{"id":41451,"date":"2013-03-07T16:24:38","date_gmt":"2013-03-07T14:24:38","guid":{"rendered":"http:\/\/www.sorubak.com\/blog\/?p=41451"},"modified":"2013-03-07T16:24:38","modified_gmt":"2013-03-07T14:24:38","slug":"yogunlasma","status":"publish","type":"post","link":"https:\/\/www.sorubak.com\/blog\/yogunlasma.html","title":{"rendered":"Yo\u011funla\u015fma"},"content":{"rendered":"<p>YO\u011eUNLA\u015eMA<br \/>\nHavadaki su buhar\u0131n\u0131n, tekrar s\u0131v\u0131 ya da kat\u0131 haldeki suya d\u00f6n\u00fc\u015fmesine yo\u011funla\u015fma denir.<br \/>\nYo\u011funla\u015fman\u0131n meydana gelmesi havan\u0131n nem bak\u0131m\u0131ndan doyma noktas\u0131n\u0131 a\u015fmas\u0131na ba\u011fl\u0131d\u0131r. Havadaki ba\u011f\u0131l nemin y\u00fczde 100\u2032e ula\u015ft\u0131\u011f\u0131 noktaya doyma noktas\u0131 denir. Doyma noktas\u0131 a\u015f\u0131ld\u0131\u011f\u0131 takdirde hava su buhar\u0131n\u0131n fazlas\u0131n\u0131 ta\u015f\u0131yamaz. Fazla olan su buhar\u0131 s\u0131v\u0131 ya da kat\u0131 hale d\u00f6n\u00fc\u015f\u00fcr.<br \/>\nYo\u011funla\u015fma sonucunda \u00e7ok k\u00fc\u00e7\u00fck su taneciklerinin biraraya gelmesiyle bulutlar olu\u015fur. Bulutlar olu\u015ftuklar\u0131 y\u00fckseklikler dikkate al\u0131narak \u00fc\u00e7 gruba ayr\u0131l\u0131r.<br \/>\nY\u00fcksek bulutlar (Sir\u00fcs\u2019ler): Sa\u00e7ak, t\u00fcy, ya da ince iplikler bi\u00e7imindeki bulutlard\u0131r. Y\u00fcksek bulutlar genelde ya\u011f\u0131\u015f getirmezler. Bunlar, bir siklonun yakla\u015ft\u0131\u011f\u0131n\u0131n ve havan\u0131n bozaca\u011f\u0131n\u0131n habercisidirler.<br \/>\nOrta y\u00fckseklikteki bulutlar (K\u00fcm\u00fcl\u00fcs\u2019ler): K\u00fcmeler bi\u00e7imindeki bulutlard\u0131r. Genelde alt k\u0131s\u0131mlar\u0131 d\u00fcz ve siyah olur. Alt k\u0131s\u0131mlar\u0131n\u0131n d\u00fcz olmas\u0131n\u0131n nedeni yo\u011funla\u015fman\u0131n ayn\u0131 seviyeden ba\u015flamas\u0131d\u0131r. Siyah olmas\u0131n\u0131n nedeni ise iri su taneciklerinden olu\u015fmas\u0131d\u0131r. Bu gruptaki baz\u0131 bulutlar y\u00fckseklere do\u011fru b\u00fcy\u00fcr ve sa\u011fanak \u015feklinde \u015fiddetli ya\u011fmurlar getirir.<br \/>\nAl\u00e7ak bulutlar (Strat\u00fcs\u2019ler): Yer\u2019in \u00fcst\u00fcnde, as\u0131l\u0131 gri bir tabaka gibi duran koyu renkli bulutlard\u0131r. Genelde ya\u011f\u0131\u015flara yol a\u00e7arlar.<br \/>\nBelirli bir anda g\u00f6ky\u00fcz\u00fcn\u00fcn bulutlarla kapl\u0131 k\u0131sm\u0131n\u0131n t\u00fcm g\u00f6ky\u00fcz\u00fcne olan oran\u0131na bulutluluk denir. Bulutluluk oran\u0131 \u00e7e\u015fitli aynalardan olu\u015fan ve nefometre ad\u0131 verilen bir aletle \u00f6l\u00e7\u00fcl\u00fcr. Buna g\u00f6re, g\u00f6ky\u00fcz\u00fcn\u00fcn oran\u0131 10 kabul edilerek;<br \/>\n\u2022 0 \u2013 2 oran\u0131 A\u00e7\u0131k havay\u0131<br \/>\n\u2022 2 \u2013 8 oran\u0131 Bulutlu havay\u0131<br \/>\n\u2022 8 \u2013 10 oran\u0131 Kapal\u0131 havay\u0131 ifade eder.<br \/>\nSis, ise yery\u00fcz\u00fcne \u00e7ok yak\u0131n olu\u015fmu\u015f ya da yery\u00fcz\u00fcne \u00e7\u00f6km\u00fc\u015f bulutlard\u0131r. S\u0131cak ve nemli bir havan\u0131n daha so\u011fuk bir yerle temas\u0131 sonucu sis olu\u015fur. S\u0131cak ve so\u011fuk hava k\u00fctlelerinin kar\u015f\u0131la\u015fmas\u0131 da sislere yol a\u00e7ar.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>YO\u011eUNLA\u015eMA Havadaki su buhar\u0131n\u0131n, tekrar s\u0131v\u0131 ya da kat\u0131 haldeki suya d\u00f6n\u00fc\u015fmesine yo\u011funla\u015fma denir. Yo\u011funla\u015fman\u0131n meydana gelmesi havan\u0131n nem bak\u0131m\u0131ndan doyma noktas\u0131n\u0131 a\u015fmas\u0131na ba\u011fl\u0131d\u0131r. Havadaki ba\u011f\u0131l nemin y\u00fczde 100\u2032e ula\u015ft\u0131\u011f\u0131 noktaya doyma noktas\u0131 denir. Doyma noktas\u0131 a\u015f\u0131ld\u0131\u011f\u0131 takdirde hava su buhar\u0131n\u0131n fazlas\u0131n\u0131 ta\u015f\u0131yamaz. Fazla olan su buhar\u0131 s\u0131v\u0131 ya da kat\u0131 hale d\u00f6n\u00fc\u015f\u00fcr. Yo\u011funla\u015fma sonucunda &#8230; <a title=\"Yo\u011funla\u015fma\" class=\"read-more\" href=\"https:\/\/www.sorubak.com\/blog\/yogunlasma.html\" aria-label=\"More on Yo\u011funla\u015fma\">Devam\u0131n\u0131 oku&#8230;<\/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":[15388,15389,15390],"class_list":["post-41451","post","type-post","status-publish","format-standard","hentry","category-cografya","tag-yogunlasma","tag-yogunlasma-nedir","tag-yogunlasma-sonucu"],"_links":{"self":[{"href":"https:\/\/www.sorubak.com\/blog\/wp-json\/wp\/v2\/posts\/41451","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=41451"}],"version-history":[{"count":0,"href":"https:\/\/www.sorubak.com\/blog\/wp-json\/wp\/v2\/posts\/41451\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.sorubak.com\/blog\/wp-json\/wp\/v2\/media?parent=41451"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.sorubak.com\/blog\/wp-json\/wp\/v2\/categories?post=41451"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.sorubak.com\/blog\/wp-json\/wp\/v2\/tags?post=41451"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}