ATMOSFER (HAVA K\u00dcRE)<\/p>\n
D\u00fcnyay\u0131 saran gaz tabakas\u0131d\u0131r,hava k\u00fcre ad\u0131na verilir. Atmosferdeki de\u011fi\u015fik gazlar yer \u00e7ekiminin etkisiyle \u00e7e\u015fitli y\u00fckseltilerde tutulur.Yer \u00e7ekiminin bitti\u011fi yerde atmosfer de biter.Uzay bo\u015flu\u011fu ba\u015flar.Atmosferi olu\u015fturan gazlar yer \u00e7ekimi etkisiyle a\u011f\u0131rl\u0131klar\u0131na g\u00f6re i\u00e7 i\u00e7e k\u00fcreler bi\u00e7iminde bulunurlar.A\u011f\u0131r gazlar (iki oksijen -azot-iki kobalt) gibi yere yak\u0131n alt tabakalarda hafif gazlar ise \u00fcst tabakalarda yer al\u0131r.( Yerden 9km y\u00fckseltiden sonra ya\u015famaya yetecek oksijen bulunmaz.17-18km sonra ise oksijen oran\u0131 iyice azal\u0131r ve bu katlarda ate\u015f yakacak kadar bir oksijen kalmaz.)<\/p>\n
Atmosferin kal\u0131nl\u0131\u011f\u0131, D\u00fcnyan\u0131n ekseni etraf\u0131nda d\u00f6nmesine ba\u011fl\u0131 olarak,kutuplarda az ekvatorda daha fazlad\u0131r.Ortalama kal\u0131nl\u0131\u011f\u0131 10.000km kadard\u0131r.<\/p>\n
<\/p>\n
ATMOSFER\u0130N ROL\u00dc<\/p>\n
1)- \u0130\u00e7erdi\u011fi oksijen arac\u0131l\u0131\u011f\u0131 ile ya\u015fama olanak tan\u0131r.<\/p>\n
2)- \u00d6zellikleri sayesinde, D\u00fcnyan\u0131n fazla \u0131s\u0131nmas\u0131n\u0131 ve fazla so\u011fumas\u0131n\u0131 \u00f6nler.<\/p>\n
3)- G\u00fcne\u015ften gelen k\u0131sa dalgal\u0131 zararl\u0131 \u0131\u015f\u0131nlar\u0131 s\u00fczerek d\u00fcnyay\u0131 ya\u015fan\u0131r hale getirir.<\/p>\n
4)- Hava ak\u0131mlar\u0131 yolu ile g\u00fcne\u015f alan yerlerin \u00e7ok s\u0131cak,olmayan yerlerin \u00e7ok so\u011fuk olmas\u0131n\u0131 \u00f6nler.E\u011fer atmosfer olmasayd\u0131 g\u00fcne\u015f alan\u0131 yerlerin tam olarak ayd\u0131nl\u0131k ve \u00e7ok s\u0131cak,g\u00f6lge yerlerin ise tam karanl\u0131k ve so\u011fuk olmas\u0131 gerekirdi.<\/p>\n
5)- G\u00fcne\u015ften gelen enerjinin uzaya d\u00f6nmesini \u00f6nleyen bir \u00f6rt\u00fc g\u00f6revi g\u00f6r\u00fcr.Atmosfer ayn\u0131 zamanda g\u00fcne\u015ften gelen \u0131\u015f\u0131\u011f\u0131n yans\u0131y\u0131p da\u011f\u0131larak g\u00f6lge yerlerinde ayd\u0131nl\u0131k olmas\u0131n\u0131 sa\u011flar.<\/p>\n
<\/p>\n
1)- TROPOSFER: Atmosferin en alt tabakas\u0131d\u0131r.ortalama13km kal\u0131nl\u0131\u011f\u0131ndaki troposfer yerden ekvatorda 16km kutuplarda 6km y\u00fcksekliktedir.troposferin kal\u0131nl\u0131\u011f\u0131ndaki de\u011fi\u015fme s\u0131cakl\u0131kla ilgilidir.(Ekvatorda \u0131s\u0131nan hava genle\u015ferek y\u00fcksektir.Kutuplarda ise so\u011fuyan hava a\u011f\u0131rla\u015farak al\u00e7al\u0131r.)<\/p>\n
* Atmosferdeki gazlar\u0131n %75’i bu katman dad\u0131r.<\/p>\n
*B\u00fct\u00fcn meteorolojik olaylar burada g\u00f6r\u00fcl\u00fcr.<\/p>\n
*Su buhar\u0131n\u0131n tamam\u0131 buradad\u0131r.<\/p>\n
*Atmosfer a\u015fa\u011f\u0131dan yukar\u0131ya do\u011fru \u0131s\u0131nd\u0131\u011f\u0131ndan,y\u00fckseldik\u00e7e s\u0131cakl\u0131k 100m. de 0,5 santigrat derece d\u00fc\u015fer.<\/p>\n
*Su buhar\u0131 troposferin d\u0131\u015f\u0131na \u00e7\u0131kmad\u0131\u011f\u0131ndan b\u00fct\u00fcn iklim olaylar\u0131 burada g\u00f6r\u00fcl\u00fcr.<\/p>\n
*Y\u00fckseldik\u00e7e \u0131s\u0131 d\u00fc\u015ft\u00fc\u011f\u00fcnden su buhar\u0131 troposferin d\u0131\u015f\u0131na \u00e7\u0131kmaz.<\/p>\n
<\/p>\n
2)-STRATOSFER:<\/p>\n
*S\u0131cakl\u0131k her yerde -50 santigrat derecede sabittir.<\/p>\n
