142321,0.000015187988,0.0036249624],"genre_scores_gemma":[0.9993012,6.549436e-7,0.0005432639,0.0000855666,0.000008743683,0.000017670967,0.000007644522,0.000005171684,0.000030107367],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986368,0.000089193265,0.0005191998,0.0001268438,0.00046712274,0.00016087451],"domain_scores_gemma":[0.99938524,0.000012346971,0.00024123584,0.00028149594,0.000037076563,0.000042623917],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032577908,0.0001205267,0.00020805055,0.000005742727,0.00006396045,0.000032918906,0.00014817991,0.00007760392,0.000048862374],"category_scores_gemma":[0.000020406005,0.00008413837,0.000057181627,0.00028588978,0.00015483938,0.00025713196,0.00006568055,0.00006559032,0.000026424927],"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":[0.00004682704,0.000012259684,0.9835482,0.00018324258,0.000015650674,0.0000040657574,0.014284691,0.0003321667,0.00010230603,0.000017162227,0.000041354728,0.001412021],"study_design_scores_gemma":[0.001439089,0.00008036864,0.97012126,0.0001789053,0.000032415974,0.000032090575,0.012293781,0.0028258718,0.01282764,5.354872e-7,0.000020776526,0.00014727545],"about_ca_topic_score_codex":0.00010110335,"about_ca_topic_score_gemma":0.000020799105,"teacher_disagreement_score":0.013427003,"about_ca_system_score_codex":0.00007635607,"about_ca_system_score_gemma":0.000023658664,"threshold_uncertainty_score":0.34310633},"labels":[],"label_agreement":null},{"id":"W6944999233","doi":"10.18739/a23r0pt92","title":"Cloud microphysical properties at Arctic atmospheric observatories: Eureka, Canada","year":2016,"lang":"en","type":"dataset","venue":"California Digital Library","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Cloud computing; Cloud top; Arctic; Liquid water content; Data set; The arctic; Atmospheric research; Cloud fraction","score_opus":0.005683342112682633,"score_gpt":0.1538684611538913,"score_spread":0.14818511904120868,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6944999233","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.035149377,0.00029662167,0.0000032520659,0.0005334347,0.0006756617,0.0003276433,0.9618963,0.000101438396,0.0010162714],"genre_scores_gemma":[0.010425755,0.00017775358,0.0000911202,0.0030566198,0.0011674085,0.00009146459,0.9649221,0.00017573162,0.019892091],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9969623,0.00004567218,0.0005369361,0.00089373614,0.0007359046,0.00082543737],"domain_scores_gemma":[0.9982037,0.00007685898,0.00026745538,0.0009307227,0.000009230777,0.0005120188],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000026271551,0.00072880735,0.00059445435,5.430197e-7,0.0002661015,0.00029634783,0.0011123988,0.00030269046,0.011871608],"category_scores_gemma":[0.00005602153,0.0004980423,0.00020433406,0.00029305986,0.00059194025,0.0007095471,0.0019928773,0.00036883992,0.009961138],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008483132,0.00007487383,0.009638238,0.00010288248,0.00004111817,0.00013518504,0.000004284895,0.000012331259,0.000020594174,0.0000010663472,0.989263,0.00062159216],"study_design_scores_gemma":[0.00019769445,0.000078423036,0.0003368626,0.00011988974,0.00003470699,0.00002296999,0.0000141103255,0.000010091357,0.00013731916,0.00008198274,0.998176,0.0007899831],"about_ca_topic_score_codex":0.022189844,"about_ca_topic_score_gemma":0.008537947,"teacher_disagreement_score":0.024723621,"about_ca_system_score_codex":0.00075002474,"about_ca_system_score_gemma":0.0004188562,"threshold_uncertainty_score":0.9997471},"labels":[],"label_agreement":null},{"id":"W6946204748","doi":"10.34657/10979","title":"Lidar Ice nuclei estimates and how they relate with airborne in-situ measurements","year":2018,"lang":"en","type":"book-chapter","venue":"TIB Repositorium","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Lidar; Aerosol; Ice nucleus; Particle (ecology); Photometer; Effective radius; Particle number","score_opus":0.012416398219772012,"score_gpt":0.19903468465649218,"score_spread":0.18661828643672018,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6946204748","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.09491791,0.00038376913,0.000061046056,0.00026687025,0.00061971426,0.00042753876,0.0000030439742,0.000101359714,0.90321875],"genre_scores_gemma":[0.6078944,0.00007996736,0.003074451,0.000082047285,0.00043503032,0.000012952593,0.0000073565407,0.000117819574,0.38829595],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99810004,0.000016933353,0.00022527893,0.0006762681,0.00063794473,0.0003435599],"domain_scores_gemma":[0.9990224,0.000023878998,0.00026031295,0.00050298497,0.000025570456,0.00016482685],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00019177493,0.00042545516,0.00037495763,0.0000036940726,0.0001597029,0.00010723422,0.00026303358,0.00032348637,0.0003997026],"category_scores_gemma":[0.000012003023,0.00033369675,0.0000524798,0.00003841217,0.0003220598,0.00017333789,0.00025938853,0.0003297993,0.00029002206],"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":[0.002441007,0.0010762726,0.65596646,0.0010060115,0.0024802117,0.004817248,0.018667702,0.00050481164,0.16676262,0.0062368955,0.1014277,0.038613066],"study_design_scores_gemma":[0.004943871,0.004283801,0.27536443,0.003271704,0.0014365013,0.0010033426,0.00033577593,0.00031464198,0.016391873,0.009026744,0.6768405,0.0067868526],"about_ca_topic_score_codex":0.00021354297,"about_ca_topic_score_gemma":0.00031169952,"teacher_disagreement_score":0.57541275,"about_ca_system_score_codex":0.00025893192,"about_ca_system_score_gemma":0.000021887796,"threshold_uncertainty_score":0.9999115},"labels":[],"label_agreement":null},{"id":"W6946207456","doi":"10.34657/5272","title":"The unprecedented 2017–2018 stratospheric smoke event: decay phase and aerosol properties observed with the EARLINET","year":2019,"lang":"en","type":"article","venue":"TIB Repositorium","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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; Stratosphere; Troposphere; Smoke; Lidar; Northern Hemisphere; Anticyclone; Southern Hemisphere; Extinction (optical mineralogy)","score_opus":0.015647026619750024,"score_gpt":0.2206802433528082,"score_spread":0.2050332167330582,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6946207456","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":[0.9934413,0.0005517474,0.000088010514,0.0007877468,0.00046741514,0.0005604913,0.0000018583003,0.00005328854,0.004048138],"genre_scores_gemma":[0.98268,0.00005505313,0.00010717592,0.00011918128,0.00015286055,0.000044279375,0.0000021565168,0.000025400295,0.016813857],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985189,0.000082647464,0.00022427068,0.00036498968,0.00044253815,0.00036669263],"domain_scores_gemma":[0.99907696,0.00005024647,0.00015247427,0.00059039786,0.000019364412,0.00011057616],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021631428,0.00021692444,0.0001605534,4.3444317e-7,0.00054815895,0.00019884511,0.00040658156,0.00007028049,0.000183821],"category_scores_gemma":[0.000007254471,0.00009896306,0.000047212077,0.00017262532,0.0003713018,0.00018015808,0.0001887135,0.00018456843,0.00012352664],"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":[0.0016055661,0.00083545974,0.5059575,0.00008346622,0.00038017766,0.00007810692,0.005015755,0.003122258,0.43713793,0.00022452272,0.035083167,0.010476119],"study_design_scores_gemma":[0.0107951155,0.006232011,0.4716403,0.00031041016,0.0004868961,0.00063461467,0.009996505,0.01891531,0.19285546,0.000052077772,0.28519213,0.0028891475],"about_ca_topic_score_codex":0.0007170416,"about_ca_topic_score_gemma":0.0002627066,"teacher_disagreement_score":0.250109,"about_ca_system_score_codex":0.00006828446,"about_ca_system_score_gemma":0.000025190218,"threshold_uncertainty_score":0.4216051},"labels":[],"label_agreement":null},{"id":"W6946357740","doi":"10.34657/7274","title":"Tropospheric and stratospheric wildfire smoke profiling with lidar: mass, surface area, CCN, and INP retrieval","year":2021,"lang":"en","type":"article","venue":"TIB Repositorium","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Smoke; AERONET; Lidar; Troposphere; Cloud condensation nuclei; Stratosphere; Aerosol; Plume","score_opus":0.006176457024742167,"score_gpt":0.19444540728836357,"score_spread":0.1882689502636214,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6946357740","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":[0.9911355,0.0013539662,0.000709173,0.00018678202,0.00025925552,0.00018798301,0.0000020474001,0.00007869702,0.0060866266],"genre_scores_gemma":[0.98040855,0.00014726528,0.015460034,0.00008429463,0.00012149759,0.0000037671457,0.000005627123,0.000036150497,0.0037328098],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982376,0.00006052832,0.00025341474,0.000635628,0.00043151728,0.00038131754],"domain_scores_gemma":[0.99923116,0.000035142108,0.0001238385,0.0003581119,0.000020435644,0.0002312918],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012736923,0.00026346865,0.00027149767,4.9742965e-7,0.000281413,0.00016593971,0.00011969398,0.00013296603,0.00025100494],"category_scores_gemma":[0.000021151089,0.0002189544,0.00003450303,0.00040206453,0.00027379463,0.00022842006,0.00016594032,0.00023187252,0.0000123495765],"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":[0.0001073687,0.000071040624,0.86895007,0.000027871098,0.00003943274,0.00032966165,0.00027333954,0.00035750706,0.12884474,0.000030049452,0.00031479963,0.0006541023],"study_design_scores_gemma":[0.0029219761,0.0016178554,0.7326754,0.00018193011,0.0003206803,0.0015399642,0.0038423573,0.0073109907,0.23558265,0.00030606095,0.011604248,0.0020959296],"about_ca_topic_score_codex":0.00026849308,"about_ca_topic_score_gemma":0.000021887197,"teacher_disagreement_score":0.13627474,"about_ca_system_score_codex":0.00010836499,"about_ca_system_score_gemma":0.000060434835,"threshold_uncertainty_score":0.8928702},"labels":[],"label_agreement":null},{"id":"W6948663990","doi":"10.5281/zenodo.10728246","title":"Aerosols and clouds affecting the radiation budget at Pituffik (Thule), northern Greenland: Insights on the installed and newly developed ground-based instruments at the Thule High Arctic Atmospheric Observatory (THAAO)","year":2023,"lang":"en","type":"dissertation","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Arctic; Observatory; Earth's energy budget; Satellite; Zenith; The arctic; Climate model; Radiative transfer","score_opus":0.018118789980266396,"score_gpt":0.2145572921262532,"score_spread":0.19643850214598682,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6948663990","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":[0.9924166,0.00012798836,0.000032199663,0.0008054262,0.00025100028,0.0012364911,0.00003527129,0.00023494811,0.004860052],"genre_scores_gemma":[0.98999906,0.00027315694,0.000055008222,0.0005324136,0.00010090461,0.0000021659546,0.0014220967,0.0009326529,0.0066825347],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9968623,0.00071183295,0.00038917497,0.0007366702,0.00082436565,0.0004756876],"domain_scores_gemma":[0.99840456,0.00026532772,0.00041007364,0.0006707271,0.00009311967,0.0001562143],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0008190077,0.00040972832,0.0002683838,0.0000063828224,0.0063474206,0.00063845236,0.00097257557,0.0001814449,0.004379348],"category_scores_gemma":[0.00041777562,0.00025120616,0.000075074866,0.0006403307,0.00042653363,0.0001789097,0.0012429558,0.0005499,0.002914226],"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":[0.0048775566,0.0014556582,0.07235506,0.0013087658,0.0016807284,0.00016561292,0.115327045,0.009767086,0.015060912,0.002294256,0.14646858,0.6292387],"study_design_scores_gemma":[0.0021634237,0.0007547307,0.77357376,0.00019025055,0.00014828528,0.000050436378,0.0047111413,0.0030420057,0.00034668844,0.000370918,0.21371078,0.00093757286],"about_ca_topic_score_codex":0.0005969541,"about_ca_topic_score_gemma":0.00087317824,"teacher_disagreement_score":0.7012187,"about_ca_system_score_codex":0.0008113641,"about_ca_system_score_gemma":0.000013514098,"threshold_uncertainty_score":0.99999404},"labels":[],"label_agreement":null},{"id":"W6949610420","doi":"10.5281/zenodo.15448614","title":"Sensitivity Study of Aerosol Direct Radiative Effects on Cloudy EarthCARE Scenes Using 1D and 3D Radiative Transfer Simulations","year":2025,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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","funders":"European Commission","keywords":"Radiative transfer; Aerosol; Shortwave; Atmospheric radiative transfer codes; Radiometer; Satellite; Radiative flux; Radiative forcing; Shortwave radiation","score_opus":0.01900390816157827,"score_gpt":0.24950600065227171,"score_spread":0.23050209249069345,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6949610420","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":[0.98582053,0.000024135637,0.002611481,0.000065224405,0.00004798815,0.0007362946,0.00004965439,0.00011021829,0.010534446],"genre_scores_gemma":[0.9994038,0.00001135735,0.00012076042,0.000061454324,0.000024816434,5.5539044e-8,0.000032050633,0.00019625277,0.00014948825],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.998313,0.00065771106,0.0001753473,0.00037774834,0.00026526998,0.00021093685],"domain_scores_gemma":[0.99943113,0.00012516153,0.000048593552,0.00024152194,0.00006796005,0.00008562185],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00029534462,0.00014099246,0.00019273798,0.000015212331,0.0012278334,0.0001082469,0.00017656061,0.000045902045,0.0011808841],"category_scores_gemma":[0.00022587097,0.00013784441,0.00003123611,0.0005472173,0.00018730029,0.00014158293,0.00037234338,0.00014997864,0.00013201947],"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":[0.0012228715,0.0044100145,0.034003027,0.00034811764,0.0008171245,0.00011599866,0.06944543,0.31735423,0.14568625,0.00096029293,0.007642732,0.4179939],"study_design_scores_gemma":[0.011009029,0.0070014694,0.66862524,0.00049053616,0.0004986691,0.000037645423,0.012277118,0.20046742,0.048274998,0.00017273253,0.049321953,0.0018232],"about_ca_topic_score_codex":0.00019146012,"about_ca_topic_score_gemma":0.000011724696,"teacher_disagreement_score":0.6346222,"about_ca_system_score_codex":0.0001313037,"about_ca_system_score_gemma":0.0000024242904,"threshold_uncertainty_score":0.9997322},"labels":[],"label_agreement":null},{"id":"W6949749698","doi":"10.5281/zenodo.3793250","title":"Gyrinus aquiris LeConte 1868","year":2008,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Nova Scotia Hospital","funders":"","keywords":"Commoner; Taxonomy (biology); Fauna; Mantis","score_opus":0.028731744963973245,"score_gpt":0.21250716349671017,"score_spread":0.18377541853273693,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6949749698","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.49591395,0.00003954429,0.003819264,0.00045445797,0.00007557585,0.00022299324,0.00002307918,0.00055220607,0.49889892],"genre_scores_gemma":[0.98811936,0.00007731653,0.000590096,0.00029576925,0.00008194283,2.5671257e-8,0.00010515481,0.0006704292,0.010059925],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9987124,0.00010558991,0.00017000479,0.00034327584,0.00032963156,0.00033908593],"domain_scores_gemma":[0.99936116,0.000008994658,0.00006266237,0.00034934978,0.000041279472,0.00017658136],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0002219547,0.00011510134,0.00010483696,0.0000050928943,0.0021445544,0.0001377624,0.00070726546,0.00004685336,0.15586856],"category_scores_gemma":[0.00012641847,0.00011499861,0.000048170645,0.0003450315,0.0003654478,0.00021821854,0.0010583834,0.00016290783,0.07300187],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004448862,0.00017055152,0.00056506007,0.000009393328,0.000022413607,0.00007479308,0.0018543748,0.0003909924,0.0065058186,0.00033604007,0.87230587,0.11772018],"study_design_scores_gemma":[0.00027685272,0.0001339044,0.014362076,0.000003857763,0.0000041782087,0.00020150242,0.00011012826,0.00037168304,0.00032059007,0.000062345534,0.98399997,0.00015288714],"about_ca_topic_score_codex":0.000075743934,"about_ca_topic_score_gemma":7.3228915e-7,"teacher_disagreement_score":0.49220538,"about_ca_system_score_codex":0.0001696088,"about_ca_system_score_gemma":0.0000013007267,"threshold_uncertainty_score":0.9991545},"labels":[],"label_agreement":null},{"id":"W6949850089","doi":"10.5281/zenodo.15448615","title":"Sensitivity Study of Aerosol Direct Radiative Effects on Cloudy EarthCARE Scenes Using 1D and 3D Radiative Transfer Simulations","year":2025,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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","funders":"European Commission","keywords":"Radiative transfer; Aerosol; Shortwave; Atmospheric radiative transfer codes; Radiometer; Satellite; Radiative flux; Radiative forcing; Shortwave radiation","score_opus":0.01900390816157827,"score_gpt":0.24950600065227171,"score_spread":0.23050209249069345,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6949850089","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":[0.98582053,0.000024135637,0.002611481,0.000065224405,0.00004798815,0.0007362946,0.00004965439,0.00011021829,0.010534446],"genre_scores_gemma":[0.9994038,0.00001135735,0.00012076042,0.000061454324,0.000024816434,5.5539044e-8,0.000032050633,0.00019625277,0.00014948825],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.998313,0.00065771106,0.0001753473,0.00037774834,0.00026526998,0.00021093685],"domain_scores_gemma":[0.99943113,0.00012516153,0.000048593552,0.00024152194,0.00006796005,0.00008562185],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00029534462,0.00014099246,0.00019273798,0.000015212331,0.0012278334,0.0001082469,0.00017656061,0.000045902045,0.0011808841],"category_scores_gemma":[0.00022587097,0.00013784441,0.00003123611,0.0005472173,0.00018730029,0.00014158293,0.00037234338,0.00014997864,0.00013201947],"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":[0.0012228715,0.0044100145,0.034003027,0.00034811764,0.0008171245,0.00011599866,0.06944543,0.31735423,0.14568625,0.00096029293,0.007642732,0.4179939],"study_design_scores_gemma":[0.011009029,0.0070014694,0.66862524,0.00049053616,0.0004986691,0.000037645423,0.012277118,0.20046742,0.048274998,0.00017273253,0.049321953,0.0018232],"about_ca_topic_score_codex":0.00019146012,"about_ca_topic_score_gemma":0.000011724696,"teacher_disagreement_score":0.6346222,"about_ca_system_score_codex":0.0001313037,"about_ca_system_score_gemma":0.0000024242904,"threshold_uncertainty_score":0.9997322},"labels":[],"label_agreement":null},{"id":"W6949950870","doi":"10.5281/zenodo.3792988","title":"Philonthus varians","year":2008,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"St. Francis Xavier University; Nova Scotia Hospital","funders":"","keywords":"Intertidal zone; Generalist and specialist species; Habitat; Cosmopolitan distribution; Algae","score_opus":0.026796265835905973,"score_gpt":0.2085285867575515,"score_spread":0.18173232092164554,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6949950870","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.21039763,0.000025644847,0.009536145,0.00072547176,0.00008191476,0.00023911872,0.000029455307,0.00067330967,0.7782913],"genre_scores_gemma":[0.9940996,0.000050589075,0.00079117075,0.00027273656,0.00008204482,1.659921e-8,0.000114889765,0.0005985674,0.003990345],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9988743,0.00009848397,0.00013599814,0.0002967324,0.00030657282,0.00028787946],"domain_scores_gemma":[0.99944735,0.000007299831,0.000047811045,0.00031159385,0.000034274435,0.00015165852],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00020187972,0.000096646065,0.000085064734,0.0000039509036,0.0022665532,0.00011303854,0.0006366504,0.000042220385,0.10434522],"category_scores_gemma":[0.00010417528,0.00009586722,0.00003696998,0.00033103404,0.00028364867,0.00017278436,0.0008428784,0.00014199309,0.036719147],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005597984,0.0003103934,0.0003738359,0.000010678417,0.000029046583,0.000101452584,0.0034076807,0.000658466,0.008093385,0.0023682588,0.87936753,0.105223306],"study_design_scores_gemma":[0.000242564,0.00011712262,0.011457394,0.0000029243383,0.0000042970605,0.00020627205,0.00008841959,0.00033428424,0.0001393664,0.00012583341,0.9871485,0.00013297175],"about_ca_topic_score_codex":0.00005402418,"about_ca_topic_score_gemma":3.7389927e-7,"teacher_disagreement_score":0.783702,"about_ca_system_score_codex":0.00012708604,"about_ca_system_score_gemma":9.354648e-7,"threshold_uncertainty_score":0.9990324},"labels":[],"label_agreement":null},{"id":"W6950011410","doi":"10.5281/zenodo.6631431","title":"JamesPHoughton/pysd: 3.2.0","year":2022,"lang":"en","type":"other","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"","keywords":"Function (biology); Value (mathematics); Selection (genetic algorithm); Identification (biology); Component (thermodynamics)","score_opus":0.014923393370175965,"score_gpt":0.2125833180282525,"score_spread":0.19765992465807655,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6950011410","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0002028084,0.00014237927,0.00049931393,0.00022521232,0.00014292964,0.0003612111,0.00018824733,0.0012527792,0.99698514],"genre_scores_gemma":[0.0035045897,0.00025872004,0.0006907075,0.00046540485,0.00026321088,1.1168697e-7,0.0018937386,0.013534697,0.97938883],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9980729,0.00021478902,0.00017781604,0.0005702986,0.00056965684,0.00039454122],"domain_scores_gemma":[0.99902695,0.0000073543997,0.00015384995,0.0006233278,0.000015908076,0.00017260648],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0002865783,0.00021636926,0.00018432572,0.000012823138,0.0013953155,0.00025328776,0.0013962793,0.000114200324,0.9019539],"category_scores_gemma":[0.000089651854,0.00022670944,0.00007291826,0.0004980291,0.00025234438,0.000069287635,0.0032910143,0.00038438803,0.07107689],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008945054,0.00006659092,0.00000953246,0.000014028719,0.00002171883,0.000016409918,0.00018945282,0.00003329323,0.00009710263,0.0002724332,0.9521651,0.04710537],"study_design_scores_gemma":[0.0002131329,0.0001099208,0.00014122446,0.000010233565,0.000013657538,0.000041161475,0.0001672989,0.00004054618,0.000008683313,0.000042785763,0.9989499,0.00026148497],"about_ca_topic_score_codex":0.00018293207,"about_ca_topic_score_gemma":0.0000021261435,"teacher_disagreement_score":0.830877,"about_ca_system_score_codex":0.00033926626,"about_ca_system_score_gemma":0.0000015722958,"threshold_uncertainty_score":0.99990475},"labels":[],"label_agreement":null},{"id":"W6950095450","doi":"10.5281/zenodo.6002422","title":"Andrena (Euandrena) algida Smith 1853","year":2017,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Paraphernalia; Netting; Point (geometry); Kleptoparasitism","score_opus":0.02495269979489709,"score_gpt":0.23447040446569045,"score_spread":0.20951770467079336,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6950095450","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.36719677,0.00004525245,0.0025665606,0.000948814,0.00013058935,0.00029089794,0.00004493104,0.000444247,0.62833196],"genre_scores_gemma":[0.9929352,0.0000619492,0.00046458672,0.00012176229,0.00009460107,2.6111213e-8,0.000084480154,0.0005963293,0.005641068],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99868375,0.00008702897,0.0001455871,0.00038238495,0.00034670281,0.00035455023],"domain_scores_gemma":[0.9988687,0.0000068310273,0.0001272434,0.0007586041,0.000044310094,0.00019429911],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00034301294,0.00012563384,0.000114601964,0.0000041746734,0.0049253413,0.00095445197,0.0014315093,0.000044417357,0.054210525],"category_scores_gemma":[0.00023239262,0.00012018332,0.000046531182,0.00011708284,0.000399416,0.0003552653,0.002073198,0.00017228874,0.024402892],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006824602,0.00019491102,0.0012226152,0.00002344722,0.000036876507,0.000053531894,0.0011375509,0.00014030776,0.0057342835,0.0012996463,0.62573487,0.3643537],"study_design_scores_gemma":[0.00040277248,0.0001342346,0.039601732,0.000011877479,0.000008323818,0.000060578703,0.00011436092,0.00035170297,0.00043060354,0.00016818383,0.9585347,0.00018090522],"about_ca_topic_score_codex":0.00007996308,"about_ca_topic_score_gemma":0.0000015137852,"teacher_disagreement_score":0.62573844,"about_ca_system_score_codex":0.00011262957,"about_ca_system_score_gemma":0.0000013691574,"threshold_uncertainty_score":0.99637014},"labels":[],"label_agreement":null},{"id":"W6950095633","doi":"10.5281/zenodo.5697650","title":"Spilotus quadripustulatus Melsheimer","year":2006,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Nova scotia; Aceraceae; Fagaceae; Fraxinus; Saccharum","score_opus":0.01564001729721107,"score_gpt":0.20857742772763016,"score_spread":0.1929374104304191,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6950095633","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.28998327,0.00006930043,0.0038988392,0.00043958487,0.0000968769,0.0002698842,0.000026391619,0.0006677369,0.7045481],"genre_scores_gemma":[0.9931788,0.000014063036,0.0007610116,0.0001502472,0.00012444763,2.3121954e-8,0.0002257264,0.00069976225,0.0048459335],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99863154,0.00010277526,0.00018480745,0.00035333054,0.00035984773,0.0003677093],"domain_scores_gemma":[0.9994266,0.000007442939,0.000065706925,0.00033843637,0.000040995255,0.000120815566],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00026311103,0.00012290647,0.00010047485,0.0000053594654,0.0014453722,0.00027879648,0.000613608,0.000050799863,0.092674136],"category_scores_gemma":[0.00005724248,0.00012056658,0.000045634744,0.000391405,0.0002169541,0.0001862839,0.0008934252,0.00014980802,0.03453652],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000044036475,0.0002898699,0.000572009,0.000011423052,0.000021322146,0.00002684969,0.0003694378,0.0014319555,0.01724726,0.0048065092,0.8605185,0.11466083],"study_design_scores_gemma":[0.0002556708,0.000100466175,0.020930104,0.000003896183,0.000008791873,0.000038537066,0.0000739133,0.0003975621,0.0004148402,0.00038430915,0.97722805,0.00016385312],"about_ca_topic_score_codex":0.000280583,"about_ca_topic_score_gemma":0.0000017101962,"teacher_disagreement_score":0.7031955,"about_ca_system_score_codex":0.00014943167,"about_ca_system_score_gemma":7.388763e-7,"threshold_uncertainty_score":0.9998546},"labels":[],"label_agreement":null},{"id":"W6950215150","doi":"10.5281/zenodo.4052032","title":"Télécharger!! Miraculous New York : les héros unis streaming vF (2020) Film Complet Streaming VF","year":2020,"lang":"fr","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Headline; Scapegoat; Subject (documents); Paraphernalia; Limiting","score_opus":0.04062036175869553,"score_gpt":0.23094661509964,"score_spread":0.1903262533409445,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6950215150","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":[0.6035945,0.007398446,0.060559068,0.056873083,0.001446225,0.0031913677,0.0031689869,0.00371496,0.2600534],"genre_scores_gemma":[0.9717664,0.0006941521,0.0037311635,0.0011670163,0.0011281143,8.659771e-8,0.0012110245,0.0023014746,0.01800054],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9961596,0.0004791981,0.0005471,0.0010171485,0.000798947,0.0009980131],"domain_scores_gemma":[0.9980222,0.000056883913,0.00027245094,0.00057923526,0.00010617486,0.00096305506],"candidate_categories":["metaepi_narrow","sts","scholarly_communication","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00038298665,0.00043303712,0.0003783406,0.000011022999,0.0036469074,0.0010473349,0.0016617664,0.00019355147,0.2174092],"category_scores_gemma":[0.00044577825,0.00049015717,0.0001534264,0.001105304,0.00064399745,0.00042904267,0.0024240958,0.00067380513,0.03952036],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006780002,0.00020663904,0.00020442488,0.00011861011,0.00007807051,0.00010756749,0.00681474,0.0018166449,0.009628132,0.0011119278,0.5763542,0.40349123],"study_design_scores_gemma":[0.00069194,0.00051803485,0.0048228865,0.00009811408,0.00005870446,0.00008547156,0.003038404,0.008938986,0.00045867628,0.00006915327,0.9806926,0.0005269815],"about_ca_topic_score_codex":0.0014396444,"about_ca_topic_score_gemma":0.000010167982,"teacher_disagreement_score":0.40433842,"about_ca_system_score_codex":0.0004437608,"about_ca_system_score_gemma":0.000013500301,"threshold_uncertainty_score":0.9999897},"labels":[],"label_agreement":null},{"id":"W6950231160","doi":"10.5281/zenodo.7629565","title":"Fig. 100. Tegulae. A in Revision of the Nearctic species of the Lasioglossum (Dialictus) gemmatum species complex (Hymenoptera: Halictidae)","year":2023,"lang":"en","type":"other","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"University of Manitoba","funders":"","keywords":"Nearctic ecozone; Species complex; Scale (ratio); Projection (relational algebra)","score_opus":0.03242554804174507,"score_gpt":0.2293161587201902,"score_spread":0.19689061067844513,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6950231160","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.010560364,0.00007640373,0.00006765141,0.0009092084,0.0002497409,0.0009066228,0.0002392371,0.00029160772,0.98669916],"genre_scores_gemma":[0.33439156,0.00053829927,0.00021271946,0.00016444201,0.00021845562,1.1530776e-7,0.00011368279,0.004895439,0.65946525],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99784774,0.00035285385,0.00037330532,0.00037967585,0.00072877493,0.000317661],"domain_scores_gemma":[0.998655,0.00002498065,0.0003569891,0.0008543524,0.000044614462,0.00006403863],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00039409596,0.00021043187,0.00029186814,0.000019096486,0.0005461026,0.00011710292,0.001717842,0.00011681578,0.09359927],"category_scores_gemma":[0.0002965129,0.00014252553,0.00012534996,0.001032418,0.00096147886,0.000065933025,0.0030002727,0.00030303467,0.0027078015],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002060485,0.000109324144,0.0007332912,0.00011579325,0.000032188553,0.000003103325,0.0011048716,0.00013990996,0.0024362127,0.0012295537,0.9875586,0.0065165507],"study_design_scores_gemma":[0.00021060563,0.000057534533,0.050333362,0.00023216772,0.000014742736,0.000005843001,0.0002743857,0.00008342321,0.00014628461,0.000045870886,0.9484591,0.00013671762],"about_ca_topic_score_codex":0.0005522639,"about_ca_topic_score_gemma":0.00004749859,"teacher_disagreement_score":0.3272339,"about_ca_system_score_codex":0.00020365413,"about_ca_system_score_gemma":0.0000040818927,"threshold_uncertainty_score":0.9980687},"labels":[],"label_agreement":null},{"id":"W6950267971","doi":"10.5281/zenodo.5747538","title":"Pontarachna punctulum Phillippi 1840","year":2021,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Mediterranean climate; Mediterranean sea; Black sea; Harbour; Radiata","score_opus":0.01776665429322457,"score_gpt":0.21087248761940902,"score_spread":0.19310583332618445,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6950267971","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.28561312,0.00008830339,0.0054468517,0.0017198547,0.00015939795,0.00023881235,0.000052350733,0.0006612794,0.70602006],"genre_scores_gemma":[0.98784906,0.000056005785,0.0010811827,0.0006025579,0.00011594487,2.5994948e-8,0.0004429284,0.00077880255,0.009073498],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99854225,0.00015044904,0.00017113698,0.00041320876,0.00037871406,0.0003442144],"domain_scores_gemma":[0.99925226,0.000010057814,0.00005689967,0.00042677854,0.00007488326,0.00017912762],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00027465238,0.00012218874,0.00011205579,0.0000038522107,0.001491489,0.00034309542,0.00060457666,0.00005255914,0.1950705],"category_scores_gemma":[0.0002120534,0.00012171406,0.000055329125,0.00047211786,0.00017452448,0.00020240343,0.0015174423,0.0001892509,0.034160644],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005205684,0.00043376497,0.0004448146,0.000029175351,0.000053094383,0.00019017195,0.0019079486,0.0005814718,0.038899884,0.0032105285,0.6199929,0.3342042],"study_design_scores_gemma":[0.00024195782,0.00007156207,0.0064311386,0.000005941595,0.0000084261455,0.0001362995,0.00026593753,0.0003023843,0.00085438543,0.00021856208,0.9913053,0.00015811253],"about_ca_topic_score_codex":0.000050525454,"about_ca_topic_score_gemma":0.000002088808,"teacher_disagreement_score":0.70223594,"about_ca_system_score_codex":0.00021641028,"about_ca_system_score_gemma":0.0000020421064,"threshold_uncertainty_score":0.99980843},"labels":[],"label_agreement":null},{"id":"W6950294776","doi":"10.5281/zenodo.7003349","title":"FIGURES 3–5. Copelatus alternatus Sharp, 1882 in An outlook on larval morphology of Copelatinae diving beetles with phylogenetic considerations (Coleoptera: Adephaga, Dytiscidae)","year":2022,"lang":"en","type":"other","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Laurentian University","funders":"","keywords":"Larva; Instar; Seta; Dorsum; Morphology (biology); Phylogenetic tree","score_opus":0.018554622605097135,"score_gpt":0.22899178573263546,"score_spread":0.21043716312753832,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6950294776","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.17744197,0.0002545936,0.00011434829,0.0001265848,0.0000970316,0.00093252474,0.00051433995,0.0003086735,0.8202099],"genre_scores_gemma":[0.9505284,0.00011061937,0.0009830599,0.00022468525,0.00008369464,6.239375e-7,0.00081985665,0.0026856556,0.04456343],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99772656,0.0004075687,0.00030732248,0.0006503538,0.00051414774,0.00039402372],"domain_scores_gemma":[0.99897474,0.00003375369,0.0002621687,0.0005490222,0.000034105753,0.00014620682],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00024997018,0.00026118988,0.00030543,0.000040634448,0.00067377504,0.00016436288,0.00073276594,0.00012937993,0.33125556],"category_scores_gemma":[0.00010626634,0.00025713848,0.00004347741,0.00033159618,0.00039854663,0.000094153955,0.0010668286,0.0004538054,0.0026768823],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028481154,0.0013020147,0.016079117,0.00016161491,0.0001882946,0.00054989697,0.0028505921,0.011537323,0.005448568,0.0018762338,0.9371351,0.022586454],"study_design_scores_gemma":[0.0019385674,0.0024425616,0.08853742,0.00019043236,0.00006378676,0.00016849775,0.00046686587,0.0006986711,0.00020455293,0.00018083425,0.9042619,0.0008459547],"about_ca_topic_score_codex":0.00052170956,"about_ca_topic_score_gemma":0.00014964507,"teacher_disagreement_score":0.7756465,"about_ca_system_score_codex":0.00022517786,"about_ca_system_score_gemma":0.000007195134,"threshold_uncertainty_score":0.9999881},"labels":[],"label_agreement":null},{"id":"W6950437364","doi":"10.5281/zenodo.8076356","title":"cf_xarray","year":2023,"lang":"en","type":"other","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Ouranos","funders":"","keywords":"Metadata; Convention; Term (time); Process (computing); Product (mathematics)","score_opus":0.019863995005612547,"score_gpt":0.22222117539356398,"score_spread":0.20235718038795142,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6950437364","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00011918024,0.00004283151,0.0009048078,0.0001933,0.00016245221,0.00027343235,0.000110787085,0.00311171,0.9950815],"genre_scores_gemma":[0.004168458,0.00025534752,0.00044251524,0.00016171411,0.0003074133,4.4449166e-8,0.00049054687,0.024454253,0.9697197],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9985347,0.00010621834,0.00014706234,0.00046399637,0.00039742552,0.00035063177],"domain_scores_gemma":[0.99923563,0.000007845812,0.00010748226,0.00047389843,0.000017536515,0.00015760148],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00024120389,0.00017741013,0.00015201632,0.000010797914,0.00080188777,0.00024092384,0.0009455162,0.00013786413,0.44507912],"category_scores_gemma":[0.00012941973,0.00017708189,0.000054934262,0.00044521026,0.00023287174,0.0000638087,0.0014756588,0.00022870203,0.22958471],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003826678,0.000028748098,0.0000063196453,0.000011755159,0.000017278184,0.000011290578,0.000121725025,0.000015295891,0.0001301024,0.00019112576,0.94177383,0.0576887],"study_design_scores_gemma":[0.00014177845,0.00006011419,0.00033876035,0.000027718195,0.000009569731,0.000015762464,0.00006740678,0.00003987879,0.000010989544,0.00004437006,0.9990414,0.00020225334],"about_ca_topic_score_codex":0.00018771755,"about_ca_topic_score_gemma":0.0000066832863,"teacher_disagreement_score":0.2154944,"about_ca_system_score_codex":0.00016947865,"about_ca_system_score_gemma":8.0667024e-7,"threshold_uncertainty_score":0.77101517},"labels":[],"label_agreement":null},{"id":"W6950443130","doi":"10.5281/zenodo.7875119","title":"FIGURES 47–52 in Morphological and molecular characterization of twenty-five new Diploneis species (Bacillariophyta) from Lake Tanganyika and its surrounding areas","year":2023,"lang":"en","type":"other","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Canadian Museum of Nature","funders":"","keywords":"Holotype; Scale (ratio); Single specimen; Characterization (materials science); Paratype","score_opus":0.020135364183301196,"score_gpt":0.2144683945925301,"score_spread":0.1943330304092289,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6950443130","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":[0.82378733,0.00043932797,0.0013786878,0.00034730393,0.00015218831,0.00084284856,0.0010923957,0.00071982417,0.1712401],"genre_scores_gemma":[0.7472646,0.0037541804,0.0005525019,0.00019539632,0.00030115352,2.775734e-7,0.0031652122,0.00735002,0.23741664],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99864554,0.00013918124,0.00020536316,0.00046151472,0.0003128784,0.00023551197],"domain_scores_gemma":[0.99946064,0.000018832092,0.00016595853,0.000203848,0.000020539117,0.00013016818],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00016567168,0.00018432958,0.00024328136,0.000022830138,0.00022341951,0.00016466895,0.00033115715,0.00014942697,0.028452685],"category_scores_gemma":[0.00020900444,0.00018284848,0.000028385615,0.00035645138,0.00018491785,0.000102836275,0.00096552947,0.00018586013,0.00092369266],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022750339,0.00042843312,0.0070723034,0.00031864698,0.00027494703,0.0005529856,0.005396742,0.00009647204,0.41850343,0.0021248595,0.4908445,0.07415919],"study_design_scores_gemma":[0.0005124942,0.00013410352,0.080873,0.00017333042,0.000025337678,0.000023384808,0.00018473121,0.00018990845,0.00056668185,0.00009243037,0.9168908,0.0003337742],"about_ca_topic_score_codex":0.00030369937,"about_ca_topic_score_gemma":0.00004458902,"teacher_disagreement_score":0.42604634,"about_ca_system_score_codex":0.000072993396,"about_ca_system_score_gemma":0.0000018111722,"threshold_uncertainty_score":0.9998542},"labels":[],"label_agreement":null},{"id":"W6950480030","doi":"10.5281/zenodo.4684432","title":"Figure 21. Dimorphostylis nordaustraliana n in Eleven New Species and a New Genus of Diastylidae (Crustacea: Cumacea) from Australia and One New Species from Canada","year":2014,"lang":"en","type":"other","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Genus; Holotype; Taxonomy (biology); Subgenus; Taxon","score_opus":0.035788913244977814,"score_gpt":0.21454115781240965,"score_spread":0.17875224456743183,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6950480030","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.4292806,0.0014432947,0.0014234538,0.0033338577,0.00035324242,0.0015470476,0.002601681,0.00040429542,0.5596125],"genre_scores_gemma":[0.0909556,0.0005593131,0.0019691263,0.00011798375,0.000526242,3.8861806e-8,0.0009791934,0.0018887885,0.9030037],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9979756,0.00012502132,0.00032028422,0.00064005883,0.0005317465,0.0004072808],"domain_scores_gemma":[0.99876744,0.00002839066,0.00024121614,0.000455245,0.000018497976,0.0004892048],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00010560157,0.0003103276,0.00041827536,0.000019336381,0.00022338494,0.00024439997,0.00067268015,0.00018059048,0.31544572],"category_scores_gemma":[0.00013158312,0.0003256396,0.00003838098,0.00030626828,0.0002598079,0.000104682535,0.0009662354,0.00033436617,0.0016102679],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003231733,0.000026944494,0.0015379298,0.000022219294,0.00005355288,0.000016884376,0.00051794515,0.000023517356,0.0011592432,0.00008819145,0.9867401,0.009781136],"study_design_scores_gemma":[0.00059309887,0.00007841766,0.104221955,0.00010799503,0.00003315218,0.0000029750042,0.00022095058,0.0000126998875,0.00011942326,0.00008057332,0.89423466,0.00029412753],"about_ca_topic_score_codex":0.77701795,"about_ca_topic_score_gemma":0.10299837,"teacher_disagreement_score":0.6740196,"about_ca_system_score_codex":0.00024587032,"about_ca_system_score_gemma":0.00003069861,"threshold_uncertainty_score":0.9999196},"labels":[],"label_agreement":null},{"id":"W6950481801","doi":"10.5284/1100491","title":"The Former R. Rudlen and Co. Ltd. Boot and Shoe Manufactory Mill Road, Wellingborough, Northamptonshire Historic Building Record","year":2018,"lang":"en","type":"article","venue":"Archaeology Data Service","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Mill; Yard; Factory (object-oriented programming); Lift (data mining); Quarter (Canadian coin); Roof","score_opus":0.022417643564006103,"score_gpt":0.25853236701602117,"score_spread":0.23611472345201506,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6950481801","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":[0.9935516,0.00095146004,0.000726616,0.0027080476,0.00031204044,0.00018595514,0.00004070913,0.000038377388,0.001485211],"genre_scores_gemma":[0.9868973,0.0017451034,0.0074992175,0.0025359706,0.00019120035,0.00001551059,0.00006648906,0.000029389532,0.0010198086],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9984062,0.000087247325,0.00023033869,0.0006342746,0.0001701087,0.00047184463],"domain_scores_gemma":[0.99861187,0.00018937438,0.00011465256,0.00092152366,0.000013411413,0.0001491481],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040811382,0.00020470937,0.00018441172,0.0000027276092,0.00066870445,0.00001897192,0.0007518768,0.0001160245,0.0004892221],"category_scores_gemma":[0.00003012618,0.00015347275,0.000016568416,0.00013171589,0.0013508752,0.0003431197,0.002112079,0.00021489414,0.00015351328],"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":[0.0001796039,0.00005045692,0.7832006,0.000042142583,0.00008664214,0.00003161584,0.0077827894,0.0000071671116,0.0014625422,0.0002525974,0.016328637,0.1905752],"study_design_scores_gemma":[0.00031471986,0.00014908919,0.20448253,0.000010264086,0.00003424555,0.000086207314,0.00046074894,0.0023860345,0.00010930327,0.0014414352,0.7902386,0.00028682387],"about_ca_topic_score_codex":0.0063729,"about_ca_topic_score_gemma":0.02021616,"teacher_disagreement_score":0.77391,"about_ca_system_score_codex":0.00006535688,"about_ca_system_score_gemma":0.000014719017,"threshold_uncertainty_score":0.99766237},"labels":[],"label_agreement":null},{"id":"W6950516331","doi":"10.5683/sp/7hdzoo","title":"Replication Data for: Hsu et al_Peak End Mental Effort_Dataset_PLOSONE_1_30_2018","year":2018,"lang":"en","type":"dataset","venue":"Borealis","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"York University","funders":"","keywords":"Replication (statistics); Selection (genetic algorithm); Context (archaeology); MEDLINE","score_opus":0.035357228131812614,"score_gpt":0.31049515580524745,"score_spread":0.2751379276734348,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6950516331","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000052173436,0.00003795356,0.00012847633,0.00041593958,0.0001923064,0.00074795895,0.99750316,0.000052472315,0.0008695571],"genre_scores_gemma":[0.000012242617,0.0003105688,0.002139038,0.0014261656,0.00041776756,0.00012225761,0.99531966,0.000040759773,0.0002115212],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9971532,0.000055399327,0.00042214198,0.001391587,0.00054012175,0.00043752708],"domain_scores_gemma":[0.99282676,0.00006048849,0.00035419982,0.0065606795,0.000013460257,0.00018440712],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007220798,0.00039002154,0.00034329516,0.000003057922,0.00023637575,0.00009531417,0.0024119057,0.00030999506,0.0034956264],"category_scores_gemma":[0.00018336475,0.00034564635,0.00008257343,0.00011880566,0.00037474837,0.00038376398,0.0019894093,0.00019835483,0.00040717892],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003266947,0.000109729815,0.00004807069,0.000023504035,0.00003879459,0.000002678275,0.00001425849,0.000001173453,0.000022146078,0.000008090152,0.99864656,0.0010523332],"study_design_scores_gemma":[0.00026501858,0.00015582051,0.00054800365,0.000025275462,0.00012191831,0.000011144196,0.000010709226,0.00015977712,0.000030031342,0.000108246284,0.9981469,0.00041717713],"about_ca_topic_score_codex":0.053346373,"about_ca_topic_score_gemma":0.036444742,"teacher_disagreement_score":0.01690163,"about_ca_system_score_codex":0.00017799303,"about_ca_system_score_gemma":0.000044129105,"threshold_uncertainty_score":0.99989957},"labels":[],"label_agreement":null},{"id":"W6950561717","doi":"10.5683/sp3/3ttjz3","title":"Saint Pascal (West) Quebec. 