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North Asia is a vast region of Asia that primarily includes Siberia and the northeastern edges of the continent. This region is characterized by diverse relief, featuring faulted and folded mountains, plateaus, and lowlands. Notable geographical features include the Central Siberian Plateau, the West Siberian Plain, and the mountains and islands of the Asian Arctic.1

The climate in North Asia is predominantly continental subarctic, marked by long, extremely cold winters and short, mild summers. Annual temperature ranges can be exceptionally large, particularly in interior Siberia. Precipitation is generally low, with most falling as snow during the winter months.2

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