Abstract

Effects of significant wave height and seaward depth on the distribution of the wave-induced set-up, wave-driven currents and the statistical moments (kurtosis and skewness) of the horizontal velocities and surface elevations of irregular waves propagating over a fringing reef are investigated using a fully non-hydrostatic wave model. It is found that wave-induced set-up and wave-driven currents obviously increase with increasing significant wave height and seaward depth. Besides, as the seaward depth is relatively shallow, the local maximum skewness of horizontal fluid velocities and surface elevations are achieved nearly at the same location. However, the location of the maximum kurtosis of the horizontal fluid velocities is on the inshore side of the flat compared to that of the surface elevations. Additionally, as a seaward depth increases, variations of skewness and kurtosis of horizontal velocities are more significant compared to surface elevations, and the maximum kurtosis and skewness of the horizontal velocities located downstream compared to those of the surface elevations.

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

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.