Non-Global Recovery of Gravity Anomalies from a Combination of Terrestrial and Satellite Altimetry Data,
OHIO STATE UNIV COLUMBUS DEPT OF GEODETIC SCIENCE
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Two methods for recovery of gravity anomalies are described. Of those, the indirect method, based on the use of the Stokes formula is chosen for its flexibility in combining any a priori information available on the anomalies and in filtering out any systematic error that may be inherent in the observations.