Results of world-wide earth-tide observations made by the Institute of Geophysics during the IGY are presented. The observations were made at 13 stations distributed around the world with two LaCoste and Romberg tidal gravity meters, each observation lasting 30 to 40 days. The data were analyzed by a method consisting of (a) a power spectrum analysis to determine the general noise background in the spectrum and (b) Fourier scanning of the major tidal lines to determine the amplitudes and phases of the gravity variation at each site as compared with the variation computed for a perfectly rigid earth. A Chebyshev window was used in the Fourier scanning to reduce contamination of the estimates by neighboring lines. Knowledge of the noise levels permits error limits to be assigned to the determination of the amplitude and phase relationships. The results obtained at the various stations differ significantly in relation to the estimated error limits and may be summarized as follows in comparison with theoretical results computed for various earth models. The amplitude ratio of the static tide on a homogeneous incompressible fluid earth to that on a rigid earth would be 1.25. For a semidiurnal tide on model earths of the Bullard I, II, Bullen B, and Gutenberg types, this ratio would have the values 1.161, 1.150, 1.162, and about 1.156, respectively. Our maximum observed value for the largest semidiurnal tide, M2, is 1.249 (Bermuda) and the minimum is 1.153 (New Delhi). The mean for the eight oceanic stations is 1.192, that for the four continental stations is 1.169, and the mean for all stations is 1.184. Thus our continental value is about 1 per cent greater than those computed for the Bullen B or Gutenberg models, but our mean oceanic value is 3 per cent greater. The causes of these variations require further investigation. It is believed that both the oceanic tides and regional geologic differences contribute to the variations. The O1 tide, whose period differs significantly from the solar day, also has a mean amplitude ratio of 1.18, but the P1 and K1 combination (whose period is 24 hours) gives the significantly different ratio 1.14 and is possibly influenced by the daily temperature cycle. The observed average phase lag of the M2 tide is compatible with the astronomical evidence concerning the changing rotation rate of the earth. However, the phases exhibit rather large local variations, the causes of which need further examination.
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