The statement which describes the interaction of forces that causes ocean tides is that tides are caused by gravitational interactions between the earth, sun, and moon.
Tides are the rise and drop of ocean levels caused by the combined impacts of the gravitational powers applied by the Moon (and to a much lesser degree, the Sun) and are moreover caused by the Soil and Moon circling one another.
Tides are commonly semi-diurnal (two tall glasses of water and two moo waters each day), or diurnal (one tidal cycle per day).
The two tall glasses of water on a given day are regularly not the same tallness (the day-by-day imbalance); these are the higher tall water and the lower tall water in tide tables.
Additionally, the two moo glasses of water each day are the higher moo water and the lower moo water. The day-by-day disparity isn't reliable and is for the most part little when the Moon is over the Equator.
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