| 1 | /* | 
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| 2 | *+ | 
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| 3 | *  Name: | 
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| 4 | *     palRefv | 
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| 5 |  | 
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| 6 | *  Purpose: | 
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| 7 | *     Adjust an unrefracted Cartesian vector to include the effect of atmospheric refraction | 
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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 | *     void palRefv ( double vu[3], double refa, double refb, double vr[3] ); | 
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| 17 |  | 
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| 18 | *  Arguments: | 
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| 19 | *     vu[3] = double (Given) | 
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| 20 | *        Unrefracted position of the source (Az/El 3-vector) | 
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| 21 | *     refa = double (Given) | 
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| 22 | *        tan Z coefficient (radian) | 
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| 23 | *     refb = double (Given) | 
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| 24 | *        tan**3 Z coefficient (radian) | 
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| 25 | *     vr[3] = double (Returned) | 
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| 26 | *        Refracted position of the source (Az/El 3-vector) | 
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| 27 |  | 
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| 28 | *  Description: | 
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| 29 | *     Adjust an unrefracted Cartesian vector to include the effect of | 
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| 30 | *     atmospheric refraction, using the simple A tan Z + B tan**3 Z | 
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| 31 | *     model. | 
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| 32 |  | 
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| 33 | *  Authors: | 
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| 34 | *     TIMJ: Tim Jenness | 
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| 35 | *     PTW: Patrick Wallace | 
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| 36 | *     {enter_new_authors_here} | 
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| 37 |  | 
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| 38 | *  Notes: | 
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| 39 | *     - This routine applies the adjustment for refraction in the | 
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| 40 | *     opposite sense to the usual one - it takes an unrefracted | 
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| 41 | *     (in vacuo) position and produces an observed (refracted) | 
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| 42 | *     position, whereas the A tan Z + B tan**3 Z model strictly | 
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| 43 | *     applies to the case where an observed position is to have the | 
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| 44 | *     refraction removed.  The unrefracted to refracted case is | 
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| 45 | *     harder, and requires an inverted form of the text-book | 
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| 46 | *     refraction models;  the algorithm used here is equivalent to | 
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| 47 | *     one iteration of the Newton-Raphson method applied to the above | 
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| 48 | *     formula. | 
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| 49 | * | 
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| 50 | *     - Though optimized for speed rather than precision, the present | 
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| 51 | *     routine achieves consistency with the refracted-to-unrefracted | 
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| 52 | *     A tan Z + B tan**3 Z model at better than 1 microarcsecond within | 
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| 53 | *     30 degrees of the zenith and remains within 1 milliarcsecond to | 
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| 54 | *     beyond ZD 70 degrees.  The inherent accuracy of the model is, of | 
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| 55 | *     course, far worse than this - see the documentation for palRefco | 
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| 56 | *     for more information. | 
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| 57 | * | 
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| 58 | *     - At low elevations (below about 3 degrees) the refraction | 
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| 59 | *     correction is held back to prevent arithmetic problems and | 
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| 60 | *     wildly wrong results.  For optical/IR wavelengths, over a wide | 
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| 61 | *     range of observer heights and corresponding temperatures and | 
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| 62 | *     pressures, the following levels of accuracy (arcsec, worst case) | 
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| 63 | *     are achieved, relative to numerical integration through a model | 
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| 64 | *     atmosphere: | 
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| 65 | * | 
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| 66 | *              ZD    error | 
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| 67 | * | 
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| 68 | *              80      0.7 | 
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| 69 | *              81      1.3 | 
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| 70 | *              82      2.5 | 
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| 71 | *              83      5 | 
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| 72 | *              84     10 | 
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| 73 | *              85     20 | 
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| 74 | *              86     55 | 
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| 75 | *              87    160 | 
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| 76 | *              88    360 | 
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| 77 | *              89    640 | 
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| 78 | *              90   1100 | 
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| 79 | *              91   1700         } relevant only to | 
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| 80 | *              92   2600         } high-elevation sites | 
