T\u00dcRK\u0130YE \u0130KL\u0130M\u0130
\nT\u00fcrkiye, genelde Akdeniz ikliminin etkisi alt\u0131ndad\u0131r. Ancak bununla beraber, birbirlerinden belirgin farklarla ayr\u0131labilen karasal ve Karadeniz iklimleri de etkili olmaktad\u0131r.
\nT\u00fcrkiye \u0130kliminde Etkili Fakt\u00f6rler
\nMatematik Konumu
\nT\u00fcrkiye konumu itibariyle g\u00fcne\u015f \u0131\u015f\u0131nlar\u0131n\u0131n dik geldi\u011fi alan\u0131n d\u0131\u015f\u0131ndad\u0131r. G\u00fcne\u015f \u0131\u015f\u0131nlar\u0131n\u0131n d\u00fc\u015fme a\u00e7\u0131s\u0131nda y\u0131l boyunca b\u00fcy\u00fck farklar vard\u0131r. Bunun sonucu olarak T\u00fcrkiye iklimlerinde y\u0131ll\u0131k s\u0131cakl\u0131k farklar\u0131 fazlad\u0131r. D\u00f6rt mevsim belirgin olarak ya\u015fan\u0131r.
\nT\u00fcrkiye bulundu\u011fu konumdan farkl\u0131 hava k\u00fctlelerinin kar\u015f\u0131la\u015ft\u0131\u011f\u0131 yerde bulunmaktad\u0131r. Bu sebeple k\u0131\u015f\u0131n g\u00f6r\u00fclen ya\u011f\u0131\u015flar genelde cephesel ya\u011f\u0131\u015f \u015feklindedir.
\nK\u0131y\u0131lar\u0131m\u0131zda s\u0131cakl\u0131k g\u00fcneyden kuzeye do\u011fru azal\u0131r.
\n Yer \u015fekilleri (Y\u00fckselti ,da\u011flar\u0131n uzan\u0131\u015f do\u011frultusu ve bak\u0131)
\nT\u00fcrkiye\u2019de yer \u015fekillerinin \u00e7e\u015fitlilik g\u00f6stermesinden dolay\u0131 k\u0131sa mesafede iklim de\u011fi\u015fimi fazlad\u0131r ve ayn\u0131 tarihlerde farkl\u0131 mevsim \u00f6zellikleri ya\u015fanabilmektedir
\nYurdumuzun kuzeyinde ve g\u00fcneyinde da\u011flar k\u0131y\u0131ya paralel uzand\u0131\u011f\u0131ndan k\u0131y\u0131 ile i\u00e7 kesim aras\u0131nda buralarda iklim farkl\u0131l\u0131\u011f\u0131 fazlad\u0131r. Ege B\u00f6lgesi\u2019nde ise da\u011flar k\u0131y\u0131ya dik uzand\u0131\u011f\u0131ndan farkl\u0131l\u0131k daha azd\u0131r. Da\u011flar\u0131n k\u0131y\u0131ya paralel uzand\u0131\u011f\u0131 yerler daha fazla ya\u011f\u0131\u015f al\u0131r. \u00d6rnek, Karadeniz ve Akdeniz k\u0131y\u0131lar\u0131 Ege k\u0131y\u0131lar\u0131ndan daha fazla ya\u011f\u0131\u015f al\u0131r.
\nY\u00fckseltinin etkisiyle s\u0131cakl\u0131k T\u00fcrkiye\u2019de bat\u0131dan do\u011fuya do\u011fru azal\u0131r. ayr\u0131ca y\u00fcksek yerler \u00e7evresine g\u00f6re daha fazla ya\u011f\u0131\u015f al\u0131rken, \u00e7ukur yerler az ya\u011f\u0131\u015f al\u0131r. \u00d6rnek, Do\u011fu Anadolu B\u00f6lgesi \u0130\u00e7 Anadolu B\u00f6lgesi’nden daha fazla ya\u011f\u0131\u015f almaktad\u0131r. Do\u011fu Anadolu’da \u00e7evresine g\u00f6re \u00e7ukurda yer alan I\u011fd\u0131r \u00e7ok az ya\u011f\u0131\u015f almaktad\u0131r.
