Nature Geoscience, 18 November 2025
Small underwater eddies contribute to nearly a fifth of total Antarctic ice shelf melting each season, but during extreme events this submarine melting can increase by as much as three-fold within hours as warm water penetrates beneath the ice. Similar to hurricanes and other large storms generated in the open ocean, these swirling eddies grow larger as they approach ice shelves and can cause substantial damage. A high-resolution ocean model in the Amundsen Sea Embayment finds that these small-scale ocean circulation patterns are intensified by ice shelf melting, creating positive feedbacks that increase ocean turbulence and ice shelf loss. The study highlights the importance of including these short-term, “weather-like” ocean processes in climate models and developing more observational tools to better anticipate future ice shelf stability.
Paper | Nature Research Briefing | News Coverage by the University of California, Irvine
Nature Climate Change, 16 February 2026 The Antarctic Ice Sheet does not respond to warming…
Frontiers in Environmental Science, 20 February 2026 The Antarctic Peninsula has been warming 0.3-0.5°C per…
Water Resources Research, 9 February 2026 Glaciers in the Tien Shan mountains of Asia are…
The Cryosphere, 8 December 2025 Present-day human choices on emissions pathways will have long-lasting consequences…
The Amazon rainforest and the Earth’s cryosphere, though geographically distant, are profoundly interconnected. Deforestation and…
Nature Communications, 11 February 2026, Early Views) The Greenland Ice Sheet has seen an increase…