{"id":877,"date":"2013-02-06T04:15:50","date_gmt":"2013-02-06T04:15:50","guid":{"rendered":"http:\/\/bizimkokpit.com\/?p=877"},"modified":"2015-06-05T04:17:19","modified_gmt":"2015-06-05T04:17:19","slug":"havacilik-meteorolojisinde-basinc-yogunluk-ve-sicaklik","status":"publish","type":"post","link":"https:\/\/bizimkokpit.com\/index.php\/2013\/02\/06\/havacilik-meteorolojisinde-basinc-yogunluk-ve-sicaklik\/","title":{"rendered":"Havac\u0131l\u0131k Meteorolojisinde Bas\u0131n\u00e7, Yo\u011funluk ve S\u0131cakl\u0131k"},"content":{"rendered":"<div>BASIN\u00c7 (PRESSURE): Meteorolojide, herhangi bir yerdeki birim alana atmosfer a\u011f\u0131rl\u0131\u011f\u0131n\u0131n yaratt\u0131\u011f\u0131 kuvvettir. Atmosfer bas\u0131nc\u0131 veya baro metrik bas\u0131n\u00e7 olarak da bilinir. Herhangi bir noktadaki atmosfer bas\u0131nc\u0131 denilince, bu nokta birim alan \u00fczerinde dikey olarak uzanan havan\u0131n a\u011f\u0131rl\u0131\u011f\u0131 akla gelir. Standart atmosferde bu de\u011fer 760 mm.lik c\u0131va s\u00fctununa e\u015fittir. Bas\u0131n\u00e7 birimlerinin \u00e7eviri form\u00fclleri ise \u015f\u00f6yledir.<\/div>\n<div><\/div>\n<div>Milibar = in\u00e7 * 2.54 * 13.5951 * 980.665 * 10 -3<\/div>\n<div><\/div>\n<div>\u2028Milibar = mm * 13.5951 * 980.665 * 10 -4<\/div>\n<div><\/div>\n<div><\/div>\n<div><\/div>\n<div>BAROMETR\u0130K BASIN\u00c7 (BAROMETRIC PRESSURE): Atmosferik bas\u0131n\u00e7 olarak ta bilinen, atmosfer taraf\u0131ndan bir noktaya yap\u0131lan bas\u0131n\u00e7t\u0131r. Milibar veya milimetre ile \u00f6l\u00e7\u00fcl\u00fcr.<\/div>\n<div><\/div>\n<div>\u0130STASYON BASINCI VE ORTALAMA DEN\u0130Z SEV\u0130YES\u0130 BASINCI (MSL): Bir havaalan\u0131nda bas\u0131n\u00e7 \u00f6l\u00e7\u00fcld\u00fc\u011f\u00fcnde, bu hava alan\u0131n\u0131n \u00fcst\u00fcndeki havan\u0131n \u00f6l\u00e7\u00fclen a\u011f\u0131rl\u0131\u011f\u0131d\u0131r. Buna istasyon bas\u0131nc\u0131 denir. Bas\u0131n\u00e7 y\u00fckseklikle birlikte azalma g\u00f6sterir, bu nedenle atmosferde y\u00fcksek noktadaki bas\u0131n\u00e7, al\u00e7ak bir seviyedekinden daha azd\u0131r. Meteoroloji haritalar\u0131n\u0131 analiz etmek i\u00e7in farkl\u0131 g\u00f6zlem istasyonlar\u0131ndaki bas\u0131n\u00e7 kar\u015f\u0131la\u015ft\u0131r\u0131lmal\u0131d\u0131r. \u0130stasyon bas\u0131nc\u0131 istasyonun y\u00fcksekli\u011fiyle de\u011fi\u015fti\u011fi i\u00e7in, b\u00fct\u00fcn istasyon bas\u0131n\u00e7lar\u0131, kar\u015f\u0131la\u015ft\u0131rma yapabilmek i\u00e7in baz\u0131 ortak seviyelere ayarlanmal\u0131d\u0131r. Ortak olarak d\u00fc\u015f\u00fcr\u00fclen seviye, ortalama deniz seviyesi (MSL) dir.