\nT\u00fcrkiye\u2019de genel olarak \u00fc\u00e7 ana iklim tipi g\u00f6r\u00fcl\u00fcr.Bunlar; Karadeniz \u0130klimi, Akdeniz \u0130klimi ve Karasal iklimdir. <\/p>\n
1)KARADEN\u0130Z \u0130KL\u0130M\u0130:Bu iklim as\u0131l olarak Kuzey Anadolu Da\u011flar\u0131n\u0131n Karadeniz\u2019e bakan yama\u00e7lar\u0131nda g\u00f6r\u00fcl\u00fcr. Genel \u00f6zellikleri \u015funlard\u0131r:
\nHer mevsim ya\u011f\u0131\u015fl\u0131d\u0131r.Do\u011fu Karadeniz B\u00f6l\u00fcm\u00fcnde maksimum ya\u011f\u0131\u015f sonbaharda, minimum ya\u011f\u0131\u015f ilkbaharda d\u00fc\u015fer. Y\u0131ll\u0131k ya\u011f\u0131\u015f miktar\u0131 2000-2500 mm\u2019dir.Bat\u0131 Karadeniz B\u00f6l\u00fcm\u00fcnde maksimum ya\u011f\u0131\u015f sonbaharda, minimum ya\u011f\u0131\u015f ilkbaharda d\u00fc\u015fer. Y\u0131ll\u0131k ya\u011f\u0131\u015f miktar\u0131 1000-1500 mm\u2019dir.Orta Karadeniz B\u00f6l\u00fcm\u00fcnde ise maksimum ya\u011f\u0131\u015f k\u0131\u015f\u0131n, minimum ya\u011f\u0131\u015f yaz\u0131n d\u00fc\u015fer. Y\u0131ll\u0131k ya\u011f\u0131\u015f miktar\u0131 700-1000 mm\u2019dir.Karadeniz ikliminin g\u00f6r\u00fcld\u00fc\u011f\u00fc alanlarda kar ya\u011f\u0131\u015fl\u0131 g\u00fcnlerin ortalamas\u0131 18 g\u00fcnd\u00fcr.
\nY\u0131ll\u0131k ortalama s\u0131cakl\u0131k 13-15\u00b0C\u2019dir.
\nOcak ay\u0131 ortalama s\u0131cakl\u0131\u011f\u0131 6-7\u00b0C\u2019dir.
\nTemmuz ay\u0131 ortalama s\u0131cakl\u0131\u011f\u0131 21-23\u00b0C\u2019dir.
\nY\u0131ll\u0131k s\u0131cakl\u0131k fark\u0131 13-15\u00b0C\u2019dir.
\nDo\u011fal bitki \u00f6rt\u00fcs\u00fc ormand\u0131r.Y\u00fcksek alanlarda Alpin \u00e7ay\u0131rlar g\u00f6r\u00fcl\u00fcr.
\n2)AKDEN\u0130Z \u0130KL\u0130M\u0130:Bu iklim tipi \u00fclkemizde en belirgin olarak Akdeniz k\u0131y\u0131lar\u0131nda g\u00f6r\u00fclmekle birlikte, Ege ve Marmara B\u00f6lgelerinde de etkili olmaktad\u0131r. Genel \u00f6zellikleri \u015funlard\u0131r:
\nYazlar s\u0131cak ve kurak, k\u0131\u015flar \u0131l\u0131k ve ya\u011f\u0131\u015fl\u0131d\u0131r.
\nMaksimum ya\u011f\u0131\u015f k\u0131\u015f\u0131n, minimum ya\u011f\u0131\u015f yaz\u0131n d\u00fc\u015fer.
\nYaz ve k\u0131\u015f ya\u011f\u0131\u015flar\u0131 aras\u0131ndaki fark olduk\u00e7a fazlad\u0131r.
\nY\u0131ll\u0131k ya\u011f\u0131\u015f ortalamas\u0131, 600-1000 mm aras\u0131ndad\u0131r.
\nY\u0131ll\u0131k s\u0131cakl\u0131k ortalamas\u0131 18-20\u00b0C\u2019dir.
