Application of double Fourier series to computing gravity anomalies and other gravimetric quantities at higher elevations, starting from given surface gravity anomalies

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1959-10

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Ohio State University. Division of Geodetic Science

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Abstract

The double Fourier series method has been developed for computing gravity anomalies at higher elevations, starting from given surface gravity anomalies. As an example of its application, the method has been used to deduce gravity anomalies at an elevation of 15.9 km above a portion of Sweden.

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Prepared for Air Force Cambridge Research Center, U.S. Air Research and Development Command, Laurence G. Hanscom Field, Bedford, Massachusetts: Contract No. AF 19(604)-1963 (OSURF Project 716)

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