New Look at the Water Exchange between the Arctic and the North Atlantic in Iceland Basin
- 作者: Gladyshev S.V.1, Gladyshev V.S.1, Klyuvitkin A.A.1, Gulev S.K.1
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隶属关系:
- Shirshov Institute of Oceanology of the Russian Academy of Sciences
- 期: 卷 485, 编号 2 (2019)
- 页面: 401-404
- 栏目: Oceanology
- URL: https://ogarev-online.ru/1028-334X/article/view/194803
- DOI: https://doi.org/10.1134/S1028334X19040020
- ID: 194803
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详细
Based on multiyear current observations along 59.5° N in the Subpolar North Atlantic, multijet transport of arctic water along the eastern slope of Reykjanes Ridge producing the Iceland–Scotland overflow water (ISOW) in Iceland Basin is revealed. The main properties of the jet, as well as their contribution to deep water transport, are discussed.
作者简介
S. Gladyshev
Shirshov Institute of Oceanology of the Russian Academy of Sciences
编辑信件的主要联系方式.
Email: sgladyshev@ocean.ru
俄罗斯联邦, Moscow, 117997
V. Gladyshev
Shirshov Institute of Oceanology of the Russian Academy of Sciences
Email: sgladyshev@ocean.ru
俄罗斯联邦, Moscow, 117997
A. Klyuvitkin
Shirshov Institute of Oceanology of the Russian Academy of Sciences
Email: sgladyshev@ocean.ru
俄罗斯联邦, Moscow, 117997
S. Gulev
Shirshov Institute of Oceanology of the Russian Academy of Sciences
Email: sgladyshev@ocean.ru
俄罗斯联邦, Moscow, 117997
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