Understanding grounding line dynamics is critical for projecting glacier evolution and sea
level rise. Observations from satellite radar interferometry reveal rapid grounding line …

Warming of the ocean waters surrounding Greenland plays a major role in driving glacier
retreat and the contribution of glaciers to sea level rise. The melt rate at the junction of the …

Satellite radar interferometry data reveals that the grounding line of Petermann Glacier,
Greenland migrates by several kilometers during the tidal cycle, bringing pressurized …

In order to accurately predict the reaction of ice sheets to climate change and their
contribution to sea level, we must understand ice sheet dynamics and incorporate these …

The Petermann ice shelf is one of the largest in Greenland, buttressing 4% of the total ice
sheet discharge, and is considered dynamically stable. In this study, we use differential …

The Petermann ice shelf is one of the largest in Greenland, buttressing 4% of the total ice
sheet discharge, and is considered dynamically stable. In this study, we use differential …

Ice melt processes that take place at the ice–ocean boundary of Greenland and Antarctic
glaciers play a pivotal role in their evolution and contribution to sea-level rise, but …

Ice velocity variations near the terminus of Jakobshavn Isbræ, Greenland, were observed
with a terrestrial radar interferometer (TRI) during three summer campaigns in 2012, 2015 …

Jakobshavn Isbræ, a major outlet glacier in Greenland, lost its protective ice shelf in 2002
and has been speeding up and retreating since. We image its grounding line for the first time …

The effect of the North Atlantic Ocean on the Greenland Ice Sheet through submarine
melting of Greenland's tidewater glacier calving fronts is thought to be a key driver of …