1:50,000. Map Sheet 021N12, ed. 1, 1955","year":2022,"lang":"en","type":"dataset","venue":"Borealis","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Pascal (unit); Georeference; General partnership; Raster graphics; SAINT; Natural (archaeology); Digital mapping; Aerial photography","score_opus":0.007840811116060385,"score_gpt":0.22352967939726426,"score_spread":0.21568886828120387,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6950561717","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00030980693,0.00026668934,0.00003516132,0.0006309626,0.0005242383,0.0003842074,0.9951033,0.000081859944,0.0026637851],"genre_scores_gemma":[0.000058492995,0.00038889833,0.00026197018,0.0018329736,0.00037291745,0.00019322093,0.992862,0.00006144603,0.003968109],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9964772,0.00016960407,0.0005236896,0.0009670163,0.0010838476,0.00077864976],"domain_scores_gemma":[0.997815,0.00007071467,0.00029078187,0.0014602772,0.000007666546,0.00035553947],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00033394623,0.00059177686,0.000560124,0.0000045301763,0.00037424263,0.00011468214,0.0013800437,0.00039405006,0.38109195],"category_scores_gemma":[0.00004016003,0.00054586795,0.0002676871,0.00020625212,0.00037163156,0.00013005458,0.0014837506,0.0007339493,0.0010524214],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025691223,0.00015733196,0.0004272308,0.00003004875,0.000036131132,0.0001411865,0.000054892338,0.00024066803,0.000004289963,0.000040391922,0.9961584,0.0026837308],"study_design_scores_gemma":[0.00023858239,0.0001129361,0.009536831,0.000016878317,0.000089361325,0.000019230669,0.00012575221,0.00002253666,0.0000028453615,0.00007979832,0.9890862,0.00066903856],"about_ca_topic_score_codex":0.77088046,"about_ca_topic_score_gemma":0.3293183,"teacher_disagreement_score":0.44156212,"about_ca_system_score_codex":0.0012240856,"about_ca_system_score_gemma":0.0000827741,"threshold_uncertainty_score":0.9997254},"labels":[],"label_agreement":null},{"id":"W6950638615","doi":"10.5281/zenodo.5626926","title":"Hysterothylacium aduncum (Rudolphi, 1802) Deardorff & Overstreet 1981","year":2016,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Excretory system; Major duodenal papilla; Caecum; Dorsum; Conoid","score_opus":0.01718328555963643,"score_gpt":0.2081927596362919,"score_spread":0.19100947407665547,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6950638615","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.44588503,0.00004589514,0.018364225,0.002356684,0.00025854137,0.0006708458,0.00022360597,0.0011616716,0.5310335],"genre_scores_gemma":[0.9887718,0.000044200096,0.0004710126,0.00025396148,0.0001222847,5.967321e-8,0.00007486257,0.00075099757,0.0095108235],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9982234,0.00016453133,0.00021409504,0.00047029168,0.00046398464,0.00046365114],"domain_scores_gemma":[0.99910617,0.000017085087,0.00009270357,0.00049458107,0.000054265332,0.00023521646],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00035204436,0.00016216542,0.00013272373,0.0000073177234,0.0011905483,0.00023494834,0.0008748398,0.000067103974,0.10332958],"category_scores_gemma":[0.00018531679,0.0001262567,0.00006171813,0.00031216448,0.00032333026,0.00031461884,0.0014433044,0.00012629034,0.05056382],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010618369,0.00018746505,0.0006584598,0.00002104194,0.00003595962,0.000030113286,0.00073703344,0.000058181726,0.044207726,0.0020937456,0.65797865,0.2938854],"study_design_scores_gemma":[0.0005419845,0.00020353388,0.007929806,0.000020284875,0.000008120194,0.000037049867,0.00012995655,0.00008559251,0.0008856193,0.00018343887,0.98976135,0.00021326273],"about_ca_topic_score_codex":0.00005742164,"about_ca_topic_score_gemma":0.0000018090383,"teacher_disagreement_score":0.54288673,"about_ca_system_score_codex":0.0002757136,"about_ca_system_score_gemma":0.0000014344911,"threshold_uncertainty_score":0.9501754},"labels":[],"label_agreement":null},{"id":"W6950671703","doi":"10.5281/zenodo.593938","title":"phylotastic/datelife: datelife v0.6.7","year":2023,"lang":"en","type":"other","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Royal Ontario Museum","funders":"","keywords":"Nucleofection; Gestational period; TSG101; Dysgeusia; Diafiltration; Liquation; Fusible alloy; Triacetin; Durvalumab","score_opus":0.022830121411518117,"score_gpt":0.22965133590965384,"score_spread":0.20682121449813573,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6950671703","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00029057014,0.00006866943,0.0014092923,0.00026106864,0.00026483837,0.0004191271,0.00037726102,0.0034003165,0.9935089],"genre_scores_gemma":[0.009784996,0.0006585666,0.00083440257,0.00038537456,0.0007193591,1.4989521e-7,0.0019019232,0.034021616,0.9516936],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99776274,0.00016411848,0.00024548374,0.00068290246,0.0006260663,0.0005186973],"domain_scores_gemma":[0.9988219,0.000015776703,0.00017270581,0.00069681683,0.00003592297,0.00025688764],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00035500663,0.00027774487,0.00023665103,0.000017482886,0.000990964,0.00037518537,0.0013836283,0.00017799398,0.34323704],"category_scores_gemma":[0.0002912451,0.00027830986,0.00007104174,0.000620553,0.00032698803,0.0001059737,0.0024928392,0.00033368057,0.2453224],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009885505,0.000054693573,0.000009536769,0.000021732361,0.000033354507,0.000023790775,0.000116283525,0.0000441272,0.00019954014,0.0001771528,0.95174336,0.04756654],"study_design_scores_gemma":[0.00023912956,0.00009302936,0.00040943245,0.000045037592,0.000019830655,0.000023622873,0.00008841517,0.00013344201,0.000023076174,0.00003159162,0.99858284,0.0003105403],"about_ca_topic_score_codex":0.0002663121,"about_ca_topic_score_gemma":0.000007651416,"teacher_disagreement_score":0.09791465,"about_ca_system_score_codex":0.00020543092,"about_ca_system_score_gemma":0.0000019994409,"threshold_uncertainty_score":0.9999669},"labels":[],"label_agreement":null},{"id":"W6950680972","doi":"10.5281/zenodo.8112741","title":"Body composition according to spinal cord injury level: a systematic review and meta-analysis","year":2021,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Tetraplegia; Spinal cord injury; Paraplegia; Anthropometry; Body mass index; Adipose tissue; Lean body mass","score_opus":0.06796924134584534,"score_gpt":0.2958341230664887,"score_spread":0.22786488172064337,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6950680972","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":[0.3312316,0.03381234,0.28270313,0.03667962,0.00031693355,0.014762299,0.0021012928,0.0037140956,0.29467872],"genre_scores_gemma":[0.9945187,0.00026983512,0.0014288076,0.0018738678,0.00001421268,3.029749e-7,0.00019935603,0.0002899149,0.0014050173],"study_design_codex":"not_applicable","study_design_gemma":"meta_analysis","domain_scores_codex":[0.99843204,0.00034626055,0.00028204036,0.00038823579,0.00033991123,0.00021150651],"domain_scores_gemma":[0.99923,0.000010780462,0.00010382992,0.00038707198,0.00009752928,0.00017073393],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00054703496,0.00012408089,0.0004948184,0.000010249047,0.0008789213,0.0003319572,0.00037881528,0.000027554079,0.027152283],"category_scores_gemma":[0.00019620961,0.00010956259,0.00015159161,0.0011011853,0.00006775187,0.00015670812,0.0011476498,0.00010768015,0.003847129],"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":[0.0011748262,0.0026455887,0.0003894787,0.12911168,0.1219074,0.00063069974,0.0041811336,0.0016447874,0.14277717,0.013004329,0.53556305,0.046969865],"study_design_scores_gemma":[0.0013492556,0.004948122,0.012708599,0.0029168832,0.5267721,0.0014623664,0.0038961007,0.0022116425,0.00438725,0.0004380762,0.4353138,0.003595842],"about_ca_topic_score_codex":0.000022468497,"about_ca_topic_score_gemma":6.266918e-7,"teacher_disagreement_score":0.6632871,"about_ca_system_score_codex":0.00010995476,"about_ca_system_score_gemma":0.0000011031389,"threshold_uncertainty_score":0.9969285},"labels":[],"label_agreement":null},{"id":"W6950681635","doi":"10.5683/sp3/vz7khy","title":"Pollinators utilize both traditional and forb-supplemented set-aside fields in agriculture","year":2025,"lang":"en","type":"dataset","venue":"Borealis","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"University of British Columbia","funders":"","keywords":"Pollinator; Agriculture; Habitat; Ecosystem; Biodiversity; Ecosystem services","score_opus":0.012061799392722755,"score_gpt":0.23405031850530114,"score_spread":0.2219885191125784,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6950681635","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0009775094,0.00010124476,0.000018521616,0.0005716241,0.00008331888,0.00026300692,0.9954218,0.000016385668,0.0025465603],"genre_scores_gemma":[0.0013956957,0.0004069768,0.00020257614,0.0009192922,0.00007028001,0.000060157763,0.9964212,0.000005938593,0.0005178652],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9986398,0.0000426433,0.00027912573,0.00042810716,0.00031286504,0.0002974277],"domain_scores_gemma":[0.9994478,0.00005482715,0.00009781019,0.00029014764,0.0000041340777,0.00010526659],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00010145083,0.00027091033,0.00027337202,0.0000045529514,0.00009857237,0.000035625562,0.00029494942,0.00034153476,0.0023404865],"category_scores_gemma":[0.000025548798,0.00021858029,0.00006990062,0.00020873257,0.00011576672,0.000075901786,0.00014704102,0.0003314358,0.0000034617005],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009848708,0.000062541956,0.001516437,0.000026552349,0.000015313411,0.000029158315,0.000044377124,0.000020132324,0.0000022099566,0.00005601493,0.9978405,0.00037687685],"study_design_scores_gemma":[0.00033700312,0.00005326896,0.028238805,0.00004470025,0.00003366806,0.0000069168486,0.00012319256,0.000022183627,0.000009638625,0.00039317345,0.97049606,0.00024140817],"about_ca_topic_score_codex":0.06679919,"about_ca_topic_score_gemma":0.08582395,"teacher_disagreement_score":0.027344497,"about_ca_system_score_codex":0.00014136732,"about_ca_system_score_gemma":0.000030313066,"threshold_uncertainty_score":0.9985715},"labels":[],"label_agreement":null},{"id":"W6950693448","doi":"10.5683/sp3/ktijtc","title":"Shaw MRI4.5 Bottom Model","year":2022,"lang":"en","type":"dataset","venue":"Borealis","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Dalhousie University","funders":"","keywords":"Data file; Numerical models; Hydrology (agriculture); Heat flow; Field (mathematics)","score_opus":0.011953093960375095,"score_gpt":0.23112375285079637,"score_spread":0.21917065889042128,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6950693448","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000044832417,0.000059219747,0.00008415921,0.00015364935,0.00010593092,0.00016746123,0.9906628,0.000046685873,0.008675255],"genre_scores_gemma":[0.000012904122,0.00026328626,0.0007268281,0.0013167675,0.000077035605,0.000094348594,0.99537677,0.000030122648,0.0021019506],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9981965,0.000040254847,0.00023869521,0.0005179479,0.00063331926,0.00037329565],"domain_scores_gemma":[0.99879324,0.000019726105,0.00014375472,0.0008894913,0.000002879576,0.00015090973],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014825516,0.00028631027,0.00026521477,0.0000015088142,0.0002296757,0.000037083595,0.0008553963,0.00019532189,0.17588508],"category_scores_gemma":[0.000017461254,0.0002668131,0.00012782693,0.00014434608,0.00013940957,0.00007369318,0.00087504165,0.00047879366,0.00020973821],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006709976,0.000057020286,0.00008249834,0.000007223189,0.000011206775,0.000029622584,0.000025415991,0.0031823325,0.000002192523,0.000013428878,0.996109,0.00047333242],"study_design_scores_gemma":[0.00010418904,0.000037638118,0.00027654876,0.000003844751,0.000042848198,0.0000059386707,0.000022039847,0.0016232777,0.0000011128898,0.00022843233,0.9973234,0.0003307425],"about_ca_topic_score_codex":0.09031298,"about_ca_topic_score_gemma":0.008575356,"teacher_disagreement_score":0.17567533,"about_ca_system_score_codex":0.0002687161,"about_ca_system_score_gemma":0.00003778992,"threshold_uncertainty_score":0.9999784},"labels":[],"label_agreement":null},{"id":"W6950790821","doi":"10.5683/sp3/r8fdjb","title":"Image dataset of various soil types in an urban city","year":2021,"lang":"en","type":"dataset","venue":"Borealis","topic":"Atmospheric aerosols and clouds","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 du Québec à Chicoutimi","funders":"","keywords":"Class (philosophy); Orientation (vector space); Image (mathematics); Urban environment; Estimation; Urban area; Soil water","score_opus":0.011650197873697098,"score_gpt":0.2490974535154899,"score_spread":0.2374472556417928,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6950790821","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.002257206,0.00006777917,0.000013038212,0.00002444064,0.00005139004,0.00009880105,0.99694455,0.000008263093,0.0005345647],"genre_scores_gemma":[0.00017309644,0.00012948293,0.0007902571,0.00021245127,0.000059586597,0.000011838903,0.9985672,0.000013892176,0.000042157717],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99856365,0.000080104495,0.00032956628,0.00044344633,0.0003272677,0.00025597776],"domain_scores_gemma":[0.99864703,0.000023835042,0.00017849669,0.0010334405,0.000007773423,0.00010944043],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00018524853,0.00021676763,0.00034309286,0.000002531114,0.00003974241,0.000031378724,0.00059036125,0.00020663977,0.0044800593],"category_scores_gemma":[0.00004173823,0.00019976754,0.000049574624,0.00019039302,0.00021610915,0.00015503976,0.00042966756,0.00023805234,0.000044046657],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009382744,0.00017759988,0.003100087,0.000023232953,0.000008434853,0.00010241132,0.000034469584,0.000023475817,0.000050057697,0.0000010420529,0.99621695,0.00025286735],"study_design_scores_gemma":[0.00014132014,0.000055413162,0.017426347,0.000019270828,0.000034132707,0.0000043822874,0.000028891389,0.000058411282,0.000035294048,0.000023767949,0.98194736,0.00022540336],"about_ca_topic_score_codex":0.225492,"about_ca_topic_score_gemma":0.19155087,"teacher_disagreement_score":0.03394114,"about_ca_system_score_codex":0.00010131425,"about_ca_system_score_gemma":0.00004754322,"threshold_uncertainty_score":0.99643},"labels":[],"label_agreement":null},{"id":"W6950865330","doi":"10.5683/sp3/eakmi0","title":"Data for: Occupancy–detection models with museum specimen data: Promise and pitfalls","year":2022,"lang":"en","type":"dataset","venue":"Borealis","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Simon Fraser University; University of British Columbia","funders":"Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung","keywords":"Suite; Occupancy; Focus (optics); Inference; Data collection; Statistical inference","score_opus":0.04619177139139337,"score_gpt":0.2645917297493378,"score_spread":0.21839995835794446,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6950865330","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00008283992,0.00010993839,0.0013576597,0.00008602934,0.000088534325,0.00082084927,0.99702054,0.000037118294,0.0003964638],"genre_scores_gemma":[0.000058294634,0.0005299993,0.0016915604,0.0001650146,0.00015505769,0.00013594651,0.9970248,0.0000391767,0.00020017284],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9976507,0.000045616518,0.0002530809,0.0012168133,0.0004855605,0.00034823018],"domain_scores_gemma":[0.9959671,0.000043136602,0.00022346406,0.0036215342,0.0000060777043,0.00013871375],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003500177,0.00032488853,0.00032585417,0.000002988768,0.00028755958,0.00009022864,0.0018835673,0.00014194247,0.003169349],"category_scores_gemma":[0.000026736468,0.0002673535,0.000023533703,0.00012798054,0.00017490347,0.0006116695,0.0033441873,0.0002698168,0.000005987631],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000101117956,0.000064946675,0.000032420176,0.000036973688,0.000043070228,0.000012676661,0.000019598989,0.00012984427,0.0000064436604,0.000003326418,0.9978967,0.0016529006],"study_design_scores_gemma":[0.000430238,0.00019312561,0.00037975246,0.000012216966,0.00017516529,0.000019850639,0.000058147507,0.003153534,0.0000023692285,0.00009802843,0.9950907,0.00038686622],"about_ca_topic_score_codex":0.042527106,"about_ca_topic_score_gemma":0.056569066,"teacher_disagreement_score":0.014041959,"about_ca_system_score_codex":0.00013172372,"about_ca_system_score_gemma":0.00004425474,"threshold_uncertainty_score":0.9999779},"labels":[],"label_agreement":null},{"id":"W6950934871","doi":"10.5683/sp2/empuzc","title":"Ontario soybean grain prices, June 2010 to 2019 [Canada]","year":2018,"lang":"en","type":"dataset","venue":"Borealis","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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 Guelph","funders":"","keywords":"Agriculture; Agribusiness; Crop; Foreign exchange; Crop production","score_opus":0.006874056006503464,"score_gpt":0.205577720921194,"score_spread":0.19870366491469055,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6950934871","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00020150747,0.00001984962,0.000022775532,0.0005948113,0.0010208901,0.00035122177,0.9903438,0.000021121436,0.0074240253],"genre_scores_gemma":[0.0000063663592,0.000020581507,0.0007798895,0.0020988458,0.00036312747,0.00003090138,0.96326786,0.000027744405,0.033404656],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9976086,0.000037335783,0.00033461265,0.0006715598,0.0007564402,0.0005914216],"domain_scores_gemma":[0.99822533,0.00002119712,0.00019423687,0.0011213449,0.000012819305,0.00042506185],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00023221623,0.00040452607,0.0003699553,0.0000026431924,0.00018087447,0.000056294644,0.0010391796,0.00026534006,0.013004267],"category_scores_gemma":[0.00003091003,0.0003582645,0.0000826502,0.00018243607,0.00015715619,0.00007364986,0.00057229755,0.00034397797,0.0007784972],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009141656,0.000038165083,0.00034968523,0.000006090608,0.000018643885,0.000033277807,0.000055119035,0.000008626078,0.00000330947,0.0000013280636,0.99909115,0.00038548445],"study_design_scores_gemma":[0.00011485351,0.00006783618,0.018750783,0.000018479255,0.000041177627,0.0000061586147,0.000011105732,0.0000015689801,0.0000056492045,0.000028061888,0.9804877,0.0004666231],"about_ca_topic_score_codex":0.9996531,"about_ca_topic_score_gemma":0.9999615,"teacher_disagreement_score":0.02707591,"about_ca_system_score_codex":0.0011826644,"about_ca_system_score_gemma":0.00041450694,"threshold_uncertainty_score":0.9999995},"labels":[],"label_agreement":null},{"id":"W6950970371","doi":"10.5291/ill-data.5-53-250","title":"Sm2Ti2O7: A Quantum Spin Ice Candidate","year":2016,"lang":"en","type":"dataset","venue":"Institut Laue-Langevin","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Winnipeg","funders":"","keywords":"Quantum; Spin (aerodynamics); Quantum dot; Quantum entanglement; Quantum system","score_opus":0.01058242186104812,"score_gpt":0.2453492054423189,"score_spread":0.23476678358127076,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6950970371","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0036416275,0.00047655226,0.00016274943,0.00033705105,0.0016368268,0.0005286287,0.98032266,0.000118080585,0.012775827],"genre_scores_gemma":[0.0033803303,0.0020808459,0.00035486143,0.0030405356,0.0014772273,0.0002444683,0.9778638,0.00010735517,0.011450558],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99705464,0.000087251035,0.000490369,0.0008974713,0.000690243,0.0007800354],"domain_scores_gemma":[0.9980338,0.000052397325,0.0003217047,0.001255312,0.0000118802545,0.00032485722],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0002669324,0.00060947443,0.00058589893,0.0000068869404,0.00027010756,0.00009222559,0.0011927312,0.0004885747,0.01729624],"category_scores_gemma":[0.000100045676,0.00045014266,0.00017726317,0.00027689623,0.0005526028,0.00026079643,0.0007543573,0.0004933836,0.01756969],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025308489,0.00008315006,0.00047758684,0.00004560487,0.00003703028,0.00020894685,0.000021969397,0.000013365255,0.000110365334,0.00006381587,0.99655586,0.0023570163],"study_design_scores_gemma":[0.00042143246,0.000095027215,0.0010434557,0.00018515534,0.000091313785,0.0000314391,0.000012938963,0.0000166345,0.000025641777,0.00009365149,0.9972901,0.0006932641],"about_ca_topic_score_codex":0.011340578,"about_ca_topic_score_gemma":0.008474784,"teacher_disagreement_score":0.002865794,"about_ca_system_score_codex":0.00039616006,"about_ca_system_score_gemma":0.00011818142,"threshold_uncertainty_score":0.999795},"labels":[],"label_agreement":null},{"id":"W6957976556","doi":"10.60692/zb065-d4f84","title":"Satellite-Surface Perspectives of Air Quality and Aerosol-Cloud Effects on the Environment: An Overview of 7-SEAS/BASELInE","year":2016,"lang":"en","type":"article","venue":"Greater South Information System","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"National Research Council Canada","funders":"","keywords":"Air quality index; Aerosol; Trace gas; Radar; Cloud computing; Satellite; Atmospheric model; Air pollution","score_opus":0.03911177837106077,"score_gpt":0.24124932913417882,"score_spread":0.20213755076311804,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6957976556","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":[0.9957056,0.000051165156,0.0026011176,0.00015129575,0.00004680936,0.00033106704,0.00004794962,0.00002564591,0.0010393654],"genre_scores_gemma":[0.9995466,0.000014126927,0.00021733428,0.000105158026,0.000016920285,0.000011699609,0.0000014517972,0.0000068707436,0.00007983411],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99861073,0.0002345935,0.00046716793,0.00016389007,0.0003694516,0.00015418087],"domain_scores_gemma":[0.9990441,0.00006483858,0.0003749181,0.00042678954,0.000014424139,0.00007490709],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007146273,0.00015440892,0.00023510223,0.0000025855718,0.00008196599,0.00001291427,0.00016152428,0.0000620553,0.00019280253],"category_scores_gemma":[0.000027638367,0.00007913699,0.000059075635,0.00008469298,0.0001925273,0.0003413496,0.00009242108,0.00004294431,0.00022390994],"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":[0.00020405602,0.00003575595,0.83423024,0.0007885447,0.00007125206,8.788898e-7,0.14915101,0.00072357943,0.002265666,0.002740072,0.00004913794,0.009739798],"study_design_scores_gemma":[0.0012856947,0.00039149704,0.93649375,0.00041921722,0.00004130084,0.000004396038,0.030022385,0.0005590966,0.030119728,0.000015626703,0.00029275825,0.0003545219],"about_ca_topic_score_codex":0.000034205477,"about_ca_topic_score_gemma":3.4657128e-7,"teacher_disagreement_score":0.11912862,"about_ca_system_score_codex":0.00009383535,"about_ca_system_score_gemma":0.0000049826767,"threshold_uncertainty_score":0.3227113},"labels":[],"label_agreement":null},{"id":"W6958911651","doi":"10.6084/m9.figshare.9999362","title":"Chemical and microphysical properties of wind-blown dust near an actively retreating glacier in Yukon, Canada","year":2019,"lang":"en","type":"article","venue":"Figshare","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Mineral dust; Aerosol; Particulates; Biogeochemical cycle; Air quality index; Mineral; Atmospheric dust; Atmosphere (unit)","score_opus":0.010360214718013332,"score_gpt":0.17999235957195028,"score_spread":0.16963214485393696,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6958911651","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":[0.99753785,0.000017900114,1.8347565e-8,0.000021434389,0.0000074592767,0.00011136074,0.0011369474,0.0000055101877,0.0011615397],"genre_scores_gemma":[0.99922115,2.786643e-7,0.000112296315,0.00006803537,0.000014175652,0.0000065135714,0.00033662122,0.000009146382,0.00023178739],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9993767,0.000013655623,0.000100648555,0.00020022305,0.00015096455,0.00015781575],"domain_scores_gemma":[0.9997606,0.000011634256,0.000044676766,0.00011720587,0.0000060290795,0.00005982859],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000014250855,0.00008640142,0.00012053867,4.3226683e-7,0.000028748202,0.000014180871,0.00010956593,0.00004638471,0.023904955],"category_scores_gemma":[0.000037955644,0.00007020697,0.000014065747,0.00008768447,0.000028142385,0.00011385785,0.00012882614,0.00009939553,0.000086422726],"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":[0.000100351266,0.0002002392,0.23874778,0.00022897273,0.000016465818,0.000026990154,0.0021200213,0.0005556188,0.7365614,0.0000019860527,0.011339387,0.010100746],"study_design_scores_gemma":[0.00084896566,0.00015536445,0.764559,0.00095222704,0.000007714075,0.000010720292,0.0008562484,0.007599927,0.21439889,0.000006253806,0.010036894,0.0005678245],"about_ca_topic_score_codex":0.048471816,"about_ca_topic_score_gemma":0.011845482,"teacher_disagreement_score":0.5258112,"about_ca_system_score_codex":0.000100140714,"about_ca_system_score_gemma":0.00005245777,"threshold_uncertainty_score":0.9769873},"labels":[],"label_agreement":null},{"id":"W6961051770","doi":"10.14288/bcs.v0i39.185514","title":"Vancouver by Eric Nicol","year":2014,"lang":"en","type":"article","venue":"Open Collections","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Exposition (narrative); Government (linguistics); Work (physics); Field (mathematics); Theme (computing)","score_opus":0.0063220172530853765,"score_gpt":0.20958444509868188,"score_spread":0.2032624278455965,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6961051770","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0047591273,0.0000033860854,0.0053599626,0.00009351902,0.0002684731,0.0002536516,0.000004482683,0.000028055107,0.9892293],"genre_scores_gemma":[0.11649854,0.0000047960166,0.002938015,0.00056111184,0.000028141123,0.00010935369,0.0000014842547,0.000011000612,0.8798476],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99943113,0.000028934197,0.00008974016,0.00019000757,0.00010623432,0.00015394656],"domain_scores_gemma":[0.99968696,0.00002242876,0.00003277462,0.00018013199,0.0000034035395,0.00007429386],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000085701315,0.00006895011,0.000080343976,3.2425532e-7,0.0012594489,0.00024258917,0.00027723418,0.000033494027,0.030099042],"category_scores_gemma":[0.00001647428,0.0000624857,0.000026058475,0.0005102988,0.00005758272,0.0001442755,0.00023472901,0.000060945364,0.0004052349],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000029781602,0.000049622984,0.00066045485,2.9221752e-7,0.0000030513181,1.7229166e-7,0.000019595058,0.00016345571,0.00022626415,0.000008709755,0.99756044,0.001304979],"study_design_scores_gemma":[0.00022529524,0.000067797,0.00089248526,0.0000016142021,0.000006262499,0.0000018297566,0.00005762278,0.0013248549,0.000152627,0.00052282755,0.99663794,0.00010886218],"about_ca_topic_score_codex":0.009410465,"about_ca_topic_score_gemma":0.0073540257,"teacher_disagreement_score":0.11173941,"about_ca_system_score_codex":0.000095865216,"about_ca_system_score_gemma":0.000008982752,"threshold_uncertainty_score":0.99718595},"labels":[],"label_agreement":null},{"id":"W6962430109","doi":"10.15468/dl.zhww67","title":"Occurrence Download","year":2023,"lang":"en","type":"dataset","venue":"Global Biodiversity Information Facility","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Download; Matching (statistics); Range (aeronautics); Real world data; State (computer science)","score_opus":0.011176506980477875,"score_gpt":0.20580065359117286,"score_spread":0.194624146610695,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6962430109","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0017606043,0.0000031965553,0.00000555565,0.00010509208,0.00052402663,0.00022737015,0.9968634,0.00013445181,0.0003762917],"genre_scores_gemma":[0.0000128661895,0.000049720034,0.0000025425852,0.000461448,0.0000011811469,0.0000041945377,0.9994669,1.6653877e-8,0.0000011165769],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99848586,0.000035050867,0.00030441987,0.00025310644,0.0005910795,0.0003304978],"domain_scores_gemma":[0.9991179,0.000013244462,0.00022105104,0.0004529458,0.000023749224,0.00017112582],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00019716426,0.00025507552,0.00021313962,0.0000025763577,0.00029401088,0.00008747158,0.0005885662,0.000296143,0.008580573],"category_scores_gemma":[0.00007395929,0.000249819,0.00012714941,0.0004386309,0.00027997946,0.00065357506,0.0008278991,0.00022653778,0.89104277],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014843741,0.000019028646,0.0062522483,0.000029013503,0.000010625935,0.000002629975,0.000023882267,0.00007829204,3.2914475e-8,1.319844e-8,0.99224186,0.0013275451],"study_design_scores_gemma":[0.00016210962,0.000026326159,0.001732839,0.0000011172317,0.000026182806,0.0000018943833,0.000099565,4.8189804e-7,5.073802e-7,9.936517e-7,0.9976812,0.00026675643],"about_ca_topic_score_codex":0.003792527,"about_ca_topic_score_gemma":0.000088512126,"teacher_disagreement_score":0.8824622,"about_ca_system_score_codex":0.00048224954,"about_ca_system_score_gemma":0.000033238954,"threshold_uncertainty_score":0.9999954},"labels":[],"label_agreement":null},{"id":"W6963626707","doi":"10.18739/a2qf8jk1x","title":"Millimeter Cloud Radar Deployed at Eureka Nunavut Canada - Image Files","year":2009,"lang":"en","type":"dataset","venue":"California Digital Library","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Cloud computing; Arctic; Radar; The arctic; Doppler radar; Atmosphere (unit); Millimeter","score_opus":0.0037947077343314663,"score_gpt":0.1677736095455602,"score_spread":0.16397890181122873,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6963626707","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.006206408,0.00033402955,0.000008137043,0.00032284137,0.00034501703,0.00031690943,0.9860322,0.00012932238,0.0063051414],"genre_scores_gemma":[0.0005592858,0.00015684452,0.00045856822,0.0039921664,0.00043428104,0.000020598356,0.98907834,0.00010240665,0.005197497],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.996965,0.000046499725,0.0005600264,0.00087375025,0.0007578298,0.00079689774],"domain_scores_gemma":[0.99818563,0.00009280111,0.00026131872,0.0008994363,0.000004611929,0.0005561892],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000037127742,0.00072171236,0.00056744146,0.000004188555,0.00023592192,0.00037119936,0.0010991003,0.00034020594,0.0248809],"category_scores_gemma":[0.000037732836,0.000612773,0.00023722334,0.00027775008,0.0003255982,0.0007440383,0.0012499633,0.00044838426,0.008762674],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000042261057,0.00007071599,0.0017086989,0.000030258883,0.0000297793,0.00039340722,0.0000021726441,0.000007638374,0.000011021506,3.6204284e-7,0.9965732,0.001130482],"study_design_scores_gemma":[0.00022099716,0.00006195376,0.00066931377,0.000038630835,0.000042325493,0.000041149888,0.000008799735,0.000010066342,0.00013488089,0.00010200772,0.99787825,0.0007915916],"about_ca_topic_score_codex":0.016500218,"about_ca_topic_score_gemma":0.016735964,"teacher_disagreement_score":0.016118225,"about_ca_system_score_codex":0.000384138,"about_ca_system_score_gemma":0.00022556394,"threshold_uncertainty_score":0.99963236},"labels":[],"label_agreement":null},{"id":"W6964431918","doi":"10.25455/wgtn.25824094","title":"Newly identified climatically and environmentally significant high-latitude dust sources","year":2024,"lang":"en","type":"article","venue":"Figshare","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Dust storm; Mineral dust; Latitude; Storm; Arctic; Spatial distribution; Land cover; Deposition (geology); Atmosphere (unit)","score_opus":0.010575224829204085,"score_gpt":0.21090329642857453,"score_spread":0.20032807159937044,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6964431918","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":[0.9317917,0.0015293796,0.00046875124,0.0015640223,0.00032047083,0.00110453,0.035902884,0.00063646457,0.026681792],"genre_scores_gemma":[0.99235713,0.000024835857,0.0018161712,0.00037616957,0.00008316326,0.00008168862,0.0027569307,0.000034256685,0.0024696633],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9987926,0.00002257498,0.0001956742,0.0004142387,0.0003026435,0.00027228557],"domain_scores_gemma":[0.9995342,0.000080622405,0.00003786623,0.00019710562,0.0000018646938,0.00014834563],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00005331412,0.00017062727,0.00013107012,0.0000018278757,0.00012814974,0.00020712036,0.00020039192,0.00008129825,0.44985518],"category_scores_gemma":[0.000051416922,0.00014393449,0.000049728464,0.000112239264,0.00005706001,0.00026187862,0.00034202705,0.00014347017,0.013487608],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003083223,0.00024240676,0.011293062,0.00055316807,0.00014155015,0.000511902,0.0020939787,0.0057872473,0.027514622,0.00063251704,0.9073204,0.043878343],"study_design_scores_gemma":[0.00075318513,0.00032371815,0.43677646,0.0015614567,0.00011198155,0.00006336178,0.00065519597,0.027532952,0.0029823354,0.0012827584,0.52638274,0.001573863],"about_ca_topic_score_codex":0.000051815397,"about_ca_topic_score_gemma":0.000017421024,"teacher_disagreement_score":0.43636757,"about_ca_system_score_codex":0.00007217659,"about_ca_system_score_gemma":0.000009069267,"threshold_uncertainty_score":0.9872805},"labels":[],"label_agreement":null},{"id":"W6964924395","doi":"10.34657/1057","title":"Laboratory-generated mixtures of mineral dust particles with biological substances: Characterization of the particle mixing state and immersion freezing behavior","year":2016,"lang":"en","type":"article","venue":"TIB Repositorium","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"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":"Ice nucleus; Aerosol; Nucleation; Particle (ecology); Mixing (physics); Mineral dust; Ice crystals","score_opus":0.008807826200221823,"score_gpt":0.1976537363507482,"score_spread":0.18884591015052637,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6964924395","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":[0.99943,0.00004184498,0.00018762574,0.00009654193,0.000101610356,0.000106876876,0.000008470123,0.0000084733865,0.000018527291],"genre_scores_gemma":[0.9995568,0.000016617043,0.00020384794,0.0000141044375,0.000029543471,0.000007801781,9.2218545e-7,0.000005960357,0.00016440568],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9993267,0.000055270677,0.00017909025,0.00015398877,0.00015239425,0.00013253385],"domain_scores_gemma":[0.99961877,0.000017121503,0.0001584634,0.00014014076,0.00002217407,0.00004330535],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000823698,0.00007752726,0.00010279712,5.52299e-7,0.00007458014,0.000009594427,0.00008024558,0.000036055582,0.000049584916],"category_scores_gemma":[0.000008894585,0.00003631645,0.000016758551,0.00015509964,0.00024524538,0.0001038614,0.000054597207,0.000029263594,0.000001684015],"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":[0.0000223717,0.000022757366,0.4532621,0.0000017650009,0.0000026161167,0.0000012295626,0.00011563022,0.0000046932964,0.5461528,0.000003833965,0.000008063761,0.00040218708],"study_design_scores_gemma":[0.00014048409,0.00005397392,0.42146486,0.000016960574,0.000009009895,0.0000015048513,0.000034868914,0.00004624559,0.578156,0.0000017870435,0.000032572523,0.000041732997],"about_ca_topic_score_codex":0.00007727084,"about_ca_topic_score_gemma":0.000015745672,"teacher_disagreement_score":0.032003224,"about_ca_system_score_codex":0.000022939044,"about_ca_system_score_gemma":0.0000075576586,"threshold_uncertainty_score":0.14809418},"labels":[],"label_agreement":null},{"id":"W6964959228","doi":"10.34657/3541","title":"Depolarization and lidar ratios at 355, 532, and 1064 nm and microphysical properties of aged tropospheric and stratospheric Canadian wildfire smoke","year":2018,"lang":"en","type":"article","venue":"TIB Repositorium","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Depolarization ratio; Troposphere; Stratosphere; Lidar; Aerosol; Wavelength; Effective radius; Tropopause","score_opus":0.005322348990841645,"score_gpt":0.17566708833609057,"score_spread":0.17034473934524894,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6964959228","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":[0.99810344,0.00065262883,0.00005967777,0.00010099976,0.00011577822,0.00020821618,0.0000020918949,0.000016561253,0.0007406118],"genre_scores_gemma":[0.9981806,0.00007710024,0.0008975481,0.00007265999,0.0001313353,0.000005591428,0.00000184407,0.00001830536,0.0006149931],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9990272,0.000049835544,0.0001949456,0.00034330445,0.00015831867,0.00022637978],"domain_scores_gemma":[0.9994907,0.000010790877,0.00009055826,0.0001583508,0.000011583419,0.00023804526],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006493237,0.00016522307,0.00018691125,0.0000014316637,0.00039411604,0.000078597244,0.0000624592,0.00009850864,0.000034884946],"category_scores_gemma":[0.00001248029,0.00013871884,0.00001471937,0.00012592506,0.0008137022,0.00017513012,0.00012566644,0.00007792652,0.0000030155325],"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":[0.000038306298,0.000022654087,0.45241493,0.000027889188,0.00001617463,0.000008333716,0.0013958241,0.00000223126,0.54347473,0.000013946117,0.00011343686,0.0024715408],"study_design_scores_gemma":[0.00045953062,0.00046991164,0.90899235,0.00003447599,0.000055603028,0.00009408603,0.00032259675,0.0009156598,0.08753707,0.00003603062,0.00077793834,0.00030473777],"about_ca_topic_score_codex":0.04821578,"about_ca_topic_score_gemma":0.01090518,"teacher_disagreement_score":0.45657742,"about_ca_system_score_codex":0.00008729062,"about_ca_system_score_gemma":0.000036054695,"threshold_uncertainty_score":0.95812225},"labels":[],"label_agreement":null},{"id":"W6969202199","doi":"10.5281/zenodo.8310096","title":"OPS