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Han et al. Satell Navig            (2021) 2:18                                           Page 7 of 10





            potentials of the space–time metric in GCRS are from   Conceptually, two space-time reference systems are
            the BCRS, the defnition of GCRS is conceptually derived   mainly involved in BDS in the operation mode supported
            from BCRS.                                        by the master control station and monitor stations. One
                                                              is GCRS which is a unifed space-time reference for its
            Geocentric terrestrial reference system           precise  orbit  determination,  time  synchronization,  and
            Te defnition of GTRS is given by IAU2000 Resolution   observation information processing, and the other is
            B1.3. It is a space coordinate system whose origin is at the   GTRS which is the reference of the Earth’s surface and
            center of the Earth and makes diurnal apparent motion   geostationary space and mainly used to express the posi-
            with the Earth. In this reference system, the coordinates   tions of the users and the ground stations.
            of points on the solid surface of the Earth remain almost   Te observation modeling of satellite precise orbit
            unchanged except of the small changes caused by geo-  determination and time  synchronization in BDS are
            physical efects. IUGG2007 Resolution 2 clarifed that   all based on GCRS. Since the positions of satellites and
            GTRS was a geocentric space–time coordinate system   ground stations are separately expressed in two spa-
            under the framework of the theory of relativity. Te coor-  tial reference systems, GCRS and GTRS, the coordinate
            dinate transformation between GTRS and GCRS is real-  transformation between them is required. Te relation-
            ized through a space rotation determined with EOP.  ship can be written as follows:
              Te International Terrestrial Reference System (ITRS)
            maintained  by  IERS  is  an  implementation  of  GTRS,   [GCRS]=Q(t)R(t)W (t)[GTRS]         (12)
            which constitutes a set of prescriptions and conventions   Here,  Q(t), R(t), W (t)  are  respectively  the  matrices  of
            together with the modeling required to defne the ori-  precession and nutation, the Earth rotation, and the polar
            gin, scale, orientation, and time evolution. Te system is   motion, and.
            realized as the International Terrestrial Reference Frame
            (ITRF) based upon the estimated coordinates and veloci-  Q(t) ≡ R 3 (−E)R 2 (−d)R 3 (E+s)    (13)
            ties of a set of stations observed by VLBI, Lunar Laser
            Ranging (LLR), GPS, Satellite Laser Ranging (SLR), and   R(t) ≡ R 3 (ω E )                   (14)
            Doppler Orbitography and Radiopositioning Integrated
            by Satellite (DORIS). According to IERS, ITRS meet the   W (t) ≡ R 3 (−s )R 2 (x p )R 1 (y p )  (15)
                                                                              ′
            following:
                                                                Where  R ,  R , and  R  represent the rotation matrices
                                                                       1
                                                                          2
                                                                                 3
              •  Te origin is at the mass center of the Earth, includ-  about the X, Y, and Z axes respectively. Te acquisition
                ing oceans and atmosphere.                    and calculation methods of each parameter were given in
              •  Te unit of length (scale) is the meter (SI).  IERS 2010 Technical Note (Petit and Luzum, 2010).
              •  Te orientation is initially given by the Bureau Inter-  Te  geocentric terrestrial reference system  used  in
                national de I’Heure(BIH) orientation at 1984.0.  BDS is called BeiDou Coordinate System (BDCS) and its
              •  Te time evolution of the orientation is ensured by   defnition is consistent  with  ITRS (Wu,  2018).  Te ori-
                using a no-net-rotation condition with regard to hor-  gin of the coordinates is at the mass center of the Earth,
                izontal tectonic motions over the whole Earth.  and the direction and scale of the coordinate axes are the
                                                              same as ITRF. Table 1 shows the reference ellipsoid and
              Up to now, there are 12 ITRF realizations: ITRF89,   the Earth’s gravitational feld constants defned in BDCS,
            ITRF90, ITRF91, ITRF92, ITRF93, ITRF94, ITRF96,   including the semi-major axis and the fatness of the ref-
            ITRF97, ITRF2000, ITRF2005, ITRF2008, ITRF2014    erence ellipsoid, the geocentric gravitational constant
            (https:// www. iers. org/).                       and the angular velocity of the Earth rotation.
                                                                Te latest implementation of BDCS is done by using
            The space–time references of BDS                  more than 100 globally distributed ground stations as
            A Global Navigation Satellite System (GNSS) involves a
            large space–time range near the Earth. To achieve high-  Table 1  The reference ellipsoid and geocentric gravitational
            precision Positioning, Navigation, and Timing (PNT), the   constant adopted in BDCS
            unifed and high-precision space–time reference systems   Semi-major axis    a = 6,378,137.0 m
            must be established. Te construction of observation   Geocentric gravitational constant (Mass   μ = 3.986,004,418 ×  10   m /s 2
                                                                                                          3
                                                                                                        14
            models for the precise satellite orbit determination, time   of Earth’s atmosphere included)
            synchronization, and other information process should   Factor of ellipsoid fatness  f = 1/298.257222101
            be performed within a framework of the same space–  Mean angular velocity of the earth   ˙ Ω e  = 7.292115 ×  10  rad/s
                                                                                                      −5
            time benchmark.                                    rotation
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