The vast majority of Siberia is located in the northern hemisphere, with a large portion of it being north of the Arctic Circle. As a result, the winters are long and severe, with temperatures often dropping below -40 degrees Celsius (-40 degrees Fahrenheit).
During the summer months, temperatures in Siberia can rise above 30 degrees Celsius (86 degrees Fahrenheit) in some areas, particularly in southern Siberia. However, these warm periods are relatively short-lived, and the overall climate remains continental with significant temperature fluctuations.
The extreme temperatures experienced in Siberia are due to its geographical location and the influence of the continental climate. The region is far from any major bodies of water, which moderates temperatures, and the lack of mountain ranges allows cold air masses from the Arctic to penetrate deep into Siberia.
As a result of the extreme climate conditions, Siberia is largely unpopulated, with most of its inhabitants concentrated in the southern and western regions, where the climate is more favorable.