\nBak\u0131 etkisinden dolay\u0131 da\u011flar\u0131m\u0131z\u0131n g\u00fcneye bakan yama\u00e7lar\u0131 b\u00fct\u00fcn y\u0131l kuzey yama\u00e7lar\u0131na g\u00f6re daha s\u0131cakt\u0131r.
\n Denize g\u00f6re konum
\nK\u0131y\u0131 b\u00f6lgelerde nem fazla oldu\u011funda buralarda hava ge\u00e7 \u0131s\u0131n\u0131r, ge\u00e7 so\u011fur. S\u0131cakl\u0131k farklar\u0131 azd\u0131r. K\u0131\u015flar \u0131l\u0131k ve ya\u011f\u0131\u015flar fazlad\u0131r. \u0130\u00e7 kesimlerde ise nem az oldu\u011fundan hava \u00e7abuk \u0131s\u0131n\u0131r, \u00e7abuk so\u011fur. S\u0131cakl\u0131k farklar\u0131 fazla olur. K\u0131\u015flar so\u011fuk ve kar ya\u011f\u0131\u015fl\u0131d\u0131r ve ya\u011f\u0131\u015f miktar\u0131 azd\u0131r.
\nR\u00fczgarlar\u0131n esme y\u00f6n\u00fc
\nT\u00fcrkiye\u2019ye kuzeyden gelen r\u00fczgarlar s\u0131cakl\u0131\u011f\u0131 d\u00fc\u015f\u00fcr\u00fcrken, g\u00fcneyden gelenler s\u0131cakl\u0131\u011f\u0131 art\u0131r\u0131r (enlem etkisinden dolay\u0131).
\nBas\u0131n\u00e7 merkezleri
\nT\u00fcrkiye etraf\u0131nda olu\u015fan bas\u0131n\u00e7 merkezleri de r\u00fczgar ve ya\u011f\u0131\u015f rejimi \u00fczerinde etkili olmaktad\u0131r.
\n Yaz mevsiminde Atlas Okyanusu \u00fczerinde olu\u015fup geni\u015fleyen y\u00fcksek bas\u0131n\u00e7 ve Basra K\u00f6rfezi \u00fczerinde olu\u015fan al\u00e7ak bas\u0131n\u00e7 etkisi alt\u0131na girer.
\nK\u0131\u015f mevsiminde ise, kuzeyden gelen so\u011fuk hava, Akdeniz \u00fczerinden gelen \u0131l\u0131k ve nemli havan\u0131n etkisine girmektedir. Bu iki hava k\u00fctlesinin kar\u015f\u0131la\u015fmas\u0131 ile cepheler olu\u015fmakta ve k\u0131y\u0131larda \u00e7o\u011funlukla ya\u011fmur, Trakya, i\u00e7 ve y\u00fcksek kesimlerde kar ya\u011f\u0131\u015f\u0131na neden olmaktad\u0131r.
\n T\u00dcRK\u0130YE’DE \u0130KL\u0130M ELEMANLARI
\nSICAKLIK T\u00fcrkiye’de s\u0131cakl\u0131k, k\u0131y\u0131larda enlem fark\u0131na, i\u00e7 kesimlerde ise denizden uzakl\u0131k, y\u00fckselti, yer \u015fekilleri gibi fakt\u00f6rlere ba\u011fl\u0131 olarak de\u011fi\u015fir.
\nS\u0131cakl\u0131\u011f\u0131n da\u011f\u0131l\u0131\u015f\u0131n\u0131 g\u00f6steren haritalara izoterm (E\u015f s\u0131cakl\u0131k) haritalar\u0131 denir.
\nGER\u00c7EK \u0130ZOTERM HAR\u0130TALARI
\nY\u00fckseltinin etkisi dikkate al\u0131narak \u00e7izilen s\u0131cakl\u0131k haritalar\u0131d\u0131r.
\n\u0130ND\u0130RGENM\u0130\u015e \u0130ZOTERM HAR\u0130TALARI
\nHer yer deniz seviyesinde kabul edilir. Y\u00fckseltinin etkisi ortadan kald\u0131r\u0131lm\u0131\u015ft\u0131r. Yani, b\u00fct\u00fcn y\u00fckseltilerin s\u0131cakl\u0131\u011f\u0131 her 200 m de 1 \u00b0C art\u0131r\u0131larak deniz seviyesine indirgenir.
