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Derivation of Theoretical Gravity Model on the Clarke 1880 Ellipsoid f
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's closed formula for normal gravity.
Tags:
Clarke1880 , Gravimetric , Gravity , Normal , Theoretical
By:
Eteje
Science & Technology
15 months ago
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Tags:
Gr , Gravity , Gravity Separator Manufacturers
By:
spectrumusa
Entertainment
79 months ago
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