Page 8: Research news on ice sheet

An ice sheet, as a geophysical substance, is a massive, contiguous body of glacial ice that covers more than 50,000 km² and is sufficiently thick (often >2–3 km) for its internal deformation and basal sliding to dominate flow dynamics. Composed primarily of recrystallized freshwater ice with embedded air bubbles, dust, and minor impurities, it exhibits anisotropic rheological behavior described by non-Newtonian creep laws (e.g., Glen’s flow law). Ice sheets thermally stratify between cold and temperate regimes, store the majority of Earth’s terrestrial freshwater, and interact with bedrock and subglacial hydrological systems, influencing isostasy, basal lubrication, and large-scale mass balance.

85 new subglacial lakes detected below Antarctica

Hidden beneath the biggest ice mass on Earth, hundreds of subglacial lakes form a crucial part of Antarctica's icy structure, affecting the movement and stability of glaciers, and consequentially influencing global sea level ...

Scientists uncover extreme life inside the Arctic ice

If you pull an ice core from the outer edges of the Arctic polar cap, you might spot what looks like a faint line of dirt. Those are diatoms—single-celled algae with outer walls made of glass. Their presence in ice isn't ...

Strong tides speed melting of Antarctic ice shelves

Antarctic ice is melting. But exactly which forces are causing it to melt and how melting will influence sea level rise are areas of active research. Understanding the decay of ice shelves, which extend off the edges of the ...

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