Abstract
In the surface wind drift layer with constant momentum flux, two sets of the consistent surface elevation expressions with breaking and occurrence conditions for breaking are deduced from the first integrals of the energy and vortex variations and the kinetic and mathematic breaking criterions, then the expression of the surface elevation with wave breaking is established by using the Heaviside function. On the basis of the form of the sea surface elevation with wave breaking and the understanding of small slope sea waves, a triple composite function of real sea waves is presented including the functions for the breaking, weak-nonlinear and basic waves. The expression of the triple composite function and the normal distribution of basic waves are the expected theoretical model for surface elevation statistics.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.