Havadaki nemin doyma noktas\u0131n\u0131 a\u015f\u0131p, su damlac\u0131klar\u0131, buz kristalleri veya buz par\u00e7ac\u0131klar\u0131 \u015feklinde yo\u011funla\u015fmas\u0131na ya\u011f\u0131\u015f denir.<\/p>\n
1) Yerde Yo\u011funla\u015fma Bi\u00e7imindeki Ya\u011f\u0131\u015flar<\/p>\n
a) \u00c7iy : Havan\u0131n a\u00e7\u0131k ve durgun oldu\u011fu gecelerde, havadaki su buhar\u0131n\u0131n so\u011fuk cisimler \u00fczerinde su damlac\u0131klar\u0131 bi\u00e7iminde yo\u011funla\u015fmas\u0131d\u0131r. \u0130lkbahar ve yaz aylar\u0131nda g\u00f6r\u00fcl\u00fcr.<\/p>\n
UYARI: Bir b\u00f6lgede ya\u011f\u0131\u015flar\u0131n olu\u015fabilmesi i\u00e7in hava s\u0131cakl\u0131\u011f\u0131n\u0131n d\u00fc\u015fmesi, hava k\u00fctlesinin y\u00fckselmesi ve havan\u0131n doyma noktas\u0131na ula\u015fmas\u0131 gerekir. Dolu ya\u011f\u0131\u015f\u0131 orta enlemlerde, genellikle sa\u011fanak ya\u011fmurlara birlikte, ilkbahar ve yaz aylar\u0131nda g\u00f6r\u00fcl\u00fcr. \u00c7iy 0\u00b0C\u2019nin \u00fczerindeki, k\u0131ra\u011f\u0131 0\u00b0C\u2019nin alt\u0131ndaki yo\u011funla\u015fmalar ile olu\u015fur.
\n b) K\u0131ra\u011f\u0131: So\u011fuyan zeminler \u00fczerindeki yo\u011funla\u015fman\u0131n buz kristalleri \u015feklinde olmas\u0131d\u0131r. K\u0131ra\u011f\u0131n\u0131n olu\u015fabilmesi i\u00e7in de havan\u0131n a\u00e7\u0131k ve durgun olmas\u0131 gerekir.<\/p>\n
c) K\u0131r\u00e7: A\u015f\u0131r\u0131 so\u011fumu\u015f su taneciklerinden olu\u015fan bir sis uzun s\u00fcre yerde kald\u0131\u011f\u0131nda, su taneciklerinin so\u011fuk cisimlere \u00e7arparak buz haline ge\u00e7mesidir.<\/p>\n
2) Troposferde Yo\u011funla\u015fma Bi\u00e7imindeki Ya\u011f\u0131\u015flar<\/p>\n
a) Ya\u011fmur: Buluttaki su taneciklerinin damlalar halinde birle\u015ferek yery\u00fcz\u00fcne d\u00fc\u015fmesidir.<\/p>\n
b) Kar: Havadaki su buhar\u0131n\u0131n 0\u00b0C\u2019nin alt\u0131nda yo\u011funla\u015farak ince taneli buz kristallerine d\u00f6n\u00fc\u015fmesidir.<\/p>\n
c) Dolu: Dikey y\u00f6nl\u00fc hava hareketlerinin \u00e7ok g\u00fc\u00e7l\u00fc oldu\u011fu bulutlarda, s\u0131cakl\u0131\u011f\u0131n birdenbire ve b\u00fcy\u00fck \u00f6l\u00e7\u00fcde d\u00fc\u015fmesiyle su tanecikleri donar.<\/p>\n
Ya\u011f\u0131\u015f Miktar\u0131 <\/p>\n
Y\u0131l i\u00e7erisinde birim alana d\u00fc\u015fen toplam ya\u011f\u0131\u015f miktar\u0131na denir. Ya\u011f\u0131\u015f, pl\u00fcviyometre ile \u00f6l\u00e7\u00fcl\u00fcr, kg\/m2 ya da mm olarak ifade edilir.<\/p>\n
