{"id":9938,"date":"2023-09-20T07:40:18","date_gmt":"2023-09-20T07:40:18","guid":{"rendered":"https:\/\/edukemy.com\/blog\/?p=9938"},"modified":"2024-01-24T06:26:00","modified_gmt":"2024-01-24T06:26:00","slug":"temperature-and-pressure-belts-of-the-world-geography-optional-notes","status":"publish","type":"post","link":"https:\/\/edukemy.com\/blog\/temperature-and-pressure-belts-of-the-world-geography-optional-notes\/","title":{"rendered":"Temperature and Pressure Belts of the World &#8211; UPSC Geography Optional Notes"},"content":{"rendered":"\n<figure class=\"wp-block-image size-full\"><a href=\"https:\/\/edukemy.com\/upsc\/upsc-geography?utm_source=Blog&amp;utm_medium=Banner&amp;utm_campaign=Geography\" target=\"_blank\" rel=\"noreferrer noopener\"><img fetchpriority=\"high\" decoding=\"async\" width=\"1280\" height=\"300\" src=\"https:\/\/edukemy.com\/blog\/wp-content\/uploads\/2024\/06\/14.png\" alt=\"\" class=\"wp-image-42410\" srcset=\"https:\/\/edukemy.com\/blog\/wp-content\/uploads\/2024\/06\/14.png 1280w, https:\/\/edukemy.com\/blog\/wp-content\/uploads\/2024\/06\/14-1170x274.png 1170w, https:\/\/edukemy.com\/blog\/wp-content\/uploads\/2024\/06\/14-585x137.png 585w\" sizes=\"(max-width: 1280px) 100vw, 1280px\" \/><\/a><\/figure>\n\n\n\n<p>The Temperature and Pressure Belts of the World constitute a fundamental aspect of global climatology, providing a comprehensive framework for understanding the distribution of temperature and atmospheric pressure across the Earth&#8217;s surface. These belts form the basis for comprehending the intricate dynamics that govern weather patterns, climate variations, and the overall functioning of the Earth&#8217;s atmosphere. In the realm of geography, particularly within the context of optional studies, a nuanced exploration of these belts unveils the interconnectedness of various climatic elements and their profound impact on ecosystems, human societies, and geographic landscapes. This study becomes imperative for geographers seeking a holistic perspective on the planet&#8217;s climatic systems, enabling them to decipher the intricate tapestry of atmospheric conditions that shape the diverse environments experienced across different latitudes.<\/p>\n\n\n\n<div id=\"ez-toc-container\" class=\"ez-toc-v2_0_73 counter-hierarchy ez-toc-counter ez-toc-grey ez-toc-container-direction\">\n<label for=\"ez-toc-cssicon-toggle-item-69d557f675a56\" class=\"ez-toc-cssicon-toggle-label\"><p class=\"ez-toc-title\" style=\"cursor:inherit\">Table of Contents<\/p>\n<span class=\"ez-toc-cssicon\"><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><\/label><input type=\"checkbox\"  id=\"ez-toc-cssicon-toggle-item-69d557f675a56\"  \/><nav><ul class='ez-toc-list ez-toc-list-level-1 ' ><li class='ez-toc-page-1 ez-toc-heading-level-2'><a class=\"ez-toc-link ez-toc-heading-1\" href=\"https:\/\/edukemy.com\/blog\/temperature-and-pressure-belts-of-the-world-geography-optional-notes\/#Distribution_of_Isolation\" title=\"Distribution of Isolation\">Distribution of Isolation<\/a><ul class='ez-toc-list-level-3' ><li class='ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-2\" href=\"https:\/\/edukemy.com\/blog\/temperature-and-pressure-belts-of-the-world-geography-optional-notes\/#Latitudinal_seasonal_Variation_of_Insolation\" title=\"Latitudinal &amp; seasonal Variation of Insolation\">Latitudinal &amp; seasonal Variation of Insolation<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-3\" href=\"https:\/\/edukemy.com\/blog\/temperature-and-pressure-belts-of-the-world-geography-optional-notes\/#Polar_Zone\" title=\"Polar Zone\">Polar Zone<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-4\" href=\"https:\/\/edukemy.com\/blog\/temperature-and-pressure-belts-of-the-world-geography-optional-notes\/#Mid-Lattitude_Zone\" title=\"Mid-Lattitude  Zone\">Mid-Lattitude  Zone<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-5\" href=\"https:\/\/edukemy.com\/blog\/temperature-and-pressure-belts-of-the-world-geography-optional-notes\/#Tropical_Zone\" title=\"Tropical Zone\">Tropical Zone<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-6\" href=\"https:\/\/edukemy.com\/blog\/temperature-and-pressure-belts-of-the-world-geography-optional-notes\/#Factors_Affecting_the_Distribution_of_Insolation\" title=\"Factors Affecting the Distribution of Insolation\">Factors Affecting the Distribution of Insolation<\/a><ul class='ez-toc-list-level-4' ><li class='ez-toc-heading-level-4'><a class=\"ez-toc-link ez-toc-heading-7\" href=\"https:\/\/edukemy.com\/blog\/temperature-and-pressure-belts-of-the-world-geography-optional-notes\/#Angle_of_the_Suns_Rays\" title=\"Angle of the Sun\u2019s Rays\">Angle of the Sun\u2019s Rays<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-4'><a class=\"ez-toc-link ez-toc-heading-8\" href=\"https:\/\/edukemy.com\/blog\/temperature-and-pressure-belts-of-the-world-geography-optional-notes\/#Length_of_Day\" title=\"Length