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Sun-synchronous orbit

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Diagram showing the orientation of a Sun-synchronous orbit (green) at four points in the year. A non-Sun-synchronous orbit (magenta) is also shown for reference. Dates are shown in white: day/month.

A Sun-synchronous orbit (SSO), also called a heliosynchronous orbit,[1] is a nearly polar orbit around a planet, in which the satellite passes over any given point of the planet's surface at the same local mean solar time.[2][3] More technically, it is an orbit arranged so that it precesses through one complete revolution each year, so it always maintains the same relationship with the Sun.



A Sun-synchronous orbit is useful for imaging, reconnaissance, and weather satellites,[4] because every time that the satellite is overhead, the surface illumination angle on the planet underneath it is nearly the same. This consistent lighting is a useful characteristic for satellites that image the Earth's surface in visible or infrared wavelengths, such as weather and spy satellites, and for other remote-sensing satellites, such as those carrying ocean and atmospheric remote-sensing instruments that require sunlight. For example, a satellite in Sun-synchronous orbit might ascend across the equator twelve times a day, each time at approximately 15:00 mean local time.

Sun-synchronous orbit from a top view of the ecliptic plane with local solar time (LST) zones for reference and a descending node of 10:30. The LST zones show how the local time beneath the satellite varies at different latitudes and different points on its orbit.

Special cases of the Sun-synchronous orbit are the noon/midnight orbit, where the local mean solar time of passage for equatorial latitudes is around noon or midnight, and the dawn/dusk orbit, where the local mean solar time of passage for equatorial latitudes is around sunrise or sunset, so that the satellite rides the terminator between day and night. Riding the terminator is useful for active radar satellites, as the satellites' solar panels can always see the Sun, without being shadowed by the Earth. It is also useful for some satellites with passive instruments that need to limit the Sun's influence on the measurements, as it is possible to always point the instruments towards the night side of the Earth. The dawn/dusk orbit has been used for solar-observing scientific satellites such as TRACE, Hinode and PROBA-2, affording them a nearly continuous view of the Sun.

Orbital precession


A Sun-synchronous orbit is achieved by having the osculating orbital plane precess (rotate) approximately one degree eastward each day with respect to the celestial sphere to keep pace with the Earth's movement around the Sun.[5] This precession is achieved by tuning the inclination to the altitude of the orbit (see Technical details) such that Earth's equatorial bulge, which perturbs inclined orbits, causes the orbital plane of the spacecraft to precess with the desired rate. The plane of the orbit is not fixed in space relative to the distant stars, but rotates slowly about the Earth's axis.

Typical Sun-synchronous orbits around Earth are about 600–800 km (370–500 mi) in altitude, with periods in the 96–100-minute range, and inclinations of around 98°. This is slightly retrograde compared to the direction of Earth's rotation: 0° represents an equatorial orbit, and 90° represents a polar orbit.[5]

Sun-synchronous orbits are possible around other oblate planets, such as Mars. A satellite orbiting a planet such as Venus that is almost spherical will need an outside push to maintain a Sun-synchronous orbit.

Technical details


The angular precession per orbit for an Earth orbiting satellite is approximately given by


J2 = 1.08263×10−3 is the coefficient for the second zonal term related to the oblateness of the Earth,
RE ≈ 6378 km is the mean radius of the Earth,
p is the semi-latus rectum of the orbit,
i is the inclination of the orbit to the equator.

An orbit will be Sun-synchronous when the precession rate ρ = dΩ/dt equals the mean motion of the Earth about the Sun nE, which is 360° per sidereal year (1.99096871×10−7 rad/s), so we must set nE = ΔΩE/TE = ρ = ΔΩ/T , where TE is the earth orbital period while T is the period of the spacecraft around the earth.

As the orbital period of a spacecraft is

where a is the semi-major axis of the orbit, and μ is the standard gravitational parameter of the planet (398600.440 km3/s2 for Earth); as pa for a circular or almost circular orbit, it follows that

or when ρ is 360° per year,

As an example, with a = 7200 km, i.e., for an altitude aRE800 km of the spacecraft over Earth's surface, this formula gives a Sun-synchronous inclination of 98.7°.

