Saturn: Difference between revisions
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{{about|the planet||Saturn (disambiguation)}} |
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{{Infobox |
{{Infobox planet |
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| name = Saturn |
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| bgcolour = #FFCC66 |
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| symbol = [[File:Saturn symbol (bold).svg|24px|♄]] |
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| name = Saturn |
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| image = [[File:Saturn during Equinox.jpg|300px]] |
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| caption = Pictured in natural color approaching [[equinox]], photographed by ''[[Cassini–Huygens|Cassini]]'' in July 2008; the dot in the bottom left corner is [[Titan (moon)|Titan]] |
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| image = [[File:Saturn during Equinox.jpg|280px|alt=The planet Saturn|The planet Saturn]] |
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| background = #f8f9fa |
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| orbit_ref = |
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| pronounced = {{IPAc-en|audio=en-us-Saturn.ogg|ˈ|s|æ|t|ər|n}}<ref name="walter2003"/> |
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<ref name="horizons">{{cite web |
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| named_after = [[Saturn (mythology)|Saturn]] |
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| last = Yeomans | first = Donald K. | date = 2006-07-13 |
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| 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|url-status = dead}}</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 | bibcode = 2010JGRA..115.8203M | doi-access = free |issn=0148-0227}}</ref> {{IPAc-en|'|k|r|ou|n|i|@|n}}<ref>{{OED|Cronian}}</ref> |
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| url = http://ssd.jpl.nasa.gov/?horizons |
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| orbit_ref = <ref name="fact" /> |
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| title = HORIZONS System | work=Solar System dynamics |publisher=National Aeronautics and Space Administration |
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| epoch = [[J2000.0]] |
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| accessdate = 2007-08-08 }} At the site, go to the "web interface" then select "Ephemeris Type: ELEMENTS", "Target Body: Saturn Barycenter" and "Center: Sun".</ref>{{ref label|B_Center|b|b}} |
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| aphelion = {{convert|1514.50|e6km|AU|4|abbr=unit}} |
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| epoch = [[Epoch (astronomy)#J2000.0|J2000]] |
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| perihelion = {{convert|1352.55|e6km|AU|4|abbr=unit}} |
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| aphelion = 1,513,325,783 km<br />10.115 958 04 [[Astronomical unit|AU]] |
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| time_periastron = 2032-Nov-29<ref>{{Cite web|url=https://ssd.jpl.nasa.gov/horizons.cgi?find_body=1&body_group=mb&sstr=699|title=HORIZONS Web-Interface|website=ssd.jpl.nasa.gov}}</ref> |
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| perihelion = 1,353,572,956 km<br />9.048 076 35 AU |
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| semimajor = {{convert|1433.53|e6km|AU|4|abbr=unit}} |
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| semimajor = 1,433,449,370 km<br />9.582 017 20 AU |
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| eccentricity = 0. |
| eccentricity = {{val|0.0565}} |
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| period = |
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| period = 10,832.327 [[day]]s<br />29.657 296 [[Julian year (astronomy)|yr]]<br /> |
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{{plainlist | |
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| synodic_period = 378.09 days<ref name="fact" /> |
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* {{val|29.4571|u=[[Julian year (astronomy)|yr]]}} |
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| avg_speed = 9.69 km/s<ref name="fact" /> |
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* {{val|fmt=commas|10759.22|u=days}} |
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| inclination = 2.485 240° to [[Ecliptic]]<br />5.51° to [[Ecliptic#Ecliptic and planets|Sun’s equator]]<br />0.93° to [[Invariable plane]]<ref>{{cite book |title=Gravity field and dynamics of the Earth |last1=Burša |first1=Milan |last2=Pĕc̆ |first2=Karel |year=1993 |publisher=Springer|isbn=9783540568179 |page=301}}</ref> |
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* {{val|fmt=commas|24491.07}} Saturnian [[solar day]]s<ref name="CSeligman" /> |
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| asc_node = 113.642 811° |
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}} |
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| arg_peri = 336.013 862° |
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| synodic_period = 378.09 days |
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| mean_anomaly = 320.346 750° |
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| avg_speed = {{convert|9.68|km/s|mi/s|sigfig=3|abbr=unit}} |
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| satellites = around 200 observed (61 with secure orbits) |
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| mean_anomaly = {{val|317.020|u=°}}<ref name="VSOP87" /> |
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|maximum distance from sun = {{convert|1500000000|km|mi|0|lk=off|abbr=on}} |
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| inclination = |
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|minimum distance from sun = {{convert|1350000000|km|mi|0|lk=on|abbr=on}} |
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{{plainlist | |
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| physical_characteristics = yes |
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* {{val|2.485|u=°}} to [[ecliptic]]<ref name="VSOP87" /> |
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| flattening = 0.097 96 ± 0.000 18 <!-- calculated using data from ref name=Seidelmann2007 --> |
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* {{val|5.51|u=°}} to [[Sun]]'s [[equator]]<ref name="VSOP87" /> |
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| equatorial_radius = 60,268 ± 4 km<ref name="Seidelmann2007">{{cite journal|last= Seidelmann|first= P. Kenneth|coauthors= Archinal, B. A.; A’hearn, M. F.; et al.|title= Report of the IAU/IAGWorking Group on cartographic coordinates and rotational elements: 2006|journal= Celestial Mech. Dyn. Astr. |volume=90|pages=155–180|year=2007|doi=10.1007/s10569-007-9072-y|url=http://adsabs.harvard.edu/doi/10.1007/s10569-007-9072-y}}</ref>{{ref label|1bar|a|a}}<br />9.4492 Earths |
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* {{val|0.93|u=°}} to [[invariable plane]]<ref name=Souami_Souchay_2012 /> |
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| polar_radius = 54,364 ± 10 km<ref name="Seidelmann2007" />{{ref label|1bar|a|a}}<br />8.5521 Earths |
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}} |
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| surface_area = 4.27{{e|10}} km²<ref name="nasafact">{{cite web |url= http://solarsystem.nasa.gov/planets/profile.cfm?Object=Saturn&Display=Facts%20NASA:%20Solar%20System%20Exploration:%20Planets:%20Saturn:%20Facts%20&%20Figures |title=Saturn |work=Solar System exploration: planets |publisher=National Aeronautics and Space Administration |year=2011-03-22 |accessdate=2011-06-19}}</ref>{{ref label|1bar|a|a}}<br />83.703 Earths |
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| asc_node = {{val|113.665|u=°}} |
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| volume = 8.2713{{e|14}} km³<ref name="fact">{{cite web |
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| arg_peri = {{val|339.392|u=°}}<ref name="VSOP87" /> |
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|url = http://nssdc.gsfc.nasa.gov/planetary/factsheet/saturnfact.html |
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| satellites = [[moons of Saturn|145]] in total [[moonlet]]s.<ref name=fact /> |
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|title = Saturn Earth comparison |
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| physical_ref = <ref name="fact" /> |
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|work= Saturn fact sheet |
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| mean_radius = {{convert|58232|km|mi|0|abbr=unit}}<ref group=lower-alpha name=1bar /> |
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|publisher=National Aeronautics and Space Administration |
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| equatorial_radius = |
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|last = Williams |
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{{plainlist | |
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|first = Dr. David R. |
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* {{convert|60268|km|mi|0|abbr=unit}}<ref group=lower-alpha name=1bar>Refers to the level of 1 bar atmospheric pressure</ref> |
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|accessdate = 2007-07-31 |
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* {{val|9.449}} Earths |
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|date = 2006-09-07}}</ref>{{ref label|1bar|a|a}}<br />763.59 Earths |
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}} |
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| mass = 5.6846{{e|26}} kg<ref name="fact" /><br />95.152 Earths |
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| polar_radius = |
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| density = 0.687 g/cm³<ref name="fact"/>{{ref label|1bar|a|a}}<br /> (less than [[water]]) |
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{{plainlist | |
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| surface_grav = 10,44 [[Acceleration|m/s²]]<ref name="fact" />{{ref label|1bar|a|a}}<br />0.914 [[g-force|''g'']] |
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* {{convert|54364|km|mi|0|abbr=unit}}<ref group=lower-alpha name=1bar /> |
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| escape_velocity = 35.5 km/s<ref name="fact" />{{ref label|1bar|a|a}} |
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* {{val|8.552|u=Earths}} |
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| sidereal_day = 0.439–0.449 days<ref name="saturnDay">{{cite web |
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}} |
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|url = http://www.space.com/scienceastronomy/070906_saturn_day.html |
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| flattening = {{val|0.09796}} |
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|title = Length of Saturn's day revised |
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| circumference = |
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|publisher = ''Space.com'' |
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{{unbulleted list |class=nowrap |
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|last = Than |
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| {{convert|365882.4|km|mi|comma=gaps|abbr=on|disp=x| <small>[[equator]]ial (|)</small>}}<ref>{{cite web |title=By the Numbers – Saturn |url=https://solarsystem.nasa.gov/planets/saturn/by-the-numbers/ |website=NASA Solar System Exploration |publisher=[[NASA]] |access-date=5 August 2020 }}</ref> |
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|first = Ker |
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}} |
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|accessdate = 2007-09-06 |
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| surface_area = |
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|date = 2007-09-06}}</ref><br /> (10 h 32 – 47 min) |
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{{plainlist | |
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| rot_velocity = 9.87 km/s{{ref label|1bar|a|a}}<br />35 500 km/h |
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* {{convert|4.27e10|km2|sqmi|abbr=unit}}<ref name="nasafact" /><ref group=lower-alpha name=1bar /> |
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| axial_tilt = 26.73°<ref name="fact" /> |
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* {{val|83.703|u=Earths}} |
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| right_asc_north_pole = 2 h 42 min 21 s<br />40.589°<ref name="Seidelmann2007" /> |
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}} |
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| declination = 83.537°<ref name="Seidelmann2007" /> |
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| volume = |
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| albedo = 0.342 ([[Bond albedo|bond]])<br /> |
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{{plainlist | |
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0.47 ([[Geometric albedo|geom.]])<ref name="fact" /> |
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* {{convert|8.2713e14|km3|cumi|abbr=unit}}<ref group=lower-alpha name=1bar /> |
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| magnitude = +1.2 to -0.24<ref name="magnitude">{{cite web |
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* {{val|763.59|u=Earths}} |
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|url = http://findarticles.com/p/articles/mi_qa4015/is_200101/ai_n8933308 |
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}} |
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|title = Wideband photoelectric magnitude measurements of Saturn in 2000 |
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| mass = |
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|accessdate = 2007-10-14 |
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{{plainlist | |
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|last = Schmude |
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* {{val|5.6834e26|u=kg}} |
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|first = Richard W Junior |
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* {{val|95.159|u=Earths}} |
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|year = 2001 |
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}} |
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|work= Georgia Journal of Science}}</ref> |
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| density = {{convert|0.687|g/cm3|lk=on|abbr=unit}}<ref group=lower-alpha name=1bar_b>Based on the volume within the level of 1 bar atmospheric pressure</ref> {{small|(less than water)}} |
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| angular_size = 14.5" – 20.1"<ref name="fact" /><br />(excludes rings) |
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| surface_grav = |
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| temperatures = yes |
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{{plainlist | |
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| temp_name1 = 1 bar level |
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* {{convert|10.44|m/s2|lk=on|abbr=unit}}<ref group=lower-alpha name=1bar /> |
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| min_temp_1 = |
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* 1.065 ''[[g-force|g]]'' |
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| mean_temp_1 = 134 [[Kelvin|K]]<ref name="fact" /> |
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}} |
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| max_temp_1 = |
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| moment_of_inertia_factor = {{val|0.22|}}<ref name="Fortney2018">{{cite book|last1= Fortney|first1= J.J.|last2= Helled|first2= R.|last3= Nettlemann|first3= N.|last4= Stevenson|first4= D.J.|last5= Marley|first5= M.S.|last6= Hubbard|first6= W.B.|last7= Iess|first7= L.|editor1= Baines, K.H.|editor2= Flasar, F.M.|editor3= Krupp, N.|editor4= Stallard, T.|title= Saturn in the 21st Century|chapter= The Interior of Saturn|chapter-url= https://books.google.com/books?id=p358DwAAQBAJ&pg=PA51 |pages= 44–68|date=6 December 2018|publisher= Cambridge University Press|isbn= 978-1-108-68393-7}}</ref> |
