A detailed analysis of all the variables that affect the tides at any particular coast reveals that nearly 400 factors are involved.
The rising and falling sea levels known as tides are a result of the gravitational pull of the Moon, Sun, and rotation of the Earth.
To determine the anticipated times and amplitude for any location, tide tables can be employed (or "tidal range"). The Sun and Moon alignment, the phase and amplitude of the tide (the pattern of tides in the deep ocean), the amphidromic systems of the oceans, the form of the shoreline, and near-shore bathymetry are only a few of the variables that affect the predictions (see Timing).
However, they are merely projections; the wind and air pressure have an impact on the tide's actual timing and height. Semi-diurnal tides—two about equal high and low tides—occur along many shorelines.
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