Abstract
In this chapter, we discuss the fundamentals of how to cast a PDE into finite difference form. More specifically, the reader will learn how to discretize the diffusion equation, and learn why some discretizations work and some do not. This will be the opportunity to introduce concepts such as numerical stability, convergence, and consistency. It will be explained how to check whether a discretization is stable and consistent, and the reader will learn about explicit and implicit schemes, the rudiments of elliptic solvers, and the concept of numerical dissipation or artificial damping inherent in our discretizations.
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- 1.
Only wavenumbers for which \(\lambda =0\) have a growth factor \(|G|=1\). However, all wavenumbers are present in any solution. Hence, the growth factor is in general less than unity.
- 2.
It is not important how fast each of them go to zero.
- 3.
For a given grid size, \(2\Delta x\) is the so-called Nüquist wavelength. Thus, wavelengths smaller than \(2\Delta x\) remain unresolved.
- 4.
- 5.
This is also commonly referred to as the mesh or grid size.
- 6.
These are oscillations in which the frequency equals the inertial frequency f.
References
Abramowitz M, Stegun I (1965) Handbook of mathematical functions, 9th edn. Dover Publications, Inc, New York
Adamec D, O’Brien JJ (1978) The seasonal upwelling in the Gulf of Guinea due to remote forcing. J Phys Oceanogr 8:1050–1060
Gill AE (1982) Atmosphere–ocean dynamics. International geophysical series, vol 30. Academic, New York
Griffies SM (2004) Fundamentals of ocean climate models. Princeton University Press, Princeton. ISBN 0-691-11892-2
Lax PD, Richtmyer RD (1956) Survey of the stability of linear finite difference equations. Commun Pure Appl Math 9:267–293, MR 79,204. https://doi.org/10.1002/cpa.3160090206
Phillips OM (1966) The dynamics of the upper ocean. Cambridge University Press, New York, 269 pp
Yoshida K (1959) A theory of the Cromwell current and of equatorial upwelling. J Oceanogr Soc Jpn 15:154–170
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Røed, L.P. (2019). Diffusion Problem. In: Atmospheres and Oceans on Computers. Springer Textbooks in Earth Sciences, Geography and Environment. Springer, Cham. https://doi.org/10.1007/978-3-319-93864-6_4
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DOI: https://doi.org/10.1007/978-3-319-93864-6_4
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