{"meta":{"page":1,"per_page":50,"max_per_page":100,"total":70,"total_is_capped":false,"direct_labels_cover":0,"predictions_cover":70,"direct_label_status":"direct model label, unvalidated","prediction_status":"machine_predicted_unvalidated (Codex and Gemma teacher distillation)","score_status":"score_only:v0-immature-baseline (scores rank; they never assert a category)","snapshot":{"source":"OpenAlex, pinned release, all 482 partitions","release":"2026-06-24","frame_built":"2026-07-12"},"query_hash":"c5a02dd169c0","filters":{"venue":"Ocean Dynamics"}},"results":[{"id":"W1969504640","doi":"10.1007/s10236-007-0104-7","title":"Recent changes of the thermohaline circulation in the subpolar North Atlantic","year":2007,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":150,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Bedford Institute of Oceanography","funders":"Bundesministerium für Bildung und Forschung","keywords":"Ocean gyre; Thermohaline circulation; Isopycnal; Geology; Oceanography; North Atlantic Deep Water; Hydrography; Westerlies; Halocline; Climatology; Water mass; North Atlantic oscillation; Salinity; Subtropics","retraction":null,"screen_n_in":null,"score":{"opus":0.008776947174695765,"gpt":0.1918613306845646,"spread":0.1830843835098688,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004594683,0.00008022205,0.00008690656,0.00001688865,0.00008388257,0.00001443273,0.0003043541,0.00003765615,0.00005617336],"category_scores_gemma":[0.00003284598,0.00004181933,0.00003185463,0.0007304818,0.00008669301,0.00004938387,0.000007870441,0.000111758,0.000002407339],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000004259233,"about_ca_system_score_gemma":0.00002320184,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0005258808,"about_ca_topic_score_gemma":0.06535298,"domain_scores_codex":[0.9992874,0.00004589749,0.0001524193,0.0001078972,0.0002237905,0.000182584],"domain_scores_gemma":[0.9995658,0.000103902,0.00009779805,0.0001783871,0.00003189396,0.00002218363],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.000008900806,0.00001376207,0.9718699,0.00001337581,0.000004137004,0.000002429567,0.0002744287,0.00103596,8.588537e-7,0.00009164914,0.00001529901,0.02666927],"study_design_scores_gemma":[0.0000805836,0.00002262788,0.9711046,0.00001248044,0.000008811926,0.000006009679,0.0003731417,0.0273673,0.000003252729,0.0003229403,0.0006395662,0.00005868004],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9970291,0.0005905492,0.0001509524,0.0007165853,0.00012277,0.0001267674,0.0000163028,0.00001056158,0.001236407],"genre_scores_gemma":[0.9990394,0.0004951292,0.00005820268,0.0002752708,0.00004495225,5.89164e-8,0.00006671693,0.000002468342,0.00001780977],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.06482711,"threshold_uncertainty_score":0.9517019,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W299769615","doi":"10.1007/s10236-013-0679-0","title":"Seasonal variation of the M 2 tide","year":2014,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":141,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Fisheries and Oceans Canada; University of Victoria","funders":"Deutsche Forschungsgemeinschaft; Rijkswaterstaat; Deutsches Klimarechenzentrum","keywords":"Barotropic fluid; Tide gauge; Stratification (seeds); Geology; Internal tide; Oceanography; Sea-surface height; Altimeter; Climatology; Baroclinity; Tidal power; Seasonality; Sea level; Amplitude; Sea surface temperature; Internal wave; Geodesy","retraction":null,"screen_n_in":null,"score":{"opus":0.003075330063664171,"gpt":0.160274440687509,"spread":0.1571991106238448,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001386542,0.00005500724,0.00006703119,0.000005287871,0.00007551487,0.00001303147,0.0001850831,0.00002961899,0.0001677002],"category_scores_gemma":[0.00005275162,0.00003487068,0.0000400691,0.0002169976,0.00006461344,0.00006809935,0.000007837019,0.00005637394,0.00001009242],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001682786,"about_ca_system_score_gemma":0.00002780272,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0001589055,"about_ca_topic_score_gemma":0.0003906912,"domain_scores_codex":[0.9995338,0.00003008135,0.00009451865,0.00008657367,0.000153096,0.0001018926],"domain_scores_gemma":[0.9996807,0.00006521295,0.00007384216,0.000121066,0.00002862834,0.00003057863],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.000004539978,0.000006462918,0.9716371,0.00001588404,0.000006432825,1.106938e-7,0.00004466632,0.002993378,0.000001101783,0.003098804,0.0001743306,0.02201717],"study_design_scores_gemma":[0.00004984611,0.00001676615,0.6247797,0.00000654599,0.00000661585,0.000001419317,0.00001841146,0.3707585,0.000003850502,0.003678623,0.0006416476,0.00003806481],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9789245,0.00005780991,0.004637451,0.0002855183,0.0002410955,0.00004495964,0.00004094831,0.00002238814,0.0157454],"genre_scores_gemma":[0.9984812,0.00001197639,0.0009692652,0.0001459937,0.00004637787,2.492871e-8,0.00002812002,0.0000016925,0.0003153393],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3677651,"threshold_uncertainty_score":0.18362,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2054638621","doi":"10.1007/s10236-011-0481-9","title":"Far-field effects of tidal energy extraction in the Minas Passage on tidal circulation in the Bay of Fundy and Gulf of Maine using a nested-grid coastal circulation model","year":2011,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":88,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada; Dalhousie University","funders":"","keywords":"Bay; Tidal power; Geology; Water column; Oceanography; Ocean current; Tidal Model; Environmental science; Marine engineering","retraction":null,"screen_n_in":null,"score":{"opus":0.01370577789061334,"gpt":0.206269944250899,"spread":0.1925641663602856,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003110363,0.00009657601,0.000144515,0.00005192451,0.00003864442,0.000009105213,0.0001187344,0.00007388037,0.000006481041],"category_scores_gemma":[0.00003876645,0.00006527553,0.00003479075,0.0003595024,0.00007137486,0.0001605272,0.000006263192,0.00009561643,7.814367e-8],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000003942155,"about_ca_system_score_gemma":0.00003026609,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001350352,"about_ca_topic_score_gemma":0.004856478,"domain_scores_codex":[0.9991873,0.0001009217,0.0002493378,0.0001283049,0.0002147657,0.0001193681],"domain_scores_gemma":[0.9993742,0.0002648843,0.0001893637,0.0001257809,0.0000293073,0.0000164238],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.00009255365,0.0001123891,0.9031446,0.000142562,0.000008548861,0.000006169458,0.001653405,0.08844184,0.0001761988,0.001213587,0.000001931295,0.005006213],"study_design_scores_gemma":[0.0001555477,0.0001103646,0.4562029,0.00003935079,0.00001306678,0.000006911125,0.0004993454,0.54177,0.00005895059,0.001098695,5.967877e-7,0.00004426612],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9876843,0.00008861544,0.01142941,0.00001991133,0.00005157171,0.000123415,0.000018447,0.000003833989,0.0005804636],"genre_scores_gemma":[0.9994882,0.00004005838,0.000363662,0.00004353743,0.00001569092,2.690788e-7,0.00004254876,0.000003056761,0.000003013567],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.4533282,"threshold_uncertainty_score":0.2710029,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2073507950","doi":"10.1007/s10236-011-0420-9","title":"Simulation and detection of tsunami signatures in ocean surface currents measured by HF radar","year":2011,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Radar Systems and Signal Processing","field":"Engineering","cited_by":86,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Radar; Geology; Remote sensing; Current (fluid); Ocean current; Backscatter (email); Oceanography; Computer science; Telecommunications","retraction":null,"screen_n_in":null,"score":{"opus":0.01159973527138565,"gpt":0.209717040619348,"spread":0.1981173053479623,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001717524,0.0001264704,0.0001683643,0.00005628722,0.00003192376,0.00001527745,0.00006668203,0.0001085709,0.000002642105],"category_scores_gemma":[0.00002405622,0.0001315211,0.0000240313,0.0001497521,0.00002260061,0.0001659425,0.00001072728,0.0001455699,4.287272e-7],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00007479893,"about_ca_system_score_gemma":0.000006897167,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00006262706,"about_ca_topic_score_gemma":0.00005631192,"domain_scores_codex":[0.999311,0.00002819883,0.000243553,0.0001324635,0.0001432755,0.0001414837],"domain_scores_gemma":[0.9997329,0.00003269253,0.00005917639,0.00009516153,0.000039239,0.00004081491],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.00003273942,0.00004143766,0.01402212,0.000377456,0.00003050252,0.000002780523,0.001094268,0.9704581,0.006860812,0.00005047588,0.00005942101,0.006969847],"study_design_scores_gemma":[0.0002434742,0.00002394381,0.001835334,0.00007620411,0.000008293443,7.132523e-7,0.0001001227,0.9955051,0.001875259,0.0001669151,0.00002808121,0.0001365832],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9734473,0.001339109,0.02441109,0.000001383633,0.0001788907,0.0001101068,0.00001643536,0.00007563659,0.0004200676],"genre_scores_gemma":[0.9996746,0.00002196645,0.0002254445,0.000001994418,0.00001205175,9.964594e-8,0.000009021847,0.00002838009,0.00002642027],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.02622734,"threshold_uncertainty_score":0.5363274,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3021470873","doi":"10.1007/s10236-020-01378-0","title":"The hydrodynamic foundation for salmon lice dispersion modeling along the Norwegian coast","year":2020,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Parasite Biology and Host Interactions","field":"Environmental Science","cited_by":83,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"Norges Forskningsråd; Havforskningsinstituttet","keywords":"Fjord; Norwegian; Aquaculture; Current (fluid); Oceanography; Fishery; Water column; Plankton; Environmental science; Geography; Geology; Fish <Actinopterygii>","retraction":null,"screen_n_in":null,"score":{"opus":0.01407299157861511,"gpt":0.2772862634969793,"spread":0.2632132719183642,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001513327,0.00009505621,0.00006387327,0.000006515809,0.0008666774,0.00005100504,0.0002821806,0.00005230466,0.00005540295],"category_scores_gemma":[0.00006469148,0.00005876457,0.00006603061,0.0000972155,0.0001173187,0.0001489032,0.00009618886,0.0001509734,0.0002197002],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000143738,"about_ca_system_score_gemma":0.000007735971,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0001376897,"about_ca_topic_score_gemma":0.002465503,"domain_scores_codex":[0.999342,0.00003942634,0.0001414013,0.0001991092,0.0000923652,0.0001857089],"domain_scores_gemma":[0.9995464,0.0001593423,0.00006296301,0.0001696582,0.000008914423,0.00005268564],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.0005579003,0.0001461381,0.1886311,0.00002271854,0.0001167979,0.000003778731,0.003953103,0.6795539,0.003824748,0.008304624,0.004082428,0.1108028],"study_design_scores_gemma":[0.00009876033,0.00004578619,0.007498513,0.000003728419,0.00001828056,0.00000396918,0.0004340559,0.9858304,0.000006612975,0.0002374352,0.005740564,0.00008185544],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9386253,0.00001062511,0.05152175,0.007372425,0.0002261691,0.0002680405,0.00002030457,0.00003234948,0.001923031],"genre_scores_gemma":[0.9983925,0.00004359741,0.0001959014,0.0005542202,0.00007142626,0.000006581291,0.00009067793,0.00001176386,0.0006333154],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3062766,"threshold_uncertainty_score":0.6665869,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2013434969","doi":"10.1007/s10236-011-0478-4","title":"Mapping bathymetry using X-band marine radar data recorded from a moving vessel","year":2011,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Underwater Acoustics Research","field":"Earth and Planetary Sciences","cited_by":71,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Defence Research and Development Canada","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Bathymetry; Radar; Geology; Remote sensing; Radar imaging; Context (archaeology); Hydrography; Shore; Echo sounding; Geodesy; Meteorology; Marine engineering; Oceanography; Geography; Computer science; Telecommunications; Engineering","retraction":null,"screen_n_in":null,"score":{"opus":0.07332478085503902,"gpt":0.2521874936700876,"spread":0.1788627128150486,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004268832,0.0001778805,0.000205008,0.0001866089,0.000201708,0.0001326902,0.0009801001,0.00009621222,0.002243669],"category_scores_gemma":[0.0000922999,0.0001677699,0.00003085065,0.0003465304,0.00009589057,0.0004390646,0.0002148731,0.0003036087,0.00008116994],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00002923327,"about_ca_system_score_gemma":0.0001108317,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.02182958,"about_ca_topic_score_gemma":0.005245956,"domain_scores_codex":[0.9983144,0.00008137711,0.0002672777,0.0005028462,0.0003520524,0.0004820576],"domain_scores_gemma":[0.9987224,0.0001582211,0.00008495136,0.0008061659,0.00004751326,0.0001806943],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.00006753515,0.00004036992,0.9519602,0.00004560103,0.00008986284,0.0001461503,0.0005579917,0.001712617,0.0002594557,0.000006401745,0.0003265325,0.0447873],"study_design_scores_gemma":[0.0002200255,0.00002738644,0.06887275,0.00002460934,0.00001794682,0.00001369542,0.0003688721,0.9282466,0.00005036228,0.001739124,0.0002027426,0.0002158517],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.8891068,0.00008412945,0.09780409,0.00003192091,0.0003791369,0.0001523963,0.001058669,0.00007605848,0.01130688],"genre_scores_gemma":[0.8870327,0.00007439197,0.1099861,0.0000612262,0.0001405153,6.318185e-8,0.002403363,0.0000154547,0.0002861083],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.926534,"threshold_uncertainty_score":0.9986684,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1570511445","doi":"10.1007/s10236-001-8175-3","title":"A