Intensification and shutdown of deep convection in the Labrador Sea were caused by changes in atmospheric and freshwater dynamics
Abstract Labrador Sea winter convection forms a cold, fresh and dense water mass, Labrador Sea Water, that sinks to the intermediate and deep layers and spreads across the ocean. Convective mixing undergoes multi-year cycles of intensification (deepening) and relaxation (shoaling), which have been a...
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| Materiálatiipa: | Artihkal |
| Giella: | English |
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Nature Portfolio
2024-03-01
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| Ráidu: | Communications Earth & Environment |
| Liŋkkat: | https://doi.org/10.1038/s43247-024-01296-9 |