{"id":67499,"date":"2025-10-08T16:44:42","date_gmt":"2025-10-08T11:14:42","guid":{"rendered":"https:\/\/vajiramandravi.com\/current-affairs\/?p=67499"},"modified":"2025-10-08T16:44:42","modified_gmt":"2025-10-08T11:14:42","slug":"primary-winds","status":"publish","type":"post","link":"https:\/\/vajiramandravi.com\/current-affairs\/primary-winds\/","title":{"rendered":"Primary Winds, Types, Formation, Distribution, Circulation Cell"},"content":{"rendered":"<p><span style=\"font-weight: 400;\">Primary winds, or planetary winds, are the large-scale, permanent air movements on Earth that blow in fixed directions throughout the year. They form part of the global atmospheric circulation system and play a crucial role in controlling weather, ocean currents, and the global climate.<\/span><\/p>\n<h2><b>Primary Winds<\/b><\/h2>\n<p><span style=\"font-weight: 400;\">Primary winds are driven by differences in atmospheric pressure and temperature between the equator and the poles. They include Trade Winds, Westerlies, and Polar Easterlies, each occupying distinct latitudinal zones. Their pattern results from Earth&#8217;s rotation (Coriolis effect) and thermal contrast between hemispheres, forming a continuous loop of global circulation.<\/span><\/p>\n<h2><b>Primary Winds Types<\/b><\/h2>\n<p><span style=\"font-weight: 400;\">Primary winds are categorized into three major systems, each with unique characteristics and climatological importance.<\/span><\/p>\n<ol>\n<li><b> Trade Winds<\/b><\/li>\n<\/ol>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Originate in subtropical highs (around 30\u00b0 N\/S) and blow toward the equatorial low.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Their meeting zone forms the<a href=\"https:\/\/vajiramandravi.com\/current-affairs\/intertropical-convergence-zone\/\" target=\"_blank\"><strong> Inter-Tropical Convergence Zone<\/strong><\/a> (ITCZ), characterized by heavy rainfall and thunderstorms.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Historically vital for navigation, they influence <a href=\"https:\/\/vajiramandravi.com\/current-affairs\/equatorial-climate\/\" target=\"_blank\"><strong>equatorial climates<\/strong><\/a> and drive ocean currents like the North and South Equatorial Currents.<\/span><\/li>\n<\/ul>\n<ol start=\"2\">\n<li><b> Westerlies<\/b><\/li>\n<\/ol>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Blow from subtropical highs toward subpolar lows between 30\u00b0-60\u00b0 latitudes.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">They are stronger in the Southern Hemisphere due to the absence of land barriers and dominate oceanic regions like the Roaring Forties and Furious Fifties.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Responsible for mid-latitude cyclones and variable weather in Europe, North America, and Australasia.<\/span><\/li>\n<\/ul>\n<ol start=\"3\">\n<li><b> Polar Easterlies<\/b><\/li>\n<\/ol>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Originate near poles from polar high-pressure zones, moving toward subpolar lows.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">These winds are cold and dry, contributing to the formation of polar deserts and Arctic anticyclones.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">They meet westerlies at polar fronts, leading to storm development and the exchange of heat between tropical and polar regions.<\/span><\/li>\n<\/ul>\n<h2><b>Primary Winds Distribution<\/b><\/h2>\n<p><span style=\"font-weight: 400;\">The Earth\u2019s atmospheric circulation divides into pressure belts and corresponding wind zones. Understanding this spatial distribution helps explain climatic diversity. These wind belts shift slightly north or south with the movement of the Sun during solstices, influencing monsoon and rainfall variations.<\/span><\/p>\n<table style=\"width: 91.2816%;\">\n<tbody>\n<tr>\n<td class=\"tb-color\" style=\"text-align: center; width: 90.3808%;\" colspan=\"4\"><b>Primary Winds Distribution<\/b><\/td>\n<\/tr>\n<tr>\n<td style=\"width: 9.41884%; text-align: center;\"><b>Latitude Zone<\/b><\/td>\n<td style=\"width: 38.3262%; text-align: center;\"><b>Pressure Belt<\/b><\/td>\n<td style=\"width: 21.2396%; text-align: center;\"><b>Primary Wind System<\/b><\/td>\n<td style=\"width: 21.3962%; text-align: center;\"><b>Direction of Flow<\/b><\/td>\n<\/tr>\n<tr>\n<td style=\"width: 9.41884%;\">\n<p><span style=\"font-weight: 400;\">0\u00b0-30\u00b0 N &amp; S<\/span><\/p>\n<\/td>\n<td style=\"width: 38.3262%;\">\n<p><span style=\"font-weight: 400;\">Subtropical High (at ~30\u00b0 latitude) to the Equatorial Low (at ~0\u20135\u00b0 latitude). Air rises at the equator and sinks at 30<\/span><\/p>\n<\/td>\n<td style=\"width: 21.2396%;\">\n<p><span style=\"font-weight: 400;\">Trade Winds<\/span><\/p>\n<\/td>\n<td style=\"width: 21.3962%;\">\n<p><span style=\"font-weight: 400;\">NE to SW (N Hemisphere); SE to NW (S Hemisphere)<\/span><\/p>\n<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 9.41884%;\">\n<p><span style=\"font-weight: 400;\">30\u00b0-60\u00b0 