Moons of Jupiter

A montage of Jupiter and its four largest moons (distance and sizes not to scale)

There are 79 known moons of Jupiter, not counting a number of moonlets likely shed from the inner moons, and S/2003 J 24, whose orbital elements have not yet been published.^[1][2][3] All together, they form a satellite system which is called the Jovian system. The most massive of the moons are the four Galilean moons: Io; Europa; Ganymede; and Callisto, which were independently discovered in 1610 by Galileo Galilei and Simon Marius and were the first objects found to orbit a body that was neither Earth nor the Sun. Much more recently, beginning in 1892, dozens of far smaller Jovian moons have been detected and have received the names of lovers (or other sexual partners) or daughters of the Roman god Jupiter or his Greek equivalent Zeus. The Galilean moons are by far the largest and most massive objects to orbit Jupiter, with the remaining 75 known moons and the rings together composing just 0.003% of the total orbiting mass.

Of Jupiter's moons, eight are regular satellites with prograde and nearly circular orbits that are not greatly inclined with respect to Jupiter's equatorial plane. The Galilean satellites are nearly spherical in shape due to their planetary mass, and so would be considered at least dwarf planets if they were in direct orbit around the Sun. The other four regular satellites are much smaller and closer to Jupiter; these serve as sources of the dust that makes up Jupiter's rings. The remainder of Jupiter's moons are irregular satellites whose prograde and retrograde orbits are much farther from Jupiter and have high inclinations and eccentricities. These moons were probably captured by Jupiter from solar orbits. Twenty-two of the irregular satellites have not yet been officially named.

Characteristics[]

The Galilean moons. From left to right, in order of increasing distance from Jupiter: Io; Europa; Ganymede; Callisto.

The physical and orbital characteristics of the moons vary widely. The four Galileans are all over 3,100 kilometres (1,900 mi) in diameter; the largest Galilean, Ganymede, is the ninth largest object in the Solar System, after the Sun and seven of the planets, Ganymede being larger than Mercury. All other Jovian moons are less than 250 kilometres (160 mi) in diameter, with most barely exceeding 5 kilometres (3.1 mi).^{[note 1]} Their orbital shapes range from nearly perfectly circular to highly eccentric and inclined, and many revolve in the direction opposite to Jupiter's rotation (retrograde motion). Orbital periods range from seven hours (taking less time than Jupiter does to rotate around its axis), to some three thousand times more (almost three Earth years).

Origin and evolution[]

The relative masses of the Jovian moons. Those smaller than Europa are not visible at this scale, and combined would only be visible at 100× magnification.

Jupiter's regular satellites are believed to have formed from a circumplanetary disk, a ring of accreting gas and solid debris analogous to a protoplanetary disk.^[4][5] They may be the remnants of a score of Galilean-mass satellites that formed early in Jupiter's history.^[4][6]

Simulations suggest that, while the disk had a relatively high mass at any given moment, over time a substantial fraction (several tens of a percent) of the mass of Jupiter captured from the solar nebula was passed through it. However, only 2% of the proto-disk mass of Jupiter is required to explain the existing satellites.^[4] Thus, several generations of Galilean-mass satellites may have been in Jupiter's early history. Each generation of moons might have spiraled into Jupiter, because of drag from the disk, with new moons then forming from the new debris captured from the solar nebula.^[4] By the time the present (possibly fifth) generation formed, the disk had thinned so that it no longer greatly interfered with the moons' orbits.^[6] The current Galilean moons were still affected, falling into and being partially protected by an orbital resonance with each other, which still exists for Io, Europa, and Ganymede. Ganymede's larger mass means that it would have migrated inward at a faster rate than Europa or Io.^[4]

The outer, irregular moons are thought to have originated from captured asteroids, whereas the protolunar disk was still massive enough to absorb much of their momentum and thus capture them into orbit. Many are believed to have broken up by mechanical stresses during capture, or afterward by collisions with other small bodies, producing the moons we see today.^[7]

Discovery[]

Jupiter and the Galilean moons through a 25 cm (10 in) Meade LX200 telescope.

