{"meta":{"query_hash":"344ddf73c0f9","filters":{"venue":"Geomorphology"},"cohort_total":208,"direct_labels_cover":0,"predictions_cover":208,"exported":208,"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/344ddf73c0f9","api":"https://metacan.xera.ac/api/v1/cohort?venue=Geomorphology"},"results":[{"id":"W1030112141","doi":"10.1016/j.geomorph.2015.07.026","title":"Late-stage phases of glacial Lake Ojibway in the central Abitibi region, eastern Canada","year":2015,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; Université du Québec à Montréal","funders":"Fonds de recherche du Québec – Nature et technologies; Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Deglaciation; Geology; Shelf ice; Shore; Glacial lake; Glacial period; Post-glacial rebound; Ice sheet; Physical geography; Stage (stratigraphy); Paleontology; Oceanography; Geomorphology; Arctic; Arctic ice pack; Geography; Antarctic sea ice","score_opus":0.04163921412098286,"score_gpt":0.24392720341614177,"score_spread":0.2022879892951589,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1030112141","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":[0.9889631,0.0002743248,0.000010140375,0.0020066195,0.00042736117,0.00013310502,0.000110248286,0.0000063040848,0.00806878],"genre_scores_gemma":[0.9980872,0.000015346153,0.00001434891,0.0008526083,0.00005681598,0.0000014352418,0.0002558034,0.0000015677824,0.00071482686],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99844235,0.0004177598,0.0002235472,0.0001939103,0.00018782825,0.0005346123],"domain_scores_gemma":[0.9992653,0.00029411144,0.00007280295,0.00020610366,0.00005214573,0.0001095371],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00045874424,0.000101192076,0.0002198036,0.00006452896,0.000065127126,0.000006251119,0.00036836942,0.00012536382,0.001920493],"category_scores_gemma":[0.00013769188,0.00007127362,0.00002640667,0.00018296794,0.00040524415,0.000049183138,0.000015820453,0.00024908446,0.00007159961],"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":[0.00013779309,0.000019271716,0.992285,0.000006363159,0.000007898147,0.0011611945,0.0003907491,0.0007378469,0.0000010782954,0.000058738293,0.005013705,0.00018033727],"study_design_scores_gemma":[0.0007873961,0.00017262957,0.97985065,0.0000040446366,0.00000625901,0.00033683184,0.0005481957,0.00036086005,0.000020356185,0.0002622366,0.01755921,0.0000913566],"about_ca_topic_score_codex":0.5019528,"about_ca_topic_score_gemma":0.9942444,"teacher_disagreement_score":0.49229157,"about_ca_system_score_codex":0.0000019503173,"about_ca_system_score_gemma":0.00047195647,"threshold_uncertainty_score":0.9989919},"labels":[],"label_agreement":null},{"id":"W1119538749","doi":"10.1016/j.geomorph.2015.08.006","title":"Evolution of a foredune and backshore river complex on a high-energy, drift-aligned beach","year":2015,"lang":"en","type":"article","venue":"Geomorphology","topic":"Coastal and Marine Dynamics","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; Hakai Institute; U.S. Geological Survey; Parks Canada","keywords":"Foredune; Beach morphodynamics; Geology; Overwash; Shore; Supralittoral zone; Plage; Aeolian processes; Accretion (finance); Geomorphology; Progradation; Erosion; Coastal erosion; Sediment transport; Intertidal zone; Oceanography; Sediment; Barrier island; Sedimentary depositional environment","score_opus":0.01761929134605506,"score_gpt":0.20424508775589242,"score_spread":0.18662579640983737,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1119538749","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":[0.9920277,0.00012132492,0.0013198588,0.00034859203,0.000249777,0.000074291784,0.00027755866,0.000021089478,0.0055597927],"genre_scores_gemma":[0.99752676,0.000008727971,0.0007048349,0.00015888372,0.000047011574,7.937271e-7,0.0009961554,0.0000025032675,0.0005543066],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99929726,0.000053120446,0.00014263656,0.00018982652,0.00011734495,0.00019983765],"domain_scores_gemma":[0.99958587,0.000048876333,0.00006329955,0.00013306385,0.00005394371,0.00011494845],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001253734,0.00009759594,0.00018461955,0.00007667509,0.0000413478,0.0000064584465,0.000099603705,0.0000727286,0.00040578443],"category_scores_gemma":[0.000024056126,0.0000811352,0.00002506778,0.000113127164,0.00025168582,0.000051173833,0.000037580005,0.00004580763,0.00002897544],"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":[0.0015075001,0.00021890696,0.6986794,0.00005110442,0.000092921466,0.00018939108,0.00086632936,0.0038944439,0.0006514379,0.120076336,0.038704094,0.13506812],"study_design_scores_gemma":[0.001469934,0.0015357326,0.91280514,0.000008703669,0.000029683644,0.00019902004,0.00024520297,0.022046253,0.000032655178,0.045614347,0.015786847,0.00022650043],"about_ca_topic_score_codex":0.027096037,"about_ca_topic_score_gemma":0.015424319,"teacher_disagreement_score":0.21412571,"about_ca_system_score_codex":0.000006433562,"about_ca_system_score_gemma":0.00003949888,"threshold_uncertainty_score":0.97938263},"labels":[],"label_agreement":null},{"id":"W1825924360","doi":"10.1016/j.geomorph.2015.10.023","title":"Patterns and rates of riverbank erosion involving ice-rich permafrost (yedoma) in northern Alaska","year":2015,"lang":"en","type":"article","venue":"Geomorphology","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":95,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal","funders":"","keywords":"Permafrost; Geology; Erosion; Thermokarst; Bluff; Denudation; Geomorphology; Hydrology (agriculture); Frost weathering; Aggradation; Physical geography; Fluvial; Tectonics; Oceanography; Soil water; Soil science","score_opus":0.049259936692650504,"score_gpt":0.2546201596308474,"score_spread":0.2053602229381969,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1825924360","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":[0.99560094,0.0013708363,0.000004287354,0.00025726992,0.0002752519,0.00011036508,0.0020462149,0.0000103404345,0.0003244661],"genre_scores_gemma":[0.9968537,0.0003676659,0.000025930298,0.00025505596,0.00006710617,0.0000012959766,0.0023757159,0.000004551682,0.000048993705],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990114,0.00009475072,0.0002279019,0.00024139996,0.00012722994,0.00029731],"domain_scores_gemma":[0.9994474,0.00013536752,0.00009061237,0.00014929973,0.000059037433,0.00011826252],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000283328,0.0001281773,0.0002460243,0.00011077784,0.00004795194,0.000018087934,0.00013595693,0.00010971156,0.0015692888],"category_scores_gemma":[0.00004170111,0.00011117797,0.000022159562,0.00014186997,0.00011589442,0.00012940388,0.000040131625,0.00012571104,0.00012204474],"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":[0.000049679813,0.000017408369,0.9956797,0.000021478276,0.0000037953569,0.00007254963,0.0017949161,0.000068563895,0.0013037011,0.0000027626834,0.00037785724,0.0006076172],"study_design_scores_gemma":[0.00069376186,0.00019028701,0.9962571,0.000026286183,0.0000076877595,0.00008393355,0.001258229,0.0004939171,0.00033682285,0.000121756806,0.00040000258,0.00013019191],"about_ca_topic_score_codex":0.020082785,"about_ca_topic_score_gemma":0.37593922,"teacher_disagreement_score":0.35585645,"about_ca_system_score_codex":0.000006163892,"about_ca_system_score_gemma":0.000032252166,"threshold_uncertainty_score":0.9993434},"labels":[],"label_agreement":null},{"id":"W1963625526","doi":"10.1016/j.geomorph.2009.12.008","title":"Reply to comment by Ó Cofaigh, Dowdeswell, King, Anderson, Clark, DJA Evans, J. Evans, Hindmarsh, Lardner and Stokes “Comments on Shaw, J., Pugin, A., Young, R., (2009): A meltwater origin for Antarctic Shelf bedforms with special attention to megalineations.” Geomorphology 102, 364–375","year":2009,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Okanagan University College; University of British Columbia, Okanagan Campus; University of British Columbia; University of Alberta","funders":"","keywords":"Meltwater; Drumlin; Criticism; Oceanography; Geology; Paleontology; Art; Glacial period; Literature","score_opus":0.016596634078487056,"score_gpt":0.26057680681842305,"score_spread":0.243980172739936,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1963625526","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":[0.910624,0.0004786484,0.00126582,0.08219636,0.0010063384,0.0021471495,0.001132866,0.00008353901,0.0010652401],"genre_scores_gemma":[0.928729,0.00015669402,0.0027204652,0.06061082,0.00041903683,0.00009396846,0.0051344,0.000026073567,0.0021095413],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99574506,0.00043591548,0.00064709934,0.0012231501,0.0004370573,0.0015117011],"domain_scores_gemma":[0.99805135,0.000365226,0.00020133445,0.0006039773,0.00022178204,0.00055631244],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011355327,0.000550174,0.0007915198,0.0004925322,0.0007160994,0.000117430354,0.0005279091,0.0004401057,0.004199106],"category_scores_gemma":[0.0001304236,0.0004372424,0.00010603787,0.00033303577,0.00041548975,0.00026807984,0.000058249752,0.00061211357,0.00068574015],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0026620862,0.00020821678,0.6890888,0.00002868284,0.0001298602,0.00018771252,0.0005828408,0.00014488822,0.0002585885,0.0001764284,0.30514485,0.0013869897],"study_design_scores_gemma":[0.0071363444,0.011193798,0.2721724,0.0000920328,0.0002480513,0.0019042403,0.0005403441,0.00036692785,0.0008887513,0.0015180617,0.702762,0.0011770368],"about_ca_topic_score_codex":0.0020646232,"about_ca_topic_score_gemma":0.0066673914,"teacher_disagreement_score":0.41691646,"about_ca_system_score_codex":0.00003221175,"about_ca_system_score_gemma":0.00008742713,"threshold_uncertainty_score":0.99980795},"labels":[],"label_agreement":null},{"id":"W1965959845","doi":"10.1016/s0169-555x(01)00068-x","title":"Annual regime of bedforms, roughness and flow resistance, Lillooet River, British Columbia, BC","year":2001,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":36,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Geology; Thalweg; Flume; Geomorphology; Bedform; Hydrology (agriculture); Sediment; Geometry; Sediment transport; Flow (mathematics); Mathematics; Geotechnical engineering","score_opus":0.004753572624456613,"score_gpt":0.18980694452530064,"score_spread":0.18505337190084403,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1965959845","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":[0.9937106,0.00043559325,0.00019044921,0.00022614122,0.00011943354,0.00012936314,0.00020034627,0.00003299868,0.004955127],"genre_scores_gemma":[0.9849895,0.0006060888,0.00083702366,0.0004591171,0.000026262327,0.000014307949,0.00007316264,0.000011410727,0.01298313],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988673,0.000038961807,0.00024447642,0.00036351246,0.0001444254,0.00034136418],"domain_scores_gemma":[0.9995794,0.00004000558,0.00008879228,0.00018781568,0.000016629498,0.00008733883],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00020084062,0.00009639584,0.00026044447,0.000017527884,0.00014724332,0.00001074629,0.00019842834,0.00018323286,0.008110553],"category_scores_gemma":[0.00001969153,0.00013650309,0.000033034034,0.00018877468,0.0011292067,0.00021732917,0.000077093646,0.00013212334,0.000092792325],"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":[0.00015015574,0.00022898708,0.92465883,0.000038599763,0.000037850692,0.000975001,0.00074373855,0.00017124697,0.00047463956,0.000027021899,0.06316346,0.009330462],"study_design_scores_gemma":[0.0013997915,0.00024131889,0.6200665,0.000025299067,0.000049945647,0.0006296845,0.00011166085,0.000046775476,0.00017664564,0.0027717247,0.37417525,0.00030534624],"about_ca_topic_score_codex":0.015519265,"about_ca_topic_score_gemma":0.09651757,"teacher_disagreement_score":0.3110118,"about_ca_system_score_codex":0.000018375047,"about_ca_system_score_gemma":0.0000126096775,"threshold_uncertainty_score":0.9927962},"labels":[],"label_agreement":null},{"id":"W1969125149","doi":"10.1016/j.geomorph.2004.02.017","title":"Till—as a glacial “tectomict”, its internal architecture, and the development of a “typing” method for till differentiation","year":2005,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":133,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Brock University","funders":"","keywords":"Geology; Glacial period; Glacier; Deposition (geology); Geomorphology; Paleontology; Timeline; Tectonics; Earth science; Geochemistry; Archaeology; Structural basin","score_opus":0.00819014898037576,"score_gpt":0.24835859401120985,"score_spread":0.2401684450308341,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1969125149","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":[0.92392445,0.00008502263,0.073021606,0.0008284691,0.00015509829,0.0003290293,0.000009090582,0.000012938092,0.0016342802],"genre_scores_gemma":[0.977408,0.000014791969,0.021582711,0.00030474865,0.000054805423,0.000033106273,0.000011063108,0.000008845631,0.00058191613],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9992462,0.00006750721,0.00022864906,0.00018654356,0.00008472725,0.00018639062],"domain_scores_gemma":[0.9996401,0.00010949739,0.00011196033,0.00009073219,0.000009280111,0.000038441467],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003699277,0.000095966076,0.0001716348,0.000028643073,0.00010031601,0.000009819545,0.00013544255,0.000089924186,0.00087592803],"category_scores_gemma":[0.000049309314,0.0000558045,0.000049136448,0.00005013852,0.00013877549,0.000025837537,0.00014833441,0.00011015532,0.000051745068],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00575054,0.00028247994,0.0056809764,0.00006718098,0.0004209022,0.000007431902,0.020834852,0.0036470904,0.11378093,0.0048529613,0.0020534052,0.84262127],"study_design_scores_gemma":[0.027276339,0.0008973564,0.12272169,0.00009936772,0.00041340932,0.0011730024,0.00029491915,0.063046664,0.18713044,0.01519285,0.58061254,0.0011414015],"about_ca_topic_score_codex":0.00005106008,"about_ca_topic_score_gemma":0.00024715043,"teacher_disagreement_score":0.84147984,"about_ca_system_score_codex":0.0000403506,"about_ca_system_score_gemma":0.000013130004,"threshold_uncertainty_score":0.95907974},"labels":[],"label_agreement":null},{"id":"W1969566724","doi":"10.1016/j.geomorph.2010.09.030","title":"Making riverscapes real","year":2011,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":215,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institut National de la Recherche Scientifique","funders":"","keywords":"Fluvial; Geology; Channel (broadcasting); Elevation (ballistics); Froude number; Habitat; Structural basin; Scale (ratio); Hydrology (agriculture); Remote sensing; Ecology; Geomorphology; Cartography; Geography; Computer science; Flow (mathematics); Geotechnical engineering","score_opus":0.038987776785536436,"score_gpt":0.2400924681021419,"score_spread":0.20110469131660547,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1969566724","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":[0.81803876,0.000010151872,0.00027230356,0.00006724982,0.00011216428,0.000041529223,0.000002432316,0.000048456775,0.18140694],"genre_scores_gemma":[0.9977681,0.000021540325,0.0011364976,0.00063272007,0.000015063629,0.000006612318,0.00000723642,0.000005658534,0.00040659538],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993698,0.000023378201,0.00009857944,0.00020799684,0.000062670755,0.00023759936],"domain_scores_gemma":[0.99979144,0.000012877895,0.00003299197,0.00012333115,0.0000024223714,0.00003690672],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00009985906,0.00007518325,0.00009098068,0.000017851247,0.000082527156,0.0000015509567,0.00017494445,0.00009026478,0.06914212],"category_scores_gemma":[0.00000438625,0.000069498165,0.000024271289,0.00007286867,0.0002975923,0.00008438998,0.000052228643,0.00008346866,0.0028844802],"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":[0.00008796963,0.000110106404,0.98612136,0.000004072165,0.000017578957,0.0004141001,0.002064413,0.0000657646,0.0035627347,0.0014581569,0.0033830188,0.002710752],"study_design_scores_gemma":[0.00048978394,0.00023937284,0.9473505,0.0000034849347,0.000038317132,0.0001272063,0.00009337099,0.00006871749,0.0044230125,0.005453477,0.0414474,0.000265368],"about_ca_topic_score_codex":0.00038431777,"about_ca_topic_score_gemma":0.0002849355,"teacher_disagreement_score":0.18100035,"about_ca_system_score_codex":0.000013347195,"about_ca_system_score_gemma":0.0000039815513,"threshold_uncertainty_score":0.9978919},"labels":[],"label_agreement":null},{"id":"W1969716855","doi":"10.1016/s0169-555x(01)00057-5","title":"Channel morphology, gradient profiles and bed stresses during flood in a step–pool channel","year":2001,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":235,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Channel (broadcasting); Shear stress; Geotechnical engineering; Flood myth; Range (aeronautics); Flow (mathematics); Debris; Geomorphology; Hydrology (agriculture); Geometry; Mechanics; Materials science; Mathematics; Composite material","score_opus":0.009888232815672098,"score_gpt":0.2098035161106148,"score_spread":0.19991528329494268,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1969716855","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":[0.9971973,0.00039874596,0.000111872476,0.0011465346,0.00017203306,0.0003458259,0.000027009912,0.00006620188,0.0005345077],"genre_scores_gemma":[0.9984278,0.0004924097,0.00009412487,0.00044979833,0.000043315882,0.00012699398,0.00005535656,0.000019513469,0.00029065576],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981355,0.000084075946,0.000316317,0.00063341606,0.00013445487,0.0006962373],"domain_scores_gemma":[0.99949396,0.000048978913,0.00008493195,0.00022971556,0.000007947501,0.00013447649],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00022210437,0.00024817136,0.00033439833,0.0001238516,0.00016858568,0.000009688967,0.00024177902,0.00024468737,0.0026480698],"category_scores_gemma":[0.000027256032,0.00023659503,0.000035844125,0.00028592092,0.00060138473,0.00017947107,0.00015775014,0.00027463806,0.0002166184],"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":[0.000723575,0.0010712887,0.9504081,0.00010915881,0.000077772915,0.0052614226,0.0027585488,0.0056534316,0.03139831,0.0000992318,0.0011242178,0.0013149296],"study_design_scores_gemma":[0.004653452,0.00065887277,0.96281797,0.00005020984,0.00006848497,0.0025705057,0.0006220638,0.0011608931,0.021813262,0.0014724939,0.0032997262,0.0008120437],"about_ca_topic_score_codex":0.0008140622,"about_ca_topic_score_gemma":0.0015801333,"teacher_disagreement_score":0.012409883,"about_ca_system_score_codex":0.000044301887,"about_ca_system_score_gemma":0.000010972719,"threshold_uncertainty_score":0.99826366},"labels":[],"label_agreement":null},{"id":"W1969725788","doi":"10.1016/j.geomorph.2010.02.016","title":"Status and evolution of the cryosphere in the Andes of Santiago (Chile, 33.5°S.)","year":2010,"lang":"en","type":"article","venue":"Geomorphology","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":103,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada; Deutscher Akademischer Austauschdienst; Department of Foreign Affairs and Trade, Australian Government","keywords":"Glacier; Rock glacier; Geology; Permafrost; Physical geography; Debris; Transect; Climate change; Context (archaeology); Landform; Hydrology (agriculture); Geomorphology; Geography; Oceanography","score_opus":0.014774356759891801,"score_gpt":0.22330371761676135,"score_spread":0.20852936085686954,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1969725788","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":[0.9963188,0.000559131,0.0000016273253,0.0003056916,0.00023848691,0.000091019465,0.00084160344,0.0000019334823,0.0016416912],"genre_scores_gemma":[0.99957407,0.00013103332,0.00001780862,0.00013779993,0.000032063374,4.8516546e-7,0.00009218944,0.0000010166162,0.000013540337],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994908,0.00007005109,0.00012319435,0.00008832745,0.00007663134,0.00015097985],"domain_scores_gemma":[0.9995955,0.0001443552,0.00006736913,0.00015835675,0.00001751934,0.000016905598],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021624756,0.00005121433,0.0001010946,0.000020481339,0.000045719135,0.0000050917884,0.00014037156,0.000062174004,0.0033742238],"category_scores_gemma":[0.00003263072,0.000027424621,0.000021181939,0.00012723329,0.00028643716,0.000035154495,0.000014348031,0.00013709792,0.000008384806],"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":[0.000017122118,0.00000986339,0.9929086,0.000010020329,0.0000020751531,0.0000020043162,0.0006100529,0.000011772806,0.0047445344,0.00012925224,0.00040989462,0.001144792],"study_design_scores_gemma":[0.0001742245,0.000054264132,0.9966825,0.0000047770773,0.000006046423,0.000042529642,0.00050606177,0.00011847565,0.00024156473,0.0006131081,0.0015231329,0.000033271306],"about_ca_topic_score_codex":0.022014542,"about_ca_topic_score_gemma":0.20054704,"teacher_disagreement_score":0.1785325,"about_ca_system_score_codex":7.226227e-7,"about_ca_system_score_gemma":0.000021539825,"threshold_uncertainty_score":0.99753684},"labels":[],"label_agreement":null},{"id":"W1971829049","doi":"10.1016/j.geomorph.2014.12.015","title":"The raft of the Saint-Jean River, Gaspé (Québec, Canada): A dynamic feature trapping most of the wood transported from the catchment","year":2014,"lang":"en","type":"article","venue":"Geomorphology","topic":"Soil erosion and sediment transport","field":"Agricultural and Biological Sciences","cited_by":50,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Rimouski; Center for Northern Studies; Université Laval","funders":"Natural Sciences and Engineering Research Council of Canada; Université du Québec à Rimouski","keywords":"River delta; Geology; Delta; Hydrology (agriculture); Channel (broadcasting); Drainage basin; Peninsula; Natural (archaeology); Erosion; Geomorphology; Archaeology; Geography; Paleontology; Geotechnical engineering","score_opus":0.005326478168768396,"score_gpt":0.16511083661726558,"score_spread":0.1597843584484972,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1971829049","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":[0.92329514,0.0003938808,0.0000056694066,0.07529168,0.00043125413,0.00029280028,0.00019267091,0.000010823344,0.00008605388],"genre_scores_gemma":[0.9966549,0.00008917037,0.0000032567375,0.0027176237,0.000046956553,0.00001185124,0.000058380352,0.0000015597134,0.00041626723],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9986575,0.00023040961,0.00028332986,0.00022224135,0.00032427488,0.00028220643],"domain_scores_gemma":[0.99880314,0.0006393399,0.00020103315,0.0002503299,0.000058546477,0.00004762688],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002868899,0.00015397367,0.00021881156,0.0000030933038,0.00047153526,0.000007995517,0.0009466576,0.00010666197,0.00020193205],"category_scores_gemma":[0.000042236083,0.00003514188,0.00016236604,0.00025348895,0.00050528935,0.00001440407,0.000045018915,0.00025983324,0.0000014022936],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041777713,0.00038082068,0.2827127,0.000019858197,0.00036727265,0.000013565354,0.0029297203,0.00035831728,0.6065582,0.0012547504,0.055048626,0.049938384],"study_design_scores_gemma":[0.00033887578,0.000070389266,0.8797259,0.000026634736,0.000052933727,0.000005074794,0.0005865247,0.00016768712,0.003293847,0.0001190911,0.115512796,0.000100244826],"about_ca_topic_score_codex":0.74363065,"about_ca_topic_score_gemma":0.9707941,"teacher_disagreement_score":0.60326433,"about_ca_system_score_codex":0.00004973534,"about_ca_system_score_gemma":0.00009947735,"threshold_uncertainty_score":0.36267155},"labels":[],"label_agreement":null},{"id":"W1972966243","doi":"10.1016/j.geomorph.2004.09.029","title":"Fluid flow and sediment transport processes in geomorphology: innovations, insights, and advances in measurement","year":2004,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal; University of Victoria","funders":"","keywords":"Geology; Sediment transport; Geomorphology; Sediment; Flow (mathematics); Geotechnical engineering; Hydrology (agriculture); Mechanics","score_opus":0.010635929750769237,"score_gpt":0.21317050279739472,"score_spread":0.20253457304662548,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1972966243","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":[0.99114084,0.0057943217,0.00058394583,0.0014513478,0.00008654033,0.0003530573,0.000012694591,0.000029376539,0.00054784515],"genre_scores_gemma":[0.995057,0.0028647883,0.0007733144,0.0011017547,0.000012367351,0.000104497034,0.000060852988,0.000012040562,0.000013379681],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983157,0.000042301595,0.0004353255,0.00057203276,0.00022920972,0.0004054117],"domain_scores_gemma":[0.99965394,0.000031957723,0.000070535585,0.00014247054,0.000023992408,0.000077091325],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046130404,0.00022020329,0.00031819666,0.0001683014,0.00009540109,0.000005812914,0.0001389277,0.00019137141,0.00056395144],"category_scores_gemma":[0.00004088802,0.00020688403,0.000012521746,0.00057538477,0.0006168015,0.0003838917,0.000043949556,0.00023992357,0.000029905523],"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":[0.00026412768,0.0006563601,0.9647116,0.00018276573,0.000018802613,0.00074427656,0.003523137,0.0136400815,0.010640976,0.00055098545,0.00006541019,0.0050014593],"study_design_scores_gemma":[0.00912526,0.0009039621,0.8961188,0.00016841666,0.00005797974,0.0005167057,0.00044846983,0.00013639024,0.011995394,0.014074885,0.065480284,0.00097341515],"about_ca_topic_score_codex":0.0005157191,"about_ca_topic_score_gemma":0.013560508,"teacher_disagreement_score":0.06859279,"about_ca_system_score_codex":0.000116770476,"about_ca_system_score_gemma":0.0000723086,"threshold_uncertainty_score":0.8436486},"labels":[],"label_agreement":null},{"id":"W1973094330","doi":"10.1016/j.geomorph.2013.03.017","title":"Correlating river terrace remnants using an Equotip hardness tester: An example from the Miño River, northwestern Iberian Peninsula","year":2013,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Windsor","funders":"Fundação para a Ciência e a Tecnologia; Centro Interdisciplinar de Investigação Marinha e Ambiental; Universidade de Santiago de Compostela; Universidade do Porto","keywords":"Terrace (agriculture); Geology; River terraces; Weathering; Peninsula; Geomorphology; Geochemistry; Tectonics; Sedimentary depositional environment; Clastic rock; Fluvial; Paleontology; Archaeology; Sedimentary rock; Geography","score_opus":0.08078034941331338,"score_gpt":0.2628150180691498,"score_spread":0.18203466865583642,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1973094330","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":[0.997178,0.0003025317,0.00020428869,0.00022122332,0.0011435569,0.00040981313,0.00013859947,0.000063896885,0.0003380759],"genre_scores_gemma":[0.99545604,0.000017217444,0.001997439,0.0008227094,0.00019826916,0.000006372577,0.0011491353,0.000011360565,0.00034144623],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99671364,0.001023003,0.00038314698,0.000728752,0.00022640171,0.00092503964],"domain_scores_gemma":[0.99792004,0.00070406165,0.00019514823,0.0007714646,0.00012109595,0.0002881941],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0005729088,0.00028346915,0.00040497567,0.00008572585,0.0008102694,0.00009574904,0.00084222807,0.00037473193,0.011174083],"category_scores_gemma":[0.00005453059,0.0002088776,0.00006133723,0.00019478933,0.0012306221,0.0006757872,0.000094343704,0.00058745866,0.002039286],"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":[0.000059153565,0.000043163815,0.992893,0.000003921157,0.00003172888,0.00018620663,0.0036858867,0.00044292994,0.00018641428,0.000006283613,0.00014604932,0.002315293],"study_design_scores_gemma":[0.0007267308,0.00024283704,0.9764668,0.0000117367235,0.00003230225,0.0007280334,0.0009262132,0.019084716,0.000032407053,0.00079070695,0.0006809062,0.0002766526],"about_ca_topic_score_codex":0.22098474,"about_ca_topic_score_gemma":0.085925445,"teacher_disagreement_score":0.1350593,"about_ca_system_score_codex":0.0000034841908,"about_ca_system_score_gemma":0.00008160153,"threshold_uncertainty_score":0.99873775},"labels":[],"label_agreement":null},{"id":"W1973976666","doi":"10.1016/j.geomorph.2012.10.020","title":"Retracing the Quaternary history of sea-level changes in the Spanish Mediterranean–Atlantic coasts: Geomorphological and sedimentological approach","year":2012,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Geology; Quaternary; Interglacial; Glacial period; Marine isotope stage; Pleistocene; Mediterranean climate; Sea level; Oceanography; Sedimentary rock; Holocene; Paleontology; Context (archaeology); Climate change; Quaternary science; Archaeology; Geography","score_opus":0.09830143133914533,"score_gpt":0.25793505324452126,"score_spread":0.15963362190537594,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1973976666","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":[0.9886609,0.0044015255,0.000038527727,0.0025443109,0.00057431235,0.00029394327,0.000042274547,0.000015435176,0.0034288135],"genre_scores_gemma":[0.99736637,0.00024917917,0.00023681081,0.0015683236,0.00014345201,0.000012129799,0.0002803379,0.0000029941928,0.00014039804],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9971518,0.001247854,0.00028624316,0.000301888,0.00026040664,0.00075179833],"domain_scores_gemma":[0.9981562,0.0012943501,0.00012529841,0.00029646282,0.000029295003,0.00009843274],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.002784534,0.00018228634,0.0003765122,0.00010278191,0.0001301594,0.000008159905,0.0005359528,0.00034199067,0.0020204831],"category_scores_gemma":[0.00015183527,0.000095246054,0.000043566983,0.00015305984,0.0018236556,0.000078692705,0.00006864936,0.00072346476,0.000079773396],"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":[0.00011654457,0.00007717923,0.9945843,0.000030672014,0.00001882199,0.00019075835,0.0018002349,0.000010686822,0.000041183943,0.00015684665,0.0025416538,0.0004311041],"study_design_scores_gemma":[0.0004143401,0.00027777159,0.98891884,0.0000077154555,0.000025591571,0.0053305426,0.0009575736,0.00069271534,0.000012701898,0.00020183236,0.003035369,0.0001250082],"about_ca_topic_score_codex":0.0024327454,"about_ca_topic_score_gemma":0.0040976056,"teacher_disagreement_score":0.008705517,"about_ca_system_score_codex":0.00000536029,"about_ca_system_score_gemma":0.000041457097,"threshold_uncertainty_score":0.99889183},"labels":[],"label_agreement":null},{"id":"W1974232401","doi":"10.1016/s0169-555x(00)00046-5","title":"The effect of bedload transport on mean and turbulent flow properties","year":2000,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":59,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institut National de la Recherche Scientifique","funders":"University at Buffalo; National Science Council","keywords":"Bed load; Flume; Turbulence; Hyperconcentrated flow; Geology; Acoustic Doppler velocimetry; Bedform; Sediment transport; Turbulence kinetic energy; Flow velocity; Flow (mathematics); Mechanics; Geotechnical engineering; Sediment; Geomorphology; Physics; Laser Doppler velocimetry; Blood flow","score_opus":0.004883420599732127,"score_gpt":0.18343637637817653,"score_spread":0.1785529557784444,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1974232401","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":[0.996263,0.00024602032,0.0000046569917,0.00072773045,0.00003969048,0.00017044836,0.0000043967275,0.000017321421,0.0025267107],"genre_scores_gemma":[0.9987144,0.00021494093,0.00001451283,0.000255857,0.0000100245015,0.000022656353,0.000007787496,0.000005834981,0.0007539909],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992584,0.00006510164,0.00014949839,0.00020328516,0.000112512476,0.0002112143],"domain_scores_gemma":[0.99971634,0.00006353575,0.000025419275,0.00015185596,0.000002071208,0.000040774106],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002619959,0.00010832466,0.00015507515,0.000009871543,0.00014948234,0.0000023447433,0.00014098677,0.000078028555,0.004568024],"category_scores_gemma":[0.000004091791,0.000060760878,0.000031553882,0.000052017866,0.0006915437,0.000037886057,0.0000076685965,0.000107831605,0.00020451851],"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":[0.008175962,0.00044841378,0.55008805,0.00018446169,0.00025458593,0.0005394508,0.0056257197,0.046469666,0.031038214,0.00010329394,0.0043754694,0.35269672],"study_design_scores_gemma":[0.005994046,0.012376383,0.39235827,0.000086802305,0.00034805268,0.00071694783,0.00007848392,0.0021929878,0.3000394,0.00050873484,0.28433526,0.00096460636],"about_ca_topic_score_codex":0.00010199684,"about_ca_topic_score_gemma":0.00013908479,"teacher_disagreement_score":0.3517321,"about_ca_system_score_codex":0.000007987616,"about_ca_system_score_gemma":0.0000032437042,"threshold_uncertainty_score":0.99634194},"labels":[],"label_agreement":null},{"id":"W1977946933","doi":"10.1016/s0169-555x(99)00097-5","title":"Canadian geomorphology 2000","year":2000,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia; Simon Fraser University","funders":"","keywords":"Geology; Geomorphology","score_opus":0.010668295940895382,"score_gpt":0.21094795064778155,"score_spread":0.20027965470688616,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1977946933","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":[0.84507936,0.0007139681,0.0000031585334,0.0040463,0.000385326,0.00014830785,0.00019885399,0.000048841484,0.14937586],"genre_scores_gemma":[0.9803815,0.00015417018,0.00018945965,0.0038686253,0.00009794739,0.0000039647907,0.0009849119,0.0000051828265,0.014314244],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99759513,0.0003093809,0.00025057726,0.00046260143,0.000119024895,0.0012632799],"domain_scores_gemma":[0.998842,0.00020291707,0.0000329734,0.00037851307,0.000044578588,0.0004990093],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00042828757,0.0001908771,0.0003122059,0.0002470779,0.0003859572,0.000018038556,0.0004715484,0.00043934397,0.5853516],"category_scores_gemma":[0.000039912262,0.00017768168,0.00006532217,0.00029104028,0.00056501373,0.00008640358,0.000008877474,0.00047731175,0.06384043],"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":[0.00006215319,0.000009669165,0.9803466,0.000002727213,0.000020650117,0.0013184699,0.00007143306,0.00028013944,0.0000032525145,0.00009592401,0.009228227,0.008560749],"study_design_scores_gemma":[0.0004674911,0.00019629067,0.7631522,0.000002063055,0.000012639294,0.004281421,0.000028008317,0.00030255286,0.000018352253,0.001456681,0.22985375,0.00022857194],"about_ca_topic_score_codex":0.34715056,"about_ca_topic_score_gemma":0.8613284,"teacher_disagreement_score":0.5215112,"about_ca_system_score_codex":0.000006434059,"about_ca_system_score_gemma":0.0004948418,"threshold_uncertainty_score":0.93688846},"labels":[],"label_agreement":null},{"id":"W1978178178","doi":"10.1016/j.geomorph.2007.11.005","title":"The role of morphology on the displacement of particles in a step–pool river system","year":2007,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":91,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal","funders":"Canada Research Chairs","keywords":"Clastic rock; Geology; Sediment transport; Sediment; Geomorphology; Stream power; River morphology; Bed load; Channel (broadcasting); Hydrology (agriculture); Geotechnical engineering","score_opus":0.006118125217702383,"score_gpt":0.20528936294832154,"score_spread":0.19917123773061915,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1978178178","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":[0.9964766,0.00013684438,0.00023912931,0.0004737423,0.00007638045,0.0002178998,0.000007509375,0.0000080922855,0.0023637945],"genre_scores_gemma":[0.99966335,0.000018547833,0.000047027035,0.00018315921,0.000007659552,0.000021395826,0.0000029268037,0.0000051826164,0.00005073151],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988643,0.000118372445,0.00035547867,0.00018174815,0.00015556854,0.0003245476],"domain_scores_gemma":[0.9991129,0.00044334342,0.00014051232,0.00026415812,0.00000786922,0.000031212614],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011451194,0.00009358457,0.0001722365,0.000026668808,0.00008939888,0.0000014506568,0.00030459464,0.00009083146,0.0006309019],"category_scores_gemma":[0.000028270506,0.0000530422,0.000037113645,0.0001600487,0.0010138465,0.000026085097,0.0000626875,0.0001318227,0.000114622744],"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":[0.001203286,0.00049010536,0.8545134,0.000028307324,0.000065704415,0.00013623979,0.0021509863,0.0030630226,0.096748605,0.032763354,0.0006345735,0.008202409],"study_design_scores_gemma":[0.0016641942,0.0010563008,0.6791007,0.000041696363,0.000065876106,0.0000984871,0.0036990698,0.0013550076,0.2891788,0.0025780916,0.020905057,0.00025672122],"about_ca_topic_score_codex":0.00056499854,"about_ca_topic_score_gemma":0.00089225254,"teacher_disagreement_score":0.1924302,"about_ca_system_score_codex":0.000037348145,"about_ca_system_score_gemma":0.000008593974,"threshold_uncertainty_score":0.69079334},"labels":[],"label_agreement":null},{"id":"W1978949875","doi":"10.1016/j.geomorph.2006.09.002","title":"Lithologic control of debris torrent occurrence","year":2007,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":27,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Debris; Geology; Watershed; Lithology; Sediment; Weathering; Debris flow; Geomorphology; Colluvium; Hydrology (agriculture); Geochemistry; Alluvium; Oceanography","score_opus":0.00775909503184333,"score_gpt":0.22862367304585507,"score_spread":0.22086457801401174,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1978949875","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":[0.9811425,0.0001952798,0.010205791,0.00016943157,0.0005216056,0.00012013792,0.00003693476,0.000027024245,0.0075812517],"genre_scores_gemma":[0.999041,0.000031459054,0.0003193767,0.0003486589,0.000021408456,0.0000025525858,0.000011446742,0.000003472768,0.0002205963],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99908596,0.000034468765,0.00023241846,0.00020325503,0.00012809983,0.000315786],"domain_scores_gemma":[0.9995516,0.000077676596,0.000098386685,0.00018710895,0.000009065969,0.000076171455],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004530937,0.000089477006,0.00017281702,0.000025637974,0.000044365952,0.0000027787949,0.00018126135,0.00013058861,0.005896819],"category_scores_gemma":[0.00003958691,0.00006437795,0.000054128595,0.00012860024,0.00030584153,0.000032283035,0.00008692639,0.00013130132,0.0005546579],"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":[0.00025181306,0.00025797155,0.90459216,0.000009587061,0.000035331585,0.0003653531,0.00033609843,0.0007787599,0.028288165,0.00036329025,0.019477775,0.045243714],"study_design_scores_gemma":[0.0024560627,0.00076014095,0.8402906,0.000013647023,0.00007248751,0.0006161864,0.00010755385,0.00033600247,0.00997204,0.00092456123,0.14404486,0.00040587832],"about_ca_topic_score_codex":0.00019276036,"about_ca_topic_score_gemma":0.000058507983,"teacher_disagreement_score":0.124567084,"about_ca_system_score_codex":0.00003743401,"about_ca_system_score_gemma":0.000005815365,"threshold_uncertainty_score":0.9950119},"labels":[],"label_agreement":null},{"id":"W1979680497","doi":"10.1016/j.geomorph.2014.05.019","title":"Modeling temporal trends in bedload transport in gravel-bed streams using hierarchical mixed-effects models","year":2014,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Bed load; STREAMS; Geology; Fluvial; Sediment transport; Hyperconcentrated flow; Sediment; Shear stress; Hydrology (agriculture); Geomorphology; Geotechnical engineering","score_opus":0.01738073963943397,"score_gpt":0.2400402517339368,"score_spread":0.22265951209450285,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1979680497","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":[0.97392416,0.000039789113,0.024420787,0.00020408627,0.00013578433,0.00013441274,0.000007779862,0.00003882171,0.0010943759],"genre_scores_gemma":[0.9975911,0.000008547614,0.0018129641,0.0003453556,0.000025415227,0.000025931078,0.00013067626,0.000020655161,0.000039398143],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9979133,0.00016586183,0.00045449683,0.00060705433,0.00019787162,0.0006614289],"domain_scores_gemma":[0.9995316,0.000055454933,0.00004877638,0.0002375035,0.0000043804143,0.00012225317],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00052624487,0.00024654105,0.00043433538,0.000238146,0.00007487451,0.0000052052824,0.00028113433,0.00032009734,0.0007399892],"category_scores_gemma":[0.000009234199,0.00024419744,0.000070562855,0.00045214136,0.00028966318,0.00023779186,0.000042374377,0.0004833805,0.000036530226],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012834449,0.00024354593,0.2788737,0.000015631918,0.0000075599683,0.00026358268,0.0006074178,0.7097349,0.0030856559,0.00031716152,0.000010201655,0.0067122523],"study_design_scores_gemma":[0.0021602125,0.0002151018,0.04164479,0.000028758119,0.000027570544,0.00006534142,0.000025334077,0.9435172,0.0010308404,0.010773942,0.00010715346,0.0004037568],"about_ca_topic_score_codex":0.0053473315,"about_ca_topic_score_gemma":0.00954712,"teacher_disagreement_score":0.23722893,"about_ca_system_score_codex":0.00007833479,"about_ca_system_score_gemma":0.000016713304,"threshold_uncertainty_score":0.99580824},"labels":[],"label_agreement":null},{"id":"W1988178827","doi":"10.1016/s0169-555x(01)00135-0","title":"Particle size and sorting characteristics of sand in transport on the stoss slope of a small reversing dune","year":2002,"lang":"en","type":"article","venue":"Geomorphology","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Trent University; University of Guelph","funders":"Natural Sciences and Engineering Research Council of Canada; Geological Society of America","keywords":"Geology; Sediment transport; Sorting; Geomorphology; Aeolian processes; Grain size; Sand dune stabilization; Crest; Graded bedding; Range (aeronautics); Sediment; Sedimentary depositional environment","score_opus":0.02066629370004398,"score_gpt":0.18956004497319212,"score_spread":0.16889375127314815,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1988178827","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":[0.99835294,0.00025578396,0.000019981606,0.00043394984,0.000046538993,0.00007925498,0.000026809772,0.0000034621132,0.00078127545],"genre_scores_gemma":[0.99957186,0.00008611693,0.00009817524,0.00018211859,0.000013017256,3.9457555e-7,0.00000474165,0.0000016205831,0.000041937517],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994348,0.00004262926,0.00019565305,0.0001073876,0.00005491043,0.0001646096],"domain_scores_gemma":[0.99945706,0.0003171068,0.00010108767,0.00008056059,0.000014190347,0.000030005025],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00024754828,0.000058136466,0.00016721674,0.000016181617,0.000042621225,0.000002755663,0.00006636839,0.00004063942,0.001049204],"category_scores_gemma":[0.00009728895,0.000041119736,0.000016839842,0.00010723575,0.00013367903,0.000026931242,0.0000041658286,0.00007966231,0.000009061514],"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":[0.00009975804,0.000031088144,0.9790709,0.00008051705,0.000007909245,0.000053793312,0.0013133144,0.00029930763,0.0015926614,0.000042336025,0.000023052751,0.017385358],"study_design_scores_gemma":[0.00031003242,0.00023525648,0.9912935,0.000042893833,0.000010584517,0.000028224844,0.0001321944,0.006306507,0.0013557028,0.0000941207,0.00013102344,0.000059949736],"about_ca_topic_score_codex":0.0005385521,"about_ca_topic_score_gemma":0.00044039384,"teacher_disagreement_score":0.017325409,"about_ca_system_score_codex":8.72819e-7,"about_ca_system_score_gemma":0.000005488728,"threshold_uncertainty_score":0.999864},"labels":[],"label_agreement":null},{"id":"W1993082896","doi":"10.1016/j.geomorph.2011.04.013","title":"Late glacial retreat and Neoglacial advance sequences in the Zillertal Alps, Austria","year":2011,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Brock University; McMaster University","funders":"Connaught Fund; University of Toronto; York University","keywords":"Moraine; Geology; Younger Dryas; Glacial period; Massif; Deglaciation; Geomorphology; Holocene; Physical geography; Paleontology; Geography","score_opus":0.03511493774810247,"score_gpt":0.24508160813497956,"score_spread":0.2099666703868771,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1993082896","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":[0.9788057,0.00061655656,0.0000042255015,0.00070722494,0.00040605225,0.00015696736,0.000022414355,0.000014754422,0.019266065],"genre_scores_gemma":[0.9987351,0.00018394616,0.00017093823,0.00048297914,0.000062684834,0.0000037894936,0.000063742664,0.0000017101873,0.00029512084],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99840343,0.00044294677,0.00018310944,0.00029733268,0.00010500878,0.00056819787],"domain_scores_gemma":[0.9993749,0.0003075371,0.00005016292,0.0001728772,0.000019531459,0.0000749725],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007331478,0.00012590815,0.0002063999,0.00009235738,0.00019026153,0.000011537784,0.00031336077,0.00023020523,0.004615293],"category_scores_gemma":[0.00011234769,0.000084507075,0.000027332952,0.00019984896,0.0008618718,0.000107331136,0.000021323403,0.00040931164,0.00044423636],"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":[0.00019404925,0.0000120205705,0.9961777,0.0000035915662,0.000007676996,0.00069815037,0.0009916187,0.000009114468,0.0000063094976,0.00029493266,0.00018780242,0.001417031],"study_design_scores_gemma":[0.00045673002,0.00024951814,0.9925314,0.0000029822954,0.000007862397,0.00095509866,0.00028457952,0.00010772135,0.000022731716,0.0037131743,0.0015624642,0.00010569033],"about_ca_topic_score_codex":0.002133901,"about_ca_topic_score_gemma":0.041051373,"teacher_disagreement_score":0.03891747,"about_ca_system_score_codex":8.5471373e-7,"about_ca_system_score_gemma":0.00004631389,"threshold_uncertainty_score":0.9962946},"labels":[],"label_agreement":null},{"id":"W1993784563","doi":"10.1016/j.geomorph.2013.09.030","title":"Glacially conditioned specific stream powers in low-relief river catchments of the southern Laurentian Great Lakes","year":2013,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":44,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Fluvial; Stream power; Glacial period; Meltwater; Hydrology (agriculture); Geomorphology; Landform; Physical geography; Erosion; Geography","score_opus":0.00538017422304819,"score_gpt":0.1901356474394193,"score_spread":0.18475547321637112,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1993784563","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":[0.99625504,0.00004936053,0.000044116714,0.0005539626,0.00020088104,0.0002613555,0.0000510998,0.000014840863,0.0025693395],"genre_scores_gemma":[0.99843025,0.000021521484,0.00003856868,0.0004373992,0.000013423331,0.000023962431,0.00007841884,0.0000084305175,0.00094801764],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989749,0.000068219066,0.00024509733,0.00026390122,0.0001588508,0.00028899315],"domain_scores_gemma":[0.99957633,0.000027193935,0.000099336445,0.00023865404,0.000009969199,0.000048512364],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00010099352,0.00012830948,0.0001758154,0.000035046723,0.000079567035,0.0000051547045,0.0003192861,0.00013286111,0.04884696],"category_scores_gemma":[0.000006585574,0.00009600126,0.0000525523,0.0001675327,0.0008383371,0.00010584658,0.00006193969,0.00014168372,0.0018464144],"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":[0.00004208183,0.00027710834,0.9809295,0.00001311998,0.000024362029,0.000031740736,0.0024790196,0.0011398754,0.008921979,0.000056993096,0.005558766,0.0005254666],"study_design_scores_gemma":[0.001655542,0.0001487668,0.9786196,0.000027196893,0.000028585737,0.000023075894,0.0004347194,0.000045631215,0.004864913,0.002783948,0.011101223,0.00026681984],"about_ca_topic_score_codex":0.0017594321,"about_ca_topic_score_gemma":0.0033832595,"teacher_disagreement_score":0.047000546,"about_ca_system_score_codex":0.000033134394,"about_ca_system_score_gemma":0.000012951349,"threshold_uncertainty_score":0.99893075},"labels":[],"label_agreement":null},{"id":"W1997288102","doi":"10.1016/j.geomorph.2006.07.040","title":"Fifty years of coastal erosion and retrogressive thaw slump activity on Herschel Island, southern Beaufort Sea, Yukon Territory, Canada","year":2007,"lang":"en","type":"article","venue":"Geomorphology","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":416,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Permafrost; Geology; Thermokarst; Arctic; Coastal erosion; Erosion; Sea ice; Oceanography; Climate change; Shore; Physical geography; Geomorphology; Geography","score_opus":0.01524527991173325,"score_gpt":0.22050597575943817,"score_spread":0.20526069584770493,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1997288102","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":[0.9864285,0.00012877522,0.0000075353605,0.00015065465,0.00041482376,0.00009919844,0.01182248,0.0000079942665,0.0009400099],"genre_scores_gemma":[0.9980226,0.00003513428,0.0000136052095,0.0003080957,0.00012321408,4.0546442e-7,0.0013554433,0.0000045985526,0.00013687705],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990565,0.000045071873,0.000140635,0.00022884959,0.00019468679,0.0003342606],"domain_scores_gemma":[0.999428,0.00017573037,0.00010363849,0.00014968036,0.000022701128,0.000120248544],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00023295906,0.00011868473,0.00020421039,0.000049772923,0.00008079887,0.000009932802,0.00009924164,0.00012083074,0.0027894182],"category_scores_gemma":[0.000016405507,0.00010765641,0.00003061562,0.00006349235,0.00016017575,0.00004546449,0.000021679136,0.0001717052,0.00003295195],"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":[0.00026725556,0.000016443206,0.9844426,0.00001102022,0.000010828705,0.00021642804,0.00038174944,0.000011296463,0.0016177276,0.0000011646837,0.0038276347,0.009195872],"study_design_scores_gemma":[0.00042835233,0.00030241092,0.9932985,0.000016982007,0.0000110815345,0.00006903307,0.00074704026,0.000108401284,0.00090264634,0.0000142232475,0.0039693746,0.00013200795],"about_ca_topic_score_codex":0.8657347,"about_ca_topic_score_gemma":0.9945812,"teacher_disagreement_score":0.12884651,"about_ca_system_score_codex":0.000007749387,"about_ca_system_score_gemma":0.0000753799,"threshold_uncertainty_score":0.99812216},"labels":[],"label_agreement":null},{"id":"W1998009077","doi":"10.1016/s0169-555x(01)00136-2","title":"Channel units in small, high gradient streams on Vancouver Island, British Columbia","year":2002,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":85,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Bedrock; Geology; Stream power; Channel (broadcasting); STREAMS; Geomorphology; Sinuosity; Cobble; Hydrology (agriculture); Sediment; Geotechnical engineering; Ecology","score_opus":0.012246889552348468,"score_gpt":0.171254664616882,"score_spread":0.15900777506453354,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1998009077","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":[0.9932806,0.00005291281,0.00003434237,0.00020093944,0.00041647215,0.00016548843,0.000057167766,0.00003621483,0.005755854],"genre_scores_gemma":[0.9909663,0.00011168963,0.000024878675,0.0018975101,0.00002821914,0.00003668778,0.000048169117,0.000013042416,0.0068734554],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9987669,0.000055543802,0.0002035317,0.00041342073,0.00010272154,0.00045788955],"domain_scores_gemma":[0.9996337,0.000042268824,0.00004941587,0.00018159949,0.000006964801,0.000086031345],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00011774264,0.00011413376,0.0002046057,0.000028406554,0.00011857903,0.000018525876,0.0002196658,0.00017969849,0.04366781],"category_scores_gemma":[0.000018199127,0.00016000571,0.000023758332,0.000296498,0.00026771784,0.00007542466,0.000046470865,0.00022978269,0.00090436527],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000885744,0.0015714692,0.4747893,0.000024919154,0.00004243816,0.0043470003,0.0011871284,0.011098009,0.0002547729,0.00003167106,0.48690376,0.019660966],"study_design_scores_gemma":[0.00941612,0.0030515022,0.7094846,0.00011225332,0.00008832215,0.0006292933,0.0002923287,0.0028394037,0.0007159439,0.005360583,0.26629663,0.0017130467],"about_ca_topic_score_codex":0.03892582,"about_ca_topic_score_gemma":0.7822746,"teacher_disagreement_score":0.7433488,"about_ca_system_score_codex":0.000055636887,"about_ca_system_score_gemma":0.000004414022,"threshold_uncertainty_score":0.9998735},"labels":[],"label_agreement":null},{"id":"W1998646911","doi":"10.1016/j.geomorph.2007.12.019","title":"Responses of three-dimensional flow to variations in the angle of incident wind and profile form of dunes: Greenwich Dunes, Prince Edward Island, Canada","year":2008,"lang":"en","type":"article","venue":"Geomorphology","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":91,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Mount Allison University; Okanagan University College; University of British Columbia, Okanagan Campus; University of British Columbia; University of Guelph; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; British Columbia Knowledge Development Fund; Rural Development Administration; Parks Canada","keywords":"Foredune; Geology; Transect; Geomorphology; Plage; Bedform; Crest; Aeolian processes; Wind direction; Wind speed; Katabatic wind; Oceanography; Atmospheric sciences; Sediment transport; Sediment; Shore","score_opus":0.010939443367707137,"score_gpt":0.20351005677996087,"score_spread":0.19257061341225373,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1998646911","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":[0.99833053,0.00030054263,0.00008963195,0.000458004,0.000073706426,0.00022740454,0.00039737544,0.0000018923591,0.0001209213],"genre_scores_gemma":[0.9990622,0.000010106353,0.0005781668,0.00019816494,0.000016273145,0.000002159826,0.000067156856,0.0000017690704,0.000064033746],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991795,0.00007087782,0.00024412012,0.00013813104,0.00019792147,0.00016949432],"domain_scores_gemma":[0.999175,0.0004510574,0.00011709812,0.00014250357,0.00007241968,0.000041890235],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028050132,0.00007724071,0.00020868143,0.00006670934,0.000062252235,0.0000017100083,0.00015019739,0.000048825765,0.00033736654],"category_scores_gemma":[0.00015737387,0.000053704753,0.000017291268,0.00024152161,0.00013092397,0.00004884588,0.000024218893,0.00006717545,0.0000032497007],"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":[0.0002482654,0.000026685168,0.9941093,0.000053904107,0.000011094336,0.000070411355,0.0008467572,0.002529482,0.00016930226,0.00003838166,0.001294807,0.0006016411],"study_design_scores_gemma":[0.00026739566,0.00029498246,0.9954996,0.000016071855,0.000007944297,0.00019861471,0.00008476836,0.002673268,0.00024635726,0.00022526667,0.000425999,0.00005973179],"about_ca_topic_score_codex":0.48691446,"about_ca_topic_score_gemma":0.9317645,"teacher_disagreement_score":0.44485006,"about_ca_system_score_codex":0.0000025997645,"about_ca_system_score_gemma":0.0003865521,"threshold_uncertainty_score":0.51650226},"labels":[],"label_agreement":null},{"id":"W1999768559","doi":"10.1016/j.geomorph.2005.07.032","title":"Emergence of the Canadian Rockies and adjacent plains: A comparison of physiography between end-of-Laramide time and the present day","year":2006,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Calgary","funders":"","keywords":"Geology; Foothills; Foreland basin; Paleontology; Clastic rock; Mesozoic; Orogeny; Sedimentary rock; Geomorphology; Denudation; Tectonics; Structural basin","score_opus":0.01484836806410836,"score_gpt":0.23653297876906418,"score_spread":0.22168461070495582,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1999768559","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":[0.99242413,0.0042464794,0.0000028593374,0.0012430362,0.0000620492,0.00020886725,0.00020395465,0.0000025389206,0.0016061066],"genre_scores_gemma":[0.9997126,0.00009545045,0.000031843796,0.000027197357,0.000017132077,0.0000014590928,0.000066996465,0.0000012647082,0.000046082427],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99878573,0.00040396815,0.00026447588,0.00015155532,0.00012618805,0.00026805178],"domain_scores_gemma":[0.9989622,0.0005982628,0.00014703168,0.00019007993,0.00004825179,0.000054173022],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045609733,0.00008623391,0.00033458575,0.00010043711,0.00019508267,0.000003532163,0.00024704187,0.00011126431,0.00061838754],"category_scores_gemma":[0.000041529398,0.000049943632,0.000048913655,0.00020052306,0.0026402844,0.000024116487,0.000040117888,0.00016917312,0.0000071229947],"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":[0.000038200713,0.000009221356,0.9979717,0.00001923508,0.000037445898,0.0000020281807,0.0002873774,0.0003121172,0.000030460556,0.00022939558,0.0007002277,0.00036257427],"study_design_scores_gemma":[0.0003678083,0.00007713123,0.9958755,0.000008407042,0.00003194751,0.000016397868,0.000118294876,0.0009411289,0.0005401407,0.0015149618,0.0004609781,0.000047313446],"about_ca_topic_score_codex":0.2323634,"about_ca_topic_score_gemma":0.560816,"teacher_disagreement_score":0.32845256,"about_ca_system_score_codex":3.3258982e-7,"about_ca_system_score_gemma":0.00006858952,"threshold_uncertainty_score":0.97282374},"labels":[],"label_agreement":null},{"id":"W2000790738","doi":"10.1016/j.geomorph.2008.04.005","title":"A meltwater origin for Antarctic shelf bedforms with special attention to megalineations","year":2008,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":54,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia, Okanagan Campus; University of British Columbia; Geological Survey of Canada; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Meltwater; Geology; Bedform; Geomorphology; Ice shelf; Drumlin; Iceberg; Lineation; Glacial period; Oceanography; Ice stream; Ice sheet; Paleontology; Sediment transport; Sediment; Sea ice; Cryosphere","score_opus":0.032345145003298985,"score_gpt":0.2574722099483561,"score_spread":0.22512706494505713,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2000790738","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":[0.99313045,0.000042430474,0.00088140514,0.0025342233,0.0003797682,0.00042493263,0.00009431357,0.000029190227,0.0024832946],"genre_scores_gemma":[0.9934039,0.00001500556,0.0030116509,0.000653977,0.00037499744,0.000021491865,0.0007377731,0.0000037953416,0.0017774256],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988609,0.00006342426,0.00016726584,0.00029992382,0.00010975922,0.00049871765],"domain_scores_gemma":[0.9994184,0.00015693698,0.000037024172,0.00016674469,0.000090765025,0.00013013711],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00017465965,0.00011749495,0.00020869759,0.00014989101,0.00038946187,0.000009289427,0.00016796414,0.00012795231,0.0058714966],"category_scores_gemma":[0.000040848554,0.00008387646,0.000045534664,0.00018800497,0.00028703324,0.00009653571,0.000010699254,0.00014599669,0.0017276678],"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":[0.000371807,0.00001920479,0.9950192,0.0000074015106,0.000027946127,0.00013358284,0.00021971289,0.00027798905,0.00001858447,0.00015609762,0.0035271014,0.0002214023],"study_design_scores_gemma":[0.0009384762,0.00081999623,0.96993333,0.0000040559285,0.000022803819,0.0022843732,0.00008030178,0.00028279686,0.000084616055,0.00055579137,0.024826003,0.00016747376],"about_ca_topic_score_codex":0.0003792608,"about_ca_topic_score_gemma":0.008837305,"teacher_disagreement_score":0.025085859,"about_ca_system_score_codex":0.0000019653442,"about_ca_system_score_gemma":0.00007069289,"threshold_uncertainty_score":0.9990496},"labels":[],"label_agreement":null},{"id":"W2002349939","doi":"10.1016/j.geomorph.2013.12.027","title":"Quaternary, catastrophic