{"meta":{"query_hash":"36e2b3097c45","filters":{"venue":"Geografiska Annaler Series A Physical Geography"},"cohort_total":34,"direct_labels_cover":0,"predictions_cover":34,"exported":34,"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/36e2b3097c45","api":"https://metacan.xera.ac/api/v1/cohort?venue=Geografiska+Annaler+Series+A+Physical+Geography"},"results":[{"id":"W1489992383","doi":"10.1111/geoa.12033","title":"Recent developments in the analysis of the black mat layer and cosmic impact at 12.8 ka","year":2013,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Laurentian University; York University","funders":"","keywords":"Geology; Glacial period; Younger Dryas; Asteroid; Paleontology; Earth science; Astrobiology; Physics","score_opus":0.01735521785002474,"score_gpt":0.24728433654562387,"score_spread":0.22992911869559912,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1489992383","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99474627,0.0004664791,3.0924906e-7,0.0017582698,0.000050226365,0.00037112055,0.000052112322,0.000012133051,0.0025430573],"genre_scores_gemma":[0.9986415,0.00066240376,0.000024713014,0.0004221044,0.000017233122,0.000014421165,0.00009858772,0.0000031244408,0.00011592215],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99801797,0.00041731092,0.00027061786,0.00033540037,0.0003747812,0.00058391155],"domain_scores_gemma":[0.9990192,0.0003010067,0.00011315809,0.0003680926,0.0000889327,0.00010957706],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00030597244,0.00022159015,0.00040924913,0.00031016103,0.0002851038,0.000054215136,0.0005143251,0.000101085956,0.0009938885],"category_scores_gemma":[0.000028546614,0.00010406117,0.00031441895,0.0020425282,0.0011221404,0.00020298337,0.0000938844,0.00032483978,0.00011001593],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007359066,0.0000622921,0.99451625,0.000011995587,0.00045167917,0.000003563315,0.0009838003,0.0003404036,0.000011931455,0.000015560603,0.00045168767,0.003077269],"study_design_scores_gemma":[0.00019461113,0.00010369097,0.9954484,0.0000072932976,0.00013731525,0.000010583945,0.00031690195,0.0005991534,0.000028117713,0.0008429043,0.002170516,0.00014048822],"about_ca_topic_score_codex":0.0012409557,"about_ca_topic_score_gemma":0.008601287,"teacher_disagreement_score":0.0073603317,"about_ca_system_score_codex":0.000001472482,"about_ca_system_score_gemma":0.0000276976,"threshold_uncertainty_score":0.99991935},"labels":[],"label_agreement":null},{"id":"W1502641253","doi":"10.1111/geoa.12035","title":"Using earthquakes to assess lichen growth rates","year":2013,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Lichen and fungal ecology","field":"Agricultural and Biological Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"McGill University","keywords":"Archaeology; Lichen; Geography; Environmental science; Library science; History; Geology; Computer science; Ecology; Biology","score_opus":0.04263956863560472,"score_gpt":0.25825251205109107,"score_spread":0.21561294341548634,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1502641253","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9926866,0.000062436084,0.000009845288,0.004903834,0.00018306026,0.00051715865,0.00004498205,0.00020268756,0.0013893952],"genre_scores_gemma":[0.99600875,0.000021622172,0.00064259203,0.002067859,0.00076030043,0.0001528851,0.00005561284,0.000004675837,0.00028570966],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99779886,0.00013769051,0.00028497668,0.0006051572,0.00031540613,0.0008579058],"domain_scores_gemma":[0.9987954,0.00018566936,0.00009738708,0.00013722903,0.0003384512,0.00044587324],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000106027146,0.0003637296,0.0004415309,0.00006323673,0.00042030148,0.00030252873,0.00047697528,0.00013949416,0.0008446324],"category_scores_gemma":[0.00005125181,0.00014255408,0.000394475,0.0013581017,0.00021297166,0.00062976533,0.00024364733,0.0002458623,0.00050329557],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013825948,0.0010368433,0.5142367,0.000040377647,0.00028082056,0.00001598896,0.00067035673,0.000035975954,0.43199447,0.0026522875,0.006629618,0.04226832],"study_design_scores_gemma":[0.00013086198,0.0006862856,0.96029586,0.000015763944,0.000035237514,0.000007738366,0.00047318422,0.00013393076,0.005106691,0.0048704753,0.02768252,0.0005614597],"about_ca_topic_score_codex":0.0013212449,"about_ca_topic_score_gemma":0.00027464624,"teacher_disagreement_score":0.44605917,"about_ca_system_score_codex":0.000008912129,"about_ca_system_score_gemma":0.000009412151,"threshold_uncertainty_score":0.9248132},"labels":[],"label_agreement":null},{"id":"W1537328901","doi":"10.1111/j.1468-0459.2012.00463.x","title":"The dendroclimatological potential of an alpine shrub, cassiope mertensiana, from mount rainier, wa, usa","year":2012,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Tree-ring climate responses","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Park Service; University of Vermont; Office of Experimental Program to Stimulate Competitive Research; Oregon State University; Washington State University","keywords":"Transect; Growing season; Environmental science; National park; Snowpack; Shrub; Ecosystem; Physical geography; Dendroclimatology; Climate change; Annual plant; Precipitation; Ecology; Geography; Biology","score_opus":0.01384375142724265,"score_gpt":0.23217708991247715,"score_spread":0.2183333384852345,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1537328901","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99516696,0.0020129676,0.000022984172,0.0007214221,0.00056586805,0.00025644555,0.0005426324,0.00011833971,0.0005923886],"genre_scores_gemma":[0.9976178,0.00042775043,0.0008043248,0.00021147163,0.00054499804,0.000010808368,0.00031442565,0.000017179826,0.00005124441],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99633145,0.00044851672,0.00054172607,0.0005612843,0.0008053834,0.0013116222],"domain_scores_gemma":[0.997695,0.00053139246,0.00027655243,0.00075446547,0.00015138614,0.0005911764],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00037810477,0.00047159602,0.0006612344,0.00017125945,0.0007310992,0.00017702348,0.00077466643,0.00016761206,0.00076281856],"category_scores_gemma":[0.000097041455,0.00027341722,0.0005496788,0.0007673112,0.0011846119,0.0009412201,0.00011193667,0.0004062955,0.00022690496],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014639733,0.0005486045,0.9369104,0.000030089324,0.00038382132,0.00007772431,0.0005502913,0.00033643233,0.0010831583,0.0003968523,0.0003572735,0.057861406],"study_design_scores_gemma":[0.00039269342,0.00053643197,0.9762524,0.000019958145,0.00012900334,0.00006432039,0.00063867966,0.0012934747,0.00052053394,0.0008995151,0.01883513,0.000417894],"about_ca_topic_score_codex":0.005047634,"about_ca_topic_score_gemma":0.0019595502,"teacher_disagreement_score":0.05744351,"about_ca_system_score_codex":0.000004430935,"about_ca_system_score_gemma":0.000036878093,"threshold_uncertainty_score":0.9999718},"labels":[],"label_agreement":null},{"id":"W1560590698","doi":"10.1111/geoa.12074","title":"Holocene soils/paleosols in the okstindan mountains, nordland: stratigraphy and extractable fe and al","year":2014,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McMaster University; York University","funders":"Brock University; York University","keywords":"Paleosol; Geology; Soil water; Gleysol; Geochemistry; Weathering; Ammonium oxalate; Vegetation (pathology); Holocene; Pedogenesis; Chronosequence; Physical geography; Soil science; Paleontology; Chemistry; Geography","score_opus":0.009401332957603542,"score_gpt":0.22809565679310218,"score_spread":0.21869432383549864,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1560590698","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9905698,0.0012572092,0.000009497083,0.0029731854,0.00006959732,0.0003001077,0.000044396696,0.000046397214,0.004729819],"genre_scores_gemma":[0.9978154,0.0005439395,0.00016764965,0.0012021445,0.00010691519,0.000018502426,0.000108637956,0.000005780982,0.000031084837],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99743354,0.0004880012,0.00026859017,0.00059403817,0.00035221133,0.0008636304],"domain_scores_gemma":[0.9988166,0.00047293966,0.000086677566,0.00034795722,0.000056655575,0.00021913344],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006678147,0.0003299637,0.00042448335,0.00027989133,0.00052277633,0.00019259476,0.0003689979,0.00015426167,0.00008953201],"category_scores_gemma":[0.000048657374,0.00020889401,0.00013403512,0.00074292626,0.0013443832,0.0004130057,0.000041599582,0.000662177,0.000025055393],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013757756,0.00008056152,0.99237823,0.00003653978,0.00004003566,0.000025738564,0.00043820695,0.000031685275,0.000006182231,0.0005504245,0.00015581828,0.006118968],"study_design_scores_gemma":[0.0005031954,0.00061081094,0.9854773,0.000016569615,0.000026589061,0.000119826094,0.00047344234,0.00094266894,0.000009591977,0.0080742175,0.0034634382,0.00028232046],"about_ca_topic_score_codex":0.0011207607,"about_ca_topic_score_gemma":0.004649051,"teacher_disagreement_score":0.007523793,"about_ca_system_score_codex":2.7400222e-7,"about_ca_system_score_gemma":0.000020475487,"threshold_uncertainty_score":0.851845},"labels":[],"label_agreement":null},{"id":"W1566040849","doi":"10.1111/geoa.12005","title":"Quantitative geomorphological analysis of drumlins in the peterborough drumlin field, ontario, canada","year":2013,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McMaster