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...
| Autores: | , , , |
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| 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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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 |
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openAccess |
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application/pdf |
| dc.publisher.none.fl_str_mv |
American Geophysical Union |
| publisher.none.fl_str_mv |
American Geophysical Union |
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Articles publicats en revistes (Física Quàntica i Astrofísica) reponame:Dipòsit Digital de la UB instname:Universidad de Barcelona |
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Universidad de Barcelona |
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Dipòsit Digital de la UB |
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Dipòsit Digital de la UB |
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15.300719 |