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Fig. 7 | Progress in Earth and Planetary Science

Fig. 7

From: A review of progress towards understanding the transient global mean surface temperature response to radiative perturbation

Fig. 7

Effective radiative forcing for the doubling of atmospheric CO2 concentration estimated with Hansen’s method and Gregory’s method for 10 CMIP5 models. See the text for the details. The data taken from Table 9.5 of Flato et al. (2013). The one-to-one line is also plotted. The number at the lower right corner of the figure indicates the fractional variance shared by the two variables. The right column lists the model names with their numbers, which are identical to those in Fig. 1

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