Atmosferde bulunan gazlar\u0131n % 75\u2019i ve su buhar\u0131n\u0131n tamam\u0131 troposferde bulunur. \u0130klim y\u00f6n\u00fcnden daha \u00e7ok atmosferin alt katlar\u0131 \u00f6nemli oldu\u011fundan burada troposfer ve stratosferin alt katlar\u0131n\u0131n bile\u015fimi incelenecektir.<\/p>\n
\u2022 Her zaman bulunan ve oran\u0131 de\u011fi\u015fmeyen gazlar; % 78 oran\u0131nda azot, % 21 oran\u0131nda oksijen, %1 oran\u0131nda asal gazlar (Hidrojen, Helyum, Argon, Kripton, Ksenon, Neon) d\u0131r.
\n \u2022 Her zaman bulunan ve oran\u0131 de\u011fi\u015fen gazlar; su buhar\u0131 ve karbondioksittir.
\n \u2022 Her zaman bulunmayan gazlar; ozon ve tozlard\u0131r. <\/p>\n
Su buhar\u0131 : Yere ve zaman g\u00f6re oran\u0131 en \u00e7ok de\u011fi\u015fen gazd\u0131r. Yery\u00fcz\u00fcn\u00fcn a\u015f\u0131r\u0131 \u0131s\u0131n\u0131p, so\u011fumas\u0131n\u0131 engeller. Ya\u011f\u0131\u015f, bulut, sis gibi hava olaylar\u0131n\u0131n do\u011fu\u015funu sa\u011flar.<\/p>\n
Karbondioksit : Atmosferin g\u00fcne\u015f \u0131\u015f\u0131nlar\u0131n\u0131 emme ve saklama yetene\u011fini art\u0131r\u0131r. Havada karbondioksit (CO2) miktar\u0131n\u0131n artmas\u0131 s\u0131cakl\u0131\u011f\u0131 art\u0131r\u0131c\u0131, azalmas\u0131 ise s\u0131cakl\u0131\u011f\u0131 d\u00fc\u015f\u00fcr\u00fcc\u00fc etki yapar.<\/p>\n
Ozon : Hava i\u00e7indeki oksijen (O2) mor \u00f6tesi (ultraviyole) \u0131\u015f\u0131nlar\u0131n\u0131n etkisi alt\u0131nda ozon (O3) haline ge\u00e7er. Ozon gaz\u0131, i\u00e7inde hayat\u0131n geli\u015fmesine olanak vermez ancak atmosferin \u00fcst katmanlar\u0131nda ultraviyole \u0131\u015f\u0131nlar\u0131n\u0131 emerek yery\u00fcz\u00fcndeki ya\u015fam \u00fczerinde olumlu bir etki yapar. Yery\u00fcz\u00fcnden 19 \u2013 45 kilometre y\u00fckseklikler aras\u0131nda bulunan ozon kat\u0131n\u0131n son y\u0131llarda inceldi\u011fi hatta yer yer delindi\u011fi belirlenmi\u015ftir. \u00d6zellikle buzdolab\u0131, so\u011futucu, araba ve spreylerden \u00e7\u0131kan gazlar\u0131n (kloroflorokarbon) neden oldu\u011fu anla\u015f\u0131lm\u0131\u015f ve bu gazlar\u0131n kullan\u0131m\u0131na k\u0131s\u0131tlamalar getirilmi\u015ftir.
\n Yery\u00fcz\u00fcne ula\u015fan mor \u00f6tesi \u0131\u015f\u0131nlardaki art\u0131\u015f, s\u0131cakl\u0131klar\u0131n artmas\u0131na, buna ba\u011fl\u0131 olarak buzullar\u0131n erimesine, bitki \u00f6rt\u00fclerinde de\u011fi\u015fimlere neden olabilecektir.<\/p>\n
S\u0131cakl\u0131k<\/p>\n
G\u00fcne\u015f I\u015f\u0131nlar\u0131n\u0131n Atmosferde Da\u011f\u0131l\u0131\u015f\u0131<\/p>\n
Yery\u00fcz\u00fcn\u00fcn \u0131s\u0131nmas\u0131nda ana enerji kayna\u011f\u0131 G\u00fcne\u015f\u2019tir. D\u00fcnya, G\u00fcne\u015f\u2019in uzaya yayd\u0131\u011f\u0131 enerjinin ancak iki milyonda birini al\u0131r. G\u00fcne\u015f\u2019ten gelen bu enerji g\u00fcne\u015f sabitesi (solar konstant) ile belirlenir. Atmosferin \u00fcst s\u0131n\u0131r\u0131nda 1 cm2\u2019ye 1 dakikada gelen kalori miktar\u0131na g\u00fcne\u015f sabitesi (solar konstant) denir.
