Type-II vortices form around a dipole-oscillating subwavelength island in gravity-capillary waves, with emergence and handedness controlled by the relative phase to an incident plane wave.
A review of the physical oceanography of the seas around New Zealand – 1982
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Wave Vortices Around Oscillating Subwavelength Holes: Water-Wave Observation
Type-II vortices form around a dipole-oscillating subwavelength island in gravity-capillary waves, with emergence and handedness controlled by the relative phase to an incident plane wave.