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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| Autori principali: | , , |
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| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
Cambridge University Press
2024-01-01
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| Serie: | Journal of Glaciology |
| Soggetti: | |
| Accesso online: | https://www.cambridge.org/core/product/identifier/S0022143024000510/type/journal_article |
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