User:SmilyMoss/sandbox

when converting between windows-1258 and VISCII, the former uses combining diacritics whilst the latter has a large selection of precomposed characters so a converter using a simple mapping between code values and Unicode code points will corrupt text when converting between them.</ref> In Unicode, the main block of combining diacritics for European languages and the International Phonetic Alphabet is U+0300–U+036F. Combining diacritical marks are also present in many other blocks of Unicode characters. In Unicode, diacritics are always added after the main character, so it is possible to add several diacritics to the same character, although as of 2010, few applications support correct rendering of such combinations.

O

Ö́ ö́

´¨ Ĕ́ ĕ́ Ĕ́ ĕ́

L͊

@̣

? Ɂ̣ ∏∐∏∐∏∐∏∐∏

∫∬

∟∠∡∢

៛₨৳₩♠♥m²₪৳₮

'Bold text' Italic text

ₔ

1. Numbered list item

<bromine />

1. REDIRECT Target page name

Heading text

Heading text

Heading text

Heading text

Heading Text

⁷²

72 _₇₂ 72

₇₂

_₇₂

_{Subscript text}

Insert non-formatted text here

ð

• Bulleted list item

ð

Big text Small text

ð

OpenType

OpenType has the ccmp "feature tag" to define glyphs that are compositions or decompositions involving combining characters.

Unicode ranges

{{Main | Combining Diacritical Marks | Combining Diacritical Marks Extended | Combining Diacritical Marks Supplement | Combining Diacritical Marks for Symbols | Combining Half Marks | l1 = Combining Diacritical Marks (Unicode block) | l2 = Combining Diacritical Marks Extended (Unicode block) | l3 = Combining Diacritical

Instant is off Manualhaskell.org

Hoogle    

a -> [a] Packages base filepath concat :: a -> [a] base Prelude, base Data.List Concatenate a list of lists. intercalate :: [a] -> a -> [a] base Data.List intercalate xs xss is equivalent to (concat (intersperse xs xss)). It inserts the list xs in between the lists in xss and concatenates the result. nmergeIO :: a -> IO [a] base Control.Concurrent transpose :: a -> a base Data.List The transpose function transposes the rows and columns of its argument. For example, > transpose [[1,2,3],[4,5,6]] == [[1,4],[2,5],[3,6]] concat :: Foldable t => t [a] -> [a] base Data.Foldable The concatenation of all the elements of a container of lists. msum :: MonadPlus m => [m a] -> m a base Control.Monad This generalizes the list-based concat function. cycle :: [a] -> [a] base Prelude, base Data.List cycle ties a finite list into a circular one, or equivalently, the infinite repetition of the original list. It is the identity on infinite lists. init :: [a] -> [a] base Prelude, base Data.List Return all the elements of a list except the last one. The list must be non-empty. reverse :: [a] -> [a] base Prelude, base Data.List reverse xs returns the elements of xs in reverse order. xs must be finite. tail :: [a] -> [a] base Prelude, base Data.List Extract the elements after the head of a list, which must be non-empty. unlines :: [String] -> String base Prelude, base Data.List, base Data.String unlines is an inverse operation to lines. It joins lines, after appending a terminating newline to each. unwords :: [String] -> String base Prelude, base Data.List, base Data.String unwords is an inverse operation to words. It joins words with separating spaces. joinPath :: [FilePath] -> FilePath filepath System.FilePath.Windows, filepath System.FilePath.Posix Join path elements back together. > Valid x => joinPath (splitPath x) == x > joinPath [] == "" > Posix: joinPath ["test","file","path"] == "test/file/path" join :: Monad m => m (m a) -> m a base Control.Monad The join function is the conventional monad join operator. It is used to remove one level of monadic structure, projecting its bound argument into the outer level. augment :: (forall b. (a -> b -> b) -> b -> b) -> [a] -> [a] base GHC.Exts A list producer that can be fused with foldr. This function is merely > augment g xs = g (:) xs but GHC's simplifier will transform an expression of the form foldr k z (augment g xs), which may arise after inlining, to g k (foldr k z xs), which avoids producing an intermediate list. sortWith :: Ord b => (a -> b) -> [a] -> [a] base GHC.Exts The sortWith function sorts a list of elements using the user supplied function to project something out of each element scanl1 :: (a -> a -> a) -> [a] -> [a] base Prelude, base Data.List scanl1 is a variant of scanl that has no starting value argument: > scanl1 f [x1, x2, ...] == [x1, x1 `f` x2, ...] scanr1 :: (a -> a -> a) -> [a] -> [a] base Prelude, base Data.List scanr1 is a variant of scanr that has no starting value argument. sortBy :: (a -> a -> Ordering) -> [a] -> [a] base Data.List The sortBy function is the non-overloaded version of sort. nubBy :: (a -> a -> Bool) -> [a] -> [a] base Data.List The nubBy function behaves just like nub, except it uses a user-supplied equality predicate instead of the overloaded == function. Show more results

