{"meta":{"query_hash":"0857d9f7cb8e","filters":{"venue":"Dynamics of Atmospheres and Oceans"},"cohort_total":6,"direct_labels_cover":0,"predictions_cover":6,"exported":6,"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/0857d9f7cb8e","api":"https://metacan.xera.ac/api/v1/cohort?venue=Dynamics+of+Atmospheres+and+Oceans"},"results":[{"id":"W2001610109","doi":"10.1016/j.dynatmoce.2008.02.001","title":"The effect of bottom roughness in two-layer flows down a slope","year":2008,"lang":"en","type":"article","venue":"Dynamics of Atmospheres and Oceans","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":23,"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 Alberta","funders":"","keywords":"Surface finish; Entrainment (biomusicology); Stratified flows; Surface roughness; Materials science; Boundary layer; Mechanics; Flow (mathematics); Geology; Stratified flow; Scale (ratio); Hydraulic roughness; Geometry; Composite material; Turbulence; Mathematics; Physics; Acoustics","score_opus":0.004123341259977807,"score_gpt":0.21406753311432522,"score_spread":0.2099441918543474,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2001610109","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988796,0.00006950555,0.00033609167,0.0000736519,0.000024029228,0.0000026868925,0.000032338838,0.000024898623,0.0005571472],"genre_scores_gemma":[0.9996544,0.00003218347,0.0000717065,0.000011587518,0.00001054238,8.9321657e-7,0.000028306684,0.000007226741,0.0001833034],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997576,0.00006248428,0.000013222011,0.00003238687,0.000023025139,0.0001113396],"domain_scores_gemma":[0.99673456,0.0019838836,0.00023005936,0.00018475972,0.00032579777,0.00054095907],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046289997,0.00045332767,0.00052824465,0.0005109588,0.0007229852,0.0013192031,0.00030062353,0.0011649355,0.0015342619],"category_scores_gemma":[0.0037500297,0.00040560836,0.00077576016,0.0003374461,0.0010059011,0.00070450467,0.0005835927,0.0008378712,0.00019004349],"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":[0.0064619323,0.0011997262,0.27896947,0.00027127133,0.00059141556,0.0022880805,0.0011233981,0.5204932,0.15615106,0.004275036,0.0024613594,0.025714098],"study_design_scores_gemma":[0.00024882564,0.0006040994,0.48954302,0.000028413611,0.00027156592,0.00016062996,0.0006620229,0.50120336,0.0055003064,0.0012847418,0.0003625822,0.0001304767],"about_ca_topic_score_codex":0.016644595,"about_ca_topic_score_gemma":0.009365963,"teacher_disagreement_score":0.016644595,"about_ca_system_score_codex":0.00044211457,"about_ca_system_score_gemma":0.0004927689,"threshold_uncertainty_score":0.03309542},"labels":[],"label_agreement":null},{"id":"W2070041872","doi":"10.1016/j.dynatmoce.2005.12.001","title":"Model multi-cloud parameterizations for convectively coupled waves: Detailed nonlinear wave evolution","year":2006,"lang":"en","type":"article","venue":"Dynamics of Atmospheres and Oceans","topic":"Climate variability and models","field":"Environmental Science","cited_by":38,"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 Victoria","funders":"Office of Naval Research; Natural Sciences and Engineering Research Council of Canada","keywords":"Parametrization (atmospheric modeling); Baroclinity; Convection; Troposphere; Kelvin wave; Radiative cooling; Atmospheric sciences; Nonlinear system; Physics; Geology; Radiative transfer; Climatology; Geophysics; Meteorology","score_opus":0.01658297982617338,"score_gpt":0.22774911827411862,"score_spread":0.21116613844794524,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2070041872","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8081781,0.00063203246,0.1684431,0.001104217,0.0002587008,0.00014720828,0.004189141,0.0013839079,0.01566351],"genre_scores_gemma":[0.98179066,0.0002175428,0.014528069,0.00010007689,0.00005905342,0.000075732576,0.0011562125,0.000278397,0.0017940848],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998902,0.00002488999,0.00001061091,0.000022868979,0.000026223963,0.000025247133],"domain_scores_gemma":[0.99955267,0.00013150151,0.000071220515,0.00009162651,0.00009704399,0.00005592253],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036077347,0.00065893226,0.0006007038,0.00048994634,0.0008023867,0.0010459597,0.0019029315,0.0014469017,0.0022882551],"category_scores_gemma":[0.0015341566,0.0006602989,0.0006592344,0.0007312956,0.00044146812,0.0021751153,0.00082062976,0.001193721,0.00040079502],"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":[0.000020389924,0.00003119321,0.0011308583,0.000008458004,0.000021321028,0.000016950056,0.0000162665,0.99415094,0.00090364454,0.0018380008,0.00028339901,0.0015785608],"study_design_scores_gemma":[0.0000127979065,0.0000018918273,0.00021825777,9.701862e-7,0.0000036299587,0.0000024632463,0.0000027269919,0.99899703,0.00017108067,0.00047718847,0.00010776255,0.000004120054],"about_ca_topic_score_codex":0.039469168,"about_ca_topic_score_gemma":0.030713303,"teacher_disagreement_score":0.039469168,"about_ca_system_score_codex":0.0015237617,"about_ca_system_score_gemma":0.0013908155,"threshold_uncertainty_score":0.07847887},"labels":[],"label_agreement":null},{"id":"W2072057410","doi":"10.1016/s0377-0265(02)00052-0","title":"Steady-state