New Zealand Scientists Unlock Antarctic Ice Melt Mystery
“Researchers have long suspected that water, from geothermal heat and other sources, flows from under the ice sheets. Satellite observations from elsewhere in West and East Antarctica have revealed active lakes under the ice caps. Our quest was not just to discover the network of hidden lakes and streams that can’t be seen from the surface, but to complete the first close-up observation of these watercourses meeting the ocean in cavities under the ice shelf. These sub-glacial watercourses play a central role in the melting of the ice shelf, so the findings will enable us to predict sea level rise more accurately.”
“The first challenge was just to get there,” says Associate Professor Horgan, who also works in Switzerland for ETH Zurich’s Laboratory of Hydraulics, Hydrology and Glaciology.
“With the help of our camera, we even discovered a school of lobster-like (amphipods) creatures, 400 kilometres from the open ocean.”
“Our first discovery was the unique shape of the under-ice cavity where the meltwater was flowing. The size of the watercourse—about 250 metres deep and 150 metres wide—was larger than expected and mostly filled with ocean water, with only a small portion being freshwater from beneath the ice sheet.”
“Understanding these hidden systems is crucial to improving climate models and predicting sea level rise more accurately. The Ross Ice Shelf and others like it play a critical role in slowing the flow of inland glaciers to the sea. Their decline will significantly accelerate global sea level rise.”
