Abstract
A two-parameter dynamic model on the shelf zone of the sea based on the K-theory is considered. The equations of balance and kinetic turbulent energy dissipation are involved for closing the set of motion equations. It is assumed that the sea is steady, horizontally homogeneous, and indifferently stratified. This paper is notable for the simultaneous description of the effect produced by the atmosphere and bottom on the shelf zone vertical structure. Model computations of the integral characteristics and profiles of turbulent parameters are given.
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.
