Teke yöresinin iklimi
Başlık çevirisi mevcut değil.
- Tez No: 20899
- Danışmanlar: PROF.DR. AYHAN SÜR
- Tez Türü: Yüksek Lisans
- Konular: Meteoroloji, Meteorology
- Anahtar Kelimeler: Belirtilmemiş.
- Yıl: 1992
- Dil: Türkçe
- Üniversite: Ankara Üniversitesi
- Enstitü: Sosyal Bilimler Enstitüsü
- Ana Bilim Dalı: Belirtilmemiş.
- Bilim Dalı: Belirtilmemiş.
- Sayfa Sayısı: 194
Özet
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Özet (Çeviri)
VI - SÜMMARY The typieal Med'iterranean C'lirnate wh1ch 1s very höt and d r y in s u inme P, and coo'l and r a in y in winter, prevails a 'l“! long t h© coast between Antalya and Fethiye wh1ch are both affected by the sea arıd in the val'leys of Esen, Demre, Karasu rivulats in Teke side of Antalya sectlon of iviediterranean Regı”on. in thls arsa, mean annlua'l tempsrature does not fail be“Iow 18.0 ”C. Ternperature in January is above 9,0“C and tenıperature in Ju'ly, the hottest month, 1s 2”f-28“C. Although the Medlter-ranean Climate 1:-s fe'lt in the area whîeh Is pörtlaTly ör comp'tete'ly f o r away f rom the effect of the sea, in su'mrner it is not; as very höt and dry &$ in the coast and in the w1nter,ifc is mosfcly snowy rather than rainy. Here the morphographic properties of this area shou'ld be high ”lighted t:or this difference between the coast and the in'land. Auturnn is generally the second hottest season in Teke Side. Spring is coo'ler because the rainfaTI period most'ly“tosts till April, which causess the teınperature to decrease, The frostly days in the coast can on ”l y be seen on“l y önce ör twince in Decernber and Janusry. But, in the ini and the nurrıber ol”days on whfch the temperature is below Ü.O°C -fs above 50 in the sföcond hal f of auturnn and in spring period. Here the ma in facrcor is topographic character it ics and continental ity. : d.''J Topographic characteristics and i the directions andc ha r a et eri t i es of a ir ma s s as a re t ha rrıaln two f aç t ör s affecting the d ist r 1 bu t i on of plesure and wind diraction and speed. Topography, air mas s es,exposure ete, a re var y Irnportant in the d îss'eribution of rainfall amount and type. For exatnple t the depressions eonıing f r örn AntcVIya and Kerner rnake ralnfall above the near mountains. But: in the c en t. r es suç h as Finike, Fethiye, Kas ete. The depresslons rrıake rnuch rainfall 1n the mauntains because of the continous extension of mauntainous area. in terrns of rainfall arnount and type, there Is di ff©rence between the coastal and maunfcainous area, and the inland. in rnauntainous area, the rainfall arnount Is above ISOOnım. However, thö rainfall amount; deoreases to 400~600rnnı and cont inental i ty is partially f el t since the rncinner that the rnountains extend obstructs the mow©ment: of depressions. Searching f ör rainfoll ef f ect i venasss by rneans of the f o r rn u "l a s o f E r' i n c, D e M a r t o n n e and T h o r n t h w a i t e, it can be seen that there is hurnid clirnate in the coast eand qu
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