“…be the velocity vector, p(x, y, z, t) be the pressure and ρ(x, y, z, t) be the density in the Cartesian coordinates (x, y, z). The starting model describing the large-scale geophysical motions for baroclinic jets that release potential energy in the atmosphere are given by nonlinear model for internal waves under the Boussinesq approximation ( [20], [21], [22], [23]):…”