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authorJoseph Hunkeler <jhunkeler@gmail.com>2015-03-04 21:21:30 -0500
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+<H2><A NAME="SECTION0004174000000000000000">SLA_UE2EL - Universal to Conventional Elements</A>
+<A NAME="xref_SLA_UE2EL">&#160;</A><A NAME="SLA_UE2EL">&#160;</A>
+</H2>
+ <DL>
+<DT><STRONG>ACTION:</STRONG>
+<DD>Transform universal elements into conventional heliocentric
+osculating elements.
+<P> <DT><STRONG>CALL:</STRONG>
+<DD><TT>CALL sla_UE2EL (
+ U, JFORMR,
+ JFORM, EPOCH, ORBINC, ANODE, PERIH,
+ AORQ, E, AORL, DM, JSTAT)</TT>
+<P> </DL>
+<P> <DL>
+<DT><STRONG>GIVEN:</STRONG>
+<DD>
+<BR>
+<TABLE CELLPADDING=3>
+<TR VALIGN="TOP"><TD ALIGN="LEFT"><EM>U</EM></TD>
+<TH ALIGN="LEFT"><B>D(13)</B></TH>
+<TD ALIGN="LEFT" NOWRAP>universal orbital elements (updated; Note&nbsp;1)</TD>
+</TR>
+<TR VALIGN="TOP"><TD ALIGN="CENTER" NOWRAP COLSPAN=1>(1)</TD>
+<TD></TD>
+<TD ALIGN="LEFT" NOWRAP>combined mass (<I>M</I>+<I>m</I>)</TD>
+</TR>
+<TR VALIGN="TOP"><TD ALIGN="CENTER" NOWRAP COLSPAN=1>(2)</TD>
+<TD></TD>
+<TD ALIGN="LEFT" NOWRAP>total energy of the orbit (<IMG WIDTH="13" HEIGHT="14" ALIGN="BOTTOM" BORDER="0"
+ SRC="img24.gif"
+ ALT="$\alpha$">)</TD>
+</TR>
+<TR VALIGN="TOP"><TD ALIGN="CENTER" NOWRAP COLSPAN=1>(3)</TD>
+<TD></TD>
+<TD ALIGN="LEFT" NOWRAP>reference (osculating) epoch (<I>t<SUB>0</SUB></I>)</TD>
+</TR>
+<TR VALIGN="TOP"><TD ALIGN="CENTER" NOWRAP COLSPAN=1>(4-6)</TD>
+<TD></TD>
+<TD ALIGN="LEFT" NOWRAP>position at reference epoch (<IMG WIDTH="17" HEIGHT="25" ALIGN="MIDDLE" BORDER="0"
+ SRC="img102.gif"
+ ALT="${\rm \bf r}_0$">)</TD>
+</TR>
+<TR VALIGN="TOP"><TD ALIGN="CENTER" NOWRAP COLSPAN=1>(7-9)</TD>
+<TD></TD>
+<TD ALIGN="LEFT" NOWRAP>velocity at reference epoch (<IMG WIDTH="19" HEIGHT="25" ALIGN="MIDDLE" BORDER="0"
+ SRC="img103.gif"
+ ALT="${\rm \bf v}_0$">)</TD>
+</TR>
+<TR VALIGN="TOP"><TD ALIGN="CENTER" NOWRAP COLSPAN=1>(10)</TD>
+<TD></TD>
+<TD ALIGN="LEFT" NOWRAP>heliocentric distance at reference epoch</TD>
+</TR>
+<TR VALIGN="TOP"><TD ALIGN="CENTER" NOWRAP COLSPAN=1>(11)</TD>
+<TD></TD>
