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Record W2105053136 · doi:10.1029/2001jd000533

Chemical depletion of Arctic ozone in winter 1999/2000

2002· article· en· W2105053136 on OpenAlex
Markus Rex, R. J. Salawitch, Neil Harris, Peter von der Gathen, G. O. Braathen, Astrid Schulz, Holger Deckelmann, Martyn P. Chipperfield, Björn‐Martin Sinnhuber, E. Reimer, R. Alfier, R. M. Bevilacqua, K. W. Hoppel, M. D. Fromm, J. D. Lumpe, H. Küllmann, A. Kleinböhl, H. Bremer, M. von König, K. Künzi, D. W. Toohey, Holger Vömel, Erik Richard, K. Aikin, Hans-Juerg Jost, Jeffery B. Greenblatt, M. Loewenstein, James R. Podolske, C. R. Webster, Gregory J. Flesch, D. C. Scott, R. L. Herman, J. W. Elkins, Eric Ray, F. L. Moore, D. F. Hurst, P. A. Romashkin, G. C. Toon, B. Sen, J. J. Margitan, P. O. Wennberg, Roland Neuber, M. Allart, Bojan Bojkov, H. Claude, J. Davies, Will Davies, H. De Backer, H. Dier, V. Dorokhov, H. Fast, Yasuyuki Kondo, Ella-Maria Kyrö, Z. Litynska, I. S. Mikkelsen, M. J. Molyneux, Emily Moran, Tomohiro Nagai, Hideaki Nakane, C. Parrondo, F. Ravegnani, P. Skřivánková, P. Viatte, V. Yushkov

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

affAt least one author lists a Canadian institution in the pinned OpenAlex snapshot.

Bibliographic record

VenueJournal of Geophysical Research Atmospheres · 2002
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicAtmospheric Ozone and Climate
Canadian institutionsEnvironment and Climate Change Canada
Fundersnot available
KeywordsOzoneStratosphereArcticPolar vortexOzone depletionAtmospheric sciencesEnvironmental scienceClimatologyOzone layerChemical transport modelMeteorologyOceanographyGeologyPhysics

Abstract

fetched live from OpenAlex

During Arctic winters with a cold, stable stratospheric circulation, reactions on the surface of polar stratospheric clouds (PSCs) lead to elevated abundances of chlorine monoxide (ClO) that, in the presence of sunlight, destroy ozone. Here we show that PSCs were more widespread during the 1999/2000 Arctic winter than for any other Arctic winter in the past two decades. We have used three fundamentally different approaches to derive the degree of chemical ozone loss from ozonesonde, balloon, aircraft, and satellite instruments. We show that the ozone losses derived from these different instruments and approaches agree very well, resulting in a high level of confidence in the results. Chemical processes led to a 70% reduction of ozone for a region ∼1 km thick of the lower stratosphere, the largest degree of local loss ever reported for the Arctic. The Match analysis of ozonesonde data shows that the accumulated chemical loss of ozone inside the Arctic vortex totaled 117 ± 14 Dobson units (DU) by the end of winter. This loss, combined with dynamical redistribution of air parcels, resulted in a 88 ± 13 DU reduction in total column ozone compared to the amount that would have been present in the absence of any chemical loss. The chemical loss of ozone throughout the winter was nearly balanced by dynamical resupply of ozone to the vortex, resulting in a relatively constant value of total ozone of 340 ± 50 DU between early January and late March. This observation of nearly constant total ozone in the Arctic vortex is in contrast to the increase of total column ozone between January and March that is observed during most years.

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.

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 categoriesInsufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.168
Threshold uncertainty score0.992

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 science0.0000.000
Research integrity0.0000.001
Insufficient payload (model declined to judge)0.0090.000

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 head0.033
GPT teacher head0.281
Teacher spread0.248 · 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