Kas\u0131rgalar\u0131n \u00d6zellikleri<\/b><\/h2>\n
Tropik b\u00f6lgelerde meydana geliyor olmas\u0131 (Okyanuslar\u0131n ekvatora yak\u0131n b\u00f6l\u00fcmlerinde tropik iklimin hakim oldu\u011fu noktalarda). Siklonik olmas\u0131, yani yaratm\u0131\u015f oldu\u011fu r\u00fczgar\u0131n, g\u00f6z olarak adland\u0131r\u0131lan bir merkezin \u00e7evresinde d\u00f6n\u00fcyor olu\u015fu. Bu d\u00f6nme hareketi kuzey yar\u0131mk\u00fcrede saatin ters y\u00f6n\u00fcnde, g\u00fcney yar\u0131mk\u00fcrede ise saat y\u00f6n\u00fcnde ger\u00e7ekle\u015fiyor. Al\u00e7ak bas\u0131n\u00e7 sistemleri olmas\u0131. Kas\u0131rgan\u0131n g\u00f6z k\u0131sm\u0131 her daim bir al\u00e7ak bas\u0131n\u00e7 b\u00f6lgesi ve g\u00fcn\u00fcm\u00fcze kadar \u00f6l\u00e7\u00fclm\u00fc\u015f en d\u00fc\u015f\u00fck barometrik bas\u0131n\u00e7lar kas\u0131rgalarda kaydedilmi\u015f. F\u0131rt\u0131na g\u00f6z\u00fcn \u00e7evresinde d\u00f6nerek esen r\u00fczgar\u0131n h\u0131z\u0131 119 km\/sa.<\/span><\/p>\n Kas\u0131rgalar, denizlerin \u0131l\u0131k (27\u00b0C civar\u0131), havan\u0131n nemli seyretti\u011fi ve bir araya gelen ekvator r\u00fczgarlar\u0131n\u0131n yer ald\u0131\u011f\u0131 tropik b\u00f6lgelerde ger\u00e7ekle\u015fir. Atlantik kas\u0131rgalar\u0131n\u0131n b\u00fcy\u00fck bir k\u0131sm\u0131 Afrika’n\u0131n bat\u0131 k\u0131y\u0131lar\u0131nda g\u00f6k g\u00fcr\u00fclt\u00fcl\u00fc ya\u011f\u0131\u015f ve f\u0131rt\u0131na ile ba\u015flayarak \u0131l\u0131k tropik okyanusa do\u011fru devam eder. Bu g\u00f6k g\u00fcr\u00fclt\u00fcs\u00fc ile seyreden f\u0131rt\u0131na kademeli olarak kas\u0131rga haline gelir.\u00a0<\/span><\/p>\n Tropik f\u0131rt\u0131na a\u015famas\u0131ndan kas\u0131rgaya olu\u015fumuna ge\u00e7i\u015f bazen bir ka\u00e7 saat s\u00fcrerken bazen bir ka\u00e7 g\u00fcn s\u00fcrebilir. Kas\u0131rgan\u0131n olu\u015fma sebebi g\u00fcn\u00fcm\u00fczde halen tam anlam\u0131 ile bilinmiyor, ancak, kas\u0131rgan\u0131n meydana gelebilmesi i\u00e7in a\u015fa\u011f\u0131da yer alan 3 olay\u0131n ger\u00e7ekle\u015fmesi gerekiyor;\u00a0<\/span><\/p>\n Okyanusun y\u00fczeyinde bulunan \u0131l\u0131k ve nemli hava h\u0131zl\u0131 bir \u015fekilde y\u00fckseli\u015fe ge\u00e7er. Il\u0131k havan\u0131n y\u00fckselmesi ile beraber, i\u00e7erisinde yer alan su buhar\u0131 da yo\u011funla\u015farak bulutlar\u0131 ve ya\u011fmur damlalar\u0131 meydana getirir. Yo\u011funla\u015fma esnas\u0131nda gizli yo\u011fu\u015fma \u0131s\u0131s\u0131 ad\u0131 verilen bir \u0131s\u0131 meydana \u00e7\u0131kar. Bu \u0131s\u0131 y\u00fcksek k\u0131s\u0131mdaki havay\u0131 \u0131s\u0131tarak y\u00fckselmesine sebep olur. Y\u00fckselen bu havan\u0131n yerine alt k\u0131s\u0131mlardan y\u00fckseli\u015fe ge\u00e7en \u0131l\u0131k ve nemli okyanus havas\u0131 yerle\u015fir. Bahsetti\u011fimiz d\u00f6ng\u00fc, f\u0131rt\u0131nan\u0131n ger\u00e7ekle\u015fmek \u00fczere olan b\u00f6lge b\u00f6lgeye a\u015fa\u011f\u0131da kalan okyanustan daha fazla rutubetli hava \u00e7ekerek daima s\u0131cak havan\u0131n a\u015fa\u011f\u0131dan yukar\u0131ya do\u011fru hareket etmesini sa\u011flar. Y\u00fczeyde meydana gelen s\u0131cakl\u0131k de\u011fi\u015fimi, bir g\u00f6z etraf\u0131nda d\u00f6nmekte olan bir hava \u00f6r\u00fcnt\u00fcs\u00fc meydana gelmesine sebep olur. Bu d\u00f6ng\u00fcy\u00fc, lavabonun giderinden a\u015fa\u011f\u0131 akan suyun d\u00f6ng\u00fcs\u00fcne benzetilir.