[1]古丽孜巴·艾尼瓦尔,麦麦提吐尔逊·艾则孜,米热古丽·艾尼瓦尔,等.基于小波分析1956-2010年焉耆盆地清水河径流量季节变化规律[J].水土保持研究,2016,23(01):210-214,220.
　Gulziba·Anwar,Mamattursun·Eziz,Mihrigul·Anwar,et al.The Seasonal Runoff Variation of Qingshui River in Yanqi Basin During Period from 1956 to 2010 Based on Wavelet Analysis[J].Research of Soil and Water Conservation,2016,23(01):210-214,220.
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基于小波分析1956-2010年焉耆盆地清水河径流量季节变化规律

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 23 期数: 2016年01期 页码: 210-214,220 栏目: 出版日期: 2016-02-28
Title:
The Seasonal Runoff Variation of Qingshui River in Yanqi Basin During Period from 1956 to 2010 Based on Wavelet Analysis
作者:
古丽孜巴·艾尼瓦尔1,2, 麦麦提吐尔逊·艾则孜1,2, 米热古丽·艾尼瓦尔3, 麦尔丹·阿不拉2
1. 新疆师范大学 新疆干旱区湖泊环境与资源实验室, 乌鲁木齐 830054;
2. 新疆师范大学 地理科学与旅游学院, 乌鲁木齐 830054;
3. 新疆大学 绿洲生态重点实验室, 乌鲁木齐 830046
Author(s):
Gulziba·Anwar1,2, Mamattursun·Eziz1,2, Mihrigul·Anwar3, Mardan·Abla2
1. Xinjiang Laboratory of Lake Environment and Resources in Arid Zone, Xinjiang Normal University, Urumqi 830054, China;
2. College of Geographical Science and Tourism, Xinjiang Normal University, Urumqi 830054, China;
3. Key Laboratory of Oasis Ecdogy, Xinjiang University, Urumqi 830046, China
关键词:
径流量; 小波分析; 清水河
Keywords:
runoff; wavelet analysis; Qingshui River
分类号:
P333.1
摘要:
基于焉耆盆地清水河1956—2010年径流量实测资料，采用小波分析法，分析了清水河平均径流量季节变化规律。研究结果表明：清水河春季、夏季、秋季、冬季平均径流量分别为4.38，24.98，11.98，5.11 m3/s。清水河四季平均径流量变化趋势有较大的差别；清水河四季平均径流量的年际变化过程中存在着多重时间尺度上的复杂嵌套结构，在不同的尺度周期中，表现出不同的丰、枯振荡规律，总体表现为由小尺度无明显规律的剧烈振荡向大尺度有明显规律的振荡变化；1956—2010年四季平均径流量变化周期总体上呈现15～22 a大尺度的变化周期以及7～12，4～5 a小尺度的变化周期。
Abstract:
Based on runoff data of Qingshui River during the period from 1956 to 2010, we analyzed the characteristics of seasonal runoff variations of Qingshui River usint the wavelet transform analysis. The results indicated that the seasonal runoff rates of Qingshui River in spring, summer, autumn and winter were 4.38, 24.98, 11.98, 5.11 m3/s, respectively. The runoff changing trend of Qingshui River in four seasonswas different; a complex nested structure for multi-time scales existed in the process of seasonal runoff change, and the oscillation trend was not consistent at different temporal scales, while it changed from a disorderly and violent oscillation at short term scale to a regular oscillation at long-term scale; the seasonal runoff change of Qingshui River showed principal change period of 15～22 years at long-term scale, and 7～12 years, 4～5 years at short-term scale during the period from 1956 to 2010.

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备注/Memo

收稿日期:2015-03-02;改回日期:2015-03-25。
基金项目:新疆师范大学地理科学与旅游学院地理学博士点支撑学科和新疆维吾尔自治区重点实验室——新疆干旱区湖泊环境与资源实验室资助项目（XJNU-DL-201319）；国家自然科学资助项目（U1138302，41201032）
作者简介:古丽孜巴·艾尼瓦尔(1990-),女(维吾尔族),新疆库车人,硕士研究生,研究方向为干旱区水资源与生态环境。E-mail:gulziba95@126.com
通讯作者:通信作者:麦麦提吐尔逊·艾则孜(1981-),男(维吾尔族),新疆喀什人,博士,副教授,硕士生导师,主要从事干旱区水资源与生态环境研究。E-mail:oasiseco@126.com

更新日期/Last Update: 1900-01-01