“…, where λ > 0 is the dissipative parameter, κ = ±1, and the real dimensionless constant b ∈ R is a parameter that provides the competition, or balance, in fluid convection between nonlinear steepening and amplification due to stretching; it is also the number of covariant dimensions associated with the momentum density m. The unknown u(t, x) stands for the horizontal velocity of the fluid, and σ (t, x) is related to the free surface elevation from equilibrium with the boundary assumption, u → 0 and σ → 1 as |x| → ∞. The system (1.1) without the dissipative terms has been studied by several authors, such as [6,7,15,26,27]. Note that the system (1.1) can be reduced to the damping perturbation of some well-known Camassa-Holm type equations.…”