Year-end Sale % OFF 
Abstract
The present paper describes a non-linear levels numerical model. The model is written in the semi-staggered grid with the forward-backwards numerical scheme. It is applied to reproduce the bora-driven circulation on the Adriatic shelf in order to relate to previous numerical studies where processes of advection of momentum and local generation of turbulence were not considered. Starting from a hydrostatic state the wind-stress produces a marked seiche and inertial oscillation in the numerical solutions. These oscillations are discussed with regard to the theory of the Adriatic seiche.
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.