<\/div>\n<div><\/div>\n<div>MSL BASINCI: Barometre bas\u0131nc\u0131ndaki en b\u00fcy\u00fck de\u011fi\u015fim y\u00fckseklikle ilgilidir. Atmosferin \u00e7o\u011funun yer \u00e7ekiminden dolay\u0131 yo\u011funla\u015ft\u0131\u011f\u0131 troposferin alt birka\u00e7 bin feet lik seviyesi dahilinde her 1.000 feet lik irtifa i\u00e7in c\u0131va cinsinden de\u011fi\u015fiklik a\u015fa\u011f\u0131 yukar\u0131 1 inch\u2019e denk gelir.<\/div>\n<div><\/div>\n<div>BASIN\u00c7 FARKLARI: Bas\u0131n\u00e7 farkl\u0131l\u0131klar\u0131, belirli bir yer ve zamanda s\u00fcrekli olarak meydana gelmektedir. Cep hesel ge\u00e7i\u015fler, orajlar, y\u00fcksek ve al\u00e7ak bas\u0131n\u00e7 sistem lerinin hareketinden \u00f6t\u00fcr\u00fc ani de\u011fi\u015fimler ger\u00e7ekle\u015fir. \u0130yi olu\u015fmu\u015f al\u00e7ak ve y\u00fcksek bas\u0131n\u00e7 ge\u00e7i\u015flerinde bazen 1 veya daha fazla inch\u2019lik b\u00fcy\u00fck de\u011fi\u015fiklikler 2-3 saat i\u00e7inde ger\u00e7ekle\u015febilir. Daha a\u015famal\u0131 farkl\u0131 l\u0131klar, haftal\u0131k, ayl\u0131k ve mevsimlik bir temelde ger\u00e7ekle\u015fir. Ancak bas\u0131n\u00e7, daha \u00e7ok dikey irtifa de\u011fi\u015fimleri ve bunun yerini tutan hava s\u0131cakl\u0131\u011f\u0131 de\u011fi\u015fimlerine g\u00f6re farkl\u0131l\u0131k g\u00f6sterir.<\/div>\n<div><\/div>\n<div>\u0130ZOBAR: Bas\u0131n\u00e7lar\u0131 e\u015fit olan noktalar\u0131 birle\u015ftiren e\u011friye izobar ad\u0131 verilir. Yer (Ortalama Deniz Seviyesi \u2013 ODS) Meteoroloji haritalar\u0131nda izobarlar belirli aral\u0131klarla genellikle 4 milibar aral\u0131klarla \u00e7izilir ler. Haritadaki m\u00fcnhaniler nas\u0131l ar\u0131za engebelerini ifade ediyorsa, izobarlarda bas\u0131n\u00e7 alanlar\u0131n\u0131 a\u015fa\u011f\u0131 yukar\u0131 ayn\u0131 tarzda ifade etmeye yararlar. Bazen bas\u0131n\u00e7 paternleri yada bas\u0131n\u00e7 sistemleri diye adland\u0131r\u0131lan a\u015fa\u011f\u0131daki be\u015f bas\u0131n\u00e7 alan\u0131 yer haritalar\u0131nda izobarlar ile g\u00f6sterilirler.<\/div>\n<div><\/div>\n<div>Al\u00e7ak Bas\u0131n\u00e7 : Al\u00e7ak, her yan\u0131 daha y\u00fcksek bas\u0131n\u00e7la sar\u0131lm\u0131\u015f olan al\u00e7ak bas\u0131nc\u0131n merkezidir.<\/div>\n<div>Y\u00fcksek Bas\u0131n\u00e7 : Y\u00fcksek, her yan\u0131 daha al\u00e7ak bas\u0131n\u00e7la sar\u0131lm\u0131\u015f olan y\u00fcksek bas\u0131nc\u0131n\u2028merkezidir.<\/div>\n<div>Ge\u00e7it : Ge\u00e7it, iki y\u00fcksek ve iki al\u00e7ak bas\u0131n\u00e7 aras\u0131ndaki boyun b\u00f6lgesidir.<\/div>\n<div>Oluk : Oluk, al\u00e7ak bas\u0131n\u00e7 alan\u0131n\u0131n uzant\u0131s\u0131d\u0131r.<\/div>\n<div>S\u0131rt : S\u0131rt, Y\u00fcksek bas\u0131n\u00e7 alan\u0131n\u0131n uzant\u0131s\u0131d\u0131r.<\/div>\n<div><\/div>\n<div>BASIN\u00c7, SICAKLIK VE YO\u011eUNLUK ARASINDAK\u0130 \u0130L\u0130\u015eK\u0130 :<\/div>\n<div>Atmosfer i\u00e7inde yo\u011funla\u015fman\u0131n meydana gelmesi i\u00e7in iki \u00f6nemli olay\u0131n vuku bulmas\u0131 gerekmektedir;<\/div>\n<div>\u2022 Havadaki su buhar\u0131n\u0131n artmas\u0131,<\/div>\n<div>\u2022 Havan\u0131n so\u011futulmas\u0131.