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Atmospheric Transmission

  • Mikaél’ A. Bramson
Part of the Optical Physics and Engineering book series (OPEG)

Abstract

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].

Keywords

Water 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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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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