An explicit solution of the pseudo-hyperbolic initial boundary value problem with a mixed boundary condition has been constructed. The problem describes the propagation of non-stationary internal waves in a stratified and rotational fluid. The generation of waves is caused by small oscillations of double-sided plates beginning at time t = 0. Dynamic pressure is specified on one set of plates and this yields the first boundary condition. Normal velocities are specified on another set of plates and this leads to an analogue of the second boundary condition with time derivatives. The solution has been obtained by the method of non-classical time-dependent dynamic potentials. The uniqueness of the solution has been studied.
IntroductionThe equation of gravity-gyroscopic waves can be classified as a linear pseudohyperbolic partial differential equation. It governs non-stationary internal waves in an ideal stratified and rotational fluid without viscosity and compressibility where the Boussinesq approximation holds.Such a model of a fluid may be used for approximate simulation of a fluid in the Arctic sea, which is stratified due to gravity force and rotates with the Earth around the axis. The derivation of the equation of gravity-gyroscopic waves (1.1) is given in the point 1 of the appendix for the convenience of readers. One can note that in some papers gravity-gyroscopic waves are called gravity-inertial waves.In [6,8,11,12,16,29] the exact solutions of non-stationary boundary value problems on small oscillations of one plate in an unbounded stratified and rotational fluid have been obtained. In doing so, the pressure or the normal velocities were specified on both sides of the plate. This led to a first or second boundary value problem.The problem on non-stationary internal waves in the two-layer stratified fluid, excited by small vibrations of a plate, placed at the boundary of separation between the layers, has been studied in [lo].In [9,23] the initial boundary value problems on small oscillations of plates in a bounded layer of a stratified fluid has been considered.