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基于经验模态分解方法和信息熵的水沙关系研究
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  • 英文篇名:Study on relationship between water and sediment based on empirical mode decomposition and information entropy
  • 作者:张金萍 ; 肖宏林 ; 张鑫
  • 英文作者:ZHANG Jinping;XIAO Honglin;ZHANG Xin;College of Water Conservancy and Environment,Zhengzhou University;
  • 关键词:径流量 ; 输沙量 ; 经验模态分解方法 ; 信息熵 ; 互信息 ; 黄河中游
  • 英文关键词:runoff;;sediment load;;empirical mode decomposition;;information entropy;;mutual information;;middle reaches of Yellow River
  • 中文刊名:SZYB
  • 英文刊名:Water Resources Protection
  • 机构:郑州大学水利与环境学院;
  • 出版日期:2019-07-20
  • 出版单位:水资源保护
  • 年:2019
  • 期:v.35
  • 基金:国家重点研发计划(2018YFC0406501);; 郑州大学2015年优秀青年教师发展(1521323002);; 2018年度河南省高校科技创新人才支持计划(18HASTIT014);; 中国水利水电科学研究院流域水循环模拟与调控国家重点实验室开放基金(IWHR-SKL-KF201802);; 天津大学水利工程仿真与安全国家重点实验室(HESS-1717);; 河南省高等学校青年骨干教师培养计划(2017GGJS006)
  • 语种:中文;
  • 页:SZYB201904005
  • 页数:6
  • CN:04
  • ISSN:32-1356/TV
  • 分类号:34-38+45
摘要
为研究黄河中游水沙关系及其细部演化特征,利用黄河中游控制性水文站——潼关水文站1919—2015年实测径流量和输沙量资料作为研究数据,采用经验模态分解方法分析径流和泥沙随机变化的复杂性,并运用信息熵理论计算不同时间尺度上径流和泥沙分解序列及原始序列的熵值、径流与泥沙各分量与其原始序列之间的互信息、径流与泥沙之间的互信息。结果表明:潼关水文站径流量与输沙量变化具有显著下降的趋势;径流量和输沙量在一定程度上表现为某种同步变化关系;径流量与输沙量的长周期分量及趋势项互信息较大,因此水沙关系宜采用长周期研究,趋势项分量数据信息阐述原始序列数据信息比较可靠。
        In order to study the relationship between water and sediment in the middle reaches of the Yellow River and its detailed evolution characteristics, the empirical mode decomposition method was used to analyze the complexity of random variation of runoff and sediment load based on the measured runoff and sediment discharge data from 1919 to 2015 at Tongguan Hydrological Station, a controlling hydrological station in the middle reaches of the Yellow River. The information entropy theory was used to calculate the entropy values of the decomposition sequence and original sequence of runoff and sediment load at different time scales. The mutual information entropy values between runoff and sediment sequences and between their decomposition sequences and original sequences were calculated too. The results show that the change of runoff and sediment load at Tongguan Hydrological Station has a significant downward trend. The relationship between runoff and sediment load is synchronous to some extent. The long-period components and residual components of runoff and sediment load have great mutual information, so studies of the relationship between water and sediment should be focused on their long-period scales. The original data information can be described by the residual components reliably.
引文
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