Ya\u011f\u0131\u015f Miktar\u0131n\u0131 Etkileyen Etmenler<\/p>\n
1) Hava K\u00fctlesi: Bir yerin ya\u011f\u0131\u015f alabilmesi i\u00e7in uygun hava k\u00fctlelerinin ve buna ba\u011fl\u0131 cephe sistemlerinin etkisi alt\u0131nda bulunmas\u0131 gerekir. Hava k\u00fctlesi nemli ise ya\u011f\u0131\u015f miktar\u0131 artar. \u00d6rne\u011fin T\u00fcrkiye\u2019de k\u0131\u015f ya\u011f\u0131\u015flar\u0131n\u0131n fazlal\u0131\u011f\u0131 \u0130zlanda Gezici Al\u00e7ak Bas\u0131nc\u0131\u2019n\u0131n k\u0131\u015f\u0131n daha etkili olmas\u0131n\u0131n bir sonucudur.<\/p>\n
2) Y\u00fckselti ve Yer \u015fekilleri: Deniz seviyesinden yakla\u015f\u0131k 1500 \u2013 2000 y\u00fckseltiye kadar her 100 m\u2019de ya\u011f\u0131\u015f miktar\u0131 50 \u2013 400 mm aras\u0131nda artar. Bu y\u00fckseltiden sonra ya\u011f\u0131\u015flar azal\u0131r. \u00c7\u00fcnk\u00fc i\u00e7indeki nemin b\u00fcy\u00fck b\u00f6l\u00fcm\u00fcn\u00fc yamac\u0131n orta b\u00f6l\u00fcmlerine b\u0131rakan hava k\u00fctlesi doruklara kuru olarak ge\u00e7er. Nemli hava k\u00fctlelerine d\u00f6n\u00fck yama\u00e7larda ya\u011f\u0131\u015f\u0131n fazla, ters yama\u00e7larda ya\u011f\u0131\u015f\u0131n az olmas\u0131 ise yer \u015fekillerinin ya\u011f\u0131\u015f miktar\u0131na etkisini kan\u0131tlar.<\/p>\n
3) Denize Etkisine Kapal\u0131l\u0131k: Denizden uzakla\u015ft\u0131k\u00e7a ya\u011f\u0131\u015f miktar\u0131 azalmaktad\u0131r. \u00c7\u00fcnk\u00fc, nemli hava k\u00fctleleri, i\u00e7indeki nemin b\u00fcy\u00fck bir b\u00f6l\u00fcm\u00fcn\u00fc k\u0131y\u0131 kesimlerinde b\u0131rak\u0131r ve i\u00e7erilere daha kuru olarak sokulur.<\/p>\n
4) Ak\u0131nt\u0131lar: S\u0131cak su ak\u0131nt\u0131lar\u0131n\u0131n etkisiyle \u0131s\u0131n\u0131p nemlenen hava k\u00fctleleri serin kara \u00fczerine geldi\u011finde ya\u011f\u0131\u015f b\u0131rak\u0131r. \u00d6rne\u011fin, \u0130ngiltere ve Japonya k\u0131y\u0131lar\u0131nda ya\u011f\u0131\u015f miktar\u0131n\u0131n fazla olmas\u0131nda s\u0131cak su ak\u0131nt\u0131lar\u0131 etkilidir. So\u011fuk su ak\u0131nt\u0131lar\u0131n\u0131n ge\u00e7ti\u011fi k\u0131y\u0131larda ise ya\u011f\u0131\u015f miktar\u0131n\u0131n azald\u0131\u011f\u0131 g\u00f6r\u00fcl\u00fcr.<\/p>\n
5) Bitki \u00d6rt\u00fcs\u00fc: \u00d6zellikle ormanlardaki terleme, nem miktar\u0131n\u0131 art\u0131rd\u0131\u011f\u0131ndan ya\u011f\u0131\u015flar %3 \u2013 6 oran\u0131nda artar.<\/p>\n
