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Polarimetric Radar Rain Estimation through Retrieval of Drop Size Distribution Using a Bayesian Approach

机译:利用贝叶斯方法反演液滴尺寸分布的极化雷达雨估计

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This study proposes a Bayesian approach to retrieve raindrop size distributions (DSDs) and to estimate rainfall rates from radar reflectivity in horizontal polarization Z_H and differential reflectivity Z_(dr)- With this approach, the authors apply aconstrained-gamma model with an updated constraining relation to retrieve DSD parameters. Long-term DSD measurements made in central Oklahoma by the two-dimensional video disdrometer (2DVD) are first used to construct a prior probability density function(PDF) of DSD parameters, which are estimated using truncated gamma fits to the second, fourth, and sixth moments of the distributions. The forward models of Z_H and Z_(DR) are then developed based on a T-matrix calculation of raindrop backscattering amplitude with the assumption of drop shape. The conditional PDF of Z_H and Z_(DR) is assumed to be a bivariate normal function with appropriate standard deviations. The Bayesian algorithm has a good performance according to the evaluation with simulated Z_H and Z_(DR). The algorithm is also tested on S-band radar data for a mesoscale convective system that passed over central Oklahoma on 13 May 2005. Retrievals of rainfall rates and 1-h rain accumulations are compared with in situ measurements from one 2DVD and six Oklahoma Mesonet rain gauges, located at distances of 28-54 km from Norman, Oklahoma. Results show that the rain estimates from the retrieval agree well with the in situ measurements, demonstrating the validity of the Bayesian retrieval algorithm.
机译:这项研究提出了一种贝叶斯方法来检索雨滴大小分布(DSDs)并根据水平极化Z_H和微分反射率Z_(dr)中的雷达反射率估算降雨率-通过这种方法,作者应用了具有更新约束关系的约束伽马模型检索DSD参数。首先使用二维视频测速仪(2DVD)在俄克拉荷马州中部进行的长期DSD测量来构建DSD参数的先验概率密度函数(PDF),使用第二,第四和第三部分的截断伽马拟合来估算DSD参数分布的第六时刻。然后基于T矩阵计算雨滴反向散射振幅并假设液滴形状,从而开发Z_H和Z_(DR)的正向模型。 Z_H和Z_(DR)的条件PDF假定为具有适当标准偏差的双变量正态函数。根据模拟的Z_H和Z_(DR)进行的评估,贝叶斯算法具有良好的性能。该算法还在2005年5月13日经过俄克拉荷马州中部的中尺度对流系统的S波段雷达数据上进行了测试。将降雨率和1小时雨量的反演结果与1张2DVD和6张俄克拉何马州Mesonet雨的实地测量值进行了比较。仪表,距俄克拉荷马州诺曼市28-54公里。结果表明,反演的降雨估计值与原位测量值吻合良好,证明了贝叶斯反演算法的有效性。

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