YA\u011eI\u015e: Havadaki su buhar\u0131n\u0131n yo\u011funla\u015farak t\u00fcrl\u00fc bi\u00e7imlerde yere d\u00fc\u015fmesidir. Herhangi bir yerde ya\u011f\u0131\u015f\u0131n ger\u00e7ekle\u015febilmesi i\u00e7in \u015fu iki ko\u015ful gerekir<\/p>\n
\u00b7Havada bir miktar nem olmas\u0131
\n\u00b7Hava s\u0131cakl\u0131\u011f\u0131n\u0131n d\u00fc\u015fmesi<\/p>\n
D\u00fcnyan\u0131n hemen her yerinde havada daima bir nem bulunur. Ya\u011f\u0131\u015flar\u0131n olu\u015fmas\u0131nda, havadaki su buhar\u0131 miktar\u0131n\u0131n yan\u0131 s\u0131ra en \u00f6nemli fakt\u00f6r havan\u0131n so\u011fumas\u0131d\u0131r. O halde ya\u011f\u0131\u015f olay\u0131; esas olarak hava s\u0131cakl\u0131\u011f\u0131n\u0131n d\u00fc\u015fmesi ile ger\u00e7ekle\u015fir. Bir yerdeki hava, neme ne kadar doymu\u015f olursa olsun, havan\u0131n s\u0131cakl\u0131\u011f\u0131 d\u00fc\u015fmedik\u00e7e ya\u011f\u0131\u015f olu\u015fmaz. Bu bak\u0131mdan ya\u011f\u0131\u015flar\u0131n s\u0131n\u0131fland\u0131r\u0131lmas\u0131nda so\u011fuman\u0131n olu\u015fma bi\u00e7imi esas al\u0131n\u0131r. \u00dc\u00e7 \u00e7e\u015fit ya\u011f\u0131\u015f tipi vard\u0131r. Bunlar;<\/p>\n
\u00b7Orografik Ya\u011f\u0131\u015flar
\n\u00b7Cephe Ya\u011f\u0131\u015flar\u0131
\n\u00b7Konveksiyonel Ya\u011f\u0131\u015flard\u0131r. <\/p>\n
OROGRAF\u0130K YA\u011eI\u015eLAR (YAMA\u00c7 YA\u011eI\u015eLARI)
\nYama\u00e7larda olu\u015fur. Yama\u00e7lar boyunca y\u00fckselen hava, giderek so\u011fur ve i\u00e7lerindeki nemi ya\u011f\u0131\u015f olarak b\u0131rak\u0131r. Yama\u00e7lar boyunca y\u00fckselen hava k\u00fctlelerinin b\u0131rakt\u0131klar\u0131 ya\u011f\u0131\u015f miktar\u0131; hava i\u00e7indeki neme, da\u011flar\u0131n y\u00fcksekli\u011fine ve yer \u015fekillerine ba\u011fl\u0131d\u0131r. Bu ya\u011f\u0131\u015f t\u00fcr\u00fc; esas olarak da\u011flar\u0131n okyanuslara, denizlere ve g\u00f6llere bakan yama\u00e7lar\u0131nda g\u00f6r\u00fcl\u00fcr. Kuzey Anadolu da\u011flar\u0131 ile Toroslar\u0131n denize bakan yama\u00e7lar\u0131, orografik ya\u011f\u0131\u015flar i\u00e7in olduk\u00e7a elveri\u015flidir. Bu nedenle buralar yurdumuzun en \u00e7ok ya\u011f\u0131\u015f alan yerleridir. T\u00fcrkiye\u2019de ya\u011f\u0131\u015f da\u011f\u0131l\u0131\u015f\u0131 haritas\u0131 ile yer \u015fekilleri haritas\u0131 aras\u0131ndaki benzerlik orografik ya\u011f\u0131\u015flar taraf\u0131ndan a\u00e7\u0131klanabilir.<\/p>\n
KONVEKS\u0130YONEL YA\u011eI\u015eLAR
\nIs\u0131nan hava y\u00fckselir. Y\u00fckselen hava ise giderek so\u011fur ve i\u00e7indeki nemi ta\u015f\u0131yamayarak b\u0131rak\u0131r. B\u00f6ylece konveksiyon ya\u011f\u0131\u015f olu\u015fur. Bu t\u00fcr ya\u011f\u0131\u015flar genellikle da\u011flarla \u00e7evrili i\u00e7 k\u0131s\u0131mlarda g\u00f6r\u00fcl\u00fcr ve \u00e7ok sa\u011fanak bi\u00e7imindedir. Ekvatoral b\u00f6lgedeki ya\u011f\u0131\u015flar\u0131n bir k\u0131sm\u0131 ile orta ku\u015fak \u00fclkelerinde yaz g\u00fcnlerinde g\u00f6r\u00fclen ya\u011f\u0131\u015flar bu t\u00fcrdendir. \u0130lkbahar mevsiminde ve yaz ba\u015flar\u0131nda g\u00f6r\u00fclen k\u0131rkikindi ya\u011f\u0131\u015flar\u0131 konveksiyonel ya\u011f\u0131\u015flardand\u0131r. K\u0131rkikindi ya\u011f\u0131\u015flar\u0131 \u00fclkemizde \u0130\u00e7 Anadolu B\u00f6lgesinde g\u00f6r\u00fcl\u00fcr. \u0130\u00e7 b\u00f6lgelerde \u0130lkbahar sonu ve yaz ba\u015f\u0131ndaki ya\u011f\u0131\u015flar\u0131n \u00e7o\u011fu bu karakterdedir.
