- Remote sensing confirms a shift from long-term freshening to increasing surface salinity south of 50° S, beginning around 2015.
- Denser surface waters are enhancing vertical mixing, allowing warmer subsurface water to reach the surface, accelerating Antarctic ice loss.
- The shift in surface salinity and stratification could impact deep ocean water formation and disrupt components of the global thermohaline circulation, including the Atlantic Meridional Overturning Circulation (AMOC).
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