The glacier “has started a phase of self-sustained retreat and will irreversibly continue its decline,” said Gael Durand, a glaciologist with France’s Grenoble Alps University.
Durand and an international team used three different models to forecast the glacier’s future based on the “grounding line,” which is the area under water where the ice shelf—a sea-floating extension of the continent-covering ice sheet—meets land.
This line has receded by about 10 kilometres (six miles) in the past decade.
The grounding line “is probably engaged in an unstable 40-km (25-mile) retreat,” said the study, published in the journal Nature Climate Change.
A massive river of ice, the glacier by itself is responsible for 20 percent of total ice loss from the West Antarctic Ice Sheet today.
On average, it shed 20 billion tonnes of ice annually from 1992-2011, a loss that is likely to increase up to and above 100 billion tonnes each year, said the study.
This is equivalent to 3.5-10 millimetres (0.14-0.4 inches) of global average sea-level rise over the next 20 years.
Read more at: Phys.org