Amalthea (moon)

Amalthea

Greyscale Galileo images of Amalthea
Discovery
Discovered by E. E. Barnard
Discovery date 9 September 1892
Designations
Adjectives Amalthean
Orbital characteristics
Periapsis 181150 km[lower-alpha 1]
Apoapsis 182840 km[lower-alpha 1]
Mean orbit radius
 181365.84±0.02 km (2.54 RJ)[1]
Eccentricity 0.00319±0.00004[1]
0.49817943±0.00000007 d (11 h, 57 min, 23 s)[1]
26.57 km/s[lower-alpha 1]
Inclination 0.374°±0.002° (to Jupiter's equator)[1]
Satellite of Jupiter
Physical characteristics
Dimensions 250 × 146 × 128 km[2]
Mean radius
 83.5±2.0 km[2]
Volume (2.43±0.22)×106 km3[3]
Mass (2.08±0.15)×1018 kg[3]
Mean density
 0.857±0.099 g/cm3[3]
≈ 0.020 m/s2 (≈ 0.002 g)[lower-alpha 1]
≈ 0.058 km/s[lower-alpha 1]
synchronous[2]
zero[2]
Albedo 0.090±0.005[4]
Surface temp. min mean max
[5] 120 K 165 K
14.1[6]

    Amalthea (/æməlˈθiːə/ am-əl-THEE-ə; Greek: Ἀμάλθεια) is the third moon of Jupiter in order of distance from the planet. It was discovered on 9 September 1892, by Edward Emerson Barnard and named after Amalthea, a nymph in Greek mythology.[7] It is also known as Jupiter V.

    Amalthea is in a close orbit around Jupiter and is within the outer edge of the Amalthea Gossamer Ring, which is formed from dust ejected from its surface.[8] From its surface, Jupiter would appear 46.5 degrees in diameter.[lower-alpha 2] Amalthea is the largest of the inner satellites of Jupiter. Irregularly shaped and reddish in color, it is thought to consist of porous water ice with unknown amounts of other materials. Its surface features include large craters and ridges.[2]

    Amalthea was photographed in 1979 by the Voyager 1 and 2 spacecraft, and later, in more detail, by the Galileo orbiter in the 1990s.[2]

    History

    Discovery

    Voyager 1 color image of Amalthea (1979)

    Amalthea was discovered on 9 September 1892, by Edward Emerson Barnard using the 36 inch (91 cm) refractor telescope at Lick Observatory.[7] It was the last planetary satellite to be discovered by direct visual observation (as opposed to photographically) and was the first new satellite of Jupiter since Galileo Galilei's discovery of the Galilean satellites in 1610.[9]

    Name

    Amalthea is named after the nymph Amalthea from Greek mythology, who nursed the infant Zeus (the Greek equivalent of Jupiter) with goat's milk.[10] Its Roman numeral designation is Jupiter V. The name "Amalthea" was not formally adopted by the IAU until 1976,[11][12] although it had been in informal use for many decades. The name was initially suggested by Camille Flammarion.[13] Before 1976, Amalthea was most commonly known simply as Jupiter V.[5]

    Orbit

    Amalthea orbits Jupiter at a distance of 181 000 km (2.54 Jupiter radii). The orbit of Amalthea has an eccentricity of 0.003 and an inclination of 0.37° relative to the equator of Jupiter.[1] Such appreciably nonzero values of inclination and eccentricity, though still small, are unusual for an inner satellite and can be explained by the influence of the innermost Galilean satellite, Io: in the past Amalthea has passed through several mean-motion resonances with Io that have excited its inclination and eccentricity (in a mean-motion resonance the ratio of orbital periods of two bodies is a rational number like m:n).[8]

    Amalthea's orbit lies near the outer edge of the Amalthea Gossamer Ring, which is composed of the dust ejected from the satellite.[14]

    Physical characteristics

    The surface of Amalthea is very red.[2] The reddish color may be due to sulfur originating from Io or some other non-ice material.[2] Bright patches of less red tint appear on the major slopes of Amalthea, but the nature of this color is currently unknown.[2] The surface of Amalthea is slightly brighter than surfaces of other inner satellites of Jupiter.[4] There is also a substantial asymmetry between leading and trailing hemispheres: the leading hemisphere is 1.3 times brighter than the trailing one. The asymmetry is probably caused by the higher velocity and frequency of impacts on the leading hemisphere, which excavate a bright material—presumably ice—from the interior of the moon.[4]

    Galileo images showing Amalthea's irregular shape
    The most detailed existing image of Amalthea (2.4 km/pix).[8] Anti-Jupiter side. Ida Facula and Lyctos Facula are on the left side (on the terminator). Bright spot underside is associated with crater Gaea. Photo by Galileo (2000)

