{"id":3883,"date":"2026-10-13T08:29:43","date_gmt":"2026-10-13T07:29:43","guid":{"rendered":"https:\/\/www.laurensoff.com\/wordpress\/?p=3883"},"modified":"2026-10-13T08:29:43","modified_gmt":"2026-10-13T07:29:43","slug":"est-ce-que-les-temperatures-en-france-sont-dues-a-el-nino","status":"publish","type":"post","link":"https:\/\/www.laurensoff.com\/wordpress\/est-ce-que-les-temperatures-en-france-sont-dues-a-el-nino\/","title":{"rendered":"Est-ce que les temp\u00e9ratures en France sont dues \u00e0 El Ni\u00f1o?"},"content":{"rendered":"<p id=\"p-rc_cff2719186679598-28\" data-path-to-node=\"0\"><b data-path-to-node=\"0\" data-index-in-node=\"0\"><span class=\"citation-131\">les temp\u00e9ratures en France m\u00e9tropolitaine ne sont pas directement caus\u00e9es par El Ni\u00f1o<\/span><\/b><span class=\"citation-131 citation-end-131\">.<\/span><\/p>\n<p id=\"p-rc_cff2719186679598-29\" data-path-to-node=\"1\"><span class=\"citation-130 citation-end-130\">Bien qu\u2019El Ni\u00f1o soit un ph\u00e9nom\u00e8ne mondial majeur, ses effets sur le climat de l&#8217;Europe de l&#8217;Ouest sont indirects, faibles et difficilement pr\u00e9visibles.<\/span><\/p>\n<h3 data-path-to-node=\"3\">1. Pourquoi El Ni\u00f1o n&#8217;a qu&#8217;un impact tr\u00e8s limit\u00e9 en France<\/h3>\n<ul data-path-to-node=\"4\">\n<li>\n<p id=\"p-rc_cff2719186679598-30\" data-path-to-node=\"4,0,0\"><b data-path-to-node=\"4,0,0\" data-index-in-node=\"0\"><span class=\"citation-129 citation-end-129\">L&#8217;\u00e9loignement g\u00e9ographique :<\/span><\/b> <span class=\"citation-128 citation-end-128\">El Ni\u00f1o se d\u00e9roule dans l&#8217;oc\u00e9an Pacifique \u00e9quatorial.<\/span> <span class=\"citation-127 citation-end-127\">Ses impacts sont directs et massifs sur les zones environnantes (Am\u00e9rique du Sud, Asie du Sud-Est, Oc\u00e9anie, Afrique), mais doivent traverser toute la circulation atmosph\u00e9rique plan\u00e9taire pour atteindre l&#8217;Europe.<\/span><\/p>\n<\/li>\n<li>\n<p id=\"p-rc_cff2719186679598-31\" data-path-to-node=\"4,1,0\"><b data-path-to-node=\"4,1,0\" data-index-in-node=\"0\">L&#8217;influence dominante de l&#8217;oc\u00e9an Atlantique :<\/b> <span class=\"citation-126\">La m\u00e9t\u00e9o en France d\u00e9pend principalement de l&#8217;oc\u00e9an Atlantique nord (notamment de l&#8217;Oscillation Nord-Atlantique et du <\/span><i data-path-to-node=\"4,1,0\" data-index-in-node=\"164\"><span class=\"citation-126\">Gulf Stream<\/span><\/i><span class=\"citation-126 citation-end-126\">), qui masque ou att\u00e9nue la plupart des signaux venus du Pacifique.<\/span><\/p>\n<\/li>\n<\/ul>\n<h3 id=\"p-rc_cff2719186679598-32\" data-path-to-node=\"5\"><span class=\"citation-125 citation-end-125\">2. L&#8217;impact r\u00e9el d&#8217;El Ni\u00f1o (le lien indirect)<\/span><\/h3>\n<p id=\"p-rc_cff2719186679598-33\" data-path-to-node=\"6\"><span class=\"citation-124 citation-end-124\">M\u00eame si El Ni\u00f1o n&#8217;explique pas les temp\u00e9ratures au jour le jour en France, il agit de deux fa\u00e7ons \u00e0 l&#8217;\u00e9chelle globale :<\/span><\/p>\n<ul data-path-to-node=\"7\">\n<li>\n<p data-path-to-node=\"7,0,0\"><b data-path-to-node=\"7,0,0\" data-index-in-node=\"0\">Un &#8220;booster&#8221; de la temp\u00e9rature moyenne mondiale :<\/b> El Ni\u00f1o lib\u00e8re une quantit\u00e9 ph\u00e9nom\u00e9nale de chaleur dans l&#8217;atmosph\u00e8re, ce qui fait grimper la temp\u00e9rature moyenne globale de la plan\u00e8te. Cette hausse g\u00e9n\u00e9rale peut indirectement accentuer des p\u00e9riodes plus chaudes dans plusieurs r\u00e9gions du globe.