{"id":36669,"date":"2026-02-18T08:36:04","date_gmt":"2026-02-18T08:36:04","guid":{"rendered":"https:\/\/bihavadis.com\/?p=36669"},"modified":"2026-02-18T08:36:04","modified_gmt":"2026-02-18T08:36:04","slug":"izmirde-50-yilda-bir-gorulen-meteorolojik-tablo","status":"publish","type":"post","link":"https:\/\/bihavadis.com\/index.php\/2026\/02\/18\/izmirde-50-yilda-bir-gorulen-meteorolojik-tablo\/","title":{"rendered":"\u0130zmir&#8217;de 50 y\u0131lda bir g\u00f6r\u00fclen meteorolojik tablo"},"content":{"rendered":"<p>\u0130zmir\u2019de en y\u00fcksek r\u00fczgar h\u0131z\u0131 137,5 km\/saate ula\u015ft\u0131. Kuvvetli lodos ve al\u00e7ak bas\u0131nc\u0131n birle\u015fik etkisiyle deniz seviyesi 60 santimetre y\u00fckselirken, 1 metreye ula\u015fan dalgalarla birlikte k\u0131y\u0131 hatt\u0131nda toplam su etkisi 1,5 metreye yakla\u015ft\u0131. \u0130ZDEN\u0130Z Y\u00f6netim Kurulu Ba\u015fkan\u0131 Dr. I\u015f\u0131khan G\u00fcler, \u201cBu tablo s\u0131radan bir lodos kabarmas\u0131 de\u011fil; \u00f6n hesaplara g\u00f6re yakla\u015f\u0131k 50 y\u0131lda bir g\u00f6r\u00fclebilecek \u00f6l\u00e7ekte dalga ve seviye ko\u015fullar\u0131na i\u015faret ediyor. Meteorolojik kaynakl\u0131 ve ge\u00e7ici olsa da, k\u0131y\u0131 \u015feridinde dikkatli olunmal\u0131\u201d de\u011ferlendirmesinde bulundu.<br \/>\u00a0<br \/>\u0130zmir, 15 \u015eubat 2026 tarihinde son y\u0131llar\u0131n en g\u00fc\u00e7l\u00fc meteorolojik olaylar\u0131ndan birini ya\u015fad\u0131. Meteoroloji Genel M\u00fcd\u00fcrl\u00fc\u011f\u00fc 2. B\u00f6lge M\u00fcd\u00fcrl\u00fc\u011f\u00fc verilerine g\u00f6re kent genelinde \u00f6l\u00e7\u00fclen en y\u00fcksek r\u00fczgar h\u0131z\u0131 137,5 km\/saate ula\u015ft\u0131. Bu de\u011fer, \u015fehir i\u00e7inde saatte 130 kilometre h\u0131zla ilerleyen bir arac\u0131n olu\u015fturdu\u011fu r\u00fczgar g\u00fcc\u00fcne yak\u0131n bir etki anlam\u0131na geliyor. Menderes\/\u00c7ileme K\u00f6y\u00fc, \u00c7i\u011fli Havaliman\u0131, Dikili\/\u00c7ukuralan, G\u00fczelbah\u00e7e Feneri ve Bal\u00e7ova ba\u015fta olmak \u00fczere bir\u00e7ok noktada 100 km\/saatin \u00fczerinde f\u0131rt\u0131na de\u011ferleri kaydedildi. K\u00f6rfez ve k\u0131y\u0131 hatt\u0131ndaki \u00f6l\u00e7\u00fcm istasyonlar\u0131nda yer yer tam f\u0131rt\u0131na \u015fiddetinde r\u00fczgar etkili oldu. Bu seviyedeki r\u00fczgar; \u00e7at\u0131lar\u0131n yerinden s\u00f6k\u00fclmesine, a\u011fa\u00e7lar\u0131n devrilmesine ve a\u00e7\u0131k alanlarda y\u00fcr\u00fcmeyi zorla\u015ft\u0131racak bir etkiye neden olabilecek g\u00fc\u00e7te.