<\/div>\n<div>Havadaki su buhar\u0131 %100\u2032l\u00fck nisbi rutubete ula\u015ft\u0131\u011f\u0131 zaman, doyma meydana gelir. Bunun \u00f6tesinde ilave edilecek su buhar\u0131, buharlar\u0131n bir k\u0131sm\u0131n\u0131n s\u0131v\u0131 hale d\u00f6n\u00fc\u015fmesine sebep olur ki, buna da yo\u011funla\u015fma diyoruz.<\/div>\n<div><\/div>\n<div>Yo\u011funla\u015fman\u0131n en \u00e7ok bilinen \u015fekilleri, bulutlar ve sistir. E\u011fer s\u00fchunet yeteri kadar d\u00fc\u015f\u00fck ise (s\u0131f\u0131r\u0131n bir hayli alt\u0131nda) su buhar\u0131 do\u011frudan do\u011fruya kat\u0131 hale yani buz kristalleri haline d\u00f6n\u00fc\u015f\u00fcr.<\/div>\n<div><\/div>\n<div>Havaya su buhar\u0131n\u0131n ilavesiyle de doyma ve yo\u011funla\u015fma meydana gelmekle beraber, havan\u0131n doymu\u015f hale gelmesi daha \u00e7ok, so\u011fuma yoluyla olmaktad\u0131r. So\u011fuma yoluyla hava doymu\u015f hale geldikten sonar bunun da \u00f6tesinde so\u011futmaya devam edilmesi halinde, genellikle yo\u011funla\u015fma ya da s\u00fcblimle\u015fme sonucu bulutlar veya sis te\u015fekk\u00fcl eder.<\/div>\n<div><\/div>\n<div>Atmosferdeki so\u011fuma a\u015fa\u011f\u0131daki \u015fekillerde olur.<\/div>\n<div><\/div>\n<div>\u2022 Havan\u0131n so\u011fuk bir y\u00fczey \u00fczerinden ge\u00e7mesiyle (adveksiyonla),<\/div>\n<div>\u2022 Y\u00fckselen havan\u0131n geni\u015fleyerek \u0131s\u0131 kaybetmesiyle (adyabatik so\u011fuma),<\/div>\n<div>\u2022 Havan\u0131n alt\u0131ndaki y\u00fczeyin gece \u0131\u015f\u0131n\u0131mla (radyasyonla) so\u011fumas\u0131 sonucu, atmosferin alt tabakas\u0131n\u0131n so\u011fumas\u0131yla. Bu \u00e7e\u015fit so\u011fuma, ekseriya buluttan \u00e7ok sis te\u015fekk\u00fcl\u00fcne sebep olur; ancak r\u00fczgar h\u0131z\u0131n\u0131n 15 Knot\u2019tan fazla olmas\u0131 halinde, sisi y\u00fckselerek al\u00e7ak bir bulut tabakas\u0131 meydana getirebilir.<\/div>\n<div><\/div>\n<div>Adyabatik so\u011fuma (geni\u015fleyerek so\u011fuma), yukar\u0131ya hareket eden havan\u0131n, daha d\u00fc\u015f\u00fck bas\u0131n\u00e7l\u0131 y\u00fcksek irtifalara \u00e7\u0131kmas\u0131 ile olur. Do\u011fal olarak kald\u0131rma, mihaniki veya \u0131s\u0131sal nedenlerle olmaktad\u0131r. Is\u0131sal kald\u0131rma (konvektif kald\u0131rma) yerin \u0131s\u0131nmas\u0131n\u0131n bir sonucudur; mihaniki kald\u0131rma ise, havan\u0131n da\u011flar \u00fczerinde (orografik olarak) so\u011fuk hava kitleleri \u00fczerinde (cephesel) ya da toplanma (conver gence) b\u00f6lgelerinde y\u00fckselmeye zorlanmas\u0131 suretiyle olur. So\u011fuk bir y\u00fczey \u00fczerinden ge\u00e7en hava da yeteri kadar so\u011fuyarak yo\u011funla\u015fmaya u\u011frar ve genellikle sis ya da al\u00e7ak bulutlar te\u015fekk\u00fcl eder.