The number of moons known for each of the four outer planets up to October 2019. Jupiter currently has 79 known satellites.

Chinese historian Xi Zezong claimed that the earliest record of a Jovian moon (Ganymede or Callisto) was a note by Chinese astronomer Gan De of an observation around 364 BC regarding a "reddish star".^[8] However, the first certain observations of Jupiter's satellites were those of Galileo Galilei in 1609.^[9] By January 1610, he had sighted the four massive Galilean moons with his 20× magnification telescope, and he published his results in March 1610.^[10]

Simon Marius had independently discovered the moons one day after Galileo, although he did not publish his book on the subject until 1614. Even so, the names Marius assigned are used today: Ganymede, Callisto, Io, and Europa.^[11] No additional satellites were discovered until E. E. Barnard observed Amalthea in 1892.^[12]

With the aid of telescopic photography, further discoveries followed quickly over the course of the 20th century. Himalia was discovered in 1904,^[13] Elara in 1905,^[14] Pasiphae in 1908,^[15] Sinope in 1914,^[16] Lysithea and Carme in 1938,^[17] Ananke in 1951,^[18] and Leda in 1974.^[19] By the time that the Voyager space probes reached Jupiter, around 1979, 13 moons had been discovered, not including Themisto, which had been observed in 1975,^[20] but was lost until 2000 due to insufficient initial observation data. The Voyager spacecraft discovered an additional three inner moons in 1979: Metis, Adrastea, and Thebe.^[21]

No additional moons were discovered for two decades, but between October 1999 and February 2003, researchers found another 34 moons using sensitive ground-based detectors.^[22] These are tiny moons, in long, eccentric, generally retrograde orbits, and averaging 3 km (1.9 mi) in diameter, with the largest being just 9 km (5.6 mi) across. All of these moons are thought to have been captured asteroidal or perhaps comet bodies, possibly fragmented into several pieces.^[23][24]

By 2015, a total of 15 additional moons were discovered.^[24] Two more were discovered in 2016 by the team led by Scott S. Sheppard at the Carnegie Institution for Science, bringing the total to 69.^[25] On 17 July 2018, the International Astronomical Union confirmed that Sheppard's team had discovered ten more moons around Jupiter, bringing the total number to 79.^[2] Among these is Valetudo, which has a prograde orbit, but crosses paths with several moons that have retrograde orbits, making an eventual collision—at some point on a billions-of-years timescale—likely.^[2]

In September 2020, researchers from the University of British Columbia identified 45 candidate moons from an analysis of archival images taken in 2010 by the Canada-France-Hawaii Telescope.^[26] These candidates were mainly small and faint, down to a magnitude of 25.7 or over 800 m (0.50 mi) in diameter. From the number of candidate moons detected within a sky area of one square degree, the team extrapolated that the population of retrograde Jovian moons brighter than magnitude 25.7 is around 600, within a factor of 2.^[27] Although the team considers their characterised candidates to be likely moons of Jupiter, they all remain unconfirmed due to their insufficient observation data for determining reliable orbits for each of them.^[26]

Naming[]

Galilean moons around Jupiter   Jupiter ·   Io ·   Europa ·   Ganymede ·   Callisto

Orbits of Jupiter's inner moons within its rings

The Galilean moons of Jupiter (Io, Europa, Ganymede, and Callisto) were named by Simon Marius soon after their discovery in 1610.^[28] However, these names fell out of favor until the 20th century. The astronomical literature instead simply referred to "Jupiter I", "Jupiter II", etc., or "the first satellite of Jupiter", "Jupiter's second satellite", and so on.^[28] The names Io, Europa, Ganymede, and Callisto became popular in the mid-20th century,^[29] whereas the rest of the moons remained unnamed and were usually numbered in Roman numerals V (5) to XII (12).^[30][31] Jupiter V was discovered in 1892 and given the name Amalthea by a popular though unofficial convention, a name first used by French astronomer Camille Flammarion.^[22][32]

