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Anglais > Français : Géodésie, 3 pages
géodésie
03 pages
en ligne
Example du texte :
The existence of topography above the geoid violates the basic assumption of Stokes’ formula for
the determination of the geoid. Usually a constant density 2.67g/cm3 is used in the determination
of the geoid. This research presents the results of some preliminary experiments conducted using
topographic density data in gravimetric geoid computations in Iran. There are many different
reasons for starting the current research in Iran. Iran is one of the most complicated areas in the
world from the view of rough topography, tectonic activity, density and geoidal height variation.
The minimum, maximum, mean and standard deviation of the topographic heights in Iran are -26,
5678, 1059 and ±734 m, respectively. Also, the geoidal height varies in the range of 50 m. After
the determination of the gravimetric geoid model (IRG04) (Kiamehr 2006a), we attempt to
improve the accuracy of this model, specially in mountainous areas by considering the effect of
lateral density variations
Language pair(s)
English
> French
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