v1.2.3 / chapter 14 of 19 / 01 jun 09 / greg goebel / public domain
* The observations of Saturn performed by planetary probes have given us new insights into the ringed world, but much more remains to be learned, with the elaborate ring system still mysterious in many ways.

* The gross properties of the Saturn system had been apparent from Earth-based observations, and so the space probes that passed by revealed little dramatically new about the planet itself. The spacecraft did confirm the existence of a strong magnetic field; Saturn's magnetic field is 1,000 times stronger than the Earth's, but only about 1/20th as strong as Jupiter's. The magnetic poles are aligned to within 1 degree of the axis of rotation. Such a close alignment is unusual.
Images of the cloud features returned from the planet were interesting, but also revealed nothing that was particularly surprising. Saturn's cloud activity was known to be subdued compared to that of Jupiter, due to lower temperatures and gravity.
The sunlight falling on Saturn is relatively faint and weak, and so the average difference between polar and equatorial temperatures there is only about five degrees Kelvin. This means that most of the weather patterns are driven by the planet's internal energy and its fast rate of rotation. The end result is the planet's banded appearance, which is a consequence of zonal winds. These winds are very fast: the equatorial belt has a velocity of 500 meters per second. The zonal winds are symmetrical with respect to the hemispheres, demonstrating the relative unimportance of solar radiation on Saturn.
The probes did observe spots, the most spectacular being "Anne's Spot", a cyclonic storm observed by the Voyagers with a width of 5,000 by 3,000 kilometers, much smaller than Jupiter's Great Red Spot. In 2006, the Cassini probe observed a particularly interesting cyclonic storm at the planet's south pole, about 8,000 kilometers across. The storm was unusual in that it featured an "eye" like that of Earthly hurricanes, which hasn't been observed in other large cyclonic storms on the gas giant planets.
* Although observations of Saturn itself were more interesting than revolutionary, of course the unprecedented close-up images of the moons and particularly the ring system provided by spacecraft flybys provided plenty of surprises.

The probes, as well as exacting Earth-based observations performed during the missions and afterward, discovered some new small moons, and provided more detailed observations of the "classic" moons of Saturn. In order from outermost to innermost:
Phoebe was imaged in considerable detail by the Cassini probe in a flyby on 17 June 2004. It is an indication of the distance of Phoebe to Saturn that Cassini didn't actually go into orbit around the planet until the end of the month! There were no great surprises, one mission scientist saying: "Phoebe looks icy and covered with dirt." -- but it was heavily battered with craters, with some of the more recent-appearing craters exposing bright patches in the dark surface, suggesting patches of water ice. Further analysis showed that Phoebe's composition was similar to that of Pluto and the other "Kuiper Belt Objects" (discussed later), hinting strongly that it was an interloper from the far regions of the Solar System that had been captured by Saturn.
Hyperion, like Phoebe, does not have a synchronous orbit. In fact, it doesn't even have a constant "day", since its rotation is "chaotic", changing on a continuous basis. The unusual appearance and rotation of Hyperion suggests that it is a fragment of a larger moon that was broken up in the distant past by an impact. The rotation should have straightened itself out, but Hyperion's 3:4 resonance with Titan may help keep the rotation in a chaotic state.
Titan appears to have a rocky core covered by a thick layer of water ice. It is covered with an opaque atmosphere consisting mostly of nitrogen, with about 6% argon and a small percentage of methane. There are traces of hydrocarbons, such as ethane and acetylene, apparently created by the breakdown of methane in sunlight, creating the hazy "smog" that hides the surface of Titan. The atmospheric pressure at the surface appears to be about 1.5 times that of the Earth's sea-level air pressure. It has been described as an icy world with hydrocarbon streams, methane rivers, and ammonia volcanoes.
Titan features dark equatorial regions that were once thought to be seas of liquids, but Cassini observations show that they are huge fields of sand dunes. This was a bit surprising since it was also believed that the winds on Titan were weak, too weak to form dunes, but as it turns out, the moon's global weather system gets considerable drive from Saturn's tidal forces.
Helene was discovered in 1980 by Earth-based observations. It is a lump with dimensions of 36 by 32 by 30 kilometers. It occupies the same orbit, or in other words is "co-orbital", with the much larger Dione. For this reason, it is sometimes referred to as "Dione B". Helene is trapped in one of the libration points, or stable gravitational positions, of the orbit, equidistant from Dione and Saturn. Helene leads Dione in their mutual orbit. Helene was finally imaged by Cassini in 2006, with the images showing an irregular dark lump.