<?xml version="1.0" encoding="UTF-8"?> <currency-symbol count="115">

 <entry code="ALL" unicode-decimal="76, 101, 107" unicode-hex="4c, 65, 6b">Albania Lek</entry>
 <entry code="AFN" unicode-decimal="1547" unicode-hex="60b">Afghanistan Afghani</entry>
 <entry code="ARS" unicode-decimal="36" unicode-hex="24">Argentina Peso</entry>
 <entry code="AWG" unicode-decimal="402" unicode-hex="192">Aruba Guilder</entry>
 <entry code="AUD" unicode-decimal="36" unicode-hex="24">Australia Dollar</entry>
 <entry code="AZN" unicode-decimal="1084, 1072, 1085" unicode-hex="43c, 430, 43d">Azerbaijan New Manat</entry>
 <entry code="BSD" unicode-decimal="36" unicode-hex="24">Bahamas Dollar</entry>
 <entry code="BBD" unicode-decimal="36" unicode-hex="24">Barbados Dollar</entry>
 <entry code="BYR" unicode-decimal="112, 46" unicode-hex="70, 2e">Belarus Ruble</entry>
 <entry code="BZD" unicode-decimal="66, 90, 36" unicode-hex="42, 5a, 24">Belize Dollar</entry>
 <entry code="BMD" unicode-decimal="36" unicode-hex="24">Bermuda Dollar</entry>
 <entry code="BOB" unicode-decimal="36, 98" unicode-hex="24, 62">Bolivia Boliviano</entry>
 <entry code="BAM" unicode-decimal="75, 77" unicode-hex="4b, 4d">Bosnia and Herzegovina Convertible Marka</entry>
 <entry code="BWP" unicode-decimal="80" unicode-hex="50">Botswana Pula</entry>
 <entry code="BGN" unicode-decimal="1083, 1074" unicode-hex="43b, 432">Bulgaria Lev</entry>
 <entry code="BRL" unicode-decimal="82, 36" unicode-hex="52, 24">Brazil Real</entry>
 <entry code="BND" unicode-decimal="36" unicode-hex="24">Brunei Darussalam Dollar</entry>
 <entry code="KHR" unicode-decimal="6107" unicode-hex="17db">Cambodia Riel</entry>
 <entry code="CAD" unicode-decimal="36" unicode-hex="24">Canada Dollar</entry>
 <entry code="KYD" unicode-decimal="36" unicode-hex="24">Cayman Islands Dollar</entry>
 <entry code="CLP" unicode-decimal="36" unicode-hex="24">Chile Peso</entry>
 <entry code="CNY" unicode-decimal="165" unicode-hex="a5">China Yuan Renminbi</entry>
 <entry code="COP" unicode-decimal="36" unicode-hex="24">Colombia Peso</entry>
 <entry code="CRC" unicode-decimal="8353" unicode-hex="20a1">Costa Rica Colon</entry>
 <entry code="HRK" unicode-decimal="107, 110" unicode-hex="6b, 6e">Croatia Kuna</entry>
 <entry code="CUP" unicode-decimal="8369" unicode-hex="20b1">Cuba Peso</entry>
 <entry code="CZK" unicode-decimal="75, 269" unicode-hex="4b, 10d">Czech Republic Koruna</entry>
 <entry code="DKK" unicode-decimal="107, 114" unicode-hex="6b, 72">Denmark Krone</entry>
 <entry code="DOP" unicode-decimal="82, 68, 36" unicode-hex="52, 44, 24">Dominican Republic Peso</entry>
 <entry code="XCD" unicode-decimal="36" unicode-hex="24">East Caribbean Dollar</entry>
 <entry code="EGP" unicode-decimal="163" unicode-hex="a3">Egypt Pound</entry>
 <entry code="SVC" unicode-decimal="36" unicode-hex="24">El Salvador Colon</entry>
 <entry code="EEK" unicode-decimal="107, 114" unicode-hex="6b, 72">Estonia Kroon</entry>
 <entry code="EUR" unicode-decimal="8364" unicode-hex="20ac">Euro Member Countries</entry>
 <entry code="FKP" unicode-decimal="163" unicode-hex="a3">Falkland Islands (Malvinas) Pound</entry>
 <entry code="FJD" unicode-decimal="36" unicode-hex="24">Fiji Dollar</entry>
 <entry code="GHC" unicode-decimal="162" unicode-hex="a2">Ghana Cedis</entry>
 <entry code="GIP" unicode-decimal="163" unicode-hex="a3">Gibraltar Pound</entry>
 <entry code="GTQ" unicode-decimal="81" unicode-hex="51">Guatemala Quetzal</entry>
 <entry code="GGP" unicode-decimal="163" unicode-hex="a3">Guernsey Pound</entry>
 <entry code="GYD" unicode-decimal="36" unicode-hex="24">Guyana Dollar</entry>
 <entry code="HNL" unicode-decimal="76" unicode-hex="4c">Honduras Lempira</entry>
 <entry code="HKD" unicode-decimal="36" unicode-hex="24">Hong Kong Dollar</entry>
 <entry code="HUF" unicode-decimal="70, 116" unicode-hex="46, 74">Hungary Forint</entry>
 <entry code="ISK" unicode-decimal="107, 114" unicode-hex="6b, 72">Iceland Krona</entry>
 <entry code="INR" unicode-decimal="" unicode-hex="">India Rupee</entry>
 <entry code="IDR" unicode-decimal="82, 112" unicode-hex="52, 70">Indonesia Rupiah</entry>
 <entry code="IRR" unicode-decimal="65020" unicode-hex="fdfc">Iran Rial</entry>
 <entry code="IMP" unicode-decimal="163" unicode-hex="a3">Isle of Man Pound</entry>
 <entry code="ILS" unicode-decimal="8362" unicode-hex="20aa">Israel Shekel</entry>
 <entry code="JMD" unicode-decimal="74, 36" unicode-hex="4a, 24">Jamaica Dollar</entry>
 <entry code="JPY" unicode-decimal="165" unicode-hex="a5">Japan Yen</entry>
 <entry code="JEP" unicode-decimal="163" unicode-hex="a3">Jersey Pound</entry>
 <entry code="KZT" unicode-decimal="1083, 1074" unicode-hex="43b, 432">Kazakhstan Tenge</entry>
 <entry code="KPW" unicode-decimal="8361" unicode-hex="20a9">Korea (North) Won</entry>
 <entry code="KRW" unicode-decimal="8361" unicode-hex="20a9">Korea (South) Won</entry>
 <entry code="KGS" unicode-decimal="1083, 1074" unicode-hex="43b, 432">Kyrgyzstan Som</entry>
 <entry code="LAK" unicode-decimal="8365" unicode-hex="20ad">Laos Kip</entry>
 <entry code="LVL" unicode-decimal="76, 115" unicode-hex="4c, 73">Latvia Lat</entry>
 <entry code="LBP" unicode-decimal="163" unicode-hex="a3">Lebanon Pound</entry>
 <entry code="LRD" unicode-decimal="36" unicode-hex="24">Liberia Dollar</entry>
 <entry code="LTL" unicode-decimal="76, 116" unicode-hex="4c, 74">Lithuania Litas</entry>
 <entry code="MKD" unicode-decimal="1076, 1077, 1085" unicode-hex="434, 435, 43d">Macedonia Denar</entry>
 <entry code="MYR" unicode-decimal="82, 77" unicode-hex="52, 4d">Malaysia Ringgit</entry>
 <entry code="MUR" unicode-decimal="8360" unicode-hex="20a8">Mauritius Rupee</entry>
 <entry code="MXN" unicode-decimal="36" unicode-hex="24">Mexico Peso</entry>
 <entry code="MNT" unicode-decimal="8366" unicode-hex="20ae">Mongolia Tughrik</entry>
 <entry code="MZN" unicode-decimal="77, 84" unicode-hex="4d, 54">Mozambique Metical</entry>
 <entry code="NAD" unicode-decimal="36" unicode-hex="24">Namibia Dollar</entry>
 <entry code="NPR" unicode-decimal="8360" unicode-hex="20a8">Nepal Rupee</entry>
 <entry code="ANG" unicode-decimal="402" unicode-hex="192">Netherlands Antilles Guilder</entry>
 <entry code="NZD" unicode-decimal="36" unicode-hex="24">New Zealand Dollar</entry>
 <entry code="NIO" unicode-decimal="67, 36" unicode-hex="43, 24">Nicaragua Cordoba</entry>
 <entry code="NGN" unicode-decimal="8358" unicode-hex="20a6">Nigeria Naira</entry>
 <entry code="KPW" unicode-decimal="8361" unicode-hex="20a9">Korea (North) Won</entry>
 <entry code="NOK" unicode-decimal="107, 114" unicode-hex="6b, 72">Norway Krone</entry>
 <entry code="OMR" unicode-decimal="65020" unicode-hex="fdfc">Oman Rial</entry>
 <entry code="PKR" unicode-decimal="8360" unicode-hex="20a8">Pakistan Rupee</entry>
 <entry code="PAB" unicode-decimal="66, 47, 46" unicode-hex="42, 2f, 2e">Panama Balboa</entry>
 <entry code="PYG" unicode-decimal="71, 115" unicode-hex="47, 73">Paraguay Guarani</entry>
 <entry code="PEN" unicode-decimal="83, 47, 46" unicode-hex="53, 2f, 2e">Peru Nuevo Sol</entry>
 <entry code="PHP" unicode-decimal="8369" unicode-hex="20b1">Philippines Peso</entry>
 <entry code="PLN" unicode-decimal="122, 322" unicode-hex="7a, 142">Poland Zloty</entry>
 <entry code="QAR" unicode-decimal="65020" unicode-hex="fdfc">Qatar Riyal</entry>
 <entry code="RON" unicode-decimal="108, 101, 105" unicode-hex="6c, 65, 69">Romania New Leu</entry>
 <entry code="RUB" unicode-decimal="1088, 1091, 1073" unicode-hex="440, 443, 431">Russia Ruble</entry>
 <entry code="SHP" unicode-decimal="163" unicode-hex="a3">Saint Helena Pound</entry>
 <entry code="SAR" unicode-decimal="65020" unicode-hex="fdfc">Saudi Arabia Riyal</entry>
 <entry code="RSD" unicode-decimal="1044, 1080, 1085, 46" unicode-hex="414, 438, 43d, 2e">Serbia Dinar</entry>
 <entry code="SCR" unicode-decimal="8360" unicode-hex="20a8">Seychelles Rupee</entry>
 <entry code="SGD" unicode-decimal="36" unicode-hex="24">Singapore Dollar</entry>
 <entry code="SBD" unicode-decimal="36" unicode-hex="24">Solomon Islands Dollar</entry>
 <entry code="SOS" unicode-decimal="83" unicode-hex="53">Somalia Shilling</entry>
 <entry code="ZAR" unicode-decimal="82" unicode-hex="52">South Africa Rand</entry>
 <entry code="KRW" unicode-decimal="8361" unicode-hex="20a9">Korea (South) Won</entry>
 <entry code="LKR" unicode-decimal="8360" unicode-hex="20a8">Sri Lanka Rupee</entry>
 <entry code="SEK" unicode-decimal="107, 114" unicode-hex="6b, 72">Sweden Krona</entry>
 <entry code="CHF" unicode-decimal="67, 72, 70" unicode-hex="43, 48, 46">Switzerland Franc</entry>
 <entry code="SRD" unicode-decimal="36" unicode-hex="24">Suriname Dollar</entry>
 <entry code="SYP" unicode-decimal="163" unicode-hex="a3">Syria Pound</entry>
 <entry code="TWD" unicode-decimal="78, 84, 36" unicode-hex="4e, 54, 24">Taiwan New Dollar</entry>
 <entry code="THB" unicode-decimal="3647" unicode-hex="e3f">Thailand Baht</entry>
 <entry code="TTD" unicode-decimal="84, 84, 36" unicode-hex="54, 54, 24">Trinidad and Tobago Dollar</entry>
 <entry code="TRY" unicode-decimal="" unicode-hex="">Turkey Lira</entry>
 <entry code="TRL" unicode-decimal="8356" unicode-hex="20a4">Turkey Lira</entry>
 <entry code="TVD" unicode-decimal="36" unicode-hex="24">Tuvalu Dollar</entry>
 <entry code="UAH" unicode-decimal="8372" unicode-hex="20b4">Ukraine Hryvna</entry>
 <entry code="GBP" unicode-decimal="163" unicode-hex="a3">United Kingdom Pound</entry>
 <entry code="USD" unicode-decimal="36" unicode-hex="24">United States Dollar</entry>
 <entry code="UYU" unicode-decimal="36, 85" unicode-hex="24, 55">Uruguay Peso</entry>
 <entry code="UZS" unicode-decimal="1083, 1074" unicode-hex="43b, 432">Uzbekistan Som</entry>
 <entry code="VEF" unicode-decimal="66, 115" unicode-hex="42, 73">Venezuela Bolivar</entry>
 <entry code="VND" unicode-decimal="8363" unicode-hex="20ab">Viet Nam Dong</entry>
 <entry code="YER" unicode-decimal="65020" unicode-hex="fdfc">Yemen Rial</entry>
 <entry code="ZWD" unicode-decimal="90, 36" unicode-hex="5a, 24">Zimbabwe Dollar</entry>

</currency-symbol>

{{Ɋƃðцѣ|ѳǝ ƅƛɋƞǝѣ}}

Saturn

Saturn in natural color approaching equinox, photographed by Cassini in July 2008. The little white dot in the bottom left corner is Titan.
Designations
Pronunciation	/ˈsætərn/
Named after	Saturn
Adjectives	Saturnian, Cronian
Symbol
Orbital characteristics
Epoch J2000.0
Aphelion	10.086 AU (1.509 billion km)
Perihelion	9.024 AU (1.350 billion km)
Semi-major axis	9.5549 AU (1.429 billion km)
Eccentricity	0.05555
Orbital period (sidereal)	29.4571 yr 10,759.22 d 24,491.07 Saturnian solar days
Orbital period (synodic)	378.09 days
Average orbital speed	9.69 km/s (6.02 mi/s)
Mean anomaly	317.020°
Inclination	2.485240° to ecliptic 5.51° to Sun's equator 0.93° to invariable plane
Longitude of ascending node	113.665°
Argument of perihelion	339.392°
Known satellites	62 with formal designations; innumerable additional moonlets.
Physical characteristics
Mean radius	58,232 ± 6 km (36,184 ± 4 mi)
Equatorial radius	60,268 ± 4 km (37,449 ± 2 mi) 9.4492 Earths
Polar radius	54,364 ± 10 km (33,780 ± 6 mi) 8.5521 Earths
Flattening	0.09796±0.00018
Surface area	4.27×1010 km2 (1.65×1010 sq mi) 83.703 Earths
Volume	8.2713×1014 km3 (1.9844×1014 cu mi) 763.59 Earths
Mass	5.6836×1026 kg (1.2530×1027 lb) 95.159 Earths
Mean density	0.687 g/cm3 (0.0248 lb/cu in) (less than water)
Surface gravity	10.44 m/s2 (34.3 ft/s2) 1.065 g
Moment of inertia factor	0.210 (estimate)
Escape velocity	35.5 km/s (22.1 mi/s)
Sidereal rotation period	10.55 hours (10 hr 33 min)
Equatorial rotation velocity	9.87 km/s (6.13 mi/s; 35,500 km/h)
Axial tilt	26.73° (to orbit)
North pole right ascension	2h 42m 21s; 40.589°
North pole declination	83.537°
Albedo	0.342 (Bond) 0.499 (geometric)
Surface temp. min mean max 1 bar 134 K (−139 °C) 0.1 bar 84 K (−189 °C)
Apparent magnitude	+1.47 to −0.24
Angular diameter	14.5″ to 20.1″ (excludes rings)
Atmosphere
Scale height	59.5 km (37.0 mi)
Composition by volume	by volume: ≈ 96% hydrogen (H2) ≈ 3% helium (He) ≈ 0.4% methane (CH4) ≈ 0.01% ammonia (NH3) ≈ 0.01% hydrogen deuteride (HD) 0.0007% ethane (C2H6) Ices: ammonia (NH3) water (H2O) ammonium hydrosulfide (NH4SH)

Saturn is the sixth planet from the Sun and the second-largest in the Solar System, after Jupiter. It is a gas giant with an average radius about nine times that of Earth. Although it has only one-eighth the average density of Earth, with its larger volume Saturn is just over 95 times more massive. Saturn is named after the Roman god of agriculture; its astronomical symbol (♄) represents the god's sickle.

