基希霍夫区层状粗糙表面电磁波的相干散射

Alireza Tabatabaeenejad, M. Moghaddam
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引用次数: 0

摘要

只提供摘要形式。具有任意层数的层状粗糙表面的电磁波散射在各种环境传感场景中得到应用,例如表征陆地土壤的层状特性。虽然许多这些应用依赖于使用非相干分析的后向散射预测,但需要预测来自分层粗糙表面的相干散射波。本文提出的模型的主要应用是森林地区地下土壤水分的遥感。该模型旨在用于NASA的机载微波观测站(AirMOSS)任务,该任务使用p波段合成孔径雷达,目前收集北美关键(植被)生物群落的数据。从雷达测量数据中获取土壤湿度需要精确有效的前向散射模型。针对植被区存在几种这样的雷达散射模型。这些模型确定了散射机制,包括来自树冠层的散射、树干的散射、树冠层与地面之间的双弹跳散射、树干与地面之间的双弹跳散射以及来自地面的反向散射。研究表明,在P和l波段,树干-地面机制占主导地位,特别是对于高大的林分。此外,正如我们将展示的,在p波段和层状结构中,次表层对入射波的全反射有重要贡献。因此,森林散射模型在模拟双弹跳机制时考虑土层间的相干过程是很重要的。为此,不仅需要相干散射模型,还需要考虑次表层。这项工作计算了基尔霍夫区域内由分层粗糙表面结构散射的波的相干分量,其中假设每个点的散射体表面具有远大于波长的曲率半径。基尔霍夫近似在单一粗糙表面电磁散射中的应用可以追溯到20世纪70年代。一些较新的研究已将这种近似应用于两层粗糙表面的散射问题,其中散射波的计算涉及数值积分。虽然在这项工作中,我们没有对层厚度做任何假设,除了我们隐含地假设它足够大以避免边界之间的空间重叠,我们对表面做了一些假设。我们假设表面不仅有大的曲率半径以允许使用Kirchhoff近似,而且有小的斜率,因此表面轮廓的偏导数将非常小。此外,我们假设粗糙度高度很小,因此散射波的相干分量将占主导地位。我们期望在低频率,如p波段,许多感兴趣的表面满足这些条件。层的边界剖面也假定是不相关的。这些假设将使我们能够用易于求值的代数表达式推导出散射波的简洁解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Coherent scattering of electromagnetic waves from layered rough surfaces within the Kirchhoff regime
Summary form only given. Scattering of electromagnetic waves from layered rough surfaces with an arbitrary number of layers finds applications in diverse environmental sensing scenarios, such as characterizing layering properties of terrestrial soil. While many of these applications rely on backscattering predictions using incoherent analyses, there is a need for prediction of the coherently scattered wave from layered rough surfaces. The primary application of the model presented in this work is remote sensing of subsurface soil moisture in forested regions. This model is intended for use in the NASA Airborne Microwave Observatory of Subcanopy and Subsurface (AirMOSS) mission, which uses a P-band synthetic aperture radar currently collecting data over key (vegetated) biomes of north America. Retrieval of soil moisture from radar measurements requires accurate and efficient forward scattering models. Several such radar scattering models exist for vegetated areas. These models identify scattering mechanisms including scattering from the crown layer, scattering from trunks, double-bounce scattering between the crown layer and ground, double-bounce scattering between trunks and ground, and backscattering from ground. It has been shown that at P- and L-bands, the trunk-ground mechanism becomes dominant, especially for tall stands. Moreover, as we will show, at P-band and in a layered structure, a subsurface layer can have a significant contribution to the total reflection of the incident wave. Therefore, it is important that a forest scattering model consider the coherent processes between soil layers in the modeling of the double-bounce mechanisms. To this end, not only a coherent scattering model is necessary but also subsurface layers should be taken into account. This work calculates the coherent component of the wave scattered by a layered rough surface structure within the Kirchhoff regime, where it is assumed that the scatterer surface at each point has a radius of curvature much larger than the wavelength. Application of the Kirchhoff approximation for electromagnetic scattering from single rough surfaces dates back to the 1970s. Several newer studies have applied this approximation to the problem of scattering from two-layer rough surfaces where calculation of the scattered wave involves numerical integration. While in this work we do not make any assumption about the layer thickness, except we implicitly assume it is large enough to avoid spatial overlaps between the boundaries, we make a few assumptions about the surfaces. We assume the surfaces not only have large radii of curvature to allow the use of the Kirchhoff approximation but also have small slopes so that the partial derivatives of surface profiles would be very small. Moreover, we assume roughness height is small so that the coherent component of the scattered wave would be dominant. We expect that at low frequencies such as P-band, many surfaces of interest satisfy these conditions. The boundary profiles of layers are also assumed to be uncorrelated. These assumptions will allow us to derive a succinct solution for the scattered wave with an algebraic expression that can readily be evaluated.
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