Hostname: page-component-77c89778f8-fv566 Total loading time: 0 Render date: 2024-07-17T13:25:53.378Z Has data issue: false hasContentIssue false

A canonical statistical theory of oceanic internal waves

Published online by Cambridge University Press:  26 April 2006

Kenneth R. Allen
Affiliation:
The Johns Hopkins University, Applied Physics Laboratory, Laurel, MD 20707–6099, USA
Richard I. Joseph
Affiliation:
Department of Electrical and Computer Engineering, The Johns Hopkins University, Baltimore, MD 21218, USA

Abstract

We use the methods of statistical mechanics to develop a theoretical relationship between the observed oceanic spectra and the probability distributions usually studied in statistical mechanics. We also find that the assumption that in terms of Lagrangian variables the oceanic internal wave field is near canonical equilibrium (i.e. the internal wave modes are populated in accordance with a Maxwell–Boltzmann-type distribution) yields expressions for the various marginal or reduced Eulerian spectra associated with both moored and towed measurements which are in striking qualitative agreement with experiment. In developing this theory it is important to distinguish carefully between Lagrangian and Eulerian variables. The important difference between the two sets of variables is due to the advective nonlinearity (i.e. (v) v where v is the Eulerian velocity) which is present only in the Eulerian frame. Our method treats the dynamics within the Lagrangian frame, where because of the absence of the advective nonlinearity it is fundamentally simpler, and then transforms to the Eulerian or measurement frame. We find that at small wavenumbers the four-dimensional Eulerian frequency wavenumber spectrum is approximately equal to the corresponding Lagrangian frequency wavenumber spectrum. At large wavenumbers, however, advective contributions become important and the two types of spectra are significantly different. While from a Lagrangian frame point of view the system is entirely wavelike, at large wavenumbers the Eulerian spectrum is not confined to the dispersion surface and the system, from an Eulerian frame point of view, is not wavelike. Further, the three-dimensional Eulerian wavenumber spectrum exhibits a large-wavenumber advective tail which decays as a power law and results in one-dimensional marginal spectra which are in excellent qualitative agreement with experiment. The above features are exhibited independent of the detailed nature of the underlying Lagrangian frequency wavenumber spectrum.

