Since 1979, humanity has watched in slow motion as 12.5 trillion tons of ice have disappeared from the poles — a loss so vast it could bury the United States under five feet of frozen water, yet so gradual it has raised the sea by only an inch. That inch, however, is not a reassurance; it is a threshold, and for millions of people living along the world's coastlines, the difference between a manageable tide and a catastrophic one is measured in centimeters. The science now understands the mechanism clearly — warming oceans hollowing ice from below, glaciers weakening like corks in bottles — an
12.5 Trillion Tons of Glacier Ice Lost Since 1979, Accelerating Sea Level Rise
Warm water is eating away at ice from below, not air melting it from above.
So we're talking about 12.5 trillion tons of ice. That's the number that keeps getting repeated. But you said it only raises sea level by an inch. How does that math work?
It's actually the geometry of it. Ice sheets are enormous, but when they melt and spread across the entire ocean surface—which covers most of the planet—that volume gets distributed. An inch sounds small until you realize what it means for people living at sea level.
But I want to be careful here. The study itself measures ice loss. The one-inch figure—that's coming from Borenstein's interpretation, right? Is that a direct finding from the paper or a calculation he's doing?
It's a calculation based on the ice loss data, but it's a standard conversion. The point is the disconnect between the number and the impact.
You mentioned that most of the melting isn't from warm air but from warm water underneath. That seems like it should change how we think about solutions.
Exactly. You can't just cool the air. The ocean is warming, and it's circulating beneath these ice sheets. It's a much harder problem to solve.
Though I should note—the study goes back to 1979, but the researchers only have detailed data through 2023. The 2024 and 2025 observations that Borenstein mentions? Those are preliminary. They're not part of the formal study yet.
What about this Thwaites Glacier everyone keeps calling the Doomsday Glacier? Is that actually a tipping point we're approaching?
It's a real concern. If it collapses, it could trigger a cascade of ice loss behind it. But the honest answer is we don't know when or if that happens.
And that's important to say clearly. Scientists don't know if we've passed the tipping point already or if we're approaching it. That uncertainty is real.
So what does the next fifty years look like?
It depends entirely on whether warming continues. If it does, we keep losing ice. If it stops, loss slows or stops. But the UN just said we're heading past 1.5 degrees Celsius, so the trajectory isn't encouraging.
El Pulso
- The melting has sharply accelerated over the past two decades, driven not by warming air but by warming ocean water silently eroding ice sheets from beneath and within.
- A brief slowdown between 2020 and 2023, caused by unusual snowfall, offered false comfort — by 2024 and 2025, the underlying acceleration had fully resumed.
- Every centimeter of sea level rise puts two to three million additional people at risk of flooding, turning what sounds like a trivial inch of water into a civilizational pressure point for coastal populations worldwide.
- Antarctica's Thwaites Glacier — the so-called Doomsday Glacier — functions as a structural cork holding back enormous reserves of ice, and scientists cannot rule out that its tipping point has already been crossed.
- The path to slowing the loss runs directly through halting warming, yet the United Nations reported in September 2026 that the world remains on course to breach the 1.5°C Paris Agreement threshold.
Since 1979, humanity has watched in slow motion as 12.5 trillion tons of ice have disappeared from the poles — a loss so vast it could bury the United States under five feet of frozen water, yet so gradual it has raised the sea by only an inch. That inch, however, is not a reassurance; it is a threshold, and for millions of people living along the world's coastlines, the difference between a manageable tide and a catastrophic one is measured in centimeters. The science now understands the mechanism clearly — warming oceans hollowing ice from below, glaciers weakening like corks in bottles — and what remains is the older, harder question of whether knowledge will move the will to act.
A study published this month in Scientific Data has put a number to one of the defining slow-motion crises of our era: since 1979, approximately 12.5 trillion tons of ice have vanished from Greenland and Antarctica. To make that volume tangible, it is enough ice to cover the entire continental United States under five feet of solid ice. Drawing on satellite data from NASA and the European Space Agency and synthesizing the work of dozens of researchers, the study reveals not just the scale of the loss but its direction — the melting has accelerated sharply, especially over the past two decades.
The mechanism behind the loss surprises many. Only about 16 percent of the ice disappears through surface melting caused by warm air. The overwhelming majority is being eaten away from below and along the sides by warming ocean water, which circulates beneath the ice sheets and hollows them out from within — relentless, invisible, and largely beyond the reach of what we can see from above.
The result so far is approximately one inch — three centimeters — of global sea level rise. That number sounds small, but coastal science reframes it quickly: for every centimeter of rise, between two and three million people face increased flooding. Storm surges ride higher, king tides push further inland, and events once considered rare become routine. Hurricane Sandy's devastation of New York in 2012 was amplified by sea level rise that was, by current standards, negligible — yet it caused tens of billions in damage.
A temporary slowdown in ice loss between 2020 and 2023, driven by unusual snowfall accumulation, briefly interrupted the trend. Even Jakobshavn, the world's fastest-shrinking glacier, losing up to 165 feet of ice per day, decelerated during this period. But monitoring through 2024 and 2025 confirmed the reprieve was short-lived. The acceleration has resumed.
