Present understanding of Greenland's subglacial geology is derived mostly from
interpolation of geologic mapping of its ice‐free margins and unconstrained by geophysical …

Abstract The Greenland Ice Sheet covers an area of 1.7 million km 2, equivalent to∼ 79% of
the surface of Kalaallit Nunaat (Greenland) and∼ 1.2% of the Earth's land surface. The …

The Greenland Ice Sheet is a key contributor to contemporary global sea level rise, but its
long-term history and response to episodes of warming in Earth's geological past remain …

In 2018 the first subglacial lake in the Canadian Arctic was proposed to exist beneath the
Devon Ice Cap, based on the analysis of airborne radar data. Here, we report a new …

In the past two decades, mass loss from the Greenland ice sheet has accelerated, partly due
to the speedup of glaciers. However, uncertainty in speed derived from satellite products …

Hydrologically active subglacial lakes can drain large volumes of water and sediment along
subglacial pathways, affecting the motion and mass balance of ice masses, and impacting …

Subglacial hydrology can exert an important control on ice flow by affecting friction at the ice‐
bedrock interface. Here, we report on a series of subglacial drainage events along the …

Here, we present a compilation of 85 ice temperature profiles from 79 boreholes from the
Greenland Ice Sheet and peripheral ice caps, as well as local ice caps in the Canadian …

Direct observations of the size of the Greenland Ice Sheet during Quaternary interglaciations
are sparse yet valuable for testing numerical models of ice-sheet history and sea level …

There is currently poor scientific agreement whether the ice-bed interface is frozen or
thawed beneath approximately one-third of the Greenland ice sheet. This disagreement in …