{"meta":{"query_hash":"03effbe7442d","filters":{"venue":"Geomagnetism and Aeronomy"},"cohort_total":12,"direct_labels_cover":0,"predictions_cover":12,"exported":12,"export_cap":100000,"truncated":false,"label_status":"direct model label, unvalidated","prediction_status":"machine_predicted_unvalidated (Codex and Gemma teacher distillation)","score_status":"score_only:v0-immature-baseline","snapshot":{"source":"OpenAlex, pinned release, all 482 partitions","release":"2026-06-24","frame_built":"2026-07-12"},"permalink":"https://metacan.xera.ac/q/03effbe7442d","api":"https://metacan.xera.ac/api/v1/cohort?venue=Geomagnetism+and+Aeronomy"},"results":[{"id":"W1988452198","doi":"10.1134/s0016793206020186","title":"What is the cause of the accelerated drift of the north magnetic pole: Jerk or reversal?","year":2006,"lang":"en","type":"article","venue":"Geomagnetism and Aeronomy","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Bayer Canada","keywords":"Jerk; Earth's magnetic field; Acceleration; Geodesy; Physics; Stochastic drift; Northern Hemisphere; Geology; Magnetic field; Geomagnetic reversal; Position (finance); Southern Hemisphere; Geomagnetic pole; Geophysics; Atmospheric sciences; Classical mechanics; Astronomy; Mathematics","score_opus":0.009539310209642105,"score_gpt":0.20889635893672062,"score_spread":0.19935704872707852,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1988452198","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.68269557,0.20433098,0.02229604,0.036165778,0.008555259,0.0003606803,0.0034415163,0.00082186505,0.041332357],"genre_scores_gemma":[0.9449759,0.034912087,0.0032551987,0.0019373995,0.0042291665,0.00004825801,0.0010846208,0.00010648414,0.009450722],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99938333,0.00009630773,0.00007140934,0.00022020958,0.00010656005,0.00012220725],"domain_scores_gemma":[0.9974165,0.00047261114,0.0010515439,0.000111040325,0.00072396686,0.00022426569],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012505662,0.0006204604,0.0015176327,0.0017773533,0.00068452646,0.002236516,0.0010184064,0.0016656949,0.0066467086],"category_scores_gemma":[0.004264469,0.0004133374,0.0007234759,0.0014684169,0.0020567754,0.0020298432,0.0005468563,0.0008089515,0.0021210082],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012317108,0.0002954585,0.57596105,0.008599264,0.001073227,0.009301183,0.0036729206,0.002943918,0.02220899,0.01348191,0.01849723,0.34273317],"study_design_scores_gemma":[0.00011025661,0.00046420388,0.897588,0.0010345938,0.00026957836,0.010419985,0.010299345,0.0032056838,0.0033145573,0.0125264255,0.06055257,0.00021468716],"about_ca_topic_score_codex":0.004633451,"about_ca_topic_score_gemma":0.0033745416,"teacher_disagreement_score":0.0066467086,"about_ca_system_score_codex":0.0008101441,"about_ca_system_score_gemma":0.0007444258,"threshold_uncertainty_score":0.022235513},"labels":[],"label_agreement":null},{"id":"W2044107334","doi":"10.1134/s0016793214020121","title":"Features of poleward expansion of the outer radiation belt during magnetospheric substorms","year":2014,"lang":"en","type":"article","venue":"Geomagnetism and Aeronomy","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Space Agency","keywords":"Substorm; Geophysics; Magnetosphere; Physics; Latitude; Van Allen radiation belt; Polar; Electron; Ionosphere; Geology; Atmospheric sciences; Plasma; Astronomy","score_opus":0.002008577906996888,"score_gpt":0.17022820574632197,"score_spread":0.1682196278393251,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2044107334","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9947137,0.0005525045,0.0010456146,0.000030518524,0.000007835669,0.0000125438455,0.00018830605,0.00005202076,0.0033969565],"genre_scores_gemma":[0.99930274,0.000096153875,0.00016244026,0.0000052167215,0.000011795673,0.0000044016633,0.0001740013,0.0000060481966,0.00023714168],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999453,0.000008103792,0.000003610331,0.000013448938,