Zonally asymmetric influences of the quasi-biennial oscillation on stratospheric ozone

While the zonal mean signals associated with the quasi-biennial oscillation (QBO) in stratospheric ozone have been relatively well documented, the zonal (longitudinal) differences have been less studied. Using satellite-based ozone data, ERA5 reanalysis and model simulations, we demonstrate that the...

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Main Authors: Wang, W., Hong, J., Shangguan, M., Wang, H., Jiang, W., Zhao, S.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020588
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5020588 2023-07-23T04:15:46+02:00 Zonally asymmetric influences of the quasi-biennial oscillation on stratospheric ozone Wang, W. Hong, J. Shangguan, M. Wang, H. Jiang, W. Zhao, S. 2023-07-11 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020588 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-3219 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020588 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-3219 2023-07-02T23:40:07Z While the zonal mean signals associated with the quasi-biennial oscillation (QBO) in stratospheric ozone have been relatively well documented, the zonal (longitudinal) differences have been less studied. Using satellite-based ozone data, ERA5 reanalysis and model simulations, we demonstrate that the influences of QBO on stratospheric ozone and total column ozone (TCO) are seasonally dependent zonally asymmetric. During boreal winter (DJF), positive anomalies of TCO and stratospheric ozone are evident during QBO westerly (QBOW) phases over the regions from North America to the North Atlantic (120˚ W–30˚ E), while significant negative anomalies exist over other longitudes in the Arctic. In boreal autumn (SON), TCO and stratospheric ozone are anomalously high during QBOW from Greenland to Eurasia (60˚ W–120˚ E) but anomalously low in other regions over the Arctic. Weak positive TCO and stratospheric ozone anomalies exist over the South America sector (90˚ W–30˚ E) of the Antarctic, while negative anomalies of TCO and stratospheric ozone are seen in other longitudes. Analysis of meteorological conditions indicates that the QBO ozone perturbations are mainly caused by dynamical transport. QBO affects the geopotential height and the polar vortex and subsequently the transport of ozone-rich air from lower latitudes to the polar region, which therefore influences the ozone concentrations over the polar region. The geopotential height anomalies associated with QBO (QBOW–QBOE) are zonally asymmetric with clear wave number 1 features, which indicates that QBO influences the polar vortex and stratospheric ozone mainly by modifying the wave number 1 activities. Conference Object Antarc* Antarctic Arctic Greenland North Atlantic GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Antarctic Arctic Greenland The Antarctic
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description While the zonal mean signals associated with the quasi-biennial oscillation (QBO) in stratospheric ozone have been relatively well documented, the zonal (longitudinal) differences have been less studied. Using satellite-based ozone data, ERA5 reanalysis and model simulations, we demonstrate that the influences of QBO on stratospheric ozone and total column ozone (TCO) are seasonally dependent zonally asymmetric. During boreal winter (DJF), positive anomalies of TCO and stratospheric ozone are evident during QBO westerly (QBOW) phases over the regions from North America to the North Atlantic (120˚ W–30˚ E), while significant negative anomalies exist over other longitudes in the Arctic. In boreal autumn (SON), TCO and stratospheric ozone are anomalously high during QBOW from Greenland to Eurasia (60˚ W–120˚ E) but anomalously low in other regions over the Arctic. Weak positive TCO and stratospheric ozone anomalies exist over the South America sector (90˚ W–30˚ E) of the Antarctic, while negative anomalies of TCO and stratospheric ozone are seen in other longitudes. Analysis of meteorological conditions indicates that the QBO ozone perturbations are mainly caused by dynamical transport. QBO affects the geopotential height and the polar vortex and subsequently the transport of ozone-rich air from lower latitudes to the polar region, which therefore influences the ozone concentrations over the polar region. The geopotential height anomalies associated with QBO (QBOW–QBOE) are zonally asymmetric with clear wave number 1 features, which indicates that QBO influences the polar vortex and stratospheric ozone mainly by modifying the wave number 1 activities.
format Conference Object
author Wang, W.
Hong, J.
Shangguan, M.
Wang, H.
Jiang, W.
Zhao, S.
spellingShingle Wang, W.
Hong, J.
Shangguan, M.
Wang, H.
Jiang, W.
Zhao, S.
Zonally asymmetric influences of the quasi-biennial oscillation on stratospheric ozone
author_facet Wang, W.
Hong, J.
Shangguan, M.
Wang, H.
Jiang, W.
Zhao, S.
author_sort Wang, W.
title Zonally asymmetric influences of the quasi-biennial oscillation on stratospheric ozone
title_short Zonally asymmetric influences of the quasi-biennial oscillation on stratospheric ozone
title_full Zonally asymmetric influences of the quasi-biennial oscillation on stratospheric ozone
title_fullStr Zonally asymmetric influences of the quasi-biennial oscillation on stratospheric ozone
title_full_unstemmed Zonally asymmetric influences of the quasi-biennial oscillation on stratospheric ozone
title_sort zonally asymmetric influences of the quasi-biennial oscillation on stratospheric ozone
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020588
geographic Antarctic
Arctic
Greenland
The Antarctic
geographic_facet Antarctic
Arctic
Greenland
The Antarctic
genre Antarc*
Antarctic
Arctic
Greenland
North Atlantic
genre_facet Antarc*
Antarctic
Arctic
Greenland
North Atlantic
op_source XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-3219
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020588
op_doi https://doi.org/10.57757/IUGG23-3219
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