N &amp; S<\/span><\/p>\n<\/td>\n<td style=\"width: 38.3262%;\">\n<p><span style=\"font-weight: 400;\">Subtropical High to Subpolar Low<\/span><\/p>\n<\/td>\n<td style=\"width: 21.2396%;\">\n<p><span style=\"font-weight: 400;\">Westerlies<\/span><\/p>\n<\/td>\n<td style=\"width: 21.3962%;\">\n<p><span style=\"font-weight: 400;\">From West to East<\/span><\/p>\n<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 9.41884%;\">\n<p><span style=\"font-weight: 400;\">60\u00b0-90\u00b0 N &amp; S<\/span><\/p>\n<\/td>\n<td style=\"width: 38.3262%;\">\n<p><span style=\"font-weight: 400;\">Polar High to Subpolar Low<\/span><\/p>\n<\/td>\n<td style=\"width: 21.2396%;\">\n<p><span style=\"font-weight: 400;\">Polar Easterlies<\/span><\/p>\n<\/td>\n<td style=\"width: 21.3962%;\">\n<p><span style=\"font-weight: 400;\">From East to West<\/span><\/p>\n<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<h2><b>Formation Mechanism of Primary Winds<\/b><\/h2>\n<p><span style=\"font-weight: 400;\">The mechanism of primary wind formation is linked to solar heating, Earth\u2019s rotation, and pressure differences.<\/span><\/p>\n<ol>\n<li><b> Unequal Solar Heating<\/b><\/li>\n<\/ol>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The equator receives maximum insolation, creating low pressure, while higher latitudes have high pressure due to cold, dense air.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">This temperature contrast generates convection cells driving surface winds.<\/span><\/li>\n<\/ul>\n<ol start=\"2\">\n<li><b> Coriolis Effect<\/b><\/li>\n<\/ol>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Caused by Earth\u2019s rotation, it deflects winds: right in the Northern Hemisphere and left in the Southern Hemisphere.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">This deflection transforms straight airflows into curved patterns forming trade winds, westerlies, and easterlies.<\/span><\/li>\n<\/ul>\n<ol start=\"3\">\n<li><b> Pressure Belts and Circulation Cells<\/b><\/li>\n<\/ol>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The Hadley Cell, Ferrel Cell, and Polar Cell together constitute the three-cell circulation model, governing the movement of primary winds.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">These cells transport heat energy from equator to poles, balancing global temperature gradients.<\/span><\/li>\n<\/ul>\n<h2><b>Circulation Cells of Primary Winds<\/b><\/h2>\n<p><span style=\"font-weight: 400;\">The primary wind systems arise from three interconnected circulation cells in each hemisphere- the Hadley Cell, Ferrel Cell, and Polar Cell, which together explain the global movement of air.<\/span><\/p>\n<ol>\n<li><b> Hadley Cell<\/b><\/li>\n<\/ol>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Extends between 0\u00b0 and 30\u00b0 latitudes.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Warm air rises at the equator due to intense heating and moves poleward aloft.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">It descends at subtropical highs (around 30\u00b0), creating high pressure and leading to the formation of Trade Winds at the surface.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Responsible for tropical climates and desert belts like the Sahara and Kalahari.<\/span><\/li>\n<\/ul>\n<ol start=\"2\">\n<li><b> Ferrel Cell<\/b><\/li>\n<\/ol>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Found between 30\u00b0 and 60\u00b0 latitudes.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Air from subtropical highs moves poleward, meeting cold polar air at the subpolar low.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">This creates the Westerlies, which dominate the temperate regions.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The cell acts as a transition zone between tropical and polar circulations.<\/span><\/li>\n<\/ul>\n<ol start=\"3\">\n<li><b> Polar Cell<\/b><\/li>\n<\/ol>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Operates from 60\u00b0 to the poles (90\u00b0).<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Cold, dense air sinks at the poles (high pressure) and flows equatorward at the surface.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Where it meets warm air at 60\u00b0, the uplift forms the Polar Front, giving rise to cyclones and frontal systems.<\/span><\/li>\n<\/ul>\n<h2><b>Mechanism of Flow of Primary Winds<\/b><\/h2>\n<p><span style=\"font-weight: 400;\">The mechanism of flow of primary winds involves the interaction of <a href=\"https:\/\/vajiramandravi.com\/upsc-exam\/solar-energy\/\" target=\"_blank\"><strong>solar energy<\/strong><\/a>, Earth\u2019s rotation, and pressure gradients that drive air circulation around the globe.<\/span><\/p>\n<ol>\n<li><b> Unequal Heating of Earth<\/b><\/li>\n<\/ol>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The equator receives maximum <a href=\"https:\/\/vajiramandravi.com\/current-affairs\/solar-radiation\/\" target=\"_blank\"><strong>solar radiation<\/strong><\/a>, creating low pressure, while the poles remain cold and high-pressure zones.