\nOcak ay\u0131 ortalamas\u0131 8-10\u00b0C\u2019dir.
\nTemmuz ay\u0131 ortalamas\u0131 28-30\u00b0C\u2019dir.
\nY\u0131ll\u0131k s\u0131cakl\u0131k fark\u0131 15-18\u00b0C\u2019dir.
\nEge B\u00f6lgesinde da\u011flar\u0131n k\u0131y\u0131ya dik uzanmas\u0131, Akdeniz \u0130kliminin i\u00e7 kesimlere ula\u015fmas\u0131na olanak sa\u011flam\u0131\u015ft\u0131r.
\nMarmara B\u00f6lgesinde g\u00f6r\u00fclen Akdeniz \u0130kliminde, yazlar Akdeniz k\u0131y\u0131lar\u0131na g\u00f6re daha serin, k\u0131\u015flar ise daha so\u011fuk ve karl\u0131d\u0131r.
\nAkdeniz \u0130kliminin karekteristik bitki \u00f6rt\u00fcs\u00fc zeytin, defne, mersin, kekik gibi bitkilerden olu\u015fan makilerdir.
\n3)KARASAL \u0130KL\u0130M:\u00dclkemizde Karasal \u0130klim, \u0130\u00e7 Anadolu, Do\u011fu Anadolu ve G\u00fcneydo\u011fu Anadolu B\u00f6lgeleri ile \u0130\u00e7 Bat\u0131 Anadolu B\u00f6l\u00fcm\u00fcnde g\u00f6r\u00fcl\u00fcr.Genel \u00f6zellikleri \u015funlard\u0131r:
\nYazlar s\u0131cak ve kurak, k\u0131\u015flar so\u011fuk ve kar ya\u011f\u0131\u015fl\u0131d\u0131r.
\n\u0130\u00e7 Anadolu B\u00f6lgesinde maksimum ya\u011f\u0131\u015f ilkbaharda, minimum ya\u011f\u0131\u015f yaz\u0131n d\u00fc\u015fer.
\n\u0130\u00e7 Anadolu da ortalama ya\u011f\u0131\u015f 300-400 mm\u2019dir.
\n\u0130\u00e7 Anadolu\u2019nun k\u0131\u015f s\u0131cakl\u0131k ortalamas\u0131, 1-2\u00b0C, yaz s\u0131cakl\u0131k ortalamas\u0131, 22-23\u00b0C, y\u0131ll\u0131k s\u0131cakl\u0131k ortalamas\u0131 ise, 10-12\u00b0C\u2019dir.
\nEge B\u00f6lgesinin \u0130\u00e7 bat\u0131 Anadolu B\u00f6l\u00fcm\u00fcnde de ya\u011f\u0131\u015flar k\u0131y\u0131 kesimine g\u00f6re azd\u0131r.
\nDo\u011fu Anadolu B\u00f6lgesinin kuzeydo\u011fu kesiminde y\u0131ll\u0131k s\u0131cakl\u0131k ortalamas\u0131, 4-6\u00b0C\u2019dir.
\nKuzeydo\u011fu Anadolu\u2019da k\u0131\u015f s\u0131cakl\u0131k ortalamas\u0131, -7, -10\u00b0C, yaz s\u0131cakl\u0131k ortalamas\u0131, 17-19\u00b0C\u2019dir.
\nY\u0131ll\u0131k ya\u011f\u0131\u015f miktar\u0131, 500-600 mm\u2019dir.
\nG\u00fcneydo\u011fu Anadolu\u2019da ise ortalama ya\u011f\u0131\u015f, 400-700 mm\u2019dir.
\nG\u00fcneydo\u011fu Anadolu B\u00f6lgesinde k\u0131\u015f mevsimi pek donlu ge\u00e7memekle beraber, yaz mevsiminde \u015fiddetli kuru s\u0131caklar egemendir.
