We use three observed coronal mass ejection (CME) events and numerical magn
etohydrodynamic simulation models to illustrate three distinct CME initiati
on processes: (1) streamer destabilization due to increase of currents, via
increase of axial fields, of the flux-rope, (2) photospheric shear and (3)
plasma flow induced CME. The 3 January 1998 event is used to illustrate th
e streamer destabilization process to initiate a CME because the observed h
eight-time curve indicates that the prominence eruption proceeds the CME in
itiation. We interpret this CME as being initiated because of destabilizati
on of the streamer due to the upward motion of the flux-rope by the additio
nal Lorentz (J x B) force. On the other hand, the 22 June 1998 event shows
that the CME was launched prior to the prominence eruption. This case is mo
deled by shear-induced loss-of-equilibrium The last case is entirely differ
ent from the previous two. The morphology of the 5 October 1996 event does
not show any relation with the filament/flux-rope. We modeled this event by
introducing a plasma flow. Using the observations and MHD models, we concl
ude that the first two categories are flux-rope driven, because the energy
source, which propels the CME, is stored in the flux-rope, and the third ca
tegory is driven by an assumed plasma flow with the effects of fast solar w
ind, because this CME appears at the boundary region of a streamer and coro
nal hole. (C) 2000 Elsevier Science Ltd. All rights reserved.