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.
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]
Peregrine (1976) identifies five major sub-classes within wave–current interaction:
interaction of waves with a large-scale currentfield, with slow – as compared to thewavelength –two-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;
Bühler, O. (2014),Waves and mean flows (2nd ed.), Cambridge University Press,ISBN978-1-107-66966-6
Peregrine, D. H. (1976), "Interaction of water waves and currents",Advances in Applied Mechanics, vol. 16, Academic Press, pp. 9–117,ISBN978-0-12-002016-4
Craik, A. D. D. (1988),Wave interactions and fluid flows, Cambridge University Press,ISBN0-521-36829-4
Prandle, D. (1992),Dynamics and exchanges in estuaries and the coastal zone, Coastal and estuarine studies, vol. 40, American Geophysical Union,ISBN0-87590-254-5
Jonsson, I. G. (1990), "Wave–current interactions", in B. Le Méhauté and D. M. Hanes (ed.),Ocean Engineering Science, The Sea, vol. 9A, Wiley Interscience, pp. 65–120,ISBN0-471-11543-6