{"id":"W2092293680","doi":"10.1175/jcli-d-13-00125.1","title":"The Origins of Late-Twentieth-Century Variations in the Large-Scale North Atlantic Circulation","year":2014,"lang":"en","type":"article","venue":"Journal of Climate","topic":"Climate variability and models","field":"Environmental Science","cited_by":167,"is_retracted":false,"has_abstract":true,"ca_institutions":"","funders":"Climate Program Office; National Oceanic and Atmospheric Administration; National Center for Atmospheric Research; National Science Foundation","keywords":"Shutdown of thermohaline circulation; Ocean gyre; Climatology; North Atlantic Deep Water; Thermohaline circulation; Atlantic Equatorial mode; Forcing (mathematics); Hindcast; Equator; Geology; Ocean current; Oceanography; Tropical Atlantic; Environmental science; Latitude; Sea surface temperature; Subtropics","routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true,"invisible_to_affiliation_only":true},"retraction":null,"screen":null,"direct_labels":[],"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002207129,0.00006738956,0.000136982,0.0000286513,0.0001680846,0.00003443259,0.0002728729,0.00003659794,0.00009886819],"category_scores_gemma":[0.00009102519,0.00003713429,0.00009120227,0.0002050446,0.00006606117,0.0001957893,0.0000579714,0.0001721064,0.00002249942],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00009309412,"about_ca_system_score_gemma":0.00001077224,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00009069054,"about_ca_topic_score_gemma":0.0008302568,"domain_scores_codex":[0.9987085,0.0001990069,0.0004752843,0.00007983115,0.000335983,0.0002013879],"domain_scores_gemma":[0.9990586,0.0003071119,0.0003725146,0.0002061818,0.00002190928,0.00003365284],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00003429979,0.00022818,0.9645065,0.00001518445,0.00001057224,0.000001467187,0.002481062,0.02518708,0.0007035561,0.006112704,0.00007811109,0.0006412857],"study_design_scores_gemma":[0.0004649871,0.00005516666,0.9416224,0.00002197953,0.00003886588,0.0000111795,0.0001992414,0.03606578,0.00001064849,0.002884259,0.01856176,0.00006376689],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9957376,0.00001691353,0.001734768,0.0007588863,0.000222485,0.0001016542,0.000006134994,0.000003104754,0.001418438],"genre_scores_gemma":[0.9989803,0.0006113451,0.0002426819,0.0001090754,0.00004276051,0.000001688987,0.000003024031,0.000004704343,0.000004422254],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.02288413,"threshold_uncertainty_score":0.1514292,"prediction_status":"machine_predicted_unvalidated"},"machine_scores":{"provisional":true,"baseline":true,"maturity_gate_passed":false,"score_opus":0.01130571493272049,"score_gpt":0.2409489098776701,"score_spread":0.2296431949449497,"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."}}