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

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
Published in:Ocean Science
Main Authors: D. G. Evans, N. P. Holliday, S. Bacon, I. Le Bras
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2023
Subjects:
G
Online Access:https://doi.org/10.5194/os-19-745-2023
https://doaj.org/article/b9a9cf58f31646929c6d36608368a021