+<TD ALIGN="LEFT" NOWRAP><IMG WIDTH="39" HEIGHT="25" ALIGN="MIDDLE" BORDER="0"
+ SRC="img104.gif"
+ ALT="${\rm \bf r}_0.{\rm \bf v}_0$"></TD>
+</TR>
+<TR VALIGN="TOP"><TD ALIGN="CENTER" NOWRAP COLSPAN=1>(12)</TD>
+<TD></TD>
+<TD ALIGN="LEFT" NOWRAP>date (<I>t</I>)</TD>
+</TR>
+<TR VALIGN="TOP"><TD ALIGN="CENTER" NOWRAP COLSPAN=1>(13)</TD>
+<TD></TD>
+<TD ALIGN="LEFT" NOWRAP>universal eccentric anomaly (<IMG WIDTH="14" HEIGHT="27" ALIGN="MIDDLE" BORDER="0"
+ SRC="img105.gif"
+ ALT="$\psi$">) of date, approx</TD>
+</TR>
+<TR VALIGN="TOP"><TD ALIGN="LEFT">&nbsp;</TD>
+<TD ALIGN="LEFT">&nbsp;</TD>
+<TD ALIGN="LEFT" NOWRAP>&nbsp;</TD>
+</TR>
+<TR VALIGN="TOP"><TD ALIGN="LEFT"><EM>JFORMR</EM></TD>
+<TD ALIGN="LEFT"><B>I</B></TD>
+<TD ALIGN="LEFT" NOWRAP>requested element set (1-3; Note&nbsp;3)</TD>
+</TR>
+</TABLE></DL>
+<P> <DL>
+<DT><STRONG>RETURNED:</STRONG>
+<DD>
+<BR>
+<TABLE CELLPADDING=3>
+<TR VALIGN="TOP"><TD ALIGN="LEFT"><EM>JFORM</EM></TD>
+<TH ALIGN="LEFT"><B>I</B></TH>
+<TD ALIGN="LEFT" NOWRAP>element set actually returned (1-3; Note&nbsp;4)</TD>
+</TR>
+<TR VALIGN="TOP"><TD ALIGN="LEFT"><EM>EPOCH</EM></TD>
+<TD ALIGN="LEFT"><B>D</B></TD>
+<TD ALIGN="LEFT" NOWRAP>epoch of elements (<I>t<SUB>0</SUB></I> or <I>T</I>, TT MJD)</TD>
+</TR>
+<TR VALIGN="TOP"><TD ALIGN="LEFT"><EM>ORBINC</EM></TD>
+<TD ALIGN="LEFT"><B>D</B></TD>
+<TD ALIGN="LEFT" NOWRAP>inclination (<I>i</I>, radians)</TD>
+</TR>
+<TR VALIGN="TOP"><TD ALIGN="LEFT"><EM>ANODE</EM></TD>
+<TD ALIGN="LEFT"><B>D</B></TD>
+<TD ALIGN="LEFT" NOWRAP>longitude of the ascending node (<IMG WIDTH="14" HEIGHT="13" ALIGN="BOTTOM" BORDER="0"
+ SRC="img99.gif"
+ ALT="$\Omega$">, radians)</TD>
+</TR>
+<TR VALIGN="TOP"><TD ALIGN="LEFT"><EM>PERIH</EM></TD>
+<TD ALIGN="LEFT"><B>D</B></TD>
+<TD ALIGN="LEFT" NOWRAP>longitude or argument of perihelion
+(<IMG WIDTH="16" HEIGHT="14" ALIGN="BOTTOM" BORDER="0"
+ SRC="img100.gif"
+ ALT="$\varpi$"> or <IMG WIDTH="13" HEIGHT="14" ALIGN="BOTTOM" BORDER="0"
+ SRC="img101.gif"
+ ALT="$\omega$">,</TD>
+</TR>
+<TR VALIGN="TOP"><TD ALIGN="LEFT"><EM></EM></TD>
+<TD ALIGN="LEFT"><B></B></TD>
+<TD ALIGN="LEFT" NOWRAP> radians)</TD>
+</TR>
+<TR VALIGN="TOP"><TD ALIGN="LEFT"><EM>AORQ</EM></TD>
