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The Northward Shift of Climatic Belts in China During the Last 50 Years and the Corresponding Seasonal Responses
作者姓名:YE Duzheng  JIANG Yundi  DONG Wenjie
作者单位:START Regional Research Center for Temperate East Asia,Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing 100029,START Regional Research Center for Temperate East Asia,Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing 100029,START Regional Research Center for Temperate East Asia,Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing 100029
基金项目:国家自然科学基金,中国科学院资助项目,the National Key Program for Developing Basic Sciences 
摘    要:Along the meridian of 105°E, the Chinese region are divided into two parts, east and west. The results show that in the east part of China the temperate extratropical belt, the warm extratropical belt,and the northern subtropical belt shift northward significantly, whereas the middle subtropical belt and the southern subtropical belt have less or no change. As for the northern subtropical belt, the maximal northward shift can reach 3.7 degrees of latitude. As for the warm extratropical belt, along the meridian of 120°-125°E, the maximal northward shift can reach 3-4 degrees. In the west part of China, each climatic belt changes little. Only in the Xinjiang area are the significant northward shifts. Correspondingly, it is found that in the last 50 years the traditional seasons have changed. For Beijing, Hailar, and Lanzhou, in general, summer becomes longer and winter shorter over the last 50 years. Summer begins early and ends late with respect to early 1950s. Contrary to the summer, winter begins la

关 键 词:中国  气象区域  北向移动  50年变化  季节变化  冬季始终曲线  夏季始终曲线

The northward shift of climatic belts in China during the last 50 years and the corresponding seasonal responses
YE Duzheng,JIANG Yundi,DONG Wenjie.The Northward Shift of Climatic Belts in China During the Last 50 Years and the Corresponding Seasonal Responses[J].Advances in Atmospheric Sciences,2003,20(6):959-967.
Authors:Ye Duzheng  Jiang Yundi  Dong Wenjie
Institution:START Regional Research Center for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029,START Regional Research Center for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029,START Regional Research Center for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029
Abstract:Along the meridian of 105°E, the Chinese region are divided into two parts, east and west. The results show that in the east part of China the temperate extratropical belt, the warm extratropical belt, and the northern subtropical belt shift northward significantly, whereas the middle subtropical belt and the southern subtropical belt have less or no change. As for the northern subtropical belt, the maximal northward shift can reach 3.7 degrees of latitude. As for the warm extratropical belt, along the meridian of 120°-125°E, the maximal northward shift can reach 3-4 degrees. In the west part of China, each climatic belt changes little. Only in the Xinjiang area are the significant northward shifts. Correspondingly, it is found that in the last 50 years the traditional seasons have changed. For Beijing, Hailar, and Lanzhou, in general, summer becomes longer and winter shorter over the last 50 years. Summer begins early and ends late with respect to early 1950s. Contrary to the summer, winter begins late and ends early with respect to early 1950s. Furthermore, spring and autumn have changed over the last 50 years: with respect to early 1950s spring begins early and autumn begins late.
Keywords:climatic belts  northward shift  seasonal responses  China
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