Ekman circulation in the Arctic Ocean: Beyond the Beaufort Gyre
Ekman circulation in the Arctic Ocean: Beyond the Beaufort Gyre
复制标题
北冰洋的埃克曼环流：波弗特环流之外
DOI：
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发表时间：
2017
期刊：
影响因子：
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通讯作者：
Craig M. Lee
中科院分区：
文献类型：
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作者：
Barry B. Ma;M. Steele;Craig M. Lee
来自卫星观测以及浮标观测和同化的数据被用来计算海洋Ekman层的传输，并评估1979-2014年期间北冰洋的长期趋势。整个北极盆地36年平均上升(下降)流为3.6 ± 2.0(−4.0 ± 2.2)Sv，其中∼0.4Sv净下降流主要由加拿大地区贡献。在长期趋势方面，整个北极盆地的年平均上(下)流以0.89(−0.96)Sv/十年的线性速度增加。加拿大/阿拉斯加海岸以及波弗特海和拉普特夫海是埃克曼运输最密集的地区。北冰洋中部和林肯海的运输也有增加的趋势。加拿大和欧亚地区各占北极盆地埃克曼垂直变化的一半左右。这篇文章受版权保护。版权所有。
Data derived from satellite based observations, with buoy-based observations and assimilations, are used to calculate ocean Ekman layer transport and evaluate long-term trends in the Arctic Ocean over the period 1979–2014. The 36-year mean of upwelling (downwelling) is 3.6 ± 2.0 (−4.0 ± 2.2) Sv for the entire Arctic Basin, with ∼0.4 Sv net downwelling contributed mostly by the Canadian region. With regard to long-term trends, the annual mean upwelling (downwelling) over the entire Arctic Basin is increasing at a linear rate of 0.89 (−0.96) Sv/decade. The Canada/Alaska coasts and Beaufort and Laptev seas are regions of greatest Ekman transport intensification. The central Arctic Ocean and Lincoln Sea also have an increasing trend in transport. The Canadian and Eurasian regions each account for about half the total vertical Ekman variations in the Arctic Basin. This article is protected by copyright. All rights reserved.
影响因子：
3.6
作者：
Timmermans, M. -L.;Proshutinsky, A.;Nishino, S.
通讯作者：
Nishino, S.