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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 In the hundred unit model if total reflection is thirty five and total longwave outgoing is sixty five what is total returned energy?

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Answer and explanation

02 Which statement shows the deepest understanding of the heat budget?

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03 In the hundred unit heat budget model what do twenty seven units reflected by clouds show?

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04 If only two units of solar energy are reflected by Earth's surface what does it indicate?

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05 Scattering and reflection of six units of energy by the atmosphere strengthens which process?

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06 If thirty five units out of one hundred return to space how many units are absorbed in the Earth atmosphere system?

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07 What is formed together by absorption of fourteen units by the atmosphere and fifty one units by the surface?

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08 After the surface absorbs fifty one units of energy by which path does that energy mainly return?

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09 Direct escape of seventeen units of terrestrial radiation to space is most closely linked with which concept?

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10 Radiation of forty eight units of energy by the atmosphere to space proves which fact?

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11 Thirty five units of reflection and sixty five units of emitted energy together balance one hundred units. Which principle does this show?

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12 If absorbed energy at the surface increases but emission remains the same what happens to the local heat budget?

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13 In which condition can the net radiation of a place become negative?

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14 Why does longwave radiation escape more effectively on a clear sky night?

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15 If clouds remain high during both day and night what effect may occur on daily temperature range?

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16 Why can net radiation increase when albedo decreases?

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17 When snow cover decreases what type of feedback is possible in the polar heat budget?

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18 Greenhouse gases mainly affect which energy flow in the heat budget?

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19 If atmospheric water vapour is high why can night cooling become slower?

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20 Closure of the atmospheric window may point toward which result?

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21 In which condition can land surface heat faster than sea surface?

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22 Why does the ocean heat budget help moderate climate?

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23 What is the heat budget based reason for large diurnal range in deserts?

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24 How do concrete and asphalt change the heat budget in an urban heat island?

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25 Why can deforestation change the local heat budget in several ways at once?

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