Modeling of Turbulent Patches Statistical Distribution in the Stratified Ocean Layers

A. M. Chukharev1, ✉, K. V. Runovsky2, O. E. Kulsha2

1 Marine Hydrophysical Institute, Russian Academy of Sciences, Sevastopol, Russian Federation

2 Branch of the M.V. Lomonosov Moscow State University in Sevastopol, Russian Federation

e-mail: alexchukh@mail.ru

Abstract

Model for the spectrum of density pulsations in a stratified layer of fluid is proposed. It assumes presence of the mechanism vertical turbulent exchange resulting from breaking of the internal waves and formation of the turbulent patches. The mechanism is considered to be quite widespread in many regions of the World Ocean. Modeling implies consideration of two sources of fluctuations: internal waves existing in the whole layer and turbulence concentrated within a certain number of patches distributed within the layer under consideration. The scale ranges of the internal waves and turbulence are partially overlapped; at that the maximum scale of turbulent pulsations is limited by a patch size. Basing on the theory of locally isotropic turbulence and assuming that the oscillations inside a patch are described by harmonic functions, it is shown that their local frequency and local amplitude are connected by the analytical relationship. In the model functions, both the amplitude and the phase of oscillations are randomized, white noise is added to them. The major features of influence of various specified characteristics of the patches and internal waves upon the spectrum shape are determined. The experimental data have being analyzed by means of the proposed model permit to evaluate the scales and amount of the patches, as well as their turbulence energy level. The model also exhibits validity of the earlier developed energy approach for defining the scales of turbulent patches.

Keywords

stratified layer, vertical exchange, internal waves, microstructure, spectral model, turbulent patch

For citation

Chukharev, A.M., Runovsky, K.V. and Kulsha, O.E., 2017. Modeling of Turbulent Patches Statistical Distribution in the Stratified Ocean Layers. Physical Oceanography, (5), pp. 31-41. doi:10.22449/1573-160X-2017-5-31-41

DOI

10.22449/1573-160X-2017-5-31-41

References

  1. Kamenkovich, V.M. and Monin, A.S. eds., 1978. Fizika Okeana, V.2. Gidrodinamika Okeana [Ocean Physics, V. 2. Ocean Hydrodynamics]. Moskow: Nauka, 455 p. (in Russian).
  2. Wunsch, C. and Ferrari, R., 2004. Vertical Mixing, Energy and the General Circulation of the Ocean. Annu. Rev. Fluid Mech., [e-journal] 36(1), pp. 281-314. doi:10.1146/annurev.fluid.36.050802.122121
  3. Hebert, D., Moum, J.N., Paulson, C.A. and Caldwell, D.R., 1992. Turbulence and Internal Waves at the Equator. Part II: Details of a Single Event. J. Phys. Oceanogr., [e-journal] 22(11), pp. 1346-1356. doi:10.1175/1520-0485(1992)022<1346:TAIWAT>2.0.CO;2
  4. Gregg, M.C., 1989. Scaling Turbulent Dissipation in the Thermocline. J. Geophys. Res., [e-journal] 94(C7), pp. 9686-9698. doi:10.1029/JC094iC07p09686
  5. Thorpe, S.A., 1973. Experiments on Instability and Turbulence in a Stratified Shear Flow. J. of Fluid Mechanics, [e-journal] 61(4), pp. 731-751. doi:10.1017/S0022112073000911
  6. Thorpe, S.A., 1987. Transitional Phenomena and the Development of Turbulence in Stratified Fluids: A Review. J. Geophys. Res., [e-journal] 92(C5), pp. 5231-5248. doi:10.1029/JC092iC05p05231.
  7. Osborn, T.R., 1974. Vertical Profiling of Velocity Microstructure. J. Phys. Oceanogr., [e-journal] 4(1), pp. 109-115. doi:10.1175/1520-0485(1974)004<0109:VPOVM>2.0.CO;2
  8. Preusse, M., Peeters, F. and Lorke, A., 2010. Internal Waves and the Generation of Turbulence in the Thermocline of a Large Lake. Limnol. Oceanogr., 55(6), pp. 2353-2365.
  9. Zonta, F., Onorato, M. and Soldati, A., 2012. Turbulence and Internal Waves in Stably-Stra-tified Channel Flow with Temperature-Dependent Fluid Properties. J. Fluid Mech., [e-journal] (697), pp. 175-203. doi:10.1017/jfm.2012.51
  10. Waterman, S., Naveira-Carabato, A.C. and Polzin, K.L., 2013. Internal Waves and Turbulence in the Antarctic Circumpolar Current. J. Phys. Oceanogr., [e-journal] 43(2), pp. 259-282. doi:10.1175/JPO-D-11-0194.1
  11. Samodurov, A.S., Lubitsky, A.A. and Panteleev, N.A., 1995. Contribution of Breaking Internal Waves to Structure Formation, Energy Dissipation, and Vertical Diffusion in the Ocean. Physical Oceanography, [e-journal] 6(3), pp. 177-190. doi:10.1007/BF02197516
  12. Chukharev, А.М., 2014. Vklad Osnovnykh Mekhanizmov Generatsiy Turbulentnosti v Vertikalnyy Obmen v Deyatelnom Sloe Morya [Contribution of the Basic Mechanisms of Turbulence Generation to Vertical Exchange in the Active Sea Layer]. Doctorate Thesis. Sevastopol, 275 p.
  13. Samodurov, A.S., Dykman, V.Z., Barabash, V.A., Efremov, O.I., Zubov, A.G., Pavlenko, O.I., Chukharev, A.M., 2005. “Sigma-1” Measuring Complex for the Investigation of Small-Scale Characteristics of Hydrophysical Fields in the Upper Layer of the Sea. Physical Oceanography, [e-journal] 15(5), pp. 311-322. https://doi:org/10.1007/s11110-006-0005-1
  14. Samodurov, A.S. and Chukharev, A.M., 2008. Experimental Estimation of the Coefficient of Vertical Turbulent Exchange in a Stratified Layer of the Black Sea near the Continental Slope. Physical Oceanography, [e-journal] 18(6), pp. 308-318. doi:10.1007/s11110-009-9032-z
  15. Monin, A.S. and Yaglom, A.M., 2007. Statistical Fluid Mechanics, Volume II: Mechanics of Turbulence. Mineola, NY: Dover Publications, 896 p.
  16. Jaffard, S., Meyer, Y. and Ryan, R.D., 2001. Wavelets. Tools for Science & Technology. Philadelphia: SIAM, 255 p.
  17. Innocent, J.-M. and Torrésani, B., 1996. A Multiresolution Strategy for Detecting Gravitational Waves Generated by Binary Coalescence. Internal Report CPT-96/P.3379, CPT-CNRS. Marseille, 13 p.
  18. Runovski, K. and Schmeisser, H.-J., 2015. Moduli of Smoothness Related to the Laplace-Operator. J. Fourier Analys. Applicat., [e-journal] 21(3), pp. 449-471. doi:10.1007/s00041-014-9373-y

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