What are the main characteristics of the Siberian High?

<p style=";text-align:left;direction:ltr">Arab Weather - The Siberian high is characterized by the following features:</p><ol style=";text-align:left;direction:ltr"><li style=";text-align:left;direction:ltr"> Extreme cold: Formed as a result of surface cooling in winter over Siberia, resulting in very low temperatures.</li><li style=";text-align:left;direction:ltr"> Dryness: The air in the Siberian High is very dry due to the extreme cold that limits the air&#39;s ability to hold moisture.</li><li style=";text-align:left;direction:ltr"> High atmospheric pressure: Characterized by very high atmospheric pressure compared to the surrounding areas, resulting in stable conditions.</li><li style=";text-align:left;direction:ltr"> Persistence: The Siberian High usually forms in winter and lasts for long periods, affecting weather in large areas of Asia.</li><li style=";text-align:left;direction:ltr"> Distribution: Affects the climate of China, Korea, Japan, and parts of Eastern Europe, causing long periods of cold, dry weather.</li></ol>