University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Drumlin; Geology; Geomorphology; Sediment; Erosion; Landform; Bedrock; Physical geography; Ice stream; Geography; Oceanography","score_opus":0.01352943222911595,"score_gpt":0.22951002482451335,"score_spread":0.2159805925953974,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1566040849","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99216884,0.00018061465,0.000007773589,0.0031077657,0.000092468465,0.00030936944,0.00007788548,0.000014361606,0.004040941],"genre_scores_gemma":[0.9984228,0.0000384714,0.00017697735,0.00092090847,0.000023719907,0.000024706549,0.00028217016,0.0000025493207,0.00010772341],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9975493,0.00044658396,0.00038791323,0.00042939687,0.00047881764,0.00070802035],"domain_scores_gemma":[0.9980674,0.0011179444,0.00013248117,0.00040764376,0.00014747641,0.0001270831],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00029469156,0.00024936598,0.0006157143,0.00034569725,0.00020805778,0.00004646102,0.0006581783,0.00013044025,0.0051672207],"category_scores_gemma":[0.00006868027,0.00014683785,0.00036883738,0.002188222,0.0006121505,0.00024142808,0.000040218576,0.00062487886,0.000055799443],"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":[0.00012977565,0.000105783074,0.9959037,0.000009803507,0.00039718123,0.00005416403,0.0011453079,0.0007911852,0.0000030658632,0.00021938162,0.00087470235,0.00036595349],"study_design_scores_gemma":[0.000183505,0.0006086509,0.9936636,0.0000057157677,0.00015652167,0.000009734919,0.0013221772,0.0009356179,0.000016589463,0.0015599773,0.001345656,0.00019221964],"about_ca_topic_score_codex":0.95392406,"about_ca_topic_score_gemma":0.99588037,"teacher_disagreement_score":0.041956276,"about_ca_system_score_codex":0.0000022794172,"about_ca_system_score_gemma":0.00015955193,"threshold_uncertainty_score":0.9957422},"labels":[],"label_agreement":null},{"id":"W1577621041","doi":"10.1111/j.1468-0459.2012.00474.x","title":"Lichenometric dating of little ice age glacier activity in the central british columbia coast mountains, canada","year":2012,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Moraine; Glacier; Geology; Physical geography; Little ice age; Ice caps; Glacier morphology; Archaeology; Climatology; Geomorphology; Geography; Ice stream; Cryosphere; Sea ice","score_opus":0.01194648053407255,"score_gpt":0.21478654036914735,"score_spread":0.2028400598350748,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1577621041","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99609345,0.0007497161,0.0000027077517,0.00022981389,0.00018552842,0.00025262663,0.0002406216,0.000017384693,0.0022281676],"genre_scores_gemma":[0.9991364,0.0000895621,0.000055823893,0.00023934773,0.00015274463,0.000010225012,0.00019481608,0.000004854422,0.00011625634],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9973409,0.00045205915,0.00024748853,0.0003033078,0.00049658306,0.0011596533],"domain_scores_gemma":[0.9987911,0.00049289875,0.000120801575,0.00030934767,0.000068021785,0.00021785972],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004743331,0.00016992347,0.00038221234,0.00012361462,0.00035792813,0.00012658042,0.000509346,0.0001022231,0.0005501113],"category_scores_gemma":[0.00009511551,0.00016077109,0.00015987796,0.0019925013,0.00059275614,0.0004502147,0.000054323194,0.0005312582,0.0000098476185],"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":[0.00004158037,0.0001574293,0.99438035,0.000049374532,0.000049362916,0.000041571544,0.0004611571,0.000034149485,0.0000053638737,0.000010710055,0.00093958253,0.0038293488],"study_design_scores_gemma":[0.00021831637,0.00012465206,0.99337715,0.000013363201,0.000022628585,0.000044237055,0.0007823575,0.00005703193,0.000008729923,0.0001665384,0.0049937204,0.00019126503],"about_ca_topic_score_codex":0.8814636,"about_ca_topic_score_gemma":0.9847725,"teacher_disagreement_score":0.1033089,"about_ca_system_score_codex":0.0000026414134,"about_ca_system_score_gemma":0.00011297801,"threshold_uncertainty_score":0.65560544},"labels":[],"label_agreement":null},{"id":"W1580167029","doi":"10.1111/geoa.12063","title":"Antecedent Controls on Rainfall Runoff Response and Sediment Transport in a High Arctic Catchment","year":2014,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Queen's University","funders":"ArcticNet","keywords":"Antecedent moisture; Surface runoff; Hydrology (agriculture); Environmental science; Sediment; Watershed; Context (archaeology); Sediment transport; Drainage basin; Fluvial; Storm; Infiltration (HVAC); Geology; Structural basin; Runoff curve number; Geography; Oceanography; Ecology; Geomorphology","score_opus":0.010436609913291768,"score_gpt":0.2158941877599926,"score_spread":0.20545757784670085,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1580167029","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949544,0.0002364427,0.0000045105307,0.0029768543,0.00020411883,0.00042824767,0.0007812196,0.00005577317,0.00035841076],"genre_scores_gemma":[0.9970104,0.0002502987,0.000031070267,0.0016556284,0.00021740445,0.000028405731,0.0007285861,0.000011033132,0.0000671917],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99768096,0.0002351985,0.0003330529,0.00059178256,0.00045501467,0.0007039632],"domain_scores_gemma":[0.9988823,0.00032744417,0.0000939326,0.00033927383,0.000050554452,0.00030653042],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0004605567,0.0003749062,0.00050304324,0.0003003772,0.00018982949,0.00008297836,0.00020686825,0.00008964746,0.0005399295],"category_scores_gemma":[0.000020855796,0.00027960117,0.00021630611,0.00047819212,0.00028832085,0.00022629587,0.000020435848,0.00028115165,0.00006901349],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0033101314,0.00024820477,0.9886146,0.000059731035,0.000058089146,0.000043672375,0.0013677697,0.00034192856,0.00033619272,0.00009486628,0.00011646711,0.0054083043],"study_design_scores_gemma":[0.0013655579,0.0018002487,0.9764922,0.00008670671,0.000036441445,0.000010320066,0.00024457957,0.00048396148,0.00009778966,0.0010626466,0.01793602,0.00038351543],"about_ca_topic_score_codex":0.007770102,"about_ca_topic_score_gemma":0.009698081,"teacher_disagreement_score":0.017819552,"about_ca_system_score_codex":0.0000061809137,"about_ca_system_score_gemma":0.000016663489,"threshold_uncertainty_score":0.9999656},"labels":[],"label_agreement":null},{"id":"W1587585133","doi":"10.1111/geoa.12008","title":"Middle–late holocene paleoclimate and weathering history in the norra storfjället mountains, sweden: deglacial record and soil stratigraphy applied to neoglaciation in lower latitudes","year":2013,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Umeå Universitet","keywords":"Moraine; Geology; Paleosol; Glacial period; Glacier; Paleoclimatology; Weathering; Physical geography; Holocene; Loess; Paleontology; Climate change; Oceanography; Geography","score_opus":0.01612350706489869,"score_gpt":0.20962798959410833,"score_spread":0.19350448252920965,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1587585133","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99370605,0.0008663471,0.0000048525812,0.0010774885,0.00013094368,0.0006598638,0.000015724421,0.00004123302,0.0034974874],"genre_scores_gemma":[0.99829847,0.00034764316,0.00021993551,0.00086200575,0.00008740188,0.00008754782,0.000051487572,0.000007835996,0.00003770149],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9977203,0.0002637917,0.00033679183,0.0005945256,0.00030295528,0.0007816314],"domain_scores_gemma":[0.99915683,0.0002321825,0.00009336832,0.00027757316,0.000054682434,0.00018533399],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041209048,0.00033284558,0.00043869286,0.00047302753,0.00023506282,0.000116223746,0.0003003967,0.00017227262,0.00017783197],"category_scores_gemma":[0.000023398428,0.00024019524,0.00010245465,0.0006951689,0.00058080634,0.00042770666,0.000050587303,0.0005296659,0.000052387688],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023225918,0.00009245912,0.9933472,0.00004909788,0.000032406566,0.000023883333,0.002403195,0.00022749379,0.000035854184,0.00016305671,0.00010086249,0.00329223],"study_design_scores_gemma":[0.0004586022,0.00039340893,0.99378866,0.000025951827,0.000015395706,0.000012430864,0.00079366233,0.0004270427,0.0000053043022,0.0023460032,0.0014280496,0.00030550425],"about_ca_topic_score_codex":0.0027544277,"about_ca_topic_score_gemma":0.028932502,"teacher_disagreement_score":0.026178075,"about_ca_system_score_codex":0.000003306214,"about_ca_system_score_gemma":0.000028174993,"threshold_uncertainty_score":0.98878694},"labels":[],"label_agreement":null},{"id":"W1588997167","doi":"10.1111/j.1468-0459.2012.00460.x","title":"Lichenometric ages of the little ice age moraines on king george island and of the last volcanic activity on penguin island (west antarctica)","year":2012,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Moraine; Glacier; Lichen; Peninsula; Volcano; Geology; Physical