simple model of seasonal open ocean convection Part II: Labrador Sea stability and stochastic forcing","year":2001,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"Universität Potsdam","keywords":"Forcing (mathematics); Climatology; Convection; Geology; Sea surface temperature; Climate model; Mixed layer; Atmospheric sciences; Climate change; Meteorology; Oceanography; Physics","retraction":null,"screen_n_in":null,"score":{"opus":0.0169079548690231,"gpt":0.2179729493526138,"spread":0.2010649944835907,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003136813,0.000161023,0.0002438466,0.00001885324,0.000288328,0.00007190463,0.0002579314,0.00006886227,0.0002822495],"category_scores_gemma":[0.00005574453,0.0001434748,0.00004355626,0.0003184376,0.0001724011,0.0004474639,0.00007016992,0.0001237132,0.000001633929],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000009623845,"about_ca_system_score_gemma":0.0001165205,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0008578388,"about_ca_topic_score_gemma":0.002530928,"domain_scores_codex":[0.9989054,0.00003287768,0.0002481393,0.0003156032,0.0002087519,0.0002892872],"domain_scores_gemma":[0.999365,0.00009514292,0.0001290903,0.0001776896,0.00007980095,0.0001532238],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.0001232871,0.00005160408,0.9409359,0.00007383579,0.00002549916,0.000002348184,0.0002796484,0.04869658,0.000001594495,0.0003400767,0.000184874,0.009284775],"study_design_scores_gemma":[0.0003462545,0.0001567556,0.0331278,0.00002281131,0.00002743084,0.00001244736,0.0005793384,0.9608054,0.000006319174,0.004686162,0.00005968986,0.0001696453],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9881862,0.0001439386,0.009763908,0.0001027939,0.0000721871,0.0002329175,0.000338085,0.00004271981,0.00111728],"genre_scores_gemma":[0.9985048,0.0000750963,0.0008817302,0.00009632517,0.00003226317,2.49689e-7,0.0002144654,0.000006765807,0.0001882809],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.9121088,"threshold_uncertainty_score":0.5850732,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2075377626","doi":"10.1007/s10236-009-0222-5","title":"Using the Regional Ocean Modeling System (ROMS) to improve the ocean circulation from a GCM 20th century simulation","year":2009,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Memorial University of Newfoundland","funders":"Lawrence Livermore National Laboratory; Norges Forskningsråd","keywords":"Climatology; Hydrography; Climate model; Environmental science; Forcing (mathematics); GCM transcription factors; Ocean current; Sea ice; General Circulation Model; Ocean heat content; Arctic; Thermohaline circulation; Climate change; Oceanography; Geology","retraction":null,"screen_n_in":null,"score":{"opus":0.02005465758281506,"gpt":0.2299942402715313,"spread":0.2099395826887163,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004398667,0.0002522844,0.0002050736,0.00006733438,0.0007961395,0.0001734751,0.0004432438,0.0001171375,0.00002793239],"category_scores_gemma":[0.00004903149,0.0001621591,0.0001219235,0.0003046572,0.00005502045,0.0002796874,0.00002721983,0.0002989649,0.00002068769],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000108594,"about_ca_system_score_gemma":0.00008542073,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001418684,"about_ca_topic_score_gemma":0.0002374325,"domain_scores_codex":[0.9981579,0.0001115115,0.0003973393,0.0004064096,0.0005059749,0.0004208297],"domain_scores_gemma":[0.9988537,0.0002490684,0.0001818946,0.0004669218,0.0001097284,0.0001386467],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.00004693931,0.00001090631,0.02094839,0.000008852204,0.00002257279,0.000004346637,0.0007957596,0.9720333,0.000005097765,0.001235239,0.00002782264,0.004860728],"study_design_scores_gemma":[0.0001788079,0.00004536776,0.0124478,0.0000585155,0.00007076256,0.00001563894,0.003005972,0.9819118,2.729337e-7,0.001967171,0.00007089818,0.0002270012],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.8559199,0.00006866995,0.1415392,0.0009884353,0.000456565,0.000421079,0.0001660084,0.00008811904,0.0003520799],"genre_scores_gemma":[0.9967156,0.00001826476,0.001198865,0.001102323,0.0004316081,8.809442e-8,0.0004885832,0.00001256991,0.00003211001],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1407957,"threshold_uncertainty_score":0.6612657,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2083489669","doi":"10.1007/s10236-003-0074-3","title":"A two-way nested-grid ocean-circulation model for the Meso-American Barrier Reef System","year":2004,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; National Oceanic and Atmospheric Administration","keywords":"Nested set model; Geology; Wind stress; Ocean current; Ocean general circulation model; Climatology; Sea surface temperature; Meteorology; Flux (metallurgy); Elevation (ballistics); Atmospheric sciences; General Circulation Model; Oceanography; Geometry; Geography; Climate change; Mathematics","retraction":null,"screen_n_in":null,"score":{"opus":0.008034683295871812,"gpt":0.2039681438126777,"spread":0.1959334605168059,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003158702,0.0002430814,0.0002529185,0.00003048374,0.0005029005,0.0001242035,0.0004120875,0.00006568876,0.00001581185],"category_scores_gemma":[0.00004879041,0.0001683757,0.0001476338,0.0005720448,0.000228763,0.0002672304,0.00001522936,0.0001554121,0.0000152036],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00003682733,"about_ca_system_score_gemma":0.0001649544,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0007478772,"about_ca_topic_score_gemma":0.001510222,"domain_scores_codex":[0.9985355,0.00002891058,0.0003080536,0.0003704995,0.0003162005,0.000440804],"domain_scores_gemma":[0.9990063,0.0001807745,0.0002018296,0.0003491678,0.0001068429,0.0001550346],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.00004351036,0.00001492042,0.1537471,0.00007830875,0.00004717048,0.000004720896,0.0002800164,0.8344656,7.135005e-7,0.003834129,0.000171344,0.007312425],"study_design_scores_gemma":[0.0004530115,0.00007012711,0.02571176,0.0000382222,0.00007231899,0.00002617367,0.001528656,0.9701011,0.00000200587,0.001565466,0.0001860398,0.0002450928],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.7571668,0.0008676904,0.2364438,0.0007934254,0.0006634603,0.0007516977,0.000499311,0.0003345367,0.002479243],"genre_scores_gemma":[0.9933994,0.000071961,0.005570069,0.0003294896,0.0002186281,0.00000137843,0.0002039859,0.00001678902,0.0001883457],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2362325,"threshold_uncertainty_score":0.6866164,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2096597498","doi":"10.1007/s10236-011-0398-3","title":"Simulating the three-dimensional circulation and hydrography of Halifax Harbour using a multi-nested coastal ocean circulation model","year":2011,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":true},"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada; Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Hydrography; Oceanography; Climatology; Geology; Environmental science; Harbour; Buoyancy","retraction":null,"screen_n_in":null,"score":{"opus":0.03137209070705558,"gpt":0.2151265184220358,"spread":0.1837544277149802,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002526416,0.0001809321,0.0001853825,0.00005036315,0.0002980918,0.00003569115,0.0001414504,0.00008973387,0.000027143],"category_scores_gemma":[0.0000314161,0.0001388896,0.0000817125,0.0004450199,0.00023181,0.0003065956,0.00002351235,0.0001285456,7.792946e-7],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000004286459,"about_ca_system_score_gemma":0.00005828948,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001413737,"about_ca_topic_score_gemma":0.001761828,"domain_scores_codex":[0.9988629,0.00004158987,0.0003198792,0.0002627078,0.0002720414,0.000240914],"domain_scores_gemma":[0.9993097,0.00008529359,0.000247187,0.0001713804,0.0001034921,0.00008292431],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.00001549289,0.00002019228,0.669853,0.00002154685,0.00002176934,0.000001511826,0.0002199048,0.3280007,0.00001002305,0.00009995977,6.343643e-7,0.001735208],"study_design_scores_gemma":[0.0001884408,0.00001820454,0.3691527,0.00002684088,0.00003432018,0.000008529466,0.0001075451,0.6289511,0.00000290708,0.001399697,2.783047e-7,0.0001093391],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9644077,0.0001935682,0.0348624,0.00001524419,0.00006553557,0.0001801164,0.0000881227,0.00004748753,0.0001398741],"genre_scores_gemma":[0.9838591,0.000007173208,0.01593921,0.00004641573,0.00002142819,8.187207e-8,0.000112817,0.000009954605,0.000003869808],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3009504,"threshold_uncertainty_score":0.5663754,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2063541232","doi":"10.1007/s10236-009-0218-1","title":"Investigation of three-dimensional circulation and hydrography over the Pearl River Estuary of China using a nested-grid coastal circulation model","year":2009,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Dalhousie University","funders":"","keywords":"Hydrography; Estuary; Forcing (mathematics); Climatology; Typhoon; Oceanography; Geology; Downscaling; Ocean current; Monsoon; Environmental science; Climate change","retraction":null,"screen_n_in":null,"score":{"opus":0.01851709650835523,"gpt":0.2197623498612912,"spread":0.201245253352936,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001000606,0.00009072826,0.0001268402,0.00007687347,0.0001108041,0.00001854352,0.00008358975,0.00006448236,0.00001609111],"category_scores_gemma":[0.00001528918,0.00006434289,0.00005730302,0.0002676884,0.0002595726,0.0001963821,0.00001198956,0.0001235996,6.268164e-7],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000004998986,"about_ca_system_score_gemma":0.00003740068,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002639315,"about_ca_topic_score_gemma":0.001727298,"domain_scores_codex":[0.9990917,0.00004972621,0.0002133811,0.0001542677,0.000345354,0.0001456092],"domain_scores_gemma":[0.9996158,0.00005289894,0.00009552611,0.0001138215,0.00004959582,0.0000723613],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00002698524,0.000008323233,0.7776783,0.00001341901,0.000007012254,7.708352e-7,0.00007494143,0.2182528,0.000231887,0.0005235946,0.00000250352,0.003179395],"study_design_scores_gemma":[0.00008816826,0.0000376457,0.4984494,0.000009098142,0.000008693023,0.000003147324,0.00000473539,0.4935831,0.000002537663,0.007776903,1.754154e-7,0.00003640786],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9963705,0.00009475183,0.003101505,0.0001373676,0.00003235181,0.0001364648,0.00005923032,0.00001107621,0.00005673716],"genre_scores_gemma":[0.9984685,0.000007036094,0.001306749,0.00003338065,0.0000338041,6.660601e-8,0.0001464707,0.000002444593,0.000001514597],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.279229,"threshold_uncertainty_score":0.3989873,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2018088272","doi":"10.1007/s10236-005-0005-6","title":"A new two-way nesting technique for ocean modeling based on the smoothed semi-prognostic method","year":2005,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Dalhousie University","funders":"National Oceanic and Atmospheric Administration","keywords":"Nesting (process); Grid; Ocean current; Nested set model; Geology; Meteorology; Computer science; Oceanography; Geography; Geodesy; Data mining","retraction":null,"screen_n_in":null,"score":{"opus":0.01428036822156645,"gpt":0.2382479213221675,"spread":0.2239675531006011,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007984531,0.0002715494,0.00022799,0.00004353315,0.0003947925,0.0001179628,0.0004638227,0.00009873786,0.0001368099],"category_scores_gemma":[0.0003075002,0.0001871287,0.0001347331,0.0005147458,0.00004675149,0.0001608985,0.00001383062,0.0002571331,0.00001055431],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001488021,"about_ca_system_score_gemma":0.0001590557,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0002536315,"about_ca_topic_score_gemma":0.0004042332,"domain_scores_codex":[0.9984779,0.00007854185,0.0003024162,0.0003968105,0.0002666638,0.0004776612],"domain_scores_gemma":[0.9982589,0.001068903,0.0001301328,0.0003105125,0.00007094009,0.0001605914],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.0000548835,0.00002246223,0.03826118,0.00004286903,0.00001639515,0.000002905759,0.00007700755,0.9099095,0.00000620772,0.001365501,0.0004980379,0.04974304],"study_design_scores_gemma":[0.0003136809,0.0001221768,0.0003252125,0.00008765349,0.00004235888,0.000009449057,0.0001490665,0.9927191,0.00005620065,0.005468074,0.0004414477,0.0002655792],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"methods","genre_gemma":"empirical","genre_scores_codex":[0.0369344,0.0001762839,0.9572422,0.001826438,0.0001022717,0.0006479153,0.00006258839,0.0001930322,0.002814853],"genre_scores_gemma":[0.7523834,0.00001171039,0.2460951,0.001011569,0.0002139871,0.000001663542,0.00008260753,0.00001786495,0.0001820765],"genre_candidate":"methods","genre_consensus":null,"teacher_disagreement_score":0.715449,"threshold_uncertainty_score":0.7630886,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1993124042","doi":"10.1007/s10236-010-0286-2","title":"Internal solitary wave-induced flow over a corrugated bed","year":2010,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Waterloo","funders":"Engineering and Physical Sciences Research Council; Core Research for Evolutional Science and Technology; Natural Sciences and Engineering Research Council of Canada; University of Dundee","keywords":"Pycnocline; Geology; Amplitude; Vortex; Mechanics; Instability; Wavelength; Internal wave; Entrainment (biomusicology); Turbulence; Shear (geology); Boundary