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Climate of Turkey
Turkey's climate is varied and generally temperate, with the regions bordering the Mediterranean and Black Sea heavily affected by the coasts, and the interior being drier and more continental.
Coastal areas in the southern half of the country, including Antalya, İzmir, Adana, feature a very typical Mediterranean climate, with hot, dry summers and mild, rainy winters. Coastal areas in the north are cooler and are either humid temperate or sub-Mediterranean, with cool, frequently rainy and occasionally snowy winters, and warm summers.
The lower plateaus of the interior are generally continental, and feature hot, dry summers, and cold, snowy winters. Winter precipitation varies widely, leading to humid precipitation regimes near areas like Bitlis, while rain-shadowed areas are semi-arid. On higher elevations, plateaus that nevertheless allow permanent settlement, like Kars and Ardahan, are high-continental and sometimes subalpine, with frigid, snowy winters, and mild, rainy summers.
Dry summers in the south and west, along with moderate aridity in the interior makes the country vulnerable to climate change.
A "true", or rather eu-Mediterranean (Köppen: Csa, Trewartha: Cs) climate exists on sea level from the coasts of Antakya to around Muğla, and north to around Manisa, which is generally considered to be its northern limit. Average temperatures range between 17–20 °C (63–68 °F); winters have means around 7–10 °C (45–50 °F), while summers have mean temperatures between 26–29 °C (79–84 °F). Precipitation amounts to around 600–1,200 millimetres (24–47 in), all of it rain. Summers get almost no rain, while winters receive plentiful, and sometimes copious amounts of it. Winter precipitation depends on local topography, with enclosed bays of convergent air,[citation needed] such as Antalya, getting almost twice the amount of rain as storm-protected areas such as Mersin.
Mountains around the region still show the Mediterranean rainfall pattern, but have mild summers and below-freezing temperatures during winter, creating a zone which may be termed oro-Mediterranean.
A pre-Mediterranean climate (Turkish: Akdeniz sâhil ardı iklimi, Köppen: Csa, Trewartha: Cs/Do/Dc) exists in relatively continental areas influenced by the Mediterranean climatic system, notably around the inner Aegean and Southeastern Anatolia. Average temperatures range between 14–18 °C (57–64 °F) with winter means around 1–6 °C (34–43 °F), and summers as hot as (or hotter than) the Mediterranean. Rainfall follows the general pattern of the Mediterranean region, but sunshine is sometimes noticeably lower, and precipitation amounts are lower than the Mediterranean region, between 400–800 millimetres (16–31 in). Snow can also fall in this area, unlike the coastal Mediterranean region.
The climate around the Marmara Sea (Turkish: Marmara geçiş iklimi, lit. 'Marmara transitional climate', Köppen: Csa/Csb/Cfa/Cfb, Trewartha: Cs/Cf/Do) is complex, transitional and often microclimatic. It wraps around the sea, covering Bursa, Bilecik, southern İzmit and İstanbul, as well as Tekirdağ. Often of a meso- or supra-Mediterranean quality at sea-level; its vegetation at sea level is similar to the lower mountains of the "true" Mediterranean region, with heat-tolerant broadleaf oaks and occasional mesophilous trees, such as beech. Therefore, it is generally considered mild-temperate and not subtropical in Turkish sources and furthermore, Bohn, in a survey of European vegetation and climate, calls the climate sub-continental sub-Mediterranean.
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Climate of Turkey
Turkey's climate is varied and generally temperate, with the regions bordering the Mediterranean and Black Sea heavily affected by the coasts, and the interior being drier and more continental.
Coastal areas in the southern half of the country, including Antalya, İzmir, Adana, feature a very typical Mediterranean climate, with hot, dry summers and mild, rainy winters. Coastal areas in the north are cooler and are either humid temperate or sub-Mediterranean, with cool, frequently rainy and occasionally snowy winters, and warm summers.
The lower plateaus of the interior are generally continental, and feature hot, dry summers, and cold, snowy winters. Winter precipitation varies widely, leading to humid precipitation regimes near areas like Bitlis, while rain-shadowed areas are semi-arid. On higher elevations, plateaus that nevertheless allow permanent settlement, like Kars and Ardahan, are high-continental and sometimes subalpine, with frigid, snowy winters, and mild, rainy summers.
Dry summers in the south and west, along with moderate aridity in the interior makes the country vulnerable to climate change.
A "true", or rather eu-Mediterranean (Köppen: Csa, Trewartha: Cs) climate exists on sea level from the coasts of Antakya to around Muğla, and north to around Manisa, which is generally considered to be its northern limit. Average temperatures range between 17–20 °C (63–68 °F); winters have means around 7–10 °C (45–50 °F), while summers have mean temperatures between 26–29 °C (79–84 °F). Precipitation amounts to around 600–1,200 millimetres (24–47 in), all of it rain. Summers get almost no rain, while winters receive plentiful, and sometimes copious amounts of it. Winter precipitation depends on local topography, with enclosed bays of convergent air,[citation needed] such as Antalya, getting almost twice the amount of rain as storm-protected areas such as Mersin.
Mountains around the region still show the Mediterranean rainfall pattern, but have mild summers and below-freezing temperatures during winter, creating a zone which may be termed oro-Mediterranean.
A pre-Mediterranean climate (Turkish: Akdeniz sâhil ardı iklimi, Köppen: Csa, Trewartha: Cs/Do/Dc) exists in relatively continental areas influenced by the Mediterranean climatic system, notably around the inner Aegean and Southeastern Anatolia. Average temperatures range between 14–18 °C (57–64 °F) with winter means around 1–6 °C (34–43 °F), and summers as hot as (or hotter than) the Mediterranean. Rainfall follows the general pattern of the Mediterranean region, but sunshine is sometimes noticeably lower, and precipitation amounts are lower than the Mediterranean region, between 400–800 millimetres (16–31 in). Snow can also fall in this area, unlike the coastal Mediterranean region.
The climate around the Marmara Sea (Turkish: Marmara geçiş iklimi, lit. 'Marmara transitional climate', Köppen: Csa/Csb/Cfa/Cfb, Trewartha: Cs/Cf/Do) is complex, transitional and often microclimatic. It wraps around the sea, covering Bursa, Bilecik, southern İzmit and İstanbul, as well as Tekirdağ. Often of a meso- or supra-Mediterranean quality at sea-level; its vegetation at sea level is similar to the lower mountains of the "true" Mediterranean region, with heat-tolerant broadleaf oaks and occasional mesophilous trees, such as beech. Therefore, it is generally considered mild-temperate and not subtropical in Turkish sources and furthermore, Bohn, in a survey of European vegetation and climate, calls the climate sub-continental sub-Mediterranean.