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降雨对Ku波段旋转扇形波束散射计影响
引用本文:李佳美,TJUATJASaibun,董晓龙,朱迪.降雨对Ku波段旋转扇形波束散射计影响[J].遥感学报,2013,17(1):98-106.
作者姓名:李佳美  TJUATJASaibun  董晓龙  朱迪
作者单位:中国科学院 空间科学与应用研究中心 微波遥感重点实验室,北京 100190;美国德州大学阿灵顿分校 电机工程波散射理论研究中心,阿灵顿;中国科学院 空间科学与应用研究中心 微波遥感重点实验室,北京 100190;中国科学院 空间科学与应用研究中心 微波遥感重点实验室,北京 100190
基金项目:National Natural Science Foundation of China (No.Y15039A090)
摘    要:星载散射计测量的归一化后向散射截面是有关海面毛细重力波的大小和方向的函数:散射计的回波强度与海面毛细重力波的振幅成正比;风向对后向散射系数具有调制作用。因此,可以利用散射计的数据,根据地球物理模型反演出具有高精确度、无雨和中低风速条件下的海面风场矢量。然而高达10%的散射计测量数据会受到降雨影响(Nie,etal.,2008),尤其工作在Ku波段的散射计。降雨对海面散射幅度的影响主要包括:(1)降雨对雷达波的衰减和散射;(2)降雨改变海洋水面形态和海面粗糙度。

关 键 词:散射计  降雨  多次散射  垂直分布  扇形波束
收稿时间:2011/12/26 0:00:00
修稿时间:2012/6/25 0:00:00

Impact of rainfall on a Ku-band rotating fan-beam scatterometer
LI Jiamei,TJUATJA Saibun,DONG Xiaolong and ZHU Di.Impact of rainfall on a Ku-band rotating fan-beam scatterometer[J].Journal of Remote Sensing,2013,17(1):98-106.
Authors:LI Jiamei  TJUATJA Saibun  DONG Xiaolong and ZHU Di
Institution:Key Laboratory of Microwave Remote Sensing, Center for Space Science and Applied Research, Chinese Academy of Sciences, Beijing 100190, China;Wave Scattering Research Center Department of Electrical Engineering, The University of Texas at Arlington UTA Box 19016, Arlington, USA;Key Laboratory of Microwave Remote Sensing, Center for Space Science and Applied Research, Chinese Academy of Sciences, Beijing 100190, China;Key Laboratory of Microwave Remote Sensing, Center for Space Science and Applied Research, Chinese Academy of Sciences, Beijing 100190, China
Abstract:The effects of rainfall backscattering on space-borne rotating fan-beam scatterometer measurements at Ku-band were investigated in this study. A new scattering model based on Integral Equation Method (IEM) for sea surface with precipitation that accounts for the effects of rain column was presented. The relation between rain scattering and incidence was analyzed, and hence the rain effects on a rotating fan-beam scatterometer are obtained. The rain column is modeled as sublayers with different physical characteristics determined by the vertical profile of rainfall. Each sublayer is assumed to be statistically homogeneous, and the gamma distribution is used to model the drop size distribution within each sublayer. Sea surface is modeled as a rough surface, and its backscattering is calculated using the IEM model. Multiple scattering within and interactions between the rain layers and sea surface are accounted for in the matrix doubling formulation. The presented model is validated using published TRMM PR measurements. Results from model analyses show that rain effects are incident angle dependent, which can lead to non-uniform impacts within the footprint of a fan-beam scatterometer; these effects are strongly related to rain column vertical profile and rain rate, as different rain rate corresponds to different physical parameters.
Keywords:scatterometer  rainfall  multiple scattering  vertical profile  fan-beam
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