Antarctic ice loss forecasts give decades to plan for rising seas

A new study indicates that reliable predictions of Antarctic ice loss are possible until around the middle of this century. This window could allow governments time to prepare for sea level rise before uncertainty grows sharply later in the century.

The research, published in Nature and led by Dr. Felicity McCormack of Monash University and Securing Antarctica's Environmental Future, found that ice sheet models can reliably project Antarctica's contribution to sea level rise over the next 30 to 50 years if they match current observations.

"If ice sheet models accurately reproduce the rates of ice loss we observe today, we can have confidence in using those same models to reliably predict Antarctica's contribution to sea level rise over the next 30 to 50 years," Dr. McCormack said.

The study notes that predictability declines after mid-century as processes like rapid ice retreat from below-sea-level bedrock become more likely. Professor Steven Chown, director of SAEF, said the findings provide a defined period for stronger monitoring and adaptation planning, particularly for Pacific Island nations.

The Intergovernmental Panel on Climate Change has estimated that Antarctic ice loss could almost double the rate of sea level rise over the next 30 years in a worst-case scenario, placing one quarter of Australian homes at flood risk under high-emission paths.

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New simulations show a 10 to 23 percent chance that the Atlantic Meridional Overturning Circulation has already reached a point of no return.

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A new study shows that channels beneath Antarctic ice shelves can trap warm ocean water and accelerate melting from below. Researchers focused on the Fimbulisen Ice Shelf in East Antarctica and found that this process may make even cold regions more vulnerable. The findings suggest current climate models could underestimate future sea level rise.

Researchers have mapped a massive fan-shaped network of basins beneath the East Antarctic Ice Sheet, linking several previously studied features into one large geological structure. The discovery, published in a 2026 study, offers new insights into the continent's tectonic past and its influence on current ice movement.

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