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《Journal of Glaciolgy and Geocryology》 2002-06
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Spatial Change of Dry and Wet Climate Boundary in China in the Recent 50 Years

YANG Jian ping 1 , DING Yong jian 1 , CHEN Ren sheng 1 , LIU Lian you 2 (1. Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou Gansu 730000, China; 2. Resources and Environment Institute, Beijing Normal University, Beijing 100875, China)  
Based on annual precipitation, annual mean wind, and solar radiation data during 1951-1999 of 295 stations, aridity index is calculated in this paper. According to the aridity index, China can be delineated into three climate zones, namely, arid zone, semi-arid zone and humid zone. Aridity index 0.20 is the boundary between arid and semi-arid zone. Aridity index 0.50 is the boundary between semi-arid and humid climate zone. The dry and wet climate boundaries in annual precipitation are compared with the ones of the aridity index in the text. The results show that there is a substantial regional difference for the arid and semi-arid boundary and the semi-arid and humid boundary, and that there is a "U" type spatial distribution under the circumstances of climate warming and of great spatial difference in precipitation. In the northern part of Northeast China, 250-mm isoline is the boundary between the arid and semi-arid zone and the arid climate zone is consistent with the original zone. 450-mm isoline becomes the boundary between semi-arid and humid. Semi-arid zone retreats westward and its range shortened in northern Northeast China. 300-mm isoline is the boundary between arid and semi-arid zone and 700-mm isoline becomes the boundary between semi-arid zone and humid zone in the southern part of Northeast China, North China, and Hetao District. Arid and semi-arid zone expands southeastward and its range enlarges. In Southwest China and the eastern part of Northwest China to the west of Hetao District, 250-mm isoline is the boundary between arid and semi-arid zone. 500-mm isoline becomes the boundary between semi-arid and humid. Arid and semi-arid climate becomes normal. The spatial change of dry and wet climate boundary in China is depended on the regional difference in precipitation. There is upward trend in precipitation in northern Northeast China. Precipitation has a downward tendency in southern Northeast China, North China and Hetao District. Precipitation is slightly increasing in Southwest China and eastern Northwest China to the west of Hetao District. Precipitation depends on southeast monsoon and southwest monsoon. The former is dependent on the location and the intensity of West Pacific Subtropical High and the latter is caused by Bengalese warm current, westerly circulation and so on.
【Fund】: 中国科学院知识创新工程重大项目(KZCX1- 10 - 0 6 );; 国家基础研究发展规划项目 (G2 0 0 0 0 4 870 5)资助
【CateGory Index】: P467
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4 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
5 LAN Yongchao; Kang Ersi; JIN Huijun; ZHANG Shengcai;CHEN Mingzheng2; CHEN Xuelin2;(1 Lanzhou Institute of Glaciology and Geocryology, CAS, Lanzhou 730000; 2 Zhangye AdministrativeOffice of Hydrology and Water Resources of Gansu Province, Zhangye 734000);Study on the Variation Characteristics and Trend of MountainousRunoff in the Heihe River Basin[J];JOURNAL OF GLACIOLGY AND GEOCRYOLOGY;1999-01
6 LEI Xiao yun 1 , CHEN Hui yuan 2 (1 Shihezi University, Shihezi Xinjiang Uygu Autonomous Region 832000, China; 2 Wuhan University of Hydraulic and Electric Engineering, Wuhan Hubei 430072, China);Study of Groundwater Prediction on Manasi River Basin of Xinjiang[J];JOURNAL OF GLACIOLGY AND GEOCRYOLOGY;1999-03
7 WU Yan-qing;MU Fu-qiang; HE Yi-xian;LAN Yong-chao (Cold and Arid Regions Environmental and Engineering Research Institute, CAS. Lanzhou Gansu 730000, China );Analysis of the Transformation Path Between Stream Flow and Groundwater from Dingxin to Shaomaying in Hei River, Catchment West China[J];JOURNAL OF GLACIOLGY AND GEOCRYOLOGY;2000-01
8 XU Zhong-min, CHENG Guo-dong (Cold and Arid Regions Environmental and Engineering Reserch Institute, CAS, Lanzhou Gansu 730000, China);The Predicted Demand of Water Resources in the Middle Reaches of the Heihe River from 1995 to 2050[J];JOURNAL OF GLACIOLGY AND GEOCRYOLOGY;2000-02
9 LAN Yong-chao, KANG Er-si (Cold and Arid Regions Environmental and Engineering Research Institute, CAS, Lanzhou Gansu 730000, China);Changing Trend and Features of the Runoff from Mountain Areas of Some Main Rivers in the Hexi Inland Region[J];JOURNAL OF GLACIOLGY AND GEOCRYOLOGY;2000-02
10 DING Yong-jian, YE Bai-sheng, LIU Shi-yin (Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou Gansu 730000. China);Impact of Climate Change on the Alpine Streamflow During the Past 40 a in the Middle Part of the Qilian Mountains, Northwestern China[J];JOURNAL OF GLACIOLGY AND GEOCRYOLOGY;2000-03
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