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Higher-degree reference field in the generalized Stokes-Helmert scheme for geoid computation
Abstract In this paper we formulate two corrections that have to be applied to the higher-degree reference spheroid if one wants to use it in conjunction with the Stokes-Helmert scheme for geoid determination. We show that in a precise geoid determination one has to apply the correction for the residual topographical potential and the correction for the earth ellipticity. Both these corrections may reach several decimetres; we show how their magnitudes vary within Canada and we give their global ranges.
Higher-degree reference field in the generalized Stokes-Helmert scheme for geoid computation
Abstract In this paper we formulate two corrections that have to be applied to the higher-degree reference spheroid if one wants to use it in conjunction with the Stokes-Helmert scheme for geoid determination. We show that in a precise geoid determination one has to apply the correction for the residual topographical potential and the correction for the earth ellipticity. Both these corrections may reach several decimetres; we show how their magnitudes vary within Canada and we give their global ranges.
Higher-degree reference field in the generalized Stokes-Helmert scheme for geoid computation
Vaníček, Petr (Autor:in) / Najafi, Mehdi (Autor:in) / Martinec, Zdeněk (Autor:in) / Harrie, Lars (Autor:in) / Sjöberg, Lars E. (Autor:in)
Journal of Geodesy ; 70
1995
Aufsatz (Zeitschrift)
Englisch
BKL:
38.73
Geodäsie
The Stokes-Helmert scheme for the evaluation of a precise geoid
Online Contents | 1994
|Topographic effects by the Stokes–Helmert method of geoid and quasi-geoid determinations
Online Contents | 2000
|On the indirect effect in the Stokes–Helmert method of geoid determination
Online Contents | 1999
|The Effect of Noise on Geoid Height in Stokes-Helmert Method
TIBKAT | 2019
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