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DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

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symmetry<br />

posite walls of the cube, then only rotations by<br />

multiples of 90 ◦ are symmetries. If the axis<br />

passes through the centers of diagonally opposite<br />

edges of the cube, then only rotations by<br />

multiples of 180 ◦ are symmetries.) Continuous<br />

symmetries of an n-dimensional space can be<br />

labeled by up to 1 2n(n + 1) parameters. For example,<br />

among two-dimensional surfaces some<br />

have no symmetry (think about the surface of a<br />

loaf of bread), some have one-parametric symmetry<br />

(think about the surface of a perfectly<br />

smooth <strong>and</strong> round doughnut, which is symmetric<br />

with respect to rotations around an axis that<br />

passes through its center: the parameter is the<br />

angle of rotation), some have a two-parametric<br />

symmetry (think about the surface of an infinite<br />

cylinder, the parameters are the angle of rotation<br />

about the axis of the cylinder <strong>and</strong> the distance<br />

of displacement along the axis), <strong>and</strong> two<br />

have three-parametric symmetries. These latter<br />

are the plane <strong>and</strong> the surface of the sphere.<br />

For the plane, the symmetries are displacements<br />

along two perpendicular directions <strong>and</strong> rotations<br />

around an axis perpendicular to the plane. For<br />

the sphere, the symmetries are rotations around<br />

three mutually perpendicular axes. A characteristic<br />

property of each collection of symmetries<br />

is the difference between the following two operations:<br />

We take two of the basic symmetries<br />

(call them a <strong>and</strong> b), apply them to a point of<br />

the space in one order (first a, then b), <strong>and</strong> then<br />

apply them in the reversed order (first b, then<br />

a). The difference may be zero (like for the<br />

two translations on a plane) or nonzero (for any<br />

two rotations on a sphere or for a translation<br />

<strong>and</strong> a rotation on a plane). The fact that on a<br />

plane there exists a pair of symmetry transformations<br />

whose final result does not depend on<br />

the order in which they are executed, while no<br />

such pair exists on a sphere, shows that these<br />

two collections of symmetries are inequivalent.<br />

Real objects usually have no symmetry in the<br />

strict sense but may be approximately symmetric.<br />

(Example: the surface of the Earth is nearly<br />

a sphere. The departures from spherical shape<br />

caused by rotational flattening <strong>and</strong> by the mountains<br />

<strong>and</strong> other irregularities of the surface can<br />

be neglected for many purposes.) Symmetries<br />

are often assumed in physics in order to solve<br />

problems that would be too difficult to consider<br />

by exact methods without such an assumption.<br />

© 2001 by CRC Press LLC<br />

466<br />

Small departures from symmetries can then be<br />

taken into account by approximate calculations.<br />

A typical example is the calculation of orbits of<br />

the planets around the sun. Both in Newtonian<br />

mechanics <strong>and</strong> in general relativity a first approximation<br />

to the realistic solution was found<br />

under the assumption of spherical symmetry,<br />

which implies that the mass distribution inside<br />

the sun is perfectly spherical, <strong>and</strong> that the orbit of<br />

a given planet is not influenced by other planets.<br />

Then, small perturbations away from spherical<br />

symmetry caused by the other planets can be<br />

considered <strong>and</strong> corrections to the orbits calculated.<br />

Calculations without any symmetries assumed<br />

have been attempted only by numerical<br />

methods. A pronounced time dependent asymmetry<br />

in a gravitating system typically results in<br />

the emission of gravitational waves.<br />

synchronous orbit For a small body orbiting<br />

a more massive one, the orbital radius for which<br />

the orbital period is equal to the rotation period<br />

of the more massive body. A satellite in a zero<br />

inclination synchronous orbit above the equator<br />

will always appear to be above a particular point<br />

on the more massive body.<br />

synchronous rotation Rotation of a planet<br />

or other secondary body so that the same side<br />

always faces the primary; for instance, the moon<br />

rotates synchronously around the Earth. In the<br />

case of the moon, this is ensured by tidal locking;<br />

for commercial communications satellites, it is<br />

accomplished by active means, such as reaction<br />

wheels or thrusters.<br />

synchrotron radiation The radiation produced<br />

by a charged particle as it gyrates around<br />

magnetic field lines. The radiation is emitted<br />

at the gyrofrequency, ω = qB/γ mc, where q<br />

is the particle charge, B is the magnetic field<br />

strength, m is the particle mass, γ is the Lorentz<br />

factor, <strong>and</strong> c is the speed of light. For an electron<br />

we have ω = 1.76 × 10 7 Bγ. Synchrotron radiation<br />

from energetic electrons is an important<br />

production mechanism for microwave emission<br />

in the solar corona.<br />

synchrotron self-Compton mechanism A<br />

mechanism suggested for the production of high<br />

energy photons in radio loud active galactic nu-

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