The other moons were simply labeled by their Roman numeral (e.g. Jupiter IX) in the majority of astronomical literature until the 1970s.^[33] Several different suggestions were made for names of Jupiter's outer satellites, but none were universally accepted until 1975 when the International Astronomical Union's (IAU) Task Group for Outer Solar System Nomenclature granted names to satellites V–XIII,^[34] and provided for a formal naming process for future satellites still to be discovered.^[34] The practice was to name newly discovered moons of Jupiter after lovers and favorites of the god Jupiter (Zeus) and, since 2004, also after their descendants.^[22] All of Jupiter's satellites from XXXIV (Euporie) onward are named after descendants of Jupiter or Zeus,^[22] except LIII (Dia), named after a lover of Jupiter. Names ending with "a" or "o" are used for prograde irregular satellites (the latter for highly inclined satellites), and names ending with "e" are used for retrograde irregulars.^[35] With the discovery of smaller, kilometre-sized moons around Jupiter, the IAU has established an additional convention to limit the naming of small moons with absolute magnitudes greater than 18 or diameters smaller than 1 km (0.62 mi).^[36] Some of the most recently confirmed moons have not received names.

Some asteroids share the same names as moons of Jupiter: 9 Metis, 38 Leda, 52 Europa, 85 Io, 113 Amalthea, 239 Adrastea. Two more asteroids previously shared the names of Jovian moons until spelling differences were made permanent by the IAU: Ganymede and asteroid 1036 Ganymed; and Callisto and asteroid 204 Kallisto.

Groups[]

The orbits of Jupiter's irregular satellites, and how they cluster into groups: by semi-major axis (the horizontal axis in Gm); by orbital inclination (the vertical axis); and orbital eccentricity (the yellow lines). The relative sizes are indicated by the circles.

Regular satellites[]

These have prograde and nearly circular orbits of low inclination and are split into two groups:

• Inner satellites or Amalthea group: Metis, Adrastea, Amalthea, and Thebe. These orbit very close to Jupiter; the innermost two orbit in less than a Jovian day. The latter two are respectively the fifth and seventh largest moons in the Jovian system. Observations suggest that at least the largest member, Amalthea, did not form on its present orbit, but farther from the planet, or that it is a captured Solar System body.^[37] These moons, along with a number of seen and as-yet-unseen inner moonlets (see Amalthea moonlets), replenish and maintain Jupiter's faint ring system. Metis and Adrastea help to maintain Jupiter's main ring, whereas Amalthea and Thebe each maintain their own faint outer rings.^[38][39]
• Main group or Galilean moons: Io, Europa, Ganymede and Callisto. They are some of the largest objects in the Solar System outside the Sun and the eight planets in terms of mass and are larger than any known dwarf planet. Ganymede exceeds (and Callisto nearly equals) even the planet Mercury in diameter, though they are less massive. They are respectively the fourth-, sixth-, first-, and third-largest natural satellites in the Solar System, containing approximately 99.997% of the total mass in orbit around Jupiter, while Jupiter is almost 5,000 times more massive than the Galilean moons.^{[note 2]} The inner moons are in a 1:2:4 orbital resonance. Models suggest that they formed by slow accretion in the low-density Jovian subnebula—a disc of the gas and dust that existed around Jupiter after its formation—which lasted up to 10 million years in the case of Callisto.^[40] Several are suspected of having subsurface oceans.

Irregular satellites[]

Orbits and positions of Jupiter's irregular satellites as of 1 January 2021. Prograde orbits are colored blue while retrograde orbits are colored red.

Inclinations (°) vs. eccentricities of Jupiter's irregular satellites, with the major groups identified. Data as of 2021.

