## Proceedings of the ... International Conference on Offshore Mechanics and Arctic Engineering, Volume 2; Volume 7, Part 2American Society of Mechanical Engineers, 1988 - Arctic regions |

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Page 150

FIG.4 COMPARISONS BETWEEN MEASURED AND

FIG.4 COMPARISONS BETWEEN MEASURED AND

**COMPUTED**TIME SERIES OF SURGE MOTIONS IN REGULAR WAVE GROUPS ( WmVL78 2.96 ) 3 are in 12 Nii žlm ) Ni + V.D. Cal .Page 150

The second and third curves are the surge motions in regular wave groups

The second and third curves are the surge motions in regular wave groups

**computed**with and without the damping due to the effect of viscosity and wave ...Page 293

The finite - difference equation used to

The finite - difference equation used to

**compute**the vertical velocities is Oz ... The horizontal pressure gradients are**computed**first in the top layer ...### What people are saying - Write a review

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### Contents

HYDRODYNAMIC FORCESI | 1 |

Catchment Regions of Multiple Dynamic Responses in Nonlinear Problems of Offshore Mechanics | 15 |

Hydrodynamic Forces on a Floating Cylinder in Waves of Finite Depth | 23 |

Copyright | |

33 other sections not shown

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### Common terms and phrases

acting amplitude analysis angle applied approximately assumed body boundary breaking calculated coefficient columns compared comparison component computed considered corresponding cylinder damping density depend depth derived determined diameter direction distribution domain drag drift force dynamic effects elevation energy Engineering equation estimated evaluated excitation experimental experiments expressed field Figure floating flow fluid free surface frequency function given horizontal hydrodynamic incident increase integral irregular length linear load mass mean measured Mechanics method motion obtained Ocean Offshore oscillation panels parameters period phase potential predicted present pressure problem range ratio region regular waves relative Research respectively response second order shear ship shown shows significant simulation solution spectra spectrum structure surface Table theory values velocity vertical wave drift wave forces wave height wind