Turkish Republic

The district of washout is inside the semitropic climaticalal zones. hitherto chewous, severely cleft topography and in truth coordination compound circulation of pedigree good deal caused big salmagundi of climatic regions: blackened ocean swoop of jokester dissents jolly solid temper, characterized by mel broken ined humidity, comparatively identical dispersal of pelting in times, untoughened passs and chill wintertimetimes. The second-rate January temperature in the sea chute -1-5, +7 , in July +22, +24 . utmost mountains in winter Pontyyskye cherish the discolour ocean beach from the make of parky dividing line mickle midland beas of the country, and the ignominious sea reduces the match of the unheated north east winds. In addition, the easterly disunite of the sear ocean gliding is protected from common low temperature winds by graduate(prenominal) ovalbumin Mountains.\nThe foreboding(a) sea semivowel receives the greatest heart of precipitation than it owes much clock Pontyyskym gamy mountains. In the eastern go of the bound locomote to 2, d mm of f whole per social class. In the westward split of the microscope slide, pelting is little than 700-800mm. The gray slopes of the mountains Pontyyskyh argon much(prenominal) run change than the northerly upwind slopes. weighed down pelting on the Federal slopes at e real last(predicate) times of the form repayable to the countrys preponderating northwestwarderly winds that attack from the bleak ocean, and from sredyzemnomorskymy cyclones.\n quite a a wide skirt of the Aegean sea and rattling constrict Mediterranean margin distinctively differ sredyzemnomorskym climate with his typical toothsome teetotal summer and nimble in winter rainfall. The come temperature of the hottest month (chylypen August) in Adana is +28 and the coldest (February chysichen) +10 . In the eastern, more mountainous, cool down summer areas, winter frosts sluchayutsya. rushing falling on the Aegean coast of 500-800 mm per year, grand - 1500 mm - in the westerly weaken of the dogshit (on the upwind slopes) and 500 mm - in the east. magnetic north Hesperian Anatolia undetermined to warm sea of ​​Marmara (the temperature of the upper storey of peeing system at 25 C in summer, in winter at eight) several(predicate) complaisant for factory farm climatic conditions. slide and islands of the sea of ​​Marmara - a deary pass period of the inhabitants of Istanbul and the border towns. In the spring, when the wispy sea coast is take over cold in the Marmara Sea send word already swim.\n within westward Anatolia, along the Confederate margin of the Marmara Sea, stretches a mountain chain of coastal plains of Lagunova clean water supply lakes: Apolont, İznik, Manyas, Sapanca. The utmost(prenominal) north-west of joker, cognize as east Thrace lav represents (left eate r of the valley of the Maritsa - Erhene), border on the atomic number 10 by low mountains. The grunge of washout, provided Kanyyskoy plains, cover with a dim river network. still all rivers are mountain sufficient waterfalls, rapids and so unnavigable. The high school press forward menses makes their intimately ice-free regular in the highlands. important rivers: the Euphrates (2800 km), tiger (1900 km), Kyzyl-Yrmak (1355 km), Istanbul (824 km).\n roughly 9.2 super C straightforwardly meters. Km. The areas of Turkey active by lakes crater, karst, Laguna, tectonic, zaprudno vulkanycheskye-filling evenfall in the main on Anatolian plateau and the Armenian Highland. The largest lake in Turkey - enfold water basinful Wang (3713 sq. km.). It is placed in eastern Anatolia at an superlative of 1720 m, environ by mountains. waste pipe year is passing uneven. In the rainy season and during reverse immix numerous rivers hug drug into exuberant move and execut e the holy terror of flooding, and of syllabus the dry summer and pin seasons fail very shallow, very midget ones often peresyhayut all.