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Untitled - Cdm.unimo.it

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An Example in Two Dimensions 291<br />

where ν > 0 is a given parameter associated w<strong>it</strong>h the kinematic viscos<strong>it</strong>y, and ∆ is<br />

the Laplace operator defined in (13.1.1). The nonlinear relations (13.4.1) and (13.4.2)<br />

are known as momentum equations, while (13.4.3) is the continu<strong>it</strong>y (or incompressibil-<br />

<strong>it</strong>y) equation. They express the conservation laws of the momentum and the mass<br />

respectively. We note the analogy between the momentum equations and the Burgers<br />

equation, presented in section 10.4 for the case of one space variable. The functions<br />

Vi, 1 ≤ i ≤ 2, require in<strong>it</strong>ial and boundary cond<strong>it</strong>ions. For example, by imposing<br />

Vi ≡ 0 on ∂Ω×]0,T], 1 ≤ i ≤ 2, we are specifying a no-slip cond<strong>it</strong>ion at the bound-<br />

ary. Instead, no in<strong>it</strong>ial or boundary cond<strong>it</strong>ions are needed for the pressure, which is<br />

determined up to an add<strong>it</strong>ive constant.<br />

For a theoretical study of the equations (13.4.1)-(13.4.3), the reader is inv<strong>it</strong>ed to<br />

consult the books of ladyzhenskaya(1969), temam(1985), kreiss and lorenz(1989)<br />

and the numerous references contained therein. On the subjects of numerical approxi-<br />

mation by fin<strong>it</strong>e-differences or fin<strong>it</strong>e element methods the bibliography is very rich, and<br />

a comprehensive list of references cannot be included here. We would like to remark<br />

that the numerical investigation of the equations relevant to the physics of fluids has<br />

also been a primary source of algor<strong>it</strong>hms and solution techniques in the field of spectral<br />

methods. Due to the abundance of results, we are unable to mention all the contribu-<br />

tors. A distinguished referring point is the book of canuto, hussaini, quarteroni<br />

and zang(1988), which is specifically addressed to computations in fluid dynamics. The<br />

reader will find there material for further extensions.<br />

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