\nD\u00fcnyay\u0131 \u00e7epe\u00e7evre saran ve i\u00e7inde \u00e7e\u015fitli gazlar\u0131n bulundu\u011fu tabakaya denir. Atmosferde %78 azot, %21 oksijen, %1 su buhar\u0131, karbondioksit vb. gazlar vard\u0131r. <\/p>\n
ATMOSFER\u0130N KATMANLARI<\/p>\n
TROPOSFER <\/p>\n
Kal\u0131nl\u0131\u011f\u0131 Ekvatorda fazla , Kutuplarda azd\u0131r.
\nBunun sebepleri:
\nS\u0131cakl\u0131\u011f\u0131n etkisiyle Ekvatorda y\u00fckselici, kutuplarda al\u00e7al\u0131c\u0131 hava hareketlerinin olmas\u0131,
\nYer\u00e7ekiminin kutuplarda fazla, ekvatorda az olmas\u0131.
\n\u00c7izgisel h\u0131z ve savrulman\u0131n Ekvatorda daha fazla olmas\u0131d\u0131r. <\/p>\n
TROPOSFER\u0130N \u00d6ZELL\u0130KLER\u0130 <\/p>\n
Atmosferde bulunan gazlar\u0131n %75 \u2018i ve su buhar\u0131n\u0131n tamam\u0131 bu katmandad\u0131r.
\nYo\u011funlu\u011fu en fazla olan katmand\u0131r.
\nYery\u00fcz\u00fcn\u00fc etkileyen b\u00fct\u00fcn iklim olaylar\u0131 bu katmanda g\u00f6r\u00fcl\u00fcr.
\nTroposfer daha \u00e7ok yerden yans\u0131yan\u0131\u015f\u0131nlarla alttan itibaren \u0131s\u0131nd\u0131\u011f\u0131 i\u00e7in y\u00fckseldik\u00e7e s\u0131cakl\u0131k azal\u0131r.
\nYatay y\u00f6nde de Ekvatordan kutuplara do\u011fru s\u0131cakl\u0131k azal\u0131r. Sebebi, d\u00fcnyan\u0131n \u015feklinden dolay\u0131 g\u00fcne\u015f \u0131\u015f\u0131nlar\u0131n\u0131n d\u00fc\u015fme a\u00e7\u0131s\u0131n\u0131n k\u00fc\u00e7\u00fclmesidir. <\/p>\n
STRATOSFER <\/p>\n
\u0130klim olaylar\u0131 g\u00f6r\u00fclmez. S\u0131cakl\u0131k de\u011fi\u015fimi yok gibidir. <\/p>\n
MEZOSFER (\u015eEMOSFER) <\/p>\n
Yery\u00fcz\u00fcndeki, \u015fiddetli patlamalar gibi a\u015f\u0131r\u0131 y\u00fcksek sesler, mezosferdeki y\u00fcksek \u0131s\u0131 tabakas\u0131 taraf\u0131ndan geriye yans\u0131t\u0131l\u0131r. <\/p>\n
OZON TABAKASI <\/p>\n
Ozon,\u00fc\u00e7 tane oksijen atomunun birle\u015fmesiyle olu\u015fmaktad\u0131r.
\nG\u00fcne\u015ften gelen zararl\u0131 \u0131\u015f\u0131nlar\u0131 tutar, a\u015f\u0131r\u0131 s\u0131nma ve so\u011fumay\u0131 \u00f6nler. <\/p>\n
TERMOSFER (\u0130YONOSFER)
\nMezosferin \u00fcst\u00fcndeki kat olup ultraviyole \u0131\u015f\u0131nlar\u0131n\u0131n emilmesi nedeniyle \u0131s\u0131, y\u00fckselti ile beraber s\u00fcrekli artar.
\nRadyo dalgalar\u0131n\u0131 en iyi yans\u0131tan tabakad\u0131r.
\nEKZOSFER
\nAtmosferin en d\u0131\u015f s\u0131n\u0131r\u0131d\u0131r. Yer \u00e7ekiminin giderek azalmas\u0131 ve tamamen kaybolmas\u0131 nedeniyle baz\u0131 hava molek\u00fclleri uzaya f\u0131rlay\u0131p giderler.Bu sebeple kal\u0131nl\u0131\u011f\u0131 tam olarak bilinmez <\/p>\n
ATMOSFER\u0130N FAYDALARI <\/p>\n
\u2022G\u00fcne\u015ften gelen zararl\u0131 \u0131\u015f\u0131nlar\u0131 s\u00fczer.
\n\u2022Meteorlar\u0131n d\u00fcnyam\u0131za d\u00fc\u015fmesini b\u00fcy\u00fck oranda engeller.
\n\u2022Canl\u0131lar i\u00e7in gerekli gazlar\u0131 bulundurur.
\n\u2022\u0130klim olaylar\u0131 meydana gelir.
\n\u2022D\u00fcnyam\u0131z\u0131n a\u015f\u0131r\u0131 \u0131s\u0131nmas\u0131n\u0131 ve so\u011fumas\u0131n\u0131 engeller.
\n\u2022G\u00fcne\u015f \u0131\u015f\u0131nlar\u0131n\u0131 da\u011f\u0131t\u0131r. B\u00f6ylece g\u00f6lgede kalan yerlerin de ayd\u0131nlanmas\u0131n\u0131 sa\u011flar.
\n\u2022D\u00fcnya ile birlikte d\u00f6nerek s\u00fcrt\u00fcnmeden do\u011facak yanmay\u0131 engeller.<\/p>\n","protected":false},"excerpt":{"rendered":"
D\u00fcnyay\u0131 \u00e7epe\u00e7evre saran ve i\u00e7inde \u00e7e\u015fitli gazlar\u0131n bulundu\u011fu tabakaya denir. Atmosferde %78 azot, %21 oksijen, %1 su buhar\u0131, karbondioksit vb. gazlar vard\u0131r. ATMOSFER\u0130N KATMANLARI TROPOSFER Kal\u0131nl\u0131\u011f\u0131 Ekvatorda fazla , Kutuplarda azd\u0131r. Bunun sebepleri: S\u0131cakl\u0131\u011f\u0131n etkisiyle Ekvatorda y\u00fckselici, kutuplarda al\u00e7al\u0131c\u0131 hava hareketlerinin olmas\u0131, Yer\u00e7ekiminin kutuplarda fazla, ekvatorda az olmas\u0131. \u00c7izgisel h\u0131z ve savrulman\u0131n Ekvatorda daha fazla …<\/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":[2796,2887,2338,2164,4251,2835],"class_list":["post-5031","post","type-post","status-publish","format-standard","hentry","category-odevler","category-sosyal-bilgiler-odevleri","tag-atmosfer","tag-ekvator","tag-karbondioksit","tag-oksijen","tag-ozon","tag-troposfer"],"_links":{"self":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/5031","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=5031"}],"version-history":[{"count":0,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/5031\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/media?parent=5031"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/categories?post=5031"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/tags?post=5031"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}