Figure 1
From: Aerosol effect on the evolution of the thermodynamic properties of warm convective cloud fields
Temporal changes compared to the initial profiles of mean environmental temperature [K] (left column) and mean water vapor mixing ratio [g/kg] (right column).
Each row shows the temporal evolution of the differences for a given aerosol concentration (5, 50, 250 and 2000 cm−3). Black lines present the 10 minutes running average of the maximum cloud top height.
