Saturn: Difference between revisions
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| pronounced = {{IPAc-en|audio=en-us-Saturn.ogg|ˈ|s|æ|t|ər|n}}<ref name="walter2003"/> | | pronounced = {{IPAc-en|audio=en-us-Saturn.ogg|ˈ|s|æ|t|ər|n}}<ref name="walter2003"/> | ||
| named_after = [[Saturn (mythology)|Saturn]] | | named_after = [[Saturn (mythology)|Saturn]] | ||
| adjectives = Saturnian {{IPAc-en|s|ə|ˈ|t|ɜr|n|i|ə|n}},<ref>{{OED|Saturnian}}</ref> Cronian<ref>{{Cite web |url=http://solarsystem.nasa.gov/multimedia/downloads/Small_RPS_Report.pdf |title=Enabling Exploration with Small Radioisotope Power Systems |date=September 2004 |access-date=26 January 2016 |publisher=NASA |archive-url=https://web.archive.org/web/20161222125722/http://solarsystem.nasa.gov/multimedia/downloads/Small_RPS_Report.pdf |archive-date=22 December 2016 | | adjectives = Saturnian {{IPAc-en|s|ə|ˈ|t|ɜr|n|i|ə|n}},<ref>{{OED|Saturnian}}</ref> Cronian<ref>{{Cite web |url=http://solarsystem.nasa.gov/multimedia/downloads/Small_RPS_Report.pdf |title=Enabling Exploration with Small Radioisotope Power Systems |date=September 2004 |access-date=26 January 2016 |publisher=NASA |archive-url=https://web.archive.org/web/20161222125722/http://solarsystem.nasa.gov/multimedia/downloads/Small_RPS_Report.pdf |archive-date=22 December 2016 }}</ref> / Kronian<ref>{{cite journal |last1=Müller |display-authors=etal |year=2010 |title=Azimuthal plasma flow in the Kronian magnetosphere |doi=10.1029/2009ja015122 |journal=Journal of Geophysical Research |volume=115 |issue=A8 |page=A08203 |article-number=2009JA015122 |bibcode=2010JGRA..115.8203M |doi-access=free |issn=0148-0227 }}</ref> {{IPAc-en|'|k|r|ou|n|i|@|n}}<ref>{{OED|Cronian}}</ref> | ||
| orbit_ref = <ref name="fact" /> | | orbit_ref = <ref name="fact" /> | ||
| epoch = [[J2000.0]] | | epoch = [[J2000.0]] | ||
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| escape_velocity = {{val|35.5|u=km/s}}<ref group=lower-alpha name=1bar /> | | escape_velocity = {{val|35.5|u=km/s}}<ref group=lower-alpha name=1bar /> | ||
| rotation = 10 h 32 m 36 s; <br/>10.5433 hours,<ref name="CSeligman"/> 10 h 39 m; <br/>10.7 hours<ref name=JPL/> | | rotation = 10 h 32 m 36 s; <br/>10.5433 hours,<ref name="CSeligman"/> 10 h 39 m; <br/>10.7 hours<ref name=JPL/> | ||
| sidereal_day = <span class="nowrap">{{RA|10|33|38}} {{+-|{{RA||1|52}}|{{RA||1|19}}}} </span><ref name="NASA-20190118">{{cite news |last1=McCartney |first1=Gretchen |last2=Wendel |first2=JoAnna |title=Scientists Finally Know What Time It Is on Saturn |url=https://www.jpl.nasa.gov/news/scientists-finally-know-what-time-it-is-on-saturn/ |date=18 January 2019 |work=[[NASA]] |access-date=3 January 2025 }}</ref><ref name="APJ-20190117">{{cite journal |author=Mankovich, Christopher |display-authors=etal |title=Cassini Ring Seismology as a Probe of Saturn's Interior. I. Rigid Rotation |date=17 January 2019 |journal=[[The Astrophysical Journal]] |volume=871 | | | sidereal_day = <span class="nowrap">{{RA|10|33|38}} {{+-|{{RA||1|52}}|{{RA||1|19}}}} </span><ref name="NASA-20190118">{{cite news |last1=McCartney |first1=Gretchen |last2=Wendel |first2=JoAnna |title=Scientists Finally Know What Time It Is on Saturn |url=https://www.jpl.nasa.gov/news/scientists-finally-know-what-time-it-is-on-saturn/ |date=18 January 2019 |work=[[NASA]] |access-date=3 January 2025 }}</ref><ref name="APJ-20190117">{{cite journal |author=Mankovich, Christopher |display-authors=etal |title=Cassini Ring Seismology as a Probe of Saturn's Interior. I. Rigid Rotation |date=17 January 2019 |journal=[[The Astrophysical Journal]] |volume=871 |page=1 |number=1 |doi=10.3847/1538-4357/aaf798 |arxiv=1805.10286 |bibcode=2019ApJ...871....1M |s2cid=67840660 |doi-access=free }}</ref> | ||
| rot_velocity = {{val|9.87|u=km/s}}<ref group=lower-alpha name=1bar /> | | rot_velocity = {{val|9.87|u=km/s}}<ref group=lower-alpha name=1bar /> | ||
| axial_tilt = 26.73° {{small|(to orbit)}} | | axial_tilt = 26.73° {{small|(to orbit)}} | ||
| Line 89: | Line 89: | ||
| angular_size = 14.5″ to 20.1″ (excludes rings) | | angular_size = 14.5″ to 20.1″ (excludes rings) | ||
| atmosphere_ref = <ref name="fact" /> | | atmosphere_ref = <ref name="fact" /> | ||
| surface_pressure = >>1000 bars<ref>{{cite web |title=On The Atmospheres Of Different Planets |first=Robin |last=Knecht |date=24 October 2005 |url=http://www.tp.umu.se/space/Proj_05/Robin.K.pdf |access-date=14 October 2017 |archive-url=https://web.archive.org/web/20171014234631/http://www.tp.umu.se/space/Proj_05/Robin.K.pdf |archive-date=14 October 2017 | | surface_pressure = >>1000 bars<ref>{{cite web |title=On The Atmospheres Of Different Planets |first=Robin |last=Knecht |date=24 October 2005 |url=http://www.tp.umu.se/space/Proj_05/Robin.K.pdf |access-date=14 October 2017 |archive-url=https://web.archive.org/web/20171014234631/http://www.tp.umu.se/space/Proj_05/Robin.K.pdf |archive-date=14 October 2017 }}</ref> | ||
| scale_height = {{val|59.5|u=km}} | | scale_height = {{val|59.5|u=km}} | ||
| atmosphere_composition = {{plainlist| | | atmosphere_composition = {{plainlist| | ||
| Line 100: | Line 100: | ||
* Icy [[Volatile (astrogeology)|volatiles]]: {{cslist|[[ammonia]]|[[ice|water ice]]|[[ammonium hydrosulfide]]}}}} | * Icy [[Volatile (astrogeology)|volatiles]]: {{cslist|[[ammonia]]|[[ice|water ice]]|[[ammonium hydrosulfide]]}}}} | ||
}} | }} | ||
'''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 of about 9 times that of [[Earth]]. It has an eighth the average density of Earth, but is over 95 times more massive. Even though Saturn is almost as big as Jupiter, Saturn has less than a third its mass. Saturn orbits the Sun at a distance of {{convert|1434|e6km|AU|2|abbr=unit|order=flip|lk=on}}, with an [[orbital period]] of 29.45 years. | '''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 of about 9 times that of [[Earth]]. It has an eighth of the average density of Earth, but is over 95 times more massive. Even though Saturn is almost as big as Jupiter, Saturn has less than a third of its mass. Saturn orbits the Sun at a distance of {{convert|1434|e6km|AU|2|abbr=unit|order=flip|lk=on}}, with an [[orbital period]] of 29.45 years. | ||
Saturn's interior is thought to be composed of a rocky core, surrounded by a deep layer of [[metallic hydrogen]], an intermediate layer of [[liquid hydrogen]] and [[liquid helium]], and an outer layer of gas. Saturn has a pale yellow hue, due to [[ammonia]] crystals in its upper atmosphere. An [[electrical current]] in 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 because of Saturn's greater size. Saturn's magnetic field strength is about a twentieth that of Jupiter.<ref name="mag" /> The outer [[atmosphere]] is generally bland and lacking in contrast, although long-lived features can appear. [[Wind speed]]s on Saturn can reach {{convert|1800|km/h|abbr=off}}. | Saturn's interior is thought to be composed of a rocky core, surrounded by a deep layer of [[metallic hydrogen]], an intermediate layer of [[liquid hydrogen]] and [[liquid helium]], and an outer layer of gas. Saturn has a pale yellow hue, due to [[ammonia]] crystals in its upper atmosphere. An [[electrical current]] in 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 because of Saturn's greater size. Saturn's magnetic field strength is about a twentieth that of Jupiter.<ref name="mag" /> The outer [[atmosphere]] is generally bland and lacking in contrast, although long-lived features can appear. [[Wind speed]]s on Saturn can reach {{convert|1800|km/h|abbr=off}}. | ||
The planet has a bright and extensive [[Rings of Saturn|system of rings]], composed mainly of ice particles, with a smaller amount of rocky debris and [[cosmic dust|dust]]. At least [[Moons of Saturn|274 moons]] orbit the planet, of which 63 are officially named; these do not include the hundreds of [[moonlet]]s in the rings. [[Titan (moon)|Titan]], Saturn's largest moon and the second largest in the Solar System, is larger (but less massive) than the planet [[Mercury (planet)|Mercury]] and is the only moon in the Solar System that has a substantial atmosphere.<ref name="Titan ref">{{cite web |url=http://saturn.jpl.nasa.gov/news/features/saturn-story/moons.cfm |title=The Story of Saturn |access-date=7 July 2007 |last=Munsell |first=Kirk |date=6 April 2005 |publisher=NASA Jet Propulsion Laboratory; California Institute of Technology |archive-url=https://web.archive.org/web/20080816074342/http://saturn.jpl.nasa.gov/news/features/saturn-story/moons.cfm |archive-date=16 August 2008 | The planet has a bright and extensive [[Rings of Saturn|system of rings]], composed mainly of ice particles, with a smaller amount of rocky debris and [[cosmic dust|dust]]. At least [[Moons of Saturn|274 moons]] orbit the planet, of which 63 are officially named; these do not include the hundreds of [[moonlet]]s in the rings. [[Titan (moon)|Titan]], Saturn's largest moon and the second largest in the Solar System, is larger (but less massive) than the planet [[Mercury (planet)|Mercury]] and is the only moon in the Solar System that has a substantial atmosphere.<ref name="Titan ref">{{cite web |url=http://saturn.jpl.nasa.gov/news/features/saturn-story/moons.cfm |title=The Story of Saturn |access-date=7 July 2007 |last=Munsell |first=Kirk |date=6 April 2005 |publisher=NASA Jet Propulsion Laboratory; California Institute of Technology |archive-url=https://web.archive.org/web/20080816074342/http://saturn.jpl.nasa.gov/news/features/saturn-story/moons.cfm |archive-date=16 August 2008 }}</ref> | ||
==Name and symbol== | ==Name and symbol== | ||
Saturn is named after the Roman [[Saturn (mythology)|god of wealth and agriculture]], who was the father of the god Jupiter. Its [[astronomical symbol]] {{nowrap|([[file:Saturn symbol (fixed width).svg|16px|♄]])}} has been traced back to the Greek [[Oxyrhynchus Papyri]], where it can be seen to be a Greek [[kappa]]-[[rho]] ligature with a [[Scribal abbreviation#Forms|horizontal stroke]], as an abbreviation for ''Κρονος'' ([[Cronus]]), the Greek name for the planet ([[File:Saturn symbol (late classical and medieval mss).png|41px]]).<ref name="jones-1999">{{cite book | Saturn is named after the Roman [[Saturn (mythology)|god of wealth and agriculture]], who was the father of the god [[Jupiter_(mythology)|Jupiter]]. Its [[astronomical symbol]] {{nowrap|([[file:Saturn symbol (fixed width).svg|16px|♄|class=skin-invert]])}} has been traced back to the Greek [[Oxyrhynchus Papyri]], where it can be seen to be a Greek [[kappa]]-[[rho]] ligature with a [[Scribal abbreviation#Forms|horizontal stroke]], as an abbreviation for ''Κρονος'' ([[Cronus]]), the Greek name for the planet ([[File:Saturn symbol (late classical and medieval mss).png|41px|class=skin-invert]]).<ref name="jones-1999">{{cite book | ||
| title=Astronomical papyri from Oxyrhynchus | | title=Astronomical papyri from Oxyrhynchus | ||
| last=Jones | | last=Jones | ||
| Line 114: | Line 114: | ||
| pages=62–63 | | pages=62–63 | ||
| publisher=American Philosophical Society | | publisher=American Philosophical Society | ||
| isbn= | | isbn=978-0-87169-233-7 | ||
| url=https://books.google.com/books?id=8MokzymQ43IC | | url=https://books.google.com/books?id=8MokzymQ43IC | ||
| quote= | | quote= | ||
| Line 126: | Line 126: | ||
== Physical characteristics == | == Physical characteristics == | ||
[[File:Saturn compared to Earth and the Moon.png|alt=Refer to caption|left|thumb| | [[File:Saturn compared to Earth and the Moon.png|alt=Refer to caption|left|thumb|The size of Saturn compared to Earth and Earth's Moon]] | ||
Saturn is the only planet of the Solar System that is less dense than water—about 30% less.<ref name=preserve/> Although Saturn's [[planetary core|core]] is considerably denser than water, the average [[relative density|specific density]] of the planet is {{val|0.69|u=g/cm3}}, because of the atmosphere. Jupiter has 318 times [[Earth mass|Earth's mass]],<ref name="Jupiter fact"/> and Saturn is 95 times Earth's mass.<ref name="fact"/><ref name="Mass ref">{{cite web |last=Brainerd |first=Jerome James |date=6 October 2004 |title=Solar System Planets Compared to Earth |url=http://www.astrophysicsspectator.com/tables/PlanetComparativeData.html | Saturn is a [[gas giant]], composed predominantly of hydrogen and helium. It lacks a definite surface, though it is likely to have a solid core.<ref name=melosh2011/> The planet's rotation makes it an [[oblate spheroid]]—a ball [[flattening|flattened]] at the [[geographical pole|poles]] and [[equatorial bulge|bulging]] at the [[equator]]. Its equatorial radius is more than 10% larger than the polar radius: 60,268 km versus 54,364 km (37,449 mi versus 33,780 mi).<ref name="fact" /> | ||
Jupiter, [[Uranus]], and [[Neptune]], the other giant planets in the Solar System, are less oblate. The combination of the bulge and the rotation rate means that the effective surface gravity along the equator, {{Val|8.96|u=m/s2}}, is 74% of what it is at the poles and is lower than the surface gravity of Earth. However, the equatorial [[escape velocity]], nearly {{Val|36|u=km/s}}, is much higher than that of Earth.<ref name=Gregersen2010>{{cite book |url=https://books.google.com/books?id=ptLFDN0z8gQC&pg=PA119 |title=Outer Solar System: Jupiter, Saturn, Uranus, Neptune, and the Dwarf Planets |publisher=The Rosen Publishing Group |editor1-first=Erik |editor1-last=Gregersen |page=119 |year=2010 |isbn=978-1-61530-014-3 |access-date=17 February 2018 |archive-date=10 June 2020 |archive-url=https://web.archive.org/web/20200610170554/https://books.google.com/books?id=ptLFDN0z8gQC&pg=PA119 |url-status=live }}</ref> | |||
Saturn is the only planet of the Solar System that is less dense than water—about 30% less.<ref name=preserve/> Although Saturn's [[planetary core|core]] is considerably denser than water, the average [[relative density|specific density]] of the planet is {{val|0.69|u=g/cm3}}, because of the atmosphere. Jupiter has 318 times [[Earth mass|Earth's mass]],<ref name="Jupiter fact"/> and Saturn is 95 times Earth's mass.<ref name="fact"/><ref name="Mass ref">{{cite web |last=Brainerd |first=Jerome James |date=6 October 2004 |title=Solar System Planets Compared to Earth |url=http://www.astrophysicsspectator.com/tables/PlanetComparativeData.html |archive-url=https://web.archive.org/web/20111001102843/http://www.astrophysicsspectator.com/tables/PlanetComparativeData.html |archive-date=1 October 2011 |access-date=5 July 2010 |publisher=The Astrophysics Spectator}}</ref><ref name="Mass ref 2">{{cite web |last=Dunbar |first=Brian |date=29 November 2007 |title=NASA – Saturn |url=http://mynasa.nasa.gov/worldbook/saturn_worldbook.html |archive-url=https://web.archive.org/web/20110929073208/http://mynasa.nasa.gov/worldbook/saturn_worldbook.html |archive-date=29 September 2011 |access-date=21 July 2011 |publisher=NASA}}</ref><ref name="Mass ref 3" /><ref name="Radius ref">{{cite web |last=Brainerd |first=Jerome James |date=24 November 2004 |title=Characteristics of Saturn |url=http://www.astrophysicsspectator.com/tables/Saturn.html |archive-url=https://web.archive.org/web/20111001102834/http://www.astrophysicsspectator.com/tables/Saturn.html |archive-date=1 October 2011 |access-date=5 July 2010 |publisher=The Astrophysics Spectator}}</ref><ref name="Radius ref 2">{{cite web |date=28 July 2011 |title=General Information about Saturn |url=http://scienceray.com/astronomy/general-information-about-saturn-2/1/ |archive-url=https://web.archive.org/web/20111007220627/http://scienceray.com/astronomy/general-information-about-saturn-2/1/ |archive-date=7 October 2011 |access-date=17 August 2011 |work=Scienceray}}</ref> Together, Jupiter and Saturn hold 92% of the total planetary mass in the Solar System.<ref name=ssr152_1_423/> | |||
=== Internal structure === | === Internal structure === | ||
[[File:Saturn diagram.svg|thumb|upright=1.5| | [[File:Saturn diagram.svg|thumb|upright=1.5|A diagram of Saturn, to scale|left]] | ||
Despite consisting mostly of hydrogen and helium, most of Saturn's mass is not in the [[gas]] [[phase (matter)|phase]], because hydrogen becomes a [[ideal solution|non-ideal liquid]] when the density is above {{val|0.01|u=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 be a metal in the deeper layers.<ref name=ssr152_1_423/> | |||
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 [[Volatile (astrogeology)|volatiles]].<ref name=guillot_et_al2009/> Analysis of the distortion shows that Saturn is substantially more centrally condensed than [[Jupiter]] and therefore contains much more material denser than [[hydrogen]] near its center. Saturn's central regions are about 50% hydrogen by mass, and Jupiter's are about 67% hydrogen.<ref>{{Cite web |title=Saturn - The interior {{!}} Britannica |url=https://www.britannica.com/place/Saturn-planet/The-interior |access-date=14 April 2022 |website=www.britannica.com |language=en}}</ref> | 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 [[Volatile (astrogeology)|volatiles]].<ref name=guillot_et_al2009/> Analysis of the distortion shows that Saturn is substantially more centrally condensed than [[Jupiter]] and therefore contains much more material denser than [[hydrogen]] near its center. Saturn's central regions are about 50% hydrogen by mass, and Jupiter's are about 67% hydrogen.<ref>{{Cite web |title=Saturn - The interior {{!}} Britannica |url=https://www.britannica.com/place/Saturn-planet/The-interior |access-date=14 April 2022 |website=www.britannica.com |language=en}}</ref> | ||
This core is similar in composition to Earth, but is more dense. The examination of Saturn's [[gravitational moment]], in combination with physical models of the interior, has allowed constraints to be placed on the mass of Saturn's core. In 2004, scientists estimated that the core must be 9–22 times the mass of Earth,<ref name="science305_5689_1414" /><ref name="apj609_2_1170" /> which corresponds to a diameter of about {{Convert|25000|km|abbr=on}}.<ref>{{cite web |url=https:// | This core is similar in composition to Earth, but is more dense. The examination of Saturn's [[gravitational moment]], in combination with physical models of the interior, has allowed constraints to be placed on the mass of Saturn's core. In 2004, scientists estimated that the core must be 9–22 times the mass of Earth,<ref name="science305_5689_1414" /><ref name="apj609_2_1170" /> which corresponds to a diameter of about {{Convert|25000|km|abbr=on}}.<ref>{{cite web |url=https://h2g2.com/edited_entry/A383960 |title=Saturn |publisher=BBC |access-date=19 July 2011 |date=2000 |archive-url=https://web.archive.org/web/20110101024556/http://www.bbc.co.uk/dna/h2g2/A383960 |archive-date=1 January 2011 |url-status=live }}</ref> Measurements of Saturn's rings suggest a much more diffuse core, with a mass equal to about 17 Earths and a radius equal to about 60% of Saturn's entire radius.<ref>{{cite journal |last1=Mankovich |first1=Christopher R. |last2=Fuller |first2=Jim |title=A diffuse core in Saturn revealed by ring seismology |url=https://www.nature.com/articles/s41550-021-01448-3 |journal=Nature Astronomy |year=2021 |volume=5 |issue=11 |pages=1103–1109 |doi=10.1038/s41550-021-01448-3 |arxiv=2104.13385 |bibcode=2021NatAs...5.1103M |s2cid=233423431 |access-date=22 August 2021 |archive-date=20 August 2021 |archive-url=https://web.archive.org/web/20210820195416/https://www.nature.com/articles/s41550-021-01448-3 |url-status=live }}</ref> This is surrounded by a thicker, liquid [[metallic hydrogen]] layer, followed by a liquid layer of helium-saturated [[molecular hydrogen]], which gradually transitions to a gas as altitude increases. The outermost layer spans about {{Convert|1000|km|abbr=on}} and consists of gas.<ref name="faure_mensing2007" /><ref name="NMM Saturn" /><ref>{{cite web |url=http://www.windows2universe.org/saturn/interior/S_int_structure_overview.html |title=Structure of Saturn's Interior |publisher=Windows to the Universe |access-date=19 July 2011 |archive-url=https://web.archive.org/web/20110917140427/http://www.windows2universe.org/saturn/interior/S_int_structure_overview.html |archive-date=17 September 2011 }}</ref> | ||
