Ice-marginal lake hydrology and the seasonal dynamical evolution of Kennicott Glacier, Alaska

Abstract Glacier basal motion is responsible for the majority of ice flux on fast-flowing glaciers, enables rapid changes in glacier motion and provides the means by which glaciers shape alpine landscapes. In an effort to enhance our understanding of basal motion, we investigate the evolution of gla...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Armstrong, William H., Anderson, Robert S.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2020
Subjects:
Online Access:http://dx.doi.org/10.1017/jog.2020.41
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143020000416