Abstract TALDICE (TALos Dome Ice CorE) is a 1620 m deep ice core drilled at Talos Dome,
an ice dome located at the edge of the East Antarctic Plateau in the Ross Sea Sector. The …

Radio-echo sounding (RES) reveals patches of high backscatter in basal ice units, which
represent distinct englacial features in the bottom parts of glaciers and ice sheets. Their …

Driven primarily by variations in the earth's axis wobble, tilt, and orbit eccentricity, our planet
experienced massive glacial/interglacial reorganizations of climate and atmospheric CO 2 …

Surface processes alter the water stable isotope signal of the surface snow after deposition.
However, it remains an open question to which extent surface post‐depositional processes …

A new micro-destructive technique for high-resolution water isotope analysis of ice samples
using a Laser Ablation (LA) system coupled with a Cavity Ring Down Spectrometer (CRDS) …

The Dome Fuji (DF) region in Antarctica is a potential site for an ice core with a record of
over 1 Myr. Here, we combine large-scale internal airborne radar stratigraphy with a 1-D …

Radio-echo sounding (RES) is a useful technique for measuring the subsurface properties
of ice sheets and glaciers. One of the most important and unique outcomes is the mapping of …

Understanding post‐depositional processes altering the layer sequence in ice cores is
especially needed to avoid misinterpretation of the oldest and most highly thinned layers …

Nitrate in Antarctic snow has seasonal cycles in nitrogen and oxygen isotopic ratios that
reflect its sources and atmospheric formation processes, and as a result, nitrate archived in …

We present an ice-penetrating radar data set which consists of 26 internal reflecting
horizons (IRHs) that cover the entire Dome C area of the East Antarctic plateau, the most …