\nG\u00fcneydo\u011fu Anadolu\u2019da y\u0131ll\u0131k ortalama s\u0131cakl\u0131k, 15-16\u00b0C, k\u0131\u015f s\u0131cakl\u0131\u011f\u0131, 3-4\u00b0C, yaz s\u0131cakl\u0131\u011f\u0131 ise, 30-35\u00b0C\u2019dir.<\/p>\n
BASIN\u00c7
\nAtmosferdeki gazlar\u0131n temas ettikleri y\u00fczeylere uygulad\u0131\u011f\u0131 kuvvete hava bas\u0131nc\u0131 denmektedir. Hava s\u0131cakl\u0131\u011f\u0131na ba\u011fl\u0131 olarak yo\u011funluktaki artma ve azalmalar sebebiyle bas\u0131n\u00e7ta de\u011fi\u015fiklikler g\u00f6r\u00fcl\u00fcr. Bunun yan\u0131 s\u0131ra hava bas\u0131nc\u0131, mevsimler, y\u00fckseklik, yer\u00e7ekimi, cephe ve bas\u0131n\u00e7 sistemlerine ba\u011fl\u0131 olarak de\u011fi\u015fmektedir.
\n2)Asor Dinamik Y.B. : 30\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). Bu bas\u0131nc\u0131n etkisiyle Ege K\u0131y\u0131lar\u0131 boyunca kuzeyden esen Etezyen r\u00fczgar\u0131 olu\u015fur. Yurdumuza kuzeybat\u0131dan sokulur. <\/p>\n
AL\u00c7AK BASIN\u00c7LAR
\n1)\u0130zlanda Dinamik A.B. : 60\u00b0 enleminde kayna\u011f\u0131n\u0131 al\u0131r. T\u00fcrkiye\u2019de 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.<\/p>\n
2)Basra Termik A.B.: (30\u00b0 Kuzey) T\u00fcrkiye\u2019de yaz\u0131n ekilidir. Yurdumuza G\u00fcney Do\u011fu Anadolu B\u00f6lgesinden itibaren sokulur ve s\u0131cakl\u0131\u011f\u0131 art\u0131r\u0131r.
\nR\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. Yurdumuza 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. Bu durum s\u0131cakl\u0131\u011f\u0131n da\u011f\u0131l\u0131\u015f\u0131nda enlem etkisine \u00f6rnektir. T\u00fcrkiye\u2019de y\u0131ll\u0131k ortalama ya\u011f\u0131\u015f bak\u0131m\u0131ndan, b\u00f6lgeler aras\u0131nda b\u00fcy\u00fck farkl\u0131l\u0131klar vard\u0131r. Baz\u0131 b\u00f6lgelerde ortalama ya\u011f\u0131\u015f 2500 mm\u2019yi bulurken, baz\u0131 b\u00f6lgelerde 250 mm\u2019nin alt\u0131na inmektedir<\/p>\n
*K\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.
\n*Ba\u011f\u0131l nem en y\u00fcksek Do\u011fu Karadeniz B\u00f6l\u00fcm\u00fcndedir. En d\u00fc\u015f\u00fck G\u00fcney Do\u011fu Anadolu\u2019dad\u0131r.
\n*En fazla ya\u011f\u0131\u015f alan b\u00f6lge Karadeniz ,B\u00f6l\u00fcm Do\u011fu Karadeniz, il Rize\u2019dir(2400 mm) .Rize\u2019nin \u00e7ok ya\u011f\u0131\u015f almas\u0131nda; g\u00fcneyindeki y\u00fcksek da\u011flar\u0131n hakim r\u00fczgar y\u00f6n\u00fcne dik olmas\u0131 etkilidir.
\n*En az ya\u011f\u0131\u015f alan b\u00f6lgemiz \u0130\u00e7 Anadolu B\u00f6lgesidir. Sebebi ; etraf\u0131n\u0131n da\u011flarla \u00e7evrili olmas\u0131d\u0131r. En az ya\u011f\u0131\u015f alan il Konya \u2018d\u0131r (330 mm).
\nNOT: 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.
\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.
\n*T\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.
