emissions are presented – the Global Warming Potential and the Global Temperature- 22.

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solar radiative forcing for understanding climate change, in lieu of direct observations of

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has been determined that when mass forces at plane deformation state aren’t considered strain communication area of initial strain viscous –elastic medium

and solar forcings [ Lambert and Faull , 2007; Andrews et al. , 2009] it is the purpose of this article to quantify and assess how robust this is across a range of different

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the Transient Climate Response to Emissions by physical feedbacks, heat uptake, radiative forcing and carbon