| 1 | /* | 
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| 2 | *+ | 
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| 3 | *  Name: | 
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| 4 | *     palPolmo | 
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| 5 |  | 
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| 6 | *  Purpose: | 
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| 7 | *     Correct for polar motion | 
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| 8 |  | 
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| 9 | *  Language: | 
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| 10 | *     Starlink ANSI C | 
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| 11 |  | 
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| 12 | *  Type of Module: | 
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| 13 | *     Library routine | 
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| 14 |  | 
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| 15 | *  Invocation: | 
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| 16 | *     palPolmo ( double elongm, double phim, double xp, double yp, | 
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| 17 | *                double *elong, double *phi, double *daz ); | 
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| 18 |  | 
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| 19 | *  Arguments: | 
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| 20 | *     elongm = double (Given) | 
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| 21 | *        Mean logitude of the observer (radians, east +ve) | 
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| 22 | *     phim = double (Given) | 
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| 23 | *        Mean geodetic latitude of the observer (radians) | 
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| 24 | *     xp = double (Given) | 
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| 25 | *        Polar motion x-coordinate (radians) | 
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| 26 | *     yp = double (Given) | 
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| 27 | *        Polar motion y-coordinate (radians) | 
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| 28 | *     elong = double * (Returned) | 
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| 29 | *        True longitude of the observer (radians, east +ve) | 
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| 30 | *     phi = double * (Returned) | 
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| 31 | *        True geodetic latitude of the observer (radians) | 
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| 32 | *     daz = double * (Returned) | 
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| 33 | *        Azimuth correction (terrestrial-celestial, radians) | 
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| 34 |  | 
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| 35 | *  Description: | 
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| 36 | *     Polar motion:  correct site longitude and latitude for polar | 
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| 37 | *     motion and calculate azimuth difference between celestial and | 
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| 38 | *     terrestrial poles. | 
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| 39 |  | 
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| 40 | *  Authors: | 
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| 41 | *     PTW: Patrick Wallace (STFC) | 
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| 42 | *     TIMJ: Tim Jenness (Cornell) | 
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| 43 | *     {enter_new_authors_here} | 
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| 44 |  | 
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| 45 | *  Notes: | 
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| 46 | *     - "Mean" longitude and latitude are the (fixed) values for the | 
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| 47 | *       site's location with respect to the IERS terrestrial reference | 
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| 48 | *       frame;  the latitude is geodetic.  TAKE CARE WITH THE LONGITUDE | 
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| 49 | *       SIGN CONVENTION.  The longitudes used by the present routine | 
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| 50 | *       are east-positive, in accordance with geographical convention | 
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| 51 | *       (and right-handed).  In particular, note that the longitudes | 
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| 52 | *       returned by the sla_OBS routine are west-positive, following | 
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| 53 | *       astronomical usage, and must be reversed in sign before use in | 
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| 54 | *       the present routine. | 
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| 55 | * | 
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| 56 | *     - XP and YP are the (changing) coordinates of the Celestial | 
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| 57 | *       Ephemeris Pole with respect to the IERS Reference Pole. | 
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| 58 | *       XP is positive along the meridian at longitude 0 degrees, | 
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| 59 | *       and YP is positive along the meridian at longitude | 
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| 60 | *       270 degrees (i.e. 90 degrees west).  Values for XP,YP can | 
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| 61 | *       be obtained from IERS circulars and equivalent publications; | 
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| 62 | *       the maximum amplitude observed so far is about 0.3 arcseconds. | 
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| 63 | * | 
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| 64 | *     - "True" longitude and latitude are the (moving) values for | 
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| 65 | *       the site's location with respect to the celestial ephemeris | 
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| 66 | *       pole and the meridian which corresponds to the Greenwich | 
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| 67 | *       apparent sidereal time.  The true longitude and latitude | 
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| 68 | *       link the terrestrial coordinates with the standard celestial | 
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| 69 | *       models (for precession, nutation, sidereal time etc). | 
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| 70 | * | 
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| 71 | *     - The azimuths produced by sla_AOP and sla_AOPQK are with | 
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| 72 | *       respect to due north as defined by the Celestial Ephemeris | 
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| 73 | *       Pole, and can therefore be called "celestial azimuths". | 
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| 74 | *       However, a telescope fixed to the Earth measures azimuth | 
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| 75 | *       essentially with respect to due north as defined by the | 
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| 76 | *       IERS Reference Pole, and can therefore be called "terrestrial | 
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| 77 | *       azimuth".  Uncorrected, this would manifest itself as a | 
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| 78 | *       changing "azimuth zero-point error".  The value DAZ is the | 
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| 79 | *       correction to be added to a celestial azimuth to produce | 
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| 80 | *       a terrestrial azimuth. | 
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| 81 | * | 
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| 82 | *     - The present routine is rigorous.  For most practical | 
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| 83 | *       purposes, the following simplified formulae provide an | 
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| 84 | *       adequate approximation: | 
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| 85 | * | 
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| 86 | *       elong = elongm+xp*cos(elongm)-yp*sin(elongm) | 
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| 87 | *       phi   = phim+(xp*sin(elongm)+yp*cos(elongm))*tan(phim) | 
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| 88 | *       daz   = -sqrt(xp*xp+yp*yp)*cos(elongm-atan2(xp,yp))/cos(phim) | 
