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. 2017 Nov 13;114(48):12685–12690. doi: 10.1073/pnas.1712273114

Table 2.

Direct and first IRF and the difference in the composition burden in FUCLI and FUALL scheme

Parameter Scenario or SOA type FUCLI* FUALL
DRF, W m−2 21M20C (2100 Met + 2000 Conc) −0.0028 −0.0028
20M21C (2000 Met + 2100 Conc) −0.0434 −0.0226
21M21C (2100 Met + 2100 Conc) −0.0470 −0.0251
First IRF, W m−2 21M20C (2100 Met + 2000 Conc) −0.0006 −0.0006
20M21C (2000 Met + 2100 Conc) −0.0028 −0.0414
21M21C (2100 Met + 2100 Conc) −0.0035 −0.0426
Difference of composition burden (future-present day), mg m−2 SOASO42− (nucleation) −0.011 −0.013
SOASO42− (Aitken) −0.001 0.094
SOASO42− (accumulation) 0.295 −0.043
SOASoot (fossil fuel) 0.074 0.053
SOASoot (biomass burning) 0.151 0.049
SOAother (sea salt + dust) 0.002 0.005
Total SOA 0.510 0.145
*

FUCLI is the scheme with only climate and CO2 change in the future.

FUALL is the scheme with the combined effects of changes in climate, anthropogenic emissions, and land use in the future.