| void eraC2t00a(double tta, double ttb, double uta, double utb, | |
| double xp, double yp, double rc2t[3][3]) | |
| /* | |
| ** - - - - - - - - - - | |
| ** e r a C 2 t 0 0 a | |
| ** - - - - - - - - - - | |
| ** | |
| ** Form the celestial to terrestrial matrix given the date, the UT1 and | |
| ** the polar motion, using the IAU 2000A nutation model. | |
| ** | |
| ** Given: | |
| ** tta,ttb double TT as a 2-part Julian Date (Note 1) | |
| ** uta,utb double UT1 as a 2-part Julian Date (Note 1) | |
| ** xp,yp double coordinates of the pole (radians, Note 2) | |
| ** | |
| ** Returned: | |
| ** rc2t double[3][3] celestial-to-terrestrial matrix (Note 3) | |
| ** | |
| ** Notes: | |
| ** | |
| ** 1) The TT and UT1 dates tta+ttb and uta+utb are Julian Dates, | |
| ** apportioned in any convenient way between the arguments uta and | |
| ** utb. For example, JD(UT1)=2450123.7 could be expressed in any of | |
| ** these ways, among others: | |
| ** | |
| ** uta utb | |
| ** | |
| ** 2450123.7 0.0 (JD method) | |
| ** 2451545.0 -1421.3 (J2000 method) | |
| ** 2400000.5 50123.2 (MJD method) | |
| ** 2450123.5 0.2 (date & time method) | |
| ** | |
| ** The JD method is the most natural and convenient to use in | |
| ** cases where the loss of several decimal digits of resolution is | |
| ** acceptable. The J2000 and MJD methods are good compromises | |
| ** between resolution and convenience. In the case of uta,utb, the | |
| ** date & time method is best matched to the Earth rotation angle | |
| ** algorithm used: maximum precision is delivered when the uta | |
| ** argument is for 0hrs UT1 on the day in question and the utb | |
| ** argument lies in the range 0 to 1, or vice versa. | |
| ** | |
| ** 2) The arguments xp and yp are the coordinates (in radians) of the | |
| ** Celestial Intermediate Pole with respect to the International | |
| ** Terrestrial Reference System (see IERS Conventions 2003), | |
| ** measured along the meridians to 0 and 90 deg west respectively. | |
| ** | |
| ** 3) The matrix rc2t transforms from celestial to terrestrial | |
| ** coordinates: | |
| ** | |
| ** [TRS] = RPOM * R_3(ERA) * RC2I * [CRS] | |
| ** | |
| ** = rc2t * [CRS] | |
| ** | |
| ** where [CRS] is a vector in the Geocentric Celestial Reference | |
| ** System and [TRS] is a vector in the International Terrestrial | |
| ** Reference System (see IERS Conventions 2003), RC2I is the | |
| ** celestial-to-intermediate matrix, ERA is the Earth rotation | |
| ** angle and RPOM is the polar motion matrix. | |
| ** | |
| ** 4) A faster, but slightly less accurate result (about 1 mas), can | |
| ** be obtained by using instead the eraC2t00b function. | |
| ** | |
| ** Called: | |
| ** eraC2i00a celestial-to-intermediate matrix, IAU 2000A | |
| ** eraEra00 Earth rotation angle, IAU 2000 | |
| ** eraSp00 the TIO locator s', IERS 2000 | |
| ** eraPom00 polar motion matrix | |
| ** eraC2tcio form CIO-based celestial-to-terrestrial matrix | |
| ** | |
| ** Reference: | |
| ** | |
| ** McCarthy, D. D., Petit, G. (eds.), IERS Conventions (2003), | |
| ** IERS Technical Note No. 32, BKG (2004) | |
| ** | |
| ** Copyright (C) 2013-2017, NumFOCUS Foundation. | |
| ** Derived, with permission, from the SOFA library. See notes at end of file. | |
| */ | |
| { | |
| double rc2i[3][3], era, sp, rpom[3][3]; | |
| /* Form the celestial-to-intermediate matrix for this TT (IAU 2000A). */ | |
| eraC2i00a(tta, ttb, rc2i ); | |
| /* Predict the Earth rotation angle for this UT1. */ | |
| era = eraEra00(uta, utb); | |
| /* Estimate s'. */ | |
| sp = eraSp00(tta, ttb); | |
| /* Form the polar motion matrix. */ | |
| eraPom00(xp, yp, sp, rpom); | |
| /* Combine to form the celestial-to-terrestrial matrix. */ | |
| eraC2tcio(rc2i, era, rpom, rc2t); | |
| return; | |
| } | |
| /*---------------------------------------------------------------------- | |
| ** | |
| ** | |
| ** Copyright (C) 2013-2017, NumFOCUS Foundation. | |
| ** All rights reserved. | |
| ** | |
| ** This library is derived, with permission, from the International | |
| ** Astronomical Union's "Standards of Fundamental Astronomy" library, | |
| ** available from http://www.iausofa.org. | |
| ** | |
| ** The ERFA version is intended to retain identical functionality to | |
| ** the SOFA library, but made distinct through different function and | |
| ** file names, as set out in the SOFA license conditions. The SOFA | |
| ** original has a role as a reference standard for the IAU and IERS, | |
| ** and consequently redistribution is permitted only in its unaltered | |
| ** state. The ERFA version is not subject to this restriction and | |
| ** therefore can be included in distributions which do not support the | |
| ** concept of "read only" software. | |
| ** | |
| ** Although the intent is to replicate the SOFA API (other than | |
| ** replacement of prefix names) and results (with the exception of | |
| ** bugs; any that are discovered will be fixed), SOFA is not | |
| ** responsible for any errors found in this version of the library. | |
| ** | |
| ** If you wish to acknowledge the SOFA heritage, please acknowledge | |
| ** that you are using a library derived from SOFA, rather than SOFA | |
| ** itself. | |
| ** | |
| ** | |
| ** TERMS AND CONDITIONS | |
| ** | |
| ** Redistribution and use in source and binary forms, with or without | |
| ** modification, are permitted provided that the following conditions | |
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| ** | |
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| ** THIS SOFTWARE IS PROVIDED BY THE COPYRIGHT HOLDERS AND CONTRIBUTORS | |
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