Estimation of extreme wave height and sea state

Abstract

BASIC CONCEPT OF EXTREME VALUES This section presents the theoretical background for predicting extreme values (extreme wave height, extreme sea state, etc.) which provide invaluable information for the design and operation of marine systems. The extreme value is defined as the largest value of a random variable expected to occur in a specified number of observations. Note that the extreme value is defined as a function of the number of samples. In the naval and ocean engineering area, however, it is highly desirable to estimate the largest wave height expected to occur in one hour, or the severest sea state expected to be encountered in 50 years, for example. This information can be obtained by estimating the number of waves (or sea states) per unit time, and thereby the number of samples necessary for evaluating the extreme value is converted to time. The concept supporting the estimation of extreme values is order statistics which is outlined in the following. Let us consider a sample set consisting of wave heights taken in the sequence of observations ( x 1 , x 2 , …, x n ). Each element of the random sample x i is assumed to be statistically independent having the same probability density function f(x) . In the case of wave height observations, each x i is considered to obey the Rayleigh probability law.