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The moon pulls the ocean on the near side of the earth more than it pulls on the center of the earth. The pull on the ocean at the far side of the earth is smaller still. This causes the near ocean to accelerate toward the moon most, the center of the earth less, and the far ocean still less.
8 Lacoste-Romberg GravimeterDrift Correction Fig. 20.3 Ocean tides are the result of the gravitational attraction of the moon and sun on the ocean. The tides formed by the moon are the lunar tides, and those formed by the sun are the solar tides. 9 Earth Tide CorrectionDrift and Tide CorrectionsRepeat Measurements.