Ice Stream C slowdown is not stabilizing West Antarctic Ice Sheet
Changes in the flow of ice stream C likely indicate a continuing slow drawdown of the Siple Coast of West Antarctica rather than a stabilizing feedback. The downglacier part of ice stream C, West Antarctica largely stagnated over the last few centuries, while upglacier regions continue to flow vigor...
Main Authors: | , , , |
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Format: | Text |
Language: | English |
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1999
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.366.9711 http://www.stolaf.edu/other/cegsic/publications/Anandakrishnan et al.pdf |