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首页> 外文期刊>Journal of hydrometeorology >Combining Radar Attenuation and Partial Beam Blockage Corrections for Improved Quantitative Application
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Combining Radar Attenuation and Partial Beam Blockage Corrections for Improved Quantitative Application

机译:结合雷达衰减和部分束阻塞校正,以改进的定量应用

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Partial beam blockage (PBB) correction is an indispensable step in weather radar data quality control and subsequent quantitative applications, such as precipitation estimation, especially in urban and/or complex terrain environments. This paper developed a novel PBB correction procedure based on the improved ZPHI method for attenuation correction and regional specific differential propagation phase (K-DP)-reflectivity (Z(H)) relationship derived from in situ raindrop size distribution (DSD) measurements. The practical performance of this PBB correction technique was evaluated through comparing the spatial continuity of reflectivity measurements, the consistency between radar-measured and DSD-derived K-DP and Z(H) relationships, as well as rainfall estimates based on R(Z(H)) and R(K-DP). The results showed that through incorporating attenuation and PBB corrections (i) the spatial continuity of Z(H) measurements can effectively be enhanced; (ii) the distribution of radar-measured K-DP versus Z(H) is more consistent with the DSD-derived K-DP versus Z(H); (iii) the measured Z(H) from a C-band radar in the PBB-affected area becomes more consistent with collocated S-band measurements, particularly in the rainstorm center area where Z(H) is larger than 30 dBZ; and (iv) rainfall estimates based on R(Z(H)) in the PBB-affected area are incrementally improved with better spatial continuity and the performance tends to be more comparable with R(K-DP).
机译:部分波束阻塞(PBB)校正是天气雷达数据质量控制和后续定量应用(如降水量估算)中不可或缺的一步,尤其是在城市和/或复杂地形环境中。本文基于改进的ZPHI衰减校正方法和由现场雨滴大小分布(DSD)测量得出的区域特定差分传播相位(K-DP)-反射率(Z(H))关系,开发了一种新的PBB校正程序。通过比较反射率测量的空间连续性、雷达测量和DSD得出的K-DP和Z(H)关系之间的一致性,以及基于R(Z(H))和R(K-DP)的降雨量估计,评估了PBB校正技术的实际性能。结果表明,通过结合衰减和PBB校正(i)可以有效地增强Z(H)测量的空间连续性;(ii)雷达测量的K-DP与Z(H)的分布与DSD得出的K-DP与Z(H)的分布更为一致;(iii)从PBB影响区的C波段雷达测得的Z(H)与并置S波段测量值更加一致,尤其是在Z(H)大于30 dBZ的暴雨中心区域;和(iv)基于PBB影响区R(Z(H))的降雨量估计值逐渐改善,具有更好的空间连续性,其性能往往与R(K-DP)更具可比性。

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