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Reference Frames in GNSS

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FundamentalsFundamentals
Title Reference Frames in GNSS
Author(s) J. Sanz Subirana, JM. Juan Zornoza and M. Hernandez-Pajares, University of Catalunia, Spain.
Level Basic
Year of Publication 2011

Brief descriptions of GPS WGS-84, GLONASS PZ-90 and Galileo GTRF reference frames are provided as follows.


GPS reference frame WGS-84

From 1987, GPS uses the World Geodetic System WGS-84, developed by the US Defence Department, which is a unified terrestrial reference system for position and vector referencing [footnotes 1]. Indeed, the GPS broadcast ephemeris are linked to the position of the satellite antenna phase centre in the WGS-84 reference frame. Thus, the user receiver coordinates will be expressed in the same ECEF frame.


The initial implementation of WGS-84 was realized from a set of more than a thousand terrestrial sites, which coordinates were derived from Transit observations [footnotes 2]. Successive refinements (which also leaded to some adjustments of the fundamental constants), using more accurate coordinates of the monitor stations, approximate to some ITRS realizations. For instance, realizations WGS84(G730) [footnotes 3] and WGS84(G873) correspond to ITRF92 and ITRF94, respectively. The refined frame WGS84(G1150) was introduced in 2002, which agrees with ITRF2000 at the centimetre level.


The parameters of the WGS-84 ellipsoid are given in the following Table 1:

Table 1: Ellipsoidal parameters WGS-84 (revised in 1997).


GLONASS reference frame PZ-90

The GLONASS broadcast ephemeris are given in the PZ-90 reference frame. As the WGS-84, this is an ECEF frame with a set of fundamental parameters associated (see table 2 from [GLONASS ICD, 2008][1]).


The determination of a set of parameters to transform the PZ-90 coordinates to the ITRF97 was the target of the International GLONASS Experiment (IGEX-98). [Boucher and Altamimi, 2001] [2]presents a review of the IGEX-98 experiment and, as a conclusion, they suggest the following transformation [footnotes 4] from [math]\displaystyle{ (x,y,z) }[/math] in PZ-90 to [math]\displaystyle{ (x',y',z') }[/math] in WGS-84, with a meter level of accuracy.


[math]\displaystyle{ \left [ \begin{array}{c} x'\\ y'\\ z'\\ \end{array} \right ] = \left [ \begin{array}{c} x\\ y\\ z\\ \end{array} \right ] + \left [ \begin{array}{ccc} -3\,ppb & -353\,mas & -4\,mas\\ 353\,mas & -3\,ppb & 19\,mas\\ 4\,mas & -19\,mas & -3\,ppb\\ \end{array} \right ] \left [ \begin{array}{c} x\\ y\\ z\\ \end{array} \right ] + \left [ \begin{array}{c} 0.07\,m\\ -0.0\,m\\ -0.77\,m\\ \end{array} \right ] \qquad\mbox{(1)} }[/math]


Following the notation of equation of Transformation between Terrestrial Frames:

[math]\displaystyle{ \left ( \begin{array}{c} x\\ y\\ z\\ \end{array} \right )_{_{TRF2}} = \left ( \begin{array}{c} x\\ y\\ z\\ \end{array} \right )_{_{TRF1}} + \left ( \begin{array}{c} T_1\\ T_2\\ T_3\\ \end{array} \right ) + \left ( \begin{array}{ccc} D & -R_3 & R_2\\ R_3 & D & -R_1\\ -R_2 & R_1 & D\\ \end{array} \right ) \left ( \begin{array}{c} x\\ y\\ z\\ \end{array} \right )_{_{TRF1}} }[/math]


the previous transformation (1) is defined by the parameters table:

GLONASS Table.png


According to the GLONASS modernisation plan, the ephemeris information implementing the PZ-90.02 reference system was updated on all operational GLONASS satellites from 12:00 to 17:00 UTC, September 20th., 2007. From this time on, the satellites are broadcasting in the PZ-90.02. This ECEF reference frame is an updated version of PZ-90, closest to the ITRF2000.


