Estimation of Dual Polarization Weather Radar Variables

Dalia A. Mahmood
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引用次数: 1

Abstract

Dual polarization weather radar has now become a widely used as instrument in meteorological offices around the world because of its capability in distinguishing different precipitation type and in improving the accuracy of quantitative precipitation estimation. The aim of this work is to estimate the polarimetry radar variables for radars of different frequency bands and study their behavior with rainfall rates. Calculations of polarimetry radar variables were made on the basis of several assumptions. The results showed that factors at horizontal and vertical polarization, ZH,V, ranges between 20 dBz respectively, and more than 55 dBz for light rain and extreme heavy rain respectively, and radar reflectivity factor at horizontal ZH is greater than radar reflectivity factor at vertical ZV for all rainfall rates. The differential reflectivity, ZDR, also increases with increasing rainfall rates since it is the difference between ZH and Zv. Calculations of specific differential attenuation indicated that X band radars are seriously atten-uated by rain and C band radars are less affected by rain. The specific differential attenuation, S band radars is very small. In addition to this feature, the results showed that the differential phase shift between return signals of horizontal and vertical polarizations for S band radars is much less than those for C and X band radars, and also, the results showed that the co-polarization correlation coefficient for S band the radars is much higher than those of C and X bands. In order to investigate the accuracy of the calculated polarimetric weather radar variables per-formed in this research, real radar measurements were used for this purpose. Results indicated that the range of values for calculated polarimetric radar variables are very consistent with range of values for measured variables
双极化天气雷达变量的估计
双极化天气雷达由于能够区分不同的降水类型,提高降水定量估计的精度,已成为世界各国气象部门广泛使用的气象仪器。本文的目的是估计不同频带雷达的极化雷达变量,并研究其随降雨率的变化规律。在几个假设的基础上进行了极化雷达变量的计算。结果表明:水平和垂直极化因子ZH、V在小雨和极端暴雨时分别在20 dBz和55 dBz之间,且水平ZH的雷达反射率因子大于垂直ZV的雷达反射率因子。差反射率ZDR也随着降雨率的增加而增加,因为它是ZH和Zv之间的差。比差衰减计算表明,X波段雷达受雨的衰减严重,C波段雷达受雨的影响较小。S波段雷达的比差衰减很小。此外,S波段雷达水平和垂直极化回波信号的差相移远小于C波段和X波段雷达,S波段雷达的共极化相关系数远高于C波段和X波段雷达。为了研究本研究中计算的极化气象雷达变量的准确性,为此使用了实际雷达测量数据。结果表明,极化雷达计算变量的取值范围与实测变量的取值范围非常一致
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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