The Climate Sensitivity and Its Components Diagnosed from Earth Radiation Budget Data

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Tropospheric Adjustment Induces a Cloud Component in CO2 Forcing (2008, background): “The same suggestion has been made regarding observed TOA variations (Forster and Gregory 2006).”
An observationally based energy balance for the Earth since 1950 (2009, background): “The open blue points are literature values including seasonal variation [Tsushima et al., 2005; Forster and Gregory, 2006].”
Time-Varying Climate Sensitivity from Regional Feedbacks (2012, methodology): “This method has been widely applied to estimate feedbacks and forcing within both models and observations (Forster and Taylor 2006; Forster and Gregory 2006; Gregory and Webb 2008; Andrews and Forster 2008;Williams et al. 2008; Murphy et al. 2009; Boer 2011; Crook et al. 2011; Andrews et al. 2012a;…”
On the generation and interpretation of probabilistic estimates of climate sensitivity (2011, methodology): “For illustration of how these prior beliefs feed through into posterior estimates of climate sensitivity, we consider the ERBE data which were recently analysed by Forster and Gregory (2006) (henceforth FG).”
How reliable are climate models? (2007, background): “By contrast, Forster and Gregory (2006) derived a lower range (1.0–4.1◦C) and best estimate (1.6◦C) from the seasonal cycles of temperature and top-of-the-atmosphere radiation balance, assuming that the same feedback processes that regulate the seasonal cycle also determine the long-term climate…”