{"id":2938,"date":"2025-12-01T07:38:48","date_gmt":"2025-12-01T12:38:48","guid":{"rendered":"https:\/\/glennspecht.com\/wp\/?p=2938"},"modified":"2025-12-05T10:05:22","modified_gmt":"2025-12-05T15:05:22","slug":"explainer-ecuador-weather","status":"publish","type":"post","link":"https:\/\/glennspecht.com\/wp\/explainer-ecuador-weather\/","title":{"rendered":"Explainer- Ecuador Weather"},"content":{"rendered":"\n<p>Here we go \u2014 weather-nerd hat on. \u2601\ufe0f\ud83c\udf27\ufe0f<\/p>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<h2 class=\"wp-block-heading\">1. Why Ecuador\u2019s weather feels \u201cweird\u201d compared to North America<\/h2>\n\n\n\n<p>Ecuador sits right on the equator, squeezed between the <strong>Pacific Ocean<\/strong> and the <strong>Andes<\/strong>, with the <strong>Amazon basin<\/strong> to the east. That combination produces:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Strong influence from <strong>ocean currents<\/strong> (Humboldt cold current and warm equatorial currents).<\/li>\n\n\n\n<li>A steep <strong>mountain wall<\/strong> that rises from sea level to >5,000 m in a short distance.<\/li>\n\n\n\n<li>Moist air masses coming from the <strong>Amazon \/ Brazilian monsoon region<\/strong> to the east.<\/li>\n<\/ul>\n\n\n\n<p>Result: <strong>very short distances, very different weather<\/strong> \u2014 classic microclimates.<\/p>\n\n\n\n<p>In North America, large areas share similar patterns (e.g., the U.S. Midwest, the Great Plains). In Ecuador, a 30\u201350 km drive can take you from coastal heat to chilly drizzle to full-on Amazon downpour.<\/p>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<h2 class=\"wp-block-heading\">2. The big pieces: currents, Andes, and the \u201cSouth American monsoon\u201d<\/h2>\n\n\n\n<h3 class=\"wp-block-heading\">2.1 Ocean currents on the Coast<\/h3>\n\n\n\n<p>Along Ecuador\u2019s coast, climate is driven by:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Humboldt (Peru) Current<\/strong> \u2013 a <strong>cold<\/strong> current flowing north from Peru\/Chile that cools the air and <strong>suppresses rainfall<\/strong>, especially in the \u201cgar\u00faa\u201d season (cool, cloudy, drizzly conditions).<\/li>\n\n\n\n<li><strong>Panama \/ Equatorial warm current<\/strong> \u2013 a <strong>warmer<\/strong> current that dominates more in the <strong>Dec\u2013May<\/strong> period, adding heat and moisture, fueling coastal rains and thunderstorms.<\/li>\n<\/ul>\n\n\n\n<p>Add to that <strong>El Ni\u00f1o\u2013Southern Oscillation (ENSO)<\/strong>:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>El Ni\u00f1o<\/strong> years: warmer Pacific sea surface temperatures near Ecuador \u2192 <strong>more convection and heavy rains<\/strong>, especially along the coast and in lowlands.<\/li>\n\n\n\n<li><strong>La Ni\u00f1a<\/strong> years: cooler waters \u2192 often <strong>drier and cooler<\/strong> along the coast, with shifts in rainfall patterns inland.<\/li>\n<\/ul>\n\n\n\n<p>So, for the Coast, the sea is the main \u201cthermostat\u201d.<\/p>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<h3 class=\"wp-block-heading\">2.2 Andes = microclimate machine<\/h3>\n\n\n\n<p>The <strong>Andes<\/strong> cut through Ecuador from north to south in two main ranges with a high inter-Andean plateau in between. That creates:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Rapid changes in altitude \u2192 temperature drops about <strong>0.6\u20130.7\u00b0C per 100 m<\/strong> (rough rule of thumb).<\/li>\n\n\n\n<li>Strong <strong>orographic rainfall<\/strong> (air forced upward \u2192 cooling \u2192 clouds and rain on windward slopes).<\/li>\n\n\n\n<li><strong>Shadow zones<\/strong> on leeward slopes (drier).<\/li>\n<\/ul>\n\n\n\n<p>So you get:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Cloud forests<\/strong> on some Western and Eastern slopes (humid, cool).