The Nordic Seas overturning is modulated by northward-propagating thermohaline anomalies

Abstract The inflow of warm waters into the Nordic Seas, crucial for sustaining the climate-regulating Atlantic overturning circulation, can be reconstructed from hydrography using a north-south dynamic height gradient across the Greenland-Scotland Ridge. Variations in this influx are herein linked...

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Bibliographic Details
Main Authors: Léon Chafik, Marius Årthun, Helene R. Langehaug, Johan Nilsson, Thomas Rossby
Format: Article
Language:English
Published: Nature Portfolio 2025-07-01
Series:Communications Earth & Environment
Online Access:https://doi.org/10.1038/s43247-025-02557-x
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