Stratospheric circulation changes: investigations using multidecadal observations and simulations of inorganic fluorine
Notice bibliographique
Résumé
The intense human activity of the past two hundred years has perturbed the subtle balance existing between the spheres of the Earth system. The atmospheric composition has been modified with massive emissions of greenhouse gases and substances depleting the life-essential ozone layer (ODSs). The most known to the general public resulting changes are certainly the global warming of the troposphere and the dramatic formation of the Antarctic ozone hole. However, it is less generally known that the most robustly modelled response to the increase of greenhouse gases, and the resulting global warming, is a speeding-up of the transport circulation occurring in the stratosphere, the atmospheric layer that is situated well above our head, between 10 and 50 km. This transport circulation, referred to as the Brewer-Dobson circulation (BDC), controls the distribution of ozone and other long-lived gaseous constituents of the stratosphere. Therefore, it is crucial to characterize the BDC and its changes to assess precisely the healing of the ozone layer, expected to occur gradually in the twenty-first century as most of ODS emissions have been successfully phased out by the Montreal Protocol on Substances that Deplete the Ozone Layer, including its Amendments and Adjustments. In this work, we investigated BDC changes through their impact on multidecadal time-series of stratospheric fluorine. To this end, we include ground-based Fourier transform infrared time-series from Jungfraujoch (Switzerland, 46°N) and Lauder (New Zealand, 45°S), Atmospheric Chemistry Experiment – Fourier Transform Spectrometer (ACE-FTS) satellite time-series and five simulations performed by the BASCOE chemical-transport model (CTM). These simulations are driven by the five modern meteorological reanalyses of the atmosphere. Thus, we assess the representation of the investigated BDC changes in state-of-the-art reanalyses which are designed to represent at best the atmospheric state over the past 30 years. We first improved the retrieval strategy of HCFC-22 (CHF2Cl), the most abundant hydrochlorofluorocarbon (HCFC) and the second source of fluorine in the stratosphere, using infrared solar spectra recorded at Jungfraujoch. We showed that HCFC-22 accumulation rates are progressively decreasing in the last decade, highlighting the success of the Montreal Protocol. Furthermore, this first step allowed us to demonstrate the validity of our BASCOE CTM set-up. Indeed, it is the first time that this model is used for such simulations, hence new features were implemented just before and during this thesis project and needed to be validated. The investigations on the impact of BDC changes on the time-series of stratospheric fluorine showed that, for the past twenty years, the BDC has been changing asymmetrically, with the Southern Hemisphere branch getting stronger relative to that of the Northern Hemisphere. Observational datasets and all of the five reanalyses are qualitatively in agreement with this change. However, this important finding is opposed to all model projections, notably used to project ozone recovery, modelling a weakening of the southern branch, in response to increases in greenhouse gases and to decreases in ODSs, calling for further investigations. Superimposed to this 20 year-trend, we have further confirmed a 5-to-7-year variability of the stratosphere, a feature which allows to put into perspective recent studies questioning specific stratospheric variabilities and associated hemispheric asymmetries.
Récupéré en direct depuis OpenAlex et désinversé. Les résumés ne sont pas conservés dans cette base de données : les index inversés représentent 8,6 Go des 9,3 Go de texte de la base, et le serveur dispose de 13 Go libres.
Comment cette classification a été obtenuedéplier
Prédiction distillée sur la base complète
Imitation des enseignantsNi prévalence calibrée, ni vérité terrain. Validation humaine à venir. Apprise à partir de 10 348 étiquettes directes de Codex et de 10 348 étiquettes directes de Gemma. Le mode candidate est l'union des têtes enseignantes seuillées; le consensus est leur intersection. Ces sorties portent le statut machine_predicted_unvalidated et ne sont ni des étiquettes humaines ni des étiquettes directes de modèles de pointe.
Scores Codex et Gemma par catégorie
| Catégorie | Codex | Gemma |
|---|---|---|
| Métarecherche | 0,000 | 0,000 |
| Méta-épidémiologie (sens strict) | 0,000 | 0,000 |
| Méta-épidémiologie (sens large) | 0,000 | 0,000 |
| Bibliométrie | 0,000 | 0,000 |
| Études des sciences et des technologies | 0,000 | 0,000 |
| Communication savante | 0,000 | 0,000 |
| Science ouverte | 0,000 | 0,000 |
| Intégrité de la recherche | 0,000 | 0,000 |
| Charge utile insuffisante (le modèle a refusé de juger) | 0,001 | 0,000 |
Scores machine (provisoires)
Les deux têtes enseignantes du modèle étudiant, lues sur ce travail. Un score ordonne la base pour la relecture; il n'affirme jamais une catégorie, et le statut de validation accompagne chaque rangée tel quel.
Scores de référence d'un modèle non mature (critères de maturité non atteints, 7 itérations). Un score ordonne; il n'affirme jamais une catégorie.
score_only:v0-immature-baseline · tel quel depuis la passe de notation : score_only signifie que le nombre peut ordonner les travaux, et qu'aucune étiquette de catégorie n'en découleClassification
machine, non validéePrédiction automatique; un appel candidat d’une seule tête enseignante, pas un consensus.
Le détail, modèle par modèle et score par score, se trouve en fin de page sous « Comment cette classification a été obtenue ».