Centre de documentation
scientifique

Global height datum unification : a new approach in gravity potential space / Alireza A. Ardalan in Journal of geodesy, vol 79 n° 9 (December 2005)  

Public [article]  inJournal of geodesy > vol 79 n° 9 (December 2005) . - pp 512 - 523 Titre : Global height datum unification : a new approach in gravity potential space Type de document : Article/Communication Auteurs : Alireza A. Ardalan, Auteur ; A. Safari, Auteur Année de publication : 2005 Article en page(s) : pp 512 - 523 Note générale : Bibliographie Langues : Anglais (eng) Descripteur : [Vedettes matières IGN] Géodésie physique [Termes IGN] géoïde terrestre [Termes IGN] International Terrestrial Reference System [Termes IGN] Iran [Termes IGN] levé gravimétrique [Termes IGN] niveau moyen des mers [Termes IGN] ondelette d'Abel-Poisson [Termes IGN] positionnement par GNSS [Termes IGN] potentiel de pesanteur terrestre [Termes IGN] problème des valeurs limites [Termes IGN] système de référence altimétrique [Termes IGN] système de référence local Résumé : (Auteur) The problem of "global height datum unification" is solved in the gravity potential space based on: (1) high-resolution local gravity field modeling, (2) geocentric coordinates of the reference benchmark, and (3) a known value of the geoid's potential. The high-resolution local gravity field model is derived based on a solution of the fixed-free two-boundary-value problem of the Earth's gravity field using (a) potential difference values (from precise leveling), (b) modulus of the gravity vector (from gravimetry), (c) astronomical longitude and latitude (from geodetic astronomy and/or combination of (GNSS) Global Navigation Satellite System observations with total station measurements), (d) and satellite altimetry. Knowing the height of the reference benchmark in the national height system and its geocentric GNSS coordinates, and using the derived high-resolution local gravity field model, the gravity potential value of the zero point of the height system is computed. The difference between the derived gravity potential value of the zero point of the height system and the geoid's potential value is computed. This potential difference gives the offset of the zero point of the height system from geoid in the "potential space", which is transferred into "geometry space" using the transformation formula derived in this paper. The method was applied to the computation of the offset of the zero point of the Iranian height datum from the geoid's potential value W0=62636855.8 m 2/S2 . According to the geometry space computations, the height datum of Iran is 0.09 m below the geoid. Numéro de notice : A2005-518 Affiliation des auteurs : non IGN Thématique : POSITIONNEMENT Nature : Article nature-HAL : ArtAvecCL-RevueIntern DOI : 10.1007/s00190-005-0001-0 En ligne : https://doi.org/10.1007/s00190-005-0001-0 Format de la ressource électronique : URL article Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=27654 [article]

Exemplaires(2)

Code-barres	Cote	Support	Localisation	Section	Disponibilité
266-05091	RAB	Revue	Centre de documentation	En réserve L003	Disponible
266-05092	RAB	Revue	Centre de documentation	En réserve L003	Disponible