“…for t > 0 and x ∈ R. In the above system, u(x, t) is a horizontal velocity, ρ(t, x) is related to the free surface elevation from equilibrium, the parameter A describes a linear underlying shear flow, σ is a real dimensionless constant, providing the competition or balance, in fluid convection between nonlinear steepening and amplification due to stretching, µ is a non-dimensional parameter, and Ω is a real number characterizing the constant rotational speed of the Earth [19]. As we all 2476 MEILING YANG, YONGSHENG LI AND ZHIJUN QIAO known, the Earth's rotation profoundly affects the dynamics of the atmosphere and of the ocean.…”