Rapid global ocean-atmosphere response to Southern Ocean freshening during the last glacial
<p>Contrasting Greenland and Antarctic temperatures during the last glacial period (115,000 to 11,650 years ago) are thought to have been driven by imbalances in the rates of formation of North Atlantic and Antarctic Deep Water (the ‘bipolar seesaw’). Here we exploit a bidecadally-resolved &l...
| Main Authors: | , , , , |
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| 格式: | Journal article |
| 出版: |
Nature Publishing Group
2017
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