Abstract
The evolution in time of three-dimensional gravity and gravity–capillary free-surface flows generated by a moving pressure distribution is considered. Solutions of the fully nonlinear equations in deep water are calculated by boundary-integral-equation methods and marching in time. Comparisons between unsteady and steady solutions are discussed.
Original language | English |
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Pages (from-to) | 291-300 |
Number of pages | 10 |
Journal | Journal of Engineering Mathematics |
Volume | 68 |
Issue number | 3-4 |
DOIs | |
Publication status | Published - 2010 |