Evaluating transience of a potential geothermal flux anomaly beneath a tributary ice stream of Thwaites Glacier, West Antarctica
The Amundsen Sea Embayment of the West Antarctic ice sheet (WAIS) is currently one of the most rapidly changing sectors of a continental ice sheet. As a marine ice sheet, the WAIS is in a potentially unstable configuration. A model is proposed to evaluate the effect of geothermal flux on flow in ice...
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| Other Authors: | , |
| Format: | Thesis |
| Language: | English |
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2013
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| Online Access: | http://hdl.handle.net/2152/20103 |