geography; Geography; Archaeology; Paleontology; Ecology; Biology","score_opus":0.016297691288026054,"score_gpt":0.23636263621446543,"score_spread":0.22006494492643938,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1588997167","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9947231,0.00044253416,9.0140645e-7,0.0009029351,0.00023888785,0.00029112902,0.00020072912,0.000014341287,0.0031854822],"genre_scores_gemma":[0.9993706,0.00013899013,0.000009785418,0.0001643671,0.00014410866,0.000005764871,0.000019674017,0.000006668565,0.00014008956],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979846,0.00043392606,0.00020934794,0.0003190473,0.00043472566,0.00061835983],"domain_scores_gemma":[0.9983077,0.00079338835,0.00019303091,0.00049775146,0.00007490358,0.00013319524],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036560258,0.00025898247,0.00041694072,0.00023719642,0.0004154988,0.00003108165,0.0004656613,0.0001232548,0.0001931934],"category_scores_gemma":[0.00016050854,0.00013533942,0.00027954657,0.0014521775,0.0014041556,0.00021181934,0.00011973105,0.0005394686,0.00001772231],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019022214,0.00023019969,0.9972954,0.00007961815,0.00009904158,0.0000022296927,0.00064392353,0.00006728313,0.000076979566,0.00013997869,0.00011624739,0.001058874],"study_design_scores_gemma":[0.00027470477,0.00050212065,0.9965882,0.000045436598,0.000056555895,0.000013680848,0.00013848733,0.000055781704,0.0005200496,0.00046520683,0.0011791213,0.00016065681],"about_ca_topic_score_codex":0.0007013267,"about_ca_topic_score_gemma":0.0069465316,"teacher_disagreement_score":0.006245205,"about_ca_system_score_codex":9.102475e-7,"about_ca_system_score_gemma":0.00002102886,"threshold_uncertainty_score":0.5518981},"labels":[],"label_agreement":null},{"id":"W1964814677","doi":"10.1111/j.1468-0459.2010.00386.x","title":"Sedimentary fluxes and budgets in changing cold environments: the global iag/aig sediment budgets in cold environments (sedibud) programme","year":2010,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Queen's University","funders":"","keywords":"Geography; Archaeology; Arctic; Physical geography; Oceanography; Geology","score_opus":0.007019018221767334,"score_gpt":0.21319330460116379,"score_spread":0.20617428637939644,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1964814677","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99344474,0.0011453516,0.000003690432,0.0029361658,0.00036839253,0.00097023766,0.00011950183,0.00003963083,0.0009723139],"genre_scores_gemma":[0.9977783,0.00039015786,0.00017235435,0.0010300953,0.00016661703,0.00011501326,0.00018298913,0.000011354634,0.00015313309],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9960571,0.0003204127,0.00043711317,0.00086467894,0.0006100715,0.0017106064],"domain_scores_gemma":[0.99876404,0.00024362108,0.00013224188,0.00048754088,0.000013518802,0.00035901097],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00066295284,0.0004967447,0.000529296,0.00039932958,0.0004816327,0.000100462166,0.000565954,0.00027119555,0.0003392906],"category_scores_gemma":[0.00002556121,0.00035925655,0.00019060088,0.0011515723,0.0017063672,0.0004542032,0.0002142911,0.0010405666,0.00013275212],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017623385,0.0004103425,0.9954384,0.000027857952,0.000100278914,0.00013798816,0.0005693968,0.00010238719,0.00017090363,0.00026837224,0.000088978944,0.0025088354],"study_design_scores_gemma":[0.0011237322,0.00049643184,0.95903015,0.000025807989,0.000039485578,0.000048116264,0.0006219805,0.000426729,0.0003349872,0.0012764807,0.03615731,0.00041880942],"about_ca_topic_score_codex":0.0009970814,"about_ca_topic_score_gemma":0.0072249775,"teacher_disagreement_score":0.036408294,"about_ca_system_score_codex":0.0000064557,"about_ca_system_score_gemma":0.000030413146,"threshold_uncertainty_score":0.9998859},"labels":[],"label_agreement":null},{"id":"W1968940443","doi":"10.1111/j.0435-3676.2000.00138.x","title":"Frozen ground phenomena in the vicinity of terra nova bay, northern victoria land, antarctica: a preliminary report","year":2000,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Polar Research and Ecology","field":"Environmental Science","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University; University of Ottawa","funders":"","keywords":"Geology; Permafrost; Debris; Geomorphology; Frost (temperature); Bay; Oceanography; Physical geography; Hydrology (agriculture); Geography; Geotechnical engineering","score_opus":0.010574690358848506,"score_gpt":0.24143531640518176,"score_spread":0.23086062604633326,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1968940443","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.981237,0.000053051204,0.000004584644,0.0010357479,0.00007584855,0.00043746977,0.000038967195,0.000035239507,0.01708211],"genre_scores_gemma":[0.9989644,0.00007158655,0.00008415481,0.0003042407,0.00022831734,0.00007524671,0.00006463627,0.000020788146,0.00018659786],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99730545,0.00024974934,0.00041893194,0.0005439774,0.0006537103,0.0008281936],"domain_scores_gemma":[0.99883014,0.0001429531,0.00012361426,0.00069734314,0.000026484277,0.00017944038],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00047499614,0.00028406322,0.0004087811,0.000105874315,0.00022513866,0.00005074861,0.0006903749,0.000092089045,0.0039137276],"category_scores_gemma":[0.000039903414,0.000186621,0.00028632936,0.0011190951,0.0009871026,0.0004480201,0.00024403371,0.0004546816,0.00027575565],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007237836,0.0011928068,0.97581196,0.000024237701,0.00007909095,0.00022157881,0.002550388,0.00010567371,0.0002344124,0.000012948448,0.00042268768,0.018620413],"study_design_scores_gemma":[0.00046075584,0.0010093243,0.96441627,0.000011556102,0.000027773842,0.0000877038,0.00028378033,0.00007237643,0.000038295537,0.0015452852,0.03181167,0.00023523369],"about_ca_topic_score_codex":0.006030734,"about_ca_topic_score_gemma":0.005684185,"teacher_disagreement_score":0.031388983,"about_ca_system_score_codex":0.000034552937,"about_ca_system_score_gemma":0.000020968615,"threshold_uncertainty_score":0.9969968},"labels":[],"label_agreement":null},{"id":"W1986607725","doi":"10.1111/j.1468-0459.2008.00335.x","title":"Influence of climate and climate anomalies on norway spruce tree‐ring growth at different altitudes and on glacier responses: examples from the central italian alps","year":2008,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Tree-ring climate responses","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Ministero dell’Istruzione, dell’Università e della Ricerca; Ontario Council on Graduate Studies, Council of Ontario Universities","keywords":"Altitude (triangle); Precipitation; Glacier; Climate change; Picea abies; Dendroclimatology; Dendrochronology; Alpine climate; Physical geography; Climatology; Karst; Environmental science; Chronology; Effects of high altitude on humans; Geology; Geography; Ecology; Meteorology; Biology","score_opus":0.01353036746427484,"score_gpt":0.21186390544832245,"score_spread":0.19833353798404763,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1986607725","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99658686,0.00072065735,3.8711653e-7,0.00047308544,0.00007379712,0.00030709582,0.001428721,0.000087238084,0.0003221738],"genre_scores_gemma":[0.99318755,0.0061572003,0.000086151405,0.00030512465,0.00011079647,0.0000105684285,0.000099798686,0.00001853285,0.000024257386],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99691343,0.00033483273,0.00041412484,0.0007552676,0.0005916377,0.0009906798],"domain_scores_gemma":[0.9974693,0.0014407092,0.00022467681,0.0004889373,0.00006927081,0.00030712585],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00015394809,0.0005361631,0.0005919401,0.00020769081,0.00091895927,0.00013406736,0.0003730794,0.00009642138,0.00006777089],"category_scores_gemma":[0.00009530947,0.00032882424,0.00023860653,0.00041115223,0.0015644524,0.00042383312,0.00017544498,0.00026381607,0.00003047898],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0029293527,0.00012317293,0.9912509,0.00007467698,0.00011288723,0.000039325663,0.0014131642,0.00024828815,0.00070473284,0.00021567459,0.00001658359,0.0028712586],"study_design_scores_gemma":[0.0005164343,0.0010207844,0.9948952,0.00017400838,0.00006419725,0.000027267064,0.00029158464,0.000094402196,0.0014518469,0.00021795563,0.0008370699,0.00040921752],"about_ca_topic_score_codex":0.0016783066,"about_ca_topic_score_gemma":0.0033114424,"teacher_disagreement_score":0.005436543,"about_ca_system_score_codex":0.000006205454,"about_ca_system_score_gemma":0.000014871172,"threshold_uncertainty_score":0.9999164},"labels":[],"label_agreement":null},{"id":"W1988319814","doi":"10.1111/j.1468-0459.2008.00168.x","title":"Identifying moraine surfaces with similar histories using lichen size distributions and the u2 statistic, southeast iceland","year":2008,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Moraine; Geology; Glacier; Physical geography; Geomorphology; Sedimentary depositional environment; Paleontology; Geography; Structural basin","score_opus":0.020150030316333344,"score_gpt":0.23057116753513435,"score_spread":0.210421137218801,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1988319814","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949598,0.0016354851,0.00024224988,0.0015897136,0.00009998468,0.00030300868,0.00040445648,0.00006960662,0.00069574727],"genre_scores_gemma":[0.9981413,0.00028846873,0.0010276353,0.00009439196,0.00009597813,0.000009897141,0.00016767402,0.000007594757,0.00016708199],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99791485,0.00033113963,0.00023719067,0.00044946276,0.0003856004,0.0006817787],"domain_scores_gemma":[0.9983906,0.00080524164,0.00012478766,0.0003076894,0.00016298362,0.00020865876],"candidate_categories":["sts"],"consensus_categories":["sts"],"category_scores_codex":[0.0002683309,0.00030443675,0.00047653005,0.000094358074,0.00181621,0.00009959027,0.00027899916,0.000094586896,0.00025092508],"category_scores_gemma":[0.00009254545,0.00017253803,0.00014483552,0.0006578788,0.0048565227,0.0003573553,0.00005548648,0.00043726378,0.000023201059],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00077959005,0.00004219202,0.9962236,0.000035370304,0.00017804597,0.00009405691,0.001725881,0.00024911892,0.0000049085475,0.00048323665,0.00007837234,0.00010559377],"study_design_scores_gemma":[0.0009998694,0.00022017668,0.99018204,0.000016515613,0.00012427768,0.00030466286,0.001082653,0.0012606906,0.000011106097,0.003927863,0.0015821825,0.0002879851],"about_ca_topic_score_codex":0.0015439269,"about_ca_topic_score_gemma":0.0023863313,"teacher_disagreement_score":0.0060416167,"about_ca_system_score_codex":0.0000011647951,"about_ca_system_score_gemma":0.00005937878,"threshold_uncertainty_score":0.9994833},"labels":[],"label_agreement":null},{"id":"W1996124874","doi":"10.1111/j.0435-3676.2004.00239.x","title":"Relict