It remains to calculate the sum of the preceding relations from $\alpha = 1, \dots, N$ and to integrate the obtained relation in $\xi, \gamma$ over $\mathbb{R}^2$ that completes the proof. ■
Remark 4.3 If we introduce a $(2N+1) \times N$ matrix $K(\xi, \gamma)$ defined by
K1,j=1,Ki+1,j=ξδi,j,Ki+N+1,j+N=γδi,j,
for $i, j = 1, \dots, N$ with $\delta_{i,j}$ the Kronecker symbol. Then, using Prop. 4.1, we can write
The numerical scheme for the model (49) proposed in this section extends the results presented by some of the authors in [5, 9, 8, 4]. Compared to these previous results, it has the following advantages
it gives a 3d approximation of the Navier-Stokes system whereas 2d situations $(x, y)$ and $(x, z)$ where considered in [5, 9, 8],
the implicit treatment of the vertical exchanges terms gives a bounded CFL condition even when the water depth vanishes,