Book contents
- Frontmatter
- Contents
- Preface
- 1 Description of random seas
- 2 Spectral analysis
- 3 Wave amplitude and height
- 4 Wave height and associated period
- 5 Sea severity
- 6 Estimation of extreme wave height and sea state
- 7 Directional characteristics of random seas
- 8 Special wave events
- 9 Non-Gaussian waves (waves in finite water depth)
- Appendix A Fundamentals of probability theory
- Appendix B Fundamentals of stochastic process theory
- Appendix C Fourier transform and Hilbert transform
- References
- Index
2 - Spectral analysis
Published online by Cambridge University Press: 15 October 2009
- Frontmatter
- Contents
- Preface
- 1 Description of random seas
- 2 Spectral analysis
- 3 Wave amplitude and height
- 4 Wave height and associated period
- 5 Sea severity
- 6 Estimation of extreme wave height and sea state
- 7 Directional characteristics of random seas
- 8 Special wave events
- 9 Non-Gaussian waves (waves in finite water depth)
- Appendix A Fundamentals of probability theory
- Appendix B Fundamentals of stochastic process theory
- Appendix C Fourier transform and Hilbert transform
- References
- Index
Summary
SPECTRAL ANALYSIS OF RANDOM WAVES
Fundamentals of stochastic processes
Throughout this chapter as well as others, we will evaluate various characteristics of wind-generated waves based on the stochastic process concept. The fundamentals of the stochastic process concept are outlined here.
First, the stochastic process (or random process), x(t), is defined as a family of random variables. In the strict sense, x(t) is a function of two arguments, time and sample space. To elaborate on this definition of a stochastic process, let us consider a set of n wave recorders (1x, 2x, 3x, …, nx) dispersed in a certain area in the ocean as illustrated in Figure 2.1 (a). Let us consider a set of time histories of wave records {1x(t), 2x(t), …, nx(t)} as illustrated in Figure 2.1(b). It is recognized that at any time tj, x(tj) is a random variable, and a set {1x(tj), 2x(tj), …, nx(tj)} can be considered as a random sample of size n. This simultaneous collection of wave data observed at a specified time is called an ensemble. If we construct a histogram from a set of ensembles of wave records, it may be normally distributed with zero mean and a certain variance as shown in Figure 2.1(c).
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- Ocean WavesThe Stochastic Approach, pp. 13 - 57Publisher: Cambridge University PressPrint publication year: 1998
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