Modelled ocean changes at the Plio-Pleistocene transition driven by Antarctic ice advance
Global deep water mass properties converged in the North Pacific and Atlantic oceans during the Pliocene-Pleistocene. Here, using a coupled ocean-atmosphere climate model, the authors show that a reduction in coastal ice in the Pacific sector of Antarctica was likely responsible for this change.
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| Autores principales: | , , |
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| Formato: | article |
| Lenguaje: | EN |
| Publicado: |
Nature Portfolio
2017
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| Materias: | |
| Acceso en línea: | https://doaj.org/article/2587fadd10274af0beb6019ae4400086 |
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