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

Table 4

Comparisons between the aerosol run and the CTL run in East China in terms of specific humidity, moisture flux, and convergence/divergence at 850 hPa.

Model name	Specific humidity (g/kg)			Water vapor flux; (g/(hPa·m·s))			Convergence/divergence; (10^−5 g/(hPa·m^2·s))
	CTL	Aerosol	Aerosol−CTL	CTL	Aerosol	Aerosol−CTL	CTL	Aerosol	Aerosol−CTL
BCC-CSM1.1	9.33	9.37	0.04	32.63	31.58	−1.05	−0.75	−0.69	0.06
CanESM2	11.79	11.54	−0.24	31.69	29.13	−2.56	−0.66	−0.56	0.10
CSIRO-Mk3.6.0	12.30	12.16	−0.14	26.50	23.74	−2.76	−0.21	−0.07	0.14
FGOALS-s2	8.60	8.70	0.10	40.70	39.09	−1.61	−0.77	−0.81	−0.04
GFDL-CM3	10.05	9.66	−0.38	21.78	19.10	−2.68	−0.03	0.18	0.21
HadGEM2-A	10.90	10.76	−0.14	23.38	20.12	−3.26	−0.91	−0.91	0.00
IPSL-CM5A-LR	9.10	9.07	−0.03	15.85	15.03	−0.82	−0.35	−0.31	0.04
MIROC5	11.50	11.10	−0.40	37.65	33.77	−3.88	−1.53	−1.08	0.45
MRI-CGCM3	7.25	7.33	0.08	24.19	23.92	−0.27	0.28	0.33	0.05
NorESM1-M	11.08	10.89	−0.19	43.00	36.05	−6.94	−0.44	−0.32	0.12
Ensemble	10.19	10.06	−0.13	29.74	27.15	−2.59	−0.54	−0.42	0.12