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《Journal of Glaciology and Geocryology》 2003-06
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Flood Detention Region in the Middle Reaches of Tarim River Mainstream and Its Impact on Ecological Environments

WANG Shun-de~1, LI Hong-de~1, XU Ze-rui~2, HAN Ping~3, WANG Jin~1 (1. Aksu Hydrology and Water Resource Bureau, Aksu Xinjiang 843000, China; 2. Hydrology and Water ResourceReconnaissance Breau of Bayingol Prefecture, Korla Xinjing 845002, China; 3. Xinjing Hydrology and WaterResource Bureau, rümqi Xinjing 830000, China)  
The Tarim River Basin is located in the southern half of Xinjiang Uygur Autonomous Region, PRC. From the confluence of its three main contributing tributaries, the Tarim River mainstream extends 1321 km to Taitema Lake. The mainstream can be classed into the upstream with 495 km from Xiaojiake to Yinbazar, the middlestream with 398 km from Yinbazar to Kara and the lowerstream with 428 km from Kara to Taitema Lake. A number of rivers fed by snowmelt and glacier melt begin in the mountains and drain into the basin with average annual virgin flow of about 35 billion m~3. A number of other subbasins exist within the Tarim Basin that does not contribute flows to the Tarim River because all of their flows either naturally evaporate in the desert or are used in irrigated agriculture areas. Peak flow months in the rivers are July, August and September. Lowest flow occurs in the period from January through April. Total streamflow of the four headstreams of the Tarim River in 2001 is 266.5×10~8m~3, more 40.70×10~8m~3 than annual mean streamflow, increasing 18% to annual mean value. Annual mean streamflow at Aler Gauging Station where the Tarim River mainstream begins was 46.00×10~8m~3. The interzone consumed water of the Tarim River mainstream are estimated to be 15.33×10~8m~3 for the upper course, account for 33.3% of Aler annual mean streamflow; 23.99×10~8m~3 for the middle course, 52.2% of Aler ones and 6.680×10~8m~3 for the downstream course , 14.5% of Aler ones. The consumed water of both upstream and middlestream courses sum up 39.32×10~8m~3, account for 85.5% of annual mean streamflow at Aler Gauging Station. Historical annual flows average over 40×10~8 m~3, but for the past two decades there has essentially been no flow below Daxihaizi Reservoir, 300 km upstream of Taitema Lake. In 2001, an emergency water diversion project was carried out in the !green corridor", transfer water from Bosten Lake to the Taitema Lake, and fed the !green corridor", ended the 30-years no flow history of 300 km upstream of the Taitema Lake, and ecological environment started to be restoring.
【Fund】: 国家自然科学基金项目(90202013;;40371026);; 中国科学院知识创新工程重大项目(KZCX1 10 06)资助
【CateGory Index】: P343.1
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3 MA Ming-guo+1, JIAO Yuan-mei+{1, 2}, CHENG Guo-dong+1 (1. State Key Laboratory of Frozen Soil Engineering, CAREERI, CAS, Lanzhou Gansu 730000, China; 2. Yunnan Normal University, Tourism and Geographic Science Institute, Kunming Yunnan 650092, China);Change in Land Coverage in Northwest China During the Past Decade Monitored by NOAA-CHAIN[J];Journal of Glaciolgy and Geocryology;2002-01
4 SHI Ya feng 1, SHEN Yong ping 1, HU Ru ji 2(1.Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Science, Lanzhou Gansu 730000, China; 2. Xinjiang Institute of Ecology and Geography, Chinese Academy of Scie;Preliminary Study on Signal, Impact and Foreground of Climatic Shift from Warm-Dry to Warm-Humid in Northwest China[J];Journal of Glaciolgy and Geocryology;2002-03
5 ;New Progress in Glacier and Water Resources Changes in Tarim Basin, Xinjiang[J];Journal of Glaciolgy and Geocryology;2002-06
6 SHEN Yong ping 1 , LIU Shi yin 1 , DING Yong jian 1 , WANG Shun de 2 (1. Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou Gansu 730000, China;2. Aksu Hydrology and Water Resource Bureau, Aksu Xinjiang 843000, China);Glacier Mass Balance Change in Tailanhe River Watersheds on the South Slope of the Tianshan Mountains and Its Impact on Water Resources[J];Journal of Glaciology and Geocryology;2003-02
7 WANG You qing, PU Jian chen, ZHANG Yong liang, SUN Wei zh en(Key Laboratory of Ice Core and Cold Region Environment, CAREERI, CAS, Lanzhou Gansu 730000, China);Characteristic of Present Warming Change Recorded in Malan Ice Core,Central Tibetan Plateau[J];Journal of Glaciology and Geocryology;2003-02
8 SU Hong chao 1, WEI Wen shou 2, HAN Ping 1(1. Xinjiang Hydrology and Water Resources Bureau, rümqi Xinjiang 830000, China; 2. Institute of DesertMeteorology, China Meteorological Administration, rümqi Xinjiang 830002, China);Changes in Air Temperature and Evaporation in Xinjiang during Recent 50 Years[J];Journal of Glaciology and Geocryology;2003-02
9 HAN Ping, XUE Yan, SU Hong chao(Xinjiang Hydrology and Water Resources Bureau, rümqi Xinjiang, 8300 00, China);Precipitation Signal of the Climatic Shift in Xinjiang Region[J];Journal of Glaciology and Geocryology;2003-02
10 ZHANG Gou wei, WU Su fen, WANG Zhi jie(Xinjiang Hydrology and Water Resources Bureau, rümqi Xinjiang 83000 0, China);The Signal of Climatic Shift in Northwest China Deduced from River Runoff Change in Xinjiang Region[J];Journal of Glaciology and Geocryology;2003-02
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