About
Contact & Profiles
Research Areas
- Cryospheric studies and observations
- Arctic and Antarctic ice dynamics
- Climate change and permafrost
- Winter Sports Injuries and Performance
University of Leeds
2025
10.1080/00167487.2024.2437946
article
EN
Geography
2025-01-02
Glaciers terminating in lakes typically flow, thin and lose mass more rapidly than those that terminate on land. This is due to a range of thermomechanical processes exerted at the lake-ice interface, where lake waters drive melt-induced undercutting, enable flotation facilitate calving. In Greenland, ice marginal (IMLs) have increased size number over recent decades now occupy 10% sheet margin. Despite this, very few observations their effects dynamics exist, meaning they remain largely...
10.5194/egusphere-egu25-12360
preprint
EN
2025-03-15
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