中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Sandy desertification status and its driving mechanism in North Tibet Plateau

文献类型:期刊论文

作者Dong Yuxiang
刊名JOURNAL OF MOUNTAIN SCIENCE
出版日期2004-04
卷号1期号:1页码:65–73
关键词North Tibet Plateau desertification status driving force
ISSN号1672-6322
通讯作者Dong YX
英文摘要As the main body of Qinghai-Tibetan Plateau, North Tibet Plateau is one of three major sandy desertification regions in China and also a representative sandy desertification zone of Qinghai-Tibet Plateau. Accordingly, it is an important region for the study of recent sandy desertification processes and formation mechanism. From such aspects as desertified land types, areas and distributions etc., this paper analyses in detail the sandy desertification status on North Tibet Plateau, and qualitatively and quantitatively deals with the main factors that affect recent sandy desertification processes and the driving mechanism. Research results show that North Tibet Plateau is an important sandy desertification region in China characterized with large desertified land areas, diversified types, high severity, extensive distributions and serious damages. Sandy desertification occurrence and development resulted from combined effects of natural factors, anthropogenic factors, natural processes and man-made processes, of which climatic change is the main driving force.
语种英语
公开日期2013-08-15
源URL[http://ir.imde.ac.cn/handle/131551/6168]  
专题成都山地灾害与环境研究所_Journal of Mountain Science _Journal of Mountain Science-2004_Vol1 No.1
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GB/T 7714
Dong Yuxiang. Sandy desertification status and its driving mechanism in North Tibet Plateau[J]. JOURNAL OF MOUNTAIN SCIENCE,2004,1(1):65–73.
APA Dong Yuxiang.(2004).Sandy desertification status and its driving mechanism in North Tibet Plateau.JOURNAL OF MOUNTAIN SCIENCE,1(1),65–73.
MLA Dong Yuxiang."Sandy desertification status and its driving mechanism in North Tibet Plateau".JOURNAL OF MOUNTAIN SCIENCE 1.1(2004):65–73.

入库方式: OAI收割

来源:成都山地灾害与环境研究所

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