GRAVITY MODEL DEVELOPMENT FOR TOPEX/POSEIDON - JOINT GRAVITY MODEL-1 AND MODEL-2

被引:129
作者
NEREM, RS
LERCH, FJ
MARSHALL, JA
PAVLIS, EC
PUTNEY, BH
TAPLEY, BD
EANES, RJ
RIES, JC
SCHUTZ, BE
SHUM, CK
WATKINS, MM
KLOSKO, SM
CHAN, JC
LUTHCKE, SB
PATEL, GB
PAVLIS, NK
WALLIAMSON, RG
RAPP, RH
BIANCALE, R
NOUEL, F
机构
[1] UNIV MARYLAND, DEPT ASTRON, COLLEGE PK, MD 20742 USA
[2] UNIV TEXAS, CTR SPACE RES, AUSTIN, TX 78712 USA
[3] HUGHES STX CORP, LANHAM, MD USA
[4] OHIO STATE UNIV, DEPT GEODET SCI & SURVEYING, COLUMBUS, OH 43210 USA
[5] CTR NATL ETUD SPATIALES, F-31055 TOULOUSE, FRANCE
关键词
D O I
10.1029/94JC01376
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
The TOPEX/POSEIDON (TIP) prelaunch Joint Gravity Model-1 (JGM-1) and the 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 surface gravimetry. While improved orbit determination accuracies for T/P have driven the improvements in the models, the models are general in application and also provide an improved geoid for oceanographic computations. The postlaunch model, JGM-2, which includes T/P satellite laser ranging (SLR) and Doppler orbitography and radiopositioning integrated by satellite (DORIS) tracking data, introduces radial orbit errors for TIP that are only 2 cm RMS with the commission errors of the marine 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 topography for wavelengths shorter than about 2500 km., Only a dedicated gravitational field satellite mission will likely provide the necessary improvement in the geoid.
引用
收藏
页码:24421 / 24447
页数:27
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