\nS\u0131cakl\u0131\u011f\u0131n farkl\u0131 da\u011f\u0131l\u0131\u015f\u0131nda yer \u015fekillerinin (Y\u00fckselti, e\u011fim, bak\u0131 ve da\u011flar\u0131n uzan\u0131\u015f do\u011frultusu) etkisi ortadan kald\u0131r\u0131larak \u00e7izilir.
\nNOT: Bir yerin ger\u00e7ek s\u0131cakl\u0131\u011f\u0131 ile indirgenmi\u015f s\u0131cakl\u0131\u011f\u0131 aras\u0131nda fark fazla ise o yerin y\u00fckseltisi fazlad\u0131r. Fark az ise y\u00fckselti de azd\u0131r
\nS\u0131cakl\u0131k \u0130le ilgili Problemler
\n\u00d6rnek 1:Bir yerin ger\u00e7ek s\u0131cakl\u0131\u011f\u0131 (-5 \u00b0C) , indirgenmi\u015f s\u0131cakl\u0131\u011f\u0131 ise 17\u00b0C ise bu yerin denizden y\u00fcksekli\u011fi ka\u00e7 metredir?
\nCevap:17- (-5)= 17+5=22 \u00b0C
\n200 m’de 1\u00b0C de\u011fi\u015fti\u011finden, 22×200=4400 metredir.
\n\u00d6rnek 2 : 2900 m’de \u00f6l\u00e7\u00fclen s\u0131cakl\u0131k (-8 \u00b0C) ise bu yerin indirgenmi\u015f s\u0131cakl\u0131\u011f\u0131 ka\u00e7 \u00b0C ‘dir?
\nCevap: 2900 \/ 200 = 14,5 \u00b0C s\u0131cakl\u0131k artacakt\u0131r. Buna g\u00f6re -8 + 14,5 = 6,5\u00b0C
\n\u00d6rnek 3 :1800 m y\u00fckseklikteki bir merkezin indirgenmi\u015f s\u0131cakl\u0131\u011f\u0131 25 \u00b0C ise bu yerin ger\u00e7ek s\u0131cakl\u0131\u011f\u0131 ka\u00e7 \u00b0C olurdu?
\nCevap:1800\/200= 9\u00b0C s\u0131cakl\u0131k azalacakt\u0131r.
\n Buna g\u00f6re, 25-9= 16 \u00b0C ‘dir.
\nY\u0131ll\u0131k Ortalama S\u0131cakl\u0131k Da\u011f\u0131l\u0131\u015f
\nK\u0131y\u0131 kesimlerin s\u0131cakl\u0131k ortalamas\u0131 deniz etkisinden dolay\u0131 i\u00e7 kesimlerden daha y\u00fcksektir.
\nEnlemin etkisiyle s\u0131cakl\u0131k genelde g\u00fcney k\u0131y\u0131lar\u0131m\u0131zdan kuzey k\u0131y\u0131lar\u0131m\u0131za do\u011fru azal\u0131r.
\n T\u00fcrkiye’de g\u00f6zlem yap\u0131lan istasyonlardaki uzun y\u0131llar ortalamalar\u0131na g\u00f6re, y\u0131ll\u0131k ortalama s\u0131cakl\u0131klar 4-20 \u00b0C aras\u0131nda de\u011fi\u015fmektedir.
\n\u00dclkenin en s\u0131cak kesimleri G\u00fcneydo\u011fu Anadolu’nun g\u00fcneyi ile Akdeniz k\u0131y\u0131 ku\u015fa\u011f\u0131d\u0131r. Buralarda y\u0131ll\u0131k ortalama s\u0131cakl\u0131k 16 \u00b0C’nin \u00fczerindedir.
\n Erzurum ve Kars platolar\u0131n\u0131n y\u00fcksek kesimlerinde 4 \u00b0C nin alt\u0131na d\u00fc\u015fer. Sebepleri : Y\u00fckseltisinin fazla olmas\u0131, karasall\u0131kt\u0131r.
