Earth responses to ice mass changing in iceland

The reological properties of the crust and the upper mantle beneath Iceland make the earth surface sensitive to recent ice mass changing. On a short time scale, strong correlation exists between seasonal variations in continuous GPS time series and snow covering. The overall retreat of Icelandic gla...

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Bibliographic Details
Main Author: Villemin, Thierry
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)
Format: Conference Object
Language:English
Published: HAL CCSD 2010
Subjects:
Online Access:https://hal.univ-brest.fr/hal-00482058
https://hal.univ-brest.fr/hal-00482058/document
https://hal.univ-brest.fr/hal-00482058/file/Villemin_resume.pdf
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Summary:The reological properties of the crust and the upper mantle beneath Iceland make the earth surface sensitive to recent ice mass changing. On a short time scale, strong correlation exists between seasonal variations in continuous GPS time series and snow covering. The overall retreat of Icelandic glaciers is causing uplift of over 2 cm/yr around Vatnajökull, the largest Icelandic ice cap. Recent modelling also suggests that the same phenomena is causing increased mantle melting and magma generation under Vatnajökull