Evidence for the influence of the North Atlantic Oscillation on the total ozone column at northern low latitudes and midlatitudes during winter and summer seasons.

The strong influence of the winter North Atlantic Oscillation (NAO) on the total ozone column (TOC) in the Northern Hemisphere has been reported in a number of previous studies. In this study we show that this influence is not restricted to the winter season but is also significant in summer. Especi...

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Autores: Ossó Castillón, Albert, Sola Salvatierra, Yolanda, Bech, Joan, Lorente, Jeroni
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2011
País:España
Institución:Universidad de Barcelona
Repositorio:Dipòsit Digital de la UB
OAI Identifier:oai:diposit.ub.edu:2445/49257
Acceso en línea:https://hdl.handle.net/2445/49257
Access Level:acceso abierto
Palabra clave:Geofísica
Ozó atmosfèric
Canvi climàtic
Atlàntic, Oceà
Climatologia
Hivern
Estiu
Mediterrània (Regió)
Geophysics
Atmospheric ozone
Climatic change
Atlantic Ocean
Climatology
Winter
Summer
Mediterranean Region
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spelling Evidence for the influence of the North Atlantic Oscillation on the total ozone column at northern low latitudes and midlatitudes during winter and summer seasons.Ossó Castillón, AlbertSola Salvatierra, YolandaBech, JoanLorente, JeroniGeofísicaOzó atmosfèricCanvi climàticAtlàntic, OceàClimatologiaHivernEstiuMediterrània (Regió)GeophysicsAtmospheric ozoneClimatic changeAtlantic OceanClimatologyWinterSummerMediterranean RegionThe strong influence of the winter North Atlantic Oscillation (NAO) on the total ozone column (TOC) in the Northern Hemisphere has been reported in a number of previous studies. In this study we show that this influence is not restricted to the winter season but is also significant in summer. Especially interesting effects of the summer NAO (SNAO) on the TOC are observed over the eastern Mediterranean region, where a strongly positive SNAO index is related to the creation of a geopotential height-negative anomaly over Greece with maximum amplitude at 200 hPa. Another anomaly was observed west of the Iberian Peninsula with similar effects on the TOC. Analyzing 26 years of Total Ozone Mapping Spectrometer (TOMS) and Ozone Monitoring Instrument (OMI) data from the equator to midlatitudes (60°) in the Northern Hemisphere, we demonstrate that the SNAO accounts for up to 30% of the TOC variability with a strong latitudinal and longitudinal dependence. Additionally, we obtain significant correlations between the NAO index and the thermal tropopause pressure and also with the geopotential heights at 200 and 500 hPa. Finally, some indirect connections between NAO and the TOC through teleconnections are also discussed.American Geophysical Union2011info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://hdl.handle.net/2445/49257Articles publicats en revistes (Física Quàntica i Astrofísica)reponame:Dipòsit Digital de la UBinstname:Universidad de BarcelonaInglésReproducció del document publicat a: http://dx.doi.org/10.1029/2011JD016539Journal of Geophysical Research, 2011, vol. 116, num. D24122, p. 1-12http://dx.doi.org/10.1029/2011JD016539(c) American Geophysical Union, 2011info:eu-repo/semantics/openAccessoai:diposit.ub.edu:2445/492572026-05-27T06:46:51Z
dc.title.none.fl_str_mv Evidence for the influence of the North Atlantic Oscillation on the total ozone column at northern low latitudes and midlatitudes during winter and summer seasons.
title Evidence for the influence of the North Atlantic Oscillation on the total ozone column at northern low latitudes and midlatitudes during winter and summer seasons.
spellingShingle Evidence for the influence of the North Atlantic Oscillation on the total ozone column at northern low latitudes and midlatitudes during winter and summer seasons.
