Page 7: 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.

Snapshot of Antarctica's past helps predict future climate

In the first study to consider the long-term evolution of the rivers that flow beneath glaciers, researchers have new insights into the future of Antarctica's melting ice that may change the way climate scientists predict ...

Carbon dioxide collapse: How water flowed on an icy Mars

On a cold, ancient Mars, rivers flowed and a lake the size of the Mediterranean Sea swelled under the protection of thick ice ceilings, according to new research published in the Journal of Geophysical Research: Planets.

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