A periglacial climate is characterized by areas that are influenced by the presence of permafrost, where temperatures remain below freezing for extended periods, but are not consistently cold enough to support glacial conditions. This climate type is often found in high-latitude regions, where the ground remains frozen beneath a layer of active soil that thaws during the warmer months. The periglacial environment creates unique landforms and processes due to the freeze-thaw cycles and the interplay between ice, soil, and vegetation.
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