Proceedings of the ... International Conference on Offshore Mechanics and Arctic Engineering, Volume 2American Society of Mechanical Engineers, 2001 - Arctic regions |
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Page 181
Sensitivity of 2 . order surge stand . dev . to numb . of wave headings ( cos ( theta
) distribution - waves only ) TABLE 3 : Comparison of low order cumulants for the
TLP surge response in unidirectional wind and waves . o 5 . 29 • - 3 wave ...
Sensitivity of 2 . order surge stand . dev . to numb . of wave headings ( cos ( theta
) distribution - waves only ) TABLE 3 : Comparison of low order cumulants for the
TLP surge response in unidirectional wind and waves . o 5 . 29 • - 3 wave ...
Page 182
FIGURE 6 : Comparison of probability density function for TLP surge response in
a combination of wind and waves . Davenport wind spectrum . Hg = 10 m . To =
11 sec , Vw = 28 m / sec 0 . 08 Exceedance probability 0 . 1 0 . 5 0 . 1 1 - 2 order ...
FIGURE 6 : Comparison of probability density function for TLP surge response in
a combination of wind and waves . Davenport wind spectrum . Hg = 10 m . To =
11 sec , Vw = 28 m / sec 0 . 08 Exceedance probability 0 . 1 0 . 5 0 . 1 1 - 2 order ...
Page 221
Therefore the wave spectrum generated by the local wind is always adjusted .
Number of Observations - 10 - g - 8 - 7 - 6 - 5 Decay n - 3 - 2 - 1 Figure 2 .
Distribution of the exponent n for the 243 selected cases of windsea decay in the
form ...
Therefore the wave spectrum generated by the local wind is always adjusted .
Number of Observations - 10 - g - 8 - 7 - 6 - 5 Decay n - 3 - 2 - 1 Figure 2 .
Distribution of the exponent n for the 243 selected cases of windsea decay in the
form ...
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