For the sets of magnetic clouds studied in this work we have shown the
existence of a relationship between their peak magnetic field strengt
h and peak velocity values, with a clear tendency that clouds which mo
ve at higher speeds also possess higher core magnetic field strengths.
This result suggests a possible intrinsic property of magnetic clouds
and also implies a geophysical consequence. The relatively low field
strengths at. low velocities is presumably the cause of the lack of in
tense storms during low speed ejecta. There is also an indication that
this type of behavior is peculiar for magnetic clouds, whereas other
types of non cloud-driver gas events do not seem to show a similar rel
ationship, at least for the data studied in this paper. We suggest tha
t a field/speed relationship for magnetic clouds, as that obtained in
our present study, could be associated with the cloud release and acce
leration mechanism at the sun. Since for magnetic clouds the total fie
ld tyically has a substantial southward component, B-s, our results im
ply that the interplanetary dawn-dusk electric field, given by v x B-s
(where v is the cloud's velocity), is enhanced by both factors. There
fore, the consequent magnetospheric energization (that, is governed by
this electric field) becomes more efficient for the occurrence of mag
netic storms.