East Antarctica’s largest glacier is melting – fast.
Now new Australian research has confirmed warm water, flowing through a deep channel under the glacier, is a major reason. The research highlights the vulnerability of the East Antarctic ice sheet to ocean heat, one of the biggest unknown factors for global sea-level rise projections.
In 2014-15, researchers aboard Australia’s Antarctic icebreaker, Aurora Australis, gathered the first oceanographic data from the calving front of the Totten Glacier, when a long crack opened up in sea ice that is normally impenetrable to ships.
Lead author, Dr Steve Rintoul, the Interim Director of CSIRO’s Climate Science Centre and ACE CRC Program Leader, said that no oceanographic measurements from the Totten Ice Shelf had been available to test the hypothesis that warm ocean waters were driving melting of the ice shelf from below.
“We knew from satellite data that the Totten has been thinning faster than other glaciers in East Antarctica, but we didn’t know why,” said Dr Rintoul. “A lucky break in the sea ice allowed us to get the ship in there and take the first measurements of the water column and sea floor in this area.”
Dr Rintoul said the team discovered a large channel in front of the western side of the Totten Glacier around 10 kilometres wide and up to a kilometre deep which warm ocean water is reaching the ice shelf through. The temperatures are high enough to drive rapid melt of the underside of the ice shelf.
This is important, Dr Rintoul says, because the ice shelf acts as a sort of plug that restricts the flow of ice from Antarctica to the ocean.
Dr Rintoul said the results also show that, on an area-averaged basis, Totten has the highest basal melt rate among Eastern Antarctic ice shelves larger than 1000 km2.
“If warm ocean waters drive more rapid melt of the Totten and other ice shelves around the edge of Antarctica, more glacial ice can flow into the ocean, raising sea level,” Dr Rintoul said. “The Totten is a big glacier, the largest in East Antarctica, and it contains enough ice to raise global sea levels by about 3.5 metres if it all melted, so it is important to know how it will behave in the future.”
The results of this research comes as scientists attempt a second expedition to the Totten Glacier front, where they hope to profile areas of ocean that were inaccessible in 2014-15 due to sea ice. A team of around 30 scientists, technicians and PhD students from CSIRO, the Antarctic Climate and Ecosystems CRC (ACE CRC), the University of Tasmania, and the Australian Antarctic Division left Hobart on December 8, aiming to arrive at the glacier in late December.
“Now that we know warm water is reaching the underside of the glacier, we want to use this voyage to learn more about the pathways that bring this warm water up from the deep ocean,” said Dr Rintoul.
“Understanding the physical processes delivering heat to the ice shelf will help us assess the vulnerability of the East Antarctic Ice Sheet to future changes in the Southern Ocean.”