The Irminger Gyre as a Key Driver of the Subpolar North Atlantic Overturning

Abstract The lower limb of the Atlantic meridional overturning circulation (AMOC) is the equatorward flow of dense waters formed through the cooling and freshening of the poleward‐flowing upper limb. In the subpolar North Atlantic (SPNA), upper limb variability is primarily set by the North Atlantic...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: A. Sanchez‐Franks, N. P. Holliday, D. G. Evans, N. Fried, O. Tooth, L. Chafik, Y. Fu, F. Li, M. F. deJong, H. L. Johnson
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2024
Subjects:
Online Access:https://doi.org/10.1029/2024GL108457
https://doaj.org/article/b334a11282db45cb9ca0dac015fb9537