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Detecting changes in extreme precipitation and extreme streamflow in the Dongjiang River Basin in southern China

机译:检测华南东江流域极端降水和极端水流的变化

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摘要

Extreme hydro-meteorological events have become the focus of more and morestudies in the last decade. Due to the complexity of the spatial pattern ofchanges in precipitation processes, it is still hard to establish a clearview of how precipitation has changed and how it will change in the future.In the present study, changes in extreme precipitation and streamflowprocesses in the Dongjiang River Basin in southern China are investigatedwith several nonparametric methods, including one method (Mann-Kendall test)for detecting trend, and three methods (Kolmogorov–Smirnov test, Levene'stest and quantile test) for detecting changes in probability distribution.It was shown that little change is observed in annual extreme precipitationin terms of various indices, but some significant changes are found in theprecipitation processes on a monthly basis, which indicates that whendetecting climate changes, besides annual indices, seasonal variations inextreme events should be considered as well. Despite of little change inannual extreme precipitation series, significant changes are detected inseveral annual extreme flood flow and low-flow series, mainly at thestations along the main channel of Dongjiang River, which are affectedsignificantly by the operation of several major reservoirs. To assess thereliability of the results, the power of three non-parametric methods areassessed by Monte Carlo simulation. The simulation results show that, whileall three methods work well for detecting changes in two groups of data withlarge sample size (e.g., over 200 points in each group) and largedifferences in distribution parameters (e.g., over 100% increase of scaleparameter in Gamma distribution), none of them are powerful enough for smalldata sets (e.g., less than 100 points) and small distribution parameterdifference (e.g., 50% increase of scale parameter in Gamma distribution).The result of the present study raises the concern of the robustness ofstatistical change-detection methods, shows the necessity of combined use ofdifferent methods including both exploratory and quantitative statisticalmethods, and emphasizes the need of physically sound explanation whenapplying statistical test methods for detecting changes.
机译:在过去的十年中,极端的水文气象事件已成为越来越多的研究重点。由于降水过程变化的空间格局的复杂性,仍然很难对降水的变化以及未来的变化有一个清晰的认识。在本研究中,东江的极端降水和水流过程的变化用几种非参数方法对华南盆地进行了调查,包括一种用于检测趋势的方法(Mann-Kendall检验)和用于检测概率分布变化的三种方法(Kolmogorov-Smirnov检验,Levene检验和分位数检验)。从各项指标来看,年度极端降水几乎没有变化,但在降水过程中每月都有一些显着变化,这表明在检测气候变化时,除年度指标外,还应考虑极端事件的季节变化。尽管年极端降水序列变化不大,但在数个年度极端洪水流量和低流量序列中却发现了显着变化,主要发生在东江主干道沿岸的站点上,这些站点受几个主要水库的运行影响很大。为了评估结果的可靠性,蒙特卡洛模拟法探讨了三种非参数方法的功效。仿真结果表明,尽管这三种方法都能很好地检测两组数据的变化,这些数据具有较大的样本量(例如,每组超过200个点)并且分布参数之间的差异较大(例如,Gamma分布的scaleparameter增加了100%以上) ,它们都不具有足够的功能来处理小数据集(例如,少于100个点)和小的分布参数差异(例如,Gamma分布中的比例参数增加50%)。本研究的结果引起了人们对统计变化的鲁棒性的关注-检测方法,显示了同时使用探索性和定量统计方法的不同方法的必要性,并强调了在应用统计测试方法来检测变化时需要有合理的解释。

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