摘要
本文在对实测资料分析的基础上,着重阐述了冰川渗浸带雪层温度的时空变化与融水渗浸规律以及产生这种特殊规律的根本原因,同时建立了冰川渗浸带与大气之间的热量交换以及在对应的交换条件下冰川内部状态;最后得出了描述渗浸带水热输运的数学模型。
The time-spatial change of snow temperature and melt-water percolation in infiltration zone of Glacier No.1 in the Urumqi River is discussed in this paper. Meantime, the sketch of heat exchange between the atomsphere and infiltration zone is given. Finaly we set up the mathematical model for calculating the snow temperature in infiltration zone of a glacier.
出处
《冰川冻土》
CSCD
北大核心
1989年第1期60-68,共9页
Journal of Glaciology and Geocryology
