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The response of a continuously stratified fluid to an oscillating flow past an obstacle

Published online by Cambridge University Press:  14 June 2013

Kraig B. Winters*
Affiliation:
Scripps Institution of Oceanography and Mechanical and Aerospace Engineering, University of California San Diego, La Jolla, CA 92093, USA
Laurence Armi
Affiliation:
Scripps Institution of Oceanography and Mechanical and Aerospace Engineering, University of California San Diego, La Jolla, CA 92093, USA
*
Email address for correspondence: kraig@coast.ucsd.edu

Abstract

An oscillating continuously stratified flow past an isolated obstacle is investigated using scaling arguments and two-dimensional non-hydrostatic numerical experiments. A new dynamic scaling is introduced that incorporates the blocking of fluid with insufficient energy to overcome the background stratification and crest the obstacle. This clarifies the distinction between linear and nonlinear flow regimes near the crest of the obstacle. The flow is decomposed into propagating and non-propagating components. In the linear limit, the non-propagating component is related to the unstratified potential flow past the obstacle and the radiating component exhibits narrow wave beams that are tangent to the obstacle at critical points. When the flow is nonlinear, the near crest flow oscillates between states that include asymmetric, crest-controlled flows. Thin, fast, supercritical layers plunge in the lee, separate from the obstacle and undergo shear instability in the fluid interior. These flow features are localized to the neighbourhood of the crest where the flow transitions from subcriticality to supercriticality and are non-propagating. The nonlinear excitation of energetic non-propagating components reduces the efficiency of topographic radiation in comparison with linear dynamics.

