Stratification and overturning circulation are intertwined controls on ocean heat uptake efficiency in climate models
<p>The global ocean takes up over 90 % of the excess heat added to the climate system due to anthropogenic emissions, thereby buffering climate change at Earth's surface. A key metric for quantifying the role of the oceanic processes removing this heat from the atmosphere and storing it i...
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| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2025-06-01
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| Series: | Ocean Science |
| Online Access: | https://os.copernicus.org/articles/21/1081/2025/os-21-1081-2025.pdf |
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