particle size distribution, AERONET and Lidar aerosol optical depth data employed in amt-2023-67","year":2023,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Université de Sherbrooke","funders":"","keywords":"Lidar; Aerosol; AERONET; Atmospheric optics; Optical depth; Atmosphere (unit); Particle size","score_opus":0.038356925723697664,"score_gpt":0.2547874165110723,"score_spread":0.2164304907873746,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6969202199","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":[0.98100734,0.000026569736,0.0012369684,0.001187871,0.000044998087,0.0003206632,0.00027510544,0.00046557572,0.015434903],"genre_scores_gemma":[0.9967696,0.00008403807,0.00027528687,0.00008907685,0.000042192925,9.706641e-8,0.0014717069,0.00032306163,0.0009449252],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9982839,0.00015500409,0.00023008804,0.0005271298,0.00035381707,0.00045003986],"domain_scores_gemma":[0.9990939,0.00004602867,0.000046574474,0.0005701631,0.000028861306,0.00021447122],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0006398998,0.00012372875,0.0001247176,0.0000031640088,0.0008402044,0.00032541252,0.00087329146,0.000056967372,0.009150944],"category_scores_gemma":[0.0007245082,0.00012440546,0.000017193304,0.0007922925,0.00031301184,0.00032384705,0.003422473,0.00018818559,0.0132682305],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022740984,0.00057904277,0.015978023,0.00006383131,0.000053931682,0.00016603521,0.002009144,0.0008451524,0.028307024,0.0020878175,0.7878388,0.16184378],"study_design_scores_gemma":[0.0010881666,0.00027310126,0.3619389,0.000023539642,0.000017361777,0.0000537727,0.0006868987,0.007989761,0.0007071908,0.00015881409,0.62668324,0.00037924544],"about_ca_topic_score_codex":0.000085528394,"about_ca_topic_score_gemma":0.000013646971,"teacher_disagreement_score":0.3459609,"about_ca_system_score_codex":0.00011852348,"about_ca_system_score_gemma":0.0000022884437,"threshold_uncertainty_score":0.99175483},"labels":[],"label_agreement":null},{"id":"W6969676522","doi":"10.5683/sp2/rbvhus","title":"Perrenoud Homestead -- Cochrane -- Laser Scanning -- July 20 2017","year":2021,"lang":"en","type":"dataset","venue":"Borealis","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"University of Calgary","funders":"","keywords":"Laser; Laser scanning; Data set; Data recording; Laser safety","score_opus":0.01303175596162335,"score_gpt":0.2590321210134829,"score_spread":0.24600036505185954,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6969676522","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00033063852,0.0006445855,0.000016126323,0.00020565603,0.00035657344,0.00018505628,0.98407745,0.00005179567,0.014132122],"genre_scores_gemma":[0.00009036852,0.001063844,0.00030636584,0.0007813903,0.00041856247,0.00004467623,0.9937343,0.000044002234,0.0035164962],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99732214,0.00008535489,0.00038616938,0.0007933716,0.00079294643,0.00061999017],"domain_scores_gemma":[0.99807644,0.00005411984,0.00025713787,0.0012980753,0.000019462972,0.00029475868],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00021718678,0.0004882334,0.0005850459,0.0000033648744,0.00028421462,0.00013618007,0.0008265388,0.00041859614,0.010670599],"category_scores_gemma":[0.000076705335,0.00044667334,0.000206332,0.00023640023,0.0003037899,0.00014088822,0.00060637837,0.0005248261,0.0010871094],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009175138,0.000085590545,0.00023147574,0.000044508008,0.000032813758,0.00032925108,0.000056131663,0.00015275259,0.0000150362575,5.920683e-7,0.99847364,0.0005690115],"study_design_scores_gemma":[0.00024830538,0.000055430246,0.003725269,0.00013053014,0.00010333364,0.00005186454,0.00013246281,0.000022746664,0.000026518408,0.000012493528,0.9949355,0.0005555395],"about_ca_topic_score_codex":0.040662497,"about_ca_topic_score_gemma":0.015651556,"teacher_disagreement_score":0.025010943,"about_ca_system_score_codex":0.00021787413,"about_ca_system_score_gemma":0.00007995342,"threshold_uncertainty_score":0.9997985},"labels":[],"label_agreement":null},{"id":"W6974013541","doi":"10.57757/iugg23-1225","title":"Distinction of Supercooled droplets from the Ice Crystals in Mixed-phase Cloud Regime: McGill Real-time Ice Nucleation Chamber (MRINC)","year":2023,"lang":"en","type":"article","venue":"Publication Database GFZ (GFZ German Research Centre for Geosciences)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"","keywords":"Supercooling; Ice nucleus; Aerosol; Nucleation; Ice crystals; Cirrus; Silver iodide; Condensation; Radiative transfer","score_opus":0.03310492024318838,"score_gpt":0.3250268872681018,"score_spread":0.2919219670249134,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6974013541","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":[0.98418283,0.000013239302,0.00047280538,0.008434625,0.00020445799,0.0013814569,0.0036667236,0.00011526559,0.0015285871],"genre_scores_gemma":[0.9867867,0.00024482576,0.0010598649,0.00020194634,0.00020027628,0.00030765767,0.0063807415,0.00004427605,0.0047737095],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99532413,0.0004999686,0.000630961,0.0009559168,0.0016406126,0.00094841846],"domain_scores_gemma":[0.99710804,0.0010224904,0.00025666397,0.0010968609,0.00022921496,0.00028671723],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.004563265,0.00021723613,0.0002442193,0.000044139815,0.0008667082,0.00015225791,0.0009815848,0.00010343047,0.0030022466],"category_scores_gemma":[0.0016958431,0.00017331258,0.000087939785,0.0033563909,0.0007693066,0.0012688572,0.0008032918,0.0002752473,0.00081151974],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006376139,0.0020374497,0.049161233,0.00012875273,0.000046072808,0.000022688013,0.003667637,0.00052239886,0.13328658,0.006804668,0.7609266,0.0427583],"study_design_scores_gemma":[0.0027625167,0.00022922868,0.29424077,0.000105566345,0.000033820066,0.000006591706,0.0025504401,0.14336067,0.0037542076,0.0012757105,0.5510555,0.000625014],"about_ca_topic_score_codex":0.014702666,"about_ca_topic_score_gemma":0.0026775324,"teacher_disagreement_score":0.24507953,"about_ca_system_score_codex":0.00034898223,"about_ca_system_score_gemma":0.00009754032,"threshold_uncertainty_score":0.99996644},"labels":[],"label_agreement":null},{"id":"W6976624414","doi":"10.60692/8kgrz-2cf44","title":"The topography contribution to the influence of the atmospheric boundary layer at high altitude stations","year":2017,"lang":"en","type":"article","venue":"Greater South Information System","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"","keywords":"Altitude (triangle); Effects of high altitude on humans; Lapse rate; Elevation (ballistics); Planetary boundary layer; Troposphere; Plateau (mathematics); Latitude; Boundary layer","score_opus":0.00918500696407355,"score_gpt":0.20042722454916914,"score_spread":0.1912422175850956,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6976624414","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":[0.99513793,0.0000030311146,0.0019302398,0.0007670438,0.00031081884,0.00055562274,0.000045667566,0.000026167798,0.0012234617],"genre_scores_gemma":[0.9990716,5.323657e-7,0.0001080375,0.00034107486,0.000023386881,0.00008923161,0.000002064212,0.000004512017,0.00035956956],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988412,0.000059589354,0.00036962616,0.00010149821,0.00041471334,0.00021334525],"domain_scores_gemma":[0.9985167,0.000014985924,0.00048350476,0.00087232416,0.000057820827,0.000054711923],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00037619512,0.000114281735,0.000105515945,7.760281e-7,0.002564904,0.00026557595,0.0007391215,0.000046896195,0.000050512117],"category_scores_gemma":[0.00005024758,0.00005214821,0.0000764852,0.00015977999,0.0002859035,0.00047399665,0.00040349498,0.00007180894,0.0005564876],"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":[0.000029350147,0.0000015790267,0.969389,0.000011878375,0.000022260165,1.7462611e-7,0.011877094,0.01693612,0.000023178292,0.00064709416,0.00072253024,0.00033971408],"study_design_scores_gemma":[0.00020819658,0.000018277047,0.9867247,0.000023297529,0.000014296126,0.0000033099386,0.0012999199,0.00069594773,0.00016561121,0.000006778314,0.010763657,0.00007601093],"about_ca_topic_score_codex":0.00026071924,"about_ca_topic_score_gemma":0.000040109062,"teacher_disagreement_score":0.017335672,"about_ca_system_score_codex":0.00015838747,"about_ca_system_score_gemma":0.000015884865,"threshold_uncertainty_score":0.99873364},"labels":[],"label_agreement":null},{"id":"W6976844019","doi":"10.60692/2qzc8-4k861","title":"Band-by-band spectral radiative kernels based on the ERA5 reanalysis","year":2024,"lang":"en","type":"article","venue":"Greater South Information System","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"","keywords":"Radiative transfer; Radiative flux; Kernel (algebra); Radiation; Spectral analysis; Spectral line; Broadband; Climate model","score_opus":0.012024485494228914,"score_gpt":0.1837861797514948,"score_spread":0.1717616942572659,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6976844019","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":[0.87128264,0.0000074130503,0.037414663,0.00069067825,0.00029063088,0.00039520013,0.000115758885,0.0002212543,0.08958179],"genre_scores_gemma":[0.99831545,1.722516e-7,0.00005919665,0.0005421726,0.000047924696,0.000042816457,0.000012611342,0.000009024272,0.0009706081],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9988076,0.00006464752,0.00032245816,0.00016699907,0.00042161698,0.00021665901],"domain_scores_gemma":[0.99949706,0.000022677126,0.0000990761,0.00029935778,0.000008028534,0.00007381725],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0003370941,0.00016276598,0.00014443071,0.000006448446,0.00018190277,0.00027203665,0.00018290593,0.000060524006,0.001642105],"category_scores_gemma":[0.0000086261025,0.00009357244,0.0001103195,0.0003486563,0.00006404905,0.00035694323,0.000020964833,0.00011184532,0.004435294],"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":[0.000268404,0.000028006005,0.52867675,0.0004386068,0.00051676255,0.00004394245,0.24214613,0.099869825,0.00016548992,0.0013609366,0.121781915,0.0047032465],"study_design_scores_gemma":[0.001465277,0.00037034386,0.13214608,0.0004041657,0.00028290332,0.00002812895,0.02106729,0.8057061,0.013758032,0.00001959022,0.023570562,0.0011815408],"about_ca_topic_score_codex":0.00004123694,"about_ca_topic_score_gemma":4.7260997e-7,"teacher_disagreement_score":0.70583624,"about_ca_system_score_codex":0.00025272658,"about_ca_system_score_gemma":0.000012444876,"threshold_uncertainty_score":0.99927056},"labels":[],"label_agreement":null},{"id":"W6979801638","doi":"","title":"Airstrike kills leader/ Iran sanctions waived/ Israeli soldier stabbed/ Canada elections","year":2015,"lang":"en","type":"other","venue":"Internet Archive (Internet Archive)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"State (computer science); Prime minister; Sanctions; Terrorism; George (robot); Parliament; Newspaper; Adversary","score_opus":0.012844847565632143,"score_gpt":0.2154201771186996,"score_spread":0.20257532955306745,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6979801638","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.002194081,0.0003090584,0.010027085,0.00033074242,0.0020138272,0.0009121763,0.0015738616,0.00038153268,0.98225766],"genre_scores_gemma":[0.03021565,0.00013784619,0.0022087889,0.0007844004,0.0007899032,0.00014670823,0.0007894696,0.00068163476,0.9642456],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9948742,0.00030669983,0.000807419,0.0015618233,0.0010740295,0.0013758738],"domain_scores_gemma":[0.9973804,0.00018311189,0.0005139211,0.0010362896,0.000022622145,0.0008636918],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00017144372,0.0010998878,0.0009053606,0.000047516223,0.00012899052,0.00011938482,0.0015334645,0.00026876727,0.088427916],"category_scores_gemma":[0.000080115526,0.0010357377,0.00037665316,0.00027027473,0.0010626444,0.00013139387,0.0012712842,0.0013537303,0.005071802],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000078515906,0.00017360119,0.0056524426,0.000032673368,0.00032260385,0.00008650428,0.0014466147,0.00013254404,0.0001980184,0.00015831308,0.99120486,0.000513283],"study_design_scores_gemma":[0.00067184406,0.00030390723,0.0028398058,0.00029044496,0.00012442544,0.000081180384,0.0003324787,0.001212014,0.00008990914,0.00050567876,0.9924387,0.001109631],"about_ca_topic_score_codex":0.9342695,"about_ca_topic_score_gemma":0.98921245,"teacher_disagreement_score":0.08335611,"about_ca_system_score_codex":0.000701263,"about_ca_system_score_gemma":0.00041111378,"threshold_uncertainty_score":0.9992093},"labels":[],"label_agreement":null},{"id":"W6980146957","doi":"","title":"AWS announces new Canadian cloud region in Calgary, Alberta","year":2021,"lang":"en","type":"other","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Cloud computing; Government (linguistics); Work (physics); Earth observation satellite","score_opus":0.009499581578430828,"score_gpt":0.2029073589586394,"score_spread":0.19340777738020856,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6980146957","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00021644899,0.0006017452,0.00013730626,0.0012671194,0.00038070054,0.00015119433,0.000001262429,0.000021932034,0.9972223],"genre_scores_gemma":[0.0007053992,0.0002633671,0.0009940682,0.0012919161,0.00023113535,0.000006175753,0.000028909426,0.00011433299,0.9963647],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.998818,0.000035136072,0.00014599501,0.00043499024,0.00018302907,0.00038287195],"domain_scores_gemma":[0.9992594,0.0000141663295,0.00005808272,0.00033003624,0.0000010971443,0.00033718662],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000046731588,0.00021881414,0.00022703207,0.0000032190114,0.00003328928,0.000025860223,0.00027870692,0.00028988128,0.12479675],"category_scores_gemma":[0.000010744375,0.00019082155,0.0000537097,0.0002187244,0.0000810783,0.000024066912,0.00009089385,0.00015063748,0.00077736005],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[8.391718e-7,0.00000939923,0.018067027,0.00000369974,0.000005505537,0.00009095566,0.00006492364,0.000009510679,0.0000022509053,0.00019184095,0.97624993,0.0053041065],"study_design_scores_gemma":[0.00010638352,0.000011747142,0.0027869968,0.000053879732,0.0000046002033,0.000008538079,0.0000634905,0.000060344068,0.0000015127856,0.000050999548,0.9965909,0.00026057666],"about_ca_topic_score_codex":0.98968214,"about_ca_topic_score_gemma":0.99784,"teacher_disagreement_score":0.124019384,"about_ca_system_score_codex":0.000307111,"about_ca_system_score_gemma":0.0001696544,"threshold_uncertainty_score":0.99916506},"labels":[],"label_agreement":null},{"id":"W6980407345","doi":"","title":"CALIPSO and the field campaigns: a convergence of interest for the study of clouds and aerosols","year":2024,"lang":"en","type":"article","venue":"HAL (Le Centre pour la Communication Scientifique Directe)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Université du Québec à Montréal","funders":"","keywords":"Convergence (economics); Field (mathematics); Lidar; Atmosphere (unit); Trajectory; Atmospheric model","score_opus":0.015530172123287923,"score_gpt":0.2385296428505644,"score_spread":0.2229994707272765,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6980407345","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":[0.96836257,0.0009367672,0.024332063,0.0042922148,0.00006642398,0.0005202722,0.0000065563154,0.000016017655,0.001467138],"genre_scores_gemma":[0.9976271,0.00022845143,0.0008949778,0.0000777011,0.000004443265,0.000045563946,0.0000012373035,0.0000072174307,0.0011133443],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99877834,0.0005829901,0.00021597296,0.0002030872,0.000117422846,0.00010216137],"domain_scores_gemma":[0.996274,0.0030850063,0.00009215056,0.000449875,0.0000634891,0.00003551117],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020584422,0.000082598235,0.00012964182,0.0000019201896,0.0001628902,0.000054140284,0.00033341718,0.000032961034,0.00014756217],"category_scores_gemma":[0.00045132957,0.00004849683,0.00004363014,0.00016793881,0.0005282881,0.00005580577,0.00034013944,0.00009160628,0.0000021029898],"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":[0.00041055988,0.00174369,0.2277303,0.0005034583,0.00047839593,0.000004834247,0.2778526,0.00024828914,0.014410019,0.2798812,0.010310414,0.18642622],"study_design_scores_gemma":[0.0108949095,0.000090432244,0.15483916,0.0027715086,0.00091662054,0.00005484495,0.060098615,0.58433175,0.10878023,0.021807274,0.053873986,0.0015406761],"about_ca_topic_score_codex":0.0019085899,"about_ca_topic_score_gemma":0.0023193003,"teacher_disagreement_score":0.58408344,"about_ca_system_score_codex":0.0000104967085,"about_ca_system_score_gemma":0.000012124473,"threshold_uncertainty_score":0.28852296},"labels":[],"label_agreement":null},{"id":"W6980681019","doi":"","title":"Comparison of simulated and observed horizontal inhomogeneities of optical thickness of Arctic stratus","year":2019,"lang":"en","type":"other","venue":"Qucosa (Saxon State and University Library Dresden)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Arctic; Radiance; Cloud top; The arctic; Spatial distribution; Dropsonde; Homogeneous; Atmospheric model","score_opus":0.016379259144000083,"score_gpt":0.21531240265855822,"score_spread":0.19893314351455815,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6980681019","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":[0.8922956,0.00058472384,0.000044247256,0.000028171171,0.00005506302,0.0002370448,0.00019995219,0.000019634877,0.10653554],"genre_scores_gemma":[0.8772095,0.0005374364,0.0006830865,0.000008761508,0.000008651528,8.92463e-8,0.000031397896,0.000050097413,0.121471],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990046,0.00006491924,0.00023919753,0.00028599447,0.00022593822,0.00017933465],"domain_scores_gemma":[0.99928373,0.00006679976,0.00032157847,0.00021799016,0.0000066818047,0.00010319909],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000035227862,0.00021108199,0.0005845101,0.000012934065,0.0000347641,0.000010092508,0.000209094,0.00021412152,0.0016065225],"category_scores_gemma":[0.0000033504066,0.00020696003,0.00006976281,0.00016383079,0.00065363635,0.00025911856,0.0003888221,0.0001572879,0.000008489206],"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":[0.00090378267,0.00054255105,0.96395683,0.0015193331,0.00041016008,0.00004917092,0.0024984672,0.0005644293,0.003121686,0.0027889682,0.018728474,0.004916158],"study_design_scores_gemma":[0.011560629,0.0065856786,0.63785803,0.0027929456,0.0013845967,0.000025166171,0.03287254,0.0048645944,0.021020664,0.0009868125,0.27634105,0.0037072832],"about_ca_topic_score_codex":0.0012824012,"about_ca_topic_score_gemma":0.00021502089,"teacher_disagreement_score":0.32609877,"about_ca_system_score_codex":0.000015156165,"about_ca_system_score_gemma":0.000037609818,"threshold_uncertainty_score":0.99930614},"labels":[],"label_agreement":null},{"id":"W6980814869","doi":"","title":"Cross-cultural influences on corrective feedback preferences in English language instruction","year":2007,"lang":"en","type":"dissertation","venue":"eScholarship@McGill (McGill)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"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":"Corrective feedback; Statistical analysis; Descriptive statistics; English language; Language proficiency; English as a second language; Preference","score_opus":0.010424946102832029,"score_gpt":0.27013048583042754,"score_spread":0.2597055397275955,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6980814869","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":[0.75594187,0.000052234074,2.9703747e-8,0.0000013676639,0.0018337868,0.0004178512,0.00017760207,0.00015204256,0.2414232],"genre_scores_gemma":[0.9927995,0.0000780107,0.00027108815,0.00017036076,0.00007820875,0.00009772181,0.00039553834,0.00006557266,0.006043996],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99605876,0.0001883112,0.00078883424,0.0011030373,0.0010863822,0.00077465357],"domain_scores_gemma":[0.99845576,0.00014117999,0.0005659792,0.000449143,0.00013390408,0.00025401163],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0005575488,0.00073062786,0.00056609005,0.00003224937,0.00068662583,0.00020997525,0.0007364365,0.0008912724,0.0024791046],"category_scores_gemma":[0.0007564932,0.0006624456,0.00020853434,0.0009217146,0.00028773575,0.0020323836,0.00014897384,0.0016715882,0.0008738056],"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":[0.0013125818,0.00046354733,0.050001897,0.00014794905,0.00013653851,0.000103653634,0.0014230073,0.0018417826,0.010380175,0.00293548,0.000023115017,0.93123025],"study_design_scores_gemma":[0.002117561,0.000636261,0.9062736,0.0005637119,0.00010325706,0.000016711238,0.017585747,0.000026005304,0.04751587,0.002913763,0.01999446,0.0022530472],"about_ca_topic_score_codex":0.004917049,"about_ca_topic_score_gemma":0.011613261,"teacher_disagreement_score":0.92897725,"about_ca_system_score_codex":0.0013251627,"about_ca_system_score_gemma":0.000022384933,"threshold_uncertainty_score":0.99990416},"labels":[],"label_agreement":null},{"id":"W6984732552","doi":"","title":"Machine","year":2000,"lang":"en","type":"other","venue":"Library and Archives Canada (Government of Canada)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Process (computing); Work (physics); Set (abstract data type); Identification (biology); Troubleshooting","score_opus":0.001492640881456211,"score_gpt":0.12213273254975117,"score_spread":0.12064009166829495,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6984732552","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00051031413,0.0005056297,0.000017531274,0.00063144165,0.00010698602,0.0001100336,0.00022494548,0.000016230457,0.9978769],"genre_scores_gemma":[0.054262847,0.00061132666,0.0010059177,0.0013292766,0.00006230377,0.0000045376873,0.000010648268,0.00012901424,0.94258416],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99811745,0.000024323941,0.00016473464,0.00026707948,0.0011759535,0.00025048706],"domain_scores_gemma":[0.9994119,0.00003110806,0.00012603353,0.00021757708,9.283058e-9,0.00021339547],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00000233885,0.0002245103,0.00024083882,0.0000010291491,0.00006694435,0.000008349689,0.00024815014,0.00004511782,0.016176429],"category_scores_gemma":[2.7901177e-7,0.0002009152,0.000024575907,0.00005018859,0.000120186785,0.00006626886,0.00016895364,0.0001188029,4.144559e-8],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016219105,0.000047405916,0.051334206,0.00012086325,0.000105518695,0.00017176781,0.000033913504,0.000094290706,0.001099267,0.0049561295,0.8845311,0.057343375],"study_design_scores_gemma":[0.0001371801,0.00002437094,0.008790722,0.000053175212,0.0000137418065,0.0000033345302,0.00007870941,0.0002570578,0.0007399495,0.00013186649,0.98951846,0.00025143445],"about_ca_topic_score_codex":0.03011479,"about_ca_topic_score_gemma":0.13801533,"teacher_disagreement_score":0.10790053,"about_ca_system_score_codex":0.0000040865334,"about_ca_system_score_gemma":0.0002225304,"threshold_uncertainty_score":0.9847229},"labels":[],"label_agreement":null},{"id":"W7000595187","doi":"","title":"Field campaign data analysis in support of the future FORUM and CAIRT ESA missions","year":2023,"lang":"en","type":"article","venue":"AMS Degree Thesis (University of Bologna)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Identification (biology); Code (set theory); Radiance; Field (mathematics); Set (abstract data type); Focus (optics); Component (thermodynamics); Satellite","score_opus":0.020488277877844106,"score_gpt":0.21269902694477746,"score_spread":0.19221074906693336,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7000595187","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":[0.9922198,0.000019103427,0.00036155956,0.004922755,0.000027868955,0.000073021045,0.000035787096,0.000012345458,0.002327767],"genre_scores_gemma":[0.9973492,0.00011426974,0.000799001,0.0001354999,0.000004765944,1.0997664e-7,0.000010038869,0.0000031308543,0.0015839827],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99933624,0.00004845717,0.00007921879,0.00022211837,0.00015808523,0.00015588914],"domain_scores_gemma":[0.9992345,0.00008423358,0.00008908254,0.00054156187,0.000004367461,0.000046267236],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001536973,0.00006979193,0.00018686842,0.000008281884,0.000116311974,0.0000024449487,0.00064207456,0.000080335536,0.0012821961],"category_scores_gemma":[0.000019758783,0.000056815374,0.00007536674,0.00087194785,0.00022911683,0.00010946996,0.000905514,0.00007960258,0.000016659133],"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":[0.00002484978,0.000029948435,0.9651449,0.000004911179,0.00006839662,0.000012431009,0.00082243414,0.00013482597,0.00054627704,0.00005052831,0.019354817,0.013805715],"study_design_scores_gemma":[0.0001675022,0.00005769622,0.977388,0.0000053523677,0.00018381422,0.0000012997181,0.014118998,0.0018566935,0.00013722853,0.00018188027,0.0058096377,0.000091874426],"about_ca_topic_score_codex":0.0023218815,"about_ca_topic_score_gemma":0.013611056,"teacher_disagreement_score":0.01371384,"about_ca_system_score_codex":0.000018212857,"about_ca_system_score_gemma":0.000012366762,"threshold_uncertainty_score":0.99963075},"labels":[],"label_agreement":null},{"id":"W7001764475","doi":"","title":"Le(s) Nord(s) imaginaire(s)","year":2004,"lang":"fr","type":"other","venue":"OpenEdition (OpenEdition)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Identity (music); Presentation (obstetrics); Period (music)","score_opus":0.006898079283914752,"score_gpt":0.21288629305708756,"score_spread":0.2059882137731728,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7001764475","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0016236873,0.0011801984,0.014757865,0.063248225,0.004999341,0.0016954229,0.0005446228,0.0002721171,0.9116785],"genre_scores_gemma":[0.18536106,0.0017206467,0.010119047,0.042183515,0.0029607737,0.000820057,0.0015198558,0.000697504,0.7546175],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.99394804,0.00027327257,0.0010888773,0.0019049204,0.001422972,0.0013619236],"domain_scores_gemma":[0.9968096,0.00012636647,0.0008715676,0.0012923714,0.000092131595,0.0008079648],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00042621515,0.0012749025,0.0010422084,0.000024544883,0.0011196095,0.0004989585,0.0015041173,0.0009355148,0.4981279],"category_scores_gemma":[0.00011548758,0.00139689,0.0005258461,0.0007759027,0.0016938327,0.008949082,0.000759335,0.0008940652,0.14335503],"study_design_candidate":"not_applicable","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":[0.00011719529,0.0017634138,0.001240614,0.0003441506,0.000280569,0.00069186644,0.00024479747,0.003789129,0.0011737519,0.6427113,0.2945443,0.053098906],"study_design_scores_gemma":[0.002136825,0.0003347266,0.059249982,0.00083669083,0.00020543819,0.00015264387,0.0002258445,0.00012843312,0.0008623624,0.005440375,0.92859274,0.001833925],"about_ca_topic_score_codex":0.0037702546,"about_ca_topic_score_gemma":0.021241544,"teacher_disagreement_score":0.6372709,"about_ca_system_score_codex":0.0013791191,"about_ca_system_score_gemma":0.0008090549,"threshold_uncertainty_score":0.99977255},"labels":[],"label_agreement":null},{"id":"W7006300463","doi":"","title":"The turbulent structure of the clear and cloud-topped convective boundary layer over land","year":2013,"lang":"en","type":"dissertation","venue":"eScholarship@McGill (McGill)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"","keywords":"Boundary layer; Convection; Turbulence; Convective Boundary Layer; Free convective layer; Planetary boundary layer","score_opus":0.00564813037050291,"score_gpt":0.20492266881158067,"score_spread":0.19927453844107776,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7006300463","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":[0.9824804,0.00029600662,4.3373447e-8,0.000045959816,0.0012546412,0.0007320911,0.00029169742,0.00003525912,0.014863899],"genre_scores_gemma":[0.9917022,0.0002055327,0.00007427042,0.0003840885,0.000052084797,0.00003181935,0.000051862437,0.00007287946,0.007425247],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9972885,0.0002693682,0.0005135095,0.0006156232,0.0008139148,0.000499077],"domain_scores_gemma":[0.9983035,0.00015553976,0.0005750164,0.00072473416,0.00006600218,0.00017525846],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002610064,0.00051460124,0.0004318685,0.0000044844364,0.0016195335,0.00012927338,0.00075761875,0.00051613076,0.0018007071],"category_scores_gemma":[0.00015024141,0.00030928437,0.0002210793,0.00026851852,0.00042407686,0.0004004105,0.00034953005,0.0011158503,0.00012792545],"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":[0.00361742,0.00079731055,0.061270352,0.00095780694,0.0025443025,0.0000747823,0.0009924427,0.0007360831,0.5136703,0.07265161,0.0033896677,0.3392979],"study_design_scores_gemma":[0.0017085782,0.00034897446,0.50020534,0.00023569932,0.00041055054,0.00004595789,0.0012861297,0.00008128902,0.055735383,0.025946721,0.4125032,0.0014921651],"about_ca_topic_score_codex":0.0016020883,"about_ca_topic_score_gemma":0.002458292,"teacher_disagreement_score":0.45793495,"about_ca_system_score_codex":0.00033325117,"about_ca_system_score_gemma":0.000027248638,"threshold_uncertainty_score":0.9999359},"labels":[],"label_agreement":null},{"id":"W7006594793","doi":"","title":"Validation radiométrique du \"Far Infrared Radiometer\" et évaluation de sa sensibilité à l'état de l'atmosphère Arctique","year":2019,"lang":"fr","type":"other","venue":"Archipelago (University of Quebec in Montreal)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Meteorological satellite; Water ice; Thermal infrared; Earth observation satellite","score_opus":0.007679761457295746,"score_gpt":0.1982005689341722,"score_spread":0.19052080747687647,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7006594793","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":[0.90831697,0.0002608463,0.04065476,0.0014083522,0.0001894107,0.0010593695,0.0000567304,0.000051335217,0.048002202],"genre_scores_gemma":[0.6939729,0.0024414447,0.050596133,0.0003556413,0.00010366808,0.0000039121255,0.00013858447,0.00014913842,0.25223857],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9959569,0.0014650384,0.0004304434,0.00085919426,0.0005445616,0.0007438687],"domain_scores_gemma":[0.9978457,0.00047922618,0.0005972271,0.0007605066,0.000037536225,0.00027979174],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014329549,0.00052027986,0.00077459746,0.000044032648,0.00017321504,0.0000381941,0.00070285355,0.000696362,0.0050091376],"category_scores_gemma":[0.00015758855,0.00066127867,0.00032666416,0.0006411046,0.00065605476,0.00041214502,0.00033911318,0.0006461821,0.00053202343],"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":[0.0005540433,0.0007708571,0.22017275,0.0003927644,0.0002768969,0.0003536534,0.13089801,0.0657242,0.010482114,0.0038630592,0.0046202596,0.5618914],"study_design_scores_gemma":[0.002195464,0.00025523102,0.9272256,0.00036979048,0.00018143584,0.000049907063,0.009253942,0.042673513,0.00024485684,0.011156515,0.005636861,0.0007568993],"about_ca_topic_score_codex":0.6734115,"about_ca_topic_score_gemma":0.7626513,"teacher_disagreement_score":0.7070528,"about_ca_system_score_codex":0.0018734498,"about_ca_system_score_gemma":0.00054683955,"threshold_uncertainty_score":0.99958384},"labels":[],"label_agreement":null},{"id":"W7008054511","doi":"","title":"Analysis of Water Content Profiles in Arctic Mixed-Phase Clouds during VERDI","year":2016,"lang":"en","type":"other","venue":"Qucosa (Saxon State and University Library Dresden)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Nucleofection; Gestational period; Diafiltration; Proteogenomics; TSG101; Articular cartilage damage; Fusible alloy; Liquation; Dysgeusia","score_opus":0.009300715249274059,"score_gpt":0.19964288101341415,"score_spread":0.1903421657641401,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7008054511","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8999111,0.000116814095,0.00006237483,0.00014378349,0.00007163137,0.0002627074,0.00028916518,0.000052037532,0.09909039],"genre_scores_gemma":[0.39546522,0.0007830004,0.00013561672,0.000034251763,0.000020661437,0.00000101216,0.00006772636,0.00006634807,0.60342616],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9986657,0.00009499462,0.00021290721,0.0004602872,0.00022091332,0.00034518365],"domain_scores_gemma":[0.99938554,0.00001965249,0.00015742517,0.00028793648,0.0000033041088,0.00014612086],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000050431518,0.0002605048,0.0005075835,0.00005023453,0.00006659234,0.000019161174,0.0002740329,0.00015397817,0.021284984],"category_scores_gemma":[0.0000015356158,0.00019653025,0.00015139717,0.00033761217,0.0002969668,0.00037735017,0.0004936435,0.00013375207,0.00016348576],"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":[0.0015240636,0.0009042905,0.8940234,0.00049572554,0.0025137053,0.0012836982,0.0028869992,0.0001564112,0.005264196,0.00033960264,0.077972434,0.012635425],"study_design_scores_gemma":[0.008034812,0.00042315436,0.29607397,0.00055327656,0.0015189825,0.000006682386,0.0027257062,0.00027566776,0.0067102895,0.00014982896,0.6817199,0.0018077146],"about_ca_topic_score_codex":0.0012859702,"about_ca_topic_score_gemma":0.00071027543,"teacher_disagreement_score":0.6037475,"about_ca_system_score_codex":0.000072138304,"about_ca_system_score_gemma":0.000014723491,"threshold_uncertainty_score":0.97960967},"labels":[],"label_agreement":null},{"id":"W7014866292","doi":"","title":"Reevaluierung und Erweiterung des Messverfahrens FRIDGE zur Bestimmung von Depositions-, Kondensations- und Immersionsgefrierkernen","year":2016,"lang":"de","type":"dissertation","venue":"Publication Server of Goethe University Frankfurt am Main (Goethe University Frankfurt)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Statistical analysis; High strength steel","score_opus":0.010983395721202336,"score_gpt":0.2317107902448073,"score_spread":0.220727394523605,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7014866292","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":[0.9278833,0.0032902295,0.028407011,0.0042454675,0.0015895137,0.00294252,0.0023188998,0.0004971448,0.028825898],"genre_scores_gemma":[0.88091105,0.0057049105,0.009865512,0.00036722052,0.0003021368,0.0000073428996,0.0035775665,0.00027141607,0.09899282],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9902231,0.0017418315,0.0014318662,0.0024859966,0.0023785406,0.0017386511],"domain_scores_gemma":[0.99138445,0.0011322624,0.002450747,0.002721805,0.0012394007,0.0010713153],"candidate_categories":["metaepi_narrow","sts","research_integrity","insufficient_payload"],"consensus_categories":["metaepi_narrow","sts","insufficient_payload"],"category_scores_codex":[0.0019082547,0.0016044517,0.0016654782,0.00036595392,0.0040180073,0.00025586336,0.0041087414,0.0018769548,0.008949071],"category_scores_gemma":[0.00039560866,0.0018094113,0.0013028056,0.0034449843,0.0029433002,0.0031724288,0.0013836189,0.0015952371,0.002207973],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.01658814,0.012186493,0.35760105,0.0050048917,0.029428644,0.001573104,0.12620321,0.007295048,0.16938734,0.07899358,0.11488363,0.08085486],"study_design_scores_gemma":[0.016372671,0.0012585034,0.59563965,0.003265873,0.015280988,0.00006443317,0.054263785,0.005819172,0.010169427,0.0034031942,0.28654525,0.0079170745],"about_ca_topic_score_codex":0.009773631,"about_ca_topic_score_gemma":0.0013501598,"teacher_disagreement_score":0.23803858,"about_ca_system_score_codex":0.0038746987,"about_ca_system_score_gemma":0.0009238652,"threshold_uncertainty_score":0.9999493},"labels":[],"label_agreement":null},{"id":"W7024048630","doi":"","title":"Province of Upper Canada Grant (vellum) to Abraham Huff of the District of Niagara","year":2016,"lang":"en","type":"other","venue":"Brock University Digital Repository (Brock University)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Crown (dentistry); Seal (emblem); Quarter (Canadian coin); West virginia; Channel (broadcasting)","score_opus":0.0036338271955412677,"score_gpt":0.1504424563455783,"score_spread":0.14680862915003703,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7024048630","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.099973425,0.000031960608,0.0006464424,0.0000087396,0.00029299082,0.0005425594,0.00056874944,0.000046249766,0.8978889],"genre_scores_gemma":[0.12443913,0.000019339968,0.00006563979,0.0000104924475,0.000021812064,6.944864e-8,0.000004097151,0.00005402475,0.8753854],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99830717,0.000053406613,0.00024667743,0.00046480395,0.0006258214,0.0003021004],"domain_scores_gemma":[0.9984528,0.000049262373,0.00062961335,0.0006215639,0.000044119406,0.00020265026],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0000023051534,0.00031463554,0.00045192716,0.000027397384,0.00012719563,0.0000090280055,0.0012807975,0.00020207737,0.00019032425],"category_scores_gemma":[0.000017026334,0.00026977243,0.00026145508,0.00050780893,0.0004371373,0.00021057812,0.0010636147,0.00013357145,0.000017641369],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014346233,0.00017093444,0.11440217,0.00011586985,0.00013704407,0.000053547315,0.000016418991,0.00013184918,0.008513726,0.00004897245,0.8754582,0.0008078262],"study_design_scores_gemma":[0.0004999368,0.0001261669,0.026581507,0.00029216864,0.00012004639,0.000008855248,0.0011807419,6.527124e-7,0.0021531535,0.0000037737248,0.96860874,0.000424258],"about_ca_topic_score_codex":0.0717094,"about_ca_topic_score_gemma":0.12632853,"teacher_disagreement_score":0.093150556,"about_ca_system_score_codex":0.00066745176,"about_ca_system_score_gemma":0.00041325475,"threshold_uncertainty_score":0.99997544},"labels":[],"label_agreement":null},{"id":"W7024051405","doi":"","title":"Pemberdayaan dan Modal Sosial Perempuan Pedagang Melalui Program KUR Mikro di Kota Surabaya","year":2019,"lang":"id","type":"dissertation","venue":"Universitas Airlangga Repository (Universitas Airlangga)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Universitas Airlangga; Universitas Indonesia; Thompson Rivers University","keywords":"Homogeneous; Order (exchange)","score_opus":0.006025321401848517,"score_gpt":0.21161917809122693,"score_spread":0.2055938566893784,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7024051405","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":[0.78404343,0.0014052971,0.00017335275,0.00024478472,0.0039179665,0.0026716662,0.0002525621,0.0007544158,0.20653653],"genre_scores_gemma":[0.8973794,0.00026366545,0.0010945561,0.000112813286,0.0006847547,0.000022774286,0.0025077225,0.0003580341,0.09757628],"study_design_codex":"observational","study_design_gemma":"qualitative","domain_scores_codex":[0.98950636,0.0006724251,0.0011006389,0.0034420267,0.0027063577,0.0025721863],"domain_scores_gemma":[0.9940541,0.0001798826,0.0016213126,0.0023420025,0.00034506878,0.0014576644],"candidate_categories":["metaepi_narrow","sts","research_integrity","insufficient_payload"],"consensus_categories":["metaepi_narrow","insufficient_payload"],"category_scores_codex":[0.00042557655,0.002369351,0.002058734,0.00016193217,0.0030515792,0.00055001955,0.0031638145,0.002133511,0.007458278],"category_scores_gemma":[0.000039673843,0.0027774414,0.0017320494,0.0015921246,0.0010423274,0.0021438643,0.0013509747,0.0022194511,0.0024390714],"study_design_candidate":"qualitative","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":[0.008872594,0.011321144,0.43968058,0.0036260204,0.008109863,0.0300904,0.089859664,0.011227008,0.0617833,0.008248041,0.29153067,0.035650715],"study_design_scores_gemma":[0.0093957335,0.0056065056,0.2469403,0.0013397295,0.007336896,0.0008497061,0.61708426,0.014485853,0.0020949852,0.000043349726,0.08551807,0.009304621],"about_ca_topic_score_codex":0.0047159325,"about_ca_topic_score_gemma":0.00060417596,"teacher_disagreement_score":0.5272246,"about_ca_system_score_codex":0.0036535845,"about_ca_system_score_gemma":0.0007130852,"threshold_uncertainty_score":0.99916196},"labels":[],"label_agreement":null},{"id":"W7024287635","doi":"","title":"Qualitative knowledge of filtering facepiece respirators for filtration performance tests during the COVID-19 pandemic","year":2020,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institut de recherche Robert-Sauvé en santé et en sécurité du travail; Concordia University","funders":"Institut de Recherche Robert-Sauvé en Santé et en Sécurité du Travail","keywords":"Respirator; Pandemic; Filtration (mathematics); Coronavirus disease 2019 (COVID-19); Pressure