Climatic response to Milankovitch forcing as simulated by a zonally averaged ocean-atmosphere-sea ice model
A reduced complexity ocean-atmosphere-sea ice model is developed to study the transient response of climate to Milankovitch forcing. The ocean component is a zonally averaged model of the meridional overturning circulation in different basins. The atmospheric component is a one-dimensional...
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| Format: | Others |
| Language: | en |
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McGill University
2009
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| Online Access: | http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=66828 |