<\/p>\n<\/li>\n<li>\n<p id=\"p-rc_cff2719186679598-34\" data-path-to-node=\"7,1,0\"><b data-path-to-node=\"7,1,0\" data-index-in-node=\"0\"><span class=\"citation-123 citation-end-123\">Impact sur les Outre-mer :<\/span><\/b> Si la m\u00e9tropole subit peu l&#8217;influence d&#8217;El Ni\u00f1o, <b data-path-to-node=\"7,1,0\" data-index-in-node=\"76\">certains territoires fran\u00e7ais d&#8217;Outre-mer<\/b> subissent des effets tr\u00e8s marqu\u00e9s (s\u00e9cheresses plus importantes en Guyane ou en Nouvelle-Cal\u00e9donie, anomalies thermiques).<\/p>\n<\/li>\n<\/ul>\n<h3 data-path-to-node=\"8\">3. Quels sont alors les vrais responsables des temp\u00e9ratures en France ?<\/h3>\n<p data-path-to-node=\"9\">Les variations et la hausse r\u00e9currente des temp\u00e9ratures en France s&#8217;expliquent principalement par :<\/p>\n<ol start=\"1\" data-path-to-node=\"10\">\n<li>\n<p id=\"p-rc_cff2719186679598-35\" data-path-to-node=\"10,0,0\"><b data-path-to-node=\"10,0,0\" data-index-in-node=\"0\"><span class=\"citation-122 citation-end-122\">Le changement climatique d&#8217;origine humaine :<\/span><\/b> <span class=\"citation-121 citation-end-121\">Il hausse la moyenne globale des temp\u00e9ratures et augmente la fr\u00e9quence ainsi que l&#8217;intensit\u00e9 des vagues de chaleur.<\/span><\/p>\n<\/li>\n<li>\n<p data-path-to-node=\"10,1,0\"><b data-path-to-node=\"10,1,0\" data-index-in-node=\"0\">La variabilit\u00e9 m\u00e9t\u00e9orologique r\u00e9gionale :<\/b> Les configurations atmosph\u00e9riques au-dessus de l&#8217;Atlantique et de l&#8217;Europe (blocages anticycloniques, remont\u00e9es d&#8217;air chaud saharien, etc.).<\/p>\n<\/li>\n<\/ol>\n<p data-path-to-node=\"11\"><span class=\"citation-120\">En r\u00e9sum\u00e9 : <\/span><b data-path-to-node=\"11\" data-index-in-node=\"12\"><span class=\"citation-120 citation-end-120\">El Ni\u00f1o participe au r\u00e9chauffement global de la plan\u00e8te, mais les temp\u00e9ratures ressenties en France d\u00e9pendent avant tout des dynamiques de l&#8217;Atlantique et du r\u00e9chauffement climatique global.<\/span><\/b><\/p>\n<p data-path-to-node=\"0\"><b data-path-to-node=\"0\" data-index-in-node=\"0\">El Ni\u00f1o<\/b> est un ph\u00e9nom\u00e8ne climatique naturel caract\u00e9ris\u00e9 par une <b data-path-to-node=\"0\" data-index-in-node=\"64\">anomalie chaude des eaux de surface de l&#8217;oc\u00e9an Pacifique<\/b> \u00e9quatorial, principalement dans sa partie centrale et orientale.<\/p>\n<p data-path-to-node=\"1\">Voici les points cl\u00e9s pour comprendre ce ph\u00e9nom\u00e8ne :<\/p>\n<h3 data-path-to-node=\"2\">1. Fonctionnement du ph\u00e9nom\u00e8ne<\/h3>\n<ul data-path-to-node=\"3\">\n<li>\n<p data-path-to-node=\"3,0,0\"><b data-path-to-node=\"3,0,0\" data-index-in-node=\"0\">\u00c9tat normal (Walker circulation) :<\/b> Habituellement, les aliz\u00e9s (vents soufflant d&#8217;est en ouest) poussent les eaux chaudes de surface vers l&#8217;Indon\u00e9sie et l&#8217;Australie. Cela provoque une remont\u00e9e d&#8217;eaux profondes et froides (upwelling) le long des c\u00f4tes de l&#8217;Am\u00e9rique du Sud.