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dc.contributor.authorNahavandchi, Hossein
dc.date.accessioned2023-04-25T06:54:26Z
dc.date.available2023-04-25T06:54:26Z
dc.date.created2004-12-13T13:55:54Z
dc.date.issued2004
dc.identifier.citationBollettino di Geodesia e Scienze Affini. 2004, 63 (1), 1-11.en_US
dc.identifier.issn0006-6710
dc.identifier.urihttps://hdl.handle.net/11250/3064779
dc.description.abstractA new procedure to the direct atmospheric gravity effect in connection with Stokes's integral formula was presented by Nahavandchi (2002). This formula was derived by combining the local contributions of the effect of atmospheric masses, computed from a detailed Digital Terrain Model (DTM) and a set of spherical harmonics to account for the global contributions. This formula is valid for a point on the geoid, which indicates this fact that the direct effect and the effect of analytical continuation of gravity anomalies to sea level due to the atmospheric masses are combined into the so-called direct atmospheric effect. These two terms are studied here and a new strategy for the effect of atmospheric masses in geoid computations is presented. This strategy has been investigated over a test area.
dc.description.abstractThe direct effect and downward continuation correction of atmospheric masses in gravimetric geoid determination
dc.language.isoengen_US
dc.publisherIstituto Geografico Mifitareen_US
dc.titleThe direct effect and downward continuation correction of atmospheric masses in gravimetric geoid determinationen_US
dc.title.alternativeThe direct effect and downward continuation correction of atmospheric masses in gravimetric geoid determinationen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionacceptedVersion
dc.source.pagenumber1-11en_US
dc.source.volume63en_US
dc.source.journalBollettino di Geodesia e Scienze Affinien_US
dc.source.issue1en_US
dc.identifier.cristin426177
cristin.ispublishedtrue
cristin.fulltextpostprint
cristin.qualitycode1


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