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Composition and Layers of Atmosphere

By ExamAtlas · 9/18/2026

NCERT Class 11 - Fundamentals of Physical Geography, Chapter 8

Composition and Layers of Atmosphere

The atmosphere is a mixture of gases, water vapour and dust particles held to the earth by gravity. It is divided into five layers by the way temperature changes with height, and nearly all weather occurs in the lowest one.

Composition

GasApproximate share by volume
NitrogenAbout 78 per cent
OxygenAbout 21 per cent
ArgonAbout 0.93 per cent
Carbon dioxideAbout 0.04 per cent
Other gasesNeon, helium, krypton, hydrogen and ozone in traces
  • Nitrogen dilutes oxygen and is essential for plant growth after it is fixed into compounds.
  • Oxygen is needed for respiration and for combustion.
  • Carbon dioxide is small in quantity but crucial - it is needed for photosynthesis and it absorbs outgoing long wave radiation, which keeps the earth warm.
  • Water vapour varies from almost nothing over deserts to about four per cent in the humid tropics; it is the source of all precipitation and also a greenhouse gas.
  • Dust particles act as nuclei of condensation, without which water vapour would not readily form droplets, and they scatter sunlight to produce the colours of sunrise and sunset.
  • Ozone in the stratosphere absorbs harmful ultraviolet radiation and acts as a shield for life.

The five layers

LayerExtent and temperatureKey feature
TroposphereUp to about 8 km at the poles and 18 km at the equator; temperature falls with heightAll weather occurs here; lapse rate about 6.5 degrees per kilometre
StratosphereUp to about 50 km; temperature rises with heightContains the ozone layer; stable air, so aircraft fly here
MesosphereUp to about 80 km; temperature falls sharplyThe coldest layer; meteors burn up here
Thermosphere or ionosphereAbout 80 to 400 km; temperature rises steeplyIonised layers reflect radio waves; auroras occur here
ExosphereBeyond the thermosphereExtremely thin, gradually merging into outer space
  • The boundaries between layers are called pauses - tropopause, stratopause and mesopause.
  • The troposphere is thicker at the equator because strong convection pushes the boundary higher, and thinner at the poles where the air is cold and dense.
  • Temperature falls in the troposphere because the atmosphere is heated from below, by the earth's surface, not directly by the sun.
  • Temperature rises in the stratosphere because ozone absorbs ultraviolet radiation and converts it to heat.

हिंदी संकेत: क्षोभमंडल में तापमान ऊंचाई के साथ घटता है क्योंकि वायुमंडल नीचे से, यानी पृथ्वी की सतह से गर्म होता है। समतापमंडल में तापमान बढ़ता है क्योंकि ओजोन पराबैंगनी किरणें सोखती है।

Exam me kaise aata hai

Factual questions ask the proportion of nitrogen and oxygen, the height of the troposphere at the equator and the poles, and which layer contains ozone. Match-the-following links layer with its characteristic. Statement-based questions test why temperature rises in the stratosphere.

UPSC / State PSC ke liye

Note that carbon dioxide and water vapour are tiny in quantity but decisive in effect, because they are transparent to incoming short wave radiation and opaque to outgoing long wave radiation - this single sentence explains both the natural greenhouse effect and global warming.

Yahan confuse hote hain

Oxygen is the most abundant atmospheric gas  |   Nitrogen is, at about 78 per cent

The troposphere is thickest at the poles  |   It is thickest at the equator and thinnest at the poles

The stratosphere is the coldest layer  |   The mesosphere is the coldest layer

Ek nazar me

  • Nitrogen about 78 per cent, oxygen about 21 per cent, argon about 0.93 and carbon dioxide about 0.04.
  • Water vapour is the source of precipitation; dust particles are nuclei of condensation.
  • Troposphere - about 8 km at the poles, 18 km at the equator; all weather occurs here.
  • Lapse rate in the troposphere is about 6.5 degrees per kilometre.
  • Stratosphere holds the ozone layer and temperature rises with height.
  • Mesosphere is the coldest layer; meteors burn up here.
  • Thermosphere reflects radio waves; the exosphere merges into space.

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