Data from GPS stations fixed on bedrock are offering an unprecedented look at the uplift process beneath Greenland.
Beata Csatho, a geologist at the University at Buffalo, says the new results suggest earlier studies may have underestimated ice loss—past and present.
“This research is a great first step toward better understanding how geologic processes below the surface of the Earth influence ice loss and, ultimately, sea level rise,” she says. “It opens up new opportunities for better understanding how the ice sheet is changing and interacting with the rocky layers of the Earth below it.”
Greenland’s ice sheet sits on the Earth’s solid crust, which is in turn perched atop a softer layer of rock called the mantle. When the ice sheet loses ice, the crust underneath rises up (similar to the way in which a compressed spring will bounce up when pressure is removed).
This uplift, called postglacial rebound, means that scientists can’t measure how much an ice sheet is shrinking by simply tracking changes in its surface elevation. They must also figure out how much of that elevation change is caused by the bedrock rising.
The paper also hints that the mantle beneath Greenland is not uniform: The ice sheet’s southeast region has experienced unexpectedly rapid uplift rates of about 12 millimeters per year, suggesting that the mantle may be hotter and less viscous here, making it springier.
“It’s a very exciting study,” Csatho says. “It’s a new and different way of understanding the ice sheet and this critical process of uplift.”
Shfaqat A. Khan of the National Space Institute at the Technical University of Denmark (DTU Space) led the study, which appears in Science Advances.
Source: University at Buffalo
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