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The geopotential variation caused by solid Earth, ocean and atmospheric tides can be estimated from artificial satellite orbit
perturbations. It is shown that the total tidal variation in geopotential field derived from satellite tracking data, combined
with the recent accurate measurements of ocean tide obtained by Topex/Poseidon and atmospheric tide model, permits the estimates
of the solid earth tide phase lags for M2 and K1 constituents (respectively 0.12° and 0.13°). This result agrees rather well
with the result 0.16° derived from satellite data by Ray and the constrained theoretical result 0.21° given by Zschau; whereas
the results given by gravity tidal methods are rather scattering in the phase lag determination. 相似文献
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