Subglacial lakes are repositories of ancient climate conditions, provide habitats for life and
modulate ice flow, basal hydrology, biogeochemical fluxes and geomorphic activity. In this …

Ice‐contact proglacial lakes are generally absent from numerical model simulations of
glacier evolution, and their effects on ice dynamics and on rates of deglaciation remain …

Global climate change gives rise to changing spatial patterns of snow and ice, especially
over mountain blocks where orographic and synoptic circulation effects play significant roles …

Ice marginal lakes are a dynamic component of terrestrial meltwater storage at the margin of
the Greenland Ice Sheet. Despite their significance to the sea level budget, local flood …

Global climate change is evidently manifest in disappearing mountain glaciers and receding
and thinning ice sheet margins. Concern about contemporaneous proglacial lake …

Ice‐marginal lakes can affect glacier dynamics but are ignored in studies of the evolution of
the Greenland ice sheet (GrIS) and of peripheral mountain glaciers and ice caps (PGICs) …

We present the first fully coupled 3D full-Stokes model of a tidewater glacier, incorporating
ice flow, subglacial hydrology, plume-induced frontal melting and calving. We apply the …

Glacier calving fronts are highly dynamic environments that are becoming ubiquitous as
glaciers recede and, in many cases, develop proglacial lakes. Monitoring of calving fronts is …

Proglacial lakes, whose numbers have been growing around the world, may drive
accelerated glacier retreat and provide valuable records of past glacier and climatic …

There has been a progressive increase in the number and area of ice-marginal lakes
situated along the south-western margin of the Greenland Ice Sheet (GrIS) since the 1980s …