Detailed measurements of the geometry and flow of Laurichard rock glacier over 67 years reveal the distinctive behavior of these landforms through periods of warming and cooling.
Seismic signals detected hundreds of kilometers away from Greenland glaciers reveal the calving style and iceberg size.
The model was previously used to describe the behavior of ferromagnets in the presence of external magnetic fields.
Firn aquifers—pockets of meltwater beneath the surface of an ice sheet—could have far-reaching impacts on subglacial hydrology, a new study finds.
Airborne radar from the Recovery Glacier system demonstrates the importance of characterizing the underlying causes of ice flow speedup to understand how glacial discharge could change in the future.
Accurately modeling melt rates in specific ice shelf locations is critical for forecasting how Antarctica’s ice sheet will respond to climate change.
New observations of surface ice velocity over northern Greenland challenge current assumptions used in ice sheet models to model the deformation mechanisms that govern ice flow.
The maps focus on surface ice velocity, showing how Antarctica’s frozen surface changed over a 7-year period.
A novel method uses shifting bedrock to trace pulses of mass that propagate down a glacier.
An uninterrupted 24-year altimetry record of Amundsen Sea Embayment glaciers indicates the initiation and pace of thinning have been inconsistent across the region.