{"id":3704,"date":"2024-07-08T14:02:02","date_gmt":"2024-07-08T14:02:02","guid":{"rendered":"https:\/\/editorial.buluttan.com\/?p=3704"},"modified":"2025-07-15T09:21:46","modified_gmt":"2025-07-15T09:21:46","slug":"doganin-gazabi-kasirgalar","status":"publish","type":"post","link":"https:\/\/editorial.buluttan.com\/?p=3704","title":{"rendered":"Do\u011fan\u0131n Gazab\u0131: Kas\u0131rgalar"},"content":{"rendered":"\n

Kas\u0131rgalar, b\u00fcy\u00fckl\u00fckleriyle ve \u00f6zellikle de arkalar\u0131nda b\u0131rakt\u0131klar\u0131 y\u0131k\u0131m\u0131n izleri ile atmosferin g\u00fcc\u00fcn\u00fc ortaya koyan do\u011fa olaylar\u0131ndan biridir. Bilimsel s\u0131n\u0131fland\u0131rmas\u0131na bakt\u0131\u011f\u0131m\u0131zda h\u0131z\u0131 saatte 119 km\u2019yi ge\u00e7en r\u00fczgarlar kas\u0131rga olarak adland\u0131r\u0131l\u0131r. Ancak kars\u0131rgalar, f\u0131rt\u0131na olarak adland\u0131r\u0131lmak i\u00e7in olduk\u00e7a b\u00fcy\u00fck meteorolojik fenomenlerdir. \u00d6rne\u011fin, sadece bir kas\u0131rga s\u0131ras\u0131nda, \u015fiddetli r\u00fczgarlar t\u00fcm d\u00fcnyan\u0131n elektrik \u00fcretim kapasitesinin yar\u0131s\u0131 kadar enerji \u00fcretebilirken<\/a>, ayn\u0131 f\u0131rt\u0131nadan kaynaklanan bulut ve ya\u011fmur olu\u015fumu bu miktar\u0131n 400 kat\u0131n\u0131 \u015fa\u015f\u0131rt\u0131c\u0131 bir \u015fekilde a\u00e7\u0131\u011fa \u00e7\u0131karabilir. <\/p>\n\n\n\n

\"hurricane
Hurricane – Photo by Canva<\/figcaption><\/figure>\n\n\n\n

Kas\u0131rgalar\u0131n Olu\u015fumu<\/h2>\n\n\n\n

Kas\u0131rgalar\u0131n ortaya \u00e7\u0131kmas\u0131 i\u00e7in \u00e7e\u015fitli ko\u015fullara ihtiya\u00e7 vard\u0131r. S\u00fcre\u00e7, genellikle tropik ve subtropikal b\u00f6lgelerdeki \u0131l\u0131k okyanus sular\u0131yla ba\u015flar. Deniz suyu s\u0131cakl\u0131\u011f\u0131 26,5\u00b0C’ye ula\u015ft\u0131\u011f\u0131nda<\/a>, ortamda; kas\u0131rgay\u0131 beslemek i\u00e7in gerekli yak\u0131t sa\u011flanm\u0131\u015f olur.<\/p>\n\n\n\n

Ancak deniz suyu s\u0131cakl\u0131\u011f\u0131n\u0131n artmas\u0131 tek ba\u015f\u0131na yeterli de\u011fildir. \u00c7o\u011funlukla tropikal bir dalga i\u00e7in okyanus ve atmosfer ortam\u0131ndaki tropikal ak\u0131\u015fta k\u00fc\u00e7\u00fck bir bozulma ya\u015fanmas\u0131 ile olu\u015fan atmosferik karars\u0131zl\u0131k gereklidir. Orta troposferdeki y\u00fcksek nem (deniz seviyesinden yakla\u015f\u0131k 5 km y\u00fcksekte<\/a>), geli\u015fen sistem i\u00e7indeki kas\u0131rga aktivitesini s\u00fcrd\u00fcrd\u00fc\u011f\u00fc i\u00e7in \u00e7ok \u00f6nemlidir.<\/p>\n\n\n\n

D\u00fcnyan\u0131n d\u00f6n\u00fc\u015f\u00fcn\u00fcn bir sonucu olan Coriolis etkisi<\/a>, f\u0131rt\u0131naya gerekli d\u00f6n\u00fc\u015f\u00fc vererek siklonik d\u00f6n\u00fc\u015f geli\u015ftirmesine olanak tan\u0131r. Ek olarak, al\u00e7ak seviyede dikey r\u00fczgar makaslamas\u0131 \u00e7ok \u00f6nemlidir; kas\u0131rgan\u0131n yap\u0131s\u0131n\u0131n sa\u011flam kalmas\u0131n\u0131 ve \u00e7e\u015fitli y\u00fcksekliklerdeki farkl\u0131 r\u00fczgar h\u0131zlar\u0131ndan etkilenmeden dikey olarak b\u00fcy\u00fcyebilmesini sa\u011flar.<\/p>\n\n\n\n

