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Calypso (moon)
Trojan moon of Saturn
Trojan moon of Saturn
| Field | Value |
|---|---|
| name | Calypso |
| image | Calypso N1644755236 1.jpg |
| caption | Calypso image from *Cassini* |
| (February 13, 2010) | |
| pronounced | |
| adjectives | Calypsoan , Calypsonian |
| named_after | Καλυψώ *Kalypsō* |
| mpc_name | Saturn XIV |
| alt_names | Tethys C |
| S/1980 S 25 | |
| discovered | March 13, 1980 |
| semimajor | |
| eccentricity | |
| period | |
| inclination | 1.56° (to Saturn's equator) |
| satellite_of | Saturn |
| group | L5 Tethys trojan |
| dimensions | km |
| (± km) | |
| mean_diameter | |
| volume | |
| mass | (assumed; unmeasured) |
| density | (assumed; unmeasured) |
| surface_grav | ≈ |
| escape_velocity | ≈ km/s at longest axis |
| to ≈ km/s at poles | |
| rotation | synchronous |
| axial_tilt | zero |
| albedo | (geometric) |
(February 13, 2010) S/1980 S 25
- Dan Pascu
- P. Kenneth Seidelmann
- William A. Baum
- Douglas G. Currie (± km) to ≈ km/s at poles NOTOC Calypso is a moon of Saturn. It was discovered in 1980, from ground-based observations, by Dan Pascu, P. Kenneth Seidelmann, William A. Baum, and Douglas G. Currie, and was provisionally designated S/1980 S 25 (the 25th satellite of Saturn discovered in 1980). Several other apparitions of it were recorded in the following months: S/1980 S 29, S/1980 S 30, S/1980 S 32, and S/1981 S 2. In 1983 it was officially named after Calypso of Greek mythology. It is also designated Saturn XIV or Tethys C.
Calypso is co-orbital with the moon Tethys, and resides in Tethys's trailing Lagrangian point (), 60 degrees behind Tethys. This relationship was first identified by Seidelmann Harrington et al. 1981}}|Seidelmann et al. in 1981. The moon Telesto resides in the other (leading) Lagrangian point of Tethys, 60 degrees in the other direction from Tethys. Calypso and Telesto have been termed "Tethys trojans", by analogy to the trojan asteroids, and are half of the four presently known trojan moons.
Like many other small Saturnian moons and small asteroids, Calypso is irregularly shaped, has overlapping large craters, and appears to also have loose surface material capable of smoothing the craters' appearance. Its surface is one of the most reflective (at visual wavelengths) in the Solar System, with a visual geometric albedo of 1.34. This very high albedo is the result of the sandblasting of particles from Saturn's E-ring, a faint ring composed of small, water-ice particles generated by Enceladus's south polar geysers.
Gallery
File:Calypso crop resize sharp.jpg|Another February 13, 2010 image showing flow-like albedo features File:Calypso image PIA07633.jpg|Cassini image from September 23, 2005 File:Calypso - Voyager 2.jpg|Calypso as seen by Voyager 2 (August 1981)
Notes
| Transactions of the International Astronomical Union, Vol. XVIIIA, 1982 (confirms Janus, names Epimetheus, Telesto, Calypso) (mentioned in IAUC 3872}}|IAUC 3872: Satellites of Jupiter and Saturn, September 30, 1983)
References
Citations
Sources
- {{cite journal | access-date = 2011-12-23
- {{cite journal | access-date = 2011-12-23
- {{cite journal | access-date = 2011-12-23
- {{cite journal | access-date = 2011-12-23
- {{cite journal |access-date=2011-12-23 |url-status=dead |archive-url=https://web.archive.org/web/20110725035059/http://www.cbat.eps.harvard.edu/iauc/03800/03872.html |archive-date=2011-07-25
- {{cite web | access-date = 2011-12-23
- (supporting online material, table S1)
- {{cite journal
References
- "Calypso". [[Oxford University Press]].
- ''The Emerson Society Quarterly'', vol. 50, p. 56, 1968
- "Calypsonian". [[Oxford University Press]].
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