Fig. 2From: Response of the atmospheric hydrological cycle over the tropical Asian monsoon regions to anthropogenic aerosols and its seasonalityClimatology in a observed and b simulated precipitation and surface winds at 10 m above the surface during June, July, and August (JJA). c and d are the same as a and b, respectively, except for December, January, and February (DJF). For the observations, the values were averaged over 30 years from 1979 to 2008, and for the HIST simulation, the values were averaged over 30 years from 1976 to 2005. For the simulated climatology, we averaged the three-ensemble membersBack to article page