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.
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Nature Publishing Group
2017-03-01
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| Series: | Nature Communications |
| Online Access: | https://doi.org/10.1038/ncomms14376 |