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/* |
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*+ |
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* Name: |
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* palPolmo |
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* Purpose: |
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* Correct for polar motion |
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* Language: |
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* Starlink ANSI C |
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* Type of Module: |
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* Library routine |
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* Invocation: |
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* palPolmo ( double elongm, double phim, double xp, double yp, |
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* double *elong, double *phi, double *daz ); |
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* Arguments: |
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* elongm = double (Given) |
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* Mean logitude of the observer (radians, east +ve) |
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* phim = double (Given) |
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* Mean geodetic latitude of the observer (radians) |
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* xp = double (Given) |
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* Polar motion x-coordinate (radians) |
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* yp = double (Given) |
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* Polar motion y-coordinate (radians) |
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* elong = double * (Returned) |
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* True longitude of the observer (radians, east +ve) |
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* phi = double * (Returned) |
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* True geodetic latitude of the observer (radians) |
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* daz = double * (Returned) |
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* Azimuth correction (terrestrial-celestial, radians) |
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* Description: |
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* Polar motion: correct site longitude and latitude for polar |
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* motion and calculate azimuth difference between celestial and |
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* terrestrial poles. |
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* Authors: |
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* PTW: Patrick Wallace (STFC) |
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* TIMJ: Tim Jenness (Cornell) |
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* {enter_new_authors_here} |
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* Notes: |
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* - "Mean" longitude and latitude are the (fixed) values for the |
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* site's location with respect to the IERS terrestrial reference |
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* frame; the latitude is geodetic. TAKE CARE WITH THE LONGITUDE |
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* SIGN CONVENTION. The longitudes used by the present routine |
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* are east-positive, in accordance with geographical convention |
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* (and right-handed). In particular, note that the longitudes |
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* returned by the sla_OBS routine are west-positive, following |
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* astronomical usage, and must be reversed in sign before use in |
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* the present routine. |
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* |
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* - XP and YP are the (changing) coordinates of the Celestial |
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* Ephemeris Pole with respect to the IERS Reference Pole. |
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* XP is positive along the meridian at longitude 0 degrees, |
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* and YP is positive along the meridian at longitude |
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* 270 degrees (i.e. 90 degrees west). Values for XP,YP can |
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* be obtained from IERS circulars and equivalent publications; |
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* the maximum amplitude observed so far is about 0.3 arcseconds. |
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* |
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* - "True" longitude and latitude are the (moving) values for |
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* the site's location with respect to the celestial ephemeris |
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* pole and the meridian which corresponds to the Greenwich |
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* apparent sidereal time. The true longitude and latitude |
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* link the terrestrial coordinates with the standard celestial |
69
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* models (for precession, nutation, sidereal time etc). |
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* |
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* - The azimuths produced by sla_AOP and sla_AOPQK are with |
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* respect to due north as defined by the Celestial Ephemeris |
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* Pole, and can therefore be called "celestial azimuths". |
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* However, a telescope fixed to the Earth measures azimuth |
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* essentially with respect to due north as defined by the |
76
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* IERS Reference Pole, and can therefore be called "terrestrial |
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* azimuth". Uncorrected, this would manifest itself as a |
78
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* changing "azimuth zero-point error". The value DAZ is the |
79
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* correction to be added to a celestial azimuth to produce |
80
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* a terrestrial azimuth. |
81
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* |
82
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* - The present routine is rigorous. For most practical |
83
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* purposes, the following simplified formulae provide an |
84
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* adequate approximation: |
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* |
86
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* elong = elongm+xp*cos(elongm)-yp*sin(elongm) |
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* phi = phim+(xp*sin(elongm)+yp*cos(elongm))*tan(phim) |
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* daz = -sqrt(xp*xp+yp*yp)*cos(elongm-atan2(xp,yp))/cos(phim) |
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* |
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* An alternative formulation for DAZ is: |
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* |
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* x = cos(elongm)*cos(phim) |
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* y = sin(elongm)*cos(phim) |
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* daz = atan2(-x*yp-y*xp,x*x+y*y) |
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* |
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* - Reference: Seidelmann, P.K. (ed), 1992. "Explanatory Supplement |
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* to the Astronomical Almanac", ISBN 0-935702-68-7, |
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* sections 3.27, 4.25, 4.52. |
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100
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* History: |
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* 2000-11-30 (PTW): |
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* SLALIB implementation. |
