D\u00fcnya\u2019da G\u00f6r\u00fclen \u0130klim Tipleri<\/p>\n
Bir yerde benzer s\u0131cakl\u0131k, bas\u0131n\u00e7, r\u00fczgar, nemlilik ve ya\u011f\u0131\u015f \u00f6zelliklerinin uzun s\u00fcre etkili olmas\u0131yla iklim tipleri belirmektedir. \u0130klimi olu\u015fturan bu \u00f6\u011felerden birinin ya da ikisinin farkl\u0131 olmas\u0131, de\u011fi\u015fik iklim tiplerinin ortaya \u00e7\u0131kmas\u0131na neden olur.<\/p>\n
D\u00fcnya\u2019da g\u00f6r\u00fclen iklimler, s\u0131cak ku\u015fak iklimleri, \u0131l\u0131man ku\u015fak iklimleri ve so\u011fuk ku\u015fak iklimleri olarak \u00fc\u00f6\u00e7 ana b\u00f6l\u00fcmde toplan\u0131r.<\/p>\n
S\u0131cak Ku\u015fak \u0130klimleri<\/p>\n
S\u0131cak Ku\u015fak \u0130klimlerinin Ortak \u00d6zellikleri <\/p>\n
Y\u0131ll\u0131k s\u0131cakl\u0131k ortalamalar\u0131 20\u00b0C\u2019nin \u00fcst\u00fcndedir.
\n S\u0131cakl\u0131k farklar\u0131 Ekvator\u2019dan uzakla\u015fd\u0131k\u00e7a artar.
\n So\u011fuk mevsim yoktur.
\n Ya\u011f\u0131\u015f \u00f6zellikleri farkl\u0131l\u0131k g\u00f6sterir. <\/p>\n
Ekvatoral \u0130klim<\/p>\n
Ekvatoral \u0130klimin \u00d6zellikleri<\/p>\n
Y\u0131ll\u0131k s\u0131cakl\u0131k ortalamas\u0131n\u0131n 20\u00b0C\u2019nin \u00fcst\u00fcnde oldu\u011fu ekvatoral iklimde y\u0131l boyunca yaz ko\u015fullar\u0131 ya\u015fan\u0131r.<\/p>\n
G\u00fcne\u015f \u0131\u015f\u0131nlar\u0131, y\u0131l boyunca dik ve dike yak\u0131n a\u00e7\u0131larla geldi\u011finden y\u0131ll\u0131k s\u0131cakl\u0131k fark\u0131 azd\u0131r.<\/p>\n
Y\u0131l boyunca y\u00fckseltici hava hareketlerine ba\u011fl\u0131 olarak konveksiyonel ya\u011f\u0131\u015f g\u00f6r\u00fcl\u00fcr.<\/p>\n
Y\u0131ll\u0131k ya\u011f\u0131\u015f miktar\u0131 2000 mm\u2019nin \u00fczerindedir. Her mevsimin ya\u011f\u0131\u015fl\u0131 oldu\u011fu ekvatoral b\u00f6lge akarsular\u0131n\u0131n rejimleri d\u00fczenlidir ve y\u0131l boyunca bol su ta\u015f\u0131r. G\u00fcne\u015f \u0131\u015f\u0131nlar\u0131n\u0131n dik geldi\u011fi Mart ve Eyl\u00fcl aylar\u0131nda ya\u011f\u0131\u015flar artar. Bu nedenle ekinokslarda (21 Mart \u2013 23 Eyl\u00fcl) akarsularda kabarma olur.<\/p>\n
Konveksiyonel Ya\u011f\u0131\u015f : Is\u0131nan havan\u0131n y\u00fckselerek so\u011fumas\u0131 ile olu\u015fan ya\u011f\u0131\u015flard\u0131r.<\/p>\n
UYARI : Ekvatoral iklimde y\u0131ll\u0131k s\u0131cakl\u0131k farklar\u0131n\u0131n az olmas\u0131 g\u00fcne\u015f \u0131\u015f\u0131nlar\u0131n\u0131n yere de\u011fme a\u00e7\u0131lar\u0131n\u0131n az de\u011fi\u015fmesiyle, g\u00fcnl\u00fck s\u0131cakl\u0131k farklar\u0131n\u0131n az olmas\u0131 ise nem oran\u0131n\u0131n y\u00fcksek olmas\u0131yla ilgilidir.<\/p>\n
Ekvatoral \u0130klimin Do\u011fal Bitki \u00d6rt\u00fcs\u00fc
