{"meta":{"query_hash":"5375ea23f073","filters":{"venue":"13th Conference on Cloud Physics/13th Conference on Atmospheric Radiation (28 June–2 July 2010)"},"cohort_total":11,"direct_labels_cover":0,"predictions_cover":11,"exported":11,"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/5375ea23f073","api":"https://metacan.xera.ac/api/v1/cohort?venue=13th+Conference+on+Cloud+Physics%2F13th+Conference+on+Atmospheric+Radiation+%2828+June%E2%80%932+July+2010%29"},"results":[{"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":"W2801632056","doi":"","title":"Examining the Impact of Smoke Aerosol on Clouds and Precipitation using a Regional Model WRF-Chem-SMOKE and A-Train Data: A Case Study of Canadian Boreal Forest Wildfires in Summer 2007","year":2010,"lang":"en","type":"article","venue":"13th Conference on Cloud Physics/13th Conference on Atmospheric Radiation (28 June–2 July 2010)","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","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; Environmental science; Precipitation; Weather Research and Forecasting Model; Aerosol; Taiga; Climatology; Boreal; Meteorology; Atmospheric sciences; Forestry; Geography; Geology","score_opus":0.13451754106487246,"score_gpt":0.309316350741133,"score_spread":0.17479880967626055,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2801632056","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963801,0.000047035934,0.00012056194,0.000136039,0.0003379052,0.00085499434,0.00033818735,0.000022651326,0.0017625194],"genre_scores_gemma":[0.99852216,0.00012407309,0.0006596304,0.000108273416,0.0002186797,0.000015213219,0.0002628393,0.00002281832,0.00006632609],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99698114,0.00021194138,0.00073360367,0.0009025494,0.0005636237,0.0006071109],"domain_scores_gemma":[0.99720246,0.0005410069,0.0006822464,0.00094682095,0.00022094263,0.00040654343],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00067449216,0.0005512112,0.0006401882,0.000027430071,0.0003334144,0.00019906137,0.00056125555,0.00026147903,0.00015498865],"category_scores_gemma":[0.00017415693,0.00043975477,0.00007069105,0.00067182817,0.00048746177,0.0005354956,0.000048629332,0.0007964068,0.0000050766193],"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":[0.001068964,0.0011145257,0.7818241,0.00013020156,0.00032187442,0.00015062113,0.015732218,0.11803906,0.0021372826,0.0019564186,0.001460335,0.07606441],"study_design_scores_gemma":[0.0014906683,0.00087557,0.4039253,0.00013178281,0.00006040878,0.00004087216,0.0033669772,0.5889158,0.00010014413,0.00060051045,0.0000205721,0.00047139436],"about_ca_topic_score_codex":0.4214059,"about_ca_topic_score_gemma":0.17917366,"teacher_disagreement_score":0.47087672,"about_ca_system_score_codex":0.000046886093,"about_ca_system_score_gemma":0.0012038425,"threshold_uncertainty_score":0.99980545},"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":"W2890227997","doi":"","title":"Ice microphysics and aerosol indirect effects based on in-situ observations collected during the ISDAC field project","year":2010,"lang":"en","type":"article","venue":"13th Conference on Cloud Physics/13th Conference on Atmospheric Radiation (28 June–2 July 2010)","topic":"Icing and De-icing Technologies","field":"Engineering","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; Environmental science; Meteorology; Atmospheric sciences; Climatology; Geology; Geography","score_opus":0.017606194898702316,"score_gpt":0.22461640600483312,"score_spread":0.2070102111061308,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2890227997","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9833633,0.000024827892,0.0037449184,0.0010393495,0.002495807,0.0015187586,0.00003705042,0.0010799273,0.0066960678],"genre_scores_gemma":[0.99649596,0.00014542087,0.0013976266,0.00052589754,0.00028689817,0.00030041748,0.00004183827,0.00009271205,0.0007132012],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99725276,0.00017584594,0.00054826424,0.00076872524,0.00051016134,0.00074422895],"domain_scores_gemma":[0.9972442,0.0010166614,0.00027080005,0.0011069186,0.0002366415,0.00012482407],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00025063704,0.0007200989,0.00068912335,0.00006868867,0.00047076252,0.00034680613,0.00065110717,0.00044825938,0.000030491648],"category_scores_gemma":[0.00040989392,0.0006265761,0.00012580796,0.0013187049,0.00021619166,0.00023133206,0.000069384376,0.001766331,0.00011525044],"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":[0.0015505365,0.0024601286,0.0131892115,0.0019137257,0.00067420467,0.000114689,0.011496396,0.068616204,0.5309623,0.07952951,0.041459158,0.24803393],"study_design_scores_gemma":[0.0046004085,0.0013511205,0.09854729,0.0011354216,0.00013475498,0.000007126104,0.00038230667,0.44963387,0.4361012,0.0037756779,0.0019837732,0.002347035],"about_ca_topic_score_codex":0.000303801,"about_ca_topic_score_gemma":0.00038570262,"teacher_disagreement_score":0.38101768,"about_ca_system_score_codex":0.0001755886,"about_ca_system_score_gemma":0.00037186508,"threshold_uncertainty_score":0.99961853},"labels":[],"label_agreement":null},{"id":"W2891490927","doi":"","title":"Comparison