Oscillatory sensitivity of Atlantic overturning to high-latitude forcing
The Atlantic Meridional Overturning Circulation (AMOC) carries warm upper waters into northern high-latitudes and returns cold deept waters southward. Under anthropogenic greenhouse gas forcing the AMOC is expected to weaken due to high-latitude warming and freshening. Here, we show that the sensiti...
| Main Authors: | , , |
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| 格式: | Journal article |
| 语言: | English |
| 出版: |
American Geophysical Union
2010
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