Low-order Boussinesq models based on coordinate series expansions
We derive weakly dispersive Boussinesq equations using a $\unicode[STIX]{x1D70E}$ coordinate for the vertical direction, employing a series expansion in powers of $\unicode[STIX]{x1D70E}$ . We restrict attention initially to the case of constant still-water depth $h$ in order to simplify subsequent...
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| Published in | Journal of fluid mechanics Vol. 896 |
|---|---|
| Main Author | |
| Format | Journal Article |
| Language | English |
| Published |
Cambridge
Cambridge University Press
10.08.2020
|
| Subjects | |
| Online Access | Get full text |
| ISSN | 0022-1120 1469-7645 |
| DOI | 10.1017/jfm.2020.376 |
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| Summary: | We derive weakly dispersive Boussinesq equations using a
$\unicode[STIX]{x1D70E}$
coordinate for the vertical direction, employing a series expansion in powers of
$\unicode[STIX]{x1D70E}$
. We restrict attention initially to the case of constant still-water depth
$h$
in order to simplify subsequent analysis, and consider equations based on expansions about the bottom elevation
$\unicode[STIX]{x1D70E}=0$
, and then about a reference elevation
$\unicode[STIX]{x1D70E}_{\unicode[STIX]{x1D6FC}}$
in order to improve linear dispersion properties. We use a perturbation analysis, suggested recently by Madsen & Fuhrman (
J. Fluid Mech.
, vol. 889, 2020, A38), to show that the resulting models are not subject to the trough instability studied there. A similar analysis is performed to develop a model for interfacial waves in a two-layer fluid, with comparable results. We argue, by extension, that a necessary condition for eliminating trough instabilities is that the model’s nonlinear dispersive terms should not contain still-water depth
$h$
and surface displacement
$\unicode[STIX]{x1D702}$
separately. |
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| Bibliography: | ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 14 |
| ISSN: | 0022-1120 1469-7645 |
| DOI: | 10.1017/jfm.2020.376 |