Measuring north and south of the equator

The celestial equator has declination zero, the north pole +90 degrees and the south pole −90 degrees. The angle is measured along the target’s hour circle in degrees, arcminutes and arcseconds.

The analogy with terrestrial latitude concerns direction, not a geographic location of the source on Earth. Declination also supplies no radial distance.

References: [1] [2]

Combining declination with RA

Declination alone selects a circle parallel to the celestial equator without locating a target along it. RA supplies the longitudinal coordinate needed for an ordinary equatorial direction.

NASA illustrates the pair using approximately RA 6 h 45 m and declination −16°43′ for Sirius. Rounded educational values are not a substitute for frame-, epoch- and motion-labelled pointing data.

References: [2] [3]

Declination is not local altitude

Negative declination means south of the celestial equator, not necessarily below an observer’s horizon. Visibility also depends on latitude, time and local conditions.

A target’s altitude rises and falls during Earth’s rotation while its catalogue declination is approximately stable over a short interval. Local pointing requires RA, site, time and the relevant corrections as well.

References: [2] [4]