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| temp_name2 = 0.1 bar |
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| escape_velocity = {{convert|35.5|km/s|mi/s|abbr=unit}}<ref group=lower-alpha name=1bar /> |
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| min_temp_2 = |
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| |
| rotation = 10 h 32 m 36 s <br/>([[synodic day|synodic; solar day]])<ref name="CSeligman"/> |
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| 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/news.php?feature=731 |date=18 January 2019 |work=[[NASA]] |access-date=18 January 2019 |archive-date=29 August 2019 |archive-url=https://web.archive.org/web/20190829054935/https://www.jpl.nasa.gov/news/news.php?feature=731 |url-status=dead }}</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 |pages=1 |number=1 |doi=10.3847/1538-4357/aaf798 |arxiv=1805.10286 |bibcode=2019ApJ...871....1M |s2cid=67840660 |doi-access=free }}</ref> |
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| max_temp = |
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| rot_velocity = {{convert|9.87|km/s|mi/s km/h|abbr=unit}}<ref group=lower-alpha name=1bar /> |
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| pronounce = {{IPA-en|ˈsætərn||en-us-Saturn.ogg}}<ref>{{cite book |
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| axial_tilt = 26.73° {{small|(to orbit)}} |
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| first=Elizabeth | last=Walter | date=2003-04-21 |
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| right_asc_north_pole = 40.589°; {{RA|2|42|21}} |
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| title=Cambridge advanced learner's dictionary |
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| declination = 83.537° |
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| publisher=Cambridge University Press |
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| albedo = |
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| edition=Second | isbn=0521531063}}</ref> |
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{{plainlist | |
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| adjectives = Saturnian |
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* 0.342 ([[Bond albedo|Bond]])<ref name="Hanel_et_al"/> |
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| atmosphere = yes |
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* 0.499 ([[Geometric albedo|geometric]])<ref name="Mallama_et_al"/> |
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| atmosphere_ref = |
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}} |
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<ref name="fact" /> |
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| temp_name1 = 1 [[bar (unit)|bar]] |
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| scale_height = 59.5 km |
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| mean_temp_1 = 134 K |
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| atmosphere_composition = |
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| temp_name2 = 0.1 [[bar (unit)|bar]] |
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<table> |
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| min_temp_2 = 88 K<ref name="min_max">{{cite web |title=Saturn's Temperature Ranges |url=https://sciencing.com/saturns-temperature-ranges-7704.html |website=Sciencing}}</ref> |
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<tr><td> |
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| mean_temp_2 = 97 K<ref>{{cite web |title=The Planet Saturn |url=https://www.weather.gov/fsd/saturn |website=National Weather Service}}</ref> |
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~96%</td><td>[[Hydrogen]] (H<sub>2</sub>) |
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| max_temp_2 = 151 K<ref name="min_max"/> |
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</td></tr><tr><td> |
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| magnitude = −0.55<ref name="Mallama_and_Hilton" /> to +1.17<ref name="Mallama_and_Hilton"/> |
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~3%</td><td>[[Helium]] |
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| angular_size = 14.5″ to 20.1″ (excludes rings) |
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</td></tr><tr><td> |
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| atmosphere_ref = <ref name="fact" /> |
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~0.4%</td><td>[[Methane]] |
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| surface_pressure = 140 kPa<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 |url-status=dead }}</ref> |
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</td></tr><tr><td> |
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| scale_height = {{convert|59.5|km|mi|abbr=unit}} |
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~0.01%</td><td>[[Ammonia]] |
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| atmosphere_composition = {{aligned table|cols=2 |
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</td></tr><tr><td> |
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| {{val|96.3|2.4|u=%}} |[[hydrogen]] ({{chem2|H2}}) |
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~0.01%</td><td>[[Hydrogen deuteride]] (HD) |
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| {{val|3.25|2.4|u=%}} |[[helium]] ({{chem2|He}}) |
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</td></tr><tr><td> |
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| {{val|0.45|0.2|u=%}} |[[methane]] ({{chem2|CH4}}) |
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0.000 7%</td><td>[[Ethane]] |
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| {{val|0.0125|0.0075|u=%}} |[[ammonia]] ({{chem2|NH3}}) |
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</td></tr><tr><td> |
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| {{val|0.0110|0.0058|u=%}} |[[hydrogen deuteride]] (HD) |
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'''Ices''':</td><td> |
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| {{val|0.0007|0.00015|u=%|fmt=none}} |[[ethane]] ({{chem2|C2H6}}) |
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</td></tr><tr><td> |
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}}'''Ices''': |
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</td><td>[[Ammonia]] |
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* [[ammonia]] ({{chem2|NH3}}) |
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</td></tr><tr><td> |
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* [[water]] ({{chem2|H2O}}) |
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* [[ammonium hydrosulfide]] ({{chem2|NH4SH}}) |
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</td></tr><tr><td> |
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</td><td>[[ammonium hydrosulfide]](NH<sub>4</sub>SH) |
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</td></tr></table> |
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|} |
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}} |
}} |
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'''Saturn''' is the sixth [[planet]] from the [[Sun]] in the [[Solar System]]. It is the second largest planet in the Solar System after [[Jupiter]]. Like Jupiter, [[Uranus]] and [[Neptune]], it is a "[[gas giant]]". |
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'''Saturn''' is the sixth [[planet]] from the [[Sun]] in the [[Solar System]]. Saturn takes about 29.5 [[Earth]] years to complete one orbit around the Sun. A day on Saturn is much shorter than an Earth day, lasting only about 10.7 hours. This means that Saturn spins much faster than Earth, completing more than two rotations in the same time it takes Earth to complete just one. <ref>{{Cite web|title=Saturn: Facts - NASA Science|url=https://science.nasa.gov/saturn/facts/|access-date=2024-07-08|website=science.nasa.gov|language=en-US}}</ref> |
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The interior of Saturn is probably a [[planetary core|core]] of [[iron]], [[nickel]], [[silicon]] and [[oxygen]] compounds, surrounded by a deep layer of [[metallic hydrogen]], then a layer of [[liquid]] [[hydrogen]] and liquid [[helium]] and finally, an outer [[gas]]eous layer.<ref name="Composition ref">{{cite web |
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| url = http://www.astrophysicsspectator.com/topics/planets/GiantGaseousPlanets.html |
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| title = Giant gaseous planets |
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| accessdate = 2010-07-05 |
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| last=Brainerd |
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| first=Jerome James |
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| date = 2004-10-27 |
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| publisher = The Astrophysics Spectator}}</ref> |
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Saturn is one of the four [[giant planet]]s in the Solar System, with [[Jupiter]], [[Uranus]], and [[Neptune]]. It is the second largest planet in the Solar System (Jupiter is the largest).<ref>{{Cite web|title=Saturn: Facts|url=https://science.nasa.gov/saturn/facts/|access-date=9 November 2023|website=[[NASA]]|language=en}}</ref> |
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Saturn has 62 known [[moons]] [[orbit]]ing the planet; 53 are officially named.<ref>{{cite web |
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|first=Enrico|last=Piazza |
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|title=Saturn's moons|editors=Kirk Munsell |
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|work=Cassini, Equinox Mission|publisher=JPL NASA |
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|url=http://saturn.jpl.nasa.gov/science/moons/ |
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|accessdate=2010-06-22}} |
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</ref> The largest moon is [[Titan (moon)|Titan]], which is larger in volume than the planet [[Mercury (planet)|Mercury]]. Titan is the second largest moon in the Solar System. The largest moon is Jupiter's moon, [[Ganymede]]. Also around Saturn there is a very large system of [[planetary ring|rings]], made of [[ice]] with smaller amounts of [[minerals|rocks]] and dust. Saturn is about 1,400,000,000 [[kilometer|km]] (869,000,000 [[mile|mi]]) from the Sun. In the time it takes Saturn to complete one orbit of the Sun, or one Saturn year, the Earth has orbited 29.6 times, or 29.6 [[Julian year (astronomy)|years]] on Earth.<ref name="fact"/> |
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Saturn was named after the [[Roman mythology|Roman god]] [[Saturn (mythology)| |
Saturn was named after the [[Roman mythology|Roman god]] [[Saturn (mythology)|Saturn]]. He was the Roman equivalent of the [[Greek mythology|Greek god]] [[Kronos]].<ref>{{cite web |url=http://www.credoreference.com/entry/hfcwd/cronia_kronia |title=Cronia (Kronia) |work=Holidays, Festivals, and Celebrations of the World Dictionary |year=2010 |access-date=July 11, 2011}}</ref> Saturn's symbol is ♄ which is the symbol of Saturnus' [[sickle]].<ref>{{cite web |last=Crystal |first=Ellie |title=Saturn Mythology |url=http://www.crystalinks.com/saturnmyth.html |work=Crystalinks.com |access-date=February 28, 2007}}</ref> |
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Inside Saturn is probably a [[planetary core|core]] of [[iron]], [[nickel]], [[silicon]] and [[oxygen]] compounds, surrounded by a deep layer of [[metallic hydrogen]], then a layer of [[liquid]] [[hydrogen]] and liquid [[helium]] and finally, an outer [[gas]]eous layer.<ref name="Composition ref">{{cite web|url=http://www.astrophysicsspectator.com/topics/planets/GiantGaseousPlanets.html| title = Giant gaseous planets| access-date = July 5, 2010| last=Brainerd, Jerome James 2004| publisher = The Astrophysics Spectator}}</ref> |
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==Physical features== |
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Saturn has 146 known [[Natural satellite|moons]] [[orbit]]ing the planet.<ref>{{cite web |
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|title=Planetary Satellite Discovery Circumstances |
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|url=https://ssd.jpl.nasa.gov/?sat_discovery |
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|publisher=NASA |
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|access-date=December 28, 2019}}</ref> The largest moon is [[Titan (moon)|Titan]]. Titan is larger in [[volume]] than the planet [[Mercury (planet)|Mercury]]. It is the second-largest moon in the Solar System. The largest moon is a moon of Jupiter, [[Ganymede (moon)|Ganymede]]. There are also many [[planetary ring|rings]] around Saturn. These rings are made of [[ice]] with some [[minerals|rocks]] and dust. Some people think that that the rings were made by a moon [[Impact event|impact]] or other event. Saturn is about 1,433,000,000 [[kilometer|km]] (870,000,000 [[mile|mi]]) on average from the Sun. Saturn takes 29.4 [[Julian year (astronomy)|Earth years]] in order to complete a revolution around the Sun.<ref>{{Cite web|title=Saturn: Facts - NASA Science|url=https://science.nasa.gov/saturn/facts/|access-date=2024-01-11|website=science.nasa.gov|language=en}}</ref> |
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== Physical features == |
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[[File:Saturn Earth Comparison.png|thumbnail|right|220 px|alt=Saturn compared to Earth|Saturn compared with the size of the [[Earth]]]] |
[[File:Saturn Earth Comparison.png|thumbnail|right|220 px|alt=Saturn compared to Earth|Saturn compared with the size of the [[Earth]]]] |
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[[File:Saturn Robert Hooke 1666.jpg|thumb|alt=Pen sketch with several labelled rings|Drawing of Saturn by [[Robert Hooke]] in 1666]] |
[[File:Saturn Robert Hooke 1666.jpg|thumb|alt=Pen sketch with several labelled rings|Drawing of Saturn by [[Robert Hooke]] in 1666]] |
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Saturn is an [[oblate spheroid]], meaning that it is flattened at the [[Geographical pole|pole]]s, and it swells out around its [[equator]].<ref name=rgo/> The planet's equatorial [[diameter]] is {{convert|120536|km|mi|0|lk=off|abbr=on}}, while its polar diameter (the distance from the north pole to the south pole) is {{convert|108728|km|mi|0|lk=off|abbr=on}}; a 9% difference.<ref>{{cite web |url= http://www.jpl.nasa.gov/news/press_kits/cassini-arrival.pdf |title=Cassini–Huygens Saturn arrival |format=PDF |page=9 |work=Press kit June 2004| publisher=National Aeronautics and Space Administration |accessdate=2011-06-25}}</ref> Saturn has a flattened shape is due to its very fast [[rotation]], rotating once every 10.8 hours.<ref name="fact"/> Saturn is the only planet in the Solar System that is less [[density|dense]] than [[water]]. Even though the planet's [[planetary core|core]] is very dense, it has a gaseous [[atmosphere]], so the average [[relative density|specific density]] of the planet is 0.69 g/cm³ (less than the density of water). This means if Saturn could be placed in a large pool of water, it would float.<ref>{{cite book |title=Voyager: Exploring the outer planets |last=Verba |first=Joan Marie |year=1991 |publisher=FTL Publications |isbn=0982523203 |page=20}}</ref> |
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Saturn is a squished sphere. This means that it is flattened at the [[Geographical pole|poles]] and wider around the [[equator]].<ref name=rgo /> The planet's [[Equator|equatorial]] [[diameter]] is {{convert|120536|km|mi|0|lk=off|abbr=on}}. Its polar diameter (the distance from the north pole to the south pole through the centre) is {{convert|108728|km|mi|0|lk=off|abbr=on}}. This is a 9% difference.<ref>{{cite web |url=http://www.jpl.nasa.gov/news/press_kits/cassini-arrival.pdf |title=Cassini–Huygens Saturn arrival |page=9 |work=Press kit June 2004| publisher=National Aeronautics and Space Administration |access-date=June 25, 2011}}</ref> Saturn has a flattened shape because of its very fast [[rotation]]. It rotates once every 10.8 Earth hours. |
