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“atmospheric attenuation”
atmospheric attenuation
1. A process in which the flux density of a parallel beam of energy decreases with increasing distance from the source as a result of absorption or scattering by the atmosphere.
2. The depletion of electromagnetic energy in the atmosphere because of absorption or diffusion.
2. The depletion of electromagnetic energy in the atmosphere because of absorption or diffusion.
This entry is located in the following units:
atmo-, atm- +
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sphero-, spher-, -sphere- +
(page 2)