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DOI | 10.5194/tc-14-477-2020 |
Sea ice volume variability and water temperature in the Greenland Sea | |
Selyuzhenok V.; Bashmachnikov I.; Ricker R.; Vesman A.; Bobylev L. | |
发表日期 | 2020 |
ISSN | 19940416 |
EISSN | 14 |
起始页码 | 477 |
结束页码 | 495 |
卷号 | 14期号:2 |
英文摘要 | This study explores a link between the long-term variations in the integral sea ice volume (SIV) in the Greenland Sea and oceanic processes. Using the Pan-Arctic Ice Ocean Modeling and Assimilation System (PIOMAS, 1979-2016), we show that the increasing sea ice volume flux through Fram Strait goes in parallel with a decrease in SIV in the Greenland Sea. The overall SIV loss in the Greenland Sea is 113km3 per decade, while the total SIV import through Fram Strait increases by 115km3 per decade. An analysis of the ocean temperature and the mixed-layer depth (MLD) over the climatic mean area of the winter marginal sea ice zone (MIZ) revealed a doubling of the amount of the upper-ocean heat content available for the sea ice melt from 1993 to 2016. This increase alone can explain the SIV loss in the Greenland Sea over the 24-year study period, even when accounting for the increasing SIV flux from the Arctic. The increase in the oceanic heat content is found to be linked to an increase in temperature of the Atlantic Water along the main currents of the Nordic Seas, following an increase in the oceanic heat flux from the subtropical North Atlantic. We argue that the predominantly positive winter North Atlantic Oscillation (NAO) index during the 4 most recent decades, together with an intensification of the deep convection in the Greenland Sea, is responsible for the intensification of the cyclonic circulation pattern in the Nordic Seas, which results in the observed long-term variations in the SIV. © 2020 BMJ Publishing Group. All rights reserved. |
学科领域 | heat flux; index method; long-term change; mixed layer; North Atlantic Oscillation; sea ice; subtropical region; upper ocean; volume; water temperature; Arctic; Arctic Ocean; Atlantic Ocean; Atlantic Ocean (North); Fram Strait; Greenland Sea; Norwegian Sea; Norwegian Sea; Simian immunodeficiency virus |
语种 | 英语 |
scopus关键词 | heat flux; index method; long-term change; mixed layer; North Atlantic Oscillation; sea ice; subtropical region; upper ocean; volume; water temperature; Arctic; Arctic Ocean; Atlantic Ocean; Atlantic Ocean (North); Fram Strait; Greenland Sea; Norwegian Sea; Norwegian Sea; Simian immunodeficiency virus |
来源期刊 | The Cryosphere
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/118761 |
作者单位 | Nansen International Environmental and Remote Sensing Centre, 14 Line V.O. 7, St. Petersburg, 199034, Russian Federation; Department of Oceanography, St. Petersburg State University, 10 Line V.O. 33, St. Petersburg, 199034, Russian Federation; Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung, Klumannstr. 3d, Bremerhaven, 27570, Germany; Atmosphere-sea Ice-ocean Interaction Department, Arctic and Antarctic Research Institute, Bering Str. 38, St. Petersburg, 199397, Russian Federation |
推荐引用方式 GB/T 7714 | Selyuzhenok V.,Bashmachnikov I.,Ricker R.,et al. Sea ice volume variability and water temperature in the Greenland Sea[J],2020,14(2). |
APA | Selyuzhenok V.,Bashmachnikov I.,Ricker R.,Vesman A.,&Bobylev L..(2020).Sea ice volume variability and water temperature in the Greenland Sea.The Cryosphere,14(2). |
MLA | Selyuzhenok V.,et al."Sea ice volume variability and water temperature in the Greenland Sea".The Cryosphere 14.2(2020). |
条目包含的文件 | 条目无相关文件。 |
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