drop","score_opus":0.09089527013681349,"score_gpt":0.3519784476407039,"score_spread":0.26108317750389043,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7024287635","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":[0.9824997,0.0000316352,0.014858731,0.00051163195,0.000026065096,0.00028720035,0.0000071736386,0.000042013147,0.0017358079],"genre_scores_gemma":[0.9971217,0.000013793774,0.0014228796,0.00073695305,0.000031823314,0.0000449153,0.0000015762279,0.000008670813,0.00061770476],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99929285,0.000054048043,0.00020449406,0.00019259487,0.00010291323,0.00015307091],"domain_scores_gemma":[0.9994785,0.00020886607,0.00009055883,0.00011437179,0.0000074642576,0.00010024136],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026635724,0.00009254165,0.000105029045,6.419934e-7,0.0001887521,0.0000102748045,0.00018429662,0.000034090695,0.00082382775],"category_scores_gemma":[0.00020817279,0.00006223567,0.000042939893,0.00017397641,0.0001376784,0.0001303409,0.00009751384,0.00006249769,0.00004888545],"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":[0.00023415145,0.00008279652,0.5229009,0.0003742566,0.000031723404,5.32886e-7,0.14622153,0.021181354,0.2972284,0.00023518,0.0044991774,0.0070100613],"study_design_scores_gemma":[0.0052005765,0.0027345102,0.56311786,0.0000900188,0.000092560316,0.00001987611,0.07186205,0.104944736,0.10943462,0.0005851829,0.140079,0.0018390141],"about_ca_topic_score_codex":0.000065816435,"about_ca_topic_score_gemma":0.00008195588,"teacher_disagreement_score":0.18779376,"about_ca_system_score_codex":0.00009006579,"about_ca_system_score_gemma":0.000019998175,"threshold_uncertainty_score":0.90203357},"labels":[],"label_agreement":null},{"id":"W7024299052","doi":"","title":"The role of Health Technology Assessment in reimbursement decisions and pricing of new medicines across diverse healthcare systems","year":2025,"lang":"en","type":"other","venue":"BCU Open Access Repository (Birmingham City University)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Reimbursement; Health technology; Negotiation; Health care; Monopoly; Technology assessment; Healthcare system; Public health","score_opus":0.0300377477838842,"score_gpt":0.3434050053170761,"score_spread":0.3133672575331919,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7024299052","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.1660985,0.008928178,0.0026929888,0.0025666151,0.0014820824,0.005861245,0.00008568639,0.0001521158,0.8121326],"genre_scores_gemma":[0.68422914,0.002686879,0.0012128311,0.000055691115,0.00004268453,0.000008873916,0.000006112121,0.00006665844,0.31169114],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9981173,0.0001730745,0.0005001523,0.0005095763,0.00037507628,0.00032479118],"domain_scores_gemma":[0.9981801,0.00010214589,0.0009887211,0.00058122893,0.00002894297,0.00011884289],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040534424,0.00022472935,0.0006320906,0.00004239591,0.0004287031,0.00009453624,0.0019496633,0.0002257125,0.00006601644],"category_scores_gemma":[0.000032953183,0.00018797535,0.000050555343,0.0009014675,0.00041632532,0.00020169656,0.0040618656,0.00028630227,7.673792e-7],"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":[0.00006472934,0.00017534061,0.9089562,0.0001772417,0.000121515746,0.00005660214,0.00078646315,0.00024142429,0.000121386445,0.0028137458,0.016257452,0.07022785],"study_design_scores_gemma":[0.002035475,0.00039773044,0.14481822,0.0042772605,0.000110380475,0.000015704056,0.06518021,0.0003303772,0.0002529231,0.00031524885,0.78161925,0.00064722414],"about_ca_topic_score_codex":0.14940554,"about_ca_topic_score_gemma":0.013035193,"teacher_disagreement_score":0.7653618,"about_ca_system_score_codex":0.00052149006,"about_ca_system_score_gemma":0.00048343837,"threshold_uncertainty_score":0.85625863},"labels":[],"label_agreement":null},{"id":"W7024353373","doi":"","title":"(Rebroadcast) August 12, 2024 Kalamazoo City Commission Regular Business Meeting","year":2024,"lang":"en","type":"other","venue":"Internet Archive (Internet Archive)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Commission; Government (linguistics); Quarter (Canadian coin)","score_opus":0.01065930286069827,"score_gpt":0.22476362973205335,"score_spread":0.21410432687135508,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7024353373","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0020359817,0.00070182007,0.008901578,0.00022588224,0.0022251832,0.0007802728,0.00028816226,0.0006280501,0.98421305],"genre_scores_gemma":[0.01634024,0.00021420298,0.005907754,0.0002722317,0.0009657592,0.00009021385,0.00026017093,0.0011029273,0.9748465],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9946527,0.00033002294,0.00090565014,0.00200689,0.0009716485,0.001133117],"domain_scores_gemma":[0.9975896,0.00013956339,0.0005347312,0.0011692031,0.0000136403605,0.0005532907],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00033365045,0.0012673236,0.001016946,0.000058267506,0.000067444766,0.00027709696,0.0019323705,0.00038959397,0.1323856],"category_scores_gemma":[0.00009207444,0.0010935899,0.0005589825,0.0003368155,0.00092270604,0.00012882888,0.0038756747,0.0014386605,0.020324219],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000114946495,0.00016294382,0.0045519294,0.00025395834,0.00027079918,0.00035094225,0.0012782507,0.00004948749,0.0006717833,0.00027623968,0.9908441,0.0011746652],"study_design_scores_gemma":[0.0004620425,0.00017593871,0.002234719,0.0030658746,0.0001742459,0.00010439823,0.00015091705,0.0027463387,0.00020273493,0.0021317971,0.9873563,0.0011947046],"about_ca_topic_score_codex":0.046721768,"about_ca_topic_score_gemma":0.021058947,"teacher_disagreement_score":0.11206138,"about_ca_system_score_codex":0.00022280247,"about_ca_system_score_gemma":0.000050665447,"threshold_uncertainty_score":0.9991514},"labels":[],"label_agreement":null},{"id":"W7024411286","doi":"","title":"A search for heavy Higgs bosons decaying into vector&#13;\\nbosons in same-sign two-lepton final states in pp&#13;\\ncollisions at √s = 13 TeV with the ATLAS detector","year":2023,"lang":"en","type":"article","venue":"UCL Discovery (University College London)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Fundação para a Ciência e a Tecnologia; Institut National de Physique Nucléaire et de Physique des Particules; Agencia Nacional de Promoción Científica y Tecnológica; Science and Technology Facilities Council; Natural Sciences and Engineering Research Council of Canada; Agencia Nacional de Investigación y Desarrollo; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; Javna Agencija za Raziskovalno Dejavnost RS; Max-Planck-Gesellschaft; Israel Science Foundation; Centre National pour la Recherche Scientifique et Technique; Bundesministerium für Wissenschaft, Forschung und Wirtschaft; Ministry of Education, Culture, Sports, Science and Technology; Nederlandse Organisatie voor Wetenschappelijk Onderzoek; Austrian Science Fund; Centre National de la Recherche Scientifique; Bundesministerium für Bildung und Forschung; Ministerstvo Školství, Mládeže a Tělovýchovy; British Columbia Knowledge Development Fund; Türkiye Enerji, Nükleer ve Maden Araştırma Kurumu; Danmarks Grundforskningsfond; CERN; Japan Society for the Promotion of Science; Conselho Nacional de Desenvolvimento Científico e Tecnológico; U.S. Department of Energy; National Natural Science Foundation of China; National Science Foundation; Compute Canada; Ministerio de Ciencia e Innovación; Canarie; Fundação de Amparo à Pesquisa do Estado de São Paulo","keywords":"Higgs boson; Boson; Large Hadron Collider; Vector boson; Standard Model (mathematical formulation); Lepton; Atlas (anatomy); ATLAS experiment; Luminosity; Scalar boson","score_opus":0.012971888540810677,"score_gpt":0.2239016037910045,"score_spread":0.2109297152501938,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7024411286","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":[0.99340403,0.00005119146,0.0012959202,0.0029409297,0.00009895192,0.0012321587,0.00035868966,0.000088276625,0.00052987074],"genre_scores_gemma":[0.9902454,0.00011490386,0.0006412307,0.00014097214,0.00003303896,0.00003820267,0.00004448612,0.000046179688,0.008695587],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9972381,0.00020486955,0.00023902775,0.00078707957,0.00059032725,0.0009405907],"domain_scores_gemma":[0.99852103,0.00064374163,0.00011330517,0.00048413174,0.00002309095,0.00021470306],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00041957083,0.0003610134,0.0004174984,0.00004094033,0.0011181476,0.00008222353,0.000762397,0.00013549396,0.00043214078],"category_scores_gemma":[0.000033043234,0.00030630533,0.0001723193,0.0027660658,0.0005039456,0.00089004147,0.0009018487,0.00038932412,0.00023337739],"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":[0.0028788052,0.0004065213,0.859384,0.00006398162,0.00007593397,0.00059323135,0.00834458,0.10049681,0.0054806536,0.00064263406,0.020509345,0.0011234934],"study_design_scores_gemma":[0.010624429,0.001469179,0.8149765,0.00028256653,0.00014046664,0.00003407607,0.054481067,0.09505286,0.005014908,0.00052787224,0.015671346,0.0017247171],"about_ca_topic_score_codex":0.021451015,"about_ca_topic_score_gemma":0.19071056,"teacher_disagreement_score":0.16925955,"about_ca_system_score_codex":0.0014631632,"about_ca_system_score_gemma":0.00018647609,"threshold_uncertainty_score":0.9999389},"labels":[],"label_agreement":null},{"id":"W7024490656","doi":"","title":"Search for ZH -&gt; l(+)l(-)b(b)over-bar production in 9.7 fb(-1) of p(p)over-bar collisions with the D0 detector","year":2013,"lang":"en","type":"article","venue":"Figshare","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Science and Technology Facilities Council; Natural Sciences and Engineering Research Council of Canada; Fundação para o Desenvolvimento da UNESP; Centre National de la Recherche Scientifique; Institut National de Physique Nucléaire et de Physique des Particules; Vetenskapsrådet; Conselho Nacional de Desenvolvimento Científico e Tecnológico; Bundesministerium für Bildung und Forschung; Russian Foundation for Basic Research; Fundação Carlos Chagas Filho de Amparo à Pesquisa do Estado do Rio de Janeiro; Korea Science and Engineering Foundation; Department of Science and Technology, Ministry of Science and Technology, India; Grantová Agentura České Republiky; Federal Agency for Science and Innovation; Deutsche Forschungsgemeinschaft; Secretaría de Ciencia y Técnica, Universidad de Buenos Aires; National Science Foundation; Science Foundation Ireland; Departamento Administrativo de Ciencia, Tecnología e Innovación (COLCIENCIAS); Fermilab; Consejo Nacional de Investigaciones Científicas y Técnicas; Fundação de Amparo à Pesquisa do Estado de São Paulo; U.S. Department of Energy","keywords":"Tevatron; Higgs boson; Fermilab; Branching fraction; Standard Model (mathematical formulation); Collider; Collider Detector at Fermilab; Detector; Boson","score_opus":0.019298870102214337,"score_gpt":0.23621006760332075,"score_spread":0.2169111975011064,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7024490656","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":[0.99274886,0.00005377035,0.000024110155,0.0004827694,0.000032774595,0.0013737992,0.00409357,0.000025580644,0.0011647925],"genre_scores_gemma":[0.9966455,0.0000030770364,0.0006615708,0.000096280084,0.00006416336,0.00071638596,0.0006506857,0.000023872974,0.0011384829],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9988468,0.000034333847,0.00016555711,0.0003113414,0.00033717966,0.0003047685],"domain_scores_gemma":[0.9993837,0.00009432817,0.000085581996,0.00033326476,0.00003110314,0.0000720329],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00008323582,0.00013701223,0.00014147046,0.000002456688,0.00014244262,0.000031539308,0.0003118131,0.00007103668,0.14228888],"category_scores_gemma":[0.000104603874,0.000087172564,0.000053436754,0.00031222214,0.000053204985,0.00020745085,0.00014564919,0.00012943387,0.0009889517],"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":[0.0001464676,0.0004595613,0.067196354,0.00022447537,0.00004411407,0.0000052964365,0.0019050532,0.013176445,0.023328422,0.000030590134,0.8671119,0.026371293],"study_design_scores_gemma":[0.0010774408,0.0007474171,0.83636624,0.00051385217,0.00001889703,0.000005628457,0.00078771135,0.005745382,0.030945973,0.00006191176,0.12321372,0.0005158325],"about_ca_topic_score_codex":0.00029090483,"about_ca_topic_score_gemma":0.00016547237,"teacher_disagreement_score":0.76916987,"about_ca_system_score_codex":0.00010900461,"about_ca_system_score_gemma":0.000032286673,"threshold_uncertainty_score":0.9997889},"labels":[],"label_agreement":null},{"id":"W7024614433","doi":"","title":"Search for new phenomena in events with three or more charged leptons in pp collisions at √ s =8 TeV with the ATLAS detector","year":2015,"lang":"en","type":"article","venue":"Lancaster EPrints (Lancaster University)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Fundação para a Ciência e a Tecnologia; Institut National de Physique Nucléaire et de Physique des Particules; Agencia Nacional de Promoción Científica y Tecnológica; Science and Technology Facilities Council; Natural Sciences and Engineering Research Council of Canada; H. Lundbeck A/S; Centre National pour la Recherche Scientifique et Technique; Georgian National Science Foundation; National Research Center \"Kurchatov Institute\"; Centre National de la Recherche Scientifique; Max-Planck-Gesellschaft; Israel Science Foundation; Israeli Centers for Research Excellence; Joint Institute for Nuclear Research; Japan Society for the Promotion of Science; Conselho Nacional de Desenvolvimento Científico e Tecnológico; Lundbeckfonden; Bundesministerium für Wissenschaft, Forschung und Wirtschaft; Leverhulme Trust; General Secretariat for Research and Technology; Ministry of Education, Culture, Sports, Science and Technology; Nederlandse Organisatie voor Wetenschappelijk Onderzoek; Austrian Science Fund; Bundesministerium für Bildung und Forschung; National Science Council; U.S. Department of Energy; National Natural Science Foundation of China; Fundação de Amparo à Pesquisa do Estado de São Paulo; Javna Agencija za Raziskovalno Dejavnost RS; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; Ministerstwo Edukacji i Nauki; CERN; Departamento Administrativo de Ciencia, Tecnología e Innovación (COLCIENCIAS); Deutsche Forschungsgemeinschaft; European Commission; Comisión Nacional de Investigación Científica y Tecnológica; Danmarks Grundforskningsfond; TRIUMF; Alexander von Humboldt-Stiftung; Services Fédéraux des Affaires Scientifiques, Techniques et Culturelles; Department of Science and Technology, Ministry of Science and Technology, India; National Science Foundation; Türkiye Atom Enerjisi Kurumu","keywords":"Lepton; Higgs boson; Large Hadron Collider; Boson; Standard Model (mathematical formulation); Excited state; Atlas (anatomy); ATLAS experiment; Hadron","score_opus":0.030972566561629968,"score_gpt":0.22486911908725724,"score_spread":0.19389655252562726,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7024614433","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":[0.9899768,0.0000100835605,0.00247362,0.0007171144,0.000038478902,0.00083409244,0.00001331608,0.00001893115,0.005917521],"genre_scores_gemma":[0.9653451,0.000005147959,0.0018228292,0.00013438633,0.000060317096,0.00001167616,0.0000063077414,0.00003344202,0.0325808],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983809,0.00006186325,0.00014751125,0.0005089896,0.00035604872,0.0005446688],"domain_scores_gemma":[0.9991352,0.0000678225,0.000076787226,0.00044485382,0.000018273757,0.00025704963],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00017073643,0.0002419489,0.00026518235,0.000015570564,0.00012919257,0.000024962035,0.00053084776,0.000079398276,0.0010098347],"category_scores_gemma":[0.000005470937,0.00014830426,0.00004084996,0.0007774022,0.00017016636,0.00024238894,0.0004929659,0.00021397311,0.00033574906],"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":[0.0017931104,0.00009389061,0.99358267,0.000008284664,0.000022936048,0.00011031602,0.0022211175,0.00018711013,0.00017033888,0.00002079557,0.00042964795,0.0013597569],"study_design_scores_gemma":[0.0058627245,0.00046174103,0.95035964,0.000075104705,0.000026420426,0.000026664811,0.0032240693,0.0014203715,0.00042962158,0.000012123482,0.037728254,0.00037324405],"about_ca_topic_score_codex":0.0007321945,"about_ca_topic_score_gemma":0.02125939,"teacher_disagreement_score":0.043223035,"about_ca_system_score_codex":0.0005523483,"about_ca_system_score_gemma":0.00009062235,"threshold_uncertainty_score":0.9999034},"labels":[],"label_agreement":null},{"id":"W7024616805","doi":"","title":"Simposi Pompeu Fabra. Institut d'Estudis Catalans (Barcelona) 26/27-IX- 1998","year":2000,"lang":"ca","type":"article","venue":"LA Referencia (Red Federada de Repositorios Institucionales de Publicaciones Científicas)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Identity (music); Perspective (graphical); Identification (biology); Context (archaeology); Action (physics)","score_opus":0.013272542212201636,"score_gpt":0.2273544779390753,"score_spread":0.21408193572687365,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7024616805","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.46833804,0.002066023,0.0012450712,0.024515765,0.0029891552,0.0018935362,0.00038298097,0.0011364181,0.497433],"genre_scores_gemma":[0.98210734,0.0017244515,0.0027712157,0.0010706732,0.001237442,0.00023871733,0.0002734252,0.00021961515,0.010357112],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.9910375,0.00060762657,0.0016320904,0.002268967,0.0021808506,0.0022729523],"domain_scores_gemma":[0.99565065,0.00027724815,0.0006444116,0.0016635248,0.00013836216,0.001625776],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":["metaepi_narrow","insufficient_payload"],"category_scores_codex":[0.00082133565,0.0014370361,0.0012010252,0.00006517243,0.0022198837,0.0006210936,0.0020159744,0.0012620351,0.0037676285],"category_scores_gemma":[0.00023245909,0.0014221305,0.0006816184,0.0016944788,0.0002663927,0.0012433,0.0008107255,0.0016086046,0.0028591997],"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":[0.0037094427,0.01481408,0.05131247,0.0011671288,0.002993538,0.0061605372,0.030943053,0.011880877,0.025191935,0.6333839,0.10501667,0.11342632],"study_design_scores_gemma":[0.0019569178,0.0002771966,0.026058514,0.00023071642,0.00027209916,0.0013315082,0.00062910235,0.001042863,0.0007480626,0.00023699226,0.9656344,0.0015816215],"about_ca_topic_score_codex":0.000046158533,"about_ca_topic_score_gemma":0.0013230677,"teacher_disagreement_score":0.86061776,"about_ca_system_score_codex":0.0022352857,"about_ca_system_score_gemma":0.0007934119,"threshold_uncertainty_score":0.99983793},"labels":[],"label_agreement":null},{"id":"W7024617001","doi":"","title":"♥╬ *⇨【+❷❼❻❽ ❶❼❽❻❼❸❼】Spiritual Healer | Native Healer | Traditional Healer And Sangoma With Strong Muthi For protection }} Bring Back Lost Lovers || Money Spells That Work Over Night For Instant Success And Real Love Binding Spells That Work Fast Get Back Ex Lover In same day {{ 100% Guaranteed Results }} In Inanda }} Johannesburg }} South Africa","year":2021,"lang":"en","type":"other","venue":"OSF Preprints (OSF Preprints)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Psychic; Wife; Work (physics); Caster; Romance","score_opus":0.030439273369824774,"score_gpt":0.23658455849084353,"score_spread":0.20614528512101876,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7024617001","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.40398917,0.00004249852,0.0020202126,0.00023655302,0.00029862157,0.00618609,0.0007186145,0.000030906525,0.58647734],"genre_scores_gemma":[0.2440086,0.0004190375,0.003573112,0.00014127341,0.00023689098,0.000059519498,0.00019122264,0.0004500953,0.75092024],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9928977,0.00046527653,0.00097590726,0.00355487,0.0009018069,0.0012044555],"domain_scores_gemma":[0.9968266,0.0005181591,0.000934594,0.0012964947,0.00003918506,0.00038495735],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0020975776,0.0010254608,0.0012410354,0.00008917879,0.00008845323,0.0002796097,0.00060048647,0.00079703954,0.12925565],"category_scores_gemma":[0.00015988774,0.0010098842,0.00022084043,0.00075641053,0.00070970645,0.00046971889,0.0007208114,0.00091271114,0.033889998],"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":[0.012583957,0.0018140537,0.768312,0.0016121224,0.0008968881,0.0002036423,0.044133723,0.010143066,0.0008386813,0.00012170991,0.1539721,0.005368078],"study_design_scores_gemma":[0.021905165,0.00014275083,0.73745,0.009399655,0.00026268547,0.00008837571,0.007009913,0.0019010387,0.0018113194,0.00046930154,0.21489574,0.0046640653],"about_ca_topic_score_codex":0.0023002021,"about_ca_topic_score_gemma":0.003489402,"teacher_disagreement_score":0.16444293,"about_ca_system_score_codex":0.0011964467,"about_ca_system_score_gemma":0.00015794768,"threshold_uncertainty_score":0.99923515},"labels":[],"label_agreement":null},{"id":"W7024617497","doi":"","title":"Shifting internal parent-child representations among caregivers of teens with serious behaviour problems: An attachment-based approach","year":2012,"lang":"en","type":"article","venue":"Summit (Simon Fraser University)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Institute of Gender and Health; Canadian Institutes of Health Research","keywords":"Psychological intervention; Checklist; Representation (politics); Intervention (counseling); Child Behavior Checklist; Attachment theory; Qualitative research; Parenting skills; Family systems","score_opus":0.011186276557811407,"score_gpt":0.21174871633711218,"score_spread":0.20056243977930077,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7024617497","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":[0.9688268,0.000010008653,0.007829286,0.000028425127,0.000047789734,0.0002897252,0.000019522839,0.00006206465,0.022886412],"genre_scores_gemma":[0.9966221,0.0000034793202,0.0024479683,0.000022803211,0.000023571361,0.000002821159,0.000046513782,0.00002151896,0.00080926274],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986521,0.000084593645,0.00015923686,0.0003680516,0.00033959444,0.00039644862],"domain_scores_gemma":[0.9991374,0.000017736438,0.00019595359,0.0003594122,0.000020197014,0.0002692901],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010230104,0.00019684274,0.00018275552,0.000014596754,0.00025008578,0.000021460955,0.00038940457,0.00008265272,0.0004344994],"category_scores_gemma":[0.000004719395,0.0001901925,0.00008060508,0.00048004655,0.000364064,0.00068860233,0.00015753272,0.00019065524,0.000014077121],"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":[0.000045817123,0.00032479677,0.9860889,0.000012178131,0.000028532035,0.000011951709,0.0003735675,0.012434729,0.00001097999,0.00003990075,0.000339902,0.00028876125],"study_design_scores_gemma":[0.0014312993,0.0002780538,0.9156732,0.000057763995,0.00019346375,7.2039995e-8,0.07698953,0.0015705624,0.0009130623,0.0000027263036,0.0024378786,0.00045241253],"about_ca_topic_score_codex":0.0046816515,"about_ca_topic_score_gemma":0.018347599,"teacher_disagreement_score":0.07661597,"about_ca_system_score_codex":0.00021222087,"about_ca_system_score_gemma":0.000018046714,"threshold_uncertainty_score":0.999565},"labels":[],"label_agreement":null},{"id":"W7024687910","doi":"","title":"Tintype of Girl Peering through Lattice [n.d.]","year":2011,"lang":"en","type":"article","venue":"Brock University Digital Repository (Brock University)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Girl; Lattice (music); Studio; Painting; White (mutation); Negotiation","score_opus":0.013705256484183479,"score_gpt":0.1719621385513959,"score_spread":0.15825688206721242,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7024687910","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":[0.56135213,0.000008765108,0.0025707092,9.061339e-7,0.00010103204,0.000089504574,0.00000828235,0.00009285658,0.43577582],"genre_scores_gemma":[0.6397858,0.0000124861135,0.0015942265,0.000013409701,0.000017180531,3.5222143e-8,0.0000026728426,0.000014251924,0.3585599],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9987601,0.000036295663,0.00015970021,0.00042061156,0.00029720992,0.00032607283],"domain_scores_gemma":[0.99921227,0.000036192738,0.00018558672,0.00034588668,0.000043807497,0.00017626157],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0000020253908,0.00021565608,0.00022304968,0.000012785079,0.00025949973,0.000022453663,0.0006468074,0.00013628449,0.00016926957],"category_scores_gemma":[0.000014151426,0.0002591395,0.0001720575,0.000526627,0.0002880635,0.0014478216,0.00072435307,0.00015765431,0.00016886904],"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":[0.0006244224,0.00064310775,0.9079442,0.000058754278,0.0001803096,0.0004164759,0.0005688734,0.0005416756,0.04530797,0.00061435386,0.041775413,0.0013244697],"study_design_scores_gemma":[0.0023799648,0.0009855314,0.29938996,0.00012698288,0.0003819486,0.00016850224,0.041639224,0.000039262548,0.015186659,0.00039766132,0.63755614,0.0017481738],"about_ca_topic_score_codex":0.000605894,"about_ca_topic_score_gemma":0.00014082126,"teacher_disagreement_score":0.60855424,"about_ca_system_score_codex":0.00028977112,"about_ca_system_score_gemma":0.000033385502,"threshold_uncertainty_score":0.9999861},"labels":[],"label_agreement":null},{"id":"W7024779044","doi":"","title":"Specifications and form of tender for grading for the Port Dalhousie and Thorold Railway","year":2016,"lang":"en","type":"other","venue":"Brock University Digital Repository (Brock University)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Grading (engineering); Port (circuit theory); Tender offer; Call for bids","score_opus":0.013796352560621393,"score_gpt":0.18823377627180732,"score_spread":0.17443742371118592,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7024779044","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.008883163,0.00024028213,0.049247693,0.000032837346,0.0002995753,0.0018782592,0.00056613516,0.00018768202,0.9386644],"genre_scores_gemma":[0.012988585,0.00021545224,0.00059720286,0.000011444556,0.000071904775,7.768497e-7,0.000011608418,0.00007208837,0.98603094],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9989941,0.000012394074,0.00012510944,0.00045230347,0.0001646254,0.00025145427],"domain_scores_gemma":[0.99910027,0.00017453292,0.00027088478,0.00028938585,0.000026050902,0.00013890195],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000003781866,0.00024112572,0.00025300813,0.00002349953,0.00039507958,0.000040680734,0.0003889848,0.00019475083,0.000046095705],"category_scores_gemma":[0.0000129098935,0.00020410662,0.0001497927,0.00013826673,0.0004072941,0.0003468901,0.00036517179,0.00007904977,0.0000055556434],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002440495,0.00010754976,0.04277387,0.00012108652,0.00028255646,0.000011281652,0.00007295393,0.000008973464,0.003853471,0.00092275493,0.94659173,0.0050097196],"study_design_scores_gemma":[0.0007133326,0.000097620505,0.004877203,0.00005135538,0.00018475017,0.000016941145,0.0027463366,0.000006703669,0.000058780068,0.00009747126,0.99085736,0.0002921337],"about_ca_topic_score_codex":0.00008420684,"about_ca_topic_score_gemma":0.0002744602,"teacher_disagreement_score":0.048650492,"about_ca_system_score_codex":0.0001418276,"about_ca_system_score_gemma":0.000033045977,"threshold_uncertainty_score":0.8323226},"labels":[],"label_agreement":null},{"id":"W7024823818","doi":"","title":"SynthÃ¨se stÃ©rÃ©ocontrÃ´lÃ©e de glycosides, application Ã  la synthÃ¨se de Lewis X, Sialyle Lewis X et mimiques de Sialyle Lewis X","year":2001,"lang":"fr","type":"other","venue":"Library and Archives Canada (Government of Canada)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Nucleofection; Gestational period; TSG101; Dysgeusia; Diafiltration; Liquation; Triacetin; Emperipolesis; Fusible alloy","score_opus":0.0030355939782528217,"score_gpt":0.16315247397533023,"score_spread":0.1601168799970774,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7024823818","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.06396095,0.0034765583,0.019642105,0.009558183,0.0002840611,0.0011091724,0.0010235099,0.0000781933,0.9008673],"genre_scores_gemma":[0.69697684,0.005209072,0.019431625,0.0052498053,0.0003798153,0.00016142483,0.000049704446,0.00030239607,0.27223933],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9946241,0.0005359184,0.0007230274,0.000958419,0.0018485186,0.0013100217],"domain_scores_gemma":[0.9968513,0.0007639654,0.0006368983,0.00068757194,0.0000012242133,0.0010590333],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00012239463,0.0008234698,0.00083837105,0.000010987646,0.00043344594,0.0001322308,0.0008879903,0.0003259714,0.0055794423],"category_scores_gemma":[0.000026425152,0.00087259914,0.00015930123,0.00021195711,0.00066529145,0.00051859935,0.0004761572,0.00058937335,5.361803e-7],"study_design_candidate":"not_applicable","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":[0.0012709536,0.00093609345,0.31434196,0.0013216042,0.001081825,0.0012617914,0.002244423,0.008626046,0.17227517,0.11438837,0.07096201,0.31128976],"study_design_scores_gemma":[0.00074974785,0.00018881628,0.059070736,0.0005544128,0.00024515396,0.00010683792,0.0023680641,0.008091046,0.037278384,0.0022776092,0.887785,0.0012841467],"about_ca_topic_score_codex":0.23721993,"about_ca_topic_score_gemma":0.29059044,"teacher_disagreement_score":0.81682307,"about_ca_system_score_codex":0.0003295448,"about_ca_system_score_gemma":0.0026893704,"threshold_uncertainty_score":0.9993725},"labels":[],"label_agreement":null},{"id":"W7024894199","doi":"","title":"“The study of the biographical trajectory of a Portuguese 12th c. illuminated manuscript: the Leccionarium Alc. 433 from Alcobaça collection held by the Biblioteca Nacional de Portugal”","year":2024,"lang":"en","type":"book-chapter","venue":"Repositorio Universidade de Évora (Universidade de Évora)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Portuguese; Timeline; Quarter (Canadian coin); Middle Ages; Trajectory; Identification (biology)","score_opus":0.007862202238157319,"score_gpt":0.19311268733555365,"score_spread":0.18525048509739633,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7024894199","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":[0.89293927,0.0036757623,0.00042928828,0.007103121,0.0027225597,0.0030534186,0.00070630695,0.00024647746,0.08912381],"genre_scores_gemma":[0.827503,0.0006274097,0.000093141665,0.00016637475,0.0002592811,0.000013718182,0.000060517526,0.000119928234,0.17115663],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.995608,0.00034707095,0.000696943,0.0009465819,0.0016257338,0.0007757253],"domain_scores_gemma":[0.9966841,0.00046718668,0.0010198229,0.0014043998,0.00013324528,0.0002912428],"candidate_categories":["metaepi_narrow","sts"],"consensus_categories":[],"category_scores_codex":[0.00072126545,0.00073470705,0.0006426534,0.000118131175,0.0014515879,0.00016010772,0.0023092844,0.0008772967,0.00048330074],"category_scores_gemma":[0.00003707331,0.00048186726,0.00082127785,0.0022058259,0.0017918932,0.00025864513,0.000922645,0.0017266861,0.000020719317],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0038651226,0.0031406593,0.063276365,0.0002941486,0.011007015,0.00353477,0.042327333,0.0036415095,0.115678884,0.0638864,0.68415076,0.005197009],"study_design_scores_gemma":[0.005290337,0.0033097386,0.21530665,0.0010347598,0.008353009,0.0010315655,0.10528373,0.0042237947,0.006396314,0.0076323813,0.63853055,0.0036071877],"about_ca_topic_score_codex":0.008825494,"about_ca_topic_score_gemma":0.0019717128,"teacher_disagreement_score":0.15203029,"about_ca_system_score_codex":0.0015962134,"about_ca_system_score_gemma":0.0004527614,"threshold_uncertainty_score":0.99984837},"labels":[],"label_agreement":null},{"id":"W7024896993","doi":"","title":"Technical Committee's member of \"The 4th INTERNATIONAL WORKSHOP ON FUNDAMENTAL ISSUES, APPLICATIONS AND FUTURE RESEARCH DIRECTIONS FOR PARALLEL MECHANISMS / MANIPULATORS / MACHINES,\" 9-11 September 2020, Belfast (UK)","year":2020,"lang":"en","type":"other","venue":"Institutional Research Information System University of Ferrara (University of Ferrara)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Nucleofection; Gestational period; TSG101; Pretext; Liquation; Dysgeusia","score_opus":0.044383485217766826,"score_gpt":0.292172862763261,"score_spread":0.24778937754549415,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7024896993","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0035202105,0.00020700891,0.063631274,0.0057814238,0.00062852196,0.0045686634,0.0020436996,0.00016002142,0.91945916],"genre_scores_gemma":[0.66946274,0.0011636332,0.04599212,0.000111283516,0.0005349581,0.000025836165,0.0010339556,0.00013919252,0.28153628],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9971135,0.00017229769,0.00029276375,0.00036194536,0.0017571998,0.00030227914],"domain_scores_gemma":[0.9986161,0.00011601515,0.0004141525,0.00043294,0.00022731231,0.0001935013],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007018051,0.00021930318,0.00038484216,0.00011478192,0.0010148996,0.000026809317,0.0011517617,0.0003965511,0.0028617964],"category_scores_gemma":[0.000031188585,0.00022906734,0.00021434271,0.0009258764,0.0016249159,0.00042992114,0.00090532214,0.0005700819,0.00012087125],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009845209,0.00037859785,0.0034350986,0.0009962666,0.00040374015,0.000014385034,0.0021306516,0.0012664975,0.0002559413,0.24279837,0.74100363,0.006332293],"study_design_scores_gemma":[0.0010405105,0.000099007404,0.00768756,0.0003424939,0.000040783136,0.000016622454,0.010865461,0.0018644365,0.00000815352,0.00021152831,0.9776035,0.00021993998],"about_ca_topic_score_codex":0.0024281149,"about_ca_topic_score_gemma":0.001441485,"teacher_disagreement_score":0.66594255,"about_ca_system_score_codex":0.0007189548,"about_ca_system_score_gemma":0.00020083429,"threshold_uncertainty_score":0.99804974},"labels":[],"label_agreement":null},{"id":"W7024921539","doi":"","title":"Terres rares : les technologies sont-elles devenues trop dépendantes de ces vitamines?","year":2016,"lang":"fr","type":"other","venue":"Bibliothèque et Archives nationales du Québec (Québec government)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Nucleofection; Gestational period; TSG101; Dysgeusia; Liquation; Diafiltration; Fusible alloy; Triacetin; Emperipolesis","score_opus":0.006753773048742741,"score_gpt":0.2136523784475618,"score_spread":0.20689860539881905,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7024921539","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.43199283,0.05221936,0.00619895,0.047507584,0.00041848546,0.0011541991,0.00081511645,0.00081585493,0.45887762],"genre_scores_gemma":[0.5724628,0.00945259,0.0042836815,0.00033330603,0.0004046314,0.0002574179,0.000012145014,0.0002679806,0.41252545],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99516976,0.0003291947,0.0008272537,0.0012131014,0.0013407868,0.0011199024],"domain_scores_gemma":[0.9920191,0.006101553,0.0009157401,0.000677239,0.000022831164,0.0002635175],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00033617634,0.0010707872,0.00079592416,0.00012289474,0.00061577803,0.00042140784,0.0020382202,0.0003762724,0.069499336],"category_scores_gemma":[0.0026390897,0.0008625541,0.00047542347,0.0005659944,0.0026856677,0.00059365423,0.001401084,0.0005526077,0.0031263498],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":true,"study_design_scores_codex":[0.00021945657,0.0007630948,0.6248601,0.00032009877,0.00060819916,0.00011598576,0.0029276293,0.00018883683,0.018841209,0.018533006,0.25203618,0.08058618],"study_design_scores_gemma":[0.00079836167,0.00023912714,0.20778798,0.0006318665,0.000108192406,0.00007747785,0.0011462668,0.00023846835,0.0031756815,0.0010314037,0.7836505,0.0011146412],"about_ca_topic_score_codex":0.11101212,"about_ca_topic_score_gemma":0.89584315,"teacher_disagreement_score":0.784831,"about_ca_system_score_codex":0.0063052964,"about_ca_system_score_gemma":0.0098459255,"threshold_uncertainty_score":0.9993825},"labels":[],"label_agreement":null},{"id":"W7024926779","doi":"","title":"Student-Athlete Mental Health: University of Montana Case Study","year":2023,"lang":"en","type":"article","venue":"The Mathematics Enthusiast","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Mental health; Athletes; Wonder; Quarter (Canadian coin); Mental healthcare; Sport psychology","score_opus":0.021677468472626284,"score_gpt":0.26198932354962295,"score_spread":0.24031185507699668,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7024926779","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":[0.9931531,0.000011878863,0.00022468208,0.00027537716,0.00006401896,0.0005165308,0.000009721681,0.0000561939,0.0056884773],"genre_scores_gemma":[0.99759895,0.00002478784,0.0006081023,0.000035095356,0.000009367648,0.0000018874871,0.0000015564052,0.0000121703915,0.0017080985],"study_design_codex":"qualitative","study_design_gemma":"qualitative","domain_scores_codex":[0.99900633,0.000059692884,0.00019056891,0.00015850361,0.000368077,0.00021685075],"domain_scores_gemma":[0.9993702,0.00004452154,0.00014316944,0.00036659074,0.0000043526206,0.00007112651],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042687403,0.00010842154,0.00017706784,0.000002264944,0.00032847148,0.000010705495,0.00033733764,0.000015954933,0.0008553919],"category_scores_gemma":[0.0000053785625,0.00007981906,0.000056213437,0.00034520158,0.000158917,0.000043869313,0.0004873703,0.00007463598,0.0004449813],"study_design_candidate":"qualitative","study_design_consensus":"qualitative","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009124748,0.0009068174,0.0048271744,0.000027426708,0.00006811145,0.000612266,0.98268104,0.000636456,0.0002715703,0.00012625288,0.006671015,0.0031627754],"study_design_scores_gemma":[0.0012652964,0.00055207376,0.04441362,0.000039923296,0.00007529023,0.00047437428,0.9419488,0.0089225285,0.00004396764,0.00007424838,0.0018633531,0.00032656625],"about_ca_topic_score_codex":0.0015809628,"about_ca_topic_score_gemma":0.0021082012,"teacher_disagreement_score":0.04073225,"about_ca_system_score_codex":0.00009121123,"about_ca_system_score_gemma":0.000009063752,"threshold_uncertainty_score":0.9365941},"labels":[],"label_agreement":null},{"id":"W7024986489","doi":"","title":"Three dimensional power spectra of motion parallax in cluttered three dimensional scenes","year":2006,"lang":"en","type":"dissertation","venue":"eScholarship@McGill (McGill)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Parallax; Observer (physics); Power (physics); Spectral density; Distribution (mathematics); Constraint (computer-aided design); Motion (physics)","score_opus":0.010006195993353477,"score_gpt":0.21493211363153933,"score_spread":0.20492591763818585,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7024986489","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":[0.97548425,0.00017001729,0.0000029883893,0.00002666222,0.00091440004,0.00069624995,0.00038490654,0.00009022578,0.022230286],"genre_scores_gemma":[0.9943288,0.000013924006,0.003089101,0.00017502233,0.000035010773,0.00006885554,0.0008550952,0.00012680376,0.0013074033],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9948658,0.0001407167,0.0012600835,0.0012287254,0.0016303473,0.00087434065],"domain_scores_gemma":[0.9980011,0.00012896743,0.0007663809,0.0007606793,0.000086334716,0.0002565274],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00057988596,0.000863583,0.00089076906,0.000036782214,0.00049048045,0.00004168232,0.0007049387,0.00083617185,0.0040810946],"category_scores_gemma":[0.000096115175,0.00084893405,0.00041607136,0.00066465605,0.00021515226,0.0007656267,0.00028635943,0.0010903863,0.0006702213],"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":[0.004121087,0.0063136285,0.19687729,0.0007396022,0.0009197064,0.00079260016,0.00005486644,0.043364156,0.48086375,0.046560526,0.0007820082,0.2186108],"study_design_scores_gemma":[0.0019495701,0.00034119713,0.9263185,0.0004258762,0.00016907825,0.000028323046,0.000047962592,0.00052792707,0.021409351,0.0441742,0.0028781202,0.0017298444],"about_ca_topic_score_codex":0.0060036867,"about_ca_topic_score_gemma":0.03486381,"teacher_disagreement_score":0.7294413,"about_ca_system_score_codex":0.00088844803,"about_ca_system_score_gemma":0.000036531805,"threshold_uncertainty_score":0.99939615},"labels":[],"label_agreement":null},{"id":"W7025016742","doi":"","title":"Sucre blanc contre sucre rouge. Stéphane Lussier-Johnson, Le sucre rouge de Duplessis, Rimouski, Éditions du Tullinois, 2023, 260 pages","year":2023,"lang":"fr","type":"article","venue":"Érudit (Université de Montréal)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"ROUGE; Baton rouge; West indies","score_opus":0.0048597549932656945,"score_gpt":0.1661031940931964,"score_spread":0.16124343909993072,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7025016742","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":[0.7156445,0.06795298,0.0028396125,0.1940175,0.0012453599,0.0010060784,0.001725991,0.0007335053,0.014834514],"genre_scores_gemma":[0.5675509,0.09284859,0.001421597,0.0008717418,0.00071279204,0.000032577325,0.00054592045,0.00015872534,0.33585718],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9947449,0.00039237234,0.00056762784,0.0012838774,0.0008494517,0.0021617804],"domain_scores_gemma":[0.99709177,0.00030558693,0.00044371432,0.0010026897,0.00007908334,0.0010771538],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00056748005,0.00085254223,0.00085797714,0.000037252805,0.0027215278,0.00013533284,0.0011642445,0.0007670266,0.008352499],"category_scores_gemma":[0.00008954032,0.0009954706,0.0005611425,0.0017699926,0.0009299016,0.0008027094,0.0011477302,0.0007473092,0.0052334825],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017136645,0.00046985317,0.027632328,0.000106384,0.0002873374,0.0063969754,0.0010455188,0.011281805,0.0021398617,0.0076764165,0.92843777,0.014354403],"study_design_scores_gemma":[0.0025810474,0.0002483836,0.101054795,0.00018947013,0.00040986447,0.00048852194,0.0062849154,0.01383533,0.00042829837,0.0009850374,0.87232286,0.0011714638],"about_ca_topic_score_codex":0.07804454,"about_ca_topic_score_gemma":0.20668696,"teacher_disagreement_score":0.32102266,"about_ca_system_score_codex":0.0083919205,"about_ca_system_score_gemma":0.00025352323,"threshold_uncertainty_score":0.9992496},"labels":[],"label_agreement":null},{"id":"W7025035908","doi":"","title":"Ãtude