The permanently frozen subsoil in the tundra is called permafrost. It consists of soil, rocks, and sediment that remain frozen for at least two consecutive years. Permafrost plays a crucial role in the tundra ecosystem and its stability is being affected by climate change.
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A vast, treeless region with permanently frozen subsoil is called tundra. This biome is typically found in high latitudes or high altitudes and experiences extreme cold temperatures, resulting in a layer of permafrost beneath the surface that remains frozen year-round.
A layer of permanently frozen subsoil in the tundra is called permafrost. It consists of soil, rock, or sediment that remains at or below 0°C for at least two consecutive years. Permafrost plays a crucial role in regulating the climate and supporting unique ecosystems in the tundra.
Permafrost is a layer of permanently frozen subsoil found in the tundra. It consists of soil, rock, or sediment that remains frozen for two or more years, even during the summer months. Permafrost plays a crucial role in maintaining the stability of Arctic ecosystems.
Tundra is the geographical feature that describes a frozen treeless landscape with low-growing vegetation, located in cold regions near the North and South poles. It is characterized by a permanently frozen subsoil layer called permafrost.
A vast flat treeless region with permanently frozen subsoil is known as a tundra. The top layer of soil thaws during the summer but remains frozen below, which is called permafrost. This type of environment is found in polar regions and high mountain tops.