0.000011162189,0.000018413557],"domain_scores_gemma":[0.99960226,0.00009330529,0.0001683615,0.000034946734,0.000048641876,0.00005251712],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011745258,0.00012712071,0.00015632482,0.0009512705,0.0002443919,0.00031112172,0.00016356527,0.00019138274,0.0011278173],"category_scores_gemma":[0.00068609917,0.00008178047,0.00010925158,0.0006498818,0.00034191413,0.00019717262,0.00027909462,0.00015480617,0.0001791492],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018580601,0.000100435434,0.7374087,0.00018550722,0.000099623336,0.009546258,0.0027515767,0.0016011912,0.1852055,0.002594677,0.0015154729,0.057133045],"study_design_scores_gemma":[0.000008427583,0.00007218569,0.99280727,0.000010625388,0.00001900459,0.002809058,0.00022211297,0.00073061604,0.0015926855,0.00033417708,0.0013863752,0.000007433991],"about_ca_topic_score_codex":0.0008425725,"about_ca_topic_score_gemma":0.00096202875,"teacher_disagreement_score":0.0011278173,"about_ca_system_score_codex":0.00011068925,"about_ca_system_score_gemma":0.000056141205,"threshold_uncertainty_score":0.0037729144},"labels":[],"label_agreement":null},{"id":"W2046012261","doi":"10.1134/s0016793209070342","title":"Ozone content of the atmosphere. 3. Statistics of extreme values of the total ozone content in the midlatitude atmosphere","year":2009,"lang":"en","type":"article","venue":"Geomagnetism and Aeronomy","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Middle latitudes; Atmosphere (unit); Atmospheric sciences; Environmental science; Ozone; Satellite; Latitude; Content (measure theory); CO2 content; Climatology; Meteorology; Geology; Geography; Carbon dioxide; Chemistry; Physics; Mathematics; Astronomy","score_opus":0.02847591995077752,"score_gpt":0.19965114648919172,"score_spread":0.1711752265384142,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2046012261","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98574126,0.00028155884,0.00057498814,0.000017339351,0.000004768139,0.000007655687,0.011775272,0.00004732534,0.0015497763],"genre_scores_gemma":[0.991232,0.00008225127,0.0003075272,0.000007052396,0.0000038456888,0.000008371247,0.007900886,0.0000042752313,0.00045373978],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991715,0.000009381492,0.000010043509,0.00001959897,0.000021626598,0.000022318227],"domain_scores_gemma":[0.9995808,0.00008851605,0.00017336637,0.00003020391,0.00007542122,0.00005166287],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012335976,0.00012957683,0.00013686827,0.0010722762,0.000120290664,0.00019038683,0.00013589826,0.000094322655,0.0017260844],"category_scores_gemma":[0.00055438,0.000060786144,0.00015566112,0.00079091283,0.00007828694,0.00010118858,0.00018168763,0.00014641174,0.00020660127],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032143903,0.000021743732,0.96512145,0.00006865581,0.0001486263,0.00013746788,0.00010972015,0.0009143133,0.019168774,0.0002359424,0.001059617,0.012692198],"study_design_scores_gemma":[0.0000012277943,0.000016806423,0.9981072,0.0000021415624,0.0000070872393,0.000089938025,0.000026469912,0.00023158596,0.0008577978,0.000026215499,0.0006320424,0.0000015411892],"about_ca_topic_score_codex":0.008782188,"about_ca_topic_score_gemma":0.011351371,"teacher_disagreement_score":0.008782188,"about_ca_system_score_codex":0.00022673834,"about_ca_system_score_gemma":0.00013665987,"threshold_uncertainty_score":0.017462134},"labels":[],"label_agreement":null},{"id":"W2076612661","doi":"10.1134/s0016793206030091","title":"The ionosphere of Europe and North America before the magnetic storm of October 28, 2003","year":2006,"lang":"en","type":"article","venue":"Geomagnetism and Aeronomy","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Geomagnetic storm; Ionosphere; Storm; Substorm; Middle latitudes; Atmospheric sciences; Flare; Latitude; Solar flare; Critical frequency; Environmental science; Climatology; Earth's magnetic