Permafrost changes in rock walls and the retreat of alpine glaciers: a thermal modelling approach
The shrinkage of Grosser Aletschgletscher changed the thermal and mechanical boundary conditions in its marginal rock walls. The temperature at the glacier bed is at the pressure melting point while the exposed rock surface (above the glacier) is subject to atmospheric conditions. At our study site,...
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Published in | Permafrost and periglacial processes Vol. 9; no. 1; pp. 23 - 33 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
Chichester
John Wiley & Sons, Ltd
01.01.1998
Wiley |
Subjects | |
Online Access | Get full text |
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