des rÃ©percussions de la division sexuelle du travail sur les pratiques d'intÃ©gration des femmes immigrantes au Saguenay","year":2013,"lang":"fr","type":"other","venue":"Library and Archives Canada (Government of Canada)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Gender relations; Gender identity; Identity (music); History of sociology","score_opus":0.003836415229627483,"score_gpt":0.15169710927393099,"score_spread":0.1478606940443035,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7025035908","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":[0.6991556,0.002288949,0.0014573879,0.0011512979,0.00011445739,0.0003048563,0.00012846796,0.000018627827,0.29538032],"genre_scores_gemma":[0.734231,0.0029905098,0.004975753,0.00028529117,0.0000752228,0.000023571285,0.0000117744685,0.00008336266,0.2573235],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9968601,0.00037252542,0.00043542625,0.00048470352,0.0012387986,0.00060842984],"domain_scores_gemma":[0.9984393,0.0005109227,0.0002939436,0.00026077547,8.7665734e-7,0.00049416604],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000042694977,0.00050045963,0.00044217388,0.0000048370853,0.0007461526,0.00009790966,0.00040204488,0.00015928118,0.0042070993],"category_scores_gemma":[0.000020114207,0.0004126712,0.000072059,0.00012218027,0.0012371792,0.00052742386,0.00028407905,0.00028172607,1.5084414e-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":[0.00007673839,0.00014648051,0.74379104,0.00034915996,0.000116633346,0.00005339066,0.0016032513,0.00043376326,0.055043027,0.0102905985,0.008055157,0.18004075],"study_design_scores_gemma":[0.00028047105,0.00016390522,0.93349695,0.0006148133,0.000054721764,0.000013019059,0.007593457,0.005003109,0.014686879,0.0008010615,0.036755096,0.0005365109],"about_ca_topic_score_codex":0.2831055,"about_ca_topic_score_gemma":0.57481015,"teacher_disagreement_score":0.29170462,"about_ca_system_score_codex":0.000085629574,"about_ca_system_score_gemma":0.0010970349,"threshold_uncertainty_score":0.9998325},"labels":[],"label_agreement":null},{"id":"W7025069132","doi":"","title":"Using Clay-Elicitation to Explore Men’s Pathways to Gender-Based Violence Prevention","year":2023,"lang":"en","type":"dissertation","venue":"eScholarship@McGill (McGill)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"","keywords":"Poison control; Human factors and ergonomics; Qualitative research; Perspective (graphical); Suicide prevention","score_opus":0.0777117095908632,"score_gpt":0.2961023054791478,"score_spread":0.21839059588828458,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7025069132","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":[0.9802923,0.000021714199,0.00007806115,0.000015340709,0.0010678265,0.0015121378,0.0002161748,0.0003895693,0.016406875],"genre_scores_gemma":[0.98538584,0.000038281207,0.010714461,0.00071272394,0.00005453956,0.000598321,0.00068389165,0.00023924746,0.0015726773],"study_design_codex":"design_other","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99492705,0.00029324862,0.0009188545,0.0014543576,0.001435113,0.0009713548],"domain_scores_gemma":[0.9978057,0.000106860985,0.00047813836,0.0008083947,0.00011664715,0.0006842694],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00069583114,0.0008022767,0.00058835925,0.000049169354,0.0011504864,0.00012535995,0.00082369405,0.0006169198,0.0011274756],"category_scores_gemma":[0.00044412832,0.00088875514,0.00033698787,0.001377004,0.000044817847,0.0007505063,0.00027238298,0.0007148991,0.00481702],"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":[0.0005425374,0.00047098685,0.00072440587,0.00033812862,0.0001315915,0.00008313477,0.00048139042,0.03620683,0.39502564,0.0022464432,0.00014365972,0.56360525],"study_design_scores_gemma":[0.0065616546,0.004176251,0.17043532,0.008421014,0.0018974436,0.000042670577,0.055786416,0.009643822,0.54862696,0.11477846,0.062596165,0.017033823],"about_ca_topic_score_codex":0.0015644484,"about_ca_topic_score_gemma":0.0009759013,"teacher_disagreement_score":0.54657143,"about_ca_system_score_codex":0.00199869,"about_ca_system_score_gemma":0.000056894627,"threshold_uncertainty_score":0.9997856},"labels":[],"label_agreement":null},{"id":"W7025078949","doi":"","title":"Ãtude DFT+U des phases structurales du La2CuO4","year":2014,"lang":"fr","type":"other","venue":"Library and Archives Canada (Government of Canada)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Nucleofection; Gestational period; Fusible alloy; TSG101; Hyporeflexia; Liquation; Diafiltration","score_opus":0.0020744356072788885,"score_gpt":0.12693793376697468,"score_spread":0.12486349815969579,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7025078949","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.20729606,0.0014920268,0.00028670314,0.0023644827,0.0004713547,0.0002423015,0.00030038063,0.000015063156,0.7875316],"genre_scores_gemma":[0.6841108,0.0010086828,0.0031286175,0.00131875,0.00022827582,0.0000070173396,0.000008914784,0.00009214626,0.31009677],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9965715,0.000109444496,0.00041301432,0.00053391326,0.0017757771,0.0005963895],"domain_scores_gemma":[0.99853724,0.00025096413,0.0003482782,0.0003377302,2.3730344e-7,0.00052554597],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000011694205,0.0005098969,0.0005260672,0.0000023732753,0.00035787196,0.000044660974,0.0005370517,0.00009003526,0.019040298],"category_scores_gemma":[0.0000059626796,0.00046106064,0.0000691029,0.00008750925,0.0008691222,0.00027669192,0.00040734318,0.0002116856,1.400978e-7],"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":[0.0004657684,0.00014990025,0.58971125,0.0009491702,0.0004875936,0.00034650794,0.0004386376,0.0012618577,0.036514092,0.10960684,0.040730488,0.2193379],"study_design_scores_gemma":[0.0005619316,0.0001887262,0.3772497,0.0004168652,0.00009694407,0.000028000066,0.0015255075,0.0026176937,0.014095631,0.0017936502,0.6005558,0.000869602],"about_ca_topic_score_codex":0.030330736,"about_ca_topic_score_gemma":0.23087625,"teacher_disagreement_score":0.55982524,"about_ca_system_score_codex":0.00003295333,"about_ca_system_score_gemma":0.0006250761,"threshold_uncertainty_score":0.9997841},"labels":[],"label_agreement":null},{"id":"W7025091716","doi":"","title":"Use of environmental DNA to investigate the distribution of microcystin-producing Microcystis in Eastern Ontario","year":2018,"lang":"en","type":"other","venue":"QSpace (Queen's University Library)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Microcystis; Cyanobacteria; Microcystin; Microcystis aeruginosa; Polymerase chain reaction; Algae; Environmental DNA; Water quality; Algal bloom","score_opus":0.007749501153376997,"score_gpt":0.16137704849013298,"score_spread":0.153627547336756,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7025091716","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9817048,0.000009294417,0.00019903862,0.0015824678,0.00009828221,0.000515993,0.00024975653,0.000045279718,0.0155951055],"genre_scores_gemma":[0.19351088,0.000038527625,0.0032086568,0.00008605361,0.000034717577,8.0834127e-7,0.000082744154,0.00009467483,0.80294293],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99861336,0.00009596808,0.00021696137,0.00051659165,0.00025670335,0.00030040226],"domain_scores_gemma":[0.9989469,0.000029660487,0.00034506395,0.0005367198,0.0000022700256,0.0001393813],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000045598936,0.0002903133,0.0003431118,0.000014659248,0.000066498586,0.000018557786,0.0005644483,0.00019698558,0.0071720816],"category_scores_gemma":[0.000009278143,0.00026697433,0.00010000977,0.00031959004,0.0005875683,0.00030931277,0.00087962055,0.00019033412,0.00027077284],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007710231,0.00008766346,0.43314227,0.000027103451,0.000033957338,0.000022224262,0.0010874226,0.00010125649,0.0008131119,0.000012501245,0.5643896,0.00020577277],"study_design_scores_gemma":[0.00024164746,0.00011263065,0.20843521,0.00021373984,0.0000456975,5.272098e-7,0.0003285731,0.0000037881043,0.0039867833,0.0000074526733,0.7862988,0.00032513877],"about_ca_topic_score_codex":0.29176375,"about_ca_topic_score_gemma":0.019928664,"teacher_disagreement_score":0.7881939,"about_ca_system_score_codex":0.00036313568,"about_ca_system_score_gemma":0.000060773105,"threshold_uncertainty_score":0.99997824},"labels":[],"label_agreement":null},{"id":"W7025124793","doi":"","title":"Transgender Erasure: Barriers facing transgender refugees in Canada","year":2023,"lang":"en","type":"article","venue":"eYLS (Yale Law School)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Refugee; Transgender; Credibility; Immigration; Parallels; Documentation","score_opus":0.011121800880222478,"score_gpt":0.22057452317551357,"score_spread":0.2094527222952911,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7025124793","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":[0.9845508,0.0000932723,0.00022118818,0.0006961712,0.00028804253,0.00020511786,0.000022065306,0.00009948972,0.013823852],"genre_scores_gemma":[0.99592423,0.000028813482,0.0003337777,0.001357735,0.000042809836,0.000038096434,0.000009742161,0.000036600926,0.002228193],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978233,0.00007499643,0.0003361837,0.0004940304,0.00057281,0.0006986957],"domain_scores_gemma":[0.99916565,0.00003779846,0.000042136104,0.0003235869,0.000004858502,0.00042594256],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00025999927,0.00023743563,0.00024282964,0.0000030526876,0.00022138597,0.000035742465,0.00034089494,0.00009427587,0.0101561975],"category_scores_gemma":[0.000019668756,0.00022718024,0.00007874723,0.0006470506,0.000109711415,0.00022435692,0.000053801585,0.00032212265,0.0005562302],"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":[0.0000953815,0.00006473361,0.82470864,0.000070227885,0.00010268065,0.0005169685,0.003190382,0.08668596,0.018576188,0.002708737,0.055452984,0.007827085],"study_design_scores_gemma":[0.0025059746,0.000120936245,0.58027613,0.00008521912,0.000056786877,0.000024809957,0.008545596,0.005424234,0.0063114325,0.0030173578,0.39142704,0.0022045115],"about_ca_topic_score_codex":0.7835712,"about_ca_topic_score_gemma":0.9601843,"teacher_disagreement_score":0.33597404,"about_ca_system_score_codex":0.00071550667,"about_ca_system_score_gemma":0.00023048637,"threshold_uncertainty_score":0.99074864},"labels":[],"label_agreement":null},{"id":"W7025150160","doi":"","title":"Today's show: Is Canada meant to have unruly provinces, Alberta's prescribed opioid strategy &amp; the age of exhausting television","year":2022,"lang":"en","type":"other","venue":"Bulletin of Miscellaneous Information (Royal Gardens Kew)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Popularity; Addiction; Harm; Harm reduction; Opioid; Opioid addiction","score_opus":0.006155337022877077,"score_gpt":0.18011645601710136,"score_spread":0.17396111899422428,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7025150160","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0015931657,0.000115821254,0.0000013621681,0.00025130526,0.00014483374,0.00082928676,0.00017799834,0.000031657928,0.99685454],"genre_scores_gemma":[0.008862928,0.00005752233,0.00081982167,0.0007815934,0.00005892423,0.000033912533,0.00014177887,0.00008655963,0.98915696],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9976076,0.000080579666,0.0006885878,0.00030466737,0.0009422908,0.0003762958],"domain_scores_gemma":[0.9985408,0.00012226768,0.000616086,0.00056353945,0.000027658958,0.00012963825],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00023723418,0.000354237,0.00040602806,0.000004407206,0.00015708395,0.000040285704,0.0007247146,0.00016846509,0.64218104],"category_scores_gemma":[0.00009897348,0.00027626342,0.000111856636,0.000019954276,0.00016296629,4.5279293e-7,0.00046378892,0.00029704574,0.0010988825],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000039186645,0.000027689519,0.000114814975,0.0001371443,0.000030389934,0.0000103244265,0.00050735014,0.0048520593,0.0000036253864,0.0000035597864,0.9911664,0.0031074444],"study_design_scores_gemma":[0.00019124424,0.0001273617,0.00012453923,0.00008199935,0.0000347956,0.000016567605,0.00070889096,0.00004528421,0.000016843542,0.000002751416,0.9983384,0.00031131826],"about_ca_topic_score_codex":0.9042712,"about_ca_topic_score_gemma":0.83577585,"teacher_disagreement_score":0.64108217,"about_ca_system_score_codex":0.00026803862,"about_ca_system_score_gemma":0.00010330483,"threshold_uncertainty_score":0.99996895},"labels":[],"label_agreement":null},{"id":"W7025172047","doi":"","title":"UNESCO, the World Bank, and the struggle over education for development through the lens of the Faure report (1972) and the Delors report (1996)","year":2023,"lang":"en","type":"article","venue":"Open Access Publications (University of Geneva Libararies)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"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 Alberta","funders":"","keywords":"Treasure; International education; Neoliberalism (international relations); Position (finance); Comparative education; Redistribution (election); Order (exchange); International development","score_opus":0.039475306753493276,"score_gpt":0.2990801982228145,"score_spread":0.25960489146932125,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7025172047","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":[0.7280196,0.00033706534,0.0021669327,0.18582393,0.00028470522,0.0039039867,0.000028759025,0.00003663885,0.0793984],"genre_scores_gemma":[0.951289,0.00012223171,0.0013265914,0.0008438328,0.000027600274,0.00007526145,0.00003521767,0.000012746793,0.046267517],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.99878156,0.0001275557,0.00027248956,0.00032348704,0.00032291195,0.00017198896],"domain_scores_gemma":[0.9980024,0.00033583175,0.00055727316,0.0009796896,0.00009209647,0.00003269977],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0011501638,0.000122021,0.00017814634,0.000006451637,0.0020635528,0.00035197003,0.002306839,0.00004528266,0.00037220266],"category_scores_gemma":[0.0001668941,0.00005769888,0.000074343065,0.0012539774,0.0020502207,0.0011548864,0.0025659895,0.00012710546,0.000003925422],"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":[0.00035671014,0.00019857023,0.15662077,0.00004186575,0.00037312694,0.0000023933917,0.025923077,0.00091234763,0.00006060391,0.41230455,0.38456422,0.018641785],"study_design_scores_gemma":[0.00066675025,0.0000053719946,0.4963344,0.0000103690245,0.00009343566,0.00001897545,0.008676002,0.0005151646,0.00005135004,0.009958162,0.4835618,0.00010818238],"about_ca_topic_score_codex":0.0053945086,"about_ca_topic_score_gemma":0.005629505,"teacher_disagreement_score":0.40234637,"about_ca_system_score_codex":0.00006052596,"about_ca_system_score_gemma":0.00032626034,"threshold_uncertainty_score":0.99923563},"labels":[],"label_agreement":null},{"id":"W7025189572","doi":"","title":"Virtual Heritage: The cases of the Byzantine Crypt of Santa Cristina and Temple C of Selinunte","year":2004,"lang":"en","type":"article","venue":"NPARC","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Byzantine architecture; Cultural heritage; Temple; Interpretation (philosophy); Texture (cosmology); Range (aeronautics)","score_opus":0.0103037757833686,"score_gpt":0.2212213326799043,"score_spread":0.21091755689653569,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7025189572","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":[0.9942094,0.00006927001,0.000119759294,0.00026655794,0.000029703542,0.000096983065,0.000013990793,0.0000039348465,0.0051904074],"genre_scores_gemma":[0.99844354,0.000038622078,0.0012475979,0.00006627285,0.000011553909,0.0000021910896,3.2525645e-7,0.000005751946,0.0001841612],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9993809,0.000026327263,0.00018559197,0.00010532883,0.00019737109,0.00010450785],"domain_scores_gemma":[0.99955934,0.00005890802,0.00012547712,0.00022554454,0.000008353784,0.000022375532],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012582865,0.000068705485,0.0001231425,4.4922137e-7,0.000072680436,0.0000029511589,0.00020184627,0.00002557136,0.0006030971],"category_scores_gemma":[0.000056021232,0.00003675849,0.000042275842,0.00012115097,0.00056844397,0.00003257195,0.00019032667,0.000057740875,0.000003479218],"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":[0.00006779694,0.0002444984,0.20775048,0.0000406857,0.00002512708,0.0000062719373,0.0026882985,0.0008647707,0.7757199,0.004300595,0.0025438056,0.005747778],"study_design_scores_gemma":[0.0012428232,0.0006881962,0.71025366,0.0001065646,0.00008299452,0.000073909636,0.005440871,0.00037801045,0.2742778,0.0039865705,0.003210974,0.0002576207],"about_ca_topic_score_codex":0.0007503676,"about_ca_topic_score_gemma":0.000106851294,"teacher_disagreement_score":0.50250316,"about_ca_system_score_codex":0.00000751805,"about_ca_system_score_gemma":0.000011718218,"threshold_uncertainty_score":0.660349},"labels":[],"label_agreement":null},{"id":"W7025224019","doi":"","title":"United States takes Canada to WTO over wine retailing | rewfinancialcontent","year":2017,"lang":"en","type":"other","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Wine; Government (linguistics); Quality (philosophy); Product (mathematics); European union","score_opus":0.008274512066667293,"score_gpt":0.2093147571803985,"score_spread":0.2010402451137312,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7025224019","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.009876311,0.00010810966,0.0004543718,0.00067391916,0.00043917316,0.00031977522,0.000059216738,0.00008946753,0.98797965],"genre_scores_gemma":[0.0032001664,0.000055263594,0.0014373584,0.0022361495,0.00019858463,0.000013644397,0.000053138225,0.00016866348,0.99263704],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99869907,0.000013846198,0.0001501301,0.00040554084,0.00037037328,0.00036104218],"domain_scores_gemma":[0.9990571,0.000011424427,0.00015610618,0.00057517237,0.0000053854983,0.00019482685],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0000660404,0.0002700537,0.00027202236,0.0000025090105,0.00012305635,0.00003528625,0.00043509807,0.00012828177,0.029058388],"category_scores_gemma":[0.000035497487,0.00021428734,0.000043269825,0.00011073961,0.00008436242,0.000029114253,0.00016190654,0.000118738986,0.00027216034],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004791553,0.000008744966,0.0040578507,0.0000055793475,0.000013965436,0.000024513713,0.000028336472,0.00017211075,0.000029851617,0.000018397388,0.99364555,0.0019903267],"study_design_scores_gemma":[0.00011402489,0.000026932472,0.0043785935,0.000067215115,0.000012757516,8.792402e-7,0.00006427248,0.00018043957,0.000026591093,0.000006964388,0.99480534,0.00031598713],"about_ca_topic_score_codex":0.97377247,"about_ca_topic_score_gemma":0.97474986,"teacher_disagreement_score":0.028786227,"about_ca_system_score_codex":0.00031064966,"about_ca_system_score_gemma":0.0000714778,"threshold_uncertainty_score":0.9718292},"labels":[],"label_agreement":null},{"id":"W7025246819","doi":"","title":"On the use of the auditory pathway for comprehending complex engineering concepts","year":2001,"lang":"en","type":"article","venue":"Canadian acoustics","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"University of Toronto","keywords":"Auditory display; Auditory pathways; Auditory masking; Computational auditory scene analysis; Auditory perception","score_opus":0.04354330867918058,"score_gpt":0.2193263359047015,"score_spread":0.17578302722552092,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7025246819","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":[0.98358494,0.0000064869705,0.014078392,0.0004430914,0.0005272574,0.00029232292,0.000077522054,0.000012149849,0.000977815],"genre_scores_gemma":[0.9969603,0.0000024386593,0.0010996766,0.0010662179,0.00009546796,0.000009368272,0.0000020224243,0.0000131593915,0.00075135287],"study_design_codex":"simulation_or_modeling","study_design_gemma":"not_applicable","domain_scores_codex":[0.99943805,0.000012210528,0.00009993539,0.000100302386,0.00011348782,0.0002360083],"domain_scores_gemma":[0.999433,0.00017765755,0.00004381125,0.00022254721,0.000007063307,0.000115965246],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000049631886,0.00008209042,0.00007384476,0.0000011804852,0.00018375406,0.000016770575,0.00023222865,0.00003864601,0.00063204527],"category_scores_gemma":[0.0000982059,0.000052850944,0.000044966062,0.000104343344,0.00014141866,0.000027310029,0.000034931534,0.00008142155,0.000016922162],"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":[0.0000072685007,0.000020798732,0.009243648,0.000012381843,0.000020719275,0.00000762675,0.00043197215,0.67815197,0.049273677,0.0028452666,0.25659886,0.0033858316],"study_design_scores_gemma":[0.0002104614,0.000056989436,0.29698285,0.000031098738,0.000022056183,0.0000054263164,0.00023015654,0.31168836,0.00015938288,0.00011684767,0.3902641,0.00023227165],"about_ca_topic_score_codex":0.0046888413,"about_ca_topic_score_gemma":0.002417927,"teacher_disagreement_score":0.3664636,"about_ca_system_score_codex":0.00019314457,"about_ca_system_score_gemma":0.000039773036,"threshold_uncertainty_score":0.70881563},"labels":[],"label_agreement":null},{"id":"W7025260987","doi":"","title":"Uso del ASQ-3 en niños prematuros hasta los dos años de edad corregida: Revisión sistemática","year":2021,"lang":"es","type":"dissertation","venue":"Repositorio de Patentes de la Universidad de Almería (Universidad de Almería)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Population; Context (archaeology); Health professionals; Hasta","score_opus":0.0056099680887244,"score_gpt":0.24313498091011349,"score_spread":0.23752501282138908,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7025260987","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":[0.93282324,0.0036023816,0.0124103185,0.000744077,0.0012660457,0.001759484,0.00024459074,0.0004819547,0.046667907],"genre_scores_gemma":[0.9107259,0.0065257116,0.0147119155,0.0006476818,0.0009160763,0.00007089585,0.00060185854,0.00050131517,0.06529865],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9878936,0.0024576436,0.0013247051,0.0028449614,0.0019285682,0.003550552],"domain_scores_gemma":[0.9920614,0.0012965006,0.0018396738,0.002226624,0.0004089353,0.002166869],"candidate_categories":["metaepi_narrow","sts","scholarly_communication","research_integrity","insufficient_payload"],"consensus_categories":["metaepi_narrow","research_integrity"],"category_scores_codex":[0.0013520769,0.0021440159,0.0020539165,0.00016392552,0.00196415,0.0011670042,0.002988727,0.0030157038,0.0025822658],"category_scores_gemma":[0.00041519594,0.0026533294,0.0017062487,0.0021370957,0.0010388613,0.0013444491,0.0010860398,0.0030118227,0.00040803215],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.003385675,0.0029852772,0.5492935,0.003333677,0.0052285763,0.039886888,0.029631505,0.011134761,0.3037711,0.0050084554,0.034268245,0.01207233],"study_design_scores_gemma":[0.013680194,0.0031657666,0.5675452,0.012974397,0.018619182,0.01379806,0.12324995,0.0660882,0.051702656,0.000799726,0.1154132,0.012963483],"about_ca_topic_score_codex":0.012444551,"about_ca_topic_score_gemma":0.0003526191,"teacher_disagreement_score":0.25206846,"about_ca_system_score_codex":0.010832551,"about_ca_system_score_gemma":0.0028987816,"threshold_uncertainty_score":0.9998699},"labels":[],"label_agreement":null},{"id":"W7025283330","doi":"","title":"The Use of Laser-Doppler Interferometry Based on a Fabry-Perot Etalon for Shock Adhesion Test Applied to Adhesively Bonded Materials","year":2008,"lang":"en","type":"article","venue":"NPARC","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Research Council Canada; Natural Sciences and Engineering Research Council of Canada; Centre National de la Recherche Scientifique","keywords":"Fabry–Pérot interferometer; Interferometry; Adhesion; Shock (circulatory); Adhesive","score_opus":0.03465723362488293,"score_gpt":0.2307900998270115,"score_spread":0.19613286620212858,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7025283330","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":[0.9933204,0.0000010771707,0.0028673506,0.00041810505,0.000092654926,0.000786232,0.000056535933,0.00003292582,0.002424731],"genre_scores_gemma":[0.9863143,0.0000048285597,0.011194837,0.0009474293,0.000035397432,0.0001898896,0.00000957451,0.000029304023,0.0012744431],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9986839,0.000031758664,0.0003023452,0.00033275524,0.0003335011,0.00031568363],"domain_scores_gemma":[0.9989658,0.00039097382,0.00011731363,0.00039533136,0.000014071301,0.00011650078],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00017116324,0.00018704278,0.00023072817,0.0000037105322,0.00024333599,0.000031125834,0.00029977487,0.00008091488,0.0013149579],"category_scores_gemma":[0.00017168172,0.00012774327,0.000075335054,0.000202843,0.00015555297,0.00006368128,0.00012728678,0.00006942836,0.00021853308],"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":[0.0006742638,0.0002524478,0.0064402525,0.000014623742,0.000009087569,0.0000029128512,0.00018520502,0.0005285074,0.9377601,0.000062863364,0.048610233,0.005459492],"study_design_scores_gemma":[0.001108356,0.0013815108,0.037812907,0.000043162534,0.000023165789,0.00000553607,0.00008848404,0.0020576448,0.9414451,0.00020301185,0.015446215,0.00038487697],"about_ca_topic_score_codex":0.00004039425,"about_ca_topic_score_gemma":0.000013097654,"teacher_disagreement_score":0.03316402,"about_ca_system_score_codex":0.00009186116,"about_ca_system_score_gemma":0.000016087208,"threshold_uncertainty_score":0.99959797},"labels":[],"label_agreement":null},{"id":"W7025288158","doi":"","title":"VÃ©rification temporelle des systÃ¨mes cycliques et acycliques basÃ©e sur lâanalyse des contraintes","year":2011,"lang":"fr","type":"other","venue":"Library and Archives Canada (Government of Canada)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Work (physics); Limiting; Domain (mathematical analysis)","score_opus":0.005816005759849369,"score_gpt":0.15435077217530843,"score_spread":0.14853476641545907,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7025288158","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.10607501,0.004344119,0.0013201296,0.0018961908,0.00020526041,0.00044782477,0.00035846667,0.000034104814,0.8853189],"genre_scores_gemma":[0.7127666,0.005184351,0.0062193135,0.0011883033,0.00008169435,0.000025817526,0.000020702879,0.00012407672,0.27438915],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9962864,0.00030125718,0.0006415257,0.00065906654,0.0014717955,0.0006399532],"domain_scores_gemma":[0.99808705,0.00036695995,0.0005686304,0.0004362004,0.0000012139566,0.00053993124],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000048735226,0.00059948995,0.0006704624,0.000006213659,0.00036811715,0.00006538119,0.000571883,0.00014362777,0.00888256],"category_scores_gemma":[0.00001667003,0.0005462637,0.00011025306,0.0001277865,0.0012834012,0.000590264,0.0003081781,0.00030252856,2.272835e-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":[0.00083493564,0.00040242542,0.6740215,0.0016201541,0.00093981775,0.00024647298,0.0029115456,0.00023821955,0.03818095,0.1615019,0.018778741,0.100323334],"study_design_scores_gemma":[0.00069551927,0.0003780326,0.655984,0.0017450184,0.0002549331,0.000027240076,0.0066356394,0.002031636,0.073209345,0.009966704,0.24752915,0.0015427718],"about_ca_topic_score_codex":0.13646726,"about_ca_topic_score_gemma":0.3906551,"teacher_disagreement_score":0.6109297,"about_ca_system_score_codex":0.00005378529,"about_ca_system_score_gemma":0.0010322455,"threshold_uncertainty_score":0.9996989},"labels":[],"label_agreement":null},{"id":"W7025297386","doi":"","title":"Untersuchung des N. vagus mittels hochauflösenden Ultraschalls bei der Parkinsonerkrankung","year":2023,"lang":"de","type":"other","venue":"Qucosa (Saxon State and University Library Dresden)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Degeneration (medical); Substantia nigra; Context (archaeology); Cerebellar Degeneration","score_opus":0.010060263269420177,"score_gpt":0.19109271440208478,"score_spread":0.1810324511326646,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7025297386","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6260569,0.020867527,0.0023104737,0.0020450586,0.0022987537,0.0023902291,0.0021960149,0.0018018644,0.34003317],"genre_scores_gemma":[0.14621848,0.051434148,0.0021188913,0.00056505576,0.00039180336,0.000003441398,0.0001379617,0.00073629606,0.7983939],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9958276,0.0003252085,0.00044568503,0.0014978672,0.0006710397,0.001232576],"domain_scores_gemma":[0.9979376,0.00019818703,0.00040045974,0.0006727598,0.000013015846,0.0007779331],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00016113321,0.0009503569,0.0008644383,0.00004725412,0.0008138381,0.00028547613,0.00091092935,0.0006126295,0.015326707],"category_scores_gemma":[0.000011244854,0.0010132196,0.0003389052,0.0008126013,0.0014086955,0.0018177555,0.0010271376,0.0006962321,0.005817073],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017179818,0.001096559,0.27385053,0.0010118143,0.0056697093,0.009681655,0.018458024,0.00066122337,0.001753053,0.0018371964,0.41464168,0.26962057],"study_design_scores_gemma":[0.0018845425,0.00034014578,0.070044845,0.0005508128,0.0007543607,0.000018946006,0.0037122753,0.00019391545,0.0005228556,0.00048532436,0.91974217,0.0017498218],"about_ca_topic_score_codex":0.0016673155,"about_ca_topic_score_gemma":0.00074964884,"teacher_disagreement_score":0.5051005,"about_ca_system_score_codex":0.00023128082,"about_ca_system_score_gemma":0.00010739361,"threshold_uncertainty_score":0.9992318},"labels":[],"label_agreement":null},{"id":"W7025359114","doi":"","title":"Western Context 322 - A Miracle on the Prairies","year":2023,"lang":"en","type":"other","venue":"Bulletin of Miscellaneous Information (Royal Gardens Kew)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Miracle; Context (archaeology); Government (linguistics); Health care","score_opus":0.00720098420810173,"score_gpt":0.18124752387357482,"score_spread":0.1740465396654731,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7025359114","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005872674,0.000073224444,2.5252345e-7,0.00066075183,0.00019580494,0.00036861986,0.000044568813,0.00022976958,0.99783975],"genre_scores_gemma":[0.006932031,0.000081519785,0.00010549557,0.0010560408,0.00009671378,0.000029556928,0.000013015386,0.00016828418,0.99151736],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99872726,0.00005173336,0.00033871375,0.00015699703,0.00044246428,0.0002828591],"domain_scores_gemma":[0.9990543,0.0001476349,0.00036258387,0.00034486264,0.0000102415925,0.00008033651],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00018387029,0.00025708522,0.00024084593,0.0000021426451,0.00009315049,0.000036233923,0.00034566378,0.0002139541,0.62213695],"category_scores_gemma":[0.00005867393,0.00018360122,0.00011212699,0.000009315385,0.00029390914,1.8405882e-7,0.00015783793,0.0002071585,0.13038889],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022588913,0.00002992472,0.00012733747,0.00003228119,0.000024557216,0.000004485726,0.00025497086,0.00011487492,8.0839264e-8,0.000027915532,0.99603844,0.0033225308],"study_design_scores_gemma":[0.00015303135,0.00008939624,0.00032725744,0.00009098181,0.000020882033,0.000009674131,0.0002844571,0.0000059464037,0.0000029377277,0.000004195711,0.9988008,0.00021039715],"about_ca_topic_score_codex":0.011068717,"about_ca_topic_score_gemma":0.010987988,"teacher_disagreement_score":0.49174806,"about_ca_system_score_codex":0.000057716636,"about_ca_system_score_gemma":0.00000623156,"threshold_uncertainty_score":0.99551666},"labels":[],"label_agreement":null},{"id":"W7025363838","doi":"","title":"Volatility Connectedness of Bank Stocks Across the Atlantic","year":2013,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Social connectedness; Volatility (finance); Financial crisis; Quarter (Canadian coin); Debt; Implied volatility","score_opus":0.00655775546289671,"score_gpt":0.2192024528771684,"score_spread":0.2126446974142717,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7025363838","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":[0.9852272,0.000007571961,0.0019165195,0.0002656108,0.000051778967,0.00020066749,0.0000010073946,0.00002135996,0.01230828],"genre_scores_gemma":[0.9967381,0.000001626992,0.00036623204,0.00019977856,0.0000109138755,0.000014758744,7.3396785e-7,0.000004619352,0.0026632664],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993466,0.000025443624,0.00014017709,0.00013833253,0.00016172935,0.00018770662],"domain_scores_gemma":[0.9995715,0.00005619192,0.00004883206,0.0002723135,0.00000828844,0.000042863496],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00011831179,0.00007165159,0.00009194232,1.057999e-7,0.000104907835,0.00001685081,0.00023358274,0.000035569778,0.028345956],"category_scores_gemma":[0.000020471483,0.00003846246,0.000037922757,0.00011108507,0.0002948232,0.0000936156,0.00017089622,0.000060149294,0.0005524182],"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":[0.0000032118542,0.00003970055,0.98587626,0.00000309581,0.000005557485,2.5199307e-7,0.00068780326,0.00008673566,0.0026904356,0.00012132345,0.005197235,0.005288384],"study_design_scores_gemma":[0.000107198066,0.000027788981,0.9893226,0.0000018602301,0.0000033982667,0.0000013851475,0.00077037525,0.0072872853,0.00067255355,0.00043061134,0.001301614,0.00007330233],"about_ca_topic_score_codex":0.0116377985,"about_ca_topic_score_gemma":0.00066083117,"teacher_disagreement_score":0.027793538,"about_ca_system_score_codex":0.000020786925,"about_ca_system_score_gemma":0.0000033364252,"threshold_uncertainty_score":0.9949438},"labels":[],"label_agreement":null},{"id":"W7025412074","doi":"","title":"The use of allusions in Charles Lamb's Essays of Elia","year":2000,"lang":"en","type":"other","venue":"Library and Archives Canada (Government of Canada)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Power (physics); George (robot); Ridiculous; Reading (process)","score_opus":0.004144185887215866,"score_gpt":0.13662750525018055,"score_spread":0.13248331936296467,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7025412074","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.022224462,0.00049761916,0.00000928836,0.0006464541,0.00008324414,0.00019109818,0.00033160672,0.0000045037036,0.97601175],"genre_scores_gemma":[0.37139428,0.004149284,0.0010267516,0.00042608456,0.00003329538,0.000009313015,0.0000069454145,0.000106523796,0.6228475],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9982558,0.00004532921,0.00027552102,0.00017902846,0.0010389944,0.0002053315],"domain_scores_gemma":[0.9992696,0.00014588326,0.00024198179,0.00024372946,5.635085e-8,0.00009872822],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000007024737,0.000163257,0.00026108004,0.000001856115,0.00005996932,0.0000059231465,0.0002814747,0.000042062988,0.0012177546],"category_scores_gemma":[0.0000016511709,0.00012192429,0.000029330324,0.000073437375,0.00027449464,0.00008122431,0.00019967373,0.00010276241,6.7280115e-9],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00072528754,0.00025360825,0.32885602,0.0004440239,0.0002877178,0.00013845759,0.00043038963,0.002123467,0.013949198,0.027346723,0.53195554,0.093489595],"study_design_scores_gemma":[0.00023894453,0.000051480125,0.07013033,0.00026347005,0.000018939445,0.0000011229997,0.00050878763,0.000568413,0.0028970495,0.00023642449,0.92483413,0.00025090305],"about_ca_topic_score_codex":0.04234909,"about_ca_topic_score_gemma":0.3102809,"teacher_disagreement_score":0.39287862,"about_ca_system_score_codex":0.0000051233915,"about_ca_system_score_gemma":0.00026053024,"threshold_uncertainty_score":0.99969524},"labels":[],"label_agreement":null},{"id":"W7025448645","doi":"","title":"Violence Risk Assessment With the HCR-20V3 in Legal Contexts: A critical Reflection","year":2022,"lang":"en","type":"article","venue":"Data Archiving and Networked Services (DANS)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Risk assessment; Legal risk; Strengths and weaknesses; Mental health; Risk management; Legal profession; Risk management tools; Forensic psychology; Legal practice","score_opus":0.00701187948981888,"score_gpt":0.25521618523997386,"score_spread":0.24820430575015498,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7025448645","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":[0.9907211,0.00016747773,0.0053558154,0.0006801188,0.00008834184,0.00017437794,0.00008523105,0.000035420784,0.002692117],"genre_scores_gemma":[0.9974887,0.00019038677,0.0014524277,0.0005951527,0.000060425096,0.00005364705,0.00007868113,0.000014316775,0.000066286964],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983227,0.00035356332,0.0001666603,0.00049792515,0.0003286158,0.00033053386],"domain_scores_gemma":[0.99905974,0.00022304548,0.000076320735,0.0005634696,0.0000027781998,0.00007465686],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00070149975,0.00014694028,0.00013699627,0.0000023573664,0.0008376003,0.00008987826,0.0008103994,0.000018852106,0.00019946278],"category_scores_gemma":[0.0000052152413,0.00009850133,0.00001608046,0.0002730092,0.00022160597,0.0003013326,0.0014522583,0.000464845,0.0000053254257],"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":[0.00027689087,0.0002287061,0.88636255,0.000038346272,0.000034119355,0.00006074317,0.003911856,0.03927285,0.0005084066,0.00038759023,0.0010708492,0.067847095],"study_design_scores_gemma":[0.00039083697,0.00025991455,0.59777033,0.00009717269,0.000041547795,0.000050669616,0.0045324755,0.3787989,0.000003174621,0.00050829374,0.017292654,0.00025402513],"about_ca_topic_score_codex":0.006834376,"about_ca_topic_score_gemma":0.011146298,"teacher_disagreement_score":0.33952606,"about_ca_system_score_codex":0.00007556054,"about_ca_system_score_gemma":0.000015233197,"threshold_uncertainty_score":0.9997792},"labels":[],"label_agreement":null},{"id":"W7025472990","doi":"","title":"13–17-VUOTIAIDEN AKTIIVISTEN LIIKUNNANHARRASTAJIEN NUKKUMISTOTTUMUKSET JA VIREYSTILA","year":2019,"lang":"fi","type":"other","venue":"UTUPub (University of Turku)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"IBM; Quarter (Canadian coin); Work (physics)","score_opus":0.00597221097016557,"score_gpt":0.16868487751044836,"score_spread":0.1627126665402828,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7025472990","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.08489147,0.0006684051,0.0013309483,0.00081809715,0.0009973235,0.00093936996,0.0004230455,0.00013391553,0.90979743],"genre_scores_gemma":[0.14214002,0.00040229823,0.0020080577,0.00018922768,0.00018727609,6.163632e-7,0.000081916296,0.00018742892,0.85480314],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99599916,0.00016598235,0.00039833714,0.0013839469,0.0010694847,0.0009831131],"domain_scores_gemma":[0.99700254,0.00008791522,0.00094899954,0.0014200034,0.000043381297,0.0004971497],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00029605403,0.0008365414,0.0011794505,0.000026095024,0.00041752303,0.000064041415,0.0022021555,0.0008994859,0.11647255],"category_scores_gemma":[0.000026435298,0.000980686,0.00065756903,0.0005421175,0.0013293654,0.0004180552,0.0013748222,0.0006772714,0.021112034],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003490379,0.0007533897,0.028056508,0.000584493,0.0007291513,0.00039583075,0.006795253,0.0015664689,0.0026700015,0.00038466646,0.90713394,0.050581258],"study_design_scores_gemma":[0.0013132761,0.00032029668,0.042943172,0.0003498313,0.00035041381,0.000023697035,0.0040383,0.0010725714,0.00003478163,0.000051952527,0.9483334,0.0011683187],"about_ca_topic_score_codex":0.009859107,"about_ca_topic_score_gemma":0.0022531734,"teacher_disagreement_score":0.09536051,"about_ca_system_score_codex":0.0006890284,"about_ca_system_score_gemma":0.00014154451,"threshold_uncertainty_score":0.99926436},"labels":[],"label_agreement":null},{"id":"W7025506489","doi":"","title":"WM Announces Fourth Quarter and Full-Year 2021 Earnings \\n\\n\\tTamar Securities Financial Portal","year":2022,"lang":"en","type":"other","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Earnings; Quarter (Canadian