layer; Physics; Optics; Petrology; Acoustics; Oceanography","retraction":null,"screen_n_in":null,"score":{"opus":0.006085882383544419,"gpt":0.1915946310547801,"spread":0.1855087486712356,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001573406,0.0002073258,0.0001937588,0.00003276302,0.000161065,0.00008544374,0.0003104541,0.0001413334,0.002177391],"category_scores_gemma":[0.00005561591,0.0001727962,0.00009145214,0.0003275719,0.0001153686,0.0002747215,0.00002413856,0.0004613916,0.00009520186],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000004845364,"about_ca_system_score_gemma":0.00008036344,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001115643,"about_ca_topic_score_gemma":0.006155272,"domain_scores_codex":[0.9987798,0.00002295392,0.0002320268,0.0003095374,0.0002536109,0.0004020745],"domain_scores_gemma":[0.9993211,0.00007398566,0.00008396048,0.0002547408,0.00005648519,0.0002097285],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.00008296236,0.00005492456,0.9235697,0.00003490998,0.00005696368,0.0001018549,0.0002096512,0.0002857511,0.0001086189,0.0003266598,0.001908118,0.0732599],"study_design_scores_gemma":[0.0003395121,0.0001066628,0.2115224,0.00001668829,0.000020307,0.00006155035,0.0001268192,0.7849623,0.0000456902,0.001622438,0.0008929707,0.0002826836],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9883298,0.00006653173,0.0003907538,0.0001525253,0.001262344,0.0000961439,0.0001143847,0.0001430397,0.009444488],"genre_scores_gemma":[0.9952438,0.00003060456,0.003354913,0.0003784499,0.0002021304,1.625596e-7,0.0002936219,0.0000100212,0.0004862944],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.7846766,"threshold_uncertainty_score":0.9987348,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2995996947","doi":"10.1007/s10236-019-01334-7","title":"High-resolution modelling of a coastal harbour in the presence of strong tides and significant river runoff","year":2019,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":true},"ca_institutions":"Bedford Institute of Oceanography; Environment and Climate Change Canada; Fisheries and Oceans Canada","funders":"Fisheries and Oceans Canada; Environment and Climate Change Canada; Government of Canada","keywords":"Bay; Surface runoff; Context (archaeology); Harbour; Geology; Shore; Oceanography; Discharge; Estuary; Environmental science; Current (fluid); River mouth; Hydrology (agriculture); Sediment; Drainage basin; Geomorphology; Geography","retraction":null,"screen_n_in":null,"score":{"opus":0.00911454411263185,"gpt":0.1765141757389744,"spread":0.1673996316263426,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002186864,0.0000757751,0.000134905,0.00002039188,0.00002953777,0.0000132115,0.0001671943,0.00003452964,0.00002722053],"category_scores_gemma":[0.00001148693,0.00005243893,0.00002351959,0.000204985,0.0001622136,0.0001477681,0.00001193131,0.00008391382,0.000001309401],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001415707,"about_ca_system_score_gemma":0.00003105084,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002581466,"about_ca_topic_score_gemma":0.0007104786,"domain_scores_codex":[0.9993407,0.00003592407,0.0001718164,0.0001316164,0.000178851,0.0001410806],"domain_scores_gemma":[0.9996026,0.0001316011,0.0001008782,0.0001128043,0.00002862889,0.00002347997],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.0000298456,0.00001593103,0.7089491,0.00005851598,0.000006548499,0.000001372043,0.0003641231,0.2875793,0.000006057469,0.00163713,0.000007151672,0.001344833],"study_design_scores_gemma":[0.0001385037,0.00008183682,0.1611724,0.00003890503,0.000007190104,0.000001206342,0.0008614655,0.8364136,0.00001079507,0.001211486,0.000005482207,0.00005706314],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.994531,0.0002290932,0.004535975,0.00003407698,0.0000460867,0.0001149175,0.00009184017,0.00000585264,0.000411191],"genre_scores_gemma":[0.997588,0.0001471732,0.002178722,0.000009342063,0.000009062172,8.070593e-8,0.00002983343,0.000001999765,0.0000357766],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.5488343,"threshold_uncertainty_score":0.3902421,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2011342595","doi":"10.1007/s10236-013-0688-z","title":"Study on subtidal circulation and variability in the Gulf of St. Lawrence, Scotian Shelf, and Gulf of Maine using a nested-grid shelf circulation model","year":2014,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Hydrography; Oceanography; Forcing (mathematics); Climatology; Mesoscale meteorology; Ocean current; Estuary; Circulation (fluid dynamics); Estuarine water circulation; Outflow; Environmental science; Advection; Geology","retraction":null,"screen_n_in":null,"score":{"opus":0.0140350638992565,"gpt":0.2200038270873574,"spread":0.2059687631881009,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001154831,0.0001353625,0.0002247301,0.00004725411,0.000092593,0.00003363951,0.0001363681,0.00006524544,0.000008182015],"category_scores_gemma":[0.00009976833,0.0001021247,0.00002613365,0.0004238824,0.000194342,0.0001980091,0.0000146199,0.0001095566,1.610627e-7],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000006692389,"about_ca_system_score_gemma":0.00004048264,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0003954599,"about_ca_topic_score_gemma":0.001066394,"domain_scores_codex":[0.9987893,0.0001925464,0.000322169,0.0002644934,0.0002725659,0.0001589646],"domain_scores_gemma":[0.9992844,0.000234288,0.0001661353,0.0002148663,0.00005657874,0.00004370338],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.00002037884,0.00007442426,0.8372347,0.00005760493,0.000007288378,6.519434e-7,0.000793335,0.1596231,0.000005982082,0.0006245991,9.115385e-7,0.001557031],"study_design_scores_gemma":[0.0001821507,0.00008446968,0.4833882,0.0000186913,0.00001697845,0.000003008802,0.0005719919,0.5121483,5.504756e-7,0.003527545,3.800621e-7,0.00005763269],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9863619,0.00003153896,0.01282578,0.00004361267,0.00005507113,0.0002826799,0.00005634924,0.00001074526,0.0003322963],"genre_scores_gemma":[0.9989416,0.00001168748,0.0009329073,0.00003040874,0.00002419557,1.850177e-7,0.00005307325,0.000004040221,0.00000192579],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3538464,"threshold_uncertainty_score":0.4164526,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1711365732","doi":"10.1007/s10236-015-0878-y","title":"Statistical estimation of extreme ocean waves over the eastern Canadian shelf from 30-year numerical wave simulation","year":2015,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Ocean Waves and Remote Sensing","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":true},"ca_institutions":"Dalhousie University","funders":"Compute Canada; Natural Sciences and Engineering Research Council of Canada; Marine Environmental Observation Prediction and Response Network; Canon Foundation for Scientific Research","keywords":"Significant wave height; Geology; Climatology; Wind wave; Wave model; Buoy; Rogue wave; Wave height; Meteorology; Storm; Surface wave; Submarine pipeline; Oceanography; Environmental science; Geography; Nonlinear system","retraction":null,"screen_n_in":null,"score":{"opus":0.02386016698085649,"gpt":0.2225326128333398,"spread":0.1986724458524833,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001887624,0.0001433643,0.0001722882,0.00006550265,0.0001142302,0.00007598766,0.0001258602,0.00008814097,0.0002645217],"category_scores_gemma":[0.0001250107,0.0001017974,0.00004167673,0.0001370092,0.0001185513,0.000138594,0.00001259147,0.0001492668,0.00007017076],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00003996896,"about_ca_system_score_gemma":0.0001658644,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.08589704,"about_ca_topic_score_gemma":0.03015513,"domain_scores_codex":[0.9988304,0.00007658034,0.0002629961,0.0002128047,0.0003363247,0.0002808594],"domain_scores_gemma":[0.9990814,0.0002315614,0.0001007556,0.0002183987,0.00006451138,0.0003033191],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.00004528411,0.00001541896,0.2188569,0.00001116792,0.000034856,0.00003203363,0.0008904251,0.714147,2.811943e-7,0.0006605946,0.0005828885,0.06472319],"study_design_scores_gemma":[0.0001622589,0.00004741931,0.208093,0.00001349141,0.00002123006,0.0000031252,0.0003288905,0.7883952,4.454688e-7,0.002668424,0.0001585466,0.0001080124],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9790796,0.00003996394,0.0169938,0.0002083426,0.0003551939,0.0001356965,0.0006131909,0.00002379141,0.002550397],"genre_scores_gemma":[0.9944965,0.000003375204,0.004250983,0.0001111106,0.0001206457,1.535092e-9,0.0008983039,0.000009177877,0.0001099661],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.07424822,"threshold_uncertainty_score":0.987542,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3021647976","doi":"10.1007/s10236-020-01373-5","title":"Low-frequency sea level variability and impact of recent sea ice decline on the sea level trend in the Arctic Ocean from a high-resolution simulation","year":2020,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"National Natural Science Foundation of China","keywords":"Arctic sea ice decline; Arctic dipole anomaly; Sea ice; Canada Basin; Arctic; Arctic ice pack; Geology; Arctic geoengineering; Oceanography; Climatology; Arctic oscillation; Sea ice concentration; Sea ice thickness; Drift ice; The arctic","retraction":null,"screen_n_in":null,"score":{"opus":0.03764038986630774,"gpt":0.2516299094078938,"spread":0.213989519541586,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009648058,0.0002527958,0.0002783872,0.00005165986,0.0002070663,0.00006065291,0.0003880037,0.0001213744,0.0002963057],"category_scores_gemma":[0.0007082983,0.0001529056,0.00009942977,0.0004739491,0.0002031789,0.0001979935,0.00004169724,0.0004323567,0.000009006313],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00008244392,"about_ca_system_score_gemma":0.0001331759,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.01195674,"about_ca_topic_score_gemma":0.009064155,"domain_scores_codex":[0.9979615,0.0004255704,0.0004380772,0.0003960797,0.0004397168,0.0003390916],"domain_scores_gemma":[0.9972587,0.001952947,0.0002146765,0.0003672585,0.00007625058,0.0001301958],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.0001935491,0.00007917696,0.8358377,0.00003571316,0.0000404405,0.000006361336,0.001016708,0.1560345,0.000002649447,0.0004388079,0.00005539134,0.006258935],"study_design_scores_gemma":[0.0002597455,0.0001583977,0.4777564,0.00001981519,0.00002889588,0.000002130251,0.0002417317,0.5176569,7.462505e-7,0.003769065,0.000005870216,0.0001003202],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9849184,0.00001706906,0.005539399,0.004532714,0.00009012511,0.0003451292,0.004295863,0.00002229725,0.0002390513],"genre_scores_gemma":[0.9963127,0.00008302213,0.0006879271,0.0008680337,0.0001039126,3.533526e-7,0.001928679,0.000009503708,0.000005861906],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3616223,"threshold_uncertainty_score":0.9946227,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1971284799","doi":"10.1007/s10236-011-0490-8","title":"Observed impact of mesoscale circulation on oceanic response to Typhoon Man-Yi (2007)","year":2011,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Manitoba; Geological Survey of Canada","funders":"Canadian Space Agency; Natural Sciences and Engineering Research Council of Canada; Korea Meteorological Administration","keywords":"Mesoscale meteorology; Typhoon; Geology; Anticyclone; Climatology; Shoaling and schooling; Entrainment (biomusicology); Oceanography","retraction":null,"screen_n_in":null,"score":{"opus":0.04457006773084751,"gpt":0.2570105861077883,"spread":0.2124405183769408,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000206015,0.0001405004,0.0001884057,0.0001150621,0.0000710858,0.00001583002,0.0002693654,0.0000935394,0.002198749],"category_scores_gemma":[0.0001405913,0.0001047792,0.0001317553,0.0003267936,0.00005952988,0.00009678018,0.00001877951,0.0001705908,0.000410306],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00003808493,"about_ca_system_score_gemma":0.00005909304,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002429553,"about_ca_topic_score_gemma":0.001088727,"domain_scores_codex":[0.9986741,0.0001453594,0.0002353043,0.0002554324,0.0003239136,0.0003659242],"domain_scores_gemma":[0.9991601,0.0001446236,0.00005119648,0.0002899193,0.00006339183,0.0002907483],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.002346827,0.00006466133,0.9882188,0.00001287515,0.00002140188,0.00001772225,0.0001113925,0.001703983,0.00009633144,0.0001978854,0.0003695378,0.006838557],"study_design_scores_gemma":[0.0002156155,0.001082937,0.9711776,0.00001320401,0.000006539116,0.000003688395,0.00002677584,0.02639106,0.00003788379,0.000834008,0.00008507799,0.0001255539],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9961379,0.00003469927,0.000268501,0.00009172724,0.0001162324,0.0001719356,0.0001297493,0.00003536455,0.003013876],"genre_scores_gemma":[0.9989823,0.00001226997,0.0005571076,0.0000762,0.00004373023,2.321791e-7,0.00007627093,0.000006721667,0.0002451462],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.02468708,"threshold_uncertainty_score":0.9987134,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2794168182","doi":"10.1007/s10236-018-1139-7","title":"Tsunami detection by high-frequency radar in British Columbia: performance assessment of the time-correlation algorithm for synthetic and real events","year":2018,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"Ocean Networks Canada Society","funders":"","keywords":"Radar; Geology; Algorithm; Seismology; SIGNAL (programming language); Subduction; Geodesy; Computer