The Juno spacecraft swings by Ganymede today, coming within 1,038 kilometers of the largest moon of Jupiter. We have to look back over twenty years to see such a close approach to Ganymede, that one conducted by the Galileo probe in 2000. Juno seems to be one of those gifts that keeps on giving, rewarding us now with new data on Ganymede’s composition, tenuous ionosphere, magnetosphere and icy surface, likely a shell over an underlying ocean.
Scott Bolton (SwRI) is Juno’s principal investigator:
“Juno carries a suite of sensitive instruments capable of seeing Ganymede in ways never before possible. By flying so close, we will bring the exploration of Ganymede into the 21st century, both complementing future missions with our unique sensors and helping prepare for the next generation of missions to the Jovian system – NASA’s Europa Clipper and ESA’s [European Space Agency’s] JUpiter ICy moons Explorer [JUICE] mission.”
Image: Left to right: The mosaic and geologic maps of Jupiter’s moon Ganymede were assembled incorporating the best available imagery from NASA’s Voyager 1 and 2 spacecraft and NASA’s Galileo spacecraft. Credits: USGS Astrogeology Science Center/Wheaton/NASA/JPL-Caltech.
The closest approach occurs at 13:35 EDT (17:35 UTC), with the craft’s science instruments beginning collecting data some three hours earlier. Especially useful here will be the Ultraviolet Spectrograph (UVS) and Jovian Infrared Auroral Mapper (JIRAM) instruments, while the Microwave Radiometer (MWR) will draw information on the composition and temperature of the crust. Bolton again:
“Ganymede’s ice shell has some light and dark regions, suggesting that some areas may be pure ice while other areas contain dirty ice. MWR will provide the first in-depth investigation of how the composition and structure of the ice varies with depth, leading to a better understanding of how the ice shell forms and the ongoing processes that resurface the ice over time.”
The animation below gives a sense of Ganymede’s geology:
Animation: A rotating globe of Ganymede, with a geologic map superimposed over a global color mosaic. Credit: USGS Astrogeology Science Center/Wheaton/ASU/NASA/JPL-Caltech.
Remember that JUICE is scheduled for launch in 2022, with multiple flybys of Europa and Callisto planned before the spacecraft moves into orbit around Ganymede, so everything we learn today with Juno will provide additional planning fodder for the mission. JUICE will fly with ice-penetrating radar, an instrument called RIME (Radar for Icy Moon Exploration) that is capable of penetrating up to 10 kilometers of ice and reflecting off subsurface features. That should obviously come in handy not just on Ganymede but Europa and Callisto as well.
A radio occultation experiment is planned for the Juno flyby using the spacecraft’s X-band and Ka-band wavelengths as a probe of the moon’s ionosphere, where solar radiation excites stray gases to form detectable ions. When Juno moves behind Ganymede, the changes in frequency observed as the radio signals pass through the ionosphere will be detected at the Deep Space Network Canberra complex in Australia. A solid reading here would be useful as scientists try to learn more not only about Ganymede’s ionosphere but also its magnetosphere. Larger than the planet Mercury, Ganymede is the only moon in the Solar System to have its own magnetosphere, a region of charged particles that form a bubble around the small world.
This will be a busy week for Juno mission scientists, with the close pass of Ganymede followed less than 24 hours later with the 33rd science pass of Jupiter. Juno’s JunoCam imager should be able to take images of Ganymede at a resolution equivalent to the best returned by Voyager and Galileo, a set of imagery that can be scanned for changes over the four decade period. Of relevance here will be new craters as we try to learn more about impacts in the outer system.
Meanwhile, the Juno Stellar Reference Unit (SRU) navigation camera should collect images with a particular import, telling us something about the radiation environment at Ganymede. Heidi Becker (JPL) is Juno radiation monitoring lead:
“The signatures from penetrating high-energy particles in Jupiter’s extreme radiation environment appear as dots, squiggles, and streaks in the images – like static on a television screen. We extract these radiation-induced noise signatures from SRU images to obtain diagnostic snapshots of the radiation levels encountered by Juno.”
A third camera is the Advanced Stellar Compass, which will measure energetic electrons penetrating its shielding every quarter of a second. NASA points out that from the perspective of Juno, Ganymede will go from being a point of light to a visible disk and back to a point of light in a mere 25 minutes, moving past the moon at about 19 kilometers per second. The ensuing Jupiter close pass will occur at 58 kilometers per second. Fast times above the cloud tops.
Comments on this entry are closed.
We’ve speculated about ice crusts on Europa and possible subsurface features. Will we detect places where the ocean lies under a thinner layer of ice, and any pockets of liquid in the ice close to the surface (< 10 km). Unlike Europa, the surface is very ancient, saturated in impacts, so I would expect there to not be any evidence of hidden crates below the surface indicating surface renewal, but who knows…that is what exploration is for.
It feels very ungrateful for me to be disappointed in this part: “Juno’s JunoCam imager should be able to take images of Ganymede at a resolution equivalent to the best returned by Voyager and Galileo.” I know they’re doing tons of exciting science, that’s the main point, and it’s childish to hope for prettier pictures because 20 years have passed. But still…
JunoCam is much more modern than Voyager or Galileo cameras : I am hopeful.
When Juno was launched, I remember reading that the camera had been added as an afterthought, mostly for PR reasons. I also remember some mild cursing at NASA PR exercises. I could have not be more wrong : Juno’s Jupiter images are stunning, far far better than any previous ones.
Yes I will be looking forward to the images and data from this flyby.
I’ll be looking forward to the Juno data
Here is an interesting one too
Evidence for a sublimated water atmosphere on Ganymede
JUNE 7, 2021
What we would have learned from NASA’s rejected missions to moons of Jupiter and Neptune
by Ashley Spindler, The Conversation
The first photos…
I noticed that almost all the larger impact craters have a sunken central peak, I do not remember seeing this in any images of the other planets and satellites.
The upper right of the full phase image there is a line of twelve impacts in a row. Could this be from a comet like the Comet Shoemaker-Levy 9 or a satellite around Ganymede that was torn apart before impact?
Ganymede from Juno
Image Credit: NASA/JPL-Caltech/SwRI/MSSS; Processing & License: Kevin M. Gill;
Explanation: What does the largest moon in the Solar System look like? Jupiter’s moon Ganymede, larger than even Mercury and Pluto, has an icy surface speckled with bright young craters overlying a mixture of older, darker, more cratered terrain laced with grooves and ridges.
The cause of the grooved terrain remains a topic of research, with a leading hypothesis relating it to shifting ice plates. Ganymede is thought to have an ocean layer that contains more water than Earth — and might contain life. Like Earth’s Moon, Ganymede keeps the same face towards its central planet, in this case Jupiter.
The featured image was captured last week by NASA’s robotic Juno spacecraft as it passed only about 1000 kilometers above the immense moon. The close pass reduced Juno’s orbital period around Jupiter from 53 days to 43 days. Juno continues to study the giant planet’s high gravity, unusual magnetic field, and complex cloud structures.
Some Jupiter news…
Amateur astronomer discovers 80th moon of Jupiter!
Astronomers solve 40 year-old mystery of the cause for Jupiter’s x-ray aurorae: