Plasmaspheric storm time erosion

Unusually low whistler mode group delay times are observed by VLF Doppler receivers at both Faraday, Antarctica, and Dunedin, New Zealand, following magnetic storms. These are typically caused by plasmaspheric electron concentration depletions near L=2.4 and not by changes in the VLF wave propagatio...

Full description

Bibliographic Details
Published in:Journal of Geophysical Research: Space Physics
Main Authors: Clilverd, Mark A., Jenkins, Barbara, Thomson, Neil R.
Format: Article in Journal/Newspaper
Language:unknown
Published: American Geophysical Union 2000
Subjects:
New Zealand
Sheffield
Faraday
Antarc*
Antarctica
Online Access:http://nora.nerc.ac.uk/id/eprint/20453/
https://doi.org/10.1029/1999JA900497

Similar Items