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: C.-F. Enell, A. Kero, E. Turunen, Th. Ulich, P. T. Verronen, A. Seppälä, S. Marple, F. Honary, A. Senior
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2005
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Online Access:https://doi.org/10.5194/angeo-23-1575-2005
https://doaj.org/article/4d96442833784a00887664d42dbe43fc