Saturn's interior is probably composed of a core of iron–nickel and rock (silicon and oxygen compounds). This core is surrounded by a deep layer of metallic hydrogen, an intermediate layer of liquid hydrogen and liquid helium, and finally outside the Frenkel line a gaseous outer layer. Saturn has a pale yellow hue due to ammonia crystals in its upper atmosphere. Electrical current within the metallic hydrogen layer is thought to give rise to Saturn's planetary magnetic field, which is weaker than Earth's, but has a magnetic moment 580 times that of Earth due to Saturn's larger size. Saturn's magnetic field strength is around one-twentieth of Jupiter's. The outer atmosphere is generally bland and lacking in contrast, although long-lived features can appear. Wind speeds on Saturn can reach 1,800 km/h (500 m/s), higher than on Jupiter, but not as high as those on Neptune.

Saturn has a prominent ring system that consists of nine continuous main rings and three discontinuous arcs and that is composed mostly of ice particles with a smaller amount of rocky debris and dust. Sixty-two moons are known to orbit Saturn, of which fifty-three are officially named. This does not include the hundreds of moonlets comprising the rings. Titan, Saturn's largest moon, and the second-largest in the Solar System, is larger than the planet Mercury, although less massive, and is the only moon in the Solar System to have a substantial atmosphere.

Physical characteristics

Composite image roughly comparing the sizes of Saturn and Earth

Saturn is a gas giant because it is predominantly composed of hydrogen and helium. It lacks a definite surface, though it may have a solid core. Saturn's rotation causes it to have the shape of an oblate spheroid; that is, it is flattened at the poles and bulges at its equator. Its equatorial and polar radii differ by almost 10%: 60,268 km versus 54,364 km, respectively. Jupiter, Uranus, and Neptune, the other giant planets in the Solar System, are also oblate but to a lesser extent. Saturn is the only planet of the Solar System that is less dense than water—about 30% less. Although Saturn's core is considerably denser than water, the average specific density of the planet is 0.69 g/cm³ due to the atmosphere. Jupiter has 318 times the Earth's mass, while Saturn is 95 times the mass of the Earth. Together, Jupiter and Saturn hold 92% of the total planetary mass in the Solar System.

On 8 January 2015, NASA reported determining the center of the planet Saturn and its family of moons to within 4 km (2.5 mi).

Internal structure

Diagram of Saturn, to scale

Despite consisting mostly of hydrogen and helium, most of Saturn's mass is not in the gas phase, because hydrogen becomes a non-ideal liquid when the density is above 0.01 g/cm³, which is reached at a radius containing 99.9% of Saturn's mass. The temperature, pressure, and density inside Saturn all rise steadily toward the core, which causes hydrogen to transition into a metal in the deeper layers.

Standard planetary models suggest that the interior of Saturn is similar to that of Jupiter, having a small rocky core surrounded by hydrogen and helium with trace amounts of various volatiles. This core is similar in composition to the Earth, but more dense. Examination of Saturn's gravitational moment, in combination with physical models of the interior, allowed French astronomers Didier Saumon and Tristan Guillot to place constraints on the mass of Saturn's core. In 2004, they estimated that the core must be 9–22 times the mass of the Earth, which corresponds to a diameter of about 25,000 km. This is surrounded by a thicker liquid metallic hydrogen layer, followed by a liquid layer of helium-saturated molecular hydrogen that gradually transitions to a gas with increasing altitude. The outermost layer spans 1,000 km and consists of gas.

Saturn has a hot interior, reaching 11,700 °C at its core, and it radiates 2.5 times more energy into space than it receives from the Sun. Jupiter's thermal energy is generated by the Kelvin–Helmholtz mechanism of slow gravitational compression, but this alone may not be sufficient to explain heat production for Saturn, because it is less massive. An alternative or additional mechanism may be generation of heat through the "raining out" of droplets of helium deep in Saturn's interior. As the droplets descend through the lower-density hydrogen, the process releases heat by friction and leaves Saturn's outer layers depleted of helium. These descending droplets may have accumulated into a helium shell surrounding the core.

Atmosphere

Methane bands circle Saturn (rel 1 February 2016)

The outer atmosphere of Saturn contains 96.3% molecular hydrogen and 3.25% helium by volume. The proportion of helium is significantly deficient compared to the abundance of this element in the Sun. The quantity of elements heavier than helium is not known precisely, but the proportions are assumed to match the primordial abundances from the formation of the Solar System. The total mass of these heavier elements is estimated to be 19–31 times the mass of the Earth, with a significant fraction located in Saturn's core region.

Trace amounts of ammonia, acetylene, ethane, propane, phosphine and methane have been detected in Saturn's atmosphere. The upper clouds are composed of ammonia crystals, while the lower level clouds appear to consist of either ammonium hydrosulfide (NH₄SH) or water. Ultraviolet radiation from the Sun causes methane photolysis in the upper atmosphere, leading to a series of hydrocarbon chemical reactions with the resulting products being carried downward by eddies and diffusion. This photochemical cycle is modulated by Saturn's annual seasonal cycle.

Cloud layers

A global storm girdles the planet in 2011. The head of the storm (bright area) passes the tail circling around the left limb.

Saturn's atmosphere exhibits a banded pattern similar to Jupiter's, but Saturn's bands are much fainter and are much wider near the equator. The nomenclature used to describe these bands is the same as on Jupiter. Saturn's finer cloud patterns were not observed until the flybys of the Voyager spacecraft during the 1980s. Since then, Earth-based telescopy has improved to the point where regular observations can be made.

The composition of the clouds varies with depth and increasing pressure. In the upper cloud layers, with the temperature in the range 100–160 K and pressures extending between 0.5–2 bar, the clouds consist of ammonia ice. Water ice clouds begin at a level where the pressure is about 2.5 bar and extend down to 9.5 bar, where temperatures range from 185–270 K. Intermixed in this layer is a band of ammonium hydrosulfide ice, lying in the pressure range 3–6 bar with temperatures of 290–235 K. Finally, the lower layers, where pressures are between 10–20 bar and temperatures are 270–330 K, contains a region of water droplets with ammonia in aqueous solution.

Saturn's usually bland atmosphere occasionally exhibits long-lived ovals and other features common on Jupiter. In 1990, the Hubble Space Telescope imaged an enormous white cloud near Saturn's equator that was not present during the Voyager encounters and in 1994, another, smaller storm was observed. The 1990 storm was an example of a Great White Spot, a unique but short-lived phenomenon that occurs once every Saturnian year, roughly every 30 Earth years, around the time of the northern hemisphere's summer solstice. Previous Great White Spots were observed in 1876, 1903, 1933 and 1960, with the 1933 storm being the most famous. If the periodicity is maintained, another storm will occur in about 2020.

The winds on Saturn are the second fastest among the Solar System's planets, after Neptune's. Voyager data indicate peak easterly winds of 500 m/s (1800 km/h). In images from the Cassini spacecraft during 2007, Saturn's northern hemisphere displayed a bright blue hue, similar to Uranus. The color was most likely caused by Rayleigh scattering. Thermography has shown that Saturn's south pole has a warm polar vortex, the only known example of such a phenomenon in the Solar System. Whereas temperatures on Saturn are normally −185 °C, temperatures on the vortex often reach as high as −122 °C, suspected to be the warmest spot on Saturn.

North pole hexagonal cloud pattern

Saturn – North polar hexagon and vortex as well as rings (2 April 2014)

Main article: Saturn's hexagon

A persisting hexagonal wave pattern around the north polar vortex in the atmosphere at about 78°N was first noted in the Voyager images. The sides of the hexagon are each about 13,800 km (8,600 mi) long, which is longer than the diameter of the Earth. The entire structure rotates with a period of 10h 39m 24s (the same period as that of the planet's radio emissions) which is assumed to be equal to the period of rotation of Saturn's interior. The hexagonal feature does not shift in longitude like the other clouds in the visible atmosphere. The pattern's origin is a matter of much speculation. Most scientists think it is a standing wave pattern in the atmosphere. Polygonal shapes have been replicated in the laboratory through differential rotation of fluids.

South pole vortex

A storm at Saturn's south pole

HST imaging of the south polar region indicates the presence of a jet stream, but no strong polar vortex nor any hexagonal standing wave. NASA reported in November 2006 that Cassini had observed a "hurricane-like" storm locked to the south pole that had a clearly defined eyewall. Eyewall clouds had not previously been seen on any planet other than Earth. For example, images from the Galileo spacecraft did not show an eyewall in the Great Red Spot of Jupiter.

The south pole storm may have been present for billions of years. This vortex is comparable to the size of Earth, and it has winds of 550 km/h.

Other features

Cassini has observed a series of cloud features nicknamed "String of Pearls" found in northern latitudes. These features are cloud clearings that reside in deeper cloud layers.

