| RAP,DAP | D | geocentric apparent |
|---|---|---|
| AOPRMS | D(14) | star-independent apparent-to-observed parameters: |
| (1) | geodetic latitude (radians) | |
| (2,3) | sine and cosine of geodetic latitude | |
| (4) | magnitude of diurnal aberration vector | |
| (5) | height (metres) | |
| (6) | ambient temperature (degrees K) | |
| (7) | pressure (mB) | |
| (8) | relative humidity (0-1) | |
| (9) | wavelength ( |
|
| (10) | lapse rate (degrees K per metre) | |
| (11,12) | refraction constants A and B (radians) | |
| (13) | longitude + eqn of equinoxes +
``sidereal |
|
| (14) | local apparent sidereal time (radians) |
| AOB | D | observed azimuth (radians: N=0, E= |
|---|---|---|
| ZOB | D | observed zenith distance (radians) |
| HOB | D | observed Hour Angle (radians) |
| DOB | D | observed Declination (radians) |
| ROB | D | observed Right Ascension (radians) |
for
. Even
at a topocentric zenith distance of
, the accuracy in elevation should be better than
1 arcminute; useful results are available for a further
, beyond which the sla_REFRO routine returns a
fixed value of the refraction. The complementary
routines sla_AOP (or sla_AOPQK) and sla_OAP (or sla_OAPQK)
are self-consistent to better than 1 microarcsecond all over
the celestial sphere.
SLALIB --- Positional Astronomy Library