Question about the Spectrum of Radiation Reaching the Earth

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SUMMARY

The discussion focuses on the spectrum of electromagnetic (EM) radiation that reaches the Earth's surface, emphasizing the predominance of visible light. Visible light, particularly wavelengths around 400nm, penetrates the atmosphere more effectively than gamma rays or longer wavelengths due to specific atmospheric transparency windows. These windows primarily exist in the optical, infrared, and radio ranges, allowing certain wavelengths to reach the surface while others are absorbed. The interaction of EM radiation with atmospheric gases, such as ionization by X-rays and gamma rays versus energy absorption by rotational and vibrational modes of N2 and O2, explains these phenomena.

PREREQUISITES
  • Understanding of electromagnetic radiation and its spectrum
  • Familiarity with atmospheric science and composition
  • Knowledge of the interaction between radiation and matter
  • Basic principles of ionization and energy absorption
NEXT STEPS
  • Research the properties of electromagnetic radiation, focusing on the visible spectrum
  • Study the Earth's atmospheric composition and its effects on radiation absorption
  • Explore the concept of atmospheric transparency windows in detail
  • Investigate the mechanisms of energy absorption in gases, particularly N2 and O2
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Students and professionals in atmospheric science, physicists studying electromagnetic radiation, and educators explaining the principles of light and its interaction with the Earth's atmosphere.

Simon777
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Radiation with a wavelength in the visible light range is what mainly reaches the Earth's surface.

What is so special about visible light that makes it so easy to reach the surface compared to something like gamma rays with a smaller wavelength or something with a larger wavelength?

Also, why does light near the 400nm range reach the Earth in greater amounts than light near the 700nm range?
 
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The Earth's atmosphere absorbs most wavelengths of EM radiation before they reach the surface. There are certain 'windows' where the atmosphere is relatively transparent. These are mainly in the optical, the infrared,and the radio. This site has a nice plot of where the atmosphere is transparent:

http://en.wikipedia.org/wiki/Optical_window

As to why the Earth's atmosphere is transparent in this range, it is a relatively complex subject of how EM radiation interacts with matter, and what the Earth's atmosphere is made of. For example, X-rays and gamma rays are energetic enough to ionize the gas atoms in the atmosphere, so they lose energy as they ionize the gas atoms along their track until ultimately the energy is all absorbed. By contrast, long-wave infrared radiation is not energetic enough to ionize the gas atoms, but it can excite rotational and vibrational modes of the N2 and O2 gas molecules, and the energy is absorbed in this way.
 

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