+<TD ALIGN="LEFT"><B>D</B></TD>
+<TD ALIGN="LEFT" NOWRAP>mean distance or perihelion distance (<I>a</I> or <I>q</I>, AU)</TD>
+</TR>
+<TR VALIGN="TOP"><TD ALIGN="LEFT"><EM>E</EM></TD>
+<TD ALIGN="LEFT"><B>D</B></TD>
+<TD ALIGN="LEFT" NOWRAP>eccentricity (<I>e</I>)</TD>
+</TR>
+<TR VALIGN="TOP"><TD ALIGN="LEFT"><EM>AORL</EM></TD>
+<TD ALIGN="LEFT"><B>D</B></TD>
+<TD ALIGN="LEFT" NOWRAP>mean anomaly or longitude
+(<I>M</I> or <I>L</I>, radians,</TD>
+</TR>
+<TR VALIGN="TOP"><TD ALIGN="LEFT"><EM></EM></TD>
+<TD ALIGN="LEFT"><B></B></TD>
+<TD ALIGN="LEFT" NOWRAP> JFORM=1,2 only)</TD>
+</TR>
+<TR VALIGN="TOP"><TD ALIGN="LEFT"><EM>DM</EM></TD>
+<TD ALIGN="LEFT"><B>D</B></TD>
+<TD ALIGN="LEFT" NOWRAP>daily motion (<I>n</I>, radians, JFORM=1 only)</TD>
+</TR>
+<TR VALIGN="TOP"><TD ALIGN="LEFT"><EM>JSTAT</EM></TD>
+<TD ALIGN="LEFT"><B>I</B></TD>
+<TD ALIGN="LEFT" NOWRAP>status:</TD>
+</TR>
+<TR VALIGN="TOP"><TD ALIGN="LEFT"><EM></EM></TD>
+<TD ALIGN="LEFT"><B></B></TD>
+<TD ALIGN="LEFT" NOWRAP> 0 = OK</TD>
+</TR>
+<TR VALIGN="TOP"><TD ALIGN="LEFT"><EM></EM></TD>
+<TD ALIGN="LEFT"><B></B></TD>
+<TD ALIGN="LEFT" NOWRAP> -1 = illegal PMASS</TD>
+</TR>
+<TR VALIGN="TOP"><TD ALIGN="LEFT"><EM></EM></TD>
+<TD ALIGN="LEFT"><B></B></TD>
+<TD ALIGN="LEFT" NOWRAP> -2 = illegal JFORMR</TD>
+</TR>
+<TR VALIGN="TOP"><TD ALIGN="LEFT"><EM></EM></TD>
+<TD ALIGN="LEFT"><B></B></TD>
+<TD ALIGN="LEFT" NOWRAP> -3 = position/velocity out of allowed range</TD>
+</TR>
+</TABLE></DL>
+<P> <DL>
+<DT><STRONG>NOTES:</STRONG>
+<DD><DL COMPACT>
+<DT>1.
+<DD>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)&nbsp;<IMG WIDTH="13" HEIGHT="14" ALIGN="BOTTOM" BORDER="0"
+ SRC="img24.gif"
+ ALT="$\alpha$">, which is proportional to the total energy of the
+ orbit, (ii)&nbsp;the heliocentric distance at epoch,
+ (iii)&nbsp;the outwards component of the velocity at the given epoch,
+ (iv)&nbsp;an estimate of <IMG WIDTH="14" HEIGHT="27" ALIGN="MIDDLE" BORDER="0"
+ SRC="img105.gif"
+ ALT="$\psi$">, the ``universal eccentric anomaly'' at a
+ given date and (v)&nbsp;that date.
+ <DT>2.
+<DD>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.
+ <DT>3.
