Waves at shallow water
Waves at shallow water develop when the ocean surface waves travel into the coastal area where the wavelength is much larger than the water depth. The normal circular motion of the water particles there is disrupted by the ocean bottom. As the water becomes shallower, the swell on the water surface becomes higher and steeper. After the wave breaks, the water flows violently, turbulently. This is where erosion of the ocean bottom and shore line intensifies dramatically. The most devastating effect may happen in the case of tsunami.
Related pages[change | change source]
Notes[change | change source]
|Wikimedia Commons has media related to Ocean surface waves.|
- "Exploring the World Ocean. Online LearningCenter". Archived from the original on 2011-05-25. Retrieved 2011-03-23.