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《Journal of Glaciology and Geocryology》 2004-01
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Climatic Features of Eco-Environment Change in the Source Regions of the Yangtze and Yellow Rivers in Recent 40 Years

YANG Jian-ping, DING Yong-jian, SHEN Yong-ping, LIU Shi-yin, CHEN Ren-sheng(Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences, Lanzhou Gansu 730000, China)  
Based on monthly data of air temperature, precipitation, maximum and minimum air temperature, duration of sunshine, the features of climatic change in the source regions of the Yangtze and Yellow Rivers are analyzed comprehensively over the last 40 years, and the climate changes in the source regions of the Yangtze and Yellow Rivers are compared with that in the Tibetan Plateau, in whole China and in the globe. It is found that air temperature in the regions as a whole has a rising trend in the recent 40 years with a rising amplitude of 0^7~0^8 ℃ in annual air temperature. So the source regions of the Yangtze and Yellow Rivers are one of unusual warming areas on he Tibetan Plateau. Major warming characteristics are increase in the minimum air temperature and duration of sunshine in the source regions of the Yellow River. Great increase in the maximum and minimum air temperatures and long duration of sunshine, longer than that in the source regions of the Yellow River, are the main features of climatic warming in the source regions of the Yangtze River. Increasing air temperature is not chief in winter, while warming in spring, summer, and autumn is greater than that in winter in the source regions of the Yangtze River, unlike in the Tibetan Plateau, the whole China and the globe. Warming is not the result of increasing air temperature in winter in the source regions of the Yellow River. Warming in autumn amounts to that in winter. Moreover, warming in other seasons cannot be neglected. Precipitation is slight increase in the source regions of the Yangtze and Yellow Rivers in the recent 40 years. But increase in precipitation reflects mainly on the noticeably increasing precipitation in winter and spring after the middle and later 1980s. As a whole, a continuous decreasing trend of precipitation can be seen in some regions, although precipitation in summer has no marked change. Comparison of climate changes in the globe, in the whole China, and on the Tibetan Plateau shows that the response of climate in the source regions of the Yangtze and Yellow Rivers to climate warming is most sensitive. Climate warming firstly began in the source regions of the Yangtze River and the Tibetan Plateau. 15 years later, markedly warming began in the source regions of the Yellow River and the whole China. Increase of precipitation in the source regions of the Yellow River and in the northern source regions of the Yangtze River indicates that climate warming is favorable for increasing precipitation on the Tibetan Plateau.
【Fund】: 国家自然科学基金项目(40301010);; 中国科学院知识创新重大项目(KZCX1 10 06)资助
【CateGory Index】: P467
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5 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
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7 Chen Quangong Liang Tiangang Wei Yaxing (Gansu Grassland Ecological Research Institute, Lanzhou 730020);Causes of Grassland Degradation in Dari County of Qinghai Province[J];ACTA PRATACULTURAL SCIENCE;1998-04
8 Lin Zhenyao Wu Xiangding (Institute of Geography, Academia Sinica);CUMATIC REGIONALIZATION OF THE QINGHAI-XIZANGPLATEAU[J];Acta Geographica Sinica;1981-01
9 Wei Fengying and Cao Hongxing(Chinese Academy Of Meteorological Sciences, Beijing 100081);Detection of Abrupt Changes and Trend Prediction of the Air Temperature in China, the Northern Hemisphere and the Globe[J];SCIENTIA ATMOSPHERICA SINICA;1995-02
10 Tao Shiyan and Zhang Qingyun (Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing100080);Response of the Asian Winter and Summer Monsoon to ENSO Events[J];SCIENTIA ATMOSPHERICA SINICA;1998-04
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