rock avalanches in the Central Apennines (Italy): Relationships with inherited tectonic features, gravity-driven deformations and the geodynamic frame","year":2014,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":40,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Geology; Tectonics; Fault (geology); Rock mass classification; Quaternary; Fault scarp; Wedge (geometry); Carbonate rock; Geomorphology; Seismology; Paleontology; Sedimentary rock; Geotechnical engineering; Geometry","score_opus":0.005284821098411138,"score_gpt":0.1843516528126015,"score_spread":0.17906683171419036,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2002349939","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":[0.99424875,0.00010427346,0.00075599423,0.0039999587,0.00006923676,0.00030152797,0.000014144348,0.000020983294,0.00048512808],"genre_scores_gemma":[0.9991456,0.00005832006,0.00016832234,0.00032439435,0.000025987254,0.000035719775,0.000106327185,0.000009757863,0.000125521],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998775,0.0003561213,0.0001810715,0.00020565318,0.00015218195,0.00032995193],"domain_scores_gemma":[0.9993751,0.00019709855,0.00009168963,0.00028480435,0.000006117874,0.000045205677],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040828896,0.00013800024,0.00016350037,0.00003575373,0.00033532066,0.000043900727,0.0002821555,0.00013033436,0.00011177887],"category_scores_gemma":[0.0000464972,0.00006367752,0.000031983895,0.00021394355,0.00041607404,0.00010207335,0.00010654217,0.0005453726,0.00009625945],"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":[0.00021866451,0.0000743965,0.9609908,0.000009805179,0.000039321385,0.000037324935,0.0040466804,0.030926073,0.00029871202,0.0017037806,0.0011601052,0.0004943222],"study_design_scores_gemma":[0.0013933817,0.00009455817,0.97836584,0.000012962274,0.000040078372,0.000807638,0.0003004974,0.014983258,0.0000045127967,0.00166594,0.0022051842,0.00012616722],"about_ca_topic_score_codex":0.0021703097,"about_ca_topic_score_gemma":0.004871683,"teacher_disagreement_score":0.017375007,"about_ca_system_score_codex":0.000043126893,"about_ca_system_score_gemma":0.00000928644,"threshold_uncertainty_score":0.32808736},"labels":[],"label_agreement":null},{"id":"W2003555355","doi":"10.1016/j.geomorph.2008.06.014","title":"A method for estimating the mean bed load flux in braided rivers","year":2008,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":95,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Bed load; Dimensionless quantity; Geology; Stream power; Shear stress; Geotechnical engineering; Flux (metallurgy); Sediment transport; Hydraulics; Transverse plane; Sediment; Mechanics; Hydrology (agriculture); Geomorphology; Materials science; Structural engineering; Engineering","score_opus":0.020185136697352515,"score_gpt":0.26377506017328217,"score_spread":0.24358992347592967,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2003555355","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":[0.9415638,0.000033091423,0.054470602,0.001532348,0.00012725695,0.00030067575,0.000008316436,0.000032138323,0.0019318089],"genre_scores_gemma":[0.9014523,0.0000040148925,0.09607226,0.0019116233,0.000024885534,0.00006703957,0.000022498452,0.000008428249,0.00043694474],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990379,0.00007871877,0.00018369916,0.0002742753,0.000108592096,0.00031679418],"domain_scores_gemma":[0.9995372,0.00020955644,0.000055554086,0.00015270608,0.0000067703863,0.00003817913],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00056301075,0.000101278965,0.00016281268,0.000021211858,0.00021661696,0.000002447112,0.00024472733,0.00009975379,0.002734981],"category_scores_gemma":[0.00006397583,0.00007685712,0.000042268533,0.00014683664,0.0003861096,0.00007659723,0.000043197728,0.0001387729,0.00021150692],"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":[0.0009181136,0.000838036,0.55471855,0.00008954097,0.00017797617,0.0015086095,0.045764964,0.18030365,0.107294634,0.0009934234,0.047768693,0.059623808],"study_design_scores_gemma":[0.021026224,0.002320405,0.42512125,0.00006375387,0.0003611299,0.004168711,0.0011172532,0.24961886,0.07178562,0.04656449,0.17523609,0.0026162046],"about_ca_topic_score_codex":0.00071184995,"about_ca_topic_score_gemma":0.0011505901,"teacher_disagreement_score":0.1295973,"about_ca_system_score_codex":0.000050337287,"about_ca_system_score_gemma":0.00002552185,"threshold_uncertainty_score":0.99817663},"labels":[],"label_agreement":null},{"id":"W2003747047","doi":"10.1016/j.geomorph.2009.12.002","title":"Shore platform downwearing in eastern Canada: The mega-tidal Bay of Fundy","year":2009,"lang":"en","type":"article","venue":"Geomorphology","topic":"Building materials and conservation","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Windsor","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Bay; Geology; Shore; Water level; Basalt; Weathering; Sea level; Hydrology (agriculture); Oceanography; Geomorphology; Geochemistry; Geotechnical engineering","score_opus":0.017936286208128198,"score_gpt":0.19394611213724394,"score_spread":0.17600982592911574,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2003747047","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":[0.99677974,0.00009452925,0.000013055369,0.001575241,0.00026601987,0.00006689297,0.000024285126,0.0000055821197,0.001174663],"genre_scores_gemma":[0.9990133,0.000006904338,0.000035410867,0.00080035103,0.000041330284,3.6284416e-7,0.000049160728,9.4569407e-7,0.000052235733],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99940383,0.000029476478,0.0001734425,0.00010765225,0.000095335185,0.00019023776],"domain_scores_gemma":[0.9997342,0.00005432199,0.000057546316,0.0001129736,0.000014898334,0.000026022148],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021815072,0.00006220087,0.00012245763,0.000027881762,0.0000416364,0.000012229703,0.00015424151,0.000045700537,0.0009752827],"category_scores_gemma":[0.000015432819,0.00004233824,0.000013443174,0.00008940053,0.000037848702,0.000053662625,0.0000068734116,0.000073092124,0.000010352691],"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":[0.000056078672,0.0000064116925,0.9800027,0.000004631922,0.000004527712,0.000035926543,0.00014431617,0.0012805632,0.00076400524,0.00022748936,0.00040164732,0.017071722],"study_design_scores_gemma":[0.00015306791,0.00006419706,0.99593055,0.000006371095,0.0000031937545,0.000032885353,0.00011541322,0.0012401901,0.0003420551,0.0005008326,0.0015561185,0.000055138564],"about_ca_topic_score_codex":0.60318017,"about_ca_topic_score_gemma":0.9107803,"teacher_disagreement_score":0.30760014,"about_ca_system_score_codex":0.000005100291,"about_ca_system_score_gemma":0.00010027666,"threshold_uncertainty_score":0.99993795},"labels":[],"label_agreement":null},{"id":"W2004853484","doi":"10.1016/j.geomorph.2014.06.031","title":"Coupling glacial lake impact, dam breach, and flood processes: A modeling perspective","year":2014,"lang":"en","type":"article","venue":"Geomorphology","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":213,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; Simon Fraser University","funders":"Bundesamt für Umwelt","keywords":"Flood myth; Glacial period; Geology; Glacial lake; Dam failure; Hazard analysis; Glacier; Perspective (graphical); Hydrology (agriculture); Geomorphology; Computer science; Geotechnical engineering; Engineering; Geography","score_opus":0.017637394177242534,"score_gpt":0.23970679774941167,"score_spread":0.22206940357216914,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2004853484","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":[0.9925276,0.0012793236,0.0041275546,0.0003905018,0.00018011771,0.00010993155,0.00009411773,0.00004253987,0.0012482817],"genre_scores_gemma":[0.9986303,0.00017740557,0.00058990764,0.00023808131,0.00022712101,0.0000023000587,0.0000907276,0.0000038572616,0.00004029807],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99919,0.00001743835,0.00013701909,0.0002707658,0.00009087398,0.00029392436],"domain_scores_gemma":[0.9995104,0.00012686133,0.00004622134,0.00010740557,0.00012637331,0.00008270385],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00017199492,0.0001217546,0.00019325453,0.000019096078,0.00028962968,0.000035207973,0.00009466631,0.000063539934,0.0010972406],"category_scores_gemma":[0.00018684306,0.0000986468,0.000030727453,0.00017941755,0.000099124096,0.00009501001,0.000021278252,0.00011328662,0.00004852656],"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":[0.0001043716,0.00004062277,0.78919595,0.000034386547,0.00009367696,0.000019300427,0.002758718,0.20145309,0.000020755837,0.00039017235,0.000694688,0.0051942393],"study_design_scores_gemma":[0.0007087109,0.00034530208,0.31839478,0.000011489384,0.000049180006,0.000126337,0.002741565,0.67128825,0.0000030506953,0.0021788916,0.0038796768,0.00027277519],"about_ca_topic_score_codex":0.005685531,"about_ca_topic_score_gemma":0.038433295,"teacher_disagreement_score":0.4708012,"about_ca_system_score_codex":0.000005075547,"about_ca_system_score_gemma":0.000054267985,"threshold_uncertainty_score":0.9998159},"labels":[],"label_agreement":null},{"id":"W2007269259","doi":"10.1016/j.geomorph.2010.01.011","title":"Thresholds of erosion and sediment movement in bedrock channels","year":2010,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":13,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Bedrock; Clastic rock; Imbrication; Flume; Erosion; Sediment transport; Geomorphology; Sediment; Bed load; Bedform; Hydrology (agriculture); Channel (broadcasting); Geotechnical engineering; Structural basin; Flow (mathematics); Tectonics; Geometry","score_opus":0.006384399407289767,"score_gpt":0.2124631782457415,"score_spread":0.20607877883845174,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007269259","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":[0.9978804,0.00003738268,0.000068020054,0.00054516585,0.00021012258,0.0001285412,0.0000048128686,0.000009397836,0.0011161608],"genre_scores_gemma":[0.998794,0.000032964555,0.00020605343,0.0008004408,0.00001295954,0.000017060813,0.000011261266,0.0000048647776,0.00012039226],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992622,0.000015388887,0.00018544677,0.00022854393,0.00009913479,0.00020925193],"domain_scores_gemma":[0.9997461,0.000022718328,0.000047523972,0.00013004369,0.0000034151933,0.000050238992],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00022628489,0.000086971966,0.00014683396,0.00003729205,0.000035599907,0.0000020168657,0.0001119528,0.00012909347,0.004670177],"category_scores_gemma":[0.000006582426,0.00007815176,0.000015161581,0.00008604378,0.0002717098,0.000063832595,0.00008097468,0.00016622608,0.000054107666],"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":[0.000036230143,0.00014350684,0.6660738,0.00000884959,0.0000038925905,0.00002422217,0.00035903454,0.00040608778,0.3316855,0.0002536861,0.0003398057,0.00066533714],"study_design_scores_gemma":[0.0021962686,0.00065292814,0.7723925,0.000015127347,0.000024719237,0.000064760075,0.00007358274,0.00055096543,0.20468292,0.007672061,0.011339246,0.00033494187],"about_ca_topic_score_codex":0.00044153057,"about_ca_topic_score_gemma":0.00095749326,"teacher_disagreement_score":0.12700261,"about_ca_system_score_codex":0.000008822695,"about_ca_system_score_gemma":0.0000050810813,"threshold_uncertainty_score":0.99623966},"labels":[],"label_agreement":null},{"id":"W2007666156","doi":"10.1016/j.geomorph.2006.06.011","title":"Sedimentary links and the spatial organization of Atlantic salmon (Salmo salar) spawning habitat in a Canadian Shield river","year":2006,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":44,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"","keywords":"Salmo; Geology; Sedimentary rock; Habitat; Sediment; Bedrock; Tributary; Hydrology (agriculture); Geomorphology; Ecology; Fishery; Paleontology; Geography; Fish <Actinopterygii>","score_opus":0.003566693902971489,"score_gpt":0.1774764103328056,"score_spread":0.1739097164298341,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007666156","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":[0.99654603,0.00006836081,0.00023057651,0.0022386839,0.00008403389,0.00015885006,0.000006593385,0.000009719898,0.0006571364],"genre_scores_gemma":[0.9988356,0.000019170307,0.00010421567,0.00087649195,0.000024736923,0.0000049373657,0.000092243485,0.000008371559,0.000034189747],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991674,0.00006670539,0.00020389495,0.00020145108,0.00008540017,0.0002751524],"domain_scores_gemma":[0.9997056,0.00007817424,0.000057310204,0.000101810605,0.0000062943514,0.000050781437],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00026767483,0.00009415386,0.00016313509,0.000048088932,0.00008998861,0.000004308787,0.0001201383,0.00018036323,0.001568668],"category_scores_gemma":[0.000021956208,0.00007498316,0.00001469966,0.00020375111,0.0006503652,0.00007024113,0.000036763748,0.00019474907,0.000046330257],"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":[0.00003225042,0.000024494637,0.9970624,0.0000056784374,0.0000054093566,0.00006824147,0.00041775,0.0009457217,0.0007410386,0.00033837443,0.0002599537,0.00009870373],"study_design_scores_gemma":[0.0011223273,0.000050198007,0.99551153,0.0000073849665,0.000027428705,0.00005433482,0.00003063949,0.00034277805,0.00087463186,0.0010204616,0.00086104963,0.00009725842],"about_ca_topic_score_codex":0.74991137,"about_ca_topic_score_gemma":0.76947516,"teacher_disagreement_score":0.01956379,"about_ca_system_score_codex":0.000048000682,"about_ca_system_score_gemma":0.000030176176,"threshold_uncertainty_score":0.99934405},"labels":[],"label_agreement":null},{"id":"W2011373971","doi":"10.1016/j.geomorph.2006.12.036","title":"Predicting landslides for risk analysis — Spatial models tested by a cross-validation technique","year":2007,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":150,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Fifth Framework Programme; Natural Resources Canada; U.S. Geological Survey","keywords":"Landslide; Hazard; Geology; Probabilistic logic; Cross-validation; Reliability (semiconductor); Statistics; Geotechnical engineering; Mathematics","score_opus":0.007928967643540992,"score_gpt":0.2535560419054098,"score_spread":0.24562707426186883,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2011373971","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":[0.5907988,0.000015990156,0.40752885,0.000025885676,0.00010456863,0.00027967413,0.00017047755,0.000058253954,0.0010174722],"genre_scores_gemma":[0.9950112,0.000019991345,0.003862854,0.00007298165,0.00006554361,0.00005970283,0.00035611945,0.000015381978,0.00053621316],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99872303,0.0000447629,0.0003170376,0.00036640355,0.00015685143,0.00039192892],"domain_scores_gemma":[0.9993206,0.00016071026,0.00019239688,0.00021716041,0.000022332786,0.00008675605],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010575379,0.00013197742,0.00021355257,0.000080490514,0.00022696792,0.000027559954,0.00016272435,0.00026882833,0.0009163189],"category_scores_gemma":[0.00008683419,0.00010693514,0.00011971634,0.00036992042,0.00014454799,0.000122062076,0.00008942414,0.00016947748,0.00003401858],"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":[0.00014516508,0.000071425704,0.941553,0.000004262911,0.00015977083,0.000012653825,0.00014431807,0.032922808,0.020036308,0.000017703771,0.0015843016,0.003348302],"study_design_scores_gemma":[0.0057698605,0.0013653362,0.38646165,0.000023424715,0.002626924,0.00019362265,0.00015185497,0.34866196,0.21082734,0.010260118,0.032132313,0.0015255869],"about_ca_topic_score_codex":0.0038294701,"about_ca_topic_score_gemma":0.0007333481,"teacher_disagreement_score":0.5550913,"about_ca_system_score_codex":0.000081240425,"about_ca_system_score_gemma":0.0000067290393,"threshold_uncertainty_score":0.99999696},"labels":[],"label_agreement":null},{"id":"W2011695369","doi":"10.1016/j.geomorph.2009.02.016","title":"Modeling aeolian sediment transport thresholds on physically rough Martian surfaces: A shear stress partitioning approach","year":2009,"lang":"en","type":"article","venue":"Geomorphology","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"Natural Sciences and Engineering Research Council of Canada; Nevada System of Higher Education; Office of Experimental Program to Stimulate Competitive Research; National Aeronautics and Space Administration","keywords":"Martian; Mars Exploration Program; Shear stress; Geology; Surface roughness; Aeolian processes; Surface finish; Shear (geology); Drag; Roughness length; Geotechnical engineering; Mechanics; Wind speed; Geomorphology; Materials science; Wind profile power law; Composite material; Physics","score_opus":0.015778448992526433,"score_gpt":0.21660928997210993,"score_spread":0.2008308409795835,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2011695369","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":[0.983489,0.00022596645,0.0068108863,0.0009107432,0.0001793126,0.00024591363,0.00011019131,0.00010094845,0.007927088],"genre_scores_gemma":[0.9960129,0.00002943179,0.0014312301,0.0016053088,0.00017823548,0.0000036758352,0.0006112726,0.0000069245534,0.000121012825],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99827504,0.00006292542,0.00026435743,0.00049442606,0.00027104703,0.00063221966],"domain_scores_gemma":[0.9994252,0.000032883563,0.000057608915,0.00025325624,0.000036102563,0.00019500557],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022371036,0.000233016,0.00030352804,0.000056972534,0.00023258766,0.00003470489,0.00023575664,0.0001409846,0.0008713325],"category_scores_gemma":[0.0000074256413,0.00019935143,0.000087381886,0.00019580487,0.00008270186,0.00018269593,0.000005698037,0.00026194323,0.00026534052],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012891814,0.00011042244,0.019584013,0.000027827102,0.000013963736,0.00009197993,0.00040719451,0.97572243,0.000043610158,0.00027897846,0.00025217186,0.003338507],"study_design_scores_gemma":[0.000629433,0.00093130965,0.05727955,0.00005489129,0.000035262205,0.00006579841,0.00018659617,0.93795043,0.00018349146,0.0017227854,0.00059103704,0.00036944266],"about_ca_topic_score_codex":0.001194671,"about_ca_topic_score_gemma":0.00034431802,"teacher_disagreement_score":0.03777201,"about_ca_system_score_codex":0.0000074800073,"about_ca_system_score_gemma":0.000045687066,"threshold_uncertainty_score":0.954048},"labels":[],"label_agreement":null},{"id":"W2011819391","doi":"10.1016/j.geomorph.2013.02.002","title":"Biogeomorphic impacts of migration and disturbance: Implications of salmon spawning and decay","year":2013,"lang":"en","type":"article","venue":"Geomorphology","topic":"Fish Ecology and Management Studies","field":"Environmental Science","cited_by":11,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Northern British Columbia","funders":"","keywords":"Disturbance (geology); Geology; Oceanography; Geomorphology","score_opus":0.0075432140118932445,"score_gpt":0.21020730536229487,"score_spread":0.20266409135040162,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2011819391","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":[0.9960319,0.00013949705,0.0001675664,0.0021070943,0.000027581798,0.0001858593,0.000010426538,0.0000071832214,0.0013229073],"genre_scores_gemma":[0.9989395,0.0002915384,0.00045977795,0.00019897877,0.0000041159856,0.000026376287,0.000011938573,0.0000031775298,0.000064593456],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995135,0.000023816454,0.00014675826,0.00015064712,0.000036865313,0.00012838916],"domain_scores_gemma":[0.99967957,0.00006145035,0.00010893136,0.00011022178,0.00001007533,0.00002973023],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008677919,0.00006398226,0.0001367902,0.00003114452,0.00007008799,0.0000029818343,0.000054894837,0.000049332495,0.00063094654],"category_scores_gemma":[0.000027244638,0.00005674187,0.000011202966,0.00008594052,0.00053244294,0.00008888155,0.00016098049,0.000036287463,0.000024191173],"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":[0.0000045250044,0.000025243706,0.97442055,0.00001259715,0.00001306704,5.3450077e-7,0.00018122648,0.0000064806486,0.017088382,0.00067702396,0.007008245,0.00056210323],"study_design_scores_gemma":[0.00017783482,0.00009302473,0.9951223,0.0000044417234,0.000017847757,0.000011332934,0.00008501838,0.000016842441,0.0015767476,0.0023752833,0.0004692191,0.000050093524],"about_ca_topic_score_codex":0.0016234402,"about_ca_topic_score_gemma":0.002311936,"teacher_disagreement_score":0.020701742,"about_ca_system_score_codex":0.0000098281425,"about_ca_system_score_gemma":0.0000019274003,"threshold_uncertainty_score":0.6908422},"labels":[],"label_agreement":null},{"id":"W2013216590","doi":"10.1016/j.geomorph.2006.07.003","title":"Comment on Lønne and Lyså (2005): “Deglaciation dynamics following the Little Ice Age on Svalbard: Implications for shaping of landscapes at high latitudes”, Geomorphology 72, 300–319","year":2006,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Deglaciation; Geology; Geomorphology; Physical geography; Glacial period; Geography","score_opus":0.021518357816450548,"score_gpt":0.25565669207081143,"score_spread":0.23413833425436087,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2013216590","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":[0.97137916,0.00040037878,0.00030296805,0.024493055,0.00032422438,0.00053286075,0.0004941866,0.000028043482,0.0020451297],"genre_scores_gemma":[0.9940208,0.00005643691,0.00036742483,0.002201051,0.0000696341,0.000030906645,0.0029384163,0.000007169022,0.00030811477],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981814,0.00028501597,0.0003557174,0.00040862654,0.00012882099,0.00064044545],"domain_scores_gemma":[0.99729306,0.0020582783,0.00018253695,0.00034040923,0.000055577948,0.00007016398],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008962769,0.00018941086,0.0003786764,0.00014645682,0.0006050315,0.000017747921,0.00028033054,0.00027205516,0.00045339752],"category_scores_gemma":[0.00011824835,0.00014551237,0.00009171856,0.00014032153,0.00031224397,0.00004802989,0.000050927618,0.00024953534,0.0001069512],"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":[0.00020641967,0.000060702114,0.97948694,0.000019820025,0.00006028156,0.000023835466,0.000058831767,0.0017713249,0.000074080766,0.013558218,0.0043087485,0.0003708099],"study_design_scores_gemma":[0.0012322139,0.0005518714,0.9808537,0.0000137386405,0.00006370685,0.00013543654,0.000051773608,0.0021372258,0.00011281243,0.007556069,0.0071159983,0.0001754529],"about_ca_topic_score_codex":0.001470845,"about_ca_topic_score_gemma":0.032611955,"teacher_disagreement_score":0.031141108,"about_ca_system_score_codex":0.000012712391,"about_ca_system_score_gemma":0.00003501383,"threshold_uncertainty_score":0.98504037},"labels":[],"label_agreement":null},{"id":"W2013286002","doi":"10.1016/j.geomorph.2011.09.024","title":"A field investigation of the influence of sediment supply on step-pool morphology and stability","year":2011,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":75,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Agence Nationale de la Recherche","keywords":"Geology; Sediment; Morphology (biology); Field (mathematics); Stability (learning theory); Geomorphology; Paleontology","score_opus":0.014706942521959029,"score_gpt":0.20174396279165582,"score_spread":0.1870370202696968,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2013286002","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":[0.9986268,0.000017994367,0.000038956998,0.00045707804,0.000056857054,0.00018437655,0.000013587226,0.0000073627357,0.0005969653],"genre_scores_gemma":[0.99859905,0.0000134286065,0.0002288659,0.0011153494,0.0000030724561,0.000013921639,0.0000033099543,0.0000035060618,0.000019521425],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991694,0.00009938008,0.00024529741,0.00022261792,0.000108471155,0.00015483817],"domain_scores_gemma":[0.9994516,0.0001054141,0.00013257984,0.00025753482,0.000012389458,0.000040499544],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00025974147,0.00008909212,0.00016341527,0.000020213465,0.00004545576,6.3210274e-7,0.00019836683,0.00012518762,0.0030021556],"category_scores_gemma":[0.000049270147,0.000064496395,0.00002632819,0.00010754868,0.0010328512,0.000058121495,0.00008767034,0.00012813635,0.000018509905],"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":[0.00014840068,0.000070598224,0.9340719,0.000018275961,0.000009903999,0.0000047092058,0.0010903822,0.000114059236,0.06377204,0.00030229407,0.00015393028,0.00024348783],"study_design_scores_gemma":[0.00024399461,0.00052975665,0.7350371,0.000007017825,0.00001727518,0.000014202547,0.000027666134,0.000012988893,0.2624224,0.0015181071,0.00011759844,0.000051884886],"about_ca_topic_score_codex":0.00092359656,"about_ca_topic_score_gemma":0.00015864978,"teacher_disagreement_score":0.19903482,"about_ca_system_score_codex":0.000011532178,"about_ca_system_score_gemma":0.000014864902,"threshold_uncertainty_score":0.99790925},"labels":[],"label_agreement":null},{"id":"W2015380342","doi":"10.1016/j.geomorph.2015.02.015","title":"Spatial–temporal evolution of aeolian blowout dunes at Cape Cod","year":2015,"lang":"en","type":"article","venue":"Geomorphology","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"National Park Service; National Oceanic and Atmospheric Administration; Canada Foundation for Innovation; Center for Selective C-H Functionalization, National Science Foundation","keywords":"Geology; Aeolian processes; Physical geography; Sedimentary depositional environment; Paleontology; Geomorphology; Geography; Structural basin","score_opus":0.015791125277732694,"score_gpt":0.20922934883959884,"score_spread":0.19343822356186616,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015380342","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":[0.9933113,0.001347778,0.0005689156,0.00036521922,0.00074829865,0.00012442927,0.00011436677,0.000034854776,0.003384839],"genre_scores_gemma":[0.99840945,0.0000119992965,0.00022303672,0.00011842041,0.00013344821,0.0000011178555,0.00030848442,0.000003889224,0.00079017004],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989947,0.000081414226,0.0002091544,0.00022306031,0.0001747657,0.00031688312],"domain_scores_gemma":[0.9993722,0.000053856522,0.00013169867,0.00017758823,0.00008681676,0.00017786266],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0002619396,0.00012032062,0.00023656654,0.00006666034,0.00006835231,0.000006570605,0.00017155256,0.00012459663,0.0022517538],"category_scores_gemma":[0.00007373315,0.000102016056,0.000043899985,0.00014909584,0.0002107866,0.00008367577,0.000020955145,0.00008358503,0.0013460558],"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":[0.00016669303,0.000017726925,0.9866093,0.00003435916,0.000013563837,0.000076778844,0.0002617111,0.0016309858,0.00016836319,0.000060611867,0.00858336,0.0023765955],"study_design_scores_gemma":[0.001836163,0.0013521471,0.92329144,0.000026643173,0.000055745582,0.00062194734,0.00041771014,0.023645973,0.0017509552,0.0036302707,0.042944334,0.00042667816],"about_ca_topic_score_codex":0.029441874,"about_ca_topic_score_gemma":0.030786326,"teacher_disagreement_score":0.06331782,"about_ca_system_score_codex":0.000009960013,"about_ca_system_score_gemma":0.00011936396,"threshold_uncertainty_score":0.9994315},"labels":[],"label_agreement":null},{"id":"W2015510940","doi":"10.1016/j.geomorph.2009.02.004","title":"Rock coast geomorphology: Recent advances and future research directions","year":2009,"lang":"en","type":"article","venue":"Geomorphology","topic":"Coastal and Marine Dynamics","field":"Earth and Planetary Sciences","cited_by":177,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Windsor","funders":"","keywords":"Landform; Coastal geography; Geology; Scope (computer science); Earth science; Temporal scales; Oceanography; Geomorphology; Shore; Ecology; Computer science","score_opus":0.01862769462236244,"score_gpt":0.26948986180757395,"score_spread":0.2508621671852115,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015510940","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":[0.841969,0.04699667,0.00025488358,0.037824757,0.0037399821,0.00076279085,0.0009530564,0.00028609257,0.06721274],"genre_scores_gemma":[0.8955218,0.095645286,0.0007543508,0.0021928,0.0011338397,0.000005506208,0.0013974439,0.000008880954,0.0033400636],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.998484,0.00016925774,0.00018950437,0.00040346175,0.00018665039,0.0005671151],"domain_scores_gemma":[0.9992863,0.0001455793,0.000048420585,0.00021651755,0.00012545656,0.00017771249],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00041355303,0.00014684722,0.000216316,0.0001682543,0.00040784862,0.000035119454,0.00018287488,0.00014296954,0.0048453254],"category_scores_gemma":[0.000054813983,0.0001240696,0.00003107805,0.0004276352,0.00017844909,0.00014814963,0.000047240497,0.00042476153,0.00026167044],"study_design_candidate":"design_other","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":[0.00011699242,0.000044054475,0.039478663,0.0000075225166,0.0000084691055,0.00014839816,0.00009441031,0.000090644346,0.0000612023,0.000444009,0.0065794843,0.95292616],"study_design_scores_gemma":[0.00025943288,0.00046859815,0.20642379,0.0000025648208,0.000006677858,0.0006357334,0.0002450223,0.00033871498,0.000009559828,0.0038638634,0.7876188,0.00012721642],"about_ca_topic_score_codex":0.0013788639,"about_ca_topic_score_gemma":0.020167353,"teacher_disagreement_score":0.9527989,"about_ca_system_score_codex":0.000006762201,"about_ca_system_score_gemma":0.00004728481,"threshold_uncertainty_score":0.997712},"labels":[],"label_agreement":null},{"id":"W2020255109","doi":"10.1016/j.geomorph.2008.05.012","title":"Crack propagation by differential insolation on desert surface clasts","year":2008,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":60,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Insolation; Groundwater recharge; Moisture; Shield; Atmospheric sciences; Geotechnical engineering; Groundwater; Climatology; Aquifer; Materials science; Petrology; Composite material","score_opus":0.023497928335699157,"score_gpt":0.22985192175347624,"score_spread":0.20635399341777708,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2020255109","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":[0.994778,0.00011913419,0.00027390197,0.0006908501,0.0003628819,0.00017409695,0.00004220599,0.00004408699,0.0035148906],"genre_scores_gemma":[0.99736583,0.0000782671,0.000093289986,0.00030235987,0.000046264657,0.0000016045999,0.0009847281,0.0000030363492,0.0011246043],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986944,0.0002777712,0.00017247669,0.00029730945,0.00015926767,0.00039877655],"domain_scores_gemma":[0.9994056,0.0002214668,0.00006281092,0.00017101328,0.00004789509,0.000091183196],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0001560894,0.00012249225,0.0001779363,0.00006403353,0.0003210216,0.000007669031,0.00016602945,0.0002401507,0.0062668016],"category_scores_gemma":[0.000063042906,0.00010383588,0.000033199987,0.00013224383,0.00034948243,0.00008855592,0.000011628632,0.00030306744,0.0035485774],"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":[0.0002398985,0.00003478157,0.9919101,0.00000417722,0.000010613313,0.000078799516,0.000068751884,0.00047485475,0.00043350656,0.000032998323,0.0064303484,0.00028118456],"study_design_scores_gemma":[0.0005165343,0.00040931604,0.99216545,0.0000027225703,0.000005297085,0.00046653507,0.000010386239,0.0031146058,0.0009412847,0.00018816363,0.0020527458,0.0001269771],"about_ca_topic_score_codex":0.00025808194,"about_ca_topic_score_gemma":0.000854796,"teacher_disagreement_score":0.0043776026,"about_ca_system_score_codex":0.0000017084027,"about_ca_system_score_gemma":0.000044320022,"threshold_uncertainty_score":0.99722725},"labels":[],"label_agreement":null},{"id":"W2020389070","doi":"10.1016/j.geomorph.2005.01.011","title":"Morphology and geotechnique of active-layer detachment failures in discontinuous and continuous permafrost, northern Canada","year":2005,"lang":"en","type":"article","venue":"Geomorphology","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":125,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Ottawa","funders":"","keywords":"Permafrost; Thermokarst; Geology; Active layer; Geomorphology; Instability; Disturbance (geology); Cohesion (chemistry); Layer (electronics); Oceanography","score_opus":0.01291463472995279,"score_gpt":0.2168906538797921,"score_spread":0.2039760191498393,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2020389070","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":[0.9929188,0.0012021222,0.00000733766,0.0019347769,0.00009180495,0.00022211316,0.0031719266,0.00001042606,0.00044072344],"genre_scores_gemma":[0.99797386,0.00026187615,0.00008903666,0.0006868334,0.00005639634,0.0000048643524,0.00081223523,0.000005451823,0.00010941697],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99883413,0.00007334991,0.00028256758,0.00031774113,0.00010284915,0.0003893629],"domain_scores_gemma":[0.99947894,0.000120843804,0.000108567416,0.00015612159,0.00003117154,0.00010437052],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00015962975,0.00017164675,0.00037506703,0.00009493449,0.000059006314,0.000011822056,0.00011831547,0.00012768454,0.0020589195],"category_scores_gemma":[0.000017231856,0.00015014598,0.00002128536,0.00008340768,0.00023511189,0.000087402215,0.00003995489,0.0001838556,0.000008459284],"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":[0.00008833543,0.0000194352,0.97764397,0.00001428127,0.000011842084,0.0001841273,0.00045095076,0.00008133654,0.0037579166,0.000012932193,0.00056460884,0.01717027],"study_design_scores_gemma":[0.00068336417,0.00016069609,0.9822165,0.000011734962,0.000014396535,0.0005721556,0.0005742898,0.00031719264,0.0012221207,0.000054676304,0.01397557,0.00019731907],"about_ca_topic_score_codex":0.79829466,"about_ca_topic_score_gemma":0.99487144,"teacher_disagreement_score":0.19657679,"about_ca_system_score_codex":0.000014120413,"about_ca_system_score_gemma":0.00007661001,"threshold_uncertainty_score":0.9988533},"labels":[],"label_agreement":null},{"id":"W2022733285","doi":"10.1016/j.geomorph.2004.12.004","title":"Critical specific stream power in gravel-bed rivers","year":2005,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":141,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Trois-Rivières","funders":"","keywords":"Stream power; Bedform; Bed load; Geology; STREAMS; Hydrology (agriculture); Drainage basin; Shear stress; Tributary; Grain size; Geomorphology; Sediment transport; Sediment; Geotechnical engineering; Geography","score_opus":0.00886594640104589,"score_gpt":0.2304228780875066,"score_spread":0.22155693168646073,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2022733285","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":[0.97868276,0.000090314636,0.00022298154,0.002164628,0.00014801594,0.000074969015,0.000009085406,0.000032532982,0.018574705],"genre_scores_gemma":[0.9974495,0.000037358786,0.00093928364,0.0012900598,0.000028220229,0.000008621992,0.000018367753,0.0000075782814,0.00022100237],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989321,0.000041993928,0.00018535445,0.00032831967,0.000113090784,0.00039912236],"domain_scores_gemma":[0.9996765,0.000054404594,0.000020003681,0.0001620754,0.000004361938,0.00008264755],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00015596265,0.00011381878,0.00015265867,0.000045395853,0.000058838985,0.00000512434,0.0001900028,0.00014606885,0.056604963],"category_scores_gemma":[0.000019857343,0.00011157629,0.000031302836,0.00014173315,0.00059006875,0.00014214663,0.000043952095,0.00019250339,0.0039475476],"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":[0.00024196296,0.0011629004,0.9247275,0.0000099822555,0.000021218162,0.0015742377,0.0020381543,0.003027619,0.026113687,0.0049682306,0.02378149,0.012333023],"study_design_scores_gemma":[0.0018354906,0.00034986957,0.6534483,0.00000803807,0.000017769924,0.00021937047,0.00012662221,0.00011582951,0.009025092,0.004289632,0.3300633,0.00050066476],"about_ca_topic_score_codex":0.00009693448,"about_ca_topic_score_gemma":0.00045264652,"teacher_disagreement_score":0.3062818,"about_ca_system_score_codex":0.00005443143,"about_ca_system_score_gemma":0.00000711199,"threshold_uncertainty_score":0.996828},"labels":[],"label_agreement":null},{"id":"W2023235133","doi":"10.1016/j.geomorph.2015.02.016","title":"Corrigendum to “OSL-based lateral progradation and aeolian sediment accumulation rates for the Apalachicola Barrier Island Complex, North Gulf of Mexico, Florida” [Geomorphology 123 (2010) 330–342]","year":2015,"lang":"en","type":"erratum","venue":"Geomorphology","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"","keywords":"Progradation; Geology; Aeolian processes; Barrier island; Geomorphology; Sediment; Oceanography; Sediment transport; Hydrology (agriculture); Geotechnical engineering; Sedimentary depositional environment; Shore","score_opus":0.05349813689916135,"score_gpt":0.28680736763042025,"score_spread":0.2333092307312589,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2023235133","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":[0.64009005,0.012276466,0.05040929,0.017241213,0.19536656,0.025069553,0.054818336,0.0005133424,0.0042151953],"genre_scores_gemma":[0.8718005,0.00023298305,0.002596072,0.005128395,0.0034985668,0.0002889159,0.08605953,0.000103235165,0.030291792],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9968895,0.00025516812,0.00068829197,0.000828265,0.00042195566,0.0009168643],"domain_scores_gemma":[0.99774283,0.00036949583,0.00057847606,0.000538633,0.0004001144,0.00037042223],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000864031,0.00056877686,0.0009020336,0.00027076708,0.00038541487,0.0000931523,0.00055285933,0.000640738,0.0016553553],"category_scores_gemma":[0.0002086171,0.0004181056,0.00013742447,0.00035325476,0.00044902493,0.00014424438,0.00007381848,0.0005441038,0.00012882496],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007657437,0.00003765998,0.11895012,0.00028026113,0.00012904059,0.000029262577,0.00036815024,0.008327979,0.000033666598,0.00001538755,0.86720073,0.0038620215],"study_design_scores_gemma":[0.0018932918,0.0020769536,0.2502935,0.00006769675,0.00027643857,0.00011075024,0.00008313011,0.15387517,0.000069810856,0.000438139,0.5901632,0.000651968],"about_ca_topic_score_codex":0.005566813,"about_ca_topic_score_gemma":0.040772557,"teacher_disagreement_score":0.27703756,"about_ca_system_score_codex":0.000028054212,"about_ca_system_score_gemma":0.00049626786,"threshold_uncertainty_score":0.9998271},"labels":[],"label_agreement":null},{"id":"W2023410506","doi":"10.1016/j.geomorph.2014.12.013","title":"Coupling channel evolution monitoring and RFID tracking in a large, wandering, gravel-bed river: Insights into sediment routing on geomorphic continuity through a riffle–pool sequence","year":2014,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":61,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Bed load; Geology; Bedform; Hydrology (agriculture); Beach morphodynamics; Sediment transport; Channel (broadcasting); Riffle; Hyperconcentrated flow; Sediment; Geomorphology; Routing (electronic design automation); STREAMS; Geotechnical engineering","score_opus":0.016774948616037285,"score_gpt":0.25020134210756045,"score_spread":0.23342639349152317,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2023410506","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":[0.9887816,0.00020428801,0.009801536,0.00017639765,0.00033739652,0.00031348327,0.000004515375,0.00009397294,0.00028682617],"genre_scores_gemma":[0.99907184,0.00010054447,0.00035528376,0.0002557505,0.000091756,0.000052172018,0.000025785717,0.000022541266,0.000024342127],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9977104,0.00009986388,0.0004376364,0.00076971494,0.000277426,0.00070493727],"domain_scores_gemma":[0.9992992,0.00013818232,0.00018415946,0.00024660234,0.000020592688,0.00011125314],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.000738608,0.00030760697,0.00041434818,0.00009226708,0.00041376564,0.000023380733,0.0002415697,0.00028783694,0.00015798458],"category_scores_gemma":[0.00008098103,0.00030588455,0.000046291734,0.00026463426,0.00045434746,0.00034324412,0.00014856578,0.00049483933,0.00007780791],"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":[0.0002877416,0.0003858888,0.885359,0.000093137394,0.00004865918,0.00026713853,0.017448127,0.033205263,0.059534952,0.0022263448,0.000024500901,0.0011192616],"study_design_scores_gemma":[0.007903275,0.0012809756,0.83993745,0.0005021721,0.000119278404,0.00020135473,0.0012351798,0.07841619,0.046498775,0.01972279,0.0025904167,0.0015921544],"about_ca_topic_score_codex":0.0019502837,"about_ca_topic_score_gemma":0.00097380154,"teacher_disagreement_score":0.04542155,"about_ca_system_score_codex":0.0002620243,"about_ca_system_score_gemma":0.000019482706,"threshold_uncertainty_score":0.9999393},"labels":[],"label_agreement":null},{"id":"W2023561289","doi":"10.1016/s0169-555x(01)00066-6","title":"The braided Milk River, northern Montana, fails the Leopold–Wolman discharge-gradient test","year":2001,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":55,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; University of Calgary","keywords":"Silt; Tributary; Geology; Hydrology (agriculture); Stream power; Channel (broadcasting); Geomorphology; Bed load; Sediment; River bed; Sediment transport; Geotechnical engineering; Geography","score_opus":0.007585429035119864,"score_gpt":0.202506590653191,"score_spread":0.19492116161807113,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2023561289","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":[0.9806999,0.0004321025,0.00022042681,0.011029075,0.00030059254,0.00028518515,0.00001596121,0.00005621346,0.0069605275],"genre_scores_gemma":[0.99403584,0.00034518098,0.000024192013,0.002049104,0.00006691015,0.000058050202,0.000030330859,0.000015788222,0.0033745833],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99834794,0.000097416225,0.00027810183,0.00040377892,0.00022365201,0.00064913323],"domain_scores_gemma":[0.9989266,0.00035110826,0.00010314701,0.00050077453,0.000011247582,0.00010714325],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0004121887,0.00020683346,0.00018252083,0.000018015888,0.00093781855,0.000027544138,0.00073613226,0.00012543856,0.003842377],"category_scores_gemma":[0.00006318115,0.00011538047,0.00008478972,0.00022616149,0.0015360963,0.0001565753,0.00011728288,0.00028797326,0.002059054],"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":[0.00008145165,0.00021446733,0.9784318,0.0000028580366,0.000047312627,0.00023624358,0.0014151307,0.0009679887,0.0019299487,0.00037745608,0.010555398,0.005739936],"study_design_scores_gemma":[0.0007786599,0.00029752712,0.40878522,0.0000042424335,0.00005818438,0.00036925843,0.0003877941,0.00031698614,0.0006817333,0.002702785,0.5852988,0.00031881803],"about_ca_topic_score_codex":0.0017466753,"about_ca_topic_score_gemma":0.030903265,"teacher_disagreement_score":0.5747434,"about_ca_system_score_codex":0.000051294137,"about_ca_system_score_gemma":0.00001564607,"threshold_uncertainty_score":0.99871796},"labels":[],"label_agreement":null},{"id":"W2026389963","doi":"10.1016/j.geomorph.2004.09.018","title":"STARTER: a statistical GIS-based model for the prediction of snow avalanche susceptibility using terrain features—application to Alta Val Badia, Italian Dolomites","year":2004,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":55,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Terrain; Snowpack; Snow; Scale (ratio); Geology; Elevation (ballistics); Digital elevation model; Remote sensing; Cartography; Geometry; Geomorphology; Mathematics; Geography","score_opus":0.015573075350769497,"score_gpt":0.25794973597775395,"score_spread":0.24237666062698446,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2026389963","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.38005567,0.00000914272,0.6175596,0.0009766339,0.00009460653,0.0005807979,0.00065856625,0.00001772458,0.00004725302],"genre_scores_gemma":[0.98472685,0.0000022718302,0.014474355,0.00043524208,0.00003679913,0.000058082464,0.0001844118,0.000012390107,0.00006962583],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9989505,0.00004482305,0.0002352373,0.00033200317,0.00015585581,0.00028160284],"domain_scores_gemma":[0.99935037,0.00014246766,0.000079387086,0.00032062392,0.000019165333,0.00008798472],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036476547,0.00011705534,0.00016247288,0.000025120818,0.00013838084,0.000010562375,0.00017638765,0.0001527471,0.0002800619],"category_scores_gemma":[0.00007916533,0.00007989472,0.000059614784,0.00010847975,0.00026918878,0.00004276607,0.000057967434,0.00013100835,0.000027937753],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004329865,0.0002382474,0.018450838,0.000023457953,0.000039111877,0.0000039652145,0.0011065535,0.89439297,0.07453882,0.0006103416,0.0047783013,0.00538442],"study_design_scores_gemma":[0.0024837693,0.00071156095,0.093121424,0.000023549263,0.00015523199,0.00005706416,0.000118163225,0.88749707,0.0057926076,0.008289164,0.0014900189,0.0002603806],"about_ca_topic_score_codex":0.001272651,"about_ca_topic_score_gemma":0.0014905388,"teacher_disagreement_score":0.6046711,"about_ca_system_score_codex":0.00016868244,"about_ca_system_score_gemma":0.000042630458,"threshold_uncertainty_score":0.32580122},"labels":[],"label_agreement":null},{"id":"W2027097413","doi":"10.1016/j.geomorph.2013.03.028","title":"Late Quaternary stream piracy and strath terrace formation along the Belle Fourche and lower Cheyenne Rivers, South Dakota and Wyoming","year":2013,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"U.S. Geological Survey; U.S. Department of Defense","keywords":"Geology; Terrace (agriculture); Fluvial; River terraces; Radiocarbon dating; Archaeology; Glacial period; Butte; Ephemeral key; Tributary; Aggradation; Geomorphology; Physiographic province; Paleontology; Structural basin; Geography","score_opus":0.01865324655274549,"score_gpt":0.21636796561052557,"score_spread":0.19771471905778007,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2027097413","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":[0.9960004,0.0011419328,0.000032396518,0.0017944874,0.00011185221,0.00023751406,0.000025975774,0.000016090404,0.0006393417],"genre_scores_gemma":[0.99869406,0.0002869476,0.00022217778,0.00030025505,0.000029664769,0.000003566303,0.000067304434,0.0000026331986,0.0003933836],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99892974,0.00019735136,0.00016088584,0.00025496155,0.000074063224,0.00038301156],"domain_scores_gemma":[0.99930763,0.00032969064,0.00007478924,0.00015308059,0.00002773338,0.00010706262],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00038865994,0.0001287916,0.00017268813,0.0000618459,0.00058757915,0.00004087159,0.00012532475,0.00015770536,0.0013844105],"category_scores_gemma":[0.00004117158,0.000087634566,0.000015498355,0.00005859424,0.0006187599,0.0002765397,0.00009142434,0.0002844294,0.00015095403],"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":[0.00004020933,0.0000058997657,0.9952057,0.000015524824,0.000017912103,0.000053881013,0.0015033887,0.00001939439,0.000049280312,0.000017264087,0.00027692024,0.0027946045],"study_design_scores_gemma":[0.0005582133,0.0002216929,0.99042296,0.000007606544,0.000019988714,0.00069707545,0.00096025335,0.0052497503,0.000034100187,0.0012669923,0.00044059876,0.00012076626],"about_ca_topic_score_codex":0.002554058,"about_ca_topic_score_gemma":0.0062941634,"teacher_disagreement_score":0.005230356,"about_ca_system_score_codex":7.09918e-7,"about_ca_system_score_gemma":0.000015164264,"threshold_uncertainty_score":0.99952847},"labels":[],"label_agreement":null},{"id":"W2036755080","doi":"10.1016/j.geomorph.2004.07.001","title":"Theoretical regime equations for mobile gravel-bed rivers with stable banks","year":2004,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":183,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Dimensionless quantity; Bed load; Geology; Sediment; Riparian zone; Geometry; Sediment transport; Suspended load; Hydraulics; Geotechnical engineering; Hydrology (agriculture); Mechanics; Geomorphology; Mathematics; Physics; Thermodynamics","score_opus":0.00751826644637542,"score_gpt":0.21697501416220746,"score_spread":0.20945674771583203,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2036755080","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":[0.9039143,0.000034709927,0.087586,0.0012948592,0.00009173395,0.00054825045,0.00004854728,0.00006960159,0.006412022],"genre_scores_gemma":[0.9950549,0.000008360527,0.003626877,0.0007636793,0.000016532267,0.00017591164,0.00010237704,0.00001172292,0.00023963403],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9990754,0.000019990326,0.00012944573,0.00030844848,0.00010680385,0.00035987434],"domain_scores_gemma":[0.9995943,0.00009525576,0.00004138265,0.00017855142,0.0000113021815,0.00007920986],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00016382388,0.000114851944,0.00014892512,0.000024601082,0.00018268378,0.000006073546,0.00017061962,0.00012112621,0.011761447],"category_scores_gemma":[0.000018014212,0.00009301374,0.000033470515,0.00012461553,0.0010691341,0.000093107046,0.000025898515,0.00010776417,0.00038869955],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015060379,0.0012052621,0.030950489,0.000050548548,0.00018488365,0.0003628928,0.0034923877,0.1380286,0.021826966,0.795841,0.0027811923,0.0037697863],"study_design_scores_gemma":[0.02060189,0.009362284,0.019372215,0.000055037,0.0006759932,0.00059891795,0.0006987069,0.0021163104,0.09615883,0.7083377,0.13979493,0.0022271436],"about_ca_topic_score_codex":0.00012132677,"about_ca_topic_score_gemma":0.00017620601,"teacher_disagreement_score":0.13701375,"about_ca_system_score_codex":0.00004761359,"about_ca_system_score_gemma":0.00003049439,"threshold_uncertainty_score":0.98914194},"labels":[],"label_agreement":null},{"id":"W2037322781","doi":"10.1016/j.geomorph.2013.04.024","title":"Evaluating the effectiveness of wood shred and agricultural straw mulches as a treatment to reduce post-wildfire hillslope erosion in southern British Columbia, Canada","year":2013,"lang":"en","type":"article","venue":"Geomorphology","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":94,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Ministry of Forests","funders":"Rocky Mountain Research Station; U.S. Forest Service; Joint Fire Science Program; U.S. Department of the Interior","keywords":"Surface runoff; Mulch; Sediment; Environmental science; Hydrology (agriculture); Erosion; Rill; Straw; Vegetation (pathology); Erosion control; Soil water; Geology; Soil science; Agronomy; Ecology; Geomorphology","score_opus":0.00797633214226134,"score_gpt":0.22238796085325843,"score_spread":0.2144116287109971,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2037322781","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":[0.99766624,0.00006199212,4.972889e-7,0.0002338035,0.0001365098,0.001658672,0.00006645224,0.000011193185,0.00016462099],"genre_scores_gemma":[0.99916977,0.0000026823375,0.00005722328,0.00012476469,0.000014178576,0.00027736256,0.000025640034,0.000012506959,0.00031586608],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99816954,0.0006525953,0.00023542425,0.0003908525,0.00021886962,0.0003327307],"domain_scores_gemma":[0.99913865,0.00043768622,0.000093940755,0.0002123361,0.000020454887,0.00009694968],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005443456,0.00012961388,0.0002840734,0.000011549407,0.00012147701,0.00006446864,0.00018231681,0.0000785374,0.0006461866],"category_scores_gemma":[0.00020079658,0.00011613693,0.000029012206,0.00017119179,0.0001210979,0.000081341095,0.00013382144,0.00008651874,0.0000866061],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000070235095,0.00014064321,0.24695295,0.000032870408,0.000027909808,0.000051802737,0.0013526928,0.00028703018,0.7183251,4.2098594e-7,0.0006640223,0.03209433],"study_design_scores_gemma":[0.0008706286,0.0010552439,0.9938392,0.00008494863,0.000013722873,0.00021392161,0.0010228355,0.00018826003,0.0025138801,0.000020457037,0.000027593895,0.00014929818],"about_ca_topic_score_codex":0.9973573,"about_ca_topic_score_gemma":0.9918707,"teacher_disagreement_score":0.74688625,"about_ca_system_score_codex":0.00045891578,"about_ca_system_score_gemma":0.0000612048,"threshold_uncertainty_score":0.70752895},"labels":[],"label_agreement":null},{"id":"W2039255694","doi":"10.1016/j.geomorph.2014.04.002","title":"Geomorphic response of Lillooet River, British Columbia, to meander cutoffs and base level lowering","year":2014,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":18,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"BGC Engineering (Canada)","funders":"","keywords":"Meander (mathematics); Geology; Geomorphology; Hydrology (agriculture); Geotechnical engineering; Geometry","score_opus":0.012056225326678756,"score_gpt":0.20327604635653523,"score_spread":0.1912198210298565,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2039255694","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":[0.99622774,0.000055548717,0.00247586,0.00035918108,0.00013079325,0.00015977361,0.000064371176,0.000031660475,0.0004950923],"genre_scores_gemma":[0.9959492,0.00002694371,0.00077529787,0.0014162167,0.000017405211,0.00001646536,0.000017871367,0.000014487988,0.0017660852],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986959,0.00011864168,0.00025332844,0.00042444596,0.00015453972,0.00035315388],"domain_scores_gemma":[0.9993539,0.00016482623,0.00006742608,0.00023340342,0.00001534004,0.000165131],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007515586,0.00010878488,0.0002742076,0.000032832115,0.0001404924,0.000018872586,0.00020255911,0.000150505,0.007431208],"category_scores_gemma":[0.00015076066,0.00015957028,0.00003436621,0.00015460685,0.0006596687,0.000097153315,0.0001400215,0.00013073432,0.00019062882],"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":[0.0008912538,0.00033709407,0.8438984,0.00006667405,0.000058405993,0.000467654,0.0011357499,0.0018879165,0.1220481,0.000021711248,0.017402666,0.011784346],"study_design_scores_gemma":[0.0012462845,0.0006377394,0.9704493,0.000025929909,0.000035684145,0.0004019061,0.000024972991,0.00015293287,0.0032790154,0.0005441636,0.022907862,0.0002941667],"about_ca_topic_score_codex":0.013701342,"about_ca_topic_score_gemma":0.015674014,"teacher_disagreement_score":0.12655091,"about_ca_system_score_codex":0.000020986081,"about_ca_system_score_gemma":0.000014025856,"threshold_uncertainty_score":0.99347615},"labels":[],"label_agreement":null},{"id":"W2039461471","doi":"10.1016/j.geomorph.2006.04.018","title":"Formation and deformation of basal till during a glacier surge; Elisebreen, Svalbard","year":2006,"lang":"en","type":"article","venue":"Geomorphology","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Brock University","funders":"Knud Højgaards Fond; Brock University; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung","keywords":"Geology; Surge; Geomorphology; Glacier; Moraine; Landform; Erosion; Seabed gouging by ice; Paleontology; Arctic ice pack; Arctic; Antarctic sea ice; Oceanography","score_opus":0.008555986630194246,"score_gpt":0.17657218757276621,"score_spread":0.16801620094257197,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2039461471","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":[0.99788797,0.00036705547,0.00029862075,0.0002678398,0.00011967829,0.00008184822,0.000053350155,0.000014483548,0.0009091323],"genre_scores_gemma":[0.9991025,0.00006976862,0.00039471532,0.00008749406,0.00004724201,0.0000011791287,0.00021780908,0.0000014098764,0.00007791542],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99944973,0.0000150672095,0.00020995238,0.00008749777,0.000081950806,0.00015579295],"domain_scores_gemma":[0.9997295,0.000038246824,0.0000909516,0.00007298653,0.000044702432,0.000023601127],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011333644,0.0000628128,0.00011733234,0.00002997309,0.00010827006,0.0000091738675,0.000042580054,0.000042352447,0.00073407864],"category_scores_gemma":[0.000011995844,0.000053730324,0.000023991357,0.00011727374,0.00006608915,0.00018698802,0.0000114499,0.00003969684,0.000032875614],"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":[0.000031494965,0.00000874135,0.99368787,0.000030953324,0.0000069131243,0.000004309476,0.00024962527,0.0014473917,0.00027045966,0.000117103395,0.0013908901,0.0027542617],"study_design_scores_gemma":[0.00026111366,0.000033209955,0.99265563,0.0000035347446,0.000008047345,0.000033284738,0.00017709367,0.0028238758,0.00027385823,0.00037057872,0.003298478,0.000061298815],"about_ca_topic_score_codex":0.0031511176,"about_ca_topic_score_gemma":0.004077641,"teacher_disagreement_score":0.002692963,"about_ca_system_score_codex":0.0000030732883,"about_ca_system_score_gemma":0.000007893908,"threshold_uncertainty_score":0.8037646},"labels":[],"label_agreement":null},{"id":"W2040245551","doi":"10.1016/j.geomorph.2008.05.027","title":"Sea level and climate changes during OIS 5e in the Western Mediterranean","year":2008,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":111,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Geology; Interglacial; Mediterranean climate; Northern Hemisphere; Oceanography; Climate change; Mediterranean sea; Climatology; Paleoclimatology; Facies; Westerlies; Glacial period; Paleontology; Physical geography; Structural basin","score_opus":0.07324286623983214,"score_gpt":0.26065147796734817,"score_spread":0.18740861172751602,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2040245551","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":[0.99244815,0.00076878566,0.0000010325774,0.0049925153,0.00017961842,0.00012956916,0.00008639659,0.000016069547,0.0013778753],"genre_scores_gemma":[0.9975972,0.000911252,0.000034970482,0.0010707085,0.00007196765,0.0000045941965,0.00014664733,0.0000022332606,0.00016038281],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985936,0.00033002047,0.00013682722,0.00025605859,0.00011944423,0.00056400953],"domain_scores_gemma":[0.999371,0.0003280412,0.000038222024,0.00018352307,0.000015201332,0.00006400994],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00052226125,0.00011356868,0.00020100678,0.00012464978,0.00031456348,0.00000886654,0.00026076354,0.00015985702,0.00090545474],"category_scores_gemma":[0.00003784303,0.00007836018,0.000018335073,0.00013911109,0.0006303472,0.000057618166,0.00003255311,0.00033008723,0.00038986804],"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":[0.000062871506,0.000009181418,0.9967558,0.00001698627,0.000006050892,0.0014219224,0.0012306897,0.000011395751,0.000013676456,0.000006162731,0.00020709919,0.0002581873],"study_design_scores_gemma":[0.00048116737,0.00011004187,0.99045384,0.0000045362867,0.0000041159997,0.007791601,0.0001503024,0.00006972695,0.00003281664,0.00004323124,0.0007714924,0.00008712728],"about_ca_topic_score_codex":0.0011601226,"about_ca_topic_score_gemma":0.06835844,"teacher_disagreement_score":0.06719832,"about_ca_system_score_codex":6.0405864e-7,"about_ca_system_score_gemma":0.000017228498,"threshold_uncertainty_score":0.9914094},"labels":[],"label_agreement":null},{"id":"W2040335708","doi":"10.1016/j.geomorph.2013.04.023","title":"Assessing significant geomorphic changes and effectiveness of dynamic restoration in a coastal dune ecosystem","year":2013,"lang":"en","type":"article","venue":"Geomorphology","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Mitacs; Parks Canada; University of Victoria","keywords":"Foredune; Geology; Sedimentary budget; Sedimentary depositional environment; Transgressive; Sediment; Vegetation (pathology); Beach ridge; Deposition (geology); Hydrology (agriculture); Sediment transport; Aeolian processes; Physical geography; Geomorphology; Geography; Structural basin","score_opus":0.011038201617732057,"score_gpt":0.22584903659951167,"score_spread":0.2148108349817796,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2040335708","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":[0.9984137,0.00038092743,0.00033495494,0.00015923624,0.00016588558,0.00035649945,0.00005126479,0.000015198853,0.00012232114],"genre_scores_gemma":[0.9995845,0.000045016044,0.00014600369,0.00003099997,0.000016940478,0.000010274203,0.00015322438,0.0000039185893,0.000009137035],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99890536,0.0003025147,0.0001772458,0.00024606183,0.00010744724,0.0002613778],"domain_scores_gemma":[0.99928796,0.00036271563,0.0001164414,0.000108652814,0.000057957273,0.00006627237],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006432223,0.00011505804,0.00027627443,0.00014598107,0.00005333702,0.00004431041,0.000087914195,0.00010531982,0.00036067166],"category_scores_gemma":[0.00006283963,0.00009812784,0.00001549857,0.00021736036,0.00010567435,0.0002599029,0.00001717074,0.00010740249,0.000058383812],"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":[0.00013438828,0.00004436821,0.9269513,0.0011786199,0.000020936728,0.00014086647,0.00023157998,0.0022680326,0.027929453,0.00007100799,0.000043299264,0.04098615],"study_design_scores_gemma":[0.00043140943,0.0002817953,0.94646007,0.00011269514,0.0000068621994,0.00009428348,0.00019614385,0.051381215,0.0004462769,0.00044654057,0.000028402716,0.00011427675],"about_ca_topic_score_codex":0.007246054,"about_ca_topic_score_gemma":0.02274652,"teacher_disagreement_score":0.049113184,"about_ca_system_score_codex":0.000005725421,"about_ca_system_score_gemma":0.000040923853,"threshold_uncertainty_score":0.9993648},"labels":[],"label_agreement":null},{"id":"W2040366226","doi":"10.1016/s0169-555x(02)00323-9","title":"The long-term control of vegetation and woody debris on channel and flood-plain evolution: insights from a paired catchment study in southeastern Australia","year":2003,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":204,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Floodplain; Geology; Riparian zone; Alluvium; Channel (broadcasting); Context (archaeology); Hydrology (agriculture); Drainage basin; Flood control; Fluvial; Debris; Flood myth; Vegetation (pathology); Alluvial plain; Physical geography; Ecology; Geomorphology; Geography; Habitat; Archaeology; Structural basin; Paleontology; Oceanography","score_opus":0.01402898531394518,"score_gpt":0.22884074970719853,"score_spread":0.21481176439325336,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2040366226","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":[0.9986063,0.00045220376,0.00028733374,0.00012733552,0.0000817577,0.0003828598,0.0000071747345,0.000006487714,0.000048513844],"genre_scores_gemma":[0.9997948,0.000020444137,0.0000075610164,0.00008382583,0.0000075594044,0.000042091004,0.000008055803,0.0000043929704,0.00003126358],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99903214,0.0001956764,0.00021487536,0.00027089877,0.00010843956,0.00017797366],"domain_scores_gemma":[0.9996409,0.00010656183,0.0000725584,0.00012867761,0.0000052872265,0.000046020614],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021302157,0.00011213708,0.00017398821,0.00002889469,0.0001076662,0.000006018122,0.00007638709,0.00008296581,0.00008403996],"category_scores_gemma":[0.000014366038,0.000082961065,0.000012916343,0.00007161309,0.0002835321,0.000052650394,0.0000157046,0.00010106327,0.000025312653],"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":[0.0001345027,0.00024125069,0.99571306,0.000005005342,0.000026375184,0.000048647842,0.0023179592,0.00037245898,0.0008766569,0.000078540674,0.0000032734324,0.00018226661],"study_design_scores_gemma":[0.0020884457,0.00047931392,0.9957133,0.000009334759,0.000035246005,0.0000075649555,0.0002855717,0.00013352951,0.000383912,0.00075834955,0.00002397658,0.00008146851],"about_ca_topic_score_codex":0.00081221753,"about_ca_topic_score_gemma":0.007860875,"teacher_disagreement_score":0.007048657,"about_ca_system_score_codex":0.000019384477,"about_ca_system_score_gemma":0.0000066346524,"threshold_uncertainty_score":0.43865526},"labels":[],"label_agreement":null},{"id":"W2042195394","doi":"10.1016/j.geomorph.2013.03.023","title":"Geomorphological mapping with a small unmanned aircraft system (sUAS): Feature detection and accuracy assessment of a photogrammetrically-derived digital terrain model","year":2013,"lang":"en","type":"article","venue":"Geomorphology","topic":"Remote Sensing and LiDAR Applications","field":"Environmental Science","cited_by":338,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Lethbridge; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; U.S. Geological Survey; Alberta Innovates; Cenovus Energy","keywords":"Orthophoto; Remote sensing; Digital elevation model; Photogrammetry; Geology; Terrain; Landform; Global Positioning System; Aerial photography; Mean squared error; Feature (linguistics); Lidar; Satellite imagery; Cartography; Geography; Geomorphology; Computer science","score_opus":0.013541401986783674,"score_gpt":0.21979000102067855,"score_spread":0.2062485990338949,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2042195394","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":[0.8413111,0.000009573302,0.15548891,0.0004961313,0.000027902906,0.0005935241,0.00001550336,0.000086598004,0.001970783],"genre_scores_gemma":[0.97032946,0.0000063937086,0.029224265,0.00014940095,0.000014062593,0.000046432284,0.000030759176,0.000018721375,0.00018047568],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99856406,0.00007292164,0.00027331998,0.0005125137,0.00019770706,0.0003794604],"domain_scores_gemma":[0.999117,0.0001365359,0.00020737374,0.0003480032,0.000038328555,0.00015272269],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016880417,0.00021339934,0.00032525786,0.00009730763,0.00016017772,0.00006376319,0.00018213759,0.0001973549,0.000092362054],"category_scores_gemma":[0.00006481014,0.00016423459,0.000056822995,0.00040892165,0.0004450032,0.00013355704,0.00018735128,0.00025529962,0.000057781308],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009876638,0.00042648628,0.020360928,0.000079607824,0.000108330365,0.0000841975,0.0007410532,0.008270841,0.8721899,0.000097278375,0.0010842144,0.0964584],"study_design_scores_gemma":[0.0027465716,0.0012807592,0.44467488,0.000117136624,0.000116785115,0.003260827,0.0026156656,0.53253686,0.008080653,0.00050885224,0.0029889192,0.001072109],"about_ca_topic_score_codex":0.0010802699,"about_ca_topic_score_gemma":0.00015177665,"teacher_disagreement_score":0.8641093,"about_ca_system_score_codex":0.00012735666,"about_ca_system_score_gemma":0.00001881143,"threshold_uncertainty_score":0.66972923},"labels":[],"label_agreement":null},{"id":"W2044492296","doi":"10.1016/j.geomorph.2009.06.029","title":"A method to assess fluvial fan channel networks, with a preliminary application to fans in coastal British Columbia","year":2009,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Government of British Columbia","funders":"","keywords":"Channel (broadcasting); Geology; Alluvial fan; Debris flow; Fluvial; Hydrology (agriculture); Sediment; Sinuosity; Debris; Geomorphology; Oceanography; Structural basin","score_opus":0.008265371421443696,"score_gpt":0.23742901564176352,"score_spread":0.22916364422031982,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2044492296","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":[0.67320025,0.000011210472,0.32465348,0.00084950123,0.000033921817,0.00053851923,0.000020695406,0.000043831675,0.00064858276],"genre_scores_gemma":[0.9856101,0.0000044535595,0.009225618,0.0044742175,0.00004107289,0.00019173454,0.0000913078,0.000012178568,0.00034929658],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985251,0.00008817901,0.0002157005,0.00055147725,0.0001423805,0.00047718905],"domain_scores_gemma":[0.9995459,0.000042513413,0.000044222877,0.00018436144,0.00001043136,0.00017262783],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00035096187,0.00012009177,0.00024035799,0.00003531248,0.00012164741,0.00003151376,0.00026131523,0.00015351146,0.000933602],"category_scores_gemma":[0.000007955319,0.00016506654,0.000022406433,0.00044803298,0.000090264184,0.00010709558,0.000060828188,0.00018745693,0.00012746213],"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":[0.0015383908,0.0013091342,0.45918468,0.00001820999,0.00003330954,0.0015157091,0.0019420309,0.3789367,0.014121189,0.000034894736,0.019082703,0.122283064],"study_design_scores_gemma":[0.00094974757,0.002392411,0.98220646,0.000021679589,0.000025535868,0.0004768273,0.00006364092,0.0028328118,0.00031361,0.0003388542,0.010009896,0.00036849492],"about_ca_topic_score_codex":0.013257984,"about_ca_topic_score_gemma":0.18527627,"teacher_disagreement_score":0.5230218,"about_ca_system_score_codex":0.00004093384,"about_ca_system_score_gemma":0.000015854272,"threshold_uncertainty_score":0.9999797},"labels":[],"label_agreement":null},{"id":"W2045088484","doi":"10.1016/j.geomorph.2012.03.015","title":"Deglaciation landforms and C-14 chronology of the Lac Guillaume-Delisle area, eastern Hudson Bay: A report on field evidence","year":2012,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval; Center for Northern Studies; Centre de Géomatique du Québec","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; Fonds Québécois de la Recherche sur la Nature et les Technologies; Université Laval","keywords":"Deglaciation; Geology; Moraine; Ice sheet; Glacier; Oceanography; Geomorphology; Landform; Terminal moraine; Paleontology; Holocene","score_opus":0.03741889102726922,"score_gpt":0.26551816399769396,"score_spread":0.22809927297042473,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045088484","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":[0.99105906,0.0011110884,0.000048925634,0.003600288,0.000634312,0.00016267486,0.00001005515,0.000013698091,0.003359894],"genre_scores_gemma":[0.99843013,0.0001050434,0.00006868715,0.00073419826,0.00006901344,0.0000035133405,0.000035037712,0.0000021878607,0.00055217714],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987185,0.0002263628,0.0002492948,0.0002287017,0.00013338063,0.00044378478],"domain_scores_gemma":[0.99865973,0.0006899363,0.00016222532,0.00035384207,0.000054689604,0.00007957525],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000768282,0.000110142995,0.00023023131,0.000072944174,0.00014204723,0.0000059240306,0.00022052256,0.0002711533,0.0021994442],"category_scores_gemma":[0.0006660074,0.00007130511,0.000042967455,0.00011891441,0.0003232039,0.000113982904,0.000053476197,0.00028026206,0.00022911276],"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":[0.00011227229,0.000014992157,0.9977807,0.000014006187,0.00001610048,0.000033130862,0.00015282122,0.000029519702,0.000020354273,0.000077370474,0.00070423645,0.0010445238],"study_design_scores_gemma":[0.00023169983,0.0003025731,0.99531287,0.00001980087,0.000015414375,0.0014794603,0.000052757023,0.00027198857,0.00039417137,0.00035655365,0.0014816187,0.000081069484],"about_ca_topic_score_codex":0.0006988444,"about_ca_topic_score_gemma":0.0049549597,"teacher_disagreement_score":0.007371078,"about_ca_system_score_codex":0.0000016151558,"about_ca_system_score_gemma":0.000042210922,"threshold_uncertainty_score":0.99871266},"labels":[],"label_agreement":null},{"id":"W2045639757","doi":"10.1016/j.geomorph.2005.12.006","title":"Contribution of remote sensing techniques to the identification and characterization of Miocene calderas, Lesvos Island, Aegean Sea, Hellas","year":2006,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":12,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Concordia University","funders":"","keywords":"Caldera; Geology; Volcano; Lava; Digital elevation model; Thematic Mapper; Stratovolcano; Seismology; Geomorphology; Remote sensing; Satellite imagery","score_opus":0.007489136284008205,"score_gpt":0.21405564250010659,"score_spread":0.20656650621609837,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045639757","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.46591192,0.000021870339,0.5294012,0.004294537,0.00006122897,0.00014681749,0.000014450806,0.000022998616,0.00012500686],"genre_scores_gemma":[0.99560016,0.00001137873,0.0038749075,0.00013950757,0.000044407767,9.5121527e-7,0.000109368906,0.0000014962962,0.00021781077],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99921125,0.00007458085,0.0002915027,0.00020399713,0.000082603205,0.00013605316],"domain_scores_gemma":[0.9991728,0.000041565512,0.00022889632,0.00027873894,0.00025974438,0.00001822502],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041171192,0.000072197,0.00014434467,0.000047868783,0.00007147425,0.000015697278,0.00016512947,0.00007932207,0.0000068630584],"category_scores_gemma":[0.00008201195,0.000059939237,0.000020499512,0.00018611993,0.000072725175,0.00005239225,0.00009684252,0.000055207765,0.0000027144486],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009043982,0.000011286309,0.00051479595,0.000016500391,0.0000041932803,0.0000037051157,0.000091010406,0.000023034236,0.97687286,0.0012913934,0.0003544229,0.020807778],"study_design_scores_gemma":[0.00013146429,0.000045573142,0.014892687,0.000023282904,0.000007435329,0.00010971573,0.0000085257725,0.008163434,0.96327376,0.0025930672,0.010674273,0.00007676467],"about_ca_topic_score_codex":0.00030345813,"about_ca_topic_score_gemma":0.00007865665,"teacher_disagreement_score":0.52968824,"about_ca_system_score_codex":0.000010382466,"about_ca_system_score_gemma":0.000014919046,"threshold_uncertainty_score":0.2444251},"labels":[],"label_agreement":null},{"id":"W2046553186","doi":"10.1016/j.geomorph.2013.10.001","title":"Dynamics of active layer in wooded palsas of northern Quebec","year":2013,"lang":"en","type":"article","venue":"Geomorphology","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Center for Northern Studies; Natural Sciences and Engineering Research Council; Université Laval","funders":"Fonds Québécois de la Recherche sur la Nature et les Technologies","keywords":"Permafrost; Active layer; Geology; Vegetation (pathology); Snow; Black spruce; Physical geography; Hydrology (agriculture); Taiga; Geomorphology; Layer (electronics); Ecology; Oceanography; Geography","score_opus":0.023028085980797204,"score_gpt":0.22706084977101684,"score_spread":0.20403276379021965,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2046553186","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":[0.99607664,0.00009966218,0.0000042590996,0.00043234217,0.000111186986,0.00012227881,0.0012652414,0.0000041936146,0.0018841855],"genre_scores_gemma":[0.99809444,0.00003353792,0.000025292027,0.00011200082,0.000018373783,0.0000015916924,0.0015147041,0.0000022752504,0.0001978034],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993688,0.00004158652,0.00020053516,0.00012267014,0.00007205593,0.000194343],"domain_scores_gemma":[0.99957705,0.00010125975,0.00010059428,0.00013142994,0.00005281441,0.000036838963],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0000779976,0.000074068164,0.00021440731,0.000078362595,0.000013519376,0.0000034129841,0.000123622,0.00008885387,0.021558477],"category_scores_gemma":[0.000014138881,0.00006239255,0.000033001405,0.00013036221,0.00012140405,0.00007241813,0.000012238231,0.00008135983,0.00027521397],"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":[0.00003189944,0.000022228263,0.9892839,0.000013473691,0.000007444905,0.000010057954,0.00069575896,0.00013307921,0.0011245644,0.000023199329,0.00013751142,0.0085168695],"study_design_scores_gemma":[0.00027924395,0.000084959116,0.99586886,0.000008074122,0.0000044610742,0.000011505807,0.0008281091,0.0016099042,0.0006174346,0.00052516407,0.00009182336,0.00007043411],"about_ca_topic_score_codex":0.4897976,"about_ca_topic_score_gemma":0.94880235,"teacher_disagreement_score":0.4590048,"about_ca_system_score_codex":0.000005548869,"about_ca_system_score_gemma":0.000029295983,"threshold_uncertainty_score":0.97933596},"labels":[],"label_agreement":null},{"id":"W2047781452","doi":"10.1016/j.geomorph.2014.04.036","title":"Seasonal-scale abrasion and quarrying patterns from a two-dimensional ice-flow model coupled to distributed and channelized subglacial drainage","year":2014,"lang":"en","type":"article","venue":"Geomorphology","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University; Trinity Western University; Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada; Simon Fraser University","keywords":"Geology; Meltwater; Plucking; Channelized; Geomorphology; Glacier; Erosion; Abrasion (mechanical); Drainage system (geomorphology); Ice sheet; Hydrology (agriculture); Drainage; Geotechnical engineering","score_opus":0.013514039511094528,"score_gpt":0.21624318591055447,"score_spread":0.20272914639945994,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2047781452","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":[0.97649455,0.0002451201,0.020218514,0.0015506835,0.00021340887,0.00016682531,0.0010450316,0.00003320582,0.000032643788],"genre_scores_gemma":[0.99386925,0.0000213101,0.0033855347,0.0013315735,0.00015581856,0.0000044165786,0.0011868741,0.0000048584366,0.00004036123],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9989173,0.00005990055,0.00017639493,0.00038385144,0.00014367673,0.00031891293],"domain_scores_gemma":[0.9992966,0.00028307372,0.00005597386,0.00013249874,0.000047432823,0.00018444103],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019292026,0.00015366451,0.00026675625,0.000022570499,0.00033575852,0.000036051188,0.00008476198,0.000072166724,0.0007334147],"category_scores_gemma":[0.00006723639,0.00013521612,0.000030241963,0.00009364827,0.0000872511,0.00006687995,0.000060316932,0.000100115816,0.000035843495],"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":[0.00036756604,0.000030924206,0.8574998,0.000015512465,0.00004828328,0.00003070859,0.0011703748,0.122572355,0.0011552684,0.00007248399,0.0014960786,0.015540675],"study_design_scores_gemma":[0.00070674415,0.00006733721,0.4517639,0.000007612835,0.00001632962,0.0000091003185,0.000079665486,0.5461075,0.0000055203095,0.0006776463,0.00044373787,0.00011495291],"about_ca_topic_score_codex":0.0067509655,"about_ca_topic_score_gemma":0.0149838375,"teacher_disagreement_score":0.4235351,"about_ca_system_score_codex":0.0000045407496,"about_ca_system_score_gemma":0.0000162018,"threshold_uncertainty_score":0.99986315},"labels":[],"label_agreement":null},{"id":"W2049049921","doi":"10.1016/j.geomorph.2008.02.009","title":"Natural levee deposition during the 2005 flood of the Saskatchewan River","year":2008,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":78,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Levee; Geology; Aggradation; Deposition (geology); Floodplain; Hydrology (agriculture); Erosion; Channel (broadcasting); Sediment; Silt; Flood myth; Sedimentation; Overbank; Geomorphology; Fluvial; Geotechnical engineering; Geography; Archaeology","score_opus":0.005249769250931363,"score_gpt":0.17829034228225057,"score_spread":0.1730405730313192,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2049049921","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":[0.9981068,0.00010181417,0.000045829085,0.0008097969,0.00018640935,0.00010445758,0.0000069431735,0.000014282732,0.00062367646],"genre_scores_gemma":[0.99800116,0.000018788416,0.000082670726,0.000575434,0.000025622929,0.000007599713,0.0000059577446,0.0000048662564,0.0012778736],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992985,0.00005866783,0.0001356981,0.00015778934,0.00012787552,0.00022145192],"domain_scores_gemma":[0.9996763,0.000028133858,0.000061637395,0.00020665933,0.000004671292,0.000022596172],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00009076523,0.00008049302,0.00009531959,0.000009579797,0.00031534856,0.0000012572682,0.0002844936,0.00007592264,0.002161884],"category_scores_gemma":[0.0000065600807,0.00004601954,0.000050987437,0.00009755722,0.000999362,0.000069417336,0.00007430914,0.00017922565,0.00013879455],"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":[0.00011468086,0.00015578562,0.7664563,0.000014236484,0.000048188373,0.00012880091,0.004540162,0.0025117954,0.22331037,0.000024276214,0.0023092336,0.00038616217],"study_design_scores_gemma":[0.0003562914,0.000026069916,0.9299675,0.0000027667725,0.000020225549,0.00050638703,0.00006440368,0.00004092978,0.06728407,0.00011147284,0.0015460677,0.00007381546],"about_ca_topic_score_codex":0.00047370535,"about_ca_topic_score_gemma":0.0014632613,"teacher_disagreement_score":0.16351119,"about_ca_system_score_codex":0.000022119371,"about_ca_system_score_gemma":0.000013387187,"threshold_uncertainty_score":0.99875027},"labels":[],"label_agreement":null},{"id":"W2049474720","doi":"10.1016/s0169-555x(01)00026-5","title":"Aeolian erosional lineations in the Libyan Desert, Dakhla Region, Egypt","year":2001,"lang":"en","type":"article","venue":"Geomorphology","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":64,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Social Sciences and Humanities Research Council of Canada; Natural Sciences and Engineering Research Council of Canada; York University","keywords":"Geology; Lineation; Aeolian processes; Geomorphology; Bedrock; Erosion; Landform; Lithology; Outcrop; Paleontology; Tectonics","score_opus":0.021525442201983234,"score_gpt":0.22449455552510028,"score_spread":0.20296911332311704,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2049474720","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":[0.9817586,0.00045980737,0.0006249052,0.0073898872,0.00026395105,0.00016787964,0.000020435673,0.00003046021,0.009284107],"genre_scores_gemma":[0.99508506,0.00013081107,0.00016746788,0.003369563,0.00017473401,0.0000044824064,0.00021627216,0.0000029665305,0.00084861973],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990414,0.00011911223,0.00016058124,0.00021110737,0.00012726449,0.00034056415],"domain_scores_gemma":[0.99944323,0.00021313872,0.00004701405,0.00020261695,0.000026437016,0.000067564404],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002477766,0.00010372117,0.00012240186,0.000072061484,0.00015159728,0.000027912229,0.00032393364,0.00009025672,0.0020894378],"category_scores_gemma":[0.000064650856,0.00006893254,0.0000355533,0.00037835073,0.00013514169,0.000110392066,0.00001234914,0.00018631078,0.0006940011],"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":[0.00005813193,0.00004120713,0.9622229,0.000008297026,0.000005181519,0.00074712414,0.0005108128,0.0037584223,0.000018957398,0.0005663712,0.023594746,0.00846789],"study_design_scores_gemma":[0.0004057729,0.00018572359,0.88158643,0.000013174199,0.000008920518,0.0017757039,0.0002655178,0.008365043,0.000016167274,0.0037827431,0.10343762,0.00015715758],"about_ca_topic_score_codex":0.0022139465,"about_ca_topic_score_gemma":0.0096834125,"teacher_disagreement_score":0.0806364,"about_ca_system_score_codex":0.0000029125383,"about_ca_system_score_gemma":0.000046194968,"threshold_uncertainty_score":0.9988228},"labels":[],"label_agreement":null},{"id":"W2050020422","doi":"10.1016/j.geomorph.2008.04.010","title":"The role of tectonic damage and brittle rock fracture in the development of large rock slope failures","year":2008,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":375,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Burnaby Hospital; Simon Fraser University","funders":"","keywords":"Rockslide; Geology; Rock mass classification; Classification of discontinuities; Tectonics; Landslide; Brittleness; Geotechnical engineering; Geological Strength Index; Fracture (geology); Shear (geology); Seismology; Petrology","score_opus":0.0046335801465542895,"score_gpt":0.2031640030088368,"score_spread":0.1985304228622825,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050020422","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":[0.9969526,0.00061366934,0.000078345154,0.00051096926,0.000028297125,0.00012246786,0.0000056937834,0.000003926986,0.0016840267],"genre_scores_gemma":[0.9993172,0.00014431182,0.00015628515,0.00017187124,0.0000064869687,0.000006791086,0.0000061146934,0.0000047440467,0.0001861919],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99926,0.000062791994,0.0002008681,0.00013060565,0.00013648295,0.00020922194],"domain_scores_gemma":[0.99963915,0.0000810024,0.00008030219,0.00017231153,0.0000056957047,0.00002152263],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027191543,0.000075228076,0.00012543073,0.000015998674,0.00018217368,0.0000037387856,0.0002364505,0.00009735736,0.00060464704],"category_scores_gemma":[0.000018718321,0.00003811505,0.000022631304,0.00011393724,0.000102500504,0.000029349974,0.00015693392,0.00016934458,0.00003879307],"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":[0.000313305,0.00074165355,0.84770375,0.000036629033,0.00015319556,0.00020183265,0.041280266,0.008309982,0.06467528,0.00055365165,0.020791415,0.015239018],"study_design_scores_gemma":[0.00056925236,0.00007364248,0.6379333,0.000007714055,0.000008782499,0.00014689671,0.0009963388,0.00029216617,0.009356883,0.00031297977,0.3502043,0.000097707605],"about_ca_topic_score_codex":0.00024126185,"about_ca_topic_score_gemma":0.0010458655,"teacher_disagreement_score":0.32941288,"about_ca_system_score_codex":0.000016232496,"about_ca_system_score_gemma":0.000019805013,"threshold_uncertainty_score":0.66204613},"labels":[],"label_agreement":null},{"id":"W2051680293","doi":"10.1016/s0169-555x(01)00084-8","title":"Rates of floodplain accretion in a tropical island river system impacted by cyclones and large floods","year":2002,"lang":"en","type":"article","venue":"Geomorphology","topic":"Flood Risk Assessment and Management","field":"Environmental Science","cited_by":73,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"","keywords":"Overbank; Floodplain; Fluvial; Geology; Accretion (finance); Hydrology (agriculture); Erosion; Sedimentation; Drainage basin; Tropical cyclone; Structural basin; Discharge; Oceanography; Sediment; Geomorphology; Geography","score_opus":0.006490072561236268,"score_gpt":0.22038257987538748,"score_spread":0.21389250731415121,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2051680293","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":[0.9971127,0.00018638565,0.000693534,0.00022079216,0.00007415975,0.0002034439,0.00004005237,0.000018238474,0.0014507127],"genre_scores_gemma":[0.9990859,0.00013614463,0.00027066923,0.00006047665,0.000011702482,0.000014902939,0.000029170571,0.000006954712,0.00038406652],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99909234,0.00010114478,0.00019889766,0.00022775283,0.00011493707,0.00026493424],"domain_scores_gemma":[0.999718,0.000033811077,0.000067086854,0.00012959992,0.0000033206159,0.000048168367],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00012620188,0.00010699486,0.00020076276,0.00004805753,0.000041341977,0.000008160883,0.00009714849,0.00008562676,0.0019046534],"category_scores_gemma":[0.00001139434,0.000092022674,0.000022289363,0.00013615492,0.00014850505,0.00009907325,0.00014113354,0.00008178411,0.000091725786],"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":[0.000045771543,0.00027984154,0.9508469,0.000038535978,0.000025054358,0.000065145316,0.0005461314,0.00006352331,0.010667683,0.0003724856,0.035787884,0.0012610082],"study_design_scores_gemma":[0.003059099,0.00033955887,0.96739924,0.000024686951,0.00004111853,0.000047398244,0.00034065224,0.014010843,0.0011825839,0.00008992329,0.013226343,0.00023855457],"about_ca_topic_score_codex":0.000979361,"about_ca_topic_score_gemma":0.0009937289,"teacher_disagreement_score":0.022561539,"about_ca_system_score_codex":0.00005150036,"about_ca_system_score_gemma":0.0000013278456,"threshold_uncertainty_score":0.99900776},"labels":[],"label_agreement":null},{"id":"W2053347587","doi":"10.1016/j.geomorph.2004.09.033","title":"Reach scale variability of turbulent flow characteristics in a gravel-bed river","year":2005,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":64,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal","funders":"Fonds Québécois de la Recherche sur la Nature et les Technologies","keywords":"Turbulence; Geology; Flow (mathematics); Surface finish; Mean flow; Scale (ratio); Geomorphology; Spatial distribution; Flow conditions; Hydraulic roughness; Length scale; Spatial ecology; Flow velocity; Hydrology (agriculture); Geotechnical engineering; Mechanics; Materials science; Geography; Physics; Cartography","score_opus":0.00644496946459388,"score_gpt":0.206787725862659,"score_spread":0.20034275639806512,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2053347587","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":[0.99713975,0.000012907019,0.0005819801,0.00073328486,0.00006559123,0.00012704468,0.000023148541,0.000016552007,0.0012997237],"genre_scores_gemma":[0.99686956,0.00002209556,0.0023713573,0.000516097,0.00002429879,0.00001426509,0.00006010134,0.0000061130854,0.000116129464],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99888927,0.00008716005,0.00033199883,0.00030045176,0.00011511224,0.00027601692],"domain_scores_gemma":[0.99957484,0.00005468376,0.0000791092,0.00022779655,0.000008369295,0.000055216948],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00049631495,0.00011030092,0.00025429964,0.000033675366,0.000032932792,0.0000015882164,0.0001900408,0.00015784737,0.008221808],"category_scores_gemma":[0.00002808947,0.00010451369,0.000035707988,0.00013652898,0.0005209504,0.00007410566,0.000050638795,0.00016503286,0.00031362067],"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":[0.00013036345,0.00053336984,0.97980803,0.000017369139,0.000009357879,0.000055324304,0.0013814637,0.0008905029,0.010686372,0.000051110503,0.00040159633,0.00603515],"study_design_scores_gemma":[0.00073986663,0.00011359749,0.9786668,0.000006492539,0.000021417633,0.00005720159,0.000009816949,0.0018134635,0.005350477,0.0008640668,0.01219026,0.00016655959],"about_ca_topic_score_codex":0.00026453452,"about_ca_topic_score_gemma":0.00032145268,"teacher_disagreement_score":0.011788663,"about_ca_system_score_codex":0.000055378896,"about_ca_system_score_gemma":0.00001302667,"threshold_uncertainty_score":0.99268484},"labels":[],"label_agreement":null},{"id":"W2055355681","doi":"10.1016/j.geomorph.2009.10.007","title":"Evidence from the northwestern Venezuelan Andes for extraterrestrial impact: The black mat enigma","year":2009,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University; University of Toronto","funders":"Korea Institute of Geoscience and Mineral Resources","keywords":"Outwash plain; Geology; Younger Dryas; Paleontology; Geochemistry; Glacial period","score_opus":0.06244742529333298,"score_gpt":0.301509394620739,"score_spread":0.23906196932740603,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2055355681","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":[0.98897505,0.0021110275,0.0001496134,0.0073787253,0.00044705239,0.00043884534,0.00020174307,0.000023064755,0.00027488667],"genre_scores_gemma":[0.9976204,0.00021544559,0.000090699774,0.0012665156,0.00035767682,0.0000053926633,0.00033394515,0.0000024305193,0.0001075136],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983483,0.00041996993,0.00021618733,0.0003106519,0.00013141165,0.0005734581],"domain_scores_gemma":[0.9964825,0.0028952898,0.00008552169,0.00040669081,0.000044539764,0.00008543906],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0007086409,0.00015984161,0.00022951562,0.000029027944,0.00041495825,0.000058991493,0.000694064,0.00019722331,0.0028088803],"category_scores_gemma":[0.00015430266,0.000078885736,0.000112183065,0.0001141446,0.0006412023,0.00010466444,0.000018517363,0.00031297855,0.0008739905],"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":[0.0005176163,0.000009312442,0.993198,0.0000018169509,0.000028495251,0.000052355033,0.0004010966,0.0003906929,0.000044996446,0.000025140185,0.0026212586,0.0027092467],"study_design_scores_gemma":[0.00049320864,0.00051400013,0.9924044,0.000012296569,0.000030795713,0.00019277108,0.000117565454,0.0009682899,0.000047492118,0.0040879687,0.0010265819,0.00010464841],"about_ca_topic_score_codex":0.0027318685,"about_ca_topic_score_gemma":0.025509905,"teacher_disagreement_score":0.022778036,"about_ca_system_score_codex":0.0000015001694,"about_ca_system_score_gemma":0.00009605753,"threshold_uncertainty_score":0.9999039},"labels":[],"label_agreement":null},{"id":"W2056982253","doi":"10.1016/s0169-555x(01)00029-0","title":"Scales of boundary resistance in coarse-grained channels: turbulent velocity profiles and implications","year":2001,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":82,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Geology; Drag; Surface finish; Shear stress; Flume; Turbulence; Hydraulic roughness; Acoustic Doppler velocimetry; Boundary layer; Shear velocity; Flow (mathematics); Geotechnical engineering; Shear (geology); Length scale; Mechanics; Geometry; Materials science; Composite material; Mathematics","score_opus":0.012409042943555606,"score_gpt":0.2328123107870771,"score_spread":0.2204032678435215,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2056982253","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":[0.99343085,0.00050468364,0.00023113056,0.0038108707,0.00003399256,0.00016393507,0.000015639418,0.000018827446,0.0017900898],"genre_scores_gemma":[0.9982912,0.0002440689,0.0006983538,0.0004003497,0.000009636126,0.000042865737,0.000036114754,0.0000052720343,0.00027213118],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991981,0.000040836178,0.00020898152,0.00026090094,0.00006881004,0.00022236684],"domain_scores_gemma":[0.9996874,0.000048194674,0.00006352727,0.0001473959,0.000007892854,0.000045593464],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00019760733,0.00008930935,0.00016570157,0.000038915965,0.00008556103,0.000003612293,0.0001333763,0.000098593446,0.0009570041],"category_scores_gemma":[0.00001853222,0.00008559237,0.000017660417,0.00018732694,0.00076957326,0.000096699354,0.000039733623,0.000097992786,0.000029669023],"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":[0.00033009227,0.00045728407,0.9722169,0.00006302052,0.00002309336,0.0001662744,0.0016341957,0.00041956684,0.0154552935,0.0022101442,0.0034537588,0.0035703909],"study_design_scores_gemma":[0.00088701176,0.00012336727,0.9316092,0.00001854031,0.000015618069,0.0001232668,0.000072845076,0.00015173544,0.0022227236,0.016718986,0.047841012,0.00021566405],"about_ca_topic_score_codex":0.0001565506,"about_ca_topic_score_gemma":0.0017436774,"teacher_disagreement_score":0.044387255,"about_ca_system_score_codex":0.000023153481,"about_ca_system_score_gemma":0.000012108434,"threshold_uncertainty_score":0.99995625},"labels":[],"label_agreement":null},{"id":"W2057060516","doi":"10.1016/j.geomorph.2013.04.006","title":"Channel and landscape dynamics in the alluvial forest mosaic of the Carmanah River valley, British Columbia, Canada","year":2013,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":42,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Ministry of Environment","keywords":"Floodplain; Disturbance (geology); Landform; Ecological succession; Chronosequence; Channel (broadcasting); Forest dynamics; Overbank; Alluvium; Geology; Vegetation (pathology); Physical geography; Hydrology (agriculture); Geography; Ecology; Fluvial; Geomorphology","score_opus":0.003245524419441457,"score_gpt":0.1548091717470059,"score_spread":0.15156364732756444,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2057060516","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":[0.99746066,0.00006885937,0.000009364462,0.001032174,0.000101182195,0.00020982053,0.00003895302,0.0000034137117,0.0010755582],"genre_scores_gemma":[0.9981307,0.000035872614,0.000007120788,0.0013940108,0.00000995796,0.000026374653,0.00003011807,0.0000042737643,0.00036159166],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993251,0.000057171193,0.00013110111,0.00015734645,0.00011877763,0.00021048132],"domain_scores_gemma":[0.9997396,0.000047821795,0.000044566943,0.00013399478,0.0000055529204,0.000028490676],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000117689786,0.00005644622,0.000111288224,0.0000053489966,0.00010365467,0.0000116390465,0.00027857057,0.000069362104,0.001861629],"category_scores_gemma":[0.000009423624,0.00005059354,0.000016538304,0.000094339186,0.0004369791,0.000053092182,0.000070626375,0.00012933365,0.000010593596],"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":[0.0000027107553,0.000027854147,0.9860944,0.0000056696854,0.0000060557736,0.00003785822,0.00022788331,0.0005893088,0.000016035372,0.000007692589,0.01269065,0.00029384534],"study_design_scores_gemma":[0.0003047085,0.000032683252,0.99463224,0.0000033153115,0.000011281026,0.000076597586,0.00017137453,0.0018433605,0.000003934444,0.00067110005,0.002184224,0.00006515647],"about_ca_topic_score_codex":0.9615011,"about_ca_topic_score_gemma":0.99873906,"teacher_disagreement_score":0.03723791,"about_ca_system_score_codex":0.00003348082,"about_ca_system_score_gemma":0.00003030855,"threshold_uncertainty_score":0.9990508},"labels":[],"label_agreement":null},{"id":"W2057346711","doi":"10.1016/s0169-555x(02)00356-2","title":"Holocene lateral channel migration and incision of the Red River, Manitoba, Canada","year":2003,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":34,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Meander (mathematics); Radiocarbon dating; Alluvium; Holocene; Floodplain; Channel (broadcasting); Geomorphology; Transect; Alluvial fan; Hydrology (agriculture); Overbank; Paleontology; Facies; Sedimentary rock; Oceanography; Geography","score_opus":0.007583092139161252,"score_gpt":0.1757746226879828,"score_spread":0.16819153054882155,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2057346711","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":[0.9984239,0.0000571815,0.000035215242,0.00063082983,0.00016380286,0.000077131845,0.000008408747,0.000004180871,0.0005993676],"genre_scores_gemma":[0.99920344,0.000029948824,0.000046923113,0.00056729367,0.0000047822427,0.0000035291587,0.0000070697033,0.0000030158974,0.00013397014],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994699,0.00005309496,0.000112137976,0.00014202468,0.000089976245,0.00013291021],"domain_scores_gemma":[0.99978924,0.00001926212,0.000049674392,0.000108876324,0.0000052405403,0.000027702537],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000104905805,0.00006228519,0.00008623859,0.000008682192,0.000085781976,0.0000012717893,0.00009118399,0.000063848674,0.0005996856],"category_scores_gemma":[0.000016821388,0.000044868633,0.000011578075,0.000074914555,0.00023127046,0.00004118776,0.00002785776,0.00006703069,0.0000068948216],"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":[0.00003279544,0.000034006232,0.9886242,0.000006748254,0.000008272027,0.000030070281,0.00025792254,0.0006903375,0.0070467778,0.000075494965,0.0028577885,0.00033556297],"study_design_scores_gemma":[0.00044486465,0.000075452874,0.95930725,0.0000041431626,0.000016912394,0.00008961978,0.000030341638,0.0001089538,0.028175544,0.0012919997,0.010358189,0.00009675218],"about_ca_topic_score_codex":0.21002375,"about_ca_topic_score_gemma":0.52333003,"teacher_disagreement_score":0.31330627,"about_ca_system_score_codex":0.000026105812,"about_ca_system_score_gemma":0.000022585135,"threshold_uncertainty_score":0.79523677},"labels":[],"label_agreement":null},{"id":"W2057728569","doi":"10.1016/j.geomorph.2007.02.039","title":"Glacial erosion at the fjord onset zone and implications for the organization of ice flow on Baffin Island, Arctic Canada","year":2007,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Department of Energy; National Science Foundation","keywords":"Fjord; Glacial period; Geology; Ice sheet; Oceanography; Ice stream; Arctic; Glacier; Quaternary; Wisconsin glaciation; Erosion; Arctic ice pack; Greenland ice sheet; Glacial landform; Geomorphology; Paleontology; Sea ice; Cryosphere; Moraine","score_opus":0.013195879113348312,"score_gpt":0.23243197003335384,"score_spread":0.2192360909200055,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2057728569","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":[0.9878173,0.00023334518,0.0010757094,0.010021626,0.00022744166,0.0002684194,0.00021940871,0.0000045864394,0.00013218824],"genre_scores_gemma":[0.998141,0.000062642896,0.000054525834,0.0009942262,0.00003665431,0.0000027189883,0.00045700822,0.0000021180458,0.00024909913],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992775,0.000093332215,0.00014351598,0.000155865,0.00007088735,0.00025891283],"domain_scores_gemma":[0.9969028,0.002716591,0.000063425265,0.00018616537,0.00008953975,0.000041468626],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005365035,0.00006912751,0.00010838604,0.00003112374,0.00052752387,0.000004976575,0.0001665577,0.00009238674,0.0011112442],"category_scores_gemma":[0.00029707162,0.000040265284,0.000013995667,0.0001710702,0.00032701643,0.00001588266,0.000021130641,0.00012759324,0.000030786927],"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":[0.00011796817,0.0000064770284,0.9948112,0.0000062827,0.0000115320745,0.000003011941,0.0000656599,0.0004131071,0.00004882971,0.00011453354,0.0030034487,0.0013980012],"study_design_scores_gemma":[0.00027619684,0.00010495897,0.9960136,0.0000018866278,0.000017416794,0.00019362386,0.00006470761,0.0003192002,0.00016593863,0.0001436831,0.0026538675,0.00004492406],"about_ca_topic_score_codex":0.114580534,"about_ca_topic_score_gemma":0.9830825,"teacher_disagreement_score":0.8685019,"about_ca_system_score_codex":0.0000034465936,"about_ca_system_score_gemma":0.000112478774,"threshold_uncertainty_score":0.9998019},"labels":[],"label_agreement":null},{"id":"W2058709091","doi":"10.1016/j.geomorph.2011.03.007","title":"Habitat effects on depth and velocity frequency distributions: Implications for modeling hydraulic variation and fish habitat suitability in streams","year":2011,"lang":"en","type":"article","venue":"Geomorphology","topic":"Fish Ecology and Management Studies","field":"Environmental Science","cited_by":57,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Raincoast Conservation Foundation; University of Calgary; Ministry of Environment","funders":"","keywords":"STREAMS; Skewness; Hydraulics; Frequency distribution; Habitat; Hydrology (agriculture); Environmental science; Spatial variability; Geology; Ecology; Statistics; Mathematics; Physics; Geotechnical engineering; Computer science","score_opus":0.02159128111290694,"score_gpt":0.237096380228334,"score_spread":0.21550509911542706,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2058709091","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":[0.98478097,0.000018962586,0.010990072,0.0020582196,0.00006487104,0.0006296317,0.000058687445,0.000025068368,0.0013735325],"genre_scores_gemma":[0.99685055,0.00004164111,0.0020107836,0.00066946074,0.000007705396,0.00034456942,0.000061009774,0.000005098532,0.000009195303],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991239,0.00006803398,0.00016134586,0.00036601134,0.000033308388,0.00024742365],"domain_scores_gemma":[0.9994977,0.00024372348,0.000048107755,0.00015993122,0.000009606613,0.000040893672],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029097413,0.00010702445,0.00015148227,0.000032595693,0.00023168956,0.000006163939,0.00007724745,0.00009066111,0.000045322708],"category_scores_gemma":[0.00025560026,0.000106148516,0.000017948416,0.000089828536,0.00020968112,0.000119790486,0.00013727702,0.000083372004,0.000011689341],"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":[0.000024028126,0.00011557481,0.9936894,0.000019968997,0.000012652885,0.0000017815864,0.00032633665,0.00005845533,0.000100427205,0.0026639272,0.0009009437,0.0020864957],"study_design_scores_gemma":[0.00045574876,0.00018979539,0.9338512,0.0000037870475,0.000021734475,0.0000036699612,0.000027744285,0.0011945848,0.000032035336,0.06409751,0.000028489847,0.00009370282],"about_ca_topic_score_codex":0.00076790917,"about_ca_topic_score_gemma":0.025953894,"teacher_disagreement_score":0.06143358,"about_ca_system_score_codex":0.000092217844,"about_ca_system_score_gemma":0.0000042458655,"threshold_uncertainty_score":0.9918199},"labels":[],"label_agreement":null},{"id":"W2059038779","doi":"10.1016/j.geomorph.2003.08.002","title":"Sediment supply from shoreface to dunes: linking sediment transport measurements and long-term morphological evolution","year":2003,"lang":"en","type":"article","venue":"Geomorphology","topic":"Coastal and Marine Dynamics","field":"Earth and Planetary Sciences","cited_by":260,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto; University of Guelph","funders":"Core Research for Evolutional Science and Technology","keywords":"Sediment transport; Geology; Beach morphodynamics; Subaerial; Sedimentary budget; Sediment; Accretion (finance); Intertidal zone; Aeolian processes; Oceanography; Shore; Erosion; Geomorphology; Paleontology","score_opus":0.020988154672603787,"score_gpt":0.21828292626527546,"score_spread":0.19729477159267167,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2059038779","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":[0.9939025,0.00035167206,0.0032517293,0.00033085397,0.00063289097,0.00033322943,0.00023471088,0.00004643357,0.00091597164],"genre_scores_gemma":[0.99673355,0.00003684832,0.0013160896,0.00065896485,0.000061247876,0.0000056796034,0.00096764846,0.0000054635557,0.00021452396],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983554,0.00010392508,0.00027983196,0.0005145113,0.00028144137,0.00046488768],"domain_scores_gemma":[0.9993982,0.000054313034,0.00005690989,0.00020080464,0.000042222335,0.0002475872],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00033854943,0.00021480212,0.00026549606,0.000077330355,0.00013742902,0.000021319724,0.00015316998,0.00013989292,0.0036705504],"category_scores_gemma":[0.000020222207,0.0001832602,0.000051063493,0.00013773252,0.0000994666,0.00008071801,0.000030329535,0.00017045105,0.00018783816],"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":[0.00008597406,0.000048430928,0.99201715,0.000007753217,0.00002896492,0.00020658976,0.0001263369,0.00092284597,0.0011426585,0.000037251928,0.00008016882,0.005295884],"study_design_scores_gemma":[0.0006055627,0.0003402145,0.9960585,0.000016541058,0.000041838317,0.00016432586,0.000051515224,0.0002281875,0.00020814688,0.00052782684,0.0015206974,0.00023659949],"about_ca_topic_score_codex":0.00335339,"about_ca_topic_score_gemma":0.010632445,"teacher_disagreement_score":0.007279055,"about_ca_system_score_codex":0.000017164612,"about_ca_system_score_gemma":0.00004474338,"threshold_uncertainty_score":0.99724025},"labels":[],"label_agreement":null},{"id":"W2060531268","doi":"10.1016/s0169-555x(02)00339-2","title":"A hydroclimatic threshold for landslide initiation on the North Shore Mountains of Vancouver, British Columbia","year":2002,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":199,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Kerr Wood Leidal Associates (Canada)","funders":"U.S. Army Corps of Engineers","keywords":"Landslide; Storm; Geology; Shore; Streamflow; Hydrology (agriculture); Drainage basin; Geomorphology; Geotechnical engineering; Geography; Cartography; Oceanography","score_opus":0.014919551376021307,"score_gpt":0.19656056097239075,"score_spread":0.18164100959636945,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060531268","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":[0.99207675,0.000035528526,0.00013473551,0.000275408,0.00023182957,0.00037306477,0.00010888983,0.00001960876,0.006744176],"genre_scores_gemma":[0.99696356,0.00008507284,0.000113370974,0.0008766508,0.00003242818,0.000055285585,0.000040764357,0.000013065455,0.0018198169],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99914545,0.000029522173,0.00021820386,0.00020046748,0.00015376435,0.00025257588],"domain_scores_gemma":[0.9994741,0.00015593924,0.000108843014,0.00020910893,0.000011212314,0.000040797513],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014804774,0.00007529113,0.00016385119,0.000011723515,0.0001578816,0.0000285455,0.00018675865,0.00010110626,0.008102538],"category_scores_gemma":[0.000057149846,0.000069527145,0.00006953137,0.00012952284,0.00016212252,0.00005150833,0.0000633471,0.00012536567,0.00012001489],"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":[0.00004175801,0.00032280857,0.46659896,0.000028994327,0.000055413293,0.00006922246,0.0007537008,0.0042093983,0.0003163695,0.00007387873,0.52321506,0.0043144277],"study_design_scores_gemma":[0.0101414565,0.004480464,0.597321,0.0002561426,0.0004808385,0.0005870782,0.0012932417,0.10314842,0.00058493076,0.013658539,0.2662645,0.0017834184],"about_ca_topic_score_codex":0.002569072,"about_ca_topic_score_gemma":0.123737946,"teacher_disagreement_score":0.25695056,"about_ca_system_score_codex":0.000055466564,"about_ca_system_score_gemma":0.0000037455138,"threshold_uncertainty_score":0.99280417},"labels":[],"label_agreement":null},{"id":"W2060970844","doi":"10.1016/j.geomorph.2013.10.031","title":"Geomorphology, internal structure, and successive development of a glacier foreland in the semiarid Chilean Andes (Cerro Tapado, upper Elqui Valley, 30°08′ S., 69°55′ W.)","year":2013,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geophysical Methods and Applications","field":"Engineering","cited_by":58,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Trois-Rivières","funders":"","keywords":"Geology; Glacier; Rock glacier; Landform; Geomorphology; Ground-penetrating radar; Debris; Moraine; Radar","score_opus":0.007553833189729103,"score_gpt":0.22747427818418686,"score_spread":0.21992044499445776,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060970844","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":[0.9917368,0.00019734784,0.0062986165,0.00023240954,0.00012701165,0.00041437923,0.000042665157,0.000031626372,0.00091911945],"genre_scores_gemma":[0.99153656,0.00002516782,0.007896059,0.0002214994,0.00006102283,0.00013189993,0.000055168224,0.000022729106,0.00004992345],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.998764,0.00009411802,0.00038356637,0.00026959617,0.00011196674,0.00037677234],"domain_scores_gemma":[0.99929434,0.0002277776,0.0000855621,0.0002662211,0.000052670166,0.000073444084],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021118426,0.00021727005,0.00033970925,0.000095564974,0.00008081287,0.000026771299,0.0003166987,0.000165084,0.0021542143],"category_scores_gemma":[0.00003957583,0.00015619725,0.000044789627,0.0001608459,0.00025211665,0.00008755896,0.0001144339,0.0003701132,0.000106821564],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021541376,0.00096848287,0.22696471,0.00079679396,0.0011035906,0.00022667799,0.023312153,0.0034798738,0.46963358,0.01913044,0.029436216,0.22473207],"study_design_scores_gemma":[0.0026956617,0.00018683172,0.9431105,0.00008208314,0.00007577671,0.00042885513,0.00091416255,0.0036999588,0.01597926,0.01948653,0.012544305,0.00079604797],"about_ca_topic_score_codex":0.00028255692,"about_ca_topic_score_gemma":0.00008675084,"teacher_disagreement_score":0.7161458,"about_ca_system_score_codex":0.000024982943,"about_ca_system_score_gemma":0.000021544261,"threshold_uncertainty_score":0.99875796},"labels":[],"label_agreement":null},{"id":"W2061159032","doi":"10.1016/j.geomorph.2010.04.010","title":"Channel patterns: Braided, anabranching, and single-thread","year":2010,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":239,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Thread (computing); Dimensionless quantity; Geology; Geometry; Channel (broadcasting); Mathematics; Computer science; Mechanics; Physics; Telecommunications","score_opus":0.007945694550993756,"score_gpt":0.20345721822777846,"score_spread":0.1955115236767847,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061159032","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":[0.99475586,0.00004437552,0.0008215405,0.0009858806,0.00033519167,0.00008739181,0.000012234449,0.00005165742,0.0029058342],"genre_scores_gemma":[0.99754024,0.000023034978,0.00018763175,0.0018957452,0.000055613455,0.000011473955,0.00002788669,0.000010798867,0.00024755448],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99911517,0.000022349583,0.00013817231,0.0003347409,0.00008285545,0.00030668985],"domain_scores_gemma":[0.99963826,0.000038747377,0.0000455637,0.0001782962,0.000003709569,0.00009539616],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00016154426,0.00012415278,0.00014380612,0.000028572225,0.000121071724,0.000009756101,0.00015948998,0.0001653848,0.0097070215],"category_scores_gemma":[0.00001973422,0.00011395799,0.00002224729,0.00006537504,0.0003970069,0.00013519767,0.000071530696,0.0002681794,0.00038882592],"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":[0.00006644724,0.0002738798,0.8526356,0.000024824792,0.000025789464,0.0003192289,0.0011878622,0.00012258929,0.1302202,0.00031012113,0.0018345461,0.012978911],"study_design_scores_gemma":[0.0027528002,0.0008620475,0.8091101,0.000017815453,0.000084262974,0.0017686067,0.0001413104,0.0003512217,0.033890553,0.014281911,0.13571179,0.0010275616],"about_ca_topic_score_codex":0.0003280281,"about_ca_topic_score_gemma":0.002125891,"teacher_disagreement_score":0.13387723,"about_ca_system_score_codex":0.0000060299585,"about_ca_system_score_gemma":0.0000038025432,"threshold_uncertainty_score":0.99119824},"labels":[],"label_agreement":null},{"id":"W2062807353","doi":"10.1016/j.geomorph.2011.08.002","title":"Medium timescale beach rotation; gale climate and offshore island influences","year":2011,"lang":"en","type":"article","venue":"Geomorphology","topic":"Coastal and Marine Dynamics","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Universidade Nova de Lisboa; Universidade de Lisboa; Federation for the Humanities and Social Sciences","keywords":"Submarine pipeline; Geology; Headland; Beach ridge; Oceanography; Intertidal zone; Shore; Accretion (finance); Climate change; Wave height; Climatology; Geomorphology","score_opus":0.012943411634811584,"score_gpt":0.19906160196498243,"score_spread":0.18611819033017085,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2062807353","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":[0.9723566,0.00018104374,0.000052468327,0.00015513427,0.00022954153,0.00008763346,0.00018867898,0.000029772025,0.026719104],"genre_scores_gemma":[0.99785197,0.0001156593,0.0006317072,0.0002762729,0.000043641277,0.0000014858109,0.00042232094,0.0000022890306,0.00065466616],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992902,0.000031726628,0.00013905969,0.00019769622,0.00007769238,0.00026362078],"domain_scores_gemma":[0.99968964,0.000047598453,0.00004731546,0.00010360811,0.000024242676,0.00008759798],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014278712,0.00009343854,0.0001304627,0.000049478724,0.00009816653,0.000014434679,0.00010954013,0.00006371943,0.0064081065],"category_scores_gemma":[0.000016867536,0.00007499877,0.000019488329,0.00007897768,0.0001978059,0.0001099315,0.00003745149,0.00009102594,0.0001663357],"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":[0.000045646488,0.000011328337,0.9805679,0.000009192152,0.000007853846,0.000043766424,0.00044797242,0.000018961966,0.00003042401,0.00008149553,0.00091237604,0.017823083],"study_design_scores_gemma":[0.00023283318,0.00018657013,0.9906523,0.0000033154854,0.000014059101,0.00018818026,0.00018206977,0.0015731332,0.000036463443,0.0017819313,0.005028495,0.00012063782],"about_ca_topic_score_codex":0.003207178,"about_ca_topic_score_gemma":0.022800526,"teacher_disagreement_score":0.026064439,"about_ca_system_score_codex":9.422597e-7,"about_ca_system_score_gemma":0.000018893625,"threshold_uncertainty_score":0.9950308},"labels":[],"label_agreement":null},{"id":"W2063826091","doi":"10.1016/j.geomorph.2013.12.029","title":"The impact of watershed management on coastal morphology: A case study using an integrated approach and numerical modeling","year":2014,"lang":"en","type":"article","venue":"Geomorphology","topic":"Coastal wetland ecosystem dynamics","field":"Environmental Science","cited_by":37,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canada Excellence Research Chairs, Government of Canada; National Research Foundation","keywords":"Watershed; Erosion; Hydrology (agriculture); Land cover; Sediment transport; Geology; Watershed management; Shore; Sedimentary budget; Sediment; Land use; Geomorphology; Ecology; Oceanography","score_opus":0.022176056877497317,"score_gpt":0.26191671517681736,"score_spread":0.23974065829932004,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2063826091","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":[0.9515698,0.0000020166892,0.047602434,0.000011147393,0.000049893366,0.0004132275,0.000017589127,0.000020696605,0.00031321787],"genre_scores_gemma":[0.9988662,0.0000011676555,0.0010241999,0.00001732771,0.000010747799,0.000016454687,0.000025221103,0.00001770482,0.000020968491],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.998489,0.00033159493,0.00028335644,0.0004011232,0.00013584051,0.00035906368],"domain_scores_gemma":[0.9993408,0.000050297705,0.00009232978,0.00040141796,0.000010403716,0.000104793246],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006496971,0.00018571298,0.00026910187,0.000049095233,0.00021881249,0.000025720683,0.00019466005,0.0000682727,0.00007257787],"category_scores_gemma":[0.0000138539035,0.00011457132,0.00004931389,0.00015065473,0.00017576199,0.00006582528,0.00037599166,0.00015365407,0.000014204028],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042791883,0.0012736868,0.12636384,0.000013063634,0.00014628317,0.0013240929,0.0017389833,0.8570599,0.0017560817,0.000048888756,0.000053627093,0.009793652],"study_design_scores_gemma":[0.00074144965,0.0010843523,0.0043678023,0.0000024006945,0.000034129072,0.0037607271,0.003947546,0.9858476,0.0000062691015,0.000064682565,0.000009083542,0.00013397081],"about_ca_topic_score_codex":0.02128595,"about_ca_topic_score_gemma":0.0011744485,"teacher_disagreement_score":0.1287877,"about_ca_system_score_codex":0.00009577054,"about_ca_system_score_gemma":0.0000045130364,"threshold_uncertainty_score":0.9852314},"labels":[],"label_agreement":null},{"id":"W2065122045","doi":"10.1016/j.geomorph.2013.11.031","title":"Impact crater morphology: The origin of the Mertz and Ninnis Glaciers, Antarctica","year":2013,"lang":"en","type":"article","venue":"Geomorphology","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"University of Colorado; Arctic Institute of North America; National Science Foundation","keywords":"Geology; Glacier; Impact crater; Structural basin; Ice sheet; Glacier morphology; Geomorphology; Antarctic ice sheet; Glaciology; Paleontology; Rock glacier; Earth science; Cryosphere; Ice stream; Oceanography; Stratigraphy; Sea ice; Tectonics; Astrobiology","score_opus":0.017019229681646895,"score_gpt":0.22973335734864023,"score_spread":0.21271412766699332,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2065122045","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":[0.9915788,0.0006680654,0.000017172619,0.006625125,0.00033017047,0.00020204441,0.000066178756,0.000008384518,0.0005040215],"genre_scores_gemma":[0.997787,0.00014289402,0.00020307838,0.0014770038,0.000037837744,0.0000039698216,0.000016464595,0.0000023015384,0.00032946627],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992552,0.00008300292,0.00015769358,0.0001566344,0.000087803084,0.0002596934],"domain_scores_gemma":[0.99935687,0.00021470535,0.000078851845,0.00025430703,0.000051479736,0.000043787077],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00013929495,0.00010027064,0.00015861233,0.000010947209,0.00027189965,0.000018932044,0.00021963124,0.000054747627,0.010764063],"category_scores_gemma":[0.000051036495,0.000044688,0.00005642594,0.00018911644,0.00062375737,0.00006191446,0.000044730026,0.00012392494,0.00012958844],"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":[0.00000867171,0.000006700163,0.9739971,0.0000023102955,0.00003718524,0.0000025643362,0.000208385,0.00008748986,0.00022912402,0.000049209244,0.023374798,0.0019964443],"study_design_scores_gemma":[0.00015279946,0.000094615265,0.9855232,0.0000018486171,0.000020512558,0.00008405116,0.0002445336,0.00036918052,0.000028253717,0.0005498714,0.012871314,0.000059821075],"about_ca_topic_score_codex":0.02414093,"about_ca_topic_score_gemma":0.0016504297,"teacher_disagreement_score":0.0224905,"about_ca_system_score_codex":0.000002985361,"about_ca_system_score_gemma":0.000028725797,"threshold_uncertainty_score":0.99014026},"labels":[],"label_agreement":null},{"id":"W2065653726","doi":"10.1016/j.geomorph.2007.04.011","title":"Quantifying