<\/span><\/p>\n Birbirinden ayr\u0131 y\u00f6nlere do\u011fru hareket etmekte olan ve birbirleriyle kar\u015f\u0131 kar\u015f\u0131ya gelerek birle\u015fen r\u00fczgarlar, y\u00fczeyde \u00e7arp\u0131\u015f\u0131r ve b\u00f6ylelikle \u0131l\u0131k ve nemli hava yukar\u0131 itilmi\u015f olur. Y\u00fckseli\u015fe ge\u00e7en \u0131l\u0131k hava, bu esnada y\u00fczeyden yukar\u0131 do\u011fru y\u00fckseli\u015fte olan havay\u0131 daha da g\u00fc\u00e7l\u00fc hale getirerek f\u0131rt\u0131nan\u0131n d\u00f6ng\u00fcs\u00fcn\u00fc ve h\u0131z\u0131n\u0131 art\u0131r\u0131r. 9000 metre gibi y\u00fckseklikte de\u011fi\u015fmeyen h\u0131zda esmekte olan g\u00fc\u00e7l\u00fc r\u00fczgar, y\u00fckseli\u015fte olan \u0131l\u0131k havan\u0131n f\u0131rt\u0131nan\u0131n merkez noktas\u0131ndan uzakla\u015fmas\u0131na sebep olur ve \u0131l\u0131k havan\u0131n a\u015fa\u011f\u0131dan yukar\u0131ya do\u011fru eylemini daimi olmas\u0131n\u0131 sa\u011flar, dolay\u0131s\u0131yla f\u0131rt\u0131na \u00f6rg\u00fctlenir. \u015eayet y\u00fcksekte bulunan kuvvetli\u00a0 r\u00fczgarlar her yerde ayn\u0131 h\u0131zda de\u011filse, bir ba\u015fka deyi\u015fle r\u00fczgar makaslar\u0131 mevcutsa, f\u0131rt\u0131na \u00f6rg\u00fctlenemez ve g\u00fc\u00e7lenemez.<\/span><\/p>\n F\u0131rt\u0131nan\u0131n merkez noktas\u0131n\u0131n \u00fcst b\u00f6l\u00fcm\u00fcnde, atmosferin \u00fcst k\u0131s\u0131mlar\u0131nda yer alan y\u00fcksek bas\u0131n\u00e7 da y\u00fckseli\u015fte olan \u0131l\u0131k havadaki s\u0131cakl\u0131\u011f\u0131 azaltarak hava d\u00f6ng\u00fcs\u00fcne katk\u0131da bulunarak kas\u0131rgan\u0131n b\u00fcy\u00fcmesine neden olur. Y\u00fcksek bas\u0131nca sahip hava, al\u00e7ak bas\u0131nca sahip olan f\u0131rt\u0131nan\u0131n merkez noktas\u0131na do\u011fru absorbe edildik\u00e7e r\u00fczgar\u0131n h\u0131z\u0131 da ayn\u0131 oranda art\u0131\u015fa ge\u00e7er. Kas\u0131rga meydana geldikten sonra 3 b\u00f6l\u00fcm haline g\u00f6r\u00fcn\u00fcr;<\/span><\/p>\n Kas\u0131rgalar fiziksel b\u00fcy\u00fckl\u00fck bak\u0131m\u0131ndan farkl\u0131 t\u00fcrlere sahiptir. Baz\u0131 f\u0131rt\u0131nalar \u00e7ok s\u0131k\u0131\u015f\u0131k yap\u0131da olup geride yaln\u0131zca biraz r\u00fczgar ku\u015fa\u011f\u0131 ve ya\u011f\u0131\u015f b\u0131rak\u0131r. Biraz daha gev\u015fek yap\u0131da olan di\u011fer t\u00fcrler ise r\u00fczgar ve ya\u011f\u0131\u015f\u0131 y\u00fczlerce km uza\u011fa ta\u015f\u0131yabiliyor. 1999 senesinde ABD’nin do\u011fusunda ger\u00e7ekle\u015fen Floyd kas\u0131rgas\u0131, Karayip Adalar\u0131\u2019ndan New England’a dek etkisini g\u00f6stermi\u015f.