Precise and efficient evaluation of gravimetric quantities at arbitrarily scattered points in space
Autor: | Pencho Petrushev, Kamen G. Ivanov, Nikolaos K. Pavlis |
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Rok vydání: | 2017 |
Předmět: |
Physics
Surface (mathematics) 010504 meteorology & atmospheric sciences Degree (graph theory) Mathematical analysis Vertical deflection Spherical harmonics 010502 geochemistry & geophysics 01 natural sciences Ellipsoid Geophysics Tensor product Geochemistry and Petrology Harmonics Harmonic Computers in Earth Sciences 0105 earth and related environmental sciences |
Zdroj: | Journal of Geodesy. 92:779-796 |
ISSN: | 1432-1394 0949-7714 |
DOI: | 10.1007/s00190-017-1094-y |
Popis: | Gravimetric quantities are commonly represented in terms of high degree surface or solid spherical harmonics. After EGM2008, such expansions routinely extend to spherical harmonic degree 2190, which makes the computation of gravimetric quantities at a large number of arbitrarily scattered points in space using harmonic synthesis, a very computationally demanding process. We present here the development of an algorithm and its associated software for the efficient and precise evaluation of gravimetric quantities, represented in high degree solid spherical harmonics, at arbitrarily scattered points in the space exterior to the surface of the Earth. The new algorithm is based on representation of the quantities of interest in solid ellipsoidal harmonics and application of the tensor product trigonometric needlets. A FORTRAN implementation of this algorithm has been developed and extensively tested. The capabilities of the code are demonstrated using as examples the disturbing potential T, height anomaly $$\zeta $$ , gravity anomaly $$\Delta g$$ , gravity disturbance $$\delta g$$ , north–south deflection of the vertical $$\xi $$ , east–west deflection of the vertical $$\eta $$ , and the second radial derivative $$T_{rr}$$ of the disturbing potential. After a pre-computational step that takes between 1 and 2 h per quantity, the current version of the software is capable of computing on a standard PC each of these quantities in the range from the surface of the Earth up to 544 km above that surface at speeds between 20,000 and 40,000 point evaluations per second, depending on the gravimetric quantity being evaluated, while the relative error does not exceed $$10^{-6}$$ and the memory (RAM) use is 9.3 GB. |
Databáze: | OpenAIRE |
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