fluvial non linearity and finding self organized criticality? Insights from simulations of river basin evolution","year":2007,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":96,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Drainage basin; Storm; Sediment; Geology; Sediment transport; Hydrology (agriculture); Fluvial; Landslide; Magnitude (astronomy); Environmental science; Structural basin; Geomorphology; Oceanography; Geotechnical engineering; Geography","score_opus":0.01726139153228588,"score_gpt":0.2607630405251123,"score_spread":0.24350164899282642,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2065653726","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":[0.9813921,0.000044073124,0.01795649,0.000121513796,0.00013195655,0.00009424836,0.000020880912,0.000029440513,0.00020932259],"genre_scores_gemma":[0.9967374,0.000005705239,0.0029498364,0.0002018052,0.00002952723,8.5772587e-7,0.00006004181,0.0000062051568,0.000008596758],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99912757,0.000052528467,0.00024686227,0.00025753374,0.00011034346,0.00020516315],"domain_scores_gemma":[0.99947524,0.00027434627,0.00005426792,0.00011523035,0.000015681131,0.00006524386],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001869899,0.00009232359,0.00017944447,0.000043981974,0.00017446943,0.0000037749805,0.00008486109,0.0001793168,0.0016711856],"category_scores_gemma":[0.00007224289,0.00009115511,0.000021386237,0.00016220145,0.00043628778,0.00014225341,0.000054700482,0.00014391563,0.00007006998],"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":[0.00009511672,0.00018287958,0.8528988,0.000011822372,0.000022023067,0.000042312775,0.0015313087,0.0005093708,0.14407474,0.0004375135,0.000043282325,0.00015085563],"study_design_scores_gemma":[0.0008820396,0.000093204864,0.9578175,0.000008319319,0.000069411886,0.00001140848,0.000081869846,0.004143808,0.03310668,0.0029291231,0.0006993898,0.00015725309],"about_ca_topic_score_codex":0.001516811,"about_ca_topic_score_gemma":0.0013236101,"teacher_disagreement_score":0.110968046,"about_ca_system_score_codex":0.000037756654,"about_ca_system_score_gemma":0.000011320504,"threshold_uncertainty_score":0.9992414},"labels":[],"label_agreement":null},{"id":"W2071950136","doi":"10.1016/j.geomorph.2011.09.014","title":"Erosion and channel change as factors of landslides and valley formation in Champlain Sea Clays: The Chacoura River, Quebec, Canada","year":2011,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":40,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Ministère des Transports; Université Laval","funders":"","keywords":"Landslide; Geology; Erosion; Channel (broadcasting); Landslide classification; Geomorphology; Debris; Ravine; Debris flow; Bank erosion; Hydrology (agriculture); Landslide mitigation; Geotechnical engineering; Geography; Archaeology; Oceanography","score_opus":0.021845172683707875,"score_gpt":0.19624462313371355,"score_spread":0.17439945045000568,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2071950136","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":[0.99865776,0.00021602717,0.000016964566,0.00039504838,0.00011423094,0.00018349754,0.000020750125,0.0000055554483,0.00039017963],"genre_scores_gemma":[0.99909955,0.0005025156,0.000014524346,0.00023725994,0.0000107744045,0.000010489638,0.00002258971,0.000005514051,0.000096793825],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993535,0.000052648393,0.00014577151,0.0001459515,0.00010308052,0.00019900272],"domain_scores_gemma":[0.99971545,0.000038361566,0.00008310544,0.00010381748,0.0000055799296,0.000053669948],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014974918,0.00009687906,0.00013841657,0.000029130304,0.00008320237,0.0000042499614,0.00008928904,0.0001023786,0.00038367845],"category_scores_gemma":[0.0000124850185,0.000058706446,0.0000126713685,0.000077107725,0.0001922746,0.00011645483,0.00012416164,0.000113400696,0.0000056332947],"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":[0.00021129257,0.00011075187,0.93652326,0.00005784429,0.00003531007,0.0001527091,0.04753868,0.000060028215,0.003764059,0.00022852332,0.004853668,0.0064638876],"study_design_scores_gemma":[0.00055682636,0.000107826636,0.99376285,0.000019390707,0.000011817897,0.00009478881,0.0012515603,0.00053718174,0.001448617,0.00042267548,0.001659508,0.00012697642],"about_ca_topic_score_codex":0.9133849,"about_ca_topic_score_gemma":0.9245885,"teacher_disagreement_score":0.057239585,"about_ca_system_score_codex":0.000055173365,"about_ca_system_score_gemma":0.000011382555,"threshold_uncertainty_score":0.420101},"labels":[],"label_agreement":null},{"id":"W2073955740","doi":"10.1016/j.geomorph.2014.11.006","title":"Architectural–landsystem analysis of a modern glacial landscape, Sólheimajökull, southern Iceland","year":2014,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"Natural Sciences and Engineering Research Council of Canada; Háskóli Íslands; McMaster University","keywords":"Geology; Colluvium; Glacial period; Glacier; Sedimentary rock; Geomorphology; Architecture; Glacial landform; Quaternary; Moraine; Landform; Paleontology; Archaeology; Geography; Alluvium","score_opus":0.011149718684366108,"score_gpt":0.2181722586682072,"score_spread":0.20702253998384107,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2073955740","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":[0.989844,0.00043266508,0.0009067291,0.00024305048,0.00017264651,0.00010516973,0.00019512993,0.00003198627,0.008068585],"genre_scores_gemma":[0.99870163,0.000007229345,0.00012632823,0.00015096726,0.000067331464,0.0000021409683,0.0006360769,0.0000032955004,0.00030496903],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981797,0.00047411156,0.00031685032,0.00035354713,0.00018178113,0.0004940275],"domain_scores_gemma":[0.9988178,0.0005236728,0.0001423385,0.00033142042,0.000064935244,0.000119806005],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00066106545,0.0001581167,0.00060339336,0.00045095515,0.00012904644,0.000011075515,0.00033236493,0.00024039962,0.005724227],"category_scores_gemma":[0.00008809093,0.000121133635,0.00013477921,0.00055220665,0.00032352604,0.000030121768,0.000025148325,0.0002570695,0.0004730556],"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":[0.00017701916,0.000013196066,0.9931953,0.000017591252,0.0003821118,0.000039466202,0.000426833,0.0035106312,0.000036433186,0.00003992874,0.00007677473,0.0020847463],"study_design_scores_gemma":[0.0006332358,0.0002386544,0.9393884,0.0000038502767,0.00034413283,0.00021167897,0.000075448675,0.05754178,0.000018166049,0.00092634826,0.00046192275,0.0001563684],"about_ca_topic_score_codex":0.00086922396,"about_ca_topic_score_gemma":0.03162033,"teacher_disagreement_score":0.054031152,"about_ca_system_score_codex":5.0341185e-7,"about_ca_system_score_gemma":0.00003094485,"threshold_uncertainty_score":0.99518466},"labels":[],"label_agreement":null},{"id":"W2074646453","doi":"10.1016/j.geomorph.2007.12.017","title":"Spatial and temporal patterns of aeolian sediment transport on an inland parabolic dune, Bigstick Sand Hills, Saskatchewan, Canada","year":2008,"lang":"en","type":"article","venue":"Geomorphology","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; University of Calgary; University of Victoria; University of Lethbridge","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; Killam Trusts","keywords":"Geology; Aeolian processes; Sediment; Erosion; Sediment transport; Sedimentary budget; Deposition (geology); Hydrology (agriculture); Geomorphology; Precipitation; Geotechnical engineering","score_opus":0.008705249479273114,"score_gpt":0.1885172189717205,"score_spread":0.17981196949244738,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074646453","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":[0.99805164,0.00021105605,0.000106737505,0.00020144465,0.0002861451,0.00014474653,0.0007907632,0.000012710939,0.00019474761],"genre_scores_gemma":[0.9981988,0.00006212054,0.000078079844,0.00068819005,0.000112149595,0.0000014891782,0.00072395813,0.000005515165,0.00012967018],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99884003,0.000060368024,0.00023922528,0.0003067523,0.00020383949,0.00034978354],"domain_scores_gemma":[0.99941164,0.00006229203,0.000098256925,0.00017082998,0.000028756685,0.0002282218],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010489992,0.00017476494,0.00031117396,0.000052958905,0.000118961114,0.0000041598064,0.00012617001,0.00009708924,0.0008515311],"category_scores_gemma":[0.0000067089704,0.00014431993,0.000024679242,0.000078020326,0.00014152456,0.000061659186,0.000006306351,0.00012992145,0.000009858576],"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":[0.00012598086,0.000027578644,0.99359107,0.000041143536,0.0000148126965,0.00046348004,0.0004574313,0.00057615724,0.000016774537,0.0000019618258,0.0007489976,0.0039346395],"study_design_scores_gemma":[0.0007125858,0.0006686942,0.9931024,0.00001576679,0.000017190298,0.00030303307,0.00019460249,0.00096660294,0.00040969992,0.00003197731,0.0033966857,0.00018076769],"about_ca_topic_score_codex":0.9237016,"about_ca_topic_score_gemma":0.94937766,"teacher_disagreement_score":0.025676066,"about_ca_system_score_codex":0.0000052004825,"about_ca_system_score_gemma":0.0003347497,"threshold_uncertainty_score":0.93236685},"labels":[],"label_agreement":null},{"id":"W2075340558","doi":"10.1016/s0169-555x(02)00166-6","title":"Complex mass wasting response of drainage basins to forest management in coastal British Columbia","year":2002,"lang":"en","type":"article","venue":"Geomorphology","topic":"Soil erosion and sediment transport","field":"Agricultural and Biological Sciences","cited_by":43,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Mass wasting; Logging; Geology; Hydrology (agriculture); Disturbance (geology); Structural basin; Bedrock; Wasting; Clearcutting; Sediment; Environmental science; Physical geography; Geomorphology; Geography; Forestry","score_opus":0.03274080744045201,"score_gpt":0.21278631965666928,"score_spread":0.18004551221621726,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2075340558","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":[0.9961363,0.000014909232,0.000014085576,0.0008785789,0.00008674074,0.0002578179,0.00018308584,0.000032081065,0.0023964194],"genre_scores_gemma":[0.996636,0.0000137954,0.00035127744,0.00082088425,0.00002263236,0.000020050511,0.000081679675,0.0000012401737,0.0020524596],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99888736,0.00010367037,0.00027438367,0.00026588835,0.00014910483,0.00031959466],"domain_scores_gemma":[0.9996502,0.00012363578,0.000051197643,0.000058337962,0.000028547602,0.00008812127],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003071425,0.00007651481,0.00020089379,0.000018725344,0.00008656002,0.00003547761,0.00019925942,0.00006879214,0.005507454],"category_scores_gemma":[0.000028471664,0.000056529672,0.000052511878,0.0003354125,0.00008274413,0.00003213866,0.000058478396,0.000073816125,0.000054915425],"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":[0.00026068866,0.00048388515,0.6969376,0.000024512548,0.000018723167,0.0012998247,0.0002077395,0.000114420814,0.2343904,0.0000792226,0.024275899,0.041907042],"study_design_scores_gemma":[0.00044334936,0.0002926767,0.9804913,0.000028120217,0.00000517313,0.000035551675,0.00031535156,0.0001588619,0.00006703885,0.000068663365,0.0179745,0.00011942789],"about_ca_topic_score_codex":0.006009995,"about_ca_topic_score_gemma":0.18917693,"teacher_disagreement_score":0.28355363,"about_ca_system_score_codex":0.00001554772,"about_ca_system_score_gemma":0.0000014834084,"threshold_uncertainty_score":0.9954016},"labels":[],"label_agreement":null},{"id":"W2076405290","doi":"10.1016/j.geomorph.2008.02.014","title":"Contemporary research in aeolian geomorphology","year":2008,"lang":"en","type":"article","venue":"Geomorphology","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Okanagan University College; University of British Columbia, Okanagan Campus; University of British Columbia","funders":"Indian Council of Agricultural Research; University of Guelph","keywords":"Aeolian processes; Geology; Sedimentology; Earth science; Arid; Physical geography; Geomorphology; Geography; Paleontology","score_opus":0.17607941798888604,"score_gpt":0.3160087482978547,"score_spread":0.13992933030896865,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076405290","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":[0.9545,0.0020337652,0.000042848867,0.0015262105,0.00046142165,0.00025979278,0.00006912478,0.000045591205,0.041061196],"genre_scores_gemma":[0.9972937,0.00018879169,0.00017714301,0.0009789361,0.00015732752,0.0000065829286,0.00028755117,0.000007399505,0.00090254087],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9975998,0.00043334186,0.00031463918,0.0004976986,0.0002707511,0.00088379736],"domain_scores_gemma":[0.998913,0.00042877812,0.00006202731,0.0003188804,0.00008162703,0.00019569782],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0010052779,0.00016674414,0.0003423999,0.0003739624,0.00026792724,0.000011927757,0.00041095886,0.00024571837,0.006908134],"category_scores_gemma":[0.000095766954,0.00015024275,0.00004771535,0.00071383076,0.0009074341,0.00016083925,0.000045855904,0.000600462,0.0039826552],"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":[0.00018537742,0.000048706857,0.924719,0.000026654607,0.000009024571,0.0077148397,0.00037639934,0.00059702515,0.000076530654,0.00010675131,0.062881686,0.003258018],"study_design_scores_gemma":[0.001404029,0.00072989654,0.9052808,0.00002343504,0.0000025445718,0.0040811677,0.00027520116,0.0025305864,0.0002335681,0.0027449143,0.082362495,0.00033134222],"about_ca_topic_score_codex":0.018432,"about_ca_topic_score_gemma":0.0039312267,"teacher_disagreement_score":0.04279368,"about_ca_system_score_codex":0.00001022385,"about_ca_system_score_gemma":0.00025863774,"threshold_uncertainty_score":0.99679285},"labels":[],"label_agreement":null},{"id":"W2077536029","doi":"10.1016/j.geomorph.2014.12.021","title":"The paraglacial geomorphology of the Fraser Lowland, southwest British Columbia and northwest Washington","year":2014,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":16,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Landform; Glacial landform; Fluvial; Glacial period; Pleistocene; Geomorphology; Context (archaeology); Quaternary; Aeolian processes; Glacier; Holocene; Physical geography; Paleontology; Moraine; Geography","score_opus":0.0029493067420726274,"score_gpt":0.17133258141940041,"score_spread":0.16838327467732778,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2077536029","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":[0.99664116,0.00008632199,0.000033851637,0.0005574047,0.00070757343,0.00018918351,0.00011146983,0.000015612337,0.0016574248],"genre_scores_gemma":[0.9974742,0.00011309701,0.000034890683,0.0005629847,0.00007668146,0.00001312957,0.000034765184,0.000015998123,0.0016742599],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985818,0.00019333935,0.00029242755,0.00032597315,0.000189946,0.0004164677],"domain_scores_gemma":[0.99913734,0.00019286839,0.00017173935,0.0003967709,0.000015868904,0.00008540413],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00049246603,0.00011521039,0.00023389667,0.000007501199,0.00060710503,0.00008694937,0.00042354158,0.00022989894,0.0029619986],"category_scores_gemma":[0.00010308618,0.000087403925,0.0000772849,0.0001376776,0.0014704643,0.00004690357,0.00041913983,0.00029904977,0.0001028812],"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":[0.000024329715,0.00003742864,0.97724646,0.0000036712051,0.000019262427,0.000024269215,0.000098637014,0.00009754048,0.00038581455,0.00003565366,0.015289571,0.0067373505],"study_design_scores_gemma":[0.0008780012,0.00012881181,0.80992687,0.000008949096,0.000037864254,0.00036965992,0.00005654722,0.00013827013,0.00006750826,0.00080596074,0.18743882,0.00014274231],"about_ca_topic_score_codex":0.10044828,"about_ca_topic_score_gemma":0.48221746,"teacher_disagreement_score":0.38176918,"about_ca_system_score_codex":0.00002505023,"about_ca_system_score_gemma":0.000014285926,"threshold_uncertainty_score":0.9979494},"labels":[],"label_agreement":null},{"id":"W2078204268","doi":"10.1016/j.geomorph.2003.07.015","title":"Replay of the 1987 Val Pola Landslide, Italian Alps","year":2003,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":169,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Landslide; Geology; Zoning; Landform; Terrain; Scale (ratio); Natural hazard; Geomorphology; Remote sensing; Seismology; Cartography; Geography; Civil engineering; Engineering","score_opus":0.005007814712962799,"score_gpt":0.19153384712103635,"score_spread":0.18652603240807356,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2078204268","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":[0.9131099,0.00007124194,0.00005405707,0.00056281156,0.000691278,0.00011383685,0.000018622857,0.000015452672,0.08536279],"genre_scores_gemma":[0.99149275,0.000017990053,0.00025886254,0.0004698506,0.000018015982,0.0000033036406,0.000005187106,0.0000092961955,0.007724767],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991088,0.00010276703,0.00018169775,0.00020211343,0.00014819615,0.00025640885],"domain_scores_gemma":[0.99945515,0.000031420263,0.000089068846,0.00036532973,0.00000552978,0.00005348028],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00024989093,0.00009217346,0.00013952004,0.000013740361,0.000094865834,0.000005038746,0.0002267389,0.00013040358,0.0072246045],"category_scores_gemma":[0.000060233422,0.000053584223,0.00007950156,0.00017004472,0.00026879358,0.000033659802,0.00011136049,0.00015317263,0.0004286051],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005129046,0.00017334467,0.8639263,0.000009114074,0.00006126505,0.000104295934,0.00063230767,0.00095479947,0.025462184,0.0040502674,0.10274196,0.0018329073],"study_design_scores_gemma":[0.0009434438,0.00014593895,0.16852972,0.000011071724,0.000045174143,0.0007249748,0.00008374819,0.000035801266,0.013725289,0.0021476916,0.8133833,0.0002238473],"about_ca_topic_score_codex":0.00042757782,"about_ca_topic_score_gemma":0.00013021908,"teacher_disagreement_score":0.7106413,"about_ca_system_score_codex":0.000030179046,"about_ca_system_score_gemma":0.000013202389,"threshold_uncertainty_score":0.9936829},"labels":[],"label_agreement":null},{"id":"W2078670842","doi":"10.1016/j.geomorph.2013.03.005","title":"Quantifying spatial and temporal trends in beach–dune volumetric changes using spatial statistics","year":2013,"lang":"en","type":"article","venue":"Geomorphology","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Core Research for Evolutional Science and Technology; Natural Sciences and Engineering Research Council of Canada; Parks Canada; Geological Society of America","keywords":"Beach morphodynamics; Foredune; Geology; Spatial analysis; Spatial distribution; Physical geography; Spatial ecology; Lidar; Sediment; Erosion; Sediment transport; Deposition (geology); Spatial variability; Hydrology (agriculture); Geomorphology; Remote sensing; Geography; Statistics; Aeolian processes; Ecology","score_opus":0.03838117535628322,"score_gpt":0.2596134430131239,"score_spread":0.22123226765684068,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2078670842","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":[0.9932505,0.00075364177,0.004878213,0.00025845246,0.00042588357,0.0001218635,0.00015706546,0.000020449746,0.00013397062],"genre_scores_gemma":[0.9951283,0.00003056343,0.0038160684,0.00017903812,0.00015116422,0.0000018614363,0.0005811243,0.000005604273,0.00010631849],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99890584,0.00008103667,0.00018370753,0.00028313362,0.000121185265,0.00042512864],"domain_scores_gemma":[0.9995474,0.00011383151,0.00009389433,0.000102216094,0.000031219242,0.00011141332],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00016217421,0.00014521068,0.00025070008,0.0003529177,0.00010274916,0.0000497182,0.00010112039,0.00011658041,0.004402808],"category_scores_gemma":[0.000052734144,0.0001303431,0.000015152641,0.00038193163,0.0001348937,0.000115016875,0.000022826407,0.00015764826,0.00010340984],"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":[0.000017473812,0.000009413139,0.70799345,0.000021745245,0.000004403929,0.00007196515,0.00009768272,0.00025317722,0.00005274988,0.0000058683695,0.0007493637,0.29072273],"study_design_scores_gemma":[0.00037407942,0.00024682848,0.7535177,0.000009068653,0.000010354707,0.00009608349,0.000054986413,0.24460755,0.0000181316,0.00015014237,0.0007633858,0.00015168414],"about_ca_topic_score_codex":0.17508839,"about_ca_topic_score_gemma":0.12151647,"teacher_disagreement_score":0.29057106,"about_ca_system_score_codex":0.000005219442,"about_ca_system_score_gemma":0.000020472668,"threshold_uncertainty_score":0.9965073},"labels":[],"label_agreement":null},{"id":"W2080041132","doi":"10.1016/j.geomorph.2006.05.004","title":"Aeolian shear stress ratio measurements within mesquite-dominated landscapes of the Chihuahuan Desert, New Mexico, USA","year":2006,"lang":"en","type":"article","venue":"Geomorphology","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":92,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"Natural Sciences and Engineering Research Council of Canada; Agricultural Research Service; U.S. Department of Agriculture; National Aeronautics and Space Administration; University of Guelph; National Science Foundation","keywords":"Aeolian processes; Geology; Shear stress; Vegetation (pathology); Surface finish; Shear (geology); Surface roughness; Hydrology (agriculture); Geomorphology; Soil science; Atmospheric sciences; Geotechnical engineering; Mechanics; Materials science; Petrology","score_opus":0.014742265153436185,"score_gpt":0.21105849820696224,"score_spread":0.19631623305352605,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2080041132","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":[0.9922463,0.00050433463,0.00022570015,0.000563184,0.0005483575,0.0002587077,0.00010550594,0.000024901847,0.005522994],"genre_scores_gemma":[0.9980954,0.000005303607,0.00029177355,0.00028531827,0.00012575096,0.0000015297467,0.00015388055,0.000006287982,0.0010347355],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985659,0.0001503875,0.00031768408,0.00027720004,0.0002985704,0.00039024002],"domain_scores_gemma":[0.9992751,0.00007581188,0.00020295268,0.0002791324,0.000064663735,0.000102377555],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003081697,0.00018024162,0.00027132695,0.00006159948,0.0001680287,0.000027210579,0.00042058632,0.00012405576,0.0025605331],"category_scores_gemma":[0.00006325616,0.00011829337,0.000073498995,0.0003047049,0.00014494202,0.0001161079,0.000030354755,0.00015537106,0.0001654237],"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":[0.00009492469,0.00003250986,0.96418285,0.000038045695,0.000028676906,0.000018264216,0.00020721214,0.026075007,0.0010522184,0.00012532962,0.006921367,0.001223591],"study_design_scores_gemma":[0.0012711757,0.0002502846,0.9461813,0.00005538847,0.00006051746,0.000097642136,0.000091130176,0.012682734,0.035296764,0.0018880778,0.0018524247,0.00027257396],"about_ca_topic_score_codex":0.014147091,"about_ca_topic_score_gemma":0.04288035,"teacher_disagreement_score":0.034244545,"about_ca_system_score_codex":0.0000053974563,"about_ca_system_score_gemma":0.00013455235,"threshold_uncertainty_score":0.9983513},"labels":[],"label_agreement":null},{"id":"W2080385250","doi":"10.1016/s0169-555x(01)00030-7","title":"The case of the missing flood: the unrecorded flood of 1935 on the James River, Mason County, Texas","year":2001,"lang":"en","type":"article","venue":"Geomorphology","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Brock University","funders":"","keywords":"Tributary; Flood myth; Geology; Floodplain; Hydrology (agriculture); Alluvium; Bedrock; Drainage basin; Archaeology; Geography; Geomorphology; Cartography","score_opus":0.009007744223513456,"score_gpt":0.2024620653313393,"score_spread":0.19345432110782584,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2080385250","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":[0.98800033,0.00010255016,0.000053562377,0.0045189275,0.0002612842,0.00022748829,0.00007177325,0.0000073895676,0.0067566847],"genre_scores_gemma":[0.9983221,0.00013759593,0.00003946705,0.00049762207,0.000019999912,0.000006431,0.000005939053,0.000008253154,0.00096255547],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99896413,0.00024052651,0.00022567785,0.00016313377,0.00016651556,0.00024001335],"domain_scores_gemma":[0.99876416,0.00045807817,0.00017901282,0.0005622203,0.000011559842,0.000024984809],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005158161,0.00011494455,0.00012542462,0.000012795914,0.00040994034,0.000017117169,0.00052512664,0.00007605936,0.0004541045],"category_scores_gemma":[0.000060469167,0.000046331177,0.00007744348,0.00020254303,0.0009911844,0.00003094045,0.00021217861,0.0002155445,0.00005549083],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00085826253,0.0014619878,0.6097214,0.00004239219,0.0006723312,0.0023212126,0.009698293,0.09729817,0.035659485,0.04693795,0.06504442,0.13028409],"study_design_scores_gemma":[0.003910113,0.001058498,0.31669462,0.00016635869,0.00070965436,0.023147997,0.003839414,0.15082726,0.013388729,0.044801857,0.44019392,0.001261613],"about_ca_topic_score_codex":0.003079547,"about_ca_topic_score_gemma":0.0019472202,"teacher_disagreement_score":0.3751495,"about_ca_system_score_codex":0.000040403665,"about_ca_system_score_gemma":0.000014540456,"threshold_uncertainty_score":0.4972126},"labels":[],"label_agreement":null},{"id":"W2081527230","doi":"10.1016/j.geomorph.2011.11.015","title":"Turbulent Reynolds stress and quadrant event activity in wind flow over a coastal foredune","year":2011,"lang":"en","type":"article","venue":"Geomorphology","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Okanagan University College; University of British Columbia, Okanagan Campus; University of British Columbia; University of Guelph; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; Rural Development Administration; Parks Canada; National Science Foundation","keywords":"Geology; Reynolds stress; Turbulence; Foredune; Streamlines, streaklines, and pathlines; Geomorphology; Aeolian processes; Mechanics; Meteorology; Physics","score_opus":0.014009352883139415,"score_gpt":0.20973458562174008,"score_spread":0.19572523273860065,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2081527230","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":[0.99832314,0.00026640555,0.00018652515,0.00016484274,0.00019218789,0.00015363847,0.0001357492,0.000015776315,0.0005617374],"genre_scores_gemma":[0.9993059,0.000058382175,0.0002817863,0.00015812872,0.00004109918,0.0000015265315,0.000060436312,0.0000036417327,0.00008906737],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990361,0.000068028945,0.00013549322,0.00028639275,0.00010212977,0.000371869],"domain_scores_gemma":[0.9996284,0.000053631207,0.00005834591,0.00013514629,0.000013645939,0.00011080251],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00018077467,0.00013400237,0.00020578918,0.00006642327,0.000057953825,0.000011906622,0.00010943089,0.000113359674,0.0024727758],"category_scores_gemma":[0.000016515254,0.00011031206,0.00002949801,0.00010696959,0.00014024842,0.00013487201,0.00002524067,0.00015499452,0.000066152796],"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":[0.00040643488,0.00009032066,0.9782871,0.00007310181,0.000017286517,0.0006748579,0.0011044288,0.0007110824,0.000090293135,0.00002968933,0.0003997123,0.018115707],"study_design_scores_gemma":[0.0006319923,0.00035670362,0.9805494,0.000025150786,0.000009107581,0.00017586644,0.00008427102,0.016700312,0.00042911211,0.0005104222,0.00037642135,0.00015124054],"about_ca_topic_score_codex":0.012736856,"about_ca_topic_score_gemma":0.028172025,"teacher_disagreement_score":0.017964467,"about_ca_system_score_codex":0.000003205249,"about_ca_system_score_gemma":0.00003424,"threshold_uncertainty_score":0.9984391},"labels":[],"label_agreement":null},{"id":"W2082656552","doi":"10.1016/j.geomorph.2008.04.007","title":"Dating, triggering, modelling, and hazard assessment of large landslides","year":2008,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":34,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Geology; Landslide; Hazard analysis; Hazard; Geomorphology; Seismology","score_opus":0.015941163273958395,"score_gpt":0.2545401175268781,"score_spread":0.23859895425291971,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082656552","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":[0.9813955,0.000115335424,0.0057414193,0.00007502122,0.00011039244,0.000094363066,0.0000229886,0.00002482162,0.012420166],"genre_scores_gemma":[0.9940261,0.00046770953,0.00424828,0.00012208961,0.000020633926,0.0000060323687,0.000023663826,0.00001113605,0.0010743145],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990505,0.00004078524,0.0002271371,0.00025106242,0.00015342476,0.00027708392],"domain_scores_gemma":[0.9995814,0.000033518692,0.00010765851,0.00019297027,0.000007943961,0.00007653129],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00023898021,0.00011124779,0.00022469116,0.0000312732,0.00013538006,0.0000045533548,0.00012182149,0.00011760369,0.0035823314],"category_scores_gemma":[0.000009539045,0.0000860856,0.00004095241,0.00008838295,0.00023424375,0.000063802494,0.00019456142,0.00015093769,0.000049030048],"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":[0.000044988825,0.0002552696,0.9523494,0.000024610277,0.00006312477,0.00026809968,0.0007341944,0.024394218,0.0033952997,0.00087186176,0.016471649,0.0011272614],"study_design_scores_gemma":[0.0061770263,0.001022111,0.48422834,0.000053360825,0.00012594232,0.0022978717,0.00020560005,0.19354148,0.0036950696,0.0013914946,0.30630243,0.0009592741],"about_ca_topic_score_codex":0.00027355002,"about_ca_topic_score_gemma":0.00003961376,"teacher_disagreement_score":0.46812108,"about_ca_system_score_codex":0.000024914276,"about_ca_system_score_gemma":0.000014325056,"threshold_uncertainty_score":0.9973285},"labels":[],"label_agreement":null},{"id":"W2082889799","doi":"10.1016/s0169-555x(99)00101-4","title":"Environmental assessment from the sedimentary record of high-latitude fiords","year":2000,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"","keywords":"Geology; Sedimentary rock; Fjord; Sedimentary depositional environment; Oceanography; Earth science; Paleontology; Physical geography; Structural basin","score_opus":0.009868647746526137,"score_gpt":0.22324441971136474,"score_spread":0.21337577196483862,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082889799","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":[0.9940488,0.0003996868,0.00001808172,0.0019407733,0.00027931167,0.00013376541,0.00041773607,0.000011419968,0.002750429],"genre_scores_gemma":[0.9959437,0.00027070066,0.0013850039,0.001147592,0.000066552435,0.0000026072373,0.0008883688,0.0000022016714,0.0002932415],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99874854,0.000317526,0.00021833787,0.0002481105,0.00015023898,0.00031724793],"domain_scores_gemma":[0.99904984,0.00054068706,0.000056818804,0.0002880311,0.0000052234263,0.000059400074],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00026505513,0.00010791036,0.00021008732,0.000025712403,0.00015940408,0.0000052669384,0.00034128065,0.0001328324,0.21673334],"category_scores_gemma":[0.0000063489147,0.00007530047,0.00004577178,0.00006395858,0.00057366036,0.0000522752,0.00002149577,0.00028167246,0.0016248467],"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":[0.00007730691,0.00003111091,0.9861406,0.0000013681083,0.00004742587,0.00005914315,0.00006145891,0.00058196124,0.00003131149,0.000019488867,0.0016989547,0.011249836],"study_design_scores_gemma":[0.00040835657,0.0001977836,0.99014425,0.0000025529619,0.000020443458,0.000067409834,0.00005950799,0.00032357598,0.00006579402,0.0013098713,0.007323166,0.000077268254],"about_ca_topic_score_codex":0.009598325,"about_ca_topic_score_gemma":0.0055902447,"teacher_disagreement_score":0.2151085,"about_ca_system_score_codex":0.0000016048308,"about_ca_system_score_gemma":0.000032836,"threshold_uncertainty_score":0.9991525},"labels":[],"label_agreement":null},{"id":"W2084198271","doi":"10.1016/j.geomorph.2015.02.025","title":"Reconsidering the glacier to rock glacier transformation problem: New insights from the central Andes of Chile","year":2015,"lang":"en","type":"article","venue":"Geomorphology","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":99,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Trois-Rivières","funders":"Fondo Nacional de Desarrollo Científico y Tecnológico","keywords":"Geology; Glacier; Rock glacier; Glacier mass balance; Permafrost; Debris; Glacier morphology; Geomorphology; Accumulation zone; Tidewater glacier cycle; Massif; Physical geography; Paleontology; Climatology; Ice stream; Cryosphere; Geography; Oceanography","score_opus":0.08150758402558536,"score_gpt":0.2171993895220364,"score_spread":0.13569180549645105,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2084198271","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":[0.98709714,0.00092713104,0.0019347336,0.007739265,0.0004372272,0.00029609894,0.00006940745,0.000015688058,0.0014833019],"genre_scores_gemma":[0.9971925,0.000052630498,0.0006974675,0.001681136,0.00014834199,0.0000025084396,0.00008634968,0.0000021030994,0.00013696385],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99929833,0.000055007462,0.00020036024,0.00012395762,0.00011882431,0.00020351987],"domain_scores_gemma":[0.9994779,0.00017165109,0.00005880555,0.00015824175,0.00004292188,0.00009047259],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000109323155,0.00008200539,0.00012827919,0.000009779557,0.00017349095,0.000021581474,0.00017591508,0.00003988841,0.0012318995],"category_scores_gemma":[0.0000478582,0.000043508247,0.0000351212,0.00018876659,0.000050430863,0.00009813017,0.000014906115,0.000079539466,0.00009819328],"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":[0.0002321429,0.000039855957,0.69656354,0.000010663008,0.00015747035,0.0000090454905,0.088888995,0.057072878,0.00026362392,0.0005648561,0.09940108,0.056795828],"study_design_scores_gemma":[0.00037693474,0.0001097753,0.8205956,0.0000074641976,0.000023189865,0.000013984577,0.0034436528,0.0010876572,0.000114190494,0.0029710142,0.17116483,0.00009167656],"about_ca_topic_score_codex":0.010059732,"about_ca_topic_score_gemma":0.028495157,"teacher_disagreement_score":0.12403207,"about_ca_system_score_codex":0.000004305017,"about_ca_system_score_gemma":0.00007019851,"threshold_uncertainty_score":0.9996811},"labels":[],"label_agreement":null},{"id":"W2085528478","doi":"10.1016/j.geomorph.2015.04.009","title":"Application of an integrated geotechnical and topographic monitoring system in the Lorano marble quarry (Apuan Alps, Italy)","year":2015,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":25,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"Ministero dell’Istruzione, dell’Università e della Ricerca","keywords":"Geology; Geomorphology; Mining engineering; Geotechnical engineering","score_opus":0.01110277532357373,"score_gpt":0.22984062713113446,"score_spread":0.21873785180756072,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2085528478","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":[0.9985013,0.00011921629,0.00040786713,0.00011973719,0.00009834669,0.00018655084,0.0000045746046,0.000025328083,0.0005370622],"genre_scores_gemma":[0.9996353,0.00001691837,0.00023796783,0.000025367732,0.000021382057,0.000025311205,0.000016023552,0.0000061448104,0.000015617801],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991874,0.00011546841,0.00019242572,0.00020205774,0.00013665145,0.000165978],"domain_scores_gemma":[0.9995889,0.000029610692,0.00006517521,0.00024656332,0.000009305695,0.0000604599],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006198801,0.000081452905,0.0001414129,0.0000426837,0.000036422345,0.000009446804,0.0002066791,0.00017118089,0.000020691929],"category_scores_gemma":[0.0000119806555,0.00005132652,0.000020383151,0.0002806948,0.00020732667,0.000070792375,0.000069723435,0.00019223096,0.00002324834],"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":[0.00043417234,0.0005869687,0.9027241,0.00007341057,0.000051399933,0.0002859508,0.0036836497,0.008143424,0.028779183,0.0024065983,0.0010497753,0.05178136],"study_design_scores_gemma":[0.004574199,0.0019741857,0.8944396,0.00012593136,0.0001499317,0.001986348,0.01777237,0.034529988,0.005222442,0.002489142,0.035877597,0.0008583092],"about_ca_topic_score_codex":0.002963591,"about_ca_topic_score_gemma":0.0001634527,"teacher_disagreement_score":0.05092305,"about_ca_system_score_codex":0.000047053043,"about_ca_system_score_gemma":0.000007612294,"threshold_uncertainty_score":0.44800827},"labels":[],"label_agreement":null},{"id":"W2089302046","doi":"10.1016/j.geomorph.2009.02.003","title":"The effect of Holocene changes in relative sea level on the morphology of rocky coasts","year":2009,"lang":"en","type":"article","venue":"Geomorphology","topic":"Coastal and Marine Dynamics","field":"Earth and Planetary Sciences","cited_by":73,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Windsor","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Holocene; Intertidal zone; Geology; Oceanography; Shore; Sea level; Erosion; Physical geography; Paleontology; Geography","score_opus":0.013793508173999054,"score_gpt":0.21611051186408786,"score_spread":0.20231700369008881,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2089302046","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":[0.9920129,0.0001392195,0.000026388441,0.003757735,0.00017529438,0.00022482238,0.00022269519,0.0000072058015,0.0034337344],"genre_scores_gemma":[0.999134,0.000084913794,0.000020258234,0.00031125208,0.000022577984,0.0000019247716,0.00008542009,0.0000020133011,0.00033762152],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998926,0.00030343738,0.00020007281,0.00017106216,0.00012019948,0.00027926874],"domain_scores_gemma":[0.9981729,0.0013946546,0.00014104054,0.00023127637,0.000029320463,0.000030851348],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006144436,0.0001225491,0.00026114626,0.00006942817,0.00007851241,0.0000037866744,0.0002841703,0.000092820155,0.0003127413],"category_scores_gemma":[0.0001990557,0.0000622218,0.00004682527,0.00022035035,0.00030376622,0.000025672929,0.0000334931,0.00022241718,0.000033272972],"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":[0.0015907891,0.000060505165,0.7662841,0.000019626674,0.000047025347,0.00013385326,0.00035269296,0.0026626717,0.0008631288,0.0029441619,0.0017428924,0.22329856],"study_design_scores_gemma":[0.0005585854,0.0032818196,0.9896889,0.000012469587,0.00001270659,0.00007427474,0.00004702646,0.0012351127,0.0022765463,0.002165659,0.00056203327,0.00008487284],"about_ca_topic_score_codex":0.0031085445,"about_ca_topic_score_gemma":0.013525806,"teacher_disagreement_score":0.22340481,"about_ca_system_score_codex":0.0000034569046,"about_ca_system_score_gemma":0.000019428457,"threshold_uncertainty_score":0.75477177},"labels":[],"label_agreement":null},{"id":"W2091126394","doi":"10.1016/j.geomorph.2007.08.012","title":"Replication of a terrain stability mapping using an Artificial Neural Network","year":2007,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":21,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Terrain; Artificial neural network; Learning vector quantization; Vector quantization; Geology; Artificial intelligence; Computer science; Remote sensing; Data mining; Cartography; Geography","score_opus":0.04065540726044532,"score_gpt":0.2730453934650072,"score_spread":0.23238998620456192,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2091126394","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":[0.99239504,0.000014458499,0.0064951945,0.00008278685,0.00020066516,0.000116688076,0.000004287575,0.000020140164,0.000670725],"genre_scores_gemma":[0.99757767,0.0000011219198,0.0021520355,0.0001357193,0.000086381995,0.0000011745137,0.000025664502,0.00000633709,0.000013875355],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9989884,0.00006408972,0.00027324422,0.00029472736,0.00009766687,0.00028186693],"domain_scores_gemma":[0.9993777,0.000030599298,0.00011567918,0.00040732563,0.0000079078245,0.00006073077],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011329796,0.00006824809,0.00012115114,0.000017406359,0.000088434215,0.000004534422,0.00011947071,0.00011194637,0.0013229667],"category_scores_gemma":[0.00003087975,0.000058084763,0.000041962772,0.00018368156,0.00020810253,0.00006643008,0.00008583227,0.00010837656,0.000024847743],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019105736,0.00022396183,0.27069852,0.000008181179,0.000018516317,0.000043073112,0.0017020765,0.029902719,0.6656579,0.0001677032,0.00043311532,0.030953191],"study_design_scores_gemma":[0.000864188,0.0005907295,0.861941,0.000020123205,0.00007100861,0.00049522164,0.0010402512,0.08342208,0.03380062,0.007518149,0.009621912,0.0006147496],"about_ca_topic_score_codex":0.00066816784,"about_ca_topic_score_gemma":0.00037684696,"teacher_disagreement_score":0.6318573,"about_ca_system_score_codex":0.000059449427,"about_ca_system_score_gemma":0.0000059138074,"threshold_uncertainty_score":0.99959},"labels":[],"label_agreement":null},{"id":"W2096169908","doi":"10.1016/s0169-555x(02)00137-x","title":"Biogeomorphology revisited: looking towards the future","year":2002,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":193,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Royal Geographical Society; Royal Society","keywords":"Landform; Temporal scales; Relevance (law); Earth science; Variety (cybernetics); Key (lock); TRACE (psycholinguistics); Sampling (signal processing); Environmental resource management; Scale (ratio); Data science; Computer science; Management science; Geology; Ecology; Environmental science; Geography; Engineering; Geomorphology; Cartography; Political science; Artificial intelligence; Biology","score_opus":0.026052313687416416,"score_gpt":0.23146241888066124,"score_spread":0.20541010519324482,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2096169908","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":[0.8996539,0.01589926,0.00005639681,0.031134339,0.0018281696,0.00035300563,0.00012789681,0.00012183905,0.05082516],"genre_scores_gemma":[0.9921139,0.0010394074,0.00018459118,0.004422612,0.00049107324,0.0000049456444,0.00021491965,0.0000054459706,0.0015231377],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9976382,0.000565066,0.00028934184,0.00045643072,0.00018868154,0.00086225517],"domain_scores_gemma":[0.9988063,0.0003472636,0.00010116845,0.0005394619,0.00007100203,0.00013477982],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00068165496,0.00021189726,0.0003359175,0.00014540799,0.0005383189,0.000028911201,0.0007097733,0.00039782206,0.08846014],"category_scores_gemma":[0.00008838666,0.00013718122,0.000103678794,0.00042168118,0.0009472969,0.00008378262,0.000053363627,0.000709208,0.010695824],"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":[0.00002779901,0.000015820631,0.96585023,0.0000074423187,0.00003438556,0.0005227847,0.0001285793,0.000027278136,0.000009681577,0.00061377115,0.021547258,0.01121498],"study_design_scores_gemma":[0.0006334726,0.00029497143,0.7512375,0.0000058964592,0.000039347517,0.0073390366,0.00024900894,0.0011976568,0.000049671762,0.0023166281,0.23634139,0.0002953967],"about_ca_topic_score_codex":0.00027103556,"about_ca_topic_score_gemma":0.0018182613,"teacher_disagreement_score":0.21479413,"about_ca_system_score_codex":0.0000015309088,"about_ca_system_score_gemma":0.000023873845,"threshold_uncertainty_score":0.99007446},"labels":[],"label_agreement":null},{"id":"W2097004312","doi":"10.1016/j.geomorph.2013.01.001","title":"Muted responses of streamflow and suspended sediment flux in a wildfire-affected watershed","year":2013,"lang":"en","type":"article","venue":"Geomorphology","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":63,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; Ministry of Forests; University of Northern British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Snowmelt; Hydrology (agriculture); Watershed; Streamflow; Precipitation; Sediment; Environmental science; Surface runoff; Vegetation (pathology); Period (music); Snow; Geology; Drainage basin; Geography; Ecology; Geomorphology; Meteorology","score_opus":0.005497837971921019,"score_gpt":0.19981148157923972,"score_spread":0.1943136436073187,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2097004312","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":[0.99802953,0.00002915965,0.0000070844003,0.00035668738,0.00011646261,0.0006702039,0.000011093178,0.000033913362,0.0007458461],"genre_scores_gemma":[0.9987915,0.000003982514,0.00033056433,0.000118451695,0.000008994775,0.00007911081,0.000033013082,0.0000144642045,0.0006198847],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.998466,0.0003668685,0.0002895884,0.0003516275,0.00015600871,0.00036989627],"domain_scores_gemma":[0.9993275,0.00018824186,0.00009639347,0.00029053297,0.000006148645,0.00009118239],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00037178196,0.00015613022,0.00030797176,0.000091558926,0.000031916625,0.000011110306,0.00016251003,0.00012657799,0.007764969],"category_scores_gemma":[0.000104757506,0.00013633091,0.00002742853,0.00020742847,0.0002604681,0.00012612985,0.00017774281,0.00011394982,0.000899373],"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":[0.00014552647,0.00020860354,0.31231013,0.000026572769,0.000022998665,0.0001194875,0.0006548351,0.000025674655,0.6750429,0.00000812318,0.007506041,0.0039290725],"study_design_scores_gemma":[0.0016259667,0.00045569552,0.9525174,0.000021223033,0.000010279708,0.00011849043,0.000086484484,0.0021216075,0.04207921,0.00014589266,0.00062617287,0.00019157736],"about_ca_topic_score_codex":0.015616892,"about_ca_topic_score_gemma":0.0014390303,"teacher_disagreement_score":0.6402073,"about_ca_system_score_codex":0.00009976797,"about_ca_system_score_gemma":0.000008927302,"threshold_uncertainty_score":0.9998785},"labels":[],"label_agreement":null},{"id":"W2100947929","doi":"10.1016/j.geomorph.2009.04.019","title":"Hydraulic and sedimentary processes causing anastomosing morphology of the upper Columbia River, British Columbia, Canada","year":2009,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":107,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Geology; Bed load; Aggradation; Stream power; River morphology; Sediment transport; Hydrology (agriculture); Geomorphology; Channel (broadcasting); Sediment; Bedform; Sedimentary rock; Bank erosion; Erosion; Tributary; Hyperconcentrated flow; Fluvial; Geotechnical engineering; Paleontology; Structural basin","score_opus":0.004296816694746844,"score_gpt":0.1762163178018378,"score_spread":0.17191950110709095,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2100947929","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":[0.9971695,0.00044534294,0.000023206529,0.001060735,0.00023006418,0.00023914868,0.00005319371,0.00002252549,0.0007563177],"genre_scores_gemma":[0.992131,0.00007901909,0.00015022578,0.007006666,0.000023690896,0.000007910485,0.000028975484,0.000011206605,0.00056128216],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99845964,0.0000828236,0.00031937286,0.00044924195,0.0002273126,0.0004615901],"domain_scores_gemma":[0.9994575,0.000068545174,0.00011621184,0.00023326365,0.000024265033,0.00010021006],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001598476,0.00012787292,0.00030435674,0.000012785085,0.00041034253,0.000034547684,0.00025395516,0.0001534319,0.0035739131],"category_scores_gemma":[0.00004158924,0.00017543786,0.00003361925,0.0003205276,0.0010117171,0.00014563226,0.00010611515,0.00022127175,0.00000510959],"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":[0.000015071812,0.00010294203,0.9698457,0.000027984308,0.000022995657,0.00030594447,0.0002177637,0.00022819957,0.0048599443,0.0000010391378,0.02170831,0.0026640734],"study_design_scores_gemma":[0.0006591482,0.00018341589,0.98082936,0.000033087472,0.00007487963,0.0014041212,0.00006891276,0.00003425259,0.0016898968,0.00052646647,0.014249874,0.00024661384],"about_ca_topic_score_codex":0.9560124,"about_ca_topic_score_gemma":0.9879876,"teacher_disagreement_score":0.031975158,"about_ca_system_score_codex":0.000090342466,"about_ca_system_score_gemma":0.00018567401,"threshold_uncertainty_score":0.997337},"labels":[],"label_agreement":null},{"id":"W2115239267","doi":"10.1016/j.geomorph.2012.10.011","title":"Environmental conditions and geomorphologic changes during the Middle–Upper Paleolithic in the southern Iberian Peninsula","year":2012,"lang":"en","type":"article","venue":"Geomorphology","topic":"Pleistocene-Era Hominins and Archaeology","field":"Social Sciences","cited_by":16,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Junta de Andalucía; Ministerio de Ciencia e Innovación","keywords":"Peninsula; Geology; Middle Paleolithic; Physical geography; Paleontology; Geomorphology; Pleistocene; Archaeology; Geography","score_opus":0.028146911226889778,"score_gpt":0.2541743897676974,"score_spread":0.22602747854080762,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2115239267","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":[0.987416,0.0008897161,0.0000024875199,0.009575066,0.00024293977,0.0003473485,0.0001581092,0.000022012604,0.0013462803],"genre_scores_gemma":[0.9965526,0.00026876776,0.000041268384,0.0019620943,0.00033872935,0.000121864025,0.000035030618,0.000010587117,0.0006690575],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978019,0.0008776666,0.00016993564,0.00023065956,0.00016676013,0.0007531056],"domain_scores_gemma":[0.9992083,0.00034887053,0.00009356792,0.00024453647,0.000007344496,0.000097437114],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011328858,0.00014722584,0.00019030267,0.0000712285,0.0009279568,0.000022370952,0.00037289952,0.00017370316,0.0015008799],"category_scores_gemma":[0.00007577934,0.0000934131,0.000042245505,0.00011991612,0.0024735455,0.00007782862,0.00015230203,0.00031309167,0.00016359027],"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":[0.000018526436,0.00008650956,0.9302424,0.000003576869,0.000011897677,0.000056741843,0.062495504,0.0000012142237,0.0022713675,0.004548593,0.00010009897,0.00016358045],"study_design_scores_gemma":[0.00044234004,0.00005162149,0.94390064,0.000004022704,0.000016359136,0.00034296382,0.03772346,0.000002306939,0.00004835181,0.0008809812,0.016442943,0.0001440151],"about_ca_topic_score_codex":0.00046343345,"about_ca_topic_score_gemma":0.013056445,"teacher_disagreement_score":0.024772044,"about_ca_system_score_codex":0.000044298842,"about_ca_system_score_gemma":0.000024862453,"threshold_uncertainty_score":0.9994119},"labels":[],"label_agreement":null},{"id":"W2120110665","doi":"10.1016/j.geomorph.2004.06.013","title":"Subglacial morphology and glacial evolution of the Palmer deep outlet system, Antarctic Peninsula","year":2005,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":124,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"Universitat de Barcelona","keywords":"Geology; Glacial period; Continental shelf; Ice shelf; Iceberg; Seabed gouging by ice; Circumpolar deep water; Ice sheet; Seafloor spreading; Oceanography; Geomorphology; Ice stream; Trough (economics); Paleontology; Sea ice; Cryosphere; North Atlantic Deep Water; Deep water","score_opus":0.009296372838140818,"score_gpt":0.21350091381230837,"score_spread":0.20420454097416757,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2120110665","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":[0.9936308,0.0010996689,0.00009704925,0.0015664917,0.00065823534,0.00022189558,0.00004300397,0.000024145138,0.0026586785],"genre_scores_gemma":[0.9992243,0.000025124804,0.00018246796,0.00021638724,0.00016378892,0.0000032649916,0.00004574171,0.0000035171072,0.00013539167],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981445,0.0005359259,0.0003145384,0.0003301115,0.00016137114,0.000513545],"domain_scores_gemma":[0.99916697,0.0002531311,0.00013886904,0.0002849871,0.00006577164,0.000090287016],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005353409,0.00015086499,0.00033109708,0.00011614573,0.00028681385,0.0000072141975,0.0003272931,0.00031729345,0.0021721008],"category_scores_gemma":[0.00010933728,0.00010887924,0.00006836741,0.00020420837,0.0012614515,0.00007569075,0.000061292776,0.00035618676,0.00045206305],"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":[0.00016353425,0.000016342936,0.9974822,0.00002695792,0.00002493337,0.00004202349,0.00020106668,0.00019866454,0.00015953422,0.0010868534,0.00013797829,0.0004599397],"study_design_scores_gemma":[0.0007151787,0.00014929159,0.992737,0.0000065274776,0.000038397695,0.0025339364,0.00023098187,0.002159553,0.00012012152,0.00031930962,0.00086875557,0.00012093808],"about_ca_topic_score_codex":0.00095780136,"about_ca_topic_score_gemma":0.015014789,"teacher_disagreement_score":0.014056987,"about_ca_system_score_codex":0.0000061177925,"about_ca_system_score_gemma":0.00008423298,"threshold_uncertainty_score":0.9987401},"labels":[],"label_agreement":null},{"id":"W2129210534","doi":"10.1016/j.geomorph.2005.06.007","title":"Morphodynamics of intertidal bars in wave-dominated coastal settings — A review","year":2005,"lang":"en","type":"review","venue":"Geomorphology","topic":"Coastal and Marine Dynamics","field":"Earth and Planetary Sciences","cited_by":219,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"","keywords":"Intertidal zone; Beach morphodynamics; Geology; Tidal range; Berm; Submarine pipeline; Shore; Oceanography; Wave height; Swash; Intertidal ecology; Storm; Sediment transport; Sediment; Geomorphology; Estuary; Geotechnical engineering","score_opus":0.01996731174651615,"score_gpt":0.26369169903360556,"score_spread":0.24372438728708942,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2129210534","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00022283621,0.9943683,0.000026763752,0.00011505844,0.00037564032,0.0007685901,0.0019195764,0.000028705814,0.0021745085],"genre_scores_gemma":[0.00011194913,0.9918918,0.00044618666,0.00033250955,0.00006162211,0.000009660398,0.0065062414,0.000018144481,0.00062191166],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9970141,0.0003241878,0.0012954917,0.0005678842,0.00020773412,0.00059060915],"domain_scores_gemma":[0.9984414,0.00030700126,0.0006342082,0.00042227024,0.000066132896,0.00012898784],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006649249,0.00050158275,0.0024792263,0.0003402178,0.00003244903,0.000011932083,0.00050138816,0.00037502768,0.004296862],"category_scores_gemma":[0.000164002,0.00041173794,0.0004327062,0.00064389704,0.00025229872,0.00008444706,0.00018495276,0.00071961357,0.00024432605],"study_design_candidate":"design_other","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":[0.000015586145,0.00003262683,0.00017484819,0.013458939,0.00003782016,0.0003021376,0.000013804887,0.000017518463,1.1517647e-7,0.000018185725,0.0008891223,0.9850393],"study_design_scores_gemma":[0.00028427565,0.00015529267,0.00031017693,0.014781387,0.0002990771,0.0016246989,0.000011230363,0.0013818763,6.0458646e-8,0.000040442203,0.9806746,0.00043685376],"about_ca_topic_score_codex":0.0034033612,"about_ca_topic_score_gemma":0.02089573,"teacher_disagreement_score":0.98460245,"about_ca_system_score_codex":0.000020629146,"about_ca_system_score_gemma":0.00026616716,"threshold_uncertainty_score":0.99983346},"labels":[],"label_agreement":null},{"id":"W2130974954","doi":"10.1016/j.geomorph.2006.10.024","title":"Embedding reach-scale fluvial dynamics within the CAESAR cellular automaton landscape evolution model","year":2007,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":187,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Environment Research Council","keywords":"Aggradation; Geology; Fluvial; Sediment transport; Cellular automaton; Overbank; Channel (broadcasting); Geomorphology; Bed load; Beach morphodynamics; Erosion; Bank erosion; Meander (mathematics); Hydrology (agriculture); Scale (ratio); Sediment; Computer science; Geometry; Geotechnical engineering; Algorithm","score_opus":0.005627062305126073,"score_gpt":0.21478056975085844,"score_spread":0.20915350744573236,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2130974954","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":[0.87542,0.000056292996,0.11828005,0.00048534438,0.00024594323,0.00013584897,0.000013035475,0.00009340392,0.00527009],"genre_scores_gemma":[0.9973511,0.0000052540163,0.0014755838,0.00047758812,0.000049098955,0.000009007017,0.000095466894,0.000015287687,0.00052162266],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99868584,0.00005031628,0.00028017297,0.000342381,0.00019811079,0.0004431606],"domain_scores_gemma":[0.9994887,0.00005377441,0.00010012221,0.00026769994,0.000008426861,0.00008128008],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008975883,0.00015594868,0.0001628479,0.000038503455,0.00033207863,0.000008577476,0.0003061595,0.00022987298,0.0010959139],"category_scores_gemma":[0.000014002556,0.00011939836,0.00005034131,0.00017219185,0.00041500494,0.00013104848,0.00007905438,0.0002859973,0.0003872209],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003551458,0.00032322068,0.27420372,0.000025254392,0.00005213206,0.00033182395,0.0036950842,0.6391901,0.06972538,0.0070814136,0.003918806,0.0010979414],"study_design_scores_gemma":[0.0005795759,0.00011424992,0.012425018,0.0000052174037,0.000060375412,0.00016900104,0.0002973505,0.97484434,0.0060800295,0.0039855377,0.0011589333,0.00028039576],"about_ca_topic_score_codex":0.0002681179,"about_ca_topic_score_gemma":0.0018767875,"teacher_disagreement_score":0.33565423,"about_ca_system_score_codex":0.000110579036,"about_ca_system_score_gemma":0.000021349606,"threshold_uncertainty_score":0.9998172},"labels":[],"label_agreement":null},{"id":"W2131755739","doi":"10.1016/s0169-555x(99)00127-0","title":"Modelling hillslope evolution: linear and nonlinear transport relations","year":2000,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":111,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Sediment transport; Fluvial; Geomorphology; Weathering; Diffusion; Soil production function; Sediment; Hydrology (agriculture); Soil science; Geotechnical engineering; Structural