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Modeling, Error Analysis, and Evaluation of Dual-Polarization Variables Obtained from Simultaneous Horizontal and Vertical Polarization Transmit Radar. Part I: Modeling and Antenna Errors

机译:从水平和垂直极化同时发射雷达获得的双极化变量的建模,误差分析和评估。第一部分:建模和天线错误

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摘要

In this two-part paper the biases of polarimetric variables from simultaneous horizontally and vertically transmitted (SHV) data are investigated. Here, in Part I, a radar-scattering model is developed and antenna polarization errors are investigated and estimated. In Part II, experimental data from the National Center for Atmospheric Research S-band dual-polarization Doppler radar (S-Pol) and the National Severe Storms Laboratory polarimetric Weather Surveillance Radar-1988 Doppler (WSR-88D) radar, KOUN, are used to illustrate biases in differential reflectivity (Z_(dr)). The biases in the SHV polarimetric variables are caused by cross coupling of the horizontally (H) and vertically (V) polarized signals. The cross coupling is caused by the following two primary sources: 1) the nonzero mean canting angle of the propagation medium and 2) antenna polarization errors. The biases are strong functions of the differential propagation phase (O_(dP)) and the phase difference between the H and V transmitted field components. The radar-scattering model developed here allows for the evaluation of biases caused by cross coupling as a function of O_(dp), with the transmission phase difference as a parameter. Also, antenna polarization errors are estimated using solar scan measurements in combination with estimates of the radar system's linear depolarization ratio (LDR) measurement limit. Plots are given that show expected biases in SHV Z_(dr) for various values of the LDR system's limit.
机译:在这篇由两部分组成的论文中,研究了水平和垂直同时传输(SHV)数据中偏振变量的偏差。在此,在第一部分中,建立了雷达散射模型,并研究和估计了天线极化误差。在第二部分中,使用了来自美国国家大气研究中心的S波段双极化多普勒雷达(S-Pol)和美国强风暴实验室偏振气象监视雷达1988多普勒(WSR-88D)雷达KOUN的实验数据。以说明差分反射率(Z_(dr))中的偏差。 SHV极化变量中的偏差是由水平(H)和垂直(V)极化信号的交叉耦合引起的。交叉耦合是由以下两个主要来源引起的:1)传播介质的非零平均倾斜角和2)天线极化误差。偏置是差分传播相位(O_(dP))和H和V传输场分量之间的相位差的强大函数。在此开发的雷达散射模型允许以传输相位差为参数,评估由交叉耦合引起的偏置,这些偏置是O_(dp)的函数。而且,天线极化误差是通过太阳扫描测量结合雷达系统线性去极化比(LDR)测量极限的估算来估算的。给出的图显示了LDR系统极限的各种值的SHV Z_(dr)的预期偏差。

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  • 来源
    《Journal of atmospheric and oceanic technology》 |2010年第10期|P.1583-1598|共16页
  • 作者单位

    National Center for Atmospheric Research,Boulder, Colorado;

    rnNational Center for Atmospheric Research,Boulder, Colorado;

    rnNational Center for Atmospheric Research,Boulder, Colorado;

    rnNational Center for Atmospheric Research,Boulder, Colorado;

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