Equatorial coordinate system
Encyclopedia : E : EQ : EQU : Equatorial coordinate system
The equatorial coordinate system is probably the most widely used celestial coordinate system, whose equatorial coordinates are:
- declination ([\delta])
- right ascension ([\alpha]) -also RA-, or hour angle ([H]) -also HA-
There are two varieties:
- the hour angle system is fixed to the Earth like the geographic coordinate system
- the right ascension system is fixed to the stars (actually, not quite, see precession and nutation). Thus, during a night or a few nights, it appears to rotate across the sky with the stars, but of course it's really the Earth rotating under the fixed sky. Because of the precession and nutation just referred to, when considering long intervals between observations it is necessary to specify an epoch (frequently J2000.0, for older data B1950.0) when specifying coordinates of planets, stars, galaxies, etc.

The latitudinal (latitude-like) angle of the equatorial system is called declination (Dec for short). It measures the angle of an object above or below the celestial equator. The longitudinal angle is called the right ascension (RA for short). It measures the angle of an object east of the vernal equinox point. Unlike longitude, right ascension is usually measured in hours instead of degrees, because the apparent rotation of the equatorial coordinate system is closely related to sidereal time and hour angle. Since a full rotation of the sky takes 24 hours to complete, there are (360 degrees / 24 hours) = 15 degrees in one hour of right ascension.
The equatorial coordinate system is commonly used by telescopes equipped equatorial mounts by employing Setting circles. Setting circles in conjunction with a star chart or ephemeris allow a telescope to be easily pointed at known objects on the celestial sphere.
This article originates from Jason Harris' Astroinfo which comes along with KStars, a Desktop Planetarium for Linux/KDE. See http://edu.kde.org/kstars/index.phtml
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