Delayed Recovery of the Irminger Interior From Cooling in 2015 Due To Widespread Buoyancy Loss and Suppressed Restratification

Watermass transformation in the Irminger Sea, a key region for the Atlantic Meridional Overturning Circulation, is influenced by atmospheric and oceanic variability. Strong wintertime atmospheric forcing in 2015 resulted in enhanced convection and the densification of the Irminger Sea. Deep convecti...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Nelson, Monica, Straneo, Fiamma, Purkey, Sarah G., De Jong, Marieke Femke
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union (AGU) 2024
Subjects:
Online Access:https://archimer.ifremer.fr/doc/00881/99312/109298.pdf
https://archimer.ifremer.fr/doc/00881/99312/109299.pdf
https://doi.org/10.1029/2023GL106501
https://archimer.ifremer.fr/doc/00881/99312/