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FIGURE 2. Northern Hemisphere mean radiative forcing.

From the following article:

Climate sensitivity constrained by temperature reconstructions over the past seven centuries

Gabriele C. Hegerl, Thomas J. Crowley, William T. Hyde and David J. Frame

Nature 440, 1029-1032 (20 April 2006)

doi:10.1038/nature04679

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Sub-annual forcing data are used in the climate model simulations, but a decadal filter is applied here for illustration only, to focus on timescales most relevant for the analysis. For tropospheric aerosol forcing (green), a range of forcing has been used; for solar (pink) and volcanic (blue) forcing, a best guess forcing (dark, thick line) and a gaussian uncertainty range has been used (2.5% and 97.5% limits are shown by light, thin lines, the lower limit for solar is on the zero line). For clarity, greenhouse gas ('GHG') and aerosol forcings are offset by 3 W m-2, and solar forcing by 1 W m-2.

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