A COMPARISON OF THE OCCURRENCE OF VERY-LOW-LATITUDE PI-2 PULSATIONS WITH MAGNETIC-FIELD AND ENERGETIC-PARTICLE FLUX VARIATIONS (30-300 KEV)AT GEOSYNCHRONOUS ALTITUDES
O. Saka et al., A COMPARISON OF THE OCCURRENCE OF VERY-LOW-LATITUDE PI-2 PULSATIONS WITH MAGNETIC-FIELD AND ENERGETIC-PARTICLE FLUX VARIATIONS (30-300 KEV)AT GEOSYNCHRONOUS ALTITUDES, Journal of Geomagnetism and Geoelectricity, 48(11), 1996, pp. 1431-1441
The occurrence of Pi 2 pulsations (20-150 s) at very-low-latitude stat
ions is compared with the energetic-particle and magnetic-field variat
ions at geosynchronous orbit during the PROMIS (Polar Region and Outer
Magnetosphere International Study) period (March 10-June 16, 1986). G
round magnetometer data from Huancayo, Peru (dip equator, 75 degrees W
), and Kuju, Japan (L = 1.2, 135 degrees E), are utilized to monitor t
he magnetic pulsations, while the particles (electron, 30-300 keV; pro
ton, 145-560 keV) and magnetic fields in space are monitored by geosyn
chronous satellites S/C1982-019, S/C1984-129, S/C1984-037, GOES-5, and
GOES-6. Of 175 Pi 2 events surveyed during the PROMIS period, 110 eve
nts are accompanied by electron flux enhancement, and 51 events have a
concurrent onset of the field-aligned current (FAG). The FAC events c
orrelated with ground Pi 2 pulsations indicate a local time change in
polarities. If currents are assumed to flow along the field lines tail
ward of the geosynchronous orbit, the polarities are upward in the pre
midnight sector and downward in the postmidnight sector. We classified
Pi 2 events in the nightside sector in several different ways. The re
sults imply that if Pi 2 events in the present study can be assumed to
be of substorm origin, then 47% of Pi 2 events occur in regions close
to geosynchronous altitude.