首页> 外文期刊>Quarterly Journal of the Royal Meteorological Society >Background error covariance functions for vector wind analyses using Doppler-radar radial-velocity observations
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Background error covariance functions for vector wind analyses using Doppler-radar radial-velocity observations

机译:使用多普勒雷达径向速度观测值进行矢量风分析的背景误差协方差函数

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摘要

A two-dimensional form of cross-covariance function between the radar radial- and tangential-components (with respect to the direction of radar beam) of background wind errors is derived. Like the previously derived auto-covariance function for the radial component, this cross-covariance function is homogeneous but nonisotropic in the horizontal. The auto- and cross-covariance functions are used with the statistical interpolation technique to perform a vector wind analysis from Doppler radial-velocity observations on a conical surface of low-elevation radar-scans. The structures of the two covariance functions are compared and interpreted in terms of the influence of a single-point radialvelocity observation on the analysed vector wind field. The utility and value of these covariance functions are demonstrated through analysis experiments that use either simulated radial-velocily data from idealized flows or real radar observations. The results of the statistical interpolation scheme utilizing theproposed covariance functions are shown to be superior to the results of traditional VAD technique. The proposed technique can actually be considered a generalization of the traditional VAD technique.
机译:推导了背景风误差的雷达径向分量和切向分量(相对于雷达波束的方向)之间的互协方差函数的二维形式。像先前导出的径向分量的自协方差函数一样,该互协方差函数在水平方向上是同质的,但各向同性。自协方差和交叉协方差函数与统计插值技术一起使用,可从低海拔雷达扫描的圆锥形表面上的多普勒径向速度观测值执行矢量风分析。根据单点径向速度观测对分析的矢量风场的影响,比较和解释了两个协方差函数的结构。这些协方差函数的效用和价值通过分析实验得到了证明,这些实验使用来自理想流的模拟径向速度数据或实际雷达观测值。使用建议的协方差函数的统计插值方案的结果显示出优于传统VAD技术的结果。所提出的技术实际上可以被认为是传统VAD技术的概括。

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