coin); Broker-dealer","score_opus":0.002933327018203101,"score_gpt":0.17866801646707162,"score_spread":0.17573468944886853,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7025506489","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.027392913,0.0004253033,0.00006976251,0.00015182233,0.00029149617,0.00018932046,0.000050000737,0.000086297376,0.9713431],"genre_scores_gemma":[0.011096543,0.00037866127,0.0016975995,0.00037548377,0.00039714764,0.00004231593,0.000050190185,0.00015657973,0.98580545],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9984896,0.000039261446,0.00018134201,0.0005131589,0.00043870692,0.00033788802],"domain_scores_gemma":[0.9994984,0.000014726273,0.00014931471,0.00023107343,0.0000024418935,0.00010399783],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00010835406,0.00029200947,0.00028787737,0.0000032921582,0.00016552172,0.000053063297,0.00022676423,0.00018539107,0.49901736],"category_scores_gemma":[0.0000116614265,0.00025561597,0.00008197694,0.00012462484,0.00029531177,0.00007561844,0.00033527554,0.00028407358,0.0006100018],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008539585,0.000026740625,0.0268056,0.000012376625,0.000014002852,0.000036716756,0.00034073598,0.0000059230415,0.000011852542,0.00021855715,0.9713252,0.0011937461],"study_design_scores_gemma":[0.00020536991,0.00018472142,0.01063867,0.000015055322,0.000018725856,0.000015944175,0.001219889,0.000026491682,8.685381e-7,0.00007065021,0.9872143,0.0003892805],"about_ca_topic_score_codex":0.0011693551,"about_ca_topic_score_gemma":0.0017378065,"teacher_disagreement_score":0.49840733,"about_ca_system_score_codex":0.000043384982,"about_ca_system_score_gemma":0.00002477565,"threshold_uncertainty_score":0.9999896},"labels":[],"label_agreement":null},{"id":"W7025564977","doi":"","title":"Vox populi : \\n Salon du livre de Montréal 2006","year":2007,"lang":"fr","type":"article","venue":"Érudit (Université de Montréal)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Nucleofection; Gestational period; TSG101; Liquation; Dysgeusia; Diafiltration; Emperipolesis; Triacetin; Demotion","score_opus":0.003083926212059932,"score_gpt":0.14974967464075883,"score_spread":0.1466657484286989,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7025564977","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":[0.8440731,0.08357991,0.009958738,0.039288055,0.0008455204,0.0003424697,0.00007227995,0.00016051819,0.02167938],"genre_scores_gemma":[0.746331,0.017937616,0.007923749,0.0011783106,0.0005652797,0.0000026173045,0.00002195561,0.00009109535,0.22594841],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9968833,0.00010561692,0.0003297729,0.00066852744,0.00054889184,0.0014639097],"domain_scores_gemma":[0.9982873,0.00009753098,0.00023817182,0.0005561437,0.000026509068,0.00079431554],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0005521331,0.00046643548,0.00038646863,0.000010622991,0.0013232309,0.00004737437,0.000626345,0.0004860009,0.004603472],"category_scores_gemma":[0.000031378793,0.00054840476,0.000297967,0.00056178664,0.0004817401,0.00037114296,0.0006518522,0.00044045842,0.0028949461],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037057104,0.00058540254,0.11926265,0.000043360764,0.00014117554,0.010131094,0.002453927,0.004419417,0.0036940651,0.0071979053,0.63053423,0.22116622],"study_design_scores_gemma":[0.0009664017,0.00024941473,0.10829588,0.000048830985,0.00017042343,0.0007658339,0.0019569038,0.002736134,0.00039166686,0.00051712536,0.8833126,0.0005888245],"about_ca_topic_score_codex":0.26798767,"about_ca_topic_score_gemma":0.3890468,"teacher_disagreement_score":0.25277835,"about_ca_system_score_codex":0.01759703,"about_ca_system_score_gemma":0.000049547532,"threshold_uncertainty_score":0.99997693},"labels":[],"label_agreement":null},{"id":"W7025606599","doi":"","title":"2002 Week 10: Patriots at Bears","year":2020,"lang":"en","type":"other","venue":"Bulletin of Miscellaneous Information (Royal Gardens Kew)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Quarter (Canadian coin); Need to know; George (robot); Theme (computing); Face (sociological concept)","score_opus":0.0052228402985705,"score_gpt":0.16553429749256895,"score_spread":0.16031145719399845,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7025606599","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00009535773,0.00023830397,4.58836e-7,0.00019637751,0.00017692956,0.00032594218,0.00008763174,0.00015251111,0.9987265],"genre_scores_gemma":[0.00023244348,0.00027280842,0.0016854318,0.00053218834,0.00012410419,0.000010713632,0.000057069214,0.00012856422,0.9969567],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9983309,0.000041321746,0.00048133405,0.00027042144,0.0005488997,0.00032714414],"domain_scores_gemma":[0.9989332,0.00003900296,0.00048008026,0.00033459946,0.000012011966,0.0002010976],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000088660985,0.00034100853,0.00037289018,0.0000025209163,0.00008107926,0.000027885895,0.00040058955,0.0003557156,0.98261845],"category_scores_gemma":[0.000047390742,0.00032754423,0.00016445098,0.000011119003,0.00023491867,1.6084974e-7,0.0003484069,0.00020446104,0.31114578],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000044412674,0.000031861102,0.000018450746,0.000088965266,0.000026348362,0.000021568827,0.00009709034,0.0003562003,7.654444e-7,0.0000015062255,0.99664485,0.0026679926],"study_design_scores_gemma":[0.0003166898,0.00016309452,0.00006729765,0.000051724302,0.000036443296,0.000024238429,0.000041647887,0.00003444636,0.0000055132023,0.0000014551817,0.998907,0.00035040706],"about_ca_topic_score_codex":0.0045594396,"about_ca_topic_score_gemma":0.0012253775,"teacher_disagreement_score":0.67147267,"about_ca_system_score_codex":0.00011699389,"about_ca_system_score_gemma":0.000009590874,"threshold_uncertainty_score":0.9999177},"labels":[],"label_agreement":null},{"id":"W7025679081","doi":"","title":"Активизация \"венгерского фактора\" во внешней политике Московского государства (последняя четверть XV - первая четверть XVI в.)","year":2015,"lang":"en","type":"article","venue":"Digital Library of the Belarusian State University (Belarusian State University)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Duchy; Treaty; Quarter (Canadian coin); Prestige; Empire; Foreign policy","score_opus":0.00674115430507716,"score_gpt":0.14533955002690338,"score_spread":0.13859839572182622,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7025679081","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":[0.6788799,0.000073249015,0.0011271635,0.0012977236,0.00043779667,0.000777721,0.0017748163,0.00042393594,0.31520766],"genre_scores_gemma":[0.76826423,0.00019541713,0.0019208986,0.0004570659,0.000069772635,5.575479e-7,0.00021576714,0.00014878983,0.22872749],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9948988,0.0003589627,0.00063599757,0.0013589755,0.0013051676,0.0014421017],"domain_scores_gemma":[0.99621326,0.000121235316,0.00076681504,0.0015093585,0.00008609276,0.0013032452],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00025231697,0.0009374308,0.00088160584,0.000118236676,0.00095174165,0.00029740122,0.0031512403,0.00033361287,0.0017335578],"category_scores_gemma":[0.000047316225,0.00091505307,0.0007129099,0.003095739,0.0019770297,0.0063462947,0.004281968,0.0008036612,0.0009879662],"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":[0.008300188,0.004648252,0.58242035,0.00039668404,0.0025234339,0.01139052,0.026803128,0.016292486,0.0018764965,0.021060785,0.23892404,0.08536363],"study_design_scores_gemma":[0.0040604584,0.00057769404,0.030881682,0.00013925837,0.00023317897,0.00009884581,0.008790073,0.00054084556,0.0007805365,0.0030923572,0.9489626,0.001842466],"about_ca_topic_score_codex":0.0008133329,"about_ca_topic_score_gemma":0.00018146084,"teacher_disagreement_score":0.71003854,"about_ca_system_score_codex":0.0007704526,"about_ca_system_score_gemma":0.00044374104,"threshold_uncertainty_score":0.9997899},"labels":[],"label_agreement":null},{"id":"W7026535994","doi":"","title":"Anoxygenic photosynthetic communities and heavy element transformations in extreme environments: hydrothermal and hypersaline ecosystems","year":2011,"lang":"en","type":"dissertation","venue":"Mspace (University of Manitoba)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Natural Sciences and Engineering Research Council of Canada; Université du Québec à Montréal; University of Washington","keywords":"Anoxygenic photosynthesis; Phototroph; Hydrothermal vent; Extremophile; Photosynthesis; Microbial mat; Anaerobic respiration","score_opus":0.017653916857818766,"score_gpt":0.1755409633480901,"score_spread":0.15788704649027135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7026535994","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":[0.9926619,0.00031600043,0.00013254714,0.00006373277,0.000046807592,0.0003638946,0.000024016827,0.000012564138,0.006378554],"genre_scores_gemma":[0.99699837,0.0013329352,0.00031792244,0.000014317174,0.00000554528,0.0000022094105,0.00007749125,0.000018199109,0.0012330139],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99919254,0.000076173834,0.00014600455,0.00019291636,0.00019571008,0.00019665842],"domain_scores_gemma":[0.99955714,0.000020000218,0.00014985542,0.00019784067,0.000003244447,0.00007190075],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012447251,0.00019856192,0.0002744615,0.000012710996,0.00019894127,0.000010899193,0.00020406165,0.00014444771,0.0004194087],"category_scores_gemma":[0.0000010659716,0.00024053598,0.000050675208,0.00007509333,0.00018647454,0.00020927461,0.00007520416,0.00017078497,0.000029669152],"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":[0.0010238315,0.0012539974,0.87831026,0.0009080114,0.00037916517,0.00006645906,0.07651964,0.0005193365,0.017289415,0.00039202036,0.0009084798,0.022429384],"study_design_scores_gemma":[0.0014382711,0.00024420474,0.7641132,0.00026608503,0.00017918578,0.000010776698,0.22135335,0.0036398561,0.0009825551,0.00007541294,0.0070667285,0.0006304111],"about_ca_topic_score_codex":0.023141263,"about_ca_topic_score_gemma":0.69290394,"teacher_disagreement_score":0.6697627,"about_ca_system_score_codex":0.00011274406,"about_ca_system_score_gemma":0.000008827433,"threshold_uncertainty_score":0.98336375},"labels":[],"label_agreement":null},{"id":"W7026629167","doi":"","title":"Associação entre fragilidade e tempo de velocidade da marcha em idosos hospitalizados","year":2018,"lang":"pt","type":"other","venue":"Lume (Universidade Federal do Rio Grande do Sul)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Poison control; Elderly people; Body weight","score_opus":0.006464556225617268,"score_gpt":0.21230237575211666,"score_spread":0.2058378195264994,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7026629167","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.48950943,0.0020972425,0.0054330165,0.0028061243,0.0027286608,0.0033236959,0.0006632312,0.00077914464,0.49265945],"genre_scores_gemma":[0.48153734,0.0007200035,0.0014888798,0.0007334258,0.000836529,0.000038668943,0.00018102507,0.0006338777,0.51383024],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9905207,0.00062943844,0.00093628233,0.002762191,0.0020660153,0.0030853532],"domain_scores_gemma":[0.99550676,0.0001509336,0.0011725188,0.00162648,0.00008252973,0.0014607479],"candidate_categories":["metaepi_narrow","sts","scholarly_communication","research_integrity","insufficient_payload"],"consensus_categories":["metaepi_narrow","insufficient_payload"],"category_scores_codex":[0.00063304947,0.0020369987,0.0018158723,0.00006591529,0.0020516645,0.0015768666,0.002700452,0.0024668372,0.17671525],"category_scores_gemma":[0.000089034445,0.0022264726,0.0012065874,0.0012631535,0.0015760412,0.0007424534,0.001494473,0.0016227532,0.015082354],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00087961275,0.0015223519,0.24082536,0.0006750861,0.0023775478,0.0019715517,0.0343071,0.00022407985,0.0018849168,0.0015927817,0.6645357,0.049203884],"study_design_scores_gemma":[0.0097444365,0.0014752775,0.12367166,0.0015628831,0.0009872776,0.00016492444,0.037119582,0.0016622473,0.00020140412,0.002482128,0.8143968,0.006531393],"about_ca_topic_score_codex":0.0038087587,"about_ca_topic_score_gemma":0.0017744788,"teacher_disagreement_score":0.1616329,"about_ca_system_score_codex":0.002811793,"about_ca_system_score_gemma":0.00034979687,"threshold_uncertainty_score":0.99945956},"labels":[],"label_agreement":null},{"id":"W7026644362","doi":"","title":"ARCHIVEIT-3490-TWELVE_HOURS-BDBRNE-20130212171817-00000-wbgrp-crawl065.us.archive.org-6681.warc.gz","year":2013,"lang":"en","type":"other","venue":"Bulletin of Miscellaneous Information (Royal Gardens Kew)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Process (computing); Identification (biology); Product (mathematics)","score_opus":0.004144560475915567,"score_gpt":0.1724001223558993,"score_spread":0.16825556187998372,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7026644362","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0010961862,0.00017947982,0.000015151403,0.00018605983,0.00045209643,0.0009674284,0.00021194364,0.00031810364,0.99657357],"genre_scores_gemma":[0.001943881,0.0005970039,0.004501517,0.00083834596,0.00032565673,0.000076105774,0.00027841245,0.00030074874,0.99113834],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9962487,0.0001554661,0.0010383283,0.0006169651,0.0010405529,0.0008999434],"domain_scores_gemma":[0.99746865,0.00013030275,0.0010006834,0.00091747445,0.00003826698,0.00044459404],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0002620646,0.0008379144,0.00081456546,0.000016950084,0.00020466853,0.00010302839,0.0010959089,0.0005849573,0.8790566],"category_scores_gemma":[0.00007336804,0.0007755266,0.000394145,0.000026613388,0.00080557005,0.0000012890065,0.00061819446,0.00068076584,0.2023299],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000055075583,0.000113346614,0.00041422452,0.00021457356,0.000082794606,0.00002311655,0.00024428056,0.00038675073,0.000007319067,0.000030254603,0.99383825,0.0045900205],"study_design_scores_gemma":[0.00064679,0.00023864477,0.00115588,0.00020982263,0.00008237299,0.00006611552,0.00014720073,0.000102160084,0.000016528476,0.00003817156,0.99644077,0.000855519],"about_ca_topic_score_codex":0.021948187,"about_ca_topic_score_gemma":0.0022211925,"teacher_disagreement_score":0.6767267,"about_ca_system_score_codex":0.00014738254,"about_ca_system_score_gemma":0.000039493185,"threshold_uncertainty_score":0.9994696},"labels":[],"label_agreement":null},{"id":"W7026693861","doi":"","title":"As crianças-soldado no direito internacional criminal : da responsabilidade do adulto à eventual responsabilidade da criança-soldado","year":2015,"lang":"pt","type":"dissertation","venue":"Repositório Institucional da Universidade Católica Portuguesa (Universidade Católica Portuguesa)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Centers for Disease Control and Prevention; Institute for Catastrophic Loss Reduction","keywords":"Criminal responsibility; Criminal liability; Criminal law; Action (physics)","score_opus":0.02093638380716569,"score_gpt":0.27180783012301746,"score_spread":0.2508714463158518,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7026693861","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":[0.860387,0.002881062,0.00045882227,0.005516819,0.008306923,0.0054650754,0.002951104,0.0013106404,0.1127225],"genre_scores_gemma":[0.8396152,0.0013903887,0.0024977303,0.001597477,0.0021045702,0.00023382856,0.010237656,0.0009889528,0.14133416],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.96805084,0.0021781758,0.005343536,0.009361525,0.009410372,0.0056555304],"domain_scores_gemma":[0.97654,0.0012935632,0.005657663,0.0065541975,0.0025350666,0.007419492],"candidate_categories":["metaepi_narrow","sts","scholarly_communication","open_science","research_integrity","insufficient_payload"],"consensus_categories":["metaepi_narrow","sts","research_integrity","insufficient_payload"],"category_scores_codex":[0.0031193902,0.006096277,0.0051782355,0.00091590045,0.0037461985,0.0017309499,0.008533476,0.005368124,0.022089258],"category_scores_gemma":[0.0024664465,0.0071797203,0.0037122022,0.004815076,0.0047984384,0.0052406043,0.0041218344,0.0066520437,0.008273612],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":true,"about_ca_system_consensus":true,"study_design_scores_codex":[0.085888624,0.01922567,0.01725025,0.004359251,0.011259163,0.0714011,0.07670395,0.0056295297,0.1812192,0.08106953,0.37838787,0.06760586],"study_design_scores_gemma":[0.0125009725,0.0060352157,0.051286455,0.00448706,0.006836019,0.005986527,0.07887172,0.0016809434,0.0023830407,0.0008191371,0.81531036,0.013802547],"about_ca_topic_score_codex":0.007740988,"about_ca_topic_score_gemma":0.0009969713,"teacher_disagreement_score":0.4369225,"about_ca_system_score_codex":0.012187915,"about_ca_system_score_gemma":0.008517879,"threshold_uncertainty_score":0.99930537},"labels":[],"label_agreement":null},{"id":"W7026850792","doi":"","title":"Appetitive-to-aversive CS-counterconditioning, positive transfer of excitatory conditioning","year":2001,"lang":"en","type":"other","venue":"Library and Archives Canada (Government of Canada)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Conditioning; Classical conditioning; Stimulus (psychology); Reinforcement; Conditioned response; Aversive Stimulus; Unconditioned stimulus; Operant conditioning","score_opus":0.0016634229137887098,"score_gpt":0.13490158893757018,"score_spread":0.13323816602378147,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7026850792","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.015173627,0.00011194076,0.000998752,0.00035088483,0.00013226121,0.00025858724,0.001012864,0.000011713842,0.9819494],"genre_scores_gemma":[0.58364654,0.0001547025,0.0008965672,0.001738832,0.000070258015,0.000015131025,0.0000453367,0.00013737258,0.41329524],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99789536,0.000042741063,0.00024188642,0.00032895393,0.0012134672,0.00027757694],"domain_scores_gemma":[0.99936974,0.00008065675,0.00014726484,0.00016305417,2.7619856e-7,0.00023899344],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00000684079,0.00025693345,0.000333763,0.0000049609316,0.00010205139,0.000009289267,0.000218113,0.000058782603,0.008363309],"category_scores_gemma":[0.0000013254995,0.00026670756,0.000044328914,0.00009246319,0.00025520337,0.00014578755,0.00011725615,0.00013174157,8.1221586e-8],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000917748,0.00033171495,0.18941976,0.0008527806,0.0013226528,0.0009957819,0.0020658267,0.0014137966,0.050964672,0.08930833,0.652218,0.010188964],"study_design_scores_gemma":[0.0014671584,0.0005132106,0.16235678,0.0019380263,0.00018601066,0.000028228396,0.012823451,0.00023401152,0.054078013,0.000746799,0.76396,0.0016683085],"about_ca_topic_score_codex":0.019003859,"about_ca_topic_score_gemma":0.04576605,"teacher_disagreement_score":0.5686541,"about_ca_system_score_codex":0.000021038308,"about_ca_system_score_gemma":0.00029252953,"threshold_uncertainty_score":0.99997854},"labels":[],"label_agreement":null},{"id":"W7027019218","doi":"","title":"Bulletin d'information : Volume 4, no 1, hiver 2007","year":2009,"lang":"fr","type":"other","venue":"Érudit documents and data repository (Érudit Consortium, University of Montreal)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Egerton University; Ruppin Academic Center; Université Lumière Lyon 2; HEC Montréal; Université de Rouen; McMaster University; De La Salle University; Université de Tunis; Universidad del Rosario; Université Laval; University of Connecticut","keywords":"Volume (thermodynamics); Noise (video); Term (time); Line (geometry)","score_opus":0.004418665139744417,"score_gpt":0.17764657875156228,"score_spread":0.17322791361181786,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7027019218","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.010471371,0.0040439456,0.0019363764,0.0019519702,0.0017740391,0.0012385478,0.0019952583,0.00012928808,0.9764592],"genre_scores_gemma":[0.0130176,0.012008267,0.0037132802,0.00030242224,0.0003808537,0.0000011707206,0.00093402865,0.0000676558,0.96957475],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9967976,0.00017476865,0.0006442415,0.0010413799,0.00071396853,0.00062801136],"domain_scores_gemma":[0.9965347,0.000099145036,0.0011788517,0.0016324575,0.00009792345,0.0004569415],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0002472263,0.00063795276,0.00077366084,0.000021587588,0.00066971185,0.00011873699,0.0014263445,0.00053838716,0.05157962],"category_scores_gemma":[0.00007752471,0.0007139014,0.00014400238,0.00017300958,0.0010987035,0.001095497,0.0013443432,0.00036600808,0.00522275],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020787143,0.00025096725,0.0111471545,0.00018199964,0.0002737054,0.00031362797,0.0001585714,0.000080542966,0.00006154173,0.00010529423,0.9302097,0.057008997],"study_design_scores_gemma":[0.0013410948,0.00025034475,0.037156858,0.00028033537,0.00047539943,0.00007162832,0.00030177677,0.0004535519,0.000010592565,0.000019735413,0.95896965,0.0006690579],"about_ca_topic_score_codex":0.057294976,"about_ca_topic_score_gemma":0.006247483,"teacher_disagreement_score":0.05633994,"about_ca_system_score_codex":0.0007075883,"about_ca_system_score_gemma":0.000100373894,"threshold_uncertainty_score":0.9995312},"labels":[],"label_agreement":null},{"id":"W7027294069","doi":"","title":"Commentary on: âThe future of health care in Canadaâ","year":2002,"lang":"en","type":"article","venue":"Europe PMC (PubMed Central)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Health care; MEDLINE; Public health; Work (physics); Health services","score_opus":0.008677361659782125,"score_gpt":0.19143559961724022,"score_spread":0.1827582379574581,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7027294069","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":[0.9566008,0.0020097508,0.000008981804,0.018308656,0.0005571,0.0004333172,0.000024432415,0.000028705175,0.022028256],"genre_scores_gemma":[0.98903793,0.00048301526,0.00020638187,0.009561726,0.0001354353,0.000013475868,0.000006964689,0.000021787488,0.0005333027],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9982997,0.00014078875,0.0002762768,0.00027223915,0.0003059667,0.00070503383],"domain_scores_gemma":[0.999362,0.000013489883,0.00010175234,0.00029485923,0.0000038981398,0.00022397954],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00013710397,0.00014935972,0.00019159398,0.0000021595563,0.00007884322,0.000008877741,0.00027898216,0.00003416391,0.0021227743],"category_scores_gemma":[0.000007937738,0.00012722674,0.0000398697,0.00031582883,0.00009066772,0.00005810133,0.000090324414,0.00017960786,0.00007137825],"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":[0.00002843705,0.00023955115,0.40613878,0.000025472023,0.000011120822,0.00005248715,0.018679459,0.0008260545,0.000026906402,0.000065506894,0.3411466,0.23275965],"study_design_scores_gemma":[0.00041344785,0.00010402354,0.45841,0.000014407636,0.0000031717946,0.0000020238072,0.0009464119,0.000044974648,0.00009958767,0.0000039451297,0.53981316,0.0001448786],"about_ca_topic_score_codex":0.0036248781,"about_ca_topic_score_gemma":0.004067255,"teacher_disagreement_score":0.23261477,"about_ca_system_score_codex":0.0004807934,"about_ca_system_score_gemma":0.000013738492,"threshold_uncertainty_score":0.9987894},"labels":[],"label_agreement":null},{"id":"W7027888953","doi":"","title":"DNV Completes Technical Review of Canadian Solar's TOPCon Modules","year":2024,"lang":"en","type":"other","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Work (physics); Term (time); Quality (philosophy); Context (archaeology)","score_opus":0.011498485441613507,"score_gpt":0.22483682401316687,"score_spread":0.21333833857155338,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7027888953","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0000052626847,0.021012932,0.000084540916,0.0007001975,0.0001091424,0.00023833035,0.000041233026,0.00007990471,0.9777284],"genre_scores_gemma":[0.0005742157,0.017820517,0.0067962334,0.0015939403,0.00007056759,0.000017433502,0.000016853397,0.00019654662,0.9729137],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990826,0.000014833755,0.0001965064,0.00029038504,0.00020071684,0.00021494487],"domain_scores_gemma":[0.99944305,0.0000065169575,0.00006590085,0.00033528043,0.0000021553158,0.0001470995],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00009253456,0.0001755916,0.00031627485,0.0000056051667,0.000015110567,0.000008271928,0.0002830212,0.00016355436,0.16967817],"category_scores_gemma":[0.000011217283,0.00013218382,0.00010644705,0.00029196983,0.00017329512,0.000012968057,0.0001301175,0.00013881645,0.0036777863],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[1.3410754e-7,0.0000064098945,0.00015354743,0.00065869495,0.000009939031,0.000005528587,0.0000024754668,3.5398992e-7,0.000032502576,0.00049302494,0.99582005,0.0028173614],"study_design_scores_gemma":[0.000018487024,0.00001775453,0.0002590065,0.0023613423,0.000032046064,0.0000040789505,0.0000052693567,0.000008663171,0.000009971007,0.00014503823,0.99697375,0.00016461556],"about_ca_topic_score_codex":0.32141337,"about_ca_topic_score_gemma":0.3693793,"teacher_disagreement_score":0.16600038,"about_ca_system_score_codex":0.00008543013,"about_ca_system_score_gemma":0.00002115879,"threshold_uncertainty_score":0.99709797},"labels":[],"label_agreement":null},{"id":"W7028128183","doi":"","title":"download [PDF] Meet Me Halfway (Learning to Love Series) BY Lilian T. James epub Download","year":2024,"lang":"en","type":"other","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Download; Popularity; Plot (graphics); Performance art; Canadian literature","score_opus":0.008428383228975227,"score_gpt":0.20898448125991329,"score_spread":0.20055609803093805,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7028128183","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000267956,0.0005382894,0.00048758244,0.0016286802,0.00022882452,0.0006125951,0.0006403794,0.0011781848,0.9944175],"genre_scores_gemma":[0.0024959338,0.00050581165,0.0003603341,0.00047326367,0.00020461518,1.8416607e-7,0.0014335451,0.00468705,0.98983926],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9969552,0.00027320898,0.00032305563,0.0010287093,0.0007298699,0.0006899127],"domain_scores_gemma":[0.9986852,0.000010882572,0.000164665,0.0006369623,0.000045963214,0.00045635577],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0004372141,0.00042453257,0.00033775056,0.00002997455,0.00064610434,0.00085544656,0.0013561453,0.00025351858,0.5707095],"category_scores_gemma":[0.00022029612,0.00041524065,0.00011013952,0.0008047209,0.00031585895,0.000178469,0.0025754203,0.00057525234,0.6146654],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026065845,0.000059645954,0.0000049883683,0.000058507147,0.000060841812,0.000027938948,0.0011709812,0.00006869695,0.0013129477,0.00007832025,0.9825074,0.014623687],"study_design_scores_gemma":[0.00019197294,0.00028483436,0.000015593521,0.00008337955,0.00003307961,0.00004588813,0.0006965457,0.00003552886,0.00011999057,0.000037156147,0.99797153,0.00048452197],"about_ca_topic_score_codex":0.00028515156,"about_ca_topic_score_gemma":0.0000068259446,"teacher_disagreement_score":0.04395586,"about_ca_system_score_codex":0.00033382903,"about_ca_system_score_gemma":0.0000034935258,"threshold_uncertainty_score":0.99982995},"labels":[],"label_agreement":null},{"id":"W7028531102","doi":"","title":"Firmin Picard et la rencontre de trois cultures littÃ©raires","year":2001,"lang":"fr","type":"other","venue":"Library and Archives Canada (Government of Canada)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Ethnic group; Subject (documents); Identity (music); Natural (archaeology)","score_opus":0.0018725070481325195,"score_gpt":0.15140071620237341,"score_spread":0.1495282091542409,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7028531102","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.03238069,0.0016643928,0.00031724139,0.00728555,0.0002043699,0.00023408345,0.00032360264,0.000014516966,0.95757556],"genre_scores_gemma":[0.36196783,0.0019989803,0.0046348283,0.0031114195,0.00015690445,0.000015065024,0.000009565917,0.000092721384,0.6280127],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9967613,0.00024491834,0.0003599615,0.0004955384,0.001553211,0.0005850317],"domain_scores_gemma":[0.99858904,0.00030076836,0.000281348,0.00031204362,1.8908278e-7,0.00051662803],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000020480318,0.0004563441,0.0004792938,0.0000022538645,0.00019251714,0.00005008683,0.0004664754,0.0001370427,0.009105584],"category_scores_gemma":[0.0000065921313,0.00041093637,0.00008252779,0.00009602157,0.00040036716,0.00021922916,0.00031866753,0.00033082953,8.99402e-8],"study_design_candidate":"not_applicable","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":[0.00049379445,0.00024983298,0.48827484,0.00047372121,0.00050968304,0.001407388,0.0015755801,0.001451096,0.016588345,0.11939829,0.15707831,0.21249913],"study_design_scores_gemma":[0.00038629322,0.0000937823,0.17304564,0.00033601138,0.000063756925,0.000035042303,0.0029331245,0.0006107736,0.00310038,0.001155524,0.8177095,0.00053020107],"about_ca_topic_score_codex":0.103706494,"about_ca_topic_score_gemma":0.37055734,"teacher_disagreement_score":0.6606312,"about_ca_system_score_codex":0.00003569085,"about_ca_system_score_gemma":0.0010410411,"threshold_uncertainty_score":0.99983424},"labels":[],"label_agreement":null},{"id":"W7035843063","doi":"","title":"ARCHIVEIT-3490-TWELVE_HOURS-FHKNCU-20130203170041-00000-crawling113.us.archive.org-6680.warc.gz","year":2013,"lang":"en","type":"other","venue":"Bulletin of Miscellaneous Information (Royal Gardens Kew)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Process (computing); Identification (biology); Product (mathematics)","score_opus":0.00416211611229367,"score_gpt":0.17191492790834134,"score_spread":0.16775281179604767,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7035843063","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0009589195,0.00014698443,0.00002137708,0.00017281798,0.00043026137,0.00090828724,0.00017847974,0.00032533112,0.9968575],"genre_scores_gemma":[0.00225,0.00046380734,0.0049001165,0.000771882,0.00034067655,0.00006512628,0.00023591975,0.00028751453,0.990685],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99645865,0.00014138728,0.0010063432,0.00057734497,0.0009748514,0.00084144744],"domain_scores_gemma":[0.99760175,0.00012599942,0.000980039,0.00084635336,0.000036521167,0.00040935658],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00025753764,0.00078164315,0.0007641441,0.000015678252,0.0001933939,0.00009697244,0.0010234558,0.0005459694,0.85739493],"category_scores_gemma":[0.00007976576,0.0007244936,0.0003765455,0.000023626408,0.000736896,0.0000010768847,0.0005728167,0.00064661587,0.1857841],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000510941,0.00010241238,0.00032415293,0.00020813571,0.00007747686,0.000020621526,0.00021311692,0.00047396767,0.000008006867,0.000035753503,0.99482095,0.0036643064],"study_design_scores_gemma":[0.0006226254,0.00022213829,0.00066516065,0.00021182427,0.00007691726,0.00005725825,0.00013066689,0.00012784233,0.000017335211,0.0000486638,0.9970204,0.0007991249],"about_ca_topic_score_codex":0.023003545,"about_ca_topic_score_gemma":0.0020305712,"teacher_disagreement_score":0.6716108,"about_ca_system_score_codex":0.00013377571,"about_ca_system_score_gemma":0.000035916513,"threshold_uncertainty_score":0.9995206},"labels":[],"label_agreement":null},{"id":"W7035900825","doi":"","title":"Analyse de l'applicabilité de la réglementation pour un changement rapide des comportements citoyens québécois en gestion des matières résiduelles","year":2016,"lang":"fr","type":"other","venue":"Knowledge UdeS (Institutional Deposit of the University of Sherbrooke)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Poison control; Limiting; Illicit drug","score_opus":0.009352360164844156,"score_gpt":0.21484917411859256,"score_spread":0.20549681395374841,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7035900825","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":[0.74314624,0.0031973997,0.16490668,0.00022172823,0.00013451006,0.00058004557,0.00003769573,0.00003131866,0.08774437],"genre_scores_gemma":[0.9279672,0.0033238255,0.04149163,0.000025182728,0.00009957405,0.0000049847,0.000012369613,0.000042718486,0.02703252],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.997794,0.00054109405,0.0003972366,0.00043626328,0.0004267389,0.0004047143],"domain_scores_gemma":[0.9989021,0.0001907983,0.00031782562,0.00035654815,0.000055521796,0.00017724944],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00052672863,0.00037582533,0.0004068019,0.000025016869,0.0006768388,0.000020116244,0.00081518886,0.00033808284,0.0073838253],"category_scores_gemma":[0.00005260479,0.00032651285,0.0003424535,0.00023834483,0.0032219035,0.00017705973,0.0005051983,0.00018673687,0.00018821648],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002130821,0.0018205083,0.5564022,0.0032201617,0.0010711334,0.000021216789,0.021398133,0.04221796,0.25766128,0.006693707,0.005131211,0.10414943],"study_design_scores_gemma":[0.0015966295,0.00014238649,0.88760376,0.004682971,0.0008384648,0.000032049986,0.0017735662,0.0074312496,0.0491405,0.0029955646,0.043240406,0.0005224493],"about_ca_topic_score_codex":0.03129769,"about_ca_topic_score_gemma":0.10654052,"teacher_disagreement_score":0.33120158,"about_ca_system_score_codex":0.0053038895,"about_ca_system_score_gemma":0.00022965546,"threshold_uncertainty_score":0.9999187},"labels":[],"label_agreement":null},{"id":"W7036126531","doi":"","title":"$$$ AVG Phone number*USA**1800-445-2790**AUS*1800059007 AVG tech support number AVG tech support phone number","year":2016,"lang":"en","type":"other","venue":"OSF Preprints (OSF Preprints)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Phone; Service (business); Phone call; Telephone number; Mobile phone","score_opus":0.008429456093453967,"score_gpt":0.2505507607870762,"score_spread":0.24212130469362225,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7036126531","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.007368603,0.0000025036677,0.003502731,0.0003312268,0.0016146098,0.0023291658,0.00025432874,0.0009564979,0.9836403],"genre_scores_gemma":[0.013476209,0.0008130645,0.007026777,0.00071078615,0.0007596686,0.0009576562,0.00016994866,0.0012895337,0.97479635],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9860413,0.0006556623,0.0020480494,0.00601917,0.0025858171,0.0026500002],"domain_scores_gemma":[0.98930866,0.00036257625,0.0016869899,0.007214556,0.000108031454,0.0013191703],"candidate_categories":["metaepi_narrow","research_integrity","insufficient_payload"],"consensus_categories":["metaepi_narrow","insufficient_payload"],"category_scores_codex":[0.003689912,0.0021479724,0.0020335997,0.000042551277,0.00055637426,0.00029066153,0.004101329,0.0022570335,0.99725884],"category_scores_gemma":[0.00048953673,0.0020872997,0.0009822383,0.0010584525,0.0015340475,0.00056171295,0.004926497,0.0019396341,0.99790484],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013533841,0.0010017297,0.1425746,0.00014780744,0.0004019206,0.0003066385,0.00052310876,0.000024162688,0.0018614811,0.00015093439,0.84475386,0.008118428],"study_design_scores_gemma":[0.0016891707,0.000002295291,0.0069194054,0.00022249705,0.00029234673,0.00058238045,0.00013809316,0.000025479349,0.0025200765,0.0012436062,0.98386866,0.002495993],"about_ca_topic_score_codex":0.0043580397,"about_ca_topic_score_gemma":0.0007916592,"teacher_disagreement_score":0.1391148,"about_ca_system_score_codex":0.0016825569,"about_ca_system_score_gemma":0.00038854862,"threshold_uncertainty_score":0.9991261},"labels":[],"label_agreement":null},{"id":"W7036658958","doi":"","title":"08/07/20: Corporate Presentation – Second Quarter 2020 Results","year":2020,"lang":"en","type":"other","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Quarter (Canadian coin); Presentation (obstetrics); Payment; Corporation","score_opus":0.012662736668097118,"score_gpt":0.2144104367966869,"score_spread":0.20174770012858978,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7036658958","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0003722231,0.0000406982,0.00071696297,0.000859314,0.00028315836,0.00033488992,0.000103509956,0.00018584522,0.9971034],"genre_scores_gemma":[0.004499835,0.00002949082,0.0033004005,0.0009505302,0.00032764746,0.000017934304,0.00015887455,0.00018869393,0.9905266],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99858654,0.00004126859,0.00025536248,0.00056559115,0.00031579708,0.00023547378],"domain_scores_gemma":[0.9991562,0.000014832847,0.00034960685,0.00031528846,0.000002167093,0.00016194908],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000056013698,0.00026232275,0.000235499,0.0000010415217,0.000041526437,0.00004148504,0.00025993114,0.00021378545,0.37744054],"category_scores_gemma":[0.000008067981,0.00021805843,0.00007307676,0.00016037213,0.0001223049,0.00006499277,0.00014115118,0.00016751754,0.032562524],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021483414,0.000019257612,0.00095505104,0.000011186401,0.000018231274,0.00002028081,0.000111263435,0.00001699616,0.00021945334,0.000021093225,0.99796337,0.0006223626],"study_design_scores_gemma":[0.00045967574,0.000086072025,0.0023891232,0.0000132956875,0.000017500997,0.0000026028115,0.000106108746,0.00039151384,0.00007449612,0.00011884924,0.99601614,0.00032464438],"about_ca_topic_score_codex":0.00043776276,"about_ca_topic_score_gemma":0.0013293562,"teacher_disagreement_score":0.34487802,"about_ca_system_score_codex":0.000045322184,"about_ca_system_score_gemma":0.000012178791,"threshold_uncertainty_score":0.9681907},"labels":[],"label_agreement":null},{"id":"W7037359480","doi":"","title":"Downslope Winds and Dust Storms in the Salton Basin Downslope Winds and Dust Storms in the Salton Basin","year":2019,"lang":"en","type":"article","venue":"eScholarship (California Digital Library)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Structural basin; Storm; Dust storm; Plume; Atmosphere (unit); Alluvial fan; Arctic","score_opus":0.007536296167643506,"score_gpt":0.19320369861868217,"score_spread":0.18566740245103866,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7037359480","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":[0.94993526,0.0002644541,0.000010844853,0.0029556681,0.000119079596,0.0008536135,0.00024985344,0.00007430746,0.045536943],"genre_scores_gemma":[0.9939584,0.00009162419,0.00021970554,0.0040095537,0.000108825785,0.000046273744,0.000121672005,0.00007762772,0.0013663254],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99643475,0.00030663755,0.0006306535,0.0008983065,0.00085656263,0.0008730671],"domain_scores_gemma":[0.9984203,0.00032122058,0.00019105639,0.00079278613,0.000006918455,0.00026770143],"candidate_categories":["metaepi_narrow","scholarly_communication","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0010570644,0.000563951,0.00047945313,0.000023499033,0.00026305145,0.0014393389,0.0011268659,0.00031729153,0.0014871517],"category_scores_gemma":[0.00010888822,0.00033360746,0.000116059295,0.001037365,0.0004914358,0.0041525606,0.00065528875,0.0011604804,0.0010263441],"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":[0.000120229,0.00022472686,0.9850849,0.000028587046,0.000010773313,0.000054647935,0.0009075152,0.000031337873,0.00009711156,0.00024849563,0.0025201237,0.010671561],"study_design_scores_gemma":[0.0010501888,0.00023619989,0.86651707,0.000077863144,0.000013226152,0.000046282526,0.0012380463,0.00013769006,0.00010272988,0.0010308946,0.1290099,0.0005399112],"about_ca_topic_score_codex":0.00020580564,"about_ca_topic_score_gemma":0.00011494018,"teacher_disagreement_score":0.12648977,"about_ca_system_score_codex":0.00012130866,"about_ca_system_score_gemma":0.00006094924,"threshold_uncertainty_score":0.9999116},"labels":[],"label_agreement":null},{"id":"W7038288138","doi":"","title":"Healthcare of Ontario Pension Plan Trust Fund Buys 13,689 Shares of Hannon Armstrong Sustainable Infrastructure Capital, Inc. (NYSE:HASI)","year":2024,"lang":"en","type":"other","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Plan (archaeology); Pension; Pension plan; Health care; Pension fund","score_opus":0.010724694158491541,"score_gpt":0.22960730266887597,"score_spread":0.21888260851038444,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7038288138","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.2037735,0.0018512852,0.000084140906,0.00014825317,0.00042194052,0.0009074096,0.00021747111,0.00013842626,0.7924576],"genre_scores_gemma":[0.27858296,0.00006955603,0.0010887366,0.00007311555,0.00008467621,0.000012956711,0.00011715398,0.00022009539,0.71975076],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9976577,0.000034847177,0.0004895363,0.0006572146,0.00059607363,0.0005646064],"domain_scores_gemma":[0.99883527,0.000013462686,0.0003760154,0.00057023007,0.0000229422,0.00018208784],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00011899944,0.00046789608,0.00065987033,0.000013809232,0.00006572637,0.000035671907,0.00044661295,0.00052841014,0.09702444],"category_scores_gemma":[0.000008450991,0.0003717984,0.00013501002,0.00023797677,0.00031461104,0.000094542964,0.0006057415,0.00048304987,0.00026837704],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000062179504,0.00009000306,0.058116175,0.0012170139,0.00010355642,0.000083227016,0.0032600537,0.00034109433,0.00021853996,0.0008785578,0.93404937,0.0015802506],"study_design_scores_gemma":[0.0005839097,0.00069248094,0.03301748,0.0005476509,0.0001243467,0.000022733502,0.008072314,0.000080480466,0.00029487725,0.0011963686,0.9545172,0.00085016835],"about_ca_topic_score_codex":0.501757,"about_ca_topic_score_gemma":0.261583,"teacher_disagreement_score":0.24017403,"about_ca_system_score_codex":0.0007589914,"about_ca_system_score_gemma":0.00026759336,"threshold_uncertainty_score":0.9998734},"labels":[],"label_agreement":null},{"id":"W7042504147","doi":"","title":"Phase equilibria and solubility measurements of gases in water in the hydrate formation region","year":2007,"lang":"en","type":"dissertation","venue":"eScholarship@McGill (McGill)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"McGill University","funders":"","keywords":"Solubility; Propane; Clathrate hydrate; Methane; Hydrate; Carbon dioxide; Phase (matter); Aqueous