Past and recent changes in the North Atlantic oscillation

The North Atlantic oscillation (NAO) is under current climate conditions the leading mode of atmospheric circulation variability over the North Atlantic region. While the pattern is present during the entire year, it is most important during winter, explaining a large part of the variability of the...

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Published in:Wiley Interdisciplinary Reviews: Climate Change
Main Authors: Pinto, Joaquim G., Raible, Christoph C.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2012
Subjects:
Online Access:https://centaur.reading.ac.uk/32749/
https://centaur.reading.ac.uk/32749/1/150_ftp.pdf
https://doi.org/10.1002/wcc.150
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spelling ftunivreading:oai:centaur.reading.ac.uk:32749 2024-06-23T07:54:55+00:00 Past and recent changes in the North Atlantic oscillation Pinto, Joaquim G. Raible, Christoph C. 2012 text https://centaur.reading.ac.uk/32749/ https://centaur.reading.ac.uk/32749/1/150_ftp.pdf https://doi.org/10.1002/wcc.150 en eng Wiley https://centaur.reading.ac.uk/32749/1/150_ftp.pdf Pinto, J. G. <https://centaur.reading.ac.uk/view/creators/90005193.html> and Raible, C. C. (2012) Past and recent changes in the North Atlantic oscillation. Wiley Interdisciplinary Reviews: Climate Change, 3 (1). pp. 79-90. ISSN 1757-7799 doi: https://doi.org/10.1002/wcc.150 <https://doi.org/10.1002/wcc.150> Article PeerReviewed 2012 ftunivreading https://doi.org/10.1002/wcc.150 2024-06-11T14:59:15Z The North Atlantic oscillation (NAO) is under current climate conditions the leading mode of atmospheric circulation variability over the North Atlantic region. While the pattern is present during the entire year, it is most important during winter, explaining a large part of the variability of the large-scale pressure field, being thus largely determinant for the weather conditions over the North Atlantic basin and over Western Europe. In this study, a review of recent literature on the basic understanding of the NAO, its variability on different time scales and driving physical mechanisms is presented. In particular, the observed NAO variations and long-term trends are put into a long term perspective by considering paleo-proxy evidence. A representative number of recently released NAO reconstructions are discussed. While the reconstructions agree reasonably well with observations during the instrumental overlapping period, there is a rather high uncertainty between the different reconstructions for the pre-instrumental period, which leads to partially incoherent results, that is, periods where the NAO reconstructions do not agree even in sign. Finally, we highlight the future need of a broader definition of the NAO, the assessment of the stability of the teleconnection centers over time, the analysis of the relations to other relevant variables like temperature and precipitation, as well as on the relevant processes involved Article in Journal/Newspaper North Atlantic North Atlantic oscillation CentAUR: Central Archive at the University of Reading Wiley Interdisciplinary Reviews: Climate Change 3 1 79 90
institution Open Polar
collection CentAUR: Central Archive at the University of Reading
op_collection_id ftunivreading
language English
description The North Atlantic oscillation (NAO) is under current climate conditions the leading mode of atmospheric circulation variability over the North Atlantic region. While the pattern is present during the entire year, it is most important during winter, explaining a large part of the variability of the large-scale pressure field, being thus largely determinant for the weather conditions over the North Atlantic basin and over Western Europe. In this study, a review of recent literature on the basic understanding of the NAO, its variability on different time scales and driving physical mechanisms is presented. In particular, the observed NAO variations and long-term trends are put into a long term perspective by considering paleo-proxy evidence. A representative number of recently released NAO reconstructions are discussed. While the reconstructions agree reasonably well with observations during the instrumental overlapping period, there is a rather high uncertainty between the different reconstructions for the pre-instrumental period, which leads to partially incoherent results, that is, periods where the NAO reconstructions do not agree even in sign. Finally, we highlight the future need of a broader definition of the NAO, the assessment of the stability of the teleconnection centers over time, the analysis of the relations to other relevant variables like temperature and precipitation, as well as on the relevant processes involved
format Article in Journal/Newspaper
author Pinto, Joaquim G.
Raible, Christoph C.
spellingShingle Pinto, Joaquim G.
Raible, Christoph C.
Past and recent changes in the North Atlantic oscillation
author_facet Pinto, Joaquim G.
Raible, Christoph C.
author_sort Pinto, Joaquim G.
title Past and recent changes in the North Atlantic oscillation
title_short Past and recent changes in the North Atlantic oscillation
title_full Past and recent changes in the North Atlantic oscillation
title_fullStr Past and recent changes in the North Atlantic oscillation
title_full_unstemmed Past and recent changes in the North Atlantic oscillation
title_sort past and recent changes in the north atlantic oscillation
publisher Wiley
publishDate 2012
url https://centaur.reading.ac.uk/32749/
https://centaur.reading.ac.uk/32749/1/150_ftp.pdf
https://doi.org/10.1002/wcc.150
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation https://centaur.reading.ac.uk/32749/1/150_ftp.pdf
Pinto, J. G. <https://centaur.reading.ac.uk/view/creators/90005193.html> and Raible, C. C. (2012) Past and recent changes in the North Atlantic oscillation. Wiley Interdisciplinary Reviews: Climate Change, 3 (1). pp. 79-90. ISSN 1757-7799 doi: https://doi.org/10.1002/wcc.150 <https://doi.org/10.1002/wcc.150>
op_doi https://doi.org/10.1002/wcc.150
container_title Wiley Interdisciplinary Reviews: Climate Change
container_volume 3
container_issue 1
container_start_page 79
op_container_end_page 90
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