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* 2014-10-18 (TIMJ): |
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* Initial version in C. |
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* {enter_further_changes_here} |
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107
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* Copyright: |
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* Copyright (C) 2000 Rutherford Appleton Laboratory. |
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* Copyright (C) 2014 Cornell University |
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* All Rights Reserved. |
111
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112
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* Licence: |
113
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* This program is free software; you can redistribute it and/or |
114
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* modify it under the terms of the GNU General Public License as |
115
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* published by the Free Software Foundation; either version 3 of |
116
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* the License, or (at your option) any later version. |
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* |
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* This program is distributed in the hope that it will be |
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* useful, but WITHOUT ANY WARRANTY; without even the implied |
120
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* warranty of MERCHANTABILITY or FITNESS FOR A PARTICULAR |
121
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* PURPOSE. See the GNU General Public License for more details. |
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* |
123
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* You should have received a copy of the GNU General Public License |
124
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* along with this program. If not, see . |
125
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126
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* Bugs: |
127
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* {note_any_bugs_here} |
128
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*- |
129
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*/ |
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131
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#include |
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133
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#include "pal.h" |
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135
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1
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void palPolmo ( double elongm, double phim, double xp, double yp, |
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double *elong, double *phi, double *daz ) { |
137
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138
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double sel,cel,sph,cph,xm,ym,zm,xnm,ynm,znm, |
139
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sxp,cxp,syp,cyp,zw,xt,yt,zt,xnt,ynt; |
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141
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/* Site mean longitude and mean geodetic latitude as a Cartesian vector */ |
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1
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sel=sin(elongm); |
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1
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cel=cos(elongm); |
144
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1
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sph=sin(phim); |
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1
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cph=cos(phim); |
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147
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1
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xm=cel*cph; |
148
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1
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ym=sel*cph; |
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zm=sph; |
150
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151
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/* Rotate site vector by polar motion, Y-component then X-component */ |
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1
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sxp=sin(xp); |
153
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1
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cxp=cos(xp); |
154
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1
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syp=sin(yp); |
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1
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cyp=cos(yp); |
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157
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1
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zw=(-ym*syp+zm*cyp); |
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159
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1
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xt=xm*cxp-zw*sxp; |
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1
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yt=ym*cyp+zm*syp; |
161
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1
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zt=xm*sxp+zw*cxp; |
162
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163
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/* Rotate also the geocentric direction of the terrestrial pole (0,0,1) */ |
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1
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xnm=-sxp*cyp; |
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ynm=syp; |
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1
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znm=cxp*cyp; |
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168
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1
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cph=sqrt(xt*xt+yt*yt); |
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1
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50
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if (cph == 0.0) xt=1.0; |
170
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1
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sel=yt/cph; |
171
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1
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cel=xt/cph; |
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173
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/* Return true longitude and true geodetic latitude of site */ |
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1
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50
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if (xt != 0.0 || yt != 0.0) { |
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1
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*elong=atan2(yt,xt); |
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} else { |
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0
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*elong=0.0; |
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} |
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1
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*phi=atan2(zt,cph); |
180
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181
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/* Return current azimuth of terrestrial pole seen from site position */ |
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1
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xnt=(xnm*cel+ynm*sel)*zt-znm*cph; |
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1
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ynt=-xnm*sel+ynm*cel; |
184
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1
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50
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if (xnt != 0.0 || ynt != 0.0) { |
185
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1
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*daz=atan2(-ynt,-xnt); |
186
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} else { |
187
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0
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*daz=0.0; |
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} |
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190
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1
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} |