Jupiter (Planet) -- Photographs from space; Jupiter probes; Voyager Project
At about 5 a.m. on March 8, Voyager had taken a historic picture.
Looking back at a crescent Io from a distance of 4.5 million kilometers,
the camera had been used to obtain a long-exposure view for the
spacecraft navigation team—one that showed the satellite against the
field of background stars. During the day, Linda Morabito, an optical
navigation engineer, began to work with this picture on her
computer-controlled image display. She noted what appeared to be a
crescent cloud, extending beyond the edge of Io. But Io has no
atmosphere, so a cloud rising hundreds of kilometers above the surface
did not seem to make sense.
The next day, working with her colleagues, Morabito eliminated all
possibilities for the new feature on Io except the obvious—a cloud. If
it were a cloud, it must be the result of an ongoing volcanic eruption
of incredible violence. The picture was shown to members of the Imaging
Team, who agreed with the identification. But it was Friday and Brad
Smith and Larry Soderblom, along with most of the other team members,
had left for the weekend to try to get some rest. The picture would have
to wait two more days.
HIGHLIGHTS OF THE VOYAGER 1 SCIENTIFIC FINDINGS[2]
Atmosphere
Uniform wind speeds for cloud features with widely different size
scales, suggesting that mass motion and not wave motion is being
observed.
Rapid formation and spreading of bright cloud material, perhaps the
result of disturbances that trigger convective activity.
A pattern of east-west winds in the polar regions, previously thought to
have been dominated by convective upwelling and downwelling.
Anticyclonic motion of material associated with the Great Red Spot, with
a rotational period of about six days.
Interactions of smaller spots with the Great Red Spot and with each
other.
Auroral emissions in the polar regions, both in the ultraviolet (which
were not present during the 1973 Pioneer encounter) and in the visible.
Cloud-top lightning bolts, similar to terrestrial superbolts, and
meteoritic fireballs.
A temperature inversion layer in the stratosphere and a temperature of
160 K at the level at which the atmospheric pressure is 0.01 bar.
Very strong ultraviolet emission from the disk, indicating a
thermospheric temperature of more than 1000 K.
A hot (1100 K) upper ionosphere on the dayside that was not observed by
Pioneer 10, suggesting there may be large temporal or spatial changes.
An atmospheric composition with volume fraction of helium of 0.11 ±
0.03.
A substantially colder atmosphere above the Great Red Spot than in the
surrounding regions.
Satellites and Rings
At least eight currently active volcanoes on Io, probably the result of
tidal heating of the interior of the satellite, with plumes extending up
to 250 kilometers above the surface.
A large hot spot on Io near the volcano Loki that is about 150 K warmer
than the surrounding surface.
Public-domain text, read in full here on John Shaqi.
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