Abstract

Measurements of the radius of Mars obtained using Earth-based telescopic measurements between 1879 and 1958 determined the altitude in the atmosphere at which the line-of-sight opacity was unity. These data can be used to estimate the dust content of the martian atmosphere during that time period. Comparison with the distribution of brightness seen in images of the limb from the Mariner 9 and Viking spacecraft suggests that the dust content prior to 1956 was substantially less than during the 1970s. In addition, the dust content in the polar regions was substantially less than in the equatorial regions. These data suggest that there is significant variability of the dust cycle on decade- or century-long time scales. The atmospheric behavior seen by Viking appears to represent an extreme behavior rather than one typical or representative of the present epoch.

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