shorelines and ice flow patterns of the northern puget lowland from lidar data and digital terrain modelling","year":2004,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Shore; Lidar; Sea level; Terrain; Oceanography; Altitude (triangle); Physical geography; Deposition (geology); Geomorphology; Sediment; Geography; Remote sensing; Cartography","score_opus":0.01711914827860228,"score_gpt":0.21974985717321133,"score_spread":0.20263070889460905,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1996124874","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99551153,0.0011517658,0.00022219979,0.0013985022,0.000086447115,0.0001813583,0.0012619417,0.000029174542,0.00015707775],"genre_scores_gemma":[0.99829966,0.00040237364,0.0003138912,0.0001155288,0.00012784054,0.0000023880718,0.0007133035,0.000006714984,0.000018330074],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984105,0.00008548841,0.00024251523,0.0005538394,0.00027976048,0.00042790174],"domain_scores_gemma":[0.9988844,0.00018938731,0.000090549336,0.0006107849,0.00007126125,0.00015363161],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013415093,0.00024265019,0.00034145347,0.000087084685,0.00029869043,0.00010452198,0.0005714395,0.000118575794,0.00004042675],"category_scores_gemma":[0.000030914136,0.00014857488,0.000109530505,0.00028026078,0.0008381701,0.00049348513,0.00022901499,0.00034101473,0.000011023889],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011429371,0.000051552448,0.9940641,0.000030560906,0.00009756737,0.000010015028,0.0007279922,0.0020883505,0.0000023947762,0.000010160114,0.0000083892,0.002794634],"study_design_scores_gemma":[0.00043188603,0.00017634821,0.97963583,0.00005108768,0.000050797276,0.000028868986,0.00033879434,0.010025917,0.000015754273,0.0081612,0.00086945365,0.00021404003],"about_ca_topic_score_codex":0.0031705697,"about_ca_topic_score_gemma":0.0079800775,"teacher_disagreement_score":0.0144282365,"about_ca_system_score_codex":3.3093744e-7,"about_ca_system_score_gemma":0.00002876227,"threshold_uncertainty_score":0.6058708},"labels":[],"label_agreement":null},{"id":"W1998835213","doi":"10.1111/j.1468-0459.2010.00387.x","title":"A framework for characterizing fluvial sediment fluxes from source to sink in cold environments","year":2010,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"European Social Fund","keywords":"Sediment; Fluvial; Sedimentary budget; Environmental science; Hydrology (agriculture); Sediment transport; Sedimentation; Bed load; Sink (geography); Geology; Geomorphology; Geography; Geotechnical engineering","score_opus":0.01232031720842822,"score_gpt":0.22214395676045964,"score_spread":0.20982363955203143,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1998835213","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99464524,0.00010158231,0.0010846782,0.0022202109,0.00070992263,0.00063149544,0.00047258034,0.000062100764,0.000072193194],"genre_scores_gemma":[0.9821129,0.00005173093,0.013970979,0.0022181836,0.0010803766,0.00010599045,0.00032238735,0.000017499298,0.000119949465],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980844,0.000033001284,0.0003016617,0.00057578925,0.00033515994,0.00066993927],"domain_scores_gemma":[0.99894327,0.00031710253,0.00009723391,0.00035139913,0.000029164554,0.00026183572],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00010369329,0.00030861708,0.0004017084,0.00008850722,0.00038789696,0.00013993116,0.00032178816,0.00011547839,0.00046510284],"category_scores_gemma":[0.000055681598,0.00025603984,0.00027106976,0.0005975584,0.00017385207,0.00029793114,0.00006616574,0.00036602127,0.00009451703],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029320215,0.00029798487,0.9572416,0.00001589121,0.00013517051,0.0000050913477,0.0019864917,0.0004570454,0.00579087,0.00037562943,0.0006222376,0.03277877],"study_design_scores_gemma":[0.0002597943,0.00026506168,0.7350606,0.00002081986,0.000025476058,3.592913e-7,0.00028333563,0.00042177853,0.00043044036,0.0022931339,0.2606482,0.00029104456],"about_ca_topic_score_codex":0.0019788765,"about_ca_topic_score_gemma":0.0021460056,"teacher_disagreement_score":0.26002595,"about_ca_system_score_codex":0.0000032756243,"about_ca_system_score_gemma":0.000014072854,"threshold_uncertainty_score":0.9999892},"labels":[],"label_agreement":null},{"id":"W2008988133","doi":"10.1111/j.0435-3676.2004.00235.x","title":"Re‐dating the moraines at skálafellsjökull and heinabergsjökull using different lichenometric methods: implications for the timing of the icelandic little ice age maximum","year":2004,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"Leverhulme Trust; Royal Geographical Society; Royal Scottish Geographical Society","keywords":"Moraine; Glacier; Geology; Glacier mass balance; Deglaciation; Population; Glacier morphology; Physical geography; Climatology; Geomorphology; Cryosphere; Ice stream; Geography; Sea ice; Glacial period; Demography","score_opus":0.04980453337517637,"score_gpt":0.31003640361331053,"score_spread":0.26023187023813416,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2008988133","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98815215,0.0036154406,0.00076440495,0.0059347297,0.00016091538,0.0007398699,0.00011228506,0.000028117669,0.0004920675],"genre_scores_gemma":[0.997572,0.00024687193,0.0015581595,0.00030820625,0.00013462915,0.000039533257,0.00005237213,0.000009003358,0.00007924057],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981521,0.00032918365,0.00030176569,0.00040026635,0.00021791784,0.00059878087],"domain_scores_gemma":[0.99691796,0.0020551048,0.00022022832,0.00058123155,0.00012153542,0.00010396191],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0005573847,0.00026049613,0.00035491004,0.0001674701,0.0017369298,0.00007810204,0.0006571053,0.000107933796,0.00007577866],"category_scores_gemma":[0.00020075723,0.00011654424,0.00034757354,0.0013840019,0.001448311,0.00013431504,0.00018097168,0.00036654374,0.000004396717],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000082981205,0.000057793444,0.99390614,0.00006507031,0.00017238224,9.690342e-7,0.00092025386,0.0012204364,0.0001402029,0.00036027975,0.000045440756,0.003028032],"study_design_scores_gemma":[0.0003212287,0.00016768699,0.98068774,0.00002265162,0.00017777336,0.00002155206,0.00064292457,0.00089133723,0.0002567904,0.015071924,0.00156753,0.00017089321],"about_ca_topic_score_codex":0.00054976786,"about_ca_topic_score_gemma":0.0016428918,"teacher_disagreement_score":0.0147116445,"about_ca_system_score_codex":0.0000023686457,"about_ca_system_score_gemma":0.000028756138,"threshold_uncertainty_score":0.9995627},"labels":[],"label_agreement":null},{"id":"W2028247580","doi":"10.1111/j.0435-3676.2000.00133.x","title":"Age and origin of upland block fields on melville peninsula, eastern canadian arctic","year":2000,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Bedrock; Geology; Meltwater; Glacial period; Peninsula; Block (permutation group theory); Glacier; Frost weathering; Geomorphology; Weathering; Gneiss; Physical geography; Solifluction; Ice sheet; Pleistocene; Paleontology; Archaeology; Geography; Metamorphic rock","score_opus":0.012288779913578598,"score_gpt":0.22243056478889373,"score_spread":0.21014178487531512,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2028247580","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9754674,0.00038550084,2.389337e-7,0.00091437116,0.000085634136,0.00017325635,0.000093206065,0.000026589922,0.022853803],"genre_scores_gemma":[0.99820095,0.0002542534,0.000045443143,0.00037717223,0.00008308968,0.000004670776,0.00011073976,0.0000050055937,0.000918664],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99834156,0.00013157044,0.00020222159,0.0003989686,0.00024821496,0.00067745475],"domain_scores_gemma":[0.9990333,0.00016189626,0.00004586098,0.00028750315,0.00006251535,0.00040893874],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00011809887,0.00023532375,0.00037321614,0.00027088713,0.00028488267,0.000043218064,0.00025485049,0.00015883158,0.0023379119],"category_scores_gemma":[0.00001666542,0.00017737348,0.00015553014,0.00044600066,0.00069296214,0.0001463435,0.000013239413,0.00037896266,0.00025982552],"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":[0.00022294828,0.00004570112,0.9938485,0.00003854166,0.0000770148,0.0001420005,0.00027959258,0.00025249406,8.920718e-7,0.00010936887,0.00012514842,0.004857789],"study_design_scores_gemma":[0.00034578374,0.0007429628,0.9824341,0.000026104146,0.000029913635,0.000058439422,0.000067294444,0.000457077,0.000017181761,0.001941362,0.01365526,0.00022453295],"about_ca_topic_score_codex":0.07290154,"about_ca_topic_score_gemma":0.23903316,"teacher_disagreement_score":0.16613162,"about_ca_system_score_codex":7.1298734e-7,"about_ca_system_score_gemma":0.000050436025,"threshold_uncertainty_score":0.9985741},"labels":[],"label_agreement":null},{"id":"W2030703660","doi":"10.1111/j.1468-0459.2010.00391.x","title":"Assessment