CONCERNING THE ORIGIN OF A THIN, ELEVATED NOCTURNAL FOG LAYER,

Abstract

The heat balance equations of a turbid isothermal layer of air warmer than the ground provided a criterion for calculating the rate of temperature change within this layer under specified conditions.

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Document Details

Document Type
Technical Report
Publication Date
Apr 01, 1967
Accession Number
AD0653166

Entities

People

  • L. M. Roev
  • L. Z. Prokh

Organizations

  • American Meteorological Society

Tags

Communities of Interest

  • Materials and Manufacturing Processes

DTIC Thesaurus Topics

  • Air Force
  • Air Masses
  • Air Temperature
  • Atmospheric Condensation
  • Boundaries
  • Boundary Layer
  • Climate Change
  • Coefficients
  • Condensation
  • Equations
  • Heat Balance
  • Heat Energy
  • Layers
  • Meteorology
  • Radiation
  • United States
  • Water Vapor

Readers

  • Atmospheric Remote Sensing.
  • Thermal Physics or Thermal Science.