basin; Pedogenesis","score_opus":0.01782284980751883,"score_gpt":0.22109251176643221,"score_spread":0.20326966195891338,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2131755739","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":[0.9795012,0.00086704403,0.0023226747,0.0011811467,0.00014678537,0.00011418685,0.00009151195,0.000046285306,0.015729195],"genre_scores_gemma":[0.99067897,0.0002045191,0.0055631427,0.00019807546,0.00009685911,0.0000015733988,0.0004211352,0.0000029429546,0.0028327873],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989755,0.000076477896,0.0001920655,0.000290863,0.00008850675,0.00037659163],"domain_scores_gemma":[0.9995264,0.00013981857,0.000024382485,0.0001588823,0.000033502474,0.00011704851],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00026043074,0.00010672611,0.00017886891,0.00007922821,0.00029844852,0.0000045320344,0.00012332526,0.00022376596,0.029203638],"category_scores_gemma":[0.000009612469,0.00009792001,0.000034045024,0.00016019586,0.0004127202,0.00009499578,0.000004298707,0.0003098122,0.0022419484],"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":[0.000054162727,0.00001329985,0.9030843,0.0000035585563,0.000011941303,0.000060949613,0.000069612324,0.09603117,0.0000011927085,0.0001445071,0.000086508866,0.00043881673],"study_design_scores_gemma":[0.00074457424,0.00018777841,0.5853696,0.000006806269,0.00003175297,0.0015612114,0.000042530908,0.37519914,0.0000039166266,0.0015327369,0.035093553,0.00022643579],"about_ca_topic_score_codex":0.00075997115,"about_ca_topic_score_gemma":0.0014788721,"teacher_disagreement_score":0.31771472,"about_ca_system_score_codex":8.7141984e-7,"about_ca_system_score_gemma":0.00005109678,"threshold_uncertainty_score":0.9985349},"labels":[],"label_agreement":null},{"id":"W2135547181","doi":"10.1016/s0169-555x(03)00141-7","title":"Zoogeomorphology in the Alpine: some observations on abiotic–biotic interactions","year":2003,"lang":"en","type":"article","venue":"Geomorphology","topic":"Ecology and Vegetation Dynamics Studies","field":"Environmental Science","cited_by":67,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Northern British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Abiotic component; Bedrock; Environmental science; Biotic component; Ecology; Ecosystem engineer; Context (archaeology); Ecosystem; Aeolian processes; Hydrology (agriculture); Geology; Geomorphology; Biology; Geotechnical engineering","score_opus":0.023814172154449312,"score_gpt":0.25365088348781545,"score_spread":0.22983671133336614,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2135547181","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":[0.97430784,0.000043094966,0.0001313626,0.008293256,0.00064354506,0.00026152146,0.000011361623,0.000022468657,0.016285554],"genre_scores_gemma":[0.98863035,0.000042745964,0.00034217333,0.009562206,0.000021218106,0.00006082137,0.00003066395,0.000008437022,0.0013013771],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986417,0.0003549706,0.00025193507,0.0003037761,0.00009675532,0.00035084042],"domain_scores_gemma":[0.9990488,0.00052710465,0.00008260038,0.00029950665,0.000009608115,0.000032334356],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00043464117,0.00013732181,0.00016808404,0.00006981637,0.00027481568,0.000009243538,0.0002461253,0.00010300977,0.0033619602],"category_scores_gemma":[0.0002874109,0.00010682416,0.000047490747,0.00029870745,0.000453199,0.00010604653,0.000057771475,0.00034061543,0.002472029],"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":[0.000044645636,0.0010835078,0.69447833,0.0000070948545,0.000056252404,0.00029783568,0.0025877915,0.009688402,0.004199961,0.24017446,0.047014475,0.00036725056],"study_design_scores_gemma":[0.00068380387,0.00022678782,0.94039285,0.000004377205,0.000023211192,0.00031899248,0.0004869532,0.0005647136,0.000110052584,0.015010362,0.04197582,0.00020209239],"about_ca_topic_score_codex":0.00014300713,"about_ca_topic_score_gemma":0.0028513258,"teacher_disagreement_score":0.24591452,"about_ca_system_score_codex":0.00009982051,"about_ca_system_score_gemma":0.000012313802,"threshold_uncertainty_score":0.99830467},"labels":[],"label_agreement":null},{"id":"W2139409798","doi":"10.1016/j.geomorph.2004.08.002","title":"Analysis of the distributions of stress in natural ridge forms: implications for the deformation mechanisms of rock slopes and the formation of sackung","year":2004,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":74,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Ridge; Landform; Fault scarp; Stress (linguistics); Deformation (meteorology); Tension (geology); Tectonics; Geotechnical engineering; Geomorphology; Seismology; Compression (physics); Paleontology","score_opus":0.005546524528109145,"score_gpt":0.21794283147447527,"score_spread":0.21239630694636613,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2139409798","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":[0.9300466,0.0000848859,0.067591704,0.0012761594,0.000029997864,0.0003782145,0.0005470976,0.0000016603462,0.000043672],"genre_scores_gemma":[0.99965644,0.000059218313,0.00013750035,0.000021579242,0.0000013446281,0.000022405628,0.000095724296,0.0000015247668,0.000004262828],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99945706,0.000029303616,0.00030101454,0.00005634985,0.00007312377,0.00008311971],"domain_scores_gemma":[0.9993944,0.00010308515,0.00029122762,0.00017669612,0.000027026585,0.0000075588014],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025987593,0.000044990855,0.00015064534,0.000035551384,0.00008669238,0.0000021560313,0.00016346283,0.000047809568,0.000014959137],"category_scores_gemma":[0.000039024984,0.000019317904,0.00008758847,0.00040466434,0.00021910421,0.000083733714,0.00007895401,0.000054300508,2.6360934e-7],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046325807,0.00035500102,0.06798271,0.00013898526,0.00074494525,1.6684085e-7,0.0068536624,0.60967255,0.08671096,0.21906589,0.00014524184,0.007866661],"study_design_scores_gemma":[0.0025942423,0.0001064468,0.84614414,0.000033563436,0.0010215483,0.000017272361,0.0013352088,0.039911658,0.07687014,0.031762805,0.000106998974,0.000095990006],"about_ca_topic_score_codex":0.0006696761,"about_ca_topic_score_gemma":0.0013566514,"teacher_disagreement_score":0.7781614,"about_ca_system_score_codex":0.00003249195,"about_ca_system_score_gemma":0.000008251279,"threshold_uncertainty_score":0.10123544},"labels":[],"label_agreement":null},{"id":"W2142870591","doi":"10.1016/j.geomorph.2003.07.006","title":"Bed load transport in an obstruction-formed pool in a forest, gravelbed stream","year":2003,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":62,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Bed load; Geology; Sediment; River morphology; Sediment transport; Hydrology (agriculture); Bedform; Debris; Flow (mathematics); Stream bed; Large woody debris; Geomorphology; Geotechnical engineering; Riparian zone; Ecology","score_opus":0.009896698484126817,"score_gpt":0.22271841378785143,"score_spread":0.21282171530372462,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2142870591","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":[0.99578106,0.000031108302,0.0001586979,0.00011200729,0.00013395892,0.00023603262,0.0000093931785,0.000029900257,0.003507833],"genre_scores_gemma":[0.99903977,0.000017382137,0.00031332698,0.00034846293,0.000008413899,0.000055989087,0.000076793454,0.000012015662,0.00012786798],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984757,0.000080202946,0.00034876508,0.00043572127,0.00016109664,0.0004985215],"domain_scores_gemma":[0.99959606,0.000031003354,0.000053914606,0.00021377817,0.0000067155474,0.00009851293],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00033184743,0.00016955579,0.00025209846,0.0000848392,0.000054913457,0.0000033983717,0.00019155901,0.00022870446,0.0065628947],"category_scores_gemma":[0.00002271227,0.00016888893,0.00003532534,0.00035142124,0.00029747994,0.00023255,0.000009078918,0.00024731772,0.00016637608],"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":[0.000096945696,0.00022830423,0.99198204,0.0000059319104,0.000004288289,0.00030285196,0.00075025385,0.0035876061,0.0020840955,0.00029226913,0.000027069489,0.0006383644],"study_design_scores_gemma":[0.001955923,0.00022258825,0.9884066,0.0000056697204,0.000012236821,0.00011661773,0.00017285405,0.00013243052,0.0020208384,0.0043957424,0.0023171145,0.00024140252],"about_ca_topic_score_codex":0.0014131507,"about_ca_topic_score_gemma":0.06008524,"teacher_disagreement_score":0.05867209,"about_ca_system_score_codex":0.0001171057,"about_ca_system_score_gemma":0.00005079422,"threshold_uncertainty_score":0.99434525},"labels":[],"label_agreement":null},{"id":"W2149111416","doi":"10.1016/j.geomorph.2012.05.004","title":"Channel morphology and bed-load yield in fluvial, formerly-glaciated headwater streams of the Columbia Mountains, Canada","year":2012,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":21,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Fluvial; STREAMS; Geology; Channel (broadcasting); Geomorphology; Bed load; Hydrology (agriculture); Archaeology; Sediment; Geography; Sediment transport; Geotechnical engineering; Structural basin","score_opus":0.007583162836566877,"score_gpt":0.18676607199314052,"score_spread":0.17918290915657364,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2149111416","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":[0.9976924,0.00019202553,0.000007667145,0.0008100708,0.00030369192,0.00020585486,0.000033641823,0.000009154933,0.00074547896],"genre_scores_gemma":[0.9980243,0.000033228895,0.000014478082,0.0015130062,0.000019353418,0.000024985773,0.000021123924,0.000009479118,0.0003400311],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986806,0.000074682575,0.0002828153,0.0002401101,0.00016443075,0.0005573533],"domain_scores_gemma":[0.9995248,0.00007104796,0.0000932683,0.00021050776,0.000009727961,0.0000907035],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003139962,0.00013336031,0.0002572141,0.000019480958,0.000113885704,0.0000036683798,0.00022672572,0.00018643952,0.0032017557],"category_scores_gemma":[0.000037789592,0.00011506166,0.00002595461,0.00017219369,0.00050526526,0.00012370004,0.00011587417,0.00021296673,0.000023184042],"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":[0.000049138078,0.000110347115,0.98621565,0.000011415127,0.000014346853,0.000025216512,0.00056281965,0.00015308784,0.008228918,0.000011123015,0.004325769,0.00029214003],"study_design_scores_gemma":[0.0010005881,0.00018246126,0.9770325,0.000013598798,0.000037584105,0.00019675985,0.00021378027,0.00006783017,0.011606203,0.00027862765,0.0091104405,0.000259643],"about_ca_topic_score_codex":0.7521805,"about_ca_topic_score_gemma":0.9403244,"teacher_disagreement_score":0.18814392,"about_ca_system_score_codex":0.00012425992,"about_ca_system_score_gemma":0.00008050782,"threshold_uncertainty_score":0.99770945},"labels":[],"label_agreement":null},{"id":"W2152273606","doi":"10.1016/s0169-555x(02)00355-0","title":"Landslide inventory in a rugged forested watershed: a comparison between air-photo and field survey data","year":2003,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":248,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Landslide; Geology; Debris; Hydrology (agriculture); Watershed; Aerial photos; Structural basin; Terrain; Colluvium; Drainage basin; Sediment; Aerial photography; Physical geography; Geomorphology; Remote sensing; Cartography; Geography; Geotechnical engineering","score_opus":0.04122562360235429,"score_gpt":0.27568241778460617,"score_spread":0.23445679418225188,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2152273606","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":[0.9968621,0.00009820759,0.00014093454,0.00017769924,0.0001212037,0.00017369232,0.000067280926,0.000019480945,0.0023393887],"genre_scores_gemma":[0.9985181,0.000036826026,0.0002392305,0.0004064291,0.000012402586,0.0000067941514,0.0004836609,0.000011434181,0.00028511157],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99850625,0.00030056035,0.00027859755,0.00041946548,0.00012289592,0.0003722527],"domain_scores_gemma":[0.9991871,0.00017839987,0.00006644434,0.0004528218,0.0000043040172,0.00011091852],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00091881125,0.00013536058,0.00028974703,0.00004797404,0.00006646505,0.000012939742,0.0003001866,0.00021004955,0.0015534282],"category_scores_gemma":[0.00015894532,0.00010684926,0.000017554716,0.00017155246,0.00013176553,0.0000994906,0.00034070137,0.00027144075,0.00014872334],"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":[0.0000384913,0.000037287715,0.9840801,0.0000040871746,0.000013215834,0.000047294434,0.00022287018,0.000055143053,0.00017075376,0.0000063333623,0.01467699,0.0006474525],"study_design_scores_gemma":[0.0014346567,0.00016127223,0.9483,0.000010355591,0.00002151697,0.000053864434,0.00008107166,0.00046439038,0.0005993135,0.00022689824,0.04841887,0.00022778283],"about_ca_topic_score_codex":0.0079530245,"about_ca_topic_score_gemma":0.015225863,"teacher_disagreement_score":0.035780072,"about_ca_system_score_codex":0.000040092124,"about_ca_system_score_gemma":0.000012755602,"threshold_uncertainty_score":0.9993593},"labels":[],"label_agreement":null},{"id":"W2157143137","doi":"10.1016/j.geomorph.2012.07.012","title":"Winter variability of aeolian sediment transport threshold on a cold-climate dune","year":2012,"lang":"en","type":"article","venue":"Geomorphology","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary; University of Lethbridge","funders":"Alberta Innovates; University of Lethbridge","keywords":"Aeolian processes; Wind speed; Snow; Environmental science; Relative humidity; Atmospheric sciences; Snowmelt; Geology; Sediment transport; Spatial variability; Sediment; Climatology; Meteorology; Geomorphology; Oceanography","score_opus":0.010978207378244493,"score_gpt":0.2147213049898736,"score_spread":0.20374309761162912,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2157143137","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":[0.98758787,0.00016597068,0.000109433924,0.00030204945,0.00065351324,0.00019776695,0.00020734705,0.000027990023,0.010748038],"genre_scores_gemma":[0.99864525,0.000023714063,0.00019537096,0.00076503074,0.00012261943,0.0000029295827,0.0001180067,0.000004398147,0.00012266435],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99875444,0.00006204127,0.0002459025,0.00022493565,0.00015725239,0.00055542187],"domain_scores_gemma":[0.999355,0.00011186034,0.00008954327,0.0002461113,0.00002825905,0.0001692301],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00066970853,0.00014534709,0.00027096568,0.000047281625,0.00006342725,0.0000036191102,0.00016108915,0.00011501086,0.008308465],"category_scores_gemma":[0.000015403004,0.00011450708,0.00007100002,0.00012184737,0.00016259757,0.00010664518,0.000010497685,0.00013882309,0.00053972955],"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":[0.00015947556,0.00010299004,0.9965645,0.000082738676,0.000020356512,0.000021313957,0.00027664873,0.0006494957,0.00026004482,0.00046337082,0.0008170848,0.0005819667],"study_design_scores_gemma":[0.0005472755,0.0005863582,0.9862009,0.000025769139,0.000039553834,0.000058851594,0.000048746802,0.00071185245,0.0025319497,0.0003356013,0.008716731,0.0001963802],"about_ca_topic_score_codex":0.00033377207,"about_ca_topic_score_gemma":0.00023260729,"teacher_disagreement_score":0.011057376,"about_ca_system_score_codex":0.0000045648703,"about_ca_system_score_gemma":0.00002405558,"threshold_uncertainty_score":0.99259806},"labels":[],"label_agreement":null},{"id":"W2158724055","doi":"10.1016/s0169-555x(03)00146-6","title":"Advances in Holocene mountain geomorphology inspired by sediment budget methodology","year":2003,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"National Science Foundation","keywords":"Geology; Varve; Sediment; Sedimentation; Sedimentary budget; Glacial period; Holocene; Fluvial; Geomorphology; Glacier; Weathering; Structural basin; Drainage basin; Hydrology (agriculture); Physical geography; Geochemistry; Sediment transport; Oceanography","score_opus":0.028024330931476292,"score_gpt":0.2821449821044697,"score_spread":0.25412065117299343,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2158724055","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":[0.9681561,0.0121017685,0.0007002993,0.0015209572,0.0009996743,0.00040438175,0.00016372057,0.00006429242,0.015888808],"genre_scores_gemma":[0.9915754,0.00185486,0.0028207079,0.0023309428,0.000035703644,0.000025248495,0.0008684667,0.000010525831,0.000478149],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9938328,0.0029574966,0.00061225466,0.0008848733,0.0002111466,0.001501405],"domain_scores_gemma":[0.9972832,0.0017685009,0.00017564921,0.00046296944,0.00007194237,0.00023769279],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0025370966,0.0003569785,0.0007899899,0.00038448308,0.00021818726,0.00001377908,0.0005246484,0.0007049484,0.01850778],"category_scores_gemma":[0.00076129474,0.00033334855,0.000082520455,0.0005487065,0.0011487892,0.00020647587,0.000041144376,0.00081337016,0.0017543188],"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":[0.00021235184,0.00008601138,0.9923752,0.000016783411,0.000022042874,0.0007450222,0.000107962805,0.0005479195,0.00015562384,0.0013532666,0.0022395523,0.0021382761],"study_design_scores_gemma":[0.0076169823,0.0024330064,0.67644215,0.00002208655,0.00006796337,0.00929577,0.00093243265,0.00058781944,0.0047353283,0.03230254,0.26405668,0.0015072252],"about_ca_topic_score_codex":0.0012152635,"about_ca_topic_score_gemma":0.0064788987,"teacher_disagreement_score":0.31593302,"about_ca_system_score_codex":0.0000089872665,"about_ca_system_score_gemma":0.00014427993,"threshold_uncertainty_score":0.99991184},"labels":[],"label_agreement":null},{"id":"W2158789815","doi":"10.1016/j.geomorph.2005.12.008","title":"Airflow and sand transport variations within a backshore–parabolic dune plain complex: NE Graham Island, British Columbia, Canada","year":2006,"lang":"en","type":"article","venue":"Geomorphology","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":72,"is_retracted":false,"has_abstract":false,"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","keywords":"Foredune; Geology; Beach morphodynamics; Aeolian processes; Sediment transport; Geomorphology; Plage; Sediment; Shore; Oceanography","score_opus":0.004982299404436133,"score_gpt":0.16743447960070956,"score_spread":0.16245218019627344,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2158789815","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":[0.9934996,0.000639613,0.00041666714,0.0004059233,0.0003480163,0.00022494816,0.0017017372,0.000032980453,0.002730511],"genre_scores_gemma":[0.9949959,0.00003771307,0.00048117898,0.00087956636,0.00015219914,0.000004340449,0.002022702,0.000006953834,0.0014194339],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998669,0.00006163413,0.0002866643,0.0003583479,0.00017145406,0.00045288116],"domain_scores_gemma":[0.99947315,0.00010468645,0.00008950631,0.00013780154,0.000042411284,0.00015245241],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000174586,0.0001342129,0.00030869688,0.000028208053,0.00034629522,0.00009043653,0.00014069957,0.00011257608,0.0057543763],"category_scores_gemma":[0.000015656624,0.0001780194,0.000029700981,0.00021344607,0.00018127143,0.00009513216,0.000007841529,0.0001588068,0.000029942423],"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":[0.000026699507,0.000023297294,0.91581035,0.000039358423,0.000022051341,0.0006314117,0.00007561689,0.0032125157,0.000027780383,0.000037168254,0.07809845,0.0019952827],"study_design_scores_gemma":[0.00075724116,0.00010664431,0.9661326,0.000012229322,0.000030719526,0.0010357158,0.00003651834,0.007638045,0.000004367021,0.0010316371,0.022978459,0.0002358148],"about_ca_topic_score_codex":0.9922007,"about_ca_topic_score_gemma":0.999777,"teacher_disagreement_score":0.055119995,"about_ca_system_score_codex":0.000007462933,"about_ca_system_score_gemma":0.0002591555,"threshold_uncertainty_score":0.9951545},"labels":[],"label_agreement":null},{"id":"W2205974339","doi":"10.1016/j.geomorph.2015.05.029","title":"Little Ice Age debris lobes and nivation hollows inside Ubehebe Crater, Death Valley, California: Analog for Mars craters?","year":2015,"lang":"en","type":"article","venue":"Geomorphology","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":4,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; The Scarborough Hospital","funders":"Natural Sciences and Engineering Research Council of Canada; Vedecká Grantová Agentúra MŠVVaŠ SR a SAV; Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; University of Nevada, Las Vegas","keywords":"Geology; Impact crater; Ejecta; Geomorphology; Debris; Rock glacier; Maar; Glacier; Mass wasting; Snow; Bedrock; Volcano; Paleontology; Landslide; Oceanography","score_opus":0.04083076251891837,"score_gpt":0.2527389822650734,"score_spread":0.21190821974615504,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2205974339","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":[0.9817732,0.00005427931,0.01610359,0.00065527495,0.00022577951,0.00022202548,0.0002716372,0.000021919619,0.000672323],"genre_scores_gemma":[0.9949055,0.000006123511,0.001270917,0.0004052474,0.0001664264,0.00003406262,0.0028077743,0.00000887534,0.00039511643],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991485,0.000045140518,0.00017992157,0.00026869815,0.00008567169,0.0002720548],"domain_scores_gemma":[0.9995471,0.000047950325,0.000076808996,0.00014202899,0.000071575865,0.00011448481],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020523883,0.00012708931,0.00018287085,0.0000508508,0.00011033368,0.00005662159,0.000101718586,0.000060238443,0.00006992881],"category_scores_gemma":[0.00001514888,0.00011525463,0.000032968823,0.000093680595,0.000070114045,0.0002701896,0.000037838854,0.0000716644,0.00019693984],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00051812705,0.0003847965,0.8157123,0.00005227957,0.0002381506,0.00016914224,0.0030604813,0.003944597,0.020525435,0.0071009654,0.12898399,0.019309746],"study_design_scores_gemma":[0.012300212,0.0025074123,0.1886117,0.00007690102,0.0004482752,0.00020234466,0.005915091,0.027406134,0.011028251,0.16603205,0.5828998,0.0025718287],"about_ca_topic_score_codex":0.0011507239,"about_ca_topic_score_gemma":0.00023853066,"teacher_disagreement_score":0.6271006,"about_ca_system_score_codex":0.000015639147,"about_ca_system_score_gemma":0.00004784528,"threshold_uncertainty_score":0.46999475},"labels":[],"label_agreement":null},{"id":"W2212460758","doi":"10.1016/j.geomorph.2015.09.026","title":"Self-organizing change? On drivers, causes and global environmental change","year":2015,"lang":"en","type":"article","venue":"Geomorphology","topic":"Ecosystem dynamics and resilience","field":"Environmental Science","cited_by":5,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Equifinality; Environmental change; Self-organization; Process (computing); Catastrophe theory; Computer science; Lead (geology); Risk analysis (engineering); Environmental resource management; Climate change; Geology; Environmental science; Business; Artificial intelligence","score_opus":0.02495813945100135,"score_gpt":0.22019973693960349,"score_spread":0.19524159748860215,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2212460758","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":[0.9965809,0.00016558792,0.00001288268,0.0004129495,0.0004511239,0.0002541603,0.000061224506,0.000044095847,0.0020170924],"genre_scores_gemma":[0.99833935,0.00013172188,0.0003126779,0.0009477617,0.00014744143,0.000022594415,0.000015758742,0.000009711293,0.00007297952],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990094,0.000049963317,0.00010570525,0.00034913607,0.00017628158,0.000309542],"domain_scores_gemma":[0.99955446,0.00001460433,0.000057535257,0.00018276916,0.0000019158404,0.00018870317],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00013314218,0.00013615692,0.00013906838,0.000017740853,0.000094694515,0.000013886269,0.0001580777,0.00009905997,0.00037016318],"category_scores_gemma":[0.000008077121,0.00012166504,0.000018274164,0.00008542411,0.00017650337,0.00012313813,0.00030856265,0.0000753582,0.0011593057],"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":[0.000013961049,0.0001103769,0.99483746,0.0000062103086,0.000010337357,0.00016004252,0.0011645752,0.000014343729,0.00068088504,0.00025879694,0.0013328021,0.0014102024],"study_design_scores_gemma":[0.0018324587,0.0011278942,0.89971495,0.000025378979,0.000050746934,0.0011270429,0.0016144135,0.003844809,0.00032928807,0.00050693913,0.089062296,0.00076379156],"about_ca_topic_score_codex":0.0006165316,"about_ca_topic_score_gemma":0.00053005054,"teacher_disagreement_score":0.09512252,"about_ca_system_score_codex":0.00027060683,"about_ca_system_score_gemma":0.000004160734,"threshold_uncertainty_score":0.9996184},"labels":[],"label_agreement":null},{"id":"W2282654770","doi":"10.1016/j.geomorph.2016.02.014","title":"Coastal erosion and mass wasting along the Canadian Beaufort Sea based on annual airborne LiDAR elevation data","year":2016,"lang":"en","type":"article","venue":"Geomorphology","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":94,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Progradation; Geology; Mass wasting; Slumping; Erosion; Permafrost; Coastal erosion; Elevation (ballistics); Aggradation; Accretion (finance); Physical geography; Landform; Digital elevation model; Sea level; Bathymetry; Sediment; Geomorphology; Oceanography; Hydrology (agriculture); Remote sensing; Fluvial; Geography; Sedimentary depositional environment","score_opus":0.043411156076611127,"score_gpt":0.2378087900257106,"score_spread":0.19439763394909948,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2282654770","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":[0.9547869,0.00011678827,0.00014650788,0.0075770295,0.00037650537,0.00016499849,0.03608692,0.00001932989,0.0007250478],"genre_scores_gemma":[0.9874919,0.00004422116,0.000053425505,0.0018692946,0.00016658715,0.0000010395621,0.010292658,0.000004171955,0.00007668726],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99899846,0.00008776002,0.00013161941,0.00028899548,0.00013381247,0.00035933426],"domain_scores_gemma":[0.99907804,0.00035090194,0.000052872634,0.00033661159,0.000034985762,0.00014657457],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005809892,0.0001063905,0.00010432253,0.00007075734,0.00035695426,0.000035980454,0.00024461435,0.000090107584,0.003596677],"category_scores_gemma":[0.00010123196,0.00006111769,0.000012680035,0.000090576854,0.00014938222,0.0001545982,0.000026714843,0.00010158594,0.00019088284],"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":[0.000028648406,0.0000031268928,0.983416,0.000004895433,0.0000030498252,0.00005087488,0.00006518436,0.00003938383,0.00042652953,0.0000066605744,0.0049648983,0.010990729],"study_design_scores_gemma":[0.00037980254,0.00014280877,0.9630245,0.000030231735,0.000011192674,0.000054883334,0.00011529585,0.010493731,0.000078563164,0.000033984834,0.02550754,0.0001274888],"about_ca_topic_score_codex":0.33815148,"about_ca_topic_score_gemma":0.96184444,"teacher_disagreement_score":0.6236929,"about_ca_system_score_codex":0.0000073825786,"about_ca_system_score_gemma":0.00010446862,"threshold_uncertainty_score":0.99731416},"labels":[],"label_agreement":null},{"id":"W2290433392","doi":"10.1016/j.geomorph.2016.02.029","title":"The Holocene deglaciation of the Byers Peninsula (Livingston Island, Antarctica) based on the dating of lake sedimentary records","year":2016,"lang":"en","type":"article","venue":"Geomorphology","topic":"Polar Research and Ecology","field":"Environmental Science","cited_by":61,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval; Center for Northern Studies","funders":"Office of Polar Programs; AXA Research Fund","keywords":"Deglaciation; Geology; Glacier; Holocene; Oceanography; Peninsula; Glacial period; Physical geography; Sedimentary rock; Paleontology; Archaeology; Geography","score_opus":0.008764239054854892,"score_gpt":0.2151045583053766,"score_spread":0.2063403192505217,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2290433392","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":[0.9883015,0.000007957675,0.0001331864,0.008514424,0.00017944869,0.00022465317,0.000060787854,0.0000054467173,0.0025725937],"genre_scores_gemma":[0.99857235,0.000024633087,0.000058207108,0.00086940546,0.000020474787,0.000016581904,0.000007022451,0.0000074047744,0.0004238965],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986097,0.00039775373,0.00020859366,0.00018325605,0.0002586875,0.00034195965],"domain_scores_gemma":[0.99825555,0.0010912598,0.00016602271,0.00043514775,0.000013562887,0.000038476577],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011596644,0.00008556745,0.000118087075,0.00002003676,0.00025743715,0.0000051582792,0.00050489034,0.000061822655,0.005917361],"category_scores_gemma":[0.00064669584,0.000035341225,0.00005832608,0.00014623994,0.0008355624,0.000047429767,0.0002525653,0.00014417764,0.00011308126],"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":[0.00020997865,0.00009061443,0.92989975,0.0000044129906,0.000023536242,0.0000045843585,0.00011452956,0.0001597352,0.046638854,0.0001307923,0.017110422,0.0056127775],"study_design_scores_gemma":[0.00097214815,0.0006299734,0.93922406,0.00002843888,0.000021702393,0.000025165775,0.00016064613,0.0019763915,0.04183258,0.0005941162,0.014411967,0.00012280396],"about_ca_topic_score_codex":0.00088521314,"about_ca_topic_score_gemma":0.002719012,"teacher_disagreement_score":0.010270872,"about_ca_system_score_codex":0.00007563904,"about_ca_system_score_gemma":0.000029381965,"threshold_uncertainty_score":0.99499136},"labels":[],"label_agreement":null},{"id":"W2300704508","doi":"10.1016/j.geomorph.2016.03.019","title":"Downstream channel adjustment in a low-relief, glacially conditioned watershed","year":2016,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":25,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"University of Toronto","keywords":"Geology; Fluvial; Channel (broadcasting); Channelized; Tributary; Watershed; Downstream (manufacturing); Hydrology (agriculture); Glacial period; Geomorphology; Sediment; Glacier; Structural basin; Geotechnical engineering; Geography","score_opus":0.006527820205467826,"score_gpt":0.20209048514041056,"score_spread":0.19556266493494273,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2300704508","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":[0.9927451,0.000034119377,0.00068507466,0.0027599912,0.00022908753,0.00020787447,0.000030449843,0.00005125218,0.0032570765],"genre_scores_gemma":[0.9973461,0.00006583247,0.000057241738,0.001502026,0.00003718527,0.00007564537,0.00006825916,0.000009809663,0.0008378762],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987233,0.000057675174,0.0002502802,0.0003885302,0.00012758556,0.0004526078],"domain_scores_gemma":[0.99961513,0.00004558809,0.000055514858,0.00019071507,0.0000059114777,0.000087155575],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00018391424,0.00015097833,0.00020048376,0.000058334965,0.000061906525,0.0000029954224,0.00020156191,0.00016635784,0.022909384],"category_scores_gemma":[0.00001650472,0.000103833816,0.00003814101,0.0001251315,0.00041138526,0.00014703255,0.000057751506,0.00008710834,0.0033577492],"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":[0.0018210538,0.003063752,0.57684755,0.00008257802,0.0001554458,0.0025545415,0.0037946035,0.0030698779,0.35683665,0.0017412821,0.025280787,0.024751883],"study_design_scores_gemma":[0.011851859,0.0012882312,0.87645984,0.000102806276,0.00007214141,0.00030251202,0.00012757939,0.00012293678,0.06411589,0.013101265,0.031324364,0.0011305712],"about_ca_topic_score_codex":0.0002380383,"about_ca_topic_score_gemma":0.00080842874,"teacher_disagreement_score":0.29961228,"about_ca_system_score_codex":0.000084831496,"about_ca_system_score_gemma":0.0000151908425,"threshold_uncertainty_score":0.9974182},"labels":[],"label_agreement":null},{"id":"W2301518653","doi":"10.1016/j.geomorph.2016.01.011","title":"Changes in the areal extents of the Athabasca River, Birch River, and Cree Creek Deltas, 1950–2014, Peace–Athabasca Delta, Canada","year":2016,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"World Wildlife Fund Canada","funders":"","keywords":"Progradation; Delta; Geology; Sediment; River delta; Hydrology (agriculture); Subaerial; Geomorphology; Geochemistry; Facies; Structural basin","score_opus":0.015538646295372624,"score_gpt":0.21574996129264204,"score_spread":0.2002113149972694,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2301518653","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":[0.9902061,0.0018228367,0.0000112839525,0.0059344806,0.00038668606,0.00029162224,0.00054314634,0.000008106281,0.000795698],"genre_scores_gemma":[0.9979743,0.00075508404,0.000056497964,0.000750215,0.00004269286,0.000008037906,0.00007045105,0.0000040262576,0.00033872155],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99760884,0.0007604604,0.0002456033,0.0003910423,0.00030878067,0.0006852782],"domain_scores_gemma":[0.99808735,0.0011512559,0.00012776542,0.00046296368,0.00006995818,0.00010071387],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00081571046,0.00017787404,0.00031318926,0.000093702765,0.000276237,0.000009979097,0.00081020774,0.0001974871,0.0019023343],"category_scores_gemma":[0.00018537608,0.00009492598,0.000048341473,0.0002208531,0.0015768571,0.0000671436,0.00010422133,0.0003221033,0.000070137794],"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":[0.000078142744,0.00001965661,0.9888872,0.000013803457,0.000022077062,0.00018869547,0.00032026946,0.0000068055197,0.0000156113,0.000039770737,0.0073331622,0.0030747973],"study_design_scores_gemma":[0.0007592077,0.00017786637,0.99123585,0.000020162606,0.000017970646,0.0006464923,0.00021073269,0.00007009624,0.000053910382,0.00047517556,0.006206474,0.00012603092],"about_ca_topic_score_codex":0.7289354,"about_ca_topic_score_gemma":0.99454826,"teacher_disagreement_score":0.26561287,"about_ca_system_score_codex":0.0000047971666,"about_ca_system_score_gemma":0.0002590515,"threshold_uncertainty_score":0.9990101},"labels":[],"label_agreement":null},{"id":"W2515129706","doi":"10.1016/j.geomorph.2016.09.002","title":"Quaternary history and landscape evolution of a high-altitude intermountain basin at the western end of the Himalayan-Tibetan orogen, Waqia Valley, Chinese Pamir","year":2016,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Science Foundation","keywords":"Geology; Moraine; Glacial period; Quaternary; Landform; Outwash plain; Glacial landform; Alluvial fan; Geomorphology; River terraces; Surface exposure dating; Terminal moraine; Holocene; Alluvium; Paleontology; Fluvial; Physical geography; Structural basin; Geography","score_opus":0.009427242190813291,"score_gpt":0.21218187315120215,"score_spread":0.20275463096038887,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2515129706","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":[0.99298596,0.002533911,0.000022803826,0.003221545,0.00044661787,0.00018006159,0.00010586493,0.000010139468,0.00049309904],"genre_scores_gemma":[0.99821067,0.00016244537,0.000018591354,0.00019675383,0.000033809505,0.000003473267,0.0000307941,0.000003822572,0.0013396452],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99832517,0.0006079908,0.0002910602,0.00027264666,0.00016407203,0.00033906303],"domain_scores_gemma":[0.99868387,0.00061549555,0.00019191115,0.00039572196,0.00005463627,0.000058347166],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00062345085,0.00014609695,0.0003118226,0.00008001781,0.00011964646,0.0000024923277,0.00043341337,0.00017603918,0.0030752849],"category_scores_gemma":[0.0000914903,0.00006581102,0.00006956229,0.000088425855,0.0017091274,0.000063132895,0.00013811409,0.00017239738,0.00016893049],"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":[0.00025864362,0.000019953563,0.9969997,0.000023255445,0.000047741698,0.000027846405,0.000224119,0.00001070429,0.0009495129,0.00008833725,0.00095532194,0.00039489818],"study_design_scores_gemma":[0.00066828215,0.00020494814,0.9959965,0.000017393453,0.000023351262,0.00062429113,0.000035171684,0.000056528846,0.0001909205,0.00053781795,0.0015638173,0.00008100799],"about_ca_topic_score_codex":0.0034388031,"about_ca_topic_score_gemma":0.031911347,"teacher_disagreement_score":0.028472543,"about_ca_system_score_codex":0.000011956249,"about_ca_system_score_gemma":0.000094751806,"threshold_uncertainty_score":0.99783605},"labels":[],"label_agreement":null},{"id":"W2554992362","doi":"10.1016/j.geomorph.2016.11.007","title":"Fluvial fluxes from the Magdalena River into Cartagena Bay, Caribbean Colombia: Trends, future scenarios, and connections with upstream human impacts","year":2016,"lang":"en","type":"article","venue":"Geomorphology","topic":"Coastal and Marine Dynamics","field":"Earth and Planetary Sciences","cited_by":61,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"International Development Research Centre","keywords":"Bay; Fluvial; Estuary; Sediment; Geology; Surface runoff; Hydrology (agriculture); Drainage basin; Discharge; Sediment transport; Oceanography; Structural basin; Geomorphology; Geography; Ecology","score_opus":0.005233514778150067,"score_gpt":0.18922565302352803,"score_spread":0.18399213824537797,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2554992362","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":[0.99151313,0.00024150517,0.00003531075,0.0049885195,0.0004339731,0.000121732526,0.0012492051,0.00004965233,0.0013669765],"genre_scores_gemma":[0.99710584,0.00009442534,0.00012535896,0.0003922766,0.00041756636,0.000002502854,0.00065327826,0.0000068250124,0.0012019009],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99889016,0.00010685394,0.00015544,0.0003575741,0.0001223856,0.00036760047],"domain_scores_gemma":[0.99922585,0.00022052812,0.00007618717,0.00027706515,0.000041074934,0.00015929247],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000107355896,0.00019885469,0.00022072838,0.000059531158,0.00047117702,0.00004251375,0.00020147908,0.00011817871,0.0032795263],"category_scores_gemma":[0.00001802572,0.00009952712,0.000044744178,0.00014059321,0.0005875964,0.00012906904,0.000066290544,0.00017042934,0.00007623046],"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":[0.00015335043,0.000027966544,0.8962081,0.0000043865207,0.000084264524,0.00011775627,0.00092421577,0.000020792406,0.0006807086,0.00030780668,0.008393937,0.09307672],"study_design_scores_gemma":[0.001130551,0.0006296577,0.9555051,0.000011814876,0.0000742508,0.0002214655,0.00046850636,0.00006751877,0.000043629465,0.0014165994,0.04020046,0.00023048148],"about_ca_topic_score_codex":0.06415563,"about_ca_topic_score_gemma":0.55639595,"teacher_disagreement_score":0.4922403,"about_ca_system_score_codex":0.000008634264,"about_ca_system_score_gemma":0.000048070924,"threshold_uncertainty_score":0.9976316},"labels":[],"label_agreement":null},{"id":"W2593543223","doi":"10.1016/j.geomorph.2017.12.011","title":"Scale-dependent behavior of the foredune: Implications for barrier island response to storms and sea-level rise","year":2017,"lang":"en","type":"article","venue":"Geomorphology","topic":"Coastal and Marine Dynamics","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Windsor","funders":"National Science Foundation","keywords":"Foredune; Barrier island; Storm; Scale (ratio); Sea level rise; Geology; Environmental science; Oceanography; Geography; Climate change; Shore; Cartography","score_opus":0.02113992342705257,"score_gpt":0.2572168844251856,"score_spread":0.23607696099813302,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2593543223","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":[0.9902537,0.000019878857,0.00043104962,0.0024479278,0.00030592334,0.00041702282,0.0058713946,0.000005730263,0.00024736914],"genre_scores_gemma":[0.9957667,0.0000075474186,0.00040677204,0.00012899582,0.000025865322,0.00001727401,0.000059470305,0.0000028628983,0.0035845137],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994353,0.00003191576,0.000121368554,0.0001731498,0.000057159294,0.00018108803],"domain_scores_gemma":[0.9992552,0.00010422131,0.00008523551,0.00041449023,0.000051499985,0.00008939811],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026556916,0.000073816766,0.00011913822,0.000031403157,0.000363897,0.000026925256,0.00031035068,0.000054556447,0.00019355906],"category_scores_gemma":[0.0001421821,0.00004446086,0.000040200543,0.000026870992,0.00019744685,0.000055616092,0.0001063363,0.000057810008,0.000009268874],"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":[0.00032513138,0.000012733897,0.94425285,0.0000057301745,0.0000052645482,0.0000016271505,0.000098133954,0.000025088037,0.0011646353,0.000025977117,0.0008908945,0.05319195],"study_design_scores_gemma":[0.00036399605,0.00015095927,0.9919883,0.0000028304112,0.000023593468,0.000064383756,0.0000343344,0.00014778461,0.00014320637,0.0006980713,0.006313163,0.000069381844],"about_ca_topic_score_codex":0.0034575,"about_ca_topic_score_gemma":0.08217843,"teacher_disagreement_score":0.07872093,"about_ca_system_score_codex":0.0000026484988,"about_ca_system_score_gemma":0.00004705521,"threshold_uncertainty_score":0.9345694},"labels":[],"label_agreement":null},{"id":"W2601100706","doi":"10.1016/j.geomorph.2017.03.023","title":"An investigation into the development of toppling at the edge of fractured rock plateaux using a numerical modelling approach","year":2017,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":49,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Geology; Classification of discontinuities; Instability; Groundwater; Landslide; Fracture (geology); Discontinuity (linguistics); Geotechnical engineering; Slab; Groundwater flow; Aquifer; Geophysics; Mechanics","score_opus":0.03290176803461803,"score_gpt":0.26207922388385535,"score_spread":0.22917745584923732,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2601100706","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":[0.91783863,0.00004199337,0.08156916,0.00012587807,0.00007703187,0.00011857197,0.0000012785276,0.0000046924474,0.0002227385],"genre_scores_gemma":[0.982691,0.0000049514324,0.017149864,0.00005706186,0.000020263125,0.000004966172,0.000012628848,0.0000073444307,0.000051944007],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99921924,0.00005369192,0.00023929567,0.0001815213,0.00015126872,0.00015496959],"domain_scores_gemma":[0.99926007,0.000030063435,0.00026702756,0.00039241082,0.000010162003,0.000040250827],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039968602,0.00008506539,0.00014023777,0.000011189754,0.00064336666,0.000013434729,0.00039082768,0.00011319866,0.00017342369],"category_scores_gemma":[0.000012476211,0.00004397895,0.000031819956,0.00004384592,0.00027440148,0.000074081356,0.00026930257,0.00014219772,0.000013406362],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004166071,0.00003644592,0.022031689,0.00000729638,0.000024701532,0.0000015310062,0.01584453,0.91886824,0.041090373,0.00003164959,0.000044982342,0.0019768863],"study_design_scores_gemma":[0.0003804312,0.000050711944,0.019809434,0.000014229343,0.000043572047,0.000036317386,0.00056148984,0.94348055,0.033336893,0.000949434,0.0011795216,0.00015743909],"about_ca_topic_score_codex":0.0011411046,"about_ca_topic_score_gemma":0.000075033524,"teacher_disagreement_score":0.06485231,"about_ca_system_score_codex":0.00006352614,"about_ca_system_score_gemma":0.00002639004,"threshold_uncertainty_score":0.4948321},"labels":[],"label_agreement":null},{"id":"W2606414509","doi":"10.1016/j.geomorph.2017.04.017","title":"The role of topography in the scaling distribution of landslide areas: A cellular automata modeling approach","year":2017,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":35,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Saint Mary's University","funders":"","keywords":"Landslide; Scaling; Geology; Exponent; Cellular automaton; Scale invariance; Instability; Power law; Hazard; Statistical physics; Stability (learning theory); Geometry; Seismology; Physics; Mechanics; Statistics; Mathematics; Computer science; Algorithm","score_opus":0.007926416560531198,"score_gpt":0.21081297713331068,"score_spread":0.20288656057277948,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2606414509","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":[0.99278235,0.00022878134,0.0029313182,0.00018865627,0.00005756012,0.00012427814,0.000021056521,0.0000057606117,0.003660219],"genre_scores_gemma":[0.99967515,0.000085483734,0.00014922692,0.000012967176,0.0000129491145,0.000008824687,0.00003954741,0.0000038060427,0.000012043969],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9992326,0.00007330329,0.00020775212,0.00014142385,0.00015283466,0.00019208853],"domain_scores_gemma":[0.99928045,0.000042871663,0.00015080028,0.0004989295,0.000007773933,0.000019174444],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006933228,0.000069177586,0.00012898394,0.000012739779,0.0002646377,0.000019651901,0.00055779185,0.00009076066,0.000027095912],"category_scores_gemma":[0.000041969048,0.00003555907,0.000064050946,0.00007331165,0.0003216492,0.000049157177,0.00016820448,0.0001379251,0.0000055538694],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000262524,0.0005372117,0.8496713,0.000034724468,0.00009266436,0.000042763524,0.003356456,0.089713685,0.017840466,0.005837065,0.0005272205,0.032083895],"study_design_scores_gemma":[0.0019831806,0.00019213292,0.21386236,0.000060434373,0.000112477726,0.0001310999,0.0033540914,0.74349844,0.0050339745,0.01803657,0.01336828,0.0003669463],"about_ca_topic_score_codex":0.0018442727,"about_ca_topic_score_gemma":0.00007234236,"teacher_disagreement_score":0.65378475,"about_ca_system_score_codex":0.000014472436,"about_ca_system_score_gemma":0.0000059863733,"threshold_uncertainty_score":0.2788001},"labels":[],"label_agreement":null},{"id":"W2619183179","doi":"10.1016/j.geomorph.2017.05.016","title":"Semi-automatic mapping of linear-trending bedforms using ‘Self-Organizing Maps’ algorithm","year":2017,"lang":"en","type":"article","venue":"Geomorphology","topic":"Remote Sensing and LiDAR Applications","field":"Environmental Science","cited_by":31,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Mars Exploration Program; Computer science; Remote sensing; Automation; Artificial intelligence; Self-organizing map; Photogrammetry; Artificial neural network; Satellite; Algorithm; Satellite imagery; Earth observation; Geology","score_opus":0.022318497899988684,"score_gpt":0.26243842216935387,"score_spread":0.24011992426936518,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2619183179","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":[0.96996665,0.000016108057,0.024582604,0.00022874406,0.00021116961,0.00014156637,0.000013286125,0.00008038515,0.004759508],"genre_scores_gemma":[0.87984526,0.000008608276,0.11976369,0.00008355593,0.00006365619,0.000001110739,0.000016154283,0.000021195412,0.00019679005],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99889976,0.000031278552,0.00028807807,0.000290398,0.00016012897,0.00033034149],"domain_scores_gemma":[0.9988396,0.0000551014,0.00034082698,0.00067567476,0.000013101148,0.00007566555],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000280031,0.000134851,0.00023536647,0.00005479148,0.0006614992,0.00003441041,0.00038264893,0.00011241886,0.0005227903],"category_scores_gemma":[0.00007600311,0.0001286832,0.000057800295,0.0001201784,0.00029834345,0.00013913626,0.00032833638,0.00014710463,0.00030391105],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000072444855,0.00035016748,0.1589402,0.000096583855,0.000172182,0.00016365078,0.0056888205,0.0022249965,0.50096494,0.00021304244,0.0034093033,0.3277689],"study_design_scores_gemma":[0.0018564614,0.00016134705,0.30434164,0.00021656576,0.00020355222,0.0014694214,0.0014488726,0.5882041,0.06120982,0.0030706213,0.036537874,0.0012797574],"about_ca_topic_score_codex":0.0011894437,"about_ca_topic_score_gemma":0.00002800454,"teacher_disagreement_score":0.58597904,"about_ca_system_score_codex":0.00010373436,"about_ca_system_score_gemma":0.000014578336,"threshold_uncertainty_score":0.5724187},"labels":[],"label_agreement":null},{"id":"W267719140","doi":"10.1016/j.geomorph.2015.05.013","title":"Freedom space for rivers: An economically viable river management concept in a changing climate","year":2015,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Watershed Management Studies","field":"Environmental Science","cited_by":106,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ouranos; Université du Québec à Montréal; Concordia University; Université du Québec à Rimouski","funders":"","keywords":"Riparian zone; Wetland; Flood myth; Flooding (psychology); River management; Flood stage; Environmental science; Cost–benefit analysis; Hydrology (agriculture); Ecosystem services; Ecosystem; Environmental resource management; Geology; Geography; Ecology; Habitat","score_opus":0.017011087248538594,"score_gpt":0.23026354755981057,"score_spread":0.21325246031127199,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W267719140","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":[0.9685487,0.000038093753,0.0062099854,0.0020310883,0.0005499588,0.0008851343,0.000034194338,0.00007402844,0.021628814],"genre_scores_gemma":[0.9867422,0.00003330806,0.00989966,0.0013962714,0.0000491271,0.00013985694,0.000055063858,0.000015485048,0.0016690032],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99865097,0.00005582308,0.0001600657,0.00039929218,0.000060377453,0.00067348394],"domain_scores_gemma":[0.99961257,0.000026007847,0.000058366302,0.00021227401,0.0000048156785,0.00008594319],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005397675,0.00013305474,0.00020348908,0.00012258312,0.0001202323,0.000009557054,0.00023207748,0.00007501594,0.0005627448],"category_scores_gemma":[0.000009702475,0.00013323942,0.00003173929,0.00012815213,0.0004106679,0.00019408668,0.00057649316,0.00006641001,0.0006771816],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014245007,0.0010327431,0.51512164,0.00008672158,0.00036336223,0.0009889016,0.024742197,0.28109545,0.0005348154,0.058778025,0.107337594,0.008494095],"study_design_scores_gemma":[0.025792073,0.0030705582,0.102984376,0.000049024715,0.00033922066,0.00008078611,0.0109341545,0.06067261,0.0007299634,0.0587871,0.7342652,0.0022949458],"about_ca_topic_score_codex":0.00026478953,"about_ca_topic_score_gemma":0.00024231402,"teacher_disagreement_score":0.6269276,"about_ca_system_score_codex":0.00013200864,"about_ca_system_score_gemma":0.000002425646,"threshold_uncertainty_score":0.8704025},"labels":[],"label_agreement":null},{"id":"W2742182798","doi":"10.1016/j.geomorph.2017.08.008","title":"Simulating bank erosion over an extended natural sinuous river reach using a universal slope stability algorithm coupled with a morphodynamic model","year":2017,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":25,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Concordia University","funders":"Fonds de recherche du Québec – Nature et technologies; Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Bank erosion; Stability (learning theory); Geotechnical engineering; Hydrology (agriculture); Erosion; Hydrostatic equilibrium; Floodplain; Natural (archaeology); Flow (mathematics); Vegetation (pathology); Geomorphology; Geometry; Computer science","score_opus":0.01772534467101677,"score_gpt":0.25410224066398546,"score_spread":0.23637689599296868,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2742182798","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":[0.9676678,0.00001780619,0.031492446,0.000066580214,0.00012284686,0.00027114895,0.000038816168,0.00007048885,0.00025207055],"genre_scores_gemma":[0.9793028,0.000006131537,0.020240067,0.00019307628,0.000023792996,0.0000057418924,0.00009628787,0.000026387432,0.000105717474],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99807996,0.000088143075,0.00024411171,0.000743928,0.00027951767,0.0005643361],"domain_scores_gemma":[0.9988345,0.000045557204,0.00023083053,0.0007154831,0.000030733536,0.00014288932],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00034763463,0.00027889718,0.0003384425,0.000039994386,0.0008940148,0.000038090715,0.00050673046,0.00022728299,0.0021483386],"category_scores_gemma":[0.000025397754,0.00024114239,0.000052313604,0.000083273,0.0013641767,0.00080082624,0.00019347142,0.00036581373,0.000029974042],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017328656,0.0008999489,0.18042475,0.000032421784,0.00010386294,0.0013350642,0.0029139437,0.5179105,0.28705144,0.000077427125,0.000032679036,0.007485108],"study_design_scores_gemma":[0.0012957178,0.0002726123,0.076279156,0.000009672176,0.00006877651,0.000096842305,0.000049934293,0.92074484,0.00051013264,0.0003519225,0.000020073549,0.00030033],"about_ca_topic_score_codex":0.003542283,"about_ca_topic_score_gemma":0.0015916545,"teacher_disagreement_score":0.40283433,"about_ca_system_score_codex":0.00019583984,"about_ca_system_score_gemma":0.000058205205,"threshold_uncertainty_score":0.99876386},"labels":[],"label_agreement":null},{"id":"W2795074621","doi":"10.1016/j.geomorph.2018.03.027","title":"Evolution of high-Arctic glacial landforms during deglaciation","year":2018,"lang":"en","type":"article","venue":"Geomorphology","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":39,"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":"Natural Environment Research Council; Royal Society; Norsk Polarinstitutt; Trent University; Nottingham Trent University","keywords":"Geology; Moraine; Landform; Deglaciation; Debris; Glacier; Glacial period; Geomorphology; Arctic; Glacial landform; Terminal moraine; Physical geography; Oceanography; Geography","score_opus":0.010845755431306258,"score_gpt":0.20168632944016962,"score_spread":0.19084057400886337,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2795074621","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":[0.9979053,0.00013315002,0.00061328564,0.0001379953,0.0006231204,0.000066173496,0.000044239332,0.00001735847,0.0004593673],"genre_scores_gemma":[0.99900085,0.000013318353,0.00042640948,0.00005310621,0.0002997359,8.582461e-7,0.000083607585,0.000001498726,0.00012061442],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994418,0.000019346991,0.0001526342,0.000121393954,0.0000883974,0.00017644334],"domain_scores_gemma":[0.99966705,0.00003710231,0.000082067054,0.00009856518,0.000087086795,0.000028129858],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00008924301,0.000057578454,0.00011407819,0.000027042779,0.00017116885,0.000004829781,0.00007289957,0.000050290717,0.0047673625],"category_scores_gemma":[0.00005740567,0.000047845908,0.000024951358,0.0001899169,0.0001360129,0.00007082793,0.000011395671,0.000042854113,0.00022933818],"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":[0.00004685736,0.0000073792035,0.99803,0.000007100385,0.000010226902,0.0000020248783,0.00011751243,0.00018891234,0.00012445096,0.00033696764,0.00019386399,0.0009346994],"study_design_scores_gemma":[0.00029224082,0.0001448744,0.9964942,0.0000034225957,0.000010258987,0.000013717934,0.000107057735,0.0004165311,0.00012296851,0.0012495198,0.0010883542,0.000056869227],"about_ca_topic_score_codex":0.014442712,"about_ca_topic_score_gemma":0.020537473,"teacher_disagreement_score":0.0060947607,"about_ca_system_score_codex":0.000010989909,"about_ca_system_score_gemma":0.000021250238,"threshold_uncertainty_score":0.9973352},"labels":[],"label_agreement":null},{"id":"W2807687923","doi":"10.1016/j.geomorph.2018.06.003","title":"Foredune morphodynamics and sediment budgets at seasonal to decadal scales: Humboldt Bay National Wildlife Refuge, California, USA","year":2018,"lang":"en","type":"article","venue":"Geomorphology","topic":"Coastal and Marine Dynamics","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia, Okanagan Campus; University of British Columbia","funders":"U.S. Fish and Wildlife Service; Flinders University; Canada Foundation for Innovation; University of Victoria; Natural Sciences and Engineering Research Council of Canada; Louisiana State University","keywords":"Foredune; Beach morphodynamics; Geology; Oceanography; Shore; Context (archaeology); Bay; Accretion (finance); Sediment transport; Sedimentary budget; Plage; Physical geography; Sediment; Hydrology (agriculture); Geomorphology; Geography","score_opus":0.009154370718108942,"score_gpt":0.2280794501930751,"score_spread":0.21892507947496614,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2807687923","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":[0.99069065,0.00005026703,0.00050734833,0.0014533359,0.00057223043,0.00020898592,0.0020283654,0.00003377111,0.004455065],"genre_scores_gemma":[0.9881784,0.000021312828,0.0028661722,0.0052460525,0.0003711474,0.0000034543757,0.0013934755,0.00000846425,0.0019115336],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99828166,0.00005681668,0.0002661715,0.00048347728,0.00037760846,0.0005342927],"domain_scores_gemma":[0.9991336,0.00012003419,0.00007657368,0.00016577024,0.00013972481,0.0003642903],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0003306776,0.00021557462,0.00024446804,0.00011217792,0.00030682632,0.000035076184,0.00021185592,0.00013218481,0.004559654],"category_scores_gemma":[0.000060648414,0.00019305889,0.000050190283,0.00019265959,0.00039788702,0.00008727341,0.00020156261,0.00013732928,0.0013904441],"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":[0.00039627423,0.000054857228,0.96385545,0.00002029322,0.00005179989,0.00011543637,0.00007883556,0.0010415983,0.00019465107,0.00104035,0.016844986,0.016305497],"study_design_scores_gemma":[0.00074715033,0.000632629,0.69735116,0.000010584598,0.000021811808,0.0009850163,0.00002172841,0.036392305,0.000036581125,0.0019433766,0.2614533,0.00040436734],"about_ca_topic_score_codex":0.0011469855,"about_ca_topic_score_gemma":0.051500883,"teacher_disagreement_score":0.2665043,"about_ca_system_score_codex":0.000034635952,"about_ca_system_score_gemma":0.00009057872,"threshold_uncertainty_score":0.9993871},"labels":[],"label_agreement":null},{"id":"W2891805470","doi":"10.1016/j.geomorph.2018.09.003","title":"A progressive entrainment runout model for debris flow analysis and its application","year":2018,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":16,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Entrainment (biomusicology); Mechanics; Geology; Turbulence; Flow (mathematics); Debris; Physics","score_opus":0.007644969074762704,"score_gpt":0.23872656507809892,"score_spread":0.23108159600333622,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2891805470","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":[0.79310167,0.00012505936,0.20488644,0.00055576855,0.000056591478,0.0005620725,0.00006948753,0.000028821876,0.000614065],"genre_scores_gemma":[0.9945504,0.000021924192,0.0044898866,0.00031960927,0.000037480026,0.00013608564,0.000062998435,0.0000070469446,0.00037457445],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99925125,0.000014112142,0.00012062446,0.00029460364,0.00008863632,0.00023075556],"domain_scores_gemma":[0.9996982,0.000015874748,0.00006267193,0.0001374982,0.000014464023,0.00007127362],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001272171,0.00008375937,0.00013521666,0.0000321714,0.00012793009,0.000008899144,0.00009006436,0.00010160014,0.0008293475],"category_scores_gemma":[0.0000103011125,0.000063967236,0.000049250935,0.00016045952,0.00015302731,0.000037850656,0.000085190724,0.00004459316,0.00012747257],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015872665,0.001388418,0.20709075,0.0000972261,0.003806189,0.00013368986,0.016988887,0.09982751,0.19576775,0.0032813328,0.031385064,0.43864593],"study_design_scores_gemma":[0.00043131367,0.00012581403,0.005453477,0.0000013868148,0.00026259545,0.00002665556,0.000014883677,0.98684233,0.002597451,0.0007618915,0.0033675684,0.00011463315],"about_ca_topic_score_codex":0.00003836962,"about_ca_topic_score_gemma":0.000091385846,"teacher_disagreement_score":0.8870148,"about_ca_system_score_codex":0.000041703737,"about_ca_system_score_gemma":0.0000056201625,"threshold_uncertainty_score":0.90807736},"labels":[],"label_agreement":null},{"id":"W2898980811","doi":"10.1016/j.geomorph.2018.10.026","title":"Can magic sand cause massive degradation of a gravel-bed river at the decadal scale? Shi‑ting River, China","year":2018,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":20,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Tsinghua University; National Natural Science Foundation of China; National Science Foundation","keywords":"Aggradation; Geology; Flood myth; Sediment; Hydrology (agriculture); Geomorphology; Degradation (telecommunications); Intermittency; Sediment