of Day\">Length of Day<\/a><\/li><\/ul><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-9\" href=\"https:\/\/edukemy.com\/blog\/temperature-and-pressure-belts-of-the-world-geography-optional-notes\/#Distance_between_the_Earth_and_the_Sun\" title=\"Distance between the Earth and the Sun\">Distance between the Earth and the Sun<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-10\" href=\"https:\/\/edukemy.com\/blog\/temperature-and-pressure-belts-of-the-world-geography-optional-notes\/#Sunspots\" title=\"Sunspots\">Sunspots<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-11\" href=\"https:\/\/edukemy.com\/blog\/temperature-and-pressure-belts-of-the-world-geography-optional-notes\/#Isotherms\" title=\"Isotherms\">Isotherms<\/a><ul class='ez-toc-list-level-4' ><li class='ez-toc-heading-level-4'><a class=\"ez-toc-link ez-toc-heading-12\" href=\"https:\/\/edukemy.com\/blog\/temperature-and-pressure-belts-of-the-world-geography-optional-notes\/#Characteristics_of_Isotherms\" title=\"Characteristics of Isotherms\">Characteristics of Isotherms<\/a><\/li><\/ul><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-13\" href=\"https:\/\/edukemy.com\/blog\/temperature-and-pressure-belts-of-the-world-geography-optional-notes\/#Temperature_Inversion\" title=\"Temperature Inversion\">Temperature Inversion<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-14\" href=\"https:\/\/edukemy.com\/blog\/temperature-and-pressure-belts-of-the-world-geography-optional-notes\/#Types_of_Temperature_Inversion\" title=\"Types of  Temperature Inversion\">Types of  Temperature Inversion<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-15\" href=\"https:\/\/edukemy.com\/blog\/temperature-and-pressure-belts-of-the-world-geography-optional-notes\/#1_Ground_Inversion\" title=\"1. Ground Inversion\">1. Ground Inversion<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-16\" href=\"https:\/\/edukemy.com\/blog\/temperature-and-pressure-belts-of-the-world-geography-optional-notes\/#2_Subsidence_Inversion\" title=\"2. Subsidence Inversion\">2. Subsidence Inversion<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-17\" href=\"https:\/\/edukemy.com\/blog\/temperature-and-pressure-belts-of-the-world-geography-optional-notes\/#Advection_Inversion\" title=\"Advection Inversion\">Advection Inversion<\/a><ul class='ez-toc-list-level-4' ><li class='ez-toc-heading-level-4'><a class=\"ez-toc-link ez-toc-heading-18\" href=\"https:\/\/edukemy.com\/blog\/temperature-and-pressure-belts-of-the-world-geography-optional-notes\/#i_Frontal_Inversion\" title=\"(i) Frontal Inversion\">(i) Frontal Inversion<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-4'><a class=\"ez-toc-link ez-toc-heading-19\" href=\"https:\/\/edukemy.com\/blog\/temperature-and-pressure-belts-of-the-world-geography-optional-notes\/#ii_Surface_Inversion\" title=\"(ii) Surface Inversion\">(ii) Surface Inversion<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-4'><a class=\"ez-toc-link ez-toc-heading-20\" href=\"https:\/\/edukemy.com\/blog\/temperature-and-pressure-belts-of-the-world-geography-optional-notes\/#iii_Valley_Inversion\" title=\"(iii) Valley Inversion\">(iii) Valley Inversion<\/a><\/li><\/ul><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-21\" href=\"https:\/\/edukemy.com\/blog\/temperature-and-pressure-belts-of-the-world-geography-optional-notes\/#Significance_of_Temperature_Inversion\" title=\"Significance of  Temperature Inversion\">Significance of  Temperature Inversion<\/a><\/li><\/ul><\/li><li class='ez-toc-page-1 ez-toc-heading-level-2'><a class=\"ez-toc-link ez-toc-heading-22\" href=\"https:\/\/edukemy.com\/blog\/temperature-and-pressure-belts-of-the-world-geography-optional-notes\/#Frequently_Asked_Questions_FAQs\" title=\"Frequently Asked Questions (FAQs)\">Frequently Asked Questions (FAQs)<\/a><ul class='ez-toc-list-level-3' ><li class='ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-23\" href=\"https:\/\/edukemy.com\/blog\/temperature-and-pressure-belts-of-the-world-geography-optional-notes\/#1_What_are_the_Temperature_and_Pressure_Belts_of_the_World\" title=\"1. What are the Temperature and Pressure Belts of the World?\">1. What are the Temperature and Pressure Belts of the World?<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-24\" href=\"https:\/\/edukemy.com\/blog\/temperature-and-pressure-belts-of-the-world-geography-optional-notes\/#2_How_do_Temperature_and_Pressure_Belts_influence_global_weather_patterns\" title=\"2. How do Temperature and Pressure Belts influence global weather patterns?\">2. How do Temperature and Pressure Belts influence global weather patterns?<\/a><\/li><li class='ez-toc-page-1 ez-toc-heading-level-3'><a class=\"ez-toc-link ez-toc-heading-25\" href=\"https:\/\/edukemy.com\/blog\/temperature-and-pressure-belts-of-the-world-geography-optional-notes\/#3_Explain_the_significance_of_the_Intertropical_Convergence_Zone_ITCZ_in_the_context_of_Temperature_and_Pressure_Belts\" title=\"3. Explain the significance of the Intertropical Convergence Zone (ITCZ) in the context of Temperature and Pressure Belts.