Changes in Arctic clouds during intervals of rapid sea ice loss

We investigate the behavior of clouds during rapid sea ice loss events (RILEs) in the Arctic, as simulated by multiple ensemble projections of the 21st century in the Community Climate System Model (CCSM3). Trends in cloud properties and sea ice coverage during RILEs are compared with their secular...

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Published in:Climate Dynamics
Other Authors: Vavrus, Steve (author), Holland, Marika (author), Bailey, David (author)
Format: Article in Journal/Newspaper
Language:English
Published: Springer 2011
Subjects:
Online Access:http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-000-133
https://doi.org/10.1007/s00382-010-0816-0
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spelling ftncar:oai:drupal-site.org:articles_17055 2023-09-05T13:16:30+02:00 Changes in Arctic clouds during intervals of rapid sea ice loss Vavrus, Steve (author) Holland, Marika (author) Bailey, David (author) 2011-04-01 application/pdf http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-000-133 https://doi.org/10.1007/s00382-010-0816-0 en eng Springer Climate Dynamics http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-000-133 doi:10.1007/s00382-010-0816-0 ark:/85065/d7tm7cdc An edited version of this paper was published by Springer. Copyright 2010, Springer-Verlag. Arctic Clouds Abrupt change Rapid change Sea ice CCSM Text article 2011 ftncar https://doi.org/10.1007/s00382-010-0816-0 2023-08-14T18:35:58Z We investigate the behavior of clouds during rapid sea ice loss events (RILEs) in the Arctic, as simulated by multiple ensemble projections of the 21st century in the Community Climate System Model (CCSM3). Trends in cloud properties and sea ice coverage during RILEs are compared with their secular trends between 2000 and 2049 during summer, autumn, and winter. The results suggest that clouds promote abrupt Arctic climate change during RILEs through increased (decreased) cloudiness in autumn (summer) relative to the changes over the first half of the 21st century. The trends in cloud characteristics (cloud amount, water content, and radiative forcing) during RILEs are most strongly and consistently an amplifying effect during autumn, the season in which RILEs account for the majority of the secular trends. The total cloud trends in every season are primarily due to low clouds, which show a more robust response than middle and high clouds across RILEs. Lead-lag correlations of monthly sea ice concentration and cloud cover during autumn reveal that the relationship between less ice and more clouds is enhanced during RILEs, but there is no evidence that either variable is leading the other. Given that Arctic cloud projections in CCSM3 are similar to those from other state-of-the-art GCMs and that observations show increased autumn cloudiness associated with the extreme 2007 and 2008 sea ice minima, this study suggests that the rapidly declining Arctic sea ice will be accentuated by changes in polar clouds. National Aeronautics and Space Administration (NASA): NNG06GB26G National Science Foundation (NSF): OPP-0327664 National Science Foundation (NSF): ARC- 0628910 National Science Foundation (NSF): OPP-0612388 National Science Foundation (NSF): ARC-0652838 Article in Journal/Newspaper Arctic Climate change Sea ice OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) Arctic Climate Dynamics 36 7-8 1475 1489
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
Clouds
Abrupt change
Rapid change
Sea ice
CCSM
spellingShingle Arctic
Clouds
Abrupt change
Rapid change
Sea ice
CCSM
Changes in Arctic clouds during intervals of rapid sea ice loss
topic_facet Arctic
Clouds
Abrupt change
Rapid change
Sea ice
CCSM
description We investigate the behavior of clouds during rapid sea ice loss events (RILEs) in the Arctic, as simulated by multiple ensemble projections of the 21st century in the Community Climate System Model (CCSM3). Trends in cloud properties and sea ice coverage during RILEs are compared with their secular trends between 2000 and 2049 during summer, autumn, and winter. The results suggest that clouds promote abrupt Arctic climate change during RILEs through increased (decreased) cloudiness in autumn (summer) relative to the changes over the first half of the 21st century. The trends in cloud characteristics (cloud amount, water content, and radiative forcing) during RILEs are most strongly and consistently an amplifying effect during autumn, the season in which RILEs account for the majority of the secular trends. The total cloud trends in every season are primarily due to low clouds, which show a more robust response than middle and high clouds across RILEs. Lead-lag correlations of monthly sea ice concentration and cloud cover during autumn reveal that the relationship between less ice and more clouds is enhanced during RILEs, but there is no evidence that either variable is leading the other. Given that Arctic cloud projections in CCSM3 are similar to those from other state-of-the-art GCMs and that observations show increased autumn cloudiness associated with the extreme 2007 and 2008 sea ice minima, this study suggests that the rapidly declining Arctic sea ice will be accentuated by changes in polar clouds. National Aeronautics and Space Administration (NASA): NNG06GB26G National Science Foundation (NSF): OPP-0327664 National Science Foundation (NSF): ARC- 0628910 National Science Foundation (NSF): OPP-0612388 National Science Foundation (NSF): ARC-0652838
author2 Vavrus, Steve (author)
Holland, Marika (author)
Bailey, David (author)
format Article in Journal/Newspaper
title Changes in Arctic clouds during intervals of rapid sea ice loss
title_short Changes in Arctic clouds during intervals of rapid sea ice loss
title_full Changes in Arctic clouds during intervals of rapid sea ice loss
title_fullStr Changes in Arctic clouds during intervals of rapid sea ice loss
title_full_unstemmed Changes in Arctic clouds during intervals of rapid sea ice loss
title_sort changes in arctic clouds during intervals of rapid sea ice loss
publisher Springer
publishDate 2011
url http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-000-133
https://doi.org/10.1007/s00382-010-0816-0
geographic Arctic
geographic_facet Arctic
genre Arctic
Climate change
Sea ice
genre_facet Arctic
Climate change
Sea ice
op_relation Climate Dynamics
http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-000-133
doi:10.1007/s00382-010-0816-0
ark:/85065/d7tm7cdc
op_rights An edited version of this paper was published by Springer. Copyright 2010, Springer-Verlag.
op_doi https://doi.org/10.1007/s00382-010-0816-0
container_title Climate Dynamics
container_volume 36
container_issue 7-8
container_start_page 1475
op_container_end_page 1489
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