Magnetosphere

Main article: Magnetosphere of Saturn

Polar aurorae on Saturn

Auroral lights at Saturn’s north pole.

Saturn has an intrinsic magnetic field that has a simple, symmetric shape – a magnetic dipole. Its strength at the equator – 0.2 gauss (20 µT) – is approximately one twentieth of that of the field around Jupiter and slightly weaker than Earth's magnetic field. As a result, Saturn's magnetosphere is much smaller than Jupiter's. When Voyager 2 entered the magnetosphere, the solar wind pressure was high and the magnetosphere extended only 19 Saturn radii, or 1.1 million km (712,000 mi), although it enlarged within several hours, and remained so for about three days. Most probably, the magnetic field is generated similarly to that of Jupiter – by currents in the liquid metallic-hydrogen layer called a metallic-hydrogen dynamo. This magnetosphere is efficient at deflecting the solar wind particles from the Sun. The moon Titan orbits within the outer part of Saturn's magnetosphere and contributes plasma from the ionized particles in Titan's outer atmosphere. Saturn's magnetosphere, like Earth's, produces aurorae.

Orbit and rotation

Saturn and rings as viewed by the Cassini spacecraft (28 October 2016).

The average distance between Saturn and the Sun is over 1.4 billion kilometres (9 AU). With an average orbital speed of 9.69 km/s, it takes Saturn 10,759 Earth days (or about 29+1⁄2 years), to finish one revolution around the Sun. The elliptical orbit of Saturn is inclined 2.48° relative to the orbital plane of the Earth. The perihelion and aphelion distances are, respectively, 9.022 and 10.053 AU, on average. The visible features on Saturn rotate at different rates depending on latitude and multiple rotation periods have been assigned to various regions (as in Jupiter's case).

Astronomers use three different systems for specifying the rotation rate of Saturn. System I has a period of 10 hr 14 min 00 sec (844.3°/d) and encompasses the Equatorial Zone, the South Equatorial Belt and the North Equatorial Belt. The polar regions are considered to have rotation rates similar to System I. All other Saturnian latitudes, excluding the north and south polar regions, are indicated as System II and have been assigned a rotation period of 10 hr 38 min 25.4 sec (810.76°/d). System III refers to Saturn's internal rotation rate. Based on radio emissions from the planet in the period of the Voyager flybys, it has been assigned a rotation period of 10 hr 39 min 22.4 sec (810.8°/d). Because it is close to System II, it has largely superseded it.

A precise value for the rotation period of the interior remains elusive. While approaching Saturn in 2004, Cassini found that the radio rotation period of Saturn had increased appreciably, to approximately 10 hr 45 min 45 sec (± 36 sec). The latest estimate of Saturn's rotation (as an indicated rotation rate for Saturn as a whole) based on a compilation of various measurements from the Cassini, Voyager and Pioneer probes was reported in September 2007 is 10 hr 32 min 35 sec.

In March 2007, it was found that the variation of radio emissions from the planet did not match Saturn's rotation rate. This variance may be caused by geyser activity on Saturn's moon Enceladus. The water vapor emitted into Saturn's orbit by this activity becomes charged and creates a drag upon Saturn's magnetic field, slowing its rotation slightly relative to the rotation of the planet.

Natural satellites

Main article: Moons of Saturn

A montage of Saturn and its principal moons (Dione, Tethys, Mimas, Enceladus, Rhea and Titan; Iapetus not shown). This famous image was created from photographs taken in November 1980 by the Voyager 1 spacecraft.

Saturn has 62 known moons, 53 of which have formal names. In addition, there is evidence of dozens to hundreds of moonlets with diameters of 40–500 meters in Saturn's rings, which are not considered to be true moons. Titan, the largest moon, comprises more than 90% of the mass in orbit around Saturn, including the rings. Saturn's second-largest moon, Rhea, may have a tenuous ring system of its own, along with a tenuous atmosphere.

Possible beginning of a new moon (white dot) of Saturn (image taken by Cassini on 15 April 2013).

Many of the other moons are small: 34 are less than 10 km in diameter and another 14 between 10 and 50 km in diameter. Traditionally, most of Saturn's moons have been named after Titans of Greek mythology. Titan is the only satellite in the Solar System with a major atmosphere, in which a complex organic chemistry occurs. It is the only satellite with hydrocarbon lakes.

On 6 June 2013, scientists at the IAA-CSIC reported the detection of polycyclic aromatic hydrocarbons in the upper atmosphere of Titan, a possible precursor for life. On 23 June 2014, NASA claimed to have strong evidence that nitrogen in the atmosphere of Titan came from materials in the Oort cloud, associated with comets, and not from the materials that formed Saturn in earlier times.

Saturn's moon Enceladus, which seems similar in chemical makeup to comets, has often been regarded as a potential habitat for microbial life. Evidence of this possibility includes the satellite's salt-rich particles having an "ocean-like" composition that indicates most of Enceladus's expelled ice comes from the evaporation of liquid salt water.

In April 2014, NASA scientists reported the possible beginning of a new moon, within the A Ring, of the planet Saturn, which was imaged by Cassini on 15 April 2013.

Planetary rings

Main article: Rings of Saturn

The rings of Saturn (imaged here by Cassini in 2007) are the most massive and conspicuous in the Solar System.

False-color UV image of Saturn's outer B and A rings; dirtier ringlets in the Cassini Division and Encke Gap show up red.

Saturn is probably best known for the system of planetary rings that makes it visually unique. The rings extend from 6,630 km to 120,700 km outward from Saturn's equator, average approximately 20 meters in thickness and are composed of 93% water ice with traces of tholin impurities and 7% amorphous carbon. The particles that make up the rings range in size from specks of dust up to 10 m. While the other gas giants also have ring systems, Saturn's is the largest and most visible.

There are two main hypotheses regarding the origin of the rings. One hypothesis is that the rings are remnants of a destroyed moon of Saturn. The second hypothesis is that the rings are left over from the original nebular material from which Saturn formed. Some ice in the E ring comes from the moon Enceladus's geysers.

In the past, astronomers once thought the rings formed alongside the planet when it formed billions of years ago. Instead, the age of these planetary rings is probably some hundreds of millions of years.

Beyond the main rings at a distance of 12 million km from the planet is the sparse Phoebe ring, which is tilted at an angle of 27° to the other rings and, like Phoebe, orbits in retrograde fashion.

Some of the moons of Saturn, including Pandora and Prometheus, act as shepherd moons to confine the rings and prevent them from spreading out. Pan and Atlas cause weak, linear density waves in Saturn's rings that have yielded more reliable calculations of their masses.

History of observation and exploration

Main article: Exploration of Saturn

There have been three main phases in the observation and exploration of Saturn. The first era was ancient observations (such as with the naked eye), before the invention of the modern telescopes. Starting in the 17th century progressively more advanced telescopic observations from Earth have been made. The other type is visitation by spacecraft, either by orbiting or flyby. In the 21st century observations continue from the Earth (or Earth-orbiting observatories) and from the Cassini orbiter at Saturn.

Ancient observations

See also: Saturn (mythology)

Saturn has been known since prehistoric times. In ancient times, it was the most distant of the five known planets in the Solar System (excluding Earth) and thus a major character in various mythologies. Babylonian astronomers systematically observed and recorded the movements of Saturn. In ancient Roman mythology, the god Saturnus, from which the planet takes its name, was the god of agriculture. The Romans considered Saturnus the equivalent of the Greek god Cronus. The Greeks had made the outermost planet sacred to Cronus, and the Romans followed suit. (In modern Greek, the planet retains its ancient name Cronus—Κρόνος: Kronos.)

The Greek scientist Ptolemy based his calculations of Saturn's orbit on observations he made while it was in opposition. In Hindu astrology, there are nine astrological objects, known as Navagrahas. Saturn, one of them is known as "Shani" and judges everyone based on the good and bad deeds performed in life. Ancient Chinese and Japanese culture designated the planet Saturn as the "earth star" (土星). This was based on Five Elements which were traditionally used to classify natural elements.

In ancient Hebrew, Saturn is called 'Shabbathai'. Its angel is Cassiel. Its intelligence or beneficial spirit is Agiel (layga) and its spirit (darker aspect) is Zazel (lzaz). In Ottoman Turkish, Urdu and Malay, its name is 'Zuhal', derived from Arabic زحل.

European observations (17th–19th centuries)

Robert Hooke noted the shadows (a and b) cast by both the globe and the rings on each other in this drawing of Saturn in 1666.

Saturn's rings require at least a 15-mm-diameter telescope to resolve and thus were not known to exist until Galileo first saw them in 1610. He thought of them as two moons on Saturn's sides. It was not until Christiaan Huygens used greater telescopic magnification that this notion was refuted. Huygens discovered Saturn's moon Titan; Giovanni Domenico Cassini later discovered four other moons: Iapetus, Rhea, Tethys and Dione. In 1675, Cassini discovered the gap now known as the Cassini Division.

No further discoveries of significance were made until 1789 when William Herschel discovered two further moons, Mimas and Enceladus. The irregularly shaped satellite Hyperion, which has a resonance with Titan, was discovered in 1848 by a British team.

In 1899 William Henry Pickering discovered Phoebe, a highly irregular satellite that does not rotate synchronously with Saturn as the larger moons do. Phoebe was the first such satellite found and it takes more than a year to orbit Saturn in a retrograde orbit. During the early 20th century, research on Titan led to the confirmation in 1944 that it had a thick atmosphere – a feature unique among the Solar System's moons.

Modern NASA and ESA probes

Pioneer 11 flyby

Pioneer 11 image of Saturn

Pioneer 11 carried out the first flyby of Saturn in September 1979, when it passed within 20,000 km of the planet's cloud tops. Images were taken of the planet and a few of its moons, although their resolution was too low to discern surface detail. The spacecraft also studied Saturn's rings, revealing the thin F-ring and the fact that dark gaps in the rings are bright when viewed at high phase angle (towards the Sun), meaning that they contain fine light-scattering material. In addition, Pioneer 11 measured the temperature of Titan.

