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The ionosphere

  • Asgeir Brekke
Chapter
Part of the Springer Atmospheric Sciences book series (SPRINGERATMO)

Abstract

The existence of an ionized layer in the upper atmosphere was probably already appreciated at the beginning of the last century when Marconi demonstrated that radiowaves could propagate across large distances beyond the free horizon, as if they were guided between a conducting layer and the ground. A conducting layer in the upper atmosphere was also inferred as early as 1880 when studies of diurnal oscillations in the Earth’s magnetic field indicated that these variations might be caused by tidal oscillations in the upper atmosphere.

Keywords

Nitric Oxide Total Electron Content Zenith Angle Scale Height Neutral Atmosphere 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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Copyright information

© Springer-Verlag GmbH Berlin Heidelberg 2013

Authors and Affiliations

  • Asgeir Brekke
    • 1
  1. 1.Department of Physics and TechnologyUniversity of TromsøTromsøNorway

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