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Published in 2024 at "Journal of Geodesy"
DOI: 10.1007/s00190-024-01844-3
Abstract: The Helmert’s second condensation method is usually used to condense the topographical masses outside the boundary surface in the determination of the geoid and quasi-geoid based on the boundary-value theory. The condensation of topographical masses…
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Keywords:
topographical effects;
boundary value;
algorithms high;
high frequency ... See more keywords