Recent decline in extratropical lower stratospheric ozone attributed to circulation changes

1998-2016 ozone trends in the lower stratosphere (LS) are examined using the Modern-Era Retrospective Analysis for Research and Applications Version 2 (MERRA-2) and related NASA products. After removing biases resulting from step-changes in the MERRA-2 ozone observations, a discernible negative tren...

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Détails bibliographiques
Publié dans:Geophysical research letters. - 1984. - 45(2018), 10 vom: 28. Mai, Seite 5166-5176
Auteur principal: Wargan, Krzysztof (Auteur)
Autres auteurs: Orbe, Clara, Pawson, Steven, Ziemke, Jerald R, Oman, Luke D, Olsen, Mark A, Coy, Lawrence, Knowland, K Emma
Format: Article en ligne
Langue:English
Publié: 2018
Accès à la collection:Geophysical research letters
Sujets:Journal Article
Description
Résumé:1998-2016 ozone trends in the lower stratosphere (LS) are examined using the Modern-Era Retrospective Analysis for Research and Applications Version 2 (MERRA-2) and related NASA products. After removing biases resulting from step-changes in the MERRA-2 ozone observations, a discernible negative trend of -1.67±0.54 Dobson units per decade (DU/decade) is found in the 10-km layer above the tropopause between 20°N and 60°N. A weaker but statistically significant trend of -1.17±0.33 DU/decade exists between 50°S and 20°S. In the Tropics, a positive trend is seen in a 5-km layer above the tropopause. Analysis of an idealized tracer in a model simulation constrained by MERRA-2 meteorological fields provides strong evidence that these trends are driven by enhanced isentropic transport between the tropical (20°S-20°N) and extratropical LS in the past two decades. This is the first time that a reanalysis dataset has been used to detect and attribute trends in lower stratospheric ozone
Description:Date Revised 04.10.2023
published: Print-Electronic
Citation Status PubMed-not-MEDLINE
ISSN:0094-8276
DOI:10.1029/2018GL077406