Extreme internal waves: gravity currents and overturning fronts
Robin Ming Chen, Samuel Walsh, Miles H. Wheeler

TL;DR
This paper rigorously analyzes internal gravity waves and hydrodynamic bores, proving overturning behavior in elevation bores and characterizing limits to gravity currents using advanced geometric analysis techniques.
Contribution
It provides the first rigorous proof of overturning in elevation bores and characterizes the limiting behavior of depression bores, including contact angles in gravity currents.
Findings
Elevation bores overturn with vertical interface tangents.
Depression bores either overturn or converge to gravity currents.
First rigorous confirmation of von Kármán's contact angle conjecture.
Abstract
Hydrodynamic bores are front-type traveling wave solutions to the two-layer free boundary Euler equations in two dimensions. The velocity field in each layer is assumed to be incompressible and irrotational, and it limits to distinct laminar flows upstream and downstream. Rigid horizontal boundaries confine the fluids from above and below. A constant gravitational force acts on the waves, but surface tension is neglected. It was recently shown by the authors that there exist two large-amplitude families of hydrodynamic bores: a curve of depression bores and a curve of elevation bores. We now prove that in the limit along the elevation bore family, the solutions must overturn: the interface separating the layers develops a vertical tangent. This type of behavior was first observed over 45 years ago in numerical computations of internal gravity waves and gravity water waves with…
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Taxonomy
TopicsOcean Waves and Remote Sensing · Oceanographic and Atmospheric Processes · Navier-Stokes equation solutions
