O. Le Contel et al., Possible control of plasma transport in the near-Earth plasma sheet via current-driven Alfven waves (f similar or equal to f(H+)), J GEO R-S P, 106(A6), 2001, pp. 10817-10827
Two time periods, each covering both quiet and disturbed conditions (growth
phase, breakup, and postbreakup phase), are studied. Electric and magnetic
field measurements, carried out in the near-Earth plasma sheet (NEPS), are
used to calculate the two components (radial and azimuthal) of the electri
c E x B/B-2 drift. These calculations are compared with independent estimat
es of the ion flow direction deduced from ion flux measurements. During act
ive periods, the two flow directions coincide to a large degree. Evidence i
s given for two regimes of transport: (1) During the growth phase, and afte
r the active phase, the electric field (radial and azimuthal) and hence the
azimuthal and radial flow velocities are small in the near-equatorial regi
on. This is interpreted as the consequence of an electrostatic field that t
ends to shield the induced electric field associated with time-varying exte
rnal conditions. (2) During active chases (breakup and pseudobreakup), howe
ver, large-amplitude bursts in E x B/B-2 radial and azimuthal components (i
nterpreted as how bursts), with typical velocities of the order of 100 kms(
-1), are observed. The direction of these flow bursts is somewhat arbitrary
, and in particular, for the two substorm events described here, sudden rev
ersals in the flow direction are observed. These fast flow bursts coincide
with intense low-frequency electromagnetic fluctuations: current-driven Alf
ven waves (CDA waves) with frequency f similar or equal to f(H+), the proto
n gyrofrequency. CDA waves produce "anomalous" collisions on timescales sho
rter than the electron bounce period, thus violating the second adiabatic i
nvariant for electrons. As a consequence, the electrostatic shielding is de
stroyed, which leads to enhanced radial transport. Thus the transport in th
e NEPS seems to be controlled by a microscopic current-driven instability.