Atmospheric Transmission

  • Mikaél’ A. Bramson
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].


Water Vapor Attenuation Coefficient Infrared Radiation Condensed Vapor Atmospheric Transmission 
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Copyright information

© Springer Science+Business Media New York 1968

Authors and Affiliations

  • Mikaél’ A. Bramson
    • 1
  1. 1.Institute of Mineral FuelsAcademy of Sciences of the USSRMoscowUSSR

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