New Look at the Water Exchange between the Arctic and the North Atlantic in Iceland Basin
- Авторлар: Gladyshev S.V.1, Gladyshev V.S.1, Klyuvitkin A.A.1, Gulev S.K.1
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Мекемелер:
- Shirshov Institute of Oceanology of the Russian Academy of Sciences
- Шығарылым: Том 485, № 2 (2019)
- Беттер: 401-404
- Бөлім: Oceanology
- URL: https://ogarev-online.ru/1028-334X/article/view/194803
- DOI: https://doi.org/10.1134/S1028334X19040020
- ID: 194803
Дәйексөз келтіру
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.
Авторлар туралы
S. Gladyshev
Shirshov Institute of Oceanology of the Russian Academy of Sciences
Хат алмасуға жауапты Автор.
Email: sgladyshev@ocean.ru
Ресей, Moscow, 117997
V. Gladyshev
Shirshov Institute of Oceanology of the Russian Academy of Sciences
Email: sgladyshev@ocean.ru
Ресей, Moscow, 117997
A. Klyuvitkin
Shirshov Institute of Oceanology of the Russian Academy of Sciences
Email: sgladyshev@ocean.ru
Ресей, Moscow, 117997
S. Gulev
Shirshov Institute of Oceanology of the Russian Academy of Sciences
Email: sgladyshev@ocean.ru
Ресей, Moscow, 117997
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