The very small moons "Telesto" and "Calypso" were discovered in 1980 by Earth-based telescopes. They are small lumps, with Telesto having dimensions of 34 by 28 by 36 kilometers and Calypso having dimensions of 34 by 22 by 22 kilometers. These two moons are co-orbital with the much larger Tethys. Telesto is in the "leading" Lagrangian point, preceding Tethys in their common orbit, while Calypso is in the "trailing" Lagrangian point.
The observation suggested that there are liquid water oceans under the surface of Enceladus. As with Jupiter's Europa, that might provide an environment where traces of life could be found. The 1:2 resonance of Dione with Enceladus may induce tidal effects responsible for Enceladus's geological activity, though the heating wouldn't be very great.
As it turned out, the radii of their orbits differ by only 50 kilometers, less than their diameters, and to make things really confusing, about every four years they pass each other and undergo a transfer of momentum that drops one into the lower orbit and kicks the other into the higher orbit. It is suspected that this unusual orbit is due to the fact that the two moons are the product of a breakup of a single body in the distant past.
* The probes provided very significant revelations about Saturn's ring system. They discovered three two more main rings, including the broad and faint outermost "E Ring" (which had been tentatively spotted by Feibelman in the 1960s), the faint but smaller "G Ring" inside the E Ring, and the strandlike "F Ring", which circled the A Ring. The rings were determined to have a typical depth of about 200 meters.
The discoveries led to a modern breakdown of the ring system as follows, arranged from outermost to innermost:
The moons Phoebe, Iapetus, Hyperion, Titan, and Rhea orbit outside of the ring system. The moons Dione, Helene, Tethys, Calypso, Telesto, Enceladus, and Mimas all pass through the E Ring. It appears that the E Ring is created by venting of ice crystals from Enceladus, which give the ring a blue color.
The F Ring should have spread out, but the two moons seem to keep it confined to its narrow width. They are known as "ring shepherd" or just "shepherd" moons for this reason, and this sort of arrangement is regarded as one of the major influences on structure in planetary ring systems.
The tiny moon Atlas orbits just outside the A Ring, probably acting as a shepherd to define the ring's boundary, while the tiny moon Pan orbits within the Encke division and is almost certainly the cause of it. There is a narrow division near the outer edge of the ring, known as the "Keeler Gap"; in 2005 the Cassini probe photographed a moonlet about six kilometers wide in the middle of the gap. The moonlet was provisionally eventually named "Daphnis" and the image revealed an interesting pattern of waves on the edge of the gap, caused by the moonlet.
One of the big surprises was that each of the "main" rings consists of hundreds of very narrow rings. One of the outer rings has an oddly twisted or braided appearance, the reason for which is still not fully understood. The spokelike features that O'Meara had vaguely seen were observed in the B Ring by Voyager 1, and still remain mysterious. They may be an interaction with Saturn's magnetic field.

Cassini returned an even bigger surprise by providing evidence that the rings are much more stable than previously thought, and in fact may have been around for billions of years. The conventional wisdom was that impacts of ring particles would gradually pulverize them and the rings would eventually dissipate, but it appears instead that the particles will either clump together or break apart, and so the rings are in a good approximation of a steady state.
* Nine new moons of Saturn were thought to have been discovered in 1981 from analysis of Voyager 2 data; seven more were thought to have been discovered in 1995 from Hubble Space Telescope imagery. All of these were in the vicinity of or associated with the ring system, but they were not confirmed and are now generally suspected to have been at best just temporary clumpings of ring material. They have now been generally discounted, though Cassini observations should provide conclusive proof one way or another. However, over 30 irregular moonlets were discovered by Earth-based telescopes in the 21st century:
The irregular moonlets occur in three groups:
Cassini observations have also suggested the existence of very small moonlets, a few hundred meters across, associated with the ring system. Given that the observations only covered a small sector of the rings, there are likely millions more moonlets of similar size. Naming them all might be a challenge. In fact, sooner or later the search for moonlets around the gas giant planets is certain to run into diminishing returns. Astronomers believe that many more moons will be found as telescope technology improves, until eventually nobody finds it interesting any more. As one astronomer put it: "At some point, you have to decide when to quit."
