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Unit 8 Earth in Space Solar Energy
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Energy From the Sun At Sun’s core: Hydrogen atoms fuse to make helium releasing HUGE amounts of energy Electromagnetic Spectrum: the energy that is radiated from the sun
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Energy Multiple nuclei are joined; large amount of energy released; i.e. solar energy A heavy nucleus is split to make smaller nuclei; large amount of energy released; i.e. nuclear power A chemical process where whole atoms recombine; small amount of energy released; i.e. burning fossil fuels Nuclear Fusion Nuclear Fission Combustion
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Why do Nuclear Reactions yield so much Energy?
Energy released (E) is equal to change in mass (m) times the speed of light (c = 3x108 m/s) E = mc2 Nuclear reactions release so much energy because there is a change in mass. There is NO change in mass in chemical combustion.
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Energy occurs in 3 forms:
Solar Energy Heat Energy Chemical Energy Solar energy is converted to heat & chemical energy when it reaches Earth Only 50% of all solar energy reaches Earth
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Solar Energy (electromagnetic radiation) travels as transverse waves.
Frequency (f) = 1 / wavelength (λ) Wavelength Shorter wavelength Higher frequency Higher energy Longer wavelength Lower frequency Lower energy
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Radiation from the Sun occurs in different forms identified by wavelength:
Gamma Ray Radio Micro wave Visible X Ray UV Infrared
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Electromagnetic Spectrum
Figure 1
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Insolation: The amount of solar energy received on Earth per unit of area per time. The amount received depends on the angle that the electromagnetic wave strikes Earth, which depends on: Time of year Location on Earth
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More direct rays lead to more insolation: Polar insolation is less than Equatorial insolation
Maximum insolation occurs in the visible light spectrum Greater insolation supports more photosynthesis and more plant growth
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Insolation Closer to poles, rays have more angle, rays are more diffuse, insolation is lower Figure 3 At the equator, rays have less angle, rays are more concentrated, insolation is higher
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Figure 5 Figure 4 Figure 2
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