Adaptivity with moving grids
Adaptivity with moving grids
Adaptivity with moving grids
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102 C. J. Budd, W. Huang and R. D. Russell<br />
where the function v(y) is given by the Barenblatt–Pattle profile (Barenblatt<br />
1996). It is also well known that any positive initial data lead to a solution<br />
u(x, t), which converges towards to a self-similar solution in the sense that<br />
t 1/3 u(t 1/3 y, t) → v(y).<br />
Similarly, it is shown in Budd et al. (1999b) that if the monitor function<br />
is chosen to give a scale-invariant scheme (for example M = u), then this<br />
scheme admits a set of discrete self-similar solutions on a <strong>moving</strong> mesh<br />
which take the form<br />
U i (t) =(t + C) −1/3 V i , X i (t) =(t + C) 1/3 Y i .<br />
Note that the product<br />
W i ≡ U i X i = V i Y i<br />
is invariant in time. In Figure 5.1 we show the results of a computation presented<br />
in the computational domain, using a scale-invariant <strong>moving</strong> mesh<br />
method <strong>with</strong> M = u and a centred finite difference discretization. In this<br />
calculation the initial data at t = 0 were taken to be an irregular function,<br />
and results are plotted at times t =0andt = 10. We also show (dashed)<br />
two discrete self-similar solutions <strong>with</strong> values of C chosen so that they initially<br />
lie above and below the solution. Note that the solution calculated is<br />
sandwiched between these two functions. We also present the corresponding<br />
mesh X i (t) and the scaled mesh Y i (t) =X i (t)/t 1/3 . It is clear from<br />
these figures that the computed solution converges towards the discrete selfsimilar<br />
solutions (in correspondence <strong>with</strong> the continuous theory) and that<br />
the <strong>moving</strong> mesh tends towards the one for which Y i is constant in time so<br />
that X i (t) scales asymptotically as t 1/3 . Similar figures for solutions of the<br />
porous medium equation computed using a scale-invariant ALE method in<br />
two dimensions are given in Baines et al. (2006).<br />
5.2. Blow-up and related problems<br />
5.2.1. Parabolic blow-up<br />
As mentioned in Section 5.1, a significant success in the application of <strong>moving</strong><br />
mesh methods occurs in the study of parabolic partial differential equations<br />
(and also of systems of PDEs) which have solutions that blow up,<br />
so that the solution, or some derivative of it, becomes infinite in a finite<br />
time T . We now consider such problems in a little more detail. Blow-up<br />
in the solution often represents an important change in the properties of<br />
the model that the equation represents (such as the ignition of a heated gas<br />
mixture), and it is important that it is reproduced accurately in a numerical<br />
computation. A survey of many different types of blow-up problem is presented<br />
in Samarskii et al. (1973). Blow-up typically occurs on increasingly<br />
small time and length scales, and hence it is usually essential to use both