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+ SUBROUTINE sla_UE2EL (U, JFORMR,
+ : JFORM, EPOCH, ORBINC, ANODE, PERIH,
+ : AORQ, E, AORL, DM, JSTAT)
+*+
+* - - - - - -
+* U E 2 E L
+* - - - - - -
+*
+* Transform universal elements into conventional heliocentric
+* osculating elements.
+*
+* Given:
+* U d(13) universal orbital elements (Note 1)
+*
+* (1) combined mass (M+m)
+* (2) total energy of the orbit (alpha)
+* (3) reference (osculating) epoch (t0)
+* (4-6) position at reference epoch (r0)
+* (7-9) velocity at reference epoch (v0)
+* (10) heliocentric distance at reference epoch
+* (11) r0.v0
+* (12) date (t)
+* (13) universal eccentric anomaly (psi) of date, approx
+*
+* JFORMR i requested element set (1-3; Note 3)
+*
+* Returned:
+* JFORM d element set actually returned (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)
+* JSTAT i status: 0 = OK
+* -1 = illegal combined mass
+* -2 = illegal JFORMR
+* -3 = position/velocity out of range
+*
+* Notes
+*
+* 1 The "universal" elements are those which define the orbit for the
+* purposes of the method of universal variables (see reference 2).
+* They consist of the combined mass of the two bodies, an epoch,
+* and the position and velocity vectors (arbitrary reference frame)
+* at that epoch. The parameter set used here includes also various
+* quantities that can, in fact, be derived from the other
+* information. This approach is taken to avoiding unnecessary
+* computation and loss of accuracy. The supplementary quantities
+* are (i) alpha, which is proportional to the total energy of the
+* orbit, (ii) the heliocentric distance at epoch, (iii) the
+* outwards component of the velocity at the given epoch, (iv) an
+* estimate of psi, the "universal eccentric anomaly" at a given
+* date and (v) that date.
+*
+* 2 The universal elements are with respect to the mean equator and
+* equinox of epoch J2000. The orbital elements produced are with
+* respect to the J2000 ecliptic and mean equinox.
+*
+* 3 Three different element-format options are supported:
+*
+* 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
+*
+* 4 It may not be possible to generate elements in the form
+* requested through JFORMR. The caller is notified of the form
+* of elements actually returned by means of the JFORM argument:
+*
+* JFORMR JFORM meaning
+*
+* 1 1 OK - elements are in the requested format
+* 1 2 never happens
+* 1 3 orbit not elliptical
+*
+* 2 1 never happens
+* 2 2 OK - elements are in the requested format
+* 2 3 orbit not elliptical
+*
+* 3 1 never happens
+* 3 2 never happens
+* 3 3 OK - elements are in the requested format
+*
+* 5 The arguments returned for each value of JFORM (cf Note 6: JFORM
+* may not be the same as JFORMR) are as follows:
+*
+* JFORM 1 2 3
+* EPOCH t0 t0 T
+* ORBINC i i i
+* ANODE Omega Omega Omega
+* PERIH curly pi omega omega
+* AORQ a a q
+* E e e e
+* AORL L M -
+* DM n - -
+*
+* where:
+*
+* t0 is the epoch of the elements (MJD, TT)
+* T " epoch of perihelion (MJD, TT)
+* i " inclination (radians)
+* Omega " longitude of the ascending node (radians)
+* curly pi " longitude of perihelion (radians)
+* omega " argument of perihelion (radians)
+* a " mean distance (AU)
+* q " perihelion distance (AU)
+* e " eccentricity
+* L " longitude (radians, 0-2pi)
+* M " mean anomaly (radians, 0-2pi)
+* n " daily motion (radians)
+* - means no value is set
+*
+* 6 At very small inclinations, the longitude of the ascending node
+* ANODE becomes indeterminate and under some circumstances may be
+* set arbitrarily to zero. Similarly, if the orbit is close to
+* circular, the true anomaly becomes indeterminate and under some
+* circumstances may be set arbitrarily to zero. In such cases,
+* the other elements are automatically adjusted to compensate,
+* and so the elements remain a valid description of the orbit.
+*
+* References:
+*
+* 1 Sterne, Theodore E., "An Introduction to Celestial Mechanics",
+* Interscience Publishers Inc., 1960. Section 6.7, p199.
+*
+* 2 Everhart, E. & Pitkin, E.T., Am.J.Phys. 51, 712, 1983.
+*
+* Called: sla_PV2EL
+*
+* P.T.Wallace Starlink 18 March 1999
+*
+* Copyright (C) 1999 Rutherford Appleton Laboratory
+*-
+
+ IMPLICIT NONE
+
+ DOUBLE PRECISION U(13)
+ INTEGER JFORMR,JFORM
+ DOUBLE PRECISION EPOCH,ORBINC,ANODE,PERIH,AORQ,E,AORL,DM
+ INTEGER JSTAT
+
+* Gaussian gravitational constant (exact)
+ DOUBLE PRECISION GCON
+ PARAMETER (GCON=0.01720209895D0)
+
+* Canonical days to seconds
+ DOUBLE PRECISION CD2S
+ PARAMETER (CD2S=GCON/86400D0)
+
+ INTEGER I
+ DOUBLE PRECISION PMASS,DATE,PV(6)
+
+
+* Unpack the universal elements.
+ PMASS = U(1)-1D0
+ DATE = U(3)
+ DO I=1,3
+ PV(I) = U(I+3)
+ PV(I+3) = U(I+6)*CD2S
+ END DO
+
+* Convert the position and velocity etc into conventional elements.
+ CALL sla_PV2EL(PV,DATE,PMASS,JFORMR,JFORM,EPOCH,ORBINC,ANODE,
+ : PERIH,AORQ,E,AORL,DM,JSTAT)
+
+ END