De. Smith et Mt. Zuber, The relationship between MOLA northern hemisphere topography and the 6.1-Mbar atmospheric pressure surface of Mars, GEOPHYS R L, 25(24), 1998, pp. 4397-4400
To assist in targeting of landers and to enable comparison of new elevation
data to previous topography models, we have re-determined the position of
the 6.1-mbar atmospheric pressure surface on Mars with respect to surface t
opography from the Mars Orbiter Laser Altimeter (MOLA). The 6.1-mbar surfac
e lies, on average, 1600 m below the geoid-defined zero level of MOLA topog
raphy, which occurs at an average pressure of 5.2 mbars at L-S=0 degrees. T
he elevation of the 6.1-mbar surface is expected to vary by 1.5-2.5 km over
the Martian year due to the seasonal exchange of CO2 between the atmospher
e and polar caps. For average Martian atmospheric conditions, the pressure
at the Mars Surveyor '98 landing site is expected to be similar to 5.0 mbar
s during the lander science phase of the mission assuming an elevation of 1
600 meters above the zero level defined by MOLA topography.