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dc.contributor.authorNahavandchi, Hossein
dc.date.accessioned2023-10-19T07:56:59Z
dc.date.available2023-10-19T07:56:59Z
dc.date.created2002-02-11T00:00:00Z
dc.date.issued2000
dc.identifier.citationJournal of Geodesy. 2000, 74 (6), 488-496.en_US
dc.identifier.issn0949-7714
dc.identifier.urihttps://hdl.handle.net/11250/3097459
dc.description.abstractThe direct topographical correction is composed of both local effects and long-wavelength contributions. This implies that the classical integral formula for determining the direct effect may have some numerical problems in representing these different signals. On the other hand, a representation by a set of harmonic coefficients of the topography to, say, degree and order 360 will omit significant short-wavelength signals. A new formula is derived by combining the classical formula and a set of spherical harmonics. Finally, the results of this solution are compared with the Moritz topographical correction in a test area.en_US
dc.description.abstractThe direct topographical correction in gravimetric geoid determination by the Stokes-Helmert methoden_US
dc.language.isoengen_US
dc.publisherSpringeren_US
dc.titleThe direct topographical correction in gravimetric geoid determination by the Stokes-Helmert methoden_US
dc.title.alternativeThe direct topographical correction in gravimetric geoid determination by the Stokes-Helmert methoden_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionacceptedVersionen_US
dc.rights.holder© 2000 Springer Natureen_US
dc.source.pagenumber488-496en_US
dc.source.volume74en_US
dc.source.journalJournal of Geodesyen_US
dc.source.issue6en_US
dc.identifier.doihttps://doi.org/10.1007/s001900000110
dc.identifier.cristin408482
cristin.ispublishedtrue
cristin.fulltextpostprint
cristin.fulltextpostprint
cristin.qualitycode1


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