of a time‐integrated fluvial suspended sediment sampler in a high arctic setting","year":2010,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Soil erosion and sediment transport","field":"Agricultural and Biological Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Queen's University","funders":"","keywords":"Sediment trap; Fluvial; Sediment; Ephemeral key; Environmental science; Hydrology (agriculture); Trap (plumbing); Arctic; Flux (metallurgy); Sedimentation; Grain size; Bed load; Geology; Sediment transport; Oceanography; Geomorphology; Ecology; Structural basin; Environmental engineering; Geotechnical engineering","score_opus":0.006732265113280829,"score_gpt":0.22199202353082867,"score_spread":0.21525975841754785,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2030703660","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973117,0.000011354108,0.0000026135408,0.0011664811,0.00023259921,0.0004036778,0.00015552853,0.00010981194,0.0006062268],"genre_scores_gemma":[0.9982046,0.00001740464,0.00056166854,0.00025813366,0.00022991418,0.0000761745,0.00055546226,0.000004287233,0.000092355556],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9975714,0.00011891586,0.00050039036,0.00057244033,0.00060944236,0.0006273893],"domain_scores_gemma":[0.9990533,0.0001911875,0.00017643948,0.00017154185,0.00019035256,0.0002171661],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00030530657,0.00035766975,0.00053597696,0.00009498241,0.00016947184,0.00006388901,0.00038201603,0.00015025183,0.0020302841],"category_scores_gemma":[0.000023709605,0.00015031372,0.00043513687,0.001250626,0.000295091,0.00024407869,0.00008537653,0.0005945765,0.000020635995],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016629737,0.0014415821,0.6226079,0.000028012913,0.00008376476,0.00001512746,0.00018413129,0.000023472985,0.36173686,0.0012131286,0.0001872429,0.012312491],"study_design_scores_gemma":[0.00058074726,0.00061069115,0.9874809,0.00004618075,0.000038443497,0.0000040242226,0.00020261058,0.0002812182,0.003102289,0.0015733392,0.0057212734,0.00035832587],"about_ca_topic_score_codex":0.002608952,"about_ca_topic_score_gemma":0.001733078,"teacher_disagreement_score":0.36487296,"about_ca_system_score_codex":0.000012158077,"about_ca_system_score_gemma":0.000026549686,"threshold_uncertainty_score":0.998882},"labels":[],"label_agreement":null},{"id":"W2067329209","doi":"10.1111/j.1468-0459.2010.00403.x","title":"Testing lake sediment and dendrogeomorphic proxies for little ice age environmental change in the upper fraser river area, british columbia, canada","year":2010,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto; Laurentian University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Sediment; Geology; Little ice age; Environmental change; Hydrology (agriculture); Physical geography; Climate change; Oceanography; Geomorphology; Geography; Geotechnical engineering","score_opus":0.01419783693845398,"score_gpt":0.20151136258637006,"score_spread":0.1873135256479161,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2067329209","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99661756,0.0003352552,3.7537532e-7,0.0010192194,0.00017073247,0.00073335227,0.0007443062,0.000021455278,0.00035777703],"genre_scores_gemma":[0.9979021,0.000039695824,0.00020646141,0.00085441023,0.00017074449,0.00013476575,0.00052682415,0.0000065795607,0.00015840422],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981334,0.00011826843,0.00018978697,0.00045011475,0.0003866304,0.0007217901],"domain_scores_gemma":[0.9990223,0.00047859814,0.00006501562,0.00023135052,0.000044890694,0.00015786687],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030811774,0.00018759431,0.00027887986,0.00005894729,0.000582635,0.0002009736,0.00032344405,0.00012395154,0.0006252058],"category_scores_gemma":[0.000059158858,0.00017480816,0.00009925198,0.0003282046,0.0010341456,0.00025626877,0.000048469356,0.00054128,0.00000892529],"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":[0.000030374244,0.00008134992,0.9945625,0.000029123872,0.00003540009,0.00013195799,0.00043739326,0.0000028775464,0.0000071509103,0.000004587233,0.00060221774,0.004075085],"study_design_scores_gemma":[0.0003887128,0.00022729092,0.96941084,0.000014629774,0.000026412836,0.00010366633,0.000388843,0.00022806818,0.0000053758276,0.00085882825,0.02811785,0.00022950424],"about_ca_topic_score_codex":0.5334687,"about_ca_topic_score_gemma":0.9934212,"teacher_disagreement_score":0.45995247,"about_ca_system_score_codex":8.852968e-7,"about_ca_system_score_gemma":0.00004883798,"threshold_uncertainty_score":0.71284693},"labels":[],"label_agreement":null},{"id":"W2068494156","doi":"10.1111/j.0435-3676.2005.00251.x","title":"Holocene carbonate precipitates on precambrian bedrock in the high arctic: age and potential for palaeoclimatic information","year":2005,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Carbonate; Holocene; Bedrock; Radiocarbon dating; Precambrian; Paleontology; Arctic; Geochemistry; Oceanography","score_opus":0.008075949235107386,"score_gpt":0.21996210004388853,"score_spread":0.21188615080878115,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2068494156","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9928295,0.00016418731,0.000011537186,0.004886414,0.000105994135,0.0006943203,0.00012277774,0.000038224327,0.0011470349],"genre_scores_gemma":[0.997768,0.00015309366,0.00038782414,0.0008833333,0.0001564472,0.00006547777,0.00054324884,0.000004440817,0.000038131868],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99820405,0.0002254613,0.00029277077,0.00030497496,0.0003100632,0.00066268235],"domain_scores_gemma":[0.9990324,0.0004266554,0.00009745719,0.00025572503,0.00007504234,0.000112759626],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037131234,0.00024881618,0.0003095157,0.00027651002,0.00035033908,0.00013759958,0.0003213811,0.00012616158,0.000081571685],"category_scores_gemma":[0.00006248504,0.00015734308,0.00015632638,0.000441193,0.0004892769,0.0006400461,0.000027560609,0.00037009432,0.00006982789],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048779583,0.00010850903,0.9847103,0.00009318564,0.000058829148,0.000015546113,0.0013481162,0.0022616792,9.129676e-7,0.00048531155,0.00013076625,0.010299043],"study_design_scores_gemma":[0.0007010898,0.0008007731,0.98497546,0.000023149263,0.000036749996,0.000033547807,0.00032436778,0.0034465105,0.000010897835,0.0073368633,0.002098636,0.00021197525],"about_ca_topic_score_codex":0.00037507023,"about_ca_topic_score_gemma":0.001304428,"teacher_disagreement_score":0.010087067,"about_ca_system_score_codex":9.545672e-7,"about_ca_system_score_gemma":0.000015952028,"threshold_uncertainty_score":0.6416264},"labels":[],"label_agreement":null},{"id":"W2072186092","doi":"10.1111/j.0435-3676.2004.00209.x","title":"Dendrogeomorphological assessment of movement at hilda rock glacier, banff national park, canadian rocky mountains","year":2004,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Tree-ring climate responses","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"","keywords":"Geology; Glacier; Picea engelmannii; Rock glacier; Glacier mass balance; Abies lasiocarpa; National park; Physical geography; Dendrochronology; Debris; Tidewater glacier cycle; Geomorphology; Glacier morphology; Montane ecology; Geography; Archaeology; Paleontology; Climatology; Ice stream; Oceanography; Ecology; Cryosphere","score_opus":0.013427896500757139,"score_gpt":0.24111065656314454,"score_spread":0.2276827600623874,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2072186092","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9924311,0.00025554097,0.00004789544,0.0011816671,0.00019521543,0.0003717272,0.0014576862,0.00010359412,0.003955561],"genre_scores_gemma":[0.9972208,0.00013020071,0.0007645227,0.0008303763,0.00015005941,0.00002101598,0.00074484246,0.000014171486,0.00012399089],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9965065,0.00013135941,0.00047686452,0.00067677675,0.001163754,0.0010447148],"domain_scores_gemma":[0.9983287,0.00015695704,0.00020704574,0.0003685045,0.00026375998,0.00067506626],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002484143,0.00044178445,0.0005233447,0.000466079,0.0005323767,0.00010210363,0.00051878416,0.0001477569,0.0013419751],"category_scores_gemma":[0.000045490866,0.00034947193,0.00046902825,0.0010150733,0.00035513454,0.00038850078,0.00008834073,0.0003146001,0.00018277952],"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":[0.0002100477,0.00030718316,0.97071767,0.000042108048,0.00021621764,0.00009525294,0.00014434177,0.024747705,0.0002750286,0.001206625,0.00034684138,0.0016910003],"study_design_scores_gemma":[0.00072805316,0.00070082204,0.97973144,0.00003255054,0.0000467709,0.00004053625,0.00013403613,0.00083518494,0.0004982281,0.0037912896,0.013006742,0.00045432124],"about_ca_topic_score_codex":0.060993314,"about_ca_topic_score_gemma":0.14077695,"teacher_disagreement_score":0.079783626,"about_ca_system_score_codex":0.000079467274,"about_ca_system_score_gemma":0.00039640514,"threshold_uncertainty_score":0.99989575},"labels":[],"label_agreement":null},{"id":"W2073456498","doi":"10.1111/j.0435-3676.2001.00144.x","title":"Physiographically controlled allometry of specific sediment yield in the canadian cordillera: a lake sediment‐based approach","year":2001,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Soil erosion and sediment transport","field":"Agricultural and Biological Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Sediment; Drainage basin; Hydrology (agriculture); Sedimentary