No 10-11 (2012): Ukrainian Antarctic Journal
Articles
Published
December 31, 2012
Keywords
- gravity,
- terrain effect,
- Moho,
- density,
- topographyc-isostatic corrections
How to Cite
Marchenko, D. O., & Maksymchuk, V. U. (2012). Parcularity of the geoid determination at the Antarctic region. Ukrainian Antarctic Journal, (10-11), 106-113. https://doi.org/10.33275/1727-7485.10-11.2012.292
Abstract
The gravitation effect of topographic masses is very important for the gravity anomaly calculations and geoid heights determination. The new approach for the computation of the topographic-isostatic corrections and indirect effect of topography in spherical approximation is developed and tested in Antarctic region.
References
- Forsberg, R. (1984). A study of terrain reductions, density anomalies and geophysical inversion methods in gravity field modeling. Reports of the Department of Geodetic Science and Surveying, Ohio State University, Report No. 355.
- Heiskanen, W.A., & Moritz, H. (1967). Physical Geodesy. W.H. Freeman, San Francisco.
- Moritz, H. (1980). Advanced Physical Geodesy. H. Wichmann, Karlsruhe.
- Moritz, H. (1990). The Figure of the Earth. Theoretical Geodesy and Earth’s Interior. Wichmann, Karlsruhe.
- Neyman, Yu.M. (1979). Variational Method of Physical Geodesy. Moscow, Nedra. (In Russian).
- Rummel, R., Rapp, R.H., Sünkel, H., & Tscherning, C.C. (1988). Comparisons of global topographic / isostatic models to the Earth’s observed gravity field. Reports of the Department of Geodetic Science and Surveying, Ohio State University, Report No. 388.
- Tsoulis, D. (2001). A comparison between the Airy/Heiskanen and the Pratt/Hayford isostatic models for the computation of potential harmonic coefficients. Journal of Geodesy, 74, 637–643.