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Climate in Serbia


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On the macro-level, the climate of Serbia is under the influences of the Atlantic Ocean and Mediterranean Sea and the landmass of Eurasia. With mean January temperatures around 0 °C (32 °F), and mean July temperatures around 22 °C (72 °F), it can be classified as transitional between oceanic (Köppen climate classification Cfb), humid subtropical (Cfa) and humid continental (Dfa). Rainfall patterns are well-distributed and average about 50 mm/month.

In the north, the climate is more continental, with cold winters, and hot, humid summers with well distributed rainfall patterns. In the south, summers and autumns are drier, and winters are relatively cold, with heavy inland snowfall in the mountains. Differences in elevation, proximity to the Adriatic Sea and large river basins, as well as exposure to the winds account for climate variations. South and South-west Serbia are subject to Mediterranean influences. However, the Dinaric Alps and other mountain ranges contribute to the cooling of most of the warm air masses. Winters are quite harsh in the Pešter plateau, because of the mountains which encircle it.

The average annual air temperature for the period 1961–90 for the area with an altitude of up to 300 m (984 ft) is 10.9 °C (51.6 °F). The areas with an altitude of 300 to 500 m (984 to 1,640 ft) have an average annual temperature of around 10.0 °C (50.0 °F), and over 1,000 m (3,281 ft) of altitude around 6.0 °C (42.8 °F). The lowest recorded temperature in Serbia was −39.5 °C (−39.1 °F) on 13 January 1985, Karajukića Bunari in Pešter, and the highest was 44.9 °C or 112.8 °F, on 24 July 2007, recorded in Smederevska Palanka
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