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Wave–current interaction

From Wikipedia, the free encyclopedia
Interaction between surface gravity waves and a mean flow

Influid dynamics,wave–current interaction is the interaction betweensurface gravity waves and amean flow. The interaction implies an exchange of energy, so after the start of the interaction both the waves and the mean flow are affected.

For depth-integrated andphase-averaged flows, the quantity of primary importance for thedynamics of the interaction is the waveradiation stress tensor.

Wave–current interaction is also one of the possible mechanisms for the occurrence ofrogue waves, such as in theAgulhas Current. When awave group encounters an opposing current, the waves in the group may pile up on top of each other which will propagate into a rogue wave.[1][2]

Classification

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Peregrine (1976) identifies five major sub-classes within wave–current interaction:

  • interaction of waves with a large-scale currentfield, with slow – as compared to thewavelengthtwo-dimensional horizontal variations of the current fields;
  • interaction of waves with small-scale current changes (in contrast with the case above), where the horizontal current varies suddenly, over alength scale comparable with the wavelength;
  • the combined wave–current motion for currents varying (strongly) with depth below thefree surface;
  • interaction of waves withturbulence; and
  • interaction of ship waves and currents, such as in the ship'swake.

See also

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Footnotes

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  1. ^Dysthe, Kristian; Krogstad, Harald E.; Müller, Peter (2008), "Oceanic rogue waves",Annual Review of Fluid Mechanics,40 (1):287–310,Bibcode:2008AnRFM..40..287D,doi:10.1146/annurev.fluid.40.111406.102203
  2. ^Peregrine (1976)

References

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Waves
Upwelling





Antarctic bottom water
Circulation
Tides
Landforms
Plate
tectonics
Ocean zones
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