EPSC07/11: THE CHANGING RINGS OF URANUS
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As the rings of Uranus swing edge-on to Earth – a short-lived view we get only once every 42 years – astronomers observing the event are getting an unprecedented, glare-free view of the rings and the fine dust that permeates them.
The rings were discovered in 1977, so this is the first opportunity astronomers have had to observe a Uranus ring crossing and perhaps to discover a new moon or two.
While the Keck II telescope and the Hubble Space Telescope have been looking at the planet for years in anticipation of this event, ground-based telescopes in Chile and southern California have joined them in targeting the planet during the actual ring crossing.
Based on the Keck observations, a team of astronomers led by Imke de Pater of University of California, Berkeley, reports today (Thursday, Aug. 23) in Science Express, the online edition of Science magazine, that the rings of micron-sized dust have changed significantly since the Voyager 2 spacecraft photographed the Uranus system 21 years ago. She will discuss the results during a talk today at the European Planetary Science Congress 2007 meeting in Potsdam, Germany.
The inner rings are much more prominent than expected, revealing material in otherwise empty regions of the system of rings.
“People tend to think of the rings as unchanging, but our observations show that not to be the case,” said de Pater, a UC Berkeley professor of astronomy. “There are a lot of forces acting on small dust grains, so it is not that crazy to find that the arrangement of rings has changed.”
Using the near infrared camera (NIRC2) and adaptive optics on the Keck II telescope on May 28, the team took striking images of the nearly edge-on ring appearing as a bright line bisecting a dim Uranus, which appears dark in the infrared. The observations were conducted during an engineering run by Marcos van Dam, adaptive optics scientist at the W. M. Keck Observatory, after the installation of a new wavefront sensor.
“The improvements to the adaptive optics systems allowed us to capture unbelievably crisp images of Uranus; it was as if the Keck telescope was orbiting in space,” said van Dam.
On Aug. 14, the Hubble Space Telescope also imaged the planet very near the moment when the rings were perfectly aligned with Earth, showing similar features but also including some recently-discovered outer rings. The image was released today by the Space Telescope Science Institute.
“The outermost ring is not visible in our infrared images,” said de Pater’s co-author, Heidi B. Hammel of the Space Science Institute in Boulder, Colo. “This ring is very blue, and therefore harder to see in the infrared. We may detect it when the rings are fully edge-on and when we can observe it for several hours.”
With further analysis of the Hubble data, astronomer Mark Showalter of the SETI Institute hopes to detect some of the small moons, and perhaps some not seen before, that shepherd the debris into distinct rings.
“Two little satellites called Cordelia and Ophelia straddle the brightest ring, the epsilon ring, and keep it in place, but people have always assumed there must be a bunch more of these satellites that are confining the nine other narrow rings,” Showalter said. “This is the unique viewing geometry that only comes along once in 42 years, when we have a chance of imaging these tiny satellites, because normally they are lost in the glare of the rings. Now, the rings are essentially invisible.”
Astronomers at the Very Large Telescope (VLT) in Chile, run by the European Southern Observatory (ESO), and at the Palomar Observatory in southern California operated by the California Institute of Technology, also observed Uranus during the current crossing.
“The VLT took data at the precise moment when the rings were edge-on to Earth,” said de Pater, who worked with two team members observing in Chile: Daphne Stam of the Technical University of Delft in the Netherlands and Markus Hartung of ESO. Meanwhile, astronomers Philip Nicholson of Cornell University and Keith Matthews of Caltech observed from atop Mt. Palomar.
Until Voyager flew by in January 1986, the rings were only known from the way they temporarily blocked the light of stars passing behind Uranus. Earth-based images have been too blurry until recently, with the advent of Keck adaptive optics and the Advanced Camera for Surveys of the Hubble telescope. Nevertheless, when the sunlit side of Uranus’s rings are in full view of Earth, the densely-packed rings reflect so much light that their glare completely dominates the fainter glow from micron-sized dust.
