deletions | additions       diff --git a/In_autorefFigureKair.tex b/In_autorefFigureKair.tex  index 76d3817..0cbe547 100644  --- a/In_autorefFigureKair.tex  +++ b/In_autorefFigureKair.tex 
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In \autoref{Figure:Kairodic} distributions obtained by applying each of the quantification approaches to the Yr587 ensemble trajectories illustrated in \autoref{Figure:ClimateQuantifications} are shown. Note that the trajectories from which were sampled to obtain the Run28 and Run45 distributions in \autoref{Figure:Kairodic}, are highlighted in \autoref{Figure:ClimateQuantifications}. The distributions thus obtained are significantly different ($D \approx 0.53, 0.65,  p < 10^{-7}$). 10^{-10}$).  The difference distributions for year 30 and Run45 is also large ($D \approx 0.28, 0.40,  p < 0.05$), 0.001$),  as is the difference differences  between the Run28 Run48  TCQ and the decade 6 (``settled'') ETCQ ($D \approx 0.41, 0.53,  p < 10^{-7}$). 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.