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

<div>Multimodel climatological mean (30 years) of the difference (aerosol run minus CTL run) of summer surface temperature (shading; units: K), SLP (contours; units: hPa), and 850 hPa winds (vectors; units: m/s).</div>

Advances in Meteorology

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Figure 3

Figure 3: On the Robustness of the Weakening Effect of Anthropogenic Aerosols on the East Asian Summer Monsoon with Multimodel Results 