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Excitation of interfacial waves via surface–interfacial wave interactions

Published online by Cambridge University Press:  23 January 2020

Joseph Zaleski
Affiliation:
Department of Mathematics, Rensselaer Polytechnic Institute, Troy, NY12180, USA
Philip Zaleski
Affiliation:
Department of Mathematics, New Jersey Institute of Technology, Newark, NJ07102, USA
Yuri V. Lvov*
Affiliation:
Department of Mathematics, Rensselaer Polytechnic Institute, Troy, NY12180, USA
*
†Email address for correspondence: lvovy@rpi.edu

Abstract

We consider interactions between surface and interfacial waves in a two-layer system. Our approach is based on the Hamiltonian structure of the equations of motion, and includes the general procedure for diagonalization of the quadratic part of the Hamiltonian. Such diagonalization allows us to derive the interaction cross-section between surface and interfacial waves and to derive the coupled kinetic equations describing spectral energy transfers in this system. Our kinetic equation allows resonant and near-resonant interactions. We find that the energy transfers are dominated by the class III resonances of Alam (J. Fluid Mech., vol. 691, 2012, pp. 267–278). We apply our formalism to calculate the rate of growth for interfacial waves for different values of wind velocity. Using our kinetic equation, we also consider the energy transfer from wind-generated surface waves to interfacial waves for the case when the spectrum of the surface waves is given by the JONSWAP spectrum and interfacial waves are initially absent. We find that such energy transfer can occur along a time scale of hours; there is a range of wind speeds for the most effective energy transfer at approximately the wind speed corresponding to white capping of the sea. Furthermore, interfacial waves oblique to the direction of the wind are also generated.

Information

Type
JFM Papers
Copyright
© The Author(s), 2020. Published by Cambridge University Press
Figure 0

Figure 1. Schematic of the surface and interface with respect to mean displacements.

Figure 1

Figure 2. The resonant set of interfacial wavenumbers for fixed surface wavenumber $\unicode[STIX]{x1D705}=(2\unicode[STIX]{x03C0}/10)~\text{m}^{-1}$. (a) Class III and surrounding resonances; (b) class I and surrounding resonances.

Figure 2

Figure 3. Schematic construction of three-wave resonances as determined by a fixed surface wave $\unicode[STIX]{x1D73F}$ and the corresponding set of resonant interfacial waves, as done in Ball (1964). Two of such triads are depicted.

Figure 3

Figure 4. Resonances are not scale-invariant: the solid curve depicts interfacial wavenumbers in resonance when one surface wavenumber is fixed to be (a) $\unicode[STIX]{x1D705}=(2\unicode[STIX]{x03C0}/25)~\text{m}^{-1}$, (b) $\unicode[STIX]{x1D705}=(3\times 2\unicode[STIX]{x03C0}/25)~\text{m}^{-1}$ and (c) $\unicode[STIX]{x1D705}=(5\times 2\unicode[STIX]{x03C0}/25)~\text{m}^{-1}$. The dashed curves correspond to scaling curve (a) by factors of 3 and 5.

Figure 4

Figure 5. (a) Comparison of numerical solution of (5.4) and the analytical value of the peak growth rate using (5.5) for a surface spectrum with wind speed of $10~\text{m}~\text{s}^{-1}$. (b) Peak growth rate of interfacial waves versus the wind speed for various values of wind speed according to both formulas.

Figure 5

Figure 6. Resonance curves as plotted in figure 4 including physical width for (a) $\unicode[STIX]{x1D706}=20~\text{m}$ surface spectrum and (b) $\unicode[STIX]{x1D706}=80~\text{m}$ surface spectrum.

Figure 6

Figure 7. The ratio between the resonance width $\unicode[STIX]{x1D6E4}_{\unicode[STIX]{x1D73F},\unicode[STIX]{x1D73F}-\boldsymbol{k}_{I},\boldsymbol{k}_{I}}^{(2)}$ and the frequency of the excited interfacial wave $\unicode[STIX]{x1D714}_{\boldsymbol{k}^{I}}^{(I)}$ for two different wind speeds, as a function of wavenumber and angle along the resonance curve.

Figure 7

Figure 8. The excitation rate, $\unicode[STIX]{x1D6FE}_{\boldsymbol{k}}^{(I)}$, plotted as a function of $\unicode[STIX]{x1D703}$, the angle between interfacial wave $\boldsymbol{k}$ and surface wave $\unicode[STIX]{x1D73F}$.

Figure 8

Figure 9. The matrix element $\unicode[STIX]{x1D611}^{(SSI)}(\unicode[STIX]{x1D73F},\unicode[STIX]{x1D73F}+\boldsymbol{k}_{I},\boldsymbol{k}_{I})$ with the resonant values of $k_{I}$ overlaid on top. Surface wavelength is (a) $\unicode[STIX]{x1D706}=8~\text{m}$, (b) $\unicode[STIX]{x1D706}=14.5~\text{m}$ and (c) $\unicode[STIX]{x1D706}=150~\text{m}$. We see a transition into a regime in which collinear resonances are no longer dominant, i.e. as the surface waves grow in wavelength the resonant curve crosses a peak spatial frequency in which energy transfer is most efficient.

Figure 9

Figure 10. (a) The fixed surface wave JONSWAP spectrum. (b) The interfacial wave spectrum over the course of 20 weeks, where $n_{\boldsymbol{k}}^{(I)}(t=0)=0$ initially.

Figure 10

Figure 11. (a) Fixed surface spectrum and (b) simulated growth rate of interfacial wave spectrum for a wind speed of $5~\text{m}~\text{s}^{-1}$.

Figure 11

Figure 12. (a) Fixed surface spectrum and (b) simulated growth rate of interfacial wave spectrum for a hurricane wind speed of $50~\text{m}~\text{s}^{-1}$.