TY - CHAP
T1 - Theory and Observations - Forward Modeling and Synthetic Seismograms
T2 - 3-D Numerical Methods
AU - Tromp, Jeroen
N1 - Funding Information:
The author would like to thank Heiner Igel, Dimitri Komatitsch, Nozomu Takeuchi, Christine Thomas, Seiji Tsuboi, and Yanbin Wang for contributing figures to this chapter. The SEM synthetics were calculated by Seiji Tsuboi on the Earth Simulator computer at the Japan Agency for Marine-Earth Science and Technology. Broadband data were obtained from the IRIS Data Management Center. This material is based in part upon work supported by the National Science Foundation under grant EAR-0309576. This is contribution No. 9124 of the Division of Geological & Planetary Sciences, California Institute of Technology.
PY - 2007
Y1 - 2007
N2 - We provide an overview of the numerical methods used to simulate seismic wave propagation at the scale of the globe. These numerical techniques may be subdivided in terms of methods based upon a differential or strong form of the equation of motion and methods based upon an integral or weak representation. In the former category we discuss finite difference and pseudospectral methods, whereas in the latter category we consider coupled mode direct solution, finite element, and spectral element techniques. To date, only coupled mode, direct solution, and spectral element methods have been able to simulate three-dimensional seismic wave propagation throughout the entire globe. We have now reached a stage where fully three-dimensional numerical methods can be effectively used to address the inverse problem. In this regard, adjoint methods appear to be particularly promising.
AB - We provide an overview of the numerical methods used to simulate seismic wave propagation at the scale of the globe. These numerical techniques may be subdivided in terms of methods based upon a differential or strong form of the equation of motion and methods based upon an integral or weak representation. In the former category we discuss finite difference and pseudospectral methods, whereas in the latter category we consider coupled mode direct solution, finite element, and spectral element techniques. To date, only coupled mode, direct solution, and spectral element methods have been able to simulate three-dimensional seismic wave propagation throughout the entire globe. We have now reached a stage where fully three-dimensional numerical methods can be effectively used to address the inverse problem. In this regard, adjoint methods appear to be particularly promising.
KW - Numerical modeling
KW - Seismic wave propagation
KW - Synthetic seismograms
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U2 - 10.1016/B978-044452748-6.00006-7
DO - 10.1016/B978-044452748-6.00006-7
M3 - Chapter
AN - SCOPUS:84882819510
SN - 9780444527486
VL - 1
SP - 191
EP - 217
BT - Treatise on Geophysics
PB - Elsevier
ER -