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Astronomical and Actinometric Values of Standard Atmospheric Transmittance

  • K. S. Shifrin
  • G. L. Shubova

Abstract

Analysis of data on the optical properties of the real cloudless atmosphere allowed us to propose as a standard of average conditions the Shifrin-Minin radiation model of the atmosphere [1]. With this model, we can calculate all of the necessary characteristics of the radiation field using the values of only three parameters: the optical thickness of the atmosphere τo for a given wavelength, the meteorological visibility So for the same wavelength, and the amount of precipitated water W. The radiation field is very sensitive to τo, which characterizes the aerosol turbidity of the atmosphere.

Keywords

Radiation Field High Transmittance Optical Thickness Vertical Transmittance Precipitate Water 
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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Literature Cited

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    K. S. Shifrin and I. N. Minin, “Toward a theory of nonhorizontal visibility,” Trudy GGO, No. 68 (1957).Google Scholar
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    K. S. Shifrin and G. L. Shubova, “Statistical variability of vertical atmospheric transmittance,” Izv. Akad. Nauk SSSR, sergiya geofiz., No. 2 (1964).Google Scholar
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Copyright information

© Consultants Bureau, New York 1970

Authors and Affiliations

  • K. S. Shifrin
  • G. L. Shubova

There are no affiliations available

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