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===Atmosphere=== |
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The outer part of Saturn's atmosphere is made up of about 96% hydrogen, 3% helium, 0.4% [[methane]] and 0.01% [[ammonia]].<ref name="fact"/> There are also very small amounts of [[acetylene]], [[ethane]] and [[phosphine]].<ref name="Mira">{{cite web |url= http://www.mira.org/fts0/planets/100/text/txt002x.htm |title= Saturn |first= |last=| |work=MIRA: field trips to the stars: the Solar System|year=2006 |publisher= [http://www.mira.org/ Monterey Institute of Research in Astronomy] |accessdate=2011-06-19}}</ref> |
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Saturn is the only planet in the Solar System that is less [[density|dense]] than [[water]]. Even though the planet's [[planetary core|core]] is very dense, it has a [[Gas|gaseous]] [[atmosphere]]. This makes its average density is 0.69 g/cm<sup>3</sup>. This means if Saturn could be placed in a large pool of water, it would float.<ref>{{cite book |title=Voyager: Exploring the outer planets |url=https://archive.org/details/voyagerexploring00verb |last=Verba |first=Joan Marie |year=1991 |publisher=FTL Publications |isbn=0-9825232-0-3 |page=[https://archive.org/details/voyagerexploring00verb/page/20 20]}}</ref> |
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=== Atmosphere === |
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The outer part of Saturn's atmosphere is made up of about 96% [[hydrogen]], 3% [[helium]], 0.4% [[methane]] and 0.01% [[ammonia]]. There are also some [[acetylene]], [[ethane]] and [[phosphine]].<ref name="Mira">{{cite web |url=http://www.mira.org/fts0/planets/100/text/txt002x.htm |title= Saturn |work=MIRA: field trips to the stars: the Solar System|year=2006 |publisher= Monterey Institute of Research in Astronomy |access-date=June 19, 2011}}</ref> |
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[[File:Saturn hexagonal north pole feature.jpg|thumbnail|right|alt=The hexagonal cloud|The north polar [[hexagon]]al cloud first found by [[Voyager 1]] and later by [[Cassini-Huygens|Cassini]]]] |
[[File:Saturn hexagonal north pole feature.jpg|thumbnail|right|alt=The hexagonal cloud|The north polar [[hexagon]]al cloud first found by [[Voyager 1]] and later by [[Cassini-Huygens|Cassini]]]] |
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Saturn's [[cloud]]s show a banded pattern, like the cloud bands seen on Jupiter. Saturn's clouds are much fainter and the bands are wider at the equator. Saturn's lowest cloud layer is made up of water ice, and is about {{convert|10|km|mi|0|lk=off|abbr=on}} thick.<ref name="Mira"/> The [[temperature]] here is quite low, at 250 [[Kelvin|K]] (-10°[[Fahrenheit|F]], -23°[[Celsius|C]]). However scientists do not agree about this. The layer above, about {{convert|77|km|mi|0|lk=off|abbr=on}} thick, is made up of [[ammonium sulfide|ammonium hydrosulfide]] ice, and above that is a layer of ammonia ice clouds {{convert|80|km|mi|0|lk=off|abbr=on}} thick.<ref name="Mira"/> The highest layer is made up of hydrogen and helium gases, which extends between {{convert|200|km|mi|0|lk=off|abbr=on}} and {{convert|270|km|mi|0|lk=off|abbr=on}} above the water cloud tops. [[Aurora]]s are also known to form in Saturn in the [[mesosphere]].<ref name="Mira"/> The temperature at Saturn's cloud tops is extremely low, at 98 K (-283°F, -175°C). The temperatures in the inner layers are much higher than the outside layers because of the [[heat]] produced by Saturn's interior.<ref name=heat>{{cite web |url= http://www.nasa.gov/mission_pages/cassini/whycassini/planet.html |title=A gas giant with super-fast winds |first= |last= |work= Cassini: unlocking Saturn's secrets| publisher=National Aeronautics and Space Administration |year=2007 |accessdate=2011-06-19}}</ref> |
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Saturn's winds are some of the fastest in the Solar System, reaching 1,800 [[kilometres per hour|km/h]] (1,118 [[miles per hour|mph]]),<ref>{{cite book |title=Probing the new solar system |last=Wilkinson |first=John |year=2009 |publisher=CSIRO Publishing |isbn=9780643095755 |page=208 |url=http://books.google.com/books?id=hXmZP40vFksC&source=gbs_navlinks_s |accessdate=2011-05-23}}</ref> ten times faster then winds on [[Earth]].<ref>{{cite web |url=http://www.nasa.gov/mission_pages/cassini/whycassini/cassini_storms_on_saturn.html |title=Saturn's storms run rings around Earth's |first=Rosemary |last=Sullivant |work=Cassini: unlocking Saturn's secrets| publisher= National Aeronautics and Space Administration |accessdate=2011-05-24}}</ref> |
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Saturn's [[cloud]]s show a banded pattern. This is like the cloud bands seen on Jupiter. Saturn's clouds are much [[wikt:faint#Adjective|fainter]] and the bands are wider at the equator. Saturn's lowest cloud layer is made up of water ice. It is about {{convert|10|km|mi|0|lk=off|abbr=on}} thick.<ref name="Mira" /> The [[temperature]] there is quite low, at 250 [[Kelvin|K]] (-10°[[Fahrenheit|F]], -23°[[Celsius|C]]). However, scientists do not all agree on this. The layer above is made up of [[ammonium sulfide|ammonium hydrosulfide]] ice. It is about {{convert|77|km|mi|0|lk=off|abbr=on}} thick. Above it is a layer of ammonia ice clouds which are {{convert|80|km|mi|0|lk=off|abbr=on}} thick.<ref name="Mira" /> The highest layer is made up of hydrogen and helium gases. It goes to between {{convert|200|km|mi|0|lk=off|abbr=on}} and {{convert|270|km|mi|0|lk=off|abbr=on}} above the water cloud tops. [[Aurora]]s can be seen in Saturn in the [[mesosphere]].<ref name="Mira" /> The temperature at Saturn's cloud tops is very low, at 98 K (-283 °F, -175 °C). The temperatures in the inner layers are much higher than the outside layers because of the [[heat]] made by Saturn's inside.<ref name=heat>{{cite web |url=http://www.nasa.gov/mission_pages/cassini/whycassini/planet.html |title=A gas giant with super-fast winds |work=Cassini: unlocking Saturn's secrets |publisher=National Aeronautics and Space Administration |year=2007 |access-date=June 19, 2011 |archive-date=March 4, 2011 |archive-url=https://web.archive.org/web/20110304152513/http://www.nasa.gov/mission_pages/cassini/whycassini/planet.html |url-status=dead }}</ref> Saturn's [[Wind|winds]] are some of the fastest in the Solar System. They can reach 1,800 [[kilometres per hour|km/h]] (1,118 [[miles per hour|mph]]),<ref>{{cite book |title=Probing the new solar system |last=Wilkinson |first=John |year=2009 |publisher=CSIRO Publishing |isbn=978-0-643-09575-5 |page=208 |url=https://books.google.com/books?id=hXmZP40vFksC |access-date=May 23, 2011}}</ref> ten times faster than winds on [[Earth]].<ref>{{cite web |url=http://www.nasa.gov/mission_pages/cassini/whycassini/cassini_storms_on_saturn.html |title=Saturn's storms run rings around Earth's |first=Rosemary |last=Sullivant |work=Cassini: unlocking Saturn's secrets |publisher=National Aeronautics and Space Administration |access-date=May 24, 2011 |archive-date=June 6, 2011 |archive-url=https://web.archive.org/web/20110606043226/http://www.nasa.gov/mission_pages/cassini/whycassini/cassini_storms_on_saturn.html |url-status=dead }}</ref> |
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====Storms and spots==== |
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Saturn's atmosphere is also known to form oval shaped clouds, similar to the clearer spots seen in Jupiter. These oval spots are cyclonic storms, the same as [[cyclone]]s seen on Earth. In 1990, the [[Hubble Space Telescope]] found a very large white cloud near Saturn's equator. Storms like the one in 1990 were known as ''[[Great White Spot]]s''. These unique storms only exist for a short time and only happen about every 30 Earth years, at the time of the summer [[solstice]] in the [[Northern Hemisphere]].<ref>{{cite web |url= http://www.sciencedirect.com/science/article/pii/S0019103505000308 |title=Saturn's cloud structure and temporal evolution from ten years of Hubble Space Telescope images (1994–2003) |first= |last=S. Pérez-Hoyos, A. Sánchez-Lavega, R.G. French, J.F. Rojas. |work=Science Direct |year=2005 |accessdate=2011-06-19}}</ref> |
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Great White Spots were also found in 1876, 1903, 1933, and 1960. If this cycle continues, another storm will form in about 2020.<ref>{{cite encyclopedia | title =The 1990 Great White Spot of Saturn | encyclopedia = 1993 Yearbook of Astronomy| volume = | pages =176–215 | publisher =W.W. Norton & Company, London | date =1992 | id = | accessdate = }}</ref> |
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==== Storms and spots ==== |
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The [[Voyager 1]] spacecraft found a [[hexagon]]al cloud pattern near Saturn's north pole at about [[longitude|78°N]]. The [[Cassini−Huygens]] probe later confirmed it in 2006. Unlike the north pole, the south pole does not show any hexagonal cloud feature. The probe also discovered a [[hurricane]]-like storm locked to the south pole that clearly showed an [[eye (cyclone)|eyewall]]. Until this discovery, eyewalls had only been seen on Earth.<ref>{{cite web |url= http://www.newscientist.com/article/dn10499 |title=Spectacular storm rages on Saturn's south pole |first= Maggie|last=McKee |work=New Scientist Magazine |year=2006-11-06 |accessdate=2011-04-21}}</ref> |
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Saturn's atmosphere can make oval shaped clouds. They are like the clearer spots seen on Jupiter. These oval spots are cyclonic storms, similar to [[cyclone]]s seen on Earth. In 1990, the [[Hubble Space Telescope]] found a very large white cloud near Saturn's equator. Storms like this one in 1990 were known as [[Great White Spot]]s. These unique storms only exist for a short time and only occur in about every 30 Earth years, in summer [[solstice]]<nowiki/>s in the [[Northern Hemisphere]].<ref>{{cite journal |url=http://www.sciencedirect.com/science/article/pii/S0019103505000308 |title=Saturn's cloud structure and temporal evolution from ten years of Hubble Space Telescope images (1994–2003) |last=S. Pérez-Hoyos, A. Sánchez-Lavega, R.G. French, J.F. Rojas. |journal=Icarus |year=2005 |volume=176 |issue=1 |pages=155–174 |doi=10.1016/j.icarus.2005.01.014 |bibcode=2005Icar..176..155P |access-date=June 19, 2011}}</ref> Great White Spots were also found in 1876, 1903, 1933, and 1960. |
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The [[Voyager 1]] spacecraft found a [[hexagon]]al cloud [[pattern]] near Saturn's north pole at about [[longitude|78°N]]. The [[Cassini−Huygens]] probe later [[wikt:confirm|confirmed]] it in 2006. Unlike the north pole, the south pole does not show any hexagonal clouds. The probe also found a [[hurricane]]-like storm on the south pole that showed an [[eye (cyclone)|eyewall]]. Until this finding, eyewalls had only been seen on Earth.<ref>{{cite web |url=https://www.newscientist.com/article/dn10499 |title=Spectacular storm rages on Saturn's south pole |first= Maggie|last=McKee |work=New Scientist Magazine |date=2006-11-06 |access-date=April 21, 2011}}</ref> |
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===Interior=== |
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Saturn's interior is similar to Jupiter's interior. It has a small rocky core about the size of the Earth at its centre.<ref name=rgo>{{cite web |url= http://www.oarval.org/section3_11.htm |title=Saturn |first= |last= |work=Information Leaflet No. 42|publisher=[[Royal Observatory, Greenwich|Royal Greenwich Observatory]] |year=2009 |accessdate=2011-04-26}}</ref> It is very hot; its [[temperature]] reaches 15,000 [[Kelvin|K]] ({{convert|26540|F|C|0|lk=off|abbr=on}}). Saturn is so hot that it gives out more [[heat energy]] into space than it receives from the [[Sun]].<ref name=heat/> Above it is a thicker layer of metallic hydrogen, about {{convert|30000|km|mi|0|lk=off|abbr=on}} deep. Above that layer is a region of liquid hydrogen and helium.<ref>{{cite web |url= http://www.nmm.ac.uk/explore/astronomy-and-time/astronomy-facts/solar-system/saturn |title=Saturn |first= |last= |work=Solar System |publisher=National Maritime Museum |year=2005-10-04 |accessdate=2011-06-19}}</ref> The core is heavy, about 9 to 22 times more mass than the Earth's core.<ref>{{cite web|url=http://www.sciencemag.org/cgi/content/full/305/5689/1414 |title=Looking into the giant planets |first=Jonathon J. |last=Fortney |work=Science 305 (5689): 1414–1415|year=2004 |accessdate= 2007-04-30}}</ref> |
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=== Interior === |
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Saturn's inside is similar to Jupiter's inside. It has a small rocky core about the size of the Earth at its [[center]].<ref name=rgo>{{cite web |url=http://www.oarval.org/section3_11.htm |title=Saturn |work=Information Leaflet No. 42|publisher=[[Royal Observatory, Greenwich|Royal Greenwich Observatory]] |year=2009 |access-date=April 26, 2011}}</ref> It is very hot. Its [[temperature]] reaches 15,000 [[Kelvin|K]] ({{convert|26540|F|C|0|lk=off|abbr=on}}). Saturn is so hot that it gives out more [[heat energy]] into space than it gets from the [[Sun]].<ref name=heat /> Above it is a thicker layer of metallic hydrogen, about {{convert|30000|km|mi|0|lk=off|abbr=on}} deep. Above that layer is a region of liquid hydrogen and helium.<ref>{{cite web |url=http://www.nmm.ac.uk/explore/astronomy-and-time/astronomy-facts/solar-system/saturn |title=Saturn |work=Solar System |publisher=National Maritime Museum |date=2005-10-04 |access-date=June 19, 2011 |archive-date=June 13, 2011 |archive-url=https://web.archive.org/web/20110613050453/http://www.nmm.ac.uk/explore/astronomy-and-time/astronomy-facts/solar-system/saturn |url-status=dead }}</ref> The core is heavy, with about 9 to 22 times more mass than the Earth's core.<ref>{{cite web|url=http://www.sciencemag.org/cgi/content/full/305/5689/1414 |title=Looking into the giant planets |first=Jonathon J. |last=Fortney |work=Science 305 (5689): 1414–1415|year=2004 |access-date= April 30, 2007}}</ref> |
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Saturn has a natural [[magnetic field]] that is weaker than Jupiter's. Like the Earth's, Saturn's field is a magnetic [[dipole]]. Saturn's field is unique in that it is perfectly symmetrical, unlike any other known planet.<ref name=sutton/> This means the field is exactly in line with the planet's [[axis of rotation|axis]].<ref name=sutton>{{cite web |url= http://books.google.com.au/books?id=oqqoUMj9-pUC&pg=PA509&lpg=PA509&dq=Saturn+symmetrical+axis&source=bl&ots=j1Gk8v8GFw&sig=6oopkQLLwSlBlHN-mLn7FAGqXCc&hl=en&ei=XZv9TcKbHoa4vwP66o2pAw&sa=X&oi=book_result&ct=result&resnum=9&ved=0CE8Q6AEwCA#v=onepage&q&f=false |title=Saturn yields to Voyager's brief caress |first=Christine |last=Sutton |work=New Scientist Magazine |year=1981-08-27 |accessdate=2011-06-19}}</ref> Saturn generates [[radio wave]]s, but they are too weak to be detected from Earth. The moon Titan orbits in the outer part of Saturn's magnetic field and gives out [[Plasma (physics)|plasma]] to the field from the [[ion]]ised particles in Titan's atmosphere.<ref>{{cite web |url= http://www-ssc.igpp.ucla.edu/personnel/russell/papers/sat_mag.html |title=Saturn: magnetic field and magnetosphere |first= |last=Russell, C. T.; Luhmann, J. G. |work=Encyclopedia of Planetary Sciences |publisher=Chapman and Hall|location=New York|pages=718—719|year=1997 |accessdate=2011-06-20}}</ref> |
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=== Magnetic field === |