*-Yatay hava hareketleri g\u00f6r\u00fcl\u00fcr.<\/p>\n
*Su buhar\u0131 olmad\u0131\u011f\u0131ndan bulut olu\u015fmaz.<\/p>\n
<\/p>\n
3)-MEZOSFER:<\/p>\n
a)-Ozonosfer:oksijen g\u00fcne\u015f \u0131\u015f\u0131klar\u0131n\u0131n etkisiyle (2oksijen) b\u00fcnyesine bir molek\u00fcl oksijen daha alarak (3oksijen) ozonu olu\u015fturur.<\/p>\n
G\u00fcne\u015ften gelen canl\u0131lar i\u00e7in zararl\u0131 olan k\u0131sa dalgal\u0131 (mor \u00f6tesi,ultravole) \u0131\u015f\u0131nlar\u0131 ozon taraf\u0131ndan tutulur.<\/p>\n
b)-Kemosfer:<\/p>\n
* Yer y\u00fcz\u00fcnden y\u00fckselen gazlar\u0131n bir k\u0131sm\u0131 lutra vole \u0131\u015f\u0131nlar\u0131n\u0131n etkisiyle iyonlar\u0131na ayr\u0131l\u0131r.\u0130yonla\u015fma sonucu \u0131s\u0131 artt\u0131\u011f\u0131ndan s\u0131cakl\u0131k 100santigratderece \u00e7\u0131kar.<\/p>\n
*G\u00fcne\u015ften gelen zararl\u0131 \u0131\u015f\u0131nlar\u0131n bir k\u0131sm\u0131 da burada tutulur.<\/p>\n
4)- \u0130YONOSFER:<\/p>\n
* Gaz molek\u00fcllerinin lutra vole \u0131\u015f\u0131nlar\u0131n\u0131n etkisiyle par\u00e7alanarak iyonlar\u0131na ayr\u0131\u015fmas\u0131 sonucunda a\u00e7\u0131\u011fa \u00e7\u0131kan enerji s\u0131cakl\u0131\u011f\u0131n 200 santigrat derece a\u015famas\u0131nda yol a\u00e7ar.<\/p>\n
* Atmosferdeki gazlar bu katmanda iyonlar\u0131na ayr\u0131l\u0131r.<\/p>\n
* \u0130yonosfer in \u00fcst kat\u0131na “Egzosfer” denir.<\/p>\n
* Egzosfer den sonra uzay bo\u015flu\u011fu ba\u015flar.<\/p>\n","protected":false},"excerpt":{"rendered":"
ATMOSFER (HAVA K\u00dcRE) D\u00fcnyay\u0131 saran gaz tabakas\u0131d\u0131r,hava k\u00fcre ad\u0131na verilir. Atmosferdeki de\u011fi\u015fik gazlar yer \u00e7ekiminin etkisiyle \u00e7e\u015fitli y\u00fckseltilerde tutulur.Yer \u00e7ekiminin bitti\u011fi yerde atmosfer de biter.Uzay bo\u015flu\u011fu ba\u015flar.Atmosferi olu\u015fturan gazlar yer \u00e7ekimi etkisiyle a\u011f\u0131rl\u0131klar\u0131na g\u00f6re i\u00e7 i\u00e7e k\u00fcreler bi\u00e7iminde bulunurlar.A\u011f\u0131r gazlar (iki oksijen -azot-iki kobalt) gibi yere yak\u0131n alt tabakalarda hafif gazlar ise \u00fcst tabakalarda yer … Devam\u0131n\u0131 oku…<\/a><\/p>\n","protected":false},"author":1685,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[23],"tags":[13053,14240,14239],"class_list":["post-40070","post","type-post","status-publish","format-standard","hentry","category-cografya","tag-atmosfer","tag-atmosfer-ders-notu","tag-hava-kure"],"_links":{"self":[{"href":"https:\/\/www.sorubak.com\/blog\/wp-json\/wp\/v2\/posts\/40070","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.sorubak.com\/blog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.sorubak.com\/blog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.sorubak.com\/blog\/wp-json\/wp\/v2\/users\/1685"}],"replies":[{"embeddable":true,"href":"https:\/\/www.sorubak.com\/blog\/wp-json\/wp\/v2\/comments?post=40070"}],"version-history":[{"count":0,"href":"https:\/\/www.sorubak.com\/blog\/wp-json\/wp\/v2\/posts\/40070\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.sorubak.com\/blog\/wp-json\/wp\/v2\/media?parent=40070"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.sorubak.com\/blog\/wp-json\/wp\/v2\/categories?post=40070"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.sorubak.com\/blog\/wp-json\/wp\/v2\/tags?post=40070"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}