\">3. Explain the significance of the Intertropical Convergence Zone (ITCZ) in the context of Temperature and Pressure Belts.<\/a><ul class='ez-toc-list-level-4' ><li class='ez-toc-heading-level-4'><a class=\"ez-toc-link ez-toc-heading-26\" href=\"https:\/\/edukemy.com\/blog\/temperature-and-pressure-belts-of-the-world-geography-optional-notes\/#In_case_you_still_have_your_doubts_contact_us_on_9811333901\" title=\"In case you still have your doubts, contact us on 9811333901.&nbsp;\">In case you still have your doubts, contact us on 9811333901.&nbsp;<\/a><\/li><\/ul><\/li><\/ul><\/li><\/ul><\/nav><\/div>\n<h2 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Distribution_of_Isolation\"><\/span>Distribution of Isolation <span class=\"ez-toc-section-end\"><\/span><\/h2>\n\n\n\n<p>On average, the amount of insolation received at the earth\u2019s surface decreases from the equator<br>towards the pole, but there is a temporal variation of insolation received at different latitudes at<br>different times of the year.<\/p>\n\n\n\n<figure class=\"wp-block-table\"><div class=\"pcrstb-wrap\"><table><tbody><tr><td>Insolation in received (%)<\/td><td>10<\/td><td>20<\/td><td>30<\/td><td>40<\/td><td> 50<\/td><td> 60<\/td><td>70<\/td><td>80<\/td><td>90<\/td><\/tr><tr><td><br>Insolation in received (%)<\/td><td>100<\/td><td>99<\/td><td>88<\/td><td>79<\/td><td>68<\/td><td>57<\/td><td>47<\/td><td>43<\/td><td>42<\/td><\/tr><\/tbody><\/table><\/div><\/figure>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full\"><img decoding=\"async\" width=\"609\" height=\"523\" data-src=\"https:\/\/edukemy.com\/blog\/wp-content\/uploads\/2023\/09\/clm-.png\" alt=\"\" class=\"wp-image-9939 lazyload\" data-srcset=\"https:\/\/edukemy.com\/blog\/wp-content\/uploads\/2023\/09\/clm-.png 609w, https:\/\/edukemy.com\/blog\/wp-content\/uploads\/2023\/09\/clm--585x502.png 585w\" data-sizes=\"(max-width: 609px) 100vw, 609px\" src=\"data:image\/gif;base64,R0lGODlhAQABAAAAACH5BAEKAAEALAAAAAABAAEAAAICTAEAOw==\" style=\"--smush-placeholder-width: 609px; --smush-placeholder-aspect-ratio: 609\/523;\" \/><\/figure><\/div>\n\n\n<p>Latitudinal and seasonal variation in the amount of insolation received at the outer surface of the earth\u2019s atmosphere (shown in broken line) and at the earth\u2019s surface (shown by solid line)<\/p>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Latitudinal_seasonal_Variation_of_Insolation\"><\/span>Latitudinal &amp; seasonal Variation of Insolation<span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<p>The insolation becomes so low at the poles, that<\/p>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full\"><img decoding=\"async\" width=\"280\" height=\"246\" data-src=\"https:\/\/edukemy.com\/blog\/wp-content\/uploads\/2023\/09\/clm1.png\" alt=\"\" class=\"wp-image-9940 lazyload\" src=\"data:image\/gif;base64,R0lGODlhAQABAAAAACH5BAEKAAEALAAAAAABAAEAAAICTAEAOw==\" style=\"--smush-placeholder-width: 280px; --smush-placeholder-aspect-ratio: 280\/246;\" \/><\/figure><\/div>\n\n\n<p>They received about 40 percent of the amount received at the equator. The tropical zone extending between the tropic of cancer (23.50 N) and Capricorn (23.5 S) receives maximum insolation. Not only this, there is very little variation of insolation during winter and summer seasons because every place within the tropics experiences overhead sun twice every year. The globe is divided into 3 zones on the basis of The amount of insolation received during the year.<\/p>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Polar_Zone\"><\/span>Polar Zone<span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<ul class=\"wp-block-list\"><li>Every place receives maximum and minimum insolation once during the course of a year but sometimes insolation becomes zero due to the absence of direct solar rays.<\/li><\/ul>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Mid-Lattitude_Zone\"><\/span>Mid-Lattitude  Zone<span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<ul class=\"wp-block-list\"><li>Insolation is never absent at any time of the year but seasonal variation increases with increasing latitude.<\/li><\/ul>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Tropical_Zone\"><\/span>Tropical Zone<span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<ul class=\"wp-block-list\"><li>All places experience the overhead sun twice during the course of a year due to the northward and southward march of the sun. The region receives the highest amount of insolation of all other zones and there is little seasonal variation.