Joint Probability Distribution of Significant Wave Height and Peak Wave Period using Gaussian Copula Method

Title
Joint Probability Distribution of Significant Wave Height and Peak Wave Period using Gaussian Copula Method
Author(s)
Lee, Uk Jae; Cho, Hong Yeon; Lee, Byeong Wook; Ko, Dong Hui
KIOST Author(s)
Lee, Uk Jae(이욱재)Cho, Hong Yeon(조홍연)Ko, Dong Hui(고동휘)
Alternative Author(s)
이욱재; 조홍연; 고동휘
Publication Year
2023-02-22
Abstract
In this study, the joint probability distribution was calculated using the significant wave height and peak wave
period observed at the HeMOSU oceanographic and meteorological observation tower located on the west coast
of Korea. Representative wave parameters such as significant wave height and peak wave period show a high
correlation between the two variables, and it is required in various fields to express the contour-line (CL) for the
target exceedance probability under the condition of considering these correlation characteristics. In the case of
waves, the design frequency level, the return period of 5, 10, 20, 30, 50, and 100 years, the frequency is
calculated according to the data used to calculate the CL. To calculate this CL, it is necessary to 1) calculate the
optimal probability density distribution for each wave variable, and 2) calculate the joint probability distribution
using methods such as copula and I-FORM. In this study, a Gaussian copula among the copula method was
used.
To estimate the fitted probability density function of each wave variable, the most widely used Maximum
Likelihood Estimation was used. The optimal probability density function of each wave variable was estimated
by applying the ‘Normal’, ‘Lognormal’, ‘Gamma’, ‘Weibull-3P’ distribution for the significant wave height and
the ‘Normal’, ‘Lognormal’, ‘Gamma’ distribution for the peak period. Meanwhile, the KS test (KolmogorovSmirnov Test) and KL Divergence (Kullback-Leibler Divergence) were used to perform the distribution fit test.
The correlation coefficient between the significant wave height and peak period observed in HeMOSU was
0.77, the significant wave height was Log-Normal distribution and the peak period was Normal distribution.
It was found that this method can be applied (excluding the introduction of physical boundary conditions) even
when information on correlation is absent along with data sets such as wind speed and wave height where high
correlation is expected.
URI
https://sciwatch.kiost.ac.kr/handle/2020.kiost/43985
Bibliographic Citation
International Conference on Aquatic Science & Technology (i-CoAST) 2023, pp.155, 2023
Publisher
international Conference on Aquatic Science & Technology (i-Coast)
Type
Conference
Language
English
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