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  2. Wave shoaling - Wikipedia

    en.wikipedia.org/wiki/Wave_shoaling

    In fluid dynamics, wave shoaling is the effect by which surface waves, entering shallower water, change in wave height. It is caused by the fact that the group velocity, which is also the wave-energy transport velocity, decreases with water depth. Under stationary conditions, a decrease in transport speed must be compensated by an increase in ...

  3. Green's law - Wikipedia

    en.wikipedia.org/wiki/Green's_law

    Propagation of shoaling long waves, showing the variation of wavelength and wave height with decreasing water depth.. In fluid dynamics, Green's law, named for 19th-century British mathematician George Green, is a conservation law describing the evolution of non-breaking, surface gravity waves propagating in shallow water of gradually varying depth and width.

  4. Shoal - Wikipedia

    en.wikipedia.org/wiki/Shoal

    Shoaling can also refract waves, so the waves change direction. For example, if waves pass over a sloping bank which is shallower at one end than the other, then the shoaling effect will result in the waves slowing more at the shallow end. Thus, the wave fronts will refract, changing direction like light passing through a prism.

  5. Wind wave - Wikipedia

    en.wikipedia.org/wiki/Wind_wave

    Video of large waves from Hurricane Marie along the coast of Newport Beach, California. In fluid dynamics, a wind wave, or wind-generated water wave, is a surface wave that occurs on the free surface of bodies of water as a result of the wind blowing over the water's surface. The contact distance in the direction of the wind is known as the fetch.

  6. 'Biggest I've ever seen': Manasquan Inlet shoal is growing ...

    www.aol.com/biggest-ive-ever-seen-manasquan...

    Significant shoaling has frequently occurred within this inlet and often dissipates due to wind/wave conditions. Coastal inlets are dynamic and can rapidly change, but it’s important for us to ...

  7. Wave nonlinearity - Wikipedia

    en.wikipedia.org/wiki/Wave_nonlinearity

    In the shoaling zone, the wave nonlinearity increases due to the decreasing depth and the sinusoidal waves approaching the coast will transform into skewed waves. As waves propagate further towards the coast, the wave shape becomes more asymmetric due to wave breaking in the surf zone until the waves run up on the beach in the swash zone.

  8. Shoaling and schooling - Wikipedia

    en.wikipedia.org/wiki/Shoaling_and_schooling

    Shoaling and schooling. These powder blue tangs are shoaling. They are swimming somewhat independently, but in such a way that they stay connected, forming a social group. These bluestripe snapper are schooling. They are all swimming in the same direction in a coordinated way. In biology, any group of fish that stay together for social reasons ...

  9. Wave setup - Wikipedia

    en.wikipedia.org/wiki/Wave_setup

    Wave setup. In fluid dynamics, wave setup is the increase in mean water level due to the presence of breaking waves. Similarly, wave setdown is a wave-induced decrease of the mean water level before the waves break (during the shoaling process). For short, the whole phenomenon is often denoted as wave setup, including both increase and decrease ...