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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 What is the simple conclusion of Earths heat budget?

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02 What is the heat budget of the earth related to?

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03 What is the main source of energy for the earth?

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04 Solar radiation mainly reaches the earth in which form?

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05 Radiation emitted by the earth is generally of which type?

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06 What does balance mean in heat budget?

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07 What is the correct meaning of albedo?

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08 Which surface generally has high albedo?

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09 Which surface is more likely to absorb more solar energy?

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10 What is the energy received from the Sun generally called in geography?

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11 What can clouds do with solar energy in the atmosphere?

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12 What is the main effect of solar energy reaching the Earth’s surface?

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13 What is called terrestrial radiation?

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14 How does the atmosphere help control the earth's temperature?

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15 How is the greenhouse effect linked with heat budget?

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16 Which gas is important in trapping Earth's heat?

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17 Why does the earth's surface become warmer during the day?

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18 Why does the earth's surface cool at night?

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19 What would happen if Earth emitted much less energy than it received?

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20 What would happen if Earth lost more energy than it received?

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21 Why is the global heat budget generally considered balanced?

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22 Reflection in Earth's heat budget occurs by which of the following?

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23 Why is some solar energy absorbed in the atmosphere?

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24 What is the simple meaning of scattering in heat budget?

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25 Which process helps keep Earth's temperature suitable for life?

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