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Cryosphere: Antarctic ice growth and retreat

By Jeff Evans

Abstract

Antarctic Ice Sheet change during the last glacial cycle is unclear. The timing of moraine development in the Ross basin suggests that the ice sheet reached maximum thickness under the warming temperatures of the last termination

Publisher: © Nature Publishing Group
Year: 2015
DOI identifier: 10.1038/ngeo2494
OAI identifier: oai:dspace.lboro.ac.uk:2134/18720
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