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1951-2010 年中国主要气候区划界线的移动
引用本文:卞娟娟,郝志新,郑景云,葛全胜,尹云鹤.1951-2010 年中国主要气候区划界线的移动[J].地理研究,2013,32(7):1179-1187.
作者姓名:卞娟娟  郝志新  郑景云  葛全胜  尹云鹤
作者单位:1. 中国科学院地理科学与资源研究所, 北京 100101; 2. 中国科学院大学, 北京 100049; 3. 上海市气象科技服务中心, 上海 200030
基金项目:中国科学院战略性先导科技专项,全球变化研究国家重大科学研究计划课题,科技基础性工作专项项目
摘    要:根据采用同一区划方法、指标体系划分的1951-1980 年及1981-2010 年中国气候区划结果,对比分析了过去60 年中国气候区划的主要界线变化特征。结果表明:1951-1980 年至1981-2010 年,我国寒温带界线西缩、北移;暖温带北界东段北移,其中最大北移幅度超过1个纬度;北亚热带北界东段平均北移1 个纬度以上,并越过淮河一线;中亚热带北界中段从江汉平原南沿移至了江汉平原北部,最大移动幅度达2 个纬度;南亚热带北界西段北移0.5~2 个纬度;青藏高原亚寒带范围缩小,高原温带范围增加。东北湿润、半湿润区虽转干与趋湿并存,但其中温带地区的湿润—半湿润东界东移,大兴安岭中部与南部的半湿润—半干旱界线北扩;其他地区的干湿分界线虽未出现明显移动,但北方半干旱及华北半湿润区总体转干,河西走廊、新疆及青藏高原的干旱、半干旱区总体转湿;而南方湿润区则趋干与转湿并存。

关 键 词:中国  1951-1980    1981-2010    气候区划界线  移动  
收稿时间:2012-11-15
修稿时间:2013-04-02

The shift on boundary of climate regionalization in China from 1951 to 2010
BIAN Juanjuan,HAO Zhixin,ZHENG Jingyun,GE Quansheng,YIN Yunhe.The shift on boundary of climate regionalization in China from 1951 to 2010[J].Geographical Research,2013,32(7):1179-1187.
Authors:BIAN Juanjuan  HAO Zhixin  ZHENG Jingyun  GE Quansheng  YIN Yunhe
Institution:1. Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101, China; 2. University of Chinese academy of sciences, Beijing 100049, China; 3. Shanghai Meteorological Sci-Tech Service Center, Shanghai 200030, China
Abstract:The paper analyzed the characteristics of changes on regionalization boundaries of climate over China, based on the regionalization scheme in 1951-1980 and 1981-2010, which was conducted using the identical classification methodologies, criteria system and homogeneous dataset. The results showed that the main boundaries of climate regionalization for 1981-2010 in China have been changed compared with 1951-1980. The boundaries of cold temperate zone shifted northward and shrank westward. The eastern part of northern boundary of warm temperate zone shifted to north with the maximal range over 1 latitude. The eastern part of northern boundary of northern sub-tropical zone shifted northward by over 1 latitude, and the northern sub-tropical zone extended to the north of the Huaihe River. The middle of northern boundary of central sub-tropical zone shifted from the southern edge of Jiang-Han Plain to north of the Plain with the maximal range of 2 latitudes. The western part of northern boundary of southern sub-tropical zone shifted northward by 0.5-2 latitudes. The area of plateau temperate zone enlarged and the plateau sub-frigid zone shrank on Qinghai-Tibet region. Although the aridification and humidification trends were both found in northeastern China, the eastern boundary of humid and sub-humid regions shifted to east, and the southern boundary of semi-arid and sub-humid regions located in the central part of Greater Khingan Mountains moved northward in central temperate zone. In the other zones of China, although the boundaries of humid regions did not show significant changes, the climate from wet to dry was found in the semi-arid and sub-humid regions in northern China, while the climate from dry to wet was found in the arid and semi-arid regions in Hexi Corridor, Xinjiang and Qinghai-Tibet Plateau. In humid region of southern China, the light aridification and light humidification trends were both found.
Keywords:China  1951-1980  1981-2010  boundary of climate regionalization  shift
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