Is the NAO winter index a reliable proxy for wind climate and storminess in northwest Europe?

Climate measures synthesized from the instrumental wind record at 53 stations in northwest Europe are compared with various derivations of the North Atlantic Oscillation (NAO) winter index. The NAO is highly correlated with wind direction frequency, with positive phases in the NAO winter index assoc...

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Bibliographic Details
Main Authors: Burningham, H, French, J
Format: Article in Journal/Newspaper
Language:unknown
Published: 2013
Subjects:
Online Access:http://discovery.ucl.ac.uk/1399199/
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spelling ftucl:oai:eprints.ucl.ac.uk.OAI2:1399199 2023-05-15T17:32:15+02:00 Is the NAO winter index a reliable proxy for wind climate and storminess in northwest Europe? Burningham, H French, J 2013-06-30 http://discovery.ucl.ac.uk/1399199/ unknown International Journal of Climatology , 33 (8) 2036 - 2049. (2013) Article 2013 ftucl 2015-02-12T23:24:20Z Climate measures synthesized from the instrumental wind record at 53 stations in northwest Europe are compared with various derivations of the North Atlantic Oscillation (NAO) winter index. The NAO is highly correlated with wind direction frequency, with positive phases in the NAO winter index associated with increased frequency of winds from the southwest. These correlations are sensitive to the choice of winter period and diminish with longer period, especially the inclusion of October. Evidence for connections between the NAO and wind speed or storminess measures is far less convincing, particularly in terms of the frequency of extreme wind speed events. These results have important implications for the use the NAO winter index as a proxy for storminess, whether in palaeoenvironmental reconstructions or as a basis for storm forecasting. © 2012 Royal Meteorological Society. Article in Journal/Newspaper North Atlantic North Atlantic oscillation University College London: UCL Discovery
institution Open Polar
collection University College London: UCL Discovery
op_collection_id ftucl
language unknown
description Climate measures synthesized from the instrumental wind record at 53 stations in northwest Europe are compared with various derivations of the North Atlantic Oscillation (NAO) winter index. The NAO is highly correlated with wind direction frequency, with positive phases in the NAO winter index associated with increased frequency of winds from the southwest. These correlations are sensitive to the choice of winter period and diminish with longer period, especially the inclusion of October. Evidence for connections between the NAO and wind speed or storminess measures is far less convincing, particularly in terms of the frequency of extreme wind speed events. These results have important implications for the use the NAO winter index as a proxy for storminess, whether in palaeoenvironmental reconstructions or as a basis for storm forecasting. © 2012 Royal Meteorological Society.
format Article in Journal/Newspaper
author Burningham, H
French, J
spellingShingle Burningham, H
French, J
Is the NAO winter index a reliable proxy for wind climate and storminess in northwest Europe?
author_facet Burningham, H
French, J
author_sort Burningham, H
title Is the NAO winter index a reliable proxy for wind climate and storminess in northwest Europe?
title_short Is the NAO winter index a reliable proxy for wind climate and storminess in northwest Europe?
title_full Is the NAO winter index a reliable proxy for wind climate and storminess in northwest Europe?
title_fullStr Is the NAO winter index a reliable proxy for wind climate and storminess in northwest Europe?
title_full_unstemmed Is the NAO winter index a reliable proxy for wind climate and storminess in northwest Europe?
title_sort is the nao winter index a reliable proxy for wind climate and storminess in northwest europe?
publishDate 2013
url http://discovery.ucl.ac.uk/1399199/
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source International Journal of Climatology , 33 (8) 2036 - 2049. (2013)
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