Geopotential models of the Earth from satellite tracking, altimeter and surface gravity observations: GEM-T3 and GEM-T3S.

Details Geopotential models of the Earth from satellite tracking, altimeter and surface gravity observations: GEM-T3 and GEM-T3S. Geopotential models of the Earth from satellite tracking, altimeter and surface gravity observations: GEM-T3 and GEM-T3S.

Jan 1992

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992gmef.book.....l&link_type=abstract

Geopotential models of the Earth from satellite tracking, altimeter and surface gravity observations: GEM-T3 and GEM-T3S., by Le

Computer Science

5

Scientific paper

Improved models of the Earth's gravitational field have been developed from conventional tracking data (GEM-T3S) and from a combination of satellite tracking, satellite altimeter and surface gravimetric data (GEM-T3). This combination model represents a significant improvement in the modeling of the gravity field at half-wavelengths of 300 km and longer. Both models are complete to degree and order 50.

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