Sublimation-Dominated Active Layers in the Highlands of the Antarctic Dry Valleys and Implications for Other Sites

Details Sublimation-Dominated Active Layers in the Highlands of the Antarctic Dry Valleys and Implications for Other Sites Sublimation-Dominated Active Layers in the Highlands of the Antarctic Dry Valleys and Implications for Other Sites

Mar 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011lpi....42.2644m&link_type=abstract

42nd Lunar and Planetary Science Conference, held March 7–11, 2011 at The Woodlands, Texas. LPI Contribution No. 1608, p.2644

Physics

Scientific paper

The high-elevation Antarctic Dry Valleys represent an extremely cold and
dry environment where subsurface liquid water is not present. Field
observations and data are used to characterize and model this system, as
well as alpine regions on Earth and Mars.

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