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Record W2165644044 · doi:10.1029/2004jd005018

Polar vortex evolution during the 2002 Antarctic major warming as observed by the Odin satellite

2005· article· en· W2165644044 on OpenAlexaff
Philippe Ricaud, Franck Lefèvre, Gwenaël Berthet, D. Murtagh, E. J. Llewellyn, G. Mégie, E. Kyrölä, G. W. Leppelmeier, Harri Auvinen, Cathy Boonne, S. Brohede, D. A. Degenstein, J. de La Noë, É. Dupuy, L. El Amraoui, Patrick Eriksson, W. F. J. Evans, U. Frisk, R. L. Gattinger, F. Girod, C. S. Haley, S. Hassinen, Alain Hauchecorne, Carlos Jiménez, E. Kyrö, Nicolas Lautié, É. Le Flochmoën, Nicholas Lloyd, J. C. McConnell, I. C. McDade, L. Nordh, M. Olberg, Andréa Pazmiño, S. V. Petelina, Å. Sandqvist, Annika Seppälä, Christopher E. Sioris, B. H. Solheim, J. Stegman, Kimberly Strong, P. Taalas, J. Urban, Christian von Savigny, F. von Schéele, G. Witt

Bibliographic record

VenueJournal of Geophysical Research Atmospheres · 2005
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicAtmospheric Ozone and Climate
Canadian institutionsUniversity of TorontoYork UniversityTrent UniversityUniversity of Saskatchewan
Fundersnot available
KeywordsPolar vortexOzone depletionStratosphereMicrowave Limb SounderAtmospheric sciencesOzoneVortexSudden stratospheric warmingEnvironmental sciencePhysicsMeteorology

Abstract

fetched live from OpenAlex

In September 2002 the Antarctic polar vortex split in two under the influence of a sudden warming. During this event, the Odin satellite was able to measure both ozone (O 3 ) and chlorine monoxide (ClO), a key constituent responsible for the so‐called “ozone hole”, together with nitrous oxide (N 2 O), a dynamical tracer, and nitric acid (HNO 3 ) and nitrogen dioxide (NO 2 ), tracers of denitrification. The submillimeter radiometer (SMR) microwave instrument and the Optical Spectrograph and Infrared Imager System (OSIRIS) UV‐visible light spectrometer (VIS) and IR instrument on board Odin have sounded the polar vortex during three different periods: before (19–20 September), during (24–25 September), and after (1–2 and 4–5 October) the vortex split. Odin observations coupled with the Reactive Processes Ruling the Ozone Budget in the Stratosphere (REPROBUS) chemical transport model at and above 500 K isentropic surfaces (heights above 18 km) reveal that on 19–20 September the Antarctic vortex was dynamically stable and chemically nominal: denitrified, with a nearly complete chlorine activation, and a 70% O 3 loss at 500 K. On 25–26 September the unusual morphology of the vortex is monitored by the N 2 O observations. The measured ClO decay is consistent with other observations performed in 2002 and in the past. The vortex split episode is followed by a nearly complete deactivation of the ClO radicals on 1–2 October, leading to the end of the chemical O 3 loss, while HNO 3 and NO 2 fields start increasing. This acceleration of the chlorine deactivation results from the warming of the Antarctic vortex in 2002, putting an early end to the polar stratospheric cloud season. The model simulation suggests that the vortex elongation toward regions of strong solar irradiance also favored the rapid reformation of ClONO 2 . The observed dynamical and chemical evolution of the 2002 polar vortex is qualitatively well reproduced by REPROBUS. Quantitative differences are mainly attributable to the too weak amounts of HNO 3 in the model, which do not produce enough NO 2 in presence of sunlight to deactivate chlorine as fast as observed by Odin.

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)0.002
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesInsufficient payload (model declined to judge)
Consensus categoriesInsufficient payload (model declined to judge)
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.324
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0020.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.001
Science and technology studies0.0010.000
Scholarly communication0.0000.001
Open science0.0010.000
Research integrity0.0000.001
Insufficient payload (model declined to judge)0.0030.001

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 head0.027
GPT teacher head0.277
Teacher spread0.249 · 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; both teacher heads agree on what is shown here.

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

Citations119
Published2005
Admission routes1
Has abstractyes

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