Global warming is leaving more and more apparent scars in the world’s permafrost regions. As the new global comparative study conducted by the international permafrost network GTN-P shows, in all regions with permafrost soils the temperature of the frozen ground at a depth of more than 10 metres rose by an average of 0.3 degrees Celsius between 2007 and 2016 – in the Arctic and Antarctic, as well as the high mountain ranges of Europe and Central Asia. The effect was most pronounced in Siberia, where the temperature of the frozen soil rose by nearly 1 degree Celsius. The pioneering study has just been released in the online journal Nature Communications.
Roughly one sixth of the land areas on our planet are considered to be permafrost regions, which means the soils there have remained permanently frozen for at least two consecutive years. In most of these regions, however, the cold penetrated the ground millennia ago; as a result, in the most extreme cases, the permafrost continues to a depth of 1.6 kilometres. Especially in the Arctic, people rely on the permafrost soil as a stable foundation for houses, roads, pipelines and airports. Yet in the wake of global warming, the integrity of these structures is increasingly jeopardised, creating enormous costs. In addition, permafrost soils contain massive quantities of preserved plant and animal matter. If this organic material thaws along with the permafrost, microorganisms will begin breaking it down – a process that could produce enough carbon dioxide and methane emissions to potentially raise the global mean temperature by an additional 0.13 to 0.27 degrees Celsius by the year 2100.
Read more at Alfred Wegener Institute for Polar and Marine Research
Photo: AWI permafrost scientists investigate the eroding coastline at the Siberian island Sobo-Sise, Eastern Lena delta. CREDIT: Guido Grosse