Observational verification of predicted increase in bedrock-to-surface amplitude transfer during a glacier surge

The amplitude ratio between surface and bedrock topography has been predicted to depend strongly on the ratio of deformational velocity to mean basal sliding velocity. Observations made prior to and during a surge of Tungnaárjökull, Vatnajökull ice cap, Iceland, allow this prediction to be tested. D...

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Bibliographic Details
Published in:Annals of Glaciology
Main Authors: Gudmundsson, Hilmar, Aðalgeirsdóttir, Guðefinna, Björnsson, Helgi
Format: Article in Journal/Newspaper
Language:unknown
Published: International Glaciological Society 2003
Subjects:
Online Access:https://nrl.northumbria.ac.uk/id/eprint/38010/
https://doi.org/10.3189/172756403781816248