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Doubly stochastic Poisson pulse model for fine-scale rainfall

机译:精细降雨的双随机泊松脉冲模型

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Stochastic rainfall models are widely used in hydrological studies because they provide a framework not only for deriving information about the characteristics of rainfall but also for generating precipitation inputs to simulation models whenever data are not available. A stochastic point process model based on a class of doubly stochastic Poisson processes is proposed to analyse finescale point rainfall time series. In this model, rain cells arrive according to a doubly stochastic Poisson process whose arrival rate is determined by a finite-state Markov chain. Each rain cell has a random lifetime. During the lifetime of each rain cell, instantaneous random depths of rainfall bursts (pulses) occur according to a Poisson process. The covariance structure of the point process of pulse occurrences is studied. Moment properties of the time series of accumulated rainfall in discrete time intervals are derived to model 5-min rainfall data, over a period of 69 years, from Germany. Second-moment as well as thirdmoment properties of the rainfall are considered. The results show that the proposed model is capable of reproducing rainfall properties well at various sub-hourly resolutions. Incorporation of third-order moment properties in estimation showed a clear improvement in fitting. A good fit to the extremes is found at larger resolutions, both at 12-h and 24-h levels, despite underestimation at 5-min aggregation. The proportion of dry intervals is studied by comparing the proportion of time intervals, from the observed and simulated data, with rainfall depth below small thresholds. A good agreement was found at 5-min aggregation and for larger aggregation levels a closer fit was obtained when the threshold was increased. A simulation study is presented to assess the performance of the estimation method.
机译:随机降雨模型在水文学研究中被广泛使用,因为它们不仅提供了一个框架来导出有关降雨特征的信息,而且还在没有数据的情况下为模拟模型生成降雨输入提供了框架。提出了基于一类双重随机泊松过程的随机点过程模型,以分析细尺度点降雨时间序列。在该模型中,雨单元根据双重随机泊松过程到达,其到达速度由有限状态马尔可夫链决定。每个雨单元的寿命都是随机的。在每个雨单元的生命周期中,根据泊松过程会出现瞬时随机深度的降雨突发(脉冲)。研究了脉冲发生点过程的协方差结构。离散时间间隔内累积降雨的时间序列的矩量特性来自于德国,以模拟5分钟的降雨数据,历时69年。考虑降雨的第二矩和第三矩特性。结果表明,所提出的模型能够在不同的亚小时分辨率下很好地再现降雨特性。在估算中纳入三阶矩特性显示出拟合的明显改善。尽管在5分钟的聚集时间中低估了分辨率,但在12h和24h的较大分辨率下都可以很好地适应极端情况。通过比较观察到的和模拟的数据中时间间隔的比例与降雨深度低于小阈值的时间间隔的比例,来研究干旱间隔的比例。在聚合时间为5分钟时发现了良好的一致性,对于较大的聚合水平,当阈值增加时,获得了更接近的拟合度。进行了仿真研究,以评估估计方法的性能。

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