Declining Basal Motion Dominates the Long‐Term Slowing of Athabasca Glacier, Canada-Reference-Cited by-同舟云学术

Declining Basal Motion Dominates the Long‐Term Slowing of Athabasca Glacier, Canada

Published:2022-10 Issue:10 Volume:127 Page:
ISSN:2169-9003
Container-title:Journal of Geophysical Research: Earth Surface
language:en
Short-container-title:JGR Earth Surface

Author:

Armstrong William H.¹^ORCID,Polashenski David²,Truffer Martin²^ORCID,Horne Greg³,Hanson Jacob B.¹,Hawley Robert L.⁴^ORCID,Hengst Anthony M.¹,Vowels Lily¹^ORCID,Menounos Brian⁵^ORCID,Wychen Wesley Van⁶

Affiliation:

1. Department of Geological and Environmental Sciences Appalachian State University Boone NC USA

2. Geophysical Institute University of Alaska Fairbanks Fairbanks AK USA

3. Jasper National Park Jasper AB Canada

4. Department of Earth Sciences Dartmouth College Hanover NH USA

5. Department of Geography, Earth, and Environmental Sciences University of Northern British Columbia Prince George BC Canada

6. Department of Geography and Environmental Management University of Waterloo Waterloo ON Canada

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Earth-Surface Processes,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021JF006439

Reference115 articles.

1. Softening of Temperate Ice by Interstitial Water

2. Improvements to shear-deformational models of glacier dynamics through a longitudinal stress factor

3. Parameterization of lateral drag in flowline models of glacier dynamics

4. Stabilizing feedbacks in glacier-bed erosion

5. Time-dependent basal stress conditions beneath Black Rapids Glacier, Alaska, USA, inferred from measurements of ice deformation and surface motion

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