\n Y\u0131l boyunca s\u0131cakl\u0131k ve nem ko\u015fullar\u0131 elveri\u015fli oldu\u011fundan s\u00fcrekli ye\u015fil kalabilen yayvan yaprakl\u0131 a\u011fa\u00e7lardan olu\u015fan g\u00fcr ormanlard\u0131r. Ya\u011fmur ormanlar\u0131 ad\u0131 verilen bu ormanlardaki a\u011fa\u00e7lar\u0131n boyu ya\u011f\u0131\u015f miktar\u0131n\u0131n fazla olmas\u0131 nedeniyle 40-60 m lere kadar \u00e7\u0131kabilir. Ormanalt\u0131 floaras\u0131 da \u00e7ok zengindir.<\/p>\n
Ormanalt\u0131 Floras\u0131 : Orman \u00f6rt\u00fcs\u00fc alt\u0131nda lo\u015f ortamda yeti\u015fen, \u00e7o\u011funlukla ot ve sarma\u015f\u0131k t\u00fcrlerinin olu\u015fturdu\u011fu bitki toplulu\u011fudur.<\/p>\n
Ekvatoral \u0130klimin G\u00f6r\u00fcld\u00fc\u011f\u00fc Yerler<\/p>\n
10\u00b0 Kuzey ve G\u00fcney enlemleri aras\u0131nda, <\/p>\n
G\u00fcney Amerika\u2019da Amazon Havzas\u0131\u2019nda,<\/p>\n
Afrika\u2019da Kongo Havzas\u0131\u2019nda ve Gine K\u00f6rfezi k\u0131y\u0131lar\u0131nda,<\/p>\n
Asya\u2019da Endonezya Adalar\u0131\u2019nda g\u00f6r\u00fcl\u00fcr.<\/p>\n
Yazlar\u0131 Ya\u011f\u0131\u015fl\u0131 Tropikal \u0130klim (Savan)<\/p>\n
Y\u0131ll\u0131k s\u0131cakl\u0131k ortalamas\u0131 20\u00b0C\u2019nin \u00fcst\u00fcndedir.<\/p>\n
Yazlar s\u0131cak ve ya\u011f\u0131\u015fl\u0131, k\u0131\u015flar s\u0131cak ve kurak ge\u00e7er<\/p>\n
G\u00fcne\u015f \u0131\u015f\u0131nlar\u0131n\u0131n dik a\u00e7\u0131yla geldi\u011fi yaz aylar\u0131nda konveksiyonel ya\u011f\u0131\u015flar g\u00f6r\u00fcl\u00fcr.<\/p>\n
K\u0131\u015f aylar\u0131nda subtropikal y\u00fcksek bas\u0131nc\u0131n (DYB) etkisinde kald\u0131\u011f\u0131ndan k\u0131\u015f kurakl\u0131\u011f\u0131 belirgindir.<\/p>\n
Y\u0131ll\u0131k ya\u011f\u0131\u015f miktar\u0131 1000 mm civar\u0131ndad\u0131r.<\/p>\n
UYARI : Savan ikliminde g\u00fcnl\u00fck s\u0131cakl\u0131k farklar\u0131, nemlilik nedeniyle yaz\u0131n az, k\u0131\u015f\u0131n fazlad\u0131r.<\/p>\n
Yazlar\u0131 Ya\u011f\u0131\u015fl\u0131 Tropikal \u0130klimin (Savan \u0130klimi) Do\u011fal Bitki \u00d6rt\u00fcs\u00fc<\/p>\n
Yaz ya\u011f\u0131\u015flar\u0131yla ye\u015feren, uzun boylu, g\u00fcr ot topluluklar\u0131d\u0131r. Bunlara savan ad\u0131 verilir. Savanlar aras\u0131nda yer yer kurak\u00e7\u0131l a\u011fa\u00e7lar g\u00f6r\u00fcl\u00fcr. Akarsu boylar\u0131nda ise galeri ormanlar\u0131 g\u00f6r\u00fcl\u00fcr.<\/p>\n
Galeri Ormanlar\u0131 : Savanlardaki, k\u00fc\u00e7\u00fck akarsu boylar\u0131nda g\u00f6r\u00fclen, \u00e7o\u011funlukla 50-100 m geni\u015fli\u011finde, bir akarsu a\u011f\u0131 bi\u00e7iminde uzanan ve s\u00fcrekli ye\u015fil kalabilen nemli ormanlard\u0131r. Galeri ormanlar\u0131 olarak adland\u0131r\u0131lmalar\u0131n\u0131n nedeni, a\u011fa\u00e7lar\u0131n, akarsuyun \u00fcst\u00fcn\u00fc bir galeri \u015feklinde kapatmas\u0131d\u0131r.<\/p>\n