The irregular satellites are substantially smaller objects with more distant and eccentric orbits. They form families with shared similarities in orbit (semi-major axis, inclination, eccentricity) and composition; it is believed that these are at least partially collisional families that were created when larger (but still small) parent bodies were shattered by impacts from asteroids captured by Jupiter's gravitational field. These families bear the names of their largest members. The identification of satellite families is tentative, but the following are typically listed:^[1][41][42]

• Prograde satellites:
  • Themisto is the innermost irregular moon and is not part of a known family.^[1][41]
  • The Himalia group is spread over barely 1.4 Gm in semi-major axes, 1.6° in inclination (27.5 ± 0.8°), and eccentricities between 0.11 and 0.25. It has been suggested that the group could be a remnant of the break-up of an asteroid from the asteroid belt.^[41]
  • Carpo is another prograde moon and is not part of a known family. It has the highest inclination of all of the prograde moons.^[1]
  • Valetudo is the outermost prograde moon and is not part of a known family. Its prograde orbit crosses paths with several moons that have retrograde orbits and may in the future collide with them.^[2]
• Retrograde satellites:
  • The Carme group is spread over only 1.2 Gm in semi-major axis, 1.6° in inclination (165.7 ± 0.8°), and eccentricities between 0.23 and 0.27. It is very homogeneous in color (light red) and is believed to have originated from a D-type asteroid progenitor, possibly a Jupiter trojan.^[23]
  • The Ananke group has a relatively wider spread than the previous groups, over 2.4 Gm in semi-major axis, 8.1° in inclination (between 145.7° and 154.8°), and eccentricities between 0.02 and 0.28. Most of the members appear gray, and are believed to have formed from the breakup of a captured asteroid.^[23]
  • The Pasiphae group is quite dispersed, with a spread over 1.3 Gm, inclinations between 144.5° and 158.3°, and eccentricities between 0.25 and 0.43.^[23] The colors also vary significantly, from red to grey, which might be the result of multiple collisions. Sinope, sometimes included in the Pasiphae group,^[23] is red and, given the difference in inclination, it could have been captured independently;^[41] Pasiphae and Sinope are also trapped in secular resonances with Jupiter.^[43]

List[]

The moons of Jupiter are listed below by orbital period. Moons massive enough for their surfaces to have collapsed into a spheroid are highlighted in bold. These are the four Galilean moons, which are comparable in size to the Moon. The other moons are much smaller, with the least massive Galilean moon being more than 7,000 times more massive than the most massive of the other moons. The irregular captured moons are shaded light gray when prograde and dark gray when retrograde. The orbits and mean distances of the irregular moons are strongly variable over short timescales due to frequent planetary and solar perturbations,^[44] therefore the epochs of all orbital elements listed are based on the Julian date of 2459200.5, or 17 December 2020.^[45] As of 2021, S/2003 J 10 is the only moon of Jupiter considered lost due to its uncertain orbit.^[46] A number of other moons have only been observed for a year or two, but have decent enough orbits to be easily measurable at present.^[44]

