The TOPEX/POSEIDON (TIP) prelaunch Joint Gravity Model-1 (JGM-1) and t
he postlaunch JGM-2 Earth gravitational models have been developed to
support precision orbit determination for T/P. Each of these models is
complete to degree 70 in spherical harmonics and was computed from a
combination of satellite tracking data, satellite altimetry, and surfa
ce gravimetry. While improved orbit determination accuracies for T/P h
ave driven the improvements in the models, the models are general in a
pplication and also provide an improved geoid for oceanographic comput
ations. The postlaunch model, JGM-2, which includes T/P satellite lase
r ranging (SLR) and Doppler orbitography and radiopositioning integrat
ed by satellite (DORIS) tracking data, introduces radial orbit errors
for TIP that are only 2 cm RMS with the commission errors of the marin
e geoid for terms to degree 70 being +/- 25 cm. Errors in modeling the
nonconservative forces acting on T/P increase the total radial errors
to only 3-4 cm RMS, a result much better than premission goals. While
the orbit accuracy goal for T/P has been far surpassed, geoid errors
still prevent the absolute determination of the ocean dynamic topograp
hy for wavelengths shorter than about 2500 km., Only a dedicated gravi
tational field satellite mission will likely provide the necessary imp
rovement in the geoid.