Type
Papers
Copyright
©2013 Cambridge University Press 

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References

Alford, M. H., MacKinnon, J. A., Nash, J. D., Simmons, H. L., Pickering, A., Klymak, J. M., Pinkel, R., Sun, O., Rainville, L., Musgrave, R., Beitzel, T., Fu, K. & Lu, C. 2011 Energy flux and dissipation in Luzon Strait: two tales of two ridges. J. Phys. Oceanogr. 41, 22112222.Google Scholar
Armi, L. & Williams, R. 1993 The hydraulics of a stratified fluid flowing through a contraction. J. Fluid Mech. 251, 355375.Google Scholar
Baidulov, V. G. & Chashechkin, Yu. D. 1996 A boundary current induced by diffusion near a motionless horizontal cylinder in a continuously stratified fluid. Izv. Atmos. Ocean. Phys. 32, 751756.Google Scholar
Baines, P. G. 1973 The generation of internal tides by flat-bump topography. Deep-Sea Res. 20, 179205.Google Scholar
Baines, P. G. 1995 Topographic Effects in Stratified Flows. Cambridge University Press.Google Scholar
Browand, F. K. & Winant, C. D. 1972 Blocking ahead of a cylinder moving in a stratified fluid: an experiment. Geophys. Fluid Dyn. 4, 2953.Google Scholar
Buijsman, M., Legg, S. & Klymak, J. 2012 Double ridge internal tide interference and its effect on dissipation in Luzon Strait. J. Phys. Oceanogr. 42, 13371356.Google Scholar
Chashechkin, Y. D. 1999 Schlieren visualization of a stratified flow around a cylinder. J. Vis. 1, 345354.Google Scholar
Cummins, P. F., Vagle, S., Armi, L. & Farmer, D. M. 2003 Stratified flow over topography: upstream influence and generation of nonlinear internal waves. Proc. R. Soc. Lond. 459A, 14671487.Google Scholar
Echeverri, P., Flynn, M. R., Winters, K. B. & Peacock, T. 2009 Low-mode internal tide generation: an experimental and numerical investigation. J. Fluid Mech. 638, 91108.CrossRefGoogle Scholar
Farmer, D. M. & Armi, L. 1999 Stratified flow over topography: the role of small scale entrainment and mixing in flow establishment. Proc. R. Soc. Lond. 455A, 32213258.Google Scholar
Gill, A. E. 1982 Atmosphere–Ocean Dynamics. Academic.Google Scholar
Garrett, C. & Gerkema, T. 2007 On the body-force term in internal-tide generation. J. Phys. Oceanogr. 37, 21722175.CrossRefGoogle Scholar
Garrett, C. & Kunze, E. 2007 Internal tide generation in the deep ocean. Annu. Rev. Fluid Mech. 39, 5787.Google Scholar
Gayan, B. & Sarkar, S. 2011 Boundary mixing by density overturns in an internal tidal beam. Geophys. Res. Lett. 38, L14608.Google Scholar
Gerkema, T. 1996 A unified model for the generation and fission of internal tides in a rotating ocean. J. Mar. Res. 54, 421450.CrossRefGoogle Scholar
Gerkema, T. & Zimmerman, J. T. F. 1995 Generation of nonlinear internal tides and solitary waves. J. Phys. Oceanogr. 25, 10811094.Google Scholar
Görtler, Von H. 1943 Über eine Schwingungserscheinung in Flüssigkeiten mit stabiler Dichteschichtung. Z. Angew. Math. Mech. 23, 6571.Google Scholar
Kao, T. W. 1965 The phenomena of blocking in stratified flows. J. Geophys. Res. 70, 815822.CrossRefGoogle Scholar
Klymak, J. M., Legg, S. & Pinkel, R. 2010 A simple parameterization of turbulent tidal mixing near supercritical topography. J. Phys. Oceanogr. 40, 20592074.Google Scholar
Kundu, P. K. 1990 Fluid Mechanics. Academic.Google Scholar
Lamb, K. G. 2004 Nonlinear interaction among internal wave beams generated by tidal flow over supercritical topography. Geophys. Res. Lett. 31, L09313.Google Scholar
Legg, S. & Klymak, J. M. 2008 Internal hydraulic jumps and overturning generated by tidal flow over a tall steep ridge. J. Phys. Oceanogr. 38, 19491964.Google Scholar
Lighthill, J. 1978 Waves in Fluids. Cambridge University Press.Google Scholar
Long, R. R. 1955 Some aspects of the flow of stratified fluids III. Continuous density gradients. Tellus 7, 341357.Google Scholar
Mowbray, D. E. & Rarity, B. S. H. 1967 A theoretical and experimental investigation of the phase configuration of internal waves of small amplitude in a density stratified liquid. J. Fluid Mech. 28, 116.Google Scholar
Peacock, T., Stocker, R. & Aristoff, J. M. 2004 An experimental investigation of the angular dependence of diffusion-driven flow. Phys. Fluids 16, 35033505.Google Scholar
Petrelis, F., Llewellyn Smith, S. & Young, W. R. 2006 Tidal conversion at a submarine ridge. J. Phys. Oceanogr. 36, 10531071.Google Scholar
Phillips, O. M. 1970 On flows induced by diffusion in a stably stratified fluid. Deep-Sea Res. 17, 435443.Google Scholar
Rapaka, N. R., Gayen, B. & Sarkar, S. 2013 Tidal conversion and turbulence at a model ridge: direct and large eddy simulations. J. Fluid Mech. 715, 181209.Google Scholar
Smith, R. B. 1985 On severe downslope winds. J. Atmos. Sci. 42, 25972603.Google Scholar
Sutherland, B. R. & Linden, P. F. 2002 Internal wave excitation by a vertically oscillating elliptical cylinder. Phys. Fluids 14, 721730.Google Scholar
Thorpe, S. A. 2005 The Turbulent Ocean. Cambridge University Press.Google Scholar
Thorpe, S. A. 2007 An Introduction to Ocean Turbulence. Cambridge University Press.Google Scholar
Tritton, D. J. 1988 Physical Fluid Dynamics, 2nd edn. Clarendon.Google Scholar
Turner, J. S. 1973 Buoyancy Effects in Fluids. Cambridge University Press.Google Scholar
Winters, K. B & Armi, L. 2012 Hydraulic control of continuously stratified flow over an obstacle. J. Fluid Mech. 700, 502513.Google Scholar
Winters, K. B., Bouruet-Aubertot, P. & Gerkema, T. 2011 Critical reflection and abyssal trapping of near-inertial waves on a $\beta $-plane. J. Fluid Mech. 684, 111136.Google Scholar
Winters, K. B. & de la Fuente, A. 2012 Modelling rotating stratified flows at laboratory-scale using spectrally-based DNS. Ocean Model. 49–50, 4759.Google Scholar
Wood, I. R. 1968 Selective withdrawal from a stably stratified fluid. J. Fluid Mech. 32, 209223.Google Scholar