Atmospheric Ray Tracing for Predicting Mirages.

Abstract

At infrared-optical frequencies the Edlen formula determines the index of refraction profile in a continuous, spherically symmetric atmosphere in terms of the pressure and temperature. Since the pressure dependence is known in terms of the temperature when equilibrium exists, a given temperature profile determines that of the index of refraction. The classical equation for rays propagating in such a medium then provides various geometrical properties of a ray, given its nearest minimum or maximum height relative to a specified viewing eye through which it passes. For altitudes above the surface of the Earth that are small compared to its radius the propagation geometry can be approximated in terms of a plane stratified medium above a flat ground surface. However, for distances large enough to include a horizon ray, a single corresponding approximate index of refraction profile is only valid for predicting the behavior of nearby rays. The slope of the index of refraction profile as well as that of the temperature determine the sign of the curvature of any ray at any height. Using the relationship between geometrical properties of the index of refraction profile it is possible to draw qualitative conclusions about the nature of possible mirages.

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Document Details

Document Type
Technical Report
Publication Date
May 01, 1995
Accession Number
ADA316593

Entities

People

  • Irvin W. Kay

Organizations

  • Institute for Defense Analyses

Tags

Communities of Interest

  • Air Platforms
  • Sensors

DTIC Thesaurus Topics

  • Altitude
  • Atmospheric Temperature
  • Barometric Pressure
  • Cartesian Coordinates
  • Coordinate Systems
  • Curvature
  • Differential Equations
  • Equations
  • Geometry
  • Lapse Rate
  • Physical Properties
  • Ray Tracing
  • Refraction
  • Refractive Index
  • Temperature Inversion
  • Two Dimensional
  • Water Vapor

Fields of Study

  • Physics

Readers

  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.
  • Wave Propagation and Nonlinear Chaotic Dynamics.