Abstract
A spatial two-dimensional version of the Zakharov equation describing the evolution of deep-water gravity waves is used to derive two fourth-order evolution equations, for the amplitudes of the surface elevation and of the velocity potential. The scaled form of the equations is presented.
Original language | English |
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Pages (from-to) | 201-205 |
Number of pages | 5 |
Journal | Journal of Fluid Mechanics |
Volume | 450 |
DOIs | |
State | Published - 10 Jan 2002 |