Dn. Baker et al., CORONAL MASS EJECTIONS, MAGNETIC CLOUDS, AND RELATIVISTIC MAGNETOSPHERIC ELECTRON EVENTS - ISTP, J GEO R-S P, 103(A8), 1998, pp. 17279-17291
The role of high-speed solar wind streams in driving relativistic elec
tron acceleration within the Earth's magnetosphere during solar activi
ty minimum conditions has been well documented. The rising phase of th
e new solar activity,cycle (cycle 23) commenced in 1996, and there hav
e recently been a number of coronal mass ejections (CMEs) and related
''magnetic clouds'' at 1 AU. As these CME/cloud systems interact with
the Earth's magnetosphere, some events produce substantial enhancement
s in the magnetospheric energetic particle population while others do
not. This paper compares and contrasts relativistic electron signature
s observed by the POLAR, SAMPEX, Highly Elliptical Orbit, and geostati
onary orbit spacecraft during two magnetic cloud events: May 27-29, 19
96, and January 10-11, 1997. Sequences were observed in each case in w
hich the interplanetary magnetic field was first strongly southward an
d then rotated northward. In both cases, there were large solar wind d
ensity enhancements toward the end of the cloud passage at 1 AU. Stron
g energetic electron acceleration was observed in the January event, b
ut not in the May event. The relative geoeffectiveness for these two c
ases is assessed, and it is concluded that large induced electric fiel
ds (partial derivative B/partial derivative t) caused in situ accelera
tion of electrons throughout the outer radiation zone during the Janua
ry 1997 event.