Saturn has a hot interior, reaching {{Convert|11700|C}} at its core, and 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 such a process alone may not be sufficient to explain heat production for Saturn, because it is less massive. An alternative or additional mechanism may be the 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.<ref name=de_pater_lissauer2010/><ref name=nasa_saturn/> These descending droplets may have accumulated into a helium shell surrounding the core.<ref name=guillot_et_al2009/> Rainfalls of [[diamond]]s have been suggested to occur within Saturn, as well as in Jupiter<ref name="SC-20131009">{{cite news |last=Kramer |first=Miriam |title=Diamond Rain May Fill Skies of Jupiter and Saturn |url=https://www.space.com/23135-diamond-rain-jupiter-saturn.html |date=9 October 2013 |work=[[Space.com]] |access-date=27 August 2017 |archive-date=27 August 2017 |archive-url=https://web.archive.org/web/20170827171415/https://www.space.com/23135-diamond-rain-jupiter-saturn.html |url-status=live }}</ref> and [[ice giant]]s Uranus and Neptune.<ref name="WP-20170825">{{cite news |last=Kaplan |first=Sarah |title=It rains solid diamonds on Uranus and Neptune |url=https://www.washingtonpost.com/news/speaking-of-science/wp/2017/08/25/it-rains-solid-diamonds-on-uranus-and-neptune/ |date=25 August 2017 |newspaper=[[The Washington Post]] |access-date=27 August 2017 |archive-date=27 August 2017 |archive-url=https://web.archive.org/web/20170827011901/https://www.washingtonpost.com/news/speaking-of-science/wp/2017/08/25/it-rains-solid-diamonds-on-uranus-and-neptune/ |url-status=live }}</ref> | Saturn has a hot interior, reaching {{Convert|11700|C}} at its core, and 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 such a process alone may not be sufficient to explain heat production for Saturn, because it is less massive. An alternative or additional mechanism may be the 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.<ref name=de_pater_lissauer2010/><ref name=nasa_saturn/> These descending droplets may have accumulated into a helium shell surrounding the core.<ref name=guillot_et_al2009/> Rainfalls of [[diamond]]s have been suggested to occur within Saturn, as well as in Jupiter<ref name="SC-20131009">{{cite news |last=Kramer |first=Miriam |title=Diamond Rain May Fill Skies of Jupiter and Saturn |url=https://www.space.com/23135-diamond-rain-jupiter-saturn.html |date=9 October 2013 |work=[[Space.com]] |access-date=27 August 2017 |archive-date=27 August 2017 |archive-url=https://web.archive.org/web/20170827171415/https://www.space.com/23135-diamond-rain-jupiter-saturn.html |url-status=live }}</ref> and [[ice giant]]s Uranus and Neptune.<ref name="WP-20170825">{{cite news |last=Kaplan |first=Sarah |title=It rains solid diamonds on Uranus and Neptune |url=https://www.washingtonpost.com/news/speaking-of-science/wp/2017/08/25/it-rains-solid-diamonds-on-uranus-and-neptune/ |date=25 August 2017 |newspaper=[[The Washington Post]] |access-date=27 August 2017 |archive-date=27 August 2017 |archive-url=https://web.archive.org/web/20170827011901/https://www.washingtonpost.com/news/speaking-of-science/wp/2017/08/25/it-rains-solid-diamonds-on-uranus-and-neptune/ |url-status=live }}</ref> | ||
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==== Cloud layers ==== | ==== Cloud layers ==== | ||
[[File:Saturn Storm.jpg|thumb|A global storm girdles the planet in 2011. The storm passes around the planet, such that the storm's head (bright area) passes its tail. | [[File:Saturn Storm.jpg|thumb|A global storm girdles the planet in 2011. The storm passes around the planet, such that the storm's head (bright area) passes its tail.]] | ||
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 Space Probe|Voyager]]'' spacecraft during the 1980s. Since then, Earth-based [[telescope|telescopy]] has improved to the point where regular observations can be made.<ref name=emp105_2_143/> | 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 Space Probe|Voyager]]'' spacecraft during the 1980s. Since then, Earth-based [[telescope|telescopy]] has improved to the point where regular observations can be made.<ref name=emp105_2_143/> | ||
The composition of the clouds varies with depth and increasing pressure. In the upper cloud layers, with temperatures in the range of 100–160 K and pressures extending between 0.5–2 [[Bar (unit)|bar]], the clouds consist of ammonia ice. Water [[ice cloud]]s begin at a level where the pressure is about 2.5 bar and extend down to 9.5 bar, where temperatures range from 185 to 270 K. Intermixed in this layer is a band of ammonium hydrosulfide ice, lying in the pressure range 3–6 bar with temperatures of 190–235 K. | The composition of the clouds varies with depth and increasing pressure. In the upper cloud layers, with temperatures in the range of 100–160 K and pressures extending between 0.5–2 [[Bar (unit)|bar]], the clouds consist of ammonia ice. Water [[ice cloud]]s begin at a level where the pressure is about 2.5 bar and extend down to 9.5 bar, where temperatures range from 185 to 270 K. Intermixed in this layer is a band of ammonium hydrosulfide ice, lying in the pressure range 3–6 bar with temperatures of 190–235 K. The lower layers, where pressures are between 10 and 20 bar and temperatures are 270–330 K, contains a region of water droplets with ammonia in aqueous solution.<ref name=dougherty_esposito2009/> | ||
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 short-lived phenomenon that occurs once every Saturnian year, roughly every 30 Earth years, around the time of the northern hemisphere's [[summer solstice]].<ref name=icarus176_1_155/> | |||
Previous Great White Spots were observed in 1876, 1903, 1933, and 1960, with the 1933 storm being the best observed.<ref>{{cite book |editor1-link=Patrick Moore |editor1-last=Moore |editor1-first=Patrick |title=1993 Yearbook of Astronomy |location=London |publisher=W.W. Norton & Company |date=1992 |first1=Mark |last1=Kidger |chapter=The 1990 Great White Spot of Saturn |pages=176–215|bibcode=1992ybas.conf.....M }}</ref> The latest giant storm was observed in 2010. In 2015, researchers used [[Very Large Array]] telescope to study Saturnian atmosphere, and reported that they found "long-lasting signatures of all mid-latitude giant storms, a mixture of equatorial storms up to hundreds of years old, and potentially an unreported older storm at 70°N".<ref>{{cite journal |last1=Li |first1=Cheng |last2=de Pater |first2=Imke |last3=Moeckel |first3=Chris |last4=Sault |first4=R. J. |last5=Butler |first5=Bryan |last6=deBoer |first6=David |last7=Zhang |first7=Zhimeng |title=Long-lasting, deep effect of Saturn's giant storms |journal=Science Advances |date=11 August 2023 |volume=9 |issue=32 |article-number=eadg9419 |doi=10.1126/sciadv.adg9419 |pmid=37566653 |pmc=10421028 |bibcode=2023SciA....9G9419L }}</ref> | |||
The winds on Saturn are the second fastest among the Solar System's planets, after Neptune's. ''Voyager'' data indicate peak easterly winds of {{convert|500|m/s|km/h|abbr=on}}.<ref name="Voyager Summary 1">{{cite web |title=Voyager Saturn Science Summary |url=http://www.solarviews.com/eng/vgrsat.htm |first=Calvin J. |last=Hamilton |access-date=5 July 2007 |date=1997 |publisher=Solarviews |archive-url=https://web.archive.org/web/20110926211656/http://www.solarviews.com/eng/vgrsat.htm |archive-date=26 September 2011 | The winds on Saturn are the second fastest among the Solar System's planets, after Neptune's. ''Voyager'' data indicate peak easterly winds of {{convert|500|m/s|km/h|abbr=on}}.<ref name="Voyager Summary 1">{{cite web |title=Voyager Saturn Science Summary |url=http://www.solarviews.com/eng/vgrsat.htm |first=Calvin J. |last=Hamilton |access-date=5 July 2007 |date=1997 |publisher=Solarviews |archive-url=https://web.archive.org/web/20110926211656/http://www.solarviews.com/eng/vgrsat.htm |archive-date=26 September 2011 }}</ref> In images from the ''[[Cassini–Huygens|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]].<ref>{{cite web |url=http://www.nasa.gov/mission_pages/cassini/multimedia/pia09188.html |title=Saturn's Strange Hexagon |access-date=6 July 2007 |date=27 March 2007 |last=Watanabe |first=Susan |publisher=NASA |archive-url=https://web.archive.org/web/20100116155833/http://www.nasa.gov/mission_pages/cassini/multimedia/pia09188.html |archive-date=16 January 2010 |url-status=live }}</ref> [[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.<ref name=MCP>{{cite web |url=http://www.mcpstars.org/node/353 |title=Warm Polar Vortex on Saturn |date=2007 |publisher=Merrillville Community Planetarium |access-date=25 July 2007 |archive-url=https://web.archive.org/web/20110921212018/http://www.mcpstars.org/node/353 |archive-date=21 September 2011 }}</ref> 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.<ref name=MCP/> | ||
==== Hexagonal cloud patterns ==== | ==== Hexagonal cloud patterns ==== | ||
{{main|Saturn's hexagon}} | {{main|Saturn's hexagon}} | ||
{{multiple image | {{multiple image | ||
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{{Anchor|North pole hexagonal cloud pattern|South pole vortex}}A persisting [[hexagon]]al wave pattern around the north polar vortex in the atmosphere at about 78°N was first noted in the ''Voyager'' images.<ref>{{cite journal |bibcode=1988Icar...76..335G |doi=10.1016/0019-1035(88)90075-9 |title=A hexagonal feature around Saturn's North Pole |date=1988 |page=335 |author=Godfrey, D. A. |volume=76 |journal=Icarus |issue=2}}</ref><ref>{{cite journal |title=Ground-based observations of Saturn's north polar SPOT and hexagon |first4=P. |last4=Laques |first3=F. |last3=Colas |first2=J. |last2=Lecacheux |journal=Science |display-authors=1 |first1=A. |last1=Sanchez-Lavega |volume=260 |issue=5106 |date=1993 |pmid=17838249 |doi=10.1126/science.260.5106.329 |bibcode=1993Sci...260..329S |pages=329–32|s2cid=45574015 }}</ref><ref name="NYT-20140806">{{cite news |last=Overbye |first=Dennis |author-link=Dennis Overbye |title=Storm Chasing on Saturn |url=https://www.nytimes.com/2014/08/06/science/space/storm-chasing-on-saturn.html |date=6 August 2014 |work=[[New York Times]] |access-date=6 August 2014 |archive-date=12 July 2018 |archive-url=https://web.archive.org/web/20180712004804/https://www.nytimes.com/2014/08/06/science/space/storm-chasing-on-saturn.html |url-status=live }}</ref> The sides of the hexagon are each about {{Convert|14500|km|mi|-2|abbr=on}} long, which is longer than the diameter of the Earth.<ref name="Hexagon ref">{{cite news |url=https://www.nbcnews.com/id/wbna34352533 |title=New images show Saturn's weird hexagon cloud |publisher=NBC News |date=12 December 2009 |access-date=29 September 2011 |archive-date=21 October 2020 |archive-url=https://web.archive.org/web/20201021075355/http://www.nbcnews.com/id/34352533 |url-status=live }}</ref> The entire structure rotates with a period of {{RA|10|39|24}} (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.<ref name=science247_4947_1206/> The hexagonal feature does not shift in longitude like the other clouds in the visible atmosphere.<ref name=pss57_14_1671/> 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.<ref>{{cite journal |doi=10.1038/news060515-17 |last1=Ball |first1=Philip |title=Geometric whirlpools revealed |journal=[[Nature (journal)|Nature]] |date=19 May 2006|s2cid=129016856 |doi-access=free }} Bizarre geometric shapes that appear at the center of swirling vortices in planetary atmospheres might be explained by a simple experiment with a bucket of water but correlating this to Saturn's pattern is by no means certain.</ref><ref name=labmodel>{{cite journal |doi=10.1016/j.icarus.2009.10.022 |display-authors=1 |last1=Aguiar |first1=Ana C. Barbosa |last2=Read |first2=Peter L. |last3=Wordsworth |first3=Robin D |title=A laboratory model of Saturn's North Polar Hexagon |volume=206 |issue=2 |date=April 2010 |pages=755–763 |last4=Salter |first4=Tara |last5=Hiro Yamazaki |first5=Y. |journal=Icarus |bibcode=2010Icar..206..755B}} Laboratory experiment of spinning disks in a liquid solution forms vortices around a stable hexagonal pattern similar to that of Saturn's.</ref> | {{Anchor|North pole hexagonal cloud pattern|South pole vortex}}A persisting [[hexagon]]al wave pattern around the north polar vortex in the atmosphere at about 78°N was first noted in the ''Voyager'' images.<ref>{{cite journal |bibcode=1988Icar...76..335G |doi=10.1016/0019-1035(88)90075-9 |title=A hexagonal feature around Saturn's North Pole |date=1988 |page=335 |author=Godfrey, D. A. |volume=76 |journal=Icarus |issue=2}}</ref><ref>{{cite journal |title=Ground-based observations of Saturn's north polar SPOT and hexagon |first4=P. |last4=Laques |first3=F. |last3=Colas |first2=J. |last2=Lecacheux |journal=Science |display-authors=1 |first1=A. |last1=Sanchez-Lavega |volume=260 |issue=5106 |date=1993 |pmid=17838249 |doi=10.1126/science.260.5106.329 |bibcode=1993Sci...260..329S |pages=329–32|s2cid=45574015 }}</ref><ref name="NYT-20140806">{{cite news |last=Overbye |first=Dennis |author-link=Dennis Overbye |title=Storm Chasing on Saturn |url=https://www.nytimes.com/2014/08/06/science/space/storm-chasing-on-saturn.html |date=6 August 2014 |work=[[New York Times]] |access-date=6 August 2014 |archive-date=12 July 2018 |archive-url=https://web.archive.org/web/20180712004804/https://www.nytimes.com/2014/08/06/science/space/storm-chasing-on-saturn.html |url-status=live }}</ref> The sides of the hexagon are each about {{Convert|14500|km|mi|-2|abbr=on}} long, which is longer than the diameter of the Earth.<ref name="Hexagon ref">{{cite news |url=https://www.nbcnews.com/id/wbna34352533 |title=New images show Saturn's weird hexagon cloud |publisher=NBC News |date=12 December 2009 |access-date=29 September 2011 |archive-date=21 October 2020 |archive-url=https://web.archive.org/web/20201021075355/http://www.nbcnews.com/id/34352533 |url-status=live }}</ref> The entire structure rotates with a period of {{RA|10|39|24}} (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.<ref name=science247_4947_1206/> The hexagonal feature does not shift in longitude like the other clouds in the visible atmosphere.<ref name=pss57_14_1671/> 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.<ref>{{cite journal |doi=10.1038/news060515-17 |last1=Ball |first1=Philip |title=Geometric whirlpools revealed |journal=[[Nature (journal)|Nature]] |date=19 May 2006|s2cid=129016856 |doi-access=free }} Bizarre geometric shapes that appear at the center of swirling vortices in planetary atmospheres might be explained by a simple experiment with a bucket of water but correlating this to Saturn's pattern is by no means certain.</ref><ref name=labmodel>{{cite journal |doi=10.1016/j.icarus.2009.10.022 |display-authors=1 |last1=Aguiar |first1=Ana C. Barbosa |last2=Read |first2=Peter L. |last3=Wordsworth |first3=Robin D |title=A laboratory model of Saturn's North Polar Hexagon |volume=206 |issue=2 |date=April 2010 |pages=755–763 |last4=Salter |first4=Tara |last5=Hiro Yamazaki |first5=Y. |journal=Icarus |bibcode=2010Icar..206..755B}} Laboratory experiment of spinning disks in a liquid solution forms vortices around a stable hexagonal pattern similar to that of Saturn's.</ref> | ||
[[Hubble Space Telescope|HST]] imaging of the south polar region indicates the presence of a [[jet stream]], but no strong polar vortex nor any hexagonal standing wave.<ref>{{Cite journal |display-authors=1 |author=Sánchez-Lavega, A. |author2=Pérez-Hoyos, S. |author3=French, R. G. |url=http://aas.org/archives/BAAS/v34n3/dps2002/10.htm |title=Hubble Space Telescope Observations of the Atmospheric Dynamics in Saturn's South Pole from 1997 to 2002 |journal=Bulletin of the American Astronomical Society |volume=34 |page=857 |access-date=6 July 2007 |date=8 October 2002 |bibcode=2002DPS....34.1307S |archive-date=30 June 2010 |archive-url=https://web.archive.org/web/20100630162647/http://aas.org/archives/BAAS/v34n3/dps2002/10.htm |url-status=live }}</ref> [[NASA]] reported in November 2006 that ''Cassini'' had observed a "[[hurricane]]-like" storm locked to the south pole that had a clearly defined [[eyewall]].<ref>{{cite web |url=http://photojournal.jpl.nasa.gov/catalog/PIA09187 |title=NASA catalog page for image PIA09187 |access-date=23 May 2007 |publisher=NASA Planetary Photojournal |archive-url=https://web.archive.org/web/20111109044235/http://photojournal.jpl.nasa.gov/catalog/PIA09187 |archive-date=9 November 2011 |url-status=live }}</ref><ref>{{cite news |url= | [[Hubble Space Telescope|HST]] imaging of the south polar region indicates the presence of a [[jet stream]], but no strong polar vortex nor any hexagonal standing wave.<ref>{{Cite journal |display-authors=1 |author=Sánchez-Lavega, A. |author2=Pérez-Hoyos, S. |author3=French, R. G. |url=http://aas.org/archives/BAAS/v34n3/dps2002/10.htm |title=Hubble Space Telescope Observations of the Atmospheric Dynamics in Saturn's South Pole from 1997 to 2002 |journal=Bulletin of the American Astronomical Society |volume=34 |page=857 |access-date=6 July 2007 |date=8 October 2002 |bibcode=2002DPS....34.1307S |archive-date=30 June 2010 |archive-url=https://web.archive.org/web/20100630162647/http://aas.org/archives/BAAS/v34n3/dps2002/10.htm |url-status=live }}</ref> [[NASA]] reported in November 2006 that ''Cassini'' had observed a "[[hurricane]]-like" storm locked to the south pole that had a clearly defined [[eyewall]].<ref>{{cite web |url=http://photojournal.jpl.nasa.gov/catalog/PIA09187 |title=NASA catalog page for image PIA09187 |access-date=23 May 2007 |publisher=NASA Planetary Photojournal |archive-url=https://web.archive.org/web/20111109044235/http://photojournal.jpl.nasa.gov/catalog/PIA09187 |archive-date=9 November 2011 |url-status=live }}</ref><ref>{{cite news |url=https://news.bbc.co.uk/2/hi/6135450.stm?lsm |title=Huge 'hurricane' rages on Saturn |work=BBC News |date=10 November 2006 |access-date=29 September 2011 |archive-url=https://web.archive.org/web/20120803115422/http://news.bbc.co.uk/2/hi/6135450.stm?lsm |archive-date=3 August 2012 |url-status=live }}</ref> Eyewall clouds had not previously been seen on any planet other than Earth. For example, images from the ''[[Galileo (spacecraft)|Galileo]]'' spacecraft did not show an eyewall in the [[Great Red Spot]] of Jupiter.<ref>{{cite web |url=http://saturn.jpl.nasa.gov/news/press-release-details.cfm?newsID=703 |title=NASA Sees into the Eye of a Monster Storm on Saturn |publisher=NASA |date=9 November 2006 |access-date=20 November 2006 |archive-url=https://web.archive.org/web/20080507154317/http://saturn.jpl.nasa.gov/news/press-release-details.cfm?newsID=703 |archive-date=7 May 2008 }}</ref> | ||
The south pole storm may have been present for billions of years.<ref name="spole"/> This vortex is comparable to the size of Earth, and it has winds of 550 km/h.<ref name="spole">{{Cite APOD | title=A Hurricane Over the South Pole of Saturn | date=13 November 2006 | access-date=1 May 2013}}</ref> | The south pole storm may have been present for billions of years.<ref name="spole"/> This vortex is comparable to the size of Earth, and it has winds of 550 km/h.<ref name="spole">{{Cite APOD | title=A Hurricane Over the South Pole of Saturn | date=13 November 2006 | access-date=1 May 2013}}</ref> | ||
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=== Magnetosphere === | === Magnetosphere === | ||
