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  2. Permafrost - Wikipedia

    en.wikipedia.org/wiki/Permafrost

    Permafrost temperature profile. Permafrost occupies the middle zone, with the active layer above it, while geothermal activity keeps the lowest layer above freezing. The vertical 0 °C or 32 °F line denotes the average annual temperature that is crucial for the upper and lower limit of the permafrost zone, while the red lines represent seasonal temperature changes and seasonal temperature ...

  3. Tundra of North America - Wikipedia

    en.wikipedia.org/wiki/Tundra_of_North_America

    These complex interactions between plants, animals and abiotic factors in the tundra are held together by the permafrost layer, located 450 metres (1,480 ft) under the soil. [3] However climate change is causing this crucial layer of frozen soil to melt. As a result, tundra communities are becoming unstable and basic processes are breaking down.

  4. Polar ecology - Wikipedia

    en.wikipedia.org/wiki/Polar_ecology

    Because of the cold weather it is hard for plants to grow. Frozen ground covers most of the polar regions for the majority of the year. Permafrost reaches a thickness of 600–1,000 m (2,000–3,300 ft) deep. Large amounts of permafrost can lead to poor water drainage. Due to the permafrost the water in the soil remains frozen for most of the year.

  5. Frost - Wikipedia

    en.wikipedia.org/wiki/Frost

    Plants that have evolved in warmer climates ... it refers to the frost that makes trees and bushes look like white hair. ... Permafrost is a layer of frozen earth ...

  6. Tundra - Wikipedia

    en.wikipedia.org/wiki/Tundra

    Permafrost tundra includes vast areas of northern Russia and Canada. [2] The polar tundra is home to several peoples who are mostly nomadic reindeer herders, such as the Nganasan and Nenets in the permafrost area (and the Sami in Sápmi). Tundra in Siberia. Arctic tundra contains areas of stark landscape and is frozen for much of the year. [5]

  7. Active layer - Wikipedia

    en.wikipedia.org/wiki/Active_layer

    This is important because roots of plants cannot penetrate beyond the active layer and are restricted by its thickness. Thus, in a continuous permafrost environment plants must have shallow roots, which restricts tree growth to specialised species such as Larix. In areas of discontinuous permafrost, most conifers are able to grow easily.

  8. Read the touching love letter Jimmy Carter wrote his wife 75 ...

    www.aol.com/read-touching-love-letter-jimmy...

    Amy Lynn Carter, daughter of Jimmy and Rosalynn Carter, read a love letter written by her father 75 years ago during Rosalynn's tribute service in Atlanta Nov. 28.

  9. Thaw depth - Wikipedia

    en.wikipedia.org/wiki/Thaw_depth

    In ecology, roots of plants cannot penetrate beyond the active layer, which places restrictions on which plants can grow in permafrost. In construction, the thaw depth is a major factor in ensuring the structural integrity of the objects in question.