Simulation of ocean-ice sheet interactions during the last deglaciation
[1] The last deglaciation, between 21 thousand years BP (kyr BP) and 8 kyr BP, was punctuated by a series of climatic oscillations, both in the Northern and Southern Hemispheres, often attributed to changes in ocean circulation. These oscillations are explored with an Earth system model of intermedi...
Published in: | Paleoceanography |
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Main Authors: | , |
Other Authors: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Amer Geophysical Union
2002
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Subjects: | |
Online Access: | http://hdl.handle.net/2078.1/41249 https://doi.org/10.1029/2001PA000702 |