Accuracy of heterogeneous staggered-grid finite-difference modeling of Rayleigh waves
By Thomas Bohlen, Erik H. Saenger. 2006
210 citations recorded by the source corpus.
Subfields: Earth-Surface Processes, Geophysics
View Paper: https://www.semanticscholar.org/paper/eaff72c56ee7ad44f8f18306bd35efab1419507d
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In Earth-Surface Processes
In Geophysics
Citations in the corpus
- An implicit staggered‐grid finite‐difference method for seismic modelling (2009, methodology): “…conventional-grid FD methods, staggered-grid FD methods have greater precision and better stability and have been widely used in seismic modelling (e.g. Madariaga 1976; Virieux 1984, 1986; Levander 1988; Graves 1996; Gottschämer & Olsen 2001; Mittet 2002; Moczo et al. 2002; Bohlen & Saenger 2006).”
- The finite-difference and finite-element modeling of seismic wave propagation and earthquake motion (2007, background): “Recently, the use of the partly-staggered grid was promoted by Saenger et al. (2000); see also Saenger and Bohlen (2004), Kruger et al. (2005), Saenger et al. (2005), Bohlen and Saenger (2006).”
- A Fourth Order Accurate SH-Wave Staggered Grid Finite-difference Algorithm with Variable Grid Size and VGR-Stress Imaging Technique (2008, background): “Bohlen and Saenger (2006) reported the need of at least 17 grid points per shortest wavelength to avoid the significant numerical dispersion of Rayleigh waves in soft rock.”