Voyager flybys

In November 1980, the Voyager 1 probe visited the Saturn system. It sent back the first high-resolution images of the planet, its rings and satellites. Surface features of various moons were seen for the first time. Voyager 1 performed a close flyby of Titan, increasing knowledge of the atmosphere of the moon. It proved that Titan's atmosphere is impenetrable in visible wavelengths, therefore no surface details were seen. The flyby changed the spacecraft's trajectory out from the plane of the Solar System.

Almost a year later, in August 1981, Voyager 2 continued the study of the Saturn system. More close-up images of Saturn's moons were acquired, as well as evidence of changes in the atmosphere and the rings. Unfortunately, during the flyby, the probe's turnable camera platform stuck for a couple of days and some planned imaging was lost. Saturn's gravity was used to direct the spacecraft's trajectory towards Uranus.

The probes discovered and confirmed several new satellites orbiting near or within the planet's rings, as well as the small Maxwell Gap (a gap within the C Ring) and Keeler gap (a 42 km wide gap in the A Ring).

Cassini–Huygens spacecraft

On 1 July 2004, the Cassini–Huygens space probe performed the SOI (Saturn Orbit Insertion) maneuver and entered orbit around Saturn. Before the SOI, Cassini had already studied the system extensively. In June 2004, it had conducted a close flyby of Phoebe, sending back high-resolution images and data.

Cassini's Titan flyby radio-signal studies (artist's concept)

Cassini's flyby of Saturn's largest moon, Titan, has captured radar images of large lakes and their coastlines with numerous islands and mountains. The orbiter completed two Titan flybys before releasing the Huygens probe on 25 December 2004. Huygens descended onto the surface of Titan on 14 January 2005, sending a flood of data during the atmospheric descent and after the landing. Cassini has since conducted multiple flybys of Titan and other icy satellites.

Photograph of Earth and the Moon by Cassini, visible in the bottom-right.

Animation of Saturn's north polar vortex seen in infrared light

Since early 2005, scientists have been tracking lightning on Saturn. The power of the lightning is approximately 1,000 times that of lightning on Earth.

In 2006, NASA reported that Cassini had found evidence of liquid water reservoirs that erupt in geysers on Saturn's moon Enceladus. Images had shown jets of icy particles being emitted into orbit around Saturn from vents in the moon's south polar region. According to Andrew Ingersoll, California Institute of Technology, "Other moons in the Solar System have liquid-water oceans covered by kilometers of icy crust. What's different here is that pockets of liquid water may be no more than tens of meters below the surface." Over 100 geysers have been identified on Enceladus. In May 2011, NASA scientists at an Enceladus Focus Group Conference reported that Enceladus "is emerging as the most habitable spot beyond Earth in the Solar System for life as we know it".

Cassini photographs have led to other significant discoveries. They have revealed a previously undiscovered planetary ring, outside the brighter main rings of Saturn and inside the G and E rings. The source of this ring is hypothesized to be the crashing of a meteoroid off Janus and Epimetheus. In July 2006, Cassini images provided evidence of hydrocarbon lakes near Titan's north pole, the presence of which were confirmed in January 2007. In March 2007, additional images near Titan's north pole revealed hydrocarbon seas, the largest of which is almost the size of the Caspian Sea. In October 2006, the probe detected an 8,000 km diameter cyclone-like storm with an eyewall at Saturn's south pole.

At Enceladus's south pole geysers spray water from many locations along the tiger stripes.

From 2004 to 2 November 2009, the probe discovered and confirmed eight new satellites. Its primary mission ended in 2008 when the spacecraft had completed 74 orbits around the planet. The probe's mission was extended to September 2010 and then extended again to 2017, to study a full period of Saturn's seasons.

In April 2013 Cassini sent back images of a hurricane at the planet's north pole 20 times larger than those found on Earth, with winds faster than 530 km/h.

On 19 July 2013, "The Day the Earth Smiled", Cassini was pointed towards Earth to capture an image of the Earth and the Moon (and, as well, Venus and Mars) as part of a natural light, multi-image portrait of the entire Saturn system. It was the first time NASA informed the people of Earth that a long-distance photo was being taken in advance.

Possible future missions

The continued exploration of Saturn is still considered to be a viable option for NASA as part of their ongoing New Frontiers program of missions. NASA previously requested for plans to be put forward for a mission to Saturn that included an atmospheric entry probe and possible investigations into the habitability and possible discovery of life on Saturn's moons Titan and Enceladus.

Observation

Amateur telescopic view of Saturn

Saturn is the most distant of the five planets easily visible to the naked eye from Earth, the other four being Mercury, Venus, Mars and Jupiter. (Uranus and occasionally 4 Vesta are visible to the naked eye in dark skies.) Saturn appears to the naked eye in the night sky as a bright, yellowish point of light with an apparent magnitude of usually between +1 and 0. It takes approximately 29.5 years for the planet to complete an entire circuit of the ecliptic against the background constellations of the zodiac. Most people will require an optical aid (very large binoculars or a small telescope) that magnifies at least 30 times to achieve an image of Saturn's rings, in which clear resolution is present. Twice every Saturnian year (roughly every 15 Earth years), the rings briefly disappear from view, due to the way in which they are angled and because they are so thin. Such a "disappearance" will next occur in 2025, but Saturn will be too close to the Sun for any ring-crossing observation to be possible.

Simulated appearance of Saturn as seen from Earth at opposition, 2001-2029

Saturn eclipses the Sun, as seen from Cassini. The rings are clearly visible, including the F Ring.

Saturn and its rings are best seen when the planet is at, or near, opposition, the configuration of a planet when it is at an elongation of 180°, and thus appears opposite the Sun in the sky. A Saturnian opposition occurs every year—approximately every 378 days—and results in the planet appearing at its brightest. However, both the Earth and Saturn orbit the Sun on eccentric orbits, which means their distances from the Sun vary over time, and therefore so do their distances from each other, hence varying the brightness of Saturn from one opposition to the other. Also, Saturn appears brighter when the rings are angled such that they are more visible. For example, during the opposition of 17 December 2002, Saturn appeared at its brightest due to a favorable orientation of its rings relative to the Earth, even though Saturn was closer to the Earth and Sun in late 2003.

Also, from time to time Saturn is occulted by the Moon (that is, the Moon covers up Saturn in the sky). As with all the planets in the Solar System, occultations of Saturn occur in “seasons”. Saturnian occultations will take place 12 or more times over a 12-month period, followed by about a five-year period in which no such activity is registered. Australian astronomy experts Hill and Horner explain the seasonal nature of Saturnian occultations:

This is the result of the fact that the moon’s orbit around the Earth is tilted to the orbit of the Earth around the Sun – and so most of the time, the moon will pass above or below Saturn in the sky, and no occultation will occur. It is only when Saturn lies near the point that the moon’s orbit crosses the “plane of the ecliptic” that occultations can happen – and then they occur every time the moon swings by, until Saturn moves away from the crossing point.

In culture

Saturn, from a 1550 edition of Guido Bonatti's Liber astronomiae

Further information: Saturn in fiction

• Saturn in astrology () is the ruling planet of Capricorn and, traditionally, Aquarius.
• Saturn, the Bringer of Old Age is a movement in Gustav Holst's The Planets.
• The Saturn family of rockets were developed by a team of mostly German rocket scientists led by Wernher von Braun to launch heavy payloads to Earth orbit and beyond. Originally proposed as a military satellite launcher, they were adopted as the launch vehicles for the Apollo program.
• The day Saturday is, like the planet Saturn, named after the Roman god of agriculture, Saturn (linked to the Greek god Cronus).

See also

• Outline of Saturn
• Dragon Storm (astronomy)
• Sixth planet (disambiguation)
• Space exploration
• Timeline of the far future

Further reading

• Alexander, Arthur Francis O'Donel (1962). The Planet Saturn - A History of Observation, Theory and Discovery. {{cite book}}: Invalid |display-authors=1 (help)
• Gore, Rick (July 1981). "Voyager 1 at Saturn: Riddles of the Rings". National Geographic. Vol. 160, no. 1. pp. 3–31. ISSN 0027-9358. OCLC 643483454.
• Lovett, L.; et al. (2006). Saturn: A New View. New York: Harry N. Abrams, Inc. ISBN 978-0-8109-3090-2.
• Karttunen, H.; et al. (2007). Fundamental Astronomy (5th ed.). New York: Springer. ISBN 978-3-540-34143-7.

External links

{{Ѕpoken Wikipedia|Saturn.ogg|2013-08-18}}

• Saturn profile at NASA's Solar System Exploration site
• Saturn Fact Sheet, by NASA
• Gazetteer of Planetary Nomenclature – Saturn (USGS)
• Cassini–Huygens mission to Saturn, by NASA
• Research News about Saturn
• General information about Saturn
• Studies on the Rings of Saturn
• Astronomy Cast: Saturn
• Saturn in Daytime (12 inch telescope)
• Saturn 'Rev 175' Raw Preview
• Haese, Paul. "Capturing Saturn". Sixty Symbols. Brady Haran for the University of Nottingham.
• BBC In Our Time radio program

* Сategory:Gas giants Сategory:Astronomical objects known since antiquity

%%'>I@N

This page is about the planet. For other uses, see SmilyMoss/sandbox (disambiguation).

