Listening to Antarctica: Seismic Thunder Beneath Thwaites Glacier Reveal Clues to Potential Collapse

Seismic waves released by earthquakes beneath the bed of the Thwaites Glacier aims to show how fast the glacier could disappear, contributing some 10 feet to global sea level rise.

By Jack Austin
Dec. 18. 2025

Amanda Willet’s research sits at the center of a high-stakes equation: predicting how fast sea levels will rise — and how coastal cities can defend themselves. An overestimate could waste billions of dollars. An underestimate could leave cities facing devastation on the scale of Hurricane Katrina.

Penn State Researcher Amanda Willet, at the Comer Climate Conference in Wisconsin, where she presented  research on seismic waves released by earthquakes beneath the bed of the Thwaites Glacier in Antarctica. (Jack Austin/ MEDILL)
Penn State Researcher Amanda Willet, at the Comer Climate Conference in Wisconsin, where she presented  research on seismic waves released by earthquakes beneath the bed of the Thwaites Glacier in Antarctica. (Jack Austin/ MEDILL)

Willet, a graduate student at Pennsylvania  State University, presented “Seismic Stories From Earth’s Frozen Frontiers: Thwaites Glacier, Antarctica,” at the fall 2025 Comer Climate Conference. She is pursuing her research with Professors Sridhar Anandakrishnan and veteran glaciologist Richard Alley,  the emcee for the annual Comer conference held in southwestern Wisconsin.

One reason sea level rise models remain uncertain, Willet said, is that scientists don’t yet know what lies beneath glaciers. Her team, in partnership with the British Antarctic Survey, is studying Thwaites — a glacier larger than Pennsylvania — because if it melts entirely, it could add 3 meters to global sea levels. That’s 9 feet, 10 inches of sea level rise, enough to inundate vast coastal areas and many islands. Thwaites is part of the West Antarctic Ice Sheet, which a Dartmouth study (combining data from 16 ice sheet models) concluded may disappear by 2300. 

“Depending on what the bottoms of these glaciers look like in big places like Antarctica depends on how much sea level rise we actually get,” Willet said. “If we want to understand sea level rise, we need to know what the bottoms of glaciers look like.”

Alley said that model predictions for Antarctica vary so widely that “nobody can reliably say what will happen.” The single biggest uncertainty, he added, is how glaciers move across the materials beneath them. Once glaciers slide beyond a bedrock foundation, tongues in the water melt much faster.

Richard Alley, professor of geosciences at Penn State University, emcees the annual fall  Comer Climate Conference that gathers together scientists pursuing research across the globe. He co-authored Willet’s  paper on her research. (Jack Austin/Medill)

The Thwaites Glacier is the ice shelf of the much larger West Antarctic ice sheet. Thwaites is considered the “Doomsday Glacier” because if it collapsed completely it could raise sea levels by some 10 feet. According to the International Thwaites Glacier Collaboration (ITGC),the massive glacier will face accelerated retreat in the 21st and 22nd centuries, with much of the glacier gone by the 23rd century. Full collapse may take hundreds to a few thousand years according to recent models. 

To study that hidden world two miles below the surface, Willet and her team use highly sensitive seismometers to listen to tiny earthquakes that can indicate cracks or breaks in the ice.

“They listen to the earthquakes and can tell where they are, how big the spot is that breaks, and how much energy it releases,” Alley said. “Those little spots are really important — they inform how glaciers move, and how the ice sheets behave. That’s what will let us build better models for what Antarctica will do.”

Willet said Thwaites’ bed is far more complex than most models suggest, with both hard and soft patches beneath the ice. That mixed environment is difficult to simulate — and potentially dangerous.

“If we have both, that’s the worst-case scenario,” Willet said. “It’s drawing down ice from inland and breaking off at the front — doing everything we wouldn’t want it to be doing. The data show the most likely scenario is this mixed environment. We want to get that information to modelers so they can make more informed decisions.”

Elizabeth Case, a PhD researcher at Columbia University who also studies the Thwaites Glacier, said the glacier may already be undergoing irreversible retreat. The bed beneath it — whether granite, sand, or clay — determines how easily it can slide or flow into the ocean.

Willet shares insights on her upcoming paper, “Seismic Stories From Earth’s Frozen Frontiers: Thwaites Glacier, Antarctica.” Willet hopes her research can help accurately predict sea level rise - a monumentally important question for coastal cities in terms of investment and protecting citizens. (Jack Austin/ MEDILL)
Willet shares insights on her upcoming paper, “Seismic Stories From Earth’s Frozen Frontiers: Thwaites Glacier, Antarctica.” Willet hopes her research can help accurately predict sea level rise – a monumentally important question for coastal cities in terms of investment and protecting citizens. (Jack Austin/ MEDILL)

“What happens at the bed affects crystal structure throughout the ice, influencing how fast Thwaites may disappear,” Case said. “This has serious implications for sea level rise, and the impacts will be felt around the world — directly along coastlines, and indirectly as displacement and migration follow rising seas.”

Willet said that improving the accuracy of those projections is essential. Most glaciologists, she believes, see current sea level predictions as overly optimistic. Alley agreed, emphasizing the urgency and value of the work.

“The costs of getting it wrong are flabbergastingly high,” Alley said. “Supporting Amanda’s research is saving you money. The cost is trivial compared to the value of what comes out.”

Willet presents graphs related to her research on Thwaites Glacier, a massive glacier, larger than her home state of Pennsylvania. The bed of Thwaites is heterogeneous, both soft and hard, Willet concluded. Understanding the bed will inform climate and sea level rise models. (Jack Austin/ MEDILL).

Though she calls herself an environmentalist — even a “tree hugger” — Willet said her motivation goes beyond nature.

“I want to protect this planet that we live on,” she said. “But more importantly, I want to protect people. Sea level rise doesn’t matter if there are no humans on the coast — but there are. We’re the ones who will struggle to live with that reality.”

Photo at top: The Thwaites Glacier, West Antarctica is melting and scientists are researching clues to how fast it could collapse. (NASA)

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