Yazlar\u0131 Ya\u011f\u0131\u015fl\u0131 Tropikal \u0130klimin (Savan \u0130klimi) G\u00f6r\u00fcld\u00fc\u011f\u00fc Yerler<\/p>\n
10\u00b0 enlemleri ile d\u00f6nenceler aras\u0131nda,<\/p>\n
Orta Amerika\u2019da,<\/p>\n
Sahra \u00c7\u00f6l\u00fc ile Ekvatoral Afrika aras\u0131nda,<\/p>\n
G\u00fcney Afrika\u2019da,<\/p>\n
G\u00fcney Amerika\u2019da,<\/p>\n
Kuzey Avustralya\u2019da,<\/p>\n
Madagaskar\u2019\u0131n bat\u0131s\u0131nda g\u00f6r\u00fcl\u00fcr.<\/p>\n
Muson \u0130klimi<\/p>\n
Muson \u0130kliminin \u00d6zellikleri<\/p>\n
K\u0131\u015f s\u0131cakl\u0131\u011f\u0131 10\u00b0C – 20\u00b0C aras\u0131nda de\u011fi\u015fir. Y\u0131ll\u0131k s\u0131cakl\u0131k ortalamas\u0131 20\u00b0C nin \u00fcst\u00fcndedir. <\/p>\n
Muson r\u00fczgarlar\u0131n\u0131n etkisiyle yazlar s\u0131cak ve bol ya\u011f\u0131\u015fl\u0131 ge\u00e7er. K\u0131\u015flar ise \u0131l\u0131k ve kurakt\u0131r.<\/p>\n
\u00c7o\u011funlukla 2000 \u2013 5000 mm aras\u0131nda de\u011fi\u015fen y\u0131ll\u0131k ya\u011f\u0131\u015f miktar\u0131 baz\u0131 yerlerde 10000 mm\u2019yi ge\u00e7mektedir. \u00d6rne\u011fin Hindistan\u2019\u0131n \u00c7erapun\u00e7i kasabas\u0131nda y\u0131ll\u0131k ya\u011f\u0131\u015f miktar\u0131 12000 mm\u2019yi bulmaktad\u0131r.<\/p>\n
Yaz aylar\u0131nda orografik ya\u011f\u0131\u015flar g\u00f6r\u00fcl\u00fcr.<\/p>\n
Orografik Ya\u011f\u0131\u015flar : Nemli hava k\u00fctlelerinin bir da\u011f yamac\u0131na \u00e7arparak y\u00fckselmesi sonucunda olu\u015fan ya\u011f\u0131\u015flard\u0131r.<\/p>\n
Muson \u0130kliminin Do\u011fal Bitki \u00d6rt\u00fcs\u00fc<\/p>\n
Ya\u011f\u0131\u015f\u0131n fazla oldu\u011fu yerlerde, k\u0131\u015f aylar\u0131nda yapraklar\u0131n\u0131 d\u00f6ken yayvan yaprakl\u0131 a\u011fa\u00e7lardan olu\u015fan ormanlar g\u00f6r\u00fcl\u00fcr. Bu ormanlara muson ormanlar\u0131 denir.<\/p>\n
Muson \u0130kliminin G\u00f6r\u00fcld\u00fc\u011f\u00fc Yerler<\/p>\n
G\u00fcney, Do\u011fu ve G\u00fcneydo\u011fu Asya k\u0131y\u0131lar\u0131nda,<\/p>\n
Madagaskar\u2019\u0131n do\u011fusunda,<\/p>\n
Avustralya\u2019n\u0131n kuzeydo\u011fusunda,<\/p>\n
Kuzey Amerika\u2019n\u0131n g\u00fcneydo\u011fu k\u0131y\u0131lar\u0131nda g\u00f6r\u00fcl\u00fcr.<\/p>\n
\u00c7\u00f6l \u0130klimi<\/p>\n
\u00c7\u00f6l \u0130kliminin \u00d6zellikleri<\/p>\n
G\u00fcnl\u00fck ve mevsimlik s\u0131cakl\u0131k farklar\u0131n\u0131n azla olmas\u0131 karakteristik \u00f6zelli\u011fidir.<\/p>\n
Ya\u011f\u0131\u015flar yok denecek kadar azd\u0131r.<\/p>\n
