Abstract
This note presents a numerical method for calculating the far field part of the Green's function for a source in steady translation below the surface of fluid of finite depth. The principal steps of the numerical scheme are outlined, with emphasis on those aspects which are needed for a computer implementation of the scheme. Numerical results are given to show the behavior of the function in various parts of the computation domain, the computer requirements of the method, and its expected accuracy.
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 callDisclaimer: 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.
