deletions | additions       diff --git a/In_autorefFigureKair.tex b/In_autorefFigureKair.tex  index 0cbe547..b3d2ffd 100644  --- a/In_autorefFigureKair.tex  +++ b/In_autorefFigureKair.tex 
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In \autoref{Figure:Kairodic} Figure \ref{Figure:Kairodic}  distributions obtained by applying each of the quantification approaches to the Yr587 ensemble trajectories illustrated in \autoref{Figure:ClimateQuantifications} Figure \ref{Figure:ClimateQuantifications}  are shown. Note that the trajectories from which were sampled to obtain the Run28 and Run45 distributions in \autoref{Figure:Kairodic}, Figure \ref{Figure:Kairodic},  are highlighted in \autoref{Figure:ClimateQuantifications}. Figure \ref{Figure:ClimateQuantifications}.  The distributions thus obtained are significantly different ($D \approx 0.65, p < 10^{-10}$). The difference distributions for year 30 and Run45 is also large ($D \approx 0.40, p < 0.001$), as is the differences between the Run48 TCQ and the decade 6 (``settled'') ETCQ ($D \approx 0.53, p < 10^{-10}$). For SO TS, 60-year climate variable distributions often (in up to $\sim 30\%$) are detectably different from one another and the overall ensemble distribution.