S\u0131cakl\u0131k farklar\u0131n\u0131n fazla olmas\u0131, kayalar\u0131n fiziksel olarak par\u00e7alan\u0131p ufalanmas\u0131na neden olur.<\/p>\n
Kimyasal \u00e7\u00f6z\u00fclme yetersiz oldu\u011fundan toprak olu\u015fumu zordur.<\/p>\n
\u00c7\u00f6l \u0130kliminin Do\u011fal Bitki \u00d6rt\u00fcs\u00fc<\/p>\n
Kurakl\u0131\u011fa uyum sa\u011flam\u0131\u015f olan kurak\u00e7\u0131l otlar ve \u00e7al\u0131lardan olu\u015fur. Kurakl\u0131\u011fa en iyi uyum sa\u011flam\u0131\u015f bitkiler, g\u00f6vdesinde \u00e7ok miktarda su biriktirebilen kakt\u00fcslerdir. \u00dczerlerindeki k\u00fc\u00e7\u00fck dikenler, bitkinin \u0131s\u0131 kayb\u0131n\u0131 azaltmaktad\u0131r. Ayr\u0131ca yer alt\u0131 sular\u0131n\u0131n y\u00fczeye \u00e7\u0131kt\u0131\u011f\u0131 yerlerde vahalar olu\u015fmu\u015ftur.<\/p>\n
Vaha : \u00c7\u00f6llerde suyun bulundu\u011fu, bitkilerin yeti\u015febildi\u011fi, insanlar\u0131n yerle\u015fip bar\u0131nd\u0131\u011f\u0131 yerdir. Vahalar akarsu boylar\u0131nda, kuyular\u0131n a\u00e7\u0131ld\u0131\u011f\u0131 yerlerde, b\u00fcy\u00fck su kaynaklar\u0131 yan\u0131nda geli\u015fmi\u015ftir.<\/p>\n
\u00c7\u00f6l \u0130kliminin G\u00f6r\u00fcld\u00fc\u011f\u00fc Yerler<\/p>\n
Asya K\u0131tas\u0131\u2019nda; Arabistan, Gobi, Taklamakan \u00c7\u00f6llerinde,<\/p>\n
Kuzey Amerika\u2019da; Kaliforniya, Nevada, Kolorado, Meksika \u00c7\u00f6llerinde,<\/p>\n
Afrika\u2019da; B\u00fcy\u00fck sahra, Kalahari, Namibya \u00c7\u00f6lleri\u2019nde,<\/p>\n
Avustralya\u2019da; B\u00fcy\u00fck Kum \u00c7\u00f6l\u00fc\u2019nde,<\/p>\n
G\u00fcney Amerika\u2019da; Atakama \u00c7\u00f6l\u00fc\u2019nde g\u00f6r\u00fcl\u00fcr.<\/p>\n
UYARI : \u00c7\u00f6llerin en b\u00fcy\u00fck b\u00f6l\u00fcm\u00fc Kuzey yar\u0131m K\u00fcre\u2019dedir. Bu durum, karalar\u0131n Kuzey Yar\u0131m K\u00fcre\u2019de G\u00fcney Yar\u0131m K\u00fcre\u2019den daha fazla olmas\u0131n\u0131n sonucudur.<\/p>\n
Il\u0131man Ku\u015fak \u0130klimleri<\/p>\n
Il\u0131man Ku\u015fak \u0130klimlerinin Ortak \u00d6zellikleri<\/p>\n
Y\u0131ll\u0131k s\u0131cakl\u0131k ortalamalar\u0131 20\u00b0C\u2019nin alt\u0131ndad\u0131r.<\/p>\n
S\u0131cakl\u0131k farklar\u0131 belirgindir.<\/p>\n
4 mevsim ya\u015fan\u0131r.<\/p>\n
Akdeniz \u0130klimi<\/p>\n
Akdeniz \u0130kliminin \u00d6zellikleri <\/p>\n
Yazlar\u0131 s\u0131cak ve kurak ge\u00e7er.<\/p>\n
Y\u0131ll\u0131k ortalama s\u0131cakl\u0131k 18\u00b0C – 20\u00b0C aras\u0131nda de\u011fi\u015fir.<\/p>\n
Yaz\u0131n geni\u015fleyen subtropikal antisiklon (DYB), Akdeniz iklim b\u00f6lgesinde yaz kurakl\u0131\u011f\u0131n\u0131 belirginle\u015ftirir.<\/p>\n
K\u0131\u015flar \u0131l\u0131k ve ya\u011f\u0131\u015fl\u0131d\u0131r. \u00c7\u00fcnk\u00fc k\u0131\u015f aylar\u0131nda gezici al\u00e7ak bas\u0131n\u00e7lar cephesel ya\u011f\u0131\u015flara neden olur.<\/p>\n
