Nearly every glacier in Greenland has thinned or retreated over the past few decades,,–,
leading to glacier acceleration, increased rates of sea-level rise and climate impacts around …

Ice sheet marine margins via outlet glaciers are susceptible to climate change and are
expected to respond through retreat, steepening, and acceleration, although with significant …

Aim Identify hotspots and areas of high species richness for Arctic marine mammals.
Location Circumpolar Arctic. Methods A total of 2115 biologging devices were deployed on …

Accurate projections of the mass loss from the Greenland Ice Sheet (GrIS) require a
complete understanding of the ice‐dynamic response to climate forcings on seasonal and …

Many marine-terminating outlet glaciers have retreated rapidly in recent decades, but these
changes have not been formally attributed to anthropogenic climate change. A key …

Abstract Frontal ablation has caused 32%–66% of Greenland Ice Sheet mass loss since
1972, and despite its importance in driving terminus change, ocean thermal forcing remains …

Greenland's glaciers have been retreating, thinning and accelerating since the mid-1990s,
with the mass loss from the Greenland Ice Sheet (GrIS) now being the largest contributor to …

Frontal ablation has caused 32–66% of Greenland Ice Sheet mass loss since 1972, and
despite its importance in driving terminus change, ocean thermal forcing remains crudely …

The mass balance of the Greenland ice sheet is strongly influenced by the dynamics of its
outlet glaciers. Therefore, it is of paramount importance to accurately and continuously …

The frontal position of an ice shelf is an important parameter for ice dynamic modelling, the
computation of mass fluxes, mapping glacier area change, calculating iceberg production …