Halo coronal mass ejections (CMEs) had been rarely reported in coronagraph
observations of the Sun before the Solar and Heliospheric Observatory (SOHO
) mission. Since mid-1996, however, the SOHO Large Angle Spectrometric Coro
nagraph (LASCO) instruments have observed many halo or partial-halo CMEs. A
halo CME, especially when associated with solar activity near sun center,
is important for space weather concerns because it suggests the launch of a
potentially geoeffective disturbance toward Earth. During the post-solar m
inimum period from December 1996 to June 1997, we found that all six halo C
MEs that were likely Earthward-directed were associated with shocks, magnet
ic clouds, and moderate geomagnetic storms at Earth 3-5 days later. The res
ults imply that magnetic cloud-like structures are a general characteristic
of CMEs. Most of the storms were driven by strong, sustained southward fie
lds either in the magnetic clouds, in the post-shock region, or both. We di
scuss the characteristics of the halo events observed during this period, t
heir associated signatures near the solar surface, and their usefulness as
predictors of space weather at Earth.