Fig. 3From: Response of the atmospheric hydrological cycle over the tropical Asian monsoon regions to anthropogenic aerosols and its seasonalityDifferences in 30-year climatological a AOD, b SAT, c clear-sky downward shortwave radiation at the surface (DSRS), d the difference between all-sky DSRS and clear-sky DSRS (indirect effect), e cloud cover, f precipitation, g precipitable water during JJA between the ensemble-averaged HIST and piAERO (HIST - piAERO). Both HIST and piAERO values were averaged over the 30-year period from 1976 to 2005. All differences are shown when the local statistical significance level is at least 95%, as determined by Student’s t testBack to article page