Widespread existing geological records from above the modern ice-sheet surface and
outboard of the current ice margin show that the Antarctic Ice Sheet (AIS) was much more …

The future response of the Antarctic ice sheet to rising temperatures remains highly
uncertain. A useful period for assessing the sensitivity of Antarctica to warming is the Last …

Until recently, little was known about the Weddell Sea sector of the West Antarctic Ice Sheet.
In the last 10 years, a variety of expeditions and numerical modelling experiments have …

Abstract The Antarctic Ice Sheet (AIS) response to past warming consistent with the 1.5–2° C
“safe limit” of the United Nations Paris Agreement is currently not well known. Empirical …

Abstract The Southern Ocean occupies 14% of the Earth's surface and plays a fundamental
role in the global carbon cycle and climate. It provides a direct connection to the deep ocean …

Reconstructing the dynamic response of the Antarctic ice sheets to warming during the Last
Glacial Termination (LGT; 18,000–11,650 yrs ago) allows us to disentangle ice-climate …

Each summer, surface melting of the margin of the Greenland Ice Sheet exposes a
distinctive visible stratigraphy that is related to past variability in subaerial dust deposition …

Structural glaci‐geological processes can entrain basal sediment into ice, leading to its
transportation and deposition downstream. Sediments potentially rich in essential nutrients …

The current ice core record extends back 800,000 years. Geologic and glaciological
evidence suggests that the Allan Hills Blue Ice Area, East Antarctica, may preserve a …

Blue ice is found in areas of Antarctica where katabatic winds, focussed by steep surface
slopes or by topography around nunataks, cause enhanced surface ablation. This process …