Mid‐Holocene Grounding Line Retreat and Readvance at Whillans Ice Stream, West Antarctica-Reference-Cited by-同舟云学术

Mid‐Holocene Grounding Line Retreat and Readvance at Whillans Ice Stream, West Antarctica

Published:2020-08-07 Issue:15 Volume:47 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Venturelli R. A.¹^ORCID,Siegfried M. R.²³^ORCID,Roush K. A.⁴,Li W.⁴,Burnett J.⁵,Zook R.⁶,Fricker H. A.³^ORCID,Priscu J. C.⁴^ORCID,Leventer A.⁷^ORCID,Rosenheim B. E.¹^ORCID

Affiliation:

1. College of Marine Science University of South Florida St. Petersburg FL USA

2. Department of Geophysics Colorado School of Mines Golden CO USA

3. Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography University of California, San Diego La Jolla CA USA

4. Department of Land Resources and Environmental Science Montana State University Bozeman MT USA

5. Applied Physics Laboratory University of Washington Seattle WA USA

6. University of Nebraska–Lincoln Lincoln NE USA

7. Department of Geology Colgate University Hamilton NY USA

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020GL088476

Reference87 articles.

1. Water-Pressure Coupling of Sliding and Bed Deformation: I. Water System

2. Effect of Sedimentation on Ice-Sheet Grounding-Line Stability

3. Deformation of till beneath ice stream B, West Antarctica

4. Discovery of Till Deposition at the Grounding Line of Whillans Ice Stream

5. Ross Sea paleo-ice sheet drainage and deglacial history during and since the LGM

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