While there are numerous hypotheses concerning glacial–interglacial environmental and
climatic regime shifts in the Arctic Ocean, a holistic view on the Northern Hemisphere's late …

A comprehensive inventory of High Arctic cross-shelf troughs is compiled from International
Bathymetric Chart of the Arctic Ocean (IBCAO) bathymetric data (v. 3.0). The location of 75 …

Our understanding of processes relating to the retreat of marine‐based ice sheets, such as
the West Antarctic Ice Sheet and tidewater‐terminating glaciers in Greenland today, is still …

Glacial erosion and sediment production are of interest to diverse scientific communities
concerned with the interaction of climatic, tectonic and surface processes that influence the …

Projections of ice sheet behavior hinge on how ice flow velocity evolves and the extent to
which marine-based grounding lines are stable. Ice flow and grounding line retreat are …

The deglaciation history and Holocene environmental evolution of northern Wijdefjorden,
Svalbard, are reconstructed using sediment cores and acoustic data (multibeam swath …

Contemporary climate change has resulted in great uncertainty in how glaciers and ice
sheets around the Earth might evolve. It has long been appreciated that the contemporary …

Abstract During the Last Glacial Maximum (LGM) the marine-terminating Barra Fan Ice
Stream (BFIS), a major conduit of the British Irish Ice Sheet (BIIS), drained much of western …

Abstract Glaciation during the Late Paleozoic Ice Age climatic interval (~ 370–260 Ma) was
likely dynamic; consisting of numerous ice centers that grew and shrank asynchronously …

Wahlenbergfjorden is a fjord situated in the western part of Nordaustlandet in northern
Svalbard. It leads into the 400 m deep Hinlopen Strait located between Nordaustlandet and …