摘要
根据西藏近2000站年的水文气象资料和笔者赴藏的工作积累,系统地分析了西藏高原的水汽输送、降水、径流和蒸发的特点,并给出西藏高原包括大气和下垫面在内的完全水平衡模型。
On the basis of the climate and physiography of the Tibet Plateau,the characteristics of water vapor transport,precipitation,runoff and evaporation,including time-space distributions and variations and thier combined effects,are explained.Then,a three-dimensional physical model of the water cycle of the Tibet Plateau is developed.The model shows the dist-inctiveness of the hydrological characteristics of the Tibet Plateau from those of other regions.
出处
《水利学报》
EI
CSCD
北大核心
1992年第5期1-8,共8页
Journal of Hydraulic Engineering
