{"id":214156,"date":"2025-04-11T14:29:43","date_gmt":"2025-04-11T08:59:43","guid":{"rendered":"https:\/\/www.oliveboard.in\/blog\/?p=214156"},"modified":"2025-04-11T14:29:44","modified_gmt":"2025-04-11T08:59:44","slug":"atmospheric-circulation-notes","status":"publish","type":"post","link":"https:\/\/www.oliveboard.in\/blog\/atmospheric-circulation-notes\/","title":{"rendered":"Atmospheric Circulation  &#8211; UGC NET Geography Notes"},"content":{"rendered":"<div id=\"ez-toc-container\" class=\"ez-toc-v2_0_77 counter-hierarchy ez-toc-counter ez-toc-grey ez-toc-container-direction\">\n<div class=\"ez-toc-title-container\">\n<p class=\"ez-toc-title\" style=\"cursor:inherit\">Table of content<\/p>\n<span class=\"ez-toc-title-toggle\"><a href=\"#\" class=\"ez-toc-pull-right ez-toc-btn ez-toc-btn-xs ez-toc-btn-default ez-toc-toggle\" aria-label=\"Toggle Table of Content\"><span class=\"ez-toc-js-icon-con\"><span class=\"\"><span class=\"eztoc-hide\" style=\"display:none;\">Toggle<\/span><span class=\"ez-toc-icon-toggle-span\"><svg style=\"fill: #999;color:#999\" xmlns=\"http:\/\/www.w3.org\/2000\/svg\" class=\"list-377408\" width=\"20px\" height=\"20px\" viewBox=\"0 0 24 24\" fill=\"none\"><path d=\"M6 6H4v2h2V6zm14 0H8v2h12V6zM4 11h2v2H4v-2zm16 0H8v2h12v-2zM4 16h2v2H4v-2zm16 0H8v2h12v-2z\" fill=\"currentColor\"><\/path><\/svg><svg style=\"fill: #999;color:#999\" class=\"arrow-unsorted-368013\" xmlns=\"http:\/\/www.w3.org\/2000\/svg\" width=\"10px\" height=\"10px\" viewBox=\"0 0 24 24\" version=\"1.2\" baseProfile=\"tiny\"><path d=\"M18.2 9.3l-6.2-6.3-6.2 6.3c-.2.2-.3.4-.3.7s.1.5.3.7c.2.2.4.3.7.3h11c.3 0 .5-.1.7-.3.2-.2.3-.5.3-.7s-.1-.5-.3-.7zM5.8 14.7l6.2 6.3 6.2-6.3c.2-.2.3-.5.3-.7s-.1-.5-.3-.7c-.2-.2-.4-.3-.7-.3h-11c-.3 0-.5.1-.7.3-.2.2-.3.5-.3.7s.1.5.3.7z\"\/><\/svg><\/span><\/span><\/span><\/a><\/span><\/div>\n<nav><ul class='ez-toc-list ez-toc-list-level-1 eztoc-toggle-hide-by-default' ><li class='ez-toc-page-1 ez-toc-heading-level-2'><a class=\"ez-toc-link ez-toc-heading-1\" href=\"https:\/\/www.oliveboard.in\/blog\/atmospheric-circulation-notes\/#What_is_Atmospheric_Circulation\" >What is Atmospheric Circulation?<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-2'><a class=\"ez-toc-link ez-toc-heading-2\" href=\"https:\/\/www.oliveboard.in\/blog\/atmospheric-circulation-notes\/#Three_Cell_Model_of_Atmospheric_Circulation\" >Three Cell Model of Atmospheric Circulation<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-2'><a class=\"ez-toc-link ez-toc-heading-3\" href=\"https:\/\/www.oliveboard.in\/blog\/atmospheric-circulation-notes\/#Major_Wind_Systems_in_Atmospheric_Circulation\" >Major Wind Systems in Atmospheric Circulation<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-2'><a class=\"ez-toc-link ez-toc-heading-4\" href=\"https:\/\/www.oliveboard.in\/blog\/atmospheric-circulation-notes\/#Pressure_Belts_and_Their_Role_in_Atmospheric_Circulation\" >Pressure Belts and Their Role in Atmospheric Circulation<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-2'><a class=\"ez-toc-link ez-toc-heading-5\" href=\"https:\/\/www.oliveboard.in\/blog\/atmospheric-circulation-notes\/#Jet_Streams_and_Their_Impact_on_Climate\" >Jet Streams and Their Impact on Climate<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-2'><a class=\"ez-toc-link ez-toc-heading-6\" href=\"https:\/\/www.oliveboard.in\/blog\/atmospheric-circulation-notes\/#Monsoons_and_Atmospheric_Circulation\" >Monsoons and Atmospheric Circulation<\/a><\/li><\/ul><\/nav><\/div>\n\n<p><strong>Atmospheric Circulation:<\/strong> Atmospheric circulation is the large-scale movement of air that regulates the Earth&#8217;s climate by redistributing heat from the equator to the poles. Driven by solar radiation, pressure belts, and the Coriolis effect, it consists of three primary cells, namely, <strong>Hadley, Ferrel, and Polar cells<\/strong> which influence global wind patterns like trade winds, westerlies, and polar easterlies. This topic is crucial in <strong><a href=\"https:\/\/www.oliveboard.in\/blog\/ugc-net-geography-syllabus\/\" target=\"_blank\" rel=\"noreferrer noopener\">UGC NET Geography<\/a><\/strong>, as it explains monsoons, jet streams, cyclones, and climate variability, making it essential for aspirants aiming to excel in climatology and physical geography.