<\/div>\n<div><\/div>\n<div>Sis ve bulutlar s\u0131v\u0131 veya kat\u0131 haldeki k\u00fc\u00e7\u00fck su damlac\u0131klar\u0131ndan meydana gelirler. K\u00fc\u00e7\u00fck su damlac\u0131klar\u0131, havada bulunan toz duman yada tuz gibi kat\u0131 maddelerin k\u00fc\u00e7\u00fck zerrecikleri \u00fczerinde olu\u015fur ve birikirler.<\/div>\n<div><\/div>\n<div>E\u011fer yo\u011funla\u015fma zerrecikleri diye adland\u0131r\u0131lan bu cisimcikler atmosferde bulunmasayd\u0131 yo\u011funla\u015fman\u0131n meydana gelmesi i\u00e7in % 400\u2032l\u00fck bir nisbi rutubete ihtiya\u00e7 duyulacakt\u0131r. Atmosferin alt tabakalar\u0131nda bu yo\u011funla\u015fma zerrecikleri mevcuttur. Onlar\u0131n atmosfer i\u00e7inde bol miktarda bulunmas\u0131 ile, yo\u011funla\u015fma genellikle nisbi rutubet %100 civar\u0131nda iken meydana gelmektedir; bununla beraber, atmosferde bazen nisbi rutubetin %85 oldu\u011fu yerlerde bile yo\u011funla\u015fman\u0131n meydana geldi\u011fi, bilinen bir ger\u00e7ektir. Bunun ortaya koydu\u011fu ger\u00e7ek \u015fudur ki, baz\u0131 yo\u011funla\u015fma zerrecikleri nisbi rutubet %100\u2032\u00fcn bir hayli alt\u0131nda iken suyu toplamaya ba\u015flamaktad\u0131rlar.<\/div>\n<div><\/div>\n<div>Atmosferde s\u0131v\u0131 haldeki su damlac\u0131klar\u0131na, donma s\u00fchunetlerinde bile, hatta -40 derece C lara kadar s\u0131k s\u0131k rastlan\u0131r. Bu duruma a\u015f\u0131r\u0131 so\u011fuma ad\u0131 verilir ve bulutlar i\u00e7inde -15 derece C\u2019 a kadar \u00e7ok yayg\u0131nd\u0131r.<\/div>\n<div><\/div>\n<div>Atmosferik Bas\u0131n\u00e7 ve Hava Yo\u011funlu\u011fu: Hava bas\u0131nc\u0131 ve hava s\u0131cakl\u0131\u011f\u0131, hava yo\u011funlu\u011funu belirler. Bu durum, di\u011fer fakt\u00f6rlerin de\u011fi\u015fmedi\u011fi kabul edildi\u011finde u\u00e7a\u011f\u0131n kald\u0131rma g\u00fcc\u00fcn\u00fc etkiler. Hava yo\u011funlu\u011fu d\u00fc\u015f\u00fck ise, bir u\u00e7ak konumunu muhafaza etmek i\u00e7in daha s\u00fcratli u\u00e7mak zorundad\u0131r. Y\u00fcksek s\u0131cakl\u0131klarda yeterli kalk\u0131\u015f h\u0131z\u0131na ula\u015fabilmek i\u00e7in pist uzunlu\u011funun artt\u0131r\u0131lmas\u0131 gerekir. Bas\u0131n\u00e7 d\u00fc\u015ft\u00fc\u011f\u00fcnde yo\u011funluk azalaca\u011f\u0131ndan kalk\u0131\u015f i\u00e7in gerekli pist uzunlu\u011fu i\u00e7in ayn\u0131 durum s\u00f6z konusu olacakt\u0131r. Kalk\u0131\u015f planlamas\u0131nda dikkate al\u0131nmas\u0131 gereken bas\u0131n\u00e7taki genel sinoptik de\u011fi\u015fimin etkisi al\u00e7ak bas\u0131n\u00e7larda \u00e7ok daha fazlad\u0131r. Bir havaalan\u0131n\u0131n rak\u0131m\u0131ndaki artma, ortalama bas\u0131nc\u0131 azalt\u0131r ve bu durum ortalama hava yo\u011funlu\u011funa etki eder. Bu nedenle y\u00fcksek rak\u0131ml\u0131 havaalanlar\u0131nda daha uzun kalk\u0131\u015f mesafelerine ihtiya\u00e7 duyulur. Hava yo\u011funlu\u011fundaki azalman\u0131n di\u011fer bir etkisi de motor g\u00fcc\u00fcn\u00fc d\u00fc\u015f\u00fcrmesidir.