Azimuth and altitude

In the common convention used by Horizons, azimuth increases eastward from true north: north 0°, east 90°, south 180° and west 270°. Altitude is measured above the local horizon toward a 90° zenith.

Other software can use different origins or signs, so conventions must be checked. Azimuth is not geographic longitude, and angular altitude is not elevation in metres above sea level.

References: [1] [2]

One catalogue direction, different local positions

Earth’s rotation changes a star’s altitude and azimuth. Changing observer latitude or longitude also changes the local direction at a given time.

Transforming RA and declination consequently requires an observing site and time. Catalogue coordinates alone usually cannot determine where an observer should point a telescope.

References: [2] [1]

Apparent directions and equipment

Horizons apparent azimuth and elevation include relevant light-time and directional corrections, with optional approximate atmospheric refraction. Refracted and airless outputs describe different conditions.

An alt-azimuth mount drives two axes. Near the zenith, azimuth can change rapidly enough to exceed mechanical tracking rates. Coordinate geometry and equipment limits jointly affect continuous observations.

References: [1] [2]