Ya\u011f\u0131\u015f Tipleri :<\/p>\n
1) Y\u00fckselim (Konveksiyon) Ya\u011f\u0131\u015flar\u0131: Is\u0131narak y\u00fckselen havan\u0131n so\u011fumas\u0131 ile olu\u015fan ya\u011f\u0131\u015flard\u0131r. <\/p>\n
Ekvator \u00e7evresinde y\u0131l boyunca orta enlemlerde ilkbahar ve yaz aylar\u0131nda bu tip ya\u011f\u0131\u015flar g\u00f6r\u00fcl\u00fcr.<\/p>\n
T\u00fcrkiye\u2019de ilkbahar ve yaz ba\u015flar\u0131nda kuzeybat\u0131dan gelen nemli ve so\u011fuk hava, \u0130\u00e7 Anadolu\u2019da \u0131s\u0131narak, y\u00fckselir ve ya\u011f\u0131\u015f b\u0131rak\u0131r. Bu ya\u011f\u0131\u015flara k\u0131rkikindi ya\u011fmurlar\u0131 denir.<\/p>\n
2) Yama\u00e7 (Orografik) Ya\u011f\u0131\u015flar\u0131: Nemli hava k\u00fctlelerinin bir da\u011f yamac\u0131na \u00e7arparak y\u00fckselmesi sonucunda olu\u015fan ya\u011f\u0131\u015flard\u0131r.<\/p>\n
Orografik ya\u011f\u0131\u015flar en \u00e7ok k\u0131y\u0131ya paralel uzanan da\u011flar\u0131n denize d\u00f6n\u00fck yama\u00e7lar\u0131nda g\u00f6r\u00fcl\u00fcr.<\/p>\n
T\u00fcrkiye\u2019de Toroslar ve Kuzey Anadolu Da\u011flar\u0131\u2019nda yama\u00e7 ya\u011f\u0131\u015f\u0131 belirgindir.<\/p>\n
UYARI: Egemen r\u00fczgar y\u00f6n\u00fcne d\u00fck uzanan da\u011f yama\u00e7lar\u0131 orografik ya\u011f\u0131\u015flar\u0131 al\u0131r.<\/p>\n
3) Cephe Ya\u011f\u0131\u015flar\u0131: S\u0131cak ve so\u011fuk hava k\u00fctlelerinin kar\u015f\u0131la\u015fma alanlar\u0131nda olu\u015fan ya\u011f\u0131\u015flard\u0131r.<\/p>\n
Yery\u00fcz\u00fcndeki ya\u011f\u0131\u015flar\u0131n \u00f6nemli bir b\u00f6l\u00fcm\u00fcn\u00fc bu tip ya\u011f\u0131\u015flar olu\u015fturur.<\/p>\n
Bat\u0131 ve Orta Avrupa ile okyanusal iklim b\u00f6lgelerinde her mevsim, Akdeniz iklim b\u00f6lgelerinde k\u0131\u015f aylar\u0131nda cephesel ya\u011f\u0131\u015flar g\u00f6r\u00fcl\u00fcr.<\/p>\n
D\u00fcnya\u2019da Ya\u011f\u0131\u015f\u0131n Da\u011f\u0131l\u0131\u015f\u0131 <\/p>\n
A) \u00c7ok Ya\u011f\u0131\u015fl\u0131 B\u00f6lgeler<\/p>\n
1) Ekvatoral B\u00f6lge: Y\u0131l boyunca \u0131s\u0131nman\u0131n fazla olmas\u0131 nedeniyle y\u00fckselim ya\u011f\u0131\u015flar\u0131 g\u00f6r\u00fcl\u00fcr. Bu b\u00f6lgede kar\u015f\u0131la\u015fan kuzey ve g\u00fcney alizeleri de y\u00fckselim ya\u011f\u0131\u015flar\u0131na yol a\u00e7ar. Her mevsim ya\u011f\u0131\u015fl\u0131 olan ekvatoral b\u00f6lgede, Mart ve Eyl\u00fcl aylar\u0131nda ya\u011f\u0131\u015f miktar\u0131 artar. Y\u0131ll\u0131k ya\u011f\u0131\u015f toplam\u0131 2000 mm civar\u0131ndad\u0131r.<\/p>\n
