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2021 | OriginalPaper | Chapter

2. Derivation of the Shallow Water Equations

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Abstract

This chapter presents a derivation of the shallow water equations, which describe flows where horizontal length-scales are much larger than the vertical. This occurs when hydrodynamic processes are small in comparison to gravity effects, and is therefore appropriate for tidal flows in channels where the tidal wavelength \(\lambda _w\) is greater than the channel depth h, such that \(\lambda _w / h \ll 2 \pi \).

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Metadata
Title
Derivation of the Shallow Water Equations
Author
Monika Johanna Kreitmair
Copyright Year
2021
DOI
https://doi.org/10.1007/978-3-030-57658-5_2