Prediction of Precipitation Rate Based on Stationary Extreme Value Theory

J. Han
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引用次数: 1

Abstract

For the determination of the effectiveness of weather forecasts such as temperature or flooding forecast, the single variable linear regression or simple exponential smoothing will not be an effective way. To accurately predict the effectiveness of such a trend, iterative and statistical methods that can determine the status of temperature or flooding in the United States were chosen in this paper. The task of modeling the pattern in a focused period and performing data analysis was performed. For the analysis, the extreme value theory was used to assess extreme events within probability distributions by quantifying tail behavior. The python tools are utilized for the analysis of big data. By analyzing the maximum values of samples, it was possible to determine probabilities for extreme events. A comparison was made with events previously observed and analyzed for authenticity. As evident in our observations, lower values of data have much shorter return periods. In other words, they are more likely to reoccur; however, as the values increase for higher precipitation values, the length of the return periods increase exponentially. Therefore, there is a tendency for precipitation values to remain in lower ranges. In this paper, the USGS geographical information and Gumbel distribution were used to find the return period corresponding to the exceedance probability. The Gumbel distribution is applied to Allegheny River, New York and Whetstone River, San Diego.
基于平稳极值理论的降水率预测
对于确定天气预报的有效性,如温度或洪水预报,单变量线性回归或简单的指数平滑将不是一个有效的方法。为了准确预测这种趋势的有效性,本文选择了可以确定美国温度或洪水状况的迭代和统计方法。完成了在重点时间段内对模式建模并执行数据分析的任务。在分析中,采用极值理论通过量化尾部行为来评估概率分布内的极端事件。python工具用于大数据分析。通过分析样本的最大值,可以确定极端事件的概率。与之前观察和分析的事件进行了比较,以确定其真实性。从我们的观察中可以明显看出,数据值越低,返回期就越短。换句话说,它们更有可能再次发生;然而,随着降水值的增加,回归期的长度呈指数增长。因此,降水值有保持在较低范围内的趋势。本文利用USGS的地理信息和Gumbel分布,求出超出概率对应的回归期。甘贝尔分布适用于纽约的阿勒格尼河和圣地亚哥的威特斯通河。
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