Full Breakdown
Potential Irreversible Collapse of West Antarctic Ice Sheet Identified
6/21/2026, 11:22:03 AM
Potential Irreversible Collapse of West Antarctic Ice Sheet
A June 2025 modelling study indicates that the West Antarctic Ice Sheet (WAIS) could enter an irreversible collapse when deep-ocean temperatures around the Amundsen Sea rise by 0 °C to 0.25 °C above present levels. Once initiated, the collapse would be self-sustaining, eventually adding roughly four metres of sea-level rise over centuries to millennia.
Marine Ice Sheet Instability
The authors identify marine ice sheet instability as the driver. WAIS rests on bedrock below sea level, with ice shelves buttressing grounded ice. Warm Circumpolar Deep Water undercuts the shelves, thinning them. Grounding-line retreat into deeper water reduces stability, enabling self-accelerating ice loss without additional warming.
Scientific Debate on WAIS Tipping Point
Using an 800 000-year model baseline, the authors—David Chandler, Petra Langebroek, Ronja Reese, Torsten Albrecht, Julius Garbe, and Ricarda Winkelmann—from the Potsdam Institute for Climate Impact Research, NORCE, and Northumbria University—note that their result is a single modelling outcome, not settled consensus. A 2023 study concluded WAIS had not yet crossed a tipping point, underscoring debate. Variations in ice physics, ocean forcing, and bedrock representation across models lead to differing thresholds.
Quantitative Outlook
- Threshold: 0 °C–0.25 °C increase in deep-ocean temperature near the Amundsen Sea embayment.
- Sea-level contribution: ~4 m at equilibrium, unfolding over centuries to millennia.
- Timescales: destabilisation can trigger within decades; full ice-sheet growth needs tens of thousands of years.
Global Implications
A four-metre sea-level rise would set a new equilibrium far beyond current infrastructure design lives, affecting coastlines worldwide. The rapid trigger versus prolonged consequence creates a “very long tail” that challenges conventional planning horizons.
Observational Gaps and Ongoing Efforts
The International Thwaites Glacier Collaboration’s field campaigns aim to provide ground-truth data for model validation. Determining whether observed deep-ocean temperatures are approaching the 0.25 °C increment remains an open question that oceanographic records will address in coming years.
Verbatim Quotes
- “25°C threshold in the model, the process continues even if ocean temperatures were to stop rising.” — Study authors
- “The four metres of sea-level rise is not a peak that would be reached and then reversed; it is the new equilibrium state the ice sheet would settle toward over the following centuries and millennia.” — Study authors
- “25°C increment the study identifies, and how quickly, is a question the oceanographic record will continue to answer over the next several years.” — Study authors
