The hemispherical asymmetry of the residual polar caps on Mars

Mathematics

Scientific paper

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Albedo, Diurnal Variations, Heat Transfer, Ice, Mars (Planet), Mars Surface, Mathematical Models, Polar Caps, Asymmetry, Carbon Dioxide, Frost, Solar Position, Zenith

Scientific paper

A model of the polar caps of Mars was created which allows: (1) for light penetration into the cap; (2) ice albedo to vary with age, latitude, hemisphere, dust content, and solar zenith angle; and (3) for diurnal variability. The model includes the radiative effects of clouds and dust, and heat transport as represented by a thermal wind. The model reproduces polar cap regression data very well, including the survival of CO2 frost at the south pole and reproduces the general trend in the Viking Lander pressure data.

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