![]() |
||
![]() |
![]() Galileo studies ring-shaped plasma cloud around Jupiter NASA/JPL STATUS REPORT Posted: June 27, 2000
The Extreme Ultraviolet Spectrometer concludes its observation campaign of the Io torus on Friday of this week. The data obtained during this campaign will allow comparison of torus shape and energy output with similar results obtained during the past 4-1/2 years of Galileo's mission at Jupiter. The Io torus is is a ring-shaped cloud of plasma characterized by intense radiation and is of interest because it acts as a source region for much of the plasma that is transported throughout Jupiter's magnetosphere. It is bounded on its inner edge by Io's orbit, is maintained by volcanic activity on Io, and is influenced by Jupiter's strong magnetic field. Data playback also continues this week. During playback, the spacecraft
computer retrieves the data stored on the tape recorder, then processes and
packages the data, and subsequently transmits the data to Earth. The data
returned this week are from Galileo's February 22, 2000 flyby of fiery Io.
The first observation contains data measurements from the Near-Infrared
Mapping Spectrometer (NIMS) and the Photopolarimeter Radiometer (PPR).
This observation captured information on the Prometheus volcanic vent.
Next on the schedule is an observation made primarily by the Solid-State
Imaging camera (SSI), but also containing data gathered by NIMS and PPR.
The observation is of Tohil Mons, one of the mountains on Io, whose
geological structure, origin and history are presently not well known. The
SSI portion of this observation will be combined with an observation taken
in October 1999 in order to produce stereo views of the region. This
week's final observation also contains data from all three instruments, but
is primarily an SSI color mosaic of the Prometheus volcanic region.
|
![]() |
![]() |
![]() |
![]() ![]() ![]() ![]() |
||