<\/p>\n<\/li>\n<li>\n<p data-path-to-node=\"3,1,0\"><b data-path-to-node=\"3,1,0\" data-index-in-node=\"0\">Pendant El Ni\u00f1o :<\/b> Les aliz\u00e9s s&#8217;affaiblissent, voire s&#8217;inversent. L&#8217;immense r\u00e9servoir d&#8217;eau chaude accumul\u00e9e \u00e0 l&#8217;ouest se d\u00e9place alors vers l&#8217;est, venant \u00e9touffer les eaux froides sud-am\u00e9ricaines.<\/p>\n<\/li>\n<\/ul>\n<h3 data-path-to-node=\"4\">2. Cons\u00e9quences climatiques mondiales<\/h3>\n<p data-path-to-node=\"5\">El Ni\u00f1o perturbe la circulation atmosph\u00e9rique globale et entra\u00eene des bouleversements m\u00e9t\u00e9orologiques majeurs \u00e0 travers la plan\u00e8te, g\u00e9n\u00e9ralement tous les 2 \u00e0 7 ans :<\/p>\n<ul data-path-to-node=\"6\">\n<li>\n<p data-path-to-node=\"6,0,0\"><b data-path-to-node=\"6,0,0\" data-index-in-node=\"0\">En Am\u00e9rique du Sud :<\/b> Fortes pluies, inondations et temp\u00eates sur la c\u00f4te pacifique (notamment au P\u00e9rou et en \u00c9quateur).<\/p>\n<\/li>\n<li>\n<p data-path-to-node=\"6,1,0\"><b data-path-to-node=\"6,1,0\" data-index-in-node=\"0\">En Asie du Sud-Est et en Oc\u00e9anie :<\/b> S\u00e9cheresses s\u00e9v\u00e8res, vagues de chaleur et risques accrus de feux de for\u00eat (en Indon\u00e9sie, en Australie, etc.).<\/p>\n<\/li>\n<li>\n<p data-path-to-node=\"6,2,0\"><b data-path-to-node=\"6,2,0\" data-index-in-node=\"0\">En Afrique et en Am\u00e9rique du Nord :<\/b> S\u00e9cheresses dans certaines r\u00e9gions (comme l&#8217;Afrique australe) et hivers plus doux ou humides dans d&#8217;autres.<\/p>\n<\/li>\n<li>\n<p data-path-to-node=\"6,3,0\"><b data-path-to-node=\"6,3,0\" data-index-in-node=\"0\">Effet global sur les temp\u00e9ratures :<\/b> Les ann\u00e9es El Ni\u00f1o co\u00efncident souvent avec des records de temp\u00e9rature moyenne mondiale \u00e0 la surface du globe.<\/p>\n<\/li>\n<\/ul>\n<h3 data-path-to-node=\"7\">3. Le cycle complet (ENSO)<\/h3>\n<p data-path-to-node=\"8\">El Ni\u00f1o fait partie d&#8217;un cycle plus large appel\u00e9 <b data-path-to-node=\"8\" data-index-in-node=\"49\">ENSO<\/b> (<i data-path-to-node=\"8\" data-index-in-node=\"55\">El Ni\u00f1o Southern Oscillation<\/i> ou Oscillation australe), qui comprend trois phases :<\/p>\n<ol start=\"1\" data-path-to-node=\"9\">\n<li>\n<p data-path-to-node=\"9,0,0\"><b data-path-to-node=\"9,0,0\" data-index-in-node=\"0\">El Ni\u00f1o<\/b> (la phase chaude).<\/p>\n<\/li>\n<li>\n<p data-path-to-node=\"9,1,0\"><b data-path-to-node=\"9,1,0\" data-index-in-node=\"0\">La Ni\u00f1a<\/b> (la phase inverse, caract\u00e9ris\u00e9e par des eaux anormalement froides dans le Pacifique).<\/p>\n<\/li>\n<li>\n<p data-path-to-node=\"9,2,0\"><b data-path-to-node=\"9,2,0\" data-index-in-node=\"0\">La phase neutre<\/b> (situation normale).