science; Meteorology; Telecommunications; Physics","retraction":null,"screen_n_in":null,"score":{"opus":0.003190085249460276,"gpt":0.1868743401378362,"spread":0.1836842548883759,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002314233,0.00006117578,0.0001224871,0.00001986076,0.0002143899,0.00003013743,0.00008598906,0.00005563623,0.00005326893],"category_scores_gemma":[0.00001882388,0.00006810929,0.00002597287,0.0001269796,0.0001113014,0.0001070401,0.000011773,0.00007639085,0.000002172954],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001969029,"about_ca_system_score_gemma":0.00002584292,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.0227494,"about_ca_topic_score_gemma":0.1969675,"domain_scores_codex":[0.9993258,0.00003928491,0.0001768536,0.0001648817,0.0001373755,0.0001558723],"domain_scores_gemma":[0.9996595,0.00007779281,0.00009472017,0.0001029047,0.00004243289,0.0000226794],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00000169944,0.000009585501,0.7292201,0.00001099989,0.000008181543,2.012068e-7,0.00001877794,0.00002039474,0.000005787074,0.000002167751,0.00002468798,0.2706774],"study_design_scores_gemma":[0.0001959693,0.0001420835,0.6484067,0.00002847128,0.00001016842,0.000005453572,0.00002276631,0.3508531,0.000006008933,0.0002653248,0.00001041546,0.00005346666],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9973125,0.00007158391,0.001281544,0.00002327321,0.0002314619,0.0002555959,0.0002254231,0.00001300138,0.0005855602],"genre_scores_gemma":[0.9976782,0.0001870276,0.001708713,0.0000125689,0.00002760324,0.000001196576,0.00005804991,0.000003845509,0.0003228185],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3508327,"threshold_uncertainty_score":0.9837582,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3164493997","doi":"10.1007/s10236-021-01461-0","title":"Quantifying wave measurement differences in historical and present wave buoy systems","year":2021,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Ocean Waves and Remote Sensing","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":true},"ca_institutions":"Environment and Climate Change Canada","funders":"Coastal and Hydraulics Laboratory; U.S. Army Corps of Engineers; National Oceanic and Atmospheric Administration; Fisheries and Oceans Canada; Environment and Climate Change Canada","keywords":"Buoy; Inclinometer; Swell; Remote sensing; Significant wave height; Wave height; Geology; Geodesy; Wind wave; Meteorology; Environmental science; Acoustics; Physics","retraction":null,"screen_n_in":null,"score":{"opus":0.07516645294677306,"gpt":0.210522259985724,"spread":0.135355807038951,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003092685,0.0001535864,0.0002680481,0.00007622939,0.0001198403,0.0001298995,0.0000584552,0.00008539003,0.00001826002],"category_scores_gemma":[0.00005378869,0.0001242245,0.00004455282,0.0001799908,0.000042643,0.00008683187,0.00002493626,0.0001874795,0.000003632593],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0001082429,"about_ca_system_score_gemma":0.00006507924,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001720287,"about_ca_topic_score_gemma":0.00438856,"domain_scores_codex":[0.9985279,0.000117904,0.0002801545,0.0003353101,0.0004222031,0.0003165092],"domain_scores_gemma":[0.9994792,0.00007972038,0.00007060452,0.0001650566,0.00007309424,0.0001322751],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.00005909375,0.0001209655,0.8434107,0.0004745947,0.0001003984,0.001530729,0.001269922,0.004371946,0.00004658213,0.001035411,0.001154068,0.1464256],"study_design_scores_gemma":[0.0001708835,0.00003703303,0.1836253,0.0001058424,0.00001282121,0.0001082836,0.0006140731,0.8144678,0.000005559332,0.0001463574,0.0005372477,0.000168842],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9894707,0.006169083,0.0002365952,0.000531233,0.001115234,0.0001292328,0.00001918126,0.00002928785,0.002299423],"genre_scores_gemma":[0.9981048,0.0003735161,0.0007009046,0.00002627243,0.0001214508,6.89615e-9,0.00003779782,0.00000555626,0.0006297287],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.8100958,"threshold_uncertainty_score":0.506573,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2528426286","doi":"10.1007/s10236-016-1003-6","title":"The effect of density stratification on the prediction of global storm surges","year":2016,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"Environment and Climate Change Canada; Dalhousie University","funders":"Environment and Climate Change Canada; Marine Environmental Observation Prediction and Response Network","keywords":"Tide gauge; Hindcast; Storm surge; Climatology; Baroclinity; Stratification (seeds); Environmental science; Surge; Standard deviation; Meteorology; Sea level; Storm; Geology; Oceanography; Geography; Statistics","retraction":null,"screen_n_in":null,"score":{"opus":0.008775855735754715,"gpt":0.2132590581155074,"spread":0.2044832023797527,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002169089,0.00005522972,0.00007943779,0.000006805588,0.0001136957,0.00001271673,0.0001704249,0.00003743022,0.0000553549],"category_scores_gemma":[0.0001600161,0.00001945513,0.00004662781,0.0001049572,0.0002081245,0.00003966987,0.000006962575,0.00005878754,0.00001184516],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001168743,"about_ca_system_score_gemma":0.00001671075,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0005568797,"about_ca_topic_score_gemma":0.006068702,"domain_scores_codex":[0.9992429,0.0001428964,0.0001358413,0.00009231557,0.0002600593,0.0001259841],"domain_scores_gemma":[0.9988543,0.0008390586,0.00005549881,0.0001769322,0.00003565542,0.00003854257],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001314563,0.000004824119,0.9339265,0.000007235658,0.000008255752,2.755705e-7,0.000002951949,0.00003379176,0.00004270782,0.006223659,0.0001028385,0.05951555],"study_design_scores_gemma":[0.0000894765,0.000432258,0.9925856,0.000009873495,0.000004998712,8.674946e-7,0.00001147797,0.00493228,0.0003505164,0.00148879,0.00007167595,0.0000222042],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9976344,0.00002779416,0.0002511148,0.001112917,0.0001042884,0.0001123051,0.0001896888,0.000009029029,0.0005585352],"genre_scores_gemma":[0.9998605,0.00004490059,0.000006967074,0.000004773322,0.00002897499,2.193631e-7,0.00001421148,8.71489e-7,0.00003856688],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.05949334,"threshold_uncertainty_score":0.3386478,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2905223493","doi":"10.1007/s10236-018-1240-y","title":"North Atlantic extratropical and subpolar gyre variability during the last 120 years: a gridded dataset of surface temperature, salinity, and density. Part 1: dataset validation and RMS variability","year":2018,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"Fisheries and Oceans Canada; Institut Polaire Français Paul Emile Victor; Natural Environment Research Council; Centre National d’Etudes Spatiales; Centre National de la Recherche Scientifique; Sight Research UK","keywords":"Ocean gyre; Climatology; Sea surface temperature; Atlantic multidecadal oscillation; Extratropical cyclone; Environmental science; North Atlantic oscillation; Oceanography; Geology; Gulf Stream; Subtropics","retraction":null,"screen_n_in":null,"score":{"opus":0.006822333833635262,"gpt":0.1990704531914212,"spread":0.1922481193577859,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007457076,0.0001701153,0.0002319117,0.00001195211,0.0002593373,0.0001258828,0.0001801551,0.00009402347,0.00004999786],"category_scores_gemma":[0.0001988647,0.0001224789,0.00001774168,0.0002533228,0.0007354182,0.0003012118,0.00009390785,0.0002006159,0.000001888563],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000004216176,"about_ca_system_score_gemma":0.00004562726,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0005777131,"about_ca_topic_score_gemma":0.00606927,"domain_scores_codex":[0.9986496,0.0002163819,0.0002830011,0.0004230364,0.0001971394,0.0002308407],"domain_scores_gemma":[0.9989777,0.0003332772,0.0001194726,0.0003813279,0.0000584661,0.0001297178],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00005273443,0.00002599366,0.9990441,0.0001461038,0.00002315379,0.000003010375,0.00008839747,0.0000371753,0.000007854421,0.00003943817,0.0003223628,0.0002096506],"study_design_scores_gemma":[0.0002529445,0.00009465832,0.9885315,0.00001883524,0.0000573674,0.00003724841,0.00009349265,0.009913693,0.00002048072,0.0005127589,0.0003120459,0.000154991],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9867453,0.00007059563,0.0001013029,0.00005908294,0.0000809815,0.0001768711,0.01273586,0.00001954368,0.00001047323],"genre_scores_gemma":[0.9884136,0.0002681004,0.0008389627,0.00004713302,0.00007911256,1.344105e-7,0.01034574,0.000004518555,0.000002712231],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.01051264,"threshold_uncertainty_score":0.4994544,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2805596999","doi":"10.1007/s10236-018-1168-2","title":"Controls on the interannual variability of hypoxia in a subtropical embayment and its adjacent waters in the Guangdong coastal upwelling system, northern South China Sea","year":2018,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Dalhousie University","funders":"Fundamental Research Funds for the Central Universities; Hong Kong Government; National Natural Science Foundation of China; Research Councils UK","keywords":"Upwelling; Bay; Oceanography; Hypoxia (environmental); Estuary; Environmental science; Discharge; Stratification (seeds); Water mass; Subtropics; Bottom water; Plume; Geology; Fishery; Oxygen; Biology","retraction":null,"screen_n_in":null,"score":{"opus":0.006801808855211042,"gpt":0.1799646610892348,"spread":0.1731628522340238,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001007639,0.0001417956,0.0002236945,0.00005082071,0.0000737996,0.00005016465,0.0002563749,0.00005129557,0.00003018017],"category_scores_gemma":[0.00005029116,0.00007603384,0.00004391054,0.0001413877,0.0000823988,0.00006047435,0.00003602053,0.0001991889,0.00001113922],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001987317,"about_ca_system_score_gemma":0.00002896644,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.003531563,"about_ca_topic_score_gemma":0.08761713,"domain_scores_codex":[0.998562,0.0003648672,0.0003469849,0.0002281196,0.0002401408,0.0002578462],"domain_scores_gemma":[0.9993973,0.0002170963,0.00009815289,0.0002067828,0.00003321069,0.0000474088],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.0001959022,0.00003706541,0.9928259,0.00007355445,0.00001313789,0.00001090598,0.003363718,0.001043898,0.000001808845,0.0011462,0.000005088722,0.001282873],"study_design_scores_gemma":[0.0003892332,0.0002530619,0.4772139,0.00008644926,0.00000824326,0.000009634997,0.003986712,0.5178484,0.000003929142,0.00008129208,0.00002734946,0.00009189661],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9963968,0.00001417121,0.0001033435,0.0003116723,0.0001402192,0.0004416385,0.0002184544,0.000009779228,0.002363918],"genre_scores_gemma":[0.999794,0.000003510264,0.000007264475,0.00006338995,0.00005761753,0.000001267819,0.00004452177,0.00000377026,0.0000246346],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.5168045,"threshold_uncertainty_score":0.9290315,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1970167185","doi":"10.1007/s10236-010-0308-0","title":"The influence of Gulf of Mexico Loop Current intrusion on the transport of the Florida Current","year":2010,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Dalhousie University","funders":"","keywords":"Current (fluid); Altimeter; Intrusion; Geology; Channel (broadcasting); Empirical orthogonal functions; Satellite; Oceanography; Climatology; Remote sensing; Telecommunications","retraction":null,"screen_n_in":null,"score":{"opus":0.005604055305469651,"gpt":0.2002871838182739,"spread":0.1946831285128042,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000390093,0.0001310379,0.0001621545,0.00001227323,0.0001848646,0.000009546578,0.0007841302,0.00004475329,0.00005348497],"category_scores_gemma":[0.0000977397,0.00005657342,0.0001136106,0.0004503601,0.0006073447,0.00007095148,0.00002253316,0.0003584022,0.000002128141],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002054077,"about_ca_system_score_gemma":0.000103829,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0001192168,"about_ca_topic_score_gemma":0.0009933593,"domain_scores_codex":[0.9988617,0.0000408673,0.0003523798,0.0001452303,0.0004183715,0.0001814502],"domain_scores_gemma":[0.9988334,0.0002796651,0.0003020221,0.0004245066,0.0001177457,0.00004265698],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0000436246,0.00004414077,0.9281181,0.00008044706,0.00001399501,1.798814e-7,0.0002314276,0.005875431,0.00003376684,0.003290871,0.00008638357,0.06218171],"study_design_scores_gemma":[0.0001509649,0.000104692,0.9642435,0.000157286,0.00003698092,0.000001741734,0.0002127874,0.02839355,0.0005581854,0.003320732,0.002695138,0.0001243938],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9975099,0.0005570259,0.00006573692,0.0003031435,0.0008387657,0.0001679535,0.0001179504,0.00000848383,0.0004310498],"genre_scores_gemma":[0.9989751,0.0008896035,0.00003415477,0.00002565816,0.0000356453,2.78707e-7,0.00001401799,0.000003460443,0.00002210538],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.06205732,"threshold_uncertainty_score":0.2306997,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2009362954","doi":"10.1007/s10236-010-0356-5","title":"A finite element sea ice model of the Canadian Arctic Archipelago","year":2010,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":true},"ca_institutions":"University of Alberta","funders":"ArcticNet","keywords":"Geology; Sea ice; Arctic ice pack; Arctic; Oceanography; Archipelago; Arctic dipole anomaly; Arctic sea ice decline; Climatology; Drift ice","retraction":null,"screen_n_in":null,"score":{"opus":0.008181623967583422,"gpt":0.1864143469434073,"spread":0.1782327229758238,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002828769,0.0001473142,0.0001403628,0.00007387107,0.0003488227,0.00003646504,0.0005066798,0.00009239596,0.0003007783],"category_scores_gemma":[0.0001183521,0.0001066674,0.00009540861,0.0001947334,0.0002460143,0.00008977952,0.00002873331,0.0004925795,0.0000308237],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00002972741,"about_ca_system_score_gemma":0.0005823075,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.1825148,"about_ca_topic_score_gemma":0.9500849,"domain_scores_codex":[0.9988176,0.0000339814,0.0002307233,0.0002005627,0.000301001,0.0004161682],"domain_scores_gemma":[0.9990506,0.0001202578,0.000107666,0.0004093645,0.00007994456,0.0002321556],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.00001129604,0.00001619582,0.8560008,0.00003549343,0.00002196261,0.000003324467,0.0005514739,0.1281621,0.000004436919,0.008134636,0.00006424695,0.006994008],"study_design_scores_gemma":[0.0001103679,0.00002215407,0.09456405,0.00001257203,0.00002385067,0.000009616202,0.0001549069,0.8968113,0.000002642915,0.007982903,0.0001781053,0.0001275293],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.983709,0.000006013763,0.001632139,0.001512625,0.0005310042,0.000206124,0.0006861434,0.00001954482,0.01169742],"genre_scores_gemma":[0.99568,0.000009522023,0.002895767,0.0006189386,0.00004993163,2.584266e-7,0.0001510242,0.000007249252,0.0005873119],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.7686492,"threshold_uncertainty_score":0.8229288,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2165185803","doi":"10.1007/s10236-007-0115-4","title":"High-resolution