Low-altitude convection, precipitation, and current patterns in the baseline magnetosphere

Details Low-altitude convection, precipitation, and current patterns in the baseline magnetosphere Low-altitude convection, precipitation, and current patterns in the baseline magnetosphere

Nov 1988

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1988rvgeo..26..792g&link_type=abstract

Reviews of Geophysics (ISSN 8755-1209), vol. 26, Nov. 1988, p. 792-808.

Physics

Geophysics

30

Convection Currents, Earth Magnetosphere, Geomagnetism, Magnetic Variations, Particle Precipitation, Auroral Zones, Electric Fields, Electron Precipitation, Field Aligned Currents, Polar Caps

Scientific paper

Various states of the magnetosphere are examined to determine a set of conditions for the baseline (quiet) magnetosphere and to show that these conditions are regularly met. The low-altitude morphology of the convection electric field, precipitating particles, and field-aligned currents are reviewed for the case where the baseline magnetosphere is well defined by the lowest intensities of each of these quantities. Consideration is given to the study of cusp entry, steady convection, and open and closed field lines, under baseline conditions.

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