Abstract
The Fast Fourier Transform (FFT) technique is an efficient and practical tool in geodesy for solving local gravity field approximation problems, among others for local geoid (quasigeoid) determination. In the future we plan to use the FFT procedure for its efficiency in computing a detailed gridded set of height anomalies for Hungary.
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Reference
Renner, J. and Szilard, J. (1959): Gravity Network of Hungary. Acta Technica Acad. Sci. Hungaricae, t. XXIII, fasc.4, pp.365–395, Budapest, l959.
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© 1991 Springer-Verlag New York Inc.
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Ádám, J., Denker, H. (1991). Test Computations for a Local Quasigeoid in Hungary Using FFT. In: Rapp, R.H., Sansò, F. (eds) Determination of the Geoid. International Association of Geodesy Symposia, vol 106. Springer, New York, NY. https://doi.org/10.1007/978-1-4612-3104-2_23
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DOI: https://doi.org/10.1007/978-1-4612-3104-2_23
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