Y\u0131ll\u0131k ortalama ya\u011f\u0131\u015f miktar\u0131 600-1000 mm aras\u0131nda de\u011fi\u015fir ve ya\u011f\u0131\u015f rejimi d\u00fczensizdir.<\/p>\n
Kar ya\u011f\u0131\u015f\u0131 ve don olay\u0131 ender g\u00f6r\u00fcl\u00fcr.<\/p>\n
Don Olay\u0131 : Havan\u0131n a\u00e7\u0131k ve durgun oldu\u011fu k\u0131\u015f gecelerinde a\u015f\u0131r\u0131 \u0131s\u0131nma nedeniyle toprak donar. Don olay\u0131 tar\u0131msal \u00fcretime b\u00fcy\u00fck \u00f6l\u00e7\u00fcde zarar verir. Karasal b\u00f6lgelerde don olay\u0131 s\u0131k g\u00f6r\u00fcl\u00fcr.<\/p>\n
Akdeniz \u0130kliminin Do\u011fal Bitki \u00d6rt\u00fcs\u00fc<\/p>\n
K\u0131sa, bodur a\u011fa\u00e7 ve \u00e7al\u0131lard\u0131r. Bu bitki \u00f6rt\u00fcs\u00fcne maki ad\u0131 verilir. Yaz kurakl\u0131\u011f\u0131na uyum sa\u011flad\u0131\u011f\u0131ndan yapraklar\u0131 genellikle sert, t\u00fcyl\u00fc, ince ve uzundur.<\/p>\n
Zeytin, defne, ke\u00e7iboynuzu, mersin, lavanta, kekik ve zakkum maki bitki toplulu\u011fu i\u00e7inde yer al\u0131r.<\/p>\n
Akdeniz \u0130kliminin G\u00f6r\u00fcld\u00fc\u011f\u00fc Yerler<\/p>\n
Akdeniz \u00e7evresindeki \u00fclkelerde,<\/p>\n
G\u00fcney Portekiz k\u0131y\u0131lar\u0131nda,<\/p>\n
Afrika\u2019da Kap B\u00f6lgesi\u2019nde,<\/p>\n
G\u00fcneybat\u0131 Avustralya k\u0131y\u0131lar\u0131nda,<\/p>\n
Orta \u015eili\u2019de,<\/p>\n
Kuzey Amerika\u2019da Kaliforniya y\u00f6resinde,<\/p>\n
G\u00fcney Afrika Cumhuriyeti\u2019nin G\u00fcney k\u0131y\u0131lar\u0131nda g\u00f6r\u00fcl\u00fcr.<\/p>\n
UYARI : Akdeniz iklimi genellikle 30\u00b0-40\u00b0 enlemleri aras\u0131nda g\u00f6r\u00fcl\u00fcr.<\/p>\n
Il\u0131man Ku\u015fak Okyanus \u0130klimi<\/p>\n
Il\u0131man Ku\u015fak Okyanus \u0130kliminin \u00d6zellikleri<\/p>\n
Orta Ku\u015fak k\u0131talar\u0131n\u0131n bat\u0131 k\u0131y\u0131lar\u0131nda, bat\u0131 r\u00fczgarlar\u0131n\u0131n ve s\u0131cak su ak\u0131nt\u0131lar\u0131n\u0131n etkisiyle geli\u015fen bir iklim tipidir.<\/p>\n
Y\u0131ll\u0131k ortalama s\u0131cakl\u0131k 20\u00b0C\u2019nin alt\u0131ndad\u0131r.<\/p>\n
S\u0131cakl\u0131k farklar\u0131 belirgin de\u011fildir.<\/p>\n
Yazlar serin ve ya\u011f\u0131\u015fl\u0131, k\u0131\u015flar \u0131l\u0131k ve ya\u011f\u0131\u015fl\u0131 ge\u00e7er.<\/p>\n
Her mevsim ya\u011f\u0131\u015fl\u0131d\u0131r. Sonbahar ve k\u0131\u015f ya\u011f\u0131\u015flar\u0131 daha belirgindir.<\/p>\n
Kar ya\u011f\u0131\u015f\u0131 ve don olay\u0131 ender g\u00f6r\u00fcl\u00fcr.<\/p>\n
K\u0131\u015f aylar\u0131nda cephesel, yaz aylar\u0131nda hem cephesel hem de y\u00fckselim ya\u011f\u0131\u015flar\u0131 g\u00f6r\u00fcl\u00fcr.<\/p>\n
