摘要
本文求解了孤立斜坡上大气的运动方程和热流量方程,揭示了坡地上风的运动变化规律,着重讨论了科氏力在坡风研究中的作用,计算了不同坡度、稳定度、纬度上坡风的强度。
In this paper, the solutions of equations of motion and heat flux on the slope are given, the intensity of slope wind was caculated, which showed:(1) the wind on the slope was combined with geostrophic drag and slope wind.(2) the larger the roughness, the larger the disturbance of temperature on che earth's surface, the larger the slope's degree and the stabler the stratification, then the larger the slope wind occured.(3) the effect of F (i.e.2Ωsin ) was ignored on the research of slope wind.
出处
《气象科学》
CSCD
北大核心
1990年第1期80-91,共12页
Journal of the Meteorological Sciences