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| 81 | * | 
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| 82 | *     The results for radio are slightly worse over most of the range, | 
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| 83 | *     becoming significantly worse below ZD=88 and unusable beyond | 
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| 84 | *     ZD=90. | 
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| 85 | * | 
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| 86 | *     - See also the routine palRefz, which performs the adjustment to | 
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| 87 | *     the zenith distance rather than in Cartesian Az/El coordinates. | 
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| 88 | *     The present routine is faster than palRefz and, except very low down, | 
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| 89 | *     is equally accurate for all practical purposes.  However, beyond | 
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| 90 | *     about ZD 84 degrees palRefz should be used, and for the utmost | 
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| 91 | *     accuracy iterative use of palRefro should be considered. | 
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| 92 |  | 
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| 93 | *  History: | 
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| 94 | *     2014-07-15 (TIMJ): | 
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| 95 | *        Initial version. A direct copy of the Fortran SLA implementation. | 
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| 96 | *        Adapted with permission from the Fortran SLALIB library. | 
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| 97 | *     {enter_further_changes_here} | 
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| 98 |  | 
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| 99 | *  Copyright: | 
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| 100 | *     Copyright (C) 2014 Tim Jenness | 
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| 101 | *     Copyright (C) 2004 Patrick Wallace | 
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| 102 | *     All Rights Reserved. | 
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| 103 |  | 
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| 104 | *  Licence: | 
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| 105 | *     This program is free software; you can redistribute it and/or | 
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| 106 | *     modify it under the terms of the GNU General Public License as | 
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| 107 | *     published by the Free Software Foundation; either version 3 of | 
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| 108 | *     the License, or (at your option) any later version. | 
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| 109 | * | 
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| 110 | *     This program is distributed in the hope that it will be | 
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| 111 | *     useful, but WITHOUT ANY WARRANTY; without even the implied | 
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| 112 | *     warranty of MERCHANTABILITY or FITNESS FOR A PARTICULAR | 
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| 113 | *     PURPOSE. See the GNU General Public License for more details. | 
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| 114 | * | 
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| 115 | *     You should have received a copy of the GNU General Public License | 
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| 116 | *     along with this program; if not, write to the Free Software | 
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| 117 | *     Foundation, Inc., 51 Franklin Street, Fifth Floor, Boston, | 
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| 118 | *     MA 02110-1301, USA. | 
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| 119 |  | 
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| 120 | *  Bugs: | 
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| 121 | *     {note_any_bugs_here} | 
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| 122 | *- | 
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| 123 | */ | 
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| 124 |  | 
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| 125 | #include "pal.h" | 
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| 126 | #include "palmac.h" | 
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| 127 | #include <math.h> | 
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| 128 |  | 
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| 129 | void palRefv ( double vu[3], double refa, double refb, double vr[3] ) { | 
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| 130 |  | 
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| 131 | double x,y,z1,z,zsq,rsq,r,wb,wt,d,cd,f; | 
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| 132 |  | 
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| 133 | /*  Initial estimate = unrefracted vector */ | 
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| 134 | x = vu[0]; | 
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| 135 | y = vu[1]; | 
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| 136 | z1 = vu[2]; | 
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| 137 |  | 
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| 138 | /*  Keep correction approximately constant below about 3 deg elevation */ | 
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| 139 | z = DMAX(z1,0.05); | 
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| 140 |  | 
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| 141 | /*  One Newton-Raphson iteration */ | 
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| 142 | zsq = z*z; | 
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| 143 | rsq = x*x+y*y; | 
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| 144 | r = sqrt(rsq); | 
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| 145 | wb = refb*rsq/zsq; | 
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| 146 | wt = (refa+wb)/(1.0+(refa+3.0*wb)*(zsq+rsq)/zsq); | 
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| 147 | d = wt*r/z; | 
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| 148 | cd = 1.0-d*d/2.0; | 
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| 149 | f = cd*(1.0-wt); | 
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| 150 |  | 
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| 151 | /*  Post-refraction x,y,z */ | 
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| 152 | vr[0] = x*f; | 
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| 153 | vr[1] = y*f; | 
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| 154 | vr[2] = cd*(z+d*r)+(z1-z); | 
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| 155 | } | 
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