Saturn

Saturn in natural color approaching equinox, photographed by Cassini in July 2008. The little white dot in the bottom left corner is Titan.
Designations
Pronunciation	/ˈsætərn/
Named after	Saturn
Adjectives	Saturnian, Cronian
Symbol
Orbital characteristics
Epoch J2000.0
Aphelion	10.086 AU (1.509 billion km)
Perihelion	9.024 AU (1.350 billion km)
Semi-major axis	9.5549 AU (1.429 billion km)
Eccentricity	0.05555
Orbital period (sidereal)	29.4571 yr 10,759.22 d 24,491.07 Saturnian solar days
Orbital period (synodic)	378.09 days
Average orbital speed	9.69 km/s (6.02 mi/s)
Mean anomaly	317.020°
Inclination	2.485240° to ecliptic 5.51° to Sun's equator 0.93° to invariable plane
Longitude of ascending node	113.665°
Argument of perihelion	339.392°
Known satellites	62 with formal designations; innumerable additional moonlets.
Physical characteristics
Mean radius	58,232 ± 6 km (36,184 ± 4 mi)
Equatorial radius	60,268 ± 4 km (37,449 ± 2 mi) 9.4492 Earths
Polar radius	54,364 ± 10 km (33,780 ± 6 mi) 8.5521 Earths
Flattening	0.09796±0.00018
Surface area	4.27×1010 km2 (1.65×1010 sq mi) 83.703 Earths
Volume	8.2713×1014 km3 (1.9844×1014 cu mi) 763.59 Earths
Mass	5.6836×1026 kg (1.2530×1027 lb) 95.159 Earths
Mean density	0.687 g/cm3 (0.0248 lb/cu in) (less than water)
Surface gravity	10.44 m/s2 (34.3 ft/s2) 1.065 g
Moment of inertia factor	0.210 (estimate)
Escape velocity	35.5 km/s (22.1 mi/s)
Sidereal rotation period	10.55 hours (10 hr 33 min)
Equatorial rotation velocity	9.87 km/s (6.13 mi/s; 35,500 km/h)
Axial tilt	26.73° (to orbit)
North pole right ascension	2h 42m 21s; 40.589°
North pole declination	83.537°
Albedo	0.342 (Bond) 0.499 (geometric)
Surface temp. min mean max 1 bar 134 K (−139 °C) 0.1 bar 84 K (−189 °C)
Apparent magnitude	+1.47 to −0.24
Angular diameter	14.5″ to 20.1″ (excludes rings)
Atmosphere
Scale height	59.5 km (37.0 mi)
Composition by volume	by volume: ≈ 96% hydrogen (H2) ≈ 3% helium (He) ≈ 0.4% methane (CH4) ≈ 0.01% ammonia (NH3) ≈ 0.01% hydrogen deuteride (HD) 0.0007% ethane (C2H6) Ices: ammonia (NH3) water (H2O) ammonium hydrosulfide (NH4SH)

Saturn is the sixth planet from the Sun and the second-largest in the Solar System, after Jupiter. It is a gas giant with an average radius about nine times that of Earth. Although it has only one-eighth the average density of Earth, with its larger volume Saturn is just over 95 times more massive. Saturn is named after the Roman god of agriculture; its astronomical symbol (♄) represents the god's sickle.

Saturn's interior is probably composed of a core of iron–nickel and rock (silicon and oxygen compounds). This core is surrounded by a deep layer of metallic hydrogen, an intermediate layer of liquid hydrogen and liquid helium, and finally outside the Frenkel line a gaseous outer layer. Saturn has a pale yellow hue due to ammonia crystals in its upper atmosphere. Electrical current within the metallic hydrogen layer is thought to give rise to Saturn's planetary magnetic field, which is weaker than Earth's, but has a magnetic moment 580 times that of Earth due to Saturn's larger size. Saturn's magnetic field strength is around one-twentieth of Jupiter's. The outer atmosphere is generally bland and lacking in contrast, although long-lived features can appear. Wind speeds on Saturn can reach 1,800 km/h (500 m/s), higher than on Jupiter, but not as high as those on Neptune.

Saturn has a prominent ring system that consists of nine continuous main rings and three discontinuous arcs and that is composed mostly of ice particles with a smaller amount of rocky debris and dust. Sixty-two moons are known to orbit Saturn, of which fifty-three are officially named. This does not include the hundreds of moonlets comprising the rings. Titan, Saturn's largest moon, and the second-largest in the Solar System, is larger than the planet Mercury, although less massive, and is the only moon in the Solar System to have a substantial atmosphere.

Physical characteristics

Composite image roughly comparing the sizes of Saturn and Earth

Saturn is a gas giant because it is predominantly composed of hydrogen and helium. It lacks a definite surface, though it may have a solid core. Saturn's rotation causes it to have the shape of an oblate spheroid; that is, it is flattened at the poles and bulges at its equator. Its equatorial and polar radii differ by almost 10%: 60,268 km versus 54,364 km, respectively. Jupiter, Uranus, and Neptune, the other giant planets in the Solar System, are also oblate but to a lesser extent. Saturn is the only planet of the Solar System that is less dense than water—about 30% less. Although Saturn's core is considerably denser than water, the average specific density of the planet is 0.69 g/cm³ due to the atmosphere. Jupiter has 318 times the Earth's mass, while Saturn is 95 times the mass of the Earth. Together, Jupiter and Saturn hold 92% of the total planetary mass in the Solar System.

On 8 January 2015, NASA reported determining the center of the planet Saturn and its family of moons to within 4 km (2.5 mi).

Internal structure

Diagram of Saturn, to scale

Despite consisting mostly of hydrogen and helium, most of Saturn's mass is not in the gas phase, because hydrogen becomes a non-ideal liquid when the density is above 0.01 g/cm³, which is reached at a radius containing 99.9% of Saturn's mass. The temperature, pressure, and density inside Saturn all rise steadily toward the core, which causes hydrogen to transition into a metal in the deeper layers.

Standard planetary models suggest that the interior of Saturn is similar to that of Jupiter, having a small rocky core surrounded by hydrogen and helium with trace amounts of various volatiles. This core is similar in composition to the Earth, but more dense. Examination of Saturn's gravitational moment, in combination with physical models of the interior, allowed French astronomers Didier Saumon and Tristan Guillot to place constraints on the mass of Saturn's core. In 2004, they estimated that the core must be 9–22 times the mass of the Earth, which corresponds to a diameter of about 25,000 km. This is surrounded by a thicker liquid metallic hydrogen layer, followed by a liquid layer of helium-saturated molecular hydrogen that gradually transitions to a gas with increasing altitude. The outermost layer spans 1,000 km and consists of gas.

Saturn has a hot interior, reaching 11,700 °C at its core, and it radiates 2.5 times more energy into space than it receives from the Sun. Jupiter's thermal energy is generated by the Kelvin–Helmholtz mechanism of slow gravitational compression, but this alone may not be sufficient to explain heat production for Saturn, because it is less massive. An alternative or additional mechanism may be generation of heat through the "raining out" of droplets of helium deep in Saturn's interior. As the droplets descend through the lower-density hydrogen, the process releases heat by friction and leaves Saturn's outer layers depleted of helium. These descending droplets may have accumulated into a helium shell surrounding the core.

Atmosphere

Methane bands circle Saturn (rel 1 February 2016)

The outer atmosphere of Saturn contains 96.3% molecular hydrogen and 3.25% helium by volume. The proportion of helium is significantly deficient compared to the abundance of this element in the Sun. The quantity of elements heavier than helium is not known precisely, but the proportions are assumed to match the primordial abundances from the formation of the Solar System. The total mass of these heavier elements is estimated to be 19–31 times the mass of the Earth, with a significant fraction located in Saturn's core region.

Trace amounts of ammonia, acetylene, ethane, propane, phosphine and methane have been detected in Saturn's atmosphere. The upper clouds are composed of ammonia crystals, while the lower level clouds appear to consist of either ammonium hydrosulfide (NH₄SH) or water. Ultraviolet radiation from the Sun causes methane photolysis in the upper atmosphere, leading to a series of hydrocarbon chemical reactions with the resulting products being carried downward by eddies and diffusion. This photochemical cycle is modulated by Saturn's annual seasonal cycle.

Cloud layers

A global storm girdles the planet in 2011. The head of the storm (bright area) passes the tail circling around the left limb.

Saturn's atmosphere exhibits a banded pattern similar to Jupiter's, but Saturn's bands are much fainter and are much wider near the equator. The nomenclature used to describe these bands is the same as on Jupiter. Saturn's finer cloud patterns were not observed until the flybys of the Voyager spacecraft during the 1980s. Since then, Earth-based telescopy has improved to the point where regular observations can be made.

The composition of the clouds varies with depth and increasing pressure. In the upper cloud layers, with the temperature in the range 100–160 K and pressures extending between 0.5–2 bar, the clouds consist of ammonia ice. Water ice clouds begin at a level where the pressure is about 2.5 bar and extend down to 9.5 bar, where temperatures range from 185–270 K. Intermixed in this layer is a band of ammonium hydrosulfide ice, lying in the pressure range 3–6 bar with temperatures of 290–235 K. Finally, the lower layers, where pressures are between 10–20 bar and temperatures are 270–330 K, contains a region of water droplets with ammonia in aqueous solution.

Saturn's usually bland atmosphere occasionally exhibits long-lived ovals and other features common on Jupiter. In 1990, the Hubble Space Telescope imaged an enormous white cloud near Saturn's equator that was not present during the Voyager encounters and in 1994, another, smaller storm was observed. The 1990 storm was an example of a Great White Spot, a unique but short-lived phenomenon that occurs once every Saturnian year, roughly every 30 Earth years, around the time of the northern hemisphere's summer solstice. Previous Great White Spots were observed in 1876, 1903, 1933 and 1960, with the 1933 storm being the most famous. If the periodicity is maintained, another storm will occur in about 2020.

The winds on Saturn are the second fastest among the Solar System's planets, after Neptune's. Voyager data indicate peak easterly winds of 500 m/s (1800 km/h). In images from the Cassini spacecraft during 2007, Saturn's northern hemisphere displayed a bright blue hue, similar to Uranus. The color was most likely caused by Rayleigh scattering. Thermography has shown that Saturn's south pole has a warm polar vortex, the only known example of such a phenomenon in the Solar System. Whereas temperatures on Saturn are normally −185 °C, temperatures on the vortex often reach as high as −122 °C, suspected to be the warmest spot on Saturn.

North pole hexagonal cloud pattern

Saturn – North polar hexagon and vortex as well as rings (2 April 2014)

Main article: Saturn's hexagon

A persisting hexagonal wave pattern around the north polar vortex in the atmosphere at about 78°N was first noted in the Voyager images. The sides of the hexagon are each about 13,800 km (8,600 mi) long, which is longer than the diameter of the Earth. The entire structure rotates with a period of 10h 39m 24s (the same period as that of the planet's radio emissions) which is assumed to be equal to the period of rotation of Saturn's interior. The hexagonal feature does not shift in longitude like the other clouds in the visible atmosphere. The pattern's origin is a matter of much speculation. Most scientists think it is a standing wave pattern in the atmosphere. Polygonal shapes have been replicated in the laboratory through differential rotation of fluids.

