I am making just another attempt to find a layman's explanation about what climate sensitivity numbers can mean about future world temperatures. (realclimate.org)
I can't tell if he's arguing for — a higher climate sensitivity number, or — a higher variability, or f — a change in trend, or — something else (realclimate.org)
So what happens if we calculate dT, dN, and dF at every gridpoint of the model, use that to solve for climate sensitivity and then take the average to have a global climate sensitivity number? (andrewgelman.com)