Table 1 Global mean values for radiative forcing from aerosol-radiation interactions (RFari) and effective radiative forcing from aerosol-radiation and aerosol-cloud interactions with rapid adjustments (ERFaer) at the top of the atmosphere, as net flux perturbations in the solar and terrestrial spectra, calculated with the Ghan96 method for the various experiments with different prescribed κ parameterizations to assess the corresponding sensitivity of ECHAM–HAM

From: Global organic and inorganic aerosol hygroscopicity and its effect on radiative forcing

Model experiment

κinorg

κorg

RFari [W m−2]

ERFaer [W m−2]

Reference case

0.60

0.06

− 0.109 ± 0.004

− 1.757 ± 0.018

κOC = κorg

0.60

0.12

− 0.110 ± 0.004

− 1.748 ± 0.019

κSU = κinorg

0.63

0.06

− 0.118 ± 0.004

− 1.771 ± 0.020

κOC = κorg & κSU = κinorg

0.63

0.12

− 0.120 ± 0.004

− 1.773 ± 0.019

  1. Uncertainty in RFari and ERFaer represents the standard deviation of the multi-year simulations.