+<DD>Three different element-format options are supported, as
+ follows. <BR>
+<P>
+JFORM=1, suitable for the major planets:
+<P> <PRE><TT>
+ EPOCH = epoch of elements <I>t<SUB>0</SUB></I> (TT MJD)
+ ORBINC = inclination <I>i</I> (radians)
+ ANODE = longitude of the ascending node <IMG WIDTH="14" HEIGHT="13" ALIGN="BOTTOM" BORDER="0"
+ SRC="img99.gif"
+ ALT="$\Omega$"> (radians)
+ PERIH = longitude of perihelion <IMG WIDTH="16" HEIGHT="14" ALIGN="BOTTOM" BORDER="0"
+ SRC="img100.gif"
+ ALT="$\varpi$"> (radians)
+ AORQ = mean distance <I>a</I> (AU)
+ E = eccentricity <I>e</I> <IMG WIDTH="83" HEIGHT="29" ALIGN="MIDDLE" BORDER="0"
+ SRC="img106.gif"
+ ALT="$( 0 \leq e < 1 )$">
+ AORL = mean longitude <I>L</I> (radians)
+ DM = daily motion <I>n</I> (radians)
+</TT></PRE>
+<P>
+JFORM=2, suitable for minor planets:
+<P> <PRE><TT>
+ EPOCH = epoch of elements <I>t<SUB>0</SUB></I> (TT MJD)
+ ORBINC = inclination <I>i</I> (radians)
+ ANODE = longitude of the ascending node <IMG WIDTH="14" HEIGHT="13" ALIGN="BOTTOM" BORDER="0"
+ SRC="img99.gif"
+ ALT="$\Omega$"> (radians)
+ PERIH = argument of perihelion <IMG WIDTH="13" HEIGHT="14" ALIGN="BOTTOM" BORDER="0"
+ SRC="img101.gif"
+ ALT="$\omega$"> (radians)
+ AORQ = mean distance <I>a</I> (AU)
+ E = eccentricity <I>e</I> <IMG WIDTH="83" HEIGHT="29" ALIGN="MIDDLE" BORDER="0"
+ SRC="img106.gif"
+ ALT="$( 0 \leq e < 1 )$">
+ AORL = mean anomaly <I>M</I> (radians)
+</TT></PRE>
+<P>
+JFORM=3, suitable for comets:
+<P> <PRE><TT>
+ EPOCH = epoch of perihelion <I>T</I> (TT MJD)
+ ORBINC = inclination <I>i</I> (radians)
+ ANODE = longitude of the ascending node <IMG WIDTH="14" HEIGHT="13" ALIGN="BOTTOM" BORDER="0"
+ SRC="img99.gif"
+ ALT="$\Omega$"> (radians)
+ PERIH = argument of perihelion <IMG WIDTH="13" HEIGHT="14" ALIGN="BOTTOM" BORDER="0"
+ SRC="img101.gif"
+ ALT="$\omega$"> (radians)
+ AORQ = perihelion distance <I>q</I> (AU)
+ E = eccentricity <I>e</I> <IMG WIDTH="91" HEIGHT="29" ALIGN="MIDDLE" BORDER="0"
+ SRC="img107.gif"
+ ALT="$( 0 \leq e \leq 10 )$"></TT></PRE>
+ <DT>4.
+<DD>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:
+<P> <PRE><TT>
+ JFORMR JFORM meaning
+&nbsp;
+ &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;1 &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;1 OK: elements are in the requested format
+ &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;1 &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;2 never happens
+ &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;1 &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;3 orbit not elliptical
+ &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;2 &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;1 never happens
+ &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;2 &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;2 OK: elements are in the requested format
+ &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;2 &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;3 orbit not elliptical
+ &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;3 &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;1 never happens
+ &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;3 &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;2 never happens
+ &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;3 &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;3 OK: elements are in the requested format
+</TT></PRE>
+ <DT>5.