* Statistics for Saturn:
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mean distance from Sun 9.54 AU (1427.0 x 10^6 kilometers)
orbital period (sidereal) 29.46 years
orbital eccentricity 0.056
orbital inclination 2.5 degrees
equatorial diameter 120,000 km (9.41 Earth)
mass (relative to Earth) 95.159
mean density (relative to water) 0.70
gravity (relative to Earth) 1.08
escape speed 35.6 kilometers per second
rotation period 0.44 days
oblateness 1/9
inclination of equator 26.7 degrees
albedo 0.47
max surface temperature -180 degrees Celsius (cloud tops)
atmosphere (major constituents ) H, He, CH4
clouds of NH3, NH4SH, H2O
atmospheric pressure at surface not applicable
number of known moons 18
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* Regular moons of Saturn, from outermost to innermost, with pronunciations
in parenthesis.

Radii are given from the center of Saturn. The abbreviation "RS" stands for
the radius of Saturn, while "RM" stands for the radius of the orbit of the
Earth's Moon, and "M" stands for the diameter or mass of the Earth's Moon.
Densities are given relative to water, which is equivalent to grams per cubic
centimeter. Orbital and rotation periods are given in days and fractions of
days, with days-hours-minutes added for periods under two days.
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PHOEBE ("FEE-bee") / Saturn IX / irregular (Norse group):
mean distance from planet 12,952,000 km / 216 RS / 33.71 RM
orbital period (sidereal) 550.46 days
orbital eccentricity 0.163
orbital inclination 175.3 degrees (retrograde)
equatorial diameter 220 km / 0.06 M
mass 0.000054 M
mean density 0.7
albedo 0.06
year of discovery 1898 (Pickering)
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IAPETUS ("eye-AP-i-tus") / Saturn VIII:
mean distance from planet 3,561,300 km / 59.4 RS / 9.26 RM
orbital period (sidereal) 79.331 days
orbital eccentricity 0.028
orbital inclination 14.7 degrees
equatorial diameter 1,460 km / 0.42 M
mass 0.026 M
mean density 1.2
albedo 0.2
year of discovery 1671 (Cassini)
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HYPERION ("hy-PEER-ee-en") / Saturn VII:
mean distance from planet 1,481,000 km / 24.7 RS / 3.85 RM
orbital period (sidereal) 21.276 days
orbital eccentricity 0.104
orbital inclination 0.4 degrees
dimensions 410 x 260 x 220 km
mass 0.00024 M
mean density 1.4
albedo 0.3
year of discovery 1848 (Bond, Bond, Lassell)
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TITAN ("TY-tun") / Saturn VI:
mean distance from planet 1,221,850 km / 20.4 RS / 3.18 RM
orbital period (sidereal) 15.945 days
orbital eccentricity 0.029
orbital inclination 0.33 degrees
equatorial diameter 5,150 km / 1.48 M
mass 1.83 M
mean density 1.88
albedo 0.21
year of discovery 1655 (Huygens)
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RHEA ("REE-a") / Saturn V:
mean distance from planet 527,040 km / 8.77 RS / 1.37 RM
orbital period (sidereal) 4.517 days / 4 days 12 hours 10 minutes
orbital eccentricity 0.001
orbital inclination 0.35 degrees
equatorial diameter 1,530 km / 0.44 M
mass 0.034 M
mean density 1.3
albedo 0.7
year of discovery 1672 (Cassini)
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DIONE ("dy-OH-nee") / Saturn IV:
mean distance from planet 377,400 km / 6.3 RS / 0.98 RM
orbital period (sidereal) 2.737 days
orbital eccentricity 0.002
orbital inclination 0.02 degrees
equatorial diameter 1,120 km / 0.32 M
mass 0.014 M
mean density 1.4
albedo 0.7
year of discovery 1684 (Cassini)
HELENE / Saturn XII:
CO-ORBITAL with Dione, at leading libration point.
