Calving, or the release of icebergs from glaciers and floating ice shelves, is an important
process transferring mass into the world's oceans. Calving glaciers and ice sheets make a …

Fine resolution topographic data derived from methods such as Structure from Motion (SfM)
and Multi-View Stereo (MVS) have the potential to provide detailed observations of …

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 …

Quantifying the impact of submarine melting on calving is central to understanding the
response of marine‐terminating glaciers to ocean forcing. Modeling and observational …

Concurrent with atmospheric warming glaciers around the world are rapidly retreating,
thinning, and losing mass. While total volume compared with the ice sheets in Greenland …

Atlantic Water is a major contributor to the largest zonal variability in ocean properties and
air-sea-ice interaction in the Nordic Seas and the European Arctic. Climate change has …

Glacier change studies in the Antarctic Peninsula region, despite their importance for global
sea level rise, are commonly restricted to the investigation of frontal position changes. Here …

The increasingly negative mass balance of the Greenland ice sheet (GrIS) over the last~ 25
years has been associated with enhanced surface melt and increased ice loss from marine …

Metals and metalloids in snow on glaciers, depending on the season of deposition, may
come from various sources: local rock dust (erosion of the geological substratum), marine …

Progressing warming in the Arctic and increased extreme weather events can significantly
influence the hydrography of Svalbard fjords, leading to changes towards more Atlantic-type …