Ozone signatures of climate patterns over the Euro-Atlantic sector in the

The influence of low-frequency tropospheric dynamics upon column ozone interannual variability is esti-mated in the spring season over the Euro-Atlantic sector. This dynamical variability of tropospheric origin is examined in terms of leading climate patterns, derived from an empirical orthogonal fu...

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Main Authors: Y. J. Orsolini, F. J. Doblas-reyes
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.526.3407
http://fmiarc.fmi.fi/candidoz/docs/QJRMS_Orsolini_Reyes.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.526.3407 2023-05-15T15:08:13+02:00 Ozone signatures of climate patterns over the Euro-Atlantic sector in the Y. J. Orsolini F. J. Doblas-reyes The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.526.3407 http://fmiarc.fmi.fi/candidoz/docs/QJRMS_Orsolini_Reyes.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.526.3407 http://fmiarc.fmi.fi/candidoz/docs/QJRMS_Orsolini_Reyes.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://fmiarc.fmi.fi/candidoz/docs/QJRMS_Orsolini_Reyes.pdf Euro-Atlantic variability Ozone trends Stratosphere text ftciteseerx 2016-01-08T10:22:26Z The influence of low-frequency tropospheric dynamics upon column ozone interannual variability is esti-mated in the spring season over the Euro-Atlantic sector. This dynamical variability of tropospheric origin is examined in terms of leading climate patterns, derived from an empirical orthogonal function analysis of the National Center for Environmental Prediction 500 mb geopotential height analyses. In order to fingerprint the spatial and temporal ozone signatures of these patterns, the Total Ozone Mapping Spectrometer satellite observa-tions of column ozone during the last two decades are used. The geographical ozone signatures of these climate patterns are extracted by linear regression and their time evolution reconstructed. Geopotential anomalies associated with four leading patterns of variability (the North Atlantic Oscillation (NAO), the Scandinavian pattern, the east Atlantic pattern and the European blocking pattern) induce column ozone anomalies in the range of 5–15 Dobson Units per standard deviation of the pattern index. The impact of these combined Euro-Atlantic climate patterns upon the regional ozone trends and interannual variability is also estimated. In order to reconstruct the regional ozone trend and variability, it proved important to incorporate several patterns, in addition to the dominant NAO. A hitherto little-known lifting of the Arctic tropopause by the polar night jet is also shown to imprint upon the ozone signatures of some patterns. Text Arctic North Atlantic North Atlantic oscillation polar night Unknown Arctic
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
topic Euro-Atlantic variability Ozone trends Stratosphere
spellingShingle Euro-Atlantic variability Ozone trends Stratosphere
Y. J. Orsolini
F. J. Doblas-reyes
Ozone signatures of climate patterns over the Euro-Atlantic sector in the
topic_facet Euro-Atlantic variability Ozone trends Stratosphere
description The influence of low-frequency tropospheric dynamics upon column ozone interannual variability is esti-mated in the spring season over the Euro-Atlantic sector. This dynamical variability of tropospheric origin is examined in terms of leading climate patterns, derived from an empirical orthogonal function analysis of the National Center for Environmental Prediction 500 mb geopotential height analyses. In order to fingerprint the spatial and temporal ozone signatures of these patterns, the Total Ozone Mapping Spectrometer satellite observa-tions of column ozone during the last two decades are used. The geographical ozone signatures of these climate patterns are extracted by linear regression and their time evolution reconstructed. Geopotential anomalies associated with four leading patterns of variability (the North Atlantic Oscillation (NAO), the Scandinavian pattern, the east Atlantic pattern and the European blocking pattern) induce column ozone anomalies in the range of 5–15 Dobson Units per standard deviation of the pattern index. The impact of these combined Euro-Atlantic climate patterns upon the regional ozone trends and interannual variability is also estimated. In order to reconstruct the regional ozone trend and variability, it proved important to incorporate several patterns, in addition to the dominant NAO. A hitherto little-known lifting of the Arctic tropopause by the polar night jet is also shown to imprint upon the ozone signatures of some patterns.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Y. J. Orsolini
F. J. Doblas-reyes
author_facet Y. J. Orsolini
F. J. Doblas-reyes
author_sort Y. J. Orsolini
title Ozone signatures of climate patterns over the Euro-Atlantic sector in the
title_short Ozone signatures of climate patterns over the Euro-Atlantic sector in the
title_full Ozone signatures of climate patterns over the Euro-Atlantic sector in the
title_fullStr Ozone signatures of climate patterns over the Euro-Atlantic sector in the
title_full_unstemmed Ozone signatures of climate patterns over the Euro-Atlantic sector in the
title_sort ozone signatures of climate patterns over the euro-atlantic sector in the
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.526.3407
http://fmiarc.fmi.fi/candidoz/docs/QJRMS_Orsolini_Reyes.pdf
geographic Arctic
geographic_facet Arctic
genre Arctic
North Atlantic
North Atlantic oscillation
polar night
genre_facet Arctic
North Atlantic
North Atlantic oscillation
polar night
op_source http://fmiarc.fmi.fi/candidoz/docs/QJRMS_Orsolini_Reyes.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.526.3407
http://fmiarc.fmi.fi/candidoz/docs/QJRMS_Orsolini_Reyes.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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