High-Order Accurate Method for Solving the Anisotropic Eikonal Equation

U. Waheed
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Abstract

High frequency asymptotic methods, based on solving the eikonal equation, are widely used in many seismic applications including Kirchhoff migration and traveltime tomography. Finite difference methods to solve the eikonal equation are computationally more efficient and attractive than ray tracing. But, finite difference solution of the eikonal equation for a point source suffers from inaccuracies due to singularity at the source location. Since the curvature of wavefront is large in the source neighborhood, the truncation error of the finite difference approximation is also significant, leading to inaccuracies in the solution. Compared to several proposed approaches to tackle source singularity, factorization of the unknown traveltime is computationally efficient and simpler to implement. Recently, a factorization algorithm has been proposed to obtain clean first order accuracy for tilted transversely isotropic (TTI) media. However, high order accuracy of traveltimes is needed for quantities that require computation of traveltime derivatives, such as take off angle and amplitude. I propose an iterative fast sweeping algorithm to obtain high order accuracy using factorization followed by Weighted Essentially Non-oscillatory (WENO) approximation of the derivatives. Although this method yields highly accurate traveltimes but it also results in increased computational load. Therefore, I propose a parallel fast sweeping algorithm to compute fast and accurate solution of the anisotropic eikonal equation. High accuracy is achieved first by using factorization followed by the WENO approximation of derivatives, whereas computational speed up is obtained by sweeping the computational domain in parallel. With a large number of CPUs, significant reduction in computational cost can be achieved for large 3D models. Numerical test shows improvements in accuracy of the TTI eikonal solution.
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求解各向异性正交方程的高阶精确方法
基于求解方程的高频渐近方法在基尔霍夫偏移和走时层析成像等地震应用中得到了广泛的应用。有限差分法在计算上比光线追踪法更有效、更有吸引力。但是,点源方程的有限差分解由于源位置的奇异性而存在不准确性。由于源附近波前曲率较大,有限差分近似的截断误差也较大,导致解不准确。与已有的几种解决源奇点的方法相比,未知旅行时间的分解计算效率高,实现简单。近年来,为了获得倾斜横各向同性(TTI)介质的一阶精度,提出了一种分解算法。然而,对于起飞角和振幅等需要计算行程时间导数的量,需要高阶精度的行程时间。我提出了一个迭代快速扫描算法,以获得高阶精度,使用因式分解,然后加权本质非振荡(WENO)近似的导数。虽然这种方法产生了高精度的行程时间,但也增加了计算量。为此,本文提出了一种并行快速扫描算法来快速准确地求解各向异性方程。首先采用因式分解,然后对导数进行WENO逼近,从而获得较高的精度,同时采用并行扫描计算域的方法提高了计算速度。使用大量的cpu,可以显著降低大型3D模型的计算成本。数值试验结果表明,TTI模型解的精度有所提高。
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