Part of the Optical Physics and Engineering book series (OPEG)
Transmittance of the atmosphere as a function of optical density: T =10-hm=10-d, where h is the mass attenuation coefficient [cm-1] and m is the reduced mass of water vapor [cm].
KeywordsWater Vapor Attenuation Coefficient Infrared Radiation Condensed Vapor Atmospheric Transmission
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.
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