<\/div>\n<div><\/div>\n<div>Rutubet : Havan\u0131n su buhar\u0131 tutma kapasitesi do\u011frudan do\u011fruya s\u0131cakl\u0131\u011f\u0131 ile ilgilidir. Genel olarak bilirli s\u0131cakl\u0131ktaki hava, belirli miktardan daha fazla su buhar\u0131 ihtiva edemez. Havan\u0131n s\u0131cakl\u0131\u011f\u0131 ne kadar y\u00fcksek olursa ta\u015f\u0131yabilece\u011fi azami su buhar\u0131 miktar\u0131 da o nispette \u00e7ok olur. Hava, ta\u015f\u0131ya bilece\u011fi azami su buhar\u0131n\u0131 ihtiva etti\u011fi zaman doymu\u015f haldedir; e\u011fer daha az su buhar\u0131 ihtiva ediyorsa doymam\u0131\u015ft\u0131r.<\/div>\n<div><\/div>\n<div>Havan\u0131n ihtiva etti\u011fi su buhar\u0131n\u0131 ifade etmek amac\u0131 ile kullan\u0131lan bir\u00e7ok terim vard\u0131r. Bunlardan yaln\u0131zca ikisini bir arada tart\u0131\u015fmam\u0131z gerekiyor. \u00c7i\u011f noktas\u0131 ve nisbi rutubet.<\/div>\n<div><a href=\"http:\/\/bizimkokpit.com\/wp-content\/uploads\/2015\/06\/meteorology-leo-02.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\" size-medium wp-image-878 alignright\" src=\"http:\/\/bizimkokpit.com\/wp-content\/uploads\/2015\/06\/meteorology-leo-02-300x226.jpg\" alt=\"meteorology-leo-02\" width=\"300\" height=\"226\" srcset=\"https:\/\/bizimkokpit.com\/wp-content\/uploads\/2015\/06\/meteorology-leo-02-300x226.jpg 300w, https:\/\/bizimkokpit.com\/wp-content\/uploads\/2015\/06\/meteorology-leo-02.jpg 524w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><\/div>\n<div>\u00c7i\u011f Noktas\u0131: \u00c7i\u011f noktas\u0131, sabit bas\u0131n\u00e7 alt\u0131nda so\u011futulan havan\u0131n doymam\u0131\u015f hale geldi\u011fi s\u00fchunettir. \u00c7i\u011f noktas\u0131 s\u00fchuneti ile ger\u00e7ek s\u00fchunet aras\u0131ndaki fark, havan\u0131n doyma durumuna ne derece yak\u0131n oldu\u011funu g\u00f6sterir. Bu iki s\u00fchunet aras\u0131ndaki fark ne kadar az ise, yo\u011funla\u015fma sonucu bulut ve sis te\u015fekk\u00fcl ihtimali o derece fazla demektir.<\/div>\n<div><\/div>\n<div>\u00c7i\u011f noktas\u0131 s\u00fchuneti ayn\u0131 zamanda atmosfer i\u00e7indeki su buhar\u0131 miktar\u0131 hakk\u0131nda da yakla\u015f\u0131k bir bilgi verir; yani herhangi bir bas\u0131n\u00e7 alt\u0131ndaki havan\u0131n \u00e7i\u011f noktas\u0131 s\u00fchuneti ne kadar y\u00fcksekse, i\u00e7indeki su buhar\u0131 miktar\u0131 da o kadar \u00e7ok demektir.