The Structure and Long-Term Variability of the Bottom Layer in the Irminger Sea
- Authors: Gladyshev S.V.1, Gladyshev V.S.1, Pautova L.A.1, Gulev S.K.1, Politova N.V.1, Sokov A.V.1
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Affiliations:
- Shirshov Institute of Oceanology
- Issue: Vol 481, No 2 (2018)
- Pages: 1025-1028
- Section: Oceanology
- URL: https://journals.rcsi.science/1028-334X/article/view/193818
- DOI: https://doi.org/10.1134/S1028334X18080044
- ID: 193818
Cite item
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