Antarctica’s Ancient Climate Tipping Point: Why 240 ppm CO₂ Changed Everything

An international team of climate scientists has peered 3 million years into Antarctica's past and uncovered a critical threshold that transformed the continent's ice sheet from a relatively stable feature into a hair-trigger system. The research, published in Nature Geoscience on May 28, 2026, by the IBS Center for Climate Physics (ICCP) at Pusan National University, found that when atmospheric carbon dioxide dropped below about 240 parts per million, the Antarctic ice sheet entered a "new dynamical regime" — a state where small changes in climate produced disproportionately large ice-sheet responses .

To build this picture, the team fed a high-resolution paleoclimate simulation — which reconstructed global temperature and rainfall patterns over the last 3 million years — into the Penn State University ice-sheet–ice-shelf model. This model simulates ice flow, thickness, temperature, and floating ice-shelf dynamics. The entire coupled system was run on one of South Korea's fastest supercomputers, producing a physically consistent, spatially continuous record of global ice-sheet evolution .

Before the shift: a moderately responsive system

Prior to the Mid-Pleistocene Transition — a major reorganization of Earth's ice age cycles that occurred approximately 1.2 million to 800,000 years ago — the Antarctic ice sheet reacted relatively modestly to climate changes. Glacial-interglacial cycles followed a 40,000-year rhythm, and the ice sheet grew and retreated in a comparatively linear fashion .

The Mid-Pleistocene Transition changed that rhythm, shifting the planet into a 100,000-year cycle with thicker, more persistent ice sheets. The ICCP study reveals that this transition was not just a timing change; it marked a fundamental shift in how sensitively the ice sheet responded to external forcings.

Crossing the ~240 ppm threshold into a new dynamical regime

After the Mid-Pleistocene Transition, the simulation reveals a starkly nonlinear behavior. Once CO₂ levels fell below approximately 240 ppm, the amplitude of Antarctic ice variations suddenly increased. The ice sheet began reacting much more strongly to changes in atmospheric and ocean temperatures, entering what the researchers call a "new dynamical regime" .

Lead author Dr. Kyung-Sook Yun explained the significance: "After this transition, the Antarctic ice sheet reacts much more strongly to changes in climate forcing. This indicates that the system does not evolve gradually but instead becomes more responsive after crossing a particular threshold" .

The accelerated ice growth observed in the model after the threshold was crossed was driven by three interacting physical mechanisms :

• Colder glacial ocean temperatures reduced melting at the base of the ice sheet, particularly below sea level.
• Lower global sea levels (roughly 50–100 meters below present) reduced pressure on the bedrock beneath ice shelves, triggering slow crustal uplift that further promoted ice thickening along the coasts.
• Together, these feedback loops established larger, more persistent Antarctic ice sheets during later glacial periods.

An ancient warning for a world above 400 ppm

The study's most urgent implication lies in reverse. Today's atmospheric CO₂ concentration sits at roughly 425 ppm — far above the 240 ppm threshold that pushed the ice sheet into its hyper-reactive state . The research demonstrates that ice sheets do not respond linearly to climate forcing; they can undergo sharp, nonlinear shifts into entirely different sensitivity regimes.

Co-author Prof. Axel Timmermann, Director of the ICCP, stated that the findings "suggest that the Antarctic ice sheet was more sensitive to external forcings than previously assumed" and that the study "raises important questions about its future response to global warming" .

If the past is any guide, the ice sheet's newfound sensitivity in the colder direction implies it could respond with similar abruptness in the opposite direction as temperatures rise. Small additional increments of warming or ocean heating could trigger disproportionately large ice loss, potentially accelerating sea-level rise well beyond the steady, gradual projections that inform many current coastal planning efforts .

The results underscore that accurate sea-level rise projections — and the infrastructure and adaptation decisions that depend on them — must account for these threshold-crossing, nonlinear behaviors that paleoclimate records now plainly reveal.