Journal
JOURNAL OF FLUID MECHANICS
Volume 896, Issue -, Pages -Publisher
CAMBRIDGE UNIV PRESS
DOI: 10.1017/jfm.2020.376
Keywords
surface gravity waves; internal waves; nonlinear instability
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Funding
- National Science Foundation, Physical Oceanography Program [OCE-1948705]
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We derive weakly dispersive Boussinesq equations using a coordinate for the vertical direction, employing a series expansion in powers of . We restrict attention initially to the case of constant still-water depth in order to simplify subsequent analysis, and consider equations based on expansions about the bottom elevation , and then about a reference elevation 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 and surface displacement separately.
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