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Differences between variable probability distributions are quantified using the Kolmogorov-Smirnov $D$-statistic. For illustrative purposes, in this work, annual-mean spatial-mean 2m air temperature (TAS) over a region denoted as the ``Southern Ocean'' (SO; the circumglobal domain defined by $-65\0{}\leq\phi\leq-40\0{},$ where $\phi$ denotes latitude) is used. For %For  the purpose of this discussion, therefore,