## 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

Generally it is assumed that the

**solution**of the complete boundary - value problem for exists , and is unique ... homogeneous**solutions**of ( 1 ) exist , i.e. the right - hand side of ( 1 ) is zero but the potential on the body ( and its ...Page 19

We are interested here in the catchment regions of these

We are interested here in the catchment regions of these

**solutions**and so to illustrate our methods we shall fix the variable coefficients so that the equation can either exhibit a harmonic**solution**or a subharmonic**solution**of order 4.Page 193

ASYMPTOTIC

ASYMPTOTIC

**SOLUTIONS**AND RADIATION CONDITIONS FOR SECONDThe asymptotic**solution**consists of three parts . The first term in eq . ( 29 ) is general**solution**associated with the homogeneous free surface condition .### 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 |

OFFSHORE TECHNOLOGY GEOTECHNICAL ENGINEERING | 21 |

Copyright | |

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acting added amplitude analysis applied approximately assumed body boundary breaker breaking calculated coefficients columns compared comparison component computations considered corresponding cylinder damping density dependence depth derived determined diameter direction distribution domain drag drift force dynamic effects elevation Engineering equation error 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 maximum mean measured Mechanics method motion obtained Ocean Offshore oscillation panels parameters period phase platform potential predicted present pressure probability problem range ratio region regular waves relative respectively response shear shown shows simulation solution spectra spectrum structure surface Table tests theory values velocity vertical vortex wave drift wave forces wave height