Finite-difference approximations for the first derivative, valid halfway between equidistant gridpoints, are in general much more accurate than the corresponding approximations, which are valid at gridpoints. The pseudospectral (Fourier) method can be viewed as the limit of finite-difference approximations when the order of accuracy tends to infinity. A fundamentally different (and more accurate) pseudospectral method is obtained from the 'halfway' approximations. This study derives these and related methods and discusses their accuracies.
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Univ Southern Calif, Southern Calif Earthquake Ctr, Los Angeles, CA 90007 USAUniv Southern Calif, Southern Calif Earthquake Ctr, Los Angeles, CA 90007 USA
O'Reilly, Ossian
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Yeh, Te-Yang
Olsen, Kim B.
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San Diego State Univ, Dept Geol Sci, San Diego, CA 92182 USAUniv Southern Calif, Southern Calif Earthquake Ctr, Los Angeles, CA 90007 USA
Olsen, Kim B.
Hu, Zhifeng
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San Diego State Univ, Dept Geol Sci, San Diego, CA 92182 USAUniv Southern Calif, Southern Calif Earthquake Ctr, Los Angeles, CA 90007 USA
Hu, Zhifeng
Breuer, Alex
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Friedrich Schiller Univ Jena, Fac Math & Comp Sci, Inst Comp Sci, Jena, GermanyUniv Southern Calif, Southern Calif Earthquake Ctr, Los Angeles, CA 90007 USA
Breuer, Alex
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Roten, Daniel
Goulet, Christine A.
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Univ Southern Calif, Southern Calif Earthquake Ctr, Los Angeles, CA 90007 USAUniv Southern Calif, Southern Calif Earthquake Ctr, Los Angeles, CA 90007 USA