field; Geology; Meteorology; Physics; Geophysics; Astrophysics; Magnetosphere; Geodesy; Magnetic field","score_opus":0.002314057986348921,"score_gpt":0.16547957420584763,"score_spread":0.1631655162194987,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076612661","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99528426,0.00056050223,0.00006820059,0.000034947185,0.000005713481,0.00000377417,0.00051970896,0.000006028329,0.0035169376],"genre_scores_gemma":[0.99782616,0.00036863537,0.00012629856,0.000025929156,0.000005334189,0.0000044562444,0.00093443383,0.0000028827128,0.000705816],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993396,0.0000088643255,0.0000033963959,0.000020684845,0.000010144794,0.000022978635],"domain_scores_gemma":[0.99986684,0.000015414618,0.00004486353,0.000011155079,0.00003925996,0.000022561682],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001125728,0.000121509554,0.0001588813,0.00035679404,0.0002846414,0.0005768646,0.00007886548,0.00014749363,0.0011694077],"category_scores_gemma":[0.00024555178,0.0000560368,0.00009019056,0.0005881456,0.0001075787,0.0002380775,0.00025997468,0.000084858526,0.00018618192],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006926688,0.00003409302,0.9612075,0.00004530197,0.00010109341,0.00043180824,0.0010658673,0.0005793171,0.015078389,0.00018124712,0.0010647635,0.019517928],"study_design_scores_gemma":[0.000003781395,0.000017599928,0.99722004,0.000006321169,0.000008889199,0.000060441827,0.0002893576,0.00005602305,0.00021460761,0.000014552401,0.0021070025,0.0000013268858],"about_ca_topic_score_codex":0.0263808,"about_ca_topic_score_gemma":0.04277044,"teacher_disagreement_score":0.0263808,"about_ca_system_score_codex":0.0003097842,"about_ca_system_score_gemma":0.0002890823,"threshold_uncertainty_score":0.05245453},"labels":[],"label_agreement":null},{"id":"W2089734624","doi":"10.1134/s0016793215010107","title":"On the magnetic precursor of the Chilean earthquake of February 27, 2010","year":2015,"lang":"en","type":"article","venue":"Geomagnetism and Aeronomy","topic":"Earthquake Detection and Analysis","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Substorm; Earth's magnetic field; Disturbance (geology); Geology; Geophysics; Seismology; Photometer; Ionosphere; Geomagnetic storm; Geodesy; Magnetosphere; Physics; Magnetic field; Astronomy; Paleontology","score_opus":0.01307742802964933,"score_gpt":0.1759632122346846,"score_spread":0.16288578420503527,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2089734624","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9827288,0.0013774838,0.00047160377,0.00041276778,0.000044532622,0.000037253885,0.001980695,0.00003461064,0.0129122855],"genre_scores_gemma":[0.99191064,0.0014029281,0.00044890505,0.00006681553,0.00008350214,0.000018840545,0.002356396,0.000011908436,0.003700071],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999207,0.000010770404,0.0000047602603,0.000013095354,0.000026808546,0.00002381847],"domain_scores_gemma":[0.99943584,0.0001093242,0.00017406348,0.000029425108,0.00019113596,0.000060185368],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017265699,0.00011526297,0.000115000024,0.0010834396,0.0003663242,0.0003088809,0.00014673431,0.00015669074,0.001698327],"category_scores_gemma":[0.00091685343,0.00006802834,0.000073029965,0.0013356507,0.00021305752,0.00014944644,0.00035125323,0.00021270757,0.00034868153],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005229846,0.00009362305,0.8535769,0.00042394854,0.00005805763,0.007426368,0.0039252643,0.0012191171,0.027198361,0.001364512,0.008217246,0.09597358],"study_design_scores_gemma":[0.0000054101038,0.00003097568,0.98344064,0.00004426128,0.0000134619795,0.00039464698,0.00084849814,0.00028701377,0.0017254339,0.000100856574,0.013102483,0.0000062778413],"about_ca_topic_score_codex":0.027734336,"about_ca_topic_score_gemma":0.05848184,"teacher_disagreement_score":0.027734336,"about_ca_system_score_codex":0.0005370224,"about_ca_system_score_gemma":0.0007461925,"threshold_uncertainty_score":0.0551458},"labels":[],"label_agreement":null},{"id":"W2135819168","doi":"10.1134/s001679320904001x","title":"Studying