“黄河流域水循环动力机制与模拟”专题研究

黄河上中游天然径流多时间尺度变化及动因分析

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  • 1. 北京师范大学环境科学研究所, 北京 100875;
    2. 中国科学院地理科学与资源研究所, 北京 100101;
    3. 西安理工大学, 陕西西安 710048
蒋晓辉(1972~),男,北京师范大学环境科学研究所博士后,研究方向为水文水资源.

收稿日期: 2002-08-29

  修回日期: 2002-12-30

  网络出版日期: 2003-04-25

基金资助

国家重点基础研究规划项目“黄河流域水资源演化规律与可再生性维持机理”(G1999043601)资助.

Multple time scales analysis and cause of runoff changes of the upper and middle reaches of the Yellow River

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  • 1. Institute of Environmental Sciences, Beijing Normal University, Beijing 100875, China;
    2. Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101, China;
    3. Xi'an University of Technology, Xi'an 710048, China

Received date: 2002-08-29

  Revised date: 2002-12-30

  Online published: 2003-04-25

摘要

运用小波分析等方法对黄河上中游天然径流序列进行了分析,揭示了河川径流多时间尺度变化规律,并对径流在不同时间尺度上变化的影响因素进行了探讨。研究结果对于认识黄河径流的变化规律、开发利用管理黄河水资源有着重要的意义。

本文引用格式

蒋晓辉, 刘昌明, 黄强, . 黄河上中游天然径流多时间尺度变化及动因分析[J]. 自然资源学报, 2003 , 18(2) : 142 -147 . DOI: 10.11849/zrzyxb.2003.02.003

Abstract

Because of the influence of climate change and human activities,runoff change has oc-curred.This paper analyzes the natural runoff series of the upper and middle reaches of the Yel-low River with the theory of wavelet transformation,reveals multi-time scale changes rule of runoff,and discusses the influencing factors of runoff multi-time scale changes.The results showed that climatic conditions such as precipitation mainly controlled river runoff variations.But varia-tions in drainage basin underlying surface and local climate factor brought by human activity af-fected natural annual runoff.The results are important to know runoff changes and to exploit wa-ter resources of the upper and middle reaches of the Yellow River.
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