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author | Joseph Hunkeler <jhunkeler@gmail.com> | 2015-07-08 20:46:52 -0400 |
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committer | Joseph Hunkeler <jhunkeler@gmail.com> | 2015-07-08 20:46:52 -0400 |
commit | fa080de7afc95aa1c19a6e6fc0e0708ced2eadc4 (patch) | |
tree | bdda434976bc09c864f2e4fa6f16ba1952b1e555 /math/slalib/doc/aop.hlp | |
download | iraf-linux-fa080de7afc95aa1c19a6e6fc0e0708ced2eadc4.tar.gz |
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diff --git a/math/slalib/doc/aop.hlp b/math/slalib/doc/aop.hlp new file mode 100644 index 00000000..dc3343bf --- /dev/null +++ b/math/slalib/doc/aop.hlp @@ -0,0 +1,166 @@ +.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 |