Do lakes have tidal waves?

Wave heights in a given part of a lake can vary considerably due to interactions that suppress some waves and amplify others. Therefore, there are waves in lakes, provided there is wind. The paths of the waves are both flattened and slowed by air resistance, which causes the wave amplitude (height) to increase and the wavelength to decrease (the waves become much steeper). The most important parameters of a wave are its wavelength (the horizontal distance between two crests or two troughs), its amplitude (the vertical distance between a trough and a crest) and its velocity (the speed at which the crests move across the water) (Figure 17).

Waves transfer energy, not water, and are usually caused by the wind as it blows across the ocean, lakes and rivers.

How do waves form on a lake?

They are quite fleeting and dissipate quickly when the wind dies down, or develop into the more common and permanent gravity waves. As the wave height increases, the sharpness of the wave crest can cause it to become unstable and break off, a process that is accelerated by the wind. The first wave motion to develop is relatively regular and consists of small, uniformly developed waves called capillary waves. Table 17.1 The parameters of wind waves in situations where the wind blows in roughly the same direction for long enough for the waves to fully develop.

When storm fronts move quickly over a large body of water such as Lake Michigan, changes in air pressure and strong wind gusts can form a large wave or series of large waves.

What are sea waves?

Although wind has the greatest influence on the formation of waves, atmospheric pressure changes can cause the water in the lake basin to slosh back and forth. As the waves push further inland past the sandbar, part of the sandbar eventually collapses, forcing the trapped water to flow back into the lake, resulting in a strong counter-current about a foot above the bottom of the water basin. The term was introduced by the Swiss hydrologist Fran├žois-Alphonse Forel in 1890, who was the first to make scientific observations of this effect in Lake Geneva. In these lakes, waves several metres high are not uncommon, although waves of about 7 metres (23 feet) are the highest to be expected.