Optimal and near-optimal advection-diffusion finite-difference schemes. Part 2: Unsteadiness and non-uniform grid

نویسنده

  • B y Ronald Smith
چکیده

∂tc+ λ c+ u ∂xc− κ ∂ xc = q + ∂xf + ∂ xg . At the grid points the extremely high order of approximation for the numerical solutions is such that if loss of accuracy is to be avoided then interpolation must use values extending beyond the local 3 by 2 computational module. Illustrative examples show that reasonable accuracy is possible with extremely long time steps on sparse non-uniform, moving grids.

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تاریخ انتشار 1999