MODIFICATION OF THE IONOSPHERE BY RADIOWAVES

Abstract

A theoretical model is presented for calculating the heating and hydrodynamic expansion of the F-layer of the ionosphere due to an incident radiowave. We find that the greatest effects occur for transmitter frequencies just above the critical frequency of the F-layer. Using a power aperture product of 1,000 sq megawatt-meter, which corresponds to a projected experiment by ESSA at Boulder, Colorado, we find a maximum increase in the electron temperature at the peak of the F-layer of about thirty percent with a reduction in the electron density of about ten percent. The time scale for achieving the density changes is predicted to be about one-half hour to an hour.

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Document Details

Document Type
Technical Report
Publication Date
Jun 01, 1969
Accession Number
AD0689662

Entities

People

  • R. E. Lelevier

Organizations

  • RAND Corporation

Tags

Communities of Interest

  • Advanced Electronics
  • Energy and Power Technologies

DTIC Thesaurus Topics

  • Climate Change
  • Collisions
  • Colorado
  • Dielectric Permittivity
  • Difference Equations
  • Differential Equations
  • Electromagnetic Fields
  • Electron Density
  • Electron Gas
  • Electrons
  • Equations
  • Frequency
  • Magnetic Fields
  • Partial Differential Equations
  • Steady State
  • Transmitters
  • United States

Fields of Study

  • Physics

Readers

  • Mathematics or Statistics
  • Solar Physics
  • Space/Atmospheric Physics.

Technology Areas

  • Microelectronics