Fig. 3From: An exponential-interval sampling method for evaluating equilibrium climate sensitivity via reducing internal variability noisea The correlation coefficient between the global-mean and annual-mean surface temperature anomalies \(\Delta T\) and TOA net radiative flux anomalies \(\Delta N\) in the abrupt4xCO2 experiments (relative to the piControl run) of LongRunMIP models. b The product of dN/dT (slope of the linear fit between \(\Delta T\) and \(\Delta N\)) and dT/dN (slope of the linear fit between \(\Delta N\) and \(\Delta T\))Back to article page