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Two-scale models for rough surface scattering: Comparison between the boundary perturbation method and the integral equation method

机译:粗糙表面散射的两尺度模型:边界摄动法和积分方程法的比较

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This paper presents a comparison between two models for rough surface scattering computations: the boundary perturbation method (BPM) and the integral equation method (IEM). They differ in two fundamental aspects: the method used to compute the electric and magnetic fields on the surface and the surface information required for the computation. The two approaches lead analytically to the same solution in the two asymptotic cases of very large and very small vertical displacements, with no intermediate scales. For a composite surface the solution of the BPM is expressed as the sum of two terms, while a series development up to higher orders can be formulated with the IEM. In this paper, the comparison is restricted to composite surfaces and, particularly, to the ocean surface. After presenting a method for the two-scale decomposition of a rough surface, which satisfies the constraints of the electromagnetic model for each scale, we compute the scattering by the ocean surface using both models for various instrumental configurations and surface conditions. We show that considering the accuracy of usual radar measurements and under the assumptions made for the development of the models, both methods give very similar results. Since the BPM is based on a simple physical argument and appears to be more efficient than the two-scale IEM with regard to the computation time, the BPM should be preferred for ocean-like rough surfaces.
机译:本文对两种用于粗糙表面散射计算的模型进行了比较:边界摄动法(BPM)和积分方程法(IEM)。它们在两个基本方面有所不同:用于计算表面电场和磁场的方法以及计算所需的表面信息。两种方法在垂直位移非常大和很小而没有中间刻度的两种渐近情况下,分析得出相同的解。对于复合表面,BPM的解表示为两个项的总和,而可以使用IEM公式化到更高阶的级数展开。在本文中,比较仅限于复合表面,尤其是海洋表面。在提出了一种满足粗糙面的两尺度分解方法之后,该方法满足了每个尺度的电磁模型的约束条件,我们使用两种模型针对各种仪器配置和表面条件计算了海洋表面的散射。我们表明,考虑到常规雷达测量的准确性,并在为模型开发做出的假设下,两种方法给出的结果非常相似。由于BPM基于简单的物理论证,并且在计算时间方面似乎比两尺度IEM更有效,因此对于海洋般的粗糙表面,应首选BPM。

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