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

Table 3

Convective precipitation (PRCC) and large-scale precipitation (PRCL) difference between the aerosol run and CTL run and the ratio of the difference to the total precipitation decrease.

Model name	Total decrease; (mm/day)	PRCC		PRCL
		Decrease; (mm/day)	Percentage; (%)	Decrease; (mm/day)	Percentage; (%)
BCC-CSM1.1	−0.01	−0.016	153.3	0.006	−53.3
CanESM2	−0.4	−0.24	58.8	−0.16	41.2
CSIRO-Mk3.6.0	−0.5	−0.47	94.0	−0.03	6.0
FGOALS-s2	−0.01	−0.03	300.0	0.02	−200.0
GFDL-CM3	−0.88	−0.72	81.8	−0.16	18.2
HadGEM2-A	−0.2	−0.12	57.9	−0.08	42.1
IPSL-CM5A-LR	−0.17	−0.27	160.1	0.10	−60.1
MIROC5	−0.89	−0.73	82.5	−0.16	17.5
MRI-CGCM3	−0.15	−0.08	55.1	−0.07	44.9
NorESM1-M	−0.17	−0.15	88.2	−0.02	11.8
Ensemble	−0.34	−0.28	82.4	−0.06	17.6