Time evolution of three-dimensional nonlinear gravity–capillary free-surface flows

E.I. Părău; J. M. Vanden-Broeck; M. J. Cooker

doi:10.1007/s10665-010-9391-y

Time evolution of three-dimensional nonlinear gravity–capillary free-surface flows

E.I. Părău, J. M. Vanden-Broeck, M. J. Cooker

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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
Pages (from-to)	291-300
Number of pages	10
Journal	Journal of Engineering Mathematics
Volume	68
Issue number	3-4
DOIs	https://doi.org/10.1007/s10665-010-9391-y
Publication status	Published - 2010

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Cite this

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title = "Time evolution of three-dimensional nonlinear gravity–capillary free-surface flows",

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.",

author = "E.I. P{\u a}r{\u a}u and Vanden-Broeck, {J. M.} and Cooker, {M. J.}",

year = "2010",

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language = "English",

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journal = "Journal of Engineering Mathematics",

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T1 - Time evolution of three-dimensional nonlinear gravity–capillary free-surface flows

AU - Părău, E.I.

AU - Vanden-Broeck, J. M.

AU - Cooker, M. J.

PY - 2010

Y1 - 2010

N2 - 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.

AB - 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.

U2 - 10.1007/s10665-010-9391-y

DO - 10.1007/s10665-010-9391-y

M3 - Article

VL - 68

SP - 291

EP - 300

JO - Journal of Engineering Mathematics

JF - Journal of Engineering Mathematics

SN - 0022-0833

IS - 3-4

ER -