Ossó Castillón, Albert
Geofísica
Ozó atmosfèric
Canvi climàtic
Atlàntic, Oceà
Climatologia
Hivern
Estiu
Mediterrània (Regió)
Geophysics
Atmospheric ozone
Climatic change
Atlantic Ocean
Climatology
Winter
Summer
Mediterranean Region
title_short Evidence for the influence of the North Atlantic Oscillation on the total ozone column at northern low latitudes and midlatitudes during winter and summer seasons.
title_full Evidence for the influence of the North Atlantic Oscillation on the total ozone column at northern low latitudes and midlatitudes during winter and summer seasons.
title_fullStr Evidence for the influence of the North Atlantic Oscillation on the total ozone column at northern low latitudes and midlatitudes during winter and summer seasons.
title_full_unstemmed Evidence for the influence of the North Atlantic Oscillation on the total ozone column at northern low latitudes and midlatitudes during winter and summer seasons.
title_sort Evidence for the influence of the North Atlantic Oscillation on the total ozone column at northern low latitudes and midlatitudes during winter and summer seasons.
dc.creator.none.fl_str_mv Ossó Castillón, Albert
Sola Salvatierra, Yolanda
Bech, Joan
Lorente, Jeroni
author Ossó Castillón, Albert
author_facet Ossó Castillón, Albert
Sola Salvatierra, Yolanda
Bech, Joan
Lorente, Jeroni
author_role author
author2 Sola Salvatierra, Yolanda
Bech, Joan
Lorente, Jeroni
author2_role author
author
author
dc.subject.none.fl_str_mv Geofísica
Ozó atmosfèric
Canvi climàtic
Atlàntic, Oceà
Climatologia
Hivern
Estiu
Mediterrània (Regió)
Geophysics
Atmospheric ozone
Climatic change
Atlantic Ocean
Climatology
Winter
Summer
Mediterranean Region
topic Geofísica
Ozó atmosfèric
Canvi climàtic
Atlàntic, Oceà
Climatologia
Hivern
Estiu
Mediterrània (Regió)
Geophysics
Atmospheric ozone
Climatic change
Atlantic Ocean
Climatology
Winter
Summer
Mediterranean Region
description The strong influence of the winter North Atlantic Oscillation (NAO) on the total ozone column (TOC) in the Northern Hemisphere has been reported in a number of previous studies. In this study we show that this influence is not restricted to the winter season but is also significant in summer. Especially interesting effects of the summer NAO (SNAO) on the TOC are observed over the eastern Mediterranean region, where a strongly positive SNAO index is related to the creation of a geopotential height-negative anomaly over Greece with maximum amplitude at 200 hPa. Another anomaly was observed west of the Iberian Peninsula with similar effects on the TOC. Analyzing 26 years of Total Ozone Mapping Spectrometer (TOMS) and Ozone Monitoring Instrument (OMI) data from the equator to midlatitudes (60°) in the Northern Hemisphere, we demonstrate that the SNAO accounts for up to 30% of the TOC variability with a strong latitudinal and longitudinal dependence. Additionally, we obtain significant correlations between the NAO index and the thermal tropopause pressure and also with the geopotential heights at 200 and 500 hPa. Finally, some indirect connections between NAO and the TOC through teleconnections are also discussed.
publishDate 2011
dc.date.none.fl_str_mv 2011
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv https://hdl.handle.net/2445/49257
url https://hdl.handle.net/2445/49257
dc.language.none.fl_str_mv Inglés
language_invalid_str_mv Inglés
dc.relation.none.fl_str_mv Reproducció del document publicat a: http://dx.doi.org/10.1029/2011JD016539
Journal of Geophysical Research, 2011, vol. 116, num. D24122, p. 1-12
http://dx.doi.org/10.1029/2011JD016539
dc.rights.none.fl_str_mv (c) American Geophysical Union, 2011
info:eu-repo/semantics/openAccess
rights_invalid_str_mv (c) American Geophysical Union, 2011
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv American Geophysical Union
publisher.none.fl_str_mv American Geophysical Union
dc.source.none.fl_str_mv Articles publicats en revistes (Física Quàntica i Astrofísica)
reponame:Dipòsit Digital de la UB
instname:Universidad de Barcelona
instname_str Universidad de Barcelona
reponame_str Dipòsit Digital de la UB
collection Dipòsit Digital de la UB
repository.name.fl_str_mv
repository.mail.fl_str_mv
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