摘要
文中求解了锋面存在时地转动量近似下的大气边界层运动方程 ,得到了边界层内冷锋流场的一些特征 ,如冷锋坡度随地转涡度增加而增加 ,随地转风速时间倾向的增加而增加 ,随沿锋面传播方向的热成风分量的减少而增加。而边界层内冷锋面上下的流场与锋面坡度、地转风及其时空变化特征有关 ,共同特点是在冷锋面高度以下有下滑运动 ,而其上有一层上滑运动区。
In this paper,we have solved the motion equation of the atmospheric boundary layer under the geostrophic momentum approximation when a front exists.and obtained the characteristics of the stream field of the cold front in the boundary layer,for example, the slope of the cold front increases with the increases of geostrophic vorticity,the tendency of the geostrophic wind speed,and also increases with the decrease of the thermal wind speed along the motion direction of the front.The stream field below and above the cold front surface in the boundary layer depends on the slope of the front,the geostrophic wind speed and its temporal and spatial distributions.The common characteristics are that there exists updraft motion above the cold front surface and downdraft motion below that.
出处
《气象学报》
CSCD
北大核心
2001年第3期271-279,共9页
Acta Meteorologica Sinica
基金
国家自然科学基金 4 97351 80
关键词
冷锋
边界层
地转动量近似
坡度
地转风
Cold front,Boundary layer,Geostrophic momentum approximation.
