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Spatial and temporal variation of extreme precipitation indices in the Yangtze River basin, China

机译:长江流域极端降水指数的时空变化

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摘要

Regional characteristics of extreme precipitation indices (EPI) of precipitation magnitude, intensity and persistence were analyzed based on a daily rainfall dataset of 135 stations during the period of 1961-2010 in the Yangtze River basin, China. The spatial distribution of temporal trends of the selected indices was regionally mapped and investigated by using non-parametric test method. Future projections of EPI changes derived from the output of general circulation model (HadCM3) under the SRES A2 and B2 emission scenarios were downscaled and analyzed. The results show that: (a) there is not a general significant increasing or decreasing trend in EPI for the Yangtze River basin based on historical recorded data;(b) the automated statistical downscaling method-based precipitation captures some spatial distribution of the EPI and the bias correction can improve the simulation results; (c) a mixed pattern of positive and negative changes is observed in most of the nine indices under both scenarios in the first half of twenty-first century, and they increase continuously in the second half of twenty-first century; and (d) the concurrent increase in the heavy rain and drought indices indicates the possibility of the sudden change from drought to water logging in the lower region of Yangtze River basin.
机译:基于1961-2010年长江流域的135个站点的日降水数据集,分析了降水量,强度和持久性的极端降水指数(EPI)的区域特征。使用非参数检验方法对选定指标的时间趋势的空间分布进行了区域映射和调查。在SRES A2和B2排放情景下,由普通循环模型(HadCM3)的输出得出的EPI变化的未来预测已缩小规模并进行了分析。结果表明:(a)基于历史记录数据,长江流域的EPI没有普遍的显着上升或下降趋势;(b)基于自动统计降尺度方法的降水捕捉到了EPI的一些空间分布;偏置校正可以改善仿真结果; (c)在二十一世纪上半叶的两种情况下,九种指数中的大多数都观察到正向和负向变化的混合模式,并在二十一世纪后半叶不断增加; (d)暴雨和干旱指数的同时增加表明长江流域下游地区突然从干旱变为涝灾。

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