Partial and full hyper-viscosity for Navier-Stokes and primitive equations

Abstract

The $3$-D primitive equations and incompressible Navier-Stokes equations with full hyper-viscosity and only horizontal hyper-viscosity are considered on the torus, i.e., the diffusion term $-Δ$ is replaced by $-Δ+ \varepsilon(-Δ)^{l}$ or by $-Δ+ \varepsilon(-Δ_H)^{l}$, respectively, where $Δ_H = \partial_x^2+\partial_y^2 $, $Δ= Δ_H + \partial_z^2$, $\varepsilon> 0$, $l>1$. Hyper-viscosity is applied in many numerical schemes, and in particular horizontal hyper-viscosity appears in meteorological models. A classical result by Lions states that for the Navier-Stokes equations uniqueness of global weak solutions for initial data in $L^2$ holds if $-Δ$ is replaced by $(-Δ)^{5/4}$. Here, for the primitive equations the corresponding result is proven for $(-Δ)^{8/5}$. For the case of horizontal hyper-viscosity $l=2$ is sufficient in both cases. Strong convergence for $\varepsilon\to 0$ of hyper-viscous solutions to a weak solution of the Navier-Stokes and primitive equations, respectively, is proven as well. The approach presented here is based on the construction of strong solutions via an evolution equation approach for initial data in $L^2$ and weak-strong uniqueness.