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A multistate first-order Markov model for modeling time distribution of extreme rainfall events

机译:一种用于建模极限降雨事件的时间分布的多态一阶马尔可夫模型

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摘要

The time distribution of extreme rainfall events is a significant property that governs the design of urban stormwater management structures. Accuracy in characterizing this behavior can significantly influence the design of hydraulic structures. Current methods used for this purpose either tend to be generic and hence sacrifice on accuracy or need a lot of model parameters and input data. In this study, a computationally efficient multistate first-order Markov model is proposed for use in characterizing the inherently stochastic nature of the dimensionless time distribution of extreme rainfall. The model was applied to bivariate extremes at 10 stations in India and 205 stations in the United States (US). A comprehensive performance evaluation was carried out with one-hundred stochastically generated extremes for each historically observed extreme rainfall event. The comparisons included: 1-h (15-min); 2-h (30-min); and, 3-h (45-min) peak rainfall intensities for India and (US) stations, respectively; number of first, second, third, and fourth-quartile storms; the dependence of peak rainfall intensity on total depth and duration; and, return levels and return periods of peak discharge when these extremes were applied on a hypothetical urban catchment. Results show that the model efficiently characterizes the time distribution of extremes with: Nash-Sutcliffe-Efficiency 0.85 for peak rainfall intensity and peak discharge; 20% error in reproducing different quartile storms; and, 0.15 error in correlation analysis at all study locations. Hence the model can be used to effectively reproduce the time distribution of extreme rainfall events, thus increasing the confidence of design of urban stormwater management structures.
机译:极端降雨事件的时间分配是一个重要的财产,管辖城市雨水管理结构的设计。表征这种行为的准确性可以显着影响液压结构的设计。用于此目的的当前方法往往是通用的,因此牺牲精度或需要大量的模型参数和输入数据。在本研究中,提出了一种计算效率的多岩一阶马尔可夫模型,用于表征极端降雨的无量纲时间分布的固有随机性质。该模型应用于印度的10站和美国(美国)的205个站点的双重电台。在历史上观察到的极端降雨事件中,用一百个随机产生的极端进行全面的绩效评估。包括比较:1-H(15分钟); 2-H(30分钟); 3-H(45分钟)峰值降雨增长,分别为印度和(美国)站;第一,第二,第三和第四四分之三的暴风雨的数量;峰值降雨强度对总深度和持续时间的依赖性;并且,当这些极端应用于假设的城市集水区时,返回水平和峰值放电的返回期。结果表明,该模型有效地表征了极端的时间分布:NASH-SUTCLIFFE-效率> 0.85峰值降雨强度和峰值放电; &再现不同的四分位数风暴20%的错误;并且,&所有研究位置的相关分析中的0.15误差。因此,该模型可用于有效地重现极端降雨事件的时间分布,从而提高了城市雨水管理结构的置信度。

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