2) Muson Asyas\u0131: Yaz musonlar\u0131n\u0131n etkisiyle yaz aylar\u0131nda bol ya\u011f\u0131\u015f al\u0131r. Ya\u011f\u0131\u015flar, yama\u00e7 ya\u011f\u0131\u015f\u0131 \u015feklindedir. K\u0131\u015f aylar\u0131 genellikle kurak ge\u00e7er. Y\u0131ll\u0131k ya\u011f\u0131\u015f miktar\u0131 2000 mm\u2019nin \u00fcst\u00fcndedir.<\/p>\n
3) Orta Ku\u015fak Karalar\u0131n Bat\u0131 K\u0131y\u0131lar\u0131: Her mevsimin ya\u011f\u0131\u015fl\u0131 oldu\u011fu b\u00f6lgelerdir. K\u0131\u015f ya\u011f\u0131\u015flar\u0131n\u0131n nedeni gezici al\u00e7ak bas\u0131n\u00e7 ve buna ba\u011fl\u0131 cephe sistemleridir. Da\u011fl\u0131k k\u0131yalarda yer \u015fekilleri ya\u011f\u0131\u015f miktar\u0131n\u0131 art\u0131r\u0131c\u0131 etki yapar. Ayr\u0131ca bu k\u0131y\u0131lar bati r\u00fczgarlar\u0131 ve s\u0131cak su ak\u0131nt\u0131lar\u0131n\u0131n etkisi alt\u0131ndad\u0131r. <\/p>\n
UYARI: Kuzey Amerika Kitasi\u2019n\u0131n do\u011fu k\u0131y\u0131s\u0131nda tropikal siklonlar nedeniyle \u00e7ok ya\u011f\u0131\u015f g\u00f6r\u00fcl\u00fcr.
\n B) Ya\u011f\u0131\u015fl\u0131 B\u00f6lgeler<\/p>\n
1) Akdeniz B\u00f6lgeleri: 30\u00b0 – 40\u00b0 enlemleri aras\u0131nda k\u0131\u015flar\u0131 ya\u011f\u0131\u015fl\u0131, yazlar\u0131 kurak bir ya\u011f\u0131\u015f rejimi geli\u015fmi\u015ftir. B\u00f6lge, yaz\u0131n subtropikal y\u00fcksek bas\u0131n\u00e7lar\u0131n, k\u0131\u015f\u0131n ise bat\u0131 r\u00fczgarlar\u0131 ve ge\u00e7ici al\u00e7ak bas\u0131n\u00e7lar\u0131n etkisinde kal\u0131r. K\u0131\u015f ya\u011f\u0131\u015flar\u0131, cephesel ya\u011f\u0131\u015flard\u0131r. Da\u011fl\u0131k alanlarda ise orografik cephesel ya\u011f\u0131lar g\u00f6r\u00fcl\u00fcr.<\/p>\n
2) Orta Ku\u015fak K\u0131talar\u0131n\u0131n Do\u011fu K\u0131y\u0131lar\u0131: Her mevsimi ya\u011f\u0131\u015fl\u0131d\u0131r. Genellikle ya\u011f\u0131\u015flar cepheseldir. Ancak yaz mevsiminde konveksiyonal ya\u011f\u0131\u015flar da g\u00f6r\u00fcl\u00fcr. So\u011fuk su ak\u0131nt\u0131lar\u0131 baz\u0131 k\u0131y\u0131larda \u00e7\u00f6llerin geli\u015fmesine neden olmu\u015ftur.<\/p>\n
3) Savan B\u00f6lgeleri: 10\u00b0 – 20\u00b0 enlemleri aras\u0131nda, k\u0131\u015flar\u0131n kurak, yazlar\u0131n ise ya\u011f\u0131\u015fl\u0131 ge\u00e7ti\u011fi b\u00f6lgelerdir. Yaz ya\u011f\u0131\u015flar\u0131 konveksiynal ya\u011f\u0131\u015flard\u0131r. K\u0131\u015f kurakl\u0131\u011f\u0131n\u0131n nedeni subtropikal y\u00fcksek bas\u0131n\u00e7 alan\u0131n\u0131n Ekvator\u2019a do\u011fru kaymas\u0131d\u0131r.<\/p>\n
