New Look at the Water Exchange between the Arctic and the North Atlantic in Iceland Basin
- Авторы: Gladyshev S.V.1, Gladyshev V.S.1, Klyuvitkin A.A.1, Gulev S.K.1
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Учреждения:
- Shirshov Institute of Oceanology of the Russian Academy of Sciences
- Выпуск: Том 485, № 2 (2019)
- Страницы: 401-404
- Раздел: Oceanology
- URL: https://journals.rcsi.science/1028-334X/article/view/194803
- DOI: https://doi.org/10.1134/S1028334X19040020
- ID: 194803
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Аннотация
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.
Об авторах
S. Gladyshev
Shirshov Institute of Oceanology of the Russian Academy of Sciences
Автор, ответственный за переписку.
Email: sgladyshev@ocean.ru
Россия, Moscow, 117997
V. Gladyshev
Shirshov Institute of Oceanology of the Russian Academy of Sciences
Email: sgladyshev@ocean.ru
Россия, Moscow, 117997
A. Klyuvitkin
Shirshov Institute of Oceanology of the Russian Academy of Sciences
Email: sgladyshev@ocean.ru
Россия, Moscow, 117997
S. Gulev
Shirshov Institute of Oceanology of the Russian Academy of Sciences
Email: sgladyshev@ocean.ru
Россия, Moscow, 117997
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