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Waves might look like chaos (top), but there is a pattern to them (bottom).
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Top image courtesy of NASA; bottom image courtesy of NOAA

Ocean Waves

Ocean waves are usually formed by wind. Large waves will form if the wind is strong, if it blows over a large distance, and if it blows for a long time.

Waves may look chaotic when they approach a beach –crashing and full of sea foam. However, waves do have organization to them, especially in open water when they are not crashing.

A wave’s highest point is called its crest. The low point between two waves is called a trough. The vertical distance between crest and trough is called the wave height. The distance between two waves is called the wavelength and it is usually measured either from one crest to the next or from one trough to the next. The time it takes for waves to pass is called the wave period.

Why is it important to make all these wave measurements? Sailors rely on reports of the size of waves when planning travel. Surfers rely on reports of the size of waves when searching for places to surf. Waves have an impact on currents at the coast and beach erosion too.

Not all waves coming into a coast are the same size. Some are larger than average and others are smaller than average. About once every hour a wave comes by that is about double the size of the others. There are other types of large waves that are very rare such as rogue waves, which are extremely large, often travel alone and not in the direction of the other waves. A tsunami is also a powerful wave that is not caused by wind. It has such a long wavelength that it is not visible until it gets near shore.

Waves that travel very long distances – far from the winds that formed them – are called swells. Swells tend to be large waves with flatter crests and are very regular in shape and size.

When over deep water, the energy in a wave moves forward, but the water does not. The water moves up and down in circles. As waves move into shallow water, they act differently. The energy in the wave runs into the shallow seafloor. This causes the wave to steepen and eventually to topple over or break.

Last modified September 18, 2008 by Lisa Gardiner.

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