11.08.2013 Views

Untitled - Cdm.unimo.it

Untitled - Cdm.unimo.it

Untitled - Cdm.unimo.it

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

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

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!