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An improved self-consistent approach to attenuation correction for C-band polarimetric radar measurements and its impact on quantitative precipitation estimation

机译:基于C波段偏振雷达测量的衰减校正及其对定量降水估计的影响改进的自我一致方法

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摘要

Attenuation correction of measured reflectivity (Z(H)) and differential reflectivity (Z(DR)) is critical in short-wavelength radar applications, especially during extreme precipitation events such as heavy rain. This paper develops an improved self-consistent approach (improved ZPHI method) for attenuation correction in practical environment. In particular, a non-negative constraint is imposed on the specific attenuation, which is inferred from the monotonic increasing characteristic of differential propagation phase (Phi(DP)). The copolar correlation coefficient (rho(HV)) is used to partition the Phi(DP) profiles into independent range segments, which are featured by different hydrometeor phases such as liquid rain or mixed-phase precipitation. Additional minimization constraint is imposed on the cost function of the difference between preprocessed Phi(DP) and reconstructed Phi(DP )to ensure its appropriate convergence. In addition, an exponential Z(DR) - Z(H) relation derived from local raindrop size distribution (DSD) data is applied in the procedure of Z(DR) correction. Polarimetric measurements from a C-band radar (CPOL) in Hangzhou of China during two extreme precipitation events are used to demonstrate the improved attenuation correction method. DSD observations from disdrometers and radar data from a nearby system operating at non-attenuated frequency (i.e., S-band) at Huangshan Mountain are used to evaluate the attenuation correction performance. This paper also studies the impact of attenuation correction on the radar-derived quantitative precipitation estimation (QPE) product, through cross-comparison with rain gauge observations. Results show that the polarimetric observations from CPOL radar are effectively enhanced and more consistent with collocated S-band measurements and the simulated radar moments based on DSD data. Hourly rainfall products derived from R(Z(H)) and R(Z(H), Z(DR)) are significantly improved, which are comparable to R(K-DP) after attenuation correction.
机译:测量反射率的衰减校正(Z(H))和差分反射率(Z(DR))在短波长雷达应用中是至关重要的,特别是在极端降水事件(如大雨)期间。本文开发了一种改进的自我一致方法(改进的ZPHI方法),用于实际环境中的衰减校正。特别地,对特定衰减施加非负约束,其从微分传播阶段的单调增加特性推断出(PHI(DP))。共同相关系数(RHO(HV))用于将PHI(DP)轮廓分配成独立的范围段,其由不同的水流仪阶段(例如液体雨或混合相沉淀)特征。对预处理PHI(DP)和重建PHI(DP)之间的差异的成本函数施加了额外的最小化约束,以确保其适当的收敛性。另外,在Z(DR)校正的过程中,应用了从本地雨滴尺寸分布(DSD)数据的指数Z(DR) - Z(H)关系。在两个极端降水事件中,中国杭州C波段雷达(CPOL)的偏振测量用于展示改进的衰减校正方法。来自Disfromers的DSD观察来自在黄山山的非减毒频率(即,S-BAND)的附近系统中的雷达数据用于评估衰减校正性能。本文还通过与雨量计观测的交叉比较来研究衰减校正对衰减校正对雷达衍生的定量降水估计(QPE)产品的影响。结果表明,基于DSD数据,有效地增强了CPOL雷达的直接观测和更加符合并置的S波段测量和模拟雷达时刻。从R(Z(H))和R(Z(H),Z(DR))衍生的每小时降雨产品显着改善,其在衰减校正后与R(K-DP)相当。

著录项

  • 来源
    《Atmospheric research》 |2019年第9期|32-48|共17页
  • 作者单位

    Hangzhou Meteorol Bur Hangzhou 310051 Zhejiang Peoples R China|Zhejiang Inst Meteorol Sci Hangzhou 321000 Zhejiang Peoples R China;

    NOAA Phys Sci Div Earth Syst Res Lab 325 Broadway Boulder CO 80305 USA|Colorado State Univ Cooperat Inst Res Atmosphere Ft Collins CO 80523 USA;

    Chengdu Univ Informat Technol Sch Atmospher Sci 24 Sect 1 Xuefu Rd Chengdu 610225 Sichuan Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    C-band; Polarimetric radar; Attenuation correction; Quantitative precipitation estimation;

    机译:C波段;偏振雷达;衰减校正;定量降水估计;

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