Northern Hemisphere Climate Variability: Character, Forcing Mechanisms, and Significance of the North Atlantic/Arctic Oscillation

Abstract The North Atlantic Oscillation (NAO) has long been recognized as an important source of climate variability over the north Atlantic region. The NAO is often referred to as the regional expression of the Arctic Oscillation that reflects a redistribution of atmospheric mass between the Arctic...

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Published in:Geography Compass
Main Author: Budikova, Dagmar
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2012
Subjects:
Online Access:http://dx.doi.org/10.1111/j.1749-8198.2012.00498.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1749-8198.2012.00498.x
http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1749-8198.2012.00498.x/fullpdf
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spelling crwiley:10.1111/j.1749-8198.2012.00498.x 2023-12-03T10:16:36+01:00 Northern Hemisphere Climate Variability: Character, Forcing Mechanisms, and Significance of the North Atlantic/Arctic Oscillation Budikova, Dagmar 2012 http://dx.doi.org/10.1111/j.1749-8198.2012.00498.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1749-8198.2012.00498.x http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1749-8198.2012.00498.x/fullpdf en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Geography Compass volume 6, issue 7, page 401-422 ISSN 1749-8198 1749-8198 Atmospheric Science Computers in Earth Sciences Earth-Surface Processes General Social Sciences Water Science and Technology journal-article 2012 crwiley https://doi.org/10.1111/j.1749-8198.2012.00498.x 2023-11-09T13:39:12Z Abstract The North Atlantic Oscillation (NAO) has long been recognized as an important source of climate variability over the north Atlantic region. The NAO is often referred to as the regional expression of the Arctic Oscillation that reflects a redistribution of atmospheric mass between the Arctic and the middle latitudes of the Northern Hemisphere (NH). This review highlights our current understanding of these prominent teleconnection patterns and discusses outstanding questions and challenges that scientists face as they continue to build our knowledge of climate variability and change across the NH. The work discusses the strengths and limitations of the multitude of methods by which these phenomena have been defined, while highlighting recent changes in their character. Addressed also are the various internal and external forcing mechanisms that shape these phenomena and ultimately help define their predictive nature. Article in Journal/Newspaper Arctic Atlantic Arctic Atlantic-Arctic North Atlantic North Atlantic oscillation Wiley Online Library (via Crossref) Arctic Geography Compass 6 7 401 422
institution Open Polar
collection Wiley Online Library (via Crossref)
op_collection_id crwiley
language English
topic Atmospheric Science
Computers in Earth Sciences
Earth-Surface Processes
General Social Sciences
Water Science and Technology
spellingShingle Atmospheric Science
Computers in Earth Sciences
Earth-Surface Processes
General Social Sciences
Water Science and Technology
Budikova, Dagmar
Northern Hemisphere Climate Variability: Character, Forcing Mechanisms, and Significance of the North Atlantic/Arctic Oscillation
topic_facet Atmospheric Science
Computers in Earth Sciences
Earth-Surface Processes
General Social Sciences
Water Science and Technology
description Abstract The North Atlantic Oscillation (NAO) has long been recognized as an important source of climate variability over the north Atlantic region. The NAO is often referred to as the regional expression of the Arctic Oscillation that reflects a redistribution of atmospheric mass between the Arctic and the middle latitudes of the Northern Hemisphere (NH). This review highlights our current understanding of these prominent teleconnection patterns and discusses outstanding questions and challenges that scientists face as they continue to build our knowledge of climate variability and change across the NH. The work discusses the strengths and limitations of the multitude of methods by which these phenomena have been defined, while highlighting recent changes in their character. Addressed also are the various internal and external forcing mechanisms that shape these phenomena and ultimately help define their predictive nature.
format Article in Journal/Newspaper
author Budikova, Dagmar
author_facet Budikova, Dagmar
author_sort Budikova, Dagmar
title Northern Hemisphere Climate Variability: Character, Forcing Mechanisms, and Significance of the North Atlantic/Arctic Oscillation
title_short Northern Hemisphere Climate Variability: Character, Forcing Mechanisms, and Significance of the North Atlantic/Arctic Oscillation
title_full Northern Hemisphere Climate Variability: Character, Forcing Mechanisms, and Significance of the North Atlantic/Arctic Oscillation
title_fullStr Northern Hemisphere Climate Variability: Character, Forcing Mechanisms, and Significance of the North Atlantic/Arctic Oscillation
title_full_unstemmed Northern Hemisphere Climate Variability: Character, Forcing Mechanisms, and Significance of the North Atlantic/Arctic Oscillation
title_sort northern hemisphere climate variability: character, forcing mechanisms, and significance of the north atlantic/arctic oscillation
publisher Wiley
publishDate 2012
url http://dx.doi.org/10.1111/j.1749-8198.2012.00498.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1749-8198.2012.00498.x
http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1749-8198.2012.00498.x/fullpdf
geographic Arctic
geographic_facet Arctic
genre Arctic
Atlantic Arctic
Atlantic-Arctic
North Atlantic
North Atlantic oscillation
genre_facet Arctic
Atlantic Arctic
Atlantic-Arctic
North Atlantic
North Atlantic oscillation
op_source Geography Compass
volume 6, issue 7, page 401-422
ISSN 1749-8198 1749-8198
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1111/j.1749-8198.2012.00498.x
container_title Geography Compass
container_volume 6
container_issue 7
container_start_page 401
op_container_end_page 422
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