\n Atmosferin etkisiyle, G\u00fcne\u015f\u2019ten gelen \u0131\u015f\u0131nlar\u0131n tamam\u0131 yere ula\u015fmaz. Atmosfer g\u00fcne\u015f \u0131\u015f\u0131nlar\u0131n\u0131 \u00e7e\u015fitli oranlarda tutar ve da\u011f\u0131t\u0131r. Bu nedenle yery\u00fcz\u00fc G\u00fcne\u015f\u2019ten gelen \u0131\u015f\u0131nlardan \u00e7ok atmosfer taraf\u0131ndan tutulan \u0131\u015f\u0131nlarla \u0131s\u0131n\u0131r.<\/p>\n
S\u0131cakl\u0131k Etmenleri <\/p>\n
Atmosferin \u0131s\u0131nmas\u0131 \u00e7e\u015fitli etmenlerin etkisi alt\u0131ndad\u0131r.<\/p>\n
G\u00fcne\u015f I\u015f\u0131nlar\u0131n\u0131n Yery\u00fcz\u00fcne De\u011fme A\u00e7\u0131s\u0131<\/p>\n
Belirli bir y\u00fczeye dik ve yat\u0131k gelen \u0131\u015f\u0131nlar\u0131n getirdikleri enerji miktarlar\u0131 aras\u0131nda belirgin bir fark vard\u0131r.
\n \u00c7\u00fcnk\u00fc bir \u0131\u015f\u0131n demeti dik geldi\u011finde daha dar bir y\u00fczeyi ayd\u0131nlat\u0131rken, ayn\u0131 \u0131\u015f\u0131n demeti yat\u0131k geldi\u011finde daha geni\u015f bir y\u00fczeyi ayd\u0131nlat\u0131r.
\n Ancak \u0131\u015f\u0131nlar\u0131n yere de\u011fme a\u00e7\u0131s\u0131 darald\u0131\u011f\u0131 i\u00e7in etkisi azal\u0131r. Bu nedenle G\u00fcne\u015f \u0131\u015f\u0131nlar\u0131n\u0131n yere de\u011fme a\u00e7\u0131s\u0131 b\u00fcy\u00fcd\u00fck\u00e7e yery\u00fcz\u00fcn\u00fc \u0131s\u0131tma g\u00fcc\u00fc de artar.
\n G\u00fcne\u015f \u0131\u015f\u0131nlar\u0131n\u0131n yery\u00fcz\u00fcne de\u011fme a\u00e7\u0131s\u0131n\u0131 etkileyen etmenler \u015funlard\u0131r:<\/p>\n
D\u00fcnya\u2019n\u0131n \u015eekli<\/p>\n
D\u00fcnya\u2019n\u0131n k\u00fcreselli\u011finin bir sonucu olarak, Ekvator\u2019dan kutuplara do\u011fru g\u00fcne\u015f \u0131\u015f\u0131nlar\u0131n\u0131n yere de\u011fme a\u00e7\u0131s\u0131 k\u00fc\u00e7\u00fcl\u00fcr. Buna ba\u011fl\u0131 olarak her iki yar\u0131m k\u00fcrede Ekvator\u2019dan kutuplara do\u011fru s\u0131cakl\u0131k azal\u0131r. Bu durum enlemin s\u0131cakl\u0131k \u00fczerindeki etkisini g\u00f6sterir.<\/p>\n
D\u00fcnya\u2019n\u0131n Eksen E\u011fikli\u011fi ve Y\u0131ll\u0131k Hareketi
\n D\u00fcnya\u2019n\u0131n eksen e\u011fikli\u011fi nedeni ile G\u00fcne\u015f \u00e7evresindeki d\u00f6n\u00fc\u015f\u00fc (y\u0131ll\u0131k hareket) s\u0131ras\u0131nda g\u00fcne\u015f \u0131\u015f\u0131nlar\u0131n\u0131n yere de\u011fme a\u00e7\u0131s\u0131 de\u011fi\u015fir.
