You may have heard of permafrost, especially if you live in the northern hemisphere. If not, then a brief tutorial is probably necessary, since a significant tectonic climate change is occurring as I write this article, as you read this article, and even before, long enough ago to become a news story—though not sufficiently covered. Permafrost is soil and subsoil that remains at a temperature of 0°C or below for at least two consecutive years. It contains mixtures of soil, stones, and old organic material that has not decomposed because it remained frozen. In the Arctic, it covers about 25% of the land area of the northern hemisphere, with widespread distribution in Siberia, Alaska, Canada, Greenland, and mountainous areas (e.g., Scandinavia, the Alps). Above it is a seasonal “active layer” of soil that thaws and freezes every year. Although the term describes “freezing,” this layer does not melt completely; it simply “thaws” during the summer. However, with the current global warming, the ice in the permafrost is now beginning to melt more and more, causing significant changes to the landscape and climate.
In recent years, the Arctic has been warming much faster than the rest of the planet, with measurements showing that Arctic temperatures have risen three to four times faster* than the global average. The annual average Arctic atmospheric temperature has risen by ~3°C since the 1970s, and in 2023 and 2024, the Arctic experienced sharp warm periods (heat waves), with record surface temperatures and heavy rainfall. As the air temperature rises, the frozen ground melts immediately, so that the increase in Arctic temperatures above zero has almost doubled the area of thawing ground in the northern hemisphere.
