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
... waves in oceans and seas , 1974 ; Davidan et . al . , 1985 ) . It is not enough to have only visual estimations to compute wind waves reliably , because they are plagued with low quality and wide spatial non- uniformity of the wind wave ...
... waves in oceans and seas , 1974 ; Davidan et . al . , 1985 ) . It is not enough to have only visual estimations to compute wind waves reliably , because they are plagued with low quality and wide spatial non- uniformity of the wind wave ...
Page 329
... wave spectrum , using the empirical proportions . Parametric models are based on the hypotheses of obtaining the stable form of wind wave spectrum controlled by nonlinear wave interactions . · The same idea can be used for the wave ...
... wave spectrum , using the empirical proportions . Parametric models are based on the hypotheses of obtaining the stable form of wind wave spectrum controlled by nonlinear wave interactions . · The same idea can be used for the wave ...
Page 336
... wave heights are estimated in shallow water according to a lognormal wave distribution . 0.99 0.95-- 0.90 0.80 0.70- 0.60- F ( h ) , ( % ) о 2 3 0.40 1.0 2.0 3.0 4.0 5.0 Mean wave height h ( m ) 6.0 7.0 Fig.9 . Distribution function for ...
... wave heights are estimated in shallow water according to a lognormal wave distribution . 0.99 0.95-- 0.90 0.80 0.70- 0.60- F ( h ) , ( % ) о 2 3 0.40 1.0 2.0 3.0 4.0 5.0 Mean wave height h ( m ) 6.0 7.0 Fig.9 . Distribution function for ...
Contents
OMAE99PA1135 | 19 |
OMAE99PA1141 | 39 |
PROPELLERICE INTERACTION | 53 |
Copyright | |
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