Min Zhang, Liming Zhou, Daiguang Fu, Shiqi Dong, Haibo Wu
{"title":"Novel Optimal Staggered Grid Finite Difference Scheme Based on Gram–Schmidt Procedure for Acoustic Wave Modelling","authors":"Min Zhang, Liming Zhou, Daiguang Fu, Shiqi Dong, Haibo Wu","doi":"10.1007/s00024-024-03652-4","DOIUrl":null,"url":null,"abstract":"<div><p>The staggered grid finite difference method is used extensively in numerical simulations of acoustic equations; however, its application is accompanied by numerical dispersion. The most representative traditional method for suppressing the numerical dispersion is the Taylor expansion method, which primarily converts the acoustic equation into a polynomial equation of the trigonometric function and subsequently expands the trigonometric function into a power function polynomial through the Taylor expansion to finally obtain the difference coefficient. However, this traditional method is only applicable to the small wavenumber range. In this study, the Gram–Schmidt orthogonalization method, combined with the binomial theorem and Euler formula was used to reverse the polynomial of power function into a polynomial of trigonometric function and to obtain a new difference coefficient. To highlight the effectiveness of the proposed method, it was compared with the Taylor expansion method (TEM) and the least-squares method (LSM) by selecting a small wavenumber, middle wavenumber, and wide wavenumber ranges. Accuracy and dispersion analyses were conducted. The results showed that the new difference coefficient generated smaller errors and induced stronger suppression of the numerical dispersion. A comparative analysis of the uniform and complex models further validated the superiority of the proposed staggered grid difference coefficient.</p></div>","PeriodicalId":21078,"journal":{"name":"pure and applied geophysics","volume":"182 1","pages":"271 - 287"},"PeriodicalIF":1.9000,"publicationDate":"2025-01-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"pure and applied geophysics","FirstCategoryId":"89","ListUrlMain":"https://link.springer.com/article/10.1007/s00024-024-03652-4","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 0
Abstract
The staggered grid finite difference method is used extensively in numerical simulations of acoustic equations; however, its application is accompanied by numerical dispersion. The most representative traditional method for suppressing the numerical dispersion is the Taylor expansion method, which primarily converts the acoustic equation into a polynomial equation of the trigonometric function and subsequently expands the trigonometric function into a power function polynomial through the Taylor expansion to finally obtain the difference coefficient. However, this traditional method is only applicable to the small wavenumber range. In this study, the Gram–Schmidt orthogonalization method, combined with the binomial theorem and Euler formula was used to reverse the polynomial of power function into a polynomial of trigonometric function and to obtain a new difference coefficient. To highlight the effectiveness of the proposed method, it was compared with the Taylor expansion method (TEM) and the least-squares method (LSM) by selecting a small wavenumber, middle wavenumber, and wide wavenumber ranges. Accuracy and dispersion analyses were conducted. The results showed that the new difference coefficient generated smaller errors and induced stronger suppression of the numerical dispersion. A comparative analysis of the uniform and complex models further validated the superiority of the proposed staggered grid difference coefficient.
期刊介绍:
pure and applied geophysics (pageoph), a continuation of the journal "Geofisica pura e applicata", publishes original scientific contributions in the fields of solid Earth, atmospheric and oceanic sciences. Regular and special issues feature thought-provoking reports on active areas of current research and state-of-the-art surveys.
Long running journal, founded in 1939 as Geofisica pura e applicata
Publishes peer-reviewed original scientific contributions and state-of-the-art surveys in solid earth and atmospheric sciences
Features thought-provoking reports on active areas of current research and is a major source for publications on tsunami research
Coverage extends to research topics in oceanic sciences
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