Future abrupt reductions in the summer Arctic sea ice

We examine the trajectory of Arctic summer sea ice in seven projections from the Community Climate System Model and find that abrupt reductions are a common feature of these 21st century simulations. These events have decreasing September ice extent trends that are typically 4 times larger than comp...

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Published in:Geophysical Research Letters
Other Authors: Holland, Marika (author), Bitz, Cecelia (author), Tremblay, Bruno (author)
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2006
Subjects:
Online Access:http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-004-535
https://doi.org/10.1029/2006GL028024
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spelling ftncar:oai:drupal-site.org:articles_7050 2023-10-01T03:49:53+02:00 Future abrupt reductions in the summer Arctic sea ice Holland, Marika (author) Bitz, Cecelia (author) Tremblay, Bruno (author) 2006-12-12 application/pdf http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-004-535 https://doi.org/10.1029/2006GL028024 en eng American Geophysical Union Geophysical Research Letters http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-004-535 doi:10.1029/2006GL028024 ark:/85065/d7gh9j7t Copyright 2006 American Geophysical Union. Arctic sea ice Global climate models Cryospheric change Text article 2006 ftncar https://doi.org/10.1029/2006GL028024 2023-09-04T18:22:10Z We examine the trajectory of Arctic summer sea ice in seven projections from the Community Climate System Model and find that abrupt reductions are a common feature of these 21st century simulations. These events have decreasing September ice extent trends that are typically 4 times larger than comparable observed trends. One event exhibits a decrease from 6 million km² to 2 million km² in a decade, reaching near ice-free September conditions by 2040. In the simulations, ice retreat accelerates as thinning increases the open water formation efficiency for a given melt rate and the ice-albedo feedback increases shortwave absorption. The retreat is abrupt when ocean heat transport to the Arctic is rapidly increasing. Analysis from multiple climate models and three forcing scenarios indicates that abrupt reductions occur in simulations from over 50% of the models and suggests that reductions in future greenhouse gas emissions moderate the likelihood of these events. Article in Journal/Newspaper albedo Arctic Sea ice OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) Arctic Geophysical Research Letters 33 23
institution Open Polar
collection OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research)
op_collection_id ftncar
language English
topic Arctic sea ice
Global climate models
Cryospheric change
spellingShingle Arctic sea ice
Global climate models
Cryospheric change
Future abrupt reductions in the summer Arctic sea ice
topic_facet Arctic sea ice
Global climate models
Cryospheric change
description We examine the trajectory of Arctic summer sea ice in seven projections from the Community Climate System Model and find that abrupt reductions are a common feature of these 21st century simulations. These events have decreasing September ice extent trends that are typically 4 times larger than comparable observed trends. One event exhibits a decrease from 6 million km² to 2 million km² in a decade, reaching near ice-free September conditions by 2040. In the simulations, ice retreat accelerates as thinning increases the open water formation efficiency for a given melt rate and the ice-albedo feedback increases shortwave absorption. The retreat is abrupt when ocean heat transport to the Arctic is rapidly increasing. Analysis from multiple climate models and three forcing scenarios indicates that abrupt reductions occur in simulations from over 50% of the models and suggests that reductions in future greenhouse gas emissions moderate the likelihood of these events.
author2 Holland, Marika (author)
Bitz, Cecelia (author)
Tremblay, Bruno (author)
format Article in Journal/Newspaper
title Future abrupt reductions in the summer Arctic sea ice
title_short Future abrupt reductions in the summer Arctic sea ice
title_full Future abrupt reductions in the summer Arctic sea ice
title_fullStr Future abrupt reductions in the summer Arctic sea ice
title_full_unstemmed Future abrupt reductions in the summer Arctic sea ice
title_sort future abrupt reductions in the summer arctic sea ice
publisher American Geophysical Union
publishDate 2006
url http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-004-535
https://doi.org/10.1029/2006GL028024
geographic Arctic
geographic_facet Arctic
genre albedo
Arctic
Sea ice
genre_facet albedo
Arctic
Sea ice
op_relation Geophysical Research Letters
http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-004-535
doi:10.1029/2006GL028024
ark:/85065/d7gh9j7t
op_rights Copyright 2006 American Geophysical Union.
op_doi https://doi.org/10.1029/2006GL028024
container_title Geophysical Research Letters
container_volume 33
container_issue 23
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