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

<div>Difference between the aerosol run and CTL run in East China of (a) summer surface (a) temperature; (b) total radiation (black), shortwave radiation (red), and longwave radiation (blue) of aerosol forcing; and (c) direct (red) and indirect (blue) radiation of aerosol forcing. 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 4

Figure 4: On the Robustness of the Weakening Effect of Anthropogenic Aerosols on the East Asian Summer Monsoon with Multimodel Results 