\n Yery\u00fcz\u00fcndeki bir noktan\u0131n g\u00fcne\u015f \u0131\u015f\u0131nlar\u0131n\u0131 y\u0131l i\u00e7inde farkl\u0131 a\u00e7\u0131larla almas\u0131 \u0131s\u0131nma farkl\u0131l\u0131klar\u0131na neden olur.<\/p>\n
D\u00fcnya\u2019n\u0131n G\u00fcnl\u00fck Hareketi<\/p>\n
D\u00fcnya\u2019n\u0131n g\u00fcnl\u00fck hareketi nedeniyle g\u00fcne\u015f \u0131\u015f\u0131nlar\u0131n\u0131n bir noktaya de\u011fme a\u00e7\u0131s\u0131 sabahtan \u00f6\u011fleye kadar artar. \u00d6\u011fleden ak\u015fama kadar ise azal\u0131r. G\u00fcn\u00fcn en y\u00fcksek s\u0131cakl\u0131\u011f\u0131, \u0131\u015f\u0131nlar\u0131n en b\u00fcy\u00fck a\u00e7\u0131 ile geldi\u011fi \u00f6\u011fle saati de\u011fil, depolanan enerjinin en fazla oldu\u011fu 13.00 \u2013 14.00 saatleri aras\u0131 \u00f6l\u00e7\u00fcl\u00fcr. \u00c7\u00fcnk\u00fc \u00f6\u011fleye kadar yerde biriken enerji, \u0131\u015f\u0131nlar\u0131n gelme a\u00e7\u0131s\u0131n\u0131n daralmas\u0131yla birlikte \u0131\u015f\u0131ma ile atmosfere iletilir. I\u015f\u0131ma gece boyu devam eder, yer so\u011fur. G\u00fcne\u015f\u2019in do\u011fu\u015f saatinde \u0131\u015f\u0131ma sona erer ve yerde enerji depolamaya ba\u015flar. I\u015f\u0131man\u0131n sona erdi\u011fi anda g\u00fcn\u00fcn en d\u00fc\u015f\u00fck s\u0131cakl\u0131\u011f\u0131 ya\u015fan\u0131r.<\/p>\n
I\u015f\u0131ma<\/p>\n
Yery\u00fcz\u00fc kazand\u0131\u011f\u0131 enerjinin bir b\u00f6l\u00fcm\u00fcn\u00fc atmosfere geri verir. Buna yer \u0131\u015f\u0131mas\u0131 denir. G\u00fcne\u015f \u0131\u015f\u0131nlar\u0131n\u0131n yery\u00fcz\u00fcne ula\u015famad\u0131\u011f\u0131 saatlerde (gece) ve g\u00fcne\u015f \u0131\u015f\u0131nlar\u0131n\u0131n yere de\u011fme a\u00e7\u0131lar\u0131n\u0131n k\u00fc\u00e7\u00fcld\u00fc\u011f\u00fc aylarda yer \u0131\u015f\u0131mas\u0131 artar. Ayr\u0131ca, zeminin yap\u0131s\u0131 da yer \u0131\u015f\u0131mas\u0131 \u00fczerinde etkilidir. \u00d6rne\u011fin yery\u00fcz\u00fcn\u00fcn bitki ile kapl\u0131 alanlar\u0131nda yer \u0131\u015f\u0131mas\u0131 az ve yava\u015fken \u00e7\u0131lak arazilerde \u0131s\u0131 kayb\u0131 daha h\u0131zl\u0131 ve fazla olur.<\/p>\n
E\u011fim ve Bak\u0131<\/p>\n
Geni\u015f bir b\u00f6lgeye d\u00fc\u015fen birbirine paralel \u0131\u015f\u0131nlar\u0131n yere d\u00fc\u015fme a\u00e7\u0131lar\u0131, yama\u00e7 e\u011fimine ve bak\u0131 durumuna (G\u00fcne\u015f\u2019e d\u00f6n\u00fckl\u00fc\u011fe) g\u00f6re de\u011fi\u015fir. Bu durum yerel \u0131s\u0131nma farklar\u0131na yol a\u00e7ar. Kuzey Yar\u0131m K\u00fcre\u2019de g\u00fcney yama\u00e7lar, G\u00fcney Yar\u0131m K\u00fcre\u2019de ise kuzey yama\u00e7lar g\u00fcne\u015f \u0131\u015f\u0131nlar\u0131n\u0131 y\u0131l boyunca daha b\u00fcy\u00fck a\u00e7\u0131 ile ald\u0131\u011f\u0131ndan daha s\u0131cak olur.