{{Main|Magnetosphere of Saturn}} | {{Main|Magnetosphere of Saturn}} | ||
[[File:Hubble sees a flickering light display on Saturn.jpg | [[File:Hubble sees a flickering light display on Saturn.jpg|thumb|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 (unit)|gauss]] (20 [[microtesla|μT]])—is approximately one twentieth of that of the field around Jupiter and slightly weaker than Earth's magnetic field.<ref name="mag" /> As a result, Saturn's [[magnetosphere]] is much smaller than Jupiter's.<ref name="mag 2">{{cite web |url=http://library.thinkquest.org/C005921/Saturn/satuAtmo.htm |title=Saturn: Atmosphere and Magnetosphere |publisher=Thinkquest Internet Challenge |access-date=15 July 2007 |last=McDermott |first=Matthew |date=2000 |archive-url=https://web.archive.org/web/20111020053039/http://library.thinkquest.org/C005921/Saturn/satuAtmo.htm |archive-date=20 October 2011 |url-status=live }}</ref> | Saturn has an intrinsic [[magnetic field]] that has a simple, symmetric shape—a magnetic [[dipole]]. Its strength at the equator—0.2 [[Gauss (unit)|gauss]] (20 [[microtesla|μT]])—is approximately one twentieth of that of the field around Jupiter and slightly weaker than Earth's magnetic field.<ref name="mag" /> As a result, Saturn's [[magnetosphere]] is much smaller than Jupiter's.<ref name="mag 2">{{cite web |url=http://library.thinkquest.org/C005921/Saturn/satuAtmo.htm |title=Saturn: Atmosphere and Magnetosphere |publisher=Thinkquest Internet Challenge |access-date=15 July 2007 |last=McDermott |first=Matthew |date=2000 |archive-url=https://web.archive.org/web/20111020053039/http://library.thinkquest.org/C005921/Saturn/satuAtmo.htm |archive-date=20 October 2011 |url-status=live }}</ref> | ||
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 (684,000 mi),<ref>{{cite web |url=http://voyager.jpl.nasa.gov/science/saturn_magnetosphere.html |title=Voyager – Saturn's Magnetosphere |publisher=NASA Jet Propulsion Laboratory |date=18 October 2010 |access-date=19 July 2011 |archive-url=https://web.archive.org/web/20120319151942/http://voyager.jpl.nasa.gov/science/saturn_magnetosphere.html |archive-date=19 March 2012 | 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 (684,000 mi),<ref>{{cite web |url=http://voyager.jpl.nasa.gov/science/saturn_magnetosphere.html |title=Voyager – Saturn's Magnetosphere |publisher=NASA Jet Propulsion Laboratory |date=18 October 2010 |access-date=19 July 2011 |archive-url=https://web.archive.org/web/20120319151942/http://voyager.jpl.nasa.gov/science/saturn_magnetosphere.html |archive-date=19 March 2012 }}</ref> although it enlarged within several hours, and remained so for about three days.<ref name="atkinson2010" /> 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.<ref name="mag 2" /> 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 [[ion]]ized particles in Titan's outer atmosphere.<ref name="mag">{{cite journal |display-authors=1 |author=Russell, C. T. |author2=Luhmann, J. G. |date=1997 |url=http://www-ssc.igpp.ucla.edu/personnel/russell/papers/sat_mag.html |title=Saturn: Magnetic Field and Magnetosphere |journal=Science |volume=207 |issue=4429 |pages=407–10 |access-date=29 April 2007 |archive-url=https://web.archive.org/web/20110927165242/http://www-ssc.igpp.ucla.edu/personnel/russell/papers/sat_mag.html |archive-date=27 September 2011 |url-status=live |bibcode=1980Sci...207..407S |doi=10.1126/science.207.4429.407 |pmid=17833549 |s2cid=41621423 |url-access=subscription }}</ref> Saturn's magnetosphere, like [[Earth's magnetic field|Earth's]], produces [[aurora]]e.<ref>{{cite web |url=http://www.windows2universe.org/saturn/upper_atmosphere.html |title=Saturn Magnetosphere Overview |author=Russell, Randy |publisher=Windows to the Universe |date=3 June 2003 |access-date=19 July 2011 |archive-url=https://web.archive.org/web/20110906031014/http://www.windows2universe.org/saturn/upper_atmosphere.html |archive-date=6 September 2011 }}</ref> | ||
== Orbit and rotation == | == Orbit and rotation == | ||
[[File:Solar system orrery outer planets.gif|thumb| | [[File:Solar system orrery outer planets.gif|thumb|An animation of Saturn and the Solar System's [[outer planet]]s orbiting the Sun]] | ||
[[File:Saturnoppositions-animated.gif|thumb| | [[File:Saturnoppositions-animated.gif|thumb|A simulated appearance of Saturn as seen from Earth (at [[Opposition (astronomy)|opposition]]) during an orbit of Saturn, 2001–2029]] | ||
The average distance between Saturn and the Sun is over 1.4 billion kilometers (9 [[astronomical unit|AU]]). With an average orbital speed of 9.68 km/s,<ref name="fact" /> it takes Saturn 10,759 Earth days (or about {{frac|29|1|2}} years)<ref name="cain2009" /> to finish one revolution around the Sun.<ref name="fact" /> As a consequence, it forms a near 5:2 [[mean-motion resonance]] with Jupiter.<ref>{{cite journal |title=Modeling the 5 : 2 Mean-Motion Resonance in the Jupiter-Saturn Planetary System |last1=Michtchenko |first1=T. A. |last2=Ferraz-Mello |first2=S. |journal=Icarus |volume=149 |issue=2 |pages=357–374 |date=February 2001 |doi=10.1006/icar.2000.6539 |bibcode=2001Icar..149..357M}}</ref> The elliptical orbit of Saturn is inclined 2.48° relative to the [[orbital plane]] of the Earth.<ref name="fact" /> The [[apsis|perihelion and aphelion]] distances are, respectively, 9.195 and 9.957 AU, on average.<ref name="fact" /><ref>Jean Meeus, ''Astronomical Algorithms'' (Richmond, VA: Willmann-Bell, 1998). Average of the nine extremes on p 273. All are within 0.02 AU of the averages.</ref> 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). | The average distance between Saturn and the Sun is over 1.4 billion kilometers (9 [[astronomical unit|AU]]). With an average orbital speed of 9.68 km/s,<ref name="fact" /> it takes Saturn 10,759 Earth days (or about {{frac|29|1|2}} years)<ref name="cain2009" /> to finish one revolution around the Sun.<ref name="fact" /> As a consequence, it forms a near 5:2 [[mean-motion resonance]] with Jupiter.<ref>{{cite journal |title=Modeling the 5: 2 Mean-Motion Resonance in the Jupiter-Saturn Planetary System |last1=Michtchenko |first1=T. A. |last2=Ferraz-Mello |first2=S. |journal=Icarus |volume=149 |issue=2 |pages=357–374 |date=February 2001 |doi=10.1006/icar.2000.6539 |bibcode=2001Icar..149..357M}}</ref> The elliptical orbit of Saturn is inclined 2.48° relative to the [[orbital plane]] of the Earth.<ref name="fact" /> The [[apsis|perihelion and aphelion]] distances are, respectively, 9.195 and 9.957 AU, on average.<ref name="fact" /><ref>Jean Meeus, ''Astronomical Algorithms'' (Richmond, VA: Willmann-Bell, 1998). Average of the nine extremes on p 273. All are within 0.02 AU of the averages.</ref> 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 {{RA|10|14|00}} (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 {{RA|10|38|25.4}} (810.76°/d). ''System III'' refers to Saturn's internal rotation rate. Based on [[radio astronomy|radio emissions]] from the planet detected by ''[[Voyager 1]]'' and ''Voyager 2'',<ref>{{cite journal|doi=10.1126/science.209.4462.1238|pmid=17811197|bibcode=1980Sci...209.1238K|title=Voyager Detection of Nonthermal Radio Emission from Saturn|journal=Science|volume=209|issue=4462|pages=1238–40|last1=Kaiser|first1=M. L.|last2=Desch|first2=M. D.|last3=Warwick|first3=J. W.|last4=Pearce|first4=J. B.|year=1980|hdl=2060/19800013712|s2cid=44313317|hdl-access=free}}</ref> System III has a rotation period of {{RA|10|39|22.4}} (810.8°/d). System III has largely superseded System II.<ref name=benton2006/> | Astronomers use three different systems for specifying the rotation rate of Saturn. ''System I'' has a period of {{RA|10|14|00}} (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 {{RA|10|38|25.4}} (810.76°/d). ''System III'' refers to Saturn's internal rotation rate. Based on [[radio astronomy|radio emissions]] from the planet detected by ''[[Voyager 1]]'' and ''Voyager 2'',<ref>{{cite journal|doi=10.1126/science.209.4462.1238|pmid=17811197|bibcode=1980Sci...209.1238K|title=Voyager Detection of Nonthermal Radio Emission from Saturn|journal=Science|volume=209|issue=4462|pages=1238–40|last1=Kaiser|first1=M. L.|last2=Desch|first2=M. D.|last3=Warwick|first3=J. W.|last4=Pearce|first4=J. B.|year=1980|hdl=2060/19800013712|s2cid=44313317|hdl-access=free}}</ref> System III has a rotation period of {{RA|10|39|22.4}} (810.8°/d). System III has largely superseded System II.<ref name=benton2006/> | ||
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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 {{RA|10|45|45}} {{+-|{{RA|||36}}}}.<ref>{{cite web |url=http://www.nasa.gov/mission_pages/cassini/media/cassini-062804.html |title=Scientists Find That Saturn's Rotation Period is a Puzzle |date=28 June 2004 |publisher=NASA |access-date=22 March 2007 |archive-url=https://web.archive.org/web/20110729155336/http://www.nasa.gov/mission_pages/cassini/media/cassini-062804.html |archive-date=29 July 2011 |url-status=live }}</ref><ref name=cain2008_15298/> An 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 is {{RA|10|32|35}}.<ref name=Anderson2007/> Studies of the planet's [[Rings of Saturn#C Ring|C Ring]] yield a rotation period of <span class="nowrap">{{RA|10|33|38}} {{+-|{{RA||1|52}}|{{RA||1|19}}}} </span>.<ref name="NASA-20190118" /><ref name="APJ-20190117" /> | 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 {{RA|10|45|45}} {{+-|{{RA|||36}}}}.<ref>{{cite web |url=http://www.nasa.gov/mission_pages/cassini/media/cassini-062804.html |title=Scientists Find That Saturn's Rotation Period is a Puzzle |date=28 June 2004 |publisher=NASA |access-date=22 March 2007 |archive-url=https://web.archive.org/web/20110729155336/http://www.nasa.gov/mission_pages/cassini/media/cassini-062804.html |archive-date=29 July 2011 |url-status=live }}</ref><ref name=cain2008_15298/> An 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 is {{RA|10|32|35}}.<ref name=Anderson2007/> Studies of the planet's [[Rings of Saturn#C Ring|C Ring]] yield a rotation period of <span class="nowrap">{{RA|10|33|38}} {{+-|{{RA||1|52}}|{{RA||1|19}}}} </span>.<ref name="NASA-20190118" /><ref name="APJ-20190117" /> | ||
In March 2007, it was found that the variation in 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.<ref>{{cite press release |url=http://www.nasa.gov/mission_pages/cassini/media/cassini-20070322.html |title=Enceladus Geysers Mask the Length of Saturn's Day |date=22 March 2007 |publisher=NASA Jet Propulsion Laboratory |access-date=22 March 2007 | In March 2007, it was found that the variation in 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.<ref>{{cite press release |url=http://www.nasa.gov/mission_pages/cassini/media/cassini-20070322.html |title=Enceladus Geysers Mask the Length of Saturn's Day |date=22 March 2007 |publisher=NASA Jet Propulsion Laboratory |access-date=22 March 2007 |archive-url=https://web.archive.org/web/20081207134416/http://saturn.jpl.nasa.gov/news/press-release-details.cfm?newsID=733 |archive-date=7 December 2008 }}</ref><ref name=science316_5823_442/><ref name=science316_5823_380/> | ||
Saturn only has one known [[trojan asteroid]], designated {{mpl|2019 UO|14}}, whose trojan configuration was announced in September 2024, orbiting the Sun at the stable [[Lagrange_point#L4_and_L5|L<sub>4</sub>]] [[Lagrange point]] 60° ahead of the planet along its orbit.<ref name="Hui2024">{{cite arXiv |last1=Hui |first1=Man-To |last2=Wiegert |first2=Paul A. |display-authors=etal |date=September 2024 |title=2019 UO14: A Transient Trojan of Saturn |eprint=2409.19725 |class=astro-ph.EP}}</ref> This discovery leaves only Mercury without any known trojans at all. [[Orbital resonance]] mechanisms, including [[secular resonance]], are believed to be the cause of the low number of known Saturnian trojans.<ref>{{cite journal |title=Saturn Trojans: a dynamical point of view |journal=Monthly Notices of the Royal Astronomical Society |display-authors=1 |last1=Hou |first1=X. Y. |last2=Scheeres |first2=D. J. |last3=Liu |first3=L. |volume=437 |issue=2 |pages=1420–1433 |date=January 2014 |doi=10.1093/mnras/stt1974 |bibcode=2014MNRAS.437.1420H|doi-access=free }}</ref> | |||
== Natural satellites == | == Natural satellites == | ||
{{Main|Moons of Saturn}} | {{Main|Moons of Saturn}} | ||
[[File:Saturn's Rings PIA03550.jpg|thumb|400x400px| | [[File:Saturn's Rings PIA03550.jpg|thumb|400x400px|An artist conception of Saturn, its rings and major icy moons—from Mimas to Rhea]] | ||
Saturn has 274 known [[natural satellite|moons]],<ref name="NYT 2025-03-13">{{cite news |author=Jonathan O'Callaghan |date=March 11, 2025 |title=Saturn Gains 128 New Moons, Bringing Its Total to 274 |url=https://www.nytimes.com/2025/03/11/science/saturn-new-moons.html |access-date=March 13, 2025 |newspaper=The New York Times | Saturn has 274 known [[natural satellite|moons]],<ref name="NYT 2025-03-13">{{cite news |author=Jonathan O'Callaghan |date=March 11, 2025 |title=Saturn Gains 128 New Moons, Bringing Its Total to 274 |url=https://www.nytimes.com/2025/03/11/science/saturn-new-moons.html |access-date=March 13, 2025 |newspaper=The New York Times}}</ref><ref>{{cite web |title=Mpec 2025-E153: Sixty-One New Saturnian Satellites |url=https://www.minorplanetcenter.net/mpec/K25/K25EF3.html}}</ref><ref>{{cite web |title=Mpec 2025-E154: Thirty-Four New Saturnian Satellites |url=https://www.minorplanetcenter.net/mpec/K25/K25EF4.html}}</ref><ref>{{cite web |title=Mpec 2025-E155: Thirty-Three New Saturnian Satellites |url=https://www.minorplanetcenter.net/mpec/K25/K25EF5.html}}</ref> 63 of which have formal names.<ref name="UBC-20230511">{{cite news|title=Saturn now leads moon race with 62 newly discovered moons|url=https://science.ubc.ca/news/saturn-now-leads-moon-race-62-newly-discovered-satellites|work=UBC Science|publisher=University of British Columbia|date=11 May 2023|access-date=11 May 2023}}</ref><ref name="JPLmoons">{{cite web |title=Solar System Dynamics – Planetary Satellite Discovery Circumstances |url=https://ssd.jpl.nasa.gov/sats/discovery.html |publisher=NASA |access-date=4 June 2022 |date=15 November 2021}}</ref> There is evidence of dozens to hundreds of [[moonlet]]s with diameters of 40–500 meters in Saturn's rings,<ref>{{cite journal |arxiv=0710.4547 |last=Tiscareno |first=Matthew |title=The population of propellers in Saturn's A Ring |date=17 July 2013 |doi=10.1088/0004-6256/135/3/1083 |volume=135 |issue=3 |journal=The Astronomical Journal |pages=1083–1091 |bibcode=2008AJ....135.1083T|s2cid=28620198 }}</ref> which are not considered to be true moons. [[Titan (moon)|Titan]], the largest moon, comprises more than 90% of the mass in orbit around Saturn, including the rings.<ref name="brunier2005" /> Saturn's second-largest moon, [[Rhea (moon)|Rhea]], may have a tenuous [[Rings of Rhea|ring system of its own]],<ref name="Jones2008" /> along with a tenuous [[atmosphere]].<ref name=atkinson20101126/><ref>{{cite web |url=http://www.sciencedaily.com/releases/2010/11/101128222041.htm |title=Thin air: Oxygen atmosphere found on Saturn's moon Rhea |website=ScienceDaily |author=NASA |date=30 November 2010 |access-date=23 July 2011 |archive-url=https://web.archive.org/web/20111108215855/http://www.sciencedaily.com/releases/2010/11/101128222041.htm |archive-date=8 November 2011 |url-status=live }}</ref><ref name=ryan20101126/> | ||
Many of the other moons are small: 131 are less than 50 km in diameter.<ref name="Saturn moons">{{cite web |url=http://www.dtm.ciw.edu/users/sheppard/satellites/satsatdata.html |title=Saturn's Known Satellites |publisher=Department of Terrestrial Magnetism |access-date=22 June 2010 |archive-url=https://web.archive.org/web/20110926210000/http://www.dtm.ciw.edu/users/sheppard/satellites/satsatdata.html |archive-date=26 September 2011 | Many of the other moons are small: 131 are less than 50 km in diameter.<ref name="Saturn moons">{{cite web |url=http://www.dtm.ciw.edu/users/sheppard/satellites/satsatdata.html |title=Saturn's Known Satellites |publisher=Department of Terrestrial Magnetism |access-date=22 June 2010 |archive-url=https://web.archive.org/web/20110926210000/http://www.dtm.ciw.edu/users/sheppard/satellites/satsatdata.html |archive-date=26 September 2011 }}</ref> 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 of Titan|atmosphere]],<ref>{{cite web |url=http://www.sciencedaily.com/releases/2009/01/090129182514.htm |title=Cassini Finds Hydrocarbon Rains May Fill Titan Lakes |website=ScienceDaily |date=30 January 2009 |access-date=19 July 2011 |archive-url=https://web.archive.org/web/20111109045639/http://www.sciencedaily.com/releases/2009/01/090129182514.htm |archive-date=9 November 2011 |url-status=live }}</ref><ref>{{cite web |url=http://voyager.jpl.nasa.gov/science/saturn_titan.html |title=Voyager – Titan |publisher=NASA Jet Propulsion Laboratory |date=18 October 2010 |access-date=19 July 2011 |archive-url=https://web.archive.org/web/20111026090736/http://voyager.jpl.nasa.gov/science/saturn_titan.html |archive-date=26 October 2011 }}</ref> in which a complex [[organic chemistry]] occurs. It is the only satellite with [[Lakes of Titan|hydrocarbon lakes]].<ref>{{cite news |url=https://www.nbcnews.com/id/wbna14029488 |title=Evidence of hydrocarbon lakes on Titan |publisher=NBC News |agency=Associated Press |date=25 July 2006 |access-date=19 July 2011 |archive-date=24 August 2014 |archive-url=https://web.archive.org/web/20140824105749/http://www.nbcnews.com/id/14029488/ |url-status=live }}</ref><ref>{{cite news |url=http://www.cosmosmagazine.com/news/2109/ethane-lake-finally-confirmed-titan |title=Hydrocarbon lake finally confirmed on Titan |work=[[Cosmos (magazine)|Cosmos Magazine]] |date=31 July 2008 |access-date=19 July 2011 |archive-url=https://web.archive.org/web/20111101134216/http://www.cosmosmagazine.com/news/2109/ethane-lake-finally-confirmed-titan |archive-date=1 November 2011 }}</ref> | ||
On 6 June 2013, scientists at the [[Instituto de Astrofísica de Andalucía|IAA-CSIC]] reported the detection of [[polycyclic aromatic hydrocarbon]]s in the [[upper atmosphere]] of Titan, a [[PAH world hypothesis|possible precursor for life]].<ref name="IAA-20130606">{{cite news |last=López-Puertas |first=Manuel |url=http://www.iaa.es/content/pahs-titans-upper-atmosphere |title=PAH's in Titan's Upper Atmosphere |date=6 June 2013 |work=[[Spanish National Research Council|CSIC]] |access-date=6 June 2013 |archive-date=22 August 2016 |archive-url=https://web.archive.org/web/20160822010505/http://www.iaa.es/content/pahs-titans-upper-atmosphere |url-status=live }}</ref> 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 [[comet]]s, and not from the materials that formed Saturn in earlier times.<ref name="NASA-201450623">{{cite web |display-authors=1 |last1=Dyches |first1=Preston |last2=Clavin |first2=Clavin |title=Titan's Building Blocks Might Pre-date Saturn |url=http://www.jpl.nasa.gov/news/news.php?release=2014-200 |date=23 June 2014 |work=NASA |access-date=24 June 2014 |archive-date=9 September 2018 |archive-url=https://web.archive.org/web/20180909162240/https://www.jpl.nasa.gov/news/news.php?release=2014-200 |url-status=live }}</ref> | On 6 June 2013, scientists at the [[Instituto de Astrofísica de Andalucía|IAA-CSIC]] reported the detection of [[polycyclic aromatic hydrocarbon]]s in the [[upper atmosphere]] of Titan, a [[PAH world hypothesis|possible precursor for life]].<ref name="IAA-20130606">{{cite news |last=López-Puertas |first=Manuel |url=http://www.iaa.es/content/pahs-titans-upper-atmosphere |title=PAH's in Titan's Upper Atmosphere |date=6 June 2013 |work=[[Spanish National Research Council|CSIC]] |access-date=6 June 2013 |archive-date=22 August 2016 |archive-url=https://web.archive.org/web/20160822010505/http://www.iaa.es/content/pahs-titans-upper-atmosphere |url-status=live }}</ref> 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 [[comet]]s, and not from the materials that formed Saturn in earlier times.<ref name="NASA-201450623">{{cite web |display-authors=1 |last1=Dyches |first1=Preston |last2=Clavin |first2=Clavin |title=Titan's Building Blocks Might Pre-date Saturn |url=http://www.jpl.nasa.gov/news/news.php?release=2014-200 |date=23 June 2014 |work=NASA |access-date=24 June 2014 |archive-date=9 September 2018 |archive-url=https://web.archive.org/web/20180909162240/https://www.jpl.nasa.gov/news/news.php?release=2014-200 |url-status=live }}</ref> | ||
