The last decade witnessed an explosion in yearly number of publications on passive glacier
seismology. The seismic signals from a wide range of glacier‐related processes fill a broad …

The aims of this review are to:(a) describe and interpret structures in valley glaciers in
relation to strain history; and (b) to explore how these structures inform our understanding of …

Glacial debris flows are a common catastrophic hazard in alpine regions due to glacier
recession and permafrost thawing. They are frequently triggered by heavy rainfall and …

Mass loss from the Greenland ice sheet (GrIS) has increased over the last two decades in
response to changes in global climate, motivating the scientific community to question how …

Rock glaciers—ice-rich creeping landforms typical of permafrost mountain ranges—can
develop an anomalous landslide-like behaviour called destabilisation. This behaviour is …

Mountain glaciers integrate climate processes to provide an unmatched signal of regional
climate forcing. However, extracting the climate signal via intercomparison of regional …

The largest uncertainty in future sea-level rise is loss of ice from the Greenland and Antarctic
Ice Sheets. Ice shelves, freely floating platforms of ice that fringe the ice sheets, play a …

Seismic source and wave propagation studies contribute to understanding structure,
transport, fracture mechanics, mass balance, and other processes within glaciers and …

Reconstruction of glacial topography is important for assessing the ice dynamics of glaciers
in the past and understanding how they may respond to climate change in the future. As an …

Albedo—a primary control on surface melt—varies considerably across the Greenland Ice
Sheet yet the specific surface types that comprise its dark zone remain unquantified. Here …