On the Robustness of the Weakening Effect of Anthropogenic Aerosols on the East Asian Summer Monsoon with Multimodel Results

<div>(a) Summer precipitation of the aerosol run (red bars) and CTL run (black bars) for each model over East China. (b) Same as (a), except for the precipitation difference between the aerosol run and CTL run (aerosol minus CTL). (c) Ratio of precipitation differences in (b) to the CTL run in each model. The far right bar and purple line in each panel are the ensemble mean and standard deviation from all simulations, respectively.</div>

Advances in Meteorology

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Figure 2

Figure 2: On the Robustness of the Weakening Effect of Anthropogenic Aerosols on the East Asian Summer Monsoon with Multimodel Results 