+<DD>The arguments returned for each value of JFORM (<I>cf</I> Note&nbsp;5:
+ JFORM may not be the same as JFORMR) are as follows:
+<P> <PRE><TT>
+ JFORM 1 2 3
+&nbsp;
+ EPOCH <I>t<SUB>0</SUB></I> <I>t<SUB>0</SUB></I> <I>T</I>
+ ORBINC <I>i</I> <I>i</I> <I>i</I>
+ ANODE <IMG WIDTH="14" HEIGHT="13" ALIGN="BOTTOM" BORDER="0"
+ SRC="img99.gif"
+ ALT="$\Omega$"> <IMG WIDTH="14" HEIGHT="13" ALIGN="BOTTOM" BORDER="0"
+ SRC="img99.gif"
+ ALT="$\Omega$"> <IMG WIDTH="14" HEIGHT="13" ALIGN="BOTTOM" BORDER="0"
+ SRC="img99.gif"
+ ALT="$\Omega$">
+ PERIH <IMG WIDTH="16" HEIGHT="14" ALIGN="BOTTOM" BORDER="0"
+ SRC="img100.gif"
+ ALT="$\varpi$"> <IMG WIDTH="13" HEIGHT="14" ALIGN="BOTTOM" BORDER="0"
+ SRC="img101.gif"
+ ALT="$\omega$"> <IMG WIDTH="13" HEIGHT="14" ALIGN="BOTTOM" BORDER="0"
+ SRC="img101.gif"
+ ALT="$\omega$">
+ AORQ <I>a</I> <I>a</I> <I>q</I>
+ E <I>e</I> <I>e</I> <I>e</I>
+ AORL <I>L</I> <I>M</I> -
+ DM <I>n</I> - -
+</TT></PRE>
+<P>
+where:
+ <PRE><TT>
+ <I>t<SUB>0</SUB></I> is the epoch of the elements (MJD, TT)
+ <I>T</I> is the epoch of perihelion (MJD, TT)
+ <I>i</I> is the inclination (radians)
+ <IMG WIDTH="14" HEIGHT="13" ALIGN="BOTTOM" BORDER="0"
+ SRC="img99.gif"
+ ALT="$\Omega$"> is the longitude of the ascending node (radians)
+ <IMG WIDTH="16" HEIGHT="14" ALIGN="BOTTOM" BORDER="0"
+ SRC="img100.gif"
+ ALT="$\varpi$"> is the longitude of perihelion (radians)
+ <IMG WIDTH="13" HEIGHT="14" ALIGN="BOTTOM" BORDER="0"
+ SRC="img101.gif"
+ ALT="$\omega$"> is the argument of perihelion (radians)
+ <I>a</I> is the mean distance (AU)
+ <I>q</I> is the perihelion distance (AU)
+ <I>e</I> is the eccentricity
+ <I>L</I> is the longitude (radians, <IMG WIDTH="48" HEIGHT="25" ALIGN="MIDDLE" BORDER="0"
+ SRC="img143.gif"
+ ALT="$0-2\pi$">) <I>M</I> is the mean anomaly (radians, <IMG WIDTH="48" HEIGHT="25" ALIGN="MIDDLE" BORDER="0"
+ SRC="img143.gif"
+ ALT="$0-2\pi$">) <I>n</I> is the daily motion (radians)
+ - means no value is set
+</TT></PRE>
+ <DT>6.
+<DD>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.
+ </DL></DL>
+<P> <DL>
+<DT><STRONG>REFERENCES:</STRONG>
+<DD><DL COMPACT>
+<DT>1.
+<DD>Sterne, Theodore E., <I>An Introduction to Celestial Mechanics,</I>
+Interscience Publishers, 1960. Section 6.7, p199.
+<DT>2.
+<DD>Everhart, E. &amp; Pitkin, E.T., Am.&nbsp;J.&nbsp;Phys.&nbsp;51, 712, 1983.
+ </DL></DL>
+<BR> <HR>
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+<P><!--End of Navigation Panel-->
+<ADDRESS>
+<I>SLALIB --- Positional Astronomy Library<BR>Starlink User Note 67<BR>P. T. Wallace<BR>12 October 1999<BR>E-mail:ptw@star.rl.ac.uk</I>
+</ADDRESS>
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