| |
|
Ground-based Images of Io:
| Image Thumbnail |
Title |
 |
Ground
based Adaptive Optics image of Io in daylight, both sides, 3.8 microns
October 20, 1996
Locator
Map |
 |
Ground
based Adaptive Optics image of Io in daylight, both sides, 3.8 microns
October 21, 1996
Locator
Map |
| Caption
for the Above two images. Also take a look at an
article based on these two images. |
| 1998 Keck speckle
images, 0.02"/pixel (0.04" resolution) at 2.2 microns,
showing a transient event near Loki. These are the same pictures Imke
de Pater and Seran Gibbard had with them at the DPS. All images are
displayed on the same (logarithmic) intensity strech. The overlaid
Io disk is only a rough alignment intended as a guideline; precise
image registration is not yet complete. (B. Macintosh, C. Max, D.
Gavel, S. Gibbard (LLNL), I. de Pater (UCB).) |
 |
July
11, 1998 |
 |
July
28, 1998 |
 |
August
4, 1998 |
 |
Groundbased
Adaptive-Optics Image of Io in Eclipse, 2.3 microns
1998/06/03, Christophe Dumas, JPL, Canada-France-Hawaii Telescope
(CFHT), Mauna Kea, "Pueo" adaptive optics system. The
images were recorded through cirrus and the extinction was very
high, about 2 magnitudes. Not too bad considering the conditions!
We also have few 1.7 mic images. The adaptive optics system was
Pueo, the CFHT system in service since summer 97. The camera was
KIR, a 1024x1024 nicmos. Click here
for a different stretch of the same image.
Note the remarkable correspondence with the NICMOS image taken
six weeks later (below), at a shorter wavelength (but note that
the image orientation is different).
|
 |
Io
(in eclipse): Keck speckle.
This is a K' speckle image obtained during the September 6, 1996 eclipse
using the 10-m W.M. Keck telescope. The image scale is 0.02 arcseconds
per pixel; resolution is 0.05 arcseconds FWHM. The image is a speckle
reconstruction of 300 exposures, each 0.15 seconds long. Four real
sources are visible - the bright transient 9608A in the center, Kanehekili
to the left and slightly down, a (presumably transient) source above
Kanehekili, and a dim (K'=14.1) source near the east limb. The latitude/longitude
grid is a preliminary registration and only intended as a rough guide.
The streaks extending from the volcanoes are artifacts of the speckle
process; the image has been displayed on a logarithmic scale to show
the faintest source.
The image was taken and processed by the LLNL speckle imaging group,
Bruce Macintosh, Don Gavel, Seran Gibbard, and Claire Max, together
with Imke de Pater (UC Berkeley) and Andrea Ghez (UCLA). |
 |
Io
(in eclipse) passing Europa (in sunlight): CFHT Adaptive Optics.
97/07/16, 2.26 microns, University of Hawaii adaptive optics system,
Canada-France-Hawaii telescope, Mauna Kea. Very preliminary reduction:
Io has been brightened relative to Europa. Observers: Christophe Dumas,
Francois Roddier, Olivier Hainaut, Laird Close, Buzz Graves, Malcolm
Northcott.
The two bright hot spots on Io are Loki (right) and Kanehekili (left) |
 |
Io (in eclipse) passing Europa
(in sunlight): IRTF Direct Imaging.
16:35 UT, 96/04/24, 3.8, 3.5, and 2.3 microns (R, G, and B respectively),
NSFCAM, IRTF (image taken half an hour after sunrise). Observers:
John Stansberry, Christophe Dumas, and John Spencer.
Io (bottom) is in darkness but shines due to thermal emission from
at least three volcanos. The brightest is Loki (on the right), the
leftmost, faintest, one is probably Kanehekili, and the lowermost
one is unnamed. Europa (top) is in full sunlight but is extremely
dark at these wavelengths due to absorption of the sunlight by water
ice, especially beyond 3 microns, so it is much bluer than Io, and
no brighter. Europa's disk is clearly resolved and shows a hint of
albedo features (?). |
 |
UH
AO Image: Io |
 |
Explanation
map of above
No Caption
|
 |
Keck
image of Tvashtar eruption in Nov. 1999 and Projove hemisphere
No Caption
|
 |
Earth-Based
Observations of a Fire Fountain on Io |
 |
Keck
I AO image of Io in H Band
Io is well known to be the most volcanically active body in the
solar system. The surface of this moon-size satellite of Jupiter
shows some dramatic features produced by the volcanic activity.
