Simultaneous Determination of Dry-Layer Thickness and Sub-Surface Ice Content in the Polar Regions of Mars: Implications for the Phoenix Landing Site Selection

Details Simultaneous Determination of Dry-Layer Thickness and Sub-Surface Ice Content in the Polar Regions of Mars: Implications for the Phoenix Landing Site Selection Simultaneous Determination of Dry-Layer Thickness and Sub-Surface Ice Content in the Polar Regions of Mars: Implications for the Phoenix Landing Site Selection

Mar 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpi....37.2376b&link_type=abstract

37th Annual Lunar and Planetary Science Conference, March 13-17, 2006, League City, Texas, abstract no.2376

Physics

2

Scientific paper

By combining data from Si and H gamma rays from the polar regions, we
can determine both the ice content of a sub-surface ice-rich layer and
the thickness of an ice-free overlying layer. The dry layer is very thin
at the Phoenix landing sites.

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