Ja. Sauvaud et al., LARGE-SCALE DYNAMICS OF THE MAGNETOSPHERIC TAIL INDUCED BY SUBSTORMS - A MULTISATELLITE STUDY, Journal of Geomagnetism and Geoelectricity, 48(5-6), 1996, pp. 675-686
The large scale dynamics of the tail during substorms are examined usi
ng multi-satellite measurements made between 18 and 22:00 UT on August
22, 1983. We use data from ISEE1/2, 1977-007, IMP-8, and ISEE-3 locat
ed in the solar wind or tail at distances along the Sun-Earth line ran
ging from +11 to -205R(E). During the period studied, which correspond
ed to a southward directed IMF, successive plasma injections were dete
cted at 6.6R(E) first during a general increase of the magnetic field
in the lobe. The magnetic field increase is attributed to an enhanced
reconnection rate, as evidenced by the close relationship between the
tail lobe magnetic energy density and the available Poynting energy in
the solar wind, for near constant solar wind pressure. A Traveling Co
mpression Region (flux rope) was detected in close association with th
e first energetic particle injection at geostationary orbit. After the
first injections, the series of injections continued and the last one
s are shown to be linked with a tailward propagating cross-tail curren
t disruption detected onboard IMP-8 at similar to 35R(E). This event i
s seen in the distant tail at 205R(E) onboard ISEE-3 as an increase of
the tail radius; the far magnetosphere engulfed the ISEE-3 satellite
which was located in the solar wind prior to the event. The characteri
stic time delay between cross-tail current disruption onset occurring
in the near-Earth plasma sheet and the enhancement of the tail diamete
r at 205R(E) is on the order of 40 minutes. Several hours before this
event, a similar case was detected in which partial cross-tail current
disruption in the mid-tail was also related to a far tail expansion.
In both cases, the observed signatures are in agreement with the conce
pt of the ejection of plasmoids from the magnetospheric tail with velo
cities comparable to that of the solar wind. These results strongly su
ggest that traveling cross-tail current disruption and plasmoid ejecti
on from the far tail are the signature of the same propagating plasma
process.