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Qué (quién) es tidal traffic - definición
![Figure 4: The Moon's gravity ''differential'' field at the surface of the Earth is known (along with another and weaker differential effect due to the Sun) as the Tide Generating Force. This is the primary mechanism driving tidal action, explaining two tidal [[equipotential]] bulges, and accounting for two high tides per day. In this figure, the Earth is the central blue circle while the Moon is far off to the right. The '''outward''' direction of the arrows on the right and left indicates that where the Moon is overhead (or at the [[nadir]]) its perturbing force opposes that between the earth and ocean.](https://commons.wikimedia.org/wiki/Special:FilePath/Field tidal.svg?width=200 "Figure 4: The Moon's gravity ''differential'' field at the surface of the Earth is known (along with another and weaker differential effect due to the Sun) as the Tide Generating Force. This is the primary mechanism driving tidal action, explaining two tidal [[equipotential]] bulges, and accounting for two high tides per day. In this figure, the Earth is the central blue circle while the Moon is far off to the right. The '''outward''' direction of the arrows on the right and left indicates that where the Moon is overhead (or at the [[nadir]]) its perturbing force opposes that between the earth and ocean.")
![publisher=[[CRC Press]]}}</ref>](https://commons.wikimedia.org/wiki/Special:FilePath/Saturn PIA06077.jpg?width=200 "publisher=[[CRC Press]]}}</ref>")
![Figure 1: [[Comet Shoemaker-Levy 9]] in 1994 after breaking up under the influence of [[Jupiter]]'s tidal forces during a previous pass in 1992.](https://commons.wikimedia.org/wiki/Special:FilePath/Shoemaker-levy-tidal-forces.jpg?width=200 "Figure 1: [[Comet Shoemaker-Levy 9]] in 1994 after breaking up under the influence of [[Jupiter]]'s tidal forces during a previous pass in 1992.")
![Aerial photo of North Sea, tidal inlets from the [[Wadden Sea]] on Scharhörn](https://commons.wikimedia.org/wiki/Special:FilePath/11-09-04-fotoflug-nordsee-by-RalfR-011.jpg?width=200 "Aerial photo of North Sea, tidal inlets from the [[Wadden Sea]] on Scharhörn")
![wake]] shows the power in the [[tidal current]].](https://commons.wikimedia.org/wiki/Special:FilePath/SeaGen installed.jpg?width=200 "wake]] shows the power in the [[tidal current]].")
Wikipedia
The tidal force is a gravitational effect that stretches a body along the line towards the center of mass of another body due to a gradient (difference in strength) in gravitational field from the other body; it is responsible for diverse phenomena, including tides, tidal locking, breaking apart of celestial bodies and formation of ring systems within the Roche limit, and in extreme cases, spaghettification of objects. It arises because the gravitational field exerted on one body by another is not constant across its parts: the nearest side is attracted more strongly than the farthest side. It is this difference that causes a body to get stretched. Thus, the tidal force is also known as the differential force, as well as a secondary effect of the gravitational field.
In celestial mechanics, the expression tidal force can refer to a situation in which a body or material (for example, tidal water) is mainly under the gravitational influence of a second body (for example, the Earth), but is also perturbed by the gravitational effects of a third body (for example, the Moon). The perturbing force is sometimes in such cases called a tidal force (for example, the perturbing force on the Moon): it is the difference between the force exerted by the third body on the second and the force exerted by the third body on the first.
