Spectral harmonic analysis and synthesis of Earth's crust gravity field
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Publication:695729
DOI10.1007/S10596-011-9264-0zbMath1254.86019OpenAlexW1988989190WikidataQ57863368 ScholiaQ57863368MaRDI QIDQ695729
Pavel Novák, Peter Vajda, Vladislav Gladkikh, Robert Tenzer, Mirza Tariq Hamayun
Publication date: 17 December 2012
Published in: Computational Geosciences (Search for Journal in Brave)
Full work available at URL: http://resolver.tudelft.nl/uuid:b66a0d9c-1e59-4706-9a08-61818dfcd263
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Cites Work
- Spectral harmonic analysis and synthesis of Earth's crust gravity field
- On the indirect effect in the Stokes-Helmert method of geoid determination
- The IAG approach to the atmospheric geoid corrections in Stokes' formula and a new strategy
- The effects of Stokes's formula for an ellipsoidal layering of the earth's atmosphere
- On Helmert's methods of condensation.
- Gravity/magnetic potential of uneven shell topography
- Topographic effects by the Stokes-Helmert method of geoid and quasi-geoid determinations.
- Convergence and optimal truncation of binomial expansions used in isostatic compensations and terrain corrections.
- A comparison between the Airy/Heiskanen and the Pratt/Hayford isostatic models for the computation of potential harmonic coefficients.
- Two different views of topographical and downward-continuation corrections in the Stokes-Helmert approach to geoid computation.
- Topographic and atmospheric corrections of gravimetric geoid determination with special emphasis on the effects of harmonics of degrees zero and one
- Effects of the spherical terrain on gravity and the geoid.
- A new strategy for the atmospheric gravity effect in gravimetric geoid determination
- The topographic bias by analytical continuation in physical geodesy
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