MOC observations of four Mars year variations in the south polar residual cap of Mars |
| |
| Authors: | Philip B James Peter C Thomas Michael J Wolff Boncho P Bonev |
| |
| Institution: | aSpace Science Institute, 4750 Walnut Street, Suite 205, Boulder, CO 80301, USA;bCenter for Radiophysics and Space Research, Cornell University, Ithaca, NY 14853, USA;cDepartment of Physics, The Catholic University of America, Washington, DC 20064, USA;dSolar System Exploration Division, Code 693, NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA |
| |
| Abstract: | The residual south polar cap of Mars (RSPC) is distinct from the residual north polar cap both in composition and in morphology. CO2 frost in the RSPC is stabilized by its high albedo during southern spring and summer despite the relatively large insolation during that period. The morphology of the RSPC in summer displays a bewildering variety of depressions that are formed in relatively thin layers of CO2. The increase of the size of these depressions between each of the first three years of Mars Global Surveyor (MGS) observations may possibly signal some sort of climate change on the planet. For example, the erosion of the bright plateaus might reduce the RSPC albedo and affect the energy balance. The Mars Orbiter Cameras (MOC) on MGS observed Mars for four consecutive martian years before contact with the spacecraft was lost in late 2006. During this period coverage of the polar regions was particularly dense because MGS flew over them on every orbit. In this paper we report on the four-year behavior of the morphological features in the RSPC and on the large-scale variability in RSPC albedo over the period. The changes in the size of the surface features in the RSPC due to backwasting that were first observed between Mars years (MY) 24 and 25 and subsequently between MY25 and M26 was observed to continue at the same rate through MY 27. The results indicate that on average thicker layers in the RSPC retreat faster than thinner ones, roughly in proportion to their thickness. We argue that a simple difference in porosity between the A and B layers can explain this difference although other factors could be involved. The large-scale albedo of the RSPC decreases as the depressions are uncovered by sublimation of seasonal CO2. However, any interannual differences in albedo due to the backwasting process are masked by interannual differences in the summer dust opacity in the RSPC region. |
| |
| Keywords: | Mars polar caps Mars polar geology Mars climate Mars atmosphere |
| 本文献已被 ScienceDirect 等数据库收录！ |
|
