Applied and Interdisciplinary Mathematics Seminar Friday, 29 September, 3:10-4:00pm, 1084 East Hall |
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Abstract |
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In this lecture I will first show there are essential differences between discretizing advection and diffusion equations: what works for one does not work for the other, and vice versa. This means that, when formulating a DG method for diffusion, one can not blindly copy what's done for the advection equation.
I will show, however, there is absolutely no conflict between the DG approach and the diffusion equation. In order to make it work two insights are needed:
(1) the realization that there are multiple representations of the
numerical solution which all are equivalent in the weak sense,
and that one may have to switch between these for the sake of
getting useful schemes;
(2) for a second-order PDE integration by parts must be done TWICE
in order to obtain the DG equations - which is not standard DG
practice.
Next, I will present the Recovery method, developed from the above starting points. Specifically, a smooth locally recovered solution is used that in the weak sense is indistinguishable from the discontinuous discrete solution. The recovery principle creates schemes that are not included in the family of traditional DG diffusion schemes, and are potentially more accurate. A way is presented to extend the family so that some recovery-based schemes are included.
An eigenvalue/eigenvector analysis suggests that the order of accuracy of the recovery schemes may be as high as 2**(p+2}, i.e., exponential. This conclusion is supported by numerical tests.
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