Abstract
In this article, we consider a non-autonomous three-dimensional primitive equations of the ocean with a singularly oscillating external force g ε = g 0(t) + ε−ρ g 1(t/ε) depending on a small parameter ε > 0 and ρ ∈ [0, 1) together with the averaged system with the external force g 0(t), formally corresponding to the case ε = 0. Under suitable assumptions on the external force, we prove as in [V.V. Chepyzhov, V. Pata, and M.M.I. Vishik, Averaging of 2D Navier–Stokes equations with singularly oscillating forces, Nonlinearity, 22 (2009), pp. 351–370] the boundness of the uniform global attractor 𝒜ε as well as the convergence of the attractors 𝒜ε of the singular systems to the attractor 𝒜0 of the averaged system as ε → 0+. When the external force is small enough and the viscosity is large enough, the convergence rate is controlled by Kε(1−ρ). Let us note that the main difference between this work and that of Chepyzhov et al. (2009) is that the non-linearity involved in the three-dimensional primitive equation is stronger than the one in the two-dimensional Navier–Stokes equations considered in Chepyzhov et al. (2009), which makes the analysis of the problem studied in this article more involved.
Acknowledgements
The author would like to thank the anonymous referees whose comments help to improve the contain of this article.