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Saturn has a natural [[magnetic field]] that is weaker than Jupiter's. Like the Earth's, Saturn's field is a magnetic [[dipole]] (it has a North and a South). Saturn's field is unique in that it is perfectly [[symmetrical]], unlike any other known planet.<ref name=sutton /> This means the field is exactly in line with the planet's [[axis of rotation|axis]].<ref name=sutton>{{cite web |url=https://books.google.com/books?id=oqqoUMj9-pUC&dq=Saturn+symmetrical+axis&pg=PA509 |title=Saturn yields to Voyager's brief caress |first=Christine |last=Sutton |work=New Scientist Magazine |date=1981-08-27 |access-date=June 19, 2011 }}{{Dead link|date=November 2023 |bot=InternetArchiveBot |fix-attempted=yes }}</ref> Saturn generates [[radio wave]]s, but they are too weak to be detected from Earth.<ref>{{cite journal|last1=Smith|first1=A. G.|last2=Carr|first2=T. D.|title=Radio-Frequency Observations of the Planets in 1957–1958|url=https://archive.org/details/sim_astrophysical-journal_1959-09_130_2/page/641|journal=The Astrophysical Journal|volume=130|pages=641–647|year=1959|doi=10.1086/146753|bibcode=1959ApJ...130..641S|ref=Smith}}</ref> The moon Titan orbits in the outer part of Saturn's magnetic field and gives out [[Plasma (physics)|plasma]] to the field from the [[ion]]ised [[Particle|particles]] in Titan's atmosphere.<ref>{{cite encyclopedia |url=http://www-ssc.igpp.ucla.edu/personnel/russell/papers/sat_mag.html |title=Saturn: magnetic field and magnetosphere |last=Russell C.T.; Luhmann J.G. |encyclopedia=Encyclopedia of Planetary Sciences |publisher=Chapman and Hall |location=New York |pages=718–719 |year=1997 |access-date=June 20, 2011 |archive-date=October 5, 2011 |archive-url=https://www.webcitation.org/62DA9rN1s?url=http://www-ssc.igpp.ucla.edu/personnel/russell/papers/sat_mag.html |url-status=dead }}</ref> |
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Saturn's average distance from the Sun is over 1,400,000,000 km (869,000,000 mi), about nine times the distance from the Earth to the Sun. It takes 10,759 days, or about 29.7 years, for Saturn to orbit around the Sun.<ref>{{cite web |url= http://www.nasa.gov/topics/nasalife/saturn_time.html |title=NASA image of Saturn featured in Time Magazine's 'Year in Pictures' |work=NASA in your life| publisher= National Aeronautics and Space Administration |year=2009-12-30 |accessdate=2011-06-24}}</ref> This is known as Saturn's ''orbital period''. |
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== Rotation and orbit == |
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Voyager 1 measured Saturn's rotation as being 10 hours 14 minutes at the equator, 10 hours 40 minutes closer to the poles, and 10 hours 39 minutes 24 seconds for the planet's interior.<ref name=mira2>{{cite web |url= http://www.mira.org/fts0/planets/100/text/txt001x.htm#orbital |title= Saturn: orbital and rotational information |first= |last= |work=MIRA: field trips to the stars: the Solar System |publisher= Monterey Institute for Research in Astronomy|year=2006 |accessdate=2011-07-06}}</ref> This is known as its ''rotational period''. |
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Saturn's average [[distance]] from the Sun is over 1,400,000,000 km (886,000,000 mi). This is about nine times the distance from the Earth to the Sun. It takes 10,756 days, or about 29.4 years, for Saturn to orbit around the Sun.<ref>{{Cite web|title=Saturn: Facts - NASA Science|url=https://science.nasa.gov/saturn/facts/|access-date=2024-01-11|website=science.nasa.gov|language=en}}</ref> This is known as Saturn's ''orbital period''. |
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Voyager 1 [[Measurement|measured]] Saturn's rotation as being 10 hours, 14 minutes at the equator, 10 hours, 40 minutes closer to the poles, and 10 hours, 39 minutes, 24 seconds for the planet's inside.<ref name=mira2>{{cite web |url=http://www.mira.org/fts0/planets/100/text/txt001x.htm#orbital |title= Saturn: orbital and rotational information |work=MIRA: field trips to the stars: the Solar System |publisher= Monterey Institute for Research in Astronomy|year=2006 |access-date=July 6, 2011}}</ref> This is known as its ''rotational period''. |
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Cassini measured the rotation of Saturn as being 10 hours 45 minutes 45 seconds ± 36 seconds.<ref name="SFTSRPiaP" /> That is about six minutes, or one percent, longer than the radio rotational period measured by the Voyager 1 and Voyager 2 spacecraft, which flew by Saturn in 1980 and 1981. |
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Cassini measured the rotation of Saturn as being 10 hours, 45 minutes, 45 seconds ± 36 seconds.<ref name="SFTSRPiaP" /> That is about six minutes longer than the radio rotational period measured by the Voyager 1 and Voyager 2 [[Spacecraft|spacecrafts]], which flew by Saturn in 1980 and 1981. |
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Saturn's rotational period is calculated by the rotation speed of radio waves released by the planet. The Cassini−Huygens spacecraft discovered that the radio waves slowed down, suggesting that the rotational period increased.<ref name="SFTSRPiaP">{{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 |first=Carolina |last=Martinez |work=Cassini: unlocking Saturn's secrets| publisher= National Aeronautics and Space Administration |year=2004-06-28 |accessdate=2011-06-24}}</ref> Since the scientists do not think Saturn's rotation is actually slowing down, the explanation may lie in the magnetic field that causes the radio waves.<ref name="SFTSRPiaP" /> |
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Saturn's rotational period is calculated by the rotation speed of radio waves given off by the planet. The Cassini−Huygens spacecraft found that the radio waves slowed down. This suggested that the rotational period [[wikt:increase|increased]].<ref name="SFTSRPiaP">{{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 |first=Carolina |last=Martinez |work=Cassini: unlocking Saturn's secrets |publisher=National Aeronautics and Space Administration |date=2004-06-28 |access-date=June 24, 2011 |archive-date=2011-08-29 |archive-url=https://web.archive.org/web/20110829082445/http://www.nasa.gov/mission_pages/cassini/media/cassini-062804.html |url-status=dead }}</ref> Since scientists do not think Saturn's rotation is actually slowing down, the explanation may be that the magnetic field causes the radio waves.<ref name="SFTSRPiaP" /> |
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==Planetary rings== |
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== Planetary rings == |
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Saturn is best known for its [[planetary rings]] which are easy to see with a [[telescope]]. There are seven named rings; A, B, C, D, E, F, and G rings.<ref name=cosmos>{{cite journal |quotes= |last=Lovett |first=Rick |authorlink= |coauthors= |year=2011 |month=June/July |title=Dance of the rings |journal=Cosmos |volume= |issue=39 |pages=57 |id= |url=http://www.cosmosmagazine.com/ |accessdate= 2011-06-21}}</ref> They were named in the order they were discovered, which is different to their order from the planet. From the planet the rings are: D, C, B, A, F, G and E.<ref name=cosmos/>{{rp|57}} |
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{{Main|Rings of Saturn}} |
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Saturn is best known for its [[planetary rings]] which are easy to see with a [[telescope]]. There are seven named rings: A, B, C, D, E, F, and G.<ref name=cosmos>{{cite journal |
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|last=Lovett |first=Rick |
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|date= June 2011 |title=Dance of the rings |
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|journal=Cosmos |issue=39 |pages=57 |
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|url=http://www.cosmosmagazine.com/ |access-date= June 21, 2011}}</ref> They were named in the order they were found, which is different to their order from the planet. From the planet the rings are ordered: D, C, B, A, F, G and E.<ref name=cosmos />{{rp|57}} |
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Some scientists think that the rings are [[material]] left after a moon broke apart.<ref name=cosmos />{{rp|60}} A new idea says that it was a very large moon, most of which crashed into the planet. This left a large amount of ice to form the rings and some of the moons. This includes [[Enceladus (moon)|Enceladus]], which is thought to be made of ice.<ref name=cosmos />{{rp|61}} |
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===History=== |
=== History === |
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The rings were first |
The rings were first found by [[Galileo Galilei]] in 1610, using his telescope. They did not look like rings to Galileo. He called them "handles". He thought that Saturn was three different planets that were right next to each other. In 1612, when the rings were facing edge on with the Earth, the rings disappeared, then reappeared again in 1613, further confusing Galileo.<ref name="history_of_the_rings">{{cite web |url=http://www2.jpl.nasa.gov/saturn/back.html |title=Historical background of Saturn's rings |first=Ron |last=Baalke |work=www2.jpl.nasa.gov |publisher=National Aeronautics and Space Administration |year=2005 |access-date=July 6, 2011 |archive-date=March 21, 2009 |archive-url=https://web.archive.org/web/20090321071339/http://www2.jpl.nasa.gov/saturn/back.html |url-status=dead }}</ref> In 1655, [[Christiaan Huygens]] was the first person to say that Saturn was surrounded by rings. Using a much more powerful telescope than Galilei's, he said that Saturn "is surrounded by a thin, flat, ring, nowhere touching...".<ref name="history_of_the_rings" /> In 1675, [[Giovanni Domenico Cassini]] found that the planet's rings were in fact made of smaller rings with gaps. The largest ring gap was later named the [[Rings of Saturn|Cassini Division]]. In 1859, [[James Clerk Maxwell]] showed that the rings cannot be solid, but are made of small particles, each orbiting Saturn on their own. Otherwise, it would become unstable or break apart.<ref>{{cite web |url=http://www-history.mcs.st-andrews.ac.uk/~history/Extras/Maxwell_Saturn.html |title=James Clerk Maxwell on the nature of Saturn's rings |first=James Clerk |last=Maxwell |work=www-history.mcs.st-andrews.ac.uk |year=1859 |access-date=June 19, 2011}}</ref> [[James Keeler]] studied the rings using a [[spectrometer|spectroscope]] in 1895 which proved Maxwell's theory.<ref>{{cite web |url=http://www.sil.si.edu/DigitalCollections/HST/Huygens/huygens-introduction.htm |title=Christiaan Huygens and his Systema Saturnium |author=Brashear, Ronald |date=May 1999 |publisher= [[Smithsonian Institution]] Libraries|access-date=April 19, 2011}}</ref> |
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===Physical features=== |
=== Physical features === |
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The rings range from {{convert|6630|km|mi|0|lk=off|abbr=on}} to {{convert|120700|km|mi|0|lk=off|abbr=on}} above the planet's equator. As proved by Maxwell, even though the rings appear to be solid and unbroken when viewed from above, the rings are made of small particles of rock and ice. They are only about {{convert|10|m|ft|0|lk=off|abbr=on}} thick; made of [[silicon dioxide|silica]] rock, [[iron oxide]] and ice particles.<ref name=cosmos/>{{rp|55}} The smallest particles are only specks of dust while the largest are the size of a house. The C and D rings also seem to have a "wave" in them, like waves in water.<ref name=cosmos/>{{rp|58}} These large waves are {{convert|500|m|ft|0|lk=off|abbr=on}} high, but only moving slowly at about {{convert|250|m|ft|0|lk=off|abbr=on}} each day.<ref name=cosmos/>{{rp|58}} Some scientists believe that the wave is caused by Saturn's moons.<ref>{{cite web |url= |
The rings range from {{convert|6630|km|mi|0|lk=off|abbr=on}} to {{convert|120700|km|mi|0|lk=off|abbr=on}} above the planet's equator. While the equatorial circumference of Saturn is 378,675 km (235,298 miles). As proved by Maxwell, even though the rings appear to be solid and unbroken when viewed from above, the rings are made of small particles of rock and ice. They are only about {{convert|10|m|ft|0|lk=off|abbr=on}} thick; made of [[silicon dioxide|silica]] rock, [[iron oxide]] and ice particles.<ref name=cosmos />{{rp|55}} The smallest particles are only specks of dust while the largest are the size of a house. The C and D rings also seem to have a "wave" in them, like waves in water.<ref name=cosmos />{{rp|58}} These large waves are {{convert|500|m|ft|0|lk=off|abbr=on}} high, but only moving slowly at about {{convert|250|m|ft|0|lk=off|abbr=on}} each day.<ref name=cosmos />{{rp|58}} Some scientists believe that the wave is caused by Saturn's moons.<ref>{{cite web |url=http://solarsystem.nasa.gov/planets/profile.cfm?Object=Saturn&Display=Rings |title=Saturn: Rings |work=Solar System exploration| publisher=National Aeronautics and Space Administration |date=2011-03-22 |access-date=June 19, 2011}}</ref> Another idea is the waves were made by a [[comet]] hitting Saturn in 1983 or 1984.<ref name=cosmos />{{rp|60}} |
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The largest gaps in the rings are the Cassini Division and the [[Rings of Saturn|Encke Division]], both visible from the [[Earth]]. The Cassini Division is the largest, measuring {{convert|4800|km|mi|0|lk=off|abbr=on}} wide.<ref name="Cassini_Division">{{cite web |url= |
The largest gaps in the rings are the Cassini Division and the [[Rings of Saturn|Encke Division]], both visible from the [[Earth]]. The Cassini Division is the largest, measuring {{convert|4800|km|mi|0|lk=off|abbr=on}} wide.<ref name="Cassini_Division">{{cite web |url=http://starchild.gsfc.nasa.gov/docs/StarChild/solar_system_level2/cassini_division.html |title=StarChild: Saturn's Cassini Division |work=The Solar System| publisher= National Aeronautics and Space Administration |year=2011 |access-date=June 19, 2011}}</ref> However, when the Voyager spacecrafts visited Saturn in 1980, they discovered that the rings are a complex structure, made out of thousands of thin gaps and ringlets. Scientists believe this is caused by the [[gravity|gravitational force]] of some of Saturn's moons. The tiny moon [[Pan (moon)|Pan]] orbits inside Saturn's rings, creating a gap within the rings. Other ringlets keep their structure due to the gravitational force of [[shepherd satellite]]s, such as [[Prometheus (moon)|Prometheus]] and [[Pandora (moon)|Pandora]]. Other gaps form due to the gravitational force of a large moon farther away. The moon [[Mimas (moon)|Mimas]] is responsible for clearing away the Cassini gap.<ref name="Cassini_Division" /> |
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Recent data from the Cassini spacecraft has shown that the rings have their own atmosphere, free from the planet's atmosphere. The rings' atmosphere is made of oxygen gas, and it is produced when the Sun's [[ultraviolet]] light breaks up the water ice in the rings. [[Chemical reaction]] also |
Recent data from the Cassini spacecraft has shown that the rings have their own atmosphere, free from the planet's atmosphere. The rings' atmosphere is made of oxygen gas, and it is produced when the Sun's [[ultraviolet]] light breaks up the water ice in the rings. [[Chemical reaction|Chemical reactions]] also occur between the ultraviolet light and the water [[molecule]]s, creating hydrogen gas. The oxygen and hydrogen atmospheres around the rings are very widely spaced.<ref>{{cite news |url=http://news.bbc.co.uk/2/hi/science/nature/4640641.stm |title=Saturn rings have own atmosphere |first=Paul |last=Rincon |work=[[BBC News]] |date=July 1, 2005 |publisher=[[BBC]] |location=London |access-date=June 19, 2011}}</ref> As well as oxygen and hydrogen gas, the rings have a thin atmosphere made of [[hydroxide]] (a combination of oxygen and hydrogen called an anion), which was discovered by the Hubble Space Telescope.<ref>{{cite journal |url=http://adsabs.harvard.edu/cgi-bin/nph-bib_query?bibcode=2006ApJ...644L.137J&db_key=AST&data_type=HTML&format=&high=42bf06f4d906731%20The%20Enceladus%20and%20OH%20Tori%20at%20Saturn |title=The Enceladus and OH Tori at Saturn |first= R.E.|last=Johnson |journal=SAO/NASA ADS Astronomy Abstract Service |year=2006 |volume=644 |issue=2 |pages=L137–L139 |doi=10.1086/505750 |bibcode=2006ApJ...644L.137J |s2cid=37698445 |access-date=June 19, 2011}}</ref> |
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===Spokes=== |
=== Spokes === |
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[[File:Voyager |
[[File:Voyager 2 - Saturn Rings - 3085 7800 2.png|thumb|right|alt=The spokes in Saturn's rings|The spokes in Saturn's rings, photographed by Voyager 2]] |