Among the most impressive are the thermal emission called hot spots,
creating rapid surface changes, plumes and volcanic features (caldera,
volcanoes..).
On this impressive Keck I AO image, the high spatial resolution
(estimated to 120 km) allows us to see a high number of details.
The intensity contrast over the satellite surface is produced by
the albedo variation of the surface component. On the eastern limb,
close to the equator, two dark area correspond to Pele and Pillan.
The Pillan area has known the largest surface change on Io, observed
by Galileo probe. The dark features, due apparently to lava flows
and detected by Galileo/SSI are clearly visible on this Keck AO
image. Pele area also appears as dark on this H band image due to
the low albedo of the deposit produced by its huge plume, previously
detected on spatial data.
The circular dark area on the other limb of the satellite, reveals
the Prometheus volcano. The largest dark area, located at the north
pole, corresponds to the enigmatic Lei-Kung Fluctus region. This
region is a very large, cool and stable lava flow area produced
by an unknow volcano.
Bright areas on the disk may indicate the presence of deposit of
sulphur dioxide in solid state (frost). Much smaller caldera, visible
on the Voyager image, are also detected on this Keck data.
Note that we do not detect any obvious presence of outburst on the
limb of the satellite as it has been once detected on the Io images
taken during the Keck II AO science verification phase.
Locator
Map - Voyager
image of Area
|
 |
ADONIS AO Image of Io showing 0012A
(Tvashtar) eruption
Example of Io image after deconvolution and subtraction of the
solar emission. The 0012A hot spot is clearly visible at the edge
of the disc (right). Taken on December 16, 2000 at 140 GMT.
Locator
Map - Deconvoluted
Image
|
|
This is from http://astron.berkeley.edu/~fmarchis/Io_OA/Run2000/
Three data sets of Io (composed of 3 or 4 final processed images
in L' band) were taken, for each of them we have a PSF data set.
On the 5 hours of observation, wee can not only determine the center-to-limb
variation of any bright hot spots, but we also increase the spatial
coverage of our survey. After applying a deconvolution process (called
MISTRAL, see Conan et al., SPIE, 4007, 913-924), we can identify
several well-known hot spots. The brightest one on this side seems
to correspond to Loki (309W, 13N). Furthermore, the emission is
quite extended in direction of Daedalus and the center-to-limb variation
do not follow a classical cos \Theta law. One basic interpretation
could be the presence of another hot spot close to Loki which may
contaminate the flux calculated. The flux estimated on the images
with Loki nearest the central meridian indicates a vertical brightness
of 85+/-10 GW/Sr/micron (similar the medium activity determined
in September 1998).
Another important active area corresponds to the Janus-Kanehikili
(J-K) group which approximately follows a cos \Theta law and is
estimated to have a vertical brightness of 46+/-10 GW/Sr/micron.
We also isolated other possible sources of emission on the last
data set (SEP longitude=3 \deg). Two eastern limb emissions correspond
to Hi'Iaka and Gish Bar. Two unknown faint emissions are located
on the internal disc: one at the NW (astronomical) of J-K (0011A)
located at (27+/-10W, 20+/-7N) and another one (0011B?) close to
the northern pole (55+/-15W, 58+/-15N). In our previous survey,
this part of the Io surface has been poorly imaged (near-limb geometry).
Therefore, it is not possible to compare and confirm the presence
of such emissions. Sengen Patera area seems not to be active on
our data (close-limb position).
|
|
|
 |
Mercator Projection of the above
images
Map of Io derived from the November (2 sets) and December (1 set)
2000 observations. The horizontal and vertical axis are west longitude
and latitude. We have overplotted the persistent (green) and transient
(yellow) hot spot locations detected by NIMS during the 10 first
Galileo orbits (Lopes-Gautier et al., Icarus, 140, 243-264, 1999).
The blue boxes correspond to the hot spot locations determined from
our previous AO data (Marchis et al., submitted to JGR, 2000)
|
 |
Eruption
at Tvashtar Catena on November 14, 2000  |
|