Importance of the Numerical Representation of Shallow and Deep Convection for Simulations of Dust Transport over a Desert Region

Figure 1

Initial vertical profiles of (a) potential temperature (in K), (b) water vapor mixing ratio (in kg kg⁻¹), and (c) horizontal wind speed (in m s⁻¹, x-component) for the EXP1 (solid lines) and the EXP2 cases (broken lines).

(a)

(b)

(c)