Quiet time plasmaspheric electric fields and plasmasphere-ionosphere coupling fluxes at L = 2.5

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Earth Ionosphere, Magnetosphere-Ionosphere Coupling, Plasma Drift, Plasmasphere, Whistlers, Atmospheric Electricity, Diurnal Variations, Geomagnetism, Very Low Frequencies

Scientific paper

Observations of whistler mode signals from VLF transmitters in the northeast U.S. are obtained in order to determine radial plasma drifts and plasmasphere-ionosphere coupling fluxes near L = 2.5. Data from nine geomagnetically quiet days in July, 1986 were used to find the diurnal variation in the east-west electric field. The most significant features in the cross L-drift were an outward drift and an inward drift, both of which had electric fields of magnitude of about 0.2 mV/m.

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