## 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 44

**Linear*** 271.0 AREG 3 Exp . Chak . $**Linear*** 2 0.341x10 -2 0.334x10 - 2 0.369x10 269.0 232.0 FIRST HARMONIC Ampl ( m ) Phase ( deg ) 0.487x10 -3106.3 ...Page 45

Exp .

Exp .

**Linear**( Eq.3 ) 3 3 2 w Chak . -4 Exp . -3**Linear**( Eq . 3 ) -5 1 -4 Time / period 0 FIG.4 RUN AREG 1 DECK DISPLACEMENT Time / period TIME HISTORIES ...Page 386

By writing the equation of motion for each point of the grid , including the one at the downstream end , a set of

By writing the equation of motion for each point of the grid , including the one at the downstream end , a set of

**linear**algebraic equations was obtained ...### 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