## Proceedings of the ... International Conference on Offshore Mechanics and Arctic Engineering, Volume 18, Part 5American Society of Mechanical Engineers, 1999 - Arctic regions |

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Page 328

To perform the model numerically let us express s ( 2,1,1 ) as a

spectrum S ( k.B , x , y , 1 ) ( where k = k ) , B = arctg ( k , / k , ) ) . Describing the

total derivative in time in the left part of Eq . ( 1 ) , we pass to the following

equation : as ...

To perform the model numerically let us express s ( 2,1,1 ) as a

**directional**spectrum S ( k.B , x , y , 1 ) ( where k = k ) , B = arctg ( k , / k , ) ) . Describing the

total derivative in time in the left part of Eq . ( 1 ) , we pass to the following

equation : as ...

Page 329

... 1988 ) , but for a shallow water , wave number spectra and

should be used instead of frequency and angle spectra . The spectrum is a

function of wave process dispersion mo , the wave number of spectral maximum

kmar ...

... 1988 ) , but for a shallow water , wave number spectra and

**directional**spectrashould be used instead of frequency and angle spectra . The spectrum is a

function of wave process dispersion mo , the wave number of spectral maximum

kmar ...

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### Contents

OMAE99PA1135 | 19 |

OMAE99PA1141 | 39 |

PROPELLERICE INTERACTION | 53 |

Copyright | |

24 other sections not shown

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