\n 2. Ocak Ay\u0131 Ortalama S\u0131cakl\u0131k Da\u011f\u0131l\u0131\u015f\u0131
\nEn y\u00fcksek s\u0131cakl\u0131klar Akdeniz b\u00f6lgesinin k\u0131y\u0131 kesiminde g\u00f6r\u00fcl\u00fcr. Sebepleri : Enlem , deniz etkisi ve Toros k\u0131vr\u0131m da\u011flar\u0131n\u0131n kuzeyden gelen so\u011fuk hava k\u00fctlelerini engellemesidir.
\nEn d\u00fc\u015f\u00fck s\u0131cakl\u0131klar Do\u011fu Anadolu\u2019da Erzurum-Kars b\u00f6l\u00fcm\u00fcnde g\u00f6r\u00fcl\u00fcr. Sebepleri : Y\u00fckseltinin fazla olmas\u0131, karasall\u0131k ,kuzeyden gelen so\u011fuk r\u00fczgarlard\u0131r.
\nK\u0131y\u0131 ile i\u00e7 kesim aras\u0131ndaki s\u0131cakl\u0131k fark\u0131 fazlad\u0131r.
\n 3. T\u00fcrkiye Temmuz Ay\u0131 S\u0131cakl\u0131k Da\u011f\u0131l\u0131\u015f\u0131
\nK\u0131y\u0131 ile i\u00e7 kesim aras\u0131nda s\u0131cakl\u0131k fark\u0131 azalm\u0131\u015ft\u0131r.
\nEn y\u00fcksek s\u0131cakl\u0131klar G\u00fcney Do\u011fu Anadolu\u2019da g\u00f6r\u00fcl\u00fcr. Sebepleri : Karasall\u0131k ve G\u00fcneyden gelen s\u0131cak r\u00fczgarlar\u0131n etkisidir.
\nEn d\u00fc\u015f\u00fck s\u0131cakl\u0131klar bu d\u00f6nemde de Erzurum-Kars B\u00f6l\u00fcm\u00fcnde g\u00f6r\u00fcl\u00fcr. Sebebi ,y\u00fckseltisinin fazla olmas\u0131d\u0131r.
\n BASIN\u00c7LAR
\nT\u00fcrkiye’de mevsimlere, yerel \u0131s\u0131nma farklar\u0131na , deniz ve karalara ba\u011fl\u0131 olarak olu\u015fan bas\u0131n\u00e7 merkezlerinin yan\u0131 s\u0131ra, T\u00fcrkiye’nin d\u0131\u015f\u0131nda olu\u015fan ve T\u00fcrkiye’yi etkisine alan gezici bas\u0131n\u00e7 merkezleri de bulunmaktad\u0131r.
\nT\u00fcrkiye’yi en \u00e7ok etkileyen bas\u0131n\u00e7 merkezleri \u015funlard\u0131r:
\n Y\u00dcKSEK BASIN\u00c7LAR
\nSibirya Termik Y.B
\n60\u00b0 enlemlerinde so\u011fuma ile olu\u015fmu\u015ftur. T\u00fcrkiye\u2019de k\u0131\u015f\u0131n etkilidir. Etkili oldu\u011fu d\u00f6nemlerde k\u0131\u015flar \u00e7ok so\u011fuk ve kar ya\u011f\u0131\u015fl\u0131 ge\u00e7er. T\u00fcrkiye\u2019ye Kuzeydo\u011fudan sokulur.
\n Asor Dinamik Y.B :
\n30\u00b0 enlemlerinden kayna\u011f\u0131n\u0131 al\u0131r. T\u00fcrkiye\u2019de b\u00fct\u00fcn y\u0131l etkilidir. En fazla yaz\u0131n etkilidir. Etkili oldu\u011fu yaz mevsiminin kurak olmas\u0131n\u0131n ba\u015fl\u0131ca sebebidir (Al\u00e7al\u0131c\u0131 hava hareketinden dolay\u0131).
