The Earth's gravity field from the STEP mission

Details The Earth's gravity field from the STEP mission The Earth's gravity field from the STEP mission

Nov 1996

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1996cqgra..13a.113s&link_type=abstract

Classical and Quantum Gravity, Volume 13, Issue 11A, pp. A113-A117 (1996).

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Scientific paper

The geodesy experiment on STEP aims at the precise and detailed determination of the spatial variations of the Earth's gravitational field by measuring the cross-track gradient along the orbit. If the envisaged gradiometer precision of 0264-9381/13/11A/015/img1 can be reached and all other potential error sources, such as alignment, pointing and time-varying eigengravitation can be kept below this limit, a spatial resolution of about 100 km half-wavelength will be attained with a cumulative geoid error of below 2 cm (except in the polar areas).

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