Order [note 3]	Label [note 4]	Name	Pronunciation	Image	Abs. magn.	Diameter (km)[note 5]	Mass (×1016 kg)	Semi-major axis (km)[47]	Orbital period (d) [47][note 6]	Inclination (°)[47]	Eccentricity [1]	Discovery year[22]	Discoverer[22]	Group [note 7]
1	XVI	Metis	/ˈmiːtɪs/		10.5	43 (60 × 40 × 34)	≈ 3.6	128852	+0.2988 (+7h 10m 16s)	2.226	0.0077	1979	Synnott (Voyager 1)	Inner
2	XV	Adrastea	/ædrəˈstiːə/		12.0	16.4 (20 × 16 × 14)	≈ 0.2	129000	+0.3023 (+7h 15m 21s)	2.217	0.0063	1979	Jewitt (Voyager 2)	Inner
3	V	Amalthea	/æməlˈθiːə/[48]		7.1	167 (250 × 146 × 128)	208	181366	+0.5012 (+12h 01m 46s)	2.565	0.0075	1892	Barnard	Inner
4	XIV	Thebe	/ˈθiːbiː/		9.0	98.6 (116 × 98 × 84)	≈ 43	222452	+0.6778 (+16h 16m 02s)	2.909	0.0180	1979	Synnott (Voyager 1)	Inner
5	I	Io♠	/ˈaɪoʊ/		−1.7	3643.2 (3660 × 3637 × 3631)	8931900	421700	+1.7691	0.050[49]	0.0041	1610	Galilei	Galilean
6	II	Europa♠	/jʊəˈroʊpə/[50]		−1.4	3121.6	4800000	671034	+3.5512	0.471[49]	0.0094	1610	Galilei	Galilean
7	III	Ganymede♠	/ˈɡænɪmiːd/[51][52]		−2.1	5268.2	14819000	1070412	+7.1546	0.204[49]	0.0011	1610	Galilei	Galilean
8	IV	Callisto♠	/kəˈlɪstoʊ/		−1.2	4820.6	10759000	1882709	+16.689	0.205[49]	0.0074	1610	Galilei	Galilean
9	XVIII	Themisto†	/θɪˈmɪstoʊ/		12.9	9	≈ 0.069	7405000	+130.18	44.590	0.2514	1975/2000	Kowal & Roemer/ Sheppard et al.	Themisto
10	XIII	Leda♣	/ˈliːdə/		12.7	21.5	≈ 0.6	11196000	+242.02	27.641	0.1648	1974	Kowal	Himalia
11	LXXI	Ersa♣	/ˈɜːrsə/		15.9	3	≈ 0.0045	11348700	+246.99	31.028	0.1043	2018	Sheppard et al.	Himalia
12	LXV	Pandia♣	/pænˈdaɪə/		16.2	3	≈ 0.0045	11462300	+250.71	27.023	0.2084	2017	Sheppard et al.	Himalia
13	VI	Himalia♣	/hɪˈmeɪliə/		7.9	139.6 (150 × 120)	420	11497400	+251.86	30.214	0.1510	1904	Perrine	Himalia
14	X	Lysithea♣	/laɪˈsɪθiə/		11.2	42.2	≈ 6.3	11628300	+256.17	27.015	0.1377	1938	Nicholson	Himalia
15	VII	Elara♣	/ˈɛlərə/		9.6	79.9	≈ 87	11671600	+257.60	30.216	0.2079	1905	Perrine	Himalia
16	LIII	Dia♣	/ˈdaɪə/		16.3	4	≈ 0.009	12304900	+278.85	27.481	0.2606	2000	Sheppard et al.	Himalia
17	XLVI	Carpo†	/ˈkɑːrpoʊ/		16.1	3	≈ 0.0045	17151800	+458.90	50.138	0.4967	2003	Sheppard et al.	Carpo
18	LXII	Valetudo†	/vælɪˈtjuːdoʊ/		17.0	1	≈ 0.00015	18819000	+527.41	32.033	0.2018	2016	Sheppard et al.	Valetudo
19	XXXIV	Euporie♦	/ˈjuːpəriː/		16.3	2	≈ 0.0015	19593900	−560.32	147.851	0.1402	2001	Sheppard et al.	Ananke
20	LX	Eupheme♦	/juːˈfiːmiː/		16.6	2	≈ 0.0015	20126300	−583.31	150.042	0.4104	2003	Sheppard et al.	Ananke
21	LV	S/2003 J 18♦			16.5	2	≈ 0.0015	20348800	−593.01	142.783	0.0465	2003	Gladman et al.	Ananke
22	LII	S/2010 J 2♦			17.3	1	≈ 0.00015	20436700	−596.86	148.697	0.3403	2010	Veillet	Ananke
23	XLV	Helike♦	/ˈhɛlɪkiː/		16.0	4	≈ 0.009	20479500	−598.74	155.067	0.1331	2003	Sheppard et al.	Ananke
24		S/2003 J 16♦			16.3	2	≈ 0.0015	20512500	−600.18	151.163	0.3331	2003	Gladman et al.	Ananke
