A Discussion on the Applicable Condition of Rayleigh Scattering

Nan Li, Yiqing Zhu, Zhenhui Wang
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引用次数: 5

Abstract

Based on the mechanism of particle scattering, rain detection radars are able to receive the backscattering and thus can detect the precipitation particles. For radars with different wavelength, scattering from precipitation particles may be approximated with different kinds of scattering theory, i.e. Mie scattering and Rayleigh scattering. When Mie scattering is used, the computation of the physical quantity that characterizes backscattering of the particle is completed, and the computation is much simpler when Rayleigh scattering is used. In traditional methods, a fixed threshold of the particle scale parameter is used as the criterion to discriminate Rayleigh scattering, that is, the particle size should be smaller than the wavelength of electromagnetic wave. In this work, the analysis on raindrop scattering against radars with different wavelength are discussed. It is concluded that the backscattering cross-section ratio of Mie scattering to Rayleigh scattering is more reasonable than the particle scale parameter for the measure of the criterion to discriminate Rayleigh scattering. Moreover, a small particle compared with the wavelength is a sufficient but not necessary condition for Rayleigh scattering.
瑞利散射适用条件的讨论
基于粒子散射的机理,雨探测雷达能够接收到后向散射,从而探测到降水粒子。对于不同波长的雷达,降水粒子的散射可以用不同的散射理论来近似,即米氏散射和瑞利散射。当使用Mie散射时,完成了表征粒子后向散射的物理量的计算,而使用瑞利散射时计算要简单得多。传统方法采用颗粒尺度参数的固定阈值作为判别瑞利散射的判据,即颗粒尺寸应小于电磁波的波长。本文讨论了雨滴对不同波长雷达的散射特性。结果表明,米氏散射与瑞利散射的后向散射截面比比粒子尺度参数更适合作为瑞利散射判别准则的度量。此外,粒子比波长小是瑞利散射的充分条件,但不是必要条件。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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