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...
Main Authors: | , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus Publications
2022
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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 |