25		S/2003 J 2♦			16.7	2	≈ 0.0015	20554400	−602.02	149.204	0.2777	2003	Sheppard et al.	Ananke
26	XXXIII	Euanthe♦	/juːˈænθiː/		16.4	3	≈ 0.0045	20583300	−603.29	146.808	0.1096	2001	Sheppard et al.	Ananke
27	LXVIII	S/2017 J 7♦			16.6	2	≈ 0.0015	20600100	−604.03	146.739	0.2626	2017	Sheppard et al.	Ananke
28	XXX	Hermippe♦	/hərˈmɪpiː/		15.6	4	≈ 0.009	20666200	−606.94	146.753	0.1981	2001	Sheppard et al.	Ananke
29	XXVII	Praxidike♦	/prækˈsɪdɪkiː/		14.9	7	≈ 0.043	20682900	−607.68	149.692	0.2959	2000	Sheppard et al.	Ananke
30	XXIX	Thyone♦	/θaɪˈoʊniː/		15.8	4	≈ 0.009	20712800	−609.00	147.328	0.1770	2001	Sheppard et al.	Ananke
31	XLII	Thelxinoe♦	/θɛlkˈsɪnoʊiː/		16.3	2	≈ 0.0015	20893300	−616.97	146.916	0.1709	2003	Sheppard et al.	Ananke
32	LXIV	S/2017 J 3♦			16.5	2	≈ 0.0015	20976900	−620.68	147.968	0.1907	2017	Sheppard et al.	Ananke
33	XII	Ananke♦	/əˈnæŋkiː/		11.7	29.1	≈ 3.0	21042500	−623.59	148.675	0.1747	1951	Nicholson	Ananke
34	XL	Mneme♦	/ˈniːmiː/		16.3	2	≈ 0.0015	21064100	−624.55	151.087	0.3428	2003	Gladman et al.	Ananke
35	LIV	S/2016 J 1♦			16.8	1	≈ 0.00015	21154000	−628.56	143.824	0.1294	2016	Sheppard et al.	Ananke
36	XXXV	Orthosie♦	/ɔːrˈθoʊziː/		16.7	2	≈ 0.0015	21171000	−629.31	148.488	0.4838	2001	Sheppard et al.	Ananke
37	XXII	Harpalyke♦	/hɑːrˈpælɪkiː/		15.9	4	≈ 0.009	21280200	−634.19	148.298	0.1602	2000	Sheppard et al.	Ananke
38	XXIV	Iocaste♦	/aɪəˈkæstiː/		15.4	5	≈ 0.019	21431800	−640.98	149.424	0.3295	2000	Sheppard et al.	Ananke
39	LXX	S/2017 J 9♦			16.1	3	≈ 0.0045	21492900	−643.72	155.775	0.2524	2017	Sheppard et al.	Ananke
40		S/2003 J 12♦			17.0	1	≈ 0.00015	21557700	−646.64	154.690	0.3657	2003	Sheppard et al.	Ananke
41		S/2003 J 4‡			16.7	2	≈ 0.0015	22048600	−668.85	149.401	0.4967	2003	Sheppard et al.	Pasiphae
42	XXV	Erinome♥	/ɛˈrɪnəmiː/ (?)		16.0	3	≈ 0.0045	22354300	−682.80	164.821	0.2052	2000	Sheppard et al.	Carme
43	XXXI	Aitne♥	/ˈeɪtniː/		16.0	3	≈ 0.0045	22386500	−684.28	166.238	0.3150	2001	Sheppard et al.	Carme
44	L	Herse♥	/ˈhɜːrsiː/		16.5	2	≈ 0.0015	22408800	−685.30	164.347	0.1854	2003	Gladman et al.	Carme
45	XX	Taygete♥	/teɪˈɪdʒɪtiː/		15.5	5	≈ 0.016	22433500	−686.44	163.261	0.3257	2000	Sheppard et al.	Carme
46	LXIII	S/2017 J 2♥			16.4	2	≈ 0.0015	22472900	−688.25	165.676	0.3852	2017	Sheppard et al.	Carme
47	LXVII	S/2017 J 6‡			16.4	2	≈ 0.0015	22543800	−691.51	155.185	0.3226	2017	Sheppard et al.	Pasiphae
48	XLVII	Eukelade♥	/juːˈkɛlədiː/		15.9	4	≈ 0.009	22576700	−693.02	163.822	0.2790	2003	Sheppard et al.	Carme
49	XI	Carme♥	/ˈkɑːrmiː/		10.6	46.7	≈ 13	22579900	−693.17	163.535	0.2295	1938	Nicholson	Carme
50	LXI	S/2003 J 19♥			16.6	2	≈ 0.0015	22752500	−701.13	167.738	0.2928	2003	Gladman et al.	Carme
51	XXVI	Isonoe♥	/aɪˈsɒnoʊiː/		16.0	4	≈ 0.009	22776700	−702.25	162.834	0.2159	2000	Sheppard et al.	Carme
52	(lost)	S/2003 J 10♥			16.8	2	≈ 0.0015	22896200	−707.78	163.481	0.2066	2003	Sheppard et al.	Carme?
