turdan
tundra
Permafrost is used for the continually frozen layer of soil underneath Earth's surface in high latitudes.
Permafrost is a permanently frozen soil, and occurs mostly in high latitudes. Permafrost comprises 24% of the land in the Northern Hemisphere, and stores a massive amounts of carbon.
High latitudes .
cause storms
tundra
tundra
Tiaga
Permafrost is used for the continually frozen layer of soil underneath Earth's surface in high latitudes.
Permafrost is when the ground is permanently frozen, while latitude is an imaginary line on the globe that tells position. At high latitudes, you'll find permafrost.
The tundra biome is typically found in high latitudes near the North and South Poles, as well as at high elevations in mountains. It is characterized by low temperatures, short growing seasons, and permafrost, which limits plant growth.
Permafrost is a permanently frozen soil, and occurs mostly in high latitudes. Permafrost comprises 24% of the land in the Northern Hemisphere, and stores a massive amounts of carbon.
The tundra region is a cold, treeless biome found in the Arctic, Antarctic, and high mountain regions. It is characterized by low temperatures, short growing seasons, and permafrost soil. Plant life in the tundra consists mainly of mosses, lichens, and low-growing shrubs adapted to the harsh conditions.
Contiguous areas with similar climate condition and geographically and climatically areas are called biomes. For Asia and North America with a high latitudes areas, they are part of a biome called taiga or boreal forest/snow forest.
The Hudson Bay lowlands are characterized by flat, swampy terrain with numerous lakes and rivers in the Hudson Bay region. The Arctic lowlands are flat, treeless expanses found in the northernmost parts of Canada, with permafrost underlying the soil. Both regions have a cold climate and limited vegetation due to their high latitudes.
The answer is tundra.Permafrost is permanently frozen ground, a common feature in the high latitudes, mostly in the tundra biome.Climate changes can expand or reduce the areas affected by permafrost, which currently includes the Arctic lands in Canada, Greenland, Scandinavia, and Russia. However, some areas have a thin layer of soil at the surface that can thaw during the summer. This is called an active layer, and can be boggy because melt water cannot drain into the underlying permafrost.
The swampy coniferous forest of high northern latitudes, esp. that between the tundra and steppes of Siberia and North America.