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Doomsday Glacier melting faster than projected, doubling sea level estimate

Doomsday Glacier melting faster than projected, doubling sea level estimate

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New model of warm seawater seeping under Thwaites glacier raises its 2100 sea level contribution to 30mm

Overview

Updated Oct 22

Warm seawater pushes several kilometers inland beneath Thwaites Glacier, and a model that accounts for it doubles the glacier's projected contribution to sea level by 2100, to about 30mm. The study was published Oct. 12 in Nature Communications.

The model reproduced nearly 30 years of satellite observations of the glacier's retreat only when it treated the boundary between grounded and floating ice as a zone 2 to 5 kilometers wide. Simulations using a 5 to 6 kilometer zone, in line with recent satellite measurements, let Thwaites detach from the ridge that currently slows it as early as 2038.

Why it matters

Thwaites holds enough ice to raise sea levels more than 2 feet, and it holds back a far larger ice sheet behind it.

Questions about this story

Free account needed to ask — your question is kept and asked for you right after sign-up. Answers are public.

By 2100 what is the consensus opinion as to how high sea levels will likely have risen?

Consensus assessments put global sea level roughly 0.3–1.3 m higher by 2100 — at least 0.3 m even with the lowest emissions, and up to ~2 m if Antarctic ice collapse accelerates.

The new Thwaites result is part of why high-end estimates keep climbing: a single glacier could add ~30 mm, twice what models previously projected.

4 details5 sources2 disagreements
  • NOAA's 2022 interagency task force: even on the lowest-emissions path (1.5°C), global mean sea level rises at least 0.3 m (1 ft) above 2000 levels by 2100; on a very high-emissions path with rapid ice-sheet collapse, it could reach 2 m (6.6 ft).
  • An expert survey in npj Climate and Atmospheric Science gives likely ranges of 0.30–0.65 m under RCP2.6 and 0.63–1.32 m under RCP8.5 by 2100 (relative to 1986–2005), with a median of 0.93 m for high emissions.
  • A structured expert judgment study in PNAS puts the ice-sheet contribution alone at a median of 26 cm for a +2°C world and 51 cm for +5°C; adding thermal expansion and glaciers pushes the 95th percentile total above 2 m.
  • The new Thwaites model, published in Nature Communications, doubles that glacier's projected contribution to ~30 mm by 2100 — roughly twice the ISMIP6 ensemble mean of 15.2 mm.
Room for disagreement
  • The main split is over the upper tail: some experts (PNAS survey) see a real chance of >2 m by 2100 under high emissions, while the NOAA task force and IPCC-style model ensembles treat multi-meter rise by 2100 as unlikely, seeing it as a later-century risk.
  • The Thwaites result itself is contested: co-author Eric Rignot argues the grounding-zone physics is missing from most models and projections are too low, while British Antarctic Survey's Robert Larter cautions the subglacial environment is more complex than the model assumes and needs direct measurement.

Okay well, that doesn't sound that bad. How many levees and dikes do you think we'll need to build to prevent overflow into cities and stuff that are by the ocean?

There is no single number, but shielding all vulnerable coastal cities would mean building and upgrading tens of thousands of kilometers of levees and sea walls — at a cost in the trillions of dollars — and even then it wouldn't fully prevent overflow.

Hardening every coastline is physically and financially impossible; the real choice is which cities to defend and which to retreat from.

4 details3 sources2 disagreements
  • One global analysis estimated that protecting the world's coastlines against a 1-meter sea-level rise could require roughly 50,000 km of new or upgraded levees and flood barriers.
  • Cost estimates for coastal protection run into the trillions of dollars: the U.S. National Climate Assessment and similar studies put the price of defending major U.S. coastal cities alone at hundreds of billions to over $1 trillion.
  • Even with levees, cities face overflow from storm surge, groundwater seepage, and rainfall flooding — water that gets around or under barriers, which is why places like New York, Rotterdam, and Jakarta are combining walls with elevated land, pumps, and planned retreat.
  • The new Thwaites study adds to the problem: its 30 mm contribution by 2100 is only one glacier, and total global sea-level rise of 0.5–1.9 m under high emissions means defenses must be built to far higher standards than most existing ones.
Room for disagreement
  • Some engineers argue mega-barriers like the Thames Barrier or the MOSE system in Venice can protect major cities for decades, while others say these projects are too slow and costly, and that managed retreat is unavoidable for many coastal areas.
  • Estimates of how much protection is needed diverge widely because they depend on emissions scenarios and on how much risk society accepts — a 0.5 m rise requires far less defense than a 2 m rise, and the new Thwaites findings push upper-end projections higher.

Well if we're talking a slow 100-year progression, I think we'll be able to figure it out.

I'll search for evidence on sea level rise acceleration, locked-in commitments, and adaptation limits to answer this skeptical follow-up.
0 AI answers with web search. May be wrong.

