Aerobraking was selected for the Mars Global Surveyor mission as a primary
and enabling operation. The application of accelerometer data for determini
ng atmospheric density during operations for the first phase of aerobraking
is reported. Acceleration was measured along the body z axis, which is the
axis nominally into the flow. For a 1-s count time, the data have a resolu
tion of 0.332 mm/s, permitting the recovery of density to 3% at nominal aer
obraking altitudes near 115 km and on many orbits, permitting the recovery
of density to altitudes as high as 180 km. Accelerometer data were analyzed
in near real time to provide estimates of density at periapsis, maximum de
nsity, density scale height, latitudinal gradient information, and longitud
inal wave variations. Summaries are given of the aerobraking phase of the m
ission, the accelerometer data analysis methods and operational procedures,
some applications to determining thermospheric properties, and some remain
ing issues on interpretation of the data. Preflight estimates of 70% 2 sigm
a natural variability are shown to be realistic, and predictions that dust
storms could produce rapid and large increases in thermospheric density hav
e been verified.