Distribution of the nonlinear random ocean wave period
OriginalPaper|Updated:2023-05-16
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Distribution of the nonlinear random ocean wave period
Distribution of the nonlinear random ocean wave period
海洋湖沼学报(英文)2009年27卷第4期 页码:919-923
Affiliations:
1. Key Laboratory of Ocean Circulation and Waves Chinese Academy of Sciences
2. Institute of Oceanology Chinese Academy of Sciences
3. Graduate School of the Chinese Academy of Sciences
Author bio:
Funds:
Supported by the National Natural Science Foundation of China (No. 40476018) and the Knowledge Innovation Program of Chinese Academy of Sciences (KZCX2-YW201)
Distribution of the nonlinear random ocean wave period[J]. 海洋湖沼学报(英文), 2009,27(4):919-923.
Hou, Y., Li, M., Song, G. et al. Distribution of the nonlinear random ocean wave period., Chin. J. Ocean. Limnol. 27, 919–923 (2009). https://doi.org/10.1007/s00343-009-9089-z
Distribution of the nonlinear random ocean wave period[J]. 海洋湖沼学报(英文), 2009,27(4):919-923. DOI: 10.1007/s00343-009-9089-z.
Hou, Y., Li, M., Song, G. et al. Distribution of the nonlinear random ocean wave period., Chin. J. Ocean. Limnol. 27, 919–923 (2009). https://doi.org/10.1007/s00343-009-9089-zDOI:
Distribution of the nonlinear random ocean wave period
摘要
Abstract
Because of the intrinsic difficulty in determining distributions for wave periods
previous studies on wave period distribution models have not taken nonlinearity into account and have not performed well in terms of describing and statistically analyzing the probability density distribution of ocean waves. In this study
a statistical model of random waves is developed using Stokes wave theory of water wave dynamics. In addition
a new nonlinear probability distribution function for the wave period is presented with the parameters of spectral density width and nonlinear wave steepness
which is more reasonable as a physical mechanism. The magnitude of wave steepness determines the intensity of the nonlinear effect
while the spectral width only changes the energy distribution. The wave steepness is found to be an important parameter in terms of not only dynamics but also statistics. The value of wave steepness reflects the degree that the wave period distribution skews from the Cauchy distribution
and it also describes the variation in the distribution function
which resembles that of the wave surface elevation distribution and wave height distribution. We found that the distribution curves skew leftward and upward as the wave steepness increases. The wave period observations for the SZFII-1 buoy
made off the coast of Weihai (37°27.6′ N
122°15.1′ E)
China
are used to verify the new distribution. The coefficient of the correlation between the new distribution and the buoy data at different spectral widths (ν=0.3−0.5) is within the range of 0.968 6 to 0.991 7. In addition
the Longuet-Higgins (1975) and Sun (1988) distributions and the new distribution presented in this work are compared. The validations and comparisons indicate that the new nonlinear probability density distribution fits the buoy measurements better than the Longuet-Higgins and Sun distributions do. We believe that adoption of the new wave period distribution would improve traditional statistical wave theory.
关键词
Keywords
references
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