If net radiation is high at a place during daytime what will generally happen at the surface?
Higher net radiation provides more energy to the surface. Link net radiation with surface heating in exams.
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SubjectsGeography
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
Up to 16 questions from this page. Select your focus, then start.
Higher net radiation provides more energy to the surface. Link net radiation with surface heating in exams.
On a clear night clouds are fewer and longwave energy escapes easily. Link clear nights with radiational cooling in exams.
During day clouds send part of solar energy back to space. Remember daytime cloud effect as reflection in exams.
Clouds can send part of terrestrial radiation back toward the surface. Link nighttime cloud effect with counter radiation in exams.
Solar energy is affected by atmospheric processes before reaching the surface. Treat surface energy as modified solar energy in exams.
Long term balance keeps Earths average temperature stable. Link heat budget with temperature stability in exams.
In the common model thirty five reflection and sixty five absorption are balanced by total hundred units returned. Remember the three numbers together.
Absorbed sixty five units are balanced by sixty five units of heat output over long time. Keep absorption and heat output equal in exams.
Reflected energy does not heat Earth so it is counted in total outgoing. Treat reflected and emitted energy as outgoing components.
Energy that is not reflected and is absorbed is the real energy gain of the Earth system. Link energy gain with absorption in exams.
Water vapour traps longwave energy and takes part in re radiation. Treat water vapour as a heat trapping gas in exams.
Carbon dioxide is a greenhouse gas that can absorb terrestrial energy. Understand it as a longwave absorber in exams.
Temperature and climate are deeply linked with energy balance. Treat heat budget as a basic climate concept in exams.
Heat budget is the full chain of incoming reflection absorption and outgoing energy. Write answers in this sequence in exams.
Most incoming solar energy reaches Earth as relatively shortwave radiation. Land and water absorb part of it, increasing their internal energy and temperature. The warmed surface then emits energy as longer-wave infrared radiation. Greenhouse gases can absorb some of this outgoing radiation and re-emit it.
Thermal or radiative balance exists when the Earth–atmosphere system absorbs approximately as much energy as it sends back to space. An imbalance occurs when incoming absorbed energy and outgoing energy are unequal. A positive imbalance stores heat and raises temperature, while a negative imbalance causes cooling. Option B describes balance, not imbalance.
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