This is a composite image showing the Saturn Lyman-alpha bulge, and emission from hydrogen which is a persistent and unexpected excess detected by three distinct NASA missions, namely Voyager 1, Cassini, and the Hubble Space Telescope between 1980 and 2017.
A Hubble near-ultraviolet image, obtained in 2017 during the Saturn summer in the northern hemisphere, is used as a reference to sketch the Lyman-alpha emission of the planet. The rings appear much darker than the planet’s body because they reflect much less ultraviolet sunlight.
Above the rings and the dark equatorial region, the Lyman-alpha bulge appears as an extended (30°) latitudinal band that is 30% brighter than the surrounding regions. A small fraction of the southern hemisphere appears between the rings and the equatorial region, but it is less brighter than the northern hemisphere.
North of the bulge region (upper-right portion of image), the disk brightness declines gradually versus latitude toward the bright aurora region that is here shown for reference. A dark spot inside the aurora region represents the footprint of the spin axis of the planet.
It’s believed that icy rings particles raining on the atmosphere at specific latitudes and seasonal effects cause an atmospheric heating that makes the upper atmosphere hydrogen reflect more Lyman-alpha sunlight in the bulge region. This unexpected interaction between the rings and the upper atmosphere is now investigated in depth to define new diagnostic tools for estimating if distant exoplanets have extended Saturn-like ring systems.
Credit: NASA, ESA, Lotfi Ben-Jaffel (IAP & LPL)
For more information, visit:
science.nasa.gov/missions/hubble/hubble-finds-saturns-rin...
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