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 array can therefore...

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Bibliographic Details
Main Authors: Evans, D. Gwyn, Holliday, N. Penny, Bacon, Sheldon, Bras, Isabela
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/egusphere-2022-1059
https://egusphere.copernicus.org/preprints/2022/egusphere-2022-1059/