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
Summary
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
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