The Coldest and Densest Overflow Branch Into the North Atlantic is Stable in Transport, But Warming

The overflow of cold water through the Faroe Bank Channel (FBC) is the densest water crossing the Greenland-Scotland Ridge and the densest source for the Atlantic Meridional Overturning Circulation (AMOC). Here, we show that the overflow volume transport remained stable from 1996 to 2022, but that t...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Larsen, Karin Margretha Húsgarð, Hansen, Bogi, Hátún, Egil Hjálmar, Johansen, Guðrið Eriksdóttir, Østerhus, Svein, Olsen, Steffen Malskær
Format: Article in Journal/Newspaper
Language:English
Published: 2024
Subjects:
Online Access:https://hdl.handle.net/11250/3151641
https://doi.org/10.1029/2024GL110097