A new study reveals that surface waters around Antarctica are growing saltier, not fresher, as sea ice rapidly declines. This unexpected trend, observed since 2015 using ESA’s SMOS satellite, challenges long-standing climate models and raises alarms over a dangerous climate feedback loop.
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- Sea surface salinity rising in Antarctic waters since 2015
- Goes against expectation: melting ice should make surface water fresher
- Over 2 million sq km sea ice lost—area equal to Greenland
- Saltier water allows heat to rise, melting ice from below
- This hinders formation of new sea ice
- Unusual reappearance of Maud Rise polynya after decades signals instability
- Less sea ice = more heat absorbed = faster global warming
- Disrupts ocean currents and global climate balance
- Threatens Antarctic species like penguins, seals losing habitat
- Study by University of Southampton, aided by ESA’s SMOS data and AI tools




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