UYARI : Okyanus ikliminin belirmesinde temel etken bat\u0131 r\u00fczgarlar\u0131 ve s\u0131cak su ak\u0131nt\u0131lar\u0131d\u0131r.<\/p>\n
Il\u0131man Ku\u015fak Okyanus \u0130kliminin Do\u011fal Bitki \u00d6rt\u00fcs\u00fc<\/p>\n
Yayvan ve i\u011fne yaprakl\u0131 a\u011fa\u00e7lardan olu\u015fan karma ormanlard\u0131r.<\/p>\n
Yer yer \u00e7ay\u0131rlar g\u00f6r\u00fcl\u00fcr.<\/p>\n
Il\u0131man Ku\u015fak Okyanus \u0130kliminin G\u00f6r\u00fcld\u00fc\u011f\u00fc Yerler<\/p>\n
Kuzey Amerika\u2019n\u0131n bat\u0131 ve g\u00fcneydo\u011fu k\u0131y\u0131lar\u0131nda, <\/p>\n
G\u00fcney Amerika\u2019n\u0131n g\u00fcneybat\u0131 k\u0131y\u0131lar\u0131nda,<\/p>\n
Bat\u0131 Avrupa\u2019n\u0131n Atlas Okyanusu k\u0131y\u0131lar\u0131nda,<\/p>\n
Yeni Zellanda\u2019da,<\/p>\n
Afrika\u2019n\u0131n g\u00fcneyinde,<\/p>\n
Avustralya\u2019n\u0131n do\u011fusunda,<\/p>\n
Tasmanya\u2019da g\u00f6r\u00fcl\u00fcr.<\/p>\n
Il\u0131man Ku\u015fak Karasal \u0130klim<\/p>\n
Il\u0131man Ku\u015fak Karasal \u0130klimin \u00d6zellikleri<\/p>\n
Yazlar s\u0131cak ve kurak, k\u0131\u015flar so\u011fuk ve kar ya\u011f\u0131\u015fl\u0131 ge\u00e7er.<\/p>\n
G\u00fcnl\u00fck ve mevsimlik s\u0131cakl\u0131k farklar\u0131 belirgindir.<\/p>\n
En ya\u011f\u0131\u015fl\u0131 mevsim ilkbahard\u0131r.<\/p>\n
Don olay\u0131 s\u0131k g\u00f6r\u00fcl\u00fcr.<\/p>\n
S\u0131cak \u00e7\u00f6llerin kenarlar\u0131nda g\u00f6r\u00fclen karasal iklimde yaz mevsimi k\u0131sa s\u00fcrer.<\/p>\n
UYARI : Il\u0131man karasal iklimde k\u0131\u015f aylar\u0131ndaki ya\u011f\u0131\u015f azl\u0131\u011f\u0131, termik y\u00fcksek bas\u0131nc\u0131n etkili olmas\u0131na ba\u011fl\u0131d\u0131r. Yaz\u0131n g\u00f6r\u00fclen ya\u011f\u0131\u015flar ise konveksiyoneldir.<\/p>\n
Il\u0131man Ku\u015fak Karasal \u0130klimin Do\u011fal Bitki \u00d6rt\u00fcs\u00fc<\/p>\n
\u0130lkbahar ya\u011f\u0131\u015flar\u0131yla ye\u015feren, yaz kurakl\u0131\u011f\u0131 ile sararan k\u0131sa boylu otlard\u0131r. Bunlara step ya da bozk\u0131r denir. Steplere Kuzey Amerika\u2019da preri, G\u00fcney Amerika\u2019da pampa ad\u0131 verilir. Y\u00fcksek yerlerde yer yer i\u011fne yaprakl\u0131 a\u011fa\u00e7lar g\u00f6r\u00fcl\u00fcr.<\/p>\n
Il\u0131man Ku\u015fak Karasal \u0130kliminin G\u00f6r\u00fcld\u00fc\u011f\u00fc Yerler<\/p>\n
Kuzey ve G\u00fcney Amerika\u2019n\u0131n i\u00e7 k\u0131s\u0131mlar\u0131nda,<\/p>\n
Anadolu\u2019nun i\u00e7 k\u0131s\u0131mlar\u0131nda, <\/p>\n
Irak\u2019ta,<\/p>\n
\u0130ran\u2019da,<\/p>\n
T\u00fcrkistan\u2019da,<\/p>\n
Afrika\u2019n\u0131n i\u00e7 k\u0131s\u0131mlar\u0131nda,<\/p>\n
Avustralya\u2019n\u0131n i\u00e7 k\u0131s\u0131mlar\u0131nda g\u00f6r\u00fcl\u00fcr.<\/p>\n
So\u011fuk Ku\u015fak \u0130klimleri<\/p>\n