Type
Research Article
Copyright
© 1989 Cambridge University Press

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Abarbanel, H. D. I. & Rouhi, A. 1987 Phase space density representation of inviscid fluid dynamics. Phys. Fluids 30, 29522964.Google Scholar
Allen, K. R. & Joseph, R. I., 1988 The relation between Lagrangian and Eulerian spectra: a connection between large-scale waves and small-scale turbulence. In Small-Scale Turbulence and Mixing in the Ocean (ed. J. C. J. Nihoul & B. M. Jamart), pp. 303318. Elsevier.
Cairns, J. L. & Williams, G. O., 1976 Internal wave observations from a midwater float, 2. J. Geophys. Res. 81, 19431950.Google Scholar
Flatté, S. M., Henyey, F. S. & Wright, J. A., 1985 Eikonal calculations of short wavelength internal-wave spectra. J. Geophys. Res. 90 (c4), 72657272.Google Scholar
Fox, R. F.: 1978 Gaussian stochastic processes in physics. Phys. Rep. 48, 179283.Google Scholar
Garrett, C. J. R. & Munk, W. H. 1972 Space–time scales of internal waves. Geophys. Fluid Dyn. 3, 225264.Google Scholar
Garrett, C. J. R. & Munk, W. H. 1975 Space–time scales of internal waves: a progress report. J. Geophys. Res. 80, 291297.Google Scholar
Green, M. S.: 1954 Markoff random processes and the statistical mechanics of time-dependent processes. II. Irreversible processes in fluids. J. Chem. Phys. 22, 398413.Google Scholar
Gregg, M. C.: 1977 A comparison of finestructure spectra from the main thermocline. J. Phys. Oceanogr. 7, 3340.Google Scholar
Hardy, R. J.: 1963 Energy-flux operator for a lattice. Phys. Rev. 132, 168177.Google Scholar
Hasselmann, K.: 1966 Feynman diagrams and interaction rules of wave–wave scattering processes. Rev. Geophys. Space Phys. 4, 132.Google Scholar
Henyey, F. S.: 1983 Hamiltonian description of stratified fluid dynamics. Phys. Fluids 26, 4047.Google Scholar
Henyey, F. S. & Pomphrey, N., 1983 Eikonal description of internal wave interactions: A nondiffusive picture of induced diffusion. Dyn. Atmos. Oceans 7, 189219.Google Scholar
Holloway, G.: 1980 Oceanic internal waves are not weak waves. J. Phys. Oceanogr. 10, 906914.Google Scholar
Holloway, G.: 1981 Theoretical approaches to interactions among internal waves, turbulence and finestructure. In AIP Conference Proceedings no. 76 (ed. B. J. West), pp. 4777.
Holloway, G.: 1982 On interaction time scales of oceanic internal waves. J. Phys. Oceanogr. 12, 293296.Google Scholar
Holloway, G.: 1986 Eddies, waves, circulation and mixing: statistical geofluid mechanics. Ann. Rev. Fluid Mech. 18, 91147.Google Scholar
van Kampen, N. G.: 1976 Stochastic differential equations. Phys. Rep. 24c, 171228.Google Scholar
Katz, E. J.: 1975 Tow spectra from MODE. J. Geophys. Res. 80, 11631167.Google Scholar
Longuet-Higgins, M. S.: 1986 Eulerian and Lagrangian aspects of surface waves. J. Fluid Mech. 173, 683707.Google Scholar
McComas, C. H. & Müller, P. 1981 The dynamic balance of internal waves. J. Phys. Oceanogr. 11, 970986.Google Scholar
Mori, H.: 1965 Transport, collective motion and Brownian motion. Prog. Theor. Phys. 33, 423455.Google Scholar
Mori, H., Oppenheim, I. & Ross, J., 1962 Some topics in quantum statistics. The Wigner function and transport theory. In Studies in Statistical Mechanics (ed. J. DeBoer & G. E. Uhlenbeck), vol. I, § c6, pp. 271298. Interscience.
Phillips, O. M.: 1969 The Dynamics of the Upper Ocean. Cambridge University Press.
Pinkel, R.: 1981 Observations of the near-surface internal wavefield. J. Phys. Oceanogr. 11, 12481257.Google Scholar
Pinkel, R.: 1984 Doppler sonar observations of internal waves: the wavenumber-frequency spectrum. J. Phys. Oceanogr. 14, 12491270.Google Scholar
Pomphrey, N.: 1981 Review of some calculations of energy transport in a Garrett–Munk ocean. In AIP Conference Proceedings no. 76 (ed. B. J. West), pp. 113128.
Pomphrey, N., Meiss, J. D. & Watson, K. M., 1980 Description of nonlinear internal wave interactions using Langevin methods. J. Geophys. Res. 85 (c2), 10851094.Google Scholar
Prigogine, I.: 1962 Non-Equilibrium Statistical Mechanics. Interscience.
Prigogine, I. & Henin, F., 1957 On the general perturbational treatment of irreversible processes. Physica 23, 585596.Google Scholar
Prigogine, I. & Henin, F., 1960 On the general theory of the approach to equilibrium. I. Interacting normal modes. J. Math. Phys. 1, 349371.Google Scholar
Seliger, R. L. & Whitham, G. B., 1968 Variational principles in continuum mechanics. Proc. R. Soc. Lond. A 305, 125.Google Scholar
Taylor, G. I.: 1921 Diffusion by continuous movements. Proc. Lond. Math. Soc. 20, 196212.Google Scholar
Tolstoy, I.: 1963 The theory of waves in stratified fluids including the effects of gravity and rotation. Rev. Mod. Phys. 35, 207230.Google Scholar
West, B. J.: 1982 Resonant-test-field model of fluctuating nonlinear waves. Phys. Rev. A 25, 16831691.Google Scholar