transport; Context (archaeology); Erosion; Fluvial; Geotechnical engineering; Turbulence; Paleontology; Archaeology","score_opus":0.009681410658917146,"score_gpt":0.22276317632818007,"score_spread":0.21308176566926293,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2898980811","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":[0.9954537,0.00005301658,0.00034877876,0.0014971483,0.00018293461,0.00017865664,0.000042721113,0.000020431284,0.0022225985],"genre_scores_gemma":[0.9979036,0.00002901693,0.00032677982,0.0006578512,0.000042955086,0.000009626252,0.00007328429,0.000010460235,0.00094643794],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998787,0.00010019106,0.00023646266,0.00034223756,0.00018294486,0.0003511669],"domain_scores_gemma":[0.9994367,0.00006845764,0.00015828994,0.00025088154,0.000017474938,0.00006823929],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00024945394,0.00015039765,0.0001908741,0.00003354394,0.00029995549,0.0000045313186,0.000276935,0.00014002166,0.0076074703],"category_scores_gemma":[0.000026141877,0.000110259665,0.000046620786,0.00018600671,0.0025599157,0.000085460946,0.00013327296,0.00014855994,0.00040144642],"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":[0.0002778141,0.00012448727,0.93652666,0.000015435835,0.00007235643,0.00011052183,0.0064066034,0.00026858784,0.047955062,0.00011139287,0.0041601267,0.0039709476],"study_design_scores_gemma":[0.0014689533,0.00048154994,0.8750084,0.000013902471,0.00016912277,0.00018459903,0.00011969457,0.0003392001,0.11332682,0.0030112157,0.005540355,0.00033617354],"about_ca_topic_score_codex":0.00205441,"about_ca_topic_score_gemma":0.006194238,"teacher_disagreement_score":0.06537175,"about_ca_system_score_codex":0.00006460507,"about_ca_system_score_gemma":0.000019262434,"threshold_uncertainty_score":0.9932997},"labels":[],"label_agreement":null},{"id":"W2902902793","doi":"10.1016/j.geomorph.2018.11.022","title":"The use of terrestrial laser scanning for the characterization of a cliff-talus system in the Thompson River Valley, British Columbia, Canada","year":2018,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":36,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Queen's University; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Cliff; Archaeology; River valley; Geomorphology; Paleontology; Geography","score_opus":0.014415802846645303,"score_gpt":0.2015946085500521,"score_spread":0.18717880570340678,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2902902793","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":[0.9981792,0.0000164068,0.00013527786,0.00031401493,0.0006826483,0.0004592581,0.00010122162,0.0000036389815,0.00010834148],"genre_scores_gemma":[0.99917984,0.000023904342,0.000028903803,0.00018039666,0.00008846381,0.000030440317,0.000022959199,0.000006682123,0.00043841705],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991271,0.00012942062,0.00024704525,0.0001322723,0.00016429595,0.00019989448],"domain_scores_gemma":[0.99928826,0.00029300313,0.00017748156,0.00020815729,0.000015388987,0.000017732735],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004177221,0.000052469888,0.0001277774,0.000005506078,0.00024448126,0.000042253985,0.00027681605,0.00007288141,0.00013679109],"category_scores_gemma":[0.000058567894,0.000034085744,0.000038226004,0.00011378858,0.00044739395,0.000045645327,0.00007903145,0.0000828887,0.0000026013372],"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":[0.0012712522,0.00028932714,0.7182234,0.00008571378,0.0003272195,0.00021762341,0.0060785813,0.0030642715,0.021248009,0.00013834504,0.16902404,0.08003224],"study_design_scores_gemma":[0.0013176558,0.00024940242,0.83026767,0.000063415304,0.00006223913,0.00015215314,0.00048022924,0.006469482,0.00024979783,0.000025645544,0.16054308,0.0001192249],"about_ca_topic_score_codex":0.8319939,"about_ca_topic_score_gemma":0.922215,"teacher_disagreement_score":0.11204429,"about_ca_system_score_codex":0.0000676869,"about_ca_system_score_gemma":0.00004891849,"threshold_uncertainty_score":0.18803768},"labels":[],"label_agreement":null},{"id":"W2908532151","doi":"10.1016/j.geomorph.2019.01.007","title":"Glacial to postglacial submarine landform assemblages in fiords of northeastern Baffin Island","year":2019,"lang":"en","type":"article","venue":"Geomorphology","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Center for Northern Studies; Université Laval","funders":"Natural Sciences and Engineering Research Council of Canada; ArcticNet","keywords":"Geology; Deglaciation; Glacial landform; Glacier; Ice sheet; Moraine; Fjord; Glacial period; Geomorphology; Landform; Ice stream; Meltwater; Seabed gouging by ice; Drumlin; Terminal moraine; Oceanography; Paleontology; Cryosphere; Sea ice","score_opus":0.010625370018119567,"score_gpt":0.21591334929345968,"score_spread":0.20528797927534012,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2908532151","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":[0.99327844,0.000076574215,0.000028540746,0.00048626255,0.0005643181,0.00018534664,0.0001072391,0.0000092050295,0.0052640755],"genre_scores_gemma":[0.9986908,0.000014694263,0.00011859444,0.00036393714,0.00008397014,0.0000014626772,0.00012644207,0.0000026125465,0.00059748057],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99919724,0.000025487827,0.00022031766,0.00018360384,0.00011263511,0.0002606841],"domain_scores_gemma":[0.9996297,0.000091366746,0.00005441059,0.00013944539,0.000036169455,0.000048929825],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014505976,0.000093258226,0.0002412807,0.000052613334,0.000034616245,0.000007904105,0.00014266418,0.00006137892,0.0062668785],"category_scores_gemma":[0.00003455158,0.00007915906,0.00003510254,0.00025596417,0.00003223392,0.000050675048,0.000026119249,0.000078609955,0.00043940297],"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":[0.00010288029,0.00001644022,0.9908154,0.0000071453483,0.0000072843923,0.000013028887,0.00031912586,0.0007022801,0.000053403317,0.000030918378,0.00038160844,0.007550485],"study_design_scores_gemma":[0.0004981002,0.0002490544,0.9871808,0.0000052563537,0.0000043208556,0.0000096985095,0.0001910172,0.0006201653,0.000017517712,0.00006224464,0.0110682,0.00009362216],"about_ca_topic_score_codex":0.016924867,"about_ca_topic_score_gemma":0.3275971,"teacher_disagreement_score":0.31067222,"about_ca_system_score_codex":0.0000037857824,"about_ca_system_score_gemma":0.000029784449,"threshold_uncertainty_score":0.99464154},"labels":[],"label_agreement":null},{"id":"W2921158359","doi":"10.1016/j.geomorph.2019.03.011","title":"Electromagnetic resistivity anisotropy in till from the Kiskatinaw streamlined landform field, northeastern British Columbia, Canada","year":2019,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Landform; Geomorphology; Anisotropy; Electrical resistivity and conductivity; Ridge; Paleontology","score_opus":0.00444268578251891,"score_gpt":0.17830346832580488,"score_spread":0.17386078254328596,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2921158359","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":[0.9967725,0.00018195609,0.0000134389675,0.00088109286,0.00027022528,0.00019980977,0.00027305423,0.000013631998,0.0013942368],"genre_scores_gemma":[0.99605614,0.000014310106,0.0002641231,0.0015435724,0.00009472644,0.0000024772744,0.0002465065,0.0000030867388,0.0017750553],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99860674,0.00022717443,0.00019990253,0.00032295703,0.0001779313,0.0004653079],"domain_scores_gemma":[0.9986406,0.0009501185,0.0000623606,0.000231943,0.000027610531,0.00008738936],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00015515799,0.00009739573,0.0002571703,0.000009054341,0.00014380596,0.00011582085,0.00028180578,0.00008721968,0.006702746],"category_scores_gemma":[0.00013279739,0.000095359566,0.000038957805,0.0002358565,0.00004228613,0.000040604402,0.00002094727,0.00029507812,0.00012607957],"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":[0.000045019,0.000018320026,0.9158071,0.0000031405768,0.0000070023766,0.000095296484,0.000008552112,0.000029872417,0.00003791448,0.0000023196435,0.0028246758,0.081120774],"study_design_scores_gemma":[0.0004247741,0.00046624042,0.98907936,0.000006886314,0.0000079657575,0.000024912842,0.000015458858,0.0011365258,0.00002204214,0.001787393,0.0068982914,0.00013012561],"about_ca_topic_score_codex":0.9981393,"about_ca_topic_score_gemma":0.9997658,"teacher_disagreement_score":0.08099065,"about_ca_system_score_codex":0.0000098515675,"about_ca_system_score_gemma":0.00016584322,"threshold_uncertainty_score":0.99420524},"labels":[],"label_agreement":null},{"id":"W2970484044","doi":"10.1016/j.geomorph.2019.106857","title":"Processes that cause natural unforested areas in Canadian Rockies below temperature treeline","year":2019,"lang":"en","type":"article","venue":"Geomorphology","topic":"Tree-ring climate responses","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; University of Calgary","keywords":"Regolith; Geology; Ridge; Bedrock; Snow; Geomorphology; Frost (temperature); Lithology; Frost heaving; Frost weathering; Soil water; Geochemistry; Astrobiology; Soil science; Paleontology","score_opus":0.011874803056619853,"score_gpt":0.21897575021733873,"score_spread":0.20710094716071886,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2970484044","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":[0.9949975,0.00182613,1.06553934e-7,0.0010717704,0.0006871925,0.00023844204,0.00030859638,0.00005525311,0.00081498054],"genre_scores_gemma":[0.9970952,0.000106775755,0.000054250682,0.0006154856,0.000061694096,0.000002480114,0.0009285926,0.000007683052,0.0011277997],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984347,0.0000925859,0.00019141342,0.00035882197,0.00015908711,0.0007633497],"domain_scores_gemma":[0.99912035,0.00027927343,0.000060851307,0.00025592823,0.00006364468,0.0002199191],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00017436387,0.00020423482,0.0002845487,0.00035187238,0.00009270801,0.000055125933,0.00029283695,0.00019681563,0.0028955264],"category_scores_gemma":[0.00022667315,0.00016443871,0.000031289732,0.00046544272,0.00009190369,0.00020583817,0.00001503315,0.0003128423,0.0009649538],"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":[0.00012150441,0.000007706544,0.9963,0.000041423336,0.0000131154575,0.0004682862,0.00025827353,0.0011236059,0.000088916364,0.000007789399,0.0007558887,0.00081349193],"study_design_scores_gemma":[0.00048748314,0.000093618284,0.98832864,0.00003651548,0.00000823705,0.00040495064,0.0002856615,0.0002828115,0.00020999424,0.000037021586,0.009606337,0.0002187241],"about_ca_topic_score_codex":0.47824532,"about_ca_topic_score_gemma":0.98903143,"teacher_disagreement_score":0.5107861,"about_ca_system_score_codex":0.000023998424,"about_ca_system_score_gemma":0.000535009,"threshold_uncertainty_score":0.9998129},"labels":[],"label_agreement":null},{"id":"W2982035569","doi":"10.1016/j.geomorph.2019.106895","title":"Development of robust evolutionary polynomial regression network in the estimation of stable alluvial channel dimensions","year":2019,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":13,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph; University of Ottawa","funders":"","keywords":"Geology; Alluvium; Channel (broadcasting); Polynomial regression; Regression; Estimation; Polynomial; Geomorphology; Statistics; Mathematics; Computer science; Mathematical analysis; Engineering","score_opus":0.013039557656170096,"score_gpt":0.2156527030600579,"score_spread":0.2026131454038878,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2982035569","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":[0.9977244,0.00007978515,0.0008036313,0.00018592438,0.00015942908,0.00019182343,0.0000043473797,0.000005883354,0.0008447514],"genre_scores_gemma":[0.9951998,0.000009532488,0.004497299,0.0001238351,0.00001228314,0.000012520563,0.00006327985,0.0000038889084,0.00007755267],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99912953,0.000066383356,0.0002824997,0.0001666164,0.00014825023,0.00020670019],"domain_scores_gemma":[0.99964315,0.00006983956,0.000116962576,0.0001450304,0.0000059971544,0.000019036093],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00040358317,0.00007898348,0.00016017353,0.000029187813,0.000071746406,8.9726797e-7,0.00017546111,0.00009949438,0.001872702],"category_scores_gemma":[0.00000980263,0.000056256336,0.000021493128,0.00017124064,0.00016453714,0.000078253775,0.00006068062,0.00010269875,0.00009738025],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002849392,0.00030873588,0.11481433,0.000026799673,0.000015511852,0.000012168645,0.0027046995,0.8653112,0.011288056,0.00011930012,0.004166518,0.000947742],"study_design_scores_gemma":[0.00254587,0.00048223982,0.9349131,0.0001306926,0.000049074555,0.00007605057,0.00051781273,0.038307905,0.009180332,0.0012024764,0.012183442,0.00041098165],"about_ca_topic_score_codex":0.0001225881,"about_ca_topic_score_gemma":0.00017166525,"teacher_disagreement_score":0.8270033,"about_ca_system_score_codex":0.000026449532,"about_ca_system_score_gemma":0.000034506582,"threshold_uncertainty_score":0.9990397},"labels":[],"label_agreement":null},{"id":"W2985368137","doi":"10.1016/j.geomorph.2019.106910","title":"Glacial geomorphology of the Neutral Hills Uplands, southeast Alberta, Canada: The process-form imprints of dynamic ice streams and surging ice lobes","year":2019,"lang":"en","type":"article","venue":"Geomorphology","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Geology; Moraine; Glacial landform; Ice stream; Glacial period; Seabed gouging by ice; Terminal moraine; Ice sheet; Geomorphology; Landform; Drumlin; Glacier; Glacier morphology; Antarctic sea ice; Cryosphere; Physical geography; Sea ice; Oceanography; Geography","score_opus":0.004859933787082644,"score_gpt":0.18587845247595636,"score_spread":0.18101851868887373,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2985368137","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":[0.9963976,0.00033130136,0.0000044460235,0.0011657834,0.00061233307,0.0002581352,0.00059396983,0.00000421621,0.00063218427],"genre_scores_gemma":[0.9992345,0.000054562523,0.000014782094,0.00028674654,0.000031355125,0.0000020618374,0.00012413373,0.0000042059983,0.0002476682],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988902,0.00006392023,0.00030838553,0.00023684498,0.000149251,0.0003513946],"domain_scores_gemma":[0.99891317,0.00044584516,0.00023908446,0.0002736999,0.00008034154,0.00004784117],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00019629911,0.00014695554,0.0003129612,0.000013024769,0.00018995244,0.000007736474,0.00033084044,0.000077811885,0.0014134814],"category_scores_gemma":[0.00005383513,0.00008605078,0.000050802555,0.00020731865,0.00034711388,0.000048439513,0.00005717666,0.00016441086,0.0000108808845],"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":[0.00005411777,0.000012371395,0.99462,0.00003259588,0.000045418765,0.0000041685716,0.00059292,0.0009217603,0.000043674318,0.00009498214,0.00022591896,0.0033520388],"study_design_scores_gemma":[0.00041584024,0.00007768255,0.9925522,0.000011958141,0.000038103095,0.00010469245,0.0022355146,0.0017892941,0.0000562471,0.000113194175,0.0024983243,0.00010692664],"about_ca_topic_score_codex":0.8416926,"about_ca_topic_score_gemma":0.96418643,"teacher_disagreement_score":0.1224938,"about_ca_system_score_codex":0.000008036682,"about_ca_system_score_gemma":0.00021127303,"threshold_uncertainty_score":0.9994994},"labels":[],"label_agreement":null},{"id":"W2999109217","doi":"10.1016/j.geomorph.2020.107043","title":"Morphometrics of China's Loess Plateau: The spatial legacy of tectonics, climate, and loess deposition history","year":2020,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":25,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Kwantlen Polytechnic University; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China; Canada Foundation for Innovation","keywords":"Geology; Plateau (mathematics); Morphometrics; Lithology; Loess; Geomorphology; Tectonics; Physical geography; Paleontology; Ecology; Geography; Biology","score_opus":0.008708064290300105,"score_gpt":0.18896543298644217,"score_spread":0.18025736869614206,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2999109217","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":[0.99561274,0.0007042641,0.0009904545,0.0005814915,0.00026672822,0.00014913472,0.000033871,0.000014888948,0.0016464392],"genre_scores_gemma":[0.9990417,0.00039634435,0.0002275071,0.00024471796,0.000025867224,0.0000031686202,0.000021259806,0.000010541244,0.00002894417],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990825,0.000062064144,0.00026473493,0.0002173253,0.00016862876,0.00020471422],"domain_scores_gemma":[0.99950457,0.000055052336,0.00019388246,0.00016789805,0.000010911609,0.00006770925],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00018306746,0.00010679452,0.0002317636,0.00003775383,0.00005966146,0.000005335892,0.00019777572,0.00013820118,0.0014000986],"category_scores_gemma":[0.000043128173,0.00007118395,0.000049455535,0.00021112533,0.0004991194,0.00007959659,0.00024414036,0.00019744162,0.000030132222],"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":[0.00204953,0.0009698891,0.45200795,0.00062447554,0.00038518477,0.0006369928,0.012528157,0.01697667,0.40377557,0.0016830727,0.03959427,0.06876824],"study_design_scores_gemma":[0.0043445746,0.0021627857,0.8840154,0.000055114473,0.00035127558,0.00067645416,0.0004987697,0.01621968,0.04526678,0.0003119012,0.045345593,0.00075166364],"about_ca_topic_score_codex":0.002098567,"about_ca_topic_score_gemma":0.000074275005,"teacher_disagreement_score":0.43200746,"about_ca_system_score_codex":0.0000682527,"about_ca_system_score_gemma":0.000014573455,"threshold_uncertainty_score":0.99951273},"labels":[],"label_agreement":null},{"id":"W3009509482","doi":"10.1016/j.geomorph.2020.107159","title":"Multi-scale site evaluation of a relict active layer detachment in a High Arctic landscape","year":2020,"lang":"en","type":"article","venue":"Geomorphology","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal; Université Laval; Center for Northern Studies; Government of Northwest Territories; Queen's University","funders":"Natural Sciences and Engineering Research Council of Canada; ArcticNet","keywords":"Permafrost; Thermokarst; Geology; Active layer; Ground-penetrating radar; Arctic; Subsidence; Landform; Geomorphology; Remote sensing; Physical geography; Radar; Layer (electronics); Oceanography; Geography","score_opus":0.08360591277955699,"score_gpt":0.28851686910908486,"score_spread":0.20491095632952788,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3009509482","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":[0.9970225,0.00031586055,0.000011679243,0.0010541251,0.00012079817,0.0002204053,0.00096468395,0.000008414045,0.0002815018],"genre_scores_gemma":[0.9963021,0.000060857652,0.00016298771,0.00086073694,0.000056617177,0.0000046503637,0.0025374126,0.0000026074986,0.000012001459],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99908286,0.00013005042,0.00018284893,0.00021627468,0.00018711478,0.0002008184],"domain_scores_gemma":[0.9996114,0.00007202972,0.000076993405,0.00010310576,0.00006451358,0.00007195976],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002978947,0.00008688647,0.00019156156,0.00005923158,0.000025768084,0.000005972048,0.00008733445,0.000072376744,0.01939602],"category_scores_gemma":[0.000038193608,0.00007598971,0.000032819313,0.00018535118,0.00004147292,0.00006212539,0.00001497236,0.00010945846,0.00040887645],"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":[0.00014045654,0.000029712131,0.9896247,0.000017071845,0.000008485634,0.000020139703,0.0023964208,0.0015823251,0.0038560466,6.159385e-7,0.00029379714,0.0020302273],"study_design_scores_gemma":[0.0013275845,0.00018904895,0.9550727,0.000009231632,0.00003241761,0.000015362097,0.0003293477,0.041990705,0.00043099254,0.000026708703,0.00049019756,0.000085712956],"about_ca_topic_score_codex":0.013242641,"about_ca_topic_score_gemma":0.068945274,"teacher_disagreement_score":0.055702634,"about_ca_system_score_codex":0.0000063904395,"about_ca_system_score_gemma":0.000031335207,"threshold_uncertainty_score":0.9933283},"labels":[],"label_agreement":null},{"id":"W3036834242","doi":"10.1016/j.geomorph.2020.107295","title":"The sediment record of the Unicorn Cave, southern Harz Mountains, Germany","year":2020,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"Deutsche Forschungsgemeinschaft","keywords":"Cave; Geology; Unicorn; Sediment; Paleontology; Archaeology; Speleothem; Geomorphology; Geography","score_opus":0.019464605106528126,"score_gpt":0.21634251986378572,"score_spread":0.1968779147572576,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3036834242","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":[0.97717327,0.00071510713,0.000010439112,0.016640885,0.00043190172,0.00019879191,0.00009716177,0.000017551445,0.0047149225],"genre_scores_gemma":[0.9969581,0.00007577824,0.000035672463,0.0020044916,0.00006248425,0.0000023998819,0.000034215638,0.0000027960612,0.0008240761],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99854046,0.00042941215,0.00023579889,0.00022177426,0.0001527178,0.00041981667],"domain_scores_gemma":[0.99906135,0.00036384142,0.00011502468,0.00031806398,0.00004872203,0.00009298676],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0004091714,0.000107273685,0.00018657926,0.000019520068,0.00037019938,0.000010274157,0.0006677875,0.00014025466,0.0030709927],"category_scores_gemma":[0.0001153576,0.000057642013,0.0000744804,0.00018726141,0.0007823965,0.000024392917,0.000056173878,0.00037871618,0.00150395],"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":[0.00010099562,0.000006053546,0.99573797,0.0000070159062,0.000028778437,0.000026435324,0.00038815985,0.0001005608,0.000061254286,0.0001672618,0.00259845,0.00077704736],"study_design_scores_gemma":[0.00054531486,0.0002875228,0.93455404,0.0000051579323,0.000028471137,0.00018199255,0.0010624098,0.0014837547,0.00027214683,0.0010210135,0.060415313,0.00014289105],"about_ca_topic_score_codex":0.000990479,"about_ca_topic_score_gemma":0.0047507747,"teacher_disagreement_score":0.061183974,"about_ca_system_score_codex":9.780007e-7,"about_ca_system_score_gemma":0.00007378898,"threshold_uncertainty_score":0.9992735},"labels":[],"label_agreement":null},{"id":"W3092214469","doi":"10.1016/j.geomorph.2020.107447","title":"Spatial scale determines how the morphological diversity relates with river biological diversity. Evidence from a mountain river in the central Chilean Andes","year":2020,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":11,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Prince Edward Island","funders":"Comisión Nacional de Investigación Científica y Tecnológica; Agence Nationale de la Recherche","keywords":"Biodiversity; Habitat; Ecology; Drainage basin; Ecosystem; Spatial ecology; Riparian zone; River ecosystem; Invertebrate; Structural basin; Fluvial; Geography; Geology; Geomorphology; Biology; Cartography","score_opus":0.03054036137460326,"score_gpt":0.20031867649563972,"score_spread":0.16977831512103647,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3092214469","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":[0.9875788,0.000103838705,0.0006282734,0.011140655,0.000055248416,0.00030367632,0.00004927114,0.000039640177,0.00010058673],"genre_scores_gemma":[0.99513197,0.00013403156,0.00018135316,0.0044159433,0.0000662636,0.000010618571,0.000041772742,0.0000049872165,0.000013077833],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99811393,0.0003899813,0.0001449155,0.00058828975,0.00027445212,0.0004884444],"domain_scores_gemma":[0.99910325,0.00047141575,0.00008642126,0.0002250126,0.000008466764,0.00010544565],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00026199862,0.00022311775,0.00026368577,0.000017551176,0.000748269,0.000019744197,0.0010218038,0.00021659097,0.0025892316],"category_scores_gemma":[0.00008498783,0.000113658454,0.00006728422,0.00023749296,0.0026966343,0.00023109306,0.0010901348,0.00043624264,0.00013677223],"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":[0.00046679645,0.00008223072,0.9867516,0.0000023473704,0.00001809595,0.00092510274,0.009885522,0.0003113478,0.00057006563,0.0000052928185,0.00060550595,0.00037608674],"study_design_scores_gemma":[0.0006527068,0.0004907558,0.9968077,0.000008511812,0.000057910045,0.00007858808,0.00045476723,0.00023732998,0.00018968772,0.00042322415,0.00041929696,0.00017953657],"about_ca_topic_score_codex":0.0057091834,"about_ca_topic_score_gemma":0.003005658,"teacher_disagreement_score":0.010056078,"about_ca_system_score_codex":0.000042798445,"about_ca_system_score_gemma":0.000011391609,"threshold_uncertainty_score":0.99832255},"labels":[],"label_agreement":null},{"id":"W3096036297","doi":"10.1016/j.geomorph.2020.107473","title":"A huge flood in the Fraser River valley, British Columbia, near the Pleistocene Termination","year":2020,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":16,"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 Northern British Columbia; Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Glacier; Plateau (mathematics); Flood myth; Pleistocene; Geomorphology; Glacial lake; Hydrology (agriculture); Shelf ice; Glacial period; Silt; Landslide; Oceanography; Paleontology; Archaeology; Ice stream; Sea ice; Cryosphere","score_opus":0.00796189200648323,"score_gpt":0.1944482837250921,"score_spread":0.18648639171860887,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3096036297","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":[0.9916901,0.00005805883,0.000032928514,0.004943003,0.00011138156,0.00025947564,0.000020016245,0.000016896924,0.0028681168],"genre_scores_gemma":[0.99259007,0.000033277785,0.00008800432,0.006638012,0.000052383617,0.000024775769,0.000022335154,0.000008467208,0.00054270355],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99909276,0.00013306376,0.00014630468,0.00022744696,0.00016919945,0.00023122224],"domain_scores_gemma":[0.9996851,0.000053513046,0.00004665373,0.00016768201,0.000004568562,0.000042498752],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00023792376,0.000062804254,0.00010490159,0.0000037571858,0.00026504626,0.00012675539,0.00036089122,0.00010940904,0.007029215],"category_scores_gemma":[0.00003919286,0.000050746567,0.00004332641,0.00019455375,0.00046037944,0.000058591668,0.00015102653,0.00025825266,0.00062623457],"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":[0.00006985029,0.00030114801,0.49320424,0.00001295262,0.000040555435,0.0019624801,0.009640485,0.0020294234,0.0006683368,0.00003699847,0.43246585,0.0595677],"study_design_scores_gemma":[0.0007871598,0.00015681253,0.8153013,0.0000045510264,0.000019265366,0.00017624984,0.000190292,0.0017427428,0.000010801858,0.00039259196,0.18110508,0.00011313789],"about_ca_topic_score_codex":0.034664854,"about_ca_topic_score_gemma":0.04849516,"teacher_disagreement_score":0.3220971,"about_ca_system_score_codex":0.00003204208,"about_ca_system_score_gemma":0.000012302485,"threshold_uncertainty_score":0.9938785},"labels":[],"label_agreement":null},{"id":"W3118830196","doi":"10.1016/j.geomorph.2020.107584","title":"Shoreline changes in coral reef islands of the Federated States of Micronesia since the mid-20th century","year":2021,"lang":"en","type":"article","venue":"Geomorphology","topic":"Coastal and Marine Dynamics","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"University of Auckland","keywords":"Reef; Shore; Atoll; Archipelago; Accretion (finance); Storm; Geology; Coral reef; Oceanography; Fringing reef; Coastal erosion; Coral; Climate change; Sea level; Physical geography; Geography","score_opus":0.008019446112538351,"score_gpt":0.1962647125684736,"score_spread":0.18824526645593526,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3118830196","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":[0.9947206,0.00065226335,0.00002015419,0.0034048809,0.0003307864,0.00008930773,0.0003505653,0.0000046053597,0.00042684324],"genre_scores_gemma":[0.9981846,0.00040506106,0.000048769787,0.0003923071,0.00002293242,5.506983e-7,0.00063202606,0.0000020931882,0.00031166588],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992618,0.00012467812,0.00018619215,0.00014172976,0.00009194859,0.0001936822],"domain_scores_gemma":[0.9995189,0.00012347635,0.0000934328,0.00017323658,0.000069964626,0.000021042315],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000157219,0.000082384606,0.00017934258,0.000027252165,0.00005325253,0.000007862872,0.0001850245,0.000053851818,0.0008164821],"category_scores_gemma":[0.000036480953,0.000046424295,0.000034757093,0.0002737778,0.00021193291,0.000019002138,0.00007641338,0.00012485438,0.0000052918135],"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":[0.00019231466,0.00007283979,0.9748369,0.000044173226,0.000024197612,0.000090221685,0.00059166475,0.0013954615,0.0062894565,0.000097361815,0.0011157697,0.015249666],"study_design_scores_gemma":[0.0005500687,0.00017528853,0.9758379,0.000023908176,0.00001872927,0.00016561906,0.0009416214,0.008864253,0.0040879617,0.00047798755,0.008738579,0.00011807338],"about_ca_topic_score_codex":0.005220505,"about_ca_topic_score_gemma":0.16720022,"teacher_disagreement_score":0.16197972,"about_ca_system_score_codex":0.00000228893,"about_ca_system_score_gemma":0.000067552864,"threshold_uncertainty_score":0.89399064},"labels":[],"label_agreement":null},{"id":"W3120001605","doi":"10.1016/j.geomorph.2021.107613","title":"Geomorphic constraints on the development of a blind-thrust induced landform, south-central Mongolia: Insights into foreberg growth","year":2021,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Research Foundation of Korea; Ministry of Education","keywords":"Geology; Denudation; Foreland basin; Landform; Alluvial fan; Tectonics; Fault (geology); Geomorphology; Thermochronology; Sinistral and dextral; Fluvial; Thrust fault; River terraces; Paleontology; Seismology; Structural basin","score_opus":0.03966315881075913,"score_gpt":0.24250749011608788,"score_spread":0.20284433130532875,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3120001605","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":[0.9892735,0.00023056816,0.000056205427,0.0012033914,0.00046883305,0.00022510134,0.000026086567,0.000021844107,0.00849451],"genre_scores_gemma":[0.9984822,0.00002720849,0.0003273999,0.0006048837,0.000049291288,0.000008770024,0.00037047206,0.000004735167,0.00012501156],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9977839,0.00038646843,0.00044841965,0.00041384235,0.00026254795,0.0007048387],"domain_scores_gemma":[0.99857515,0.00058751414,0.00015086417,0.00033192808,0.00018926297,0.00016526024],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00047117093,0.00021347956,0.00039273812,0.00014579728,0.00040505457,0.000016658714,0.00040411862,0.00035299236,0.011098454],"category_scores_gemma":[0.0002896816,0.00014568046,0.000079876416,0.00036645212,0.0008856136,0.00005681942,0.0000651616,0.0005851954,0.00081985386],"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":[0.00018403042,0.000057331155,0.99306786,0.000027076392,0.000111066714,0.0003219823,0.0031054185,0.000034620425,0.00017922338,0.0016528117,0.00019171536,0.0010668598],"study_design_scores_gemma":[0.0016226012,0.00026365748,0.98235905,0.000030139612,0.000028030909,0.00044486206,0.0013979446,0.0002312413,0.009815054,0.0028149895,0.0007177958,0.00027464976],"about_ca_topic_score_codex":0.00015243383,"about_ca_topic_score_gemma":0.009299562,"teacher_disagreement_score":0.010708829,"about_ca_system_score_codex":0.000003770747,"about_ca_system_score_gemma":0.0005460941,"threshold_uncertainty_score":0.9999581},"labels":[],"label_agreement":null},{"id":"W3154311621","doi":"10.1016/j.geomorph.2021.107736","title":"A simple test of lichenometric dating using bidecadal growth of Rhizocarpon geographicum agg. and structure-from-motion photogrammetry","year":2021,"lang":"en","type":"article","venue":"Geomorphology","topic":"Lichen and fungal ecology","field":"Agricultural and Biological Sciences","cited_by":5,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Brock University","funders":"Parks Canada; National Geographic Society","keywords":"Thallus; Lichen; Geology; Botany; Biology","score_opus":0.016356378905882242,"score_gpt":0.21920267396884677,"score_spread":0.20284629506296453,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3154311621","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":[0.9985907,0.00046928684,0.000031835112,0.00008760285,0.000112648806,0.0000913638,0.0005186002,0.000014958703,0.00008297603],"genre_scores_gemma":[0.9986917,0.000036699195,0.0006068672,0.00015364762,0.00009108795,0.0000017335745,0.00041135636,0.0000015867971,0.0000053219815],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99882203,0.00011415116,0.00034719135,0.00033268353,0.000115789386,0.00026812195],"domain_scores_gemma":[0.998717,0.0006968603,0.0002580652,0.000075629134,0.0001776759,0.00007476308],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00016497207,0.00012966915,0.00036177115,0.000073314615,0.00008423533,0.000012933098,0.00014124221,0.00020661538,0.0009872691],"category_scores_gemma":[0.00057175226,0.00006604631,0.00007422925,0.0012774882,0.00017957797,0.00005816794,0.00017937896,0.00014263493,0.0000013013045],"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":[0.000008777085,0.000057495894,0.4547856,0.000010093843,0.000017281904,0.000008774244,0.00001855356,9.375448e-7,0.5409316,0.0000631537,0.000013891401,0.004083897],"study_design_scores_gemma":[0.00028631752,0.00032991997,0.8780972,0.000008410353,0.000051291197,0.000083057406,0.00027109103,0.0002519927,0.11893457,0.0013785477,0.00016582881,0.00014179686],"about_ca_topic_score_codex":0.0075338543,"about_ca_topic_score_gemma":0.0015955139,"teacher_disagreement_score":0.4233116,"about_ca_system_score_codex":0.0000108482245,"about_ca_system_score_gemma":0.000015352658,"threshold_uncertainty_score":0.999926},"labels":[],"label_agreement":null},{"id":"W3184565785","doi":"10.1016/j.geomorph.2021.107863","title":"Rainfall spatial-heterogeneity accelerates landscape evolution processes","year":2021,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Watershed Management Studies","field":"Environmental Science","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Storm; Spatial heterogeneity; Erosion; Context (archaeology); Spatial ecology; Streamflow; Drainage basin; Deposition (geology); Spatial variability; Environmental science; Hydrology (agriculture); Spatial distribution; Common spatial pattern; Surface runoff; Sediment; Geology; Physical geography; Ecology; Geomorphology; Geography; Oceanography","score_opus":0.012236291041085982,"score_gpt":0.22246702706756166,"score_spread":0.21023073602647568,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3184565785","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":[0.9814362,0.00025859024,0.002461283,0.0019445157,0.00022739357,0.000101526326,0.000009218481,0.0000629785,0.0134983],"genre_scores_gemma":[0.9972774,0.000083049476,0.00021009898,0.0011492264,0.0000437577,0.000028468345,0.000060933824,0.000007131504,0.0011399753],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990394,0.00007825215,0.00013416042,0.00034651108,0.00009279617,0.00030886],"domain_scores_gemma":[0.9996659,0.000040232848,0.000047762467,0.00018590775,0.000018333223,0.000041826603],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00013540288,0.000114984534,0.0001528118,0.000021944783,0.00019364807,0.000012706337,0.0001325403,0.00008486711,0.0062672994],"category_scores_gemma":[0.000086997214,0.00010446449,0.000029691217,0.00018208098,0.00020153073,0.00009568362,0.0003729887,0.00008409815,0.0014768207],"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":[0.0000343631,0.00012937338,0.96839756,0.000025194742,0.00005998071,0.00023081886,0.0002400039,0.0013315468,0.005636294,0.00010055678,0.022981565,0.0008327615],"study_design_scores_gemma":[0.001238943,0.00019454004,0.87266564,0.000008423801,0.000090663874,0.00021445096,0.00021098761,0.00044043112,0.02405396,0.0043058405,0.096083,0.0004931046],"about_ca_topic_score_codex":0.0003059636,"about_ca_topic_score_gemma":0.0026524686,"teacher_disagreement_score":0.09573189,"about_ca_system_score_codex":0.000033675733,"about_ca_system_score_gemma":0.000013490168,"threshold_uncertainty_score":0.99930066},"labels":[],"label_agreement":null},{"id":"W3185699184","doi":"10.1016/j.geomorph.2021.107865","title":"Reply to comment by Wasson et al. on “Recasting Geomorphology as a Landscape Science” by Slaymaker, Spencer and Embleton-Hamann (2021)","year":2021,"lang":"en","type":"article","venue":"Geomorphology","topic":"Wildlife-Road Interactions and Conservation","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Geomorphology","score_opus":0.010057626601542862,"score_gpt":0.2657084239536143,"score_spread":0.25565079735207147,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3185699184","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":[0.82890594,0.00008404375,0.00030723153,0.16138202,0.00046625422,0.00020950485,0.00007797589,0.000027437827,0.008539625],"genre_scores_gemma":[0.55925614,0.00012033563,0.0011671507,0.43358058,0.000039883085,0.000083684965,0.00027641197,0.000028308461,0.005447542],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9975953,0.0001611848,0.00033734378,0.0009503308,0.00036497496,0.00059083145],"domain_scores_gemma":[0.99889195,0.00019579427,0.00014385866,0.00047777971,0.00005218643,0.0002384346],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00073380227,0.00022525284,0.00026537903,0.00008635814,0.00037277496,0.00011097106,0.00027027432,0.00008719501,0.01764798],"category_scores_gemma":[0.00030469563,0.00022351743,0.000041357704,0.0004655912,0.00036515397,0.00024363457,0.00048644116,0.00030190818,0.0015579743],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000054346616,0.0001461776,0.014768191,0.0000014151975,0.00000988185,0.00009546858,0.00021048119,0.000089316505,0.1157389,0.00009974544,0.86467505,0.0041110534],"study_design_scores_gemma":[0.000582378,0.00048997975,0.006994262,0.00002040557,0.00001253122,0.0006351887,0.00029264492,0.00040384583,0.01228435,0.00013139362,0.97788113,0.0002719151],"about_ca_topic_score_codex":0.0036597387,"about_ca_topic_score_gemma":0.00021526535,"teacher_disagreement_score":0.27219856,"about_ca_system_score_codex":0.0001836985,"about_ca_system_score_gemma":0.00006581216,"threshold_uncertainty_score":0.9992194},"labels":[],"label_agreement":null},{"id":"W3200203514","doi":"10.1016/j.geomorph.2021.107947","title":"Vermicular Ridge Features on Dundas Harbour, Devon Island, Nunavut","year":2021,"lang":"en","type":"article","venue":"Geomorphology","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université Laval; Center for Northern Studies; Western University","funders":"","keywords":"Moraine; Geology; Ridge; Geomorphology; Debris; Glacial period; Landform; Terminal moraine; Paleontology; Oceanography","score_opus":0.02210398748123236,"score_gpt":0.23469676639624415,"score_spread":0.2125927789150118,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3200203514","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":[0.9792914,0.0017492397,0.000005260803,0.0017520925,0.0011458979,0.00007974748,0.0065755243,0.000030293491,0.009370545],"genre_scores_gemma":[0.9629543,0.000595587,0.000057374295,0.0074319798,0.00052374037,0.000002258719,0.025858993,0.000009193583,0.002566612],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988122,0.00010318806,0.00014575025,0.00035708598,0.00015728048,0.00042448373],"domain_scores_gemma":[0.99936897,0.00013680193,0.000047792193,0.00028442123,0.00004425169,0.000117780044],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00012669191,0.00015901418,0.00021915749,0.000058986305,0.00016367319,0.0000515606,0.00015807722,0.00015547106,0.08978004],"category_scores_gemma":[0.00004394004,0.0001369102,0.00007969999,0.00015780432,0.0000878871,0.000058821774,0.000021530455,0.00022715756,0.0035455362],"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":[0.00017222458,0.000074946496,0.8236059,0.000030578318,0.00005223008,0.006685909,0.00047116328,0.00028135435,0.0040831165,0.0002532561,0.15985318,0.004436152],"study_design_scores_gemma":[0.00069485,0.0002134735,0.7070315,0.000020126507,0.000026187818,0.0016454791,0.00014589826,0.00013958053,0.0035202187,0.0004066116,0.28586173,0.00029434945],"about_ca_topic_score_codex":0.0027760773,"about_ca_topic_score_gemma":0.1211271,"teacher_disagreement_score":0.12600856,"about_ca_system_score_codex":0.0000041840676,"about_ca_system_score_gemma":0.000050523755,"threshold_uncertainty_score":0.9972303},"labels":[],"label_agreement":null},{"id":"W4200384220","doi":"10.1016/j.geomorph.2021.108061","title":"Sedimentary characteristics and morphologic change of till-bedded semi-alluvial streams: Medway Creek, Southern Ontario, Canada","year":2021,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Western University","keywords":"Bedform; Geology; Bedrock; Alluvium; Geomorphology; Clastic rock; Alluvial fan; STREAMS; Sediment transport; Sedimentary rock; Bed load; Erosion; Sediment; Hydrology (agriculture); Alluvial plain; Channel (broadcasting); Geochemistry; Structural basin; Paleontology; Geotechnical engineering","score_opus":0.01148828874700699,"score_gpt":0.1888387801868863,"score_spread":0.1773504914398793,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200384220","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":[0.9972898,0.00014797032,0.000019055826,0.0006487748,0.00038260562,0.0001427037,0.00028537944,0.000021691358,0.0010620306],"genre_scores_gemma":[0.9944245,0.000056651617,0.00015958864,0.0031975044,0.000071139606,0.000023628983,0.00048159188,0.000014138142,0.0015712506],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99850136,0.000076997276,0.00033293653,0.00045992064,0.000220209,0.00040857316],"domain_scores_gemma":[0.99937063,0.00006911874,0.00014324517,0.00025786215,0.00002061572,0.00013853323],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00015484568,0.00019615248,0.00037702653,0.000020249172,0.000115230054,0.0000069085727,0.00019118408,0.0001843474,0.041699663],"category_scores_gemma":[0.000019285464,0.00020091589,0.00003826164,0.00011325171,0.00042131884,0.000080907295,0.00015589898,0.00023573311,0.00005797499],"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":[0.000079212194,0.00017193012,0.9779088,0.000027481597,0.00007049928,0.0016116167,0.0021296262,0.000023030943,0.011965525,0.000010902746,0.0043085795,0.0016928214],"study_design_scores_gemma":[0.0018946083,0.00048867136,0.9018242,0.000030689414,0.00023573055,0.00071548636,0.001019703,0.000081433776,0.01134253,0.00025980023,0.08139858,0.00070857065],"about_ca_topic_score_codex":0.9117906,"about_ca_topic_score_gemma":0.98219955,"teacher_disagreement_score":0.077089995,"about_ca_system_score_codex":0.00012786342,"about_ca_system_score_gemma":0.0001823091,"threshold_uncertainty_score":0.95917636},"labels":[],"label_agreement":null},{"id":"W4210276771","doi":"10.1016/j.geomorph.2022.108125","title":"Late Glacial deglaciation of the Zackenberg area, NE Greenland","year":2022,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval; Center for Northern Studies","funders":"Ministerio de Economía y Competitividad; Centre National de la Recherche Scientifique; Generalitat de Catalunya; Agence Nationale de la Recherche; Ministerio de Ciencia, Innovación y Universidades","keywords":"Deglaciation; Moraine; Geology; Glacier; Glacial period; Glacial landform; Landform; Physical geography; Geomorphology; Ice sheet; Terminal moraine; Quaternary; Last Glacial Maximum; Arctic; Glacier morphology; Paleontology; Oceanography; Arctic ice pack; Antarctic sea ice; Geography","score_opus":0.018257325087843605,"score_gpt":0.22010244001318385,"score_spread":0.20184511492534024,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4210276771","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":[0.99178445,0.00022122284,0.000010347665,0.0014994025,0.0006947872,0.00013199633,0.0001114603,0.000011239769,0.005535109],"genre_scores_gemma":[0.99818295,0.000012007617,0.000029498695,0.00044259228,0.000031516167,0.0000038424155,0.00018087195,0.0000016119799,0.0011151173],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99869657,0.00046732937,0.00017603772,0.00017978778,0.00017730996,0.00030294328],"domain_scores_gemma":[0.9993982,0.00020748295,0.00010964222,0.00021420346,0.000031882642,0.000038641774],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004984903,0.000075037926,0.00016466924,0.00006881866,0.0004284375,0.000003370319,0.00035819312,0.00008091898,0.020743962],"category_scores_gemma":[0.000064131156,0.000055641387,0.000057486137,0.0002603075,0.00031018537,0.00003207234,0.00007852953,0.0003322017,0.0001535823],"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":[0.00010833426,0.0000136049875,0.9960733,0.0000035182761,0.000015486741,0.000033880628,0.00012493173,0.00191715,0.00003708541,0.00009704628,0.001009541,0.0005660874],"study_design_scores_gemma":[0.00036549833,0.0001508025,0.9912702,8.270307e-7,0.0000116231795,0.00030883818,0.000053832406,0.0009124809,0.000063409396,0.001755202,0.0050450643,0.00006220862],"about_ca_topic_score_codex":0.0006690679,"about_ca_topic_score_gemma":0.006395658,"teacher_disagreement_score":0.02059038,"about_ca_system_score_codex":0.0000014749081,"about_ca_system_score_gemma":0.00006968235,"threshold_uncertainty_score":0.98015124},"labels":[],"label_agreement":null},{"id":"W4211204043","doi":"10.1016/j.geomorph.2022.108161","title":"Characteristics of surge-type tributary glaciers, Karakoram","year":2022,"lang":"en","type":"article","venue":"Geomorphology","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Wilfrid Laurier University","funders":"National Aeronautics and Space Administration","keywords":"Surge; Tributary; Glacier; Geology; Glacier morphology; Glacier terminus; Geomorphology; Ice stream; Oceanography; Cryosphere; Geography; Sea ice","score_opus":0.019290775180752465,"score_gpt":0.2097303074621332,"score_spread":0.19043953228138072,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4211204043","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":[0.99551594,0.0007446879,0.000039040984,0.0005232551,0.0017867256,0.000083681305,0.0008263838,0.000019170211,0.0004611002],"genre_scores_gemma":[0.99750966,0.00013469192,0.00017348169,0.0006080216,0.000056066496,0.0000017404079,0.001050728,0.0000023139457,0.00046327277],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992191,0.00006952837,0.00021077797,0.00014776216,0.0001344973,0.00021833862],"domain_scores_gemma":[0.9995061,0.00014737989,0.00010683572,0.00015037463,0.000047687136,0.000041589876],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00022086686,0.00007208293,0.00020543719,0.000024494226,0.00026067815,0.0000041742237,0.0001562699,0.000026140484,0.025542732],"category_scores_gemma":[0.0000584518,0.00006987163,0.00004337544,0.00033844294,0.000097681776,0.000026901687,0.00004735273,0.00012248772,0.000063275955],"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":[0.0000764177,0.000025436027,0.9727198,0.000005377858,0.000023411898,0.000048855552,0.000118079006,0.0004758311,0.000028511902,0.00009147535,0.018901562,0.0074852295],"study_design_scores_gemma":[0.00013412455,0.00020321853,0.7617456,5.22457e-7,0.000011741422,0.000036232508,0.00020306453,0.00046364247,0.0000042084607,0.00009774546,0.23703356,0.000066353154],"about_ca_topic_score_codex":0.001963999,"about_ca_topic_score_gemma":0.00020810385,"teacher_disagreement_score":0.21813199,"about_ca_system_score_codex":0.000004938305,"about_ca_system_score_gemma":0.00004956097,"threshold_uncertainty_score":0.97534806},"labels":[],"label_agreement":null},{"id":"W4230375324","doi":"10.1016/j.geomorph.2009.09.027","title":"Preface","year":2009,"lang":"en","type":"article","venue":"Geomorphology","topic":"","field":"","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ministry of Forests; Government of British Columbia; Saint Mary's University","funders":"","keywords":"Geology; Geomorphology","score_opus":0.011432285249503843,"score_gpt":0.26192229045204873,"score_spread":0.2504900052025449,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4230375324","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":[0.94820654,0.00015640269,0.00023374504,0.0016517551,0.00019132758,0.00013312306,0.000036721915,0.00033249482,0.049057916],"genre_scores_gemma":[0.9949752,0.0000024120022,0.0008079751,0.0018964867,0.00007175566,0.0000038840367,0.000038478738,0.000017561886,0.0021862262],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991678,0.000058385005,0.00011853043,0.00021862134,0.00008708727,0.0003495556],"domain_scores_gemma":[0.9995107,0.000022117873,0.00004516245,0.0003175924,0.000035159876,0.000069289235],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0001533859,0.00009338662,0.00013713466,0.00006741425,0.000044313674,0.0000076287015,0.00017525823,0.00008365375,0.0027372742],"category_scores_gemma":[0.000057224777,0.00009094079,0.000033241893,0.00016182208,0.00007470523,0.000050685227,0.000022957927,0.0001169518,0.039823465],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014989874,0.00026403152,0.003994135,0.0000021650217,0.000021355147,0.0004873434,0.00026253806,0.0001387309,0.45116276,0.017855328,0.51439124,0.011270479],"study_design_scores_gemma":[0.0017276459,0.0006998055,0.23277426,0.0000051452666,0.000030474526,0.001418764,0.000038621165,0.00010604725,0.021752369,0.013475991,0.7275471,0.0004237877],"about_ca_topic_score_codex":0.000023535038,"about_ca_topic_score_gemma":0.000011534755,"teacher_disagreement_score":0.42941037,"about_ca_system_score_codex":0.000031944306,"about_ca_system_score_gemma":0.000020343485,"threshold_uncertainty_score":0.99817437},"labels":[],"label_agreement":null},{"id":"W4237276108","doi":"10.1016/j.geomorph.2003.09.016","title":"Aeolian research","year":2003,"lang":"en","type":"article","venue":"Geomorphology","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"","keywords":"Geology; Aeolian processes; Geomorphology","score_opus":0.06011500422212456,"score_gpt":0.30400233463609094,"score_spread":0.24388733041396637,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4237276108","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":[0.8110534,0.00094672525,0.00014752959,0.00052127946,0.0004975304,0.00012245605,0.000018062503,0.00003761622,0.18665537],"genre_scores_gemma":[0.997026,0.000036050456,0.00041359206,0.00042011065,0.00006473062,0.0000012448685,0.000031383053,0.000002540181,0.0020043275],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9987899,0.00023126902,0.000093716175,0.00021790374,0.00016070365,0.0005065003],"domain_scores_gemma":[0.9994488,0.00018117281,0.000018822033,0.00017247837,0.000054597156,0.00012416714],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00079966674,0.000069420494,0.00010395658,0.00008189528,0.00019201823,0.000019888337,0.0001580791,0.000083982304,0.02101096],"category_scores_gemma":[0.00018682335,0.000057321307,0.000023302362,0.00030194552,0.00020317722,0.00006123825,0.000006889462,0.00021203853,0.0065025166],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007746925,0.000051339794,0.81886774,0.00006222347,0.00002723004,0.00085964496,0.00048703636,0.0018677149,0.0002159148,0.017352577,0.10965444,0.05047668],"study_design_scores_gemma":[0.0005322276,0.0005094934,0.20775151,0.000009307855,0.000006301151,0.00072438095,0.00033153407,0.0014197174,0.0009732514,0.030490456,0.7569868,0.00026502644],"about_ca_topic_score_codex":0.0010851996,"about_ca_topic_score_gemma":0.0011048077,"teacher_disagreement_score":0.6473324,"about_ca_system_score_codex":0.0000023474827,"about_ca_system_score_gemma":0.000061239276,"threshold_uncertainty_score":0.99427104},"labels":[],"label_agreement":null},{"id":"W4308928312","doi":"10.1016/j.geomorph.2022.108524","title":"Deep learning for pockmark detection: Implications for quantitative seafloor characterization","year":2022,"lang":"en","type":"article","venue":"Geomorphology","topic":"Underwater Acoustics Research","field":"Earth and Planetary Sciences","cited_by":13,"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; Bathymetry; Seafloor spreading; Oceanography","score_opus":0.03920293585092755,"score_gpt":0.28728654789880165,"score_spread":0.2480836120478741,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4308928312","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.09120462,0.00003867225,0.90523297,0.0016356718,0.0003048282,0.0007328706,0.0006791046,0.00004468937,0.00012657836],"genre_scores_gemma":[0.98863304,0.000009486033,0.00536936,0.0003496959,0.00007989076,0.00023867222,0.004807285,0.000007988653,0.00050460617],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99902815,0.00013246805,0.00015222307,0.00026439517,0.00009206555,0.00033069245],"domain_scores_gemma":[0.9991462,0.00048850843,0.00007574569,0.00010912954,0.00012123617,0.00005914718],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00039490534,0.000076993536,0.00011604595,0.00012609632,0.0009770173,0.000030639254,0.00017011122,0.000040530867,0.001573995],"category_scores_gemma":[0.00012412189,0.000081075144,0.000047371886,0.00020715332,0.00005788241,0.00007345166,0.000025107836,0.00015534059,0.000036575282],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014638626,0.00012251944,0.12005357,0.00011009899,0.00015401276,0.000009380075,0.0012800362,0.500103,0.14956845,0.00056125695,0.001066621,0.22550721],"study_design_scores_gemma":[0.0009582592,0.0020059247,0.20542884,0.0000011280536,0.000033788696,0.000129508,0.0005781523,0.6964908,0.0007739198,0.0033164714,0.09003891,0.00024423748],"about_ca_topic_score_codex":0.00014159818,"about_ca_topic_score_gemma":0.00048335348,"teacher_disagreement_score":0.8998636,"about_ca_system_score_codex":0.00001752068,"about_ca_system_score_gemma":0.000037605743,"threshold_uncertainty_score":0.9993387},"labels":[],"label_agreement":null},{"id":"W4318035603","doi":"10.1016/j.geomorph.2023.108604","title":"Characterizing the response of the coastal Rio Grande to upstream damming","year":2023,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Institute for Advanced Research","funders":"","keywords":"Tributary; Geology; Hydrology (agriculture); Channel (broadcasting); Sediment transport; Floodplain; Sediment; Alluvium; Erosion; Subaerial; Alluvial fan; Bathymetry; Sedimentary budget; Geomorphology; Oceanography; Geochemistry; Geotechnical engineering; Geography","score_opus":0.01148709833279622,"score_gpt":0.2267085288128367,"score_spread":0.2152214304800405,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4318035603","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":[0.9921228,0.0000046732143,0.00004903812,0.0067260126,0.00021098818,0.0001552781,0.000026798556,0.000032167853,0.0006721933],"genre_scores_gemma":[0.9971533,0.0000063604152,0.000019646139,0.0016245634,0.000017200693,0.000021642221,0.000010677681,0.0000073032857,0.0011393357],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99910706,0.00014156035,0.00015912954,0.00018815718,0.00013436726,0.00026974737],"domain_scores_gemma":[0.99942684,0.00020298161,0.000056057273,0.000271385,0.000004594781,0.000038140457],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007009692,0.00008396018,0.00011574156,0.000025945765,0.0002143232,0.000004255602,0.00038884734,0.00006365183,0.001434596],"category_scores_gemma":[0.00008219266,0.000048772356,0.000046139172,0.00037684522,0.00038410723,0.000042410968,0.00018780408,0.00012508396,0.00066913205],"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":[0.0007589075,0.000054757784,0.5172222,0.000007524882,0.000023339762,0.00007122153,0.004763023,0.0012350036,0.4706286,0.000061804334,0.0034655756,0.0017080192],"study_design_scores_gemma":[0.00025612675,0.00009786388,0.89846486,0.0000070313004,0.000016922531,0.000046159425,0.0001765265,0.000030020701,0.040558103,0.00015765081,0.06010332,0.00008539768],"about_ca_topic_score_codex":0.00018365339,"about_ca_topic_score_gemma":0.00048088716,"teacher_disagreement_score":0.4300705,"about_ca_system_score_codex":0.0000064998785,"about_ca_system_score_gemma":0.000013001597,"threshold_uncertainty_score":0.9994782},"labels":[],"label_agreement":null},{"id":"W4319756605","doi":"10.1016/j.geomorph.2023.108618","title":"Intra- and Inter-site variability of the beach dune profile and vegetation line: Is there a scale-invariant profile?","year":2023,"lang":"en","type":"article","venue":"Geomorphology","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Windsor","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Plage; Shore; Foredune; Overwash; Storm; Sediment transport; Sea level; Barrier island; Geomorphology; Sand dune stabilization; Oceanography; Sediment","score_opus":0.008629876057264391,"score_gpt":0.21519924550831834,"score_spread":0.20656936945105395,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4319756605","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":[0.99661297,0.00034766653,0.0001395128,0.0014568086,0.00019923579,0.00030788995,0.0001592005,0.000026968475,0.00074975507],"genre_scores_gemma":[0.9989813,0.000052669515,0.00027798236,0.0002650365,0.000044448945,0.000005464372,0.00011491837,0.0000033817212,0.0002548239],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99911064,0.00014518047,0.0001743589,0.00026488176,0.000090739646,0.00021418894],"domain_scores_gemma":[0.99944156,0.0001934063,0.000089842084,0.0001758878,0.000042434967,0.000056850036],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048975175,0.00010191255,0.00017635117,0.000037728772,0.00010348737,0.000017555129,0.00010906445,0.000102062906,0.0006280776],"category_scores_gemma":[0.00010024812,0.00006544355,0.000024964538,0.00026975555,0.00026774866,0.000076741504,0.00004663539,0.00013644825,0.00007473724],"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":[0.00007581122,0.000018809638,0.9735558,0.00040702528,0.0000227156,0.000015590591,0.0017348786,0.00009653174,0.0008253852,0.00008184153,0.0017039473,0.02146169],"study_design_scores_gemma":[0.00029117856,0.00020130356,0.95627236,0.00003921035,0.00002321468,0.00007862764,0.000103119964,0.039678708,0.00090449874,0.0017810749,0.0005341081,0.00009256102],"about_ca_topic_score_codex":0.00071398995,"about_ca_topic_score_gemma":0.0007093332,"teacher_disagreement_score":0.039582178,"about_ca_system_score_codex":0.0000016965452,"about_ca_system_score_gemma":0.00003618269,"threshold_uncertainty_score":0.68770087},"labels":[],"label_agreement":null},{"id":"W4320169050","doi":"10.1016/j.geomorph.2023.108591","title":"Revising supraglacial rock avalanche magnitudes and frequencies in Glacier Bay National Park, Alaska","year":2023,"lang":"en","type":"article","venue":"Geomorphology","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ministry of Forests; University of Calgary","funders":"National Oceanic and Atmospheric Administration; U.S. Geological Survey; Universität Zürich; Newcastle University","keywords":"Permafrost; Debris; Geology; Glacier; Glacial period; Physical geography; National park; Rock glacier; Landslide; Geomorphology; Landform; Bay; Climate