摘要
本文根据两层斜压模式得到大尺度地形对1000—500mb平均温度场的常定扰动.结果得到大地形对温度槽脊的形成具有一定的作用,而地形所造成的高度槽在垂直方向上没有倾斜现象.
Taking two layer baroclinic model,as given by Sawyer and Bushby,and introducing the topographical effect,we obtain the following equations from the linearized vorticity equation and adiabatic equation ■,where η=η(x,y) is the topography of the earth’s surface,H=RT_(0)/g,and ■,in which p_(0)=1000mb,p_(1)=200mb.
作者
朱抱真
CHU PAO-CHEN(Institute of Geophysics and Meteorology,Academia Sinica)
出处
《气象学报》
1957年第4期315-318,共4页
Acta Meteorologica Sinica
