Carbon cycle implications of terrestrial weathering changes since the last glacial maximum

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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Bibliographic Details
Main Authors: M.-O. Brault, L.A. Mysak, H.D. Matthews
Format: Article
Language:English
Published: Canadian Science Publishing 2017-03-01
Series:FACETS
Subjects:
deglacial climate change
paleoclimatology
climate modeling
biogeochemistry
weathering
Online Access:http://www.facetsjournal.com/doi/10.1139/facets-2016-0040

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http://www.facetsjournal.com/doi/10.1139/facets-2016-0040

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