The transformation from PZ-90.02 to ITRF2000 contains only an origin shift vector, but no rotations nor scale factor, as it is shown in equation (2) [Revnivykh, 2007] [3]


[math]\displaystyle{ \left [ \begin{array}{c} x\\ y\\ z\\ \end{array} \right ]_{ITRF2000} = \left [ \begin{array}{c} x\\ y\\ z\\ \end{array} \right ]_{PZ-90.02} + \left [ \begin{array}{r} -0.36\,m\\ 0.08 \,m\\ 0.18 \,m\\ \end{array} \right ] \qquad\mbox{(2)} }[/math]


The parameters associated to the PZ-90 and PZ-90.02 are given in the next table 2 ([GLONASS ICD, 1998][4] and [GLONASS ICD, 2008]):


Table 2: Ellipsoidal parameters of PZ-90 and PZ-90.02.


Galileo reference frame (GTRF)

A consortium named the Galileo Geodetic Service Provider (GGSP), consisting of seven institutions under the lead of GeoForschungsZentrum Potsdam, is in charge of building up a prototype for the development of the Galileo Terrestrial Reference Frame (GTRF) and the establishment of a service with products and information for the potential users. This is a project fully funded by the Sixth Framework Program, under contract by the GSA, to be developed between 2005 and 2009 (http://www.ggsp.eu).

The initial coordinates for the reference stations are provided using GPS observations, because the GTRF is already being required by the time when the first Galileo signals are emitted during the IOV phase. Subsequent GTRF versions will use both GPS and Galileo observations. Weekly solutions will be performed for the long-term maintenance of the GTRF.

The connection to the ITRF is realized and validated by International GNSS Service (IGS) stations [footnotes 5], which are part of the ITRF, and especially by local ties to other geodetic techniques like satellite laser ranging and VLBI.

As is the case for GPS and GLONASS, the Galileo satellites will broadcast the satellite orbits in its own GTRF system, which will have centimetre-level alignment to ITRF [footnotes 6][5].


Notes

  1. ^ The document ``Modern Terrestrial Reference Systems PART 3: WGS-84 and ITRS contains data and interesting references about WGS-84 and ITRS (http://www.ngs.noaa.gov/CORS/Articles/Reference-Systems-Part-3.pdf).
  2. ^ With accuracy at the level of 1-2 meters, while the accuracy of the ITRF reference stations is at the centimetre level.
  3. ^ ``G indicates that it has exclusively been obtained with GPS observations and 730 indicates the GPS week.
  4. ^ [math]\displaystyle{ mas: }[/math] mili-arcseconds ([math]\displaystyle{ 1 mas = 4.84813681 \cdot 10^{-9} }[/math] radians). [math]\displaystyle{ ppb: }[/math] parts per billion ([math]\displaystyle{ 1 ppb=10^{-9} }[/math]).
  5. ^ The Galileo tracking stations (i.e., GSS), form a sparse global network. Thence, it is necessary to densify the network with additional stations to get the highest possible precision and stability for the GTRF.
  6. ^ In theory, GTRF is identical to ITRF2005 [Hofmann-Wellenhof et al., 2008].


References

  1. ^ [GLONASS ICD, 2008] GLONASS ICD, 2008. Technical report. v.5.1.
  2. ^ [Boucher and Altamimi, 2001] Boucher, C. and Altamimi, Z., 2001. ITRS, PZ-90 and WGS 84: current realizations and the related transformation parameters. Journal of Geodesy 75, pp. 613-619.
  3. ^ [Revnivykh, 2007] Revnivykh, S., 2007. GLONASS Status and Progress. In: Minutes of the 47th CGSIC Meeting, Forth Worth, Tx.
  4. ^ [GLONASS ICD, 1998] GLONASS ICD, 1998. Technical report. v.4.0.
  5. ^ [Hofmann-Wellenhof et al., 2008] Hofmann-Wellenhof, B., Lichtenegger, H., K. and Wasle, E., 2008. GNSS - Global Navigation Satellite Systems..Springer-Verlag, Wien, Austria.