dimensions 36 x 32 x 30 km
mass UNKNOWN
albedo 0.7
year of discovery 1980 (Laques, Lecacheux)
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POLYDEUCES ("polly-deuces") / Saturn XXXIV (S/2004 S5)
mean distance from planet 377,396 km / 6.29 RS / 0.99 RM
orbital period (sidereal) 2.737 days
orbital eccentricity 0
orbital inclination 0
equatorial diameter 3.5 km
mass / density: UNKNOWN
albedo UNKNOWN
year of discovery 2004 (Cassini)
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TETHYS ("TEE-this") / Saturn III:
mean distance from planet 294,660 km / 4.92 RS / 0.77 RM
orbital period (sidereal) 1.888 days / 1 day 21 hours 19 minutes
orbital eccentricity 0
orbital inclination 1.1 degrees
equatorial diameter 1,060 km / 0.30 M
mass 0.010 M
mean density 1.2
albedo 0.9
year of discovery 1684 (Cassini)
CALYPSO ("ka-LIP-so") / Saturn XIV:
CO-ORBITAL with Tethys, at leading libration point
dimensions 34 x 22 x 22 km
mass / density UNKNOWN
albedo 0.6
year of discovery 1980 (Pascu, Seidelmann, Baum, Currie)
TELESTO ("ta-LESS-toh") / Saturn XIII:
CO-ORBITAL with Tethys, at trailing libration point
dimensions 34 x 28 x 26 km
mass / density UNKNOWN
albedo 0.5
year of discovery 1980 (Smith, Larson, Reitsma)
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ENCELADUS ("en-SELL-a-dus") / Saturn II:
mean distance from planet 238,000 km / 3.97 RS / 0.62 RM
orbital period (sidereal) 1.370 days / 1 day 8 hours 53 minutes
orbital eccentricity 0.004
orbital inclination 0.02 degrees
equatorial diameter 500 km / 0.14 M
mass 0.0011 M
mean density 1.24
albedo 1.0
year of discovery 1789 (Herschel)
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PALLENE ("pah-LEE-nee") / Saturn XXXIII (S/2004 S2)
mean distance from planet 212,280 km / 3.54 RS / 0.56 RM
orbital period (sidereal) 1.154 days / 27 hours 42 minutes
orbital eccentricity 0
orbital inclination 0.2
equatorial diameter 4 km
mass / density: UNKNOWN
albedo UNKNOWN
year of discovery 2004 (Cassini)
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METHONE ("me-THO-nee") / Saturn XXXII (S/2004 S1)
mean distance from planet 194,440 km / 3.24 RS / 0.51 RM
orbital period (sidereal) 1.010 days / 24 hours 14 minutes
orbital eccentricity 0
orbital inclination 0
equatorial diameter ~3 km
mass / density: UNKNOWN
albedo UNKNOWN
year of discovery 2004 (Cassini)
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MIMAS ("MY-mass") / Saturn I:
mean distance from planet 185,520 km / 3.12 RS / 0.49 RM
orbital period (sidereal) 0.942 days / 22 hours 36 minutes
orbital eccentricity 0.020
orbital inclination 1.5 degrees
equatorial diameter 392 km / 0.11 M
mass 0.00052 M
mean density 1.17
albedo 0.5
year of discovery 1789 (Herschel)
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JANUS ("JAY-nus") / Saturn X:
CO-ORBITAL with Epimetheus, in unusual "reciprocal" orbit.
mean distance from planet 151,472 km / 2.52 RS / 0.39 RM
orbital period (sidereal) 0.694 days / 16 hours 39 minutes
orbital eccentricity 0.007
orbital inclination 0.14 degrees
dimensions 196 x 192 x 150 km
mass 0.000003 M?
mean density 0.67?
albedo 0.8
year of discovery 1966 (Dollfus)
EPIMETHEUS ("ep-eh-MEE-thee-us") / Saturn XI
CO-ORBITAL with Janus, in unusual "reciprocal" orbit.
dimensions 144 x 108 x 98 km
mass 0.000008 M?
mean density 0.7?
albedo 0.8
year of discovery 1966 (Fountain, Larson)
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PANDORA ("pan-DOH-uh") / Saturn XVII:
mean distance from planet 141,700 km / 2.37 RS / 0.37 RM
orbital period (sidereal) 0.628 days / 15 hours 4 minutes
orbital eccentricity 0.004
orbital inclination 0
dimensions 114 x 84 x 62 km
mass 0.000003 M?
mean density 0.7?
albedo 0.9
year of discovery 1980 (Collins, Carlson)
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PROMETHEUS ("pra-MEE-the-us") / Saturn XVI:
mean distance from planet 139,350 km / 2.32 RS / 0.36 RM
orbital period (sidereal) 0.613 days / 14 hours 17 minutes
orbital eccentricity 0.003
orbital inclination 0
dimensions 145 x 85 x 65 km
mass 0.000004 M?