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The Voyager space probe discovered features shaped like [[ray]]s, called ''spokes''.<ref name=malik>{{cite web |url= http://www.space.com/1554-cassini-probe-spies-spokes-saturn-rings.html |title=Cassini Probe spies spokes in Saturn's rings |first=Tariq |last=Malik |work=space.com |year=2005-09-15 |accessdate=2011-04-26}}</ref> These were also seen later by the Hubble telescope. The Cassini probe [[photograph]]ed the spokes in 2005.<ref name=malik/> They are seen as dark when under sunlight, and appear light when against the unlit side. At first it was thought the spokes were made of microscopic dust particles but new evidence shows that they are made of ice.<ref>{{cite web |url= http://www.nasa.gov/mission_pages/cassini/media/cassini-070204.html |title=Cassini exposes puzzles about ingredients in Saturn's rings |work=Cassini: unlocking Saturn's secrets| publisher= National Aeronautics and Space Administration |year=2009-06-02 |accessdate=2011-05-24}}</ref> |
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They rotate at the same time with the planet's [[magnetosphere]], therefore, it is believed that they have a connection with [[electromagnetism]]. However, what cause the spokes to form is still unknown. They appear to be [[season]]al, disappearing during solstice and appearing again during [[equinox]].<ref>{{cite web |url= http://apod.nasa.gov/apod/ap090602.html |title=Spoke's reappear on Saturn's rings |work=Astronomy Picture Of The Day| publisher=National Aeronautics and Space Administration |year=2009-06-02 |accessdate=2011-04-26}}</ref> |
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The Voyager space probe discovered features shaped like [[ray]]s, called spokes.<ref name=malik>{{cite web |url=http://www.space.com/1554-cassini-probe-spies-spokes-saturn-rings.html |title=Cassini Probe spies spokes in Saturn's rings |first=Tariq |last=Malik |work=space.com |date=2005-09-15 |access-date=April 26, 2011}}</ref> These were also seen later by the Hubble telescope. The Cassini probe [[photograph]]ed the spokes in 2005.<ref name=malik /> They appear dark when lit by sunlight, and appear light against the unlit side of the planet. At first it was thought the spokes were made of microscopic dust particles, but new evidence shows that they are made of ice.<ref>{{cite web |url=http://www.nasa.gov/mission_pages/cassini/media/cassini-070204.html |title=Cassini exposes puzzles about ingredients in Saturn's rings |work=Cassini: unlocking Saturn's secrets |publisher=National Aeronautics and Space Administration |date=2009-06-02 |access-date=May 24, 2011 |archive-date=2010-12-24 |archive-url=https://web.archive.org/web/20101224112125/http://www.nasa.gov/mission_pages/cassini/media/cassini-070204.html |url-status=dead }}</ref> |
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==Moons== |
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They rotate at the same rate as the planet's [[magnetosphere]], therefore, it is believed that they have a connection with [[electromagnetism]]. However, what causes the spokes to form is still unknown. They appear to be [[season]]al, disappearing during [[solstice]] and appearing again during [[equinox]].<ref>{{cite web |url=http://apod.nasa.gov/apod/ap090602.html |title=Spoke's reappear on Saturn's rings |work=Astronomy Picture Of The Day| publisher=National Aeronautics and Space Administration |date=2009-06-02 |access-date=April 26, 2011}}</ref> |
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[[File:Huygens on Titan.jpg|thumb|alt=Round space probe sitting on rocky ground| Drawing of Huygens on Titan]] |
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Saturn has [[List of Saturn's moons|53 named moons]], and another nine which are still being studied.<ref>{{cite web |url= http://solarsystem.nasa.gov/planets/profile.cfm?Object=Saturn&Display=Moons |title=Saturn: Moons |first= |last= |work=Solar System exploration: planets |publisher=National Aeronautics and Space Administration |year=2011 |accessdate=2011-04-21}}</ref> Many of the moons are very small: 33 are less than {{convert|10|km|mi|0|lk=off|abbr=on}} in diameter and 13 moons are less than {{convert|50|km|mi|0|lk=off|abbr=on}}.<ref>{{cite web |url= http://saturn.jpl.nasa.gov/science/moons/ |title=About Saturn and its moons |work=Cassini Solstice Mission| publisher= National Aeronautics and Space Administration |year=2011 |accessdate=2011-06-25}}</ref> Seven moons are large enough to be a near perfect [[sphere]] caused by their own [[gravity|gravitation]]. These moons are Titan, [[Rhea (moon)|Rhea]], [[Iapetus (moon)|Iapetus]], [[Dione (moon)|Dione]], [[Tethys (moon)|Tethys]], [[Enceladus (moon)|Enceladus]] and Mimas.<ref name="SpaceStottCarole">{{cite book |last=Stott |first=Carole||coauthors= Robert Dinwiddle, David Hughes, Giles Sparrow|title=Space|url=http://books.google.com/books?id=PA0Zj07An30C&source=gbs_navlinks_s|publisher=DK Books|year=2010|isbn=978-0-7566-6738-2|page=161|accessdate=2011-06-20}}</ref> Titan is the largest moon, larger than the planet Mercury, and it is the only moon in the Solar System to have a thick, dense atmosphere.<ref>{{cite web |url= http://www.astrobio.net/index.php?option=com_retrospection&task=detail&id=1755 |title=Titan: a moon with atmosphere |first=Chris |last=McKay |work=Astrobiology Magazine |year=2005-10-27 |accessdate=2011-06-20}}</ref><ref name=Zubrin> |
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{{cite book |author=Zubrin, Robert|title=Entering space: creating a spacefaring civilization |location=Section: Titan |pages=163–166 |publisher=Tarcher/Putnam |year=1999 |isbn=9781585420360}}</ref> [[Hyperion (moon)|Hyperion]] and [[Phoebe (moon)|Phoebe]] are the next largest moons, larger than {{convert|200|km|mi|0|lk=off|abbr=on}} in diameter. |
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== Moons == |
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In December 2004 and January 2005 a man-made satellite called the Cassini−Huygens probe took lots of close photos of Titan. One part of this satellite, known as the Huygens probe, then landed on Titan. Named after the Dutch astronomer Christiaan Huygens, it was the first spacecraft to land in the outer Solar System.<ref name="hug">{{cite web |url= http://solarsystem.nasa.gov/missions/profile.cfm?Sort=Target&Target=Saturn&MCode=Huygens |title=Huygens |work=Solar System exploration| publisher=National Aeronautics and Space Administration |year=2011 |accessdate=2011-04-22}}</ref> The probe was designed to float in case it landed in water.<ref name="hug"/> |
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Enceladus, the sixth largest moon, is about {{convert|500|km|mi|0|lk=off|abbr=on}} in diameter. It is one of the few outer solar system objects that shows [[volcano|volcanic]] activity.<ref name="lloyd">{{cite web |url= http://www.cosmosmagazine.com/news/4251/footprint-detected-one-saturns-moons |title=Footprint detected from one of Saturn's moons |first=James |last=Lloyd|work=cosmosmagazine.com |year=2011-04-21 |accessdate=2011-04-21}}</ref> In 2011, scientists discovered an electric link between Saturn and Enceladus. This is caused by [[ionization|ionised]] particles from volcanos on the small moon interacting with Saturn's magnetic fields.<ref name="lloyd"/> Similar interactions cause the [[aurora|northern lights]] on Earth.<ref>{{cite web |url= http://www.bbc.co.uk/news/science-environment-13131537 |title=Aurora from Saturn moon 'circuit' |first= |last= |work=BBC News |publisher=British Broadcasting Corporation |year=2011-04-21 |accessdate=2011-07-06}}</ref> |
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Saturn has a total of 146 moons; [[List of Saturn's moons|53 are named moons]], and another 29 are still being studied.<ref>{{cite web |url=http://solarsystem.nasa.gov/planets/profile.cfm?Object=Saturn&Display=Moons |title=Saturn: Moons |work=Solar System exploration: planets |publisher=National Aeronautics and Space Administration |year=2011 |access-date=April 21, 2011 |archive-date=March 16, 2011 |archive-url=https://web.archive.org/web/20110316014904/http://solarsystem.nasa.gov/planets/profile.cfm?Object=Saturn&Display=Moons |url-status=dead }}</ref> Many of the moons are very small: 33 are less than {{convert|10|km|mi|0|lk=off|abbr=on}} in diameter and 13 moons are less than {{convert|50|km|mi|0|lk=off|abbr=on}}.<ref>{{cite web |url=http://saturn.jpl.nasa.gov/science/moons/ |title=About Saturn and its moons |work=Cassini Solstice Mission| publisher= National Aeronautics and Space Administration |year=2011 |access-date=June 25, 2011}}</ref> Seven moons are large enough to be a near perfect [[sphere]] caused by their own [[gravity]]. These moons are [[Titan (moon)|Titan]], [[Rhea (moon)|Rhea]], [[Iapetus (moon)|Iapetus]], [[Dione (moon)|Dione]], [[Tethys (moon)|Tethys]], [[Enceladus (moon)|Enceladus]] and Mimas.<ref name="SpaceStottCarole">{{cite book |last= Stott |first=Carole |author2= Robert Dinwiddle, David Hughes and Giles Sparrow |title= Space |url=https://books.google.com/books?id=PA0Zj07An30C |publisher=DK Books |year=2010 |isbn=978-0-7566-6738-2 |page=161 |access-date= June 20, 2011}}</ref> Titan is the largest moon, larger than the planet Mercury, and it is the only moon in the Solar System to have a thick, dense atmosphere.<ref>{{cite web |url=http://www.astrobio.net/index.php?option=com_retrospection&task=detail&id=1755 |title=Titan: a moon with atmosphere |first=Chris |last=McKay |work=Astrobiology Magazine |date=2005-10-27 |access-date= June 20, 2011}}</ref><ref name=Zubrin>{{cite book |author=Zubrin, Robert |title= Entering space: creating a spacefaring civilization |url=https://archive.org/details/enteringspacecre0000zubr |location=Section: Titan |pages=[https://archive.org/details/enteringspacecre0000zubr/page/163 163]–166 |publisher=Tarcher/Putnam |year=1999 |isbn= 978-1-58542-036-0}}</ref> [[Hyperion (moon)|Hyperion]] and [[Phoebe (moon)|Phoebe]] are the next largest moons, larger than {{cvt|200|km|mi|0}} in diameter. |
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==Exploration== |
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Between December 2004 and January 2005 a man-made satellite called the Cassini−Huygens probe took lots of close photos of Titan. One part of this satellite, known as the Huygens probe, landed on Titan, on land. Named after the Dutch astronomer Christiaan Huygens, it was the first spacecraft to land in the outer Solar System.<ref name="hug">{{cite web |url=http://solarsystem.nasa.gov/missions/profile.cfm?Sort=Target&Target=Saturn&MCode=Huygens |title=Huygens |work=Solar System exploration |publisher=National Aeronautics and Space Administration |year=2011 |access-date=April 22, 2011 |archive-date=August 8, 2011 |archive-url=https://web.archive.org/web/20110808211722/http://solarsystem.nasa.gov/missions/profile.cfm?Sort=Target&Target=Saturn&MCode=Huygens |url-status=dead }}</ref> The probe was designed to float in case it landed in liquid.<ref name="hug" /> Its batteries lasted about 3 hours. Enceladus, the sixth largest moon, is about {{cvt|500|km|mi|0}} in diameter. It is one of the few outer solar system objects that shows [[volcano|volcanic]] activity.<ref name="lloyd">{{cite web |url=http://www.cosmosmagazine.com/news/4251/footprint-detected-one-saturns-moons |title=Footprint detected from one of Saturn's moons |first=James |last=Lloyd |work=cosmosmagazine.com |date=2011-04-21 |access-date=April 21, 2011 |archive-date=July 4, 2011 |archive-url=https://web.archive.org/web/20110704210340/http://www.cosmosmagazine.com/news/4251/footprint-detected-one-saturns-moons |url-status=dead }}</ref> In 2011, scientists discovered an electric link between Saturn and Enceladus. This is caused by [[ionization|ionised]] particles from volcanos on the small moon interacting with Saturn's magnetic fields.<ref name="lloyd" /> Similar interactions cause the [[aurora|northern lights]] on Earth.<ref>{{cite web |url=https://www.bbc.co.uk/news/science-environment-13131537 |title=Aurora from Saturn moon 'circuit' |work=BBC News |publisher=BBC |date=2011-04-21 |access-date=July 6, 2011}}</ref> |
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== Exploration == |
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[[File:Saturn from Cassini Orbiter (2007-01-19).jpg|thumbnail|right|alt=Saturn from Cassini orbiter|Saturn as seen from the Cassini spacecraft in 2007]] |
[[File:Saturn from Cassini Orbiter (2007-01-19).jpg|thumbnail|right|alt=Saturn from Cassini orbiter|Saturn as seen from the Cassini spacecraft in 2007]] |
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Saturn was first explored by the [[Pioneer 11]] spacecraft |
Saturn was first explored by the [[Pioneer 11]] spacecraft in September 1979. It flew as close as {{convert|20000|km|mi|0|lk=off|abbr=on}} above the planet's cloud tops. It took photographs of the planet and a few of its moons, but were low in [[wikt:resolution|resolution]]. It discovered a new, thin ring called the F ring. It also discovered that the dark ring gaps appear bright when viewed towards the [[Sun]], which shows the gaps are not empty. The spacecraft measured the temperature of the moon Titan.<ref>{{cite web |url=http://spaceprojects.arc.nasa.gov/Space_Projects/pioneer/PN10&11.html |title=The Pioneer 10 & 11 Spacecraft |archive-url=https://web.archive.org/web/20060130100401/http://spaceprojects.arc.nasa.gov/Space_Projects/pioneer/PN10%2611.html |publisher=Ames Research Center, NASA |date=October 8, 2005 |archive-date=January 30, 2006 |access-date=September 13, 2020 |url-status=dead }} Mission Descriptions. Retrieved July 5, 2007.</ref> |
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In November 1980, Voyager 1 visited Saturn |
In November 1980, Voyager 1 visited Saturn and took higher resolution photographs of the planet, rings, and moons. These photos showed some of the surface features of the moons. Voyager 1 went close to Titan and gained much information about its atmosphere. In August 1981, [[Voyager 2]] continued to study the planet. Photos taken by the space probe showed that changes were happening to the rings and atmosphere. The Voyager spacecraft discovered a number of moons orbiting close to Saturn's rings, as well as discovering new ring gaps. |
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[[File:Cassini Saturn Orbit Insertion.jpg|thumbnail|right| |
[[File:Cassini Saturn Orbit Insertion.jpg|thumbnail|right|Drawing of Cassini in orbit around Saturn]] |
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On July 1, 2004, the Cassini−Huygens probe entered into orbit around Saturn. Before then, it flew close to [[Phoebe (moon)|Phoebe]], taking very high resolution photos of its surface and collecting data. On December 25, 2004, the Huygens probe separated from the Cassini probe before moving down towards Titan's surface and landed there on January 14, 2005. It landed on a dry surface, but it found that large bodies of liquid exist on the moon. The Cassini probe continued to collect data from Titan and a number of the icy moons. It found evidence that the moon Enceladus had water erupting from its [[geyser]]s.<ref>{{cite web |url= http://science.nasa.gov/science-news/science-at-nasa/2006/09mar_enceladus/ |title=Radical! Liquid water on Enceladus |first= |last= |work=Science News|publisher=National Aeronautics and Space Administration |year=2006-03-09 |accessdate=2011-06-20}}</ref> Cassini also proved, in July 2006, that Titan had [[Lakes of Titan|hydrocarbon lake]]s, located near its north pole. In March 2007, it discovered a large hydrocarbon lake the size of the [[Caspian Sea]] near its north pole.<ref>{{cite news |url= http://news.bbc.co.uk/2/hi/science/nature/6449081.stm |title=Probe reveals seas on Saturn moon |first=Paul |last=Rincon|work=BBC News |date=2007-03-14 |publisher=British Broadcasting Corporation |location=London|accessdate=2011-06-20}}</ref> |
