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The most robust change consists of cooling (and freshening) on isopycnals, with peak differences exceeding -1.0°C (-0.25 pss) at the base of the subtropical thermocline. The cooling and freshening starts above the stratification minimum of the Subantarctic Mode Water and persists to below the salinity minimum of the Antarctic Intermediate Water. Amplitudes are largest at 48°S, near where these water...