An enhanced model of the contemporary and long-term (200 ka) sublimation of the massive subsurface ice in Beacon Valley, Antarctica-Reference-Cited by-同舟云学术

An enhanced model of the contemporary and long-term (200 ka) sublimation of the massive subsurface ice in Beacon Valley, Antarctica

Author:

Liu Lu¹,Sletten Ronald S.¹,Hagedorn Birgit²,Hallet Bernard¹,McKay Christopher P.³,Stone John O.¹

Affiliation:

1. Department of Earth and Space Sciences; University of Washington; Seattle Washington USA

2. Environment and Natural Resources Institute; University of Alaska Anchorage; Anchorage Alaska USA

3. Space Science Division; NASA Ames Research Center; Moffett Field California USA

Funder

National Science Foundation

NASA Mars Science Laboratory

Publisher

American Geophysical Union (AGU)

Subject

Earth-Surface Processes,Geophysics

Link

Reference60 articles.

1. An Antarctic analog of Martian permafrost terrain;Anderson;Antarct. J. U. S.,1972

3. Hydrothermal regimen of patterned ground, Victoria Land, Antarctica;Black;Int. Assoc. Sci. Hydrol. Comm. Snow Ice,1963

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