Importance of the Numerical Representation of Shallow and Deep Convection for Simulations of Dust Transport over a Desert Region
Figure 5
Power spectral density distribution for the x-direction variation of vertical velocity at five levels for EXP1 at (a) 0800 LT, (b) 0900 LT, (c) 1000 LT, and (d) 1100 LT.