solution","score_opus":0.03332275531254305,"score_gpt":0.2742399171296039,"score_spread":0.24091716181706083,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7042504147","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":[0.97663176,0.00005864475,7.9825395e-7,0.000013732784,0.00016420305,0.00069313654,0.00002899386,0.000020327901,0.022388425],"genre_scores_gemma":[0.99908423,0.000053406628,0.0001529341,0.0001355058,0.000007430796,0.000057737,0.00022185675,0.000029565326,0.0002573404],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9970176,0.0003568865,0.0008542325,0.0004982509,0.0007621541,0.00051086117],"domain_scores_gemma":[0.99903214,0.0000718873,0.00033238556,0.00043503684,0.000034388984,0.00009416805],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.001925526,0.00037012354,0.00039723518,0.000022096956,0.00024093296,0.000037188714,0.00041153442,0.00034070993,0.00019943394],"category_scores_gemma":[0.00015769116,0.00026781735,0.000101524696,0.00036401668,0.00011187603,0.0011657377,0.00011490401,0.0005602649,0.000055187116],"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":[0.0021365786,0.0026148888,0.020175673,0.00069079926,0.00006290031,0.0001144573,0.00072757324,0.0002494153,0.61835825,0.0009046538,0.000024178149,0.3539406],"study_design_scores_gemma":[0.0114764385,0.0014937015,0.15427664,0.0010315657,0.00026910927,0.00006911716,0.0042866385,0.0008023042,0.7906946,0.023105398,0.0099619785,0.0025325362],"about_ca_topic_score_codex":0.0016182535,"about_ca_topic_score_gemma":0.0066815433,"teacher_disagreement_score":0.35140806,"about_ca_system_score_codex":0.00045595583,"about_ca_system_score_gemma":0.0000075535527,"threshold_uncertainty_score":0.9999774},"labels":[],"label_agreement":null},{"id":"W7042950800","doi":"","title":"Radiative contribution to the formation and development of Arctic continental air masses over northwest Canada","year":2018,"lang":"en","type":"dissertation","venue":"eScholarship@McGill (McGill)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Fonds Québécois de la Recherche sur la Nature et les Technologies; Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Radiative transfer; Longwave; Radiative cooling; Albedo (alchemy); Air mass (solar energy); Arctic; Middle latitudes; Snow; Polar; Cryosphere","score_opus":0.005730112626406174,"score_gpt":0.20119216774826004,"score_spread":0.19546205512185386,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7042950800","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":[0.9951194,0.00004486172,0.0000051778293,0.000029054145,0.00048361588,0.0007161525,0.00058542995,0.000021949041,0.0029943434],"genre_scores_gemma":[0.9972089,0.000022168628,0.000941621,0.0003795019,0.000020137022,0.00009700605,0.0007908949,0.000030829993,0.00050892343],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9977629,0.00010178037,0.0006103247,0.00041398045,0.0007145515,0.00039641562],"domain_scores_gemma":[0.9988193,0.00007953343,0.0005145515,0.00026741877,0.000114391725,0.00020481535],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0003508075,0.00037487556,0.00035833224,0.00000786575,0.00088474114,0.000029161929,0.00031882597,0.00019158423,0.00052295986],"category_scores_gemma":[0.00021038616,0.00030477613,0.00006253124,0.00026401374,0.00007889285,0.0005312878,0.00015080726,0.00031273687,0.00009418426],"study_design_candidate":"design_other","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":[0.002527791,0.00093484233,0.08936286,0.0012768593,0.0013778084,0.00007131437,0.0018248167,0.0014710198,0.042581264,0.0123856785,0.0013347752,0.84485096],"study_design_scores_gemma":[0.0008720163,0.00015989345,0.51606697,0.00019173339,0.00010739084,0.000010040505,0.0014088685,0.000062013496,0.0448246,0.00026987898,0.4352434,0.00078317587],"about_ca_topic_score_codex":0.14240839,"about_ca_topic_score_gemma":0.85436946,"teacher_disagreement_score":0.8440678,"about_ca_system_score_codex":0.0014984562,"about_ca_system_score_gemma":0.00009515582,"threshold_uncertainty_score":0.99994045},"labels":[],"label_agreement":null},{"id":"W7046072180","doi":"","title":"Comparison of Satellite and Ground-Based Data on Polar Mesospheric Clouds","year":2006,"lang":"en","type":"article","venue":"Digital Commons - USU (Utah State University)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Mesopause; Satellite; Aeronomy; Backscatter (email); Mesosphere; Twilight; Polar; Latitude","score_opus":0.01971736418754824,"score_gpt":0.2275233208372238,"score_spread":0.20780595664967555,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7046072180","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":[0.9231079,0.000077875295,0.0015080177,0.00008272611,0.000034976976,0.00013221131,0.0002996901,0.000052806816,0.07470375],"genre_scores_gemma":[0.9969462,0.000014469327,0.00058203435,0.00003946692,0.000008373345,1.5663367e-7,0.00020641332,0.000016808426,0.0021860625],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998787,0.000042664386,0.00020690248,0.00039984344,0.0002768148,0.0002867848],"domain_scores_gemma":[0.9990425,0.00009608492,0.00014852126,0.00058599835,0.000010505878,0.000116389034],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006782276,0.00019987838,0.00026563182,0.0000068727977,0.00016513279,0.0000759472,0.0005789927,0.00005777293,0.00013847585],"category_scores_gemma":[0.000007637767,0.00020518024,0.000052238793,0.0004891909,0.00044902525,0.0005371615,0.000546592,0.0001373708,0.00005992393],"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":[0.00020893311,0.00067899784,0.96719193,0.000018620822,0.000033095755,0.000064836255,0.0001772701,0.0042733783,0.00031912967,0.0013320607,0.0020255297,0.023676235],"study_design_scores_gemma":[0.0014821572,0.0007177982,0.57531226,0.000041332172,0.0000726746,0.000004498866,0.00092629483,0.009062101,0.00045552806,0.00061726425,0.41056967,0.00073844916],"about_ca_topic_score_codex":0.0015138625,"about_ca_topic_score_gemma":0.000577595,"teacher_disagreement_score":0.40854415,"about_ca_system_score_codex":0.0001152031,"about_ca_system_score_gemma":0.000017671324,"threshold_uncertainty_score":0.8367008},"labels":[],"label_agreement":null},{"id":"W7083321870","doi":"10.5114/phr.2025.154444","title":"Physical activity and cognitive function in breast cancer survivors: a cross-sectional comparative study","year":2025,"lang":"en","type":"article","venue":"Physiotherapy Review","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Breast cancer; Physical activity; Cognition; Physical exercise; Function (biology); Cancer","score_opus":0.021662990904899395,"score_gpt":0.3679308078702628,"score_spread":0.3462678169653634,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7083321870","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":[0.99438936,0.0039272443,0.00011477228,0.00012592791,0.000057576723,0.00068306754,0.000010605776,0.000015461568,0.0006759671],"genre_scores_gemma":[0.99567866,0.003286509,0.000005048083,0.0005199597,0.00003566138,0.00021166842,0.000001174098,0.0000061522196,0.00025518367],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991238,0.00012665786,0.000116410345,0.00033986758,0.0001587263,0.00013450607],"domain_scores_gemma":[0.9997368,0.00005767531,0.00006448272,0.00009652038,0.000013070498,0.00003145183],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000117436015,0.00014272686,0.0002957293,0.0000016670665,0.000095350726,0.0000242458,0.000067002715,0.000020725705,0.00080387807],"category_scores_gemma":[0.0000023757696,0.00011285981,0.000051182345,0.00037936232,0.00013506413,0.00016767625,0.000054269425,0.00011638234,0.00002723642],"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":[0.00014057478,0.00088199496,0.96189165,0.00010648339,0.000052893607,4.3561744e-7,0.00027326032,0.000034622244,0.0012089516,0.0000114950635,0.00009313625,0.03530449],"study_design_scores_gemma":[0.00048293782,0.00007080348,0.9983029,0.00028939007,0.000024251609,5.120462e-7,0.00005726998,0.00031991,0.000027126902,0.0000848256,0.00022922613,0.00011085519],"about_ca_topic_score_codex":0.0032115034,"about_ca_topic_score_gemma":0.0012039777,"teacher_disagreement_score":0.03641123,"about_ca_system_score_codex":0.00007694302,"about_ca_system_score_gemma":0.0000141598075,"threshold_uncertainty_score":0.88019013},"labels":[],"label_agreement":null},{"id":"W7084401249","doi":"10.1656/045.032.0310","title":"A Remarkable Specimen Record of an Apparently Wild Gray Wolf (Canis lupus) from Upstate New York","year":2025,"lang":"en","type":"article","venue":"Northeastern Naturalist","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Canis; Gray wolf; Gray (unit); Introgression; National park; Carnivore","score_opus":0.009551089997864413,"score_gpt":0.22427004448118318,"score_spread":0.21471895448331876,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7084401249","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":[0.9681621,0.00022458575,0.00033148832,0.00042396376,0.0007600319,0.00025358837,0.000035651563,0.00005971517,0.029748846],"genre_scores_gemma":[0.9517701,0.00002660124,0.0050506247,0.00048895756,0.000109202214,0.0000076038355,0.00005673372,0.00002533583,0.042464808],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982315,0.00007249518,0.000405204,0.00055367366,0.00037213138,0.0003650145],"domain_scores_gemma":[0.9989031,0.00004436622,0.00019509417,0.0006526627,0.0000131995885,0.00019160111],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00012339436,0.00025752533,0.00033887097,0.00000454378,0.00010482799,0.000058311987,0.00059778616,0.000117713775,0.0076781316],"category_scores_gemma":[0.000015879808,0.00021663493,0.00011574647,0.00039964248,0.00016775494,0.00023462262,0.00022754907,0.0002242379,0.00021235328],"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":[0.0002644268,0.00013020221,0.9197365,0.000013317754,0.00005826157,0.000012041728,0.0006130894,0.000246235,0.001584263,0.00008012997,0.018602552,0.058659],"study_design_scores_gemma":[0.0032403676,0.00031978512,0.5616559,0.0003309026,0.00021708058,0.000015539152,0.0016769395,0.0053030145,0.002529621,0.007931886,0.4155058,0.0012731672],"about_ca_topic_score_codex":0.049221754,"about_ca_topic_score_gemma":0.029291471,"teacher_disagreement_score":0.39690325,"about_ca_system_score_codex":0.00013832624,"about_ca_system_score_gemma":0.000032984568,"threshold_uncertainty_score":0.993229},"labels":[],"label_agreement":null},{"id":"W7095642969","doi":"","title":"Atmospheric Chemistry and Physics Simulation of mineral dust aerosol with Piecewise Log-normal Approximation (PLA) in CanAM4-PAM","year":2012,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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; Mineral dust; Radiative transfer; Deposition (geology); Piecewise; Atmospheric model; Earth's energy budget; Optical depth","score_opus":0.0064977706954422974,"score_gpt":0.20208473892654932,"score_spread":0.19558696823110702,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7095642969","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":[0.9716168,0.000023425775,0.019753383,0.00002068033,0.000015948941,0.00013543197,0.000001336518,0.00001512413,0.008417858],"genre_scores_gemma":[0.9868892,0.0000033009005,0.012186375,0.00003931118,0.00004021822,0.0000102927925,0.0000062614818,0.000010798307,0.0008142559],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9992301,0.0000122201845,0.00016582252,0.00015585414,0.00019426686,0.00024176436],"domain_scores_gemma":[0.99966645,0.000019705316,0.00009204124,0.00012794603,0.000006487539,0.00008738479],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008206714,0.00012371618,0.00013303019,9.6912046e-8,0.000038405098,0.000008968184,0.00006335717,0.000062458355,0.0007351953],"category_scores_gemma":[0.0000065822933,0.00009911121,0.000016560043,0.00018990684,0.00012974076,0.00034416377,0.000058918147,0.00007267013,0.0000086141945],"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":[0.000035677196,0.00014409717,0.8457635,0.000026291884,0.000005582867,6.490293e-7,0.00050882174,0.13456056,0.010660873,0.000023574714,0.0000725566,0.008197821],"study_design_scores_gemma":[0.00081021746,0.0000686254,0.44751117,0.00001538241,0.000018814679,0.0000048512843,0.00048528175,0.54543525,0.005240917,0.000023456165,0.000107347725,0.00027869802],"about_ca_topic_score_codex":0.0010652828,"about_ca_topic_score_gemma":0.00019910144,"teacher_disagreement_score":0.41087466,"about_ca_system_score_codex":0.00008362848,"about_ca_system_score_gemma":0.000009148419,"threshold_uncertainty_score":0.8049873},"labels":[],"label_agreement":null},{"id":"W7096310755","doi":"","title":"ENVISAT Data Validation with Ground-based Differential Absorption Raman Lidar (DIAL) at Toronto (73.8N, 79.5W) under A.O. ID 153","year":2012,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Lidar; Absorption (acoustics); Calibration; Differential (mechanical device); Data acquisition; Raman spectroscopy; Atmospheric optics","score_opus":0.02185149895526539,"score_gpt":0.23836113432115894,"score_spread":0.21650963536589354,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7096310755","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":[0.9262338,0.00004532665,0.06361218,0.0002115725,0.00028825513,0.00029294984,0.000015822592,0.00009977888,0.009200277],"genre_scores_gemma":[0.9929937,0.000017837847,0.002154164,0.00043203135,0.0002676806,0.00001891784,0.00044557854,0.000036426598,0.0036336677],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981251,0.00007820238,0.00023921776,0.0004929904,0.000568641,0.0004958626],"domain_scores_gemma":[0.99873924,0.00003908242,0.00012027665,0.00086356566,0.0000048586894,0.00023298436],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00021125632,0.00026051753,0.00018374581,0.000001203544,0.00027502235,0.00008157643,0.0004339359,0.000121963385,0.03547906],"category_scores_gemma":[0.00000639267,0.00019111227,0.000043536915,0.00008261607,0.00017647857,0.0011072134,0.00044092952,0.0000898932,0.0010580096],"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":[0.0007747284,0.0021453379,0.8467856,0.000058546404,0.00018575463,0.000008306169,0.0015963407,0.0047764536,0.08960593,0.0029199286,0.036211215,0.014931849],"study_design_scores_gemma":[0.0021957292,0.0003758302,0.9578065,0.000021058095,0.00019443111,0.000017993645,0.0008783423,0.007617492,0.0058591384,0.00017276085,0.023757057,0.0011036119],"about_ca_topic_score_codex":0.006029706,"about_ca_topic_score_gemma":0.0061021624,"teacher_disagreement_score":0.111020945,"about_ca_system_score_codex":0.0008677411,"about_ca_system_score_gemma":0.000012747152,"threshold_uncertainty_score":0.9997198},"labels":[],"label_agreement":null},{"id":"W7096813816","doi":"","title":"2004: Aerosol properties and chemical apportionment of aerosol optical depth at locations off the United States east coast in July and August","year":2016,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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; Single-scattering albedo; Albedo (alchemy); Sulfate; Optical depth; Mass concentration (chemistry); In situ; East coast","score_opus":0.017267220602380434,"score_gpt":0.20462469162404587,"score_spread":0.18735747102166544,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7096813816","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":[0.99605334,0.00009906094,0.0010199258,0.0015324699,0.000011619087,0.00023600674,0.0000047714034,0.00001503551,0.0010277885],"genre_scores_gemma":[0.9966377,0.0001544832,0.00047852602,0.00015225798,0.000006848174,0.000035860303,0.000004201029,0.000009375885,0.0025207384],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990811,0.000025820085,0.0002508246,0.00022902078,0.00020272382,0.00021056233],"domain_scores_gemma":[0.99962056,0.00004317814,0.000058235575,0.0001689986,0.000008445472,0.000100567835],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012176241,0.00012186381,0.0001269714,0.0000017877555,0.00008350343,0.000014721346,0.00010619887,0.000051353523,0.000430285],"category_scores_gemma":[0.000023526607,0.000060068327,0.00001746984,0.00012104104,0.000908094,0.00009230379,0.0002742309,0.000056652156,0.000037856054],"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":[0.0002312537,0.0006160513,0.5202156,0.0000457117,0.000044392524,0.000005236431,0.0028359764,0.0010115041,0.44123152,0.0003343658,0.0109549835,0.022473397],"study_design_scores_gemma":[0.006432051,0.00087346946,0.5075508,0.0004072961,0.0001587507,0.0001450312,0.01044117,0.015212738,0.44524378,0.00030120497,0.011475376,0.0017583828],"about_ca_topic_score_codex":0.00038633376,"about_ca_topic_score_gemma":0.0006405691,"teacher_disagreement_score":0.020715015,"about_ca_system_score_codex":0.00008496716,"about_ca_system_score_gemma":0.000009600585,"threshold_uncertainty_score":0.4711319},"labels":[],"label_agreement":null},{"id":"W7096925887","doi":"","title":"Station Name Station","year":2014,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Latent heat; Storm; Weather station; Automatic weather station; Sea ice","score_opus":0.0051526046489474885,"score_gpt":0.20679034295228013,"score_spread":0.20163773830333265,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7096925887","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":[0.7175276,0.0000011978949,0.16484973,0.00016847509,0.00003696354,0.000035561647,3.712186e-7,0.000031381966,0.11734868],"genre_scores_gemma":[0.9827897,0.000001846705,0.010681442,0.00040713718,0.000014879266,0.0000031784389,0.0000044973294,0.0000036367044,0.006093661],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99964947,0.00001374831,0.000058039714,0.000089152585,0.00011096179,0.00007864921],"domain_scores_gemma":[0.9998658,0.000012225178,0.000020531003,0.000068835805,0.0000018367035,0.00003082979],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00007292451,0.000034788878,0.000029182102,1.5878739e-7,0.00004154518,0.000010161822,0.00004127003,0.000015103867,0.009937191],"category_scores_gemma":[0.000010145131,0.000027916649,0.0000097094035,0.000042641048,0.000027101467,0.000089335444,0.000019643554,0.000019297358,0.0018347852],"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":[0.000015162833,0.00009245797,0.33320093,0.0000053209615,0.0000059235977,7.896566e-7,0.0011837739,0.010742183,0.013200364,0.016526086,0.054802924,0.57022405],"study_design_scores_gemma":[0.00033828078,0.00014389041,0.7883646,0.000002034888,0.000005843801,0.0000011072264,0.00029145402,0.06205765,0.0018887831,0.0072411816,0.13944922,0.00021593519],"about_ca_topic_score_codex":0.00039762488,"about_ca_topic_score_gemma":0.00009256047,"teacher_disagreement_score":0.57000816,"about_ca_system_score_codex":0.000028762746,"about_ca_system_score_gemma":0.0000012067671,"threshold_uncertainty_score":0.9989424},"labels":[],"label_agreement":null},{"id":"W7097792437","doi":"","title":"Hazardous Liquid Airborne Lidar Observation Study (HALOS)................................................230 New Technologies to Meet Waste Program Needs.................................................................259 Quantum Cascade Lasers for Molecu","year":2013,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Hazardous waste; Cascade; Laser; Lidar; Emerging technologies","score_opus":0.0165429928044939,"score_gpt":0.25046969323597834,"score_spread":0.23392670043148445,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7097792437","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":[0.6200037,0.0031631433,0.076352425,0.031534556,0.021142503,0.11267743,0.0033824672,0.04909485,0.082648925],"genre_scores_gemma":[0.6840099,0.00090510014,0.1052485,0.022348361,0.011916666,0.0884555,0.0037734008,0.012343096,0.07099945],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.8747079,0.0070380573,0.029932246,0.030903466,0.021493606,0.035924766],"domain_scores_gemma":[0.9080236,0.010023162,0.012871102,0.030721696,0.011253008,0.027107425],"candidate_categories":["metaresearch","metaepi_narrow","metaepi_broad","bibliometrics","sts","scholarly_communication","open_science","research_integrity","insufficient_payload"],"consensus_categories":["metaepi_narrow","metaepi_broad","bibliometrics","sts","scholarly_communication","open_science","research_integrity","insufficient_payload"],"category_scores_codex":[0.015909003,0.031255133,0.026076896,0.01161047,0.014441239,0.012886959,0.035970975,0.0127027305,0.034087483],"category_scores_gemma":[0.014828736,0.03318576,0.015781011,0.049796987,0.00799344,0.022374379,0.019539002,0.013174799,0.049558274],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":true,"about_ca_system_consensus":true,"study_design_scores_codex":[0.012631145,0.022235852,0.02605591,0.0014431665,0.0071968525,0.0016428119,0.008715345,0.026710695,0.025476675,0.015662238,0.73519385,0.11703546],"study_design_scores_gemma":[0.070281446,0.0453114,0.011200439,0.00261101,0.009102941,0.0042312406,0.042649057,0.037937887,0.024690485,0.033278722,0.66304547,0.055659935],"about_ca_topic_score_codex":0.022604926,"about_ca_topic_score_gemma":0.0056963637,"teacher_disagreement_score":0.072148405,"about_ca_system_score_codex":0.022338029,"about_ca_system_score_gemma":0.009849119,"threshold_uncertainty_score":0.99959207},"labels":[],"label_agreement":null},{"id":"W7097904098","doi":"","title":"q 2001 American Meteorological Society Assessing Cloud-Phase Conditions","year":2000,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Liquid water content; Drizzle; Icing; Ice water; Volume (thermodynamics); Snow; Range (aeronautics); Particle (ecology)","score_opus":0.015835893977132292,"score_gpt":0.3030468027814024,"score_spread":0.2872109088042701,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7097904098","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":[0.85208255,0.0000052768683,0.0031768968,0.00054500776,0.000031341315,0.000066544126,0.0000039149686,0.00009692354,0.14399157],"genre_scores_gemma":[0.96843785,0.000036236845,0.019854086,0.003111463,0.00006331031,0.000012658919,0.000008653493,0.000009214902,0.0084665315],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99900985,0.000037447902,0.00014763299,0.00026957446,0.000189661,0.00034581462],"domain_scores_gemma":[0.99959254,0.000036874255,0.000040372808,0.00017444264,0.0000026071898,0.000153131],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00011669488,0.00011716431,0.00014035353,2.5601258e-7,0.00028154626,0.000045199013,0.00015338592,0.00004566497,0.23458266],"category_scores_gemma":[0.0000060135144,0.00008916657,0.0001131348,0.00023682768,0.00064347725,0.00016331345,0.000053085954,0.0001144604,0.002232656],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000386051,0.0016132985,0.08966887,0.0000030788815,0.0000718704,0.000041792813,0.00046810592,0.0036895664,0.021609815,0.0006809378,0.5625345,0.3195795],"study_design_scores_gemma":[0.0028817197,0.0011701158,0.45690185,0.000009060304,0.0001254859,0.00007984494,0.0031493057,0.046656724,0.0013466539,0.0028819044,0.48336646,0.0014308785],"about_ca_topic_score_codex":0.0003593689,"about_ca_topic_score_gemma":0.000021332142,"teacher_disagreement_score":0.36723298,"about_ca_system_score_codex":0.000071166454,"about_ca_system_score_gemma":0.00000778457,"threshold_uncertainty_score":0.9985442},"labels":[],"label_agreement":null},{"id":"W7098145904","doi":"","title":"© Author(s) 2009. This work is distributed under the Creative Commons Attribution 3.0 License. Atmospheric Chemistry and Physics Large surface radiative forcing from topographic blowing snow residuals measured in the High Arctic at Eureka","year":2009,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Snow; Ice crystals; Arctic; Permafrost; Forcing (mathematics); Radiative transfer; Cryosphere; Radiative forcing; Sea ice thickness; Premelting","score_opus":0.012245411872755251,"score_gpt":0.22749266486712294,"score_spread":0.2152472529943677,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7098145904","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":[0.971988,0.0005068008,0.020003024,0.00591472,0.000045467743,0.00044985744,0.00013660983,0.000051895095,0.0009035904],"genre_scores_gemma":[0.9964163,0.00006503778,0.00096416316,0.0012910173,0.00006329733,0.0000169813,0.000097844975,0.000017504504,0.0010678757],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99768215,0.000320509,0.0003298359,0.0005352374,0.0005588487,0.0005734277],"domain_scores_gemma":[0.99868983,0.0004782515,0.00018894149,0.0005062081,0.000024476796,0.00011229069],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006513455,0.00033948515,0.00032782945,2.9128293e-7,0.00079864566,0.000107854314,0.00038417583,0.00017126923,0.0017504524],"category_scores_gemma":[0.000054121792,0.00021405594,0.00011905589,0.0011102816,0.000294638,0.00020070461,0.00018002136,0.00042400774,0.00003263707],"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":[0.00022476223,0.0005652319,0.94017196,0.00001105959,0.00020921006,0.000021121865,0.013068409,0.01083133,0.0047055725,0.0008138027,0.026457218,0.0029203324],"study_design_scores_gemma":[0.0008055938,0.000059726368,0.9835801,0.000069282294,0.00011320351,0.0000031089455,0.0034925465,0.0045690746,0.0020950236,0.0036433642,0.0011719766,0.00039696874],"about_ca_topic_score_codex":0.0029279017,"about_ca_topic_score_gemma":0.0005031091,"teacher_disagreement_score":0.04340818,"about_ca_system_score_codex":0.00036044375,"about_ca_system_score_gemma":0.000017502898,"threshold_uncertainty_score":0.9991621},"labels":[],"label_agreement":null},{"id":"W7099014129","doi":"","title":"Distribution of Caribou in North America............................................................... 6 Caribou Morphology and Taxonomy With Emphasis on Canada‟s Arctic Islands","year":2009,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Taxonomy (biology); Arctic; The arctic; Distribution (mathematics); Morphology (biology)","score_opus":0.005724060981822974,"score_gpt":0.18071528747780433,"score_spread":0.17499122649598134,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7099014129","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":[0.9341828,0.0015366954,0.0036102396,0.003447531,0.0015920772,0.007493313,0.0020462333,0.0016427849,0.044448283],"genre_scores_gemma":[0.97400665,0.0016681302,0.006531642,0.008598996,0.00075200904,0.002014805,0.002896473,0.0010922403,0.0024390675],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.95953745,0.0023403002,0.009824151,0.01008039,0.008452394,0.00976529],"domain_scores_gemma":[0.97766566,0.0033305276,0.004974398,0.008116788,0.0013301197,0.0045824996],"candidate_categories":["metaepi_narrow","sts","open_science","research_integrity","insufficient_payload"],"consensus_categories":["metaepi_narrow","sts","research_integrity"],"category_scores_codex":[0.0031534822,0.008476773,0.00944366,0.0012950092,0.0019876703,0.0007592137,0.006595351,0.0026809422,0.0036442964],"category_scores_gemma":[0.0016299392,0.007890287,0.0017930152,0.0142262075,0.005151424,0.003716696,0.002209917,0.006506425,0.00059767964],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.014407749,0.009550534,0.668326,0.0011645701,0.001820386,0.006526973,0.0034549264,0.06676189,0.002738727,0.020529449,0.0508559,0.15386285],"study_design_scores_gemma":[0.028712213,0.012312014,0.7183448,0.0017819926,0.001397605,0.0027265337,0.004942168,0.007535988,0.003579095,0.0019352039,0.20174979,0.014982617],"about_ca_topic_score_codex":0.24335413,"about_ca_topic_score_gemma":0.38800648,"teacher_disagreement_score":0.15089388,"about_ca_system_score_codex":0.00913921,"about_ca_system_score_gemma":0.004007931,"threshold_uncertainty_score":0.9993116},"labels":[],"label_agreement":null},{"id":"W7099121826","doi":"","title":"ARCTIC Observations of Thick-billed Murres (Uria Zomvia) and Other Seabirds","year":2014,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Cape; Arctic; Seabird; Coastal zone; Beaufort scale; The arctic","score_opus":0.01667277739538251,"score_gpt":0.22010224640176043,"score_spread":0.20342946900637793,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7099121826","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":[0.9606919,0.000012291256,0.0024019217,0.00037738896,0.000039041286,0.000075085416,9.315057e-7,0.000026195914,0.03637523],"genre_scores_gemma":[0.9893021,0.000005070162,0.0067378655,0.0006909599,0.000017855034,0.0000047184963,4.0210816e-7,0.000008916222,0.0032321261],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994666,0.000025695039,0.00011718666,0.00014285633,0.0001338848,0.00011376404],"domain_scores_gemma":[0.99968785,0.000048063295,0.000042931853,0.00016390705,0.000004648639,0.00005260988],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00013286533,0.00006804233,0.000094557785,5.188917e-7,0.00006469963,0.000009768153,0.00009432425,0.00003880224,0.0046726656],"category_scores_gemma":[0.000038064474,0.000050525796,0.0000251293,0.00009145995,0.00017054573,0.00006020146,0.00008623829,0.000042828357,0.000078986974],"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":[0.0000054378825,0.000041878004,0.9842914,0.000008817535,0.0000071275476,1.1502486e-7,0.00032833416,0.00014802869,0.0075288625,0.003466839,0.0012170817,0.0029561091],"study_design_scores_gemma":[0.00028327492,0.00006678485,0.9722636,0.000007818962,0.000011090367,0.000001457337,0.00015496685,0.0044108666,0.0004912388,0.0020977142,0.020093618,0.00011758622],"about_ca_topic_score_codex":0.0010468296,"about_ca_topic_score_gemma":0.00021511738,"teacher_disagreement_score":0.033143103,"about_ca_system_score_codex":0.000015073161,"about_ca_system_score_gemma":0.000002718594,"threshold_uncertainty_score":0.9962372},"labels":[],"label_agreement":null},{"id":"W7100053172","doi":"","title":"METHODS","year":2016,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Dementia; Cognition; Association (psychology); Confounding; Cognitive impairment; Memory clinic; Memory impairment; Population","score_opus":0.008785937820207491,"score_gpt":0.2839191317824386,"score_spread":0.2751331939622311,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7100053172","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.123523735,0.0000040225736,0.42775193,0.00074220914,0.000046276007,0.00002039257,9.3004275e-8,0.000035977333,0.44787535],"genre_scores_gemma":[0.6725526,0.000004010152,0.2588309,0.0004192601,0.000013311121,0.000002741298,1.945363e-8,0.00000342253,0.06817372],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9997326,0.000014760463,0.000037734786,0.000082147155,0.00004905621,0.0000836609],"domain_scores_gemma":[0.9998419,0.000023383396,0.000007782526,0.00009118338,4.934879e-7,0.000035234523],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000085270396,0.000028585979,0.000027677504,5.530018e-8,0.000020458705,0.0000023475445,0.000065086606,0.000013403591,0.06840729],"category_scores_gemma":[0.000010039216,0.0000131086335,0.000014844728,0.000035109068,0.00005129243,0.000044359203,0.00006183693,0.000008190619,0.0033265592],"study_design_candidate":"design_other","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":[0.0000012568827,0.000008650593,0.06382401,1.1899927e-7,0.0000012710697,5.9594254e-7,0.000017691476,0.0000016779862,0.078366905,0.0013387545,0.016254392,0.8401847],"study_design_scores_gemma":[0.00022177551,0.0000420129,0.21343052,0.0000020399607,0.0000031397853,0.0000036969857,0.000030536336,0.00009388005,0.0346023,0.0065384693,0.7448673,0.0001642988],"about_ca_topic_score_codex":0.000039352435,"about_ca_topic_score_gemma":0.0000058984897,"teacher_disagreement_score":0.84002036,"about_ca_system_score_codex":0.00002003445,"about_ca_system_score_gemma":7.839518e-7,"threshold_uncertainty_score":0.99744946},"labels":[],"label_agreement":null},{"id":"W7100566163","doi":"","title":"UDC 661.676.155l.s68.21(74) (084.1) PICTURE OF THE MONTH Orographic Fibrous Plumes Over New England","year":2013,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Cirrus; Orographic lift; Cloud cover; Snow; TOPS; Albedo (alchemy); Advanced very-high-resolution radiometer; Emissivity; Radiometer; Optical depth","score_opus":0.0032416563962904548,"score_gpt":0.17194438026935052,"score_spread":0.16870272387306007,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7100566163","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":[0.9686379,0.00013911881,0.00040855425,0.00048656206,0.00018412776,0.00033929507,0.000002699418,0.00004933055,0.0297524],"genre_scores_gemma":[0.97010404,0.000037257247,0.0015363065,0.0006156428,0.00009566018,0.000012702522,0.0000014906873,0.000019394416,0.027577534],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99867713,0.000040142608,0.00023497637,0.0003032662,0.00040361885,0.00034085094],"domain_scores_gemma":[0.99917805,0.0000422273,0.0001095137,0.00050452666,0.000007667258,0.00015803425],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00007036363,0.00020655907,0.00019816919,0.0000013590044,0.00012655351,0.00004054621,0.00046997218,0.00012808345,0.026196472],"category_scores_gemma":[0.000016599395,0.00011563542,0.00014725028,0.00028538462,0.00031325434,0.00019596408,0.0002930368,0.00016111291,0.00027105503],"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":[0.000022567961,0.00013079452,0.86524326,0.00001620146,0.00004992121,0.000002948806,0.0016423704,0.0011185062,0.0059679053,0.00031205226,0.09466773,0.030825729],"study_design_scores_gemma":[0.0010286352,0.0001573752,0.93921065,0.000019544672,0.000032878237,0.000008947165,0.00038203035,0.0010574694,0.0013043345,0.0021045136,0.054372534,0.00032108458],"about_ca_topic_score_codex":0.007831301,"about_ca_topic_score_gemma":0.0010301773,"teacher_disagreement_score":0.07396738,"about_ca_system_score_codex":0.000037135676,"about_ca_system_score_gemma":0.000017431825,"threshold_uncertainty_score":0.99877566},"labels":[],"label_agreement":null},{"id":"W7104446062","doi":"10.71781/13306","title":"Measuring and modelling mineral dust emissions from Canadian proglacial valleys","year":2025,"lang":"en","type":"dissertation","venue":"Open MIND","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Disdrometer; Sugar industry; Environmental policy","score_opus":0.03797956176920262,"score_gpt":0.25597216638317694,"score_spread":0.21799260461397432,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7104446062","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":[0.77752304,0.00008522465,0.000059269918,0.0000627522,0.00019031132,0.00032658994,0.00002766243,0.0000012669382,0.2217239],"genre_scores_gemma":[0.8199161,0.000037092028,0.015907248,0.00004356089,0.00010252289,0.000040807878,0.00054072787,0.00002718631,0.16338472],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9988469,0.000022406808,0.000193581,0.0004838109,0.00018659288,0.00026671853],"domain_scores_gemma":[0.99945146,0.000015193907,0.00007523963,0.00018348393,0.000008373777,0.00026627004],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00009343974,0.00020174938,0.00021487099,0.0000029381881,0.00031908829,0.00018490713,0.00039306039,0.00023157263,0.010194993],"category_scores_gemma":[0.0000144920095,0.000195311,0.000038347313,0.00010196804,0.000026315038,0.00012479136,0.00012557089,0.0002193655,0.000173961],"study_design_candidate":"design_other","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":[0.00024646512,0.00019246644,0.049574044,0.00005235134,0.00024123662,0.00016303938,0.019667882,0.024929691,0.006798441,0.000026008389,0.011255679,0.8868527],"study_design_scores_gemma":[0.0033283222,0.00021663735,0.10645486,0.002433589,0.0010883899,0.000009880721,0.01863969,0.17678654,0.006187316,0.0016393805,0.6779466,0.0052687535],"about_ca_topic_score_codex":0.39027485,"about_ca_topic_score_gemma":0.64585805,"teacher_disagreement_score":0.8815839,"about_ca_system_score_codex":0.00017725665,"about_ca_system_score_gemma":0.0002295808,"threshold_uncertainty_score":0.99070984},"labels":[],"label_agreement":null},{"id":"W7106787309","doi":"10.5194/egusphere-2025-5710","title":"Vertically-resolved source contributions to climate-relevant aerosol properties in Southern Greenlandic fjord systems","year":2025,"lang":"","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Swiss Polar Institute; École Polytechnique Fédérale de Lausanne; European Commission; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; National Science Foundation","keywords":"Aerosol; Fjord; Plume; Biomass (ecology); Biomass burning; Atmosphere (unit); Pollution; Supersaturation","score_opus":0.008697028783587288,"score_gpt":0.2315439258146261,"score_spread":0.22284689703103883,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7106787309","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":[0.93856204,0.0015561122,0.04378885,0.0038049011,0.00081104075,0.0026047172,0.00014347998,0.00016929509,0.008559579],"genre_scores_gemma":[0.9719079,0.00016043331,0.000194192,0.001057842,0.00007564568,0.00026231288,0.0000049900473,0.000042989333,0.02629366],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9949924,0.00023943804,0.0013076896,0.0010903304,0.0006814556,0.0016887008],"domain_scores_gemma":[0.99840987,0.00011877022,0.00013912622,0.00075555866,0.000063551975,0.0005131153],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0007322365,0.000609168,0.00081418117,0.000013324245,0.0006346176,0.00031931067,0.0007944868,0.0003812598,0.0022611455],"category_scores_gemma":[0.00021822237,0.000479988,0.00020629098,0.0010876772,0.00056608184,0.00017935863,0.0010236002,0.00048382624,0.004223428],"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":[0.0025868309,0.0050002923,0.680455,0.0010383597,0.0005511384,0.00014258837,0.015369141,0.104167886,0.14651516,0.0074518556,0.008578437,0.028143259],"study_design_scores_gemma":[0.016983742,0.0037376105,0.13221309,0.007749864,0.0011266958,0.0000516331,0.09542786,0.6639919,0.014941352,0.0004124176,0.055805128,0.0075586783],"about_ca_topic_score_codex":0.009244252,"about_ca_topic_score_gemma":0.0032371928,"teacher_disagreement_score":0.55982405,"about_ca_system_score_codex":0.0010000569,"about_ca_system_score_gemma":0.00014978112,"threshold_uncertainty_score":0.99976516},"labels":[],"label_agreement":null},{"id":"W7108671351","doi":"10.71889/5fylantbak.30789470","title":"A Multi-Year Study Of Lower Tropospheric Aerosol Variability And Systematic Relationships From Four North American Regions","year":2015,"lang":"","type":"article","venue":"Appalachian State University","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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; Context (archaeology); Troposphere; Mixing ratio; Seasonality; Atmospheric dynamics; Atmosphere (unit)","score_opus":0.024082261109120474,"score_gpt":0.2022172509950712,"score_spread":0.17813498988595072,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7108671351","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":[0.9847485,0.000024117466,0.012661637,0.00006328714,0.00014908458,0.0016820806,0.00015336815,0.000048385435,0.0004695822],"genre_scores_gemma":[0.9907798,0.00005678405,0.00810279,0.000016476892,0.000015212911,0.0000028845461,0.0000064321493,0.000029236951,0.0009903788],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9958306,0.0015237343,0.0006116354,0.00093655847,0.00062316423,0.0004743095],"domain_scores_gemma":[0.9971195,0.00031441252,0.0007856308,0.0009962195,0.00008938739,0.0006948597],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0007022196,0.00042844817,0.00088310294,0.0000075728112,0.0005526287,0.000049295122,0.0005416559,0.00009207408,0.00013863732],"category_scores_gemma":[0.00018952845,0.0004411257,0.00012706363,0.0011326429,0.0011867009,0.00042530827,0.00063250447,0.0005073591,0.000097902455],"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":[0.00034108156,0.0016882882,0.9777821,0.0002246869,0.00020993664,0.00007246546,0.017018376,0.0024214827,0.000017878296,0.000022108734,0.00008351668,0.000118099844],"study_design_scores_gemma":[0.0027144141,0.0012743653,0.89635813,0.00013563453,0.00056022446,0.0000036981567,0.08866616,0.009742612,0.0000011733956,0.000036603218,0.000029915862,0.00047708445],"about_ca_topic_score_codex":0.015148351,"about_ca_topic_score_gemma":0.0147197135,"teacher_disagreement_score":0.08142397,"about_ca_system_score_codex":0.0006050641,"about_ca_system_score_gemma":0.00010524572,"threshold_uncertainty_score":0.9998041},"labels":[],"label_agreement":null},{"id":"W7108701346","doi":"10.71889/5fylantbak.30789470.v1","title":"A Multi-Year Study Of Lower Tropospheric Aerosol Variability And Systematic Relationships From Four North American Regions","year":2015,"lang":"","type":"article","venue":"Figshare","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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; Context (archaeology); Troposphere; Mixing ratio; Seasonality; Atmospheric dynamics; Atmosphere (unit)","score_opus":0.06609107292262364,"score_gpt":0.24881619572016092,"score_spread":0.18272512279753728,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7108701346","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":[0.9697373,0.00015974515,0.00014686922,0.00003730278,0.000106285974,0.0025926016,0.026894225,0.00005259876,0.00027309734],"genre_scores_gemma":[0.9955207,0.0000063136945,0.002813932,0.000032338237,0.00005266371,0.00031501142,0.0009585036,0.00004849346,0.00025205547],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99607384,0.0008784878,0.000940289,0.000899453,0.00076007354,0.0004478665],"domain_scores_gemma":[0.9967376,0.00052991253,0.0008931962,0.0011557218,0.00011411534,0.00056945794],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0003187678,0.00044153878,0.0008950577,0.0000028984614,0.00031363333,0.00009774048,0.00053360336,0.00012768051,0.02845165],"category_scores_gemma":[0.002930726,0.0003973991,0.0001266468,0.000918773,0.00017809831,0.00033146903,0.0006139453,0.0004610666,0.0013139269],"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":[0.0002009191,0.004261044,0.95581,0.0026164707,0.0003323082,0.00007633351,0.017549535,0.004605468,0.000031226933,0.0000023309815,0.014206297,0.00030804522],"study_design_scores_gemma":[0.0018187555,0.0016220429,0.95606107,0.0025451495,0.0003064112,0.000007449897,0.019306973,0.017600508,0.0000035737185,0.00001501599,0.00007969044,0.00063333707],"about_ca_topic_score_codex":0.001517963,"about_ca_topic_score_gemma":0.00279797,"teacher_disagreement_score":0.027137723,"about_ca_system_score_codex":0.00031369954,"about_ca_system_score_gemma":0.00009068375,"threshold_uncertainty_score":0.99984777},"labels":[],"label_agreement":null},{"id":"W7111287983","doi":"10.1021/acsestair.5c00035.s001","title":"Effects