Abstract
Under the assumptions of long wavelength, small amplitude, and propagation in one direction, it is well known that the water wave equations in the lowest order of approximation with slow variation in time and space can be reduced to the Korteweg–de Vries (KdV) equation. Linear inhomogeneous equations with their coefficients, as well as the inhomogeneous terms depending on the solutions of the lower-order equations, have been obtained in the next order and the third order of approximation. An accurate numerical method is used to integrate these equations for an overtaking interaction between two solitary waves. It is found, up to the second order of approximation, that the collision is elastic, i.e., the solitary waves regain their original form without giving rise to any secondary wave. The results of second-order solution are in good agreement with the analytic solution of Sachs [SIAM J. Math. Anal. 15, 468 (1984)]. However, the numerical computation on the third-order equation shows a secondary wave train trailing behind the smaller wave after the collision.
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.