Thermal regime in steep permafrost rockwalls (Aiguille du Midi, 3842 m a.s.l., Mont Blanc massif) based on borehole data and 2D numerical modelling

Since permafrost in steep rockwalls is mainly climatically controlled, the ongoing climate warming potentially strongly impacts frequency and magnitude of rockfalls in high-alpine rock faces in the near future. However, knowledge about the role of permafrost is still limited. This is especially beca...

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Bibliographic Details
Main Authors: Magnin, Florence, Deline, Philip, Ravanel, Ludovic, Noetzli, Jeannette
Other Authors: Environnements, Dynamiques et Territoires de Montagne (EDYTEM), Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS), Glaciology, Geomorphodynamics and Geochronology, Department of Geography Zürich, Universität Zürich Zürich = University of Zurich (UZH)-Universität Zürich Zürich = University of Zurich (UZH)
Format: Conference Object
Language:English
Published: HAL CCSD 2012
Subjects:
Online Access:https://hal.science/halsde-00878144