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Record W2083980676 · doi:10.1029/2009jd013347

Anthropogenic forcing of the Northern Annular Mode in CCMVal‐2 models

2010· article· en· W2083980676 on OpenAlexaff
Olaf Morgenstern, Hideharu Akiyoshi, Slimane Bekki, Peter Braesicke, Neal Butchart, Martyn P. Chipperfield, David Cugnet, Makoto Deushi, Sandip Dhomse, Rolando R. García, Andrew Gettelman, Nathan P. Gillett, Steven C. Hardiman, Julien Jumelet, D. E. Kinnison, Jean‐François Lamarque, François Lott, Marion Marchand, Martine Michou, Tetsu Nakamura, Dirk Olivié, Thomas Peter, David A. Plummer, J. A. Pyle, Eugene Rozanov, David Saint‐Martin, John Scinocca, Kiyotaka Shibata, Michael Sigmond, Dan Smale, H. Teyssèdre, Wenshou Tian, Aurore Voldoire, Y. Yamashita

Bibliographic record

VenueJournal of Geophysical Research Atmospheres · 2010
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicAtmospheric Ozone and Climate
Canadian institutionsUniversity of VictoriaUniversity of TorontoEnvironment and Climate Change Canada
FundersNatural Environment Research CouncilEngineering and Physical Sciences Research CouncilGoddard Space Flight CenterOffice of ScienceScheme for Promotion of Academic and Research CollaborationNational Center for Atmospheric ResearchMinistry of Education, IndiaUniversity of EdinburghMet OfficeNational Oceanic and Atmospheric AdministrationSight Research UKUniversity Corporation for Atmospheric ResearchNational Aeronautics and Space AdministrationDepartment for Environment, Food and Rural Affairs, UK GovernmentNational Science Foundation
KeywordsStratosphereGeopotential heightTroposphereClimatologyEnvironmental scienceAtmospheric sciencesForcing (mathematics)Climate modelGreenhouse gasOzone depletionCoherence (philosophical gambling strategy)Mode (computer interface)Horizontal resolutionClimate changeMeteorologyGeologyPhysicsOceanography

Abstract

fetched live from OpenAlex

We address the question of how ozone and long‐lived greenhouse gas changes impact the Northern Annular Mode (NAM). Using reanalyses and results from the Chemistry‐Climate Model Validation 2 (CCMVal‐2) initiative, we calculate seasonal NAM indices from geopotential height for winter and spring. From these, we determine the strength of stratosphere‐troposphere coupling in the model simulations and the reanalyses. For both seasons, we find a large spread in the ability of models to represent the vertical coherence of the NAM, although most models are within the 95% confidence interval. In winter, many models underestimate the vertical coherence derived from the reanalyses. Some models exhibit substantial differences in vertical coherence between simulations driven with modeled and observed ocean conditions. In spring, in the simulations using modeled ocean conditions, models with poorer horizontal or vertical resolution tend to underestimate the vertical coupling, and vice versa for models with better resolution. Accounting for model deficits in producing an appropriate troposphere‐stratosphere coupling, we show significant correlations of the NAM in winter with three indices representing the anthropogenic impact. Analysis of cross‐correlations between these indices suggests that increasing CO 2 is the main reason for these correlations in this season. In the CCMVal‐2 simulations, CO 2 increases are associated with a weakening of the NAM in winter. For spring, we show that the dominant effect is chemical ozone depletion leading to a transient strengthening of the NAM, with CO 2 changes playing an insignificant role.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.001
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.119
Threshold uncertainty score0.997

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.001
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0010.000
Research integrity0.0000.001
Insufficient payload (model declined to judge)0.0010.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.028
GPT teacher head0.305
Teacher spread0.276 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one teacher head, not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designObservational
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations40
Published2010
Admission routes1
Has abstractyes

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