Accession Number : ADP005693
Title : Magnetospheric Control of the Bulk Ionospheric Plasma,
Corporate Author : UTAH STATE UNIV LOGAN CENTER FOR ATMOSPHERIC AND SPACE SCIENCES
Personal Author(s) : Sojka, J. J. ; Schunk, R. W.
Report Date : MAY 1987
Pagination or Media Count : 14
Abstract : The temperature, composition, and circulation of the high latitude, ionosphere display a marked variation with altitude, latitude, longitude, universal time, season, solar cycle, and geomagnetic activity. This variation is largely a consequence of the effect that magnetospheric electric fields, particle precipitation, and heat flows have on the ionosphere. At F-region altitudes, the entire ionosphere drifts in response to magnetospheric electric fields, with the horizontal drift generally displaying a two-cell pattern of antisunward flow over the polar cap and return flow at lower latitudes. This ionospheric motion, in combination with downward magnetospheric heat flows and ion production due to energetic particle precipitation, act to produce interesting ionospheric features such as ion and electron temperature hot spots, plasma blobs, localized ionization troughs, and extended tongue of ionization, and anomalous F-region peak altitudes and densities. The time delay for the ionosphere to respond to changing magnetospheric conditions is a strong function of altitude and can be as long as 3 to 4 hours in the upper F-region. The ionosphere's response to changing magnetospheric conditions are described using a time-dependent high latitude ionospheric model.
Descriptors : *IONOSPHERE, *MAGNETOSPHERE, INTERACTIONS, ELECTRIC FIELDS, HEAT TRANSFER, DRIFT, IONS, F REGION, ELECTRON ENERGY, ANOMALIES, DELAY, ATMOSPHERIC MOTION, IONOSPHERIC MODELS, TEMPERATURE, IONIZATION, SPATIAL DISTRIBUTION, POLAR CAP, HIGH LATITUDES, VARIATIONS, ALTITUDE.
Subject Categories : Atmospheric Physics
Distribution Statement : APPROVED FOR PUBLIC RELEASE