Restratification structure and processes in the Irminger Sea

The Irminger Sea is one of the few regions in the ocean where deep (>1,000 m) convection occurs. Convection is followed by restratification during summer, when the stratification of the water column is reestablished and the convectively formed water is exported at depth. There are currently no de...

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Bibliographic Details
Published in:Journal of Geophysical Research: Oceans
Main Authors: Sterl, M.F., de Jong, M.F.
Format: Article in Journal/Newspaper
Language:English
Published: 2022
Subjects:
Online Access:https://www.vliz.be/imisdocs/publications/35/385935.pdf