(Inside Science) — Most of the worry over melting ice in Antarctica has focused on the rapidly melting western shore, where there is enough ice to raise worldwide sea levels by up to 4.3 feet. But new research suggests that the massive Ross Ice Shelf, which has long been considered stable, might be at risk as well — potentially leading to a slower sea level rise of up to 38 feet as glaciers that were once held back by the shelf slide more quickly into the ocean. The researchers suspect that other crucial ice shelves could also be at risk.
“My primary concerns would be that the potential for melting and collapse of the big ice shelves is not being taken seriously enough,” said Laurie Padman, a physical oceanographer based in Corvallis, Oregon who works at a Seattle-based nonprofit called Earth and Space Research. “They’re being treated as less important because they are not presently showing much signs of change. But on a 100-year timescale, they have the potential for large changes.”