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Study finds seawater under Thwaites Glacier doubles sea-level threat

A new study published in Nature Communications finds that seawater seeping under Thwaites Glacier could double its projected contribution to sea-level rise by 2100.

By Hermes-Vector AI Desk

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Illustration for: Study finds seawater under Thwaites Glacier doubles sea-level threat

In brief

  • Thwaites Glacier could contribute up to 30 millimeters to global sea-level rise by 2100, doubling previous estimates.
  • Satellite data shows seawater penetrates several kilometres beneath the glacier, accelerating melting and retreat.
  • There is a 60% chance the glacier detaches from the Mouginot Ridge before 2100 in best-fit simulations.
  • The study was published in Nature Communications and led by researchers from UC Irvine and NASA JPL.

Study finds seawater under Thwaites Glacier doubles sea-level threat

A new study published in Nature Communications estimates that Thwaites Glacier in West Antarctica could contribute up to 1.2 inches (30 millimeters) of global sea-level rise by 2100, even without additional climate warming. The findings, led by glaciologists from the University of California and NASA’s Jet Propulsion Laboratory, suggest the glacier’s threat to coastal areas is roughly double previous estimates.

Grounding Zone Dynamics

The study focuses on the "grounding zone," the area where ice transitions from resting on bedrock to floating on the ocean. Traditional models treated this boundary as a narrow, stable line. However, satellite radar data from the ICEYE constellation revealed that the grounding zone is several kilometres wide and shifts with the tides. This movement allows pressurized seawater to penetrate beneath the glacier’s grounded ice, lifting it and carrying ocean heat farther inland.

Eric Rignot, a professor of Earth system science at the University of California, Irvine, and co-author of the study, noted the significance of these findings. "We have documented and quantified the impacts of climate change on our planet’s sensitive ice sheets for decades, but a mounting realization gained in recent years of what is happening on the undersides of glaciers like Thwaites is leading to an even greater sense of alarm," Rignot said in a statement. "Our new model with more complete physics is able to match the record and then produces projections that are twice as large as before."

Model Projections and Uncertainty

The research team used the Ice-sheet and Sea-level System Model (ISSM) to simulate the glacier’s behavior. By incorporating a grounding zone that allows ocean melting to reach beneath the grounded ice, the model reproduced satellite observations of the glacier’s retreat, thinning, and acceleration over the past 20 years.

The study projects a 30-millimeter rise with an uncertainty of about 6 millimeters. This figure contrasts with the average of 15.2 millimeters projected by the international ISMIP6 model ensemble under the same conditions. The new model indicates that the glacier’s main trunk is currently held back by the Mouginot Ridge, a seafloor feature about 950 metres below sea level. According to the study, there is about a 60% chance the glacier slips off this ridge before the end of the century in simulations that best match current radar data. If this occurs, the seafloor deepens inland, potentially accelerating ice loss.

Limitations and Future Risks

The authors emphasize that the 30-millimeter projection is a lower-bound scenario. It assumes the ocean and climate remain at their 1996 to 2023 average, excluding further warming or changes in warm water layers that could increase melting. The model also simplifies certain factors, such as holding the width of the grounding zone fixed and ignoring iceberg calving.

Despite these limitations, the study highlights a specific vulnerability. "The Thwaites main trunk is being temporarily stabilized by the Mouginot Ridge," said Mattia Poinelli, the study’s lead author. The researchers argue that actively melting grounding zones must be integrated into regional and continental ice-sheet models to improve future predictions.

Why it matters

Thwaites Glacier, often referred to as the "Doomsday Glacier," holds enough ice to raise global sea levels by approximately 65 centimeters if it were to melt completely. The region behind the glacier already accounts for about a third of the ice Antarctica loses. An increase in projected sea-level rise from this single glacier raises the baseline for coastal flooding risks worldwide, affecting high tides and storm surges in the coming decades.


Sources

This article was drafted with AI assistance and checked against the sources above. Company claims are reported as claims. Cover image is AI-generated.

Questions readers ask

How much sea-level rise could Thwaites Glacier contribute by 2100?
A new study estimates that Thwaites Glacier could contribute up to 1.2 inches (30 millimeters) of global sea-level rise by 2100. This figure is roughly double previous estimates and assumes no additional climate warming.
Why is the grounding zone important for Thwaites Glacier?
The grounding zone is where ice transitions from resting on bedrock to floating on the ocean. Satellite data revealed it is several kilometres wide and shifts with tides, allowing pressurized seawater to penetrate beneath the glacier and carry ocean heat inland.
What feature currently stabilizes the main trunk of Thwaites Glacier?
The glacier's main trunk is currently held back by the Mouginot Ridge, a seafloor feature about 950 metres below sea level. The study indicates there is about a 60% chance the glacier slips off this ridge before the end of the century.
What are the limitations of the 30-millimeter projection?
The 30-millimeter projection is a lower-bound scenario that assumes the ocean and climate remain at their 1996 to 2023 average. It excludes further warming and simplifies factors like holding the grounding zone width fixed and ignoring iceberg calving.
Why is Thwaites Glacier called the "Doomsday Glacier"?
Thwaites Glacier holds enough ice to raise global sea levels by approximately 65 centimeters if it were to melt completely. The region behind the glacier already accounts for about a third of the ice Antarctica loses.

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