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. 2019 Dec 11;124(23):12824–12844. doi: 10.1029/2019JD030581

Table 1.

PDRMIP Multimodel Mean Radiative Forcing (See section 2.3 for Definitions), GSAT Response, Climate Feedback Parameter Calculated Using First 20 years (α_20), Final 80 years (α_80), and Full 100 years (α) of Simulations, and Efficacies (See section 2.4 for Definitions) for the Five Core Experiments

2×CO2 3×CH4 2%SOL 5×SO4 10×BC
IRF trop (W m−2) 4.45 ± 0.11 1.04 ± 0.09
IRF toa (W m−2) 2.20 ± 0.22 1.13 ± 0.13 4.81 ± 0.05 −1.73 ± 1.02 2.17 ± 1.08
RF strat (W m−2) 3.76 ± 0.27 1.21 ± 0.28 4.55 ± 0.06 −3.64 ± 1.20 2.29 ± 1.15
ERF sst (W m−2) 3.71 ± 0.30 1.15 ± 0.25 4.17 ± 0.13 −3.71 ± 1.94 1.18 ± 0.75
ERF ssta (W m−2) 4.19 ± 0.35 1.25 ± 0.31 4.32 ± 0.12 −3.78 ± 1.99 1.25 ± 0.80
ERF reg (W m−2) 3.81 ± 0.57 1.06 ± 0.25 3.89 ± 0.29 −3.70 ± 1.79 0.83 ± 0.53
ΔT (K) 2.44 ± 0.75 0.67 ± 0.33 2.46 ± 0.97 −2.45 ± 1.85 0.74 ± 0.54
α (W m−2/K) −1.19 ± 0.50 −1.06 ± 0.53 −1.24 ± 0.51 −1.11 ± 0.34 −0.89 ± 0.46
α_20 (W m−2/K) −1.27 ± 0.52 −1.28 ± 0.57 −1.36 ± 0.51 −1.51 ± 0.85 −0.97 ± 0.77
α_80 (W m−2/K) −1.03 ± 0.57 −0.93 ± 0.73 −1.04 ± 0.51 −0.80 ± 0.36 −0.78 ± 0.60
ΔT/IRF trop (K/W m−2) 0.55 ± 0.19 0.61 ± 0.33
ΔT/IRF toa (K/W m−2) 1.14 ± 0.44 0.57 ± 0.35 0.52 ± 0.21 1.25 ± 0.81 0.25 ± 0.21
ΔT/RF strat (K/W m−2) 0.66 ± 0.24 0.57 ± 0.29 0.54 ± 0.21 0.66 ± 0.25 0.40 ± 0.25
ΔT/ERF sst (K/W m−2) 0.67 ± 0.22 0.58 ± 0.23 0.59 ± 0.23 0.62 ± 0.19 0.63 ± 0.37
ΔT/ERF ssta (K/W m−2) 0.59 ± 0.19 0.54 ± 0.22 0.57 ± 0.22 0.61 ± 0.18 0.60 ± 0.34
ΔT/ERF reg (K/W m−2) 0.66 ± 0.25 0.66 ± 0.32 0.63 ± 0.25 0.63 ± 0.22 1.22 ± 1.45
E irf_trop 1.09 ± 0.35 0.89 ± 0.09 2.97 ± 1.86 0.54 ± 0.29
E irf_toa 0.48 ± 0.17 0.44 ± 0.04 1.50 ± 0.99 0.27 ± 0.13
E rf_strat 0.84 ± 0.21 0.81 ± 0.06 0.99 ± 0.09 0.55 ± 0.16
E erf_sst 0.87 ± 0.15 0.87 ± 0.07 0.94 ± 0.16 0.87 ± 0.31
E erf_ssta 0.91 ± 0.18 0.95 ± 0.07 1.04 ± 0.16 0.93 ± 0.32
E erf_reg 0.97 ± 0.23 0.96 ± 0.09 0.95 ± 0.25 1.48 ± 1.09
E α 1.22 ± 0.47 0.97 ± 0.12 1.01 ± 0.29 1.36 ± 0.26

Note. Uncertainty bounds are the standard deviation of the intermodel spread.