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