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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.

Easy · Level 7 · 16 questions

Practice questions

01What happens to the density of air when it is heated?

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02Why does cold air sink downward?

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03Why does rising air cool?

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04Why does descending air warm?

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05How can high humidity affect night temperature?

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06Why can daily temperature range be larger in a dry-air region?

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07Temperature change by horizontal movement of an air mass indicates which process?

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08Why can sea breeze reduce daytime temperature over land?

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09Which option is not a correct process of heat transfer?

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10In which process is heat transferred by actual up-and-down movement of matter?

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11What is the simplest difference between radiation and conduction?

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12What is the directional difference between convection and advection?

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13Why can temperature be relatively lower in areas with more vegetation?

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14Why can dry bare land heat quickly during the day?

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15Why can heating and cooling create differences in air pressure?

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16What is the main effect of atmospheric heating and cooling on weather?

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