Interaction of plasma cloud with external electric field in lower ionosphere
In the auroral lower-E and upper-D region of the ionosphere, plasma clouds, such as sporadic-E layers and meteor plasma trails, occur daily. Large-scale electric fields, created by the magnetospheric dynamo, will polarize these highly conducting clouds, redistributing the electrostatic potential...
Main Authors: | Y. S. Dimant, M. M. Oppenheim |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2010-03-01
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Series: | Annales Geophysicae |
Online Access: | https://www.ann-geophys.net/28/719/2010/angeo-28-719-2010.pdf |
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