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2017 | OriginalPaper | Chapter

3. Climate

Authors : Pavle Pavlović, Nikola Kostić, Branko Karadžić, Miroslava Mitrović

Published in: The Soils of Serbia

Publisher: Springer Netherlands

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Abstract

A mild temperate (mesothermal) climate (i.e. Köppen’s ‘C climate’) dominates in Serbia. However, on high mountains (i.e. at altitudes above 1,500 m), the climate is ‘boreal’ or microthermal (i.e. Köppen’s ‘D climate’), while the Tundra climate (Köppen’s ‘ET climate’) is only sporadically represented, occurring in regions above 2,000 m. The Dinaric Mountains form a topographic barrier that affects the precipitation pattern of the Balkan Peninsula with the west-facing side of the Dinarides receiving large amounts of rainfall. A semi arid season lasting from July to October is characteristic for the Pannonian region, while in eastern lowland regions (the Danube and Timok river valleys), seasonal drought is more severe, with the dry period lasting from July to September. 

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Metadata
Title
Climate
Authors
Pavle Pavlović
Nikola Kostić
Branko Karadžić
Miroslava Mitrović
Copyright Year
2017
Publisher
Springer Netherlands
DOI
https://doi.org/10.1007/978-94-017-8660-7_3