Turbulence Induced by Storm Waves on Deep Water
S.Yu. Kuznetsov1, Ya.V. Saprykina1, V.A. Dulov2, ✉, A.M. Chukharev2
1 Shirshov Oceanological Institute, Russian Academy of Sciences, Moscow, Russian Federation
2 Marine Hydrophysical Institute, Russian Academy of Sciences, Sevastopol, Russian Federation
✉ e-mail: dulov1952@gmail.com
Abstract
Results of laboratory and field experiments performed in November–December, 2014 to study turbulence induced by wave motion are represented. Elevations of free sea surface and fluctuations of three components of water particle velocity are synchronously measured at calm conditions when wave breaking is absent. The data is obtained in the ranges of wave and turbulence frequencies, and in the depth range from the surface to half a length of surface waves. A method for separating the measured velocity fluctuations into at a wave and two turbulence components (the one is induced by wave motions and another is a background hydrodynamic turbulence) is developed. In field experiments the bound frequency of ~0.8 Hz had been determined. The coherence of the turbulent fluctuations and sea surface elevations sharply decreases above this frequency. Direct instrumental measurements confirmed stratification of a wave flow into a near-surface turbulent layer induced by wave motion and an underlying layer with the background hydrodynamic turbulence. The characteristics of turbulence in a near-surface layer are connected linearly with magnitude of envelope of vertical component velocity. This fact enables to attribute the turbulent fluctuations in this layer to wave-induced turbulence. Based on analysis of experiments the conclusion about existence of wave-induced turbulence in absentia other sources of turbulence such as wave breaking, wind stresses and Langmuir circulations is drawn.
Keywords
wave induced turbulence, background turbulence, field experiment, storm waves
For citation
Kuznetsov, S.Yu., Saprykina, Ya.V., Dulov, V.A. and Chukharev, A.M., 2015. Turbulence Induced by Storm Waves on Deep Water. Physical Oceanography, (5), pp. 22-31. doi:10.22449/1573-160X-2015-5-22-31
DOI
10.22449/1573-160X-2015-5-22-31
References
- Monin, A.S., Ozmidov R.V., 1978, “Turbulentnost' v okeane [Turbulence in the ocean]”, Okeanologiya. Fizika okeana, vol. 1 Gidrofizika okeana, Moscow, Nauka, pp. 148-207 (in Russian).
- Dmitriev, A.A., Bonchkovskaya, T.V., 1953, “K voprosu o turbulentnosti v volne [On the issue on the turbulence in a wave]”, Dokl. AN SSSR, vol. 91, no. 1, pp. 31-33 (in Russian).
- Dobroklonskii, S.V., Kontoboitseva, N.V., 1973, “Eksperimenty po opredeleniyu tolshchiny turbulentnogo sloya v volnakh monokhromaticheskogo tipa [Experiments on turbulent layer detection in monochromatic type waves]”, Izv. AN SSSR. Fizika atmosfery i okeana, vol. 9, no. 2, pp. 210-212 (in Russian).
- Donelan, M.A., 1987, “The effect of swell on the growth of wind waves’, Johns Hopkins APL Technical Digest., vol. 1, pp. 18-23.
- Kitaigorodskii, S.A., Lumley, J.L., 1983, “Wave turbulence interactions in the upper ocean. Part I: The energy balance of the interacting fields of surface wind waves and wind-induced three-dimensional turbulence”, J. Phys. Oceanogr., vol. 13, no. 11, pp. 1977-1987.
- Craig, P.D., Banner, M.L., 1994, “Modelling of wave-enhanced turbulence in the ocean surface layer”, Ibid., vol. 24, no. 12, pp. 2546-2559.
- Drennan, W.M, Donelan, M.A. & Terray, E.A. [et al.], 1996, “Oceanic turbulence dissipation measurements in SWADE”, Ibid., vol. 26, no. 5, pp. 800-815.
- Kudryavtsev, V., Shrira, V., Dulov, V. [et al.], 2008, “On vertical structure of wind-driven sea surface currents”, Ibid., vol. 38, no. 10, pp. 1-2144.
- Babanin, A.V., 2006, “On a wave-induced turbulence and a wave-mixed upper ocean layer”, Geophys. Res. Lett., vol.33, L20605, 6 p., doi:10.1029/2006GL027308.
- Dai, D., Qiao, F. & Sulisz, W. [et al.], 2010, “An experiment on the nonbreaking surface-wave-induced vertical mixing”, J. Phys. Oceanogr., vol. 40, no. 9, pp. 2180-2188.
- Chukharev, A.M., 2013, “Model' turbulentnosti so mnogimi vremennymi masshtabami dlya pripoverkhnostnogo sloya morya [Multitime scale model of turbulence in the sea surface layer]”, 2013, Izv. RAN. Fizika atmosfery i okeana, vol. 49, no. 4, pp. 439-449 (in Russian).
- Efimov, V.V., 1981, “Dinamika volnovykh protsessov v pogranichnykh sloyakh atmosfery i okeana [Dynamics of the wave processes in the boundary sea and ocean layers]”, Kiev, Naukova Dumka, 256 p. (in Russian).
- Qiao, F., Yuan, Y. & Ezer, T. [et al.], 2010, “A three-dimensional surface wave-ocean circulation coupled model and its initial testing”, Ocean Dyn., iss. 5, pp. 1339-1355.
- Samodurov. A.S., Dykman, V.Z. & Barabash, V.A. [et al.], 2005, “Izmeritel'nyy kompleks “Sigma-1” dlya issledovaniya melkomasshtabnykh kharakteristik gidrofizicheskikh poley v verkhnem sloe morya [“Sigma-1” measuring equipment for research of small-scale features of hydrophysical fields in the sea upper layer]”, Morskoy Gidrofizicheskiy Zhurnal, no. 5, pp. 60-71 (in Russian).
- Malinovskii,V.V., Dulov, V.A. & Korinenko, A.E. [et al.], 2014, “Kompleks apparatury dlya podsputnikovykh izmereniy so statsionarnoy okeanograficheskoy platformy v Katsiveli [Set of the equipment for sub-satellite measurements from the stationary oceanographic platform in Katsiveli]”, Monitoring pribrezhnoy zony na Chernomorskom eksperimental'nom podsputnikovom poligone, Sevastopol, MGI NAN Ukrainy, pp. 128-149 (in Russian).
- Lavrentyev, M.A., Shabat, B.V., 1973, “Problemy gidrodinamiki i ikh matematicheskie modeli [Problems of hydrodynamics and their mathematical models]”, Moscow, Nauka, 416 p. (in Russian).
- Stewart, R.W., Grant, H.L., 1962, “Determination of the rate of dissipation of turbulent energy near the sea surface in the presence of waves”, J. Geophys. Res., vol. 67, pp. 3177-3180.
- Kuznetsov, S.Yu., Dachev, V.Zh. & Speranskii, N.S., 1992, “Nelineynye volny i turbulentnost' v beregovoy zone morya [Non-linear waves and turbulence in the coastal area]”, Okeanologia BAN, vol. 21, pp. 3-13 (in Russian).