\n Ekvator \u00e7evresinde bak\u0131n\u0131n etkisi t\u00fcm yama\u00e7larda g\u00f6r\u00fcl\u00fcr.<\/p>\n
Bak\u0131n\u0131n Etkisi<\/p>\n
G\u00fcne\u015fe d\u00f6n\u00fck olan e\u011fimli yama\u00e7larda;
\n \u2022 S\u0131cakl\u0131k daha y\u00fcksektir.
\n \u2022 G\u00fcne\u015flenme s\u00fcresi daha uzundur.
\n \u2022 Karlar\u0131n yerde kalma s\u00fcresi daha k\u0131sad\u0131r.
\n \u2022 Kal\u0131c\u0131 karlar\u0131n ba\u015flama y\u00fcksekli\u011fi daha fazlad\u0131r.
\n \u2022 Tar\u0131m \u00fcr\u00fcnlerinin olgunla\u015fma s\u00fcresi daha k\u0131sad\u0131r.
\n \u2022 Ormanlar\u0131n y\u00fckselti s\u0131n\u0131r\u0131 daha fazlad\u0131r. <\/p>\n
Y\u00fckselti<\/p>\n
Deniz seviyesinden y\u00fckseldik\u00e7e atmosferin yo\u011funlu\u011funun ve i\u00e7indeki su buhar\u0131n\u0131n azalmas\u0131 ile troposferin daha \u00e7ok yerden yans\u0131yan \u0131\u015f\u0131nlarla \u0131s\u0131nmas\u0131 nedeniyle s\u0131cakl\u0131k, her 100 m\u2019de yakla\u015f\u0131k 0,5\u00b0C azal\u0131r. Bu nedenle enlemi ayn\u0131 olan iki farkl\u0131 noktadan daha y\u00fcksekte olan, di\u011ferine g\u00f6re her zaman daha so\u011fuk olur. \u00d6rne\u011fin deniz seviyesinden 155 m y\u00fckseklikteki Bursa\u2019da s\u0131cakl\u0131k 25\u00b0C iken ayn\u0131 enlemde bulunmas\u0131na kar\u015f\u0131n 2543 m y\u00fckseklikteki Uluda\u011f\u2019da s\u0131cakl\u0131\u011f\u0131n 12\u00b0C olmas\u0131 y\u00fckseltinin s\u0131cakl\u0131\u011fa etkisini g\u00f6sterir.<\/p>\n
\u0130ndirgenmi\u015f S\u0131cakl\u0131k<\/p>\n
Yery\u00fcz\u00fcnde s\u0131cakl\u0131\u011f\u0131n enleme ba\u011fl\u0131 da\u011f\u0131l\u0131\u015f\u0131n\u0131 g\u00f6steren haritalar \u00e7izilirken y\u00fckseltinin s\u0131cakl\u0131k \u00fczerindeki etkisini ortadan kald\u0131rmak i\u00e7in indirgenmi\u015f s\u0131cakl\u0131k de\u011ferleri kullan\u0131l\u0131r.
\n Bir yerin y\u00fckseltisinin s\u0131f\u0131r (0 m) kabul edilerek hesaplanan s\u0131cakl\u0131\u011f\u0131na indirgenmi\u015f s\u0131cakl\u0131k denir.
\n Bir yerin indirgenmi\u015f s\u0131cakl\u0131\u011f\u0131n\u0131 hesaplamak i\u00e7in y\u00fckseltiden kaynaklanan s\u0131cakl\u0131k fark\u0131 hesaplan\u0131r.
\n Bu fark o yerin ger\u00e7ek s\u0131cakl\u0131\u011f\u0131na eklenir.
\n \u00d6rnek :
\n 900 m y\u00fckseklikteki Ankara\u2019da Ocak ay\u0131 ortalama s\u0131cakl\u0131\u011f\u0131 -2\u00b0C\u2019dir. Ankara\u2019n\u0131n deniz seviyesine indirgenmi\u015f s\u0131cakl\u0131\u011f\u0131 ka\u00e7 \u00b0C dir?
\n \u00c7\u00f6z\u00fcm :
\n 100 m\u2019de s\u0131cakl\u0131k 0,5\u00b0C azal\u0131rsa
\n 900 m\u2019de X\u00b0C azal\u0131r.
