STABILITY OF ATMOSPHERIC OPTICAL PROPERTIES,

Abstract

The extent of the changes in atmospheric transparency were studied analytically to determine its effect on the optical stability of the atmosphere, given by a stability criterion. A progressive method of measuring the optical properties of the atmosphere is proposed, and a coefficient n is defined as the degree of atmospheric instability. A set of 80 observations was selected over a period of 50 days, 60 of which showed n not exceeding 0.03. It was found that n could vary in a given day (during the observation series) with different filters. This was attributed to the change in aerosol quantity in the atmosphere as well as the aerosol spectra. All data were limited to clear atmospheric conditions with high transparency.

Document Details

Document Type
Technical Report
Publication Date
Aug 18, 1967
Accession Number
AD0667701

Entities

People

  • G. Sh. Livshits

Organizations

  • National Air and Space Intelligence Center

Tags

DTIC Thesaurus Topics

  • Atmospheres
  • Coefficients
  • Instability
  • Observation
  • Optical Properties
  • Photographic Materials
  • Photography
  • Physical Properties
  • Spectra
  • Transparence
  • Transparencies

Fields of Study

  • Environmental science

Readers

  • Mathematics or Statistics
  • Ocean-Atmosphere Mesoscale Modeling, Data Assimilation, and Flux Boundary Layers
  • Optical Physics and Photonics.