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And R. Rummel, Theory of satellite geodesy and gravity field determination, Lecture Notes in Earth Sciences, SpringerVerlag, N. , 1989. 3. Lerch, F. J. , A geopotential model from satellite tracking, altimeter and surface gravity data: GEM-T3, J. Geophys. , 99, 28 15-2839, 1994. 4. K. Pavlis, The development and analysis of geopotential coefficient models to spherical harmonic degree 360, J. Geophys. , 95, 21885-21911, 1990. 5. Kaula, W. , Theory of Satellite Geodesy, Blaisdell Publ. , N. , 1966.

F. Eddy, N. L. Chandler, D. S. Chinn, S. Kapoor, K. E. Rachlin, L. E. Braatz and E. C. Pavlis, The GEM-T2 gravitational model, J. Geophys. , 95, 2204322071, 1990. McFadden, L. A. , D. J. Tholen and G. J. Vedder, Physical properties of Aten, Apollo and Amor Asteroids, in Asteroids II, edited by R. P. Binzel, T. Gehrels and M. S. Matthews, Univ. of Arizona Press, Tucson, 1258pp, 1992. , N. J. Borderies, W. L. Sjogren, Global Gravity and Topography, J. Geophys. , Planets, 98, 9113-9128, 1993. , Geodetic reference system 1980, in The Geodesist’s Handbook: 1984, edited by C.

Angle between the normal to the geoid and the normal to the ellipsoid). Ag is related to the perturbing potential through g is mean surface gravity The actual gravity vector is g=gradW The gravity perturbation vector on the geoid is given by (14) The deflection of the vertical has two components (northsouth 5 and east-west 11). The relationships between components &, and q of the deflection of the vertical, and CAZENAVE lfib b 120 140 160 2d0 240 2$0 3iE 320 340 35 368 Fig. 2 : Marine geoid mapped by satellite altimetry.

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