The processing of Doppler data has been the primary method for deriving models of the Mars gravity field. Since the Mariner 9 and Viking spacecraft were placed in orbit about Mars, many models from degree and order 6 to degree and order 50 have been developed. However, during the Viking mission, some 26,000 range measurements to the two Viking Orbiters were also obtained. These data have not previously been used in the derivation of Mars gravity models. A portion of these range data have been processed simultaneously with the Doppler data. Normal equations were generated for both sets of data and were used to create two solutions complete to degree and order 30: a nominal solution including both the range and the Doppler data (MGM-R100), and another solution including only the Doppler data (MGM-R101). Tests with the covariances of these solutions, as well as with orbit overlap tests indicate that the interplanetary range data can be used to improve the modeling of the Mars gravity field.
The processing of the Viking Orbiter range data and its contribution to Mars gravity solutions
1992-01-01
Conference paper
No indication
English
TIBKAT | 1980
|Imaging experiment - The Viking Mars Orbiter.
NTRS | 1972
|Viking Mars Orbiter 1975 Solar Energy Controller
AIAA | 1977
|The Viking Mars Orbiter 1975 solar energy controller
AIAA | 1975
|The Viking Mars Orbiter 1975 solar energy controller
NTRS | 1975
|