High-order exponential integration for seismic wave modeling

IF 2.1 3区 地球科学 Q3 COMPUTER SCIENCE, INTERDISCIPLINARY APPLICATIONS
Fernando V. Ravelo, Martin Schreiber, Pedro S. Peixoto
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引用次数: 0

Abstract

Seismic imaging is a major challenge in geophysics with broad applications. It involves solving wave propagation equations with absorbing boundary conditions (ABC) multiple times. This drives the need for accurate and efficient numerical methods. This study examines a collection of exponential integration methods, known for their good numerical properties on wave representation, to investigate their efficacy in solving the wave equation with ABC. The purpose of this research is to assess the performance of these methods. We compare a recently proposed Exponential Integration based on Faber polynomials with well-established Krylov exponential methods alongside a high-order Runge-Kutta scheme and low-order classical methods. Through our analysis, we found that the exponential integrator based on the Krylov subspace exhibits the best convergence results among the high-order methods. We also discovered that high-order methods can achieve computational efficiency similar to low-order methods while allowing for considerably larger time steps. Most importantly, the possibility of undertaking large time steps could be used for important memory savings in full waveform inversion imaging problems.

Abstract Image

地震波建模的高阶指数积分法
地震成像是地球物理学的一项重大挑战,具有广泛的应用前景。它涉及多次求解具有吸收边界条件 (ABC) 的波传播方程。这就需要精确高效的数值方法。本研究考察了一系列指数积分方法,这些方法以其在波表示方面的良好数值特性而著称,研究它们在求解带 ABC 的波方程时的功效。本研究的目的是评估这些方法的性能。我们将最近提出的基于 Faber 多项式的指数积分法与成熟的 Krylov 指数法、高阶 Runge-Kutta 方案和低阶经典方法进行了比较。通过分析,我们发现基于 Krylov 子空间的指数积分法在高阶方法中表现出最佳的收敛效果。我们还发现,高阶方法可以实现与低阶方法类似的计算效率,同时允许更大的时间步长。最重要的是,在全波形反演成像问题中,可以利用大时间步长来节省内存。
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来源期刊
Computational Geosciences
Computational Geosciences 地学-地球科学综合
CiteScore
6.10
自引率
4.00%
发文量
63
审稿时长
6-12 weeks
期刊介绍: Computational Geosciences publishes high quality papers on mathematical modeling, simulation, numerical analysis, and other computational aspects of the geosciences. In particular the journal is focused on advanced numerical methods for the simulation of subsurface flow and transport, and associated aspects such as discretization, gridding, upscaling, optimization, data assimilation, uncertainty assessment, and high performance parallel and grid computing. Papers treating similar topics but with applications to other fields in the geosciences, such as geomechanics, geophysics, oceanography, or meteorology, will also be considered. The journal provides a platform for interaction and multidisciplinary collaboration among diverse scientific groups, from both academia and industry, which share an interest in developing mathematical models and efficient algorithms for solving them, such as mathematicians, engineers, chemists, physicists, and geoscientists.
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