Increased variability of the Arctic summer ice extent in a warmer climate, Geophys

[1] Simulations performed with general circulation models and a model of intermediate complexity show that the variability of the September sea ice extent in the Arctic of the 21st century increases first when the mean extent decreases from present-day values. A maximum of the variance is found when...

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Main Authors: O. Arzel, C. M. Bitz
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.697.2697
http://web.maths.unsw.edu.au/%7Eoarzel/publis/Goosse_et_al.GRL2009.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.697.2697 2023-05-15T13:58:30+02:00 Increased variability of the Arctic summer ice extent in a warmer climate, Geophys O. Arzel C. M. Bitz The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.697.2697 http://web.maths.unsw.edu.au/%7Eoarzel/publis/Goosse_et_al.GRL2009.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.697.2697 http://web.maths.unsw.edu.au/%7Eoarzel/publis/Goosse_et_al.GRL2009.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://web.maths.unsw.edu.au/%7Eoarzel/publis/Goosse_et_al.GRL2009.pdf text ftciteseerx 2016-01-08T18:41:59Z [1] Simulations performed with general circulation models and a model of intermediate complexity show that the variability of the September sea ice extent in the Arctic of the 21st century increases first when the mean extent decreases from present-day values. A maximum of the variance is found when the mean September ice extent is around 3 million km2. For lower extents, the variance declines with the mean extent. The behavior is clearly different in Antarctica where the variance always decreases as the mean ice extent decreases, following roughly a square-root law compatible with very simple geometric arguments. Several mechanisms are responsible for the non-linear behavior of the Arctic. However, the strong interhemispheric contrast suggests that the difference in geometrical setting, with an open ocean in the south and a semi-closed basin in the north, plays a Text Antarc* Antarctica Arctic Sea ice Unknown Arctic
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description [1] Simulations performed with general circulation models and a model of intermediate complexity show that the variability of the September sea ice extent in the Arctic of the 21st century increases first when the mean extent decreases from present-day values. A maximum of the variance is found when the mean September ice extent is around 3 million km2. For lower extents, the variance declines with the mean extent. The behavior is clearly different in Antarctica where the variance always decreases as the mean ice extent decreases, following roughly a square-root law compatible with very simple geometric arguments. Several mechanisms are responsible for the non-linear behavior of the Arctic. However, the strong interhemispheric contrast suggests that the difference in geometrical setting, with an open ocean in the south and a semi-closed basin in the north, plays a
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author O. Arzel
C. M. Bitz
spellingShingle O. Arzel
C. M. Bitz
Increased variability of the Arctic summer ice extent in a warmer climate, Geophys
author_facet O. Arzel
C. M. Bitz
author_sort O. Arzel
title Increased variability of the Arctic summer ice extent in a warmer climate, Geophys
title_short Increased variability of the Arctic summer ice extent in a warmer climate, Geophys
title_full Increased variability of the Arctic summer ice extent in a warmer climate, Geophys
title_fullStr Increased variability of the Arctic summer ice extent in a warmer climate, Geophys
title_full_unstemmed Increased variability of the Arctic summer ice extent in a warmer climate, Geophys
title_sort increased variability of the arctic summer ice extent in a warmer climate, geophys
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.697.2697
http://web.maths.unsw.edu.au/%7Eoarzel/publis/Goosse_et_al.GRL2009.pdf
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genre_facet Antarc*
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http://web.maths.unsw.edu.au/%7Eoarzel/publis/Goosse_et_al.GRL2009.pdf
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