C) Az Ya\u011f\u0131\u015fl\u0131 B\u00f6lgeler<\/p>\n
Orta ku\u015fak karasal b\u00f6lgelerde k\u0131\u015f\u0131n, karalar\u0131n i\u00e7 k\u0131s\u0131mlar\u0131nda havan\u0131n so\u011fuk olmas\u0131 nedeniyle antisiklon alanlar\u0131 olu\u015fur. Nemli havan\u0131n i\u00e7 k\u0131s\u0131mlara sokulmas\u0131n\u0131 \u00f6nler. Buralarda k\u0131\u015flar biraz nemli ancak ya\u011f\u0131\u015fs\u0131zd\u0131r. \u0130lkbahar ve yaz aylar\u0131nda ise \u0131s\u0131nmaya ba\u011fl\u0131 konveksiyonal ya\u011f\u0131\u015flar g\u00f6r\u00fcl\u00fcr.<\/p>\n
D) Kurak B\u00f6lgeler<\/p>\n
1) Subtropikal Y\u00fcksek Bas\u0131n\u00e7 B\u00f6lgeleri: 20\u00b0 – 30\u00b0 enlemleri aras\u0131nda y\u0131l boyunca ya\u011f\u0131\u015f\u0131n \u00e7ok az g\u00f6r\u00fcld\u00fc\u011f\u00fc hatta baz\u0131 y\u0131llarda ya\u011f\u0131\u015f\u0131n hi\u00e7 g\u00f6r\u00fclmedi\u011fi b\u00f6lgeler vard\u0131r. Al\u00e7al\u0131c\u0131 hava hareketleri nem a\u00e7\u0131\u011f\u0131n\u0131 b\u00fcy\u00fct\u00fcr ve kurakl\u0131\u011f\u0131n belirginle\u015fmesine neden olur. Bu b\u00f6lgeler, B\u00fcy\u00fck Sahra, Arabistan ve Avustralya\u2019da geni\u015ftir. G\u00fcney Afrika, G\u00fcney Amerika ve Meksika\u2019da daha dar alanl\u0131d\u0131r.<\/p>\n
2) Orta Ku\u015fak K\u0131talar\u0131n\u0131n Deniz Etkisine Kapal\u0131 \u0130\u00e7 K\u0131s\u0131mlar\u0131: Denizden \u00e7ok uzak olan bu b\u00f6lgelere nemli r\u00fczgarlar ula\u015famaz. K\u0131y\u0131ya paralel uzanan da\u011f s\u0131ralar\u0131 da nemli r\u00fczgarlar\u0131 engelledi\u011fi i\u00e7in bu b\u00f6lgelerde kurakl\u0131k belirgindir. \u00d6rne\u011fin Orta Asya \u00e7\u00f6llerinin olu\u015fumu buna ba\u011fl\u0131d\u0131r.<\/p>\n
3) Kutuplar: Kutuplar \u00e7evresi so\u011fuk oldu\u011fundan havan\u0131n mutlak nemi d\u00fc\u015f\u00fck ve ya\u011f\u0131\u015f miktar\u0131 azd\u0131r. Ayr\u0131ca buralarda y\u00fcksek bas\u0131n\u00e7 alan\u0131n\u0131n egemen olmas\u0131 ya\u011f\u0131\u015flar\u0131 \u00f6nler. Buralara daha \u00e7ok so\u011fuk \u00e7\u00f6ller denir.<\/p>\n
T\u00fcrkiye\u2019de Ya\u011f\u0131\u015f\u0131n Da\u011f\u0131l\u0131\u015f\u0131<\/p>\n
\u2022 T\u00fcrkiye\u2019de genellikle Akdeniz ya\u011f\u0131\u015f rejiminin etkisi g\u00f6r\u00fcl\u00fcr.
