Q: What is the Siberian High?

The Siberian Anticyclone is a huge mass of cold air that gathers over the Siberian region in northeastern Eurasia. It is formed as a result of intense surface cooling over the continental regions far from marine influences. The Siberian Anticyclone is one of the Cold Continental Anticyclones. ), and because the cold air pressure is high, high pressure prevails in the areas it affects, and the temperature decreases, as extreme cold and drought are among the most important features of the Siberian high air. More