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Subjects

Geography

The heat budget of the earth

पृथ्वी का ऊष्मा बजट

Class 11 Geography explores the heat budget of the Earth as the balance between incoming solar radiation and outgoing terrestrial radiation. Students learn how the atmosphere, land, oceans, clouds, and ice reflect, absorb, store, and redistribute heat, and why the Earth’s average temperature remains broadly stable. The topic connects this balance with the greenhouse effect, latitudinal differences in heating, and the movement of heat through the atmosphere and oceans.

Practice questions

01 Increased carbon dioxide in the atmosphere will affect which process more?

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Answer and explanation

02 How do the importance of the ozone layer and carbon dioxide differ?

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03 Through which process is the effect of greenhouse gases on heat balance most clearly seen?

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04 Why is it useful to study water vapour and carbon dioxide together in atmospheric composition?

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05 How can imbalance of atmospheric gases become an environmental problem?

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06 What is the shared role of water vapour and carbon dioxide in the greenhouse effect?

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07 Why is it necessary to link water vapour with temperature regulation along with rainfall?

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08 How does understanding atmospheric gases and particles help explain evidence of climate change?

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09 Why is carbon dioxide considered climatically important despite being a minor atmospheric component?

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10 Which atmospheric component is most directly involved in Earth radiative balance?

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11 Why can a high concentration of aerosols produce short-term climate effects?

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12 Which two features of the stratosphere are associated with the presence of ozone?

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13 Why is temperature in the troposphere more directly related to Earth’s surface?

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14 Which statement best explains the fall of temperature in the mesosphere?

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15 In the hundred unit solar energy model which relation between reflected and absorbed energy is correct?

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16 What is formed when fourteen units directly absorbed by the atmosphere and thirty four units received from the surface combine?

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17 How is the fifty one units of energy absorbed by the surface later considered to be divided?

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18 How are total hundred units returned to space in Earths heat budget?

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19 In the hundred unit model how is reflection by clouds compared with reflection by the surface?

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20 The about six units reflected by atmospheric scattering are counted in which part of the heat budget?

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21 In the heat budget the main energy exchange between Earths surface and atmosphere is linked with what?

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22 If cloud reflection increases what will generally happen to solar energy absorbed by the surface?

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23 In the heat budget the effect of greenhouse gases strengthens which process?

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24 If energy going directly from Earths surface to space decreases what could be a possible reason?

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25 What can be the general climatic effect of energy surplus in the heat budget?

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Answer and explanation

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