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《Journal of Glaciolgy and Geocryology》 2001-04
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Spatial Variation of Climate for Different Landscape Areas in the Heihe River Basin

GONG Jia-dong, LI Xiao yan (Cold and Arid Regions Environmental and Engineering Research Institute, CAS, Lanzhou Gansu 730000, China)  
For an inland river basin in the arid regions of Northwest, there are many different landscape patterns, such as alpine snow-ice frozen zone, alpine shrub and meadow zone, intermontane basin, mid-montane forest zone, piedmont diluvial-alluvial plain and oasis zone, terminal lake, and Gobi and sandy desert. Therefore, to understand the responses of different landscape patterns, especially the large irrigated oasis, to the global warming is very important for the inland river management effectively. Heihe River Basin, located in the middle section of the Hexi Corridor, is a representative inland watershed in northwest China with relative abundance meteorological records. Most meteorological records of the Heihe River Basin started from the end of the 1950's, while in the Jiuquan Meteorological Station it is farther. The data for analysis were selected based on the following principles: 1) The station is the in a representative area, 2) The data series must be longer than 30 years, 3) The station less moved its location. There are 14 meteorological stations meeting the above principles. In addition, there are many precipitation stations and hydrological stations operating in the same period, 24 of which are chosen for analysis. Through analyzing the meteorological records during 1961 ~ 1995 in the Heihe River Basin, the change of air temperature and precipitation dependent on vertical zones have been established. It is true that the responses of air temperature and precipitation to climate change were different in different landscape patterns. The increase of air temperature was 0.6 ℃ between the 1960s and the 1990s in the semi-humid and humid areas of high/mid-mountains of the upper reaches, when a higher precipitation increae occurred. While the increase of air temperature was 1.3 ℃ in the desert areas of the outer hills at the same time, when precipitation variation was unstable. In the irrigated oasis of the piedmont plains, the increase of air temperature was 0.5~0.6 ℃ at the same time, when precipitation stably increased a little. In the terminal extreme arid section, air temperature increased 1.4 ℃ and precipitation decreased about 0.5 mm·a -1 . It is believed that there are two reasons leastwise for these spatial variations. First, the effect of climate types in an inland river basin, such as humid and semi-humid in the upper reaches of mountainous area, arid in the middle reaches of the piedmont area, and extreme arid in the lower reaches. Secondly, the effect of the local environment, such as the large irrigated areas intensively contrasted with desert areas due to the mesoclimate circulation. However, there are some uncertainties, for example, lack of meteorological station in desert area.
【Fund】: 国家重点基础研究发展规划项目 (G19990 435 0 6 0 1);; 中国科学院知识创新工程重大项目 (KZCX1 0 9 0 3);; 中国科学院寒区旱区环境与工程研究所知识创新工程项目 (CACX2 10 0 30 );; 中国科学院博士后基金资助
【CateGory Index】: P467
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