Enhanced vertical mixing in the glacial ocean inferred from sedimentary carbon isotopes
Vertical mixing in the Atlantic Ocean during the Last Glacial Maximum may have been enhanced, not reduced, due to more vigorous tidal dissipation, suggest an ensemble of ocean simulations and glacial sediment carbon isotope records.
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| Autores principales: | , , |
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| Formato: | article |
| Lenguaje: | EN |
| Publicado: |
Nature Portfolio
2021
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| Materias: | |
| Acceso en línea: | https://doaj.org/article/44d05e95e5794c39974bc239eef7ad1d |
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