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By Jia-Rui Cook, Jet Propulsion Laboratory February 11, 2014 Ultraviolet and infrared images from NASA’s Cassini spacecraft and Hubble Space Telescope show active and quiet auroras at Saturn’s north and south poles. Image credit: NASA/JPL-Caltech/University of Colorado/Central Arizona College and NASA/ESA/University of Leicester and NASA/JPL-Caltech/University of Arizona/Lancaster University

A new video from NASA’s Cassini spacecraft and Hubble Space Telescope show a 360-degree view of Saturn’s auroras.

NASA trained several pairs of eyes on Saturn as the planet put on a dancing light show at its poles. While NASA’s Hubble Space Telescope, orbiting around Earth, was able to observe the northern auroras in ultraviolet wavelengths, NASA’s Cassini spacecraft, orbiting around Saturn, got complementary close-up views in infrared, visible-light and ultraviolet wavelengths. Cassini could also see northern and southern parts of Saturn that don’t face Earth.

“Saturn’s auroras can be fickle — you may see fireworks, you may see nothing,” said Jonathan Nichols of the University of Leicester in England, who led the work on the Hubble images. “In 2013, we were treated to a veritable smorgasbord of dancing auroras, from steadily shining rings to super-fast bursts of light shooting across the pole.”

“This is our best look yet at the rapidly changing patterns of auroral emission,” said Wayne Pryor, a Cassini co-investigator at Central Arizona College in Coolidge, Ariz. “Some bright spots come and go from image to image. Other bright features persist and rotate around the pole, but at a rate slower than Saturn’s rotation.”

“Scientists have wondered why the high atmospheres of Saturn and other gas giants are heated far beyond what might normally be expected by their distance from the sun,” said Sarah Badman, a Cassini visual and infrared mapping spectrometer team associate at Lancaster University, England. “By looking at these long sequences of images taken by different instruments, we can discover where the aurora heats the atmosphere as the particles dive into it and how long the cooking occurs.”

The visible-light data have helped scientists figure out the colors of Saturn’s auroras. While the curtain-like auroras we see at Earth are green at the bottom and red at the top, Cassini’s imaging cameras have shown us similar curtain-like auroras at Saturn that are red at the bottom and purple at the top, said Ulyana Dyudina, an imaging team associate at the California Institute of Technology, Pasadena, California.

The color difference occurs because Earth’s auroras are dominated by excited nitrogen and oxygen molecules, and Saturn’s auroras are dominated by excited hydrogen molecules.

“While we expected to see some red in Saturn’s aurora because hydrogen emits some red light when it gets excited, we also knew there could be color variations depending on the energies of the charged particles bombarding the atmosphere and the density of the atmosphere,” Dyudina said. “We were thrilled to learn about this colorful display that no one had seen before.”

“The auroras at Saturn are some of the planet’s most glamorous features – and there was no escaping NASA’s paparazzi-like attention”, said Marcia Burton, a Cassini fields and particles scientist at NASA’s Jet Propulsion Laboratory, Pasadena, California, who is helping to coordinate these observations. “As we move into the part of the 11-year solar cycle where the sun is sending out more blobs of plasma, we hope to sort out the differences between the effects of solar activity and the internal dynamics of the Saturn system.”

There is still more work to do. A group of scientists led by Tom Stallard at the University of Leicester is busy analyzing complementary data taken during the same time window by two ground-based telescopes in Hawaii — the W.M. Keck Observatory and NASA’s Infrared Telescope Facility. The results will help them understand how particles are ionized in Saturn’s upper atmosphere and will help them put a decade of ground-based telescope observations of Saturn in perspective, because they can see what disturbance in the data comes from Earth’s atmosphere.

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