source: trunk/FACT++/pal/palPolmo.c@ 19102

Last change on this file since 19102 was 18347, checked in by tbretz, 9 years ago
File size: 6.1 KB
Line 
1/*
2*+
3* Name:
4* palPolmo
5
6* Purpose:
7* Correct for polar motion
8
9* Language:
10* Starlink ANSI C
11
12* Type of Module:
13* Library routine
14
15* Invocation:
16* palPolmo ( double elongm, double phim, double xp, double yp,
17* double *elong, double *phi, double *daz );
18
19* Arguments:
20* elongm = double (Given)
21* Mean logitude of the observer (radians, east +ve)
22* phim = double (Given)
23* Mean geodetic latitude of the observer (radians)
24* xp = double (Given)
25* Polar motion x-coordinate (radians)
26* yp = double (Given)
27* Polar motion y-coordinate (radians)
28* elong = double * (Returned)
29* True longitude of the observer (radians, east +ve)
30* phi = double * (Returned)
31* True geodetic latitude of the observer (radians)
32* daz = double * (Returned)
33* Azimuth correction (terrestrial-celestial, radians)
34
35* Description:
36* Polar motion: correct site longitude and latitude for polar
37* motion and calculate azimuth difference between celestial and
38* terrestrial poles.
39
40* Authors:
41* PTW: Patrick Wallace (STFC)
42* TIMJ: Tim Jenness (Cornell)
43* {enter_new_authors_here}
44
45* Notes:
46* - "Mean" longitude and latitude are the (fixed) values for the
47* site's location with respect to the IERS terrestrial reference
48* frame; the latitude is geodetic. TAKE CARE WITH THE LONGITUDE
49* SIGN CONVENTION. The longitudes used by the present routine
50* are east-positive, in accordance with geographical convention
51* (and right-handed). In particular, note that the longitudes
52* returned by the sla_OBS routine are west-positive, following
53* astronomical usage, and must be reversed in sign before use in
54* the present routine.
55*
56* - XP and YP are the (changing) coordinates of the Celestial
57* Ephemeris Pole with respect to the IERS Reference Pole.
58* XP is positive along the meridian at longitude 0 degrees,
59* and YP is positive along the meridian at longitude
60* 270 degrees (i.e. 90 degrees west). Values for XP,YP can
61* be obtained from IERS circulars and equivalent publications;
62* the maximum amplitude observed so far is about 0.3 arcseconds.
63*
64* - "True" longitude and latitude are the (moving) values for
65* the site's location with respect to the celestial ephemeris
66* pole and the meridian which corresponds to the Greenwich
67* apparent sidereal time. The true longitude and latitude
68* link the terrestrial coordinates with the standard celestial
69* models (for precession, nutation, sidereal time etc).
70*
71* - The azimuths produced by sla_AOP and sla_AOPQK are with
72* respect to due north as defined by the Celestial Ephemeris
73* Pole, and can therefore be called "celestial azimuths".
74* However, a telescope fixed to the Earth measures azimuth
75* essentially with respect to due north as defined by the
76* IERS Reference Pole, and can therefore be called "terrestrial
77* azimuth". Uncorrected, this would manifest itself as a
78* changing "azimuth zero-point error". The value DAZ is the
79* correction to be added to a celestial azimuth to produce
80* a terrestrial azimuth.
81*
82* - The present routine is rigorous. For most practical
83* purposes, the following simplified formulae provide an
84* adequate approximation:
85*
86* elong = elongm+xp*cos(elongm)-yp*sin(elongm)
87* phi = phim+(xp*sin(elongm)+yp*cos(elongm))*tan(phim)
88* daz = -sqrt(xp*xp+yp*yp)*cos(elongm-atan2(xp,yp))/cos(phim)
89*
90* An alternative formulation for DAZ is:
91*
92* x = cos(elongm)*cos(phim)
93* y = sin(elongm)*cos(phim)
94* daz = atan2(-x*yp-y*xp,x*x+y*y)
95*
96* - Reference: Seidelmann, P.K. (ed), 1992. "Explanatory Supplement
97* to the Astronomical Almanac", ISBN 0-935702-68-7,
98* sections 3.27, 4.25, 4.52.
99
100* History:
101* 2000-11-30 (PTW):
102* SLALIB implementation.
103* 2014-10-18 (TIMJ):
104* Initial version in C.
105* {enter_further_changes_here}
106
107* Copyright:
108* Copyright (C) 2000 Rutherford Appleton Laboratory.
109* Copyright (C) 2014 Cornell University
110* All Rights Reserved.
111
112* Licence:
113* This program is free software; you can redistribute it and/or
114* modify it under the terms of the GNU General Public License as
115* published by the Free Software Foundation; either version 3 of
116* the License, or (at your option) any later version.
117*
118* This program is distributed in the hope that it will be
119* useful, but WITHOUT ANY WARRANTY; without even the implied
120* warranty of MERCHANTABILITY or FITNESS FOR A PARTICULAR
121* PURPOSE. See the GNU General Public License for more details.
122*
123* You should have received a copy of the GNU General Public License
124* along with this program. If not, see <http://www.gnu.org/licenses/>.
125
126* Bugs:
127* {note_any_bugs_here}
128*-
129*/
130
131#include <math.h>
132
133#include "pal.h"
134
135void palPolmo ( double elongm, double phim, double xp, double yp,
136 double *elong, double *phi, double *daz ) {
137
138 double sel,cel,sph,cph,xm,ym,zm,xnm,ynm,znm,
139 sxp,cxp,syp,cyp,zw,xt,yt,zt,xnt,ynt;
140
141 /* Site mean longitude and mean geodetic latitude as a Cartesian vector */
142 sel=sin(elongm);
143 cel=cos(elongm);
144 sph=sin(phim);
145 cph=cos(phim);
146
147 xm=cel*cph;
148 ym=sel*cph;
149 zm=sph;
150
151 /* Rotate site vector by polar motion, Y-component then X-component */
152 sxp=sin(xp);
153 cxp=cos(xp);
154 syp=sin(yp);
155 cyp=cos(yp);
156
157 zw=(-ym*syp+zm*cyp);
158
159 xt=xm*cxp-zw*sxp;
160 yt=ym*cyp+zm*syp;
161 zt=xm*sxp+zw*cxp;
162
163 /* Rotate also the geocentric direction of the terrestrial pole (0,0,1) */
164 xnm=-sxp*cyp;
165 ynm=syp;
166 znm=cxp*cyp;
167
168 cph=sqrt(xt*xt+yt*yt);
169 if (cph == 0.0) xt=1.0;
170 sel=yt/cph;
171 cel=xt/cph;
172
173 /* Return true longitude and true geodetic latitude of site */
174 if (xt != 0.0 || yt != 0.0) {
175 *elong=atan2(yt,xt);
176 } else {
177 *elong=0.0;
178 }
179 *phi=atan2(zt,cph);
180
181 /* Return current azimuth of terrestrial pole seen from site position */
182 xnt=(xnm*cel+ynm*sel)*zt-znm*cph;
183 ynt=-xnm*sel+ynm*cel;
184 if (xnt != 0.0 || ynt != 0.0) {
185 *daz=atan2(-ynt,-xnt);
186 } else {
187 *daz=0.0;
188 }
189
190}
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