An inverse problem related to a finite part of a compact surface: Potential deduced from gravity gradients in space

Details An inverse problem related to a finite part of a compact surface: Potential deduced from gravity gradients in space An inverse problem related to a finite part of a compact surface: Potential deduced from gravity gradients in space

Oct 1993

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1993jgr....9817773b&link_type=abstract

Journal of Geophysical Research (ISSN 0148-0227), vol. 98, no. B10, p. 17,773-17,785

Physics

Earth Surface, Geodesy, Gravitational Fields, Gravity Anomalies, Boundary Value Problems, Gravity Gradiometers, Satellite-Borne Instruments

Scientific paper

Mean values for gravity and potential at the surface of the Earth are derived for limited areas in terms of mean anomalies using the cross-track and radial components of the Eoetvoes tensor derived from space-borne gradiometer data at satellite altitude. Stability, resolution, and precision are investigated, and reliability criteria are established. The inverse boundary value problem is discussed for specific solutions for smaller and larger areas at the Earth's surface; discrete area means and point values are considered.

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