New Look at the Water Exchange between the Arctic and the North Atlantic in Iceland Basin
- Autores: Gladyshev S.V.1, Gladyshev V.S.1, Klyuvitkin A.A.1, Gulev S.K.1
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Afiliações:
- Shirshov Institute of Oceanology of the Russian Academy of Sciences
- Edição: Volume 485, Nº 2 (2019)
- Páginas: 401-404
- Seção: Oceanology
- URL: https://ogarev-online.ru/1028-334X/article/view/194803
- DOI: https://doi.org/10.1134/S1028334X19040020
- ID: 194803
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Resumo
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.
Sobre autores
S. Gladyshev
Shirshov Institute of Oceanology of the Russian Academy of Sciences
Autor responsável pela correspondência
Email: sgladyshev@ocean.ru
Rússia, Moscow, 117997
V. Gladyshev
Shirshov Institute of Oceanology of the Russian Academy of Sciences
Email: sgladyshev@ocean.ru
Rússia, Moscow, 117997
A. Klyuvitkin
Shirshov Institute of Oceanology of the Russian Academy of Sciences
Email: sgladyshev@ocean.ru
Rússia, Moscow, 117997
S. Gulev
Shirshov Institute of Oceanology of the Russian Academy of Sciences
Email: sgladyshev@ocean.ru
Rússia, Moscow, 117997
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