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. 2009 Jun 12;44(37):4678–4734. doi: 10.1016/j.atmosenv.2009.06.005

Fig. 21.

Fig. 21

Summary of radiative forcing per component in 2050 (mW m−2), O3 and H2O radiative forcing average values and variability were calculated using the DLR model radiative code applied to O3 and H2O changes (S6-S4) calculated by UCAM, ULAQ, DLR and UiO CTMs (Pitari et al., 2008).