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Science 29 November 2002:
Vol. 298. no. 5599, pp. 1737 - 1742
DOI: 10.1126/science.1076024

Review

The Spectral-Element Method, Beowulf Computing, and Global Seismology

Dimitri Komatitsch,* Jeroen Ritsema, Jeroen Tromp

The propagation of seismic waves through Earth can now be modeled accurately with the recently developed spectral-element method. This method takes into account heterogeneity in Earth models, such as three-dimensional variations of seismic wave velocity, density, and crustal thickness. The method is implemented on relatively inexpensive clusters of personal computers, so-called Beowulf machines. This combination of hardware and software enables us to simulate broadband seismograms without intrinsic restrictions on the level of heterogeneity or the frequency content.

Seismological Laboratory, California Institute of Technology, 1200 East California Boulevard, Pasadena, CA 91125, USA.
*   To whom correspondence should be addressed; E-mail: komatits{at}gps.caltech.edu


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THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
Effects of Realistic Surface Topography on Seismic Ground Motion in the Yangminshan Region of Taiwan Based Upon the Spectral-Element Method and LiDAR DTM.
S.-J. Lee, Y.-C. Chan, D. Komatitsch, B.-S. Huang, and J. Tromp (2009)
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The Prospect of Using Three-Dimensional Earth Models to Improve Nuclear Explosion Monitoring and Ground-motion Hazard Assessment.
J. J. Zucca, W. R. Walter, A. J. Rodgers, P. Richards, M. E. Pasyanos, S. C. Myers, T. Lay, D. Harris, and T. Antoun (2009)
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Between a rock and a hot place: the core-mantle boundary.
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Three-Dimensional Simulations of Seismic-Wave Propagation in the Taipei Basin with Realistic Topography Based upon the Spectral-Element Method.
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Modeling of the Perfectly Matched Layer Absorbing Boundaries and Intrinsic Attenuation in Explicit Finite-Element Methods.
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Rupture Process of the 2004 Sumatra-Andaman Earthquake.
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