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New Studies Trace Self-Reinforcing Antarctic Ice Retreat as Thwaites Shelf Weakens

Meltwater freshens the ocean surface, strengthening stratification that draws warm deep water beneath ice shelves.

Overview

  • Peer-reviewed research in Nature Geoscience led by Yusuke Suganuma identifies a cascading feedback that can drive widespread Antarctic retreat.
  • Sediment records from Lützow-Holm Bay show an ice-shelf collapse about 9,000 years ago with inland thinning up to roughly 400 meters.
  • A companion study in JGR: Earth Surface led by Debangshu Banerjee documents a four-stage rift-driven failure of the Thwaites Eastern Ice Shelf from 2002 to 2022.
  • The Thwaites work finds a positive feedback between rift damage and upstream acceleration after the shelf lost a stabilizing fixpoint.
  • Satellite observations indicate warm Circumpolar Deep Water is already reaching major West Antarctic shelves, raising concern that modern change may progress faster under human-driven warming.