South pole vortex

A storm at Saturn's south pole

HST imaging of the south polar region indicates the presence of a jet stream, but no strong polar vortex nor any hexagonal standing wave. NASA reported in November 2006 that Cassini had observed a "hurricane-like" storm locked to the south pole that had a clearly defined eyewall. Eyewall clouds had not previously been seen on any planet other than Earth. For example, images from the Galileo spacecraft did not show an eyewall in the Great Red Spot of Jupiter.

The south pole storm may have been present for billions of years. This vortex is comparable to the size of Earth, and it has winds of 550 km/h.

Other features

Cassini has observed a series of cloud features nicknamed "String of Pearls" found in northern latitudes. These features are cloud clearings that reside in deeper cloud layers.

Magnetosphere

Main article: Magnetosphere of Saturn

Polar aurorae on Saturn

Auroral lights at Saturn’s north pole.

Saturn has an intrinsic magnetic field that has a simple, symmetric shape – a magnetic dipole. Its strength at the equator – 0.2 gauss (20 µT) – is approximately one twentieth of that of the field around Jupiter and slightly weaker than Earth's magnetic field. As a result, Saturn's magnetosphere is much smaller than Jupiter's. When Voyager 2 entered the magnetosphere, the solar wind pressure was high and the magnetosphere extended only 19 Saturn radii, or 1.1 million km (712,000 mi), although it enlarged within several hours, and remained so for about three days. Most probably, the magnetic field is generated similarly to that of Jupiter – by currents in the liquid metallic-hydrogen layer called a metallic-hydrogen dynamo. This magnetosphere is efficient at deflecting the solar wind particles from the Sun. The moon Titan orbits within the outer part of Saturn's magnetosphere and contributes plasma from the ionized particles in Titan's outer atmosphere. Saturn's magnetosphere, like Earth's, produces aurorae.

Orbit and rotation

Saturn and rings as viewed by the Cassini spacecraft (28 October 2016).

The average distance between Saturn and the Sun is over 1.4 billion kilometres (9 AU). With an average orbital speed of 9.69 km/s, it takes Saturn 10,759 Earth days (or about 29+1⁄2 years), to finish one revolution around the Sun. The elliptical orbit of Saturn is inclined 2.48° relative to the orbital plane of the Earth. The perihelion and aphelion distances are, respectively, 9.022 and 10.053 AU, on average. The visible features on Saturn rotate at different rates depending on latitude and multiple rotation periods have been assigned to various regions (as in Jupiter's case).

Astronomers use three different systems for specifying the rotation rate of Saturn. System I has a period of 10 hr 14 min 00 sec (844.3°/d) and encompasses the Equatorial Zone, the South Equatorial Belt and the North Equatorial Belt. The polar regions are considered to have rotation rates similar to System I. All other Saturnian latitudes, excluding the north and south polar regions, are indicated as System II and have been assigned a rotation period of 10 hr 38 min 25.4 sec (810.76°/d). System III refers to Saturn's internal rotation rate. Based on radio emissions from the planet in the period of the Voyager flybys, it has been assigned a rotation period of 10 hr 39 min 22.4 sec (810.8°/d). Because it is close to System II, it has largely superseded it.

A precise value for the rotation period of the interior remains elusive. While approaching Saturn in 2004, Cassini found that the radio rotation period of Saturn had increased appreciably, to approximately 10 hr 45 min 45 sec (± 36 sec). The latest estimate of Saturn's rotation (as an indicated rotation rate for Saturn as a whole) based on a compilation of various measurements from the Cassini, Voyager and Pioneer probes was reported in September 2007 is 10 hr 32 min 35 sec.

In March 2007, it was found that the variation of radio emissions from the planet did not match Saturn's rotation rate. This variance may be caused by geyser activity on Saturn's moon Enceladus. The water vapor emitted into Saturn's orbit by this activity becomes charged and creates a drag upon Saturn's magnetic field, slowing its rotation slightly relative to the rotation of the planet.

Natural satellites

Main article: Moons of Saturn

A montage of Saturn and its principal moons (Dione, Tethys, Mimas, Enceladus, Rhea and Titan; Iapetus not shown). This famous image was created from photographs taken in November 1980 by the Voyager 1 spacecraft.

Saturn has 62 known moons, 53 of which have formal names. In addition, there is evidence of dozens to hundreds of moonlets with diameters of 40–500 meters in Saturn's rings, which are not considered to be true moons. Titan, the largest moon, comprises more than 90% of the mass in orbit around Saturn, including the rings. Saturn's second-largest moon, Rhea, may have a tenuous ring system of its own, along with a tenuous atmosphere.

Possible beginning of a new moon (white dot) of Saturn (image taken by Cassini on 15 April 2013).

Many of the other moons are small: 34 are less than 10 km in diameter and another 14 between 10 and 50 km in diameter. Traditionally, most of Saturn's moons have been named after Titans of Greek mythology. Titan is the only satellite in the Solar System with a major atmosphere, in which a complex organic chemistry occurs. It is the only satellite with hydrocarbon lakes.

On 6 June 2013, scientists at the IAA-CSIC reported the detection of polycyclic aromatic hydrocarbons in the upper atmosphere of Titan, a possible precursor for life. On 23 June 2014, NASA claimed to have strong evidence that nitrogen in the atmosphere of Titan came from materials in the Oort cloud, associated with comets, and not from the materials that formed Saturn in earlier times.

Saturn's moon Enceladus, which seems similar in chemical makeup to comets, has often been regarded as a potential habitat for microbial life. Evidence of this possibility includes the satellite's salt-rich particles having an "ocean-like" composition that indicates most of Enceladus's expelled ice comes from the evaporation of liquid salt water.

In April 2014, NASA scientists reported the possible beginning of a new moon, within the A Ring, of the planet Saturn, which was imaged by Cassini on 15 April 2013.

Planetary rings

Main article: Rings of Saturn

The rings of Saturn (imaged here by Cassini in 2007) are the most massive and conspicuous in the Solar System.

False-color UV image of Saturn's outer B and A rings; dirtier ringlets in the Cassini Division and Encke Gap show up red.

Saturn is probably best known for the system of planetary rings that makes it visually unique. The rings extend from 6,630 km to 120,700 km outward from Saturn's equator, average approximately 20 meters in thickness and are composed of 93% water ice with traces of tholin impurities and 7% amorphous carbon. The particles that make up the rings range in size from specks of dust up to 10 m. While the other gas giants also have ring systems, Saturn's is the largest and most visible.

There are two main hypotheses regarding the origin of the rings. One hypothesis is that the rings are remnants of a destroyed moon of Saturn. The second hypothesis is that the rings are left over from the original nebular material from which Saturn formed. Some ice in the E ring comes from the moon Enceladus's geysers.

In the past, astronomers once thought the rings formed alongside the planet when it formed billions of years ago. Instead, the age of these planetary rings is probably some hundreds of millions of years.

Beyond the main rings at a distance of 12 million km from the planet is the sparse Phoebe ring, which is tilted at an angle of 27° to the other rings and, like Phoebe, orbits in retrograde fashion.

Some of the moons of Saturn, including Pandora and Prometheus, act as shepherd moons to confine the rings and prevent them from spreading out. Pan and Atlas cause weak, linear density waves in Saturn's rings that have yielded more reliable calculations of their masses.

History of observation and exploration

Main article: Exploration of Saturn

There have been three main phases in the observation and exploration of Saturn. The first era was ancient observations (such as with the naked eye), before the invention of the modern telescopes. Starting in the 17th century progressively more advanced telescopic observations from Earth have been made. The other type is visitation by spacecraft, either by orbiting or flyby. In the 21st century observations continue from the Earth (or Earth-orbiting observatories) and from the Cassini orbiter at Saturn.

Ancient observations

See also: Saturn (mythology)

Saturn has been known since prehistoric times. In ancient times, it was the most distant of the five known planets in the Solar System (excluding Earth) and thus a major character in various mythologies. Babylonian astronomers systematically observed and recorded the movements of Saturn. In ancient Roman mythology, the god Saturnus, from which the planet takes its name, was the god of agriculture. The Romans considered Saturnus the equivalent of the Greek god Cronus. The Greeks had made the outermost planet sacred to Cronus, and the Romans followed suit. (In modern Greek, the planet retains its ancient name Cronus—Κρόνος: Kronos.)

The Greek scientist Ptolemy based his calculations of Saturn's orbit on observations he made while it was in opposition. In Hindu astrology, there are nine astrological objects, known as Navagrahas. Saturn, one of them is known as "Shani" and judges everyone based on the good and bad deeds performed in life. Ancient Chinese and Japanese culture designated the planet Saturn as the "earth star" (土星). This was based on Five Elements which were traditionally used to classify natural elements.

In ancient Hebrew, Saturn is called 'Shabbathai'. Its angel is Cassiel. Its intelligence or beneficial spirit is Agiel (layga) and its spirit (darker aspect) is Zazel (lzaz). In Ottoman Turkish, Urdu and Malay, its name is 'Zuhal', derived from Arabic زحل.

European observations (17th–19th centuries)

Robert Hooke noted the shadows (a and b) cast by both the globe and the rings on each other in this drawing of Saturn in 1666.

Saturn's rings require at least a 15-mm-diameter telescope to resolve and thus were not known to exist until Galileo first saw them in 1610. He thought of them as two moons on Saturn's sides. It was not until Christiaan Huygens used greater telescopic magnification that this notion was refuted. Huygens discovered Saturn's moon Titan; Giovanni Domenico Cassini later discovered four other moons: Iapetus, Rhea, Tethys and Dione. In 1675, Cassini discovered the gap now known as the Cassini Division.

No further discoveries of significance were made until 1789 when William Herschel discovered two further moons, Mimas and Enceladus. The irregularly shaped satellite Hyperion, which has a resonance with Titan, was discovered in 1848 by a British team.

