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Radar Volume Backscatter From Spatially Extended Geophysical Targets in a “Slice” Approach

机译:通过“切片”方法从空间扩展的地球物理目标进行雷达体积反向散射

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This paper presents an assessment of the radar backscatter from a spatially extended geophysical target (SEGT) based on a semiempirical (SE) model. An SEGT is any geophysical object that is at least semitransparent to radar illumination (clouds, rain, snowfall in the atmosphere, thick snow cover of the ground). The existing SE model does not take into account the statistical properties of the SEGT''s media. To improve the SE model, a so-called “slice” approach is applied. In this approach, the particles located close to the wavefront of the radar illumination are assumed to produce backscatter that is mainly coherent. This method allows the contribution of the microphysical parameters of the scattering media to the volume component of the radar cross section to be described more comprehensively than the SE model based on the incoherent approach. It is shown that the slice concept results in the original SE model in the particular case when the particle number fluctuation within the slices pertains to the Poisson law.
机译:本文提出了基于半经验(SE)模型的空间扩展地球物理目标(SEGT)对雷达反向散射的评估。 SEGT是至少对雷达照明半透明的任何地球物理物体(云,雨,大气中的降雪,地面厚厚的积雪)。现有的SE模型未考虑SEGT媒体的统计属性。为了改善SE模型,应用了所谓的“切片”方法。在这种方法中,假定位于雷达照明波前附近的粒子会产生主要是相干的反向散射。与基于非相干方法的SE模型相比,该方法可以更全面地描述散射介质的微物理参数对雷达横截面体积分量的贡献。结果表明,在特定情况下,当切片中的粒子数量波动符合泊松定律时,切片概念会导致原始SE模型。

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