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Saltier Southern Ocean Fuels Antarctic Ice Loss as U.S. Data Cuts Loom

Accelerating Antarctic ice loss through a salt-driven feedback loop, researchers now face the end of U.S. microwave data access on July 31

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Overview

  • Since 2015 surface salinity south of 50° latitude has surged, reversing decades of freshening and weakening the ocean’s stratification
  • Saltier surface waters draw deep heat upward in a feedback loop that has driven Antarctic sea ice to record lows and reopened the Maud Rise polynya
  • Summers with extreme ice loss now produce more than twice as many icebergs, exposing ice shelves and threatening species like emperor penguins and krill
  • The Southern Ocean retains excess heat for up to three years after low-ice summers, compounding warming and challenging existing climate models
  • The U.S. Department of Defense will stop delivering SSMIS microwave data after July 31, jeopardizing long-term monitoring of future sea ice extremes