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Climate of Kosovo
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Climate of Kosovo : ウィキペディア英語版
Climate of Kosovo

Kosovo is a relatively small territory. Because of the climatic position and complicated structure of the relief, Kosovo has a variety of climate systems. Kosovo lies in the south part of the middle geographical latitude of the northern hemisphere and it is affected by the Mediterranean mild climate and European continental climate. Important factors that affect Kosovo's climate are: its position towards Eurasia and Africa, hydrographic masses (Atlantic ocean and Mediterranean sea), atmospheric masses (tropic, arctic and continental) etc. Minor factors that affect Kosovo's climate are: relief, hydrography, plain and vegetation.〔Riza Çavolli 1993, p. 22〕
==Climatic areas==

The climatic area of the Ibar valley is influenced by continental air masses. For this reason, in this part of the region, the winters are colder with medium temperatures above , but sometimes down to . The summers are very hot with average temperatures of , sometimes up to . This area is characterized by a dry climate and a total annual precipitation of 600 mm per year, approximately. The climatic area of Metohija, which includes the watershed of the White Drin river, is influenced very much by the hot air masses, which cross the Adriatic Sea. Medium temperatures during winter range from to sometimes . The average annual precipitation of this climatic area is about per year. The winter is characterized by heavy snowfalls. The climatic area of the mountains and forest parts is characterised by a typical forest clime, that is associated with heavy rainfalls ( per year), and summers that are very short and cold, and winters that are cold and with a lot of snow. Finally, it can be stated that the Kosovo territory is characterised by a sunny climate with variable temperature and humidity conditions.〔()〕

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