53	XXVIII	Autonoe‡	/ɔːˈtɒnoʊiː/		15.5	4	≈ 0.009	22933400	−709.51	148.145	0.4290	2001	Sheppard et al.	Pasiphae
54	LVIII	Philophrosyne‡	/fɪləˈfrɒzɪniː/		16.7	2	≈ 0.0015	22939900	−709.81	147.900	0.3013	2003	Sheppard et al.	Pasiphae
55	XLVIII	Cyllene‡	/sɪˈliːniː/		16.3	2	≈ 0.0015	22965200	−710.99	150.047	0.6079	2003	Sheppard et al.	Pasiphae
56	XXXVIII	Pasithee♥	/ˈpæsɪθiː/		16.8	2	≈ 0.0015	22967800	−711.11	164.727	0.2097	2001	Sheppard et al.	Carme
57	LI	S/2010 J 1♥			16.4	2	≈ 0.0015	22986900	−712.00	164.559	0.2937	2010	Jacobson et al.	Carme
58	VIII	Pasiphae‡	/pəˈsɪfeɪiː/		10.1	57.8	≈ 30	23119300	−718.16	151.998	0.4362	1908	Melotte	Pasiphae
59	XXXVI	Sponde‡	/ˈspɒndiː/		16.7	2	≈ 0.0015	23146500	−719.42	144.563	0.3455	2001	Sheppard et al.	Pasiphae
60	LXIX	S/2017 J 8♥			17.0	1	≈ 0.00015	23173700	−720.69	166.071	0.2039	2017	Sheppard et al.	Carme
61	XXXII	Eurydome‡	/jʊəˈrɪdəmiː/		16.2	3	≈ 0.0045	23214500	−722.59	150.289	0.2975	2001	Sheppard et al.	Pasiphae
62	LXVI	S/2017 J 5♥			16.5	2	≈ 0.0015	23352500	−729.05	166.555	0.2460	2017	Sheppard et al.	Carme
63	XXIII	Kalyke♥	/ˈkælɪkiː/		15.4	6.9	≈ 0.04	23377400	−730.21	166.899	0.2660	2000	Sheppard et al.	Carme
64	XXXIX	Hegemone‡	/hɪˈdʒɛməniː/		15.9	3	≈ 0.0045	23422300	−732.32	154.675	0.3358	2003	Sheppard et al.	Pasiphae
65	XXXVII	Kale♥	/ˈkeɪliː/		16.4	2	≈ 0.0015	23512200	−736.54	166.177	0.2893	2001	Sheppard et al.	Carme
66	XLIV	Kallichore♥	/kəˈlɪkəriː/		16.4	2	≈ 0.0015	23552900	−738.45	167.727	0.3183	2003	Sheppard et al.	Carme
67	LXXII	S/2011 J 1♥			16.7	2	≈ 0.0015	23714400	−746.06	164.799	0.3193	2011	Sheppard et al.	Carme
68	LIX	S/2017 J 1‡			16.6	2	≈ 0.0015	23753600	−747.91	147.253	0.4500	2017	Sheppard et al.	Pasiphae
69	XXI	Chaldene♥	/kælˈdiːniː/		16.0	4	≈ 0.009	23848300	−752.39	162.749	0.2705	2000	Sheppard et al.	Carme
70	XLIII	Arche♥	/ˈɑːrkiː/		16.2	3	≈ 0.0045	23926500	−756.09	166.408	0.2367	2002	Sheppard et al.	Carme
71	LVII	Eirene♥	/aɪˈriːniː/		15.8	4	≈ 0.009	23934500	−756.47	162.713	0.2413	2003	Sheppard et al.	Carme
72	XLIX	Kore‡	/ˈkɔːriː/		16.6	2	≈ 0.0015	23999700	−759.56	136.628	0.2347	2003	Sheppard et al.	Pasiphae
73	LVI	S/2011 J 2‡			16.8	1	≈ 0.00015	24114700	−765.03	152.125	0.1729	2011	Sheppard et al.	Pasiphae
74		S/2003 J 9♥			16.9	1	≈ 0.00015	24168700	−767.60	166.334	0.1702	2003	Sheppard et al.	Carme
75	XIX	Megaclite‡	/ˌmɛɡəˈklaɪtiː/		15.0	5	≈ 0.021	24212300	−769.68	145.574	0.3139	2000	Sheppard et al.	Pasiphae
76	XLI	Aoede‡	/eɪˈiːdiː/		15.6	4	≈ 0.009	24283000	−773.05	151.908	0.3131	2003	Sheppard et al.	Pasiphae
77		S/2003 J 23‡			16.6	2	≈ 0.0015	24678200	−792.00	146.155	0.3208	2003	Sheppard et al.	Pasiphae
78	XVII	Callirrhoe‡	/kəˈlɪroʊiː/		13.9	9.6	≈ 0.087	24692400	−792.69	149.792	0.3562	1999	Scotti et al.	Pasiphae
79	IX	Sinope‡	/sɪˈnoʊpiː/		11.1	35	≈ 7.5	24864100	−800.97	158.597	0.1669	1914	Nicholson	Pasiphae

