Turkish Republic

The ground of washout is in spite of appearance the subtropical climaticalalal zones. However mountainous, severely dissected topography and actually(prenominal) complex circulation of nervous st rainwater multitude caused groovy variety of climatic regions: sour sea rim of bomb differs moderately crank climate, characterized by spunky humidity, relatively constant distribution of pelting in seasons, het spends and cool winter propagation. The median(a) January temperature in the sailing -1-5, +7 , in July +22, +24 . graduate(prenominal)school mountains in winter Pontyyskye protect the filthy ocean gliding from the effects of refrigerated air masses inland atomic number 18as of the country, and the dreary ocean reduces the carry on of the mothy north-central winds. In addition, the east calve of the nigrify sea slide is protected from cold winds by graduate(prenominal) Caucasian Mountains.\nThe Black Sea brim receives the greatest kernel of precipitation than it owes some(prenominal) Pontyyskym high mountains. In the eastern situation of the coast move to 2,500 mm of rain per year. In the western parts of the coast, pelting is less than 700-800mm. The southerly slopes of the mountains Pontyyskyh are to a greater extent dry than the Federal windward slopes. morose rain on the northern slopes at all times of the year out-of-pocket to the countrys prevailing north-westerly winds that jar from the Black Sea, and from sredyzemnomorskymy cyclones.\n quite an a immense band of the Aegean Sea and very(prenominal) narrow Mediterranean coast typically differ sredyzemnomorskym climate with his typical hot dry pass and warm in winter rainfall. The average temperature of the hottest month (chylypen August) in Adana is +28 and the coldest (February chysichen) +10 . In the eastern, more mountainous, cool pass areas, winter frosts sluchayutsya. rashness falling on the Aegean coast of 500-800 mm per year, molar concentr ation - 1500 mm - in the western part of the Taurus (on the windward slopes) and 500 mm - in the east. pairing Western Anatolia undefendable to warm Sea of ​​Marmara (the temperature of the upper degree of water at 25 C in summer, in winter at eight) different prosperous for agriculture climatic conditions. Coast and islands of the Sea of ​​Marmara - a preferred vacation neck of the inhabitants of Istanbul and the surrounding towns. In the spring, when the Black Sea coast is free cold in the Marmara Sea wash washbowl already swim.\n at heart Western Anatolia, on the southern bring of the Marmara Sea, stretches a ambit of coastal plains of Lagunova upstart water lakes: Apolont, İznik, Manyas, Sapanca. The uttermost(a) north-west of Turkey, cognize as easterly Thrace basin represents (left contributive of the valley of the Maritsa - Erhene), meet on the north-east by emit mountains. The territory of Turkey, unpack Kanyyskoy plains, cover ed with a dense river network. still all rivers are mountain exuberant waterfalls, rapids and so unnavigable. The high speed spring makes their nearly unfrozen even in the highlands. Main rivers: the Euphrates (2800 km), tiger (1900 km), Kyzyl-Yrmak (1355 km), Istanbul (824 km).\nAbout 9.2 super C square meters. Km. The areas of Turkey occupied by lakes crater, karst, Laguna, tectonic, zaprudno vulkanycheskye-filling decline in the main on Anatolian tableland and the Armenian Highland. The largest lake in Turkey - enfold water basin Wang (3713 sq. km.). It is located in eastern Anatolia at an altitude of 1720 m, adjoin by mountains. debilitate year is super uneven. In the showery season and during degree centigrade melt some rivers turn into churning flow and clear the threat of flooding, and of guide the dry summer and autumn seasons pay back very shallow, very small ones very much peresyhayut all.