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On the role of thermohaline advection and sea ice in glacial transitions

✍ Scribed by Kravtsov, S.


Book ID
119658607
Publisher
American Geophysical Union
Year
2003
Tongue
English
Weight
591 KB
Volume
108
Category
Article
ISSN
0148-0227

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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