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">This temperature gradient initiates pressure-driven circulation from high to low pressure.<\/span><\/li>\n<\/ul>\n<ol start=\"2\">\n<li><b> Pressure Gradient Force (PGF)<\/b><\/li>\n<\/ol>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Air moves horizontally from high-pressure to low-pressure regions.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">The greater the pressure difference, the stronger the wind velocity.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">PGF is the initial driver of all wind systems.<\/span><\/li>\n<\/ul>\n<ol start=\"3\">\n<li><b> Coriolis Effect<\/b><\/li>\n<\/ol>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Due to Earth\u2019s rotation, moving air is deflected:<\/span>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"2\"><span style=\"font-weight: 400;\">Rightward in the Northern Hemisphere<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"2\"><span style=\"font-weight: 400;\">Leftward in the Southern Hemisphere<\/span><\/li>\n<\/ul>\n<\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">This deflection shapes the directions of trade winds, westerlies, and polar easterlies.<\/span><\/li>\n<\/ul>\n<ol start=\"4\">\n<li><b> Frictional Force<\/b><\/li>\n<\/ol>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Friction with Earth\u2019s surface slows wind velocity, especially near the ground, and reduces Coriolis deflection.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Strongest over rugged terrains and weakest over oceans.<\/span><\/li>\n<\/ul>\n<ol start=\"5\">\n<li><b> Centrifugal and Gradient Forces<\/b><\/li>\n<\/ol>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">In curved motion (around pressure centers), winds balance between PGF, Coriolis, and centrifugal forces, maintaining the flow pattern of cyclones and anticyclones.<\/span><\/li>\n<\/ul>\n<h2><b>Primary Winds influence on Ocean Currents<\/b><\/h2>\n<p><span style=\"font-weight: 400;\">Primary winds are the driving force behind global ocean circulation patterns that regulate marine climates. Key Effects:<\/span><\/p>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><b>Trade Winds:<\/b><span style=\"font-weight: 400;\"> The westward movement of water from the trade winds causes it to pile up in the western sections of ocean basins. This creates a small sea-level gradient, which helps power eastward-flowing counter-currents.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><b>Westerlies:<\/b><span style=\"font-weight: 400;\"> It<\/span> <span style=\"font-weight: 400;\">drives mid-latitude gyres, influencing warm and cold currents such as the Gulf Stream and Kuroshio Current.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><b>Polar Easterlies: <\/b><span style=\"font-weight: 400;\">It<\/span> <span style=\"font-weight: 400;\">helps form cold currents like the East Greenland Current and Antarctic Drift, maintaining global heat balance.<\/span><\/li>\n<\/ul>\n<h2><b>Primary Winds Impact on Climate<\/b><\/h2>\n<p><span style=\"font-weight: 400;\">The climatic zones of Earth correspond closely with primary wind belts, influencing rainfall, vegetation, and temperature.<\/span><\/p>\n<ol>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><b>Equatorial Zone:<\/b><span style=\"font-weight: 400;\"> Trade winds converge causing convectional rainfall and forming dense equatorial rainforests.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><b>Subtropical Zones:<\/b><span style=\"font-weight: 400;\"> Descending dry air from Hadley Cells leads to desert formation (e.g., Sahara, Atacama).<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><b>Temperate Regions:<\/b><span style=\"font-weight: 400;\"> Westerlies bring cyclonic activity and frequent precipitation.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><b>Polar Regions: <\/b><span style=\"font-weight: 400;\">Polar easterlies maintain extreme cold and minimal moisture.<\/span><\/li>\n<\/ol>\n<h2><b>Impact of Climate Change on Primary Winds<\/b><\/h2>\n<p><span style=\"font-weight: 400;\">Modern climate studies highlight significant changes in wind circulation due to global warming. Key Developments:<\/span><\/p>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">AR6 Synthesis Report (2023) noted shifting Hadley Cell boundaries poleward by ~1\u00b0 per decade.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">NASA\u2019s Earth Observatory observed weakening trade winds in the Pacific linked to El Ni\u00f1o intensification.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">WMO in several reports highlighted increased jet stream variability caused by altered westerly patterns, impacting weather extremes in mid-latitudes.