The Structure and Long-Term Variability of the Bottom Layer in the Irminger Sea


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Abstract

This paper shows the important role that circulation can play in the long-term variability of thermohaline properties of the bottom layer in the Irminger Sea, and the increase in salinity in the 21st century in spite of intense ice melting in the Arctic and freshening of the upper and intermediate layers that started over the last 5–7 years in the North Atlantic.

About the authors

S. V. Gladyshev

Shirshov Institute of Oceanology

Author for correspondence.
Email: sgladyshev@ocean.ru
Russian Federation, Moscow, 117218

V. S. Gladyshev

Shirshov Institute of Oceanology

Email: sgladyshev@ocean.ru
Russian Federation, Moscow, 117218

L. A. Pautova

Shirshov Institute of Oceanology

Email: sgladyshev@ocean.ru
Russian Federation, Moscow, 117218

S. K. Gulev

Shirshov Institute of Oceanology

Email: sgladyshev@ocean.ru
Russian Federation, Moscow, 117218

N. V. Politova

Shirshov Institute of Oceanology

Email: sgladyshev@ocean.ru
Russian Federation, Moscow, 117218

A. V. Sokov

Shirshov Institute of Oceanology

Email: sgladyshev@ocean.ru
Russian Federation, Moscow, 117218


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