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Modeling Broad-Frequency-Band Water-Wave Experiments with Generalizations of the Nonlinear Schrodinger Equation
Waves generated by storms gradually disperse, forming swells that can travel thousands of kilometers across the ocean's surface. The evolution of deep-water swells, which are unaffected by the seafloor, can be modeled by the nonlinear Schrodinger (NLS) equation and its generalizations. These models
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