The city possesses a humid continental climate to frosts.
The distribution of precipitation is determined by the circulation of air masses, relief, and air temperatures. The main part of the precipitation is brought by cyclones with a western air mass transfer, that is, from the European part of Russia, while their average annual amount is 542 mm. The maximum falls on a warm season, during which about 60–70% of the annual amount falls. For the winter period is characterized by snow cover with an average capacity of 40–50 cm. The coefficient of moistening [ru] (the ratio of yearly precipitation and potential evaporation) – 1.
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