Saturn’s atmosphere normally appears placid and calm. But about once per Saturn year (about 30 Earth years), as spring comes to the northern hemisphere of the giant planet, something stirs deep below the clouds that leads to a dramatic planet-wide disturbance.
The latest such storm was first detected by the radio and plasma wave science instrument on NASA’s Cassini spacecraft, in orbit around the planet, and also tracked by amateur astronomers in December 2010. It has now been studied in detail using the VISIR infrared camera on ESO’s VLT in conjunction with observations from the Composite Infrared Spectrometer on Cassini.
This is only the sixth of these huge storms to be spotted since 1876. It is the first ever studied in the thermal infrared — to see the variations of temperature within a saturnian storm — and the first ever observed by an orbiting spacecraft.
“This disturbance in the northern hemisphere of Saturn has created a gigantic, violent, and complex eruption of bright cloud material, which has spread to encircle the entire planet,” said Leigh Fletcher from the University of Oxford, United Kingdom. “Having both the VLT and Cassini investigating this storm at the same time gives us a great chance to put the Cassini observations into context. Previous studies of these storms have only been able to use reflected sunlight, but now, by observing thermal infrared light for the first time, we can reveal hidden regions of the atmosphere and measure the really substantial changes in temperatures and winds associated with this event.”
The storm may have originated deep down in the water clouds where a phenomenon similar to a thunderstorm drove the creation of a giant convective plume; just as hot air rises in a heated room, this mass of gas headed upwards and punched through Saturn’s usually serene upper atmosphere. These huge disturbances interact with the circulating winds moving east and west and cause dramatic temperature changes high up in the atmosphere.
“Our new observations show that the storm had a major effect on the atmosphere, transporting energy and material over great distances, modifying the atmospheric winds — creating meandering jet streams and forming giant vortices — and disrupting Saturn’s slow seasonal evolution,” said Glenn Orton from the Jet Propulsion Laboratory in Pasadena, California.
Some of the unexpected features seen in the new imaging from VISIR have been named stratospheric beacons. These are strong temperature changes high in the saturnian stratosphere, 155 to 185 miles (250 to 300 kilometers) above the cloud tops of the lower atmosphere that show how far up into the atmosphere the effects of the storm extend. The temperature in Saturn’s stratosphere is normally around –200° Fahrenheit (–130° Celsius) at this season, but the beacons are measured to be 60° to 70° F (15° to 20° C) warmer.
The beacons are completely invisible in reflected sunlight but can outshine the emission from the rest of the planet in the thermal infrared light detected by VISIR. They had never been detected before, so astronomers are not sure if they are common features in such storms.
“We were lucky to have an observing run scheduled for early in 2011, which ESO allowed us to bring forward so that we could observe the storm as soon as possible. It was another stroke of luck that Cassini’s CIRS instrument could also observe the storm at the same time, so we had imaging from VLT and spectroscopy of Cassini to compare,” said Leigh Fletcher. “We are continuing to observe this once-in-a-generation event.”
Saturn’s atmosphere normally appears placid and calm. But about once per Saturn year (about 30 Earth years), as spring comes to the northern hemisphere of the giant planet, something stirs deep below the clouds that leads to a dramatic planet-wide disturbance.
The latest such storm was first detected by the radio and plasma wave science instrument on NASA’s Cassini spacecraft, in orbit around the planet, and also tracked by amateur astronomers in December 2010. It has now been studied in detail using the VISIR infrared camera on ESO’s VLT in conjunction with observations from the Composite Infrared Spectrometer on Cassini.
This is only the sixth of these huge storms to be spotted since 1876. It is the first ever studied in the thermal infrared — to see the variations of temperature within a saturnian storm — and the first ever observed by an orbiting spacecraft.
“This disturbance in the northern hemisphere of Saturn has created a gigantic, violent, and complex eruption of bright cloud material, which has spread to encircle the entire planet,” said Leigh Fletcher from the University of Oxford, United Kingdom. “Having both the VLT and Cassini investigating this storm at the same time gives us a great chance to put the Cassini observations into context. Previous studies of these storms have only been able to use reflected sunlight, but now, by observing thermal infrared light for the first time, we can reveal hidden regions of the atmosphere and measure the really substantial changes in temperatures and winds associated with this event.”
The storm may have originated deep down in the water clouds where a phenomenon similar to a thunderstorm drove the creation of a giant convective plume; just as hot air rises in a heated room, this mass of gas headed upwards and punched through Saturn’s usually serene upper atmosphere. These huge disturbances interact with the circulating winds moving east and west and cause dramatic temperature changes high up in the atmosphere.
“Our new observations show that the storm had a major effect on the atmosphere, transporting energy and material over great distances, modifying the atmospheric winds — creating meandering jet streams and forming giant vortices — and disrupting Saturn’s slow seasonal evolution,” said Glenn Orton from the Jet Propulsion Laboratory in Pasadena, California.
Some of the unexpected features seen in the new imaging from VISIR have been named stratospheric beacons. These are strong temperature changes high in the saturnian stratosphere, 155 to 185 miles (250 to 300 kilometers) above the cloud tops of the lower atmosphere that show how far up into the atmosphere the effects of the storm extend. The temperature in Saturn’s stratosphere is normally around –200° Fahrenheit (–130° Celsius) at this season, but the beacons are measured to be 60° to 70° F (15° to 20° C) warmer.
The beacons are completely invisible in reflected sunlight but can outshine the emission from the rest of the planet in the thermal infrared light detected by VISIR. They had never been detected before, so astronomers are not sure if they are common features in such storms.
“We were lucky to have an observing run scheduled for early in 2011, which ESO allowed us to bring forward so that we could observe the storm as soon as possible. It was another stroke of luck that Cassini’s CIRS instrument could also observe the storm at the same time, so we had imaging from VLT and spectroscopy of Cassini to compare,” said Leigh Fletcher. “We are continuing to observe this once-in-a-generation event.”