    Amalthea is irregularly shaped, with the best ellipsoidal approximation being 250 × 146 × 128 km.[2] From this, Amalthea's surface area is likely between 88,000 and 170,000 square kilometers, or somewhere near 130,000. Like all other inner moons of Jupiter it is tidally locked with the planet, the long axis pointing towards Jupiter at all times.[8] Its surface is heavily scarred by craters, some of which are extremely large relative to the size of the moon: Pan, the largest crater, measures 100 km across and is at least 8 km deep.[2] Another crater, Gaea, measures 80 km across and is likely twice as deep as Pan.[2] Amalthea has several prominent bright spots, two of which are named. They are Lyctos Facula and Ida Facula, with width reaching up to 25 km. They are located on the edge of ridges.[2]

    Amalthea's irregular shape and large size led in the past to a conclusion that it is a fairly strong, rigid body,[8] where it was argued that a body composed of ices or other weak materials would have been pulled into a more spherical shape by its own gravity. However, on 5 November 2002, the Galileo orbiter made a targeted flyby that came within 160 km of Amalthea and the deflection of its orbit was used to compute the moon's mass (its volume had been calculated previously—to within 10% or so—from a careful analysis of all extant images).[2] In the end, Amalthea's density was found to be as low as 0.86 g/cm3,[3][15] so it must be either a relatively icy body or very porous "rubble pile" or, more likely, something in between. Recent measurements of infrared spectra from the Subaru telescope suggest that the moon indeed contains hydrous minerals (or organic materials), indicating that it cannot have formed in its current position, since the hot primordial Jupiter would have melted it.[16] It is therefore likely to have formed farther from the planet or to be a captured Solar System body.[3] No images were taken during this flyby (Galileo's cameras had been deactivated due to radiation damage in January 2002), and the resolution of other available images is generally low.

    Amalthea radiates slightly more heat than it receives from the Sun, which is probably due to the influence of Jovian heat flux (<9 kelvin), sunlight reflected from the planet (<5 K), and charged particle bombardment (<2 K).[5] This is a trait shared with Io, although for different reasons.

    Named geological features

    There are four named geological features on Amalthea: two craters and two faculae (bright spots).[17] The faculae are located on the edge of a ridge on the anti-Jupiter side of Amalthea.[2]

    Leading side of Amalthea. North is up, and Jupiter is beyond the right side. Crater Pan is seen on the upper right edge, and Gaea on the lower. Ida Facula and Lyctos Facula are on the left end (upper and lower brightenings respectively)
    Feature Named after
    Pan (crater) Pan, Greek god
    Gaea (crater) Gaia, Greek goddess
    Lyctos Facula Lyctus, Crete
    Ida Facula Mount Ida, Crete

    Relationship with Jupiter's rings

    Due to tidal force from Jupiter and Amalthea's low density and irregular shape, the escape velocity at its surface points closest to and furthest from Jupiter is no more than 1 m/s and dust can easily escape from it after, e.g. micrometeorite impacts; this dust forms the Amalthea Gossamer Ring.[8]

    During its flyby of Amalthea, the Galileo orbiter's star scanner detected nine flashes that appear to be small moonlets near the orbit of Amalthea. Because they were sighted only from one location, their true distances could not be measured. These moonlets may be anywhere in size from gravel to stadium-sized. Their origins are unknown, but they may be gravitationally captured into current orbit or they may be ejecta from meteor impacts on Amalthea. On the next and final orbit (just an hour before destruction), Galileo detected one more such moonlet. However, this time Amalthea was on the other side of the planet, so it is probable that the particles form a ring around the planet near Amalthea's orbit.[18][19][20][21]

    Views to and from Amalthea

    From Jupiter's surface—or rather, from just above its cloudtops—Amalthea would appear very bright, shining with a magnitude of −4.7,[lower-alpha 2] similar to that of Venus from Earth. At only 8 arcminutes across,[lower-alpha 3] its disc would be barely discernible. Amalthea's orbital period is only slightly longer than its parent planet's day (about 20% in this case), which means it would cross Jupiter's sky very slowly. The time between moonrise and moonset would be over 29 hours.[lower-alpha 2]

    Simulated view of Jupiter from Amalthea.

