Mars 5, 68-75, 2010 | doi:10.1555/mars.2010.0003
Received March 11, 2010 | Accepted July 23, 2010 | Published August 3, 2010
A comparison of Viking and Phoenix surface pressure data on Mars shows an increase in atmospheric mass that is consistent with that estimated to be eroding from the south polar residual cap. However, the increase does not rise above the uncertainties in the data.
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