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《Journal of Glaciology and Geocryology》 2006-05
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Climate Change in Tuotuohe Area at the Headwaters of Yangtze River

ZHANG Gou-sheng~1,2, SHI Xing-he~3, LI Dong-liang~4, WANG Qing-chun~1, DAI Sheng~1 (1.The Meteorological Bureau of Qinghai Province,Xining Qinghai 810001,China ;2.Key Laboratory for Climate Studyies,China Meteorological Administration,Beijing 100081,China;3.The Meteorological Station of Qinghai Province,Xining Qinghai 810001,China;4.Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences,Lanzhou Gansu 730000,China)  
Using the data of temperature,precipitation,snow cover and so on from the Tuotuohe Meteorological Station at the headwaters of Yangtze River from 1959 to 2003,the annual and seasonal series of meteorological factors are worked out.The interannual and decadal climate changing features are analyzed preliminarily by using the climate diagnosis method.It is found that in the recent 40 years,summer air temperature increased obviously in the region.The annual maximum,minimum and seasonal mean air temperatures in the 1990s were 0.6~1.2℃ higher than that in the 1980s(or the 1960s).In the 1980s the air temperature was the lowest. Precipitation has an increasing trend in winter and a decreasing trend in summer.precipitation in spring and autumn increased but snow depth decreased.Strong wind days were more in the 1980s and the 1990s than that in the 1960s and the 1970s.In general,summer temperature increase,precipitation decrease,and strong wind days increase in the 1980s.This climate changes were strengthened in the 1990s,and expanded to spring and autumn,as a result,grassland deteriorating,permafrost thawing and glacier retreating quickly,wetland shrinking,and finally,eco-environment worsening.
【Fund】: 国家自然科学基金项目(40465002);; 中国科学院知识创新工程重大项目(KZCX1-SW-04);; 中国气象局气候变化专项(CCSF2005-2-QH23)资助
【CateGory Index】: P467
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