Accurate bed topography is critical for predicting Antarctica's future ice discharge and sea-level contribution, yet lar...
As new airborne surveys of the Antarctic ice sheet are completed, the ever-enlarging survey dataset provides an opportun...
Grounding zones have long been recognized as critical for understanding the past, present and future evolution of ice sh...
Airborne radio-echo sounding (RES) surveys are currently the primary method of measuring ice sheet thickness to derive s...
Ice-penetrating radar observation of bed echoes is a core geophysical technique in glaciology. In early and ongoing expl...
Identifying basal wetness conditions beneath the Antarctic ice sheet is essential for understanding subglacial hydrology...
Multichannel ice-penetrating radar systems can be used to generate radar volumes: three-dimensional data structures that...
Antarctic bed mapping underpins our understanding of ice-sheet stability, grounding-line retreat and future sea-level ri...
The Intergovernmental Panel on Climate Change (IPCC) AR6 report (2021) provides a range of projections on greenhouse gas...
Despite decades of effort to map bed elevation under the Antarctic Ice Sheet, significant gaps remain in this geometric ...
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