Effect of Uncertainty on Slow Drift Motion of TLP

Author(s):  
Vini Anna Varghese ◽  
Nilanjan Saha
1993 ◽  
Vol 20 (3) ◽  
pp. 233-246 ◽  
Author(s):  
H.S. Choi ◽  
J.Y.K. Lou

Author(s):  
Richard C. Lupton ◽  
Robin S. Langley

As offshore wind turbines are installed in deeper water, interest is growing in floating wind turbines because, among other reasons, they may become cheaper than fixed-bottom turbines at greater depths. When analysing floating wind turbines, linear diffraction theory is commonly used to model the hydrodynamic loads on the platform. While it well known that slow drift motion due to second-order loads can be important for other floating offshore platforms, it has not yet been established how important such effects are for floating wind turbines. In this paper we aim to give a general result by developing approximate closed-form expressions to estimate the second-order slow drift motion of platforms of different sizes. The values are bench-marked against a typical calculation of the slow-drift response of a platform. The results show that floating wind turbines, which tend to have smaller dimensions than other floating structures, may be expected to show smaller slow-drift motions.


1989 ◽  
Vol 1989 (166) ◽  
pp. 151-162
Author(s):  
Takeshi Kinoshita ◽  
Kazuhito Takaiwa ◽  
Takahiro Murakami ◽  
Koichi Masuda

Author(s):  
Bernard Molin ◽  
Fabien Remy ◽  
Yanan Liu ◽  
Marie-Christine Rouault

An experimental campaign is reported on the slow-drift motion of a rectangular barge moored in irregular beam seas. The 24 m long false bottom of the basin is raised and inclined at a slope of 5%, from 1.05 m below the free surface to 0.15 m above. The barge is moored successively at 4 different locations, in water-depths ranging from 54 to 21 cm. The measured slow-drift component of the sway motion is compared with state-of-the-art calculations based on Newman approximation. At 54 cm depth good agreement is obtained between calculations and measurements. At 21 cm depth the Newman calculation exceeds the measured value. When the flat bottom setdown contribution is added up, the calculated value is 2 to 3 times larger than the measured one. A second-order model is proposed to account for the shoaling of a bichromatic sea-state propagating in decreasing water-depth. Application of this numerical model to the scale-model tests shows that in shoaling conditions the setdown contribution to the slow-drift excitation can counteract and not necessarily add up to the Newman component.


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