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On July 1, 2004, the Cassini−Huygens probe entered into orbit around Saturn. Before then, it flew close to [[Phoebe (moon)|Phoebe]], taking very high-resolution photos of its surface and collecting data. On December 25, 2004, the Huygens probe separated from the Cassini probe before moving towards Titan's surface and landed on January 14, 2005. It landed on a dry surface, but it found that large bodies of liquid exist on the moon. The Cassini probe continued to collect data from Titan and a number of the icy moons. It found evidence that the moon Enceladus had water erupting from its [[geyser]]s.<ref>{{cite web |url=http://science.nasa.gov/science-news/science-at-nasa/2006/09mar_enceladus/ |title=Radical! Liquid water on Enceladus |work=Science News |publisher=National Aeronautics and Space Administration |date=2006-03-09 |access-date=June 20, 2011 |archive-date=2011-06-23 |archive-url=https://web.archive.org/web/20110623093434/http://science.nasa.gov/science-news/science-at-nasa/2006/09mar_enceladus/ |url-status=dead }}</ref> Cassini also proved, in July 2006, that Titan had [[Lakes of Titan|hydrocarbon lakes]], located near its north pole. In March 2007, it discovered a large hydrocarbon lake the size of the [[Caspian Sea]] near its north pole.<ref>{{cite news |url=http://news.bbc.co.uk/2/hi/science/nature/6449081.stm |title=Probe reveals seas on Saturn moon |first=Paul |last=Rincon|work=BBC News |date=March 14, 2007 |publisher=BBC |location=London|access-date=June 20, 2011}}</ref> |
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Cassini observed [[lightning]] occurring in Saturn since early 2005. The power of the lightning was measured to be 1,000 times more powerful than lightning on Earth. Astronomers believe that the lightning observed in Saturn is the strongest ever seen.<ref>{{cite web |url= http://www.sciencedaily.com/releases/2006/02/060215090726.htm |title=Astronomers find giant lightning storm at Saturn |first= |last= |work=sciencedaily.com |year=2006-02-15 |accessdate=2011-06-20}}</ref> |
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Cassini observed [[lightning]] occurring in Saturn since early 2005. The power of the lightning was measured to be 1,000 times more powerful than lightning on Earth. Astronomers believe that the lightning observed in Saturn is the strongest ever seen.<ref>{{cite web |url=http://www.sciencedaily.com/releases/2006/02/060215090726.htm |title=Astronomers find giant lightning storm at Saturn |work=sciencedaily.com |date=2006-02-15 |access-date=June 20, 2011}}</ref> |
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==Notes== |
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== Notes == |
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*{{note label|1bar|a|a}}Refers to the level of one bar [[atmospheric pressure]] |
*{{note label|1bar|a|a}}Refers to the level of one bar [[atmospheric pressure]] |
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*{{note label|B_Center|b|b}}Orbital information is based on the [[barycentre]] of the Saturn system, the centre of [[mass]], not the [[geometry|geometric centre]]. Barycentre measurements are used because they are not changed by the daily movement of the moons.<ref>{{cite |
*{{note label|B_Center|b|b}}Orbital information is based on the [[barycentre]] of the Saturn system, the centre of [[mass]], not the [[geometry|geometric centre]]. Barycentre measurements are used because they are not changed by the daily movement of the moons.<ref>{{cite book |
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|first1=James H. |
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|last1=Shirley |
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|first2=Rhodes W. |
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|last2=Fairbridge |
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|date=1997 |
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|title=Encyclopedia of Planetary Sciences |
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|publisher=Springer |
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|location=New York |
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|page=62 |
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|url=https://books.google.com/books?id=dw2GadaPkYcC&dq=Barycenter&pg=PA62 |
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|isbn=978-0-412-06951-2}}</ref> |
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==Related pages== |
== Related pages == |
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* [[List of planets]] |
* [[List of planets]] |
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==References== |
== References == |
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{{reflist |
{{reflist |
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| refs = |
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<ref name="CSeligman">{{cite web |url=http://cseligman.com/text/sky/rotationvsday.htm |title=Rotation Period and Day Length |last=Seligman |first=Courtney |access-date=13 August 2009 |archive-url=https://web.archive.org/web/20110728200555/http://cseligman.com/text/sky/rotationvsday.htm |archive-date=28 July 2011 |url-status=live }}</ref> |
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==Other websites== |
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{{commonscat|Saturn (planet)}} |
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{{sisterlinks|Saturn}} |
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* {{cite web |url= http://www.spacetelescope.org/images/?search=SATURN |title=Images of Saturn |work=spacetelescope.org |year=2011 |accessdate=2011-06-19}} |
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* {{cite web |url= http://nssdc.gsfc.nasa.gov/planetary/factsheet/saturnfact.html |title=Saturn Earth comparison |work=Saturn fact Sheet| publisher=National Aeronautics and Space Administration |year=2011 |accessdate=2011-06-19}} |
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* {{cite web |url= http://www.affs.org/html/studies_on_the_rings_of_saturn.html |title=Studies on the Rings of Saturn |last=Vladimir V. Tchernyi, Andrew Ju. Pospelov, Serge V. Girich |work=The Academy for Future Science |year=2009 |accessdate=2011-06-19}} Theoretical description of the rings of Saturn |
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*{{cite web |url= http://www.nasa.gov/mission_pages/cassini/multimedia/pia07966.html |title=Eerie sounds of Saturn's radio emissions |first= |last= |work=Cassini: unlocking Saturn's secrets|publisher=National Aeronautics and Space Administration |year=2008 |accessdate=2011-06-19}} A [[WAV]] file of radio emissions from Saturn |
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* {{cite web |url= http://www.jpl.nasa.gov/news/news.cfm?release=2007-034 |title=Bizarre hexagon on Saturn |first= |last= |work=News and Features| publisher=National Aeronautics and Space Administration |year=2011 |accessdate=2011-06-19}} |
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<ref name=Souami_Souchay_2012>{{cite journal |
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{{Solar System}} |
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| title=The solar system's invariable plane |
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| last1=Souami | first1=D. | last2=Souchay | first2=J. |
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| journal=Astronomy & Astrophysics |
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| volume=543 | id=A133 | pages=11 | date=July 2012 |
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| doi=10.1051/0004-6361/201219011 | bibcode=2012A&A...543A.133S | doi-access=free }}</ref> |
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<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 |url-status=dead }}</ref> |
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[[Category:Planets]] |
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[[Category:Gas giants]] |
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[[Category:Solar System]] |
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<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 |url-status=dead }}</ref> |
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{{Link FA|af}} |
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{{Link FA|cs}} |
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<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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{{Link FA|de}} |
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{{Link FA|en}} |
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<ref name=VSOP87>{{cite journal |title=Numerical expressions for precession formulae and mean elements for the Moon and planets |journal=Astronomy and Astrophysics |volume=282 |issue=2 |pages=663–683 |date=February 1994 |last1=Simon |first1=J.L. |last2=Bretagnon |first2=P. |last3=Chapront |first3=J. |last4=Chapront-Touzé |first4=M. |last5=Francou |first5=G. |last6=Laskar |first6=J. |bibcode=1994A&A...282..663S}}</ref> |
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{{Link FA|es}} |
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{{Link FA|hr}} |
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<ref Name="Mallama_and_Hilton">{{cite journal |author=Mallama, A. |author2=Hilton, J.L. |title=Computing Apparent Planetary Magnitudes for The Astronomical Almanac |journal=Astronomy and Computing |volume=25 | pages=10–24 |date=2018 |doi=10.1016/j.ascom.2018.08.002 |bibcode=2018A&C....25...10M|arxiv=1808.01973 |s2cid=69912809 }}</ref> |
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{{Link FA|id}} |
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{{Link FA|sk}} |
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<ref name="Hanel_et_al">{{cite journal |title=Albedo, internal heat flux, and energy balance of Saturn |first1=R.A. |last1=Hanel |display-authors=etal |journal=Icarus |volume=53 |issue=2 |pages=262–285 |date=1983 |doi=10.1016/0019-1035(83)90147-1 |bibcode=1983Icar...53..262H }}</ref> |
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{{Link FA|ar}} |
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{{Link FA|ca}} |
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<ref name="Mallama_et_al">{{cite journal |title=Comprehensive wide-band magnitudes and albedos for the planets, with applications to exo-planets and Planet Nine |journal=Icarus |first1=Anthony |last1=Mallama |first2=Bruce |last2=Krobusek |first3=Hristo |last3=Pavlov |volume=282 |pages=19–33 |date=2017 |doi=10.1016/j.icarus.2016.09.023 |bibcode=2017Icar..282...19M |arxiv=1609.05048 |s2cid=119307693 }}</ref> |
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{{Link FA|pl}} |
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}} |
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'''Notes''' |
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{{Reflist|group=lower-alpha}} |
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== Further reading == |
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{{sisterlinks|Saturn|commonscat=yes|commons=Saturn (planet)}} |
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* {{cite web |url=http://www.spacetelescope.org/images/?search=SATURN |title=Images of Saturn |work=spacetelescope.org |year=2011 |access-date=June 19, 2011 |archive-date=August 9, 2011 |archive-url=https://web.archive.org/web/20110809042235/http://www.spacetelescope.org/images/?search=SATURN |url-status=dead }} |
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* {{cite web |url=http://nssdc.gsfc.nasa.gov/planetary/factsheet/saturnfact.html |title=Saturn Earth comparison |work=Saturn fact Sheet| publisher=NASA |year=2011 |access-date=June 19, 2011}} |
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* {{cite web |url=http://www.affs.org/html/studies_on_the_rings_of_saturn.html |title=Studies on the Rings of Saturn |last=Vladimir V. Tchernyi, Andrew Ju. Pospelov, Serge V. Girich |work=The Academy for Future Science |year=2009 |access-date=June 19, 2011 |archive-date=June 11, 2016 |archive-url=https://web.archive.org/web/20160611212635/http://www.affs.org/html/studies_on_the_rings_of_saturn.html |url-status=dead }} Theoretical description of the rings of Saturn. |
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*{{cite web |url=http://www.nasa.gov/mission_pages/cassini/multimedia/pia07966.html |title=Eerie sounds of Saturn's radio emissions |work=Cassini: unlocking Saturn's secrets |publisher=NASA |year=2008 |access-date=June 19, 2011 |archive-date=March 28, 2023 |archive-url=https://web.archive.org/web/20230328102645/https://www.nasa.gov/mission_pages/cassini/multimedia/pia07966.html |url-status=dead }} A [[WAV]] file of radio emissions from Saturn. |
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* {{cite web |url=http://www.jpl.nasa.gov/news/news.cfm?release=2007-034 |title=Bizarre hexagon on Saturn |work=News and Features |publisher=NASA |year=2011 |access-date=June 19, 2011 |archive-date=December 16, 2009 |archive-url=https://web.archive.org/web/20091216231717/http://www.jpl.nasa.gov/news/news.cfm?release=2007-034 |url-status=dead }} |
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{{Solar System}} |
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Latest revision as of 15:01, 24 September 2024
Designations | |||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Pronunciation | /ˈsætərn/ (listen)[1] | ||||||||||||
Named after | Saturn | ||||||||||||
Adjectives | Saturnian /səˈtɜːrniən/,[2] Cronian[3] / Kronian[4] /ˈkroʊniən/[5] | ||||||||||||
Orbital characteristics[10] | |||||||||||||
Epoch J2000.0 | |||||||||||||
Aphelion | 1,514.50 million km (10.1238 AU) | ||||||||||||
Perihelion | 1,352.55 million km (9.0412 AU) | ||||||||||||
1,433.53 million km (9.5826 AU) | |||||||||||||
Eccentricity | 0.0565 | ||||||||||||
| |||||||||||||
378.09 days | |||||||||||||
Average orbital speed | 9.68 km/s (6.01 mi/s) | ||||||||||||
317.020°[7] | |||||||||||||
Inclination | |||||||||||||
113.665° | |||||||||||||
2032-Nov-29[9] | |||||||||||||
339.392°[7] | |||||||||||||
Known satellites | 145 in total moonlets.[10] | ||||||||||||
Physical characteristics[10] | |||||||||||||
Mean radius | 58,232 km (36,184 mi)[a] | ||||||||||||
Equatorial radius |
| ||||||||||||
Polar radius |
| ||||||||||||
Flattening | 0.09796 | ||||||||||||
Circumference |
| ||||||||||||
Volume |
| ||||||||||||
Mass |
| ||||||||||||
Mean density | 0.687 g/cm3 (0.0248 lb/cu in)[b] (less than water) | ||||||||||||
0.22[13] | |||||||||||||
35.5 km/s (22.1 mi/s)[a] | |||||||||||||
10 h 32 m 36 s (synodic; solar day)[6] | |||||||||||||
Sidereal rotation period | 10h 33m 38s + 1m 52s − 1m 19s [14][15] | ||||||||||||
Equatorial rotation velocity | 9.87 km/s (6.13 mi/s; 35,500 km/h)[a] | ||||||||||||
26.73° (to orbit) | |||||||||||||
North pole right ascension | 40.589°; 2h 42m 21s | ||||||||||||
North pole declination | 83.537° | ||||||||||||
Albedo | |||||||||||||
| |||||||||||||
−0.55[18] to +1.17[18] | |||||||||||||
14.5″ to 20.1″ (excludes rings) | |||||||||||||
Atmosphere[10] | |||||||||||||
Surface pressure | 140 kPa[21] | ||||||||||||
59.5 km (37.0 mi) | |||||||||||||
Composition by volume |
| ||||||||||||
Saturn is the sixth planet from the Sun in the Solar System. Saturn takes about 29.5 Earth years to complete one orbit around the Sun. A day on Saturn is much shorter than an Earth day, lasting only about 10.7 hours. This means that Saturn spins much faster than Earth, completing more than two rotations in the same time it takes Earth to complete just one. [22]
Saturn is one of the four giant planets in the Solar System, with Jupiter, Uranus, and Neptune. It is the second largest planet in the Solar System (Jupiter is the largest).[23]
Saturn was named after the Roman god Saturn. He was the Roman equivalent of the Greek god Kronos.[24] Saturn's symbol is ♄ which is the symbol of Saturnus' sickle.[25]
Inside Saturn is probably a core of iron, nickel, silicon and oxygen compounds, surrounded by a deep layer of metallic hydrogen, then a layer of liquid hydrogen and liquid helium and finally, an outer gaseous layer.[26]
Saturn has 146 known moons orbiting the planet.[27] The largest moon is Titan. Titan is larger in volume than the planet Mercury. It is the second-largest moon in the Solar System. The largest moon is a moon of Jupiter, Ganymede. There are also many rings around Saturn. These rings are made of ice with some rocks and dust. Some people think that that the rings were made by a moon impact or other event. Saturn is about 1,433,000,000 km (870,000,000 mi) on average from the Sun. Saturn takes 29.4 Earth years in order to complete a revolution around the Sun.[28]
Physical features
[change | change source]Saturn is a squished sphere. This means that it is flattened at the poles and wider around the equator.[29] The planet's equatorial diameter is 120,536 km (74,898 mi). Its polar diameter (the distance from the north pole to the south pole through the centre) is 108,728 km (67,560 mi). This is a 9% difference.[30] Saturn has a flattened shape because of its very fast rotation. It rotates once every 10.8 Earth hours.
