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DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

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(at least), <strong>and</strong> different observers use different<br />

space <strong>and</strong> time coordinate functions. Although<br />

the notation {x,y,z} suggests rectangular coordinates,<br />

the constant x− surfaces can in fact<br />

be curved, for instance, if x is really the radius<br />

from the origin in a spherical coordinate system.<br />

In general, the coordinate functions can lead to<br />

curved constant-coordinate surfaces (curvilinear<br />

coordinates). Then the four spacetime coordinates<br />

form a set of functions, sayφ α (P) where<br />

φ α ,α= 0, 1, 2, 3 correspond to the time <strong>and</strong> the<br />

three spatial coordinate functions;P represents<br />

a point in spacetime.<br />

A coordinate system is closely related to a<br />

reference frame. For instance, one can align<br />

basis vectors (which constitute the frame) along<br />

the intersection of constant-coordinate surfaces,<br />

with some rule for assigning length or magnitude<br />

of the basis vectors.<br />

coordinate time Time defined relative to<br />

an inertial (in particular, nonrotating) reference<br />

frame, whose relationship with time measured<br />

on the surface of the Earth can be calculated<br />

using relativity (not to be confused with<br />

“coordinated time” like Coordinated Universal<br />

Time). General uses are “Geocentric Coordinate<br />

Time” (TCG) <strong>and</strong> “Barycentric Coordinate<br />

Time” (TCB), the latter referring to the solar<br />

system barycenter.<br />

coordinate transformation in special relativity<br />

The transformation of space-time coordinates<br />

between two reference systems that are<br />

moving uniformly with respect to each other.<br />

Classically, any physical system is composed of<br />

particles, <strong>and</strong> a full description of the system<br />

is obtained if all the positions of each particle<br />

are known for any given time. The position of<br />

each particle is represented by a trio of numbers<br />

whose value depends on the location of the reference<br />

system. Thus if two observers used two<br />

different systems of reference, then a coordinate<br />

transformation is needed in order to compare the<br />

observations. Classically time is considered to<br />

be an absolute variable; that is its value is the<br />

same regardless of the reference system. Thus,<br />

classical coordinate transformations transform<br />

an arbitrary trio of spatial coordinates at any<br />

given time. Special relativity states that the velocity<br />

of light is constant for two reference sys-<br />

© 2001 by CRC Press LLC<br />

core<br />

tems that are moving at constant velocities with<br />

respect to each other. In order for this to hold<br />

time can no longer be an absolute variable, <strong>and</strong><br />

its value must depend on the reference system.<br />

The universal character of the speed of light plus<br />

the assumption that space is homogeneous <strong>and</strong><br />

isotropic leads to the Lorentz transformation of<br />

space-time coordinates. The Lorentz transformations<br />

transform an arbitrary foursome of coordinates<br />

(three spatial coordinates plus time)<br />

from one system of reference to another that is<br />

moving uniformly with respect to the first.<br />

Copernicus, Nicholas Astronomer (1473–<br />

1543). Proposed that the sun, rather than the<br />

Earth, was the center of the solar system.<br />

coplanarity theorem In magnetohydrodynamics,<br />

the coplanarity theorem<br />

n · (Bd × Bu) = 0<br />

states that the shock normal n <strong>and</strong> the magnetic<br />

fields Bu <strong>and</strong> Bd in the upstream <strong>and</strong> downstream<br />

medium all lie in the same plane. The coplanarity<br />

theorem is a consequence of the jump<br />

conditions for the electromagnetic field at the<br />

shock as described by the Rankine–Hugoniot<br />

equations. See Rankine–Hugoniot relations.<br />

Cordelia Moon of Uranus also designated<br />

UV. Discovered by Voyager 2 in 1986, it is a<br />

small, irregular, body, approximately 13 km in<br />

radius. Its orbit has an eccentricity of 0, an inclination<br />

of 0.1 ◦ , a precession of 550 ◦ yr −1 , <strong>and</strong> a<br />

semimajor axis of 4.98 × 10 4 km. It is the inner<br />

shepherding satellite for Uranus’ epsilon ring.<br />

Its surface is very dark, with a geometric albedo<br />

of less than 0.1. Its mass has not been measured.<br />

It orbits Uranus once every 0.335 Earth days.<br />

cordillera An extensive chain of parallel<br />

mountains or mountain ranges, especially the<br />

principal mountain chain of a continent. The<br />

term was originally used to describe the parallel<br />

chains of mountains in South America (las<br />

Cordilleras de los Andes).<br />

core Differentiated central volume of the<br />

Earth <strong>and</strong> (some) other planets. Cores vary in<br />

composition, size, <strong>and</strong> physical state among the<br />

different solar system bodies. In geophysics,

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