correlations between the coronal hole area, solar wind velocity, and local magnetic indices in the Canadian region during the decline phase of cycle 23","year":2009,"lang":"en","type":"article","venue":"Geomagnetism and Aeronomy","topic":"Solar and Space Plasma Dynamics","field":"Physics and Astronomy","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Solar wind; Coronal hole; Earth's magnetic field; Physics; Coronal mass ejection; Atmospheric sciences; Solar cycle; Solar minimum; Ionosphere; Geophysics; Plasma; Magnetic field","score_opus":0.01236181199834769,"score_gpt":0.23267024550192386,"score_spread":0.22030843350357618,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2135819168","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99802005,0.00017393578,0.00013783449,0.000016100943,0.0000024798876,0.000007868314,0.00048817217,0.0000049497735,0.0011485659],"genre_scores_gemma":[0.9987796,0.00008893194,0.00013970585,0.0000029951395,0.0000012831762,0.0000025864717,0.00054728385,0.0000019751594,0.00043568658],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998128,0.000014170894,0.000005982268,0.000037875496,0.00006615533,0.000063086314],"domain_scores_gemma":[0.99939287,0.00007804037,0.00008742233,0.000020383302,0.00031420024,0.00010708143],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029617472,0.00022658058,0.00025897348,0.0013366822,0.0007671392,0.0006002277,0.00029839965,0.00012847569,0.0009355855],"category_scores_gemma":[0.0011878161,0.00011655289,0.00017979846,0.002397261,0.00033370798,0.00012841493,0.00030812208,0.000149737,0.00008476997],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000080759455,0.0000086550945,0.98982924,0.000019191968,0.00006036991,0.00007163794,0.00041500342,0.00054121204,0.0013008786,0.0001573928,0.0002671733,0.0072484394],"study_design_scores_gemma":[8.192179e-7,0.0000044222857,0.9991953,0.0000019797444,0.0000065077766,0.000012641753,0.00018442128,0.00022415243,0.000059538474,0.0000065318327,0.0003017515,0.0000020936507],"about_ca_topic_score_codex":0.9536778,"about_ca_topic_score_gemma":0.98158133,"teacher_disagreement_score":0.046322227,"about_ca_system_score_codex":0.003973187,"about_ca_system_score_gemma":0.005403596,"threshold_uncertainty_score":0.093190014},"labels":[],"label_agreement":null},{"id":"W2136782024","doi":"10.1134/s0016793209040057","title":"Burst regimes of long-period irregular pulsations at frequencies of 2.0–6.0 mHz and substorm activity in the nightside magnetosphere","year":2009,"lang":"en","type":"article","venue":"Geomagnetism and Aeronomy","topic":"Earthquake Detection and Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Resources Canada","keywords":"Substorm; Magnetosphere; Physics; Geophysics; Astrophysics; Amplitude; Solar wind; Cusp (singularity); Plasma sheet; Magnetosheath; Magnetic field; Magnetopause","score_opus":0.007406161760001499,"score_gpt":0.18614865286650098,"score_spread":0.17874249110649948,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2136782024","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989587,0.00007476931,0.00018559754,0.0000055284677,0.0000014291811,0.0000044036997,0.00023204651,0.000009491449,0.00052805204],"genre_scores_gemma":[0.99876654,0.000047597812,0.00019848051,0.0000044550025,0.000009337584,0.000007408436,0.0007479195,0.000004801669,0.00021343032],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998816,0.000013516704,0.00000838257,0.0000354705,0.000028730612,0.000032317887],"domain_scores_gemma":[0.99947816,0.000078644385,0.00022593696,0.00005732894,0.00006329615,0.00009674329],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017153687,0.00016947345,0.00021111622,0.00091136893,0.00017346391,0.00022651903,0.00011294268,0.00016828779,0.0008620236],"category_scores_gemma":[0.00037777115,0.00012323889,0.00018109492,0.00064120855,0.00018665561,0.00016727413