New Look at the Water Exchange between the Arctic and the North Atlantic in Iceland Basin


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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.

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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© Pleiades Publishing, Ltd., 2019