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authorJoe Hunkeler <jhunkeler@gmail.com>2015-08-11 16:51:37 -0400
committerJoe Hunkeler <jhunkeler@gmail.com>2015-08-11 16:51:37 -0400
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+.help aop Jun99 "Slalib Package"
+.nf
+
+ SUBROUTINE slAOP (RAP, DAP, DATE, DUT, ELONGM, PHIM, HM,
+ : XP, YP, TDK, PMB, RH, WL, TLR,
+ : AOB, ZOB, HOB, DOB, ROB)
+
+ - - - -
+ A O P
+ - - - -
+
+ Apparent to observed place, for optical sources distant from
+ the solar system.
+
+ Given:
+ RAP d geocentric apparent right ascension
+ DAP d geocentric apparent declination
+ DATE d UTC date/time (Modified Julian Date, JD-2400000.5)
+ DUT d delta UT: UT1-UTC (UTC seconds)
+ ELONGM d mean longitude of the observer (radians, east +ve)
+ PHIM d mean geodetic latitude of the observer (radians)
+ HM d observer's height above sea level (metres)
+ XP d polar motion x-coordinate (radians)
+ YP d polar motion y-coordinate (radians)
+ TDK d local ambient temperature (DegK; std=273.155D0)
+ PMB d local atmospheric pressure (mB; std=1013.25D0)
+ RH d local relative humidity (in the range 0D0-1D0)
+ WL d effective wavelength (micron, e.g. 0.55D0)
+ TLR d tropospheric lapse rate (DegK/metre, e.g. 0.0065D0)
+
+ Returned:
+ AOB d observed azimuth (radians: N=0,E=90)
+ ZOB d observed zenith distance (radians)
+ HOB d observed Hour Angle (radians)
+ DOB d observed Declination (radians)
+ ROB d observed Right Ascension (radians)
+
+ Notes:
+
+ 1) This routine returns zenith distance rather than elevation
+ in order to reflect the fact that no allowance is made for
+ depression of the horizon.
+
+ 2) The accuracy of the result is limited by the corrections for
+ refraction. Providing the meteorological parameters are
+ known accurately and there are no gross local effects, the
+ predicted apparent RA,Dec should be within about 0.1 arcsec
+ for a zenith distance of less than 70 degrees. Even at a
+ topocentric zenith distance of 90 degrees, the accuracy in
+ elevation should be better than 1 arcmin; useful results
+ are available for a further 3 degrees, beyond which the
+ slRFRO routine returns a fixed value of the refraction.
+ The complementary routines slAOP (or slAOPQ) and slOAP
+ (or slOAPQ) are self-consistent to better than 1 micro-
+ arcsecond all over the celestial sphere.
+
+ 3) It is advisable to take great care with units, as even
+ unlikely values of the input parameters are accepted and
+ processed in accordance with the models used.
+
+ 4) "Apparent" place means the geocentric apparent right ascension
+ and declination, which is obtained from a catalogue mean place
+ by allowing for space motion, parallax, precession, nutation,
+ annual aberration, and the Sun's gravitational lens effect. For
+ star positions in the FK5 system (i.e. J2000), these effects can
+ be applied by means of the slMAP etc routines. Starting from
+ other mean place systems, additional transformations will be
+ needed; for example, FK4 (i.e. B1950) mean places would first
+ have to be converted to FK5, which can be done with the
+ slFK45 etc routines.
+
+ 5) "Observed" Az,El means the position that would be seen by a
+ perfect theodolite located at the observer. This is obtained
+ from the geocentric apparent RA,Dec by allowing for Earth
+ orientation and diurnal aberration, rotating from equator
+ to horizon coordinates, and then adjusting for refraction.
+ The HA,Dec is obtained by rotating back into equatorial
+ coordinates, using the geodetic latitude corrected for polar
+ motion, and is the position that would be seen by a perfect
+ equatorial located at the observer and with its polar axis
+ aligned to the Earth's axis of rotation (n.b. not to the
+ refracted pole). Finally, the RA is obtained by subtracting
+ the HA from the local apparent ST.
