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and

κα={κif α=10if α1,να+1/2={0if α=0,Nνif α=1,,N1,Wα={Wif α=N0if αN(36) \kappa_{\alpha} = \begin{cases} \kappa & \text{if } \alpha = 1 \\ 0 & \text{if } \alpha \neq 1 \end{cases}, \quad \nu_{\alpha+1/2} = \begin{cases} 0 & \text{if } \alpha = 0, N \\ \nu & \text{if } \alpha = 1, \dots, N-1 \end{cases}, \quad W_{\alpha} = \begin{cases} W & \text{if } \alpha = N \\ 0 & \text{if } \alpha \neq N \end{cases} \tag{36}

The vertical velocities {$w_\alpha$}$_{\alpha=1}^N$ are defined by (27). For smooth solutions, the system (30)-(31) admits the energy balance

tα=1NEα+x,yα=1Nuα(Eα+g2hαhhαΣα)=α=1N1uα+1uα22Gα+1/2α=1N1hα+1+hα2νΣα+1/22α=1N12νuα+1uα2hα+1+hακu12+WuNts,(37) \frac{\partial}{\partial t} \sum_{\alpha=1}^{N} E_{\alpha} + \nabla_{x,y} \cdot \sum_{\alpha=1}^{N} \mathbf{u}_{\alpha} \left( E_{\alpha} + \frac{g}{2} h_{\alpha} h - h_{\alpha} \boldsymbol{\Sigma}_{\alpha} \right) = - \sum_{\alpha=1}^{N-1} \frac{|\mathbf{u}_{\alpha+1} - \mathbf{u}_{\alpha}|^2}{2} |G_{\alpha+1/2}| \\ - \sum_{\alpha=1}^{N-1} \frac{h_{\alpha+1} + h_{\alpha}}{2\nu} \boldsymbol{\Sigma}_{\alpha+1/2}^2 - \sum_{\alpha=1}^{N-1} 2\nu \frac{|\mathbf{u}_{\alpha+1} - \mathbf{u}_{\alpha}|^2}{h_{\alpha+1} + h_{\alpha}} - \kappa |\mathbf{u}_1|^2 + W \mathbf{u}_N \cdot \mathbf{t}_s, \quad (37)

with $E_\alpha$ defined by (23) and $\Sigma_{\alpha+1/2}^2 = \sum_{i,j} \Sigma_{i,j,\alpha+1/2}^2$. Relation (37) is consistent with a layer-averaged discretization of the equation (10).

Notice that in (37), we use the notation

uαΣα=(uαΣxx,α+vαΣyx,αuαΣxy,α+vαΣyy,α). \mathbf{u}_{\alpha}\boldsymbol{\Sigma}_{\alpha} = \begin{pmatrix} u_{\alpha}\boldsymbol{\Sigma}_{xx,\alpha} + v_{\alpha}\boldsymbol{\Sigma}_{yx,\alpha} \\ u_{\alpha}\boldsymbol{\Sigma}_{xy,\alpha} + v_{\alpha}\boldsymbol{\Sigma}_{yy,\alpha} \end{pmatrix}.

Proof of prop. 3.4 The proof is given in appendix A. ■

Remark 3.2 Notice that in the definition (35), since we consider viscous terms we use a centered approximation.

3.2.2 Simplified rheology

The viscous terms in the layer-averaged Navier-Stokes system are difficult to discretize especially when a discrete version of the energy balance has to be preserved. Hence, we propose a modified version of the model given in prop. 3.4.

Proposition 3.5 The layer-averaged Navier-Stokes can be written under the form

α=1Nhαt+α=1Nx,y.(hαuα)=0,(38) \sum_{\alpha=1}^{N} \frac{\partial h_{\alpha}}{\partial t} + \sum_{\alpha=1}^{N} \nabla_{x,y}.(h_{\alpha} \mathbf{u}_{\alpha}) = 0, \tag{38}

hαt+x,y(hαuαuα)+x,y(g2hα)=ghαx,yzb+uα+1/2Gα+1/2uα1/2Gα1/2+x,y(hαΣα0)Tα+Λα+1/2(uα+1uα)Λα1/2(uαuα1)καuα+Wαts, \begin{equation} \begin{split} & \frac{\partial h_\alpha}{\partial t} + \nabla_{x,y} (h_\alpha \mathbf{u}_\alpha \otimes \mathbf{u}_\alpha) + \nabla_{x,y} (\frac{g}{2} h_\alpha) \\ & \qquad = -gh_\alpha \nabla_{x,y} z_b \\ & \qquad + \mathbf{u}_{\alpha+1/2} G_{\alpha+1/2} - \mathbf{u}_{\alpha-1/2} G_{\alpha-1/2} + \nabla_{x,y} (h_\alpha \boldsymbol{\Sigma}_\alpha^0) - \mathbf{T}_\alpha \\ & \qquad + \Lambda_{\alpha+1/2} (\mathbf{u}_{\alpha+1} - \mathbf{u}_\alpha) - \Lambda_{\alpha-1/2} (\mathbf{u}_\alpha - \mathbf{u}_{\alpha-1}) - \kappa_\alpha \mathbf{u}_\alpha + W_\alpha \mathbf{t}_s, \end{split} \tag{39} \end{equation}

and

Σxx,α+1/20=να+1/2hα+1+hα(hαuαx+hα+1uα+1x),(40) \Sigma_{xx,\alpha+1/2}^0 = \frac{\nu_{\alpha+1/2}}{h_{\alpha+1} + h_{\alpha}} \left(h_{\alpha} \frac{\partial u_{\alpha}}{\partial x} + h_{\alpha+1} \frac{\partial u_{\alpha+1}}{\partial x}\right), \quad (40)

Σxy,α+1/20=να+1/2hα+1+hα(hαuαy+hα+1uα+1y),(41) \Sigma^0_{xy,\alpha+1/2} = \frac{\nu_{\alpha+1/2}}{h_{\alpha+1} + h_{\alpha}} \left( h_{\alpha} \frac{\partial u_{\alpha}}{\partial y} + h_{\alpha+1} \frac{\partial u_{\alpha+1}}{\partial y} \right), \quad (41)

and similar definitions for $\Sigma^0_{yx,\alpha+1/2}$, $\Sigma^0_{yy,\alpha+1/2}$. We also denote

Tx,α+1/2=2να+1/2hα+1+hαx,yzα+1/2(hαx,yuα+hα+1x,yuα+1),(42) T_{x,\alpha+1/2} = \frac{2\nu_{\alpha+1/2}}{h_{\alpha+1} + h_{\alpha}} \nabla_{x,y} z_{\alpha+1/2} (h_{\alpha} \nabla_{x,y} u_{\alpha} + h_{\alpha+1} \nabla_{x,y} u_{\alpha+1}), \quad (42)