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Scirj Volume VII, Issue II, February 2019 Edition ISSN: 2201-2796 Derivation of Theoretical Gravity Model on the Clarke 1880 Ellipsoid for Practical Local Geoid Model Determination Eteje S. O., Oduyebo O. F. and Ono M. N. Abstract: The application of gravity anomalies for gravimetric geoid model determination has necessitated the computation of normal gravity on the WGS 84 ellipsoid using the International Gravity Formula. For local gravimetric geoid model determination, the gravity anomalies are computed on the local ellipsoid adopted for geodetic computation in the area/region of study. To determine precise local gravimetric geoid model in countries where Clarke 1880 ellipsoid is adopted for geodetic computation, the theoretical gravity must be computed on the adopted geodetic computation surface. As a result, this paper derives a local theoretical gravity model on the Clarke 1880 ellipsoid for practical local geoid model determination. The model was derived using the Clarke 1880 ellipsoid parameters, angular velocity, gravitational constant and the Somiglinana closed formula for normal gravity. The derived model was presented in two forms, model A and model B. The two forms of the derived model were compared to determine their suitability as well as agreement. The comparison results show that the two forms of the model agree. Thus, any of the model forms can be applied for accurate normal gravity computation where Clarke 1880 ellipsoid is adopted as a computation surface. Reference this Paper: Derivation of Theoretical Gravity Model on the Clarke 1880 Ellipsoid for Practical Local Geoid Model Determination by Eteje S. O., Oduyebo O. F. and Ono M. N. published at: "Scientific Research Journal (Scirj), Volume VII, Issue II, February 2019 Edition, Page 12-19 ". Search Terms: normal, theoretical, gravity, Clarke 1880, ellipsoid, gravimetric, local geoid, model [Read Research Paper] [Full Screen] |
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