| TYPE | C*(*) | type of coordinates - `R', `H' or `A' (see below) |
|---|---|---|
| OB1 | D | observed Az, HA or RA (radians; Az is N=0, E= |
| OB2 | D | observed zenith distance or |
| 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 (HM) | |
| (6) | ambient temperature (TDK) | |
| (7) | pressure (PMB) | |
| (8) | relative humidity (RH) | |
| (9) | wavelength (WL) | |
| (10) | lapse rate (TLR) | |
| (11,12) | refraction constants A and B (radians) | |
| (13) | longitude + eqn of equinoxes +
``sidereal |
|
| (14) | local apparent sidereal time (radians) |
| RAP,DAP | D | geocentric apparent |
|---|
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