,0.00032331102,0.00014035989,0.00018460634],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00094015425,0.00008140086,0.8741497,0.000064728505,0.00009095023,0.0004537604,0.0007524477,0.0005622198,0.104286924,0.00009701215,0.00024981648,0.01827092],"study_design_scores_gemma":[0.000002287603,0.000041403728,0.9985788,0.0000015020019,0.0000048778793,0.00013859593,0.000037453556,0.00016334938,0.0008638937,0.000013106085,0.00015243387,0.000002220564],"about_ca_topic_score_codex":0.0009502812,"about_ca_topic_score_gemma":0.0009693524,"teacher_disagreement_score":0.0009502812,"about_ca_system_score_codex":0.0001230124,"about_ca_system_score_gemma":0.00006658534,"threshold_uncertainty_score":0.002883792},"labels":[],"label_agreement":null},{"id":"W2346038752","doi":"10.1134/s0016793216010096","title":"Peculiarities of the azimuthal propagation of perturbations in discrete auroral arcs during the substorm growth phase","year":2016,"lang":"en","type":"article","venue":"Geomagnetism and Aeronomy","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Substorm; Azimuth; Geophysics; Phase (matter); Physics; Ionosphere; Computational physics; Geology; Magnetosphere; Plasma; Optics","score_opus":0.003470476246397192,"score_gpt":0.19538043235340521,"score_spread":0.19190995610700803,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2346038752","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99817467,0.00006967497,0.0006441301,0.0000110645105,0.000001809725,0.000004639355,0.00014023563,0.000018444694,0.00093523326],"genre_scores_gemma":[0.99970007,0.000029839988,0.0001122569,0.0000010681056,0.0000019010033,0.0000013016241,0.000079506244,0.0000017269097,0.00007239209],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999602,0.0000054912,0.0000021641815,0.000010747619,0.000011496101,0.000010035382],"domain_scores_gemma":[0.999566,0.0000864366,0.0001703461,0.000028878812,0.00008898177,0.000059228412],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012358463,0.00010851627,0.00007167486,0.00061838416,0.00018286251,0.0002053154,0.00010063154,0.000093094335,0.000443903],"category_scores_gemma":[0.0006049642,0.00007125602,0.0000735165,0.00046863355,0.00020656681,0.00013319806,0.00017905905,0.00012643551,0.00006848345],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003047774,0.000023284705,0.9247036,0.000030403728,0.000037969916,0.00033869402,0.0005671614,0.0021882649,0.05138245,0.0003996868,0.00017771202,0.019846028],"study_design_scores_gemma":[0.0000017944653,0.000015971673,0.99801373,0.0000013795907,0.000004983072,0.00006391717,0.000052251817,0.0009473965,0.0007452444,0.000028018436,0.00012338262,0.0000019510303],"about_ca_topic_score_codex":0.008528958,"about_ca_topic_score_gemma":0.010509125,"teacher_disagreement_score":0.008528958,"about_ca_system_score_codex":0.0002142766,"about_ca_system_score_gemma":0.000106999134,"threshold_uncertainty_score":0.016958594},"labels":[],"label_agreement":null},{"id":"W2808265507","doi":"10.1134/s001679321803009x","title":"Periodic Restructuring of Auroral Arcs as an Indicator of Alfvén Resonance in the Region of Substorm Onset","year":2018,"lang":"en","type":"article","venue":"Geomagnetism and Aeronomy","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Russian Academy of Sciences","keywords":"Substorm; Ionosphere; Resonance (particle physics); Geophysics; Physics; Alfvén wave; Magnetosphere; Oscillation (cell signaling); Satellite; Astrophysics; Atmospheric sciences; Magnetic field; Atomic