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Geography

Layers of the atmosphere

In Class 11 Geography, this topic explains how Earth’s atmosphere is arranged into distinct layers—troposphere, stratosphere, mesosphere, thermosphere and exosphere—and how temperature, pressure, density and composition change with altitude. Students connect the troposphere with weather and climate, the stratosphere with the ozone layer, and the upper layers with satellites and auroras. The lesson builds a clear foundation for understanding the composition and structure of the atmosphere and its importance for life and human activities.

Medium · Level 3 · 25 questions

TOPIC PRACTICE

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25 questions

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  1. The Sun attracts only the troposphere
  2. Gravity keeps air denser near Earth’s surface
  3. There are no gases in the stratosphere
  4. The exosphere is made of solid rock
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  1. Because weather is linked with the troposphere and radio communication with the ionosphere
  2. Because both occur only in the exosphere
  3. Because both occur only inside the ground
  4. Because neither is related to the atmosphere
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  1. A warmer region with stronger convection
  2. A region of complete darkness
  3. A planet without oceans
  4. A region covered only by glaciers
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  1. Weak vertical mixing can slow the vertical spread of gases
  2. It instantly turns every gas into rain
  3. No chemical processes occur there
  4. It is located inside Earth
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  1. Because more ultraviolet radiation can reach the surface and affect living things
  2. Because it changes Earth’s rotation speed
  3. Because it destroys all mountains
  4. Because it makes the oceans solid
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  1. Because it is a region of ionised particles in the upper atmosphere
  2. Because it occurs only in seawater
  3. Because it lies below the troposphere
  4. Because it has no electrical properties
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  1. Stratosphere
  2. Thermosphere
  3. Troposphere
  4. Mesosphere
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  1. Because different atmospheric layers absorb and transfer energy in different ways
  2. Because pressure and temperature always change in the same direction
  3. Because sunlight reaches only the troposphere
  4. Because the upper atmospheric layers contain no energy
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  1. Stratosphere: stability and ozone absorption
  2. Exosphere: dense clouds and rainfall
  3. Mesosphere: maximum water vapour and monsoon
  4. Troposphere: outer space region of satellites
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  1. Temperature trend plays a major role in identifying layers
  2. Nitrogen is found only in the exosphere
  3. Oxygen is found only in the mesosphere
  4. Water vapour is equal in all layers
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  1. Because the gas is extremely sparse, so molecules undergo very few collisions
  2. Because rainfall pushes them upward
  3. Because mountains at the surface throw them upward
  4. Because ozone makes them heavier there
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  1. Carbon dioxide is completely absent there
  2. Sea winds reach there
  3. A thick cloud layer exists there
  4. Temperature generally decreases with height through the mesosphere
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  1. Air particles are extremely sparse
  2. Ozone warms very little
  3. Air pressure is equal to that at sea level
  4. Water vapour is very abundant
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  1. It forms rainfall
  2. It can bend or reflect some radio waves back toward Earth
  3. It forms polar ice
  4. It blocks surface winds
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  1. Weather-related turbulence is often less vigorous there
  2. Rainfall is greatest there
  3. Oxygen is most abundant there
  4. Clouds must form there every day
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  1. Heating and convection are stronger near the equator
  2. The Sun is always directly overhead at the poles
  3. Gravity disappears near the equator
  4. There is no ozone over the poles
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  1. Stratosphere
  2. Troposphere
  3. Mesosphere
  4. Exosphere
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  1. It contains abundant water vapour and dust, and has active vertical air movement
  2. It has no air pressure
  3. It contains only hydrogen gas
  4. Meteors stop in it
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  1. Troposphere, Stratosphere, Mesosphere, Thermosphere
  2. Stratosphere, Troposphere, Thermosphere, Mesosphere
  3. Mesosphere, Troposphere, Exosphere, Stratosphere
  4. Thermosphere, Mesosphere, Troposphere, Stratosphere
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  1. Troposphere
  2. Mesosphere
  3. Thermosphere
  4. Stratosphere
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  1. Lower troposphere
  2. Marine boundary layer
  3. Exosphere
  4. Lower stratosphere
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  1. Troposphere
  2. Stratosphere
  3. Mesosphere
  4. Thermosphere
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  1. Stratosphere
  2. Mesosphere
  3. Troposphere
  4. Exosphere
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  1. Tropopause
  2. Stratopause
  3. Thermopause
  4. Mesopause
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  1. Because layers are mainly defined by temperature change with height
  2. Because gases are completely different in all layers
  3. Because temperature is same everywhere
  4. Because gases have no mass

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