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Inside a wave | Measurement | How waves break

When a wave crashes ashore, do you think about the wind thousands of miles away? The larger the wave, the farther away it probably came from.

Inside a wave

Waves, either on the ocean or on a lake, are created as the wind blows over the water, turning particles of water in circles. Imagine the force of a breaking wave as accumulated wind energy near the water's surface. Each particle of water transmits energy to the next.

Wave size depends on how hard the wind blows, and how long it blows in one direction (scientists call this "fetch"). As waves move, each particle of water stays in roughly the same area.

Measuring waves

A wave's amplitude is the distance between equilibrium and a crest, or equilibrium and a trough. The distance between wave crests is called wavelength. The longer the wavelength, the faster a wave moves.

How waves break

As the seafloor becomes less deep near the coast, it drags on the wave and slows it down. This compresses the distance between wave crests and increases the height. Finally, the top of the wave falls down, or breaks.

Though commonly confused, wind waves are not the same as tsunamis. ez

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