Abstract
As discussed in the preceding chapter, there are two conceptually different ways to represent continuous functions on digital computers: as a finite set of gridpoint values or as a finite set of series-expansion functions. The grid-point approach is used in conjunction with finite-difference methods, which were widely implemented on digital computers somewhat earlier than the series-expansion techniques. In addition, the theory for these methods is somewhat simpler than that for series-expansion methods. We will parallel this historical development by studying finite-difference methods in this chapter and deferring the treatment of series expansion methods to Chapter 4. Moreover, it is useful to understand finitedifference methods before investigating series-expansion techniques because even when series expansions are used to represent the spatial dependence of some atmospheric quantity, the time dependence is almost always discretized and treated with finite differences.
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© 1999 Springer Science+Business Media New York
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Durran, D.R. (1999). Basic Finite-Difference Methods. In: Numerical Methods for Wave Equations in Geophysical Fluid Dynamics. Texts in Applied Mathematics, vol 32. Springer, New York, NY. https://doi.org/10.1007/978-1-4757-3081-4_2
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DOI: https://doi.org/10.1007/978-1-4757-3081-4_2
Publisher Name: Springer, New York, NY
Print ISBN: 978-1-4419-3121-4
Online ISBN: 978-1-4757-3081-4
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