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.

Scientists identify hidden accelerant in Antarctic ice loss

For years, scientists have warned that melting Antarctic ice could push sea levels dangerously higher by the end of this century. But a new study led by University of Maryland scientist Madeleine Youngs suggests those warnings ...

Ancient iceberg scratches reveal reverse Great Lakes snowbelt

Buffalo's legendary snowfall totals are largely the result of one unlucky geographic reality: the city sits east of the Great Lakes instead of west. Anyone who has lived through a winter in Buffalo, Cleveland or any snowbelt ...

Glaciers may flow into the ocean more quickly than we think

Models of glacial flow and retreat rely on estimates of glacial ice viscosity, the measure of the ice's resistance to flow. Ice viscosity is dependent on the stress applied to the glacier. Most ice sheet models use a standard ...

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