Carbon cycle implications of terrestrial weathering changes since the last glacial maximum
We examine the importance of the rock weathering feedback mechanism during the last deglacial period (∼16 000-4000 BCE) using an Earth system model of intermediate complexity (the University of Victoria Earth System Climate Model (UVic ESCM)) with four box-model parameterizations of terrestrial weat...
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Format: | Book |
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Canadian Science Publishing,
2017-03-01T00:00:00Z.
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Internet
Connect to this object online.3rd Floor Main Library
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A1234.567 |
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Copy 1 | Available |