<\/li>\n\n\n\n<li><strong>Dry inter-Andean valleys<\/strong> just a ridge away (sunny, semi-arid).<\/li>\n\n\n\n<li>Cities like <strong>Quito, Cuenca, Loja<\/strong> with \u201ceternal spring\u201d climates \u2014 mild year-round, big day\u2013night swings, modest seasonal changes.<\/li>\n<\/ul>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<h3 class=\"wp-block-heading\">2.3 The South American Monsoon &amp; Amazon influence<\/h3>\n\n\n\n<p>There isn\u2019t a \u201cmonsoon over Brazil\u201d in the Asian sense, but there <em>is<\/em> what climatologists call the <strong>South American Monsoon System (SAMS)<\/strong>.<\/p>\n\n\n\n<p>Simplifying a bit:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>In the <strong>austral summer (roughly Nov\u2013March)<\/strong>, strong solar heating over central\u2013western Brazil and the Amazon pulls in moist air from the Atlantic.<\/li>\n\n\n\n<li>This moisture moves westward, feeding <strong>deep convection (big thunderstorms)<\/strong>, and pushes up against the Andes.<\/li>\n\n\n\n<li>When that humid air hits the Andes, it\u2019s forced upward \u2192 heavy rains in the <strong>Amazon side of Ecuador<\/strong> and on some Andean slopes.<\/li>\n<\/ul>\n\n\n\n<p>For Ecuador, this means:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>The <strong>Amazon region (Oriente)<\/strong> has a <strong>pronounced rainy season<\/strong> (roughly Dec\u2013May), though it\u2019s humid and rainy most of the year.<\/li>\n\n\n\n<li>Some Andean slopes get <strong>enhanced rainfall<\/strong> when Amazon-side moisture is strong.<\/li>\n\n\n\n<li>Interaction with ENSO can modulate how much of that moisture crosses over and where the heaviest bands set up.<\/li>\n<\/ul>\n\n\n\n<p>So yes, what happens in <strong>Brazil\u2019s convective \u201cmonsoon\u201d region<\/strong> matters for Ecuador\u2019s rain patterns, especially east of the Andes.<\/p>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<h2 class=\"wp-block-heading\">3. Seasons in Ecuador: not really four<\/h2>\n\n\n\n<p>Instead of <strong>winter\/spring\/summer\/fall<\/strong>, Ecuador mostly has:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Rainy season<\/strong> (invierno \/ \u00e9poca lluviosa)<\/li>\n\n\n\n<li><strong>Dry season<\/strong> (verano \/ \u00e9poca seca)<\/li>\n<\/ul>\n\n\n\n<p>\u2026but the details depend heavily on region and altitude.<\/p>\n\n\n\n<h3 class=\"wp-block-heading\">3.1 Coast (Costa)<\/h3>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>General pattern:<\/strong>\n<ul class=\"wp-block-list\">\n<li><strong>Dec\u2013May:<\/strong> <strong>warmer and wetter<\/strong>, thunderstorms and heavy showers; more humidity, more heat.<\/li>\n\n\n\n<li><strong>Jun\u2013Nov:<\/strong> <strong>cooler, cloudier, drier<\/strong>, influenced by the Humboldt Current; lots of low stratus, drizzle (\u201cgar\u00faa\u201d) in some areas.<\/li>\n<\/ul>\n<\/li>\n\n\n\n<li>In <strong>El Ni\u00f1o<\/strong> years: rains can be <strong>much heavier<\/strong>, with floods, landslides, and coastal erosion.<\/li>\n\n\n\n<li>In <strong>La Ni\u00f1a<\/strong> years: often <strong>drier<\/strong>, but not uniformly.<\/li>\n<\/ul>\n\n\n\n<h3 class=\"wp-block-heading\">3.2 Highlands (Sierra)<\/h3>\n\n\n\n<ul class=\"wp-block-list\">\n<li>The Sierra tends to have <strong>two moderate rainy peaks<\/strong>:\n<ul class=\"wp-block-list\">\n<li>One around <strong>March\u2013April<\/strong><\/li>\n\n\n\n<li>Another around <strong>October\u2013November<\/strong><br>with somewhat drier stretches in between.<\/li>\n<\/ul>\n<\/li>\n\n\n\n<li>Cities like <strong>Quito, Cuenca, Loja<\/strong>:\n<ul class=\"wp-block-list\">\n<li>Temperatures are relatively stable year-round (altitude-driven), but:<\/li>\n\n\n\n<li>Daily weather swings a lot (sun \u2192 clouds \u2192 afternoon shower \u2192 clear night).