

{"id":4241,"date":"2026-03-04T12:49:03","date_gmt":"2026-03-04T07:19:03","guid":{"rendered":"https:\/\/vajiramandravi.com\/upsc-exam\/?p=4241"},"modified":"2026-03-11T18:32:12","modified_gmt":"2026-03-11T13:02:12","slug":"composition-and-structure-of-atmosphere","status":"publish","type":"post","link":"https:\/\/vajiramandravi.com\/upsc-exam\/composition-and-structure-of-atmosphere\/","title":{"rendered":"Composition and Structure of Atmosphere, UPSC Prelims 2025"},"content":{"rendered":"<p>The atmosphere is the layer of gases surrounding Earth. The air is an essential component of the earth's mass, and 99 percent of the total mass of the atmosphere is concentrated at a height of 32 kilometres above the earth's surface, held in place by gravity. Nitrogen and oxygen account for 99 percent of the gases in dry air, with argon, carbon dioxide, helium, neon, and other gases making up the remaining volume. The combination of gases in the atmosphere forms a complex system divided into layers that support life on Earth.<\/p>\r\n<p>The atmosphere can be divided into five layers - Troposphere, Ionosphere, Stratosphere, Exosphere, and Mesosphere. These atmospheric layers are characterised by variations in temperature resulting primarily from the absorption of solar radiation.<\/p>\r\n<h2>Atmosphere Composition<\/h2>\r\n<p>Earth\u2019s atmosphere comprises about 78 percent nitrogen, 21 percent oxygen, 0.9 percent argon, and 0.1 percent other gases. The remaining 0.1% of gases includes a trace amount of neon, water vapour, carbon dioxide, methane and others. Water vapour and Carbon dioxide are found up to 90 km from the earth's surface.<\/p>\r\n<ul>\r\n\t<li><strong>Nitrogen:<\/strong>\u00a0Nitrogen is the most prevalent element in the atmosphere's dry composition. At the Earth's surface, nitrogen slows down the rate of burning and dilutes oxygen. Living things require nitrogen to synthesise\u00a0<strong>proteins<\/strong>.<\/li>\r\n\t<li><strong>Oxygen:\u00a0<\/strong>It is essential for\u00a0<strong>respiration\u00a0<\/strong>and necessary for\u00a0<strong>combustion (burning).\u00a0<\/strong><\/li>\r\n\t<li><strong>Carbon dioxide:<\/strong>\r\n<ul>\r\n\t<li>It is essential for\u00a0<strong><a href=\"https:\/\/vajiramandravi.com\/upsc-exam\/photosynthesis\/\" target=\"_blank\">photosynthesis<\/a>\u00a0<\/strong>by plants, algae and photosynthetic bacteria, to be used by living things as food.<\/li>\r\n\t<li>It acts as a blanket that prevents heat from escaping into space called the\u00a0<strong>greenhouse effect<\/strong>. It absorbs some of the terrestrial radiation and reflects some of it toward the surface of the earth.<\/li>\r\n<\/ul>\r\n<\/li>\r\n\t<li><strong>Ozone:<\/strong>\u00a0It serves as a\u00a0<strong>filter\u00a0<\/strong>and can be found between 10 and 50 kilometres above the surface of the earth which absorbs harmful<strong>\u00a0ultraviolet rays<\/strong>\u00a0from the sun and stops them from reaching the earth's surface.<\/li>\r\n\t<li><strong>Water Vapour:<\/strong>\u00a0It is typically present in up to 4% of the total volume, depending on location. With an increase in altitude, water vapour levels decline<strong>.<\/strong>\r\n<ul>\r\n\t<li>When dry winds blow through the\u00a0<strong>Earth's desert regions (30\u00b0 N\/S)<\/strong>, the contribution of water vapour to the composition of the atmosphere is nearly zero.<\/li>\r\n<\/ul>\r\n<\/li>\r\n\t<li><strong>Dust Particles:<\/strong>\u00a0In the lower layers of the atmosphere, dust particles are typically concentrated, but\u00a0<strong>convectional air currents\u00a0<\/strong>can carry them to great heights.