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In fluid dynamics, wave–current interaction is the interaction between surface gravity waves and a mean 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 and phase-averaged flows, the quantity of primary importance for the dynamics of the interaction is the wave radiation stress tensor.
Wave–current interaction is also one of the possible mechanisms for the occurrence of rogue waves, such as in the Agulhas Current. When a wave 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:
Ocean, Atlantic Ocean, Oceanography, Marine geology, Geology
Soliton, Statistics, Oceanography, North Sea, Tsunami
Physical oceanography, Ocean, Wind, Tsunami, Wave power
Physical oceanography, Ocean, Antarctica, Thermohaline circulation, Coriolis effect
Physical oceanography, Wind wave, Ocean current, Coastal geography, Ocean
Physical oceanography, Coastal geography, Continental shelf, Wind wave, Coastal management
Physical oceanography, Coastal geography, Marine pollution, Ocean, Oceanic basin