Improvement of the Earth's gravity field from terrestrial and satellite data

Details Improvement of the Earth's gravity field from terrestrial and satellite data Improvement of the Earth's gravity field from terrestrial and satellite data

Jan 1987

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1987osu..repts.....&link_type=abstract

Status Report, 1 Nov. 1984 - 31 Dec. 1986 Ohio State Univ., Columbus. Dept. of Geodetic Science and Surveying.

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Applications

Anomalies, Data Bases, Earth (Planet), Earth Gravitation, Geoids, Gravitational Fields, Satellite Tracking, Spherical Harmonics, Geopotential Research Mission, Laser Applications, Least Squares Method, Satellite Observation

Scientific paper

The terrestrial gravity data base was updated. Studies related to the Geopotential Research Mission (GRM) have primarily considered the local recovery of gravity anomalies on the surface of the Earth based on satellite to satellite tracking or gradiometer data. A simulation study was used to estimate the accuracy of 1 degree-mean anomalies which could be recovered from the GRM data. Numerous procedures were developed for the intent of performing computations at the laser stations in the SL6 system to improve geoid undulation calculations.

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