\"hurricane
Hurricane Eye – Photo by Canva<\/figcaption><\/figure>\n\n\n\n

Kas\u0131rgalar\u0131n Kategorilendirilmesi<\/h3>\n\n\n\n

Kas\u0131rgalar r\u00fczgar\u0131n h\u0131z\u0131na ba\u011fl\u0131 olarak 1 ile 5 aras\u0131nda kategorize edilirler. R\u00fczgar\u0131n h\u0131z\u0131 artt\u0131k\u00e7a kas\u0131rgan\u0131n zarar verme g\u00fcc\u00fc de buna ba\u011fl\u0131 olarak artar. \u00d6rne\u011fin kas\u0131rgalar r\u00fczgar\u0131n h\u0131z\u0131na ba\u011fl\u0131 olarak 1 ile 5 aras\u0131nda kategorize edilirler. R\u00fczgar\u0131n h\u0131z\u0131 artt\u0131k\u00e7a kas\u0131rgan\u0131n zarar verme g\u00fcc\u00fc de buna ba\u011fl\u0131 olarak artar. \u00d6rne\u011fin Atlantik Okyanusu’nda olu\u015fan ve \u015fu anda Karayipleri vuran Beryl Kas\u0131rgas\u0131 5. kategoriye kadar \u00e7\u0131km\u0131\u015f durumda, bu kas\u0131rgan\u0131n vurdu\u011fu yerlere yerlere a\u011f\u0131r hasar verdi\u011fi ve saatte 269 kilometreyi bulan h\u0131z\u0131yla \u00e7ok \u015fiddetli bir etkisi oldu\u011funu ifade ediyor. Atlantik Okyanusu’nda olu\u015fan ve \u015fu anda Karayipleri vuran Beryl Kas\u0131rgas\u0131 5. kategoriye kadar \u00e7\u0131km\u0131\u015f durumda<\/a>, bu kas\u0131rgan\u0131n vurdu\u011fu yerlere yerlere a\u011f\u0131r hasar verdi\u011fi ve saatte 269 kilometreyi bulan h\u0131z\u0131yla \u00e7ok \u015fiddetli bir etkisi oldu\u011funu ifade ediyor.<\/p>\n\n\n\n

Kas\u0131rgalar Nerelerde G\u00f6r\u00fcl\u00fcr?<\/h3>\n\n\n\n

Kas\u0131rgalar, Do\u011fu B\u00fcy\u00fck Okyanus ve G\u00fcney Atlantik hari\u00e7 subtropikal ve tropikal iklim ku\u015fa\u011f\u0131ndaki s\u0131cak denizlerde<\/a> s\u0131k s\u0131k meydana geliyor. \u00dclkemizin co\u011frafi konumundan dolay\u0131 her ne kadar kas\u0131rgalar\u0131 birinci elden ya\u015fam\u0131yor olsak da Akdeniz \u00e7evresinde ‘medicane<\/a>‘ ad\u0131 verilen kas\u0131rgalar g\u00f6r\u00fclebiliyor. Akdeniz ve Ege denizleri \u00fczerinde zaman zaman \u00e7ok g\u00fc\u00e7l\u00fc siklonlar olu\u015fabiliyor. \u0130talya, Yunanistan, Malta, T\u00fcrkiye gibi \u00fclkeler bu g\u00fc\u00e7l\u00fc siklonlar nedeniyle risk alt\u0131nda olabiliyorlar.<\/p>\n\n\n\n

\"hurricane
Photo by Canva<\/figcaption><\/figure>\n\n\n\n

Kas\u0131rgan\u0131n Etkileri ve Y\u0131k\u0131m<\/strong><\/h2>\n\n\n\n

Kas\u0131rgalar, a\u011fa\u00e7lar\u0131 s\u00f6kebilen, binalara ve elektrik hatlar\u0131na zarar veren \u015fiddetli r\u00fczgarlara, su bask\u0131nlar\u0131na ve sele neden olan aral\u0131ks\u0131z ya\u011f\u0131\u015f olaylar\u0131na, deniz seviyesinin anormal art\u0131\u015f\u0131na yol a\u00e7an f\u0131rt\u0131na kabarmalar\u0131na neden olur. Ayr\u0131ca kas\u0131rgalar ba\u015fka bir y\u0131k\u0131m katman\u0131 daha eklenerek tornadolar\u0131 \u00fcretebilirler.<\/p>\n\n\n\n

Kas\u0131rgalar D\u00fcnyam\u0131z\u0131n bir par\u00e7as\u0131 ancak k\u00fcresel \u0131s\u0131nma kas\u0131rgalar\u0131n \u015fiddetini g\u00fcnden g\u00fcne artt\u0131r\u0131yor.<\/p>\n\n\n\n

\u00d6nlem almak m\u00fcmk\u00fcn!<\/h2>\n\n\n\n