摘要
使用美国NCAR非静力平衡模式MM 5V3,模拟了黑河地区非均匀下垫面局地小气候效应 ,再现了山谷风环流及夏季“绿洲效应”、沙漠上的“逆湿”和由于地表热力分布不均匀引起的绿洲—沙漠垂直环流等绿洲—沙漠相互作用的典型特征 ,较全面地揭示了非均匀地表大气边界层内的风、温、湿度场与陆面相互作用的物理机理 。
The local climatic effect of heterogeneous underlying surface was simulated through the MM5V3 meso-scale model. The simulations reappear the some typical characteristics of the oasis-desert interaction such as mountain valley wind, 'oasis effect' in the summer, and 'inverse humidity' on desert and oasis-desert vertical circulation which are caused by the thermodynamic distinctions of different underlying surfaces and reveal the physical mechanicsm of the interaction between the land surface and wind field, temperature and humidity in atmospheric boundary layer over heterogeneous land surface. Namely, the results of the numerical simulations in the paper have well tested the ones in field experiments.
出处
《高原气象》
CSCD
北大核心
2001年第4期354-361,共8页
Plateau Meteorology
基金
"我国重大气候和天气灾害形成机理和预测理论的研究"第一部分 :"我国重大气候灾害的形成机理和预测理论"项目(G19980 40 90 4 2 )
国家自然科学基金项目 ( 4 9775 2 6 9)资助