{"id":4812,"date":"2011-12-20T14:42:12","date_gmt":"2011-12-20T12:42:12","guid":{"rendered":"http:\/\/www.islamidavet.com\/kutuphane\/\/?p=4812"},"modified":"2011-12-20T14:42:12","modified_gmt":"2011-12-20T12:42:12","slug":"atmosferin-faydalari","status":"publish","type":"post","link":"https:\/\/www.islamidavet.com\/kutuphane\/atmosferin-faydalari\/","title":{"rendered":"Atmosferin faydalar\u0131"},"content":{"rendered":"<p>\u0130klim olaylar\u0131 meydana gelir.<br \/>\nCanl\u0131 ya\u015fam\u0131 i\u00e7in gerekli gazlar\u0131 ihtiva eder.<br \/>\nG\u00fcne\u015f\u2019ten gelen zararl\u0131 \u0131\u015f\u0131nlar\u0131 tutar.<br \/>\nD\u00fcnya\u2019n\u0131n a\u015f\u0131r\u0131 \u0131s\u0131nmas\u0131n\u0131 ve so\u011fumas\u0131n\u0131 engeller.<br \/>\nD\u00fcnya ile birlikte d\u00f6nerek s\u00fcrt\u00fcnmeden do\u011facak yanmay\u0131 engeller.<br \/>\nUzaydan gelen meteorlar\u0131n par\u00e7alanmas\u0131na neden olur.<br \/>\nG\u00fcne\u015f \u0131\u015f\u0131nlar\u0131n\u0131n da\u011f\u0131lmas\u0131n\u0131 sa\u011flayarak, g\u00f6lgede kalan k\u0131s\u0131mlar\u0131n da ayd\u0131nlanmas\u0131n\u0131 sa\u011flar. Bir ba\u015fka ifade ile g\u00f6lgelerin tam karanl\u0131k olmas\u0131n\u0131 \u00f6nler.<br \/>\nI\u015f\u0131\u011f\u0131, sesi, s\u0131cakl\u0131\u011f\u0131 ge\u00e7irir ve iletilmesini sa\u011flar.<br \/>\nHava ak\u0131mlar\u0131 sayesinde g\u00fcnd\u00fcz olan kesimlerin a\u015f\u0131r\u0131 s\u0131cak, gece olan kesimlerin de a\u015f\u0131r\u0131 so\u011fuk olmas\u0131n\u0131 engeller. <\/p>\n<p>ATMOSFER\u0130N KATMANLARI<\/p>\n<p>Atmosferde, yer\u00e7ekimi etkisiyle i\u00e7 i\u00e7e k\u00fcrelerden meydana gelmi\u015ftir. Bunlar\u0131n yo\u011funluklar\u0131 ve bile\u015fimleri birbirinden farkl\u0131d\u0131r.<\/p>\n<p>Troposfer: Atmosferin en alt tabakas\u0131d\u0131r. Ekvator \u00fczerindeki kal\u0131nl\u0131\u011f\u0131 16 &#8211; 17 km, 45\u00b0 enlemlerinde 12 km, kutuplardaki kal\u0131nl\u0131\u011f\u0131 ise 9 &#8211; 10 km dir. Bunun nedeni, Ekvator\u2019daki hava k\u00fctlelerinin \u0131s\u0131narak y\u00fckselmesi, kutuplarda ise so\u011fuyan havan\u0131n a\u011f\u0131rla\u015farak al\u00e7almas\u0131d\u0131r. iklim olaylar\u0131 troposferin 3 &#8211; 4 km lik k\u0131sm\u0131nda meydana gelir. \u00c7\u00fcnk\u00fc, iklim olaylar\u0131nda \u00e7ok etkili olan su buhar\u0131 troposferin 3 &#8211; 4 km lik k\u0131sm\u0131nda bulunur. Troposfer daha \u00e7ok yerden yans\u0131yan \u0131\u015f\u0131nlarla \u0131s\u0131n\u0131r.<\/p>\n<p>Atmosferdeki gazlar\u0131n % 75&#8217;i troposfer kat\u0131nda bulunmaktad\u0131r. <\/p>\n<p>Stratosfer: Troposferden itibaren 17 &#8211; 30 km ler aras\u0131nda bulunur. Bu tabakada su buhar\u0131 olmad\u0131\u011f\u0131 i\u00e7in, iklim olay\u0131 g\u00f6r\u00fclmez. Stratosferde s\u0131cakl\u0131k de\u011fi\u015fimi yok gibidir. S\u0131cakl\u0131k \u201345\u00b0C civar\u0131ndad\u0131r. Stratosferde yer\u00e7ekimi \u00e7ok azald\u0131\u011f\u0131 i\u00e7in cisimler ger\u00e7ek a\u011f\u0131rl\u0131klar\u0131n\u0131 kaybederler. \u00dcst k\u0131s\u0131mlar\u0131nda ozon gaz\u0131 bulunur.<\/p>\n<p>\u015eemosfer: Stratosferden sonra 30 &#8211; 90 km ler aras\u0131nda bulunur. iki k\u0131s\u0131mdan olu\u015fur.