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首页> 外文期刊>Hydrology and Earth System Sciences >Detecting changes in extreme precipitation and extreme streamflow in the Dongjiang River Basin in southern China
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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 more studies in the last decade. Due to the complexity of the spatial pattern of changes in precipitation processes, it is still hard to establish a clear view of how precipitation has changed and how it will change in the future. In the present study, changes in extreme precipitation and streamflow processes in the Dongjiang River Basin in southern China are investigated with several nonparametric methods, including one method (Mann-Kendall test) for detecting trend, and three methods (Kolmogorov-Smirnov test, Levene's test and quantile test) for detecting changes in probability distribution. It was shown that little change is observed in annual extreme precipitation in terms of various indices, but some significant changes are found in the precipitation processes on a monthly basis, which indicates that when detecting climate changes, besides annual indices, seasonal variations in extreme events should be considered as well. Despite of little change in annual extreme precipitation series, significant changes are detected in several annual extreme flood flow and low-flow series, mainly at the stations along the main channel of Dongjiang River, which are affected significantly by the operation of several major reservoirs. To assess the reliability of the results, the power of three non-parametric methods are assessed by Monte Carlo simulation. The simulation results show that, while all three methods work well for detecting changes in two groups of data with large sample size (e.g., over 200 points in each group) and large differences in distribution parameters (e.g., over 100% increase of scale parameter in Gamma distribution), none of them are powerful enough for small data sets (e.g., less than 100 points) and small distribution parameter difference (e.g., 50% increase of scale parameter in Gamma distribution). The result of the present study raises the concern of the robustness of statistical change-detection methods, shows the necessity of combined use of different methods including both exploratory and quantitative statistical methods, and emphasizes the need of physically sound explanation when applying 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研究的焦点。由于降水过程变化的空间模式的复杂性,仍然很难就降水如何变化以及未来如何变化建立清晰的视图。在本研究中,使用几种非参数方法研究了华南东江流域极端降水和流量过程的变化,包括一种用于检测趋势的方法(Mann-Kendall检验)和三种方法(Kolmogorov-Smirnov检验,Levene检验)。测试和分位数测试)来检测概率分布的变化。结果表明,从各项指标来看,年度极端降水几乎没有变化,但在每月降水过程中却发现了一些显着变化,这表明在检测气候变化时,除年度指标外,极端事件的季节性变化也应该考虑。尽管年度极端降水量序列变化不大,但在几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,这受到几个主要水库运行的影响。为了评估结果的可靠性,通过蒙特卡洛模拟评估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)并且分布参数的差异较大(例如,比例参数增加了100%以上)在Gamma分布中),它们都没有足够强大的功能来处理较小的数据集(例如,少于100个点)和较小的分布参数差异(例如,在Gamma分布中缩放参数增加50%)。本研究的结果引起了人们对统计变化检测方法的鲁棒性的关注,表明了结合使用包括探索性和定量统计方法在内的不同方法的必要性,并强调了在将统计测试方法应用于以下方面时,需要有合理的解释。检测变化。

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