\r\n\r\n<ul>\r\n\t<li>They are more concentrated in subtropical and temperate regions than in equatorial and polar regions due to dry winds.<\/li>\r\n<\/ul>\r\n<\/li>\r\n<\/ul>\r\n<h2>Atmosphere Structure<\/h2>\r\n<p>The atmosphere is divided into<strong>\u00a0five layers,\u00a0<\/strong>depending on temperature and density. In general, both temperature and density decrease with increasing altitude.<\/p>\r\n<figure>\r\n<table>\r\n<tbody>\r\n<tr>\r\n<td class=\"tb-color\" colspan=\"2\"><strong>Layers of the Atmosphere<\/strong><\/td>\r\n<\/tr>\r\n<tr>\r\n<td><strong>Troposphere<\/strong><\/td>\r\n<td>\r\n<p>- The troposphere is the<strong>\u00a0lowest layer<\/strong>\u00a0and its average\u00a0<strong>height is 13 km<\/strong>\u00a0and extends roughly to a<strong>\u00a0height of 8 km near the poles<\/strong>\u00a0and about\u00a0<strong>18 km at the equator<\/strong>.<\/p>\r\n<p>- It is\u00a0<strong>thickest at the equator<\/strong>\u00a0because heat is transported to great heights by\u00a0<strong>strong convection currents<\/strong>\u00a0and much\u00a0<strong>thinner\u00a0<\/strong>at the<strong>\u00a0North and South Poles.\u00a0<\/strong><\/p>\r\n<p>- Approximately\u00a0<strong>75 and 80 percent of the mass<\/strong>\u00a0of the entire atmosphere is contained in the troposphere.<\/p>\r\n<p>- Most of the<strong>\u00a0water vapour<\/strong>\u00a0in the\u00a0<strong>atmosphere<\/strong>, along with dust and ash particles, are found in the troposphere that\u2019s why most of<strong>\u00a0Earth\u2019s clouds<\/strong>\u00a0are located in this layer.<\/p>\r\n<p>- Temperatures in the troposphere\u00a0<strong>decrease with altitude.<\/strong><\/p>\r\n<p><strong>Tropopause:<\/strong>\u00a0The<strong>\u00a0zone separating the troposphere from the stratosphere<\/strong>\u00a0is known as the tropopause.<\/p>\r\n<ul>\r\n\t<li>At the tropopause, the temperature of the air is about\u00a0<strong>minus 80\u00b0C over the equator<\/strong>\u00a0and about\u00a0<strong>minus 45\u00b0C over the poles.<\/strong><\/li>\r\n<\/ul>\r\n<\/td>\r\n<\/tr>\r\n<tr>\r\n<td><strong>Stratosphere<\/strong><\/td>\r\n<td>\r\n<p>- The stratosphere rises to a\u00a0<strong>height of 50 km<\/strong>, above the tropopause.<\/p>\r\n<p>- It contains the\u00a0<strong>ozone layer<\/strong>\u00a0which absorbs<strong>\u00a0ultravioletradiation\u00a0<\/strong>and shields life on the earth from intense, harmful forms of\u00a0<strong>energy<\/strong>.<\/p>\r\n<p><strong>- Temperature\u00a0<\/strong>in the stratosphere\u00a0<strong>increases with altitude\u00a0<\/strong>as a result of heat that is produced during the\u00a0<strong>formation of ozone.<\/strong><\/p>\r\n<p>- There is almost\u00a0<strong>no water vapour<\/strong>\u00a0in the stratosphere.<\/p>\r\n<p>- Although the stratosphere is\u00a0<strong>nearly cloudy and weather-free<\/strong>, polar stratospheric clouds can occasionally be found at its lowest, coldest altitudes.<\/p>\r\n<p>- It's the highest point in the atmosphere that\u00a0<strong>jet planes can access.<\/strong><\/p>\r\n<p>- The top of the stratosphere is called the\u00a0<strong>stratopause<\/strong>.<\/p>\r\n<\/td>\r\n<\/tr>\r\n<tr>\r\n<td><strong>Mesosphere<\/strong><\/td>\r\n<td>\r\n<p>- It is located between<strong>\u00a050 and 80 kilometres<\/strong>\u00a0above the surface of the Earth.<\/p>\r\n<p>- The\u00a0<strong>temperature\u00a0<\/strong>in the stratosphere\u00a0<strong>decreases with altitude.