The missing Northern European winter cooling response to Arctic sea ice loss

It is proposed that Arctic sea ice loss may be a cause of colder European winters, by promoting the negative phase of the North Atlantic Oscillation (NAO). Here, the author shows that despite an intensification of negative NAO events, sea ice loss does not lead to cooling, and cold extremes actually...

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Main Author: James A. Screen
Format: Article
Language:English
Published: Nature Publishing Group 2017-03-01
Series:Nature Communications
Online Access:https://doi.org/10.1038/ncomms14603
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spelling doaj-cdad26db52344dd987d1d6024d1668522021-05-11T07:17:34ZengNature Publishing GroupNature Communications2041-17232017-03-01811910.1038/ncomms14603The missing Northern European winter cooling response to Arctic sea ice lossJames A. Screen0College of Engineering, Mathematics and Physical Sciences, University of ExeterIt is proposed that Arctic sea ice loss may be a cause of colder European winters, by promoting the negative phase of the North Atlantic Oscillation (NAO). Here, the author shows that despite an intensification of negative NAO events, sea ice loss does not lead to cooling, and cold extremes actually decrease.https://doi.org/10.1038/ncomms14603
collection DOAJ
language English
format Article
sources DOAJ
author James A. Screen
spellingShingle James A. Screen
The missing Northern European winter cooling response to Arctic sea ice loss
Nature Communications
author_facet James A. Screen
author_sort James A. Screen
title The missing Northern European winter cooling response to Arctic sea ice loss
title_short The missing Northern European winter cooling response to Arctic sea ice loss
title_full The missing Northern European winter cooling response to Arctic sea ice loss
title_fullStr The missing Northern European winter cooling response to Arctic sea ice loss
title_full_unstemmed The missing Northern European winter cooling response to Arctic sea ice loss
title_sort missing northern european winter cooling response to arctic sea ice loss
publisher Nature Publishing Group
series Nature Communications
issn 2041-1723
publishDate 2017-03-01
description It is proposed that Arctic sea ice loss may be a cause of colder European winters, by promoting the negative phase of the North Atlantic Oscillation (NAO). Here, the author shows that despite an intensification of negative NAO events, sea ice loss does not lead to cooling, and cold extremes actually decrease.
url https://doi.org/10.1038/ncomms14603
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AT jamesascreen missingnortherneuropeanwintercoolingresponsetoarcticseaiceloss
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