Saturn's moon [[Enceladus]], which seems similar in chemical makeup to comets,<ref name="NS-20080326">{{cite web |last=Battersby |first=Stephen |title=Saturn's moon Enceladus surprisingly comet-like |url=https://www.newscientist.com/article/dn13541-saturns-moon-enceladus-surprisingly-cometlike.html |date=26 March 2008 |work=[[New Scientist]] |access-date=16 April 2015 |archive-date=30 June 2015 |archive-url=https://web.archive.org/web/20150630011601/http://www.newscientist.com/article/dn13541-saturns-moon-enceladus-surprisingly-cometlike.html |url-status=live }}</ref> has often been regarded as a potential [[Planetary habitability|habitat]] for [[Microorganism|microbial life]].<ref>{{cite web |url=http://www.sciencedaily.com/releases/2008/04/080420122601.htm |title=Could There Be Life On Saturn's Moon Enceladus? |website=ScienceDaily |author=NASA |date=21 April 2008 |access-date=19 July 2011 |archive-url=https://web.archive.org/web/20111109041043/http://www.sciencedaily.com/releases/2008/04/080420122601.htm |archive-date=9 November 2011 |url-status=live }}</ref><ref name=madrigal20090624/><ref name=spotts20050928/><ref>{{cite web |url=http://scienceray.com/astronomy/enceladus-saturns-moon-has-liquid-ocean-of-water/ |title=Enceladus: Saturn′s Moon, Has Liquid Ocean of Water |last=Pili |first=Unofre |work=Scienceray |date=9 September 2009 |access-date=21 July 2011 |archive-url=https://web.archive.org/web/20111007220555/http://scienceray.com/astronomy/enceladus-saturns-moon-has-liquid-ocean-of-water/ |archive-date=7 October 2011 | Saturn's moon [[Enceladus]], which seems similar in chemical makeup to comets,<ref name="NS-20080326">{{cite web |last=Battersby |first=Stephen |title=Saturn's moon Enceladus surprisingly comet-like |url=https://www.newscientist.com/article/dn13541-saturns-moon-enceladus-surprisingly-cometlike.html |date=26 March 2008 |work=[[New Scientist]] |access-date=16 April 2015 |archive-date=30 June 2015 |archive-url=https://web.archive.org/web/20150630011601/http://www.newscientist.com/article/dn13541-saturns-moon-enceladus-surprisingly-cometlike.html |url-status=live }}</ref> has often been regarded as a potential [[Planetary habitability|habitat]] for [[Microorganism|microbial life]].<ref>{{cite web |url=http://www.sciencedaily.com/releases/2008/04/080420122601.htm |title=Could There Be Life On Saturn's Moon Enceladus? |website=ScienceDaily |author=NASA |date=21 April 2008 |access-date=19 July 2011 |archive-url=https://web.archive.org/web/20111109041043/http://www.sciencedaily.com/releases/2008/04/080420122601.htm |archive-date=9 November 2011 |url-status=live }}</ref><ref name=madrigal20090624/><ref name=spotts20050928/><ref>{{cite web |url=http://scienceray.com/astronomy/enceladus-saturns-moon-has-liquid-ocean-of-water/ |title=Enceladus: Saturn′s Moon, Has Liquid Ocean of Water |last=Pili |first=Unofre |work=Scienceray |date=9 September 2009 |access-date=21 July 2011 |archive-url=https://web.archive.org/web/20111007220555/http://scienceray.com/astronomy/enceladus-saturns-moon-has-liquid-ocean-of-water/ |archive-date=7 October 2011 }}</ref> 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.<ref>{{cite news |url=http://www.physorg.com/news/2011-06-strongest-evidence-icy-saturn-moon.html |title=Strongest evidence yet indicates Enceladus hiding saltwater ocean |publisher=Physorg |date=22 June 2011 |access-date=19 July 2011 |archive-url=https://web.archive.org/web/20111019155718/http://www.physorg.com/news/2011-06-strongest-evidence-icy-saturn-moon.html |archive-date=19 October 2011 |url-status=live }}</ref><ref>{{cite news |url=https://www.washingtonpost.com/national/health-science/saturns-moon-enceladus-shows-evidence-of-an-ocean-beneath-its-surface/2011/06/22/AGWYaPgH_story.html |title=Saturn′s moon Enceladus shows evidence of an ocean beneath its surface |newspaper=[[The Washington Post]] |last=Kaufman |first=Marc |date=22 June 2011 |access-date=19 July 2011 |archive-url=https://web.archive.org/web/20121112193955/http://www.washingtonpost.com/national/health-science/saturns-moon-enceladus-shows-evidence-of-an-ocean-beneath-its-surface/2011/06/22/AGWYaPgH_story.html |archive-date=12 November 2012 |url-status=live }}</ref><ref>{{cite news |url=http://www.nasa.gov/mission_pages/cassini/whycassini/cassini20110622.html |title=Cassini Captures Ocean-Like Spray at Saturn Moon |publisher=NASA |display-authors=1 |author=Greicius, Tony |author2=Dunbar, Brian |date=22 June 2011 |access-date=17 September 2011 |archive-url=https://web.archive.org/web/20110914203739/http://www.nasa.gov/mission_pages/cassini/whycassini/cassini20110622.html |archive-date=14 September 2011 |url-status=live }} | ||
</ref> A 2015 flyby by ''Cassini'' through a plume on Enceladus found most of the ingredients to sustain life forms that live by [[methanogenesis]].<ref name="nasa20170413">{{cite web |url=https://www.nasa.gov/press-release/nasa-missions-provide-new-insights-into-ocean-worlds-in-our-solar-system |title=NASA Missions Provide New Insights into 'Ocean Worlds' in Our Solar System |first1=Felicia |last1=Chou |first2=Preston |last2=Dyches |first3=Donna |last3=Weaver |first4=Ray |last4=Villard |publisher=NASA |date=13 April 2017 |access-date=20 April 2017 |archive-date=20 April 2017 |archive-url=https://web.archive.org/web/20170420143202/https://www.nasa.gov/press-release/nasa-missions-provide-new-insights-into-ocean-worlds-in-our-solar-system/ |url-status=live }}</ref> | </ref> A 2015 flyby by ''Cassini'' through a plume on Enceladus found most of the ingredients to sustain life forms that live by [[methanogenesis]].<ref name="nasa20170413">{{cite web |url=https://www.nasa.gov/press-release/nasa-missions-provide-new-insights-into-ocean-worlds-in-our-solar-system |title=NASA Missions Provide New Insights into 'Ocean Worlds' in Our Solar System |first1=Felicia |last1=Chou |first2=Preston |last2=Dyches |first3=Donna |last3=Weaver |first4=Ray |last4=Villard |publisher=NASA |date=13 April 2017 |access-date=20 April 2017 |archive-date=20 April 2017 |archive-url=https://web.archive.org/web/20170420143202/https://www.nasa.gov/press-release/nasa-missions-provide-new-insights-into-ocean-worlds-in-our-solar-system/ |url-status=live }}</ref> | ||
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== Planetary rings == | == Planetary rings == | ||
{{Main|Rings of Saturn}} | {{Main|Rings of Saturn}} | ||
[[File:Saturn from Cassini Orbiter (2004-10-06).jpg|thumb|The [[rings of Saturn]] | [[File:Saturn from Cassini Orbiter (2004-10-06).jpg|thumb|The [[rings of Saturn]], imaged here by ''[[Cassini–Huygens|Cassini]]'' in October 2004, are the most massive and conspicuous in the Solar System.<ref name="NMM Saturn" />]] | ||
Saturn is probably best known for the system of [[planetary ring]]s that makes it visually unique.<ref name="NMM Saturn">{{cite web |title=Saturn |url=http://www.nmm.ac.uk/server/show/conWebDoc.286 |publisher=National Maritime Museum |access-date=6 July 2007 |archive-url=https://web.archive.org/web/20080623204304/http://www.nmm.ac.uk/server/show/conWebDoc.286 |archive-date=23 June 2008 | |||
Saturn is probably best known for the system of [[planetary ring]]s that makes it visually unique.<ref name="NMM Saturn">{{cite web |title=Saturn |url=http://www.nmm.ac.uk/server/show/conWebDoc.286 |publisher=National Maritime Museum |access-date=6 July 2007 |archive-url=https://web.archive.org/web/20080623204304/http://www.nmm.ac.uk/server/show/conWebDoc.286 |archive-date=23 June 2008 |date=20 August 2015 }}</ref> The rings extend from {{convert|6630|to|120700|km|mi}} outward from Saturn's equator and average approximately {{convert|20|m|ft}} in thickness. They are composed predominantly of water ice, with trace amounts of [[tholin]] impurities and a peppered coating of approximately 7% amorphous [[carbon]].<ref>{{cite journal |title=The Composition of Saturn's Rings |display-authors=1 |author=Poulet F. |author2=Cuzzi J.N. |journal=Icarus |doi=10.1006/icar.2002.6967 |volume=160 |page=350 |date=2002 |bibcode=2002Icar..160..350P |issue=2 |url=https://zenodo.org/record/1229856 |access-date=28 June 2019 |archive-date=29 July 2019 |archive-url=https://web.archive.org/web/20190729190601/https://zenodo.org/record/1229856 |url-status=live }}</ref> The particles that make up the rings range in size from specks of dust up to 10 m.<ref>{{cite web |last=Porco |first=Carolyn |author-link=Carolyn Porco |title=Questions about Saturn's rings |website=CICLOPS web site |url=http://www.ciclops.org/sci/common_questions.php#ring |access-date=18 June 2017 |archive-date=3 October 2012 |archive-url=https://web.archive.org/web/20121003073842/http://www.ciclops.org/sci/common_questions.php#ring |url-status=live }}</ref> While the other [[gas giant]]s also have ring systems, Saturn's is the largest and most visible. | |||
There is a debate on the age of the rings. One side supports that they are ancient, and were [[Formation and evolution of the Solar System|created simultaneously with Saturn from the original nebular material]] (around 4.6 billion years ago),<ref>{{cite journal |last1=Canup |first1=Robin M. |title=Origin of Saturn's rings and inner moons by mass removal from a lost Titan-sized satellite |journal=Nature |date=December 2010 |volume=468 |issue=7326 |pages=943–946 |doi=10.1038/nature09661 |pmid=21151108 |bibcode=2010Natur.468..943C |url=https://www.nature.com/articles/nature09661 |access-date=22 May 2024 |language=en |issn=1476-4687|url-access=subscription }}</ref> or shortly after the [[Late Heavy Bombardment|LHB]] (around 4.1 to 3.8 billion years ago).<ref>{{cite journal |last1=Crida |first1=A. |last2=Charnoz |first2=S. |title=Formation of Regular Satellites from Ancient Massive Rings in the Solar System |journal=Science |date=30 November 2012 |volume=338 |issue=6111 |pages=1196–1199 |doi=10.1126/science.1226477 |pmid=23197530 | There is a debate on the age of the rings. One side supports that they are ancient, and were [[Formation and evolution of the Solar System|created simultaneously with Saturn from the original nebular material]] (around 4.6 billion years ago),<ref>{{cite journal |last1=Canup |first1=Robin M. |title=Origin of Saturn's rings and inner moons by mass removal from a lost Titan-sized satellite |journal=Nature |date=December 2010 |volume=468 |issue=7326 |pages=943–946 |doi=10.1038/nature09661 |pmid=21151108 |bibcode=2010Natur.468..943C |url=https://www.nature.com/articles/nature09661 |access-date=22 May 2024 |language=en |issn=1476-4687|url-access=subscription }}</ref> or shortly after the [[Late Heavy Bombardment|LHB]] (around 4.1 to 3.8 billion years ago).<ref>{{cite journal |last1=Crida |first1=A. |last2=Charnoz |first2=S. |title=Formation of Regular Satellites from Ancient Massive Rings in the Solar System |journal=Science |date=30 November 2012 |volume=338 |issue=6111 |pages=1196–1199 |doi=10.1126/science.1226477 |pmid=23197530 |arxiv=1301.3808 |bibcode=2012Sci...338.1196C }}</ref><ref>{{cite journal |last1=Charnoz |first1=Sébastien |last2=Morbidelli |first2=Alessandro |last3=Dones |first3=Luke |last4=Salmon |first4=Julien |title=Did Saturn's rings form during the Late Heavy Bombardment? |url=https://www.sciencedirect.com/science/article/abs/pii/S0019103508003825 |journal=Icarus |date=February 2009 |volume=199 |issue=2 |pages=413–428 |doi=10.1016/j.icarus.2008.10.019 |access-date=22 May 2024 |arxiv=0809.5073 |bibcode=2009Icar..199..413C }}</ref> The other side supports that they are much younger, created around 100 million years ago.<ref>{{cite journal |last1=Kempf |first1=Sascha |last2=Altobelli |first2=Nicolas |last3=Schmidt |first3=Jürgen |last4=Cuzzi |first4=Jeffrey N. |last5=Estrada |first5=Paul R. |last6=Srama |first6=Ralf |title=Micrometeoroid infall onto Saturn's rings constrains their age to no more than a few hundred million years |journal=Science Advances |date=12 May 2023 |volume=9 |issue=19 |article-number=eadf8537 |doi=10.1126/sciadv.adf8537 |pmid=37172091 |pmc=10181170 |bibcode=2023SciA....9F8537K }}</ref><ref name="NYT-210230928">{{cite news |last=Andrew |first=Robin George |title=Saturn's Rings May Have Formed in a Surprisingly Recent Crash of 2 Moons - Researchers completed a complex simulation that supports the idea that the giant planet's jewelry emerged hundreds of millions of years ago, not billions. |url=https://www.nytimes.com/2023/09/28/science/saturn-rings-moons-formation.html |date=28 September 2023 |work=[[The New York Times]] |url-status=live |archive-url=https://archive.today/20230929044637/https://www.nytimes.com/2023/09/28/science/saturn-rings-moons-formation.html |archive-date=29 September 2023 |access-date=29 September 2023 }}</ref><ref name="TAJ-20230927">{{cite journal |author=Teodoro, L.F.A. |display-authors=et al |title=A Recent Impact Origin of Saturn's Rings and Mid-sized Moons |date=27 September 2023 |journal=[[The Astrophysical Journal]]|volume=955 |number=2 |page=137 |doi=10.3847/1538-4357/acf4ed |arxiv=2309.15156 |bibcode=2023ApJ...955..137T |doi-access=free }}</ref> An [[Massachusetts Institute of Technology|MIT]] research team, supporting the latter theory, proposed that the rings are remnant of a destroyed moon of Saturn, named [[Chrysalis (hypothetical moon)|″Chrysalis″]].<ref name="chrysalis">{{Cite journal|url=https://www.science.org/doi/10.1126/science.abn1234|title=Loss of a satellite could explain Saturn's obliquity and young rings|first1=Jack|last1=Wisdom|first2=Rola|last2=Dbouk|first3=Burkhard|last3=Militzer|first4=William B.|last4=Hubbard|first5=Francis|last5=Nimmo|first6=Brynna G.|last6=Downey|first7=Richard G.|last7=French|date=16 September 2022|journal=Science|volume=377|issue=6612|pages=1285–1289|doi=10.1126/science.abn1234|pmid=36107998|bibcode=2022Sci...377.1285W |hdl=1721.1/148216 |s2cid=252310492 |url-access=subscription|hdl-access=free}}</ref> | ||
Beyond the main rings, at a distance of 12 million km (7.5 million mi) from the planet is the sparse Phoebe ring. It is tilted at an angle of 27° to the other rings and, like [[Phoebe (moon)|Phoebe]], orbits in [[Retrograde motion|retrograde]] fashion.<ref>{{cite web |first=Rob |last=Cowen |date=7 November 1999 |url=http://www.sciencenews.org/view/generic/id/48097/title/Largest_known_planetary_ring_discovered |title=Largest known planetary ring discovered |work=Science News |access-date=9 April 2010 |archive-url=https://web.archive.org/web/20110822023022/http://www.sciencenews.org/view/generic/id/48097/title/Largest_known_planetary_ring_discovered |archive-date=22 August 2011 |url-status=live }}</ref> | Beyond the main rings, at a distance of 12 million km (7.5 million mi) from the planet is the sparse Phoebe ring. It is tilted at an angle of 27° to the other rings and, like [[Phoebe (moon)|Phoebe]], orbits in [[Retrograde motion|retrograde]] fashion.<ref>{{cite web |first=Rob |last=Cowen |date=7 November 1999 |url=http://www.sciencenews.org/view/generic/id/48097/title/Largest_known_planetary_ring_discovered |title=Largest known planetary ring discovered |work=Science News |access-date=9 April 2010 |archive-url=https://web.archive.org/web/20110822023022/http://www.sciencenews.org/view/generic/id/48097/title/Largest_known_planetary_ring_discovered |archive-date=22 August 2011 |url-status=live }}</ref> | ||
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Some of the moons of Saturn, including [[Pandora (moon)|Pandora]] and [[Prometheus (moon)|Prometheus]], act as [[shepherd moon]]s to confine the rings and prevent them from spreading out.<ref name=russell2004/> [[Pan (moon)|Pan]] and [[Atlas (moon)|Atlas]] cause weak, linear density waves in Saturn's rings that have yielded more reliable calculations of their masses.<ref>{{cite web |url=http://www.sciencedaily.com/releases/2005/02/050225110106.htm |title=NASA's Cassini Spacecraft Continues Making New Discoveries |website=ScienceDaily |author=NASA Jet Propulsion Laboratory |date=3 March 2005 |access-date=19 July 2011 |archive-url=https://web.archive.org/web/20111108223641/http://www.sciencedaily.com/releases/2005/02/050225110106.htm |archive-date=8 November 2011 |url-status=live }}</ref> | Some of the moons of Saturn, including [[Pandora (moon)|Pandora]] and [[Prometheus (moon)|Prometheus]], act as [[shepherd moon]]s to confine the rings and prevent them from spreading out.<ref name=russell2004/> [[Pan (moon)|Pan]] and [[Atlas (moon)|Atlas]] cause weak, linear density waves in Saturn's rings that have yielded more reliable calculations of their masses.<ref>{{cite web |url=http://www.sciencedaily.com/releases/2005/02/050225110106.htm |title=NASA's Cassini Spacecraft Continues Making New Discoveries |website=ScienceDaily |author=NASA Jet Propulsion Laboratory |date=3 March 2005 |access-date=19 July 2011 |archive-url=https://web.archive.org/web/20111108223641/http://www.sciencedaily.com/releases/2005/02/050225110106.htm |archive-date=8 November 2011 |url-status=live }}</ref> | ||
{{wide image|Saturn's rings dark side mosaic.jpg|2200px| | {{wide image|Saturn's rings dark side mosaic.jpg|2200px|A natural-color mosaic of ''Cassini'' narrow-angle camera images of the unilluminated side of Saturn's D, C, B, A, and F rings (left to right), taken on 9 May 2007. Distances are to Saturn's center.}} | ||
== History of observation and exploration == | == History of observation and exploration == | ||
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{{See also|Saturn (mythology)|Planets in astrology#Saturn}} | {{See also|Saturn (mythology)|Planets in astrology#Saturn}} | ||
