Untitled - Cdm.unimo.it
Untitled - Cdm.unimo.it
Untitled - Cdm.unimo.it
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234 Polynomial Approximation of Differential Equations<br />
Once the stabil<strong>it</strong>y of the scheme is achieved, error estimates are obtained by applying<br />
the same proof to the error pn − Un, where Un ∈ Pn, n ≥ 1 , is a su<strong>it</strong>able projection<br />
of U. The same argument was used in section 10.2 for the heat equation (see also<br />
canuto, hussaini, quarteroni and zang(1988), chapter 10). Other spectral type<br />
approximations and theoretical results relative to equation (10.3.1) are considered in<br />
gottlieb and orszag(1977), section 8, gottlieb(1981), canuto and quarteroni<br />
(1982b), mercier(1982), mercier(1989), tal-ezer(1986b), dubiner(1987).<br />
Similar results are available for the equation<br />
(10.3.20)<br />
∂U ∂U<br />
(x,t) = ζ (x,t), ∀x ∈ [−1,1[, ∀t ∈]0,T],<br />
∂t ∂x<br />
when the boundary cond<strong>it</strong>ion is imposed at the point x = 1.<br />
The reader should pay a l<strong>it</strong>tle more care to the theoretical analysis of partial differ-<br />
ential equations, before trying experiments on general problems, such as the following<br />
one:<br />
(10.3.21)<br />
∂U<br />
(x,t) = A(x,U(x,t))∂U (x,t), x ∈] − 1,1[, t ∈]0,T],<br />
∂t ∂x<br />
where A :] − 1,1[×R → R is given.<br />
An analysis for equations such as (10.3.21) is carried out in smoller(1983), rhee,<br />
aris and amundson(1986), kreiss and lorenz(1989). It is known that the solution<br />
of (10.3.21) maintains a constant value along the so-called characteristic curves. These<br />
are parallel straight-lines in the (x,t) plane w<strong>it</strong>h slope 1/ζ for equation (10.3.1), and<br />
slope −1/ζ for equation (10.3.20). In the former case, the solution U(x, ·), x ∈ [−1,1],<br />
shifts on the right-hand side during the time evolution. W<strong>it</strong>h terminology deriving from<br />
fluid physics, the point x = −1 is the inflow boundary, while x = 1 is the outflow<br />
boundary. The s<strong>it</strong>uation is reversed for equation (10.3.20). The characteristic curves<br />
are no longer straight-lines when A is not a constant. Even in the case of smooth in<strong>it</strong>ial<br />
cond<strong>it</strong>ions and smooth boundary data, the solution can loose regular<strong>it</strong>y and shocks can<br />
be generated when two or more characteristic curves intersect. The numerical analysis<br />
becomes a delicate issue in this s<strong>it</strong>uation, especially for spectral methods which are