THE APPARENT DEPENDENCE OF TERRESTRIAL SCINTILLATION INTENSITY UPON ATMOSPHERIC HUMIDITY.
Abstract
Observations indicate a direct relationship between terrestrial scintillation intensity and relative humidity (RH). A developed theory supplementing air-refractive and diffractive treatments attributes this increased modulation intensity to water droplets formed either gradually or instantaneously at 70% RH or higher. Modulation at visible wavelengths is attributed to scattering, while spectral absorption causes far-infrared-wavelength modulation. The report contains limited experimental substantiation of this theory. A comparative discussion of atmosphere opacity at far-infrared wavelengths (10-micron region) under high- and low-humidity conditions is presented. An empirical equation for determination of the 'scintillation intensity index' is presented, with graphical presentations of conclusions. (Author)
Document Details
- Document Type
- Technical Report
- Publication Date
- Nov 01, 1965
- Accession Number
- AD0630117
Entities
People
- Hugh R. Carlon
Organizations
- Edgewood Chemical Biological Center