physics; Astronomy; Magnetohydrodynamics","score_opus":0.006547922812953857,"score_gpt":0.21954120410905492,"score_spread":0.21299328129610107,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2808265507","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983467,0.00009364637,0.0004307655,0.00000766797,0.0000019047425,0.00000879991,0.000098280674,0.000020389265,0.0009918369],"genre_scores_gemma":[0.99948776,0.000041629606,0.00023263018,0.000004419646,0.000003920424,0.000005177952,0.000118365744,0.000003275578,0.000102780774],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999348,0.000010121495,0.000006308406,0.000016238953,0.000010497423,0.00002199944],"domain_scores_gemma":[0.99954504,0.00008301356,0.00020444649,0.000035500918,0.0000474602,0.000084472966],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017558126,0.00011180128,0.00011775548,0.00074542384,0.00020896993,0.00034988063,0.00011916815,0.00016159279,0.00077723304],"category_scores_gemma":[0.0004939274,0.000078898505,0.00009337503,0.00043171772,0.00023255331,0.00021408097,0.00037028827,0.00019284802,0.000114306444],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008000007,0.00005333567,0.7433298,0.000069858805,0.000033470642,0.0007245772,0.0011603661,0.00042702464,0.24041218,0.00022837069,0.00015468405,0.012606296],"study_design_scores_gemma":[0.0000024277924,0.000045372948,0.99656385,0.0000023651382,0.0000056432095,0.000110381516,0.00013181301,0.00026916253,0.002673102,0.000027734339,0.00016646381,0.0000016727271],"about_ca_topic_score_codex":0.0021290379,"about_ca_topic_score_gemma":0.003361067,"teacher_disagreement_score":0.0021290379,"about_ca_system_score_codex":0.00016083909,"about_ca_system_score_gemma":0.00010943301,"threshold_uncertainty_score":0.004233241},"labels":[],"label_agreement":null},{"id":"W3010644958","doi":"10.1134/s0016793219080048","title":"Rhythms of Banded Glacial Clays of the Paleoproterozoic (~2 Ga Ago) and Modern Cycles of Solar Activity","year":2019,"lang":"en","type":"article","venue":"Geomagnetism and Aeronomy","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Glacial period; Geology; Earth science; Geochemistry; Astrobiology; Geophysics; Paleontology; Physics","score_opus":0.008477409025825357,"score_gpt":0.17059632155647933,"score_spread":0.16211891253065397,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3010644958","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99885345,0.00007893031,0.000071419076,0.000008235157,0.0000017793972,0.000002047519,0.00052857626,0.0000045872553,0.00045094313],"genre_scores_gemma":[0.99893886,0.000041695406,0.00008342545,0.0000022286306,0.0000023899456,0.0000019388285,0.0006874469,0.0000023160017,0.00023975933],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999465,0.0000053899626,0.0000057829275,0.00001611895,0.000011884643,0.000014242053],"domain_scores_gemma":[0.9996829,0.000033556975,0.000120997836,0.000019291518,0.00008420501,0.00005905338],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020504267,0.00014705394,0.00014081647,0.0017955832,0.00027374463,0.00039111546,0.000148846,0.00015695077,0.0010639871],"category_scores_gemma":[0.00043298464,0.00010585357,0.00011343474,0.001504208,0.00038909834,0.00016743116,0.0003454804,0.00013942028,0.00014978583],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018013452,0.000014979325,0.97322863,0.00004267925,0.000060057984,0.00014667322,0.0009365764,0.00032383116,0.019333947,0.00022318505,0.00018580422,0.005323383],"study_design_scores_gemma":[8.414673e-7,0.0000033022125,0.99961144,0.0000011178417,0.0000019829067,0.000018248056,0.000041801584,0.00005109543,0.000098858465,0.0000056138356,0.00016486965,8.1481926e-7],"about_ca_topic_score_codex":0.029499892,"about_ca_topic_score_gemma":0.089683436,"teacher_disagreement_score":0.029499892,"about_ca_system_score_codex":0.0005074254,"about_ca_system_score_gemma":0.0002587785,"threshold_uncertainty_score":0.058656335},"labels":[],"label_agreement":null},{"id":"W4318714268","doi":"10.1134/s0016793222080138","title":"Analysis of Ionospheric TEC Variations Due to X, M & C Class Solar Flares during the Years 2003 to 2018 and Comparison with IRI Models","year":2022,"lang":"en","type":"article","venue":"Geomagnetism and Aeronomy","topic":"Solar and Space Plasma Dynamics","field":"Physics and Astronomy","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Trinity College","funders":"","keywords":"TEC; Ionosphere; Solar flare; Sunspot; Physics; Atmospheric