Extrapolating EISCAT Pedersen conductances to other parts of the sky using ground-based TV auroral images

Ionospheric conductivity is not very easily measured directly. Incoherent scatter radars perhaps offer the best method but can only measure at one point in the sky at any one time and are limited in their time resolution. Statistical models of average conductivity are available but these may not...

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Bibliographic Details
Main Authors: M. J. Kosch, T. Hagfors, K. Schlegel
Format: Article
Language:English
Published: Copernicus Publications 1998-05-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/16/583/1998/angeo-16-583-1998.pdf