<\/li><\/ul>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Factors_Affecting_the_Distribution_of_Insolation\"><\/span>Factors Affecting the Distribution of Insolation<span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<h4 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Angle_of_the_Suns_Rays\"><\/span>Angle of the Sun\u2019s Rays<span class=\"ez-toc-section-end\"><\/span><\/h4>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"alignright size-full\"><img decoding=\"async\" width=\"301\" height=\"262\" data-src=\"https:\/\/edukemy.com\/blog\/wp-content\/uploads\/2023\/09\/nclp-.png\" alt=\"\" class=\"wp-image-9941 lazyload\" src=\"data:image\/gif;base64,R0lGODlhAQABAAAAACH5BAEKAAEALAAAAAABAAEAAAICTAEAOw==\" style=\"--smush-placeholder-width: 301px; --smush-placeholder-aspect-ratio: 301\/262;\" \/><\/figure><\/div>\n\n\n<p>As per the rule, vertical rays bring more<br>insolation than oblique rays. As the angle of<br>the sun\u2019s rays decreases poleward, the amount of<br>insolation received also decreases in that<br>direction. Oblique rays have to pass through<br>have to pass through a thicker portion of the<br>atmosphere than vertical rays.<\/p>\n\n\n\n<h4 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Length_of_Day\"><\/span>Length of Day<span class=\"ez-toc-section-end\"><\/span><\/h4>\n\n\n\n<p>Places having a longer length of day and vertical sun\u2019s rays will receive maximum insolation. The shorter the duration of sunshine and longer periods of night, the lesser amount of collation received at the earth\u2019s surface. The length of the day varies at all places except at the equator due to the inclination of the earth\u2019s axis.<\/p>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Distance_between_the_Earth_and_the_Sun\"><\/span>Distance between the Earth and the Sun<span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"alignright size-full\"><img decoding=\"async\" width=\"463\" height=\"127\" data-src=\"https:\/\/edukemy.com\/blog\/wp-content\/uploads\/2023\/09\/clm-3.png\" alt=\"\" class=\"wp-image-9942 lazyload\" src=\"data:image\/gif;base64,R0lGODlhAQABAAAAACH5BAEKAAEALAAAAAABAAEAAAICTAEAOw==\" style=\"--smush-placeholder-width: 463px; --smush-placeholder-aspect-ratio: 463\/127;\" \/><\/figure><\/div>\n\n\n<p>Earth revolves around the sun in an elliptical orbit. The average distance between the sun and the earth is about 93 million miles. At the time of perihelion on January 3 the Earth is<br>nearest to the sun and at the time of aphelion on July 4, it is farthest from the sun.<br>Winter is 7 percent less severe in January in the northern hemisphere but summer is 7 percent more intense in the southern hemisphere at the time of perihelion while Summer is 7 percent less intense in July in the northern hemisphere but winter is 7 percent more intense in the southern hemisphere at the time of aphelion.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><a href=\"https:\/\/edukemy.com\/upsc\/upsc-essay?utm_source=Blog&amp;utm_medium=Banner&amp;utm_campaign=Essay\" target=\"_blank\" rel=\"noreferrer noopener\"><img decoding=\"async\" width=\"1280\" height=\"300\" data-src=\"https:\/\/edukemy.com\/blog\/wp-content\/uploads\/2024\/06\/10.png\" alt=\"\" class=\"wp-image-42412 lazyload\" data-srcset=\"https:\/\/edukemy.com\/blog\/wp-content\/uploads\/2024\/06\/10.png 1280w, https:\/\/edukemy.com\/blog\/wp-content\/uploads\/2024\/06\/10-1170x274.png 1170w, https:\/\/edukemy.com\/blog\/wp-content\/uploads\/2024\/06\/10-585x137.png 585w\" data-sizes=\"(max-width: 1280px) 100vw, 1280px\" src=\"data:image\/gif;base64,R0lGODlhAQABAAAAACH5BAEKAAEALAAAAAABAAEAAAICTAEAOw==\" style=\"--smush-placeholder-width: 1280px; --smush-placeholder-aspect-ratio: 1280\/300;\" \/><\/a><figcaption><a href=\"https:\/\/edukemy.com\/upsc\/upsc-essay?utm_source=Blog&amp;utm_medium=Link&amp;utm_campaign=Essay\">UPSC Essay Course<\/a><\/figcaption><\/figure>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Sunspots\"><\/span>Sunspots<span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<p>Sunspots are defined as dark spots within the photosphere of the sun and are surrounded by chromospheres, disturbances, and explosions. The number of sunspots varies from year to year. The amount of insolation received at the earth\u2019s surface decreases with a decrease in the number of sunspots due to less emission of radiation from the sun.<\/p>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Isotherms\"><\/span>Isotherms<span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<p>Isotherms are the imaginary lines drawn on the maps joining places of equal temperature reduced to sea level.<\/p>\n\n\n\n<h4 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Characteristics_of_Isotherms\"><\/span><strong>Characteristics of Isotherms<\/strong><span class=\"ez-toc-section-end\"><\/span><\/h4>\n\n\n\n<p>\u2022 It is necessary to reduce the actual temperature of all places at sea level before drawing isotherms.