sciences; Geology; Meteorology; Geophysics; Geodesy; Astrophysics; Magnetic field","score_opus":0.006638150854448016,"score_gpt":0.20578026200500255,"score_spread":0.19914211115055452,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4318714268","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957962,0.00008661731,0.0005480478,0.0000406253,0.000013698903,0.0000067602496,0.0019483468,0.00012678762,0.0014329504],"genre_scores_gemma":[0.99747735,0.00004555821,0.00016309733,0.000007936469,0.0000062736376,0.000004156103,0.0021000803,0.000011937754,0.00018362148],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989855,0.000008607123,0.0000090834465,0.000029052671,0.000028571336,0.000026078931],"domain_scores_gemma":[0.9997776,0.000048316255,0.000052839845,0.00002640238,0.000073069,0.000021809621],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023496662,0.0003051019,0.0002281031,0.0007357653,0.00021581666,0.00045232795,0.00030030328,0.00031073458,0.0005899407],"category_scores_gemma":[0.0005795131,0.00009580595,0.00045325764,0.0010122885,0.00012411608,0.00024397865,0.00019155272,0.00022837774,0.00017808645],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00085130555,0.00013952964,0.7418185,0.00017107565,0.00034113752,0.0010380168,0.000466701,0.19278578,0.019476388,0.00042169797,0.004714893,0.03777486],"study_design_scores_gemma":[0.000022136555,0.00012414789,0.8581811,0.000020092613,0.00009176433,0.0003057364,0.00030757417,0.13326764,0.0052137855,0.00012822638,0.0023071617,0.00003067778],"about_ca_topic_score_codex":0.027049765,"about_ca_topic_score_gemma":0.020930773,"teacher_disagreement_score":0.027049765,"about_ca_system_score_codex":0.0004401644,"about_ca_system_score_gemma":0.00019773874,"threshold_uncertainty_score":0.05378467},"labels":[],"label_agreement":null},{"id":"W4392792925","doi":"10.1134/s0016793223600601","title":"Performance Analysis of NeQuick-G, IRI-2016, IRI-Plas 2017 and AfriTEC Models over the African Region during the Geomagnetic Storm of March 2015","year":2023,"lang":"en","type":"article","venue":"Geomagnetism and Aeronomy","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Geomagnetic storm; Earth's magnetic field; Meteorology; Storm; Environmental science; Physics; Magnetic field","score_opus":0.009310628076395547,"score_gpt":0.2121491137593444,"score_spread":0.20283848568294885,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392792925","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9937209,0.00022218002,0.0021804783,0.00019392346,0.000032551645,0.000020085114,0.0007454288,0.00032496854,0.0025595517],"genre_scores_gemma":[0.9974356,0.000061094,0.0011211565,0.000022545126,0.000007753599,0.000015386026,0.0008674895,0.000034998524,0.00043396876],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998591,0.000041236395,0.000009120987,0.000036059548,0.000022671422,0.00003178277],"domain_scores_gemma":[0.99952507,0.00018595885,0.00005727496,0.000039990395,0.00013280555,0.00005880119],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00069585483,0.00097313337,0.0006602904,0.0003457161,0.0003893499,0.000734394,0.00090862386,0.0009274133,0.0011456284],"category_scores_gemma":[0.0014849048,0.00028280145,0.000757765,0.00034082035,0.00027692303,0.0004490934,0.000442162,0.00061402086,0.00028140665],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018781866,0.00006563864,0.01868492,0.00003784275,0.000080200945,0.000061392464,0.0000368126,0.9753268,0.0011600115,0.00016284683,0.00047704283,0.0037187955],"study_design_scores_gemma":[0.000037401885,0.000060784278,0.0060570952,0.000010401056,0.000027820843,0.000011887886,0.000041393676,0.99275756,0.00066040107,0.00006287439,0.0002631841,0.000009297527],"about_ca_topic_score_codex":0.10298086,"about_ca_topic_score_gemma":0.047160175,"teacher_disagreement_score":0.10298086,"about_ca_system_score_codex":0.0010450593,"about_ca_system_score_gemma":0.0011364325,"threshold_uncertainty_score":0.20476288},"labels":[],"label_agreement":null}]}