<\/p>\n<p data-path-to-node=\"0\"><b data-path-to-node=\"0\" data-index-in-node=\"0\">La Ni\u00f1a<\/b> est la phase froide du cycle climatique <b data-path-to-node=\"0\" data-index-in-node=\"48\">ENSO<\/b> (<i data-path-to-node=\"0\" data-index-in-node=\"54\">El Ni\u00f1o Southern Oscillation<\/i>). C&#8217;est le ph\u00e9nom\u00e8ne exactement inverse d&#8217;El Ni\u00f1o.<\/p>\n<p data-path-to-node=\"1\">Voici ce qu&#8217;il faut savoir sur La Ni\u00f1a :<\/p>\n<h3 data-path-to-node=\"3\">1. Comment fonctionne La Ni\u00f1a ?<\/h3>\n<p data-path-to-node=\"4\">Pendant une p\u00e9riode La Ni\u00f1a, la circulation atmosph\u00e9rique et oc\u00e9anique normale s&#8217;intensifie fortement :<\/p>\n<ul data-path-to-node=\"5\">\n<li>\n<p data-path-to-node=\"5,0,0\"><b data-path-to-node=\"5,0,0\" data-index-in-node=\"0\">Des aliz\u00e9s plus puissants :<\/b> Les vents d&#8217;est soufflent beaucoup plus fort que d&#8217;habitude le long de l&#8217;\u00e9quateur.<\/p>\n<\/li>\n<li>\n<p data-path-to-node=\"5,1,0\"><b data-path-to-node=\"5,1,0\" data-index-in-node=\"0\">Refroidissement des eaux :<\/b> Ces vents pouss\u00e9s vers l&#8217;ouest accumulent les eaux chaudes pr\u00e8s de l&#8217;Asie et de l&#8217;Australie, ce qui provoque une remont\u00e9e exceptionnelle d&#8217;eaux froides profondes (<i data-path-to-node=\"5,1,0\" data-index-in-node=\"190\">upwelling<\/i>) le long des c\u00f4tes de l&#8217;Am\u00e9rique du Sud.<\/p>\n<\/li>\n<li>\n<p data-path-to-node=\"5,2,0\"><b data-path-to-node=\"5,2,0\" data-index-in-node=\"0\">Anomalie thermique :<\/b> Les eaux de surface du Pacifique \u00e9quatorial central et oriental deviennent nettement plus froides que la normale.<\/p>\n<\/li>\n<\/ul>\n<h3 data-path-to-node=\"7\">2. Cons\u00e9quences climatiques globales<\/h3>\n<p data-path-to-node=\"8\">Tout comme El Ni\u00f1o, La Ni\u00f1a perturbe le climat mondial, mais souvent de mani\u00e8re oppos\u00e9e :<\/p>\n<table data-path-to-node=\"9\">\n<thead>\n<tr>\n<td><strong>R\u00e9gion<\/strong><\/td>\n<td><strong>Effets habituels de La Ni\u00f1a<\/strong><\/td>\n<\/tr>\n<\/thead>\n<tbody>\n<tr>\n<td><span data-path-to-node=\"9,1,0,0\"><b data-path-to-node=\"9,1,0,0\" data-index-in-node=\"0\">Asie du Sud-Est &amp; Australie<\/b><\/span><\/td>\n<td><span data-path-to-node=\"9,1,1,0\">Fortes pluies, moussons plus intenses et risques accrus d&#8217;inondations.<\/span><\/td>\n<\/tr>\n<tr>\n<td><span data-path-to-node=\"9,2,0,0\"><b data-path-to-node=\"9,2,0,0\" data-index-in-node=\"0\">Am\u00e9rique du Sud (c\u00f4te pacifique)<\/b><\/span><\/td>\n<td><span data-path-to-node=\"9,2,1,0\">Temps plus sec et plus frais que la normale (favorable \u00e0 la p\u00eache gr\u00e2ce aux eaux profondes riches en nutriments).<\/span><\/td>\n<\/tr>\n<tr>\n<td><span data-path-to-node=\"9,3,0,0\"><b data-path-to-node=\"9,3,0,0\" data-index-in-node=\"0\">Am\u00e9rique du Nord<\/b><\/span><\/td>\n<td><span data-path-to-node=\"9,3,1,0\">Hivers plus frais et humides au nord-ouest des \u00c9.-U. \/ Canada, mais plus secs et chauds au sud.<\/span><\/td>\n<\/tr>\n<tr>\n<td><span data-path-to-node=\"9,4,0,0\"><b data-path-to-node=\"9,4,0,0\" data-index-in-node=\"0\">Atlantique Nord<\/b><\/span><\/td>\n<td><span data-path-to-node=\"9,4,1,0\">Augmentation de l&#8217;activit\u00e9 des <b data-path-to-node=\"9,4,1,0\" data-index-in-node=\"31\">cyclones et ouragans<\/b>.