of FirePlume Height on the Geophysical Estimationof Surface Fine Particulate Matter from Satellite Aerosol OpticalDepth during North American Wildfires","year":2025,"lang":"","type":"article","venue":"Figshare","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Plume; Satellite; Particulates; Aerosol; Data assimilation; Visibility; Optical depth; Panache","score_opus":0.00612435346867015,"score_gpt":0.20617236479056505,"score_spread":0.2000480113218949,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7111287983","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":[0.98641276,0.00028630774,0.000011907001,0.0009464192,0.000077569544,0.0007721667,0.010846066,0.000040646708,0.0006061365],"genre_scores_gemma":[0.99679995,0.000028025972,0.0003528613,0.0005416009,0.0000676862,0.00011897945,0.0013389108,0.000039057082,0.0007129353],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9972381,0.00017998317,0.0005747763,0.0007969075,0.00054957747,0.00066065777],"domain_scores_gemma":[0.9975997,0.0009863739,0.00037200507,0.00082367414,0.000026010437,0.00019221827],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000044783144,0.00049325003,0.0005723278,0.0000027221788,0.00036295425,0.00011607676,0.00064937613,0.00009752805,0.08163362],"category_scores_gemma":[0.00022748744,0.0003634257,0.00024953188,0.00070335926,0.0002870041,0.00017442589,0.000603685,0.00038453387,0.007828991],"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":[0.0006163918,0.0025055162,0.8230061,0.0016713926,0.0010314987,0.00019508984,0.0023731436,0.058471236,0.014067548,0.000055389013,0.058531016,0.03747567],"study_design_scores_gemma":[0.00035434906,0.00014868735,0.95061684,0.0013838505,0.00007989634,5.458151e-7,0.000022370494,0.012343446,0.034304336,0.000029910272,0.00035660763,0.00035917218],"about_ca_topic_score_codex":0.00060552976,"about_ca_topic_score_gemma":0.00012696827,"teacher_disagreement_score":0.12761073,"about_ca_system_score_codex":0.00015549912,"about_ca_system_score_gemma":0.00003653804,"threshold_uncertainty_score":0.99988174},"labels":[],"label_agreement":null},{"id":"W7111992306","doi":"","title":"Yukon Dust from Source to Sink: Characterizing the St. Elias Mountains as a High-Latitude Dust Source","year":2025,"lang":"","type":"article","venue":"Digital Commons - Colby (Colby College)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Albedo (alchemy); Loess; Bedrock; Glacial period; Precipitation; Sediment; Climate change","score_opus":0.009683646234119488,"score_gpt":0.22537277708586334,"score_spread":0.21568913085174385,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7111992306","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":[0.93426675,0.0004026963,0.006980172,0.013383443,0.0013580722,0.00410034,0.0036597317,0.00035489068,0.035493925],"genre_scores_gemma":[0.9304993,0.00005008515,0.00048298598,0.00859163,0.00042415372,0.0004159854,0.0001574046,0.0002021575,0.059176277],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9913105,0.0003488129,0.0018759927,0.002343855,0.0018002136,0.0023206256],"domain_scores_gemma":[0.99412966,0.0011447077,0.00071917166,0.0027718577,0.00013454512,0.0011000634],"candidate_categories":["metaepi_narrow","sts","scholarly_communication","insufficient_payload"],"consensus_categories":["metaepi_narrow","insufficient_payload"],"category_scores_codex":[0.0005935369,0.0016496178,0.0015379995,0.000043323216,0.0033054103,0.0029713854,0.0035213768,0.0007663043,0.004917449],"category_scores_gemma":[0.00035457817,0.001501748,0.0006668152,0.0034955614,0.0014786486,0.0015604289,0.004571731,0.0016106374,0.0038130803],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.005843216,0.011064244,0.33481118,0.00036882,0.0040529026,0.000988759,0.018153988,0.07422512,0.018211937,0.019737639,0.35253692,0.16000529],"study_design_scores_gemma":[0.0025801803,0.0009696714,0.15575813,0.0006624236,0.00042538153,0.000027964836,0.008357101,0.012417272,0.0009627253,0.00088660524,0.8145753,0.0023772211],"about_ca_topic_score_codex":0.008132777,"about_ca_topic_score_gemma":0.003976875,"teacher_disagreement_score":0.4620384,"about_ca_system_score_codex":0.0021285145,"about_ca_system_score_gemma":0.0005515681,"threshold_uncertainty_score":0.9996251},"labels":[],"label_agreement":null},{"id":"W7112350168","doi":"","title":"Measurementsof microphysics in Cold Air Outbreaks","year":2023,"lang":"en","type":"article","venue":"Research Explorer (The University of Manchester)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Cloud condensation nuclei; Sea ice; Aerosol; Range (aeronautics); Ice crystals; Cloud physics; Marine stratocumulus; Cloud computing","score_opus":0.06929235708427642,"score_gpt":0.2695837912183747,"score_spread":0.2002914341340983,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7112350168","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":[0.99648935,0.000010321692,0.00008988905,0.0009804579,0.000028322902,0.00022287991,0.0000019279687,0.000023492981,0.0021533389],"genre_scores_gemma":[0.9992608,0.00011130084,0.0001510951,0.000036666406,0.000015514424,0.0000016012483,0.000002770598,0.0000097737175,0.00041052044],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983885,0.00016738402,0.00009821747,0.0002466915,0.0006975849,0.00040157852],"domain_scores_gemma":[0.99942243,0.000092198476,0.000037410275,0.00034793388,0.000023416937,0.000076585944],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00083328283,0.00008470936,0.0001253164,0.0000091198735,0.00021170956,0.000007722771,0.00061926316,0.00004969031,0.00060895784],"category_scores_gemma":[0.000022121832,0.00007535602,0.00005991867,0.0008660562,0.0005653325,0.00014895656,0.0006798978,0.00024667758,0.0015782926],"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":[0.00029628596,0.00060618966,0.61925167,0.00010760051,0.0000870579,0.00027554095,0.09982125,0.0064689177,0.15923859,0.00042817206,0.094118804,0.019299917],"study_design_scores_gemma":[0.001148259,0.0001853812,0.85213715,0.000074593605,0.000012932377,0.0000011816294,0.04995684,0.001274066,0.007562099,0.00066651334,0.086698085,0.0002829089],"about_ca_topic_score_codex":0.00022808692,"about_ca_topic_score_gemma":0.000045407265,"teacher_disagreement_score":0.23288547,"about_ca_system_score_codex":0.00022989743,"about_ca_system_score_gemma":0.000022127642,"threshold_uncertainty_score":0.9991991},"labels":[],"label_agreement":null},{"id":"W7117739103","doi":"10.1002/qj.70098","title":"Thermodynamic and microphysical properties of summertime marine fog observed from Sable Island","year":2025,"lang":"en","type":"article","venue":"Quarterly Journal of the Royal Meteorological Society","topic":"Atmospheric aerosols and clouds","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":false,"ca_institutions":"Ontario Tech University","funders":"Office of Naval Research","keywords":"Radiosonde; Visibility; Advection; Stratification (seeds); Precipitation; Warm front; Attenuation; Precipitable water","score_opus":0.008838619572662753,"score_gpt":0.1857189836508502,"score_spread":0.17688036407818747,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7117739103","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":[0.9977525,0.00025143096,0.0004948765,0.0007656091,0.000110131135,0.00009778768,0.0000037198197,0.0000056601293,0.0005183159],"genre_scores_gemma":[0.99730617,0.000013804051,0.0017421755,0.00032956945,0.00003802343,0.0000021541987,2.522106e-7,0.000005742889,0.00056213106],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9989164,0.00012402324,0.00036884713,0.00016393486,0.00023046913,0.000196335],"domain_scores_gemma":[0.99942386,0.000079905054,0.0002451527,0.00017367143,0.000019431513,0.000057985544],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023916463,0.00014350307,0.00034044482,7.531713e-7,0.00012393847,0.000025005296,0.00040310787,0.000112339876,0.0004787772],"category_scores_gemma":[0.000021587231,0.0000711815,0.00032664373,0.00011136911,0.00047822905,0.000060962433,0.00016007581,0.0002779706,0.0000046339464],"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":[0.00079409935,0.00082463544,0.36048073,0.00004769544,0.0006881259,0.0000075521034,0.0024519698,0.0014245693,0.57423687,0.00013356686,0.003939059,0.054971155],"study_design_scores_gemma":[0.0017733648,0.0016798028,0.9476035,0.000093891504,0.00030507956,0.000006107939,0.0011041849,0.025689358,0.009315687,0.011637808,0.0005006746,0.0002905023],"about_ca_topic_score_codex":0.00044360853,"about_ca_topic_score_gemma":0.000031754418,"teacher_disagreement_score":0.5871228,"about_ca_system_score_codex":0.00005578462,"about_ca_system_score_gemma":0.000013810432,"threshold_uncertainty_score":0.52422744},"labels":[],"label_agreement":null},{"id":"W7128205266","doi":"10.1088/1755-1315/1522/1/012001","title":"The performance of modified CCCma RTM in representing the Global Clear-sky Downwelling Shortwave Flux","year":2025,"lang":"","type":"article","venue":"IOP Conference Series Earth and Environmental Science","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"","keywords":"Shortwave; Downwelling; Albedo (alchemy); Flux (metallurgy); Radiative transfer; Aerosol; Atmospheric radiative transfer codes; Radiative flux","score_opus":0.009501937128253545,"score_gpt":0.21222896305327357,"score_spread":0.20272702592502004,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7128205266","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":[0.97951144,0.0009795962,0.00007927003,0.00095127104,0.00038164257,0.00055958057,0.00002567458,0.000013463505,0.017498042],"genre_scores_gemma":[0.9915563,0.0049287453,0.0002145671,0.00014345229,0.000027023438,0.000021467344,0.0000022371978,0.00000896195,0.003097269],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99589324,0.000118476615,0.000799911,0.0010226207,0.0010055593,0.0011602148],"domain_scores_gemma":[0.998485,0.000119412936,0.000303345,0.00085425016,0.000013308904,0.00022465357],"candidate_categories":["metaepi_narrow","sts"],"consensus_categories":["sts"],"category_scores_codex":[0.0014553745,0.00042331123,0.00037453522,0.000008545942,0.0023443312,0.0004324803,0.0014835038,0.00013905721,0.0005930181],"category_scores_gemma":[0.000067961104,0.00028320204,0.00009623775,0.0011187801,0.012067899,0.0009746455,0.0017197455,0.0004503917,0.00004121522],"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":[0.0006775829,0.00026199175,0.5476209,0.00008555868,0.00004616373,0.000015798792,0.0032082743,0.016633922,0.08197619,0.008825704,0.00004123731,0.34060666],"study_design_scores_gemma":[0.00043715106,0.00031845117,0.8890744,0.0001545407,0.00003123558,0.000020254442,0.008323649,0.061214436,0.03733797,0.00046252552,0.0022244998,0.00040088352],"about_ca_topic_score_codex":0.00069356523,"about_ca_topic_score_gemma":0.00057458144,"teacher_disagreement_score":0.3414535,"about_ca_system_score_codex":0.00022243346,"about_ca_system_score_gemma":0.00017160724,"threshold_uncertainty_score":0.99996203},"labels":[],"label_agreement":null},{"id":"W7128886080","doi":"","title":"Méthode avancée de caractérisation des aérosols par sondage lidar et photométrie solaire","year":2018,"lang":"en","type":"article","venue":"theses.fr (ABES)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Meteorological satellite; Repartition; Qualitative analysis","score_opus":0.027804002116441327,"score_gpt":0.2712222369140886,"score_spread":0.24341823479764726,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7128886080","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":[0.88761467,0.000056747187,0.015181109,0.00015708999,0.00013762576,0.00025215404,0.000011808324,0.00014784877,0.09644093],"genre_scores_gemma":[0.9860152,0.00008842549,0.012045069,0.00093792356,0.00020417092,0.000035365963,0.000006407312,0.00005201422,0.000615405],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99802196,0.00018445753,0.0002797358,0.0004534871,0.00040136842,0.000658988],"domain_scores_gemma":[0.99898964,0.00011486255,0.0001460777,0.00049993175,0.00002118553,0.00022827667],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0007280724,0.00027540277,0.0002487693,0.0000029360212,0.0004403706,0.000092155235,0.00041443077,0.00015661695,0.0051578963],"category_scores_gemma":[0.0001404843,0.00024068276,0.00010338438,0.0002556577,0.0007513788,0.00041948038,0.00023810336,0.00022207327,0.0023378034],"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":[0.00017566561,0.0005144591,0.70028174,0.000049605416,0.00008269628,0.00006984594,0.03940009,0.0006532463,0.20700519,0.0030666462,0.004882532,0.0438183],"study_design_scores_gemma":[0.0013704307,0.00069996883,0.6733734,0.0001395008,0.00012249425,0.000080168065,0.005309022,0.004904712,0.19039202,0.015361578,0.1068096,0.001437133],"about_ca_topic_score_codex":0.0036565254,"about_ca_topic_score_gemma":0.0010896048,"teacher_disagreement_score":0.101927064,"about_ca_system_score_codex":0.00029267053,"about_ca_system_score_gemma":0.000047517744,"threshold_uncertainty_score":0.998439},"labels":[],"label_agreement":null},{"id":"W7132997645","doi":"","title":"Aerosol-cloud condensation nuclei closure at a semi-rural site","year":2006,"lang":"","type":"dissertation","venue":"TSpace","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Cloud condensation nuclei; Condensation; Diffusion; Surface tension; Cloud chamber; Thermal; Atmosphere (unit); Closure (psychology)","score_opus":0.007908264521425604,"score_gpt":0.2580808507152714,"score_spread":0.2501725861938458,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7132997645","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":[0.9500415,0.0009079207,0.00021370636,0.00042065748,0.0020759213,0.001046183,0.000058020087,0.00016350638,0.045072637],"genre_scores_gemma":[0.71844405,0.00022719304,0.00039819116,0.000259587,0.00053616165,0.00005294649,0.0011611745,0.00014979368,0.27877092],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99455863,0.00020914554,0.0009918815,0.001399171,0.0015356763,0.0013054884],"domain_scores_gemma":[0.9972274,0.000107997075,0.0011446981,0.0010024303,0.00007333719,0.0004441848],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00032539223,0.0012150313,0.0009346406,0.0000068239638,0.0011612397,0.00023096867,0.00065405684,0.0012529761,0.03183913],"category_scores_gemma":[0.000044509656,0.0012705463,0.0005485204,0.0006716583,0.00049713167,0.00032342653,0.00033932243,0.0008566788,0.01138107],"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":[0.0012236066,0.00090752286,0.25198194,0.00055649556,0.00032170117,0.00017457163,0.060068928,0.012299587,0.5268284,0.00030864886,0.1407303,0.004598268],"study_design_scores_gemma":[0.007291291,0.0017573356,0.7484919,0.0013470759,0.0019346984,0.00017319662,0.0575816,0.016471375,0.07669306,0.0004169091,0.07833772,0.009503872],"about_ca_topic_score_codex":0.007959155,"about_ca_topic_score_gemma":0.006001141,"teacher_disagreement_score":0.4965099,"about_ca_system_score_codex":0.0014697541,"about_ca_system_score_gemma":0.00009821624,"threshold_uncertainty_score":0.99897444},"labels":[],"label_agreement":null},{"id":"W7139269946","doi":"","title":"Fiscal Year 2010","year":2011,"lang":"en","type":"article","venue":"University of North Texas Digital Library (University of North Texas)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Drizzle; Metric (unit); Range (aeronautics); Liquid water content; Quarter (Canadian coin); Cloud top; Cloud computing","score_opus":0.010151883171402651,"score_gpt":0.14814331195668254,"score_spread":0.1379914287852799,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7139269946","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":[0.91477054,0.000009597997,0.0005041733,0.00008035216,0.000062801446,0.00015575998,0.00032006323,0.00009824047,0.083998464],"genre_scores_gemma":[0.9660678,0.00005415277,0.0035470868,0.000037954283,0.000014370539,7.756419e-9,0.00010462411,0.000019232251,0.030154774],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99865586,0.000032159234,0.00015432513,0.00044464282,0.0003607714,0.00035222096],"domain_scores_gemma":[0.9989751,0.00003307629,0.000251808,0.00043774085,0.000016856342,0.00028543852],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000031528496,0.0002312023,0.00033614607,0.000018817747,0.00019352336,0.000015463409,0.0011317019,0.00010536051,0.012763199],"category_scores_gemma":[0.0000056538033,0.00029234684,0.00025447048,0.00051882217,0.001005681,0.0024627873,0.0011603836,0.00020173826,0.0014846891],"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":[0.00018126171,0.00026187042,0.9803901,0.000015912168,0.0000496387,0.000103400824,0.00014804007,0.00004964695,2.039215e-7,0.00007660199,0.013154377,0.005568945],"study_design_scores_gemma":[0.0005603988,0.00021744765,0.9629561,0.000013117816,0.0000447309,0.0000039578795,0.00012636236,0.000066061635,0.00000972415,0.00007595019,0.035627868,0.00029829142],"about_ca_topic_score_codex":0.0009856804,"about_ca_topic_score_gemma":0.0010947371,"teacher_disagreement_score":0.05384369,"about_ca_system_score_codex":0.000045794044,"about_ca_system_score_gemma":0.000043555698,"threshold_uncertainty_score":0.99995285},"labels":[],"label_agreement":null},{"id":"W7148856803","doi":"10.70675/0ec4283dz6e6az4d82zaa65za309d272e628","title":"Advanced aerosol characterization using sun/sky photometer and multi-wavelength Mie-Raman lidar measurements","year":2018,"lang":"","type":"dissertation","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Lidar; Photometer; Repartition; Aerosol","score_opus":0.03854304355627437,"score_gpt":0.2797971676170637,"score_spread":0.24125412406078933,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7148856803","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":[0.97713107,0.0001132678,0.018045977,0.000016669366,0.0014519577,0.0017190824,0.000045075663,0.00006925983,0.0014076361],"genre_scores_gemma":[0.94343203,0.00056593755,0.041723676,0.00032504703,0.00020140056,0.000080146885,0.00061116385,0.0001839945,0.012876614],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9943,0.000165456,0.0012208954,0.0018874196,0.0013191233,0.00110711],"domain_scores_gemma":[0.99756306,0.000029505496,0.0010510007,0.00071898144,0.000118352335,0.0005190743],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004529946,0.001188062,0.00089742045,0.000016915568,0.0010221553,0.00035743025,0.00052534754,0.0007776846,0.0066904854],"category_scores_gemma":[0.00007389353,0.0011550396,0.0002289243,0.0006663577,0.00046335591,0.0010980101,0.00026653954,0.00044176806,0.0005019142],"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":[0.00020156738,0.00038419783,0.015560018,0.00012027709,0.00011516245,0.000005124959,0.0021680247,0.00002176752,0.9203394,0.0000012519957,0.000009159522,0.061074045],"study_design_scores_gemma":[0.0054723076,0.0012302195,0.29283634,0.0009992955,0.00076338626,0.00003172598,0.0040453975,0.0994005,0.58795726,0.000011048407,0.0029079285,0.0043445756],"about_ca_topic_score_codex":0.0004838766,"about_ca_topic_score_gemma":0.0004035876,"teacher_disagreement_score":0.3323821,"about_ca_system_score_codex":0.0005241059,"about_ca_system_score_gemma":0.000086791675,"threshold_uncertainty_score":0.99908996},"labels":[],"label_agreement":null},{"id":"W7150958654","doi":"10.70675/c36ec938za275z4072z847dz2e151b2acde6","title":"Restitution du contenu en glace des nuages à partir de mesures à haute résolution spectrale dans l’infrarouge des instruments satellitaires IASI et IASI-NG","year":2021,"lang":"","type":"dissertation","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Western europe; Nova scotia","score_opus":0.011509230852435152,"score_gpt":0.27737964391911263,"score_spread":0.26587041306667747,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7150958654","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":[0.9508911,0.001788499,0.008483445,0.00025744777,0.0005661538,0.0008199906,0.00005561949,0.00016262042,0.036975157],"genre_scores_gemma":[0.96187,0.01400953,0.010065994,0.00023499381,0.0001852937,0.00013361563,0.00063871086,0.00010421503,0.0127576385],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9934714,0.0010343997,0.0012607591,0.0015870223,0.0010834924,0.001562921],"domain_scores_gemma":[0.99784625,0.00020251557,0.00055957795,0.0007488966,0.00008680714,0.0005559718],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010882057,0.0011460577,0.0009126851,0.000014425163,0.002121092,0.00065284566,0.0008010218,0.00085312314,0.009936641],"category_scores_gemma":[0.0003308295,0.0011335161,0.00048804408,0.00073132257,0.0023910715,0.0015963711,0.00024370753,0.00075737364,0.00043057144],"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":[0.0006023784,0.0013231772,0.69625163,0.0005430762,0.0005311925,0.00025403706,0.0652661,0.011001159,0.143917,0.008320768,0.0009927527,0.07099674],"study_design_scores_gemma":[0.00087150314,0.00036464972,0.8729507,0.00068886345,0.00034921413,0.00008975389,0.032788087,0.0030982713,0.08271961,0.0035670241,0.0013015303,0.0012108281],"about_ca_topic_score_codex":0.015117194,"about_ca_topic_score_gemma":0.014193196,"teacher_disagreement_score":0.17669904,"about_ca_system_score_codex":0.0018611435,"about_ca_system_score_gemma":0.00041913762,"threshold_uncertainty_score":0.999178},"labels":[],"label_agreement":null},{"id":"W7161798340","doi":"10.82308/3296","title":"Environmental conditions favouring ice pellet aggregation","year":2008,"lang":"en","type":"dissertation","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Precipitation; Freezing rain; Rain and snow mixed; Atmosphere (unit); Precipitation types; Ice nucleus","score_opus":0.005731118960343053,"score_gpt":0.21239943933328911,"score_spread":0.20666832037294605,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7161798340","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":[0.75223815,0.00007536646,0.000066509616,0.000022114773,0.0002546508,0.00023577707,0.000016507984,0.00006186936,0.24702904],"genre_scores_gemma":[0.83965045,0.00039218133,0.0007338419,0.00013558872,0.00008546953,0.000049522987,0.001082889,0.000041584914,0.15782847],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9985872,0.000023135151,0.00027199063,0.00042506526,0.00042577359,0.0002668396],"domain_scores_gemma":[0.9994419,0.000022304344,0.00017675536,0.00024734353,0.00000195069,0.00010969943],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000039942912,0.00026993616,0.00018543364,0.00000225893,0.00035295935,0.000023387187,0.00020828602,0.00022911995,0.04641509],"category_scores_gemma":[0.000007157921,0.0002643488,0.00012643136,0.000091078684,0.000103458144,0.00016272767,0.000050806528,0.00022886506,0.005132762],"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":[0.00042815204,0.002196798,0.20116796,0.00019095106,0.00047269018,0.00041529487,0.019458001,0.0068967305,0.11643322,0.0009516415,0.5235715,0.12781711],"study_design_scores_gemma":[0.0014340681,0.00016115501,0.8907142,0.00008394608,0.00015601842,0.00007532974,0.0067873104,0.00096488534,0.012743801,0.00050077663,0.0845954,0.0017831073],"about_ca_topic_score_codex":0.00027621418,"about_ca_topic_score_gemma":0.00021565589,"teacher_disagreement_score":0.6895462,"about_ca_system_score_codex":0.00023624963,"about_ca_system_score_gemma":0.000012971942,"threshold_uncertainty_score":0.99998087},"labels":[],"label_agreement":null},{"id":"W7161818413","doi":"10.82308/34147","title":"Detecting and understanding climate change using hyperspectral radiative measurements","year":2024,"lang":"en","type":"dissertation","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Radiance; High resolution; Hyperspectral imaging; Interferometry","score_opus":0.11285986907401044,"score_gpt":0.2973421319617755,"score_spread":0.18448226288776506,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7161818413","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":[0.92258775,0.0006573804,0.00028981778,0.000026845104,0.00059387204,0.0003149106,0.0000032940595,0.00008059974,0.0754455],"genre_scores_gemma":[0.9966264,0.000142755,0.002106608,0.000056058056,0.00010732602,0.000014913413,0.000011050159,0.000048250567,0.00088667625],"study_design_codex":"observational","study_design_gemma":"qualitative","domain_scores_codex":[0.9987654,0.000021465885,0.00016333487,0.000416484,0.00030330938,0.00033001372],"domain_scores_gemma":[0.99972165,0.000014107566,0.00009097401,0.000089529036,0.0000035215073,0.000080251295],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016606566,0.000230617,0.0001859407,0.0000035355197,0.0002502437,0.00008891387,0.000077855904,0.0001407432,0.00080466515],"category_scores_gemma":[0.000009261342,0.00020441784,0.000057458565,0.00017105631,0.000043113116,0.00015410602,0.00006144175,0.00020217756,0.00007310288],"study_design_candidate":"qualitative","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":[0.00075844594,0.00041732818,0.35908806,0.0030850081,0.0015591072,0.0003541798,0.25381038,0.0018635402,0.23406582,0.010104387,0.0015723751,0.13332136],"study_design_scores_gemma":[0.0035839942,0.0011352566,0.18271947,0.004381671,0.0033256214,0.00015794465,0.5592506,0.18449683,0.026414355,0.024433881,0.0007564526,0.00934392],"about_ca_topic_score_codex":0.0006207109,"about_ca_topic_score_gemma":0.001034772,"teacher_disagreement_score":0.30544022,"about_ca_system_score_codex":0.0007520613,"about_ca_system_score_gemma":0.000008290806,"threshold_uncertainty_score":0.8810519},"labels":[],"label_agreement":null},{"id":"W7161969471","doi":"10.82308/16735","title":"Characterization of cloud and precipitation features over the eastern Canadian Artic as inferred from CloudSat and Aqua","year":2010,"lang":"en","type":"dissertation","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Terrain; Precipitation; Gloom; Ceilometer","score_opus":0.0036773343774637313,"score_gpt":0.20614516960766577,"score_spread":0.20246783523020204,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7161969471","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":[0.9934514,0.00005431729,0.00001665608,0.00013612487,0.00040346757,0.00029259417,0.000027202219,0.000010052967,0.005608146],"genre_scores_gemma":[0.99118185,0.000076459735,0.000084130035,0.00024005986,0.00008342894,0.000014738637,0.00053740694,0.000019580757,0.007762322],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991553,0.000033093787,0.00019163515,0.00026481898,0.00020062317,0.00015455025],"domain_scores_gemma":[0.9994753,0.000037387104,0.00017093861,0.00018005435,0.000011068912,0.00012524142],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000070003356,0.00017486754,0.00016125351,0.0000029309824,0.0001226884,0.0000684275,0.000112699134,0.000256731,0.0014506531],"category_scores_gemma":[0.00002838575,0.00012478435,0.000026622018,0.000076769735,0.0000986988,0.00012420746,0.00003189653,0.00019670963,0.000033948592],"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":[0.00017947529,0.000059367696,0.6885041,0.00005749288,0.00009770451,0.0000039420065,0.023056246,0.000013429295,0.2286334,0.00063193653,0.0009475664,0.057815325],"study_design_scores_gemma":[0.00014558661,0.000035388915,0.9953779,0.000023750903,0.00004540017,0.0000010706304,0.0006457982,0.00036845866,0.0014756628,0.0005322982,0.0011937041,0.00015501125],"about_ca_topic_score_codex":0.26718473,"about_ca_topic_score_gemma":0.6054458,"teacher_disagreement_score":0.33826104,"about_ca_system_score_codex":0.000034889206,"about_ca_system_score_gemma":0.00003573705,"threshold_uncertainty_score":0.9994621},"labels":[],"label_agreement":null},{"id":"W7407898","doi":"","title":"FY 2010 Fourth Quarter Report: Evaluation of the Dependency of Drizzle Formation on Aerosol Properties","year":2010,"lang":"en","type":"article","venue":"University of North Texas Digital Library (University of North Texas)","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"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":"Drizzle; Aerosol; Meteorology; Weather Research and Forecasting Model; Environmental science; Dependency (UML); Tower; Quarter (Canadian coin); Atmospheric sciences; Computer science; Geography; Physics","score_opus":0.012126958790061943,"score_gpt":0.16874794377570335,"score_spread":0.1566209849856414,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7407898","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":[0.9876539,0.000006230188,0.00026774427,0.00018697372,0.0001000587,0.0004331288,0.0001553798,0.000031264906,0.011165325],"genre_scores_gemma":[0.9955886,0.000011805538,0.00054613024,0.000014813307,0.000010629079,4.4985423e-8,0.000069544825,0.000010902887,0.0037475296],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982649,0.00006753752,0.00027589677,0.00030761948,0.0008771478,0.00020690575],"domain_scores_gemma":[0.9983947,0.000036892103,0.0007847542,0.00058914436,0.00009297451,0.000101528894],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00013268262,0.00018664975,0.00030046687,0.000020967178,0.00019277865,0.000013418928,0.0008497043,0.00010527,0.0013401331],"category_scores_gemma":[0.0000295392,0.0001782311,0.00024371051,0.00041599208,0.00079003617,0.0024802168,0.00052899425,0.00023198465,0.000060483202],"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":[0.00013016038,0.000259076,0.9903759,0.000040014664,0.00003554844,0.000009281097,0.00021332565,0.0011935184,0.000032002037,0.00002586847,0.001450295,0.0062350063],"study_design_scores_gemma":[0.0006479983,0.00021421547,0.99543583,0.00004047251,0.0000922478,0.000008631935,0.0001927056,0.00143656,0.00058579823,0.000060587303,0.0011007236,0.0001842334],"about_ca_topic_score_codex":0.00053821964,"about_ca_topic_score_gemma":0.0026719405,"teacher_disagreement_score":0.007934704,"about_ca_system_score_codex":0.000046246838,"about_ca_system_score_gemma":0.00011368542,"threshold_uncertainty_score":0.99957275},"labels":[],"label_agreement":null},{"id":"W765537382","doi":"10.1016/0967-0653(96)89924-8","title":"10.1016/0967-0653(96)89924-8","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Thermal diffusivity; Optics; Field (mathematics); Direction cosine; Diaphragm (acoustics); Trigonometric functions; Remote sensing; Acoustics; Physics; Geology; Mathematics; Geometry; Vibration","score_opus":0.003906747923973831,"score_gpt":0.15684238069704126,"score_spread":0.15293563277306743,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W765537382","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00969996,0.000017422075,0.0000043502137,0.00022993796,0.0000014915476,0.00012702268,0.000003909391,0.000087920125,0.989828],"genre_scores_gemma":[0.0015749058,2.5666557e-7,0.00051741913,0.00013883335,0.00006636023,0.000014886679,0.000004325283,0.00002037103,0.99766266],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990219,0.0000215622,0.00013736422,0.00027449892,0.00023307058,0.0003116318],"domain_scores_gemma":[0.99949014,0.000015011172,0.000021986922,0.00028424102,0.0000028695038,0.00018575475],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000086788255,0.0001350705,0.000121557154,7.8278407e-7,0.00010616822,0.000027500742,0.00027301736,0.000055960543,0.99983793],"category_scores_gemma":[0.000008285089,0.00012151757,0.000051933697,0.00019587982,0.00007923289,0.00009840039,0.00009630108,0.00008094726,0.99940157],"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":[0.00002019285,0.000039349397,0.0000063176153,7.775677e-7,0.0000038554026,0.0000045342194,0.000024570081,0.00058084,0.00007334097,3.4231218e-7,0.33294487,0.666301],"study_design_scores_gemma":[0.00011827081,0.0000986973,0.00056610286,0.0000035945504,0.0000072553935,0.000004796838,0.0000017934663,0.00033703292,0.00007879159,0.000010147372,0.9985941,0.00017940091],"about_ca_topic_score_codex":0.00013010969,"about_ca_topic_score_gemma":8.72954e-7,"teacher_disagreement_score":0.6661216,"about_ca_system_score_codex":0.00007076986,"about_ca_system_score_gemma":0.00000534392,"threshold_uncertainty_score":0.4955343},"labels":[],"label_agreement":null},{"id":"W84077831","doi":"10.1007/978-1-4419-5582-1_14","title":"Standoff Aerosol Size Determination based on Multiple-Field-Of-View of Elastic Scattering","year":2014,"lang":"en","type":"book-chapter","venue":"Integrated analytical systems","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Defence Research and Development Canada","funders":"","keywords":"Aerosol; Lidar; Bioaerosol; Attenuation; Scattering; Optics; Remote sensing; Transmission (telecommunications); Light scattering; Field (mathematics); Materials science; Environmental science; Physics; Computer science; Meteorology; Geology; Mathematics","score_opus":0.012236599898638071,"score_gpt":0.23587946922786227,"score_spread":0.2236428693292242,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W84077831","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.059028197,0.0002939854,0.17585467,0.0002214675,0.0015965204,0.0024115045,0.00021624094,0.0002105344,0.7601669],"genre_scores_gemma":[0.9700647,0.000013001613,0.00020529648,0.000075885,0.0000627478,0.0000141123965,0.000013870686,0.000049641865,0.02950075],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9975729,0.00006402277,0.0009263173,0.00047225502,0.0006962981,0.00026818883],"domain_scores_gemma":[0.99745584,0.0013371954,0.00054641295,0.00044371298,0.000065753666,0.0001511181],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00029146127,0.0004084935,0.00087176124,0.000009118548,0.000046459365,0.000028275888,0.00034459744,0.00042392313,0.0023582417],"category_scores_gemma":[0.0004722395,0.00031140613,0.00027042453,0.00010140951,0.0002606417,0.00003501429,0.00007054133,0.00036086628,0.00019893626],"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":[0.005359328,0.0031809714,0.11025175,0.015920196,0.002852893,0.000693813,0.0012327944,0.23025627,0.08551516,0.099605106,0.022557802,0.42257392],"study_design_scores_gemma":[0.0012547354,0.0018099966,0.0004724718,0.0060289875,0.00040377924,0.000011511983,0.00006750174,0.96854806,0.0020077762,0.0001973299,0.018110888,0.0010869754],"about_ca_topic_score_codex":0.0004860282,"about_ca_topic_score_gemma":0.000064401516,"teacher_disagreement_score":0.9110365,"about_ca_system_score_codex":0.00024989925,"about_ca_system_score_gemma":0.00003434103,"threshold_uncertainty_score":0.9999338},"labels":[],"label_agreement":null},{"id":"W86560332","doi":"","title":"Real-Time Cloud, Radiation, and Aircraft Icing Parameters from GOES over the USA","year":2004,"lang":"en","type":"article","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":25,"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":"Ceilometer; Icing; Meteorology; Environmental science; Cloud computing; Altitude (triangle); Remote sensing; Computer science; Geology; Geography; Mathematics","score_opus":0.005878028670771554,"score_gpt":0.20631335669305434,"score_spread":0.20043532802228278,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W86560332","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":[0.9902041,0.000020119602,0.0008383682,0.0005133579,0.00006373845,0.000097157324,0.000002093668,0.000029654217,0.0082314415],"genre_scores_gemma":[0.99111295,0.000093856506,0.006545647,0.0007814764,0.00004852143,0.0000049085465,0.0000020954062,0.000008707556,0.0014018321],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993365,0.000019148081,0.00011485182,0.00020721146,0.00015905089,0.00016327146],"domain_scores_gemma":[0.99964815,0.00006185619,0.000039635317,0.00018502034,0.0000014359244,0.00006387751],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00008258557,0.000093935974,0.00008299479,3.7341502e-7,0.00015384362,0.000039222377,0.00012072466,0.00003935912,0.0040272893],"category_scores_gemma":[0.000011479361,0.000057682177,0.000028091396,0.00008237492,0.00016842636,0.000117124444,0.00008715467,0.000054070748,0.000571069],"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":[0.000021533651,0.00007037284,0.9257005,0.0000019007165,0.000044409593,0.000008160326,0.0025860996,0.019179992,0.024965677,0.0009962303,0.009981422,0.016443739],"study_design_scores_gemma":[0.0003541127,0.00003611201,0.9917556,0.000004172509,0.000015916634,0.0000019111299,0.0001562681,0.0011707766,0.0016026177,0.0026691796,0.0020833022,0.00015002517],"about_ca_topic_score_codex":0.027243754,"about_ca_topic_score_gemma":0.00073192077,"teacher_disagreement_score":0.06605514,"about_ca_system_score_codex":0.000075614975,"about_ca_system_score_gemma":0.000005711042,"threshold_uncertainty_score":0.99688315},"labels":[],"label_agreement":null},{"id":"W878131592","doi":"10.1016/j.optcom.2015.06.071","title":"Analytical algorithm to determine the spherical particle size distribution from spectral absorption measurements","year":2015,"lang":"en","type":"article","venue":"Optics Communications","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":5,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"National Natural Science Foundation of China","keywords":"Optics; Smoothing; Inversion (geology); Algorithm; Refractive index; Inverse transform sampling; Diffraction; Computational physics; Computer science; Physics; Geology","score_opus":0.07578074493804891,"score_gpt":0.2900405401988511,"score_spread":0.2142597952608022,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W878131592","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":[0.89662784,0.000054656695,0.08198484,0.008253241,0.00009153415,0.00030499647,0.00003960155,0.000060048995,0.012583229],"genre_scores_gemma":[0.91263133,0.000014728004,0.086571634,0.00029340136,0.000044808952,0.00003195513,0.00003771608,0.000008901329,0.0003654996],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9989879,0.000099943,0.00020423574,0.00016228468,0.00033539292,0.00021021871],"domain_scores_gemma":[0.9985203,0.00012776972,0.000049549868,0.0010555874,0.00002724331,0.00021955007],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002669429,0.00009635256,0.00009547701,2.6115987e-7,0.00022586746,0.000058354406,0.00068038964,0.00004115883,0.00037820038],"category_scores_gemma":[0.00019636778,0.00007409877,0.000043169035,0.0002610059,0.00022630265,0.00009210717,0.00050448533,0.00013608366,0.00071829965],"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":[0.00021257924,0.0046790517,0.5327116,0.000004340682,0.0003298655,0.000013934205,0.007601997,0.025592843,0.023954151,0.014446684,0.039421327,0.3510316],"study_design_scores_gemma":[0.00057488866,0.00017196215,0.28978238,0.000008489243,0.0001013945,0.0000035865612,0.0006724068,0.6774675,0.00090466987,0.0020425657,0.027952245,0.00031787352],"about_ca_topic_score_codex":0.00046295498,"about_ca_topic_score_gemma":0.00022243687,"teacher_disagreement_score":0.65187466,"about_ca_system_score_codex":0.00024900984,"about_ca_system_score_gemma":0.000016615342,"threshold_uncertainty_score":0.9232529},"labels":[],"label_agreement":null},{"id":"W977725538","doi":"10.2172/1040616","title":"Cloud system resolving modelling and 3D solar radiative transfer","year":2012,"lang":"en","type":"report","venue":"","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","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":"Environment and Climate Change Canada","funders":"","keywords":"Radiative transfer; Cloud computing; Atmospheric radiative transfer codes; Environmental science; Meteorology; Thermal radiation; Cloud physics; Radiation; Atmospheric sciences; Computer science; Physics; Optics","score_opus":0.03271999073812069,"score_gpt":0.22788184372802459,"score_spread":0.1951618529899039,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W977725538","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.033163156,0.004095515,0.3400955,0.000027945967,0.0012328193,0.0005721216,0.000022738814,0.00018403871,0.6206062],"genre_scores_gemma":[0.966638,0.0019998662,0.007145631,0.000057311652,0.000807969,0.000034858807,0.000011763089,0.000094440176,0.02321014],"study_design_codex":"simulation_or_modeling","study_design_gemma":"not_applicable","domain_scores_codex":[0.9976912,0.000060317216,0.0004120385,0.00054387527,0.0007789009,0.00051362894],"domain_scores_gemma":[0.99927634,0.00005036695,0.00009472384,0.00032189753,0.000015750782,0.00024089818],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00070294726,0.00037039947,0.00048911327,0.0000018391958,0.0002280699,0.000049633803,0.00019178732,0.00039526413,0.0021145418],"category_scores_gemma":[0.000007760143,0.00029708818,0.00011658757,0.00009462537,0.00015220752,0.00017528265,0.0001494286,0.00038826469,0.00021219514],"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":[0.0004114884,0.0009590797,0.21694888,0.0066057756,0.0021615871,0.0005862227,0.029870871,0.3836011,0.001371196,0.0037026056,0.17429027,0.17949092],"study_design_scores_gemma":[0.00088269566,0.00026516736,0.0036037904,0.000794888,0.0008268757,0.00038506524,0.002860897,0.22608565,0.0004313778,0.00006571344,0.76069784,0.003100071],"about_ca_topic_score_codex":0.0028342959,"about_ca_topic_score_gemma":0.00008425092,"teacher_disagreement_score":0.93347484,"about_ca_system_score_codex":0.0006457989,"about_ca_system_score_gemma":0.000061018032,"threshold_uncertainty_score":0.99994814},"labels":[],"label_agreement":null}]}