Saturn has been known since prehistoric times,<ref name="NMM Saturn 2">{{cite web |title=Observing Saturn |url=http://www.nmm.ac.uk/server/show/conWebDoc.13852/viewPage/5 |publisher=[[National Maritime Museum]] |access-date=6 July 2007 |archive-url=https://web.archive.org/web/20070422014136/http://www.nmm.ac.uk/server/show/conWebDoc.13852/viewPage/5 <!--Added by H3llBot--> |archive-date=22 April 2007|date=20 August 2015 }}</ref> and in early recorded history it was a major character in various mythologies. [[Babylonian astronomy|Babylonian astronomers]] systematically observed and recorded the movements of Saturn.<ref name=ptrsl276_1257_43/> In ancient Greek, the planet was known as {{lang|grc|Φαίνων}} '''''[[Phaenon|Phainon]]''''',<ref>{{LSJ|*fai/nwn|Φαίνων|ref|mLSJ}}.</ref> and in Roman times it was known as the "star of [[Saturn (mythology)|Saturn]]" or the "star of the [[Sun]] (i.e. [[Helios]])".<ref>Cicero, ''De Natura Deorum''.</ref><ref>{{Cite journal |last1=Neuhäuser |first1=R |last2=Torres |first2=G |last3=Mugrauer |first3=M |last4=Neuhäuser |first4=D L |last5=Chapman |first5=J |last6=Luge |first6=D |last7=Cosci |first7=M |date=2022-10-11 |title=Colour evolution of Betelgeuse and Antares over two millennia, derived from historical records, as a new constraint on mass and age |url=https://academic.oup.com/mnras/article/516/1/693/6651563 |journal=Monthly Notices of the Royal Astronomical Society |volume=516 |issue=1 |pages=693–719 |doi=10.1093/mnras/stac1969 |doi-access=free |issn=0035-8711|arxiv=2207.04702 }}</ref> In [[Roman mythology|ancient Roman mythology]], the planet Phainon was sacred to this agricultural god, from which the planet takes its modern name.<ref name="Saturn in ancient mythologies" /> The Romans considered the god Saturnus the equivalent of the [[Greek mythology|Greek god]] [[Cronus]] | Saturn has been known since prehistoric times,<ref name="NMM Saturn 2">{{cite web |title=Observing Saturn |url=http://www.nmm.ac.uk/server/show/conWebDoc.13852/viewPage/5 |publisher=[[National Maritime Museum]] |access-date=6 July 2007 |archive-url=https://web.archive.org/web/20070422014136/http://www.nmm.ac.uk/server/show/conWebDoc.13852/viewPage/5 <!--Added by H3llBot--> |archive-date=22 April 2007|date=20 August 2015 }}</ref> and in early recorded history it was a major character in various mythologies. [[Babylonian astronomy|Babylonian astronomers]] systematically observed and recorded the movements of Saturn.<ref name=ptrsl276_1257_43/> In ancient Greek, the planet was known as {{lang|grc|Φαίνων}} '''''[[Phaenon|Phainon]]''''',<ref>{{LSJ|*fai/nwn|Φαίνων|ref|mLSJ}}.</ref> and in Roman times it was known as the "star of [[Saturn (mythology)|Saturn]]" or the "star of the [[Sun]] (i.e. [[Helios]])".<ref>Cicero, ''De Natura Deorum''.</ref><ref>{{Cite journal |last1=Neuhäuser |first1=R |last2=Torres |first2=G |last3=Mugrauer |first3=M |last4=Neuhäuser |first4=D L |last5=Chapman |first5=J |last6=Luge |first6=D |last7=Cosci |first7=M |date=2022-10-11 |title=Colour evolution of Betelgeuse and Antares over two millennia, derived from historical records, as a new constraint on mass and age |url=https://academic.oup.com/mnras/article/516/1/693/6651563 |journal=Monthly Notices of the Royal Astronomical Society |volume=516 |issue=1 |pages=693–719 |doi=10.1093/mnras/stac1969 |doi-access=free |issn=0035-8711|arxiv=2207.04702 }}</ref> In [[Roman mythology|ancient Roman mythology]], the planet Phainon was sacred to this agricultural god, from which the planet takes its modern name.<ref name="Saturn in ancient mythologies" /> The Romans considered the god Saturnus the equivalent of the [[Greek mythology|Greek god]] [[Cronus]]. In modern [[Greek language|Greek]], the planet retains the name ''Cronus''—{{Langx|el|Κρόνος|label=none}}: ''Kronos''.<ref>{{cite web |url=http://www.greek-names.info/greek-names-of-the-planets/ |title=Greek Names of the Planets |access-date=14 July 2012 |quote=The Greek name of the planet Saturn is Kronos. The Titan Cronus was the father of [[Zeus]], while Saturn was the Roman God of agriculture. |date=25 April 2010 |archive-date=9 May 2010 |archive-url=https://web.archive.org/web/20100509164917/http://www.greek-names.info/greek-names-of-the-planets/ |url-status=live }} See also the [[:el:Κρόνος (πλανήτης)|Greek article about the planet]].</ref> | ||
The Greek scientist [[Ptolemy]] based his calculations of Saturn's orbit on observations he made while it was in [[opposition (astronomy)|opposition]].<ref name=ps04_1893_862/> In [[Jyotisha|Hindu astrology]], there are nine astrological objects, known as [[Navagraha]]s. Saturn is known as "[[Shani]]" and judges everyone based on the good and bad deeds performed in life.<ref name="Saturn in ancient mythologies">{{cite web |title=Starry Night Times |url=http://www.starrynight.com/sntimes/2006/2006-01-full.html |access-date=5 July 2007 |date=2006 |publisher=Imaginova Corp. |archive-url=https://web.archive.org/web/20091001001723/http://starrynight.com/sntimes/2006/2006-01-full.html |archive-date=1 October 2009 | The Greek scientist [[Ptolemy]] based his calculations of Saturn's orbit on observations he made while it was in [[opposition (astronomy)|opposition]].<ref name=ps04_1893_862/> In [[Jyotisha|Hindu astrology]], there are nine astrological objects, known as [[Navagraha]]s. Saturn is known as "[[Shani]]" and judges everyone based on the good and bad deeds performed in life.<ref name="Saturn in ancient mythologies">{{cite web |title=Starry Night Times |url=http://www.starrynight.com/sntimes/2006/2006-01-full.html |access-date=5 July 2007 |date=2006 |publisher=Imaginova Corp. |archive-url=https://web.archive.org/web/20091001001723/http://starrynight.com/sntimes/2006/2006-01-full.html |archive-date=1 October 2009 }}</ref><ref name=ps04_1893_862/> Ancient [[Chinese astrology|Chinese]] and Japanese culture designated the planet Saturn as the "earth star" or "soil star" ({{lang|zh|土星}}). This was based on [[Five elements (Chinese philosophy)|Five Elements]] which were traditionally used to classify natural elements.<ref>{{cite book |first=Jan Jakob Maria |last=De Groot |year=1912 |title=Religion in China: universism. a key to the study of Taoism and Confucianism |series=American lectures on the history of religions |volume=10 |page=300 |publisher=G. P. Putnam's Sons |url=https://books.google.com/books?id=ZAaP7dyjCrAC&pg=PA300 |access-date=8 January 2010 |archive-date=22 July 2011 |archive-url=https://web.archive.org/web/20110722005812/http://books.google.com/books?id=ZAaP7dyjCrAC&pg=PA300 |url-status=live }}</ref><ref>{{cite book |first=Thomas |last=Crump |year=1992 |title=The Japanese numbers game: the use and understanding of numbers in modern Japan |pages=39–40 |publisher=Routledge |isbn=978-0-415-05609-0}}</ref><ref>{{cite book |first=Homer Bezaleel |last=Hulbert |year=1909 |title=The passing of Korea |page=[https://archive.org/details/passingkorea01hulbgoog/page/n538 426] |publisher=Doubleday, Page & company |url=https://archive.org/details/passingkorea01hulbgoog |access-date=8 January 2010}}</ref> | ||
In [[Hebrew language|Hebrew]], Saturn is called ''[[Shabtai|Shabbathai]]''.<ref>{{cite news |url=http://www.universetoday.com/45087/when-was-saturn-discovered/ |title=When Was Saturn Discovered? |work=Universe Today |last=Cessna |first=Abby |date=15 November 2009 |access-date=21 July 2011 |archive-url=https://web.archive.org/web/20120214113458/http://www.universetoday.com/45087/when-was-saturn-discovered/ |archive-date=14 February 2012 |url-status=live }}</ref> Its angel is [[Cassiel]]. Its intelligence or beneficial spirit is [[Agiel|'Agȋȇl]] ({{langx|he|אגיאל|ʿAgyal}}),<ref name="TheMagus" /> and its darker spirit ([[demon]]) is [[Zazel (spirit)|Zȃzȇl]] ({{langx|he|זאזל|Zazl}}).<ref name="TheMagus">{{cite web |title=The Magus, Book I: The Celestial Intelligencer: Chapter XXVIII |url=http://www.sacred-texts.com/grim/magus/ma150.htm |work=Sacred-Text.com |access-date=4 August 2018 |archive-date=19 June 2018 |archive-url=https://web.archive.org/web/20180619080731/http://www.sacred-texts.com/grim/magus/ma150.htm |url-status=live }}</ref><ref name="CrystalLinks">{{cite web |title=Saturn in Mythology |url=http://www.crystalinks.com/saturn.mythology.html |work=CrystalLinks.com |access-date=5 August 2018 |archive-date=8 July 2018 |archive-url=https://web.archive.org/web/20180708190230/http://crystalinks.com/saturn.mythology.html |url-status=live }}</ref><ref name="TC-20170308">{{cite web |last=Beyer |first=Catherine |title=Planetary Spirit Sigils – 01 Spirit of Saturn |url=https://www.thoughtco.com/planetary-spirit-sigils-4123081 |date=8 March 2017 |work=ThoughtCo.com |access-date=3 August 2018 |archive-date=4 August 2018 |archive-url=https://web.archive.org/web/20180804014119/https://www.thoughtco.com/planetary-spirit-sigils-4123081 |url-status=live }}</ref> Zazel has been described as a [[Angel|great angel]], invoked in [[Solomon#Angels and magic|Solomonic magic]], who is "effective in [[Evocation|love conjurations]]".<ref name="FE-2014">{{cite web |url=http://baby-names.familyeducation.com/name-meaning/zazel |title=Meaning and Origin of: Zazel |work=FamilyEducation.com |date=2014 |access-date=3 August 2018 |quote=Latin: Angel summoned for love invocations |archive-date=2 January 2015 |archive-url=https://web.archive.org/web/20150102063304/http://baby-names.familyeducation.com/name-meaning/zazel |url-status=live }}</ref><ref name="HP-1998">{{cite web |url=http://hafapea.com/angelpages/angels7.html |title=Angelic Beings |work=Hafapea.com |date=1998 |access-date=3 August 2018 |quote=a Solomonic angel of love rituals |archive-date=22 July 2018 |archive-url=https://web.archive.org/web/20180722154808/http://hafapea.com/angelpages/angels7.html | In [[Hebrew language|Hebrew]], Saturn is called ''[[Shabtai|Shabbathai]]''.<ref>{{cite news |url=http://www.universetoday.com/45087/when-was-saturn-discovered/ |title=When Was Saturn Discovered? |work=Universe Today |last=Cessna |first=Abby |date=15 November 2009 |access-date=21 July 2011 |archive-url=https://web.archive.org/web/20120214113458/http://www.universetoday.com/45087/when-was-saturn-discovered/ |archive-date=14 February 2012 |url-status=live }}</ref> Its angel is [[Cassiel]]. Its intelligence or beneficial spirit is [[Agiel|'Agȋȇl]] ({{langx|he|אגיאל|ʿAgyal}}),<ref name="TheMagus" /> and its darker spirit ([[demon]]) is [[Zazel (spirit)|Zȃzȇl]] ({{langx|he|זאזל|Zazl}}).<ref name="TheMagus">{{cite web |title=The Magus, Book I: The Celestial Intelligencer: Chapter XXVIII |url=http://www.sacred-texts.com/grim/magus/ma150.htm |work=Sacred-Text.com |access-date=4 August 2018 |archive-date=19 June 2018 |archive-url=https://web.archive.org/web/20180619080731/http://www.sacred-texts.com/grim/magus/ma150.htm |url-status=live }}</ref><ref name="CrystalLinks">{{cite web |title=Saturn in Mythology |url=http://www.crystalinks.com/saturn.mythology.html |work=CrystalLinks.com |access-date=5 August 2018 |archive-date=8 July 2018 |archive-url=https://web.archive.org/web/20180708190230/http://crystalinks.com/saturn.mythology.html |url-status=live }}</ref><ref name="TC-20170308">{{cite web |last=Beyer |first=Catherine |title=Planetary Spirit Sigils – 01 Spirit of Saturn |url=https://www.thoughtco.com/planetary-spirit-sigils-4123081 |date=8 March 2017 |work=ThoughtCo.com |access-date=3 August 2018 |archive-date=4 August 2018 |archive-url=https://web.archive.org/web/20180804014119/https://www.thoughtco.com/planetary-spirit-sigils-4123081 |url-status=live }}</ref> Zazel has been described as a [[Angel|great angel]], invoked in [[Solomon#Angels and magic|Solomonic magic]], who is "effective in [[Evocation|love conjurations]]".<ref name="FE-2014">{{cite web |url=http://baby-names.familyeducation.com/name-meaning/zazel |title=Meaning and Origin of: Zazel |work=FamilyEducation.com |date=2014 |access-date=3 August 2018 |quote=Latin: Angel summoned for love invocations |archive-date=2 January 2015 |archive-url=https://web.archive.org/web/20150102063304/http://baby-names.familyeducation.com/name-meaning/zazel |url-status=live }}</ref><ref name="HP-1998">{{cite web |url=http://hafapea.com/angelpages/angels7.html |title=Angelic Beings |work=Hafapea.com |date=1998 |access-date=3 August 2018 |quote=a Solomonic angel of love rituals |archive-date=22 July 2018 |archive-url=https://web.archive.org/web/20180722154808/http://hafapea.com/angelpages/angels7.html }}</ref> In [[Ottoman Turkish language|Ottoman Turkish]], [[Urdu]], and [[Malay language|Malay]], the name of Zazel is 'Zuhal', derived from the [[Arabic language]] ({{langx|ar|زحل|Zuhal}}).<ref name="CrystalLinks" /> | ||
=== Telescopic pre-spaceflight observations === | === Telescopic pre-spaceflight observations === | ||
[[File:Galileo.arp.300pix.jpg|thumb|180px|[[Galileo Galilei]] observed the rings of Saturn in 1610, but was unable to determine what they were.]] | [[File:Galileo.arp.300pix.jpg|thumb|180px|[[Galileo Galilei]] observed the rings of Saturn in 1610, but was unable to determine what they were.]] | ||
[[File:Saturn Robert Hooke 1666.jpg|thumb|[[Robert Hooke]] noted the shadows ({{Var|a}} and {{Var|b}}) cast by both the globe and the rings on each other in this drawing of Saturn in 1666.|left]] | |||
[[ | Saturn's rings require at least a 15-mm-diameter [[telescope]]<ref name=binoculars/> to resolve and were not known to exist until [[Christiaan Huygens]] saw them in 1655 and published his observations in 1659. [[Galileo]], with his primitive telescope in 1610,<ref name=chan2000/><ref name=cain2008_15390/> incorrectly thought of Saturn's appearing not quite round as two moons on Saturn's sides.<ref name=cain2008_15418/><ref name=cain2008_46237/> | ||
When Huygens used greater telescopic magnification this notion was refuted, and the rings were truly seen for the first time. Huygens discovered Saturn's [[Titan (moon)|moon Titan]]. [[Giovanni Domenico Cassini]] later discovered four other moons: [[Iapetus (moon)|Iapetus]], [[Rhea (moon)|Rhea]], [[Tethys (moon)|Tethys]], and [[Dione (moon)|Dione]]. In 1675, Cassini discovered the gap now known as the [[Cassini Division]].<ref name=micek2007/> | |||
No further discoveries of significance were made until 1789 when [[William Herschel]] discovered two further moons, [[Mimas (moon)|Mimas]] and [[Enceladus]]. The irregularly shaped satellite [[Hyperion (moon)|Hyperion]], which has a [[orbital resonance|resonance]] with Titan, was discovered in 1848 by a British team.<ref name=pa54_122/> | No further discoveries of significance were made until 1789 when [[William Herschel]] discovered two further moons, [[Mimas (moon)|Mimas]] and [[Enceladus]]. The irregularly shaped satellite [[Hyperion (moon)|Hyperion]], which has a [[orbital resonance|resonance]] with Titan, was discovered in 1848 by a British team.<ref name=pa54_122/> | ||
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[[File:P11saturnb.jpg|thumb|''Pioneer 11'' image of Saturn]] | [[File:P11saturnb.jpg|thumb|''Pioneer 11'' image of Saturn]] | ||
''[[Pioneer 11]]'' made the first flyby of Saturn in September 1979, when it passed within {{Convert|20000|km|abbr=on}} 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 a high [[Phase angle (astronomy)|phase angle]] (towards the Sun), meaning that they contain fine light-scattering material. In addition, ''Pioneer 11'' measured the temperature of Titan.<ref>{{cite web |url=http://spaceprojects.arc.nasa.gov/Space_Projects/pioneer/PN10&11.html |title=The Pioneer 10 & 11 Spacecraft |access-date=5 July 2007 |publisher=Mission Descriptions |archive-url=https://web.archive.org/web/20060130100401/http://spaceprojects.arc.nasa.gov/Space_Projects/pioneer/PN10%2611.html |archive-date=30 January 2006 | ''[[Pioneer 11]]'' made the first flyby of Saturn in September 1979, when it passed within {{Convert|20000|km|abbr=on}} 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 a high [[Phase angle (astronomy)|phase angle]] (towards the Sun), meaning that they contain fine light-scattering material. In addition, ''Pioneer 11'' measured the temperature of Titan.<ref>{{cite web |url=http://spaceprojects.arc.nasa.gov/Space_Projects/pioneer/PN10&11.html |title=The Pioneer 10 & 11 Spacecraft |access-date=5 July 2007 |publisher=Mission Descriptions |archive-url=https://web.archive.org/web/20060130100401/http://spaceprojects.arc.nasa.gov/Space_Projects/pioneer/PN10%2611.html |archive-date=30 January 2006 }}</ref> | ||
==== ''Voyager'' flybys ==== | ==== ''Voyager'' flybys ==== | ||
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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. 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.<ref name="Voyager" /> | 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. 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.<ref name="Voyager" /> | ||
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 [[Rings of Saturn#C Ring|C Ring]]) and [[Keeler gap]] (a 42 km-wide gap in the [[A Ring]]).<ref>{{Cite book |last=Spence |first=Pam |url=https://books.google.com/books?id=DwR7JtuXnaQC |title=The Universe Revealed |date=1999 |publisher=Cambridge University Press |isbn=978-0-521-64239-2 | | 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 [[Rings of Saturn#C Ring|C Ring]]) and [[Keeler gap]] (a 42 km-wide gap in the [[A Ring]]).<ref>{{Cite book |last=Spence |first=Pam |url=https://books.google.com/books?id=DwR7JtuXnaQC |title=The Universe Revealed |date=1999 |publisher=Cambridge University Press |isbn=978-0-521-64239-2 |page=64 |language=en}}</ref> | ||
==== ''Cassini–Huygens'' spacecraft ==== | ==== ''Cassini–Huygens'' spacecraft ==== | ||
{{main|Cassini–Huygens}}[[File:Enceladus geysers June 2009.jpg|thumb|At Enceladus's south pole geysers spray water from many locations along the [[Tiger stripes (Enceladus)|tiger stripes]].<ref name="NASA-20140728" /> | {{main|Cassini–Huygens}} | ||
[[File:Enceladus geysers June 2009.jpg|thumb|At Enceladus's south pole, geysers spray water from many locations along the [[Tiger stripes (Enceladus)|tiger stripes]].<ref name="NASA-20140728" />]] | |||
The ''[[Cassini–Huygens]]'' [[space probe]] entered orbit around Saturn on 1 July 2004. In June 2004, it conducted a close flyby of [[Phoebe (moon)|Phoebe]], sending back high-resolution images and data. ''Cassini''{{'s}} flyby of Saturn's largest moon, Titan, captured radar images of large lakes and their coastlines with numerous islands and mountains. The orbiter completed two Titan flybys before releasing the [[Huygens (spacecraft)|''Huygens'' probe]] on 25 December 2004. ''Huygens'' descended onto the surface of Titan on 14 January 2005.<ref name="nature438_7069_758" /> | The ''[[Cassini–Huygens]]'' [[space probe]] entered orbit around Saturn on 1 July 2004. In June 2004, it conducted a close flyby of [[Phoebe (moon)|Phoebe]], sending back high-resolution images and data. ''Cassini''{{'s}} flyby of Saturn's largest moon, Titan, captured radar images of large lakes and their coastlines with numerous islands and mountains. The orbiter completed two Titan flybys before releasing the [[Huygens (spacecraft)|''Huygens'' probe]] on 25 December 2004. ''Huygens'' descended onto the surface of Titan on 14 January 2005.<ref name="nature438_7069_758" /> | ||
Starting in early 2005, scientists used ''Cassini'' to track lightning on Saturn. The power of the lightning is approximately 1,000 times that of lightning on Earth.<ref>{{cite web |url=http://www.sciencedaily.com/releases/2006/02/060215090726.htm |title=Astronomers Find Giant Lightning Storm At Saturn |date=2007 |access-date=27 July 2007 |publisher=ScienceDaily LLC |archive-url=https://web.archive.org/web/20110828092204/http://www.sciencedaily.com/releases/2006/02/060215090726.htm |archive-date=28 August 2011 |url-status=live }}</ref> | Starting in early 2005, scientists used ''Cassini'' to track lightning on Saturn. The power of the lightning is approximately 1,000 times that of lightning on Earth.<ref>{{cite web |url=http://www.sciencedaily.com/releases/2006/02/060215090726.htm |title=Astronomers Find Giant Lightning Storm At Saturn |date=2007 |access-date=27 July 2007 |publisher=ScienceDaily LLC |archive-url=https://web.archive.org/web/20110828092204/http://www.sciencedaily.com/releases/2006/02/060215090726.htm |archive-date=28 August 2011 |url-status=live }}</ref> | ||
