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Record W2282675050

Variability and Trends in Ozone since 2002 from the GOMOS/ENVISAT IPF V6 Reprocessing

2012· preprint· en· W2282675050 on OpenAlexaboutno aff
Alain Hauchecorne, Jean‐Loup Bertaux, Beatriz M. Funatsu, F. Dalaudier, G. Barrot, Laurent Blanot, Viktoria Sofieva, E. Kyrölä, Johanna Tamminen, D. Fussen, F. Vanhellemont, Angelika Dehn, L. Saavedra de Miguel

Bibliographic record

VenueHAL (Le Centre pour la Communication Scientifique Directe) · 2012
Typepreprint
Languageen
FieldEarth and Planetary Sciences
TopicAtmospheric Ozone and Climate
Canadian institutionsnot available
Fundersnot available
KeywordsStratosphereEnvironmental scienceOzone layerOccultationTotal Ozone Mapping SpectrometerRemote sensingAtmospheric sciencesAtmosphere (unit)OzoneRadiative transferSatelliteSpectrometerRadianceMeteorologyPhysicsGeologyOpticsAstrophysicsAstronomy
DOInot available

Abstract

fetched live from OpenAlex

Following the Montreal protocol and its amendments, the concentration of Ozone Depleting Gases (ODP) is decreasing slowly in the stratosphere. We expect a progressive recovery of the ozone layer during the next decades. However, due to complex interactions between radiative, dynamical and chemical processes in the atmosphere, the rate at which the recovery will take place is still very uncertain. Furthermore, the ozone layer is perturbed by external forcings like solar variability and volcanic eruptions. Accurate measurements of the 3D distribution of stratospheric ozone are strongly required to understand all causes of the ozone layer variability in order to better predict its future evolution. The global coverage can be only obtained from satellite observations and a validation with ground-based NDACC instruments is needed to assess the quality of the data. The GOMOS instrument on board ENVISAT (launched in 2002 in a helio-synchronous polar orbit) measures the vertical profiles of stratospheric and mesospheric constituents using the stellar occultation technique with a UV-visible spectrometer (250 to 680 nm) for O3, NO2, NO3 and aerosols and two dedicated near IR spectrometers centred at 760 nm for O2 and 940 nm for H2O. The atmospheric transmission is computed by the ratio between a star spectrum measured through the atmosphere and a reference star spectrum measured outside the atmosphere. Vertical profiles of constituents are obtained by a global spectral inversion followed by a vertical inversion using a Tikhonov regularization. GOMOS is by principle an auto-calibrated instrument because it does not depend on radiometric calibration. However, due to the ageing of the CCD detector, creating an increase in the dark charge not perfectly corrected in Version 5 algorithms, a bias was detected in the difference between GOMOS and NDACC ozone LIDARs during recent years (Keckhut et al., ACP, 2010). A full reprocessing of GOMOS data since 2002 using V6 algorithms is in progress. This new version handles correctly the CCD dark charge increase and the bias is expected to disappear. The GOMOS V6 ozone climatology for the period 2002-2011 from 15 to 100 km will be presented. A comparison will be made with NDACC ozone LIDARs for the common altitude range (15-40 km). The ozone evolution during this period and the attribution to various forcings (ODP, Brewer-Dobson circulation, solar cycle, QBO, ENSO, ...) will be discussed.

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 machine prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.001
Version: metacan-v3-hybrid-931329e0061cValidation 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 score0.051
Threshold uncertainty score0.101

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.002
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
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 head0.017
GPT teacher head0.220
Teacher spread0.203 · 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 source (direct Gemma or distilled Codex), 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

Citations0
Published2012
Admission routes1
Has abstractyes

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