On the Non-stationary Atmospheric Currents. (2nd Paper)

[摘要] In my previous paper the general solution of the equation of motion on the non-stationary atomospheric currents was shown. And in this paper for convenience of numerical calculations under the special conditions such asFor the examples of the above solution when initially wind-velocity (Wχ=Wν=0) is zero and(1) the pressure gradient is constant (see Fig. 4. and Fig. 5)(2) the pressure gradient increases linearly with time (see Fig.6)(3) (a)the constant pressure gradient rotates gradually with the clock's hand (see Fig. 7 and Fig. 8)(b) the constant pressure gradient rotates gradually with the counter-clock's _??_ and (see Fig. 9. and Fig. 10), the wind-velocities are calculated by which we can see what manner the surface winds develop with time.

[学科分类] 大气科学