In 2006, NASA reported that ''Cassini'' had found evidence of liquid [[Reservoir|water reservoirs]] no more than tens of meters below the surface that erupt in [[geyser]]s on Saturn's moon [[Enceladus (moon)|Enceladus]]. These jets of icy particles are emitted into orbit around Saturn from vents in the moon's south polar region.<ref>{{cite web |last1=Pence |first1=Michael |url=http://www.nasa.gov/mission_pages/cassini/media/cassini-20060309.html |title=NASA's Cassini Discovers Potential Liquid Water on Enceladus |date=9 March 2006 |publisher=[[NASA Jet Propulsion Laboratory]] |access-date=3 June 2011 |archive-url=https://web.archive.org/web/20110811013419/http://www.nasa.gov/mission_pages/cassini/media/cassini-20060309.html |archive-date=11 August 2011 |url-status=live }}</ref> Over 100 geysers have been identified on Enceladus.<ref name="NASA-20140728">{{cite web |display-authors=1 |last1=Dyches |first1=Preston |last2=Brown |first2=Dwayne |last3=Mullins |first3=Steve |title=Cassini Spacecraft Reveals 101 Geysers and More on Icy Saturn Moon |url=http://www.jpl.nasa.gov/news/news.php?release=2014-246&2 |date=28 July 2014 |work=NASA |access-date=29 July 2014 |archive-date=14 July 2017 |archive-url=https://web.archive.org/web/20170714031155/https://www.jpl.nasa.gov/news/news.php?release=2014-246&2 |url-status=live }}</ref> In May 2011, NASA scientists reported that Enceladus "is emerging as the most habitable spot beyond Earth in the Solar System for life as we know it".<ref>{{cite journal |last1=Lovett |first1=Richard A. |title=Enceladus named sweetest spot for alien life |url=http://www.nature.com/news/2011/110531/full/news.2011.337.html |date=31 May 2011 |access-date=3 June 2011 |doi=10.1038/news.2011.337 |archive-url=https://web.archive.org/web/20110905061010/http://www.nature.com/news/2011/110531/full/news.2011.337.html |archive-date=5 September 2011 |url-status=live |journal=Nature | | In 2006, NASA reported that ''Cassini'' had found evidence of liquid [[Reservoir|water reservoirs]] no more than tens of meters below the surface that erupt in [[geyser]]s on Saturn's moon [[Enceladus (moon)|Enceladus]]. These jets of icy particles are emitted into orbit around Saturn from vents in the moon's south polar region.<ref>{{cite web |last1=Pence |first1=Michael |url=http://www.nasa.gov/mission_pages/cassini/media/cassini-20060309.html |title=NASA's Cassini Discovers Potential Liquid Water on Enceladus |date=9 March 2006 |publisher=[[NASA Jet Propulsion Laboratory]] |access-date=3 June 2011 |archive-url=https://web.archive.org/web/20110811013419/http://www.nasa.gov/mission_pages/cassini/media/cassini-20060309.html |archive-date=11 August 2011 |url-status=live }}</ref> Over 100 geysers have been identified on Enceladus.<ref name="NASA-20140728">{{cite web |display-authors=1 |last1=Dyches |first1=Preston |last2=Brown |first2=Dwayne |last3=Mullins |first3=Steve |title=Cassini Spacecraft Reveals 101 Geysers and More on Icy Saturn Moon |url=http://www.jpl.nasa.gov/news/news.php?release=2014-246&2 |date=28 July 2014 |work=NASA |access-date=29 July 2014 |archive-date=14 July 2017 |archive-url=https://web.archive.org/web/20170714031155/https://www.jpl.nasa.gov/news/news.php?release=2014-246&2 |url-status=live }}</ref> In May 2011, NASA scientists reported that Enceladus "is emerging as the most habitable spot beyond Earth in the Solar System for life as we know it".<ref>{{cite journal |last1=Lovett |first1=Richard A. |title=Enceladus named sweetest spot for alien life |url=http://www.nature.com/news/2011/110531/full/news.2011.337.html |date=31 May 2011 |access-date=3 June 2011 |doi=10.1038/news.2011.337 |archive-url=https://web.archive.org/web/20110905061010/http://www.nature.com/news/2011/110531/full/news.2011.337.html |archive-date=5 September 2011 |url-status=live |journal=Nature |article-number=news.2011.337 |url-access=subscription }}</ref><ref>{{cite web |last1=Kazan |first1=Casey |title=Saturn's Enceladus Moves to Top of "Most-Likely-to-Have-Life" List |url=http://www.dailygalaxy.com/my_weblog/2011/06/saturns-enceladus-moves-to-top-of-most-likely-to-have-life-list.html |date=2 June 2011 |publisher=The Daily Galaxy |access-date=3 June 2011 |archive-url=https://web.archive.org/web/20110806103640/http://www.dailygalaxy.com/my_weblog/2011/06/saturns-enceladus-moves-to-top-of-most-likely-to-have-life-list.html |archive-date=6 August 2011 |url-status=live }}</ref> | ||
[[File:Saturn eclipse.jpg|thumb|Saturn eclipses the Sun, as seen from ''[[Cassini–Huygens|Cassini]]''. The rings are visible, including the [[F Ring]].]] | |||
''Cassini'' photographs 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 (moon)|Janus]] and [[Epimetheus (moon)|Epimetheus]].<ref>{{cite web |url=https://www.newscientist.com/article/dn10124-faint-new-ring-discovered-around-saturn/ |title=Faint new ring discovered around Saturn |access-date=8 July 2007 |date=20 September 2007 |last=Shiga |first=David |publisher=NewScientist.com |archive-url=https://web.archive.org/web/20080503212602/http://space.newscientist.com/channel/solar-system/cassini-huygens/dn10124-faint-new-ring-discovered-around-saturn.html |archive-date=3 May 2008 |url-status=live }}</ref> In July 2006, images were returned of hydrocarbon lakes near Titan's north pole, the presence of which were confirmed in January 2007. In March 2007, hydrocarbon seas were found near the North pole, the largest of which is almost the size of the [[Caspian Sea]].<ref>{{cite news |url= | ''Cassini'' photographs 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 (moon)|Janus]] and [[Epimetheus (moon)|Epimetheus]].<ref>{{cite web |url=https://www.newscientist.com/article/dn10124-faint-new-ring-discovered-around-saturn/ |title=Faint new ring discovered around Saturn |access-date=8 July 2007 |date=20 September 2007 |last=Shiga |first=David |publisher=NewScientist.com |archive-url=https://web.archive.org/web/20080503212602/http://space.newscientist.com/channel/solar-system/cassini-huygens/dn10124-faint-new-ring-discovered-around-saturn.html |archive-date=3 May 2008 |url-status=live }}</ref> In July 2006, images were returned of hydrocarbon lakes near Titan's north pole, the presence of which were confirmed in January 2007. In March 2007, hydrocarbon seas were found near the North pole, the largest of which is almost the size of the [[Caspian Sea]].<ref>{{cite news |url=https://news.bbc.co.uk/1/hi/sci/tech/6449081.stm |title=Probe reveals seas on Saturn moon |publisher=BBC |last=Rincon |first=Paul |access-date=26 September 2007 |date=14 March 2007 |archive-url=https://web.archive.org/web/20111111135219/http://news.bbc.co.uk/2/hi/science/nature/6449081.stm |archive-date=11 November 2011 |url-status=live }}</ref> In October 2006, the probe detected an {{Convert|8000|km|abbr=on}} diameter cyclone-like storm with an eyewall at Saturn's south pole.<ref>{{cite news |url=https://news.bbc.co.uk/2/hi/science/nature/6135450.stm |title=Huge 'hurricane' rages on Saturn |publisher=BBC |last=Rincon |first=Paul |access-date=12 July 2007 |date=10 November 2006 |archive-url=https://web.archive.org/web/20110902214204/http://news.bbc.co.uk/2/hi/science/nature/6135450.stm |archive-date=2 September 2011 |url-status=live }}</ref> | ||
From 2004 to 2 November 2009, the probe discovered and confirmed eight new satellites.<ref>{{cite web |url=http://saturn.jpl.nasa.gov/mission/introduction/ |title=Mission overview – introduction |date=2010 |work=Cassini Solstice Mission |publisher=NASA / JPL |access-date=23 November 2010 |archive-url=https://web.archive.org/web/20110807005756/http://saturn.jpl.nasa.gov/mission/introduction/ |archive-date=7 August 2011 | From 2004 to 2 November 2009, the probe discovered and confirmed eight new satellites.<ref>{{cite web |url=http://saturn.jpl.nasa.gov/mission/introduction/ |title=Mission overview – introduction |date=2010 |work=Cassini Solstice Mission |publisher=NASA / JPL |access-date=23 November 2010 |archive-url=https://web.archive.org/web/20110807005756/http://saturn.jpl.nasa.gov/mission/introduction/ |archive-date=7 August 2011 }}</ref> 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 {{convert|530|km/h|mph|abbr=on}}.<ref>{{cite news |url=http://www.3news.co.nz/Massive-storm-at-Saturns-north-pole/tabid/1160/articleID/296026/Default.aspx |work=3 News NZ |title=Massive storm at Saturn's north pole |date=30 April 2013 |access-date=30 April 2013 |archive-date=19 July 2014 |archive-url=https://web.archive.org/web/20140719200738/http://www.3news.co.nz/Massive-storm-at-Saturns-north-pole/tabid/1160/articleID/296026/Default.aspx |url-status=live }}</ref> On 15 September 2017, the ''Cassini–Huygens'' spacecraft performed the "Grand Finale" of its mission: a number of passes through gaps between Saturn and Saturn's inner rings.<ref name="NASA-20170915">{{cite news |last1=Brown |first1=Dwayne |last2=Cantillo |first2=Laurie |last3=Dyches |first3=Preston |title=NASA's Cassini Spacecraft Ends Its Historic Exploration of Saturn |url=https://www.jpl.nasa.gov/news/news.php?feature=6948 |date=15 September 2017 |work=NASA |access-date=15 September 2017 |archive-date=9 May 2019 |archive-url=https://web.archive.org/web/20190509044122/https://www.jpl.nasa.gov/news/news.php?feature=6948 |url-status=live }}</ref><ref name="NYT-20170914">{{cite news |last=Chang |first=Kenneth |title=Cassini Vanishes Into Saturn, Its Mission Celebrated and Mourned |url=https://www.nytimes.com/2017/09/14/science/cassini-grand-finale-saturn.html |date=14 September 2017 |work=[[The New York Times]] |access-date=15 September 2017 |archive-date=8 July 2018 |archive-url=https://web.archive.org/web/20180708162700/https://www.nytimes.com/2017/09/14/science/cassini-grand-finale-saturn.html |url-status=live }}</ref> The [[atmospheric entry]] of ''Cassini'' ended the mission. | ||
==== Possible future missions ==== | ==== Possible future missions ==== | ||
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== Observation == | == Observation == | ||
[[File:Saturn-27-03-04.jpeg|thumb| | [[File:Saturn-27-03-04.jpeg|thumb|An 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 (planet)|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. The mean [[apparent magnitude]] of Saturn is 0.46 with a standard deviation of 0.34.<ref name="Mallama_and_Hilton" /> Most of the magnitude variation is due to the inclination of the ring system relative to the Sun and Earth. The brightest magnitude, −0.55, occurs near the time when the plane of the rings is inclined most highly, and the faintest magnitude, 1.17, occurs around the time when they are least inclined.<ref name="Mallama_and_Hilton" /> | |||
{{wikinews|20-year-old astrophotographer captures rare solar eclipse on Saturn}}It takes approximately 29.4 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 a clear resolution is present.<ref name="NMM Saturn" /><ref name="binoculars" /> | |||
When Earth passes through the ring plane, which occurs twice every Saturnian year (roughly every 15 Earth years), the rings briefly disappear from view because they are so thin. Such a "disappearance" most recently occurred in 2025, but Saturn was too close to the Sun for observations.<ref>{{cite web |url=http://www.classicalastronomy.com/news/anmviewer.asp?a=313&z=28 |title=Saturn's Rings Edge-On |date=2013 |publisher=Classical Astronomy |archive-url=https://web.archive.org/web/20131105231722/http://www.classicalastronomy.com/news/anmviewer.asp?a=313&z=28 |archive-date=5 November 2013 |access-date=4 August 2013 }}</ref> | |||
Saturn and its rings are best seen when the planet is at, or near, [[opposition (astronomy)|opposition]], the configuration of a planet when it is at an [[Elongation (astronomy)|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. 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 next. Saturn also 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 the favorable [[:File:Saturnoppositions.jpg|orientation of its rings]] relative to the Earth,<ref name="opp2002">{{cite journal |title=Saturn in 2002–03 |last=Schmude |first=Richard W. Jr. |date=Winter 2003 |journal=Georgia Journal of Science |issn=0147-9369 |volume=61 |issue=4 |url=http://www.freepatentsonline.com/article/Georgia-Journal-Science/113429393.html |access-date=29 June 2015 |archive-date=24 September 2015 |archive-url=https://web.archive.org/web/20150924052153/http://www.freepatentsonline.com/article/Georgia-Journal-Science/113429393.html |url-status=live }}</ref> even though Saturn was closer to the Earth and Sun in late 2003.<ref name="opp2002" /> | Saturn and its rings are best seen when the planet is at, or near, [[opposition (astronomy)|opposition]], the configuration of a planet when it is at an [[Elongation (astronomy)|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. 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 next. Saturn also 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 the favorable [[:File:Saturnoppositions.jpg|orientation of its rings]] relative to the Earth,<ref name="opp2002">{{cite journal |title=Saturn in 2002–03 |last=Schmude |first=Richard W. Jr. |date=Winter 2003 |journal=Georgia Journal of Science |issn=0147-9369 |volume=61 |issue=4 |url=http://www.freepatentsonline.com/article/Georgia-Journal-Science/113429393.html |access-date=29 June 2015 |archive-date=24 September 2015 |archive-url=https://web.archive.org/web/20150924052153/http://www.freepatentsonline.com/article/Georgia-Journal-Science/113429393.html |url-status=live }}</ref> even though Saturn was closer to the Earth and Sun in late 2003.<ref name="opp2002" /> | ||
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==See also== | ==See also== | ||
* [[Moons of Saturn]] | |||
* [[List of gravitationally rounded objects of the Solar System#Planets|Statistics of planets in the Solar System]] | * [[List of gravitationally rounded objects of the Solar System#Planets|Statistics of planets in the Solar System]] | ||
* [[Outline of Saturn]] | * [[Outline of Saturn]] | ||
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| last1=Souami | first1=D. | last2=Souchay | first2=J. | | last1=Souami | first1=D. | last2=Souchay | first2=J. | ||
| journal=Astronomy & Astrophysics | | journal=Astronomy & Astrophysics | ||
| volume=543 | id=A133 | | | volume=543 | id=A133 | page=11 | date=July 2012 | ||
| doi=10.1051/0004-6361/201219011 | bibcode=2012A&A...543A.133S | doi-access=free }}</ref> | | doi=10.1051/0004-6361/201219011 | bibcode=2012A&A...543A.133S | doi-access=free }}</ref> | ||
<ref name="nasafact">{{cite web |url=http://solarsystem.nasa.gov/planets/profile.cfm?Object=Saturn&Display=Facts |title=NASA: Solar System Exploration: Planets: Saturn: Facts & Figures |publisher=Solarsystem.nasa.gov |date=22 March 2011 |access-date=8 August 2011 |archive-url=https://web.archive.org/web/20110902084432/http://solarsystem.nasa.gov/planets/profile.cfm?Object=Saturn&Display=Facts |archive-date=2 September 2011 | <ref name="nasafact">{{cite web |url=http://solarsystem.nasa.gov/planets/profile.cfm?Object=Saturn&Display=Facts |title=NASA: Solar System Exploration: Planets: Saturn: Facts & Figures |publisher=Solarsystem.nasa.gov |date=22 March 2011 |access-date=8 August 2011 |archive-url=https://web.archive.org/web/20110902084432/http://solarsystem.nasa.gov/planets/profile.cfm?Object=Saturn&Display=Facts |archive-date=2 September 2011 }}</ref> | ||
<ref name="fact">{{cite web |url=http://nssdc.gsfc.nasa.gov/planetary/factsheet/saturnfact.html |title=Saturn Fact Sheet |publisher=NASA |last=Williams |first=David R. |access-date=12 October 2017 |date=23 December 2016 |archive-url=https://web.archive.org/web/20170717071200/https://nssdc.gsfc.nasa.gov/planetary/factsheet/saturnfact.html |archive-date=17 July 2017 | <ref name="fact">{{cite web |url=http://nssdc.gsfc.nasa.gov/planetary/factsheet/saturnfact.html |title=Saturn Fact Sheet |publisher=NASA |last=Williams |first=David R. |access-date=12 October 2017 |date=23 December 2016 |archive-url=https://web.archive.org/web/20170717071200/https://nssdc.gsfc.nasa.gov/planetary/factsheet/saturnfact.html |archive-date=17 July 2017 }}</ref> | ||
<ref name=walter2003>{{cite book |first=Elizabeth |last=Walter |date=21 April 2003 |title=Cambridge Advanced Learner's Dictionary |publisher=Cambridge University Press |edition=Second |isbn=978-0-521-53106-1}}</ref> | <ref name=walter2003>{{cite book |first=Elizabeth |last=Walter |date=21 April 2003 |title=Cambridge Advanced Learner's Dictionary |publisher=Cambridge University Press |edition=Second |isbn=978-0-521-53106-1}}</ref> | ||
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<ref name=pa54_122>{{cite magazine |last1=Barton |first1=Samuel G. |title=The names of the satellites |magazine=Popular Astronomy |volume=54 |pages=122–130 |date=April 1946 |bibcode=1946PA.....54..122B}}</ref> | <ref name=pa54_122>{{cite magazine |last1=Barton |first1=Samuel G. |title=The names of the satellites |magazine=Popular Astronomy |volume=54 |pages=122–130 |date=April 1946 |bibcode=1946PA.....54..122B}}</ref> | ||
<ref name=binoculars>{{cite web |last=Eastman |first=Jack |url=http://www.thedas.org/dfiles/eastman_saturn.html |title=Saturn in Binoculars |date=1998 |publisher=The Denver Astronomical Society |access-date=3 September 2008 |archive-url=https://web.archive.org/web/20110728093200/http://www.thedas.org/dfiles/eastman_saturn.html |archive-date=28 July 2011 | <ref name=binoculars>{{cite web |last=Eastman |first=Jack |url=http://www.thedas.org/dfiles/eastman_saturn.html |title=Saturn in Binoculars |date=1998 |publisher=The Denver Astronomical Society |access-date=3 September 2008 |archive-url=https://web.archive.org/web/20110728093200/http://www.thedas.org/dfiles/eastman_saturn.html |archive-date=28 July 2011 }}</ref> | ||
<ref name=chan2000>{{cite web |url=http://library.thinkquest.org/C005921/Saturn/satuHist.htm |title=Saturn: History Timeline |access-date=16 July 2007 |date=2000 |last=Chan |first=Gary |archive-url=https://web.archive.org/web/20110716153718/http://library.thinkquest.org/C005921/Saturn/satuHist.htm |archive-date=16 July 2011 |url-status=live }}</ref> | <ref name=chan2000>{{cite web |url=http://library.thinkquest.org/C005921/Saturn/satuHist.htm |title=Saturn: History Timeline |access-date=16 July 2007 |date=2000 |last=Chan |first=Gary |archive-url=https://web.archive.org/web/20110716153718/http://library.thinkquest.org/C005921/Saturn/satuHist.htm |archive-date=16 July 2011 |url-status=live }}</ref> | ||
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<ref name=cain2008_46237>{{cite news |url=http://www.universetoday.com/46237/who-discovered-saturn/ |title=Who Discovered Saturn? |work=Universe Today |first1=Fraser |last1=Cain |date=27 November 2009 |access-date=17 September 2011 |archive-url=https://web.archive.org/web/20120718184312/http://www.universetoday.com/46237/who-discovered-saturn/ |archive-date=18 July 2012 |url-status=live }}</ref> | <ref name=cain2008_46237>{{cite news |url=http://www.universetoday.com/46237/who-discovered-saturn/ |title=Who Discovered Saturn? |work=Universe Today |first1=Fraser |last1=Cain |date=27 November 2009 |access-date=17 September 2011 |archive-url=https://web.archive.org/web/20120718184312/http://www.universetoday.com/46237/who-discovered-saturn/ |archive-date=18 July 2012 |url-status=live }}</ref> | ||
<ref name=micek2007>{{cite web |url=http://huygensgcms.gsfc.nasa.gov/Shistory.htm |title=Saturn: History of Discoveries |access-date=15 July 2007 |first1=Catherine |last1=Micek |archive-url=https://web.archive.org/web/20110723173328/http://huygensgcms.gsfc.nasa.gov/Shistory.htm |archive-date=23 July 2011 | <ref name=micek2007>{{cite web |url=http://huygensgcms.gsfc.nasa.gov/Shistory.htm |title=Saturn: History of Discoveries |access-date=15 July 2007 |first1=Catherine |last1=Micek |archive-url=https://web.archive.org/web/20110723173328/http://huygensgcms.gsfc.nasa.gov/Shistory.htm |archive-date=23 July 2011 }}</ref> | ||
<ref name=apj100_378>{{cite journal |last1=Kuiper |first1=Gerard P. |author-link=Gerard Kuiper |title=Titan: a Satellite with an Atmosphere |journal=Astrophysical Journal |volume=100 |pages=378–388 |date=November 1944 |doi=10.1086/144679 |bibcode=1944ApJ...100..378K}}</ref> | <ref name=apj100_378>{{cite journal |last1=Kuiper |first1=Gerard P. |author-link=Gerard Kuiper |title=Titan: a Satellite with an Atmosphere |journal=Astrophysical Journal |volume=100 |pages=378–388 |date=November 1944 |doi=10.1086/144679 |bibcode=1944ApJ...100..378K}}</ref> | ||