frictional geostrophic circulation in a one-layer ocean model with thermodynamics","year":2002,"lang":"en","type":"article","venue":"Dynamics of Atmospheres and Oceans","topic":"Climate variability and models","field":"Environmental Science","cited_by":4,"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; Natural Sciences and Engineering Research Council of Canada","keywords":"Ocean gyre; Geostrophic wind; Adiabatic process; Thermodynamics; Mixing (physics); Steady state (chemistry); Mechanics; Enthalpy; Boundary layer; Temperature gradient; Physics; Materials science; Meteorology; Chemistry; Subtropics","score_opus":0.017183499961941035,"score_gpt":0.19977280374106518,"score_spread":0.18258930377912413,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2072057410","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93633056,0.0008645039,0.047276646,0.001697602,0.00021355935,0.000058156926,0.00094604946,0.00043308095,0.012179874],"genre_scores_gemma":[0.99509287,0.00020434066,0.0018342133,0.000071388,0.000059329326,0.000031071595,0.00016485178,0.00008775458,0.0024541854],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99984586,0.00005790814,0.000014672418,0.000029562007,0.000021246931,0.000030808766],"domain_scores_gemma":[0.99950314,0.0002178207,0.000084749736,0.00005227248,0.00006135882,0.00008068371],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040873667,0.00059791945,0.0009214253,0.0004272081,0.000832814,0.001333591,0.0012844965,0.0016654657,0.0015306459],"category_scores_gemma":[0.0029275294,0.0009593597,0.0008183051,0.0005662312,0.0017129985,0.0025820804,0.001332737,0.0011962081,0.00023547527],"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":[0.00006984611,0.000028717921,0.0012014124,0.000023864504,0.000028306982,0.00006059556,0.00003942645,0.990189,0.00064151175,0.006695511,0.00023051865,0.0007913382],"study_design_scores_gemma":[0.00002954565,0.0000119388205,0.00042736522,0.0000025718407,0.000011833581,0.0000042459947,0.000008097408,0.9977101,0.00008024343,0.0016180066,0.00008745643,0.000008556369],"about_ca_topic_score_codex":0.0416254,"about_ca_topic_score_gemma":0.018354945,"teacher_disagreement_score":0.0416254,"about_ca_system_score_codex":0.0013192125,"about_ca_system_score_gemma":0.0014253238,"threshold_uncertainty_score":0.082766235},"labels":[],"label_agreement":null},{"id":"W2095779529","doi":"10.1016/j.dynatmoce.2013.02.002","title":"A diapycnal diffusivity model for stratified environmental flows","year":2013,"lang":"en","type":"article","venue":"Dynamics of Atmospheres and Oceans","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":168,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; Natural Sciences and Engineering Research Council of Canada; Water Research Foundation","keywords":"Buoyancy; Turbulence; Thermal diffusivity; Turbulence kinetic energy; Prandtl number; Turbulent diffusion; Mechanics; Turbulence modeling; Stratified flows; Physics; Thermodynamics; Stratified flow; Environmental science; Convection","score_opus":0.00595897065387898,"score_gpt":0.17668634773134928,"score_spread":0.1707273770774703,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2095779529","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.233165,0.0012693269,0.73366857,0.0016141199,0.00042277845,0.00015220081,0.002849459,0.0010519328,0.025806567],"genre_scores_gemma":[0.91570544,0.0007059794,0.06639207,0.000203919,0.00014598541,0.00022256,0.001069702,0.00028247994,0.015271868],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992216,0.000024712208,0.0000066294983,0.00001766951,0.000014947773,0.000013837699],"domain_scores_gemma":[0.99982774,0.000057472895,0.000019986217,0.000023211143,0.000040012423,0.00003150171],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002480328,0.00043738465,0.00061489403,0.0003140467,0.0005276021,0.000834611,0.0010104986,0.0011982368,0.0020595097],"category_scores_gemma":[0.0010390042,0.00047032244,0.0005046692,0.00044285844,0.00048405296,0.0010652123,0.0008640972,0.000864371,0.00049461715],"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":[0.000028994964,0.000022871462,0.00064281776,0.000017681888,0.00001670772,0.00004368912,0.000026226013,0.9660429,0.0018175822,0.027214803,0.00080752035,0.003318328],"study_design_scores_gemma":[0.00000784615,0.0000025313689,0.000059501814,0.0000013416922,0.000002144795,0.000003111939,0.000001581405,0.99768996,0.00007672838,0.001685912,0.00046624962,0.000003107615],"about_ca_topic_score_codex":0.023497298,"about_ca_topic_score_gemma":0.010679738,"teacher_disagreement_score":0.023497298,"about_ca_system_score_codex":0.0008310141,"about_ca_system_score_gemma":0.0014506093,"threshold_uncertainty_score":0.04672104},"labels":[],"label_agreement":null},{"id":"W2903569684","doi":"10.1016/j.dynatmoce.2018.12.002","title":"Influence