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Subjects

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 2 · 25 questions

TOPIC PRACTICE

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  1. The equatorial region
  2. The polar night
  3. The exosphere
  4. The mesopause
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  1. The ozone layer
  2. Relatively stable air
  3. Most daily weather events
  4. Temperature generally increases with height
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  1. Thermosphere
  2. Troposphere
  3. Stratosphere
  4. Lithosphere
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  1. It is the outer, very rarefied region of the atmosphere
  2. It is the layer with the most rainfall
  3. It is the main ozone-rich region
  4. It is the first layer above Earth’s surface
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  1. Because equatorial areas have greater heating and vertical convection
  2. Because the Sun is always overhead at the poles
  3. Because gravity is absent at the equator
  4. Because there is no atmosphere at the poles
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  1. The ionised region of the thermosphere
  2. The lower troposphere
  3. A dense rainfall zone
  4. The ozone layer of the stratosphere
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  1. Gravity keeps air denser near Earth’s surface
  2. The Sun heats only this layer
  3. Other layers contain no gases
  4. It is the outermost layer
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  1. Because more harmful ultraviolet radiation can reach Earth’s surface
  2. Because gravity ends
  3. Because all weather stops
  4. Because rivers dry up
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  1. Stratosphere
  2. Troposphere
  3. Lower troposphere
  4. Surface boundary layer
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  1. They are among the light gases present in this very thin outer layer, and some particles can escape into space
  2. They form raindrops
  3. They form the ozone layer
  4. They form fog at Earth’s surface
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  1. Stratosphere
  2. Troposphere
  3. Mesosphere
  4. Exosphere
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  1. Because it is a region of ionised particles across upper layers
  2. Because it exists only at the surface
  3. Because it is only inside oceans
  4. Because it has no electrical property
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  1. Troposphere
  2. Exosphere
  3. Upper thermosphere
  4. Mesopause
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  1. Warm equatorial regions
  2. Cold polar regions
  3. Above permanent ice regions
  4. During the polar winter night
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  1. Ionised particles
  2. Large raindrops
  3. Sea waves
  4. Mountain glaciers
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  1. Stratosphere
  2. Troposphere
  3. Lower surface layer
  4. Exosphere
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  1. Exosphere—main rainfall region
  2. Troposphere—weather
  3. Stratosphere—ozone
  4. Mesosphere—meteor burning
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  1. Because each major layer has a different pattern of temperature change with height
  2. Because all layers have the same temperature
  3. Because layers are identified only by rainfall
  4. Because the layers are unrelated to Earth’s rotation
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  1. Mesosphere
  2. Stratosphere
  3. Exosphere
  4. Troposphere
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  1. Greater heating and stronger convection in equatorial regions
  2. The ozone layer is completely absent at the poles
  3. Air pressure is always zero at the equator
  4. The stratosphere does not form over the poles
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  1. The troposphere does not have a fixed thickness; it varies with thermal conditions
  2. The tropopause forms only over oceans
  3. The stratosphere ends at the poles
  4. All atmospheric layers have equal thickness
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  1. Troposphere
  2. Thermosphere
  3. Stratosphere
  4. Lower troposphere
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  1. Condensation of water vapour
  2. Bending of waves by ionised particles
  3. Rainfall formation by ozone
  4. Ice formation by dust particles
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  1. Because temperature changes differently with altitude in different layers
  2. Because every layer contains the same gases in equal amounts
  3. Because altitude has no physical meaning
  4. Because atmospheric layers form only above oceans
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  1. Ocean tides and the Moon’s shadow
  2. Interactions between charged particles and gases in the upper atmosphere
  3. Mist and fog in the troposphere
  4. Ordinary clouds in the stratosphere

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