Abstract

We previously derived a general criterion for optimally accurate numerical operators for the calculation of synthetic seismograms in the frequency domain (Geller & Takeuchi 1995). We then derived modified operators for the Direct Solution Method (DSM) (Geller & Ohminato 1994) which satisfy this general criterion, thereby yielding significantly more accurate synthetics (for any given numerical grid spacing) without increasing the computational requirements (Cummins 1994; Takeuchi, Geller & Cummins 1996; Cummins, Takeuchi & Geller 1997). In this paper, we derive optimally accurate time-domain finite difference (FD) operators which are second order in space and time using a similar approach. As our FD operators are local, our algorithm is well suited to massively parallel computers. Our approach can be extended to other methods (e.g. pseudo-spectral) for solving the elastic equation of motion. It might also be possible to extend this approach to equations other than the elastic equation of motion, including non-linear equations.

Highlights

  • We previously derived a general criterion for optimally accurate numerical operators for the calculation of synthetic seismograms in the frequency domain

  • Our approach can be extended to other methods for solving the elastic equation of motion

  • It might be possible to extend this approach to equations other than the elastic equation of motion, including non-linear equations

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Summary

SUMMA RY

We previously derived a general criterion for optimally accurate numerical operators for the calculation of synthetic seismograms in the frequency domain We derived modi¢ed operators for the Direct Solution Method. (DSM) (Geller & Ohminato 1994) which satisfy this general criterion, thereby yielding signi¢cantly more accurate synthetics (for any given numerical grid spacing) without increasing the computational requirements We derive optimally accurate time-domain ¢nite di¡erence (FD) operators which are second order in space and time using a similar approach. Our approach can be extended to other methods (e.g. pseudo-spectral) for solving the elastic equation of motion. It might be possible to extend this approach to equations other than the elastic equation of motion, including non-linear equations

IN T ROD UCTION
Lu k
Operators for boundaries
STA BI LITYAND AC C U R AC Y
Lo Lp
NUMER ICA L E XA MPL E S
CPU time
AC K NOW L ED GMENTS
REFERE NC E S
IMPLEMENTATION OF ALGORITHMS
Full Text
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