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Full instability of boundary layers with the Navier boundary condition

Lorenzo Quarisa, José L. Rodrigo

Abstract

We consider the problem of the stability of the Navier-Stokes equations in $\mathbb{T}\times \mathbb{R}_+$ near shear flows which are linearly unstable for the Euler equation. In \cite{greniernguyen}, the authors prove an $L^{\infty}$ instability result for the no-slip boundary condition which also denies the validity of the Prandtl boundary layer expansion. In this paper, we generalise this result to a Navier slip boundary condition with viscosity dependent slip length: $\partial_y u =ν^{-γ}u$ at $y=0$, where $γ>1/2$. This range includes the physical slip rate $γ=1$.

Full instability of boundary layers with the Navier boundary condition

Abstract

We consider the problem of the stability of the Navier-Stokes equations in near shear flows which are linearly unstable for the Euler equation. In \cite{greniernguyen}, the authors prove an instability result for the no-slip boundary condition which also denies the validity of the Prandtl boundary layer expansion. In this paper, we generalise this result to a Navier slip boundary condition with viscosity dependent slip length: at , where . This range includes the physical slip rate .
Paper Structure (12 sections, 13 theorems, 175 equations, 2 figures)

This paper contains 12 sections, 13 theorems, 175 equations, 2 figures.

Key Result

Theorem 1.1

Let $\gamma>1/2$. For $\nu >0$, let $\mathbf{U}^{\nu}=(U^{\nu},0)\in C^{\infty}(\mathbb{R}_+)$ be a family of shear flows constructed in eq:shflows and with $U_0$ linearly unstable for Euler and satisfying eq:uscond. Then for any $s\geq 0,N_0\in \mathbb{Z}_{\geq 1}$ there exists a family of solution

Figures (2)

  • Figure 1: Case of $U_0(y)=ye^{-y^2}$.
  • Figure 2: Case of $U_0(y)=e^{-1/y}$: $L^2$ norm of $\partial_y^{10} w^{\nu}(t,\cdot)$.

Theorems & Definitions (32)

  • Theorem 1.1
  • Proposition 2.1
  • Remark 2.2
  • Definition 2.3
  • Proposition 2.4
  • Proposition 2.5
  • Proposition 2.6
  • Remark 2.7
  • Definition 2.8
  • Definition 3.1
  • ...and 22 more