of Longwave Atmospheric Fluxes and Cloud Radiative Forcing over Barrow, Alaska and Eureka, Nunavut","year":2010,"lang":"en","type":"article","venue":"13th Conference on Cloud Physics/13th Conference on Atmospheric Radiation (28 June–2 July 2010)","topic":"Meteorological Phenomena and Simulations","field":"Earth and Planetary Sciences","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":"Longwave; Environmental science; Radiative forcing; Atmospheric sciences; Climatology; Meteorology; Forcing (mathematics); Radiative transfer; Cloud forcing; Geography; Geology; Aerosol","score_opus":0.03312832368129233,"score_gpt":0.2710770325830994,"score_spread":0.23794870890180708,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2891490927","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97841823,0.00031435335,0.0025001692,0.00054077886,0.00302804,0.0009662297,0.00025922814,0.00013659478,0.013836374],"genre_scores_gemma":[0.99444705,0.00032722464,0.0027457504,0.00046561062,0.0007351194,0.000020015434,0.00022652445,0.000033099845,0.0009995864],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.995719,0.00038129583,0.0010343376,0.0011928915,0.0008241618,0.0008483101],"domain_scores_gemma":[0.99621373,0.0010829782,0.00094311056,0.000752981,0.0003662017,0.0006409826],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005364074,0.00079628127,0.0011909951,0.000023569146,0.000574564,0.0003352507,0.0005488085,0.00042597426,0.0038272485],"category_scores_gemma":[0.00030582733,0.00069263345,0.00017006313,0.0006472333,0.0007563033,0.0005597744,0.000063604195,0.0011231239,0.00023398148],"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":[0.0009600421,0.0007999945,0.6471633,0.00022418833,0.00037085434,0.000015957987,0.008203346,0.03415318,0.002590774,0.08369641,0.00641427,0.21540773],"study_design_scores_gemma":[0.0018210704,0.0012389335,0.4699967,0.00009240909,0.00011480031,0.0000035984776,0.000541133,0.5054934,0.00036600395,0.016108958,0.003255708,0.0009672503],"about_ca_topic_score_codex":0.0007254763,"about_ca_topic_score_gemma":0.00072653545,"teacher_disagreement_score":0.47134024,"about_ca_system_score_codex":0.000030181718,"about_ca_system_score_gemma":0.00036728277,"threshold_uncertainty_score":0.9995525},"labels":[],"label_agreement":null},{"id":"W2893320781","doi":"","title":"GCIP measurements of precipitation and fog during SNOW-V10 and FRAM projects","year":2010,"lang":"en","type":"article","venue":"13th Conference on Cloud Physics/13th Conference on Atmospheric Radiation (28 June–2 July 2010)","topic":"Meteorological Phenomena and Simulations","field":"Earth and Planetary Sciences","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":"Snow; Precipitation; Environmental science; Meteorology; Atmospheric sciences; Climatology; Geology; Geography","score_opus":0.05355922635494888,"score_gpt":0.2521878069827727,"score_spread":0.19862858062782385,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2893320781","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9827324,0.00007241732,0.00060976425,0.0004245883,0.0013798373,0.0009032189,0.00009329189,0.0000953367,0.013689159],"genre_scores_gemma":[0.99635094,0.00014859365,0.0021252753,0.00018790204,0.00030867863,0.000023606271,0.00013930358,0.000017608267,0.00069806265],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99695915,0.00025820345,0.00064323284,0.0008409431,0.000745664,0.000552803],"domain_scores_gemma":[0.9977117,0.00043294585,0.00056679826,0.0005256351,0.00039063624,0.00037225668],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00050307193,0.00048402778,0.00057909405,0.00003777558,0.00041762347,0.00023457181,0.0003447562,0.0002768452,0.0013847349],"category_scores_gemma":[0.0003776734,0.00042094357,0.00008422359,0.00042234318,0.0003554691,0.00047051738,0.00003365936,0.00063811423,0.00017994113],"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":[0.0016594542,0.0011200776,0.4419152,0.00050412177,0.00041625096,0.000012755722,0.009726347,0.014518883,0.029812086,0.054352596,0.0015276067,0.4444346],"study_design_scores_gemma":[0.0022774085,0.0011093346,0.866793,0.00014966914,0.00009023313,0.0000036693718,0.00028136876,0.10531033,0.0017788921,0.020691039,0.0006315897,0.00088349363],"about_ca_topic_score_codex":0.0005027818,"about_ca_topic_score_gemma":0.00040792697,"teacher_disagreement_score":0.44355112,"about_ca_system_score_codex":0.000018223034,"about_ca_system_score_gemma":0.00026365544,"threshold_uncertainty_score":0.9998242},"labels":[],"label_agreement":null},{"id":"W2894342635","doi":"","title":"Characteristics