<\/span><\/li>\n<\/ul>\n<h2><b>Primary Winds and Jet Streams<\/b><\/h2>\n<p><span style=\"font-weight: 400;\"><a href=\"https:\/\/vajiramandravi.com\/current-affairs\/jet-streams\/\" target=\"_blank\"><strong>Jet streams<\/strong><\/a> are narrow, fast-moving air currents located near the upper troposphere that align with planetary wind systems. Connection of Jet Streams with Primary Winds:<\/span><\/p>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Subtropical Jet Streams form at the boundary between trade winds and westerlies (~30\u00b0 N\/S).<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Polar Jet Streams develop between westerlies and polar easterlies (~60\u00b0 N\/S).<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Variations in jet stream strength affect aviation, weather prediction, and monsoon patterns over South Asia (as reported by IMD, 2023).<\/span><\/li>\n<\/ul>\n<h2><b>Primary Winds Significance<\/b><\/h2>\n<p><span style=\"font-weight: 400;\">The global economy and <a href=\"https:\/\/vajiramandravi.com\/upsc-exam\/ecosystem\/\" target=\"_blank\"><strong>ecosystems<\/strong><\/a> depend heavily on the behavior of primary winds.<\/span><\/p>\n<ol>\n<li><b> Renewable Energy<\/b><\/li>\n<\/ol>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Wind energy potential in regions like North Sea and Australian coasts depends on strong westerlies.<\/span><\/li>\n<\/ul>\n<ol start=\"2\">\n<li><b> Agriculture and Rainfall<\/b><\/li>\n<\/ol>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Shifts in trade winds alter monsoon onset and rainfall patterns affecting crop yields.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">FAO (2022) linked trade wind anomalies with drought conditions in Sub-Saharan Africa.<\/span><\/li>\n<\/ul>\n<ol start=\"3\">\n<li><b> Navigation and Transport<\/b><\/li>\n<\/ol>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Knowledge of prevailing westerlies and trade winds optimizes air and sea navigation routes, saving time and fuel.<\/span><\/li>\n<\/ul>\n<h2><b>Primary Winds in India<\/b><\/h2>\n<p><span style=\"font-weight: 400;\">India\u2019s climate, particularly the monsoon system, is closely related to primary wind circulation. India\u2019s primary winds are mostly the trade winds that reverse direction seasonally to form the monsoon winds. These winds bring over 70% of India\u2019s annual rainfall.<\/span><\/p>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><b>Southwest Monsoon (May-September):<\/b><span style=\"font-weight: 400;\"> The trade winds cross the equator and blow as moist southwesterlies, causing heavy rainfall across India. It brings monsoon to the Coromandel Coast.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><b>Northeast Monsoon (October-December):<\/b><span style=\"font-weight: 400;\"> Winds reverse to dry northeasterlies due to Coriolis effect, giving heavy rain to areas like Tamil Nadu and Andhra Pradesh.<\/span><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><b>Wind Shifts and Cyclones:<\/b><span style=\"font-weight: 400;\"> IMD\u2019s 2024 data show changing wind flow patterns linked to cyclones and early monsoon onset, affecting rainfall spread across the country.<\/span><\/li>\n<\/ul>\n<h2><b>Primary Winds UPSC<\/b><\/h2>\n<p><span style=\"font-weight: 400;\">Recent climatological reports underscore how changes in primary wind systems are central to current affairs. The WMO Global Annual to Decadal Climate Update 2025-2029 indicates persistent global warming and altered circulation patterns, which can shift trade winds and mid-latitude wind belts. In India, the IMD\u2019s 2024 monsoon report documented anomalies in low-pressure systems and wind flow over the Bay of Bengal, influencing monsoon onset and rainfall distribution. The resurgence of La Ni\u00f1a conditions projected for late 2025 is expected to strengthen trade winds across the Pacific, thereby affecting global wind dynamics and monsoon variability.<\/span><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Learn about Primary Winds, their types, formation &#038; circulation. Discover how Trade Winds, Westerlies &#038; Polar Easterlies affect weather &#038; climate globally.<\/p>\n","protected":false},"author":11,"featured_media":66932,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[786],"tags":[3138],"class_list":{"0":"post-67499","1":"post","2":"type-post","3":"status-publish","4":"format-standard","5":"has-post-thumbnail","7":"category-general-studies","8":"tag-primary-winds","9":"no-featured-image-padding"},"acf":[],"_links":{"self":[{"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/posts\/67499","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/users\/11"}],"replies":[{"embeddable":true,"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/comments?post=67499"}],"version-history":[{"count":0,"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/posts\/67499\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/media\/66932"}],"wp:attachment":[{"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/media?parent=67499"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/categories?post=67499"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/vajiramandravi.com\/current-affairs\/wp-json\/wp\/v2\/tags?post=67499"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}