\u00a0<\/strong><\/p>\r\n<p>- With a temperature of about\u00a0<strong>-90\u00b0C<\/strong>, the top of this layer is the\u00a0<strong>coldest place on Earth.<\/strong><\/p>\r\n<p>- Noctilucent clouds (night-shining clouds) or<strong>\u00a0polar mesospheric clouds<\/strong>\u00a0are formed by the extremely rare water vapour that is found at the top of the mesosphere.<\/p>\r\n<p><strong>- Meteors\u00a0<\/strong>typically burn up in this layer of the atmosphere.<\/p>\r\n<p>- Both\u00a0<strong>Sounding rockets<\/strong>\u00a0and\u00a0<strong>rocket-powered aircraft<\/strong>\u00a0are capable of reaching the mesosphere.<\/p>\r\n<p>- The\u00a0<strong>upper boundary<\/strong>\u00a0of the mesosphere is called the\u00a0<strong>mesopause<\/strong>.<\/p>\r\n<\/td>\r\n<\/tr>\r\n<tr>\r\n<td><strong>Thermosphere<\/strong><\/td>\r\n<td>\r\n<p>- The Thermosphere is located between about\u00a0<strong>80 and 700 kilometres<\/strong>\u00a0above Earth\u2019s surface<\/p>\r\n<p>- The\u00a0<strong>ionosphere\u00a0<\/strong>(<strong>between 80 and 400 km) is a part of it.\u00a0<\/strong><\/p>\r\n<ul>\r\n\t<li>It contains\u00a0<strong>ions<\/strong>, which are charged particles.<\/li>\r\n\t<li><strong>Radio waves<\/strong>\u00a0transmitted from the earth are reflected to the earth by this layer.<\/li>\r\n\t<li>The temperature\u00a0<strong>increases with height.<\/strong><\/li>\r\n\t<li>The D layer, the E layer, and the F layer are the three major ionosphere layers\/regions.<\/li>\r\n\t<li>These regions\u00a0<strong>lack distinct borders<\/strong>\u00a0and the altitudes at which they are found change throughout the day and from season to season.<\/li>\r\n<\/ul>\r\n<p>- The Thermosphere is both\u00a0<strong>cloud and water-vapour-free.\u00a0<\/strong><\/p>\r\n<p>- Here, one can occasionally see the\u00a0<strong>aurora australis<\/strong>\u00a0and\u00a0<strong>borealis<\/strong>.<\/p>\r\n<p>- The<strong>\u00a0International Space Station orbits<\/strong>\u00a0in the thermosphere.<\/p>\r\n<\/td>\r\n<\/tr>\r\n<tr>\r\n<td><strong>Exosphere<\/strong><\/td>\r\n<td>\r\n<p>- The topmost layer of Earth's atmosphere is known as the\u00a0<strong>exosphere<\/strong>.<\/p>\r\n<p>- Located between about<strong>\u00a0700 and 10,000 kilometres\u00a0<\/strong>above the surface of the Earth.<\/p>\r\n<p>- Because the molecules in this layer have a very\u00a0<strong>low density<\/strong>, this layer does not behave like gases and allows particles to escape into space.<\/p>\r\n<p>- The<strong>\u00a0bottom of the exosphere<\/strong>\u00a0is also known as the exobase<strong>.\u00a0<\/strong><\/p>\r\n<\/td>\r\n<\/tr>\r\n<\/tbody>\r\n<\/table>\r\n<\/figure>\r\n<h2>Role of Atmosphere<\/h2>\r\n<p>The atmosphere plays a crucial role in maintaining life on Earth. Without it, the temperature would fall well below the freezing point everywhere on the surface. The heat absorbed and trapped by the atmosphere helps regulate Earth\u2019s average temperature, making it suitable for living organisms. Gases such as carbon dioxide are particularly effective at absorbing and re-emitting infrared radiation, thereby warming the planet through the greenhouse effect.<\/p>\r\n<h2>Weather<\/h2>\r\n<p>Weather is a combination of events that occur in our atmosphere daily. The weather varies around the world and changes over a few minutes, hours, days, and weeks. The\u00a0<strong>troposphere<\/strong>, the region of Earth's atmosphere closest to the ground, is where most weather happens.