Scattering From Fractal Surfaces Based on Decomposition and Reconstruction Theorem

A decomposition and reconstruction theorem (DRT) is introduced to advance computation and provide physical understanding for the scattering from fractal surfaces (FPs). The profile of FP is decomposed into test profiles (TPs), and the scattering of FP is reconstructed using the scattering of TPs to enhance the computational efficiency. A new method that applies DRT on the extended boundary condition method combined with the truncated singular value decomposition technique (TEBCM) is presented and referred to as TEBCM-DRT. The method of TEBCM-DRT is employed to solve the scattering from realistic soil surfaces, and the results are validated against other scattering models. Moreover, the efficiency of TEBCM-DRT and its validity range are investigated. The result shows that TEBCM-DRT improves computational efficiency to 1.95 x 10(5) and 7.35 x 10(2) times, respectively, compared to TEBCM and the conventional method of moments for a wide range of roughness. In addition, TEBCM-DRT indicates that the amplitude and direction of propagation of scattering modes are dependent on deterministic TPs. This relationship benefits for obtaining the accurate height of an arbitrary point on the profile from bistatic scattering coefficients.

Automated summary

The introduction of a Decomposition and Reconstruction Theorem (DRT) enhances computational efficiency and provides physical understanding for scattering from fractal surfaces. The TEBCM-DRT method significantly improves computational efficiency in solving scattering from realistic soil surfaces, demonstrating its validity and efficiency compared to other scattering models.