The relative variation of the vertical gravity gradient on the level ellipsoid.

Physics

Scientific paper

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Potential Theory: Gravitation Theory, Geopotential

Scientific paper

The relative variation of the vertical gravity gradient on an equipotential ellipsoid is given as a function of the geometrical flattening f of the ellipsoid and of the rotational parameter m up to the second order in the quantities f and m. General formulae are also obtained for the relative variation of vertical derivatives of the geopotential with differentiation order higher than two; it is seen that particularly simple first-order formulae are obtained. A possible application of the concept of "flattening" of the vertical derivatives of the geopotential is also suggested.

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