Table S1.

Diagnostic quantities displayed as the mean and SD within the moderate subsidence regimes ($18\le {\omega }_{500}\le 28$ hPa⋅d⁻¹) over tropical oceans (35°S−35°N)

Model	SWCRE	LCL	${\text{CF}}_{\text{LCL}}$	${\text{CF}}_{850}$	LTS	${\text{RH}}_{850}$	$\mathrm{\Delta }\text{R}{\text{H}}_{700-850}$	${\text{p}}_{\mathrm{inv}}$
ERAI/Satellite	−37 ± 11	957 ± 7	17.4 ± 8.9	6.8 ± 6.17	16.2 ± 1.12	60.6 ± 7.50	−29.2 ± 9.0	811 ± 56
BCC-CSM1-1-m	−50 ± 13	954 ± 13	21.0 ± 7.19	14 ± 4.11	16.1 ± 1.42	63.7 ± 7.03	−28.4 ± 9.2	775 ± 71
CanAM4	−38 ± 13	950 ± 12	20.8 ± 7.87	3.75 ± 3.04	14.7 ± 1.29	56.6 ± 9.06	−23.8 ± 11.1	808 ± 67
CCSM4	−40 ± 16	946 ± 20	16.5 ± 5.82	16.2 ± 4.7	15.7 ± 1.2	69.7 ± 7.06	−33.0 ± 10.2	741 ± 62
CESM1-CAM5	−37 ± 10	925 ± 18	19.3 ± 5.46	7.87 ± 4.86	15.2 ± 1.24	66 ± 8.04	−19.6 ± 6.9	756 ± 68
CNRM-CM5	−26 ± 11	938 ± 22	7.48 ± 4.13	6.86 ± 3.74	15.6 ± 1.07	61.9 ± 8.38	−34.5 ± 10.5	815 ± 49
GFDL-CM3	−35 ± 12	945 ± 17	10.9 ± 6.36	8.09 ± 5.31	16.7 ± 1.33	65.5 ± 8.71	−35.1 ± 11.8	816 ± 55
HadGEM2-A	−37 ± 12	953 ± 15	9.97 ± 6.06	8.51 ± 4.14	15.3 ± 1.31	58.4 ± 8.25	−27.1 ± 10.7	796 ± 72
IPSL-CM5A-LR	−41 ± 14	957 ± 16	15.3 ± 9.07	2.16 ± 2.07	15.4 ± 1.24	59.4 ± 8.54	−20.6 ± 12.4	745 ± 71
IPSL-CM5B-LR	−41 ± 15	948 ± 14	20.3 ± 11	2.3 ± 2.5	14.1 ± 1.16	65.4 ± 8.35	−20.7 ± 9.7	704 ± 60
MIROC5	−58 ± 12	914 ± 18	21.6 ± 6.78	14.1 ± 6.13	14.4 ± 1.33	68.2 ± 9.69	−29.3 ± 12.3	821 ± 47
MPI-ESM-LR	−35 ± 15	960 ± 16	10.8 ± 8.67	2.49 ± 2.61	14.6 ± 1.38	64.9 ± 7.41	−23.4 ± 10.5	758 ± 60
MRI-CGCM3	−41 ± 16	944 ± 13	8.42 ± 5.38	7.13 ± 3.7	15.4 ± 1.29	65.5 ± 7.11	−24.4 ± 9.1	754 ± 60

From left to right are SWCRE, pressure of diagnosed LCL, CF at that model level, CF at the model level nearest 850 hPa, LTS, relative humidity at 850 hPa, $\mathrm{\Delta }{\text{RH}}_{700-850}$, and the inversion level ($p_{\mathrm{inv}}$). The variability reported is the area-weighted average of the temporal SD; the average area-weighted SD is larger for all quantities because of the spatial variability.