Backscattering by Nonspherical Hydrometeors as Calculated by the Coupled-Dipole Method: An Application in Radar Meteorology

Backscattering by Nonspherical Hydrometeors as Calculated by the Coupled-Dipole Method: An Application in Radar Meteorology
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耦合偶极子法计算的非球形水凝物后向散射:雷达气象学中的应用

DOI:
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发表时间:
1993
期刊:
影响因子:
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通讯作者:
C. Bohren
C. Bohren
中科院分区:
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文献类型:
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作者:
C. Dungey;C. Bohren

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Abstract The severest test of a theory of scattering by particles is how well it calculates scattering in the backward direction. The coupled-dipole method can be used for accurately calculating backscattering at 94 GHz by hexagonal ice crystals.柱体的后向散射与板体的后向散射明显不同,这表明利用最近开发的毫米波雷达推断冰晶的尺寸和形状分布是可能的。
Abstract The severest test of a theory of scattering by particles is how well it calculates scattering in the backward direction. The coupled-dipole method can be used for accurately calculating backscattering at 94 GHz by hexagonal ice crystals. Backscattering by columns is markedly different from that by plates, which indicates that it might be possible to infer size and shape distributions of ice crystals using recently developed millimeter wave radar.