Satellite data from early 2025 revealed extensive melting at Antarctica’s Amery Ice Shelf, highlighting its vulnerability. As a natural barrier against ice flow, its weakening could accelerate sea level rise.

By late 2024, Antarctica experienced significant melting along its coastal regions, even though the melt season was less than halfway through. As 2025 began, meltwater was still visible on the ice sheet’s surface, stretching from the Antarctic Peninsula in the west to ice shelves in the east, including the Amery Ice Shelf in East Antarctica.

Satellite Observations and Glacial Dynamics

On January 1, 2025, the Operational Land Imager (OLI) on NASA’s Landsat 8 satellite captured images of the region. In these images, three major glaciers—the Lambert, Mellor, and Fisher—are seen converging near the edge of the continent. The ice from these glaciers flows outward, extending from the coast onto the ocean’s surface to form the Amery Ice Shelf, which fills Prydz Bay. The shelf’s southern, or interior, side is visible near its grounding line in the middle-right portion of the image above. A broader view of the entire ice shelf is available in this image captured by NASA’s Terra satellite.

The grounding line is the transition zone where a glacier or ice sheet shifts from resting on land to floating as part of an ice shelf. This boundary is not a single line but a gradual area where ice starts to lose contact with the bedrock.

“The Amery is unique among Antarctic ice shelves given its long interior extent—greater than 500 kilometers (300 miles)—and extensive bordering bedrock exposures,” said Christopher Shuman, a glaciologist at the University of Maryland, Baltimore County. “Yet, even in the deep chill of East Antarctica, the change of seasons causes surface melting far inland from the coastal ice front.”

Role of Ice Shelves in Climate Regulation

Ice shelves like the Amery play an important role in holding back, or buttressing, the flow of ice from inland and upstream. Such buttressing can slow the discharge of glacial ice into the ocean, limiting contributions to sea level rise compared to unbuttressed ice areas. Thick, stable ice shelves perform this buttressing role most effectively. But when meltwater drains through fractures within the ice, it can weaken the ice shelf.

Melting on the ice shelf is evident in the detailed image above. The blue puddles are melt ponds—areas where the snow has melted and pooled in low spots on the shelf. Melt ponds commonly form on the Amery during the Antarctic melt season, which occurs each year from November 1 through March 31 with the rising air temperatures of austral summer. Winds can also play a role, removing winter snow and exposing bare, blue ice that is more prone to melting because its dark color absorbs more heat.

Bert Wouters, a researcher at TU Delft, said that he has seen more extensive melt ponding atop the Amery in past seasons. “But on the other hand, it’s still relatively early, so it’s likely that we’ll see more ponding in the coming weeks,” he said.

Melting Trends and Future Projections

The ponding visible here came after a widespread melt event around the Antarctic Ice Sheet’s margins in mid-December 2024, followed by more melting toward the end of the month that culminated in an all-time record melt extent on December 25 and 26, according to the National Snow and Ice Data Center. At that time, satellite-based passive microwave sensors detected melting across more than 3 percent of the ice sheet’s surface.

Ponding on the Amery is generally limited to areas near the shelf’s grounding line, according to Wouters. He noted that closer to the ice shelf’s front (beyond this scene, to the right), ponding is prevented by colder and drier conditions that allow meltwater to refreeze within the snowpack. But research has shown, Wouters said, “that it only takes a few more degrees of warming to make these regions vulnerable to ponding.”