Error sources in basal yield stress inversions for Jakobshavn Isbræ, Greenland, derived from residual patterns of misfit to observations

The basal interface of glaciers is generally not directly observable. Geophysical inverse methods are therefore used to infer basal parameters from surface observations. Such methods can also provide information about potential inadequacies of the forward model. Ideally an inverse problem can be reg...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: MARIJKE HABERMANN, MARTIN TRUFFER, DAVID MAXWELL
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2017
Subjects:
Online Access:https://doi.org/10.1017/jog.2017.61
https://doaj.org/article/a535d76128074176b5af29f0ffc7f7c1