Earth’s orbit around the sun permits three opportunities to view the rings edge-on: Uranus made its first ring crossing as seen from Earth on May 3, it made its second crossing on Aug. 16, and will cross for the third and last time on Feb 20, 2008. Though the last ring crossing relative to Earth will be hidden behind the sun, most of Earth’s premier telescopes, including Keck, Hubble, VLT and Palomar, plan to focus on the planet again in the days following Dec. 7.
“December 7 is the Uranian equinox, when the rings are perfectly edge-on to the sun, and after that, there is a brief period again when we will view the dark side of the rings, before they become illuminated again for another 42 years,” Hammel said.
The advantage of observations at a ring-plane crossing is that it becomes possible to look at the rings from the shadowed side. From that vantage, the normally-bright outer rings grow fainter because their centimeter- to meter-sized rocks obscure one another, while the dim inner rings get brighter as their material merges into a thin band along the line of sight.
The dust belts that Voyager saw differ radically from today’s dust distribution, according to coauthors de Pater and Showalter. Most interesting is a broad, inner ring called zeta, whose position today is several thousand kilometers farther from the planet than when it was discovered by Voyager.
“The ring may have moved, or it may be an entirely new ring,” noted Showalter.
Similar, dramatic changes in dust distribution have also been observed recently in Saturn’s and Neptune’s rings. This is not surprising, because gravity keeps the larger ring particles in orbit, but other smaller forces can nudge the tiny dust grains around, de Pater said. These forces include pressure from sunlight, drag produced as the dust plows through ionized plasma around Uranus, and even drag from the planet’s magnetic field.
“Impacts into the larger bodies in the system also could knock dust off and create new rings,” de Pater said.
“With further observations, the time scales over which these variations occur should provide new insight into the physical processes at work,” the authors concluded.
Support for the Keck observations came from the National Science Foundation, the National Aeronautics and Space Administration, the Keck Observatory and the UC Santa Cruz Technology Center for Adaptive Optics.
NOTE: Imke de Pater is in Potsdam, Germany, but may be reached through the Europlanet press office at +49-331-907-30229, or via e-mail at imke@berkeley.eduThisemail address is being protected from spam bots, you need Javascript enabled to view it . Heidi Hammel is at (203) 438-3506 or hbh@alum.mit.eduThis email address is being protected from spam bots, you need Javascript enabled to view it . Mark Showalter can be reached at (650) 810-0234 or mshowalter@seti.orgThis email address is being protected from spam bots, you need Javascript enabled to view it ; or through Karen Randall, Director of Special Projects at the SETI Institute: (650) 960-4537.
The dark side of the rings of Uranus
The dark side of the rings of Uranus, as imaged by Keck adaptive optics on 28 May 2007. The image was taken at 2.2 mm. At this wavelength, methane and hydrogen gases absorb sunlight so that Uranus looks relatively dark, allowing ring material to be traced very close to the planet. This image was taken in May just after Earth had crossed Uranus’s ring plane (see Fig.below). The Sun, however, has not yet crossed the ring plane, and thus this is the first image of the unlit side of the rings of Uranus. The brightest ring in this image is the inner “zeta” ring, first identified in Keck images in 2004 and virtually undetectable prior to that. It appears bright because sunlight is scattered by its fine dust particles on its way through the rings to the dark side.
Comparison of the lit and unlit sides of the rings of Uranus.
Imke de Pater (UC Berkeley), Heidi B. Hammel (SSI, Boulder), and
Comparison of the lit and unlit sides of the rings of Uranus. (A) The lit side in early July 2004, when the ring opening angle to Earth B = 11°, and the angle Bo to the Sun =13.2° (5). (B) The lit side on 1 August 2006 when B = 3.6° and Bo = 5.2°. (C) The unlit side on 28 May 2007 when B = 0.7° and Bo= 2.0°. The dotted lines show the position of rings epsilon (upper line) and zeta (lower line). The pericenter of epsilon was near the tip of the ring in 2006, at ~11 o’clock in 2004, and at ~ 2 o’clock position in 2007.
