Fig. 3 | Nature Communications

Fig. 3

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

Fig. 3

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

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