<\/p>\n\n\n\n<div class=\"wp-block-buttons is-layout-flex wp-block-buttons-is-layout-flex\">\n<div class=\"wp-block-button aligncenter\"><a class=\"wp-block-button__link\" href=\"https:\/\/www.oliveboard.in\/ugc-net-mock-test\/?ref=contstuti-ugc-net\" target=\"_blank\" rel=\"noreferrer noopener\">UGC NET Mock Test 2025<\/a><\/div>\n<\/div>\n\n\n\n<h2 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"What_is_Atmospheric_Circulation\"><\/span>What is Atmospheric Circulation?<span class=\"ez-toc-section-end\"><\/span><\/h2>\n\n\n\n<p>Atmospheric circulation is the large-scale movement of air that distributes heat and moisture across the Earth, maintaining global climate balance. <strong>Here are its features:<\/strong><\/p>\n\n\n\n<ul class=\"wp-block-list\"><li>In physical geography, atmospheric circulation is crucial for understanding climate zones, weather patterns, and monsoons. <\/li><li>It influences temperature distribution, precipitation, and ocean currents, shaping ecosystems and human activities worldwide.<\/li><\/ul>\n\n\n\n<h2 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Three_Cell_Model_of_Atmospheric_Circulation\"><\/span>Three Cell Model of Atmospheric Circulation<span class=\"ez-toc-section-end\"><\/span><\/h2>\n\n\n\n<p>The Three-Cell Model explains global wind circulation, driven by solar heating, Coriolis force, and pressure gradients. It consists of three key cells influencing weather patterns, climate zones, and monsoons, which is a crucial topic for UGC NET Geography.<\/p>\n\n\n\n<h3 class=\"wp-block-heading\">1. Hadley Cell \u2013 Trade Winds and Equatorial Convection<\/h3>\n\n\n\n<p>Operating between<strong> 0\u00b0\u201330\u00b0 latitude<\/strong>, the Hadley Cell drives equatorial convection as warm air rises at the ITCZ, moves poleward, cools, and sinks at 30\u00b0 latitude, creating subtropical high-pressure zones. This forms trade winds, influencing monsoons and tropical climates.<\/p>\n\n\n\n<h3 class=\"wp-block-heading\">2. Ferrel Cell \u2013 Westerlies and Mid-Latitude Weather<\/h3>\n\n\n\n<p>Located between <strong>30\u00b0\u201360\u00b0 latitude<\/strong>, the Ferrel Cell transports air poleward, generating westerlies that drive temperate zone cyclones and storm systems, impacting North America and Europe.<\/p>\n\n\n\n<h3 class=\"wp-block-heading\">3. Polar Cell \u2013 Polar Easterlies and Cold Air Movement<\/h3>\n\n\n\n<p>Extending from 60\u00b0 to the poles, the Polar Cell pushes cold, dense air equatorward, forming polar easterlies. Its interaction with westerlies creates polar fronts, storms, and Arctic climate variability.<\/p>\n\n\n\n<h2 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Major_Wind_Systems_in_Atmospheric_Circulation\"><\/span>Major Wind Systems in Atmospheric Circulation<span class=\"ez-toc-section-end\"><\/span><\/h2>\n\n\n\n<p>Global wind systems play a crucial role in climate regulation, weather patterns, and ocean currents. The three primary wind belts: Trade Winds, Westerlies, and Polar Easterlies, are driven by Earth\u2019s rotation, pressure gradients, and solar heating. <\/p>\n\n\n\n<h3 class=\"wp-block-heading\">1. Trade Winds \u2013 Impact on Monsoons and Tropical Weather<\/h3>\n\n\n\n<p>The Trade Winds blow from subtropical high-pressure zones (30\u00b0 latitude) toward the equator (ITCZ), moving from northeast in the Northern Hemisphere and southeast in the Southern Hemisphere due to the Coriolis effect. These winds:<\/p>\n\n\n\n<ul class=\"wp-block-list\"><li>Drive tropical cyclones, hurricanes, and typhoons.