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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 6 · 25 questions

Practice questions

01Why does temperature remain relatively higher on a cloudy night?

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02Why does a surface cool during evaporation?

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03What happens when water vapour changes into water droplets?

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04Why does land surface heat faster than water?

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05Why does sea temperature change slowly?

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06Which temperature pattern is most characteristic of a coastal location compared with an inland location at the same latitude?

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07Why can temperature range be greater in continental interiors?

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08Generally, what happens to temperature as altitude increases?

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09What does normal lapse rate show?

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10What is the feature of temperature inversion?

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11Why does the chance of frost increase on a clear calm night?

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12Why does the day's maximum temperature often occur after noon?

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13When is the daily minimum temperature usually found?

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14Which energy is more important in the greenhouse effect?

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15Which gas contributes to the greenhouse effect?

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16How does water vapour help keep the atmosphere warm?

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17Why are desert nights often cold?

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18Why does a black road feel hotter during the day?

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19Why does a white or snowy surface heat less?

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20Why can cities be warmer in the urban heat island effect?

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21How can vegetation help reduce local temperature?

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22Heat balance shows balance between what?

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23Outgoing heat from Earth is mainly in which form?

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24Shortwave radiation is related to what?

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25Longwave radiation is related to what?

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