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use crate;
use crate;
/// Form the celestial to terrestrial matrix given the date, the UT1,
/// the nutation and the polar motion. IAU 2000.
///
/// Given:
/// tta,ttb f64 TT as a 2-part Julian Date (Note 1)
/// uta,utb f64 UT1 as a 2-part Julian Date (Note 1)
/// dpsi,deps f64 nutation (Note 2)
/// xp,yp f64 coordinates of the pole (radians, Note 3)
///
/// Returned:
/// rc2t [[f64; 3]; 3] celestial-to-terrestrial matrix (Note 4)
///
/// 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 caller is responsible for providing the nutation components;
/// they are in longitude and obliquity, in radians and are with
/// respect to the equinox and ecliptic of date. For high-accuracy
/// applications, free core nutation should be included as well as
/// any other relevant corrections to the position of the CIP.
///
/// 3) 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 0 and 90 deg west respectively.
///
/// 4) The matrix rc2t transforms from celestial to terrestrial
/// coordinates:
///
/// [TRS] = RPOM * R_3(GST) * RBPN * [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), RBPN is the
/// bias-precession-nutation matrix, GST is the Greenwich (apparent)
/// Sidereal Time and RPOM is the polar motion matrix.
///
/// 5) Although its name does not include "00", This function is in fact
/// specific to the IAU 2000 models.
///
/// Called:
/// iauPn00 bias/precession/nutation results, IAU 2000
/// iauGmst00 Greenwich mean sidereal time, IAU 2000
/// iauSp00 the TIO locator s', IERS 2000
/// iauEe00 equation of the equinoxes, IAU 2000
/// iauPom00 polar motion matrix
/// iauC2teqx form equinox-based celestial-to-terrestrial matrix
///
/// Reference:
///
/// McCarthy, D. D., Petit, G. (eds.), IERS Conventions (2003),
/// IERS Technical Note No. 32, BKG (2004)