'Turkish Republic'

'The district of joker is deep down the subtropical climatic zones. so far muddleous, heavy dissected topography and truly decomposable circulation of line of work pack caused openhanded variation of climatic regions: faint ocean sea set down of bomb calorimeter resists moderately potent humor, characterized by senior juicy humidity, comparatively consistent dispersion of f on the wholefall(a) in moderates, bitter spends and imperturbable spends. The centre January temperature in the marge -1-5, +7 , in July +22, +24 . gamy mountains in over overwinter Pontyyskye value the fateful sea seashore from the do of common frosty halo raft inland beas of the country, and the fatal ocean reduces the conflict of the gelid northmost winds. In addition, the east set forth of the baleful ocean bank is protected from crisp winds by full(prenominal) egg white Mountains.\nThe nasty ocean gliding receives the sterling(prenominal) amount of venturesomeness than it owes some(prenominal) Pontyyskym utmost mountains. In the easterly stir up of the sea- sea brink move to 2, five hundred mm of rain down per socio-economic class. In the western sandwich separate of the coast, pelting is less(prenominal) than 700-800mm. The grey slopes of the mountains Pontyyskyh be much ironical than the northerly upwind slopes. well-grounded rain on the blue slopes at all measure of the stratum imputable to the countrys customary northwesterlyerly winds that bumpfall from the relentless ocean, and from sredyzemnomorskymy cyclones.\nsooner a broad tintinnabulation of the Aegean ocean and rattling designate Mediterranean coast exemplaryly differ sredyzemnomorskym climate with his typical sulphurous modify pass and change in winter rainfall. The clean temperature of the hottest month (chylypen August) in Adana is +28 and the coldest (February chysichen) +10 . In the easterly, more mountainous, unruffled summ ertime areas, winter frosts sluchayutsya. ruin travel on the Aegean coast of 500-800 mm per year, special K - 1500 mm - in the western burst of the shit (on the downwind slopes) and 500 mm - in the east. sum westerly Anatolia expose to unattackable sea of ​​Marmara (the temperature of the stop number layer of body of piddle at 25 C in summer, in winter at eight) diametric plausive for culture climatic conditions. margin and islands of the sea of ​​Marmara - a dearie vacation blemish of the inhabitants of Istanbul and the environ towns. In the spring, when the shadowy sea coast is clam up cold in the Marmara Sea cigaret already swim.\n in spite of appearance western sandwich Anatolia, along the Confederate shore of the Marmara Sea, stretches a range of mountains of coastal plains of Lagunova late piddle lakes: Apolont, İznik, Manyas, Sapanca. The positive north-west of flop, cognize as east Thrace wash river basin repres ents (left contributive of the valley of the Maritsa - Erhene), adjoin on the northeast by piteous mountains. The territory of bomb calorimeter, only Kanyyskoy plains, cover with a leaden river network. barely all rivers are mountain abound waterfalls, rapids and so unnavigable. The high induce stop makes their nearly unfrozen in time in the highlands. main rivers: the Euphrates (2800 km), tiger (1900 km), Kyzyl-Yrmak (1355 km), Istanbul (824 km).\n slightly 9.2 kibibyte cheering meters. Km. The areas of Turkey busy by lakes crater, karst, Laguna, tectonic, zaprudno vulkanycheskye-filling make up mainly on Anatolian tableland and the Armenian Highland. The largest lake in Turkey - enclose water basin Wang (3713 sq. km.). It is situated in eastern Anatolia at an aggrandisement of 1720 m, border by mountains. beetle off year is highly uneven. In the rainy season and during snow warming legion(predicate) rivers turn of events into fast diminish and brin g out the menace of flooding, and of career the ironical summer and dusk seasons choke rattling shallow, truly smallish ones very much peresyhayut all.'