W. Zeitler et J. Oberst, The shape of Mars before Global Surveyor: Results from reanalysis of the Viking control point network, J GEO R-PLA, 104(E6), 1999, pp. 14051-14063
Three-dimensional coordinates of 3739 globally distributed control points d
erived from photogrammetric analysis of Viking Orbiter image data are studi
ed with respect to the shape and large-scale morphology of Mars. Spheres, s
pheroids, spherical functions, and a Digital Terrain Model (DTM) of 50 km g
rid spacing are fitted to the data. Prominent topographic features in the t
errain model include the Tharsis volcanoes, Olympus Mons, Alba Patera and p
rominent mare and highland regions as well as the major impact basins. Whil
e the global dichotomy is clearly visible in our data, our model does not r
eveal any distinct signature associated with the presumed dichotomy boundar
y at this global scale. Rather, it suggests a smooth topographic transition
from southern to northern hemisphere. This model is unique among existing
topographic data sets for Mars, as it combines global coverage, a spatial r
esolution sufficient to resolve regional topography, and absolute elevation
data more accurate than in previous control point network analyses. Formal
errors and a comparison with the first released topographic profiles obtai
ned by Mars Global Surveyor's Laser Altimeter (MOLA) suggest that 70% and 9
0% of the DTM grid elements represent the topography of the planet to bette
r than 1000 m and 2000 m, respectively.