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+Astronomical Tools:
+
+Precession: These routines probably have some history even before the
+ authors quoted as original sources. They have been collected and
+ some rewritten into SPP by F. Valdes (NOAO), March 1986. PRECES.F
+ was used originally in V2.3-V2.5 IRAF by George Jacoby. It has
+ been replaced by ASTPRECESS.X which is the only procedure in the
+ library.
+
+ astprecess.x -- Precession written by F. Valdes based on Astronomical
+ Almanac using new IAU system.
+ precessmgb.x -- Precession + aberration + nutation based on the work of
+ Manchester, Gordon, and Ball
+ precessgj.x -- Originally written by G. Jacoby in Fortran and distributed
+ with V2.3-V2.5 IRAF. Transcribed to SPP by F. Valdes
+
+ Notes:
+ 1. The differences between ASTPRECESS.X and PRECESSGJ.X (
+ and a routine written by D. Wells for the Cyber and later
+ used in other NOAO software) are on the order of a few
+ tenths of a second of arc. I believe the differences are
+ due to using 1984 almanac methods in the former and much
+ earlier methods for the latter.
+ 3. PRECESSMGB.X differs considerably from the others to the order
+ of many seconds of arc. It does include other effects not
+ present in the other routines. It totally fails at DEC=+-90.
+ It is based on roughly 1970 almanac methods.
+ 4. See PRECESS.DOC for comparison.
+
+Radial Velocity: These formulas for these routines were partly obtained
+ by inspection of the code for the subroutine DOP in the program DOPSET
+ written by R. N. Manchester and M. A. Gordon of NRAO dated January 1970.
+ They have been restructured, revised, and coded in SPP by F. Valdes.
+
+ astvr.x -- Project a velocity vector in radial velocity along line of sight.
+ astvbary.x -- Radial velocity component of center of the Earth relative to
+ to the barycenter of the Earth-Moon system.
+ astvrotate.x -- Radial velocity component of the observer relative to
+ the center of the Earth due to the Earth's rotation.
+ astvorbit.x -- Radial velocity component of the observer relative to
+ the center of the Earth due to the Earth's rotation.
+ astvsun.x -- Projection of the sun's velocity along the given direction.
+
+Coordinates:
+
+ astarcsep.x -- Arc distance (arcsec) between two spherical coordinates
+ (hours, degrees).
+ astcoord.x -- This procedure converts the longitude-latitude coordinates
+ (a1, b1) of a point on a sphere into corresponding coordinates
+ (a2, b2) in a different coordinate system that is specified by
+ the coordinates of its origin (ao, bo) and its north pole (ap,
+ bp) in the original coordinate system. The range of a2 will be
+ from -pi to pi.
+ astgalactic.x -- Convert equatorial coordinates (1950) to galactic
+ coordinates.
+ astgaltoeq.x -- Convert galactic coordinates to equitorial (1950).
+
+Dates and times:
+
+ asttimes.x:
+ AST_DATE_TO_EPOCH -- Convert Gregorian date and solar mean time to
+ a Julian epoch. A Julian epoch has 365.25 days per year and 24
+ hours per day.
+ AST_EPOCH_TO_DATE -- Convert a Julian epoch to year, month, day, and
+ time.
+ AST_DAY_OF_YEAR -- The day number for the given year is returned.
+ AST_DAY_OF_WEEK -- Return the day of the week for the given Julian day.
+ The integer day of the week is 0=Sunday - 6=Saturday. The
+ character string is the three character abbreviation for the day
+ of the week. Note that the day of the week is for Greenwich
+ if the standard UT is used.
+ AST_JULDAY -- Convert epoch to Julian day.
+ AST_DATE_TO_JULDAY -- Convert date to Julian day.
+ AST_JULDAY_TO_DATE -- Convert Julian day to date.
+ AST_MST -- Mean sidereal time of the epoch at the given longitude.
+ This procedure may be used to optain Greenwich Mean Sidereal Time
+ (GMST) by setting the longitude to 0.
