Time-variable aliasing effects of ocean tides, atmosphere, and continental water mass on monthly mean GRACE gravity field

Author:

Han Shin-Chan1,Jekeli Christopher1,Shum C. K.1

Affiliation:

1. Laboratory for Space Geodesy and Remote Sensing Research, Department of Civil and Environmental Engineering and Geodetic Science; Ohio State University; Columbus Ohio USA

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference28 articles.

1. Bettadpur , S. M. Watkins 2000 GRACE gravity science and its impact on mission design Eos Trans. AGU 81 19 Spring Meet. Suppl.

2. Temporal variation of the Earth's low-degree zonal gravitational field caused by atmospheric mass redistribution: 1980-1988;Chao;J. Geophys. Res.,1991

3. Gravitational perturbation theory for intersatellite tracking;Cheng;J. Geod.,2002

4. Eanes , R. S. Bettadpur 1995 The CSR 3.0 global ocean tide model Tech. Memo. CSR-TM-95 06 Cent. for Space Res., Univ. of Tex. Austin

5. Ge , S. C. Shum J. Wickert C. Reigber 2002 Atmospheric limb-sounding using GPS occultation Global Navigation Satellite System Workshop Wuhan, China

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