Saturn is the only planet in the Solar System that is less dense than water. Even though the planet's core is very dense, it has a gaseous atmosphere. This makes its average density is 0.69 g/cm3. This means if Saturn could be placed in a large pool of water, it would float.[31]
Atmosphere
[change | change source]The outer part of Saturn's atmosphere is made up of about 96% hydrogen, 3% helium, 0.4% methane and 0.01% ammonia. There are also some acetylene, ethane and phosphine.[32]
Saturn's clouds show a banded pattern. This is like the cloud bands seen on Jupiter. Saturn's clouds are much fainter and the bands are wider at the equator. Saturn's lowest cloud layer is made up of water ice. It is about 10 km (6 mi) thick.[32] The temperature there is quite low, at 250 K (-10°F, -23°C). However, scientists do not all agree on this. The layer above is made up of ammonium hydrosulfide ice. It is about 77 km (48 mi) thick. Above it is a layer of ammonia ice clouds which are 80 km (50 mi) thick.[32] The highest layer is made up of hydrogen and helium gases. It goes to between 200 km (124 mi) and 270 km (168 mi) above the water cloud tops. Auroras can be seen in Saturn in the mesosphere.[32] The temperature at Saturn's cloud tops is very low, at 98 K (-283 °F, -175 °C). The temperatures in the inner layers are much higher than the outside layers because of the heat made by Saturn's inside.[33] Saturn's winds are some of the fastest in the Solar System. They can reach 1,800 km/h (1,118 mph),[34] ten times faster than winds on Earth.[35]
Storms and spots
[change | change source]Saturn's atmosphere can make oval shaped clouds. They are like the clearer spots seen on Jupiter. These oval spots are cyclonic storms, similar to cyclones seen on Earth. In 1990, the Hubble Space Telescope found a very large white cloud near Saturn's equator. Storms like this one in 1990 were known as Great White Spots. These unique storms only exist for a short time and only occur in about every 30 Earth years, in summer solstices in the Northern Hemisphere.[36] Great White Spots were also found in 1876, 1903, 1933, and 1960.
The Voyager 1 spacecraft found a hexagonal cloud pattern near Saturn's north pole at about 78°N. The Cassini−Huygens probe later confirmed it in 2006. Unlike the north pole, the south pole does not show any hexagonal clouds. The probe also found a hurricane-like storm on the south pole that showed an eyewall. Until this finding, eyewalls had only been seen on Earth.[37]
Interior
[change | change source]Saturn's inside is similar to Jupiter's inside. It has a small rocky core about the size of the Earth at its center.[29] It is very hot. Its temperature reaches 15,000 K (26,540 °F (14,727 °C)). Saturn is so hot that it gives out more heat energy into space than it gets from the Sun.[33] Above it is a thicker layer of metallic hydrogen, about 30,000 km (18,641 mi) deep. Above that layer is a region of liquid hydrogen and helium.[38] The core is heavy, with about 9 to 22 times more mass than the Earth's core.[39]
Magnetic field
[change | change source]Saturn has a natural magnetic field that is weaker than Jupiter's. Like the Earth's, Saturn's field is a magnetic dipole (it has a North and a South). Saturn's field is unique in that it is perfectly symmetrical, unlike any other known planet.[40] This means the field is exactly in line with the planet's axis.[40] Saturn generates radio waves, but they are too weak to be detected from Earth.[41] The moon Titan orbits in the outer part of Saturn's magnetic field and gives out plasma to the field from the ionised particles in Titan's atmosphere.[42]
Rotation and orbit
[change | change source]Saturn's average distance from the Sun is over 1,400,000,000 km (886,000,000 mi). This is about nine times the distance from the Earth to the Sun. It takes 10,756 days, or about 29.4 years, for Saturn to orbit around the Sun.[43] This is known as Saturn's orbital period.
Voyager 1 measured Saturn's rotation as being 10 hours, 14 minutes at the equator, 10 hours, 40 minutes closer to the poles, and 10 hours, 39 minutes, 24 seconds for the planet's inside.[44] This is known as its rotational period.
Cassini measured the rotation of Saturn as being 10 hours, 45 minutes, 45 seconds ± 36 seconds.[45] That is about six minutes longer than the radio rotational period measured by the Voyager 1 and Voyager 2 spacecrafts, which flew by Saturn in 1980 and 1981.
Saturn's rotational period is calculated by the rotation speed of radio waves given off by the planet. The Cassini−Huygens spacecraft found that the radio waves slowed down. This suggested that the rotational period increased.[45] Since scientists do not think Saturn's rotation is actually slowing down, the explanation may be that the magnetic field causes the radio waves.[45]
Planetary rings
[change | change source]Saturn is best known for its planetary rings which are easy to see with a telescope. There are seven named rings: A, B, C, D, E, F, and G.[46] They were named in the order they were found, which is different to their order from the planet. From the planet the rings are ordered: D, C, B, A, F, G and E.[46]: 57
Some scientists think that the rings are material left after a moon broke apart.[46]: 60 A new idea says that it was a very large moon, most of which crashed into the planet. This left a large amount of ice to form the rings and some of the moons. This includes Enceladus, which is thought to be made of ice.[46]: 61
History
[change | change source]The rings were first found by Galileo Galilei in 1610, using his telescope. They did not look like rings to Galileo. He called them "handles". He thought that Saturn was three different planets that were right next to each other. In 1612, when the rings were facing edge on with the Earth, the rings disappeared, then reappeared again in 1613, further confusing Galileo.[47] In 1655, Christiaan Huygens was the first person to say that Saturn was surrounded by rings. Using a much more powerful telescope than Galilei's, he said that Saturn "is surrounded by a thin, flat, ring, nowhere touching...".[47] In 1675, Giovanni Domenico Cassini found that the planet's rings were in fact made of smaller rings with gaps. The largest ring gap was later named the Cassini Division. In 1859, James Clerk Maxwell showed that the rings cannot be solid, but are made of small particles, each orbiting Saturn on their own. Otherwise, it would become unstable or break apart.[48] James Keeler studied the rings using a spectroscope in 1895 which proved Maxwell's theory.[49]
Physical features
[change | change source]The rings range from 6,630 km (4,120 mi) to 120,700 km (75,000 mi) above the planet's equator. While the equatorial circumference of Saturn is 378,675 km (235,298 miles). As proved by Maxwell, even though the rings appear to be solid and unbroken when viewed from above, the rings are made of small particles of rock and ice. They are only about 10 m (33 ft) thick; made of silica rock, iron oxide and ice particles.[46]: 55 The smallest particles are only specks of dust while the largest are the size of a house. The C and D rings also seem to have a "wave" in them, like waves in water.[46]: 58 These large waves are 500 m (1,640 ft) high, but only moving slowly at about 250 m (820 ft) each day.[46]: 58 Some scientists believe that the wave is caused by Saturn's moons.[50] Another idea is the waves were made by a comet hitting Saturn in 1983 or 1984.[46]: 60
The largest gaps in the rings are the Cassini Division and the Encke Division, both visible from the Earth. The Cassini Division is the largest, measuring 4,800 km (2,983 mi) wide.[51] However, when the Voyager spacecrafts visited Saturn in 1980, they discovered that the rings are a complex structure, made out of thousands of thin gaps and ringlets. Scientists believe this is caused by the gravitational force of some of Saturn's moons. The tiny moon Pan orbits inside Saturn's rings, creating a gap within the rings. Other ringlets keep their structure due to the gravitational force of shepherd satellites, such as Prometheus and Pandora. Other gaps form due to the gravitational force of a large moon farther away. The moon Mimas is responsible for clearing away the Cassini gap.[51]
Recent data from the Cassini spacecraft has shown that the rings have their own atmosphere, free from the planet's atmosphere. The rings' atmosphere is made of oxygen gas, and it is produced when the Sun's ultraviolet light breaks up the water ice in the rings. Chemical reactions also occur between the ultraviolet light and the water molecules, creating hydrogen gas. The oxygen and hydrogen atmospheres around the rings are very widely spaced.[52] As well as oxygen and hydrogen gas, the rings have a thin atmosphere made of hydroxide (a combination of oxygen and hydrogen called an anion), which was discovered by the Hubble Space Telescope.[53]
Spokes
[change | change source]The Voyager space probe discovered features shaped like rays, called spokes.[54] These were also seen later by the Hubble telescope. The Cassini probe photographed the spokes in 2005.[54] They appear dark when lit by sunlight, and appear light against the unlit side of the planet. At first it was thought the spokes were made of microscopic dust particles, but new evidence shows that they are made of ice.[55] They rotate at the same rate as the planet's magnetosphere, therefore, it is believed that they have a connection with electromagnetism. However, what causes the spokes to form is still unknown. They appear to be seasonal, disappearing during solstice and appearing again during equinox.[56]
Moons
[change | change source]Saturn has a total of 146 moons; 53 are named moons, and another 29 are still being studied.[57] Many of the moons are very small: 33 are less than 10 km (6 mi) in diameter and 13 moons are less than 50 km (31 mi).[58] Seven moons are large enough to be a near perfect sphere caused by their own gravity. These moons are Titan, Rhea, Iapetus, Dione, Tethys, Enceladus and Mimas.[59] Titan is the largest moon, larger than the planet Mercury, and it is the only moon in the Solar System to have a thick, dense atmosphere.[60][61] Hyperion and Phoebe are the next largest moons, larger than 200 km (124 mi) in diameter.
Between December 2004 and January 2005 a man-made satellite called the Cassini−Huygens probe took lots of close photos of Titan. One part of this satellite, known as the Huygens probe, landed on Titan, on land. Named after the Dutch astronomer Christiaan Huygens, it was the first spacecraft to land in the outer Solar System.[62] The probe was designed to float in case it landed in liquid.[62] Its batteries lasted about 3 hours. Enceladus, the sixth largest moon, is about 500 km (311 mi) in diameter. It is one of the few outer solar system objects that shows volcanic activity.[63] In 2011, scientists discovered an electric link between Saturn and Enceladus. This is caused by ionised particles from volcanos on the small moon interacting with Saturn's magnetic fields.[63] Similar interactions cause the northern lights on Earth.[64]
Exploration
[change | change source]Saturn was first explored by the Pioneer 11 spacecraft in September 1979. It flew as close as 20,000 km (12,427 mi) above the planet's cloud tops. It took photographs of the planet and a few of its moons, but were low in resolution. It discovered a new, thin ring called the F ring. It also discovered that the dark ring gaps appear bright when viewed towards the Sun, which shows the gaps are not empty. The spacecraft measured the temperature of the moon Titan.[65]
In November 1980, Voyager 1 visited Saturn and took higher resolution photographs of the planet, rings, and moons. These photos showed some of the surface features of the moons. Voyager 1 went close to Titan and gained much information about its atmosphere. In August 1981, Voyager 2 continued to study the planet. Photos taken by the space probe showed that changes were happening to the rings and atmosphere. The Voyager spacecraft discovered a number of moons orbiting close to Saturn's rings, as well as discovering new ring gaps.
On July 1, 2004, the Cassini−Huygens probe entered into orbit around Saturn. Before then, it flew close to Phoebe, taking very high-resolution photos of its surface and collecting data. On December 25, 2004, the Huygens probe separated from the Cassini probe before moving towards Titan's surface and landed on January 14, 2005. It landed on a dry surface, but it found that large bodies of liquid exist on the moon. The Cassini probe continued to collect data from Titan and a number of the icy moons. It found evidence that the moon Enceladus had water erupting from its geysers.[66] Cassini also proved, in July 2006, that Titan had hydrocarbon lakes, located near its north pole. In March 2007, it discovered a large hydrocarbon lake the size of the Caspian Sea near its north pole.[67]
Cassini observed lightning occurring in Saturn since early 2005. The power of the lightning was measured to be 1,000 times more powerful than lightning on Earth. Astronomers believe that the lightning observed in Saturn is the strongest ever seen.[68]
Notes
[change | change source]- a Refers to the level of one bar atmospheric pressure
- b Orbital information is based on the barycentre of the Saturn system, the centre of mass, not the geometric centre. Barycentre measurements are used because they are not changed by the daily movement of the moons.[69]
Related pages
[change | change source]References
[change | change source]- ↑ Walter, Elizabeth (21 April 2003). Cambridge Advanced Learner's Dictionary (Second ed.). Cambridge University Press. ISBN 978-0-521-53106-1.
