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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.

Expert · Level 7 · 1 questions

TOPIC PRACTICE

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  1. Surface is dry dark and produces more sensible heat
  2. There is no cold advection and sky is clear
  3. A large part of energy goes into evaporation and heat storage in soil
  4. Air is stable and latent heat is zero

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