\n X=900 x 0,5 \/ 100 = 4,5 \u00b0C\u2019dir.<\/p>\n
\u0130ndirgenmi\u015f S\u0131cakl\u0131k = Ger\u00e7ek S\u0131cakl\u0131k + S\u0131cakl\u0131k Fark\u0131
\n \u0130ndirgenmi\u015f S\u0131cakl\u0131k = -2 +4,5
\n \u0130ndirgenmi\u015f S\u0131cakl\u0131k = 2,5\u00b0C\u2019dir.<\/p>\n
Kara ve Deniz Da\u011f\u0131l\u0131\u015f\u0131<\/p>\n
Karalar denizlere g\u00f6re daha \u00e7ok ve \u00e7abuk \u0131s\u0131n\u0131p, so\u011furlar. Bu nedenle, karalar\u0131n daha fazla yer kaplad\u0131\u011f\u0131 Kuzey Yar\u0131m K\u00fcre\u2019nin y\u0131ll\u0131k ortalama s\u0131cakl\u0131\u011f\u0131 G\u00fcney Yar\u0131m K\u00fcre\u2019den daha fazlad\u0131r.
\n Ayr\u0131ca her iki yar\u0131m k\u00fcrede kara ve denizlerin da\u011f\u0131l\u0131\u015f\u0131ndaki farkl\u0131l\u0131k termik ekvatorun yer ekvatorundan sapmas\u0131na neden olmu\u015ftur.<\/p>\n
Termik Ekvator : Meridyenlerin en s\u0131cak noktalar\u0131n\u0131 birle\u015ftiren e\u011friye termik ekvator denir.<\/p>\n
Atmosferdeki Nem Oran\u0131 <\/p>\n
Atmosferdeki nem;
\n \u2022 G\u00fcne\u015ften gelen ve yery\u00fcz\u00fcnden yans\u0131yan \u0131\u015f\u0131nlar\u0131 emerek tutar.
\n \u2022 Yery\u00fcz\u00fcn\u00fcn a\u015f\u0131r\u0131 \u0131s\u0131n\u0131p so\u011fumas\u0131n\u0131 \u00f6nler.
\n \u2022 Is\u0131n\u0131p so\u011fuman\u0131n yava\u015f ve dengeli olmas\u0131n\u0131 sa\u011flar. Bu nedenle nemli b\u00f6lgelerde g\u00fcnl\u00fck ve s\u0131cakl\u0131k farklar\u0131 daha azd\u0131r. <\/p>\n
Okyanus Ak\u0131nt\u0131lar\u0131<\/p>\n
Enlemin etkisine ba\u011fl\u0131 olarak, ekvatoral b\u00f6lgeden gelen ak\u0131nt\u0131lar s\u0131cak su, kutup b\u00f6lgelerinden gelen ak\u0131nt\u0131lar ise so\u011fuk su ta\u015f\u0131rlar.
\n S\u0131cak su ak\u0131nt\u0131lar\u0131 ge\u00e7tikleri k\u0131y\u0131larda s\u0131cakl\u0131\u011f\u0131 y\u00fckseltici, so\u011fuk su ak\u0131nt\u0131lar\u0131 ise s\u0131cakl\u0131\u011f\u0131 d\u00fc\u015f\u00fcr\u00fcc\u00fc etki yapar.<\/p>\n
R\u00fczgarlar<\/p>\n
R\u00fczgarlar geldikleri yerlerin \u00f6zelliklerine g\u00f6re, estikleri b\u00f6lgelerin s\u0131cakl\u0131\u011f\u0131n\u0131 y\u00fckseltici ya da d\u00fc\u015f\u00fcr\u00fcc\u00fc etki yapar. Bu durum enlemin s\u0131cakl\u0131k \u00fczerindeki etkisini g\u00f6sterir. \u00d6rne\u011fin Kuzey Yar\u0131m K\u00fcre\u2019de yer alan T\u00fcrkiye\u2019de kuzeyden esen r\u00fczgarlar s\u0131cakl\u0131\u011f\u0131 d\u00fc\u015f\u00fcr\u00fcc\u00fc g\u00fcneyden esen r\u00fczgarlar s\u0131cakl\u0131\u011f\u0131 art\u0131r\u0131c\u0131 etki yapar.<\/p>\n
Zeminin Yap\u0131s\u0131<\/p>\n
Karalar\u0131 olu\u015fturan ta\u015f ve topraklar\u0131n fiziksel \u00f6zellikleri (rengi, parlakl\u0131\u011f\u0131, g\u00f6zenekli\u011fi gibi \u00f6zellikleri) yery\u00fcz\u00fcnde \u0131s\u0131nma farkl\u0131l\u0131klar\u0131na neden olur. Ayr\u0131ca zeminin bitki \u00f6rt\u00fcs\u00fc ile kapl\u0131 olup olmamas\u0131, bitki \u00f6rt\u00fcs\u00fcn\u00fcn yo\u011funlu\u011fu, kar ya da toprak \u00f6rt\u00fcs\u00fcn\u00fcn bulunup bulunmamas\u0131 s\u0131cakl\u0131k da\u011f\u0131l\u0131\u015f\u0131 \u00fczerinde etkilidir.
