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


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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.

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S. Gladyshev

Shirshov Institute of Oceanology

编辑信件的主要联系方式.
Email: sgladyshev@ocean.ru
俄罗斯联邦, Moscow, 117218

V. Gladyshev

Shirshov Institute of Oceanology

Email: sgladyshev@ocean.ru
俄罗斯联邦, Moscow, 117218

L. Pautova

Shirshov Institute of Oceanology

Email: sgladyshev@ocean.ru
俄罗斯联邦, Moscow, 117218

S. Gulev

Shirshov Institute of Oceanology

Email: sgladyshev@ocean.ru
俄罗斯联邦, Moscow, 117218

N. Politova

Shirshov Institute of Oceanology

Email: sgladyshev@ocean.ru
俄罗斯联邦, Moscow, 117218

A. Sokov

Shirshov Institute of Oceanology

Email: sgladyshev@ocean.ru
俄罗斯联邦, Moscow, 117218

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