首页 | 官方网站   微博 | 高级检索  
     

冰雪区局地环流及气候特征探讨
引用本文:康兴成.冰雪区局地环流及气候特征探讨[J].地理学报,1991,46(4):449-459.
作者姓名:康兴成
作者单位:中国科学院兰州冰川冻土研究所
摘    要:本文以西昆仑山崇侧冰帽区为例,根据大量观测资料,讨论了冰川存在对其所在地区气候的影响。得出冰川风是影响冰雪区气候特征的重要因素,是冰-气作用中的一个主要因子。这里的冰川风是一种独成体系的局地环流,它既不同于山谷冰川上出现的冰川风,也不同于山谷风。其强度随着离开冰雪区距离的增长而减弱。在冰雪区前缘地带形成风向、温湿度急剧变化区,使温度梯度从非冰川区到冰川区发生大的变化。

关 键 词:冰雪区  环流  气候  冰川  大气

A STUDY ON LOCAL CIRCULATION AND CLIMATIC CHARA-CTERISTICS IN GLACIER AREA
Kang Xingcheng.A STUDY ON LOCAL CIRCULATION AND CLIMATIC CHARA-CTERISTICS IN GLACIER AREA[J].Acta Geographica Sinica,1991,46(4):449-459.
Authors:Kang Xingcheng
Abstract:This paper took the Chongce ice cap in west Kunlun Mountains as an example, and discussed the existence of the glacier affecting he climate of the glacial area. It was revealed that the glacier wind is an important influencing factor for climatic condition in this area and the main factor in the interaction between ice and atomsphere. The glacier wind in this region is a kind of special local circulation. It was different from the regular diurnal mountain-valley winds and also different from the typical glacier wind occurring in valley glacier areas. The intensity of this wind decreases with distance from the glacier. The zone of dras'ic changes of wind direction, temperature and humidity occurred at fhe front edge of the glacier tongue, lapse rate of temperature here has a large variation from nonglacial area to glacial area.
Keywords:Glacial area  Glacier wind  Local circulation  North wind  South wind
本文献已被 CNKI 维普 等数据库收录!
点击此处可从《地理学报》浏览原始摘要信息
点击此处可从《地理学报》下载全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司    京ICP备09084417号-23

京公网安备 11010802026262号