\n Ekvatoral b\u00f6lgelerin bol ya\u011f\u0131\u015fl\u0131 olmas\u0131n\u0131 sa\u011flayan etmen, burada y\u00fckselici hava hareketlerinin olmas\u0131 sonucu, konveksiyonel ya\u011f\u0131\u015flar\u0131n y\u0131l\u0131n b\u00fcy\u00fck bir b\u00f6l\u00fcm\u00fcnde ger\u00e7ekle\u015fmesidir.<\/p>\n
CEPHE YA\u011eI\u015eLARI
\nS\u0131cakl\u0131klar\u0131 ve yo\u011funluklar\u0131 farkl\u0131 hava k\u00fctlelerinin kar\u015f\u0131la\u015ft\u0131klar\u0131 yerlere cephe denir. S\u0131cak ve so\u011fuk hava k\u00fctlelerinin kar\u015f\u0131la\u015fma alanlar\u0131nda olu\u015furlar. S\u0131cak ve so\u011fuk hava k\u00fctleleri kar\u015f\u0131la\u015f\u0131nca so\u011fuk hava, so\u011fuk hava s\u0131cak havan\u0131n alt\u0131na girer ve onun s\u0131cakl\u0131\u011f\u0131n\u0131 d\u00fc\u015f\u00fcr\u00fcr. S\u0131cak havan\u0131n yo\u011funlu\u011fu az oldu\u011fundan kar\u015f\u0131la\u015fma b\u00f6lgesinde so\u011fuk havan\u0131n \u00fczerine do\u011fru y\u00fckselir. Hem y\u00fckselme hem de so\u011fuk havayla kar\u015f\u0131la\u015fman\u0131n etkisiyle so\u011fuyan s\u0131cak hava k\u00fctlesi, yeterince nem ta\u015f\u0131yorsa ya\u011f\u0131\u015f b\u0131rak\u0131r. B\u00f6ylece cephe ya\u011f\u0131\u015f\u0131 meydana gelmi\u015f olur. Cephe ya\u011f\u0131\u015flar\u0131, hava k\u00fctlelerinin hareketlerine ba\u011fl\u0131 olarak de\u011fi\u015fik yer ve zamanda g\u00f6r\u00fcl\u00fcrler. Yurdumuzdaki ya\u011f\u0131\u015flar\u0131n \u00e7o\u011fu bu karakterdedir. Sonbahardan itibaren \u00f6zellikle Balkanlar \u00fczerinden gelen so\u011fuk hava k\u00fctleleri, g\u00fcneyden sokulan s\u0131cak cephelerle kar\u015f\u0131la\u015f\u0131nca, ba\u015fta Marmara ve Ege b\u00f6lgeleri olmak \u00fczere Bat\u0131 Anadolu bol ya\u011f\u0131\u015f al\u0131r. Akdeniz \u00fczerinde olu\u015fan cephelerde Akdeniz ve Ege b\u00f6lgelerini etkiler. Bu cephesel faaliyetler sayesinde Marmara, Ege ve Akdeniz b\u00f6lgelerinde k\u0131\u015f mevsimi bol ya\u011f\u0131\u015fl\u0131 ge\u00e7er. \u0130lkbaharla birlikte bu cephelerin kuzeye ve do\u011fuya \u00e7ekilmesiyle Bat\u0131 Anadolu ve Akdeniz\u2019de ya\u011f\u0131\u015fs\u0131z d\u00f6nem ba\u015flar.<\/p>\n","protected":false},"excerpt":{"rendered":"
YA\u011eI\u015e: Havadaki su buhar\u0131n\u0131n yo\u011funla\u015farak t\u00fcrl\u00fc bi\u00e7imlerde yere d\u00fc\u015fmesidir. Herhangi bir yerde ya\u011f\u0131\u015f\u0131n ger\u00e7ekle\u015febilmesi i\u00e7in \u015fu iki ko\u015ful gerekir \u00b7Havada bir miktar nem olmas\u0131 \u00b7Hava s\u0131cakl\u0131\u011f\u0131n\u0131n d\u00fc\u015fmesi D\u00fcnyan\u0131n hemen her yerinde havada daima bir nem bulunur. Ya\u011f\u0131\u015flar\u0131n olu\u015fmas\u0131nda, havadaki su buhar\u0131 miktar\u0131n\u0131n yan\u0131 s\u0131ra en \u00f6nemli fakt\u00f6r havan\u0131n so\u011fumas\u0131d\u0131r. O halde ya\u011f\u0131\u015f olay\u0131; esas olarak …<\/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":[3707,10203,10815,10814],"class_list":["post-5141","post","type-post","status-publish","format-standard","hentry","category-odevler","category-sosyal-bilgiler-odevleri","tag-cephe-yagislari","tag-konveksiyonel-yagislar","tag-orografik-yagislar","tag-yagislar-ve-olusum-bicimleri"],"_links":{"self":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/5141","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=5141"}],"version-history":[{"count":0,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/5141\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/media?parent=5141"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/categories?post=5141"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/tags?post=5141"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}