The Siberian climate is characterized by its extreme temperatures, with long, harsh winters and short, mild summers. Winter temperatures can drop below -40°C (-40°F), while summer temperatures can reach up to 30°C (86°F) in some areas. This climate is primarily influenced by its high latitude and distance from the ocean. Precipitation in Siberia is relatively low, mostly falling during the summer months. The region experiences a continental climate, meaning there are significant temperature variations between seasons. The vast Siberian Taiga, a dense forest, plays a crucial role in the ecosystem, supporting diverse wildlife adapted to these conditions.