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An Examination of Propagation Effects in Rainfall on Radar Measurements at Microwave Frequencies

机译:降雨对微波频率下雷达测量传播效应的检验

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摘要

Propagation effects in rainfall are examined at three microwave frequencies corresponding to S (3.0 GHz), C (5.5 GHz), and X ( 10.0 GHz) bands. Attenuation at horizontal polarization, as well a s differential attenuation and differential propagation phase between horizontal (HI and vertical ( V ) polarizations are considered. It is shown that at the three frequencies both attenuation and differential attenuation are nearly linearly related to differential propagation phase ( cbDP). This is shown through simulation using ( a ) gamma raindrop size distributions (RSD) with three parameters (No, DO. m ) that are varied over a very wide range representing a variety of rainfall types, and ( b ) measured raindrop size distributions at a single location using a disdrometer. Measurements of X-band specific attenuation and S-band specific differential phase in convective rainshafts using the National Center for Atmospheric Research CP-2 radar are presented in order to experimentally demonstrate the linear relationship between attenuation and differential propagation phase. Correction procedures for reflectivity and differential reflectivity (&) are developed assuming that differential propagation phase is measured using a radar that alternately transmits H and V polarized waves with copolar reception through the same receiver and processor system. The correction procedures are not dependent on the actual rainrate profile between the radar and the range location of interest. The accuracy of the procedure depends on, (a) RSD fluctuations, (b) variability in the estimate of differential propagation phase due to measurement fluctuations, and ( c ) nonzero values of the backscatter differential phase ( & ) between H and V polarizations. Simulations are used to gauge the accuracy of correction procedures at S- and C-bands assuming 6 is negligible. The correction accuracy for attenuation at S-band is estimated to be -0.05 dB while at C-band it is estimated to be within I dB if (IDP G 60 deg). Simulations further indicate that C-band differential attenuations effects can be corrected to within -35% of the mean value.
机译:在对应于S(3.0 GHz),C(5.5 GHz)和X(10.0 GHz)频段的三个微波频率下检查降雨中的传播效应。研究了水平极化时的衰减,以及水平(HI)和垂直(V)极化之间的差分衰减和差分传播相位,结果表明,在三个频率上,衰减和差分衰减都几乎与差分传播相位(cbDP)呈线性关系)。这是通过使用(a)具有三个参数(No,DO。m)的伽玛雨滴大小分布(RSD)进行模拟显示的,这些参数在很宽的范围内变化,代表了各种降雨类型,并且(b)测得的雨滴大小美国国家大气研究中心的CP-2雷达介绍了对流雨井X波段特定衰减和S波段特定微分相位的测量,目的是通过实验证明了衰减与噪声之间的线性关系。差分传播阶段反射率和差分反射率的校正程序vity(&)的开发假设使用一个雷达测量差分传播相位,该雷达通过同一个接收器和处理器系统以同极接收方式交替发送H和V极化波。校正程序不依赖于雷达和目标测距位置之间的实际降雨率分布。该过程的准确性取决于(a)RSD波动,(b)由于测量波动而导致的差分传播相位估计的可变性以及(c)H和V极化之间的反向散射差分相位(&)的非零值。假设6可以忽略不计,可以使用仿真来评估S和C波段校正程序的准确性。 S波段衰减的校正精度估计为-0.05 dB,而C波段,如果(IDP G 60度)估计误差在I dB以内。仿真进一步表明,C波段差分衰减效应可以校正到平均值的-35%以内。

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