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Study on Retrieving Three-Dimensional Wind Using Simulated Dual-Doppler Radar Data in the Cartesian Space

机译:笛卡尔空间中利用模拟双多普勒雷达数据反演三维风的研究

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This paper investigates a technique of retrieving three-dimensional wind fields from the dual-Doppler weather radar radial wind which is based on the Cartesian space using variational method. This technology provides a simultaneous resolution of three wind components and satisfies both the minimal dual-equation system and the continuity equation. The main advantage of this method is that it can remove the potential drawback of an iterative solution of Cartesian dual-Doppler analysis techniques which is a major demerit when one retrieves the vertical velocity using mass continuity equation with iterative method. The data pre-processing technology and interpolation are also studied. This work developed a three-dimensional Cressman weighting function to process the interpolation. In order to test the capability and advantage of this method, one numerical experiment based on simulating dual-Doppler radar observations is designed.Firstly, we synthesize the dual-Doppler radar radial velocity and reflectivity from the numerical model Then,the three-dimensional wind components are retrieved from the radial velocity and reflectivity using this technique. The retrieved three-dimensional wind fields are found to be quite consisted with those previously simulated wind fields. Mean difference, root-mean-square error, and relative deviation are defined to test the precision of the method. These statistic errors reveal the accuracy and the advantage of this method. The numerical experiment has definitely testified that this technique can be used to retrieve the three-dimensional wind fields from the radial velocity and reflectivity detected by the real dual-Doppler weather radar.
机译:本文研究了一种基于笛卡尔空间的双多普勒天气雷达径向风反演的三维风场的变分方法。这项技术可同时解决三个风分量,并满足最小对偶方程组和连续性方程。该方法的主要优点是,它可以消除笛卡尔双多普勒分析技术的迭代解的潜在缺点,这在使用迭代方法使用质量连续性方程来检索垂直速度时是一个主要缺点。还研究了数据预处理技术和插值。这项工作开发了三维Cressman加权函数来处理插值。为了测试该方法的能力和优势,设计了一个基于模拟双多普勒雷达观测值的数值实验。首先,从数值模型中合成了双多普勒雷达的径向速度和反射率。使用该技术从径向速度和反射率中检索出分量。发现检索到的三维风场与以前模拟的风场完全一致。定义均值差,均方根误差和相对偏差以测试该方法的精度。这些统计误差揭示了此方法的准确性和优势。数值实验无疑证明了该技术可用于从真实双多普勒天气雷达检测到的径向速度和反射率中检索三维风场。

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