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Zhang et al. Satell Navig            (2021) 2:11                                         Page 2 of 10





            land-vehicle  navigation  (Rabbou  and  El-Rabbany  2015;   (Liu et al. 2017, 2018) and time transfer (Ge et al. 2019;
            Wielgosz et  al.  2005). In recent years, the efcient and   Tu et  al.  2019). Tis latter assumption causes adverse
            fexible PPP technique has also played a crucial role in   efects in these applications will be shown. In this regard,
            several non-positioning applications, especially in atmos-  the Modifed PPP (MPPP) functional model in iono-
            pheric (ionosphere and troposphere) sounding (Rovira-  spheric STEC retrieval and timing will be the focus of the
            Garcia et al. 2015; Shi et al. 2014; Yuan et al. 2014) as well   research. Te precise satellite orbit and clock products
            as time and frequency transfer (Defraigne et al. 2007; Ge   from an external provider such as the IGS are applied as
            et al. 2019; Orgiazzi et al. 2005; Tu et al. 2019).  deterministic corrections when conducting PPP, hence
              In the implementation of PPP, one needs to formulate   the MPPP proposed in this work is to be considered as a
            the functional model (i.e., observation equations), relat-  geometry-based method. Te model can simultaneously
            ing the GPS observations to the parameters to be esti-  obtain the variations of receiver code biases at two difer-
            mated. One assumption underlying this formulation is   ent frequencies using raw observations. In contrast, the
            that the receiver code biases do not change signifcantly   MCCL method that is actually a kind of geometry-free
            over time (Banville and Langley 2011b; Håkansson et al.   method (Zhang et al. 2019) can only detect the between-
            2017). A vast amount of work has cast considerable doubt   epoch fuctuations of Receiver Diferential Code Biases
            on the validity of this assumption (Bruyninx et al. 1999;   (RDCBs) and cannot be applicable to time or frequency
            Coster et al. 2013; Wanninger et al. 2017) and found that   transfer  because  the  receiver  clock  parameter  is elimi-
            the phenomenon of receiver code bias variation, which   nated in the geometry-free combinations of code and
            is  closely  related  to the  ambient temperature,  is  wide-  phase observations.
            spread. For example, the Geometry-Free  (GF) receiver   Te organization of this work proceeds as follows. In
            code biases, known as receiver Diferential Code Biases   “Methods” section, the full-rank functional model for the
            (DCBs) (Montenbruck et al. 2014; Sardon et al. 1994), has   original as well as the modifed PPP are constructed, fol-
            been found to exhibit an apparent intraday variability of   lowed by the interpretation of the estimable parameters.
            4 ns to 9 ns (Ciraolo et al. 2007), far exceeding the code   “Results” secrtion provides numerical insights into the
            noise level (depending on the receiver type, but gener-  ability of the MPPP to exclude the efects that the short-
            ally smaller than 1 ns). If the assumption of time-constant   term temporal variability of the receiver code biases has
            receiver code biases is taken, PPP solutions will be biased   on ambiguity estimation, ionospheric STEC retrieval and
            and hence the performances in PPP applications will be   timing. “Conclusions” section concludes the study with a
            degraded. For the ionospheric Slant Total Electron Con-  short discussion.
            tent (STEC) retrieval, the Modifed Carrier-to-Code Lev-
            eling (MCCL) method (Zhang et al. 2019), as well as the   Methods
            integer-levelling procedure (Banville and Langley 2011a;   In this section, the rank-defcient system of GPS obser-
            Banville et  al.  2012) can both efectively eliminate the   vation equations is taken as a starting point, and then
            efect of receiver code bias variations. As far as the GPS-  the two PPP models are presented (i.e., original and
            based  timing  application  is  concerned,  there  are  still  a   modifed), focusing mainly on developing the functional
            limited amount of research focusing on how to cope with   model and interpreting the estimable parameters.
            the time-varying receiver code biases.
              In this study, a modifed version of PPP is proposed,   GPS observation equations
            whose functional model contains time-varying receiver   Let us consider a scenario where m satellites, transmit-
            code  biases,  and  is  formulated  based  on  raw  observa-  ting  signals  on  f   frequencies,  are  tracked  by a  single
            tions instead of the Ionosphere-Free (IF) combinations.   receiver over t epochs. Under this scenario, the system of
            Te rank defciencies are removed, which are caused by   observation equations has the following form (Leick et al.
            the functional model and lead to the non-estimability of   2015),
            all the parameters, by fxing a minimum set of parame-  s    s     s            s     s         s
            ters to their prior values, resulting in a full-rank system   p (i) = l (i) + m τ r (i) + dt r (i) − dt (i) + µ j ι (i) + d r,j − d j
                                                                   r,j
                                                                                                  r
                                                                               r
                                                                         r
                                                                         s
                                                                   s
                                                                               s
                                                                                                   s
                                                                                            s
            of observation equations (Odijk et  al.  2016; Teunissen   φ (i) = l (i) + m τ r (i) + dt r (i) − dt (i) − µ j ι (i) + a s r,j
                                                                                                   r
                                                                               r
                                                                         r
                                                                   r,j
            1985). In this system of observation equations, the tem-                                      (1)
            poral  variations of  the  receiver  code  biases  on  two  fre-  with  r ,  s = 1, . . . , m ,  j = 1, . . . , f  and  i = 1, . . . , t being
            quencies become estimable. It will be shown that the   the receiver, satellite, frequency and epoch indices,
            ambiguity  parameters,  ionospheric  delay,  and  receiver   respectively, and where  p (i) and φ (i) denote, respec-
                                                                                            s
                                                                                   s
                                                                                            r,j
                                                                                   r,j
            clock ofset directly absorb the combination of time-  tively, the code and phase observables, l (i) the receiver-
                                                                                               s
                                                                                               r
            varying receiver code biases, which are normally con-  satellite range, τ (i) the zenith troposphere delay and m
                                                                                                            s
                                                                                                            r
                                                                           r
            sidered as constant in subsequent ionospheric modeling   the corresponding troposphere mapping function, dt r (i)
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