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Tide

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.

"Ebbing" redirects here. For the song by the Swans, see The Beggar. For the fictional town, see Ebbing, Missouri.

Tide tables can be used for any given locale to find the predicted times and amplitude (or "tidal range"). 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). They are however only predictions, the actual time and height of the tide is affected by wind and atmospheric pressure. Many shorelines experience semi-diurnal tides—two nearly equal high and low tides each day. Other locations have a diurnal tide—one high and low tide each day. A "mixed tide"—two uneven magnitude tides a day—is a third regular category.[1][2][a]


Tides vary on timescales ranging from hours to years due to a number of factors, which determine the lunitidal interval. To make accurate records, tide gauges at fixed stations measure water level over time. Gauges ignore variations caused by waves with periods shorter than minutes. These data are compared to the reference (or datum) level usually called mean sea level.[3]


While tides are usually the largest source of short-term sea-level fluctuations, sea levels are also subject to change from thermal expansion, wind, and barometric pressure changes, resulting in storm surges, especially in shallow seas and near coasts.


Tidal phenomena are not limited to the oceans, but can occur in other systems whenever a gravitational field that varies in time and space is present. For example, the shape of the solid part of the Earth is affected slightly by Earth tide, though this is not as easily seen as the water tidal movements.

The water stops falling, reaching a called low tide.

local minimum

Sea level rises over several hours, covering the ; flood tide.

intertidal zone

The water stops rising, reaching a called high tide.

local maximum

Sea level falls over several hours, revealing the intertidal zone; ebb tide.

Spring tide: Sun and Moon on the same side (0°)

Spring tide: Sun and Moon on the same side (0°)

Neap tide: Sun and Moon at 90°

Neap tide: Sun and Moon at 90°

Spring tide: Sun and Moon at opposite sides (180°)

Spring tide: Sun and Moon at opposite sides (180°)

Neap tide: Sun and Moon at 270°

Neap tide: Sun and Moon at 270°

Spring tide: Sun and Moon at the same side (cycle restarts)

Spring tide: Sun and Moon at the same side (cycle restarts)

The vertical (or radial) velocity is negligible, and there is no vertical —this is a sheet flow.

shear

The forcing is only horizontal ().

tangential

The appears as an inertial force (fictitious) acting laterally to the direction of flow and proportional to velocity.

Coriolis effect

The surface height's rate of change is proportional to the negative divergence of velocity multiplied by the depth. As the horizontal velocity stretches or compresses the ocean as a sheet, the volume thins or thickens, respectively.

the twice-daily variation

the difference between the first and second tide of a day

the spring–neap cycle

the annual variation

Misnomers

Tsunamis, the large waves that occur after earthquakes, are sometimes called tidal waves, but this name is given by their resemblance to the tide, rather than any causal link to the tide. Other phenomena unrelated to tides but using the word tide are rip tide, storm tide, hurricane tide, and black or red tides. Many of these usages are historic and refer to the earlier meaning of tide as "a portion of time, a season" and "a stream, current or flood".[83]

Simon, Bernard (2013) [2007]. . Translated by Manley, David. Institut océanographique, Fondation Albert Ier, Prince de Monaco. ISBN 978-2-903581-83-1. Archived from the original on 2022-11-13. Retrieved 2021-10-18.

Coastal Tides

NOAA Tides and Currents information and data

Archived 2015-05-09 at the Wayback Machine

History of tide prediction

Archived 2016-03-04 at the Wayback Machine

Department of Oceanography, Texas A&M University

UK Admiralty Easytide

UK, South Atlantic, British Overseas Territories and Gibraltar tide times from the UK National Tidal and Sea Level Facility

Tide Predictions for Australia, South Pacific & Antarctica

Tide and Current Predictor, for stations around the world