{"id":"W4304203533","doi":"10.1038/s41467-022-33231-x","title":"The unquantified mass loss of Northern Hemisphere marine-terminating glaciers from 2000–2020","year":2022,"lang":"en","type":"article","venue":"Nature Communications","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"ca_institutions":"University of Lethbridge; University of Waterloo; University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada; National Aeronautics and Space Administration; ArcticNet; Uniwersytet Śląski w Katowicach; Nuclear Safety and Security Commission; University of Ottawa","keywords":"Glacier; Geology; Fjord; Arctic; Glacier ice accumulation; Oceanography; Northern Hemisphere; Glacier terminus; Ablation zone; Glacier morphology; Climate change; Climatology; Physical geography; Greenland ice sheet; Cryosphere; Sea ice; Arctic ice pack; Ice stream; Antarctic sea ice; Geomorphology; Geography","routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false,"invisible_to_affiliation_only":false},"retraction":null,"screen":null,"direct_labels":[],"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000281531,0.00009272034,0.0001225475,0.00000897371,0.002230896,0.00003513081,0.001388796,0.00005404828,0.001069018],"category_scores_gemma":[0.0001745663,0.00007242029,0.00007391612,0.0004877992,0.0002319312,0.00005595815,0.0002888163,0.0007948714,0.00001188411],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001751428,"about_ca_system_score_gemma":0.00008118914,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002634259,"about_ca_topic_score_gemma":0.04343111,"domain_scores_codex":[0.9990193,0.000173185,0.0002475417,0.0001444579,0.0002512081,0.0001643323],"domain_scores_gemma":[0.9972705,0.001354797,0.0001748332,0.001065421,0.00009586287,0.00003864328],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00001715275,0.00002416609,0.9637741,0.000003107473,0.0000605401,0.000001782597,0.0007193986,0.00143232,0.00003451673,0.0005713105,0.002682283,0.0306793],"study_design_scores_gemma":[0.0001723763,0.00002457737,0.6909976,0.000004491436,0.00002924886,0.000002500063,0.005632068,0.01070978,0.00001441947,0.001142902,0.291141,0.0001290345],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.933723,0.03380655,0.00006391828,0.01397948,0.000866093,0.0004003223,0.0009726853,0.00008075569,0.01610715],"genre_scores_gemma":[0.9949639,0.0009177519,0.002678406,0.0002763628,0.0000394399,0.00001165041,0.0005554555,0.000004631083,0.000552349],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2884587,"threshold_uncertainty_score":0.9998441,"prediction_status":"machine_predicted_unvalidated"},"machine_scores":{"provisional":true,"baseline":true,"maturity_gate_passed":false,"score_opus":0.01658192500917759,"score_gpt":0.2410861274800087,"score_spread":0.2245042024708311,"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."}}