budget; Structural basin; Geology; Fluvial; Drainage; Denudation; Yield (engineering); Sediment transport; Geomorphology; Ecology; Geography; Tectonics","score_opus":0.02031732467909769,"score_gpt":0.20616157725793918,"score_spread":0.1858442525788415,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2073456498","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9863795,0.0002657833,0.0000059085214,0.004582686,0.00013317526,0.0011612924,0.00012852905,0.00008339102,0.0072597573],"genre_scores_gemma":[0.9963166,0.00019490156,0.00007259319,0.0024850848,0.00026003673,0.0002599892,0.0003590361,0.000005098477,0.00004663949],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9965778,0.00020786833,0.0005947051,0.0006588204,0.0010605409,0.00090027595],"domain_scores_gemma":[0.9986698,0.00031863558,0.00018842376,0.00027926278,0.00018647562,0.00035739003],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042285825,0.00046508102,0.00080202235,0.00026107673,0.0004180988,0.00013058305,0.0007813428,0.00019272689,0.00056177564],"category_scores_gemma":[0.000016291195,0.00017148542,0.0010056192,0.003742133,0.00047371347,0.00020467033,0.00003971739,0.00048022295,0.000011858571],"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":[0.0052305055,0.013126243,0.90605086,0.00010991699,0.00079163385,0.0001933362,0.0015409638,0.0005397496,0.038541663,0.0022635476,0.0066084587,0.02500313],"study_design_scores_gemma":[0.0023522424,0.0011820138,0.9244198,0.000066058026,0.00009209783,0.000006679309,0.000984419,0.00031303856,0.00030400837,0.00035435893,0.06934012,0.0005851307],"about_ca_topic_score_codex":0.0120515665,"about_ca_topic_score_gemma":0.068346664,"teacher_disagreement_score":0.06273166,"about_ca_system_score_codex":0.000014702177,"about_ca_system_score_gemma":0.000036413185,"threshold_uncertainty_score":0.9945273},"labels":[],"label_agreement":null},{"id":"W2081216632","doi":"10.1111/1468-0459.00188","title":"Decadal variability in climate and glacier fluctuations on mt baker, washington, usa","year":2003,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Glacier; Pacific decadal oscillation; Precipitation; Climatology; Glacier mass balance; Climate change; Structural basin; Geology; El Niño Southern Oscillation; Environmental science; Physical geography; Oceanography; Geography; Meteorology; Geomorphology","score_opus":0.011457754058620264,"score_gpt":0.2195212588737785,"score_spread":0.20806350481515823,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2081216632","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99346167,0.00023785386,0.00006986244,0.0005531335,0.0002458496,0.0003532682,0.00013583877,0.000056521953,0.004886025],"genre_scores_gemma":[0.9976752,0.0004677024,0.0010288316,0.00055297464,0.00009523333,0.00002926029,0.0000746462,0.0000078504845,0.00006830243],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979037,0.0002086794,0.00031573733,0.00057507254,0.00033601874,0.0006607801],"domain_scores_gemma":[0.99888957,0.00041496288,0.00008220684,0.0003342123,0.00008501432,0.00019401923],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044886634,0.00029446222,0.0003472176,0.000102545186,0.0005361222,0.00012587442,0.00016417797,0.000078744524,0.00065402145],"category_scores_gemma":[0.00017609166,0.0002252557,0.0001803576,0.0011961604,0.00037386044,0.00039418458,0.000032007127,0.00028331377,0.00006084176],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000057039768,0.00014783003,0.9825121,0.000018778488,0.000036738144,0.00000471561,0.00036350696,0.00060898956,0.00000947466,0.0032703548,0.00015070596,0.012819725],"study_design_scores_gemma":[0.0003171226,0.00021794329,0.9422215,0.0000143869665,0.00002504476,0.0000035014757,0.0003304803,0.0009983652,0.000013245808,0.005688065,0.04988142,0.00028889964],"about_ca_topic_score_codex":0.0008831502,"about_ca_topic_score_gemma":0.0033503948,"teacher_disagreement_score":0.049730714,"about_ca_system_score_codex":0.0000042847723,"about_ca_system_score_gemma":0.000026573649,"threshold_uncertainty_score":0.9185661},"labels":[],"label_agreement":null},{"id":"W2083579298","doi":"10.1111/j.0435-3676.2001.00148.x","title":"Morphometric controls and basin response in the cascade mountains","year":2001,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia; Okanagan University College","funders":"University of British Columbia; University of Canterbury","keywords":"Debris; Geology; Structural basin; Debris flow; Drainage basin; Snow; Geomorphology; Hydrology (agriculture); Geography; Oceanography; Cartography","score_opus":0.006412101102007738,"score_gpt":0.21780198395509526,"score_spread":0.21138988285308752,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2083579298","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9928073,0.00029342194,0.000021148076,0.0039666155,0.00005659446,0.00035629774,0.000018801798,0.000050896575,0.002428904],"genre_scores_gemma":[0.9975625,0.00056710053,0.000080553335,0.0013388165,0.00008175213,0.00007006595,0.000008915018,0.00001882023,0.00027141985],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99782664,0.00031340015,0.0002496091,0.00046585035,0.0005102768,0.00063424965],"domain_scores_gemma":[0.9990907,0.00026940988,0.00007798413,0.00039121014,0.000013973891,0.00015673015],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00054742163,0.00028123643,0.00031906372,0.00023892964,0.0002840278,0.00013656025,0.0003751794,0.00011593548,0.00023293852],"category_scores_gemma":[0.00005771237,0.00015695234,0.00022584638,0.002642422,0.0006209856,0.00036529606,0.00018122086,0.00041576228,0.000087517656],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0036662742,0.0008685517,0.96674097,0.000012309968,0.00011156068,0.00042890437,0.0031366767,0.00071408006,0.0018037946,0.00031282406,0.0019658208,0.020238208],"study_design_scores_gemma":[0.00074705936,0.00047367494,0.87907845,0.000010097863,0.000035671597,0.000113594055,0.00047776077,0.00034992656,0.000038925777,0.0012433344,0.11717188,0.00025963358],"about_ca_topic_score_codex":0.0008300327,"about_ca_topic_score_gemma":0.00010120659,"teacher_disagreement_score":0.11520606,"about_ca_system_score_codex":0.000023977134,"about_ca_system_score_gemma":0.000007473829,"threshold_uncertainty_score":0.64003307},"labels":[],"label_agreement":null},{"id":"W2092588070","doi":"10.1111/j.0435-3676.2005.00276.x","title":"The identification of debris torrent basins using morphometric measures derived within a gis","year":2005,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia, Okanagan Campus; University of British Columbia; Nipissing University","funders":"Nipissing University","keywords":"Digital elevation model; Elevation (ballistics); Geology; Debris; Kurtosis; Structural basin; Standard deviation; Physical geography; Geomorphology; Hydrology (agriculture); Geography; Statistics; Remote sensing; Mathematics; Geometry","score_opus":0.011051637905748472,"score_gpt":0.22593870657362053,"score_spread":0.21488706866787205,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2092588070","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973986,0.00050203427,0.0004737551,0.00066617574,0.00021594582,0.00027405657,0.000033140775,0.00006336112,0.00037289486],"genre_scores_gemma":[0.9986012,0.00034309624,0.000636748,0.00008562929,0.00012048109,0.000027564543,0.000011054356,0.000024419316,0.00014982335],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9976841,0.00010925202,0.00055841985,0.00041724608,0.0007551663,0.00047581014],"domain_scores_gemma":[0.9988345,0.00006909275,0.00036913806,0.0005017917,0.00006856548,0.0001569338],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035007103,0.00026417873,0.00028686956,0.00014830801,0.0005659604,0.00011858257,0.00044960232,0.00009334289,0.00010267939],"category_scores_gemma":[0.00005499881,0.0001556044,0.00040475724,0.0018618243,0.00074550376,0.00041069687,0.00020989115,0.0002394104,0.000059162045],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008164045,0.0022907292,0.34063426,0.0000678817,0.001072624,0.000014114305,0.006151988,0.066737406,0.25766158,0.0005375775,0.0036129334,0.3204025],"study_design_scores_gemma":[0.00092113065,0.00044072387,0.79013336,0.000057814865,0.0003714488,0.000035344758,0.00077246997,0.023707535,0.06753187,0.0016080503,0.113501064,0.00091921055],"about_ca_topic_score_codex":0.000383258,"about_ca_topic_score_gemma":0.00021732405,"teacher_disagreement_score":0.44949907,"about_ca_system_score_codex":0.00004527639,"about_ca_system_score_gemma":0.000015707563,"threshold_uncertainty_score":0.6345363},"labels":[],"label_agreement":null},{"id":"W2094934291","doi":"10.1111/j.0435-3676.2004.00218.x","title":"Holocene alluvial chronology of one tree creek, southern alberta, canada","year":2004,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; University of Glasgow","keywords":"Geology; Radiocarbon dating; Tributary; Fluvial; Chronology; Holocene; Bedrock; Alluvium; Allerød oscillation; Quaternary; Palaeochannel; Alluvial fan; Terrace (agriculture); Geomorphology; Younger Dryas; Paleontology; Archaeology; Structural