The gravitational pull of the moon and sun is the primary force behind ocean tides, with the moon's influence being particularly significant. Wind and atmospheric pressure also affect tides but do not create them; they can, however, contribute to phenomena like storm surges. The difference in gravitational acceleration between the Earth's surface and its center leads to tidal acceleration, resulting in high tides on both the near and far sides of the Earth. Understanding tides involves recognizing the interaction of these large masses and their gravitational fields, rather than just the moon's pull. Overall, the periodic nature of tides is influenced by the orbits and positions of the moon and sun relative to the Earth.