<\/p>\n<p>Ancak tablo yaln\u0131zca r\u00fczgarla s\u0131n\u0131rl\u0131 kalmad\u0131. Bostanl\u0131 ve Pasaport istasyonlar\u0131ndan al\u0131nan verilere g\u00f6re al\u00e7ak bas\u0131n\u00e7 sistemi nedeniyle \u0130zmir K\u00f6rfezi\u2019nde deniz seviyesi son 24 saatte yakla\u015f\u0131k 60 santimetre y\u00fckseldi. Kuvvetli lodosun olu\u015fturdu\u011fu 90 santimetre ile 1 metre aras\u0131ndaki dalgalarla birlikte k\u0131y\u0131 hatt\u0131nda hissedilen toplam su etkisi yer yer 1,5 metreye ula\u015ft\u0131. Bu durum \u00f6zellikle d\u00fc\u015f\u00fck kotlu b\u00f6lgelerde deniz bask\u0131n\u0131, dalga a\u015fmas\u0131 ve ya\u011fmursuyu sistemlerinde geri basma riskini art\u0131rd\u0131. \u0130zmir B\u00fcy\u00fck\u015fehir Belediyesi ve \u0130ZSU ekipleri k\u0131y\u0131 hatt\u0131nda ve riskli b\u00f6lgelerde su tahliyesi ve kontrol \u00e7al\u0131\u015fmalar\u0131n\u0131 aral\u0131ks\u0131z s\u00fcrd\u00fcr\u00fcyor.<br \/>\u00a0<br \/><strong>Dr. I\u015f\u0131khan G\u00fcler: Bu de\u011ferler yakla\u015f\u0131k 50 y\u0131lda bir g\u00f6r\u00fclebilecek \u00f6l\u00e7ekte<\/strong><br \/>\u0130ZDEN\u0130Z Y\u00f6netim Kurulu Ba\u015fkan\u0131 Dr. I\u015f\u0131khan G\u00fcler, ya\u015fanan s\u00fcreci teknik verilerle de\u011ferlendirerek, \u201c\u0130zmir\u2019de \u015fu an g\u00fcneyli r\u00fczg\u00e2rlar zaman zaman 35\u201340 knot h\u0131zlara ula\u015f\u0131yor. K\u00f6rfez genelinde dalga y\u00fcksekli\u011fi 90 santimetre ile 1 metre aras\u0131nda \u00f6l\u00e7\u00fcl\u00fcyor. Uzun s\u00fcredir etkili olan d\u00fc\u015f\u00fck bas\u0131n\u00e7 sistemi ise deniz seviyesinde yakla\u015f\u0131k 60 santimetrelik bir y\u00fckselmeye neden olmu\u015f durumda. Bu iki etki birle\u015fti\u011finde k\u0131y\u0131 hatt\u0131nda 1,5 metreye varan bir su etkisi olu\u015fuyor. \u00d6n hesaplamalar\u0131m\u0131za g\u00f6re bug\u00fcn g\u00f6zlenen dalga ko\u015fullar\u0131 istatistiksel olarak yakla\u015f\u0131k 50 y\u0131lda bir g\u00f6r\u00fclebilecek \u015fiddette bir olaya i\u015faret ediyor. Bu s\u0131radan bir lodos kabarmas\u0131 de\u011fildir\u201d diye konu\u015ftu.<br \/>\u00a0<br \/><strong>Sal\u0131 g\u00fcn\u00fcne dikkat<\/strong><br \/>G\u00fcler, Alsancak ve Kar\u015f\u0131yaka k\u0131y\u0131lar\u0131nda g\u00f6zlenen geri basmalar\u0131n yap\u0131sal bir sorundan de\u011fil, e\u015f zamanl\u0131 meteorolojik ko\u015fullardan kaynakland\u0131\u011f\u0131n\u0131 vurgulayarak, \u201cD\u00fc\u015f\u00fck bas\u0131n\u00e7 deniz seviyesini do\u011fal olarak y\u00fckseltir. R\u00fczg\u00e2r bu suyu k\u0131y\u0131ya do\u011fru itti\u011finde dalga a\u015fmalar\u0131 g\u00f6r\u00fclebilir. Ayn\u0131 d\u00f6nemde ya\u011f\u0131\u015f\u0131n devam etmesi, ya\u011fmursuyu sistemlerinin denize de\u015farj\u0131n\u0131 zorla\u015ft\u0131rarak mazgallardan geri basmaya neden olur. Bu ge\u00e7ici bir meteorolojik tablodur. Bas\u0131n\u00e7 y\u00fckselip r\u00fczg\u00e2r zay\u0131flad\u0131\u011f\u0131nda deniz seviyesi normale d\u00f6necektir. Sal\u0131 g\u00fcn\u00fc \u00f6\u011fle saatlerinde bas\u0131nc\u0131n 1000 mb\u2019nin alt\u0131na d\u00fc\u015fmesinin bekleniyor.Bu nedenle deniz seviyesinde k\u0131sa s\u00fcreli yeni bir art\u0131\u015f daha ya\u015fanabilecek\u201d dedi.<br \/>\u00a0<br \/><strong>Neden deniz y\u00fckseldi?<\/strong><br \/>Uzmanlara g\u00f6re \u00fc\u00e7 ana etken ayn\u0131 anda devreye girdi:<br \/>\u2022Al\u00e7ak bas\u0131n\u00e7: Deniz seviyesinde yakla\u015f\u0131k 60 cm y\u00fckselmeye neden oldu.