atmospheric forcing for regional oceanic model: the Iroise Sea","year":2007,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Climate variability and models","field":"Environmental Science","cited_by":16,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Canadian Association for Laboratory Animal Science","funders":"","keywords":"Forcing (mathematics); Weather Research and Forecasting Model; Environmental science; Climatology; Sea surface temperature; Mesoscale meteorology; Atmospheric model; Downscaling; Planetary boundary layer; Meteorology; Geology; Climate change; Geography; Oceanography","retraction":null,"screen_n_in":null,"score":{"opus":0.01424307064201705,"gpt":0.2295064088467881,"spread":0.215263338204771,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007843199,0.0001381539,0.0001132136,0.00000531323,0.0003225122,0.0000267457,0.0002685562,0.00009112038,0.0000536226],"category_scores_gemma":[0.00003795907,0.00010876,0.00009835955,0.000162773,0.0001579019,0.0001696745,0.0001313345,0.0001213142,0.00002153344],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0005480736,"about_ca_system_score_gemma":0.0000151599,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0002052732,"about_ca_topic_score_gemma":0.0007339678,"domain_scores_codex":[0.9988109,0.00001806371,0.0002306147,0.0003004521,0.0002360685,0.0004038742],"domain_scores_gemma":[0.999324,0.0001626516,0.00008338484,0.0003343928,0.00001290888,0.00008269125],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.00009052204,0.00008588415,0.007592942,0.00001650367,0.000009378965,0.000001100498,0.0002583753,0.948894,0.0001222821,0.03818906,0.003016832,0.00172308],"study_design_scores_gemma":[0.000256182,0.00003570386,0.003838925,0.000006045193,0.00002112382,0.000005088533,0.00007998192,0.9719942,0.000009120776,0.02309739,0.0005159662,0.0001403174],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.6076339,0.000009600104,0.3902818,0.0005530062,0.00008964353,0.000294419,0.00002724776,0.00005204525,0.001058297],"genre_scores_gemma":[0.9762802,0.0000187699,0.02224869,0.000512949,0.00005349588,0.000004456406,0.00007096155,0.00002594848,0.0007845739],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3686462,"threshold_uncertainty_score":0.4435106,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2084153882","doi":"10.1007/s10236-008-0149-2","title":"Process study of coastal circulation over the inner Scotian Shelf using a nested-grid ocean circulation model, with a special emphasis on the storm-induced circulation during tropical storm Alberto in 2006","year":2008,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Dalhousie University","funders":"","keywords":"Hydrography; Climatology; Downscaling; Storm; Circulation (fluid dynamics); Forcing (mathematics); Barotropic fluid; Storm surge; Geology; Oceanography; Ocean current; Environmental science; Meteorology; Geography; Climate change","retraction":null,"screen_n_in":null,"score":{"opus":0.01675214320215106,"gpt":0.2142026923632236,"spread":0.1974505491610725,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002042794,0.0002916293,0.0002940357,0.0001026981,0.0005547236,0.00006336212,0.0002811206,0.0001044835,0.00003596617],"category_scores_gemma":[0.00004611645,0.0001865454,0.00006639976,0.001242273,0.0001585813,0.0005202536,0.00001808867,0.0003095506,0.00000155679],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00006168065,"about_ca_system_score_gemma":0.0001953951,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001601687,"about_ca_topic_score_gemma":0.03456311,"domain_scores_codex":[0.9978452,0.0001398011,0.0004667323,0.0004252164,0.0007635683,0.0003594394],"domain_scores_gemma":[0.9990618,0.0001010836,0.0003172007,0.0003145434,0.0001270762,0.00007829231],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00009952828,0.0001238178,0.5859319,0.00001808436,0.00002179465,0.000008633147,0.002348084,0.4112516,0.000004214792,0.00002038134,0.000002862418,0.000169125],"study_design_scores_gemma":[0.0005155659,0.00009610245,0.5443516,0.00003216376,0.00002617052,0.00002085428,0.001466068,0.4533024,0.000002249742,0.00004596711,4.006281e-7,0.0001404207],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9983885,0.00001670272,0.0004352894,0.00008067164,0.0001522787,0.0007436086,0.00003326547,0.000035952,0.0001137392],"genre_scores_gemma":[0.9995351,0.000006624743,0.00004923404,0.00004753879,0.0002738133,0.000001098238,0.00006088961,0.00001908441,0.000006571027],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.04205087,"threshold_uncertainty_score":0.9830536,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2151081461","doi":"10.1007/s10236-011-0498-0","title":"A numerical study of the circulation and monthly-to-seasonal variability in the Caribbean Sea: the role of Caribbean eddies","year":2011,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"ASL Environmental Sciences (Canada); Dalhousie University","funders":"","keywords":"Eddy; Climatology; Circulation (fluid dynamics); Forcing (mathematics); Ocean current; Boundary current; Oceanography; Ridge; Geology; Geography; Environmental science; Meteorology; Turbulence; Cartography","retraction":null,"screen_n_in":null,"score":{"opus":0.007663473223406521,"gpt":0.183107723649744,"spread":0.1754442504263375,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007394411,0.0001100649,0.0001623651,0.00001274345,0.0001446809,0.00001671808,0.0004136593,0.0000390352,0.00002548802],"category_scores_gemma":[0.0001014499,0.00005325413,0.00004460966,0.0004937113,0.0001941149,0.00007666792,0.00003331395,0.0001493722,4.82603e-7],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000004578654,"about_ca_system_score_gemma":0.00004492471,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.007057594,"about_ca_topic_score_gemma":0.005732269,"domain_scores_codex":[0.9988605,0.0002738162,0.0002296638,0.0001837519,0.000290583,0.0001616834],"domain_scores_gemma":[0.9992566,0.0002495037,0.0001108933,0.000298064,0.00004778151,0.00003723024],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0000264683,0.000102713,0.984627,0.00001325147,0.00001823161,5.627795e-7,0.008001458,0.002706737,2.910712e-7,0.0003304226,0.000007007441,0.004165831],"study_design_scores_gemma":[0.0001013359,0.0001069916,0.8467904,0.000006525929,0.00002762801,0.000001712476,0.009857388,0.1399837,0.000002186988,0.003048458,0.00001668933,0.00005703626],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9968553,0.0001459184,0.00007992086,0.0001357577,0.00005475374,0.0003718433,0.00007083541,0.000007537825,0.002278149],"genre_scores_gemma":[0.9998081,0.000005130931,0.0001041235,0.000051761,0.00001551351,9.072576e-7,0.000008784908,0.000002769956,0.000002935482],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1378366,"threshold_uncertainty_score":0.9995545,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1994326051","doi":"10.1007/s10236-011-0519-z","title":"Ensemble numerical forecasts of the sporadic Kuroshio water intrusion (kyucho) into shelf and coastal waters","year":2012,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"","funders":"Japan Society for the Promotion of Science; Ontario Council on Graduate Studies, Council of Ontario Universities","keywords":"Argo; Hindcast; Predictability; Downscaling; Climatology; Data assimilation; Geology; Environmental science; Meteorology; Oceanography; Geography; Statistics; Mathematics; Climate change","retraction":null,"screen_n_in":null,"score":{"opus":0.004597059558157647,"gpt":0.1741335505090705,"spread":0.1695364909509128,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001868978,0.0001443948,0.0001658199,0.00001680435,0.0001721823,0.0000286335,0.0001933849,0.00006954594,0.0001277112],"category_scores_gemma":[0.00001494402,0.00007662496,0.00005621793,0.0001853306,0.0002224745,0.0002648162,0.00005739525,0.0001289432,0.00001296002],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000004272539,"about_ca_system_score_gemma":0.00001851388,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0004138937,"about_ca_topic_score_gemma":0.0002483849,"domain_scores_codex":[0.9990446,0.00003696356,0.0001900517,0.0001600657,0.0002087617,0.0003595815],"domain_scores_gemma":[0.9995761,0.00003789405,0.00006502568,0.0001594887,0.00002487048,0.0001366335],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00003022104,0.00002289456,0.9760036,0.00004523453,0.00001117721,0.000001550137,0.0009220834,0.0001681478,0.00002437769,0.00009733478,0.0001293843,0.02254403],"study_design_scores_gemma":[0.0006091697,0.0002651622,0.8745113,0.00006809259,0.00007936941,0.0001138491,0.00149996,0.1136923,0.001395949,0.003358249,0.00388245,0.0005241664],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9974239,0.0002284402,0.0006054989,0.0002413138,0.0003616393,0.00009789031,0.00002452214,0.00002348901,0.000993317],"genre_scores_gemma":[0.9986177,0.00007205558,0.0008677098,0.0001299048,0.00006427507,1.344703e-7,0.00007254293,0.000006356767,0.0001693182],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1135242,"threshold_uncertainty_score":0.3124675,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3027632660","doi":"10.1007/s10236-020-01363-7","title":"On the use of long-term observation of water level and temperature along the shore for a better understanding of the dynamics: example of Toulon area, France","year":2020,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Université du Québec à Rimouski","funders":"","keywords":"Bay; Water level; Shore; Tide gauge; Geology; Piezometer; Submarine pipeline; Sea level; Oceanography; Plume; Environmental science; Hydrology (agriculture); Meteorology; Groundwater; Geography","retraction":null,"screen_n_in":null,"score":{"opus":0.07762953709547964,"gpt":0.206206070519814,"spread":0.1285765334243343,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001524597,0.0001137593,0.0001862162,0.00000926772,0.0001063443,0.00002130403,0.0002574935,0.00006330834,0.00002380511],"category_scores_gemma":[0.00006041315,0.00004998798,0.00007564508,0.0002179976,0.000278384,0.0001246383,0.00002333172,0.0001133081,6.394653e-8],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000004653321,"about_ca_system_score_gemma":0.00002299878,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0002707713,"about_ca_topic_score_gemma":0.001611664,"domain_scores_codex":[0.9992316,0.00003702101,0.0002575016,0.000147698,0.0001951581,0.000131007],"domain_scores_gemma":[0.9991092,0.00041424,0.0001872225,0.0001962417,0.00006964169,0.00002345296],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00006413397,0.00001196419,0.993147,0.0002486432,0.00004232553,3.107173e-7,0.001231172,0.002903689,0.0000927524,0.001236137,0.00008884902,0.0009329849],"study_design_scores_gemma":[0.0002527099,0.0002026996,0.6867861,0.0001890401,0.00005869904,0.000001553296,0.001099412,0.3089139,0.0007352075,0.001635834,0.00001328089,0.0001115517],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9927624,0.00009172018,0.004169963,0.002171564,0.00005259961,0.000276482,0.0004561578,0.000004719292,0.00001434052],"genre_scores_gemma":[0.9990043,0.00004479749,0.0003799313,0.0004091476,0.00001435709,3.905158e-7,0.0001051432,0.000005349112,0.00003659467],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.306361,"threshold_uncertainty_score":0.2038451,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2024532166","doi":"10.1007/s10236-010-0320-4","title":"Eddy-permitting simulations of the sub-polar North Atlantic: impact of the model bias on water mass properties and circulation","year":2010,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"Bedford Institute of Oceanography; Dalhousie University; Memorial University of Newfoundland","funders":"Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Ocean gyre; Water mass; Water column; Polar; Temperature salinity diagrams; Climatology; Geology; Salinity; Ocean current; Environmental science; Thermohaline circulation; Atmospheric sciences; Oceanography; Physics","retraction":null,"screen_n_in":null,"score":{"opus":0.01581706440627133,"gpt":0.1917751632181115,"spread":0.1759580988118401,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001066237,0.00009949946,0.0001085158,0.00001379127,0.0001942309,0.00002449433,0.0001810374,0.0000489772,0.00001541473],"category_scores_gemma":[0.00005712128,0.0000418958,0.00007861063,0.0001791624,0.0001709889,0.0001176635,0.00001682512,0.0001494238,6.269617e-7],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002719362,"about_ca_system_score_gemma":0.00005256305,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0004854809,"about_ca_topic_score_gemma":0.002631806,"domain_scores_codex":[0.9993587,0.00002891431,0.0001757291,0.0001154961,0.0001775308,0.000143632],"domain_scores_gemma":[0.9995465,0.0000518078,0.0001067862,0.0002027443,0.00006163384,0.00003051666],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.000005762133,0.000006394639,0.6545331,0.0000181456,0.000009097982,5.440756e-8,0.0001588299,0.3445774,0.0003311324,0.00001878807,0.000001906821,0.0003393618],"study_design_scores_gemma":[0.00004565072,0.00001403419,0.4429657,0.00001291817,0.00001171683,0.000001101303,0.00002289392,0.5564087,0.0001629727,0.0003132594,0.000001141809,0.00003988119],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9993461,0.00002070521,0.000135468,0.00008123959,0.00007728205,0.0001288536,0.00009151881,0.000009681016,0.0001091914],"genre_scores_gemma":[0.9997439,0.00001070904,0.0001380445,0.00002246653,0.00001894803,5.95979e-8,0.00002888104,0.000004254768,0.00003267087],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2118313,"threshold_uncertainty_score":0.1708461,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W4375850440","doi":"10.1007/s10236-023-01556-w","title":"Non-linear