Spatial variability in the seasonal south polar CAP of Mars

Details Spatial variability in the seasonal south polar CAP of Mars Spatial variability in the seasonal south polar CAP of Mars

Oct 1994

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1994jgr....9921143c&link_type=abstract

Journal of Geophysical Research (ISSN 0148-0227), vol. 99, no. E10, p. 21,143-21,152

Astronomy and Astrophysics

Astronomy

28

Astronomical Models, Astronomical Spectroscopy, Carbon Dioxide, Ice, Infrared Astronomy, Infrared Photography, Infrared Spectra, Mars (Planet), Mars Photographs, Planetary Composition, Polar Caps, Spaceborne Astronomy, Absorption Spectra, Annual Variations, Infrared Spectrometers, Infrared Spectroscopy, Mariner 7 Space Probe, Mathematical Models, Spectral Reflectance

Scientific paper

The first comprehensive discussion of the south seasonal polar cap spectra obtained by the Mariner 7 infrared spectrometer in the short-wavelength region (2-4 microns) is presented. The infrared spectra is correlated with images acquired by the wide-angle camera. Significant spectral variation is noted in the cap interior and regions of varying water frost abundance, CO2 ice/frost cover, and CO2-ice path length can be distinguished. Many of these spectral variations correlate with heterogeneity noted in the camera images, but certain significant infrared spectral variations are not discernible in the visible. Simple reflectance models are used to classify the observed spectral variations into four regions. Region I is at the cap edge, where there is enhanced absorption beyond 3 microns inferred to be caused by an increased abundance of water frost. The increase in water abundance over that in the interior is on the level of a few parts per thousand or less. Region II is the typical cap interior characterized by spectral features of CO2 ice at grain sizes of several millimeters to centimeters. These spectra also indicate the presence of water frost at the parts per thousand level. A third, unusual region (III), is defined by three spectra in which weak CO2 absorption features are as much as twice as strong as in the average cap spectra and are assumed to be caused by an increased path length in the CO2. Such large paths are inconsistent with the high reflectance in the visible and at 2.2 microns and suggest layered structures or deposition conditions that are not accounted for in current reflectance models. The final region (IV) is an area of thinning frost coverage or transparent ice well in the interior of the seasonal cap. These spectra are a combination of CO2 and ground signatures.

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