Effects of D-region RF heating studied with the Sodankylä Ion Chemistry model

The upper mesosphere and lower thermosphere, or ionospheric D region, is an atmospheric layer which is difficult to access experimentally. A useful method that also has a large potential for further studies is artificial heating of electrons by means of powerful radio transmitters. Here we estimate...

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Bibliographic Details
Published in:Annales Geophysicae
Main Authors: Enell, C.-F., Kero, A., Turunen, E., Ulich, Th., Verronen, P. T., Seppälä, A., Marple, S., Honary, F., Senior, A.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/angeo-23-1575-2005
https://angeo.copernicus.org/articles/23/1575/2005/