of tropical-extratropical interactions on the dynamics of extreme rainfall event: A case study from Indian region","year":2018,"lang":"en","type":"article","venue":"Dynamics of Atmospheres and Oceans","topic":"Climate variability and models","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":"Institut National de la Recherche Scientifique","funders":"","keywords":"Climatology; Extratropical cyclone; Environmental science; Atmospheric sciences; Middle latitudes; Special sensor microwave/imager; Forcing (mathematics); Instability; Anomaly (physics); Geology; Physics","score_opus":0.018046245572584156,"score_gpt":0.248517665923707,"score_spread":0.23047142035112284,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2903569684","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99781716,0.00007049234,0.000107070555,0.00015517641,0.0000040436375,0.0000033185029,0.00012372852,0.000008268403,0.0017106726],"genre_scores_gemma":[0.999668,0.000072687995,0.000046447654,0.000008031556,0.0000033789602,0.0000011797706,0.00004630489,0.0000020382274,0.00015202783],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99978966,0.000074156254,0.000011657524,0.000023137989,0.000019601632,0.000081879974],"domain_scores_gemma":[0.9993222,0.0003309999,0.000111560905,0.00004131452,0.00007058351,0.00012351612],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031872647,0.00015711879,0.00019873446,0.00037729248,0.00066394726,0.0010582014,0.00059005065,0.0004918294,0.0015502528],"category_scores_gemma":[0.0009732994,0.00013890235,0.00047078356,0.00089524407,0.00046657777,0.0004576864,0.00075031753,0.00053328706,0.000099033285],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003375489,0.00028595974,0.89314735,0.00010136486,0.00027216898,0.00987463,0.002652884,0.072398104,0.004826756,0.0037540004,0.0017818918,0.010567439],"study_design_scores_gemma":[0.000024477687,0.00012385863,0.89456815,0.000035137447,0.00022201877,0.0011081708,0.012478134,0.08648601,0.001134815,0.0009897986,0.0027821139,0.000047239966],"about_ca_topic_score_codex":0.078888334,"about_ca_topic_score_gemma":0.08804986,"teacher_disagreement_score":0.078888334,"about_ca_system_score_codex":0.0008962738,"about_ca_system_score_gemma":0.00068366004,"threshold_uncertainty_score":0.15685827},"labels":[],"label_agreement":null},{"id":"W4414032757","doi":"10.1016/j.dynatmoce.2025.101597","title":"Compounded influence of extreme coastal water level and subsidence on coastal flooding from satellite showcased at Saint-Louis (Senegal, West Africa)","year":2025,"lang":"en","type":"article","venue":"Dynamics of Atmospheres and Oceans","topic":"Flood Risk Assessment and Management","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 du Québec à Rimouski","funders":"","keywords":"SAINT; Flooding (psychology); Oceanography; Satellite; Subsidence; Coastal flood; Geology; Climatology; Geography; Sea level rise; Climate change; Geomorphology; History","score_opus":0.014499879516279103,"score_gpt":0.2165871266774934,"score_spread":0.20208724716121432,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414032757","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994553,0.000015001888,0.000021402717,0.000011428169,3.9054171e-7,0.0000011351596,0.0002240855,0.0000034296017,0.0002679756],"genre_scores_gemma":[0.9993455,0.000026877833,0.000059105667,0.000003654916,6.252221e-7,0.0000017792045,0.00036704302,0.000001314691,0.00019415945],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999453,0.00001459263,0.0000030855244,0.000011305167,0.000009550423,0.00001621987],"domain_scores_gemma":[0.9998412,0.000034720062,0.000051023948,0.000012405797,0.00003909792,0.000021584017],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011419347,0.00015920446,0.000094775525,0.00049021747,0.00018240696,0.00037772412,0.000095608,0.0001228448,0.00067246624],"category_scores_gemma":[0.00036383834,0.00007105625,0.00011918395,0.0007850552,0.00020903311,0.00014205615,0.00025142735,0.00010744174,0.000081133265],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012601147,0.000020062784,0.97797763,0.000039541002,0.00006976656,0.0005927528,0.0005359168,0.0032841584,0.00776115,0.000085784144,0.0003292434,0.009177926],"study_design_scores_gemma":[0.0000013284179,0.000013323185,0.99796873,0.0000046010205,0.000008120127,0.000041665124,0.00033878046,0.0009368643,0.00032793885,0.000009157589,0.0003460232,0.0000033825258],"about_ca_topic_score_codex":0.15924637,"about_ca_topic_score_gemma":0.34171045,"teacher_disagreement_score":0.15924637,"about_ca_system_score_codex":0.0005057416,"about_ca_system_score_gemma":0.00032214492,"threshold_uncertainty_score":0.31663895},"labels":[],"label_agreement":null}]}