PDF Download

[1]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.

Copy

Research on Period of Annual Runoff in Kaidu River Based on Wavelet Analysis

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 21 Number of periods: 2014 01 Page number: 142-146,151 Column: Public date: 2014-02-28

Title:: Research on Period of Annual Runoff in Kaidu River Based on Wavelet Analysis

Author(s):: Shakure·Tahir¹, Hamid·Yimit^2,3, Mamattursun·Eziz^2,3, 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

Keywords:: runoff change; wavelet analysis; Kaidu River

CLC:: P333.1

DOI:: -

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.

References:: [1] 张士锋,华东,孟秀敬.三江源气候变化及其对径流的驱动分析[J].地理学报,2011,66(1):13-24.
[2] 白红英,侯钦磊,马新萍,等.50年来秦岭金钱河流域水文特征及其对降水变化的响应[J].地理科学,2012,10(3):1230-1235.
[3] 王晓杰,刘海隆,包安明.气候变化对玛纳斯河的径流量影响预测模拟分析[J].冰川冻土,2012,34(5):1220-1228.
[4] 邴龙飞,邵全琴,刘纪远,等.基于小波分析的长江和黄河源区汛期、枯水期径流特征[J].地理科学,2011,31(2):232-238.
[5] 王钧,蒙吉军.黑河流域近60年来径流量的变化及影响因素[J].地理科学,2008,28(1):83-88.
[6] 凌红波,徐海量,张青青,等.新疆塔里木河三源流径流量变化趋势分析[J].地理科学,2011,31(6):728-733.
[7] 王建,李硕.气候变化对中国内陆干旱区山区融雪径流的影响[J].中国科学:D辑,2005,35(7):664-670.
[8] 曹丽青,葛朝霞,薛梅.1951-2006年新疆地区气候变化特征及其与水资源的关系[J].河海大学学报:自然科学版,2009,37(3):281-283.
[9] 崔步礼,李小雁,李岳坦,等.青海湖流域河川径流特征及其对降水的滞后效应[J].中国沙漠,2011,31(1):247-253.
[10] 陈忠升,陈亚宁,李卫红,等.塔里木河干流径流损耗及其人类活动影响强度变化[J].地理学报,2011,66(1):90-97.
[11] 陈亚宁,郝兴明,徐长春,等.新疆塔里木河流域径流变化趋势分析[J].自然科学进展,2007,17(2):205-210.
[12] 李红军,江志红,刘新春,等.阿克苏河径流变化与北大西洋涛动的关系[J].地理学报,2008,63(5):491-501.
[13] 麦麦提吐尔逊·艾则孜,海米提·依米提,祖皮艳木·买买提,等.焉耆盆地土地利用变化对生态服务价值的影响[J].水土保持研究,2012,19(6):138-141.
[14] 郭高轩,辛宝东.基于小波变换的北京地区1724-2009年降水量多尺度分析[J].水文,2012,32(3):29-33.
[15] 桑燕芳,王栋.水文序列小波分析中小波函数选择方法[J].水利学报,2008,39(3):295-306.
[16] 程正兴.小波分析算法与应用[M].西安:西安交通大学出版社,1998.
[17] 王文圣,丁晶,李跃清,等.水文小波分析[M].北京:化学工业出版社,2005.
[18] 毕雪丽.新疆博斯腾湖流域气候变化及地表径流响应[D].上海:华东师范大学,2012.

Similar References:

Memo

Last Update: 1900-01-01