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Seasonality of meridional overturning in the subpolar North Atlantic: implications for relying on the streamfunction maximum as a metric of AMOC slowdown (2025)

First Author: Fox A

Attributed to: The UK Overturning in the Subpolar North Atlantic Program (UK-OSNAP) funded by NERC

Abstract

No abstract provided

Bibliographic Information

Digital Object Identifier: http://dx.doi.org/10.5194/egusphere-2025-616

Publication URI: http://dx.doi.org/10.5194/egusphere-2025-616

Type: Preprint