Physics
Scientific paper
Dec 2002
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002agufm.p72a0492k&link_type=abstract
American Geophysical Union, Fall Meeting 2002, abstract #P72A-0492
Physics
5464 Remote Sensing, 5470 Surface Materials And Properties, 6225 Mars
Scientific paper
Analyses of TES-based bolometric albedo, thermal inertia, and spectral emissivity-derived hematite index for the Hematite region in Terra Meridiani (centered at 1.5 deg S and 3.0 deg W) indicate the terrain to be homogenous at resolutions of 3 km per pixel. In contrast, MOC NA frames with a maximum resolution of ~1.5 meters per pixel show that though the Hematite region is composed primarily of smooth, dark, pervasive dune-forms, there are also exposures of a ubiquitous bright material. This high albedo etched unit is interpreted to be a resistant substrate that extends beyond the borders of the overlying hematite-bearing plains. In order to quantify the relative superficial abundance of bright substrate and dark plains, we conduct high-resolution mapping of the hematite-bearing unit using MOC NA frames processed to ISIS level 2 (map projected with units proportional to radiance on sensor). As an illustrative example, MOC NA E03-01763 exhibits the etched unit in three typical settings: young crater rims, older craters which have lost much of their topographic signature but retain bright rims, and intercrater plains underlying dark, motley dunes. By area, 9.1% of the frame consists of bright material distributed uniformly across the scene. In general, MOC frames from the Hematite unit exhibit bright materials with an areal coverage ranging from 3% to 12%. This analysis demonstrates that the Mars Exploration Rover will be able to perform in-situ analyses of both the dark, hematite-bearing plains and the bright substrate over the course of the primary 90 sol mission.
Arvidson Ray E.
Koeppen William C.
Seelos Frank P.
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