<\/li><li>Influence monsoon patterns, especially in South Asia.<\/li><li>Power ocean currents like the North and South Equatorial Currents, affecting marine ecosystems.<\/li><\/ul>\n\n\n\n<h3 class=\"wp-block-heading\">2. Westerlies \u2013 Influence on Mid-Latitude Cyclones<\/h3>\n\n\n\n<p>The Westerlies blow from 30\u00b0\u201360\u00b0 latitude, moving west to east. Stronger in winter, they are responsible for:<\/p>\n\n\n\n<ul class=\"wp-block-list\"><li>Mid-latitude cyclones that impact North America, Europe, and Asia.<\/li><li>Steering jet streams, affecting weather variability.<\/li><li>Driving ocean currents like the Gulf Stream, influencing climate in Europe.<\/li><\/ul>\n\n\n\n<h3 class=\"wp-block-heading\">3. Polar Easterlies \u2013 Role in Extreme Weather Near the Poles<\/h3>\n\n\n\n<p>The Polar Easterlies originate from high-pressure polar regions (90\u00b0 latitude) and move toward lower latitudes (60\u00b0). They:<\/p>\n\n\n\n<ul class=\"wp-block-list\"><li>Cause cold waves and Arctic storms.<\/li><li>Form the polar vortex, leading to extreme winter conditions.<\/li><li>Interact with westerlies, creating polar fronts and storm activity.<\/li><\/ul>\n\n\n\n<p><strong>Also Check: <a href=\"https:\/\/www.oliveboard.in\/blog\/geomorphic-cycle\/\" target=\"_blank\" rel=\"noreferrer noopener\">Geomorphic Cycle &#8211; UGC NET Geography Notes<\/a><\/strong><\/p>\n\n\n\n<h2 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Pressure_Belts_and_Their_Role_in_Atmospheric_Circulation\"><\/span>Pressure Belts and Their Role in Atmospheric Circulation<span class=\"ez-toc-section-end\"><\/span><\/h2>\n\n\n\n<p>Pressure belts are global zones of high and low pressure that drive wind circulation, monsoons, and climate patterns. Formed due to Earth\u2019s rotation and uneven heating, they influence global wind systems.<\/p>\n\n\n\n<h3 class=\"wp-block-heading\">1. Equatorial Low (0\u00b0 Latitude) \u2013 Intense Convection and Rainfall<\/h3>\n\n\n\n<ul class=\"wp-block-list\"><li>Located at the Intertropical Convergence Zone (ITCZ).<\/li><li>Warm air rises, creating low pressure and heavy rainfall (e.g., Amazon Rainforest).<\/li><li>Drives trade winds and monsoon formation.<\/li><\/ul>\n\n\n\n<h3 class=\"wp-block-heading\">2. Subtropical High (30\u00b0 Latitude) \u2013 Dry and Stable Conditions<\/h3>\n\n\n\n<ul class=\"wp-block-list\"><li>Sinking air creates high pressure, leading to dry climates and deserts (e.g., Sahara).<\/li><li>Generates trade winds (toward the equator) and westerlies (toward mid-latitudes).<\/li><\/ul>\n\n\n\n<h3 class=\"wp-block-heading\">3. Subpolar Low (60\u00b0 Latitude) \u2013 Storm Formation<\/h3>\n\n\n\n<ul class=\"wp-block-list\"><li>Rising air from westerlies and polar easterlies creates low pressure.<\/li><li>Drives storm systems and mid-latitude cyclones (e.g., North Atlantic storms).<\/li><\/ul>\n\n\n\n<h3 class=\"wp-block-heading\">4. Polar High (90\u00b0 Latitude) \u2013 Extreme Cold and Dense Air<\/h3>\n\n\n\n<ul class=\"wp-block-list\"><li>Sinking cold air forms high-pressure zones at the poles.<\/li><li>Generates polar easterlies, leading to Arctic and Antarctic weather extremes.<\/li><\/ul>\n\n\n\n<h3 class=\"wp-block-heading\">Pressure Belts and Global Wind Patterns<\/h3>\n\n\n\n<ul class=\"wp-block-list\"><li>Low-pressure belts (Equatorial, Subpolar) \u2192 Warm air rises, creating clouds and precipitation.<\/li><li>High-pressure belts (Subtropical, Polar) \u2192 Air sinks, leading to dry and stable weather.<\/li><\/ul>\n\n\n\n<p>These belts drive Trade Winds, Westerlies, and Polar Easterlies, shaping global weather and climate.