<br>\u2022 They do not represent the real temperature of the places through which they pass rather they show the temperature of the sea level<br>\u2022 They run east-west and are generally parallel to latitudes<br>\u2022 They show the horizontal distribution of temperature<br>\u2022 They are more irregular in the northern hemisphere because of the large extent of continents, but they are more regular in the southern hemisphere due to over dominance of oceans.<br>\u2022 They are generally closed-spaced in the northern hemisphere and widely spaced in the southern hemisphere.<br>\u2022 The closely spaced isotherm denotes the rapid rate of change of temperature and steep temperature gradient.<br>\u2022 The widely spaced isotherm denotes the slow rate of temperature change and low-temperature gradient.<br>\u2022 Isotherm on average trending from land towards the ocean bend equator wards during summer and poleward during winter.<br>\u2022 On the other hand, isotherm trending from the ocean to the continents bend poleward during summer and equatorward during winter.<br>\u2022 The isotherm during January and June, are taken as representatives for the study of horizontal distribution of temperature during winter and summer seasons respectively, because they represent seasonal extremes.<br>\u2022 If positive anomaly, then shifts of isotherm is polewards, and if negative anomaly, the shift of isotherm is towards equator wards.<\/p>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full\"><img decoding=\"async\" width=\"499\" height=\"331\" data-src=\"https:\/\/edukemy.com\/blog\/wp-content\/uploads\/2023\/09\/jnc.png\" alt=\"\" class=\"wp-image-9943 lazyload\" data-srcset=\"https:\/\/edukemy.com\/blog\/wp-content\/uploads\/2023\/09\/jnc.png 499w, https:\/\/edukemy.com\/blog\/wp-content\/uploads\/2023\/09\/jnc-263x175.png 263w\" data-sizes=\"(max-width: 499px) 100vw, 499px\" src=\"data:image\/gif;base64,R0lGODlhAQABAAAAACH5BAEKAAEALAAAAAABAAEAAAICTAEAOw==\" style=\"--smush-placeholder-width: 499px; --smush-placeholder-aspect-ratio: 499\/331;\" \/><figcaption>Fig: Isotherm representing the horizontal distribution of temperature in January<\/figcaption><\/figure><\/div>\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full\"><img decoding=\"async\" width=\"480\" height=\"315\" data-src=\"https:\/\/edukemy.com\/blog\/wp-content\/uploads\/2023\/09\/abc-.png\" alt=\"\" class=\"wp-image-9944 lazyload\" src=\"data:image\/gif;base64,R0lGODlhAQABAAAAACH5BAEKAAEALAAAAAABAAEAAAICTAEAOw==\" style=\"--smush-placeholder-width: 480px; --smush-placeholder-aspect-ratio: 480\/315;\" \/><figcaption>Fig: Isotherm representing the horizontal distribution of temperature in June<\/figcaption><\/figure><\/div>\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Temperature_Inversion\"><\/span>Temperature Inversion <span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<p>Temperature inversion is a deviation in the normally decreasing vertical temperature gradient in the troposphere, such that air is colder near the Earth&#8217;s surface and overlain by warm air. <\/p>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full\"><img decoding=\"async\" width=\"517\" height=\"544\" data-src=\"https:\/\/edukemy.com\/blog\/wp-content\/uploads\/2023\/09\/abcd.png\" alt=\"\" class=\"wp-image-9945 lazyload\" src=\"data:image\/gif;base64,R0lGODlhAQABAAAAACH5BAEKAAEALAAAAAABAAEAAAICTAEAOw==\" style=\"--smush-placeholder-width: 517px; --smush-placeholder-aspect-ratio: 517\/544;\" \/><\/figure><\/div>\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full\"><img decoding=\"async\" width=\"505\" height=\"238\" data-src=\"https:\/\/edukemy.com\/blog\/wp-content\/uploads\/2023\/09\/abcs.png\" alt=\"\" class=\"wp-image-9946 lazyload\" src=\"data:image\/gif;base64,R0lGODlhAQABAAAAACH5BAEKAAEALAAAAAABAAEAAAICTAEAOw==\" style=\"--smush-placeholder-width: 505px; --smush-placeholder-aspect-ratio: 505\/238;\" \/><\/figure><\/div>\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Types_of_Temperature_Inversion\"><\/span><br>Types of  Temperature Inversion<span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<h3 class=\"has-normal-font-size wp-block-heading\"><span class=\"ez-toc-section\" id=\"1_Ground_Inversion\"><\/span>1. Ground Inversion<span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<ul class=\"has-normal-font-size wp-block-list\"><li> Also called radiation inversion<\/li><li>Occurs near the Earth&#8217;s surface.