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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| Auteurs principaux: | , , , , |
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| Format: | Artigo |
| Langue: | Inglês |
| Publié: |
Nature Portfolio
2025-07-01
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| Collection: | Communications Earth & Environment |
| Accès en ligne: | https://doi.org/10.1038/s43247-025-02557-x |
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