<\/span><\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<h3 data-path-to-node=\"11\">3. Quel est l&#8217;impact de La Ni\u00f1a sur les temp\u00e9ratures mondiales et en France ?<\/h3>\n<ul data-path-to-node=\"12\">\n<li>\n<p data-path-to-node=\"12,0,0\"><b data-path-to-node=\"12,0,0\" data-index-in-node=\"0\">\u00c0 l&#8217;\u00e9chelle mondiale :<\/b> La Ni\u00f1a a un effet <b data-path-to-node=\"12,0,0\" data-index-in-node=\"42\">temporairement refroidissant<\/b> sur la temp\u00e9rature moyenne de la plan\u00e8te, car l&#8217;oc\u00e9an Pacifique absorbe davantage de chaleur. Cependant, elle ne stoppe pas le r\u00e9chauffement climatique global provoqu\u00e9 par les activit\u00e9s humaines (une ann\u00e9e La Ni\u00f1a aujourd&#8217;hui reste souvent plus chaude que les ann\u00e9es El Ni\u00f1o d&#8217;il y a quelques d\u00e9cennies).<\/p>\n<\/li>\n<li>\n<p data-path-to-node=\"12,1,0\"><b data-path-to-node=\"12,1,0\" data-index-in-node=\"0\">En France :<\/b> Tout comme pour El Ni\u00f1o, l&#8217;effet direct de La Ni\u00f1a sur la France m\u00e9tropolitaine est <b data-path-to-node=\"12,1,0\" data-index-in-node=\"96\">tr\u00e8s faible \u00e0 n\u00e9gligeable<\/b>. La m\u00e9t\u00e9o fran\u00e7aise reste domin\u00e9e par l&#8217;influence de l&#8217;oc\u00e9an Atlantique et par les variations locales des masses d&#8217;air.\u00a0 <img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-full wp-image-3887\" src=\"https:\/\/www.laurensoff.com\/wordpress\/wp-content\/uploads\/2026\/10\/images-3-4.jpg\" alt=\"\" width=\"640\" height=\"427\" srcset=\"https:\/\/www.laurensoff.com\/wordpress\/wp-content\/uploads\/2026\/10\/images-3-4.jpg 640w, https:\/\/www.laurensoff.com\/wordpress\/wp-content\/uploads\/2026\/10\/images-3-4-300x200.jpg 300w, https:\/\/www.laurensoff.com\/wordpress\/wp-content\/uploads\/2026\/10\/images-3-4-600x400.jpg 600w\" sizes=\"auto, (max-width: 640px) 100vw, 640px\" \/><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-full wp-image-3885\" src=\"https:\/\/www.laurensoff.com\/wordpress\/wp-content\/uploads\/2026\/10\/images-1-7.jpg\" alt=\"\" width=\"399\" height=\"501\" srcset=\"https:\/\/www.laurensoff.com\/wordpress\/wp-content\/uploads\/2026\/10\/images-1-7.jpg 399w, https:\/\/www.laurensoff.com\/wordpress\/wp-content\/uploads\/2026\/10\/images-1-7-239x300.jpg 239w\" sizes=\"auto, (max-width: 399px) 100vw, 399px\" \/><\/p>\n<\/li>\n<\/ul>\n<\/li>\n<\/ol>\n","protected":false},"excerpt":{"rendered":"<p>les temp\u00e9ratures en France m\u00e9tropolitaine ne sont pas directement caus\u00e9es par El Ni\u00f1o. Bien qu\u2019El&#8230;<\/p>\n","protected":false},"author":1,"featured_media":3884,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_jetpack_newsletter_access":"","_jetpack_dont_email_post_to_subs":false,"_jetpack_newsletter_tier_id":0,"_jetpack_memberships_contains_paywalled_content":false,"_jetpack_feature_clip_id":0,"_jetpack_memberships_contains_paid_content":false,"footnotes":"","jetpack_publicize_message":"","jetpack_publicize_feature_enabled":true,"jetpack_social_post_already_shared":true,"jetpack_social_options":{"image_generator_settings":{"template":"highway","default_image_id":0,"font":"","enabled":