basin; Geography","score_opus":0.009392677697194428,"score_gpt":0.19811998100968364,"score_spread":0.18872730331248921,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2094934291","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98953843,0.00038893716,0.000011888165,0.002505179,0.00020829737,0.0002153628,0.00017771607,0.000047729907,0.0069064703],"genre_scores_gemma":[0.99842054,0.000069788235,0.00023799652,0.00035089554,0.00017376,0.000007990489,0.00026451005,0.000009078911,0.00046542665],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99749863,0.00015939276,0.00036461916,0.00054981344,0.00044467038,0.0009828447],"domain_scores_gemma":[0.99872303,0.0002246544,0.00015664184,0.00045813888,0.00014642502,0.00029112434],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001325031,0.00030385805,0.0006168375,0.00017228215,0.0003097407,0.000027863762,0.00057022984,0.00020235984,0.0015936403],"category_scores_gemma":[0.000048838436,0.00026227557,0.00028083444,0.00067766773,0.0013370661,0.00018129809,0.0000575074,0.00047045253,0.00020518762],"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":[0.00032441143,0.00017123045,0.99543613,0.000038203874,0.0002320992,0.000043398788,0.0003665003,0.0006712805,0.000012395006,0.00015856134,0.00016722616,0.0023785688],"study_design_scores_gemma":[0.0008412321,0.0008124777,0.9904936,0.00001900346,0.00005988352,0.000045620905,0.00035884627,0.000045557466,0.00026955514,0.0047274325,0.0019928599,0.0003339151],"about_ca_topic_score_codex":0.8546195,"about_ca_topic_score_gemma":0.9774769,"teacher_disagreement_score":0.12285742,"about_ca_system_score_codex":0.0000024349056,"about_ca_system_score_gemma":0.00035616808,"threshold_uncertainty_score":0.99998295},"labels":[],"label_agreement":null},{"id":"W2133058250","doi":"10.1111/j.1468-0459.2011.00447.x","title":"The austrian alps and paraglaciation","year":2012,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Glacial period; Physical geography; Confusion; Geology; Geography; Archaeology; Geomorphology; Psychology","score_opus":0.012004873230985817,"score_gpt":0.2306989497550718,"score_spread":0.21869407652408598,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2133058250","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9872934,0.0023698357,0.000004784846,0.0028350495,0.00030623967,0.00018910412,0.00001981655,0.000060045055,0.0069217156],"genre_scores_gemma":[0.99855906,0.0005231126,0.00005775895,0.00018428659,0.00030474816,0.000009771688,0.00006753098,0.0000034833818,0.0002902692],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982839,0.00022637018,0.00016196627,0.0002330003,0.00024481554,0.00084990554],"domain_scores_gemma":[0.9989643,0.00040072325,0.00006809173,0.00024155265,0.000056040368,0.00026927178],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039375233,0.00018109419,0.00019596034,0.00008849454,0.0009448673,0.00009186421,0.0002156816,0.000104393206,0.00019583944],"category_scores_gemma":[0.00004569157,0.00010414241,0.00012734605,0.00043674945,0.0008631904,0.00045091016,0.000034559143,0.00032289713,0.00024833978],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008653876,0.00002948871,0.9856081,0.000007058254,0.00005707466,0.0000023077955,0.00023558416,0.000007082183,0.0000013944746,0.00064970594,0.00033617546,0.01297948],"study_design_scores_gemma":[0.00015693245,0.00014314527,0.9522849,0.0000029473892,0.00002380494,0.000035564557,0.00021727459,0.0001073065,0.000020092031,0.003004453,0.0438553,0.00014831476],"about_ca_topic_score_codex":0.00015295764,"about_ca_topic_score_gemma":0.0006521078,"teacher_disagreement_score":0.043519124,"about_ca_system_score_codex":3.4145413e-7,"about_ca_system_score_gemma":0.000012970707,"threshold_uncertainty_score":0.7267251},"labels":[],"label_agreement":null},{"id":"W2767863034","doi":"10.1080/04353676.2017.1366830","title":"Sediment loading of alpine debris-flow channels by snow avalanches, Canadian Rocky Mountains","year":2017,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia, Okanagan Campus; University of British Columbia","funders":"University of British Columbia; Parks Canada","keywords":"Deposition (geology); Geology; Debris; Sediment; Debris flow; Hydrology (agriculture); Geomorphology; Snow; Meltwater; Channel (broadcasting); Snowmelt; Geotechnical engineering; Oceanography","score_opus":0.00610813922510684,"score_gpt":0.21084294408452484,"score_spread":0.204734804859418,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2767863034","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98333925,0.00031564853,0.00008197395,0.0028822445,0.00058852934,0.0005098441,0.00044669167,0.00009662127,0.011739219],"genre_scores_gemma":[0.99770594,0.00027968982,0.00024192533,0.00034006865,0.00021571158,0.000045131328,0.000144216,0.000042233125,0.0009851016],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9973888,0.00004758352,0.00034210677,0.0006306927,0.00058041443,0.0010104083],"domain_scores_gemma":[0.9980915,0.000026922027,0.0002832969,0.00089385605,0.000045565816,0.00065882335],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.000170551,0.00041894507,0.0005089142,0.00012642669,0.0009934356,0.00019713912,0.0008519256,0.00018691467,0.00082811585],"category_scores_gemma":[0.00003053644,0.00031487588,0.0004352866,0.00033100168,0.0007716565,0.00060418586,0.00037117157,0.00034962792,0.00020747287],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034583695,0.0011933061,0.8173526,0.00012118405,0.0010639635,0.00012706214,0.0031353533,0.0040760087,0.008836754,0.00021427701,0.10554145,0.057992212],"study_design_scores_gemma":[0.0018172477,0.0010360219,0.41589627,0.0002085281,0.00028087595,0.000031555766,0.00034273212,0.0053257262,0.013698921,0.0024254397,0.5572797,0.0016569669],"about_ca_topic_score_codex":0.074367136,"about_ca_topic_score_gemma":0.009610211,"teacher_disagreement_score":0.45173827,"about_ca_system_score_codex":0.00007318693,"about_ca_system_score_gemma":0.000033300472,"threshold_uncertainty_score":0.9999303},"labels":[],"label_agreement":null},{"id":"W2768003968","doi":"10.1080/04353676.2017.1313095","title":"Volume change of tropical Peruvian glaciers from multi-temporal digital elevation models and volume–surface area scaling","year":2017,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Lethbridge","funders":"National Aeronautics and Space Administration","keywords":"Glacier; Geology; Digital elevation model; Glacier morphology; Volume (thermodynamics); Scaling; Glacier mass balance; Climatology; Remote sensing; Environmental science; Physical geography; Geomorphology; Geography; Ice stream; Cryosphere; Geometry","score_opus":0.0452916285023009,"score_gpt":0.23451787977922578,"score_spread":0.18922625127692488,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2768003968","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952002,0.00068545836,0.0016249531,0.0009245947,0.00020571923,0.0002995166,0.00085494027,0.00006303688,0.00014155662],"genre_scores_gemma":[0.9967184,0.0002127286,0.0022328864,0.000097814685,0.00025070683,0.000008010319,0.00033720187,0.000010625189,0.00013162341],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982885,0.0000315403,0.00031404523,0.0005131224,0.00038307064,0.00046972255],"domain_scores_gemma":[0.99881333,0.00005414809,0.00027544185,0.00047644644,0.00015745741,0.00022317866],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00005779073,0.00030340106,0.00046196394,0.000046392553,0.00086443726,0.00038833296,0.00036409698,0.00009716218,0.00013478215],"category_scores_gemma":[0.000041957,0.00024451123,0.00028163427,0.00024177514,0.0009770558,0.0017518534,0.000102352315,0.00019232716,0.000015853346],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007736707,0.00008106078,0.9787485,0.000018189552,0.00009654724,0.0000036239721,0.000956127,0.0004136283,0.000009981081,0.000035277193,0.00007102385,0.019488648],"study_design_scores_gemma":[0.0003858987,0.0001863745,0.9031541,0.000028065526,0.000048895105,8.7719735e-7,0.0007175636,0.089791246,0.0000060781576,0.0013630472,0.0040285587,0.00028930782],"about_ca_topic_score_codex":0.00731079,"about_ca_topic_score_gemma":0.0011323355,"teacher_disagreement_score":0.08937762,"about_ca_system_score_codex":0.000002756389,"about_ca_system_score_gemma":0.000015949308,"threshold_uncertainty_score":0.9992996},"labels":[],"label_agreement":null},{"id":"W2884021519","doi":"10.1080/04353676.2018.1488538","title":"Global and regional climate responses to national-committed emission reductions under the Paris agreement","year":2018,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Beijing Education Committee Cooperation Building Foundation Project; National Natural Science Foundation of China; Swedish Foundation for International Cooperation in Research and Higher Education; National Key Research and Development Program of China; U.S. Department of Energy","keywords":"Precipitation; Climatology; Climate change; Environmental science; Mean radiant temperature; Global warming; Climate model; Arctic; The arctic; Global temperature; Global change; Mediterranean climate; Coupled model intercomparison project; Range (aeronautics); Geography; Atmospheric sciences; Meteorology; Oceanography; Geology","score_opus":0.010245320110851459,"score_gpt":0.2471726864197758,"score_spread":0.23692736630892433,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2884021519","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9853037,0.00004818517,0.0007710205,0.010090131,0.00011941442,0.0003002042,0.00003428035,0.00007184025,0.0032612425],"genre_scores_gemma":[0.99247235,0.00019225497,0.0030053211,0.0031048032,0.00024262957,0.0000795353,0.000018050257,0.000018145629,0.0008669303],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979576,0.000102557184,0.00022003718,0.0005373853,0.00067287555,0.00050956],"domain_scores_gemma":[0.99923503,0.000046701363,0.000086801454,0.00034014723,0.000029060842,0.00026222673],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017808874,0.00027360217,0.00018262517,0.000018210258,0.0009160437,0.00007912214,0.0002810483,0.0000675187,0.00031403557],"category_scores_gemma":[0.000011864958,0.00018242851,0.00015904022,0.0008461887,0.001605899,0.00026289758,0.0005674076,0.00013331612,0.00015973464],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018338126,0.0012842845,0.8814895,0.000018208433,0.00032349894,0.000008381529,0.0019950122,0.013018784,0.0017379109,0.0036001178,0.0648327,0.029857755],"study_design_scores_gemma":[0.00019009446,0.0003650598,0.88534665,0.000011942399,0.000037783302,0.000024031699,0.0008318657,0.001019179,0.000028260856,0.005538688,0.10632368,0.00028274755],"about_ca_topic_score_codex":0.00031485167,"about_ca_topic_score_gemma":0.00006719024,"teacher_disagreement_score":0.04149098,"about_ca_system_score_codex":0.00008653951,"about_ca_system_score_gemma":0.0000097160655,"threshold_uncertainty_score":0.7439219},"labels":[],"label_agreement":null},{"id":"W2898468399","doi":"10.1080/04353676.2018.1522958","title":"Revisiting