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Modélisation, analyse mathématique et simulations numériques de ...

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tel-00656013, version 1 - 3 Jan 2012<br />

Ö×ÙÖ<br />

54 A dynamic multilayer shallow water mo<strong>de</strong>l<br />

z<br />

z4+1/2 = η(t, x)<br />

z3+1/2(t, x) u4(t, x)<br />

z2+1/2(t, x)<br />

z1+1/2(t, x)<br />

z1/2 = zb(x)<br />

0<br />

u3(t, x)<br />

u2(t, x)<br />

u1(t, x)<br />

H(t, x)<br />

h4(t, x)<br />

h3(t, x)<br />

h2(t, x)<br />

ÓØØÓÑ<br />

h1(t, x)<br />

Figure 2.2: Classical multilayer approach.<br />

equations by the heights, we rewrite the system on the unknown (U,h) = (u1 ... uN,h) T<br />

as follows.<br />

⎧<br />

⎨<br />

where the source terms are <strong>de</strong>scribed below.<br />

⎧<br />

⎪⎨<br />

⎪⎩<br />

⎩<br />

∂tU−µ∂xxU = S,<br />

∂th+∂x(huN) = F ,<br />

S = Sb +Sl +Snl,<br />

N−1 <br />

F = wN−1/2 = −<br />

where Sb refers to the bottom source term<br />

i=1<br />

Sb = −g∂xzb(1,...,1) T ,<br />

∂x(hiui) ,<br />

x<br />

(2.3.1)

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