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Spherical astronomy

From Wikipedia, the free encyclopedia
Branch of astronomy about the celestial sphere
Diagram of several terms in positional astronomy

Spherical astronomy, orpositional astronomy, is a branch ofobservational astronomy used to locateastronomical objects on thecelestial sphere, as seen at a particular date, time, and location onEarth. It relies on the mathematical methods ofspherical trigonometry and the measurements ofastrometry.

This is the oldest branch of astronomy and dates back toantiquity. Observations of celestial objects have been, and continue to be, important for religious andastrological purposes, as well as fortimekeeping andnavigation. The science of actually measuring positions of celestial objects in the sky is known as astrometry.

The primary elements of spherical astronomy arecelestial coordinate systems and time. The coordinates of objects on the sky are listed using theequatorial coordinate system, which is based on the projection of Earth'sequator onto the celestial sphere. The position of an object in this system is given in terms ofright ascension (α) anddeclination (δ). The latitude and local time can then be used to derive the position of the object in thehorizontal coordinate system, consisting of thealtitude andazimuth.

The coordinates of celestial objects such asstars andgalaxies are tabulated in astar catalog, which gives the position for a particular year. However, the combined effects ofaxial precession andnutation will cause the coordinates to change slightly over time. The effects of these changes in Earth's motion are compensated by the periodic publication of revised catalogs.

To determine the position of theSun andplanets, an astronomicalephemeris (a table of values that gives the positions of astronomical objects in the sky at a given time) is used, which can then be converted into suitable real-world coordinates.

Theunaided human eye can perceive about 6,000 stars, of which about half are below thehorizon at any one time. On modernstar charts, thecelestial sphere is divided into88 constellations. Every star lies within aconstellation. Constellations are useful for navigation.Polaris lies nearly due north to an observer in theNorthern Hemisphere. Thispole star is always ata position nearlydirectly above theNorth Pole.

Positional phenomena

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  • Planets which are inconjunction form a line which passes through the center of theSolar System.
  • Theecliptic is theplane which contains the orbit of a planet, usually in reference toEarth.
  • Elongation refers to theangle formed by a planet, with respect to the system's center and a viewingpoint.
    • Aquadrature occurs when the position of a body (moon or planet) is such that its elongation is 90° or 270°; i.e. the body-earth-sun angle is 90°
  • Superior planets have a largerorbit than Earth's, while theinferior planets (Mercury and Venus) orbit the Sun inside Earth's orbit.
  • Atransit may occur when an inferior planet passes through a point of conjunction.

Ancient structures associated with positional astronomy include

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Main article:Archaeoastronomy

See also

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References

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  • Robin M. Green,Spherical Astronomy,1985, Cambridge University Press,ISBN 0-521-31779-7
  • William M. Smart, edited by Robin M. Green,Textbook on Spherical Astronomy,1977, Cambridge University Press,ISBN 0-521-29180-1. (This classic text has been re-issued)

External links

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Software
  • NOVAS is an integrated package of subroutines for the computation of a wide variety of common astrometric quantities and transformations, in Fortran and C, from the U.S. Naval Observatory.
  • jNOVAS is a java wrapper for library developed and distributed by The United States Naval Meteorology and Oceanography Command (NMOC) with included JPL planetary and lunar ephemeris DE421 binary file published by the Jet Propulsion Laboratory.
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