The Sensitivity of the Receiver Coherence Diameter and Modulation Transfer Function to Variations of a Damp Unstable Atmosphere

Abstract

The purpose of this study was to examine the sensitivity of the receiver coherence diameter, r sub o, and the modulation transfer function (MTF) to variations of the natural atmosphere from an assumed ideal average state and from misrepresentation of the atmospheric effects due to errors in measurement and processing of the basic meteorological parameters. The concept was simplified by assuming that all natural variations and errors due to sensor performance and positioning can be lumped and that collectively are normally distributed, even though the natural variations are known not to be normal. For this study, the authors selected two sets of data to analyze. The data from Davis, California, were collected during unstable conditions with clear skies. Bar graphs were used to show distributions resulting from total errors. They include the friction velocity u*; windspeed V sub r; temperature scaling parameter T*; specific humidity scaling parameter q*; Obukhov scaling length L; structure parameter (C sub n)sq.; and receiver coherence diameter r sub o. Additionally, the authors take the minimum, maximum, and mean r sub o for each case and plot the resulting near and far-field slow MTF.

Open PDF

Document Details

Document Type
Technical Report
Publication Date
Jul 01, 1992
Accession Number
ADA253269

Entities

People

  • Arnold Tunick
  • Henry Rachele

Tags

Communities of Interest

  • Sensors
  • Space
  • Weapons Technologies

DTIC Thesaurus Topics

  • Artillery
  • Atmospheres
  • Atmospheric Sciences
  • Atmospheric Temperature
  • Boundary Layer
  • California
  • Diameters
  • Far Field
  • Friction
  • Heat Flux
  • Humidity
  • Measurement
  • Military Research
  • Modulation
  • Refractive Index
  • Transfer Functions
  • Warfare

Readers

  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.
  • Computational Modeling and Simulation
  • Fluid Dynamics.