Models of glacial flow and retreat rely on estimates of glacial ice viscosity, the measure of the ice's resistance to flow.
Melt water flowing through ice sheets via crevasses, fractures and large drains called moulins can carry warmth into ice sheet interiors, greatly accelerating the thermal response of an ice sheet to ...
Just as explorers once searched the vast reaches of Africa’s Nile River for clues to its behavior and ultimate source, modern-day scientists are searching Antarctica for its hidden lakes and waterways ...
Lakes collecting along the retreating edge of the Greenland ice sheet are not passive meltwater pools. New research shows ...
Melt water flowing through ice sheets via crevasses, fractures and large drains called moulins can carry warmth into ice sheet interiors, greatly accelerating the thermal response of an ice sheet to ...