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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.

TOPIC PRACTICE

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Up to 16 questions from this page. Select your focus, then start.

16 questions

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Medium · Level 7
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  1. Tendency of surface warming will increase
  2. Surface temperature will always fall
  3. Solar energy will completely stop
  4. Reflection will necessarily be hundred percent
Medium · Level 7
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  1. Loss of longwave terrestrial energy
  2. Arrival of shortwave solar energy
  3. Direct absorption of solar energy
  4. Daytime cloud reflection
Medium · Level 7
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  1. Reflection of shortwave solar energy
  2. Counter radiation of longwave energy
  3. Storage of ground heat
  4. Stopping of ocean currents
Medium · Level 7
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  1. Counter radiation of longwave energy
  2. Complete absence of shortwave energy
  3. Greater obliqueness of solar rays
  4. High albedo of snow
Medium · Level 7
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  1. Atmosphere changes energy through reflection scattering and absorption
  2. The Sun gives no energy
  3. Earths surface takes no energy
  4. Oceans stop all rays
Medium · Level 7
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  1. Continuous uncontrolled warming or cooling of Earth
  2. Rotation of Earth
  3. Flowing of rivers
  4. Formation of clouds
Medium · Level 7
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  1. Out of hundred thirty five reflected sixty five absorbed and hundred total returned
  2. Out of hundred sixty five reflected and thirty five absorbed
  3. Out of hundred all energy stored at surface
  4. Out of hundred no energy goes to space
Medium · Level 7
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  1. Sixty five units
  2. Thirty five units
  3. Hundred units
  4. Fourteen units
Medium · Level 7
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  1. Because it returns to space before being absorbed by the Earth system
  2. Because it heats the surface most
  3. Because it becomes longwave in atmosphere
  4. Because it becomes salt in ocean
Medium · Level 7
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  1. Absorbed energy remaining after reflection
  2. Total reflected energy
  3. Only lunar energy
  4. Only sound energy
Medium · Level 7
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  1. It absorbs terrestrial longwave energy
  2. It creates solar energy
  3. It changes Earths axis
  4. It always makes reflection zero
Medium · Level 7
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  1. Absorption of longwave terrestrial radiation
  2. Complete reflection of solar energy from surface
  3. Height of sea waves
  4. Formation of soil colour
Medium · Level 7
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  1. It explains thermal conditions through energy input output and distribution
  2. It only tells direction of rivers
  3. It only tells mountain height
  4. It only corrects language spelling
Medium · Level 7
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  1. Solar energy arrives some is reflected some is absorbed and Earth returns longwave energy
  2. First terrestrial energy arrives then the Sun forms
  3. All energy remains permanently locked in clouds
  4. Solar energy returns only as sound
Medium · Level 7
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  1. The surface absorbs it and re-emits longwave heat
  2. The Sun immediately cools down
  3. Radiation directly turns into water
  4. Air turns it into rock
Medium · Level 7
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  1. Incoming energy absorbed by Earth and energy leaving for space are unequal
  2. Incoming solar energy and reflected solar energy are equal
  3. Heat being transferred in the atmosphere only by convection
  4. All parts of Earth being at the same temperature

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