<\/p>\r\n<ul>\r\n\t<li><strong>Air Pressure and Weather:\u00a0<\/strong>Changes in atmospheric pressure determine the weather that occurs in a region.\r\n\r\n<ul>\r\n\t<li>Usually,\u00a0<strong>clear, blue skies\u00a0<\/strong>are present when\u00a0<strong>air pressure is high.<\/strong>\u00a0The high pressure prevents clouds from forming by causing air to flow down and fan out when it gets close to the ground.<\/li>\r\n\t<li><strong>Low air pressure\u00a0<\/strong>causes air to flow together before converging upward, where it rises, cools, and forms clouds.<\/li>\r\n<\/ul>\r\n<\/li>\r\n<\/ul>\r\n<h2>Climate<\/h2>\r\n<p>Climate refers to an area's average weather pattern over a long period. The weather is what we see outside on any particular day; the climate is the average of that weather. Different regions have different regional climates.<\/p>\r\n<ul>\r\n\t<li><strong>Global climate:<\/strong>\u00a0The average of all regional climates is referred to as the global climate<strong>.\u00a0<\/strong>Weather patterns are anticipated to change along with the global climate.<\/li>\r\n\t<li><strong>Elements of Climate:<\/strong>\u00a0The main elements of climate are\u00a0<strong>temperature<\/strong>,\u00a0<strong>pressure<\/strong>,\u00a0<strong>winds<\/strong>, and\u00a0<strong>rainfall<\/strong>. All these elements are\u00a0<strong>highly variable<\/strong>\u00a0and constitute the\u00a0<strong>climate<\/strong>.\r\n\r\n<ul>\r\n\t<li>They are inextricably linked, and any change in one of them usually causes changes in the others.<\/li>\r\n\t<li>The variations in\u00a0<strong>climate\u00a0<\/strong>are largely the result of variations in the amount,\u00a0<strong>intensity<\/strong>, and\u00a0<strong>distribution\u00a0<\/strong>of these elements over the\u00a0<strong>earth<\/strong>.<\/li>\r\n<\/ul>\r\n<\/li>\r\n\t<li><strong>Climate Controls<\/strong>: The important factors that influence the regional climates are:\r\n\r\n<ul>\r\n\t<li>latitude<\/li>\r\n\t<li>altitude<\/li>\r\n\t<li>winds and air masses<\/li>\r\n\t<li>distribution of land and water, distance from the sea<\/li>\r\n\t<li>semi-permanent high and low-pressure systems<\/li>\r\n\t<li>atmospheric disturbances or storms<\/li>\r\n\t<li>ocean currents<\/li>\r\n\t<li>mountain barriers<\/li>\r\n\t<li>natural vegetation<\/li>\r\n<\/ul>\r\n<\/li>\r\n<\/ul>\r\n<h2>Atmosphere UPSC PYQs<\/h2>\r\n<p><strong>Question 1:\u00a0<\/strong>Troposphere is a very significant atmosphere layer that determines weather processes. How?\u00a0<strong>(UPSC Mains 2022)<\/strong><\/p>\r\n<p><strong>Question 2: <\/strong><span style=\"font-weight: 400\">Consider the following statements: <strong>(UPSC Prelims 2025)<\/strong><\/span><\/p>\r\n<ol>\r\n\t<li><span style=\"font-weight: 400\"> Without the <\/span>atmosphere<span style=\"font-weight: 400\">, temperature would be well below freezing point everywhere on the Earth's surface.<\/span><\/li>\r\n\t<li><span style=\"font-weight: 400\"> Heat absorbed and trapped by the atmosphere maintains our planet's -average temperature.<\/span><\/li>\r\n\t<li>Atmosphere's gases, like carbon dioxide, are particularly good at absorbing and trapping radiation.<\/li>\r\n<\/ol>\r\n<p><span style=\"font-weight: 400\">Which of the statements given above are correct?