+ asthjd.x:
+ AST_HJD -- Helocentic Julian Day for a direction of observation.
+ AST_JD_TO_HJD -- Helocentic Julian Day for a direction of observation.
+
+Helocentric Parameters:
+
+ astdsun.x:
+ AST_DSUN - Distance to Sun in AU.
+
+Misc:
+
+ astlvac.x:
+ AST_LVAC - Convert air wavelengths to vacuum wavelengths (Angstroms)
+
+Y2K:
+ Most routines work in Julian days or epochs. If they have an input
+ year it is converted to one of these forms by calling
+ ast_date_to_julday. This is the only routine that has a Y2K
+ connection. It assumes two digit years are 20th century. These
+ routines are Y2K correct.
+
+
+The following are the comments and references from the DOPSET program
+noted above. The HJD routine was also derived from this code.
+
+C MODIFIED FOR IBM 360 BY R.N.MANCHESTER AND M.A.GORDON
+C JANUARY 1970
+C
+C
+C DOP CALCULATES THE VELOCITY COMPONENT OF THE OBSERVER WITH RESPECT
+C TO THE LOCAL STANDARD OF REST AS PROJECTED ONTO A LINE SPECIFIED BY T
+C ASCENSION AND DECLINATION (RAHRS, RAMIN, RASEC, DDEG, DMIN, DSEC) EPO
+C DATE, FOR A TIME SPECIFIED AS FOLLOWS: NYR = LAST TWO DIGITS OF THE
+C (FOR 19XX A.D.), NDAY = DAY NUMBER (GMT), NHUT, NMUT, NSUT = HRS, MIN
+C (GMT). THE LOCATION OF THE OBSERVER IS SPECIFIED BY THE LATITUDE (AL
+C LONGITUDE (OLONG) (GEODETIC) (IN DEGREES) AND ELEVATION (ELEV) (IN ME
+C ABOVE MEAN SEA LEVEL. THE SUBROUTINE OUTPUTS THE LOCAL MEAN SIDEREAL
+C (XLST IN DAYS), THE COMPONENT OF THE SUN*S MOTION WITH RESPECT TO THE
+C STANDARD OF REST AS PROJECTED ONTO THE LINE OF SIGHT TO THE SOURCE (V
+C KM/SEC) AS WELL AS THE TOTAL VELOCITY COMPONENT V1 (KM/SEC). POSITIV
+C VELOCITY CORRESPONDS TO INCREASING DISTANCE BETWEEN SOURCE AND OBSERV
+C
+C THIS VERSION OF DOP TAKES INTO ACCOUNT COMPONENTS OF THE OBSERVER*S
+C MOTION DUE TO THE ROTATION OF THE EARTH, THE REVOLUTION OF THE EARTH-
+C BARYCENTER ABOUT THE SUN, AND THE MOTION OF THE EARTH*S CENTER ABOUT
+C EARTH-MOON BARYCENTER. THE PERTURBATIONS OF THE EARTH*S ORBIT DUE TO
+C PLANETS ARE NEGLECTED. THE ABSOLUTE PRECISION OF THIS VERSION OF DOP
+C ABOUT 0.004 KM/SEC, BUT SINCE THE DOMINANT ERROR TERM IS SLOWLY VARYI
+C RELATIVE ERROR WILL BE CONSIDERABLY LESS FOR TIMES UP TO A WEEK OR SO
+C
+C REFERENCES: MCRAE, D. A., WESTERHOUT, G., TABLE FOR THE REDUCTION OF
+C VELOCITIES TO THE LOCAL STANDARD OF REST, THE OBSERVAY=2.
+C LUND, SWEDEN, 1956.
+C SMART, W. M., TEXT-BOOK ON SPHERICAL ASTRONOMY, CAMBRIDG
+C UNIV. PRESS, 1962.
+C THE AMERICAN EPHEMERIS AND NAUTICAL ALMANAC
+C THE SUPPLEMENT TO THE ABOVE
+C
+C VERSION OF JUNE 1969
+