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 …

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

We present a highly detailed study of calving dynamics at Tunabreen, a tidewater glacier in
Svalbard. A time-lapse camera was trained on the terminus and programmed to capture …

Glacier flow instabilities can rapidly increase sea level through enhanced ice discharge.
Surge-type glacier accelerations often occur with a decadal to centennial cyclicity …

Geophysical methods have a varying degree of potential for detailed characterization of
landslides and their dynamics. In this study, the application of four well-established seismic …

The flow of glaciers is largely controlled by changes at the ice–bed interface, where basal
slip and sediment deformation drive basal glacier motion. Determining subglacial conditions …

Ice‐penetrating radar observations are critical for projecting ice‐sheet contribution to sea‐
level rise; however, these prognostic models have significant uncertainties due to an …

Locating and monitoring passive seismic sources provides us important information for
studying subsurface rock deformation, injected fluid migration, regional stress conditions as …

Frontal ablation contributes significantly to the mass balance of tidewater glaciers in
Svalbard and can be recovered with high temporal resolution using continuous seismic …

We analyze data from passive and active seismic experiments conducted in the
Adventdalen valley of Svalbard in the Norwegian Arctic. Our objective is to characterize the …