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Radar rainfall uncertainty modelling influenced by wind

机译:风云影响的雷达降雨不确定性建模

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Radar-based estimates of rainfall are affected by many sources of uncertainties, which would propagate through the hydrological model when radar rainfall estimates are used as input or initial conditions. An elegant solution to quantify these uncertainties is to model the empirical relationship between radar measurements and rain gauge observations (as the ground reference'). However, most current studies only use a fixed and uniform model to represent the uncertainty of radar rainfall, without consideration of its variation under different synoptic regimes. Wind is such a typical weather factor, as it not only induces error in rain gauge measurements but also causes the raindrops observed by weather radar to drift when they reach the ground. For this reason, as a first attempt, this study introduces the wind field into the uncertainty model and designs the radar rainfall uncertainty model under different wind conditions. We separate the original dataset into three subsamples according to wind speed, which are named as WDI (0-2m/s), WDII (2-4m/s) and WDIII (4m/s). The multivariate distributed ensemble generator is introduced and established for each subsample. Thirty typical events (10 at each wind range) are selected to explore the behaviours of uncertainty under different wind ranges. In each time step, 500 ensemble members are generated, and the values of 5th to 95th percentile values are used to produce the uncertainty bands. Two basic features of uncertainty bands, namely dispersion and ensemble bias, increase significantly with the growth of wind speed, demonstrating that wind speed plays a considerable role in influencing the behaviour of the uncertainty band. On the basis of these pieces of evidence, we conclude that the radar rainfall uncertainty model established under different wind conditions should be more realistic in representing the radar rainfall uncertainty. This study is only a start in incorporating synoptic regimes into rainfall uncertainty analysis, and a great deal of more effort is still needed to build a realistic and comprehensive uncertainty model for radar rainfall data. Copyright (c) 2014 John Wiley & Sons, Ltd.
机译:基于雷达的降雨估计受到许多不确定性来源的影响,当雷达降雨估计用作输入或初始条件时,将通过水文模型传播。优雅的解决方案来量化这些不确定性是模拟雷达测量和雨量仪观测(作为地参考')之间的经验关系。然而,大多数目前的研究只使用固定和统一的模型来代表雷达降雨的不确定性,而不考虑其在不同的舞蹈制度下的变化。风是如此典型的天气系数,因为它不仅在雨量测量测量中引起误差,而且还导致天气雷达观察到的雨滴在到达地面时漂移。出于这个原因,作为第一次尝试,本研究将风力引入不确定性模型,并在不同风条件下设计雷达降雨不确定性模型。我们根据风速将原始数据集分成三个子样本,该风速被命名为WDI(0-2M / s),WDII(2-4M / s)和WDIII(> 4m / s)。为每个子样本引入并建立多变量分布式集合发生器。选择三十个典型事件(每个风距10个)以探索不同风测距下不确定性的行为。在每个时间步骤中,生成500个集合构件,并且第5到第95百分位值的值用于产生不确定性频带。不确定条带的两个基本特征,即色散和集成偏差,随着风速的增长而显着增加,展示风速在影响不确定性频带的行为方面发挥着相当大的作用。在这些证据的基础上,我们得出结论,在不同风力条件下建立的雷达降雨不确定性模型应该更加现实地代表雷达降雨不确定性。本研究只是将舞台制度纳入降雨不确定性分析的开始,仍然需要大量的努力来构建雷达降雨数据的现实和全面的不确定性模型。版权所有(c)2014 John Wiley&Sons,Ltd。

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