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Numerical simulations of single and multiple scattering by fractal ice clusters

机译:分形冰簇单散射和多散射的数值模拟

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We consider the scattering model in the form of a vertically and horizontally homogeneous particulate slab of an arbitrary optical thickness composed of widely separated fractal aggregates built of small spherical ice monomers. The aggregates are generated by applying three different approaches, including simulated cluster-cluster aggregation (CCA) and diffusion-limited aggregation (DLA) procedures. Having in mind radar remote-sensing applications, we report and analyze the results of computations of the backscattering circular polarization ratio obtained using efficient superposition T-matrix and vector radiative-transfer codes. The computations have been performed at a wavelength of 12.6cm for fractal aggregates with the following characteristics: monomer refractive index m=1.78+i0.003, monomer radius r=1cm, monomer packing density p=0.2, overall aggregate radii R in the range 4≤R≤10cm and fractal dimensions D_f=2.5 and 3.We show that for aggregates generated with simulated CCA and DLA procedures, the respective values of the backscattering circular polarization ratio differ weakly for D_f=2.5, but the differences can increase somewhat for D_f=3, especially in case of an optically semi-infinite medium. For aggregates with a spheroidal overall shape, the dependence of the circular polarization ratio on the cluster morphology can be quite significant and increases with increasing the aspect ratio of the circumscribing spheroid.
机译:我们以垂直和水平均匀的颗粒板的形式考虑散射模型,该颗粒板具有任意光学厚度,由由小球形冰单体构建的广泛分离的分形聚集体组成。聚合是通过应用三种不同的方法生成的,包括模拟簇-簇聚合 (CCA) 和扩散限制聚合 (DLA) 过程。考虑到雷达遥感应用,我们报告并分析了使用高效叠加T矩阵和矢量辐射传输码获得的后向散射圆极化比的计算结果。在12.6cm的波长下,对具有以下特征的分形聚集体进行了计算:单体折射率m=1.78+i0.003,单体半径r=1cm,单体堆积密度p=0.2,总聚集体半径R在4≤R≤10cm范围内,分形维数D_f=2.5和3.我们表明,对于使用模拟CCA和DLA程序生成的聚集体, 当D_f=2.5时,后向散射圆偏振比的相应值差异较弱,但当D_f=3时,差异可能会有所增加,特别是在光学半无限介质的情况下。对于整体形状为球状的聚集体,圆偏振比对团簇形态的依赖性可能相当显著,并且随着外接球体长宽比的增加而增加。

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