Climate of Serbia
The Serbian climate is between a continental climate in the north, with cold dry winters, and warm, humid summers with well distributed rainfall patterns, and a more Mediterranean climate in the south with hot, dry summers and autumns and average relatively cool and more rainy winters with heavy mountain snowfall. Differences in elevation, proximity to the Adriatic Sea and Aegean Sea and large river basins, as well as exposure to the winds account for climate differences. Northern Serbia possesses typical continental climate, with air masses from northern and western Europe which shape its climatic profile. South and  South-east of Serbia is subject to strong Mediterranean influences (hotter summers and milder winters). However, the Dinaric Alps and other mountain ranges contribute to the cooling down a large part of the warm air masses. Winters are quite harsh in Raška (region) because of the mountains which encircle the plateau. Mediterranean micro-regions exist throughout southern Serbia, in Zlatibor and the Pčinja District around valley and river Pčinja. The average annual air temperature for the period 1981–2017 for the area with an altitude of up to is . The areas with an altitude of have an average annual temperature of  around , and over of altitude around . The lowest recorded temperature in Serbia was (January 26, 2006, Karajukića Bunari in Pešter), and the highest was (July 24, 2007, Leskovac).