As climate warms, Arctic rivers carry higher flows and flood earlier in the spring, causing underlying permafrost to thaw rapidly.
Seismic signals detected hundreds of kilometers away from Greenland glaciers reveal the calving style and iceberg size.
Geophysicists have discovered a way to monitor permafrost thaw by measuring seismic waves so gentle they don’t shake a thing.
An increase in activity of hundreds of slow-moving landslides during extreme wet conditions in California provides insights into the landscape response to ongoing climate change.
High-resolution mapping efforts could improve predictions of coastal changes as glaciers shrink around the world.
New radio sounding study finds little evidence of lakes under Antarctica’s Recovery Glacier.
The GeoClaw model is used to simulate a landslide-dam outburst flood through rugged Himalayan topography.
A rare submarine landslide provides researchers with a reference point for modeling the biggest tsunamis.
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.
Grain size and sediment delivery pathways from the Ganges delta have been used to model downstream facies changes.