<\/li>\n\n\n\n<li>Nights can be quite cool, even when days are mild.<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n\n\n\n<p>Because of microclimates, <strong>north vs south<\/strong> and <strong>east vs west<\/strong> facing slopes can behave differently even at the same elevation.<\/p>\n\n\n\n<h3 class=\"wp-block-heading\">3.3 Amazon (Oriente)<\/h3>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Very wet overall<\/strong>, with:\n<ul class=\"wp-block-list\">\n<li>A main rainy season (often <strong>Dec\u2013May<\/strong>) with more intense storms.<\/li>\n\n\n\n<li>A slightly \u201cless rainy\u201d season (still humid and cloudy) in other months.<\/li>\n<\/ul>\n<\/li>\n\n\n\n<li>Local topography (valleys, foothills) creates its own micro-variability.<\/li>\n<\/ul>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<h2 class=\"wp-block-heading\">4. Microclimates: the \u201cshort-distance chaos\u201d<\/h2>\n\n\n\n<p>In Ecuador, microclimates come from:<\/p>\n\n\n\n<ol class=\"wp-block-list\">\n<li><strong>Altitude differences<\/strong> over short distances.<\/li>\n\n\n\n<li><strong>Slope orientation<\/strong> (sun-facing vs shade-facing).<\/li>\n\n\n\n<li><strong>Proximity to the ocean vs. Amazon<\/strong>.<\/li>\n\n\n\n<li><strong>Local land cover<\/strong> (forest, pasture, urban heat island).<\/li>\n<\/ol>\n\n\n\n<p>Examples:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>On the road from the Coast up to the Sierra, you may pass:\n<ul class=\"wp-block-list\">\n<li>Hot &amp; humid lowlands<br>\u2192 cloudy, dripping <strong>cloud forest<\/strong><br>\u2192 cool highland plains with sun and wind<br>all in a <strong>1\u20132 hour drive<\/strong>.<\/li>\n<\/ul>\n<\/li>\n\n\n\n<li>On the coast, small differences in exposure to wind and currents (e.g., a bay vs open coast) can produce noticeably different patterns of cloud, fog, and rain.<\/li>\n<\/ul>\n\n\n\n<p>For forecasting, this means a model grid cell might say \u201c30% chance of showers\u201d, but in reality:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>One valley gets a heavy thunderstorm,<\/li>\n\n\n\n<li>The neighbouring ridge stays dry and sunny.<\/li>\n<\/ul>\n\n\n\n<p>From a user point of view, that feels like the forecast was \u201cwrong\u201d, when in fact it was describing probabilities over a <strong>very complex micro-scale terrain<\/strong>.<\/p>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<h2 class=\"wp-block-heading\">5. Why forecasting is harder than in much of North America<\/h2>\n\n\n\n<h3 class=\"wp-block-heading\">5.1 Observation network and data<\/h3>\n\n\n\n<p>North America (especially the U.S. and Canada) has:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Very dense <strong>weather station networks<\/strong>.<\/li>\n\n\n\n<li>Extensive <strong>radar coverage<\/strong>.<\/li>\n\n\n\n<li>Many <strong>upper-air soundings<\/strong>, aircraft data, remote sensors, etc.<\/li>\n\n\n\n<li>Decades of heavy investment in <strong>supercomputers and numerical weather prediction<\/strong>.<\/li>\n<\/ul>\n\n\n\n<p>Ecuador (like many tropical countries) typically has:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Fewer ground stations, often unevenly distributed.<\/li>\n\n\n\n<li>Limited or patchy <strong>radar coverage<\/strong> (and radar is crucial for short-term rain forecasts).<\/li>\n\n\n\n<li>Fewer resources for maintaining and upgrading instruments.<\/li>\n<\/ul>\n\n\n\n<p>Less data \u2192 models start with a fuzzier picture of the atmosphere \u2192 more uncertainty, especially at local scales.<\/p>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<h3 class=\"wp-block-heading\">5.2 Tropical convection is intrinsically tricky<\/h3>\n\n\n\n<p>Forecasting in the <strong>deep tropics<\/strong> is harder because:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Much of the rain comes from <strong>convective storms<\/strong> (thunderstorms), not just large-scale frontal systems.