The North Atlantic Oscillation signal in a regional climate simulation for the European region

The North Atlantic Oscillation (NAO) is a dominant pattern of large-scale variability in the Northern Hemisphere, with important regional effects on the winter climate of Europe. Nested regional climate models (RCMs) can be useful tools for studying the regional signal of the NAO. Therefore, it is i...

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Published in:Tellus A
Main Authors: Filippo Giorgi, Roxana Bojariu
Format: Article in Journal/Newspaper
Language:English
Published: 2005
Subjects:
Online Access:https://www.openaccessrepository.it/record/104259
https://doi.org/10.1111/j.1600-0870.2005.00122.x
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spelling ftopenaccessrep:oai:zenodo.org:104259 2023-10-25T01:41:14+02:00 The North Atlantic Oscillation signal in a regional climate simulation for the European region Filippo Giorgi Roxana Bojariu 2005-01-01 https://www.openaccessrepository.it/record/104259 https://doi.org/10.1111/j.1600-0870.2005.00122.x eng eng url:https://www.openaccessrepository.it/communities/itmirror https://www.openaccessrepository.it/record/104259 doi:10.1111/j.1600-0870.2005.00122.x info:eu-repo/semantics/openAccess Atmospheric Science Oceanography info:eu-repo/semantics/article publication-article 2005 ftopenaccessrep https://doi.org/10.1111/j.1600-0870.2005.00122.x 2023-09-26T22:22:02Z The North Atlantic Oscillation (NAO) is a dominant pattern of large-scale variability in the Northern Hemisphere, with important regional effects on the winter climate of Europe. Nested regional climate models (RCMs) can be useful tools for studying the regional signal of the NAO. Therefore, it is important to assess whether they can reproduce the observed NAO signal over Europe when driven by lateral boundary conditions from global climate models. In this paper we investigate the NAO-related winter variability over Europe in a RCM simulation driven by large-scale fields from an atmospheric global model simulation forced with historic sea surface temperature and sea ice distribution for the period 1961–1990. We show that (1) the NAO-related winter variability signal over the European region shows substantial topographically induced fine-scale features, both for temperature and precipitation, and (2) the model is capable of reproducing many aspects of this fine-scale regional signal and, in particular, the topographically forced regional response of precipitation to NAO-type circulations. We conclude that nested regional climate models can be used to study the fine-scale regional signature of the NAO under different climatic conditions. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Sea ice Istituto Nazionale di Fisica Nucleare (INFN): Open Access Repository Tellus A 57 4 641 653
institution Open Polar
collection Istituto Nazionale di Fisica Nucleare (INFN): Open Access Repository
op_collection_id ftopenaccessrep
language English
topic Atmospheric Science
Oceanography
spellingShingle Atmospheric Science
Oceanography
Filippo Giorgi
Roxana Bojariu
The North Atlantic Oscillation signal in a regional climate simulation for the European region
topic_facet Atmospheric Science
Oceanography
description The North Atlantic Oscillation (NAO) is a dominant pattern of large-scale variability in the Northern Hemisphere, with important regional effects on the winter climate of Europe. Nested regional climate models (RCMs) can be useful tools for studying the regional signal of the NAO. Therefore, it is important to assess whether they can reproduce the observed NAO signal over Europe when driven by lateral boundary conditions from global climate models. In this paper we investigate the NAO-related winter variability over Europe in a RCM simulation driven by large-scale fields from an atmospheric global model simulation forced with historic sea surface temperature and sea ice distribution for the period 1961–1990. We show that (1) the NAO-related winter variability signal over the European region shows substantial topographically induced fine-scale features, both for temperature and precipitation, and (2) the model is capable of reproducing many aspects of this fine-scale regional signal and, in particular, the topographically forced regional response of precipitation to NAO-type circulations. We conclude that nested regional climate models can be used to study the fine-scale regional signature of the NAO under different climatic conditions.
format Article in Journal/Newspaper
author Filippo Giorgi
Roxana Bojariu
author_facet Filippo Giorgi
Roxana Bojariu
author_sort Filippo Giorgi
title The North Atlantic Oscillation signal in a regional climate simulation for the European region
title_short The North Atlantic Oscillation signal in a regional climate simulation for the European region
title_full The North Atlantic Oscillation signal in a regional climate simulation for the European region
title_fullStr The North Atlantic Oscillation signal in a regional climate simulation for the European region
title_full_unstemmed The North Atlantic Oscillation signal in a regional climate simulation for the European region
title_sort north atlantic oscillation signal in a regional climate simulation for the european region
publishDate 2005
url https://www.openaccessrepository.it/record/104259
https://doi.org/10.1111/j.1600-0870.2005.00122.x
genre North Atlantic
North Atlantic oscillation
Sea ice
genre_facet North Atlantic
North Atlantic oscillation
Sea ice
op_relation url:https://www.openaccessrepository.it/communities/itmirror
https://www.openaccessrepository.it/record/104259
doi:10.1111/j.1600-0870.2005.00122.x
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1111/j.1600-0870.2005.00122.x
container_title Tellus A
container_volume 57
container_issue 4
container_start_page 641
op_container_end_page 653
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