Thwaites Glacier Model Doubles Its Sea Level Rise by 2100
Topics: Planet & Energy

Jeff's Daily Pick. A UC Irvine and NASA JPL model says Antarctica's Thwaites Glacier could add up to 30 mm (about 3 cm, 1.2 inches) to global sea level by 2100, about double earlier projections, even with no further warming (Nature Communications).
In the United States, glaciologists at the University of California, Irvine and NASA's Jet Propulsion Laboratory published a study in Nature Communications on October 12, 2026 on Thwaites Glacier in West Antarctica, often called the Doomsday Glacier. Lead author Mattia Poinelli, now at UCLA, and coauthor Eric Rignot of UC Irvine changed how a computer model handles the place where the ice lifts off the seafloor.
From a line to a zone
Most ice sheet models treat the grounding line, where grounded ice starts to float, as a sharp boundary. Radar images from the ICEYE satellite constellation show something else on Thwaites: seawater pushes several kilometers under the grounded ice and lifts it with each tide, flushing warm water underneath. The team built this grounding zone into the ISSM ice sheet model and tested it against the observed retreat, thinning and speedup of the glacier from 1996 to 2023. The model matched the record only when the zone was 2 to 5 km wide. Runs without a grounding zone were four times less likely to reproduce it.
The numbers, read carefully
With a 5 km zone, close to what satellites show today, the model gives 30.1 mm of sea level rise from Thwaites by 2100, plus or minus 5.7 mm. That is twice the 15.2 mm average of the ISMIP6 group of models under the same constant climate. With a 3 km zone, the most likely value in the calibration, it gives 19.4 mm. With no grounding zone, 8.3 mm. Ocean conditions are held at their 1996 to 2023 average, so the authors call these lower bound figures.
Thwaites is now held in place by an undersea ridge, Mouginot Ridge. With a 4 to 6 km zone, the model puts the chance it breaks free by 2100 at about 60%, as early as 2038 in the widest runs. The 30 mm is not the 65 cm often quoted for Thwaites. That 65 cm is the glacier's total sea level equivalent, the rise if all its ice were lost, and this study does not project that for this century.
What it shows / what it doesn't
- Shows: adding the observed seawater intrusion lets a model reproduce nearly three decades of retreat, and doubles its projection for 2100.
- Doesn't show: a collapse of Thwaites this century.
- Doesn't show: the effect of future ocean warming. In a side test, water 0.5 to 0.7 °C warmer raised the projected loss by about 15%.
- Limits: the ice front is fixed, calving is left out and the zone width is held constant over time.
- Status: peer reviewed modeling study, funded by NASA grants with NSF and foundation support.
Thwaites sits in the Amundsen Sea sector, which accounts for about a third of the ice lost from the Antarctic Ice Sheet. For another large scale picture of the planet's changes, see our piece on 2025 deforestation.
Sources
Peer reviewed modeling study (Nature Communications)Poinelli M, Rignot E, Seroussi H, Cuzzone J, Pelle T, Larour E. Sea-level contribution from Thwaites Glacier doubles in an observation-constrained ice-sheet model. Nature Communications 17, 10364 (2026), published October 12, 2026. doi:10.1038/s41467-026-77976-1. nature.com
UC Irvine. UC Irvine, NASA JPL: Melting of Antarctica's Thwaites Glacier worse than thought. News release, October 12, 2026. ps.uci.edu
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