Question about the Spectrum of Radiation Reaching the Earth

AI Thread Summary
Visible light is primarily what reaches the Earth's surface due to its interaction with the atmosphere, which absorbs most other wavelengths of electromagnetic radiation. Gamma rays and X-rays are absorbed because they can ionize gas atoms, while long-wave infrared radiation is absorbed by exciting molecular vibrations rather than ionization. The atmosphere has specific 'windows' where it is transparent, particularly in the optical, infrared, and radio ranges. Light around 400nm is more prevalent at the surface than light near 700nm due to these atmospheric absorption characteristics. Understanding these interactions is crucial for comprehending the spectrum of radiation that reaches Earth.
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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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