\n Bu nedenle ta\u015f ve topraklar\u0131n \u0131s\u0131n\u0131p so\u011fuma s\u00fcreleri farkl\u0131l\u0131k g\u00f6sterir.
\n \u00d6rne\u011fin a\u00e7\u0131k renkli ve gev\u015fek yap\u0131ya sahip kumsallarda \u0131s\u0131nma ve so\u011fuma \u00e7abuk ger\u00e7ekle\u015fir.<\/p>\n
S\u0131cakl\u0131k Ku\u015faklar\u0131<\/p>\n
Matematik iklim ku\u015faklar\u0131n\u0131n s\u0131cakl\u0131k etmenlerinin etkisi ile de\u011fi\u015fikli\u011fe u\u011framas\u0131 sonucu belirlenmi\u015ftir. Kara ve denizlerin da\u011f\u0131l\u0131\u015f\u0131 bu belirlemede temel etkendir.
\n Kuzey Yar\u0131m K\u00fcre\u2019de karalar\u0131n daha geni\u015f yer kaplamas\u0131, yaz s\u00fcrelerinin daha uzun olmas\u0131, s\u0131cak su ak\u0131nt\u0131lar\u0131n\u0131n daha etkili olmas\u0131 ve G\u00fcney Yar\u0131m K\u00fcre\u2019de buzullarla kapl\u0131, geni\u015f Antartika K\u0131tas\u0131\u2019n\u0131n bulunmas\u0131 nedeniyle s\u0131cak ve \u0131l\u0131man ku\u015fak Kuzey Yar\u0131m K\u00fcre\u2019de, so\u011fuk ku\u015fak ise G\u00fcney Yar\u0131m K\u00fcre\u2019de daha geni\u015ftir.<\/p>\n
Matematik \u0130klim Ku\u015faklar\u0131 : D\u00fcnya\u2019n\u0131n eksen e\u011fikli\u011fine g\u00f6re belirlendi\u011fi i\u00e7in, s\u0131n\u0131rlar\u0131 d\u00f6nenceler ve kutup daireleridir.<\/p>\n","protected":false},"excerpt":{"rendered":"
Atmosferde bulunan gazlar\u0131n % 75\u2019i ve su buhar\u0131n\u0131n tamam\u0131 troposferde bulunur. \u0130klim y\u00f6n\u00fcnden daha \u00e7ok atmosferin alt katlar\u0131 \u00f6nemli oldu\u011fundan burada troposfer ve stratosferin alt katlar\u0131n\u0131n bile\u015fimi incelenecektir. \u2022 Her zaman bulunan ve oran\u0131 de\u011fi\u015fmeyen gazlar; % 78 oran\u0131nda azot, % 21 oran\u0131nda oksijen, %1 oran\u0131nda asal gazlar (Hidrojen, Helyum, Argon, Kripton, Ksenon, Neon) d\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":[2842,3681,10702,2338,4267,2980,4251,3198,3901,2835],"class_list":["post-5371","post","type-post","status-publish","format-standard","hentry","category-odevler","category-sosyal-bilgiler-odevleri","tag-atmosferde-bulunan-gazlar","tag-dunyanin-gunluk-hareketi","tag-indirgenmis-sicaklik","tag-karbondioksit","tag-matematik-iklim-kusaklari","tag-okyanus-akintilari","tag-ozon","tag-sicaklik-kusaklari","tag-su-buhari","tag-troposfer"],"_links":{"self":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/5371","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=5371"}],"version-history":[{"count":0,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/5371\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/media?parent=5371"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/categories?post=5371"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/tags?post=5371"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}