Note that according to this approximation cos i equals −1 when the semi-major axis equals 12352 km, which means that only lower orbits can be Sun-synchronous. The period can be in the range from 88 minutes for a very low orbit (a = 6554 km, i = 96°) to 3.8 hours (a = 12352 km, but this orbit would be equatorial, with i = 180°). A period longer than 3.8 hours may be possible by using an eccentric orbit with p < 12352 km but a > 12352 km.

If one wants a satellite to fly over some given spot on Earth every day at the same hour, the satellite must complete a whole number of orbits per day. Assuming a circular orbit, this comes down to between 7 and 16 orbits per day, as doing less than 7 orbits would require an altitude above the maximum for a Sun-synchronous orbit, and doing more than 16 would require an orbit inside the Earth's atmosphere or surface. The resulting valid orbits are shown in the following table. (The table has been calculated assuming the periods given. The orbital period that should be used is actually slightly longer. For instance, a retrograde equatorial orbit that passes over the same spot after 24 hours has a true period about 365/364 ≈ 1.0027 times longer than the time between overpasses. For non-equatorial orbits the factor is closer to 1.)

per day
Period (h) Altitude
16 ⁠1+1/2 = 1:30 274 83.4° 96.6°
15 ⁠1+3/5 = 1:36 567 82.3° 97.7°
14 ⁠1+5/7 ≈ 1:43 894 81.0° 99.0°
13 ⁠1+11/13 ≈ 1:51 1262 79.3° 100.7°
12 2 1681 77.0° 103.0°
11 ⁠2+2/11 ≈ 2:11 2162 74.0° 106.0°
10 ⁠2+2/5 = 2:24 2722 69.9° 110.1°
9 ⁠2+2/3 = 2:40 3385 64.0° 116.0°
8 3 4182 54.7° 125.3°
7 ⁠3+3/7 ≈ 3:26 5165 37.9° 142.1°

When one says that a Sun-synchronous orbit goes over a spot on the Earth at the same local time each time, this refers to mean solar time, not to apparent solar time. The Sun will not be in exactly the same position in the sky during the course of the year (see Equation of time and Analemma).

Sun-synchronous orbits are mostly selected for Earth observation satellites, with an altitude typically between 600 and 1000 km over the Earth surface. Even if an orbit remains Sun-synchronous, however, other orbital parameters such as argument of periapsis and the orbital eccentricity evolve, due to higher-order perturbations in the Earth's gravitational field, the pressure of sunlight, and other causes. Earth observation satellites, in particular, prefer orbits with constant altitude when passing over the same spot. Careful selection of eccentricity and location of perigee reveals specific combinations where the rate of change of perturbations are minimized, and hence the orbit is relatively stable – a frozen orbit, where the motion of position of the periapsis is stable.[6] The ERS-1, ERS-2 and Envisat of European Space Agency, as well as the MetOp spacecraft of EUMETSAT and RADARSAT-2 of the Canadian Space Agency, are all operated in such Sun-synchronous frozen orbits.[7]

See also



  1. ^ Tscherbakova, N. N.; Beletskii, V. V.; Sazonov, V. V. (1999). "Stabilization of heliosynchronous orbits of an Earth's artificial satellite by solar pressure". Cosmic Research. 37 (4): 393–403. Bibcode:1999KosIs..37..417S. Archived from the original on 3 March 2016. Retrieved 19 May 2015.
  3. ^ "Types of Orbits". marine.rutgers.edu. Archived from the original on 22 August 2019. Retrieved 24 June 2017.
  4. ^ Our Changing Planet: The View from Space (1st ed.). Cambridge University Press. 2007. p. 339. ISBN 978-0521828703.
  5. ^ a b Rosengren, M. (November 1992). "ERS-1 - An Earth Observer that exactly follows its Chosen Path". ESA Bulletin. 72 (72). European Space Agency: 76. Bibcode:1992ESABu..72...76R.
  6. ^ Low, Samuel Y. W. (January 2022). "Designing a Reference Trajectory for Frozen Repeat Near-Equatorial Low Earth Orbits". AIAA Journal of Spacecraft and Rockets. 59 (1): 84–93. Bibcode:2022JSpRo..59...84L. doi:10.2514/1.A34934. S2CID 236275629.
  7. ^ Rosengren, Mats (1989). "Improved technique for Passive Eccentricity Control (AAS 89-155)". Advances in the Astronautical Sciences. Vol. 69. AAS/NASA. Bibcode:1989ommd.proc...49R.

Further reading