What caused Earths temperature variations during the last 800,000 years? Data-based evidences on radiative forcing and constraints on climate sensitivity

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Earth's energy imbalance and implications (2011, background): “aximum and the Holocene to be 3.3 W/m2, and they thus infer that climate sensitivity for doubled CO 2 is 1.8 ± 0.5°C for doubled CO 2. With the same approach, but assuming a dust forcing of 1.9 W/m2, Kohler et al. (2010) conclude that climate sensitivity is in the range 1.4‒5.2°C for doubled CO 2. B”
Paleoclimate Implications for Human-Made Climate Change (2011, background): “aximum and the Holocene to be 3.3 W/m2, and they thus infer that climate sensitivity for doubled CO 2 is 1.8 ± 0.5°C for doubled CO 2. With the same approach, but assuming a dust forcing of 1.9 W/m2, Kohler et al. (2010) conclude that climate sensitivity is in the range 1.4‒5.2°C for doubled CO 2. B”
Deglaciation in the tropical Indian Ocean driven by interplay between the regional monsoon and global teleconnections (2013, background): “Tropical changes in response to rising northern hemisphere insolation and/or rising greenhouse gases have been identified as a potential factor driving deglaciation (Rodgers et al., 2003; Ivanochko et al., 2005; Chiang, 2009; Köhler et al., 2010).”