mean density 0.7?
albedo 0.6
year of discovery 1980 (Collins, Carlson)
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ATLAS / Saturn XV:
mean distance from planet 137,640 km / 2.28 RS / 0.36 RM
orbital period (sidereal) 0.602 days / 14 hours 27 minutes
orbital eccentricity 0
orbital inclination 0
dimensions 40 x 30 km
mass / density: UNKNOWN
albedo 0.9
year of discovery 1980 (Terrile)
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DAPHNIS ("dafniss") / Saturn XXXV (S/2005 S1)
mean distance from planet 136,504 km / 2.28 RS / 0.36 RM
orbital period (sidereal) 0.594 days / 14 hours 15 minutes
orbital eccentricity 0
orbital inclination 0
equatorial diameter ~7 km
mass / density: UNKNOWN
albedo UNKNOWN
year of discovery 2005 (Cassini)
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PAN / Saturn XVIII:
mean distance from planet 133,583 km / 2.23 RS / 0.35 RM
orbital period (sidereal) 0.575 days / 13 hours 48 minutes
orbital eccentricity 0
orbital inclination 0
equatorial diameter 20 km
mass / density: UNKNOWN
albedo 0.5
year of discovery 1990 (Showalter)
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* Irregular moons of Saturn:
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preliminary
moon designation group
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YMIR Saturn XIX S/2000 S1 Norse group
PAALIAQ Saturn XX S/2000 S2 Inuit group
TARVOS Saturn XXI S/2000 S4 Gallic group
IIJIRAQ Saturn XXII S/2000 S6 Inuit group
SUTTUNGR Saturn XXIII S/2000 S12 Norse group
KIVIUQ Saturn XXIV S/2000 S5 Inuit group
MUNDILFARI Saturn XXV S/2000 S9 Norse group
ALBIORIX Saturn XXVI S/2000 S11 Gallic group
SKATHI Saturn XXVII S/2000 S8 Norse group
ERRIAPUS Saturn XXVIII S/2000 S10 Gallic group
SIARNAQ Saturn XXIX S/2000 S3 Inuit group
THRYMR Saturn XXX S/2000 S7 Norse group
NARVI Saturn XXXI S/2003 S1 Norse group
AEGIR Saturn XXXVI S/2004 S10 Norse group
BEBHIONN Saturn XXXVII S/2004 S11 Gallic group
BERGELMIR Saturn XXXVIII S/2004 S15 Norse group
BESTLA Saturn XXXIX S/2004 S18 Norse group
FARBAUTI Saturn XL S/2004 S9 Norse group
FENRIR Saturn XLI S/2004 S16 Norse group
FORNJOT Saturn XLII S/2004 S8 Norse group
HATI Saturn XLIII S/2004 S14 Norse group
HYRROKKIN Saturn XLIV S/2004 S19 Norse group
KARI Saturn XLV S/2006 S2 Norse group
LOGE Saturn XLVI S/2006 S5 Norse group
SKOLL Saturn XLVII S/2006 S6 Norse group
SURTUR Saturn XLVIII S/2006 S7 Norse group
JARNSAXA Saturn L S/2006 S6 Norse group
GREIP Saturn LI S/2006 S4 Norse group
TARQEQ Saturn S/2007 S1 Inuit group
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unnamed moons, all of Norse group:
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S/2004 S7
S/2004 S12
S/2004 S13
S/2004 S17
S/2006 S1
S/2006 S3
S/2007 S2
S/2007 S3
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* Rings of Saturn:
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E RING 480,000 - 180,000 km / 8.0 - 3.0 RS / 1.25 - 0.47 RM
G RING 173,800 - 165,800 km / 2.9 - 2.76 RS / 0.45 - 0.43 RM
F RING 140,350 - 140,200 km / 2.34 RS / 0.37 RM
A RING 136,000 - 122,200 km / 2.27 - 2.04 RS / 0.35 - 0.32 RM
cassini division
B RING 117,500 - 92,000 km / 1.96 - 1.53 RS / 0.31 - 0.24 RM
maxwell division
C RING 92,000 - 74,500 km / 1.53 - 1.24 RS / 0.24 - 0.19 RM
guerin division
D RING 74,500 - 67,000 km / 1.24 - 1.12 RS / 0.19 - 0.17 RM
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The Encke division bisects the A Ring at 2.23 RS.
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