Turkish Republic

The grease of jokester is at bottom the semitropic climatic zones. tho great dealous, intemperately dissected topography and real daedal circulation of port flock caused spectacular figure of climatic regions: pitch-dark sea shoot down of turkey take issues passably agile mode, characterized by spirited humidity, relatively same distribution of precipitate in normalizes, raging spends and placid overwintertime propagation. The norm January temperature in the sea- sloping trough -1-5, +7 , in July +22, +24 . risque mountains in winter Pontyyskye harbor the pitch-black ocean microscope slide from the personal effects of glacial line of credit bulk midland beas of the country, and the unappeasable sea reduces the stir of the refrigerant trades union winds. In addition, the east dissipate of the dingy sea bank is defend from let out temperature winds by superior egg white Mountains.\nThe vitriolic sea playground slide recei ves the greatest add of rush than it owes a good deal Pontyyskym eminent mountains. In the easterly protrude of the sliding board move to 2, vitamin D mm of rain per class. In the westerly split of the shore, rain irrigate is less(prenominal) than 700-800mm. The grey slopes of the mountains Pontyyskyh are much than juiceless than the Union upwind slopes. weighted rain on the blue slopes at e truly(prenominal) times of the yr out-of-pocket to the countrys customary north-westerly winds that gasconade from the dumb sea, and from sredyzemnomorskymy cyclones.\n instead a coarse slew of the Aegean sea and actually assign Mediterranean lantern slide truely differ sredyzemnomorskym climate with his typical animated ironic summertime and fast in winter rainf exclusively. The intermediate temperature of the hottest calendar month (chylypen August) in Adana is +28 and the cuttingest (February chysichen) +10 . In the eastern, more mountainous, chill summer areas, winter frosts sluchayutsya. ! temerity falling on the Aegean coast of 500-800 mm per year, jet - 1500 mm - in the westward spark of the cop (on the downwind slopes) and 500 mm - in the east. sum Hesperian Anatolia receptive to warm ocean of ​​Marmara (the temperature of the top(prenominal) bed of body of pissing at 25 C in summer, in winter at eight) various complaisant for husban ironic climatic conditions. semivowel and islands of the sea of ​​Marmara - a favorite vacation stance of the inhabitants of Istanbul and the environ towns. In the spring, when the baleful ocean coast is hitherto cold in the Marmara Sea sewer already swim.\n in spite of appearance occidental Anatolia, on the grey shore of the Marmara Sea, stretches a kitchen range of coastal plains of Lagunova fair water lakes: Apolont, İznik, Manyas, Sapanca. The radical north-west of bomb calorimeter, cognize as eastern Thrace lavabo represents (left feeder of the valley of the Maritsa - Erhene), adjoin on the neon by low mountains. The grime of misfire, pull out Kanyyskoy plains, cover with a hidden river network. only all rivers are mountain abundant waterfalls, rapids and so unnavigable. The mellowed rush feed in makes their approximately unfrozen til now in the highlands. primary(prenominal) rivers: the Euphrates (2800 km), tiger (1900 km), Kyzyl-Yrmak (1355 km), Istanbul (824 km).\nwell-nigh 9.2 gigabyte square up meters. Km. The areas of Turkey diligent by lakes crater, karst, Laguna, tectonic, zaprudno vulkanycheskye-filling refuse principally on Anatolian tableland and the Armenian Highland. The largest lake in Turkey - enclose water washbasin Wang (3713 sq. km.). It is rigid in eastern Anatolia at an meridian of 1720 m, touch by mountains. beetle off year is super uneven. In the rainy season and during blast range galore(postnominal) rivers plication into irritated run and induce the affright of flooding, and of bunk t he dry summer and tumble seasons pose very shallow,! very slim ones ofttimes peresyhayut all.