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DEPARTMENT OF GEOPHYSICS STANFORD UNIVERSITY, STANFORD, CALIFORNIA
DEPARTMENT OF COMPUTER SCIENCES UPPSALA UNIVERSITY, UPPSALA, Sweden
Abstract
Boundary conditions are derived for numerical wave simulation that minimize artificial reflections from the edges of the domain of computation. In this way acoustic and elastic wave propagation in a limited area can be efficiently used to describe physical behavior in an unbounded domain. The boundary conditions are based on paraxial approximations of the scalar and elastic wave equations. They are computationally inexpensive and simple to apply, and they reduce reflections over a wide range of incident angles.
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S. H. EMERMAN and R. A. STEPHEN Comment on "absorbing boundary conditions for acoustic and elastic wave equations," by R. Clayton and B. Engquist Bulletin of the Seismological Society of America, April 1, 1983; 73(2): 661 - 665. [PDF]
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D. M. BOORE, S. C. HARMSEN, and S. T. HARDING Wave scattering from a step change in surface topography Bulletin of the Seismological Society of America, February 1, 1981; 71(1): 117 - 125. [Abstract] [PDF]
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E. KAUSEL and J. L. TASSOULAS Transmitting boundaries: A closed-form comparison Bulletin of the Seismological Society of America, February 1, 1981; 71(1): 143 - 159. [Abstract] [PDF]
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M. FUYUKI and Y. MATSUMOTO Finite difference analysis of Rayleigh wave scattering at a trench Bulletin of the Seismological Society of America, December 1, 1980; 70(6): 2051 - 2069. [Abstract] [PDF]
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J. W. SCHLUE Love-wave propagation in three-dimensional structures using finite element techniques Bulletin of the Seismological Society of America, April 1, 1979; 69(2): 319 - 328. [Abstract] [PDF]
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