HR: 1340h
AN: SM43A-1152 [Abstracts]
TI: The Spatial Distribution of the Io Plasma Torus
AU: * Herbert, F
EM: herbert@vega.LPL.arizona.edu
AF: Lunar and Planetary Lab
University of Arizona, Sonett Space Science Bldg
1541 East University Blvd, Tucson, AZ 85721-0063
United States
AU: Schneider, N M
EM: nick.schneider@lasp.colorado.edu
AF: Laboratory for Astophysics and Space Science
University of Colorado, Campus Box 392, Boulder, CO 80309-0392
United States
AU: Dessler, A J
EM: dessler@vega.LPL.arizona.edu
AF: Lunar and Planetary Lab
University of Arizona, Sonett Space Science Bldg
1541 East University Blvd, Tucson, AZ 85721-0063
United States
AB:
Ground-based coronographic images of the Io plasma torus in
S$^+$~6371\AA\ emission have been pseudo-tomographically deconvolved
from their inherent line-of-sight integration, yielding
estimates of their three-dimensional (3D)
S$^+$\ density distributions with spatial resolution of
$\sim$0.05$R_{\mbox{\rm \scriptsize J}}$.
By interpreting this derived time-dependent structure we can infer
some of the characteristics of torus formation mechanisms.
For example, the dawn-to-dusk electric field in the torus region
of Jupiter's magnetosphere causes the warm outer torus
(including the ``ribbon'' feature) and the outer edge of the cold torus
(which is the innermost region of the torus) to
move closer to Jupiter by $\sim$0.3$R_{\mbox{\rm \scriptsize J}}$\ as
the torus plasma rotates from the dawn region to dusk.
Although this electric field is often approximated as spatially
uniform, the initial analyses of these and other observations
(Dessler and Sandel, {\em GRL 19}:2099, 1992;
Schneider and Trauger, {\em ApJ 450}:450, 1995) implied a variation of
the field strength with subsolar magnetic longitude.
Now, preliminary results of our analyses of these observations imply
differential motion between the inner and outer edges of the cold
torus, indicating that the field strength varies spatially as well,
appearing at times to diminish at the inner edge of the cold torus.
Such behavior can result from a process known as magnetospheric
``shielding'', which has been noted in the magnetospheres of Earth and
possibly Uranus but this would be the first instance where it has been
seen at Jupiter.
This and other anomalies of torus structure, such as
the difference in magnetic latitudes of the warm and cold tori and
the large gap between them, will be discussed at the meeting.
This work was supported by NASA under grants NAG5-12944 and 9079
(Geospace Sciences Program) and NAG5-8952 (Planetary Atmospheres
Program).
DE: 5737 Magnetospheres (2756)
DE: 5757 Remote sensing
DE: 5780 Tori and exospheres
DE: 2732 Magnetosphere interactions with satellites and rings
DE: 2740 Magnetospheric configuration and dynamics
SC: SPA-Magnetospheric Physics [SM]
MN: 2004 AGU Fall Meeting