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/content/aip/journal/pof2/25/9/10.1063/1.4821810
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/content/aip/journal/pof2/25/9/10.1063/1.4821810
2013-09-20
2016-12-10

Abstract

We present a laboratory experiment in a large directional wave basin to discuss the instability of a plane wave to oblique side band perturbations in finite water depth. Experimental observations, with the support of numerical simulations, confirm that a carrier wave becomes modulationally unstable even for relative water depths < 1.36 (with the wavenumber of the plane wave and the water depth), when it is perturbed by appropriate oblique disturbances. Results corroborate that the underlying mechanism is still a plausible explanation for the generation of rogue waves in finite water depth.

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