of orographic cloud and precipitation in the Arctic during STAR","year":2010,"lang":"en","type":"article","venue":"13th Conference on Cloud Physics/13th Conference on Atmospheric Radiation (28 June–2 July 2010)","topic":"Methane Hydrates and Related Phenomena","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 Manitoba","funders":"","keywords":"Orographic lift; Precipitation; Climatology; Arctic; Orography; Meteorology; Cloud computing; Environmental science; Atmospheric sciences; Geography; Geology; Computer science; Oceanography","score_opus":0.013966788975618085,"score_gpt":0.22600835860096777,"score_spread":0.21204156962534967,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2894342635","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99172646,0.000030169083,0.00019010704,0.0008430647,0.0016592978,0.0008760231,0.00004036933,0.000053250093,0.0045812353],"genre_scores_gemma":[0.99732184,0.0006456396,0.00066887325,0.00025860328,0.00028529434,0.000091831396,0.00006611133,0.000044910008,0.00061688654],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.9965948,0.0003704294,0.0008015883,0.0008126255,0.0008024394,0.00061811303],"domain_scores_gemma":[0.99773574,0.00031580744,0.0007631139,0.0008447142,0.00011743445,0.00022318242],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00072662754,0.0005297116,0.0005705268,0.000030165998,0.00028102472,0.00018311653,0.0006609013,0.0002884758,0.0013155488],"category_scores_gemma":[0.00015248099,0.0004218651,0.00011800396,0.0008420209,0.0005725744,0.0003415429,0.00010221464,0.0011775632,0.00034104678],"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":[0.0023692728,0.0062135635,0.21059863,0.0010047138,0.0005427026,0.00008560211,0.05593612,0.007277504,0.15304403,0.32401004,0.0030774218,0.23584038],"study_design_scores_gemma":[0.0030784416,0.0010682822,0.9108673,0.00033785062,0.0001529749,0.000014014499,0.0010025724,0.047962606,0.0019246872,0.028428562,0.003718947,0.0014437804],"about_ca_topic_score_codex":0.0007644646,"about_ca_topic_score_gemma":0.00021963583,"teacher_disagreement_score":0.7002686,"about_ca_system_score_codex":0.00010034359,"about_ca_system_score_gemma":0.0001167121,"threshold_uncertainty_score":0.99982333},"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":"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":"W2946185971","doi":"","title":"Sampling of cloud and clear-sky radiances over Arctic from two-satellite system on Molniya orbit","year":2010,"lang":"en","type":"article","venue":"13th Conference on Cloud Physics/13th Conference on Atmospheric Radiation (28 June–2 July 2010)","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","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":"Satellite; Remote sensing; Sky; Cloud computing; Orbit (dynamics); Environmental science; Arctic; Sampling (signal processing); Meteorology; Radiance; Geography; Computer science; Astronomy; Geology; Telecommunications; Physics; Engineering; Aerospace engineering; Oceanography","score_opus":0.025349120542726967,"score_gpt":0.24536709918542968,"score_spread":0.2200179786427027,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2946185971","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9693557,0.0004682106,0.0010163868,0.0005432485,0.006244497,0.0009535087,0.0005022712,0.0002758383,0.020640342],"genre_scores_gemma":[0.9921753,0.0013180642,0.003194733,0.0005786751,0.0015017556,0.000020322184,0.0003247298,0.000058774214,0.0008276469],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9947573,0.00034179213,0.0011502998,0.0015153909,0.0011575047,0.0010777139],"domain_scores_gemma":[0.9956315,0.00090698875,0.0011740843,0.0012561982,0.00037714743,0.000654084],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0005747817,0.0009840576,0.0012301091,0.000021081018,0.0005123597,0.0004829027,0.00088537787,0.00043786375,0.00360298],"category_scores_gemma":[0.00014715742,0.00088667177,0.00025998734,0.00071488146,0.0005658513,0.00057064113,0.000053758133,0.0013275914,0.0017596934],"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":[0.003183862,0.00068132265,0.123312734,0.0006788959,0.0007233461,0.00008206838,0.0045795697,0.017030938,0.003943898,0.17140666,0.0025979942,0.67177874],"study_design_scores_gemma":[0.007729911,0.0036390766,0.5572284,0.0020160708,0.0005238702,0.000029356699,0.0032549787,0.36428332,0.002291541,0.028121775,0.026483793,0.0043979213],"about_ca_topic_score_codex":0.0070097614,"about_ca_topic_score_gemma":0.0011711667,"teacher_disagreement_score":0.6673808,"about_ca_system_score_codex":0.000067318215,"about_ca_system_score_gemma":0.0005185578,"threshold_uncertainty_score":0.9996027},"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}]}