Climate of Greece

The climate of Greece can be categorised into three types (the Mediterranean, the Alpine and the Temperate) that influence well-defined regions of its territory. The Pindus mountain range strongly affects the climate of the country by making the western side of it (areas prone to the south-westerlies) wetter on average than the areas lying to the east of it (lee side of the mountains). The Mediterranean type of climate features mild, wet winters and hot, dry summers. The Cyclades, the Dodecanese, Crete, the Eastern Peloponnese and parts of the Sterea Ellada (Central Continental Grece) region are mostly affected by this particular type of climate. Temperatures rarely reach extreme values along the coasts, although, with Greece being a highly mountainous country, snowfalls occur frequently in winter. It sometimes snows even in the Cyclades or the Dodecanese.

The Alpine type is dominant mainly in the mountainous areas of Northwestern Greece (parts of Epirus, Central Greece, Thessaly, Western Macedonia) as well as in the central parts of Peloponnese, including parts of the prefectures of Achaia, Arcadia and Laconia, where extensions of the Pindus mountain range pass by. Finally, the Temperate type affects Central Macedonia and East Macedonia and Thrace; it features cold, damp winters and hot, dry summers with frequent thunderstorms. Athens is located in a transitional area featuring both the Mediterranean and the Temperate types. The city's northern suburbs are dominated by the temperate type while the downtown area and the southern suburbs enjoy a typical Mediterranean type.
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