Infrared images of Uranus
These infrared images of Uranus from the W.M. Keck Observatory show the rare ring-plane crossing in 2007. The pictures were obtained from 2001 to 2007 using Keck’s adaptive optics system. This series of images at a wavelength of 2.2 microns shows the change in viewing aspect, or ring opening angle. At this wavelength, methane and hydrogen gases absorb sunlight so that Uranus looks relatively dark, allowing ring material to be traced very close to the planet. Cloud features are visible as bright spots on some of the images, as are small moons. The 2007 image (far right) was taken in May just after Earth had crossed Uranus’s ring plane. The Sun, however, has not yet crossed the ring plane, and thus this is the first image of the unlit side of the rings of Uranus. The bright “epsilon” ring which dominates the 2001-2005 images began to fade in 2006 due to large ring particles blocking one another as the rings’ opening angle decreased; it essentially disappeared in 2007. The brightest ring in 2007 is the inner “zeta” ring, first identified in Keck images in 2004 and virtually undetectable prior to that. It appears bright because sunlight is scattered by its fine dust particles on its way through the rings to the dark side. A second ring-plane crossing visible from Earth took place on 16 August 2007, and telescopes around the world were trained on Uranus to capture the event. The Sun itself will cross the ring plane of Uranus on 7 December 2007.
Courtesy: Imke de Pater (UC Berkeley), Heidi B. Hammel (SSI, Boulder), and
the W.M. Keck Observatory.
Uranus ring-crossing observed by Very Large Telescope
The rings of Uranus are shown here captured almost exactly edge-on to Earth. This false-color image was obtained by the NAOS-CONICA infrared camera on the Very Large Telescope at Paranal, Chile. It was taken at 9:00 UT on 16 August 2007, just two hours after Earth had just crossed to the lit side of the ring plane. We are peering over the sunlit face of the rings at an opening of only 0.003°, an angle so small that the thin rings nearly disappear. At right, the region around the planet has been enhanced to show a thin line, which is sunlight glinting off the ring edges and also reflected by dust clouds embedded within the system. The pictures at left shows the planet and identifies four of its largest moons. One can clearly discern banding in the atmosphere and a bright cloud feature near the planet’s south polar collar, on the left side of the image.
This is a composite of images taken at infrared wavelengths. The planet is shown in false color, based on images taken at wavelengths of 1.2 and 1.6 microns. The rings are extracted from an image taken at 2.2 microns, where the planet is darker and therefore the rings are easier to detect.
Courtesy: Daphne Stam (TU Delft), Markus Hartung (ESO, Chile), Mark Showalter (SETI) and Imke de Pater (UC Berkeley and TU Delft).
GOING, GOING, GONE: HUBBLE CAPTURES URANUS’S RINGS ON EDGE
Rings of Uranus observed by Hubble Space Telescope in 2003 and 2007
This series of images from the NASA/ESA Hubble Space Telescope shows how the ring system around the distant planet Uranus appears at ever more oblique (shallower) tilts as viewed from Earth – culminating in the rings being seen edge-on in three observing opportunities in 2007. The best of these events appears in the far right image taken with Hubble’s Wide Field Planetary Camera 2 on August 14, 2007.
Credit: NASA, ESA, and M. Showalter (SETI Institute)
Rings of Uranus edge-on observed by Hubble on 14th August 2007
The rings or Uranus were photographed with Hubble’s Wide Field Planetary Camera 2 on August 14, 2007. The edge-on rings appear as spikes above and below the planet. The rings cannot be seen running fully across the face of the planet because the bright glare of the planet has been blocked out in the HST photo (a small amount of residual glare appears as a fan-shaped image artifact, along with an edge between the exposure for the inner and outer rings).
A much shorter color exposure of the planet has been photo-composited to show its size and position relative to the ring plane.
Earthbound astronomers only see the ring’s edge every 42 years as the planet follows a leisurely 84-year orbit about the Sun. However, the last time the rings were tilted edge-on to Earth astronomers didn’t even know they existed.
The fainter outer rings appear in the 2003 Hubble Space Telescope images, but were not noticed there until they were seen in the 2005 images and the previous ones were analyzed more carefully. Uranus has a total of 13 dusty rings.
Credit: NASA, ESA, and M. Showalter (SETI Institute)
