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 329
... deep water . These methods allow to diminish significantly the calculations and to make up poor knowledge of the physical mechanisms , which form the wind - wave spectrum , using the empirical proportions . Parametric models are based ...
... deep water . These methods allow to diminish significantly the calculations and to make up poor knowledge of the physical mechanisms , which form the wind - wave spectrum , using the empirical proportions . Parametric models are based ...
Page 336
... deep water regions of the Barents Sea , it is possible to calculate their extreme values by lognormal distribution , using the initial wave heights in deep water . Then we can estimate the corresponding mean wave heights at a given ...
... deep water regions of the Barents Sea , it is possible to calculate their extreme values by lognormal distribution , using the initial wave heights in deep water . Then we can estimate the corresponding mean wave heights at a given ...
Page 337
... deep water with h100 = 5.8 m one get σx , ≈0.1 , x , = 5.8 ± 0.16 , = 1.028 . XFIST Due to the presented relation one may conclude that ( for 95 % confidence interval ) ho.1 % changes in the range from 9,6 m to 10,2 m at a calculated ...
... deep water with h100 = 5.8 m one get σx , ≈0.1 , x , = 5.8 ± 0.16 , = 1.028 . XFIST Due to the presented relation one may conclude that ( for 95 % confidence interval ) ho.1 % changes in the range from 9,6 m to 10,2 m at a calculated ...
Contents
OMAE99PA1135 | 19 |
OMAE99PA1141 | 39 |
PROPELLERICE INTERACTION | 53 |
Copyright | |
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