Volume 1: Offshore Technology 2020
DOI: 10.1115/omae2020-18806
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Model Tests and Numerical Prediction of the Low Frequency Motions of a Moored Ship in Shallow Water With a Wave Splitting Method

Abstract: Prediction of shallow water low frequency (LF) motions of vessels in the context of mooring analysis is challenging. Model tests are often performed to calibrate and validate numerical models and, in this way, reduce the uncertainty. Model tests are part of the positioning system qualifying process. However, model tests also present challenges and uncertainties related to parasitic low frequency wave systems which are unavoidable in shallow water ocean basin conditions. The paper presents model … Show more

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Cited by 3 publications
(3 citation statements)
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“…The LF-spectral shape must be the same for all positions in each realization. If not, this may suggest the presence of spurious free-waves or LF-reflection (see [2], [3] and [5]).…”
Section: Second Order Low-frequency (Lf) Bound Wavesmentioning
confidence: 99%
See 1 more Smart Citation
“…The LF-spectral shape must be the same for all positions in each realization. If not, this may suggest the presence of spurious free-waves or LF-reflection (see [2], [3] and [5]).…”
Section: Second Order Low-frequency (Lf) Bound Wavesmentioning
confidence: 99%
“…The mechanical generation of water waves in conventional experimental facilities can be hampered by the intrinsic boundary conditions of the laboratory. Wave reflection [1], spurious waves ( [2], [3], [4], [5]) and eigenmodes [6] are typical issues researchers must deal with when assessing model responses during test campaigns. However, in such facilities, the complex nonlinear physics of wave propagation is simply enforced by the laws of nature.…”
Section: Introductionmentioning
confidence: 99%
“…The second reason for the better agreement is the similar wave reflection behavior between the model test and the numerical simulation with active absorption. Because the location of the free surface elevation is known for each time step at all locations, it is possible to split the free surface elevation into incoming and reflected wave by use of two-dimensional Fouriertransformation from space-time representation to wave number and wave frequency representation [29]. Estimation of the reflected wave time series at wave gauge location 4 shows (Figure 6) that the significant wave height of the reflected wave time series is about 11% of the incident wave time series, i.e.…”
Section: Comparison Of One Realizationmentioning
confidence: 99%