Details
Original language | English |
---|---|
Pages (from-to) | 279-296 |
Number of pages | 18 |
Journal | Applied Ocean Research |
Volume | 53 |
Publication status | Published - Oct 2015 |
Abstract
In this paper, the evolution of focused waves using different paddle displacements (piston type) under laboratory conditions is presented. It is well known that in intermediate water depths, linear paddle displacements will generate spurious, free, sub and super harmonics. Thus, a second order correction to suppress these spurious free sub and super harmonics was used to generate the focused waves. The focused waves were generated in the laboratory using a linear superimposition principle, in which the wave paddle displacement is derived based on the sum of a number of sinusoidal components at discrete frequencies, whose phases are accordingly set to focus at a particular location. For this method of generation, the second order wave maker theory proposed by Schäffer [24] can be easily adopted and was used in the present study. Two different centre frequencies (fc=0.68Hz and 1.08Hz) with three different bandwidth ratios (δf/fc=0.5, 0.75 and 1.0) were tested in a constant water depth, to consider both narrow and broadband spectra. These test cases correspond to wave focusing packets propagating in intermediate and deep water regions. Further, for each wave packet, two different amplitudes were considered in order to analyze non-breaking and breaking cases. Thus, by systematically generating the wave packets using the linear and second order paddle displacements, the analysis was carried out for the spectral and temporal evolution of selected long waves. The temporal evolution of the selected harmonics was analyzed using the Inverse Fast Fourier Transform (IFFT), to show the propagation of the spurious, free, long waves. Further, the variations in energy for the lower, higher and primary frequency ranges are reported for different wave paddle displacements. The analysis revealed that for the broadband spectrum the differences are more pronounced when using linear paddle displacements. We have also noticed a shift in focusing/breaking location and time (i.e. premature) due to the increase in crest height using linear displacements. The experiment data used in this paper has been provided as a supplementary, which can be used to validate the numerical models.
ASJC Scopus subject areas
- Engineering(all)
- Ocean Engineering
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In: Applied Ocean Research, Vol. 53, 10.2015, p. 279-296.
Research output: Contribution to journal › Article › Research › peer review
}
TY - JOUR
T1 - Focused wave evolution using linear and second order wavemaker theory
AU - Sriram, V.
AU - Schlurmann, T.
AU - Schimmels, S.
N1 - Cited By :39 Export Date: 1 February 2021 Funding details: Alexander von Humboldt-Stiftung Funding text 1: This research work is a part of ‘Violent wave–current interactions with offshore wind energy structure’ funded by Alexander Von Humboldt Foundation , Germany. Their support is acknowledged by the first author. Many fruitful discussions by the first author with Prof. K.F. Deamerich are greatly acknowledged, particularly the idea to represent the bound long waves in time domain for broad band spectra.
PY - 2015/10
Y1 - 2015/10
N2 - In this paper, the evolution of focused waves using different paddle displacements (piston type) under laboratory conditions is presented. It is well known that in intermediate water depths, linear paddle displacements will generate spurious, free, sub and super harmonics. Thus, a second order correction to suppress these spurious free sub and super harmonics was used to generate the focused waves. The focused waves were generated in the laboratory using a linear superimposition principle, in which the wave paddle displacement is derived based on the sum of a number of sinusoidal components at discrete frequencies, whose phases are accordingly set to focus at a particular location. For this method of generation, the second order wave maker theory proposed by Schäffer [24] can be easily adopted and was used in the present study. Two different centre frequencies (fc=0.68Hz and 1.08Hz) with three different bandwidth ratios (δf/fc=0.5, 0.75 and 1.0) were tested in a constant water depth, to consider both narrow and broadband spectra. These test cases correspond to wave focusing packets propagating in intermediate and deep water regions. Further, for each wave packet, two different amplitudes were considered in order to analyze non-breaking and breaking cases. Thus, by systematically generating the wave packets using the linear and second order paddle displacements, the analysis was carried out for the spectral and temporal evolution of selected long waves. The temporal evolution of the selected harmonics was analyzed using the Inverse Fast Fourier Transform (IFFT), to show the propagation of the spurious, free, long waves. Further, the variations in energy for the lower, higher and primary frequency ranges are reported for different wave paddle displacements. The analysis revealed that for the broadband spectrum the differences are more pronounced when using linear paddle displacements. We have also noticed a shift in focusing/breaking location and time (i.e. premature) due to the increase in crest height using linear displacements. The experiment data used in this paper has been provided as a supplementary, which can be used to validate the numerical models.
AB - In this paper, the evolution of focused waves using different paddle displacements (piston type) under laboratory conditions is presented. It is well known that in intermediate water depths, linear paddle displacements will generate spurious, free, sub and super harmonics. Thus, a second order correction to suppress these spurious free sub and super harmonics was used to generate the focused waves. The focused waves were generated in the laboratory using a linear superimposition principle, in which the wave paddle displacement is derived based on the sum of a number of sinusoidal components at discrete frequencies, whose phases are accordingly set to focus at a particular location. For this method of generation, the second order wave maker theory proposed by Schäffer [24] can be easily adopted and was used in the present study. Two different centre frequencies (fc=0.68Hz and 1.08Hz) with three different bandwidth ratios (δf/fc=0.5, 0.75 and 1.0) were tested in a constant water depth, to consider both narrow and broadband spectra. These test cases correspond to wave focusing packets propagating in intermediate and deep water regions. Further, for each wave packet, two different amplitudes were considered in order to analyze non-breaking and breaking cases. Thus, by systematically generating the wave packets using the linear and second order paddle displacements, the analysis was carried out for the spectral and temporal evolution of selected long waves. The temporal evolution of the selected harmonics was analyzed using the Inverse Fast Fourier Transform (IFFT), to show the propagation of the spurious, free, long waves. Further, the variations in energy for the lower, higher and primary frequency ranges are reported for different wave paddle displacements. The analysis revealed that for the broadband spectrum the differences are more pronounced when using linear paddle displacements. We have also noticed a shift in focusing/breaking location and time (i.e. premature) due to the increase in crest height using linear displacements. The experiment data used in this paper has been provided as a supplementary, which can be used to validate the numerical models.
KW - Focused waves
KW - Fully nonlinear potential flow theory
KW - Linear wavemaker theory
KW - Second order wavemaker theory
KW - Sub and super harmonics
KW - Fast Fourier transforms
KW - Wave packets
KW - Fully nonlinear potential flow
KW - Inverse fast Fourier transforms
KW - Laboratory conditions
KW - Second-order correction
KW - Sinusoidal components
KW - Super-harmonic
KW - Wavemaker theories
KW - Harmonic analysis
KW - Fourier transform
KW - harmonic analysis
KW - numerical model
KW - ocean wave
KW - wave modeling
UR - http://www.scopus.com/inward/record.url?scp=84945589577&partnerID=8YFLogxK
U2 - 10.1016/j.apor.2015.09.007
DO - 10.1016/j.apor.2015.09.007
M3 - Article
AN - SCOPUS:84945589577
VL - 53
SP - 279
EP - 296
JO - Applied Ocean Research
JF - Applied Ocean Research
SN - 0141-1187
ER -