lähisarktiline

Lähisarktiline refers to a subarctic climate zone. This region is characterized by long, cold winters and short, mild summers. The temperatures are significantly lower than in temperate zones but not as extreme as in the true Arctic. Precipitation is generally low, often falling as snow during the winter months.

The vegetation in Lähisarktiline areas is typically sparse, dominated by tundra and coniferous forests, often referred to as taiga or boreal forest. Permafrost, a layer of soil that remains frozen throughout the year, is common in many Lähisarktiline regions, influencing drainage patterns and plant life.

These zones are found in the northern latitudes of continents, bordering the Arctic Circle. Examples of Lähisarktiline regions include large parts of Canada, Alaska, Siberia, and Scandinavia. The low population density and challenging environmental conditions mean that human settlements are often scattered and reliant on natural resources. Wildlife in these areas is adapted to the cold climate, with species like reindeer, arctic foxes, and various migratory birds being characteristic. The transition between the Lähisarktiline and the temperate zones is gradual, marked by changes in vegetation and temperature regimes.