Page 3: Research news on permafrost

Permafrost is a cryospheric topic referring to ground (soil, sediment, or rock, with included ice and organic material) that remains at or below 0 °C for at least two consecutive years. Its thermal and hydrological regimes are governed by surface energy balance, snow cover, vegetation, and ground ice content, leading to stratified active layers that thaw seasonally above a perennially frozen substrate. Permafrost dynamics influence geomorphological processes such as thermokarst formation, ground subsidence, and slope instability, and critically regulate carbon and methane fluxes from frozen organic matter. Research on permafrost integrates climatology, biogeochemistry, geotechnical engineering, and remote sensing to quantify its stability and feedbacks within the Earth system.

Greenland's caves preserve an ancient climate archive

In a remote cave in northern Greenland, a research team led by geologists Gina Moseley, Gabriella Koltai, and Jonathan Baker from the University of Innsbruck has discovered evidence of a significantly warmer Arctic. The cave ...

A new explanation for Siberia's giant exploding craters

Scientists may be a step closer to solving the mystery of Siberia's giant exploding craters. First spotted in the Yamal and Gydan peninsulas of Western Siberia in 2012, these massive holes, known as giant gas emission craters ...

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