<\/li>\n\n\n\n<li>These convection cells are <strong>small, short-lived, and extremely sensitive<\/strong> to tiny variations in:\n<ul class=\"wp-block-list\">\n<li>Moisture,<\/li>\n\n\n\n<li>Local heating (e.g., a sunny patch of ground),<\/li>\n\n\n\n<li>Topography.<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n\n\n\n<p>Even with powerful models, predicting exactly <strong>where<\/strong> and <strong>when<\/strong> a thunderstorm will pop in a mountainous tropical country is tougher than predicting a synoptic-scale cold front crossing the U.S. or Canada.<\/p>\n\n\n\n<p>So you get forecasts like:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>\u201cScattered showers and thunderstorms in the afternoon\u201d \u2014 which is correct statistically, but not a precise \u201cit will rain on your street at 3:15 pm\u201d.<\/li>\n<\/ul>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<h3 class=\"wp-block-heading\">5.3 Complex terrain vs coarse model grids<\/h3>\n\n\n\n<p>Global and regional models use <strong>grid boxes<\/strong> that may be 10\u201325 km wide (or finer for high-resolution models). In Ecuador, within 10\u201320 km you might have:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>A coastal plain,<\/li>\n\n\n\n<li>A steep canyon,<\/li>\n\n\n\n<li>A 3,000 m ridge.<\/li>\n<\/ul>\n\n\n\n<p>When the model \u201caverages\u201d terrain in a grid cell, it can\u2019t capture every valley or slope orientation. That leads to:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Rain shifted a <strong>few kilometres<\/strong> from where it really falls,<\/li>\n\n\n\n<li>Temperature biases (model thinks elevation is lower\/higher than reality),<\/li>\n\n\n\n<li>Difficulty in forecasting local wind patterns (sea breeze, mountain-valley circulations).<\/li>\n<\/ul>\n\n\n\n<p>In a flat region like the U.S. Midwest, a 10\u201325 km grid \u201crepresents reality\u201d much better than over the Andes.<\/p>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<h3 class=\"wp-block-heading\">5.4 Institutional capacity and communication<\/h3>\n\n\n\n<p>Weather services in North America are:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Heavily funded,<\/li>\n\n\n\n<li>Deeply integrated into aviation, agriculture, logistics, and media,<\/li>\n\n\n\n<li>Very good at <strong>probabilistic communication<\/strong> (\u201c20% chance of showers, confidence high\/low\u201d).<\/li>\n<\/ul>\n\n\n\n<p>In Ecuador and similar countries, meteorological services work with:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Smaller budgets,<\/li>\n\n\n\n<li>Less computing power,<\/li>\n\n\n\n<li>Fewer staff for tailored local products.<\/li>\n<\/ul>\n\n\n\n<p>So even when the <strong>science<\/strong> is solid, the <strong>last mile<\/strong> (how forecasts are turned into user-friendly, location-specific information) is often weaker.<\/p>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<h2 class=\"wp-block-heading\">6. So what can residents realistically expect?<\/h2>\n\n\n\n<p>For Ecuador, a realistic expectation is:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Pretty good sense<\/strong> of:\n<ul class=\"wp-block-list\">\n<li>General seasonal behaviour (rainy vs dry season).<\/li>\n\n\n\n<li>Large-scale events (El Ni\u00f1o \/ La Ni\u00f1a, strong cold fronts over the Pacific, big Amazon convective episodes).<\/li>\n<\/ul>\n<\/li>\n\n\n\n<li><strong>Reasonable 1\u20133 day guidance<\/strong> at regional scale (e.g., \u201ccoast will have more rain\u201d, \u201cSierra afternoon storms likely\u201d, \u201ccold, wet spell coming\u201d).