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Reduced basal motion responsible for 50 years of declining ice velocities on Athabasca Glacier

The time-evolution of glacier basal motion remains poorly constrained, despite its importance in understanding the response of glaciers to climate warming. Athabasca Glacier provides an ideal site for observing changes in basal motion over long timescales. Studies from the 1960s provide an in situ b...

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Autors principals: David Polashenski, Martin Truffer, William Henry Armstrong
Format: Artigo
Idioma:Inglês
Publicat: Cambridge University Press 2024-01-01
Col·lecció:Journal of Glaciology
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Accés en línia:https://www.cambridge.org/core/product/identifier/S0022143024000510/type/journal_article
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