The Arctic Sea ice in the CMIP3 climate model ensemble – variability and anthropogenic change

The strongest manifestation of global warming is observed in the Arctic. The warming in the Arctic during the recent decades is about twice as strong as in the global average and has been accompanied by a summer sea ice decline that is very likely unprecedented during the last millennium. Here, Arct...

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Main Authors: Behrens, L. K., Martin, Thomas, Semenov, Vladimir, Latif, Mojib
Format: Article in Journal/Newspaper
Language:English
Published: 2012
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/20094/
https://oceanrep.geomar.de/id/eprint/20094/1/tcd-6-5317-2012.pdf
https://doi.org/10.5194/tcd-6-5317-2012
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spelling ftoceanrep:oai:oceanrep.geomar.de:20094 2023-05-15T14:26:54+02:00 The Arctic Sea ice in the CMIP3 climate model ensemble – variability and anthropogenic change Behrens, L. K. Martin, Thomas Semenov, Vladimir Latif, Mojib 2012 text https://oceanrep.geomar.de/id/eprint/20094/ https://oceanrep.geomar.de/id/eprint/20094/1/tcd-6-5317-2012.pdf https://doi.org/10.5194/tcd-6-5317-2012 en eng https://oceanrep.geomar.de/id/eprint/20094/1/tcd-6-5317-2012.pdf Behrens, L. K., Martin, T. , Semenov, V. and Latif, M. (2012) The Arctic Sea ice in the CMIP3 climate model ensemble – variability and anthropogenic change. Open Access The Cryosphere Discussions, 6 (6). pp. 5317-5344. DOI 10.5194/tcd-6-5317-2012 <https://doi.org/10.5194/tcd-6-5317-2012>. doi:10.5194/tcd-6-5317-2012 cc_by_3.0 info:eu-repo/semantics/openAccess Article NonPeerReviewed info:eu-repo/semantics/article 2012 ftoceanrep https://doi.org/10.5194/tcd-6-5317-2012 2023-04-07T15:07:42Z The strongest manifestation of global warming is observed in the Arctic. The warming in the Arctic during the recent decades is about twice as strong as in the global average and has been accompanied by a summer sea ice decline that is very likely unprecedented during the last millennium. Here, Arctic sea ice variability is analyzed in the ensemble of CMIP3 models. Complementary to several previous studies, we focus on regional aspects, in particular on the Barents Sea. We also investigate the changes in the seasonal cycle and interannual variability. In all regions, the models predict a reduction in sea ice area and sea ice volume during 1900–2100. Toward the end of the 21st century, the models simulate higher sea ice area variability in September than in March, whereas the variability in the preindustrial control runs is higher in March. Furthermore, the amplitude and phase of the sea ice seasonal cycle change in response to enhanced greenhouse warming. The amplitude of the sea ice area seasonal cycle increases due to the very strong sea ice area decline in September. The seasonal cycle amplitude of the sea ice volume decreases due to the stronger reduction of sea ice volume in March. Multi-model mean estimates for the late 20th century are comparable with observational data only for the entire Arctic and the Central Arctic. In the Barents Sea, differences between the multi-model mean and the observational data are more pronounced. Regional sea ice sensitivity to Northern Hemisphere average surface warming has been investigated. Article in Journal/Newspaper Arctic Arctic Barents Sea Global warming Sea ice The Cryosphere The Cryosphere Discussions OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Arctic Barents Sea
institution Open Polar
collection OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel)
op_collection_id ftoceanrep
language English
description The strongest manifestation of global warming is observed in the Arctic. The warming in the Arctic during the recent decades is about twice as strong as in the global average and has been accompanied by a summer sea ice decline that is very likely unprecedented during the last millennium. Here, Arctic sea ice variability is analyzed in the ensemble of CMIP3 models. Complementary to several previous studies, we focus on regional aspects, in particular on the Barents Sea. We also investigate the changes in the seasonal cycle and interannual variability. In all regions, the models predict a reduction in sea ice area and sea ice volume during 1900–2100. Toward the end of the 21st century, the models simulate higher sea ice area variability in September than in March, whereas the variability in the preindustrial control runs is higher in March. Furthermore, the amplitude and phase of the sea ice seasonal cycle change in response to enhanced greenhouse warming. The amplitude of the sea ice area seasonal cycle increases due to the very strong sea ice area decline in September. The seasonal cycle amplitude of the sea ice volume decreases due to the stronger reduction of sea ice volume in March. Multi-model mean estimates for the late 20th century are comparable with observational data only for the entire Arctic and the Central Arctic. In the Barents Sea, differences between the multi-model mean and the observational data are more pronounced. Regional sea ice sensitivity to Northern Hemisphere average surface warming has been investigated.
format Article in Journal/Newspaper
author Behrens, L. K.
Martin, Thomas
Semenov, Vladimir
Latif, Mojib
spellingShingle Behrens, L. K.
Martin, Thomas
Semenov, Vladimir
Latif, Mojib
The Arctic Sea ice in the CMIP3 climate model ensemble – variability and anthropogenic change
author_facet Behrens, L. K.
Martin, Thomas
Semenov, Vladimir
Latif, Mojib
author_sort Behrens, L. K.
title The Arctic Sea ice in the CMIP3 climate model ensemble – variability and anthropogenic change
title_short The Arctic Sea ice in the CMIP3 climate model ensemble – variability and anthropogenic change
title_full The Arctic Sea ice in the CMIP3 climate model ensemble – variability and anthropogenic change
title_fullStr The Arctic Sea ice in the CMIP3 climate model ensemble – variability and anthropogenic change
title_full_unstemmed The Arctic Sea ice in the CMIP3 climate model ensemble – variability and anthropogenic change
title_sort arctic sea ice in the cmip3 climate model ensemble – variability and anthropogenic change
publishDate 2012
url https://oceanrep.geomar.de/id/eprint/20094/
https://oceanrep.geomar.de/id/eprint/20094/1/tcd-6-5317-2012.pdf
https://doi.org/10.5194/tcd-6-5317-2012
geographic Arctic
Barents Sea
geographic_facet Arctic
Barents Sea
genre Arctic
Arctic
Barents Sea
Global warming
Sea ice
The Cryosphere
The Cryosphere Discussions
genre_facet Arctic
Arctic
Barents Sea
Global warming
Sea ice
The Cryosphere
The Cryosphere Discussions
op_relation https://oceanrep.geomar.de/id/eprint/20094/1/tcd-6-5317-2012.pdf
Behrens, L. K., Martin, T. , Semenov, V. and Latif, M. (2012) The Arctic Sea ice in the CMIP3 climate model ensemble – variability and anthropogenic change. Open Access The Cryosphere Discussions, 6 (6). pp. 5317-5344. DOI 10.5194/tcd-6-5317-2012 <https://doi.org/10.5194/tcd-6-5317-2012>.
doi:10.5194/tcd-6-5317-2012
op_rights cc_by_3.0
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.5194/tcd-6-5317-2012
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