60\u00b0 – 90\u00b0 enlemleri aras\u0131nda g\u00f6r\u00fcl\u00fcr.<\/p>\n
S\u0131cakl\u0131k y\u0131l boyunca d\u00fc\u015f\u00fckt\u00fcr.<\/p>\n
\u0130klimin elveri\u015fsiz olmas\u0131 tar\u0131m\u0131 s\u0131n\u0131rland\u0131rmaktad\u0131r.<\/p>\n
So\u011fuk Ku\u015fak Karasal \u0130klim<\/p>\n
So\u011fuk Ku\u015fak Karasal \u0130klimin \u00d6zellikleri<\/p>\n
Bu iklim iki alt b\u00f6l\u00fcme ayr\u0131l\u0131r.<\/p>\n
Yaz\u0131 ve K\u0131\u015f\u0131 So\u011fuk Karasal \u0130klim<\/p>\n
Y\u0131ll\u0131k s\u0131cakl\u0131k farklar\u0131 belirgindir.<\/p>\n
Yazlar so\u011fuk, yer yer serin ve k\u0131sa, k\u0131\u015flar ise \u00e7ok so\u011fuk, uzun ve karl\u0131 ge\u00e7er. Kar uzun s\u00fcre toprakta kal\u0131r.<\/p>\n
En ya\u011f\u0131\u015fl\u0131 mevsim yazd\u0131r ve konveksiyonel ya\u011f\u0131\u015f g\u00f6r\u00fcl\u00fcr.<\/p>\n
S\u0131cakl\u0131k ortalamalar\u0131n\u0131n Ekvator\u2019a do\u011fru gidildik\u00e7e artmas\u0131na ba\u011fl\u0131 olarak bu iklim tipi de\u011fi\u015fir ve yazlar\u0131 s\u0131cak karasal iklime ge\u00e7ilir.<\/p>\n
Yazlar\u0131 S\u0131cak Karasal \u0130klim<\/p>\n
K\u0131\u015f s\u0131caklar\u0131 -10\u00b0C\u2019nin alt\u0131na inmez.<\/p>\n
Yaz s\u0131cakl\u0131klar\u0131 20\u00b0C nin \u00fcst\u00fcne \u00e7\u0131kar.<\/p>\n
Ya\u011f\u0131\u015f miktar\u0131 fazlad\u0131r. \u0130lkbahar ve yaz ya\u011f\u0131\u015flar\u0131 daha belirgindir.<\/p>\n
So\u011fuk Ku\u015fak Karasal \u0130klimin Do\u011fal Bitki \u00d6rt\u00fcs\u00fc<\/p>\n
\u0130\u011fne yaprakl\u0131 a\u011fa\u00e7lardan olu\u015fan ormanlard\u0131r. Bu bitki \u00f6rt\u00fcs\u00fcne tayga ad\u0131 verilir.<\/p>\n
Yer yer \u00e7ay\u0131rlar g\u00f6r\u00fcl\u00fcr.<\/p>\n
So\u011fuk Ku\u015fak Karasal \u0130klimin G\u00f6r\u00fcld\u00fc\u011f\u00fc Yerler<\/p>\n
So\u011fuk ku\u015fa\u011f\u0131n yazlar\u0131 s\u0131cak karasal iklimi,<\/p>\n
ABD\u2019nin kuzeydo\u011fusunda,<\/p>\n
Kanada\u2019da,<\/p>\n
Kuzey \u00c7in\u2019de,<\/p>\n
Man\u00e7urya\u2019da,<\/p>\n
Rusya\u2019da,<\/p>\n
Orta Sibirya\u2019da g\u00f6r\u00fcl\u00fcr.<\/p>\n
So\u011fuk ku\u015fa\u011f\u0131n yazlar\u0131 da so\u011fuk karasal iklimi,<\/p>\n
Asya, Avrupa ve Amerika k\u0131talar\u0131n\u0131n kuzeyinde, tundra ikliminin alt\u0131nda bir ku\u015fak halinde g\u00f6r\u00fcl\u00fcr.<\/p>\n
Tundra \u0130klimi<\/p>\n
Tundra \u0130kliminin \u00d6zellikleri
\n Yazlar \u00e7ok k\u0131sa ve serin ge\u00e7er. Yaz s\u0131cakl\u0131\u011f\u0131 10\u00b0C\u2019nin \u00fcst\u00fcne \u00e7\u0131kmaz.
\n Y\u0131ll\u0131k ya\u011f\u0131\u015f miktar\u0131 250 mm civar\u0131ndad\u0131r.
\n K\u0131\u015flar \u00e7ok so\u011fuk ve uzun ge\u00e7er.
\n Toprak k\u0131\u015f aylar\u0131nda donmu\u015f haldedir.