+
+ 6) To predict the required setting of a real telescope, the
+ observed place produced by this routine would have to be
+ adjusted for the tilt of the azimuth or polar axis of the
+ mounting (with appropriate corrections for mount flexures),
+ for non-perpendicularity between the mounting axes, for the
+ position of the rotator axis and the pointing axis relative
+ to it, for tube flexure, for gear and encoder errors, and
+ finally for encoder zero points. Some telescopes would, of
+ course, exhibit other properties which would need to be
+ accounted for at the appropriate point in the sequence.
+
+ 7) This routine takes time to execute, due mainly to the
+ rigorous integration used to evaluate the refraction.
+ For processing multiple stars for one location and time,
+ call slAOPA once followed by one call per star to slAOPQ.
+ Where a range of times within a limited period of a few hours
+ is involved, and the highest precision is not required, call
+ slAOPA once, followed by a call to slAOPT each time the
+ time changes, followed by one call per star to slAOPQ.
+
+ 8) The DATE argument is UTC expressed as an MJD. This is,
+ strictly speaking, wrong, because of leap seconds. However,
+ as long as the delta UT and the UTC are consistent there
+ are no difficulties, except during a leap second. In this
+ case, the start of the 61st second of the final minute should
+ begin a new MJD day and the old pre-leap delta UT should
+ continue to be used. As the 61st second completes, the MJD
+ should revert to the start of the day as, simultaneously,
+ the delta UTC changes by one second to its post-leap new value.
+
+ 9) The delta UT (UT1-UTC) is tabulated in IERS circulars and
+ elsewhere. It increases by exactly one second at the end of
+ each UTC leap second, introduced in order to keep delta UT
+ within +/- 0.9 seconds.
+
+ 10) IMPORTANT -- TAKE CARE WITH THE LONGITUDE SIGN CONVENTION.
+ The longitude required by the present routine is east-positive,
+ in accordance with geographical convention (and right-handed).
+ In particular, note that the longitudes returned by the
+ slOBS routine are west-positive, following astronomical
+ usage, and must be reversed in sign before use in the present
+ routine.
+
+ 11) The polar coordinates XP,YP can be obtained from IERS
+ circulars and equivalent publications. The maximum amplitude
+ is about 0.3 arcseconds. If XP,YP values are unavailable,
+ use XP=YP=0D0. See page B60 of the 1988 Astronomical Almanac
+ for a definition of the two angles.
+
+ 12) The height above sea level of the observing station, HM,
+ can be obtained from the Astronomical Almanac (Section J
+ in the 1988 edition), or via the routine slOBS. If P,
+ the pressure in millibars, is available, an adequate
+ estimate of HM can be obtained from the expression
+
+ HM ~ -29.3D0*TSL*LOG(P/1013.25D0).
+
+ where TSL is the approximate sea-level air temperature in
+ deg K (see Astrophysical Quantities, C.W.Allen, 3rd edition,
+ section 52.) Similarly, if the pressure P is not known,
+ it can be estimated from the height of the observing
+ station, HM as follows:
+
+ P ~ 1013.25D0*EXP(-HM/(29.3D0*TSL)).
+
+ Note, however, that the refraction is proportional to the
+ pressure and that an accurate P value is important for
+ precise work.
+
+ 13) The azimuths etc produced by the present routine are with
+ respect to the celestial pole. Corrections to the terrestrial
+ pole can be computed using slPLMO.
+
+ Called: slAOPA, slAOPQ
+
+ P.T.Wallace Starlink 9 June 1998
+
+ Copyright (C) 1998 Rutherford Appleton Laboratory
+ Copyright (C) 1995 Association of Universities for Research in Astronomy Inc.
+
+.fi
+.endhelp