Monitoring of Permafrost Ice Wedge Degradation in the Arctic National Parks
Ice wedges are a common feature of permafrost regions that form when cracks in frozen ground are filled by ice. Because they are located near the ground surface and have little covering insulation, they are susceptible to thaw and can be an early warning sign of permafrost loss. Ice wedges are also responsible for much of the unique polygonal patterned ground in the Arctic.