THE FLUCTUATIONS OF DRY AND WET CLIMATE BOUNDARY AND ITS CAUSAL ANALYSES IN CHINA

被引:5
作者
杨建平
丁永建
陈仁升
刘连友
机构
[1] Cold and Arid Regions Environmental and Engineering Research Institute
[2] Chinese Academy of Sciences
[3] Resources and Environment Institute
[4] Beijing Normal
关键词
D O I
暂无
中图分类号
P461 [气候的形成和影响气候的因素];
学科分类号
摘要
<正> Based on yearly precipitation and Φ20 evaporation pan data during 1951 to 1999 of 295 stations,the aridity index is calculated in this paper.According to the aridity index,the climatic regions in China are divided into three types:the arid zone,the semi-arid zone and the humid zone. Isoline 0.20 is the boundary between arid and semi-arid zones.Isoline 0.50 is the boundary between semi-arid and humid zones.The fluctuations of dry and wet climate boundaries are very substantial,have greatly regional difference,and have the features of the whole shifting along the same direction and of the opposite moving along the contrary direction over the past 50 years.The semi-arid zone is a transitional zone between humid and arid zones,a border belt of monsoon,and a susceptible zone of environmental evolution in China. In the period of the late 1960s to the early 1970s,remarkable change had occurred for dry and wet climate in China.It manifests significantly that climate is from wetter into drought in most regions of northern China.Moreover,drought has an increasing trend.The fluctuations of climatic boundaries and the dry and wet variations in climate have substantial inter-decadal features. The main factors affecting the dry and wet climate boundary fluctuations and the dry and wet variations of climate in China are East Asian summer monsoon,Indian Monsoon,plateau monsoon in the Tibetan Plateau,westerly circulation,and West Pacific subtropical high.The different types of circulations and the strong and weak combinations of these circulations result in the regional differences of dry and wet climate changes in China.Inter-decadal variations of the dry and wet climate boundary fluctuations and of the arid and humid climate result from the inter-decadal changes of East Asian summer monsoon,Indian Monsoon,plateau monsoon,westerly circulation, and West Pacific subtropical high.The anomalous general atmospheric circulation in the Northern Hemisphere during the late 1960s to the early 1970s is the causes of arid and humid climate remarkable change in China.
引用
收藏
页码:211 / 226
页数:16
相关论文
共 9 条
  • [1] 近百年夏季西太平洋副热带高压的变化
    慕巧珍
    王绍武
    朱锦红
    龚道溢
    [J]. 大气科学, 2001, (06) : 787 - 797
  • [2] 20世纪北大西洋温盐环流的年代际变化试评估
    周天军
    王绍武
    [J]. 气候与环境研究, 2001, (03) : 294 - 304
  • [3] 1880年以来华北降水及水资源的变化.[J].张庆云.高原气象.1999, 04
  • [4] 我国夏季降水的年代际变化及华北干旱化趋势
    黄荣辉
    徐予红
    周连童
    不详
    [J]. 高原气象 , 1999, (04) : 465 - 476
  • [5] 本世纪青藏高原气候的三次突变及与天文因素的相关
    汤懋苍
    白重瑗
    冯松
    蔡英
    [J]. 高原气象 , 1998, (03) : 29 - 36
  • [6] 夏季东亚季风区水汽输送特征及其与南亚季风区水汽输送的差别
    黄荣辉
    张振洲
    黄刚
    任保华
    [J]. 大气科学 , 1998, (04) : 76 - 85
  • [7] 东亚夏季风强度指数及其变化的分析.[J].郭其蕴.地理学报.1983, 03
  • [8] DECADAL VARIATIONS IN CLIMATE ASSOCIATED WITH THE NORTH ATLANTIC OSCILLATION.[J].JAMES W. HURRELL;HARRY VAN LOON.Climatic Change.1997, 3
  • [9] All-India monthly and seasonal rainfall series: 1871–1993.[J].B. Parthasarathy;A. A. Munot;D. R. Kothawale.Theoretical and Applied Climatology.1994, 4