The mountain cryosphere of mainland Europe is recognized to have important impacts on a
range of environmental processes. In this paper, we provide an overview on the current …

Radar sounding is a powerful geophysical approach for characterizing the subsurface
conditions of terrestrial and planetary ice masses at local to global scales. As a result, a wide …

The Antarctic ice sheet has been losing mass over past decades through the accelerated
flow of its glaciers, conditioned by ocean temperature and bed topography. Glaciers …

Abstract Knowledge of the ice thickness distribution of the world's glaciers is a fundamental
prerequisite for a range of studies. Projections of future glacier change, estimates of the …

Greenland's bed topography is a primary control on ice flow, grounding line migration,
calving dynamics, and subglacial drainage. Moreover, fjord bathymetry regulates the …

The melting of glaciers and ice caps accounts for about one-third of current sea-level rise,–,
exceeding the mass loss from the more voluminous Greenland or Antarctic Ice Sheets,. The …

Ice discharge from large ice sheets plays a direct role in determining rates of sea-level rise.
We map present-day Antarctic-wide surface velocities using Landsat 7 and 8 imagery …

We present Bedmap2, a new suite of gridded products describing surface elevation, ice-
thickness and the seafloor and subglacial bed elevation of the Antarctic south of 60° S. We …

We measure the grounding line retreat of glaciers draining the Amundsen Sea sector of
West Antarctica using Earth Remote Sensing (ERS‐1/2) satellite radar interferometry from …

Surface ice velocity is a fundamental characteristic of glaciers and ice sheets that quantifies
the transport of ice. Changes in ice dynamics have a major impact on ice sheet mass …