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Chen Zhao, University of Tasmania and Ben Galton-Fenzi, Australian Antarctic DivisionOne of the biggest challenges in predicting Antarctica’s deeply uncertain future is understanding exactly what’s driving its ice loss.
A vast network of lakes and streams lies beneath the thick ice sheet. This water can lubricate the ice, allowing it to slide more rapidly toward the ocean.
Our new research shows “subglacial water” plays a far larger role in Antarctic ice loss than previously thought. If it’s not properly accounted for, future sea-level rise may be vastly underestimated.
Including the effects of evolving subglacial water in ice sheet models can triple the amount of ice flowing to the ocean. This adds more than two metres to global sea levels by 2300, with potentially enormous consequences for coastal communities worldwide.
How hidden lakes threaten Antarctic Ice Sheet stability. (European Space Agency)
Understanding the role of subglacial water
Subglacial water forms when the base of the ice sheet melts. This occurs either due to friction from the movement of the ice, or geothermal heat from the bedrock below.
The presence of subglacial water enables ice to slide over the bedrock more easily. It can also cause further melting under ice shelves, leading to...