false},"version":2},"jetpack_post_was_ever_published":false},"categories":[741,7983,483,13613,13614],"tags":[13652,13659,13633,13657,13621,13658,760,13628,13662,3583,13632,6923,13619,13636,13649,13630,13654,13661,13615,3579,13617,6933,366,13653,13627,13631,13646,13616,13635,13642,13643,13655,13622,242,13651,13641,13640,13618,13650,13656,13639,2015,13620,2942,11676,13645,13623,13624,13629,13638,13660,13644,5121,13626,13625,13648,13637,13647,13634],"class_list":["post-3883","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-741","category-automne","category-documentaire","category-el-nino","category-la-nina","tag-activite-humaine","tag-agriculture","tag-alizes","tag-amerique-du-sud","tag-anomalie-thermique","tag-asie-du-sud-est","tag-australie","tag-baisse-des-temperatures","tag-biodiversite","tag-changement-climatique","tag-circulation-atmospherique","tag-climat","tag-climatologie","tag-courants-marins","tag-cyclones","tag-echelle-mondiale","tag-ecologie","tag-ecosysteme-marin","tag-el-nino","tag-empreinte-carbone","tag-enso","tag-environnement","tag-france","tag-gaz-a-effet-de-serre","tag-hausse-des-temperatures","tag-impact-mondial","tag-inondations","tag-la-nina","tag-masses-dair","tag-meteo","tag-meteorologie","tag-metropole","tag-modification-thermique","tag-monde","tag-moussons","tag-ocean-atlantique","tag-ocean-pacifique","tag-oscillation-australe","tag-ouragans","tag-outre-mer","tag-pacifique-equatorial","tag-peche","tag-phenomene-climatique","tag-planete","tag-pluies-diluviennes","tag-precipitations","tag-rechauffement-climatique","tag-rechauffement-global","tag-record-de-temperature","tag-remontee-deau-froide","tag-ressources-halieutiques","tag-secheresse","tag-temperature","tag-temperature-moyenne","tag-temperatures","tag-tempetes","tag-upwelling","tag-vagues-de-chaleur","tag-vents"],"jetpack_publicize_connections":[],"jetpack_sharing_enabled":true,"jetpack_featured_media_url":"https:\/\/www.laurensoff.com\/wordpress\/wp-content\/uploads\/2026\/10\/images-4-3.jpg","_links":{"self":[{"href":"https:\/\/www.laurensoff.com\/wordpress\/wp-json\/wp\/v2\/posts\/3883","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.laurensoff.com\/wordpress\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.laurensoff.com\/wordpress\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.laurensoff.com\/wordpress\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.laurensoff.com\/wordpress\/wp-json\/wp\/v2\/comments?post=3883"}],"version-history":[{"count":1,"href":"https:\/\/www.laurensoff.com\/wordpress\/wp-json\/wp\/v2\/posts\/3883\/revisions"}],"predecessor-version":[{"id":3888,"href":"https:\/\/www.laurensoff.com\/wordpress\/wp-json\/wp\/v2\/posts\/3883\/revisions\/3888"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.laurensoff.com\/wordpress\/wp-json\/wp\/v2\/media\/3884"}],"wp:attachment":[{"href":"https:\/\/www.laurensoff.com\/wordpress\/wp-json\/wp\/v2\/media?parent=3883"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.laurensoff.com\/wordpress\/wp-json\/wp\/v2\/categories?post=3883"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.laurensoff.com\/wordpress\/wp-json\/wp\/v2\/tags?post=3883"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}