In 1899 William Henry Pickering discovered Phoebe, a highly irregular satellite that does not rotate synchronously with Saturn as the larger moons do. Phoebe was the first such satellite found and it takes more than a year to orbit Saturn in a retrograde orbit. During the early 20th century, research on Titan led to the confirmation in 1944 that it had a thick atmosphere – a feature unique among the Solar System's moons.

Modern NASA and ESA probes

Pioneer 11 flyby

Pioneer 11 image of Saturn

Pioneer 11 carried out the first flyby of Saturn in September 1979, when it passed within 20,000 km of the planet's cloud tops. Images were taken of the planet and a few of its moons, although their resolution was too low to discern surface detail. The spacecraft also studied Saturn's rings, revealing the thin F-ring and the fact that dark gaps in the rings are bright when viewed at high phase angle (towards the Sun), meaning that they contain fine light-scattering material. In addition, Pioneer 11 measured the temperature of Titan.

Voyager flybys

In November 1980, the Voyager 1 probe visited the Saturn system. It sent back the first high-resolution images of the planet, its rings and satellites. Surface features of various moons were seen for the first time. Voyager 1 performed a close flyby of Titan, increasing knowledge of the atmosphere of the moon. It proved that Titan's atmosphere is impenetrable in visible wavelengths, therefore no surface details were seen. The flyby changed the spacecraft's trajectory out from the plane of the Solar System.

Almost a year later, in August 1981, Voyager 2 continued the study of the Saturn system. More close-up images of Saturn's moons were acquired, as well as evidence of changes in the atmosphere and the rings. Unfortunately, during the flyby, the probe's turnable camera platform stuck for a couple of days and some planned imaging was lost. Saturn's gravity was used to direct the spacecraft's trajectory towards Uranus.

The probes discovered and confirmed several new satellites orbiting near or within the planet's rings, as well as the small Maxwell Gap (a gap within the C Ring) and Keeler gap (a 42 km wide gap in the A Ring).

Cassini–Huygens spacecraft

On 1 July 2004, the Cassini–Huygens space probe performed the SOI (Saturn Orbit Insertion) maneuver and entered orbit around Saturn. Before the SOI, Cassini had already studied the system extensively. In June 2004, it had conducted a close flyby of Phoebe, sending back high-resolution images and data.

Cassini's Titan flyby radio-signal studies (artist's concept)

Cassini's flyby of Saturn's largest moon, Titan, has captured radar images of large lakes and their coastlines with numerous islands and mountains. The orbiter completed two Titan flybys before releasing the Huygens probe on 25 December 2004. Huygens descended onto the surface of Titan on 14 January 2005, sending a flood of data during the atmospheric descent and after the landing. Cassini has since conducted multiple flybys of Titan and other icy satellites.

Photograph of Earth and the Moon by Cassini, visible in the bottom-right.

Animation of Saturn's north polar vortex seen in infrared light

Since early 2005, scientists have been tracking lightning on Saturn. The power of the lightning is approximately 1,000 times that of lightning on Earth.

In 2006, NASA reported that Cassini had found evidence of liquid water reservoirs that erupt in geysers on Saturn's moon Enceladus. Images had shown jets of icy particles being emitted into orbit around Saturn from vents in the moon's south polar region. According to Andrew Ingersoll, California Institute of Technology, "Other moons in the Solar System have liquid-water oceans covered by kilometers of icy crust. What's different here is that pockets of liquid water may be no more than tens of meters below the surface." Over 100 geysers have been identified on Enceladus. In May 2011, NASA scientists at an Enceladus Focus Group Conference reported that Enceladus "is emerging as the most habitable spot beyond Earth in the Solar System for life as we know it".

Cassini photographs have led to other significant discoveries. They have revealed a previously undiscovered planetary ring, outside the brighter main rings of Saturn and inside the G and E rings. The source of this ring is hypothesized to be the crashing of a meteoroid off Janus and Epimetheus. In July 2006, Cassini images provided evidence of hydrocarbon lakes near Titan's north pole, the presence of which were confirmed in January 2007. In March 2007, additional images near Titan's north pole revealed hydrocarbon seas, the largest of which is almost the size of the Caspian Sea. In October 2006, the probe detected an 8,000 km diameter cyclone-like storm with an eyewall at Saturn's south pole.

At Enceladus's south pole geysers spray water from many locations along the tiger stripes.

From 2004 to 2 November 2009, the probe discovered and confirmed eight new satellites. Its primary mission ended in 2008 when the spacecraft had completed 74 orbits around the planet. The probe's mission was extended to September 2010 and then extended again to 2017, to study a full period of Saturn's seasons.

In April 2013 Cassini sent back images of a hurricane at the planet's north pole 20 times larger than those found on Earth, with winds faster than 530 km/h.

On 19 July 2013, "The Day the Earth Smiled", Cassini was pointed towards Earth to capture an image of the Earth and the Moon (and, as well, Venus and Mars) as part of a natural light, multi-image portrait of the entire Saturn system. It was the first time NASA informed the people of Earth that a long-distance photo was being taken in advance.

Possible future missions

The continued exploration of Saturn is still considered to be a viable option for NASA as part of their ongoing New Frontiers program of missions. NASA previously requested for plans to be put forward for a mission to Saturn that included an atmospheric entry probe and possible investigations into the habitability and possible discovery of life on Saturn's moons Titan and Enceladus.

Observation

Amateur telescopic view of Saturn

Saturn is the most distant of the five planets easily visible to the naked eye from Earth, the other four being Mercury, Venus, Mars and Jupiter. (Uranus and occasionally 4 Vesta are visible to the naked eye in dark skies.) Saturn appears to the naked eye in the night sky as a bright, yellowish point of light with an apparent magnitude of usually between +1 and 0. It takes approximately 29.5 years for the planet to complete an entire circuit of the ecliptic against the background constellations of the zodiac. Most people will require an optical aid (very large binoculars or a small telescope) that magnifies at least 30 times to achieve an image of Saturn's rings, in which clear resolution is present. Twice every Saturnian year (roughly every 15 Earth years), the rings briefly disappear from view, due to the way in which they are angled and because they are so thin. Such a "disappearance" will next occur in 2025, but Saturn will be too close to the Sun for any ring-crossing observation to be possible.

Simulated appearance of Saturn as seen from Earth at opposition, 2001-2029

Saturn eclipses the Sun, as seen from Cassini. The rings are clearly visible, including the F Ring.

Saturn and its rings are best seen when the planet is at, or near, opposition, the configuration of a planet when it is at an elongation of 180°, and thus appears opposite the Sun in the sky. A Saturnian opposition occurs every year—approximately every 378 days—and results in the planet appearing at its brightest. However, both the Earth and Saturn orbit the Sun on eccentric orbits, which means their distances from the Sun vary over time, and therefore so do their distances from each other, hence varying the brightness of Saturn from one opposition to the other. Also, Saturn appears brighter when the rings are angled such that they are more visible. For example, during the opposition of 17 December 2002, Saturn appeared at its brightest due to a favorable orientation of its rings relative to the Earth, even though Saturn was closer to the Earth and Sun in late 2003.

Also, from time to time Saturn is occulted by the Moon (that is, the Moon covers up Saturn in the sky). As with all the planets in the Solar System, occultations of Saturn occur in “seasons”. Saturnian occultations will take place 12 or more times over a 12-month period, followed by about a five-year period in which no such activity is registered. Australian astronomy experts Hill and Horner explain the seasonal nature of Saturnian occultations:

This is the result of the fact that the moon’s orbit around the Earth is tilted to the orbit of the Earth around the Sun – and so most of the time, the moon will pass above or below Saturn in the sky, and no occultation will occur. It is only when Saturn lies near the point that the moon’s orbit crosses the “plane of the ecliptic” that occultations can happen – and then they occur every time the moon swings by, until Saturn moves away from the crossing point.

In culture

Saturn, from a 1550 edition of Guido Bonatti's Liber astronomiae

Further information: Saturn in fiction

• Saturn in astrology () is the ruling planet of Capricorn and, traditionally, Aquarius.
• Saturn, the Bringer of Old Age is a movement in Gustav Holst's The Planets.
• The Saturn family of rockets were developed by a team of mostly German rocket scientists led by Wernher von Braun to launch heavy payloads to Earth orbit and beyond. Originally proposed as a military satellite launcher, they were adopted as the launch vehicles for the Apollo program.
• The day Saturday is, like the planet Saturn, named after the Roman god of agriculture, Saturn (linked to the Greek god Cronus).

See also

• Outline of Saturn
• Dragon Storm (astronomy)
• Sixth planet (disambiguation)
• Space exploration
• Timeline of the far future

Further reading

• Alexander, Arthur Francis O'Donel (1962). The Planet Saturn - A History of Observation, Theory and Discovery. {{cite book}}: Invalid |display-authors=1 (help)
• Gore, Rick (July 1981). "Voyager 1 at Saturn: Riddles of the Rings". National Geographic. Vol. 160, no. 1. pp. 3–31. ISSN 0027-9358. OCLC 643483454.
• Lovett, L.; et al. (2006). Saturn: A New View. New York: Harry N. Abrams, Inc. ISBN 978-0-8109-3090-2.
• Karttunen, H.; et al. (2007). Fundamental Astronomy (5th ed.). New York: Springer. ISBN 978-3-540-34143-7.

External links

{{Spoken Wikipedia|Saturn.ogg|date=2013-08-18}}

• Saturn profile at NASA's Solar System Exploration site
• Saturn Fact Sheet, by NASA
• Gazetteer of Planetary Nomenclature – Saturn (USGS)
• Cassini–Huygens mission to Saturn, by NASA
• Research News about Saturn
• General information about Saturn
• Studies on the Rings of Saturn
• Astronomy Cast: Saturn
• Saturn in Daytime (12 inch telescope)
• Saturn 'Rev 175' Raw Preview
• Haese, Paul. "Capturing Saturn". Sixty Symbols. Brady Haran for the University of Nottingham.
• BBC In Our Time radio program

* Category:Gas giants Category:Astronomical objects known since antiquity