The record of seismic, hydroacoustic, and infrasonic waves is essential to detect, identify,
and localize sources of both natural and anthropogenic origin. To guarantee traceability and …

Ice doline is a particular kind of ice morphology, usually scattered on ice streams which are
mostly far from the existing research bases. For this reason, glaciologists rarely have …

Seismicity at glaciers, ice sheets, and ice shelves provides observational constraint on a
number of glaciological processes. Detecting and locating this seismicity, specifically …

Both submarine melt and calving are important for the overall mass balance of marine-
terminating glaciers, but uncertainty is rife with regards to the magnitude of the processes …

Measurements of underwater sound are still scarce in the rapidly changing Arctic. Tele-
seismically detectable glacial earthquakes caused by iceberg calving have been known for …

Measurement of the geometry of marine-terminating glaciers is challenging due to the lack
of stable ground areas in close proximity to the glacier. This precludes the use of fixed …

Seismic signals generated by iceberg calving can be used to monitor ice loss at tidewater
glaciers with high temporal resolution and independent of visibility. We combine the …

Accurate estimates of calving fluxes are essential in understanding small-scale glacier
dynamics and quantifying the contribution of marine-terminating glaciers to both eustatic sea …

Narwhal acoustic phonation is embedded in the icy cacophony of one of the noisiest
soundscapes in the ocean. The high susceptibility of the narwhal to climate change …

Calving is a crucial process for the recently observed dynamic mass loss changes of the
Greenland ice sheet. Despite its importance for global sea level change, major limitations in …