<\/li><li>Occurs during long cold winter nights in mid and high-latitudes<\/li><li>CAUSE\/MECHANISM <\/li><li>Excessive nocturnal cooling of ground due to rapid loss of heat from the ground<\/li><\/ul>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full\"><img decoding=\"async\" width=\"195\" height=\"147\" data-src=\"https:\/\/edukemy.com\/blog\/wp-content\/uploads\/2023\/09\/abcsd-1.png\" alt=\"\" class=\"wp-image-9949 lazyload\" src=\"data:image\/gif;base64,R0lGODlhAQABAAAAACH5BAEKAAEALAAAAAABAAEAAAICTAEAOw==\" style=\"--smush-placeholder-width: 195px; --smush-placeholder-aspect-ratio: 195\/147;\" \/><\/figure><\/div>\n\n\n<p>Air, near the surface in direct contact with cold earth becomes cold, while the air above does not lose heat as quickly, making it relatively warmer. Temperature inversion (cold air below, warm air above)<\/p>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full\"><img decoding=\"async\" width=\"466\" height=\"132\" data-src=\"https:\/\/edukemy.com\/blog\/wp-content\/uploads\/2023\/09\/abs-.png\" alt=\"\" class=\"wp-image-9947 lazyload\" src=\"data:image\/gif;base64,R0lGODlhAQABAAAAACH5BAEKAAEALAAAAAABAAEAAAICTAEAOw==\" style=\"--smush-placeholder-width: 466px; --smush-placeholder-aspect-ratio: 466\/132;\" \/><\/figure><\/div>\n\n\n<ul class=\"wp-block-list\"><li>Since ground inversion in static atmospheric conditions (very little movement of air), it is also called static or non-advection inversion.<\/li><li>In low latitudes, it occurs only in winter heights and disappears with sunrise. Height is 30-40 ft.<\/li><li>In mid-latitudes, it can persist tile noon and extend up to a few hundred feet above the surface. Thus, duration and height increase poleward.<\/li><\/ul>\n\n\n\n<figure class=\"wp-block-image size-full is-resized\"><a href=\"https:\/\/edukemy.com\/upsc\/upsc-essay?utm_source=Blog&amp;utm_medium=Banner&amp;utm_campaign=Essay\" target=\"_blank\" rel=\"noreferrer noopener\"><img decoding=\"async\" data-src=\"https:\/\/edukemy.com\/blog\/wp-content\/uploads\/2024\/06\/UPSC-Essay-Course-1280\u00d7300-1-3.svg\" alt=\"\" class=\"wp-image-42688 lazyload\" width=\"781\" height=\"182\" src=\"data:image\/gif;base64,R0lGODlhAQABAAAAACH5BAEKAAEALAAAAAABAAEAAAICTAEAOw==\" style=\"--smush-placeholder-width: 781px; --smush-placeholder-aspect-ratio: 781\/182;\" \/><\/a><\/figure>\n\n\n\n<h3 class=\"has-normal-font-size wp-block-heading\"><span class=\"ez-toc-section\" id=\"2_Subsidence_Inversion\"><\/span>2. Subsidence Inversion<span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"alignright size-full\"><img decoding=\"async\" width=\"148\" height=\"178\" data-src=\"https:\/\/edukemy.com\/blog\/wp-content\/uploads\/2023\/09\/asrd.png\" alt=\"\" class=\"wp-image-9955 lazyload\" src=\"data:image\/gif;base64,R0lGODlhAQABAAAAACH5BAEKAAEALAAAAAABAAEAAAICTAEAOw==\" style=\"--smush-placeholder-width: 148px; --smush-placeholder-aspect-ratio: 148\/178;\" \/><\/figure><\/div>\n\n\n<ul class=\"has-normal-font-size wp-block-list\"><li> Develops when a widespread layer of air descends.<\/li><li>It is called upper air inversion as it occurs at higher altitudes.<\/li><li><strong>Mechanism<\/strong><\/li><li>The descending air layer is compressed: Higher pressure<\/li><li> This creates adiabatic warming of this air.<\/li><li> The sinking air gets warm to the point that it is warmer than the air below it.<\/li><li>This can happen even hundreds of feet above the earth&#8217;s surface.<\/li><li>Subsidence inversion is common over the northern continents in winter and over the subtropical oceans<\/li><li>These regions generally have subsiding air because they are located under large high-pressure centers.<\/li><\/ul>\n\n\n\n<h3 class=\"has-normal-font-size wp-block-heading\"><span class=\"ez-toc-section\" id=\"Advection_Inversion\"><\/span>Advection Inversion<span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<ul class=\"has-normal-font-size wp-block-list\"><li> Also dynamic inversion is always caused due to horizontal\/ vertical movements of air.<\/li><li>It is of 3 subtypes: (i) Frontal (ii) Valley (iii) surface advection inversion<\/li><\/ul>\n\n\n\n<h4 class=\"has-normal-font-size wp-block-heading\"><span class=\"ez-toc-section\" id=\"i_Frontal_Inversion\"><\/span>(i) Frontal Inversion<span class=\"ez-toc-section-end\"><\/span><\/h4>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"alignright size-full\"><img decoding=\"async\" width=\"175\" height=\"123\" data-src=\"https:\/\/edukemy.com\/blog\/wp-content\/uploads\/2023\/09\/asdf.png\" alt=\"\" class=\"wp-image-9954 lazyload\" src=\"data:image\/gif;base64,R0lGODlhAQABAAAAACH5BAEKAAEALAAAAAABAAEAAAICTAEAOw==\" style=\"--smush-placeholder-width: 175px; --smush-placeholder-aspect-ratio: 175\/123;\" \/><\/figure><\/div>\n\n\n<ul class=\"has-normal-font-size wp-block-list\"><li>Occurs when a cold air mass undercuts a warm air mass and lifts it aloft (at a cold front)<\/li><li> Alternatively, a similar inversion can be created when a warm air mass overrides a colder one along a warm front.<\/li><li> Frontal inversions have a considerable slope, whereas inversion is nearly horizontal.<\/li><li> They are associated with temperate cyclones; in the Northern Hemisphere convergence of warm Westerlies with cold polar winds.<\/li><li> Another point of note is that, unlike other inversions, air moisture increases upward in frontal inversion.