PERMAFROST

Eng./Esp.

In geology Permafrost, cryotic soil or permafrost soil, is soil at or below the freezing point of water (0°C or 32°F) for two or more years. The extent of it can vary as the climate changes. Today, a considerable area of the Arctic is covered by Permafrost . https://phys.org/tags/permafrost/

Revegetation in extremely degraded grassland improves permafrost instability on Qinghai-Tibetan plateu.

Pandoravirus : The Melting Arctic is releasing ancient germs – how worry should we be?

NASA fieldwork studies signs of climate change in Arctic and boreal regions.

New research shows Antarctic summer thaw stars earlier , ends later than previously believed.

Vegetation regulates energy exchange in the Arctic.

Microbes in Arctic soil are primed to react to climate change.

Permafrost emissions must be factored into global climate targets, says study.

Study reveals current state and past changes in frozen ground at Earth’s Third Pole.

Melting Permafrost increases greenhouse gas…