    From the surface of Amalthea, Jupiter would look enormous: 46 degrees across,[lower-alpha 3] it would appear roughly 92 times larger than the full moon. Because Amalthea is in synchronous rotation, Jupiter would not appear to move, and would not be visible from one side of Amalthea. The Sun would disappear behind Jupiter's bulk for an hour and a half each revolution, and Amalthea's short rotation period gives it just under six hours of daylight. Though Jupiter would appear 900 times brighter than the full moon, its light would be spread over an area some 8500 times greater and it would not look as bright per surface unit.[lower-alpha 2]

    Exploration

    During 1979, the unmanned Voyager 1 and Voyager 2 space probes obtained the first images of Amalthea to resolve its surface features.[2] They also measured the visible and infrared spectra and surface temperature.[5] Later, the Galileo orbiter completed the imaging of Amalthea's surface. Galileo made its final satellite fly-by at a distance of approximately 244 km (152 mi) from Amalthea's center (at a height of about 160–170 km) on 5 November 2002, permitting the moon's mass to be accurately determined, while changing Galileo's trajectory so that it would plunge into Jupiter in September 2003 at the end of its mission.[3] In 2006, Amalthea's orbit was refined with measurements from New Horizons.

    In fiction

    Main article: Amalthea in fiction

    Amalthea is the setting of several works of science fiction, including stories by Arthur C. Clarke and James Blish.

    Notes

    1. 1 2 3 4 5 Calculated on the basis of other parameters.
    2. 1 2 3 4 Calculated on the basis of known distances, sizes, periods and visual magnitudes as visible from the Earth. Visual magnitudes as seen from Jupiter mj are calculated from visual magnitudes on Earth mv using the formula mj=mv−log2.512(Ij/Iv), where Ij and Iv are respective brightnesses (see visual magnitude), which scale according to the inverse square law. For visual magnitudes see http://www.oarval.org/ClasSaten.htm and Jupiter (planet).
    3. 1 2 Calculated from the known sizes and distances of the bodies, using the formula 2*arcsin(Rb/Ro), where Rb is the radius of the body and Ro is the radius of Amalthea's orbit or distance from the Jovian surface to Amalthea.

    References

    1. 1 2 3 4 5 Cooper Murray et al. 2006.
    2. 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 Thomas Burns et al. 1998.
    3. 1 2 3 4 5 6 Anderson Johnson et al. 2005.
    4. 1 2 3 Simonelli Rossier et al. 2000.
    5. 1 2 3 4 Simonelli 1983.
    6. ↑ Observatorio ARVAL.
    7. 1 2 Barnard 1892.
    8. 1 2 3 4 5 6 Burns Simonelli et al. 2004.
    9. ↑ Bakich M. E. (2000). The Cambridge Planetary Handbook. Cambridge University Press. pp. 220–221. ISBN 9780521632805.
    10. ↑ "Planet and Satellite Names and Discoverers". Gazetteer of Planetary Nomenclature. International Astronomical Union (IAU) Working Group for Planetary System Nomenclature (WGPSN). Archived from the original on 2014-08-21. Retrieved 2014-10-08.
    11. ↑ Blunck J. (2010). Solar System Moons: Discovery and Mythology (PDF). Springer. pp. 9–15. Bibcode:2010ssm..book.....B. doi:10.1007/978-3-540-68853-2. ISBN 978-3-540-68852-5.
    12. ↑ Flammarion C.; Kowal C.; Blunck J. (1975-10-07). "Satellites of Jupiter". International Astronomical Union Circular 2846. Central Bureau for Astronomical Telegrams. Archived from the original on 2014-02-22. Retrieved 2014-10-17. (Bibcode: 1975IAUC.2846....6F)
    13. ↑ Flammarion 1893.
    14. ↑ Burns Showalter et al. 1999.
    15. ↑ Swiss Cheese Moon.
    16. ↑ Takato Bus et al. 2004.
    17. ↑ USGS: Jupiter: Amalthea.
    18. ↑ Fieseler P. D.; Adams O. W.; Vandermey N.; Theilig E. E.; Schimmels K. A.; Lewis G. D.; Ardalan S. M.; Alexander C. J. (2004). "The Galileo star scanner observations at Amalthea". Icarus. 169 (2): 390–401. Bibcode:2004Icar..169..390F. doi:10.1016/j.icarus.2004.01.012.
    19. ↑ "Another Find for Galileo". Jet Propulsion Laboratory. 9 April 2003. Archived from the original on 2004-11-04. Retrieved 2012-03-27.
    20. ↑ Fieseler P. D.; Ardalan S. M. (2003-04-04). "Objects near Jupiter V (Amalthea)". International Astronomical Union Circular 8107. Central Bureau for Astronomical Telegrams. Archived from the original on 2014-03-02. Retrieved 2014-10-12. (Bibcode: 2003IAUC.8107....2F)
    21. ↑ Emily Lakdawalla (2013-05-17). "A serendipitous observation of tiny rocks in Jupiter's orbit by Galileo". The Planetary Society. Archived from the original on 2014-08-14. Retrieved 2014-10-14.

    Cited sources

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