The deepest concern among scientists centers on irreversible tipping points. East Antarctica has actually been gaining mass through snowfall, but West Antarctica and the Antarctic Peninsula are losing ice rapidly. At the heart of West Antarctica sits the Thwaites Glacier — sometimes called the Doomsday Glacier — which acts as a structural barrier holding back vast reserves of ice behind it. As warming water weakens it, the risk grows that its eventual failure could trigger an unstoppable cascade. Scientists cannot say with certainty when that threshold might arrive, or whether it has already been crossed.
The trajectory from here depends on whether warming continues. The United Nations reported in early September 2026 that the world is on course to exceed the 1.5 degrees Celsius limit nations pledged to respect under the Paris Agreement. Thirty years ago, glacier melt wasn't even included in sea level rise projections. The science has caught up. The question now is whether the response will.
A study published this month in Scientific Data has quantified something almost impossible to visualize: since 1979, roughly 12.5 trillion tons of ice have vanished from the glaciers and ice sheets of Greenland and Antarctica. To make that number concrete, imagine covering the continental United States in five feet of solid ice—that's the volume we're talking about. The research, which synthesized work from dozens of scientists using satellite data from NASA and the European Space Agency, reveals not just the scale of the loss but its trajectory. The melting has accelerated sharply, particularly over the past two decades, marking a departure from the slower decline observed in the 1990s and early 2000s.
What makes this acceleration especially troubling is where the ice is actually going. Most people assume that warming air melts glaciers from above, but the data tells a different story. Only about 16 percent of the ice loss comes from surface melting. The rest—the vast majority—is being eaten away from below and along the sides by warming ocean water. The mechanism is straightforward and relentless: warmer water circulates beneath and around the ice sheets, hollowing them out from within. It's as if someone poured hot coffee into a cup of ice. Within minutes, the ice is gone, not because the air warmed up, but because liquid heat did the work.
Yet here is where the numbers become almost deceptive in their smallness. Those 12.5 trillion tons of melted ice have raised global sea levels by approximately one inch—three centimeters. To the ear, that sounds negligible. An inch of water, what's the harm? But the science of coastal vulnerability tells a different story. For every centimeter of global sea level rise, between two and three million people face increased flooding. The reason is simple: roughly half the world's population lives near coastlines. When sea level rises, even modestly, it doesn't rise uniformly. Storm surge rides higher. King tides push further inland. The baseline shifts upward, and what were once rare inundations become routine. Hurricane Sandy, which devastated New York in 2012, was amplified by sea level rise that was globally minuscule by the standards we're discussing now—yet it caused tens of billions of dollars in damage.
The study also captured an interesting anomaly. From 2020 to 2023, the rate of ice loss actually slowed. Increased snowfall in both Greenland and Antarctica temporarily offset some of the melting. But researchers who continued monitoring the data into 2024 and 2025 found the slowdown was temporary—a blip of natural variation. The underlying trend has resumed. The acceleration continues.
What concerns scientists most is the possibility of irreversible tipping points. In Antarctica, the story is geographically split. East Antarctica, the larger and colder portion, has actually been growing as more snow accumulates. West Antarctica and the Antarctic Peninsula tell the opposite story: rapid, accelerating ice loss. Within West Antarctica sits the Thwaites Glacier, sometimes called the Doomsday Glacier, a name that captures both the drama and the genuine concern. The glacier functions as a cork in a bottle, holding back a vast reservoir of ice behind it. As warming water eats away at Thwaites, the cork weakens. If it fails entirely, the glaciers behind it will begin flowing seaward in a cascade that may be impossible to reverse. Scientists don't know when—or if—that point will arrive. There's a distinct possibility we've already passed it without realizing.
In Greenland, the Jakobshavn Glacier holds the grim distinction of being the world's fastest-shrinking glacier. It loses up to 165 feet of ice per day—roughly eight feet per hour. During the 2020-2023 slowdown, even this glacier decelerated. But the trend has reversed again.
The path forward depends almost entirely on whether warming stops or continues. If global temperatures stabilize, ice loss will likely slow or cease in many cases. But that's a conditional statement, and the conditions are not being met. The United Nations reported in early September 2026 that global warming is on track to exceed the 1.5 degrees Celsius threshold that nations committed to avoiding under the Paris Agreement in 2015. As long as air and water continue warming, the ice will continue melting. Scientists now understand this mechanism far better than they did thirty years ago, when glacier melt wasn't even factored into sea level rise projections. The surprise is gone. What remains is the question of whether understanding will lead to action.
Citas Notables
As long as the air and the water keep warming, scientists figure the ice will keep melting. If warming stops or slows down and then stops, the theory is that in many cases, unfortunately, not all, the ice sheet loss will either slow or stop.— Seth Borenstein, science writer, Associated Press
For every third of an inch of sea level rise globally, we see two to three million people flooded, because so many people in the world live by the coast.— Seth Borenstein, science writer, Associated Press