<\/li><\/ul>\n\n\n\n<h4 class=\"has-normal-font-size wp-block-heading\"><span class=\"ez-toc-section\" id=\"ii_Surface_Inversion\"><\/span><br>(ii) Surface Inversion<span class=\"ez-toc-section-end\"><\/span><\/h4>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"alignright size-full\"><img decoding=\"async\" width=\"220\" height=\"145\" data-src=\"https:\/\/edukemy.com\/blog\/wp-content\/uploads\/2023\/09\/asd.png\" alt=\"\" class=\"wp-image-9952 lazyload\" src=\"data:image\/gif;base64,R0lGODlhAQABAAAAACH5BAEKAAEALAAAAAABAAEAAAICTAEAOw==\" style=\"--smush-placeholder-width: 220px; --smush-placeholder-aspect-ratio: 220\/145;\" \/><\/figure><\/div>\n\n\n<ul class=\"has-normal-font-size wp-block-list\"><li> Caused by horizontal movement of air<\/li><li> Either warm air invades the area of cold air or vice versa.<\/li><li> Warm air being lighter is pushed upward by the relatively denser cold air.<\/li><li> For example along the Californian coast, cool ocean breeze brings cold air to the coast in summer.<\/li><\/ul>\n\n\n\n<h4 class=\"has-normal-font-size wp-block-heading\"><span class=\"ez-toc-section\" id=\"iii_Valley_Inversion\"><\/span><br>(iii) Valley Inversion<span class=\"ez-toc-section-end\"><\/span><\/h4>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"alignright size-full\"><img decoding=\"async\" width=\"195\" height=\"150\" data-src=\"https:\/\/edukemy.com\/blog\/wp-content\/uploads\/2023\/09\/clmh-.png\" alt=\"\" class=\"wp-image-9951 lazyload\" src=\"data:image\/gif;base64,R0lGODlhAQABAAAAACH5BAEKAAEALAAAAAABAAEAAAICTAEAOw==\" style=\"--smush-placeholder-width: 195px; --smush-placeholder-aspect-ratio: 195\/150;\" \/><\/figure><\/div>\n\n\n<ul class=\"has-normal-font-size wp-block-list\"><li>Occurs in valleys, basins, and hollows<\/li><li> It is due to radiation and vertical air movement<\/li><li> At night, rapid loss of heat causes near-surface air to get cold and dense<\/li><li> This air descends\/drains toward the valley floor.<\/li><li> Warm air further away from the surface is further pushed higher up.<\/li><li> Valley inversion creates severe frosts in valley floors; hence human settlements are avoided.<\/li><li> Some Brazil and apple orchards in the Himalayas avoid such frost pockets in the lower slopes of the valley.<\/li><\/ul>\n\n\n\n<h3 class=\"has-normal-font-size wp-block-heading\"><span class=\"ez-toc-section\" id=\"Significance_of_Temperature_Inversion\"><\/span><br>Significance of  Temperature Inversion <span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<p class=\"has-normal-font-size\">\u2022 FOG: the most visible consequence of inversion; it affects visibility and mobility.<br>Inversion in cities can trap pollutants, leading to Smog, London smog (1952).<br>For example: Advection fogs near Newfoundland due to the meeting of cold &amp; warm ocean<br>currents &amp; accompanying air masses.<\/p>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full\"><img decoding=\"async\" width=\"478\" height=\"220\" data-src=\"https:\/\/edukemy.com\/blog\/wp-content\/uploads\/2023\/09\/clmf.png\" alt=\"\" class=\"wp-image-9950 lazyload\" src=\"data:image\/gif;base64,R0lGODlhAQABAAAAACH5BAEKAAEALAAAAAABAAEAAAICTAEAOw==\" style=\"--smush-placeholder-width: 478px; --smush-placeholder-aspect-ratio: 478\/220;\" \/><\/figure><\/div>\n\n\n<p class=\"has-normal-font-size\">\u2022 Frost as discussed in valley inversion affects the location of human settlements and plantations.<br>\u2022 Atmospheric stability: upward ascent or descent of air. It discourages rainfall and favors dry conditions. It acts as a lid and expresses convection<\/p>\n\n\n\n<h2 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"Frequently_Asked_Questions_FAQs\"><\/span>Frequently Asked Questions (FAQs)<span class=\"ez-toc-section-end\"><\/span><\/h2>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"1_What_are_the_Temperature_and_Pressure_Belts_of_the_World\"><\/span>1. What are the Temperature and Pressure Belts of the World?<span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<p><strong>Answer:<\/strong> Temperature and Pressure Belts of the World refer to distinct zones characterized by specific temperature and atmospheric pressure patterns across the Earth&#8217;s surface. These belts are a result of the unequal distribution of solar energy due to the Earth&#8217;s spherical shape and axial tilt. The primary belts include the Equatorial Low, Subtropical Highs, Subpolar Lows, and Polar Highs.<\/p>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"2_How_do_Temperature_and_Pressure_Belts_influence_global_weather_patterns\"><\/span>2. How do Temperature and Pressure Belts influence global weather patterns?<span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<p><strong>Answer:<\/strong> Temperature and Pressure Belts play a crucial role in shaping global weather patterns. The differential heating of the Earth&#8217;s surface leads to the formation of atmospheric circulation cells, such as the Hadley, Ferrel, and Polar cells. These cells drive the movement of air masses, resulting in the creation of prevailing winds, jet streams, and ocean currents. The convergence and divergence of air at these belts also contribute to the development of major climatic zones and influence regional climates.