A sublimation model for martian south polar ice features

Science. 2003 Feb 14;299(5609):1051-3. doi: 10.1126/science.1080148.

Abstract

In their pioneering work, Leighton and Murray argued that the Mars atmosphere, which at present is 95% carbon dioxide, is controlled by vapor equilibrium with a much larger polar reservoir of solid carbon dioxide. Here we argue that the polar reservoir is small and cannot function as a long-term buffer to the more massive atmosphere. Our work is based on modeling of the circular depressions commonly found on the south polar cap. We argue that a carbon dioxide ice layer about 8 meters thick is being etched away to reveal water ice underneath. This is consistent with thermal infrared data from the Mars Odyssey mission.

Publication types

  • Research Support, U.S. Gov't, Non-P.H.S.

MeSH terms

  • Atmosphere
  • Carbon Dioxide
  • Dry Ice*
  • Ice*
  • Mars*
  • Models, Theoretical*
  • Seasons
  • Temperature
  • Water

Substances

  • Dry Ice
  • Ice
  • Water
  • Carbon Dioxide