O the Gravity Gradient at Satellite Altitudes

Computer Science

Scientific paper

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Scientific paper

The horizontal and vertical components of the gravity gradient are computed along equipotential surfaces at altitudes of 0, 500, 1000, 5000, 10,000, 50,000, and 100,000 km, from Kozai's (1964) and Gaposchkin's (1966) harmonic coefficients. Accuracy estimates for the gravity gradients, as obtained from satellite orbits, are derived from a comparison with Kaula's (1966) CA solution.

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