On the ellipsoidal correction to the spherical Stokes solution of the gravimetric geoid |
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Authors: | J Huang M Véronneau S D Pagiatakis |
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Institution: | (1) Geodetic Survey Division, Natural Resources Canada, 615 Booth Street, Ottawa, Ontario, Canada, K1A 0E9;(2) Department of Earth and Atmospheric Science, York University, Toronto, Ontario, Canada, M3J 1P3 |
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Abstract: | The solutions of four ellipsoidal approximations for the gravimetric geoid are reviewed: those of Molodenskii et al., Moritz, Martinec and Grafarend, and Fei and Sideris. The numerical results from synthetic tests indicate that Martinec and Grafarends solution is the most accurate, while the other three solutions contain an approximation error which is characterized by the first-degree surface spherical harmonic. Furthermore, the first 20 degrees of the geopotential harmonic series contribute approximately 90% of the ellipsoidal correction. The determination of a geoid model from the generalized Stokes scheme can accurately account for the ellipsoidal effect to overcome the first-degree surface spherical harmonic error regardless of the solution used. |
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Keywords: | Ellipsoidal correction Geoid Geodetic boundary value problem |
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