On the implementation of perfectly matched layers in a three‐dimensional fourth‐order velocity‐stress finite difference scheme

By C. Marcinkovich, Kim B. Olsen. 2003

136 citations recorded by the source corpus.

Subfields: Electrical and Electronic Engineering, Geophysics

View Paper: https://www.semanticscholar.org/paper/26a9e28ebd511258131bb07fb5bca844c095cb4d

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Electrical and Electronic Engineering

1. Wei Zhang
2. Yang Shen
3. Thomas H. Jordan
4. Pengcheng Liu
5. S. Hartzell
6. R. Archuleta
7. Steven M. Day
8. Po Chen

In Geophysics

1. Po Chen
2. Thomas H. Jordan
3. Yang Shen
4. Li Zhao
5. Qinya Liu
6. Wei Zhang
7. R. Archuleta
8. Steven M. Day

Citations in the corpus

• Frechet Kernels for Imaging Regional Earth Structure Based on Three-Dimensional Reference Models (2005, methodology): “…finite-difference algorithm includes an accurate treatment of the free-surface boundary condition (Gottschaemmer and Olsen, 2001) and adopts the method of perfectly matched layers (PML) formulated for fourth-order staggered grids for the absorbing boundary condition (Marcinkovich and Olsen, 2003).”
• Unsplit complex frequency-shifted PML implementation using auxiliary differential equations for seismic wave modeling (2010, methodology): “…1994 , an ABL technique, effectively absorb waves at a wide range of incident angles with only several to tens of layers and has become widely used in elastic wave modeling Chew and Liu, 1996; Hastings et al., 1996; Collino and Tsogka, 2001; Marcinkovich and Olsen, 2003; Wang and Tang, 2003 .”
• Strong shaking in Los Angeles expected from southern San Andreas earthquake (2006, methodology): “, 2003], and Perfectly Matched Layers (PML) absorbing boundary conditions on the sides and bottom [Marcinkovich and Olsen, 2003].”
• Prediction of Broadband Ground-Motion Time Histories: Hybrid Low/High- Frequency Method with Correlated Random Source Parameters (2006, methodology): “This FD code uses the perfectly matched layer method to model an artificial boundary (Collino and Tsogka, 2001; Marcinkovich and Olsen, 2003) and a coarse-grained method to model attenuation (Day and Bradley, 2001; Liu and Archuleta, 2006).”
• The ShakeOut earthquake scenario: Verification of three simulation sets (2010, methodology): “In contrast, SDSU/SDSC uses a more accurate implementation based on the multi-axial perfectly matching layers (M-PML) adapted from the original formulation in electromagnetism by Berenger (1994) and its implementation in a staggered grid by Marcinkovich & Olsen (2003).”
• The Newmark scheme as velocity–stress time-staggering: an efficient PML implementation for spectral element simulations of elastodynamics (2005, background): “…wave propagation (Chew & Liu 1996; Hastings et al. 1996; Liu & Tao 1997; Collino & Tsogka 2001; Festa & Nielsen 2003; Komatitsch & Tromp 2003; Marcinkovich & Olsen 2003; Wang & Tang 2003), anisotropic elasticity (Collino & Tsogka 2001; Bécache et al. 2003), poroelasticity (Zeng et al. 2001)…”
• A support-operator method for viscoelastic wave modelling in 3-D heterogeneous media (2008, background): “Marcinkovich & Olsen (2003) present a PML absorbing boundary condition for the velocity-stress formulation of elastodynamics.”