Abstract
The development and application of a heterogenous level method for three-dimensional hydrodynamics and salinity modelling is described. In this model the number of levels in the vertical dimension is adjusted according to the bathymetry at each horizontal node. The generalized wave continuity equation is solved first for the free surface elevation, then the horizontal velocities are obtained by solving the horizontal momentum equations. Next the vertical velocity is solved with the three-dimensional primitive equation. Finally the transport equation is solved for the salinity. Two examples are presented for the effectiveness of this model.
Sign-in/Register to access full text options 
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.
