Email this article New Look at the Water Exchange between the Arctic and the North Atlantic in Iceland Basin
- Authors: Gladyshev S.V.1, Gladyshev V.S.1, Klyuvitkin A.A.1, Gulev S.K.1
-
Affiliations:
- Shirshov Institute of Oceanology of the Russian Academy of Sciences
- Issue: Vol 485, No 2 (2019)
- Pages: 401-404
- Section: Oceanology
- URL: https://ogarev-online.ru/1028-334X/article/view/194803
- DOI: https://doi.org/10.1134/S1028334X19040020
- ID: 194803
Cite item
Open Access
Access granted
Subscription Access
Abstract
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.
About the authors
S. V. Gladyshev
Shirshov Institute of Oceanology of the Russian Academy of Sciences
Author for correspondence.
Email: sgladyshev@ocean.ru
Russian Federation, Moscow, 117997
V. S. Gladyshev
Shirshov Institute of Oceanology of the Russian Academy of Sciences
Email: sgladyshev@ocean.ru
Russian Federation, Moscow, 117997
A. A. Klyuvitkin
Shirshov Institute of Oceanology of the Russian Academy of Sciences
Email: sgladyshev@ocean.ru
Russian Federation, Moscow, 117997
S. K. Gulev
Shirshov Institute of Oceanology of the Russian Academy of Sciences
Email: sgladyshev@ocean.ru
Russian Federation, Moscow, 117997
Supplementary files
