The seasonal behavior of water ice clouds in the Tharsis and Valles Marineris regions of Mars: Mars Orbiter Camera Observations

• Published in: Icarus (New York, N.Y. 1962) N.Y. 1962), 2003-09, Vol.165 (1), p.34-52
• Main Authors: Benson, Jennifer L., Bonev, Boncho P., James, Philip B., Shan, Kathy J., Cantor, Bruce A., Caplinger, Michael A.
• Format: Article
• Language: English
• Subjects: Mars; Mars atmosphere
• ISSN: 0019-1035; 1090-2643
• DOI: 10.1016/S0019-1035(03)00175-1

The Mars Global Surveyor Mars Orbiter Camera was used to obtain global maps of the martian surface with equatorial resolution of 7.5 km/pixel in two wavelength ranges: blue (400–450 nm) and red (575–625 nm). The maps used were acquired between March 15, 1999 ( L s =110°) and July 31, 2001 ( L s =205°), corresponding to approximately one and a quarter martian years. Using the global maps, cloud area (in km 2) has been measured daily for water ice clouds topographically corresponding to Olympus Mons, Ascraeus Mons, Pavonis Mons, Arsia Mons, Alba Patera, the western Valles Marineris canyon system, and for other small surface features in the region. Seasonal trends in cloud activity have been established for the three Tharsis volcanoes, Olympus Mons, and Alba Patera. Olympus, Ascraeus, and Pavonis Mons show cloud activity from about L s =0°–220° with a peak in cloud area near L s =100°. One of our most interesting observational results is that Alba Patera shows a double peaked feature in the cloud area with peaks at L s =60° and 140° and a minimum near L s =100°. Arsia Mons shows nearly continuous cloud activity. The altitudes of several of these clouds have been determined from the locations of the visual cloud tops, and optical depths were measured for a number of them using the DISORT code of Stamnes et al. (1988, Appl. Opt. 27, 2502–2509). Several aspects of the observations (e.g., cloud heights, effects of increased dust on cloud activity) are similar to simulations in Richardson et al. (2002, J. Geophys. Res. 107, 5064). A search for short period variations in the cloud areas revealed only indirect evidence for the diurnal cloud variability in the afternoon hours; unambiguous evidence for other periodicities was not found.