Mixing and air-sea buoyancy fluxes set the time-mean overturning circulation in the subpolar North Atlantic

The overturning streamfunction as measured at the OSNAP (Overturning in the Subpolar North Atlantic Program) mooring array represents the transformation of warm/salty Atlantic Water into cold/fresh North Atlantic Deep Water (NADW). The magnitude of the overturning at the OSNAP mooring array can ther...

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Bibliographic Details
Main Authors: Evans, D. Gwyn, Holliday, N. Penny, Bacon, Sheldon, Le Bras, Isabela
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2022
Subjects:
Online Access:https://doi.org/10.5194/egusphere-2022-1059
https://noa.gwlb.de/receive/cop_mods_00062892
https://egusphere.copernicus.org/preprints/egusphere-2022-1059/egusphere-2022-1059.pdf