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Synchronous orbit

From Wikipedia, the free encyclopedia

A synchronous orbit is an orbit in which an orbiting body (usually a satellite) has a period equal to the average rotational period of the body being orbited (usually a planet), and in the same direction of rotation as that body.[1]

Simplified meaning

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A synchronous orbit is an orbit in which the orbiting object (for example, an artificial satellite or a moon) takes the same amount of time to complete an orbit as it takes the object it is orbiting to rotate once.

Properties

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A satellite in a synchronous orbit that is both equatorial and circular will appear to be suspended motionless above a point on the orbited planet's equator. For synchronous satellites orbiting Earth, this is also known as a geostationary orbit. However, a synchronous orbit need not be equatorial; nor circular. A body in a non-equatorial synchronous orbit will appear to oscillate north and south above a point on the planet's equator, whereas a body in an elliptical orbit will appear to oscillate eastward and westward. As seen from the orbited body the combination of these two motions produces a figure-8 pattern called an analemma.

Nomenclature

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There are many specialized terms for synchronous orbits depending on the body orbited. The following are some of the more common ones. A synchronous orbit around Earth that is circular and lies in the equatorial plane is called a geostationary orbit. The more general case, when the orbit is inclined to Earth's equator or is non-circular is called a geosynchronous orbit. The corresponding terms for synchronous orbits around Mars are areostationary and areosynchronous orbits. [citation needed]

Formula

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For a stationary synchronous orbit:

[2]
G = Gravitational constant
m2 = Mass of the celestial body
T = Sidereal rotational period of the body
= Radius of orbit

By this formula, one can find the synchronous orbital radius of a body, given its mass and sidereal rotational period.

Orbital speed (how fast a satellite is moving through space) is calculated by multiplying the angular speed of the satellite by the orbital radius.[3]

Due to obscure quirks of orbital mechanics, no tidally locked body in a 1:1 spin-orbit resonance (i.e. a moon locked to a planet or a planet locked to a star) can have a stable satellite in a synchronous orbit, as the synchronous orbital radius lies outside the body's Hill sphere.[4] This is universal and irrespective of the masses and distances involved.

Examples

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An astronomical example is Pluto's largest moon Charon.[5] Much more commonly, synchronous orbits are employed by artificial satellites used for communication, such as geostationary satellites.

For natural satellites, which can attain a synchronous orbit only by tidally locking their parent body, it always goes in hand with synchronous rotation of the satellite. This is because the smaller body becomes tidally locked faster, and by the time a synchronous orbit is achieved, it has had a locked synchronous rotation for a long time already.[citation needed]

The following table lists select Solar System bodies' masses, sidereal rotational periods, and the semi-major axises and altitudes of their synchronous orbital radii (calculated by the formula in the above section):

Body Body's Mass (kg) Sidereal Rotation period Semi-major axis of synchronous orbit (km) Altitude of synchronous orbit (km) Synchronous orbit within Hill sphere?
Mercury[6] 0.33010×1024 1407.6 h 242,895 km 240,454 km No
Venus[7] 4.8673×1024 5832.6 h 1,536,578 km 1,530,526 km No
Earth[8] 5.9722×1024 23.9345 h 42,164 km 35,786 km Yes
Moon[9] 0.07346×1024 655.72 h 88,453 km 86,715 km No
Mars[10] 0.64169×1024 24.6229 h 20,428 km 17,031 km Yes
Ceres[11] 0.09393×1022 9.074 h 1,192 km 723 km Yes
Jupiter[12] 1898.13×1024 9.925 h 169,010 km 88,518 km Yes
Saturn[13] 568.32×1024 10.656 h 112,239 km 51,971 km Yes
Uranus[14] 86.811×1024 17.24 h 82,686 km 57,127 km Yes
Neptune[15] 102.409×1024 16.11 h 83,508 km 58,744 km Yes
Pluto[16] 0.01303×1024 153.2928 h 18,860 km 17,672 km Yes

See also

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References

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  1. ^ Holli, Riebeek (2009-09-04). "Catalog of Earth Satellite Orbits : Feature Articles". earthobservatory.nasa.gov. Retrieved 2016-05-08.
  2. ^ "Calculating the Radius of a Geostationary Orbit - Ask Will Online". Ask Will Online. 2012-12-27. Retrieved 2017-11-21.
  3. ^ see Circular motion#Formulas
  4. ^ "Is it possible to achieve a stable "selenostationary" orbit around the Moon?". Astronomy Stack Exchange. Retrieved 2025-05-29.
  5. ^ S.A. Stern (1992). "The Pluto-Charon system". Annual Review of Astronomy and Astrophysics. 30: 190. Bibcode:1992ARA&A..30..185S. doi:10.1146/annurev.aa.30.090192.001153. Charon's orbit is (a) synchronous with Pluto's rotation and (b) highly inclined to the plane of the ecliptic.
  6. ^ "Mercury Fact Sheet". nssdc.gsfc.nasa.gov. Retrieved 2025-05-30.
  7. ^ "Venus Fact Sheet". nssdc.gsfc.nasa.gov. Retrieved 2025-05-30.
  8. ^ "Earth Fact Sheet". nssdc.gsfc.nasa.gov. Retrieved 2025-05-30.
  9. ^ "Moon Fact Sheet". nssdc.gsfc.nasa.gov. Retrieved 2025-05-30.
  10. ^ "Mars Fact Sheet". nssdc.gsfc.nasa.gov. Retrieved 2025-05-30.
  11. ^ "Asteroid Fact Sheet". nssdc.gsfc.nasa.gov. Retrieved 2025-05-30.
  12. ^ "Jupiter Fact Sheet". nssdc.gsfc.nasa.gov. Retrieved 2025-05-30.
  13. ^ "Saturn Fact Sheet". nssdc.gsfc.nasa.gov. Retrieved 2025-05-30.
  14. ^ "Uranus Fact Sheet". nssdc.gsfc.nasa.gov. Retrieved 2025-05-30.
  15. ^ "Neptune Fact Sheet". nssdc.gsfc.nasa.gov. Retrieved 2025-05-30.
  16. ^ "Pluto Fact Sheet". nssdc.gsfc.nasa.gov. Retrieved 2025-05-30.