<\/p>\n\n\n\n<h2 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Jet_Streams_and_Their_Impact_on_Climate\"><\/span>Jet Streams and Their Impact on Climate<span class=\"ez-toc-section-end\"><\/span><\/h2>\n\n\n\n<p>Jet streams are fast-moving, narrow air currents in the upper troposphere, driven by temperature gradients and Earth&#8217;s rotation. <\/p>\n\n\n\n<h3 class=\"wp-block-heading\">Types of Jet Streams<\/h3>\n\n\n\n<ul class=\"wp-block-list\"><li><strong>Polar Jet Stream (30\u00b0\u201360\u00b0 latitude): <\/strong>Strongest in winter, it steers mid-latitude cyclones, cold waves, and storm tracks.<\/li><li><strong>Subtropical Jet Stream (20\u00b0\u201330\u00b0 latitude):<\/strong> Influences monsoons, El Ni\u00f1o events, and upper-level weather patterns.<\/li><\/ul>\n\n\n\n<h3 class=\"wp-block-heading\">Influence on Weather Systems, Monsoons, and Cyclones<\/h3>\n\n\n\n<ul class=\"wp-block-list\"><li>Guides cyclones and storms, impacting rainfall and extreme weather.<\/li><li>Controls monsoon onset and withdrawal, crucial for South Asian rainfall.<\/li><li>Disruptions (El Ni\u00f1o, La Ni\u00f1a) affect global temperature and precipitation patterns.<\/li><\/ul>\n\n\n\n<p><strong>Also Check: <a href=\"https:\/\/www.oliveboard.in\/blog\/concept-of-continental-drift-theory\/\">Concept of Continental Drift Theory<\/a><\/strong><\/p>\n\n\n\n<h2 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Monsoons_and_Atmospheric_Circulation\"><\/span>Monsoons and Atmospheric Circulation<span class=\"ez-toc-section-end\"><\/span><\/h2>\n\n\n\n<p>Monsoons are seasonal wind shifts caused by differential heating of land and ocean, driven by atmospheric circulation and pressure belts. They are essential for agriculture, water availability, and climate stability, particularly in South Asia.<\/p>\n\n\n\n<h3 class=\"wp-block-heading\">How Atmospheric Circulation Affects Monsoons in South Asia?<\/h3>\n\n\n\n<p>Monsoons are always affected by atmospheric circulations. <strong>Here are the features of atmospheric circulations on monsoon:<\/strong><\/p>\n\n\n\n<ul class=\"wp-block-list\"><li><strong>Summer Monsoon (June\u2013September):<\/strong> Land heats faster than the ocean, creating low pressure over India, pulling in moist southwest winds, causing heavy rainfall.<\/li><li><strong>Winter Monsoon (October\u2013March):<\/strong> Cooling landforms high pressure, pushing dry northeast winds, leading to dry conditions.<\/li><\/ul>\n\n\n\n<h3 class=\"wp-block-heading\">Seasonal Wind Shifts and Rainfall Impact<\/h3>\n\n\n\n<ul class=\"wp-block-list\"><li>Jet streams influence monsoon strength and variability.<\/li><li>El Ni\u00f1o weakens monsoons, while La Ni\u00f1a strengthens them.<\/li><li>Anomalies in monsoonal circulation impact Indian agriculture, floods, and droughts.<\/li><\/ul>\n","protected":false},"excerpt":{"rendered":"<p>Atmospheric Circulation: Atmospheric circulation is the large-scale movement of air that regulates the Earth&#8217;s climate by redistributing heat from the<\/p>\n","protected":false},"author":50,"featured_media":214157,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1,11846,17417],"tags":[17505,17456],"class_list":["post-214156","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-articles","category-ugc-net-teaching-exams","category-ugc-net-geography-study-material","tag-atmospheric-circulation","tag-ugc-net-geography-notes","generate-columns","tablet-grid-50","mobile-grid-100","grid-parent","grid-50"],"yoast_head":"<!-- This site is optimized with the Yoast SEO Premium plugin v26.6 (Yoast SEO v26.6) - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Atmospheric Circulation - UGC NET Geography Notes<\/title>\n<meta name=\"description\" content=\"Understand Atmospheric Circulation with UGC NET Geography notes. 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