Courtesy of NASA, November 11, 2010

Ed Stone, project scientist for NASA's Voyager mission, remembers the first time he saw the kinks in one of Saturn's narrowest rings. It was the day the Voyager 1 spacecraft made its closest approach to the giant ringed planet, 30 years ago. Scientists were gathering in front of television monitors and in one another's offices every day during this heady period to pore over the bewildering images and other data streaming down to NASA's Jet Propulsion Laboratory in Pasadena, Calif.

Stone drew a crude sketch of this scalloped, multi-stranded ring, known as the F ring, in his notebook, but with no explanation next to it. The innumerable particles comprising the broad rings are in near-circular orbits about Saturn. So, it was a surprise to find that the F ring, discovered just a year before by NASA's Pioneer 11 spacecraft, had clumps and wayward kinks. What could have created such a pattern?

<b>Saturn's Kinked F Ring</b> The day NASA's Voyager 1 spacecraft made its closest approach to Saturn, it revealed the kinks in one of Saturn's narrowest rings. The nature of Saturn's F ring was one of the biggest surprises of the Voyager spacecrafts' encounters with Saturn. The image on the left from Voyager 1 was released on Nov. 12, 1980. The image on the right shows a closer view of the F ring obtained by NASA's Cassini spacecraft on April 13, 2005. The moon Pandora is to the left (exterior) of the ring and the moon Prometheus is to the right (interior) of the ring. Voyager discovered the two moons Prometheus and Pandora, but images from Cassini spacecraft, in orbit around Saturn since 2004, finally allowed scientists to understand how the two moons sculpt the ring's kinked shape. Data from Cassini show how the gravitational pull of the moons sloshes ring material around, creating wake channels and triggering the formation of clumps as large as 20 kilometers (12 miles) in diameter. Scientists have also made a movie from several Cassini images taken on April 13, 2005 at http://photojournal.jpl.nasa.gov/catalog/PIA07712 .

"It was clear Voyager was showing us something different at Saturn," said Stone, now based at the California Institute of Technology in Pasadena. "Over and over, the spacecraft revealed so many unexpected things that it often took days, months and even years to figure them out."

The F ring curiosity was only one of many strange phenomena discovered in the Voyager close encounters with Saturn, which occurred on Nov. 12, 1980, for Voyager 1, and Aug. 25, 1981, for Voyager 2. The Voyager encounters were responsible for finding six small moons and revealing the half-young, half-old terrain of Enceladus that had to point to some kind of geological activity.

<b>The Puzzling Hexagon</b> The puzzling hexagon-shaped weather pattern around Saturn's north pole was first found in images from NASA's Voyager 2 spacecraft. In 1988, David A. Godfrey, of the National Optical Astronomy Observatories, Tuscon, Ariz., used images obtained by Voyager 2 in 1981 to create the mosaic image on the left. He added a grid showing latitude and longitude. The mosaic image on the right was created from images obtained by NASA's Cassini spacecraft on Jan. 3, 2009. Cassini has obtained higher-resolution pictures of the hexagon – which tell scientists the hexagon is a remarkably stable wave in one of the jet streams that remains 30 years later. But they are still not sure what forces maintain the hexagon.

Images from the two encounters also exposed individual storms roiling the planet's atmosphere, which did not show up at all in data from Earth-based telescopes. Scientists used Voyager data to resolve a debate about whether Titan had a thick or thin atmosphere, finding that Titan was shrouded in a thick haze of hydrocarbons in a nitrogen-rich atmosphere. The finding led scientists to predict there could be seas of liquid methane and ethane on Titan's surface.

"When I look back, I realize how little we actually knew about the solar system before Voyager," Stone added. "We discovered things we didn't know were there to be discovered, time after time."

Ghostly Spokes in the Rings Scientists first saw these somewhat wedge-shaped, transient clouds of tiny particles known as "spokes" in images from NASA's Voyager spacecraft. They dubbed these features in Saturn's B ring "spokes" because they looked like bicycle spokes. An electrostatic charge, the way static electricity on Earth can raise the hair on your arms, appears to be levitating tiny ring particles above the ring plane, but scientists are still figuring out how the particles get that charge as they analyze images from NASA's Cassini spacecraft. The image on the left was obtained by Voyager 2 on Aug. 22, 1981. The image on the right was obtained by Cassini on Nov. 2, 2008.

In fact, the Voyager encounters sparked so many new questions that another spacecraft, NASA's Cassini, was sent to probe those mysteries. While Voyager 1 got to within about 126,000 kilometers (78,300 miles) above Saturn's cloud tops, and Voyager 2 approached as close as about 100,800 kilometers (62,600 miles), Cassini has dipped to this altitude and somewhat lower in its orbits around Saturn since 2004.

Because of Cassini's extended journey around Saturn, scientists have found explanations for many of the mysteries first seen by Voyager. Cassini has uncovered a mechanism to explain the new terrain on Enceladus – tiger stripe fissures with jets of water vapor and organic particles. It revealed that Titan indeed does have stable lakes of liquid hydrocarbons on its surface and showed just how similar to Earth that moon really is. Data from Cassini have also resolved how two small moons discovered by Voyager – Prometheus and Pandora – tug on the F ring to create its kinked shape and wakes that form snowballs.

