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A semidiurnal tide is a tidal phenomenon that occurs twice a day. This means there are two high tides and two low tides within approximately a 24-hour and 50-minute period. This type of tide is prevalent along the eastern coast of the Atlantic Ocean and much of the Americas. The solid Earth also experiences semidiurnal tides, influenced by the gravitational pull of the Sun and Moon, though these typically have a smaller vertical amplitude of about one foot or less.123

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