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<ref name=nature438_7069_758>{{cite journal |display-authors=1 |last1=Lebreton |first1=Jean-Pierre |last2=Witasse |first2=Olivier |last3=Sollazzo |first3=Claudio |last4=Blancquaert |first4=Thierry |last5=Couzin |first5=Patrice |last6=Schipper |first6=Anne-Marie |last7=Jones |first7=Jeremy B. |last8=Matson |first8=Dennis L. |last9=Gurvits |first9=Leonid I. |title=An overview of the descent and landing of the Huygens probe on Titan |journal=Nature |volume=438 |issue=7069 |pages=758–764 |date=December 2005 |doi=10.1038/nature04347 |bibcode=2005Natur.438..758L |pmid=16319826|s2cid=4355742 }}</ref> | <ref name=nature438_7069_758>{{cite journal |display-authors=1 |last1=Lebreton |first1=Jean-Pierre |last2=Witasse |first2=Olivier |last3=Sollazzo |first3=Claudio |last4=Blancquaert |first4=Thierry |last5=Couzin |first5=Patrice |last6=Schipper |first6=Anne-Marie |last7=Jones |first7=Jeremy B. |last8=Matson |first8=Dennis L. |last9=Gurvits |first9=Leonid I. |title=An overview of the descent and landing of the Huygens probe on Titan |journal=Nature |volume=438 |issue=7069 |pages=758–764 |date=December 2005 |doi=10.1038/nature04347 |bibcode=2005Natur.438..758L |pmid=16319826|s2cid=4355742 }}</ref> | ||
<ref name="Jones2008">{{cite journal |display-authors=1 |last1=Jones |first1=G. H. |last2=Roussos |first2=E. |last3=Krupp |first3=N. |last4=Beckmann |first4=U. |last5=Coates |first5=A. J. |last6=Crary |first6=F. |last7=Dandouras |first7=I. |last8=Dikarev |first8=V. |last9=Dougherty |first9=M. K. |title=The Dust Halo of Saturn's Largest Icy Moon, Rhea |journal=Science |volume=319 |issue=5868 |pages=1380–1384 |date=7 March 2008 |doi=10.1126/science.1151524 |pmid=18323452 |bibcode=2008Sci...319.1380J|s2cid=206509814 |url=https://pdfs.semanticscholar.org/0d74/d7801493544d2f60b90f17c64d89fcf8594e.pdf |archive-url=https://web.archive.org/web/20180308165130/https://pdfs.semanticscholar.org/0d74/d7801493544d2f60b90f17c64d89fcf8594e.pdf | <ref name="Jones2008">{{cite journal |display-authors=1 |last1=Jones |first1=G. H. |last2=Roussos |first2=E. |last3=Krupp |first3=N. |last4=Beckmann |first4=U. |last5=Coates |first5=A. J. |last6=Crary |first6=F. |last7=Dandouras |first7=I. |last8=Dikarev |first8=V. |last9=Dougherty |first9=M. K. |title=The Dust Halo of Saturn's Largest Icy Moon, Rhea |journal=Science |volume=319 |issue=5868 |pages=1380–1384 |date=7 March 2008 |doi=10.1126/science.1151524 |pmid=18323452 |bibcode=2008Sci...319.1380J|s2cid=206509814 |url=https://pdfs.semanticscholar.org/0d74/d7801493544d2f60b90f17c64d89fcf8594e.pdf |archive-url=https://web.archive.org/web/20180308165130/https://pdfs.semanticscholar.org/0d74/d7801493544d2f60b90f17c64d89fcf8594e.pdf |archive-date=8 March 2018 }}</ref> | ||
<ref name="Mass ref 3">{{cite news |first1=Fraser |last1=Cain |url=http://www.universetoday.com/15378/mass-of-saturn/ |title=Mass of Saturn |work=Universe Today |date=3 July 2008 |access-date=17 August 2011 |archive-date=26 September 2011 |archive-url=https://web.archive.org/web/20110926234258/http://www.universetoday.com/15378/mass-of-saturn/ |url-status=live }}</ref> | <ref name="Mass ref 3">{{cite news |first1=Fraser |last1=Cain |url=http://www.universetoday.com/15378/mass-of-saturn/ |title=Mass of Saturn |work=Universe Today |date=3 July 2008 |access-date=17 August 2011 |archive-date=26 September 2011 |archive-url=https://web.archive.org/web/20110926234258/http://www.universetoday.com/15378/mass-of-saturn/ |url-status=live }}</ref> | ||
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<ref name=atkinson2010>{{cite news |url=http://www.universetoday.com/81713/hot-plasma-explosions-inflate-saturns-magnetic-field/ |title=Hot Plasma Explosions Inflate Saturn's Magnetic Field |work=Universe Today |first1=Nancy |last1=Atkinson |date=14 December 2010 |access-date=24 August 2011 |archive-url=https://web.archive.org/web/20111101143836/http://www.universetoday.com/81713/hot-plasma-explosions-inflate-saturns-magnetic-field/ |archive-date=1 November 2011 |url-status=live }}</ref> | <ref name=atkinson2010>{{cite news |url=http://www.universetoday.com/81713/hot-plasma-explosions-inflate-saturns-magnetic-field/ |title=Hot Plasma Explosions Inflate Saturn's Magnetic Field |work=Universe Today |first1=Nancy |last1=Atkinson |date=14 December 2010 |access-date=24 August 2011 |archive-url=https://web.archive.org/web/20111101143836/http://www.universetoday.com/81713/hot-plasma-explosions-inflate-saturns-magnetic-field/ |archive-date=1 November 2011 |url-status=live }}</ref> | ||
<ref name=science316_5823_442>{{cite journal |display-authors=1 |last1=Gurnett |first1=D. A. |last2=Persoon |first2=A. M. |last3=Kurth |first3=W. S. |last4=Groene |first4=J. B. |last5=Averkamp |first5=T. F. |last6=Dougherty |first6=M. K. |last7=Southwood |first7=D. J. |title=The Variable Rotation Period of the Inner Region of Saturn's Plasma Disc |date=2007 |volume=316 |journal=[[Science (journal)|Science]] |pmid=17379775 |issue=5823 |pages=442–5 |bibcode=2007Sci...316..442G |doi=10.1126/science.1138562|s2cid=46011210 |url=https://pdfs.semanticscholar.org/50a8/0b218aefb851697d4916558fef1c61b03f0c.pdf |archive-url=https://web.archive.org/web/20200212013130/https://pdfs.semanticscholar.org/50a8/0b218aefb851697d4916558fef1c61b03f0c.pdf | <ref name=science316_5823_442>{{cite journal |display-authors=1 |last1=Gurnett |first1=D. A. |last2=Persoon |first2=A. M. |last3=Kurth |first3=W. S. |last4=Groene |first4=J. B. |last5=Averkamp |first5=T. F. |last6=Dougherty |first6=M. K. |last7=Southwood |first7=D. J. |title=The Variable Rotation Period of the Inner Region of Saturn's Plasma Disc |date=2007 |volume=316 |journal=[[Science (journal)|Science]] |pmid=17379775 |issue=5823 |pages=442–5 |bibcode=2007Sci...316..442G |doi=10.1126/science.1138562|s2cid=46011210 |url=https://pdfs.semanticscholar.org/50a8/0b218aefb851697d4916558fef1c61b03f0c.pdf |archive-url=https://web.archive.org/web/20200212013130/https://pdfs.semanticscholar.org/50a8/0b218aefb851697d4916558fef1c61b03f0c.pdf |archive-date=12 February 2020 }}</ref> | ||
<ref name=science316_5823_380>{{cite journal |last1=Bagenal |first1=F. |pmid=17446379 |title=A New Spin on Saturn's Rotation |journal=Science |volume=316 |issue=5823 |pages=380–1 |date=2007 |doi=10.1126/science.1142329|s2cid=118878929 }}</ref> | <ref name=science316_5823_380>{{cite journal |last1=Bagenal |first1=F. |pmid=17446379 |title=A New Spin on Saturn's Rotation |journal=Science |volume=316 |issue=5823 |pages=380–1 |date=2007 |doi=10.1126/science.1142329|s2cid=118878929 }}</ref> | ||
<ref name=Anderson2007>{{cite journal |journal=Science |title=Saturn's gravitational field, internal rotation and interior structure |volume=317 |pages=1384–1387 |date=2007 |doi=10.1126/science.1144835 |pmid=17823351 |first1=J. D. |last1=Anderson |first2=G. |last2=Schubert |issue=5843 |bibcode=2007Sci...317.1384A|s2cid=19579769 |url=http://pdfs.semanticscholar.org/98cf/84491154ff17b7a0596d5150f9029512d682.pdf |archive-url=https://web.archive.org/web/20200412141659/http://pdfs.semanticscholar.org/98cf/84491154ff17b7a0596d5150f9029512d682.pdf | <ref name=Anderson2007>{{cite journal |journal=Science |title=Saturn's gravitational field, internal rotation and interior structure |volume=317 |pages=1384–1387 |date=2007 |doi=10.1126/science.1144835 |pmid=17823351 |first1=J. D. |last1=Anderson |first2=G. |last2=Schubert |issue=5843 |bibcode=2007Sci...317.1384A|s2cid=19579769 |url=http://pdfs.semanticscholar.org/98cf/84491154ff17b7a0596d5150f9029512d682.pdf |archive-url=https://web.archive.org/web/20200412141659/http://pdfs.semanticscholar.org/98cf/84491154ff17b7a0596d5150f9029512d682.pdf |archive-date=12 April 2020 }}</ref> | ||
<ref name=russell2004>{{cite web |url=http://www.windows2universe.org/saturn/moons_and_rings.html |title=Saturn Moons and Rings |publisher=Windows to the Universe |first1=Randy |last1=Russell |date=7 June 2004 |access-date=19 July 2011 |archive-url=https://web.archive.org/web/20110904042359/http://www.windows2universe.org/saturn/moons_and_rings.html |archive-date=4 September 2011 |url-status=live }}</ref> | <ref name=russell2004>{{cite web |url=http://www.windows2universe.org/saturn/moons_and_rings.html |title=Saturn Moons and Rings |publisher=Windows to the Universe |first1=Randy |last1=Russell |date=7 June 2004 |access-date=19 July 2011 |archive-url=https://web.archive.org/web/20110904042359/http://www.windows2universe.org/saturn/moons_and_rings.html |archive-date=4 September 2011 |url-status=live }}</ref> | ||
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<ref name=faure_mensing2007>{{cite book |first1=Gunter |last1=Faure |first2=Teresa M. |last2=Mensing |title=Introduction to planetary science: the geological perspective |publisher=Springer |date=2007 |isbn=978-1-4020-5233-0 |page=337 |url=https://books.google.com/books?id=U4FZp6f6q6MC&pg=PA337 |access-date=9 February 2016 |archive-date=16 February 2017 |archive-url=https://web.archive.org/web/20170216225727/https://books.google.com/books?id=U4FZp6f6q6MC&pg=PA337 |url-status=live }}</ref> | <ref name=faure_mensing2007>{{cite book |first1=Gunter |last1=Faure |first2=Teresa M. |last2=Mensing |title=Introduction to planetary science: the geological perspective |publisher=Springer |date=2007 |isbn=978-1-4020-5233-0 |page=337 |url=https://books.google.com/books?id=U4FZp6f6q6MC&pg=PA337 |access-date=9 February 2016 |archive-date=16 February 2017 |archive-url=https://web.archive.org/web/20170216225727/https://books.google.com/books?id=U4FZp6f6q6MC&pg=PA337 |url-status=live }}</ref> | ||
<ref name=nasa_saturn>{{cite web |url=http://www.nasa.gov/worldbook/saturn_worldbook.html |title=NASA – Saturn |publisher=NASA |access-date=27 July 2007 |date=2004 |archive-url=https://web.archive.org/web/20101229031643/http://www.nasa.gov/worldbook/saturn_worldbook.html |archive-date=29 December 2010 | <ref name=nasa_saturn>{{cite web |url=http://www.nasa.gov/worldbook/saturn_worldbook.html |title=NASA – Saturn |publisher=NASA |access-date=27 July 2007 |date=2004 |archive-url=https://web.archive.org/web/20101229031643/http://www.nasa.gov/worldbook/saturn_worldbook.html |archive-date=29 December 2010 }}</ref> | ||
<ref name=de_pater_lissauer2010>{{cite book |first1=Imke |last1=de Pater |first2=Jack J. |last2=Lissauer |title=Planetary Sciences |edition=2nd |publisher=Cambridge University Press |date=2010 |isbn=978-0-521-85371-2 |pages=254–255 |url=https://books.google.com/books?id=a_ijoTgDhnEC&pg=PA254 |access-date=9 February 2016 |archive-date=17 February 2017 |archive-url=https://web.archive.org/web/20170217000421/https://books.google.com/books?id=a_ijoTgDhnEC&pg=PA254 |url-status=live }}</ref> | <ref name=de_pater_lissauer2010>{{cite book |first1=Imke |last1=de Pater |first2=Jack J. |last2=Lissauer |title=Planetary Sciences |edition=2nd |publisher=Cambridge University Press |date=2010 |isbn=978-0-521-85371-2 |pages=254–255 |url=https://books.google.com/books?id=a_ijoTgDhnEC&pg=PA254 |access-date=9 February 2016 |archive-date=17 February 2017 |archive-url=https://web.archive.org/web/20170217000421/https://books.google.com/books?id=a_ijoTgDhnEC&pg=PA254 |url-status=live }}</ref> | ||
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<ref name=dougherty_esposito2009>{{Cite book |publisher=Springer |date=2009 |isbn=978-1-4020-9216-9 |page=162 |url=https://books.google.com/books?id=M56CHHxVMP4C&pg=PA162 |bibcode=2009sfch.book.....D |doi=10.1007/978-1-4020-9217-6 |editor1-last=Dougherty |editor1-first=Michele K. |editor2-last=Esposito |editor2-first=Larry W. |editor3-last=Krimigis |editor3-first=Stamatios M. |last1=Dougherty |first1=Michele K. |last2=Esposito |first2=Larry W. |last3=Krimigis |first3=Stamatios M. |title=Saturn from Cassini-Huygens |access-date=9 February 2016 |archive-date=16 April 2017 |archive-url=https://web.archive.org/web/20170416202411/https://books.google.com/books?id=M56CHHxVMP4C&pg=PA162 |url-status=live }}</ref> | <ref name=dougherty_esposito2009>{{Cite book |publisher=Springer |date=2009 |isbn=978-1-4020-9216-9 |page=162 |url=https://books.google.com/books?id=M56CHHxVMP4C&pg=PA162 |bibcode=2009sfch.book.....D |doi=10.1007/978-1-4020-9217-6 |editor1-last=Dougherty |editor1-first=Michele K. |editor2-last=Esposito |editor2-first=Larry W. |editor3-last=Krimigis |editor3-first=Stamatios M. |last1=Dougherty |first1=Michele K. |last2=Esposito |first2=Larry W. |last3=Krimigis |first3=Stamatios M. |title=Saturn from Cassini-Huygens |access-date=9 February 2016 |archive-date=16 April 2017 |archive-url=https://web.archive.org/web/20170416202411/https://books.google.com/books?id=M56CHHxVMP4C&pg=PA162 |url-status=live }}</ref> | ||
<ref name="Jupiter fact">{{Cite web |url=http://nssdc.gsfc.nasa.gov/planetary/factsheet/jupiterfact.html |title=Jupiter Fact Sheet |publisher=NASA |last=Williams |first=David R. |date=16 November 2004 |access-date=2 August 2007 |archive-url=https://web.archive.org/web/20110926211234/http://nssdc.gsfc.nasa.gov/planetary/factsheet/jupiterfact.html |archive-date=26 September 2011 | <ref name="Jupiter fact">{{Cite web |url=http://nssdc.gsfc.nasa.gov/planetary/factsheet/jupiterfact.html |title=Jupiter Fact Sheet |publisher=NASA |last=Williams |first=David R. |date=16 November 2004 |access-date=2 August 2007 |archive-url=https://web.archive.org/web/20110926211234/http://nssdc.gsfc.nasa.gov/planetary/factsheet/jupiterfact.html |archive-date=26 September 2011 }}</ref> | ||
<ref name=preserve>{{Cite web |url=http://www.preservearticles.com/201101233659/saturn-the-most-beautiful-planet-of-our-solar-system.html |title=Saturn – The Most Beautiful Planet of our solar system |work=Preserve Articles |date=23 January 2011 |access-date=24 July 2011 |archive-url=https://web.archive.org/web/20120120134152/http://www.preservearticles.com/201101233659/saturn-the-most-beautiful-planet-of-our-solar-system.html |archive-date=20 January 2012 |url-status=live }}</ref> | <ref name=preserve>{{Cite web |url=http://www.preservearticles.com/201101233659/saturn-the-most-beautiful-planet-of-our-solar-system.html |title=Saturn – The Most Beautiful Planet of our solar system |work=Preserve Articles |date=23 January 2011 |access-date=24 July 2011 |archive-url=https://web.archive.org/web/20120120134152/http://www.preservearticles.com/201101233659/saturn-the-most-beautiful-planet-of-our-solar-system.html |archive-date=20 January 2012 |url-status=live }}</ref> | ||
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== Further reading == | == Further reading == | ||
* {{cite book |last=Alexander |first=Arthur Francis O'Donel |author-link=Arthur Francis O'Donel Alexander |title=The Planet Saturn – A History of Observation, Theory and Discovery |publisher=Dover |date=1980 |orig- | * {{cite book |last=Alexander |first=Arthur Francis O'Donel |author-link=Arthur Francis O'Donel Alexander |title=The Planet Saturn – A History of Observation, Theory and Discovery |publisher=Dover |date=1980 |orig-date=1962 |isbn=978-0-486-23927-9}} | ||
* {{cite magazine |last=Gore |first=Rick |title=Voyager 1 at Saturn: Riddles of the Rings |magazine=[[National Geographic]] |volume=160 |issue=1 |pages=3–31 |date=July 1981 |issn=0027-9358 |oclc=643483454}} | * {{cite magazine |last=Gore |first=Rick |title=Voyager 1 at Saturn: Riddles of the Rings |magazine=[[National Geographic]] |volume=160 |issue=1 |pages=3–31 |date=July 1981 |issn=0027-9358 |oclc=643483454}} | ||
* {{cite book |last1=Lovett |first1=L. |last2=Horvath |first2=J. |last3=Cuzzi |first3=J. |display-authors=1 |title=Saturn: A New View |publisher=Harry N. Abrams |date=2006 |isbn=978-0-8109-3090-2}} | * {{cite book |last1=Lovett |first1=L. |last2=Horvath |first2=J. |last3=Cuzzi |first3=J. |display-authors=1 |title=Saturn: A New View |publisher=Harry N. Abrams |date=2006 |isbn=978-0-8109-3090-2}} | ||
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{{Spoken Wikipedia|Saturn.ogg|date=18 August 2013}} | {{Spoken Wikipedia|Saturn.ogg|date=18 August 2013}} | ||
* [https://solarsystem.nasa.gov/planets/saturn/overview/ Saturn overview] by NASA's [[Science Mission Directorate]] | * [https://solarsystem.nasa.gov/planets/saturn/overview/ Saturn overview] by NASA's [[Science Mission Directorate]] | ||
* [https://nssdc.gsfc.nasa.gov/planetary/factsheet/saturnfact.html Saturn fact sheet] at the [[NASA Space Science Data Coordinated Archive]] | * [https://nssdc.gsfc.nasa.gov/planetary/factsheet/saturnfact.html Saturn fact sheet] {{Webarchive|url=https://web.archive.org/web/20180529214002/https://nssdc.gsfc.nasa.gov/planetary/factsheet/saturnfact.html |date=29 May 2018 }} at the [[NASA Space Science Data Coordinated Archive]] | ||
* [https://web.archive.org/web/20180219090345/https://planetarynames.wr.usgs.gov/Page/SATURN/system Saturnian System terminology] by the IAU Gazetteer of Planetary Nomenclature | * [https://web.archive.org/web/20180219090345/https://planetarynames.wr.usgs.gov/Page/SATURN/system Saturnian System terminology] by the IAU Gazetteer of Planetary Nomenclature | ||
* [https://web.archive.org/web/20020330192909/http://saturn.jpl.nasa.gov/ ''Cassini-Huygens'' legacy website] by the [[Jet Propulsion Laboratory]] | * [https://web.archive.org/web/20020330192909/http://saturn.jpl.nasa.gov/ ''Cassini-Huygens'' legacy website] by the [[Jet Propulsion Laboratory]] | ||
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{{Solar System}} | {{Solar System}} | ||
{{Atmospheres}} | {{Atmospheres}} | ||
{{Authority control}} | |||
{{Portal bar|Stars|Spaceflight|Outer space}} | {{Portal bar|Stars|Spaceflight|Outer space}} | ||
[[Category:Saturn| ]] | [[Category:Saturn| ]] | ||
[[Category:Astronomical objects known since antiquity]] | [[Category:Astronomical objects known since antiquity]] | ||
Latest revision as of 09:09, 23 October 2025
Template:Short description Script error: No such module "about". Script error: No such module "redirect hatnote". Template:Main other Template:Pp-semi-indef Template:Pp-move Template:Use American English Template:Use dmy dates Script error: No such module "infobox".Script error: No such module "Check for unknown parameters". 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 of about 9 times that of Earth. It has an eighth of the average density of Earth, but is over 95 times more massive. Even though Saturn is almost as big as Jupiter, Saturn has less than a third of its mass. Saturn orbits the Sun at a distance of Template:Convert, with an orbital period of 29.45 years.
Saturn's interior is thought to be composed of a rocky core, surrounded by a deep layer of metallic hydrogen, an intermediate layer of liquid hydrogen and liquid helium, and an outer layer of gas. Saturn has a pale yellow hue, due to ammonia crystals in its upper atmosphere. An electrical current in 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 because of Saturn's greater size. Saturn's magnetic field strength is about a twentieth that of Jupiter.[1] The outer atmosphere is generally bland and lacking in contrast, although long-lived features can appear. Wind speeds on Saturn can reach Template:Convert.
The planet has a bright and extensive system of rings, composed mainly of ice particles, with a smaller amount of rocky debris and dust. At least 274 moons orbit the planet, of which 63 are officially named; these do not include the hundreds of moonlets in the rings. Titan, Saturn's largest moon and the second largest in the Solar System, is larger (but less massive) than the planet Mercury and is the only moon in the Solar System that has a substantial atmosphere.[2]
Name and symbol
Saturn is named after the Roman god of wealth and agriculture, who was the father of the god Jupiter. Its astronomical symbol (♄) has been traced back to the Greek Oxyrhynchus Papyri, where it can be seen to be a Greek kappa-rho ligature with a horizontal stroke, as an abbreviation for Κρονος (Cronus), the Greek name for the planet (File:Saturn symbol (late classical and medieval mss).png).[3] It later came to look like a lower-case Greek eta, with the cross added at the top in the 16th century to Christianize this pagan symbol.