Exploration[]

The orbit and motion of the Galilean moons around Jupiter, as captured by JunoCam aboard the Juno spacecraft.

The first spacecraft to visit Jupiter were Pioneer 10 in 1973, and Pioneer 11 a year later, taking low-resolution images of the four Galilean moons and returning data on their atmospheres and radiation belts.^[53] The Voyager 1 and Voyager 2 probes visited Jupiter in 1979, discovering the volcanic activity on Io and the presence of water ice on the surface of Europa. The Cassini probe to Saturn flew by Jupiter in 2000 and collected data on interactions of the Galilean moons with Jupiter's extended atmosphere. The New Horizons spacecraft flew by Jupiter in 2007 and made improved measurements of its satellites' orbital parameters.

The Galileo spacecraft was the first to enter orbit around Jupiter, arriving in 1995 and studying it until 2003. During this period, Galileo gathered a large amount of information about the Jovian system, making close approaches to all of the Galilean moons and finding evidence for thin atmospheres on three of them, as well as the possibility of liquid water beneath the surfaces of Europa, Ganymede, and Callisto. It also discovered a magnetic field around Ganymede.

Ganymede taken by Juno during its 34th perijove.

In 2016, the Juno spacecraft imaged the Galilean moons from above their orbital plane as it approached Jupiter orbit insertion, creating a time-lapse movie of their motion.^[54]

See also[]

• Jupiter's moons in fiction
• Satellite system (astronomy)

Notes[]

References[]

External links[]

Wikimedia Commons has media related to Moons of Jupiter.

• Jupiter's Known Satellites
• The Jupiter Satellite and Moon Page
• Jupiter Moons by NASA's Solar System Exploration
• Archive of Jupiter System Articles in Planetary Science Research Discoveries