<\/p>\n\n\n\n<h3 class=\"wp-block-heading\"><span class=\"ez-toc-section\" id=\"3_Explain_the_significance_of_the_Intertropical_Convergence_Zone_ITCZ_in_the_context_of_Temperature_and_Pressure_Belts\"><\/span>3. Explain the significance of the Intertropical Convergence Zone (ITCZ) in the context of Temperature and Pressure Belts.<span class=\"ez-toc-section-end\"><\/span><\/h3>\n\n\n\n<p><strong>Answer:<\/strong> The Intertropical Convergence Zone (ITCZ) is a low-pressure belt located near the equator, where trade winds from the Northern and Southern Hemispheres converge. It is a region of intense vertical convection and heavy rainfall. The ITCZ is significant as it marks the meeting point of the Hadley cells, playing a crucial role in the Earth&#8217;s heat distribution. The movement of the ITCZ throughout the year influences the monsoons and rainfall patterns in tropical regions, impacting agriculture and the ecosystem.<\/p>\n\n\n<h4><span class=\"ez-toc-section\" id=\"In_case_you_still_have_your_doubts_contact_us_on_9811333901\"><\/span><strong>In case you still have your doubts, contact us on 9811333901.<\/strong>&nbsp;<span class=\"ez-toc-section-end\"><\/span><\/h4>\n<p><!-- \/wp:heading --><!-- wp:paragraph --><\/p>\n<p>For UPSC Prelims Resources, <a href=\"https:\/\/edukemy.com\/upsc-cse-prelims-resource-centre\" target=\"_blank\" rel=\"noreferrer noopener\">Click here<\/a><\/p>\n<p><!-- \/wp:paragraph --><!-- wp:paragraph --><\/p>\n<p>For Daily Updates and Study Material:<\/p>\n<p><!-- \/wp:paragraph --><!-- wp:paragraph --><\/p>\n<p>Join our Telegram Channel &#8211; <a href=\"https:\/\/t.me\/WithEdukemy4IAS\" target=\"_blank\" rel=\"noreferrer noopener\">Edukemy for IAS<\/a><\/p>\n<p><!-- \/wp:paragraph --><!-- wp:list --><\/p>\n<ul>\n<li>1. Learn through Videos &#8211; <a href=\"https:\/\/bit.ly\/3vOD8sU\" target=\"_blank\" rel=\"noreferrer noopener\">here<\/a><\/li>\n<li>2. Be Exam Ready by Practicing Daily MCQs &#8211; <a href=\"https:\/\/bit.ly\/3Q9z2nF\" target=\"_blank\" rel=\"noreferrer noopener\">here<\/a><\/li>\n<li>3. Daily Newsletter &#8211; Get all your Current Affairs Covered &#8211; <a href=\"https:\/\/bit.ly\/3bE2y5J\" target=\"_blank\" rel=\"noreferrer noopener\">here<\/a><\/li>\n<li>4. Mains Answer Writing Practice &#8211; <a href=\"https:\/\/bit.ly\/3mZuVxl\" target=\"_blank\" rel=\"noreferrer noopener\">here<\/a><\/li>\n<\/ul>\n<p><!-- \/wp:list --><!-- wp:paragraph --><\/p>\n<p>Visit our YouTube Channel &#8211; <a href=\"https:\/\/www.youtube.com\/@ShabbirsEduKemyforIAS\" target=\"_blank\" rel=\"noreferrer noopener\">here<\/a><\/p>","protected":false},"excerpt":{"rendered":"<p>The Temperature and Pressure Belts of the World constitute a fundamental aspect of global climatology, providing a comprehensive framework for understanding the distribution of temperature and atmospheric pressure across the Earth&#8217;s surface. <\/p>\n","protected":false},"author":17,"featured_media":20347,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_eb_attr":"","om_disable_all_campaigns":false,"_monsterinsights_skip_tracking":false,"_monsterinsights_sitenote_active":false,"_monsterinsights_sitenote_note":"","_monsterinsights_sitenote_category":0,"_uf_show_specific_survey":0,"_uf_disable_surveys":false,"_lmt_disableupdate":"","_lmt_disable":"","footnotes":""},"categories":[280],"tags":[143,1131,232,213,140],"class_list":["post-9938","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-geography-optional-notes","tag-geography_optional","tag-temperature-and-pressure-belts","tag-upsc","tag-upsc-notes","tag-upsc_preparation_strategy"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/edukemy.com\/blog\/wp-json\/wp\/v2\/posts\/9938","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/edukemy.com\/blog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/edukemy.com\/blog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/edukemy.com\/blog\/wp-json\/wp\/v2\/users\/17"}],"replies":[{"embeddable":true,"href":"https:\/\/edukemy.com\/blog\/wp-json\/wp\/v2\/comments?post=9938"}],"version-history":[{"count":7,"href":"https:\/\/edukemy.com\/blog\/wp-json\/wp\/v2\/posts\/9938\/revisions"}],"predecessor-version":[{"id":23284,"href":"https:\/\/edukemy.com\/blog\/wp-json\/wp\/v2\/posts\/9938\/revisions\/23284"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/edukemy.com\/blog\/wp-json\/wp\/v2\/media\/20347"}],"wp:attachment":[{"href":"https:\/\/edukemy.com\/blog\/wp-json\/wp\/v2\/media?parent=9938"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/edukemy.com\/blog\/wp-json\/wp\/v2\/categories?post=9938"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/edukemy.com\/blog\/wp-json\/wp\/v2\/tags?post=9938"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}