[1]夏库热·塔依尔,海米提·依米提,麦麦提吐尔逊·艾则孜,等.基于小波分析的开都河径流变化周期研究[J].水土保持研究,2014,21(01):142-146,151.
　Shakure·Tahir,Hamid·Yimit,Mamattursun·Eziz,et al.Research on Period of Annual Runoff in Kaidu River Based on Wavelet Analysis[J].Research of Soil and Water Conservation,2014,21(01):142-146,151.
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基于小波分析的开都河径流变化周期研究

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 21 期数: 2014年01期 页码: 142-146,151 栏目: 出版日期: 2014-02-28
Title:
Research on Period of Annual Runoff in Kaidu River Based on Wavelet Analysis
作者:
夏库热·塔依尔1, 海米提·依米提2,3, 麦麦提吐尔逊·艾则孜2,3, 米热古丽·艾尼瓦尔1, 李建涛1
1. 新疆大学 资源与环境科学学院, 乌鲁木齐 830046;
2. 新疆干旱区湖泊环境与资源重点实验室, 新疆师范大学, 乌鲁木齐 830054;
3. 新疆师范大学 地理科学与旅游学院, 乌鲁木齐 830054
Author(s):
Shakure·Tahir1, Hamid·Yimit2,3, Mamattursun·Eziz2,3, Mihrigul·Anwar1, LI Jian-tao1
1. College of Resources and Environment Science, Xinjiang University, Urumqi 830046, China;
2. Xinjiang Laboratory of Lake Environment and Resources in Arid Zone, Urumqi 830054, China;
3. College of Geographical Science and Tourism, Xinjiang Normal University, Urumqi 830054, China
关键词:
径流变化; 小波分析; 开都河
Keywords:
runoff change; wavelet analysis; Kaidu River
分类号:
P333.1
摘要:
基于开都河1956—2010年径流量资料，采用小波分析法对开都河径流变化特征进行研究，讨论开都河年径流在不同时间尺度下的小波变换时频分布特征及其丰、枯交替变化的周期规律。研究结果表明，开都河年径流变化具有同步性，现正处于偏丰期；年内径流分配主要集中于6—8月，各站点最大月径流量均出现在7月。55 a来开都河流域大山口站年径流量呈现递增趋势，变化率为1.382 m3/s，、焉耆站年径流量呈现下降趋势，变化率为-0.113 m3/s。开都河大山口和焉耆两站20~30 a左右时间尺度的周期震荡最显著，其次，11~17 a左右时间尺度的周期震荡也较为显著；开都河流域径流量变化的主周期为27 a，次周期为16 a。
Abstract:
Based on the data of annual runoff from 1956 to 2010 of the Kaidu river, the characteristics of annual runoff variation trends was researched by the method of wavelet analysis,and the periodicity and mutability were discussed, the wavelet transform analysis was jointly adopted to unravel characteristics of runoff variations of the Kaidu River. Results of wavelet analysis show that annual runoff at two stations generally presented an increasing and a decreasing trend, the change rates were 1.382 m3/s and -0.113 m3/s, respectively. Annual distributions were mainly concentrated in June to Augest; the biggest monthly runoff at Dashankou and Yanqi station both occurred in July. The runoff in 11~17 a oscillation period was most notable and it was relatively notable in 20~30 a period. Principal periods of annual runoff at the Dashankou and Yanqi stations were found to be 27 a, and the secondary periods were 16 a.

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备注/Memo

收稿日期:2013-09-10;改回日期:2013-11-26。
基金项目:国家自然科学基金项目（U113830，41201032）
作者简介:夏库热·塔依尔(1987-),女(维吾尔族),新疆伊宁人,硕士研究生,主要研究方向为干旱区水资源与生态环境。E-mail:xaku0102@126.com
通讯作者:海米提·依米提(1960-),男(维吾尔族),教授,博士,主要从事干旱区水资源与生态环境研究。E-mail:yimith@yahoo.com

更新日期/Last Update: 1900-01-01