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Second-order multiple-scattering theory associated with backscattering enhancement for a millimeter wavelength weather radar with a finite beam width

机译:与有限波束宽度的毫米波波长气象雷达的反向散射增强相关的二阶多重散射理论

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摘要

Effects of multiple scattering on reflectivity are studied for millimeter wavelength weather radars. A time-independent vector theory, including up to second-order scattering, is derived for a single layer of hydrometeors of a uniform density and a uniform diameter. In this theory, spherical waves with a Gaussian antenna pattern are used to calculate ladder and cross terms in the analytical scattering theory. The former terms represent the conventional multiple scattering, while the latter terms cause backscattering enhancement in both the copolarized and cross-polarized components. As the optical thickness of the hydrometeor layer increases, the differences from the conventional plane wave theory become more significant, and essentially, the reflectivity of multiple scattering depends on the ratio of mean free path to radar footprint radius. These results must be taken into account when analyzing radar reflectivity for use in remote sensing.
机译:对于毫米波长天气雷达,研究了多重散射对反射率的影响。对于具有均匀密度和均匀直径的单层水凝物,推导了一个时间无关的矢量理论,包括高达二阶的散射。在此理论中,具有高斯天线方向图的球面波被用于计算解析散射理论中的阶梯项和正交项。前一项表示常规的多次散射,而后一项则引起同极化和交叉极化分量的反向散射增强。随着水凝膜层光学厚度的增加,与常规平面波理论的差异变得更加明显,并且本质上,多重散射的反射率取决于平均自由程与雷达足迹半径的比率。分析用于遥感的雷达反射率时,必须考虑这些结果。

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