

The finding comes from a study of prehistoric sea-deposits found on the shores surrounding the “doomsday” Thwaites Glacier and the neighboring Pine Island Glacier, both located on the West Antarctic Ice Sheet.  The chilling news?  Antarctica’s glacial melt, driven by climate change, is advancing faster than ever before in recorded history, researchers have reported June 9 in the journal Nature Geoscience(opens in new tab).

“These currently elevated rates of ice melting may signal that those vital arteries from the heart of the West Antarctic Ice Sheet have been ruptured, leading to accelerating flow into the ocean that is potentially disastrous for future global sea level in a warming world,” co-author Dylan Rood, an Earth scientist at Imperial College London, said in a statement.

“Is it too late to stop the bleeding?” Rood asked.

As one of Antarctica’s fastest-melting glaciers, Thwaites has earned the nickname”Doomsday Glacier.” Since the 1980s, Thwaites has lost an estimated 595 billion tons (540 billion metric tons) of ice, contributing to a 4% rise in global sea levels. Thwaites and its northern neighbor, the Pine Island Glacier, cover enormous expanses; Thwaites has a surface area of about 74,130 square miles (192,000 square kilometers) (making it nearly as big as Great Britain) and Pine Island 62,660 square miles (162,300 square km).



The researchers estimated the ages of the shorelines by collecting ancient shells and tiny fragments of penguin bones, before analyzing the ancient biomatter with radiocarbon dating. This method identifies the age of organic material by measuring the amount of carbon-14, a radioactive carbon isotope, or variant with a different number of neutrons, which is found everywhere on Earth and is easily absorbed by plants and animals. When animals die, they stop accumulating carbon-14 in their tissues and the amount that they’ve already absorbed begins to decay. The half-life of carbon-14 (or the time it takes for half of it to decay) is 5,730 years, and scientists can pinpoint the ages of animals that died thousands of years ago by measuring quantities of undecayed carbon-14 in the remains.

After dating penguin bones and shells from more than 20 different shorelines, the scientists found that the oldest and highest beach began to form roughly 5,500 years ago. From that moment in time until about 30 years ago, ice loss exposed the shorelines at a rate of about 0.14 inches (3.5 millimeters) each year, the researchers reported. But over the past three decades, the rate of shoreline advance has skyrocketed — up to 1.6 inches (40 mm) per year.

 “Although these vulnerable glaciers were relatively stable during the past few millennia, their current rate of retreat is accelerating and already raising global sea levels,” Rood said.