change; Arctic; Oceanography; Archaeology; Geography","score_opus":0.032990903977771935,"score_gpt":0.24580896408510425,"score_spread":0.2128180601073323,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4320169050","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":[0.99503815,0.00086084363,0.000029884835,0.0014507275,0.00031181634,0.00009685806,0.00008815593,0.000042356784,0.0020812186],"genre_scores_gemma":[0.9974414,0.0005228419,0.00035434967,0.0006832778,0.00013969983,0.0000035675755,0.00023614768,0.0000029600892,0.00061572634],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990835,0.000053355594,0.00018425286,0.000225679,0.00015666083,0.00029655203],"domain_scores_gemma":[0.9994972,0.00029778847,0.00004064951,0.00006998002,0.000049282215,0.000045097306],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00035622864,0.00009603681,0.00016143578,0.00006269476,0.00017347971,0.000029308201,0.00008721592,0.00006513874,0.0024403364],"category_scores_gemma":[0.00022031169,0.000085628606,0.000024287323,0.000421433,0.00008805021,0.00009740172,0.000027682545,0.000109305714,0.00041535197],"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":[0.000009431747,0.0000048727247,0.9899059,0.000009307608,0.000007906549,0.000039866285,0.00029408536,0.0010587698,0.000041286195,0.00012594652,0.0058602756,0.0026423787],"study_design_scores_gemma":[0.00022699058,0.000035169967,0.9577091,0.000007091862,0.000004560802,0.000028788534,0.00034142248,0.0014855234,0.0000040671384,0.0011463688,0.038912125,0.00009880204],"about_ca_topic_score_codex":0.00080201577,"about_ca_topic_score_gemma":0.007381102,"teacher_disagreement_score":0.03305185,"about_ca_system_score_codex":0.0000069633934,"about_ca_system_score_gemma":0.000045858465,"threshold_uncertainty_score":0.99847156},"labels":[],"label_agreement":null},{"id":"W4323031139","doi":"10.1016/j.geomorph.2023.108642","title":"Coastal cliff evolution: Modelling the long-term interplay between marine erosion, initial topography, and uplift in an arid environment","year":2023,"lang":"en","type":"article","venue":"Geomorphology","topic":"Coastal and Marine Dynamics","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Fondo Nacional de Desarrollo Científico y Tecnológico; Prix Inspiration Arctique; Agencia Nacional de Investigación y Desarrollo","keywords":"Cliff; Geology; Erosion; Arid; Geomorphology; Tectonic uplift; Sea level; Terrace (agriculture); Aeolian processes; Tectonics; Coastal erosion; Oceanography; Paleontology; Physical geography; Geography","score_opus":0.018441273875539746,"score_gpt":0.24374921026700397,"score_spread":0.22530793639146424,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4323031139","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":[0.99567074,0.000033254175,0.0030545925,0.00032856458,0.00022219929,0.00015908905,0.00022794017,0.000036946527,0.00026665998],"genre_scores_gemma":[0.9976746,0.00011832369,0.00009179763,0.00008959466,0.00012770554,0.000003369124,0.0017705531,0.000004492267,0.000119551216],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989041,0.00008891547,0.00023046863,0.0003042002,0.00012378223,0.00034854418],"domain_scores_gemma":[0.9995308,0.000121599885,0.000048937567,0.00019056752,0.000009685397,0.00009841626],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002906964,0.00013694547,0.00017498656,0.00013437064,0.00014428762,0.000033240583,0.00018890025,0.00008503413,0.0007914227],"category_scores_gemma":[0.0000054594857,0.00010393423,0.00003651518,0.0001931657,0.00025591566,0.00011583713,0.00020660549,0.0002295665,0.00009866474],"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":[0.000052766973,0.000013746524,0.96617216,0.0000059918834,0.000007134241,0.00008405591,0.00010823396,0.011171695,0.000012171943,0.00006052188,0.00003156897,0.022279939],"study_design_scores_gemma":[0.00031418563,0.00023148354,0.9460105,0.000005160742,0.000012151444,0.00005887446,0.00007806752,0.051188637,0.0000030933932,0.0017674544,0.00020462209,0.00012578558],"about_ca_topic_score_codex":0.00758694,"about_ca_topic_score_gemma":0.035735156,"teacher_disagreement_score":0.04001694,"about_ca_system_score_codex":0.0000043309637,"about_ca_system_score_gemma":0.000016768097,"threshold_uncertainty_score":0.99902165},"labels":[],"label_agreement":null},{"id":"W4362472164","doi":"10.1016/j.geomorph.2023.108667","title":"Hydration caves and cavities from the recent weathering zone of anhydrites at Dingwall (Nova Scotia, Canada)","year":2023,"lang":"en","type":"article","venue":"Geomorphology","topic":"Karst Systems and Hydrogeology","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Uniwersytet Warszawski; Wydział Chemii, Uniwersytet Warszawski; Ministerstwo Edukacji i Nauki; Politechnika Warszawska","keywords":"Cave; Geology; Anhydrite; Weathering; Gypsum; Halite; Breccia; Geomorphology; Landform; Geochemistry; Mineralogy; Paleontology; Archaeology","score_opus":0.016379969520282915,"score_gpt":0.18857119290038096,"score_spread":0.17219122338009804,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4362472164","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":[0.9949521,0.0014355229,0.0000071126474,0.0020314122,0.0006322408,0.00009994285,0.00028774247,0.00001929178,0.0005346673],"genre_scores_gemma":[0.99853235,0.00019223985,0.00002666347,0.0003142913,0.00008556543,6.836086e-7,0.00035068401,0.0000033166762,0.0004941716],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991363,0.0000918454,0.00020175328,0.00019387806,0.00012969863,0.00024646893],"domain_scores_gemma":[0.9993345,0.0003499595,0.000092140086,0.00015255902,0.000023881923,0.000046951136],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021233615,0.00009438438,0.00020144487,0.00003586371,0.0001321908,0.000010970071,0.000120854595,0.00006874766,0.0021889696],"category_scores_gemma":[0.000036797308,0.000067828805,0.000016939552,0.00013000364,0.00018373864,0.00004017668,0.00003583376,0.00007398731,0.000081143575],"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":[0.000020050247,0.0000023583916,0.98806554,0.000008898522,0.000027757433,0.00004710497,0.000837676,0.00082420954,0.0017637452,0.000046563073,0.006169596,0.0021865196],"study_design_scores_gemma":[0.00021553658,0.00007702674,0.966265,0.000014846505,0.000015761112,0.00007618071,0.00069961976,0.0020619314,0.00086043973,0.00021948357,0.029378068,0.000116076975],"about_ca_topic_score_codex":0.9350328,"about_ca_topic_score_gemma":0.9906274,"teacher_disagreement_score":0.055594623,"about_ca_system_score_codex":0.000007954831,"about_ca_system_score_gemma":0.00006565011,"threshold_uncertainty_score":0.99872315},"labels":[],"label_agreement":null},{"id":"W4362721878","doi":"10.1016/j.geomorph.2023.108694","title":"Distribution and morphometry of pingos, western Canadian Arctic, Northwest Territories, Canada","year":2023,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Carleton University; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Arctic; Physical geography; Geomorphology; Oceanography; Geography","score_opus":0.012231666296195516,"score_gpt":0.21219692155297343,"score_spread":0.1999652552567779,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4362721878","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":[0.99437714,0.0002464784,0.000002570234,0.0022225217,0.0005300121,0.00008357799,0.0023106018,0.000016008238,0.00021110484],"genre_scores_gemma":[0.9928683,0.00008644924,0.000010823859,0.000246401,0.00004148171,0.0000015965761,0.0065913214,0.0000021052251,0.00015154055],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99884975,0.00010180187,0.00017537091,0.00022036232,0.00011854541,0.00053417525],"domain_scores_gemma":[0.9992329,0.00024742275,0.000048280323,0.00016043751,0.00006979453,0.00024120627],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026019834,0.000098185934,0.0002117094,0.00013773519,0.00018052975,0.000007731672,0.00016387778,0.00014586361,0.0009011058],"category_scores_gemma":[0.00012833058,0.00009378053,0.000016258879,0.00038955605,0.0003436063,0.000042825133,0.000019827216,0.00019408895,0.00009019147],"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":[0.000013431204,0.0000021609485,0.9975842,0.000022371776,0.000016292312,0.00033318746,0.00002869641,0.000044421333,0.0000019497313,0.000042479864,0.0015756488,0.00033513457],"study_design_scores_gemma":[0.00016253135,0.000062547806,0.9811325,0.000004827652,0.00000750285,0.00034942344,0.000073482384,0.000088464425,0.000019544106,0.00010469431,0.017908506,0.00008599531],"about_ca_topic_score_codex":0.9986353,"about_ca_topic_score_gemma":0.9999572,"teacher_disagreement_score":0.016451746,"about_ca_system_score_codex":0.0000072737644,"about_ca_system_score_gemma":0.00065252074,"threshold_uncertainty_score":0.98664767},"labels":[],"label_agreement":null},{"id":"W4375869478","doi":"10.1016/j.geomorph.2023.108710","title":"Multi-decadal changes in river morphology in an urbanizing watershed: Highland Creek, Toronto, Canada","year":2023,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":20,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Stream power; Land cover; Hydrology (agriculture); Fluvial; Geology; Watershed; Channel (broadcasting); Flood myth; Drainage basin; Physical geography; Surface runoff; Land use; Streamflow; Floodplain; Structural basin; Erosion; Geomorphology; Geography; Cartography; Archaeology","score_opus":0.017027120756663735,"score_gpt":0.23105222768144273,"score_spread":0.214025106924779,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4375869478","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":[0.99808466,0.00008099947,0.0000148094905,0.0009872173,0.00029711728,0.00016503832,0.000029567653,0.000053745134,0.00028685317],"genre_scores_gemma":[0.99751616,0.000068680805,0.00019523352,0.0013286091,0.000029807885,0.00004657704,0.00021178197,0.000017441465,0.00058571866],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982109,0.00012283235,0.00024841703,0.00053872576,0.00014743562,0.00073170726],"domain_scores_gemma":[0.99955535,0.00005728938,0.000047897687,0.00022332199,0.0000055344954,0.00011061859],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003355622,0.00017343774,0.00028621798,0.00006281617,0.000079388876,0.000006804237,0.0003306106,0.00022244187,0.0077692247],"category_scores_gemma":[0.000016763146,0.00018073978,0.000016364002,0.00026915662,0.00027661913,0.00018911593,0.00010979365,0.00021350486,0.00019710494],"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":[0.00005356737,0.00008788304,0.97637755,0.0000073148954,0.0000056378453,0.002362926,0.0011938108,0.0019045763,0.015089963,0.0000063941657,0.0024080263,0.000502353],"study_design_scores_gemma":[0.001238228,0.00014719724,0.9861017,0.0000046486934,0.000006934537,0.000058199894,0.00025766453,0.0008990499,0.0009112573,0.000058634658,0.010069145,0.00024735444],"about_ca_topic_score_codex":0.8927154,"about_ca_topic_score_gemma":0.99859166,"teacher_disagreement_score":0.10587628,"about_ca_system_score_codex":0.00027320374,"about_ca_system_score_gemma":0.000046934387,"threshold_uncertainty_score":0.99313784},"labels":[],"label_agreement":null},{"id":"W4377965460","doi":"10.1016/j.geomorph.2023.108748","title":"Meta-analysis of a large bedload transport rate dataset","year":2023,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Deutsche Forschungsgemeinschaft","keywords":"Bed load; Hyperconcentrated flow; Sediment transport; Flume; Geology; Hydraulics; Hydrology (agriculture); Fluvial; Environmental science; Sediment; Structural basin; Flow (mathematics); Geomorphology; Geotechnical engineering; Mathematics","score_opus":0.05122460377807683,"score_gpt":0.2857018207509757,"score_spread":0.2344772169728989,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4377965460","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":[0.9893889,0.00010865743,0.00051422993,0.0009715383,0.000059094447,0.00012570708,0.00795302,0.000064245716,0.0008146113],"genre_scores_gemma":[0.98698884,0.00004346512,0.00005898507,0.0013054485,0.000004466803,0.000031556337,0.010924921,0.0000073704955,0.0006349262],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99869716,0.000083717896,0.00032101813,0.0003781365,0.00015324054,0.00036672226],"domain_scores_gemma":[0.99938196,0.000085980544,0.00009289768,0.00036697192,0.00000601342,0.00006617731],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00084300956,0.0001324421,0.00066773186,0.00015659048,0.000074646174,0.0000015159792,0.00029399703,0.00011554578,0.08073267],"category_scores_gemma":[0.000008809716,0.00010893236,0.0003259539,0.0013800452,0.00026384252,0.00009017094,0.000049868857,0.00010380969,0.0015385122],"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":[0.00037640915,0.0010607776,0.5496769,0.00007372245,0.24370156,0.0022601502,0.0025308763,0.06707607,0.031070236,0.0009063783,0.101061985,0.00020496146],"study_design_scores_gemma":[0.0010268688,0.00022149547,0.41654745,6.589683e-7,0.3102666,0.000018792522,0.000081163336,0.001319171,0.0054906183,0.00066366734,0.26385662,0.00050690403],"about_ca_topic_score_codex":0.00037020352,"about_ca_topic_score_gemma":0.0015736383,"teacher_disagreement_score":0.16279462,"about_ca_system_score_codex":0.000006670866,"about_ca_system_score_gemma":0.000008034715,"threshold_uncertainty_score":0.9992389},"labels":[],"label_agreement":null},{"id":"W4378717945","doi":"10.1016/j.geomorph.2023.108754","title":"Permafrost degradation in the ice-wedge tundra terrace of Paulatuk Peninsula (Darnley Bay, Canada)","year":2023,"lang":"en","type":"article","venue":"Geomorphology","topic":"Climate change and permafrost","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":"Center for Northern Studies; Natural Resources Canada","funders":"Horizon 2020 Framework Programme; Natural Resources Canada; Crown-Indigenous Relations and Northern Affairs Canada; European Commission","keywords":"Permafrost; Tundra; Thermokarst; Arctic; Geology; Physical geography; Bay; Oceanography; Geography","score_opus":0.037754493680565514,"score_gpt":0.2409889899897902,"score_spread":0.2032344963092247,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4378717945","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":[0.98786074,0.00022524496,0.000004681688,0.0028117904,0.00049988047,0.00016810537,0.0059670676,0.000015453028,0.002447014],"genre_scores_gemma":[0.9866363,0.00011284393,0.000010514234,0.0009432128,0.00007999679,0.0000031943127,0.011786168,0.0000039988886,0.000423813],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988176,0.000115835646,0.0002421994,0.00020749052,0.00024646774,0.00037040346],"domain_scores_gemma":[0.99925286,0.0003445866,0.00008517088,0.00023445043,0.000031932435,0.000050984054],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004183031,0.00011739996,0.00018879367,0.00010742477,0.00011804241,0.000019063997,0.00030994718,0.00008378945,0.005319469],"category_scores_gemma":[0.000053952215,0.00008731279,0.000033357333,0.00050460396,0.00011203692,0.0000988994,0.00002224744,0.00016779236,0.00019101152],"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":[0.000034376008,0.00001323984,0.9748882,0.000020668678,0.000005955314,0.00020139244,0.0012471341,0.00032889322,0.0015670961,0.0000396033,0.020890309,0.000763155],"study_design_scores_gemma":[0.00030575227,0.0000549685,0.9675377,0.000008588347,0.000008488631,0.00014391229,0.0017362518,0.001943233,0.00006189782,0.0000660961,0.028021324,0.0001117758],"about_ca_topic_score_codex":0.60393244,"about_ca_topic_score_gemma":0.9816105,"teacher_disagreement_score":0.37767807,"about_ca_system_score_codex":0.000008235165,"about_ca_system_score_gemma":0.00013980678,"threshold_uncertainty_score":0.9955898},"labels":[],"label_agreement":null},{"id":"W4379879740","doi":"10.1016/j.geomorph.2023.108781","title":"Recent basement fault reactivation and fluvial drainage modification in an intraplate setting, eastern Bundelkhand Craton, Madhya Pradesh, India","year":2023,"lang":"en","type":"article","venue":"Geomorphology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; Queen's University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Monocline; Fluvial; Basement; Geomorphology; Fault (geology); Paleontology; Craton; Archean; Palaeochannel; Precambrian; Geochemistry; Structural basin; Tectonics","score_opus":0.030555739589969797,"score_gpt":0.26209779432215047,"score_spread":0.23154205473218067,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4379879740","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":[0.99660176,0.00021822541,0.00003690477,0.0013131945,0.000216567,0.00026340896,0.000060868824,0.0000659629,0.0012231072],"genre_scores_gemma":[0.99801695,0.00051690894,0.000103710045,0.0002982906,0.000070590904,0.000009007902,0.0008649394,0.000004536164,0.0001150332],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99874026,0.00015384663,0.00024666885,0.0003640619,0.00014515892,0.00034999457],"domain_scores_gemma":[0.99950445,0.00012232208,0.00009976047,0.00016302803,0.000036865968,0.00007359196],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00053235714,0.00013175698,0.0001659086,0.00020218568,0.00015972748,0.000042750566,0.00009351393,0.000103437065,0.00056706864],"category_scores_gemma":[0.000065606284,0.00012156754,0.000014576651,0.0003369937,0.00009836913,0.00019521732,0.000022487257,0.0001681846,0.0001986469],"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":[0.00009181464,0.000032974363,0.717466,0.000015757705,0.000018585604,0.00009962861,0.0017963038,0.00033529248,0.00075521035,0.0001142247,0.0005047856,0.27876946],"study_design_scores_gemma":[0.00059824437,0.00024908318,0.9852761,0.00001050758,0.000008274153,0.00002456923,0.0006239195,0.0067099654,0.00023766184,0.001088716,0.005028765,0.00014417867],"about_ca_topic_score_codex":0.0013133212,"about_ca_topic_score_gemma":0.00795248,"teacher_disagreement_score":0.27862528,"about_ca_system_score_codex":0.000008383335,"about_ca_system_score_gemma":0.000032860982,"threshold_uncertainty_score":0.6209004},"labels":[],"label_agreement":null},{"id":"W4380319595","doi":"10.1016/j.geomorph.2023.108783","title":"The 51st Binghamton Geomorphology Symposium: An introduction to the special issue “Geomorphology in the Anthropocene”","year":2023,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Biogeoscience Institute, University of Calgary","keywords":"Anthropocene; Geology; Climate change; Theme (computing); Earth science; Natural (archaeology); Earth system science; Environmental ethics; Geomorphology; Oceanography; Paleontology","score_opus":0.007885956760795353,"score_gpt":0.24379200439959586,"score_spread":0.23590604763880052,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4380319595","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":[0.74439955,0.000063868,0.000050552484,0.24339904,0.0066979546,0.000914064,0.00006862944,0.000102347694,0.0043040104],"genre_scores_gemma":[0.9661049,0.0013762951,0.00009535594,0.011471977,0.014194513,0.00034488068,0.00064291194,0.000100754485,0.0056683565],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9960164,0.000920278,0.00054550514,0.00088262017,0.00043066306,0.0012045664],"domain_scores_gemma":[0.9980556,0.00037311582,0.0001649987,0.0012418582,0.00002831286,0.00013614252],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0026969353,0.0003319387,0.00035216822,0.00012982247,0.0012163896,0.000102607,0.0015251943,0.00037070454,0.011136625],"category_scores_gemma":[0.0001576879,0.00016611691,0.00010270989,0.0015077313,0.0015052537,0.00013723846,0.00061582995,0.00081551296,0.009380891],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026831325,0.00015106556,0.009932489,0.0000030285469,0.000030740943,0.000599213,0.0024230424,0.008989937,0.0050332127,0.0009906238,0.9626107,0.008967603],"study_design_scores_gemma":[0.00057832646,0.0005770941,0.038970657,0.000002738818,0.000032986474,0.0014375148,0.001202044,0.00039588913,0.00038973146,0.000754117,0.95539874,0.00026016813],"about_ca_topic_score_codex":0.002370212,"about_ca_topic_score_gemma":0.0058417106,"teacher_disagreement_score":0.23192707,"about_ca_system_score_codex":0.00016729138,"about_ca_system_score_gemma":0.000034402212,"threshold_uncertainty_score":0.9913904},"labels":[],"label_agreement":null},{"id":"W4385766912","doi":"10.1016/j.geomorph.2023.108862","title":"Morphometric analysis of the North Liuleng Shan Fault in the northern Shanxi Graben System, China: Insights into active deformation pattern and fault evolution","year":2023,"lang":"en","type":"article","venue":"Geomorphology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University; University of Toronto","funders":"National Key Research and Development Program of China; China Scholarship Council; University of Toronto; National Natural Science Foundation of China","keywords":"Geology; Sinuosity; Graben; Fault (geology); Structural basin; Active fault; Half-graben; Geomorphology; Echelon formation; Strike-slip tectonics; Fault scarp; Seismology; Tectonics; Plateau (mathematics); Quaternary; Paleontology","score_opus":0.01063620591043577,"score_gpt":0.20409182772009057,"score_spread":0.1934556218096548,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385766912","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":[0.9981626,0.00066461816,0.00008433441,0.00023605948,0.00016240795,0.00026315203,0.00010948424,0.00002872213,0.0002886006],"genre_scores_gemma":[0.9994203,0.00017153694,0.0000041102444,0.00006700937,0.000027359358,0.0000084697895,0.00028673993,0.0000027707358,0.000011700638],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998619,0.00027630455,0.00030246805,0.00024160165,0.00027164322,0.00028893896],"domain_scores_gemma":[0.99918026,0.00028076,0.00019135282,0.00026063612,0.000057613823,0.000029367979],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037845856,0.00014013374,0.0003091648,0.00068521063,0.0002814326,0.000018276505,0.0002838031,0.00008505946,0.00004219653],"category_scores_gemma":[0.00009069276,0.00007717496,0.00009323699,0.0041381256,0.00014558318,0.00012397378,0.00005032743,0.0002025108,0.000052694126],"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":[0.000012418085,0.00000965784,0.9734459,0.00002571881,0.00016581504,0.00001079703,0.0052970774,0.005252848,0.0000056254357,0.00002448743,0.00001779549,0.015731841],"study_design_scores_gemma":[0.00021281793,0.00008130604,0.97365,0.0000114174745,0.00015905839,0.000012977364,0.003482722,0.022149626,0.000008220496,0.00009302586,0.000050919163,0.000087946406],"about_ca_topic_score_codex":0.03528089,"about_ca_topic_score_gemma":0.43660027,"teacher_disagreement_score":0.40131938,"about_ca_system_score_codex":0.000020290285,"about_ca_system_score_gemma":0.000027969942,"threshold_uncertainty_score":0.97114325},"labels":[],"label_agreement":null},{"id":"W4386318706","doi":"10.1016/j.geomorph.2023.108886","title":"Subglacial deformation of permafrost beneath Wright Lower Glacier, Antarctica as revealed by direct observations and measurements from a subglacial tunnel","year":2023,"lang":"en","type":"article","venue":"Geomorphology","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Marsden Fund; Natural Sciences and Engineering Research Council of Canada; University of Otago","keywords":"Permafrost; Geology; Glacier; Geomorphology; Ice stream; Oceanography; Sea ice; Cryosphere","score_opus":0.03558243432875412,"score_gpt":0.227882875876424,"score_spread":0.1923004415476699,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386318706","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":[0.99443156,0.00046585436,0.000027578104,0.0007884282,0.0006633676,0.0002302204,0.0027635873,0.00005659983,0.000572829],"genre_scores_gemma":[0.9938691,0.0004647987,0.0002865344,0.0004841117,0.00011996746,0.000007977832,0.0044607176,0.0000063921275,0.0003003592],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99857974,0.00006105569,0.00037010948,0.00029886546,0.0003425129,0.00034770663],"domain_scores_gemma":[0.99922717,0.00017449225,0.00014525065,0.00018785066,0.00016494165,0.00010029143],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00034370477,0.00016358956,0.00030320184,0.00005150746,0.00037599832,0.000028677998,0.00015087385,0.00011034219,0.0021097793],"category_scores_gemma":[0.00016496313,0.00014530815,0.00006121837,0.0004965704,0.00018825197,0.00020647468,0.00003712764,0.000103178914,0.00015576997],"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":[0.0000997505,0.000028725899,0.984472,0.000009723494,0.000055099903,0.000009288573,0.00066202896,0.00008248316,0.0012255082,0.000020733069,0.012402389,0.00093230663],"study_design_scores_gemma":[0.000614328,0.00014612448,0.97846293,0.0000103423645,0.000051722265,0.0000072661696,0.0002716402,0.00058818253,0.00008820396,0.00036394922,0.019237198,0.00015810621],"about_ca_topic_score_codex":0.008250764,"about_ca_topic_score_gemma":0.0158565,"teacher_disagreement_score":0.007605736,"about_ca_system_score_codex":0.0000140894745,"about_ca_system_score_gemma":0.000068613466,"threshold_uncertainty_score":0.9988024},"labels":[],"label_agreement":null},{"id":"W4386570728","doi":"10.1016/j.geomorph.2023.108897","title":"Late Oligocene–Early Miocene incision of the Three Gorges and the initial establishment of an east-flowing Yangtze River","year":2023,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Key Laboratory of Tectonics and Petroleum Resources, Ministry of Education, China; Chengdu University of Technology; China Scholarship Council; Natural Science Foundation of Hubei Province; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Geology; Structural basin; Paleontology; Provenance; Three gorges; Fission track dating; Cenozoic; Geomorphology; Tectonics","score_opus":0.018969138551268874,"score_gpt":0.21630332922194553,"score_spread":0.19733419067067665,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386570728","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":[0.99772924,0.00019078517,0.000008307014,0.0013926546,0.00011943191,0.00009635409,0.000089845926,0.0000136823965,0.0003597235],"genre_scores_gemma":[0.9995012,0.00004553521,0.00009258048,0.00022402062,0.0000371174,0.0000010619831,0.000060586975,0.0000014834276,0.000036406218],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989789,0.00015610168,0.00024044208,0.00019740194,0.00019762987,0.00022949331],"domain_scores_gemma":[0.99930334,0.00028905188,0.000080339436,0.00021792376,0.00005146584,0.000057854726],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004953918,0.00009562429,0.0002590504,0.00004782669,0.00011024283,0.000010203349,0.00030658787,0.00007731603,0.0013126739],"category_scores_gemma":[0.00014325416,0.00004485962,0.00008951686,0.00041167962,0.0007680039,0.00006611697,0.000112574344,0.00012109927,0.000034594403],"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":[0.00026015614,0.000027977745,0.97599465,0.000013186854,0.00005618478,0.000024651685,0.00053454115,0.0020466258,0.0014208477,0.00014417796,0.000106127445,0.019370884],"study_design_scores_gemma":[0.0005359408,0.00010913337,0.97370327,0.0000070467395,0.0000471209,0.000010818828,0.00007121664,0.0043859864,0.0013346651,0.01962907,0.00010245611,0.00006328005],"about_ca_topic_score_codex":0.009622102,"about_ca_topic_score_gemma":0.0027903202,"teacher_disagreement_score":0.019484892,"about_ca_system_score_codex":9.918581e-7,"about_ca_system_score_gemma":0.000013030668,"threshold_uncertainty_score":0.9996003},"labels":[],"label_agreement":null},{"id":"W4387190862","doi":"10.1016/j.geomorph.2023.108919","title":"Identification of morphostructures by utilizing Knickpoint Ranks, a method to avoid the camouflage effect in knickpoint analysis","year":2023,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Universidade Federal do Paraná; Conselho Nacional de Desenvolvimento Científico e Tecnológico; Coordenação de Aperfeiçoamento de Pessoal de Nível Superior","keywords":"Geology; Lithology; Geomorphology; Paleontology","score_opus":0.005733602417939704,"score_gpt":0.26412260798842124,"score_spread":0.25838900557048156,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387190862","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":[0.99286133,0.0001049956,0.0051242276,0.001141381,0.00009168638,0.00037547568,0.00005305763,0.000046525896,0.00020133913],"genre_scores_gemma":[0.9988006,0.000025383497,0.00021395124,0.00048683773,0.000008662398,0.00008970641,0.00011409332,0.000011678093,0.00024911133],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99790376,0.0004446464,0.0005232044,0.00050116767,0.00023154069,0.00039570086],"domain_scores_gemma":[0.99893534,0.0004089141,0.00015327446,0.00042647554,0.000009673862,0.000066302484],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0024795115,0.00017109573,0.0004028541,0.00022687188,0.00011742088,0.00000950834,0.0004499414,0.00014996823,0.0036015988],"category_scores_gemma":[0.00012585947,0.00012702735,0.0001284663,0.0020797607,0.00025493064,0.000074274656,0.00013573522,0.00022318328,0.00048503472],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023328222,0.00007191849,0.15672107,0.00004589152,0.00022307168,0.00007938891,0.0021838155,0.04851437,0.7813271,0.00008405237,0.0050089085,0.005507109],"study_design_scores_gemma":[0.0011376581,0.00032150868,0.5986014,0.000012985332,0.0006028426,0.000030547806,0.00031960267,0.008633116,0.38378212,0.0017658361,0.004378165,0.00041422155],"about_ca_topic_score_codex":0.0014224802,"about_ca_topic_score_gemma":0.001043399,"teacher_disagreement_score":0.44188032,"about_ca_system_score_codex":0.000048456015,"about_ca_system_score_gemma":0.0000096409185,"threshold_uncertainty_score":0.99730927},"labels":[],"label_agreement":null},{"id":"W4388012007","doi":"10.1016/j.geomorph.2023.108950","title":"Morphosedimentary response of a fluvio-estuarine beach to interannual variability in landfast ice dynamics","year":2023,"lang":"en","type":"article","venue":"Geomorphology","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval","funders":"","keywords":"Geology; Beach morphodynamics; Fluvial; Hydrometeorology; Context (archaeology); Sea ice; Oceanography; Sediment; Physical geography; Sediment transport; Geomorphology; Meteorology; Precipitation; Geography; Structural basin; Paleontology","score_opus":0.008825442781544091,"score_gpt":0.23023767094770856,"score_spread":0.22141222816616446,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388012007","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":[0.9957889,0.0000063387884,0.00070129737,0.0017679713,0.00043579258,0.00022669973,0.0005189103,0.00004685198,0.00050726975],"genre_scores_gemma":[0.9969158,0.000008013878,0.00088509475,0.00063202844,0.00003761812,0.0000037571579,0.0011597198,0.0000056906842,0.00035226872],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99820465,0.00042053158,0.00038791492,0.00035080215,0.0001828706,0.0004532425],"domain_scores_gemma":[0.99845266,0.0010113274,0.00007215466,0.00029144913,0.000046848738,0.00012556207],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0021835442,0.00015088226,0.00031109914,0.0002658542,0.000067295354,0.0000077838795,0.0002974849,0.0001065934,0.0016090028],"category_scores_gemma":[0.00039051904,0.00014038899,0.000052006537,0.0007172558,0.0001767543,0.000082218234,0.00008258674,0.00023525457,0.00035982652],"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":[0.0015364757,0.000061214174,0.9851586,0.000023170178,0.000019503761,0.00024441152,0.0013399775,0.0034483236,0.0002094155,0.000081139675,0.0009130457,0.006964696],"study_design_scores_gemma":[0.0005772611,0.00042867154,0.96983504,0.000018629566,0.000013151903,0.00009435952,0.0014763989,0.026052605,0.00003568709,0.0004899376,0.0008118464,0.0001664076],"about_ca_topic_score_codex":0.011937713,"about_ca_topic_score_gemma":0.0066002575,"teacher_disagreement_score":0.022604283,"about_ca_system_score_codex":0.000028541279,"about_ca_system_score_gemma":0.00008290521,"threshold_uncertainty_score":0.99930364},"labels":[],"label_agreement":null},{"id":"W4388169122","doi":"10.1016/j.geomorph.2023.108946","title":"Stability and failure modes of slopes with anisotropic strength: Insights from discrete element models","year":2023,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":22,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Accessible Media; Université de Lorraine","keywords":"Isotropy; Anisotropy; Geometry; Instability; Transverse plane; Orientation (vector space); Perpendicular; Slope stability analysis; Geology; Transverse isotropy; Curvature; Deformation (meteorology); Brittleness; Discrete element method; Mechanics; Slope stability; Geotechnical engineering; Materials science; Physics; Structural engineering; Optics; Mathematics; Composite material","score_opus":0.010540699154423341,"score_gpt":0.2016930880379721,"score_spread":0.19115238888354874,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388169122","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":[0.99783534,0.00006289992,0.0007722295,0.00029051516,0.00003143853,0.00013123977,0.000102183774,0.000034596804,0.00073957595],"genre_scores_gemma":[0.9983686,0.0001201899,0.0012878304,0.000037229198,0.000010175827,0.000009711743,0.00008416852,0.000008944696,0.00007312736],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991209,0.000050185936,0.00016529443,0.00030503186,0.00015371802,0.00020485531],"domain_scores_gemma":[0.9995961,0.00004671947,0.00006177103,0.00022219749,0.0000071127965,0.00006608108],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000056412497,0.00011307175,0.00019170005,0.000022310049,0.00007000544,0.000008343515,0.00011390861,0.00008997442,0.0012114461],"category_scores_gemma":[0.0000046481737,0.00007126743,0.000022244987,0.000146084,0.00030202875,0.00010247113,0.0002065482,0.00009844036,0.00004261948],"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":[0.00097359216,0.0004822279,0.5643083,0.000103701226,0.0005662428,0.0004949306,0.010858624,0.11232408,0.28164998,0.009461507,0.006800395,0.01197646],"study_design_scores_gemma":[0.010198688,0.0033729973,0.56034,0.0001483126,0.00046314954,0.00009501307,0.007661516,0.1812743,0.103140876,0.10564453,0.025667977,0.0019926527],"about_ca_topic_score_codex":0.0014114723,"about_ca_topic_score_gemma":0.0014925128,"teacher_disagreement_score":0.1785091,"about_ca_system_score_codex":0.00002607076,"about_ca_system_score_gemma":0.000008487317,"threshold_uncertainty_score":0.99970156},"labels":[],"label_agreement":null},{"id":"W4388830863","doi":"10.1016/j.geomorph.2023.108978","title":"Geomorphology and Late Quaternary evolution of Lake Manicouagan, a deep impounded impact crater-fjord-lake of the eastern Canadian Shield hinterland","year":2023,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université Laval","funders":"","keywords":"Geology; Quaternary; Bathymetry; Geomorphology; Fjord; Glacial period; Paleontology; Landform; Impact crater; Oceanography","score_opus":0.0071118015871086794,"score_gpt":0.21491892871874743,"score_spread":0.20780712713163876,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388830863","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":[0.99721694,0.00007131069,0.00003709422,0.00072834926,0.00048099566,0.00024264534,0.00021192885,0.000021441123,0.0009892973],"genre_scores_gemma":[0.9982212,0.00006329972,0.000013059835,0.00014268566,0.000023526227,0.00000810424,0.000069774185,0.000019256353,0.0014390806],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99846077,0.0001354549,0.00039277624,0.0003207389,0.00016994208,0.00052029896],"domain_scores_gemma":[0.9991771,0.00005894232,0.00021372228,0.0003709077,0.000017855915,0.00016148429],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003667161,0.00019037374,0.0003774399,0.00012178467,0.000113154325,0.000012189093,0.0003370334,0.0002726178,0.0033925406],"category_scores_gemma":[0.000030336312,0.00012035874,0.0001271482,0.00031839573,0.00052015414,0.00007393277,0.00030669494,0.00022673744,0.00021400915],"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":[0.0001234004,0.000025577036,0.9892912,0.000014385592,0.00007698132,0.0001628995,0.000544356,0.000859522,0.0070902295,0.00003568516,0.0013356796,0.000440118],"study_design_scores_gemma":[0.001230473,0.00033650754,0.9880517,0.00002956826,0.00007118193,0.00063587446,0.00014441196,0.0046606464,0.00041883034,0.0015101554,0.0027058271,0.00020483731],"about_ca_topic_score_codex":0.15100767,"about_ca_topic_score_gemma":0.72118086,"teacher_disagreement_score":0.5701732,"about_ca_system_score_codex":0.000106038955,"about_ca_system_score_gemma":0.000059802733,"threshold_uncertainty_score":0.9975185},"labels":[],"label_agreement":null},{"id":"W4389003223","doi":"10.1016/j.geomorph.2023.109003","title":"Short communication: Perception of coastal barrier landscapes and implications for selection of landscape morphometrics","year":2023,"lang":"en","type":"article","venue":"Geomorphology","topic":"Land Use and Ecosystem Services","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Windsor; University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Morphometrics; Landform; Geology; Selection (genetic algorithm); Artificial intelligence; Ecology; Computer science; Biology; Paleontology","score_opus":0.01697499460860666,"score_gpt":0.25457400259548807,"score_spread":0.2375990079868814,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389003223","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":[0.99870294,0.000034403587,0.00029756306,0.00023090863,0.00002924658,0.00015967598,0.00015950606,0.000021858034,0.0003638653],"genre_scores_gemma":[0.99895024,0.00021963788,0.00046785385,0.000020911537,0.000012312846,0.000039593593,0.000246655,0.0000060361053,0.000036738813],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994918,0.000027372842,0.00017917593,0.00012843506,0.000056616365,0.00011656761],"domain_scores_gemma":[0.9996127,0.00011023141,0.000068388785,0.00015154734,0.000025348048,0.000031816064],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023889063,0.000054964585,0.00013706513,0.000085779226,0.00008390094,0.000004476948,0.000108578526,0.000066500295,0.00049540336],"category_scores_gemma":[0.000019027288,0.00004813019,0.00002826988,0.00042255834,0.00003048307,0.00006937874,0.000095794356,0.00003218702,0.0000241943],"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":[0.000018177447,0.000023008644,0.97885215,0.000026638145,0.0000111293875,1.03731026e-7,0.00014237512,0.00035602407,0.015448559,0.000047854523,0.0024401944,0.0026337807],"study_design_scores_gemma":[0.0002304918,0.00009024827,0.9939643,0.000004737008,0.000021249529,0.000019082492,0.00023242236,0.0027306655,0.00054033543,0.00019632844,0.0019120908,0.00005803955],"about_ca_topic_score_codex":0.00019498455,"about_ca_topic_score_gemma":0.0009963049,"teacher_disagreement_score":0.015112154,"about_ca_system_score_codex":0.000008031467,"about_ca_system_score_gemma":0.000004382545,"threshold_uncertainty_score":0.54243195},"labels":[],"label_agreement":null},{"id":"W4389340221","doi":"10.1016/j.geomorph.2023.109006","title":"Multi-dimensional approach for interpreting the structure of barrier island morphology","year":2023,"lang":"en","type":"article","venue":"Geomorphology","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo; University of Windsor","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Landform; Geology; Barrier island; Overwash; Ridge; Morphology (biology); Shore; Crest; Geomorphology; Paleontology; Oceanography","score_opus":0.01346283378319619,"score_gpt":0.2323686238107819,"score_spread":0.21890579002758573,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389340221","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":[0.99385315,0.00021812056,0.0038706912,0.0002730457,0.00046933367,0.00028855712,0.0008344033,0.000033506156,0.00015918913],"genre_scores_gemma":[0.994727,0.0000053208355,0.0036454268,0.0005750859,0.00008459882,0.000002441851,0.0007044471,0.000005133546,0.00025054408],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9990737,0.0000757716,0.00017878841,0.00024558566,0.000088456225,0.00033770362],"domain_scores_gemma":[0.9992365,0.0004095425,0.00009243412,0.00016302998,0.00004892231,0.00004957421],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000266434,0.000111791145,0.00020087864,0.000064067644,0.0001448569,0.000008367874,0.00024204967,0.00012370883,0.0014443409],"category_scores_gemma":[0.00015296738,0.00006917388,0.00006119651,0.0002014643,0.00023497442,0.00003764844,0.000032708733,0.0001351662,0.00005239228],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000990719,0.000060224498,0.48791695,0.0004741205,0.00026422922,0.00012651735,0.0028901992,0.3412286,0.059101187,0.00028868293,0.089031294,0.017627295],"study_design_scores_gemma":[0.0013465696,0.0004629232,0.12409899,0.0000150799915,0.000048737835,0.00048485957,0.00046419073,0.8643719,0.0030806093,0.001624379,0.0037095493,0.0002922268],"about_ca_topic_score_codex":0.00032598746,"about_ca_topic_score_gemma":0.00038850063,"teacher_disagreement_score":0.5231433,"about_ca_system_score_codex":0.000001371709,"about_ca_system_score_gemma":0.000034659042,"threshold_uncertainty_score":0.99946845},"labels":[],"label_agreement":null},{"id":"W4389375633","doi":"10.1016/j.geomorph.2023.109002","title":"Response of a small, forested stream to a large input of sediment","year":2023,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":6,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; University of British Columbia; Canada Foundation for Innovation","keywords":"Sediment; Bed load; Channel (broadcasting); Hydrology (agriculture); Geology; Sediment transport; Beach morphodynamics; Flood myth; Debris; Sedimentary budget; Geomorphology; Geotechnical engineering; Oceanography; Geography","score_opus":0.014758805036390038,"score_gpt":0.24256063760403393,"score_spread":0.22780183256764389,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389375633","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":[0.998036,0.000011998581,0.00037784112,0.0007874335,0.000077164295,0.00019101695,0.000079718346,0.000040266943,0.00039851558],"genre_scores_gemma":[0.9985209,0.0000075407784,0.00028366724,0.0005807621,0.000005343487,0.000028571236,0.000043798886,0.000008396464,0.00052103394],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99895597,0.00008971195,0.00026446267,0.00023530901,0.0001345952,0.00031992825],"domain_scores_gemma":[0.9994685,0.00013793957,0.00007668037,0.00022876899,0.000011238504,0.00007687131],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006665353,0.00009526704,0.00021842224,0.00010005567,0.000038572987,9.914762e-7,0.00022208603,0.00010903328,0.0035327347],"category_scores_gemma":[0.00007444281,0.00008847676,0.00004196522,0.00050910475,0.00018284103,0.000032800443,0.00013736168,0.00006924689,0.00058194424],"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":[0.0032473905,0.00055675,0.65836835,0.000052138486,0.00007174112,0.00028306263,0.0031356423,0.006689391,0.31541085,0.0002535049,0.01088001,0.001051206],"study_design_scores_gemma":[0.0016231376,0.0016193843,0.84886473,0.000020845018,0.000041157095,0.000024861845,0.00018582305,0.0003117006,0.11094074,0.0004916828,0.035664514,0.00021141436],"about_ca_topic_score_codex":0.0001548127,"about_ca_topic_score_gemma":0.0003131915,"teacher_disagreement_score":0.2044701,"about_ca_system_score_codex":0.000017697615,"about_ca_system_score_gemma":0.000020833433,"threshold_uncertainty_score":0.9973782},"labels":[],"label_agreement":null},{"id":"W4389789270","doi":"10.1016/j.geomorph.2023.109025","title":"Statistical perspectives on the ripple index from a case study of aeolian megaripples","year":2023,"lang":"en","type":"article","venue":"Geomorphology","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Context (archaeology); Metric (unit); Statistic; Bedform; Mathematics; Statistics; Geology; Geomorphology","score_opus":0.023272222566599114,"score_gpt":0.25096242389113455,"score_spread":0.22769020132453544,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389789270","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":[0.9978229,0.00009070951,0.00009764564,0.00040852086,0.00015538195,0.00024408325,0.00052783714,0.000038955728,0.00061395665],"genre_scores_gemma":[0.99954677,0.000014057954,0.00003818696,0.00014046278,0.00006982409,0.00000527308,0.00009689897,0.000003887796,0.000084652405],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99894476,0.00018426449,0.00015688057,0.0002822963,0.00016581187,0.00026600357],"domain_scores_gemma":[0.99853635,0.0010647225,0.00006363238,0.00023327622,0.000032519954,0.00006948457],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00025042903,0.00011239114,0.00019688946,0.00006985178,0.00017183229,0.000016877779,0.00018473052,0.00005941855,0.005391525],"category_scores_gemma":[0.00014841804,0.00007108459,0.000025575591,0.00029318195,0.00020547915,0.000033833112,0.000026108792,0.00016748309,0.0005030525],"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":[0.0003276516,0.0002906676,0.9178145,0.00002169205,0.00016548623,0.016235022,0.028945545,0.0066288454,0.00002358157,0.00127334,0.01848509,0.00978856],"study_design_scores_gemma":[0.0008627059,0.0016453381,0.8056281,0.00000855721,0.00004405445,0.0006606576,0.16503242,0.021353988,0.000024908317,0.0036088463,0.00093455997,0.00019582684],"about_ca_topic_score_codex":0.057635803,"about_ca_topic_score_gemma":0.026227577,"teacher_disagreement_score":0.13608687,"about_ca_system_score_codex":0.0000025656088,"about_ca_system_score_gemma":0.000031318228,"threshold_uncertainty_score":0.9955177},"labels":[],"label_agreement":null},{"id":"W4392504388","doi":"10.1016/j.geomorph.2024.109121","title":"Repeated failures of the giant Beshkiol Landslide and their impact on the long-term Naryn Basin floodings, Kyrgyz Tien Shan","year":2024,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Université de Versailles Saint-Quentin-en-Yvelines; Institut de Radioprotection et de SÛreté Nucléaire; Centre National d’Etudes Spatiales; Centre National de la Recherche Scientifique; Aix-Marseille Université","keywords":"Geology; Landslide; Drainage basin; Fluvial; Structural basin; Hydrology (agriculture); Flood myth; River terraces; Erosion; Geomorphology; Physical geography; Archaeology; Geography","score_opus":0.007382672777602016,"score_gpt":0.2193207020016344,"score_spread":0.21193802922403238,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392504388","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":[0.9931957,0.00034518584,0.000018669922,0.0039124517,0.0002749185,0.0002256433,0.00008058599,0.000035121797,0.0019117359],"genre_scores_gemma":[0.9984923,0.00012125759,0.000010972218,0.00039987377,0.000042653355,0.000008457255,0.000017435917,0.000017296068,0.0008897284],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989306,0.00012372826,0.0001967657,0.00031163087,0.00013962333,0.00029768446],"domain_scores_gemma":[0.9993298,0.00016648811,0.000064043925,0.00037253386,0.000006359783,0.000060780432],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00034739924,0.00018687765,0.00020322105,0.000032024418,0.00015938364,0.000040425406,0.00031552938,0.00015254573,0.0027932995],"category_scores_gemma":[0.000032498105,0.00006859257,0.00012771842,0.0002126984,0.00042087716,0.0000517588,0.00027706785,0.00032113143,0.00012575061],"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":[0.00052187446,0.00030039594,0.7189904,0.00009873394,0.00077658467,0.00074418355,0.007704534,0.0015472588,0.15080893,0.001423616,0.08653447,0.03054906],"study_design_scores_gemma":[0.00063352904,0.0006659643,0.95447475,0.00022476386,0.00010167601,0.0011793155,0.00022826072,0.0016572217,0.023694228,0.0009496905,0.015834715,0.00035586942],"about_ca_topic_score_codex":0.00075490744,"about_ca_topic_score_gemma":0.00014894936,"teacher_disagreement_score":0.2354844,"about_ca_system_score_codex":0.000053911357,"about_ca_system_score_gemma":0.000017270075,"threshold_uncertainty_score":0.9981183},"labels":[],"label_agreement":null},{"id":"W4393857501","doi":"10.1016/j.geomorph.2024.109184","title":"Geomorphological signature of topographically controlled ice flow-switching at a glacier margin: Breiðamerkurjökull (Iceland) as a modern analogue for palaeo-ice sheets","year":2024,"lang":"en","type":"article","venue":"Geomorphology","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":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"UK Research and Innovation; Quaternary Research Association; British Society for Geomorphology","keywords":"Geology; Meltwater; Deglaciation; Ice stream; Geomorphology; Ice sheet; Ice divide; Landform; Glacier; Glacier morphology; Glacial landform; Cryosphere; Glacial period; Physical geography; Moraine; Climatology; Sea ice","score_opus":0.015100155188323775,"score_gpt":0.23196932555247482,"score_spread":0.21686917036415104,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4393857501","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":[0.9649165,0.011812218,0.013698054,0.0031137303,0.001500018,0.00123914,0.0013030143,0.00016014802,0.0022571238],"genre_scores_gemma":[0.99309456,0.00040534828,0.002462222,0.0021562714,0.0002572676,0.000046077792,0.0009055281,0.0000146764805,0.0006580566],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9975391,0.00016126155,0.0006005633,0.00070821895,0.00030470573,0.0006861446],"domain_scores_gemma":[0.997371,0.0018106428,0.00015996849,0.00031620282,0.00016607903,0.00017608964],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007408805,0.00033749285,0.00082095515,0.00011261702,0.00034935153,0.000058942955,0.00036208727,0.0003817262,0.006985205],"category_scores_gemma":[0.00031043423,0.00024752232,0.00041228518,0.0005441556,0.00025811538,0.00010391599,0.00007463034,0.00041242462,0.00012509018],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.026323965,0.0010022988,0.45787978,0.0018165986,0.0071995794,0.008623047,0.01214852,0.10427998,0.027080154,0.011402114,0.14110076,0.20114319],"study_design_scores_gemma":[0.0090539735,0.0020977769,0.35680318,0.00013595226,0.0007660532,0.001002228,0.00070334476,0.48138264,0.00006380236,0.013337967,0.13348462,0.0011684569],"about_ca_topic_score_codex":0.0017284944,"about_ca_topic_score_gemma":0.0033469412,"teacher_disagreement_score":0.37710267,"about_ca_system_score_codex":0.000017979128,"about_ca_system_score_gemma":0.000111969595,"threshold_uncertainty_score":0.9999977},"labels":[],"label_agreement":null},{"id":"W4397009717","doi":"10.1016/j.geomorph.2024.109260","title":"A conceptual model on the influence of logjam formation on longitudinal and lateral sediment dynamics in forested streams","year":2024,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada; University of British Columbia","funders":"","keywords":"STREAMS; Geology; Sediment; Conceptual model; Hydrology (agriculture); Geomorphology; Geotechnical engineering","score_opus":0.013516491593434168,"score_gpt":0.2267881580169115,"score_spread":0.21327166642347734,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4397009717","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":[0.9979701,0.000023007991,0.00034299502,0.00087364856,0.000032236738,0.00014655509,0.000026064068,0.000015160958,0.0005702324],"genre_scores_gemma":[0.999391,0.000020016658,0.000019402423,0.00046206173,0.000003920097,0.000020063058,0.000030334499,0.000004369007,0.000048810558],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99934185,0.000030214382,0.00016690383,0.00018908907,0.00010598246,0.00016597654],"domain_scores_gemma":[0.999753,0.00009112054,0.000030961415,0.00009761722,0.000003697425,0.000023629824],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016137924,0.00009102292,0.00010497156,0.000039544975,0.00003946181,0.0000055854803,0.000097110664,0.00008309971,0.000242689],"category_scores_gemma":[0.00000825226,0.00006251846,0.000015995985,0.00010126619,0.00042888618,0.00011753559,0.000032367065,0.00015937167,0.000042487518],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027197134,0.00014102293,0.26312798,0.000030418532,0.00001930938,0.000114679395,0.0020191164,0.7024362,0.0012305147,0.029194413,0.00023895715,0.0011754283],"study_design_scores_gemma":[0.000678526,0.0008372721,0.21456064,0.000079566176,0.000023076338,0.000059905906,0.00017129687,0.77525896,0.0013529719,0.0065920465,0.00020413748,0.00018156765],"about_ca_topic_score_codex":0.00016390454,"about_ca_topic_score_gemma":0.0008010372,"teacher_disagreement_score":0.072822794,"about_ca_system_score_codex":0.00006908169,"about_ca_system_score_gemma":0.000008811195,"threshold_uncertainty_score":0.26572743},"labels":[],"label_agreement":null},{"id":"W4402240171","doi":"10.1016/j.geomorph.2024.109416","title":"Multi-millennia surface dynamics: Novel investigation approach unveils climate relation to mountain erosion (Serra da Estrela, Portugal)","year":2024,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Foundation for Research in Science and the Humanities; Universität Zürich; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung","keywords":"Geology; Erosion; Geomorphology; Relation (database); Physical geography; Earth science; Geography","score_opus":0.03505109868348029,"score_gpt":0.26154378278122953,"score_spread":0.22649268409774925,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402240171","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":[0.9878823,0.0009837952,0.005615889,0.0022195063,0.0008241021,0.00048241092,0.00032803445,0.00018185303,0.0014821034],"genre_scores_gemma":[0.9812623,0.0001393512,0.013151438,0.00046377841,0.000054699805,0.000008550482,0.004205458,0.0000124172975,0.00070195965],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.997491,0.0002905867,0.00042342825,0.0007669208,0.00022999318,0.0007980584],"domain_scores_gemma":[0.9988873,0.00033834387,0.00007888682,0.0003511915,0.00007566058,0.0002686239],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0011639214,0.0002588844,0.00032356317,0.00027128364,0.00032440777,0.000074487616,0.0003166933,0.00051306665,0.0010820517],"category_scores_gemma":[0.000110097535,0.00023548171,0.00006920213,0.0005845919,0.00037080108,0.00024551433,0.00006303456,0.00064736535,0.003045687],"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":[0.00007232912,0.000030076422,0.977807,0.0000702264,0.00002720737,0.00010172662,0.00039018906,0.018506087,0.0010361928,0.00097473135,0.00051619386,0.00046804675],"study_design_scores_gemma":[0.00039048534,0.00018789344,0.67084634,0.000030655203,0.000026844302,0.00049106876,0.0002447082,0.3265835,0.000052900923,0.00031235252,0.00057943433,0.0002538077],"about_ca_topic_score_codex":0.001638841,"about_ca_topic_score_gemma":0.0043727006,"teacher_disagreement_score":0.30807742,"about_ca_system_score_codex":0.000015023294,"about_ca_system_score_gemma":0.00013217244,"threshold_uncertainty_score":0.9998311},"labels":[],"label_agreement":null},{"id":"W4403064739","doi":"10.1016/j.geomorph.2024.109439","title":"Bedform generation beneath shoaling nonlinear internal waves on a mild slope","year":2024,"lang":"en","type":"article","venue":"Geomorphology","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":false,"ca_institutions":"Queen's University","funders":"Natural Sciences and Engineering Research Council of Canada; Queen's University","keywords":"Geology; Shoaling and schooling; Bedform; Geomorphology; Geotechnical engineering; Seismology; Sediment transport; Sediment; Oceanography","score_opus":0.015911910926086105,"score_gpt":0.24521400564716295,"score_spread":0.22930209472107685,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403064739","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":[0.98298144,0.00021442783,0.0009996232,0.001057324,0.0013871511,0.00010092438,0.00003018249,0.000074231386,0.0131546855],"genre_scores_gemma":[0.9914953,0.00015910596,0.0020719732,0.0009743131,0.00046456288,0.000008827174,0.00011827562,0.000021592556,0.004686065],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99912494,0.000022011847,0.00016291514,0.0003068716,0.00014093518,0.00024234796],"domain_scores_gemma":[0.999741,0.000023835422,0.00002259127,0.00014444577,0.0000038618773,0.000064233995],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00016064008,0.00011505335,0.00010870906,0.000042188643,0.000090275134,0.000047590886,0.00012933812,0.00013159242,0.006647258],"category_scores_gemma":[0.000009442224,0.00008144939,0.000059902814,0.00010565803,0.00008502419,0.00007866079,0.00010667088,0.00022855088,0.0022870197],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004405918,0.00060427457,0.025759153,0.00008505813,0.00047913028,0.004143198,0.0053221243,0.07758464,0.25977376,0.0074813752,0.26800048,0.3503262],"study_design_scores_gemma":[0.0009305626,0.0009454783,0.006080557,0.00011807118,0.00009455309,0.0008768228,0.00009033909,0.288069,0.023599325,0.00094270986,0.6775899,0.00066269917],"about_ca_topic_score_codex":0.000232637,"about_ca_topic_score_gemma":0.00013226448,"teacher_disagreement_score":0.40958938,"about_ca_system_score_codex":0.00009080561,"about_ca_system_score_gemma":0.000009705476,"threshold_uncertainty_score":0.9984898},"labels":[],"label_agreement":null},{"id":"W4404161120","doi":"10.1016/j.geomorph.2024.109494","title":"Applying geoarchaeological principles to marine archaeology: A new reappraisal of the “first marine” and “in-situ” lithic scatters, Murujuga (Dampier Archipelago), NW Australia","year":2024,"lang":"en","type":"article","venue":"Geomorphology","topic":"Maritime and Coastal Archaeology","field":"Arts and Humanities","cited_by":4,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Heritage Medical Research Clinic","funders":"","keywords":"Geology; Archipelago; Archaeology; Marine geology; Oceanography; Paleontology; Geography","score_opus":0.04180522443506048,"score_gpt":0.25860343994641827,"score_spread":0.21679821551135778,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404161120","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":[0.9666042,0.00018288162,0.00011410828,0.018563656,0.0009454936,0.0008846769,0.000051144634,0.000088578876,0.012565269],"genre_scores_gemma":[0.9824642,0.00005514202,0.00074039114,0.0016567,0.00044197432,0.00021040399,0.000050273513,0.000032087413,0.014348848],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.9975531,0.00019022092,0.0005832198,0.0007048359,0.0002003935,0.00076823577],"domain_scores_gemma":[0.99879193,0.00042133345,0.0000897232,0.0004655551,0.000048871472,0.00018260573],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00046115782,0.00033839385,0.0005554504,0.00036178078,0.00016295887,0.000035065365,0.00056006573,0.00018732956,0.0042439583],"category_scores_gemma":[0.00010712898,0.0002456011,0.00014167391,0.00017289528,0.0032929464,0.0000850963,0.003683214,0.00070599455,0.00012271629],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00052436604,0.0001452156,0.18008617,0.00038235643,0.0001529995,0.0007243474,0.03944671,0.00003733294,0.0008812015,0.7271686,0.0024625475,0.047988147],"study_design_scores_gemma":[0.000714949,0.0004945353,0.1479113,0.00011928857,0.00006463458,0.0008681155,0.0007616779,0.0001001985,0.00014234032,0.052776106,0.79562867,0.0004182137],"about_ca_topic_score_codex":0.014526504,"about_ca_topic_score_gemma":0.18825613,"teacher_disagreement_score":0.7931661,"about_ca_system_score_codex":0.000021110722,"about_ca_system_score_gemma":0.00009785022,"threshold_uncertainty_score":0.99999964},"labels":[],"label_agreement":null},{"id":"W4404679010","doi":"10.1016/j.geomorph.2024.109523","title":"Toward flow forces acting on a step-pool unit","year":2024,"lang":"en","type":"article","venue":"Geomorphology","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"National Natural Science Foundation of China","keywords":"Geology; Flow (mathematics); Unit (ring theory); Geometry; Mathematics","score_opus":0.02241337102128664,"score_gpt":0.24818467685743925,"score_spread":0.22577130583615262,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404679010","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":[0.96592855,0.00022535784,0.0042630257,0.0026104834,0.0006517669,0.00015066627,0.000022236194,0.00022271599,0.025925182],"genre_scores_gemma":[0.99634737,0.00003875817,0.00040539497,0.0013777479,0.00006421371,0.000021962816,0.000038128823,0.000014108782,0.0016923116],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9989913,0.000037232698,0.00014697138,0.00036348848,0.0001275952,0.00033337742],"domain_scores_gemma":[0.9996526,0.000114639675,0.000021429425,0.00014296988,0.0000029318817,0.000065422384],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00019774634,0.00013099116,0.00013559678,0.00004508016,0.00010588479,0.000017565028,0.00019091213,0.00013701536,0.02243433],"category_scores_gemma":[0.000017407428,0.00011092044,0.000045980272,0.00018216063,0.00020371925,0.00012428343,0.00004920686,0.0002468615,0.0049522636],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009739123,0.0008116121,0.121374585,0.0005403063,0.00052720826,0.011657345,0.011680977,0.055454448,0.036847275,0.008179737,0.11229047,0.63966215],"study_design_scores_gemma":[0.0005169622,0.00063298974,0.0056175217,0.000047240028,0.00007104029,0.00027596005,0.00017854698,0.012200905,0.0080783665,0.0016754606,0.97029006,0.00041495851],"about_ca_topic_score_codex":0.00013380207,"about_ca_topic_score_gemma":0.0001236032,"teacher_disagreement_score":0.85799956,"about_ca_system_score_codex":0.000027098835,"about_ca_system_score_gemma":0.000013004681,"threshold_uncertainty_score":0.9958225},"labels":[],"label_agreement":null},{"id":"W4405249475","doi":"10.1016/j.geomorph.2024.109564","title":"Analog