<b>Hazy Titan</b> Before NASA's Voyager spacecraft visited Saturn in 1980 and 1981, scientists were not sure whether Saturn's moon Titan had a thick or thin atmosphere. Using images such as the one on the left, taken by Voyager 1 on Nov. 12, 1980, scientists learned that Titan was shrouded in a thick haze of hydrocarbons in a nitrogen-rich atmosphere. The finding led scientists to predict there could be seas of liquid methane and ethane on Titan's surface. Since NASA's Cassini spacecraft arrived at Saturn in 2004, it has focused much of its attention at peering underneath the haze, capturing images such as the one on the right with its radar mapping instrument. This image of one of the lakes of liquid hydrocarbons that Cassini has found on Titan's surface was obtained on Jan. 12, 2010. (A related flyover of the area can be seen here: http://photojournal.jpl.nasa.gov/catalog/PIA13173 .) This lake, known as Ontario Lacus, has a surface area of about 15,000 square kilometers (6,000 square miles), slightly smaller than its terrestrial namesake, Lake Ontario. Voyager 1 approached within about 6,500 kilometers of Titan's surface. Cassini has approached to within about 880 kilometers of Titan's surface.

"Cassini is indebted to Voyager for its many fascinating discoveries and for paving the way for Cassini," said Linda Spilker, Cassini project scientist at JPL, who started her career working on Voyager from 1977 to 1989. "On Cassini, we still compare our data to Voyager's and proudly build on Voyager's heritage."

But Voyager left a few mysteries that Cassini has not yet solved. For instance, scientists first spotted a hexagonal weather pattern when they stitched together Voyager images of Saturn's north pole. Cassini has obtained higher-resolution pictures of the hexagon – which tells scientists it's a remarkably stable wave in one of the jet streams that remains 30 years later – but scientists are still not sure what forces maintain the hexagon.

<b>Faces of Enceladus</b> NASA's Voyager spacecraft were the first to take images of Saturn's moon Enceladus close-up in 1980, but it wasn't until NASA's Cassini spacecraft visited the icy moon in 2005 that scientists discovered jets of water vapor and organic particles shooting from the surface. The mosaic image on the left was made from images obtained by Voyager 2, which flew to within about 87,000 kilometers of the icy moon's surface in 1981. From images like these, scientists learned that Enceladus had half-young, half-old terrain. They inferred that Enceladus must have had some kind of recent geological activity. Cassini mission planners made sure to include a scan of Enceladus's south polar region, an area that Voyager 2 was not able to image. Magnetic field data from Cassini's magnetometer instrument, followed by heat mapping from the composite infrared spectrometer and images from the visible-light cameras revealed the presence of a plume flaring out of vast fractures on the surface. Scientists then realized that plume material falling back onto the surface and churning ice underneath could continually repave the "young" terrain of Enceladus. A closer view of one of the fractures, nicknamed "tiger stripes," can be seen here: http://www.jpl.nasa.gov/images/cassini/20100816/cassini20100816-c-full.jpg .

Even more perplexing are the somewhat wedge-shaped, transient clouds of tiny particles that Voyager discovered orbiting in Saturn's B ring. Scientists dubbed them "spokes" because they looked like bicycle spokes. Cassini scientists have been searching for them since the spacecraft first arrived. As Saturn approached equinox, and the sun's light hit the rings edge-on, the spokes did reappear in the outer part of Saturn's B ring. But Cassini scientists are still testing their theories of what might be causing these odd features.

"The fact that we still have mysteries today goes to show how much we still have to learn about our solar system," said Suzanne Dodd, Voyager's project manager, based at JPL. "Today, the Voyager spacecraft continue as pioneers traveling toward the edge of our solar system. We can't wait for the Voyager spacecraft to enter interstellar space – true outer space – and make more unexpected discoveries."

<b>Tempestuous Saturn</b> Data from Earth-based telescopes did not prepare scientists working with NASA's Voyager spacecraft for their first images of the individual storms roiling Saturn's upper atmosphere. The image on the left from Voyager 1 shows convective clouds in the northern hemisphere of Saturn on Nov. 5, 1980. NASA's Cassini spacecraft was able to follow up on Voyager's discoveries. The right hand image shows the so-called "dragon storm" from September 2004. The storm was a powerful source of radio emissions detected by Cassini. The radio emissions resembled short bursts of static generated by lightning on Earth. In August 2009, Cassini was finally able to capture visible-light images of lightning flashing in Saturn's atmosphere. A movie combining the imaging data and the radio emissions can be seen here: http://photojournal.jpl.nasa.gov/catalog/PIA12576 .

Voyager 1, which was launched on Sept. 5, 1977, is currently about 17 billion kilometers (11 billion miles) away from the sun. It is the most distant spacecraft. Voyager 2, which was launched on Aug. 20, 1977, is currently about 14 billion kilometers (9 billion miles) away from the sun.

The Voyagers were built by JPL, which continues to operate both spacecraft. Caltech manages JPL for NASA. The Cassini-Huygens mission is a cooperative project of NASA, the European Space Agency and the Italian Space Agency. JPL manages Cassini for NASA. The Cassini orbiter and its two onboard cameras were designed, developed and assembled at JPL.

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