\n*T\u00fcrkiye\u2019de k\u0131\u015f\u0131n g\u00f6r\u00fclen ya\u011f\u0131\u015flar genelde cephesel k\u00f6kenlidir. Bu t\u00fcr ya\u011f\u0131\u015f olu\u015fumu en fazla Akdeniz B\u00f6lgesinde g\u00f6r\u00fcl\u00fcr.
\n*\u0130lkbahar ve yaz\u0131n g\u00f6r\u00fclen ya\u011f\u0131\u015flar genelde Konveksiyon ya\u011f\u0131\u015f\u0131 \u015feklindedir. En fazla \u0130\u00e7 Anadolu B\u00f6lgesinde g\u00f6r\u00fcl\u00fcr.
\n*Orografik (yama\u00e7) ya\u011f\u0131\u015flar\u0131 genelde Karadeniz ve Akdeniz B\u00f6lgelerinde g\u00f6r\u00fcl\u00fcr. Fakat en fazla Karadeniz B\u00f6lgesinde g\u00f6r\u00fcl\u00fcr.<\/p>\n
YA\u011eMUR<\/p>\n
YA\u011eMUR: \u0130kiye ayr\u0131l\u0131r. K\u00fc\u00e7\u00fck taneli ve yava\u015f ya\u011fana \u00c7\u0130SEL\u0130, iri taneli ve h\u0131zl\u0131 ya\u011fana SA\u011eANAK ya\u011f\u0131\u015f denir. \u00c7iseli ya\u011fmur daha zarars\u0131zd\u0131r. Ancak sa\u011fanak ya\u011f\u0131\u015flarla toprak fazla ya\u011f\u0131\u015f\u0131 hemen ememez ve sellere, dolay\u0131s\u0131yla erozyona neden olur. Tar\u0131msal alanlar\u0131n, hidroelektrik santrallerinin su ihtiyac\u0131, kurak b\u00f6lgelerin i\u00e7me ve sulama suyu, meralar\u0131n ye\u015ferebilmesi (hayvanc\u0131l\u0131k a\u00e7\u0131s\u0131ndan) ya\u011fmurlar\u0131n etkisiyle olur. Buda insan hayat\u0131 i\u00e7in \u00e7ok \u00f6nemlidir.
\nKAR: Kar a\u015f\u0131r\u0131 ya\u011fmad\u0131k\u00e7a tar\u0131msal \u00fcr\u00fcnlere zarar vermez hatta onlar\u0131 dondan korur. Yava\u015f yava\u015f eriyerek erozyona sebep olmaz, topra\u011f\u0131n su ihtiyac\u0131n\u0131 kar\u015f\u0131lar yeralt\u0131 sular\u0131n\u0131 besler. Ancak a\u015f\u0131r\u0131 olan\u0131 ula\u015f\u0131m\u0131 etkiler. Kar\u0131n yerde kalma s\u00fcresi B \u2019dan D \u2019ya do\u011fru artar.
\nDOLU: Zararl\u0131 etkileri fazla olan bir ya\u011f\u0131\u015f \u00e7e\u015fididir. Yere d\u00fc\u015f\u00fcnce \u00e7abuk erir ve sellere yol a\u00e7ar, tar\u0131m \u00fcr\u00fcnlerine ve hatta e\u015fyalara zarar verir. S\u0130S: Kara, K\u0131y\u0131 Yama\u00e7(orografik) ve cephe sisleri gibi \u00e7e\u015fitleri vard\u0131r. G\u00f6r\u00fc\u015f mesafesi 1 km\u2019den az oldu\u011funda meteorolojik anlamda o g\u00fcn sisli g\u00fcn say\u0131l\u0131r. En fazla sisli g\u00fcn say\u0131s\u0131 \u0130\u00e7 Anadolu\u2019dad\u0131r. Akdeniz k\u0131y\u0131 kesiminde ise sis neredeyse hi\u00e7 g\u00f6r\u00fclmez. Ula\u015f\u0131m\u0131 olumsuz etkiler.
