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Simulation of the last glacial inception and rapid ice sheet growth in the McGill Paleoclimate Model

โœ Scribed by Wang, Zhaomin

Book ID
119657358
Publisher
American Geophysical Union
Year
2002
Tongue
English
Weight
328 KB
Volume
29
Category
Article
ISSN
1944-8007

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A fully integrated ice-sheet and glacio-isostatic numerical model was run in order to investigate the crustal response to ice loading during the Late Weichselian glaciation of the Barents Sea. The model was used to examine the hypothesis that relative reductions in water depth, caused by glacio-isos