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1 Introduction The Southern Ocean (SO) is characterized by the zonally unbounded energetic flow of the Antarctic Circumpolar Current (ACC), which consists of several jets that delineate hydrographic properties (Orsi et al., 1995). South of the Antarctic Polar Front (PF), salinity is the dominant property of density in the upper ocean due to a low thermal expansion coefficient (Roquet et al., 2022; Stewart & Haine, 2016).
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