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Spectral ray tracer: a class of accurate two-point ray tracers

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Języki publikacji
EN
Abstrakty
EN
The recent development of high resolution seismic tomography and the in-creasing necessity for high precision seismic (acoustic) source locations calls for robust and very precise numerical methods of estimating of seismic (acoustic) wave travel times and propagation ray paths. This paper deals with two issues. First of all we present a ray path tracing algorithm based on the parameterization of ray paths by a series of Chebyshev polynomials. This pseudo-spectral method combined with the accurate Gauss-Lobbato integration procedure allows to reach a very high relative accuracy of travel time calculation, of the order of t/t 10(-7). The pseudo-spectral representation of sought ray paths turns the ray tracing problem into a numerical optimization task which, depending on the requirements, can be solved by a properly chosen optimizer. The used numerical representation designates the developed algorithm for tomography/location applications when no sharp interfaces occur. Secondly, we consider the question of the accuracy of the ray path tracing and travel time calculations. Achieving the highest tracing accuracy in terms of both accurate travel time estimation and precise spatial tracing (ray path geometry) requires a very careful analysis of all classes of errors. Some of them are caused by the numerical approximation (discretization) of the (continuous) physical law underlying a chosen computational algorithm. We demonstrate that these errors can degrade the ray tracing accuracy even by two orders of magnitude. To suppress this type of inaccuracy we propose to use a damping mechanism which introduces a kind of "tension" to the numerically generated ray paths. When properly applied, it suppresses the artificial spatial oscillations caused by the approximation errors and improves the ray tracing accuracy. The damping mechanism can also be regarded as the a priori requirement to keep the physical ray path trajectory as simple (smooth) as possible.
Słowa kluczowe
Rocznik
Strony
1--14
Opis fizyczny
Bibliogr. 25 poz.
Twórcy
autor
  • Institute of Geophysics, Polish Academy of Sciences, ul. Księcia Janusza 64, 01-452 Warszawa
autor
  • Research Center for Seismology and Volcanology, Nagoya University, Nagoya Japan
Bibliografia
  • 1. Aki, K., and P.G. Richards, 1985, Quantitative Seismology, Freeman and Co, San Francisco.
  • 2. Arfken, G., 1989, Mathematical Methods for Physicists, Academic Press, San Diego, III edition.
  • 3. Boyd, J.P., 1989, Chebyshev and Fourier Spectral Methods, Lecture Notes in Engineering, Spring-Verlag, New York.
  • 4. Canuto, C., M.Y. Hussaini, A. Quarteroni and T.A. Zang, 1988, Spectral Methods in Fluid Dynamics, Spring-Verlag, New York.
  • 5. Červeny, V., 2001, Seismic Ray Theory, Cambridge University Press, New York.
  • 6. Červeny, V., LA. Molotkov and I. Pšenćik, 1997, Ray Method in Seismology, Univerzita Karlova, Praha.
  • 7. Dębski, W., and R.P. Young, 2002, Tomographic imaging of thermally induced fractures in granite using Bayesian inversion, Pure Appl. Geophys. 159, 1-3, 277-307.
  • 8. Ferretti, G., D. Spallarossa, D. Bindi, P. Augliera, and M. Cattaneo, 2001, Comparison of two "pseudo-bending" raytracers, Phys. Earth Planet. Int. 123, 115-126.
  • 9. Fornberg, B., 1996, A Practical Guide to Pseudospectral Methods, Cambridge University Press, New York.
  • 10. Gottlieb D., and S. A. Orszag, 1977, Numerical Analysis of Spectral Methods: Theory and Application, Soc. Indust. Appl. Math., Philadelphia.
  • 11. Haslinger, F., and E. Kissling, 2001, Investigating effects of 3-D ray tracing methods in local earthquake tomography, Phys. Earth Planet. Int. 123, 103-114.
  • 12. Hori, M., 2001, Inverse analysis method using spectral decomposition of Green's function, Geophys. J. Int. 147, 77-87.
  • 13. lyer, H.M., and K. Hirahara, 1993, Seismic Tomography, Theory and Practice, Chapman and Hall, London.
  • 14. Koketsu, K., 1991, Three-dimensional ray tracing in a subduction zone, J. Seism. Soc. Japan 44, 165-176.
  • 15. Obana, K., H. Katao and M. Ando, 1999, Sea-floor positioning with global positioning system-acoustic link system, The Island Arc. 8, 245-258.
  • 16. Pereyra, V., 1992, Two-point ray tracing in general 3D media, Geophys. Prosp. 40, 267-287.
  • 17. Press, W.H., B.P. Flannery, S.A. Teukolsky and W.T. Vetterling, 1992, Numerical Recipes in C. The Art of Scientific Computing, Cambridge University Press, Cambridge.
  • 18. Prothero, W.A., W.J. Taylor and J.A. Eickemeyer, 1988, A fast, two-point, three-dimensional raytracing algorithm using a simple step search method, Bull. Seismol. Soc. Am. 78, 3,1190-1198.
  • 19. Sadeghi, H., S. Suzuki and H. Takenaka, 1999, A two-point, three-dimensional seismic ray tracing using genetic algorithms, Phys. Earth Planet. Int. 113, 355-365.
  • 20. Tadokoro, K., M. Ando, K. Sato, T. Yamada, T. Okuda, H. Katao and K. Kishimoto, 2001, Development of an observation system for ocean bottom crustal deformation using acoustic ranging-GPS link, J. Geography 110, 521-528.
  • 21. Tarantola, A., 1987, Inverse Problem Theory: Methods for Data Fitting and Model Parameter Estimation, Elsevier, Amsterdam.
  • 22. Um, J., and C. Thurber, 1987, A fast algorithm for two-point seismic ray tracing, Bull. Seis¬mol. Soc. Am. 77, 3, 972-986.
  • 23. Velis, D.R., and T.J. Ulrych, 1996, Simulated annealing two-point ray tracing, Geophys. Res. Lett. 23, 2, 201-204.
  • 24. Velis, D.R., and T.J. Ulrych, 2001, Simulated annealing ray tracing in complex three-dimensional media, Geophys. J. Int. 145, 447-459.
  • 25. Virieux, J., V. Farrara and R. Madariaga, 1988, Ray tracing for earthquake location in laterally heterogeneous media, J. Geophys. Res. 93, B6, 6585-6599.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BSL7-0007-0070
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