a case study of storm commencement and recovery plasmaspheric electric fields near l=2.5 at equinox
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ID: 241656
1994
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Abstract
Data from the VLF Doppler experiment at
Faraday, Antarctica (65° S, 64° W) are used to study the penetration of the
high-latitude convection electric field to lower latitudes during severely
disturbed conditions. Alterations of the electric field at L-values
within the range 2.0 - 2.7 are studied for two cases at equinox (10 - 12
September 1986 and 1 - 3 May 1986). The recovery of the electric field is found
to be approximately an exponential function of time. Values for the equatorial
meridional E×B drift velocity, inferred from
the data, are used as inputs to a model of the plasmasphere and ionosphere. The
model and experimental results are used to investigate the post-storm alteration
of ionospheric coupling processes. The magnitude of the effect of ionosphere-plasmasphere
coupling fluxes on NmF2 values and the O+-H+
transition height is dependent on the local time of storm commencement, and on
the orientation of the electric field. The coupling fluxes appear to have a
maximum influence on ionospheric content during the main phase of geomagnetic
activity that produces outward motion of plasmaspheric whistler ducts.
| Reference Key |
balmforth1994annalesa
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|---|---|
| Authors | ;H. F. Balmforth;M. A. Clilverd;A. J. Smith |
| Journal | journal of food measurement and characterization |
| Year | 1994 |
| DOI |
10.1007/s00585-994-0625-z
|
| URL | |
| Keywords |
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