...
首页> 外文期刊>Hydrological ProcHydrological Processesrnesses >Flood changes during the past 50 years in Wujiang River, South China
【24h】

Flood changes during the past 50 years in Wujiang River, South China

机译:中国南方吴江过去50年的洪水变化

获取原文
获取原文并翻译 | 示例
   

获取外文期刊封面封底 >>

       

摘要

Changing trends of peak flood and flood duration in the Wujiang River Basin are detected with the help of the Mann–Kendall test and the Pettitt analysis during the past 50 years. Results indicate that the peak flood and the flood duration at Lishi Station have different changing features. The peak flood showed only marginally increasing trend, whereas the flood duration exhibited decreasing trend at the significance level of 90%. The result shows a weak positive correlation between the peak flood and the flood duration. The changes of flood duration are influenced by the total rainfall duration, which is in downward trend at significance level 90%. In addition, the changing trends of peak flood are similar to the total rainfall amount. In the change-point analysis, 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 flood duration. The periodicity of the peak flood during the period 1955–2007 at Lishi Station is detected by using the wavelet analysis. The result indicates that the peak flood at Lishi Station displayed alternation between big floods and small floods on the 25- to 26-year period. At the same timescale, the peak flood of Wujiang River showed an evidence of change between big floods and small floods. It was essential to be prepared and aware of the consequences of climate changes and human influences affecting the water resources in the Wujiang River Basin. This result is expected to draw more attention from the local governments in its decision making and water resource management. Copyright © 2012 John Wiley & Sons, Ltd.
机译:借助Mann–Kendall检验和Pettitt分析,在过去50年中,吴江流域的洪峰高峰和洪灾持续时间变化趋势得以检测。结果表明,离石站洪水高峰和洪水持续时间具有不同的变化特征。洪峰高峰仅表现出小幅增加的趋势,而洪灾持续时间在显着性水平为90%时呈现下降趋势。结果表明,洪水高峰和洪水持续时间之间存在弱的正相关性。洪水持续时间的变化受总降雨持续时间的影响,在显着性水平为90%时呈下降趋势。此外,洪峰的变化趋势与总降雨量相似。在变化点分析中,发现峰值洪水和洪水持续时间序列的变化点分别在1993年和1966年。诸如水库建设等人类活动是导致洪水持续时间发生变化的主要动力。利用小波分析方法检测了离石站1955-2007年洪峰的周期性。结果表明,离石站的洪峰高峰在25至26年间呈现出大洪水和小洪水之间的交替。在同一时间尺度上,乌江的洪峰表明大洪水和小洪水之间发生了变化。必须做好准备,并了解气候变化的后果以及影响乌江流域水资源的人类影响。预期这一结果将引起地方政府在决策和水资源管理方面的更多关注。版权所有©2012 John Wiley&Sons,Ltd.

著录项

  • 来源
  • 作者单位

    School of Geography South China Normal University Guangzhou China;

    CSIRO Mathematics Informatics and Statistics/Environmental Informatics–Water Resources Monitoring and Modelling Wembley WA Australia;

    Center for Water Resources and Environment Sun Yat-sen University Guangzhou China;

    Key Laboratory of Water cycle and water security in Southern China of Guangdong Higher Education Institutes Sun Yat-sen University Guangzhou China;

    Department of natural resources and Environment Guangdong University of Business Guangzhou China;

    Center for Water Resources and Environment Sun Yat-sen University Guangzhou China;

    Key Laboratory of Water cycle and water security in Southern China of Guangdong Higher Education Institutes Sun Yat-sen University Guangzhou China;

  • 收录信息
  • 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;变化点;Mann–Kendall检验;小波分析;

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号