Triggered daytime breakups in the case of the northward IMF

Details Triggered daytime breakups in the case of the northward IMF Triggered daytime breakups in the case of the northward IMF

Apr 1993

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1993ge%26ae..33..150g&link_type=abstract

Geomagnetizm i Aeronomiya (ISSN 0016-7940), vol. 33, no. 2, p. 150-153.

Computer Science

Atmospheric Ionization, E Region, Interplanetary Magnetic Fields, Magnetic Field Reconnection, Polar Cusps, Auroras, Daytime, Particle Precipitation

Scientific paper

The anomalous ionization observed in the E-layer in the region of the near-polar boundary of the daytime cusp in the case of the northward IMF might be caused by the pulsed precipitation of particles during reconnection of the geomagnetic field with the northward IMF. It is shown that in about half the cases an increase in anomalous ionization is observed in the case of a sharp reduction in the magnitude of the northward IMF component or in the case of short Bz less than 0 pulses on the background of the positive direction of the IMF.

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