NASA NTRS · 19730018607
Earth's isostatic gravity anomaly field: Contributions to National Geodetic Satellite Program
Abstract
On the assumption that the compensation for the topographic load is achieved in the manner of Airy-Heiskenenan hypothesis at a compensation depth of 30 kilometers, the spherical harmonic coefficients of the isostatic reduction potential U are computed. The degree power spectra of these coefficients are compared with the power spectra of the isostatic reduction coefficients given by Uotila. Results are presented in tabular form.
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Khan, M. A.. 1973-06-01. Earth's isostatic gravity anomaly field: Contributions to National Geodetic Satellite Program. https://ntrs.nasa.gov/citations/19730018607
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