The Romans named the seventh day of the week Saturday, Sāturni diēs, "Saturn's Day", for the planet Saturn.[4]
Physical characteristics
Saturn is a gas giant, composed predominantly of hydrogen and helium. It lacks a definite surface, though it is likely to have a solid core.[5] The planet's rotation makes it an oblate spheroid—a ball flattened at the poles and bulging at the equator. Its equatorial radius is more than 10% larger than the polar radius: 60,268 km versus 54,364 km (37,449 mi versus 33,780 mi).[6]
Jupiter, Uranus, and Neptune, the other giant planets in the Solar System, are less oblate. The combination of the bulge and the rotation rate means that the effective surface gravity along the equator, Template:Val, is 74% of what it is at the poles and is lower than the surface gravity of Earth. However, the equatorial escape velocity, nearly Template:Val, is much higher than that of Earth.[7]
Saturn is the only planet of the Solar System that is less dense than water—about 30% less.[8] Although Saturn's core is considerably denser than water, the average specific density of the planet is Template:Val, because of the atmosphere. Jupiter has 318 times Earth's mass,[9] and Saturn is 95 times Earth's mass.[6][10][11][12][13][14] Together, Jupiter and Saturn hold 92% of the total planetary mass in the Solar System.[15]
Internal structure
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 Template:Val, 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 be a metal in the deeper layers.[15]
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.[16] Analysis of the distortion shows that Saturn is substantially more centrally condensed than Jupiter and therefore contains much more material denser than hydrogen near its center. Saturn's central regions are about 50% hydrogen by mass, and Jupiter's are about 67% hydrogen.[17]
This core is similar in composition to Earth, but is more dense. The examination of Saturn's gravitational moment, in combination with physical models of the interior, has allowed constraints to be placed on the mass of Saturn's core. In 2004, scientists estimated that the core must be 9–22 times the mass of Earth,[18][19] which corresponds to a diameter of about Template:Convert.[20] Measurements of Saturn's rings suggest a much more diffuse core, with a mass equal to about 17 Earths and a radius equal to about 60% of Saturn's entire radius.[21] This is surrounded by a thicker, liquid metallic hydrogen layer, followed by a liquid layer of helium-saturated molecular hydrogen, which gradually transitions to a gas as altitude increases. The outermost layer spans about Template:Convert and consists of gas.[22][23][24]
Saturn has a hot interior, reaching Template:Convert at its core, and 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 such a process alone may not be sufficient to explain heat production for Saturn, because it is less massive. An alternative or additional mechanism may be the 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.[25][26] These descending droplets may have accumulated into a helium shell surrounding the core.[16] Rainfalls of diamonds have been suggested to occur within Saturn, as well as in Jupiter[27] and ice giants Uranus and Neptune.[28]
Atmosphere
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.[16] The quantity of elements heavier than helium (metallicity) 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 Earth, with a significant fraction located in Saturn's core region.[29]
Trace amounts of ammonia, acetylene, ethane, propane, phosphine, and methane have been detected in Saturn's atmosphere.[30][31][32] The upper clouds are composed of ammonia crystals, while the lower level clouds appear to consist of either ammonium hydrosulfide (Template:Chem2) or water.[33] 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.[32] Cassini observed a series of cloud features found in northern latitudes, nicknamed the "String of Pearls". These features are cloud clearings that reside in deeper cloud layers.[34]
Cloud layers
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.[35]
The composition of the clouds varies with depth and increasing pressure. In the upper cloud layers, with temperatures in the range of 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 to 270 K. Intermixed in this layer is a band of ammonium hydrosulfide ice, lying in the pressure range 3–6 bar with temperatures of 190–235 K. The lower layers, where pressures are between 10 and 20 bar and temperatures are 270–330 K, contains a region of water droplets with ammonia in aqueous solution.[36]
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 short-lived phenomenon that occurs once every Saturnian year, roughly every 30 Earth years, around the time of the northern hemisphere's summer solstice.[37]
Previous Great White Spots were observed in 1876, 1903, 1933, and 1960, with the 1933 storm being the best observed.[38] The latest giant storm was observed in 2010. In 2015, researchers used Very Large Array telescope to study Saturnian atmosphere, and reported that they found "long-lasting signatures of all mid-latitude giant storms, a mixture of equatorial storms up to hundreds of years old, and potentially an unreported older storm at 70°N".[39]
The winds on Saturn are the second fastest among the Solar System's planets, after Neptune's. Voyager data indicate peak easterly winds of Template:Convert.[40] 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.[41] 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.[42] 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.[42]
Hexagonal cloud patterns
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Script error: No such module "anchor".A persisting hexagonal wave pattern around the north polar vortex in the atmosphere at about 78°N was first noted in the Voyager images.[43][44][45] The sides of the hexagon are each about Template:Convert long, which is longer than the diameter of the Earth.[46] The entire structure rotates with a period of Template:RA (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.[47] The hexagonal feature does not shift in longitude like the other clouds in the visible atmosphere.[48] 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.[49][50]
HST imaging of the south polar region indicates the presence of a jet stream, but no strong polar vortex nor any hexagonal standing wave.[51] NASA reported in November 2006 that Cassini had observed a "hurricane-like" storm locked to the south pole that had a clearly defined eyewall.[52][53] 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.[54]
The south pole storm may have been present for billions of years.[55] This vortex is comparable to the size of Earth, and it has winds of 550 km/h.[55]
Magnetosphere
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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.[1] As a result, Saturn's magnetosphere is much smaller than Jupiter's.[56]
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 (684,000 mi),[57] although it enlarged within several hours, and remained so for about three days.[58] 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.[56] 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.[1] Saturn's magnetosphere, like Earth's, produces aurorae.[59]
Orbit and rotation
The average distance between Saturn and the Sun is over 1.4 billion kilometers (9 AU). With an average orbital speed of 9.68 km/s,[6] it takes Saturn 10,759 Earth days (or about <templatestyles src="Fraction/styles.css" />29+1⁄2 years)[60] to finish one revolution around the Sun.[6] As a consequence, it forms a near 5:2 mean-motion resonance with Jupiter.[61] The elliptical orbit of Saturn is inclined 2.48° relative to the orbital plane of the Earth.[6] The perihelion and aphelion distances are, respectively, 9.195 and 9.957 AU, on average.[6][62] 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 Template:RA (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 Template:RA (810.76°/d). System III refers to Saturn's internal rotation rate. Based on radio emissions from the planet detected by Voyager 1 and Voyager 2,[63] System III has a rotation period of Template:RA (810.8°/d). System III has largely superseded System II.[64]
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 Template:RA Template:+-.[65][66] An 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 is Template:RA.[67] Studies of the planet's C Ring yield a rotation period of Template:RA Template:+- .[68][69]
In March 2007, it was found that the variation in 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.[70][71][72]
Saturn only has one known trojan asteroid, designated Template:Mpl, whose trojan configuration was announced in September 2024, orbiting the Sun at the stable L4 Lagrange point 60° ahead of the planet along its orbit.[73] This discovery leaves only Mercury without any known trojans at all. Orbital resonance mechanisms, including secular resonance, are believed to be the cause of the low number of known Saturnian trojans.[74]
Natural satellites
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Saturn has 274 known moons,[75][76][77][78] 63 of which have formal names.[79][80] There is evidence of dozens to hundreds of moonlets with diameters of 40–500 meters in Saturn's rings,[81] 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.[82] Saturn's second-largest moon, Rhea, may have a tenuous ring system of its own,[83] along with a tenuous atmosphere.[84][85][86]
Many of the other moons are small: 131 are less than 50 km in diameter.[87] 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,[88][89] in which a complex organic chemistry occurs. It is the only satellite with hydrocarbon lakes.[90][91]
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.[92] 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.[93]
Saturn's moon Enceladus, which seems similar in chemical makeup to comets,[94] has often been regarded as a potential habitat for microbial life.[95][96][97][98] 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.[99][100][101] A 2015 flyby by Cassini through a plume on Enceladus found most of the ingredients to sustain life forms that live by methanogenesis.[102]
In April 2014, NASA scientists reported the possible beginning of a new moon within the A Ring, which was imaged by Cassini on 15 April 2013.[103]
Planetary rings
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Saturn is probably best known for the system of planetary rings that makes it visually unique.[23] The rings extend from Template:Convert outward from Saturn's equator and average approximately Template:Convert in thickness. They are composed predominantly of water ice, with trace amounts of tholin impurities and a peppered coating of approximately 7% amorphous carbon.[104] The particles that make up the rings range in size from specks of dust up to 10 m.[105] While the other gas giants also have ring systems, Saturn's is the largest and most visible.
There is a debate on the age of the rings. One side supports that they are ancient, and were created simultaneously with Saturn from the original nebular material (around 4.6 billion years ago),[106] or shortly after the LHB (around 4.1 to 3.8 billion years ago).[107][108] The other side supports that they are much younger, created around 100 million years ago.[109][110][111] An MIT research team, supporting the latter theory, proposed that the rings are remnant of a destroyed moon of Saturn, named ″Chrysalis″.[112]
Beyond the main rings, at a distance of 12 million km (7.5 million mi) from the planet is the sparse Phoebe ring. It is tilted at an angle of 27° to the other rings and, like Phoebe, orbits in retrograde fashion.[113]
Some of the moons of Saturn, including Pandora and Prometheus, act as shepherd moons to confine the rings and prevent them from spreading out.[114] Pan and Atlas cause weak, linear density waves in Saturn's rings that have yielded more reliable calculations of their masses.[115]
History of observation and exploration
The observation and exploration of Saturn can be divided into three phases: (1) pre-modern observations with the naked eye, (2) telescopic observations from Earth beginning in the 17th century, and (3) visitation by space probes, in orbit or on flyby. In the 21st century, telescopic observations continue from Earth (including Earth-orbiting observatories like the Hubble Space Telescope) and, until its 2017 retirement, from the Cassini orbiter around Saturn.
Pre-telescopic observation
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Saturn has been known since prehistoric times,[116] and in early recorded history it was a major character in various mythologies. Babylonian astronomers systematically observed and recorded the movements of Saturn.[117] In ancient Greek, the planet was known as Script error: No such module "Lang". Phainon,[118] and in Roman times it was known as the "star of Saturn" or the "star of the Sun (i.e. Helios)".[119][120] In ancient Roman mythology, the planet Phainon was sacred to this agricultural god, from which the planet takes its modern name.[121] The Romans considered the god Saturnus the equivalent of the Greek god Cronus. In modern Greek, the planet retains the name Cronus—Template:Langx: Kronos.[122]
The Greek scientist Ptolemy based his calculations of Saturn's orbit on observations he made while it was in opposition.[123] In Hindu astrology, there are nine astrological objects, known as Navagrahas. Saturn is known as "Shani" and judges everyone based on the good and bad deeds performed in life.[121][123] Ancient Chinese and Japanese culture designated the planet Saturn as the "earth star" or "soil star" (Script error: No such module "Lang".). This was based on Five Elements which were traditionally used to classify natural elements.[124][125][126]
In Hebrew, Saturn is called Shabbathai.[127] Its angel is Cassiel. Its intelligence or beneficial spirit is 'Agȋȇl (Template:Langx),[128] and its darker spirit (demon) is Zȃzȇl (Template:Langx).[128][129][130] Zazel has been described as a great angel, invoked in Solomonic magic, who is "effective in love conjurations".[131][132] In Ottoman Turkish, Urdu, and Malay, the name of Zazel is 'Zuhal', derived from the Arabic language (Template:Langx).[129]
Telescopic pre-spaceflight observations
Saturn's rings require at least a 15-mm-diameter telescope[133] to resolve and were not known to exist until Christiaan Huygens saw them in 1655 and published his observations in 1659. Galileo, with his primitive telescope in 1610,[134][135] incorrectly thought of Saturn's appearing not quite round as two moons on Saturn's sides.[136][137]
When Huygens used greater telescopic magnification this notion was refuted, and the rings were truly seen for the first time. 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.[138]
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.[139]
In 1899, William Henry Pickering discovered Phoebe, a highly irregular satellite that does not rotate synchronously with Saturn as the larger moons do.[139] Phoebe was the first such satellite found and it took 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.[140]
Spaceflight missions
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Pioneer 11 flyby
Pioneer 11 made the first flyby of Saturn in September 1979, when it passed within Template:Convert 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 a high phase angle (towards the Sun), meaning that they contain fine light-scattering material. In addition, Pioneer 11 measured the temperature of Titan.[141]
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 at visible wavelengths; therefore no surface details were seen. The flyby changed the spacecraft's trajectory out of the plane of the Solar System.[142]
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. 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.[142]
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).[143]
Cassini–Huygens spacecraft
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The Cassini–Huygens space probe entered orbit around Saturn on 1 July 2004. In June 2004, it conducted a close flyby of Phoebe, sending back high-resolution images and data. CassiniTemplate:'s flyby of Saturn's largest moon, Titan, 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.[145]
Starting in early 2005, scientists used Cassini to track lightning on Saturn. The power of the lightning is approximately 1,000 times that of lightning on Earth.[146]
In 2006, NASA reported that Cassini had found evidence of liquid water reservoirs no more than tens of meters below the surface that erupt in geysers on Saturn's moon Enceladus. These jets of icy particles are emitted into orbit around Saturn from vents in the moon's south polar region.[147] Over 100 geysers have been identified on Enceladus.[144] In May 2011, NASA scientists reported that Enceladus "is emerging as the most habitable spot beyond Earth in the Solar System for life as we know it".[148][149]
Cassini photographs 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.[150] In July 2006, images were returned of hydrocarbon lakes near Titan's north pole, the presence of which were confirmed in January 2007. In March 2007, hydrocarbon seas were found near the North pole, the largest of which is almost the size of the Caspian Sea.[151] In October 2006, the probe detected an Template:Convert diameter cyclone-like storm with an eyewall at Saturn's south pole.[152]
From 2004 to 2 November 2009, the probe discovered and confirmed eight new satellites.[153] 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 Template:Convert.[154] On 15 September 2017, the Cassini–Huygens spacecraft performed the "Grand Finale" of its mission: a number of passes through gaps between Saturn and Saturn's inner rings.[155][156] The atmospheric entry of Cassini ended the mission.
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 the Saturn Atmospheric Entry Probe, and possible investigations into the habitability and possible discovery of life on Saturn's moons Titan and Enceladus by Dragonfly.[157][158]
Observation
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. The mean apparent magnitude of Saturn is 0.46 with a standard deviation of 0.34.[159] Most of the magnitude variation is due to the inclination of the ring system relative to the Sun and Earth. The brightest magnitude, −0.55, occurs near the time when the plane of the rings is inclined most highly, and the faintest magnitude, 1.17, occurs around the time when they are least inclined.[159]
Template:Sister projectIt takes approximately 29.4 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 a clear resolution is present.[23][133]
When Earth passes through the ring plane, which occurs twice every Saturnian year (roughly every 15 Earth years), the rings briefly disappear from view because they are so thin. Such a "disappearance" most recently occurred in 2025, but Saturn was too close to the Sun for observations.[160]
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. 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 next. Saturn also 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 the favorable orientation of its rings relative to the Earth,[161] even though Saturn was closer to the Earth and Sun in late 2003.[161]
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 monthly for about a 12-month period, followed by about a five-year period in which no such activity is registered. The Moon's orbit is inclined by several degrees relative to Saturn's, so occultations will only occur when Saturn is near one of the points in the sky where the two planes intersect (both the length of Saturn's year and the 18.6-Earth-year nodal precession period of the Moon's orbit influence the periodicity).[162]
In fiction
Script error: No such module "Labelled list hatnote". Saturn has frequently appeared in fiction since at least 1752, when Voltaire published his novel Micromégas.[163] Early works generally depicted it as solid,[164] whereas Saturn is later correctly described as a gaseous planet. Saturn's moons are also featured in fiction, especially Titan.[165]
See also
Notes
References
Further reading
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External links
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- Saturn overview by NASA's Science Mission Directorate
- Saturn fact sheet Template:Webarchive at the NASA Space Science Data Coordinated Archive
- Saturnian System terminology by the IAU Gazetteer of Planetary Nomenclature
- Cassini-Huygens legacy website by the Jet Propulsion Laboratory
- Interactive 3D gravity simulation of the Cronian system Template:Webarchive
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<ref>tag; no text was provided for refs namedmartinez20050905 - ↑ Script error: No such module "citation/CS1".
- ↑ Cite error: Invalid
<ref>tag; no text was provided for refs namedemp105_2_143 - ↑ Cite error: Invalid
<ref>tag; no text was provided for refs nameddougherty_esposito2009 - ↑ Cite error: Invalid
<ref>tag; no text was provided for refs namedicarus176_1_155 - ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "Citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ a b Script error: No such module "citation/CS1".
- ↑ Script error: No such module "Citation/CS1".
- ↑ Script error: No such module "Citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Cite error: Invalid
<ref>tag; no text was provided for refs namedscience247_4947_1206 - ↑ Cite error: Invalid
<ref>tag; no text was provided for refs namedpss57_14_1671 - ↑ Script error: No such module "Citation/CS1". Bizarre geometric shapes that appear at the center of swirling vortices in planetary atmospheres might be explained by a simple experiment with a bucket of water but correlating this to Saturn's pattern is by no means certain.
- ↑ Script error: No such module "Citation/CS1". Laboratory experiment of spinning disks in a liquid solution forms vortices around a stable hexagonal pattern similar to that of Saturn's.
- ↑ Script error: No such module "Citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ a b Template:Cite APOD
- ↑ a b Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Cite error: Invalid
<ref>tag; no text was provided for refs namedatkinson2010 - ↑ Script error: No such module "citation/CS1".
- ↑ Cite error: Invalid
<ref>tag; no text was provided for refs namedcain2009 - ↑ Script error: No such module "Citation/CS1".
- ↑ Jean Meeus, Astronomical Algorithms (Richmond, VA: Willmann-Bell, 1998). Average of the nine extremes on p 273. All are within 0.02 AU of the averages.
- ↑ Script error: No such module "Citation/CS1".
- ↑ Cite error: Invalid
<ref>tag; no text was provided for refs namedbenton2006 - ↑ Script error: No such module "citation/CS1".
- ↑ Cite error: Invalid
<ref>tag; no text was provided for refs namedcain2008_15298 - ↑ Cite error: Invalid
<ref>tag; no text was provided for refs namedAnderson2007 - ↑ Cite error: Invalid
<ref>tag; no text was provided for refs namedNASA-20190118 - ↑ Cite error: Invalid
<ref>tag; no text was provided for refs namedAPJ-20190117 - ↑ Script error: No such module "citation/CS1".
- ↑ Cite error: Invalid
<ref>tag; no text was provided for refs namedscience316_5823_442 - ↑ Cite error: Invalid
<ref>tag; no text was provided for refs namedscience316_5823_380 - ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "Citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "Citation/CS1".
- ↑ Cite error: Invalid
<ref>tag; no text was provided for refs namedbrunier2005 - ↑ Cite error: Invalid
<ref>tag; no text was provided for refs namedJones2008 - ↑ Cite error: Invalid
<ref>tag; no text was provided for refs namedatkinson20101126 - ↑ Script error: No such module "citation/CS1".
- ↑ Cite error: Invalid
<ref>tag; no text was provided for refs namedryan20101126 - ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Cite error: Invalid
<ref>tag; no text was provided for refs namedmadrigal20090624 - ↑ Cite error: Invalid
<ref>tag; no text was provided for refs namedspotts20050928 - ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "Citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "Citation/CS1".
- ↑ Script error: No such module "Citation/CS1".
- ↑ Script error: No such module "Citation/CS1".
- ↑ Script error: No such module "Citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "Citation/CS1".
- ↑ Script error: No such module "Citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Cite error: Invalid
<ref>tag; no text was provided for refs namedrussell2004 - ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Cite error: Invalid
<ref>tag; no text was provided for refs namedptrsl276_1257_43 - ↑ Template:LSJ.
- ↑ Cicero, De Natura Deorum.
- ↑ Script error: No such module "Citation/CS1".
- ↑ a b Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1". See also the Greek article about the planet.
- ↑ a b Cite error: Invalid
<ref>tag; no text was provided for refs namedps04_1893_862 - ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ a b Script error: No such module "citation/CS1".
- ↑ a b Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ a b Cite error: Invalid
<ref>tag; no text was provided for refs namedbinoculars - ↑ Cite error: Invalid
<ref>tag; no text was provided for refs namedchan2000 - ↑ Cite error: Invalid
<ref>tag; no text was provided for refs namedcain2008_15390 - ↑ Cite error: Invalid
<ref>tag; no text was provided for refs namedcain2008_15418 - ↑ Cite error: Invalid
<ref>tag; no text was provided for refs namedcain2008_46237 - ↑ Cite error: Invalid
<ref>tag; no text was provided for refs namedmicek2007 - ↑ a b Cite error: Invalid
<ref>tag; no text was provided for refs namedpa54_122 - ↑ Cite error: Invalid
<ref>tag; no text was provided for refs namedapj100_378 - ↑ Script error: No such module "citation/CS1".
- ↑ a b Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ a b Script error: No such module "citation/CS1".
- ↑ Cite error: Invalid
<ref>tag; no text was provided for refs namednature438_7069_758 - ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "Citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ a b Cite error: Invalid
<ref>tag; no text was provided for refs namedMallama_and_Hilton - ↑ Script error: No such module "citation/CS1".
- ↑ a b Script error: No such module "Citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "citation/CS1".