<\/p>\n<p>a. Ozonosfer: i\u00e7erisinde bulundurdu\u011fu ozon gaz\u0131ndan dolay\u0131 bu ismi alm\u0131\u015ft\u0131r. G\u00fcne\u015f\u2019ten gelen ve canl\u0131 ya\u015fam\u0131 i\u00e7in zararl\u0131 olan \u0131\u015f\u0131nlar\u0131 (Ultraviyole \u0131\u015f\u0131nlar\u0131 gibi) tutar. Bundan dolay\u0131 canl\u0131lar\u0131n koruyucu kat\u0131d\u0131r. D\u00fcnya\u2019n\u0131n a\u015f\u0131r\u0131 \u0131s\u0131n\u0131p, so\u011fumas\u0131n\u0131 \u00f6nler.<\/p>\n<p>b. Kemosfer: Bu katmana kemosfer denilmesinin nedeni, i\u00e7erisinde baz\u0131 kimyasal olaylar\u0131n meydana gelmesidir. Az miktarda zararl\u0131 \u0131\u015f\u0131nlar\u0131n tutulmas\u0131 burada da g\u00f6r\u00fcl\u00fcr.<\/p>\n<p>\u0130yonosfer: \u015eemosferden sonra 90 &#8211; 300 km\u2019ler aras\u0131nda bulunur. Bu tabakadaki gazlar ultraviyole \u0131\u015f\u0131nlar\u0131n\u0131n etkisi ile iyonlara ayr\u0131lm\u0131\u015ft\u0131r. iyonla\u015fma s\u0131ras\u0131nda a\u00e7\u0131\u011fa \u00e7\u0131kan enerji ile s\u0131cakl\u0131\u011f\u0131 y\u00fckselmi\u015ftir. (250\u00b0C) iyonlar aras\u0131nda elektron al\u0131\u015fveri\u015fi son derece fazlad\u0131r. Bundan dolay\u0131 haberle\u015fme sinyalleri, radyo dalgalar\u0131 bu tabakadan yans\u0131r.<\/p>\n<p>Eksosfer: Atmosferin en \u00fcst ve en d\u0131\u015f s\u0131n\u0131r\u0131n\u0131 olu\u015fturur. Eksosferde baz\u0131 gaz molek\u00fclleri yer\u00e7ekimi etkisinden kurtularak uzaya ka\u00e7ar. Bu nedenle d\u0131\u015f s\u0131n\u0131r\u0131 kesin olarak tespit edilememekte, 10.000 km ye kadar \u00e7\u0131kt\u0131\u011f\u0131 san\u0131lmaktad\u0131r.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>\u0130klim olaylar\u0131 meydana gelir. Canl\u0131 ya\u015fam\u0131 i\u00e7in gerekli gazlar\u0131 ihtiva eder. G\u00fcne\u015f\u2019ten gelen zararl\u0131 \u0131\u015f\u0131nlar\u0131 tutar. D\u00fcnya\u2019n\u0131n a\u015f\u0131r\u0131 \u0131s\u0131nmas\u0131n\u0131 ve so\u011fumas\u0131n\u0131 engeller. D\u00fcnya ile birlikte d\u00f6nerek s\u00fcrt\u00fcnmeden do\u011facak yanmay\u0131 engeller. Uzaydan gelen meteorlar\u0131n par\u00e7alanmas\u0131na neden olur. G\u00fcne\u015f \u0131\u015f\u0131nlar\u0131n\u0131n da\u011f\u0131lmas\u0131n\u0131 sa\u011flayarak, g\u00f6lgede kalan k\u0131s\u0131mlar\u0131n da ayd\u0131nlanmas\u0131n\u0131 sa\u011flar. Bir ba\u015fka ifade ile g\u00f6lgelerin tam karanl\u0131k olmas\u0131n\u0131 \u00f6nler. &hellip;<\/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":[10364,3193,2730,2925,2839,2837,2836,2838,2835],"class_list":["post-4812","post","type-post","status-publish","format-standard","hentry","category-odevler","category-sosyal-bilgiler-odevleri","tag-atmosferin-faydalari","tag-eksosfer","tag-gunes","tag-iklim","tag-iyonosfer","tag-kemosfer","tag-ozonosfer","tag-stratosfer","tag-troposfer"],"_links":{"self":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/4812","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=4812"}],"version-history":[{"count":0,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/4812\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/media?parent=4812"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/categories?post=4812"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/tags?post=4812"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}