Changes in Winter Temperature Extremes From Future Arctic Sea‐Ice Loss and Ocean Warming

Abstract Observed rapid Arctic warming and sea‐ice loss are likely to continue in the future, unless and after greenhouse gas emissions are reduced to net‐zero. Here, we examine the possible effects of future sea‐ice loss at 2°C global warming above pre‐industrial levels on winter temperature extrem...

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Published in:Geophysical Research Letters
Main Authors: Y. T. Eunice Lo, Dann M. Mitchell, Peter A. G. Watson, James A. Screen
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:https://doi.org/10.1029/2022GL102542
https://doaj.org/article/6c77d5584a3e42fe9c7240f74e71aef4
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spelling ftdoajarticles:oai:doaj.org/article:6c77d5584a3e42fe9c7240f74e71aef4 2024-09-15T18:08:05+00:00 Changes in Winter Temperature Extremes From Future Arctic Sea‐Ice Loss and Ocean Warming Y. T. Eunice Lo Dann M. Mitchell Peter A. G. Watson James A. Screen 2023-02-01T00:00:00Z https://doi.org/10.1029/2022GL102542 https://doaj.org/article/6c77d5584a3e42fe9c7240f74e71aef4 EN eng Wiley https://doi.org/10.1029/2022GL102542 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2022GL102542 https://doaj.org/article/6c77d5584a3e42fe9c7240f74e71aef4 Geophysical Research Letters, Vol 50, Iss 3, Pp n/a-n/a (2023) Geophysics. Cosmic physics QC801-809 article 2023 ftdoajarticles https://doi.org/10.1029/2022GL102542 2024-08-05T17:49:23Z Abstract Observed rapid Arctic warming and sea‐ice loss are likely to continue in the future, unless and after greenhouse gas emissions are reduced to net‐zero. Here, we examine the possible effects of future sea‐ice loss at 2°C global warming above pre‐industrial levels on winter temperature extremes across the Northern Hemisphere, using coordinated experiments from the Polar Amplification Model Intercomparison Project. 1‐in‐20‐year cold extremes are simulated to become less severe at high‐ and mid‐latitudes in response to Arctic sea‐ice loss. 1‐in‐20‐year winter warm extremes become warmer at northern high latitudes due to sea‐ice loss, but warm by less than cold extremes. We compare the response to sea‐ice loss to that from global sea surface temperature (SST) change also at 2°C global warming. SST change causes less severe cold extremes and more severe warm extremes globally. Except northern high latitudes, the response to SST change is of larger magnitude than that to Arctic sea‐ice loss. Article in Journal/Newspaper Global warming Sea ice Directory of Open Access Journals: DOAJ Articles Geophysical Research Letters 50 3
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Geophysics. Cosmic physics
QC801-809
spellingShingle Geophysics. Cosmic physics
QC801-809
Y. T. Eunice Lo
Dann M. Mitchell
Peter A. G. Watson
James A. Screen
Changes in Winter Temperature Extremes From Future Arctic Sea‐Ice Loss and Ocean Warming
topic_facet Geophysics. Cosmic physics
QC801-809
description Abstract Observed rapid Arctic warming and sea‐ice loss are likely to continue in the future, unless and after greenhouse gas emissions are reduced to net‐zero. Here, we examine the possible effects of future sea‐ice loss at 2°C global warming above pre‐industrial levels on winter temperature extremes across the Northern Hemisphere, using coordinated experiments from the Polar Amplification Model Intercomparison Project. 1‐in‐20‐year cold extremes are simulated to become less severe at high‐ and mid‐latitudes in response to Arctic sea‐ice loss. 1‐in‐20‐year winter warm extremes become warmer at northern high latitudes due to sea‐ice loss, but warm by less than cold extremes. We compare the response to sea‐ice loss to that from global sea surface temperature (SST) change also at 2°C global warming. SST change causes less severe cold extremes and more severe warm extremes globally. Except northern high latitudes, the response to SST change is of larger magnitude than that to Arctic sea‐ice loss.
format Article in Journal/Newspaper
author Y. T. Eunice Lo
Dann M. Mitchell
Peter A. G. Watson
James A. Screen
author_facet Y. T. Eunice Lo
Dann M. Mitchell
Peter A. G. Watson
James A. Screen
author_sort Y. T. Eunice Lo
title Changes in Winter Temperature Extremes From Future Arctic Sea‐Ice Loss and Ocean Warming
title_short Changes in Winter Temperature Extremes From Future Arctic Sea‐Ice Loss and Ocean Warming
title_full Changes in Winter Temperature Extremes From Future Arctic Sea‐Ice Loss and Ocean Warming
title_fullStr Changes in Winter Temperature Extremes From Future Arctic Sea‐Ice Loss and Ocean Warming
title_full_unstemmed Changes in Winter Temperature Extremes From Future Arctic Sea‐Ice Loss and Ocean Warming
title_sort changes in winter temperature extremes from future arctic sea‐ice loss and ocean warming
publisher Wiley
publishDate 2023
url https://doi.org/10.1029/2022GL102542
https://doaj.org/article/6c77d5584a3e42fe9c7240f74e71aef4
genre Global warming
Sea ice
genre_facet Global warming
Sea ice
op_source Geophysical Research Letters, Vol 50, Iss 3, Pp n/a-n/a (2023)
op_relation https://doi.org/10.1029/2022GL102542
https://doaj.org/toc/0094-8276
https://doaj.org/toc/1944-8007
1944-8007
0094-8276
doi:10.1029/2022GL102542
https://doaj.org/article/6c77d5584a3e42fe9c7240f74e71aef4
op_doi https://doi.org/10.1029/2022GL102542
container_title Geophysical Research Letters
container_volume 50
container_issue 3
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