Page 8: 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.

Permafrost thaw: Gradual change or climate tipping point?

The Arctic is warming almost four times faster than the rest of the planet. High temperatures are already causing the permanently frozen ground, known as permafrost, to thaw. The carbon contained in this soil is then released ...

Thawing permafrost dots Siberia with rash of mounds

In the vast white expanse around Churapcha in eastern Siberia, the ever more rapid thaw of the permafrost is changing the landscape, cracking up houses and releasing greenhouse gases.

When glaciers roamed Mars

The surface of Mars is known for being an extremely cold, desiccated, and irradiated place. But as its many surface features attest, the red planet was once a warmer, wetter place with flowing water and glaciers. Today, most ...

page 8 from 8