\n \u2022 En \u00e7ok ya\u011f\u0131\u015f k\u0131y\u0131 b\u00f6lgelerde g\u00f6r\u00fcl\u00fcr. \u0130\u00e7 k\u0131s\u0131mlara gidildik\u00e7e ya\u011f\u0131\u015f miktar\u0131 azal\u0131r.
\n \u2022 En az ya\u011f\u0131\u015f alan yer Konya ve Tuz G\u00f6l\u00fc \u00e7evresi ile baz\u0131 derin yar\u0131lm\u0131\u015f akarsu vadilerinin tabanlar\u0131d\u0131r.
\n \u2022 Karadeniz k\u0131y\u0131lar\u0131nda sonbahar, Akdeniz k\u0131y\u0131lar\u0131nda k\u0131\u015f, \u0130\u00e7 Anadolu\u2019da \u0130lkbahar ve Erzurum \u2013 Kars B\u00f6l\u00fcm\u00fcnde az ya\u011f\u0131\u015flar\u0131 belirgindir.
\n \u2022 T\u00fcrkiye genelinde k\u0131\u015f aylar\u0131nda g\u00f6r\u00fclen ya\u011f\u0131\u015flar cephesel ya\u011f\u0131\u015flard\u0131r. \u00c7\u00fcnk\u00fc k\u0131\u015f aylar\u0131nda Anadolu, gezici al\u00e7ak ve y\u00fcksek bas\u0131n\u00e7lar\u0131n etkisi alt\u0131ndad\u0131r. Bu bas\u0131n\u00e7lar cephesel ya\u011f\u0131\u015flara neden olur. <\/p>\n
UYARI: 30\u00b0 Kuzey enlemindeki dinamik y\u00fcksek bas\u0131n\u00e7 alan\u0131n\u0131n yaz aylar\u0131nda 40\u00b0 Kuzey enlemine do\u011fru geni\u015flemesi nedeniyle Karadeniz k\u0131y\u0131lar\u0131 d\u0131\u015f\u0131nda yaz kurakl\u0131\u011f\u0131 olu\u015fur.<\/p>\n","protected":false},"excerpt":{"rendered":"
Havadaki nemin doyma noktas\u0131n\u0131 a\u015f\u0131p, su damlac\u0131klar\u0131, buz kristalleri veya buz par\u00e7ac\u0131klar\u0131 \u015feklinde yo\u011funla\u015fmas\u0131na ya\u011f\u0131\u015f denir. 1) Yerde Yo\u011funla\u015fma Bi\u00e7imindeki Ya\u011f\u0131\u015flar a) \u00c7iy : Havan\u0131n a\u00e7\u0131k ve durgun oldu\u011fu gecelerde, havadaki su buhar\u0131n\u0131n so\u011fuk cisimler \u00fczerinde su damlac\u0131klar\u0131 bi\u00e7iminde yo\u011funla\u015fmas\u0131d\u0131r. \u0130lkbahar ve yaz aylar\u0131nda g\u00f6r\u00fcl\u00fcr. UYARI: Bir b\u00f6lgede ya\u011f\u0131\u015flar\u0131n olu\u015fabilmesi i\u00e7in hava s\u0131cakl\u0131\u011f\u0131n\u0131n d\u00fc\u015fmesi, hava …<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1403,1406],"tags":[3707,3702,2887,3150,3703,3704,3062,2835,3708,3705,3700,3706,3701],"class_list":["post-1263","post","type-post","status-publish","format-standard","hentry","category-odevler","category-sosyal-bilgiler-odevleri","tag-cephe-yagislari","tag-ciy","tag-ekvator","tag-kar","tag-kiragi","tag-kirc","tag-nem","tag-troposfer","tag-turkiyede-yagisin-dagilisi","tag-yagis-miktarini-etkileyen-etmenler","tag-yagis-nedir","tag-yagis-tipleri","tag-yerde-yogunlasma-bicimindeki-yagislar"],"_links":{"self":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/1263","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/comments?post=1263"}],"version-history":[{"count":0,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/1263\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/media?parent=1263"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/categories?post=1263"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/tags?post=1263"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}