This "geothermal heat flux" is key data required by scientists in order to model how the White Continent is going to react to climate change. If the rock bed's temperature is raised, it makes it easier for the ice above to move. And if global warming is already forcing change on the ice sheet, a higher flux could accelerate matters. "The heat coming from the Earth’s interior is important to understand the overall conditions that control the dynamics at the base of the ice sheet and hence the ice flow,”
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