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Performance evaluation of a new dual-polarization microphysical algorithm based on long-term X-band radar and disdrometer observations

机译:基于长期X波段雷达和测速仪观测的新型双极化微物理算法的性能评估

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摘要

Accurate estimation of precipitation at high spatial and temporal resolution of weather radars is an open problem in hydrometeorological applications. The use of dual polarization gives the advantage of multiparameter measurements using orthogonal polarization states. These measurements carry significant information, useful for estimating rain-path signal attenuation, drop size distribution (DSD), and rainfall rate. This study evaluates a new self-consistent with optimal parameterization attenuation correction and rain microphysics estimation algorithm (named SCOP-ME). Long-term X-band dual-polarization measurements and disdrometer DSD parameter data, acquired in Athens, Greece, have been used to quantitatively and qualitatively compare SCOP-ME retrievals of median volume diameter D0 and intercept parameter NW with two existing rain microphysical estimation algorithms and the SCOP-ME retrievals of rain rate with three available radar rainfall estimation algorithms. Error statistics for rain rate estimation, in terms of relative mean and root-mean-square error and efficiency, show that the SCOP-ME has low relative error if compared to the other three methods, which systematically underestimate rainfall. The SCOP-ME rain microphysics algorithm also shows a lower relative error statistic when compared to the other two microphysical algorithms. However, measurement noise or other signal degradation effects can significantly affect the estimation of the DSD intercept parameter from the three different algorithms used in this study. Rainfall rate estimates with SCOP-ME mostly depend on the median volume diameter, which is estimated much more efficiently than the intercept parameter. Comparisons based on the long-term dataset are relatively insensitive to pathintegrated attenuation variability and rainfall rates, providing relatively accurate retrievals of the DSD parameters when compared to the other two algorithms.
机译:在气象雷达的高时空分辨率下,准确估算降水是水文气象应用中的一个开放问题。双极化的使用提供了使用正交极化状态进行多参数测量的优势。这些测量结果携带大量信息,可用于估算雨径信号衰减,液滴尺寸分布(DSD)和降雨率。本研究评估了一种新的自洽方法,该方法具有最佳的参数化衰减校正和降雨微物理学估计算法(名为SCOP-ME)。在希腊雅典获得的长期X波段双极化测量和测速仪DSD参数数据已用于定性和定性比较SCOP-ME中位数直径D0和截距参数NW的SCOP-ME取值与现有的两种雨水微物理估算算法SCOP-ME利用三种可用的雷达降雨估计算法检索降雨率。就相对均值和均方根误差及效率而言,降雨率估计的误差统计表明,与其他三种系统地低估降雨的方法相比,SCOP-ME的相对误差较低。与其他两种微物理算法相比,SCOP-ME雨微物理算法还显示出较低的相对误差统计量。但是,测量噪声或其他信号降级影响会严重影响本研究中使用的三种不同算法对DSD截距参数的估计。用SCOP-ME估算降雨率主要取决于中值体积直径,该直径的估算效率比截距参数高得多。基于长期数据集的比较对路径积分衰减变化率和降雨率相对不敏感,与其他两种算法相比,DSD参数的获取相对准确。

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