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| 89 | * | 
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| 90 | *       An alternative formulation for DAZ is: | 
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| 91 | * | 
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| 92 | *       x = cos(elongm)*cos(phim) | 
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| 93 | *       y = sin(elongm)*cos(phim) | 
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| 94 | *       daz = atan2(-x*yp-y*xp,x*x+y*y) | 
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| 95 | * | 
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| 96 | *     - Reference:  Seidelmann, P.K. (ed), 1992.  "Explanatory Supplement | 
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| 97 | *                   to the Astronomical Almanac", ISBN 0-935702-68-7, | 
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| 98 | *                   sections 3.27, 4.25, 4.52. | 
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| 99 |  | 
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| 100 | *  History: | 
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| 101 | *     2000-11-30 (PTW): | 
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| 102 | *        SLALIB implementation. | 
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| 103 | *     2014-10-18 (TIMJ): | 
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| 104 | *        Initial version in C. | 
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| 105 | *     {enter_further_changes_here} | 
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| 106 |  | 
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| 107 | *  Copyright: | 
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| 108 | *     Copyright (C) 2000 Rutherford Appleton Laboratory. | 
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| 109 | *     Copyright (C) 2014 Cornell University | 
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| 110 | *     All Rights Reserved. | 
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| 111 |  | 
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| 112 | *  Licence: | 
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| 113 | *     This program is free software; you can redistribute it and/or | 
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| 114 | *     modify it under the terms of the GNU General Public License as | 
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| 115 | *     published by the Free Software Foundation; either version 3 of | 
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| 116 | *     the License, or (at your option) any later version. | 
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| 117 | * | 
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| 118 | *     This program is distributed in the hope that it will be | 
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| 119 | *     useful, but WITHOUT ANY WARRANTY; without even the implied | 
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| 120 | *     warranty of MERCHANTABILITY or FITNESS FOR A PARTICULAR | 
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| 121 | *     PURPOSE. See the GNU General Public License for more details. | 
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| 122 | * | 
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| 123 | *     You should have received a copy of the GNU General Public License | 
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| 124 | *     along with this program.  If not, see <http://www.gnu.org/licenses/>. | 
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| 125 |  | 
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| 126 | *  Bugs: | 
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| 127 | *     {note_any_bugs_here} | 
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| 128 | *- | 
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| 129 | */ | 
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| 130 |  | 
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| 131 | #include <math.h> | 
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| 132 |  | 
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| 133 | #include "pal.h" | 
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| 134 |  | 
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| 135 | void palPolmo ( double elongm, double phim, double xp, double yp, | 
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| 136 | double *elong, double *phi, double *daz ) { | 
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| 137 |  | 
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| 138 | double  sel,cel,sph,cph,xm,ym,zm,xnm,ynm,znm, | 
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| 139 | sxp,cxp,syp,cyp,zw,xt,yt,zt,xnt,ynt; | 
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| 140 |  | 
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| 141 | /*  Site mean longitude and mean geodetic latitude as a Cartesian vector */ | 
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| 142 | sel=sin(elongm); | 
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| 143 | cel=cos(elongm); | 
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| 144 | sph=sin(phim); | 
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| 145 | cph=cos(phim); | 
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| 146 |  | 
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| 147 | xm=cel*cph; | 
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| 148 | ym=sel*cph; | 
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| 149 | zm=sph; | 
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| 150 |  | 
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| 151 | /*  Rotate site vector by polar motion, Y-component then X-component */ | 
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| 152 | sxp=sin(xp); | 
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| 153 | cxp=cos(xp); | 
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| 154 | syp=sin(yp); | 
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| 155 | cyp=cos(yp); | 
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| 156 |  | 
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| 157 | zw=(-ym*syp+zm*cyp); | 
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| 158 |  | 
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| 159 | xt=xm*cxp-zw*sxp; | 
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| 160 | yt=ym*cyp+zm*syp; | 
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| 161 | zt=xm*sxp+zw*cxp; | 
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| 162 |  | 
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| 163 | /*  Rotate also the geocentric direction of the terrestrial pole (0,0,1) */ | 
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| 164 | xnm=-sxp*cyp; | 
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| 165 | ynm=syp; | 
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| 166 | znm=cxp*cyp; | 
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| 167 |  | 
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| 168 | cph=sqrt(xt*xt+yt*yt); | 
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| 169 | if (cph == 0.0) xt=1.0; | 
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| 170 | sel=yt/cph; | 
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| 171 | cel=xt/cph; | 
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| 172 |  | 
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| 173 | /*  Return true longitude and true geodetic latitude of site */ | 
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| 174 | if (xt != 0.0 || yt != 0.0) { | 
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| 175 | *elong=atan2(yt,xt); | 
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| 176 | } else { | 
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| 177 | *elong=0.0; | 
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| 178 | } | 
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| 179 | *phi=atan2(zt,cph); | 
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| 180 |  | 
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| 181 | /*  Return current azimuth of terrestrial pole seen from site position */ | 
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| 182 | xnt=(xnm*cel+ynm*sel)*zt-znm*cph; | 
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| 183 | ynt=-xnm*sel+ynm*cel; | 
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| 184 | if (xnt != 0.0 || ynt != 0.0) { | 
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| 185 | *daz=atan2(-ynt,-xnt); | 
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| 186 | } else { | 
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| 187 | *daz=0.0; | 
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| 188 | } | 
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| 189 |  | 
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| 190 | } | 
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