Because
astronomical objects are at such remote distances, casual observation of the
sky offers no information on their actual distances. All celestial objects seem
equally far away, as if
fixed onto the inside of a
sphere with a large but unknown radius, which
appears to rotate westward overhead; meanwhile,
Earth underfoot seems to remain still. For purposes of
spherical astronomy, which is concerned only with the
directions to celestial objects, it makes no difference if this is actually the case or if it is Earth that is
rotating while the celestial sphere is stationary. The celestial sphere can be considered to be
infinite in
radius. This means any
point within it, including that occupied by the observer, can be considered the
center. It also means that all
parallel lines, be they
millimetres apart or across the
Solar System from each other, will seem to intersect the sphere at a single point, analogous to the
vanishing point of
graphical perspective. All parallel
planes will seem to intersect the sphere in a coincident
great circle (a "vanishing circle"). Conversely, observers looking toward the same point on an infinite-radius celestial sphere will be looking along parallel lines, and observers looking toward the same great circle, along parallel planes. On an infinite-radius celestial sphere, all observers see the same things in the same direction. For some objects, this is over-simplified. Objects which are relatively near to the observer (for instance, the
Moon) will seem to change position against the distant celestial sphere if the observer moves far enough, say, from one side of planet Earth to the other. This effect, known as
parallax, can be represented as a small offset from a mean position. The celestial sphere can be considered to be centered at the
Earth's center, the
Sun's center, or any other convenient location, and offsets from positions referred to these centers can be calculated. In this way,
astronomers can predict
geocentric or
heliocentric positions of objects on the celestial sphere, without the need to calculate the individual
geometry of any particular observer, and the utility of the celestial sphere is maintained. Individual observers can work out their own small offsets from the mean positions, if necessary. In many cases in astronomy, the offsets are insignificant.
Determining location of objects The celestial sphere can thus be thought of as a kind of astronomical
shorthand, and is applied very frequently by astronomers. For instance, the
Astronomical Almanac for 2010 lists the apparent geocentric position of the
Moon on January 1 at 00:00:00.00
Terrestrial Time, in
equatorial coordinates, as
right ascension 6h 57m 48.86s,
declination +23° 30' 05.5". Implied in this position is that it is as projected onto the celestial sphere; any observer at any location looking in that direction would see the "geocentric Moon" in the same place against the stars. For many rough uses (e.g. calculating an approximate phase of the Moon), this position, as seen from the Earth's center, is adequate. For applications requiring precision (e.g. calculating the shadow path of an
eclipse), the
Almanac gives formulae and methods for calculating the
topocentric coordinates, that is, as seen from a particular place on the Earth's surface, based on the geocentric position. This greatly abbreviates the amount of detail necessary in such almanacs, as each observer can handle their own specific circumstances. == Greek history on celestial spheres ==