\n K\u0131\u015f mevsiminde Sibirya Y.B ile birle\u015ferek T\u00fcrkiye \u00fczerinde etkili oldu\u011funda \u0130zlanda A.B T\u00fcrkiye’ye sokulamaz. Bunun sonucunda da \u00fclkemizde k\u0131\u015flar so\u011fuk, sert ve kar ya\u011f\u0131\u015fl\u0131 ge\u00e7er.
\n \u0130zlanda Dinamik A.B
\n60\u00b0 enleminde kayna\u011f\u0131n\u0131 al\u0131r. T\u00fcrkiye\u2019de b\u00fct\u00fcn y\u0131l etkilidir. Ancak en fazla k\u0131\u015f\u0131n etkilidir. Etkili oldu\u011fu d\u00f6nemde k\u0131\u015flar \u0131l\u0131k ve ya\u011f\u0131\u015fl\u0131 ge\u00e7er. Kuzeybat\u0131dan sokulur.
\n Basra Termik A.B
\nBasra K\u00f6rfezi \u00e7evresinin a\u015f\u0131r\u0131 \u0131s\u0131nmas\u0131yla olu\u015fur. T\u00fcrkiye\u2019de yaz\u0131n ekilidir. Samyeli r\u00fczgarlar\u0131 vas\u0131tas\u0131yla Akdeniz ve G\u00fcneydo\u011fu Anadolu b\u00f6lgelerinde etkili olur. 30\u00b0 Kuzey enlemi \u00e7evresinde olu\u015fmas\u0131na ra\u011fmen, \u0131s\u0131nmadan dolay\u0131 termik k\u00f6kenlidir .
\n R\u00dcZGARLAR
\nT\u00fcrkiye bat\u0131 r\u00fczgarlar\u0131 ku\u015fa\u011f\u0131nda olmas\u0131na ra\u011fmen daha \u00e7ok yerel r\u00fczgarlar\u0131n etkisindedir. Sebebi yer \u015fekilleridir.
\n R\u00fczgar frekans g\u00fcl\u00fcnde g\u00f6sterilen r\u00fczgarlar haricinde yaz mevsiminde Ege k\u0131y\u0131lar\u0131nda deniz meltemi olan imbat r\u00fczgar\u0131 etkilidir. Ege Denizi’nde, yaz\u0131n kuzeyden poyraz benzeri r\u00fczgarlar eserler. Bu r\u00fczgarlara etezyen denilmektedir.
\nAyr\u0131ca , \u00f6zellikle Karadeniz ve Akdeniz B\u00f6lgelerinde F\u00f6hn r\u00fczgar\u0131 da etkilidir. <\/p>\n
NEML\u0130L\u0130K VE YA\u011eI\u015e
\nK\u0131y\u0131 b\u00f6lgelerinin nemlili\u011fi i\u00e7 kesimlerden daha y\u00fcksektir. Bundan dolay\u0131 k\u0131y\u0131 kesimlerde ya\u011f\u0131\u015flar fazla ve s\u0131cakl\u0131k farklar\u0131 azd\u0131r.
\nBa\u011f\u0131l (nispi) nem en y\u00fcksek Do\u011fu Karadeniz B\u00f6l\u00fcm\u00fcndedir. En d\u00fc\u015f\u00fck G\u00fcney Do\u011fu Anadolu\u2019dad\u0131r. G\u00fcney Do\u011fu Anadolu\u2019da ba\u011f\u0131l(nispi) nem %40-%50, Karadeniz B\u00f6lgesinde ise %70-%80 civar\u0131ndad\u0131r.
\n T\u00fcrkiye\u2019de bulut kapal\u0131l\u0131\u011f\u0131 kuzeyde fazla, g\u00fcneyde azd\u0131r. Do\u011fu Karadeniz\u2019de kapal\u0131l\u0131\u011f\u0131n y\u00fcksek olmas\u0131 ile ya\u011f\u0131\u015flar aras\u0131nda do\u011fru bir orant\u0131 vard\u0131r.
\n G\u00fcne\u015flenme s\u00fcresi bulut kapal\u0131l\u0131\u011f\u0131 ile ters orant\u0131l\u0131d\u0131r. G\u00fcneydo\u011fu Anadolu ve Akdeniz B\u00f6lgelerinde g\u00fcne\u015flenme s\u00fcresi daha fazlad\u0131r.