interactions between tides and storm surges during extreme weather events over the eastern Canadian shelf","year":2023,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":true},"ca_institutions":"Dalhousie University","funders":"Ocean Frontier Institute; Natural Sciences and Engineering Research Council of Canada; Mitacs; Marine Environmental Observation Prediction and Response Network","keywords":"Barotropic fluid; Climatology; Baroclinity; Storm surge; Storm; Advection; Forcing (mathematics); Storm track; Environmental science; Geology; Atmospheric sciences; Winter storm; Oceanography; Meteorology; Geography; Physics","retraction":null,"screen_n_in":null,"score":{"opus":0.02704094212681054,"gpt":0.2480871242057123,"spread":0.2210461820789017,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000861083,0.0001065936,0.0001145913,0.000106304,0.0003314919,0.00006280166,0.0001881812,0.00004718138,0.0004315146],"category_scores_gemma":[0.00002345317,0.00007073741,0.00004534081,0.0002507488,0.00007346785,0.0001373884,0.00002984289,0.0002332976,0.0002676174],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00002088799,"about_ca_system_score_gemma":0.0000402582,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.1905231,"about_ca_topic_score_gemma":0.7743282,"domain_scores_codex":[0.9990366,0.00003471255,0.0001319106,0.0001913172,0.0002011374,0.0004043841],"domain_scores_gemma":[0.9994075,0.0001288379,0.00002181424,0.0001472694,0.00001862698,0.0002759055],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.000007242759,0.000002898821,0.9939411,0.00001072158,0.00001768509,0.00001559701,0.00007506955,0.0001622636,0.000001290617,0.00001922991,0.0001237698,0.005623093],"study_design_scores_gemma":[0.00009045548,0.00002243213,0.9244039,0.00001205971,0.000006537797,0.000003918355,0.0001268753,0.07301634,8.017181e-7,0.0002103352,0.002018893,0.00008745606],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9977317,0.00003222718,0.00001570573,0.001132725,0.0001553711,0.00009736171,0.0001826579,0.00003500942,0.0006172702],"genre_scores_gemma":[0.9973823,0.00005942851,0.00002242712,0.00003706445,0.0001897883,4.709859e-7,0.0001325795,0.000006503964,0.002169391],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.5838051,"threshold_uncertainty_score":0.8148673,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3184088746","doi":"10.1007/s10236-021-01468-7","title":"Spectral shapes and parameters from three different wave sensors","year":2021,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Ocean Waves and Remote Sensing","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Environment and Climate Change Canada","funders":"Norges Forskningsråd; ConocoPhillips","keywords":"Swell; Buoy; Significant wave height; Wave height; Wind wave; Wind wave model; Remote sensing; Geology; Wave radar; Radar; Meteorology; Wave model; Environmental science; Wave shoaling; Calibration; Geodesy; Wave propagation; Physics; Optics; Radar engineering details; Radar imaging; Computer science; Longitudinal wave; Telecommunications; Mechanical wave","retraction":null,"screen_n_in":null,"score":{"opus":0.0122659557854808,"gpt":0.1807409754391778,"spread":0.168475019653697,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00003886209,0.0001560743,0.0001889063,0.00002996373,0.0001176344,0.0001224178,0.00005563903,0.00007043123,0.0002171053],"category_scores_gemma":[0.00001884294,0.0001225962,0.00006586756,0.00007976315,0.00008873438,0.00006951012,0.00001909852,0.0001549449,0.00001718598],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000008104596,"about_ca_system_score_gemma":0.00001654348,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0004347409,"about_ca_topic_score_gemma":0.006942956,"domain_scores_codex":[0.9990835,0.00003577354,0.0001462599,0.0003073107,0.0001537512,0.0002733759],"domain_scores_gemma":[0.9995338,0.000127196,0.00004335649,0.0001370637,0.00001810892,0.0001405195],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.00007024201,0.00004802228,0.7758648,0.00004506401,0.0002103292,0.001458193,0.0006990983,0.0108034,0.0000879685,0.0005579575,0.0002415197,0.2099133],"study_design_scores_gemma":[0.0001185996,0.00002472402,0.3662914,0.00001599905,0.00002018625,0.00004528145,0.0002503838,0.6296268,0.00006525512,0.003372619,0.00003416708,0.0001345648],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9966241,0.0003002731,0.0001217921,0.0003625123,0.0003597583,0.00005060148,0.0001703522,0.00003640834,0.001974185],"genre_scores_gemma":[0.9942344,0.0001656678,0.004813861,0.0001242177,0.0001051699,7.822092e-10,0.0002974075,0.000006673109,0.0002525942],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.6188234,"threshold_uncertainty_score":0.499933,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2030366821","doi":"10.1007/s10236-013-0672-7","title":"Modelling study of three-dimensional circulation and particle movement over the Sable Gully of Nova Scotia","year":2013,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada; Dalhousie University","funders":"","keywords":"Geology; Canyon; Current meter; Thalweg; Oceanography; Hydrology (agriculture); Ravine; Ocean current; Geomorphology; Geography; Sediment","retraction":null,"screen_n_in":null,"score":{"opus":0.01242561088476412,"gpt":0.1925258901437347,"spread":0.1801002792589706,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001381277,0.00007475807,0.0001096494,0.000008746063,0.00006236231,0.00002005347,0.0000926197,0.00002276352,0.0002704387],"category_scores_gemma":[0.000006004768,0.00004966515,0.00002090759,0.0001950389,0.00006832225,0.0001618948,0.00001512253,0.00004806052,0.000004073157],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001985433,"about_ca_system_score_gemma":0.00001805089,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.009536139,"about_ca_topic_score_gemma":0.003802688,"domain_scores_codex":[0.9993177,0.00001704252,0.0002011514,0.0001249871,0.0002155171,0.0001235941],"domain_scores_gemma":[0.9996077,0.00006218628,0.0001041248,0.0001255742,0.00006564531,0.00003477686],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.000005084036,0.00004083244,0.6422995,0.00001384119,0.000015096,1.714049e-7,0.0001024804,0.3566711,0.000003623728,0.00008425868,0.00001473684,0.0007493172],"study_design_scores_gemma":[0.0001326041,0.00007249738,0.397393,0.000008248525,0.00001187712,2.74943e-7,0.0003078587,0.6002923,0.000004583613,0.001739515,5.540012e-7,0.00003664988],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9976815,0.000194977,0.001681823,0.00004373069,0.00005519187,0.0002203058,0.000009820604,0.000007793938,0.0001048481],"genre_scores_gemma":[0.9993007,0.000007522233,0.0006170231,0.00003783884,0.000009224021,1.196806e-7,0.000009854094,0.000002561446,0.00001511813],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2449065,"threshold_uncertainty_score":0.9970595,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1998769658","doi":"10.1007/s10236-009-0212-7","title":"Effect of stratification on tidal circulation over the Scotian Shelf and Gulf of St. Lawrence: a numerical study using a three-dimensional shelf circulation model","year":2009,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"Bedford Institute of Oceanography; Environment and Climate Change Canada; Fisheries and Oceans Canada; Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Stratification (seeds); Baroclinity; Oceanography; Hydrography; Geology; Circulation (fluid dynamics); Continental shelf; Water column; Climatology; Pressure gradient; Mechanics","retraction":null,"screen_n_in":null,"score":{"opus":0.01024791779352093,"gpt":0.2346163604193448,"spread":0.2243684426258239,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003743778,0.0001458678,0.0002028957,0.00003391087,0.0001412319,0.00003095757,0.0001191798,0.00006341754,0.00002681626],"category_scores_gemma":[0.00003190711,0.0001008266,0.00004883825,0.0003606083,0.0001001682,0.0001872366,0.000006690859,0.00011035,5.747727e-7],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000009113382,"about_ca_system_score_gemma":0.00005439571,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0001970223,"about_ca_topic_score_gemma":0.0001584114,"domain_scores_codex":[0.9988492,0.00008875812,0.0002824395,0.0002406744,0.0003968986,0.0001420314],"domain_scores_gemma":[0.9993622,0.0001445276,0.0002036112,0.0001841038,0.00005826222,0.0000473492],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.00006862907,0.00006137347,0.5536008,0.00002132819,0.00001413389,5.8774e-7,0.00012525,0.4379708,0.00003425213,0.0002277508,0.000002456937,0.007872573],"study_design_scores_gemma":[0.0001901434,0.0003824873,0.4328289,0.00001945402,0.00003266482,0.000002062487,0.00003190827,0.5652885,0.00000599418,0.00115899,8.561801e-8,0.00005871005],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.990528,0.00007166372,0.008804035,0.00003639479,0.00004854637,0.0003591245,0.00004023522,0.0000172245,0.00009476557],"genre_scores_gemma":[0.9993618,0.000002830272,0.0005077042,0.00002701398,0.00002089632,1.954661e-7,0.00007317566,0.000003829837,0.000002531357],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1273178,"threshold_uncertainty_score":0.411159,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2211348225","doi":"10.1007/s10236-015-0883-1","title":"Modelling subglacial discharge and its influence on ocean heat transport in Arctic fjords","year":2015,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Manitoba","funders":"Energistyrelsen; ArcticNet","keywords":"Geology; Fjord; Glacier; Plume; Tidewater glacier cycle; Entrainment (biomusicology); Arctic; Oceanography; Glacier ice accumulation; Geomorphology; Ice stream; Sea ice; Cryosphere; Meteorology","retraction":null,"screen_n_in":null,"score":{"opus":0.02340478424869509,"gpt":0.2138365531370333,"spread":0.1904317688883383,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001683813,0.0001247539,0.0001493098,0.00003208009,0.0001067178,0.00002276296,0.000100781,0.00004699756,0.00002578966],"category_scores_gemma":[0.0000247968,0.0001094802,0.00002483176,0.00022664,0.00003985212,0.0001818328,0.000006959336,0.0001377554,0.00001344004],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001928335,"about_ca_system_score_gemma":0.00003678036,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002026591,"about_ca_topic_score_gemma":0.009604758,"domain_scores_codex":[0.9991513,0.00001676625,0.0001817664,0.0002187156,0.0001863383,0.0002450579],"domain_scores_gemma":[0.9996567,0.00004941761,0.00002503023,0.0000975818,0.00004134889,0.0001299208],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.00002220454,0.000009633577,0.6034359,0.000008649914,0.000003008423,0.00000534738,0.0004033323,0.3955109,5.770725e-8,0.0003999657,0.00001189887,0.0001891196],"study_design_scores_gemma":[0.0002037033,0.00006005142,0.3495168,0.00001785071,0.00000554968,0.00000203846,0.0002645669,0.6491731,2.214791e-7,0.0004722469,0.0001808185,0.0001030651],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9981133,0.0003010852,0.0002987057,0.000325635,0.0001510962,0.0001216663,0.00006438615,0.0000241469,0.0005999292],"genre_scores_gemma":[0.9991634,0.0001799165,0.0001918503,0.0001774141,0.00004649499,1.992008e-7,0.00009571847,0.00000473505,0.0001403017],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2539192,"threshold_uncertainty_score":0.535968,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1980085487","doi":"10.1007/s10236-014-0799-1","title":"Behavior and mixing of a cold intermediate layer near a sloping boundary","year":2015,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Fisheries and Oceans Canada; Université du Québec à Rimouski","funders":"","keywords":"Geology; Dissipation; Sill; Internal tide; Stratification (seeds); Internal wave; Turbulence; Boundary layer; Turbulence kinetic energy; Mooring; Mechanics; Oceanography; Physics","retraction":null,"screen_n_in":null,"score":{"opus":0.01393877201786522,"gpt":0.2164245493024385,"spread":0.2024857772845732,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016358,0.0001027869,0.0001541811,0.00001793818,0.00008350179,0.00007247296,0.000127923,0.00005131168,0.00003035524],"category_scores_gemma":[0.0000344024,0.00008954237,0.00002955244,0.0002000814,0.0002274816,0.0001925165,0.00002204618,0.0000945456,0.000005923732],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000004596789,"about_ca_system_score_gemma":0.0001076067,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.000236657,"about_ca_topic_score_gemma":0.0004588245,"domain_scores_codex":[0.999306,0.00001901209,0.0001694621,0.0001571067,0.0001598968,0.0001885706],"domain_scores_gemma":[0.9995836,0.00003976398,0.00008431605,0.0001001192,0.00005050181,0.0001417256],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00001619226,0.00001283569,0.9872096,0.00004042594,0.000009417182,0.00001513823,0.0003390679,0.00009504889,0.000001829724,0.0001187077,0.0001192451,0.01202256],"study_design_scores_gemma":[0.001029492,0.0005127205,0.684836,0.000168586,0.0001031327,0.00006385671,0.002324572,0.303894,0.0000562972,0.001434426,0.005057632,0.0005193536],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.996906,0.0009424055,0.0002772439,0.00004670141,0.000192987,0.00008298036,0.00004962389,0.00003464102,0.001467453],"genre_scores_gemma":[0.9962687,0.00008102989,0.003348745,0.00008885826,0.00003124719,2.041547e-7,0.00003715241,0.00000465957,0.0001394299],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3037989,"threshold_uncertainty_score":0.3651432,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2294601980","doi":"10.1007/s10236-016-0926-2","title":"Numerical study of tides in Ontario Lacus, a hydrocarbon lake on the surface of the Saturnian moon Titan","year":2016,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Titan (rocket family); Bathymetry; Geology; Submarine pipeline; Shore; Clockwise; Oceanography; Geodesy; Geometry; Astrobiology; Rotation (mathematics); Physics","retraction":null,"screen_n_in":null,"score":{"opus":0.00796600714362339,"gpt":0.176812268998071,"spread":0.1688462618544476,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002135822,0.0001181447,0.0001773745,0.00001249006,0.00005657683,0.00001004921,0.0003768917,0.00004444329,0.0001998272],"category_scores_gemma":[0.00004518206,0.00005024248,0.00005104333,0.0003555265,0.0001227252,0.00005788798,0.00001765292,0.0001559592,0.000005532978],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0000124723,"about_ca_system_score_gemma":0.00008023804,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.01928438,"about_ca_topic_score_gemma":0.5806355,"domain_scores_codex":[0.9990694,0.00008481873,0.0002251716,0.0001671103,0.0002767303,0.0001767853],"domain_scores_gemma":[0.9993033,0.0002285915,0.0001343936,0.0002768961,0.00002249599,0.00003426741],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00004104244,0.00009709181,0.9958029,0.00000630001,0.00001497923,0.000001851401,0.0005471816,0.002509002,0.000003821664,0.00008392512,0.00004645927,0.0008454306],"study_design_scores_gemma":[0.0002740428,0.0003222574,0.9899004,0.00006599333,0.00001190191,0.000001364802,0.0006223284,0.007971198,0.00002537403,0.0005486936,0.0001682633,0.00008823317],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9953304,0.0000408285,0.00001004637,0.0002786407,0.00009095902,0.0001843298,0.0000251721,0.000009944431,0.004029694],"genre_scores_gemma":[0.9993811,0.00001136954,0.00003727163,0.00006071904,0.000008047394,1.302338e-7,0.000003445248,0.000003907509,0.0004940503],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.5613511,"threshold_uncertainty_score":0.9872463,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2024424258","doi":"10.1007/s10236-008-0132-y","title":"Airside velocity measurements over the wind-sheared water surface using particle image velocimetry","year":2008,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Ocean Waves and Remote Sensing","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Concordia University","funders":"","keywords":"Particle image velocimetry; Vorticity; Mechanics; Reynolds stress; Wind speed; Airflow; Reynolds number; Dissipation; Geology; Physics; Meteorology; Vortex; Turbulence; Thermodynamics","retraction":null,"screen_n_in":null,"score":{"opus":0.0296035782842941,"gpt":0.2202617085663727,"spread":0.1906581302820786,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003916004,0.0001921709,0.0001822155,0.00002657887,0.0007355165,0.00008424338,0.0002127435,0.00008073137,0.0002427007],"category_scores_gemma":[0.00002638728,0.0001151319,0.00009756762,0.0002042816,0.0002467627,0.000253573,0.00003455071,0.0002190066,0.0001203869],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00003783195,"about_ca_system_score_gemma":0.00005088661,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001426998,"about_ca_topic_score_gemma":0.0003069598,"domain_scores_codex":[0.9983515,0.0001137095,0.0002443668,0.0002817918,0.0004494807,0.0005591224],"domain_scores_gemma":[0.999383,0.00004993027,0.0000623751,0.0003036984,0.00006664701,0.0001343921],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.0000906635,0.00006261301,0.8995134,0.00003474164,0.0001302546,0.0001756406,0.002024816,0.09012063,0.001791522,0.00001262822,0.0008491921,0.005193864],"study_design_scores_gemma":[0.0002437506,0.0000235532,0.2636868,0.00001183712,0.00002206085,0.00007915197,0.0001697259,0.7341745,0.001196606,0.00008446454,0.0001199746,0.000187562],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9974293,0.00009266981,0.0002085007,0.0002385349,0.0003816638,0.0001442328,0.00002568259,0.00005381126,0.001425673],"genre_scores_gemma":[0.9955279,0.00001841498,0.003672567,0.0002490311,0.00009412437,1.001806e-9,0.00005817054,0.00001268991,0.0003670789],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.6440539,"threshold_uncertainty_score":0.5657073,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2071769506","doi":"10.1007/s10236-007-0120-7","title":"Numerical study of circulation and temperature-salinity distributions in the Bras d’Or Lakes","year":2007,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Bedford Institute of Oceanography; Dalhousie University; Cape Breton University","funders":"","keywords":"Geology; Estuary; Oceanography; Hydrography; Estuarine water circulation; Forcing (mathematics); Ocean current; Current (fluid); Buoyancy; Surface runoff; Discharge; Climatology; Drainage basin; Geography","retraction":null,"screen_n_in":null,"score":{"opus":0.01003629810487734,"gpt":0.2323813924214049,"spread":0.2223450943165276,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003915598,0.0000744307,0.0001047871,0.00001703918,0.0001106878,0.00002885187,0.0001175589,0.00004255286,0.00002647256],"category_scores_gemma":[0.00006983877,0.00004497137,0.00001681031,0.0005683592,0.00007307288,0.00009616704,0.00000468587,0.0001226913,7.697538e-7],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00000274064,"about_ca_system_score_gemma":0.0000276123,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0005222548,"about_ca_topic_score_gemma":0.005738463,"domain_scores_codex":[0.9993514,0.00004695065,0.0001837863,0.0001242201,0.0001566253,0.0001370557],"domain_scores_gemma":[0.9995499,0.0002311447,0.00005619372,0.0001012236,0.0000257461,0.00003585458],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0000375095,0.0001096386,0.9956533,0.00001095074,0.00000597031,0.000009487451,0.0004456186,0.001052157,6.698401e-7,0.0001814591,0.00001117916,0.002482002],"study_design_scores_gemma":[0.0001935664,0.0001497308,0.970294,0.000006162047,0.00001027169,0.000009346854,0.003596277,0.02528538,0.00000109117,0.0003675436,0.00002381879,0.00006279912],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9986216,0.00008772858,0.0005382927,0.00005939498,0.00004714168,0.0001418012,0.00003869941,0.00001330092,0.000452033],"genre_scores_gemma":[0.9997119,0.00001662578,0.0001265372,0.00003381974,0.00002105432,1.050523e-7,0.00007918056,0.000001479792,0.000009301374],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.02535934,"threshold_uncertainty_score":0.3202197,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2062616035","doi":"10.1007/s10236-011-0497-1","title":"Sensitivity of acoustic propagation to uncertainties in the marine environment as characterized by various rapid environmental assessment methods","year":2011,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Underwater Acoustics Research","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Defence Research and Development Canada","funders":"","keywords":"Sonar; Bathymetry; Sensitivity (control systems); Propagation of uncertainty; Environmental data; Data set; Monte Carlo method; Environmental science; Computer science; Geology; Meteorology; Oceanography; Statistics; Algorithm; Geography; Engineering; Mathematics; Artificial intelligence","retraction":null,"screen_n_in":null,"score":{"opus":0.01731742885045025,"gpt":0.2579044419474382,"spread":0.240587013096988,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001756457,0.0001552334,0.0001948752,0.0001012309,0.00007784717,0.00003363598,0.0002282918,0.00006011941,0.001024569],"category_scores_gemma":[0.00002332487,0.0001143294,0.00003847293,0.0001119493,0.0001416674,0.0001063908,0.00007022009,0.0002162976,0.00003891959],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00007716277,"about_ca_system_score_gemma":0.00004011106,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002048618,"about_ca_topic_score_gemma":0.0005735431,"domain_scores_codex":[0.9980192,0.0007014024,0.0002622334,0.0002652169,0.0004434155,0.0003085656],"domain_scores_gemma":[0.9992906,0.0002617637,0.00008686841,0.0002677708,0.000008414083,0.00008451813],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.0003582368,0.0007833593,0.5512909,0.0001362183,0.0001161039,0.0001213389,0.00484723,0.03949096,0.03451477,0.00005490048,0.00008594537,0.3682],"study_design_scores_gemma":[0.0002462118,0.0003931037,0.3591615,0.000006138194,0.00002400179,0.0000202585,0.0007037742,0.6379601,0.0006630296,0.0004974325,0.0001553743,0.0001690689],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.6588563,0.00001328254,0.3379221,0.0001464857,0.00006406489,0.0008415631,0.000252433,0.00001349962,0.001890186],"genre_scores_gemma":[0.9797534,0.00008727168,0.01932154,0.0001114096,0.0000149007,0.000003777374,0.0004741533,0.000007029121,0.0002265308],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.5984691,"threshold_uncertainty_score":0.9998887,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W4402782544","doi":"10.1007/s10236-024-01634-7","title":"A new high-resolution Coastal Ice-Ocean Prediction System for the East Coast of Canada","year":2024,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada; Canadian Hydrographic Service","funders":"","keywords":"Geology; Oceanography; East coast; Climatology; Sea ice; High resolution; Remote sensing","retraction":null,"screen_n_in":null,"score":{"opus":0.005573362734358543,"gpt":0.170524524222774,"spread":0.1649511614884155,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002629918,0.000148403,0.0001606206,0.00004436871,0.0002625139,0.00005945323,0.0002122038,0.00006462689,0.00004709888],"category_scores_gemma":[0.00002788884,0.0001054672,0.0000753428,0.0002085265,0.00006562851,0.0001380962,0.00001760907,0.0001504859,0.000003811666],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00007252342,"about_ca_system_score_gemma":0.0008042105,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.3928296,"about_ca_topic_score_gemma":0.7820899,"domain_scores_codex":[0.9988402,0.00002801189,0.0002822373,0.0002216112,0.0003252595,0.0003027237],"domain_scores_gemma":[0.9992898,0.0002643096,0.0000845235,0.0001808322,0.00006233464,0.0001181936],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.000682122,0.00004950399,0.3490749,0.002728369,0.0007952893,0.00009188153,0.002638603,0.3645629,0.00001051348,0.07790367,0.0817859,0.1196763],"study_design_scores_gemma":[0.0001960574,0.00009407537,0.02172137,0.000117812,0.00009665594,0.0000562555,0.003520882,0.9712421,0.000001497496,0.0002254471,0.002615385,0.0001124412],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.6140153,0.0005746401,0.3563091,0.00316553,0.007822531,0.001077431,0.01447751,0.0002957377,0.002262236],"genre_scores_gemma":[0.9967912,0.00002270304,0.0008358649,0.00004053363,0.0003139657,3.587915e-7,0.000834815,0.00001024762,0.001150309],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.6066792,"threshold_uncertainty_score":0.6112136,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W4401057598","doi":"10.1007/s10236-024-01629-4","title":"Seasonal variation of chlorophyll-a in South Java over the past quarter-century","year":2024,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Climate variability and models","field":"Environmental Science","cited_by":8,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"Universitas Diponegoro","keywords":"Quarter (Canadian coin); Variation (astronomy); Java; Seasonality; Geology; Climatology; Oceanography; Geography; Astronomy; Archaeology; Statistics; Mathematics","retraction":null,"screen_n_in":null,"score":{"opus":0.005943122650882972,"gpt":0.2061962295081886,"spread":0.2002531068573056,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002953639,0.00008283565,0.00008207302,0.00002376033,0.00003474256,0.00003267603,0.0001462248,0.0000535744,0.0003747449],"category_scores_gemma":[0.00001225708,0.00006129162,0.0000508716,0.0002225192,0.00008976343,0.0001252244,0.0000902806,0.0001266205,0.00005482518],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0001949582,"about_ca_system_score_gemma":0.00001188563,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0001318888,"about_ca_topic_score_gemma":0.0001332494,"domain_scores_codex":[0.9992332,0.00003859638,0.0001710298,0.0002029446,0.0002039678,0.0001502454],"domain_scores_gemma":[0.9996696,0.00006815053,0.00003431231,0.000195512,0.00000341399,0.00002907531],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.00012192,0.0006605178,0.7716506,0.0003222337,0.00006537417,0.00002900292,0.04231097,0.1082667,0.001539483,0.06224128,0.001223842,0.01156804],"study_design_scores_gemma":[0.0001005818,0.00002257247,0.2408694,0.00001875798,0.00001042858,0.00000134047,0.000193486,0.7562684,0.00000144969,0.00209748,0.000343287,0.00007276138],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9958498,0.00002087938,0.001509042,0.0003199636,0.0001938954,0.0001226153,0.00007224749,0.00002313374,0.001888353],"genre_scores_gemma":[0.9996515,0.0000136984,0.0001220591,0.00005978213,0.00003182752,0.00000163609,0.00002356729,0.000009253838,0.00008669559],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.6480017,"threshold_uncertainty_score":0.4103194,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3022852959","doi":"10.1007/s10236-020-01375-3","title":"The impact of the planetary β-effect on the vertical structure of a coherent vortex in the South China Sea","year":2020,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"Dalhousie University","funders":"Shenzhen Peacock Plan; Natural Sciences and Engineering Research Council of Canada; National Key Research and Development Program of China; Ocean Frontier Institute","keywords":"Geology; Eddy; Mesoscale meteorology; Advection; Vortex; Anticyclone; Geophysics; Climatology; Mechanics; Turbulence; Physics","retraction":null,"screen_n_in":null,"score":{"opus":0.005285923961300625,"gpt":0.191398003724698,"spread":0.1861120797633974,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002422865,0.0001606005,0.0001799206,0.000005828928,0.0001790509,0.00003638339,0.0007970065,0.00005600518,0.0001077343],"category_scores_gemma":[0.0001371704,0.00005044926,0.0001453198,0.0004711685,0.0003055614,0.00003667774,0.00002356287,0.000370983,0.000002665164],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000004216503,"about_ca_system_score_gemma":0.0000709358,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0005661458,"about_ca_topic_score_gemma":0.0009048433,"domain_scores_codex":[0.9988559,0.0002446962,0.0002101991,0.0001503535,0.0003112801,0.0002275806],"domain_scores_gemma":[0.9989387,0.0006032408,0.00009563348,0.0002986859,0.00001445712,0.00004923514],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001509299,0.00001222002,0.9849824,0.00002636122,0.00004663918,0.00000244955,0.001066304,0.01095449,0.000003678644,0.0002694725,0.0002989063,0.002186186],"study_design_scores_gemma":[0.000143854,0.0004350948,0.8150226,0.00001944647,0.00002288921,0.00000393142,0.0004640695,0.1829845,0.00001555933,0.0008065146,0.00001795052,0.0000635694],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9971366,0.000242631,0.00001017088,0.001336318,0.00007149517,0.0003007138,0.0002859223,0.000008549539,0.0006075812],"genre_scores_gemma":[0.9996241,0.00002694436,0.000006448156,0.0002552398,0.00003990773,1.646487e-7,0.0000383812,0.000003865997,0.000004937333],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.17203,"threshold_uncertainty_score":0.2057261,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2147448537","doi":"10.1007/s10236-011-0386-7","title":"Decadal