Transient overturning changes cause an upper-ocean nutrient decline in a warming climate
Abstract Models and proxy data suggest multi-centennial nutrient reorganization and biological productivity changes under sustained climate warming. These changes have traditionally been attributed to processes in the Southern Ocean. Here we instead show that transient overturning circulation adjust...
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| Principais autores: | , , , |
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| Format: | Artigo |
| Sprog: | Inglês |
| Udgivet: |
Nature Portfolio
2024-09-01
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| Serier: | Nature Communications |
| Online adgang: | https://doi.org/10.1038/s41467-024-52200-0 |
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