Fig. 3
From: Aerosol-induced intensification of cooling effect of clouds during Indian summer monsoon

Variation in occurrence of tower and anvil clouds under low and high aerosol loading scenarios. Contour plot of TAR versus CTP as a function of cloud frequency for a low AOD, b high AOD, and c difference (high–low AOD). d WRF model simulated difference (high–low aerosol) in the cloud frequency as a function of cloud thickness and cloud top height for the deep convection clouds