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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Bibliographic Details
Published inPermafrost and periglacial processes Vol. 9; no. 1; pp. 23 - 33
Main Authors Wegmann, Matthias, Gudmundsson, G. Hilmar, Haeberli, Wilfried
Format Journal Article
LanguageEnglish
Published Chichester John Wiley & Sons, Ltd 01.01.1998
Wiley
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