Periodic changes of stream flow in the last 40 years in Tarim River Basin, Xinjiang, China

被引:25
|
作者
Chen, Yaning [2 ]
Pang, Zhonghe [1 ]
Hao, Xingming [2 ]
Xu, Changchun [2 ]
Chen, Yapeng [2 ]
机构
[1] Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
[2] Chinese Acad Sci, Xinjiang Inst Ecol & Geog, Urumqi 830011, Peoples R China
基金
中国国家自然科学基金;
关键词
time series; climate change; prediction; arid inland river basin;
D O I
10.1002/hyp.7024
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Using the annual runoff series for the last 40 years from the Tarim River Basin, their periodic properties were analysed and their future trends predicted. Runoff data were collected at five hydrological gauging stations in the three main branches of the Tarim River. An extrapolation method and variance analysis were used to identify periods in annual runoff and a trend superposition model to predict future changes. Results show that, there is a common period of 17 years in annual runoff changes for all three branches, with Hotan River showing an additional period of 10 years. Based on this trend, it is suggested that the annual runoff of the Tarim River should decrease in the period of 2006-2008, but increase ill year 2009. a and the How may possibly begin to decrease significantly in veal 2010. The long term trend of runoff In Tarim Basin has followed the global prediction of GCMs, i.e. began to increase in accordance with global increase of air temperature and precipitation in 1990. However, it has shown a local feature of uneven changes among, the head streams in the same basin, which needs to be further investigated. Copyright (c) 2008 John Wiley & Sons. Ltd.
引用
收藏
页码:4214 / 4221
页数:8
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