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The visible surface albedo of the martian residual south polar cap is an important parameter with respect to understanding the stability and evolution of the cap, as well as for investigating the interactions between the surface of the cap and the atmosphere. Extraction of the surface albedo from spacecraft images requires the removal of atmospheric effects, caused primarily by dust aerosols. Such...
The Mars Color Imager (MARCI) camera on the Mars Reconnaissance Orbiter provides daily synoptic coverage that allows monitoring of seasonal cap retreat and interannual changes that occur between Mars Years (MY) and over the southern summer. We present the first analysis of this data for the southern seasonal cap evolution observed in MY 28, 29, 30 and 31 (2/2007 to 07/2013). Observation over multiple...
Erosion of pits in the residual south polar cap (RSPC) of Mars concurrent with deposition and fluctuating cap boundaries raises questions about the mass balance and long term stability of the cap. Determining a mass balance by measurement of a net gain or loss of atmospheric CO2 by direct pressure measurements (Haberle, R.M. et al. [2014]. Secular climate change on Mars: An update using one Mars year...
The MARCI camera on the Mars Reconnaissance Orbiter provides daily synoptic coverage that allows monitoring of seasonal cap retreat and interannual changes that occur between Mars year (MY) and over the northern summer. The northern seasonal cap evolution was observed in MY 29, 30 and 31 (12/2007–04/2012). Observation over multiple Mars years allows us to compare changes between years as well as longer-term...
The residual south polar cap (RSPC) of Mars has been subject to competing processes during recent Mars years of high resolution image coverage: continuing erosion of scarps while the maximum extent grows as well as shrinks (Piqueux, S., Christensen, P.R. [2008]. J. Geophys. Res. (Planets) 113, 2006; James, P.B., Thomas, P.C., Malin, M.C. [2010]. Icarus 208, 82–85). Additionally, the cap has a variety...
We have used Mars Reconnaissance Orbiter data from 2007 and 2009 to compare summer behaviors of the seasonal and residual south polar caps of Mars in those two years. We find that the planet-encircling dust storm that occurred in the first of the two Mars years enhanced the loss of seasonal CO 2 deposits relative to the second year but did not have a large effect on the continuing erosion...
The residual south polar cap (RSPC) of Mars includes a group of different depositional units of CO 2 ice undergoing a variety of erosional processes. Complete summer coverage of the RSPC by ∼6-m/pixel data of the Context Imager (CTX) on Mars Reconnaissance Orbiter (MRO) has allowed mapping and inventory of the units in the RSPC. Unit maps and estimated thicknesses indicate the total volume...
The south residual polar cap of Mars, rich in CO 2 ice, is compositionally distinct from the north residual cap which is dominantly H 2 O ice. The south cap is also morphologically distinct, displaying a bewildering variety of depressions formed in thin layered deposits, which have been observed to change by scarp retreat over an interval of one Mars year (Malin et al., 2001, Science...
The seasonal CO 2 cycle on Mars refers to the exchange of carbon dioxide between dry ice in the seasonal polar caps and gaseous carbon dioxide in the atmosphere. This review focuses on breakthroughs in understanding the process involving seasonal carbon dioxide phase changes that have occurred as a result of observations by Mars Global Surveyor.
MOC wide-angle cameras routinely produce daily global maps of Mars in two colors at ~7.5 km/pixel resolution. These images have been used to study several seasonal phenomena linked to atmospheric processes and condensate cycles: dust storms, clouds, and polar recessions. Preliminary results of observations of polar caps and dust storms are presented here.
Content addressable memories are important components in high-speed networking equipment. This paper describes the design of a wide CAM suitable for use as an IPv6 traffic classifier for a 622Mb/s communications link. The design flow uses a combination of standard design tools in conjunction with JBits, a low-level configuration API for manipulating programmable resources. The CAMs are 320 bits wide...
The combined analysis of microwave temperature and water profiling of the Mars atmosphere indicates that low- to mid-latitude water vapor saturation typically occurs at much lower altitudes (below 10 km) during northern spring/summer than observed during this Mars aphelion season in the dusty, warm period of Viking observations (above 25 km). Temperatures profiles of the 0–60 km global Mars atmosphere...
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