Grade 10 Physics · Strand 4: Environment and Space Physics · Greenhouse Effect and Climate Change
The Natural Greenhouse Effect and Earth's Energy Balance
A short Grade 10 Physics lesson for the CBE curriculum, part of Environment and Space Physics: Greenhouse Effect and Climate Change. Learn it on any phone with notes and slides, then check yourself with a quick quiz and earn XP. This lesson is free.
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3 questions from this lesson’s quiz. Start the lesson to answer them and see the right answers.
1. Why do nitrogen (N_2) and oxygen (O_2) not act as greenhouse gases in Earth's atmosphere?
- A. Their symmetrical diatomic molecules show no change in dipole moment when they vibrate, so they do not absorb infrared
- B. They exist only as liquid droplets in high clouds
- C. They reflect all incoming shortwave radiation before it reaches the surface
- D. Their molecular mass is too small to interact with electromagnetic radiation
2. Which statement correctly compares the radiation that Earth receives with the radiation that Earth's surface emits?
- A. Earth receives mainly shortwave radiation and the warm surface emits longwave infrared
- B. Earth receives mainly longwave infrared and the warm surface emits shortwave radiation
- C. Both the incoming and outgoing radiation are mainly ultraviolet
- D. Both the incoming and outgoing radiation are mainly microwaves
3. At the top of the atmosphere, Earth receives an average of 340 W/m^2 of solar power. About 100 W/m^2 is reflected directly to space. If Earth is in thermal equilibrium, how much power must be emitted as thermal infrared radiation?
Type your answer (in W/m^2) in the lesson.
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