variability of the Arctic Ocean thermal structure","year":2011,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Climatology; Advection; Arctic; Ocean heat content; Canada Basin; Environmental science; Oceanic basin; Zonal and meridional; The arctic; Geology; Structural basin; North Atlantic oscillation; Sea surface temperature; Heat flux; Empirical orthogonal functions; Oceanography; Heat transfer","retraction":null,"screen_n_in":null,"score":{"opus":0.007423152678636817,"gpt":0.1743276081082149,"spread":0.1669044554295781,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000294517,0.0001732628,0.0001879501,0.00002972274,0.0001813636,0.00001402202,0.0005593654,0.0001108276,0.001466685],"category_scores_gemma":[0.0001007903,0.000110175,0.0001188744,0.0002168373,0.0003554445,0.0001354795,0.00004810749,0.000293464,0.000009271751],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001835982,"about_ca_system_score_gemma":0.00009779072,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001282816,"about_ca_topic_score_gemma":0.00103046,"domain_scores_codex":[0.9987636,0.0001281911,0.0002786382,0.0002429249,0.0002740401,0.0003125908],"domain_scores_gemma":[0.9990745,0.0001271868,0.000163438,0.0004717724,0.00007075937,0.00009234234],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00003422247,0.00002268939,0.9928219,0.00003571908,0.00002510985,0.000002530064,0.0006350888,0.0007084623,0.000002773735,0.002705487,0.00001746784,0.002988596],"study_design_scores_gemma":[0.0001448256,0.00005523074,0.9062636,0.00001601308,0.00004422553,0.00002376086,0.0003015509,0.08135916,0.00001698467,0.01159413,0.00003229644,0.0001482715],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9905851,0.000009426798,0.0004309139,0.00009520262,0.0004864278,0.0001493223,0.0002591504,0.00002685151,0.007957635],"genre_scores_gemma":[0.9978218,0.000005603989,0.001700318,0.0001721096,0.00005552996,3.694797e-8,0.00006134795,0.000007220588,0.0001760445],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.08655829,"threshold_uncertainty_score":0.9994461,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1775995791","doi":"10.1007/s10236-015-0877-z","title":"The implementation of sea ice model on a regional high-resolution scale","year":2015,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Centre For Cold Ocean Resources Engineering; Memorial University of Newfoundland","funders":"European Organization for the Exploitation of Meteorological Satellites; U.S. Department of Energy","keywords":"Sea ice; Satellite; Sea ice thickness; Sea ice concentration; Environmental science; Climatology; Radiometer; Remote sensing; Advanced very-high-resolution radiometer; Bay; Scale (ratio); Forcing (mathematics); Horizontal resolution; Meteorology; Geology; Arctic ice pack; Oceanography; Geography","retraction":null,"screen_n_in":null,"score":{"opus":0.01671951946660993,"gpt":0.2383992415500325,"spread":0.2216797220834226,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003253619,0.00009103042,0.00008887445,0.00003182775,0.0001832073,0.00002288831,0.0001745101,0.00004196002,0.00002326929],"category_scores_gemma":[0.00001544758,0.00006450045,0.00003955793,0.0001116643,0.0001173856,0.0001151893,0.00001222546,0.0001000093,0.00002314519],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00003061805,"about_ca_system_score_gemma":0.0001288634,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002402502,"about_ca_topic_score_gemma":0.005277109,"domain_scores_codex":[0.9990869,0.00004264154,0.0001850402,0.0001385941,0.0003408567,0.0002059914],"domain_scores_gemma":[0.999456,0.0000909698,0.0001131779,0.0001657229,0.00008257364,0.00009152648],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.0002353051,0.00005226627,0.5028763,0.00002347134,0.00004549936,0.000004261814,0.001214134,0.3781151,0.000001907442,0.02572022,0.005211724,0.08649976],"study_design_scores_gemma":[0.0002824483,0.0001277429,0.03742151,0.000006859225,0.00001408103,0.000006740122,0.002010582,0.9524553,0.000002450995,0.007423806,0.0001673424,0.00008110741],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.988625,0.00002116184,0.007438617,0.001411197,0.0001868127,0.0001249098,0.0002137597,0.00002303934,0.001955431],"genre_scores_gemma":[0.9967557,0.00004808082,0.002167045,0.0002191618,0.00004525776,2.748248e-7,0.0004556031,0.000003991437,0.0003049112],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.5743402,"threshold_uncertainty_score":0.363188,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1006495188","doi":"10.1007/s10236-015-0862-6","title":"Numerical study of seasonal circulation and variability over the inner shelf of the northern South China Sea","year":2015,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Dalhousie University","funders":"","keywords":"Climatology; Oceanography; Hydrography; Ocean current; Forcing (mathematics); Geology; Barotropic fluid; Baroclinity; Current (fluid); Monsoon; Circulation (fluid dynamics); Advection; Boundary current; Submarine pipeline; Environmental science","retraction":null,"screen_n_in":null,"score":{"opus":0.007049959422727313,"gpt":0.1910006918935143,"spread":0.183950732470787,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004355937,0.00008812683,0.0001304697,0.000005957203,0.000095427,0.00001603894,0.0002010031,0.0000359485,0.00003078305],"category_scores_gemma":[0.00009616141,0.00004556194,0.00003517146,0.0003508965,0.0002017926,0.00008022047,0.00002691626,0.0001057377,6.315345e-7],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000004425568,"about_ca_system_score_gemma":0.00007525274,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0008886264,"about_ca_topic_score_gemma":0.0007555758,"domain_scores_codex":[0.9991303,0.0001227347,0.0001709824,0.0001470263,0.0003098385,0.0001191192],"domain_scores_gemma":[0.9994636,0.00007346382,0.000133416,0.0002091696,0.00006693811,0.00005336779],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00002026762,0.0000591,0.9819734,0.00001452235,0.00001966718,2.523576e-7,0.001758959,0.01389519,7.283585e-8,0.00005194124,0.000008694868,0.002197944],"study_design_scores_gemma":[0.0001660831,0.00006313296,0.7264456,0.000003640029,0.00002026312,0.000001444741,0.0008640487,0.2714014,2.098509e-7,0.0009852084,0.000005879201,0.0000430913],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.998612,0.00005784042,0.0003841885,0.0000912752,0.00008866621,0.0001632592,0.00004860368,0.000009447534,0.0005447202],"genre_scores_gemma":[0.9998665,0.000001792115,0.00005527935,0.00002446926,0.00002334152,1.26276e-7,0.00001224765,0.000002707963,0.00001355266],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2575062,"threshold_uncertainty_score":0.1857962,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2015092975","doi":"10.1007/s10236-015-0827-9","title":"The international workshop on wave hindcasting and forecasting and the coastal hazards symposium","year":2015,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Ocean Waves and Remote Sensing","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Environment and Climate Change Canada","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Hindcast; Coastal hazards; Wind wave; Wave model; Natural hazard","retraction":null,"screen_n_in":null,"score":{"opus":0.02270109999977732,"gpt":0.2036679624863489,"spread":0.1809668624865716,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007136784,0.0001054744,0.00009926197,0.00002526596,0.0004007851,0.0003280576,0.000111271,0.00003949233,0.000002803979],"category_scores_gemma":[0.0002206741,0.00005368051,0.00002720668,0.00005990406,0.0002684728,0.00008329927,0.00005123004,0.0001883931,0.000002272969],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000006242066,"about_ca_system_score_gemma":0.00002805505,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0001949228,"about_ca_topic_score_gemma":0.001809287,"domain_scores_codex":[0.9991999,0.00005172885,0.0001519357,0.0001623415,0.0002371613,0.0001969168],"domain_scores_gemma":[0.9990551,0.0006184711,0.00008511883,0.0001024947,0.00004634717,0.00009240244],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.0006279141,0.00001051685,0.05450457,0.00001523312,0.00009454573,0.00006261092,0.002402436,0.01903841,0.000002136687,0.005178651,0.0009774436,0.9170855],"study_design_scores_gemma":[0.0004876081,0.00002938679,0.005067538,0.00003264495,0.000009041477,0.0001436423,0.001890762,0.9900267,8.550722e-7,0.001302538,0.0009257711,0.00008348125],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9582901,0.000208992,0.0001462003,0.005241917,0.0008598913,0.0001119771,0.00003064138,0.00002193488,0.03508837],"genre_scores_gemma":[0.9976999,0.000112147,0.0005771224,0.000227677,0.0002303523,4.536819e-9,0.00003489851,0.000005141469,0.001112749],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.9709883,"threshold_uncertainty_score":0.3163467,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1967644456","doi":"10.1007/s10236-010-0361-8","title":"Near-surface flow structure over wind-generated water waves, part I: wave-induced flow characteristics","year":2010,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Ocean Waves and Remote Sensing","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"Western University; Concordia University","funders":"Core Research for Evolutional Science and Technology; Natural Sciences and Engineering Research Council of Canada; Concordia University","keywords":"Momentum transfer; Fetch; Mechanics; Reynolds stress; Wind wave; Turbulence; Wind stress; Wave shoaling; Geology; Reynolds number; Surface wave; Airflow; Vorticity; Flow (mathematics); Breaking wave; Meteorology; Physics; Wave propagation; Atmospheric sciences; Vortex; Mechanical wave; Optics; Longitudinal wave; Geomorphology","retraction":null,"screen_n_in":null,"score":{"opus":0.007179335092076149,"gpt":0.1835126635600592,"spread":0.1763333284679831,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002044879,0.0004033981,0.0003724691,0.00003711483,0.0004826187,0.0003824519,0.0002486444,0.00039282,0.002137393],"category_scores_gemma":[0.00003132159,0.0002817882,0.0001146901,0.0001884434,0.0001463776,0.0002385706,0.00003966012,0.0008653877,0.0001479266],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001535724,"about_ca_system_score_gemma":0.00008585517,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0001902659,"about_ca_topic_score_gemma":0.001494736,"domain_scores_codex":[0.9978287,0.0000697732,0.0004056277,0.0005271314,0.0003881241,0.0007806158],"domain_scores_gemma":[0.9988955,0.00004307588,0.0001105075,0.0005243247,0.0001029845,0.0003236259],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.0005181286,0.0002505185,0.2715275,0.0003730485,0.000679173,0.001594882,0.004449133,0.2191071,0.05936711,0.0002398032,0.00949755,0.4323961],"study_design_scores_gemma":[0.0003020767,0.00006459952,0.06249097,0.00001733618,0.00003448306,0.00008419868,0.0000333419,0.9306296,0.0008787235,0.0001601783,0.004840924,0.0004636216],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9934803,0.00001524875,0.0000259629,0.0002906711,0.003977981,0.0001870914,0.0009303236,0.0001122034,0.0009801686],"genre_scores_gemma":[0.9853008,0.00001838847,0.008188643,0.0003441057,0.0007957249,1.780303e-9,0.004035792,0.00003272045,0.001283862],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.7115225,"threshold_uncertainty_score":0.9999634,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2047363835","doi":"10.1007/s10236-010-0266-6","title":"Assimilation of sea surface temperature into CECOM by flux correction","year":2010,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"","keywords":"Data assimilation; Sea surface temperature; Environmental science; Climatology; Thermal diffusivity; Meteorology; Geology; Physics","retraction":null,"screen_n_in":null,"score":{"opus":0.002173138259297708,"gpt":0.1785353956321753,"spread":0.1763622573728776,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001385215,0.0001163548,0.000128739,0.0000134908,0.0001322879,0.00004090154,0.0001514528,0.0001386279,0.0004824459],"category_scores_gemma":[0.00003979542,0.00009981602,0.00004173798,0.0003557482,0.00009278693,0.0002239376,0.000006586802,0.0002633398,0.00001390336],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000003452793,"about_ca_system_score_gemma":0.00004836123,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0005059125,"about_ca_topic_score_gemma":0.003711909,"domain_scores_codex":[0.999301,0.00001986871,0.000165787,0.0001795541,0.0001805945,0.0001531532],"domain_scores_gemma":[0.9995353,0.00006699105,0.0001044171,0.0001418621,0.00007591445,0.00007547565],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.00001254991,0.00001840471,0.9736444,0.00002452292,0.000009492622,7.174961e-7,0.00008575543,0.002282236,0.0003449984,0.00002324659,0.01050706,0.01304662],"study_design_scores_gemma":[0.0002300882,0.0001269787,0.3115203,0.00002078089,0.0000231669,0.00001372131,0.0003386261,0.6821024,0.001482473,0.0007063226,0.003151323,0.0002837895],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9936549,0.000105742,0.000319182,0.0001542148,0.001176271,0.00006996753,0.00009814509,0.00005790306,0.004363672],"genre_scores_gemma":[0.9956115,0.00004339756,0.002214695,0.0000627303,0.00005098616,4.281817e-8,0.0008293932,0.000004945645,0.001182314],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.6798202,"threshold_uncertainty_score":0.5282444,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null}]}