Lakes collapse during winter in Greenland

A team of international researchers has shown for the first time how 18 meltwater lakes in Greenland collapse during winter, causing the edges of the ice to flow faster. This new knowledge is essential for understanding how climate change influences the flow of ice masses in the Arctic. 

Ice movement and sea level rise

New research from the Geological Survey of Denmark and Greenland and University of Copenhagen shows that meltwater in tunnels beneath Greenland’s ice sheet causes it to change speed, and in some places, accelerate greatly towards the ocean. This can cause an increase in melting, especially in a warming climate.

Greenland ice streams

Scientists now know that major ice streams can shut down, shifting rapid ice transport to other parts of the ice sheet, within a few thousand years. This was found in reconstructions of two ice streams, based on ice-penetrating radar scans of the Greenland ice sheet by a team led by the Alfred Wegener Institute. 

Melt ponds in West Greenland

During spring and summer, as the air warms up and the sun shines down on the Greenland Ice Sheet, melt ponds form. Melt ponds are extensive pools of open water that form on both sea ice and ice sheets and are visible from space.