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| Content Provider | Springer Nature Link |
|---|---|
| Author | Vaľko, M. Mojzeš, M. Janák, J. Papčo, J. |
| Copyright Year | 2008 |
| Abstract | The main purpose of this paper is comparison of two different approaches of solution to the Simple Molodensky’s Problem, the Molodensky’s Approach and the Analytical Continuation Approach, based on numerical computation. Although these approaches have been described theoretically by several authors, e.g. Molodensky et al. (1960), Heiskanen and Moritz (1967), Vaníček (1974), Moritz (1980) and Holota (1991, unpublished results) and theoretical proof of equivalence was given by Heiskanen and Moritz (1967), Moritz (1971), Ecker (1971) and Pellinen (1972, unpublished results), only very few practical experiences about the differences between particular solutions and computational efficiency exist. In this paper we compare the above two mentioned approaches in terms of the G$_{1}$-effect on quasigeoid. Both quasigeoid solutions are tested by the independent GPS/levelling approach and are also compared with the previous quasigeoid model of Slovakia where the G$_{1}$-term has been approximated using the classical terrain correction. The effect of the G$_{2}$-term is also numerically estimated, revealing that it might be significant for the precise quasigeoid determination. Some practical comments and recommendations are given at the end of the paper. |
| Starting Page | 71 |
| Ending Page | 86 |
| Page Count | 16 |
| File Format | |
| ISSN | 00393169 |
| Journal | Studia Geophysica et Geodaetica |
| Volume Number | 52 |
| Issue Number | 1 |
| e-ISSN | 15731626 |
| Language | English |
| Publisher | Springer US |
| Publisher Date | 2008-04-30 |
| Publisher Place | Boston |
| Access Restriction | One Nation One Subscription (ONOS) |
| Subject Keyword | simple Molodensky’s problem boundary value problem gradient solution G $_{1}$ term telluroid Meteorology/Climatology Structural Geology Geophysics/Geodesy |
| Content Type | Text |
| Resource Type | Article |
| Subject | Geochemistry and Petrology Geophysics |
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