Analysis and regionalization of northern european winter precipitation based on its relationship with the North Atlantic oscillation

The relationship between the North Atlantic oscillation (NAO) and winter temperature and precipitation over northern Europe has long been known. However, its strength is variable within this region. In this paper, an analysis of the regional variability of the influence of the NAO on winter precipit...

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Published in:International Journal of Climatology
Main Author: Bertacchi Uvo, Cintia
Format: Article in Journal/Newspaper
Language:English
Published: John Wiley & Sons Inc. 2003
Subjects:
NAO
Online Access:https://lup.lub.lu.se/record/304326
https://doi.org/10.1002/joc.930
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spelling ftulundlup:oai:lup.lub.lu.se:76c03757-b6da-44f1-8c0a-ef8838ebd1f2 2023-05-15T17:28:21+02:00 Analysis and regionalization of northern european winter precipitation based on its relationship with the North Atlantic oscillation Bertacchi Uvo, Cintia 2003 https://lup.lub.lu.se/record/304326 https://doi.org/10.1002/joc.930 eng eng John Wiley & Sons Inc. https://lup.lub.lu.se/record/304326 http://dx.doi.org/10.1002/joc.930 wos:000184607600003 scopus:0042425021 International Journal of Climatology; 23(10), pp 1185-1194 (2003) ISSN: 1097-0088 Water Engineering northern North Atlantic oscillation European precipitation NAO winter precipitation regionalization precipitation Europe contributiontojournal/article info:eu-repo/semantics/article text 2003 ftulundlup https://doi.org/10.1002/joc.930 2023-02-01T23:32:27Z The relationship between the North Atlantic oscillation (NAO) and winter temperature and precipitation over northern Europe has long been known. However, its strength is variable within this region. In this paper, an analysis of the regional variability of the influence of the NAO on winter precipitation in northern Europe is developed using empirical orthogonal function analysis, cluster analysis and simple correlation. Results show that precipitation in most of the region studied is affected by the NAO, although with varying intensity. The NAO strongly influences winter precipitation along the Norwegian coast, in northern Sweden and in southern Finland. It is evident that the region on the lee side of the Scandes (the mountain chain between Norway and Sweden) is protected from the effects of the moist western winds from the Atlantic that, in turn, are strongly related to the NAO. As a result, precipitation in this shielded area is mainly related to southeasterly winds. Copyright (C) 2003 Royal Meteorological Society. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Northern Sweden Lund University Publications (LUP) Norway International Journal of Climatology 23 10 1185 1194
institution Open Polar
collection Lund University Publications (LUP)
op_collection_id ftulundlup
language English
topic Water Engineering
northern
North Atlantic oscillation
European precipitation
NAO
winter precipitation
regionalization
precipitation
Europe
spellingShingle Water Engineering
northern
North Atlantic oscillation
European precipitation
NAO
winter precipitation
regionalization
precipitation
Europe
Bertacchi Uvo, Cintia
Analysis and regionalization of northern european winter precipitation based on its relationship with the North Atlantic oscillation
topic_facet Water Engineering
northern
North Atlantic oscillation
European precipitation
NAO
winter precipitation
regionalization
precipitation
Europe
description The relationship between the North Atlantic oscillation (NAO) and winter temperature and precipitation over northern Europe has long been known. However, its strength is variable within this region. In this paper, an analysis of the regional variability of the influence of the NAO on winter precipitation in northern Europe is developed using empirical orthogonal function analysis, cluster analysis and simple correlation. Results show that precipitation in most of the region studied is affected by the NAO, although with varying intensity. The NAO strongly influences winter precipitation along the Norwegian coast, in northern Sweden and in southern Finland. It is evident that the region on the lee side of the Scandes (the mountain chain between Norway and Sweden) is protected from the effects of the moist western winds from the Atlantic that, in turn, are strongly related to the NAO. As a result, precipitation in this shielded area is mainly related to southeasterly winds. Copyright (C) 2003 Royal Meteorological Society.
format Article in Journal/Newspaper
author Bertacchi Uvo, Cintia
author_facet Bertacchi Uvo, Cintia
author_sort Bertacchi Uvo, Cintia
title Analysis and regionalization of northern european winter precipitation based on its relationship with the North Atlantic oscillation
title_short Analysis and regionalization of northern european winter precipitation based on its relationship with the North Atlantic oscillation
title_full Analysis and regionalization of northern european winter precipitation based on its relationship with the North Atlantic oscillation
title_fullStr Analysis and regionalization of northern european winter precipitation based on its relationship with the North Atlantic oscillation
title_full_unstemmed Analysis and regionalization of northern european winter precipitation based on its relationship with the North Atlantic oscillation
title_sort analysis and regionalization of northern european winter precipitation based on its relationship with the north atlantic oscillation
publisher John Wiley & Sons Inc.
publishDate 2003
url https://lup.lub.lu.se/record/304326
https://doi.org/10.1002/joc.930
geographic Norway
geographic_facet Norway
genre North Atlantic
North Atlantic oscillation
Northern Sweden
genre_facet North Atlantic
North Atlantic oscillation
Northern Sweden
op_source International Journal of Climatology; 23(10), pp 1185-1194 (2003)
ISSN: 1097-0088
op_relation https://lup.lub.lu.se/record/304326
http://dx.doi.org/10.1002/joc.930
wos:000184607600003
scopus:0042425021
op_doi https://doi.org/10.1002/joc.930
container_title International Journal of Climatology
container_volume 23
container_issue 10
container_start_page 1185
op_container_end_page 1194
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