The Siberian High (also Russo-Siberian High/Anticyclone) is a massive collection of cold or very cold dry air that accumulates on the Eurasian terrain for much of the year, usually centred around Lake Baikal.“The Siberian High and Climate Change over Middle to High-Latitude Asia” It reaches its greatest size and strength in the winter, when the air temperature near the center of the high-pressure cell or anticyclone is often lower than .
详细百科解释