Abstract
The original, as well as any type of modified Stokes’ formula, requires a number of corrections as Stokes’ integral allows no masses outside the sphere of integration . The corrections include direct topographic, atmospheric and ellipsoidal effects and a downward continuation (DWC) effect on the surface gravity anomaly to be applied prior to Stokes’ integration. After integration, indirect effects are applied to the potential for restoration of masses as well as for corrections to the potential on the reference ellipsoid (rather than the sphere of integration). These are the classical corrections that are used more or less also in the modern remove-restore technique. The KTH method for geoid determination uses “additive corrections” to the preliminary geoid heights computed directly from the surface gravity anomalies. These corrections are therefore combinations of direct and indirect effects on potential/geoid height , implying several advantages. For example, the numerical solution to the DWC effect on the potential is much more stable than the corresponding effect on the gravity anomaly.
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Sjöberg, L.E., Bagherbandi, M. (2017). Corrections in Geoid Determination. In: Gravity Inversion and Integration. Springer, Cham. https://doi.org/10.1007/978-3-319-50298-4_5
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