\nT\u00fcrkiye\u2019de Ya\u011f\u0131\u015f\u0131n Da\u011f\u0131l\u0131\u015f\u0131 T\u00fcrkiye\u2019de genel olarak k\u0131y\u0131 kesimler ve y\u00fcksek da\u011f yama\u00e7lar\u0131 bol ya\u011f\u0131\u015fl\u0131 denize kapal\u0131 i\u00e7 kesimler ve \u00e7ukur yerler az ya\u011f\u0131\u015fl\u0131d\u0131r. Ya\u011f\u0131\u015f: Atmosferdeki yo\u011funla\u015fma sonucu meydana gelen su damlac\u0131klar\u0131 ba\u015flang\u0131\u00e7ta birka\u00e7 mikronla 100 mikron \u00e7ap\u0131ndad\u0131r. Bunlar\u0131n bir arada toplanmas\u0131ndan bulutlar meydana gelir. Fakat her buluttan ya\u011f\u0131\u015f d\u00fc\u015fmemektedir. Ya\u011f\u0131\u015f\u0131n d\u00fc\u015febilmesi i\u00e7in damlac\u0131klar\u0131n birle\u015fip 0.5 mm \u00e7ap\u0131na ula\u015fmas\u0131 gerekir. Ya\u011f\u0131\u015f\u0131n meydana gelmesinde esas rol\u00fc oynayan yo\u011funla\u015fma i\u015fleminde havan\u0131n so\u011fumas\u0131 \u00f6nemli bir etkendir. Bu y\u00fczden ya\u011f\u0131\u015f tiplerini so\u011fuma \u015fekillerine g\u00f6re incelemek m\u00fcmk\u00fcnd\u00fcr.
\na) Konvektif ya\u011f\u0131\u015flar: Yerdeki s\u0131cak hava k\u00fctlesinin konvektif y\u00fckselmesiyle meydana gelen genellikle sa\u011fanak \u015feklindeki ya\u011f\u0131\u015flard\u0131r.
\nb) Orografik Ya\u011f\u0131\u015flar: Hava k\u00fctlelerinin bir engebeye \u00e7arparak y\u00fckselmesi ve so\u011fuyarak yo\u011funla\u015fmas\u0131 sonucu meydana gelen ya\u011f\u0131\u015flard\u0131r.
\nc) Cephesel Ya\u011f\u0131\u015flar: Hava k\u00fctleleri aras\u0131ndaki cephelere ba\u011fl\u0131 meydana gelen ya\u011f\u0131\u015flard\u0131r. Yery\u00fcz\u00fcndeki ya\u011f\u0131\u015flar\u0131n b\u00fcy\u00fck k\u0131sm\u0131 bu \u015fekildedir.
\nMevsimlik ya\u011f\u0131\u015flar\u0131n alansal da\u011f\u0131l\u0131m\u0131na bakt\u0131\u011f\u0131m\u0131zda Akdeniz B\u00f6lgesinin ya\u011f\u0131\u015flar\u0131n\u0131n \u00e7o\u011funu K\u0131\u015f aylar\u0131nda ald\u0131\u011f\u0131n\u0131 g\u00f6r\u00fcyoruz. Akdeniz\u2019de bu ya\u011f\u0131\u015f\u0131 b\u0131rakan sistemler da\u011flar\u0131n etkisiyle i\u00e7 b\u00f6lgelerde daha az ya\u011f\u0131\u015f b\u0131rakmaktad\u0131r.
\nKaradeniz B\u00f6lgesinin ise her mevsim ya\u011f\u0131\u015fl\u0131 oldu\u011funu g\u00f6rmekteyiz.Yaz aylar\u0131nda ise kuzey b\u00f6lgelerimiz daha fazla ya\u011f\u0131\u015f almaktad\u0131r. M.Polar hava k\u00fctleleri Karadeniz \u00fczerinde nem kazan\u0131p Rize ve Hopa \u00e7evresinde y\u00fckseli\u015fe ge\u00e7erek orografik ya\u011f\u0131\u015flar b\u0131rak\u0131r. Bu d\u00f6nemde g\u00fcney b\u00f6lgelerimizde ya\u011f\u0131\u015flar\u0131n olduk\u00e7a azald\u0131\u011f\u0131n\u0131 s\u00f6yleyebiliriz. Kuzeyli ve g\u00fcneyli ak\u0131mlarda i\u00e7 b\u00f6lgeler az ya\u011f\u0131\u015f al\u0131r. \u0130\u00e7 b\u00f6lgeler ancak bat\u0131l\u0131 ak\u0131mlarda ya\u011f\u0131\u015f al\u0131r.