- ↑ "Saturnian". Oxford English Dictionary. Oxford University Press. 2nd ed. 1989.
- ↑ "Enabling Exploration with Small Radioisotope Power Systems" (PDF). NASA. September 2004. Archived from the original (PDF) on 22 December 2016. Retrieved 26 January 2016.
- ↑ Müller; et al. (2010). "Azimuthal plasma flow in the Kronian magnetosphere". Journal of Geophysical Research. 115 (A8): A08203. Bibcode:2010JGRA..115.8203M. doi:10.1029/2009ja015122. ISSN 0148-0227.
- ↑ "Cronian". Oxford English Dictionary. Oxford University Press. 2nd ed. 1989.
- ↑ 6.0 6.1 Seligman, Courtney. "Rotation Period and Day Length". Archived from the original on 28 July 2011. Retrieved 13 August 2009.
- ↑ 7.0 7.1 7.2 7.3 Simon, J.L.; Bretagnon, P.; Chapront, J.; Chapront-Touzé, M.; Francou, G.; Laskar, J. (February 1994). "Numerical expressions for precession formulae and mean elements for the Moon and planets". Astronomy and Astrophysics. 282 (2): 663–683. Bibcode:1994A&A...282..663S.
- ↑ Souami, D.; Souchay, J. (July 2012). "The solar system's invariable plane". Astronomy & Astrophysics. 543: 11. Bibcode:2012A&A...543A.133S. doi:10.1051/0004-6361/201219011. A133.
- ↑ "HORIZONS Web-Interface". ssd.jpl.nasa.gov.
- ↑ 10.0 10.1 10.2 10.3 Williams, David R. (23 December 2016). "Saturn Fact Sheet". NASA. Archived from the original on 17 July 2017. Retrieved 12 October 2017.
- ↑ "By the Numbers – Saturn". NASA Solar System Exploration. NASA. Retrieved 5 August 2020.
- ↑ "NASA: Solar System Exploration: Planets: Saturn: Facts & Figures". Solarsystem.nasa.gov. 22 March 2011. Archived from the original on 2 September 2011. Retrieved 8 August 2011.
- ↑ Fortney, J.J.; Helled, R.; Nettlemann, N.; Stevenson, D.J.; Marley, M.S.; Hubbard, W.B.; Iess, L. (6 December 2018). "The Interior of Saturn". In Baines, K.H.; Flasar, F.M.; Krupp, N.; Stallard, T. (eds.). Saturn in the 21st Century. Cambridge University Press. pp. 44–68. ISBN 978-1-108-68393-7.
- ↑ McCartney, Gretchen; Wendel, JoAnna (18 January 2019). "Scientists Finally Know What Time It Is on Saturn". NASA. Archived from the original on 29 August 2019. Retrieved 18 January 2019.
- ↑ Mankovich, Christopher; et al. (17 January 2019). "Cassini Ring Seismology as a Probe of Saturn's Interior. I. Rigid Rotation". The Astrophysical Journal. 871 (1): 1. arXiv:1805.10286. Bibcode:2019ApJ...871....1M. doi:10.3847/1538-4357/aaf798. S2CID 67840660.
- ↑ Hanel, R.A.; et al. (1983). "Albedo, internal heat flux, and energy balance of Saturn". Icarus. 53 (2): 262–285. Bibcode:1983Icar...53..262H. doi:10.1016/0019-1035(83)90147-1.
- ↑ Mallama, Anthony; Krobusek, Bruce; Pavlov, Hristo (2017). "Comprehensive wide-band magnitudes and albedos for the planets, with applications to exo-planets and Planet Nine". Icarus. 282: 19–33. arXiv:1609.05048. Bibcode:2017Icar..282...19M. doi:10.1016/j.icarus.2016.09.023. S2CID 119307693.
- ↑ 18.0 18.1 Mallama, A.; Hilton, J.L. (2018). "Computing Apparent Planetary Magnitudes for The Astronomical Almanac". Astronomy and Computing. 25: 10–24. arXiv:1808.01973. Bibcode:2018A&C....25...10M. doi:10.1016/j.ascom.2018.08.002. S2CID 69912809.
- ↑ 19.0 19.1 "Saturn's Temperature Ranges". Sciencing.
- ↑ "The Planet Saturn". National Weather Service.
- ↑ Knecht, Robin (24 October 2005). "On The Atmospheres Of Different Planets" (PDF). Archived from the original (PDF) on 14 October 2017. Retrieved 14 October 2017.
- ↑ "Saturn: Facts - NASA Science". science.nasa.gov. Retrieved 2024-07-08.
- ↑ "Saturn: Facts". NASA. Retrieved 9 November 2023.
- ↑ "Cronia (Kronia)". Holidays, Festivals, and Celebrations of the World Dictionary. 2010. Retrieved July 11, 2011.
- ↑ Crystal, Ellie. "Saturn Mythology". Crystalinks.com. Retrieved February 28, 2007.
- ↑ Brainerd, Jerome James 2004. "Giant gaseous planets". The Astrophysics Spectator. Retrieved July 5, 2010.
{{cite web}}
: CS1 maint: numeric names: authors list (link) - ↑ "Planetary Satellite Discovery Circumstances". NASA. Retrieved December 28, 2019.
- ↑ "Saturn: Facts - NASA Science". science.nasa.gov. Retrieved 2024-01-11.
- ↑ 29.0 29.1 "Saturn". Information Leaflet No. 42. Royal Greenwich Observatory. 2009. Retrieved April 26, 2011.
- ↑ "Cassini–Huygens Saturn arrival" (PDF). Press kit June 2004. National Aeronautics and Space Administration. p. 9. Retrieved June 25, 2011.
- ↑ Verba, Joan Marie (1991). Voyager: Exploring the outer planets. FTL Publications. p. 20. ISBN 0-9825232-0-3.
- ↑ 32.0 32.1 32.2 32.3 "Saturn". MIRA: field trips to the stars: the Solar System. Monterey Institute of Research in Astronomy. 2006. Retrieved June 19, 2011.
- ↑ 33.0 33.1 "A gas giant with super-fast winds". Cassini: unlocking Saturn's secrets. National Aeronautics and Space Administration. 2007. Archived from the original on March 4, 2011. Retrieved June 19, 2011.
- ↑ Wilkinson, John (2009). Probing the new solar system. CSIRO Publishing. p. 208. ISBN 978-0-643-09575-5. Retrieved May 23, 2011.
- ↑ Sullivant, Rosemary. "Saturn's storms run rings around Earth's". Cassini: unlocking Saturn's secrets. National Aeronautics and Space Administration. Archived from the original on June 6, 2011. Retrieved May 24, 2011.
- ↑ S. Pérez-Hoyos, A. Sánchez-Lavega, R.G. French, J.F. Rojas. (2005). "Saturn's cloud structure and temporal evolution from ten years of Hubble Space Telescope images (1994–2003)". Icarus. 176 (1): 155–174. Bibcode:2005Icar..176..155P. doi:10.1016/j.icarus.2005.01.014. Retrieved June 19, 2011.
{{cite journal}}
: CS1 maint: multiple names: authors list (link) - ↑ McKee, Maggie (2006-11-06). "Spectacular storm rages on Saturn's south pole". New Scientist Magazine. Retrieved April 21, 2011.
- ↑ "Saturn". Solar System. National Maritime Museum. 2005-10-04. Archived from the original on June 13, 2011. Retrieved June 19, 2011.
- ↑ Fortney, Jonathon J. (2004). "Looking into the giant planets". Science 305 (5689): 1414–1415. Retrieved April 30, 2007.
- ↑ 40.0 40.1 Sutton, Christine (1981-08-27). "Saturn yields to Voyager's brief caress". New Scientist Magazine. Retrieved June 19, 2011.[permanent dead link]
- ↑ Smith, A. G.; Carr, T. D. (1959). "Radio-Frequency Observations of the Planets in 1957–1958". The Astrophysical Journal. 130: 641–647. Bibcode:1959ApJ...130..641S. doi:10.1086/146753.
- ↑ Russell C.T.; Luhmann J.G. (1997). "Saturn: magnetic field and magnetosphere". Encyclopedia of Planetary Sciences. New York: Chapman and Hall. pp. 718–719. Archived from the original on October 5, 2011. Retrieved June 20, 2011.
{{cite encyclopedia}}
: CS1 maint: multiple names: authors list (link) - ↑ "Saturn: Facts - NASA Science". science.nasa.gov. Retrieved 2024-01-11.
- ↑ "Saturn: orbital and rotational information". MIRA: field trips to the stars: the Solar System. Monterey Institute for Research in Astronomy. 2006. Retrieved July 6, 2011.
- ↑ 45.0 45.1 45.2 Martinez, Carolina (2004-06-28). "Scientists find that Saturn's rotation period is a puzzle". Cassini: unlocking Saturn's secrets. National Aeronautics and Space Administration. Archived from the original on 2011-08-29. Retrieved June 24, 2011.
- ↑ 46.0 46.1 46.2 46.3 46.4 46.5 46.6 46.7 Lovett, Rick (June 2011). "Dance of the rings". Cosmos (39): 57. Retrieved June 21, 2011.
- ↑ 47.0 47.1 Baalke, Ron (2005). "Historical background of Saturn's rings". www2.jpl.nasa.gov. National Aeronautics and Space Administration. Archived from the original on March 21, 2009. Retrieved July 6, 2011.
- ↑ Maxwell, James Clerk (1859). "James Clerk Maxwell on the nature of Saturn's rings". www-history.mcs.st-andrews.ac.uk. Retrieved June 19, 2011.
- ↑ Brashear, Ronald (May 1999). "Christiaan Huygens and his Systema Saturnium". Smithsonian Institution Libraries. Retrieved April 19, 2011.
- ↑ "Saturn: Rings". Solar System exploration. National Aeronautics and Space Administration. 2011-03-22. Retrieved June 19, 2011.
- ↑ 51.0 51.1 "StarChild: Saturn's Cassini Division". The Solar System. National Aeronautics and Space Administration. 2011. Retrieved June 19, 2011.
- ↑ Rincon, Paul (July 1, 2005). "Saturn rings have own atmosphere". BBC News. London: BBC. Retrieved June 19, 2011.
- ↑ Johnson, R.E. (2006). "The Enceladus and OH Tori at Saturn". SAO/NASA ADS Astronomy Abstract Service. 644 (2): L137–L139. Bibcode:2006ApJ...644L.137J. doi:10.1086/505750. S2CID 37698445. Retrieved June 19, 2011.
- ↑ 54.0 54.1 Malik, Tariq (2005-09-15). "Cassini Probe spies spokes in Saturn's rings". space.com. Retrieved April 26, 2011.
- ↑ "Cassini exposes puzzles about ingredients in Saturn's rings". Cassini: unlocking Saturn's secrets. National Aeronautics and Space Administration. 2009-06-02. Archived from the original on 2010-12-24. Retrieved May 24, 2011.
- ↑ "Spoke's reappear on Saturn's rings". Astronomy Picture Of The Day. National Aeronautics and Space Administration. 2009-06-02. Retrieved April 26, 2011.
- ↑ "Saturn: Moons". Solar System exploration: planets. National Aeronautics and Space Administration. 2011. Archived from the original on March 16, 2011. Retrieved April 21, 2011.
- ↑ "About Saturn and its moons". Cassini Solstice Mission. National Aeronautics and Space Administration. 2011. Retrieved June 25, 2011.
- ↑ Stott, Carole; Robert Dinwiddle, David Hughes and Giles Sparrow (2010). Space. DK Books. p. 161. ISBN 978-0-7566-6738-2. Retrieved June 20, 2011.
- ↑ McKay, Chris (2005-10-27). "Titan: a moon with atmosphere". Astrobiology Magazine. Retrieved June 20, 2011.
- ↑ Zubrin, Robert (1999). Entering space: creating a spacefaring civilization. Section: Titan: Tarcher/Putnam. pp. 163–166. ISBN 978-1-58542-036-0.
- ↑ 62.0 62.1 "Huygens". Solar System exploration. National Aeronautics and Space Administration. 2011. Archived from the original on August 8, 2011. Retrieved April 22, 2011.
- ↑ 63.0 63.1 Lloyd, James (2011-04-21). "Footprint detected from one of Saturn's moons". cosmosmagazine.com. Archived from the original on July 4, 2011. Retrieved April 21, 2011.
- ↑ "Aurora from Saturn moon 'circuit'". BBC News. BBC. 2011-04-21. Retrieved July 6, 2011.
- ↑ "The Pioneer 10 & 11 Spacecraft". Ames Research Center, NASA. October 8, 2005. Archived from the original on January 30, 2006. Retrieved September 13, 2020. Mission Descriptions. Retrieved July 5, 2007.
- ↑ "Radical! Liquid water on Enceladus". Science News. National Aeronautics and Space Administration. 2006-03-09. Archived from the original on 2011-06-23. Retrieved June 20, 2011.
- ↑ Rincon, Paul (March 14, 2007). "Probe reveals seas on Saturn moon". BBC News. London: BBC. Retrieved June 20, 2011.
- ↑ "Astronomers find giant lightning storm at Saturn". sciencedaily.com. 2006-02-15. Retrieved June 20, 2011.
- ↑ Shirley, James H.; Fairbridge, Rhodes W. (1997). Encyclopedia of Planetary Sciences. New York: Springer. p. 62. ISBN 978-0-412-06951-2.
Notes
Further reading
[change | change source]Definitions from Wiktionary | |
Media from Commons | |
News stories from Wikinews | |
Quotations from Wikiquote | |
Source texts from Wikisource | |
Textbooks from Wikibooks | |
Learning resources from Wikiversity |
- "Images of Saturn". spacetelescope.org. 2011. Archived from the original on August 9, 2011. Retrieved June 19, 2011.
- "Saturn Earth comparison". Saturn fact Sheet. NASA. 2011. Retrieved June 19, 2011.
- Vladimir V. Tchernyi, Andrew Ju. Pospelov, Serge V. Girich (2009). "Studies on the Rings of Saturn". The Academy for Future Science. Archived from the original on June 11, 2016. Retrieved June 19, 2011.
{{cite web}}
: CS1 maint: multiple names: authors list (link) Theoretical description of the rings of Saturn. - "Eerie sounds of Saturn's radio emissions". Cassini: unlocking Saturn's secrets. NASA. 2008. Archived from the original on March 28, 2023. Retrieved June 19, 2011. A WAV file of radio emissions from Saturn.
- "Bizarre hexagon on Saturn". News and Features. NASA. 2011. Archived from the original on December 16, 2009. Retrieved June 19, 2011.