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Identification of temporal fluctuations in the annual flood series of Karoun and Dez rivers in Iran

机译:识别伊朗Karoun和Dez河流年度洪水序列中的时间波动

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Annual flood series in seven main stations in the Large Karoun river (consist of Karoun and Dez rivers) in Iran, measured during 1958 - 2009, were examined to identify the temporal character of changes in flood series . Two approaches were used to evaluate temporal changes in flood series during the period 1958 -2009. The first approach is based on an analysis of standardized departures, and the second approach based on a Multiple trend tests were computed by varying the beginning and ending date ofthe time series.These method are used for identification of an abrupt change in flood series rather than a gradual trend. Results indicate a noticeable step increase in flood series around 1983 rather than as a gradual trend. This step change is that theclimate system has shifted to a new regime that will likely remain relatively constant until a new shift or step change occurs.
机译:研究人员调查了1958年至2009年期间伊朗大卡鲁恩河(由卡鲁恩河和代兹河组成)的七个主要站的年度洪水序列,以确定洪水序列变化的时间特征。在1958年至2009年期间,使用两种方法评估洪水序列的时间变化。第一种方法基于对标准离差的分析,第二种方法是通过更改时间序列的开始和结束日期来计算基于多重趋势检验的方法,这些方法用于识别洪水序列的突然变化,而不是用于识别洪水序列的突然变化逐渐的趋势。结果表明,1983年左右洪水系列明显增加,而不是逐步趋势。这种逐步变化是指气候系统已经转移到一个新的状态,该状态可能会保持相对恒定,直到发生新的变化或逐步变化为止。

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