<\/li>\n\n\n\n<li>But <strong>much more uncertainty<\/strong> than North America at:\n<ul class=\"wp-block-list\">\n<li>The neighbourhood level,<\/li>\n\n\n\n<li>Exact timing of showers and thunderstorms,<\/li>\n\n\n\n<li>Fine-scale microclimate differences.<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n\n\n\n<p>Local experience still matters a lot: people who have lived in a valley\/ barrio for years often have a better \u201cgut\u201d model of that spot than the formal forecast.<\/p>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<h2 class=\"wp-block-heading\">7. Short English\u2013Spanish roundup<\/h2>\n\n\n\n<p><strong>EN \u2013 Short recap:<\/strong><br>Ecuador\u2019s weather is shaped by warm and cold Pacific currents, the Andean wall, and moist air from the Amazon and the South American monsoon region over Brazil. Instead of four seasons, most of the country flips between rainy and dry periods, with big differences between Coast, Sierra and Amazon. The complex terrain, strong microclimates, limited observation networks and tropical storm behaviour make day-to-day local forecasts less precise than in much of North America, even though large-scale patterns can still be predicted reasonably well.<\/p>\n\n\n\n<p><strong>ES \u2013 Resumen breve:<\/strong><br>El clima de Ecuador est\u00e1 determinado por las corrientes c\u00e1lidas y fr\u00edas del Pac\u00edfico, la barrera de los Andes y el aire h\u00famedo que llega desde la Amazon\u00eda y la zona monz\u00f3nica de Brasil. En vez de cuatro estaciones marcadas, el pa\u00eds se organiza en \u00e9pocas lluviosas y secas, con grandes diferencias entre Costa, Sierra y Amazon\u00eda. La combinaci\u00f3n de relieve muy complejo, microclimas fuertes, redes de observaci\u00f3n limitadas y lluvias de tipo convectivo hace que los pron\u00f3sticos locales d\u00eda a d\u00eda sean menos precisos que en gran parte de Norteam\u00e9rica, aunque los patrones a gran escala se pueden anticipar de manera razonable.<\/p>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<p><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Here we go \u2014 weather-nerd hat on. \u2601\ufe0f\ud83c\udf27\ufe0f 1. Why Ecuador\u2019s weather feels \u201cweird\u201d compared to North America Ecuador sits [&hellip;]<\/p>\n","protected":false},"author":31,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_monsterinsights_skip_tracking":false,"_monsterinsights_sitenote_active":false,"_monsterinsights_sitenote_note":"","_monsterinsights_sitenote_category":0,"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"default","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"ngg_post_thumbnail":0,"footnotes":""},"categories":[389,398],"tags":[],"class_list":["post-2938","post","type-post","status-publish","format-standard","hentry","category-explainer","category-geography"],"_links":{"self":[{"href":"https:\/\/glennspecht.com\/wp\/wp-json\/wp\/v2\/posts\/2938","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/glennspecht.com\/wp\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/glennspecht.com\/wp\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/glennspecht.com\/wp\/wp-json\/wp\/v2\/users\/31"}],"replies":[{"embeddable":true,"href":"https:\/\/glennspecht.com\/wp\/wp-json\/wp\/v2\/comments?post=2938"}],"version-history":[{"count":1,"href":"https:\/\/glennspecht.com\/wp\/wp-json\/wp\/v2\/posts\/2938\/revisions"}],"predecessor-version":[{"id":2939,"href":"https:\/\/glennspecht.com\/wp\/wp-json\/wp\/v2\/posts\/2938\/revisions\/2939"}],"wp:attachment":[{"href":"https:\/\/glennspecht.com\/wp\/wp-json\/wp\/v2\/media?parent=2938"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/glennspecht.com\/wp\/wp-json\/wp\/v2\/categories?post=2938"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/glennspecht.com\/wp\/wp-json\/wp\/v2\/tags?post=2938"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}