<br \/>\u2022Kuvvetli lodos (35\u201340 knot): Denizi k\u0131y\u0131ya do\u011fru iterek 90 cm\u20131 m dalga olu\u015fturdu.<br \/>\u2022Ya\u011f\u0131\u015f: Suyun denize ak\u0131\u015f\u0131n\u0131 zorla\u015ft\u0131rarak geri basma riskini art\u0131rd\u0131. Bu \u00fc\u00e7l\u00fc etki birle\u015fince \u00f6zellikle d\u00fc\u015f\u00fck kotlu alanlarda deniz bask\u0131n\u0131 riski ortaya \u00e7\u0131kt\u0131. Yetkililer, k\u0131y\u0131 tahkimatlar\u0131n\u0131n normal dalga ko\u015fullar\u0131na g\u00f6re tasarland\u0131\u011f\u0131n\u0131; ancak \u00e7ok kuvvetli r\u00fczg\u00e2r, d\u00fc\u015f\u00fck bas\u0131n\u00e7 ve y\u00fckselen deniz seviyesinin ayn\u0131 anda etkili oldu\u011fu ekstrem durumlarda dalga a\u015fmalar\u0131n\u0131n g\u00f6r\u00fclebilece\u011fini vurguluyor. Bu durum yap\u0131sal bir yetersizlik de\u011fil, ola\u011fan\u00fcst\u00fc meteorolojik ko\u015fullar\u0131n ge\u00e7ici sonucudur.<\/p>\n<p>\u00a0<\/p>\n<p>Kaynak: (BYZHA) Beyaz Haber Ajans\u0131<\/p>\n","protected":false},"excerpt":{"rendered":"<p>\u0130zmir\u2019de en y\u00fcksek r\u00fczgar h\u0131z\u0131 137,5 km\/saate ula\u015ft\u0131. Kuvvetli lodos ve al\u00e7ak bas\u0131nc\u0131n birle\u015fik etkisiyle deniz seviyesi 60 santimetre y\u00fckselirken, 1 metreye ula\u015fan dalgalarla birlikte k\u0131y\u0131 hatt\u0131nda toplam su etkisi 1,5 metreye yakla\u015ft\u0131.<\/p>\n","protected":false},"author":1,"featured_media":36670,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[4],"tags":[5257,850,59,244,549],"class_list":["post-36669","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-gundem","tag-dalga","tag-deniz","tag-deniz-seviyesi","tag-etki","tag-ruzgar"],"_links":{"self":[{"href":"https:\/\/bihavadis.com\/index.php\/wp-json\/wp\/v2\/posts\/36669","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/bihavadis.com\/index.php\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/bihavadis.com\/index.php\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/bihavadis.com\/index.php\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/bihavadis.com\/index.php\/wp-json\/wp\/v2\/comments?post=36669"}],"version-history":[{"count":1,"href":"https:\/\/bihavadis.com\/index.php\/wp-json\/wp\/v2\/posts\/36669\/revisions"}],"predecessor-version":[{"id":36671,"href":"https:\/\/bihavadis.com\/index.php\/wp-json\/wp\/v2\/posts\/36669\/revisions\/36671"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/bihavadis.com\/index.php\/wp-json\/wp\/v2\/media\/36670"}],"wp:attachment":[{"href":"https:\/\/bihavadis.com\/index.php\/wp-json\/wp\/v2\/media?parent=36669"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/bihavadis.com\/index.php\/wp-json\/wp\/v2\/categories?post=36669"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/bihavadis.com\/index.php\/wp-json\/wp\/v2\/tags?post=36669"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}