Co-orbital moon

Co-orbital moon

Co-orbital moons are natural satellites that orbit at the same (or very similar) distance from their parent planet as each other. Only the Saturn system is known to have co-orbital moons, and it has three sets.

Two of these are sets of Trojan moons, which are unique only in that they orbit a planet rather than the Sun (there are several thousand known Trojan asteroids). In a Trojan configuration, one or more moons orbits at the stable Lagrange point, 60° behind or ahead of a much more massive moon. The massive moon is not perceptibly affected by the relatively tiny Trojans (see restricted three-body problem). Saturn's moon Tethys has two Trojan moons (Telesto and Calypso), and Dione also has two Trojan moons (Helene and Polydeuces).

Much more unique are the Saturnian moons Janus and Epimetheus, which are truly co-orbital and are not Trojans. Janus is more massive than Epimetheus, but only by a factor of four, so each moon exerts a significant influence on the other. In this case, the two moons "both" oscillate about their mass-weighted mean orbit.

Orbital relationship between Epimetheus and Janus

Janus and Epimetheus are "co-orbital:" Janus' mean orbital radius from Saturn is currently only 50 km less than that of Epimetheus. This is smaller than either moon's diameter. Since closer orbits have higher velocities, the two moons must inevitably approach each other, and it would seem at first glance that a collision would be inevitable. But as the inner moon catches up with the outer moon their mutual gravitational attraction boosts the inner moon's momentum and raises its orbit, causing it to slow down. At the same time, the outer moon equally loses momentum and drops into a lower orbit. The moons thus "trade" orbits and begin to move apart again, since the forward moon is now in the lower, faster orbit. The nearest they ever approach is some 10,000 km. The exchange takes place about once every four years; the last close approach was on 21 January, 2006, [NASA JPL, [http://saturn.jpl.nasa.gov/multimedia/images/image-details.cfm?imageID=2103 "Cassini-Huygens Multimedia: The Dancing Moons"] , May 3, 2006] the next will be in 2010. At that time, Janus' orbital radius will increase by ~20 km, while Epimetheus' decreases by ~80 km; Janus' orbit is less affected because it is 4 times more massive than Epimetheus. As far as it is currently known, this arrangement is unique in the solar system.

The orbital relationship between Janus and Epimetheus can be understood in terms of the circular restricted three-body problem, as a case in which the two moons (the third body being Saturn) are similar in size to each other. Other examples of the three-body problem include the Lagrangian points, Trojan asteroids and Trojan moons, the "horseshoe" orbit of Cruithne with respect to Earth, and potentially dozens of other objects in similar orbits. [Lloyd, R.; [http://www.space.com/scienceastronomy/solarsystem/second_moon_991029.html "More Moons Around Earth? Its Not So Loony"] , Space.com, 29 October 1999]

ee also

* Trojan moons
* Trojan (astronomy)
* Natural satellite
* Quasi-satellite

References


Wikimedia Foundation. 2010.

Игры ⚽ Поможем сделать НИР

Look at other dictionaries:

  • Moon Impact Probe — Operator Indian Space Research Organisation Mission type Impactor Satellite of Moon …   Wikipedia

  • Orbital inclination change — is an orbital maneuver aimed at changing the inclination of an orbiting body s orbit. This maneuver is also known as an orbital plane change as the plane of the orbit is tipped. This maneuver requires a change in the orbital velocity vector… …   Wikipedia

  • Orbital decay — is the process of prolonged reduction in the altitude of a satellite s orbit. This can be due to drag produced by an atmosphere due to frequent collisions between the satellite and surrounding air molecules. The drag experienced by the object is… …   Wikipedia

  • Moon Mineralogy Mapper — Left side of the Moon Mineralogy Mapper Operator NASA Major contractors JPL Mission type …   Wikipedia

  • Orbital elements — are the parameters required to uniquely identify a specific orbit. In celestial mechanics these elements are generally considered in classical two body systems, where a Kepler orbit is used (derived from Newton s laws of motion and Newton s law… …   Wikipedia

  • Moon — This article is about Earth s Moon. For moons in general, see Natural satellite. For other uses, see Moon (disambiguation) …   Wikipedia

  • moon — mooner, n. moonless, adj. /moohn/, n. 1. the earth s natural satellite, orbiting the earth at a mean distance of 238,857 miles (384,393 km) and having a diameter of 2160 miles (3476 km). 2. this body during a particular lunar month, or during a… …   Universalium

  • Moon — /moohn/, n. Sun Myung /sun myung/, born 1920, Korean religious leader: founder of the Unification Church. * * * Sole natural satellite of Earth, which it orbits from west to east at a mean distance of about 238,900 mi (384,400 km). It is less… …   Universalium

  • Orbital perturbation analysis (spacecraft) — Isaac Newton in his Philosophiæ Naturalis Principia Mathematica demonstrated that the gravitational force between two mass points is inversely proportional to the square of the distance between the points and fully solved corresponding two body… …   Wikipedia

  • Orbital period — For the music album, see Orbital Period (album). The orbital period is the time taken for a given object to make one complete orbit about another object. When mentioned without further qualification in astronomy this refers to the sidereal period …   Wikipedia

Share the article and excerpts

Direct link
Do a right-click on the link above
and select “Copy Link”