<\/span><\/p>\n Kas\u0131rgalar, karada i\u00e7 kesimlerde dahi seller meydana getirecek kadar \u00e7ok ya\u011f\u0131\u015f b\u0131rak\u0131r. \u00c7ok g\u00fc\u00e7l\u00fc r\u00fczgarlar kentlerde son derece harabiyet olu\u015fturur; a\u011fa\u00e7lar\u0131 k\u00f6k\u00fcnden s\u00f6ker, arabalar\u0131 ters \u00e7evirir, denizde dalgalar\u0131n b\u00fcy\u00fcmesine sebep olarak k\u0131y\u0131 \u015feridinde yer alan kentlerde su bask\u0131nlar\u0131na neden olabilir. Kas\u0131rgada bulunan dominant r\u00fczgarlar, f\u0131rt\u0131na dalgas\u0131 ad\u0131 verilen \u00e7ok miktarda suyu iterek getirir. Bu y\u00fckselen su olay\u0131 ile kas\u0131rga bir araya gelirse, k\u0131y\u0131 \u015feridinde su ta\u015fk\u0131nlar\u0131 ya\u015fan\u0131r ve kent hasar g\u00f6r\u00fcr. Kas\u0131rga r\u00fczgarlar\u0131, genellikte hortum da meydana getirir ve daha fazla zarar verebilir.<\/span><\/p>\n Kas\u0131rgalar ilk olarak g\u00f6rsel belirtilere, yani bulutlar ve bulutlar\u0131n d\u00f6n\u00fc\u015f \u015fekillerine bak\u0131larak tahmin edilmeye \u00e7al\u0131\u015f\u0131l\u0131yor. Teknik a\u00e7\u0131dan ise, radar ve doppler radar\u0131 ile ya\u011f\u0131\u015f, r\u00fczgar h\u0131z\u0131 ve ya\u011f\u0131\u015f miktar\u0131n\u0131n \u00f6l\u00e7\u00fclmesi ile toplanan bilgilerle tahminler yap\u0131l\u0131yor. Bunlar\u0131n yan\u0131 s\u0131ra k\u0131z\u0131l \u00f6tesi \u0131\u015f\u0131nlarla s\u0131cakl\u0131k de\u011fi\u015fimleri ve bulut y\u00fckseklikleri tespit edilerek tahminler yap\u0131l\u0131yor.<\/span><\/p>\n D\u00fcnya Sava\u015f\u0131\u2019na kadar erkek isimleri verilen kas\u0131rgalara sonras\u0131nda alfabetik olarak kad\u0131n isimleri verilmeye ba\u015flanm\u0131\u015f. Bu durum, kad\u0131n haklar\u0131 dernekleri taraf\u0131ndan tepki g\u00f6r\u00fcnce 1970\u2019li y\u0131llar\u0131n son d\u00f6nemlerinde kas\u0131rgalara bir erkek bir kad\u0131n ismi verilerek bu durum dengelenmi\u015f. Bug\u00fcn ise, insan isimlerinden \u00e7ok delta, epsilon, zeta gibi isimler veriliyor.<\/p>\n","protected":false},"excerpt":{"rendered":" Tan\u0131m Miami’de yer alan Ulusal Kas\u0131rga Merkezi’ne verilerinde, Atlantik Okyanusu\u2019nda meydana gelen, \u2018tropik siklona hurricane\u2019 t\u00fcrk\u00e7e kar\u015f\u0131l\u0131\u011f\u0131 ile kas\u0131rga. Tropik […]<\/p>\n","protected":false},"author":10,"featured_media":36477,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1],"tags":[],"class_list":["post-36475","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-genel"],"yoast_head":"\n![\"\"](\"https:\/\/www.hepsiburada.com\/hayatburada\/wp-content\/uploads\/2023\/06\/kasirgalar3.jpg\")
<\/p>\nKas\u0131rga Nas\u0131l Olu\u015fur?<\/b><\/h2>\n
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![\"\"](\"https:\/\/www.hepsiburada.com\/hayatburada\/wp-content\/uploads\/2023\/06\/kasirgalar4.jpg\")
<\/p>\nR\u00fczgar \u00d6r\u00fcnt\u00fcleri<\/b><\/h2>\n
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Kas\u0131rgalar\u0131n U\u011fratt\u0131\u011f\u0131 Zararlar<\/b><\/h2>\n
Kas\u0131rga Kategorileri<\/b><\/h2>\n
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![\"\"](\"https:\/\/www.hepsiburada.com\/hayatburada\/wp-content\/uploads\/2023\/06\/kasirgalar2.jpg\")
<\/p>\nNas\u0131l \u0130zleniyor?<\/b><\/h2>\n
Kas\u0131rga \u0130simleri<\/b><\/h2>\n