![]() ![]() Tides vary on timescales ranging from hours to years due to a number of factors, which determine the lunitidal interval. ![]() A "mixed tide"-two uneven magnitude tides a day-is a third regular category. Other locations have a diurnal tide-one high and low tide each day. Many shorelines experience semi-diurnal tides-two nearly equal high and low tides each day. They are however only predictions, the actual time and height of the tide is affected by wind and atmospheric pressure. The predictions are influenced by many factors including the alignment of the Sun and Moon, the phase and amplitude of the tide (pattern of tides in the deep ocean), the amphidromic systems of the oceans, and the shape of the coastline and near-shore bathymetry (see Timing). Tide tables can be used for any given locale to find the predicted times and amplitude (or " tidal range"). ![]() Tides are the rise and fall of sea levels caused by the combined effects of the gravitational forces exerted by the Moon (and to a much lesser extent, the Sun) and are also caused by the Earth and Moon orbiting one another. Tide coming in, video stops about 1 + 1⁄ 2 hours before high tide In Maine (U.S.), low tide occurs roughly at moonrise and high tide with a high Moon, corresponding to the simple gravity model of two tidal bulges at most places however, the Moon and tides have a phase shift. Earth's rotation drags the position of the tidal bulge ahead of the position directly under the Moon showing the lag angle. Simplified schematic of only the lunar portion of Earth's tides, showing (exaggerated) high tides at the sublunar point and its antipode for the hypothetical case of an ocean of constant depth without land, and on the assumption that Earth is not rotating otherwise there is a lag angle. For other uses, see Tide (disambiguation). ![]()
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