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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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Gliders were deployed for the very first time in the Agulhas Current region to investigate processes of interactions between western boundary currents and shelf waters. Continuous observations from the gliders in water depths of 100–1000?m and over a period of 1?month provide the first high resolution observations of the Agulhas Current's inshore front.
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