# Declination

In astronomy declination (dec) is one of the two coordinates of the equatorial coordinate system, the other being either right ascension or hour angle. Dec is comparable to latitude, projected unto the celestial sphere, and is measured in degrees north of the celestial equator. Therefore, points north of the celestial equator have positive declination, while those to the south have negative declination.

Note that the sign must be included even if positive.

A celestial object that passes over zenith, has a declination equal to the observer's latitude, with northern latitudes yielding positive declinations. A pole star therefore has the declination +90 or -90. Conversely, celestial objects with a declination higher than [itex]90^o - l[itex], where l is the latitude, are visible the whole sidereal day. Such stars are called circumpolar, while the phenomenon of a sun not setting is called midnight sun.

 Contents

## Varying declination

The declination of all celestial objects vary over time, in different periods.

### Sun

The declination of the sun (Sun Dec) is the angle between the rays of the sun and the plane of the earth equator. Since the angle between the earth axis and the plane of the earth orbit is nearly constant, Sun Dec varies with the seasons and its period is one year, that is the time needed by the earth to complete its revolution around the sun.

When the projection of the earth axis on the plane of the earth orbit is on the same line linking the earth and the sun, the angle between the rays of the sun and the plane of the earth equator is maximum and its value is 2327'. This happens at the solstices. Therefore Sun Dec is +2327' at the northern hemisphere summer solstice and -2327' at the northern hemisphere winter solstice.

When the projection of the earth axis on the plane of the earth orbit is perpendicular to line linking the earth and the sun, the angle between the rays of the sun and the plane of the earth equator is null. This happens at the equinoxes. Therefore Sun Dec is 0 at the equinoxes.

Since the eccentricity of the earth orbit is quite low, it can be approximated to a circle, and Sun Dec is approximately given by the following expression:

[itex]\delta = -23.45^\circ \cdot \cos \left ( \frac{360}{365} \cdot \left ( N + 10 \right ) \right )[itex] if cos operates on degrees

[itex]\delta = -23.45^\circ \cdot \cos \left ( \frac{2\pi}{365} \cdot \left ( N + 10 \right ) \right )[itex] if cos operates on radians

where [itex]N[itex] is Day of the Year, that is the number of days spent since January 1.

The errors caused by this approximation are then contemplated by the Equation of Time.

A diagram demonstrating how the Sun's path over the celestial sphere changes with the varying declination during the year, marking the Azimuths in N where the sun rises and sets at summer and winter solstice at a place of 56N latitude.

### Moon

The Moon also has an annual cycle, with maximum declination at northern hemisphere midwinter and minimum at midsummer. There is also an approximately 19 year long cycle, varying the maximum declination from +2835' to +1818' and the minimum from -1818' to -2835'.

### Stars

The stars have approximately the same declination from year to year, but they do have proper motion that can be measured in whole degrees after the passing of centuries.

## See also

Declination is used in some contexts that rule out astronomical declination, to mean the same as magnetic declination.

Declination is occasionally and erroneously used to refer to the linguistic term declension.bg:Деклинация cs:Deklinace de:Deklination (Astronomie) fr:Dclinaison (astronomie) it:Declinazione (astronomia) nl:Declinatie nn:Deklinasjon ja:赤緯 pl:Deklinacja (astronomia) fi:Deklinaatio

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