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Tides

Tides are the regular rise and fall of sea level produced by the gravitational attraction of the Moon and, to a lesser extent, the Sun on the Earth's oceans. The Moon's gravity pulls most strongly on the water nearest to it, drawing it into a bulge, while a second bulge forms on the opposite side of the Earth. As the planet rotates beneath these bulges, most coasts experience the sea rising to high tide and falling to low tide in a repeating cycle through the day.

The Sun also raises tides, but because it is far more distant its tidal effect is weaker than the Moon's despite its enormous mass. The combined pull of the two bodies varies as their positions change. When the Sun, Earth, and Moon are aligned, at new and full Moon, their gravitational forces reinforce one another to produce spring tides, with the greatest difference between high and low water. When the Sun and Moon are at right angles relative to the Earth, their effects partly cancel, giving the smaller neap tides.

The strength of tides also changes with the Moon's varying distance from the Earth along its orbit. When the Moon is nearest, its gravitational pull is stronger and the resulting tides are higher, so that especially large spring tides occur when alignment coincides with the Moon's closest approach. Because tides follow the predictable motions of the Moon and Sun, their timing and height can be forecast far in advance, which is important for navigation, fishing, and coastal activities.

Frequently asked questions

What causes tides?
Tides are caused mainly by the Moon's gravitational pull on the oceans, which raises bulges of water, with a smaller contribution from the Sun.
What is the difference between spring and neap tides?
Spring tides, with the largest range, occur when the Sun and Moon align and reinforce each other. Neap tides, with the smallest range, occur when they are at right angles.
Why is the Sun's tidal effect weaker than the Moon's?
Although the Sun is far more massive, it is much more distant, and tidal force falls off sharply with distance, so the nearer Moon dominates the tides.





Tides visit also Space: earth and moon, The Moon, Tidal Power
Causes of tides interaction of the earth and the moon , effect of the earth's ocean basins and land masses
Earth, moon and ocean interaction in the sea
Gravity applications
Mathematical explanation of tides
Perigean spring tides Perigean spring tides
Tidal movements The tide is the vertical rise and fall of the sea level surface caused primarily by the change in gravitational attraction of the moon, and to a lesser extent the sun, ...
Tidal prediction Tidal prediction
Tidal theory The word "tides" is a generic term used to define the alternating rise and fall in sea level with respect to the land, produced, in part, by the gravitational attraction of the moon and sun. There are additional nonastronomical factors influencing local heights and times of tides such as configuration of the coastline, depth of the water, ocean-floor topography, and other hydrographic and meteorological influences, pdf file
Tide generating forces the tide generating force is the sum of gravitational and centrifugal forces
Tide glossary
Tide prediction from charts and tables
Tides applet (scroll down)
Tides the tidal forces can be defined as the variation of the local surface gravity, under the influence of celestial bodies (Sun, Moon)
Tides What are Tides
Tides What are Tides
Tides Comprehend general causes and types of tides, Understand tidal reference planes and their uses as depth and height references on nautical charts, pdf file
Tides A dynamical picture of the oceanic tides, pdf file
Tides Moon's Gravity, Spring Tides, Neap Tides
TIDES AND TIDAL CURRENTS Tides are the periodic motion of the waters of the sea due to changes in the attractive forces of the Moon and Sun upon the rotating Earth, pdf file
Tides and tide prediction Tides and tide prediction
Tides and Water Levels Tides and Water Levels, What are Tides? What Causes Tides? Gravity, Inertia, and Bulges, Changing Angles and Tides, The Frequency of Tides, Tidal Variations, Types and Causes of Tidal Cycles, What Else Affects Tides? Monitoring the Tides, How are Tides Measured
Tides: lunar tides The tides at a given place in the Earth's oceans occur about an hour later each day. Since the Moon passes overhead about an hour later each day, it was long suspected that the Moon was associated with tides. Newton's Law of Gravitation provided a quantitative understanding of that association
Tides: misconceptions about tides
Tides: oceanography lecture notes
Tides: ocean tides an ocean tide refers to the cyclic rise and fall of seawater. Tides are caused by slight variations in gravitational attraction between the Earth and the moon and the sun in geometric relationship with locations on the Earth's surface. Tides are periodic primarily because of the cyclical influence of the Earth's rotation
Tides Online High Water Condition
Types of Tides and Tidal Currents At most places on earth, there are two high tides and two low tides a day. They follow a cycle that coincides with the 24- hour 50- minute lunar day, the time it takes earth to make one, pdf file

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