Extreme warming in the Kara Sea and Barents Sea during the winter period 2000-16

The regional climate model COSMO in Climate Limited-Area Mode (COSMO-CLM or CCLM) is used with a high resolution of 15 km for the entire Arctic for all winters 2002/03-2014/15. The simulations show a high spatial and temporal variability of the recent 2-m air temperature increase in the Arctic. The...

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Published in:Journal of Climate
Main Authors: Kohnemann, S., Heinemann, G., Bromwich, D., Gutjahr, O.
Format: Article in Journal/Newspaper
Language:English
Published: 2017
Subjects:
Online Access:http://hdl.handle.net/11858/00-001M-0000-002E-249E-5
http://hdl.handle.net/11858/00-001M-0000-002E-9BB2-4
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spelling ftpubman:oai:pure.mpg.de:item_2496080 2023-08-27T04:07:38+02:00 Extreme warming in the Kara Sea and Barents Sea during the winter period 2000-16 Kohnemann, S. Heinemann, G. Bromwich, D. Gutjahr, O. 2017 application/pdf http://hdl.handle.net/11858/00-001M-0000-002E-249E-5 http://hdl.handle.net/11858/00-001M-0000-002E-9BB2-4 eng eng info:eu-repo/semantics/altIdentifier/doi/10.1175/JCLI-D-16-0693.1 http://hdl.handle.net/11858/00-001M-0000-002E-249E-5 http://hdl.handle.net/11858/00-001M-0000-002E-9BB2-4 info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by-nc-nd/3.0/ Journal of Climate info:eu-repo/semantics/article 2017 ftpubman https://doi.org/10.1175/JCLI-D-16-0693.1 2023-08-02T01:55:33Z The regional climate model COSMO in Climate Limited-Area Mode (COSMO-CLM or CCLM) is used with a high resolution of 15 km for the entire Arctic for all winters 2002/03-2014/15. The simulations show a high spatial and temporal variability of the recent 2-m air temperature increase in the Arctic. The maximum warming occurs north of Novaya Zemlya in the Kara Sea and Barents Sea between March 2003 and 2012 and is responsible for up to a 20°C increase. Land-based observations confirm the increase but do not cover the maximum regions that are located over the ocean and sea ice. Also, the 30-km version of the Arctic System Reanalysis (ASR) is used to verify the CCLM for the overlapping time period 2002/03-2011/12. The differences between CCLM and ASR 2-m air temperatures vary slightly within 1°C for the ocean and sea ice area. Thus, ASR captures the extreme warming as well. The monthly 2-m air temperatures of observations and ERA-Interim data show a large variability for the winters 1979-2016. Nevertheless, the air temperature rise since the beginning of the twenty-first century is up to 8 times higher than in the decades before. The sea ice decrease is identified as the likely reason for the warming. The vertical temperature profiles show that the warming has a maximum near the surface, but a 0.5°C yr-1 increase is found up to 2 km. CCLM, ASR, and also the coarser resolved ERA-Interim data show that February and March are the months with the highest 2-m air temperature increases, averaged over the ocean and sea ice area north of 70°N; for CCLM the warming amounts to an average of almost 5°C for 2002/03-2011/12. © 2017 American Meteorological Society. Article in Journal/Newspaper Arctic Barents Sea Kara Sea Novaya Zemlya Sea ice Max Planck Society: MPG.PuRe Arctic Barents Sea Kara Sea Journal of Climate 30 22 8913 8927
institution Open Polar
collection Max Planck Society: MPG.PuRe
op_collection_id ftpubman
language English
description The regional climate model COSMO in Climate Limited-Area Mode (COSMO-CLM or CCLM) is used with a high resolution of 15 km for the entire Arctic for all winters 2002/03-2014/15. The simulations show a high spatial and temporal variability of the recent 2-m air temperature increase in the Arctic. The maximum warming occurs north of Novaya Zemlya in the Kara Sea and Barents Sea between March 2003 and 2012 and is responsible for up to a 20°C increase. Land-based observations confirm the increase but do not cover the maximum regions that are located over the ocean and sea ice. Also, the 30-km version of the Arctic System Reanalysis (ASR) is used to verify the CCLM for the overlapping time period 2002/03-2011/12. The differences between CCLM and ASR 2-m air temperatures vary slightly within 1°C for the ocean and sea ice area. Thus, ASR captures the extreme warming as well. The monthly 2-m air temperatures of observations and ERA-Interim data show a large variability for the winters 1979-2016. Nevertheless, the air temperature rise since the beginning of the twenty-first century is up to 8 times higher than in the decades before. The sea ice decrease is identified as the likely reason for the warming. The vertical temperature profiles show that the warming has a maximum near the surface, but a 0.5°C yr-1 increase is found up to 2 km. CCLM, ASR, and also the coarser resolved ERA-Interim data show that February and March are the months with the highest 2-m air temperature increases, averaged over the ocean and sea ice area north of 70°N; for CCLM the warming amounts to an average of almost 5°C for 2002/03-2011/12. © 2017 American Meteorological Society.
format Article in Journal/Newspaper
author Kohnemann, S.
Heinemann, G.
Bromwich, D.
Gutjahr, O.
spellingShingle Kohnemann, S.
Heinemann, G.
Bromwich, D.
Gutjahr, O.
Extreme warming in the Kara Sea and Barents Sea during the winter period 2000-16
author_facet Kohnemann, S.
Heinemann, G.
Bromwich, D.
Gutjahr, O.
author_sort Kohnemann, S.
title Extreme warming in the Kara Sea and Barents Sea during the winter period 2000-16
title_short Extreme warming in the Kara Sea and Barents Sea during the winter period 2000-16
title_full Extreme warming in the Kara Sea and Barents Sea during the winter period 2000-16
title_fullStr Extreme warming in the Kara Sea and Barents Sea during the winter period 2000-16
title_full_unstemmed Extreme warming in the Kara Sea and Barents Sea during the winter period 2000-16
title_sort extreme warming in the kara sea and barents sea during the winter period 2000-16
publishDate 2017
url http://hdl.handle.net/11858/00-001M-0000-002E-249E-5
http://hdl.handle.net/11858/00-001M-0000-002E-9BB2-4
geographic Arctic
Barents Sea
Kara Sea
geographic_facet Arctic
Barents Sea
Kara Sea
genre Arctic
Barents Sea
Kara Sea
Novaya Zemlya
Sea ice
genre_facet Arctic
Barents Sea
Kara Sea
Novaya Zemlya
Sea ice
op_source Journal of Climate
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1175/JCLI-D-16-0693.1
http://hdl.handle.net/11858/00-001M-0000-002E-249E-5
http://hdl.handle.net/11858/00-001M-0000-002E-9BB2-4
op_rights info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by-nc-nd/3.0/
op_doi https://doi.org/10.1175/JCLI-D-16-0693.1
container_title Journal of Climate
container_volume 30
container_issue 22
container_start_page 8913
op_container_end_page 8927
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