The singularities that arise in polar and spherical coordinates have in the past caused significant difficulties in obtaining accurate solutions to convection–diffusion-type problems in many fields (astrophysics, geophysics, meteorology, etc.). Viewing pseudospectral methods as a limiting case of finite difference methods (rather than as based on expansions in terms of orthogonal functions) leads naturally to very simple, yet highly effective, fast Fourier transform (FFT)-based pseudospectral methods in such geometries.
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Bengt Fornberg (1995) studied this question.
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