## 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 5

Generally it is assumed that the solution of the complete boundary - value

Generally it is assumed that the solution of the complete boundary - value

**problem**for $ exists , and is unique ; mathematical proofs exist only for ...Page 132

+ 8 2012 } .2100034 , g at дz at ? the complete second - order

+ 8 2012 } .2100034 , g at дz at ? the complete second - order

**problem**is not attempted . Instead , an approximate solution is sought in which the ...Page 191

For The far field asymptotic solutions for the 2ndorder diffracted waves have been developed , both in three - and two - dimensional

For The far field asymptotic solutions for the 2ndorder diffracted waves have been developed , both in three - and two - dimensional

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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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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