= Siberian High
{wiki=Siberian_High}
The Siberian High, also known as the Siberian Anticyclone, is a vast area of high atmospheric pressure that forms over Siberia during the winter months. This meteorological phenomenon is characterized by cold, dense air that accumulates due to extremely low temperatures in the region. The Siberian High typically develops in late fall and persists through the winter, influencing weather patterns not only in Siberia but also in surrounding areas, including parts of East Asia and the Arctic.
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