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Sixth-order accurate pseudo-spectral method for solving one-way wave equation. / Pleshkevich, Alexander; Vishnevskiy, Dmitriy; Lisitsa, Vadim.

In: Applied Mathematics and Computation, Vol. 359, 15.10.2019, p. 34-51.

Research output: Contribution to journalArticlepeer-review

Harvard

Pleshkevich, A, Vishnevskiy, D & Lisitsa, V 2019, 'Sixth-order accurate pseudo-spectral method for solving one-way wave equation', Applied Mathematics and Computation, vol. 359, pp. 34-51. https://doi.org/10.1016/j.amc.2019.04.029

APA

Pleshkevich, A., Vishnevskiy, D., & Lisitsa, V. (2019). Sixth-order accurate pseudo-spectral method for solving one-way wave equation. Applied Mathematics and Computation, 359, 34-51. https://doi.org/10.1016/j.amc.2019.04.029

Vancouver

Pleshkevich A, Vishnevskiy D, Lisitsa V. Sixth-order accurate pseudo-spectral method for solving one-way wave equation. Applied Mathematics and Computation. 2019 Oct 15;359:34-51. doi: 10.1016/j.amc.2019.04.029

Author

Pleshkevich, Alexander ; Vishnevskiy, Dmitriy ; Lisitsa, Vadim. / Sixth-order accurate pseudo-spectral method for solving one-way wave equation. In: Applied Mathematics and Computation. 2019 ; Vol. 359. pp. 34-51.

BibTeX

@article{e69fdcb343334901808117e6aff86a54,
title = "Sixth-order accurate pseudo-spectral method for solving one-way wave equation",
abstract = "In this paper, we present a pseudo-spectral method to solve the one-way wave equation. The approach is a generalization of the phase-shift plus interpolation technique which is used in geophysical applications. We construct a solution at each depth layer as a linear combination of the solutions corresponding to the models with uniform reference velocities. We suggest using three-term relations to interpolate the solution with the sixth order of accuracy to the deviation from the vertical direction. Standard phase-shift plus interpolation technique uses two-terms relation interpolating the solution with the fourth order. As a result, the numerical error of the suggested approach is one half of that of the PSPI methods for a fixed set of reference velocities for a wide range of spatial discretizations and directions of wave propagation. Consequently, to compute a solution with prescribed accuracy, the presented approach allows using 20% fewer reference velocities than the PSPI. Additionally provided experiments illustrate the efficiency of the suggested approach for simulation of down-going wave propagation in complex geological media, making the algorithm a promising one for the seismic imaging procedures.",
keywords = "Numerical dispersion, One-way wave equation, Pseudo-spectral methods, MIGRATION, DISCONTINUOUS-GALERKIN, APPROXIMATION, BOUNDARY-CONDITIONS, INTERPOLATION, SCHEME, ELEMENT, NUMERICAL-SIMULATION, FINITE-DIFFERENCE, PROPAGATION",
author = "Alexander Pleshkevich and Dmitriy Vishnevskiy and Vadim Lisitsa",
note = "Publisher Copyright: {\textcopyright} 2019 Elsevier Inc.",
year = "2019",
month = oct,
day = "15",
doi = "10.1016/j.amc.2019.04.029",
language = "English",
volume = "359",
pages = "34--51",
journal = "Applied Mathematics and Computation",
issn = "0096-3003",
publisher = "Elsevier Science Inc.",

}

RIS

TY - JOUR

T1 - Sixth-order accurate pseudo-spectral method for solving one-way wave equation

AU - Pleshkevich, Alexander

AU - Vishnevskiy, Dmitriy

AU - Lisitsa, Vadim

N1 - Publisher Copyright: © 2019 Elsevier Inc.

PY - 2019/10/15

Y1 - 2019/10/15

N2 - In this paper, we present a pseudo-spectral method to solve the one-way wave equation. The approach is a generalization of the phase-shift plus interpolation technique which is used in geophysical applications. We construct a solution at each depth layer as a linear combination of the solutions corresponding to the models with uniform reference velocities. We suggest using three-term relations to interpolate the solution with the sixth order of accuracy to the deviation from the vertical direction. Standard phase-shift plus interpolation technique uses two-terms relation interpolating the solution with the fourth order. As a result, the numerical error of the suggested approach is one half of that of the PSPI methods for a fixed set of reference velocities for a wide range of spatial discretizations and directions of wave propagation. Consequently, to compute a solution with prescribed accuracy, the presented approach allows using 20% fewer reference velocities than the PSPI. Additionally provided experiments illustrate the efficiency of the suggested approach for simulation of down-going wave propagation in complex geological media, making the algorithm a promising one for the seismic imaging procedures.

AB - In this paper, we present a pseudo-spectral method to solve the one-way wave equation. The approach is a generalization of the phase-shift plus interpolation technique which is used in geophysical applications. We construct a solution at each depth layer as a linear combination of the solutions corresponding to the models with uniform reference velocities. We suggest using three-term relations to interpolate the solution with the sixth order of accuracy to the deviation from the vertical direction. Standard phase-shift plus interpolation technique uses two-terms relation interpolating the solution with the fourth order. As a result, the numerical error of the suggested approach is one half of that of the PSPI methods for a fixed set of reference velocities for a wide range of spatial discretizations and directions of wave propagation. Consequently, to compute a solution with prescribed accuracy, the presented approach allows using 20% fewer reference velocities than the PSPI. Additionally provided experiments illustrate the efficiency of the suggested approach for simulation of down-going wave propagation in complex geological media, making the algorithm a promising one for the seismic imaging procedures.

KW - Numerical dispersion

KW - One-way wave equation

KW - Pseudo-spectral methods

KW - MIGRATION

KW - DISCONTINUOUS-GALERKIN

KW - APPROXIMATION

KW - BOUNDARY-CONDITIONS

KW - INTERPOLATION

KW - SCHEME

KW - ELEMENT

KW - NUMERICAL-SIMULATION

KW - FINITE-DIFFERENCE

KW - PROPAGATION

UR - http://www.scopus.com/inward/record.url?scp=85065253849&partnerID=8YFLogxK

U2 - 10.1016/j.amc.2019.04.029

DO - 10.1016/j.amc.2019.04.029

M3 - Article

AN - SCOPUS:85065253849

VL - 359

SP - 34

EP - 51

JO - Applied Mathematics and Computation

JF - Applied Mathematics and Computation

SN - 0096-3003

ER -

ID: 20051335