The Impact of Climatic Changes on Permafrost Degradation in Source Region of the Yangtze River
During the past fifty years,permafrost in source region of the Yangtze River (SRYR) has been degrading at a rapid rate due to the influence of increasing human activities and climatic changes.As we all know,the population density in SRYR is not more than one person per square kilometer,so impact of human activities on permafrost is far less than that of climatic changes.Increase of air temperature has resulted in an increase in ground temperature,deepening of permafrost table and shrinkage of permafrost area.In addition to air temperature,many other meteorological factors especially sunshine duration and annual snow cover also have a direct effect on permafrost temperature and can modify the effect of changes in air temperature.In this paper,we analyzed the status of permafrost degradation and the variations of air temperature,sunshine duration and snow cover,pointed out the relationship between permafrost degradation and climatic changes.
Source region of the Yangtze River permafrost degradation climatic changes
Jin Chen Dongqing Li Qingzhou Meng Guowucai Yong
SKLFSE,Cold and Arid Regions Environmental and Engineering Research Institute,CAS,320 West Donggang Road,Lanzhou,Gansu Province,China 730000
国际会议
第16届国际地理信息科学与技术大会(16th International Conference on GeoInformatics and the Joint Conference)
广州
英文
2008-06-28(万方平台首次上网日期,不代表论文的发表时间)