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
... wave parameters adduced in different manuals are rather different . Usually they are based on visual observations ... energy dissipation and G is nonlinear interaction in wind wave spectrum . One can consider that the dissipation of wave ...
... wave parameters adduced in different manuals are rather different . Usually they are based on visual observations ... energy dissipation and G is nonlinear interaction in wind wave spectrum . One can consider that the dissipation of wave ...
Page 329
equations of spectral parameters ( Davidan et . al , 1988 ; Ocean wave modeling , 1985 ) . Parametric methods have ... energy dissipation . But due to wind activity , its combination with the other mechanisms brings the spectrum to invariant ...
equations of spectral parameters ( Davidan et . al , 1988 ; Ocean wave modeling , 1985 ) . Parametric methods have ... energy dissipation . But due to wind activity , its combination with the other mechanisms brings the spectrum to invariant ...
Page 330
20 20. Fig.1 . General chart of water depths for wind wave numerical simulation ... wave parameters for large wind speeds and forecast the most dangerous waves ... energy , the semi- Lagrangian multiplier method is used ( Lavrenov , 1998 ) ...
20 20. Fig.1 . General chart of water depths for wind wave numerical simulation ... wave parameters for large wind speeds and forecast the most dangerous waves ... energy , the semi- Lagrangian multiplier method is used ( Lavrenov , 1998 ) ...
Contents
OMAE99PA1135 | 19 |
OMAE99PA1141 | 39 |
PROPELLERICE INTERACTION | 53 |
Copyright | |
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analysis angle applied Arctic ASME assumed average blade block boundary calculated Canada channel coefficient component conducted considered constant Copyright crack creep crushed dependence depth determined direction distribution effect Engineering equation estimate experiments factor failure field Figure floes flow force frequency friction function given height horizontal ice force ice loads ice sheet ice thickness iceberg icebreaker included increase indentation indentor interaction International layer length material maximum mean measured Mechanics method Newfoundland observed obtained occurred Offshore operations parameters peak performance predicted present pressure propeller range ratio region Report Research resistance salinity scale scour shape shear ship shown shows similar soil speed stamukha strain strength stress structure surface Table temperature tests thrust torque values vertical wave width wind zone