Interaction of Dense Shelf Waters of the Barents and Kara Seas with the Eddy Structures

Purpose. Considered are the processes of dense bottom water formation in winter in the region of the Novaya Zemlya northwestern coast, its further propagation (cascading) towards the St. Anna trough and then to the open ocean. The goal of the paper is to show that the process of such propagation is...

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Bibliographic Details
Published in:Physical Oceanography
Main Authors: G.A. Platov, E.N. Golubeva
Format: Article in Journal/Newspaper
Language:English
Published: Federal State Budget Scientific Institution «Marine Hydrophysical Institute of RAS» 2019
Subjects:
Online Access:https://doi.org/10.22449/1573-160X-2019-6-484-503
https://doaj.org/article/6c2499713d4348738e0e28a6b204e0a8