Subglacial hydrology is a leading control on basal friction and the dynamics of glaciers and
ice sheets. At low discharge, subglacial water flows through high-pressure, sheet-like …

The international endeavour to retrieve a continuous ice core, which spans the middle
Pleistocene climate transition ca. 1.2–0.9 Myr ago, encompasses a multitude of field and …

The area near Dome C, East Antarctica, is thought to be one of the most promising targets
for recovering a continuous ice-core record spanning more than a million years. The …

Subglacial lakes are unique environments that, despite the extreme dark and cold
conditions, have been shown to host microbial life. Many subglacial lakes have been …

The European Beyond EPICA project aims to extract a continuous ice core of up to 1.5 Ma,
with a maximum age density of 20 kyr m− 1 at Little Dome C (LDC). We present a 1D …

Abstract Aurora Subglacial Basin (ASB), which feeds Totten Glacier, is a marine basin lying
below sea level and contains up to 3.5 m of global sea level equivalent. Rates of future sea …

To resolve the mechanisms behind the major climate reorganisation, which occurred
between 0.9 and 1.2 Ma, the recovery of a suitable 1.5 million-year-old ice core is …

Identifying the location of the ice–bedrock interface of glaciers and ice sheets is crucial for a
wide range of geophysical applications, such as searching for liquid water in basal regions …

Ice sheets provide exceptional archives of past changes in polar climate, regional
environment and global atmospheric composition. The oldest dated deep ice core drilled in …

Quantification of land surface–atmosphere fluxes of carbon dioxide (CO 2) and their trends
and uncertainties is essential for monitoring progress of the EU27+ UK bloc as it strives to …