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Portrait of an Imperfect but Beautiful Spiral - Messier 96, aka NGC 3368
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In case you donāt know, the Juno spacecraft entered orbit around the gas giant on July 4, 2016ā¦about a year ago. Since then, it has been collecting data and images from this unique vantage point.
Juno is in a polar orbit around Jupiter, which means that the majority of each orbit is spent well away from the gas giant. But once every 53 days its trajectory approaches Jupiter from above its north pole, where it begins a close two-hour transit flying north to south with its eight science instruments collecting data and its JunoCam camera snapping pictures.
Space Fact: The download of six megabytes of data collected during the two-hour transit can take one-and-a-half days!
Juno and her cloud-piercing science instruments are helping us get a better understanding of the processes happening on Jupiter. These new results portray the planet as a complex, gigantic, turbulent world that we still need to study and unravel its mysteries.
Junoās imager, JunoCam, has showed us that both of Jupiterās poles are covered in tumultuous cyclones and anticyclone storms, densely clustered and rubbing together. Some of these storms as large as Earth!
These storms are still puzzling. Weāre still not exactly sure how they formed or how they interact with each other. Future close flybys will help us better understand these mysterious cyclones.Ā
Seen above, waves of clouds (at 37.8 degrees latitude) dominate this three-dimensional Jovian cloudscape. JunoCam obtained this enhanced-color picture on May 19, 2017, at 5:50 UTC from an altitude of 5,500 miles (8,900 kilometers). Details as small as 4 miles (6 kilometers) across can be identified in this image.
An even closer view of the same image shows small bright high clouds that are about 16 miles (25 kilometers) across and in some areas appear to form āsquall linesā (a narrow band of high winds and storms associated with a cold front). On Jupiter, clouds this high are almost certainly comprised of water and/or ammonia ice.
Junoās Microwave Radiometer is an instrument that samples the thermal microwave radiation from Jupiterās atmosphere from the tops of the ammonia clouds to deep within its atmosphere.
Data from this instrument suggest that the ammonia is quite variable and continues to increase as far down as we can see with MWR, which is a few hundred kilometers.Ā In the cut-out image below, orange signifies high ammonia abundance and blue signifies low ammonia abundance. Jupiter appears to have a band around its equator high in ammonia abundance, with a column shown in orange.
Why does this ammonia matter? Well, ammonia is a good tracer of other relatively rare gases and fluids in the atmosphereā¦like water. Understanding the relative abundances of these materials helps us have a better idea of how and when Jupiter formed in the early solar system.
This instrument has also given us more information about Jupiterās iconic belts and zones. Data suggest that the belt near Jupiterās equator penetrates all the way down, while the belts and zones at other latitudes seem to evolve to other structures.
Prior to Juno, it was known that Jupiter had the most intense magnetic field in the solar systemā¦but measurements from Junoās magnetometer investigation (MAG) indicate that the gas giantās magnetic field is even stronger than models expected, and more irregular in shape.
At 7.766 Gauss, it is about 10 times stronger than the strongest magnetic field found on Earth! What is Gauss? Magnetic field strengths are measured in units called Gauss or Teslas. A magnetic field with a strength of 10,000 Gauss also has a strength of 1 Tesla. Ā
Juno is giving us a unique view of the magnetic field close to Jupiter that weāve never had before. For example, data from the spacecraft (displayed in the graphic above) suggests that the planetās magnetic field is ālumpyā, meaning its stronger in some places and weaker in others. This uneven distribution suggests that the field might be generated by dynamo action (where the motion of electrically conducting fluid creates a self-sustaining magnetic field) closer to the surface, above the layer of metallic hydrogen. Junoās orbital track is illustrated with the black curve.Ā
Juno also observed plasma wave signals from Jupiterās ionosphere.Ā This movie shows results from Junoās radio wave detector that were recorded while it passed close to Jupiter. Waves in the plasma (the charged gas) in the upper atmosphere of Jupiter have different frequencies that depend on the types of ions present, and their densities.Ā
Mapping out these ions in the jovian system helps us understand how the upper atmosphere works including the aurora. Beyond the visual representation of the data, the data have been made into sounds where the frequencies and playback speed have been shifted to be audible to human ears.
The complexity and richness of Jupiterās āsouthern lightsā (also known as auroras) are on display in this animation of false-color maps from our Juno spacecraft. Auroras result when energetic electrons from the magnetosphere crash into the molecular hydrogen in the Jovian upper atmosphere. The data for this animation were obtained by Junoās Ultraviolet Spectrograph.Ā
During Junoās next flyby on July 11, the spacecraft will fly directly over one of the most iconic features in the entire solar system ā one that every school kid knows ā Jupiterās Great Red Spot! If anybody is going to get to the bottom of what is going on below those mammoth swirling crimson cloud tops, itās Juno.
Learn more about the Juno spacecraft and its mission at Jupiter HERE.
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