Research news on glaciation

Glaciation refers to the climatic and geophysical processes leading to the formation, expansion, and persistence of glaciers and ice sheets, and their subsequent sculpting of the Earth’s surface. It encompasses large-scale cooling, snow accumulation exceeding ablation, and dynamic ice flow driven by gravity and basal sliding. Glaciation cycles, governed primarily by orbital forcing (Milankovitch cycles), greenhouse gas concentrations, and feedbacks involving albedo and ocean circulation, produce glacial–interglacial variations in global climate. These events generate diagnostic landforms (e.g., moraines, drumlins, U-shaped valleys) and stratigraphic signatures, and they are central topics in Quaternary science, paleoclimatology, and Earth system modeling.

Why Antarctica froze millions of years before the Arctic

East Antarctica hosts the largest ice sheet on Earth, containing enough water to raise global sea levels by 52 meters (171 feet) were it to fully melt. Yet scientists have been puzzled for decades about how and why this ice ...

Data suggest greater glacial flood risk faced by Bhutan

Researchers at Newcastle University have carried out the first comprehensive modeling of glacial lake outburst flood (GLOF) risk in Bhutan and identified previously unrecognized high-risk lakes.

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