Debye–Waller factor

Motion of the Solar System barycenter relative to the Sun

In astronomy, barycentric coordinates are non-rotating coordinates with origin at the center of mass of two or more bodies.

The barycenter (or barycentre; from the Greek βαρύ-ς heavy + κέντρ-ον centre + -ic) is the point between two objects where they balance each other. For example, it is the center of mass where two or more celestial bodies orbit each other. When a moon orbits a planet, or a planet orbits a star, both bodies are actually orbiting around a point that is not at the center of the primary (the larger body). For example, the Moon does not orbit the exact center of the Earth, but a point on a line between the center of the Earth and the Moon, approximately 1,710 km below the surface of the Earth, where their respective masses balance. This is the point about which the Earth and Moon orbit as they travel around the Sun.

Two-body problem

The barycenter is one of the foci of the elliptical orbit of each body. This is an important concept in the fields of astronomy, astrophysics, and the like (see two-body problem). In a simple two-body case, r₁, the distance from the center of the primary to the barycenter is given by:

$r_1=a\cdot \frac{m_2}{m_1+m_2}=\frac{a}{1+m_1/m_2}$

where:

a is the distance between the centers of the two bodies;

m₁ and m₂ are the masses of the two bodies.

If a is the semi-major axis of the system, r₁ is the semi-major axis of the primary's orbit around the barycenter, and r₂ = a − r₁ is the semi-major axis of the secondary's orbit. When the barycenter is located within the more massive body, that body will appear to "wobble" rather than following a discernible orbit.

Examples

<Sun-Jupiter barycenter>...</Sun-Jupiter barycenter> The following table sets out some examples from the Solar System. Figures are given rounded to three significant figures. The last two columns show R₁, the radius of the first (more massive) body, and r₁ / R₁, the ratio of the distance to the barycenter and that radius: a value less than one shows that the barycenter lies inside the first body.

Examples

Larger body	m1 (mE=1)	Smaller body	m2 (mE=1)	a (km)	r1 (km)	R1 (km)	r1 / R1
Remarks
Earth	1	Moon	0.0123	384,000	4,670	6,380	0.732
The Earth has a perceptible "wobble"; see tides.
Pluto	0.0021	Charon	0.000254 (0.121 mPluto)	19,600	2,110	1,150	1.83
Both bodies have distinct orbits around the barycenter, and as such Pluto and Charon were considered as a double planet by many before the redefinition of planet in August 2006.
Sun	333,000	Earth	1	150,000,000 (1 AU)	449	696,000	0.000646
The Sun's wobble is barely perceptible.
Sun	333,000	Jupiter	318 (0.000955 mSun)	778,000,000 (5.20 AU)	742,000	696,000	1.07
The Sun orbits a barycenter just above its surface.

Inside or outside the Sun?

If m₁ ≫ m₂ — which is true for the Sun and any planet — then the ratio r₁/R₁ approximates to:

$\frac{a}{R_1}\cdot \frac{m_2}{m_1}$

Hence, the barycenter of the Sun–planet system will lie outside the Sun only if:

$\frac{a}{R_{⨀}}\cdot \frac{m_{planet}}{m_{⨀}}>1\Rightarrow a\cdot m_{planet}>R_{⨀}\cdot m_{⨀}\approx 2.3\times 10^{11}{m}_{Earth}\text{km}\approx 1530m_{Earth}\text{AU}$

That is, where the planet is heavy and far from the Sun.

If Jupiter had Mercury's orbit (57,900,000 km, 0.387 AU), the Sun–Jupiter barycenter would be approximately 55,000 km from the center of the Sun (r₁/R₁ ~ 0.08). But even if the Earth had Eris' orbit (68 AU), the Sun–Earth barycenter would still be within the Sun (just over 30,000 km from the center).

To calculate the actual motion of the Sun, you would need to sum all the influences from all the planets, comets, asteroids, etc. of the Solar System (see n-body problem). If all the planets were aligned on the same side of the Sun, the combined center of mass would lie about 500,000 km above the Sun's surface.

The calculations above are based on the mean distance between the bodies and yield the mean value r₁. But all celestial orbits are elliptical, and the distance between the bodies varies between the apses, depending on the eccentricity, e. Hence, the position of the barycenter varies too, and it is possible in some systems for the barycenter to be sometimes inside and sometimes outside the more massive body. This occurs where:

$\frac{1}{1-e}>\frac{r_1}{R_1}>\frac{1}{1+e}$

Note that the Sun–Jupiter system, with e_Jupiter = 0.0484, just fails to qualify: 1.05 ≯ 1.07 > 0.954.

Animations

Images are representative (made by hand), not simulated.

Two bodies with the same mass orbiting a common barycenter (similar to the 90 Antiope system)	Two bodies with a difference in mass orbiting a common barycenter external to both bodies, as in the Pluto–Charon system	Two bodies with a major difference in mass orbiting a common barycenter internal to one body (similar to the Earth–Moon system)	Two bodies with an extreme difference in mass orbiting a common barycenter internal to one body (similar to the Sun–Earth system)
Two bodies with the same mass orbiting a common barycenter, external to both bodies, with eccentric elliptic orbits (a common situation for binary stars)

Relativistic corrections

In classical mechanics, this definition simplifies calculations and introduces no known problems. In general relativity, problems arise because, while it is possible, within reasonable approximations, to define the barycenter, the associated coordinate system does not fully reflect the inequality of clock rates at different locations. Brumberg explains how to set up barycentric coordinates in general relativity.

The coordinate systems involve a world-time, i.e. a global time coordinate that could be set up by telemetry. Individual clocks of similar construction will not agree with this standard, because they are subject to differing gravitational potentials or move at various velocities, so the world-time must be slaved to some ideal clock that is assumed to be very far from the whole self-gravitating system. This time standard is called Barycentric Coordinate Time, "TCB".

Selected barycentric orbital elements

Barycentric osculating orbital elements for some objects in the Solar System:

Object	Semi-major axis (in AU)	Apoapsis (in AU)	Orbital period (in years)
C/2006 P1 (McNaught)	2050	4100	92600
Comet Hyakutake	1700	3410	70000
C/2006 M4 (SWAN)	1300	2600	47000
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Systems Analyst Kepp from Lloydminster, loves bird watching, property developers in singapore and fossils. Advocates that you simply journey to Gulf of Porto: Calanche of Piana. Take a look at my blog post ... apartment for sale	549	1078	12800
90377 Sedna	506	937	11400
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For objects at such high eccentricity, the Sun's barycentric coordinates are more stable than heliocentric coordinates.

References

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