Morainal Bank Evolution and Impact on Terminus Dynamics During a Tidewater Glacier Stillstand-Reference-Cited by-同舟云学术

Morainal Bank Evolution and Impact on Terminus Dynamics During a Tidewater Glacier Stillstand

Published:2020-10-26 Issue:11 Volume:125 Page:
ISSN:2169-9003
Container-title:Journal of Geophysical Research: Earth Surface
language:en
Short-container-title:J. Geophys. Res. Earth Surf.

Author:

Eidam E. F.¹^ORCID,Sutherland D. A.²^ORCID,Duncan D.³,Kienholz C.⁴^ORCID,Amundson J. M.⁴^ORCID,Motyka R. J.⁴⁵

Affiliation:

1. Department of Marine Sciences University of North Carolina at Chapel Hill Chapel Hill NC USA

2. Department of Earth Sciences University of Oregon Eugene OR USA

3. Institute for Geophysics University of Texas at Austin Austin TX USA

4. Department of Natural Sciences University of Alaska Southeast Juneau AK USA

5. Geophysical Institute University of Alaska Fairbanks Fairbanks AK USA

Funder

National Geographic Society

National Science Foundation of Sri Lanka

Publisher

American Geophysical Union (AGU)

Subject

Earth-Surface Processes,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019JF005359

Reference110 articles.

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2. Sedimentary processes may cause fluctuations of tidewater glaciers

3. Till beneath ice stream B: 3. Till deformation: Evidence and implications

4. A mass-flux perspective of the tidewater glacier cycle

5. Amundson J. Kienholz C. Motyka R. Sutherland D. Nash J. Jackson R. &Carroll D.(2017).Collaborative research: Impact of subglacial discharge on turbulent plume dynamics and ocean‐glacier heat and mass transfer Southeast Alaska 2016–2017 Arctic Data Center.https://doi.org/10.18739/A22G44

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