Combining Viking pressure and temperature data with Mars Orbital Laser Alti
meter topography data, we have computed the fraction of the martian year du
ring which pressure and temperature allow for liquid water to be stable on
the martian surface. We find that liquid water would be stable within the H
ellas and Argyre basin and over the northern lowlands equatorward of about
40 degrees, The location with the maximum period of stable conditions for l
iquid water is in the southeastern portion of Utopia Planitia, where 34% of
the year liquid water would be stable if it were present. Locations of sta
bility appear to correlate with the distribution of valley networks.