Microphysical and Meteorological Measurements of Fog Supersaturation.

Abstract

Liquids, Atmospheric temperature, Profiles, Cooling, Microstructure, Correlation techniquesIt has been surmised that fog supersaturation lies well below a few tenths of one percent, but it cannot be directly measured at present. In this paper, theoretical and empirical equations are developed which render it possible to calculate fog supersaturation from simultaneous microphysical and meteorological measurements at regular time intervals. Such measurements became available on four occasions. With the aid of these equations, comparisons are carried out in terms of several supersaturation parameters, as well as in terms of the change in isobaric cooling. When the nature of the data is taken into consideration, the results of these comparisons appear to lend support to the use of these equations in the calculation of fog supersaturation. (Author)

Document Details

Document Type
Technical Report
Publication Date
Dec 01, 1973
Accession Number
AD0771056

Entities

People

  • Richard D. H. Low

Organizations

  • United States Army Communications-Electronics Command

Tags

DTIC Thesaurus Topics

  • Atmospheric Temperature
  • Equations
  • Intervals
  • Measurement
  • Microstructure
  • Supersaturation
  • Time Intervals

Fields of Study

  • Environmental science

Readers

  • Atmospheric Science/Meteorology
  • Materials Science and Engineering.
  • Regression Analysis.