{"id":"W4281616579","doi":"10.1139/as-2021-0039","title":"Anomalous surface elevation, velocity, and area changes of Split Lake Glacier, western Prince of Wales Icefield, Canadian High Arctic","year":2022,"lang":"en","type":"article","venue":"Arctic Science","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"ca_institutions":"University of Ottawa; University of Waterloo","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; Environment and Climate Change Canada; University of Waterloo; ArcticNet; University of Ottawa","keywords":"Ice field; Glacier; Surge; Geology; Elevation (ballistics); Glacier morphology; Arctic; Physical geography; Bedrock; Glacier mass balance; Accumulation zone; Geomorphology; Climatology; Oceanography; Ice stream; Geography; Arctic ice pack; Antarctic sea ice; Sea ice; Cryosphere; Geometry","routes":{"ca_aff":true,"ca_fund":true,"ca_venue":true,"about_ca":true,"invisible_to_affiliation_only":false},"retraction":null,"screen":null,"direct_labels":[],"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001974303,0.0001750645,0.0001234461,0.001154,0.0007054402,0.0005680781,0.0002194291,0.00009857755,0.0004547756],"category_scores_gemma":[0.0007280491,0.0001271494,0.000127628,0.001297348,0.0003099316,0.0001826438,0.0002755302,0.000150657,0.00009420014],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.002678353,"about_ca_system_score_gemma":0.002251697,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.9324937,"about_ca_topic_score_gemma":0.9805494,"domain_scores_codex":[0.9998432,0.000009630809,0.000005951811,0.00002704285,0.0000619577,0.00005214526],"domain_scores_gemma":[0.9996269,0.00003901836,0.00006550786,0.00002173052,0.0001786574,0.00006823054],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00006000283,0.0000144759,0.9886534,0.00001373621,0.00003398372,0.00006929321,0.0006113556,0.0005553587,0.002298304,0.00006254946,0.0003543665,0.007273302],"study_design_scores_gemma":[8.301554e-7,0.000003479122,0.9989543,0.000002439599,0.000003126631,0.00001675323,0.0002583347,0.0003365405,0.000125169,0.000005022048,0.0002915915,0.000002387654],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.998781,0.00004217247,0.00004240145,0.00001142371,8.871969e-7,0.000002545266,0.0006412734,0.000004428757,0.0004738231],"genre_scores_gemma":[0.9974664,0.00006844262,0.0002426358,0.000007745553,9.97665e-7,0.000003758547,0.001873888,0.000002339832,0.0003337611],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.06750631,"threshold_uncertainty_score":0.1358077,"prediction_status":"machine_predicted_unvalidated"},"machine_scores":{"provisional":true,"baseline":true,"maturity_gate_passed":false,"score_opus":0.02124906436465077,"score_gpt":0.2103031746047903,"score_spread":0.1890541102401395,"validation_status":"score_only:v0-immature-baseline","note":"Baseline scores from an immature model (maturity gate not passed). Scores rank; they never assert a category."}}