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《Journal of Glaciology and Geocryology》 2003-04
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Comparison Analysis of Runoff Change in the Source Regions of the Yangtze and Yellow Rivers

XIE Chang-wei, DING Yong-jian, LIU Shi-yin, WANG Gen-xu (Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academyof Sciences, Lanzhou Gansu 730000, China)  
Climate and water environment is different between the source regions of the Yangtze River and that of Yellow River. Climate in the source regions of the Yangtze River is colder, with mean annual temperature below 0 ℃ in the most of the regions. But mean annual temperature of the source regions of the Yellow River is higher than 0 ℃. Precipitation is less in the source regions of the Yangtze River, ranging from 250 to 480 mm, while precipitation ranges from 300 to 760 mm in the source regions of the Yellow River. So the surface runoffs in the two hydrological systems have some difference in distribution within a year and multi-annual variation. By analyzing runoff variations within a year and multi-annual variation in the source regions of the Yangtze and Yellow Rivers, it is found that the surface runoff in the source regions of the Yellow River has uniformity distribution feature in comparison with that in the source of the Yangtze River. It is identified that there were 21 low water years and 19 rich water years in the period from 1961 to 2000 in the source regions of the Yangtze River. But in the source regions of the Yellow River there were 27 low water years and 17 rich water years from 1956 to 1999. In the recent 40 years, the runoff evolution in the source regions of the Yangtze River experiences a process of wet-dry-wet-dry. However in the source regions of the Yellow River it is a process of dry-wet-dry. Mean annual runoff in the source regions of the Yangtze River has a period of 8~9 a obviously. But in the source regions of the Yellow River the period is 7~8 a. The factors, such as precipitation and temperature, which influence runoff mainly, are analyzed by multiple regressions. It is found that temperature is more active in the source regions of the Yangtze River and precipitation is more prominent in the source regions of the Yellow River. Water environment in the cold regions is more important in the source regions of the Yangtze River rather than in the source regions of the Yellow River. It is the leading cause why there is different in runoff between the source regions of the Yangtze River and the Yellow River.
【Fund】: 中国科学院知识创新重大项目 (KZCX1 10 0 6 ) ;; 国家自然科学基金重大项目 (90 2 0 2 0 13)资助
【CateGory Index】: P343.1
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3 Yang Daqing, Jiang Tong, Zhang Yinsheng and Kang Ersi (Lanzhou Institute of Glaciology & Geocryology, Chinese Academy of Sciences);Analysis and Correction of Errors in PrecipitationMeasurement at the Head of UrumqiRiver,Tianshan[J];Journal of Glaciology and Geocryology;1988-04
4 Lan Yongchao Lanzhou Institute of Glaciology and Geocryology, Chinese Academy of Sciences );Spring Runoff Characteristics of the Upper Yellow River[J];Journal of Glaciology and Geocryology;1989-04
5 DING Yongjian; YE Baisheng; ZHOU Wenjuan;(Lanzhou Institute of Glaciology and Geocryology, CAS, Lanzhou 730000);Temporal and Spatial Precipitation Distribution in the HeiheCatchment, Northwest China, During the Past 40 a[J];JOURNAL OF GLACIOLGY AND GEOCRYOLOGY;1999-01
6 LAN Yong chao 1 , KANG Er si 1 , MA Quan jie 2 , YANG Wen hua 3 , YAO Zhi zong 3 (1 Lanzhou Institute of Glaciology and Geocryology, CAS, Lanzhou Gansu 730000, China; 2 Lanzhou Administrative Office of Hydrology and Water;The Trend Prediction and Characteristics of the Variation of the Runoff into the Longyangxia Reservoir[J];JOURNAL OF GLACIOLGY AND GEOCRYOLOGY;1999-03
7 ZHANG Xin-ping; YAO Tan-dong; JIN Hui-jun ( Territory Institute, Hunan Normal University, Changsha Hunan 410081. Chian ; Cold and Arid Regions Environmental and Engineering Research Institute, Lanzhou Gansu 730000, China );The Influence of ENSO Event on the Modern δ~(1 8)O on the Guliya Ice Core[J];JOURNAL OF GLACIOLGY AND GEOCRYOLOGY;2000-01
8 WANG Gen-xu, SHEN Yong-ping, CHENG Guo-dong (State Key Laboratory of Frozen Soil Engineering, CAREERI, CAS, Lanzhou Gansu 730000. China) (Resource and Environment College of Lanzhou University: Lanzhou Gansu 730000. China);Eco-environmental Changes and Causal Analysis in the Source Regions of the Yellow River[J];JOURNAL OF GLACIOLGY AND GEOCRYOLOGY;2000-03
9 SU Zhen, SHI Ya-feng (Cold and Arid Regions Environmental and Engineering Research Institute, CCAS, Lanzhou Gansu 730000. China);Response of Monsoonal Temperate Glaciers in China to Global Warming Since the Little Ice Age[J];JOURNAL OF GLACIOLGY AND GEOCRYOLOGY;2000-03
10 PU Jian-chen, YAO Tan-dong, WANG Ning-lian, DING Liang-fu, ZHANG Qi-hua (Cold and Arid Regions Environmental and Engineering Research Institute, CAS, Lanzhou Gansu 730000, China);Recent Variation of the Malan Glacier in Hoh Xil Region of the Tibetan Plateau[J];Journal of Glaciolgy and Geocryology;2001-02
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