Importance of the Numerical Representation of Shallow and Deep Convection for Simulations of Dust Transport over a Desert Region
Figure 3
Horizontal cross-section of vertical velocity in the EXP1 case at 200 m height at (a) 0900 LT and at (b) 1500 LT, at 2 km height at (c) 0900 LT and (d) 1500 LT, and at 6 km height at (e) 0900 LT and at (f) 1500 LT. Contour intervals are indicated at the bottom of each panel. Positive (negative) values are indicated by solid (dashed) lines. The contour line of zero velocity is omitted.