<\/div>\n<div><\/div>\n<div>Nispi Rutubet: Nispi rutubet, belirli bir s\u00fchunetteki havan\u0131n i\u00e7indeki su buhar\u0131 miktar\u0131n\u0131n , ayn\u0131 havay\u0131 doymu\u015f hale getirecek su buhar\u0131 miktar\u0131na oran\u0131d\u0131r. Bu oran, y\u00fczde ile ifade edilir ve atmosferin doymu\u015f hale yak\u0131nl\u0131\u011f\u0131 hakk\u0131nda fikir veren ba\u015fka bir olgudur. \u00d6rne\u011fin, hava belirli bir s\u00fchunetteki m\u00fcmk\u00fcn olan t\u00fcm su buhar\u0131n\u0131 ihtiva ediyorsa nisbi rutubeti %100 olarak ifade edilir. Ta\u015f\u0131yabilece\u011fi t\u00fcm su buhar\u0131 miktar\u0131n\u0131n sadece yar\u0131s\u0131n\u0131 ihtiva ediyorsa, nisbi rutubeti %50 olur. Arada bir baz\u0131 \u015fartlar alt\u0131nda atmosferde k\u0131sa s\u00fcreli olarak %100\u2032\u00fc a\u015fan nisbi rutubetlere rastlanmaktad\u0131r.<\/div>\n","protected":false},"excerpt":{"rendered":"<p>BASIN\u00c7 (PRESSURE): Meteorolojide, herhangi bir yerdeki birim alana atmosfer a\u011f\u0131rl\u0131\u011f\u0131n\u0131n yaratt\u0131\u011f\u0131 kuvvettir. Atmosfer bas\u0131nc\u0131 veya baro metrik bas\u0131n\u00e7 olarak da bilinir. Herhangi bir noktadaki atmosfer bas\u0131nc\u0131 denilince, bu nokta birim alan \u00fczerinde dikey olarak uzanan havan\u0131n a\u011f\u0131rl\u0131\u011f\u0131 akla gelir. Standart atmosferde bu de\u011fer 760 mm.lik c\u0131va s\u00fctununa e\u015fittir. Bas\u0131n\u00e7 birimlerinin \u00e7eviri form\u00fclleri ise \u015f\u00f6yledir. Milibar<\/p>\n","protected":false},"author":1,"featured_media":878,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[78,77],"tags":[],"class_list":["post-877","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-meteoroloji","category-temel-bilgiler"],"_links":{"self":[{"href":"https:\/\/bizimkokpit.com\/index.php\/wp-json\/wp\/v2\/posts\/877","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/bizimkokpit.com\/index.php\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/bizimkokpit.com\/index.php\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/bizimkokpit.com\/index.php\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/bizimkokpit.com\/index.php\/wp-json\/wp\/v2\/comments?post=877"}],"version-history":[{"count":1,"href":"https:\/\/bizimkokpit.com\/index.php\/wp-json\/wp\/v2\/posts\/877\/revisions"}],"predecessor-version":[{"id":879,"href":"https:\/\/bizimkokpit.com\/index.php\/wp-json\/wp\/v2\/posts\/877\/revisions\/879"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/bizimkokpit.com\/index.php\/wp-json\/wp\/v2\/media\/878"}],"wp:attachment":[{"href":"https:\/\/bizimkokpit.com\/index.php\/wp-json\/wp\/v2\/media?parent=877"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/bizimkokpit.com\/index.php\/wp-json\/wp\/v2\/categories?post=877"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/bizimkokpit.com\/index.php\/wp-json\/wp\/v2\/tags?post=877"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}