2.5 ITRS and other terrestrial reference systems

\subsection{Relation of the ITRS to other terrestrial reference systems} It is worthwhile to look at the relation of the ITRF to other global frames. For practical purposes, some global systems were introduced on national level. Of particular interest here is the World Geodetic System (WGS), which is still widely used in nonscientific applications. A first World Geodetic Reference System was in 1960 introduced by the U.S. Department of Defense (DoD) as WGS60 and later updated through WGS66 and WGS72. In 1984, the DoD introduced the World Geodetic System 1984 (WGS84). The first materialization of the WGS84 was based on observations from the U.S. Navy Navigation Satellite System (Doppler Transit). This materialization of the WGS84 was achieved by aligning as closed as possible the DoD reference frame NSWC-9Z2 to the BIH Conventional Terrestrial System (BTS) at the epoch 1984.0. The latler was realized by the adopted coordinates of a globally distributed set of tracking stations with an estimated accuracy of 1-2 meters. In January 1987, the U.S. Defense Mapping Agency (DMA) started using the WGS84 for the computation of the precise ephemerides of the TRANSIT satellites. Using these ephemerides, the coordinates of the ten DoD GPS monitoring stations were determined by Doppler tracking. Until recently, GPS broadcast orbits were generated from GPS tracking data from these stations, fixing the Doppler derived coordinates of these stations (i.e.~neglecting any station movement, including tectonic plate motions). Based on broadcast ephemeries, GPS receivers provide coordinates in the WGS84, and for many practical purposes such as air navigation, the WGS84 is in use\footnote{see www.wgs84.com/default.htm for an example}. Therefore, it is worthwhile to consider the current relation between WGS84 and the more accurate ITRF. In 1994, the DoD made an attempt to align WGS84 with ITRF. For that, new coordinates for the ten DoD tracking stations were determined at the epoch 1994.0 used GPS tracking data collected at these sites together with a subset of the IGS tracking stations, with the ITRF91 coordinates of the later stations being held fixed in the process. This refined WGS84 realization is denoted as WGS84 (G730), with the 'G' indicating that the frame is GPS derived and '730' denoting the GPS week number when the new coordinates where implemented by DMA in their orbit processing. Moreover, the original WGS84 GM value was replaced by the value given in the IERS 1992 standards \cite[see][the value there is $3986004.418 \cdot 10^8$ m$^3$/s$^2$]{mccarthy92}. The introduction of this new frame for GPS resulted in more precise ephemeris in the GPS broadcast messages. For the original realization of the WGS84, transformation parameters between the ITRF and WGS84 are available for the ITRF90. Based on a comparison of ITRF and WGS84 (G730) and the later WGS84 (G873), it is found that these new WGS84 realizations are coincident with ITRF at about the 0.1 meter level. For these realizations there are no official transformation parameters available. This means that one can consider ITRF coordinates also to be expressed in WGS84 at the 10 cm level. The importance of the ITRF as the most accurate global reference frame is increasingly acknowledged outside the scientific community. For example, the European Commission and the Government of the United States of America recently agreed to align the reference systems of Galileo and GPS as close as possible to the ITRS, in order to ensure the interoperability of the two GNSS \cite[]{europeancom2004}.