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Flood changes during the past 50 years in Wujiang River, South China (pages 3561–3569)

机译:洪水在华南河南省过去50年的洪水变化(第3561-3569页)

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摘要

Changing trends of peak flood and flood duration in the Wujiang River Basin are detected with the help of the Mann–Kendall testand the Pettitt analysis during the past 50 years. Results indicate that the peak flood and the flood duration at Lishi Station havedifferent changing features. The peak flood showed only marginally increasing trend, whereas the flood duration exhibiteddecreasing trend at the significance level of 90%. The result shows a weak positive correlation between the peak flood and theflood duration. The changes of flood duration are influenced by the total rainfall duration, which is in downward trend atsignificance level 90%. In addition, the changing trends of peak flood are similar to the total rainfall amount. In the change-pointanalysis, it was found that the change points for the peak flood and flood duration series were in the years 1993 and 1966,respectively. Human activities such as the construction of reservoirs were the main driving forces causing the change of floodduration. The periodicity of the peak flood during the period 1955–2007 at Lishi Station is detected by using the waveletanalysis. The result indicates that the peak flood at Lishi Station displayed alternation between big floods and small floods on the25- to 26-year period. At the same timescale, the peak flood of Wujiang River showed an evidence of change between big floodsand small floods. It was essential to be prepared and aware of the consequences of climate changes and human influencesaffecting the water resources in the Wujiang River Basin. This result is expected to draw more attention from the localgovernments in its decision making and water resource management. Copyright © 2012 John Wiley & Sons, Ltd.
机译:在Mann-Kendall测试的帮助下,检测到乌江流域洪水洪水和洪水持续时间的变化趋势和过去50年的Pettitt分析。结果表明,利什站的峰洪水和洪水持续时间有不同的更改功能。峰值洪水仅表现出略微增加的趋势,而洪水持续时间呈现减少趋势,意义程度为90%。结果表明了峰值洪水与较弱的正相关性洪水持续时间。洪水持续时间的变化受到降雨持续时间的影响,这是下降趋势意义程度90%。此外,峰值洪水的变化趋势与雨量总量类似。在改变点分析,发现峰洪水和洪水持续时间系列的变化点在1993年和1966年,分别。诸如建设水库建设的人类活动是导致洪水变化的主要驱动力期间。利用小波检测在Lishi站的1955 - 2007期间洪水洪水的周期性分析。结果表明,里力站的峰洪水在大洪水和小洪水之间显示出交替25至26期。在相同的时间表,吴江峰洪水洪水展示了大洪水之间变化的证据和小洪水。必须准备和意识到气候变化和人类影响的后果影响乌江流域水资源。这结果预计将更多地引起当地的关注政府在其决策和水资源管理中。版权所有©2012 John Wiley&Sons,Ltd。

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  • 来源
    《Hydrological Processes》 |2012年第23期|p.1-9|共9页
  • 作者单位

    1 School of Geography South China Normal University Guangzhou 510631 China2 CSIRO Mathematics Informatics and Statistics/Environmental Informatics–Water Resources Monitoring and Modelling Private Bag 5 Wembley WA 6913 Australia3 Center for Water Resources and Environment Sun Yat-sen University Guangzhou 510275 China4 Key Laboratory of Water cycle and water security in Southern China of Guangdong Higher Education Institutes Sun Yat-sen University Guangzhou510275 China5 Department of natural resources and Environment Guangdong University of Business Guangzhou 510320 China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    trend analysis; change points; Mann–Kendall test; wavelet analysis;

    机译:趋势分析;改变积分;Mann-Kendall测试;小波分析;

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