\n Karasal iklim b\u00f6lgelerinde k\u0131\u015f\u0131n g\u00f6r\u00fclen ya\u011f\u0131\u015flar genellikle kar \u015feklindedir. T\u00fcrkiye\u2019de karla \u00f6rt\u00fcl\u00fc g\u00fcn say\u0131s\u0131n\u0131n en fazla oldu\u011fu b\u00f6lge Do\u011fu Anadolu B\u00f6lgesidir.
\nT\u00fcrkiye\u2019de kar \u00f6rt\u00fclerinin yerde kalma s\u00fcresi bat\u0131dan do\u011fuya do\u011fru artar. Kar ya\u011f\u0131\u015f\u0131 ve don olay\u0131n\u0131n en az g\u00f6r\u00fcld\u00fc\u011f\u00fc b\u00f6lgemiz Akdeniz B\u00f6lgesidir.
\nYA\u011eI\u015e OLU\u015eUM \u015eEK\u0130LLER\u0130
\nORO\u011eRAF\u0130K (YAMA\u00c7) YA\u011eI\u015eLARI <\/p>\n
Yer \u015fekillerinin etkisiyle olu\u015furlar. Nemli hava k\u00fctlesinin bir da\u011f yamac\u0131na \u00e7arparak y\u00fckselmesi ve so\u011fumas\u0131 sonucu olu\u015furlar. T\u00fcrkiye\u2019de en fazla Karadeniz B\u00f6lgesi’nde g\u00f6r\u00fcl\u00fcr.
\n Hava k\u00fctleleri yama\u00e7 boyunca y\u00fckselirken en fazla ya\u011f\u0131\u015f\u0131 500 – 1000 m y\u00fckseltiler aras\u0131na b\u0131rak\u0131rlar. Y\u00fckselti artt\u0131k\u00e7a (1000 m\u2019lerden sonra) mutlak nem azald\u0131\u011f\u0131 i\u00e7in ya\u011f\u0131\u015f da azal\u0131r.
\nKONVEKS\u0130YON (Y\u00dcKSEL\u0130M, KIRK\u0130K\u0130ND\u0130) YA\u011eI\u015eLARI <\/p>\n
Is\u0131nan havan\u0131n y\u00fckselerek so\u011fumas\u0131 sonucu olu\u015furlar. T\u00fcrkiye genelinde s\u0131cak d\u00f6nemlerde g\u00f6r\u00fclen ya\u011f\u0131\u015flar bu \u015fekildedir. En fazla \u0130\u00e7 Anadolu ve Do\u011fu Anadolu B\u00f6lgelerinde g\u00f6r\u00fcl\u00fcr. Bu ya\u011f\u0131\u015flara halk aras\u0131nda K\u0131rkikindi ya\u011f\u0131\u015flar\u0131 denir.
\nCEPHESEL (FRONTAL )YA\u011eI\u015eLAR <\/p>\n
S\u0131cak ve so\u011fuk hava k\u00fctlelerinin kar\u015f\u0131la\u015fma alanlar\u0131nda meydana gelen ya\u011f\u0131\u015flard\u0131r.
\nSadece Orta ku\u015fakta \u00fclkelerinde k\u0131\u015f\u0131n g\u00f6r\u00fcl\u00fcr. T\u00fcrkiye’de, \u00f6zellikle k\u0131\u015f mevsiminde g\u00f6r\u00fclen ya\u011f\u0131\u015flar\u0131n \u00e7o\u011fu cephesel k\u00f6kenlidir. En fazla Akdeniz B\u00f6lgesinde g\u00f6r\u00fcl\u00fcr. <\/p>\n
T\u00fcrkiye’de ya\u011f\u0131\u015f\u0131n da\u011f\u0131l\u0131\u015f\u0131n\u0131 inceledi\u011fimizde \u015fu \u00f6zellikler g\u00f6r\u00fcl\u00fcr:
\nT\u00fcrkiye’de ya\u011f\u0131\u015f da\u011f\u0131l\u0131\u015f\u0131 haritas\u0131 ile yer \u015fekilleri haritas\u0131 kar\u015f\u0131la\u015ft\u0131r\u0131ld\u0131\u011f\u0131nda, aralar\u0131nda yak\u0131n ilgi bulundu\u011fu tespit edilmektedir.
