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authorJoseph Hunkeler <jhunkeler@gmail.com>2015-07-08 20:46:52 -0400
committerJoseph Hunkeler <jhunkeler@gmail.com>2015-07-08 20:46:52 -0400
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+.help plante Jun99 "Slalib Package"
+.nf
+
+ SUBROUTINE slPLTE (DATE, ELONG, PHI, JFORM, EPOCH,
+ : ORBINC, ANODE, PERIH, AORQ, E,
+ : AORL, DM, RA, DEC, R, JSTAT)
+
+ - - - - - - -
+ P L T E
+ - - - - - - -
+
+ Topocentric apparent RA,Dec of a Solar-System object whose
+ heliocentric orbital elements are known.
+
+ Given:
+ DATE d MJD of observation (JD - 2400000.5)
+ ELONG d observer's east longitude (radians)
+ PHI d observer's geodetic latitude (radians)
+ JFORM i choice of element set (1-3; Note 4)
+ EPOCH d epoch of elements (TT MJD)
+ ORBINC d inclination (radians)
+ ANODE d longitude of the ascending node (radians)
+ PERIH d longitude or argument of perihelion (radians)
+ AORQ d mean distance or perihelion distance (AU)
+ E d eccentricity
+ AORL d mean anomaly or longitude (radians, JFORM=1,2 only)
+ DM d daily motion (radians, JFORM=1 only )
+
+ Returned:
+ RA,DEC d RA, Dec (topocentric apparent, radians)
+ R d distance from observer (AU)
+ JSTAT i status: 0 = OK
+ -1 = illegal JFORM
+ -2 = illegal E
+ -3 = illegal AORQ
+ -4 = illegal DM
+ -5 = numerical error
+
+ Notes:
+
+ 1 DATE is the instant for which the prediction is required. It is
+ in the TT timescale (formerly Ephemeris Time, ET) and is a
+ Modified Julian Date (JD-2400000.5).
+
+ 2 The longitude and latitude allow correction for geocentric
+ parallax. This is usually a small effect, but can become
+ important for Earth-crossing asteroids. Geocentric positions
+ can be generated by appropriate use of routines slEVP and
+ slPLNE.
+
+ 3 The elements are with respect to the J2000 ecliptic and equinox.
+
+ 4 Three different element-format options are available:
+
+ Option JFORM=1, suitable for the major planets:
+
+ EPOCH = epoch of elements (TT MJD)
+ ORBINC = inclination i (radians)
+ ANODE = longitude of the ascending node, big omega (radians)
+ PERIH = longitude of perihelion, curly pi (radians)
+ AORQ = mean distance, a (AU)
+ E = eccentricity, e
+ AORL = mean longitude L (radians)
+ DM = daily motion (radians)
+
+ Option JFORM=2, suitable for minor planets:
+
+ EPOCH = epoch of elements (TT MJD)
+ ORBINC = inclination i (radians)
+ ANODE = longitude of the ascending node, big omega (radians)
+ PERIH = argument of perihelion, little omega (radians)
+ AORQ = mean distance, a (AU)
+ E = eccentricity, e
+ AORL = mean anomaly M (radians)
+
+ Option JFORM=3, suitable for comets:
+
+ EPOCH = epoch of perihelion (TT MJD)
+ ORBINC = inclination i (radians)
+ ANODE = longitude of the ascending node, big omega (radians)
+ PERIH = argument of perihelion, little omega (radians)
+ AORQ = perihelion distance, q (AU)
+ E = eccentricity, e
+
+ 5 Unused elements (DM for JFORM=2, AORL and DM for JFORM=3) are
+ not accessed.
+
+ Called: slGMST, slDT, slEPJ, slPVOB, slPRNU,
+ slPLNE, slDMXV, slDC2S, slDA2P
+
+ P.T.Wallace Starlink 17 March 1999
+
+ Copyright (C) 1999 Rutherford Appleton Laboratory
+ Copyright (C) 1995 Association of Universities for Research in Astronomy Inc.
+
+.fi
+.endhelp