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By Dress A.W.M., Koolen J.

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31)  cos 0 . 31) are used in the combination of results from local terrestrial observations and from satellite techniques, either in the global Cartesian system or in the local astronomical system. 4 Ellipsoidal Reference Coordinate Systems For most practical applications ellipsoidal coordinate systems are preferred because they closely approximate Earth’s surface, and they facilitate a separation of horizontal position and height. Usually a rotational ellipsoid is selected which is flattened at the poles and which is created by rotating the meridian ellipse about its minor axis b.

It should be noted that the results of different observation methods in satellite geodesy refer to particular reference coordinate systems which are related to the individual methods. These particular systems are not necessarily identical because they may be based on different data and different definitions. Often the relationship between these particular systems is known with an accuracy lower than the accuracy of the individual observation techniques. The establishment of precise transformation formulas between systems is one of the most important tasks in satellite geodesy.

Mueller, 1969; Schödlbauer, 2000). 6. 1 Reference Coordinate Systems 21 The relative orientation of the XCT -axis depends directly on Earth rotation and is determined through the apparent (= true) Greenwich Sidereal Time GAST (cf. 2]). The symbol θ is often used to denote GAST. 25)  xp −yp  . 26) For most practical purposes, the pole of the instantaneous true space-fixed equatorial system can be considered to be identical to the so-called Celestial Ephemeris Pole (CEP). ), 1992). The observed differences between the CEP and the conventional precession-nutation model are named celestial pole offsets dψ, dε.

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