modeling of landslide dynamics: Case study from the Andean Mesón Alto deposit, Central Chile (∼33°40′S)","year":2024,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"Fondo Nacional de Desarrollo Científico y Tecnológico; Agencia Nacional de Investigación y Desarrollo","keywords":"Geology; Landslide; Geomorphology; Seismology; Physical geography; Geochemistry; Geography","score_opus":0.009042913509801853,"score_gpt":0.22755552147170033,"score_spread":0.21851260796189848,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405249475","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":[0.99431175,0.00045302315,0.0027824456,0.0003019701,0.00048206188,0.00025349387,0.00019159724,0.000049556766,0.001174123],"genre_scores_gemma":[0.9993158,0.000064513246,0.00015646381,0.00015029416,0.00008112457,0.000008975776,0.00008433391,0.000019208142,0.00011931464],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9986553,0.00011742421,0.00029428146,0.0003894509,0.00017812896,0.000365385],"domain_scores_gemma":[0.9994164,0.00010387456,0.00004694042,0.0003379304,0.0000065677154,0.00008827297],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00024934462,0.000157135,0.00023145137,0.000028280532,0.00015832241,0.00003583464,0.00025231065,0.00012149458,0.0013886979],"category_scores_gemma":[0.000012115251,0.000095207935,0.00008879055,0.00019364663,0.00012643552,0.00007113527,0.00024263439,0.00029658663,0.000107529435],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015371144,0.0004506066,0.8234846,0.000017743916,0.00051020307,0.021981861,0.00997595,0.12705861,0.0008969933,0.00013083174,0.0047369082,0.010601967],"study_design_scores_gemma":[0.0010599736,0.00037453132,0.02716226,0.00003771288,0.00034970255,0.004780574,0.004897675,0.958714,0.00007983778,0.00073829846,0.0014677393,0.00033766797],"about_ca_topic_score_codex":0.056637272,"about_ca_topic_score_gemma":0.025376445,"teacher_disagreement_score":0.83165544,"about_ca_system_score_codex":0.000108438355,"about_ca_system_score_gemma":0.000016621565,"threshold_uncertainty_score":0.9995242},"labels":[],"label_agreement":null},{"id":"W4405982789","doi":"10.1016/j.geomorph.2024.109588","title":"Back-analysis of the 2000 Yigong dam breach flood morphodynamics: Challenges and promises","year":2025,"lang":"en","type":"article","venue":"Geomorphology","topic":"Dam Engineering and Safety","field":"Engineering","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"China Scholarship Council; National Natural Science Foundation of China","keywords":"Beach morphodynamics; Geology; Flood myth; Geomorphology; Hydrology (agriculture); Sediment transport; Geotechnical engineering; Sediment; Archaeology; Geography","score_opus":0.007237512990647807,"score_gpt":0.19850033865124989,"score_spread":0.19126282566060207,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405982789","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":[0.97094667,0.009400936,0.002304036,0.0005298384,0.000729897,0.00020497128,0.00011299058,0.00012887894,0.015641775],"genre_scores_gemma":[0.9975614,0.0012061667,0.0003289611,0.000037374426,0.00001907434,0.000014352916,0.000023819182,0.000015362695,0.00079351524],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99927545,0.00003417833,0.0002227249,0.0001870166,0.00006630408,0.00021435981],"domain_scores_gemma":[0.99944127,0.00006920389,0.00002665024,0.00040255825,0.000028967832,0.000031361116],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014774974,0.0001424109,0.00037371137,0.0002020756,0.000031929154,0.0000063583198,0.00019938624,0.0001204614,0.00013646754],"category_scores_gemma":[0.000023733648,0.00011509245,0.00010213999,0.00038227497,0.0000886349,0.000028773633,0.000077428565,0.00015051558,0.0000100170855],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000059552538,0.00024215676,0.020335749,0.0012591118,0.01217459,0.000035987174,0.0050674584,0.8679351,0.020730164,0.014252193,0.006237533,0.05167037],"study_design_scores_gemma":[0.0012455042,0.000059385235,0.71095896,0.00010470919,0.002578182,0.00006721876,0.0003826758,0.26114616,0.0017685022,0.00049953326,0.020620326,0.00056888355],"about_ca_topic_score_codex":0.000050914598,"about_ca_topic_score_gemma":0.00015747959,"teacher_disagreement_score":0.69062316,"about_ca_system_score_codex":0.000034019085,"about_ca_system_score_gemma":0.000018656625,"threshold_uncertainty_score":0.4693334},"labels":[],"label_agreement":null},{"id":"W4406501756","doi":"10.1016/j.geomorph.2025.109610","title":"Analyzing topographic change profiles in coastal foredune systems: Methodological recommendations","year":2025,"lang":"en","type":"article","venue":"Geomorphology","topic":"Coastal and Marine Dynamics","field":"Earth and Planetary Sciences","cited_by":3,"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 Guelph; Mount Allison University; University of British Columbia, Okanagan Campus","funders":"Parks Canada","keywords":"Foredune; Geology; Geomorphology; Oceanography; Hydrology (agriculture); Physical geography; Aeolian processes; Geotechnical engineering; Geography","score_opus":0.07247098710543518,"score_gpt":0.30194751103994166,"score_spread":0.2294765239345065,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406501756","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":[0.9733324,0.00089771545,0.0062533813,0.0051499195,0.0017913784,0.0006384536,0.00055906206,0.000092950046,0.01128475],"genre_scores_gemma":[0.9959641,0.00017895708,0.0017066188,0.00030830532,0.000055701687,0.000020430989,0.0010844843,0.0000017731554,0.00067961466],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988777,0.00027081222,0.0002469508,0.0002518269,0.00005135523,0.00030137523],"domain_scores_gemma":[0.99940896,0.00032600298,0.00005601136,0.00013428385,0.000028934523,0.000045797573],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005645019,0.00010645348,0.00024363257,0.00031749753,0.000088197274,0.000024561265,0.00015745868,0.00010156778,0.0008427949],"category_scores_gemma":[0.00009763311,0.000088714885,0.00004903131,0.00059919304,0.000102540886,0.00008968331,0.000058098703,0.00018052406,0.000027901171],"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":[0.000040327912,0.000025658448,0.9125677,0.000029849196,0.000016356944,0.000046248297,0.000051562427,0.00024415596,0.000020450536,0.0033959164,0.0005819486,0.08297985],"study_design_scores_gemma":[0.00040092622,0.00013416019,0.9641526,0.000037198482,0.0000195736,0.00006226822,0.00046410534,0.013477741,0.000006126687,0.004079323,0.017003316,0.00016270038],"about_ca_topic_score_codex":0.017104743,"about_ca_topic_score_gemma":0.06740042,"teacher_disagreement_score":0.08281715,"about_ca_system_score_codex":0.0000038517614,"about_ca_system_score_gemma":0.000027040467,"threshold_uncertainty_score":0.98944044},"labels":[],"label_agreement":null},{"id":"W4407252353","doi":"10.1016/j.geomorph.2025.109641","title":"Formation and evolution of grus deposits in the Çine Submassif, Southwest Türkiye: A multi-proxy approach","year":2025,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Türkiye Bilimsel ve Teknolojik Araştırma Kurumu","keywords":"Geology; Grus (genus); Proxy (statistics); Paleontology; Physical geography; Earth science; Geography; Population","score_opus":0.012795821435905333,"score_gpt":0.20052475530877364,"score_spread":0.18772893387286832,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407252353","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":[0.99295473,0.00090835546,0.0037633742,0.0006595198,0.000030766765,0.00012388131,0.000023045648,0.000007952586,0.0015283824],"genre_scores_gemma":[0.9985856,0.000023827131,0.00097413664,0.00019487555,0.000008930364,0.0000035481933,0.00016577564,4.167619e-7,0.0000429175],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99929047,0.00011063237,0.00020021434,0.00015494965,0.00007449284,0.00016927399],"domain_scores_gemma":[0.99969655,0.00009435036,0.000057802776,0.0001013932,0.000026950775,0.000022928212],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025931475,0.00007221402,0.00015819648,0.0000880742,0.00006122747,0.000008884007,0.0001374692,0.00008150148,0.00016504677],"category_scores_gemma":[0.00006373695,0.000042903055,0.000033139833,0.00038913797,0.00014221467,0.000053653566,0.000017918057,0.000112076836,0.000014445045],"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":[0.000030462488,0.00004714568,0.995538,0.000024440418,0.00000821852,0.0000051819893,0.00015376021,0.0004277426,0.00053426425,0.00035900567,0.00005013284,0.002821672],"study_design_scores_gemma":[0.0003435983,0.000046884088,0.9721944,0.000004472543,0.000024370767,0.00003111173,0.00043871082,0.023567041,0.00013323812,0.0030662154,0.00010061216,0.00004934771],"about_ca_topic_score_codex":0.007199564,"about_ca_topic_score_gemma":0.008911613,"teacher_disagreement_score":0.023343576,"about_ca_system_score_codex":0.0000028832662,"about_ca_system_score_gemma":0.000010654256,"threshold_uncertainty_score":0.9994116},"labels":[],"label_agreement":null},{"id":"W4407439040","doi":"10.1016/j.geomorph.2025.109669","title":"Rapid and large-scale landscape modification caused by the draining of a glacier-dammed lake in British Columbia, Canada","year":2025,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Positive Living North; Government of British Columbia; University of Northern British Columbia; Simon Fraser University","funders":"Ministry of Forests, Lands and Natural Resource Operations","keywords":"Geology; Glacier; Scale (ratio); Physical geography; Hydrology (agriculture); Geomorphology; Cartography; Geotechnical engineering; Geography","score_opus":0.004693725509800435,"score_gpt":0.1918926255542047,"score_spread":0.18719890004440426,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407439040","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":[0.99641025,0.00033429323,0.000064681706,0.0007645675,0.000114724986,0.00014020945,0.00010811839,0.00000623835,0.0020569381],"genre_scores_gemma":[0.9971097,0.000104001985,0.000020292093,0.0005450093,0.0000046707723,0.00001417825,0.00006251651,0.0000040775153,0.0021355525],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992702,0.00006231481,0.00017314413,0.00018796425,0.000091891394,0.00021450291],"domain_scores_gemma":[0.9997098,0.00006081326,0.00005400205,0.00013753721,0.000006208148,0.0000316574],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002584738,0.000047806814,0.00013631051,0.000010515773,0.00009991737,0.000021923324,0.00012005487,0.00008686843,0.0012911255],"category_scores_gemma":[0.00002532427,0.00005120466,0.000014049039,0.00018935754,0.00013946145,0.000025754814,0.000085890286,0.00012563707,0.0000025860359],"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":[0.000011129225,0.000051622825,0.90669686,0.000009670386,0.000017466735,0.000032828728,0.00042931215,0.00013431566,0.0013437093,0.0000051238612,0.078255616,0.013012347],"study_design_scores_gemma":[0.001368997,0.000032480264,0.8399746,0.000018609215,0.000017787917,0.000038370898,0.0006672158,0.0021214413,0.000092826296,0.00011014598,0.15545467,0.00010288845],"about_ca_topic_score_codex":0.7196884,"about_ca_topic_score_gemma":0.9957369,"teacher_disagreement_score":0.2760485,"about_ca_system_score_codex":0.00003910501,"about_ca_system_score_gemma":0.000049043847,"threshold_uncertainty_score":0.9996218},"labels":[],"label_agreement":null},{"id":"W4407490812","doi":"10.1016/j.geomorph.2025.109665","title":"Analysis of the fundamental differences between dam-forming landslides and all landslides","year":2025,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"China Scholarship Council","keywords":"Landslide; Geology; Landslide classification; Geomorphology; Geotechnical engineering","score_opus":0.011769082555058992,"score_gpt":0.24160034503230884,"score_spread":0.22983126247724986,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407490812","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":[0.99521935,0.00013195175,0.00008346145,0.0005454697,0.00012410893,0.000090466,0.000051346113,0.000012899448,0.003740946],"genre_scores_gemma":[0.99853814,0.000082294326,0.00007819979,0.0002643334,0.0000114253335,0.0000046448768,0.000026472022,0.000003709797,0.0009907974],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991157,0.00006193566,0.00023118424,0.00023555092,0.00013123371,0.00022436287],"domain_scores_gemma":[0.9994987,0.00013519934,0.000099131394,0.00021962242,0.0000055103415,0.00004178845],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00019960747,0.00011350897,0.00031296708,0.00008921508,0.00013227422,0.000017034548,0.00024891403,0.00011563607,0.0009207617],"category_scores_gemma":[0.000023092218,0.000064616106,0.00010205249,0.0005091284,0.00037441883,0.000048306996,0.00038634252,0.00013076604,0.000011395955],"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":[0.000010839634,0.000016790329,0.99458295,0.0000050103445,0.00050010375,0.000002803113,0.00021661226,0.00008623912,0.0008319918,0.00008415868,0.0004033126,0.003259202],"study_design_scores_gemma":[0.0002794494,0.000036378497,0.9921997,0.000010766991,0.0008731967,0.000004890061,0.00013945084,0.00039268818,0.00052431034,0.0004131596,0.005042049,0.00008391704],"about_ca_topic_score_codex":0.0010107132,"about_ca_topic_score_gemma":0.0006643636,"teacher_disagreement_score":0.0046387366,"about_ca_system_score_codex":0.000031048676,"about_ca_system_score_gemma":0.00000833236,"threshold_uncertainty_score":0.99999255},"labels":[],"label_agreement":null},{"id":"W4408087971","doi":"10.1016/j.geomorph.2025.109702","title":"Delineating sediment compartment boundaries in an urbanised embayment for geomorphic management of decadal-scale coastal dynamics","year":2025,"lang":"en","type":"article","venue":"Geomorphology","topic":"Coastal and Marine Dynamics","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Stantec (Canada)","funders":"","keywords":"Geology; Sediment; Scale (ratio); Oceanography; Geomorphology; Geography; Cartography","score_opus":0.010596972064958373,"score_gpt":0.2448279415912657,"score_spread":0.23423096952630731,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408087971","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":[0.9764365,0.00011946114,0.018328916,0.0004791307,0.00061355793,0.00079627766,0.00095588475,0.000031051728,0.0022392124],"genre_scores_gemma":[0.9884542,0.000022503136,0.007073234,0.00026465638,0.000018961959,0.000025391033,0.0033502034,0.0000050025133,0.0007857969],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9984818,0.000058190144,0.000507974,0.00036114824,0.00016159214,0.00042927943],"domain_scores_gemma":[0.9993954,0.000085189735,0.00012436969,0.0002440141,0.00007456856,0.00007651287],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003501022,0.00018807386,0.00035170623,0.00015304181,0.00017173174,0.000046979487,0.000241328,0.00007678957,0.0003049718],"category_scores_gemma":[0.0000062721806,0.00018148393,0.000067045425,0.00022550182,0.00024142273,0.00008080498,0.000100216545,0.00010644491,0.000006779937],"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":[0.00095752266,0.0004671136,0.8469511,0.00044392643,0.00014773165,0.00008871894,0.0003073629,0.03034739,0.000090282825,0.012997495,0.00071587757,0.10648548],"study_design_scores_gemma":[0.0038604138,0.0010283545,0.41734347,0.00010778428,0.000113933085,0.00002418538,0.0019115217,0.5586821,0.00018624227,0.0057618944,0.010574032,0.0004060914],"about_ca_topic_score_codex":0.004445941,"about_ca_topic_score_gemma":0.14398246,"teacher_disagreement_score":0.5283347,"about_ca_system_score_codex":0.00003047247,"about_ca_system_score_gemma":0.00009822938,"threshold_uncertainty_score":0.87163764},"labels":[],"label_agreement":null},{"id":"W4409106245","doi":"10.1016/j.geomorph.2025.109740","title":"Reconstructing the geological and geomorphological history of Morella Crater, Mars","year":2025,"lang":"en","type":"article","venue":"Geomorphology","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Indian Space Research Organisation; Department of Science and Technology, Ministry of Science and Technology, India","keywords":"Geology; Impact crater; Mars Exploration Program; Geomorphology; Paleontology; Archaeology; Astrobiology; Geography","score_opus":0.016657618363320085,"score_gpt":0.21681837869361917,"score_spread":0.2001607603302991,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409106245","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":[0.988815,0.00024681306,0.0009891165,0.000843718,0.00044347346,0.00009088538,0.000017001863,0.000010529038,0.008543435],"genre_scores_gemma":[0.99791956,0.000011926109,0.00030100206,0.00042008763,0.000037870912,0.000008187964,0.000089195004,0.0000017163974,0.0012104284],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99929243,0.00008316681,0.00019378198,0.00019960704,0.000050330924,0.00018068362],"domain_scores_gemma":[0.9995662,0.00014312663,0.000085908614,0.00015060577,0.000028549932,0.000025622812],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002482054,0.000084362575,0.00016866958,0.000042962176,0.00006987482,0.000006726216,0.0001512737,0.000055265384,0.00080427306],"category_scores_gemma":[0.000015683085,0.000055575892,0.000031349056,0.00007863816,0.0006195176,0.000054319087,0.00007854849,0.00014477147,0.000039110357],"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":[0.000069254806,0.00007132119,0.89657736,0.0000098545315,0.00005494604,0.000023060355,0.00032043058,0.00025288918,0.012104916,0.0444513,0.03281985,0.013244848],"study_design_scores_gemma":[0.003994502,0.0009286316,0.44922945,0.00008539895,0.00028463657,0.00049354864,0.0057086484,0.015824411,0.004463254,0.17133567,0.3464995,0.0011523739],"about_ca_topic_score_codex":0.0002623361,"about_ca_topic_score_gemma":0.0000062100685,"teacher_disagreement_score":0.44734788,"about_ca_system_score_codex":0.000015309677,"about_ca_system_score_gemma":0.000059557588,"threshold_uncertainty_score":0.8806226},"labels":[],"label_agreement":null},{"id":"W4409459008","doi":"10.1016/j.geomorph.2025.109766","title":"Corrigendum to “Reconstructing the geological and geomorphological history of Morella Crater, Mars” [Geomorphology 479 (2025) 109740]","year":2025,"lang":"en","type":"erratum","venue":"Geomorphology","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Geology; Impact crater; Mars Exploration Program; Geomorphology; Astrobiology","score_opus":0.03041961485937538,"score_gpt":0.23338756686925205,"score_spread":0.20296795200987666,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409459008","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.46493012,0.0110439705,0.0074484674,0.011391686,0.2741882,0.0048105386,0.0060949107,0.00035173836,0.21974036],"genre_scores_gemma":[0.16815828,0.000498521,0.0015287399,0.0066825463,0.0031055873,0.00031802896,0.019267118,0.00008259047,0.8003586],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99609774,0.00044351516,0.0009538238,0.0012056439,0.00031361377,0.0009856515],"domain_scores_gemma":[0.9977929,0.00029555234,0.0006447382,0.0008266342,0.00021040258,0.00022979149],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007546443,0.0006499526,0.0012749402,0.00033456253,0.00024955903,0.00003966893,0.0010084653,0.0007983621,0.008225472],"category_scores_gemma":[0.000111939094,0.00048806312,0.00021121177,0.0003387818,0.0015842627,0.00011365487,0.00066793035,0.0015642276,0.0005889768],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000085850515,0.00007975003,0.012176593,0.000034066463,0.00010879077,0.00013083532,0.00024737458,0.00006502167,0.0006685401,0.0018697272,0.9820832,0.002450265],"study_design_scores_gemma":[0.0005787242,0.0004876918,0.004180876,0.0000731811,0.0001882049,0.00025920803,0.0005065571,0.0005001063,0.000073203875,0.0028047992,0.98971957,0.00062784937],"about_ca_topic_score_codex":0.0020052318,"about_ca_topic_score_gemma":0.00011833277,"teacher_disagreement_score":0.5806182,"about_ca_system_score_codex":0.00014245938,"about_ca_system_score_gemma":0.00076694484,"threshold_uncertainty_score":0.9997571},"labels":[],"label_agreement":null},{"id":"W4409817121","doi":"10.1016/j.geomorph.2025.109794","title":"Decoding surface processes from escarpment to watershed: Insights from karst landscapes using cosmogenic nuclides and geochemical data","year":2025,"lang":"en","type":"article","venue":"Geomorphology","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":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"ASTER","funders":"Centre National de la Recherche Scientifique; Conselho Nacional de Desenvolvimento Científico e Tecnológico; Coordenação de Aperfeiçoamento de Pessoal de Nível Superior; Institut de Recherche pour le Développement","keywords":"Escarpment; Geology; Karst; Cosmogenic nuclide; Surface exposure dating; Watershed; Geomorphology; Earth science; Geochemistry; Paleontology; Glacier; Moraine","score_opus":0.03980707375231371,"score_gpt":0.2773893183214376,"score_spread":0.23758224456912388,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409817121","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":[0.9929378,0.00459289,0.00013565364,0.00089718367,0.00028141937,0.00018097521,0.0005872359,0.000034948032,0.0003519155],"genre_scores_gemma":[0.99298686,0.00019600573,0.0032731828,0.00058252964,0.00004744575,0.00000122838,0.0028660118,0.0000034177478,0.00004334257],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99829984,0.00017049744,0.00025238795,0.0007089406,0.00011488135,0.0004534601],"domain_scores_gemma":[0.99838865,0.0009203671,0.000048052716,0.0004432475,0.00005443094,0.00014525304],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001846837,0.00018132299,0.00035623106,0.000104250066,0.00026395827,0.000049658855,0.0005867124,0.00023923734,0.0013542962],"category_scores_gemma":[0.00020599624,0.00015247645,0.00001885384,0.00023367628,0.00021679688,0.00013878822,0.00027311762,0.00023818576,0.00023259615],"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":[0.00014091723,0.000016275944,0.99603415,0.00002113115,0.000077914985,0.00010080608,0.00021075139,0.0002884755,0.002091439,0.000008684552,0.0007446126,0.00026486214],"study_design_scores_gemma":[0.0016362922,0.00018615832,0.95457727,0.00012147792,0.00021275363,0.00017001579,0.00080251304,0.015385397,0.011386703,0.0076249167,0.007259894,0.00063658564],"about_ca_topic_score_codex":0.0050197006,"about_ca_topic_score_gemma":0.02263259,"teacher_disagreement_score":0.041456837,"about_ca_system_score_codex":0.0000026150612,"about_ca_system_score_gemma":0.00012172844,"threshold_uncertainty_score":0.9995586},"labels":[],"label_agreement":null},{"id":"W4410234284","doi":"10.1016/j.geomorph.2025.109813","title":"Denudation asymmetries and drainage divide migration: Insights into the evolution of the Devonian Escarpment in Paraná, Brazil","year":2025,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"ASTER","funders":"Centre National de la Recherche Scientifique; Coordenação de Aperfeiçoamento de Pessoal de Nível Superior; Institut de Recherche pour le Développement","keywords":"Denudation; Escarpment; Geology; Devonian; Paleontology; Geomorphology; Tectonics","score_opus":0.005634584736931466,"score_gpt":0.2088550288073366,"score_spread":0.20322044407040515,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410234284","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":[0.98796684,0.0025794562,0.00070422096,0.0054177158,0.00014888994,0.00014685556,0.000006827224,0.0000057748107,0.003023406],"genre_scores_gemma":[0.99932015,0.00006795422,0.00007360878,0.0003584721,0.000008856954,0.0000036742322,0.000043550965,4.3422455e-7,0.00012331782],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994282,0.000116136434,0.00017725618,0.00010240155,0.00007612714,0.000099862205],"domain_scores_gemma":[0.9995764,0.00020198166,0.00006164283,0.00011072317,0.000036249785,0.0000129872915],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022310512,0.000057184247,0.000087006236,0.00008344134,0.00021091355,0.000019194471,0.00014400785,0.00005680678,0.00015156878],"category_scores_gemma":[0.00013348847,0.000029911618,0.000016797892,0.00050707365,0.00022689124,0.00010505115,0.000026395031,0.00008051141,0.000010829929],"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":[0.000022401198,0.000011924265,0.96592635,0.00002530952,0.000007963137,0.0000010519417,0.0016038378,0.0011577727,0.000033378088,0.013085544,0.0002956465,0.017828826],"study_design_scores_gemma":[0.00013454065,0.000037513128,0.9368398,0.00001083283,0.0000065730437,0.0000042219535,0.000500714,0.0008683234,0.00019785328,0.052251246,0.009113838,0.000034541456],"about_ca_topic_score_codex":0.0067142146,"about_ca_topic_score_gemma":0.06774733,"teacher_disagreement_score":0.06103312,"about_ca_system_score_codex":0.0000073128895,"about_ca_system_score_gemma":0.00005209689,"threshold_uncertainty_score":0.99990016},"labels":[],"label_agreement":null},{"id":"W4411371916","doi":"10.1016/j.geomorph.2025.109885","title":"Erosional dynamics and escarpment retreat at the southern end of the South American passive margin escarpment","year":2025,"lang":"en","type":"article","venue":"Geomorphology","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":"University of Toronto","funders":"National Science Foundation","keywords":"Escarpment; Geology; Margin (machine learning); Geomorphology; Passive margin; Paleontology; Rift; Structural basin","score_opus":0.006232357094292626,"score_gpt":0.21043745144580067,"score_spread":0.20420509435150805,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411371916","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":[0.98695064,0.0005965678,0.000021684305,0.008651287,0.0002752781,0.00022660726,0.00034917705,0.000007970694,0.0029208027],"genre_scores_gemma":[0.99351823,0.00006224548,0.000042362837,0.0007066957,0.00001233638,0.000005707275,0.00012334962,0.000002026872,0.005527019],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986217,0.0003734033,0.00019890531,0.00028164525,0.00016126691,0.00036310314],"domain_scores_gemma":[0.99899036,0.00047501258,0.00012165757,0.00032226596,0.000039790444,0.00005089448],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00031488863,0.00013100002,0.00023969526,0.00006114346,0.00038719206,0.000008603304,0.00033291316,0.00010730106,0.002253265],"category_scores_gemma":[0.00005339141,0.000070659786,0.00006510671,0.0002210352,0.0024694903,0.000013635039,0.00016053373,0.0002679437,0.00012196767],"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":[0.00010889344,0.000010919667,0.9956813,0.000010757429,0.00004946129,0.000013092645,0.0003721589,0.00009193359,0.00001724411,0.00034217784,0.00066028273,0.0026417794],"study_design_scores_gemma":[0.00034320523,0.00009691816,0.99567044,0.000009973424,0.000036094585,0.00010579662,0.0013033282,0.00076421833,0.0001274345,0.00065693224,0.0008106078,0.00007504609],"about_ca_topic_score_codex":0.0011679028,"about_ca_topic_score_gemma":0.030599145,"teacher_disagreement_score":0.029431242,"about_ca_system_score_codex":0.0000064611795,"about_ca_system_score_gemma":0.0000854746,"threshold_uncertainty_score":0.99865884},"labels":[],"label_agreement":null},{"id":"W4411918631","doi":"10.1016/j.geomorph.2025.109905","title":"Coastal gullies formed by piping on a permafrost marine terrace near Iqaluktuuttiaq (Cambridge Bay), Nunavut, Canada","year":2025,"lang":"en","type":"article","venue":"Geomorphology","topic":"Climate change and permafrost","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":"Dalhousie University; Université Laval; Center for Northern Studies; Université du Québec à Rimouski","funders":"Natural Sciences and Engineering Research Council of Canada; Crown-Indigenous Relations and Northern Affairs Canada","keywords":"Geology; Permafrost; Bay; Terrace (agriculture); Piping; Oceanography; Geomorphology; Archaeology; Geography","score_opus":0.012298501151507947,"score_gpt":0.21669442272900677,"score_spread":0.20439592157749883,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411918631","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":[0.9405949,0.00039256192,0.000023481422,0.0043916544,0.0014364235,0.0002500344,0.033465806,0.00004374164,0.019401398],"genre_scores_gemma":[0.9354214,0.00023903734,0.00004500612,0.011735471,0.00016052628,0.000008312013,0.044280965,0.000011538558,0.008097754],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982187,0.00008194804,0.00030719853,0.00044264778,0.00022763791,0.0007218653],"domain_scores_gemma":[0.9991117,0.00027622338,0.000088168876,0.00031804084,0.000047685124,0.00015818622],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014248422,0.0002706754,0.00036068851,0.00008330177,0.0004123279,0.000084524494,0.0003220299,0.0001388221,0.020278381],"category_scores_gemma":[0.000054209915,0.00024469235,0.00006258873,0.00024249907,0.0001781973,0.00010271047,0.00008109358,0.00029907594,0.0002973563],"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":[0.0001553355,0.000023842264,0.6454848,0.000036663874,0.000029240422,0.00016901297,0.000115099145,0.00008272942,0.0005333794,0.000042981563,0.34922826,0.004098637],"study_design_scores_gemma":[0.00081274513,0.00020340848,0.5605666,0.00003453987,0.00002697219,0.0001294697,0.00041441218,0.0021011448,0.00030451932,0.000056773344,0.43501258,0.0003368116],"about_ca_topic_score_codex":0.8139962,"about_ca_topic_score_gemma":0.99176663,"teacher_disagreement_score":0.17777039,"about_ca_system_score_codex":0.000029523266,"about_ca_system_score_gemma":0.00035478498,"threshold_uncertainty_score":0.9978264},"labels":[],"label_agreement":null},{"id":"W4412425681","doi":"10.1016/j.geomorph.2025.109920","title":"Multi-scale analysis on the geomorphic evolution of Macao debris flow gully (NW China)","year":2025,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Ministry of Science and Technology of the People's Republic of China; National Natural Science Foundation of China","keywords":"Debris flow; Geology; Hyperconcentrated flow; Geomorphology; China; Scale (ratio); Debris; Hydrology (agriculture); Geotechnical engineering; Sediment transport; Sediment; Archaeology; Cartography; Oceanography; Geography","score_opus":0.005584236594184918,"score_gpt":0.21509263584210303,"score_spread":0.20950839924791811,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412425681","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":[0.978347,0.00012496974,0.0121749025,0.0029642053,0.0002525571,0.00021551896,0.0000601682,0.000029980902,0.005830668],"genre_scores_gemma":[0.99435246,0.000056876645,0.0009851368,0.00044366295,0.000013844116,0.000016320919,0.000034519282,0.0000071990453,0.00409],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99879783,0.00013324624,0.00024875815,0.00033416823,0.00018423806,0.0003017368],"domain_scores_gemma":[0.9992867,0.00007683971,0.00010926682,0.00046744398,0.000013568813,0.000046149285],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00030230373,0.00014085053,0.0002764794,0.0001230889,0.00018686283,0.000009459851,0.00033767722,0.00018757311,0.006468818],"category_scores_gemma":[0.00004421063,0.000087897206,0.00018381579,0.0009829851,0.00036488654,0.00003378274,0.00019554213,0.00023987265,0.00038196132],"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":[0.00029365928,0.0006445482,0.7586749,0.000022931585,0.0011731487,0.00007253533,0.0005756664,0.1497705,0.033126928,0.0008704919,0.045054816,0.009719852],"study_design_scores_gemma":[0.00070984586,0.00012603862,0.9095424,0.000014581639,0.0004913627,0.000018068773,0.00008234489,0.07772631,0.0020307743,0.00070644147,0.008379867,0.00017200483],"about_ca_topic_score_codex":0.0023903803,"about_ca_topic_score_gemma":0.00088646944,"teacher_disagreement_score":0.15086743,"about_ca_system_score_codex":0.00014284565,"about_ca_system_score_gemma":0.00001904273,"threshold_uncertainty_score":0.9944394},"labels":[],"label_agreement":null},{"id":"W4412603324","doi":"10.1016/j.geomorph.2025.109938","title":"Mapping of glacial erratic boulders for mineral exploration: A review with LiDAR-based examples from modern and ancient glaciated terrains","year":2025,"lang":"en","type":"review","venue":"Geomorphology","topic":"Remote Sensing and LiDAR Applications","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; The Scarborough Hospital","funders":"Commission Géologique du Canada; Natural Sciences and Engineering Research Council of Canada; Natural Resources Canada; University of Toronto","keywords":"Geology; Glacial period; Mineral exploration; Terrain; Geomorphology; Lidar; Physical geography; Drumlin; Remote sensing; Geochemistry; Cartography; Oceanography; Geography; Cryosphere; Ice stream","score_opus":0.04811996599649921,"score_gpt":0.29408411478008173,"score_spread":0.24596414878358253,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412603324","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00059858826,0.9541923,0.041568354,0.00043648924,0.000095651536,0.0023607751,0.00026506145,0.000038940318,0.0004438861],"genre_scores_gemma":[0.000367627,0.98522806,0.010994225,0.00084923126,0.00005422967,0.00026554373,0.0019272253,0.000036126152,0.0002777198],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99821955,0.00016393856,0.00057084387,0.00060569396,0.00016347176,0.0002764778],"domain_scores_gemma":[0.99875945,0.0002483473,0.0004295149,0.00045871688,0.000027949787,0.000076003846],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00023709411,0.0003195134,0.0012076563,0.00009226285,0.00013167885,0.000018643907,0.00020415113,0.00019367403,0.00013398155],"category_scores_gemma":[0.00008852166,0.0002547096,0.00016097986,0.00040887014,0.00037491706,0.000051465984,0.00008082207,0.00015597185,0.000012739786],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027831973,0.00012819003,0.000057554582,0.016020875,0.00013813685,0.000009365025,0.00050058146,0.00013152233,0.00017079982,0.000022950591,0.010974561,0.9718176],"study_design_scores_gemma":[0.0004916566,0.00012907843,0.00009291011,0.013044529,0.0006807637,0.000024831092,0.000042313834,0.000578447,0.0000056258164,0.0001646712,0.9843791,0.00036608565],"about_ca_topic_score_codex":0.0004322438,"about_ca_topic_score_gemma":0.0005122389,"teacher_disagreement_score":0.9734045,"about_ca_system_score_codex":0.000091851325,"about_ca_system_score_gemma":0.00017052882,"threshold_uncertainty_score":0.9999905},"labels":[],"label_agreement":null},{"id":"W4412982060","doi":"10.1016/j.geomorph.2025.109945","title":"A multi-event paleoseismic record from the northern Alpine Fault at Marble Hill, Aotearoa New Zealand","year":2025,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Hazards Research Platform; Ministry for Business Innovation and Employment; Western Washington University; Salt Spring Island Foundation","keywords":"Geology; Aotearoa; Fault (geology); Seismology; Fault scarp; Archaeology; Paleontology; Geomorphology; Geography; Law","score_opus":0.017442149585153305,"score_gpt":0.24788825530028755,"score_spread":0.23044610571513424,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412982060","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":[0.97312874,0.0019191088,0.000100371544,0.021782514,0.00094849593,0.00030981892,0.00017474752,0.000050507355,0.001585691],"genre_scores_gemma":[0.89261025,0.00040670557,0.0006434957,0.005091139,0.00015539906,0.000008077472,0.0012221369,0.000006413664,0.099856354],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99771607,0.0006157518,0.00032941607,0.0005137666,0.00013479008,0.00069020875],"domain_scores_gemma":[0.9981063,0.0010791277,0.00009913369,0.00051190646,0.000049538652,0.00015401382],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00055441336,0.00021109064,0.0003485918,0.00008835867,0.0003695161,0.000022348557,0.00060328405,0.00037000165,0.012813718],"category_scores_gemma":[0.00018737181,0.00014540361,0.00010275378,0.00025912983,0.00043021698,0.000047714882,0.00010550552,0.0005865101,0.0044746366],"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":[0.00020324501,0.00002328795,0.94245845,0.0000037735624,0.00008349732,0.00012514845,0.0001990375,0.0002511693,0.00003772034,0.0000041197973,0.04781314,0.008797417],"study_design_scores_gemma":[0.0010615861,0.00009417914,0.81635743,0.000010847384,0.000032706863,0.00011220477,0.00005060638,0.0021315666,0.000023741111,0.0013654134,0.1786251,0.0001346202],"about_ca_topic_score_codex":0.039467,"about_ca_topic_score_gemma":0.3754499,"teacher_disagreement_score":0.33598292,"about_ca_system_score_codex":0.0000046446016,"about_ca_system_score_gemma":0.00017180503,"threshold_uncertainty_score":0.9963005},"labels":[],"label_agreement":null},{"id":"W4413020451","doi":"10.1016/j.geomorph.2025.109959","title":"Shrinking salt crusts of the Bonneville Basin, Utah: Observations from multispectral remote sensing","year":2025,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":1,"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; Multispectral image; Salt lake; Geomorphology; Structural basin; Remote sensing; Multispectral pattern recognition; Hydrology (agriculture); Geotechnical engineering","score_opus":0.020456854783253584,"score_gpt":0.23297973937204464,"score_spread":0.21252288458879104,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413020451","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":[0.59864825,0.00016954195,0.3600887,0.03025671,0.0013214477,0.00018931218,0.00001431248,0.00011928919,0.009192416],"genre_scores_gemma":[0.93927085,0.000006472673,0.057361674,0.0021059345,0.000046155652,6.20718e-7,0.000010208763,0.0000021623619,0.0011959454],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99883235,0.00011608369,0.00028824023,0.0003617824,0.00011071181,0.00029082777],"domain_scores_gemma":[0.9986249,0.00027267626,0.00014918776,0.0007869646,0.00013674327,0.000029491666],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021909863,0.00012127209,0.00021696469,0.00004544108,0.00021265727,0.000026363812,0.00076099444,0.00012920915,0.000055497992],"category_scores_gemma":[0.00041214848,0.00010049992,0.00009021407,0.00046197954,0.00014335972,0.00007008579,0.00057034864,0.00022381285,0.000008759409],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000059654758,0.00020016007,0.06220946,0.00017476833,0.0003460973,0.0003433258,0.003542946,0.006652282,0.655967,0.13184422,0.03367037,0.10498974],"study_design_scores_gemma":[0.001482611,0.00005344497,0.2956106,0.00034171768,0.000066199245,0.00019346208,0.00022397397,0.2044559,0.20624264,0.19160344,0.09917286,0.0005531608],"about_ca_topic_score_codex":0.0014131285,"about_ca_topic_score_gemma":0.00018998598,"teacher_disagreement_score":0.44972435,"about_ca_system_score_codex":0.00002781531,"about_ca_system_score_gemma":0.00009701989,"threshold_uncertainty_score":0.4098268},"labels":[],"label_agreement":null},{"id":"W4413982904","doi":"10.1016/j.geomorph.2025.110003","title":"Detection of cryptotephra in sedimentary profiles using reflectance spectroscopy","year":2025,"lang":"en","type":"article","venue":"Geomorphology","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","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 the Fraser Valley; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; University of British Columbia","keywords":"Geology; Sedimentary rock; Reflectivity; Geochemistry; Mineralogy; Remote sensing; Geomorphology; Optics","score_opus":0.009104925885045896,"score_gpt":0.25765816539162706,"score_spread":0.24855323950658118,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413982904","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":[0.99163234,0.00018709025,0.0016467022,0.000119903445,0.00026037986,0.00016318909,0.00000300989,0.000011178903,0.0059761913],"genre_scores_gemma":[0.99642617,0.000034477187,0.0030936692,0.00023120228,0.000010710678,0.0000073744736,0.0000043430064,0.000005319682,0.00018674687],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99920434,0.000076651355,0.00021661114,0.00021691697,0.000073475385,0.0002119901],"domain_scores_gemma":[0.9997221,0.000028498722,0.000074105345,0.00015021804,0.0000037360323,0.000021333404],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00017552354,0.0000833568,0.00015668188,0.00006008417,0.000039616647,0.0000025866664,0.00010449718,0.0000910781,0.0014172385],"category_scores_gemma":[0.0000111461195,0.00007727143,0.000024954707,0.00042311015,0.0001551842,0.000048085916,0.00008788947,0.00015071633,0.000045919824],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005573371,0.000045836543,0.023541683,0.000008484862,0.000008162576,0.000010586195,0.00007967434,0.0023184144,0.9732944,0.00006894747,0.00009033003,0.00047777325],"study_design_scores_gemma":[0.0007059687,0.0001428749,0.03220271,0.00003471473,0.000020880314,0.000022593906,0.00008264933,0.0038131233,0.95612997,0.0054183993,0.0012881819,0.00013795469],"about_ca_topic_score_codex":0.001229643,"about_ca_topic_score_gemma":0.00017837265,"teacher_disagreement_score":0.017164426,"about_ca_system_score_codex":0.00014272344,"about_ca_system_score_gemma":0.000011637688,"threshold_uncertainty_score":0.9994956},"labels":[],"label_agreement":null},{"id":"W4414871943","doi":"10.1016/j.geomorph.2025.110045","title":"Can through-water Structure-from-Motion photogrammetry characterize topographic statistics of gravel-bed surfaces?","year":2025,"lang":"en","type":"article","venue":"Geomorphology","topic":"Remote Sensing and LiDAR Applications","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"National Key Research and Development Program of China; Chinese Academy of Sciences; National Natural Science Foundation of China","keywords":"Flume; Photogrammetry; Bedform; Surface finish; Flow (mathematics); Channel (broadcasting); Scale (ratio); Underwater; Refraction","score_opus":0.008157454108291823,"score_gpt":0.2281313722404452,"score_spread":0.21997391813215336,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414871943","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":[0.9805029,0.000014574807,0.016989304,0.0005618023,0.00027102587,0.00018512631,0.0005648848,0.00003120463,0.00087918795],"genre_scores_gemma":[0.9917836,0.00002253601,0.006642789,0.00046290157,0.000015348029,0.000002157681,0.00082637207,0.000009917616,0.00023437789],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9989303,0.00007665428,0.0002661826,0.00032379464,0.00012848,0.0002746231],"domain_scores_gemma":[0.99940485,0.000055425557,0.00009626601,0.00038262145,0.0000197119,0.00004113939],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000088575885,0.00013539637,0.00022302986,0.0000519341,0.00010237481,0.000014098181,0.000183536,0.00012942885,0.0019310496],"category_scores_gemma":[0.000019038227,0.00011330456,0.000043434,0.00028714145,0.0004005611,0.000031074367,0.00010622258,0.00014429571,0.00006222635],"study_design_candidate":"bench_or_experimental","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":[0.000026946776,0.000078545556,0.02883063,0.000012317121,0.000045578654,0.000008714283,0.0004913856,0.00010365698,0.9535836,0.0005557742,0.0025055378,0.013757296],"study_design_scores_gemma":[0.0008081685,0.000093572446,0.5363913,0.000015203008,0.00010613948,0.000026463209,0.00013311075,0.0007191663,0.3903987,0.04616771,0.024802964,0.00033746497],"about_ca_topic_score_codex":0.018767467,"about_ca_topic_score_gemma":0.0028172538,"teacher_disagreement_score":0.5631849,"about_ca_system_score_codex":0.000041420997,"about_ca_system_score_gemma":0.000009998255,"threshold_uncertainty_score":0.9989813},"labels":[],"label_agreement":null},{"id":"W4415015832","doi":"10.1016/j.geomorph.2025.110050","title":"RGIK guidelines for compiling consistent rock glacier inventories","year":2025,"lang":"en","type":"article","venue":"Geomorphology","topic":"Climate change and permafrost","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":false,"ca_institutions":"University of Ottawa","funders":"International Permafrost Association; Université de Fribourg; European Space Agency","keywords":"Rock glacier; Glacier; Permafrost; Landform; Geohazard; Moraine; Rockfall; Glacier mass balance","score_opus":0.1365041837372382,"score_gpt":0.3385034926948977,"score_spread":0.20199930895765952,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415015832","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":[0.9439994,0.0076405145,0.0025261457,0.018766737,0.0070185205,0.0008520573,0.007421313,0.0001371155,0.011638202],"genre_scores_gemma":[0.94687235,0.00052946777,0.0018931038,0.02778374,0.00084207946,0.000024576966,0.012639365,0.000010034697,0.009405294],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990851,0.00003124865,0.00026926136,0.00023214227,0.00006964037,0.00031257104],"domain_scores_gemma":[0.99929404,0.00023115541,0.00005463397,0.0001621499,0.00020054984,0.00005749661],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00022831062,0.00011587951,0.00021600566,0.00007922538,0.00019264041,0.000032064156,0.0001526333,0.00009129142,0.0048674163],"category_scores_gemma":[0.00015147543,0.00009911782,0.00007395229,0.00013309564,0.000072565344,0.000048793503,0.00002064563,0.00006695791,0.00020350798],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017349668,0.000020850519,0.76144826,0.000094274525,0.000054772776,0.000026563239,0.00023298197,0.0009918693,0.0006694593,0.0008215198,0.23050362,0.0049623507],"study_design_scores_gemma":[0.0010486381,0.00015221014,0.0715207,0.000041286334,0.00005540137,0.000062135936,0.0007023703,0.011309144,0.0005298404,0.0031042143,0.9112291,0.00024501132],"about_ca_topic_score_codex":0.001736185,"about_ca_topic_score_gemma":0.012150275,"teacher_disagreement_score":0.6899275,"about_ca_system_score_codex":0.0000044115786,"about_ca_system_score_gemma":0.000053776886,"threshold_uncertainty_score":0.99604225},"labels":[],"label_agreement":null},{"id":"W4415215221","doi":"10.1016/j.geomorph.2025.110061","title":"Extreme Mediterranean rainfall impact on sedimentary routing systems: what can we learn from Storm Alex using in situ detrital 10Be?","year":2025,"lang":"en","type":"article","venue":"Geomorphology","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":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Musée de la Civilisation","funders":"Conseil National de la Recherche Scientifique; Bureau de Recherches Géologiques et Minières; Institut national des sciences de l'Univers; Université de Lorraine","keywords":"Sediment; Denudation; Sedimentary budget; Storm; Sedimentary rock; Sediment transport; Mediterranean climate; Flash flood; Glacial period; Climate change","score_opus":0.04888035212061465,"score_gpt":0.2839018235721064,"score_spread":0.23502147145149177,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415215221","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":[0.9894052,0.005264691,0.00002554344,0.0016130451,0.0019286211,0.0003181094,0.00013103784,0.000038687573,0.001275061],"genre_scores_gemma":[0.99769294,0.00022260517,0.000083567495,0.00080979767,0.00014838469,0.0000031721142,0.00084215705,0.000005818867,0.00019158183],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9971899,0.0006935474,0.00042403393,0.00056694297,0.0002189086,0.0009066985],"domain_scores_gemma":[0.9982309,0.0011242355,0.00011324451,0.0003324873,0.000040495943,0.00015866713],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007915651,0.00027684923,0.0005371118,0.000506098,0.000244176,0.00007351343,0.0004008766,0.0004115621,0.0027131222],"category_scores_gemma":[0.000102112164,0.00023611009,0.00009307932,0.0004436855,0.00034298544,0.00024313634,0.000056399163,0.0007501944,0.00027212477],"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":[0.00029153196,0.00003465262,0.99079347,0.00001994782,0.00008874728,0.0009057734,0.0007133479,0.0045614354,0.00026962374,0.000010816672,0.0004264602,0.0018841719],"study_design_scores_gemma":[0.002015053,0.00044790236,0.9765211,0.00029991678,0.000049199312,0.00042972117,0.003998281,0.014701758,0.00017823123,0.0004425992,0.0005322814,0.00038399964],"about_ca_topic_score_codex":0.032509103,"about_ca_topic_score_gemma":0.07209229,"teacher_disagreement_score":0.039583184,"about_ca_system_score_codex":0.000027183927,"about_ca_system_score_gemma":0.00020706523,"threshold_uncertainty_score":0.9981985},"labels":[],"label_agreement":null},{"id":"W4415348092","doi":"10.1016/j.geomorph.2025.110057","title":"A giant Early Holocene tsunamigenic rock-ice avalanche in South Greenland preconditioned by glacial debuttressing","year":2025,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Swiss Polar Institute; Novo Nordisk Fonden; Danmarks Frie Forskningsfond; Agence Nationale de la Recherche; Villum Fonden","keywords":"Deglaciation; Landform; Surface exposure dating; Moraine; Debris; Glacial period; Holocene; Cosmogenic nuclide","score_opus":0.005095156633412183,"score_gpt":0.2118596024395077,"score_spread":0.20676444580609551,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415348092","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":[0.99274707,0.00026674825,0.0012881344,0.0004266069,0.00031413647,0.00018427953,0.00005585314,0.000041732164,0.004675426],"genre_scores_gemma":[0.99547815,0.000030012077,0.00014168968,0.0005376327,0.00002624949,0.000022608629,0.00007778019,0.000011975475,0.003673917],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986152,0.00010879216,0.00027815395,0.00041454894,0.00012784629,0.00045546435],"domain_scores_gemma":[0.99957114,0.000046671765,0.00008491823,0.00021694707,0.0000068073487,0.00007349997],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021911203,0.0001625012,0.00024049326,0.0000770608,0.00022687156,0.000022435615,0.00022033964,0.00026761668,0.0028354432],"category_scores_gemma":[0.000028693456,0.00013666497,0.000057249454,0.00031606058,0.00012462323,0.00009354877,0.00023548988,0.00029789066,0.00052736624],"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":[0.00034627953,0.00026304074,0.9432224,0.000022289487,0.000083725485,0.00033150744,0.0032802422,0.0016814534,0.019340394,0.0000559603,0.021633299,0.009739424],"study_design_scores_gemma":[0.0032228262,0.00015784685,0.98041093,0.000058005568,0.000061585975,0.000084394116,0.00014139633,0.001841098,0.0026459736,0.0010422198,0.009921171,0.00041256403],"about_ca_topic_score_codex":0.0009060008,"about_ca_topic_score_gemma":0.0003216237,"teacher_disagreement_score":0.037188534,"about_ca_system_score_codex":0.00012547051,"about_ca_system_score_gemma":0.000025210715,"threshold_uncertainty_score":0.9980761},"labels":[],"label_agreement":null},{"id":"W4415817066","doi":"10.1016/j.geomorph.2025.110085","title":"Morphometrics and process regimes: Defining the beach-dune transition zone on an evolving coast","year":2025,"lang":"en","type":"article","venue":"Geomorphology","topic":"Coastal and Marine Dynamics","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Windsor; University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada; Parks Canada","keywords":"Elevation (ballistics); Storm; Morphometrics; Landform; Sea level; Plage; Shore","score_opus":0.008040227454400983,"score_gpt":0.2216132460735747,"score_spread":0.21357301861917372,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415817066","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":[0.98766714,0.0008379621,0.0031550245,0.0016438069,0.0003605159,0.00017995016,0.0001476446,0.000054219614,0.0059537184],"genre_scores_gemma":[0.9970726,0.000068111774,0.0003132729,0.0013194373,0.000030640065,0.0000026412276,0.00061262207,0.0000030654544,0.00057764805],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9991204,0.000077892335,0.00015471273,0.00027349353,0.00011577615,0.0002577261],"domain_scores_gemma":[0.99942243,0.00023854512,0.00005068193,0.00017467876,0.000053536667,0.000060110557],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029177716,0.00012293016,0.00015952515,0.00018407339,0.00027053177,0.00005472695,0.00016117994,0.00008037516,0.00027256942],"category_scores_gemma":[0.000082233906,0.00008817313,0.000024968529,0.00053580623,0.00015566719,0.00013259791,0.00001958351,0.0002157925,0.000020853486],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000643535,0.00022117664,0.26874086,0.0001967156,0.00010175455,0.00026074506,0.0026079891,0.017790148,0.00011747169,0.0073344572,0.0074883164,0.6944968],"study_design_scores_gemma":[0.0017453273,0.0015506663,0.7973426,0.000088882676,0.00012982548,0.0005338396,0.0042483737,0.17040801,0.00007789171,0.0055549336,0.017764645,0.00055499875],"about_ca_topic_score_codex":0.0028766016,"about_ca_topic_score_gemma":0.007441733,"teacher_disagreement_score":0.69394183,"about_ca_system_score_codex":0.0000038305043,"about_ca_system_score_gemma":0.000044624358,"threshold_uncertainty_score":0.43485805},"labels":[],"label_agreement":null},{"id":"W649483834","doi":"10.1016/j.geomorph.2015.04.033","title":"Diagnostic characteristics and paleodynamics of supraglacial rock avalanches, Innerdalen, Western Norway","year":2015,"lang":"en","type":"article","venue":"Geomorphology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":31,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Norges Geologiske Undersøkelse","keywords":"Moraine; Geology; Terminal moraine; Landform; Geomorphology; Pleistocene; Glacier; Elevation (ballistics); Cosmogenic nuclide; Paleontology; Geometry","score_opus":0.00906573343611617,"score_gpt":0.21044539536741314,"score_spread":0.20137966193129697,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W649483834","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":[0.99755335,0.0000802151,0.00045318683,0.00022311612,0.0003978085,0.000103659026,0.00006088758,0.0000140388565,0.0011137184],"genre_scores_gemma":[0.9987617,0.00016717396,0.00014996393,0.00016133621,0.000064635,0.0000054578713,0.00005691859,0.000012132099,0.0006206419],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991073,0.000050270533,0.00023320082,0.00021758203,0.00014384705,0.00024778128],"domain_scores_gemma":[0.999435,0.00011317926,0.00011293529,0.00017785124,0.000016365066,0.00014468141],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018303412,0.00012103668,0.00023594177,0.000025439114,0.000038232036,0.00000882093,0.00013413969,0.0001682849,0.00062702235],"category_scores_gemma":[0.00017342682,0.0000980791,0.000025286392,0.0000846022,0.00018625022,0.000055649154,0.00022334239,0.00014847216,0.00043864024],"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":[0.00004241809,0.000058882804,0.9946105,0.000009755098,0.000013233384,0.00010030405,0.0004559177,0.00022314163,0.0008047733,0.000031882762,0.0017134574,0.0019357268],"study_design_scores_gemma":[0.0010844546,0.00034360558,0.97136176,0.000014751708,0.00005302078,0.00036854632,0.00006058306,0.001226247,0.00016213082,0.00034623995,0.024742339,0.00023634954],"about_ca_topic_score_codex":0.00016734794,"about_ca_topic_score_gemma":0.0002069021,"teacher_disagreement_score":0.023248775,"about_ca_system_score_codex":0.000036789228,"about_ca_system_score_gemma":0.000016270107,"threshold_uncertainty_score":0.6865455},"labels":[],"label_agreement":null},{"id":"W826306592","doi":"10.1016/j.geomorph.2015.07.006","title":"Glacier change from the early Little Ice Age to 2005 in the Torngat Mountains, northern Labrador, Canada","year":2015,"lang":"en","type":"article","venue":"Geomorphology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Ottawa; Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada; Memorial University of Newfoundland; W. Garfield Weston Foundation; ArcticNet","keywords":"Glacier; Geology; Glacier morphology; Physical geography; Moraine; Glacier mass balance; Rock glacier; Arctic; Tidewater glacier cycle; Climate change; Surge; Ice field; Accumulation zone; Climatology; Cryosphere; Geomorphology; Oceanography; Geography; Ice stream; Sea ice","score_opus":0.045362963033546824,"score_gpt":0.2390649593988728,"score_spread":0.19370199636532598,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W826306592","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":[0.97561526,0.0011182,0.000002429065,0.020461231,0.0005449366,0.00032732272,0.0002452567,0.000010495945,0.001674862],"genre_scores_gemma":[0.9864384,0.000020553989,0.000036275494,0.012475621,0.00022126653,0.000015849942,0.00032840174,0.000003302962,0.0004603459],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99791986,0.0006851994,0.00017272269,0.00029059072,0.00026067448,0.0006709505],"domain_scores_gemma":[0.9985949,0.00073449424,0.00004043647,0.0004122577,0.000045789773,0.0001721507],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0009163099,0.00013735631,0.00019754362,0.00004195597,0.0001736961,0.000028368062,0.00079925614,0.00014589442,0.0015119499],"category_scores_gemma":[0.0001632703,0.00008017885,0.000024422881,0.00025734556,0.00023439273,0.000069020716,0.00004573872,0.0004356855,0.0014068792],"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":[0.00007068133,0.00000966919,0.9836118,9.635413e-7,0.000012300292,0.0007094265,0.0030109917,0.000056248406,0.0000012074836,0.000023054752,0.011913154,0.0005804587],"study_design_scores_gemma":[0.00028776968,0.00008919381,0.91547203,0.000002434011,0.000006345042,0.000103790946,0.0013071744,0.000044704506,0.000002235285,0.0003039547,0.08228273,0.00009765059],"about_ca_topic_score_codex":0.9461027,"about_ca_topic_score_gemma":0.99912554,"teacher_disagreement_score":0.07036957,"about_ca_system_score_codex":0.000008349582,"about_ca_system_score_gemma":0.00029106415,"threshold_uncertainty_score":0.9994008},"labels":[],"label_agreement":null},{"id":"W831149547","doi":"10.1016/j.geomorph.2015.06.036","title":"Using LiDAR to characterize logjams in lowland rivers","year":2015,"lang":"en","type":"article","venue":"Geomorphology","topic":"Remote Sensing and LiDAR Applications","field":"Environmental Science","cited_by":31,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ministry of Forests; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Lidar; Riparian zone; Vegetation (pathology); Watershed; Hydrology (agriculture); Environmental science; STREAMS; Channel (broadcasting); Field (mathematics); Remote sensing; Geology; Habitat; Ecology","score_opus":0.05375708325117837,"score_gpt":0.27250653266367575,"score_spread":0.21874944941249738,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W831149547","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":[0.99095833,0.0000038500334,0.002169042,0.0006703635,0.00012989531,0.00012277807,0.000006684493,0.000019499605,0.0059195394],"genre_scores_gemma":[0.991751,0.000001161337,0.0070999805,0.00076101883,0.00003262426,0.0000014501353,0.000013373068,0.000007948953,0.0003314274],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9993029,0.000041638774,0.00011410672,0.00022369884,0.00008943054,0.00022818353],"domain_scores_gemma":[0.9996122,0.000011143385,0.000030170071,0.00020300347,0.0000055632636,0.00013787854],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001757933,0.00007239237,0.00010919423,0.00004106289,0.000035115692,0.000009334845,0.000118625205,0.000061167106,0.00035686995],"category_scores_gemma":[0.000029457766,0.00007192272,0.000015634061,0.00021151936,0.00010352683,0.000042048396,0.000104735205,0.000080176156,0.0020228978],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012974128,0.00029648887,0.3437187,0.0000048559787,0.00001508047,0.00041392376,0.005541182,0.014467628,0.57215446,0.00014106884,0.022346625,0.04077023],"study_design_scores_gemma":[0.0017323644,0.00023586182,0.705644,0.000017214728,0.00001839477,0.00056421367,0.00040749952,0.00538238,0.005174169,0.0014777065,0.2787557,0.0005904914],"about_ca_topic_score_codex":0.0030930773,"about_ca_topic_score_gemma":0.00030420636,"teacher_disagreement_score":0.5669803,"about_ca_system_score_codex":0.00013387323,"about_ca_system_score_gemma":0.00001283771,"threshold_uncertainty_score":0.99875414},"labels":[],"label_agreement":null}]}