\n T\u00fcrkiye’de fazla ya\u011f\u0131\u015f alan yerler (800 mm. den fazla)
\nDo\u011fu ve Bat\u0131 Karadeniz b\u00f6l\u00fcmleri , Ege\u2019de Mente\u015fe y\u00f6resi, Akdeniz\u2019de Bat\u0131 ve Orta Toroslar, Hatay\u2019da Nur Da\u011flar\u0131 ve G.Do\u011fu Toroslar\u2019da Hakkari \u00e7evresidir. Ayr\u0131ca Do\u011fu ve Bat\u0131 Anadolu\u2019daki baz\u0131 y\u00fcksek da\u011flar.
\nEn fazla ya\u011f\u0131\u015f alan yer Rize \u00e7evresidir. (2400 mm. den fazla) Sebebi;g\u00fcneyindeki y\u00fcksek da\u011flar\u0131n hakim r\u00fczgar y\u00f6n\u00fcne dik olmas\u0131 etkilidir.
\nT\u00fcrkiye’de az ya\u011f\u0131\u015f alan yerler (500 mm\u2019nin alt\u0131nda), \u0130\u00e7 Anadolu, G\u00fcneydo\u011fu Anadolu ve yer yer Do\u011fu Anadolu’nun \u00e7ukur yerleridir. En az ya\u011f\u0131\u015f alan yer, Tuz G\u00f6l\u00fc \u00e7evresi ile I\u011fd\u0131r Ovas\u0131 civar\u0131d\u0131r (250 mm nin alt\u0131nda) .
\n NOT: En az ya\u011f\u0131\u015f alan b\u00f6lge \u0130\u00e7 Anadolu B\u00f6lgesi olmas\u0131na ra\u011fmen en kurak b\u00f6lge G\u00fcney Do\u011fu Anadolu B\u00f6lgesidir. Sebebi ; buharla\u015fman\u0131n fazla olmas\u0131d\u0131r.
\nYa\u011f\u0131\u015f\u0131n mevsimlere da\u011f\u0131l\u0131m\u0131 (ya\u011f\u0131\u015f rejimi) bak\u0131m\u0131ndan b\u00f6lgeler aras\u0131nda \u00f6nemli farkl\u0131l\u0131klar g\u00f6r\u00fcl\u00fcr.<\/p>\n","protected":false},"excerpt":{"rendered":"
T\u00dcRK\u0130YE \u0130KL\u0130M\u0130 T\u00fcrkiye, genelde Akdeniz ikliminin etkisi alt\u0131ndad\u0131r. Ancak bununla beraber, birbirlerinden belirgin farklarla ayr\u0131labilen karasal ve Karadeniz iklimleri de etkili olmaktad\u0131r. T\u00fcrkiye \u0130kliminde Etkili Fakt\u00f6rler Matematik Konumu T\u00fcrkiye konumu itibariyle g\u00fcne\u015f \u0131\u015f\u0131nlar\u0131n\u0131n dik geldi\u011fi alan\u0131n d\u0131\u015f\u0131ndad\u0131r. G\u00fcne\u015f \u0131\u015f\u0131nlar\u0131n\u0131n d\u00fc\u015fme a\u00e7\u0131s\u0131nda y\u0131l boyunca b\u00fcy\u00fck farklar vard\u0131r. Bunun sonucu olarak T\u00fcrkiye iklimlerinde y\u0131ll\u0131k s\u0131cakl\u0131k farklar\u0131 fazlad\u0131r. …<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1403,1406],"tags":[2790,3729,10092,3180,3814],"class_list":["post-4661","post","type-post","status-publish","format-standard","hentry","category-odevler","category-sosyal-bilgiler-odevleri","tag-akdeniz-iklimi","tag-basinc-merkezleri","tag-matematik-konum","tag-turkiye-iklimi","tag-yer-sekilleri"],"_links":{"self":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/4661","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/comments?post=4661"}],"version-history":[{"count":0,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/4661\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/media?parent=4661"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/categories?post=4661"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/tags?post=4661"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}