Abstract
The inverse problem of the mathematical theory of tides is considered, i.e., a problem of functions defining boundary values on liquid parts of the boundary. A closure equation is based on the observation data on the function of the sea level (free surface elevation) on a part of the boundary. The existence and uniqueness of the solution is investigated. We formulate an iteration algorithm for solving the problem studied.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have