PFS-MEX observation of ices in the residual south polar cap of Mars

Abstract

The Mars Express spacecraft has a highly inclined orbit around Mars and so has been able to observe the south pole of Mars in illuminated conditions at the end of the southern summer ( L s = 330 ). Spectra from the planetary Fourier spectrometer (PFS) short wavelength (SW) channel were recorded over the permanent ice cap to study its composition in terms of CO 2 ice and H 2O ice. Models are fitted to the observed data, which include a spatial mixture of soil (not covered by ice) and CO 2 frost (with a specific grain size and a small amount of included dust and H 2O ice). Two different kinds of spectra were observed: those over the permanent polar cap with almost pure CO 2 ice, negligible water ice, no soil fraction required, and bright; and those over mixed terrain (at the edge of the cap or near troughs) containing a significant soil spatial fraction, more water ice and smaller CO 2 grain size. The amount of water ice given by fits to scaled albedo models is less than 10 ppm by weight. When using multi-stream reflectance models with the appropriate lighting geometry, the water amount must be 2–5 times greater than the albedo fit (less than 50 ppm). At the periphery of the residual polar cap, we found a region almost completely covered by water frost, modeled as a mixture of micron-sized and sub-mm sized grains. Our result using a granular mixture of micron-sized grains of water ice and dust with the CO 2 grains is different from the modeling of OMEGA polar cap observations using molecular mixtures.