\nT\u00fcrkiye ya\u011f\u0131\u015f a\u00e7\u0131s\u0131ndan \u00e7ok \u00e7e\u015fitlilik g\u00f6stermektedir. Genelde sahil kesimlerimiz 1000 mm nin \u00fczerinde ya\u011f\u0131\u015f al\u0131rken Rize 2300; Orta Anadolu ise sadece 300 mm civar\u0131nda ya\u011f\u0131\u015f almaktad\u0131r. Bu da s\u0131cakl\u0131\u011f\u0131n ve buharla\u015fman\u0131n artt\u0131\u011f\u0131 yaz aylar\u0131nda kurakl\u0131\u011fa sebep olmaktad\u0131r.
\nY\u0131ll\u0131k ya\u011f\u0131\u015f zaman serisi grafi\u011fi de bize ya\u011f\u0131\u015ftaki sal\u0131n\u0131mlar\u0131 g\u00f6stermektedir. T\u00fcrkiye y\u0131ll\u0131k ortalama ya\u011f\u0131\u015f\u0131 630 kg. civar\u0131ndad\u0131r. Bu grafikten 72-73, 89-90, 99-2000 y\u0131llar\u0131nda normalin alt\u0131nda ya\u011f\u0131\u015flar alarak kurakl\u0131k ya\u015fad\u0131\u011f\u0131m\u0131z\u0131 g\u00f6rmekteyiz.<\/p>\n","protected":false},"excerpt":{"rendered":"
T\u00fcrkiye\u2019de genel olarak \u00fc\u00e7 ana iklim tipi g\u00f6r\u00fcl\u00fcr.Bunlar; Karadeniz \u0130klimi, Akdeniz \u0130klimi ve Karasal iklimdir. 1)KARADEN\u0130Z \u0130KL\u0130M\u0130:Bu iklim as\u0131l olarak Kuzey Anadolu Da\u011flar\u0131n\u0131n Karadeniz\u2019e bakan yama\u00e7lar\u0131nda g\u00f6r\u00fcl\u00fcr. Genel \u00f6zellikleri \u015funlard\u0131r: Her mevsim ya\u011f\u0131\u015fl\u0131d\u0131r.Do\u011fu Karadeniz B\u00f6l\u00fcm\u00fcnde maksimum ya\u011f\u0131\u015f sonbaharda, minimum ya\u011f\u0131\u015f ilkbaharda d\u00fc\u015fer. Y\u0131ll\u0131k ya\u011f\u0131\u015f miktar\u0131 2000-2500 mm\u2019dir.Bat\u0131 Karadeniz B\u00f6l\u00fcm\u00fcnde maksimum ya\u011f\u0131\u015f sonbaharda, minimum ya\u011f\u0131\u015f ilkbaharda …<\/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":[2790,2796,2800,2794,2795,2797,2798,2793,2789,2791,2799,2792,2788],"class_list":["post-937","post","type-post","status-publish","format-standard","hentry","category-odevler","category-sosyal-bilgiler-odevleri","tag-akdeniz-iklimi","tag-atmosfer","tag-cephesel-yagislar","tag-dogu-anadolu","tag-guneydogu-anadolu","tag-hava-basinci","tag-hidroelektrik","tag-ic-anadolu","tag-karadeniz-iklimi","tag-karasal-iklim","tag-orografik","tag-orta-karadeniz","tag-turkiyenin-iklim-ozellikleri"],"_links":{"self":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/937","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=937"}],"version-history":[{"count":0,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/937\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/media?parent=937"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/categories?post=937"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/tags?post=937"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}