Key Indicators

30mm
Projected sea level rise from Thwaites by 2100 — double prior estimate
Up from roughly 15mm. The projection assumes no additional global warming.
2038
Earliest year Thwaites could unpin from Mouginot Ridge
In simulations using a 5 to 6 kilometer grounding zone, matching recent satellite measurements of seawater intrusion.
60%
Chance Thwaites unpins from Mouginot Ridge by 2100
For grounding zones 4 to 6 kilometers wide. Zones of 2 to 3 kilometers lower the odds to about 45%.
4x
How much closer the model matched satellite data than models without a grounding zone
Compared against satellite records of retreat, thinning and acceleration dating back to the 1990s.
4%
Thwaites' current share of global sea level rise
The glacier has lost more than 1,000 billion tonnes of ice since 2000.
50 billion tonnes/yr
Annual ice loss rate
Ongoing loss driven by warm ocean water melting the glacier from beneath.

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People Involved

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Timeline

4 events Latest: October 20th, 2026 · 3 weeks ago
Tap a bar to jump to that date
  1. NASA publishes its own readout of the Thwaites model

    Latest Research

    A NASA Science News writeup says the model matched satellite records from the 1990s onward four times more closely than models without a grounding zone, and names Dartmouth College as a partner with UC Irvine and JPL.

  2. New model doubles Thwaites sea level projection

    Research

    Study incorporating a wide grounding zone with tidal pumping finds Thwaites could add 30mm to sea level by 2100 — twice prior estimates — even without further warming.

  3. Grounding-zone model published in Nature Communications

    Publication

    UC Irvine and NASA JPL researchers publish an ice-sheet model that treats the grounding line as a zone up to 5 kilometers wide, where tides push warm seawater deep under the ice.

  4. Separate modeling shows Thwaites retreat is locked in

    Research

    A second study finds Thwaites will continue losing ice for at least 150 years even if ocean melting stops entirely, though the rate of loss would slow.

Scenarios

1

Under-ice sensors confirm Thwaites tidal pumping

Likely Resolves by End of 2028

Discussed by: Study authors Mattia Poinelli and Eric Rignot; independent expert Robert Larter of British Antarctic Survey

Researchers agree the environment beneath Thwaites is hard to reach and the model lacks direct confirmation. If drilling or seafloor sensors document warm seawater intrusion at the grounding zone, the doubled projection gains strong support.

2

International ice-sheet models adopt the grounding-zone approach

Possible Resolves by End of 2030

Discussed by: Eric Rignot and the broader glaciology community

If the new grounding-zone treatment spreads into the international ice-sheet models that feed the next IPCC assessment, global sea level projections would rise accordingly. This depends on replication and acceptance by other modeling groups.

3

Satellites detect accelerating unpinning from Mouginot Ridge

Possible Resolves by End of 2032

Discussed by: Study authors and NASA satellite monitoring programs

The study puts a 60% chance that Thwaites unpins from Mouginot Ridge by 2100. Continuous satellite tracking could show the grounding line retreating faster than its historical trend well before mid-century, providing an early warning signal.

4

Thwaites unpins from Mouginot Ridge before 2050

Possible Resolves by End of 2050

Discussed by: Study authors Mattia Poinelli and colleagues at UC Irvine and NASA JPL

Simulations with a 5 to 6 kilometer grounding zone, matching recent satellite measurements of seawater intrusion, put unpinning as early as 2038. Once the ridge stops holding the glacier, retreat continues across a downhill seafloor toward the next high point, South Ridge.

Historical Context

2 moments from history that rhyme with this story — and how they unfolded.

February-March 2002

Larsen B ice shelf collapse (2002)

The Larsen B ice shelf on the Antarctic Peninsula, an area roughly the size of Rhode Island, disintegrated into thousands of icebergs over about five weeks. Satellite images showed the shelf shattering after decades of warming and surface meltwater flooding its crevasses.

Then

Glaciers behind the shelf accelerated their flow into the ocean several-fold within months, showing how quickly ice can respond when a floating barrier is removed.

Now

The collapse became the benchmark case for rapid, non-linear ice-sheet response, and it surprised scientists who had assumed such disintegration took centuries.

Why this matters now

Like Thwaites today, Larsen B showed Antarctic ice can change faster than models projected. The new Thwaites research extends that lesson to a far larger glacier with global sea level consequences.

1990s-2010s

Jakobshavn Isbræ glacier acceleration (Greenland, 2000s-2010s)

Jakobshavn Isbræ, Greenland's fastest-flowing glacier, doubled its flow speed over roughly a decade as warm ocean water melted the base of its floating tongue. The glacier's front retreated more than 20 kilometers inland.

Then

The meltwater it discharged into the ocean drew global attention and became the Greenland ice sheet's single largest contributor to sea level rise.

Now

Monitoring continued to show it can re-advance when ocean temperatures cool slightly, evidence that some glaciers respond to forcing changes while others do not.

Why this matters now

Jakobshavn shows ocean-warming-driven glacier acceleration can be detected and tracked in near-real time. The same satellite tools are now the primary evidence base for measuring Thwaites' ongoing retreat.

Sources

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