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DOI10.1175/JCLI-D-16-0693.1
Extreme Warming in the Kara Sea and Barents Sea during the Winter Period 2000-16
Kohnemann, Svenja H. E.1; Heinemann, Guenther1; Bromwich, David H.2; Gutjahr, Oliver3
2017-11-01
发表期刊JOURNAL OF CLIMATE
ISSN0894-8755
EISSN1520-0442
出版年2017
卷号30期号:22
文章类型Article
语种英语
国家Germany; USA
英文摘要

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 degrees 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 degrees 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 degrees 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 degrees N; for CCLM the warming amounts to an average of almost 5 degrees C for 2002/03-2011/12.


领域气候变化
收录类别SCI-E
WOS记录号WOS:000416488200004
WOS关键词ARCTIC AMPLIFICATION ; ICE PRODUCTION ; CLIMATE MODEL ; ATTRIBUTION ; REANALYSIS ; DECLINE
WOS类目Meteorology & Atmospheric Sciences
WOS研究方向Meteorology & Atmospheric Sciences
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文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/20264
专题气候变化
作者单位1.Univ Trier, Environm Meteorol, Trier, Germany;
2.Ohio State Univ, Byrd Polar & Climate Res Ctr, Polar Meteorol Grp, Columbus, OH 43210 USA;
3.Max Planck Inst Meteorol, Hamburg, Germany
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GB/T 7714
Kohnemann, Svenja H. E.,Heinemann, Guenther,Bromwich, David H.,et al. Extreme Warming in the Kara Sea and Barents Sea during the Winter Period 2000-16[J]. JOURNAL OF CLIMATE,2017,30(22).
APA Kohnemann, Svenja H. E.,Heinemann, Guenther,Bromwich, David H.,&Gutjahr, Oliver.(2017).Extreme Warming in the Kara Sea and Barents Sea during the Winter Period 2000-16.JOURNAL OF CLIMATE,30(22).
MLA Kohnemann, Svenja H. E.,et al."Extreme Warming in the Kara Sea and Barents Sea during the Winter Period 2000-16".JOURNAL OF CLIMATE 30.22(2017).
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