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

Table 2

The EASMI calculated by the Guo and Han indices in the CTL and aerosol runs.

Model	Guo index; (CTL run)	Guo index; (aerosol run)	Han index; (CTL run)	Han index; (aerosol run)
BCC-CSM1.1	−31.41	−30.93	−4.82	−5.03
CanESM2	−48.66	−46.9	−7.99	−8.7
CSIRO-Mk3.6.0	−55.31	−53.4	−9.13	−9.31
FGOALS-s2	−39.86	−39.29	−4.44	−5.10
GFDL-CM3	Null	−28.84	−9.40	−10.8
HadGEM2-A	−47.21	−46.6	−3.47	−4.7
IPSL-CM5A-LR	−31.07	−30.80	−13.50	−13.40
MIROC5	−54.13	−49.0	−5.40	−7.3
MRI-CGCM3	−21.10	−20.68	−13.98	−14.4
NorESM1-M	−44.02	−42.74	−5.62	−6.9
Ensemble results	−41.00	−39.4	−7.10	−7.7

Significant at the 0.10 level; significant at the 0.01 level; “Null” indicates that the SLP data in the GFDL-CM3 CTL run are missing.