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 be...

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Bibliographic Details
Published in:Annales Geophysicae
Main Authors: Kosch, M. J., Hagfors, T., Schlegel, K.
Format: Article in Journal/Newspaper
Language:English
Published: Springer Verlag 1998
Subjects:
Online Access:https://doi.org/10.1007/s00585-998-0583-y
https://noa.gwlb.de/receive/cop_mods_00037304
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00037258/angeo-16-583-1998.pdf
https://angeo.copernicus.org/articles/16/583/1998/angeo-16-583-1998.pdf