<\/span><\/p>\r\n<p><span style=\"font-weight: 400\">a) 1 and 3 only<\/span><\/p>\r\n<p><span style=\"font-weight: 400\">b) 1 and 2 only<\/span><\/p>\r\n<p><span style=\"font-weight: 400\">c) 1, 2 and 3<\/span><\/p>\r\n<p><span style=\"font-weight: 400\">d) 2 and 3 only<\/span><\/p>\r\n<p><strong>Ans: (d)<\/strong><\/p>\r\n<p><strong>Question 3: <\/strong>Normally, the temperature decreases with the increase in height from the Earth\u2019s surface, because<strong>\u00a0(UPSC Prelims 2012)<\/strong><\/p>\r\n<ol>\r\n\t<li>the atmosphere can be heated upwards only from the Earth\u2019s surface<\/li>\r\n\t<li>there is more moisture in the upper atmosphere<\/li>\r\n\t<li>the air is less dense in the upper atmosphere<\/li>\r\n<\/ol>\r\n<p>Select the correct answer using the codes given below<\/p>\r\n<p><span style=\"font-weight: 400\">a) <\/span>1 only<\/p>\r\n<p><span style=\"font-weight: 400\">b) <\/span>2 and 3 only<\/p>\r\n<p><span style=\"font-weight: 400\">c) <\/span>1 and 3 only<\/p>\r\n<p><span style=\"font-weight: 400\">d) <\/span>1, 2 and 3<\/p>\r\n<p><strong>Answer: (c)<\/strong><\/p>\r\n<p><strong>Question 4: <\/strong>A layer in the Earth\u2019s atmosphere called Ionosphere facilitates radio communication. Why?\u00a0<strong>(UPSC Prelims 2011)<\/strong><\/p>\r\n<ol>\r\n\t<li>The presence of ozone causes the reflection of radio waves to Earth.<\/li>\r\n\t<li>Radio waves have a very long wavelength.<\/li>\r\n<\/ol>\r\n<p>Which of the statement(s) given above is\/are correct?<\/p>\r\n<p><span style=\"font-weight: 400\">a) <\/span>1 only<\/p>\r\n<p><span style=\"font-weight: 400\">b) <\/span>2 only<\/p>\r\n<p><span style=\"font-weight: 400\">c) <\/span>Both 1 and 2<\/p>\r\n<p><span style=\"font-weight: 400\">d) <\/span>Neither 1 nor 2<\/p>\r\n<p><strong>Answer: (d)<\/strong><\/p>\r\n<table style=\"border-collapse: collapse;width: 100%;height: 150px\">\r\n<tbody>\r\n<tr style=\"height: 25px\">\r\n<td class=\"tb-color\" style=\"width: 50%;text-align: center;height: 25px\" colspan=\"2\"><strong>Other Related Posts<\/strong><\/td>\r\n<\/tr>\r\n<tr style=\"height: 25px\">\r\n<td style=\"width: 50%;text-align: center;height: 25px\"><a 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density.<\/p>\n","protected":false},"author":6,"featured_media":17610,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[173],"tags":[184,40],"class_list":{"0":"post-4241","1":"post","2":"type-post","3":"status-publish","4":"format-standard","5":"has-post-thumbnail","7":"category-quest-level-3","8":"tag-composition-and-structure-of-atmosphere","9":"tag-quest"},"acf":[],"_links":{"self":[{"href":"https:\/\/vajiramandravi.com\/upsc-exam\/wp-json\/wp\/v2\/posts\/4241","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/vajiramandravi.com\/upsc-exam\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/vajiramandravi.com\/upsc-exam\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/vajiramandravi.com\/upsc-exam\/wp-json\/wp\/v2\/users\/6"}],"replies":[{"embeddable":true,"href":"https:\/\/vajiramandravi.com\/upsc-exam\/wp-json\/wp\/v2\/comments?post=4241"}],"version-history":[{"count":1,"href":"https:\/\/vajiramandravi.com\/upsc-exam\/wp-json\/wp\/v2\/posts\/4241\/revisions"}],"predecessor-version":[{"id":19735,"href":"https:\/\/vajiramandravi.com\/upsc-exam\/wp-json\/wp\/v2\/posts\/4241\/revisions\/19735"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/vajiramandravi.com\/upsc-exam\/wp-json\/wp\/v2\/media\/17610"}],"wp:attachment":[{"href":"https:\/\/vajiramandravi.com\/upsc-exam\/wp-json\/wp\/v2\/media?parent=4241"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/vajiramandravi.com\/upsc-exam\/wp-json\/wp\/v2\/categories?post=4241"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/vajiramandravi.com\/upsc-exam\/wp-json\/wp\/v2\/tags?post=4241"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}