Bulatov V.V., Vladimirov Yu.V.
The paper is devoted to the solution of the fundamental problem of mathematical modeling of ocean dynamics, related to the theoretical study of the propagation of disturbances, and evolution of far fields of internal gravity waves in inhomogeneous and non-stationary stratified media. The problem is solved using the suggested modified spatiotemporal ray-tracing method. The numerical results based on the suggested asymptotic formulas and real parameters of the ocean are presented.
