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


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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.

作者简介

S. Gladyshev

Shirshov Institute of Oceanology of the Russian Academy of Sciences

编辑信件的主要联系方式.
Email: sgladyshev@ocean.ru
俄罗斯联邦, Moscow, 117997

V. Gladyshev

Shirshov Institute of Oceanology of the Russian Academy of Sciences

Email: sgladyshev@ocean.ru
俄罗斯联邦, Moscow, 117997

A. Klyuvitkin

Shirshov Institute of Oceanology of the Russian Academy of Sciences

Email: sgladyshev@ocean.ru
俄罗斯联邦, Moscow, 117997

S. Gulev

Shirshov Institute of Oceanology of the Russian Academy of Sciences

Email: sgladyshev@ocean.ru
俄罗斯联邦, Moscow, 117997

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