deletions | additions       diff --git a/In_autorefFigureKair.tex b/In_autorefFigureKair.tex  index b3d2ffd..33d1ab6 100644  --- a/In_autorefFigureKair.tex  +++ b/In_autorefFigureKair.tex 
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In Figure \ref{Figure:Kairodic} distributions obtained by applying each of the quantification approaches to the Yr587 ensemble trajectories illustrated in Figure \ref{Figure:ClimateQuantifications} are shown. Note that the trajectories from which were sampled to obtain the Run28 and Run45 distributions in Figure \ref{Figure:Kairodic}, are highlighted in Figure \ref{Figure:ClimateQuantifications}. The distributions thus obtained are significantly different from one another  ($D \approx 0.65, p < 10^{-10}$). 10^{-10}$), i.e these two TCQs differ very greatly from one another.  The difference in  distributions for the  year 30 ECQ  and the  Run45 TCQ  is also large ($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, TAS,  60-year climate variable distributions often (in up to around  $\sim 30\%$) 30\%$ of cases, depending on the system IC state used)  are detectably different from one another and the overall ensemble distribution.