Abstract
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Within our study of the plausibility of a subglacial lake under the Amundsenisen Icefield in Southern Spitzbergen, Svalbard achipelago (Glowacki et al., 2007), here we focus on the sensitivity of the system to the thermal effect of the firn and snow layers. Rough heat balance analysis shows that the firn layer plays an important role by driving the heat release to the atmosphere, so that its influence on the ice-water phase transition cannot be neglected (Bucchignani et al., 2012). | |
International
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Si |
Congress
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European Geosciences Union General Assembly 2013 |
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960 |
Place
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Viena, Austria |
Reviewers
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Si |
ISBN/ISSN
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1607-7962 |
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Start Date
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07/04/2013 |
End Date
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12/04/2013 |
From page
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1 |
To page
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1 |
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Geophysical Research Abstracts, Vol. 15, EGU2013-9289, 2013. |