\n Yaz aylar\u0131nda topra\u011f\u0131n \u00fcst k\u0131s\u0131mlar\u0131nda \u00e7\u00f6z\u00fclmeler g\u00f6r\u00fcl\u00fcr ve batakl\u0131klar olu\u015fur. <\/p>\n
Tundra \u0130kliminin Do\u011fal Bitki \u00d6rt\u00fcs\u00fc<\/p>\n
D\u00fc\u015f\u00fck s\u0131cakl\u0131\u011fa ve kurakl\u0131\u011fa uyum sa\u011flam\u0131\u015f olan k\u0131sa boylu \u00e7al\u0131lar, otlar ve yosunlard\u0131r.<\/p>\n
Bu bitki \u00f6rt\u00fcs\u00fcne tundra ad\u0131 verilir.<\/p>\n
Tundra \u0130kliminin G\u00f6r\u00fcld\u00fc\u011f\u00fc Yerler<\/p>\n
60\u00b0-70\u00b0 enlemleri aras\u0131nda,<\/p>\n
Asya\u2019da,<\/p>\n
Avrupa\u2019da,<\/p>\n
Kanada\u2019n\u0131n kuzey k\u0131s\u0131mlar\u0131nda,<\/p>\n
G\u00fcney Amerika\u2019n\u0131n g\u00fcney k\u0131s\u0131mlar\u0131nda g\u00f6r\u00fcl\u00fcr.<\/p>\n
Kutup \u0130klimi<\/p>\n
Kutup \u0130kliminin \u00d6zellikleri<\/p>\n
S\u0131cakl\u0131k y\u0131l boyunca 0\u00b0C\u2019nin alt\u0131ndad\u0131r.<\/p>\n
S\u0131cakl\u0131\u011f\u0131n d\u00fc\u015f\u00fck olmas\u0131 buharla\u015fmay\u0131 engelledi\u011fi i\u00e7in ya\u011f\u0131\u015f az ve kar bi\u00e7imindedir.<\/p>\n
S\u00fcrekli donmu\u015f halde olan toprak kar ve buz ile kapl\u0131d\u0131r.<\/p>\n
Kutup \u0130kliminin Do\u011fal Bitki \u00d6rt\u00fcs\u00fc<\/p>\n
Toprak , s\u00fcrekli kar ve buz \u00f6rt\u00fcs\u00fc ile kapl\u0131 oldu\u011fu i\u00e7in bitki \u00f6rt\u00fcs\u00fcnden s\u00f6z edilemez.<\/p>\n
Kutup \u0130kliminin G\u00f6r\u00fcld\u00fc\u011f\u00fc Yerler<\/p>\n
Kutuplar \u00e7evresinde,<\/p>\n
Gr\u00f6nland\u2019da,<\/p>\n
Antartika\u2019da g\u00f6r\u00fcl\u00fcr.<\/p>\n","protected":false},"excerpt":{"rendered":"
D\u00fcnya\u2019da G\u00f6r\u00fclen \u0130klim Tipleri Bir yerde benzer s\u0131cakl\u0131k, bas\u0131n\u00e7, r\u00fczgar, nemlilik ve ya\u011f\u0131\u015f \u00f6zelliklerinin uzun s\u00fcre etkili olmas\u0131yla iklim tipleri belirmektedir. \u0130klimi olu\u015fturan bu \u00f6\u011felerden birinin ya da ikisinin farkl\u0131 olmas\u0131, de\u011fi\u015fik iklim tiplerinin ortaya \u00e7\u0131kmas\u0131na neden olur. D\u00fcnya\u2019da g\u00f6r\u00fclen iklimler, s\u0131cak ku\u015fak iklimleri, \u0131l\u0131man ku\u015fak iklimleri ve so\u011fuk ku\u015fak iklimleri olarak \u00fc\u00f6\u00e7 ana b\u00f6l\u00fcmde …<\/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":[2158,3778,3769,3770,3773,3775,3774,3776,3777,3687,3134,3771,3772,3779],"class_list":["post-1295","post","type-post","status-publish","format-standard","hentry","category-odevler","category-sosyal-bilgiler-odevleri","tag-basinc","tag-col-iklimi","tag-dunyada-iklim-ve-dogal-bitki-ortusu","tag-dunyada-gorulen-iklim-tipleri","tag-ekvatoral-iklim","tag-ekvatoral-iklimin-goruldugu-yerler","tag-konveksiyonel-yagis","tag-muson-iklimi","tag-muson-ikliminin-ozellikleri","tag-nemlilik","tag-ruzgar","tag-sicak-kusak-iklimleri","tag-sicak-kusak-iklimlerinin-ortak-ozellikleri","tag-vaha"],"_links":{"self":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/1295","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=1295"}],"version-history":[{"count":0,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/1295\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/media?parent=1295"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/categories?post=1295"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/tags?post=1295"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}