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


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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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