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祁连山西段喀克图地区冻土和冰缘的基本特征
引用本文:王绍令.祁连山西段喀克图地区冻土和冰缘的基本特征[J].干旱区资源与环境,1992,6(3):9-17.
作者姓名:王绍令
作者单位:中国科学院兰州冰川冻土研究所 兰州,730000
摘    要:考察区属中亚极大陆型干寒区,水分是区内植被、多年冻土的分布、发育和冰缘作用过程及其地貌类型组合的关键因素。与同纬度的祁连山东、中段相比,本区降水少、植被稀疏,雪线、冰缘带下界和多年冻土下界均高,而且冰缘带下界高于多年冻土下界。

关 键 词:干寒区  植被  多年冻土  冰缘

BASIC FEATURES OF FROZEN GROUND AND PERIGLACIAL IN THE KAKITU REGION OF WESTERN PART OF THE QILIAN MOUNTAINS
Wang Shaoling Lanzhou Institute of Glaciology and Geocryology,Chinese Academy of Sciences.BASIC FEATURES OF FROZEN GROUND AND PERIGLACIAL IN THE KAKITU REGION OF WESTERN PART OF THE QILIAN MOUNTAINS[J].Journal of Arid Land Resources and Environment,1992,6(3):9-17.
Authors:Wang Shaoling Lanzhou Institute of Glaciology and Geocryology  Chinese Academy of Sciences
Abstract:The investigated region is located in extreme continental, arid and fri- gid area in the Mid-Asia.The moisture condition is the key factor for the development and distribution of permafrost and periglacial action and the formation of the periglacial landform.Compared with the east and mid Qi- lian mountains with same latitute zone, the Kakitu region shows that the precipitation is little and the vegetation is rare,meanwhile, the snow-line and the lowest limit of periglacial zone and permafrost are higher, and the periglacial zone higher than permafrost.
Keywords:Arid-frigid Area  Vegetation  Permafrost  Periglacial
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