
Spherical harmonic decompositions of the tides play an important role in many aspects of geodesy. This is especially so for the degree1 and degree2 components. The degree1 components are directly proportional to the tidal displacements of the geocenter. The degree2 components are related to the inertiatensor contributions to polar motion and Universal Time, and certain of them are directly proportional to the rate of working of gravitational tidal forces. Because of the importance of these lowdegree terms, the IERS Special Bureau for Tides is tabulating a large number of estimates of them from various models. The more reliable ocean models are based on Topex/Poseidon altimeter measurements, supplemented as necessary by hydrodynamic models in polar seas.
The spherical harmonic coefficients tabulated on these pages follow a consistent convention. In general, only a few of the lower degree and order coefficients are given, with some selected higher degree coefficients added because of their importance to satellite geodesy.
Still under construction.