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

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 glacier velo...

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Bibliographic Details

Published in:	Journal of Glaciology
Main Authors:	William H. Armstrong, Robert S. Anderson
Format:	Article
Language:	English
Published:	Cambridge University Press 2020-10-01
Subjects:	Arctic glaciology glacier hydrology ice velocity subglacial processes
Online Access:	https://www.cambridge.org/core/product/identifier/S0022143020000416/type/journal_article