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Subjects

Geography

Heating and cooling of the atmosphere

In this Class 11 Geography topic, students learn how the atmosphere is heated and cooled through incoming solar radiation and outgoing terrestrial radiation. The lesson explains Earth’s heat balance and the roles of conduction, convection, advection, and latent heat in transferring energy through the atmosphere. Students also examine how land and water surfaces, cloud cover, humidity, and atmospheric circulation influence temperature patterns and help produce differences between places and times.

Hard · Level 7 · 2 questions

TOPIC PRACTICE

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  1. Because cooling air has greater chance of condensation
  2. Because water vapour ends as air rises
  3. Because a hot surface pulls clouds downward
  4. Because solar radiation completely stops at height
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  1. Strong hot dry wind and clear afternoon
  2. Thick clouds and intense vertical mixing
  3. Clear calm night and enough moisture near the surface
  4. Very low humidity and hot bare surface

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