glaciological measurements on Haupapa/Tasman Glacier, New Zealand, in a contemporary context","year":2018,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"National Oceanic and Atmospheric Administration; Victoria University; Foundation for Research, Science and Technology; Department of Conservation, New Zealand; University of Victoria; University of Canterbury; Comer Science and Education Foundation","keywords":"Glacier; Context (archaeology); Geology; Geodesy; Geography; Physical geography; Archaeology","score_opus":0.06896654544798415,"score_gpt":0.26308407314366417,"score_spread":0.19411752769568003,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2898468399","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99025387,0.00095711485,0.000015755913,0.0026781862,0.00039431377,0.00041976426,0.00007897941,0.00013617353,0.0050658425],"genre_scores_gemma":[0.99579316,0.00010233922,0.0002522036,0.0021047643,0.0011423638,0.00001098878,0.00014355099,0.00001071851,0.000439892],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9973737,0.00016818935,0.000465853,0.00068647007,0.0005471597,0.0007586347],"domain_scores_gemma":[0.99879336,0.00018631647,0.00017284109,0.0003800932,0.0001549604,0.00031242875],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00030453407,0.00040171787,0.0005682418,0.0001296712,0.00044896788,0.00012606879,0.00037331393,0.00010803166,0.0006806008],"category_scores_gemma":[0.00010642562,0.0002855948,0.00033318132,0.0011826041,0.0005317092,0.00036171556,0.00005447062,0.00033701787,0.0002833659],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043194587,0.00009542448,0.9425702,0.000009569179,0.000088066576,0.000014373565,0.0006239052,0.00004698599,0.000015316242,0.00009276511,0.005063067,0.050948367],"study_design_scores_gemma":[0.0007741139,0.00094862614,0.8615592,0.00007204843,0.000017399176,0.000003168266,0.0005247797,0.00018386397,0.000028561191,0.0013467212,0.13418679,0.0003547054],"about_ca_topic_score_codex":0.005346837,"about_ca_topic_score_gemma":0.00310542,"teacher_disagreement_score":0.12912373,"about_ca_system_score_codex":0.000006425359,"about_ca_system_score_gemma":0.00005772496,"threshold_uncertainty_score":0.99995965},"labels":[],"label_agreement":null},{"id":"W2999114806","doi":"10.1080/04353676.2020.1711665","title":"Boulder barricades in an emerging hypertidal environment: the case of Ungava Bay, northern Quebec, Canada","year":2020,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université Laval; Center for Northern Studies","funders":"","keywords":"Landform; Intertidal zone; Geology; Bay; Coastal geography; Physical geography; Tundra; Oceanography; Sea level; Arctic; Holocene; Coastal erosion; Geomorphology; Geography; Shore","score_opus":0.014458598195903866,"score_gpt":0.2200316560507772,"score_spread":0.20557305785487334,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2999114806","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99199224,0.0006634788,0.000003884042,0.006499648,0.000052407042,0.00021314155,0.000082528815,0.000023019176,0.00046966886],"genre_scores_gemma":[0.9989402,0.00006342349,0.000029732284,0.00073217216,0.0001008818,0.000007968934,0.00008829815,0.0000069511702,0.000030333267],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99790263,0.0003752148,0.00030907555,0.0004588093,0.00029111156,0.0006631299],"domain_scores_gemma":[0.99902236,0.00020396133,0.00009711385,0.00032142046,0.000047356276,0.00030781046],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014192144,0.00025524816,0.00037965993,0.00009415629,0.00032821778,0.000034341774,0.00046105398,0.00009719024,0.00075778447],"category_scores_gemma":[0.000029963045,0.0001664522,0.00015721661,0.00066210615,0.00078913127,0.00028502423,0.000057214966,0.000541379,0.000029765011],"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":[0.0001497103,0.00005302217,0.9920798,0.000029916473,0.00005956458,0.00066437136,0.0012016488,0.002741533,0.000014103806,0.00003713214,0.00009417863,0.0028750005],"study_design_scores_gemma":[0.0002716845,0.0002621494,0.9897383,0.0000065606882,0.00003174644,0.00009992934,0.0023552524,0.003151258,0.00006321623,0.00037903714,0.0033904049,0.00025046556],"about_ca_topic_score_codex":0.492727,"about_ca_topic_score_gemma":0.982051,"teacher_disagreement_score":0.489324,"about_ca_system_score_codex":0.0000015902032,"about_ca_system_score_gemma":0.00012203469,"threshold_uncertainty_score":0.82972085},"labels":[],"label_agreement":null},{"id":"W4379538204","doi":"10.1080/04353676.2023.2217047","title":"The effect of valley confluence and bedrock geology upon the location and depth of glacial overdeepenings","year":2023,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Bedrock; Landform; Glacial period; Geomorphology; Glacial landform; Glacier; Confluence; Physical geography; Paleontology; Moraine; Geography","score_opus":0.007093556366725478,"score_gpt":0.23452380020217217,"score_spread":0.2274302438354467,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4379538204","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968457,0.0011128527,0.000004857722,0.0011988161,0.00008564561,0.00027121246,0.000012875801,0.0000276745,0.0004403419],"genre_scores_gemma":[0.9990483,0.00077322876,0.000009150736,0.000040879917,0.000039261362,0.000010782351,0.000032683583,0.0000031371899,0.0000425812],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99844915,0.00039313454,0.00021736283,0.0002756428,0.0002384067,0.00042630514],"domain_scores_gemma":[0.99786365,0.0015878883,0.00013219044,0.00023376115,0.00010304779,0.000079446436],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005722317,0.00016692268,0.00032038862,0.00011618086,0.00050134916,0.000026579828,0.00027658747,0.00010295708,0.00002492113],"category_scores_gemma":[0.00013442704,0.000085378866,0.00010203731,0.00074537547,0.002299077,0.00012936819,0.00008218563,0.00025816626,0.000016485044],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044986253,0.000006808147,0.9929075,0.00007473126,0.000084257576,0.000003487634,0.00038358147,0.00014089001,0.0000291773,0.00037727228,0.000051728934,0.005490667],"study_design_scores_gemma":[0.0003065088,0.0010869676,0.9934646,0.000012652224,0.000040572508,0.000026694284,0.00017351631,0.0011840336,0.00027430188,0.0025127316,0.000823765,0.00009367396],"about_ca_topic_score_codex":0.00056892954,"about_ca_topic_score_gemma":0.002016899,"teacher_disagreement_score":0.0053969934,"about_ca_system_score_codex":1.8117233e-7,"about_ca_system_score_gemma":0.000018220335,"threshold_uncertainty_score":0.84710455},"labels":[],"label_agreement":null},{"id":"W4394618953","doi":"10.1080/04353676.2024.2321426","title":"Summer snowline altitude gradients in Western Norway are influenced by maritime climate","year":2023,"lang":"en","type":"article","venue":"Geografiska Annaler Series A Physical Geography","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Snow line; Altitude (triangle); Physical geography; Snow; Geography; Effects of high altitude on humans; Oceanography; Climatology; Environmental science; Meteorology; Geology; Snow cover","score_opus":0.013929150504020665,"score_gpt":0.2348289170329885,"score_spread":0.22089976652896784,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4394618953","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958369,0.0005285637,0.000004982357,0.0015073249,0.00031008798,0.00031711272,0.0008323764,0.00020291285,0.00045972175],"genre_scores_gemma":[0.9957466,0.0015401621,0.000095290634,0.0009631414,0.00020214397,0.000040207997,0.00096492533,0.000017785602,0.00042975324],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99728906,0.000075170945,0.00041441043,0.0006311031,0.00047765567,0.0011125912],"domain_scores_gemma":[0.9990076,0.00013791426,0.00014816056,0.00036255887,0.000103136925,0.00024067081],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00016687602,0.00037910722,0.0005027034,0.00019222878,0.00043315938,0.00013392272,0.00039596276,0.00009180406,0.00040096117],"category_scores_gemma":[0.000029467403,0.0003043804,0.00028790254,0.002771002,0.00032725875,0.0005262069,0.000109399596,0.00029540094,0.00077011785],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007184419,0.00012056269,0.9891981,0.000038238824,0.00006420653,0.000030049203,0.00033782158,0.00089506304,0.000019967803,0.000015864343,0.0037376708,0.0054706465],"study_design_scores_gemma":[0.00046073776,0.00017703472,0.9328658,0.00004509801,0.00002521811,0.0000017398062,0.00047854413,0.00094289647,0.000010183334,0.000350736,0.06425133,0.00039070626],"about_ca_topic_score_codex":0.002689692,"about_ca_topic_score_gemma":0.011308939,"teacher_disagreement_score":0.06051366,"about_ca_system_score_codex":0.0000045649813,"about_ca_system_score_gemma":0.00001431617,"threshold_uncertainty_score":0.9999408},"labels":[],"label_agreement":null}]}