{"id":"W2097900558","doi":"10.1175/2008jcli2215.1","title":"The Impact of Stratospheric Ozone Recovery on Tropopause Height Trends","year":2008,"lang":"en","type":"article","venue":"Journal of Climate","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":88,"is_retracted":false,"has_abstract":true,"ca_institutions":"Environment and Climate Change Canada; University of Toronto","funders":"Lawrence Livermore National Laboratory; Scheme for Promotion of Academic and Research Collaboration; University of Toronto; Branco Weiss Fellowship – Society in Science; Goddard Space Flight Center; National Oceanic and Atmospheric Administration; York University; National Aeronautics and Space Administration; U.S. Department of Energy; National Science Foundation","keywords":"Tropopause; Stratosphere; Climatology; Environmental science; Atmospheric sciences; Ozone depletion; Southern Hemisphere; Climate change; Ozone layer; Northern Hemisphere; Climate model; Ozone; Meteorology; Geology; 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":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007592259,0.0001699155,0.0002338467,0.0003604445,0.0002672361,0.0005726456,0.0003662055,0.0003600258,0.0009538938],"category_scores_gemma":[0.002621773,0.0001131254,0.0004294282,0.0004653049,0.0002136646,0.0005035918,0.0004520719,0.0003773948,0.00009420624],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0004052543,"about_ca_system_score_gemma":0.0002795359,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.01540933,"about_ca_topic_score_gemma":0.01282703,"domain_scores_codex":[0.999813,0.00005052768,0.0000130163,0.00003264637,0.00004553208,0.00004530771],"domain_scores_gemma":[0.9991248,0.0003150988,0.0002476416,0.0001253446,0.0001327271,0.0000544529],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0009989692,0.0001210475,0.8679163,0.0001022335,0.0005166656,0.0003002254,0.0001482679,0.08562062,0.02511473,0.001294027,0.0006224007,0.0172445],"study_design_scores_gemma":[0.00002369656,0.0001752079,0.9336132,0.00001169246,0.0001274485,0.00006797123,0.0001048984,0.05752135,0.007018698,0.0003959061,0.0009238473,0.00001599141],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9979841,0.0001633614,0.0003396345,0.00009745765,0.000005681665,0.000002710911,0.0006239178,0.00002374746,0.000759409],"genre_scores_gemma":[0.9994453,0.00004209304,0.00007696459,0.000007390739,0.000002889842,0.000001243482,0.0003580786,0.000003567567,0.00006251886],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.01540933,"threshold_uncertainty_score":0.03063923,"prediction_status":"machine_predicted_unvalidated"},"machine_scores":{"provisional":true,"baseline":true,"maturity_gate_passed":false,"score_opus":0.01487682028516484,"score_gpt":0.2485127949517512,"score_spread":0.2336359746665864,"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."}}