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Frequency diffusion of waves by unsteady flows

Published online by Cambridge University Press:  04 November 2020

Wenjing Dong*
Affiliation:
Courant Institute of Mathematical Sciences, New York University, NY10012, USA
Oliver Bühler
Affiliation:
Courant Institute of Mathematical Sciences, New York University, NY10012, USA
K. Shafer Smith
Affiliation:
Courant Institute of Mathematical Sciences, New York University, NY10012, USA
*
Email address for correspondence: [email protected]

Abstract

The production of broadband frequency spectra from narrowband wave forcing in geophysical flows remains an open problem. Here we consider a related theoretical problem that points to the role of time-dependent vortical flow in producing this effect. Specifically, we apply multi-scale analysis to the transport equation of wave action density in a homogeneous stationary random background flow under the Wentzel–Kramers–Brillouin approximation. We find that, when some time dependence in the mean flow is retained, wave action density diffuses both along and across surfaces of constant frequency in wavenumber–frequency space; this stands in contrast to previous results showing that diffusion occurs only along constant-frequency surfaces when the mean flow is steady. A self-similar random background velocity field is used to show that the magnitude of this frequency diffusion depends non-monotonically on the time scale of variation of the velocity field. Numerical solutions of the ray-tracing equations for rotating shallow water illustrate and confirm our theoretical predictions. Notably, the mean intrinsic wave frequency increases in time, which by wave action conservation implies a concomitant increase of wave energy at the expense of the energy of the background flow.

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

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References

REFERENCES

Barkan, R., Winters, K. B. & McWilliams, J. C. 2017 Stimulated imbalance and the enhancement of eddy kinetic energy dissipation by internal waves. J. Phys. Oceanogr. 47 (1), 181198.CrossRefGoogle Scholar
Bôas, A. B. V. & Young, W. R. 2020 Directional diffusion of surface gravity wave action by ocean macroturbulence. J. Fluid Mech. 890, R4.Google Scholar
Bretherton, F. P. & Garrett, C. J. R. 1968 Wavetrains in inhomogeneous moving media. Proc. R. Soc. Lond. A 302 (1471), 529554.Google Scholar
Gardiner, C. W. 1985 Handbook of Stochastic Methods, vol. 3. Springer.Google Scholar
Kafiabad, H. A., Savva, M. A. C. & Vanneste, J. 2019 Diffusion of inertia–gravity waves by geostrophic turbulence. J. Fluid Mech. 869, R7.CrossRefGoogle Scholar
Kunze, E. 1985 Near-inertial wave propagation in geostrophic shear. J. Phys. Oceanogr. 15 (5), 544565.2.0.CO;2>CrossRefGoogle Scholar
Lelong, M.-P. & Riley, J. J. 1991 Internal wave–vortical mode interactions in strongly stratified flows. J. Fluid Mech. 232, 119.CrossRefGoogle Scholar
MacKinnon, J. A., Zhao, Z., Whalen, C. B., Waterhouse, A. F., Trossman, D. S., Sun, O. M., St. Laurent, L. C., Simmons, H. L., Polzin, K., Pinkel, R. et al. 2017 Climate process team on internal wave–driven ocean mixing. Bull. Am. Meteorol. Soc. 98 (11), 24292454.CrossRefGoogle Scholar
McComas, C. Henry & Bretherton, F. P. 1977 Resonant interaction of oceanic internal waves. J. Geophys. Res. 82 (9), 13971412.CrossRefGoogle Scholar
Polzin, K. L. & Lvov, Y. V. 2017 An oceanic ultra-violet catastrophe, wave-particle duality and a strongly nonlinear concept for geophysical turbulence. Fluids 2 (3), 36.CrossRefGoogle Scholar
Savva, M. A. C. & Vanneste, J. 2018 Scattering of internal tides by barotropic quasigeostrophic flows. J. Fluid Mech. 856, 504530.CrossRefGoogle Scholar
Sun, H. & Kunze, E. 1999 Internal wave–wave interactions. Part 2. Spectral energy transfer and turbulence production. J. Phys. Oceanogr. 29 (11), 29052919.2.0.CO;2>CrossRefGoogle Scholar
Thomas, J. & Arun, S. 2020 Near-inertial waves and geostrophic turbulence. Phys. Rev. Fluids 5 (1), 014801.CrossRefGoogle Scholar
Wagner, G. L., Ferrando, G. & Young, W. R. 2017 An asymptotic model for the propagation of oceanic internal tides through quasi-geostrophic flow. J. Fluid Mech. 828, 779811.CrossRefGoogle Scholar
Ward, M. L. & Dewar, W. K. 2010 Scattering of gravity waves by potential vorticity in a shallow-water fluid. J. Fluid Mech. 663, 478506.CrossRefGoogle Scholar
Young, W. R. & Jelloul, M. B. 1997 Propagation of near-inertial oscillations through a geostrophic flow. J. Mar. Res. 55 (4), 735766.CrossRefGoogle Scholar