Abrupt cooling over the North Atlantic in modern climate models
Concerns on climate change include the risk of abrupt cooling in the North Atlantic. Here, the authors analyse CMIP5 projections and show that a convection collapse in the subpolar gyre can cool this region by up to 3°C in 10 years, which is as likely to occur by 2100 as a continuous warming.
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ftdoajarticles:oai:doaj.org/article:b1dc2057869c42498fcea48f9df6056c 2023-05-15T17:26:31+02:00 Abrupt cooling over the North Atlantic in modern climate models Giovanni Sgubin Didier Swingedouw Sybren Drijfhout Yannick Mary Amine Bennabi 2017-02-01T00:00:00Z https://doi.org/10.1038/ncomms14375 https://doaj.org/article/b1dc2057869c42498fcea48f9df6056c EN eng Nature Portfolio https://doi.org/10.1038/ncomms14375 https://doaj.org/toc/2041-1723 doi:10.1038/ncomms14375 2041-1723 https://doaj.org/article/b1dc2057869c42498fcea48f9df6056c Nature Communications, Vol 8, Iss 1, Pp 1-12 (2017) Science Q article 2017 ftdoajarticles https://doi.org/10.1038/ncomms14375 2022-12-31T09:31:50Z Concerns on climate change include the risk of abrupt cooling in the North Atlantic. Here, the authors analyse CMIP5 projections and show that a convection collapse in the subpolar gyre can cool this region by up to 3°C in 10 years, which is as likely to occur by 2100 as a continuous warming. Article in Journal/Newspaper North Atlantic Directory of Open Access Journals: DOAJ Articles Nature Communications 8 1 |
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Open Polar |
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Directory of Open Access Journals: DOAJ Articles |
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ftdoajarticles |
language |
English |
topic |
Science Q |
spellingShingle |
Science Q Giovanni Sgubin Didier Swingedouw Sybren Drijfhout Yannick Mary Amine Bennabi Abrupt cooling over the North Atlantic in modern climate models |
topic_facet |
Science Q |
description |
Concerns on climate change include the risk of abrupt cooling in the North Atlantic. Here, the authors analyse CMIP5 projections and show that a convection collapse in the subpolar gyre can cool this region by up to 3°C in 10 years, which is as likely to occur by 2100 as a continuous warming. |
format |
Article in Journal/Newspaper |
author |
Giovanni Sgubin Didier Swingedouw Sybren Drijfhout Yannick Mary Amine Bennabi |
author_facet |
Giovanni Sgubin Didier Swingedouw Sybren Drijfhout Yannick Mary Amine Bennabi |
author_sort |
Giovanni Sgubin |
title |
Abrupt cooling over the North Atlantic in modern climate models |
title_short |
Abrupt cooling over the North Atlantic in modern climate models |
title_full |
Abrupt cooling over the North Atlantic in modern climate models |
title_fullStr |
Abrupt cooling over the North Atlantic in modern climate models |
title_full_unstemmed |
Abrupt cooling over the North Atlantic in modern climate models |
title_sort |
abrupt cooling over the north atlantic in modern climate models |
publisher |
Nature Portfolio |
publishDate |
2017 |
url |
https://doi.org/10.1038/ncomms14375 https://doaj.org/article/b1dc2057869c42498fcea48f9df6056c |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Nature Communications, Vol 8, Iss 1, Pp 1-12 (2017) |
op_relation |
https://doi.org/10.1038/ncomms14375 https://doaj.org/toc/2041-1723 doi:10.1038/ncomms14375 2041-1723 https://doaj.org/article/b1dc2057869c42498fcea48f9df6056c |
op_doi |
https://doi.org/10.1038/ncomms14375 |
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Nature Communications |
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8 |
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1766118209398767616 |