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Antarctic sea ice control on ocean circulation in present and glacial climates
In the modern climate, the ocean below 2 km is mainly filled by waters sinking into the abyss around Antarctica and in the North Atlantic. Paleoproxies indicate that waters of North Atlantic origin were instead absent below 2 km at the Last Glacial Maximum, resulting in an expansion of the volume oc...
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| Autors principals: | , , , , , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
National Academy of Sciences
2014
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4066517/ https://ncbi.nlm.nih.gov/pubmed/24889624 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1323922111 |
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